| 0 | NA 86666 | SE-2017-010A | Quercus sp. | Georgia, United States | NA | | | 2017 | COLLECTED | 10/13/2017 | Fall Line Sandhills Wildlife Management Area. | 32.57050000, -84.28230000 | 216 | Sandy old beach dune. | Wild material | Recorded at the U.S. National Arboretum as Quercus incana W. Bartram (non Q. incana Roxb., which is a synonym of Q. leucotrichophora; see the Flora of North America treatment for further information).This (along with NA 86667 and 86668) were missing from the other collection data used for initial accessioning; see NA 86648-86664 for the rest of the collections from this expedition. | 2141803 | NA 86666 |
| 1 | Ames 19367 | Ames 19367 | Quercus ×schochiana Dieck | Missouri, United States | NC7 |  | | 1992 | COLLECTED | | Missouri: southeastern corner of state. | 37.14982600, -90.76904300 | | | Wild material | Accession was separated during a grow out at NCRPIS from a seed lot of Ames 4723, which was originally received by the Missouri Dept. of Conservation as Quercus phellos. This hybrid is assumed to be a hybrid between Quercus phellos and Quercus palustris based on morphological characters being intermediate of both species. | 1082829 | Ames 19367 |
| 2 | PI 655784 | S040.CPG94 | Lotus palustris Willd. | Sardegna, Italy | W6 |  | | 1994 | COLLECTED | 07/05/1994 | Near Arzachena, 2 k west of Arzachena on road Bassacutena-Arzachena. | 41.08583333, 9.35861111 | 20 | Grazed. Slope 0-5%, aspect NE. Open. Soil clay, pH 6.0-6.5. Rainfall 770 mm. Seasonally inundated, stream terrace. Vegetation closed, evergreen broad-leafed herb veg. Surrounding veg. evergreen open forest with closed lower layers. | Wild material | Population abundance frequent, distribution patchy. Growth habit prostrate. Flower yellow. | 1480129 | PI 655784 |
| 3 | NA 88542 | RJLSEUS2022-014 | Rosa palustris Marshall | Georgia, United States | NA | | | 2023 | COLLECTED | 12/09/2022 | Plants growing around a pond and associated wetland on the property of Monica Williams north of Albany, Georgia. Common along the transitional edges from wet to dry. | 31.63723900, -84.13776200 | 60 | Plants are growing in full sun mostly in the transitional edges of the pond where conditions are generally moist mesic. Even so, this species appears quite adaptable and can be found in quite moist as well as drier soil conditions.
Soils: The underlying geology of this area is of Eocene origin and characterized as Ocala Limestone. The Ocala Limestone consists of almost pure limestones with occasional dolomites. It can be subdivided into both lower and upper facies with the lower facies composed of a whitish to cream-colored, fine to medium grained, poorly to moderately hard, fossil rich grainstone and packstone. The upper Ocala is white and somewhat weak and poorly sorted. It is extremely fossil rich grainstone, packstone and wackestone and some chert is common in the upper facies.
Source: USGS Georgia Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=GANu%3B1)
The primary soil types in the collection area are classified as Herod and Muckalee Series soils. The Herod Series consists of poorly drained moderately permeable soils formed in loamy alluvium. These soils are on flood plains of streams in the Coastal Plain. Slopes range from 0 to 2 percent. The Muckalee Series consists of poorly drained moderately permeable soils formed in loamy and sandy alluvium. These soils are on flood plains of streams in the Coastal Plain. Slopes range from 0 to 2 percent.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2140817 | NA 88542 |
| 4 | 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 |
| 5 | NA 88435 | MARSB-255 | Rosa palustris Marshall | New York, United States | NA |  | | 2019 | | | | | | | Wild material | | 2097542 | NA 88435 |
| 6 | WLP 1190 | NA 85118 | Dirca palustris L. | Iowa, United States | NA |  | | 2018 | COLLECTED | 05/31/2018 | Private property located 3.35 miles southwest of Luther near Des Moines River, T82N R26W SW 1/4 SW 1/4 Sec. 3, Boone County | 41.93795800, -93.87109500 | 317 | Dense shade of mature oak forest. Deep ravines. | Wild material | Specimens measuring approximately 2-5' in height. Noticeable new growth (5-8") at time of seed collection. Population was in peak bloom 24 April 2018 with peak fruit maturity occuring on 30 May 2018. Fruits readily dropping when distrubed. Very slight tinge of white color to fully mature fruits. Seeds measuring approximately 0.5-0.7 cm in length. | 1963390 | WLP 1190 |
| 7 | PI 691215 | V. arboreum GN2018 Manatee Springs State Park1 | Vaccinium arboreum Marshall | Florida, United States | COR | | | 2019 | COLLECTED | 12/06/2018 | Manatee Springs State Park | 29.49358600, -82.97336900 | 23 | NNW exposure/aspect. Next to driving road by gate to the north trail.Vegetation nearby included; Crowngrass (Paspalum spp.), water oak (Quercus nigra), saw palmetto (Serenoa repens), longleaf pine (Pinus palustris), slash pine (pinus elliottii). | Wild material | Gerardo Nunez USDA plant collecting trip to Florida 2018, 2019 | 2094707 | PI 691215 |
| 8 | PI 671849 | FL2010WW-6 | Amphicarpaea bracteata (L.) Fernald | Florida, United States | W6 |  | | 2010 | COLLECTED | 11/09/2010 | Columbia County; Ichetucknee State Park; South entrance; 0.4 miles from entrance; immediately after kiosk, turn left into parking lot; parking lot near maintenance shed; lot perimeter about 15-25 m out | 29.95299000, -82.77148000 | 5 | sand hill; dry, well-drained soil; sunny, open location, edge of open forest dominated by Pinus palustris with an understory of Quercus laevis, Quercus stellata, invasive Quercus laurifolia, Vitis spp, Carya spp. and many annuals | Wild material | Very abundant; prostrate vines; very mature leaves; insect damage; no flowers; few green pods; dry and dehisced pods; small root tuber with fibrous roots extending; adventitious roots from tuber and from lower nodes, growing out to produce other daughter plants; small white ?nodule? on white adventitious roots with more white root growing from it; the main plant often has many satellite plants attached to it. Sample size 750 meters square. | 1854396 | PI 671849 |
| 9 | PI 657223 | V. corymbosum HD-2007-016 | Vaccinium corymbosum L. | South Carolina, United States | COR | | | 2007 | COLLECTED | 06/03/2007 | Northwest of Little Rock, Dillon County. Intersection of SR-57 and McLaurin Lake Circle. Growing in a drainage ditch west side of road. | 34.50649000, -79.47892000 | 20 | Flat terrain. Associated with: Smilax, Acer rubrum, Liquidambar styraciflua, Quercus velutina, Sasafras albidum, Lonicera japonica, Pinus palustris and Campsus radicans. | Wild material | Kim Hummer, Michael Dossett collected from South Carolina. V. corymbosum diploid
| 1730114 | PI 657223 |
| 10 | PI 598839 | MO30.CPG94 | Lolium perenne L. | Morocco | W6 |  | | 1994 | COLLECTED | 07/13/1994 | Near Taza, 16 km south of Taza near Ras-El-Oued on road S311. | 34.14500000, -4.01416667 | 1120 | Grazed. Slope 11-40%, aspect NE. Light open. Soil hillside loam on calcareous dolomite bedrock, pH 7.5-8.0. Moist, ravine, mid slope. Vegetation closed, seasonal tall grass. Surrounding veg. evergreen open forest with closed lower layers. | Wild material | Dominant tree species Quercus ilex. Dom. shrub sp. Calycotome villosa, Juniperus sp. Dom. herb/grass sp. perennial clovers, grasses, couch. Population distribution patchy, abundance frequent. Growth habit semi-erect. | 1480220 | PI 598839 |
| 11 | PI 598840 | MO32.CPG94 | Dactylis glomerata L. | Morocco | W6 | | | 1994 | COLLECTED | 07/13/1994 | Near Taza, 16 km south of Taza near Ras-El-Oued on road S311. | 34.14500000, -4.01416667 | 1120 | Grazed. Slope 11-40%, aspect NE. Light open. Soil loam on calcareous dolomite bedrock, pH 7.5-8.0. Moist, ravine, mid slope. Vegetation closed, seasonal tall grass. Surrounding vegetation evergreen open forest with closed lower layers. | Wild material | Dominant tree species Quercus ilex. Dom. shrub sp., Calycotome villosa, Juniperus sp. Dom. herb/grass sp. perennial clovers, grasses, couch. Population distribution patchy, abundance frequent. Growth habit erect. | 1480222 | PI 598840 |
| 12 | PI 598841 | MO35.CPG94 | Festuca arundinacea Schreb. | Morocco | W6 | | | 1994 | COLLECTED | 07/13/1994 | Near Taza, 16 km south of Taza near Ras-El-Oued on road S311. | 34.14500000, -4.01416667 | 1120 | Grazed. Slope 11-40%, aspect NE. Open. Loam on calcareous dolomite bedrock, pH 7.5-8.0. Rainfall 900 mm. Moist, ravine, mid slope, spring weep. Veg. closed, seasonal tall grass.Surrounding veg. evergreen open forest with closed lower layers | Wild material | Dominant tree species Quercus ilex. Dom. shrub sp. Calycotome villosa, Juniperus sp. Dom. herb/grass sp. perennial clovers, grasses, couch. Population distribution patchy, abundance frequent. Growth habit erect. | 1480225 | PI 598841 |
| 13 | PI 598867 | MO81.CPG94 | Lolium rigidum Gaudin | Morocco | W6 |  | | 1994 | COLLECTED | 07/18/1994 | Near Azrou, 7 km northwest of Azrou on road P21, El-Hajeb-Azrou. | 33.49361111, -5.26361111 | 1270 | Grazed. Slope 11-40%, aspect SE. Open. Soil loam on calcareous rock, pH 9.5-10.0. Rainfall 825 mm. Moist, ravine, spring bog. Vegetation closed, seasonal tall grass. Surrounding veg. cereal-pasture-orchard agriculture. | Wild material | Population distribution patchy, abundance frequent. Growth habit semi-erect. | 1480270 | PI 598867 |
| 14 | PI 610939 | S043.CPG94 | Lolium perenne L. | Sardegna, Italy | W6 |  | | 1994 | COLLECTED | 07/05/1994 | Near Aggius, 3 k north of Aggius on road SS127 to Trinita. | 40.93666667, 9.05555556 | 550 | Grazed. Slope 0-5%, aspect N. Area open. Soil loam, alluvial, pH 5.0. Rainfall 1000 mm. Seasonally dry, alluvial fan. Vegetation closed, seasonal tall grass. Surrounding veg. closed evergreen scrub with scattered trees. | Wild material | Population abundance frequent, distribution patchy. Growth habit semi-erect. | 1480132 | PI 610939 |
