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ACCESSIONPLANT NAMETAXONOMYORIGINGENEBANKIMAGEAVAILABILITYRECEIVEDSOURCE TYPESOURCE DATECOLLECTION SITECOORDINATESELEVATIONHABITATIMPROVEMENT LEVELNARRATIVE
0PI 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
1PI 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
2PI 64902146Actaea racemosa L. Missouri, United StatesNC72004Wild material1 meter tall.1668177PI 649021
3NA 89196KVRHamamelis virginiana L. Wisconsin, United StatesNA2025COLLECTED08/22/2024Kickapoo Valley Reserve.43.62650770, -90.64627490299Shade in thick, clayey, organic soil with sand. Slope: 45 degrees. Aspect: Northeast. Silver maple-boxelder-elm vegetative community.Wild material2171017NA 89196
4NA 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
5NA 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
6Ames 36193Mounds SPMonarda sp.Indiana, United StatesNC7LEAF2023COLLECTED09/17/2023Mounds State Park located approximately 3.15 miles east of Anderson, T19N R8E NE 1/4 Sec. 16.40.10142600, -85.62065300258Floodplain.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 central Indiana (Mounds State Park). Plants at the collection site in nature peaked flower 8 July (2023). Plants in nature generally reaching 1.0-1.3 meters in height with about 10 percent having stacked heads. Majority of plants unbranched. 2159165Ames 36193
7WLP 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
8NA 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
9NA 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
10WLP 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
11WLP 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
12WLP 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
13Ames 35750Ames 35750Blephilia ciliata (L.) Benth. Iowa, United StatesNC7FLOWER2021COLLECTED09/27/2021Located approximately 3 miles south, southeast of Fairfield, T71N R9W SW1/4 Sec. 740.96338000, -91.94686900223Woodland openings/edges, disturbed areasWild material2122068Ames 35750
14NA 86873QLG193Tsuga chinensis (Franch.) E. Pritz. Shaanxi Sheng, ChinaNA2021COLLECTED10/18/1996Ningxi Preserve, near Caiziping Forest Station town, behind the hospital valley33.73361111, 108.316944441855Very steep slope in a deep shaded woodland valley in a dry streambed with a heavy boulder field; 60% NW slope; growing w/ Asarum sp., Kerria japonica, Clematis sp., bamboo, Betula sp., Meliosma sp., Cimicifuga japonica and Alangium sp.Wild materialFull name as recorded at U.S. National Arboretum: Tsuga chinensis. Two plants picked up by USNA staff on 6/23/2021. Unaccessioned at Morris Arboretum (recorded with greenhouse number 2013x004); from cuttings of a single plant, MA 1996-535*B. Seven additional plants were received previously (10/15/2020) but unrecorded earlier; they will also be treated under this number. See NA 67823 for the original accession of this wild collection at USNA, as well as its decimal derivatives (plants grown from cuttings of NA 67823). Form received: rooted cutting.2155007NA 86873
15OPGC 7495CBG-9545Symphyotrichum shortii (Lindl.) G. L. Nesom Illinois, United StatesOPGCSEED2019Wild material2092813OPGC 7495
16Ames 33736JDC/BA/2016/028/743Betula alleghaniensis Britton Iowa, United StatesNC7BARK2016COLLECTED09/02/2016Fallen Rock State Preserve approximately 1.9 miles southwest of Steamboat Rock, T88N R19W NW ¼ Sec. 32.42.39459000, -93.09423600310High-quality, native, mesic deciduous woods on loose, loamy sandstone amongst very large boulders. North-facing with variable 10-50 degree slopes. Majority of specimens located at base of bluff or near water’s edge (Iowa River).Wild materialThe native range of Betula alleghaniensis is concentrated in the northeastern U.S. with disjunct populations in Iowa (Little, 1971). This accession represents a collection of Betula alleghaniensis germplasm from the extreme western edge of the species native range. The next closest occurrence is in Mitchell County, Iowa (60 miles). As of 2025, two trees at Fallen Rock State Preserve currently represent the state of Iowa's 1st and 2nd largest yellow birch specimens measuring 22.76" DBH; 70.83' height; 40' average crow spread (151.83 points) and 17.18" DBH; 65.33' height; 33.75' average crow spread (127.76 points), respectively (Rouw, M., personal communication, 13 May 2018). 1942689Ames 33736
