| 0 | PI 604721 | 164 | Trifolium repens L. | Russian Federation | W6 | | | 1996 | COLLECTED | 08/23/1995 | Province Souchi, 3-4 km north of Ismyolfka. | 43.62666667, 39.80361111 | 250 | Past logged, now grazed and cultivated. Slope 11-40%, aspect S. Light open. Soil yellow clay, pH basic. Seasonally dry, mid slope. Vegetation closed, evergreen broad-leafed herb vegetation. | Wild material | Surrounding vegetation open deciduous forest with closed lower layers. Dominant tree species Castanea sp., Carpinus sp., Quercus sp. Dominant shrub species Laurocerasus sp., Ribes sp. Dominant herb/grass species Trifolium sp., annual grasses. Open degraded slope, 15% cover. Population distribution patchy. 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). | 1530924 | PI 604721 |
| 1 | PI 604766 | D165 | Trifolium pratense L. | Krasnodar, Russian Federation | W6 | | | 1996 | COLLECTED | 09/20/1995 | Krasnodarskiy kray, nearest village is Temnolesskaya. | | | Now logged. Slope 6-10%. 1/4 shade. Moist, mid slope. Vegetation closed, primary deciduous forest, scrub with scattered trees. | Wild material | Dominant tree species Carpinus betulus, Quercus robur, Castanea vulgaris. Dominant shrub species Rosa sp., Corylus avellana, Salix caprea. Dominant herb/grass species Calamogrostis sp., Doricnium graecum, Trifolium medium. Population distribution uniform, abundance rare. Growth habit spreading. 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). | 1531075 | PI 604766 |
| 2 | PI 611051 | VIR 137 | Dactylis glomerata L. | Russian Federation | W6 | | | 1996 | COLLECTED | 08/21/1995 | Province Novorossiysk, south of Aguaye on beach. | 44.14833333, 39.02222222 | 15 | Past logged, now settlement. slope 0-5%, aspect S. Light 1/4 shade. Soil clay, pH 7.5. Seasonally dry, cliff, beach. Vegetation closed, open deciduous forest with closed lower layers. Surrounding vegetation evergreen short grass. | Wild material | Dominant tree species Quercus sp, Castanea sp. Dominant shrub species Laurocerasus sp. Dominant herb/grass species Bermuda grass, Trifolium f. Lotus tenuis. Population abundance occasional. 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). | 1517972 | PI 611051 |
| 3 | PI 611055 | VIR 305 | Dactylis glomerata L. | Russian Federation | W6 | | | 1996 | COLLECTED | 09/20/1995 | Krasnodarskiy kray. Nearest village Temnolesskaya. | 44.26472222, 40.08750000 | 900 | Area logged. Slope 6-10%. 1/4 shade. Moist, mid-slope. pH 5.3. Vegetation closed, deciduous forest primary, closed scrub with scattered trees. | Wild material | Dominant tree species Carpinus betulus, Quercus robur, Castanea vulgaris. Dominant shrub species Rosa sp., Corylus avellana, Salix caprea. Dominant herb/grass species Calamagrostis sp., Dorycnium graecum, Trifolium medium. Population distribution uniform, abundance rare. 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). | 1517984 | PI 611055 |
| 4 | PI 631665 | 141 | Trifolium fragiferum L. | Russian Federation | W6 |  | | 1996 | COLLECTED | 08/21/1995 | Province Novorossiysk-Tuapsf, south of Aguaye (Agoy) on beach. | 44.14833333, 39.02222222 | 50 | Past logged, now settlement. Slope 0-5%, aspect S. Light 1/4 shade. Soil clay, limestone, beach platy stones, pH basic. Seasonally dry, cliff, beach. Vegetation closed, open deciduous forest with closed lower layers. | Wild material | Surrounding vegetation evergreen short grass. Dominant tree species Quercus sp., Castanea sp. Dominant shrub species Laurocerasus sp. Dominant herb/grass species Bermuda grass, Trifolium fragiferum, Lotus tenuis. Population abundance occasional. Growth habit prostrate. 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). | 1530902 | PI 631665 |
| 5 | PI 634061 | 304 | Trifolium medium L. | Krasnodar, Russian Federation | W6 | | | 1996 | COLLECTED | 09/20/1995 | Krasnodarskiy kray, nearest village is Temnolesskaya. | | | Now logged. Slope 6-10%. 1/4 shade. Moist, mid slope. Vegetation closed, primary deciduous forest, scrub with scattered trees. | Wild material | Dominant tree species Carpinus betulus, Quercus robur, Castanea vulgaris. Dominant shrub species Rosa sp., Corylus avellana, Salix caprea. Dominant herb/grass species Calamogrostis sp., Doricnium graecum, Trifolium medium. Population distribution patchy, abundance occasional. Growth habit prostrate. 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). | 1531028 | PI 634061 |
