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ACCESSIONPLANT NAMETAXONOMYORIGINGENEBANKIMAGEAVAILABILITYRECEIVEDSOURCE TYPESOURCE DATECOLLECTION SITECOORDINATESELEVATIONHABITATIMPROVEMENT LEVELNARRATIVE
0NA 88132NEWFS-320Lindera benzoin (L.) Blume Massachusetts, United StatesNASEED2019Wild material2098196NA 88132
1NA 88092MARSB-164Lindera benzoin (L.) Blume Delaware, United StatesNASEED2019Wild material2097504NA 88092
2NA 88120MARSB-651Lindera benzoin (L.) Blume Delaware, United StatesNA2019Wild material2097672NA 88120
3NA 88023NCBG-300Lindera benzoin (L.) Blume Maryland, United StatesNASEED2018Wild material1965905NA 88023
4NA 88024NCBG-316Lindera benzoin (L.) Blume Virginia, United StatesNASEED2018Wild material1965909NA 88024
5WLP 1354JDC/LB/2009/089/239Lindera benzoin (L.) Blume Ohio, United StatesNA2009COLLECTED10/15/2009Near Lake Katherine, SW 1/4 of NW 1/4 of Section 13, T7N, R19W, Jackson Quad, Jackson County.39.08250000, -82.6775000023610% slope, north facing. Compacted soils. Associated with with Acer saccharum, Cornus florida, Magnolia tripetela, Oxydendrum arboreum, Quercus, and Tsuga canadensis.Wild material1823931WLP 1354
6WLP 1369JDC/LB/2008/044/114Lindera benzoin (L.) Blume Missouri, United StatesNAHABITAT2008COLLECTED10/09/2008Missouri: Bollinger County; Amidon Memorial Conservation Area, near Stannett Creek, south edge of NE 1/4 of SE 1/4 of Section 10.37.56027778, -90.13972222232Common in understory/fairly shaded areas. Associated with Acer saccharum, Carpinus caroliniana, Cercis canadensis, Fraxinus americana, Juglans nigra, Quercus muhlenbergii, Staphylea trifolia, Ulmus, and Viburnum prunifolium.Wild materialSome original plants with yellow fall color.1788215WLP 1369
7NA 63273NG 14Lindera benzoin (L.) Blume Maryland, United StatesNA1991COLLECTED10/02/1991Maryland, Caroline County, Tuckahoe State ParkWild materialSmall tree. Bright red fruit.1494721NA 63273
8NA 61256GU 106Lindera benzoin (L.) Blume United StatesNA1989COLLECTED09/26/1989Blue Ridge mile 36.1, George Washington National Forest, Blue Ridge Parkway, Virginia37.81056600, -79.23047600650Wild material1112021NA 61256
9PI 702691MARSB-322Chasmanthium laxum (L.) H. O. Yates New Jersey, United StatesS9SEED2019Wild material2097574PI 702691
10PI 702701MARSB-249Dichanthelium clandestinum (L.) Gould New York, United StatesS9SEED2019Wild material2097541PI 702701
11PI 675142ccc-021Actaea racemosa L. West Virginia, United StatesNC72009Wild materialPlants 5-8 feet in height; 3 ternately divided leaves; primary leaflet pinnately compound, odd, opposite; terminal pinnule 3x4 inch palmate with deep sinus; opposite pinnules 2x3 inch palmate with 4 sinus/4 lobes; rounded base; acuminate apex; margin doubly serrate/twice incised; venation palmate/textured beneath; dark brown above; brown below; glabrous hair; blue black petiole; ripe green to brown ovules of fruit; 8 brown/black crescent-shaped seeds within each tiny dried black orb, hanging in two rows on upper stalk.1829509PI 675142
12PI 675143ccc-024Actaea racemosa L. New Jersey, United StatesNC72009Wild materialPlants 1.5 feet in height; 3 ternately divided leaves; primary leaflet pinnately compound, odd, opposite; terminal pinnule 3x4 inch palmate with deep sinus; opposite pinnules 2x3 inch palmate with 4 sinus/4 lobes; rounded base; acuminate apex; margin doubly serrate/twice incised; venation palmate/textured beneath; pale green above; light green below; fair luster; glabrous hair; blue black petiole.1829510PI 675143
13PI 64902146Actaea racemosa L. Missouri, United StatesNC72004Wild material1 meter tall.1668177PI 649021
14PI 64908260Hypericum punctatum Lam. Arkansas, United StatesNC7PLANT2004COLLECTED10/22/2004Home of Don Matt and Judy Griffith, Ninestone Land Trust, 973 County Road 512, Berryville, Carroll County.36.22913300, -93.55115000399Wet, seeping bog. Western aspect. Wild material5-10 feet tall.1668194PI 649082
15PI 597623Index Seminum 47Spiraea alba Du Roi var. latifolia (Aiton) Dippel Pennsylvania, United StatesNC71993COLLECTEDChester County. Serpentine Barrens, Piedmont Province.39.73333333, -76.03333333130Near stream, shady and moist. Growing with Acer rubrum and Lindera benzoin.Wild material1086008PI 597623
16PI 649698Index Seminum 32Physocarpus opulifolius (L.) Maxim. Pennsylvania, United StatesNC7PLANT1993COLLECTEDAlong Butter Creek, Manderville Preserve, Piedmont Province, Bucks County.40.38333333, -75.36666667150Moist deciduous woods on slope. Wild materialMay harbor genes for dwarf plant form (see Ames 27797 which was a clonal selection from PI 649698, made because of the dwarf habit of one seedling in the PI 649698 grow-out).1086004PI 649698
17NA 891582025RJLSEUS-06Cornus florida L. Alabama, United StatesNA2025COLLECTED10/01/2025Coosa Wildlife Management Area: along the edge of gated dirt road on the west side of Coosa County Road 29, 0.3 kilometers north of Hatchet Creek.32.86402200, -86.33871400108Plants are growing in part sun to shade on dry-mesic slopes above the road cut on the gated dirt road; most likely a road for access for fire control/forest management. The forest is a combination of deciduous and evergreen with evergreens primarily comprised of Pinus taeda. The habitat was quite dry during this time of year. Slope: 5 to 20 percent. Aspect: North. Soils: The primary soil in the area of this collection is classified as Madison-Louisa Series complex, 15 to 30 percent slopes, moderately eroded (MdE2). The Madison Series soils are very deep, well drained soils with medium runoff found on Piedmont uplands in interstream divides, ridges and side slopes. They are comprised of residuum weathered from felsic or intermediate, high-grade metamorphic or igneous rocks high in content of mica. Slopes range from 2 to 60 percent and soil is typically strongly acidic. Louisa Series soils The Louisa Series soils consist of shallow, somewhat excessively drained soils which formed over mica gneiss and schist bedrock. They occur on Piedmont uplands. Slopes are 6 to 80 percent. This soil is moderately acid. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). Geology: The underlying geology of this area is of Precambrian to Paleozoic origin and characterized as Hatchet Creek Group; Pinchoulee Gneiss Formation. It is characterized by medium to fine-grained migmatitic, locally garnetiferous biotite-feldspar gneiss, commonly saturated with granitic pods. (Source: USGS Alabama Geologic Map Data).Wild material2193004NA 89158
18NA 890772024RJLPA-003Viburnum acerifolium L. Pennsylvania, United StatesNA2024COLLECTED09/19/2024Birdell Road, near parking lot to trail where the road ends at Chambers Lake, which is part of Hibernia County Park.40.03559500, -75.85708600187Plants are growing in deep shade of a dry deciduous forest dominated by Fagus grandifolia. Slope: 0 percent. Aspect: N/A. Geology: The underlying geology of this area is of Precambrian origin and characterized as Banded Mafic Gneiss. It is characterized as dark and fine to medium grained. This formation includes rocks of probable sedimentary origin; may be equivalent to "PZmgh." (Source: USGS Pennsylvania Geologic Map Data). Soils: The primary soil type in the area of this collection is classified as Neshaminy Series Silt Loam, very deep over mafic gneiss, 3 to 8 percent slopes (NvB). (Source: USDA-NRCS Official Soil Series Descriptions). EPA Ecoregion (Level III): Northern Piedmont (64). EPA Ecoregion (Level IV): Piedmont Uplands (64c).Wild material2169041NA 89077
