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ACCESSIONPLANT NAMETAXONOMYORIGINGENEBANKIMAGEAVAILABILITYRECEIVEDSOURCE TYPESOURCE DATECOLLECTION SITECOORDINATESELEVATIONHABITATIMPROVEMENT LEVELNARRATIVE
0NA 67878QLG246Cornus kousa Hance subsp. chinensis (Osborn) Q. Y. Xiang Gansu Sheng, ChinaNA1996COLLECTED10/18/1996Xiao Long Shan Forest Bureau, Guang Ying Forest Station, Wang Jia Gou34.18361111, 106.000277781550Along woodland edge in upper canopy in full sun; 35% NW slope; clay-loam soil; w/ Symplocos paniculata, Populus sp., Quercus sp., Lindera sp., Campylotropis sp., Corylus sp., Sorbaria sp., Lonicera japonica and numerous herbaceous sp.Wild material9 meters; single-stemmed deciduous tree with upright vase-shaped habit; absolutely loaded with fruit; D.B.H. 18 cm; bark gray-brown to tan and exfoliating; fruit red, globe-shaped, 2-3 cm diameter 1579681NA 67878
1NA 67880 NA 67880QLG248Cornus controversa Hemsl. Gansu Sheng, ChinaNA1996COLLECTED10/06/1996Qinling Mountains: Tianshui City: Xiaolongshan Forestry Experimental Bureau, Guangying Forest Station, Wangjiagou.34.18516000, 106.010520001540Growing one meter above the stream in open, full sun and heavily grazed area among boulders; growing in clay-loam soil. Slope: Less than 3 percent. Aspect: North.Wild material1951538NA 67880 NA 67880
2NA 88748SOKO2024-001Viburnum dilatatum Thunb. Gangwon-do, Korea, SouthNA2025COLLECTED09/19/2024Yeongwol-gun: Yeongheung-ri: Jangneung Mulmurigol Marsh.37.20005000, 128.44996000244Boardwalk separating woodland edge and marsh in 50 percent shade. Organic soil [locally known for calcareous soils]. Slope: 5 to 10 degrees. Aspect: South-southwest.Wild material2172323NA 88748
3NA 890792024RJLPA-005Viburnum prunifolium L. Pennsylvania, United StatesNA2024COLLECTED09/20/2024Along gated road about 0.33 kilometers southwest of the Lake Ontelaunee Trail parking lot.40.50062600, -75.8900490094Plants are growing on moist, well-drained in part shade of a deciduous forest. Slope: 0 percent. Aspect: N/A. Geology: The underlying geology of this area is of Ordovician origin and characterized as Shale and graywacke of Hamburg sequence. It is characterized by shale containing zones of conspicuous graywacke. (Source: USGS Pennsylvania Geologic Map Data). Soils: The primary soil type in the area of this collection is classified as Holly Series Silt Loam (Ho). The Holly Series consists of very deep, very poorly and poorly drained soils formed in loamy alluvium on flood plains. Saturated hydraulic conductivity is moderately high through high in the mineral soil. Slope ranges from 0 through 3 percent. (Source: USDA-NRCS Official Soil Series Descriptions). EPA Ecoregion (Level III): Ridge and Valley (67). EPA Ecoregion (Level IV): Northern Shale Valleys (67b).Wild material2169043NA 89079
4NA 890812024RJLPA-009Rosa carolina L. Pennsylvania, United StatesNA2024COLLECTED09/22/2024Lancaster and York Counties: outcrops along the Susquehanna River, accessed from the Historic Lock 12 parking lot off of Pennsylvania Road 372.39.81483500, -76.3276220034Plants are growing from part-sun to full sun in crevices of the outcrops and where organic debris has accumulated in between boulders along the Susquehanna River. The sites range from nearly xeric to dry mesic, at least on the surface. Plants are generally growing 4-10 m above the normal flow of the river; however, the Holtwood Dam is less than 1 kilometer upstream and debris found trapped in the boulders indicates that there is periodic flooding, at least, in the lower zone of 4+ meters or so above normal river flow. This habitat has a diverse assemblage of deciduous trees and shrubs as well as abundant herbaceous taxa. Slope: 0 to 60 percent. Aspect: Northeast (generally). Geology: The underlying geology of this area is probably of lower Paleozoic age and characterized as the Octoraro Formation. It includes albite-chlorite schist, phyllite, some