| 0 | PI 479486 NA 51302 | JH-283-82 | Magnolia obovata Thunb. | Hokkaidô, Japan | NA | | | 1982 | COLLECTED | 10/06/1982 | Hokkaido Prefecture, Oshima Subprefecture, Kayabe-gun: Mori-machi: Akaigawa, Mori National Forest. | 42.00000000, 140.65000000 | 200 | Growing on the edge of the woodland. | Wild material | | 1374422 | PI 479486 NA 51302 |
| 1 | PI 479487 NA 51330 | JH-309-82 | Magnolia obovata Thunb. | Honshu, Japan | NA | | | 1982 | COLLECTED | 10/08/1982 | Aomori Prefecture: Towada-shi: Tsutanuma (pond), Towada-Hachimantai National Park. | 40.55000000, 140.96666667 | 470 | | Wild material | | 1374423 | PI 479487 NA 51330 |
| 2 | NA 89117 | TLM25-06 | Magnolia virginiana L. | Louisiana, United States | NA | | | 2025 | COLLECTED | 07/11/2025 | Natchitoches Parish Road 380, approximately 0.30 km south of the junction with Bayou Camp Forest Route 321 just past the sign for a natural water spring; the site is located on the west side of hte road. | 31.48284200, -93.07549400 | 88 | This habitat is comprised of a botanically rich full sun, hillside seepage area with masses of wetland plant species, dominated by Sarracenia alata. The seepage area, which is 40-60 meters wide, is ultimately funneled downslope, to create the headwaters for a small stream that flows into and through the high understory shade of a longleaf pine forest. This streamside habitat, created by erosion, forms a series of sloping terraces that are home to plant communities ranging from obligate upland species on the upper terraces to facultative wetland species found at the base of the terraces along the stream edge. The range of plant communities and niches created in just a short distance from upper hillside seepage area to the emergent stream, offers a remarkably array of plant diversity. Magnolia virginiana can be found throughout the habitat as well as along the more mesic edge of this site. Slope: 10 to 15 percent. Aspect: southwest. Soils: The primary soil type in the collection area is Kisatchie Series clay, 1 to 15 percent slopes, severely eroded (Kt). The Kisatchie Series soil consists of moderately deep, well drained, very slowly permeable soils that formed clayey sediments over siltstone or sandstone on Tertiary age uplands. These soils are on moderately sloping to steep coastal plains. They are not saturated with water. Water runs off the surface at a moderate to rapid rate. Slope ranges from 1 to 40 percent. The solum is 50 to 100 cm thick over siltstone or sandstone and ranges from moderately to extremely acidic. (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. In the area of the collection the Catahoula Formation is primarily gray to white sandstones; loose quartz sand, tuffaceous sandstone, volcanic ash, and brown sandy clays; petrified wood locally. (Source: USGS Louisiana Geologic Map Data). | Wild material | | 2191656 | NA 89117 |
| 3 | NA 81460 | B-44474 | Magnolia kobus DC. | | NA | | | 2021 | | | | | | | | Historic plant from Glenn Dale; on 1965 inventory as plant number 173 in plot P1, and Bell number 44474. | 2120190 | NA 81460 |
| 4 | NA 87109 | NCTN18 | Magnolia fraseri Walter | North Carolina, United States | NA | | | 2020 | COLLECTED | 09/15/2019 | Swain County, along north side of Needmore Rd. on the Little Tennessee River; where distribution of M. fraseri meets M. tripetala | 35.29821000, -83.51430000 | 556 | Montane inland floodplain | Wild material | Seedlings received. | 2109421 | NA 87109 |
| 5 | NA 87111 | NCTN70 | Magnolia fraseri Walter | Tennessee, United States | NA | | | 2020 | COLLECTED | 09/26/2019 | Oconee County | 34.99894000, -83.05389000 | | | Wild material | Seedlings received. | 2109473 | NA 87111 |
| 6 | 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 |
| 7 | NA 84643 | NACPEC16-029 | Magnolia officinalis Rehder & E. H. Wilson | Sichuan Sheng, China | NA | | | 2017 | COLLECTED | 09/19/2016 | Mianyang Prefecture, Pingwu County
Town of Shuijingzhen. | 32.46591000, 104.16977000 | 1544 | Mesic mixed deciduous forest with cultivated areas; northeast-running [valley]; groves of cultivated trees. Soil rocky, organic. | Wild material | | 2132837 | NA 84643 |
| 8 | NA 84578 | RJL-RM002 | Magnolia pyramidata W. Bartram | Texas, United States | NA | | | 2017 | COLLECTED | 07/22/2017 | Newton County Road 425, about 2.8 miles south of Texas Recreational Road 255. | 30.85996000, -93.89596000 | 105 | Along roadsides and among young loblolly pines in forestry plantation. Plants growing in part shade to full sun in heavily regenerating roadside woodlands associated with loblolly pine plantations. Plants are growing in well drained, highly sandy soils. | Wild material | | 1953814 | NA 84578 |
| 9 | 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 |
| 10 | 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 |
| 11 | NA 82059 | JDC/MM/2014/088/590 | Magnolia macrophylla Michx. | Alabama, United States | NA | | | 2014 | COLLECTED | 09/23/2014 | Franklin County and Lawrence County; Small tributary to Little Bear Creek (Frankllin County) and also William B. Bankhead National Forest (Lawrence County). | 34.43544700, -87.58959100 | 293 | | Wild material | | 1922360 | NA 82059 |
| 12 | NA 81935 | NA 81935 | Magnolia virginiana L. | South Carolina, United States | NA | | | 2013 | COLLECTED | 08/29/2009 | In or near Francis Marion National Forest, distributed along Highway 17 ca. 2 miles S of Awendaw. [GPS provided is incorrect; uncertain which is correct longitude; latitude missing. Longitude provided: 1) 79 deg. 38' 38.74" W or 2) 79 deg/ 38' 9.78" W -SBL] | | | Open, swampy areas. | | Received as M. virginiana var. pumila | 1951852 | NA 81935 |
| 13 | 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 |
| 14 | NA 81939 | NA 81939 | Magnolia virginiana L. | Tennessee, United States | NA | | | 2013 | COLLECTED | 08/18/2008 | On west side of Main Street directly across from the Bethel Springs City Hall. | 35.23170000, -88.60690000 | | Growing in a saturated slough originating from a nearby spring. | | | 1952583 | NA 81939 |
| 15 | TARS 18264 | TARS 18264 | Magnolia sp. | | MAY | | | 2013 | | | | | | | | Possibly Magnolia obovata. | 1908199 | TARS 18264 |
| 16 | NA 80283 | RL 11005 | Magnolia macrophylla Michx. | Kentucky, United States | NA | | | 2011 | COLLECTED | 08/27/2011 | | | | | Wild material | | 1914116 | NA 80283 |
| 17 | NA 78354 | BCJMMT 279 | Magnolia stellata (Siebold & Zucc.) Maxim. | Honshu, Japan | NA | | | 2009 | COLLECTED | 10/10/2007 | Gifu Prefecture: Sentan-bayashi, Nakatsugawa City. | 35.49253000, 137.45573000 | 355 | Localised in sun on moist medium loam on the edge of a pond close to farmland in the hedgerow with Hydrangea paniculata. | Wild material | | 1951245 | NA 78354 |
| 18 | NA 78355 | NORI 17 | Magnolia stellata (Siebold & Zucc.) Maxim. | Honshu, Japan | NA | | | 2009 | COLLECTED | 2007 | Aichi Prefecture: Ikawadu, Tahara-shi. | 34.61972000, 137.14916000 | 30 | Grows in the boggy area from the spring water, around the edge of the woodland which is a secondary forest with cryptomerias, Aruncus and Heloniopsis underneath, making a colony with about 100 plants.. Near the bottom of a north facing slope. | Wild material | | 1951201 | NA 78355 |
| 19 | NA 77584 | RL 08024 | Magnolia tripetala (L.) L. | North Carolina, United States | NA | | | 2008 | COLLECTED | 09/02 | Harmon Den, along Forest Service road west of I-40 and near river. | 35.73280000, -83.02531000 | | | Wild material | | 1896039 | NA 77584 |
| 20 | NA 72443 | NACPEC02058 | Magnolia biondii Pamp. | Shanxi Sheng, China | NA | | | 2002 | COLLECTED | 09/24/2002 | Shanxi Province, Yang Cheng County, Yang Cheng Xiam, Gao Shi | 35.28633000, 112.52016000 | | Backyard garden of house next to small stream in small village, slope 0 degrees, aspect N ( North face of east running stream), Moist loess | Uncertain improvement status | After questions over its species identity (it did not appear to be M. denudata), material from this accession was tested in 2013 for ploidy (chromosome count) by Richard Olsen using flow cytometry, and was shown to be a diploid. Thus, it is not pure M. denudata (a hexaploid) as collected. This material has been provisionally identified as M. biondii by Richard Figlar, Erland Edjer and others. | 1777432 | NA 72443 |
| 21 | NA 71216 | USNAKY2001-004 | Magnolia macrophylla Michx. | Kentucky, United States | NA | | | 2001 | COLLECTED | 10/03/2001 | Kentucky, McCreary County, ~5.5 miles north of Marshes Siding on unnumbered residential road between Kentucky State Hwy. 1651, there is an immediate left turn onto the unnamed road. | 36.76425000, -84.48002000 | | full sun in a highly disturbed roadside on steep slopes- essentially a pioneer site; growing with Rhus copallina, Liriodendron tulipifera, Rhus sp., Similax sp., Acer rubrum, Cornus florida, Oxydendrum arboreum, Pycnanthemum sp. and Aralia spinosa., slope 3aspect w | Wild material | | 1777223 | NA 71216 |
| 22 | NA 70935 | NA 70935 | Magnolia acuminata (L.) L. | Virginia, United States | NA | | | 2001 | COLLECTED | 05/16/2001 | Wintergreen Resort. | 37.93242000, -78.94277000 | 984 | | | | 1951270 | NA 70935 |
| 23 | NA 70402 | MWPCC00-032 | Magnolia virginiana L. | Virginia, United States | NA | | | 2000 | COLLECTED | 09/12/2000 | Seeds were collected for teh expedition by Paul James, the group's local guide. No field data or herbarium specimens collected with the seed. | 38.00285700, -79.45777100 | | | Wild material | | 1607108 | NA 70402 |
| 24 | NA 70422 | MWPCC00-078 | Magnolia acuminata (L.) L. | North Carolina, United States | NA | | | 2000 | COLLECTED | 09/14/2000 | Blue Ridge Parkway pullover, N of marker 417. | 35.32333333, -82.82694444 | 1353 | Just in from mowed roadside. Slope: 15 degrees, Aspect: East, 3/4 day sun, Soil Type: gritty loam, well-drained, moist bottom of slope. | Wild material | | 1608250 | NA 70422 |
| 25 | NA 68900 | NACPEC97141 | Magnolia sieboldii K. Koch | Liaoning Sheng, China | NA | | | 1997 | COLLECTED | 10/01/1997 | Shenyang | 41.76666667, 123.43333333 | | In the Arboretum of the Shenyang Institute of Applied Ecology | Cultivated material | 3-6 m; small understory tree; fruit red, seeds orange | 1579192 | NA 68900 |
| 26 | NA 61237 | GU 102 | Magnolia virginiana L. | Virginia, United States | NA | | | 1989 | COLLECTED | 09/25/1989 | Magnolia swamp, George Washington National Forest, Blue Ridge Parkway | 38.32684300, -79.29107700 | | | Wild material | | 1112015 | NA 61237 |
| 27 | NA 58294 | NA 58294 | Magnolia stellata (Siebold & Zucc.) Maxim. | Honshu, Japan | NA | | | 1986 | COLLECTED | | Honshu, Gifu Prefecture, Mizurami-shi, Oniiwa (hot springs) | | | | Wild material | | 1111618 | NA 58294 |
| 28 | NA 56621 | KSW 3677 | Magnolia kobus DC. | Korea, South | NA | | | 1985 | COLLECTED | 10/04/1985 | Chintung village, Mongsan-ri 5-ku, Mangyong Myon, Kimje Gun, Cholla Pukto In garden of Mr. Kwak, Uk Chang. | 35.90000000, 126.83333333 | | | Cultivated material | Single-trunked small decid. tree ca 3 m tall with spreading slightly pendant branches, dbh 10 cm; lvs. med. green, dull to lustrous above, midvein yellow beneath; follicles dark purple-brown; arils glossy, light orange, 9 mm long, 6 mm wide. Tree very heavily fruited. | 1111142 | NA 56621 |
| 29 | PI 618194 | 'Magnolia' | Vaccinium hybr. | Florida, United States | COR | | | 1998 | DEVELOPED | 12/29/1994 | | | | | Cultivar | Berry: size medium; scar small; color, firmness, and flavor good. Flowers later than the earliest rabbiteye varieties at Poplarville, but ripens 2 weeks earlier. Plant: vigorous; productive; spreading; meidum height; should be planted with other southern highbush cultivars for pollination. Adapted to U.S. Dept. of Agriculture plant hardiness zone 8.MAGNOLIA, tested as MS162, originated from a cross of (Harrison x Avonblue) x Florida 2-5 made by Paul Lyrene at the University of Florida who sent seedlings to the USDA-ARS blueberry breeders at Poplarville, Mississippi. The seedlings were established in the field in south Mississippi and was selected in 1982 by J. M. Spiers, C. L. Gupton and A. D. Draper. Plants have a spreading growth habit and are medium in height, productive and vigorous after field establishment. Small plants require good management in planting to ensure a good stand. Fruit is medium in size, and has good flavor, color and firmness with small picking scar. Plants bloom later and ripen their fruit about two weeks before the earliest rabbiteye cultivars. Should be interplanted with other southern highbush cultivars to facilitate fruit set, early ripening, and maximum yield. No virus symptoms have been observed.
