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ACCESSIONPLANT NAMETAXONOMYORIGINGENEBANKIMAGEAVAILABILITYRECEIVEDSOURCE TYPESOURCE DATECOLLECTION SITECOORDINATESELEVATIONHABITATIMPROVEMENT LEVELNARRATIVE
0PI 638735P. pensylvanicaPrunus pensylvanica L. f. Russian FederationGENFRUIT1999DONATEDCultivar1589513PI 638735
1GPRU 163MARSB-153Prunus maritima Marshall Delaware, United StatesGENSEED2019Wild material2097500GPRU 163
2GPRU 164MARSB-290Prunus maritima Marshall New Jersey, United StatesGENSEED2019Wild material2097559GPRU 164
3GPRU 168MARSB-577Prunus serotina Ehrh. New York, United StatesGENSEED2019Wild material2097661GPRU 168
4GPRU 160MARSB-576Prunus maritima Marshall New York, United StatesGENSEED2018Wild material1964799GPRU 160
5NA 88123MARSB-798Morella pensylvanica (Mirb.) Kartesz New York, United StatesNASEED2019Wild material2097709NA 88123
6NA 88033NCBG-403Morella pensylvanica (Mirb.) Kartesz Virginia, United StatesNASEED2018Wild material1965944NA 88033
7NA 87990MARSB-150Morella pensylvanica (Mirb.) Kartesz Delaware, United StatesNASEED2018Wild material1964723NA 87990
8NA 87995MARSB-224Morella pensylvanica (Mirb.) Kartesz New York, United StatesNASEED2018Wild material1964741NA 87995
9NA 87996MARSB-291Morella pensylvanica (Mirb.) Kartesz New Jersey, United StatesNASEED2018Wild material1964750NA 87996
10NA 87999MARSB-468Morella pensylvanica (Mirb.) Kartesz New Jersey, United StatesNASEED2018Wild material1964778NA 87999
11NA 88000MARSB-579Morella pensylvanica (Mirb.) Kartesz New York, United StatesNASEED2018Wild material1964800NA 88000
12NA 88001MARSB-595Morella pensylvanica (Mirb.) Kartesz New York, United StatesNASEED2018Wild material1964805NA 88001
13NA 88003MARSB-639Morella pensylvanica (Mirb.) Kartesz Delaware, United StatesNASEED2018Wild material1964813NA 88003
14Ames 38800Camp MitigwaAmelanchier arborea (F. Michx.) Fernald Iowa, United StatesNC7FRUIT2026COLLECTED06/01/2026Mitigwa Scout Camp located on west side of Des Moines River watershed approximately 7.50 miles south, southwest of Boone, T82N R26W N 1/4 Sec. 5 and T83N R26W S 1/4 Sec. 32.41.94894500, -93.90537200310High-quality white oak - ironwood, mature woods.Wild materialThe native range of Amelanchier arborea is concentrated in the eastern half of the U.S. (Little, 1977). This accession represents a collection of A. arborea germplasm from the western edge of the species native range, specifically central Iowa. Specimens sampled at the collection site in nature were small to medium understory or woodland edge single and/or multi-trunked trees with a few trees getting close to being deemed as canopy specimens. Bark smooth and light grey in color. Specimens sampled in nature ranging 15-50' in height. Peak flowering occurred on 8 April 2026 with white flowers appearing prior to leaf expansion. Fall colors ranging from orange to orange-red peaking typically at the end of September (central Iowa). Fruits, dark-pink to red, maturing in early June (peak in 2026 occurred on 2 June) averaging 8 mm in diameter, except for mother tree #6 that had rather large fruits at 11 mm in diameter. 2197049Ames 38800
15W6 62512FWS0300-100Sporobolus cryptandrus (Torr.) A. Gray Michigan, United StatesW6SEED2025Wild material2192210W6 62512
16W6 62513FWS0300-102Sorghastrum nutans (L.) Nash Michigan, United StatesW6SEED2025Wild materialNear active artillery range2192211W6 62513
17W6 62524FWS0300-120Liatris aspera Michx. Michigan, United StatesW6SEED2025Wild material2192222W6 62524
18W6 62526FWS0300-127Bromus kalmii A. Gray Michigan, United StatesW6SEED2025Wild materialNear active artillery range. The above population size does not include vegetative plants.2192224W6 62526
19W6 62527FWS0300-130Solidago hispida Muhl. ex Willd. Michigan, United StatesW6SEED2025Wild materialReceived as: Solidago hispida2192225W6 62527
20W6 62538FWS0300-153Monarda punctata L. Michigan, United StatesW6SEED2025Wild material2192236W6 62538
21W6 62542FWS0300-66Danthonia spicata (L.) P. Beauv. ex Roem. & Schult. Michigan, United StatesW6SEED2025Wild material2192240W6 62542
22W6 62543FWS0300-67Avenella flexuosa (L.) Parl. Michigan, United StatesW6SEED2025Wild material2192241W6 62543
23W6 62546FWS0300-97Schizachyrium scoparium (Michx.) Nash Michigan, United StatesW6SEED2025Wild materialThere is Solidago vossii in the area.2192244W6 62546
24W6 62547FWS0300-98Andropogon gerardi Vitman Michigan, United StatesW6SEED2025Wild materialThere is Solidago vossii in the area.2192245W6 62547