hornblende gneiss, and granitized members. Soils: The area where this species occurs is right on the edge of two soil zones that transition from the river’s edge to mesic conditions upslope. The first is generally referred to as Rock Outcrop. This terrestrial matrix in which plants grow is largely exposed underlying rock geology with accumulated outwash, rock decomposition, and organic debris buildup. The second is Mt. Airy (80%) and Manor (20%) Series soils, 25 to 60 percent slopes, extremely stony (MRF). (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). EPA Ecoregion (Level III): Northern Piedmont (64). EPA Ecoregion (Level IV): Piedmont Uplands (64c).Wild material2169045NA 89081
5NA 890832024RJLPA-012Rhododendron periclymenoides (Michx.) Shinners Pennsylvania, United StatesNA2024COLLECTED09/22/2024Outcrops along the Susquehanna River, accessed from the Historic Lock 12 parking lot off of Pennsylvania Road 372.39.81477400, -76.3280730035Plants are growing from shade to part-sun and occasionally full sun in crevices of the outcrops and where organic debris has accumulated in between boulders along the Susquehanna River. The sites range from nearly xeric to mesic, at least on the surface. Plants are generally growing 4-10 m above the normal flow of the river; however, the Holtwood Dam is less than 1 kilometer upstream and debris found trapped in the boulders indicates that there is periodic flooding, at least, in the lower zone of 4+ meters or so above normal river flow. This habitat has a diverse assemblage of deciduous trees and shrubs as well as abundant herbaceous taxa. Slope: 0 to 60 percent. Aspect: Northeast (generally). Geology: The underlying geology of this area is probably of lower Paleozoic age and characterized as the Octoraro Formation. It includes albite-chlorite schist, phyllite, some hornblende gneiss, and granitized members. Soils: The area where this species occurs is right on the edge of two soil zones that transition from the river’s edge to mesic conditions upslope. The first is generally referred to as Rock Outcrop. This terrestrial matrix in which plants grow is largely exposed underlying rock geology with accumulated outwash, rock decomposition, and organic debris buildup. The second is Mt. Airy (80%) and Manor (20%) Series soils, 25 to 60 percent slopes, extremely stony (MRF). (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). EPA Ecoregion (Level III): Northern Piedmont (64). EPA Ecoregion (Level IV): Piedmont Uplands (64c).Wild material2169047NA 89083
6NA 890842024RJLPA-013Physocarpus opulifolius (L.) Maxim. Pennsylvania, United StatesNA2024COLLECTED09/22/2024Outcrops along the Susquehanna River, accessed from the Historic Lock 12 parking lot off of Pennsylvania Road 372.39.81466300, -76.3283390036Plants are growing from shade to part-sun where organic debris has accumulated in between boulders as well as further upslope in deeper mesic soils along the Susquehanna River. This habitat has a diverse assemblage of deciduous trees and shrubs as well as abundant herbaceous taxa. Slope: 10 to 25 percent. Aspect: Northeast (generally). Geology: The underlying geology of this area is probably of lower Paleozoic age and characterized as the Octoraro Formation. It includes albite-chlorite schist, phyllite, some hornblende gneiss, and granitized members. Soils: The area where this species occurs is right on the edge of two soil zones that transition from the river’s edge to mesic conditions upslope. The first is generally referred to as Rock Outcrop. This terrestrial matrix in which plants grow is largely exposed underlying rock geology with accumulated outwash, rock decomposition, and organic debris buildup. The second is Mt. Airy (80%) and Manor (20%) Series soils, 25 to 60 percent slopes, extremely stony (MRF). (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). EPA Ecoregion (Level III): Northern Piedmont (64). EPA Ecoregion (Level IV): Piedmont Uplands (64c).Wild material2169048NA 89084