19NA 890782024RJLPA-004Staphylea trifolia L. Pennsylvania, United StatesNA2024COLLECTED09/20/2024Along gated road about 0.33 kilometers southwest of the Lake Ontelaunee Trail parking lot.40.49850800, -75.8912130094Plants are growing on well-drained steep slopes in shade to part shade of a deciduous forest. Slope: 35 to 50 percent. Aspect: East-southeast. 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 Berks-Weikert Complex, 25 to 60% slopes (BkF). Dominantly sloping to very steep, moderately deep and shallow, well drained soils underlain by acid shale bedrock. (Source: UPenn State University Soil Info Website). EPA Ecoregion (Level III): Ridge and Valley (67). EPA Ecoregion (Level IV): Northern Shale Valleys (67b).Wild material2169042NA 89078
20NA 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
21NA 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
22NA 890822024RJLPA-010Amorpha fruticosa L. Pennsylvania, United StatesNA2024COLLECTED09/22/2024Outcrops along the Susquehanna River, accessed from the Historic Lock 12 parking lot off of Pennsylvania Road 372.39.81481500, -76.3275790034Plants 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 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 material2169046NA 89082
23NA 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
24NA 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
25NA 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
26NA 890872024RJLPA-016Hydrangea arborescens L. Pennsylvania, United StatesNA2024COLLECTED09/22/2024Outcrops along the Susquehanna River, accessed from the Historic Lock 12 parking lot off of Pennsylvania Road 372.39.81489000, -76.3291220043Plants are growing in deep shade of the deciduous woodlands on outcrops and the steep slopes where organic debris and detritus has accumulated. This habitat has a diverse assemblage of deciduous trees and shrubs as well as abundant herbaceous taxa. Slope: 30 to 90 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. (Source: Source: USGS Pennsylvania Geologic Map Data). 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 material2169051NA 89087
27WLP 3492St. Francois State ParkHydrangea arborescens L. Missouri, United StatesNAHABITAT2024COLLECTED01/19/2024St. Francois State Park, 8920 US Highway 67 North, approximately 3.2 miles north-northeast of Bonne Terre.37.96381000, -90.53403000202Rocky outcrops above Big River and rocky areas on bank of Big River.Wild material2166135WLP 3492
28NA 88671RJL2023PA-005Rhododendron maximum L. Pennsylvania, United StatesNA2023COLLECTED10/16/2023Appalachian National Scenic Trail: Pulpit Rock and Pinnacle Loop. Rocky woodlands along Furnace Creek as well as steep rocky slopes above Pulpit Rock Reservoir associated with the Pulpit Rock and Pinnacle Loop Trail.40.59226100, -75.94588800301Well-drained and very rocky dry deciduous woodlands in part shade to full shade. Slope: 0-30%. Aspect: variable. The underlying geology of this area is of Silurian origin and characterized as the Shawangunk Formation. It is characterized by light- to dark-gray, fine- to very coarse-grained sandstone and conglomerate containing thin shale interbeds. Includes four members, in descending order: Tammany--conglomerate and sandstone; Lizard Creek--sandstone and red or green shale; Minsi--sandstone and conglomerate; Weiders--conglomerate. Tammany and Lizard Creek Members together are approximately equivalent to Clinton Group to the west; Minsi and Weiders Members together are equivalent to Tuscarora Formation to the west. (Source: USGS Pennsylvania Geologic Map Data). The primary soil type in the collection area is classified as Hazleton Series. The Hazleton series consists of deep and very deep, well drained soils formed in residuum of acid gray, brown or red sandstone on uplands. Slope ranges from 0 to 80 percent. Permeability is moderately rapid to rapid. Solum thickness ranges from 60 to 120 centimeters. Depth to lithic contact ranges from 1 to 2 meters. Rock fragments of angular sandstone, dominantly less than 25 cm in size, range from 5 to 70 percent in individual horizons. Boulders, stones, flags and channers cover about 5 to 60 percent of the surface of some pedons. Reaction ranges from strongly acid through extremely acid throughout. (Source: NRCS Web Soil Survey).Wild material2159062NA 88671
29NA 88672RJL2023PA-006Rhododendron periclymenoides (Michx.) Shinners Pennsylvania, United StatesNA2023COLLECTED10/16/2023Appalachian National Scenic Trail: Pulpit Rock and Pinnacle Loop. Rocky woodland edges above Furnace Creek around Pulpit Rock and Pinnacle Loop Trail.40.58668200, -75.94269600247Well-drained and very rocky dry deciduous woodlands in part shade to full shade. Slope: 10%. Aspect: East. The underlying geology of this area is of Silurian origin and characterized as the Shawangunk Formation. It is characterized by light- to dark-gray, fine- to very coarse-grained sandstone and conglomerate containing thin shale interbeds. Includes four members, in descending order: Tammany--conglomerate and sandstone; Lizard Creek--sandstone and red or green shale; Minsi--sandstone and conglomerate; Weiders--conglomerate. Tammany and Lizard Creek Members together are approximately equivalent to Clinton Group to the west; Minsi and Weiders Members together are equivalent to Tuscarora Formation to the west. (Source: USGS Pennsylvania Geologic Map Data). The primary soil type in the collection area is classified as Hazleton Series. The Hazleton series consists of deep and very deep, well drained soils formed in residuum of acid gray, brown or red sandstone on uplands. Slope ranges from 0 to 80 percent. Permeability is moderately rapid to rapid. Solum thickness ranges from 60 to 120 centimeters. Depth to lithic contact ranges from 1 to 2 meters. Rock fragments of angular sandstone, dominantly less than 25 cm in size, range from 5 to 70 percent in individual horizons. Boulders, stones, flags and channers cover about 5 to 60 percent of the surface of some pedons. Reaction ranges from strongly acid through extremely acid throughout. (Source: NRCS Web Soil Survey).Wild material2159063NA 88672
30NA 88673RJL2023PA-007Rhododendron pilosum (Michx.) Craven Pennsylvania, United StatesNA2023COLLECTED10/25/2023Ned Smith Center for Art and Nature.40.53367300, -76.92715700147Well-drained and very rocky, dry slopes above 10-50 meters above Wiconisco Creek in mixed deciduous and evergreen woodlands in part shade to full shade. Slope: 10-40%. Aspect: North. The underlying geology of this area is of Mississippian origin and characterized as the Pocono Formation. It is comprised of light-gray to buff or light-olive-gray, medium-grained, crossbedded sandstone and minor siltstone; commonly conglomeratic at base and in middle; medial conglomerate, where present, is used to divide into Mount Carbon and Beckville Members; equivalent to Burgoon Sandstone of Allegheny Plateau. (Source: USGS Pennsylvania Geologic Map Data). The primary soil type in the collection area is classified as Laidig Series. The Laidig series consists of very deep, well drained soils formed in colluvium from sandstone, siltstone, and some shale. They are gently sloping to very steep soils on benches and foot slopes. Permeability is moderate or moderately rapid above the fragipan and moderately slow or slow in the fragipan. Slope ranges from 0 to 55 percent. Solum thickness ranges from 1.25 to 2.0 meters or more. Depth to the fragipan ranges from 0.75 to 1.25 meters. The particle-size control section averages less than 35 percent rock fragments. Rock fragments range from 5 to 50 percent in individual subhorizons of the A, E, BE, BA and Bt horizons; 15 to 70 percent in individual subhorizons of the Btx horizon; and 20 to 70 percent in the C horizon. Rock fragments are mostly sandstone but include siltstone and shale. Rock fragments include channers, cobbles, flagstones, and stones. Soils range from extremely acid through strongly acid throughout. (Source: NRCS Web Soil Survey).Wild material2159064NA 88673