| 15 | PI 610946 | MO78.CPG94 | Festuca arundinacea Schreb. | Morocco | W6 | | | 1994 | COLLECTED | 07/18/1994 | Near Azrou, 7 km. northwest of Azrou on road P21, El-Hajeb-Azrou. | 33.49361111, -5.26361111 | 1270 | Grazed. Slope 11-40%, aspect SE. Open. Soil loam on calcareous rock, pH 9.5-10.0. Rainfall 825 mm. Moist, ravine, spring bog. Vegetation closed, seasonal tall grass. Surrounding veg. cereal-pasture-orchard agriculture. | Wild material | Population distribution patchy, abundance frequent. Growth habit erect. | 1480267 | PI 610946 |
| 16 | PI 610957 | S032.CPG94 | Festuca arundinacea Schreb. | Sardegna, Italy | W6 | | | 1994 | COLLECTED | 07/05/1994 | Near Tempio, 11 north on road S133 to Luogosanto. | 40.95277778, 9.09638889 | 315 | Grazed. Slope 0-5%, aspect E. Area open. Soil loam, pH 5.5. Rainfall 1000 mm. Moist, stream terrace, meadow. Vegetation closed, seasonal tall grass. Surrounding veg. evergreen open forest with closed lower layers, dryland pasture/forage. | Wild material | Population abundance occasional, distribution patchy. Growth habit erect. | 1480121 | PI 610957 |
| 17 | PI 631738 | MO80.CPG94 | Trifolium pratense L. | Morocco | W6 | | | 1994 | COLLECTED | 07/18/1994 | Near Azrou, 7 km. northwest of Azrou on road P21, El-Hajeb-Azrou. | 33.49361111, -5.26361111 | 1270 | Grazed. Slope 11-40%, aspect SE. Open. Soil loam on calcareous rock, pH 9.5-10.0. Rainfall 825 mm. Moist, ravine, spring bog.Vegetation closed,seasonal tall grass.Surrounding veg.cereal-pasture-orchard agriculture.Area sampled 20,000 sq. m. | Wild material | Population distribution patchy, abundance frequent. Growth habit semi-erect. Flower red. | 1480269 | PI 631738 |
| 18 | PI 655708 | MOO2.CPG94 | Trifolium repens L. | Morocco | W6 | | | 1994 | COLLECTED | 07/12/1994 | Near Chefchaouen, 6 km. southeast of Chefchaouen on P39 (412). | 35.12472222, -5.28833333 | 460 | Grazed. Slope 6-10%, aspect. Light open. Soil loam, hydromorphis, from shale & sandstones, pH 6.5-7.0. Rainfall 900 mm. Seasonally inundated, basin, spring weep/bog next to road. Area sampled 20,000 sq. m. | Wild material | Dominant tree species Quercus suber. Dom. shrub sp. Pistacia lentiscus. Dom. herb/grass sp. Juncus sp. Population distribution patchy, abundance occasional. Growth habit prostrate. Flower white. | 1480194 | PI 655708 |
| 19 | PI 655717 | MO34.CPG94 | Trifolium repens L. | Morocco | W6 | | | 1994 | COLLECTED | 07/13/1994 | 16 km. south of Taza near Ras-El-Oved on road S311. | 34.14027778, -4.00861111 | 1120 | Grazed. Slope 11-40%, aspect NE. Open. Loam on calcareous dolomite bedrock, pH 7.5-8.0. Rainfall 900 mm. Moist, ravine, mid slope, spring weep. Veg. closed, seasonal tall grass.Surrounding veg. evergreen open forest with closed lower layers | Wild material | Dominant tree species Quercus ilex. Dom. shrub sp. Calycotome villosa, Juniperus sp. Dom. herb/grass sp. perennial clovers, grasses, couch. Population distribution patchy, abundance occasional. Growth habit prostrate. Flower white. | 1480224 | PI 655717 |
| 20 | PI 655725 | MO79.CPG94 | Trifolium fragiferum L. | Morocco | W6 | | | 1994 | COLLECTED | 07/18/1994 | Near Azrou, 7 km. northwest of Azrou on road P21, El-Hajeb-Azrou. | 33.49361111, -5.26361111 | 1270 | Grazed. Slope 11-40%, aspect SE. Open. Soil loam on calcareous rock, pH 9.5-10.0. Rainfall 825 mm. Moist, ravine, spring bog. Vegetation closed, seasonal tall grass. Surrounding veg. cereal-pasture-orchard agriculture. | Wild material | Population distribution patchy, abundance frequent. Growth habit prostrate. Flower color rose. | 1480268 | PI 655725 |
| 21 | Ames 38800 | Camp Mitigwa | Amelanchier arborea (F. Michx.) Fernald | Iowa, United States | NC7 |  | | 2026 | COLLECTED | 06/01/2026 | Mitigwa Scout Camp located on west side of Des Moines River watershed approximately 7.50 miles south, southwest of Boone, T82N R26W N 1/4 Sec. 5 and T83N R26W S 1/4 Sec. 32. | 41.94894500, -93.90537200 | 310 | High-quality white oak - ironwood, mature woods. | Wild material | The native range of Amelanchier arborea is concentrated in the eastern half of the U.S. (Little, 1977). This accession represents a collection of A. arborea germplasm from the western edge of the species native range, specifically central Iowa. Specimens sampled at the collection site in nature were small to medium understory or woodland edge single and/or multi-trunked trees with a few trees getting close to being deemed as canopy specimens. Bark smooth and light grey in color. Specimens sampled in nature ranging 15-50' in height. Peak flowering occurred on 8 April 2026 with white flowers appearing prior to leaf expansion. Fall colors ranging from orange to orange-red peaking typically at the end of September (central Iowa). Fruits, dark-pink to red, maturing in early June (peak in 2026 occurred on 2 June) averaging 8 mm in diameter, except for mother tree #6 that had rather large fruits at 11 mm in diameter. | 2197049 | Ames 38800 |
| 22 | NA 89180 | TJK | Rhododendron minus Michx. var. chapmanii (Alph. Wood) W. H. Duncan & Pullen | Florida, United States | NA | | Contact Site | 2026 | COLLECTED | 04/01/2025 | St. Joseph Bay State Buffer Preserve. Collected from 29.7187833056, -85.2683638611 to 29.7186610833, -85.2689666667 [Note: latitude and longitude of record is selected from the first set of coordinates rather than an average; see the additional field collection note regarding population concentrations.] | 29.71878331, -85.26836386 | 3 | This population is growing in full sun in an area that has been burned in recent years (time frame unknown) and possibly logged. There are scattered large pines, but little shade. This are has been heavily impacted by Category 4/5 hurricanes in recent years and some of the current conditions are undoubtedly a result of this. Soil: The soils of this site are classified as Leon fine sand, 0 to 2 percent slopes (22). The Leon series consists of very deep, very poorly and poorly drained, moderately rapid to moderately slowly permeable soils on upland flats, depressions, stream terraces and tidal areas. They formed in sandy marine sediments of the Eastern Gulf Coast Flatwoods (MLRA 152A), the Atlantic Coast Flatwoods (MLRA 153A) and to a lesser extent in the Southern Coastal Plain (MLRA 133A) and the North-Central Florida Ridge (MLRA 138). Near the type location, the mean annual temperature is about 68 degrees F., and the mean annual precipitation is about 65 inches. Slopes range from 0 to 5 percent. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). Geology: The underlying geology of this area is characterized as Beach Ridge and Dune from the Pleistocene/Holocene which is 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 to facilitate a better understanding of the State's geology. The siliciclastics are light gray, tan, brown to black, unconsolidated to poorly consolidated, clean to clayey, silty, unfossiliferous, variably organic-bearing sands to blue green to olive green, poorly to moderately consolidated, sandy, silty clays. Gravel is occasionally present in the panhandle. Organics occur as plant debris, roots, disseminated organic matrix and beds of peat. Freshwater carbonates, often referred to as marls in the literature, are scattered over much of the State. In southern Florida, freshwater carbonates are nearly ubiquitous in the Everglades. These sediments are buff colored to tan, unconsolidated to poorly consolidated, fossiliferous carbonate muds. Sand, silt and clay may be present in limited quantities. These carbonates often contain organics. The dominant fossils in the freshwater carbonates are mollusks. (Source: USGS Florida Geologic Map Data). | Wild material | Received as R. chapmanii | 2193314 | NA 89180 |
| 23 | NA 89174 | 2025RJLSEUS-16 | Kalmia hirsuta Walter | Florida, United States | NA | | | 2026 | COLLECTED | 10/04/2025 | Eglin Air Force Base: collected along Florida National Scenic Trail/Eglin AFB unnamed road. | 30.43936000, -86.84404500 | 7 | Growing in full sun in dry areas above stream. Slope: 0 percent. Aspect: N/A. Soil: 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). Geology: 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). | Wild material | | 2193308 | NA 89174 |
| 24 | NA 89173 | 2025RJLSEUS-14 | Chionanthus sp. | Florida, United States | NA | | | 2026 | COLLECTED | 10/03/2025 | Choctawhatchee National Forest: the collection site is reached by foot (~0.5 km) along a loose sand road/firebreak from Martin Luther King, Jr. Boulevard, just east of the boundary for Hurlburt Field in Hurlburt Field/Ft. Walton Beach, FL. Collected from 30 deg. 26.859', -86 deg. 39.577' to 30 deg. 27.137', -86 deg. 39.580'; latitude and longitude of record calculated at the midpoint of these coordinates. | 30.44996000, -86.65965000 | 10 | Dry to xeric conditions of well-drained, deep sandy soils on a relatively level area bordering a powerline in an open mixed mostly mixed evergreen and deciduous, somewhat disturbed habitat in sun to part shade. In areas “broadleaved scrub” vegetation is so dense, that it is almost impenetrable. Elevation: 9 to 11 meters. Slope: 0 to 3 percent. Aspect: Variable. Soil: The soils of this area are characterized as Foxworth Series (95 percent) sand, 0 to 5 percent slopes (8). Other soil series interbedded with the Foxworth Series, vary in percentages from 1-4 percent including Lakeland and Chipley. The Foxworth Series consists of very deep, moderately well to somewhat excessively drained, rapid to very rapid permeable soils on broad uplands and side slopes. They formed in sandy marine or eolian sediments in the Southern Coastal Plain (MLRA 133A), The Eastern Gulf Coast Flatwoods (MLRA 152A), The Atlantic Coast Flatwoods (153A) and the Tidewater Area (153B). Thickness of the grayish brown to light yellowish-brown sand exceeds 2 meters. Reaction ranges from very strongly acid to slightly acid throughout. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). Geology: The underlying geology of this area is characterized as undifferentiated Quaternary Sediments. Much of Florida's surface is covered by a varying thickness of undifferentiated sediments consisting of siliciclastics, organics and freshwater carbonates. Where these sediments exceed 6.1 meters thick, they were mapped as discrete units. To subdivide the undifferentiated sediments, those sediments occurring in flood plains were mapped as alluvial and flood plain deposits (Qal). Sediments showing surficial expression of beach ridges and dunes were mapped separately (Qbd) as were the sediments composing Trail Ridge (Qtr). Terrace sands were not mapped (refer to Healy [1975] for a discussion of the terraces in Florida). The subdivisions of the Undifferentiated Quaternary Sediments (Qu) are not lithostratigraphic units but are utilized to facilitate a better understanding of the State's geology. The siliciclastics are light gray, tan, brown to black, unconsolidated to poorly consolidated, clean to clayey, silty, unfossiliferous, variably organic-bearing sands to blue green to olive green, poorly to moderately consolidated, sandy, silty clays. Gravel is occasionally present in the panhandle. Organics occur as plant debris, roots, disseminated organic matrix and beds of peat. Freshwater carbonates, often referred to as marls in the literature, are scattered over much of the State. In southern Florida, freshwater carbonates are nearly ubiquitous in the Everglades. These sediments are buff colored to tan, unconsolidated to poorly consolidated, fossiliferous carbonate muds. Sand, silt and clay may be present in limited quantities. These carbonates often contain organics. The dominant fossils in the freshwater carbonates are mollusks. (Source: USGS Florida Geologic Map Data). | Wild material | Received as C. cf. henryae | 2193307 | NA 89173 |
