| 0 | NA 81861 | VIRG-005 | Quercus virginiana Mill. | Virginia, United States | NA | | | 2012 | COLLECTED | 10/21/2012 | Joseph Bryan Park. Along Joseph Bryan Lane (entrance drive) on the left before the lower intersection with Gabriel Posser Circle and before the bridge over Princeton Creek. | 37.59526000, -77.46816000 | 51 | Cultivated in city park | Wild material | Collected during an expedition seeking material of Quercus virginiana near the species' northern natural limit | 2115755 | NA 81861 |
| 1 | NA 81860 | NA 81860 | Quercus virginiana Mill. | | NA | | | 2012 | | | | | | | Cultivated material | | 1940388 | NA 81860 |
| 2 | NA 61037 | NA 61037 | Quercus virginiana Mill. | United States | NA | | | 1985 | COLLECTED | 11/14/1985 | Cape Henry, Virginia | 36.92973700, -76.01997400 | | | Wild material | | 1111915 | NA 61037 |
| 3 | MIA 25237 | | Quercus virginiana Mill. | Florida, United States | MIA | | | 1978 | COLLECTED | | | | | | Wild material | | 1091148 | MIA 25237 |
| 4 | Ames 36184 | Ames 36184 | Quercus durandii Buckley var. breviloba (Torr.) E. J. Palmer | Oklahoma, United States | NC7 |  | | 2023 | COLLECTED | 2022 | Private property located 11.0 miles west of Clinton just northeast of intersection of Highway 73 and N2140 Road, T12N R19W NE 1/4 SW 1/4 SW 1/4 Sec. 13 | 35.51213100, -99.16652700 | 518 | Rocky knolls consisting of red Permian sandstone scree and red shale outcroppings with a high pH (estimated 8.0-8.5 pH). | Wild material | Accession represents genetics of a disjunct population that is approximately 150 miles northwest of the nearest population of this taxon. Estimated to reach a mature height at 18-20’ and spread at 12-15’. Leaves are rather persistent (strong marcescence) throughout winter. Specimens are shrubby, multi-stemmed and low-branching. Often referred to as Bigelow oak and typically found throughout most of central Texas and parts of southern Oklahoma. According to Lance (2022), “Bigelow oak is mostly allopatric from typical Durand Oak in its range. East of this range, errors in herbarium annotations of juvenile Durand Oak material, where leaf shapes may mimic Bigelow oak, have caused confusion and inaccurate range extensions.” | 2159016 | Ames 36184 |
| 5 | NA 85961 | PCC15-SEUSA025 | Quercus boyntonii Beadle | Alabama, United States | NA | | | 2017 | COLLECTED | 10/28/2015 | Shelby County; Birmingham; Off parking lot of EBSCO Industries, Inc., located at 5724 US-280, Birmingham, Alabama. | 33.37888000, -86.67333000 | | Ridge of Appalachian forest. | Wild material | | 2109093 | NA 85961 |
| 6 | NA 85963 | PCC15-SEUSA045 | Quercus arkansana Sarg. | Alabama, United States | NA | | | 2017 | COLLECTED | 10/30/2015 | Sumter County; ; Roadside, unincorporated area of Sumter County. | 32.56277000, -88.02721000 | | Prairie woods, roadside. | | Seed from plant. Ground, vouchered. [Seed from plant and ground?] Ca five plants in area. No threats observed. | 2109095 | NA 85963 |
| 7 | NA 84715 | TDAAR17-015 | Quercus acerifolia (E. J. Palmer) Stoynoff & W. J. Hess ex R. J. Jensen | Arkansas, United States | NA | | | 2017 | COLLECTED | 09/12/2017 | Ouachita National Forest: Porter Mountain area. | 34.38602000, -94.06165000 | 609 | | Wild material | | 1954038 | NA 84715 |
| 8 | NA 84716 | TDAAR17-017 | Quercus acerifolia (E. J. Palmer) Stoynoff & W. J. Hess ex R. J. Jensen | Arkansas, United States | NA |  | | 2017 | COLLECTED | 09/13/2017 | Montgomery County: Ouachita National Forest: Pryor Mountain. | 34.36113000, -93.87164000 | 532 | | Wild material | See also NA 87260 for material of this same collection received in 2022 from Morris Arboretum. | 1953991 | NA 84716 |
| 9 | NA 82040 | JDC/QM/2014/057/559 | Quercus muehlenbergii Engelm. | Arkansas, United States | NA | | | 2014 | COLLECTED | 09/20/2014 | Arkansas: Lee County; St. Francis National Forest along Lee County Road 230. | 34.73003400, -90.72795500 | 87 | Roadside. Dry, higher elevation than surrounding area. Growing in association with Callicarpa americana, Celtis sp., and Juniperus virginiana. | Wild material | Acorns approximately 4-7 days from peak maturity. | 1922341 | NA 82040 |
| 10 | NA 82071 | JDC/QM/2014/103/605 | Quercus michauxii Nutt. | Mississippi, United States | NA | | | 2014 | COLLECTED | 09/25/2014 | Chinchahoma Creek watershed near Ennis Road. | 33.38574900, -88.92255600 | 98 | Wet, deciduous woods. | Wild material | Specimen sampled measured 26.75" d.b.h. and approximately 110' in height. Fruits still green. | 1922372 | NA 82071 |
| 11 | NA 82077 | JDC/QI/2014/118/620 | Quercus imbricaria Michx. | Iowa, United States | NA | | | 2014 | COLLECTED | 09/28/2014 | Iowa: Davis County; Near Davis and Wapello County line along Highway 63. | 40.89305600, -92.40904200 | 234 | Dry woods. Growing in association with Fraxinus pennsylvanica, Ulmus sp., Quercus sp., and Juniperus virginiana. | Wild material | Optimum timing for harvest. Acorns just starting to drop. | 1922378 | NA 82077 |
| 12 | Ames 23752 | NSA 960194 | Quercus hybr. | Nebraska, United States | NC7 |  | | 1997 | COLLECTED | PRE 1997 | Southwest of Salem approximately 2.6 miles, T1N R15E NW 1/4 NW 1/4 Sec. 21, Richardson County. | 40.04268000, -95.74558000 | 330 | Prairie knoll/ridge, very dry and rocky substrate. Growing in association with Rhus sp., Liatris aspera (white and purple), Juniperus virginiana, Quercus rubra, Quercus macrocarpa, and Schizachyrium scoparium. | Wild material | Specimens at the collection site in nature are represented as very large/old plants, approximately 5.0 meters in height with trunk diameters to 25.0 cm. After 15 years of growth in cultivation in central Iowa, specimens average approximately 3.5 x 3.5 meters. This species is reported to sucker, but all specimens of this accession have shown no signs of suckering while grown in cultivation. Peak fall color tends to occur during the second week in October in central Iowa ranging from reddish-orange; brownish-red, brownish-orange, etc. Acorn production tends to be consistently heavy every year and can initiate production after three years in age. Peak fruiting tends to occur between 5-15 of September in central Iowa, which is approximately 1 week prior to Q. muehlenbergii. Acorns are extremely favored by deer, rabbits, raccoons, turkeys and bluejays. Quercus prinoides in Nebraska is extremely rare. To date (2022), only two counties totalling four localities have recorded this taxa including Richardson County: two areas near Salem; one in Indian Caves State Park and one in Nemaha County described as near Nemaha. Species tends to be restricted to dry rocky upland hills and bluffs. Recent research (Hipp et al., 2019), noted that using the unweighted pair group method with arithmetic mean and non-metric multidimensional scaling ordination did not separate individuals of Q. muehlenbergii and Q. prinoides as distinct species. However, W. M. Keith Jr. (1957) states that "Q. muehlenbergii never spreads vegetatively and acorns are rarely borne until it has attained small tree size whereas Q. prinoides bears at extremely small sizes, usually a foot or so high and spreads vegetatively via rhizomes". Therefore, genetics of this accession most likely represents the hybrid of Q. prinoides x Q. muehlenbergii under the assumption that the true Q. prinoides is represented only by those that clonally spread via rhizomes. Further research is needed to clarify the identity of Q. prinoides. This accession is therefore being listed as Q. hybr. Specimens are clearly "dwarf" or shrubby in growth habit and produce acorns at extremely early ages, but do not spread via rhizomes. | 1543547 | Ames 23752 |
| 13 | PI 710503 | CBG-4508 | Tephrosia virginiana (L.) Pers. | Illinois, United States | S9 | | | 2016 | | | | | | | Wild material | | 1942747 | PI 710503 |
| 14 | PI 710504 | CBG-5562 | Tephrosia virginiana (L.) Pers. | Illinois, United States | S9 | | | 2016 | | | | | | | Wild material | | 1942792 | PI 710504 |
| 15 | PI 616939 | F. virginiana subsp. virginiana NC 98-2-2 | Fragaria virginiana Mill. subsp. virginiana | Tennessee, United States | COR | | Out of Season | 2000 | COLLECTED | 09/25/1998 | From I-40 take Strawberry Plains PIke north for 1.9 miles to McCubbins Cemetary Lane. Turn right and go 0.1 mile to Mcubbins Cemetary. Site is McCubbins Cemetary grounds. Knox county. | 36.01917000, -83.74694000 | 425 | Dry uplands, silty topsoil, shale underneath. Quercus alba, Pinus virginiana, Pespalum subsp., Potentilla canadensis, Andropogon sp., Plantogo sp., Ulmus sp., Acer rubra and Acer barbatum. Mosses, lichens and grasses. | Wild material | | 1603151 | PI 616939 |
| 16 | PI 616940 | F. virginiana subsp. virginiana NC 98-2-3 | Fragaria virginiana Mill. subsp. virginiana | Tennessee, United States | COR | | Out of Season | 2000 | COLLECTED | 09/25/1998 | From I-40 take Strawberry Plains PIke north for 1.9 miles to McCubbins Cemetary Lane. Turn right and go 0.1 mile to Mcubbins Cemetary. Site is McCubbins Cemetary grounds. Knox county. | 36.01917000, -83.74694000 | 425 | Dry uplands, silty topsoil, shale underneath. Quercus alba, Pinus virginiana, Pespalum subsp., Potentilla canadensis, Andropogon sp., Plantogo sp., Ulmus sp., Acer rubra and Acer barbatum. Mosses, lichens and grasses. | Wild material | | 1603152 | PI 616940 |
| 17 | PI 616941 | F. virginiana subsp. virginiana NC 98-2-3 | Fragaria virginiana Mill. subsp. virginiana | Tennessee, United States | COR | | Out of Season | 2000 | COLLECTED | 09/25/1998 | From I-40 take Strawberry Plains PIke north for 1.9 miles to McCubbins Cemetary Lane. Turn right and go 0.1 mile to Mcubbins Cemetary. Site is McCubbins Cemetary grounds. Knox county. | 36.01917000, -83.74694000 | 425 | Dry uplands, silty topsoil, shale underneath. Quercus alba, Pinus virginiana, Pespalum subsp., Potentilla canadensis, Andropogon sp., Plantogo sp., Ulmus sp., Acer rubra and Acer barbatum. Mosses, lichens and grasses. | Wild material | | 1603153 | PI 616941 |
| 18 | NA 89193 | DLSP-SB | Hamamelis virginiana L. | Wisconsin, United States | NA | | | 2025 | COLLECTED | 08/21/2024 | Devil's Lake State Park: South Bluff. | 43.41164210, -89.74057740 | 327 | Shade to partial shade in clayey, organic, mesic material on boulders. Slope: 45 degrees. Aspect: Northwest. White oak-sugar maple vegetative community. | Wild material | | 2171014 | NA 89193 |
| 19 | NA 88666 | RJL2023PA-003 | Hamamelis virginiana L. | Pennsylvania, United States | NA | | | 2023 | COLLECTED | 10/01/2023 | Collected primarily along the woodland edge along Northside Road on Pennsylvania State Gamelands No. 43 as well as a few on nearby roads. | 40.17974200, -75.76790700 | 176 | Plants were growing in mesic well-drained conditions on moderately sloping sites of a deciduous upland forest. This species grows well in shade to part-sun. Most abundant fruit development is found where plants are exposed to sunlight for a portion of the day. Slope: 15%. Aspect: North-northwest. The underlying geology of this area is of Precambrian origin and characterized as the Graphitic Felsic Gneiss. This includes Pickering Gneiss and small areas of marble; dominantly quartz and feldspar with varying amounts of graphite and various metamorphic minerals; medium grained, light to dark gray and greenish gray; sedimentary origin. (Source: USGS Pennsylvania Geologic Map Data.) The primary soil type in the area of this collection is classified as Gladstone Gravelly Loam Series (8 to 15 percent slopes). The Gladstone Series consists of very deep, well drained soils formed in residuum and colluvium from granitic gneiss. Saturated hydraulic conductivity is moderately high to high. Solum thickness ranges from 75 to 125 cm. Depth to granitic gneiss bedrock is 1.6 meters or more. The bedrock may be strongly weathered in the upper part. Gravel content ranges from 5 to 35 percent throughout the solum, and 10 to 40 percent in the C horizons. Fragments, larger than 3 inches in diameter, range from 0 to 20 percent by volume in the surface layer and 0 to 10 percent in the subsoil and substratum layers. Reaction is strongly or very strongly acid throughout the soil, unless limed. Areas that have been limed range to moderately acid in the upper part of the profile. (Source: NRCS Web Soil Survey.) | Wild material | | 2158815 | NA 88666 |
| 20 | NA 88620 | KY23-024 | Hamamelis virginiana L. | Kentucky, United States | NA | | | 2023 | COLLECTED | 09/10/2023 | The Gulf - Natural Arch Scenic Area Panoramic Trail. | 36.84624000, -84.52807000 | 380 | Ridgeline. Elevation: 1248 feet. Aspect: South. | Wild material | | 2158712 | NA 88620 |
| 21 | WLP 3138 | TJK2023AL-002 | Hamamelis virginiana L. | Alabama, United States | NA | | | 2023 | COLLECTED | 08/15/2023 | Haines Island Park; overlooks the Alabama River. | 31.72074000, -87.46362000 | 94 | Beautiful Pine-Oak forest sits atop the Buhrstone Questa, an escarpment that rises over 350 feet. Southern Red Hills Region. Slope: 12%. Aspect: West. Elevation recorded as 308 feet. | Wild material | WLPGR contract collection. | 2158470 | WLP 3138 |
| 22 | NA 88485 | RJL2022MD-006 | Hamamelis virginiana L. | Maryland, United States | NA | | | 2022 | COLLECTED | 09/04/2022 | Plants growing at Elkton State Forest on Elk Neck Trail #3 (Starkey Lane) labelled as the address of 717 Irishtown Rd, North East, MD 21901. This species was infrequent throughout most of Elk Neck State Park, but relatively common. | 39.58790000, -75.88853100 | 54 | Plants are growing in a mesic to dry, well-drained habitat of mixed deciduous and evergreen woodlands comprised primarily of acid-loving plants. Plants are growing in part shade to shade. The soils in the collection area are generally described as a complex series of fluviomarine deposits. The soils range from a thin loam layer at the surface to varying levels of loam to sandy loam and/or extremely gravelly sandy clay loam strata, depending upon geographical location (ie. Hillslope summits, slopes, footslopes, swales, etc.). The primary soil types in the collection area are classified as Russett-Christiana-Hambrook Complex and/or Sassafras and Croom Soils; though, others may intersect and overlay in specific areas.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2139364 | NA 88485 |
| 23 | OPGC 8339 | CBG-10556 | Anemone virginiana L. | Illinois, United States | OPGC | | | 2021 | | | | | | | Wild material | GPS coordinates incomplete. | 2120152 | OPGC 8339 |
| 24 | NA 87997 | MARSB-311 | Juniperus virginiana L. | New Jersey, United States | NA |  | | 2018 | | | | | | | Wild material | | 1964757 | NA 87997 |
| 25 | OPGC 6376 | CBG-8085 | Anemone virginiana L. | Illinois, United States | OPGC |  | | 2017 | | | | | | | Wild material | | 1954753 | OPGC 6376 |
| 26 | WLP 1432 | NA 83894 | Ostrya virginiana (Mill.) K. Koch | Kentucky, United States | NA | | | 2016 | COLLECTED | 09/27/2016 | Cumberland Falls State Park, Cumberland Falls Visitor Center. | 36.84000000, -84.34300000 | 258 | | | | 1952033 | WLP 1432 |
| 27 | W6 51598 | CBG-4308 | Physalis virginiana Mill. | Illinois, United States | W6 | | | 2016 | | | | | | | Wild material | | 1942728 | W6 51598 |
| 28 | DDIO 266 | JDC/DV/2014/050/552 | Diospyros virginiana L. | Missouri, United States | DAV | | | 2015 | COLLECTED | 09/19/2014 | PIKE COUNTY: Buffalo Knob along MO highway WW. | 39.27421400, -91.04618000 | 270 | Dry woods, rocky south-facing steep slope. Growing in association with Quercus muehlenbergii, Fraxinus americana, Fraxinus quadrangulata, Juniperus virginiana, Ulmus sp., Cercis canadensis, and Lonicera maackia. | Wild material | | 1927163 | DDIO 266 |
| 29 | OPGC 6154 | CBG-2479 | Tradescantia virginiana L. | Illinois, United States | OPGC |  | | 2015 | | | | | | | Wild material | | 1926012 | OPGC 6154 |
| 30 | NA 82052 | JDC/MV/2014/078/580 | Magnolia virginiana L. | Mississippi, United States | NA | | | 2014 | COLLECTED | 09/22/2014 | Mississippi: Tishomingo County; Bottomlands of Foote Branch Creek off Highway 982. | 34.87692100, -88.28330100 | 150 | Deciduous woods. Growing in association with Quercus michauxii, Acer rubrum, Alnus sp., Liquidambar styraciflua, Toxicodendron radicans, Pinus sp., Nyssa sylvatica, and Vaccinum sp. | Wild material | Impressive specimens. Optimum timing of harvest. Largest specimen measuring 19" d.b.h. and approximately 80' in height. | 1922353 | NA 82052 |
| 31 | NA 81936 | NA 81936 | Magnolia virginiana L. | Texas, United States | NA | | | 2013 | COLLECTED | 04/11/2011 | On S side of County Road 59 ca. 1000 ft. W of it's juncture with Private Road 335 and ca. 0.25 miles N of Highway 255. | 31.05566000, -94.15485000 | | Growing in seepage areas of otherwise dry Pinus palustris forest. | | | 1951206 | NA 81936 |
| 32 | WLP 1411 | JDC/OV/2010/049/319 | Ostrya virginiana (Mill.) K. Koch | Arkansas, United States | NA |  | | 2010 | COLLECTED | 09/16/2010 | Gamaliel Recreation Area, along Norfork Lake, Baxter County. | 36.42831000, -92.21806000 | 216 | Rock outcrop with underground seep. East facing slope (65%). Associated with Cotinus obovatus, Acer saccharum, Juniperus virginiana, Viburnum sp., Quercus muehlenbergii, Frangula caroliniana, Hydrangea arborescens, Cornus florida, Smilax sp., and Ulmus sp. (likely U. alata). | Wild material | | 1848910 | WLP 1411 |
| 33 | WLP 2120 | 302025 | Juniperus virginiana L. | Virginia, United States | NA |  | | 2008 | COLLECTED | 12/28/2005 | | | 89 | Slope: 0 Aspect: NE Soil: Clay-loam, Land form: Upland meadow. Mowed. | Wild material | | 1780179 | WLP 2120 |
| 34 | PI 704859 sos | V. fuscatum NCBG-440 | Vaccinium fuscatum Aiton | North Carolina, United States | COR | | | 2021 | | | | | | | Wild material | PI assigned before phyical inventory of W6 shipment and is missing. Maintain COR as site in case seeds are recovered. Berries glaucous, calyx not oppressed | 2116310 | PI 704859 sos |
| 35 | PI 704860 sos | V. fuscatum NCBG-441 | Vaccinium fuscatum Aiton | North Carolina, United States | COR | | | 2021 | | | | | | | Wild material | PI assigned before phyical inventory of W6 shipment and is missing. Maintain COR as site in case seeds are recovered. Berries black, glabrous | 2116311 | PI 704860 sos |
| 36 | PI 702725 | NCBG-428 | Schizachyrium scoparium (Michx.) Nash | Maryland, United States | S9 |  | | 2019 | | | | | | | Wild material | | 2098447 | PI 702725 |
| 37 | PI 704823 sos | V. corymbosum MARSB-141 | Vaccinium corymbosum L. | Delaware, United States | COR |  | | 2019 | | | | | | | Wild material | | 2097497 | PI 704823 sos |
| 38 | PI 664805 | JDC/HX/2010/035/305 | Helianthus mollis Lam. | Kansas, United States | NC7 | | | 2010 | COLLECTED | 09/14/2010 | Roadside along Kansas Rd, west of Hwy 3 south of Uniontown, Bourbon County. | 37.81978000, -94.98685000 | 325 | Uplands. Associated with Andropogon gerardii, Bidens polylepis, Chamaechrista fasciculata, Cornus, Diospyros virginiana, Gleditsia triacanthos, Juglans nigra, Maclura pomifera, Monarda, Pycnanthemum virginianum, Quercus, Rhus glabra, and Sorghastrum nutans. | Wild material | | 1848907 | PI 664805 |
| 39 | PI 654985 | C. americana Delaware | Corylus americana Marshall | Delaware, United States | COR | | | 2007 | COLLECTED | 10/25/2007 | New Castle County, Bellevue State Park (800 Carr Road, Wilmington), off the Northern Delaware Greenway Trail, growing in understory of beach-oak forest. | 39.78180000, -75.50080000 | 70 | Growing in woodland duff. Associated plants: Sasafras lbidum, Euonymous americana, Fagus grandifolia, Liquidambar styrasiflua, Quercus alba, Hamamelis virginiana. | Wild material | | 1743480 | PI 654985 |
| 40 | PI 657226 | V. pallidum Stumphouse HD-2007-025 | Vaccinium pallidum Aiton | South Carolina, United States | COR |  | | 2007 | COLLECTED | 06/04/2007 | Stumphouse Mountain, Oconee County. Northwest of Walhalla off SR-107, Ross Mountain Road, near Gramling Drive, edge of trail. | 34.82217000, -83.10895000 | 487 | Red sandy loam associated with: Liriodendron tulipifera, Oxydendron arboreum, Kalmia latifolia, Acer rubrum, Quercus nigra, Cornus florida and Prunus virginiana. | Wild material | Kim Hummer, Michael Dossett collected from South Carolina.
| 1730117 | PI 657226 |
| 41 | PI 657195 | V. fuscatum HL-2006-041 | Vaccinium fuscatum Aiton | Florida, United States | COR |  | | 2006 | COLLECTED | 05/26/2006 | Among residential roads on eastern shore of Lake Marion, southeast of Haines City, Polk county. | 28.09643000, -81.50633000 | 30 | North florida swamp plants. Ecotome between wet bay head and sand scrub plants. Rhododendron viscosisimum cerulatum, Diospyros virginiana, Magnolia virginianum Nyssa biflorida, Persia pulustris and Quercus nigra. | Wild material | Eastern edge of Lake Wales Ridge region. Housing developments encroaching into natural areas. | 1702644 | PI 657195 |
| 42 | PI 656829 | JM2005805 | Trichostema dichotomum L. | South Carolina, United States | NC7 | | | 2006 | COLLECTED | 09/28/2005 | Along Highway 17 to Bailey Island, 100 meters off Pine Landing Road, Charleston County. | 33.15000000, -80.43527778 | 3 | Barrier island; live oak community; weedy; sandy loam soil. | Wild material | | 1704277 | PI 656829 |
| 43 | PI 649085 | 130 | Hypericum punctatum Lam. | Missouri, United States | NC7 |  | | 2004 | COLLECTED | 10/28/2004 | Roadside, west edge of Hawn State Park, Ste. Genevieve County. | 37.82760000, -90.25840000 | 286 | Short leaf pine forest. | Wild material | | 1668206 | PI 649085 |
| 44 | PI 656838 | 106 | Triadenum walteri (J. F. Gmel.) Gleason | Arkansas, United States | NC7 | | | 2004 | COLLECTED | 10/25/2004 | Trailside, seepy area next to lake, Village Creek State Park, Cross County. | 35.15298300, -90.71776600 | 128 | Seepy area, lakeside, oak-hickory bottom land forest. 1-3 degrees of slope with a northeastern aspect. Loess soil. | Wild material | 1 meter tall. | 1668211 | PI 656838 |
| 45 | PI 664833 | 143 | Echinacea purpurea (L.) Moench | Missouri, United States | NC7 |  | | 2004 | COLLECTED | 06/23/2004 | Private property located just west of Branson West, T23N R23W Sec. 17 | 36.69485000, -93.44073300 | 326 | 10-20% slope with a northwestern aspect. Dolomitic glade soil, bedrock at or near surface. | Wild material | Plants in nature measuring approximately 1 foot in height. | 1668184 | PI 664833 |
| 46 | PI 664856 | 2 | Hypericum perforatum L. | Missouri, United States | NC7 |  | | 2004 | COLLECTED | 10/19/2004 | Roadside along Interstate 44/Historic Route 66, Franklin County. | 38.26538300, -91.11135000 | 281 | Overgrown prairie roadside. 5 degrees of slope with a northern aspect. | Wild material | Opposite leaves. 20-40 cm tall. | 1668195 | PI 664856 |
| 47 | PI 664868 | 131 | Hypericum prolificum L. | Missouri, United States | NC7 |  | | 2004 | COLLECTED | 10/28/2004 | Near campground, Hawn State Park, Ste. Genevieve County. | 37.82756600, -90.25841600 | 286 | Riverine/creekside. 1-5% slope with a northwestern aspect. Sandy/gravelly soil. | Wild material | | 1668193 | PI 664868 |
| 48 | PI 658645 | 18-78 | Monarda fistulosa L. | Arkansas, United States | NC7 |  | | 2004 | COLLECTED | 10/23/2004 | East loop of Benefield Trail, Magazine Mountain State Park, Logan County. | 35.16250000, -93.60083333 | 711 | Oak-Hickory forest. 5-10% slope with a northern aspect. Loess soil. | Wild material | 2-3 feet tall. During a grow out of 15 Monarda fistulosa accessions at NCRPIS during 2020-2021, this accession had the palest pink flowers. Flower color ranged from pure white in some plants to very faint pink in others. | 1667593 | PI 658645 |
| 49 | PI 662022 | Ames 27628 | Euonymus atropurpureus Jacq. | Iowa, United States | NC7 | | | 2004 | COLLECTED | 10/09/2004 | Point on southwest side at the top of Rattlesnake Bluff, Van Buren County. | 40.76361111, -91.90361111 | 195 | | Wild material | | 1665916 | PI 662022 |
| 50 | PI 649704 | 39 | Physocarpus opulifolius (L.) Maxim. | Iowa, United States | NC7 |  | | 2003 | COLLECTED | 09/24/2003 | Starr's Cave State Preserve located just northwest of Burlington, T70N, R2W NW 1/4 of NW 1/4 of Sec. 19, West Burlington Quad, Des Moines County | 40.85194444, -91.13722222 | 183 | Edge of limestone bluff. 1/2 to 3/4 sunny. Steep slope with a southern aspect. Thin, very rocky soil, well drained | Wild material | | 1649673 | PI 649704 |
| 51 | PI 649703 | 14 | Physocarpus opulifolius (L.) Maxim. | Iowa, United States | NC7 |  | | 2003 | COLLECTED | 09/14/2003 | Fish Farm Mounds, New Albin, SW 1/4 of SW 1/4 of NW 1/4 of Section 26, T100N, R4W, New Albin Quad, Allamakee County. | 43.45111111, -91.28222222 | 280 | Sandstone ridge just above goat prairie. 1/2 sun. 30-50% slope w/ NW aspect. Sandy loam soil w/ some stoniness, well drained | Wild material | Medium sized shrubs. | 1649463 | PI 649703 |
| 52 | PI 649714 | 13a | Drymocallis arguta (Pursh) Rydb. | Iowa, United States | NC7 |  | | 2003 | COLLECTED | 09/14/2003 | North Bear Creek Wildlife Area near Highlandville, T100N, R7W N edge of SE 1/4 of SW 1/4 of Sec. 25, Dorchester Quad, Winneshiek County. | 43.44583333, -91.62222222 | 311 | Dolomite cliffs. Half sunny. Edge of sheer cliff with a north to northwest aspect. Rock crevices. | Wild material | | 1649464 | PI 649714 |
| 53 | PI 656820 | Ames 27186 | Physocarpus opulifolius (L.) Maxim. | Iowa, United States | NC7 |  | | 2003 | COLLECTED | 08/24/2003 | Along Old Indian Trail, overlooking Pease Creek, Ledges State Park, S 1/2 of SE 1/4 of SW 1/4 of Section 16, T83N, R26W, Madrid NW Quad, Boone County. | 41.99500000, -93.88583333 | 289 | Sandstone ridge. | Wild material | Shrubs to 2 meters tall. | 1648564 | PI 656820 |
| 54 | PI 635440 | H. lupulus var. neomexicanus OCJ-14 | Humulus lupulus L. var. neomexicanus A. Nelson & Cockerell | Colorado, United States | COR | | | 2002 | COLLECTED | 09/12/2002 | South from Craig on State Road 13 past Axial to between mile post (MP) 61 and MP 62 along Good Spring Creek. | 40.26306000, -107.78861000 | 1994 | Raparian; among Ribes aureum, Prunus virginiana and Quercus gambelii. | Wild material | | 1642199 | PI 635440 |
| 55 | PI 631294 | 038 | Echinacea hybr. | Arkansas, United States | NC7 |  | | 1997 | COLLECTED | 08/18/1997 | Near Mountain View, Stone County. Please contact curator for specific site location. | 36.05000000, -92.11666667 | 320 | Limestone glade. Full exposure, ~30 degrees of slope with a southern aspect. Calcareous, well drained soil with high stoniness. | Wild material | Plants were up to ~2 feet tall, occasional, and unbranched with yellow flowers. | 1548362 | PI 631294 |
| 56 | PI 631295 | 039 | Echinacea pallida (Nutt.) Nutt. | Arkansas, United States | NC7 |  | | 1997 | COLLECTED | 08/18/1997 | Near Mountain View, Stone County. Please contact curator for specific site location. | 36.05000000, -92.11666667 | 320 | Limestone glade. Full exposure, ~30 degrees of slope with a southern aspect. Calcareous, well drained soil with high stoniness. | Wild material | Plants were up to ~2.5 feet tall, occasional, and unbranched with very pale pink flowers. | 1548363 | PI 631295 |
| 57 | PI 589766 | GMAL 2367 | Malus angustifolia (Aiton) Michx. | Virginia, United States | GEN | | | 1987 | COLLECTED | 08/27/1987 | Virginia, Shenandoah Co. 5.4 mi SE of junction US 11 and Co. 675 on Co. 675 at W. corner of unmarked dirt Rd to the W. | | | | | Comments: 20 ft. tall, 6 cm diameter. Population of 6 large trees and 20+ smaller trees. Ostoya Virginia, Cornus, Pinus virginiana, Carya, Ovata, Carya cordiformis, Quercus. | 1019975 | PI 589766 |
| 58 | Ames 38800 | Camp Mitigwa | Amelanchier arborea (F. Michx.) Fernald | Iowa, United States | NC7 |  | | 2026 | COLLECTED | 06/01/2026 | Mitigwa Scout Camp located on west side of Des Moines River watershed approximately 7.50 miles south, southwest of Boone, T82N R26W N 1/4 Sec. 5 and T83N R26W S 1/4 Sec. 32. | 41.94894500, -93.90537200 | 310 | High-quality white oak - ironwood, mature woods. | Wild material | The native range of Amelanchier arborea is concentrated in the eastern half of the U.S. (Little, 1977). This accession represents a collection of A. arborea germplasm from the western edge of the species native range, specifically central Iowa. Specimens sampled at the collection site in nature were small to medium understory or woodland edge single and/or multi-trunked trees with a few trees getting close to being deemed as canopy specimens. Bark smooth and light grey in color. Specimens sampled in nature ranging 15-50' in height. Peak flowering occurred on 8 April 2026 with white flowers appearing prior to leaf expansion. Fall colors ranging from orange to orange-red peaking typically at the end of September (central Iowa). Fruits, dark-pink to red, maturing in early June (peak in 2026 occurred on 2 June) averaging 8 mm in diameter, except for mother tree #6 that had rather large fruits at 11 mm in diameter. | 2197049 | Ames 38800 |
| 59 | NA 89173 | 2025RJLSEUS-14 | Chionanthus sp. | Florida, United States | NA | | | 2026 | COLLECTED | 10/03/2025 | Choctawhatchee National Forest: the collection site is reached by foot (~0.5 km) along a loose sand road/firebreak from Martin Luther King, Jr. Boulevard, just east of the boundary for Hurlburt Field in Hurlburt Field/Ft. Walton Beach, FL. Collected from 30 deg. 26.859', -86 deg. 39.577' to 30 deg. 27.137', -86 deg. 39.580'; latitude and longitude of record calculated at the midpoint of these coordinates. | 30.44996000, -86.65965000 | 10 | Dry to xeric conditions of well-drained, deep sandy soils on a relatively level area bordering a powerline in an open mixed mostly mixed evergreen and deciduous, somewhat disturbed habitat in sun to part shade. In areas “broadleaved scrub” vegetation is so dense, that it is almost impenetrable. Elevation: 9 to 11 meters. Slope: 0 to 3 percent. Aspect: Variable. Soil: The soils of this area are characterized as Foxworth Series (95 percent) sand, 0 to 5 percent slopes (8). Other soil series interbedded with the Foxworth Series, vary in percentages from 1-4 percent including Lakeland and Chipley. The Foxworth Series consists of very deep, moderately well to somewhat excessively drained, rapid to very rapid permeable soils on broad uplands and side slopes. They formed in sandy marine or eolian sediments in the Southern Coastal Plain (MLRA 133A), The Eastern Gulf Coast Flatwoods (MLRA 152A), The Atlantic Coast Flatwoods (153A) and the Tidewater Area (153B). Thickness of the grayish brown to light yellowish-brown sand exceeds 2 meters. Reaction ranges from very strongly acid to slightly acid throughout. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). Geology: The underlying geology of this area is characterized as undifferentiated Quaternary Sediments. Much of Florida's surface is covered by a varying thickness of undifferentiated sediments consisting of siliciclastics, organics and freshwater carbonates. Where these sediments exceed 6.1 meters thick, they were mapped as discrete units. To subdivide the undifferentiated sediments, those sediments occurring in flood plains were mapped as alluvial and flood plain deposits (Qal). Sediments showing surficial expression of beach ridges and dunes were mapped separately (Qbd) as were the sediments composing Trail Ridge (Qtr). Terrace sands were not mapped (refer to Healy [1975] for a discussion of the terraces in Florida). The subdivisions of the Undifferentiated Quaternary Sediments (Qu) are not lithostratigraphic units but are utilized to facilitate a better understanding of the State's geology. The siliciclastics are light gray, tan, brown to black, unconsolidated to poorly consolidated, clean to clayey, silty, unfossiliferous, variably organic-bearing sands to blue green to olive green, poorly to moderately consolidated, sandy, silty clays. Gravel is occasionally present in the panhandle. Organics occur as plant debris, roots, disseminated organic matrix and beds of peat. Freshwater carbonates, often referred to as marls in the literature, are scattered over much of the State. In southern Florida, freshwater carbonates are nearly ubiquitous in the Everglades. These sediments are buff colored to tan, unconsolidated to poorly consolidated, fossiliferous carbonate muds. Sand, silt and clay may be present in limited quantities. These carbonates often contain organics. The dominant fossils in the freshwater carbonates are mollusks. (Source: USGS Florida Geologic Map Data). | Wild material | Received as C. cf. henryae | 2193307 | NA 89173 |
| 60 | NA 89171 | 2025RJLSEUS-04 | Rhododendron catawbiense Michx. | Alabama, United States | NA | | | 2026 | COLLECTED | 09/30/2025 | Scarham Creek: southeast of the Pea Ridge Road bridge, approximately 50-80 meters on the south side of the creek. | 34.32559600, -86.16054600 | 266 | Growing near the base of the slopes above the riparian zone, generally on the exposed geology under very well-drained conditions. The woodlands are primarily deciduous with a few evergreens infrequently mixed. Slope: 15 to 30 percent. Aspect: Northeast. Soil: The primary soil type in the area of this collection is classified as Rockland Series sandstone (Rc). The Rockland series consists of well drained soils formed in loamy colluvium from rotational landslides on slopes of stream valleys and dissections of ground moraines. Saturated hydraulic conductivity is moderate in the upper part of the profile and moderately slow in the lower part. Slopes range from 18 to 70 percent. Some pedons have buried leaves, twigs, and moss. Mass soil movement has left random remnants of soil structure from prior upslope soil development and has buried tree branches, leaves and moss. The upper 0-2 cm of soil contains slightly decomposed organic matter while lower soils layers to a depth of 58 cm are comprised of dark reddish-brown to brown silt loam and are moderately acidic. Below 58 cm the soils are generally dark reddish-brown silt loam and strongly to moderately alkaline. (Source:California Soil Resource Lab/NRCS Official Soil Series Descriptions). Geology: The underlying geology of this area is of Pennsylvanian origin and characterized as Pottsville Formation. It is characterized by light-gray thin to thick-bedded quartzose sandstone and conglomerate containing interbedded dark-gray shale, siltstone, and coal. Mapped on Lookout Mountain, Blount and Chandler Mountains, and Sand Mountain northeast of Blount County, and on the mountains of Jackson, Marshall, and Madison Counties north and west of the TN river. (Source: USGS Alabama Geologic Map Data). | Wild material | Received as R. catawbiense vsr. insularis | 2193305 | NA 89171 |
| 61 | NA 89155 | 2025RJLSEUS-02 | Ilex longipes Chapm. ex Trel. | Alabama, United States | NA | | | 2025 | COLLECTED | 09/30/2025 | Scarham Creek: southeast of the Pea Ridge Road bridge, approximately 50-80 meters on the south side of the creek. | 34.32520700, -86.15967000 | 261 | Plants are growing on relatively steep woodland slopes in shade. The woodlands are primarily deciduous with a few evergreens infrequently mixed. Slope: 15 to 30 percent. Aspect: Northeast. Soil: The primary soil type in the area of this collection is classified as Rockland Series sandstone (Rc). The Rockland series consists of well drained soils formed in loamy colluvium from rotational landslides on slopes of stream valleys and dissections of ground moraines. Saturated hydraulic conductivity is moderate in the upper part of the profile and moderately slow in the lower part. Slopes range from 18 to 70 percent. Some pedons have buried leaves, twigs, and moss. Mass soil movement has left random remnants of soil structure from prior upslope soil development and has buried tree branches, leaves and moss. The upper 0-2 cm of soil contains slightly decomposed organic matter while lower soils layers to a depth of 58 cm are comprised of dark reddish-brown to brown silt loam and are moderately acidic. Below 58 cm the soils are generally dark reddish-brown silt loam and strongly to moderately alkaline. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). Geology: The underlying geology of this area is of Pennsylvanian origin and characterized as Pottsville Formation. It is characterized by light-gray thin to thick-bedded quartzose sandstone and conglomerate containing interbedded dark-gray shale, siltstone, and coal. Mapped on Lookout Mountain, Blount and Chandler Mountains, and Sand Mountain northeast of Blount County, and on the mountains of Jackson, Marshall, and Madison Counties north and west of the TN river. (Source: USGS Alabama Geologic Map Data). | Wild material | | 2193001 | NA 89155 |
| 62 | NA 89156 | 2025RJLSEUS-03 | Euonymus americanus L. | Alabama, United States | NA | | | 2025 | COLLECTED | 09/30/2025 | Scarham Creek: southeast of the Pea Ridge Road bridge, approximately 50-80 meters on the south side of the creek. | 34.32577600, -86.16071000 | 260 | Plants are growing on relatively steep woodland slopes in shade. The woodlands are primarily deciduous with a few evergreens infrequently mixed. Slope: 15 to 30 percent. Aspect: Northeast. Soil: The primary soil type in the area of this collection is classified as Rockland Series sandstone (Rc). The Rockland series consists of well drained soils formed in loamy colluvium from rotational landslides on slopes of stream valleys and dissections of ground moraines. Saturated hydraulic conductivity is moderate in the upper part of the profile and moderately slow in the lower part. Slopes range from 18 to 70 percent. Some pedons have buried leaves, twigs, and moss. Mass soil movement has left random remnants of soil structure from prior upslope soil development and has buried tree branches, leaves and moss. The upper 0-2 cm of soil contains slightly decomposed organic matter while lower soils layers to a depth of 58 cm are comprised of dark reddish-brown to brown silt loam and are moderately acidic. Below 58 cm the soils are generally dark reddish-brown silt loam and strongly to moderately alkaline. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). Geology: The underlying geology of this area is of Pennsylvanian origin and characterized as Pottsville Formation. It is characterized by light-gray thin to thick-bedded quartzose sandstone and conglomerate containing interbedded dark-gray shale, siltstone, and coal. Mapped on Lookout Mountain, Blount and Chandler Mountains, and Sand Mountain northeast of Blount County, and on the mountains of Jackson, Marshall, and Madison Counties north and west of the TN river. (Source: USGS Alabama Geologic Map Data). | Wild material | | 2193002 | NA 89156 |
| 63 | NA 89158 | 2025RJLSEUS-06 | Cornus florida L. | Alabama, United States | NA | | | 2025 | COLLECTED | 10/01/2025 | Coosa Wildlife Management Area: along the edge of gated dirt road on the west side of Coosa County Road 29, 0.3 kilometers north of Hatchet Creek. | 32.86402200, -86.33871400 | 108 | Plants are growing in part sun to shade on dry-mesic slopes above the road cut on the gated dirt road; most likely a road for access for fire control/forest management. The forest is a combination of deciduous and evergreen with evergreens primarily comprised of Pinus taeda. The habitat was quite dry during this time of year. Slope: 5 to 20 percent. Aspect: North. Soils: The primary soil in the area of this collection is classified as Madison-Louisa Series complex, 15 to 30 percent slopes, moderately eroded (MdE2). The Madison Series soils are very deep, well drained soils with medium runoff found on Piedmont uplands in interstream divides, ridges and side slopes. They are comprised of residuum weathered from felsic or intermediate, high-grade metamorphic or igneous rocks high in content of mica. Slopes range from 2 to 60 percent and soil is typically strongly acidic. Louisa Series soils The Louisa Series soils consist of shallow, somewhat excessively drained soils which formed over mica gneiss and schist bedrock. They occur on Piedmont uplands. Slopes are 6 to 80 percent. This soil is moderately acid. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). Geology: The underlying geology of this area is of Precambrian to Paleozoic origin and characterized as Hatchet Creek Group; Pinchoulee Gneiss Formation. It is characterized by medium to fine-grained migmatitic, locally garnetiferous biotite-feldspar gneiss, commonly saturated with granitic pods. (Source: USGS Alabama Geologic Map Data). | Wild material | | 2193004 | NA 89158 |
| 64 | NA 89161 | 2025RJLSEUS-10 | Stewartia malacodendron L. | Florida, United States | NA | | | 2025 | COLLECTED | 10/02/2025 | Eglin Air Force Base: woodlands along Weaver Creek accessed from unnamed dirt road, 0.82 kilometers west of junction with Eglin AFB 720; approximately 0.73 kilometers north of junction with Choctaw Nolf Airfield Road and Eglin AFB 720. | 30.51708000, -86.91515000 | 11 | Moist, well-drained, sandy soils above Weaver Creek in a mixed broadleaved evergreen and deciduous woodland habitat in part shade to shade of west facing slopes several meters above the wetland zone. A high-competition, richly diverse environment. Elevation: 7 to 15 meters. Slope: 1 to 15 percent. Aspect: West. Soils: The soils of this area are characterized as Lakeland Series which consist of very deep, excessively drained, rapid to very rapidly permeable soils on uplands. They formed in thick beds of eolian or marine and/or fluvio-marine sands. Thickness of the sand exceeds 2 meters. Silt plus clay in the upper meter ranges from 5-10 percent. Reaction ranges from very strongly acid to moderately acid throughout. (Source: USDA-NRCS Official Soil Series Descriptions). Geology: The underlying geology of this area is the Citronelle Formation, of Pliocene origin, and consists of gray to orange, often mottled, unconsolidated to poorly consolidated, very fine to very coarse, poorly sorted, clean to clayey sands. It contains significant amounts of clay, silt and gravel which may occur as beds and lenses and may vary considerably over short distances. Limonite nodules and limonite-cemented beds are common. (Source: USGS Florida Geologic Map Data). | Wild material | | 2193007 | NA 89161 |
| 65 | Ames 36697 | APS/JC/2025/XXX/XXX | Juniperus communis L. | Iowa, United States | NC7 |  | | 2025 | COLLECTED | 09/15/2025 | Located off Iowa River Drive approximately 2.5 miles southwest of New Albin, T100N R4W NE 1/4 NW 1/4 Sec. 21. | 43.46830000, -91.32128000 | 207 | Sandy ridge of a power line cut. | Wild material | | 2192820 | Ames 36697 |
| 66 | W6 62527 | FWS0300-130 | Solidago hispida Muhl. ex Willd. | Michigan, United States | W6 |  | | 2025 | | | | | | | Wild material | Received as: Solidago hispida | 2192225 | W6 62527 |
| 67 | W6 62530 | FWS0300-133 | Crocanthemum canadense (L.) Britton | Michigan, United States | W6 |  | | 2025 | | | | | | | Wild material | Helianthemum bicknellii also present, but easily distinguishable | 2192228 | W6 62530 |
| 68 | NA 89115 | TLM25-04a | Hamamelis ovalis S. W. Leonard | Texas, United States | NA | | | 2025 | COLLECTED | 07/10/2025 | State Highway 87 approximately 3.25 kilometers north of the crossroad junction with Texas Recreational Road 255 (RE 255); plants were growing in the narrow buffer woods along the east side of the highway. | 31.12051300, -93.72628100 | 138 | The habitat is an upland mixed coniferous and deciduous woodlands in part to full shade and dry conditions, often under drought stress. Plants seem to always occur on the top of dry ridges or well-drained slopes. Slope: 0 to 1 percent. Aspect: N/A. Soils: The soils of this collection area are classified as Tehran-Letney Association, hilly (TLE) soils. The Tehran Series (55%) consists of deep, somewhat excessively drained, moderately rapidly permeable soils on uplands. They formed in thick loamy and sandy sediments on the Western Coastal Plain. These soils are on gently sloping to moderately steep uplands with slopes ranging from 1 to 20 percent. The Letney Series (30%) consists of deep, well drained, moderately rapidly permeable, upland soils. They formed in thick sandy and loamy sediments of the coastal plains. These soils are on gently sloping to moderately steep uplands with slopes ranging from 1 to 20 percent. Soil pH ranges from 4.5 to 6.0. The minor soil components include Doucette Series (10%) and Boykin Series (5%) soils. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). Geology: The underlying geology of this area is of Oligocene origin and characterized as Catahoula Formation. This formation is extensive and deep in Texas, up to 185 meters thick. In the area of the collection the Catahoula Formation is primarily mudstone and sand. The upper 90-150 meters is mudstone that is tuffaceous, and sandy; also, occasionally, with some bentonitic clay. (Source: USGS Texas Geologic Map Data). | Wild material | | 2191654 | NA 89115 |
| 69 | NA 88928 | 24Flam6 | Rhododendron minus Michx. | Georgia, United States | NA | | | 2025 | COLLECTED | 09/09/2024 | Cumming, GA: Sawnee Mountain Preserve: primarily downslope of Mountainside Trail, with a fwe plants upslope of trail. | 34.23730000, -84.15298000 | 489 | Growing in half shade. Slope: 30 to 40 degrees. Aspect: East-northeast. | Wild material | | 2172811 | NA 88928 |
| 70 | NA 88931 | 24Flam27 | Rhododendron flammeum (Michx.) Sarg. | Georgia, United States | NA | | | 2025 | COLLECTED | 09/10/2024 | DeKalb County: Stone Mountain: Stone Mountain Park along Evergreen Trail by resort, growing within 40 feet of Venable Lake. GPS coordinates a general locality for population and each seed lot for 24Flam27-30 was collected progressively further west). | 33.79769000, -84.13420000 | 291 | Dry, somewhat shady forest adjacent to lake, some plants hanging over edge. Primarily close to the water on flat ground, though some on slope. Growing in half shade. Slope: Flat to 30 degrees. Aspect: North. | Wild material | Note: Seeds from three different lots collected at the same spot were bulked together in this accession; the lowest field collection number (24Flam27) has been chosen as the primary for this record. | 2172814 | NA 88931 |
| 71 | NA 88984 | TXWL2025-034 | Ilex opaca Aiton | Texas, United States | NA | | | 2025 | COLLECTED | 01/13/2025 | Fairmount Township: Sabine National Forest C-139: Foxhunters Hill. | 31.18153000, -93.72368000 | | Baygall below a longleaf pine stand. Same system as 035 [NA 88985]. | Wild material | | 2170968 | NA 88984 |
| 72 | NA 88987 | TXWL2025-037 | Ilex opaca Aiton | Texas, United States | NA | | | 2025 | COLLECTED | 01/13/2025 | Fairmount Township: Sabine National Forest C-139: Foxhunters Hill. | 31.18365000, -93.72211000 | | Baygall below a longleaf pine stand. | Wild material | | 2170971 | NA 88987 |
| 73 | NA 88578 | 2024RJLFL-004 | Ilex vomitoria Aiton | Florida, United States | NA | | | 2024 | COLLECTED | 11/12/2024 | Collected along Florida National Scenic Trail/Eglin Air Force Base unnamed road. | 30.44526100, -86.86094700 | 4 | Mixed evergreen and deciduous forests in part shade to full sun. Slope: 5 to 10 percent. Aspect: Various. The underlying geology of this area is characterized as Citronelle Formation of the Pliocene period. The Citronelle Formation is widespread in the Gulf Coastal Plain. The type section for the Citronelle Formation, named by Matson (1916), is near Citronelle, Alabama. The Citronelle Formation grades laterally, through a broad facies transition, into the Miccosukee Formation of the eastern Florida panhandle. Coe (1979) investigated the Citronelle Formation in portions of the western Florida panhandle. The Citronelle Formation is a siliciclastic, deltaic deposit that is lithologically similar to, and time equivalent with, the Cypresshead Formation and, at least in part, the Long Key Formation (Cunningham et al., 1998) of the peninsula. In the western panhandle, some of the sediments mapped as Citronelle Formation may be reworked Citronelle. The lithologies are the same and there are few fossils present to document a possible younger age. The Citronelle Formation consists of gray to orange, often mottled, unconsolidated to poorly consolidated, very fine to very coarse, poorly sorted, clean to clayey sands. It contains significant amounts of clay, silt and gravel which may occur as beds and lenses and may vary considerably over short distances. Limonite nodules and limonite-cemented beds are common. Marine fossils are rare but fossil pollen, plant remains and occasional vertebrates are found. Much of the Citronelle Formation is highly permeable. It forms the Sand and Gravel Aquifer of the surficial aquifer system contain organics. The dominant fossils in the freshwater carbonates are mollusks. (Source: USGS Florida Geologic Map Data). The soils of this are characterized as Lakeland Series Sand, 5 to 12 percent slopes. The Lakeland series consists of very deep, excessively drained, rapid to very rapidly permeable soils on uplands. They formed in thick beds of eolian or marine and/or fluvio-marine sands in the Southern Coastal Plain MLRA (133A), the Carolina and Georgia Sandhills (MLRA 137), the Eastern Gulf Coast Flatwoods (MLRA 152A) and the Atlantic Coast Flatwoods (MLRA 153A). Slopes are dominantly from 0 to 12 percent but can range to 85 percent in dissected areas. Thickness of the sand exceeds 200 cm. Silt plus clay in the 25 to 100 cm control section ranges from 5 to 10 percent. Reaction ranges from very strongly acid to moderately acid throughout. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). | Wild material | | 2169915 | NA 88578 |
| 74 | NA 88579 | 2024RJLFL-007 | Ilex myrtifolia Walter | Florida, United States | NA | | | 2024 | COLLECTED | 11/13/2024 | Wetlands accessed from Miller Bluff Road. | 30.62251200, -86.86030700 | 8 | Open, wet areas and woodland edge slightly above permanently wet habitat in part shade to full sun. Slope: 0 percent. Aspect: N/A. | Wild material | | 2169916 | NA 88579 |
| 75 | NA 88580 | 2024RJLFL-009 | Ilex myrtifolia Walter | Florida, United States | NA | | | 2024 | COLLECTED | 11/13/2024 | Woodlands on the north side of Fisher Old Mill Road about 0.10 kilometers west of intersection with DOF Y12. | 30.62693800, -86.83962200 | 6 | Mixed evergreen and deciduous moist to wet forest in part shade to full sun. From the associated taxa, this site can be quite wet during the growing season; however, it was dry during this collection time; likely due to extended drought. Slope: 0 percent. Aspect: South. | Wild material | | 2169917 | NA 88580 |
| 76 | NA 88584 | 2024RJLFL-016 | Cornus florida L. | Florida, United States | NA | | | 2024 | COLLECTED | 11/14/2024 | Both sides of Kennedy Bridge Road approximately 0.27 kilometers west of the junction with Hurricane Lake South Entrance Road. | 30.93159700, -86.74928000 | 43 | Mesic to mesic-moist conditions in a mixed and deciduous evergreen forest in part shade. Slope: 5 to 10 percent. Aspect: Various. The underlying geology of this area is characterized as Citronelle Formation of the Pliocene period. The Citronelle Formation is widespread in the Gulf Coastal Plain. The type section for the Citronelle Formation, named by Matson (1916), is near Citronelle, Alabama. The Citronelle Formation grades laterally, through a broad facies transition, into the Miccosukee Formation of the eastern Florida panhandle. Coe (1979) investigated the Citronelle Formation in portions of the western Florida panhandle. The Citronelle Formation is a siliciclastic, deltaic deposit that is lithologically similar to, and time equivalent with, the Cypresshead Formation and, at least in part, the Long Key Formation (Cunningham et al., 1998) of the peninsula. In the western panhandle, some of the sediments mapped as Citronelle Formation may be reworked Citronelle. The lithologies are the same and there are few fossils present to document a possible younger age. The Citronelle Formation consists of gray to orange, often mottled, unconsolidated to poorly consolidated, very fine to very coarse, poorly sorted, clean to clayey sands. It contains significant amounts of clay, silt and gravel which may occur as beds and lenses and may vary considerably over short distances. Limonite nodules and limonite-cemented beds are common. Marine fossils are rare but fossil pollen, plant remains and occasional vertebrates are found. Much of the Citronelle Formation is highly permeable. It forms the Sand and Gravel Aquifer of the surficial aquifer system contain organics. The dominant fossils in the freshwater carbonates are mollusks. (Source: USGS Florida Geologic Map Data). The soils of this are characterized as Dothan Series loamy sand, 5 to 8 percent slopes. The Dothan Series consists of very deep, well drained soils that formed in thick beds of unconsolidated, medium to fine-textured marine sediments. Dothan soils are on interfluves. Slopes range from 0 to 15 percent. The surface 0-33 cm is characterized by sandy-loam, well-drained soils that are strongly acid. From 33-200 cm they are characterized by sandy clay loam soils that are more moisture retentive and strongly acid. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). | Wild material | | 2169921 | NA 88584 |
| 77 | NA 88585 | 2024RJLFL-018 | Rhododendron canescens (Michx.) Sweet | Florida, United States | NA | | | 2024 | COLLECTED | 11/14/2024 | Woodlands in the riparian zone of a headwater spring and wetland leading to Panther Creek. The area is accessed from High Bridge Road by turning south on an unnamed dirt/sand road and driving about 0.27 kilometers to a pond. | 30.90865300, -86.69107200 | 49 | Mostly deciduous woodlands in the riparian zone of a headwater spring and wetland in shade to part shade. Slope: 5 to 8 percent. Aspect: N/A. The underlying geology of this area is characterized as Citronelle Formation of the Pliocene period. The Citronelle Formation is widespread in the Gulf Coastal Plain. The type section for the Citronelle Formation, named by Matson (1916), is near Citronelle, Alabama. The Citronelle Formation grades laterally, through a broad facies transition, into the Miccosukee Formation of the eastern Florida panhandle. Coe (1979) investigated the Citronelle Formation in portions of the western Florida panhandle. The Citronelle Formation is a siliciclastic, deltaic deposit that is lithologically similar to, and time equivalent with, the Cypresshead Formation and, at least in part, the Long Key Formation (Cunningham et al., 1998) of the peninsula. In the western panhandle, some of the sediments mapped as Citronelle Formation may be reworked Citronelle. The lithologies are the same and there are few fossils present to document a possible younger age. The Citronelle Formation consists of gray to orange, often mottled, unconsolidated to poorly consolidated, very fine to very coarse, poorly sorted, clean to clayey sands. It contains significant amounts of clay, silt and gravel which may occur as beds and lenses and may vary considerably over short distances. Limonite nodules and limonite-cemented beds are common. Marine fossils are rare but fossil pollen, plant remains and occasional vertebrates are found. Much of the Citronelle Formation is highly permeable. It forms the Sand and Gravel Aquifer of the surficial aquifer system contain organics. The dominant fossils in the freshwater carbonates are mollusks. (Source: USGS Florida Geologic Map Data). The surface soil profile is classified as Troup-Orangeburg-Cowarts complex, 5 to 12 percent slopes. The Troup series consists of very deep, somewhat excessively drained soils formed in unconsolidated sandy and loamy marine sediments. Troup soils are found on ridges and hillslopes. The Orangeburg series consists of very deep, well drained, moderately permeable soils on uplands of the Southern Coastal Plain. They formed in loamy and clayey marine sediments. The Cowarts series consists of very deep, moderately well and well drained soils on ridge tops and side slopes on uplands of the Coastal Plain Major Land Resource Area. They formed in loamy marine sediments. The reaction of all these soils ranges from very strongly acid to strongly acid. (Source: USDA-NRCS Official Soil Series Descriptions). | Wild material | | 2169922 | NA 88585 |
| 78 | NA 88589 | 2024RM-002 | Lyonia ferruginea (Walter) Nutt. | Florida, United States | NA | | | 2024 | COLLECTED | 11/21/2024 | Eglin Air Force Base: collected along an unnamed sand road that leads to the former Flowers Boat Landing (now permanently closed) along the Yellow River. Accessed by boat. | 30.60823600, -86.83595500 | 6 | Mixed evergreen and deciduous open habitat in part shade to full sun. Slope: 0 to 1 percent. Aspect: N/A. The underlying geology of this area is characterized as Alluvium from undifferentiated Quaternary Sediments. Much of Florida's surface is covered by a varying thickness of undifferentiated sediments consisting of siliciclastics, organics and freshwater carbonates. Where these sediments exceed 20 feet (6.1 meters) thick, they were mapped as discrete units. To subdivide the undifferentiated sediments, those sediments occurring in flood plains were mapped as alluvial and flood plain deposits (Qal). Sediments showing surficial expression of beach ridges and dunes were mapped separately (Qbd) as were the sediments composing Trail Ridge (Qtr). Terrace sands were not mapped (refer to Healy [1975] for a discussion of the terraces in Florida). The subdivisions of the Undifferentiated Quaternary Sediments (Qu) are not lithostratigraphic units but are utilized to facilitate a better understanding of the State's geology. The siliciclastics are light gray, tan, brown to black, unconsolidated to poorly consolidated, clean to clayey, silty, unfossiliferous, variably organic-bearing sands to blue green to olive green, poorly to moderately consolidated, sandy, silty clays. Gravel is occasionally present in the panhandle. Organics occur as plant debris, roots, disseminated organic matrix and beds of peat. Freshwater carbonates, often referred to as marls in the literature, are scattered over much of the State. In southern Florida, freshwater carbonates are nearly ubiquitous in the Everglades. These sediments are buff colored to tan, unconsolidated to poorly consolidated, fossiliferous carbonate muds. Sand, silt and clay may be present in limited quantities. These carbonates often contain organics. The dominant fossils in the freshwater carbonates are mollusks. (Source: USGS Florida Geologic Map Data). The soils of this are characterized as Dorovan-Pamlico Series association. The Dorovan Series consists of very deep, very poorly drained, moderately permeable soils on densely forested flood plains, hardwood swamps, and depressions in the Atlantic Coast Flatwoods (153A), Eastern Gulf Coast Flatwoods (152A), and Southern Coastal Plain Major (133A) Land Resource Areas. They formed in highly decomposed acid-organic materials. Slopes are less than 1 percent. The organic material ranges from 1.3 to 2 meters or more thick. Reaction is extremely acid to very strongly acid in the organic layers and very strongly acid or strongly acid in the mineral layers. The Pamlico Series consists of very poorly drained soils that formed in decomposed organic material underlain by dominantly sandy sediment. The soils are on nearly level flood plains, bays, and depressions of the Coastal Plain. Slopes are less than 1 percent. Pamlico soils have 0.4 to 1.3 meters of organic material over dominantly sandy sediments. Reaction is extremely acid (less than 4.5 in 0.01 M calcium chloride) in the organic layers, and ranges from extremely acid to strongly acid in the underlying mineral layers. | Wild material | | 2169926 | NA 88589 |