31NA 88674RJL2023PA-008Kalmia latifolia L. Pennsylvania, United StatesNA2023COLLECTED10/25/2023Ned Smith Center for Art and Nature.40.53463500, -76.92616300130Well-drained and very rocky, dry slopes above 10-50 meters above Wiconisco Creek in mixed deciduous and evergreen woodlands in part shade to full shade. Slope: 10-40%. Aspect: North. The underlying geology of this area is of Mississippian origin and characterized as the Pocono Formation. It is comprised of light-gray to buff or light-olive-gray, medium-grained, crossbedded sandstone and minor siltstone; commonly conglomeratic at base and in middle; medial conglomerate, where present, is used to divide into Mount Carbon and Beckville Members; equivalent to Burgoon Sandstone of Allegheny Plateau. (Source: USGS Pennsylvania Geologic Map Data). The primary soil type in the collection area is classified as Laidig Series. The Laidig series consists of very deep, well drained soils formed in colluvium from sandstone, siltstone, and some shale. They are gently sloping to very steep soils on benches and foot slopes. Permeability is moderate or moderately rapid above the fragipan and moderately slow or slow in the fragipan. Slope ranges from 0 to 55 percent. Solum thickness ranges from 1.25 to 2.0 meters or more. Depth to the fragipan ranges from 0.75 to 1.25 meters. The particle-size control section averages less than 35 percent rock fragments. Rock fragments range from 5 to 50 percent in individual subhorizons of the A, E, BE, BA and Bt horizons; 15 to 70 percent in individual subhorizons of the Btx horizon; and 20 to 70 percent in the C horizon. Rock fragments are mostly sandstone but include siltstone and shale. Rock fragments include channers, cobbles, flagstones, and stones. Soils range from extremely acid through strongly acid throughout. (Source: NRCS Web Soil Survey).Wild material2159065NA 88674
32NA 88675RJL2023PA-009Viburnum acerifolium L. Pennsylvania, United StatesNA2023COLLECTED10/25/2023Ned Smith Center for Art and Nature.40.53539200, -76.92313500136Well-drained and very rocky dry deciduous woodlands in part shade to full shade. Slope: 10-30%. Aspect: North. The underlying geology of this area is of Mississippian origin and characterized as the Pocono Formation. It is comprised of light-gray to buff or light-olive-gray, medium-grained, crossbedded sandstone and minor siltstone; commonly conglomeratic at base and in middle; medial conglomerate, where present, is used to divide into Mount Carbon and Beckville Members; equivalent to Burgoon Sandstone of Allegheny Plateau. (Source: USGS Pennsylvania Geologic Map Data). The primary soil type in the collection area is classified as Laidig Series. The Laidig series consists of very deep, well drained soils formed in colluvium from sandstone, siltstone, and some shale. They are gently sloping to very steep soils on benches and foot slopes. Permeability is moderate or moderately rapid above the fragipan and moderately slow or slow in the fragipan. Slope ranges from 0 to 55 percent. Solum thickness ranges from 1.25 to 2.0 meters or more. Depth to the fragipan ranges from 0.75 to 1.25 meters. The particle-size control section averages less than 35 percent rock fragments. Rock fragments range from 5 to 50 percent in individual subhorizons of the A, E, BE, BA and Bt horizons; 15 to 70 percent in individual subhorizons of the Btx horizon; and 20 to 70 percent in the C horizon. Rock fragments are mostly sandstone but include siltstone and shale. Rock fragments include channers, cobbles, flagstones, and stones. Soils range from extremely acid through strongly acid throughout. (Source: NRCS Web Soil Survey).Wild material2159066NA 88675
33NA 88676RJL2023PA-010Staphylea trifolia L. Pennsylvania, United StatesNA2023COLLECTED10/25/2023Seed collected along the Appalachian National Scenic Trail, accessed from the Duncannon Entrance.40.38132600, -77.02965700103Well-drained and very rocky deciduous woodlands where soil has accumulated in part shade to full shade. Slope: 0-30%. Aspect: variable. The underlying geology of this area is of Devonian origin and characterized as the Duncannon Member of Catskill Formation. It is characterized by grayish-red sandstone, siltstone, and mudstone in fining-upward cycles; conglomerate occurs at base of some cycles. The sandstones which comprise the Duncannon Member are fine to very coarse grained and grayish red to grayish red-purple in color. The Duncannon Member is known to be crossbedded to planar bedded in beds anywhere from 3 to 9 meters thick. Conglomerates have been spotted at the base of the Duncannon Member. The Duncannon Member is poorly exposed in most areas except along the Lehigh River. The conglomerate portion of this member has been known to form ridges and ledges with thicknesses approaching 228 meters. (Source: USGS Pennsylvania Geologic Map Data). The primary soil type in the collection area is classified as Hazleton Series. The Hazleton series consists of deep and very deep, well drained soils formed in residuum of acid gray, brown or red sandstone on uplands. Slope ranges from 0 to 80 percent. Permeability is moderately rapid to rapid. Solum thickness ranges from 60 to 120 centimeters. Depth to lithic contact ranges from 1 to 2 meters. Rock fragments of angular sandstone, dominantly less than 25 cm in size, range from 5 to 70 percent in individual horizons. Boulders, stones, flags and channers cover about 5 to 60 percent of the surface of some pedons. Reaction ranges from strongly acid through extremely acid throughout. (Source: NRCS Web Soil Survey).Wild material2159067NA 88676
34NA 88678RJL2023PA-012Viburnum acerifolium L. Pennsylvania, United StatesNA2023COLLECTED10/27/2023Slopes on the east side of Creek Road above the North Branch of White Clay Creek.39.78552600, -75.8025190090Well-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 material2159069NA 88678
35Ames 36185APS/BP/2023/076/286Betula populifolia Marshall Indiana, United StatesNC7LEAF2023COLLECTED11/02/2023Indiana Dunes State Park just 3.40 miles northeast of Chesterton, T37N R5W NE 1/4 SE 1/4 SW 1/4 Sec. 1841.65352700, -87.03831500186Low depressions with some standing water. Woodland edge.Wild materialRepresents a disjunct population in northwest Indiana and the extreme western edge of the species native range. Trees sampled in nature averaging 30-45' in height with trunks ranging from 3" up to 8" DBH. Bark dull-white to grey. Typically multi-stemmed trunks. Leaves with acuminate tips and branches with typically one male catkin at terminal end of branches, but occassionally two male catkins. 2159042Ames 36185
36NA 88667RJL2023PA-004Viburnum acerifolium L. Pennsylvania, United StatesNA2023Wild material2158816NA 88667