J. Spiers, C. Gupton, and A. Draper cultivar release released in 1994 Original cross by Paul Lyrene in Florida
| 1560113 | PI 618194 |
| 30 | PI 582925 | MAGNOLIA | Vigna unguiculata (L.) Walp. subsp. unguiculata Unguiculata Group | | S9 | | | 1992 | DONATED | 08/1992 | | | | | Cultivated material | | 1477896 | PI 582925 |
| 31 | PI 548467 | 'Magnolia' | Glycine max (L.) Merr. | Kyonggi, Korea, South | SOY | | | 1991 | COLLECTED | | | | | | Cultivar | Released by 1939 | 1443403 | PI 548467 |
| 32 | PI 529033 | SA 963 | Gossypium hirsutum L. | Texas, United States | COT | | | 1989 | DONATED | 02/1989 | | | | | | | 1423969 | PI 529033 |
| 33 | PI 552354 | TC 210 | Nicotiana tabacum L. | Florida, United States | TOB | /2013/Field 2013/TC 210_thumbnail.jpg "Click for 5 image(s) for this accession.") | | 1961 | DONATED | 1961 | | | | | Cultivar | | 1447326 | PI 552354 |
| 34 | DVIT 2197 | Magnolia | Vitis rotundifolia Michx. | Georgia, United States | DAV | | | 1986 | DONATED | POST 05/29/1986 | | | | | Cultivated material | Type = Rotundifolia. Per Andersen (see citation): "Muscadine grapes (Vitis rotundifolia Michx.) are indigenous to the southeastern United States. Currently 4,000 acres are under cultivation, and the muscadine industry in Florida is stable with about 400-500 acres. Olien summarized the strenghths of the muscadine industry to include a greater resistance to insects and diseases, increased vine longevity and increased market diversity compared to Euvitis table grapes. Poor tolerance to wet soils, uneven fruit ripening, wet stem scar, lack of seedlessness, unstable markets and low prices for processed fruit were cited as weaknesses of the muscadine industry. [...] Cultivars with a soluble solids less than 14.0% were 'Magnolia.' [...] Cultivars that had less than 75% dry scar, indicative of a poorly formed abscission layer at the point of berry attachment, included . . . 'Magnolia' [etc.]" | 1018815 | DVIT 2197 |
| 35 | DFIC 34 | Brunswick | Ficus carica L. | California, United States | DAV |  | | 1982 | DONATED | 01/1982 | | | | | | The above UNVERIFIED accession names were cited as synonyms in Fig Varieties: Hilgardia, Vol. 23, No. 11, 1955, p. 416, by Condit; and in Fig Growing in the South, USDA, Handbook 196, p. 5, by Krezdorn and Adriance. Rating of this variety by fig grower, Mr. Ray Givan, in Pomona, Vol. XXIX, No. 1, Winter 1996: Very good; sweet and rich, but sours in rainy weather. Info. on this variety from Watts, Figs in Coastal Southern California, Fruit Gardeners, California Rare Fruit Growers, Vol. 23, No. 6, December 1991: Large, brownish skin, reddish pulp. Coarse skin. Used mostly for preserves without the skin in Texas. Ripens too slowly on coast. Bland tasting. Poor on coast. | 1001195 | DFIC 34 |
| 36 | CIor 8318 | 'Magnolia' | Oryza sativa L. | Louisiana, United States | NSGC |  | | 1943 | DEVELOPED | 1945 | | | | | Cultivar | Medium-grain rice. | 1043213 | CIor 8318 |
| 37 | PI 664517 | 'Bettergro Blackeye' | Vigna unguiculata (L.) Walp. subsp. unguiculata Unguiculata Group | South Carolina, United States | S9 | | | 2011 | DEVELOPED | 07/24/1991 | | | | | Cultivar | 'Bettergro Blackeye' has a tall, upright plant habit. Maturity is usually concurrent with that of 'Pinkeye Purple Hull'. The pods are usually borne in a scattered fashion at foliage level. Pod color is light green when immature, a cream yellow at green-shell maturity, and a light-straw color when dry. The green-shell maturity pods have a touch of reddish shading and reddish tips. A typical pod is slightly curved, 17 to 20 cm long, and contains 12 or 13 peas. The size, shape, and eye pattern of 'Bettergro Blackeye' peas are similar to those characteristic of the leading pinkeye-type cultivars Pinkeye Purple Hull and Coronet. The shape of the dry peas is intermediate between the ovoid/ovate and kidney shapes. Seed size is medium (15 g/100 dry peas; 36 g/100 fresh peas). The fresh peas are light yellow. The dry seed testa is rough and light tan in color. 'Bettergro Blackeye' has a level of resistance to the cowpea curculio similar to that of 'Carolina Cream', 'Carolina Crowder', and the breeding line Ala. 963.8. 'Bettergro Blackeye' has excellent yield potential. 'Bettergro Blackeye' is homozygous for the Rk gene that conditions resistance to root-knot nematodes (Meloidogyne spp.). Observations of natural epiphytotics indicate that 'Bettergro Blackeye' is resistant to rust (Uromyces phaseoli (Pers.) Wint. var. vignae (Barcl.) Arth.) and powdery mildew (Erysiphe polygoni DC. ex St. Amans). 'Bettergro Blackeye' is susceptible to Blackeye cowpea mosaic virus. | 1892378 | PI 664517 |
| 38 | PI 657176 | V. elliottii HL 2006-002 | Vaccinium elliottii Chapm. | Florida, United States | COR |  | | 2006 | COLLECTED | 05/22/2006 | Blountstown, Calhoun county. Southwest from city center on the east side of Chipopla Road, 100 m north of Magnolia Avenue. Across from the Paramore Restaurant. | 30.43768000, -85.05820000 | 31 | Sandy soil, forest edge where open, scatered throughout around wooded area | Wild material | Not a flat wood species; likes to be on hillier land; companion plant with rabbiteye blueberry - Vaccinium virgatum (synonym V. ashei), but, V. virgatum has a more limited range. V. elliottii blooms early and ripens earlier than other Vaccinium in Florida. It has a dark black-blue fruit with some bloom on it. Distribution for V. elliottii is from Gainesville west through Texas. It has not been found south of or to the Northeast of Gainesville in Florida. Although, it is present in eastern Georgia north through North Carolina and west to Missouri.This species is a diploid and crosses readily with V. darrowii and with any diploid cyanococcus species throughout the state. | 1702613 | PI 657176 |
| 39 | PI 657177 | V. darrowii HL 2006-004 | Vaccinium darrowii Camp | Florida, United States | COR | | | 2006 | COLLECTED | 05/23/2006 | Blountstown, Calhoun county. Southwest from city center on the east side of Chipopla Road, 100 m north of Magnolia Avenue. Across from the Paramore Restaurant. | 30.43768000, -85.05820000 | 31 | Sandy soil, forest edge where open, scatered throughout around wooded area | Wild material | Collected by Kim Hummer and Paul Lyrene
| 1702614 | PI 657177 |
| 40 | 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 |
| 41 | PI 649024 | PA1 | Actaea racemosa L. | Pennsylvania, United States | NC7 |  | | 2005 | | | | | | | Wild material | | 1698894 | PI 649024 |
| 42 | PI 664813 | KY1 | Actaea racemosa L. | Kentucky, United States | NC7 | | | 2005 | | | | | | | Wild material | | 1698887 | PI 664813 |
| 43 | PI 664820 | VA2 | Actaea racemosa L. | Virginia, United States | NC7 | | | 2005 | | | | | | | Wild material | | 1698898 | PI 664820 |
| 44 | PI 664821 | WV1 | Actaea racemosa L. | West Virginia, United States | NC7 | | | 2005 | | | | | | | Wild material | | 1698899 | PI 664821 |
| 45 | PI 656815 | JM2004010 | Monarda clinopodia L. | South Carolina, United States | NC7 |  | | 2004 | COLLECTED | 10/05/2004 | Wadakoe Mountain, Pickens County. | 34.98055556, -82.84361111 | 464 | Cove-hardwood community. | Wild material | | 1667582 | PI 656815 |
| 46 | PI 664873 | JM2004005 | Prunella vulgaris L. | North Carolina, United States | NC7 | | | 2004 | COLLECTED | 10/02/2004 | Highway 276 to East Fork Road, Pine Shore Lakes, Brevard, Transylvania County. | 35.12611111, -82.72944444 | 851 | Pine-oak forest. Lakeside on private land. 15 degrees of slope with a northwestern aspect. | Wild material | 15-40 cm tall. | 1667584 | PI 664873 |
| 47 | PI 637120 | FB0007-3-1-6-1 | Oryza sativa L. | Nigeria | NSGC |  | | 1998 | DEVELOPED | | | | | | Breeding material | | 1569928 | PI 637120 |
| 48 | PI 616874 | F. virginiana subsp. virginiana NC 96-4-2 | Fragaria virginiana Mill. subsp. virginiana | North Carolina, United States | COR |  | Out of Season | 1996 | COLLECTED | 05/14/1996 | Highway US 117, 1.4 miles north of Magnolia city limits , Duplin county, North Carolina. Roadside on right heading north. | 34.92000000, -78.06472000 | | Roadside between ditch and woods of mixed pines and hardwoods. Plants scattered with P. canadensis, Rubus ssp. among grasses and herbs. | Wild material | USDA Sponsored plant collecting expedition, 1996 | 1536037 | PI 616874 |
| 49 | PI 603107 | Ames 19995 | Aronia ×prunifolia (Marshall) Rehder | Virginia, United States | NC7 |  | | 1992 | COLLECTED | | George Washington National Forest along Blue Ridge Parkway, Augusta County | 37.90340700, -78.99173400 | 708 | Magnolia swamp. | Wild material | Accession separated from Ames 13825 (PI 578096). Accession is vigorous with abundant fruits initiating color in September with peak maturity the end of October (central Iowa). | 1083927 | PI 603107 |
| 50 | PI 649004 | 9028411 | Tridens flavus (L.) Hitchc. | Arkansas, United States | NC7 | | | 1992 | COLLECTED | | | | | | Wild material | Composite from Magnolia area. | 1082186 | PI 649004 |
| 51 | PI 578119 | NA 61766 | Spiraea miyabei Koidz. | Korea, South | NC7 | | | 1991 | COLLECTED | 10/11/1989 | On the road to Osaek, Route 44, Kang-won Do. | 38.08333333, 128.41666667 | 700 | Along trail to mineral spring in an open woodland. | Wild material | Multi-stem shrub, .75 to 1.0m tall. Leaves dull green, acuminate. Flowers inflorescence, flat-topped. Growing with Magnolia sieboldii, Taxus cuspidata, Quercus, Abies holophylla, Ulmus, Betula, Acer pseudosieboldianum and Stephanandra. | 1473090 | PI 578119 |
| 52 | PI 578096 | GU 103 | Aronia arbutifolia (L.) Pers. | Virginia, United States | NC7 |  | | 1990 | COLLECTED | | George Washington National Forest along Blue Ridge Parkway, Augusta County | 37.90340700, -78.99173400 | 708 | Magnolia swamp. | Wild material | | 1473067 | PI 578096 |
| 53 | PI 589772 | GMAL 2374 | Malus angustifolia (Aiton) Michx. | North Carolina, United States | GEN |  | | 1987 | COLLECTED | 08/26/1987 | N. Carolina, Clay Co., 0.8 mi. S.E. from Hwy 64 on U.S. Forest Service Rd. 71. Soil brownish. | | | | | Comments: 40 ft. tall, branching at 10 ft. , 10 cm. diam. Single tree with few fruit. Red Oak, White Oak, Red Maple, Yellow Birch Magnolia frazierl, Beech, Sourwood, Witch Hazel, Ilex , Amelanchier, Rhododendron. | 1020024 | PI 589772 |
| 54 | PI 462270 | 2686 | Paspalum ionanthum Chase | Tacuarembó, Uruguay | S9 | | | 1981 | COLLECTED | 12/26/1980 | Sandy fld. near stream, Est. Exp. La Magnolia, Tres Cruces, Tacuarembo Dept | | | | | Collected by B. Bemhaja. | 1357206 | PI 462270 |
| 55 | PI 554818 | 'Scammell' | Vaccinium corymbosum L. | New Jersey, United States | COR |  | | 1980 | DEVELOPED | 1931 | | | | | Cultivar | Cross made in 1915. Fruit: cluster tight, long; berry size medium; ripens midseason. Bush: productive, especially in North Carolina; resistant to canker. - Brooks and Olmo Register of Fruit and Nut Varieties. 1997. ASHS Press. p. 186.Fredrick V. Coville, Principal Botanist, Division of Plant Exploration and Introduction, Bureau of Plant Industry, 1937. Improving the Wild Blueberry. Yearbook of Agriculture. USDA. Govt. Printing Office. Washington, D.C. p. 569'The Scammell blueberry is named for H. B. Scammell, of Toms River, N. J., who first showed how good are the qualities of this berry under field conditions. One of the parents of the Scammell was a cross between the wild blueberries Brooks and Chatsworth. This Brooks-Chatsworth parent, which was never planted in the field, was recorded in the greenhouse in Washington as having 'Berries of delicious taste, sweet, slightly acid and of pronounced flavor.' This plant was pollinated with Rubel pollen in 1915 and the Scammell blueberry was one of the resulting seedlings. In the field the original bush of Scammell bore berries up to a diameter of 20.5 mm. On budded plants in the greenhouse in Washington they reached more than 22 mm. The berries have a medium blue color, firm texture and a small scar, and the calyx is almost wanting. The leaves are smaller than on most varieties of highbush ancestry, commonly 1.5 to 2 inches in length and five-eighths to three-quarters of an inch in width. The berries are sweet, subacid and have a high degree of flavor. They ripen in late midseason. Among New Jersey growers there has been little planing of this variety, apparently from doubt regarding its vegetative vigor. In North Carolina, However, at Double Trouble Company's blueberry plantation near magnolia, it is regarded as one of their best varieties.'
Frederick V. Coville cultivar release cross made in 1915, introduced in 1931
NAMED FOR= H. B. Scammell of Toms River NJ | 1449790 | PI 554818 |
| 56 | PI 389997 | 'Nato' | Oryza sativa L. | Louisiana, United States | NSGC |  | | 1974 | DEVELOPED | | | | | | Cultivar | Originally received as CIor 8998. | 1293065 | PI 389997 |
| 57 | PI 279982 | WC 2485 | Oryza sativa L. | Piemonte, Italy | NSGC |  | | 1962 | DEVELOPED | | | | | | Breeding material | | 1208578 | PI 279982 |
| 58 | PI 279995 | WC 2496 | Oryza sativa L. | Piemonte, Italy | NSGC |  | | 1962 | DEVELOPED | | | | | | Breeding material | | 1208589 | PI 279995 |
| 59 | NA 89159 | 2025RJLSEUS-07 | Persea borbonia (L.) Spreng. | Florida, United States | NA | | | 2025 | COLLECTED | 10/02/2025 | Eglin Air Force Base: Plants are found on a coastal dune ridge and surrounding xeric habitats on Eglin AFB behind businesses located along Florida State Highway 98. The site is accessed through a now gated and permanently closed Eglin AFB, East River Unit, A-21 Road (now open to pedestrian traffic only with a valid Eglin user permit). After walking through the gated road, the site is to the west along 4-wheeling trails. | 30.41249300, -86.77374700 | 9 | Shade to full sun in a primarily evergreen extremely dry dune community with a mixed understory of deciduous and evergreen plants. Slope: 0 to 2 percent. Aspect: Various. Soils: The soils of this are characterized as Kureb Series sand, 0 to 8 percent slopes. The Kureb series consists of very deep, excessively drained, gently sloping to moderately steep soils on Coastal Plain uplands and on side slopes along streams and bays. They have formed in marine, aeolian, or fluvial sands. Slopes range from 0 to 20 percent. The thickness of the sandy horizon is more than 2 meters. Soil reaction is neutral to extremely acid throughout. All horizons are fine sand, sand, or coarse sand. Silt plus clay content is less than 5 percent. (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 | | 2193005 | NA 89159 |
| 60 | NA 89160 | 2025RJLSEUS-08 | Ilex hybr. | Florida, United States | NA | | | 2025 | COLLECTED | 10/02/2025 | Eglin Air Force Base: coastal dune ridge on Eglin AFB behind businesses located along Florida State Highway 98. The site is accessed through a now gated and permanently closed Eglin AFB, East River Unit, A-21 Road (now open to pedestrian traffic only with a valid Eglin user permit). After walking through the gated road, the site is to the west along 4-wheeling trails. | 30.41191000, -86.77315800 | 8 | Part shade in a primarily evergreen extremely dry dune community with a mixed understory of deciduous and evergreen plants. Slope: 0 to 2 percent. Soils: The soils of this are characterized as Kureb Series sand, 0 to 8 percent slopes. The Kureb series consists of very deep, excessively drained, gently sloping to moderately steep soils on Coastal Plain uplands and on side slopes along streams and bays. They have formed in marine, aeolian, or fluvial sands. Slopes range from 0 to 20 percent. The thickness of the sandy horizon is more than 2 meters. Soil reaction is neutral to extremely acid throughout. All horizons are fine sand, sand, or coarse sand. Silt plus clay content is less than 5 percent. (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 | | 2193006 | NA 89160 |
| 61 | 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 |
| 62 | NA 89181 | WV25-01 | Ilex montana Torr. & A. Gray | West Virginia, United States | NA | | | 2025 | COLLECTED | 09/12/2025 | Monongahela National Forest: found while driving down US-250, on the south side of the road, beyond the drainage cut. | 38.60535544, -79.86114341 | 1127 | | Wild material | Herbarium voucher deposited USNA | 2192760 | NA 89181 |
| 63 | NA 89183 | WV25-04 | Crataegus punctata Jacq. | West Virginia, United States | NA | | | 2025 | COLLECTED | 09/12/2025 | Monongahela National Forest. | 38.60064841, -79.85440929 | 1134 | | Wild material | Herbarium voucher deposited USNA | 2192763 | NA 89183 |
| 64 | NA 89184 | WV25-05 | Ilex collina Alexander | West Virginia, United States | NA | | | 2025 | COLLECTED | 09/12/2025 | Monongahela National Forest. The only individual found during a 0.6-mile transect on the SW side of US 250. | 38.60075654, -79.85492012 | 1134 | A relatively open, sunny moor with thin soil. | Wild material | Herbarium voucher deposited USNA | 2192764 | NA 89184 |
| 65 | NA 89185 | WV25-06 | Ilex collina Alexander | West Virginia, United States | NA | | | 2025 | COLLECTED | 09/12/2025 | Monongahela National Forest. This population was on the NE side of US-250. | 38.60211468, -79.85426212 | 1124 | Growing in mostly shade within a densely vegetated peaty bog. | Wild material | Herbarium voucher deposited USNA | 2192765 | NA 89185 |
| 66 | NA 89189 | WV25-11 | Viburnum lantanoides Michx. | West Virginia, United States | NA | | | 2025 | COLLECTED | 09/13/2025 | Monongahela National Forest. | 38.53027974, -79.93898451 | 1165 | Steep, eroded mountain drain. | Wild material | Herbarium voucher deposited USNA | 2192769 | NA 89189 |
| 67 | NA 89190 | WV25-12 | Ilex collina Alexander | West Virginia, United States | NA | | | 2025 | COLLECTED | 09/13/2025 | Monongahela National Forest. | 38.52413054, -79.93789223 | 1136 | Steep, southwest-facing slope above parking area. | Wild material | Herbarium voucher deposited USNA | 2192770 | NA 89190 |
| 68 | NA 89191 | WV25-14 | Ilex montana Torr. & A. Gray | West Virginia, United States | NA | | | 2025 | COLLECTED | 09/13/2025 | Monongahela National Forest: east side of Forest Road 233. | 38.57289483, -79.90066843 | 1109 | Growing on east side of road. | Wild material | Herbarium voucher deposited USNA | 2192772 | NA 89191 |
| 69 | NA 89113 | TLM25-01 | Zanthoxylum clava-herculis L. | Texas, United States | NA | | | 2025 | COLLECTED | 07/08/2025 | Packery Channel Oak Motte Sanctuary on Padre Island. Plants were growing on the dune edge of the Sanctuary at the intersection of Villa Maria Isabel Avenue and Sand Dollar Avenue. | 27.62564900, -97.21972000 | 3 | Plants are growing in part shade to full sun, deep sandy, and dry conditions. Plants are sheltered from direct impact of winds and surf by the dunes where they reside. The dunes appear relatively stable with a dense "motte" of Quercus fusiformis and other plants species, all of which appear to quite mature. Soils: The soils of this site are classified as Galveston and Mustang fine sands, occasionally flooded (Gm). The Galveston Series (~50%) consists of very deep, somewhat excessively drained, high saturated hydraulic conductivity (rapidly permeable soils) that formed in sandy eolian deposits derived from igneous, metamorphic and sedimentary rock. These nearly level to strongly sloping soils occur on back-barrier flats on barrier islands. Slope ranges from 0 to 3 percent. The soils are occasionally flooded with salt water during severe storms. The Mustang Series (~30%) consists of very deep, poorly drained, very slowly permeable soils that formed in sandy eolian and storm washover sediments. These nearly level soils are on planar to concave barrier island flats. These soils are subject to occasional flooding by high storm surge from strong tropical storms and are ponded after periods of heavy rainfall. Slope ranges from 0 to 1 percent. Galveston and Mustang fine sands range from slightly alkaline to moderately alkaline. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). Geology: The underlying geology of this area is characterized as Barrier Ridge and Barrier Flat Deposits of Quaternary, Holocene origin. It is comprised of sand, silt, and clay; mostly sand, well sorted, and fine grained with abundant shells and shell fragments. Interfingers have silt and clay in landward direction; includes beach ridge, spit, tidal channel, tidal flats, washover fian, and sand dune deposits. (Source: USGS Texas Geologic Map Data). Slope: 1 to 5 percent. Aspect: west to northwest. | Wild material | | 2191652 | NA 89113 |
| 70 | NA 89051 | AFGN25-01 | Hydrangea barbara (L.) Bernd Schulz | Alabama, United States | NA | | | 2025 | COLLECTED | 05/31/2025 | Ebeneezer Swamp Ecological Preserve. | 33.16818000, -86.81243000 | 148 | Swamp forest with slow moving water. Dominant canopy consisted of Nyssa aquatica, Magnolia virginiana, and Acer rubrum. | Wild material | | 2191418 | NA 89051 |
