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ACCESSIONPLANT NAMETAXONOMYORIGINGENEBANKIMAGEAVAILABILITYRECEIVEDSOURCE TYPESOURCE DATECOLLECTION SITECOORDINATESELEVATIONHABITATIMPROVEMENT LEVELNARRATIVE
0NA 85963PCC15-SEUSA045Quercus arkansana Sarg. Alabama, United StatesNA2017COLLECTED10/30/2015Sumter County; ; Roadside, unincorporated area of Sumter County.32.56277000, -88.02721000Prairie woods, roadside.Seed from plant. Ground, vouchered. [Seed from plant and ground?] Ca five plants in area. No threats observed.2109095NA 85963
1W6 58576MARSB-240Pityopsis falcata (Pursh) Nutt. New York, United StatesW62021Wild materialYellow flowers, thin sickle-shaped leaves2113506W6 58576
2PI 702725NCBG-428Schizachyrium scoparium (Michx.) Nash Maryland, United StatesS9SEED2019Wild material2098447PI 702725
3PI 656838106Triadenum walteri (J. F. Gmel.) Gleason Arkansas, United StatesNC72004COLLECTED10/25/2004Trailside, seepy area next to lake, Village Creek State Park, Cross County.35.15298300, -90.71776600128Seepy area, lakeside, oak-hickory bottom land forest. 1-3 degrees of slope with a northeastern aspect. Loess soil. Wild material1 meter tall.1668211PI 656838
4PI 649051C-H148Hypericum gentianoides (L.) Britton et al. Florida, United StatesNC72004COLLECTED11/03/2000Adjacent to a pine plantation, south side of Highway 231, 5 miles south Alford, Washington County.30.62054300, -85.39622500Wild materialPlant about 1 meter tall.1659755PI 649051
5PI 604739D2Trifolium pratense L. Krasnodar, Russian FederationW61996COLLECTEDProvince Krasnodar, 5 km south of Il'skaya, southwest of Krasnodar.44.78333333, 38.56666667190Grazed, Slope 0-10%, aspect NE. Light open. Soil sand, loam, pH 4.6-5.3. Seasonally dry, upper slope. Vegetation closed, seasonal broad-leafed herb vegetation. Surrounding vegetation open deciduous forest with closed lower layers.Wild materialDominant tree species Quercus sp. Dominant shrub species Ribes sp., Prunus sp., Caprinus sp., Crataegus sp. Dominant herb/grass species Daucus carota, Potentilla sp., Festuca pratensis, Medicago falcata, Lotus c., Dorycnium intermedium, Dorycnium graceum. Extensive regional climate data available in spreadsheet format or image maps in raster format suitable for GIS analysis. Contact Dr. Stephanie L. Greene (sgreene@ars-grin.gov).1531080PI 604739
6PI 604754125Trifolium medium L. Russian FederationW61996COLLECTED08/21/1995Province Novorossiysk, 10 km north of Michaelovski-Perival.44.55833333, 38.36333333690Past logged, now grazed. Slope 0-5%, aspect NW. Light open. Soil clay, limestone/slate, shales, sandstones, pH 5.6-7.5. Seasonally dry, ridgetop, upper slope. Vegetation closed, evergreen broad-leafed herb vegetation.Wild materialSurrounding vegetation open deciduous forest with closed lower layers. Dominant tree species Quercus sp. Dominant shrub species Caprinus sp., Quercus sp., Ribes sp. Dominant herb/grass species Trifolium sp., Festuca pratensis, Poa sp., Potentilla sp., Medicago falcata, Onobrychis sp., Aster sp., Dactylis glomerata, Geranium sp. Population distribution patchy. Growth habit erect. Flower red-purple. Extensive regional climate data available in spreadsheet format or image maps in raster format suitable for GIS analysis. Contact Dr. Stephanie L. Greene (sgreene@ars-grin.gov).1530892PI 604754
7PI 611037VIR 129Dactylis glomerata L. Russian FederationW61996COLLECTED08/21/1995Province Novorossiysk, 10 km. north of Michaelovskiperival.44.55833333, 38.36333333700Past logged, now grazed. Slope 0-5%, aspect NW. Light open. Soil sandy-clay, pH 4.5-5.5. Seasonally dry, ridgetop, upper slope. Vegetation closed, evergreen broad-leafed. Surrounding veg. open deciduous forest with closed lower layers.Wild materialDominant tree species Quercus sp. Dominant shrub species Carpinus sp., Quercus sp., Ribes sp. Dominant herb/grass species Trifolium sp., Festuca pratensis, Poa sp., Potentilla sp., Medicago falcata, Onobrychis sp., Aster sp., Dactylis glomerata, Geranium sp. Population abundance frequent. Growth habit erect. Extensive regional climate data available in spreadsheet format or image maps in raster format suitable for GIS analysis. Contact Dr. Stephanie L. Greene (sgreene@ars-grin.gov).1517970PI 611037
8PI 631654044Medicago sativa L. subsp. falcata (L.) Arcang. Russian FederationW6FLOWER1996COLLECTED07/25/1995Province Maykop, 1 km northwest of Psauch'ye-Dakha.44.21666667, 41.85000000700Past logged, now grazed. Slope 11-40%, aspect SE. Light open. Soil clay with gravel, pH 7.4-8.0, some sand layer, mainly tertiary clays. Seasonally dry, upper slope, landslide slope. Vegetation closed evergreen broad-leafed herb vegetation.Wild materialSurrounding vegetation open deciduous forest with closed lower layers. Dominant tree species Quercus sp., Q. robur. Dominant shrub species Carpinus c., Q. petraea. Population distribution patchy, abundance frequent. Growth habit erect. Flower yellow. Extensive regional climate data available in spreadsheet format or image maps in raster format suitable for GIS analysis. Contact Dr. Stephanie L. Greene (sgreene@ars-grin.gov).1530834PI 631654
9PI 631660090Medicago sativa L. subsp. falcata (L.) Arcang. Krasnoyarsk, Russian FederationW61996COLLECTED08/17/1995Province Krymsk, between Krasnodar and Novorossiysk, west of Krymsk.44.91083333, 37.9625000070Past and current grazing. Slope 6-40%, aspect NE. Light open. Soil calcareous loams/sands, clay, pH 7.6-7.9. Seasonally dry, lower to mid slope, active slope movement. Vegetation closed, seasonal broad-leafed herb vegetation.Wild materialSurrounding vegetation open deciduous forest with closed lower layers. Dominant tree species Quercus robur, Quercus sp. Dominant shrub species Ribes sp. Dominant herb/grass species broadleaves, Trifoliums, Lotus corniculatus, Bermuda grass, Bothriochloa ischaemum, Senecio grandidentatus, Tussilago farfara, Coronilla varia, Xanthium strumarium, Daucus carota, Convolvulus arvensis, Achillea millefolium. Population distribution patchy, abundance occasional. Growth habit semi-erect. Flower yellow. Extensive regional climate data available in spreadsheet format or image maps in raster format suitable for GIS analysis. Contact Dr. Stephanie L. Greene (sgreene@ars-grin.gov).1530870PI 631660
10PI 631663128Medicago sativa L. subsp. falcata (L.) Arcang. Russian FederationW61996COLLECTED08/21/1995Province Novorossiysk, 10 km north of Michaelovski-Pervial.44.55833333, 38.36333333690Past logged, now grazed. Slope 0-5%, aspect NW. Light open. Soil clay, limestone/slate, shales, sandstones, pH 5.6-7.5. Seasonally dry, ridgetop, upper slope. Vegetation closed, evergreen broad-leafed herb vegetation.Wild materialSurrounding vegetation open deciduous forest with closed lower layers. Dominant tree species Quercus sp. Dominant shrub species Caprinus sp., Quercus sp., Ribes sp. Dominant herb/grass species Trifolium sp., Festuca pratensis, Poa sp., Potentilla sp., Medicago falcata, Onobrychis sp., Aster sp., Dactylis glomerata, Geranium sp. Population abundant. Growth habit erect. Flower yellow. Extensive regional climate data available in spreadsheet format or image maps in raster format suitable for GIS analysis. Contact Dr. Stephanie L. Greene (sgreene@ars-grin.gov).1530895PI 631663
11PI 631667241Medicago sativa L. subsp. falcata (L.) Arcang. Chelyabinsk, Russian FederationW61996COLLECTED09/05/1995Province Cherkessk-Karachayeysk Republic, 2 km east of Pregradnayc.43.91666667, 41.23305556850Past logged, now grazed, hayed. Slope 0-5%, aspect S. Light open. Soil loam, pH neutral. Moist to seasonally dry, stream terrace. Vegetation closed, evergreen broad-leafed herb vegetation.Wild materialSurrounding vegetation open deciduous forest with closed lower layers. Dominant tree species Fagus o., Quercus sp., Betula p. Dominant shrub species Laurocerasus officinalis, Ribes sp., Rosa sp. Dominant herb/grass species Achillea sp., Trifolium sp., Medicago sp., Geranium sp., Ambrosia sp., Daucus, Chicory, Dactylis g., Phleum p., Lolium p. Population distribution patchy, abundance frequent. Growth habit erect. Flower yellow. Extensive regional climate data available in spreadsheet format or image maps in raster format suitable for GIS analysis. Contact Dr. Stephanie L. Greene (sgreene@ars-grin.gov).1530971PI 631667