37NA 88666RJL2023PA-003Hamamelis virginiana L. Pennsylvania, United StatesNA2023COLLECTED10/01/2023Collected primarily along the woodland edge along Northside Road on Pennsylvania State Gamelands No. 43 as well as a few on nearby roads.40.17974200, -75.76790700176Plants were growing in mesic well-drained conditions on moderately sloping sites of a deciduous upland forest. This species grows well in shade to part-sun. Most abundant fruit development is found where plants are exposed to sunlight for a portion of the day. Slope: 15%. Aspect: North-northwest. The underlying geology of this area is of Precambrian origin and characterized as the Graphitic Felsic Gneiss. This includes Pickering Gneiss and small areas of marble; dominantly quartz and feldspar with varying amounts of graphite and various metamorphic minerals; medium grained, light to dark gray and greenish gray; sedimentary origin. (Source: USGS Pennsylvania Geologic Map Data.) The primary soil type in the area of this collection is classified as Gladstone Gravelly Loam Series (8 to 15 percent slopes). The Gladstone Series consists of very deep, well drained soils formed in residuum and colluvium from granitic gneiss. Saturated hydraulic conductivity is moderately high to high. Solum thickness ranges from 75 to 125 cm. Depth to granitic gneiss bedrock is 1.6 meters or more. The bedrock may be strongly weathered in the upper part. Gravel content ranges from 5 to 35 percent throughout the solum, and 10 to 40 percent in the C horizons. Fragments, larger than 3 inches in diameter, range from 0 to 20 percent by volume in the surface layer and 0 to 10 percent in the subsoil and substratum layers. Reaction is strongly or very strongly acid throughout the soil, unless limed. Areas that have been limed range to moderately acid in the upper part of the profile. (Source: NRCS Web Soil Survey.)Wild material2158815NA 88666
38NA 88665RJL2023PA-002Ilex verticillata (L.) A. Gray Pennsylvania, United StatesNA2023COLLECTED10/01/2023Woodlands along Pine Creek near the Harmonyville Road bridge.40.18764500, -75.76732200141Moist to mucky, wet woodland conditions along Pine Creek. Much of the site is very wet due to recent rains; though, earlier in the year, the soils were only moist. Plants grow in both well-drained mesic conditions as well as seasonally wet conditions. They do not grow in standing water anywhere in this location. Plants in this population are found mostly in the shade and partial shade of deciduous trees; there are occasional gaps that offer higher light conditions as well. Slope: 0-2%. Aspect: N/A. The underlying geology of this area is of Precambrian origin and characterized as the Graphitic Felsic Gneiss. This includes Pickering Gneiss and small areas of marble; dominantly quartz and feldspar with varying amounts of graphite and various metamorphic minerals; medium grained, light to dark gray and greenish gray; sedimentary origin. (Source: USGS Pennsylvania Geologic Map Data). The primary soil type in the area of this collection is classified as Hatboro Silt Loam Series. The Hatboro Series consists of very deep and poorly drained soils formed in alluvium derived from metamorphic and crystalline rock. They are on flood plains. Slopes range from 0 to 3 percent. Saturated hydraulic conductivity is moderately high to high. Solum thickness ranges from 50 to 150 cm. Depth to bedrock ranges from 1.5 to 3 meters or more. Organic carbon decreases irregularly with depth or is greater than 0.2 percent directly above any strongly contrasting C horizon. The depth to strongly contrasting sand and gravel is more than 100 cm or the transition is greater than 12.5 cm. Content of gravel ranges from 0 to 10 percent in the solum and from 0 to 80 percent in the C horizon. Mica flakes are common in the solum, and the C horizon contains thin lenses of mica. Reaction ranges from very strongly acid through neutral to a depth of 75 cm and from moderately acid through slightly acid below 75 cm. (Source: NRCS Web Soil Survey.)Wild material2158814NA 88665
39NA 88664RJL2023PA-001Viburnum acerifolium L. Pennsylvania, United StatesNA2023COLLECTED10/01/2023Seed collected from plants growing along a two-mile stretch of Harmonyville Road on the woodland edge next to the road. [Note: latitude and longitude were collected at the location of the largest seed collection.]40.18482200, -75.78145100158Plants were growing in well-drained and rocky mesic-dry woodlands from part shade along the road edge to full shade in the understory of the woodlands. Slope: 2-10%. Aspect: Variable. The underlying geology of this area is of Triassic origin and characterized as the Stockton Formation. It is characterized by light-gray to buff, coarse-grained, arkosic sandstone; includes reddish-brown to grayish-purple sandstone, siltstone, and mudstone. (Source: USGS Pennsylvania Geologic Map Data.) The primary soil type in the area of this collection is classified as Edgemont Channery Sandy Loam Series (8 to 25 percent slopes), extremely stony. The Edgemont Series consists of deep and very deep, well drained soils formed in the weathered residuum of quartzitic rocks. They have moderately high to high saturated hydraulic conductivity. Slopes range from 0 to 70 percent. Solum thickness ranges from 50 to 10 cm. Depth to bedrock ranges from about 1.5 to 2.2 meters. Kaolinite is the dominant mineral in the clay fraction with detectable amounts of illite, vermiculite, montmorillonite, chlorite and interstratified clays. Gravel, channers, and stone size fragments of quartzite and quartz are present throughout the profile. Rock fragments range from 5 to 40 percent in the horizons of the solum and from 10 to 90 percent in the C horizon. Reaction ranges from extremely acid to strongly acid throughout. (Source: NRCS Web Soil Survey.)Wild material2158813NA 88664
40NA 89008WLP 3120Morus rubra L. Kentucky, United StatesNA2023COLLECTED06/05/2023Swan Pond Bottom. Riparian buffer and historic floodplain of Cumberland River, approximately 4 river miles downstream of Wolf Creek Dam.36.90259500, -85.13557900Riparian buffer and historic river floodplain. Slope: <5%. Aspect: North.Wild material2158092NA 89008
41Ames 36139Berea College ForestMorus rubra L. Kentucky, United StatesNAPLANT2023COLLECTED05/31/2023Between West and East Pinnacles of Berea College Forest just 3.25 miles east, southeast of Berea37.55656100, -84.23777600338Mid-lower slopes of moist, deciduous woods.Wild materialSpecies rather abundant throughout site with little to no presence of Morus alba. Majority of specimens noted measuring 8" DBH or smaller. Largest specimen noted reaching approximately 60' in height. 2158344Ames 36139
42NA 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
43NA 88514RJL2022MD-019Kalmia latifolia L. Maryland, United StatesNA2022COLLECTED11/04/2022Plants are growing on both sides of a fire road on Maryland Heights along the edge with Harpers Ferry National Historic Park. This location was accessed from the east where Miller Avenue meets the fire road, approximately 2 kilometers away. There is no vehicular access to the collecting area. Becoming locally uncommon. This local population is likely to be extirpated in the next 20-30 years. This collector has hiked through this area for more than 35 years and seen dramatic changes in the population. When first observed, Kalmia latifolia was a dominant understory shrub on south- to west-facing slopes beneath a mature forest canopy. Over the years, at least one forest fire has significantly reduced the population, along with a continuing increase in deer populations, resulting in catastrophic browse damage. The absence of a mature forest canopy and periods of drought have almost certainly also resulted in decline of this population. While collecting seed from scattered mature plants well above deer browse levels, this collector also noted that there was virtually no recruitment taking place.39.32811200, -77.72242400287Plants are growing in part-shade to shade of a deciduous upland, very rocky, and dry forest community. Plants are frequently found growing among boulders, rock outcrops, and steep-slope erosional areas, although, not exclusively.
Soils: The underlying geology of this area is of Late Cambrian to Cambrian origin and comprised of Chilhowee Group; Weverton Formation. This includes interbedded white to dark gray, thin-bedded, micaceous, ferruginous, and sericitic quartzites, phyllites, and white, thick-bedded, ledge-making quartzites; some gray to brown ferruginous quartz conglomerate and purple-banded phyllite.