| 71 | NA 89070 | AFGN25-16 | Rubus odoratus L. | North Carolina, United States | NA | | | 2025 | COLLECTED | 06/03/2025 | Ball Creek Rd (83). | 35.03127000, -83.45786000 | 1334 | Mixed mesophytic Appalachian forest. | Wild material | | 2191433 | NA 89070 |
| 72 | NA 89073 | AFGN25-19 | Hydrangea radiata Walter | South Carolina, United States | NA | | | 2025 | COLLECTED | 06/03/2025 | Ashmore Heritage Preserve Trail. | 35.08236000, -82.58239000 | 350 | Mixed mesophytic Appalachian forest. | Wild material | | 2191436 | NA 89073 |
| 73 | NA 88930 | 24Flam16 | Rhododendron canescens (Michx.) Sweet | Georgia, United States | NA | | | 2025 | COLLECTED | 09/10/2024 | DeKalb County: Stone Mountain: Stone Mountain Park: slope near Robert E. Lee Boulevard. | 33.80238000, -84.15508000 | 286 | Dry, shady slope. Growing in 3/4 shade. Slope: 30 to 45 degrees. Aspect: West-southwest. | Wild material | Note: Seeds from three different plants collected at the same spot were bulked together in this accession; the lowest field collection number (24Flam16) has been chosen as the primary for this record. It appears from the notes that the identity is slightly uncertain; possibly not pure R. canescens. | 2172813 | NA 88930 |
| 74 | 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 |
| 75 | NA 88936 | 24Flam54 | Kalmia latifolia L. | Georgia, United States | NA | | | 2025 | COLLECTED | 09/12/2025 | Clyo, GA: Metzger Farm, on a shelf above Savannah River. GPS points are a general location for the population, not individual plants [note: collections were combined into this USNA accession.] | 32.49317000, -81.22832000 | 50 | Wet woods on a steep, steep shelf above Savannah River. Growing in 3/4 shade. Slope: 45 to 60 degrees. Aspect: Northeast. | Wild material | | 2172819 | NA 88936 |
| 76 | NA 88746 | TXWL2025-039 | Ilex verticillata (L.) A. Gray | Louisiana, United States | NA | | | 2025 | COLLECTED | 01/24/2025 | Kistachie National Forest: Compartment 49, Indian Creek. | 31.09110000, -93.53333000 | | Slough/baygall area with standing water below a longleaf pine stand. | Wild material | | 2171020 | NA 88746 |
| 77 | NA 88595 | 2024RJLFL-021 | Rhododendron serrulatum (Small) Millais | Florida, United States | NA | | | 2025 | COLLECTED | 11/14/2024 | South side of Crain Road (Westwood Drive) about 0.32 kilometers west of the junction with Green Road. | 30.88851800, -86.84913900 | 55 | Edge of moist, mixed evergreen and deciduous forests in part shade. Slope: 0 to 2 percent. Aspect: North. 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. 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, 0 to 5 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 | | 2170964 | NA 88595 |
| 78 | 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 |
| 79 | 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 |
| 80 | NA 88577 | 2024RJLFL-001 | Ilex myrtifolia Walter | Florida, United States | NA | | | 2024 | COLLECTED | 11/12/2024 | Yellow River Marsh Preserve State Park: collected along trail from the parking lot. The property is accessed from a parking area located on Dickerson City Road. | 30.48472300, -87.07110400 | 5 | Mostly found in moist flatwoods in mixed evergreen and deciduous forest. Slope: N/A. Aspect: Various. 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. In an effort 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 in order 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 Goldhead Series consists of poorly drained and very poorly drained soils on broad areas of the flatwoods and in depressions. They formed in thick beds of stratified unconsolidated loamy and sandy marine sediments. Slopes range from 0 to 5 percent. The solum thickness ranges from 35 to greater than 60 inches. Soil reaction ranges from very strongly acid to mildly alkaline in the A and E horizons, and very strongly acid to moderately alkaline in the B and C horizons. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). | Wild material | | 2169914 | NA 88577 |
| 81 | 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 |
| 82 | 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 |
| 83 | NA 88582 | 2024RJLFL-013 | Cornus florida L. | Florida, United States | NA | | | 2024 | COLLECTED | 11/13/2024 | Woodland edge along the south side of Bud Bass Road (DOF B48), 0.30 kilometers east of the junction with Norman Riley Road. | 30.75753300, -86.80457600 | 39 | Mixed evergreen and deciduous forests in part shade in a mesic- to mesic-dry situation. Slope: 0 percent. Aspect: North. 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 Troup Series loamy sand, 0 to 5 percent slopes. The Troup series consists of very deep, somewhat excessively drained soils that formed in unconsolidated sandy and loamy marine sediments. Troup soils are on ridges and hillslopes. Slopes predominantly range from 0 to 15 percent but range to 45 percent. The soil pH is generally strongly acid. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). | Wild material | | 2169919 | NA 88582 |
| 84 | 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 |
| 85 | 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 |
| 86 | NA 88586 | 2024RJLFL-020 | Vaccinium arboreum Marshall | Florida, United States | NA | | | 2024 | COLLECTED | 11/14/2024 | Woodland edge off of Ralf Laurant Road, above the wetland/headwaters of Danley Branch along the edge of a young longleaf pine plantation. | 30.90104300, -86.78878100 | 61 | Edge of a mixed evergreen and deciduous forest in part shade to full sun on a mesic to mesic-dry slope, adjacent to a young longleaf pine plantation. Slope: 3 to 8 percent. Aspect: West. 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. The dominant fossils in the freshwater carbonates are mollusks. (Source: USGS Florida Geologic Map Data). The surface soil profile is classified as Troup Series loamy sand, 5 to 8 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. These soils are very strongly acid to strongly acid. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). | Wild material | | 2169923 | NA 88586 |
| 87 | NA 88587 | 2024RJLFL-023 | Persea borbonia (L.) Spreng. | Florida, United States | NA | | | 2024 | COLLECTED | 11/15/2024 | Dune ridge behind businesses located along Florida State Highway 98. Site was accessed through a now pedestrian-only (gated) Eglin Air Force Base, East River Unit, A-21 Road. After walking through the gated road, the site is to the west along four-wheeling vehicle trails. | 30.41249300, -86.77374700 | 9 | Primarily evergreen, extremely dry dune community with a mixed understory of deciduous and evergreen plants in part shade to full sun. Slope: 0 to 2 percent. Aspect: Various. 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). The soils of this are characterized as Kureb Series sand, 0 to 8 percent slopes. The Kureb series consists of very deep, excessively drained, gently sloping to moderately steep soils on Coastal Plain uplands and on side slopes along streams and bays. They have formed in marine, aeolian, or fluvial sands. Slopes range from 0 to 20 percent. The thickness of the sandy horizon is more than 2 meters. Soil reaction is neutral to extremely acid throughout. All horizons are fine sand, sand, or coarse sand. Silt plus clay content is less than 5 percent. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). | Wild material | | 2169924 | NA 88587 |
| 88 | NA 88588 | 2024RM-001 | Hydrangea radiata Walter | Georgia, United States | NA | | | 2024 | COLLECTED | 10/24/2024 | Chattahoochee National Forest: Warwoman Wildlife Management Area: north side of Overflow Creek Road just west of the bridge over the Chattooga River. | 34.94956600, -83.20652000 | 498 | Mixed evergreen and deciduous moist mesic forest in part shade. The underlying geology of this area is characterized as Metagraywacke/Mica Schist Formation of the Precambrian-Paleozoic period. (Source: USGS Georgia Geologic Map Data). The soils of this are characterized as Tusquitee Series 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. Solum thickness ranges from 1 to 3+ meters. Reaction is very strongly acid to slightly acid, in the A horizon. The Bw and lower horizons are very strongly acid to moderately acid. In the upper 1 meter, content of rock fragments, dominantly of gravel to stone size, ranges up to 35 percent. Below 1 meter, rock fragment content may range up to 60 percent. Content of mica flakes ranges from few to common. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). | Wild material | | 2169925 | NA 88588 |
| 89 | 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 |
| 90 | 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 |
| 91 | 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 |
| 92 | 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 |
| 93 | 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 |
| 94 | 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 |
| 95 | NA 87838 | TRX241117-03NC | Ilex coriacea (Pursh) Chapm. | North Carolina, United States | NA | | | 2024 | COLLECTED | 11/17/2024 | Boiling Spring Lakes Community Center nature trail. | 34.02040000, -78.06469000 | 16 | | Wild material | | 2169891 | NA 87838 |
| 96 | NA 87839 | TRX241117-04NC | Ilex cassine L. | North Carolina, United States | NA | | | 2024 | COLLECTED | 11/17/2024 | Boiling Spring Lakes Community Center nature trail. | 34.02040000, -78.06469000 | 16 | | Wild material | | 2169892 | NA 87839 |
| 97 | NA 87840 | TRX241117-05NC | Ilex cassine L. | North Carolina, United States | NA | | | 2024 | COLLECTED | 11/17/2024 | Boiling Spring Lakes Community Center nature trail. | 34.02040000, -78.06469000 | 16 | | Wild material | | 2169893 | NA 87840 |
| 98 | NA 87842 | TRX241117-08SC | Ilex opaca Aiton | South Carolina, United States | NA | | | 2024 | COLLECTED | 11/17/2024 | Francis Marion National Forest. | 33.15167000, -79.60253000 | 31 | | Wild material | | 2169895 | NA 87842 |
| 99 | 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 |
| 100 | NA 88475 | TXWL2024-025 | Ilex coriacea (Pursh) Chapm. | Texas, United States | NA | | | 2024 | COLLECTED | 10/16/2024 | Sabine National Forest C-142. | | | Baygall below longleaf [pine] forest. | Wild material | | 2169441 | NA 88475 |
| 101 | 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 |
| 102 | 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 |
| 103 | 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 |
| 104 | NA 87824 | FL24-02 | Ilex cassine L. | Florida, United States | NA | | | 2024 | COLLECTED | 09/05/2024 | Wickham Park. | 28.17068273, -80.66140942 | | A very open, sandy, and xeric forest that rapidly turns wet and boggy where P. palustris (and Ilex cassine) occurs. EPA Ecoregion III: Southern Coastal Plain (75). EPA Ecoregion IV: Eastern Florida Flatwoods (75d). Geology: Anastasia Formation. Soil: Myakka Series Sand, 0 to 2 percent slopes. | Wild material | | 2168974 | NA 87824 |
| 105 | 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 |
| 106 | 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 |
| 107 | WLP 3429 | TJK2023FL-049 | Persea palustris (Raf.) Sarg. | Florida, United States | NA | | | 2024 | COLLECTED | 01/07/2024 | 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). | 30.41000000, -86.92940000 | 11 | Successional flatwoods, forested wetlands, depressional wetland. Slope: less than 2%. Aspect: South Elevation: 36 feet. | Wild material | | 2165768 | WLP 3429 |
| 108 | NA 88851 | TJK2023FL-046 | Aronia arbutifolia (L.) Pers. | Florida, United States | NA |  | | 2024 | COLLECTED | 12/26/2023 | George Washington Swamp, Highway 98, approximately 0.1 miles west of Twine Rd. | 29.77650000, -85.27540000 | 5 | Roadside. Wet wooded edge running along George Washington Swamp bottom. Slope: less than 4%. Aspect: South-southwest. Elevation: 16 feet. | Wild material | | 2165706 | NA 88851 |
| 109 | NA 88852 | TJK2023FL-047 | Ilex glabra (L.) A. Gray | Florida, United States | NA | | | 2024 | COLLECTED | 12/26/2023 | South of Highway 98, west of Twine Road. Track has a very large powerline right-of-way to the east, and George Washington Swamp bottom to the west. | 29.77640000, -85.27410000 | 6 | Longleaf Pine-Saw Palmetto. This area appears to be declining in quality, as witnessed by the declining in Rhododendron stem/plant density. Possible contributing issues: lacking necessary fire regime, has not seen fire in 8-10 years, encroaching woody shrub layer, accumulating organic matter (pine needle), expanding tree canopy, Hurricane Michael. Slope: less than 7%. Aspect: West. Elevation: 20 feet. | Wild material | | 2165707 | NA 88852 |
| 110 | NA 88853 | TJK2023FL-048 | Lyonia ferruginea (Walter) Nutt. | Florida, United States | NA | | | 2024 | COLLECTED | 12/26/2023 | South of Highway 98, west of Twine Road. Track has a very large powerline right-of-way to the east, and George Washington Swamp bottom to the west. | 29.77560000, -85.27400000 | 6 | Longleaf Pine-Saw Palmetto. This area appears to be declining in quality, as witnessed by the declining in Rhododendron stem/plant density. Possible contributing issues: lacking necessary fire regime, has not seen fire in 8-10 years, encroaching woody shrub layer, accumulating organic matter (pine needle), expanding tree canopy, Hurricane Michael. Slope: less than 2%. Aspect: Northeast. Elevation: 20 feet. | Wild material | | 2165708 | NA 88853 |
| 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 88830 | RJL-RM2023FLAL-004 | Morella caroliniensis (Mill.) Small | Florida, United States | NA | | | 2023 | COLLECTED | 12/05/2023 | Yellow River Wildlife Management Area, along DOF [Department of Forestry] Y15 dirt road. | 30.62822600, -86.83975700 | 6 | Growing in sun in moist to wet flat woods along the side of the dirt road in shallow ditches on the edges of the longleaf pine forest. The nearby 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 | | 2165660 | NA 88830 |
| 113 | NA 88831 | Serrulatum Group | Rhododendron viscosum (L.) Torr. | Florida, United States | NA | | | 2023 | COLLECTED | 12/05/2023 | Yellow River Wildlife Management Area, along DOF [Department of Forestry] Y15 dirt road. | 30.62897100, -86.84116800 | 6 | Growing in sun in moist to wet flat woods along the side of the dirt road in shallow ditches on the edges of the longleaf pine forest. The nearby 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 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.) | Wild material | Full name: Rhododendron viscosum Serrulatum Group. Received as Rhododendron serrulatum. | 2165661 | NA 88831 |
| 114 | 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 |
| 115 | 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 |
| 116 | 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 |
| 117 | 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 |
| 118 | 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 |
| 119 | NA 88840 | RJL-RM2023FLAL-014 | Rhododendron viscosum (L.) Torr. | Florida, United States | NA | | | 2023 | COLLECTED | 12/11/2023 | Property of Floyd Griffith off View Drive on the southwest side of McCormick Lake. | 30.63247000, -85.33718200 | 56 | Plants are growing primarily in part shade a few meters above the lake, generally in areas that appear dry, but clearly are associated with hillside seeps. While much of the area has been cultivated, the remnant native flora are largely broadleaved evergreen shrub and deciduous shrub and tree species. 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 surface soil profile of this area is primarily Pamlico-Pantego-Rutlege Association. 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. The Pantego series consists of very deep, very poorly drained, moderately permeable soils that formed in thick loamy sediments on the Southern Coastal Plain and Atlantic Coast Flatwoods. Slopes are less than 2 percent. This soil is strongly acid. 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. (Source: NRCS Web Soil Survey.) | Wild material | | 2165670 | NA 88840 |
| 120 | NA 88841 | RJL-RM2023FLAL-015 | Pinckneya bracteata (W. Bartram) Raf. | Florida, United States | NA | | | 2023 | COLLECTED | 12/11/2023 | West side of Marville Drive on the edge of the woodlands just a few hundred feet south of Fairway Drive. | 30.60665300, -85.32572200 | 79 | Plants are growing on the edge of a wetland acid habitat in the transitional zone between the obligate and facultative zones. They are growing in part-shade to shade with lower woody competition due to the moist conditions. 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 Pamlico-Pantego-Rutlege Association. 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. The Pantego series consists of very deep, very poorly drained, moderately permeable soils that formed in thick loamy sediments on the Southern Coastal Plain and Atlantic Coast Flatwoods. Slopes are less than 2 percent. This soil is strongly acid. 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. (Source: NRCS Web Soil Survey.) | Wild material | | 2165671 | NA 88841 |
| 121 | NA 88842 | RJL-RM2023FLAL-016 | Pinckneya bracteata (W. Bartram) Raf. | Florida, United States | NA | | | 2023 | COLLECTED | 12/11/2023 | West side of Scott Road in woodlands approximately 0.13 kilometers north of where the road crosses Ecofina Creek. As of 2023, this road appears permanently closed from previous hurricane damage. | 30.55633300, -85.43520000 | 38 | Plants are growing in the understory of a mixed evergreen and deciduous bottomland forest associated with the Ecofina Creek. Plans are growing mostly on hummocks in a very wet, acidic wetland habitat. Slope: N/A. Aspect: N/A. 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 Pamlico-Pantego-Rutlege Association. 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. The Pantego series consists of very deep, very poorly drained, moderately permeable soils that formed in thick loamy sediments on the Southern Coastal Plain and Atlantic Coast Flatwoods. Slopes are less than 2 percent. This soil is strongly acid. 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. (Source: NRCS Web Soil Survey.) | Wild material | | 2165672 | NA 88842 |
| 122 | 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 |
| 123 | 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 |
| 124 | WLP 3377 | TXWL2023-024 | Viburnum dentatum L. | Texas, United States | NA | | | 2023 | COLLECTED | 12/13/2023 | Roadside between Big Cow Creek and Hardy Cemetery. | 31.03548900, -93.85086800 | | Roadside; mesic, mixed hardwood/pine forest. | Wild material | | 2165656 | WLP 3377 |
| 125 | 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 |
| 126 | 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 |
| 127 | NA 88823 | TJK2023FL-040 | Cyrilla racemiflora L. | Florida, United States | NA | | | 2023 | COLLECTED | 12/11/2023 | Eglin Air Force Base, Range Road 352, south of Basin Bayou Reservation Area, north of Alaqua Bayou. | 30.48550000, -86.22020000 | 4 | Wet pine flatwoods. Slope: 3%. Aspect: Southeast. Elevation: 14 feet. | Wild material | | 2165652 | NA 88823 |
| 128 | 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 |
| 129 | NA 88690 | RJL2023NJ-003 | Ilex verticillata (L.) A. Gray | 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 below the dam at the far end of McCarthys Lakes. Plants accessed by foot along trails throughout property. | 39.57407200, -74.92518600 | 28 | 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. The area appears to be inundated year-round with plants growing on low mounds surrounded by obligate wetland species. 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 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 | | 2159118 | NA 88690 |
| 130 | NA 88691 | RJL2023NJ-004 | Ilex laevigata (Pursh) A. Gray | 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 below the dam at the far end of McCarthys Lakes. Plants accessed by foot along trails throughout property. | 39.57404200, -74.92523700 | 28 | 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. The area appears to be inundated year-round with plants growing on low mounds surrounded by obligate wetland species. 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 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 | | 2159119 | NA 88691 |
| 131 | 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 |
| 132 | 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 |
| 133 | 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 |
| 134 | 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 |