25W6 62548FWS0300-99Elymus canadensis L. Michigan, United StatesW6SEED2025Wild material2192246W6 62548
26OPGC 8857Marietta Sand PrairieVerbena stricta Vent. Iowa, United StatesOPGC2024COLLECTED09/04/2024Marietta Sand Prairie State Preserve located 7.5 miles northwest of Marshalltown on Knapp Avenue, T84N R19W SW ¼ Sec. 11.42.09711200, -93.03873400297Remnant sand prairie.Wild material2170474OPGC 8857
27NA 885932024RJLNJ-001Ilex glabra (L.) A. Gray New Jersey, United StatesNA2024COLLECTED11/24/2024Mullica Township: Both sides of Duerer Street, approximately 0.37 kilometers southeast of 4th Avenue.39.55885000, -74.6644250021Shade to almost full sun on compacted seasonally moist to temporarily wet areas of a mixed evergreen and deciduous woodland dominated by Pinus rigida. Vegetation of this area is very much defined by small changes in elevation that go from wet to very dry. Ilex glabra remains abundant throughout, though. Slope: N/A. Aspect: N/A. The underlying geology of this area is the Cohansey Formation of middle Miocene origin and comprised of sand, white to yellow with local gravel and clay. It is sometimes locally stained red or orange brown by iron oxides and (or) cemented into large blocks of ironstone. Unweathered clay is typically dark gray, but commonly weathers white where it is interbedded with thin beds of ironstone. Sand is typically medium grained and moderately sorted although it ranges from fine to very coarse grained and from poorly to well sorted. Sand consists of quartz and siliceous rock fragments. Some beds are locally micaceous. Maximum thickness in the map area is about 60 meters; however, thickness is difficult to determine because of the irregular basal contact and extensive post-depositional erosion. (Source: USGS New Jersey Geologic Map Data). The primary soil type in the area of this collection is classified as Mullica Series sandy loam, 0 to 2 percent slopes. These soils are typically coarse-loamy, siliceous, semiactive, and mesic typic humaquepts that are strongly to extremely acidic throughout the profile. The typical solum thickness ranges from 50-150+ cm. These soils are generally considered to be poorly drained. (Source: NRCS Web Soil Survey).Wild material2169930NA 88593
28NA 890802024RJLPA-006Ilex montana Torr. & A. Gray Pennsylvania, United StatesNA2024COLLECTED09/20/2024Berks and Schuylkill Counties: Hawk Mountain Sanctuary.40.64162200, -75.99122600418Plants are growing from shade to full sun on a dry-mesic to very dry, well-drained upland/montane habitat characterized by an upland mixed deciduous and evergreen forest that is very rocky. All the plants found in this habitat go through periods of drought during the growing season due to the limited litter/soil layer in which moisture can be held. Elevation: 405 to 430 meters. Slope: 5 to 25 percent. Aspect: various. Geology: The underlying geology of this area is of Silurian origin and comprised of Shawangunk Formation. This formation is primarily light- to dark-gray, fine- to very coarse-grained sandstone and conglomerate containing thin shale interbeds. (Source: USGS Pennsylvania Geologic Map Data). Soils: The surface soil profile of this area is characterized as the Hazleton Series which consists of deep and very deep, well drained soils formed in residuum of acid gray, brown or red sandstone on uplands. The matrix includes a considerable accumulation of thin, flat, coarse fragments of sandstone, limestone, or schist with diameters up to 15 cm. Slope ranges from 0-80%. Permeability is moderately rapid to rapid. (Source: USDA-NRCS Official Soil Series Descriptions). EPA Ecoregion (Level III): Ridge and Valley (67). EPA Ecoregion (Level IV): Northern Sandstone Ridges (67c).Wild material2169044NA 89080
29OPGC 8803CBG- 10754Aquilegia canadensis L. Illinois, United StatesOPGC2023Wild material2142225OPGC 8803
30OPGC 8813CBG- 10781Hieracium scabrum Michx. Illinois, United StatesOPGC2023Wild material2142247OPGC 8813
31OPGC 8820CBG- 10801Apocynum androsaemifolium L. Illinois, United StatesOPGC2023Wild material2142260OPGC 8820
32W6 61358CBG- 10772Carex cephalophora Muhl. ex Willd. Wisconsin, United StatesW6SEED2023Wild material2142240W6 61358
33WLP 2673RJL2022NJ-004Lyonia mariana (L.) D. Don New Jersey, United StatesNA2022COLLECTED10/24/2022Plants growing on both sides of Duerer Street approximately 0.37 kilometers southeast of 4th Avenue, Mullica Township, New Jersey. Plants are common but scattered on both sides of the road at this site. 39.55730700, -74.6637610022Plants grow from part shade to full sun throughout the habit from the upper edges of the ditches through the herbaceous grass dominant buffer and all the way to the part shade of the woodland edge. Plants transition through moist/wet conditions in full sun to quite dry conditions in part shade and seem equally adapted.