7NA 890852024RJLPA-014Rhododendron arborescens (Pursh) Torr. Pennsylvania, United StatesNA2024COLLECTED09/22/2024Outcrops along the Susquehanna River, accessed from the Historic Lock 12 parking lot off of Pennsylvania Road 372.39.81618100, -76.3306980038Plants are growing from shade to part-sun and occasionally full sun in crevices of the outcrops and where organic debris has accumulated in between boulders along the Susquehanna River. The sites range from nearly xeric to mesic, at least on the surface. Plants are generally growing 4-10 m above the normal flow of the river; however, the Holtwood Dam is less than 1 kilometer upstream and debris found trapped in the boulders indicates that there is periodic flooding, at least, in the lower zone of 4+ meters or so above normal river flow. This habitat has a diverse assemblage of deciduous trees and shrubs as well as abundant herbaceous taxa. Slope: 0 to 75 percent. Aspect: Northeast (generally). Geology: The underlying geology of this area is probably of lower Paleozoic age and characterized as the Octoraro Formation. It includes albite-chlorite schist, phyllite, some hornblende gneiss, and granitized members. Soils: The area where this species occurs is right on the edge of two soil zones that transition from the river’s edge to mesic conditions upslope. The first is generally referred to as Rock Outcrop. This terrestrial matrix in which plants grow is largely exposed underlying rock geology with accumulated outwash, rock decomposition, and organic debris buildup. The second is Mt. Airy (80%) and Manor (20%) Series soils, 25 to 60 percent slopes, extremely stony (MRF). (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). EPA Ecoregion (Level III): Northern Piedmont (64). EPA Ecoregion (Level IV): Piedmont Uplands (64c).Wild material2169049NA 89085
8NA 890862024RJLPA-015Ilex verticillata (L.) A. Gray Pennsylvania, United StatesNA2024COLLECTED09/22/2024Outcrops along the Susquehanna River, accessed from the Historic Lock 12 parking lot off of Pennsylvania Road 372.39.81656600, -76.3313660038Plants are growing from part-sun to full sun in crevices of the outcrops and where organic debris has accumulated in between boulders along the Susquehanna River. The sites range from nearly xeric to dry mesic, at least on the surface. Plants are generally growing 4-10 m above the normal flow of the river; however, the Holtwood Dam is less than 1 kilometer upstream and debris found trapped in the boulders indicates that there is periodic flooding, at least, in the lower zone of 4+ meters or so above normal river flow. This habitat has a diverse assemblage of deciduous trees and shrubs as well as abundant herbaceous taxa. Slope: 0 to 10 percent. Aspect: Northeast (generally). Geology: The underlying geology of this area is probably of lower Paleozoic age and characterized as the Octoraro Formation. It includes albite-chlorite schist, phyllite, some hornblende gneiss, and granitized members. Soils: The area where this species occurs is right on the edge of two soil zones that transition from the river’s edge to mesic conditions upslope. The first is generally referred to as Rock Outcrop. This terrestrial matrix in which plants grow is largely exposed underlying rock geology with accumulated outwash, rock decomposition, and organic debris buildup. The second is Mt. Airy (80%) and Manor (20%) Series soils, 25 to 60 percent slopes, extremely stony (MRF). (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). EPA Ecoregion (Level III): Northern Piedmont (64). EPA Ecoregion (Level IV): Piedmont Uplands (64c).Wild material2169050NA 89086
9WLP 3418HOKY23-13Acer tataricum L. subsp. aidzuense (Franch.) P. C. DeJong Honshu, JapanNA2024COLLECTED09/22/2023Tochigi Prefecture: Moka-shi: Utsunomiya University Farm.36.50005000, 139.98623330108Mesic woodland-farmfield edges above small stream. Growing in open to quarter-shade. Soil: Rich, organic-rich loam. Slope: 10°. Aspect: West. Elevation: 353 feet.Wild material2165756WLP 3418