12PI 631668253Medicago sativa L. subsp. falcata (L.) Arcang. Karelia, Russian FederationW61996COLLECTED09/06/1995Province Karachayevo-Cherkesskaya Republic, 1 km northwest of Ordzhanikedevskiy.43.85833333, 41.90194444790Past and current grazing. Lower slope 6-10%, upper slope 41-60%, aspect SE. Light open. Soil sandy loam, sandstone rock outcrop, pH upper 5.8, lower 6.3-6.4. Seasonally dry, lower slope, rock outcrop. Vegetation closed, seasonal tall grass.Wild materialSurrounding vegetation open deciduous forest with closed lower layers. Dominant tree species Beech, Oak, Fagus o., Quercus sp. Dominant shrub species Artemisia sp., Rosa sp. Dominant herb/grass species Achillea sp., Medicago sp., Bothriochloa i., Festuca v. Population distribution uniform, abundant. Growth habit erect. Flower yellow. Extensive regional climate data available in spreadsheet format or image maps in raster format suitable for GIS analysis. Contact Dr. Stephanie L. Greene (sgreene@ars-grin.gov).1530980PI 631668
13PI 634036124Trifolium hybridum L. Russian FederationW61996COLLECTED08/21/1995Province Novorossiysk, 10 km north of Michaelovski-Perival.44.55833333, 38.36333333690Past logged, now grazed. Slope 0-5%, aspect NW. Light open. Soil clay, limestone/slate, some shales, sandstones, pH 5.6-7.5. Seasonally dry, ridgetop, upper slope. Vegetation closed, evergreen broad-leafed herb vegetation.Wild materialSurrounding vegetation open deciduous forest with closed lower layers. Dominant tree species Quercus sp. Dominant shrub species Caprinus sp., Quercus sp., Ribes sp. Dominant herb/grass species Trifolium sp., Festuca pratensis, Poa sp., Potentilla sp., Medicago falcata, Onobrychis sp., Aster sp., Dactylis glomerata, geranium sp. Population abundance frequent. Growth habit erect. Flower rose. Extensive regional climate data available in spreadsheet format or image maps in raster format suitable for GIS analysis. Contact Dr. Stephanie L. Greene (sgreene@ars-grin.gov).1530891PI 634036
14PI 641447126Lotus corniculatus L. Russian FederationW6SEED1996COLLECTED08/21/1995Province Novorossiysk, 10 km north of Michaelovski-Perival.44.55833333, 38.36333333690Past logged, now grazed. Slope 0-5%, aspect NW. Light open. Soil clay, limestone/slate, shales, sandstones, pH 5.6-7.5. Seasonally dry, ridgetop, upper slope. Vegetation closed, evergeen broad-leafed herb vegetation.Wild materialSurrounding vegetation open deciduous forest with closed lower layers. Dominant tree species Quercus sp. Dominant shrub species Caprinus sp., Quercus sp., Ribes sp. Dominant herb/grass species Trifolium sp., Festuca pratensis, Poa sp., Potentilla sp., Mdicago falcata, Onobrychis sp., Aster sp., Dactylis glomerata, Geranium sp. Population abundant. Growth habit semi-erect. Flower yellow. Extensive regional climate data available in spreadsheet format or image maps in raster format suitable for GIS analysis. Contact Dr. Stephanie L. Greene (sgreene@ars-grin.gov).1530893PI 641447
15PI 641463223Medicago sativa L. subsp. falcata (L.) Arcang. Russian FederationW61996COLLECTED09/04/1995Province Maykop/Labinsk, 5 km south of Vladimirskaya.44.48027778, 40.81472222360Past and current grazing, cut hay. Slope 11-40%, aspect SW. Light open. Soil clay, pH basic-7.7. Moist, lower slope. Unstable site. Vegetation closed, seasonal tall grass. Surrounding veg. open deciduous forest with closed lower layers.Wild materialDominant tree species Crataegus sp., Quercus sp., Hornbeam-Oak. Dominant shrub species Sambucus sp., Rosa sp., Prunus sp. Dominant herb/grass species Achillea sp., Daucus c., Medicago f., Bothriochloa i., Erytregia sp. Population distribution uniform, abundant. Growth habit erect. Flower yellow. Extensive regional climate data available in spreadsheet format or image maps in raster format suitable for GIS analysis. Contact Dr. Stephanie L. Greene (sgreene@ars-grin.gov).1530963PI 641463
16PI 641727D3Trifolium striatum L. Krasnodar, Russian FederationS91996COLLECTEDProvince Krasnodar, 5 km south of Il'skaya, southwest of Krasnodar.44.78333333, 38.56666667190Grazed. Slope 0-10%, aspect NE. Light open. Soil sand, loam, pH 4.6-5.3. Seasonally dry, upper slope. Vegetation closed, seasonal broad-leafed herb vegetation. Surrounding vegetation open deciduous forest with closed lower layers.Wild materialDominant tree species Quercus sp. Dominant shrub species Ribes sp., Prunus sp., Caprinus sp., Crataegus sp. Dominant herb/grass species Daucus carota, Potentilla sp., Festuca pratensis, Medicago falcata, Lotus c., Dorycnium intermedium, Dorycnium graceum. Extensive regional climate data available in spreadsheet format or image maps in raster format suitable for GIS analysis. Contact Dr. Stephanie L. Greene (sgreene@ars-grin.gov).1531085PI 641727
17PI 655805001Trifolium repens L. Krasnodar, Russian FederationW6SEED1996COLLECTED08/07/1995South of Il'skaya (Azovskaya), 5 km southwest of Krasnodar.44.78333333, 38.56666667190Past and current grazing.Slope 1-10%, aspect NE.Open light.Sandy loam, pH 4.6-5.3. Seasonally dry, upper slope.Vegetation closed, seasonal broad-leafed herb.Surrounding veg.open deciduous forest with closed lower layers, agri. disturbance.Wild materialDominant tree species Quercus sp. Dominant shrub species Ribes sp., Prunus sp., Caprinus sp., Crataegus sp. Dominant herb/grass species Daucus carota, Potentilla sp., Festuca pratensis, Medicago falcata, Lotus cauc., Dorycnium intermedium, Dorycnium graceum. Population distibution patchy, abundance frequent. Growth habit prostrate. Flower white. Extensive regional climate data available in spreadsheet format or image maps in raster format suitable for GIS analysis. Contact Dr. Stephanie L. Greene (sgreene@ars-grin.gov).1530806PI 655805
18NA 891712025RJLSEUS-04Rhododendron catawbiense Michx. Alabama, United StatesNA2026COLLECTED09/30/2025Scarham Creek: southeast of the Pea Ridge Road bridge, approximately 50-80 meters on the south side of the creek.34.32559600, -86.16054600266Growing near the base of the slopes above the riparian zone, generally on the exposed geology under very well-drained conditions. The woodlands are primarily deciduous with a few evergreens infrequently mixed. Slope: 15 to 30 percent. Aspect: Northeast. Soil: The primary soil type in the area of this collection is classified as Rockland Series sandstone (Rc). The Rockland series consists of well drained soils formed in loamy colluvium from rotational landslides on slopes of stream valleys and dissections of ground moraines. Saturated hydraulic conductivity is moderate in the upper part of the profile and moderately slow in the lower part. Slopes range from 18 to 70 percent. Some pedons have buried leaves, twigs, and moss. Mass soil movement has left random remnants of soil structure from prior upslope soil development and has buried tree branches, leaves and moss. The upper 0-2 cm of soil contains slightly decomposed organic matter while lower soils layers to a depth of 58 cm are comprised of dark reddish-brown to brown silt loam and are moderately acidic. Below 58 cm the soils are generally dark reddish-brown silt loam and strongly to moderately alkaline. (Source:California Soil Resource Lab/NRCS Official Soil Series Descriptions). Geology: The underlying geology of this area is of Pennsylvanian origin and characterized as Pottsville Formation. It is characterized by light-gray thin to thick-bedded quartzose sandstone and conglomerate containing interbedded dark-gray shale, siltstone, and coal. Mapped on Lookout Mountain, Blount and Chandler Mountains, and Sand Mountain northeast of Blount County, and on the mountains of Jackson, Marshall, and Madison Counties north and west of the TN river. (Source: USGS Alabama Geologic Map Data).Wild materialReceived as R. catawbiense vsr. insularis2193305NA 89171