| 25 | 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 |
| 26 | 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 |
| 27 | 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 |
| 28 | NA 88578 | 2024RJLFL-004 | Ilex vomitoria Aiton | Florida, United States | NA | | | 2024 | COLLECTED | 11/12/2024 | Collected along Florida National Scenic Trail/Eglin Air Force Base unnamed road. | 30.44526100, -86.86094700 | 4 | Mixed evergreen and deciduous forests in part shade to full sun. Slope: 5 to 10 percent. Aspect: Various. The underlying geology of this area is characterized as Citronelle Formation of the Pliocene period. The Citronelle Formation is widespread in the Gulf Coastal Plain. The type section for the Citronelle Formation, named by Matson (1916), is near Citronelle, Alabama. The Citronelle Formation grades laterally, through a broad facies transition, into the Miccosukee Formation of the eastern Florida panhandle. Coe (1979) investigated the Citronelle Formation in portions of the western Florida panhandle. The Citronelle Formation is a siliciclastic, deltaic deposit that is lithologically similar to, and time equivalent with, the Cypresshead Formation and, at least in part, the Long Key Formation (Cunningham et al., 1998) of the peninsula. In the western panhandle, some of the sediments mapped as Citronelle Formation may be reworked Citronelle. The lithologies are the same and there are few fossils present to document a possible younger age. The Citronelle Formation consists of gray to orange, often mottled, unconsolidated to poorly consolidated, very fine to very coarse, poorly sorted, clean to clayey sands. It contains significant amounts of clay, silt and gravel which may occur as beds and lenses and may vary considerably over short distances. Limonite nodules and limonite-cemented beds are common. Marine fossils are rare but fossil pollen, plant remains and occasional vertebrates are found. Much of the Citronelle Formation is highly permeable. It forms the Sand and Gravel Aquifer of the surficial aquifer system contain organics. The dominant fossils in the freshwater carbonates are mollusks. (Source: USGS Florida Geologic Map Data). The soils of this are characterized as Lakeland Series Sand, 5 to 12 percent slopes. The Lakeland series consists of very deep, excessively drained, rapid to very rapidly permeable soils on uplands. They formed in thick beds of eolian or marine and/or fluvio-marine sands in the Southern Coastal Plain MLRA (133A), the Carolina and Georgia Sandhills (MLRA 137), the Eastern Gulf Coast Flatwoods (MLRA 152A) and the Atlantic Coast Flatwoods (MLRA 153A). Slopes are dominantly from 0 to 12 percent but can range to 85 percent in dissected areas. Thickness of the sand exceeds 200 cm. Silt plus clay in the 25 to 100 cm control section ranges from 5 to 10 percent. Reaction ranges from very strongly acid to moderately acid throughout. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). | Wild material | | 2169915 | NA 88578 |
| 29 | 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 |
| 30 | 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 |
| 31 | NA 88581 | 2024RJLFL-012 | Ilex ambigua Torr. | 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. | 30.75763200, -86.80184300 | 32 | Woodland edge. Slope: 3 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 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 | | 2169918 | NA 88581 |
| 32 | 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 |
| 33 | 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 |
| 34 | 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 |
| 35 | 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 |
| 36 | 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 |
| 37 | 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 |
| 38 | 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 |
| 39 | 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 |
| 40 | NA 89091 | 2024RM-TK-004 | Prunus sp. | Florida, United States | NA | | | 2024 | COLLECTED | 09/05/2024 | Blackwater River Wildlife Management Area: on the south side of Boundary Line Road about 0.32 kilometers west of Deaton Bridge Road along an area edged by a barbed wire fence. | 30.68579800, -86.87964300 | 45 | Plants are growing from part-sun to full sun. Plants are growing in an area that is frequently burned with a lot of [Prunus sp. (orig. listed as Prunus alabamensis)] scattered throughout. This habitat is a longleaf pine-wiregrass community with scattered turkey (Quercus laevis) and blackjack oaks (Quercus incana). There is a slight slope downward. The line of [Prunus sp.] goes along a semi-ditch on the side of a dirt road. The plants probably get a bit more water than the plants out in the open forest. The [Prunus sp.] are most often without any other close woody companions. Slope: 0 percent. Aspect: North. Geology: The underlying geology of this area is probably of lower Pliocene age and characterized as the Citronelle Formation. The Citronelle Formation is widespread in the Gulf Coastal Plain. The type section for the Citronelle Formation, named by Matson (1916), is near Citronelle, Alabama. The Citronelle Formation grades laterally, through a broad facies transition, into the Miccosukee Formation of the eastern Florida panhandle. Coe (1979) investigated the Citronelle Formation in portions of the western Florida panhandle. The Citronelle Formation is a siliciclastic, deltaic deposit that is lithologically similar to, and time equivalent with, the Cypresshead Formation and, at least in part, the Long Key Formation (Cunningham et al., 1998) of the peninsula. In the western panhandle, some of the sediments mapped as Citronelle Formation may be reworked Citronelle. The lithologies are the same and there are few fossils present to document a possible younger age. The Citronelle Formation consists of gray to orange, often mottled, unconsolidated to poorly consolidated, very fine to very coarse, poorly sorted, clean to clayey sands. It contains significant amounts of clay, silt and gravel which may occur as beds and lenses and may vary considerably over short distances. Limonite nodules and limonite-cemented beds are common. Marine fossils are rare but fossil pollen, plant remains and occasional vertebrates are found. Much of the Citronelle Formation is highly permeable. It forms the Sand and Gravel Aquifer of the surficial aquifer system. (Source: USGS Florida Geologic Map Data). Soils: The soil of this area is characterized as Lakeland Series Sand, 0 to 5 percent slopes (21). The Lakeland Series consists of very deep, excessively drained, rapid to very rapidly permeable soils on uplands. They formed in thick beds of eolian or marine and/or fluvio-marine sands in the Southern Coastal Plain MLRA (133A), the Carolina and Georgia Sandhills (MLRA 137), the Eastern Gulf Coast Flatwoods (MLRA 152A) and the Atlantic Coast Flatwoods (MLRA 153A). (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). EPA Ecoregion (Level III): Southeastern Plains (65). EPA Ecoregion (Level IV): Southern Pine Plains and Hills (65f). | Wild material | Received as Prunus alabamensis; other collections of this material have proven not to be Prunus serotina var. alabamensis, but actually a species of plum; this will likewise be treated as unidentified material until its species can be ascertained. Collectors' notes refer to the plant by the name under which it was collected. | 2169055 | NA 89091 |