| 135 | NA 88698 | RJL2023NCSC-003 | Ilex laevigata (Pursh) A. Gray | North Carolina, United States | NA | | | 2023 | COLLECTED | 11/13/2023 | Sandhills Game Land: north side of Pulpwood Road approximately 0.11 km southwest of the junction with Tyner Road. | 34.95939500, -79.48676300 | 114 | Plants growing in shade to part-shade of a spring fed wetland that is a mixed evergreen and deciduous woodland habitat. Slope: 3 to 10 percent. Aspect: Northeast. The underlying geology of this area is of Tertiary origin and characterized as Pinehurst Formation. It is comprised of sand that is medium- to coarse-grained, cross-bedding and rhythmic bands of clayey sand common, unconsolidated. (Source: USGS North Carolina Geologic Map Data.) The primary soil type in the area of this collection is classified as Pelion loamy sand, 6 to 10 percent slopes. Pelion Series soils are very deep, moderately well-drained soils with moderately slow to slow permeability. The upper 30 cm of the strata is sandy loam to sandy clay loam ranging from grayish brown to reddish yellow. This stratum has a weak fine granular structure and is very friable. It contains many fine roots and is moderately acid. Deeper strata to 2 m range from yellow to yellowish red sandy clay, often with masses of oxidized iron and few fine prominent light gray iron depletions; they are strongly acid. (Source: NRCS Web Soil Survey.) | Wild material | | 2159126 | NA 88698 |
| 136 | NA 88699 | RJL2023NCSC-004 | Lyonia ligustrina (L.) DC. | North Carolina, United States | NA | | | 2023 | COLLECTED | 11/13/2023 | Sandhills Game Land: north side of Pulpwood Road approximately 0.11 km southwest of the junction with Tyner Road. | 34.95949000, -79.48665600 | 107 | Plants growing in part-shade to sun on the moist margins of a spring fed wetland that is a mixed evergreen and deciduous woodland habitat. The underlying soils are moist even during dry periods due to seepage from the wetland. Slope: 3 to 10 percent. Aspect: Northeast. The underlying geology of this area is of Tertiary origin and characterized as Pinehurst Formation. It is comprised of sand that is medium- to coarse-grained, cross-bedding and rhythmic bands of clayey sand common, unconsolidated. (Source: USGS North Carolina Geologic Map Data.) The primary soil type in the area of this collection is classified as Pelion loamy sand, 6 to 10 percent slopes. Pelion Series soils are very deep, moderately well-drained soils with moderately slow to slow permeability. The upper 30 cm of the strata is sandy loam to sandy clay loam ranging from grayish brown to reddish yellow. This stratum has a weak fine granular structure and is very friable. It contains many fine roots and is moderately acid. Deeper strata to 2 m range from yellow to yellowish red sandy clay, often with masses of oxidized iron and few fine prominent light gray iron depletions; they are strongly acid. (Source: NRCS Web Soil Survey.) | Wild material | | 2159127 | NA 88699 |
| 137 | NA 88700 | RJL2023NCSC-005 | Clethra alnifolia L. | North Carolina, United States | NA | | | 2023 | COLLECTED | 11/13/2023 | Sandhills Game Land: north side of Pulpwood Road approximately 0.11 km southwest of the junction with Tyner Road. | 34.96008500, -79.48751100 | 108 | Plants growing in shade to part-shade as well as sun (when moisture is abundant) of a spring fed wetland that is comprised of a mixed evergreen and deciduous woodland habitat. Slope: 3 to 10 percent. Aspect: Various. : The underlying geology of this area is of Cretaceous origin and characterized as Middendorf Formation. It is characterized by sand, sandstone, and mudstone, gray to pale gray with an orange cast, mottled; clay balls and iron-cemented concretions common, beds laterally discontinuous, cross-bedding common. (Source: USGS North Carolina Geologic Map Data.) The primary soil type in the area of this collection is classified as Pelion loamy sand, 6 to 10 percent slopes. Pelion Series soils are very deep, moderately well-drained soils with moderately slow to slow permeability. The upper 30 cm of the strata is sandy loam to sandy clay loam ranging from grayish brown to reddish yellow. This stratum has a weak fine granular structure and is very friable. It contains many fine roots and is moderately acid. Deeper strata to 2 m range from yellow to yellowish red sandy clay, often with masses of oxidized iron and few fine prominent light gray iron depletions; they are strongly acid. (Source: NRCS Web Soil Survey.) | Wild material | | 2159128 | NA 88700 |
| 138 | NA 88701 | RJL2023NCSC-006 | Zenobia pulverulenta (W. Bartram ex Willd.) Pollard | North Carolina, United States | NA | | | 2023 | COLLECTED | 11/13/2023 | Sandhills Game Land: north side of Pulpwood Road approximately 0.11 km southwest of the junction with Tyner Road. | 34.96066900, -79.48735300 | 111 | Plants growing in moist-mesic to seasonally saturated soils in part-shade of a spring fed wetland that is a mixed evergreen and deciduous woodland habitat. Slope: 0 to 5 percent. Aspect: Northeast. The underlying geology of this area is of Tertiary origin and characterized as Pinehurst Formation. It is comprised of sand that is medium- to coarse-grained, cross-bedding and rhythmic bands of clayey sand common, unconsolidated. (Source: USGS North Carolina Geologic Map Data.) The primary soil type in the area of this collection is classified as Pelion loamy sand, 6 to 10 percent slopes. Pelion Series soils are very deep, moderately well-drained soils with moderately slow to slow permeability. The upper 30 cm of the strata is sandy loam to sandy clay loam ranging from grayish brown to reddish yellow. This stratum has a weak fine granular structure and is very friable. It contains many fine roots and is moderately acid. Deeper strata to 2 m range from yellow to yellowish red sandy clay, often with masses of oxidized iron and few fine prominent light gray iron depletions; they are strongly acid. (Source: NRCS Web Soil Survey.) | Wild material | | 2159129 | NA 88701 |
| 139 | NA 88702 | RJL2023NCSC-007 | Rhododendron viscosum (L.) Torr. | North Carolina, United States | NA | | | 2023 | COLLECTED | 11/13/2023 | Sandhills Game Land: north side of Pulpwood Road approximately 0.11 km southwest of the junction with Tyner Road. | 34.96080300, -79.48730200 | 113 | Plants growing in moist-mesic to seasonally saturated soils in shade to part-shade of a spring fed wetland that is a mixed evergreen and deciduous woodland habitat. Prescribed fires have burned a portion of the wetland edge where plants are resprouting vigorously. Slope: 0 to 5 percent. Aspect: Norhteast. The underlying geology of this area is of Tertiary origin and characterized as Pinehurst Formation. It is comprised of sand that is medium- to coarse-grained, cross-bedding and rhythmic bands of clayey sand common, unconsolidated. (Source: USGS North Carolina Geologic Map Data.) The primary soil type in the area of this collection is classified as Pelion loamy sand, 6 to 10 percent slopes. Pelion Series soils are very deep, moderately well-drained soils with moderately slow to slow permeability. The upper 30 cm of the strata is sandy loam to sandy clay loam ranging from grayish brown to reddish yellow. This stratum has a weak fine granular structure and is very friable. It contains many fine roots and is moderately acid. Deeper strata to 2 m range from yellow to yellowish red sandy clay, often with masses of oxidized iron and few fine prominent light gray iron depletions; they are strongly acid. (Source: NRCS Web Soil Survey.) | Wild material | | 2159130 | NA 88702 |
| 140 | NA 88703 | RJL2023NCSC-008 | Lyonia lucida (Lam.) K. Koch | North Carolina, United States | NA | | | 2023 | COLLECTED | 11/13/2023 | Sandhills Game Land: north side of Pulpwood Road approximately 0.11 km southwest of the junction with Tyner Road. | 34.95848900, -79.48618700 | 101 | Plants growing in moist-mesic to seasonally saturated soils in shade to part-shade of a spring fed wetland that is a mixed evergreen and deciduous woodland habitat. Slope: 0 to 5 percent. Aspect: Various. The underlying geology of this area is of Tertiary origin and characterized as Pinehurst Formation. It is comprised of sand that is medium- to coarse-grained, cross-bedding and rhythmic bands of clayey sand common, unconsolidated. (Source: USGS North Carolina Geologic Map Data.) The primary soil type in the area of this collection is classified as Pelion loamy sand, 6 to 10 percent slopes. Pelion Series soils are very deep, moderately well-drained soils with moderately slow to slow permeability. The upper 30 cm of the strata is sandy loam to sandy clay loam ranging from grayish brown to reddish yellow. This stratum has a weak fine granular structure and is very friable. It contains many fine roots and is moderately acid. Deeper strata to 2 m range from yellow to yellowish red sandy clay, often with masses of oxidized iron and few fine prominent light gray iron depletions; they are strongly acid. (Source: NRCS Web Soil Survey.) | Wild material | | 2159131 | NA 88703 |
| 141 | NA 88704 | RJL2023NCSC-009 | Rhododendron viscosum (L.) Torr. | North Carolina, United States | NA | | | 2023 | COLLECTED | 11/13/2023 | Sandhills Game Land: wetlands and moist depressions along Hoffman Road, Scotland County Road 1328, | 34.95510000, -79.51769700 | 112 | Plants are growing in sun in an acidic wetland habitat rich in sphagnum and other wetland species. The habitat is moist to wet year-round and periodically has surface runoff occurring; even so, this habitat can become quite dry during seasonal periods without rainfall. Slope: 2 to 3 percent. Aspect: Northeast. The underlying geology of this area is of Tertiary origin and characterized as Pinehurst Formation. It is comprised of medium- to coarse-grained sand as well as cross-bedding and rhythmic bands of clayey sand that are unconsolidated. (Source: USGS North Carolina Geologic Map Data.) The primary soil type in the collection area is classified as Pelion Loamy Sand (2 to 6 percent slopes). The Pelion Loamy Sand series consists of very deep, moderately well-drained marine deposits, fluviomarine deposits, and sand sheets. Permeability is moderately slow or slow. Surface layers 0-25 cm deep are comprised of loamy sand with a weak fine granular structure and are very friable. Deeper horizons are comprised of sandy loam, sandy clay loam, or clay loam in the upper part and includes sandy clay or clay in the deepest part. Soils are extremely acid to strongly acid. (Source: NRCS Web Soil Survey.) | Wild material | | 2159132 | NA 88704 |
| 142 | NA 88705 | RJL2023NCSC-010 | Zenobia pulverulenta (W. Bartram ex Willd.) Pollard | North Carolina, United States | NA | | | 2023 | COLLECTED | 11/13/2023 | Sandhills Game Land: wetlands and moist depressions along Hoffman Road, Scotland County Road 1328, | 34.95510000, -79.51769700 | 112 | Plants are growing in part-shade to sun in an acidic wetland habitat rich in sphagnum and other obligate wetland species. The habitat is moist to wet year-round and periodically has surface runoff occurring; even so, this habitat can become quite dry during seasonal periods without rainfall. Slope: 2 to 3 percent. Aspect: Northeast. The underlying geology of this area is of Tertiary origin and characterized as Pinehurst Formation. It is comprised of medium- to coarse-grained sand as well as cross-bedding and rhythmic bands of clayey sand that are unconsolidated. (Source: USGS North Carolina Geologic Map Data.) The primary soil type in the collection area is classified as Pelion Loamy Sand (2 to 6 percent slopes). The Pelion Loamy Sand series consists of very deep, moderately well-drained marine deposits, fluviomarine deposits, and sand sheets. Permeability is moderately slow or slow. Surface layers 0-25 cm deep are comprised of loamy sand with a weak fine granular structure and are very friable. Deeper horizons are comprised of sandy loam, sandy clay loam, or clay loam in the upper part and includes sandy clay or clay in the deepest part. Soils are extremely acid to strongly acid. (Source: NRCS Web Soil Survey.) | Wild material | | 2159133 | NA 88705 |
| 143 | NA 88706 | RJL2023NCSC-011 | Smilax laurifolia L. | North Carolina, United States | NA | | | 2023 | COLLECTED | 11/13/2023 | Sandhills Game Land: wetland associated with the West Prong of Juniper Creek on the north side of Whisky Still Road approximately 0.63 kilometers northeast of Hoffman Road, Scotland County Road 1328. | 34.95683200, -79.51146200 | 103 | Plants are growing in part-shade to sun in an acidic wetland habitat rich in sphagnum and other wetland species. The habitat is moist to wet year-round and periodically has surface runoff occurring; even so, this habitat can become quite dry during seasonal periods without rainfall. Slope: N/A. Aspect: N/A. The underlying geology of this area is of Tertiary origin and characterized as Pinehurst Formation. It is comprised of medium- to coarse-grained sand as well as cross-bedding and rhythmic bands of clayey sand that are unconsolidated. (Source: USGS North Carolina Geologic Map Data.) The primary soil type in the collection area is classified as Johnston Series soils, 0 to 2 percent slopes, frequently flooded. The Johnson Series consists of very deep, very poorly drained coarse-loamy, siliceous, active, acid, thermic Cumulic Humaquepts. The upper 0-75 cm is black, mucky loam that is friable and very strongly acid. The lower strata to 1.75 m is dark gray, loamy fine sand, single grained, loose and very strongly acid. (Source: NRCS Web Soil Survey.) | Wild material | | 2159134 | NA 88706 |
| 144 | NA 88707 | RJL2023NCSC-012 | Rhododendron viscosum (L.) Torr. | North Carolina, United States | NA | | | 2023 | COLLECTED | 11/13/2023 | Sandhills Game Land: wetland associated with the West Prong of Juniper Creek on the north side of Whisky Still Road approximately 0.63 kilometers northeast of Hoffman Road, Scotland County Road 1328. | 34.95683200, -79.51146200 | 103 | Plants are growing in part-shade to sun in an acidic wetland habitat rich in sphagnum and other wetland species. The habitat is moist to wet year-round and periodically has surface runoff occurring; even so, this habitat can become quite dry during seasonal periods without rainfall. Slope: N/A. Aspect: N/A. The underlying geology of this area is of Tertiary origin and characterized as Pinehurst Formation. It is comprised of medium- to coarse-grained sand as well as cross-bedding and rhythmic bands of clayey sand that are unconsolidated. (Source: USGS North Carolina Geologic Map Data.) The primary soil type in the collection area is classified as Johnston Series soils, 0 to 2 percent slopes, frequently flooded. The Johnson Series consists of very deep, very poorly drained coarse-loamy, siliceous, active, acid, thermic Cumulic Humaquepts. The upper 0-75 cm is black, mucky loam that is friable and very strongly acid. The lower strata to 1.75 m is dark gray, loamy fine sand, single grained, loose and very strongly acid. (Source: NRCS Web Soil Survey.) | Wild material | | 2159135 | NA 88707 |
| 145 | NA 88708 | RJL2023NCSC-013 | Zenobia pulverulenta (W. Bartram ex Willd.) Pollard | North Carolina, United States | NA | | | 2023 | COLLECTED | 11/13/2023 | Wetlands associated with Bones Fork and accessed from Nursery Lane onto unnamed road. From Derby Road (Scotland Co Road 1003), turn west onto Nursery Lane and go 3.11 kilometers to unnamed road and turn right. Travel north along Bones Fork on foot for 0.11 kilometers to the collecting site. | 35.05753000, -79.61873900 | 108 | Plants growing in shade to part-shade of a moist to wet woodland habitat that is mostly evergreen and deciduous acidic habitat. Slope: N/A. Aspect: N/A. The underlying geology of this area is of Cretaceous origin and characterized as Middendorf Formation. It is composed of sand, sandstone, and mudstone, gray to pale gray with an orange cast, mottled; clay balls and iron-cemented concretions common, beds laterally discontinuous, cross-bedding common. (Source: USGS North Carolina Geologic Map Data.) The primary soil type in the collection area is classified as Ailey Series loamy sand, 8 to 15 percent slopes. The Ailey Series consists of moderately deep or deep to fragic soil properties and deep or very deep to densic materials. This soil is well drained or somewhat excessively drained. The upper layer (0-12.5 cm) of this soil is dark grayish brown loamy sand that is frequently dry. It has a weak fine granular structure, is very friable, non-sticky, non-plastic, and is strongly acid. The lower strata soils (12.5-90 cm) are yellowish brown loamy sand, with weak fine granular structure, very friable, non-sticky, non-plastic, and moderately acid. Deeper depths (below 90 cm) are characterized by slightly greater clay content that is slightly more plastic and strongly acid. (Source: NRCS Web Soil Survey.) | Wild material | | 2159136 | NA 88708 |
| 146 | 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 |
| 147 | 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 |
| 148 | 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 |
| 149 | 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 |
| 150 | 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 |
| 151 | NA 88715 | RJL2023NCSC-020 | Zenobia pulverulenta (W. Bartram ex Willd.) Pollard | South Carolina, United States | NA | | | 2023 | COLLECTED | 11/14/2023 | Francis Marion National Forest: plants growing in open wetlands/swamps on the south side of US Forest Service Road 5097 approximately 0.07 kilometers southwest of the junction with US Forest Service Road 223. | 33.06791000, -79.67213400 | 11 | Plants are growing in full sun to part-shade along the edges of an extensive acid wetland in seasonally inundated habitat. The vegetation, is a mix of evergreen and deciduous species; it is so dense that it is almost impenetrable. 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 Seewee Complex soils. The Seewee series consists of very deep, somewhat poorly drained, moderately rapidly permeable soils that formed in sandy marine sediments. Slopes range from 0 to 2 percent. The upper strata soil, 0-38 cm, is black, loamy fine sand, friable, and extremely acid. The lower strata soil, 38-75 cm, is fine sand, commonly mottled with shades of brown or yellow and very strongly acid to moderately acid. (Source: NRCS Web Soil Survey.) | Wild material | | 2159143 | NA 88715 |
| 152 | NA 88716 | RJL2023NCSC-021 | Ilex myrtifolia Walter | South Carolina, United States | NA | | | 2023 | COLLECTED | 11/14/2023 | Francis Marion National Forest: plants growing in a pond cypress-water tupelo swamp on the west side of Thompson Branch Road just south of the junction with Round Pond Road B. | 33.15167800, -79.60253700 | 31 | Plants are growing in part-shade to shade as understory trees among the pond cypress-water tupelo forest throughout the acid swamp which is seasonally inundated. The overstory is largely deciduous and comprised of pond cypress and water tupelo, while the understory is a mix of evergreen and deciduous broadleaved shrubs and understory trees. 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 Pickney Series loamy fine sand. The Pickney Series consists of very deep, very poorly drained, persistently wet, permeable soils that formed from marine or fluvial sediments. Slopes range from 0 to 2 percent. The upper strata soil, 0-75 cm, is black loamy fine sand that is very friable and extremely acid. The lower strata, 75-120 cm is dark gray fine sand with occasional white mottling, loose, and moderately acid. (Source: NRCS Web Soil Survey.) | Wild material | | 2159144 | NA 88716 |
| 153 | NA 88717 | RJL2023NCSC-022 | Ilex opaca Aiton | South Carolina, United States | NA | | | 2023 | COLLECTED | 11/14/2023 | Francis Marion National Forest: plants growing in a pond cypress-water tupelo swamp on the west side of Thompson Branch Road just south of the junction with Round Pond Road B. | 33.15161300, -79.60217900 | 22 | Plants are growing in part-shade to shade as understory trees among the pond cypress-water tupelo forest, mostly along the edges of the acid swamp which is seasonally inundated. The overstory is largely deciduous and comprised of pond cypress and water tupelo, while the understory is a mix of evergreen and deciduous broadleaved shrubs and understory trees. 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 Pickney Series loamy fine sand. The Pickney Series consists of very deep, very poorly drained, persistently wet, permeable soils that formed from marine or fluvial sediments. Slopes range from 0 to 2 percent. The upper strata soil, 0-75 cm, is black loamy fine sand that is very friable and extremely acid. The lower strata, 75-120 cm is dark gray fine sand with occasional white mottling, loose, and moderately acid. (Source: NRCS Web Soil Survey.) | Wild material | | 2159145 | NA 88717 |
| 154 | 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 |
| 155 | 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 |
| 156 | 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 |