Source: USGS Maryland Geologic Map Data https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=MDKp%3B5
The primary soil types in the collection area are classified as Dekalb-Bagtown-Rock outcrop complex, 25 to 65 percent slopes. The Dekalb series consists of moderately deep, excessively drained soils formed in material weathered from gray and brown acid sandstone in places interbedded with shale and graywacke. Slope ranges from 0 to 80 percent. Permeability is rapid. Solum thickness and depth to bedrock range from 50 to 100 cm. Flat, subangular or angular, sandstone fragments, 2.5-25 cm across increase with depth and range from 10-60 percent in individual horizons of the solum and from 50-90 percent or more in the C horizon. The amount of rock fragments typically increases with depth. Cobbly, channery, and very stony phases are common. Reaction ranges from extremely through strongly acid.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2139821NA 88514
44WLP 2670RJL2022PA-016Acer negundo L. Pennsylvania, United StatesNA2022COLLECTED10/21/2022Plants 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. Plants are found regularly but scattered in the understory of the woodlands. 39.80426000, -75.82609300105Plants growing in a mesic, well-drained habitat of deciduous woodlands along streams and above the riparian zone that drains toward a small unnamed creek that feeds into the Middle Branch White Clay Creek. Plants generally grow in part shade to full sun, but perform best and fruit more heavily in full sun where there is abundant access to moisture. 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. Despite this fact, Acer negundo is highly competitive and competes well.
Soils: The underlying geology of this area is the Glenarm Wissahickon Formation of lower Paleozoic origin and lithologically similar to oligoclase-mica schist of the Wissahickon Formation (PZw), but also includes lenticular amphibolite bodies having ocean-floor basalt chemistry.
Source: USGS Pennsylvania Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=PAPZgw%3B0)
The primary soil type in the area of this collection is classified as Glenelg silt loam, 3 to 8 percent slopes. 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.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2139661WLP 2670
45NA 89047RJL2022PA-015Cephalanthus occidentalis L. Pennsylvania, United StatesNA2022COLLECTED10/09/2022Plants growing in the floodplain of Octoraro Creek near 698 Lees Bridge Road, West Nottingham Township, Pennsylvania on the south side of the road. Plants are locally common and spread out in the floodplain area along the Octoraro Creek. 39.73540700, -76.0922650060Plants of this species are growing in full sun to part shade of a moist to seasonally mucky and wide flood plain area adjacent to Octoraro Creek. The area is dominated by deciduous herbaceous plants, scrambling vines, shrubs and occasional small trees. Much of this wet “meadow” is dominated by aggressive stands of grasses and members of the sedge family.
Soils: The underlying geology of this area is estimated to be of lower Paleozoic origin and comprised of Peters Creek Schist. This is comprised of chlorite-sericite schist containing interbedded quartzite. Interestingly, this area is very close to and may interface with the adjacent formation of Ultramafic Rocks that includes serpentine, steatite, and other products of alteration of peridotites and pyroxenites.
Source: USGS Pennsylvania Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=PAPZpc%3B0)
The primary soil types in the collection area are classified as Hatboro Silt Loam which consists of soils formed in alluvium derived from metamorphic and crystalline rock. They are on flood plains. Slopes range from 0 to 3 percent. Hatboro Silt Loam soils are poorly drained and have a high to very high surface runoff index. These soils are subject to periodic stream overflow, which usually occurs during the winter and spring months. The A and B horizons are moderately acidic to neutral, generally to a depth of 1-2 meters; the C horizon below ranges from a depth of 2-3 meters with uniformly acidic soils.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2139612NA 89047
46NA 89046RJL2022PA-014Alnus serrulata (Aiton) Willd. Pennsylvania, United StatesNA2022COLLECTED10/09/2022Plants growing in the floodplain of Octoraro Creek near 698 Lees Bridge Road, West Nottingham Township, Pennsylvania on the south side of the road. Plants are locally common and spread out in the floodplain area along the Octoraro Creek. 39.73579900, -76.0923830060Plants of this species are growing in full sun of a moist to seasonally mucky and wide flood plain area adjacent to Octoraro Creek. The area is dominated by deciduous herbaceous plants, scrambling vines, shrubs and occasional small trees. Much of this wet “meadow” is dominated by aggressive stands of grasses and members of the sedge family.
Soils: The underlying geology of this area is estimated to be of lower Paleozoic origin and comprised of Peters Creek Schist. This is comprised of chlorite-sericite schist containing interbedded quartzite. Interestingly, this area is very close to and may interface with the adjacent formation of Ultramafic Rocks that includes serpentine, steatite, and other products of alteration of peridotites and pyroxenites.
Source: USGS Pennsylvania Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=PAPZpc%3B0)
The primary soil types in the collection area are classified as Hatboro Silt Loam which consists of soils formed in alluvium derived from metamorphic and crystalline rock. They are on flood plains. Slopes range from 0 to 3 percent. Hatboro Silt Loam soils are poorly drained and have a high to very high surface runoff index. These soils are subject to periodic stream overflow, which usually occurs during the winter and spring months. The A and B horizons are moderately acidic to neutral, generally to a depth of 1-2 meters; the C horizon below ranges from a depth of 2-3 meters with uniformly acidic soils.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2139611NA 89046
47NA 89045RJL2022PA-013Tsuga canadensis (L.) Carrière Pennsylvania, United StatesNA2022COLLECTED10/07/2022Plants growing on the steep banks along Octoraro Creek accessed by canoe. Plants are locally common but generally infrequent along the Octoraro Creek. 39.74442700, -76.0885640066Plants are growing in part-shade to sun of mixed deciduous and evergreen forests on steep rocky habitats overlain by relatively deep soil over occasionally exposed geology along the Octoraro Creek.
Soils: The underlying geology of this area is estimated to be of lower Paleozoic origin and comprised of Peters Creek Schist. This is comprised of chlorite-sericite schist containing interbedded quartzite.
Source: USGS Pennsylvania Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=PAPZpc%3B0)
The primary soil types in the collection area are classified as Manor loam, 25 to 35 percent slopes, very stony. The soils in the collecting area originated as residuum, weathered from the micaceous schist exposed geology and are generally considered coarse-loamy, micaceous, mesic typic dystrudepts that are very acidic and well-drained. There is a variable depth of soil depending upon the steepness of slopes. Some areas contain significant exposed Peters Creek Schist overlain by a highly decomposed organic mat intermingled with a dense root mat of woody and herbaceous plants.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2139610NA 89045
48NA 89044RJL2022PA-012Rhododendron maximum L. Pennsylvania, United StatesNA2022COLLECTED10/07/2022Plants growing on the steep banks along Octoraro Creek accessed by canoe. Plants are locally common but generally uncommon along the Octoraro Creek. 39.75272200, -76.0827150063Plants are growing in part-shade to part-sun of mixed deciduous and evergreen forests on steep rocky habitats along the Octoraro Creek.
Soils: The underlying geology of this area is estimated to be of lower Paleozoic origin and comprised of Peters Creek Schist. This is comprised of chlorite-sericite schist containing interbedded quartzite.
Source: USGS Pennsylvania Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=PAPZpc%3B0)
The primary soil types in the collection area are classified as Manor loam, 25 to 60 percent slopes, very stony. The soils in the collecting area originated as residuum, weathered from the micaceous schist exposed geology and are generally considered coarse-loamy, micaceous, mesic typic dystrudepts that are very acidic and well-drained. There is a variable depth of soil depending upon the steepness of slopes. Some areas contain significant exposed Peters Creek Schist overlain by a highly decomposed organic mat intermingled with a dense root mat of woody and herbaceous plants.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2139609NA 89044
49NA 88488RJL2022PA-004Viburnum acerifolium L. Pennsylvania, United StatesNA2022COLLECTED09/03/2022Plants growing in woodlands on the east side of Shed Road in French Creek State Park. Plants are common and found scattered along the edges of the road and into the woodlands. 40.21969200, -75.77373600238Plants are growing in a mesic to dry, well-drained habitat of upland deciduous forest which is very rocky. The understory layer is generally not as rich due to the rock-laden ground layer. Plants are growing in part shade to shade. The underlying geology of this area is comprised of Hammer Creek Conglomerate, characterized by cobble and pebble quartz conglomerate interbedded with red sandstone.