| 41 | NA 89093 | 2024RM-TK-006 | Ilex ambigua Torr. | Florida, United States | NA | | | 2024 | COLLECTED | 09/29/2024 | Blackwater River Wildlife Management Area: growing on the south side of Bud Bass Road, approximately 0.3 kilometers east of Training Center R./Norma Riley Rd. | 30.75759720, -86.80187220 | 29 | This plant is growing in part-shade under mesic conditions along the edge of a longleaf pine plantation. Slope: 0 percent. Aspect: North. Geology: The underlying geology of this area is probably of lower Pliocene age and characterized as the Citronelle Formation. The Citronelle Formation is widespread in the Gulf Coastal Plain. The type section for the Citronelle Formation, named by Matson (1916), is near Citronelle, Alabama. The Citronelle Formation grades laterally, through a broad facies transition, into the Miccosukee Formation of the eastern Florida panhandle. Coe (1979) investigated the Citronelle Formation in portions of the western Florida panhandle. The Citronelle Formation is a siliciclastic, deltaic deposit that is lithologically similar to, and time equivalent with, the Cypresshead Formation and, at least in part, the Long Key Formation (Cunningham et al., 1998) of the peninsula. In the western panhandle, some of the sediments mapped as Citronelle Formation may be reworked Citronelle. The lithologies are the same and there are few fossils present to document a possible younger age. The Citronelle Formation consists of gray to orange, often mottled, unconsolidated to poorly consolidated, very fine to very coarse, poorly sorted, clean to clayey sands. It contains significant amounts of clay, silt and gravel which may occur as beds and lenses and may vary considerably over short distances. Limonite nodules and limonite-cemented beds are common. Marine fossils are rare but fossil pollen, plant remains and occasional vertebrates are found. Much of the Citronelle Formation is highly permeable. It forms the Sand and Gravel Aquifer of the surficial aquifer system. (Source: USGS Florida Geologic Map Data). Soils: The soil of this area is characterized as Lakeland Series Sand, 0 to 5 percent slopes (21). The Lakeland Series consists of very deep, excessively drained, rapid to very rapidly permeable soils on uplands. They formed in thick beds of eolian or marine and/or fluvio-marine sands in the Southern Coastal Plain MLRA (133A), the Carolina and Georgia Sandhills (MLRA 137), the Eastern Gulf Coast Flatwoods (MLRA 152A) and the Atlantic Coast Flatwoods (MLRA 153A). (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). EPA Ecoregion (Level III): Southeastern Plains (65). EPA Ecoregion (Level IV): Southern Pine Plains and Hills (65f). | Wild material | | 2169057 | NA 89093 |
| 42 | NA 87823 | FL24-01 | Ilex cassine L. | Florida, United States | NA | | | 2024 | COLLECTED | 09/05/2024 | Matanzas State Forest. | 29.72143991, -81.28386478 | | Boggy blackwater ditches along edge of dirt road. EPA Ecoregion III: Southern Coastal Plain (75). EPA Ecoregion IV: Eastern Florida Flatwoods (75d). Geology: Beach Ridge and Dune. Soil: Immokalee Series Fine Sand. | Wild material | | 2168973 | NA 87823 |
| 43 | Ames 36260 | Thomson Causeway Recreation Area | Cornus drummondii C. A. Mey. | Illinois, United States | NC7 |  | | 2024 | COLLECTED | 08/19/2024 | Thomson Causeway Recreation Area, approximately 1 mile southwest of Thomson. Scattered along Potter Road starting just east of the causeway heading west, and along the gravel service road to the south. T23N R3E SE 1/4 Sec. 26. | 41.94919700, -90.11822100 | 179 | Floodplain of wetland complex along east bank of Mississippi River. Soils are moist and seasonally inundated with high organic matter content. | Wild material | Shrubs in nature measuring approximately 10 feet in height (to 15 feet) with varying degrees of red pigmentation on the pedicles. Peak fruit ripening occurred in late August 2024. Minor foliar disease noted at the time of collection. Growing as individual shrubs in shadier locations and forming thickets in sunnier sites. | 2168984 | Ames 36260 |
| 44 | 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 |
| 45 | 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 |
| 46 | WLP 3411 | TJK2023FL-044 | Cyrilla racemiflora L. | Florida, United States | NA |  | | 2024 | COLLECTED | 12/26/2023 | Forest Hill Cemetery, east fence line, 0.4 mi north of Hwy 98, off Twine Rd. | 29.78030000, -85.27160000 | 7 | Growing on the edge of a wet pine savanna/flatwood. Slope: flat. Aspect: Southeast. Elevation: 23 feet. | Wild material | | 2165704 | WLP 3411 |
| 47 | WLP 3412 | TJK2023FL-045 | Lyonia lucida (Lam.) K. Koch | Florida, United States | NA | | | 2024 | COLLECTED | 12/26/2023 | East backwoods adjacent to Forest Hill Cemetery, 0.4 mi north of Hwy 98, off Twine Rd. | 29.78030000, -85.27160000 | 7 | Edge of a wet pine savanna/flatwood. Slope: flat. Aspect: Southeast. Elevation: 23 feet. | Wild material | | 2165705 | WLP 3412 |
| 48 | NA 88827 | RJL-RM2023FLAL-001 | Ilex ambigua Torr. | Florida, United States | NA | | | 2023 | COLLECTED | 12/05/2023 | Yellow River Wildlife Management Area, along DOF [Department of Forestry] Y9 dirt road 0.08 kilometers east of Miller Bluff Road. | 30.65289100, -86.87602800 | 44 | Growing in part shade to sun in very dry, highly competitive site still recovering from the logging of pines in the past decade. This young woodland is comprised of a combination of evergreen and deciduous species competing for available resources and light before the young sand pines begin to dominate the upper canopy. Slope: 0 percent. Aspect: N/A. The underlying geology of this area is the Citronelle Formation, of Pliocene origin, and consists of gray to orange, often mottled, unconsolidated to poorly consolidated, very fine to very coarse, poorly sorted, clean to clayey sands. It contains significant amounts of clay, silt and gravel which may occur as beds and lenses and may vary considerably over short distances. Limonite nodules and limonite-cemented beds are common. (Source: USGS Florida Geologic Map Data.) The primary soil type in the collection area is classified as Lakeland Sand soils (0 to 5 percent slopes). The surface soil profile of this area is primarily the Lakeland series which consists of very deep, excessively drained, rapid to very rapidly permeable soils on uplands. They formed in thick beds of eolian or marine and/or fluvio-marine sands. Thickness of the sand exceeds 2 meters. Silt plus clay in the upper meter ranges from 5-10 percent. Reaction ranges from very strongly acid to moderately acid throughout. (Source: NRCS Web Soil Survey.) | Wild material | | 2165657 | NA 88827 |
| 49 | NA 88828 | RJL-RM2023FLAL-002 | Vaccinium arboreum Marshall | Florida, United States | NA | | | 2023 | COLLECTED | 12/05/2023 | Yellow River Wildlife Management Area, along DOF [Department of Forestry] Y9 dirt road 0.08 kilometers east of Miller Bluff Road. | 30.65289100, -86.87608500 | 44 | Growing in part shade to sun in very dry, highly competitive site still recovering from the logging of pines in the past decade. This young woodland is comprised of a combination of evergreen and deciduous species competing for available resources and light before the young sand pines begin to dominate the upper canopy. Slope: 0 percent. Aspect: N/A. The underlying geology of this area is the Citronelle Formation, of Pliocene origin, and consists of gray to orange, often mottled, unconsolidated to poorly consolidated, very fine to very coarse, poorly sorted, clean to clayey sands. It contains significant amounts of clay, silt and gravel which may occur as beds and lenses and may vary considerably over short distances. Limonite nodules and limonite-cemented beds are common. (Source: USGS Florida Geologic Map Data.) The primary soil type in the collection area is classified as Lakeland Sand soils (0 to 5 percent slopes). The surface soil profile of this area is primarily the Lakeland series which consists of very deep, excessively drained, rapid to very rapidly permeable soils on uplands. They formed in thick beds of eolian or marine and/or fluvio-marine sands. Thickness of the sand exceeds 2 meters. Silt plus clay in the upper meter ranges from 5-10 percent. Reaction ranges from very strongly acid to moderately acid throughout. (Source: NRCS Web Soil Survey.) | Wild material | | 2165658 | NA 88828 |
| 50 | 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 |
| 51 | 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 |
| 52 | 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 |
| 53 | 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 |
| 54 | 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 |
| 55 | 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 |
| 56 | 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 |
| 57 | NA 88850 | RJL-RM2023FLAL-024 | Rhododendron austrinum (Small) Rehder | Florida, United States | NA | | | 2023 | COLLECTED | 12/13/2023 | Yellow River Water Management Area, found in an area where an unnamed unpaved road winds along the edges of the Yellow River. This unpaved road is accessed from Old River Road to the east near the junction with Shockley Springs Road. Individuals are found along the roadside for at least 6 kilometers from the point where the unnamed road splits and turns south. | 30.82647700, -86.60892000 | 23 | Plants are growing primarily in part shade to shade in mesic conditions in a mixed evergreen and deciduous forest. Fruiting plants are more abundant where plants receive more sunlight. Slope: 0 to 2 percent. Aspect: Various. The underlying geology of this area is the Alum Bluff Group of Miocene origin. It includes the Chipola Formation, Oak Grove Sand, Shoal River Formation, Choctawhatchee Formation and the Jackson Bluff Formation. The formations included in this group are generally defined on the basis of their molluscan faunas and stratigraphic position. Puri (1953) described sediment facies as they relate to the formations of the Alum Bluff Group. These sediments are lithologically distinct as a group, not as individual units. The Alum Bluff Group crops out or is beneath a thin overburden in the western panhandle from river valleys in Okaloosa County eastward to western Jackson County. The Alum Bluff Group consists of clays, sands and shell beds which may vary from fossiliferous, sandy clays to unfossiliferous sands and clays and occasional carbonate beds. Mica is a common constituent and glauconite and phosphate occur sporadically. Induration varies from essentially nonindurated in sands to well indurated in carbonate lenses. Colors range from cream to olive gray with mottled reddish brown in weathered sections. Sand grain size varies from very fine to very coarse with sporadic occurrences of gravel. These sediments generally have low permeabilities and are part of the intermediate confining unit/aquifer system. (Source: USGS Florida Geologic Map Data.) The surface soil profile of this area is primarily Yemassee, Garcon, and Bigbee soils that are occasionally flooded. The Yemassee Series consists of very deep, somewhat poorly drained, moderately permeable, loamy soils that formed in marine sediments. These soils are on terraces and broad flats of the lower Coastal Plain and very strongly acid. Slopes range from 0 to 2 percent. The Garcon Series consists of very deep, somewhat poorly drained, moderately permeable soils on terraces and in the broad flats of the lower Coastal Plain. They formed in sandy and loamy marine sediments. This soil ranges from very strongly acid to extremely acid. The Bigbee series consists of very deep, excessively drained, rapidly permeable soils that are on natural levees and higher positions in flood plains along stream flood plains in the Southern Coastal Plain (MLRA 133A) and the Eastern Gulf Coast Flatwoods (MLRA 152A). They formed in thick sandy alluvial sediments. They range from strongly acid to very strongly acid. (Source: NRCS Web Soil Survey.) | Wild material | | 2165680 | NA 88850 |