10NA 88802TJK2023LA/TX-002Ilex decidua Walter Louisiana, United StatesNA2023COLLECTED11/21/2023Interstate 20, westbound, approximately 6 miles west of U.S. Highway 65 and 7.5 miles east of Louisiana Highway 577. Tensas River watershed.32.41950000, -91.2967000021Damp wooded treeline. Slope: 12%. Aspect: West-southwest. Elevation: 69 feet.Wild material2159185NA 88802
11NA 88803TJK2023LA/TX-003Crataegus viridis L. Louisiana, United StatesNA2023COLLECTED11/21/2023Interstate 20, westbound, approximately 7 miles west of Louisiana Highway 17 and 8.5 miles east of U.S. Highway 425. Tensas River watershed.32.41940000, -91.2967000021Damp wooded treeline. Slope: 12%. Aspect: West-southwest. Elevation: 69 feet.Wild material2159186NA 88803
12NA 88804TJK2023LA/TX-004Crataegus viridis L. Louisiana, United StatesNA2023COLLECTED11/21/2023Walnut Bayou (Mississippi River bottom): Interstate 20, westbound, approximately 10 miles west of the Mississippi River and 8.25 miles east of U.S. Highway 65.32.34130000, -91.0717000026Damp wooded treeline. Slope: 10%. Aspect: North-northeast. Elevation: 84 feet.Wild material2159187NA 88804
13Ames 35792APS/ID/2022/027/489Ilex decidua Walter Arkansas, United StatesNC7FRUIT2022COLLECTED03/15/2022Located approximately 3.75 miles east of Allison just off Round Bottom Road.35.93670000, -92.04891000133Dry west facing slope in a pine, oak, and hickory forest.Wild materialPlants sampled in nature with bright red fruits measuring 7-9 mm in diameter.2137431Ames 35792
14NA 86885RJL2021PA-004Ilex verticillata (L.) A. Gray Pennsylvania, United StatesNA2021COLLECTED11/16/2021Plants growing in woodlands along a small unnamed creek corridor dumping into the Middle Branch White Clay Creek in Goddard Park, West Grove Pennsylvania, off of Wickerton Road, Chester County.39.81063861, -75.82750806124Plants are growing in a range of habitats from mesic woodlands to saturated streamside settings of deciduous woodlands that drain toward the Middle Branch White Clay Creek. Plants grow in high understory shade with dappled to indirect sunlight. The only female (fruiting) plants were found in areas along the creek where soils are moist to saturated. Numerous male specimens were found in the areas described above. Soils: Soils found in the areas where this collection was made are comprised primarily of Baile silt loam (Ba), Hatboro silt loam (Ha), and Glenelg silt loam, 8 to 15 percent slopes (GgC). Baile silt loam consists of very deep, poorly drained, moderately low to moderately high saturated hydraulic conductivity, soils on upland depressions and footslopes that were formed in local alluvium over residuum from acid crystalline rocks, chiefly mica schist and granitized schist and gneiss; slope ranges from 0 to 8 percent. Hatboro silt loam consists of very deep and poorly drained soils formed in deposited alluvium derived from metamorphic and crystalline rock. They are on flood plains. Slopes range from 0 to 3 percent. Glenelg silt loam, 8 to 15 percent slopes consists of very deep, well drained soils formed in residuum weathered from micaceous schist on uplands of the Blue Ridge and the Northern Piedmont. This soil is undifferentiated, mostly poorly drained sandy bottomland soils intermingled with decomposing organic litter and eroded silts and clays due to erosion. Slope: 0 to 15% Aspect: Variable.Wild material2123125NA 86885