| 157 | NA 88722 | RJL2023NCSC-027 | Kalmia angustifolia L. var. carolina (Small) Fernald | 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): Marsh Lake Road, 1.23 kilometers north of South Carolina Highway 917. | 34.15010900, -79.19136900 | 13 | Plants growing in part-shade to sun on the edge of an acid seasonally inundated depression as well as further away in longleaf pine understory. The site is currently dry but, based on the associated vegetation, has periods of moisture on or near the surface. 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 | | 2159150 | NA 88722 |
| 158 | NA 88723 | RJL2023NCSC-028 | Ilex myrtifolia Walter | North Carolina, United States | NA | | | 2023 | COLLECTED | 11/15/2023 | Juniper Creek State Game Lands (along Brunswick County Road 1340): swamps/wetlands associated with Juniper Creek. | 34.12438700, -78.39310700 | 13 | Plants growing in shade to part-shade of a swamp habitat along Juniper Creek. At the time of collection, the swamp was relatively dry with water found only in deep depressions. Slope: N/A. Aspect: N/A. The underlying geology of this area is of Cretaceous origin and characterized as Peedee Formation - Black Creek Group, undivided. The Peedee Formation is primarily unconsolidated, coarse-detrital, sand that is dark-green or gray, finely micaceous, more or less glauconitic, and argillitic sand, many layers of which are calcareous (impure limestone). Irregular concretionary masses of impure calcium carbonate occur in places. Dark marine clays are interstratified with sand. The Black Creek Group consists of irregularly bedded, laminated, carbonaceous clays and thin laminae and lenses of sand; lignite and pyrite present; glauconitic in places; massive interbedded layers of glauconitic sand present toward top of unit. Light-colored clays and coarse arkosic sands also found. (Source: USGS North Carolina Geologic Map Data.) The primary soil type in this collection area is classified as Dorovan Series muck. 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, Eastern Gulf Coast Flatwoods, and Southern Coastal Plain Major Land Resource Areas. They formed in highly decomposed acid-organic materials and have slopes that are less than 1 percent. (Source: NRCS Web Soil Survey.) | Wild material | | 2159151 | NA 88723 |
| 159 | NA 88682 | TJK2023FL-029 | Rhododendron canescens (Michx.) Sweet | Florida, United States | NA | | | 2023 | COLLECTED | 11/08/2023 | Blackwater State Forest, Hutton Tract. | 30.69037000, -86.88088000 | 32 | Rim of steephead. Slope: 20%. Aspect: Southwest. Elevation: 105 feet. | Wild material | | 2159094 | NA 88682 |
| 160 | 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 |
| 161 | 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 |
| 162 | WLP 3274 | TJK2023FL-022 | Smilax auriculata Walter | Florida, United States | NA | | | 2023 | COLLECTED | 10/20/2023 | Santa Rosa Island: White Sands Blvd, Navarre Beach at Santa Rosa Sound, soundside. | 30.37828000, -86.89761000 | 6 | First dunes off the sound. Slope: 30%. Aspect: West. Elevation: 21 feet. | Wild material | | 2159054 | WLP 3274 |
| 163 | WLP 3276 | TJK2023FL-024 | Crataegus lacrimata Small | Florida, United States | NA | | | 2023 | COLLECTED | 10/20/2023 | Santa Rosa Island: White Sands Blvd, Navarre Beach at Santa Rosa Sound, soundside. | 30.37843000, -86.89778000 | 5 | Base of the first dunes off the sound. Slope: 15%. Aspect: North. Elevation: 15 feet. | Wild material | | 2159056 | WLP 3276 |
| 164 | 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 |
| 165 | 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 |
| 166 | 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 |
| 167 | NA 89247 | Pulverulentus Group | Styrax americanus Lam. | Texas, United States | NA | | | 2023 | COLLECTED | 09/25/2023 | Along FM (Farm to Market Road) 943 roadside. | 30.46908000, -94.45061000 | | Roadside. Low area ordinarily with pooled water, absent due to unusually dry conditions during the year of collection. | Wild material | Full name as recorded at the U.S. National Arboretum: Styrax americanus Pulverulentus Group. | 2158801 | NA 89247 |
| 168 | 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 |
| 169 | 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 |
| 170 | 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 |
| 171 | NA 88662 | TJK2023FL-016 | Sideroxylon sp. | Florida, United States | NA | | | 2023 | COLLECTED | 09/16/2023 | East River Unit, Eglin Air Force Base. Near A-21 Rd. | 30.41250000, -86.77110000 | 7 | Xeric shrub, xeric sandhills community. Elevation: 26 feet. Slope: 2%. Aspect: South. | Wild material | | 2158796 | NA 88662 |
| 172 | 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 |
| 173 | NA 88606 | KY23-008 | Ilex montana Torr. & A. Gray | Kentucky, United States | NA | | | 2023 | COLLECTED | 09/09/2023 | Black Mountain summit (second location, bulked with the first: Black Mountain; lat/long 36. 91614, -82. 89873) | 36.91434000, -82.89463000 | 1261 | Moist woods. Elevation: 4138 feet. Aspect: West. (Second location, bulked with first: Elevation: 4071 feet. Aspect: West.) | Wild material | | 2158698 | NA 88606 |
| 174 | NA 88607 | KY23-009 | Hydrangea arborescens L. | Kentucky, United States | NA | | | 2023 | COLLECTED | 09/09/2023 | Black Mountain summit. | 36.91312000, -82.89516000 | 1257 | Moist woods. Elevation: 4124 feet. Aspect: South. | Wild material | | 2158699 | NA 88607 |
| 175 | NA 88609 | KY23-011 | Hamamelis virginiana L. | Kentucky, United States | NA | | | 2023 | COLLECTED | 09/09/2023 | Black Mountain summit: along roadside on Black Mountain (Lynch property). (Second location, bulked with first: Black Mountain summit.) | 36.91584000, -82.89479000 | 1241 | Along roadside. Elevation: 4072 feet. Aspect: Northwest. (Second location, bulked with first: Elevation: 4120 feet. Aspect: North.) | Wild material | | 2158701 | NA 88609 |
| 176 | NA 88611 | KY23-013 | Acer pensylvanicum L. | Kentucky, United States | NA | | | 2023 | COLLECTED | 09/09/2023 | Black Mountain summit, along gas pipeline road. | 36.91742000, -82.90279000 | 1237 | Along gas line trail. Elevation: 4058 feet. Aspect: Southwest. | Wild material | | 2158703 | NA 88611 |
| 177 | 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 |
| 178 | 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 |
| 179 | NA 88628 | KY23-031 | Rhododendron arborescens (Pursh) Torr. | Kentucky, United States | NA | | | 2023 | COLLECTED | 09/11/2023 | Daniel Boone National Forest: Bee Rock Loop Trail along Rockcastle River. | 37.03497974, -84.30580649 | 229 | Riverscour grassland, edge of river, river scour/boulder pile. Elevation: 750 feet. Aspect: Southeast. | Wild material | | 2158720 | NA 88628 |
| 180 | NA 88630 | KY23-033 | Rhododendron periclymenoides (Michx.) Shinners | Kentucky, United States | NA | | | 2023 | COLLECTED | 09/11/2023 | Daniel Boone National Forest: Bee Rock Loop Trail along Rockcastle River. | 37.03537000, -84.30551000 | 229 | Riverscour grassland, edge of river, river scour/boulder pile. Elevation: 750 feet. Aspect: Southeast. | Wild material | Initial identification: Rhododendron periclymenoides aff. | 2158722 | NA 88630 |
| 181 | NA 88644 | KY23-047 | Stewartia ovata (Cav.) Weath. | Kentucky, United States | NA | | | 2023 | COLLECTED | 09/12/2023 | Cumberland Falls Trail #2. | 36.83847000, -84.33115000 | 271 | Elevation: 889 feet. Aspect: South. | Wild material | | 2158736 | NA 88644 |
| 182 | WLP 3213 | TXWL2023-001 | Lyonia mariana (L.) D. Don | Texas, United States | NA | | | 2023 | COLLECTED | 08/22/2023 | Angelina National Forest. | 31.05522100, -94.26205200 | | Baygall below longleaf [pine] stand. | Wild material | | 2158757 | WLP 3213 |
| 183 | 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 |
| 184 | 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 |
| 185 | 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 |
| 186 | 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 |
| 187 | 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 |
| 188 | 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 |
| 189 | NA 89263 | TJK2023FL-001 | Smilax laurifolia L. | Florida, United States | NA | | | 2023 | COLLECTED | 01/18/2023 | Midway, Florida: Pensacola State College, 1/4 mile south of Highway 98, west of main road towards main building. | 30.39570000, -87.01300000 | 8 | Ilex myrtifolia depressional wetland. Slope: 2%. Aspect: Southeast. Elevation recorded as 25 feet. | Wild material | WLPGR contract collection. | 2158246 | NA 89263 |
| 190 | NA 89271 | TJK2023FL-009 | Vaccinium stamineum L. | Florida, United States | NA | | | 2023 | COLLECTED | 07/16/2023 | Eglin Air Force Base: Weaver Creek area west of Highway 87, north of Choctaw Nolf Airfield Road (Escrobano Point). | 30.50710000, -86.91220000 | 33 | Xeric oak-pine uplands above Weaver Creek Bayhead. Slope: 5%. Aspect: Northwest. Elevation recorded as 107 feet. | Wild material | WLPGR contract collection. | 2158254 | NA 89271 |
| 191 | Ames 36155 | JDC/MM/2023/052/1084 | Monarda maxmedleyi J. J. N. Campb. & Floden | Kentucky, United States | NC7 |  | | 2023 | COLLECTED | 08/09/2023 | Star Gap Road between Red River and Campton Road located 3.0 miles north, northwest of Slade | 37.83158300, -83.72674500 | 265 | Edges of woods/roadsides. Localized to west and southeast facing slopes. | Wild material | Plants measuring 12-18" in height. Spreading vegetatively via rhizomes. Most specimens had pale pink flowers with some having white flowers. Peak flowering at collection site occurred near 29th of May (2023). | 2158360 | Ames 36155 |
| 192 | OPGC 8851 | AS/OF/2023/068/278 | Oenothera fruticosa L. subsp. glauca (Michx.) Straley | Kentucky, United States | OPGC |  | | 2023 | COLLECTED | 08/09/2023 | Star Gap Road between Red River and Campton Road located 3.0 miles north, northwest of Slade | 37.83158300, -83.72674500 | 260 | Edges of woods/roadsides. Localized to west and southeast facing slopes. | Wild material | Plants in nature measuring approximately 3.0' in height. Bright yellow flowers peaking in early June (central Kentucky) measuring approximately 1-2" across. | 2158361 | OPGC 8851 |
| 193 | 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 |
| 194 | WLP 3087 | RM2023-005 | Rhododendron minus Michx. var. minus | Alabama, United States | NA | | | 2023 | COLLECTED | 12/29/2022 | This plant is growing along the edges of Gantt Lake, accessed by boat. Occasional in shaded areas around Gantt Lake. | 31.40780000, -86.46770000 | 68 | The plants were growing in open conditions on a steep north-facing bluff above Gantt Lake.
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 surface soil profile of this area is primarily Eunola Series Loamy Fine Sand (0 to 2 percent slopes, rarely flooded). The Eunola series consists of very deep, moderately well drained, moderately permeable loamy soils that formed in fluvial or marine sediments. They are on low stream or marine terraces of the Southern Coastal Plain. They are strongly acid. Slopes are dominantly 0 to 3 percent but range up to 6 percent.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2141441 | WLP 3087 |
| 195 | WLP 3088 | RM2023-006 | Kalmia latifolia L. | Alabama, United States | NA | | | 2023 | COLLECTED | 12/29/2022 | This plant is growing along the edges of Gantt Lake, accessed by boat. Occasional in shaded areas around Gantt Lake. | 31.40780000, -86.46770000 | 68 | The plants were growing in open conditions on a steep north-facing bluff above Gantt Lake.
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 surface soil profile of this area is primarily Eunola Series Loamy Fine Sand (0 to 2 percent slopes, rarely flooded). The Eunola series consists of very deep, moderately well drained, moderately permeable loamy soils that formed in fluvial or marine sediments. They are on low stream or marine terraces of the Southern Coastal Plain. They are strongly acid. Slopes are dominantly 0 to 3 percent but range up to 6 percent.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2141442 | WLP 3088 |
| 196 | WLP 3089 | RM2023-007 | Oxydendrum arboreum (L.) DC. | Alabama, United States | NA | | | 2023 | COLLECTED | 12/29/2022 | This plant is growing along the edges of Gantt Lake, accessed by boat. Occasional around Gantt Lake. | 31.41156000, -86.46920000 | 70 | The plants were growing in open sunny conditions on a steep east-facing bluff above Gantt Lake.
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 surface soil profile of this area is primarily Eunola Series Loamy Fine Sand (0 to 2 percent slopes, rarely flooded). The Eunola series consists of very deep, moderately well drained, moderately permeable loamy soils that formed in fluvial or marine sediments. They are on low stream or marine terraces of the Southern Coastal Plain. They are strongly acid. Slopes are dominantly 0 to 3 percent but range up to 6 percent.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2141443 | WLP 3089 |
| 197 | WLP 3090 | RM2023-008 | Lyonia lucida (Lam.) K. Koch | Alabama, United States | NA | | | 2023 | COLLECTED | 12/29/2022 | This plant is growing along the steep edges of Gantt Lake, accessed by boat. Occasional in shaded areas around Gantt Lake. | 31.40780000, -86.46770000 | 68 | The plants were growing in open conditions on a steep north-facing bluff above Gantt Lake.
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 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 | | 2141444 | WLP 3090 |
| 198 | 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 |
| 199 | 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 |
| 200 | NA 87348 | TJK2022FL-003 | Quercus chapmanii Sarg. | Florida, United States | NA | | | 2023 | COLLECTED | 11/01/2022 | Okaloosa County: Eglin Air Force Base: East River Unit H-3, Range Road 259, north of Highway 98. | 30.41220000, -86.77320000 | 0 | Xeric Scrub/Upland Sandhill community. | Wild material | Received as Quercus chapmanii; accessioned at U.S. National Arboretum under that name. | 2141639 | NA 87348 |
| 201 | NA 87349 | TJK2022FL-004 | Cartrema americana (L.) G. L. Nesom | Florida, United States | NA | | | 2023 | COLLECTED | 11/02/2022 | Okaloosa County: Eglin Air Force Base: East River Unit H-3, Range Road 259, north of Highway 98. | 30.41300000, -86.77480000 | 0 | A wet stringer surrounded by Xeric Scrub/Upland Sandhill community. | Wild material | | 2141640 | NA 87349 |
| 202 | NA 87350 | TJK2022FL-005 | Ilex ambigua Torr. | Florida, United States | NA | | | 2023 | COLLECTED | 11/02/2022 | Okaloosa County: Eglin Air Force Base: East River Unit H-3, Range Road 259, north of Highway 98. | 30.41190000, -86.77320000 | 0 | Xeric Scrub/Upland Sandhill community. | Wild material | | 2141641 | NA 87350 |
| 203 | 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 |
| 204 | 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 |
| 205 | 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 |
| 206 | NA 88527 | RM-TK2022-015 | Rhododendron viscosum (L.) Torr. | Florida, United States | NA | | | 2023 | COLLECTED | 11/06/2022 | Along Florida Department of Forestry Road Y15, Yellow River Wildlife Management Area | 30.62820000, -86.83870000 | 7 | 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 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 (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2140808 | NA 88527 |
| 207 | NA 88530 | RJLSEUS2022-001 | Oxydendrum arboreum (L.) DC. | North Carolina, United States | NA | | | 2023 | COLLECTED | 12/06/2022 | Plants growing around a wetland on both sides of Scotland Lake Road, approximately 1.1 kilometers southwest of the junction with Hoffman Road (Scotland Co. Road 1328) in the Sandhills Game Lands. This plant is a common component along the mesic/moist boundary on the upper edge of the understory shrub in the moist woodland habitat not far from the wetland. | 34.98402000, -79.54267200 | 116 | Plants are growing in full sun to part-shade in the moist, well-drained, mesic conditions just above a wetland area occupied by obligate wetland species. The underlying geology of this area is of Tertiary origin and characterized as Pinehurst Formation. It is composed of medium- to coarse-grained sand as well as cross-bedding and rhythmic bands of clayey sand that are unconsolidated.
Source: USGS North Carolina Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=NCTp%3B11)
The primary soil type in the collection area is Pelion Loamy Sand soil (6 to 10 percent slopes). The Pelion Loamy Sand series consists of very deep, moderately well-drained marine deposits, fluviomarine deposits, and sand sheets. Permeability is moderately slow or slow. Surface layers 0-25 cm deep are comprised of loamy sand with a weak fine granular structure and are very friable. Deeper horizons are comprised of sandy loam, sandy clay loam, or clay loam in the upper part and include sandy clay or clay in the deepest strata. Soils are extremely acid to strongly acid.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2140759 | NA 88530 |
| 208 | NA 88531 | RJLSEUS2022-002 | Cyrilla racemiflora L. | North Carolina, United States | NA | | | 2023 | COLLECTED | 12/06/2022 | Plants growing around a wetland on both sides of Scotland Lake Road, approximately 1.1 kilometers southwest of the junction with Hoffman Road (Scotland Co. Road 1328) in the Sandhills Game Lands. This plant is a common component of moist to wet areas of the wetland habitats in this area. | 34.98418000, -79.54079800 | 120 | Plants are growing in part-shade to sun in a wetland habitat as well as nearby seasonally drier mesic habitat.
Soils: The underlying geology of this area is of Tertiary origin and characterized as Pinehurst Formation. It is comprised of medium- to coarse-grained sand as well as cross-bedding and rhythmic bands of clayey sand that are unconsolidated.
Source: USGS North Carolina Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=NCTp%3B11)
The primary soil type in the collection area is classified as Johnston Series soils (0 to 2 percent slopes, frequently flooded). The Johnston series consists of very deep, very poorly drained soils that are occasionally to frequently flooded for short to extended periods. Permeability is moderate to rapid. These nearly level soils are alluvial in origin and typical of floodplains and swamp. Slopes range from 0 to 2 percent. Johnston Series soils are comprised of mucky loam that is friable with siliceous elements in the upper 0-75 cm. Lower strata range in percentages of mucky loam and loamy fine sand.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2140760 | NA 88531 |
| 209 | NA 88532 | RJLSEUS2022-003 | Alnus serrulata (Aiton) Willd. | North Carolina, United States | NA | | | 2023 | COLLECTED | 12/06/2022 | Plants growing around a wetland on both sides of Scotland Lake Road, approximately 1.1 kilometers southwest of the junction with Hoffman Road (Scotland Co. Road 1328) in the Sandhills Game Lands. This plant is a common component of the moist to wet areas of the wetland habitats in this area. | 34.98413200, -79.54196300 | 118 | Plants are growing in part-shade to sun in a wet to inundated habitat that contains standing water and/or significant moisture year-round.
Soils: The underlying geology of this area is of Tertiary origin and characterized as Pinehurst Formation. It is comprised of medium- to coarse-grained sand as well as cross-bedding and rhythmic bands of clayey sand that are unconsolidated.
Source: USGS North Carolina Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=NCTp%3B11)
The primary soil type in the collection area is classified as Johnston Series soils (0 to 2 percent slopes, frequently flooded). The Johnston series consists of very deep, very poorly drained soils that are occasionally to frequently flooded for short to extended periods. Permeability is moderate to rapid. These nearly level soils are alluvial in origin and typical of floodplains and swamp. Slopes range from 0 to 2 percent. Johnston Series soils are comprised of mucky loam that is friable with siliceous elements in the upper 0-75 cm. Lower strata range in percentages of mucky loam and loamy fine sand.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2140761 | NA 88532 |
| 210 | NA 88533 | RJLSEUS2022-004 | Zenobia pulverulenta (W. Bartram ex Willd.) Pollard | North Carolina, United States | NA | | | 2023 | COLLECTED | 12/06/2022 | Plants growing in the wetlands and moist depressions along Scotland Co. Road 1328 in the Sandhills Game Lands. This plant is somewhat infrequent and sporadic, but abundant in places with moist to wet habitats in this area. | 34.95510000, -79.51769700 | 112 | Plants are growing in part-shade to sun in an acidic wetland habitat rich in sphagnum and other obligate wetland species. The habitat is moist to wet year-round and periodically has surface runoff occurring; even so, this habitat can become quite dry during seasonal periods without rainfall.
Soils: The underlying geology of this area is of Tertiary origin and characterized as Pinehurst Formation. It is comprised of medium- to coarse-grained sand as well as cross-bedding and rhythmic bands of clayey sand that are unconsolidated.