| 58 | NA 88800 | TXWL2023-015 | Ilex longipes Chapm. ex Trel. | Texas, United States | NA | | | 2023 | COLLECTED | 11/15/2023 | Sabine National Forest: Compartment 65 along County Road 131 near White Rock, Texas. | 31.55793500, -94.01980900 | | Upland; mixed hardwood and pine; sandy soil; rocky outcrops. | Wild material | | 2159157 | NA 88800 |
| 59 | WLP 3343 | TXWL2023-014 | Croton michauxii G. L. Webster | Texas, United States | NA | | | 2023 | COLLECTED | 11/07/2023 | Angelina National Forest: Compartment 84 Black Branch Area. | 31.03849000, -94.18679000 | | Glade area on the Catahould/Fleming formation. | Wild material | | 2159156 | WLP 3343 |
| 60 | NA 88709 | RJL2023NCSC-014 | Rhododendron minus Michx. | South Carolina, United States | NA | | | 2023 | COLLECTED | 11/13/2023 | Northwest side of the junction of Wire Road and Prichard Horse Road. | 34.49925200, -80.27470600 | 146 | Plants growing in shade to part-shade of dry steep slope woodland habitat that is primarily composed of Pinus palustris. Slope: 2 to 20 percent. Aspect: North. 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 South Carolina Geologic Map Data.) The primary soil type in the collection area is classified as Ailey Series sand, moderately wet, 2 to 6 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 | | 2159137 | NA 88709 |
| 61 | 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 |
| 62 | 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 |
| 63 | 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 |
| 64 | 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 |
| 65 | 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 |
| 66 | 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 |
| 67 | 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 |
| 68 | 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 |
| 69 | 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 |
| 70 | NA 88665 | RJL2023PA-002 | Ilex verticillata (L.) A. Gray | Pennsylvania, United States | NA | | | 2023 | COLLECTED | 10/01/2023 | Woodlands along Pine Creek near the Harmonyville Road bridge. | 40.18764500, -75.76732200 | 141 | Moist to mucky, wet woodland conditions along Pine Creek. Much of the site is very wet due to recent rains; though, earlier in the year, the soils were only moist. Plants grow in both well-drained mesic conditions as well as seasonally wet conditions. They do not grow in standing water anywhere in this location. Plants in this population are found mostly in the shade and partial shade of deciduous trees; there are occasional gaps that offer higher light conditions as well. Slope: 0-2%. Aspect: N/A. The underlying geology of this area is of Precambrian origin and characterized as the Graphitic Felsic Gneiss. This includes Pickering Gneiss and small areas of marble; dominantly quartz and feldspar with varying amounts of graphite and various metamorphic minerals; medium grained, light to dark gray and greenish gray; sedimentary origin. (Source: USGS Pennsylvania Geologic Map Data). The primary soil type in the area of this collection is classified as Hatboro Silt Loam Series. The Hatboro Series consists of very deep and poorly drained soils formed in alluvium derived from metamorphic and crystalline rock. They are on flood plains. Slopes range from 0 to 3 percent. Saturated hydraulic conductivity is moderately high to high. Solum thickness ranges from 50 to 150 cm. Depth to bedrock ranges from 1.5 to 3 meters or more. Organic carbon decreases irregularly with depth or is greater than 0.2 percent directly above any strongly contrasting C horizon. The depth to strongly contrasting sand and gravel is more than 100 cm or the transition is greater than 12.5 cm. Content of gravel ranges from 0 to 10 percent in the solum and from 0 to 80 percent in the C horizon. Mica flakes are common in the solum, and the C horizon contains thin lenses of mica. Reaction ranges from very strongly acid through neutral to a depth of 75 cm and from moderately acid through slightly acid below 75 cm. (Source: NRCS Web Soil Survey.) | Wild material | | 2158814 | NA 88665 |
| 71 | 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 |
| 72 | 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 |
| 73 | 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 |
| 74 | WLP 3136 | TJK2023FL-010 | Morella cerifera (L.) Small | Florida, United States | NA | | | 2023 | COLLECTED | 08/18/2023 | Blackwater State Forest: Wolfe Creek. | 30.80751000, -86.95774000 | 52 | Beautiful xeric pine-oak upland community. Transitions to mesic slopes and then to seepage bottom, stringer wetland community adjacent to the Wolfe Creek. Area is on a regular 2-4[-year] burn cycle. Slope: 10%. Aspect: South. Elevation recorded as 172 feet. | Wild material | Received as Morella pumila (Morella cerifera var. pumila). Treated tentatively as Morella cerifera Pumila Group. WLPGR contract collection. | 2158468 | WLP 3136 |
| 75 | NA 89264 | TJK2023FL-002 | Gaylussacia frondosa (L.) Torr. & A. Gray var. nana A. Gray | Florida, United States | NA | | | 2023 | COLLECTED | 05/19/2023 | Blackwater State Forest: Wolfe Creek. | 30.80760000, -86.96250000 | 49 | Beautiful xeric pine-oak upland community. Transitions to mesic slopes and then to seepage bottom, stringer wetland community adjacent to the Wolfe Creek. Area is on a regular 2-4[-year] burn cycle. Slope: 5%. Aspect: Northwest. Elevation recorded as 161 feet. | Wild material | WLPGR contract collection. Received as Gaylussacia tomentosa (nana). | 2158247 | NA 89264 |
| 76 | NA 89265 | TJK2023FL-003 | Ceanothus sp. | Florida, United States | NA | | | 2023 | COLLECTED | 05/19/2023 | Blackwater State Forest: Wolfe Creek. | 30.80650000, -86.95840000 | 49 | Beautiful xeric pine-oak upland community. Transitions to mesic slopes and then to seepage bottom, stringer wetland community adjacent to the Wolfe Creek. Slope: 20%. Aspect: Northwest. Elevation recorded as 162 feet. | Wild material | WLPGR contract collection. Received as Ceanothus microphyllus. | 2158248 | NA 89265 |
| 77 | NA 89267 | TJK2023FL-005 | Ceanothus americanus L. | Florida, United States | NA | | | 2023 | COLLECTED | 06/10/2023 | Blackwater State Forest: Wolfe Creek. | 30.80760000, -86.96250000 | 49 | Beautiful xeric pine-oak upland community. Transitions to mesic slopes and then to seepage bottom, stringer wetland community adjacent to the Wolfe Creek. Area is on a regular 2-4[-year] burn cycle. Slope: 5%. Aspect: Northwest. Elevation recorded as 161 feet. | Wild material | WLPGR contract collection. | 2158250 | NA 89267 |
| 78 | NA 89269 | TJK2023FL-007 | Vaccinium darrowii Camp | Florida, United States | NA | | | 2023 | COLLECTED | 06/10/2023 | Blackwater State Forest: Wolfe Creek. | 30.80560000, -86.95770000 | 60 | Beautiful xeric pine-oak upland community. Transitions to mesic slopes and then to seepage bottom, stringer wetland community adjacent to the Wolfe Creek. Area is on a regular 2-4[-year] burn cycle. Slope: 2%. Aspect: West-northwest. Elevation recorded as 197 feet. | Wild material | WLPGR contract collection. | 2158252 | NA 89269 |
| 79 | 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 |
| 80 | WLP 3084 | RM2023-002 | Rhododendron viscosum (L.) Torr. | Florida, United States | NA | | | 2023 | COLLECTED | 09/15/2022 | This species is growing in the Blackwater River State Forest approximately 0.24 kilometers north of Wof W20 and approximately 0.93 kilometers west of the junction of 3 Notch Trail/Road. | 30.84510000, -86.94940000 | 38 | The plants were growing in part shade of a moist mesic transition slope between a dry upland habitat and a bog.
Soils: The underlying geology of this area is the Citronelle Formation, of Pliocene origin, and consists of gray to orange, often mottled, unconsolidated to poorly consolidated, very fine to very coarse, poorly sorted, clean to clayey sands. It contains significant amounts of clay, silt and gravel which may occur as beds and lenses and may vary considerably over short distances. Limonite nodules and limonite-cemented beds are common. Source: USGS Florida Geologic Map Data (https://mrdata.usgs.gov/geology/state/state.php?state=fl)
The surface soil profile found in this area is primarily Troup Series. These soils are sandy and loamy marine deposits. They are well drained and typically on the tops and sides of broad and narrow ridges on uplands typically with 0-12% slopes. These soils are very strongly acid with a depth of 2-3 meters. Pactolus Series soils comprise a minor, but important percentage of the lower slopes that are nearly level to gently sloping and account for the somewhat poorly drained, yet, sandy conditions. These soils are also strongly acid with very dark gray loamy sands.
Source: Soil Survey of Santa Rosa County and NRCS Web Soil Survey (https://www.nrcs.usda.gov/Internet/FSE_MANUSCRIPTS/florida/FL113/0/SantaRosa.pdf and https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2141438 | WLP 3084 |
| 81 | 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 |
| 82 | 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 |
| 83 | NA 88522 | RM-TK2022-010 | Viburnum dentatum L. var. scabrellum Torr. & A. Gray | Florida, United States | NA | | | 2023 | COLLECTED | 10/10/2022 | Plants growing in woodlands via an unnamed dirt road accessed from Old Ferry Road. | 30.91880000, -87.25990000 | 43 | Plants are growing in an upland habitat on the edge of south-facing woodland in part-shade.