19NA 891552025RJLSEUS-02Ilex longipes Chapm. ex Trel. Alabama, United StatesNA2025COLLECTED09/30/2025Scarham Creek: southeast of the Pea Ridge Road bridge, approximately 50-80 meters on the south side of the creek.34.32520700, -86.15967000261Plants are growing on relatively steep woodland slopes in shade. The woodlands are primarily deciduous with a few evergreens infrequently mixed. Slope: 15 to 30 percent. Aspect: Northeast. Soil: The primary soil type in the area of this collection is classified as Rockland Series sandstone (Rc). The Rockland series consists of well drained soils formed in loamy colluvium from rotational landslides on slopes of stream valleys and dissections of ground moraines. Saturated hydraulic conductivity is moderate in the upper part of the profile and moderately slow in the lower part. Slopes range from 18 to 70 percent. Some pedons have buried leaves, twigs, and moss. Mass soil movement has left random remnants of soil structure from prior upslope soil development and has buried tree branches, leaves and moss. The upper 0-2 cm of soil contains slightly decomposed organic matter while lower soils layers to a depth of 58 cm are comprised of dark reddish-brown to brown silt loam and are moderately acidic. Below 58 cm the soils are generally dark reddish-brown silt loam and strongly to moderately alkaline. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). Geology: The underlying geology of this area is of Pennsylvanian origin and characterized as Pottsville Formation. It is characterized by light-gray thin to thick-bedded quartzose sandstone and conglomerate containing interbedded dark-gray shale, siltstone, and coal. Mapped on Lookout Mountain, Blount and Chandler Mountains, and Sand Mountain northeast of Blount County, and on the mountains of Jackson, Marshall, and Madison Counties north and west of the TN river. (Source: USGS Alabama Geologic Map Data).Wild material2193001NA 89155
20NA 891562025RJLSEUS-03Euonymus americanus L. Alabama, United StatesNA2025COLLECTED09/30/2025Scarham Creek: southeast of the Pea Ridge Road bridge, approximately 50-80 meters on the south side of the creek.34.32577600, -86.16071000260Plants are growing on relatively steep woodland slopes in shade. The woodlands are primarily deciduous with a few evergreens infrequently mixed. Slope: 15 to 30 percent. Aspect: Northeast. Soil: The primary soil type in the area of this collection is classified as Rockland Series sandstone (Rc). The Rockland series consists of well drained soils formed in loamy colluvium from rotational landslides on slopes of stream valleys and dissections of ground moraines. Saturated hydraulic conductivity is moderate in the upper part of the profile and moderately slow in the lower part. Slopes range from 18 to 70 percent. Some pedons have buried leaves, twigs, and moss. Mass soil movement has left random remnants of soil structure from prior upslope soil development and has buried tree branches, leaves and moss. The upper 0-2 cm of soil contains slightly decomposed organic matter while lower soils layers to a depth of 58 cm are comprised of dark reddish-brown to brown silt loam and are moderately acidic. Below 58 cm the soils are generally dark reddish-brown silt loam and strongly to moderately alkaline. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). Geology: The underlying geology of this area is of Pennsylvanian origin and characterized as Pottsville Formation. It is characterized by light-gray thin to thick-bedded quartzose sandstone and conglomerate containing interbedded dark-gray shale, siltstone, and coal. Mapped on Lookout Mountain, Blount and Chandler Mountains, and Sand Mountain northeast of Blount County, and on the mountains of Jackson, Marshall, and Madison Counties north and west of the TN river. (Source: USGS Alabama Geologic Map Data).Wild material2193002NA 89156
21NA 89115TLM25-04aHamamelis ovalis S. W. Leonard Texas, United StatesNA2025COLLECTED07/10/2025State Highway 87 approximately 3.25 kilometers north of the crossroad junction with Texas Recreational Road 255 (RE 255); plants were growing in the narrow buffer woods along the east side of the highway.31.12051300, -93.72628100138The habitat is an upland mixed coniferous and deciduous woodlands in part to full shade and dry conditions, often under drought stress. Plants seem to always occur on the top of dry ridges or well-drained slopes. Slope: 0 to 1 percent. Aspect: N/A. Soils: The soils of this collection area are classified as Tehran-Letney Association, hilly (TLE) soils. The Tehran Series (55%) consists of deep, somewhat excessively drained, moderately rapidly permeable soils on uplands. They formed in thick loamy and sandy sediments on the Western Coastal Plain. These soils are on gently sloping to moderately steep uplands with slopes ranging from 1 to 20 percent. The Letney Series (30%) consists of deep, well drained, moderately rapidly permeable, upland soils. They formed in thick sandy and loamy sediments of the coastal plains. These soils are on gently sloping to moderately steep uplands with slopes ranging from 1 to 20 percent. Soil pH ranges from 4.5 to 6.0. The minor soil components include Doucette Series (10%) and Boykin Series (5%) soils. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). Geology: The underlying geology of this area is of Oligocene origin and characterized as Catahoula Formation. This formation is extensive and deep in Texas, up to 185 meters thick. In the area of the collection the Catahoula Formation is primarily mudstone and sand. The upper 90-150 meters is mudstone that is tuffaceous, and sandy; also, occasionally, with some bentonitic clay. (Source: USGS Texas Geologic Map Data).Wild material2191654NA 89115
22NA 8892924Flam8Rhododendron hybr.Georgia, United StatesNA2025COLLECTED09/09/2024Smyrna, GA: private residence.33.84871000, -84.51773000303Dry slope in backyard of residence, primarily open with some large oaks. Open conditions. Slope: 30 degrees. Aspect: Northwest.Wild material2172812NA 88929
23NA 8893024Flam16Rhododendron canescens (Michx.) Sweet Georgia, United StatesNA2025COLLECTED09/10/2024DeKalb County: Stone Mountain: Stone Mountain Park: slope near Robert E. Lee Boulevard.33.80238000, -84.15508000286Dry, shady slope. Growing in 3/4 shade. Slope: 30 to 45 degrees. Aspect: West-southwest.Wild materialNote: Seeds from three different plants collected at the same spot were bulked together in this accession; the lowest field collection number (24Flam16) has been chosen as the primary for this record. It appears from the notes that the identity is slightly uncertain; possibly not pure R. canescens.2172813NA 88930
24NA 88747TXWL2025-038Ilex opaca Aiton Texas, United StatesNA2025COLLECTED01/23/2025Milam, Texas: On flat road, private land.31.43288000, -93.88208000Upland shortleaf pine stand with sandy loam; closed canopy.Wild material2171021NA 88747
25NA 88982TXWL2025-032Ilex opaca Aiton Texas, United StatesNA2025COLLECTED01/07/2025South of Jericho community.31.66973000, -94.25613000Western sandy lands; edge of small grove of Ilex opaca with sun exposure in upland position above a baygall. Bare ground cover with Ilex opaca regeneration. Adjacent to a new longleaf pine plantation located on fireline.Wild material2170966NA 88982
26NA 88983TXWL2025-033Ilex opaca Aiton Texas, United StatesNA2025COLLECTED01/12/2025Adjacent to Toledo Bend reservoir in Huxley Bay community, eastern Shelby County.31.77133000, -93.85094000Low area with heavy duff near reservoir.Wild material2170967NA 88983
27NA 885802024RJLFL-009Ilex myrtifolia Walter Florida, United StatesNA2024COLLECTED11/13/2024Woodlands on the north side of Fisher Old Mill Road about 0.10 kilometers west of intersection with DOF Y12.30.62693800, -86.839622006Mixed 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 material2169917NA 88580