Source: USGS North Carolina Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=NCTp%3B11)
The primary soil type in the collection area is classified as Pelion Loamy Sand (2 to 6 percent slopes). The Pelion Loamy Sand series consists of very deep, moderately well-drained marine deposits, fluviomarine deposits, and sand sheets. Permeability is moderately slow or slow. Surface layers 0-25 cm deep are comprised of loamy sand with a weak fine granular structure and are very friable. Deeper horizons are comprised of sandy loam, sandy clay loam, or clay loam in the upper part and includes sandy clay or clay in the deepest part. Soils are extremely acid to strongly acid.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2140762 | NA 88533 |
| 211 | 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 |
| 212 | 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 |
| 213 | 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 |
| 214 | 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 |
| 215 | NA 88539 | RJLSEUS2022-011 | Clethra tomentosa Lam. | Georgia, United States | NA | | | 2023 | COLLECTED | 12/08/2022 | Plants growing in the upper edges of a wetland in Longleaf pine forest on the north side of Old GA State Route 33, approximately 2.11 kilometers southwest of the junction with GA Hwy 33. Common at this site on the margins of the wetland community. | 31.42763000, -83.85190700 | 108 | Plants are growing in part-shade of a Longleaf pine forest along the upper edges of a wetland community. Soils range seasonally from moist to mucky with occasional standing water in depressions.
Soils: 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. Unit is characterized by in situ weathered feldspar and an abundance of quartzite gravel and cobbles.
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 Pelham Loamy Sand soil (0 to 2 percent slopes). The Pelham Series consists of very deep, poorly drained, moderately permeable soils that formed in unconsolidated Coastal Plain sediments. These soils are on nearly level broad flats, toe slopes, depressions and drainageways. Slopes range from 0 to 5 percent. These soils are comprised of loamy sands that are friable to a depth of approximately 1 meter and sandy clay loam to a depth in the lower strata to about 2 meters. They are also strongly acid.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2140766 | NA 88539 |
| 216 | 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 |
| 217 | 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 |
| 218 | 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 |
| 219 | 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 |
| 220 | NA 88547 | RJLSEUS2022-019 | Alnus serrulata (Aiton) Willd. | Alabama, United States | NA | | | 2023 | COLLECTED | 12/10/2022 | Poke Springs Branch inlet accessed by boat from Walter F. George Reservoir. Frequent plants. | 31.72236600, -85.12793700 | 63 | Plants are growing in full sun on the eroded bank of the lake. The plants have access to abundant moisture with root systems extended into the lake.
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 soils (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 | | 2140773 | NA 88547 |
| 221 | NA 88548 | RJLSEUS2022-020 | Morella cerifera (L.) Small | Alabama, United States | NA | | | 2023 | COLLECTED | 12/10/2022 | Poke Springs Branch inlet accessed by boat from Walter F. George Reservoir. Common frequency. | 31.72236600, -85.12793700 | 63 | Plants are growing in full sun on the eroded bank of the lake. The plants have access to abundant moisture with root systems extended into the lake.
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 soils (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 | | 2140774 | NA 88548 |
| 222 | 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 |
| 223 | 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 |
| 224 | 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 |
| 225 | 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 |
| 226 | 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 |
| 227 | 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 |
| 228 | 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 |
| 229 | 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 |
| 230 | 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 |
| 231 | 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 |
| 232 | NA 88561 | RJLSEUS2022-034 | Hydrangea quercifolia W. Bartram | Alabama, United States | NA | | | 2023 | COLLECTED | 12/12/2022 | Plants growing in the woodlands at Haines Island Park at the foot of Tallahatta cuesta, accessed by foot via Ferry Road. Common at this site. | 31.72178200, -87.46589600 | 66 | Plants are growing in part-shade to shade of a moist mesic, well-drained conditions on rocks and in the eroding matrix of the Tallahatta Questa.
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 | | 2140786 | NA 88561 |
| 233 | 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 |
| 234 | 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 |
| 235 | NA 88566 | RJLSEUS2022-039 | Rhododendron viscosum (L.) Torr. | Florida, United States | NA | | | 2023 | COLLECTED | 12/14/2022 | Plants growing in woodlands at Escribano Point Bayou Campground not far from the parking lot. Occasional. | 30.50990400, -87.00414900 | 1 | Plants are growing in shade to part-shade of dense mesic vegetation only a few meters from the edge of mixed evergreen and deciduous woodland associated with the Yellow River Marsh Aquatic Preserve. While this habitat is typical mesic and well-drained, it is clearly subject to periods of inundation from high tides or storms as it is a meter or less above the marsh habitat. Additionally, it seems likely that there is plentiful moisture further down in the soil profile based on some of the plant associates.
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 FL Map Data (https://mrdata.usgs.gov/geology/state/state.php?state=fl)
The primary soil types in the collection area are classified as Ortega Sand soils (0 to 5 percent slopes). The Ortega Series consists of very deep, moderately well drained soils that formed in a sandy deposit on marine terraces. These soils are on nearly level to strongly sloping upland landscapes. Slopes range from 0 to 12 percent. They are extremely acid to slightly acid throughout. They are fine sand or sand to depths of more than 2 meters. Silt plus clay totals less than 5 percent between 25 cm and 1 meter depth.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2140788 | NA 88566 |
| 236 | NA 88567 | RJLSEUS2022-040 | Chamaecyparis thyoides (L.) Britton et al. | Florida, United States | NA | | | 2023 | COLLECTED | 12/14/2022 | Plants growing in woodlands at Escribano Point Bayou Campground not far from the parking lot. Occasional. | 30.51018200, -87.00448800 | 1 | Plants are growing in part-shade of dense mesic vegetation only a few meters from the edge of mixed evergreen and deciduous woodland associated with the Yellow River Marsh Aquatic Preserve. While this habitat surface is typical mesic and well-drained, it is clearly subject to periods of inundation from high tides or storms as it is a meter or less above the marsh habitat. Additionally, it seems likely that there is plentiful moisture further down in the soil profile based on some of the plant associates.
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 FL Map Data (https://mrdata.usgs.gov/geology/state/state.php?state=fl)
The primary soil types in the collection area are classified as Ortega Sand soils (0 to 5 percent slopes). The Ortega Series consists of very deep, moderately well drained soils that formed in a sandy deposit on marine terraces. These soils are on nearly level to strongly sloping upland landscapes. Slopes range from 0 to 12 percent. They are extremely acid to slightly acid throughout. They are fine sand or sand to depths of more than 2 meters. Silt plus clay totals less than 5 percent between 25 cm and 1 meter depth.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2140789 | NA 88567 |
| 237 | 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 |
| 238 | 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 |
| 239 | 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 |
| 240 | 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 |
| 241 | 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 |
| 242 | 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 |
| 243 | 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 |
| 244 | 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 |
| 245 | 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 |
| 246 | 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 |
| 247 | WLP 2674 | RJL2022NJ-005 | Alnus serrulata (Aiton) Willd. | New Jersey, United States | NA | | | 2022 | COLLECTED | 10/24/2022 | Plants growing on the east side of Atlantic County Road 543, Green Bank Road, in wetlands of the Mullica River, approximately 1.01 kilometers southwest of the intersection with River Road in Green Bank, New Jersey. Plants are common but scattered on the east side of the road at this location. | 39.60472300, -74.59378100 | 2 | Plants grow in full sun to light shade throughout this permanently wet to inundated habitat that is comprised mostly of emergent and obligate wetland herbaceous plants, deciduous shrubs, and Chamaecyparis thyoides, none reaching more than 5-10 meters tall. There are small elevation changes throughout this wetland, but the location is surrounded by water year-round.
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 Manahawkin muck, 0 to 2 percent slopes, frequently flooded. This soil is moderately high to high in the organic layers and high in the mineral layers comprised of sandy or sandy-skeletal, siliceous, dysic, mesic terric haplosaprists. This soil is considered extremely acid or very strongly acid in the surface tier and very strongly acid or strongly acid in the lower tiers and in the mineral substratum. The mineral content of organic layers ranges from 5 to 80 percent. Organic layers consist of mostly sapric material. Some pedons have subhorizons or a surface horizon of hemic material up to 25 cm. Woody fragments range from 0 to 50 percent, by volume, in the organic layers. These fragments are mostly twigs, branches, or logs ranging in size from 3 mm to 51 cm in diameter and completely break down when rubbed or crushed. The depth of this soil ranges from 0.2-2 meters. This soil is considered wet to inundated year-round.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2139665 | WLP 2674 |
| 248 | 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 |
| 249 | 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 |
| 250 | 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 |
| 251 | 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 |
| 252 | 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 |
| 253 | 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 |
| 254 | 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 |
| 255 | 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 |
| 256 | WLP 2611 | 2022VA-02 | Euonymus americanus 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 uncommon at this location. | 36.73888200, -76.24327700 | 9 | Plant is 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. | Wild material | | 2139349 | WLP 2611 |
| 257 | 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 |
| 258 | 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 |
| 259 | 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 |
| 260 | 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 |
| 261 | 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 |
| 262 | 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 |
| 263 | 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 |
| 264 | WLP 2594 | RJL2022FLAL-016 | Stewartia malacodendron L. | Florida, United States | NA | | | 2022 | COLLECTED | 08/01/2022 | Woodlands at the north end of the parking lot at Chumukla Springs Boat Ramp to the Escambia River. | 30.83077100, -87.29754900 | 9 | Growing as an understory element in high understory dappled shade under well-drained conditions in mixed deciduous and evergreen flatwoods, surrounded by drainage areas and nearby marshlands of the Escambia River. 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 | | 2138704 | WLP 2594 |
| 265 | WLP 2595 | RJL2022FLAL-017 | Rhododendron austrinum (Small) Rehder | Florida, United States | NA | | | 2022 | COLLECTED | 08/01/2022 | Woodlands at the north end of the parking lot at Chumukla Springs Boat Ramp to the Escambia River. | 30.83079400, -87.29756200 | 9 | Growing as an understory element in high understory dappled shade under well-drained conditions in mixed deciduous and evergreen flatwoods, surrounded by drainage areas and nearby marshlands of the Escambia River. 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 | | 2138705 | WLP 2595 |
| 266 | 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 |
| 267 | W6 60456 | CA180-249 | Thysanocarpus curvipes Hook. | California, United States | W6 |  | | 2022 | | | | | | | Wild material | Small white to purple flowers born on a raceme; styles <.7mm. Leaves lanceolate, bases lobed, clasping. Stems fuzzy. Winged fruit pedicels in a continuous 1.5-12mm arc. Fruit, <6mm, entire, crenate or perforated. | 2138394 | W6 60456 |
| 268 | NA 88301 | NCBG-753 | Clethra alnifolia L. | North Carolina, United States | NA | | | 2021 | | | | | | | Wild material | | 2132950 | NA 88301 |
| 269 | OPGC 8368 | CA180-215 | Calochortus albus (Benth.) Douglas ex Benth. | California, United States | OPGC | | | 2021 | | | | | | | Wild material | White nodding flower can be pale pink. Nectary crescent shaped with yellow or white glandular hairs. Bracts lanceolate. Ovate sepals are paired with elliptic petals. Winged capsule turns from green to tan when dark seed are ripe. Green strappy leaves are basal from bulb as well as along flower stem. | 2120357 | OPGC 8368 |
| 270 | OPGC 8370 | CA180-220 | Clarkia purpurea (Curtis) A. Nelson & J. F. Macbr. subsp. quadrivulnera (Douglas ex Lindl.) F. H. Lewis & M. E. Lewis | California, United States | OPGC | | | 2021 | | | | | | | Wild material | Petals purple to wine red often with a contrasting purple spot in center or edge but highly variable. | 2120361 | OPGC 8370 |
| 271 | OPGC 8372 | CA180-225 | Clarkia unguiculata Lindl. | California, United States | OPGC | | | 2021 | | | | | | | Wild material | Lavender pink or salmon petals; four; claws end in a diamond shape. Outer anthers are 8 red. Stigma exserted beyond anthers. Sepals have hairs. Erect stem with lanceolate to ovate leaves. | 2120366 | OPGC 8372 |
| 272 | W6 59307 | CA180-221 | Brodiaea elegans Hoover | California, United States | W6 | | | 2021 | | | | | | | Wild material | Flower tube funnel shaped, violet, ascending; tips recurved. Staminodesûheld away from stamens which are flat and white. Three chambered fruit not split when ripe. Tiny black seeds.û | 2120362 | W6 59307 |
| 273 | NA 86846 | MSD19-001 | Acer pycnanthum K. Koch | Honshu, Japan | NA | | | 2021 | COLLECTED | 05/23/2019 | Gifu Prefecture: Nakatsugawa: farm of Mr. Asano. | 35.49533000, 137.45438000 | 270 | Mesic woods adjacent rice paddies; much of overstory was Cryptomeria (planted); poor drainage throughout; most trees growing at edges where light was abundant. Soil highly organic and shallow. | Wild material | Full name as recorded at U.S. National Arboretum: Acer pycnanthum. Plants picked up by USNA staff on 6/23/2021. | 2154981 | NA 86846 |
| 274 | NA 86847 | MSD19-002 | Acer pycnanthum K. Koch | Honshu, Japan | NA | | | 2021 | COLLECTED | 05/24/2019 | Nagano Prefecture, Shimoina District; Achii; Bicchuubara, in woods owned by Mrs. Noguchi. | 35.42873000, 137.74935000 | 612 | Mesic forest fed by natural springs and with many small (and old) canals diverting water; large Cryptomeria and Acer pycnanthum comprising much of the canopy; rich understory below. Soil organic and humusy over brown loam. | Wild material | Full name as recorded at U.S. National Arboretum: Acer pycnanthum. Plants picked up by USNA staff on 6/23/2021. | 2154982 | NA 86847 |
| 275 | W6 59016 | NCBG-472 | Schoenoplectus pungens (Vahl) Palla | North Carolina, United States | W6 | | | 2021 | | | | | | | Wild material | | 2116334 | W6 59016 |
| 276 | W6 59021 | NCBG-501 | Fimbristylis autumnalis (L.) Roem. & Schult. | North Carolina, United States | W6 | | | 2021 | | | | | | | Wild material | | 2116339 | W6 59021 |
| 277 | NA 88151 | NCBG-319 | Callicarpa americana L. | North Carolina, United States | NA |  | | 2019 | | | | | | | Wild material | | 2098411 | NA 88151 |
| 278 | WLP 2491 | Florida Caverns State Park | Hydrangea quercifolia W. Bartram | Florida, United States | NA |  | | 2019 | COLLECTED | 10/26/2017 | Florida Caverns State Park, Jackson County. Large population growing in two disjunct groups. Larger group is growing on the outcrops along Bluff Trail near the mouth of the cave. The smaller group is growing ca. 40 m north (This group is most accessible from the road to the campground, approximately 50 m east of the Chipola River). | 30.81017000, -85.22830000 | | Limestone outcrops above Taxodium distichum dominated swamp. | Wild material | Measurements of sampled specimens taken in nature: Height 53 to 168 in.; width 40 to 196 in. Measurements for each specimen sampled may be provided upon request (NA 86152.01 through 86152.27.) Most of the specimens in this population noted in nature (16 October 2017) had powdery mildew and/or bacterial leaf spot. | 2106201 | WLP 2491 |
