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ACCESSIONPLANT NAMETAXONOMYORIGINGENEBANKIMAGEAVAILABILITYRECEIVEDSOURCE TYPESOURCE DATECOLLECTION SITECOORDINATESELEVATIONHABITATIMPROVEMENT LEVELNARRATIVE
0NA 61910NA 61910Juniperus rigida Siebold & Zucc. Korea, SouthNA1990COLLECTEDPyongyang: NE part of the city Chujak peak, Province of Pyongyang City.39.08333333, 125.75000000125Wild material1496790NA 61910
1NA 56614KSW 3669Juniperus rigida Siebold & Zucc. Jeollabuk-do, Korea, SouthNA1985COLLECTED10/03/1985Buan-gun, Jinseo-myeon: Byeonsan-bando (peninsula): Unho-ri, Jungma-dong [Originally listed as Cholla Pukto, Puan Gun, Chinso Myon, Unho-ri, Chungma Dong.]34.59166000, 126.54166000100Common on west-facing rock face in poor soil, sun.Wild material1499044NA 56614
2NA 88389NEWFS-739Juniperus virginiana L. var. virginiana Massachusetts, United StatesNA2021Wild materialSmall conical shrub with waxy blue green fruits and tight scale like leaves.2138832NA 88389
3NA 88081NEWFS-739Juniperus virginiana L. var. virginiana Massachusetts, United StatesNASEED2019Wild material1976341NA 88081
4NA 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
5NA 88693RJL2023NJ-006Clethra alnifolia L. New Jersey, United StatesNA2023COLLECTED11/10/2023Franklin Township: Piney Hollow Preservation Area (the site is owned by Franklin Township). Plants accessed by foot along trails throughout property.39.57319800, -74.9290890029Plants growing in shade to part-shade over a wide range of habitats from mesic to mesic-dry as well as moist to wetland habitats. The woodlands are mostly deciduous, but also include occasional pine overstory. Slope: N/A. Aspect: N/A. The underlying geology of this area is of Middle Miocene, Serravallian origin and characterized as an Cohansey Formation. It is comprised of sand, white to yellow with local gravel and clay. 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 interbedded with thin beds of ironstone. Unit is a complex of interfingering marine and nonmarine facies. 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. In general, the sand is crossbedded, although the style of crossbedding varies significantly with the paleoenvironment. Trough crossbedding predominates, especially in the nonmarine channel fill deposits, and the scale of the crossbeds varies from small to large. Maximum thickness in the map area is about 60 m; however, thickness is difficult to determine because of the irregular basal contact and extensive post-depositional erosion. There is as much as 18 m of relief along the basal contact. The basal contact is sharp, undulatory, and directly overlain by a thin gravel bed. The Cohansey Formation unconformably overlies the Kirkwood Formation and is found in channels cut down into the Kirkwood. Where the Kirkwood consists of sandy, light-colored sediments, the basal contact of the Cohansey is drawn below crossbedded sediments. Where the Kirkwood consists of dark-colored silty beds, the basal contact is drawn between light-colored Cohansey sediments and the underlying dark-colored sediments. The Cohansey was markedly thinned because of erosion prior to deposition of overlying units in the western and southern parts of the southern sheet. The unit has been extensively eroded and stripped from large areas of the New Jersey Coastal Plain, particularly in the central sheet where outliers are common. In spite of its widespread nature, the Cohansey is poorly exposed because of its loose sandy composition, which causes it to erode easily. (Source: USGS New Jersey Geologic Map Data.) The primary soil types in the area of this collection is classified as Atsion sand, 0 to 2 percent slopes, Northern Tidewater Area and Downer loamy sand, 0 to 5 percent slopes, Northern Coastal Plain. Atsion Series soils are very deep, poorly drained with moderate to rapid permeability above 70 cm and slower beneath. They are classified as sandy, siliceous, mesic Aeric Alaquods. The upper stratum from 0 to 25 cm is dark gray sand, dry, single grained and lose with many fine roots. It is extremely acid. Lower strata are light gray to dark brown with small percentages of rounded quartzose pebbles and are extremely acid. Downer Series soils are very deep, well-drained soils that are coarse-loamy, siliceous, semiactive, mesic Typic Hapludults. The upper stratum of Downer Series from 0 to 25 cm is dark grayish brown, brown loamy sand that is dry with weak fine granular structure. It is very friable and strongly acid. Lower strata from 25 to 76 cm are yellowish brown single grain, loose loamy sand with few extremely weakly cemented masses of oxidized iron in the lower part. This layer is very strongly acid. (Source: NRCS Web Soil Survey.)Wild material2159121NA 88693
6WLP 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
7NA 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
8NA 89037RJL2022KS-004 Fraxinus pennsylvanica Marshall Kansas, United StatesNAImage2022COLLECTED09/21/2022 Coronado Heights Park, Smoky View, Kansas hillsides surrounding the historic WPA circa 1932 Coronado Heights Castle located about 91 meters above the surrounding land. This plant is scattered and infrequent on the slopes of this site.38.61065700, -97.70408300448Plants growing in full sun, under extreme exposure, rocky, dry and thin soils of this short grass prairie habitat on the slopes surrounding the summit of Coronado Heights Park. Plants tend
Soils: The underlying geology of this area is of Upper Cretaceous origin and comprised of Kiowa Shale or FM- light -gray to black illitic shale with thin coquinoidal limestone beds at the base; sandstone lenses are common. Cheyenne Sandstone-massive to cross-bedded, light-gray to buff fine-grained sandstone with lenses to be found in runoff zones where moisture is temporarily more abundant.of gray sandy shale and conglomerate.