17Ames 33357JDC/UT/2016/018/733Ulmus thomasii Sarg. Iowa, United StatesNC7SEED2016COLLECTED06/03/2016Malanaphy Springs State Preserve just northwest of Decorah, T99N R8W SW ¼ NW ¼ SE ¼ Sec. 3143.34713800, -91.83840000302Deciduous woods. Rocky substrate. 20 degree northwest-facing slopeWild materialUlmus thomasii (Rock elm) is an underutilized tree species both in conservation and in the urban landscape. Charles Sprague Sargent (first director of the Arnold Arboretum of Harvard University, Boston, MA) described the wood of Rock Elm as "heavy, hard, very strong and tough, closely grained, and susceptible of receiving a beautiful polish". Historically noted for a variety of uses in woodworking including furniture, heavy agricultural implements, timber frame buildings, pianos, hockey sticks, and hand tools. U. thomasii is extremely drought tolerant, adaptable to very calcareous soils, and compared to U. americana or U. rubra has a very conservative growth rate requiring minimal attention in regards to pruning. Rock elm naturally tends to develop into a nice structural specimen in the landscape, unlike other fast growing U. americana cultivars in the nursery trade needing frequent attention. Rock elm has very fissured bark and is well known for maintaining a strong central leader resulting in a very attractive, pyramidal form. Despite many literature sources stating that "wings" on the stems are a key identifiying characteristic, this trait is not reliable and many genotypes may completely lack "wings" on the stems. While growth habit and morphology of dormant buds (very pointy) are good traits to help aid in identification, fruits are the best way to confirm identity. Fruits are densly pubescent, often described as "inflated" and generally reach maturity a couple weeks after U. rubra and U. americana. U. thomasii flowering in central Iowa typically occurs the last week in April into the first week in May and are rather distinguishable from other Ulmus in being pendulous. Fruits are extremely prized treats for many birds, where fruits are often "robbed" prior to full maturity. Fruits are also highly prized by many other animals such as mice, squirrels, chipmunks, turkeys, etc. and are generally consumed within hours after fruit abscission. The native range of U. thomasii is concentrated in the northeastern United States and into Canada with disjunct populations documented in northwestern Missouri and northwestern Arkansas (Little, E. L. Jr. 1971). In the 1895 Silva of North America (vol. 7) it was stated that, “The value of the wood of the Rock Elm threatens its extinction and most of the large trees have already been cut.” Today, since rock elm is rather rare, especially in areas near the edges of its range, many states list the species as endangered or threatened warranting preservation efforts. This accession represents genetics from northeast Iowa (Winneshiek County). In an assessment of some of the largest Ulmus thomasii (native and cultivated) across Iowa, four of the nine largest specimens in Iowa are present in Malanaphy Springs State Preserve where this accession was sampled. The second largest U. thomasii in the state located in Malanaphy Springs was measured on 22 May 2020 with a circumference of 6.42', height of 86.58', and an average crown spread of 68.00' (180 points) (Rouw, M., personal communication, 8 February 2021).1940580Ames 33357
18WLP 1967HBC1401Viburnum opulus L. var. americanum Aiton North Dakota, United StatesNA2014COLLECTED09/29/2014Jay Wessels Wildlife Management Area located in Pembina County.48.80000000, -97.83000000312Diverse habitats including edge of swamp and also upland sandy soils. Growing in association Fraxinus pennsylvanica, Fraxinus nigra, Quercus macrocarpa, Acer negundo, Ulmus americana, Populus tremuloides, Populus balsamifera, Toxicodendron radicans, Cornus sericea, Rosa sp., Corylus sp., Prunus virginiana, Ribes sp., Equisetum sp., Rubus sp., IMpatiens capensis, Thalictrum dasycarpum, Fragaria virginiana, Asarum canadense, Calamagrostis canadensis, Sium suave, Solidago gigantea, Poa pratensis, and Bromus inermis.Wild material1921830WLP 1967