Source: USGS Pennsylvania Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=PATRhc%3B2) The surface soil profile of this area is Joanna Loam (JpD), 8 to 25 percent slopes which is extremely stony. It is represented by residuum weathered from sandstone and/or residuum weathered from conglomerate. Joanna Loam is moderately to well-drained and 1.8 meters to 2.5 meters to the lithic bedrock described above.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2139367NA 88488
50WLP 26142022VA-05Euonymus americanus L. Virginia, United StatesNA2022COLLECTED09/12/2022In Colonial Williamsburg, park in the Providence Hall Directors Wing parking lot and enter the Bassett Trace Nature Trail; this species is found in the woodlands on either side of the trail and over a bridge until the it turns right. This plant is infrequent, but occasionally found in the mesic woodlands throughout this location.37.26681600, -76.6925280021Plants growing in shade to part-shade of the mixed deciduous and evergreen mesic woodland. This species is generally growing in areas with an abundant organic, mature woodland that is relatively undisturbed.
The underlying geology of this area is Windsor Formation of Tertiary-Quaternary origin (lower Pleistocene or upper Pliocene). It is comprised of gray and yellowish- to reddish-brown sand, gravel, silt, and clay. It constitutes surficial deposits of extensive plain and fluvial-estuarine terraces above elevations of 10 meters. The thickness of the Windsor Formation is 0 to 12.5 meters.
Source: USGS Virginia Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=VAQTw%3B0)
The surface soil profile of this area is Emporia Complex, 15 to 25 percent slopes. This soil as moderately well-drained, acidic, and found on sloping and elevated terraces. They are comprised of fine sandy loam, loam, and sandy clay 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 material2139352WLP 2614
51NA 88464NCBG-372Viburnum nudum L. Virginia, United StatesNA2021Wild materialBRIGHT BLUE DRUPES2132870NA 88464
52NA 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
53WLP 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
54WLP 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
55WLP 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
56WLP 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
57W6 58997NCBG-445Glyceria striata (Lam.) Hitchc. Maryland, United StatesW62021Wild materialdrooping inflorescence2116315W6 58997
58WLP 121103Hydrangea arborescens L. Kentucky, United StatesNA2020COLLECTED10/14/2020Powell County; Natural Bridge State Park along Powell County; Natural Bridge State Park along the Whittleton Branch trail between Whittleton Branch Campground and KY 1537.78466700, -83.66700000257Along hiking trial growing in seeps along rock walls and rocky slopesWild material2110297WLP 121
59WLP 92101Euonymus americanus L. Kentucky, United StatesNA2020COLLECTED10/14/2020Powell County; Natural Bridge State Park along the Whittleton Branch trial between Whittleton Branch campground and KY1537.78450000, -83.66805556264Floodplain and streambank slopesWild material2 vouchers made2109486WLP 92
60NA 88465F012Viburnum dentatum L. Pennsylvania, United StatesNA2020COLLECTED09/06/2020J. Edward Mack Boy Scout Camp near Brickerville, PA: located between old logging road and power lines. [Longitude was entered incorrectly and has been estimated; it needs to be confirmed with original data.]40.26002778, -76.32097200Wild material2109476NA 88465
61NA 88467F014Viburnum prunifolium L. Pennsylvania, United StatesNA2020COLLECTED09/24/2020J. Edward Mack Boy Scout Camp near Brickerville, PA.40.25944000, -76.32416600Near power lines, mostly on western slopes.Wild material2109478NA 88467
62NA 88471F019Cephalanthus occidentalis L. Pennsylvania, United StatesNA2020COLLECTED10/04/2020Camp Rocky Creek (YMCA), Cornwall/Lebanon, PA. [originally listed as Camp Shand.]40.24500000, -76.39750000Marshy area.Wild material2109483NA 88471
63NA 88472F020Ilex verticillata (L.) A. Gray Pennsylvania, United StatesNA2020COLLECTED10/04/2020Camp Rocky Creek (YMCA), Cornwall/Lebanon, PA. [originally listed as Camp Shand.]40.24944400, -76.38666000Marshy area along power line cut.Wild material2109484NA 88472
64NA 88473F021Viburnum dentatum L. Pennsylvania, United StatesNA2020COLLECTED09/29/2020Camp Rocky Creek (YMCA), Cornwall/Lebanon, PA. [originally listed as Camp Shand.]40.24944400, -76.38666000Marshy area along power line cut.Wild material2109485NA 88473
65WLP 2054MARSB-1023Viburnum nudum L. New York, United StatesNA2020COLLECTED12/19/2019Orange County; Warwick; West St, on residential property.61Wet meadow in full sun; growing in moist loamy sand.Seeds collected from 35+ individuals in a population of 50+ individuals, growing over an area 500 meters by 500 meters in size. Common. Seed maturation: late.2109215WLP 2054
66WLP 2026MARSB-993Viburnum acerifolium L. New York, United StatesNA2019COLLECTED09/06/2019Tompkins County; ; Cornell Botanical Gardens: Cayuga Monkey Run Trail.42.45601000, -76.45154000Hillside forest in full shade; growing in moist, well-drained silt/clay soil.Seed harvested from 10+ individuals in a population of 40+. Common. Seed 85 percent healthy; seed maturation middle, late.2109175WLP 2026
67WLP 2031MARSB-998Viburnum acerifolium L. New York, United StatesNA2019COLLECTED09/20/2019Monroe County; Perinton; Horizon Hill Conservation Area [side of Interstate 490 west, alongside Bushnell's Basin exit (Exit 27).]43.04778000, -77.46235000189Oak/hickory forest in partial shade; growing in moist, well-drained loam soil.Seeds collected from 40 individuals in a population of 100 plants spread across a 60 m by 60 m area; scattered distribution. 95 percent healthy seed. Seed maturation: middle.2109180WLP 2031
68WLP 2034MARSB-1001Viburnum acerifolium L. New York, United StatesNA2019COLLECTED07/08/2019Dutchess County; Tivoli; Bard College campus.122Oak woodland in partial shade; growing in dry loamy sand.Seeds collected from 75 individuals in a population of 100+ plants spread across a ca 1 square mile area; common. Seed maturation: late.2109183WLP 2034
69WLP 2035MARSB-1002Viburnum acerifolium L. New York, United StatesNA2019COLLECTED09/05/2019Dutchess County; Barrytown; Rokeby Rd. [Locality not recorded, but inferred from similarity of other data, including recorded landowner, to MARSB-1006/MARSB_MM_015/NA 86371. -SBL]91Oak-hickory woodland in partial shade; g rowing in dry loam soil.Seeds collected from 50+ individuals in a population of 100+ plants; common. Seed maturation: middle. Birds & herbivory, low fruit set noted.2109184WLP 2035
70WLP 2036MARSB-1003Viburnum opulus L. var. americanum Aiton New York, United StatesNA2019COLLECTED08/30/2019Columbia County; Germantown; Rt. 9 (9G?)/Main St. right-of-way, Germantown.183Roadside right-of-way in full sun; growing in moist loamy sand.Seeds collected from 40 individuals in a population of 50+ plants occurring over an area 300 meters by 500 meters in size; common. Seed maturation: middle.2109185WLP 2036