| 279 | WLP 2502 | Old Cove Nature Preserve. | Hydrangea quercifolia W. Bartram | Mississippi, United States | NA |  | | 2019 | COLLECTED | 12/16/2017 | Old Cove Nature Preserve (TNC Preserve), Webster County. 9.7 mi northwest of Eupora. Approximately 180 m north of Old Cove Heath Rd (Highway 30). | 33.61379200, -89.40890300 | | Ravines and steep slopes above intermittent stream. | Wild material | Specimens noted in nature were sparsely flowering (2017). | 2106212 | WLP 2502 |
| 280 | WLP 2510 | Tunica Hills | Hydrangea quercifolia W. Bartram | Louisiana, United States | NA |  | | 2019 | COLLECTED | 10/14/2018 | Tunica Hills Wildlife Management Area, West Feliciana Parish. Approximately 4 miles south of Louisiana/Mississippi state line along Old Tunica Rd (Cr-268). | 30.93931900, -91.50825500 | | Shady roadside embankments and surrounding ravines. | Wild material | Measurements of sampled specimens taken in nature: Height 34 to 193 in.; width 66 to 129 in. Measurements for each specimen sampled may be provided upon request (NA 86171.01 through 86171.11). | 2106220 | WLP 2510 |
| 281 | WLP 2512 | Kisatchie National Forest | Hydrangea quercifolia W. Bartram | Louisiana, United States | NA |  | | 2019 | COLLECTED | 10/12/2018 | Kisatchie National Forest, Rapides Parish. Approximately 4.2 miles west of Castor Plunge and 7.2 miles northeast of Hineston. Bluff above Long Branch approximately 10 meters north of the Wild Azalea Trail. | 31.21523300, -92.67101500 | | Shady river bank. | Wild material | Measurements of sampled specimens taken in nature: Height 69 and 133 in., width 45 and 104 in., for NA 86173.01 and 86173.02, respectively. | 2106222 | WLP 2512 |
| 282 | WLP 2513 | MaryAnn Brown Nature Preserve | Hydrangea quercifolia W. Bartram | Louisiana, United States | NA |  | | 2019 | COLLECTED | 10/15/2018 | MaryAnn Brown Nature Preserve (TNC Preserve), West Feliciana Parish. 7.3 miles east-northeast of St. Francisville and 12.3 miles south of Louisiana/Mississippi state line. | 30.82582900, -91.26548200 | | Small ravines and streambanks in shady understory. | Wild material | Measurements of sampled specimens taken in nature: Height 63 and 105 in., width 107 and 99 in., for NA 86174.01 and 86174.02, respectively. | 2106223 | WLP 2513 |
| 283 | WLP 2517 | Falling Waters State Park | Hydrangea quercifolia W. Bartram | Florida, United States | NA |  | | 2019 | COLLECTED | 11/07/2018 | Falling Waters State Park, Washington County. Approximately 4 miles south of Chipley. | 30.72491900, -85.53055000 | | Edges of limestone sinkholes next to waterfall. | Wild material | These were the largest Hydrangea quercifolia observed out of 75 populations throughout the species' native range. Measurements of sampled specimens taken in nature: Height 97 and 192 (or more) in., width 133 and 192 (or more) in., for NA 86178.01 and 86178.02, respectively. | 2106227 | WLP 2517 |
| 284 | WLP 2518 | River Bluff Recreational Area | Hydrangea quercifolia W. Bartram | Georgia, United States | NA |  | | 2019 | COLLECTED | 11/12/2018 | River Bluff Recreation Area, Quitman County. Adjacent to Walter F. George Reservoir (eastern edge), across from Eufaula and approximately 0.9 miles north of Georgetown. | 31.89845700, -85.10882700 | | Shady bluffs adjacent to reservoir. | Wild material | Measurements of sampled specimens taken in nature: Height 78 to 158 in.; width 57 to 157 in. Measurements for each specimen sampled may be provided upon request. | 2106228 | WLP 2518 |
| 285 | WLP 2523 | RE Bob Woodruff Park | Hydrangea quercifolia W. Bartram | Alabama, United States | NA |  | | 2019 | COLLECTED | 11/29/2018 | RE Bob Woodruff Park, Augauga County. Approximately 7.8 miles west-southwest of Autaugaville, near the confluence of Ivy Creek with the Alabama River. | 32.39995500, -86.78419600 | | Ravines and bluffs with very soft soil. | Wild material | Measurements of sampled specimens taken in nature: Height 65 to 94 in.; width 42 to 139 in. Measurements for each specimen sampled may be provided upon request. | 2106233 | WLP 2523 |
| 286 | WLP 2524 | Coon Creek Forever Wild Tract | Hydrangea quercifolia W. Bartram | Alabama, United States | NA |  | | 2019 | COLLECTED | 11/29/2018 | Coon Creek Forever Wild Tract, Tallapoosa County. Approximately 4.25 miles north-northeast of Tallassee, near the confluence of Coon Creek with the Tallapoosa River. | 32.59593400, -85.88035200 | | Steep streambank. | Wild material | Measurements of sampled specimens taken in nature: Height 87 to 152 in.; width 66 to 124 in. Measurements for each specimen sampled may be provided upon request. | 2106234 | WLP 2524 |
| 287 | WLP 2526 | Franklin D. Roosevelt State Park | Hydrangea quercifolia W. Bartram | Georgia, United States | NA |  | | 2019 | COLLECTED | 11/28/2018 | Franklin D. Roosevelt State Park, Harris County. Approximately 1.9 miles southeast of Pine Mountain along Mountain Creek. | 32.84099500, -84.83899300 | | Shady streambank. | Wild material | Measurements of sampled specimen taken in nature: Height 47 to 101 in.; width 27 to 99 in. | 2106236 | WLP 2526 |
| 288 | WLP 2529 | Buck's Pocket State Park | Hydrangea quercifolia W. Bartram | Alabama, United States | NA |  | | 2019 | COLLECTED | 12/15/2018 | Buck's Pocket State Park, DeKalb County, 20 miles west-northwest of Forth Payne. | 34.47262200, -86.05294300 | | Shady slopes. | Wild material | Measurements of sampled specimens taken in nature: Height 53 to 114 in.; width 54 to 166 in. Measurements for each specimen sampled may be provided upon request. | 2106239 | WLP 2529 |
| 289 | WLP 2534 | Rocky Branch Public Use Area | Hydrangea quercifolia W. Bartram | Alabama, United States | NA |  | | 2019 | COLLECTED | 11/30/2018 | Rocky Branch Public Use Area, Tuscaloosa County. Approximately 10.5 miles northeast of Tuscaloosa near Holt Lake (in the Black Warrior River). Approximately 1,250 feet north of Rocky Branch Road. Along trail to Lock 14. | 33.28046900, -87.40678500 | | Shady hillsides and ravines. | Wild material | Measurements of sampled specimens taken in nature: Height 58 to 125 in.; width 99 to 109 in. Measurements for each specimen sampled may be provided upon request. | 2106244 | WLP 2534 |
| 290 | WLP 173 | NACPEC19-075 | Euonymus americanus L. | Georgia, United States | NA | | | 2019 | COLLECTED | 09/17/2019 | Rabun County; Chattahoochee-Oconee National Forest: Chattooga River Trail approximately 1/4 mile down trail from parking lot (off of Highway 76). About 0.09 miles North of Long Creek Highway (2) as the crow flies; Township unicorporated | 34.81549600, -83.30747100 | 393 | Trail edge, steep slope, 400 feet up the slope on West bank (Georgia side): Mixed mesophytic Maple-Hickory-Oak woodland | Wild material | | 2110487 | WLP 173 |
| 291 | WLP 174 | NACPEC19-076 | Clethra acuminata Michx. | Georgia, United States | NA | | | 2019 | COLLECTED | 09/17/2019 | Rabun County; Chattahoochee-Oconee National Forest: Chattooga River Trail approximately 1/2 mile down trail from parking lot (off of Highway 76); Township unicorporated | 34.81757600, -83.30720600 | 423 | Trail edge, steep slope, 400 feet up the slope on West bank (Georgia side): Mixed mesophytic Maple-Hickory-Oak woodland | Wild material | | 2110488 | WLP 174 |
| 292 | WLP 175 | NACPEC19-084 | Crataegus sp. | North Carolina, United States | NA | | | 2019 | COLLECTED | 09/18/2019 | Clay County; Nantahala National Forest: Forest Road 6269: Buck Creek Serpentine Barrens: main trail | 35.08578100, -83.61498800 | 1036 | Pinus rigida-Quercus alba / Sporobulus heterolepis-Andropogon gerardii Woodland OR Southern Blue Ridge Ultramafic Outcrop Barren | Wild material | | 2110489 | WLP 175 |
| 293 | WLP 176 | NACPEC19-085 | Viburnum cassinoides L. | North Carolina, United States | NA | | | 2019 | COLLECTED | 09/18/2019 | Clay County; Nantahala National Forest: Forest Road 6269: Buck Creek Serpentine Barrens: main trail | 35.08593700, -83.61539800 | 1057 | Pinus rigida-Quercus alba / Sporobulus heterolepis-Andropogon gerardii Woodland OR Southern Blue Ridge Ultramafic Outcrop Barren | Wild material | | 2110490 | WLP 176 |
| 294 | WLP 326 | MSD19-002 | Acer pycnanthum K. Koch | Honshu, Japan | NA | | | 2019 | COLLECTED | 05/24/2019 | Nagano Prefecture, Shimoina District; Achii; Bicchuubara, in woods owned by Mrs. Noguchi. | 35.42873000, 137.74935000 | 612 | Mesic forest fed by natural springs and with many small (and old) canals diverting water; large Cryptomeria and Acer pycnanthum comprising much of the canopy; rich understory below. Soil organic and humusy over brown loam. | Wild material | See NA 86847 for seedlings of this collection received later from the Morris Arboretum. | 2109075 | WLP 326 |
| 295 | WLP 1194 | NACPEC18-004 | Emmenopterys henryi Oliv. | Hubei Sheng, China | NA | | | 2018 | COLLECTED | 09/14/2018 | Hefeng County; Yanzi; Xinxingcun. "Backyard" at Hongjiang Hotel. | 29.95641000, 110.21043000 | 926 | Mixed natural and cultivated area. Talus slope. | | Emmenopterys certified by property owner as wild. Seeds and four herbarium specimens collected from three plants. Photographed. | 2108944 | WLP 1194 |
| 296 | WLP 1720 | NACPEC18-001 | Rosa helenae Rehder & E. H. Wilson | Hubei Sheng, China | NA | | | 2018 | COLLECTED | 09/13/2018 | Xuanen County; Chunmuyin; Changpo. | 30.18445000, 109.78723000 | 1623 | Disturbed roadside scrub. Brown forest soil. | | Seeds and three herbarium specimens collected from one plant. Photographed. | 2108941 | WLP 1720 |
| 297 | WLP 1876 | PCC18-HON-009 | Stachyurus praecox Siebold & Zucc. | Honshu, Japan | NA | | | 2018 | COLLECTED | 09/14/2018 | Tochigi Prefecture, Shioya-gun; Shioya-machi; Funyu Forest - Utsunomiya University Forest. | 36.78111000, 139.82640000 | 316 | Bouldery stream edge at base of hinoki (Chamaecyparis obtusa), along forestry road. Soil is rocky/gravel. | | Seed collected from two plants; three herbarium vouchers collected; photographed. | 2108914 | WLP 1876 |
| 298 | WLP 1536 | GF2018-04 | Pinckneya bracteata (W. Bartram) Raf. | Georgia, United States | NA | | | 2018 | COLLECTED | 11/06/2018 | Screven County; ; Along the side of Oliver Hwy, 230 ft. north of Nancy Branch Creek. | 32.54847000, -81.52067000 | 38 | In swampy thicket near a pond. | | It looks like the area was cleared in the last 5-6 years with many other small trees about the same height. | 2108886 | WLP 1536 |
| 299 | WLP 1187 | NACPEC17-006 | Euptelea pleiosperma Hook. f. & Thomson | Sichuan Sheng, China | NA | | | 2017 | COLLECTED | 09/21/2017 | Pingwu County; Si Er; Si Er Cun. Opening below the forest ridge and Magnolia officinalis plantation. | 32.34928000, 104.98164000 | 2064 | Beat up roadside edge, growing in rubble and rock, little to no A or O soil horizon. | | Seed collected from one plant. Three herbarium specimens collected; photographed. | 2108802 | WLP 1187 |
| 300 | 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 |
| 301 | 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 |
| 302 | Ames 34190 | Ames 34190 | Alnus serrulata (Aiton) Willd. | Kentucky, United States | NC7 | | | 2016 | COLLECTED | 09/28/2016 | | 36.83800000, -84.33100000 | 288 | River's edge below canopy. | | | 1952456 | Ames 34190 |
| 303 | NA 83911 | PCCKY16-038 | Hydrangea arborescens L. | Kentucky, United States | NA | | | 2016 | COLLECTED | 09/27/2016 | Daniel Boone National Forest, Yahoo Falls Loop Trail at Forest Road #660. Steep north cliff along stairs. | 36.77300000, -84.52100000 | 278 | Steep north cliff along stairs. | Wild material | | 1951652 | NA 83911 |
| 304 | 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 |
| 305 | WLP 1436 | NA 83951 | Oxydendrum arboreum (L.) DC. | Kentucky, United States | NA | | | 2016 | COLLECTED | 09/29/2016 | Kentenia State Forest, Pine Mountain, opening in canopy on Route 1679, south side. | 36.92000000, -83.24200000 | 795 | Roadside, opening in canopy. | | | 1951128 | WLP 1436 |
| 306 | 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 |
| 307 | 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 |
| 308 | WLP 1704 | NA 83942 | Rhus glabra L. | Kentucky, United States | NA | | | 2016 | COLLECTED | 09/29/2016 | Kentenia State Forest, Pine Mountain, on Route 1679, south side. | 36.90500000, -83.29100000 | 771 | Roadside. | | | 1953164 | WLP 1704 |
| 309 | WLP 1705 | NA 83948 | Rhododendron maximum L. | Kentucky, United States | NA | | | 2016 | COLLECTED | 09/29/2016 | Kentenia State Forest, Pine Mountain, on Route 1679, north side. | 36.91400000, -83.25900000 | 758 | Roadside. | | | 1950864 | WLP 1705 |
| 310 | 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 |
| 311 | WLP 654 | NA 83913 | Actaea racemosa L. | Kentucky, United States | NA | | | 2016 | COLLECTED | 09/27/2016 | Daniel Boone National Forest, Yahoo Falls Loop Trail at Forest Road #660. | 36.77300000, -84.52000000 | 251 | Washout below north cliff. | | | 1953602 | WLP 654 |
| 312 | WLP 872 | NA 83949 | Clethra acuminata Michx. | Kentucky, United States | NA | | | 2016 | COLLECTED | 09/29/2016 | Kentenia State Forest, Pine Mountain, on Route 1679, south side. | 36.91500000, -83.25900000 | 760 | Roadside. | | | 1951703 | WLP 872 |
| 313 | 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 |
| 314 | 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 |
| 315 | 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 |
| 316 | 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 |
| 317 | Ames 33078 | TDAAR15-050 | Aronia arbutifolia (L.) Pers. | Arkansas, United States | NC7 |  | | 2015 | COLLECTED | 09/24/2015 | Moro Big Pines Natural Area along Route 34, approximately 200 yards north of junction with Route 29 (five points area), T15S R13W Sec. 23, Calhoun County | 33.39953300, -92.41401700 | 34 | | Wild material | | 1932076 | Ames 33078 |
| 318 | 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 |
| 319 | 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 |
| 320 | 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 |
| 321 | WLP 1966 | JDC/VA/2014/096/598 | Viburnum acerifolium L. | Alabama, United States | NA | | | 2014 | COLLECTED | 09/23/2014 | Alabama: Lawrence County; William B. Bankhead National Forest, small tributary to Sipsey Fork near Cranal Road. | 34.28161300, -87.40651600 | 199 | Growing in association with Tsuga canadensis, Cornus florida, Magnolia macrophylla, Castanea dentata, Carpinus caroliniana, Quercus alba, and Pinus sp. | Wild material | Limited fruit production. Very shaded. Fruits black. | 1922367 | WLP 1966 |
| 322 | WLP 218 | JDC/TC/2014/089/591A | Tsuga canadensis (L.) Carrière | Alabama, United States | NA | | | 2014 | COLLECTED | 09/23/2014 | Alabama: Franklin County; William B. Bankhead National Forest, north-facing banks of Bear Creek watershed. | 34.33924600, -87.54771500 | 285 | Growing in association with Quercus alba, Cornus florida, Pueraria montana var. lobata, Magnolia macrophylla, Platanus occidentalis, Liquidambar styraciflua, and Fagus grandifolia. | Wild material | Excellent cone production. Optimum timing for harvest. Species infrequent to locally abundant across a 12 mile linear stretch of the southeast corner of Franklin County to north-central Winston County. | 1922361 | WLP 218 |
| 323 | 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 |
| 324 | OPGC 4162 | BFLA03 | Begonia cucullata Willd. | Florida, United States | OPGC | | | 2013 | COLLECTED | 09/07/2013 | Palatka, Putnam County, Florida. Ravine Gardens. | | | Exposure: part sun/part shade. Site Physical Description: Mesophytic forest, spring-fed running water, garden site at one time (1930s). Site Vegetation Description: Magnolia sp., Liquidambar, Ferns, Dioscorea bulbifera. | Wild material | | 1914853 | OPGC 4162 |
| 325 | OPGC 4168 | BFLA09 A and B | Begonia cucullata Willd. | Florida, United States | OPGC | | | 2013 | COLLECTED | 09/09/2013 | South Fork, Florida. Little Manatee River State Park | | | Exposure: partial sun to full shade. Site Physical Description: roadside, gravel-sandy area, near wet stream, somewhat disturbed. Site Vegetation Description: Magnolia virginiana, Baptisia sp., wild grape. | Wild material | | 1914859 | OPGC 4168 |
| 326 | OPGC 4169 | BFLA10 A and B | Begonia cucullata Willd. | Florida, United States | OPGC | | | 2013 | COLLECTED | 09/09/2013 | Marion county, Florida. Rainbow Springs State Park. | | | Exposure: full sun to full shade. Site Physical Description: garden setting, established in the 1930s, Begonia growing in creeks and outside of natural spring, plants were along spring walls, also growing in water (but appearing chlorotic). Site Vegetation Description: Magnolia sp., Ilex sp.,Devil�s walking stick, wild tarot. | Wild material | | 1914860 | OPGC 4169 |
| 327 | 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 |
| 328 | NA 81416 | Serrulatum Group | Rhododendron viscosum (L.) Torr. | Florida, United States | NA | | | 2013 | COLLECTED | 11/16/2012 | Blackwater State Forest, near an abandoned bridge. | 30.79862000, -86.79650000 | | On the edge of an acidic stream in pinewoods. | Wild material | Rooted cutting; received as Rhododendron viscosum var. serrulatum. | 1940403 | NA 81416 |
| 329 | WLP 1642 | NA 81413 | Leucothoe axillaris (Lam.) D. Don | Florida, United States | NA | | | 2013 | COLLECTED | | Blackwater State Forest | 30.84513000, -86.95438000 | | Along a small stream. | | | 1952344 | WLP 1642 |
| 330 | Ames 31053 | 380 | Betula alleghaniensis Britton | Pennsylvania, United States | NC7 |  | | 2011 | COLLECTED | 09/15/2011 | State Game Lands #282, floodplain of Conewango Creek Watershed, Warren County. | 41.98200000, -79.13500000 | 389 | Mixed hardwood forest and wetlands. | Wild material | | 1891439 | Ames 31053 |
| 331 | Ames 31075 | 698 | Fraxinus americana L. | New York, United States | NC7 |  | | 2011 | COLLECTED | 09/13/2011 | 7238 Hungry Hollow Road, Cattaraugus County. | 42.23000000, -78.70800000 | 659 | Upland forest edges. | Wild material | | 1891461 | Ames 31075 |