Soils: The underlying geology of this area is classified as Alluvium of Pleistocene/Holocene origin and consists of undifferentiated Quaternary sediments of varying thickness including siliciclastics, organics and freshwater carbonates. The siliciclastics are light gray, tan, brown to black, unconsolidated to poorly consolidated, clean to clayey, silty, unfossiliferous, variably organic-bearing sands to blue green to olive green, poorly to moderately consolidated, sandy, silty clays. Organics occur as plant debris, roots, disseminated organic matrix and beds of peat. Freshwater carbonates, often referred to as marls in the literature, are scattered.
Source: USGS Florida Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=FLPSHal%3B0)
The primary soil type in the collection area is classified as Orangeburg sandy loam soil (2 to 5 percent slopes). The Orangeburg Series consists of very deep, well drained, moderately permeable soils on uplands of the Southern Coastal Plain. They formed in loamy and clayey marine sediments. The reaction of all this soil ranges from very strongly acid to strongly acid.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2140803 | NA 88522 |
| 84 | NA 88523 | RM-TK2022-011 | Ilex ambigua Torr. | Florida, United States | NA | | | 2023 | COLLECTED | 10/16/2022 | Blackwater River State Park: growing along unnamed dirt road approximately 0.26 kilometers north of the intersection with Boundary Line Road. | 30.68790000, -86.86230000 | 56 | Plants are growing in hot, dry, full sun conditions. 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). The primary soil type in the collection area is classified as Lakeland Sand soils (5 to 12 percent slopes). The surface soil profile of this area is primarily the Lakeland series which consists of very deep, excessively drained, rapid to very rapidly permeable soils on uplands. They formed in thick beds of eolian or marine and/or fluvio-marine sands. Thickness of the sand exceeds 2 meters. Silt plus clay in the upper meter ranges from 5-10 percent. Reaction ranges from very strongly acid to moderately acid throughout. (Source: NRCS Web Soil Survey). | Wild material | | 2140804 | NA 88523 |
| 85 | 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 |
| 86 | 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 |
| 87 | 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 |
| 88 | 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 |
| 89 | 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 |
| 90 | NA 88545 | RJLSEUS2022-017 | Cephalanthus occidentalis 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. Infrequent frequency. | 31.63802000, -84.13499000 | 59 | Plants are growing in part-shade to sun in the wetland associated with a large pond. This area is frequently wet during the growing season, but drier during the winter months.
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 | | 2140771 | NA 88545 |
| 91 | 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 |
| 92 | 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 |
| 93 | NA 88562 | RJLSEUS2022-035 | Kalmia latifolia L. | Alabama, United States | NA | | | 2023 | COLLECTED | 12/12/2022 | Plants growing on both sides of River Ridge Road accessed from Alabama State Hwy 41 via Tin Cup Alley Road. Common at this site | 31.73823700, -87.35821100 | 132 | Plants are growing in part-shade to full sun on top of a very exposed ridge top under dry conditions.
Soils: The underlying geology of this area is of Eocene origin and characterized as Claiborne Group; Gosport Sand and Lisbon Formation Undifferentiated in part. Greenish-gray calcareous, glauconitic, fossiliferous clayey sand; marl; carbonaceous sand; carbonaceous silty clay; and coarse glauconitic, fossiliferous, quartz sand.
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 Saffell Very Gravelly Sandy Loam soil (5 to 8 percent slopes). 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.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2140787 | NA 88562 |
| 94 | 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 |
| 95 | 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 |
| 96 | NA 88565 | RJLSEUS2022-038 | Ilex ambigua Torr. | Florida, United States | NA | | | 2023 | COLLECTED | 12/14/2022 | Eglin Air Force Base: growing along the east side of Eglin AFB Choctaw Nolf Road northwest of Choctaw Navy Outlying Field. This road goes west and takes circuitous route to the north around the Field en route to Escribano Point Wildlife Management Area. | 30.51507900, -86.96767100 | 14 | Full sun on the top of the roadside slope in well-drained to dry conditions, 1-2 meters above surrounding lower, moist area. The underlying geology of this area is the Citronelle Formation, of Pliocene origin, and consists of gray to orange, often mottled, unconsolidated to poorly consolidated, very fine to very coarse, poorly sorted, clean to clayey sands. It contains significant amounts of clay, silt and gravel which may occur as beds and lenses and may vary considerably over short distances. Limonite nodules and limonite-cemented beds are common. (Source: USGS Florida Geologic Map Data). The primary soil type in the collection area is classified as Lakeland Sand soils (5 to 12 percent slopes). The surface soil profile of this area is primarily the Lakeland series which consists of very deep, excessively drained, rapid to very rapidly permeable soils on uplands. They formed in thick beds of eolian or marine and/or fluvio-marine sands. Thickness of the sand exceeds 2 meters. Silt plus clay in the upper meter ranges from 5-10 percent. Reaction ranges from very strongly acid to moderately acid throughout. (Source: NRCS Web Soil Survey). | Wild material | | 2140822 | NA 88565 |
| 97 | 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 |
| 98 | 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 |
| 99 | NA 88568 | RJLSEUS2022-041 | Oxydendrum arboreum (L.) DC. | Florida, United States | NA | | | 2023 | COLLECTED | 12/14/2022 | Plants growing along the south 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. Common at the location; infrequent, otherwise. | 30.51525300, -87.00563800 | 2 | Trees are growing in full sun to part-shade in mesic habitat associate with a nearby wet depression, less than 0.2 meters above the high moisture zone. The trees also extend into slightly drier mesic to the marginally xeric zone.
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.
The primary soil types in the collection area are classified as Leon Sand soils (0 to 2 percent slopes). The Leon Series consists of very deep, very poorly and poorly drained, moderately rapid to moderately slowly permeable soils on upland flats, depressions, stream terraces and tidal areas. They formed in sandy marine sediments of the Eastern Gulf Coast Flatwoods, the Atlantic Coast Flatwoods, and to a lesser extent in the Southern Coastal Plain, and the North-Central Florida Ridge. Slopes range from 0 to 5 percent. Leon series is comprised of 95%+ sand in the strata to 3+ meters deep.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2140790 | NA 88568 |
| 100 | Ames 35968 | GLT2022-006 | Hypericum kalmianum L. | Michigan, United States | NC7 |  | | 2022 | COLLECTED | 09/24/2022 | Grand Beach Marsh Nature Preserve lcoated approximately 2.30 miles southwest of Buffalo on highway 12, T8S R21W NW 1/4 SW 1/4 Sec. 17. | 41.77560800, -86.78127800 | 187 | Central coastal plain marsh/sand prairie. Granby-Morocco complex soil type. | Wild material | Description of plants sampled in nature: Upright, branching shrubs with few basal stems/ramets; to1.5 m in height and 1.5 to 2 cm basal diameter; bark grayish-brown to coppery and exfoliating with age; leaves blue-green and narrowly ovate to oblong; capsules 5-angled/ribbed, yellowish-green, typically 3 but up to to 15 per dichasium. | 2140747 | Ames 35968 |
| 101 | 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 |
| 102 | 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 |
| 103 | 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 |
| 104 | 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 |
| 105 | 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 |
| 106 | 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 |
| 107 | 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 |
| 108 | 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 |
| 109 | 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 |
| 110 | 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 |
| 111 | W6 59929 | CBG-10652 | Hottonia inflata Elliott | Illinois, United States | W6 | | | 2021 | | | | | | | Wild material | | 2132508 | W6 59929 |
| 112 | Ames 35750 | Ames 35750 | Blephilia ciliata (L.) Benth. | Iowa, United States | NC7 |  | | 2021 | COLLECTED | 09/27/2021 | Located approximately 3 miles south, southeast of Fairfield, T71N R9W SW1/4 Sec. 7 | 40.96338000, -91.94686900 | 223 | Woodland openings/edges, disturbed areas | Wild material | | 2122068 | Ames 35750 |
| 113 | OPGC 8343 | CBG-10575 | Euthamia graminifolia (L.) Nutt. | Illinois, United States | OPGC | | | 2021 | | | | | | | Wild material | Plant numbers sampled estimated. | 2120166 | OPGC 8343 |
| 114 | OPGC 8359 | CBG-10615 | Symphyotrichum drummondii (Lindl.) G. L. Nesom | Illinois, United States | OPGC | | | 2021 | | | | | | | Wild material | Plant numbers sampled estimated. | 2120231 | OPGC 8359 |
| 115 | W6 59222 | CBG-10529 | Gratiola neglecta Torr. | Illinois, United States | W6 | | | 2021 | | | | | | | Wild material | Plant numbers estimated. | 2120137 | W6 59222 |