71WLP 2039MARSB-1006Viburnum lentago L. New York, United StatesNA2019COLLECTED09/19/2019Dutchess County; Barrytown; Rokeby Rd.122Edge of ditch along oak forest parcel in full sun; growing in moist clay-loam soil.Seeds collected from 20 individuals in a population of 50+ plants; common. Seed maturation: middle.2109188WLP 2039
72WLP 2043MARSB-1012Viburnum opulus L. var. americanum Aiton New York, United StatesNA2019COLLECTED08/30/2019Dutchess County; Rhinebeck; Rt. 9 right-of-way, on border of Red Hook and Rhinebeck.183Roadside right-of-way in partial shade; growing in moist loamy sand.Seeds collected from 15 to 20 individuals in a population of 15 to 20 individuals, growing over an area 300 meters by 300 meters in size. Scattered distribution. Seed maturation: middle.2109192WLP 2043
73NA 88146NCBG-309Aralia spinosa L. Virginia, United StatesNASEED2019Wild material2098406NA 88146
74W6 57474NCBG-294Mikania scandens (L.) Willd. Maryland, United StatesW6SEED2019Wild material2098398W6 57474
75W6 57549NCBG-566Parthenocissus quinquefolia (L.) Planch. Maryland, United StatesW6SEED2019Wild material2098473W6 57549
76W6 57551NCBG-578Saururus cernuus L. Maryland, United StatesW6SEED2019Wild material2098475W6 57551
77W6 57388NEWFS-288Carex crinita Lam. Massachusetts, United StatesW6SEED2019Wild material2098185W6 57388
78W6 57168MARSB-389Ageratina altissima (L.) R. M. King & H. Rob. Delaware, United StatesW6SEED2019Wild material2097607W6 57168
79WLP 2016F008Viburnum acerifolium L. Pennsylvania, United StatesNA2019COLLECTED09/30/2019Lancaster County; Poplar Grove (Elizabeth Township); Along Horshoe Trail (hiking area) east of US 322.40.24250000, -76.33466000Large population, little seed.2109122WLP 2016
80WLP 2003MARSB-968Viburnum dentatum L. New York, United StatesNA2019COLLECTED08/04/2019Ulster County; Gardiner; Private residence at 844 Route 208, Gardiner, New York 12525.41.65848000, -74.14236000122Forest, marsh/pond shore in partial to full shade; poorly drained, clay loam soil, seasonally wet/moist.Seeds collected from plant. Many seeds had already dropped or been eaten; seeds collected from an approximately 1 acre (or 4000 square meters) area with Viburnum dentatum growing in several dense patches and sparsely between. Species common, scattered in area; 100-plus individuals estimated in approximately 4000 square meters.2109099WLP 2003
81WLP 2015F006Viburnum dentatum L. Pennsylvania, United StatesNA2019COLLECTED09/12/2019Lebanon County; South Lebanon Township; 40.25505000, -76.35025000Large population; little seed set. Heavy viburnum leaf beetle damage.2109113WLP 2015
82Ames 35216Potato Creek SPMonarda sp.Indiana, United StatesNC7Flower2019COLLECTED09/02/2019Potato Creek State Park located approximately 2.6 miles northeast of North Liberty, T36N R1E extreme eastern edge of NW 1/4 SW 1/4 Sec. 23.41.55439400, -86.38375900222Degraded floodplain, along sides of elevated road bed.Wild materialThis taxa is currently undescribed and according to Campbell and Medley in The atlas of vascular plants in Kentucky (Accessed 06 September 2019) was provisionally named Monarda serotina by R.T. Simmers. Described as a broad-leaved form of M. fistulosa, generally intermediate between M. fistulosa and M. clinopodia, with probable hybrid origin. Typcial habitat is mesic woods and edges on lowlands. In contrast to M. fistulosa, this taxon has longer petioles (usually 2-3 cm versus 0.5-2.0 cm), lower leaf surfaces with scattered spreading hairs, and corollas are paler pink at tips to almost white with peak flowering occurring prior to M. fistulosa by approximately 1-2 weeks. Leaves are rather rugose, where upper leaf tissue between veins is visibly raised. This accession represents genetics from northern Indiana (Potato Creek State Park). Plants at the collection site in nature peaked flowering near 8 July 2019 where flower colors were more lavender in sun but pale in shade (Namestnik, S., personal communication, 15 July 2020). Peak fruiting occurs mid-August. Average height of plants sampled in nature estimated at 4.5' in height.2097752Ames 35216
83NA 88062NEWFS-233Clethra alnifolia L. Massachusetts, United StatesNASEED2019Wild material1976185NA 88062
84W6 54032MARSB-287Carex crinita Lam. New Jersey, United StatesW6SEED2018Wild materialCarex crinita1964748W6 54032
85W6 54033MARSB-288Carex lurida Wahlenb. New Jersey, United StatesW6SEED2018Wild materialCarex lurida1964749W6 54033
86WLP 1980MARSB-795Viburnum acerifolium L. New Jersey, United StatesNA2017COLLECTED08/29/2017Morris County; ; Hacklebarney State Park; all trails in park.40.74913000, -74.72916000153Upland hardwood forest; hills. Loam soil (Parker series). Land used for conservation and recreation.Seeds collected from 75 plants; 400+ plants found in an area of 40 acres. Population is present and spread out throughout park along all trails. One herbarium voucher collected on 29 Aug. 2017; held at Smithsonian. Material identified by Clara Holmes from pressed specimen on 16 Nov. 2017. Ecoregion: 58E -- Northeastern Highlands (Omernik).2108824WLP 1980
87WLP 1981MARSB-797Viburnum acerifolium L. New Jersey, United StatesNA2017COLLECTED09/07/2017Morris County; ; Berkshire Wildlife Management Area: Gordon Road. [From Roxbury fire Co. 3, drive west for 1,500 feet to the end of Gordon Road. Take trail that leads North on foot. Population is spread evenly throughout the WMA.]40.91772000, -74.62291000247Upland hardwood forest; ground moraines. Coarse loam soil (Rockaway series). Land used for conservation and recreation.Seeds collected from 100 plants; 500 plants found in an area of 50 acres. Population is spread evenly throughout the wildlife management area. One herbarium voucher collected on 9 Sep. 2017; held at Smithsonian. Material identified by Clara Holmes from pressed specimen on 16 Nov. 2017. Ecoregion: 58E -- Northeastern Highlands (Omernik).2108825WLP 1981
88Ames 33990JDC/FQ/2017/046/800Fraxinus quadrangulata Michx. Ohio, United StatesNC7SEED2017COLLECTED07/15/2017Sharon Woods Metro Park within city limits of Columbus, T2N R18W, Franklin County40.12267100, -82.96668000275Deciduous woods.Wild material1950073Ames 33990
89Ames 33288APS/GD/2016/009/244Gymnocladus dioicus (L.) K. Koch Michigan, United StatesNC7Fruit2016COLLECTED04/05/2016Ottawa County: T7N R13W SW 1/4 SW 1/4 NE 1/4 Sec. 32; T7N R13W NE 1/4 NE 1/4 SW 1/4 Sec. 29; and T7N R14W NW 1/4 NW 1/4 Sec. 10 along Grand River both north (approximately 2.87 miles) and east (approximately 3.84 miles) of Allendale.43.00148000, -85.91236400184Floodplain. Wild material1940345Ames 33288
90Ames 33289APS/GD/2016/010/245Gymnocladus dioicus (L.) K. Koch Michigan, United StatesNC7Fruit2016COLLECTED04/05/2016Ionia County: T5N R5W SW 1/4 SW 1/4 SE 1/4 Sec. 21; T5N R5W NE 1/4 NW 1/4 NW 1/4 Sec. 20; and T5N R5W SW 1/4 SW 1/4 SE 1/4 Sec. 20 along Grand River approximately 4.80 miles south and slightly west of Portland.42.80296200, -84.91275400231Floodplain. Wild material1940346Ames 33289