Soils: The underlying geology of this area is the Cohansey Formation of middle Miocene origin and comprised of sand, white to yellow with local gravel and clay. It is sometimes locally stained red or orange brown by iron oxides and (or) cemented into large blocks of ironstone. Unweathered clay is typically dark gray, but commonly weathers white where it is interbedded with thin beds of ironstone. Sand is typically medium grained and moderately sorted although it ranges from fine to very coarse grained and from poorly to well sorted. Sand consists of quartz and siliceous rock fragments. Some beds are locally micaceous. Maximum thickness in the map area is about 60 meters; however, thickness is difficult to determine because of the irregular basal contact and extensive post-depositional erosion.
Source: USGS New Jersey Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=NJTch%3B1)
The primary soil type in the area of this collection is classified as Mullica sandy loam, 0 to 2 percent slopes. These soils are typically coarse-loamy, siliceous, semiactive, and mesic typic humaquepts that are strongly to extremely acidic throughout the profile. The typical solum thickness ranges from 50-150+ cm. These soils are generally considered to be poorly drained.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2139664WLP 2673
34NA 88500RJL2022NJ-002Ilex glabra (L.) A. Gray New Jersey, United StatesNA2022COLLECTED10/24/2022Mullica Township: both sides of Duerer Street, approximately 0.37 kilometers southeast of 4th Avenue.39.55885000, -74.6644250021Plants growing in shade to almost full sun on compacted seasonally moist to temporarily wet areas of a mixed evergreen and deciduous woodland dominated by Pinus rigida. Vegetation of this area is very much defined by small changes in elevation that go from wet to very dry. Ilex glabra remains abundant throughout, though. Plants are abundant on the edge of the woodlands as well as the understory of the woodlands. Soils: The underlying geology of this area is the Cohansey Formation of middle Miocene origin and comprised of sand, white to yellow with local gravel and clay. It is sometimes locally stained red or orange brown by iron oxides and (or) cemented into large blocks of ironstone. Unweathered clay is typically dark gray, but commonly weathers white where it is interbedded with thin beds of ironstone. Sand is typically medium grained and moderately sorted although it ranges from fine to very coarse grained and from poorly to well sorted. Sand consists of quartz and siliceous rock fragments. Some beds are locally micaceous. Maximum thickness in the map area is about 60 meters; however, thickness is difficult to determine because of the irregular basal contact and extensive post-depositional erosion. (Source: USGS New Jersey Geologic Map Data). The primary soil type in the area of this collection is classified as Mullica sandy loam, 0 to 2 percent slopes. These soils are typically coarse-loamy, siliceous, semiactive, and mesic typic humaquepts that are strongly to extremely acidic throughout the profile. The typical solum thickness ranges from 50-150+ cm. These soils are generally considered to be poorly drained. (Source: NRCS Web Soil Survey).Wild material2139663NA 88500
35NA 88489RJL2022PA-005Kalmia latifolia L. Pennsylvania, United StatesNA2022COLLECTED09/10/2022Plants are growing on the lands of Hawk Mountain Sanctuary. This species is very common and abundant. It is one of the most dominant understory plants in woodlands. This species is a common understory shrub throughout the entire region in upland dry woodland habitats.40.63862000, -75.99071200430Plants are growing primarily in shade to part-shade on a dry-mesic to very dry, well-drained upland/montane habitat characterized by upland mixed deciduous and evergreen forest that is very rocky. All of the plants found in this habitat go through periods of drought during the growing season due to the limited litter/soil layer in which moisture can be held. The underlying geology of this area is of Silurian origin and comprised of Shawangunk Formation. This formation is primarily light- to dark-gray, fine- to very coarse-grained sandstone and conglomerate containing thin shale interbeds.