28NA 885842024RJLFL-016Cornus florida L. Florida, United StatesNA2024COLLECTED11/14/2024Both sides of Kennedy Bridge Road approximately 0.27 kilometers west of the junction with Hurricane Lake South Entrance Road.30.93159700, -86.7492800043Mesic 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 material2169921NA 88584
29NA 885862024RJLFL-020Vaccinium arboreum Marshall Florida, United StatesNA2024COLLECTED11/14/2024Woodland edge off of Ralf Laurant Road, above the wetland/headwaters of Danley Branch along the edge of a young longleaf pine plantation.30.90104300, -86.7887810061Edge 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 material2169923NA 88586
30NA 890892024RM-TK-002Viburnum acerifolium L. Alabama, United StatesNA2024COLLECTED09/19/2024Woodland slopes around and below the hilltop parking area leading down to the Silver Creek Lake Campground off of Silver Creek Lake Road.31.66612294, -87.5756986049Plants are growing in shade of upland dry mesic, mature mixed deciduous and evergreen woodland. Generally, the overstory is thinner and there is less leaf litter cover, making the surface soil conditions drier. Slope: 5 to 10 percent. Aspect: Southeast. Geology: The underlying geology of this area is Claiborne Group, Tallahatta Formation, of Eocene origin, with white to very light-greenish-gray thin-bedded to massive siliceous claystone; interbedded with thin layers of fossiliferous clay, sandy clay, and glauconitic sand and sandstone. (Source: USGS Alabama Geologic Map Data). Soils: The primary soil types in the collection area are classified as Arundel-Cantuche Complex soils (15 to 35 percent slopes). The Arundel Series consists of moderately deep, well drained, very slowly permeable soils on dissected uplands of the Southern Coastal Plain. They formed in marine deposits consisting of acid clays underlain by horizontally bedded sandstone, buhrstone and siltstone. These soils are strongly acid. Slopes range from 2 to 60 percent. The Cantuche Series consists of shallow, well drained, moderately permeable soils that formed over horizontally bedded claystone. These soils are on narrow ridgetops and narrow benches on steep side-slopes of dissected landscapes in the Coastal Plain. They are strongly acid. Slopes range from 2 to 35 percent. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). EPA Ecoregion (Level III): Southeastern Plains (65). EPA Ecoregion (Level IV): Buhrstone/Lime Hills (65q).Wild material2169053NA 89089
31NA 88844RJL-RM2023FLAL-018Clethra alnifolia L. Florida, United StatesNA2023COLLECTED12/13/2023Yellow 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, -86.6200540027Plants 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 material2165674NA 88844
32WLP 3377TXWL2023-024Viburnum dentatum L. Texas, United StatesNA2023COLLECTED12/13/2023Roadside between Big Cow Creek and Hardy Cemetery.31.03548900, -93.85086800Roadside; mesic, mixed hardwood/pine forest.Wild material2165656WLP 3377
33NA 88812TXWL2023-018Ilex ambigua Torr. Texas, United StatesNA2023COLLECTED12/05/2023Davy Crockett National Forest: Forest Service Road 526 roadside.31.49017400, -95.22343300Roadside. Shortleaf mixed upland hardwood forest; dry-mesic.Wild material2165615NA 88812
34NA 88814TXWL2023-021Ilex ambigua Torr. Texas, United StatesNA2023COLLECTED12/09/2023Roadside between Big Cow Creek and Hardy Cemetery.31.03548900, -93.85086800Roadside; mesic, mixed hardwood/pine forest.Wild material2165618NA 88814
35NA 88689RJL2023NJ-002Kalmia latifolia L. New Jersey, United StatesNA2023COLLECTED11/10/2023Franklin Township: Piney Hollow Preservation Area (the site is owned by Franklin Township). Plants accessed by foot along trails throughout property.39.57400900, -74.9360240032Plants growing in shade to part-shade of a mesic to mesic-dry woodland habitat that is mostly deciduous, but also includes pine overstory. Slope: N/A. Aspect: N/A. Soils: The underlying geology of this area is of Middle Miocene, Serravallian origin and characterized as an Cohansey Formation. It is comprised of sand, white to yellow with local gravel and clay. Locally stained red or orange brown by iron oxides and (or) cemented into large blocks of ironstone. Unweathered clay is typically dark gray, but commonly weathers white where interbedded with thin beds of ironstone. Unit is a complex of interfingering marine and nonmarine facies. Sand is typically medium grained and moderately sorted although it ranges from fine to very coarse grained and from poorly to well sorted. Sand consists of quartz and siliceous rock fragments. Some beds are locally micaceous. In general, the sand is crossbedded, although the style of crossbedding varies significantly with the paleoenvironment. Trough crossbedding predominates, especially in the nonmarine channel fill deposits, and the scale of the crossbeds varies from small to large. Maximum thickness in the map area is about 60 m; however, thickness is difficult to determine because of the irregular basal contact and extensive post-depositional erosion. There is as much as 18 m of relief along the basal contact. The basal contact is sharp, undulatory, and directly overlain by a thin gravel bed. The Cohansey Formation unconformably overlies the Kirkwood Formation and is found in channels cut down into the Kirkwood. Where the Kirkwood consists of sandy, light-colored sediments, the basal contact of the Cohansey is drawn below crossbedded sediments. Where the Kirkwood consists of dark-colored silty beds, the basal contact is drawn between light-colored Cohansey sediments and the underlying dark-colored sediments. The Cohansey was markedly thinned because of erosion prior to deposition of overlying units in the western and southern parts of the southern sheet. The unit has been extensively eroded and stripped from large areas of the New Jersey Coastal Plain, particularly in the central sheet where outliers are common. In spite of its widespread nature, the Cohansey is poorly exposed because of its loose sandy composition, which causes it to erode easily. (Source: USGS New Jersey Geologic Map Data.) The primary soil type in the location of this collection is classified as Downer loamy sand, 0 to 5 percent slopes, Northern Coastal Plain. Downer Series soils are very deep, well-drained soils that are coarse-loamy, siliceous, semiactive, mesic Typic Hapludults. The upper strata of Downer Series from 0 to 25 cm is dark grayish brown, brown loamy sand that is dry with weak fine granular structure. It is very friable and strongly acid. Lower strata from 25 to 76 cm are yellowish brown single grain, loose loamy sand with few extremely weakly cemented masses of oxidized iron in the lower part. This layer is very strongly acid. (Source: NRCS Web Soil Survey.)Wild material2159117NA 88689
36NA 88693RJL2023NJ-006Clethra alnifolia L. New Jersey, United StatesNA2023COLLECTED11/10/2023Franklin Township: Piney Hollow Preservation Area (the site is owned by Franklin Township). Plants accessed by foot along trails throughout property.39.57319800, -74.9290890029Plants growing in shade to part-shade over a wide range of habitats from mesic to mesic-dry as well as moist to wetland habitats. The woodlands are mostly deciduous, but also include occasional pine overstory. Slope: N/A. Aspect: N/A. The underlying geology of this area is of Middle Miocene, Serravallian origin and characterized as an Cohansey Formation. It is comprised of sand, white to yellow with local gravel and clay. Locally stained red or orange brown by iron oxides and (or) cemented into large blocks of ironstone. Unweathered clay is typically dark gray, but commonly weathers white where interbedded with thin beds of ironstone. Unit is a complex of interfingering marine and nonmarine facies. Sand is typically medium grained and moderately sorted although it ranges from fine to very coarse grained and from poorly to well sorted. Sand consists of quartz and siliceous rock fragments. Some beds are locally micaceous. In general, the sand is crossbedded, although the style of crossbedding varies significantly with the paleoenvironment. Trough crossbedding