91WLP 1098JDC/CO/2015/030/686Cotinus obovatus Raf. Arkansas, United StatesNAPLANT2015COLLECTED05/20/2015T18N R15W NW 1/4 Sec. 15 and SE 1/4 Sec. 10 Marion County. Hall Mountain area along County Road 6074.36.20574400, -92.56150900239Rocky, very shallow soils. Growing in association with Quercus muehlenbergii, Juniperus virginiana, Acer saccharum, Cercis canadensis, Lindera benzoin, Diospyros virginiana, Silphium terebinthinaceum, Baptisia sp., Rudbeckia sp., and Rhus glabra.Wild material1926260WLP 1098
92Ames 32892APS/GD/2015/014/196Gymnocladus dioicus (L.) K. Koch Oklahoma, United StatesNC7Fruit2015COLLECTED03/13/2015Wagoner County: Billy Creek watershed, T17N R17E NE 1/4 Sec. 22. McClellen-Kerr Wildlife Management Area (Billy Creek WDU) portion approximatley 4 miles west, southwest of Wagoner.35.94442000, -95.48112700171Floodplain.Wild material1925358Ames 32892
93Ames 32886APS/GD/2015/002/184Gymnocladus dioicus (L.) K. Koch Missouri, United StatesNC7Fruit2015COLLECTED03/03/2015Douglas County: North Fork River watershed, T26N R12W Sec. 13. Private property approximately 5.3 miles east, southeast of Vanzant.36.93971400, -92.21469500264Floodplain. Riverbank in pure sand.Wild material1924364Ames 32886
94Ames 32887APS/GD/2015/003/185Gymnocladus dioicus (L.) K. Koch Arkansas, United StatesNC7Fruit2015COLLECTED03/04/2015Stone and Izard Counties: White River watershed, Ozark National Forest, Sylamore State Wildlife Management Area near Allison.35.95017300, -92.11129600126Floodplain, base of slopes.Wild material1924365Ames 32887
95NA 83061ZARKS-005Gymnocladus dioicus (L.) K. Koch Arkansas, United StatesNA2015COLLECTED10/02/2014Frog Valley (private property). West bank of North Fork of Saline River.34.76276000, -92.71386000133Alluvial low floodplain, in sandy clay soil. Slope: 0 degrees. Elevation: 435 feet.Wild material1950627NA 83061
96NA 83062NA 83062Taxodium distichum (L.) Rich. Arkansas, United StatesNA2015COLLECTED10/02/2014Frog Valley (private property). Banks of North Fork of Saline River.34.76443000, -92.71338000135Alluvial low floodplain, in gravel bank.1951432NA 83062
97NA 83063NA 83063Hamamelis vernalis Sarg. Arkansas, United StatesNA2015COLLECTED10/02/2014Frog Valley (private property). Gravel bar along North Fork of Saline River.34.76543000, -92.71353000134Alluvial low floodplain; gravel bar.1950887NA 83063
98W6 48819MARSB-101Boehmeria cylindrica (L.) Sw. Maryland, United StatesW6SEED2015Wild material1922836W6 48819
99W6 48853MARSB-102Eragrostis spectabilis (Pursh) Steud. Maryland, United StatesW6SEED2015Wild material1922857W6 48853
100Ames 32080JDC/FQ/2013/039/483Fraxinus quadrangulata Michx. Indiana, United StatesNC7SEED2013COLLECTED08/16/2013Bock Nature Preserve, Section 7, T30N, R5E, Akron Quad, near Akron, Kosciusko County.41.06352100, -86.01666100274Mesic forest. Wild material1913266Ames 32080
101Ames 31992APS/GD/2013/017/102Gymnocladus dioicus (L.) K. Koch Kentucky, United StatesNC7FRUIT2013COLLECTED03/04/2013Dinsmore Woods, Boone County.38.99959500, -84.81492800189Base of south-facing bluff.Wild material1908270Ames 31992
102Ames 31998APS/GD/2013/026/111Gymnocladus dioicus (L.) K. Koch Indiana, United StatesNC7FRUIT2013COLLECTED03/07/2013Tunnelton, Lawrence County.38.76121800, -86.35236900179East Fork White River Watershed. Mid-elevation of east-facing limestone bluffs. Wild material1908276Ames 31998
103Ames 30488APS/GD/2010/009/044Gymnocladus dioicus (L.) K. Koch Kentucky, United StatesNC7FRUIT2010COLLECTED02/21/2010Alum Hill and Big Slough Creek, near Hites Falls, Grayson County.37.53600000, -86.59630000159Floodplain of Big Slough and base of bluffs on northeast-facing slope of Alum Hill.Wild material#140 measured 12" d.b.h. at 70', #141 measured 8.5" d.b.h. and 40', #142 measured 12" and 80', #143 measured 9.5" and 60', #144 measured 7.5" d.b.h. and 40', #145 measured 12" d.b.h. and 40', #146 measured 7.3" d.b.h. and 50', and #147 measured 14.25" d.b.h. and 75'.1831347Ames 30488
104Ames 30489APS/GD/2010/010/045Gymnocladus dioicus (L.) K. Koch Kentucky, United StatesNC7FRUIT2010COLLECTED02/22/2010Yellowbank Wildlife Management Area, near Lick Run Creek, on Ammons Church Road and slope on Jays Lane, north of Ammons, Breckinridge County.37.96060000, -86.49880000130Northeast-facing slope.Wild material#148 measured 16.5" d.b.h. and 100', #149 measured 14.5" d.b.h. and 90', #150 measured 16" d.b.h. and 90', and #151 measured 18" d.b.h. and 80'.1831348Ames 30489
105Ames 30387JDC/PO/2009/104/254Physocarpus opulifolius (L.) Maxim. Ohio, United StatesNC7SEED2009COLLECTED10/17/2009Near Snake Hollow, Shawnee State Forest, Otway Quad, Scioto County.38.80166667, -83.15666667241Edges of rocky creek. Wild material1823939Ames 30387
106WLP 1413JDC/OA/2009/087/237Oxydendrum arboreum (L.) DC. Ohio, United StatesNA2009COLLECTED10/15/2009Near Lake Katherine, SW 1/4 of NW 1/4 of Section 13, T7N, R19W, Jackson Quad, Jackson County.39.08444444, -82.67833333225Lake edge. Associated with with Acer saccharum, Cornus florida, Lindera benzoin, Magnolia tripetela, Nyssa sylvatica, Sassafras albidum, and Tsuga canadensis.Wild material1823935WLP 1413
107WLP 1415JDC/OA/2009/103/253Oxydendrum arboreum (L.) DC. Ohio, United StatesNA2009COLLECTED10/17/2009Snake Hollow, Shawnee State Forest, Otway Quad, Scioto County.38.80722222, -83.15555556239Cool moist woods. Associated with with Carpinus caroliniana, Carya, Corylus americana, Fagus sylvatica, Lindera benzoin, Nyssa sylvatica, Picea abies, Platanus occidentalis, Sassafras albidum, Tsuga canadensis, and Viburnum dentatum.Wild material1823938WLP 1415
108Ames 28322JDC-0142006Betula pumila L. Michigan, United StatesNC7SEED2006COLLECTED10/04/2006Sarett Nature Preserve, 2300 Benton Center Road, Benton Harbor.42.15916667, -86.37944444180Full sun; no slope. Growing in standing water ~0-4 inches deep. Abundant population (>75) with uniform distribution. Wild materialSmall plants; approximately 3-7 feet in height. Yellow fall color.1711421Ames 28322
109Ames 28324JDC-0162006Physocarpus opulifolius (L.) Maxim. Michigan, United StatesNC7SEED2006COLLECTED10/04/2006Sarett Nature Preserve, just north of Benton Harbor, T3S R18W SE 1/4 SE 1/4 Sec. 34, Benton Heights Quad., Berrien County.42.15916667, -86.37944444180Floodplain of Paw Paw River. Full sun with no slope. Very wet soil; standing water approximately 0-4 inches deep. Occasional population abundance. Wild materialPlants 5-7 feet in height.1711424Ames 28324
110Ames 2773363Hypericum prolificum L. Arkansas, United StatesNC7SEED2004COLLECTED10/22/2004Ninestone Land Trust located off 973 County Road 512 approximately 9.5 miles south of Berryville36.22913300, -93.55131600403Grassy area above wet bog, beside open field. Eastern aspect.Wild materialShrubs with shedding, brown bark in nature measuring approximately 5-10 feet tall.1668192Ames 27733