Source: USGS Pennsylvania Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=PASs%3B14)
The surface soil profile of this area is the Hazleton series consists of deep and very deep, well drained soils formed in residuum of acid gray, brown or red sandstone on uplands. The matrix includes a considerable accumulation of thin, flat, coarse fragments of sandstone, limestone, or schist with diameters up to 15 cm. Slope ranges from 0-80%. Permeability is moderately rapid to rapid.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2139368NA 88489
36NA 88490RJL2022PA-006Ilex montana Torr. & A. Gray Pennsylvania, United StatesNA2022COLLECTED09/10/2022Hawk Mountain Sanctuary.40.64162200, -75.99122600420Plants are growing from shade to full sun on a dry-mesic to very dry, well-drained upland/montane habitat characterized by an upland mixed deciduous and evergreen forest that is very rocky. All of the plants found in this habitat go through periods of drought during the growing season due to the limited litter/soil layer in which moisture can be held. The underlying geology of this area is of Silurian origin and comprised of Shawangunk Formation. This formation is primarily light- to dark-gray, fine- to very coarse-grained sandstone and conglomerate containing thin shale interbeds. (Source: USGS Pennsylvania Geologic Map Data). The surface soil profile of this area is the Hazleton series consists of deep and very deep, well drained soils formed in residuum of acid gray, brown or red sandstone on uplands. The matrix includes a considerable accumulation of thin, flat, coarse fragments of sandstone, limestone, or schist with diameters up to 15 cm. Slope ranges from 0-80%. Permeability is moderately rapid to rapid. (Source: NRCS Web Soil Survey).Wild material2139369NA 88490
37NA 88491RJL2022PA-007Rhododendron maximum L. Pennsylvania, United StatesNA2022COLLECTED09/10/2022Plants are growing on the lands of Hawk Mountain Sanctuary. This species was common, but generally restricted to steep rocky outcrops.40.63813900, -75.98835200420Plants are growing from shade to full sun on a dry-mesic to very dry, well-drained upland/montane habitat characterized by an upland mixed deciduous and evergreen forest that is very rocky. Even so, most heavily fruited plants were growing in part shade to almost full sun. All of the plants found in this habitat go through periods of drought during the growing season due to the limited litter/soil layer in which moisture can be held. The underlying geology of this area is of Silurian origin and comprised of Shawangunk Formation. This formation is primarily light- to dark-gray, fine- to very coarse-grained sandstone and conglomerate containing thin shale interbeds.