| 79 | NA 88590 | 2024RM-003 | Ilex verticillata (L.) A. Gray | Florida, United States | NA | | | 2024 | COLLECTED | 11/21/2024 | Along the west/north side of the Yellow River about 0.33 kilometers (as the crow flies) upstream from the channel that leads the Fisher Old Mill Road Boat Ramp. This site was accessed by boat. | 30.62868600, -86.80748000 | 4 | Plants are found growing primarily in permanently saturated to submersed conditions along the edge of the Yellow River in part shade. The riverine habitat is comprised of a wide array of deciduous and evergreen trees, shrubs, and perennial plant species. Most of the plants along the river are adapted to acidic conditions and, while the aquatic habitat is generally fresh water, there is occasionally tidal or hurricane-caused saltwater intrusions. Slope: 0 percent. Aspect: East-southeast. The underlying geology of this area is characterized as Alluvium from undifferentiated Quaternary Sediments. Much of Florida's surface is covered by a varying thickness of undifferentiated sediments consisting of siliciclastics, organics and freshwater carbonates. Where these sediments exceed 20 feet (6.1 meters) thick, they were mapped as discrete units. To subdivide the undifferentiated sediments, those sediments occurring in flood plains were mapped as alluvial and flood plain deposits (Qal). Sediments showing surficial expression of beach ridges and dunes were mapped separately (Qbd) as were the sediments composing Trail Ridge (Qtr). Terrace sands were not mapped (refer to Healy [1975] for a discussion of the terraces in Florida). The subdivisions of the Undifferentiated Quaternary Sediments (Qu) are not lithostratigraphic units but are utilized to facilitate a better understanding of the State's geology. The siliciclastics are light gray, tan, brown to black, unconsolidated to poorly consolidated, clean to clayey, silty, unfossiliferous, variably organic-bearing sands to blue green to olive green, poorly to moderately consolidated, sandy, silty clays. Gravel is occasionally present in the panhandle. Organics occur as plant debris, roots, disseminated organic matrix and beds of peat. Freshwater carbonates, often referred to as marls in the literature, are scattered over much of the State. In southern Florida, freshwater carbonates are nearly ubiquitous in the Everglades. These sediments are buff colored to tan, unconsolidated to poorly consolidated, fossiliferous carbonate muds. Sand, silt and clay may be present in limited quantities. These carbonates often contain organics. The dominant fossils in the freshwater carbonates are mollusks. (Source: USGS Florida Geologic Map Data). The soils of this are characterized as Bibb-Kinston Series association. The Bibb Series consists of very deep, poorly drained, moderately permeable soils on flood plains of streams in the Southern Coastal Plain (133A) Major Land Resource Area. They formed in stratified loamy and sandy alluvium that are commonly and frequently flooded and water runs off the surface very slowly. Slopes range from 0 to 2 percent. Reaction ranges from extremely acid to strongly acid throughout. Content of mica flakes ranges from none to common. Content of rounded gravel typically ranges from 0 to 10 percent throughout, but may range to 50 percent in thin strata below a depth of 1 meter. Buried soil horizons, present in many pedons have the same range in color and texture as the surface horizon which has iron and organic matter concentrations in shades of brown and yellow ranging from none to common. Texture is sand, loamy sand, loamy fine sand, fine sandy loam, sandy loam, loam or silt loam. The Kinston Series consists of very deep, poorly drained, moderately permeable soils found on flood plains. They were formed in alluvial depositions. Slopes range from 0 to 2 percent. Soil reaction ranges from strongly acid to very strongly acid. Typical texture across the pedons is loamy, gravelly loam, sandy loam, and clay loam with dark concretions often present. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). | Wild material | | 2169927 | NA 88590 |
| 80 | NA 88591 | 2024RM-004 | Ilex opaca Aiton | Florida, United States | NA | | | 2024 | COLLECTED | 11/21/2024 | Along the west/north side of the Yellow River about 5.5 kilometers upstream from the State Highway 87 boat ramp. This site was accessed by boat. | 30.59986000, -86.87936000 | 2 | Plants are found growing primarily in permanently saturated to submersed conditions along the edge of the Yellow River in part shade. The riverine habitat is comprised of a wide array of deciduous and evergreen trees, shrubs, and perennial plant species. Most of the plants along the river are adapted to acidic conditions and, while the aquatic habitat is generally fresh water, there is occasionally tidal or hurricane-caused saltwater intrusions. Slope: 0 percent. Aspect: East-southeast. The underlying geology of this area is characterized as Alluvium from undifferentiated Quaternary Sediments. Much of Florida's surface is covered by a varying thickness of undifferentiated sediments consisting of siliciclastics, organics and freshwater carbonates. Where these sediments exceed 20 feet (6.1 meters) thick, they were mapped as discrete units. To subdivide the undifferentiated sediments, those sediments occurring in flood plains were mapped as alluvial and flood plain deposits (Qal). Sediments showing surficial expression of beach ridges and dunes were mapped separately (Qbd) as were the sediments composing Trail Ridge (Qtr). Terrace sands were not mapped (refer to Healy [1975] for a discussion of the terraces in Florida). The subdivisions of the Undifferentiated Quaternary Sediments (Qu) are not lithostratigraphic units but are utilized to facilitate a better understanding of the State's geology. The siliciclastics are light gray, tan, brown to black, unconsolidated to poorly consolidated, clean to clayey, silty, unfossiliferous, variably organic-bearing sands to blue green to olive green, poorly to moderately consolidated, sandy, silty clays. Gravel is occasionally present in the panhandle. Organics occur as plant debris, roots, disseminated organic matrix and beds of peat. Freshwater carbonates, often referred to as marls in the literature, are scattered over much of the State. In southern Florida, freshwater carbonates are nearly ubiquitous in the Everglades. These sediments are buff colored to tan, unconsolidated to poorly consolidated, fossiliferous carbonate muds. Sand, silt and clay may be present in limited quantities. These carbonates often contain organics. The dominant fossils in the freshwater carbonates are mollusks. (Source: USGS Florida Geologic Map Data). The soils of this are characterized as Bibb-Kinston Series association. The Bibb Series consists of very deep, poorly drained, moderately permeable soils on flood plains of streams in the Southern Coastal Plain (133A) Major Land Resource Area. They formed in stratified loamy and sandy alluvium that are commonly and frequently flooded and water runs off the surface very slowly. Slopes range from 0 to 2 percent. Reaction ranges from extremely acid to strongly acid throughout. Content of mica flakes ranges from none to common. Content of rounded gravel typically ranges from 0 to 10 percent throughout, but may range to 50 percent in thin strata below a depth of 1 meter. Buried soil horizons, present in many pedons have the same range in color and texture as the surface horizon which has iron and organic matter concentrations in shades of brown and yellow ranging from none to common. Texture is sand, loamy sand, loamy fine sand, fine sandy loam, sandy loam, loam or silt loam. The Kinston Series consists of very deep, poorly drained, moderately permeable soils found on flood plains. They were formed in alluvial depositions. Slopes range from 0 to 2 percent. Soil reaction ranges from strongly acid to very strongly acid. Typical texture across the pedons is loamy, gravelly loam, sandy loam, and clay loam with dark concretions often present. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). | Wild material | | 2169928 | NA 88591 |
| 81 | NA 88592 | 2024RM-005 | Ilex sp. | Florida, United States | NA | | | 2024 | COLLECTED | 11/21/2024 | Along the west/north side of the Yellow River about 1.1 kilometers upstream from the State Highway 87 boat ramp. This site was accessed by boat. | 30.57956000, -86.91916400 | 1 | Plants are found growing primarily in permanently saturated to submersed conditions along the edge of the Yellow River in part shade. The riverine habitat is comprised of a wide array of deciduous and evergreen trees, shrubs, and perennial plant species. Most of the plants along the river are adapted to acidic conditions and, while the aquatic habitat is generally fresh water, there is occasionally tidal or hurricane-caused saltwater intrusions. Slope: 0 percent. Aspect: North. The underlying geology of this area is characterized as Alluvium from undifferentiated Quaternary Sediments. Much of Florida's surface is covered by a varying thickness of undifferentiated sediments consisting of siliciclastics, organics and freshwater carbonates. Where these sediments exceed 20 feet (6.1 meters) thick, they were mapped as discrete units. To subdivide the undifferentiated sediments, those sediments occurring in flood plains were mapped as alluvial and flood plain deposits (Qal). Sediments showing surficial expression of beach ridges and dunes were mapped separately (Qbd) as were the sediments composing Trail Ridge (Qtr). Terrace sands were not mapped (refer to Healy [1975] for a discussion of the terraces in Florida). The subdivisions of the Undifferentiated Quaternary Sediments (Qu) are not lithostratigraphic units but are utilized to facilitate a better understanding of the State's geology. The siliciclastics are light gray, tan, brown to black, unconsolidated to poorly consolidated, clean to clayey, silty, unfossiliferous, variably organic-bearing sands to blue green to olive green, poorly to moderately consolidated, sandy, silty clays. Gravel is occasionally present in the panhandle. Organics occur as plant debris, roots, disseminated organic matrix and beds of peat. Freshwater carbonates, often referred to as marls in the literature, are scattered over much of the State. In southern Florida, freshwater carbonates are nearly ubiquitous in the Everglades. These sediments are buff colored to tan, unconsolidated to poorly consolidated, fossiliferous carbonate muds. Sand, silt and clay may be present in limited quantities. These carbonates often contain organics. The dominant fossils in the freshwater carbonates are mollusks. (Source: USGS Florida Geologic Map Data). The soils of this are characterized as Bibb-Kinston Series association. The Bibb Series consists of very deep, poorly drained, moderately permeable soils on flood plains of streams in the Southern Coastal Plain (133A) Major Land Resource Area. They formed in stratified loamy and sandy alluvium that are commonly and frequently flooded and water runs off the surface very slowly. Slopes range from 0 to 2 percent. Reaction ranges from extremely acid to strongly acid throughout. Content of mica flakes ranges from none to common. Content of rounded gravel typically ranges from 0 to 10 percent throughout, but may range to 50 percent in thin strata below a depth of 1 meter. Buried soil horizons, present in many pedons have the same range in color and texture as the surface horizon which has iron and organic matter concentrations in shades of brown and yellow ranging from none to common. Texture is sand, loamy sand, loamy fine sand, fine sandy loam, sandy loam, loam or silt loam. The Kinston Series consists of very deep, poorly drained, moderately permeable soils found on flood plains. They were formed in alluvial depositions. Slopes range from 0 to 2 percent. Soil reaction ranges from strongly acid to very strongly acid. Typical texture across the pedons is loamy, gravelly loam, sandy loam, and clay loam with dark concretions often present. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). | Wild material | | 2169929 | NA 88592 |
| 82 | NA 88593 | 2024RJLNJ-001 | Ilex glabra (L.) A. Gray | New Jersey, United States | NA | | | 2024 | COLLECTED | 11/24/2024 | Mullica Township: Both sides of Duerer Street, approximately 0.37 kilometers southeast of 4th Avenue. | 39.55885000, -74.66442500 | 21 | Shade to almost full sun on compacted seasonally moist to temporarily wet areas of a mixed evergreen and deciduous woodland dominated by Pinus rigida. Vegetation of this area is very much defined by small changes in elevation that go from wet to very dry. Ilex glabra remains abundant throughout, though. Slope: N/A. Aspect: N/A. The underlying geology of this area is the Cohansey Formation of middle Miocene origin and comprised of sand, white to yellow with local gravel and clay. It is sometimes locally stained red or orange brown by iron oxides and (or) cemented into large blocks of ironstone. Unweathered clay is typically dark gray, but commonly weathers white where it is interbedded with thin beds of ironstone. Sand is typically medium grained and moderately sorted although it ranges from fine to very coarse grained and from poorly to well sorted. Sand consists of quartz and siliceous rock fragments. Some beds are locally micaceous. Maximum thickness in the map area is about 60 meters; however, thickness is difficult to determine because of the irregular basal contact and extensive post-depositional erosion. (Source: USGS New Jersey Geologic Map Data). The primary soil type in the area of this collection is classified as Mullica Series sandy loam, 0 to 2 percent slopes. These soils are typically coarse-loamy, siliceous, semiactive, and mesic typic humaquepts that are strongly to extremely acidic throughout the profile. The typical solum thickness ranges from 50-150+ cm. These soils are generally considered to be poorly drained. (Source: NRCS Web Soil Survey). | Wild material | | 2169930 | NA 88593 |
| 83 | NA 88731 | RonMiller2022-Old Land Place | Gordonia lasianthus (L.) J. Ellis | Florida, United States | NA | | | 2024 | COLLECTED | 04/2022 | Yellow River Marsh State Aquatic Preserve, "Old Land Place" along Weaver River, 1.47 miles south of the confluence with the Yellow River. | 30.55318000, -87.93656000 | 3 | Moist to wet areas in wetland adjacent to the river in association with a range of evergreen and deciduous forest elements. | Wild material | From open-pollinated, but presumed isolated, seeds of NA 87342-H, -J, and -L (three young plants flowering in containers in production during 2024). Seed was harvested over a period roughly from October through December 2024 as fruits matured. From the record of the parent accession, NA 87342: Exact date of collection unknown. | 2170992 | NA 88731 |
| 84 | NA 88479 | TXWL2024-029 | Ilex longipes Chapm. ex Trel. | Texas, United States | NA | | | 2024 | COLLECTED | 11/20/2024 | Little Cow Creek. | 31.06221000, -93.79603000 | | Upland position above perennial creek. | Wild material | | 2169906 | NA 88479 |
| 85 | NA 87844 | TRX241118-02GA | Ilex cassine L. | Georgia, United States | NA | | | 2024 | COLLECTED | 11/18/2024 | St. Simons Island: Frederica Park. | 31.23766000, -81.35638000 | 6 | | Wild material | | 2169897 | NA 87844 |
| 86 | NA 87845 | TRX241119-01GA | Ilex coriacea (Pursh) Chapm. | Georgia, United States | NA | | | 2024 | COLLECTED | 11/19/2024 | St. Simons Island: Guale Preserve. | 31.21861000, -81.36872000 | 6 | | Wild material | | 2169898 | NA 87845 |
| 87 | NA 89075 | 2024RJLPA-001 | Rhododendron maximum L. | Pennsylvania, United States | NA | | | 2024 | COLLECTED | 09/18/2024 | Fieldstone Farm Tank Creek Nature Preserve (a property of the Pocono Heritage Land Trust): Collected along Tank Creek. The property is accessed from a parking area located on Devil's Hole Road. | 41.13862300, -75.34562700 | 493 | Mostly found in mixed deciduous forest with occasional conifers and evergreen shrubs generally on steep slopes above Tank Creek in rocky well-drained soils in shade to part-shade. The slopes are abundant in decomposed organic matter and runoff soils. Slope: 5 to 30 percent. Aspect: various. Geology: The underlying geology of this area is of Devonian origin and characterized as the Long Run Member of Catskill Formation. It is comprised of gray and grayish-red sandstone and grayish-red siltstone and mudstone in fining-upward cycles. (Source: USGS Pennsylvania Geologic Map Data). Soils: The primary soil type found here is classified as Alluvial Land. In geology, alluvial land refers to areas of land that are formed by the deposition of sediments carried by rivers, or other surface water. EPA Ecoregion (Level III): North Central Appalachians (62). EPA Ecoregion (Level IV): Low Poconos (62b). | Wild material | | 2169039 | NA 89075 |
| 88 | NA 89076 | 2024RJLPA-002 | Kalmia latifolia L. | Pennsylvania, United States | NA | | | 2024 | COLLECTED | 09/18/2024 | Fieldstone Farm Tank Creek Nature Preserve (a property of the Pocono Heritage Land Trust): Collected along Tank Creek. The property is accessed from a parking area located on Devil's Hole Road. | 41.13862300, -75.34562700 | 493 | Mostly found in mixed deciduous forest with occasional conifers and evergreen shrubs generally on sloping sites as an understory shrub in rocky well-drained soils in shade to part-shade. Slope: 5 to 15 percent. Aspect: various. Geology: The underlying geology of this area is of Devonian origin and characterized as the Long Run Member of Catskill Formation. It is comprised of gray and grayish-red sandstone and grayish-red siltstone and mudstone in fining-upward cycles. (Source: USGS Pennsylvania Geologic Map Data). Soils: The primary soil type found here is classified as Alluvial Land. In geology, alluvial land refers to areas of land that are formed by the deposition of sediments carried by rivers, or other surface water. EPA Ecoregion (Level III): North Central Appalachians (62). EPA Ecoregion (Level IV): Low Poconos (62b). | Wild material | | 2169040 | NA 89076 |
| 89 | NA 89077 | 2024RJLPA-003 | Viburnum acerifolium L. | Pennsylvania, United States | NA | | | 2024 | COLLECTED | 09/19/2024 | Birdell Road, near parking lot to trail where the road ends at Chambers Lake, which is part of Hibernia County Park. | 40.03559500, -75.85708600 | 187 | Plants are growing in deep shade of a dry deciduous forest dominated by Fagus grandifolia. Slope: 0 percent. Aspect: N/A. Geology: The underlying geology of this area is of Precambrian origin and characterized as Banded Mafic Gneiss. It is characterized as dark and fine to medium grained. This formation includes rocks of probable sedimentary origin; may be equivalent to "PZmgh." (Source: USGS Pennsylvania Geologic Map Data). Soils: The primary soil type in the area of this collection is classified as Neshaminy Series Silt Loam, very deep over mafic gneiss, 3 to 8 percent slopes (NvB). (Source: USDA-NRCS Official Soil Series Descriptions). EPA Ecoregion (Level III): Northern Piedmont (64). EPA Ecoregion (Level IV): Piedmont Uplands (64c). | Wild material | | 2169041 | NA 89077 |
| 90 | NA 89078 | 2024RJLPA-004 | Staphylea trifolia L. | Pennsylvania, United States | NA | | | 2024 | COLLECTED | 09/20/2024 | Along gated road about 0.33 kilometers southwest of the Lake Ontelaunee Trail parking lot. | 40.49850800, -75.89121300 | 94 | Plants are growing on well-drained steep slopes in shade to part shade of a deciduous forest. Slope: 35 to 50 percent. Aspect: East-southeast. Geology: The underlying geology of this area is of Ordovician origin and characterized as Shale and graywacke of Hamburg sequence. It is characterized by shale containing zones of conspicuous graywacke. (Source: USGS Pennsylvania Geologic Map Data). Soils: The primary soil type in the area of this collection is classified as Berks-Weikert Complex, 25 to 60% slopes (BkF). Dominantly sloping to very steep, moderately deep and shallow, well drained soils underlain by acid shale bedrock. (Source: UPenn State University Soil Info Website). EPA Ecoregion (Level III): Ridge and Valley (67). EPA Ecoregion (Level IV): Northern Shale Valleys (67b). | Wild material | | 2169042 | NA 89078 |
| 91 | NA 89080 | 2024RJLPA-006 | Ilex montana Torr. & A. Gray | Pennsylvania, United States | NA | | | 2024 | COLLECTED | 09/20/2024 | Berks and Schuylkill Counties: Hawk Mountain Sanctuary. | 40.64162200, -75.99122600 | 418 | Plants are growing from shade to full sun on a dry-mesic to very dry, well-drained upland/montane habitat characterized by an upland mixed deciduous and evergreen forest that is very rocky. All the plants found in this habitat go through periods of drought during the growing season due to the limited litter/soil layer in which moisture can be held. Elevation: 405 to 430 meters. Slope: 5 to 25 percent. Aspect: various. Geology: The underlying geology of this area is of Silurian origin and comprised of Shawangunk Formation. This formation is primarily light- to dark-gray, fine- to very coarse-grained sandstone and conglomerate containing thin shale interbeds. (Source: USGS Pennsylvania Geologic Map Data). Soils: The surface soil profile of this area is characterized as the Hazleton Series which consists of deep and very deep, well drained soils formed in residuum of acid gray, brown or red sandstone on uplands. The matrix includes a considerable accumulation of thin, flat, coarse fragments of sandstone, limestone, or schist with diameters up to 15 cm. Slope ranges from 0-80%. Permeability is moderately rapid to rapid. (Source: USDA-NRCS Official Soil Series Descriptions). EPA Ecoregion (Level III): Ridge and Valley (67). EPA Ecoregion (Level IV): Northern Sandstone Ridges (67c). | Wild material | | 2169044 | NA 89080 |
| 92 | NA 89081 | 2024RJLPA-009 | Rosa carolina L. | Pennsylvania, United States | NA | | | 2024 | COLLECTED | 09/22/2024 | Lancaster and York Counties: outcrops along the Susquehanna River, accessed from the Historic Lock 12 parking lot off of Pennsylvania Road 372. | 39.81483500, -76.32762200 | 34 | Plants are growing from part-sun to full sun in crevices of the outcrops and where organic debris has accumulated in between boulders along the Susquehanna River. The sites range from nearly xeric to dry mesic, at least on the surface. Plants are generally growing 4-10 m above the normal flow of the river; however, the Holtwood Dam is less than 1 kilometer upstream and debris found trapped in the boulders indicates that there is periodic flooding, at least, in the lower zone of 4+ meters or so above normal river flow. This habitat has a diverse assemblage of deciduous trees and shrubs as well as abundant herbaceous taxa. Slope: 0 to 60 percent. Aspect: Northeast (generally). Geology: The underlying geology of this area is probably of lower Paleozoic age and characterized as the Octoraro Formation. It includes albite-chlorite schist, phyllite, some hornblende gneiss, and granitized members. Soils: The area where this species occurs is right on the edge of two soil zones that transition from the river’s edge to mesic conditions upslope. The first is generally referred to as Rock Outcrop. This terrestrial matrix in which plants grow is largely exposed underlying rock geology with accumulated outwash, rock decomposition, and organic debris buildup. The second is Mt. Airy (80%) and Manor (20%) Series soils, 25 to 60 percent slopes, extremely stony (MRF). (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). EPA Ecoregion (Level III): Northern Piedmont (64). EPA Ecoregion (Level IV): Piedmont Uplands (64c). | Wild material | | 2169045 | NA 89081 |
| 93 | NA 89082 | 2024RJLPA-010 | Amorpha fruticosa L. | Pennsylvania, United States | NA | | | 2024 | COLLECTED | 09/22/2024 | Outcrops along the Susquehanna River, accessed from the Historic Lock 12 parking lot off of Pennsylvania Road 372. | 39.81481500, -76.32757900 | 34 | Plants are growing from part-sun to full sun in crevices of the outcrops and where organic debris has accumulated in between boulders along the Susquehanna River. The sites range from nearly xeric to dry mesic, at least on the surface. Plants are generally growing 4-10 m above the normal flow of the river; however, the Holtwood Dam is less than 1 kilometer upstream and debris found trapped in the boulders indicates that there is periodic flooding, at least, in the lower zone of 4+ meters or so above normal river flow. This habitat has a diverse assemblage of deciduous trees and shrubs as well as abundant herbaceous taxa. Slope: 0 to 25 percent. Aspect: Northeast (generally). Geology: The underlying geology of this area is probably of lower Paleozoic age and characterized as the Octoraro Formation. It includes albite-chlorite schist, phyllite, some hornblende gneiss, and granitized members. Soils: The area where this species occurs is right on the edge of two soil zones that transition from the river’s edge to mesic conditions upslope. The first is generally referred to as Rock Outcrop. This terrestrial matrix in which plants grow is largely exposed underlying rock geology with accumulated outwash, rock decomposition, and organic debris buildup. The second is Mt. Airy (80%) and Manor (20%) Series soils, 25 to 60 percent slopes, extremely stony (MRF). (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). EPA Ecoregion (Level III): Northern Piedmont (64). EPA Ecoregion (Level IV): Piedmont Uplands (64c). | Wild material | | 2169046 | NA 89082 |
| 94 | NA 89083 | 2024RJLPA-012 | Rhododendron periclymenoides (Michx.) Shinners | Pennsylvania, United States | NA | | | 2024 | COLLECTED | 09/22/2024 | Outcrops along the Susquehanna River, accessed from the Historic Lock 12 parking lot off of Pennsylvania Road 372. | 39.81477400, -76.32807300 | 35 | Plants are growing from shade to part-sun and occasionally full sun in crevices of the outcrops and where organic debris has accumulated in between boulders along the Susquehanna River. The sites range from nearly xeric to mesic, at least on the surface. Plants are generally growing 4-10 m above the normal flow of the river; however, the Holtwood Dam is less than 1 kilometer upstream and debris found trapped in the boulders indicates that there is periodic flooding, at least, in the lower zone of 4+ meters or so above normal river flow. This habitat has a diverse assemblage of deciduous trees and shrubs as well as abundant herbaceous taxa. Slope: 0 to 60 percent. Aspect: Northeast (generally). Geology: The underlying geology of this area is probably of lower Paleozoic age and characterized as the Octoraro Formation. It includes albite-chlorite schist, phyllite, some hornblende gneiss, and granitized members. Soils: The area where this species occurs is right on the edge of two soil zones that transition from the river’s edge to mesic conditions upslope. The first is generally referred to as Rock Outcrop. This terrestrial matrix in which plants grow is largely exposed underlying rock geology with accumulated outwash, rock decomposition, and organic debris buildup. The second is Mt. Airy (80%) and Manor (20%) Series soils, 25 to 60 percent slopes, extremely stony (MRF). (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). EPA Ecoregion (Level III): Northern Piedmont (64). EPA Ecoregion (Level IV): Piedmont Uplands (64c). | Wild material | | 2169047 | NA 89083 |
| 95 | NA 89084 | 2024RJLPA-013 | Physocarpus opulifolius (L.) Maxim. | Pennsylvania, United States | NA | | | 2024 | COLLECTED | 09/22/2024 | Outcrops along the Susquehanna River, accessed from the Historic Lock 12 parking lot off of Pennsylvania Road 372. | 39.81466300, -76.32833900 | 36 | Plants are growing from shade to part-sun where organic debris has accumulated in between boulders as well as further upslope in deeper mesic soils along the Susquehanna River. This habitat has a diverse assemblage of deciduous trees and shrubs as well as abundant herbaceous taxa. Slope: 10 to 25 percent. Aspect: Northeast (generally). Geology: The underlying geology of this area is probably of lower Paleozoic age and characterized as the Octoraro Formation. It includes albite-chlorite schist, phyllite, some hornblende gneiss, and granitized members. Soils: The area where this species occurs is right on the edge of two soil zones that transition from the river’s edge to mesic conditions upslope. The first is generally referred to as Rock Outcrop. This terrestrial matrix in which plants grow is largely exposed underlying rock geology with accumulated outwash, rock decomposition, and organic debris buildup. The second is Mt. Airy (80%) and Manor (20%) Series soils, 25 to 60 percent slopes, extremely stony (MRF). (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). EPA Ecoregion (Level III): Northern Piedmont (64). EPA Ecoregion (Level IV): Piedmont Uplands (64c). | Wild material | | 2169048 | NA 89084 |
| 96 | NA 89085 | 2024RJLPA-014 | Rhododendron arborescens (Pursh) Torr. | Pennsylvania, United States | NA | | | 2024 | COLLECTED | 09/22/2024 | Outcrops along the Susquehanna River, accessed from the Historic Lock 12 parking lot off of Pennsylvania Road 372. | 39.81618100, -76.33069800 | 38 | Plants are growing from shade to part-sun and occasionally full sun in crevices of the outcrops and where organic debris has accumulated in between boulders along the Susquehanna River. The sites range from nearly xeric to mesic, at least on the surface. Plants are generally growing 4-10 m above the normal flow of the river; however, the Holtwood Dam is less than 1 kilometer upstream and debris found trapped in the boulders indicates that there is periodic flooding, at least, in the lower zone of 4+ meters or so above normal river flow. This habitat has a diverse assemblage of deciduous trees and shrubs as well as abundant herbaceous taxa. Slope: 0 to 75 percent. Aspect: Northeast (generally). Geology: The underlying geology of this area is probably of lower Paleozoic age and characterized as the Octoraro Formation. It includes albite-chlorite schist, phyllite, some hornblende gneiss, and granitized members. Soils: The area where this species occurs is right on the edge of two soil zones that transition from the river’s edge to mesic conditions upslope. The first is generally referred to as Rock Outcrop. This terrestrial matrix in which plants grow is largely exposed underlying rock geology with accumulated outwash, rock decomposition, and organic debris buildup. The second is Mt. Airy (80%) and Manor (20%) Series soils, 25 to 60 percent slopes, extremely stony (MRF). (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). EPA Ecoregion (Level III): Northern Piedmont (64). EPA Ecoregion (Level IV): Piedmont Uplands (64c). | Wild material | | 2169049 | NA 89085 |
| 97 | NA 89086 | 2024RJLPA-015 | Ilex verticillata (L.) A. Gray | Pennsylvania, United States | NA | | | 2024 | COLLECTED | 09/22/2024 | Outcrops along the Susquehanna River, accessed from the Historic Lock 12 parking lot off of Pennsylvania Road 372. | 39.81656600, -76.33136600 | 38 | Plants are growing from part-sun to full sun in crevices of the outcrops and where organic debris has accumulated in between boulders along the Susquehanna River. The sites range from nearly xeric to dry mesic, at least on the surface. Plants are generally growing 4-10 m above the normal flow of the river; however, the Holtwood Dam is less than 1 kilometer upstream and debris found trapped in the boulders indicates that there is periodic flooding, at least, in the lower zone of 4+ meters or so above normal river flow. This habitat has a diverse assemblage of deciduous trees and shrubs as well as abundant herbaceous taxa. Slope: 0 to 10 percent. Aspect: Northeast (generally). Geology: The underlying geology of this area is probably of lower Paleozoic age and characterized as the Octoraro Formation. It includes albite-chlorite schist, phyllite, some hornblende gneiss, and granitized members. Soils: The area where this species occurs is right on the edge of two soil zones that transition from the river’s edge to mesic conditions upslope. The first is generally referred to as Rock Outcrop. This terrestrial matrix in which plants grow is largely exposed underlying rock geology with accumulated outwash, rock decomposition, and organic debris buildup. The second is Mt. Airy (80%) and Manor (20%) Series soils, 25 to 60 percent slopes, extremely stony (MRF). (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). EPA Ecoregion (Level III): Northern Piedmont (64). EPA Ecoregion (Level IV): Piedmont Uplands (64c). | Wild material | | 2169050 | NA 89086 |
| 98 | NA 89087 | 2024RJLPA-016 | Hydrangea arborescens L. | Pennsylvania, United States | NA | | | 2024 | COLLECTED | 09/22/2024 | Outcrops along the Susquehanna River, accessed from the Historic Lock 12 parking lot off of Pennsylvania Road 372. | 39.81489000, -76.32912200 | 43 | Plants are growing in deep shade of the deciduous woodlands on outcrops and the steep slopes where organic debris and detritus has accumulated. This habitat has a diverse assemblage of deciduous trees and shrubs as well as abundant herbaceous taxa. Slope: 30 to 90 percent. Aspect: Northeast (generally). Geology: The underlying geology of this area is probably of lower Paleozoic age and characterized as the Octoraro Formation. It includes albite-chlorite schist, phyllite, some hornblende gneiss, and granitized members. (Source: Source: USGS Pennsylvania Geologic Map Data). Soils: The area where this species occurs is right on the edge of two soil zones that transition from the river’s edge to mesic conditions upslope. The first is generally referred to as Rock Outcrop. This terrestrial matrix in which plants grow is largely exposed underlying rock geology with accumulated outwash, rock decomposition, and organic debris buildup. The second is Mt. Airy (80%) and Manor (20%) Series soils, 25 to 60 percent slopes, extremely stony (MRF). (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). EPA Ecoregion (Level III): Northern Piedmont (64). EPA Ecoregion (Level IV): Piedmont Uplands (64c). | Wild material | | 2169051 | NA 89087 |
| 99 | NA 89088 | 2024RM-TK-001 | Viburnum acerifolium L. | Alabama, United States | NA | | | 2024 | COLLECTED | 09/19/2024 | Haines Island Park. Follow Ferry Road to the top of the hill entering the park where a picnic shelter is located. Plants are growing along trails to the north of the picnic shelter. | 31.72132026, -87.46408910 | 81 | Plants are growing from part-sun to full shade in the understory of a mixed deciduous and coniferous forest on very dry upland habitat. Slope: 10 to 20 percent. Aspect: North. Geology: The underlying geology of this area is probably of Eocene age and characterized as the Claiborne Group: Tallahatta Formation. It is comprised of white to very light-greenish-gray thin-bedded to massive siliceous claystone; interbedded with thin layers of fossiliferous clay, sandy clay, and glauconitic sand and sandstone. White to light-greenish-gray fine to coarse sand and fine gravel occur at the base of the formation in southwest Alabama (Meridian Sand Member). (Source: USGS Alabama Geologic Map Data). Soils: The area of this occurrence is characterized as Arundel Series Loam, 8 to 35 percent slopes (ArF). The Arundel series consists of moderately deep, well drained, very slowly permeable soils on dissected uplands of the Southern Coastal Plain Major Land Resource Area (MLRA 133A). They formed in marine deposits consisting of acid clays underlain by horizontally bedded sandstone, buhrstone and siltstone. Slopes range from 2 to 60 percent. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). EPA Ecoregion (Level III): Southeastern Plains (65). EPA Ecoregion (Level IV): Buhrstone/Lime Hills (65q). | Wild material | | 2169052 | NA 89088 |
| 100 | NA 89089 | 2024RM-TK-002 | Viburnum acerifolium L. | Alabama, United States | NA | | | 2024 | COLLECTED | 09/19/2024 | Woodland slopes around and below the hilltop parking area leading down to the Silver Creek Lake Campground off of Silver Creek Lake Road. | 31.66612294, -87.57569860 | 49 | Plants are growing in shade of upland dry mesic, mature mixed deciduous and evergreen woodland. Generally, the overstory is thinner and there is less leaf litter cover, making the surface soil conditions drier. Slope: 5 to 10 percent. Aspect: Southeast. Geology: The underlying geology of this area is Claiborne Group, Tallahatta Formation, of Eocene origin, with white to very light-greenish-gray thin-bedded to massive siliceous claystone; interbedded with thin layers of fossiliferous clay, sandy clay, and glauconitic sand and sandstone. (Source: USGS Alabama Geologic Map Data). Soils: The primary soil types in the collection area are classified as Arundel-Cantuche Complex soils (15 to 35 percent slopes). The Arundel Series consists of moderately deep, well drained, very slowly permeable soils on dissected uplands of the Southern Coastal Plain. They formed in marine deposits consisting of acid clays underlain by horizontally bedded sandstone, buhrstone and siltstone. These soils are strongly acid. Slopes range from 2 to 60 percent. The Cantuche Series consists of shallow, well drained, moderately permeable soils that formed over horizontally bedded claystone. These soils are on narrow ridgetops and narrow benches on steep side-slopes of dissected landscapes in the Coastal Plain. They are strongly acid. Slopes range from 2 to 35 percent. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). EPA Ecoregion (Level III): Southeastern Plains (65). EPA Ecoregion (Level IV): Buhrstone/Lime Hills (65q). | Wild material | | 2169053 | NA 89089 |
| 101 | NA 89090 | 2024RM-TK-003 | Ilex longipes Chapm. ex Trel. | Alabama, United States | NA | | | 2024 | COLLECTED | 09/19/2024 | Woodland slopes around and below the hilltop parking area leading down to the Silver Creek Lake Campground off of Silver Creek Lake Road. | 31.66612294, -87.57569860 | 39 | Plants are growing in part-shade to shade of a moist mesic deciduous and evergreen woodland on dry, well-drained soil to an area 1-2 meters above a small seasonally spring-fed creek at 31.664428°, -87.574614°. Slope: 5 to 10 percent. Aspect: Southeast. Geology: The underlying geology of this area is Claiborne Group, Tallahatta Formation, of Eocene origin, with white to very light-greenish-gray thin-bedded to massive siliceous claystone; interbedded with thin layers of fossiliferous clay, sandy clay, and glauconitic sand and sandstone. (Source: USGS Alabama Geologic Map Data). Soils: The primary soil types in the collection area are classified as Arundel-Cantuche Complex soils (15 to 35 percent slopes). The Arundel Series consists of moderately deep, well drained, very slowly permeable soils on dissected uplands of the Southern Coastal Plain. They formed in marine deposits consisting of acid clays underlain by horizontally bedded sandstone, buhrstone and siltstone. These soils are strongly acid. Slopes range from 2 to 60 percent. The Cantuche Series consists of shallow, well drained, moderately permeable soils that formed over horizontally bedded claystone. These soils are on narrow ridgetops and narrow benches on steep side-slopes of dissected landscapes in the Coastal Plain. They are strongly acid. Slopes range from 2 to 35 percent. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). EPA Ecoregion (Level III): Southeastern Plains (65). EPA Ecoregion (Level IV): Buhrstone/Lime Hills (65q). | Wild material | | 2169054 | NA 89090 |
| 102 | NA 89091 | 2024RM-TK-004 | Prunus sp. | Florida, United States | NA | | | 2024 | COLLECTED | 09/05/2024 | Blackwater River Wildlife Management Area: on the south side of Boundary Line Road about 0.32 kilometers west of Deaton Bridge Road along an area edged by a barbed wire fence. | 30.68579800, -86.87964300 | 45 | Plants are growing from part-sun to full sun. Plants are growing in an area that is frequently burned with a lot of [Prunus sp. (orig. listed as Prunus alabamensis)] scattered throughout. This habitat is a longleaf pine-wiregrass community with scattered turkey (Quercus laevis) and blackjack oaks (Quercus incana). There is a slight slope downward. The line of [Prunus sp.] goes along a semi-ditch on the side of a dirt road. The plants probably get a bit more water than the plants out in the open forest. The [Prunus sp.] are most often without any other close woody companions. Slope: 0 percent. Aspect: North. Geology: The underlying geology of this area is probably of lower Pliocene age and characterized as the Citronelle Formation. The Citronelle Formation is widespread in the Gulf Coastal Plain. The type section for the Citronelle Formation, named by Matson (1916), is near Citronelle, Alabama. The Citronelle Formation grades laterally, through a broad facies transition, into the Miccosukee Formation of the eastern Florida panhandle. Coe (1979) investigated the Citronelle Formation in portions of the western Florida panhandle. The Citronelle Formation is a siliciclastic, deltaic deposit that is lithologically similar to, and time equivalent with, the Cypresshead Formation and, at least in part, the Long Key Formation (Cunningham et al., 1998) of the peninsula. In the western panhandle, some of the sediments mapped as Citronelle Formation may be reworked Citronelle. The lithologies are the same and there are few fossils present to document a possible younger age. The Citronelle Formation consists of gray to orange, often mottled, unconsolidated to poorly consolidated, very fine to very coarse, poorly sorted, clean to clayey sands. It contains significant amounts of clay, silt and gravel which may occur as beds and lenses and may vary considerably over short distances. Limonite nodules and limonite-cemented beds are common. Marine fossils are rare but fossil pollen, plant remains and occasional vertebrates are found. Much of the Citronelle Formation is highly permeable. It forms the Sand and Gravel Aquifer of the surficial aquifer system. (Source: USGS Florida Geologic Map Data). Soils: The soil of this area is characterized as Lakeland Series Sand, 0 to 5 percent slopes (21). The Lakeland Series consists of very deep, excessively drained, rapid to very rapidly permeable soils on uplands. They formed in thick beds of eolian or marine and/or fluvio-marine sands in the Southern Coastal Plain MLRA (133A), the Carolina and Georgia Sandhills (MLRA 137), the Eastern Gulf Coast Flatwoods (MLRA 152A) and the Atlantic Coast Flatwoods (MLRA 153A). (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). EPA Ecoregion (Level III): Southeastern Plains (65). EPA Ecoregion (Level IV): Southern Pine Plains and Hills (65f). | Wild material | Received as Prunus alabamensis; other collections of this material have proven not to be Prunus serotina var. alabamensis, but actually a species of plum; this will likewise be treated as unidentified material until its species can be ascertained. Collectors' notes refer to the plant by the name under which it was collected. | 2169055 | NA 89091 |
| 103 | NA 87823 | FL24-01 | Ilex cassine L. | Florida, United States | NA | | | 2024 | COLLECTED | 09/05/2024 | Matanzas State Forest. | 29.72143991, -81.28386478 | | Boggy blackwater ditches along edge of dirt road. EPA Ecoregion III: Southern Coastal Plain (75). EPA Ecoregion IV: Eastern Florida Flatwoods (75d). Geology: Beach Ridge and Dune. Soil: Immokalee Series Fine Sand. | Wild material | | 2168973 | NA 87823 |
| 104 | Ames 36251 | JDC/UT/2024/008/1130 | Ulmus thomasii Sarg. | Minnesota, United States | NC7 |  | | 2024 | COLLECTED | 06/05/2024 | Near southeast edge of Kasota Lake approximately 9.0 miles east, southeast of Willmar, T119N R34W SE 1/4 NE 1/4 Sec. 36 and also Robbins Island Park in Wilmar, T119N R35W Sec. 11. | 45.07399600, -94.88484100 | 352 | Deciduous woods | Wild material | Ulmus thomasii (Rock elm) is an underutilized tree species both in conservation and in the urban landscape. Described by Charles Sprague Sargent (first director for the Arnold Arborteum) as "heavy, hard, very strong and tough, closely grained, and susceptible of receiving a beautiful polish". Historically noted for a variety of uses in woodworking including furniture, heavy agricultural implements, timber frame buildings, pianos, hockey sticks, and hand tools. Ulmus thomasii is extremely drought tolerant, adaptable to very calcareous soils, and compared to U. americana or U. rubra has a very conservative growth rate requiring minimal attention in regards to pruning. Rock elm naturally tends to develop into a nice structural specimen in the landscape, unlike other fast growing cultivars in the nursery trade needing frequent attention. Rock elm has very fissured bark and is well known for maintaining a strong central leader resulting in a very attractive, pyramidal form. Despite many literature sources stating that "wings" on the stems are a key identifiying characteristic, this trait is not reliable and many genotypes may completely lack "wings" on the stems. While growth habit and morphology of dormant buds (very pointy) are good traits to help aid in identification, fruits are the best way to confirm identity. Fruits are densly pubescent, often described as "inflated" and generally reach maturity a couple weeks after Ulmus rubra and Ulmus americana. U. thomasii inflorescences are rather distinguishable from other Ulmus in being pendulous. Fruits are extremely prized treats for many birds, where fruits are often "robbed" prior to full maturity. Fruits are also highly prized by many other animals such as mice, squirrels, chipmunks, turkeys, etc. and are generally consumed within hours after fruit abscission. The native range of U. thomasii is concentrated in the northeastern United States and into Canada with disjunct populations documented in northwestern Missouri and northwestern Arkansas (Little, E. L. Jr. 1971). In the 1895 Silva of North America (vol. 7) it was stated that, “The value of the wood of the Rock Elm threatens its extinction and most of the large trees have already been cut.” Today, while rock elm is rather rare, especially in areas near the edges of its range, many states list the species as endangered or threatened warranting preservation efforts. Genetics of this accession would be representative of the species northwestern edge of its native range. Majority of specimens noted did not have characteristic "wings" on the stems and measured approximately 20" DBH or more with a few specimens nearing 30". Heights estimated between 70-90'. Rock elm in this area could be classified as locally abundant. | 2167953 | Ames 36251 |
| 105 | Ames 36248 | Robert's Creek | Salix bebbiana Sarg. | Iowa, United States | NC7 |  | | 2024 | COLLECTED | 05/15/2024 | Robert’s Creek Preserve just north of Forest Road approximately 4.2 miles north, northeast of Elkader, T94N R5W near center of Sec. 36. | 42.91366500, -91.37990600 | 260 | Mixed hardwood forest. Very steep, moist, north-facing slope. | Wild material | Bebb's willow, Salix bebbiana, is a tight, clump forming, multi-stemmed shrub that can reach up to 25' in height that forms a rather distinct, mounded growth habit. Native to North America, the native range covers mostly Canada, but extending south into the northeastern US and also the Rocky Mountains range stretching as far south as New Mexico and Arizona (Little, E. L. Jr. 1977). In Iowa, this species seems to only be known from northeastern Iowa. Salix bebbiana can be found in a variety of habitats from pond margins/swamps to even moderately well-drained open fields. The female capsules are long (5-9 mm) with a very slender beak held on the longest stalk of any N. American Salix. This accession represents genetics from northeastern Iowa at the southern edge of its range in northeastern N. America. Specimens sampled were estimated at 30' in height. Some of the oldest, largest specimens sampled measuring approximately 8" DBH were showing signs of decline. Immature leaves are reddish or yellow green and rather rugose. | 2167645 | Ames 36248 |
| 106 | WLP 3432 | RM2023-001 | Rhododendron minus Michx. | Georgia, United States | NA | | | 2024 | COLLECTED | 10/21/2023 | Plants growing along Patterson Gap Road. | 34.96995500, -83.47722800 | 1005 | Plants growing in part shade to sun in an upland, very dry and rocky, mostly deciduous habitat. The site is steeply sloped, underlain by rock, with rocky outcrops. Slope: 15 to 65 percent. Aspect: Variable. The underlying geology of this area is Quartzite/Mica Schist, primarily of Precambrian-Paleozoic origin. (Source: USGS North Carolina Geologic Map Data.) The primary soil type in the collection area is classified as Ashe Series that is stony and very steep. The Ashe series consists of moderately deep, somewhat excessively drained soils on gently sloping to very steep ridges and side slopes of the Blue Ridge. They formed in residuum that is affected by soil creep in the upper part, and weathered from felsic or mafic igneous and high-grade metamorphic rocks such as granite, hornblende gneiss, granodiorite, biotite gneiss, and high-grade metagraywacke. Slope ranges from 2 to 95 percent. The surface layer to 5cm deep is comprised of moderately decomposed organic matter and leaves, twigs, and roots. Layers to 70cm deep range from very dark grayish brown to brown sandy loam with weak medium and coarse granular structure that is friable. A few fine flakes of mica can be found and these soils are very strongly acid. (Source: NRCS Web Soil Survey.) | Wild material | | 2166141 | WLP 3432 |
| 107 | WLP 3433 | RM2023-002 | Clethra acuminata Michx. | Georgia, United States | NA | | | 2024 | COLLECTED | 10/21/2023 | Plants growing along Patterson Gap Road. | 34.97299200, -83.46003100 | 789 | Plants growing in part shade in a very dry and rocky, mostly deciduous habitat. The site is steeply sloped, underlain by rock, with rocky outcrops. Slope: 15 percent. Aspect: Variable. The underlying geology of this area is Biotite Gneiss, primarily of Precambrian-Paleozoic origin. (Source: USGS North Carolina Geologic Map Data.) The primary soil type in the collection area is classified as Tusquitee loam, 10 to 25 percent slopes. The Tusquitee series consists of very deep, well drained soils on gently sloping to very steep benches, foot slopes, toe slopes, and fans in coves in the Southern Blue Ridge mountains, MLRA 130B. These soils formed in colluvium derived from materials weathered from igneous and high-grade metamorphic crystalline rocks such as granite, mica gneiss, hornblende gneiss, and schist. Slope ranges from 2 to 95 percent. The surface layer to 5cm deep is comprised of moderately decomposed organic matter and leaves, twigs, and roots. Layers to 2m deep range from very dark grayish brown to brown sandy loam with weak medium and coarse granular structure that is friable. A few fine flakes of mica can be found and these soils are very strongly acid. (Source: NRCS Web Soil Survey.) | Wild material | | 2166142 | WLP 3433 |
| 108 | WLP 3434 | RM2023-003 | Hydrangea arborescens L. | Georgia, United States | NA | | | 2024 | COLLECTED | 10/21/2023 | Plants growing along Patterson Gap Road. | 34.97369800, -83.46276600 | 809 | Plants growing in part shade in a very dry and rocky, mostly deciduous habitat. Slope: 25 percent. Aspect: variable. The underlying geology of this area is Biotite Gneiss, primarily of Precambrian-Paleozoic origin. (Source: USGS North Carolina Geologic Map Data.) The primary soil type in the collection area is classified as Porters Series which is stony and steep. The Porters series consists of deep, well drained, moderately permeable soils on cool, north- to east-facing or shaded ridges and side slopes in the Southern Blue Ridge mountains. These soils formed in residuum, affected by soil creep in the upper part, that has weathered from felsic to mafic, high-grade metamorphic and igneous rocks such as granite, gneiss, hornblende gneiss, mica gneiss, and amphibolite. Slope ranges from 2 to 95 percent. The surface layer to 18cm deep is very dark grayish brown loam; moderate fine and medium granular structure; very friable; many fine roots; few fine mica flakes; slightly acid. From 18 to 90 cm soil range from brown loam with weak fine and medium subangular blocky structure, few mica flakes, and few medium gneiss and quartz fragments that is moderately acid to sandy loam with gneiss saprolite with quartz, weathered feldspar, hornblende, mica and other minerals that is slightly acid and grades into hard rock. (Source: NRCS Web Soil Survey.) | Wild material | | 2166143 | WLP 3434 |
| 109 | NA 88827 | RJL-RM2023FLAL-001 | Ilex ambigua Torr. | Florida, United States | NA | | | 2023 | COLLECTED | 12/05/2023 | Yellow River Wildlife Management Area, along DOF [Department of Forestry] Y9 dirt road 0.08 kilometers east of Miller Bluff Road. | 30.65289100, -86.87602800 | 44 | Growing in part shade to sun in very dry, highly competitive site still recovering from the logging of pines in the past decade. This young woodland is comprised of a combination of evergreen and deciduous species competing for available resources and light before the young sand pines begin to dominate the upper canopy. Slope: 0 percent. Aspect: N/A. The underlying geology of this area is the Citronelle Formation, of Pliocene origin, and consists of gray to orange, often mottled, unconsolidated to poorly consolidated, very fine to very coarse, poorly sorted, clean to clayey sands. It contains significant amounts of clay, silt and gravel which may occur as beds and lenses and may vary considerably over short distances. Limonite nodules and limonite-cemented beds are common. (Source: USGS Florida Geologic Map Data.) The primary soil type in the collection area is classified as Lakeland Sand soils (0 to 5 percent slopes). The surface soil profile of this area is primarily the Lakeland series which consists of very deep, excessively drained, rapid to very rapidly permeable soils on uplands. They formed in thick beds of eolian or marine and/or fluvio-marine sands. Thickness of the sand exceeds 2 meters. Silt plus clay in the upper meter ranges from 5-10 percent. Reaction ranges from very strongly acid to moderately acid throughout. (Source: NRCS Web Soil Survey.) | Wild material | | 2165657 | NA 88827 |
| 110 | NA 88828 | RJL-RM2023FLAL-002 | Vaccinium arboreum Marshall | Florida, United States | NA | | | 2023 | COLLECTED | 12/05/2023 | Yellow River Wildlife Management Area, along DOF [Department of Forestry] Y9 dirt road 0.08 kilometers east of Miller Bluff Road. | 30.65289100, -86.87608500 | 44 | Growing in part shade to sun in very dry, highly competitive site still recovering from the logging of pines in the past decade. This young woodland is comprised of a combination of evergreen and deciduous species competing for available resources and light before the young sand pines begin to dominate the upper canopy. Slope: 0 percent. Aspect: N/A. The underlying geology of this area is the Citronelle Formation, of Pliocene origin, and consists of gray to orange, often mottled, unconsolidated to poorly consolidated, very fine to very coarse, poorly sorted, clean to clayey sands. It contains significant amounts of clay, silt and gravel which may occur as beds and lenses and may vary considerably over short distances. Limonite nodules and limonite-cemented beds are common. (Source: USGS Florida Geologic Map Data.) The primary soil type in the collection area is classified as Lakeland Sand soils (0 to 5 percent slopes). The surface soil profile of this area is primarily the Lakeland series which consists of very deep, excessively drained, rapid to very rapidly permeable soils on uplands. They formed in thick beds of eolian or marine and/or fluvio-marine sands. Thickness of the sand exceeds 2 meters. Silt plus clay in the upper meter ranges from 5-10 percent. Reaction ranges from very strongly acid to moderately acid throughout. (Source: NRCS Web Soil Survey.) | Wild material | | 2165658 | NA 88828 |
| 111 | NA 88829 | RJL-RM2023FLAL-003 | Oxydendrum arboreum (L.) DC. | Florida, United States | NA | | | 2023 | COLLECTED | 12/05/2023 | Yellow River Wildlife Management Area, along DOF [Department of Forestry] Y15 dirt road 0.06 kilometers north of Fisher Old Mill Road. | 30.62728600, -86.83824600 | 7 | Growing in part shade to sun in moist to wet flat woods of the longleaf pine forest. The woodland is comprised mostly of open habitat of longleaf pine and an understory tree and shrub layer of evergreen and deciduous species. There is also a wealth of herbaceous species in moist to wet conditions of the habitat where there is rich organic matter in the surface layer. Slope: 0 percent. Aspect: N/A. The underlying geology of this area is classified as Alluvium, of Pleistocene/Holocene origin and consists of undifferentiated Quaternary sediments of varying thickness including siliciclastics, organics and freshwater carbonates. The siliciclastics are light gray, tan, brown to black, unconsolidated to poorly consolidated, clean to clayey, silty, unfossiliferous, variably organic-bearing sands to blue green to olive green, poorly to moderately consolidated, sandy, silty clays. Organics occur as plant debris, roots, disseminated organic matrix and beds of peat. Freshwater carbonates, often referred to as marls in the literature, are scattered. (Source: USGS Florida Geologic Map Data.) The primary soil types in the collection area are classified as Pactolus Loamy Sand soils (0 to 5 percent slopes). The Pactolus Series consists of very deep, moderately well to somewhat poorly drained soils. Permeability is rapid. These Coastal Plain soils, typically found with streams and marine terraces and were formed by loamy and sandy fluvial sediments and marine sediments. The strata is, generally, uniformly loamy sand that is very friable and strongly acid from the surface to a depth of 1.8 meters. (Source: NRCS Web Soil Survey.) | Wild material | | 2165659 | NA 88829 |
| 112 | NA 88834 | RJL-RM2023FLAL-008 | Rhododendron canescens (Michx.) Sweet | Florida, United States | NA | | | 2023 | COLLECTED | 12/06/2023 | Blackwater State Forest: plants are growing in wetlands accessed by foot from Buddy Hardy Road. The collection site is approximately 0.14 kilometers west and downhill from the road. | 30.80736700, -86.95784700 | 53 | Growing in shade to part-shade of the well-drained moist mesic habitat about 1 m above the wetland which appears to be formed by a nearby hillside seepage area. In this zone there are numerous facultative wetland species as well as high competition from facultative upland plants. Slope: 5 to 10 percent. Aspect: Variable. The underlying geology of this area is the Citronelle Formation of Pliocene origin and consists of gray to orange, often mottled, unconsolidated to poorly consolidated, very fine to very coarse, poorly sorted, clean to clayey sands. It contains significant amounts of clay, silt and gravel which may occur as beds and lenses and may vary considerably over short distances. Limonite nodules and limonite-cemented beds are common. (Source: USGS Florida Geologic Map Data.) The Troup Series (5 to 8% slopes) consists of very deep, somewhat excessively drained soil formed in unconsolidated sandy and loamy marine sediments. Troup soils are on ridges and hillslopes. The upper 0-13 cm is comprised primarily of decomposing sphagnum peat with a significant amount of fibrous root content. From 15-112 cm the soil is comprised primarily of fine-grained yellowish-brown sand with varying amounts of root content; this zone is strongly acid. From 112-203 cm the soil is comprised of light-red to red sandy clay loam that is discontinuous, generally friable, and strongly acid. (Source: NRCS Web Soil Survey.) | Wild material | | 2165664 | NA 88834 |
| 113 | NA 88835 | RJL-RM2023FLAL-009 | Rhododendron viscosum (L.) Torr. | Florida, United States | NA | | | 2023 | COLLECTED | 12/06/2023 | Blackwater State Forest: plants are growing in wetlands accessed by foot from Buddy Hardy Road. The collection site is approximately 0.14 kilometers west and downhill from the road. | 30.80841000, -86.96283300 | 43 | Growing in part-shade of the well-drained moist-dry mesic habitat about 2-3 m above the wetland. In this zone there are numerous facultative wetland species as well as high competition from facultative upland plants. Slope: 5 to 10 percent. Aspect: Variable. The underlying geology of this area is the Citronelle Formation of Pliocene origin and consists of gray to orange, often mottled, unconsolidated to poorly consolidated, very fine to very coarse, poorly sorted, clean to clayey sands. It contains significant amounts of clay, silt and gravel which may occur as beds and lenses and may vary considerably over short distances. Limonite nodules and limonite-cemented beds are common. (Source: USGS Florida Geologic Map Data.) The Troup Series (5 to 8% slopes) consists of very deep, somewhat excessively drained soil formed in unconsolidated sandy and loamy marine sediments. Troup soils are on ridges and hillslopes. The upper 0-13 cm is comprised primarily of decomposing sphagnum peat with a significant amount of fibrous root content. From 15-112 cm the soil is comprised primarily of fine-grained yellowish-brown sand with varying amounts of root content; this zone is strongly acid. From 112-203 cm the soil is comprised of light-red to red sandy clay loam that is discontinuous, generally friable, and strongly acid. (Source: NRCS Web Soil Survey.) | Wild material | | 2165665 | NA 88835 |