predominates, especially in the nonmarine channel fill deposits, and the scale of the crossbeds varies from small to large. Maximum thickness in the map area is about 60 m; however, thickness is difficult to determine because of the irregular basal contact and extensive post-depositional erosion. There is as much as 18 m of relief along the basal contact. The basal contact is sharp, undulatory, and directly overlain by a thin gravel bed. The Cohansey Formation unconformably overlies the Kirkwood Formation and is found in channels cut down into the Kirkwood. Where the Kirkwood consists of sandy, light-colored sediments, the basal contact of the Cohansey is drawn below crossbedded sediments. Where the Kirkwood consists of dark-colored silty beds, the basal contact is drawn between light-colored Cohansey sediments and the underlying dark-colored sediments. The Cohansey was markedly thinned because of erosion prior to deposition of overlying units in the western and southern parts of the southern sheet. The unit has been extensively eroded and stripped from large areas of the New Jersey Coastal Plain, particularly in the central sheet where outliers are common. In spite of its widespread nature, the Cohansey is poorly exposed because of its loose sandy composition, which causes it to erode easily. (Source: USGS New Jersey Geologic Map Data.) The primary soil types in the area of this collection is classified as Atsion sand, 0 to 2 percent slopes, Northern Tidewater Area and Downer loamy sand, 0 to 5 percent slopes, Northern Coastal Plain. Atsion Series soils are very deep, poorly drained with moderate to rapid permeability above 70 cm and slower beneath. They are classified as sandy, siliceous, mesic Aeric Alaquods. The upper stratum from 0 to 25 cm is dark gray sand, dry, single grained and lose with many fine roots. It is extremely acid. Lower strata are light gray to dark brown with small percentages of rounded quartzose pebbles and are extremely acid. Downer Series soils are very deep, well-drained soils that are coarse-loamy, siliceous, semiactive, mesic Typic Hapludults. The upper stratum of Downer Series from 0 to 25 cm is dark grayish brown, brown loamy sand that is dry with weak fine granular structure. It is very friable and strongly acid. Lower strata from 25 to 76 cm are yellowish brown single grain, loose loamy sand with few extremely weakly cemented masses of oxidized iron in the lower part. This layer is very strongly acid. (Source: NRCS Web Soil Survey.)Wild material2159121NA 88693
37NA 88709RJL2023NCSC-014Rhododendron minus Michx. South Carolina, United StatesNA2023COLLECTED11/13/2023Northwest side of the junction of Wire Road and Prichard Horse Road.34.49925200, -80.27470600146Plants 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 material2159137NA 88709
38NA 88719RJL2023NCSC-024Ilex laevigata (Pursh) A. Gray South Carolina, United StatesNA2023COLLECTED11/15/2023Little Pee Dee Heritage Preserve/Wildlife Management Area (South Carolina Department of Natural Resources Public Lands, on South Carolina Highway 917).34.14123300, -79.1953210013Plants 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 material2159147NA 88719
39NA 88720RJL2023NCSC-025Zenobia pulverulenta (W. Bartram ex Willd.) Pollard South Carolina, United StatesNA2023COLLECTED11/15/2023Little Pee Dee Heritage Preserve/Wildlife Management Area (South Carolina Department of Natural Resources Public Lands, on South Carolina Highway 917).34.13990000, -79.1969170014Plants 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 material2159148NA 88720
40NA 88721RJL2023NCSC-026Ilex opaca Aiton South Carolina, United StatesNA2023COLLECTED11/15/2023Little Pee Dee Heritage Preserve/Wildlife Management Area (South Carolina Department of Natural Resources Public Lands, on South Carolina Highway 917).34.14091500, -79.1955520013Plants 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 material2159149NA 88721
41NA 88668TXWL2023-011Amorpha paniculata Torr. & A. Gray Texas, United StatesNA2023COLLECTED10/02/2023Angelina National Forest: Forest Service Road 302A roadside [Note: GPS coordinates are west of FS Road 302A, closer to County Road 348B.]31.09190000, -94.29072400Roadside.Wild material2159043NA 88668
42NA 88670TXWL2023-013Maclura pomifera (Raf.) C. K. Schneid. Texas, United StatesNA2023COLLECTED2023Caddo National Grasslands: C-6 near Telephone, Texas [Note: C-6 may refer to Hunter Camp 6 along FM (Farm to Market Road) 409 north of Coffee Mill Lake.]Wild material2159045NA 88670
43NA 88662TJK2023FL-016Sideroxylon sp.Florida, United StatesNA2023COLLECTED09/16/2023East River Unit, Eglin Air Force Base. Near A-21 Rd.30.41250000, -86.771100007Xeric shrub, xeric sandhills community. Elevation: 26 feet. Slope: 2%. Aspect: South.Wild material2158796NA 88662
44WLP 3136TJK2023FL-010 Morella cerifera (L.) Small Florida, United StatesNA2023COLLECTED08/18/2023Blackwater State Forest: Wolfe Creek.30.80751000, -86.9577400052Beautiful 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 materialReceived as Morella pumila (Morella cerifera var. pumila). Treated tentatively as Morella cerifera Pumila Group. WLPGR contract collection.2158468WLP 3136
45NA 89264TJK2023FL-002Gaylussacia frondosa (L.) Torr. & A. Gray var. nana A. Gray Florida, United StatesNA2023COLLECTED05/19/2023Blackwater State Forest: Wolfe Creek.30.80760000, -86.9625000049Beautiful 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 materialWLPGR contract collection. Received as Gaylussacia tomentosa (nana).2158247NA 89264
46NA 89265TJK2023FL-003Ceanothus sp.Florida, United StatesNA2023COLLECTED05/19/2023Blackwater State Forest: Wolfe Creek.30.80650000, -86.9584000049Beautiful 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 materialWLPGR contract collection. Received as Ceanothus microphyllus.2158248NA 89265
47NA 89266TJK2023FL-004Gaylussacia dumosa (Andrews) Torr. & A. Gray Florida, United StatesNA2023COLLECTED05/31/2023Blackwater State Forest: Wolfe Creek.30.80560000, -86.9589000049Beautiful xeric pine-oak upland community. Transitions to mesic slopes and then to seepage bottom, stringer wetland community adjacent to the Wolfe Creek. Slope: 15%. Aspect: Northwest. Elevation recorded as 160 feet.Wild materialWLPGR contract collection.2158249NA 89266
48NA 89267TJK2023FL-005Ceanothus americanus L. Florida, United StatesNA2023COLLECTED06/10/2023Blackwater State Forest: Wolfe Creek.30.80760000, -86.9625000049Beautiful 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 materialWLPGR contract collection.2158250NA 89267
49NA 89269TJK2023FL-007Vaccinium darrowii Camp Florida, United StatesNA2023COLLECTED06/10/2023Blackwater State Forest: Wolfe Creek.30.80560000, -86.9577000060Beautiful 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 materialWLPGR contract collection.2158252NA 89269
50WLP 3092RJLSEUS2022-021Rhododendron prunifolium (Small) Millais Alabama, United StatesNA2023COLLECTED12/10/2023Slopes along Poke Springs Branch inlet accessed by boat from Walter F. George Reservoir. Generally uncommon, but frequent at this site. 31.72318400, -85.1290780069Plants 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 material2141446WLP 3092
51NA 87350TJK2022FL-005Ilex ambigua Torr. Florida, United StatesNA2023COLLECTED11/02/2022Okaloosa County: Eglin Air Force Base: East River Unit H-3, Range Road 259, north of Highway 98.30.41190000, -86.773200000Xeric Scrub/Upland Sandhill community.Wild material2141641NA 87350
52NA 88540RJLSEUS2022-012Rhododendron austrinum (Small) Rehder Georgia, United StatesNA2023COLLECTED12/09/2022Plants growing along the edge of a moist woodland habitat on the property at the end of the Lavender Lane cul-de-sac adjoining that of Monica Williams, in Albany, Georgia. Infrequent on the woodland edge at this site.31.63812300, -84.1406650064Plants are growing in part-shade of a moist mesic, mostly deciduous, woodland along the upper fringes of seasonally moist to wet drainage area leading to a large pond and wetland habitat further downstream.