Source: USGS Pennsylvania Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=PASs%3B14)
The surface soil profile of this area is the Hazleton series consists of deep and very deep, well drained soils formed in residuum of acid gray, brown or red sandstone on uplands. The matrix includes a considerable accumulation of thin, flat, coarse fragments of sandstone, limestone, or schist with diameters up to 15 cm. Slope ranges from 0-80%. Permeability is moderately rapid to rapid.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2139370NA 88491
38OPGC 7587Marietta Sand PrairiePackera plattensis (Nutt.) W. A. Weber & Á. Löve Iowa, United StatesOPGCFLOWER2022COLLECTED06/03/2022Marietta Sand Prairie State Preserve located 12.0 km northwest of Marshalltown and 10.0 km north of Highway 30 on Knapp Avenue, T84N R19W W ½ Sec. 11.42.09835700, -93.03457900299Remnant sand prairie.Wild materialPlants in nature are approximately one to two feet in height. Peak flower and fruiting in 2022 occurred on 26 May and 3 June, respectively.2138177OPGC 7587
39OPGC 8519MARSB-415Limonium carolinianum (Walter) Britton New York, United StatesOPGC2021Wild material2137176OPGC 8519
40W6 60082MARSB-144Hudsonia tomentosa Nutt. New Jersey, United StatesW62021Wild materialScale like leaves, blueish tint, yellow flowers.2137167W6 60082
41NA 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
42WLP 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
43WLP 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
44WLP 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
45W6 58574MARSB-176Cyperus grayi Torr. Delaware, United StatesW62021Wild materialInflorescence looks like fireworks, bulbous root growths. Grows in clumps.2113504W6 58574
46W6 58628MARSB-553Avenella flexuosa (L.) Parl. New York, United StatesW62021Wild materialRound stem, inflorescence with thin wiry branches and tan seed. Large tufts of straight, wiry basal leaves.2113558W6 58628
47W6 58631MARSB-580Cyperus grayi Torr. New York, United StatesW62021Wild materialTriangular stem, branches fork from one point at the top of the stem, flat, feather-like inflorescences, bulbous root nodules.2113561W6 58631
48NA 88106MARSB-412Baccharis halimifolia L. New York, United StatesNASEED2019Wild material2097620NA 88106
49NA 88125MARSB-875Juniperus virginiana L. New Jersey, United StatesNASEED2019Wild material2097745NA 88125
50NA 88440MARSB-419Rosa virginiana Mill. New York, United StatesNASEED2019Wild material2097623NA 88440
51W6 57056MARSB-138Avenella flexuosa (L.) Parl. New York, United StatesW6SEED2019Wild material2097495W6 57056
52W6 57057MARSB-140Hudsonia tomentosa Nutt. New York, United StatesW6SEED2019Wild material2097496W6 57057
53W6 57083MARSB-212Carex silicea Olney New York, United StatesW6SEED2019Wild material2097522W6 57083
54W6 57086MARSB-223Cyperus grayi Torr. New York, United StatesW6SEED2019Wild material2097525W6 57086
55W6 57124MARSB-300Cyperus grayi Torr. New Jersey, United StatesW6SEED2019Wild material2097563W6 57124
56W6 57139MARSB-329Hexasepalum teres (Walter) J. H. Kirkbr. New Jersey, United StatesW6SEED2019Wild material2097578W6 57139
57W6 57182MARSB-416Parthenocissus quinquefolia (L.) Planch. New York, United StatesW6SEED2019Wild material2097621W6 57182
58W6 57183MARSB-418Pseudognaphalium obtusifolium (L.) Hilliard & B. L. Burtt New York, United StatesW6SEED2019Wild material2097622W6 57183
59Ames 34781MARSB-594Rhus copallinum L. New York, United StatesNC7SEED2018COLLECTED09/20/2016Brooklyn Marine Park just off Gerritsen Avenue.40.59222000, -73.918220002Maritime successional forestWild material1964804Ames 34781
60NA 87998MARSB-417Baccharis halimifolia L. New York, United StatesNASEED2018Wild material1964771NA 87998
61OPGC 6539MARSB-445Solidago sempervirens L. New Jersey, United StatesOPGCSEED2018Wild materialSolidago sempervirens1964772OPGC 6539
62W6 54020MARSB-211Juncus gerardi Loisel. New York, United StatesW6SEED2018Wild materialJuncus gerardii1964736W6 54020
63W6 54027MARSB-232Schoenoplectus pungens (Vahl) Palla New York, United StatesW6SEED2018Wild materialSchoenoplectus pungens1964743W6 54027
64Ames 34780MARSB-396Rhus copallinum L. New York, United StatesNC7SEED2017COLLECTED11/03/2015Jones Beach State Park (Field 6).40.61213000, -73.420440003Atlantic coastal beach, north Atlantic coastal shrub and grass duneWild material1954643Ames 34780