| 114 | NA 88836 | RJL-RM2023FLAL-010 | Leucothoe axillaris (Lam.) D. Don | Florida, United States | NA | | | 2023 | COLLECTED | 12/08/2023 | Along Gin/Camp Road at the bridge over Thomas Creek on the east side of the road. | 30.75018700, -87.23492900 | 21 | Growing in shade of the moist to wet habitat along Thomas Creek. Plants receive regular moisture and are occasionally flooded in this habitat. Slope: N/A. Aspect: N/A. The underlying geology of this area is the Citronelle Formation of Pliocene origin and consists of gray to orange, often mottled, unconsolidated to poorly consolidated, very fine to very coarse, poorly sorted, clean to clayey sands. It contains significant amounts of clay, silt and gravel which may occur as beds and lenses and may vary considerably over short distances. Limonite nodules and limonite-cemented beds are common. (Source: USGS Florida Geologic Map Data.) The surface soil profile of this area is primarily Bibb-Kinston series association. Bibb series soils are coarse-loamy, sandy, acid soils that are poorly drained. They are soils of flood plains and streams subject to frequent flooding. These are found in association with Kinston series soils that are fine-loamy, sandy, acid soils of flood plains and stream subject to frequent flooding. The Bibb-Kinston association ranges from 1-1.5 meters thick and is strongly acid. (Source: NRCS Web Soil Survey.) | Wild material | | 2165666 | NA 88836 |
| 115 | NA 88838 | RJL-RM2023FLAL-012 | Ilex opaca Aiton | Florida, United States | NA | | | 2023 | COLLECTED | 12/08/2023 | North side of Sid Hayes Road approximately 65 m southeast of the junction with Watson Road. | 30.83277400, -87.24324500 | 32 | Growing in shade, part shade and light shade in dry mesic to moist, occasionally wet, habitats along the edge of the road and in the woodland interior. This species is remarkably adaptable. The only drawback to the range of habitats is that in deep shade, very few fruit can be found, presumably because there is far less flower production and/or fewer pollinators. Slope: 0 to 3 percent. Aspect: South. The underlying geology of this area is the Citronelle Formation of Pliocene origin and consists of gray to orange, often mottled, unconsolidated to poorly consolidated, very fine to very coarse, poorly sorted, clean to clayey sands. It contains significant amounts of clay, silt and gravel which may occur as beds and lenses and may vary considerably over short distances. Limonite nodules and limonite-cemented beds are common. (Source: USGS Florida Geologic Map Data.) The surface soil profile of this area is Dothan Series fine sandy loam soils (5 to 8 percent slopes). The Dothan Series consists of very deep, well drained soils that formed in thick beds of unconsolidated, medium to fine-textured marine sediments. Dothan soils are on interfluves. The surface 0-33 cm is characterized by sandy-loam, well-drained soils that are strongly acid. From 33-200 cm they are characterized by sandy clay loam soils that are more moisture retentive and strongly acid. (Source: NRCS Web Soil Survey.) | Wild material | | 2165668 | NA 88838 |
| 116 | NA 88839 | RJL-RM2023FLAL-013 | Rhododendron austrinum (Small) Rehder | Florida, United States | NA | | | 2023 | COLLECTED | 12/10/2023 | Along the Florida Trail, accessed from Miller Bluff Road. Plants were found infrequently but regularly along the trail over 1 kilometer or more. | 30.61991500, -86.86521000 | 4 | Plants are growing primarily in shade to dappled shade, above a small stream in moist mesic conditions along and below the Florida Trail. The mixed evergreen and deciduous forest is quite diverse with an excellent litter layer. Slope: 2 to 8 percent. Aspect: South. The underlying geology of this area is classified as Alluvium, of Pleistocene/Holocene origin and consists of undifferentiated Quaternary sediments of varying thickness including siliciclastics, organics and freshwater carbonates. The siliciclastics are light gray, tan, brown to black, unconsolidated to poorly consolidated, clean to clayey, silty, unfossiliferous, variably organic-bearing sands to blue green to olive green, poorly to moderately consolidated, sandy, silty clays. Organics occur as plant debris, roots, disseminated organic matrix and beds of peat. Freshwater carbonates, often referred to as marls in the literature, are scattered. (Source: USGS Florida Geologic Map Data.) The surface soil profile of this area is primarily Bibb-Kinston Series Association. Bibb Series soils are coarse-loamy, sandy, acid soils that are poorly drained. They are soils of flood plains and streams subject to frequent flooding. These are found in association with Kinston Series soils that are fine-loamy, sandy, acid soils of flood plains and stream subject to frequent flooding. The Bibb-Kinston association ranges from 1-1.5 meters thick and is strongly acid. (Source: NRCS Web Soil Survey.) | Wild material | | 2165669 | NA 88839 |
| 117 | NA 88843 | RJL-RM2023FLAL-017 | Rhododendron austrinum (Small) Rehder | Florida, United States | NA | | | 2023 | COLLECTED | 12/11/2023 | Holmes Creek at Live Oak Landing: plants found on the low bluff along the south side of Holmes Creek accessed by foot from a parking lot on Live Oak Landing Road that dead ends into the creek. | 30.59043500, -85.83899800 | 7 | Plants are growing in part shade to shade on the top and slope of the low bluff overlooking Holmes Creek in a mixed deciduous and evergreen forest. The dry mesic habitat has relatively low competition and is quite acidic. Slope: 0 to 45 percent. Aspect: Northwest. The underlying geology of this area is classified as Alluvium, of Pleistocene/Holocene origin and consists of undifferentiated Quaternary sediments of varying thickness including siliciclastics, organics and freshwater carbonates. The siliciclastics are light gray, tan, brown to black, unconsolidated to poorly consolidated, clean to clayey, silty, unfossiliferous, variably organic-bearing sands to blue green to olive green, poorly to moderately consolidated, sandy, silty clays. Organics occur as plant debris, roots, disseminated organic matrix and beds of peat. Freshwater carbonates, often referred to as marls in the literature, are scattered. (Source: USGS Florida Geologic Map Data.) The surface soil profile of this area is primarily Nankin-Cowarts-Lakeland Complex. The Nankin Series consists of very deep, well drained, moderately slowly permeable soils on uplands of the Coastal Plain. They formed in stratified loamy and clayey marine sediments. Slopes range from 0 to 60 percent. Soils are comprised of sandy loam in the upper 25 cm to sandy clay loam and sandy clay in lower strata to about 1.7 meters deep; these soils are strongly acid. The Cowarts Series consists of very deep, moderately well and well drained soils on ridge tops and side slopes on uplands of the Coastal Plain Major Land Resource Area. They formed in loamy marine sediments. Slopes range from 1 to 60 percent. The Lakeland series consists of very deep, excessively drained, rapid to very rapidly permeable soils on uplands. They formed in thick beds of eolian or marine and/or fluvio-marine sands. Thickness of the sand exceeds 2 meters. Silt plus clay in the upper meter ranges from 5-10 percent. Reaction ranges from very strongly acid to moderately acid throughout. (Source: NRCS Web Soil Survey.) | Wild material | | 2165673 | NA 88843 |
| 118 | NA 88844 | RJL-RM2023FLAL-018 | Clethra alnifolia L. | Florida, United States | NA | | | 2023 | COLLECTED | 12/13/2023 | Yellow River Water Management Area, accessed off of Old River Road by vehicle on an unmaintained sand road for approximately 1.68 kilometers. Upon reaching the destination, plants are accessed by foot along unmaintained trail to the east. | 30.83495500, -86.62005400 | 27 | Plants are growing primarily in part shade as understory shrubs in mixed evergreen and deciduous, moist to wet, acidic woodlands. Plants form large colonies and appear to have been subjected to prescribed fire in recent years. Slope: 10 to 15 percent. Aspect: Northeast. The underlying geology of this area is the Citronelle Formation of Pliocene origin and consists of gray to orange, often mottled, unconsolidated to poorly consolidated, very fine to very coarse, poorly sorted, clean to clayey sands. It contains significant amounts of clay, silt and gravel which may occur as beds and lenses and may vary considerably over short distances. Limonite nodules and limonite-cemented beds are common. (Source: USGS Florida Geologic Map Data.) The soil profile for this area is classified as the Bonifay Soil Series. Bonifay soil consists of very deep, well drained, moderately slowly permeable soils on ridges and side slopes in the Southern Coastal Plain. They formed in thick beds of sandy and loamy marine sediments. Solum thickness ranges from 1.5-2.0 m. Soil reaction ranges from very strongly acid to moderately acid throughout, except where the surface has been limed. Ironstone pebbles, 2 to 15 mm in size, range from 0 to 5 percent, by volume. Depth to the plinthic horizon ranges from 1.1-1.7 m. Some horizons contain up to 25 percent plinthite by volume. (Source: NRCS Web Soil Survey.) | Wild material | | 2165674 | NA 88844 |
| 119 | NA 88850 | RJL-RM2023FLAL-024 | Rhododendron austrinum (Small) Rehder | Florida, United States | NA | | | 2023 | COLLECTED | 12/13/2023 | Yellow River Water Management Area, found in an area where an unnamed unpaved road winds along the edges of the Yellow River. This unpaved road is accessed from Old River Road to the east near the junction with Shockley Springs Road. Individuals are found along the roadside for at least 6 kilometers from the point where the unnamed road splits and turns south. | 30.82647700, -86.60892000 | 23 | Plants are growing primarily in part shade to shade in mesic conditions in a mixed evergreen and deciduous forest. Fruiting plants are more abundant where plants receive more sunlight. Slope: 0 to 2 percent. Aspect: Various. The underlying geology of this area is the Alum Bluff Group of Miocene origin. It includes the Chipola Formation, Oak Grove Sand, Shoal River Formation, Choctawhatchee Formation and the Jackson Bluff Formation. The formations included in this group are generally defined on the basis of their molluscan faunas and stratigraphic position. Puri (1953) described sediment facies as they relate to the formations of the Alum Bluff Group. These sediments are lithologically distinct as a group, not as individual units. The Alum Bluff Group crops out or is beneath a thin overburden in the western panhandle from river valleys in Okaloosa County eastward to western Jackson County. The Alum Bluff Group consists of clays, sands and shell beds which may vary from fossiliferous, sandy clays to unfossiliferous sands and clays and occasional carbonate beds. Mica is a common constituent and glauconite and phosphate occur sporadically. Induration varies from essentially nonindurated in sands to well indurated in carbonate lenses. Colors range from cream to olive gray with mottled reddish brown in weathered sections. Sand grain size varies from very fine to very coarse with sporadic occurrences of gravel. These sediments generally have low permeabilities and are part of the intermediate confining unit/aquifer system. (Source: USGS Florida Geologic Map Data.) The surface soil profile of this area is primarily Yemassee, Garcon, and Bigbee soils that are occasionally flooded. The Yemassee Series consists of very deep, somewhat poorly drained, moderately permeable, loamy soils that formed in marine sediments. These soils are on terraces and broad flats of the lower Coastal Plain and very strongly acid. Slopes range from 0 to 2 percent. The Garcon Series consists of very deep, somewhat poorly drained, moderately permeable soils on terraces and in the broad flats of the lower Coastal Plain. They formed in sandy and loamy marine sediments. This soil ranges from very strongly acid to extremely acid. The Bigbee series consists of very deep, excessively drained, rapidly permeable soils that are on natural levees and higher positions in flood plains along stream flood plains in the Southern Coastal Plain (MLRA 133A) and the Eastern Gulf Coast Flatwoods (MLRA 152A). They formed in thick sandy alluvial sediments. They range from strongly acid to very strongly acid. (Source: NRCS Web Soil Survey.) | Wild material | | 2165680 | NA 88850 |
| 120 | NA 88820 | TJK2023AL-005 | Hydrangea arborescens L. | Alabama, United States | NA | | | 2023 | COLLECTED | 12/07/2023 | Between Monroe County Route 1 and Tom Hayles Road. | 31.40575900, -87.54924000 | 22 | In woodlands on limestone outcrop. While the upper area of slopes is covered by a thin soil layer, the exposed limestone rock outcrop on the northwestern edge of this area is a low competition niche for plants like the Hydrangea to gain a foothold. Slope: 60% (plus). Aspect: Northwest. Elevation: 72 feet. | Wild material | | 2165649 | NA 88820 |
| 121 | NA 88821 | TJK2023AL-006 | Hydrangea quercifolia W. Bartram | Alabama, United States | NA | | | 2023 | COLLECTED | 12/07/2023 | Between Monroe County Route 1 and Tom Hayles Road. | 31.40580000, -87.54890000 | 22 | In woodlands on limestone outcrop. While the upper area of slopes is covered by a thin soil layer, the exposed limestone rock outcrop on the northwestern edge of this area is a low competition niche for plants like the Hydrangea to gain a foothold. Slope: 60% (plus). Aspect: Northwest. Elevation: 72 feet. | Wild material | | 2165650 | NA 88821 |
| 122 | NA 88814 | TXWL2023-021 | Ilex ambigua Torr. | Texas, United States | NA | | | 2023 | COLLECTED | 12/09/2023 | Roadside between Big Cow Creek and Hardy Cemetery. | 31.03548900, -93.85086800 | | Roadside; mesic, mixed hardwood/pine forest. | Wild material | | 2165618 | NA 88814 |
| 123 | NA 88806 | TJK2023LA/TX-006 | Vaccinium arboreum Marshall | Texas, United States | NA | | | 2023 | COLLECTED | 11/21/2023 | Interstate 20, westbound, approximately 2.2 miles west of FM (farm-to-market road) 2015 and 0.8 miles east of FM 14. | 32.45250000, -95.26960000 | 10 | Xeric shortleaf pine-post oak-blackjack oak uplands. Slope: flat. Aspect: West. Elevation: 32 feet. | Wild material | | 2159189 | NA 88806 |
| 124 | NA 88689 | RJL2023NJ-002 | Kalmia latifolia L. | New Jersey, United States | NA | | | 2023 | COLLECTED | 11/10/2023 | Franklin Township: Piney Hollow Preservation Area (the site is owned by Franklin Township). Plants accessed by foot along trails throughout property. | 39.57400900, -74.93602400 | 32 | Plants growing in shade to part-shade of a mesic to mesic-dry woodland habitat that is mostly deciduous, but also includes pine overstory. Slope: N/A. Aspect: N/A. Soils: The underlying geology of this area is of Middle Miocene, Serravallian origin and characterized as an Cohansey Formation. It is comprised of sand, white to yellow with local gravel and clay. Locally stained red or orange brown by iron oxides and (or) cemented into large blocks of ironstone. Unweathered clay is typically dark gray, but commonly weathers white where interbedded with thin beds of ironstone. Unit is a complex of interfingering marine and nonmarine facies. Sand is typically medium grained and moderately sorted although it ranges from fine to very coarse grained and from poorly to well sorted. Sand consists of quartz and siliceous rock fragments. Some beds are locally micaceous. In general, the sand is crossbedded, although the style of crossbedding varies significantly with the paleoenvironment. Trough crossbedding predominates, especially in the nonmarine channel fill deposits, and the scale of the crossbeds varies from small to large. Maximum thickness in the map area is about 60 m; however, thickness is difficult to determine because of the irregular basal contact and extensive post-depositional erosion. There is as much as 18 m of relief along the basal contact. The basal contact is sharp, undulatory, and directly overlain by a thin gravel bed. The Cohansey Formation unconformably overlies the Kirkwood Formation and is found in channels cut down into the Kirkwood. Where the Kirkwood consists of sandy, light-colored sediments, the basal contact of the Cohansey is drawn below crossbedded sediments. Where the Kirkwood consists of dark-colored silty beds, the basal contact is drawn between light-colored Cohansey sediments and the underlying dark-colored sediments. The Cohansey was markedly thinned because of erosion prior to deposition of overlying units in the western and southern parts of the southern sheet. The unit has been extensively eroded and stripped from large areas of the New Jersey Coastal Plain, particularly in the central sheet where outliers are common. In spite of its widespread nature, the Cohansey is poorly exposed because of its loose sandy composition, which causes it to erode easily. (Source: USGS New Jersey Geologic Map Data.) The primary soil type in the location of this collection is classified as Downer loamy sand, 0 to 5 percent slopes, Northern Coastal Plain. Downer Series soils are very deep, well-drained soils that are coarse-loamy, siliceous, semiactive, mesic Typic Hapludults. The upper strata of Downer Series from 0 to 25 cm is dark grayish brown, brown loamy sand that is dry with weak fine granular structure. It is very friable and strongly acid. Lower strata from 25 to 76 cm are yellowish brown single grain, loose loamy sand with few extremely weakly cemented masses of oxidized iron in the lower part. This layer is very strongly acid. (Source: NRCS Web Soil Survey.) | Wild material | | 2159117 | NA 88689 |
| 125 | NA 88692 | RJL2023NJ-005 | Ilex opaca Aiton | New Jersey, United States | NA | | | 2023 | COLLECTED | 11/10/2023 | Franklin Township: Piney Hollow Preservation Area (the site is owned by Franklin Township). This species was found on as well as below the dam at the far end of McCarthys Lakes. Plants accessed by foot along trails throughout property. | 39.57423200, -74.92525600 | 29 | Plants growing in part-shade to sun of the moist to saturated areas below the McCarthys Lakes dam in the wetlands associated with the New Squankum Branch. Plants were also found growing on the slopes of the dam in well-drained mesic to dry-mesic conditions. This species is clearly adaptable to a variety of conditions. Slope: 0 to 15 percent. Aspect: East. Elevation: 28 to 30 meters. NOTE: In addition to the soil type described below, this species was also growing on the slopes of a constructed earthen dam of unknown soil origin. The underlying geology of this area is of Middle Miocene, Serravallian origin and characterized as an Cohansey Formation. It is comprised of sand, white to yellow with local gravel and clay. Locally stained red or orange brown by iron oxides and (or) cemented into large blocks of ironstone. Unweathered clay is typically dark gray, but commonly weathers white where interbedded with thin beds of ironstone. Unit is a complex of interfingering marine and nonmarine facies. Sand is typically medium grained and moderately sorted although it ranges from fine to very coarse grained and from poorly to well sorted. Sand consists of quartz and siliceous rock fragments. Some beds are locally micaceous. In general, the sand is crossbedded, although the style of crossbedding varies significantly with the paleoenvironment. Trough crossbedding predominates, especially in the nonmarine channel fill deposits, and the scale of the crossbeds varies from small to large. Maximum thickness in the map area is about 60 m; however, thickness is difficult to determine because of the irregular basal contact and extensive post-depositional erosion. There is as much as 18 m of relief along the basal contact. The basal contact is sharp, undulatory, and directly overlain by a thin gravel bed. The Cohansey Formation unconformably overlies the Kirkwood Formation and is found in channels cut down into the Kirkwood. Where the Kirkwood consists of sandy, light-colored sediments, the basal contact of the Cohansey is drawn below crossbedded sediments. Where the Kirkwood consists of dark-colored silty beds, the basal contact is drawn between light-colored Cohansey sediments and the underlying dark-colored sediments. The Cohansey was markedly thinned because of erosion prior to deposition of overlying units in the western and southern parts of the southern sheet. The unit has been extensively eroded and stripped from large areas of the New Jersey Coastal Plain, particularly in the central sheet where outliers are common. In spite of its widespread nature, the Cohansey is poorly exposed because of its loose sandy composition, which causes it to erode easily. (Source: USGS New Jersey Geologic Map Data.) The primary soil type in the collection area is classified as Manahawkin Series muck, 0 to 2 percent slopes, frequently flooded, Northern Coastal Plain. Manahawkin Series soils are very deep, very poorly drained soils that are sandy or sandy-skeletal, siliceous, dysic, mesic Terric Haplosaprists high in organic deposits that are found in lake basins, back swamps, floodplains, and freshwater channels. The soils are classified in the dysic reaction class because pH in water dominantly ranges from 4.5 to 5.0. The zone from the soil surface to a depth of 200 cm is continuously saturated (endosaturation). The upper strata of Manahawkin Series from 0 to 76 cm is black broken face and rubbed muck; 10 percent fibers, less than 2 percent rubbed; moderate medium granular structure; mat of many fine roots; identifiable material is primarily herbaceous with a trace of woody fragments; 85-95 percent organic matter; extremely acid. Lower strata to 200 cm are gray sand, single grained and loose; strongly acid. (Source: NRCS Web Soil Survey.) | Wild material | | 2159120 | NA 88692 |
| 126 | NA 88693 | RJL2023NJ-006 | Clethra alnifolia L. | New Jersey, United States | NA | | | 2023 | COLLECTED | 11/10/2023 | Franklin Township: Piney Hollow Preservation Area (the site is owned by Franklin Township). Plants accessed by foot along trails throughout property. | 39.57319800, -74.92908900 | 29 | Plants growing in shade to part-shade over a wide range of habitats from mesic to mesic-dry as well as moist to wetland habitats. The woodlands are mostly deciduous, but also include occasional pine overstory. Slope: N/A. Aspect: N/A. The underlying geology of this area is of Middle Miocene, Serravallian origin and characterized as an Cohansey Formation. It is comprised of sand, white to yellow with local gravel and clay. Locally stained red or orange brown by iron oxides and (or) cemented into large blocks of ironstone. Unweathered clay is typically dark gray, but commonly weathers white where interbedded with thin beds of ironstone. Unit is a complex of interfingering marine and nonmarine facies. Sand is typically medium grained and moderately sorted although it ranges from fine to very coarse grained and from poorly to well sorted. Sand consists of quartz and siliceous rock fragments. Some beds are locally micaceous. In general, the sand is crossbedded, although the style of crossbedding varies significantly with the paleoenvironment. Trough crossbedding predominates, especially in the nonmarine channel fill deposits, and the scale of the crossbeds varies from small to large. Maximum thickness in the map area is about 60 m; however, thickness is difficult to determine because of the irregular basal contact and extensive post-depositional erosion. There is as much as 18 m of relief along the basal contact. The basal contact is sharp, undulatory, and directly overlain by a thin gravel bed. The Cohansey Formation unconformably overlies the Kirkwood Formation and is found in channels cut down into the Kirkwood. Where the Kirkwood consists of sandy, light-colored sediments, the basal contact of the Cohansey is drawn below crossbedded sediments. Where the Kirkwood consists of dark-colored silty beds, the basal contact is drawn between light-colored Cohansey sediments and the underlying dark-colored sediments. The Cohansey was markedly thinned because of erosion prior to deposition of overlying units in the western and southern parts of the southern sheet. The unit has been extensively eroded and stripped from large areas of the New Jersey Coastal Plain, particularly in the central sheet where outliers are common. In spite of its widespread nature, the Cohansey is poorly exposed because of its loose sandy composition, which causes it to erode easily. (Source: USGS New Jersey Geologic Map Data.) The primary soil types in the area of this collection is classified as Atsion sand, 0 to 2 percent slopes, Northern Tidewater Area and Downer loamy sand, 0 to 5 percent slopes, Northern Coastal Plain. Atsion Series soils are very deep, poorly drained with moderate to rapid permeability above 70 cm and slower beneath. They are classified as sandy, siliceous, mesic Aeric Alaquods. The upper stratum from 0 to 25 cm is dark gray sand, dry, single grained and lose with many fine roots. It is extremely acid. Lower strata are light gray to dark brown with small percentages of rounded quartzose pebbles and are extremely acid. Downer Series soils are very deep, well-drained soils that are coarse-loamy, siliceous, semiactive, mesic Typic Hapludults. The upper stratum of Downer Series from 0 to 25 cm is dark grayish brown, brown loamy sand that is dry with weak fine granular structure. It is very friable and strongly acid. Lower strata from 25 to 76 cm are yellowish brown single grain, loose loamy sand with few extremely weakly cemented masses of oxidized iron in the lower part. This layer is very strongly acid. (Source: NRCS Web Soil Survey.) | Wild material | | 2159121 | NA 88693 |
| 127 | NA 88694 | RJL2023NJ-007 | Spiraea tomentosa L. | New Jersey, United States | NA | | | 2023 | COLLECTED | 11/10/2023 | Franklin Township: Piney Hollow Preservation Area (the site is owned by Franklin Township). Plants accessed by foot along trails throughout property. | 39.57318200, -74.92673700 | 28 | Plants growing in part-shade to sun along the edges of McCarthys Lakes in moist-mesic to wet areas dominated by herbaceous plants. Slope: N/A. Aspect: N/A. | Wild material | | 2159122 | NA 88694 |
| 128 | NA 88695 | RJL2023NJ-008 | Aronia arbutifolia (L.) Pers. | New Jersey, United States | NA | | | 2023 | COLLECTED | 11/10/2023 | Franklin Township: Piney Hollow Preservation Area (the site is owned by Franklin Township). Plants accessed by foot along trails throughout property. | 39.57262400, -74.92606900 | 28 | Plants growing in part-shade to sun along the edges of McCarthys Lakes and in the understory of a mixed deciduous and evergreen forest in moist-mesic to wet conditions. Slope: N/A. Aspect: N/A. | Wild material | | 2159123 | NA 88695 |
| 129 | NA 88696 | RJL2023NCSC-001 | Rhododendron catawbiense Michx. | North Carolina, United States | NA | | | 2023 | COLLECTED | 11/12/2023 | Duke Forest property along New Hope Creek. The collection site is accesses by foot along trails. | 35.98317700, -79.01856200 | 103 | Plants growing in shade to part-shade of an upland very dry woodland habitat that is mostly deciduous. The site is steeply sloped underlain by rocky outcrop. Slope: 15 to 25 percent. Aspect: Northwest. The underlying geology of this area is of Cambrian/Late Proterozoic origin and characterized as a Metamorphosed Granitic Rock. It is megacrystic and well foliated; locally contains hornblende. Chapel Hill, Chatham, Farrington, Meadow Flats, Mt. Moriah, Parks Crossroads plutons, and Roxboro and Vance County suites. (Source: USGS North Carolina Geologic Map Data.) The primary soil type in the collection area is classified as Wedowee sandy loam, 15 to 25 percent slopes. Wedowee Series consists of very deep, well drained, moderately permeable soils that formed in residuum weathered from felsic igneous and metamorphic rocks of the Piedmont uplands. These soils are on narrow ridges and on side slopes of uplands. Slopes are dominantly 6 to 25 percent but ranges from 0 to 60 percent. The strata range from dark brown and brownish yellow to strong brown. They are mostly sandy loam; moderate fine granular structure; very friable; strongly acid. (Source: NRCS Web Soil Survey.) | Wild material | | 2159124 | NA 88696 |
| 130 | NA 88710 | RJL2023NCSC-015 | Cephalanthus occidentalis L. | South Carolina, United States | NA | | | 2023 | COLLECTED | 11/14/2023 | Francis Marion National Forest: plants growing in wetlands/swamps on US Forest Service Road 223 approximately 0.57 kilometers southeast from the junction with Halfway Creek Road. | 33.06771000, -79.67769700 | 20 | Plants are growing in part-shade to sun along the edges of the swamp in seasonally inundated acidic wetland habitat. Slope: N/A. Aspect: N/A. The underlying geology of this area is of Pleistocene origin and characterized as an Socastee Formation. This is a low coastal formation in the Carolinas like Penholoway but younger and lower in altitude. It is comprised primarily of unconsolidated, fine-detrital clay. It is described as variegated quartzose sands, argillaceous sands, and clays, 5 m thick at the type section near Socastee Swamp. (Source: USGS South Carolina Geologic Map Data.) The primary soil type in this collection area is classified as Rutlege Series loamy fine sand. Rutlege Series soils are very deep, very poorly drained soils that are sandy, siliceous, thermic Typic Humaquepts. Upper strata soils (0-38 cm) are black loamy sand with weak medium granular structure. They are loose and very strongly acid. Lower strata (38-175 cm) range from dark gray to dark brown sand that is single grained, loose, and very strongly acid. (Source: NRCS Web Soil Survey.) | Wild material | | 2159138 | NA 88710 |
| 131 | NA 88711 | RJL2023NCSC-016 | Ilex myrtifolia Walter | South Carolina, United States | NA | | | 2023 | COLLECTED | 11/14/2023 | Francis Marion National Forest: plants growing in wetlands/swamps on US Forest Service Road 223 approximately 0.57 kilometers southeast from the junction with Halfway Creek Road. | 33.06786200, -79.67761800 | 11 | Plants are growing in shade to part-shade in the swamp in seasonally inundated acidic wetland habitat. Slope: N/A. Aspect: N/A. The underlying geology of this area is of Pleistocene origin and characterized as an Socastee Formation. This is a low coastal formation in the Carolinas like Penholoway but younger and lower in altitude. It is comprised primarily of unconsolidated, fine-detrital clay. It is described as variegated quartzose sands, argillaceous sands, and clays, 5 m thick at the type section near Socastee Swamp. (Source: USGS South Carolina Geologic Map Data.) The primary soil type in this collection area is classified as Rutlege Series loamy fine sand. Rutlege Series soils are very deep, very poorly drained soils that are sandy, siliceous, thermic Typic Humaquepts. Upper strata soils (0-38 cm) are black loamy sand with weak medium granular structure. They are loose and very strongly acid. Lower strata (38-175 cm) range from dark gray to dark brown sand that is single grained, loose, and very strongly acid. (Source: NRCS Web Soil Survey.) | Wild material | | 2159139 | NA 88711 |
| 132 | NA 88712 | RJL2023NCSC-017 | Itea virginica L. | South Carolina, United States | NA | | | 2023 | COLLECTED | 11/14/2023 | Francis Marion National Forest: plants growing in wetlands/swamps on US Forest Service Road 223 approximately 0.57 kilometers southeast from the junction with Halfway Creek Road. | 33.06755600, -79.67789100 | 11 | Plants are growing in the understory of the acidic swamp that is seasonally inundated in shade. Slope: N/A. Aspect: N/A. The underlying geology of this area is of Pleistocene origin and characterized as an Socastee Formation. This is a low coastal formation in the Carolinas like Penholoway but younger and lower in altitude. It is comprised primarily of unconsolidated, fine-detrital clay. It is described as variegated quartzose sands, argillaceous sands, and clays, 5 m thick at the type section near Socastee Swamp. (Source: USGS South Carolina Geologic Map Data.) The primary soil type in this collection area is classified as Rutlege Series loamy fine sand. Rutlege Series soils are very deep, very poorly drained soils that are sandy, siliceous, thermic Typic Humaquepts. Upper strata soils (0-38 cm) are black loamy sand with weak medium granular structure. They are loose and very strongly acid. Lower strata (38-175 cm) range from dark gray to dark brown sand that is single grained, loose, and very strongly acid. (Source: NRCS Web Soil Survey.) | Wild material | | 2159140 | NA 88712 |
| 133 | NA 88713 | RJL2023NCSC-018 | Ilex opaca Aiton | South Carolina, United States | NA | | | 2023 | COLLECTED | 11/14/2023 | Francis Marion National Forest: plants growing in wetlands/swamps on US Forest Service Road 223 approximately 0.57 kilometers southeast from the junction with Halfway Creek Road. | 33.06783000, -79.67749100 | 11 | Plants are growing in part shade to shade of a swamp in seasonally inundated acidic wetland habitat. Slope: N/A. Aspect: N/A. The underlying geology of this area is of Pleistocene origin and characterized as an Socastee Formation. This is a low coastal formation in the Carolinas like Penholoway but younger and lower in altitude. It is comprised primarily of unconsolidated, fine-detrital clay. It is described as variegated quartzose sands, argillaceous sands, and clays, 5 m thick at the type section near Socastee Swamp. (Source: USGS South Carolina Geologic Map Data.) The primary soil type in this collection area is classified as Rutlege Series loamy fine sand. Rutlege Series soils are very deep, very poorly drained soils that are sandy, siliceous, thermic Typic Humaquepts. Upper strata soils (0-38 cm) are black loamy sand with weak medium granular structure. They are loose and very strongly acid. Lower strata (38-175 cm) range from dark gray to dark brown sand that is single grained, loose, and very strongly acid. (Source: NRCS Web Soil Survey.) | Wild material | | 2159141 | NA 88713 |
| 134 | NA 88714 | RJL2023NCSC-019 | Smilax walteri Pursh | South Carolina, United States | NA | | | 2023 | COLLECTED | 11/14/2023 | Francis Marion National Forest: plants growing in wetlands/swamps on US Forest Service Road 223 approximately 0.57 kilometers southeast from the junction with Halfway Creek Road. | 33.06757700, -79.67792800 | 11 | Plants are growing in shade, part-shade and sun in the acid soils of a swamp and along the edges of the swamp where the soils are seasonally inundated. Slope: N/A. Aspect: N/A. The underlying geology of this area is of Pleistocene origin and characterized as a Socastee Formation. This is a low coastal formation in the Carolinas like Penholoway but younger and lower in altitude. It is comprised primarily of unconsolidated, fine-detrital clay. It is described as variegated quartzose sands, argillaceous sands, and clays, 5 m thick at the type section near Socastee Swamp. (Source: USGS South Carolina Geologic Map Data.) The primary soil type in this collection area is classified as Rutlege Series loamy fine sand. Rutlege Series soils are very deep, very poorly drained soils that are sandy, siliceous, thermic Typic Humaquepts. Upper strata soils (0-38 cm) are black loamy sand with weak medium granular structure. They are loose and very strongly acid. Lower strata (38-175 cm) range from dark gray to dark brown sand that is single grained, loose, and very strongly acid. (Source: NRCS Web Soil Survey.) | Wild material | | 2159142 | NA 88714 |
| 135 | NA 88719 | RJL2023NCSC-024 | Ilex laevigata (Pursh) A. Gray | South Carolina, United States | NA | | | 2023 | COLLECTED | 11/15/2023 | Little Pee Dee Heritage Preserve/Wildlife Management Area (South Carolina Department of Natural Resources Public Lands, on South Carolina Highway 917). | 34.14123300, -79.19532100 | 13 | Plants growing in high understory shade to part-shade of a moist to relatively dry pine forest with occasional deciduous trees. The litter layer in the woodlands is very deep with longleaf pine needles, while the edges of the woodlands are much drier with exposed white sand and little to no litter layer. Slope: N/A. Aspect: N/A. The underlying geology of this area is of Pleistocene origin and characterized as Waccamaw Formation. This formation is another Carolina coastalized terrace that is deeply weathered. It is characterized by unconsolidated, coarse-detrital, soft sand limestones and loose gray to buff fine quartz sands in which occasional small quartz pebbles are present. It also includes sedimentary, carbonate, soft limestones. (Source: USGS South Carolina Geologic Map Data.) The primary soil type in this collection area is classified as Lynn Haven Series sand. The Lynn Haven Series consists of very deep, poorly and very poorly drained, moderate or moderately rapid, permeable soils in low areas and depressions in Atlantic Flatwoods and the Gulf. They formed in thick deposits of sandy marine sediments. Th Lynn Haven Series soil is approximately 2 m thick and ranges from black near the surface to yellow brown in the deepest strata. Most of the strata are comprised of fine sands that are friable with the deepest strata also including a small percentage of organic matter. Reaction ranges from extremely acid to strongly acid throughout the profile. The water table is at 0-15 cm for periods of 2 to 6 months annually and within a depth 1 m for more than 6 months during most years; during extended dry periods it is below 1 meter. Depressional areas are ponded for long duration in most years. (Source: NRCS Web Soil Survey.) | Wild material | | 2159147 | NA 88719 |
| 136 | NA 88720 | RJL2023NCSC-025 | Zenobia pulverulenta (W. Bartram ex Willd.) Pollard | South Carolina, United States | NA | | | 2023 | COLLECTED | 11/15/2023 | Little Pee Dee Heritage Preserve/Wildlife Management Area (South Carolina Department of Natural Resources Public Lands, on South Carolina Highway 917). | 34.13990000, -79.19691700 | 14 | Plants growing in high understory shade to part-shade of a moist to relatively dry pine forest with occasional deciduous trees. The litter layer in the woodlands is very deep with longleaf pine needles, while the edges of the woodland are much drier with exposed white sand and little to no litter layer. Slope: N/A. Aspect: N/A. The underlying geology of this area is of Pleistocene origin and characterized as Waccamaw Formation. This formation is another Carolina coastalized terrace that is deeply weathered. It is characterized by unconsolidated, coarse-detrital, soft sand limestones and loose gray to buff fine quartz sands in which occasional small quartz pebbles are present. It also includes sedimentary, carbonate, soft limestones. (Source: USGS South Carolina Geologic Map Data.) The primary soil type in this collection area is classified as Lynn Haven Series sand. The Lynn Haven Series consists of very deep, poorly and very poorly drained, moderate or moderately rapid, permeable soils in low areas and depressions in Atlantic Flatwoods and the Gulf. They formed in thick deposits of sandy marine sediments. Th Lynn Haven Series soil is approximately 2 m thick and ranges from black near the surface to yellow brown in the deepest strata. Most of the strata are comprised of fine sands that are friable with the deepest strata also including a small percentage of organic matter. Reaction ranges from extremely acid to strongly acid throughout the profile. The water table is at 0-15 cm for periods of 2 to 6 months annually and within a depth 1 m for more than 6 months during most years; during extended dry periods it is below 1 meter. Depressional areas are ponded for long duration in most years. (Source: NRCS Web Soil Survey.) | Wild material | | 2159148 | NA 88720 |
| 137 | NA 88721 | RJL2023NCSC-026 | Ilex opaca Aiton | South Carolina, United States | NA | | | 2023 | COLLECTED | 11/15/2023 | Little Pee Dee Heritage Preserve/Wildlife Management Area (South Carolina Department of Natural Resources Public Lands, on South Carolina Highway 917). | 34.14091500, -79.19555200 | 13 | Plants growing in high understory shade to part-shade of a moist to relatively dry pine forest with occasional deciduous trees. The litter layer in the woodlands is very deep with longleaf pine needles, while the edges of the woodlands are much drier with exposed white sand and little to no litter layer. Slope: N/A. Aspect: N/A. The underlying geology of this area is of Pleistocene origin and characterized as Waccamaw Formation. This formation is another Carolina coastalized terrace that is deeply weathered. It is characterized by unconsolidated, coarse-detrital, soft sand limestones and loose gray to buff fine quartz sands in which occasional small quartz pebbles are present. It also includes sedimentary, carbonate, soft limestones. (Source: USGS South Carolina Geologic Map Data.) The primary soil type in this collection area is classified as Lynn Haven Series sand. The Lynn Haven Series consists of very deep, poorly and very poorly drained, moderate or moderately rapid, permeable soils in low areas and depressions in Atlantic Flatwoods and the Gulf. They formed in thick deposits of sandy marine sediments. Th Lynn Haven Series soil is approximately 2 m thick and ranges from black near the surface to yellow brown in the deepest strata. Most of the strata are comprised of fine sands that are friable with the deepest strata also including a small percentage of organic matter. Reaction ranges from extremely acid to strongly acid throughout the profile. The water table is at 0-15 cm for periods of 2 to 6 months annually and within a depth 1 m for more than 6 months during most years; during extended dry periods it is below 1 meter. Depressional areas are ponded for long duration in most years. (Source: NRCS Web Soil Survey.) | Wild material | | 2159149 | NA 88721 |
| 138 | NA 88686 | TJK2023FL-033 | Ilex glabra (L.) A. Gray | Florida, United States | NA | | | 2023 | COLLECTED | 11/18/2023 | Navarre, Florida: Adams St. cul-de-sac, on nine-acre private property. Infrastructure development began and was terminated due to the lack of any engineering or environmental site planning (designated wetland status). It has remained idle for a number of years. | 30.40970000, -86.92980000 | 11 | Wet pine flatwood transitioning to a shrub bog habitat under fire suppression. Slope: 3.5%. Aspect: West. Elevation: 36 feet. | Wild material | | 2159098 | NA 88686 |
| 139 | NA 88687 | TJK2023FL-034 | Clethra alnifolia L. | Florida, United States | NA | | | 2023 | COLLECTED | 11/18/2023 | Navarre, Florida: Adams St. cul-de-sac, on nine-acre private property. Infrastructure development began and was terminated due to the lack of any engineering or environmental site planning (designated wetland status). It has remained idle for a number of years. | 30.41000000, -86.92890000 | 11 | Wet Pine Flatwood transitioning to a shrub bog habitat under fire suppression. Slope: less than 2%. Aspect: North. Elevation: 36 feet. | Wild material | | 2159099 | NA 88687 |
| 140 | NA 88671 | RJL2023PA-005 | Rhododendron maximum L. | Pennsylvania, United States | NA | | | 2023 | COLLECTED | 10/16/2023 | Appalachian National Scenic Trail: Pulpit Rock and Pinnacle Loop. Rocky woodlands along Furnace Creek as well as steep rocky slopes above Pulpit Rock Reservoir associated with the Pulpit Rock and Pinnacle Loop Trail. | 40.59226100, -75.94588800 | 301 | Well-drained and very rocky dry deciduous woodlands in part shade to full shade. Slope: 0-30%. Aspect: variable. The underlying geology of this area is of Silurian origin and characterized as the Shawangunk Formation. It is characterized by light- to dark-gray, fine- to very coarse-grained sandstone and conglomerate containing thin shale interbeds. Includes four members, in descending order: Tammany--conglomerate and sandstone; Lizard Creek--sandstone and red or green shale; Minsi--sandstone and conglomerate; Weiders--conglomerate. Tammany and Lizard Creek Members together are approximately equivalent to Clinton Group to the west; Minsi and Weiders Members together are equivalent to Tuscarora Formation to the west. (Source: USGS Pennsylvania Geologic Map Data). The primary soil type in the collection area is classified as Hazleton Series. The Hazleton series consists of deep and very deep, well drained soils formed in residuum of acid gray, brown or red sandstone on uplands. Slope ranges from 0 to 80 percent. Permeability is moderately rapid to rapid. Solum thickness ranges from 60 to 120 centimeters. Depth to lithic contact ranges from 1 to 2 meters. Rock fragments of angular sandstone, dominantly less than 25 cm in size, range from 5 to 70 percent in individual horizons. Boulders, stones, flags and channers cover about 5 to 60 percent of the surface of some pedons. Reaction ranges from strongly acid through extremely acid throughout. (Source: NRCS Web Soil Survey). | Wild material | | 2159062 | NA 88671 |
| 141 | NA 88672 | RJL2023PA-006 | Rhododendron periclymenoides (Michx.) Shinners | Pennsylvania, United States | NA | | | 2023 | COLLECTED | 10/16/2023 | Appalachian National Scenic Trail: Pulpit Rock and Pinnacle Loop. Rocky woodland edges above Furnace Creek around Pulpit Rock and Pinnacle Loop Trail. | 40.58668200, -75.94269600 | 247 | Well-drained and very rocky dry deciduous woodlands in part shade to full shade. Slope: 10%. Aspect: East. The underlying geology of this area is of Silurian origin and characterized as the Shawangunk Formation. It is characterized by light- to dark-gray, fine- to very coarse-grained sandstone and conglomerate containing thin shale interbeds. Includes four members, in descending order: Tammany--conglomerate and sandstone; Lizard Creek--sandstone and red or green shale; Minsi--sandstone and conglomerate; Weiders--conglomerate. Tammany and Lizard Creek Members together are approximately equivalent to Clinton Group to the west; Minsi and Weiders Members together are equivalent to Tuscarora Formation to the west. (Source: USGS Pennsylvania Geologic Map Data). The primary soil type in the collection area is classified as Hazleton Series. The Hazleton series consists of deep and very deep, well drained soils formed in residuum of acid gray, brown or red sandstone on uplands. Slope ranges from 0 to 80 percent. Permeability is moderately rapid to rapid. Solum thickness ranges from 60 to 120 centimeters. Depth to lithic contact ranges from 1 to 2 meters. Rock fragments of angular sandstone, dominantly less than 25 cm in size, range from 5 to 70 percent in individual horizons. Boulders, stones, flags and channers cover about 5 to 60 percent of the surface of some pedons. Reaction ranges from strongly acid through extremely acid throughout. (Source: NRCS Web Soil Survey). | Wild material | | 2159063 | NA 88672 |
| 142 | NA 88673 | RJL2023PA-007 | Rhododendron pilosum (Michx.) Craven | Pennsylvania, United States | NA | | | 2023 | COLLECTED | 10/25/2023 | Ned Smith Center for Art and Nature. | 40.53367300, -76.92715700 | 147 | Well-drained and very rocky, dry slopes above 10-50 meters above Wiconisco Creek in mixed deciduous and evergreen woodlands in part shade to full shade. Slope: 10-40%. Aspect: North. The underlying geology of this area is of Mississippian origin and characterized as the Pocono Formation. It is comprised of light-gray to buff or light-olive-gray, medium-grained, crossbedded sandstone and minor siltstone; commonly conglomeratic at base and in middle; medial conglomerate, where present, is used to divide into Mount Carbon and Beckville Members; equivalent to Burgoon Sandstone of Allegheny Plateau. (Source: USGS Pennsylvania Geologic Map Data). The primary soil type in the collection area is classified as Laidig Series. The Laidig series consists of very deep, well drained soils formed in colluvium from sandstone, siltstone, and some shale. They are gently sloping to very steep soils on benches and foot slopes. Permeability is moderate or moderately rapid above the fragipan and moderately slow or slow in the fragipan. Slope ranges from 0 to 55 percent. Solum thickness ranges from 1.25 to 2.0 meters or more. Depth to the fragipan ranges from 0.75 to 1.25 meters. The particle-size control section averages less than 35 percent rock fragments. Rock fragments range from 5 to 50 percent in individual subhorizons of the A, E, BE, BA and Bt horizons; 15 to 70 percent in individual subhorizons of the Btx horizon; and 20 to 70 percent in the C horizon. Rock fragments are mostly sandstone but include siltstone and shale. Rock fragments include channers, cobbles, flagstones, and stones. Soils range from extremely acid through strongly acid throughout. (Source: NRCS Web Soil Survey). | Wild material | | 2159064 | NA 88673 |
| 143 | NA 88674 | RJL2023PA-008 | Kalmia latifolia L. | Pennsylvania, United States | NA | | | 2023 | COLLECTED | 10/25/2023 | Ned Smith Center for Art and Nature. | 40.53463500, -76.92616300 | 130 | Well-drained and very rocky, dry slopes above 10-50 meters above Wiconisco Creek in mixed deciduous and evergreen woodlands in part shade to full shade. Slope: 10-40%. Aspect: North. The underlying geology of this area is of Mississippian origin and characterized as the Pocono Formation. It is comprised of light-gray to buff or light-olive-gray, medium-grained, crossbedded sandstone and minor siltstone; commonly conglomeratic at base and in middle; medial conglomerate, where present, is used to divide into Mount Carbon and Beckville Members; equivalent to Burgoon Sandstone of Allegheny Plateau. (Source: USGS Pennsylvania Geologic Map Data). The primary soil type in the collection area is classified as Laidig Series. The Laidig series consists of very deep, well drained soils formed in colluvium from sandstone, siltstone, and some shale. They are gently sloping to very steep soils on benches and foot slopes. Permeability is moderate or moderately rapid above the fragipan and moderately slow or slow in the fragipan. Slope ranges from 0 to 55 percent. Solum thickness ranges from 1.25 to 2.0 meters or more. Depth to the fragipan ranges from 0.75 to 1.25 meters. The particle-size control section averages less than 35 percent rock fragments. Rock fragments range from 5 to 50 percent in individual subhorizons of the A, E, BE, BA and Bt horizons; 15 to 70 percent in individual subhorizons of the Btx horizon; and 20 to 70 percent in the C horizon. Rock fragments are mostly sandstone but include siltstone and shale. Rock fragments include channers, cobbles, flagstones, and stones. Soils range from extremely acid through strongly acid throughout. (Source: NRCS Web Soil Survey). | Wild material | | 2159065 | NA 88674 |
| 144 | NA 88675 | RJL2023PA-009 | Viburnum acerifolium L. | Pennsylvania, United States | NA | | | 2023 | COLLECTED | 10/25/2023 | Ned Smith Center for Art and Nature. | 40.53539200, -76.92313500 | 136 | Well-drained and very rocky dry deciduous woodlands in part shade to full shade. Slope: 10-30%. Aspect: North. The underlying geology of this area is of Mississippian origin and characterized as the Pocono Formation. It is comprised of light-gray to buff or light-olive-gray, medium-grained, crossbedded sandstone and minor siltstone; commonly conglomeratic at base and in middle; medial conglomerate, where present, is used to divide into Mount Carbon and Beckville Members; equivalent to Burgoon Sandstone of Allegheny Plateau. (Source: USGS Pennsylvania Geologic Map Data). The primary soil type in the collection area is classified as Laidig Series. The Laidig series consists of very deep, well drained soils formed in colluvium from sandstone, siltstone, and some shale. They are gently sloping to very steep soils on benches and foot slopes. Permeability is moderate or moderately rapid above the fragipan and moderately slow or slow in the fragipan. Slope ranges from 0 to 55 percent. Solum thickness ranges from 1.25 to 2.0 meters or more. Depth to the fragipan ranges from 0.75 to 1.25 meters. The particle-size control section averages less than 35 percent rock fragments. Rock fragments range from 5 to 50 percent in individual subhorizons of the A, E, BE, BA and Bt horizons; 15 to 70 percent in individual subhorizons of the Btx horizon; and 20 to 70 percent in the C horizon. Rock fragments are mostly sandstone but include siltstone and shale. Rock fragments include channers, cobbles, flagstones, and stones. Soils range from extremely acid through strongly acid throughout. (Source: NRCS Web Soil Survey). | Wild material | | 2159066 | NA 88675 |
| 145 | NA 88677 | RJL2023PA-011 | Hydrangea arborescens L. | Pennsylvania, United States | NA | | | 2023 | COLLECTED | 10/25/2023 | Seed collected along the Appalachian National Scenic Trail, accessed from the Duncannon Entrance. | 40.37735300, -77.03997300 | 239 | Well-drained and very rocky dry deciduous woodlands in part shade to full shade. Slope: 20-50%. Aspect: Northwest. The underlying geology of this area is of Devonian origin and characterized as the Duncannon Member of Catskill Formation. It is characterized by grayish-red sandstone, siltstone, and mudstone in fining-upward cycles; conglomerate occurs at base of some cycles. The sandstones which comprise the Duncannon Member are fine to very coarse grained and grayish red to grayish red-purple in color. The Duncannon Member is known to be crossbedded to planar bedded in beds anywhere from 3 to 9 meters thick. Conglomerates have been spotted at the base of the Duncannon Member. The Duncannon Member is poorly exposed in most areas except along the Lehigh River. The conglomerate portion of this member has been known to form ridges and ledges with thicknesses approaching 228 meters. (Source: USGS Pennsylvania Geologic Map Data). The primary soil type in the collection area is classified as Dystrochrepts, boulder soils. These soils are characterized by coarse-silty loess over residuum weathered from sedimentary rock and located on steep ridges along the upper third of the mountainflank. These soils are comprised of cobbles, stones or boulders (9%), well-drained, and approximately 1 meter or less to lithic bedrock. (Source: NRCS Web Soil Survey). | Wild material | | 2159068 | NA 88677 |
| 146 | NA 88678 | RJL2023PA-012 | Viburnum acerifolium L. | Pennsylvania, United States | NA | | | 2023 | COLLECTED | 10/27/2023 | Slopes on the east side of Creek Road above the North Branch of White Clay Creek. | 39.78552600, -75.80251900 | 90 | Well-drained mesic-dry to rocky dry deciduous woodlands in part shade to full shade. Slope: 15-35%. Aspect: West to northwest. The underlying geology of this area includes two formations. The first and primary formation is Lower Paleozoic Glenarm Wissahickon Formation, lithologically similar to oligoclase-mica schist of the Wissahickon Formation, but also includes lenticular amphibolite bodies having ocean-floor basalt chemistry. The second formation is Lower Paleozoic Mafic Gneiss Formation that is dark and medium grained. It includes rocks of probable sedimentary origin. (Sources: USGS Pennsylvania Geologic Map Data). The primary soil type in the collection area is classified as Manor Series. The Manor Series consists of well-drained residuum weathered from micaceous schist. Soils in the upper pedon (0-33 cm) are very dark grayish brown loam with strong fine granular structure; also, very friable with fine mica flakes and strongly acid. Lower pedon soils (34-56 cm) are strong brown, sandy loams. They have weak medium sub-angular blocky structure, are friable with many fine and a few medium mica flakes; this pedon is very strongly acid. (Source: NRCS Web Soil Survey). | Wild material | | 2159069 | NA 88678 |
| 147 | NA 88680 | RJL2023PA-014 | Kalmia latifolia L. | Pennsylvania, United States | NA | | | 2023 | COLLECTED | 10/30/2023 | West side of Pennsylvania Route 487 within the boundary of Ricketts Glen State Park. | 41.31733100, -76.30259500 | 699 | Growing in dense thickets in well-drained habitat in a mixed evergreen and deciduous woodland on shallow to moderate slopes. Slope: 3-8%. Aspect: various. The underlying geology of this area is of Mississippian and Devonian origin and characterized as the Huntley Mountain Formation. It is comprised of greenish-gray and light-olive-gray, flaggy, fine-grained sandstone, siltstone, and a few red shale interbeds; includes lower "Pocono" plus "Oswayo" of earlier workers. This formation forms a transition between Catskill Formation and Burgoon Sandstone. (Source: USGS Pennsylvania Geologic Map Data). The primary soil type in the collection area is classified as Oquaga and Lordstown Series. The Oquaga Series consists of moderately deep, somewhat excessively drained and well drained soils formed in a thin mantle of till over sandstone, siltstone, and shale bedrock on nearly level to very steep uplands. Slope ranges from 0 to 70 percent. Depth to bedrock ranges from 50 to 100 cm. Content of rock fragments ranges from 15 to 60 percent in surface horizons and from 25 to 70 percent in the subsoil, and 25 to 85 percent in the substratum. Soil reaction ranges from extremely acid to moderately acid. The Lordstown series consists of moderately deep, well drained soils formed in till and cryoturbated material derived from siltstone and sandstone on bedrock-controlled landforms of glaciated dissected plateaus. They are nearly level to very steep soils on hillsides and hilltops in glaciated bedrock-controlled uplands. Slope ranges from 0 to 90 percent. Thickness of solum and depth to bedrock ranges from 51 to 102 cm. Rock fragments are dominantly flat angular fragments and flagstones and occupy 10 to 35 percent of the volume in the Ap horizon and 20 to 60 percent in the B and C horizons. Reaction is very strongly acid through neutral in the surface layer, very strongly acid to moderately acid in the subsoil and strongly acid or moderately acid in the substratum. (Source: NRCS Web Soil Survey). | Wild material | | 2159071 | NA 88680 |
| 148 | NA 88681 | RJL2023PA-015 | Ilex verticillata (L.) A. Gray | Pennsylvania, United States | NA | | | 2023 | COLLECTED | 10/30/2023 | Wetlands near Phillips Creek: seed collected from plants on the north and south (further east) side of Pennsylvania Route 188 approximately 6.9 kilometers east of the junction with Pennsylvania Route 487. | 41.30353100, -76.22452800 | 381 | Boggy to moist habitats associated with wetlands of Phillips Creek in shade to full sun next to the road. Slope: 0%. Aspect: various. The underlying geology of this area is of Devonian origin and characterized as the Catskill Formation. It is comprised of grayish-red sandstone, siltstone, shale, and mudstone; units of gray sandstone occur in upper part; lithologies in upper part arranged in fining-upward cycles. In the Altoona area, the Catskill Formation is mapped as the Duncannon, Sherman Creek, and Irish Valley Members, which are described under "Central and Eastern Pennsylvania" provinces. (Source: USGS Pennsylvania Geologic Map Data). The primary soil type in the collection area is classified as Wellsboro Series. The Wellsboro Series consists of very deep, moderately well- and somewhat poorly-drained soils formed in till derived from red sandstone, siltstone, and shale. Slope ranges from 0 to 50 percent. Saturated hydraulic conductivity is moderately high or high in the mineral surface layer, subsurface layer, and upper part of the subsoil; and low or moderately low in the lower part of the subsoil (fragipan) and the substratum. Solum thickness is greater than 102 cm. Depth to the fragipan ranges from 36 to 76 cm. Depth to bedrock is 152 cm or more. Rock fragments of subangular and rounded sandstone, siltstone or shale range from 5 to 40 percent in the A and B horizons, and from 15 to 50 percent in the Bx and C horizons. Typically, rock fragments average about 5 to 25 percent by volume above the fragipan and 15 to 40 percent by volume in and below the fragipan. Reaction commonly ranges from very strongly acid through moderately acid. (Source: NRCS Web Soil Survey). | Wild material | | 2159072 | NA 88681 |