| 6 | PI 655813 | 136 | Lotus tenuis Waldst. & Kit. ex Willd. | Russian Federation | W6 |  | | 1996 | COLLECTED | 08/21/1995 | Province Novorossiysk-Tuapsf, south of Aguaye (Agoy) on beach. | 44.14833333, 39.02222222 | 50 | Past logged, now settlement. Slope 0-5%, aspect S. Light 1/4 shade. Soil clay, limestone rock, beach platy stones, pH basic. Seasonally dry, cliff, beach. Vegetation closed, open deciduous forest with closed lower layers. | Wild material | Surrounding vegetation evergreen short grass. Dominant tree species Quercus sp., Castanea sp. Dominant shrub species Laurocerasus sp. Dominant herb/grass species Bermuda grass, Trifolium fragiferum, Lotus tenuis. Population abundance frequent. 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 (greene@ars-grin.gov). | 1530899 | PI 655813 |
| 7 | 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 |
| 8 | 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 |
| 9 | NA 88678 | RJL2023PA-012 | Viburnum acerifolium L. | Pennsylvania, United States | NA | | | 2023 | COLLECTED | 10/27/2023 | Slopes on the east side of Creek Road above the North Branch of White Clay Creek. | 39.78552600, -75.80251900 | 90 | Well-drained mesic-dry to rocky dry deciduous woodlands in part shade to full shade. Slope: 15-35%. Aspect: West to northwest. The underlying geology of this area includes two formations. The first and primary formation is Lower Paleozoic Glenarm Wissahickon Formation, lithologically similar to oligoclase-mica schist of the Wissahickon Formation, but also includes lenticular amphibolite bodies having ocean-floor basalt chemistry. The second formation is Lower Paleozoic Mafic Gneiss Formation that is dark and medium grained. It includes rocks of probable sedimentary origin. (Sources: USGS Pennsylvania Geologic Map Data). The primary soil type in the collection area is classified as Manor Series. The Manor Series consists of well-drained residuum weathered from micaceous schist. Soils in the upper pedon (0-33 cm) are very dark grayish brown loam with strong fine granular structure; also, very friable with fine mica flakes and strongly acid. Lower pedon soils (34-56 cm) are strong brown, sandy loams. They have weak medium sub-angular blocky structure, are friable with many fine and a few medium mica flakes; this pedon is very strongly acid. (Source: NRCS Web Soil Survey). | Wild material | | 2159069 | NA 88678 |
| 10 | NA 88489 | RJL2022PA-005 | Kalmia latifolia L. | Pennsylvania, United States | NA | | | 2022 | COLLECTED | 09/10/2022 | Plants are growing on the lands of Hawk Mountain Sanctuary. This species is very common and abundant. It is one of the most dominant understory plants in woodlands. This species is a common understory shrub throughout the entire region in upland dry woodland habitats. | 40.63862000, -75.99071200 | 430 | Plants are growing primarily in shade to part-shade on a dry-mesic to very dry, well-drained upland/montane habitat characterized by upland mixed deciduous and evergreen forest that is very rocky. All of the plants found in this habitat go through periods of drought during the growing season due to the limited litter/soil layer in which moisture can be held. The underlying geology of this area is of Silurian origin and comprised of Shawangunk Formation. This formation is primarily light- to dark-gray, fine- to very coarse-grained sandstone and conglomerate containing thin shale interbeds.
Source: USGS Pennsylvania Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=PASs%3B14)
The surface soil profile of this area is the Hazleton series consists of deep and very deep, well drained soils formed in residuum of acid gray, brown or red sandstone on uplands. The matrix includes a considerable accumulation of thin, flat, coarse fragments of sandstone, limestone, or schist with diameters up to 15 cm. Slope ranges from 0-80%. Permeability is moderately rapid to rapid.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2139368 | NA 88489 |
| 11 | NA 88491 | RJL2022PA-007 | Rhododendron maximum L. | Pennsylvania, United States | NA | | | 2022 | COLLECTED | 09/10/2022 | Plants are growing on the lands of Hawk Mountain Sanctuary. This species was common, but generally restricted to steep rocky outcrops. | 40.63813900, -75.98835200 | 420 | Plants are growing from shade to full sun on a dry-mesic to very dry, well-drained upland/montane habitat characterized by an upland mixed deciduous and evergreen forest that is very rocky. Even so, most heavily fruited plants were growing in part shade to almost full sun. All of the plants found in this habitat go through periods of drought during the growing season due to the limited litter/soil layer in which moisture can be held. The underlying geology of this area is of Silurian origin and comprised of Shawangunk Formation. This formation is primarily light- to dark-gray, fine- to very coarse-grained sandstone and conglomerate containing thin shale interbeds.