| 116 | W6 59234 | CBG-10548 | Dasistoma macrophyllum (Nutt.) Raf. | Illinois, United States | W6 | | | 2021 | | | | | | | Wild material | Received as Dasistoma macrophylla. Plant numbers estimated. Few this year; abundant other years in numerous locations. | 2120206 | W6 59234 |
| 117 | W6 59238 | CBG-10552 | Agrostis perennans (Walter) Tuck. | Illinois, United States | W6 |  | | 2021 | | | | | | | Wild material | Collection date assumption. Plant numbers estimated. | 2120151 | W6 59238 |
| 118 | W6 59243 | CBG-10560 | Cinna arundinacea L. | Illinois, United States | W6 | | | 2021 | | | | | | | Wild material | Plant numbers estimated. | 2120155 | W6 59243 |
| 119 | W6 59267 | CBG-10590 | Muhlenbergia glabrifloris Scribn. | Illinois, United States | W6 | | | 2021 | | | | | | | Wild material | Received as: Muhlenbergia glabriflora. Plant numbers sampled estimated. | 2120210 | W6 59267 |
| 120 | W6 59274 | CBG-10598 | Scrophularia marilandica L. | Illinois, United States | W6 | | | 2021 | | | | | | | Wild material | Plant numbers sampled estimated. | 2120183 | W6 59274 |
| 121 | Ames 35668 | Iroquois County Conservation Area | Aronia ×prunifolia (Marshall) Rehder | Illinois, United States | NC7 |  | | 2021 | COLLECTED | 05/05/2021 | Iroquois County Conservation Area located approximately 4.5 miles northeast of Beaverville in Beaverville Township, T29N R11W NE1/4 Sec. 22 | 40.99154700, -87.58073200 | 198 | Woodland edge of wet sand prairie | Wild material | Wide variety of genotypes noted in nature averaging 3.5-7' in height. Some growing in shade of oak forest were sparse suckering and open branching compared to open grown specimens that were extremely dense with suckers. | 2115977 | Ames 35668 |
| 122 | NA 88281 | MARSB-497 | Cephalanthus occidentalis L. | New Jersey, United States | NA | | | 2021 | | | | | | | Wild material | Growth formûthe plant is a shrub (i.e., a woody plant with several stems growing from the base)ûLeaf typeûthe leaf blade is simple (i.e., lobed or unlobed but not separated into leaflets)ûLeaves per nodeûthere are three leaves per node along the stemûthere are two leaves per node along the stemûLeaf blade edgesûthe edge of the leaf blade has teethûLeaf durationûthe leaves drop off in winter (or they wither but persist on the plant)ûarmature on plantûthe plant does not have spines, prickles, or thornsûLeaf blade lengthû80–150 mmûLeaf blade widthû23–150 mmûLeaf stalkûthe leaves have leaf stalksûFruit type (general)ûthe fruit is dry but does not split open when ripeûBark textureûthe bark of an adult plant is ridged or platedûthe bark of an adult plant is thin and smoothûTwig winter colorûbrownûgrayûredûBud scale numberûthere are no scales on the winter buds | 2113542 | NA 88281 |
| 123 | WLP 2021 | MARSB-980 | Viburnum dentatum L. | New York, United States | NA | | | 2019 | COLLECTED | 08/16/2019 | Richmond County; Staten Island; Blue Heron Park. | | | Red maple forest in full shade; growing in moist, poorly drained silt/sand soil. | | Seed collected from 3 plants in population of 25, over an area of 20 square meters; population shaded out, very little seed/flower. Deer browse also heavy throughout park. Seed maturation: middle. | 2109170 | WLP 2021 |
| 124 | NA 88095 | MARSB-256 | Ilex verticillata (L.) A. Gray | New York, United States | NA |  | | 2019 | COLLECTED | 10/07/2015 | In Sag Harbor, NY, park in Mashashimuet Park. Walk along the Long Pond Greenbelt Trail. The population is along the edges of Long Pond and Crooked Pond, the first and third ponds on the left, respectively. | 40.96283000, -72.29366000 | 5 | Central shrub & herb depression pond. | Wild material | | 2097543 | NA 88095 |
| 125 | NA 88096 | MARSB-258 | Ilex glabra (L.) A. Gray | New York, United States | NA |  | | 2019 | COLLECTED | 10/08/2015 | In Sag Harbor, park in Mashashimuet Park. Enter the Long Pond Greenbelt and walk along it until you reach Crooked Pond, the third pond on the left. The population is along pond edges. | 40.96283000, -72.29366000 | 5 | Central shrub & herb depression pond. | Wild material | | 2097545 | NA 88096 |
| 126 | OPGC 7884 | MARSB-259 | Rhexia virginica L. | New York, United States | OPGC |  | | 2019 | | | | | | | Wild material | | 2097546 | OPGC 7884 |
| 127 | Ames 35220 | Ames 35220 | Aronia ×prunifolia (Marshall) Rehder | Wisconsin, United States | NC7 |  | | 2019 | COLLECTED | 09/04/2019 | Watershed area of Brule River. Collection site located approximately 3.75 miles southwest of Winneboujou, 0.30 miles west of intersection of Francis Willard Road and Forestry Road, T46N R10W SW1/4 SW1/4 Sec. 8, Douglas County | 46.47574000, -91.65172000 | 359 | Ecotone of Tamarack Swamp, Northern Sedge Meadow and Upland Northern Hardwood Forest | Wild material | Plants in nature ranging from 1.0-2.5 meters in height. Fruits measuring approximately 7-9mm in diameter and dark reddish-purple at time of collection (4 September 2019). | 2097756 | Ames 35220 |
| 128 | W6 56616 | CBG-8805 | Carex lupulina Muhl. ex Willd. | Illinois, United States | W6 |  | | 2019 | | | | | | | Wild material | | 2092715 | W6 56616 |
| 129 | Ames 34610 | JDC/MB/2019/015/894 | Monarda brevis (Fosberg & Artz) Floden | West Virginia, United States | NC7 |  | | 2019 | | | | | | | Wild material | Many genets noted at collection site in nature consisted of 25-30 stems, but individual stems are widely spaced (e.g. 1-5") apart compared to other populations (four) noted (2019 reconnaisance) where stem spacing was typically observed at 0.25-0.5" apart. Very healthy, dark-green leaves noted in early/mid June, but leaf quality greatly declined when observed in mid-August in contrast to other populations observed in nature that seemed to maintain leaf quality throughout the season. Many plants at this site were defoliated likely due to disease (leaf spot) or tattered likely due to possible insect feeding. Specimens noted were circa 10-12 days from initiation of flowering on 12 June 2019 and during mid-August a few specimens were still observed flowering with about 10-20% of infructescences were still green. The overall phenology of this M. brevis population at this site is quite different in comparison to other populations (four) observed in 2019, with flowering being much later (e.g. 10-25 days); leaf quality lower; and synchronization of flowering extremely variable within genets of this population. | 2092646 | Ames 34610 |
| 130 | NA 88006 | MARSB-740 | Clethra alnifolia L. | New York, United States | NA |  | | 2018 | | | | | | | Wild material | | 1964840 | NA 88006 |
| 131 | W6 53028 | CBG-7314 | Carex tribuloides Wahlenb. | Illinois, United States | W6 |  | | 2017 | | | | | | | Wild material | | 1954779 | W6 53028 |
| 132 | Ames 34160 | Ames 34160 | Fraxinus americana L. | Pennsylvania, United States | NC7 |  | | 2017 | COLLECTED | 11/01/2017 | Urban loaction near the intersection of Pennsylvania ave. and Fort Washington Ave. Fort Washington, Montgomery County. | 40.13730600, -75.21111800 | 66 | Specimens located along a possible eixisting naural hedge row along the rightway of two existing parking lots. | Uncertain improvement status | | 1957726 | Ames 34160 |
| 133 | Ames 33358 | 730-1 | Betula nigra L. | Illinois, United States | NC7 |  | | 2016 | COLLECTED | 06/07/2016 | Momence wetlands - Kankakee River watershed, Kankakee County | 41.16335000, -87.52944100 | | Floodplain | Wild material | | 1940581 | Ames 33358 |
| 134 | Ames 32963 | JDC/BA/2015/049/706 | Betula alleghaniensis Britton | Iowa, United States | NC7 | | | 2015 | COLLECTED | 09/14/2015 | Bixby State Preserve, T91N R5W extreme southern edge of Sec. 23 basically restricted to W 1/2 of Sec. 23. | 42.67470300, -91.39917300 | 308 | North-facing algific talus slope (45-60 degrees) adjacent to Bear Creek. Moist deciduous woods. Growing in association with Diervilla lonicera, Hamamelis virginiana, Corylus sp., Viburnum opulus var. americanum, Cornus rugosa (few), Cornus alternifolia, Fraxinus nigra, Quercus rubra, Viburnum lentago, Ribes sp., Rubus idaeus subsp. strigosus, Rhamnus alnifolia (few), Rosa sp., Taxus canadensis, Prunus virginiana, Impatiens sp., Dirca palustris, and Pinus strobus (few). | Wild material | | 1927433 | Ames 32963 |
| 135 | Ames 32965 | JDC/BA/2015/051/708 | Betula alleghaniensis Britton | Iowa, United States | NC7 | | | 2015 | COLLECTED | 09/15/2015 | Yellow River State Forest, T97N R4W northern edge of SW 1/4 NW 1/4 Sec. 36 | 43.17782100, -91.26584600 | 227 | North-facing algific talus slope (45-60 degrees) adjacent to Paint Creek. Moist deciduous woods. Growing in association with Fraxinus nigra, Staphylea trifolia, Carpinus caroliniana, Quercus rubra, Acer saccharum, Cornus alternifolia, Amelanchier arborea, Ostrya virginiana, Viburnum opulus var. americanum, Cornus rugosa, Cornus alternifolia, Zanthoxylum americanum, Viburnum rafinesqueanum, Cypripedium pubescens, Ribes sp.,Corylus sp., Juniperus virginiana, Dirca palustris, Ulmus thomasii, Prunella vulgaris, Diervilla lonicera, Quercus macrocarpa, Carya cordiformis, Taxus canadensis, Tilia americana, Adiantum pedatum, and Aconitum noveboracense. | Wild material | | 1927435 | Ames 32965 |