| 149 | WLP 3280 | TJK2023FL-028 | Kalmia hirsuta Walter | Florida, United States | NA | | | 2023 | COLLECTED | 11/02/2023 | Navarre, Florida: Adams St. cul-de-sac, on nine-acre private property. Infrastructure development began and was terminated due to the lack of any engineering or environmental site planning (designated wetland status). It has remained idle for a number of years. | 30.41080000, -86.92840000 | 11 | Wet Pine Flatwood transitioning to a shrub bog habitat under fire suppression. Slope: flat. Aspect: East Elevation: 36 feet. | Wild material | | 2159060 | WLP 3280 |
| 150 | NA 88669 | TXWL2023-012 | Ilex decidua Walter | Texas, United States | NA | | | 2023 | COLLECTED | 10/21/2023 | County Road 3218 en route to Camp Wohaleta, north of Caddo National Grasslands. | 33.75626700, -95.97888900 | | Roadside. | Wild material | | 2159044 | NA 88669 |
| 151 | NA 89011 | TJK2023FL-019 | Kalmia hirsuta Walter | Florida, United States | NA | | | 2023 | COLLECTED | 10/10/2023 | Blackwater State Forest, a few hundred yards from Juniper Creek. | 30.80110600, -86.89107500 | 15 | Elevation: 52 feet. Slope: 0%. Aspect: Southeast. | Wild material | | 2158904 | NA 89011 |
| 152 | NA 89013 | TJK2023FL-021 | Smilax pumila Walter | Florida, United States | NA | | | 2023 | COLLECTED | 10/15/2023 | Collected at 1985 Reagan Rd in Navarre, Florida. | 30.40680000, -86.93090000 | 9 | Disturbed native residential woods. Elevation: 32 feet. Slope: 3%. Aspect: Southeast. | Wild material | | 2158906 | NA 89013 |
| 153 | NA 88667 | RJL2023PA-004 | Viburnum acerifolium L. | Pennsylvania, United States | NA | | | 2023 | | | | | | | Wild material | | 2158816 | NA 88667 |
| 154 | NA 88665 | RJL2023PA-002 | Ilex verticillata (L.) A. Gray | Pennsylvania, United States | NA | | | 2023 | COLLECTED | 10/01/2023 | Woodlands along Pine Creek near the Harmonyville Road bridge. | 40.18764500, -75.76732200 | 141 | Moist to mucky, wet woodland conditions along Pine Creek. Much of the site is very wet due to recent rains; though, earlier in the year, the soils were only moist. Plants grow in both well-drained mesic conditions as well as seasonally wet conditions. They do not grow in standing water anywhere in this location. Plants in this population are found mostly in the shade and partial shade of deciduous trees; there are occasional gaps that offer higher light conditions as well. Slope: 0-2%. Aspect: N/A. The underlying geology of this area is of Precambrian origin and characterized as the Graphitic Felsic Gneiss. This includes Pickering Gneiss and small areas of marble; dominantly quartz and feldspar with varying amounts of graphite and various metamorphic minerals; medium grained, light to dark gray and greenish gray; sedimentary origin. (Source: USGS Pennsylvania Geologic Map Data). The primary soil type in the area of this collection is classified as Hatboro Silt Loam Series. The Hatboro Series consists of very deep and poorly drained soils formed in alluvium derived from metamorphic and crystalline rock. They are on flood plains. Slopes range from 0 to 3 percent. Saturated hydraulic conductivity is moderately high to high. Solum thickness ranges from 50 to 150 cm. Depth to bedrock ranges from 1.5 to 3 meters or more. Organic carbon decreases irregularly with depth or is greater than 0.2 percent directly above any strongly contrasting C horizon. The depth to strongly contrasting sand and gravel is more than 100 cm or the transition is greater than 12.5 cm. Content of gravel ranges from 0 to 10 percent in the solum and from 0 to 80 percent in the C horizon. Mica flakes are common in the solum, and the C horizon contains thin lenses of mica. Reaction ranges from very strongly acid through neutral to a depth of 75 cm and from moderately acid through slightly acid below 75 cm. (Source: NRCS Web Soil Survey.) | Wild material | | 2158814 | NA 88665 |
| 155 | NA 88664 | RJL2023PA-001 | Viburnum acerifolium L. | Pennsylvania, United States | NA | | | 2023 | COLLECTED | 10/01/2023 | Seed collected from plants growing along a two-mile stretch of Harmonyville Road on the woodland edge next to the road. [Note: latitude and longitude were collected at the location of the largest seed collection.] | 40.18482200, -75.78145100 | 158 | Plants were growing in well-drained and rocky mesic-dry woodlands from part shade along the road edge to full shade in the understory of the woodlands. Slope: 2-10%. Aspect: Variable. The underlying geology of this area is of Triassic origin and characterized as the Stockton Formation. It is characterized by light-gray to buff, coarse-grained, arkosic sandstone; includes reddish-brown to grayish-purple sandstone, siltstone, and mudstone. (Source: USGS Pennsylvania Geologic Map Data.) The primary soil type in the area of this collection is classified as Edgemont Channery Sandy Loam Series (8 to 25 percent slopes), extremely stony. The Edgemont Series consists of deep and very deep, well drained soils formed in the weathered residuum of quartzitic rocks. They have moderately high to high saturated hydraulic conductivity. Slopes range from 0 to 70 percent. Solum thickness ranges from 50 to 10 cm. Depth to bedrock ranges from about 1.5 to 2.2 meters. Kaolinite is the dominant mineral in the clay fraction with detectable amounts of illite, vermiculite, montmorillonite, chlorite and interstratified clays. Gravel, channers, and stone size fragments of quartzite and quartz are present throughout the profile. Rock fragments range from 5 to 40 percent in the horizons of the solum and from 10 to 90 percent in the C horizon. Reaction ranges from extremely acid to strongly acid throughout. (Source: NRCS Web Soil Survey.) | Wild material | | 2158813 | NA 88664 |
| 156 | NA 88658 | TJK2023FL-012 | Ilex verticillata (L.) A. Gray | Florida, United States | NA | | | 2023 | COLLECTED | 09/10/2023 | Lower Yellow River. | 30.62868600, -86.80748000 | 3 | Beautiful riverine system. Elevation: 13 feet. Slope: 0 (none). Aspect: Northwest. | Wild material | | 2158792 | NA 88658 |
| 157 | NA 88659 | TJK2023FL-013 | Ilex sp. | Florida, United States | NA | | | 2023 | COLLECTED | 09/15/2023 | Lower Yellow River. | 30.58170000, -86.91770000 | 1 | Elevation: 3 feet. Slope: 0 percent. Aspect: North. | Wild material | | 2158793 | NA 88659 |
| 158 | NA 88660 | TJK2023FL-014 | Rhododendron austrinum (Small) Rehder | Florida, United States | NA | | | 2023 | COLLECTED | 09/15/2023 | Lower Yellow River, Grimes Lake. | 30.61930000, -86.81490000 | 3 | Elevation: 13 feet. Slope: 0 percent. Aspect: West-southwest. | Wild material | | 2158794 | NA 88660 |
| 159 | NA 88663 | TJK2023FL-017 | Rhododendron austrinum (Small) Rehder | Florida, United States | NA | | | 2023 | COLLECTED | 09/17/2023 | Lower Yellow River, below the Old Land Place. | 30.55513000, -86.94659000 | 0 | An area with very nice Pink R. austrinum. Elevation: 0. Slope: 0 percent. Aspect: South-southwest. | Wild material | | 2158797 | NA 88663 |
| 160 | OPGC 8853 | JDC/AA/2023/078/1110 | Arnoglossum atriplicifolium (L.) H. Rob. | Iowa, United States | OPGC | | | 2023 | COLLECTED | 09/21/2023 | Iowa Army Ammunition Plant located 5.09 miles southwest of Burlington along south side of road, Union Township T69N R3W SE 1/4 SE 1/4 SW 1/4 Sec. 7 | 40.78416600, -91.24800000 | 191 | Woodland edges/roadsides. | Wild material | | 2159005 | OPGC 8853 |
| 161 | NA 88602 | KY23-003 | Oxydendrum arboreum (L.) DC. | Kentucky, United States | NA | | | 2023 | COLLECTED | 09/08/2023 | Warbler Ridge Preserve, Pine Mountain | 36.96943000, -83.08047000 | 791 | Rock outcrop on Pine Mountain (oak/pine barren). Elevation: 2594 feet. Aspect: Southeast. | Wild material | | 2158693 | NA 88602 |
| 162 | NA 88603 | KY23-005 | Aronia melanocarpa (Michx.) Elliott | Kentucky, United States | NA | | | 2023 | COLLECTED | 09/08/2023 | Warbler Ridge Preserve, Pine Mountain | 36.96937000, -83.08034000 | 787 | Rock outcrop on Pine Mountain. Elevation: 2581 feet. Aspect: Southeast. | Wild material | Initial identification: Aronia arbutifolia | 2158695 | NA 88603 |
| 163 | NA 88615 | KY23-019 | Mitchella repens L. | Kentucky, United States | NA | | | 2023 | COLLECTED | 09/09/2023 | Kingdom Come State Park, Pine Mountain: Along Laurel Cove Trail across from pond in Pine Mountain State Park. | 36.99160000, -82.98471000 | 712 | Along trail across from pond. Elevation: 2337 feet. Aspect: South. | Wild material | | 2158707 | NA 88615 |
| 164 | NA 88616 | KY23-020 | Clethra acuminata Michx. | Kentucky, United States | NA | | | 2023 | COLLECTED | 09/09/2023 | Kingdom Come State Park, Pine Mountain. | 36.99160000, -82.98471000 | 712 | Elevation: 2337 feet. Aspect: South. | Wild material | | 2158708 | NA 88616 |
| 165 | NA 88647 | KY23-051 | Stewartia ovata (Cav.) Weath. | Kentucky, United States | NA | | | 2023 | COLLECTED | 09/12/2023 | Daniel Boone National Forest: Marsh Creek south of KY-478. | 36.71494000, -84.35537000 | 319 | Right off the road at bridge, along stream edge of Coddle branch of Marsh Creek, west side [is part of] Daniel Boone National Forest. Elevation: 1045 feet. Aspect: East. | Wild material | | 2158740 | NA 88647 |
| 166 | WLP 3214 | TXWL2023-002 | Stewartia malacodendron L. | Texas, United States | NA | | | 2023 | COLLECTED | 08/27/2023 | Little Cow Creek. | 31.06090300, -93.79570300 | | Mesic mixed hardwood-pine forest adjacent to riparian area. Some blowdown evident. | Wild material | | 2158758 | WLP 3214 |
| 167 | WLP 3215 | TXWL2023-003 | Stewartia malacodendron L. | Texas, United States | NA | | | 2023 | COLLECTED | 08/27/2023 | Little Cow Creek. | 31.06228800, -93.79734300 | | Mesic mixed hardwood-pine forest adjacent to riparian area. Some blowdown evident. | Wild material | | 2158759 | WLP 3215 |
| 168 | WLP 3218 | TJK2023FL-011 | Stewartia malacodendron L. | Florida, United States | NA | | | 2023 | COLLECTED | 08/26/2023 | Weaver Creek Bayhead, Eglin Air Force Base. Common in scattered patches along both sides of Weaver Creek. | 30.51679000, -86.91493400 | 81 | Rich, loamy moist mesic slopes; mixed deciduous-evergreen woodlands. Elevation: 268 feet. Slope: 15%. Aspect: West. | Wild material | | 2158791 | WLP 3218 |
| 169 | Ames 36168 | Mount Magazine | Ptelea trifoliata L. | Arkansas, United States | NC7 |  | | 2023 | COLLECTED | 08/26/2023 | Mount Magazine State Park primarily localized to the northwest rim of the mountain along the trails heading west from Brown's Spring, T6N R25W Sec. 21. | 35.17130900, -93.65582200 | 786 | Top of sky-island mountain. Localized along the rims just above steep cliffs on north facing slopes. | Wild material | Plants in nature ranging from three to fifteen feet in height with peak bloom observed during the first week of May (2023). | 2158787 | Ames 36168 |
| 170 | WLP 3345 | AS/SG/2023/025/235 | Styrax grandifolius Aiton | Arkansas, United States | NA |  | | 2023 | COLLECTED | 08/27/2023 | Ouachita National Forest - Winona Wildlife Management Area/South Fourche Botanical Area. Approximately 20 miles southwest of Danville, along County Road 362, east of Scenic Highway 7. T3N R20W Sec. 23. | 34.89619000, -93.10769400 | 275 | Uplands and on bluffs; understory of pine-hardwood forest. | Wild material | Plants in nature are large, clonally spreading colonies to 20 feet in height and similar width. Peak bloom occurred the last week of April (2023). | 2158786 | WLP 3345 |
| 171 | WLP 3142 | WLP 3142 | Amelanchier arborea (F. Michx.) Fernald | Kentucky, United States | NA | | | 2023 | COLLECTED | 05/31/2023 | Berea College Forest on Indian Fort Lookout. | 37.56437000, -84.23348000 | | On sandstone cliffs. | Wild material | WLPGR contract collection. | 2158474 | WLP 3142 |
| 172 | WLP 3140 | TJK2023AL-004 | Viburnum acerifolium L. | Alabama, United States | NA | | | 2023 | COLLECTED | 08/15/2023 | Haines Island Park; overlooks the Alabama River. | 31.72057000, -87.46543000 | 86 | Beautiful Pine-Oak forest sits atop the Buhrstone Questa, an escarpment that rises over 350 feet. Southern Red Hills Region. Slope: 10%. Aspect: North. Elevation recorded as 281 feet. | Wild material | WLPGR contract collection. | 2158472 | WLP 3140 |
| 173 | WLP 3137 | TJK2023AL-001 | Cornus alternifolia L. f. | Alabama, United States | NA | | | 2023 | COLLECTED | 08/15/2023 | Claiborne Bluffs, above the Alabama River. | 31.54883000, -87.51417000 | 16 | Slope: 35%. Aspect: West-northwest. Elevation recorded as 52 feet. | Wild material | WLPGR contract collection. | 2158469 | WLP 3137 |
| 174 | WLP 3136 | TJK2023FL-010 | Morella cerifera (L.) Small | Florida, United States | NA | | | 2023 | COLLECTED | 08/18/2023 | Blackwater State Forest: Wolfe Creek. | 30.80751000, -86.95774000 | 52 | Beautiful xeric pine-oak upland community. Transitions to mesic slopes and then to seepage bottom, stringer wetland community adjacent to the Wolfe Creek. Area is on a regular 2-4[-year] burn cycle. Slope: 10%. Aspect: South. Elevation recorded as 172 feet. | Wild material | Received as Morella pumila (Morella cerifera var. pumila). Treated tentatively as Morella cerifera Pumila Group. WLPGR contract collection. | 2158468 | WLP 3136 |
| 175 | NA 89264 | TJK2023FL-002 | Gaylussacia frondosa (L.) Torr. & A. Gray var. nana A. Gray | Florida, United States | NA | | | 2023 | COLLECTED | 05/19/2023 | Blackwater State Forest: Wolfe Creek. | 30.80760000, -86.96250000 | 49 | Beautiful xeric pine-oak upland community. Transitions to mesic slopes and then to seepage bottom, stringer wetland community adjacent to the Wolfe Creek. Area is on a regular 2-4[-year] burn cycle. Slope: 5%. Aspect: Northwest. Elevation recorded as 161 feet. | Wild material | WLPGR contract collection. Received as Gaylussacia tomentosa (nana). | 2158247 | NA 89264 |
| 176 | NA 89265 | TJK2023FL-003 | Ceanothus sp. | Florida, United States | NA | | | 2023 | COLLECTED | 05/19/2023 | Blackwater State Forest: Wolfe Creek. | 30.80650000, -86.95840000 | 49 | Beautiful xeric pine-oak upland community. Transitions to mesic slopes and then to seepage bottom, stringer wetland community adjacent to the Wolfe Creek. Slope: 20%. Aspect: Northwest. Elevation recorded as 162 feet. | Wild material | WLPGR contract collection. Received as Ceanothus microphyllus. | 2158248 | NA 89265 |
| 177 | NA 89266 | TJK2023FL-004 | Gaylussacia dumosa (Andrews) Torr. & A. Gray | Florida, United States | NA | | | 2023 | COLLECTED | 05/31/2023 | Blackwater State Forest: Wolfe Creek. | 30.80560000, -86.95890000 | 49 | Beautiful xeric pine-oak upland community. Transitions to mesic slopes and then to seepage bottom, stringer wetland community adjacent to the Wolfe Creek. Slope: 15%. Aspect: Northwest. Elevation recorded as 160 feet. | Wild material | WLPGR contract collection. | 2158249 | NA 89266 |
| 178 | NA 89267 | TJK2023FL-005 | Ceanothus americanus L. | Florida, United States | NA | | | 2023 | COLLECTED | 06/10/2023 | Blackwater State Forest: Wolfe Creek. | 30.80760000, -86.96250000 | 49 | Beautiful xeric pine-oak upland community. Transitions to mesic slopes and then to seepage bottom, stringer wetland community adjacent to the Wolfe Creek. Area is on a regular 2-4[-year] burn cycle. Slope: 5%. Aspect: Northwest. Elevation recorded as 161 feet. | Wild material | WLPGR contract collection. | 2158250 | NA 89267 |
| 179 | NA 89269 | TJK2023FL-007 | Vaccinium darrowii Camp | Florida, United States | NA | | | 2023 | COLLECTED | 06/10/2023 | Blackwater State Forest: Wolfe Creek. | 30.80560000, -86.95770000 | 60 | Beautiful xeric pine-oak upland community. Transitions to mesic slopes and then to seepage bottom, stringer wetland community adjacent to the Wolfe Creek. Area is on a regular 2-4[-year] burn cycle. Slope: 2%. Aspect: West-northwest. Elevation recorded as 197 feet. | Wild material | WLPGR contract collection. | 2158252 | NA 89269 |
| 180 | Ames 36152 | JDC/MM/2023/048/1080 | Monarda maxmedleyi J. J. N. Campb. & Floden | Kentucky, United States | NC7 |  | | 2023 | COLLECTED | 08/10/2023 | Owsley Fork Road (roadsides) just 2.3 miles east, southeast of Big Hill, along the north edge of the reservior. | 37.54038300, -84.17209500 | 252 | Moist and dry slopes. Woodland edges; open woods; densely shaded woods; and wooded roadsides. | Wild material | Plants measuring 12-18" in height. Spreading vegetatively via rhizomes. Flower color on the majority of specimens is mostly white with some specimens having a hint of pink. Peak flowering at collection site occurred near 28th of May (2023). Some specimens flowering in heavy shade. | 2158357 | Ames 36152 |
| 181 | Ames 36154 | JDC/MM/2023/051/1083 | Monarda maxmedleyi J. J. N. Campb. & Floden | Kentucky, United States | NC7 |  | | 2023 | COLLECTED | 08/08/2023 | Located just east of highway 213 (Morris Creek Road) near Powell and Montgomery County line. Population in both counties. | 37.90554800, -83.86808700 | 359 | Dry, steep hillside (roadside). Localized to south-facing slopes. | Wild material | Plants measuring 12-18" in height. Peak flowering at collection site occurred near 24th of May (2023). Some specimens extremely vigorous forming dense clonal patches covering a 5' x 5' area. Majority of specimens with mostly white flowers. | 2158359 | Ames 36154 |
| 182 | Ames 36157 | JDC/MM/2023/054/1086 | Monarda maxmedleyi J. J. N. Campb. & Floden | Kentucky, United States | NC7 |  | | 2023 | COLLECTED | 08/08/2023 | Located along Nichols Branch Road and Dry Creek Road, 2.0 miles east of Clearfield both north and south of Dry Creek Road intersection | 38.14977900, -83.38992200 | 259 | Localized to south and west-facing moist slopes with steep (65 degree) slopes. | Wild material | Plants measuring 12-18" in height. Spreading vegetatively via rhizomes. Near split of white and light pink flowered specimens. Peak flowering at collection site occurred near 25th of May (2023). | 2158362 | Ames 36157 |
| 183 | Ames 36158 | JDC/MM/2023/058/1090 | Monarda maxmedleyi J. J. N. Campb. & Floden | Kentucky, United States | NC7 |  | | 2023 | COLLECTED | 08/09/2023 | South of Morehead approximately 5.8 miles on Pretty Ridge Road (highway 1274) just north of intersection with Road 801 | 38.10409000, -83.42610600 | 353 | Roadside. High-quality remnant prairie/open woods in immediate area. | Wild material | Plants measuring 12-18" in height. Spreading vegetatively via rhizomes. Majority of specimens with light pink flowers but a few have white flowers. Peak flowering at collection site occurred near 25th of May (2023). | 2158363 | Ames 36158 |
| 184 | Ames 36159 | JDC/MM/2023/062/1094 | Monarda maxmedleyi J. J. N. Campb. & Floden | Kentucky, United States | NC7 |  | | 2023 | COLLECTED | 08/09/2023 | Daniel Boone National Forest on north and south sides along Zilpo Road with the highest abundance being across from intersection with Dogwood Lane. | 38.05551500, -83.53288600 | 354 | Edges of woods/roadsides. Localized to west and southeast facing slopes. | Wild material | Plants measuring 12-18" in height. Spreading vegetatively via rhizomes. Flower color varies within the population from white to pink. Peak flowering at collection site occurred near 27th of May (2023). | 2158364 | Ames 36159 |
| 185 | Ames 36161 | JDC/MM/2023/066/1098 | Monarda maxmedleyi J. J. N. Campb. & Floden | Kentucky, United States | NC7 |  | | 2023 | COLLECTED | 08/09/2023 | Daniel Boone National Forest on west and east side of NF-227 (Sweet Lick Road) just north (0.65 miles) of intersection with Henry Ridge Road | 37.74303300, -83.93589700 | 387 | Ridge tops/highest elevations, dry open woods. | Wild material | Plants measuring 8-14" in height. Spreading vegetatively via rhizomes. Population mostly represented as specimens with white flowers. Peak flowering at collection site occurred near 27th of May (2023). | 2158366 | Ames 36161 |
| 186 | Ames 36163 | AS/RA/2023/069/279 | Rhus aromatica Aiton | Illinois, United States | NC7 |  | | 2023 | COLLECTED | 08/11/2023 | Located just east of Sand Prairie Scrub Oak Nature Preserve approximately 3.75 miles east of Bath, T20N R9W SW 1/4 SW 1/4 Sec. 12. | 40.19175000, -90.06813000 | 155 | Dry sand. Roadside and woodland edges. | Wild material | Plants ranging in height from 2-5' in nature. Plants seemed to make large clonal patches mostly by layering rather than suckering. | 2158368 | Ames 36163 |
| 187 | Ames 36073 | JDC/UT/2022/028/1009 | Ulmus thomasii Sarg. | Iowa, United States | NC7 |  | | 2023 | COLLECTED | 06/05/2023 | Ledges State Park approximately 4.75 miles south of Boone, T83N R26W (Madrid NW Quad.) near center of SE ¼ Sec. 16 and also NW ¼ SW ¼ Sec. 21. | 41.99780200, -93.87967900 | 288 | Moist deciduous woods typically on mid-slopes to base of slopes and also well-drained floodplains. | Wild material | Ulmus thomasii (Rock elm) is an underutilized tree species both in conservation and in the urban landscape. Charles Sprague Sargent (first director of the Arnold Arboretum of Harvard University, Boston, MA) described the wood of Rock Elm as "heavy, hard, very strong and tough, closely grained, and susceptible of receiving a beautiful polish". Historically noted for a variety of uses in woodworking including furniture, heavy agricultural implements, timber frame buildings, pianos, hockey sticks, and hand tools. U. thomasii is extremely drought tolerant, adaptable to very calcareous soils, and compared to U. americana or U. rubra has a very conservative growth rate requiring minimal attention in regards to pruning. Rock elm naturally tends to develop into a nice structural specimen in the landscape, unlike other fast growing U. americana cultivars in the nursery trade needing frequent attention. Rock elm has very fissured bark and is well known for maintaining a strong central leader resulting in a very attractive, pyramidal form. Despite many literature sources stating that "wings" on the stems are a key identifiying characteristic, this trait is not reliable and many genotypes may completely lack "wings" on the stems. While growth habit and morphology of dormant buds (very pointy) are good traits to help aid in identification, fruits are the best way to confirm identity. Fruits are densly pubescent, often described as "inflated" and generally reach maturity a couple weeks after U. rubra and U. americana. U. thomasii flowering in central Iowa typically occurs the last week in April into the first week in May and are rather distinguishable from other Ulmus in being pendulous. Fruits are extremely prized treats for many birds, where fruits are often "robbed" prior to full maturity. Fruits are also highly prized by many other animals such as mice, squirrels, chipmunks, turkeys, etc. and are generally consumed within hours after fruit abscission. The native range of U. thomasii is concentrated in the northeastern United States and into Canada with disjunct populations documented in northwestern Missouri and northwestern Arkansas (Little, E. L. Jr. 1971). In the 1895 Silva of North America (vol. 7) it was stated that, “The value of the wood of the Rock Elm threatens its extinction and most of the large trees have already been cut.” Today, since rock elm is rather rare, especially in areas near the edges of its range, many states list the species as endangered or threatened warranting preservation efforts. Genetics of this accession would be representative of the species southwestern edge of its native range. At the collection site in nature (Ledges State Park), out of approximately 100 specimens noted only 1-2% of specimens had characteristic "wings" on the stems. Research was executed (Moore, P., 2024) involving the core sampling of U. thomasii and U. americana specimens in Ledges State Park to make growth ring widths and basal area increment comparisons. Results determined that the average age of cored trees U. thomasii (n=4) and U. americana (n=4) of both species was roughly 80 years, excluding the exceptional case of tree #007 (Ames 36073 23ncao02 SD). Tree #007 was aged at 300 years of age and currently (2025) ranks as the 14th largest U. thomasii in Iowa measuring 21" DBH with a height of 75' 5" and a spread of 43' 5" totalling 152.21 points (Rouw, M., personal communication, 4 May 2022). The computed mean density at 𝑀𝑀 = 12% for U. thomasii was 0.80 g/cm3, and for U. americana was 0.672 g/cm3. These values are both higher than the representative values inferred from the Woods Database which are 0.755 g/cm3 for U. thomasii and 0.56 g/cm3 for U. americana. To date, there is little to no information regarding U. thomasii resistance to Dutch Elm Disease. Collections of U. thomasii at the Arnold Arboretum have over-time succumbed to DED (Pruka, B., 2016). However, data recorded by Moore (2024) indicates that U. thomasii growing in central Iowa can surpass 300 years in age verifying it's long-term utilization in the landscape. | 2142915 | Ames 36073 |
| 188 | Ames 36139 | Berea College Forest | Morus rubra L. | Kentucky, United States | NA |  | | 2023 | COLLECTED | 05/31/2023 | Between West and East Pinnacles of Berea College Forest just 3.25 miles east, southeast of Berea | 37.55656100, -84.23777600 | 338 | Mid-lower slopes of moist, deciduous woods. | Wild material | Species rather abundant throughout site with little to no presence of Morus alba. Majority of specimens noted measuring 8" DBH or smaller. Largest specimen noted reaching approximately 60' in height. | 2158344 | Ames 36139 |
| 189 | W6 61403 | CBG- 10836 | Triosteum aurantiacum E. P. Bicknell | Wisconsin, United States | W6 |  | | 2023 | | | | | | | Wild material | | 2142285 | W6 61403 |
| 190 | Ames 36024 | AS/FN/2023/011/221 | Fraxinus nigra Marshall | Wisconsin, United States | NC7 |  | | 2023 | COLLECTED | 02/26/2023 | Located just north of Leland approximately 0.70 miles along Hemlock Road, T10N R5E SW 1/4 NW 1/4 Sec. 18 | 43.34472800, -89.95099700 | 242 | Floodplain | Wild material | Single mother tree sample with signs of wood pecker damage on trunk. | 2141557 | Ames 36024 |
| 191 | NA 88598 | RJL2023FL-002a | Agarista populifolia (Lam.) Judd | Florida, United States | NA | | | 2023 | COLLECTED | 02/14/2023 | Plants growing in woodlands of Wekiwa Springs State Park along trails accessed from the Sand Lake parking lot at the end of Palmetto Avenue. From the parking lot, take the main trail south for about 18 meters and immediately take a cut-through trail on the left to the location of this population. | 28.72398600, -81.47205400 | 10 | Plants were growing in shade to part-shade of moist mesic hammocks of lowland transitional woodlands eventually becoming wetland habitats that are comprised primarily of evergreen plants with fewer deciduous plants. The underlying geology of this area is of Pliocene origin and characterized as the Cypresshead Formation. The Cypresshead Formation named by Huddlestun (1988), is composed of siliciclastics and occurs only in the peninsula and eastern Georgia. It is at or near the surface from northern Nassau County southward to Highlands County forming the peninsular highlands. It appears that the Cypresshead Formation occurs in the subsurface southward from the outcrop region and similar sediments, the Long Key Formation, underlie the Florida Keys. The Cypresshead Formation is a shallow marine, near shore deposit equivalent to the Citronelle Formation deltaic sediments and the Miccosukee Formation prodeltaic sediments. The Cypresshead Formation consists of reddish brown to reddish orange, unconsolidated to poorly consolidated, fine to very coarse grained, clean to clayey sands. Cross bedded sands are common within the formation. Discoid quartzite pebbles and mica are often present. Clay beds are scattered and not areally extensive. In general, the Cypresshead Formation in exposure occurs above 100 feet (30 meters) above mean sea level (msl). Original fossil material is not present in the sediments although poorly preserved molds and casts of mollusks and burrow structures are occasionally present. The presence of these fossil "ghosts" and trace fossils documents marine influence on deposition of the Cypresshead sediments. The permeable sands of the Cypresshead Formation form part of the surficial aquifer system. | Wild material | | 2141479 | NA 88598 |
| 192 | NA 88599 | RJL2023NC-001 | Ilex decidua Walter | North Carolina, United States | NA | | | 2023 | COLLECTED | 02/18/2023 | Plants growing along a fenceline on a hillside about 10 meters from Interstate 85 (south bound) and approximately 0.65 kilometers south of the North Carolina-Virginia border. | 36.53904800, -78.18822500 | 86 | The plant was growing on the upper shoulder of a slope about 7 meters above the highway in part-shade to sun of an upland, well-drained, dry mesic somewhat disturbed site on the fenceline boundary of Interstate 85 (south bound). The area was originally cleared of all vegetation and now, many years later, native and non-native plant species have aggressively recolonized the area. This early successional habitat is dominated by Juniperus virginiana and Liquidambar styraciflua, as well as, non-native species such as Ligustrum sinense, Lonicera japonica, and Ailanthus altissima. The underlying geology of this area is of Permian/Pennsylvanian origin and characterized as the Granitic Rock Formation. It is characterized by megacrystic to equigranular components and includs Castalia and Wilton intrusives. | Wild material | | 2141480 | NA 88599 |
| 193 | WLP 3084 | RM2023-002 | Rhododendron viscosum (L.) Torr. | Florida, United States | NA | | | 2023 | COLLECTED | 09/15/2022 | This species is growing in the Blackwater River State Forest approximately 0.24 kilometers north of Wof W20 and approximately 0.93 kilometers west of the junction of 3 Notch Trail/Road. | 30.84510000, -86.94940000 | 38 | The plants were growing in part shade of a moist mesic transition slope between a dry upland habitat and a bog.
Soils: The underlying geology of this area is the Citronelle Formation, of Pliocene origin, and consists of gray to orange, often mottled, unconsolidated to poorly consolidated, very fine to very coarse, poorly sorted, clean to clayey sands. It contains significant amounts of clay, silt and gravel which may occur as beds and lenses and may vary considerably over short distances. Limonite nodules and limonite-cemented beds are common. Source: USGS Florida Geologic Map Data (https://mrdata.usgs.gov/geology/state/state.php?state=fl)
The surface soil profile found in this area is primarily Troup Series. These soils are sandy and loamy marine deposits. They are well drained and typically on the tops and sides of broad and narrow ridges on uplands typically with 0-12% slopes. These soils are very strongly acid with a depth of 2-3 meters. Pactolus Series soils comprise a minor, but important percentage of the lower slopes that are nearly level to gently sloping and account for the somewhat poorly drained, yet, sandy conditions. These soils are also strongly acid with very dark gray loamy sands.
Source: Soil Survey of Santa Rosa County and NRCS Web Soil Survey (https://www.nrcs.usda.gov/Internet/FSE_MANUSCRIPTS/florida/FL113/0/SantaRosa.pdf and https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2141438 | WLP 3084 |
| 194 | WLP 3085 | RM2023-003 | Hibiscus laevis All. | Florida, United States | NA | | | 2023 | COLLECTED | 10/01/2022 | This species is growing along the Escambia River and accessed by boat. | 30.62930000, -87.25830000 | 1 | The plants were growing on stumps in full sun on the edge of a semi-alluvial area of the river.
Soils: The underlying geology of this area is classified as Alluvium, of Pleistocene/Holocene origin and consists of undifferentiated Quaternary sediments of varying thickness including siliciclastics, organics and freshwater carbonates. The siliciclastics are light gray, tan, brown to black, unconsolidated to poorly consolidated, clean to clayey, silty, unfossiliferous, variably organic-bearing sands to blue green to olive green, poorly to moderately consolidated, sandy, silty clays. Organics occur as plant debris, roots, disseminated organic matrix and beds of peat. Freshwater carbonates, often referred to as marls in the literature, are scattered.
Source: USGS Florida Geologic Map Data (https://mrdata.usgs.gov/geology/state/state.php?state=fl)
The surface soil profile of this area is primarily Chewacla-Wahee-Riverview Association. The Chewacla Series soils are dark yellowish brown silty clay loam soils, that are strongly acidic and somewhat poorly drained. They are soils of flood plains and streams subject to frequent flooding. The Wahee Series soils are dark gray clayey and loamy marine or fluviomarine sediments that are strongly acidic and somewhat poorly drained. The Riverview series consists of very deep, well drained, moderately permeable soils that formed in loamy alluvium on flood plains. Slopes range from 0 to 5 percent.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2141439 | WLP 3085 |
| 195 | WLP 3092 | RJLSEUS2022-021 | Rhododendron prunifolium (Small) Millais | Alabama, United States | NA | | | 2023 | COLLECTED | 12/10/2023 | Slopes along Poke Springs Branch inlet accessed by boat from Walter F. George Reservoir. Generally uncommon, but frequent at this site. | 31.72318400, -85.12907800 | 69 | Plants are growing in part-shade to shade on the well-drained mostly deciduous woodland slopes approximately 3-6 meters above the inlet.
Soils: The underlying geology of this area is of Cretaceous origin and characterized as Selma Group; Providence Sand. The upper part of the profile consists of cross-bedded fine to coarse sand and white, dark-gray and pale-red-purple mottled clay containing lignite, sand, and kaolin. The lower part consists of dark-gray laminated to thin-bedded silty clay and abundantly micaceous, carbonaceous, fossiliferous very fine to fine sand.
Source: USGS Alabama Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=ALKp%3B1)
The primary soil types in the collection area are classified as Nankin-Lucy Complex soil (20 to 60 percent slopes). The Nankin Series consists of very deep, well drained, moderately slowly permeable soils on uplands of the Coastal Plain. They formed in stratified loamy and clayey marine sediments. Slopes range from 0 to 60 percent. Soils are comprised of sandy loam in the upper 25 cm to sandy clay loam and sandy clay in lower strata to about 1.7 meters deep; these soils are strongly acid. The Lucy Series consists of very deep, well drained, moderately permeable soils on uplands. They formed in sandy and loamy marine and fluvial sediments of the Southern Coastal Plain. Slopes vary from 0 to 45 percent. These soils are generally loamy to sandy loam in the upper 25 cm and sandy clay loam in the lower strata to 2 meters; these are strongly acid soils.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2141446 | WLP 3092 |
| 196 | WLP 2795 | RJL2023NJ-001 | Rhododendron atlanticum (Ashe) Rehder | New Jersey, United States | NA | | | 2023 | COLLECTED | 01/16/2023 | Plants growing in woodlands on the south side of a powerline right-of-way approximately 0.72 kilometers southwest of Indian Trail Road. The site was accessed by foot. Plants are infrequent at this site and considered rare in New Jersey. | 39.05653200, -74.87482500 | 5 | Plants growing in shade to part-shade of a dry woodland habitat that is mostly deciduous. Nearby, as the elevation changes slightly, there is more abundant soil moisture, becoming a bit more mesic. Soils: The underlying geology of this area is of Upper Pliocene origin and characterized as an Unnamed Formation at Cape May. It is comprised of interbedded gravel, sand, and clay, massive to thickly-bedded. This is an informal unit described from a core hole at the Cape May Airport. The lower 18.3 meters consists of interbedded gravel; medium- to very coarse grained, poorly sorted sand; and thin to thick beds of medium- to dark-gray, very woody clay. Gravel clasts are typically less than 0.64 mm in diameter. The upper 12.2 meters consists of a thick-bedded, medium-gray, extensively bioturbated clay-silt, which is overlain by an extensively burrowed, fine- to medium-grained glauconitic (about 5 percent) quartz sand. Quartz and siliceous rock fragments compose most sand grains. Feldspar is present in most samples but usually constitutes less than 10 percent of the sand fraction. No calcareous macrofossils were found in the burrowed intervals. This unit is known only to occur on the Cape May peninsula where it lies within a large channel. The unit is about 60 m in maximum thickness. The contact with the underlying Belleplain Member of the Kirkwood Formation is sharp and unconformable; a basal gravel bed as much as 1 m thick is present along the contact. The pollen assemblage in the lower part of the unit is dominated by pine and oak with somewhat lesser amounts of hickory and basswood. Spruce, hemlock, beech, alder, and black gum are minor constituents. Traces of fir, willow, birch, and sweet gum are present, as is exotic Engelhardia. The non-arboreal pollen are a Multisia-type composite of the present-day Andean provenance which indicate an exotic cool climate. The lower assemblage suggests a cool-temperate climatic regimen. The pollen assemblage in the upper beds is dominated by oak and hickory with minor amounts of basswood, sweet gum, pine, and Multisia-type composite. Traces of cedar, willow, birch, alder, grass, and Sphagnum spores also are present. This assemblage probably represents a temperate climatic regimen (Les Sirkin, Adelphi University, written commun., 1991). The low percentage of exotic species is characteristic of the late Pliocene, and therefore, the unnamed unit at Cape May could be equivalent to the Beaverdam Formation of the Delmarva Peninsula of Delaware, Maryland, and Virginia. Source: USGS New Jersey Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=NJTc%3B1) The primary soil type in the area of this collection is classified as Berryland and Mullica soils (0 to 2 percent slopes, occasionally flooded). Berryland Series soils are very deep, very poorly drained soils of the Coastal Plains formed by sandy eolian deposits and/or fluviomarine sediments. Th upper 30 cm of the strata is sandy, dry, very friable and extremely acid. The lower strata to 1.8 meters contains loamy sand coated with organic matter, weakly cemented organ nodules and additional layers of sand occasionally containing rounded quartzose pebbles. The Mullica Series soils are typically coarse-loamy, siliceous, semiactive, and mesic typic humaquepts that are strongly to extremely acidic throughout the profile. The typical solum thickness ranges from 50-150+ cm. These soils are generally considered to be poorly drained. Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2141140 | WLP 2795 |
| 197 | NA 87346 | TJK2022FL-001 | Cornus florida L. | Florida, United States | NA | | | 2023 | COLLECTED | 10/27/2022 | Okaloosa County: Duke Field AFS; Eglin Air Force Base, approximately 1.3 miles southeast of Military Rd 231, Juniper Creek Bayhead. | 30.62890000, -86.50000000 | 42 | Rich evergreen and deciduous Bayhead Community. Extensive Quercus arkansana along the bluff top to mid-slope, with Magnolia ashei in steephead bottom to lower half of slope. Cornus at toe of slope on the first bench, off bottom. | Wild material | | 2141637 | NA 87346 |
| 198 | NA 87814 | RM-TK2022-003 | Nyssa ogeche W. Bartram ex Marshall | Florida, United States | NA | | | 2023 | COLLECTED | 09/06/2022 | Hightower Landing on Holmes Creek, off of Hightower Road. This location is off of Florida State Hwy. 79. | 30.60539000, -85.76513400 | 5 | Trees growing on the edge of the water along Holmes Creek.
Soils: The underlying geology of this area is classified as Alluvium of Pleistocene/Holocene origin and consists of undifferentiated Quaternary sediments of varying thickness including siliciclastics, organics and freshwater carbonates. The siliciclastics are light gray, tan, brown to black, unconsolidated to poorly consolidated, clean to clayey, silty, unfossiliferous, variably organic-bearing sands to blue green to olive green, poorly to moderately consolidated, sandy, silty clays. Organics occur as plant debris, roots, disseminated organic matrix and beds of peat. Freshwater carbonates, often referred to as marls in the literature, are scattered.
Source: USGS Florida Geologic Map Data (https://mrdata.usgs.gov/geology/state/state.php?state=fl)
The primary soil types in the collection area are classified as Rutlege, Pickney and Pamlico soils, frequently flooded. The Rutlege series comprises very deep, very poorly drained persistently wet soils on flats, depressions and floodplains where shallow ponding is common. They are of marine or fluvial sediment origin. Thickness of these loamy sandy soils is greater than 1.5 meters and a reaction from extremely acid to strongly acid. The Pickney Series consists of very deep, very poorly drained soils. Permeability is rapid. These nearly level soils have negligible runoff and were formed by marine or fluvial sediments in the lower coastal plain on flats, depressions, stream terraces, and flood plains. Slopes range from 0 to 2 percent. The soils of this series are loamy fine sand that is very friable and extremely acid in the upper 0-25 cm. The lower strata are similar, while the lower strata from 0.8-2 meters are comprised of fine sand. The Pamlico series consists of very poorly drained soils that formed in decomposed organic material underlain by dominantly sandy sediment. The soils are on nearly level flood plains, bays, and depressions of the Coastal Plain. Slopes are less than 1 percent. Pamlico soils have 0.4-1.3 meters of organic material over dominantly sandy sediments. Reaction is extremely in the organic layers and ranges from extremely acid to strongly acid in the underlying mineral layers.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2140796 | NA 87814 |
| 199 | NA 88520 | RM-TK2022-008 | Rhododendron canescens (Michx.) Sweet | Mississippi, United States | NA | | | 2023 | COLLECTED | 10/06/2022 | Along Black Creek, approximately 0.2 kilometers north of Berry Road in the Pascagoula River State Wildlife Management Area. Accessed by boat. | 30.74160000, -88.69890000 | 11 | Plants growing on the high bluffs about 5 meters above Black Creek
Soils: The underlying geology of this area is classified as Pascagoula and Hattiesburg Formation of Miocene origin. This formation consists of green and bluish-green clay, sandy clay, and sand; gray siltstone and sand; locally fossiliferous.
Source: USGS Mississippi Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=MSMIph%3B0)
The primary soil types in this collection area are Urbo-Mooreville-Una Complex soils (0 to 3 percent slopes, frequently flooded). The Urbo series consists of deep, somewhat poorly drained soils. Permeability is very slow. These nearly level to gently sloping soils formed in clayey alluvium on flood plains of streams that drain uplands of the Southern Coastal Plain and Blackland Prairie Major Land Resource Areas. Slopes range from 0 to 3 percent. The Mooreville series consist of very deep, moderately well drained, moderately permeable soils that formed in loamy alluvium. These soils are on flood plains of streams draining areas of the Southern Coastal Plain and the Blackland Prairie. Slopes range from 0 to 2 percent. The Una series consists of deep, poorly drained soils on floodplains of streams in areas of the Southern Coastal Plain and Blackland Prairie Major Land Resource Areas. Permeability is very slow. Soils formed in acid clayey alluvium. The seasonal high water table is near the surface during wet periods. Slopes range from 0 to 4 percent. All of these soil series are strongly acid.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2140801 | NA 88520 |
| 200 | NA 88521 | RM-TK2022-009 | Rhododendron austrinum (Small) Rehder | Mississippi, United States | NA | | | 2023 | COLLECTED | 10/06/2022 | Along Black Creek, approximately 0.46 kilometers south of Berry Road in the Pascagoula River State Wildlife Management Area. Accessed by boat. | 30.73720000, -88.70020000 | 12 | Plants growing on the slopes and high bluffs about 2-5 meters above Black Creek.
Soils: The underlying geology of this area is classified as Pascagoula and Hattiesburg Formation of Miocene origin. This formation consists of green and bluish-green clay, sandy clay, and sand; gray siltstone and sand; locally fossiliferous.
Source: USGS Mississippi Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=MSMIph%3B0)
The primary soil types in this collection area are Urbo-Mooreville-Una Complex soils (0 to 3 percent slopes, frequently flooded). The Urbo series consists of deep, somewhat poorly drained soils. Permeability is very slow. These nearly level to gently sloping soils formed in clayey alluvium on flood plains of streams that drain uplands of the Southern Coastal Plain and Blackland Prairie Major Land Resource Areas. Slopes range from 0 to 3 percent. The Mooreville series consist of very deep, moderately well drained, moderately permeable soils that formed in loamy alluvium. These soils are on flood plains of streams draining areas of the Southern Coastal Plain and the Blackland Prairie. Slopes range from 0 to 2 percent. The Una series consists of deep, poorly drained soils on floodplains of streams in areas of the Southern Coastal Plain and Blackland Prairie Major Land Resource Areas. Permeability is very slow. Soils formed in acid clayey alluvium. The seasonal high water table is near the surface during wet periods. Slopes range from 0 to 4 percent. All of these soil series are strongly acid.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2140802 | NA 88521 |
| 201 | NA 88522 | RM-TK2022-010 | Viburnum dentatum L. var. scabrellum Torr. & A. Gray | Florida, United States | NA | | | 2023 | COLLECTED | 10/10/2022 | Plants growing in woodlands via an unnamed dirt road accessed from Old Ferry Road. | 30.91880000, -87.25990000 | 43 | Plants are growing in an upland habitat on the edge of south-facing woodland in part-shade.
Soils: The underlying geology of this area is classified as Alluvium of Pleistocene/Holocene origin and consists of undifferentiated Quaternary sediments of varying thickness including siliciclastics, organics and freshwater carbonates. The siliciclastics are light gray, tan, brown to black, unconsolidated to poorly consolidated, clean to clayey, silty, unfossiliferous, variably organic-bearing sands to blue green to olive green, poorly to moderately consolidated, sandy, silty clays. Organics occur as plant debris, roots, disseminated organic matrix and beds of peat. Freshwater carbonates, often referred to as marls in the literature, are scattered.
Source: USGS Florida Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=FLPSHal%3B0)
The primary soil type in the collection area is classified as Orangeburg sandy loam soil (2 to 5 percent slopes). The Orangeburg Series consists of very deep, well drained, moderately permeable soils on uplands of the Southern Coastal Plain. They formed in loamy and clayey marine sediments. The reaction of all this soil ranges from very strongly acid to strongly acid.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2140803 | NA 88522 |
| 202 | NA 88525 | RM-TK2022-013 | Macranthera flammea (W. Bartram) Pennell | Florida, United States | NA | | | 2023 | COLLECTED | 11/04/2022 | Growing in wetland in Blackwater River State Forest. | 30.80870000, -86.96270000 | 42 | Plants are typically found growing in part shade to sun in saturated streamside wetland/seep areas at the base of the slope in sphagnum moss. This appears to be year-round wetland habitat.
Soils: The underlying geology of this area is the Citronelle Formation of Pliocene origin and consists of gray to orange, often mottled, unconsolidated to poorly consolidated, very fine to very coarse, poorly sorted, clean to clayey sands. It contains significant amounts of clay, silt and gravel which may occur as beds and lenses and may vary considerably over short distances. Limonite nodules and limonite-cemented beds are common. Source: USGS Florida Geologic Map Data (https://mrdata.usgs.gov/geology/state/state.php?state=fl)
The surface soil profile found in this area is primarily Troup Series. These soils are sandy and loamy marine deposits. They are well drained and typically on the tops and sides of broad and narrow ridges on uplands typically with 0-12% slopes. These soils are very strongly acid with a depth of 2-3 meters. Pactolus Series soils comprise a minor, but important percentage of the lower slopes that are nearly level to gently sloping and account for the somewhat poorly drained, yet, sandy conditions. These soils are also strongly acid with very dark gray loamy sands.
Source: Soil Survey of Santa Rosa County and NRCS Web Soil Survey (https://www.nrcs.usda.gov/Internet/FSE_MANUSCRIPTS/florida/FL113/0/SantaRosa.pdf and https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2140806 | NA 88525 |
| 203 | NA 88526 | RM-TK2022-014 | Oxydendrum arboreum (L.) DC. | Florida, United States | NA | | | 2023 | COLLECTED | 11/06/2022 | Growing along an unnamed dirt road leading to “Old Land Place” on the edge of Eglin AFB accessed from the Yellow River. | 30.55320000, -86.93730000 | 2 | The underlying geology of this area is classified as Alluvium of Pleistocene/Holocene origin and consists of undifferentiated Quaternary sediments of varying thickness including siliciclastics, organics and freshwater carbonates. The siliciclastics are light gray, tan, brown to black, unconsolidated to poorly consolidated, clean to clayey, silty, unfossiliferous, variably organic-bearing sands to blue green to olive green, poorly to moderately consolidated, sandy, silty clays. Organics occur as plant debris, roots, disseminated organic matrix and beds of peat. Freshwater carbonates, often referred to as marls in the literature, are scattered.
Source: USGS Florida Geologic Map Data (https://mrdata.usgs.gov/geology/state/state.php?state=fl)
The surface soil profile of this area is primarily Bibb-Kinston Series Association. Bibb Series soils are coarse-loamy, sandy, acid soils that are poorly drained. They are soils of flood plains and streams subject to frequent flooding. These are found in association with Kinston Series soils that are fine-loamy, sandy, acid soils of flood plains and stream subject to frequent flooding. The Bibb-Kinston association ranges from 1-1.5 meters thick and is strongly acid.
Source: Soil Survey of Santa Rosa County and NRCS Web Soil Survey (https://www.nrcs.usda.gov/Internet/FSE_MANUSCRIPTS/florida/FL113/0/SantaRosa.pdf and https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2140807 | NA 88526 |
| 204 | NA 88534 | RJLSEUS2022-005 | Leucothoe axillaris (Lam.) D. Don | North Carolina, United States | NA | | | 2023 | COLLECTED | 12/06/2022 | Plants growing in the wetlands and other moist depressions along Scotland Co. Road 1328 in the Sandhills Game Lands. Common at this site This plant is somewhat sporadic in its distribution, but abundant in places where it is found in moist to wet habitats of bottomlands in this area. | 34.88545200, -79.44597500 | 71 | Plants are growing in shade of acid bottomland wet woodlands along streams or adjoining wetlands with constant sub-surface moisture. It prefers areas above the permanently wet conditions and can go through periods of drought.
Soils: The underlying geology of this area is of Cretaceous origin and characterized as Mittendorf Formation. The formation is comprised of sand, sandstone, and mudstone, gray to pale gray with an orange cast, and mottled. Clay balls and iron-cemented concretions are common, beds are laterally discontinuous, and cross-bedding is common.
Source: USGS North Carolina Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=NCKm%3B11)
The primary soil type in the collection area is classified as Paxville loam soil (0 to 1 percent slopes, rarely flooded). The Paxville Series consists of very deep, very poorly drained soils. Permeability is moderate. These nearly level soils formed from marine deposits, fluviomarine deposits, and alluvium. They range from 0 to 2 percent slopes. The frequency of flooding is typically very rare to brief periods. The upper strata, 0-1.2 meters, is comprised of fine sandy loam that is friable, non-sticky and non-plastic; it does contain small amounts clean quartz grains and is strongly acid. Lower strata to a depth of 2.5 meters are similar with fine sandy loam in the upper portions and progressively more sandy loam to fine sand in the deepest strata.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2140763 | NA 88534 |
| 205 | NA 88536 | RJLSEUS2022-007 | Leucothoe axillaris (Lam.) D. Don | South Carolina, United States | NA | | | 2023 | COLLECTED | 12/07/2022 | Plants growing along the margin of Sandy Run and its associated wetland on the north side of Paradise Rd. (State Rd. S-15-403). Common at this site and throughout the drainage of Sandy Run and its associated wetland. | 32.83900000, -80.81014400 | 27 | Plants are growing in part-shade to shade of a moist mesic woodland habitat along a small wetland associated with Sandy Run. Plants are located in an area that occasionally floods, but is not permanently wet.
Soils: The underlying geology of this area is of Pliocene origin and characterized as Bear Bluff Formation. This formation is considered one of the older coastal terrace sequences in the Carolinas. Bear Bluff Formation consists of gray to cream, fossiliferous, coarse-grained calcareous sand, and sandy limestone. It is typically 3-40 meters thick.
Source: USGS South Carolina Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=SCTbb%3B1)
The primary soil type in the collection area is classified as Pickney Loamy Sand soils. The Pickney Series consists of very deep, very poorly drained soils. Permeability is rapid. These nearly level soils have negligible runoff and were formed by marine or fluvial sediments in the lower coastal plain on flats, depressions, stream terraces, and flood plains. Slopes range from 0 to 2 percent. The soils of this series are loamy fine sand that is very friable and extremely acid in the upper 0-25 cm. The lower strata are similar, while the lower strata from 0.8-2 meters are comprised of fine sand.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | Leucothoe axillaris/fontanesiana | 2140764 | NA 88536 |
| 206 | NA 88537 | RJLSEUS2022-009 | Rhododendron canescens (Michx.) Sweet | South Carolina, United States | NA | | | 2023 | COLLECTED | 12/07/2022 | Plants growing along the upper margin of a small stream and associated wetland on the northwest side of Paradise Rd. (State Rd. S-15-403). Common at this site and throughout the drainage of the stream and associated wetland. | 32.83868100, -80.81099200 | 28 | Plants are growing in part-shade to shade of a moist mesic woodland habitat along a small wetland associated with a creek. Plants are located in an area that occasionally floods, but is not permanently wet.
Soils: The underlying geology of this area is of Pliocene origin and characterized as Bear Bluff Formation. This formation is considered one of the older coastal terrace sequences in the Carolinas. Bear Bluff Formation consists of gray to cream, fossiliferous, coarse-grained calcareous sand, and sandy limestone. It is typically 3-4 meters thick.
Source: USGS South Carolina Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=SCTbb%3B1)
The primary soil type in the collection area is classified as Pickney Loamy Sand soils. The Pickney Series consists of very deep, very poorly drained soils. Permeability is rapid. These nearly level soils have negligible runoff and were formed by marine or fluvial sediments in the lower coastal plain on flats, depressions, stream terraces, and flood plains. Slopes range from 0 to 2 percent. The soils of this series are loamy fine sand that is very friable and extremely acid in the upper 0-25 cm. The lower strata are similar, while the lower strata from 0.8-2 meters are comprised of fine sand.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2140765 | NA 88537 |
| 207 | NA 88538 | RJLSEUS2022-010 | Ilex glabra (L.) A. Gray | Georgia, United States | NA | | | 2023 | COLLECTED | 12/08/2022 | Junction of Old Whitley Rd & Irwinville Hwy (GA 125). | 31.64601300, -83.33625800 | 111 | Low woods, a remnant woodland/low moist habitat between agricultural fields. Growing in part shade to shade of a moist mesic (occasionally temporarily wet) mixed evergreen and deciduous woodland along the edge where light conditions are slightly higher. The underlying geology of this area is of Neogene origin and characterized as Neogene Undifferentiated. It includes poorly sorted clayey sand and gravel deposited in a fluvial environment in South Carolina but becoming more fluvio-marine in Georgia. This unit is characterized by in situ weathered feldspar and an abundance of quartzite gravel and cobbles. (Source: USGS Georgia Geologic Map Data). The primary soil types in the collection area are classified as Alapaha Loamy Sand soil (0 to 2 percent slopes, occasionally flooded). The Alapaha Series consists of very deep, poorly drained, moderately slow to slowly permeable soils in small drainageways, flats, seepage areas, and depressions. They formed in sandy and loamy marine deposits of the Southern Coastal Plain. Slopes range from 0 to 5 percent. This series consists of deep, somewhat poorly drained soils. Permeability is very slow. These nearly level to gently sloping soils formed in clayey alluvium on flood plains of streams that drain uplands of the Southern Coastal Plain. The water table ranges from 0-25 cm below the surface and the soils are strongly acid. (Source: NRCS Web Soil Survey). | Wild material | | 2140816 | NA 88538 |
| 208 | NA 88540 | RJLSEUS2022-012 | Rhododendron austrinum (Small) Rehder | Georgia, United States | NA | | | 2023 | COLLECTED | 12/09/2022 | Plants growing along the edge of a moist woodland habitat on the property at the end of the Lavender Lane cul-de-sac adjoining that of Monica Williams, in Albany, Georgia. Infrequent on the woodland edge at this site. | 31.63812300, -84.14066500 | 64 | Plants are growing in part-shade of a moist mesic, mostly deciduous, woodland along the upper fringes of seasonally moist to wet drainage area leading to a large pond and wetland habitat further downstream.
Soils: The underlying geology of this area is of Eocene origin and characterized as Ocala Limestone. The Ocala Limestone consists of almost pure limestones with occasional dolomites. It can be subdivided into both lower and upper facies with the lower facies composed of a whitish to cream-colored, fine to medium grained, poorly to moderately hard, fossil rich grainstone and packstone. The upper Ocala is white and somewhat weak and poorly sorted. It is extremely fossil rich grainstone, packstone and wackestone and some chert is common in the upper facies.
Source: USGS Georgia Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=GANu%3B1)
The primary soil types in the collection area are classified as Herod and Muckalee Series soils. The Herod Series consists of poorly drained moderately permeable soils formed in loamy alluvium. These soils are on flood plains of streams in the Coastal Plain. Slopes range from 0 to 2 percent. The Muckalee Series consists of poorly drained moderately permeable soils formed in loamy and sandy alluvium. These soils are on flood plains of streams in the Coastal Plain. Slopes range from 0 to 2 percent.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2140767 | NA 88540 |
| 209 | NA 88541 | RJLSEUS2022-013 | Rhododendron viscosum (L.) Torr. | Georgia, United States | NA | | | 2023 | COLLECTED | 12/09/2022 | Plants growing around a pond and associated wetland on the property of Monica Williams north of Albany, Georgia. Common along the edges of the pond and wetland area. | 31.63828300, -84.13827000 | 62 | Plants are growing in part-shade to sun of a wetland habitat on the edge of a large pond. The habitat is comprised of numerous hummocks where this species grows, slightly above the permanently wet, inundated edges of the pond. Some plants are growing in more shade under moist mesic conditions as well.
Soils: The underlying geology of this area is of Eocene origin and characterized as Ocala Limestone. The Ocala Limestone consists of almost pure limestones with occasional dolomites. It can be subdivided into both lower and upper facies with the lower facies composed of a whitish to cream-colored, fine to medium grained, poorly to moderately hard, fossil rich grainstone and packstone. The upper Ocala is white and somewhat weak and poorly sorted. It is extremely fossil rich grainstone, packstone and wackestone and some chert is common in the upper facies.