Soils: The underlying geology of this area is of Eocene origin and characterized as Ocala Limestone. The Ocala Limestone consists of almost pure limestones with occasional dolomites. It can be subdivided into both lower and upper facies with the lower facies composed of a whitish to cream-colored, fine to medium grained, poorly to moderately hard, fossil rich grainstone and packstone. The upper Ocala is white and somewhat weak and poorly sorted. It is extremely fossil rich grainstone, packstone and wackestone and some chert is common in the upper facies.
Source: USGS Georgia Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=GANu%3B1)
The primary soil types in the collection area are classified as Herod and Muckalee Series soils. The Herod Series consists of poorly drained moderately permeable soils formed in loamy alluvium. These soils are on flood plains of streams in the Coastal Plain. Slopes range from 0 to 2 percent. The Muckalee Series consists of poorly drained moderately permeable soils formed in loamy and sandy alluvium. These soils are on flood plains of streams in the Coastal Plain. Slopes range from 0 to 2 percent.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2140767NA 88540
53NA 88554RJLSEUS2022-027Rhododendron alabamense Rehder Alabama, United StatesNA2023COLLECTED12/12/2022Plants growing on woodland slopes around and below the hilltop parking area leading down to the Silver Creek Lake Campground off of Silver Creek Lake Road. Occasional in the upland woodlands. 31.66613100, -87.5762570049Plants are growing in shade of upland dry mesic mature mixed deciduous and evergreen woodland. Generally, the overstory is thinner and there is less leaf litter cover, making the surface soil conditions drier.
Soils: The underlying geology of this area is Claiborne Group, Tallahatta Formation, of Eocene origin, with white to very light-greenish-gray thin-bedded to massive siliceous claystone; interbedded with thin layers of fossiliferous clay, sandy clay, and glauconitic sand and sandstone.
Source: USGS Alabama Geological Map Data (https://mrdata.usgs.gov/geology/state/state.php?state=AL)
The primary soil types in the collection area are classified as Smithdale-Boykin Complex soils (2 to 5 percent slopes). The Smithdale Series consists of very deep, well drained, moderately permeable soils on ridge tops and hill slopes in dissected uplands of the Southern Coastal Plain and in the Western Coastal Plain. They formed in thick beds of loamy marine sediments and are strongly acid. Slopes range from 1 to 60 percent. The Boykin Series consists of deep, well drained, moderately permeable soils that formed in sandy and loamy coastal plain sediments of Pleistocene age. These soils are on gently sloping to moderately steep uplands. Slopes range from 1 to 20 percent.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2140781NA 88554
54NA 88558RJLSEUS2022-031Ilex decidua Walter Alabama, United StatesNA2023COLLECTED12/12/2022Silver Creek Lake Campground off of Silver Creek Lake Road: Silver Creek Lake, at the edge of the campground.31.66344600, -87.5710840016Part shade to sun along the eroding banks of Silver Creek Lake in moist-mesic, mixed deciduous and evergreen woodland, 2-3 meters above the water. The underlying geology of this area is Claiborne Group, Tallahatta Formation, of Eocene origin, with white to very light-greenish-gray thin-bedded to massive siliceous claystone; interbedded with thin layers of fossiliferous clay, sandy clay, and glauconitic sand and sandstone. (Source: USGS Alabama Geological Map Data). The primary soil types in the collection area are classified as Riverview Fine Sandy Loam soils (0 to 2 percent slopes, occasionally flooded). The Riverview Series consists of very deep, well drained, moderately permeable soils that formed in loamy alluvium on flood plains. Slopes range from 0 to 5 percent. Riverview soils fare on high parts of flood plains of rivers and streams draining the Coastal Plain and Southern Piedmont. Runoff is slow. Permeability is moderate. These soils flood for short periods mostly in winter or early spring months. (Source: NRCS Web Soil Survey).Wild material2140819NA 88558
55NA 88562RJLSEUS2022-035Kalmia latifolia L. Alabama, United StatesNA2023COLLECTED12/12/2022Plants 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, -87.35821100132Plants 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 material2140787NA 88562
56NA 88565RJLSEUS2022-038Ilex ambigua Torr. Florida, United StatesNA2023COLLECTED12/14/2022Eglin 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, -86.9676710014Full 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 material2140822NA 88565
57NA 88509RJL2022TX-004Ilex decidua Walter Texas, United StatesNA2022COLLECTED11/01/2022Low woodlands along the north side of Texas State Hwy 190 between the highway and an unnamed paved service road that leads down to the Sabine River; the turn for the service road is approximately 0.62 kilometers west of the Sabine River. Near the bridge over the Sabine River.30.74730000, -93.6156890020Plants are growing in part-shade to shade of a moist mesic (occasionally temporarily wet) woodland. Ilex decidua can be in the low woods most of the way down to the river. Plant is a common understory shrub in the moist woodland habitat not far from the Sabine River. Soils: The underlying geology of this area is of Holocene origin and characterized as Alluvium. The alluvium and low terrace deposits along streams include sand, silt, clay, and gravel. Thickness is variable. In this case alluvium is from the Sabine River. (Source: USGS Texas Geologic Map Data). The primary soil types in the collection area are classified as Urbo and Mantachie soils. The Urbo series consists of deep, somewhat poorly drained soils. Permeability is very slow. These nearly level to gently sloping soils formed in clayey alluvium on flood plains of streams that drain uplands of the Southern Coastal Plain. Slopes range from 0 to 3 percent. In wet seasons late in winter and early in spring, the water table is at a depth of 1 to 2 feet and most areas of Urbo soils are subject to either occasional or frequent flooding of brief to long duration. The Mantachie series consists of very deep, somewhat poorly drained, moderately permeable soils on flood plains of the Southern Coastal Plain. They formed in loamy alluvium and considered acidic. Mantachie soils are subject to rare to frequent flooding in the winter and early spring for brief to long duration, unless protected. The seasonal high water table ranges from 1.0 to 1.5 feet of the surface during periods of high rainfall. (Source: NRCS Web Soil Survey).Wild material2139816NA 88509
58NA 88510RJL2022TX-005Crataegus marshallii Eggl. Texas, United StatesNA2022COLLECTED11/01/2022Plants growing along the west side of Texas State Hwy 87 on the edge of the woodlands. Plant is infrequently found, but a regular member of the woodlands as well as forest edge communities along the highway. 31.15847300, -93.73852000115Plants are growing in part-shade to sun on upland dry hills. In shade they survive, but in part-shade to sun they develop excellent flowering and fruiting.