19Ames 31065354Diervilla lonicera Mill. New York, United StatesNC7SEED2011COLLECTED09/10/2011Along Emery Hill Road42.07700000, -79.08400000446Roadside. East-facing slope. Rocky substrate with very tiny spring creek at base of slope.Wild material1891451Ames 31065
20WLP 229NA 80349Tsuga canadensis (L.) Carrière New York, United StatesNA2011COLLECTED09/10/2011Along Emery Hill Road.42.07700000, -79.08400000433Roadside. East-facing slope. Rocky substrate with very tiny spring creek at base of slope. Associated with Acer saccharum, Asarum canadense, Diervilla lonicera, Fraxinus americana, Hamamelis virginiana, Impatiens capensis, Rubus, Solidago, and Tilia americana.Wild material1891488WLP 229
21Ames 30061JDC/CA/2009/015/165Cornus alternifolia L. f. Illinois, United StatesNC7SEED2009COLLECTED08/06/2009Southwest edge of Pierce Lake, Rock Cut State Park, SW 1/4 of SE 1/4 of Section 27, T45N, R2E, Caledonia Quad, Rockford, Winnebago County.42.34333333, -88.98638889259Rich woods. Wild materialUp to 20-30 feet in height.1812364Ames 30061
22Ames 25515WSYUS 22Euonymus verrucosus Scop. Chernihiv, UkraineNC7LEAF1999COLLECTED09/10/1999Near local forest station in forest north of Pryluky.50.69416667, 32.43444444160Within forest at the west edge. Very droughty area. Under shade of canopy, 0-1% slope. Sandy loam soil with good drainage. Wild materialPlants were frequently abundant. Leggy shrub of 3-5 feet, scattered in forest. Pollen yellow (4 stamens, sessile filament), sepal length 3mm and sepal width 5mm, petioule (flower) approximately 25-30 mm in length, petioule (leaf) approximately 4-5 mm in length, leaves approximately 50-65 mm in length and approximately 22-35 mm in width (widest point). with interesting pseudoleaves present (opposite arrangement) approximately 3-4 mm from flower ranging in length from 3-4 mm in length and only 0.5 mm wide, length of pistil is essentially sessile. Initial observations seem to indicate absence of anthers/filaments and pistils on some flowers. These reproductive structures may persist for only a short period of time.1586074Ames 25515
23NA 67660QLG034Deutzia vilmoriniae Lemoine Shaanxi Sheng, ChinaNA1996COLLECTED10/18/1996Hanzhong District, Foping County (Qinling Mountains): Foping Nature Preserve, San Guan Miao Forest Station, along trail en route to summit.33.66666667, 107.816944441923Growing in open woodland in part to full sun in a dense forest. Growing amid boulders with moist, organic soils between and sphagnum moss on top. Slope: 5 percent. Aspect: Southeast.Wild material1579550NA 67660
24NA 67823QLG193Tsuga chinensis (Franch.) E. Pritz. Shaanxi Sheng, ChinaNA1996COLLECTED10/18/1996Ankang District, Ningshan County (Qinling Mountains): Ningxi Preserve, near Caiziping Forest Station town, behind the hospital valley.33.73911000, 108.329580001855Very steep slope in a deep, shaded woodland valley. Growing in a dry streambed with a heavy boulder field. Slope: 60 percent. Aspect:Northwest.Wild material1579668NA 67823
25WLP 1236QLG226Hydrangea heteromalla D. Don Gansu Sheng, ChinaNA1996COLLECTED10/18/1996Xiao Long Shan Forest Bureau, Dang Chuan Forest Station, Mai Chao Gou34.28361111, 106.183611111625Rocky ledge in part shade three meters above the path; 70% N slope; highly organic soils in thick layers among rocks; growing w/ Asarum, ferns, Acer, Salix, Sorbaria, and numerous herbaceous species.Wild material3-4 meters; multi-stemmed, deciduous shrub with arching branches; collected from 2-5 plants 1579663WLP 1236
26Ames 2917JDC/GD/2013/001/445Gymnocladus dioicus (L.) K. Koch Illinois, United StatesNC7FRUIT1984COLLECTED08/26/1982East bank of the Mazon River, SE 1/4 of SW 1/4 of Section 12, T33N R7E, Morris Quad, Grundy County.41.34600000, -88.37740000159Mesic floodplain forest.Wild materialLarge tree.1022538Ames 2917