Source: USGS Georgia Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=GANu%3B1)
The primary soil types in the collection area are classified as Herod and Muckalee Series soils. The Herod Series consists of poorly drained moderately permeable soils formed in loamy alluvium. These soils are on flood plains of streams in the Coastal Plain. Slopes range from 0 to 2 percent. The Muckalee Series consists of poorly drained moderately permeable soils formed in loamy and sandy alluvium. These soils are on flood plains of streams in the Coastal Plain. Slopes range from 0 to 2 percent.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2140768 | NA 88541 |
| 210 | NA 88542 | RJLSEUS2022-014 | Rosa palustris Marshall | Georgia, United States | NA | | | 2023 | COLLECTED | 12/09/2022 | Plants growing around a pond and associated wetland on the property of Monica Williams north of Albany, Georgia. Common along the transitional edges from wet to dry. | 31.63723900, -84.13776200 | 60 | Plants are growing in full sun mostly in the transitional edges of the pond where conditions are generally moist mesic. Even so, this species appears quite adaptable and can be found in quite moist as well as drier soil conditions.
Soils: The underlying geology of this area is of Eocene origin and characterized as Ocala Limestone. The Ocala Limestone consists of almost pure limestones with occasional dolomites. It can be subdivided into both lower and upper facies with the lower facies composed of a whitish to cream-colored, fine to medium grained, poorly to moderately hard, fossil rich grainstone and packstone. The upper Ocala is white and somewhat weak and poorly sorted. It is extremely fossil rich grainstone, packstone and wackestone and some chert is common in the upper facies.
Source: USGS Georgia Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=GANu%3B1)
The primary soil types in the collection area are classified as Herod and Muckalee Series soils. The Herod Series consists of poorly drained moderately permeable soils formed in loamy alluvium. These soils are on flood plains of streams in the Coastal Plain. Slopes range from 0 to 2 percent. The Muckalee Series consists of poorly drained moderately permeable soils formed in loamy and sandy alluvium. These soils are on flood plains of streams in the Coastal Plain. Slopes range from 0 to 2 percent.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2140817 | NA 88542 |
| 211 | NA 88543 | RJLSEUS2022-015 | Rhododendron alabamense Rehder | Georgia, United States | NA | | | 2023 | COLLECTED | 12/09/2022 | Plants growing above a pond in drier upland conditions as well as along the banks of the Muckalee Creek on the property of Monica Williams north of Albany, Georgia. Infrequent, but occasionally seen in drier woods; more common along Muckalee Creek. | 31.63566400, -84.13379600 | 61 | Plants are growing in part-shade to shade of well-drained to drier understory conditions of a mixed evergreen and deciduous woodland, approximately 2 meters above Muckalee Creek, on sandy benches where occasional scouring has resulted in lower competition. Plants are occasionally impacted by flooding; however, they are not subjected to extended periods of high moisture on a regular basis.
Soils: The underlying geology of this area is of Eocene origin and characterized as Ocala Limestone. The Ocala Limestone consists of almost pure limestones with occasional dolomites. It can be subdivided into both lower and upper facies with the lower facies composed of a whitish to cream-colored, fine to medium grained, poorly to moderately hard, fossil rich grainstone and packstone. The upper Ocala is white and somewhat weak and poorly sorted. It is extremely fossil rich grainstone, packstone and wackestone and some chert is common in the upper facies.
Source: USGS Georgia Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=GANu%3B1)
The primary soil types in the collection area are classified as Herod and Muckalee Series soils. The Herod Series consists of poorly drained moderately permeable soils formed in loamy alluvium. These soils are on flood plains of streams in the Coastal Plain. Slopes range from 0 to 2 percent. The Muckalee Series consists of poorly drained moderately permeable soils formed in loamy and sandy alluvium. These soils are on flood plains of streams in the Coastal Plain. Slopes range from 0 to 2 percent.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2140769 | NA 88543 |
| 212 | NA 88544 | RJLSEUS2022-016 | Itea virginica L. | Georgia, United States | NA | | | 2023 | COLLECTED | 12/09/2022 | Plants growing around a pond and associated wetland on the property of Monica Williams north of Albany, Georgia as well as the edges of nearby Muckalee Creek. Common in the wetland habitat edges. | 31.63834700, -84.13835600 | 63 | Plants are growing in part-shade to sun in wet to inundated conditions along the edges of a pond as well as the edges of Muckalee Creek. This species is found in conditions of abundant, year-round moisture.
Soils: The underlying geology of this area is of Eocene origin and characterized as Ocala Limestone. The Ocala Limestone consists of almost pure limestones with occasional dolomites. It can be subdivided into both lower and upper facies with the lower facies composed of a whitish to cream-colored, fine to medium grained, poorly to moderately hard, fossil rich grainstone and packstone. The upper Ocala is white and somewhat weak and poorly sorted. It is extremely fossil rich grainstone, packstone and wackestone and some chert is common in the upper facies.
Source: USGS Georgia Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=GANu%3B1)
The primary soil types in the collection area are classified as Herod and Muckalee Series soils. The Herod Series consists of poorly drained moderately permeable soils formed in loamy alluvium. These soils are on flood plains of streams in the Coastal Plain. Slopes range from 0 to 2 percent. The Muckalee Series consists of poorly drained moderately permeable soils formed in loamy and sandy alluvium. These soils are on flood plains of streams in the Coastal Plain. Slopes range from 0 to 2 percent.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2140770 | NA 88544 |
| 213 | NA 88549 | RJLSEUS2022-022 | Rhododendron minus Michx. var. minus | Georgia, United States | NA | | | 2023 | COLLECTED | 12/10/2022 | East side of Georgia State Hwy. 39, on the south side of Kolomoki Creek approximately 11 kilometers south of Fort Gaines, Georgia. Common on this site, but otherwise infrequent. This species is near the southernmost end of its natural range. | 31.52053400, -85.02351600 | 53 | Plants are growing in part-shade to shade of deciduous upland, dry, deciduous woodlands on steep slopes 10-15 meters above Kolomoki Creek.
Soils: The underlying geology of this area is of Paleocene origin and characterized as Tuscahoma Sand. As mapped this formation includes lower Eocene Bashi Marl Member of the Hatchetigbee Formation. This formation consists of light-gray to light-olive-gray laminated and thin-bedded carbonaceous silt and clay interbedded with fine sand; thin lignite beds occur locally. Lower part of the formation includes beds of fossiliferous, glauconitic fine quartz sand containing spheroidal sandstone concretions, gravel and clay pebbles.
Source: USGS Georgia Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=GANu%3B1)
The primary soil types in the collection area are classified as Ailey-Cowarts Complex Series soils (8 to 25 percent slopes). The Ailey Series consists of well drained or somewhat excessively drained soils formed by fluviomarine and marine deposits. These soils are found marine terraces and low hills of the upper coastal plain and sandhills; they are strongly acidic. The Cowarts Series consists of very deep, moderately well and well drained soils on ridge tops and side slopes on uplands of the Coastal Plain Major Land Resource Area. They formed in loamy marine sediments. Slopes range from 1 to 60 percent.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2140776 | NA 88549 |
| 214 | NA 88550 | RJLSEUS2022-023 | Kalmia latifolia L. | Georgia, United States | NA | | | 2023 | COLLECTED | 12/10/2022 | East side of Georgia State Hwy. 39, on the south side of Kolomoki Creek approximately 11 kilometers south of Fort Gaines, Georgia. Common on this site, but otherwise infrequent. This species is near the southernmost end of its natural range. | 31.52053400, -85.02351600 | 53 | Plants are growing in part-shade to shade of deciduous upland, dry, deciduous woodlands on steep slopes 10-15 meters above Kolomoki Creek.
Soils: The underlying geology of this area is of Paleocene origin and characterized as Tuscahoma Sand. As mapped this formation includes lower Eocene Bashi Marl Member of the Hatchetigbee Formation. This formation consists of light-gray to light-olive-gray laminated and thin-bedded carbonaceous silt and clay interbedded with fine sand; thin lignite beds occur locally. Lower part of the formation includes beds of fossiliferous, glauconitic fine quartz sand containing spheroidal sandstone concretions, gravel and clay pebbles.
Source: USGS Georgia Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=GANu%3B1)
The primary soil types in the collection area are classified as Ailey-Cowarts Complex Series soils (8 to 25 percent slopes). The Ailey Series consists of well drained or somewhat excessively drained soils formed by fluviomarine and marine deposits. These soils are found marine terraces and low hills of the upper coastal plain and sandhills; they are strongly acidic. The Cowarts Series consists of very deep, moderately well and well drained soils on ridge tops and side slopes on uplands of the Coastal Plain Major Land Resource Area. They formed in loamy marine sediments. Slopes range from 1 to 60 percent.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2140777 | NA 88550 |
| 215 | NA 88551 | RJLSEUS2022-024 | Rhododendron minus Michx. var. minus | Alabama, United States | NA | | | 2023 | COLLECTED | 12/10/2022 | Plants growing on the west side of George H. Grimsley Highway (Alabama State Hwy. 95) on the bluffs above the south side of Abbie Creek. Common on this site, but otherwise infrequent. This species is near the southernmost end of its natural range. | 31.47254800, -85.16304800 | 67 | Plants are growing in part-shade to shade of a mixed evergreen and deciduous woodland on the dry well-drained bluffs 4-5 meters above Abbie Creek.
Soils: The underlying geology of this area is of Holocene origin and characterized as Alluvial, coastal and low terrace deposits. Varicolored fine to coarse quartz sand containing clay lenses and gravel in places.
Source: USGS Alabama Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=ALHalt%3B0)
The primary soil types in the collection area are classified as Bonneau Loamy Fine Sand soil (0 to 2 percent slopes). The Bonneau Series consists of very deep, well drained, moderately permeable soils on the middle and upper coastal plain. They were formed by marine and fluviomarine deposits. Slopes range from 0 to 12 percent. Soils are comprised of very friable loamy sand that is strongly acid in the upper 0.7 meters. The lower strata to 2 meters are comprised of sandy clay loam that is friable, sometimes with oxidized iron, and strongly acid.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2140778 | NA 88551 |
| 216 | NA 88552 | RJLSEUS2022-025 | Hydrangea quercifolia W. Bartram | Alabama, United States | NA | | | 2023 | COLLECTED | 12/12/2022 | Claiborne Bluffs area along unnamed road to boat ramp on the east side of the Alabama River at the U.S. Highway 84 bridge over the river. Common at this location and along the nearby Alabama River. | 31.54879700, -87.51416400 | 40 | Plants are growing in part-shade to shade of mesic, well-drained, circum-neutral slopes and benches in mature mixed deciduous and evergreen woodlands with good litter layer. Soils: The underlying geology of this area is the Jackson Group Undifferentiated. The units of the Jackson Group are the Yazoo Clay and Crystal River and Moodys Branch Formations. Descriptions of the members of the Yazoo Clay follow in descending order. Shubuta Member - in western Alabama consists of light-greenish-gray to white plastic fossiliferous, calcareous clay containing irregular calcareous nodules. From the Tombigbee River eastward, the Shubuta becomes more calcareous and grades into massive clayey glauconitic limestone. Eastward from the Alabama River, equivalent beds grade into the Crystal River Formation. Pachuta Marl Member - light-greenish-grey glauconitic, fossiliferous clayey sand and sandy limestone traceable from western Alabama eastward to Covington County where it grades into the Crystal River Formation. Cocoa Sand Member - yellowish-gray firm calcareous, fossiliferous fine to medium sand or sandy limestone or greenish-grey micaceous, calcareous, very clayey sand. Calcareous and clayey sand equivalent to the Cocoa is traceable from western Alabama to the Conecuh River area. (Source: USGS Alabama Geological Map Data). The surface soil profile of this portion of the bluffs along the Alabama River are characterized as Saffell-Lucy (Flomaton) Series Complex soils. The Saffell Series consists of very deep, well drained, moderately permeable soils that formed in loamy and gravelly marine sediments of the Tertiary Age and have acid reaction. These soils are found on the upper portion of the bluffs along the Alabama River. The Lucy Series consists of very deep, well drained, moderately permeable soils on uplands. They formed in sandy and loamy marine and fluvial sediments of the Southern Coastal Plain Major Land Resource Area. Soil reaction runs from strongly to moderately acid. The Flomaton Series consists of very deep, excessively drained, rapidly permeable soils on uplands of the Southern Coastal Plain Major Land Resource Area. They formed in gravelly sandy marine sediments and also have an acid reaction. The remainder of soils are of miscellaneous origin. (Source: USDA-NRCS Official Soil Series Descriptions). | Wild material | | 2140779 | NA 88552 |
| 217 | NA 88553 | RJLSEUS2022-026 | Hydrangea arborescens L. | Alabama, United States | NA | | | 2023 | COLLECTED | 12/12/2022 | Claiborne Bluffs area along unnamed road to boat ramp on the east side of the Alabama River at the U.S. Highway 84 bridge over the river. Occasionally found in the woodlands. | 31.54940700, -87.51366200 | 25 | Plants are growing in part-shade to shade of mesic, well-drained, circum-neutral slopes mature mixed deciduous and evergreen woodlands where slopes are exposed and detritus does not build up.
Soils: The underlying geology of this area is the Jackson Group Undifferentiated. The units of the Jackson Group are the Yazoo Clay and Crystal River and Moodys Branch Formations. Descriptions of the members of the Yazoo Clay follow in descending order. Shubuta Member - in western Alabama consists of light-greenish-gray to white plastic fossiliferous, calcareous clay containing irregular calcareous nodules. From the Tombigbee River eastward, the Shubuta becomes more calcareous and grades into massive clayey glauconitic limestone. Eastward from the Alabama River, equivalent beds grade into the Crystal River Formation. Pachuta Marl Member - light-greenish-grey glauconitic, fossiliferous clayey sand and sandy limestone traceable from western Alabama eastward to Covington County where it grades into the Crystal River Formation. Cocoa Sand Member - yellowish-gray firm calcareous, fossiliferous fine to medium sand or sandy limestone or greenish-grey micaceous, calcareous, very clayey sand. Calcareous and clayey sand equivalent to the Cocoa is traceable from western Alabama to the Conecuh River area.
Source: USGS Alabama Geological Map Data (https://mrdata.usgs.gov/geology/state/state.php?state=AL)
The surface soil profile of this portion of the bluffs along the Alabama River are characterized by Saffell-Lucy (Flomaton) Series Complex soils. The Saffell Series consists of very deep, well drained, moderately permeable soils that formed in loamy and gravelly marine sediments of the Tertiary Age and have acid reaction. These soils are found on the upper portion of the bluffs along the Alabama River. The Lucy Series consists of very deep, well drained, moderately permeable soils on uplands. They formed in sandy and loamy marine and fluvial sediments of the Southern Coastal Plain Major Land Resource Area. Soil reaction runs from strongly to moderately acid. The Flomaton Series consists of very deep, excessively drained, rapidly permeable soils on uplands of the Southern Coastal Plain Major Land Resource Area. They formed in gravelly sandy marine sediments and also have an acid reaction. The remainder of soils are of miscellaneous origin.
Source: USDA-NRCS Official Soil Series Descriptions (https://soilseries.sc.egov.usda.gov/osdname.aspx) | Wild material | | 2140780 | NA 88553 |
| 218 | NA 88554 | RJLSEUS2022-027 | Rhododendron alabamense Rehder | Alabama, United States | NA | | | 2023 | COLLECTED | 12/12/2022 | Plants growing on woodland slopes around and below the hilltop parking area leading down to the Silver Creek Lake Campground off of Silver Creek Lake Road. Occasional in the upland woodlands. | 31.66613100, -87.57625700 | 49 | Plants are growing in shade of upland dry mesic mature mixed deciduous and evergreen woodland. Generally, the overstory is thinner and there is less leaf litter cover, making the surface soil conditions drier.
Soils: The underlying geology of this area is Claiborne Group, Tallahatta Formation, of Eocene origin, with white to very light-greenish-gray thin-bedded to massive siliceous claystone; interbedded with thin layers of fossiliferous clay, sandy clay, and glauconitic sand and sandstone.
Source: USGS Alabama Geological Map Data (https://mrdata.usgs.gov/geology/state/state.php?state=AL)
The primary soil types in the collection area are classified as Smithdale-Boykin Complex soils (2 to 5 percent slopes). The Smithdale Series consists of very deep, well drained, moderately permeable soils on ridge tops and hill slopes in dissected uplands of the Southern Coastal Plain and in the Western Coastal Plain. They formed in thick beds of loamy marine sediments and are strongly acid. Slopes range from 1 to 60 percent. The Boykin Series consists of deep, well drained, moderately permeable soils that formed in sandy and loamy coastal plain sediments of Pleistocene age. These soils are on gently sloping to moderately steep uplands. Slopes range from 1 to 20 percent.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2140781 | NA 88554 |
| 219 | NA 88555 | RJLSEUS2022-028 | Rhododendron canescens (Michx.) Sweet | Alabama, United States | NA | | | 2023 | COLLECTED | 12/12/2022 | Plants growing on woodland slopes below the hilltop parking area leading down to the Silver Creek Lake Campground off of Silver Creek Lake Road. Occasional in the woodlands. | 31.66549700, -87.57624500 | 45 | Plants are growing in shade of moist mesic deciduous and evergreen woodland, mid-slope between the upland dry mesic zone and the creekside habitat below.
Soils: The underlying geology of this area is Claiborne Group, Tallahatta Formation, of Eocene origin, with white to very light-greenish-gray thin-bedded to massive siliceous claystone; interbedded with thin layers of fossiliferous clay, sandy clay, and glauconitic sand and sandstone.
Source: USGS Alabama Geological Map Data (https://mrdata.usgs.gov/geology/state/state.php?state=AL)
The primary soil types in the collection area are classified as Luverne Sandy Loam soils (15 to 35 percent slopes). The Luverne Series consists of very deep, well drained, moderately slowly permeable soils on dissected uplands of the Southern Coastal Plain. They formed in stratified marine sediments and are strongly acid. The lower strata of this series are clay and clay loam. Slopes range from 1 to 45 percent.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2140782 | NA 88555 |
| 220 | NA 88556 | RJLSEUS2022-029 | Rhododendron colemanii R. F. Mill. | Alabama, United States | NA | | | 2023 | COLLECTED | 12/12/2022 | Plants growing on woodland slopes below the hilltop parking area leading down to the Silver Creek Lake Campground off of Silver Creek Lake Road. Occasional in the woodlands. | 31.66503300, -87.57468000 | 43 | Plants are growing in shade of moist mesic deciduous and evergreen woodland on rich slopes 1-3 meters above a small spring-fed creek.
Soils: The underlying geology of this area is Claiborne Group, Tallahatta Formation, of Eocene origin, with white to very light-greenish-gray thin-bedded to massive siliceous claystone; interbedded with thin layers of fossiliferous clay, sandy clay, and glauconitic sand and sandstone.
Source: USGS Alabama Geological Map Data (https://mrdata.usgs.gov/geology/state/state.php?state=AL)
The primary soil types in the collection area are classified as Smithdale-Boykin Complex soils (2 to 5 percent slopes). The Smithdale Series consists of very deep, well drained, moderately permeable soils on ridge tops and hill slopes in dissected uplands of the Southern Coastal Plain and in the Western Coastal Plain. They formed in thick beds of loamy marine sediments and are strongly acid. Slopes range from 1 to 60 percent. The Boykin Series consists of deep, well drained, moderately permeable soils that formed in sandy and loamy coastal plain sediments of Pleistocene age. These soils are on gently sloping to moderately steep uplands. Slopes range from 1 to 20 percent.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2140783 | NA 88556 |
| 221 | NA 88557 | RJLSEUS2022-030 | Ilex longipes Chapm. ex Trel. | Alabama, United States | NA | | | 2023 | COLLECTED | 12/12/2022 | Silver Creek Lake Campground off of Silver Creek Lake Road: woodland slopes below the hilltop parking lot leading down to the campground. | 31.66442800, -87.57461400 | 39 | Part shade of moist-mesic, mixed deciduous and evergreen woodland on dry, well-drained bank, 1-2 meters above a small spring-fed creek. The underlying geology of this area is Claiborne Group, Tallahatta Formation, of Eocene origin, with white to very light-greenish-gray thin-bedded to massive siliceous claystone; interbedded with thin layers of fossiliferous clay, sandy clay, and glauconitic sand and sandstone. (Source: USGS Alabama Geological Map Data). The primary soil types in the collection area are classified as Arundel-Cantuche Complex soils (15 to 35 percent slopes). The Arundel Series consists of moderately deep, well drained, very slowly permeable soils on dissected uplands of the Southern Coastal Plain. They formed in marine deposits consisting of acid clays underlain by horizontally bedded sandstone, buhrstone and siltstone. These soils are strongly acid. Slopes range from 2 to 60 percent. The Cantuche Series consists of shallow, well drained, moderately permeable soils that formed over horizontally bedded claystone. These soils are on narrow ridgetops and narrow benches on steep side-slopes of dissected landscapes in the Coastal Plain. They are strongly acid. Slopes range from 2 to 35 percent. (Source: NRCS Web Soil Survey). | Wild material | | 2140818 | NA 88557 |
| 222 | NA 88560 | RJLSEUS2022-033 | Hydrangea arborescens L. | Alabama, United States | NA | | | 2023 | COLLECTED | 12/12/2022 | Plants growing along the west side of Ferry Road at Haines Island Park leading down to the Alabama River. | 31.72299700, -87.46798200 | 46 | Plants are growing in part-shade in the scoured ditch and slope alongside Ferry Road; occasionally in moss where seed undoubtedly germinated.
Soils: The underlying geology of this area is Claiborne Group, Tallahatta Formation, of Eocene origin, with white to very light-greenish-gray thin-bedded to massive siliceous claystone; interbedded with thin layers of fossiliferous clay, sandy clay, and glauconitic sand and sandstone.
Source: USGS Alabama Geological Map Data (https://mrdata.usgs.gov/geology/state/state.php?state=AL)
The primary soil type in the collection area is classified as Arundel Loam soil (8 to 35 percent slopes). The Arundel Series consists of moderately deep, well drained, very slowly permeable soils on dissected uplands of the Southern Coastal Plain. They formed in marine deposits consisting of acid clays underlain by horizontally bedded sandstone, buhrstone and siltstone. These soils are strongly acid. Slopes range from 2 to 60 percent.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2140785 | NA 88560 |
| 223 | NA 88563 | RJLSEUS2022-036 | Ilex myrtifolia Walter | Florida, United States | NA | | | 2023 | COLLECTED | 12/14/2022 | Eglin Air Forece Base: growing along the east side of Eglin AFB Choctaw Nolf Road northwest of Choctaw Navy Outlying Field. This road goes west and takes a circuitous route to the north around the Field en route to Escribano Point Wildlife Management Area. | 30.52650500, -86.96471100 | 10 | Part shade to sun in permanently wet areas of mixed evergreen and deciduous woodlands, mostly along the edges where higher light conditions prevail. The underlying geology of this area is the Citronelle Formation, of Pliocene origin, and consists of gray to orange, often mottled, unconsolidated to poorly consolidated, very fine to very coarse, poorly sorted, clean to clayey sands. It contains significant amounts of clay, silt and gravel which may occur as beds and lenses and may vary considerably over short distances. Limonite nodules and limonite-cemented beds are common. (Source: USGS Florida Geologic Map Data). The primary soil types in the collection area are classified as Pactolus Loamy Sand soils (0 to 5 percent slopes). The Pactolus Series consists of very deep, moderately well to somewhat poorly drained soils. Permeability is rapid. These Coastal Plain soils, typically found with streams and marine terraces and were formed by loamy and sandy fluvial sediments and marine sediments. The strata is, generally, uniformly loamy sand that is very friable and strongly acid from the surface to a depth of 1.8 meters. (Source: NRCS Web Soil Survey). | Wild material | | 2140820 | NA 88563 |
| 224 | NA 88564 | RJLSEUS2022-037 | Aronia arbutifolia (L.) Pers. | Florida, United States | NA | | | 2023 | COLLECTED | 12/14/2022 | Plants growing along the west side of Eglin AFB Choctaw Nolf Road northwest of Choctaw Navy Outlying Field. This road goes west and takes circuitous route to the north around the Field enroute to Escribano Point Wildlife Management Area. Frequent in wet areas. | 30.52667900, -86.96485200 | 60 | Plants are growing in part-shade to full sun of moist to wet depressions in areas where wetland herbaceous plants dominate allowing for more light.
Soils: The underlying geology of this area is the Citronelle Formation, of Pliocene origin, and consists of gray to orange, often mottled, unconsolidated to poorly consolidated, very fine to very coarse, poorly sorted, clean to clayey sands. It contains significant amounts of clay, silt and gravel which may occur as beds and lenses and may vary considerably over short distances. Limonite nodules and limonite-cemented beds are common. Source: USGS Florida Geologic Map Data (https://mrdata.usgs.gov/geology/state/state.php?state=fl)
The surface soil profile of this area is primarily Dorovan-Pamlico Series Association. The Dorovan Series consists of very deep, very poorly drained, moderately permeable soils on densely forested flood plains, hardwood swamps and Southern Coastal Plain Major Land Resource Areas. They were formed in highly decomposed acid-organic materials. Slopes are less than 1 percent. The organic material ranges from 1.3-2.1 meters thick. Reaction is extremely acid to very strongly acid in the organic layers and very strongly acid or strongly acid in the mineral layers. The Pamlico Series consists of very poorly drained soils that formed in decomposed organic material underlain by dominantly sandy sediment. The soils are on nearly level flood plains, bays, and depressions of the Coastal Plain. Slopes are less than 1 percent. Pamlico soils have 0.4-1.3 meters of organic material over dominantly sandy sediments. Reaction is extremely in the organic layers and ranges from extremely acid to strongly acid in the underlying mineral layers.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2140821 | NA 88564 |
| 225 | NA 88565 | RJLSEUS2022-038 | Ilex ambigua Torr. | Florida, United States | NA | | | 2023 | COLLECTED | 12/14/2022 | Eglin Air Force Base: growing along the east side of Eglin AFB Choctaw Nolf Road northwest of Choctaw Navy Outlying Field. This road goes west and takes circuitous route to the north around the Field en route to Escribano Point Wildlife Management Area. | 30.51507900, -86.96767100 | 14 | Full sun on the top of the roadside slope in well-drained to dry conditions, 1-2 meters above surrounding lower, moist area. The underlying geology of this area is the Citronelle Formation, of Pliocene origin, and consists of gray to orange, often mottled, unconsolidated to poorly consolidated, very fine to very coarse, poorly sorted, clean to clayey sands. It contains significant amounts of clay, silt and gravel which may occur as beds and lenses and may vary considerably over short distances. Limonite nodules and limonite-cemented beds are common. (Source: USGS Florida Geologic Map Data). The primary soil type in the collection area is classified as Lakeland Sand soils (5 to 12 percent slopes). The surface soil profile of this area is primarily the Lakeland series which consists of very deep, excessively drained, rapid to very rapidly permeable soils on uplands. They formed in thick beds of eolian or marine and/or fluvio-marine sands. Thickness of the sand exceeds 2 meters. Silt plus clay in the upper meter ranges from 5-10 percent. Reaction ranges from very strongly acid to moderately acid throughout. (Source: NRCS Web Soil Survey). | Wild material | | 2140822 | NA 88565 |
| 226 | NA 88569 | RJLSEUS2022-042 | Ilex hybr. | Florida, United States | NA | | | 2023 | COLLECTED | 12/15/2022 | Yellow River: this plant is growing on the edge of the Yellow River and accessed by boat. This collection located approximately 0.4 kilometers north of the Yellow River Boat Ramp on the east side of Florida State Hwy 87. | 30.57317600, -86.92367500 | 1 | This plant was found growing in full sun in permanently saturated to submersed conditions along the edge of the Yellow River, growing in an open river edge with no overstory. Like most of the plants along the river, this collection is adapted to acidic conditions and while the aquatic habitats are generally fresh water, there can occasionally be tidal or hurricane-caused saltwater intrusions. The underlying geology of this area is classified as Alluvium, of Pleistocene/Holocene origin and consists of undifferentiated Quaternary sediments of varying thickness including siliciclastics, organics and freshwater carbonates. The siliciclastics are light gray, tan, brown to black, unconsolidated to poorly consolidated, clean to clayey, silty, unfossiliferous, variably organic-bearing sands to blue green to olive green, poorly to moderately consolidated, sandy, silty clays. Organics occur as plant debris, roots, disseminated organic matrix and beds of peat. Freshwater carbonates, often referred to as marls in the literature, are scattered. (Source: USGS Florida Geologic Map Data). The surface soil profile of this area is primarily Bibb-Kinston Series Association. Bibb Series soils are coarse-loamy, sandy, acid soils that are poorly drained. They are soils of flood plains and streams subject to frequent flooding. These are found in association with Kinston Series soils that are fine-loamy, sandy, acid soils of flood plains and stream subject to frequent flooding. The Bibb-Kinston association ranges from 1-1.5 meters thick and is strongly acid. (Source: Soil Survey of Santa Rosa County and NRCS Web Soil Survey). | Wild material | Ilex putative natural hybrid (I. myrtifolia x I. opaca) | 2140823 | NA 88569 |
| 227 | NA 88570 | RJLSEUS2022-043 | Ilex myrtifolia Walter | Florida, United States | NA | | | 2023 | COLLECTED | 12/15/2022 | Yellow River: plants are growing along a several mile stretch of the Yellow River and accessed by boat via the Yellow River Boat Ramp on the east side of Florida State Hwy 87. | 30.58148800, -86.91121900 | 1 | Plants are typically found growing in full sun to part shade in permanently saturated to submersed conditions along the edge of the Yellow River, growing in association with a wide array of deciduous and evergreen trees, shrubs and perennial plant species. Most of the plants along the river are adapted to acidic conditions and, while the aquatic habitats are generally fresh water, there is occasionally tidal or hurricane-caused saltwater intrusions. The underlying geology of this area is classified as Alluvium, of Pleistocene/Holocene origin and consists of undifferentiated Quaternary sediments of varying thickness including siliciclastics, organics and freshwater carbonates. The siliciclastics are light gray, tan, brown to black, unconsolidated to poorly consolidated, clean to clayey, silty, unfossiliferous, variably organic-bearing sands to blue green to olive green, poorly to moderately consolidated, sandy, silty clays. Organics occur as plant debris, roots, disseminated organic matrix and beds of peat. Freshwater carbonates, often referred to as marls in the literature, are scattered. (Source: USGS Florida Geologic Map Data). The surface soil profile of this area is primarily Bibb-Kinston Series association. Bibb Series soils are coarse-loamy, sandy, acid soils that are poorly drained. They are soils of flood plains and streams subject to frequent flooding. These are found in association with Kinston Series soils that are fine-loamy, sandy, acid soils of flood plains and stream subject to frequent flooding. The Bibb-Kinston association ranges from 1-1.5 meters thick and is strongly acid. (Source: Soil Survey of Santa Rosa County and NRCS Web Soil Survey). | Wild material | | 2140824 | NA 88570 |
| 228 | NA 88571 | RJLSEUS2022-044 | Itea virginica L. | Florida, United States | NA | | | 2023 | COLLECTED | 12/15/2022 | Plants are growing along a several mile stretch of the Yellow River and accessed by boat via the Yellow River Boat Ramp on the east side of Florida State Hwy 87. The species is common along several miles of the Yellow River. | 30.55805600, -86.93544500 | 1 | Plants are typically found growing in part-shade to sun in permanently saturated to submersed conditions along the edge of the Yellow River, growing in association with a wide array of deciduous and evergreen trees, shrubs and perennial plant species. Most of the plants along the river are adapted to acidic conditions and, while the aquatic habitats are generally fresh water, there is occasionally tidal or hurricane-caused saltwater intrusions.
Soils: The underlying geology of this area is classified as Alluvium, of Pleistocene/Holocene origin and consists of undifferentiated Quaternary sediments of varying thickness including siliciclastics, organics and freshwater carbonates. The siliciclastics are light gray, tan, brown to black, unconsolidated to poorly consolidated, clean to clayey, silty, unfossiliferous, variably organic-bearing sands to blue green to olive green, poorly to moderately consolidated, sandy, silty clays. Organics occur as plant debris, roots, disseminated organic matrix and beds of peat. Freshwater carbonates, often referred to as marls in the literature, are scattered.
Source: USGS Florida Geologic Map Data (https://mrdata.usgs.gov/geology/state/state.php?state=fl)
The surface soil profile of this area is primarily Bibb-Kinston Series association. Bibb Series soils are coarse-loamy, sandy, acid soils that are poorly drained. They are soils of flood plains and streams subject to frequent flooding. These are found in association with Kinston Series soils that are fine-loamy, sandy, acid soils of flood plains and stream subject to frequent flooding. The Bibb-Kinston Association ranges from 1-1.5 meters thick and is strongly acid.
Source: Soil Survey of Santa Rosa County and NRCS Web Soil Survey (https://www.nrcs.usda.gov/Internet/FSE_MANUSCRIPTS/florida/FL113/0/SantaRosa.pdf and https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2140791 | NA 88571 |
| 229 | NA 88572 | RJLSEUS2022-045 | Ilex verticillata (L.) A. Gray | Florida, United States | NA | | | 2023 | COLLECTED | 12/15/2022 | Yellow River: plants are growing along a several mile stretch of the Yellow River and accessed by boat via the Yellow River Boat Ramp on the east side of Florida State Hwy 87. | 30.57947400, -86.91906100 | 1 | Plants are typically found growing in full sun to part shade in permanently saturated to submersed conditions along the edge of the Yellow River, growing in association with a wide array of deciduous and evergreen trees, shrubs and perennial plant species. Most of the plants along the river are adapted to acidic conditions and, while the aquatic habitats are generally fresh water, there is occasionally tidal or hurricane-caused saltwater intrusions. The underlying geology of this area is classified as Alluvium, of Pleistocene/Holocene origin and consists of undifferentiated Quaternary sediments of varying thickness including siliciclastics, organics and freshwater carbonates. The siliciclastics are light gray, tan, brown to black, unconsolidated to poorly consolidated, clean to clayey, silty, unfossiliferous, variably organic-bearing sands to blue green to olive green, poorly to moderately consolidated, sandy, silty clays. Organics occur as plant debris, roots, disseminated organic matrix and beds of peat. Freshwater carbonates, often referred to as marls in the literature, are scattered. (Source: USGS Florida Geologic Map Data). The surface soil profile of this area is primarily Bibb-Kinston Series association. Bibb Series soils are coarse-loamy, sandy, acid soils that are poorly drained. They are soils of flood plains and streams subject to frequent flooding. These are found in association with Kinston Series soils that are fine-loamy, sandy, acid soils of flood plains and stream subject to frequent flooding. The Bibb-Kinston association ranges from 1-1.5 meters thick and is strongly acid. (Source: Soil Survey of Santa Rosa County and NRCS Web Soil Survey). | Wild material | | 2140825 | NA 88572 |
| 230 | NA 88573 | RJLSEUS2022-046 | Ilex myrtifolia Walter | Florida, United States | NA | | | 2023 | COLLECTED | 12/15/2022 | Yellow River: this plant is growing on the edge of the Yellow River and accessed by boat. This collection is located approximately 3.2 kilometers by boat north and east of the Yellow River Boat Ramp on the east side of Florida State Hwy 87. | 30.58188200, -86.91220500 | 1 | This plant is growing in full sun in permanently saturated conditions along the edge of the Yellow River, growing in association with a wide array of deciduous and evergreen trees, shrubs and perennial plant species. Most of the plants along the river are adapted to acidic conditions and, while the aquatic habitats are generally fresh water, there is occasionally tidal or hurricane-caused saltwater intrusions. The underlying geology of this area is classified as Alluvium, of Pleistocene/Holocene origin and consists of undifferentiated Quaternary sediments of varying thickness including siliciclastics, organics and freshwater carbonates. The siliciclastics are light gray, tan, brown to black, unconsolidated to poorly consolidated, clean to clayey, silty, unfossiliferous, variably organic-bearing sands to blue green to olive green, poorly to moderately consolidated, sandy, silty clays. Organics occur as plant debris, roots, disseminated organic matrix and beds of peat. Freshwater carbonates, often referred to as marls in the literature, are scattered. (Source: USGS Florida Geologic Map Data). The surface soil profile of this area is primarily Bibb-Kinston Series Association. Bibb Series soils are coarse-loamy, sandy, acid soils that are poorly drained. They are soils of flood plains and streams subject to frequent flooding. These are found in association with Kinston Series soils that are fine-loamy, sandy, acid soils of flood plains and stream subject to frequent flooding. The Bibb-Kinston Association ranges from 1-1.5 meters thick and is strongly acid. (Source: Soil Survey of Santa Rosa County and NRCS Web Soil Survey). | Wild material | orange-fruited form | 2140826 | NA 88573 |
| 231 | NA 88574 | RJLSEUS2022-047 | Rhododendron austrinum (Small) Rehder | Florida, United States | NA | | | 2023 | COLLECTED | 12/15/2022 | Plants are growing along a several mile stretch of the Yellow River and accessed by boat via the Yellow River Boat Ramp on the east side of Florida State Hwy 87. The species is found frequently along several miles of the Yellow River. | 30.58133600, -86.89953900 | 2 | Plants are found growing in part-shade to shade along areas of the river where natural levies, 1-3 meters tall, have formed, depositing sand and organic matter. The plants grow well-above normal flow of the river in well-drained to dry conditions. Even so, they are periodically subjected to inundation from floodwaters.
Soils: The underlying geology of this area is classified as Alluvium, of Pleistocene/Holocene origin and consists of undifferentiated Quaternary sediments of varying thickness including siliciclastics, organics and freshwater carbonates. The siliciclastics are light gray, tan, brown to black, unconsolidated to poorly consolidated, clean to clayey, silty, unfossiliferous, variably organic-bearing sands to blue green to olive green, poorly to moderately consolidated, sandy, silty clays. Organics occur as plant debris, roots, disseminated organic matrix and beds of peat. Freshwater carbonates, often referred to as marls in the literature, are scattered.
Source: USGS Florida Geologic Map Data (https://mrdata.usgs.gov/geology/state/state.php?state=fl)
The surface soil profile of this area is primarily Bibb-Kinston Series Association. Bibb Series soils are coarse-loamy, sandy, acid soils that are poorly drained. They are soils of flood plains and streams subject to frequent flooding. These are found in association with Kinston Series soils that are fine-loamy, sandy, acid soils of flood plains and stream subject to frequent flooding. The Bibb-Kinston Association ranges from 1-1.5 meters thick and is strongly acid.
Source: Soil Survey of Santa Rosa County and NRCS Web Soil Survey (https://www.nrcs.usda.gov/Internet/FSE_MANUSCRIPTS/florida/FL113/0/SantaRosa.pdf and https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | Yellow River Pink Austrinum | 2140792 | NA 88574 |
| 232 | NA 88576 | RJLSEUS2022-049 | Rhododendron atlanticum (Ashe) Rehder | South Carolina, United States | NA | | | 2023 | COLLECTED | 12/16/2022 | Plants growing in mixed evergreen and deciduous woods on the east side of Ip Canal Road approximately 0.33 kilometers south of Pleasant Hill Drive (Georgetown County Road 251). Frequent at this location. | 33.63226900, -79.25831700 | 8 | Plants are growing in part-shade to shade of a dry to periodically moist mesic woodland. Given some of the plant associates, there may be an impermeable subsurface soil layer to add moisture availability.
Soils: The underlying geology of this area is of Pleistocene origin and characterized as Socastee Formation. This is a low coastal formation in the Carolinas like Penholoway but younger and lower in altitude. The Socastee Formation lies seaward of the Penholoway and Canepatch Formations and is the next younger surficial unit. It is exposed in a belt approximately 25 km wide at elevations between 9 and 15 m above sea level. It is described as variegated quartzose sands, argillaceous sands, and clays, 5 m thick at the type section near Socastee Swamp. Unconformably overlies Canepatch Formation; unconformably underlies Waiter Island Formation and Ocean Forest Peat.
Source: USGS Texas Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=SCQso%3B1)
The primary soil type in the collection area is classified as Centenary Fine Sand. The Centenary Fine Sand Series consists of deep, well drained or somewhat excessively drained single-grained sand that is loose and moderately acid. The upper layer ranges from 7.5cm to 25cm thick. Deeper layers vary in percentage of single-grained sands and clay.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2140794 | NA 88576 |
| 233 | NA 88506 | RJL2022TX-001 | Itea virginica L. | Texas, United States | NA | | | 2022 | COLLECTED | 10/31/2022 | Plants growing at Shangri La Botanical Gardens and Nature Center, Orange, TX along Adams Bayou, accessed via internal service roads. Plant is infrequent at this site. | 30.10322000, -93.76271700 | 1 | Plants are growing in shade to part-shade of a Taxodium distichum-Nyssa aquatica dominated forested swampland associated with Adams Bayou in a wet low-lying area that is frequently inundated.
Soils: The underlying geology of this area is of Quaternary to Late Pleistocene origin and comprised of the Beaumont Formation. This formation is yellowish- to brownish-gray, locally reddish orange with very fine to fine quartz sand, silt, and minor fine gravel, intermixed and interbedded. It also includes stream channel, point-bar, cravasse-splay, and natural levee ridge deposits, and clayey fill in abandoned channels. Channel fill is dark brown to brownish-gray with laminated clay and silt that is organic-rich. Includes marine delta-front sand, lagoonal clay, and near-shore marine sand beneath and landward of bays along the coast. Depth of this unconsolidated outwash ranges from 3-100 meters thick.
Source: USGS Texas Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=TXQbs%3B0)
The primary soil types in the collection area are classified as Cowmarsh series. The Cowmarsh series consists of very deep, very poorly drained soils that formed in mucky silty clayey alluvial deposits of Holocene age. These depressional soils are oxbows and relict channels of rivers where flooding and ponding is frequent. Slope ranges from 0 to 1 percent but mainly less than 1 percent. very poorly drained. Runoff is negligible. Frequently flooded for very long periods from February through May and surface remains saturated for very long periods once flood waters have receded.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2139813 | NA 88506 |
| 234 | NA 88507 | RJL2022TX-002 | Fraxinus caroliniana Mill. | Texas, United States | NA | | | 2022 | COLLECTED | 10/31/2022 | Plants growing at Shangri La Botanical Gardens and Nature Center, Orange, TX along Adams Bayou, accessed via internal service roads. Plant is relatively common along Adams Bayou but scattered. | 30.09989400, -93.75239700 | 1 | Plants are growing in part-shade to sun of a Taxodium distichum-Nyssa aquatica dominated forested swampland associated with Adams Bayou in a wet low-lying area that is frequently inundated. While found as an occasional understory element, it is more common on the edge of the swampland forest where there are high light conditions.
Soils: The underlying geology of this area is of Quaternary to Late Pleistocene origin and comprised of the Beaumont Formation. This formation is yellowish- to brownish-gray, locally reddish orange with very fine to fine quartz sand, silt, and minor fine gravel, intermixed and interbedded. It also includes stream channel, point-bar, cravasse-splay, and natural levee ridge deposits, and clayey fill in abandoned channels. Channel fill is dark brown to brownish-gray with laminated clay and silt that is organic-rich. Includes marine delta-front sand, lagoonal clay, and near-shore marine sand beneath and landward of bays along the coast. Depth of this unconsolidated outwash ranges from 3-100 meters thick.
Source: USGS Texas Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=TXQbs%3B0)
The primary soil types in the collection area are classified as Cowmarsh series. The Cowmarsh series consists of very deep, very poorly drained soils that formed in mucky silty clayey alluvial deposits of Holocene age. These depressional soils are oxbows and relict channels of rivers where flooding and ponding is frequent. Slope ranges from 0 to 1 percent but mainly less than 1 percent. very poorly drained. Runoff is negligible. Frequently flooded for very long periods from February through May and surface remains saturated for very long periods once flood waters have receded.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2139814 | NA 88507 |
| 235 | NA 88508 | RJL2022TX-003 | Morella cerifera (L.) Small | Texas, United States | NA | | | 2022 | COLLECTED | 10/31/2022 | Plants growing at Shangri La Botanical Gardens and Nature Center Orange, TX along Adams Bayou, accessed via internal service roads. Plant is relatively common along Adams Bayou but scattered in the understory. | 30.10035500, -93.75288700 | 1 | Plants are growing in part-shade to shade of a Taxodium distichum-Nyssa aquatica dominated forested swampland associated with Adams Bayou in a wet low-lying area that is frequently inundated.
Soils: The underlying geology of this area is of Quaternary to Late Pleistocene origin and comprised of the Beaumont Formation. This formation is yellowish- to brownish-gray, locally reddish orange with very fine to fine quartz sand, silt, and minor fine gravel, intermixed and interbedded. It also includes stream channel, point-bar, cravasse-splay, and natural levee ridge deposits, and clayey fill in abandoned channels. Channel fill is dark brown to brownish-gray with laminated clay and silt that is organic-rich. Includes marine delta-front sand, lagoonal clay, and near-shore marine sand beneath and landward of bays along the coast. Depth of this unconsolidated outwash ranges from 3-100 meters thick.
Source: USGS Texas Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=TXQbs%3B0)
The primary soil types in the collection area are classified as Cowmarsh series. The Cowmarsh series consists of very deep, very poorly drained soils that formed in mucky silty clayey alluvial deposits of Holocene age. These depressional soils are oxbows and relict channels of rivers where flooding and ponding is frequent. Slope ranges from 0 to 1 percent but mainly less than 1 percent. very poorly drained. Runoff is negligible. Frequently flooded for very long periods from February through May and surface remains saturated for very long periods once flood waters have receded.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2139815 | NA 88508 |
| 236 | NA 88511 | RJL2022TX-006 | Persea palustris (Raf.) Sarg. | Texas, United States | NA | | | 2022 | COLLECTED | 11/01/2022 | Plants growing in a wetland on the north side of Clarktown Road approximately 1.5 kilometers west of Texas State Hwy 87 in Sabine National Forest. Plant is common in the moist-wet and mesic edges of the wetland habitat where it is best adapted. | 31.17114800, -93.75106200 | 71 | Plants are growing in part-shade in a depression wetland of a small upland valley stream area surrounded by upland Pinus palustris and Pinus taeda forests. While the region had a severe drought during 2022, this depression wetland remained mucky wet throughout. Higher light conditions that supported heavy fruit production on the Persea may have been due to nearby harvesting of forest sections adjacent to the wetland.
Soils: The underlying geology of this area is of Oligocene origin and characterized as Catahoula Formation. This formation is extensive and deep in Texas, up to 185 meters thick. In the area of the collection the Catahoula Formation is primarily mudstone and sand. The upper 90-150 meters is mudstone that is tuffaceous, and sandy; also, occasionally, with some bentonitic clay.
Source: USGS Texas Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=TXQbs%3B0
The primary soil types in the collection area are classified as Letney soils. These soils consist of deep, somewhat excessively drained, moderately rapidly permeable soils on uplands. They were formed in thick loamy and sandy sediments on the Western Coastal Plain. The Letney soils are on gently sloping uplands with slopes ranging from 1 to 5 percent. They are typically strongly acidic. It should be noted that the upper surface, to an unknown depth has a significant amount of decomposed and undecomposed organic litter, presumably from sphagnum, at least, in part.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2139818 | NA 88511 |
| 237 | NA 88512 | RJL2022TX-007 | Morella caroliniensis (Mill.) Small | Texas, United States | NA | | | 2022 | COLLECTED | 11/01/2022 | Plants growing in a wetland on the north side of Clarktown Road approximately 1.5 kilometers west of Texas State Hwy 87 in Sabine National Forest. Plant is relatively common in the moist-wet and mesic edges of the wetland habitat. | 31.17181200, -93.75118000 | 81 | Plants are growing in part-shade to part-sun in a depression wetland and slightly upslope of a small upland valley stream area surrounded by upland Pinus palustris and Pinus taeda forests. While the region had a severe drought during 2022, this depression wetland remained mucky wet throughout.
Soils: The underlying geology of this area is of Oligocene origin and characterized as Catahoula Formation. This formation is extensive and deep in Texas, up to 185 meters thick. In the area of the collection the Catahoula Formation is primarily mudstone and sand. The upper 90-150 meters is mudstone that is tuffaceous, and sandy; also, occasionally, with some bentonitic clay.
Source: USGS Texas Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=TXQbs%3B0
The primary soil types in the collection area are classified as Letney soils. These soils consist of deep, somewhat excessively drained, moderately rapidly permeable soils on uplands. They were formed in thick loamy and sandy sediments on the Western Coastal Plain. The Letney soils are on gently sloping uplands with slopes ranging from 1 to 5 percent. They are typically strongly acidic. It should be noted that the upper surface, to an unknown depth has a significant amount of decomposed and undecomposed organic litter, presumably from sphagnum, at least, in part.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2139819 | NA 88512 |
| 238 | NA 88513 | RJL2022TX-008 | Cephalanthus occidentalis L. | Texas, United States | NA | | | 2022 | COLLECTED | 11/01/2022 | Plants growing in moist sites on the north and south side of Clarktown Road approximately 0.5 kilometers west of Texas State Hwy 87 in Sabine National Forest. Plant is relatively common in the moist-wet and seasonally wet locations; absent elsewhere. | 31.17294500, -93.74133900 | 92 | Plants are growing in part-shade to part-sun in moist-wet areas with low competition. The area generally retains moisture throughout the growing season.
Soils: The underlying geology of this area is of Oligocene origin and characterized as Catahoula Formation. This formation is extensive and deep in Texas, up to 185 meters thick. In the area of the collection the Catahoula Formation is primarily mudstone and sand. The upper 90-150 meters is mudstone that is tuffaceous, and sandy; also, occasionally, with some bentonitic clay.
Source: USGS Texas Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=TXQbs%3B0
The primary soil types in the collection area are classified as Mattex-Iulus complex soils. The Mattex series consists of very deep, somewhat poorly drained, slowly permeable, acidic loamy soils. They formed in loamy and clayey alluvium. These are nearly level soils on flood plains. Slopes range from 0 to 1 percent. The Iulus series consists of very deep, moderately well drained, moderately permeable, soils on flood plains. These soils formed in recent alluvium derived from coastal plain sediments, often containing fine sandy elements and are extremely acidic. The slope ranges from 0 to 1 percent.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2139820 | NA 88513 |
| 239 | NA 88514 | RJL2022MD-019 | Kalmia latifolia L. | Maryland, United States | NA | | | 2022 | COLLECTED | 11/04/2022 | Plants are growing on both sides of a fire road on Maryland Heights along the edge with Harpers Ferry National Historic Park. This location was accessed from the east where Miller Avenue meets the fire road, approximately 2 kilometers away. There is no vehicular access to the collecting area. Becoming locally uncommon. This local population is likely to be extirpated in the next 20-30 years. This collector has hiked through this area for more than 35 years and seen dramatic changes in the population. When first observed, Kalmia latifolia was a dominant understory shrub on south- to west-facing slopes beneath a mature forest canopy. Over the years, at least one forest fire has significantly reduced the population, along with a continuing increase in deer populations, resulting in catastrophic browse damage. The absence of a mature forest canopy and periods of drought have almost certainly also resulted in decline of this population. While collecting seed from scattered mature plants well above deer browse levels, this collector also noted that there was virtually no recruitment taking place. | 39.32811200, -77.72242400 | 287 | Plants are growing in part-shade to shade of a deciduous upland, very rocky, and dry forest community. Plants are frequently found growing among boulders, rock outcrops, and steep-slope erosional areas, although, not exclusively.
Soils: The underlying geology of this area is of Late Cambrian to Cambrian origin and comprised of Chilhowee Group; Weverton Formation. This includes interbedded white to dark gray, thin-bedded, micaceous, ferruginous, and sericitic quartzites, phyllites, and white, thick-bedded, ledge-making quartzites; some gray to brown ferruginous quartz conglomerate and purple-banded phyllite.
Source: USGS Maryland Geologic Map Data https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=MDKp%3B5
The primary soil types in the collection area are classified as Dekalb-Bagtown-Rock outcrop complex, 25 to 65 percent slopes. The Dekalb series consists of moderately deep, excessively drained soils formed in material weathered from gray and brown acid sandstone in places interbedded with shale and graywacke. Slope ranges from 0 to 80 percent. Permeability is rapid. Solum thickness and depth to bedrock range from 50 to 100 cm. Flat, subangular or angular, sandstone fragments, 2.5-25 cm across increase with depth and range from 10-60 percent in individual horizons of the solum and from 50-90 percent or more in the C horizon. The amount of rock fragments typically increases with depth. Cobbly, channery, and very stony phases are common. Reaction ranges from extremely through strongly acid.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2139821 | NA 88514 |
| 240 | WLP 2673 | RJL2022NJ-004 | Lyonia mariana (L.) D. Don | New Jersey, United States | NA | | | 2022 | COLLECTED | 10/24/2022 | Plants growing on both sides of Duerer Street approximately 0.37 kilometers southeast of 4th Avenue, Mullica Township, New Jersey. Plants are common but scattered on both sides of the road at this site. | 39.55730700, -74.66376100 | 22 | Plants grow from part shade to full sun throughout the habit from the upper edges of the ditches through the herbaceous grass dominant buffer and all the way to the part shade of the woodland edge. Plants transition through moist/wet conditions in full sun to quite dry conditions in part shade and seem equally adapted.
Soils: The underlying geology of this area is the Cohansey Formation of middle Miocene origin and comprised of sand, white to yellow with local gravel and clay. It is sometimes locally stained red or orange brown by iron oxides and (or) cemented into large blocks of ironstone. Unweathered clay is typically dark gray, but commonly weathers white where it is interbedded with thin beds of ironstone. Sand is typically medium grained and moderately sorted although it ranges from fine to very coarse grained and from poorly to well sorted. Sand consists of quartz and siliceous rock fragments. Some beds are locally micaceous. Maximum thickness in the map area is about 60 meters; however, thickness is difficult to determine because of the irregular basal contact and extensive post-depositional erosion.
Source: USGS New Jersey Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=NJTch%3B1)
The primary soil type in the area of this collection is classified as Mullica sandy loam, 0 to 2 percent slopes. These soils are typically coarse-loamy, siliceous, semiactive, and mesic typic humaquepts that are strongly to extremely acidic throughout the profile. The typical solum thickness ranges from 50-150+ cm. These soils are generally considered to be poorly drained.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2139664 | WLP 2673 |
| 241 | NA 88500 | RJL2022NJ-002 | Ilex glabra (L.) A. Gray | New Jersey, United States | NA | | | 2022 | COLLECTED | 10/24/2022 | Mullica Township: both sides of Duerer Street, approximately 0.37 kilometers southeast of 4th Avenue. | 39.55885000, -74.66442500 | 21 | Plants growing in shade to almost full sun on compacted seasonally moist to temporarily wet areas of a mixed evergreen and deciduous woodland dominated by Pinus rigida. Vegetation of this area is very much defined by small changes in elevation that go from wet to very dry. Ilex glabra remains abundant throughout, though. Plants are abundant on the edge of the woodlands as well as the understory of the woodlands. Soils: The underlying geology of this area is the Cohansey Formation of middle Miocene origin and comprised of sand, white to yellow with local gravel and clay. It is sometimes locally stained red or orange brown by iron oxides and (or) cemented into large blocks of ironstone. Unweathered clay is typically dark gray, but commonly weathers white where it is interbedded with thin beds of ironstone. Sand is typically medium grained and moderately sorted although it ranges from fine to very coarse grained and from poorly to well sorted. Sand consists of quartz and siliceous rock fragments. Some beds are locally micaceous. Maximum thickness in the map area is about 60 meters; however, thickness is difficult to determine because of the irregular basal contact and extensive post-depositional erosion. (Source: USGS New Jersey Geologic Map Data). The primary soil type in the area of this collection is classified as Mullica sandy loam, 0 to 2 percent slopes. These soils are typically coarse-loamy, siliceous, semiactive, and mesic typic humaquepts that are strongly to extremely acidic throughout the profile. The typical solum thickness ranges from 50-150+ cm. These soils are generally considered to be poorly drained. (Source: NRCS Web Soil Survey). | Wild material | | 2139663 | NA 88500 |
| 242 | WLP 2670 | RJL2022PA-016 | Acer negundo L. | Pennsylvania, United States | NA | | | 2022 | COLLECTED | 10/21/2022 | Plants growing in woodlands above a small unnamed creek that dumps into the Middle Branch White Clay Creek in Goddard Park, West Grove Pennsylvania, off of Wickerton Road, Chester County. Plants are found regularly but scattered in the understory of the woodlands. | 39.80426000, -75.82609300 | 105 | Plants growing in a mesic, well-drained habitat of deciduous woodlands along streams and above the riparian zone that drains toward a small unnamed creek that feeds into the Middle Branch White Clay Creek. Plants generally grow in part shade to full sun, but perform best and fruit more heavily in full sun where there is abundant access to moisture. The remnant woodlands exist mostly along the steep slopes, wetlands and seeps of seasonal and year-round creeks flowing into the Middle Branch White Clay Creek. The woodlands are bordered by numerous housing developments and land converted to meadows; hence there is significant first order edge that is heavily impacted by invasive plant intrusion. Despite this fact, Acer negundo is highly competitive and competes well.
Soils: The underlying geology of this area is the Glenarm Wissahickon Formation of lower Paleozoic origin and lithologically similar to oligoclase-mica schist of the Wissahickon Formation (PZw), but also includes lenticular amphibolite bodies having ocean-floor basalt chemistry.
Source: USGS Pennsylvania Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=PAPZgw%3B0)
The primary soil type in the area of this collection is classified as Glenelg silt loam, 3 to 8 percent slopes. This series consists of very deep, well drained soils formed in residuum weathered from micaceous schist on uplands of the Blue Ridge and the Northern Piedmont. Saturated hydraulic conductivity is moderately high in the subsoil and moderately high to high in the substratum. This upper horizon of this soil is undifferentiated, mostly poorly drained sandy bottomland soils intermingled with decomposing organic litter and eroded silts and clays due to erosion.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2139661 | WLP 2670 |
| 243 | WLP 2668 | RJL2022MD-014 | Aronia arbutifolia (L.) Pers. | Maryland, United States | NA | | | 2022 | COLLECTED | 10/05/2022 | Plant growing at Elkton State Forest along road in wet woodlands near the Elk Neck State Forest Shooting Range labelled as the address of 717 Irishtown Rd, North East, MD 21901. Plant is uncommon at this site. | 39.58716100, -75.91419000 | 55 | Plants are growing in part-shade to part sun of a deciduous forest on hummocks in a very moist to wet low-lying area along a seasonal or year-round flowing seep.
