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ACCESSIONPLANT NAMETAXONOMYORIGINGENEBANKIMAGEAVAILABILITYRECEIVEDSOURCE TYPESOURCE DATECOLLECTION SITECOORDINATESELEVATIONHABITATIMPROVEMENT LEVELNARRATIVE
0WLP 177NACPEC19-090Aralia spinosa L. North Carolina, United StatesNA2019COLLECTED09/18/2019Clay County; Nantahala National Forest: Winding Stair Gap Parking Lot, Murphy Road, U.S. Hwy 64, Appalachian Trail Trailhead Parking35.11992300, -83.548046001134Parking lot edge of mixed mesophytic forest, drainage ditch adjacentWild material2110491WLP 177
1PI 675313R10-22-087Brachypodium rupestre (Host) Roem. & Schult. Stavropol, Russian FederationW6FLOWER2011COLLECTED07/24/2010Temperate deciduous forest understory. Granitic parent material, NW facing slope to flat meadow, 0-45% slope: seed collected from >100 plantsWild material1883180PI 675313
2PI 610911M189.CPG94Dactylis glomerata L. MoroccoW61994COLLECTED07/27/1994Near Taroudannt, 71 k northeast of Taroudant on road S501, to Marrakech, 19 k northeast of intersection with P32.30.81888889, -8.394722221240Grazed, protected. Slope 11-40%, aspect W. 1/4 shade. Soil sandy loam on calcareous rock, pH 9.0. Rainfall 350 mm. Seasonally dry, upper-mid slope. Vegetation closed, evergreen open forest with closed lower layers.Wild materialPopulation abundance frequent, distribution patchy. Growth habit erect.1480386PI 610911
3NA 88834RJL-RM2023FLAL-008Rhododendron canescens (Michx.) Sweet Florida, United StatesNA2023COLLECTED12/06/2023Blackwater 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, -86.9578470053Growing 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 material2165664NA 88834
4NA 88835RJL-RM2023FLAL-009Rhododendron viscosum (L.) Torr. Florida, United StatesNA2023COLLECTED12/06/2023Blackwater 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, -86.9628330043Growing 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 material2165665NA 88835
5NA 88820TJK2023AL-005Hydrangea arborescens L. Alabama, United StatesNA2023COLLECTED12/07/2023Between Monroe County Route 1 and Tom Hayles Road.31.40575900, -87.5492400022In woodlands on limestone outcrop. While the upper area of slopes is covered by a thin soil layer, the exposed limestone rock outcrop on the northwestern edge of this area is a low competition niche for plants like the Hydrangea to gain a foothold. Slope: 60% (plus). Aspect: Northwest. Elevation: 72 feet.Wild material2165649NA 88820
6NA 88821TJK2023AL-006Hydrangea quercifolia W. Bartram Alabama, United StatesNA2023COLLECTED12/07/2023Between Monroe County Route 1 and Tom Hayles Road.31.40580000, -87.5489000022In woodlands on limestone outcrop. While the upper area of slopes is covered by a thin soil layer, the exposed limestone rock outcrop on the northwestern edge of this area is a low competition niche for plants like the Hydrangea to gain a foothold. Slope: 60% (plus). Aspect: Northwest. Elevation: 72 feet.Wild material2165650NA 88821
7NA 88561RJLSEUS2022-034Hydrangea quercifolia W. Bartram Alabama, United StatesNA2023COLLECTED12/12/2022Plants growing in the woodlands at Haines Island Park at the foot of Tallahatta cuesta, accessed by foot via Ferry Road. Common at this site. 31.72178200, -87.4658960066Plants are growing in part-shade to shade of a moist mesic, well-drained conditions on rocks and in the eroding matrix of the Tallahatta Questa.
Soils: The underlying geology of this area is Claiborne Group, Tallahatta Formation, of Eocene origin, with white to very light-greenish-gray thin-bedded to massive siliceous claystone; interbedded with thin layers of fossiliferous clay, sandy clay, and glauconitic sand and sandstone.
Source: USGS Alabama Geological Map Data (https://mrdata.usgs.gov/geology/state/state.php?state=AL)
The primary soil type in the collection area is classified as Arundel Loam soil (8 to 35 percent slopes). The Arundel Series consists of moderately deep, well drained, very slowly permeable soils on dissected uplands of the Southern Coastal Plain. They formed in marine deposits consisting of acid clays underlain by horizontally bedded sandstone, buhrstone and siltstone. These soils are strongly acid. Slopes range from 2 to 60 percent.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)
Wild material2140786NA 88561
8WLP 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
9WLP 2568APS/HA/2022/028/490Hydrangea arborescens L. Arkansas, United StatesNAHABITAT2022COLLECTED03/15/2022Located approximately 3.75 miles east of Allison just off Round Bottom Road.35.93357000, -92.05110000144Moist, low deciduous forest with scattered rock outcrops, growing along base of hill and bank of seasonal stream. Wild material2137430WLP 2568
10NA 86845NACPEC15-004Acer oblongum Wall. ex DC. Gansu Sheng, ChinaNA2021COLLECTED10/05/2015Hui Xian: Jialingjiang. Santan33.65962500, 106.2134630070590 deg slope; N-facing; soil rock face with tussocks of organic material. Rock face above road along the Jialingjiang RiverWild material2116462NA 86845
11Ames 34787NCBG-330Rhus copallinum L. North Carolina, United StatesNC7SEED2018COLLECTED10/07/2015Dismal Swamp State Park areas of Laurel Hill Trail and Corapeake Road.36.54783000, -76.427630005Hardwood swamp roadsideWild material1965913Ames 34787
12Ames 29829NACPEC08-041Fraxinus paxiana Lingelsh. Shaanxi Sheng, ChinaNC7SEED2009COLLECTED09/26/2008Gua Tian Pu Bu, Zhu Que Township, Hu Xian District.33.81583300, 108.596500001953South-running stream valley; mesic, mixed deciduous forest. Thin, rocky soil.Wild materialTree; multi-stemmed; 4 meters in height; 8 cm DBH. Brown bark. Opposite leaves, pinnately compound, up to 30 cm long, 7 leaflets. Fruit: terminal panicles, each samara 3 cm long.1792100Ames 29829
13NA 67869QLG237Sophora davidii (Franch.) Skeels Gansu Sheng, ChinaNA1996COLLECTED10/18/1996Xiao Long Shan Forest Bureau, Dang Chuan Forest Station, Xian Ren Yan34.38333333, 106.033611111470Open sunny site on a steep slope; 35% S slope; sandy-loam well-drained soils over sandstone parent soils; growing w/ Quercus, Cotinus coggyria, Quercus spinosa, Cotoneaster horizontalis, ferns and numerous herbaceous species.Wild material2 meters; multi-stemmed deciduous shrub with upright spreading habit with very thorny stems; collected from 1-3 plants; bark dark brown to black 1579520NA 67869
14NA 67875QLG243Syringa oblata Lindl. subsp. oblata Gansu Sheng, ChinaNA1996COLLECTED10/18/1996Xiao Long Shan Forest Bureau, Dang Chuan Forest Station, Xian Ren Yan34.38333333, 106.033611111530Part shade to full sun; 40-60% W,E,S slopes; sandy-loam well-drained soils over sandstone parent soils; w/ Pinus bungeana, Platycladus orientalis, Cotoneaster, Ulmus, Quercus spinosa, Pinus tabuliformis and numerous herbaceous plt species.Wild material3-4 meters; multi-stemmed, deciduous shrub with upright arching habit; collected from about 10 plants 1579470NA 67875