15WLP 1731RJL2021PA-001Viburnum acerifolium L. Pennsylvania, United StatesNA2021COLLECTED11/05/2021Plants growing in woodlands above a small unnamed creek that dumps into the Middle Branch White Clay Creek in Goddard Park, West Grove Pennsylvania, off of Wickerton Road, Chester County.39.80462083, -75.82888750103Plants growing in a mesic, well-drained habitat of deciduous woodlands, for the most part, above the riparian zone that drains toward a small unnamed creek that feeds into the Middle Branch White Clay Creek. Plants are growing in high understory shade with very little direct sun during most of the day. The remnant woodlands exist mostly along the steep slopes, wetlands and seeps of seasonal and year-round creeks flowing into the Middle Branch White Clay Creek. The woodlands are bordered by numerous housing developments and land converted to meadows; hence there is significant first order edge that is heavily impacted by invasive plant intrusion. Soils: Soils are classified as Glenelg silt loam, 8 to 15% slopes (GgC); this series consists of very deep, well drained soils formed in residuum weathered from micaceous schist on uplands of the Blue Ridge and the Northern Piedmont. Saturated hydraulic conductivity is moderately high in the subsoil and moderately high to high in the substratum. This upper horizon of this soil is undifferentiated, mostly poorly drained sandy bottomland soils intermingled with decomposing organic litter and eroded silts and clays due to erosion. Slope: 8 to 15% Aspect: West.Wild material2123080WLP 1731
16WLP 1732RJL2021PA-002Viburnum prunifolium L. Pennsylvania, United StatesNA2021COLLECTED11/05/2021Plants growing in woodlands along a small unnamed creek corridor dumping into the Middle Branch White Clay Creek in Goddard Park, West Grove Pennsylvania, off of Wickerton Road, Chester County.39.80462083, -75.82888750102Plants are growing in a range of habitats from drier upland woods to moist creekside settings of deciduous woodlands that drain toward the Middle Branch White Clay Creek. Plants grow in part shade to high understory shade with dappled to indirect direct sunlight. Plants achieve their largest size and fruiting potential in part sun of the riparian zone of the creek where woodland canopy is thinner. Soils: Soils found in the areas where this collection was made are comprised primarily of flood plain Hatboro silt loam (Ha) and well-drained, upland Glenelg silt loam, 8 to 15 percent slopes (GgC). Hatboro silt loam consists of very deep and poorly drained soils formed in deposited alluvium derived from metamorphic and crystalline rock. They are on flood plains. Slopes range from 0 to 3 percent. Glenelg silt loam, 8 to 15 percent slopes consists of very deep, well drained soils formed in residuum weathered from micaceous schist on uplands of the Blue Ridge and the Northern Piedmont. This soil is undifferentiated, mostly poorly drained sandy bottomland soils intermingled with decomposing organic litter and eroded silts and clays due to erosion. Slope: 0 to 15% Aspect: Variable.Wild material2123098WLP 1732
17WLP 1733RJL2021PA-003Viburnum dentatum L. Pennsylvania, United StatesNA2021COLLECTED11/05/2021Plants growing in woodlands along a small unnamed creek corridor dumping into the Middle Branch White Clay Creek in Goddard Park, West Grove Pennsylvania, off of Wickerton Road, Chester County.39.80522167, -75.82928139107Plants are growing in a range of habitats from mesic woodland to moist creekside settings of deciduous woodlands that drain toward the Middle Branch White Clay Creek. Plants grow in high understory shade with dappled to indirect sunlight. Soils: Soils found in the areas where this collection was made are comprised primarily of flood plain Hatboro silt loam (Ha) and well-drained, upland Glenelg silt loam, 8 to 15 percent slopes (GgC). Hatboro silt loam consists of very deep and poorly drained soils formed in deposited alluvium derived from metamorphic and crystalline rock. They are on flood plains. Slopes range from 0 to 3 percent. Glenelg silt loam, 8 to 15 percent slopes consists of very deep, well drained soils formed in residuum weathered from micaceous schist on uplands of the Blue Ridge and the Northern Piedmont. This soil is undifferentiated, mostly poorly drained sandy bottomland soils intermingled with decomposing organic litter and eroded silts and clays due to erosion. Slope: 0 to 15% Aspect: Variable.Wild material2123124WLP 1733