Soils: The underlying geology of this area is of Cretaceous origin and comprised of Potomac Group, including Raritan and Patapsco Formations, and Patuxent Formation. The Potomac Group includes: interbedded quartzose gravels; proto-quartzitic to orthoquartzitic argillaceous sands; and white, dark gray, and multicolored silts and clays. Included withing this zone are Raritan and Patapsco Formations comprised of gray, brown, and red variegated silts and clays; lenticular, cross-bedded, argillaceous, subrounded sands; minor gravels; thickness. The Patuxent Formation is also interbedded in this zone and comprised of white or light gray to orange-brown, moderately sorted, cross-bedded, argillaceous, angular sands and subrounded quartz gravels; silts and clays subordinate that are predominantly pale gray.
Source: USGS Maryland Geologic Map Data https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=MDKp%3B5
The primary soil types in the collection area are classified as Russett-Christiana-Hambrook Complex and/or Sassafras and Croom Soils; though, others may intersect and overlay in specific areas. The soils in the collecting area are generally described as a complex series of fluviomarine deposits. The soils range from a thin loam layer at the surface to varying levels of loam to sandy loam and/or extremely gravelly sandy clay loam strata, depending upon geographical location (ie. Hillslope summits, slopes, footslopes, swales, etc.).
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2139659 | WLP 2668 |
| 244 | NA 89045 | RJL2022PA-013 | Tsuga canadensis (L.) Carrière | Pennsylvania, United States | NA | | | 2022 | COLLECTED | 10/07/2022 | Plants growing on the steep banks along Octoraro Creek accessed by canoe. Plants are locally common but generally infrequent along the Octoraro Creek. | 39.74442700, -76.08856400 | 66 | Plants are growing in part-shade to sun of mixed deciduous and evergreen forests on steep rocky habitats overlain by relatively deep soil over occasionally exposed geology along the Octoraro Creek.
Soils: The underlying geology of this area is estimated to be of lower Paleozoic origin and comprised of Peters Creek Schist. This is comprised of chlorite-sericite schist containing interbedded quartzite.
Source: USGS Pennsylvania Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=PAPZpc%3B0)
The primary soil types in the collection area are classified as Manor loam, 25 to 35 percent slopes, very stony. The soils in the collecting area originated as residuum, weathered from the micaceous schist exposed geology and are generally considered coarse-loamy, micaceous, mesic typic dystrudepts that are very acidic and well-drained. There is a variable depth of soil depending upon the steepness of slopes. Some areas contain significant exposed Peters Creek Schist overlain by a highly decomposed organic mat intermingled with a dense root mat of woody and herbaceous plants.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2139610 | NA 89045 |
| 245 | NA 89044 | RJL2022PA-012 | Rhododendron maximum L. | Pennsylvania, United States | NA | | | 2022 | COLLECTED | 10/07/2022 | Plants growing on the steep banks along Octoraro Creek accessed by canoe. Plants are locally common but generally uncommon along the Octoraro Creek. | 39.75272200, -76.08271500 | 63 | Plants are growing in part-shade to part-sun of mixed deciduous and evergreen forests on steep rocky habitats along the Octoraro Creek.
Soils: The underlying geology of this area is estimated to be of lower Paleozoic origin and comprised of Peters Creek Schist. This is comprised of chlorite-sericite schist containing interbedded quartzite.
Source: USGS Pennsylvania Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=PAPZpc%3B0)
The primary soil types in the collection area are classified as Manor loam, 25 to 60 percent slopes, very stony. The soils in the collecting area originated as residuum, weathered from the micaceous schist exposed geology and are generally considered coarse-loamy, micaceous, mesic typic dystrudepts that are very acidic and well-drained. There is a variable depth of soil depending upon the steepness of slopes. Some areas contain significant exposed Peters Creek Schist overlain by a highly decomposed organic mat intermingled with a dense root mat of woody and herbaceous plants.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2139609 | NA 89044 |
| 246 | NA 89043 | RJL2022MD-017 | Cephalanthus occidentalis L. | Maryland, United States | NA | | | 2022 | COLLECTED | 10/05/2022 | Plants growing at Elkton State Forest along road and in wet woodlands near the Elk Neck State Forest Shooting Range labelled as the address of 717 Irishtown Rd, North East, MD 21901. Plants are locally common but restricted to the low-lying wet woodlands. | 39.58727700, -75.91403900 | 55 | Plants are growing in part-shade to part-sun of deciduous forests on hummocks in very moist to wet low-lying areas along seasonal or year-round flowing seeps.
Soils: The underlying geology of this area is of Cretaceous origin and comprised of Potomac Group, including Raritan and Patapsco Formations, and Patuxent Formation. The Potomac Group includes: interbedded quartzose gravels; proto-quartzitic to orthoquartzitic argillaceous sands; and white, dark gray, and multicolored silts and clays. Included withing this zone are Raritan and Patapsco Formations comprised of gray, brown, and red variegated silts and clays; lenticular, cross-bedded, argillaceous, subrounded sands; minor gravels; thickness. The Patuxent Formation is also interbedded in this zone and comprised of white or light gray to orange-brown, moderately sorted, cross-bedded, argillaceous, angular sands and subrounded quartz gravels; silts and clays subordinate that are predominantly pale gray.
Source: USGS Maryland Geologic Map Data https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=MDKp%3B5
The primary soil types in the collection area are classified as Russett-Christiana-Hambrook Complex and/or Sassafras and Croom Soils; though, others may intersect and overlay in specific areas. The soils in the collecting area are generally described as a complex series of fluviomarine deposits. The soils range from a thin loam layer at the surface to varying levels of loam to sandy loam and/or extremely gravelly sandy clay loam strata, depending upon geographical location (ie. Hillslope summits, slopes, footslopes, swales, etc.).
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2139608 | NA 89043 |
| 247 | NA 89042 | RJL2022MD-016 | Aronia ×prunifolia (Marshall) Rehder | Maryland, United States | NA | | | 2022 | COLLECTED | 10/05/2022 | Plants growing at Elkton State Forest along road and in wet woodlands near the Elk Neck State Forest Shooting Range labelled as the address of 717 Irishtown Rd, North East, MD 21901. Plants are infrequent and were found in this one area of low-lying wet woodlands. Perhaps others would have been found upon investigation of other similar habitats. | 39.58730200, -75.91415800 | 55 | Plants are growing in part-sun to part-shade of deciduous forests on moist slopes and on hummocks in very moist to wet low-lying areas along seasonal or year-round flowing seeps.
Soils: The underlying geology of this area is of Cretaceous origin and comprised of Potomac Group, including Raritan and Patapsco Formations, and Patuxent Formation. The Potomac Group includes: interbedded quartzose gravels; proto-quartzitic to orthoquartzitic argillaceous sands; and white, dark gray, and multicolored silts and clays. Included withing this zone are Raritan and Patapsco Formations comprised of gray, brown, and red variegated silts and clays; lenticular, cross-bedded, argillaceous, subrounded sands; minor gravels; thickness. The Patuxent Formation is also interbedded in this zone and comprised of white or light gray to orange-brown, moderately sorted, cross-bedded, argillaceous, angular sands and subrounded quartz gravels; silts and clays subordinate that are predominantly pale gray.
Source: USGS Maryland Geologic Map Data https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=MDKp%3B5
The primary soil types in the collection area are classified as Russett-Christiana-Hambrook Complex and/or Sassafras and Croom Soils; though, others may intersect and overlay in specific areas. The soils in the collecting area are generally described as a complex series of fluviomarine deposits. The soils range from a thin loam layer at the surface to varying levels of loam to sandy loam and/or extremely gravelly sandy clay loam strata, depending upon geographical location (ie. Hillslope summits, slopes, footslopes, swales, etc.).
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2139607 | NA 89042 |
| 248 | NA 89041 | RJL2022MD-015 | Lyonia ligustrina (L.) DC. | Maryland, United States | NA | | | 2022 | COLLECTED | 10/05/2022 | Plants growing at Elkton State Forest along road and in wet woodlands near the Elk Neck State Forest Shooting Range labelled as the address of 717 Irishtown Rd, North East, MD 21901. Plants are common but scattered on the edges and in the understory of low-lying wet woodlands. | 39.58716100, -75.91419000 | 55 | Plants are growing in part-shade to shade of deciduous forests on moist slopes and on hummocks in very moist to wet low-lying areas along seasonal or year-round flowing seeps.
Soils: The underlying geology of this area is of Cretaceous origin and comprised of Potomac Group, including Raritan and Patapsco Formations, and Patuxent Formation. The Potomac Group includes: interbedded quartzose gravels; proto-quartzitic to orthoquartzitic argillaceous sands; and white, dark gray, and multicolored silts and clays. Included withing this zone are Raritan and Patapsco Formations comprised of gray, brown, and red variegated silts and clays; lenticular, cross-bedded, argillaceous, subrounded sands; minor gravels; thickness. The Patuxent Formation is also interbedded in this zone and comprised of white or light gray to orange-brown, moderately sorted, cross-bedded, argillaceous, angular sands and subrounded quartz gravels; silts and clays subordinate that are predominantly pale gray.
Source: USGS Maryland Geologic Map Data https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=MDKp%3B5
The primary soil types in the collection area are classified as Russett-Christiana-Hambrook Complex and/or Sassafras and Croom Soils; though, others may intersect and overlay in specific areas. The soils in the collecting area are generally described as a complex series of fluviomarine deposits. The soils range from a thin loam layer at the surface to varying levels of loam to sandy loam and/or extremely gravelly sandy clay loam strata, depending upon geographical location (ie. Hillslope summits, slopes, footslopes, swales, etc.).
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2139606 | NA 89041 |
| 249 | NA 89040 | RJL2022MD-013 | Eubotrys racemosus (L.) Nutt. | Maryland, United States | NA | | | 2022 | COLLECTED | 10/05/2022 | Plants growing at Elkton State Forest along road and in wet woodlands over a distance of about 0.55 kilometers near the Elk Neck State Forest Shooting Range labelled as the address of 717 Irishtown Rd, North East, MD 21901. Plants are common but scattered on the edges and in the understory of low-lying wet woodlands. | 39.58227200, -75.91328800 | 57 | Plants are growing in part-shade to shade of deciduous forests on moist slopes and on hummocks in very moist to wet low-lying areas along seasonal or year-round flowing seeps.
Soils: The underlying geology of this area is of Cretaceous origin and comprised of Potomac Group, including Raritan and Patapsco Formations, and Patuxent Formation. The Potomac Group includes: interbedded quartzose gravels; proto-quartzitic to orthoquartzitic argillaceous sands; and white, dark gray, and multicolored silts and clays. Included withing this zone are Raritan and Patapsco Formations comprised of gray, brown, and red variegated silts and clays; lenticular, cross-bedded, argillaceous, subrounded sands; minor gravels; thickness. The Patuxent Formation is also interbedded in this zone and comprised of white or light gray to orange-brown, moderately sorted, cross-bedded, argillaceous, angular sands and subrounded quartz gravels; silts and clays subordinate that are predominantly pale gray.
Source: USGS Maryland Geologic Map Data https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=MDKp%3B5
The primary soil types in the collection area are classified as Russett-Christiana-Hambrook Complex and/or Sassafras and Croom Soils; though, others may intersect and overlay in specific areas. The soils in the collecting area are generally described as a complex series of fluviomarine deposits. The soils range from a thin loam layer at the surface to varying levels of loam to sandy loam and/or extremely gravelly sandy clay loam strata, depending upon geographical location (ie. Hillslope summits, slopes, footslopes, swales, etc.).
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2139605 | NA 89040 |
| 250 | NA 89039 | RJL2022IL-001 | Ptelea trifoliata L. | Illinois, United States | NA | | | 2022 | COLLECTED | 09/28/2022 | Site of plant habitat is located at 823 E Co Rd 1220, Hamilton, IL 62341 which is the property where Jacob's Geode Shop and Mine is located. This species is scattered and relatively common throughout the woodlands on this site. | 40.37848400, -91.35390200 | 175 | Plants growing in shade to part-shade of deciduous woodlands above a small creek.
Soils: The underlying geology of this area is of Mississippian origin and comprised of Warsaw Formation and Salem Limestone. Major lithological components include limestone that can be shaly, oolitic, bioclastic, or cherty. Minor lithological components include siltstone that can contain geodes or drusy quartz and can be calcareous.
Source: USGS Illinois Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=ILMws%3B0)
The surface soil profile of this area is Coffeen silt loam, 0 to 2 percent slopes, that are frequently flooded. The Coffeen series consists of very deep, somewhat poorly drained, moderately permeable soils on flood plains, low terraces or benches, toe slopes, and alluvial fans. They formed in silty alluvium. Much of the alluvium is of local origin derived from the nearby loess-covered uplands.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2139604 | NA 89039 |
| 251 | NA 89033 | RJL2022MD-010 | Clethra alnifolia L. | Maryland, United States | NA | | | 2022 | COLLECTED | 09/15/2022 | Plants growing in low woodlands at the end of Greenway Avenue near a boat dock that leads to the Pocomoke River, adjacent to Winter Quarters Golf Course, Pocomoke City. Plants common throughout the wetland area as well as mesic edges of the woodlands. | 38.08305100, -75.56527800 | | Plants growing in the flood plain of the Pocomoke River in shade to part sun of a mixed deciduous and evergreen bottomland habitat about 10 meters from the edge of the golf course fairway. The habitat is a mucky swamp edge habitat next to the Pocomoke River, most of which seems wet year-round and grades slightly upslope to more mesic conditions.
The underlying geology of this area is comprised of Quaternary Deposits of Wisconsin to Holocene origin. The composition is primarily undifferentiated gray to buff sand and gravel, gray to brown lignitic silt and clay, occasional boulders, and rare shell beds. Surficial deposits occur as shell-bearing estuarine clays and silts.
Source: USGS Maryland Geologic Map Data https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=MDQdu%3B5
The surface soil profile of this habitat is classified as Puckum Muck which is frequently flooded. These highly saturated soils are found in flats, depressions and swales. The soil reaction of Puckum Muck is extremely acid to strongly acid throughout the profile. The depth to bedrock is generally greater than 150 cm. Wood fragments comprise 0-25%, by volume of the Puckum Muck throughout the profile which includes mostly twigs, branches, logs, or stumps and are 1.5-30 cm in diameter. The composition of these highly saturated soils, are classified as muck (sapric soil material) or mucky peat (hemic soil material) throughout most of the upper 150 cm and may contain thin layers of mucky silt loam, silty clay loam, sandy loam and/or sand.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2139598 | NA 89033 |
| 252 | NA 89032 | RJL2022MD-009 | Rhododendron viscosum (L.) Torr. | Maryland, United States | NA | | | 2022 | COLLECTED | 09/15/2022 | Plants growing in low woodlands at the end of Greenway Avenue near a boat dock that leads to the Pocomoke River, adjacent to Winter Quarters Golf Course, Pocomoke City. Plants scattered throughout the wetland area. Infrequent, but regularly found. | 38.08235200, -75.56566500 | 1 | Plants growing in the flood plain of the Pocomoke River in part shade to shade of a mixed deciduous and evergreen bottomland habitat about 10 meters from the edge of the golf course fairway. The habitat is a mucky swamp edge habitat next to the Pocomoke River, most of which seems wet year-round.
The underlying geology of this area is comprised of Quaternary Deposits of Wisconsin to Holocene origin. The composition is primarily undifferentiated gray to buff sand and gravel, gray to brown lignitic silt and clay, occasional boulders, and rare shell beds. Surficial deposits occur as shell-bearing estuarine clays and silts.
Source: USGS Maryland Geologic Map Data https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=MDQdu%3B5
The surface soil profile of this habitat is classified as Puckum Muck which is frequently flooded. These highly saturated soils are found in flats, depressions and swales. The soil reaction of Puckum Muck is extremely acid to strongly acid throughout the profile. The depth to bedrock is generally greater than 150 cm. Wood fragments comprise 0-25%, by volume of the Puckum Muck throughout the profile which includes mostly twigs, branches, logs, or stumps and are 1.5-30 cm in diameter. The composition of these highly saturated soils, are classified as muck (sapric soil material) or mucky peat (hemic soil material) throughout most of the upper 150 cm and may contain thin layers of mucky silt loam, silty clay loam, sandy loam and/or sand.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2139597 | NA 89032 |
| 253 | NA 88481 | RJL2022MD-002 | Kalmia latifolia L. | Maryland, United States | NA | | | 2022 | COLLECTED | 09/04/2022 | Plants growing at Elkton State Forest along roads and woodlands over a distance of approximately 5 kilometers labelled as the address of 717 Irishtown Rd, North East, MD 21901. Kalmia is very common along the unnamed gravel road as well as the understory of the upland woodlands. | 39.58852900, -75.90452900 | 60 | Plants are growing in a mesic to dry, well-drained habitat of mixed deciduous and evergreen woodlands comprised primarily of acid-loving plants. Plants are growing in shade to part shade along the unnamed road as well as the woodlands. The soils in the collection area are generally described as a complex series of fluviomarine deposits. The soils range from a thin loam layer at the surface to varying levels of loam to sandy loam and/or extremely gravelly sandy clay loam strata, depending upon geographical location (ie. Hillslope summits, slopes, footslopes, swales, etc.). The primary soil types in the collection area are classified as Russett-Christiana-Hambrook Complex and/or Sassafras and Croom Soils; though, others may intersect and overlay in specific areas. | Wild material | | 2139360 | NA 88481 |
| 254 | NA 88482 | RJL2022MD-003 | Rhododendron periclymenoides (Michx.) Shinners | Maryland, United States | NA | | | 2022 | COLLECTED | 09/04/2022 | Plants growing at Elkton State Forest along roads and woodlands over a distance of approximately 5 kilometers labelled as the address of 717 Irishtown Rd, North East, MD 21901. Plants are found infrequently and scattered along the unnamed gravel road | 39.58852900, -75.90452900 | 51 | Plants are growing in a mesic to dry, well-drained habitat of mixed deciduous and evergreen woodlands comprised primarily of acid-loving plants. Plants are growing in part shade. The soils in the collection area are generally described as a complex series of fluviomarine deposits. The soils range from a thin loam layer at the surface to varying levels of loam to sandy loam and/or extremely gravelly sandy clay loam strata, depending upon geographical location (ie. Hillslope summits, slopes, footslopes, swales, etc.). The primary soil types in the collection area are classified as Russett-Christiana-Hambrook Complex and/or Sassafras and Croom Soils; though, others may intersect and overlay in specific areas. | Wild material | | 2139361 | NA 88482 |
| 255 | NA 88483 | RJL2022MD-004 | Clethra alnifolia L. | Maryland, United States | NA | | | 2022 | COLLECTED | 09/04/2022 | Plants growing at Elkton State Forest along roads and woodlands over a distance of approximately 5 kilometers labelled as the address of 717 Irishtown Rd, North East, MD 21901. Plants are found regularly but scattered along the unnamed gravel road as well as in open understory of the upland woodlands. | 39.58531200, -75.89566100 | 47 | Plants are growing in a mesic to moist, well-drained habitat of mixed deciduous and evergreen woodlands comprised primarily of acid-loving plants. Plants are growing in part shade and open understory shade. The soils in the collection area are generally described as a complex series of fluviomarine deposits. The soils range from a thin loam layer at the surface to varying levels of loam to sandy loam and/or extremely gravelly sandy clay loam strata, depending upon geographical location (ie. Hillslope summits, slopes, footslopes, swales, etc.). The primary soil types in the collection area are classified as Russett-Christiana-Hambrook Complex and/or Sassafras and Croom Soils; though, others may intersect and overlay in specific areas. | Wild material | | 2139362 | NA 88483 |
| 256 | NA 88484 | RJL2022MD-005 | Aronia melanocarpa (Michx.) Elliott | Maryland, United States | NA | | | 2022 | COLLECTED | 09/04/2022 | Plants growing at Elkton State Forest on Elk Neck Trail #3 (Starkey Lane) labelled as the address of 717 Irishtown Rd, North East, MD 21901. This was the only plant observed during several visits to Elk Neck State Forest during early and mid-summer | 39.58531200, -75.89566100 | 55 | Plants are growing in a mesic to dry, well-drained habitat of mixed deciduous and evergreen woodlands comprised primarily of acid-loving plants. Plants are growing in part shade to part-sun. The soils in the collection area are generally described as a complex series of fluviomarine deposits. The soils range from a thin loam layer at the surface to varying levels of loam to sandy loam and/or extremely gravelly sandy clay loam strata, depending upon geographical location (ie. Hillslope summits, slopes, footslopes, swales, etc.). The primary soil types in the collection area are classified as Russett-Christiana-Hambrook Complex and/or Sassafras and Croom Soils; though, others may intersect and overlay in specific areas.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | received as A. prunifolia, on further examination by collector it was determined to be A. melanocarpa | 2139363 | NA 88484 |
| 257 | NA 88488 | RJL2022PA-004 | Viburnum acerifolium L. | Pennsylvania, United States | NA | | | 2022 | COLLECTED | 09/03/2022 | Plants growing in woodlands on the east side of Shed Road in French Creek State Park. Plants are common and found scattered along the edges of the road and into the woodlands. | 40.21969200, -75.77373600 | 238 | Plants are growing in a mesic to dry, well-drained habitat of upland deciduous forest which is very rocky. The understory layer is generally not as rich due to the rock-laden ground layer. Plants are growing in part shade to shade. The underlying geology of this area is comprised of Hammer Creek Conglomerate, characterized by cobble and pebble quartz conglomerate interbedded with red sandstone.
Source: USGS Pennsylvania Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=PATRhc%3B2) The surface soil profile of this area is Joanna Loam (JpD), 8 to 25 percent slopes which is extremely stony. It is represented by residuum weathered from sandstone and/or residuum weathered from conglomerate. Joanna Loam is moderately to well-drained and 1.8 meters to 2.5 meters to the lithic bedrock described above.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2139367 | NA 88488 |
| 258 | NA 88489 | RJL2022PA-005 | Kalmia latifolia L. | Pennsylvania, United States | NA | | | 2022 | COLLECTED | 09/10/2022 | Plants are growing on the lands of Hawk Mountain Sanctuary. This species is very common and abundant. It is one of the most dominant understory plants in woodlands. This species is a common understory shrub throughout the entire region in upland dry woodland habitats. | 40.63862000, -75.99071200 | 430 | Plants are growing primarily in shade to part-shade on a dry-mesic to very dry, well-drained upland/montane habitat characterized by upland mixed deciduous and evergreen forest that is very rocky. All of the plants found in this habitat go through periods of drought during the growing season due to the limited litter/soil layer in which moisture can be held. The underlying geology of this area is of Silurian origin and comprised of Shawangunk Formation. This formation is primarily light- to dark-gray, fine- to very coarse-grained sandstone and conglomerate containing thin shale interbeds.
Source: USGS Pennsylvania Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=PASs%3B14)
The surface soil profile of this area is the Hazleton series consists of deep and very deep, well drained soils formed in residuum of acid gray, brown or red sandstone on uplands. The matrix includes a considerable accumulation of thin, flat, coarse fragments of sandstone, limestone, or schist with diameters up to 15 cm. Slope ranges from 0-80%. Permeability is moderately rapid to rapid.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2139368 | NA 88489 |
| 259 | NA 88490 | RJL2022PA-006 | Ilex montana Torr. & A. Gray | Pennsylvania, United States | NA | | | 2022 | COLLECTED | 09/10/2022 | Hawk Mountain Sanctuary. | 40.64162200, -75.99122600 | 420 | Plants are growing from shade to full sun on a dry-mesic to very dry, well-drained upland/montane habitat characterized by an upland mixed deciduous and evergreen forest that is very rocky. All of the plants found in this habitat go through periods of drought during the growing season due to the limited litter/soil layer in which moisture can be held. The underlying geology of this area is of Silurian origin and comprised of Shawangunk Formation. This formation is primarily light- to dark-gray, fine- to very coarse-grained sandstone and conglomerate containing thin shale interbeds. (Source: USGS Pennsylvania Geologic Map Data). The surface soil profile of this area is the Hazleton series consists of deep and very deep, well drained soils formed in residuum of acid gray, brown or red sandstone on uplands. The matrix includes a considerable accumulation of thin, flat, coarse fragments of sandstone, limestone, or schist with diameters up to 15 cm. Slope ranges from 0-80%. Permeability is moderately rapid to rapid. (Source: NRCS Web Soil Survey). | Wild material | | 2139369 | NA 88490 |
| 260 | NA 88491 | RJL2022PA-007 | Rhododendron maximum L. | Pennsylvania, United States | NA | | | 2022 | COLLECTED | 09/10/2022 | Plants are growing on the lands of Hawk Mountain Sanctuary. This species was common, but generally restricted to steep rocky outcrops. | 40.63813900, -75.98835200 | 420 | Plants are growing from shade to full sun on a dry-mesic to very dry, well-drained upland/montane habitat characterized by an upland mixed deciduous and evergreen forest that is very rocky. Even so, most heavily fruited plants were growing in part shade to almost full sun. All of the plants found in this habitat go through periods of drought during the growing season due to the limited litter/soil layer in which moisture can be held. The underlying geology of this area is of Silurian origin and comprised of Shawangunk Formation. This formation is primarily light- to dark-gray, fine- to very coarse-grained sandstone and conglomerate containing thin shale interbeds.
Source: USGS Pennsylvania Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=PASs%3B14)
The surface soil profile of this area is the Hazleton series consists of deep and very deep, well drained soils formed in residuum of acid gray, brown or red sandstone on uplands. The matrix includes a considerable accumulation of thin, flat, coarse fragments of sandstone, limestone, or schist with diameters up to 15 cm. Slope ranges from 0-80%. Permeability is moderately rapid to rapid.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2139370 | NA 88491 |
| 261 | NA 88495 | RJL2022PA-011 | Sorbus americana Marshall | Pennsylvania, United States | NA | | | 2022 | COLLECTED | 09/10/2022 | Plants are growing on the lands of Hawk Mountain Sanctuary. This plant is frequent but scattered on the exposed north, northeast, and east-facing steep slopes and ridge areas. | 40.63793500, -75.98778000 | 430 | part sun to full sun on a dry-mesic to very dry, well-drained upland/montane habitat characterized by an upland mixed deciduous and evergreen forest that is very rocky. All of the plants found in this habitat go through periods of drought during the growing season due to the limited litter/soil layer in which moisture can be held.
The underlying geology of this area is of Silurian origin and comprised of Shawangunk Formation. This formation is primarily light- to dark-gray, fine- to very coarse-grained sandstone and conglomerate containing thin shale interbeds.
Source: USGS Pennsylvania Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=PASs%3B14)
The surface soil profile of this area is the Hazleton series consists of deep and very deep, well drained soils formed in residuum of acid gray, brown or red sandstone on uplands. The matrix includes a considerable accumulation of thin, flat, coarse fragments of sandstone, limestone, or schist with diameters up to 15 cm. Slope ranges from 0-80%. Permeability is moderately rapid to rapid.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2139374 | NA 88495 |
| 262 | WLP 2610 | 2022VA-01 | Stewartia malacodendron L. | Virginia, United States | NA | | | 2022 | COLLECTED | 09/12/2022 | Woodlands adjacent to and bounded by the interchange of Business Route 168 (N. Battlefield Avenue) and Route 168, next to a detention basin and shopping plaza on the west side of Battlefield Avenue. Accessed by parking in the cul-de-sac at the south end of Kingsborough Square Street. This plant is a very common and abundant component of this woodland with significant recruitment continuing | 36.73888200, -76.24327700 | 9 | Plants growing in rich mesic, moist but well-drained conditions in the high understory shade of a mixed deciduous and evergreen woodland, primarily comprised of deciduous trees in the over-story and a mixture of deciduous and evergreen species in the sub-canopy.
Soils: The underlying geology of this area is the Tabb Formation of Quaternary origin which is comprised of undifferentiated sand, silt, and peat and subdivided into three members. Within the Tabb Formation lies the Sedgefield Member, a pebbly to bouldery, clayey sand and fine to medium, shell-rich sand that grades upward into sandy and clayey silt; locally, channel fill at the base of unit includes as much as 15 meters of fine to coarse, cross-bedded sand and clayey silt and peat containing in-situ tree stumps. Sandy bay facies commonly contain numerous mollusks as well as coral. Thickness is 0 to 15.8 meters.
Source: USGS Virginia Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=VAQts%3B0)
The surface soil profile of this area is Tetotum fine sandy loam, 0 to 2 percent slopes. Forming primarily terraces, these soils are moderately well-drained and highly acidic. They are generally 100-150 cm thick, the upper 20 inches of the horizon averages more than 30 percent silt or more than 40 percent silt plus very fine sand.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2139348 | WLP 2610 |
| 263 | WLP 2612 | 2022VA-03 | Styrax grandifolius Aiton | Virginia, United States | NA | | | 2022 | COLLECTED | 09/12/2022 | Northwest River Park on the south side of Indian Springs Road behind the Equestrian Center along a bridle trail. This plant is a common in the mesic woodlands at this location. | 36.58361100, -76.16277800 | 21 | Plants growing in shade to part-shade of the mixed deciduous and evergreen mesic woodland about 1 to 2 meters above a nearby wetland area.
The underlying geology of this area is the Tabb Formation of Quaternary origin which is comprised of undifferentiated sand, silt, and peat and subdivided into three members. Within the Tabb Formation lies the Lynnhaven Member with pebbly and cobbly, fine to coarse gray sand grades upward into clayey and silty fine sand and sandy silt. Extensive low lands bounded on the landward side by river-, bay-, and ocean-facing scarps having toe altitudes of 5-6 meters. Thickness is 0 to 6.5 meters.
Source: USGS Virginia Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=VAQtl%3B0)
The surface soil profile of this area is Chapanoke-Yeopim complex, 0 to 3 percent slopes. These soil as somewhat poorly to moderately drained, acidic, and found on marine terraces and summits of low elevation coastal plain areas. They are comprised of silt loam, silty clay loam, sandy clay loam and loam in varying quantities across the profile; the depth to parent geology is approximately 200 cm.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx | Wild material | | 2139350 | WLP 2612 |
| 264 | WLP 2614 | 2022VA-05 | Euonymus americanus L. | Virginia, United States | NA | | | 2022 | COLLECTED | 09/12/2022 | In Colonial Williamsburg, park in the Providence Hall Directors Wing parking lot and enter the Bassett Trace Nature Trail; this species is found in the woodlands on either side of the trail and over a bridge until the it turns right. This plant is infrequent, but occasionally found in the mesic woodlands throughout this location. | 37.26681600, -76.69252800 | 21 | Plants growing in shade to part-shade of the mixed deciduous and evergreen mesic woodland. This species is generally growing in areas with an abundant organic, mature woodland that is relatively undisturbed.
The underlying geology of this area is Windsor Formation of Tertiary-Quaternary origin (lower Pleistocene or upper Pliocene). It is comprised of gray and yellowish- to reddish-brown sand, gravel, silt, and clay. It constitutes surficial deposits of extensive plain and fluvial-estuarine terraces above elevations of 10 meters. The thickness of the Windsor Formation is 0 to 12.5 meters.
Source: USGS Virginia Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=VAQTw%3B0)
The surface soil profile of this area is Emporia Complex, 15 to 25 percent slopes. This soil as moderately well-drained, acidic, and found on sloping and elevated terraces. They are comprised of fine sandy loam, loam, and sandy clay loam in varying quantities across the profile; the depth to parent geology is approximately 200 cm.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2139352 | WLP 2614 |
| 265 | WLP 2599 | RJL2022FLAL-028 | Viburnum nitidum Aiton | Florida, United States | NA | | | 2022 | COLLECTED | 08/07/2022 | Eglin AFB, in woodlands along Weaver Creek accessed from unnamed dirt road, 0.82 kilometers west of junction with Eglin AFB 720; approximately 0.73 kilometers north of junction with Choctaw Nolf Airfield Road and Eglin AFB 720. | 30.51753300, -86.91490000 | 13 | Plants are found growing in part shade to nearly full sun of a mixed deciduous and broadleaved evergreen woodland along Weaver Creek where there is a wider stream edge with low to flat slopes above the normal creek flow. The underlying geology of this area is the Citronelle Formation, of Pliocene origin, and consists of gray to orange, often mottled, unconsolidated to poorly consolidated, very fine to very coarse, poorly sorted, clean to clayey sands. It contains significant amounts of clay, silt and gravel which may occur as beds and lenses and may vary considerably over short distances. Limonite nodules and limonite-cemented beds are common. | Wild material | | 2138709 | WLP 2599 |
| 266 | WLP 2600 | RJL2022FLAL-029 | Stewartia malacodendron L. | Florida, United States | NA | | | 2022 | COLLECTED | 08/07/2022 | Eglin AFB, in woodlands along Weaver Creek accessed from unnamed dirt road, 0.82 kilometers west of junction with Eglin AFB 720; approximately 0.73 kilometers north of junction with Choctaw Nolf Airfield Road and Eglin AFB 720. | 30.51680000, -86.91469400 | 15 | Growing in moist, well-drained sandy soils above Weaver Creek in mixed broadleaved evergreen and deciduous woodland habitat in part shade to shade of west facing slopes several meters above the wetland zone. The Stewartia is growing in a high competition habitat. The underlying geology of this area is the Citronelle Formation, of Pliocene origin, and consists of gray to orange, often mottled, unconsolidated to poorly consolidated, very fine to very coarse, poorly sorted, clean to clayey sands. It contains significant amounts of clay, silt and gravel which may occur as beds and lenses and may vary considerably over short distances. Limonite nodules and limonite-cemented beds are common. | Wild material | | 2138710 | WLP 2600 |
| 267 | Ames 35906 | Turkey Mounds State Preserve | Heuchera richardsonii R. Br. | Iowa, United States | NC7 | | | 2022 | COLLECTED | 07/30/2022 | Turkey River Mounds State Preserve located 5.50 miles south, southeast of Guttenberg, T91N R2W SE ¼ NE ¼ Sec. 11. | 42.71399000, -91.03844000 | 228 | Narrow ridge with precipitous bluffs rising 250 feet above the Mississippi River floodplain | Wild material | | 2139635 | Ames 35906 |
| 268 | Ames 36026 | RJL2022FLAL-007 | Fraxinus caroliniana Mill. | Florida, United States | NC7 |  | | 2022 | COLLECTED | 07/28/2022 | Growing along the Yellow River and reached by boat. | 30.58025000, -86.91052800 | 1 | Trees are typically found growing in full sun in permanently saturated to submersed conditions along the edge of the Yellow River, growing in association with a wide array of deciduous and evergreen trees, shrubs and perennial plant species. This species requires acidic conditions. While the aquatic habitats are generally fresh water, there is occasionally tidal or hurricane-caused saltwater intrusions. The underlying geology of this area is classified as Alluvium, of Pleistocene/Holocene origin and consists of undifferentiated Quaternary sediments of varying thickness including siliciclastics, organics and freshwater carbonates. The siliciclastics are light gray, tan, brown to black, unconsolidated to poorly consolidated, clean to clayey, silty, unfossiliferous, variably organic-bearing sands to blue green to olive green, poorly to moderately consolidated, sandy, silty clays. Organics occur as plant debris, roots, disseminated organic matrix and beds of peat. Freshwater carbonates, often referred to as marls in the literature, are scattered. | Wild material | | 2138696 | Ames 36026 |
| 269 | NA 87204 | RJL2022FLAL-019 | Ilex coriacea (Pursh) Chapm. | Florida, United States | NA | | | 2022 | COLLECTED | 08/02/2022 | Corner of San Jose Street and South 28th Avenue just east of Avalon Beach, FL. | 30.53172700, -87.09058900 | 3 | Growing in full sun to part shade in moist to wet areas, often with sphagnum moss along the edges, just above the water in ditches and waterways. Population is so dense that plants are crowding out other species. The underlying geology of this area is classified as Alluvium, of Pleistocene/Holocene origin and consists of undifferentiated Quaternary sediments of varying thickness including siliciclastics, organics and freshwater carbonates. The siliciclastics are light gray, tan, brown to black, unconsolidated to poorly consolidated, clean to clayey, silty, unfossiliferous, variably organic-bearing sands to blue green to olive green, poorly to moderately consolidated, sandy, silty clays. Organics occur as plant debris, roots, disseminated organic matrix and beds of peat. Freshwater carbonates, often referred to as marls in the literature, are scattered. | Wild material | | 2138707 | NA 87204 |
| 270 | WLP 2584 | RJL2022FLAL-005 | Styrax americanus Lam. | Florida, United States | NA | | | 2022 | COLLECTED | 07/28/2022 | Growing along the Yellow River and reached by boat. | 30.57944000, -86.91689800 | 1 | Plants are typically found growing in shade to full sun in permanently saturated to submersed conditions along the edge of the Yellow River, growing in association with a wide array of deciduous and evergreen trees, shrubs and perennial plant species. Most of the plants along the river are adapted to acidic conditions and while the aquatic habitats are generally fresh water, there is occasionally tidal or hurricane-caused saltwater intrusions. The underlying geology of this area is classified as Alluvium, of Pleistocene/Holocene origin and consists of undifferentiated Quaternary sediments of varying thickness including siliciclastics, organics and freshwater carbonates. The siliciclastics are light gray, tan, brown to black, unconsolidated to poorly consolidated, clean to clayey, silty, unfossiliferous, variably organic-bearing sands to blue green to olive green, poorly to moderately consolidated, sandy, silty clays. Organics occur as plant debris, roots, disseminated organic matrix and beds of peat. Freshwater carbonates, often referred to as marls in the literature, are scattered. | Wild material | | 2138694 | WLP 2584 |
| 271 | WLP 2585 | RJL2022FLAL-006 | Nyssa biflora Walter | Florida, United States | NA | | | 2022 | COLLECTED | 07/28/2022 | Growing along the Yellow River and reached by boat. | 30.58013800, -86.91556800 | 1 | Trees are typically found growing in full sun in permanently saturated to submersed conditions along the edge of the Yellow River, growing in association with a wide array of deciduous and evergreen trees, shrubs and perennial plant species. This species requires acidic conditions. While the aquatic habitats are generally fresh water, there is occasionally tidal or hurricane-caused saltwater intrusions. The underlying geology of this area is classified as Alluvium, of Pleistocene/Holocene origin and consists of undifferentiated Quaternary sediments of varying thickness including siliciclastics, organics and freshwater carbonates. The siliciclastics are light gray, tan, brown to black, unconsolidated to poorly consolidated, clean to clayey, silty, unfossiliferous, variably organic-bearing sands to blue green to olive green, poorly to moderately consolidated, sandy, silty clays. Organics occur as plant debris, roots, disseminated organic matrix and beds of peat. Freshwater carbonates, often referred to as marls in the literature, are scattered. | Wild material | | 2138695 | WLP 2585 |
| 272 | WLP 2596 | RJL2022FLAL-018 | Viburnum nitidum Aiton | Florida, United States | NA | | | 2022 | COLLECTED | 08/02/2022 | Along Gin/Camp Road at the bridge over Thomas Creek on the east side of the road. | 30.75027700, -87.23473700 | 21 | Growing in part shade on the sandy bench about a meter above the creek in mixed evergreen and deciduous riparian habitat. Plants have ample access to moisture, but are not obligate wetland plants. Fruiting is occurring where increased sunlight is available; however, most plants appear to be middle understory in this habitat. The underlying geology of this area is the Citronelle Formation, of Pliocene origin, and consists of gray to orange, often mottled, unconsolidated to poorly consolidated, very fine to very coarse, poorly sorted, clean to clayey sands. It contains significant amounts of clay, silt and gravel which may occur as beds and lenses and may vary considerably over short distances. Limonite nodules and limonite-cemented beds are common. | Wild material | | 2138706 | WLP 2596 |
| 273 | Ames 35945 | AS/ML/2022/012/143 | Monarda lindheimeri Engelm. & A. Gray | Texas, United States | NC7 |  | | 2022 | COLLECTED | 08/06/2022 | Located approximately 6.5 miles north of Columbus along FM 109 just north of Redgate Creek and also area 1.75 miles to the west along Brune Lane. | 29.80034600, -96.53240000 | 73 | Woodland edges and fencelines. | Wild material | | 2140535 | Ames 35945 |
| 274 | Ames 35948 | AS/ML/2022/017/147 | Monarda lindheimeri Engelm. & A. Gray | Texas, United States | NC7 |  | | 2022 | COLLECTED | 08/06/2022 | Located near Grimes County line along highway 6 approximately 6.5 miles north of Hempstead. | 30.22891300, -96.05532600 | 68 | Woodland edge. | Wild material | Plants in nature measuring up to approximately 3.0-3.5' in height with very long internodes. Extreme variation noted on stem color from green, to purple to green with purple edges. | 2140538 | Ames 35948 |
| 275 | Ames 35951 | AS/ML/2022/020/151 | Monarda lindheimeri Engelm. & A. Gray | Texas, United States | NC7 |  | | 2022 | COLLECTED | 08/07/2022 | Located northwest of Navasota approximately 5.60 miles along Old Highway 6. | 30.44628200, -96.15333200 | 67 | Powerline cut. | Wild material | Accession consisting of both white flowering specimens and multi-colored (pinkish) flowering specimens. Inventory 01 represented as rather robust plants up to 40" tall that display a rather to somewhat clump type growth habit (possibly due to growing in more of a prairie habitat/full sun), but also includes adjacent specimens that are rhizomatous. Inventory 02 represents a more rhizomatous growth habit and shorter in height (e.g. less than 20" tall). Plants sampled ranging from 1.0-4.5' in height. | 2140541 | Ames 35951 |
| 276 | Ames 35954 | AS/ML/2022/023/154 | Monarda lindheimeri Engelm. & A. Gray | Texas, United States | NC7 |  | | 2022 | COLLECTED | 08/07/2022 | Located just southwest of College Station on both Los Robles Dr and White Creek Rd. | 30.57630900, -96.38686600 | 91 | Roadside, woodland edge and savannah. | Wild material | Very rhizamatous specimens noted in nature. In comparison to other M. lindheimeri noted in Texas in 2022, this population is one of the earliest flowering populations, nearly 2-3 weeks earlier typically peaking in mid-April. In 2022, population peaked flower on 18 April. | 2140544 | Ames 35954 |
| 277 | Ames 35957 | AS/ML/2022/026/157 | Monarda luteola Singhurst & W. C. Holmes | Texas, United States | NC7 |  | | 2022 | COLLECTED | 08/05/2022 | Located north of Palestine approximately 3.60 miles on AN Country Road 404 (west side) just 0.7 miles north from intersection with AN Country Road 403 | 31.81051200, -95.63928400 | 185 | Roadside, woodland edge. | Wild material | Lemon-scented foliage when crushed. Population in nature noted slightly prior to peak flowering on 28 April (2022) at collection site. | 2140547 | Ames 35957 |
| 278 | WLP 2704 | AS/CV/2022/028/159 | Chionanthus virginicus L. | Arkansas, United States | NA |  | | 2022 | COLLECTED | 08/08/2022 | Just south and southwest of Potter Junction by approximately 1.1 miles; along Highway 59 and Highway 78 | 34.53717900, -94.31379200 | 336 | Roadside, moist woods. | Wild material | Specimens in nature peaked flower on 29 April (2022). | 2140549 | WLP 2704 |
| 279 | Ames 35887 | JDC/MR/2022/034/1014 | Morus rubra L. | Iowa, United States | NC7 |  | | 2022 | COLLECTED | 07/12/2022 | Waubonsie State Park located north, northwest of Hamburg, T68N R42W Sec. 29 and Sec. 32. | 40.67552500, -95.68690400 | 355 | Mid slope (ranging from 10-30 degrees) to base of slopes and along all drainages and valleys of deciduous woods. | Wild material | The native range for Red Mulberry is reported from the eastern margin of the Great Plains, extending north to southern Ontario, Canada, and distributed as far south as southern Florida (Little, 1971). Conservation assessments in North America indicate current (2026) and future concern for the species including Michigan (threatened); Massachusetts (endangered); Ontario Canada (endangered); with NatureServe's 2025 global G5 rank due to genetic swamping and habitat pressure. Red Mulberry seems to be extremely localized to moist, floodplain areas that are high-quality bottomland forests. This accession represents genetics collected from the northwestern edge of the species native range. Specimens sampled in nature displayed the following morphological characters: acuminate leaf tips, impressed veins, pubescent upper and lower leaves, flaky bark (often with tiny pin holes (insect emergence holes)), cordate leaf base, and umbrella-shaped growth habit. M. rubra specimens noted ranged in size from 1"-23" inches DBH with some of the tallest specimens reaching 70' in height. The largest specimen sampled (#172-13) measuring 23.25" DBH. Estimated hundreds, perhaps a thousand specimens of M. rubra noted within the park with very little representation of hybrids or Morus alba. Representation of M. rubra outside of park boundaries is near completely absent and the presence of hybrids and M. alba is extremely evident. Soluble solids content from fruits collected in the wild ranged from 19.0-32.9 degrees Brix. This range of Brix values is likely a result of genetic diversity and also variation in maturity of fruits. Fruits selected for Brix measurements were black in color. The specimen sampled with the highest Brix value was #172-9. All M. rubra specimens noted at time of sampling (12 July 2022) were exhibiting determinate growth compared to local hybrids and M. alba, which were still actively growing with newly emerging leaves. The first study (Adhikari et al. 2026) on the mitogenome of M. rubra utilized sample #172-13 (Ames 35887 Tree #13) reporting 359,221 base pairs (bp) long with 45.8% GC content, comprising 57 genes: 32 protein-coding, 21 transfer, and four ribosomal RNAs. | 2138220 | Ames 35887 |
| 280 | WLP 2576 | RJL2022-001 | Amelanchier arborea (F. Michx.) Fernald | Maryland, United States | NA | | | 2022 | COLLECTED | 05/25/2022 | Plants growing in open woodlands and part shade along unnamed Elkton State Forest gravel road over a distance of approximately 5 kilometers labelled as the address of 717 Irishtown Rd, North East, MD 21901. | 39.58089500, -75.91505900 | 73 | Plants are found regularly but scattered along the unnamed gravel road as well as in open understory of the upland woodlands. Plants growing in a mesic to dry, well-drained habitat of mixed deciduous and evergreen woodlands comprised primarily of acid-loving plants. Plants are growing in part shade and open understory shade. The soils in the collection area are generally described as a complex series of fluviomarine deposits. The soils range from a thin loam layer at the surface to varying levels of loam to sandy loam and/or extremely gravelly sandy clay loam strata, depending upon geographical location (ie. Hillslope summits, slopes, footslopes, swales, etc.). The primary soil types in the collection area are classified as Russett-Christiana-Hambrook Complex and/or Sassafras and Croom Soils; though, others may intersect and overlay in specific areas. | Wild material | | 2138095 | WLP 2576 |
| 281 | Ames 35804 | Kuehn Prairie | Salix humilis Marshall var. tristis (Aiton) Griggs | Iowa, United States | NC7 |  | | 2022 | COLLECTED | 05/12/2022 | Kuehn Conservation Area located 4.90 miles north of Earlham on east side of Houston Trail Road, T78N R29W SE ¼ SE ¼ Sec. 12. | 41.56328500, -94.12929100 | 313 | Xeric prairie remnant. Hilltop/knoll. | Wild material | Plants in nature measuring approximately 2.0-2.5' in height. Specimens noted during peak flowering and seed dispersal on 9 April and 1 May (2021), respectively. Normally for central Iowa peak flowering and fruiting occurs in late April and mid-May, respectively. | 2137910 | Ames 35804 |
| 282 | Ames 35792 | APS/ID/2022/027/489 | Ilex decidua Walter | Arkansas, United States | NC7 |  | | 2022 | COLLECTED | 03/15/2022 | Located approximately 3.75 miles east of Allison just off Round Bottom Road. | 35.93670000, -92.04891000 | 133 | Dry west facing slope in a pine, oak, and hickory forest. | Wild material | Plants sampled in nature with bright red fruits measuring 7-9 mm in diameter. | 2137431 | Ames 35792 |
| 283 | OPGC 5799 | 284806 | Brickellia dentata (DC.) Sch. Bip. | Texas, United States | OPGC |  | | 2021 | | | | | | | Wild material | | 1895216 | OPGC 5799 |
| 284 | OPGC 5807 | 283315 | Echinocereus enneacanthus Engelm. | West Virginia, United States | OPGC |  | Contact Site | 2021 | | | | | | | Wild material | | 1895253 | OPGC 5807 |
| 285 | OPGC 5808 | 284839 | Echinocereus reichenbachii (Terscheck ex Walp.) hort. ex Haage | Texas, United States | OPGC |  | Contact Site | 2021 | | | | | | | Wild material | | 1895254 | OPGC 5808 |
| 286 | OPGC 5810 | 283876 | Heterotheca canescens (DC.) Shinners | Texas, United States | OPGC |  | | 2021 | | | | | | | Wild material | | 1895291 | OPGC 5810 |
| 287 | OPGC 5820 | 231202 | Sedum nuttallii Torr. & E. James ex Eaton | Texas, United States | OPGC |  | | 2021 | | | | | | | Wild material | | 1895406 | OPGC 5820 |
| 288 | OPGC 8497 | NCBG-374 | Asclepias syriaca L. | Virginia, United States | OPGC | | | 2021 | | | | | | | Wild material | | 2132872 | OPGC 8497 |
| 289 | W6 59998 | NCBG-395 | Eupatorium hyssopifolium L. | Maryland, United States | W6 | | | 2021 | | | | | | | Wild material | | 2132880 | W6 59998 |
| 290 | W6 60006 | NCBG-504 | Cyperus grayi Torr. | North Carolina, United States | W6 | | | 2021 | | | | | | | Wild material | | 2132888 | W6 60006 |
| 291 | W6 60083 | MARSB-267 | Elymus virginicus L. | New York, United States | W6 | | | 2021 | | | | | | | Wild material | | 2137168 | W6 60083 |
| 292 | WLP 1731 | RJL2021PA-001 | Viburnum acerifolium L. | Pennsylvania, United States | NA | | | 2021 | COLLECTED | 11/05/2021 | Plants growing in woodlands above a small unnamed creek that dumps into the Middle Branch White Clay Creek in Goddard Park, West Grove Pennsylvania, off of Wickerton Road, Chester County. | 39.80462083, -75.82888750 | 103 | Plants growing in a mesic, well-drained habitat of deciduous woodlands, for the most part, above the riparian zone that drains toward a small unnamed creek that feeds into the Middle Branch White Clay Creek. Plants are growing in high understory shade with very little direct sun during most of the day. The remnant woodlands exist mostly along the steep slopes, wetlands and seeps of seasonal and year-round creeks flowing into the Middle Branch White Clay Creek. The woodlands are bordered by numerous housing developments and land converted to meadows; hence there is significant first order edge that is heavily impacted by invasive plant intrusion. Soils: Soils are classified as Glenelg silt loam, 8 to 15% slopes (GgC); this series consists of very deep, well drained soils formed in residuum weathered from micaceous schist on uplands of the Blue Ridge and the Northern Piedmont. Saturated hydraulic conductivity is moderately high in the subsoil and moderately high to high in the substratum. This upper horizon of this soil is undifferentiated, mostly poorly drained sandy bottomland soils intermingled with decomposing organic litter and eroded silts and clays due to erosion. Slope: 8 to 15% Aspect: West. | Wild material | | 2123080 | WLP 1731 |
| 293 | W6 59898 | CP3-70 | Chaenactis douglasii (Hook.) Hook. & Arn. | Utah, United States | W6 |  | | 2021 | | | | | | | Wild material | Cream colored flowers with many inflorescences. Red stem. | 2132477 | W6 59898 |
| 294 | W6 59930 | CBG-10653 | Carex gracillima Schwein. | Illinois, United States | W6 | | | 2021 | | | | | | | Wild material | | 2132509 | W6 59930 |
| 295 | W6 59961 | CBG-10690 | Dasiphora fruticosa (L.) Rydb. | Illinois, United States | W6 | | | 2021 | | | | | | | Wild material | | 2132539 | W6 59961 |
| 296 | Ames 35752 | #476-477 | Rhus glabra L. | Iowa, United States | NC7 |  | | 2021 | COLLECTED | 09/29/2021 | Upper Iowa River area near Bluffton, T99N R9W NE1/4 Sec. 9 and S1/2 Sec. 10 | 43.40275000, -91.90494000 | 299 | High bluffs, roadside and stream banks | Wild material | Plants sampled in nature (29 September 2021) during peak fall color displaying bright reds to maroonish colors while measuring approximately 12-15 feet in height. One clonal patch noted was estimated to have 1,000+ ramets. | 2122093 | Ames 35752 |
| 297 | OPGC 7574 | Ledges State Park | Solidago ulmifolia Muhl. ex Willd. | Iowa, United States | OPGC |  | | 2021 | COLLECTED | 09/15/2021 | Ledges State Park, approximately 4.5 miles south of Boone, T83N R26W Sec. 20 | 41.98266200, -93.89314800 | 287 | Understory of hardwood forest. | Wild material | Plants in nature were generally two to three feet in height, growing in sparsely spreading colonies. This population has a large amount of diversity for flowering time with the first plants in the population beginning to flower on 22 July 2021 and the last plants to flower were still blooming at the end of September. Some plants in the population had a muted red fall foliage color at the end of October 2021. This accession represents genetics from near the northwest edge of the species range of occurence. | 2132828 | OPGC 7574 |
| 298 | OPGC 7575 | Ledges State Park | Solidago flexicaulis L. | Iowa, United States | OPGC |  | | 2021 | COLLECTED | 10/03/2021 | Ledges State Park, approximately 4.5 miles south of Boone, T83N R26W Sec. 21 | 41.98338100, -93.89052800 | 288 | Understory of hardwood forest. | Wild material | Plants in nature ranged in height from approximately one to three feet, growing in sparsely spreading colonies. Peak bloom in 2021 occurred near 15 September. Several specimens had branched inflorescences. | 2132829 | OPGC 7575 |
| 299 | Ames 35750 | Ames 35750 | Blephilia ciliata (L.) Benth. | Iowa, United States | NC7 |  | | 2021 | COLLECTED | 09/27/2021 | Located approximately 3 miles south, southeast of Fairfield, T71N R9W SW1/4 Sec. 7 | 40.96338000, -91.94686900 | 223 | Woodland openings/edges, disturbed areas | Wild material | | 2122068 | Ames 35750 |
| 300 | NA 86933 | PCCKY16-024 | Viburnum deamii (Rehder) Bush | Ohio, United States | NA | | | 2021 | COLLECTED | 09/07/2019 | Lynx Township: Edge of Appalachia Preserve System: The E. Lucy Braun Lynx Prairie Preserve. | 38.76479000, -83.40996000 | 266 | Oak-hickory woodland over Devonian shale (Ohio shale). Slope: 0 degrees. Aspect: Northwest. | Wild material | Full name as recorded at U.S. National Arboretum: Viburnum dentatum var. deamii. See NA 86224 for original wild-collected seed received from the Arnold Arboretum in 2019. | 2155046 | NA 86933 |
| 301 | Ames 35746 | Guye Woods | Acer saccharum Marshall subsp. nigrum (F. Michx.) Desmarais | Iowa, United States | NC7 |  | | 2021 | COLLECTED | 09/08/2021 | Guye Woods County Park located 6.0 miles northeast of Winterset, T76N R27W NE1/4 Sec. 4 | 41.41235000, -93.96373000 | 278 | Moist deciduous maple, oak, hickory forest, northwest facing slope above the North River. | Wild material | Multiple specimens in this population were observed to be 24" diameter at breast height (DBH) or larger with the largest specimen encountered at the time of collection measuring 36.5" DBH.