| 332 | WLP 1956 | 378 | Viburnum lentago L. | Pennsylvania, United States | NA | | | 2011 | COLLECTED | 09/15/2011 | State Game Lands #282, floodplain of Conewango Creek Watershed, Warren County. | 41.98700000, -79.13100000 | 379 | Mixed hardwood forest and wetlands. Associated with Betula alleghaniensis, Carpinus caroliniana, Cornus amomum, Fraxinus, Magnolia acuminata, Spiraea alba, Tsuga canadensis, and Viburnum dentatum. | Wild material | | 1891494 | WLP 1956 |
| 333 | WLP 217 | 379 | Tsuga canadensis (L.) Carrière | Pennsylvania, United States | NA | | | 2011 | COLLECTED | 09/15/2011 | State Game Lands #282, floodplain of Conewango Creek Watershed, Warren County. | 41.98300000, -79.13400000 | 392 | Mixed hardwood forest and wetlands. Associated with Betula alleghaniensis, Carpinus caroliniana, Cornus amomum, Fraxinus, Magnolia acuminata, Spiraea alba, Viburnum dentatum, and Viburnum lentago. | Wild material | | 1891489 | WLP 217 |
| 334 | Ames 31028 | MPW/MSD 703 | Cornus alternifolia L. f. | Pennsylvania, United States | NC7 |  | | 2011 | COLLECTED | 07/27/2011 | Along Martin Road, Warren County. | 41.98090000, -79.13630000 | 385 | Rich woods. | Wild material | | 1886743 | Ames 31028 |
| 335 | OPGC 3949 | PZSH2011-26 | Phlox divaricata L. subsp. laphamii (Alph. Wood) Wherry | Mississippi, United States | OPGC |  | | 2011 | COLLECTED | 04/09/2011 | Wilkinson County; approx 5 miles W of the juncture of Fort Adams Pond Road and Woodville Pinckneyville Road; Roadside S of Woodville Pinckneyville Road. | 31.04413000, -91.31003000 | 117 | Roadside at forest edge, mixed hardwood forest; Faguds grandifolia, Magnolia grandiflora, Magnolia pyramidata, Viola walteri, Pteris cretica, Trillium foetidissimum, Ostrya virginiana, Arundinaria gigantea. | Wild material | Plants erect, 30-45 cm tall, flowers lavender purple to purple, some with reddish purple star-shaped eye; leaves distinctively lanceolate. | 1907083 | OPGC 3949 |
| 336 | OPGC 3457 | PZ10-209 | Phlox paniculata L. | Ohio, United States | OPGC | | | 2010 | COLLECTED | 09/01/2010 | Scioto Co. Just S of juncture of Rocky Fork Rd. (Co. Rd. 40) and Tick Hill-Koenig Rd. On W side of road. | 38.49520000, -83.14058000 | 191 | Roadsie ditch; Impatiens pallida, Eupatorium purpureum, Aplectrum hyemale, Trillium grandiflorum, Polystichum acrostichoides, Magnolia tripetala, Liquidambar styraciflua | Wild material | Erect, slender perennial to 1 m tall; flowers magenta-pink; leaves ovate-lanceolate with areolate veins, glabrous | 1897773 | OPGC 3457 |
| 337 | Ames 30543 | UC 109 | Aronia arbutifolia (L.) Pers. | Tennessee, United States | NC7 |  | | 2010 | COLLECTED | 10/22/2009 | Near Rock Quarry Road, Newcomb, Campbell County | 36.53751700, -84.15580000 | 541 | Very dry, exposed rock spine with primarily organic soil and plants growing in cracks and pockets. | Wild material | Received as plants grown from seed collected from native/wild population. Accession is extremely vigorous and dense, with a relatively upright growth habit that is broad. Leaves are larger than the average A. arbutifolia. | 1843097 | Ames 30543 |
| 338 | Ames 33371 | KY-2009-025 | Spiraea betulifolia Pall. | Kentucky, United States | NC7 | | | 2009 | COLLECTED | 10/21/2009 | Daniel Boone National Forest, Morgan County. Along Leisure Paragon Road. | 38.04483000, -83.30707000 | 237 | Roadside on slope above flare of a natural drainage., Undefined slope. Growing in association with Cornus sp., Magnolia acuminata, Magnolia tripetala, Tsuga canadensis, Fagus grandifolia, Ulmus sp., Rhododendron maximum, and Symphyotrichum sp. | Wild material | | 1922708 | Ames 33371 |
| 339 | Ames 30360 | JDC/BL/2009/105/255 | Betula lenta L. | Ohio, United States | NC7 |  | | 2009 | COLLECTED | 10/17/2009 | Along Pond Run Road, Shawnee State Forest, Pond Run Quad, Scioto County. | 38.67805556, -83.20611111 | 271 | Floodplain. | Wild material | | 1823912 | Ames 30360 |
| 340 | WLP 1354 | JDC/LB/2009/089/239 | Lindera benzoin (L.) Blume | Ohio, United States | NA | | | 2009 | COLLECTED | 10/15/2009 | Near Lake Katherine, SW 1/4 of NW 1/4 of Section 13, T7N, R19W, Jackson Quad, Jackson County. | 39.08250000, -82.67750000 | 236 | 10% slope, north facing. Compacted soils. Associated with with Acer saccharum, Cornus florida, Magnolia tripetela, Oxydendrum arboreum, Quercus, and Tsuga canadensis. | Wild material | | 1823931 | WLP 1354 |
| 341 | WLP 1413 | JDC/OA/2009/087/237 | Oxydendrum arboreum (L.) DC. | Ohio, United States | NA | | | 2009 | COLLECTED | 10/15/2009 | Near Lake Katherine, SW 1/4 of NW 1/4 of Section 13, T7N, R19W, Jackson Quad, Jackson County. | 39.08444444, -82.67833333 | 225 | Lake edge. Associated with with Acer saccharum, Cornus florida, Lindera benzoin, Magnolia tripetela, Nyssa sylvatica, Sassafras albidum, and Tsuga canadensis. | Wild material | | 1823935 | WLP 1413 |
| 342 | NA 78359 | NA 78359 | Thujopsis dolabrata (Thunb. ex L. f.) Siebold & Zucc. | Honshu, Japan | NA | | | 2009 | COLLECTED | 09/15/2005 | At side of track off Rt 26 between Aomori city and Goshagawara city, 5km from Aomori City. | 40.85883000, 140.59113000 | 310 | Growing in full sun on mountainside in mixed forest | | | 1951627 | NA 78359 |
| 343 | Ames 29654 | JDC/FP/2008/038/108 | Fraxinus pennsylvanica Marshall | Missouri, United States | NC7 |  | | 2008 | COLLECTED | 10/08/2008 | Along White Sands Road, near Magnolia Hollow Conservation Area, T38N, R8E, Bloomsdale Quad, Ste. Genevieve County. | 38.01277778, -90.18888889 | 119 | Along bankside of creek. | Wild material | A couple of original specimens were very tall (80 feet). | 1788209 | Ames 29654 |
| 344 | NA 78035 | AL #44 | Philadelphus inodorus L. | Alabama, United States | NA | | | 2008 | COLLECTED | 09/17/2008 | Just above the Cahaba River, near end of road and Caffee Creek. | | | | Wild material | | 1913895 | NA 78035 |
| 345 | Ames 27648 | JM2004009 | Actaea racemosa L. | South Carolina, United States | NC7 | | | 2004 | | | | | | | Wild material | | 1667568 | Ames 27648 |
| 346 | WLP 1215 | NA 78171 | Hydrangea arborescens L. | North Carolina, United States | NA |  | | 2004 | COLLECTED | 10/02/2004 | Highway 276 to East Fork Road, Pine Shore Lakes, Brevard, Transylvania County. | 35.12611111, -82.72944444 | 851 | Pine-oak forest. Lakeside on private land. 15 degrees of slope. Associated with Acer, Cornus florida, Magnolia, Pinus strobus, and Quercus. | Wild material | 1-4 meters tall. | 1667573 | WLP 1215 |
| 347 | NA 72839 | NA 72839 | Taxus cuspidata Siebold & Zucc. | Korea, South | NA | | Contact Site | 2002 | COLLECTED | 10/1993 | Western slope of Hallasan [mountain]. [Originally listed as Cheju Island, Mt. Halla, Western Slope.] | 33.38333000, 126.50000000 | | | | | 1952662 | NA 72839 |
| 348 | NA 72840 | NA 72840 | Taxus cuspidata Siebold & Zucc. | Korea, South | NA | | Contact Site | 2002 | COLLECTED | 10/1993 | Western slope of Hallasan [mountain]. [Originally listed as Cheju Island, Mt. Halla, Western Slope.] | 33.38333000, 126.50000000 | | | | | 1952663 | NA 72840 |
| 349 | NA 72841 | NA 72841 | Taxus cuspidata Siebold & Zucc. | Korea, South | NA | | Contact Site | 2002 | COLLECTED | 10/1993 | Western slope of Hallasan [mountain]. [Originally listed as Cheju Island, Mt. Halla, Western Slope.] | 33.38333000, 126.50000000 | | | | | 1950268 | NA 72841 |
| 350 | NA 71793 | NA 71793 | Torreya taxifolia Arn. | Florida, United States | NA | | Contact Site | 2002 | COLLECTED | 11/1989 | Southern side of Flat Creek | 30.62777000, 84.83750000 | 50 | slopes of ravine with Ostrya, Magnolia, Acer | Wild material | | 1952384 | NA 71793 |
| 351 | NA 71799 | NA 71799 | Torreya taxifolia Arn. | Florida, United States | NA | | Contact Site | 2002 | COLLECTED | 11/1989 | Sotera Lumber Company land, 1 mile due south of Rosedale. | 30.63750000, 84.80194000 | | Slopes of mixed forest; Pine, Magnolia, Liquidambar, Quercus, Acer, Ilex | Wild material | | 1952552 | NA 71799 |
| 352 | NA 71800 | NA 71800 | Torreya taxifolia Arn. | Florida, United States | NA | | Contact Site | 2002 | COLLECTED | 11/1989 | Sotera Lumber Company land, 1 mile due south of Rosedale. | 30.63750000, 84.80194000 | | Slopes of mixed forest; Pine, Magnolia, Liquidambar, Quercus, Acer, Ilex | | | 1952415 | NA 71800 |
| 353 | NA 71804 | NA 71804 | Torreya taxifolia Arn. | Florida, United States | NA | | Contact Site | 2002 | COLLECTED | 11/1989 | Sotera Lumber Company land, 1 mile due south of Rosedale. | 30.63750000, 84.80194000 | | Slopes of mixed forest; Pine, Magnolia, Liquidambar, Quercus, Acer, Ilex | | | 1953301 | NA 71804 |
| 354 | NA 71808 | NA 71808 | Torreya taxifolia Arn. | Florida, United States | NA | | Contact Site | 2002 | COLLECTED | 11/1989 | Sotera Lumber Company land, 1 mile due south of Rosedale. | 30.63750000, 84.80194000 | | Slopes of mixed forest; Pine, Magnolia, Liquidambar, Quercus, Acer, Ilex | | | 1951998 | NA 71808 |
| 355 | NA 64819 | WD052 | Euonymus hamiltonianus Wall. | Hubei Sheng, China | NA | | | 1994 | COLLECTED | 09/18/1994 | Wudang Shan. | 32.40222222, 110.99666667 | | Along ridge of Wudang Shan with Pinus tabulaeformis, Cornus kousa, Cornus controversa, Rhus verniciflua, Magnolia denudata, Quercus aliena. | Wild material | | 1511200 | NA 64819 |
| 356 | NA 61679 | NEKG 76 | Lindera obtusiloba Blume | Gangwon-do, Korea, South | NA | | | 1989 | COLLECTED | 09/24/1989 | Pyeongchang-gun, Jinbu-myeon: Gariwangsan [mountain], about 2 km down mountain road from NEKG 70, above road cut. [Originally listed as Kang-won Do. Kariwang San. About 2km down mountain road from NEKG 70. Woodland above road cut.] | 37.48611000, 128.50972000 | 820 | Woodland above road cut. | Wild material | | 1776926 | NA 61679 |
| 357 | WLP 1581 | NEKG 166 | Rhododendron mucronulatum Turcz. | Gangwon-do, Korea, South | NA | | | 1989 | COLLECTED | 10/14/1989 | Sokcho-si: Seorak-dong: Seoraksan [mountain], on trail to Daecheongbong [peak], above Hangyeryeong [pass/ridge]. [Originally listed as Kang-won Do, Sorak San. On trail to Tae-chong Bong, above Han-gyae-Ryong.] | 38.10000000, 128.40972222 | 1000 | Rocky outcroppings - open. | Wild material | | 1506693 | WLP 1581 |
| 358 | NA 61236 | GU 101 | Ilex verticillata (L.) A. Gray | Virginia, United States | NA | | | 1989 | COLLECTED | 09/25/1989 | George Washington National Forest. [Note: latitude and longitude have been estimated based on the locality data and are only approximate.] | 38.32684300, -79.29107700 | | Magnolia swamp. | Wild material | In December 2024, female seedling individual NA 61236-008 was earmarked as a potential evaluation selection and reaccessioned as NA 87858. | 1112014 | NA 61236 |
| 359 | NA 60670 | SAS 022 | Euonymus carnosus Hemsl. | Anhui Sheng, China | NA | | | 1988 | COLLECTED | 10/02/1988 | Huangshan Mountains: Ku Zhu Xi (Bitter Bamboo Stream) south of Yun Gu Si Temple (Cloud Valley Monastery) site. | | 857 | Along streamside within reach of high water, south bank with northeast aspect. | Wild material | | 2108371 | NA 60670 |
| 360 | CIor 9933 | C72-681 | Oryza sativa L. | Louisiana, United States | NSGC |  | | 1973 | DEVELOPED | | | | | | Breeding material | | 1050932 | CIor 9933 |
| 361 | CIor 9939 | C72-670 | Oryza sativa L. | Louisiana, United States | NSGC |  | | 1973 | DEVELOPED | | | | | | Breeding material | | 1050960 | CIor 9939 |
| 362 | CIor 9897 | Cro 71-314 | Oryza sativa L. | Louisiana, United States | NSGC |  | | 1972 | DEVELOPED | | | | | | Breeding material | | 1050757 | CIor 9897 |
| 363 | CIor 9895 | C71-301 | Oryza sativa L. | Louisiana, United States | NSGC |  | | 1972 | DEVELOPED | | | | | | Breeding material | | 1050745 | CIor 9895 |
| 364 | CIor 9854 | C70-5296 | Oryza sativa L. | Louisiana, United States | NSGC |  | | 1971 | DEVELOPED | | | | | | Breeding material | | 1050533 | CIor 9854 |
| 365 | CIor 9856 | C70-5285 | Oryza sativa L. | Louisiana, United States | NSGC |  | | 1971 | DEVELOPED | | | | | | Breeding material | | 1050543 | CIor 9856 |
| 366 | CIor 9858 | C70-5300 | Oryza sativa L. | Louisiana, United States | NSGC |  | | 1971 | DEVELOPED | | | | | | Breeding material | | 1050551 | CIor 9858 |
| 367 | CIor 9888 | C70-5247 | Oryza sativa L. | Louisiana, United States | NSGC |  | | 1971 | DEVELOPED | | | | | | Breeding material | | 1050710 | CIor 9888 |
| 368 | CIor 9889 | C70-5008 | Oryza sativa L. | Louisiana, United States | NSGC |  | | 1971 | DEVELOPED | | | | | | Breeding material | | 1050711 | CIor 9889 |
| 369 | CIor 9703 | Cro 68-201 | Oryza sativa L. | Louisiana, United States | NSGC |  | | 1969 | DEVELOPED | | | | | | Breeding material | | 1049909 | CIor 9703 |
| 370 | CIor 9676 | 67 Cro-5028 | Oryza sativa L. | Louisiana, United States | NSGC |  | | 1968 | DEVELOPED | | | | | | Breeding material | | 1049780 | CIor 9676 |
| 371 | CIor 9677 | C67-5045 | Oryza sativa L. | Louisiana, United States | NSGC |  | | 1968 | DEVELOPED | | | | | | Breeding material | | 1049781 | CIor 9677 |
| 372 | CIor 9683 | 67 Cro-5218 | Oryza sativa L. | Louisiana, United States | NSGC |  | | 1968 | DEVELOPED | | | | | | Breeding material | | 1049810 | CIor 9683 |
| 373 | CIor 9684 | C67-5229 | Oryza sativa L. | Louisiana, United States | NSGC |  | | 1968 | DEVELOPED | | | | | | Breeding material | | 1049819 | CIor 9684 |
| 374 | CIor 9658 | Cro 66-5062 | Oryza sativa L. | Louisiana, United States | NSGC |  | | 1967 | DEVELOPED | | | | | | Breeding material | | 1049699 | CIor 9658 |
| 375 | CIor 9661 | C66-5218 | Oryza sativa L. | Louisiana, United States | NSGC |  | | 1967 | DEVELOPED | | | | | | Breeding material | | 1049709 | CIor 9661 |
| 376 | CIor 9671 | C66-5228 | Oryza sativa L. | Louisiana, United States | NSGC |  | | 1967 | DEVELOPED | | | | | | Breeding material | | 1049756 | CIor 9671 |
| 377 | CIor 12346 | 'Vista' | Oryza sativa L. | Louisiana, United States | NSGC |  | | 1966 | DEVELOPED | 1971 | | | | | Cultivar | Medium-grain rice. | 1060149 | CIor 12346 |
| 378 | CIor 9624 | 65Cro-5030 | Oryza sativa L. | Louisiana, United States | NSGC |  | | 1966 | DEVELOPED | | | | | | Breeding material | | 1049539 | CIor 9624 |
| 379 | CIor 9625 | 65Cro-5035 | Oryza sativa L. | Louisiana, United States | NSGC |  | | 1966 | DEVELOPED | | | | | | Breeding material | | 1049540 | CIor 9625 |
| 380 | CIor 9629 | C65-5220 | Oryza sativa L. | Louisiana, United States | NSGC |  | | 1966 | DEVELOPED | | | | | | Breeding material | | 1049561 | CIor 9629 |
| 381 | CIor 9630 | C65-5217 | Oryza sativa L. | Louisiana, United States | NSGC |  | | 1966 | DEVELOPED | | | | | | Breeding material | | 1049564 | CIor 9630 |
| 382 | CIor 9594 | C63-5717 | Oryza sativa L. | Louisiana, United States | NSGC |  | | 1964 | DEVELOPED | | | | | | Breeding material | | 1049406 | CIor 9594 |
| 383 | CIor 9595 | 63Cro-5064 | Oryza sativa L. | Louisiana, United States | NSGC |  | | 1964 | DEVELOPED | | | | | | Breeding material | | 1049407 | CIor 9595 |
| 384 | CIor 9553 | WC 1189 | Oryza sativa L. | Louisiana, United States | NSGC |  | | 1963 | DEVELOPED | | | | | | Breeding material | | 1049212 | CIor 9553 |
| 385 | CIor 9548 | C61-5318 | Oryza sativa L. | Louisiana, United States | NSGC |  | | 1962 | DEVELOPED | | | | | | Breeding material | | 1049189 | CIor 9548 |
| 386 | CIor 9539 | Cro 1961-50014 | Oryza sativa L. | Louisiana, United States | NSGC |  | | 1962 | DEVELOPED | | | | | | Breeding material | | 1049129 | CIor 9539 |
| 387 | CIor 9540 | 'Saturn' | Oryza sativa L. | Louisiana, United States | NSGC |  | | 1962 | DEVELOPED | 1964 | | | | | Cultivar | Medium-grain rice. | 1049140 | CIor 9540 |
| 388 | CIor 9482 | WC 1140 | Oryza sativa L. | Louisiana, United States | NSGC |  | | 1961 | DEVELOPED | | | | | | Breeding material | | 1048836 | CIor 9482 |
| 389 | CIor 9461 | Cro 59V237 | Oryza sativa L. | Louisiana, United States | NSGC |  | | 1960 | DEVELOPED | | | | | | Breeding material | | 1048745 | CIor 9461 |
| 390 | CIor 9474 | C59V5097 | Oryza sativa L. | Louisiana, United States | NSGC |  | | 1960 | DEVELOPED | | | | | | Breeding material | | 1048801 | CIor 9474 |
| 391 | CIor 9475 | C59V5107 | Oryza sativa L. | Louisiana, United States | NSGC |  | | 1960 | DEVELOPED | | | | | | Breeding material | | 1048802 | CIor 9475 |
| 392 | CIor 9451 | C58-5066 | Oryza sativa L. | Louisiana, United States | NSGC |  | | 1959 | DEVELOPED | | | | | | Breeding material | | 1048701 | CIor 9451 |
| 393 | CIor 9430 | C57-V505 | Oryza sativa L. | Louisiana, United States | NSGC |  | | 1958 | DEVELOPED | | | | | | Breeding material | | 1048600 | CIor 9430 |
| 394 | CIor 8996 | 42C-403-103 | Oryza sativa L. | Louisiana, United States | NSGC |  | | 1954 | DEVELOPED | | | | | | Breeding material | | 1046084 | CIor 8996 |
| 395 | CIor 8998 | 'Nato' | Oryza sativa L. | Louisiana, United States | NSGC |  | | 1954 | DEVELOPED | 1956 | | | | | Cultivar | Medium-grain rice. The name 'NATO' was chosen for the 'North Atlantic Treaty Organization', alluding to the incorporation in the new variety of strong contributions from several sources. | 1046093 | CIor 8998 |
| 396 | CIor 9001 | 44C-5-4090 | Oryza sativa L. | Louisiana, United States | NSGC |  | | 1954 | DEVELOPED | | | | | | Breeding material | | 1046107 | CIor 9001 |
| 397 | CIor 9168 | C53-4003 | Oryza sativa L. | Louisiana, United States | NSGC |  | | 1954 | DEVELOPED | | | | | | Breeding material | | 1046995 | CIor 9168 |
| 398 | CIor 9172 | C53-17 | Oryza sativa L. | Louisiana, United States | NSGC |  | | 1954 | DEVELOPED | | | | | | Breeding material | | 1047021 | CIor 9172 |
| 399 | CIor 9173 | C53-4035 | Oryza sativa L. | Louisiana, United States | NSGC |  | | 1954 | DEVELOPED | | | | | | Breeding material | | 1047025 | CIor 9173 |