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-Tehran 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-Tehran soils are on gently sloping to moderately steep uplands with slopes ranging from 1 to 20 percent. They are typically strongly acidic.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2139817NA 88510
59NA 88511RJL2022TX-006Persea palustris (Raf.) Sarg. Texas, United StatesNA2022COLLECTED11/01/2022Plants 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, -93.7510620071Plants 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 material2139818NA 88511
60NA 88512RJL2022TX-007Morella caroliniensis (Mill.) Small Texas, United StatesNA2022COLLECTED11/01/2022Plants 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, -93.7511800081Plants 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 material2139819NA 88512
61NA 87267(female selection)Ilex vomitoria Sol. ex Aiton f. pendula Foret & SolymosyTexas, United StatesNA2022COLLECTED01/27/2020Plants growing on the north side of the unpaved Private Road 6061, approximately 0.4 kilometers east of Texas State Hwy 87.31.16207000, -93.72862000132Growing in almost full sun on a south-facing roadside slope in very dry upland conditions. Soils are deep, somewhat excessively well-drained, and typically strongly acidic. Slope: 8 percent. Aspect: South. 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. The primary soil types in the collection area are classified as Letney-Tehran 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-Tehran soils are on gently sloping to moderately steep uplands with slopes ranging from 1 to 20 percent. They are typically strongly acidic.Wild materialFull name as recorded at U.S. National Arboretum: Ilex vomitoria forma pendula (female selection). Six plants of a selection of weeping yaupon holly sent from Shangri La Botanical Gardens & Nature Center (Rick Lewandowski facilitated the distribution in retirement). It is evidently from a selection discovered growing in Newton County, Texas, presumably from the wild. A date of 11/25/2020 is on the plant's tag from the source, but it is unknown if this is a propagation date or an accession date. Form received: rooted cutting.2158071NA 87267
62NA 88481RJL2022MD-002Kalmia latifolia L. Maryland, United StatesNA2022COLLECTED09/04/2022Plants growing at Elkton State Forest along roads and woodlands over a distance of approximately 5 kilometers labelled as the address of 717 Irishtown Rd, North East, MD 21901. Kalmia is very common along the unnamed gravel road as well as the understory of the upland woodlands.39.58852900, -75.9045290060Plants are growing in a mesic to dry, well-drained habitat of mixed deciduous and evergreen woodlands comprised primarily of acid-loving plants. Plants are growing in shade to part shade along the unnamed road as well as the woodlands. The soils in the collection area are generally described as a complex series of fluviomarine deposits. The soils range from a thin loam layer at the surface to varying levels of loam to sandy loam and/or extremely gravelly sandy clay loam strata, depending upon geographical location (ie. Hillslope summits, slopes, footslopes, swales, etc.). The primary soil types in the collection area are classified as Russett-Christiana-Hambrook Complex and/or Sassafras and Croom Soils; though, others may intersect and overlay in specific areas.Wild material2139360NA 88481
63NA 88482RJL2022MD-003Rhododendron periclymenoides (Michx.) Shinners Maryland, United StatesNA2022COLLECTED09/04/2022Plants growing at Elkton State Forest along roads and woodlands over a distance of approximately 5 kilometers labelled as the address of 717 Irishtown Rd, North East, MD 21901. Plants are found infrequently and scattered along the unnamed gravel road39.58852900, -75.9045290051Plants are growing in a mesic to dry, well-drained habitat of mixed deciduous and evergreen woodlands comprised primarily of acid-loving plants. Plants are growing in part shade. The soils in the collection area are generally described as a complex series of fluviomarine deposits. The soils range from a thin loam layer at the surface to varying levels of loam to sandy loam and/or extremely gravelly sandy clay loam strata, depending upon geographical location (ie. Hillslope summits, slopes, footslopes, swales, etc.). The primary soil types in the collection area are classified as Russett-Christiana-Hambrook Complex and/or Sassafras and Croom Soils; though, others may intersect and overlay in specific areas.Wild material2139361NA 88482
64NA 88484RJL2022MD-005Aronia melanocarpa (Michx.) Elliott Maryland, United StatesNA2022COLLECTED09/04/2022Plants growing at Elkton State Forest on Elk Neck Trail #3 (Starkey Lane) labelled as the address of 717 Irishtown Rd, North East, MD 21901. This was the only plant observed during several visits to Elk Neck State Forest during early and mid-summer39.58531200, -75.8956610055Plants are growing in a mesic to dry, well-drained habitat of mixed deciduous and evergreen woodlands comprised primarily of acid-loving plants. Plants are growing in part shade to part-sun. The soils in the collection area are generally described as a complex series of fluviomarine deposits. The soils range from a thin loam layer at the surface to varying levels of loam to sandy loam and/or extremely gravelly sandy clay loam strata, depending upon geographical location (ie. Hillslope summits, slopes, footslopes, swales, etc.). The primary soil types in the collection area are classified as Russett-Christiana-Hambrook Complex and/or Sassafras and Croom Soils; though, others may intersect and overlay in specific areas.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild materialreceived as A. prunifolia, on further examination by collector it was determined to be A. melanocarpa2139363NA 88484
65NA 88485RJL2022MD-006Hamamelis virginiana L. Maryland, United StatesNA2022COLLECTED09/04/2022Plants growing at Elkton State Forest on Elk Neck Trail #3 (Starkey Lane) labelled as the address of 717 Irishtown Rd, North East, MD 21901. This species was infrequent throughout most of Elk Neck State Park, but relatively common.39.58790000, -75.8885310054Plants are growing in a mesic to dry, well-drained habitat of mixed deciduous and evergreen woodlands comprised primarily of acid-loving plants. Plants are growing in part shade to shade. The soils in the collection area are generally described as a complex series of fluviomarine deposits. The soils range from a thin loam layer at the surface to varying levels of loam to sandy loam and/or extremely gravelly sandy clay loam strata, depending upon geographical location (ie. Hillslope summits, slopes, footslopes, swales, etc.). The primary soil types in the collection area are classified as Russett-Christiana-Hambrook Complex and/or Sassafras and Croom Soils; though, others may intersect and overlay in specific areas.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2139364NA 88485
66WLP 26102022VA-01Stewartia malacodendron L. Virginia, United StatesNA2022COLLECTED09/12/2022Woodlands 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 continuing36.73888200, -76.243277009Plants 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 material2139348WLP 2610
67WLP 26122022VA-03Styrax grandifolius Aiton Virginia, United StatesNA2022COLLECTED09/12/2022Northwest River Park on the south side of Indian Springs Road behind the Equestrian Center along a bridle trail. This plant is a common in the mesic woodlands at this location.36.58361100, -76.1627780021Plants growing in shade to part-shade of the mixed deciduous and evergreen mesic woodland about 1 to 2 meters above a nearby wetland area.
The underlying geology of this area is the Tabb Formation of Quaternary origin which is comprised of undifferentiated sand, silt, and peat and subdivided into three members. Within the Tabb Formation lies the Lynnhaven Member with pebbly and cobbly, fine to coarse gray sand grades upward into clayey and silty fine sand and sandy silt. Extensive low lands bounded on the landward side by river-, bay-, and ocean-facing scarps having toe altitudes of 5-6 meters. Thickness is 0 to 6.5 meters.
Source: USGS Virginia Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=VAQtl%3B0)
The surface soil profile of this area is Chapanoke-Yeopim complex, 0 to 3 percent slopes. These soil as somewhat poorly to moderately drained, acidic, and found on marine terraces and summits of low elevation coastal plain areas. They are comprised of silt loam, silty clay loam, sandy clay loam and loam in varying quantities across the profile; the depth to parent geology is approximately 200 cm.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx		Wild material2139350WLP 2612