Morphological traits of leaves suggests sampled specimens are true to type of Acer saccharum subsp. nigrum including leaves with three distinct points, leathery/thick, and drooping in appearance. On September 25, 2020 (Schmitz, A., personal communication, 31 January 2022), peak fall color on Acer saccharum subsp. nigrum at Guye Woods was observed with specimens having a clean yellow fall color, also indicative of Acer saccharum subsp. nigrum.
| 2122010 | Ames 35746 |
| 302 | Ames 35738 | AS/PT/2021/016/116 | Ptelea trifoliata L. | Illinois, United States | NC7 |  | | 2021 | COLLECTED | 08/26/2021 | State Route 71 along Illinois River located approximately 1.30 miles southwest of Ottawa, T33N R3E NE1/4 Sec. 15 | 41.33370200, -88.86061200 | 148 | Roadside at top of limestone cliff above Illinois River. | Wild material | Trees measuring approximately 20-25' in height. Peak flowering and fruiting occurred 4 May and approximately 10 September 2021, respectively. | 2120342 | Ames 35738 |
| 303 | WLP 2484 | AS/TO/2021/017/117 | Thuja occidentalis L. | Illinois, United States | NA |  | | 2021 | COLLECTED | 08/26/2021 | State Route 71 along Illinois River located approximately 1.30 miles southwest of Ottawa, T33N R3E SW1/4 NE1/4 Sec. 15 | 41.33211800, -88.86347300 | 146 | Roadside at top of limestone cliff above Illinois River. | Wild material | Thuja occidentalis is a medium sized, evergreen tree that is native throughout northeastern North America stretching from Minnesota to Maine with scattered distributions in the Appalachian Mountains. In Illinois, Northern White Cedar was formerly listed as a state-threatened species, but delisted in 2004 (Mankowski 2012) and is localized to bluffs and cliffs of St. Peter sandstone and rocky outcroppings. Elsewhere, the species is abundant in sphagnum peat swamps, lake shorelines, and moist woods. This accession was collected on the southwest edge of the species native range and is one of the southern-most, known native localities in Illinois and thus may contain genetics for heat and drought tolerance. Genetics for this accessions were collected from two areas separated by approximately 6.50 miles. | 2120343 | WLP 2484 |
| 304 | Ames 35734 | Ledges State Park | Teucrium canadense L. | Iowa, United States | NC7 |  | | 2021 | COLLECTED | 08/23/2021 | Ledges State Park located approximately 4.75 miles south of Boone T83N R26W Sec. 16 & 21 | 41.99262400, -93.87724800 | 330 | Edges of woods | Wild material | | 2120338 | Ames 35734 |
| 305 | OPGC 8344 | CBG-10576 | Gillenia stipulata (Muhl. ex Willd.) Nutt. | Illinois, United States | OPGC | | | 2021 | | | | | | | Wild material | plant numbers sampled estimated. | 2120167 | OPGC 8344 |
| 306 | W6 59171 | CBG-10456 | Carex annectens (E. P. Bicknell) E. P. Bicknell | Illinois, United States | W6 | | | 2021 | | | | | | | Wild material | | 2120093 | W6 59171 |
| 307 | W6 59183 | CBG-10474 | Leersia virginica Willd. | Illinois, United States | W6 | | | 2021 | | | | | | | Wild material | | 2120104 | W6 59183 |
| 308 | W6 59200 | CBG-10494 | Cinna arundinacea L. | Illinois, United States | W6 | | | 2021 | | | | | | | Wild material | | 2120119 | W6 59200 |
| 309 | W6 59234 | CBG-10548 | Dasistoma macrophyllum (Nutt.) Raf. | Illinois, United States | W6 | | | 2021 | | | | | | | Wild material | Received as Dasistoma macrophylla. Plant numbers estimated. Few this year; abundant other years in numerous locations. | 2120206 | W6 59234 |
| 310 | NA 86881 | ASA-009A | Ilex vomitoria Aiton | Virginia, United States | NA | | | 2021 | COLLECTED | 01/13/2020 | Virginia Beach: First Landing State Park. Collected in the park campground, near the location of VIRG-015. One plant at campsite #166, the other near site #73 | 36.91886900, -76.05188900 | 2 | 15 deg slope; SE-facing; sand. Dunes with live oaks | Wild material | | 2116470 | NA 86881 |
| 311 | NA 88399 | NCBG-670 | Kalmia latifolia L. | Maryland, United States | NA | | | 2021 | | | | | | | Wild material | | 2116373 | NA 88399 |
| 312 | W6 59005 | NCBG-455 | Avenella flexuosa (L.) Parl. | Virginia, United States | W6 | | | 2021 | | | | | | | Wild material | inflorescence drooping/nodding | 2116323 | W6 59005 |
| 313 | W6 59062 | NCBG-676 | Andropogon gerardi Vitman | Virginia, United States | W6 | | | 2021 | | | | | | | Wild material | | 2116376 | W6 59062 |
| 314 | Ames 35666 | Starved Rock State Park | Aronia melanocarpa (Michx.) Elliott | Illinois, United States | NC7 |  | | 2021 | COLLECTED | 05/04/2021 | Two areas sampled between Ottawa and North Utica including Starved Rock State Park (Lover's Leap and also LaSalle/Tonti Canyon) in Deer Park Township (T33N R2E) and also along IL 71/Courtney Street on bluffs above Illinois River in South Ottawa Township (T33N R3E). | 41.33565600, -88.85903400 | 142 | Sandstone outcropping | Wild material | Genotypes in nature noted were averaging 3.0' in height with sparse suckering and relatively open branching. A small, widely scattered population localized to steep sandstone bluffs. | 2115975 | Ames 35666 |
| 315 | Ames 35667 | Kankakee Sands Preserve | Aronia ×prunifolia (Marshall) Rehder | Illinois, United States | NC7 |  | | 2021 | COLLECTED | 05/04/2021 | Kankakee Sands Preserve located approximately 2.3 miles southwest of Wilmington in Custer Township, T32N R9E NE 1/4 Sec. 11 | 41.27166000, -88.15701800 | 170 | Sand shrub prairie | Wild material | Genotypes noted in nature were averaging 5.0-6.0' in height, relatively upright in growth habit and extremely dense suckering. Numerous clones noted covering expansive areas (e.g. 30 yards by 20 yards, etc.). Variation in branching and glossiness of leaves noted across genotypes present in nature. | 2115976 | Ames 35667 |
| 316 | Ames 35668 | Iroquois County Conservation Area | Aronia ×prunifolia (Marshall) Rehder | Illinois, United States | NC7 |  | | 2021 | COLLECTED | 05/05/2021 | Iroquois County Conservation Area located approximately 4.5 miles northeast of Beaverville in Beaverville Township, T29N R11W NE1/4 Sec. 22 | 40.99154700, -87.58073200 | 198 | Woodland edge of wet sand prairie | Wild material | Wide variety of genotypes noted in nature averaging 3.5-7' in height. Some growing in shade of oak forest were sparse suckering and open branching compared to open grown specimens that were extremely dense with suckers. | 2115977 | Ames 35668 |
| 317 | Ames 35660 | Kiamichi Mountains | Ptelea trifoliata L. | Oklahoma, United States | NC7 | | | 2021 | COLLECTED | 07/19/2018 | Kiamichi Mountains of Ouachita National Forest along Road 6025 just west of State Highway 259, T2N R25E SW 1/4 NE 1/4 SW 1/4 Sec. 27 | 34.61314900, -94.67035700 | 651 | Open, dry ridgetop, rocky roadside. | Wild material | Specimens sampled measuring approximately 20-25' in height. | 2114985 | Ames 35660 |
| 318 | NA 88190 | MARSB-749 | Baccharis halimifolia L. | New York, United States | NA | | | 2021 | | | | | | | Wild material | Simple, alternate, toothed leaves. White flowers that become conscpicuously fluffy when ripe. | 2113604 | NA 88190 |
| 319 | Ames 35649 | Backbone | Pinus strobus L. | Iowa, United States | NC7 |  | | 2021 | COLLECTED | 03/04/2021 | Backbone State Park located approximately 5.15 miles south, southwest of Strawberry Point, T90N R6W NW1/4 Sec. 16 | 42.61131500, -91.56098900 | 316 | Cliff edges and steep slopes above the Maquoketa River, including the ridge known as the "Backbone". | Wild material | The native range of Pinus strobus is concentrated in the northeastern United States extending south into the northern edge of Georgia and west to central Minnesota. In Iowa, there are scattered populations in a few northeastern counties and also a very small disjunct population in central Iowa (Hardin County, Ames 32758) and also one in southeastern Iowa (Muscatine County, Ames 35635). This accession represents genetics from "legacy" specimens from northeastern Iowa in Backbone State Park (Delaware County). Although a significant number of P. strobus were planted at this park in the 1920's a significant number of native specimens still exist throughout the park typically found on extreme topographical features such as steep slopes and rock outcroppings. Genetics from this site likely represents the extreme southwestern edge of the species native range. Genetics may likely be adapted/tolerant to drought and also late winter/early spring extreme temperature fluctuations. Accession was collected as scions in winter to capture genetics that are of known origin. | 2113351 | Ames 35649 |
| 320 | Ames 35650 | Bixby | Pinus strobus L. | Iowa, United States | NC7 |  | | 2021 | COLLECTED | 03/04/2021 | Bixby State Preserve on slopes above Bear Creek, located approximately 6.25 miles east of Strawberry Point, T91N R5W SE1/4 Sec. 22 | 42.67534800, -91.41301000 | 324 | Cliff edges and steep slopes. | Wild material | The native range of Pinus strobus is concentrated in the northeastern United States extending south into the northern edge of Georgia and west to central Minnesota. In Iowa, there are scattered populations in a few northeastern counties and also a very small disjunct population in central Iowa (Hardin County, Ames 32758) and also one in southeastern Iowa (Muscatine County, Ames 35635). This accession represents genetics from "legacy" specimens from northeastern Iowa in Bixby State Preserve (Clayton County). Genetics from this site likely represents the extreme southwestern edge of the species native range. Genetics may likely be adapted/tolerant to drought and also late winter/early spring extreme temperature fluctuations. Accession was collected as scions in winter to capture genetics that are of known origin. | 2113352 | Ames 35650 |
| 321 | Ames 35635 | Wildcat Den | Pinus strobus L. | Iowa, United States | NC7 |  | | 2021 | COLLECTED | 03/02/2021 | Wildcat Den State Preserve near Muscatine, T77N R1E SW1/4 SW1/4 Sec. 17 | 41.46735000, -90.88171000 | 185 | Canyon edges and valleys. | Wild material | The native range of Pinus strobus is concentrated in the northeastern United States extending south into the northern edge of Georgia and west to central Minnesota. In Iowa, there are scattered populations in a few northeastern counties and also a very small disjunct population in central Iowa (Hardin County, Ames 32758) and one in southeastern Iowa (Muscatine County). This accession represents genetics from five mother "legacy" trees located in Wildcat Den State Park (Muscatine County). Although a significant number of P. strobus were planted at this park in the early 1900's a significant number of native specimens still exist as a localized grouping within the central portion of the park in the deep valleys and also one specimen on an extreme rock outcropping. P. strobus from this site represents the extreme southwestern edge of the species native range. Genetics may likely be adapted/tolerant to drought and also late winter/early spring extreme temperature fluctuations. Specimen #1 sampled at this site is currently ranked as the 6th largest Pinus strobus in the state (M. Rouw, pers. comm. 28 February 2021) measuring 11'6" circumference; 127.5' height; and 45' crown spread (Total Points: 276.75). Accession was collected as scions in winter to capture genetics that are of known origin. | 2113335 | Ames 35635 |
| 322 | Ames 35612 | Ames 35612 | Agastache nepetoides (L.) Kuntze | Iowa, United States | NC7 |  | | 2020 | COLLECTED | 10/15/2020 | Private property located approximately 5.8 miles southeast of Westfield on both sides of N Ridge Road, T91N R48W SW 1/4 Sec. 16, Sioux Twp., Plymouth County | 42.69938500, -96.51933700 | 419 | Savanna (bur oak, walnut, hackberry). Loess hills and valleys. Distrurbed open forest. | Wild material | Plants sampled in nature measuring approximately 3-4 feet in height. | 2110274 | Ames 35612 |
| 323 | NA 87611 | ZARKS-030 | Rhododendron prinophyllum (Small) Millais | Arkansas, United States | NA | | | 2020 | COLLECTED | 10/05/2014 | King's River Falls Natural Area; King's River, downstream of junction of county roads 3415 and 3500 along trail leading from parking area and trail sign. | 35.90106000, -93.57456000 | 514 | Mesic, mixed deciduous forest; growing on ledge along river, in rocky soil. | Wild material | See NA 84645 for material received from the Arnold Arboretum in 2017. | 2115796 | NA 87611 |
| 324 | NA 88466 | F013 | Viburnum dentatum L. | Pennsylvania, United States | NA | | | 2020 | COLLECTED | 09/09/2020 | Schaefferstown, PA: Middle Creek Wildlife Management Area, along the Middle Creek power lines on the southern side, starting near Laurel Drive and hiking east to Middle Creek. | 40.26400000, -76.25333000 | | | Wild material | | 2109477 | NA 88466 |
| 325 | Ames 35547 | White Pine Hollow | Pinus strobus L. | Iowa, United States | NC7 |  | | 2020 | COLLECTED | 08/20/2020 | White Pine Hollow State Preserve located approximately 2.65 miles northwest of Luxemburg, T90N R2W SE 1/4 Sec. 7, Dubuque County | 42.61954600, -91.11933000 | 308 | High-quality remant mixed woods | Wild material | The native range of Pinus strobus is concentrated in the northeastern United States extending south into the northern edge of Georgia and west to central Minnesota. In Iowa, there are scattered populations in a few northeastern counties and also a very small disjunct population in central Iowa (Hardin County, Ames 32758) and also in southeastern Iowa (Muscatine County, Ames 35635). This accession represents genetics from northesastern Iowa in White Pine Hollow (WPH) in Dubuque County and is known to harbor the largest stand of white pine in Iowa dating back to the 1870's. WPH was the first woodland in Iowa to be dedicated (1967) as a state preserve and was previously known to contain Iowa's oldest white oak with a core date estimated back to the year 1580 (Duvick and Blasing 1983). WPH is home to the largest native specimen of Pinus strobus measuring 11’1.5” circumference, 142’ tall, and 44’ spread for a total of 286.3 points (Rouw, M., personal communication, 21 September 2020). “In an assessment of 92 of the largest white pines (native and cultivated) across Iowa, 68 occur in WPH. Out of 40 that exceed a height of 130', 38 are found in WPH with seven of those exceeding 140' and two surpassing 147' (Rouw, M., personal communication, 18 September 2020). The site is also the location of height records (Iowa) for several tree species including Ulmus americana 108', Tilia americana 105.5', Acer saccharum 109', Quercus alba 107', and Carya ovata 109’ (Rouw, M., personal communication, 18 September 2020). P. strobus in WPH is the dominant overstory species specifically in areas next to ravines/valleys and some immediately adjacent uplands. P. strobus from this site represents the extreme western edge of the species native range. Genetics may likely be adapted/tolerant to drought and also late winter/early spring extreme temperature fluctuations. Accession was collected both as seeds (2020) and as scions (2021). | 2106728 | Ames 35547 |
| 326 | NA 86848 | ZARKS-025 | Acer saccharum Marshall subsp. leucoderme (Small) Desmarais | Arkansas, United States | NA | | | 2020 | COLLECTED | 10/09/2014 | Cedar Fourche Creek; Harper Grocery Rd. at Rock Springs Rd. | 34.66470800, -93.26778900 | 209 | Mesic, mixed deciduous forest; growing on the bank just above a small stream | Wild material | | 2115797 | NA 86848 |
| 327 | NA 87370 | NCTN59 | Hydrangea barbara (L.) Bernd Schulz | Tennessee, United States | NA | | | 2020 | COLLECTED | 22/09/2019 | | 35.10423000, -84.61030000 | 256 | Mesic oak-pine forest edge, growing up trunks of trees on a steep, rocky slope. | Wild material | Three seedlings received along with NA 87106-87112, but not requested for accessioning at the same time. | 2141752 | NA 87370 |
| 328 | NA 87036 | Site 3A/Live Oak Landing/Holmes Creek Site | Magnolia ashei Weath. | Florida, United States | NA | | | 2020 | COLLECTED | 07/15/2020 | Along Holmes Creek at Live Oak Landing. | 30.59208000, -85.83750000 | 11 | Shade to partial shade of bluffs above the creek in well-drained mesic to dry deciduous woodlands with a few broadleaved and coniferous evergreens. | Wild material | Although these were collected without any field collection number, seeds from individual trees were separated with letter identifiers that will be maintained with the qualifier (seedling) records. The relationships are as follows: 1. Maternal letter G, NA 87036-J, L, P, and T; maternal letter H, NA 87036-V; maternal letter K, NA 87036-X, Z, and H1; maternal letter N, NA 87036-H2. In addition, three seedlings' maternal letters were lost, and these will be NA 87036-H3, H4, and H5. See the following accessions for earlier collections from this same site/population, listed in our records as "Site 3A/Live Oak Landing/Holmes Creek Site": NA 81555 (2013), NA 82745 (2015), and NA 82745.01 (2019). | 2109403 | NA 87036 |
| 329 | NA 86434 | Pulverulentus Group | Styrax americanus Lam. | Texas, United States | NA | | | 2020 | COLLECTED | 09/08/2018 | Near Gum Slough, on the edges of woodlands along the north side of road FM 2246. | 30.33332000, -93.94704000 | 15 | Plants are found along the edges and moist to wet areas of Gum Slough in part shade to full sun of a mixed deciduous and broadleaved evergreen woodlands. Soils are generally acidic with loamy to clayey sediments, but with some areas consisting of deep, nearly level loamy, poorly drained soil. | Wild material | Species occurrence is infrequent at this location. Collector's note on the name under which this material was gathered, Styrax americanus var. pulverulentus: "In general, the var. pulverulentus is considered "taxonomically inconsequential" by many botanists. Even so, this densely pubescent characteristic is highly uniform across every plant I observed in the sampled population. Weakley notes that "true" var. pulverulentus can be found as far west as East Texas and, in my humble opinion, the population sampled herein represents this "taxon". Regardless, for the purposes of drawing distinction between "typical" Styrax americanus and the densely pubescent form, I've chosen to use this varietal name. It will be interesting to observe whether the seedling progeny are uniformly similar to their parents when they germinate." [Actual altitude recorded was 14.8 m, but decimals can't be used in the database, so the number was rounded.] | 2109219 | NA 86434 |
| 330 | WLP 2024 | MARSB-988 | Viburnum acerifolium L. | New York, United States | NA | | | 2019 | COLLECTED | 08/30/2019 | Onondaga County; Geddes; Long Branch County Park. | 43.11757000, -76.25210000 | | Growing in full shade in forest, in moist to dry, well-drained silt/sand soil. | | Seed harvested from 35+ individuals in a population of 100+. Common. Seed 100 percent healthy; seed maturation middle. | 2109173 | WLP 2024 |
| 331 | WLP 2025 | MARSB-992 | Viburnum acerifolium L. | New York, United States | NA | | | 2019 | COLLECTED | 09/06/2019 | Tioga County; Candor; Carolina Pinnacles Unique Area (owned by Cornell University, and administered as part of Cornell Botanical Gardens), near Nanticoke Creek. [Originally listed as Willseyville, NY 13864.] | 42.26431000, -76.37186000 | | Forested hillside in full shade; growing in dry, well-drained silt/loam soil. | | Seed harvested from 20+ individuals in a population of 75+. Common. Seed 90 percent healthy; seed maturation middle, late. | 2109174 | WLP 2025 |
| 332 | NA 88161 | NCBG-354 | Ilex opaca Aiton | Virginia, United States | NA |  | | 2019 | COLLECTED | 10/14/2015 | Belle Isle State Park (Rappahanock River): from park entrance, continue on State Rte. 683/Belle Isle Rd. Turn right onto Creek Landing Road. Park at end of road, follow Mulberry Trail. Population along boardwalk as you walk toward the canoe launch. | 37.78222000, -76.60419000 | 2 | Riverside forest. | Wild material | | 2098425 | NA 88161 |
| 333 | NA 88171 | NCBG-667 | Kalmia latifolia L. | Maryland, United States | NA |  | | 2019 | | | | | | | Wild material | | 2098506 | NA 88171 |
| 334 | OPGC 7975 | NCBG-416 | Lechea maritima Legg. ex Britton | North Carolina, United States | OPGC |  | | 2019 | | | | | | | Wild material | | 2098440 | OPGC 7975 |
| 335 | OPGC 7985 | NCBG-609 | Lechea maritima Legg. ex Britton | North Carolina, United States | OPGC |  | | 2019 | | | | | | | Wild material | | 2098485 | OPGC 7985 |
| 336 | OPGC 7986 | NCBG-617 | Lechea maritima Legg. ex Britton | North Carolina, United States | OPGC |  | | 2019 | | | | | | | Wild material | | 2098491 | OPGC 7986 |
| 337 | W6 57453 | NCBG-233 | Teucrium canadense L. | North Carolina, United States | W6 |  | | 2019 | | | | | | | Wild material | | 2098377 | W6 57453 |
| 338 | W6 57560 | NCBG-608 | Chrysopsis gossypina (Michx.) Elliott subsp. gossypina | North Carolina, United States | W6 |  | | 2019 | | | | | | | Wild material | | 2098484 | W6 57560 |
| 339 | W6 57591 | NCBG-694 | Juncus scirpoides Lam. | Virginia, United States | W6 |  | | 2019 | | | | | | | Wild material | | 2098515 | W6 57591 |
| 340 | W6 57403 | NEWFS-334 | Carex crinita Lam. | New Hampshire, United States | W6 |  | | 2019 | | | | | | | Wild material | | 2098200 | W6 57403 |
| 341 | NA 88358 | MARSB-341 | Iva frutescens L. | New Jersey, United States | NA |  | | 2019 | | | | | | | Wild material | | 2097587 | NA 88358 |
| 342 | W6 57055 | MARSB-130 | Danthonia spicata (L.) P. Beauv. ex Roem. & Schult. | New Jersey, United States | W6 |  | | 2019 | | | | | | | Wild material | | 2097494 | W6 57055 |
| 343 | WLP 1686 | APS/RS/2019/067/396 | Rosa setigera Michx. | Arkansas, United States | NA |  | | 2019 | COLLECTED | 11/07/2019 | Located near intersection of Smith Mountain Road and Newton County 8828 Road approximately 6.00 miles north of Deer, Newton County | 35.91212000, -93.21112000 | 636 | Roadside, upland with rocky soils | Wild material | | 2097789 | WLP 1686 |
| 344 | Ames 35237 | Ames 35237 | Monarda fistulosa L. | New Mexico, United States | NC7 |  | | 2019 | COLLECTED | 10/03/2019 | Railroad Canyon located approximately 6.38 miles west of Kingston just north of highway 152, T16S R10W Grant County | 32.91279900, -107.81640300 | 2173 | Sparsely wooded canyon with small creek. | Wild material | | 2097773 | Ames 35237 |
| 345 | WLP 1685 | JDC/RS/2019/036/915 | Rosa setigera Michx. | Iowa, United States | NA |  | | 2019 | COLLECTED | 10/17/2019 | Ledges State Park located approximately 4.75 miles south of Boone, just south of the Oakwoods Shelter/Picnic area, T83N R26W NE1/4 NE1/4 and also NW1/4 NE1/4 Sec. 21, Boone County | 41.99262400, -93.87724800 | 330 | Edges of woods (adjacent to prairie) and also within 20-25 yards from woods in prairie. Noted in east, west, and south-facing edges of woods (no specimens noted on north-facing woodland edges) | Wild material | Woody shrub/vine stretching up to 12' in length. Alternate compound leaves usually consisting of five lealets. Leaf rachis and stipule margins glandular. Mature hypanthium and pedicel with stipitate glandular hairs. Mature hypanthium mostly bright to dark red in color with a few dark orange noted at time of harvest (17 October 2019). Leaves rather to somewhat glossy. This collection represents genetics from the northwestern edge of the species range, likely suggesting good cold-hardiness (USDA Zone 5a). | 2097769 | WLP 1685 |
| 346 | WLP 156 | NACPEC19-022 | Oxydendrum arboreum (L.) DC. | Kentucky, United States | NA | | | 2019 | COLLECTED | 09/09/2019 | Madison County; Berea College Forest: Around the corner from Upper Indian Fort Trail Junction, on top of the Davis Hollow "holler" | 37.56414400, -84.23341800 | 477 | Sandstone outcrop, incredibly thin, low pH <4. Very heavy foot traffic | Wild material | | 2110468 | WLP 156 |
| 347 | WLP 158 | NACPEC19-029 | Rhus glabra L. | Kentucky, United States | NA | | | 2019 | COLLECTED | 09/09/2019 | Madison County; Berea College Forest: Radio Tower Service Trail | 37.55289700, -84.28793400 | 379 | Xeric shade knob, limestone shale conglomerate material | Wild material | | 2110470 | WLP 158 |
| 348 | WLP 163 | NACPEC19-046B | Hydrangea cinerea Small | Georgia, United States | NA | | | 2019 | COLLECTED | 09/14/2019 | Walker County; Lula Lake Land Trust: Bridge from parking lot to South Creek Trail | 34.92114500, -85.38035700 | 373 | Limestone bluffs surrounding dry creek bed in mixed mesophytic forest | Wild material | | 2110475 | WLP 163 |
| 349 | WLP 164 | NACPEC19-047 | Kalmia latifolia L. | Georgia, United States | NA | | | 2019 | COLLECTED | 09/14/2019 | Walker County; Lula Lake Land Trust: Off of South Creek trail on North side of bridge from parking lot | 34.92134100, -85.38051100 | 373 | Riparian zone, wet slope of creek, moist, sandy banks | Wild material | | 2110476 | WLP 164 |
| 350 | WLP 167 | NACPEC19-053 | Mitchella repens L. | Georgia, United States | NA | | | 2019 | COLLECTED | 09/14/2019 | Walker County; Lula Lake Land Trust: Middle Trail near top, also collected along Connector Trail to Middle Trail from parking lot. | 34.93141800, -85.36991400 | 469 | Mesic, sandy, rocky Oak-Hickory woodland slope - likely acidic | Wild material | | 2110479 | WLP 167 |
| 351 | WLP 168 | NACPEC19-054 | Viburnum acerifolium L. | Georgia, United States | NA | | | 2019 | COLLECTED | 09/14/2019 | Walker County; Lula Lake Land Trust: Middle Trail near top. | 34.93146200, -85.37018800 | 449 | Mesic, sandy, rocky Oak-Hickory woodland slope - likely acidic | Wild material | | 2110480 | WLP 168 |
| 352 | WLP 172 | NACPEC19-069 | Smilax lasioneura Hook. | North Carolina, United States | NA | | | 2019 | COLLECTED | 09/16/2019 | Transylvania County; Southern Highland Reserve: Toxaway Mountain, Service Road (name unknown), adjacent to Southern Highlands Reserve: Power line cut. | 35.13228000, -82.98331400 | 1455 | Roadside edge, disturbed opening: mountaintop mixed Oak-Chestnut woodland (forest margin at high elevation) | Wild material | | 2110486 | WLP 172 |
| 353 | Ames 35229 | JDC/AS/2019/020/899 | Agastache scrophulariifolia (Willd.) Kuntze | Iowa, United States | NC7 |  | | 2019 | COLLECTED | 10/01/2019 | Hertz Family Woods & Nature Preserve just 2.25 miles south of Nevada (T83N R22W NW1/4 NW1/4 Sec. 20) and Robison Wildlife Acres just 6.75 miles south of Nevada (T82N R22W NE1/4 SW1/4 Sec. 8), Story County | 41.99070000, -93.44186700 | 285 | Moist, semi-shaded, deciduous woods. | Wild material | Plants measuring approximately 6' in height with somewhat short (perhaps due to dense shade) 2-3" spikes rather white or extremely pale pink in color. Peak flowering occurred circa 26 August 2019 in nature. | 2097765 | Ames 35229 |
| 354 | Ames 35228 | JDC/AS/2019/031/910 | Agastache scrophulariifolia (Willd.) Kuntze | Iowa, United States | NC7 |  | | 2019 | COLLECTED | 09/30/2019 | Ledges State Park located approximately 4.75 miles south of Boone, just east and south of the Carl Fritz Henning Shelter, T83N R26W SW1/4 SE1/4 NW1/4 Sec. 21, Boone County | 41.98786200, -93.88824500 | 276 | Moist, semi-shaded, deciduous woods. Recently disturbed. | Wild material | Plants measuring approximately 6-8' in height with 4-5" spikes rather white or extremely pale pink in color. Peak flowering occurred circa 26 August 2019 in nature. | 2097764 | Ames 35228 |
| 355 | Ames 34943 | JDC/BC/2019/025/904 | Blephilia ciliata (L.) Benth. | West Virginia, United States | NC7 |  | | 2019 | COLLECTED | 08/10/2019 | Smoke Hole Region: Powers Hollow. Located approximately 5.2 miles west of Petersburg on the east side of Powers Hollow Road, Grant County | 39.00611600, -79.22179200 | 482 | Open woodland. Dry, rock with sparse vegetation. | Wild material | Plants approximately 12" in height. Specimens at time of sampling (10 August 2019) were completely dried to soil line with no leaves remaining. | 2096625 | Ames 34943 |
| 356 | Ames 34944 | JDC/HD/2019/023/902 | Helianthus divaricatus L. | West Virginia, United States | NC7 |  | | 2019 | COLLECTED | 08/10/2019 | Smoke Hole Region: Eagle Rock. Located on east side of South Branch Potomac River approximately 2.85 miles north of Upper Tract and 0.5 miles northeast of Eagle Rock formation, Pendleton County | 38.82840700, -79.28397500 | 702 | Open woodland. Dry, rock with sparse vegetation. | Wild material | Majority of specimens noted were close to peak fruit maturity with a few specimens just past peak flowering. Specimens approximately 3' in height. | 2096626 | Ames 34944 |
| 357 | Ames 34946 | JDC/LL/2019/024/903 | Linum lewisii Pursh | West Virginia, United States | NC7 |  | | 2019 | COLLECTED | 08/10/2019 | Smoke Hole Region: Eagle Rock. Located on east side of South Branch Potomac River approximately 2.85 miles north of Upper Tract and 0.5 miles northeast of Eagle Rock formation, Pendleton County | 38.82840700, -79.28397500 | 702 | Exposed rock cliff edges. | Wild material | Plants approximately 20-24" in height. Fruits persisting and fully mature at time of sampling (10 August 2019). Noted a few plants actively blooming. | 2096628 | Ames 34946 |
| 358 | Ames 34948 | JDC/PO/2019/026/905 | Physocarpus opulifolius (L.) Maxim. | West Virginia, United States | NC7 |  | | 2019 | COLLECTED | 08/10/2019 | Smoke Hole Region: Powers Hollow. Located approximately 5.2 miles west of Petersburg on the east side of Powers Hollow Road, Grant County | 39.00339500, -79.22036500 | 455 | Exposed rock cliff edges. | Wild material | Fruits close to peak maturity. Small plants approximately 3-4' in height and spread likely due to extremely harsh habitat. In cultivation (NCRPIS), plants grow greater than 5' in height. | 2096630 | Ames 34948 |
| 359 | OPGC 7572 | JDC/HX/2019/028/907 | Heuchera alba Rydb. | West Virginia, United States | OPGC |  | | 2019 | COLLECTED | 08/10/2019 | Smoke Hole Region: Powers Hollow. Located approximately 5.2 miles west of Petersburg on the east side of Powers Hollow Road, Grant County | 39.00339500, -79.22036500 | 455 | Exposed rock cliff edges. | Wild material | Heuchera alba is a narrow Appalachian endemic and globally imperiled (G2) taxon recorded only from West Virginia and Virginia that occurs in sympatry with H. pubescens and H. americana. According to Scheutte et al. 2018, the range for H. alba is restricted to high elevation acidic sandstone ridges and outcrops in the Ridge-and-Valley province of West Virginia and Virginia. In cultivation (central Iowa) the leaves emerge with subtle variegation that is lost by early summer. Flowers are creamy white to pale green. | 2096627 | OPGC 7572 |
| 360 | OPGC 7463 | CBG-8629 | Delphinium tricorne Michx. | Idaho, United States | OPGC |  | | 2019 | | | | | | | Wild material | | 2092684 | OPGC 7463 |
| 361 | OPGC 7496 | CBG-9546 | Solidago ulmifolia Muhl. ex Willd. | Illinois, United States | OPGC |  | | 2019 | | | | | | | Wild material | | 2092814 | OPGC 7496 |
| 362 | Ames 34606 | JDC/MB/2019/011/890 | Monarda brevis (Fosberg & Artz) Floden | West Virginia, United States | NC7 |  | | 2019 | | | | | | | Wild material | Variation in flower color present from near white, faint pink to faint "smoky" purple. Majority of specimens noted at collection site in nature were approximately 3-5 days past peak flower on 10 June 2019 with seeds reaching maturity approximately 55 days later. Majority of specimens observed were approximately 10" in height. Very healthy, dark-green leaves that maintained quality throughout the season (observed mid-August 2019). Some specimens consisting of 25-30 flowering stems encompassing a 1.5 sq. ft. area. | 2092642 | Ames 34606 |
| 363 | Ames 34607 | JDC/MB/2019/012/891 | Monarda brevis (Fosberg & Artz) Floden | West Virginia, United States | NC7 |  | | 2019 | | | | | | | Wild material | This accession likely represents the holotype for Monarda brevis that was vouchered by Lena Artz in 1953 (Catalog No. 2097485). Variation in flower color present from near white, faint pink to faint "smoky" purple. Majority of specimens noted at collection site in nature were approximately 3-5 days past peak flower on 10 June 2019 with seeds reaching maturity approximately 55 days later. Majority of specimens observed were apprxoimately 10" in height. Very healthy, dark-green leaves that maintained quality throughout the season (observed mid-August 2019). | 2092643 | Ames 34607 |
| 364 | Ames 34608 | JDC/MB/2019/013/892 | Monarda brevis (Fosberg & Artz) Floden | West Virginia, United States | NC7 |  | | 2019 | | | | | | | Wild material | Majority of specimens noted at collection site in nature were approximately 5-7 days past peak flower on 11 June 2019 with seeds reaching maturity approximately 55 days later. Very healthy, dark-green leaves near peak flowering with some minor decline in leaf quality later in the season (observed mid-August 2019). Majority of specimens less than 10" in height. A few specimens with noteable hairs on stems, specifically near soil line. | 2092644 | Ames 34608 |
| 365 | Ames 34609 | JDC/MB/2019/014/893 | Monarda brevis (Fosberg & Artz) Floden | West Virginia, United States | NC7 |  | | 2019 | | | | | | | Wild material | Variation in flower color present from near white, faint pink to faint "smoky" purple. Majority of specimens noted at collection site in nature were approximately 3-5 days past peak flower on 10 June 2019 with seeds reaching maturity approximately 55 days later. Majority of specimens observed were approximately 10" in height. Very healthy, dark-green leaves that maintained quality throughout the season (observed mid-August 2019). | 2092645 | Ames 34609 |
| 366 | Ames 34610 | JDC/MB/2019/015/894 | Monarda brevis (Fosberg & Artz) Floden | West Virginia, United States | NC7 |  | | 2019 | | | | | | | Wild material | Many genets noted at collection site in nature consisted of 25-30 stems, but individual stems are widely spaced (e.g. 1-5") apart compared to other populations (four) noted (2019 reconnaisance) where stem spacing was typically observed at 0.25-0.5" apart. Very healthy, dark-green leaves noted in early/mid June, but leaf quality greatly declined when observed in mid-August in contrast to other populations observed in nature that seemed to maintain leaf quality throughout the season. Many plants at this site were defoliated likely due to disease (leaf spot) or tattered likely due to possible insect feeding. Specimens noted were circa 10-12 days from initiation of flowering on 12 June 2019 and during mid-August a few specimens were still observed flowering with about 10-20% of infructescences were still green. The overall phenology of this M. brevis population at this site is quite different in comparison to other populations (four) observed in 2019, with flowering being much later (e.g. 10-25 days); leaf quality lower; and synchronization of flowering extremely variable within genets of this population. | 2092646 | Ames 34610 |
| 367 | WLP 686 | NA 85862 | Amelanchier arborea (F. Michx.) Fernald | Kentucky, United States | NA | | | 2019 | COLLECTED | 06/15/2019 | Madison County; ; South of Berea. | 37.55708000, -84.29542000 | | Growing on the side of a steep Devonian black shale embankment, partly shaded by the canopy above. | | There were other Amelanchier arborea trees in the immediate vicinity, however, these trees did not have any significant amount of viable berries. These berries were harvested from approximately 8 m high in the tree. | 2109078 | WLP 686 |
| 368 | Ames 34361 | Ames 34361 | Monarda punctata L. | Wisconsin, United States | NC7 |  | | 2018 | COLLECTED | 10/11/2018 | Fort McCoy Military Training Area located 5.0 miles northeast of Sparta, T17N R3W S edge of Sec. 3; NE 1/4 and NE 1/4 of NW1/4 of Sec. 10; NE 1/4 of Sec. 9; and SE 1/4 of Sec. 4, Monroe County. | 43.97153900, -90.72177200 | 282 | Oak and pine barren community dominated (80%) by sand on variable 0 to 45% slopes. | Wild material | | 1968260 | Ames 34361 |
| 369 | WLP 307 | AF2018-001 | Acer saccharum Marshall subsp. floridanum (Chapm.) Desmarais | Virginia, United States | NA | | | 2018 | COLLECTED | 09/10/2018 | James City County; ; Near Grove Creek, near the roadside in front of the wastewater plant at the end of Log Cabin Beach Rd. | 37.21613000, -76.63348000 | 47 | Roadside near creek. | | Several large trees along roadside, fairly common. Herbarium voucher collected (see barcode NA0103770). | 2108850 | WLP 307 |
| 370 | Ames 34790 | NCBG-535 | Rhus copallinum L. | Virginia, United States | NC7 |  | | 2018 | COLLECTED | 09/21/2016 | Occoquan Bay National Wildlife Refuge just southeast of Woodbridge. | 38.64347000, -77.23675000 | 4 | Meadow | Wild material | | 1965972 | Ames 34790 |
| 371 | GPRU 165 | NCBG-218 | Prunus serotina Ehrh. | North Carolina, United States | GEN | | | 2018 | | | | | | | Wild material | | 1965868 | GPRU 165 |
| 372 | NA 88020 | NCBG-254 | Morella pensylvanica (Mirb.) Kartesz | North Carolina, United States | NA |  | | 2018 | | | | | | | Wild material | | 1965890 | NA 88020 |
| 373 | W6 54633 | NCBG-208 | Bolboschoenus robustus (Pursh) Soják | North Carolina, United States | W6 | | | 2018 | | | | | | | Wild material | Bolboschoenus robustus | 1965859 | W6 54633 |
| 374 | W6 54702 | NCBG-359 | Distichlis spicata (L.) Greene | Virginia, United States | W6 |  | | 2018 | | | | | | | Wild material | Distichlis spicata | 1965928 | W6 54702 |
| 375 | OPGC 6537 | MARSB-380 | Solidago sempervirens L. | New Jersey, United States | OPGC |  | | 2018 | | | | | | | Wild material | Solidago sempervirens | 1964769 | OPGC 6537 |
| 376 | W6 54050 | MARSB-352 | Juncus effusus L. | New York, United States | W6 |  | | 2018 | | | | | | | Wild material | Juncus effusus | 1964766 | W6 54050 |
| 377 | Ames 34307 | JDC/EP/2018/051/864 | Echinacea paradoxa (Norton) Britton | Missouri, United States | NC7 |  | | 2018 | COLLECTED | 07/16/2018 | Auxvasse Natural Area located 8.44 miles southeast of Fulton, T46N R8W S 1/4 Sec. 9, Callaway County | 38.76733000, -91.82958500 | 205 | Dolomite glade. Large (110 acres) and exceptionally diverse (220 plant species identified). According to local MDC biologists, this is one of the best glades north of the Missouri River in Missouri. Northern most, native population of Echinacea paradoxa in Missouri. | Wild material | Plants reached peak flower on 30 May 2018. Specimens ranged from 2.0-4.0' in height. | 1964614 | Ames 34307 |
| 378 | Ames 34310 | JDC/MB/2018/050/863 | Monarda bradburiana L. C. Beck | Missouri, United States | NC7 |  | | 2018 | COLLECTED | 07/16/2018 | Auxvasse Natural Area located 8.44 miles southeast of Fulton, T46N R8W S 1/4 Sec. 9, Callaway County | 38.76733000, -91.82958500 | 205 | Dolomite glade. Large (110 acres) and exceptionally diverse (220 plant species identified). According to local MDC biologists, this is one of the best glades north of the Missouri River in Missouri. | Wild material | Plants measuring circa 1.0' in height. Peak flowering occurred around 18 May 2018. Seeds likely reached full maturity around first week in July (2018). | 1964617 | Ames 34310 |
| 379 | Ames 34320 | JDC/MR/2018/058/871 | Monarda russeliana Nutt. ex Sims | Oklahoma, United States | NC7 |  | | 2018 | COLLECTED | 07/19/2018 | Kiamichi Mountains of Ouachita National Forest along Road 6025 just west of highway 259, T2N R25E S 1/2 Sec. 27 and S 1/2 Sec. 28 Le Flore County. | 34.61320100, -94.66641200 | 651 | Open, dry, rocky woods. | Wild material | Petite plants with only 1-3 stems per plant ranging from 1.0-1.5' in height. At time of collection (19 July 2018) peduncle showing 1-2" of dead/brown tissue. Leaves twice as long (or more) as wide. Generally three pairs of opposite leaves per stem. Slight pubescence on leaves with 1-2 mm petiole. Leaves rather flat. Seeds likely reached peak maturity around first week in July. | 1964627 | Ames 34320 |
| 380 | Ames 34321 | JDC/MR/2018/061/874 | Monarda russeliana Nutt. ex Sims | Oklahoma, United States | NC7 |  | | 2018 | COLLECTED | 07/19/2018 | On the northwest side of Wister Lake along the north side of Wister Lake MGMT Road, T5N R24E NW 1/4 NW 1/4 and NE 1/4 NW 1/4 Sec. 6, Le Flore County. | 34.93915700, -94.81967400 | 160 | Open, dry, rocky woods. | Wild material | Petite plants with only 1-3 stems per plant ranging from 1.0-1.5' in height. At time of collection (19 July 2018) peduncle showing 1-2" of dead/brown tissue. Leaves twice as long (or more) as wide. Generally three pairs of opposite leaves per stem. Slight pubescence on leaves with 1-2 mm petiole. Leaves rather flat. Seeds likely reached peak maturity around first week in July. | 1964628 | Ames 34321 |
| 381 | OPGC 5470 | JDC/BN/2018/056/869 | Baptisia nuttalliana Small | Arkansas, United States | OPGC |  | | 2018 | COLLECTED | 07/17/2018 | Located circa 2.60 miles northwest of Brightstar off Miller Road 159, Miller Road 74, Miller Road 75, Miller Road 154 and highway 237, Miller County | 33.14091000, -94.02229000 | 109 | Roadside. Edges of woods. | Wild material | Plants essentially all black with seeds past maturity by approximately 2-3 weeks, plants starting to break off at ground level and fruiting capsules starting to split at time of collection (17 July 2018). Seed quality rather poor at time of collection largely due to weevils. | 1964612 | OPGC 5470 |
| 382 | WLP 1190 | NA 85118 | Dirca palustris L. | Iowa, United States | NA |  | | 2018 | COLLECTED | 05/31/2018 | Private property located 3.35 miles southwest of Luther near Des Moines River, T82N R26W SW 1/4 SW 1/4 Sec. 3, Boone County | 41.93795800, -93.87109500 | 317 | Dense shade of mature oak forest. Deep ravines. | Wild material | Specimens measuring approximately 2-5' in height. Noticeable new growth (5-8") at time of seed collection. Population was in peak bloom 24 April 2018 with peak fruit maturity occuring on 30 May 2018. Fruits readily dropping when distrubed. Very slight tinge of white color to fully mature fruits. Seeds measuring approximately 0.5-0.7 cm in length. | 1963390 | WLP 1190 |
| 383 | Ames 34160 | Ames 34160 | Fraxinus americana L. | Pennsylvania, United States | NC7 |  | | 2017 | COLLECTED | 11/01/2017 | Urban loaction near the intersection of Pennsylvania ave. and Fort Washington Ave. Fort Washington, Montgomery County. | 40.13730600, -75.21111800 | 66 | Specimens located along a possible eixisting naural hedge row along the rightway of two existing parking lots. | Uncertain improvement status | | 1957726 | Ames 34160 |
| 384 | Ames 34052 | PB1701 | Betula papyrifera Marshall | Minnesota, United States | NC7 |  | | 2017 | COLLECTED | 09/16/2017 | Detroit Mountain area just east of Detroit Lakes approximately 2.9 miles, T139N R40W SW 1/4 NE 1/4 and NE 1/4 NE 1/4 NW 1/4 Sec. 21, Becker County | 46.81210900, -95.78208300 | 457 | Mixed deciduous woods. | Wild material | | 1954341 | Ames 34052 |
| 385 | Ames 34014 | Ames 34014 | Aronia melanocarpa (Michx.) Elliott | Illinois, United States | NC7 |  | | 2017 | COLLECTED | 09/03/2017 | Nachusa Grasslands - locally known as Coyote Point approximately 3.80 miles northwest of Franklin Grove just 0.60 miles west of Lowden Road, T22N R10E NE 1/4 NE 1/4 SW 1/4 Sec. 21, Lee County | 41.87972200, -89.35305600 | 220 | St. Peter's sandstone cliff, specimens noted on ridgetop and on slopes. | Wild material | This accession based on morphological/phenological observations at NCRPIS field plots seems to represent the "southern form" of A. melanocarpa, potentially a new Aronia species. This southern form was originally discovered by Brand et al. 2022 (Ploidy, genetic diversity and speciation of the genus Aronia) and is known for having glabrous stems and leaves and a distinct phyllotaxy than other Aronia species. In addition, plants tend to bloom approximately two weeks later than all other Aronia taxonomic groups and the inflorescences/infructescences are more spreading and extended due to longer peduncles and pedicels within the cyme. Fruit maturity tends to occur 2 to 4 weeks later than tetraploid A. melanocarpa and 4 to 6 weeks later than diploid A. melanocarpa. Phenolic levels are much higher in comparison to other A. melanocarpa accessions (Brand et al., 2017 - Anthocyanins, total phenolics, ORAC and moisture content of wild and cultivated dark-fruited Aronia species.) | 1953928 | Ames 34014 |
| 386 | Ames 34007 | JDC/PP/2017/052/806 | Pinus ponderosa P. Lawson & C. Lawson | Nebraska, United States | NC7 |  | | 2017 | COLLECTED | 08/29/2017 | Areas on both north and south sides of the Niobrara River between Long Pine and Springview, T32N R21W; T32N R20W; and T31N R21W in Brown and Keya Paha Counties. | 42.75716800, -99.74657300 | 685 | Dry, rocky ridgetops. | Wild material | Genetics represent the extreme eastern edgeo of the species native range. | 1953921 | Ames 34007 |
| 387 | WLP 2602 | JDC/TA/2017/053/807 | Tilia americana L. | Nebraska, United States | NA |  | | 2017 | COLLECTED | 08/29/2017 | Niobrara River Valley just 25.9 miles east, southeast of Valentine, T33N R23W Sec. 32 and Sec. 33. | 42.78284200, -100.05716700 | 658 | Floodplain and also base of adjacent bluffs/slopes (north-facing). | Wild material | Genetics represent the extreme western edge of the species native range. | 1953922 | WLP 2602 |
| 388 | Ames 34015 | Ames 34015 | Cornus rugosa Lam. | Minnesota, United States | NC7 | | | 2017 | COLLECTED | 08/23/2017 | Smoky Hills State Forest between Snellman and Osage, T139N R37W Sec. 2, 9, 11, and 14 and also T140N R37W Sec. 26 and 34. | 46.89278300, -95.35163300 | 501 | Mixed pine and deciduous moist woods. | Wild material | | 1953929 | Ames 34015 |
| 389 | NA 84645 | ZARKS-030 | Rhododendron prinophyllum (Small) Millais | Arkansas, United States | NA | | | 2017 | COLLECTED | 10/05/2014 | King's River Falls Natural Area; King's River, downstream of junction of county roads 3415 and 3500 along trail leading from parking area and trail sign. | 35.90106000, -93.57456000 | 514 | Mesic, mixed deciduous forest; growing on ledge along river, in rocky soil. | Wild material | See NA 87611 for plants of the same collection received from Morris Arboretum in 2020. | 2108758 | NA 84645 |
| 390 | NA 84577 | RJL-RM001 | Halesia diptera J. Ellis | Texas, United States | NA | | | 2017 | COLLECTED | 07/22/2017 | Along either side of a clear creek on private property approximately 1.42 kilometers north of Texas Recreational Road 255 in northeastern Jasper County. | 31.07135000, -93.94985000 | 107 | Plants growing along the embankments of the clear creek just above normal flood stage in primarily deciduous woodlands with some broadleaved evergreens and conifers. Plants are growing in part shade; some direct sunlight occurs during mid-day hours for 1-2 hours. Soils sandy and topped with a generous undisturbed decomposed litter layer. Slope: 10 percent. Aspect: variable. | Wild material | | 1953812 | NA 84577 |
| 391 | Ames 33976 | JDC/BX/2017/029/783 | Baptisia aberrans (Larisey) Weakley | Tennessee, United States | NC7 |  | | 2017 | COLLECTED | 07/07/2017 | Just east of Murfreesboro off Factory Road, Rutherford County. | 35.85458800, -86.29682300 | 207 | Remnant cedar glade recently cleared of woody vegetation resulting in flowering of numerous native plants. | Wild material | Plants in cultivation (central Iowa) measuring 0.16 m tall x 0.42 m wide with leaflets oriented in a vertical plane; petioles 2.0-3.0 mm long; leaflets 2.2-2.3 cm long and 1.1-1.2 cm wide; fertile stems 0.42 m tall with leafy branches spreading horizontally. Flowers dark purple peaking in late May (central Iowa) when grown in cultivation. | 1950059 | Ames 33976 |
| 392 | Ames 33979 | JDC/FQ/2017/031/785 | Fraxinus quadrangulata Michx. | Tennessee, United States | NC7 |  | | 2017 | COLLECTED | 07/08/2017 | Along highway 52 approximately 2.30 miles northwest of Celina, Clay County | 36.57174000, -85.53638800 | 190 | Dry, rocky soils. | Wild material | | 1950062 | Ames 33979 |
| 393 | Ames 33980 | JDC/FQ/2017/035/789 | Fraxinus quadrangulata Michx. | Kentucky, United States | NC7 |  | | 2017 | COLLECTED | 07/09/2017 | North Rolling Rock watershed and nearby tributaries approximately 3.3 miles south of Mitchellsburg, Boyle County | 37.55385900, -84.96328900 | 267 | Mixed wooded deciduous forests, including dry, rocky areas with shallow substrate, steep (65 degree +) slopes, and base of slopes, generally with underground seeps. | Wild material | | 1950063 | Ames 33980 |
| 394 | Ames 33981 | JDC/FQ/2017/036/790 | Fraxinus quadrangulata Michx. | Kentucky, United States | NC7 |  | | 2017 | COLLECTED | 07/10/2017 | Two areas sampled just south and southwest of Wilmore, including Sally Brown Preserve/Bowmans Bend on south side of Kentucky River, Garrard County and along Corman Lane approximately 0.86 miles from junction with Route 1268 on north side of Kentucky River, Jessamine County | 37.80093600, -84.70302000 | 231 | Deciduous forest, rocky substrate. | Wild material | | 1950064 | Ames 33981 |
| 395 | Ames 33987 | JDC/FQ/2017/043/797 | Fraxinus quadrangulata Michx. | Ohio, United States | NC7 |  | | 2017 | COLLECTED | 07/12/2017 | Strait Creek Prairie Bluffs Preserve between Peebles and Sinking Spring along highway 41 (Crooked Creek, Strait Creek and Scioto Brush Creek watersheds), Adams and Highland County | 39.00561100, -83.37365400 | 235 | Mixed deciduous woods, generally on top of moist seep, but also on rocky gentle (30-45 degree) slopes. | Wild material | | 1950070 | Ames 33987 |
| 396 | Ames 33988 | JDC/FQ/2017/044/798 | Fraxinus quadrangulata Michx. | Ohio, United States | NC7 |  | | 2017 | COLLECTED | 07/13/2017 | Baker Tract Preserve (Athens Conservancy) due east approximately 5.68 miles of Athens, T5N R13W SE 1/4 Sec. 16, Athens County | 39.32744200, -81.99581300 | 239 | Deciduous woods, rather steep (45 degree) slopes mostly southeast or southwest facing or found on ridge top. | Wild material | | 1950071 | Ames 33988 |
| 397 | Ames 33965 | JDC/PG/2017/013/767 | Populus grandidentata Michx. | Iowa, United States | NC7 |  | | 2017 | COLLECTED | 05/07/2017 | Private property approximately 2.98 miles west of Luther, T83N R26W NE 1/4 SE 1/4 NE 1/4 Sec. 28., Boone County | 41.97486900, -93.87548500 | 328 | Woodland. Deciduous forest. | Wild material | The native range of Populus grandidentata is concentrated througout the northeastern United States with disjunct populations in far south as Kentucky and as far west as central Iowa (Little, E. L. Jr. 1971). Bigtooth aspens are known to be fast-growing trees, making for a quick source of shade in the landscape. As a pioneer species in nature, P. grandidentata is adaptable to a wide range of environments but is considered to be slightly less adaptable than quaking aspen. However, bigtooth aspen is more resistant to canker diseases than quaking aspen (Laidly 1990), potentially making it slightly longer-lived. Bark on big-tooth aspens is generally greyish to greyish-yellow or olive-green compared to quaking aspens where bark is typically white to greyish-white. Leaves and leaf serrations are larger, and the degree of suckering is lower in big-tooth aspens. Both species are well known for their leaves to quake or tremble as the lengthy petioles allow leaves to swivel in the slightest amount of wind. Populus use is well-documented throughout the world and encompasses a wide range of products including energy feedstock, wood chips for pulping fibers, veneer logs, agro-forestry, and phyto-remediation as well as several other environmental applications. Interspecific hybrids of P. grandidentata and P. canescens have superior performance in yield; Hypoxylon canker resistance; and rooting ability compared to pure, N. American aspen genetics. This accession represents genetics acquired from the Des Moines River Valley of central Iowa and considered a disjunct population. P. grandidentata is infrequent to somewhat common throughout parts of the Des Moines River Valley, but very localized. The next closest, native population would be found in Hardin County (Iowa) approximately 50 miles to the northeast near Eldora. In central Iowa, this accession has been noted to have excellent, yellow fall color that typically peaks in mid-October (e.g. 21 October 2015). Fruits usually mature in early May (e.g. 3 May 2017) coinciding with flower initiation on local genotypes of Prunus virginiana. Specimens sampled in nature measuring approximately 60' in height and 16-22" dbh. Due to this accession originating from the western and southern edge of the species native range, it is suspected that this accession would have excellent heat and drought tolerance compared to genetics from areas in the northeastern U.S. | 1949856 | Ames 33965 |
| 398 | W6 52001 | UT933-415 | Balsamorhiza sagittata (Pursh) Nutt. | Utah, United States | W6 | | | 2017 | | | | | | | Wild material | | 1947134 | W6 52001 |
| 399 | Ames 33918 | APS/GD/2017/008/267 | Gymnocladus dioicus (L.) K. Koch | Minnesota, United States | NC7 |  | | 2017 | COLLECTED | 03/16/2017 | Minnesota River watershed covering approximately 9.0 river miles between Redwood Falls and Vicksburg Park, Renville County | 44.61447700, -95.14878600 | 254 | Mixed habitats, both upland dry sites, wet sites, and rocky sites. | Wild material | | 1946985 | Ames 33918 |
| 400 | Ames 33921 | APS/GD/2016/001/236 | Gymnocladus dioicus (L.) K. Koch | Minnesota, United States | NC7 |  | | 2017 | COLLECTED | 03/17/2017 | Blue Earth River watershed covering approximately 9.0 river miles from Vernon Center south to the county line, Blue Earth and Faribault Counties | 43.87215300, -94.17375800 | 316 | Mixed habitats, both upland dry and wet sites. | Wild material | | 1946988 | Ames 33921 |
| 401 | Ames 33909 | APS/DL/2017/002/261 | Diervilla lonicera Mill. | Iowa, United States | NC7 |  | | 2017 | COLLECTED | 02/07/2017 | Cedar Bluffs State Preserve approximately 3 miles east southeast of Tracy, T75N R17W SE 1/4 NW 1/4 Sec. 33 | 41.25648000, -92.82437000 | 235 | Deciduous woods, north facing (70-80 degrees) slope above a deep moist ravine, sandstone ledges along ravine. | Wild material | | 1946805 | Ames 33909 |
| 402 | WLP 1437 | NA 84027 | Oxydendrum arboreum (L.) DC. | Florida, United States | NA | | | 2016 | COLLECTED | 11/11/2016 | Woodlands associated with Miller Bayou, south of housing subdivision off of Pearl Court. | 30.46413000, -86.92804000 | 2 | Full sun to partial shade in mixed coniferous/broadleaved evergreen woodlands, with a mixture of deciduous plants in highly acidic sandy soils approximately 100-300 ft. from the salt marsh edge associated with Miller Bayou. | | | 1950372 | WLP 1437 |