18WLP 1747RJL2021PA-005Rosa palustris Marshall Pennsylvania, United StatesNA2021COLLECTED11/20/2021Plants growing in wetland seeps surrounded by mown hayfields just west of the Middle Branch White Clay Creek in Goddard Park, West Grove Pennsylvania, off of Wickerton Road, Chester County.39.80090528, -75.82383250100Habitat Notes: Plants are growing in permanently saturated to moist soils in wetland habitats. Plants appear to be obligate wetland plants and are found only in permanent to nearly permanent wet habitats observed. Generally, the shrubs are found in part shade to full sun. Soils: Soils found in the areas where this collection was made are comprised primarily of Hatboro silt loam (Ha). Hatboro silt loam consists of very deep and poorly drained soils formed in deposited alluvium derived from metamorphic and crystalline rock. They are on flood plains. Slopes range from 0 to 3 percent. Slope: 0 to 3% Aspect: Variable.Wild material2123715WLP 1747
19NA 88332CBG-10580Hypericum prolificum L. Illinois, United StatesNA2021Wild materialPlant numbers sampled estimated.2120171NA 88332
20NA 88438MARSB-202Rosa palustris Marshall Delaware, United StatesNA2020Wild materialWoody plant with stems covered in recurved thorns. Mature fruit a scarlet hip.2106461NA 88438
21WLP 1996NACPEC18-112Viburnum henryi Hemsl. Hubei Sheng, ChinaNA2018COLLECTED09/22/2018Shennongjia Forest District; Muyuping; Quinn Jia Ping. [Mistake for Senjiping? Name appears to be wrong in any case (the first word does not fit with any Chinese character); cannot determine the intended locality name with certainty. Valley is unnamed on Google Maps, but is near something labeled "Xiaoping" in addition to "Senjiping".]31.43195000, 110.402480001482Wet flush on moss-covered cliff face. Growing in moss-covered, saturated soil.Seeds and four herbarium specimens collected from one plant. Photographed.2109000WLP 1996
22WLP 880NACPEC18-024Carpinus viminea Wall. ex Lindl. Hubei Sheng, ChinaNA2018COLLECTED09/15/2018Wufeng County; Shilingsi; Tupo.30.13663000, 110.630250001331Disturbed roadside with ruderals overlooking steep slope. Growing in humus and talus at base of cliff.Seeds and four herbarium specimens collected from one plant. Photographed.2108958WLP 880
23Ames 34790NCBG-535Rhus copallinum L. Virginia, United StatesNC7SEED2018COLLECTED09/21/2016Occoquan Bay National Wildlife Refuge just southeast of Woodbridge.38.64347000, -77.236750004MeadowWild material1965972Ames 34790
24WLP 1189NACPEC17-028Deutzia longifolia Franch. Sichuan Sheng, ChinaNA2017COLLECTED09/24/2017Pingwu County; Si Er; Si Er Cun; trail to Songpan.32.35074000, 103.961840002228Early successional woods on edge of trail, covered with lots of Artemisia vulgaris and terrestrial leeches. Soil gravelly, with some organic layer A-horizon.Seed collected from three plants. Four herbarium specimens collected; photographed.2108815WLP 1189
25WLP 2120302025Juniperus virginiana L. Virginia, United StatesNASEED2008COLLECTED12/28/200589Slope: 0 Aspect: NE Soil: Clay-loam, Land form: Upland meadow. Mowed.Wild material1780179WLP 2120
26WLP 1235SHX023Hydrangea sp.Shaanxi Sheng, ChinaNA1995COLLECTED04/09/1995Hei Wan, enroute to remote station, Beiba Province Grade Forest Station, Beiba County, Hanzhong District.32.69416667, 107.136111111590In stream valley among boulders on a north-facing slope in moist, but well-drained soils. In association with Aconitum sp., ferns, Cornus sp., Kerria japonica, bamboo, sedges, Astilbe sp., Rhododendron sp., and other species.Wild materialMulti-stemmed upright deciduous shrub, 2.5 meters tall with prominent tan-brown exfoliating bark; seed are borne in terminal clusters of panicle-like inflorescences with tiny capsules.1496753WLP 1235