68WLP 2600RJL2022FLAL-029Stewartia malacodendron L. Florida, United StatesNA2022COLLECTED08/07/2022Eglin AFB, in woodlands along Weaver Creek accessed from unnamed dirt road, 0.82 kilometers west of junction with Eglin AFB 720; approximately 0.73 kilometers north of junction with Choctaw Nolf Airfield Road and Eglin AFB 720.30.51680000, -86.9146940015Growing in moist, well-drained sandy soils above Weaver Creek in mixed broadleaved evergreen and deciduous woodland habitat in part shade to shade of west facing slopes several meters above the wetland zone. The Stewartia is growing in a high competition habitat. The underlying geology of this area is the Citronelle Formation, of Pliocene origin, and consists of gray to orange, often mottled, unconsolidated to poorly consolidated, very fine to very coarse, poorly sorted, clean to clayey sands. It contains significant amounts of clay, silt and gravel which may occur as beds and lenses and may vary considerably over short distances. Limonite nodules and limonite-cemented beds are common. Wild material2138710WLP 2600
69WLP 2576RJL2022-001Amelanchier arborea (F. Michx.) Fernald Maryland, United StatesNA2022COLLECTED05/25/2022Plants growing in open woodlands and part shade along unnamed Elkton State Forest gravel road over a distance of approximately 5 kilometers labelled as the address of 717 Irishtown Rd, North East, MD 21901.39.58089500, -75.9150590073Plants are found regularly but scattered along the unnamed gravel road as well as in open understory of the upland woodlands. Plants growing in a mesic to dry, well-drained habitat of mixed deciduous and evergreen woodlands comprised primarily of acid-loving plants. Plants are growing in part shade and open understory shade. The soils in the collection area are generally described as a complex series of fluviomarine deposits. The soils range from a thin loam layer at the surface to varying levels of loam to sandy loam and/or extremely gravelly sandy clay loam strata, depending upon geographical location (ie. Hillslope summits, slopes, footslopes, swales, etc.). The primary soil types in the collection area are classified as Russett-Christiana-Hambrook Complex and/or Sassafras and Croom Soils; though, others may intersect and overlay in specific areas.Wild material2138095WLP 2576
70W6 59998NCBG-395Eupatorium hyssopifolium L. Maryland, United StatesW62021Wild material2132880W6 59998
71NA 88399NCBG-670Kalmia latifolia L. Maryland, United StatesNA2021Wild material2116373NA 88399
72W6 58592MARSB-450Danthonia spicata (L.) P. Beauv. ex Roem. & Schult. New Jersey, United StatesW62021Wild materialDense tufts. Leaves born mostly near base, blades curly. lower sheaths often contain cleistogamous spikelets. inflorescence contracted, racemiform.2113522W6 58592
73OPGC 7975NCBG-416Lechea maritima Legg. ex Britton North Carolina, United StatesOPGCSEED2019Wild material2098440OPGC 7975
74WLP 172NACPEC19-069Smilax lasioneura Hook. North Carolina, United StatesNA2019COLLECTED09/16/2019Transylvania County; Southern Highland Reserve: Toxaway Mountain, Service Road (name unknown), adjacent to Southern Highlands Reserve: Power line cut.35.13228000, -82.983314001455Roadside edge, disturbed opening: mountaintop mixed Oak-Chestnut woodland (forest margin at high elevation)Wild material2110486WLP 172
75OPGC 5470JDC/BN/2018/056/869Baptisia nuttalliana Small Arkansas, United StatesOPGCFRUIT2018COLLECTED07/17/2018Located circa 2.60 miles northwest of Brightstar off Miller Road 159, Miller Road 74, Miller Road 75, Miller Road 154 and highway 237, Miller County33.14091000, -94.02229000109Roadside. Edges of woods.Wild materialPlants essentially all black with seeds past maturity by approximately 2-3 weeks, plants starting to break off at ground level and fruiting capsules starting to split at time of collection (17 July 2018). Seed quality rather poor at time of collection largely due to weevils. 1964612OPGC 5470
76Ames 34204JDC/ML/2018/030/843Monarda luteola Singhurst & W. C. Holmes Arkansas, United StatesNC7Image2018COLLECTED05/22/2018Located 2.62 miles northwest of Brightstar off Miller Road 159 just 0.54 miles north of junction with state highway 160, Miller County33.14091000, -94.02229000109Roadside. Open woods.Wild materialPlants with lemon scent, pubescent stems and leaves with faint yellow flowers measuring circa 2.0' in height. Leaves longer than internodes. Plants likely reached peaked flower around 16 May 2018. Seeds likely reached full maturity around first week in July (2018).1963387Ames 34204
77NA 84577RJL-RM001Halesia diptera J. Ellis Texas, United StatesNA2017COLLECTED07/22/2017Along either side of a clear creek on private property approximately 1.42 kilometers north of Texas Recreational Road 255 in northeastern Jasper County.31.07135000, -93.94985000107Plants growing along the embankments of the clear creek just above normal flood stage in primarily deciduous woodlands with some broadleaved evergreens and conifers. Plants are growing in part shade; some direct sunlight occurs during mid-day hours for 1-2 hours. Soils sandy and topped with a generous undisturbed decomposed litter layer. Slope: 10 percent. Aspect: variable.Wild material1953812NA 84577
78WLP 1437NA 84027Oxydendrum arboreum (L.) DC. Florida, United StatesNA2016COLLECTED11/11/2016Woodlands associated with Miller Bayou, south of housing subdivision off of Pearl Court.30.46413000, -86.928040002Full sun to partial shade in mixed coniferous/broadleaved evergreen woodlands, with a mixture of deciduous plants in highly acidic sandy soils approximately 100-300 ft. from the salt marsh edge associated with Miller Bayou.1950372WLP 1437
79NA 83904NA 83904Clethra acuminata Michx. Kentucky, United StatesNA2016COLLECTED09/27/2016Daniel Boone National Forest, Forest Service Road 828/Route 927, Panoramic View Trail #528.36.84200000, -84.52900000390Ridgetop trail.Wild material1952034NA 83904
80WLP 1433NA 83908Oxydendrum arboreum (L.) DC. Kentucky, United StatesNA2016COLLECTED09/27/2016Daniel Boone National Forest, Forest Service Road 828/Route 927, Panoramic View Trail #528.36.84400000, -84.52700000400Ridgetop trail.1951131WLP 1433
81NA 82643NA 82643Lonicera sempervirens L. Texas, United StatesNA2015COLLECTED07/20/2014East side of Texas Route 87 approximately 0.52 miles south of Trout Creek, Texas.30.61156000, -93.8050600021Southwest-facing edge of mature woodland in part to full sun; well-drained, seasonally moist soils that are sandy loam; surface has an excellent organic litter layer.1952603NA 82643
82NA 82648NA 82648Viburnum acerifolium L. Texas, United StatesNA2015COLLECTED08/31/2013West side of the road along Texas Route 87 north of Burkeville, Texas.31.11950000, -93.72656000141Dry, acidic woodlands in full shade beneath trees; soils sandy loam and are very loose and drought prone.Wild material1953129NA 82648
83NA 82043JDC/AP/2014/063/565Aesculus pavia L. Arkansas, United StatesNAFLOWER2014COLLECTED09/20/2014St. Francis National Forest.34.68710800, -90.67734100108Deciduous woods. Valleys, slopes, and ridges.Wild materialCollected as Aesculus parviflora and initially accessioned under that name. Renamed to A. pavia based on ID by Pablo Jourdan (Director, Ornamental Plant Germplasm Center at Ohio State University).1922344NA 82043
84NA 81984Lactea GroupCallicarpa americana L. Texas, United StatesNA2014COLLECTED08/30/2013Woodlands above Boykin Spring Lake.31.06266000, -94.2756500056Growing in partial shade of mixed deciduous and evergreen woodlands in well-drained to dry conditions.1951711NA 81984
85W6 33752UJO 53254Oxytropis pallasii Pers. Krym, UkraineW62008COLLECTED05/30/2008Outskirts of Alushta. From junction of P-34 and P-29, E on M-18, .91 km, then due S, .5 km.44.66694400, 34.39962100128Associated Species: Quercus pubescens, Pistacea mutica, Medicago falcata, M. sativa, Dorycnium graeacum; Land Element: ridge; Aspect: S; Exposure: unknown; Slope: 6-10%; Soil pH: unknown; Soil Moisture: dry; Soil Texture: unknownWild material1790445W6 33752
86W6 33754UJO 53203Medicago orbicularis (L.) Bartal. Krym, UkraineW62008COLLECTED06/13/2008Outskirts of Alushta. From junction of P-34 and P-29, E on M-18, .91 km, then due S, .5 km.44.66694400, 34.39962100128Associated Species: Quercus pubescens, Pistacea mutica, Medicago falcata, M. sativa, Dorycnium graeacum; Land Element: ridge; Aspect: S; Exposure: unknown; Slope: 6-10%; Soil pH: unknown; Soil Moisture: dry; Soil Texture: unknownWild material1790390W6 33754
87NA 78035AL #44Philadelphus inodorus L. Alabama, United StatesNA2008COLLECTED09/17/2008Just above the Cahaba River, near end of road and Caffee Creek.Wild material1913895NA 78035
88WLP 2120302025Juniperus virginiana L. Virginia, United StatesNASEED2008COLLECTED12/28/200589Slope: 0 Aspect: NE Soil: Clay-loam, Land form: Upland meadow. Mowed.Wild material1780179WLP 2120
89DVIT 3151RJL VA2003-005Vitis rotundifolia Michx. Virginia, United StatesDAV2003COLLECTED09/05/2003Collected from Chesapeake, VA at the interchange of Business Route 168 (Battlefield Ave) and Route 168, next to a detention basin and shopping plaza on the west side of Battlefield Ave.36.73861111, -76.242500005Mixed 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. Plants growing in part-shade to full sun where they produce abundant fruit.Breeding materialSeed collected from many individuals and massed. Associated plants: Acer rubrum, Carpinus caroliniana, Clethra alnifolia, fagus grandifolia, gelsemium nudiflorum, Hamamelis virginiana, Ilex opaca, Leucothoe racemosa, liquidambar styraciflua, Liriodendron tulipfera, Nyssa sylvatica, Oxydendrum arboreum, Persea borbonia, Quercus falcata, Quercus michauxii, Smilax sp., Stewartia malacodendron, Symplocos tinctoria and Vaccinium sp.1651338DVIT 3151