| 403 | NA 83904 | NA 83904 | Clethra acuminata Michx. | Kentucky, United States | NA | | | 2016 | COLLECTED | 09/27/2016 | Daniel Boone National Forest, Forest Service Road 828/Route 927, Panoramic View Trail #528. | 36.84200000, -84.52900000 | 390 | Ridgetop trail. | Wild material | | 1952034 | NA 83904 |
| 404 | WLP 1180 | NA 83893 | Euonymus americanus L. | Kentucky, United States | NA | | | 2016 | COLLECTED | 09/27/2016 | Cumberland Falls State Park, Trail #6 (Cumberland Falls Trail). Stairs above visitor center entrance at Trail #6 trailhead. | 36.83700000, -84.34300000 | 273 | | | | 1951485 | WLP 1180 |
| 405 | WLP 1375 | NA 83887 | Kalmia latifolia L. | Kentucky, United States | NA | | | 2016 | COLLECTED | 09/27/2016 | Cumberland Falls State Park, Trail #6 (Cumberland Falls Trail). | 36.83700000, -84.34000000 | 302 | Break in canopy along trail near telephone pole. | | | 1953494 | WLP 1375 |
| 406 | WLP 1433 | NA 83908 | Oxydendrum arboreum (L.) DC. | Kentucky, United States | NA | | | 2016 | COLLECTED | 09/27/2016 | Daniel Boone National Forest, Forest Service Road 828/Route 927, Panoramic View Trail #528. | 36.84400000, -84.52700000 | 400 | Ridgetop trail. | | | 1951131 | WLP 1433 |
| 407 | WLP 147 | NA 83890 | Mitchella repens L. | Kentucky, United States | NA | | | 2016 | COLLECTED | 09/27/2016 | Whitley County; Cumberland Falls State Park, Trail #6 | 36.83700000, -84.34000000 | 301 | | Wild material | | 2110320 | WLP 147 |
| 408 | WLP 1700 | NA 83905 | Rhododendron cumberlandense E. L. Braun | Kentucky, United States | NA | | | 2016 | COLLECTED | 09/27/2016 | Daniel Boone National Forest, Forest Service Road 828/Route 927, Panoramic View Trail #528. | 36.84200000, -84.53000000 | 402 | Ridgetop trail, uphill side of hill. | | | 1950763 | WLP 1700 |
| 409 | WLP 1969 | NA 83888 | Vaccinium sp. | Kentucky, United States | NA | | | 2016 | COLLECTED | 09/27/2016 | Cumberland Falls State Park, Trail #6 (Cumberland Falls Trail). Open cliff edge across from bench. | 36.83700000, -84.34000000 | 308 | Open cliff edge. Sandy slope. | Wild material | | 1951081 | WLP 1969 |
| 410 | WLP 1972 | NA 83906 | Vaccinium sp. | Kentucky, United States | NA | | | 2016 | COLLECTED | 09/27/2016 | Daniel Boone National Forest, Forest Service Road 828/Route 927, Panoramic View Trail #528. | 36.84300000, -84.52800000 | 406 | Ridgetop trail. | Wild material | | 1950956 | WLP 1972 |
| 411 | Ames 33745 | UC 108 | Aronia melanocarpa (Michx.) Elliott | Tennessee, United States | NC7 |  | | 2016 | COLLECTED | 10/01/2009 | Near Caryville, Campbell County | 36.35786670, -84.21851670 | 532 | Powerline cut and surrounding area of dry and wet woods. | Wild material | This accession is rather unique as it seems to morphologically/phenologically (NCRPIS field plots) represent the "southern form" of A. melanocarpa, a potentially a new Aronia species. This southern form was originally discovered by Brand et al. 2022 (Ploidy, genetic diversity and speciation of the genus Aronia) and is known for having glabrous stems and leaves and a distinct phyllotaxy than other Aronia species. However, this accession based on Brand et al. 2022 AFLP dendogram fits with diploid A. melanocarpa, but flow cytometry indicates it is tetraploid. Fruits tend to ripen the same time as diploid A. melanocarpa and three weeks ahead of tetraploid A. melanocarpa. | 1942831 | Ames 33745 |
| 412 | Ames 33746 | UC 110a | Aronia melanocarpa (Michx.) Elliott | Tennessee, United States | NC7 |  | | 2016 | COLLECTED | 10/01/2009 | Near Newcomb, Campbell County | 36.53751670, -84.15580000 | 541 | Very dry, exposed rock spine with primarily organic soil and plants growing in cracks and pockets. Growing in association with Pinus virginiana, Quercus, Vaccinium, Gaylussacia, Castanea, Amelanchier, Magnolia ashei, Magnolia tripetala, Oxydendrum, Nyssa, Liquidambar styraciflua. | Wild material | This accession has been confirmed to represent the "southern form" of A. melanocarpa, potentially a new Aronia species. This southern form was originally discovered by Brand et al. 2022 (Ploidy, genetic diversity and speciation of the genus Aronia) and is known for having glabrous stems and leaves and a distinct phyllotaxy than other Aronia species. In addition, plants tend to bloom approximately two weeks later than all other Aronia taxonomic groups and the inflorescences/infructescences are more spreading and extended due to longer peduncles and pedicels within the cyme. Fruit maturity tends to occur 2 to 4 weeks later than tetraploid A. melanocarpa and 4 to 6 weeks later than diploid A. melanocarpa. Phenolic levels are much higher in comparison to other A. melanocarpa accessions (Brand et al., 2017 - Anthocyanins, total phenolics, ORAC and moisture content of wild and cultivated dark-fruited Aronia species.) | 1942832 | Ames 33746 |
| 413 | W6 51565 | CBG-4001 | Dicentra cucullaria (L.) Bernh. | Illinois, United States | W6 | | | 2016 | | | | | | | Wild material | | 1942695 | W6 51565 |
| 414 | Ames 33736 | JDC/BA/2016/028/743 | Betula alleghaniensis Britton | Iowa, United States | NC7 |  | | 2016 | COLLECTED | 09/02/2016 | Fallen Rock State Preserve approximately 1.9 miles southwest of Steamboat Rock, T88N R19W NW ¼ Sec. 32. | 42.39459000, -93.09423600 | 310 | High-quality, native, mesic deciduous woods on loose, loamy sandstone amongst very large boulders. North-facing with variable 10-50 degree slopes. Majority of specimens located at base of bluff or near water’s edge (Iowa River). | Wild material | The native range of Betula alleghaniensis is concentrated in the northeastern U.S. with disjunct populations in Iowa (Little, 1971). This accession represents a collection of Betula alleghaniensis germplasm from the extreme western edge of the species native range. The next closest occurrence is in Mitchell County, Iowa (60 miles). As of 2025, two trees at Fallen Rock State Preserve currently represent the state of Iowa's 1st and 2nd largest yellow birch specimens measuring 22.76" DBH; 70.83' height; 40' average crow spread (151.83 points) and 17.18" DBH; 65.33' height; 33.75' average crow spread (127.76 points), respectively (Rouw, M., personal communication, 13 May 2018). | 1942689 | Ames 33736 |
| 415 | Ames 33735 | PB16014001 | Betula papyrifera Marshall | North Dakota, United States | NC7 |  | | 2016 | COLLECTED | 08/18/2016 | Bottineau County, North Dakota: Turtle Mountains located approximately 11 miles north, northeast of Bottineau. T163N R74W N1/2 Sec. 16 and T163N R75W NW 1/4 NW 1/4 and also NW 1/4 NE 1/4 Sec. 5. | 48.96006100, -100.31819400 | 700 | Mixed upland forest and wetlands. Growing in association with Quercus macrocarpa, Populus balsamifera, Populus tremuloides, Fraxinus pennsylvanica, Amelanchier sp., Symphoricarpos albus, Corylus sp., Prunus virginiana, Rubus sp., Viburnum opulus var. americanum, and Cirsium arvense. | Wild material | | 1942686 | Ames 33735 |
| 416 | Ames 33363 | JDC/MB/2016/022/737 | Monarda bradburiana L. C. Beck | Missouri, United States | NC7 | | | 2016 | COLLECTED | 06/28/2016 | Spring Creek Gap Conservation Area approximately 3.54 miles northwest of Vichy, T39N R8W Sec. 4, Maries County. | 38.14201800, -91.81278200 | 209 | Cedar glade remnant. | Wild material | | 1940865 | Ames 33363 |
| 417 | NA 83681 | Ron Miller 08302014 | Viburnum obovatum Walter | Florida, United States | NA | | | 2016 | COLLECTED | 08/30/2014 | Along Holmes Creek not far from the boat ramp on Hightowers Road. | 30.60560000, -85.76490000 | 5 | Boggy edge of creek in mixed deciduous and evergreen bottomland woodlands that are periodically inundated for extended periods. | Wild material | | 1951230 | NA 83681 |
| 418 | Ames 33289 | APS/GD/2016/010/245 | Gymnocladus dioicus (L.) K. Koch | Michigan, United States | NC7 |  | | 2016 | COLLECTED | 04/05/2016 | Ionia County: T5N R5W SW 1/4 SW 1/4 SE 1/4 Sec. 21; T5N R5W NE 1/4 NW 1/4 NW 1/4 Sec. 20; and T5N R5W SW 1/4 SW 1/4 SE 1/4 Sec. 20 along Grand River approximately 4.80 miles south and slightly west of Portland. | 42.80296200, -84.91275400 | 231 | Floodplain. | Wild material | | 1940346 | Ames 33289 |
| 419 | Ames 33290 | APS/GD/2016/012/247 | Gymnocladus dioicus (L.) K. Koch | Michigan, United States | NC7 |  | | 2016 | COLLECTED | 04/06/2016 | Gratiot and Clinton Counties: T9N R3W SW 1/4 Sec. 35 (Gratiot County) and T8N R4W NW 1/4 NW 1/4 Sec. 14 (Clinton County) along Maple River both northeast (approximately 3.34 miles (Clinton County)) and southwest (approximately 3.00 miles (Gratiot County)) of Maple Rapids. | 43.10603700, -84.70504200 | 205 | Floodplain. | Wild material | | 1940347 | Ames 33290 |
| 420 | Ames 33229 | JDC/SO/2016/001/716 | Symphoricarpos orbiculatus Moench | Missouri, United States | NC7 | | | 2016 | COLLECTED | 01/13/2016 | Access road near Scobee Lake, NE 1/4 of NE 1/4 of Section 32, T64N R16W, approximately 10.5 miles northwest of Kirksville, Adair County. | 40.30655000, -92.71615200 | | | Wild material | Plants approximately 4 feet in height. Fruits red in color. Variation noted in fruits ranging from bright red to dark red in color. | 1936479 | Ames 33229 |
| 421 | Ames 33220 | NA 82306 | Spiraea tomentosa L. | Maryland, United States | NC7 | | | 2015 | COLLECTED | 10/17/2012 | Along Powell Road, Chesapeake Forest Public Hunting Area, Wicomico State Forest, between Sixty Foot Road and Morris Road, Wicomico County. | 38.35340000, -75.41360000 | 12 | Roadside. Upland forest edge. | Wild material | | 1932218 | Ames 33220 |
| 422 | Ames 32959 | JDC/FN/2015/045/702 | Fraxinus nigra Marshall | Iowa, United States | NC7 | | | 2015 | COLLECTED | 09/11/2015 | Ruby Woodland, T88N R19W NW 1/4 Sec. 8 Hardin County. | 42.45105400, -93.09686700 | 318 | Mid portions of north-facing slope (45 degrees) in cool, moist deciduous woods. Growing in association with Betula papyrifera, Staphylea trifolia, Carpinus caroliniana, Quercus rubra, Fraxinus americana, Acer saccharum, Cornus alternifolia, Carya ovata, Urtica dioica, Amelanchier arborea, Ostrya virginiana, Hepatica sp., and Allium tricoccum. | Wild material | | 1927429 | Ames 32959 |
| 423 | Ames 32960 | JDC/BP/2015/046/703 | Betula papyrifera Marshall | Iowa, United States | NC7 | | | 2015 | COLLECTED | 09/11/2015 | Ruby Woodland, T88N R19W NW 1/4 Sec. 8 Hardin County. | 42.45099600, -93.09671200 | 328 | Mid portions of north-facing slope (45-60 degrees) in cool, moist deciduous woods. Growing in association with Fraxinus nigra, Staphylea trifolia, Carpinus caroliniana, Quercus rubra, Fraxinus americana, Acer saccharum, Cornus alternifolia, Carya ovata, Urtica dioica, Amelanchier arborea, Ostrya virginiana, Hepatica sp., Smilax rotudifolia, Prunus Virginiana, Betula papyrifera, Betula alleghaniensis, Populus deltoides, Tilia americana, and Allium tricoccum. | Wild material | | 1927430 | Ames 32960 |
| 424 | Ames 32963 | JDC/BA/2015/049/706 | Betula alleghaniensis Britton | Iowa, United States | NC7 | | | 2015 | COLLECTED | 09/14/2015 | Bixby State Preserve, T91N R5W extreme southern edge of Sec. 23 basically restricted to W 1/2 of Sec. 23. | 42.67470300, -91.39917300 | 308 | North-facing algific talus slope (45-60 degrees) adjacent to Bear Creek. Moist deciduous woods. Growing in association with Diervilla lonicera, Hamamelis virginiana, Corylus sp., Viburnum opulus var. americanum, Cornus rugosa (few), Cornus alternifolia, Fraxinus nigra, Quercus rubra, Viburnum lentago, Ribes sp., Rubus idaeus subsp. strigosus, Rhamnus alnifolia (few), Rosa sp., Taxus canadensis, Prunus virginiana, Impatiens sp., Dirca palustris, and Pinus strobus (few). | Wild material | | 1927433 | Ames 32963 |
| 425 | Ames 32965 | JDC/BA/2015/051/708 | Betula alleghaniensis Britton | Iowa, United States | NC7 | | | 2015 | COLLECTED | 09/15/2015 | Yellow River State Forest, T97N R4W northern edge of SW 1/4 NW 1/4 Sec. 36 | 43.17782100, -91.26584600 | 227 | North-facing algific talus slope (45-60 degrees) adjacent to Paint Creek. Moist deciduous woods. Growing in association with Fraxinus nigra, Staphylea trifolia, Carpinus caroliniana, Quercus rubra, Acer saccharum, Cornus alternifolia, Amelanchier arborea, Ostrya virginiana, Viburnum opulus var. americanum, Cornus rugosa, Cornus alternifolia, Zanthoxylum americanum, Viburnum rafinesqueanum, Cypripedium pubescens, Ribes sp.,Corylus sp., Juniperus virginiana, Dirca palustris, Ulmus thomasii, Prunella vulgaris, Diervilla lonicera, Quercus macrocarpa, Carya cordiformis, Taxus canadensis, Tilia americana, Adiantum pedatum, and Aconitum noveboracense. | Wild material | | 1927435 | Ames 32965 |
| 426 | Ames 32966 | JDC/VA/2015/052/709 | Viburnum opulus L. var. americanum Aiton | Iowa, United States | NC7 |  | | 2015 | COLLECTED | 09/15/2015 | Yellow River State Forest, T97N R4W northern edge of SW ¼ NW ¼ Sec. 36. | 43.17778200, -91.26642800 | 239 | North-facing algific talus slope (45-60 degrees) adjacent to Paint Creek. Moist deciduous woods. | Wild material | Formerly known as Viburnum trilobum, American highbush cranberry (V. opulus var. americanum) is a North American native shrub that is utilized as an important ornamental and conservation plant that is also harvested as a minor fruit crop (jams/jellies). In nature, this variety is generally found in moist habitats typically along stream banks and swamps where ample moisture is readily available. The native range of V. opulus var. americana is concentrated in the northeastern United States and into Canada (Little, E. L. Jr. 1977). Attractive ornamental characteristics includes showy lacecap flowers in spring and bright red fruits and foliage in the fall. Fruits are tart with a hint of sweetness. The European highbush cranberry (V. opulus var. opulus) is nearly identical to American highbush cranberry other than small glands (<1 mm) on the petiole making the exact determination very challenging resulting in common misidentifications. A major difference between the American and European highbush cranberries is that the European variety produces unpalatable fruit. Recent research has shown that American and European highbush cranberries are genetically distinct and that plants of hybrid origin are uncommon (Tork et al. 2025). Vigorous early spring growth and good tolerance to late spring frosts. Genetic analysis from Tork et al. 2025 confirmed that genetics of this accession represents American highbush Cranberry (Viburnum opulus var. americanum). This accession represents genetics from northeast Iowa and thus the extreme western edge of the species native range. | 1927436 | Ames 32966 |
| 427 | NA 82746 | Site 3B/Hightower Road at Holmes Creek | Magnolia ashei Weath. | Florida, United States | NA | | | 2015 | COLLECTED | 07/31/2015 | Along Holmes Creek 0.2 miles west-southwest of Hard Castle Landing boat ramp at hte end of Hightower Road. | 30.60401000, -85.76883000 | 11 | Shade to partial shade of deciduous woodlands 10 to 15 feet above the creek, surrounded by low lying swampy area. | Wild material | Originally just called Site 3, but the "A/B" has been added to distinguish the Live Oak Landing (3A) and Hightower Road (3B) material. For previous collections of this population, see NA 81556 (2013); for later collection, see NA 82746.01 (2019). | 1950860 | NA 82746 |
| 428 | WLP 699 | NA 82755 | Amelanchier spicata (Lam.) K. Koch | Maine, United States | NA | | | 2015 | COLLECTED | 07/07/2015 | Roadside near the parking area for Bluberry Barrens (also known as Kennebunk Plains), ca. 4.5 miles west of Kennebunk. | 43.40231000, -70.62462000 | | Roadside, along shoulder of road. | | | 1952492 | WLP 699 |
| 429 | WLP 683 | JDC/AA/2015/040/697 | Amelanchier arborea (F. Michx.) Fernald | Iowa, United States | NA |  | | 2015 | COLLECTED | 06/16/2015 | Elk Rock State Park approximately 6.25 miles north of Knoxville. Extreme northern point of park. T76N R19W SW 1/4 SW 1/4 Sec. 5 Marion County | 41.40879000, -93.07958000 | 219 | Relatively steep, north-facing slopes (55 degrees). Growing in association with Diervilla lonicera (rare), Tilia americana (large and abundant), Rosa multiflora, Lonicera maackia, Eleagnus umbellata, Quercus rubra, Viburnum rafinesqueanum, Sanguinaria canadensis, Staphylea trifolia, and Ostrya virginiana. | Wild material | Fruits harvested at peak maturity. Numerous fruits were soft and/or dropped when distrurbed. Fruit color ranged from dark red with tinge of blue/purple to light red. Fruit diameter averaged 10.28 mm (0.83 stdev), range min 9.00 mm to max 12.00 mm (random sample of 20 fruits). Stalk length (fruits) averaged 22.08 mm (5.28 stdev), range min 13.89 mm to max 35.00 mm (random sample of 20 fruits with intact stalks). | 1926845 | WLP 683 |
| 430 | Ames 32923 | JDC/FQ/2015/038/694 | Fraxinus quadrangulata Michx. | Oklahoma, United States | NC7 |  | | 2015 | COLLECTED | 05/22/2015 | T19 R12E N 1/4 Sec. 18 and extreme SE 1/4 Sec. 7 Tulsa County. Chandler Park. | 36.13235400, -96.07376000 | 264 | Rocky, very shallow soils on north and northwest-facing slopes. Growing in association with Fraxinus americana, Cotinus obovatus, Celtis sp., Cornus sp., Ulmus sp., Cercis canadensis, Juniperus virginiana, Quercus muehlenbergii, Smilax sp., Toxicodendron radicans, Quercus texana, and Quercus stellata (chlorotic). | Wild material | | 1926265 | Ames 32923 |
| 431 | WLP 1096 | JDC/CO/2015/025/681 | Cotinus obovatus Raf. | Missouri, United States | NA |  | | 2015 | COLLECTED | 05/19/2015 | T24N R16W NW 1/4 Sec. 4, SW 1/4 SW 1/4 Sec. 17, and SW 1/4 Sec. 9 Ozark County. Mark Twain National Forest Caney Picnic Area (County Road 935) | 36.79873000, -92.71575700 | 407 | Rocky, very shallow soils. Growing in association with Quercus muehlenbergii, Diospyros virginiana, Cercis canadensis, Viburnum rufidulum, Delphinium carolinianum, Penstemon cobea, Rudbeckia sp., Fraxinus americana, Fraxinus quadrangulata (few), Cornus florida, Oenothera macrocarpa, Juniperus virginiana, Tradescantia sp., and Silphium terebinthinaceum. | Wild material | | 1926254 | WLP 1096 |
| 432 | WLP 1097 | JDC/CO/2015/026/682 | Cotinus obovatus Raf. | Missouri, United States | NA | | | 2015 | COLLECTED | 05/19/2015 | T22N R20W N1/2 Sec. 33 and SW 1/4 Sec. 27 Taney County. Gunnison Road, adjacent to Bee Creek, a tributary to Fox Creek and also surrounding area. | 36.52401500, -93.09755700 | 350 | Steep, west-facing slope on rocky, loose substrate. Growing in association with Fraxinus quadrangulata, Quercus muehlenbergii, Hydrangea arborescens, Physocarpus opulifolius, Viburnum rufidulum, Cornus florida, Carpinus caroliniana (abundant), Rhus aromatica, Lonicera sp. (vine), Cornus sp., Salix sp., Juniperus virginiana, Tilia americana, Hamamelis sp. (abundant) and Staphylea trifolia. | Wild material | | 1926259 | WLP 1097 |
| 433 | WLP 1098 | JDC/CO/2015/030/686 | Cotinus obovatus Raf. | Arkansas, United States | NA |  | | 2015 | COLLECTED | 05/20/2015 | T18N R15W NW 1/4 Sec. 15 and SE 1/4 Sec. 10 Marion County. Hall Mountain area along County Road 6074. | 36.20574400, -92.56150900 | 239 | Rocky, very shallow soils. Growing in association with Quercus muehlenbergii, Juniperus virginiana, Acer saccharum, Cercis canadensis, Lindera benzoin, Diospyros virginiana, Silphium terebinthinaceum, Baptisia sp., Rudbeckia sp., and Rhus glabra. | Wild material | | 1926260 | WLP 1098 |
| 434 | WLP 1099 | JDC/CO/2015/031/687 | Cotinus obovatus Raf. | Arkansas, United States | NA |  | | 2015 | COLLECTED | 05/20/2015 | T16N R10W SW 1/4 Sec. 35 and SE 1/4 Sec. 34 and also T15N R10W S 1/2 Sec. 3 Izard County. Brandenburg Mountain area, along highway 9 between Allison and Melbourne. | 35.99358500, -92.02874700 | 170 | Rocky, very shallow soils. Growing on both north, southeast, and west-facing slopes in association with Quercus muehlenbergii, Quercus stellata, Juniperus virginiana, Cercis canadensis, Delphinium carolinianum, Echinacea sp., Fraxinus americana, and Yucca sp. | Wild material | | 1926261 | WLP 1099 |
| 435 | WLP 1100 | JDC/CO/2015/034/690 | Cotinus obovatus Raf. | Arkansas, United States | NA | | | 2015 | COLLECTED | 05/21/2015 | T10N R20W SE 1/4 NW 1/4 Sec. 6 Pope County. Long Pool Recreation Area between Big Piney Creek and Newton Hill. | 35.54962900, -93.15052600 | 229 | Rocky, likely somewhat acidic substrate on north-facing slopes. Growing in association with Acer saccharum, Juniperus virginiana, Vaccinum sp., Quercus stellata, Rhododendron spp, Viburnum rufidulum, Castanea ozarkensis, Amelanchier sp., Ostrya virginiana, Nyssa sylvatica, Quercus alba, and Pinus sp.. | Wild material | | 1926262 | WLP 1100 |
| 436 | WLP 1101 | JDC/CO/2015/036/692 | Cotinus obovatus Raf. | Oklahoma, United States | NA |  | | 2015 | COLLECTED | 05/21/2015 | T16N R20E W 1/2 Sec. 18 Wagoner and Cherokee Counties. Fort Gibson Lake Dam. | 35.86228100, -95.22575600 | 170 | Growing on shallow, rocky soils in association with Carya illinoinensis, Quercus muehlenbergii, Cornus sp., Cercis canadensis, Fraxinus americana, Platanus occidentalis, Ulmus sp., Diospyros virginiana, Sapindus saponaria var. drummondii, Lonicera sempervirens, Smilax sp., Toxicodendron radicans, and Robinia pseudoacacia. | Wild material | | 1926263 | WLP 1101 |
| 437 | WLP 1102 | JDC/CO/2015/037/693 | Cotinus obovatus Raf. | Oklahoma, United States | NA |  | | 2015 | COLLECTED | 05/22/2015 | T19 R12E N 1/4 Sec. 18 and extreme SE 1/4 Sec. 7 Tulsa County. Chandler Park. | 36.13366000, -96.06623100 | 264 | Rocky, very shallow soils on north and northwest-facing slopes. Growing in association with Fraxinus americana, Fraxinus quadrangulata, Celtis sp., Cornus sp., Ulmus sp., Cercis canadensis, Juniperus virginiana, Quercus muehlenbergii, Smilax sp., Toxicodendron radicans, Quercus texana, and Quercus stellata (chlorotic). | Wild material | | 1926264 | WLP 1102 |
| 438 | OPGC 6167 | CBG-2811 | Ruellia humilis Nutt. | Illinois, United States | OPGC |  | | 2015 | | | | | | | Wild material | | 1926146 | OPGC 6167 |
| 439 | W6 49517 | CBG-2452 | Koeleria macrantha (Ledeb.) Schult. | Illinois, United States | W6 |  | | 2015 | | | | | | | Wild material | | 1925997 | W6 49517 |
| 440 | NA 82643 | NA 82643 | Lonicera sempervirens L. | Texas, United States | NA | | | 2015 | COLLECTED | 07/20/2014 | East side of Texas Route 87 approximately 0.52 miles south of Trout Creek, Texas. | 30.61156000, -93.80506000 | 21 | Southwest-facing edge of mature woodland in part to full sun; well-drained, seasonally moist soils that are sandy loam; surface has an excellent organic litter layer. | | | 1952603 | NA 82643 |
| 441 | NA 82646 | NA 82646 | Nyssa ogeche W. Bartram ex Marshall | Florida, United States | NA | | | 2015 | COLLECTED | 07/20/2014 | Along Holmes Creek approximately 0.7 miles east of the Hightower Road boat camp. | 30.60636000, -85.75341000 | 6 | On Holmes Creek on a muddy flat along spring-fed stream. | | | 1952137 | NA 82646 |
| 442 | Ames 32894 | APS/GD/2015/017/199 | Gymnocladus dioicus (L.) K. Koch | Oklahoma, United States | NC7 |  | | 2015 | COLLECTED | 03/14/2015 | Cleveland County: T10N R5W SW 1/4 SW 1/4 Sec. 7. John Nichols Camp located on north side of Canadian River approxiamtely 4.25 miles south and southeast of Mustang. | 35.35029600, -97.66952200 | 395 | Higher elevations. Dry, relatively thin soils. | Wild material | | 1925360 | Ames 32894 |
| 443 | Ames 32895 | APS/GD/2015/018/200 | Gymnocladus dioicus (L.) K. Koch | Oklahoma, United States | NC7 |  | | 2015 | COLLECTED | 03/15/2015 | Canadian County: Near/adjacent to unnamed creek that empties into the Canadian River, T12N R10W SW 1/4 Sec. 20. Private property approximately 4 miles northeast of Hinton. | 35.49409300, -98.28655400 | 434 | Bottomland. | Wild material | | 1925361 | Ames 32895 |
| 444 | Ames 32902 | APS/GD/2015/030/212 | Gymnocladus dioicus (L.) K. Koch | Oklahoma, United States | NC7 |  | | 2015 | COLLECTED | 03/18/2015 | Logan County: T18N R2W N 1/2 Sec. 36. Private property approximately 1.5 miles east of the confluence of Skeleton Creek and Cimarron River approximately 5.25 miles south southeast of Mulhall. | 35.99593500, -97.36486800 | 288 | Transition zone between higher elevations and bottomlands. | Wild material | | 1925368 | Ames 32902 |
| 445 | Ames 32903 | APS/GD/2015/031/213 | Gymnocladus dioicus (L.) K. Koch | Oklahoma, United States | NC7 |  | | 2015 | COLLECTED | 03/19/2015 | Osage County: Arkansas River watershed area known as Souters Bend, T21N R7E. Keystone Wildlife Management Area (John Lowery Unit) approximatley 3 miles west of Cleveland. | 36.30185300, -96.53051000 | 222 | Floodplain, but one specimen sampled was located on dry, rocky (large boulders) bluff. | Wild material | | 1925369 | Ames 32903 |
| 446 | Ames 32904 | APS/GD/2015/032/214 | Gymnocladus dioicus (L.) K. Koch | Oklahoma, United States | NC7 |  | | 2015 | COLLECTED | 03/19/2015 | Osage County: Sand Creek watershed area, T27N R8E SE 1/4 NW 1/4 Sec. 10. Tallgrass Prairie Preserve approximately 13 miles northwest of Pawhuska. | 36.83425300, -96.43091600 | 307 | Dry, rocky outcroppings and floodplain. | Wild material | | 1925370 | Ames 32904 |
| 447 | NA 83060 | NA 83060 | Prunus hortulana L. H. Bailey | | NA | | | 2015 | | | | | | | | | 1950570 | NA 83060 |
| 448 | NA 83068 | NA 83068 | Philadelphus pubescens Loisel. | Arkansas, United States | NA | | | 2015 | COLLECTED | 10/06/2014 | Mount Magazine State Park; Brown's Spring Picnic Area trail. | 36.16768000, -93.66583000 | 796 | Moist bluff line community, growing in moist organic soil layer over rocks. | | | 1952927 | NA 83068 |
| 449 | Ames 34697 | MARSB-080 | Cornus amomum Mill. | Pennsylvania, United States | NC7 |  | | 2015 | COLLECTED | 09/11/2013 | Allegheny National Forest -Minister Creek watershed just south of Minister. | 41.61593000, -79.15109000 | 369 | | Wild material | | 1922851 | Ames 34697 |
| 450 | Ames 34289 | MARSB-090 | Rhus copallinum L. | New York, United States | NC7 |  | | 2015 | COLLECTED | 09/26/2013 | Great Kills Park near Oakwood Beach. | 40.55428000, -74.10738000 | 3 | | Wild material | | 1922928 | Ames 34289 |
| 451 | W6 48845 | MARSB-58 | Danthonia spicata (L.) P. Beauv. ex Roem. & Schult. | New York, United States | W6 |  | | 2015 | | | | | | | Wild material | | 1922913 | W6 48845 |
| 452 | W6 48848 | MARSB-057 | Avenella flexuosa (L.) Parl. | New York, United States | W6 |  | | 2015 | | | | | | | Wild material | | 1922914 | W6 48848 |
| 453 | Ames 32847 | JDC/DL/2014/150/653 | Diervilla lonicera Mill. | Iowa, United States | NC7 |  | | 2014 | COLLECTED | 11/23/2014 | Wild Cat Den State Park located approximately 9.00 miles northeast of Muscatine, T77N R1E SW 1/4 SW 1/4 and also SE 1/4 SW 1/4Sec. 17 | 41.46820900, -90.87994300 | 215 | Mixed decidous woods. Northeast and east-facing, extremely steep slopes on loose soils. | Wild material | | 1921868 | Ames 32847 |
| 454 | Ames 32849 | JDC/DL/2014/151/654 | Diervilla lonicera Mill. | Iowa, United States | NC7 | | | 2014 | COLLECTED | 11/23/2014 | Fern Cliff County Park located approximatley 3.75 miles west, southwest of Crawfordsville, T74N R7W southern edge of N 1/2 Sec. 24 | 41.19958700, -91.60874700 | 208 | Steep north-facing slopes on loose soils. | Wild material | | 1921870 | Ames 32849 |
| 455 | Ames 32835 | GA14014001 | Fraxinus pennsylvanica Marshall | North Dakota, United States | NC7 |  | | 2014 | COLLECTED | 10/30/2014 | Bottineau County, Turtle Mountains. | 48.97000000, -100.45000000 | 737 | Mixed oak-aspen forest | Wild material | | 1921828 | Ames 32835 |
| 456 | WLP 1746 | Ames 32838 | Viburnum opulus L. var. americanum Aiton | North Dakota, United States | NA | | | 2014 | COLLECTED | 10/31/2014 | Turtle Mountains - Bottineau County. | 48.95000000, -100.43000000 | 692 | Wet, aspen forest. Growing in association with Sanicula marilandica, Fragaria virginiana, Trifolium repens, Rubus sp., Typha latifolia, Prunus pensylvanica, Prunus virginiana, Corylus sp., Crataegus sp., Viburnum lentago, Rosa sp., Cornus sericea, Amelanchier sp., Symphoricarpos sp., Salix sp., Betula papyrifera, Populus tremuloides, Ulmus americana, Acer negundo, Quercus macrocarpa, and Fraxinus pennsylvanica. | Wild material | | 1921831 | WLP 1746 |
| 457 | WLP 1967 | HBC1401 | Viburnum opulus L. var. americanum Aiton | North Dakota, United States | NA | | | 2014 | COLLECTED | 09/29/2014 | Jay Wessels Wildlife Management Area located in Pembina County. | 48.80000000, -97.83000000 | 312 | Diverse habitats including edge of swamp and also upland sandy soils. Growing in association Fraxinus pennsylvanica, Fraxinus nigra, Quercus macrocarpa, Acer negundo, Ulmus americana, Populus tremuloides, Populus balsamifera, Toxicodendron radicans, Cornus sericea, Rosa sp., Corylus sp., Prunus virginiana, Ribes sp., Equisetum sp., Rubus sp., IMpatiens capensis, Thalictrum dasycarpum, Fragaria virginiana, Asarum canadense, Calamagrostis canadensis, Sium suave, Solidago gigantea, Poa pratensis, and Bromus inermis. | Wild material | | 1921830 | WLP 1967 |
| 458 | Ames 32826 | JDC/DL/2014/148/651 | Diervilla lonicera Mill. | Iowa, United States | NC7 |  | | 2014 | COLLECTED | 11/04/2014 | Elk Rock State Park (extreme northern point of park) approximately 6.25 miles north of Knoxville, T76N R19W SW 1/4 SW 1/4 Sec. 5 | 41.40879000, -93.07958000 | 219 | Extremely steep, north-facing slopes. | Wild material | | 1921786 | Ames 32826 |
| 459 | Ames 32822 | JDC/DL/2014/139/642 | Diervilla lonicera Mill. | Iowa, United States | NC7 |  | | 2014 | COLLECTED | 10/28/2014 | Clayton Road (C17) approximately 0.25 mile west of Kestrel Road, 1.50 miles east of Garnavillo on a steep north-facing slope T93N R3W near center of NW 1/4 Sec. 16 and also at the end of 250th Street approximatley 2.25 miles east of Garnavillo on a steep north, northwest-facing slope of Buck Creek watershed T93N R3W SE 1/4 SE 1/4 SE 1/4 Sec. 16 | 42.87344100, -91.20649600 | 264 | | Wild material | | 1921782 | Ames 32822 |
| 460 | Ames 32820 | APS/EA/2013/041/126 | Euonymus atropurpureus Jacq. | Iowa, United States | NC7 |  | | 2014 | COLLECTED | 10/10/2014 | Midland Trail Road near North Racoon River watershed. Dallas County T80N R27W SW 1/4 NW 1/4 Sec. 30 | 41.71142000, -94.04538000 | 299 | Wooded roadside. | Wild material | | 1921780 | Ames 32820 |
| 461 | NA 82043 | JDC/AP/2014/063/565 | Aesculus pavia L. | Arkansas, United States | NA |  | | 2014 | COLLECTED | 09/20/2014 | St. Francis National Forest. | 34.68710800, -90.67734100 | 108 | Deciduous woods. Valleys, slopes, and ridges. | Wild material | Collected as Aesculus parviflora and initially accessioned under that name. Renamed to A. pavia based on ID by Pablo Jourdan (Director, Ornamental Plant Germplasm Center at Ohio State University). | 1922344 | NA 82043 |
| 462 | WLP 1093 | JDC/CF/2014/097/599 | Cornus florida L. | Alabama, United States | NA | | | 2014 | COLLECTED | 09/23/2014 | Alabama: Winston County; William B. Bankhead National Forest along County Road 8. | 34.06143000, -87.31290200 | 211 | Growing in association with Quercus sp., Pinus sp., and Diospyros virginiana. | Wild material | Variation in fruit size noticed across specimens sampled. | 1922368 | WLP 1093 |
| 463 | WLP 1251 | JDC/HQ/2014/067/569 | Hydrangea quercifolia W. Bartram | Mississippi, United States | NA |  | | 2014 | COLLECTED | 09/21/2014 | Mississippi: Lafayette County; Holly Springs National Forest along County Road 244. | 34.51468900, -89.45669300 | 132 | Deciduous woods. Higher elevation than surrounding area. East, northeast-facing 45 degree slope. Growing in association with Cornus florida, Nyssa sylvatica, Quercus alba, Pinus sp., Liquidambar styraciflua, Juniperus virginiana, Carya tomentosa, and Rhus typhina. | Wild material | Numerous specimens. Attractive peeling bark and large (10" long) infructescences. | 1922345 | WLP 1251 |
| 464 | WLP 1252 | JDC/HQ/2014/084/586 | Hydrangea quercifolia W. Bartram | Mississippi, United States | NA |  | | 2014 | COLLECTED | 09/22/2014 | Mississippi: Tishomingo County; Extreme northeast corner of Tishomingo County near J.P. Coleman State Park. | 34.98857300, -88.20347900 | 194 | Steep (60-70 degrees), north, northeast-facing slope. Growing in association with Quercus montana (abundant), Hamamelis sp., Quercus alba, Rhododendron arborescens, Amelanchier sp., Ostrya virginiana, Vaccinum sp., and Vitis sp. | Wild material | Numerous specimens. Some specimens approximately 6-7' in height. | 1922357 | WLP 1252 |
| 465 | WLP 1253 | JDC/HQ/2014/090/592 | Hydrangea quercifolia W. Bartram | Alabama, United States | NA |  | | 2014 | COLLECTED | 09/23/2014 | Alabama: Lawrence County; Near Franklin and Lawrence County line off County Road 303. | 34.33701600, -87.52906200 | 332 | Growing in association with Quercus alba, Quercus montana, Cornus florida, Rhus glabra, Liriodendron tulipifera, Pinus virginiana, Pinus sp., Acer rubrum, and Frangula alnus. | Wild material | Some specimens with infructescences averaging 12" in length. | 1922364 | WLP 1253 |
| 466 | WLP 1304 | JDC/IF/2014/101/603 | Illicium floridanum J. Ellis | Alabama, United States | NA | | | 2014 | COLLECTED | 09/24/2014 | Alabama: Lamar County; Banks of Clear Creek between Millport and Kennedy near Alabama Highway 96. | 33.56897100, -88.02468300 | 111 | Wet, deciduous woods. Growing in association with Magnolia virginiana, Betula nigra, and Quercus nigra. | Wild material | Species locally abundant. Abundant fruit production. | 1922371 | WLP 1304 |
| 467 | WLP 1422 | JDC/NS/2014/068/570 | Nyssa sylvatica Marshall | Mississippi, United States | NA | | | 2014 | COLLECTED | 09/21/2014 | Mississippi: Lafayette County; Holly Springs National Forest along County Road 244. | 34.50982900, -89.35716800 | 95 | Floodplain. Wet woods. Growing in association with Liquidambar styraciflua, Acer negundo, Cetlis sp., Juniperus virginiana, Carya illinoinensis, Quercus nigra, and Quercus phellos. | Wild material | Fruits rather green. | 1922346 | WLP 1422 |
| 468 | WLP 689 | BJP/AI/2014/001 | Amelanchier intermedia Spach | Maine, United States | NA | | | 2014 | COLLECTED | 07/17/2014 | Woods at the edge of a small cemetery on Pigeon Hill Road, just east of its intersection with Main Street (Hwy. 1), approximately .2.5 miles southwest of Milbridge. | 44.51051000, -67.91188000 | | Woods at the edge of a small cemetery. | Wild material | | 1922791 | WLP 689 |
| 469 | WLP 700 | BJP/AS/2014/002 | Amelanchier spicata (Lam.) K. Koch | New Hampshire, United States | NA | | | 2014 | COLLECTED | 07/03/2014 | Rye: West side of Ocean Boulevard in Rye, on shoulder of road. | 43.01886000, -70.73382000 | | Plants on shoulder of road adjacent to marshy field. | Wild material | Full name as recorded at the U.S. National Arboretum: Amelanchier spicata (''maritima''). Received as Amelanchier spicata ''maritima.'' | 1922824 | WLP 700 |
| 470 | Ames 32760 | JDC/AB/2014/040/542 | Abies balsamea (L.) Mill. | Iowa, United States | NC7 | | | 2014 | COLLECTED | 09/03/2014 | Bluffton Fir State Preserve, near Bluffton, Winneshiek County. | 43.40106767, -91.90659200 | 326 | High quality, native woods. Steep slope, northwest-facing, and relatively flat portion on top of bluff (powerline) | Wild material | | 1921308 | Ames 32760 |
| 471 | Ames 32758 | Fallen Rock | Pinus strobus L. | Iowa, United States | NC7 |  | | 2014 | COLLECTED | 08/21/2014 | Fallen Rock State Preserve and adjacent private property just north of Eldora, T88N R19W SW ¼ Sec. 28 and N ¼ Sec. 32 and also T87N R19W N ½ Sec. 5. | 42.39548900, -93.09165200 | 311 | Cool moist woods. Slopes averaging 60 degrees. Northern and eastern aspects. Localized to bluffs above Iowa River. | Wild material | The native range of Pinus strobus is concentrated in the northeastern United States extending south into the northern edge of Georgia and west to central Minnesota. In Iowa, scattered native populations exist in a few northeastern counties as well as small disjunct populations in central and southeastern counties (Little, 1971). This accession includes genetics from legacy mother trees located in Fallen Rock State Preserve and nearby private property to the south. This area is near Pine Lake State Park, which in 2009 was devastated by a severe hailstorm of "supersized softballs" resulting in significant cambial damage to many species of trees. Damage to the majority of P. strobus specimens throughout the area was so severe that losses occurred immediately. Additional losses in subsequent years continued to occur likely due to additional stress by drought and destruction by bark beetles. The loss of approximately 75% of the P. strobus specimens at Pine Lake State Park was attributed to the 2009 hailstorm prompted efforts to preserve genetics of the white pines here. In 2014, specimens in parts of Pine Lake State Park and also one specimen at Fallen Rock State Preserve were sampled (Carstens, J.) as seeds from specimens ranging in size from 9.25 inches to 31.75 inches d.b.h. However, in 2021, it was determined (Place, A. pers. comm. 24 February 2021 and Carstens, J. & Sherwood, A., pers. observations 1 March 2021) that likely most if not all of the specimens in Pine Lake State Park are planted specimens of unknown origin because P. strobus specimens located at the far east end of Lower Lake (south side) were noted (Carstens and Sherwood, pers. observations 1 March 2021) growing with uncharacteristic associated taxa including Acer saccharinum and Gymnocladus dioicus. Two documents that support these observations includes: 1. Letter signed by Louis H. Pammel (March 25, 1925) to G.B. McDonald of the Iowa State University Forestry Department asking for 200 white pine to be planted at Pine Lake. 2. "Trees to Be Set Out by CCC Workers" in the Eldora Herald (May 9, 1935) referencing the CCC (Civilian Conservation Corps) to plant “1,000 white pines at Pine Lake State Park". Therefore, if obtained, increment borer measurements of specimens that are 94 years of age at present (2014) or older would suggest those as being true, native remnants. Documents that supports the position of remnant specimens at Fallen Rock State Preserve includes: 1. "Picturesque Drives About Eldora", in the Eldora Herald (December 8, 1910) by Clara Estabrook stating "Miss Stoddard of the Iowa Falls school says these (only 11 trees left) are the only native pines (those restricted to the sandstone cliffs) found in Hardin County" and suggested a movement to have them preserved. 2. Forest Flora of Hardin County (1899) by L. H. Pammel stating that the Iowa valley serves as the western limits for white pine and also refers to David D. Owen's geological report from 1839 indicating the occurrences of white pines on the summits of the hills along the Iowa River. In addition, a photo of white pines growing at Steamboat Rock taken by L. H. Pammel was featured on the front page of the 1919 report of the State Board of Conservation titled "Iowa Parks: Conservation of Iowa Historic, Scenic and Scientific Areas." Due to the significant presence of planted specimens of unknown origin in Pine Lake State Park and surrounding private properties, samples collected in 2014 as seeds may likely contain genetics (pollen donors) from specimens of unknown origin. This resulted in the resampling of specimens in 2021 (USFS - IAHA#'s) and 2023 as dormant scions that are from locations known to be untouched by the CCC and thus represent true, remnant specimens. To date (2021), there are only eight legacy specimens left in this population (four specimens at Fallen Rock State Preserve and four specimens at the nearby private property). The largest specimen of P. strobus (Ames 32758) is #IAHA-08 located at (42.395489, -93.091652) measuring (13 May 2018) 35.65" DBH with a height of 78.33' and a spread of 26' totalling 197 points (Rouw, M., personal communication, 8 February 2023). This germplasm represents the southwestern most population of native P. strobus in Iowa and one of the western most populations in North America. Germplasm likely is adapted to Midwestern climatic extremes and potentially very drought tolerant in comparison to other provenances from the eastern or northeastern U.S. | 1921270 | Ames 32758 |
| 472 | NA 81984 | Lactea Group | Callicarpa americana L. | Texas, United States | NA | | | 2014 | COLLECTED | 08/30/2013 | Woodlands above Boykin Spring Lake. | 31.06266000, -94.27565000 | 56 | Growing in partial shade of mixed deciduous and evergreen woodlands in well-drained to dry conditions. | | | 1951711 | NA 81984 |
| 473 | Ames 32387 | JDC/BN/2014/014/516 | Betula nigra L. | Iowa, United States | NC7 |  | | 2014 | COLLECTED | 06/05/2014 | Chia Fen, T81N R5W NW 1/4 of NW 1/4 Sec. 13. | 41.82947400, -91.38152400 | 226 | Sand prairie with likely high water table. | Wild material | | 1919308 | Ames 32387 |
| 474 | Ames 32197 | GA13009001 | Fraxinus pennsylvanica Marshall | Minnesota, United States | NC7 |  | | 2014 | COLLECTED | 09/23/2013 | Clearwater County. | 47.18397220, -95.47407220 | | Mixed upland deciduous forest. | Wild material | | 1917223 | Ames 32197 |
| 475 | NA 81709 | CSF-13-22 | Cephalanthus occidentalis L. | Maryland, United States | NA | | | 2013 | COLLECTED | 11/04/2013 | Cedarville State Forest near Brandywine/Waldorf, MD, at power transmission line corridor along small stream. | 38.64824000, -76.83493000 | 61 | Growing along small stream that crossed the transmission line right-of-way. | Wild material | | 1951113 | NA 81709 |
| 476 | Ames 32096 | BA13009001 | Fraxinus nigra Marshall | Minnesota, United States | NC7 |  | | 2013 | COLLECTED | 09/23/2013 | T144N R38W, Clearwater County. | 47.25711000, -95.49000667 | 543 | Edges of lakes and forest edges. Growing in association with Fraxinus pennsylvanica, Quercus macrocarpa, Ulmus americana, Populus tremuloides, Populus balsamifera, Acer saccharum, Betula papyrifera, Salix sp., Larix laricina, Quercus rubra, Abies balsamea, Picea glauca, Sambucus canadensis, Cornus rugosa, Acer spicatum, Rosa sp., Viburnum opulus var. americanum, Viburnum dentatum, Alnus sp., Cornus canadensis, Corylus sp., Prunus virginiana, Ribes sp., Prunus pensylvanica, Rhamnus alnifolia, Equisetum sp., Carex sp., Rubus sp., Impatiens capensis, Bromus sp., and Thalictrum dasycarpum. | Wild material | D.B.H. ranged between 3 and 6 inches. | 1914713 | Ames 32096 |
| 477 | WLP 1079 | NA 81742 | Cornus florida L. | Missouri, United States | NA | | | 2013 | COLLECTED | 09/26/2013 | Springfield Township: NW 1/4 of Section 20. | 38.41792000, -93.60433000 | | Growing in and around sandstone ravines. | Wild material | Voucher specimen being processed at time of accessioning; will be forwarded to USNA once prepared. | 1922751 | WLP 1079 |
| 478 | Ames 32093 | JDC/CC/2013/048/492 | Carpinus caroliniana Walter | Iowa, United States | NC7 | | | 2013 | COLLECTED | 10/25/2013 | Ledges State Park mostly from specimens adjacent to Peas Creek, NE ¼ of SE ¼ of Sec. 16, T83N R26W, Des Moines Quad. | 41.99910000, -93.87880000 | 328 | North and northwest-facing slopes. | Wild material | The native range of Carpinus caroliniana is concentrated in the eastern half of the U.S. with a very small disjunct population in central Iowa (Little, 1971). This accession represents a collection of C. caroliniana germplasm from the extreme western edge of the species native range, specifically the central Iowa disjunct population at Ledges State Park. The next closest occurrence is in eastern Iowa (100-150 miles). As of 2025, one specimen at Ledges State Park (McCoy Wildlife Area) currently represents the state of Iowa's largest C. caroliniana specimen measuring 6.68" DBH, 41.67’ in height, and 23.75’ average crown spread for a total of 68.608 points (Rouw, M., personal communication, 4 May 2022). This accession does include genotypes that do tend to sucker/form clonal colonies. Fall color (red/orange) tends to peak in the last week of October (central Iowa) with peak fruiting occurring simultaneously. Bark smooth, grey. | 1914037 | Ames 32093 |
| 479 | Ames 32094 | Ames 32094 | Symphoricarpos orbiculatus Moench | Iowa, United States | NC7 |  | | 2013 | COLLECTED | PRE 10/25/2013 | Bluffs along Des Moines River, SE 1/4 of Section 9, T82N R26W, Madrid NW Quad, Boone County. | 41.92480000, -93.87550000 | 328 | Edge of dry woods. Western exposure. | Wild material | Plants donated were grown from original seed. | 1914038 | Ames 32094 |
| 480 | Ames 32092 | Ames 32092 | Viburnum rufidulum Raf. | Missouri, United States | NC7 | | | 2013 | COLLECTED | 10/13/2013 | Private property, north of 27640 EE Highway, NE 1/4 of SE 1/4 of Section 4, T47N R15W, Prairie Home, Prairie Home Quad, Cooper County. | 38.85910000, -92.56030000 | 236 | Wooded hillside. North-facing slope. | Wild material | | 1914036 | Ames 32092 |
| 481 | DPRU 3195 | DPRU 3195 | Prunus hortulana L. H. Bailey | Missouri, United States | DAV |  | | 2013 | COLLECTED | 08/13/2013 | Property of Prairie Garden Trust (Henry and Lorna Domke), New Bloomfield Quad, northeast of New Bloomfield, Callaway County. | 38.74118667, -92.03118433 | 235 | Numerous specimens scattered throughout property, but localized/common to small drainage ditches; associated with Diospyros virginiana, Juglans nigra, Juniperus virginiana, Prunus serotina, Quercus imbricaria, Toxicodendron radicans, Carya ovata, Cornus florida, and Robinia pseudoacacia. | Wild material | Specimen 1: fruit diameter ranged between 17 mm-20 mm; approximately 20 feet in height and 20 feet in spread; leaves papery thin to the touch and glabrous. Specimen 2: fruit diameter ranged between 15 mm and 17 mm; fruits mostly red. Specimen 3: fruit diameter ranged between 18 mm and 19 mm; fruits mostly red. Specimen 4: fruit diameter ranged between 18 mm and 19 mm; fruits mostly green (a few red). Specimen 5: fruit diameter ranged between 15 mm-17 mm, fruits slightly longer (1 mm) than wide; approximately 15 feet in height; leaves papery thin to the touch and glabrous. Specimen 6: fruit diameter ranged between 20 mm and 22 mm; fruits mostly red. | 1912772 | DPRU 3195 |
| 482 | DPRU 3196 | DPRU 3196 | Prunus hortulana L. H. Bailey | Missouri, United States | DAV |  | | 2013 | COLLECTED | 08/14/2013 | Specimen 1 along South Rangeline Road, SW 1/4 of Section 30; Specimen 2 along State Road H (East Englewood Road), NW 1/4 of SE 1/4 of Section 30; Specimen 3 near State Road H (East Englewood Road), SE 1/4 of NE 1/4 of SE 1/4 of Section 30; Specimen 4 along South Rangeline Road, near airport, NW 1/4 of NW 1/4 of NW 1/4 of Section 30; Millersburg SW Quad, Boone County. | 38.82384400, -92.20357575 | 267 | Specimen 1 growing roadside, associated with Festuca and Solidago. Specinen 2 growing roadside, associated with Quercus bicolor, Toxicodendron radicans, and Ulmus. Specimen 3 growing in windbreak, associated with Celtis occidentalis, Juniperus virginiana, Lonicera maackia, Toxicodendron radicans, and Ulmus. Specimen 4 growing roadside associated with Celtis occidentalis, Diospyros virginiana, Euonymus atropurpueraus, Juniperus virginiana, Lonicera maackia, Salix, Toxicodendron radicans, Ulmus, and Vitis riparia. | Wild material | Specimen 1: fruit diameter ranged between 18 mm and 20 mm; fruits approximately 1 mm wider than long; approximately 10 feet in height and 6 feet in spread; leaves papery thin to the touch and glabrous; purple-copper colored bark with obvious lenticels. Specimen 2: fruit diameter ranged between 19 mm and 22 mm; approximately 15 feet in height and 10 feet in spread; leaves papery thin to the touch and glabrous; purple-copper colored bark on younger branches with exfoliating grayish bark on trunk. Specimen 3: fruit diameter ranged between 21 mm and 25 mm; approximately 20 feet in height and 10 feet in spread; leaves papery thin to the touch and glabrous; greyish, exfoliating bark. Specimen 4: fruit diameter ranged between 19 mm and 20 mm; approximately 20 feet in height and 10 feet in spread; leaves papery thin to the touch and glabrous; greyish, exfoliating bark. | 1912773 | DPRU 3196 |
| 483 | NA 81603 | (seedling of pink form) | Rhododendron austrinum (Small) Rehder | Florida, United States | NA | | | 2013 | COLLECTED | 2013 | On the Escambia river near the mouth of the Yellow River. [GPS coordinates are actually at the confluence of the White River, the Little Simpson River, and the Buzzard Lake River (and gas line canal). -SBL] | 30.59699000, -87.22295000 | | Plants were collected along along the sandy berms along river delta. | | | 1950972 | NA 81603 |
| 484 | Ames 32018 | APS/GD/2013/032/117 | Gymnocladus dioicus (L.) K. Koch | Missouri, United States | NC7 |  | | 2013 | COLLECTED | 04/09/2013 | Poosey Conservation Area, Livingston County. | 39.94995200, -93.71471700 | 267 | Floodplain. | Wild material | A total of four areas containing Gymnocladus dioicus were noted throughout Poosey Conservation Area. Each area was represented by approximately 2-6 specimens. Specimens ranged between 14-22.5 inches d.b.h. and approximately 90-110 feet in height. Pod production during the 2012 growing season was minimal/below average. Samples 473-1 and 473-2 were very close together (approximately 10 feet apart) and samples 473-3 and 473-4 were also very close together (approximately 48 feet apart). Samples this close together may potentially represent material from a single clone due to the clonal suckering habit of Gymnocladus dioicus. | 1908307 | Ames 32018 |
| 485 | Ames 31982 | APS/GD/2013/004/089 | Gymnocladus dioicus (L.) K. Koch | Kansas, United States | NC7 |  | | 2013 | COLLECTED | 02/18/2013 | Walnut Creek watershed, southwest of Marysville, Sections 5, 8, and 17, T3S R6E, Marshall County. | 39.79300943, -96.78506600 | 382 | Dry floodplain. | Wild material | | 1907535 | Ames 31982 |
| 486 | Ames 31983 | APS/GD/2013/006/091 | Gymnocladus dioicus (L.) K. Koch | Kansas, United States | NC7 |  | | 2013 | COLLECTED | 02/19/2013 | Beaver Creek, south of Scandia, Sections 7, 12, and extreme NW 1/4 of NW 1/4 of Section 8, T4S R5W, Republic County. | 39.72143025, -97.81205050 | 432 | Dry floodplain. | Wild material | | 1907536 | Ames 31983 |
| 487 | Ames 31988 | APS/GD/2013/012/097 | Gymnocladus dioicus (L.) K. Koch | Kansas, United States | NC7 |  | | 2013 | COLLECTED | 02/21/2013 | Canville Creek, west of Savonburg, SW 1/4 of Section 25, T26S R20E, Allen County. | 37.74857200, -95.17660125 | 304 | Dry floodplain. | Wild material | Largest Gymnocladus dioicus specimen was 29.5 inches d.b.h. | 1907541 | Ames 31988 |
| 488 | Ames 31989 | APS/GD/2009/001/010 | Gymnocladus dioicus (L.) K. Koch | Kansas, United States | NC7 |  | | 2013 | COLLECTED | 02/21/2013 | Clinton State Park, west of Lawrence, Section 12, T13S R18E, Douglas County. | 38.93730038, -95.36213950 | 282 | Fairly dry, upland site. Majority of specimens found on upland areas. | Wild material | | 1907542 | Ames 31989 |
| 489 | Ames 31676 | GA12010001 | Fraxinus pennsylvanica Marshall | Minnesota, United States | NC7 |  | | 2012 | COLLECTED | NEAR 09/24/2012 | Near Mashaug Creek just north of Twin Valley, Norman County. | 47.28851660, -96.26865000 | 327 | Upland forest, dominated by Populus deltoides. | Wild material | | 1906587 | Ames 31676 |
| 490 | Ames 31679 | GA12011001 | Fraxinus pennsylvanica Marshall | North Dakota, United States | NC7 |  | | 2012 | COLLECTED | NEAR 09/27/2012 | Sheyenne National Grassland along the Sheyenne River just east of Lisbon near Richland and Ransom County line. | 46.53246660, -97.26656660 | 302 | Riverbank and transition area of tallgrass prairie and riparian forest. Sandy-silt soil with good drainage and ph of ~7 | Wild material | Population located close to windbreak planted with Fraxinus. | 1906590 | Ames 31679 |
| 491 | WLP 1124 | MA-2012-015 | Crataegus sp. | Massachusetts, United States | NA | | | 2012 | COLLECTED | 08/26/2012 | Hampshire County; Pelham; Collection made on Shutesbury Road 0.5 miles northwest of the intersection with Route 202. | 42.40153000, -72.40946000 | 351 | Upland mixed forest. | | Seed and herbarium specimen collected. | 2108860 | WLP 1124 |
| 492 | Ames 31524 | JDC/FQ/2012/033/426 | Fraxinus quadrangulata Michx. | Indiana, United States | NC7 |  | | 2012 | COLLECTED | 07/22/2012 | Near Devil's Backbone, along Fort Ritner Road, S 1/2 of Section 17, and Section 18, T4N, R2E, Tunnelton Quad, just north and northeast of Tunnelton, Lawrence County. | 38.77591000, -86.32114800 | 202 | Dry, rocky, steep, north and south-facing slopes. | Wild material | | 1903751 | Ames 31524 |
| 493 | Ames 31526 | JDC/FQ/2012/035/428 | Fraxinus quadrangulata Michx. | Indiana, United States | NC7 |  | | 2012 | COLLECTED | 07/23/2012 | Along Trailhead #1, Charlestown State Park, near Charlestown, Clark County. | 38.44706000, -85.64315400 | 180 | Open grown specimens in glade, and also localized population amongst dense canopy forest on southeast-facing slope. Very shallow soils. | Wild material | | 1903753 | Ames 31526 |
| 494 | Ames 31529 | JDC/FQ/2012/038/431 | Fraxinus quadrangulata Michx. | Indiana, United States | NC7 |  | | 2012 | COLLECTED | 07/24/2012 | Lick Creek Summit Nature Preserve, NW 1/4 of Section 23, T13N, R2W, Richmond Quad, near Richmond, Wayne County. | 39.78453000, -84.95276400 | 267 | Dry woods. Bluffs. Shallow soils. | Wild material | | 1903756 | Ames 31529 |
| 495 | W6 43740 | NYCPDR-BBG-096 | Avenella flexuosa (L.) Parl. | New York, United States | W6 |  | | 2012 | | | | | | | Wild material | | 1900131 | W6 43740 |
| 496 | Ames 31254 | JDZ/11/007/001 | Fraxinus pennsylvanica Marshall | North Dakota, United States | NC7 |  | | 2011 | COLLECTED | 10/26/2011 | North side of Devil's Lake, Gilbert C. Grafton State Military Reservation, Sections 20, 28, and 29, T153N, R64W, Camp Grafton Quad, Ramsey County. | 48.05360000, -98.90790000 | 450 | | Wild material | D.B.H. between 4 and 14 inches. | 1897492 | Ames 31254 |
| 497 | Ames 31255 | JDZ/11/008/001 | Fraxinus pennsylvanica Marshall | North Dakota, United States | NC7 |  | | 2011 | COLLECTED | 10/26/2011 | South side of Devil's Lake, Sully's Hill National Game Preserve, Section 15, T152N, R65W, Fort Totten Quad, Benson County. | 47.98560000, -98.96810000 | 475 | 10 degrees of slope with southern and southwestern aspects. | Wild material | D.B.H. between 4 and 14 inches. | 1897493 | Ames 31255 |
| 498 | Ames 32418 | 193818 | Anemone berlandieri Pritz. | California, United States | NC7 |  | | 2011 | COLLECTED | 03/31/2003 | Near front entrance of Lady Bird Johnson Wildflower Center, Travis County. | 30.18667000, -97.87138000 | | | Wild material | | 1895199 | Ames 32418 |
| 499 | Ames 32492 | 180078 | Helenium amarum (Raf.) H. Rock | United States | NC7 |  | | 2011 | COLLECTED | 05/21/2002 | | | | Associated with Croton monanthogynus, Juniperus ashei, Nassella leucotricha, and Quercus virginiana. | Wild material | | 1895284 | Ames 32492 |