| 136 | Ames 32966 | JDC/VA/2015/052/709 | Viburnum opulus L. var. americanum Aiton | Iowa, United States | NC7 |  | | 2015 | COLLECTED | 09/15/2015 | Yellow River State Forest, T97N R4W northern edge of SW ¼ NW ¼ Sec. 36. | 43.17778200, -91.26642800 | 239 | North-facing algific talus slope (45-60 degrees) adjacent to Paint Creek. Moist deciduous woods. | Wild material | Formerly known as Viburnum trilobum, American highbush cranberry (V. opulus var. americanum) is a North American native shrub that is utilized as an important ornamental and conservation plant that is also harvested as a minor fruit crop (jams/jellies). In nature, this variety is generally found in moist habitats typically along stream banks and swamps where ample moisture is readily available. The native range of V. opulus var. americana is concentrated in the northeastern United States and into Canada (Little, E. L. Jr. 1977). Attractive ornamental characteristics includes showy lacecap flowers in spring and bright red fruits and foliage in the fall. Fruits are tart with a hint of sweetness. The European highbush cranberry (V. opulus var. opulus) is nearly identical to American highbush cranberry other than small glands (<1 mm) on the petiole making the exact determination very challenging resulting in common misidentifications. A major difference between the American and European highbush cranberries is that the European variety produces unpalatable fruit. Recent research has shown that American and European highbush cranberries are genetically distinct and that plants of hybrid origin are uncommon (Tork et al. 2025). Vigorous early spring growth and good tolerance to late spring frosts. Genetic analysis from Tork et al. 2025 confirmed that genetics of this accession represents American highbush Cranberry (Viburnum opulus var. americanum). This accession represents genetics from northeast Iowa and thus the extreme western edge of the species native range. | 1927436 | Ames 32966 |
| 137 | W6 48814 | MARSB-115 | Aristida purpurascens Poir. | New Jersey, United States | W6 |  | | 2015 | | | | | | | Wild material | | 1922907 | W6 48814 |
| 138 | W6 48819 | MARSB-101 | Boehmeria cylindrica (L.) Sw. | Maryland, United States | W6 |  | | 2015 | | | | | | | Wild material | | 1922836 | W6 48819 |
| 139 | W6 48822 | MARSB-46 | Carex atlantica L. H. Bailey | New Jersey, United States | W6 |  | | 2015 | | | | | | | Wild material | | 1922838 | W6 48822 |
| 140 | W6 48846 | MARSB-112 | Decodon verticillatus (L.) Elliott | New York, United States | W6 |  | | 2015 | | | | | | | Wild material | | 1922900 | W6 48846 |
| 141 | W6 48853 | MARSB-102 | Eragrostis spectabilis (Pursh) Steud. | Maryland, United States | W6 |  | | 2015 | | | | | | | Wild material | | 1922857 | W6 48853 |
| 142 | W6 48854 | MARSB-106 | Eragrostis spectabilis (Pursh) Steud. | New Jersey, United States | W6 |  | | 2015 | | | | | | | Wild material | | 1922916 | W6 48854 |
| 143 | W6 48902 | MARSB-114 | Tridens flavus (L.) Hitchc. | New Jersey, United States | W6 |  | | 2015 | | | | | | | Wild material | | 1922931 | W6 48902 |
| 144 | Ames 32784 | JDC/FP/2014/048/550 | Fraxinus pennsylvanica Marshall | Iowa, United States | NC7 |  | | 2014 | COLLECTED | 09/19/2014 | Along Prairie Street, near confluence of Iowa and Mississippi Rivers, SE 1/4 of NE 1/4 Section 2, T73N, R2W, Louisa County. | 41.15349500, -91.04686500 | 161 | Native wet, woods. | Wild material | | 1921795 | Ames 32784 |
| 145 | Ames 32798 | JDC/FP/2014/116/618 | Fraxinus pennsylvanica Marshall | Mississippi, United States | NC7 |  | | 2014 | COLLECTED | 09/27/2014 | Hushpuckena River/Sunflower Bend bottomlands, NW 1/4 of SW 1/4 of SE 1/4 of Section 30, T27N, R5W, Coahoma County. | 34.17974600, -90.75379300 | 55 | Wet woods. Extremely large, open grown specimens of green ash. | Wild material | | 1921809 | Ames 32798 |
| 146 | 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 |
| 147 | Ames 32388 | JDC/BN/2014/015/517 | Betula nigra L. | Iowa, United States | NC7 |  | | 2014 | COLLECTED | 06/05/2014 | Princeton Wildlife Management Area, T80N R5E NE 1/4 Sec. 35. | 41.69417800, -90.34158400 | 177 | Wet, heavy soil floodplain. | Wild material | | 1919309 | Ames 32388 |
| 148 | Ames 32390 | JDC/BN/2014/017/519 | Betula nigra L. | Iowa, United States | NC7 |  | | 2014 | COLLECTED | 06/06/2014 | Chariton River Watershed, T68N R17W NE 1/4 Sec. 3. | 40.72516900, -92.79660900 | 262 | Diverse areas of floodplain type habitats. | Wild material | | 1919311 | Ames 32390 |
| 149 | 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 |
| 150 | Ames 31522 | JDC/FQ/2012/031/424 | Fraxinus quadrangulata Michx. | Indiana, United States | NC7 |  | | 2012 | COLLECTED | 07/22/2012 | Turkey Run State Park, S 1/2 of Section 27, T17N, R7W, Wallace Quad, near Marshall, Vermillion County. | 39.88732800, -87.19895200 | 200 | Mature, moist woods. Rolling hills. | Wild material | | 1903749 | Ames 31522 |
| 151 | Ames 30882 | JDC/CI/2010/078/348 | Carya illinoinensis (Wangenh.) K. Koch | Iowa, United States | NC7 |  | | 2011 | COLLECTED | 10/04/2011 | Throughout Port Louisa National Wildlife Refuge, Toolesboro Quad., T74N R2W N 1/2 Sec. 8. | 41.22793000, -91.11041000 | 166 | Floodplain. | Wild material | Pecan is native to portions of the south-central Midwest (Carya illinoinensis Native Distribution from Elbert Little's "Atlas of United States Trees") stretching from Iowa along the Mississippi floodplain south to Texas and is well-known for high-quality fall color (yellow) and edible nuts. The species is relatively tolerant to alkaline and slightly acidic soils and can tolerate both extreme drought and severe flood events. However, well-drained soils are preferred. Genetics of this accession represent the extreme northern edge of the species native range with nuts typically reaching maturity in the last week of September into the first week of October in Iowa. Specimens at the collection site in nature measured ~25 inches DBH, with the largest specimen sampled measuring 40.5 inches DBH. Nut measurements (determined by averaging measurements (mm) from 5 randomly selected nuts off a single mother tree) were variable. Averaged measurements (length/width) recorded from 5 mother trees are as follows: tree #4: 23/15 mm, tree #5: 17/12 mm, tree #6: 26/16 mm, tree #7: 24/15 mm, and tree #8: 24/12 mm. Noted observations of progeny from the 2011 collection noted Tree#4 as having strong resistance to the black pecan aphid, Melanocallis caryaefoliae (Davis)(Hemiptera: Aphidadae). Recollection in 2024 found Tree#4 measuring 42.5" DBH dead as the result of major flooding events in 2013, 2014, and 2019 where floods in 2013 persisted for nearly three months. Flood stage for this population of pecan resides at 538 MSL (Mean Sea Level) which can be compared against data from the Mississippi River Lock and Dam 17 (Flood Events 2009-2024), where water levels were recorded 10-12' above ground level where multiple trees of Ames 30882 have been sampled. | 1865828 | Ames 30882 |
| 152 | W6 40685 | CP1-79 | Muhlenbergia tricholepis (Torr.) Columbus | Arizona, United States | W6 |  | | 2011 | | | | | | | Wild material | | 1865147 | W6 40685 |
| 153 | Ames 30389 | JDC/PV/2009/116/266 | Prunella vulgaris L. | Ohio, United States | NC7 |  | | 2009 | COLLECTED | 10/19/2009 | Erie Sand Barrens State Nature Preserve, Kimball Quad, Erie County. | 41.35861111, -82.70805556 | 209 | Sandy, dry soils. | Wild material | | 1823941 | Ames 30389 |
| 154 | Ames 30393 | JDC/RT/2009/115/265 | Rhus typhina L. | Ohio, United States | NC7 |  | | 2009 | COLLECTED | 10/19/2009 | Along West Oak Hickory Trail, 0.5 mile southeast of Driver and Smoky Road intersection, Edison Woods, Berlin Heights Quad, Erie County | 41.35138889, -82.47722222 | 205 | | Wild material | | 1823945 | Ames 30393 |
| 155 | Ames 29529 | JDC/FQ/2008/006/076 | Fraxinus quadrangulata Michx. | Illinois, United States | NC7 |  | | 2008 | COLLECTED | 08/01/2008 | Cottonhill Park (West), NE 1/4 of SE 1/4 of Section 3 and NW 1/4 of SW 1/4 of Section 2, T14N, R5W, near Springfield, Chatham Quad. | 39.69055556, -89.63000000 | 175 | Mature kept in park near lake. 25% slope with northern and northwestern exposure. | Wild material | 4-5 feet diameter breast height. | 1782752 | Ames 29529 |
| 156 | W6 15760 | MO31.CPG94 | Phalaris aquatica L. | Morocco | W6 | | | 1994 | COLLECTED | 07/13/1994 | Near Taza, 16 km. south of Taza near Ras-El-Oued on road S311. | 34.14500000, -4.01416667 | 1120 | Grazed. Slope 11-40%, aspect NE. Light open. Soil hillside loam on calcareous dolomite bedrock, pH 7.5-8.0. Moist, ravine, mid slope. Vegetation closed, seasonal tall grass. Surrounding veg. evergreen open forest with closed lower layers. | Wild material | Dominant tree species Quercus ilex. Dom. shrub sp. Calycotome villosa, Juniperus sp. Dom. herb/grass sp. perennial clovers, grasses, couch. Population distribution patchy, abundance occasional. Growth habit erect. | 1480221 | W6 15760 |
| 157 | W6 16119 | S014.CPG94 | Dactylis glomerata L. | Sardegna, Italy | W6 | | | 1994 | COLLECTED | 07/04/1994 | Near Chiaramonti, 3 k southeast of Chiaramonti on road SS132, Chiaramonte-Ozieri. | 40.72083333, 8.83083333 | 400 | Grazed. Slope 6-10%, aspect N. Open. Soil clay, pH 5-5.5. Rainfall 650 mm. Moist, basin. Vegetation closed, seasonal tall grass. Surrounding veg. dryland cereal/forage. Dominant tree Quercus suber. Dom. shrub Cistus sp. Dom. grass annuals. | Wild material | Population abundance frequent, distribution patchy. Growth habit erect. | 1480103 | W6 16119 |
| 158 | W6 16138 | S033.CPG94 | Phalaris aquatica L. | Sardegna, Italy | W6 | | | 1994 | COLLECTED | 07/05/1994 | Near Tempio, 11 k north on road S133 to Luogosanto. | 40.95277778, 9.09638889 | 315 | Grazed. Slope 0-5%, aspect E. Area open. Soil loam, pH 5.5. Rainfall 1000 mm. Moist, stream terrace, meadow. Vegetation closed, seasonal tall grass. Surrounding veg. evergreen open forest with closed lower layers, dryland pasture/forage. | Wild material | Population abundance rare, distribution patchy. Growth habit erect. | 1480122 | W6 16138 |