Source: USGS Pennsylvania Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=PASs%3B14)
The surface soil profile of this area is the Hazleton series consists of deep and very deep, well drained soils formed in residuum of acid gray, brown or red sandstone on uplands. The matrix includes a considerable accumulation of thin, flat, coarse fragments of sandstone, limestone, or schist with diameters up to 15 cm. Slope ranges from 0-80%. Permeability is moderately rapid to rapid.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2139370 | NA 88491 |
| 12 | NA 87204 | RJL2022FLAL-019 | Ilex coriacea (Pursh) Chapm. | Florida, United States | NA | | | 2022 | COLLECTED | 08/02/2022 | Corner of San Jose Street and South 28th Avenue just east of Avalon Beach, FL. | 30.53172700, -87.09058900 | 3 | Growing in full sun to part shade in moist to wet areas, often with sphagnum moss along the edges, just above the water in ditches and waterways. Population is so dense that plants are crowding out other species. The underlying geology of this area is classified as Alluvium, of Pleistocene/Holocene origin and consists of undifferentiated Quaternary sediments of varying thickness including siliciclastics, organics and freshwater carbonates. The siliciclastics are light gray, tan, brown to black, unconsolidated to poorly consolidated, clean to clayey, silty, unfossiliferous, variably organic-bearing sands to blue green to olive green, poorly to moderately consolidated, sandy, silty clays. Organics occur as plant debris, roots, disseminated organic matrix and beds of peat. Freshwater carbonates, often referred to as marls in the literature, are scattered. | Wild material | | 2138707 | NA 87204 |
| 13 | Ames 33746 | UC 110a | Aronia melanocarpa (Michx.) Elliott | Tennessee, United States | NC7 |  | | 2016 | COLLECTED | 10/01/2009 | Near Newcomb, Campbell County | 36.53751670, -84.15580000 | 541 | Very dry, exposed rock spine with primarily organic soil and plants growing in cracks and pockets. Growing in association with Pinus virginiana, Quercus, Vaccinium, Gaylussacia, Castanea, Amelanchier, Magnolia ashei, Magnolia tripetala, Oxydendrum, Nyssa, Liquidambar styraciflua. | Wild material | This accession has been confirmed to represent the "southern form" of A. melanocarpa, potentially a new Aronia species. This southern form was originally discovered by Brand et al. 2022 (Ploidy, genetic diversity and speciation of the genus Aronia) and is known for having glabrous stems and leaves and a distinct phyllotaxy than other Aronia species. In addition, plants tend to bloom approximately two weeks later than all other Aronia taxonomic groups and the inflorescences/infructescences are more spreading and extended due to longer peduncles and pedicels within the cyme. Fruit maturity tends to occur 2 to 4 weeks later than tetraploid A. melanocarpa and 4 to 6 weeks later than diploid A. melanocarpa. Phenolic levels are much higher in comparison to other A. melanocarpa accessions (Brand et al., 2017 - Anthocyanins, total phenolics, ORAC and moisture content of wild and cultivated dark-fruited Aronia species.) | 1942832 | Ames 33746 |
| 14 | W6 18396 | 138 | Medicago polymorpha L. | Russian Federation | W6 | | | 1996 | COLLECTED | 08/21/1995 | Province Novorossiysk-Tuapsf, south of Aguaye (Agoy) on beach. | 44.14833333, 39.02222222 | 50 | Past logged, now settlement. Slope 0-5%, aspect S. Light 1/4 shade. Soil clay, limestone rock, beach platy stones, pH basic. Seasonally dry, cliff, beach. Vegetation closed, open deciduous forest with closed lower layers. | Wild material | Surrounding vegetation evergreen short grass. Dominant tree species Quercus sp., Castanea sp. Dominant shrub species Laurocerasus sp. Dominant herb/grass species Bermuda grass, Trifolium fragiferum, Lotus tenuis. Population distribution patchy. Growth habit prostrate. 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). | 1530900 | W6 18396 |