65WLP 1984MARSB-809Viburnum dentatum L. New York, United StatesNA2017COLLECTED08/24/2017Suffolk County; ; Hither Hills State Park: Cemetery Road & Old Montauk Highway.41.00577000, -72.02097000Mid-succession scrubland; roadside. Sand soil (Dune Land, Montauk Loam). Land used for conservation and recreation.Wild materialSeeds collected from 80 plants; 100 plants found in an area of three acres. Two herbarium vouchers collected on 24 Aug. 2017; held at Smithsonian and MARSB. Material identified in field by Clara Holmes on 24 Nov. 2017. Ecoregion: 84E -- Atlantic Coastal Pine Barrens (Omernik).2108828WLP 1984
66Ames 34014Ames 34014Aronia melanocarpa (Michx.) Elliott Illinois, United StatesNC7Flower2017COLLECTED09/03/2017Nachusa Grasslands - locally known as Coyote Point approximately 3.80 miles northwest of Franklin Grove just 0.60 miles west of Lowden Road, T22N R10E NE 1/4 NE 1/4 SW 1/4 Sec. 21, Lee County41.87972200, -89.35305600220St. Peter's sandstone cliff, specimens noted on ridgetop and on slopes.Wild materialThis accession based on morphological/phenological observations at NCRPIS field plots seems to represent the "southern form" of A. melanocarpa, potentially a new Aronia species. This southern form was originally discovered by Brand et al. 2022 (Ploidy, genetic diversity and speciation of the genus Aronia) and is known for having glabrous stems and leaves and a distinct phyllotaxy than other Aronia species. In addition, plants tend to bloom approximately two weeks later than all other Aronia taxonomic groups and the inflorescences/infructescences are more spreading and extended due to longer peduncles and pedicels within the cyme. Fruit maturity tends to occur 2 to 4 weeks later than tetraploid A. melanocarpa and 4 to 6 weeks later than diploid A. melanocarpa. Phenolic levels are much higher in comparison to other A. melanocarpa accessions (Brand et al., 2017 - Anthocyanins, total phenolics, ORAC and moisture content of wild and cultivated dark-fruited Aronia species.)1953928Ames 34014
67W6 48847MARSB-054Avenella flexuosa (L.) Parl. New York, United StatesW6SEED2015Wild material1922854W6 48847
68Ames 32835GA14014001Fraxinus pennsylvanica Marshall North Dakota, United StatesNC7SEED2014COLLECTED10/30/2014Bottineau County, Turtle Mountains.48.97000000, -100.45000000737Mixed oak-aspen forestWild material1921828Ames 32835
69WLP 1746Ames 32838Viburnum opulus L. var. americanum Aiton North Dakota, United StatesNA2014COLLECTED10/31/2014Turtle Mountains - Bottineau County.48.95000000, -100.43000000692Wet, aspen forest. Growing in association with Sanicula marilandica, Fragaria virginiana, Trifolium repens, Rubus sp., Typha latifolia, Prunus pensylvanica, Prunus virginiana, Corylus sp., Crataegus sp., Viburnum lentago, Rosa sp., Cornus sericea, Amelanchier sp., Symphoricarpos sp., Salix sp., Betula papyrifera, Populus tremuloides, Ulmus americana, Acer negundo, Quercus macrocarpa, and Fraxinus pennsylvanica.Wild material1921831WLP 1746
70Ames 32096BA13009001Fraxinus nigra Marshall Minnesota, United StatesNC7SEED2013COLLECTED09/23/2013T144N R38W, Clearwater County.47.25711000, -95.49000667543Edges of lakes and forest edges. Growing in association with Fraxinus pennsylvanica, Quercus macrocarpa, Ulmus americana, Populus tremuloides, Populus balsamifera, Acer saccharum, Betula papyrifera, Salix sp., Larix laricina, Quercus rubra, Abies balsamea, Picea glauca, Sambucus canadensis, Cornus rugosa, Acer spicatum, Rosa sp., Viburnum opulus var. americanum, Viburnum dentatum, Alnus sp., Cornus canadensis, Corylus sp., Prunus virginiana, Ribes sp., Prunus pensylvanica, Rhamnus alnifolia, Equisetum sp., Carex sp., Rubus sp., Impatiens capensis, Bromus sp., and Thalictrum dasycarpum.Wild materialD.B.H. ranged between 3 and 6 inches.1914713Ames 32096
71Ames 31677GA12001001Fraxinus pennsylvanica Marshall Minnesota, United StatesNC7SEED2012COLLECTED09/24/2012Southwest Becker County near Lake Cormorant and Lake Maud..46.73903330, -95.97883330415Edge of slough and forest. Wild material1906588Ames 31677
72Ames 31074697Fraxinus americana L. New York, United StatesNC7SEED2011COLLECTED09/13/2011Two Mile Road, Allegany County.42.03800000, -78.46400000524Wild material1891460Ames 31074
73NA 70422MWPCC00-078Magnolia acuminata (L.) L. North Carolina, United StatesNA2000COLLECTED09/14/2000Blue Ridge Parkway pullover, N of marker 417.35.32333333, -82.826944441353Just in from mowed roadside. Slope: 15 degrees, Aspect: East, 3/4 day sun, Soil Type: gritty loam, well-drained, moist bottom of slope.Wild material1608250NA 70422