Source: USGS Kansas Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=KSKkc%3B0)
The surface soil profile of this area is Lancaster-Hedville complex, 3 to 20 percent slopes. The Lancaster series consists of moderately deep, well drained soils that formed in residuum from sandstone and sandy shales; it can be up to 200 cm deep. Slopes range from 1-20%. Hedville soils have bedrock within 50 centimeters of the surface and occur on similar hillslope positions.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2139602NA 89037
9NA 89036RJL2022KS-003Cornus drummondii C. A. Mey. Kansas, United StatesNA2022COLLECTED09/21/2022Coronado Heights Park, Smoky View, Kansas hillsides surrounding the historic WPA circa 1932 Coronado Heights Castle located about 91 meters above the surrounding land. This plant is common and abundant on the slopes of this site.38.61348400, -97.70343100475 Plants growing in part shade to full sun, under extreme exposure, rocky, dry and thin soils of this short grass prairie habitat on the slopes surrounding the summit of Coronado Heights Park. The underlying geology of this area is of Upper Cretaceous origin and comprised of Kiowa Shale or FM- light -gray to black illitic shale with thin coquinoidal limestone beds at the base; sandstone lenses are common. Cheyenne Sandstone-massive to cross-bedded, light-gray to buff fine-grained sandstone with lenses of gray sandy shale and conglomerate.
Source: USGS Kansas Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=KSKkc%3B0)
The surface soil profile of this area is Lancaster-Hedville complex, 3 to 20 percent slopes. The Lancaster series consists of moderately deep, well drained soils that formed in residuum from sandstone and sandy shales; it can be up to 200 cm deep. Slopes range from 1-20%. Hedville soils have bedrock within 50 centimeters of the surface and occur on similar hillslope positions.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)
Slope: 5-20% Aspect: all		Wild material2139601NA 89036
10NA 89035RJL2022KS-002Rosa arkansana Porter Kansas, United StatesNA2022COLLECTED09/20/2022Coronado Heights Park, Smoky View, Kansas hillsides surrounding the historic WPA circa 1932 Coronado Heights Castle located about 91 meters above the surrounding land. This plant is quite abundant on the slopes of this site and highly competitive.38.61158800, -97.70427000475Plants growing in part-sun to full sun, under extreme exposure, rocky, dry and thin soils of this short grass prairie habitat on the slopes surrounding the summit of Coronado Heights Park.
The underlying geology of this area is of Upper Cretaceous origin and comprised of Kiowa Shale or FM- light -gray to black illitic shale with thin coquinoidal limestone beds at the base; sandstone lenses are common. Cheyenne Sandstone-massive to cross-bedded, light-gray to buff fine-grained sandstone with lenses of gray sandy shale and conglomerate.
Source: USGS Kansas Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=KSKkc%3B0)
The surface soil profile of this area is Lancaster-Hedville complex, 3 to 20 percent slopes. The Lancaster series consists of moderately deep, well drained soils that formed in residuum from sandstone and sandy shales; it can be up to 200 cm deep. Slopes range from 1-20%. Hedville soils have bedrock within 50 centimeters of the surface and occur on similar hillslope positions.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2139600NA 89035
11W6 59558OR050-300Erigeron linearis (Hook.) Piper Oregon, United StatesW62021Wild materialPerennial, leaves linear and basal, yellow ray and disc flowers, flowerheads single.2120725W6 59558
12W6 58574MARSB-176Cyperus grayi Torr. Delaware, United StatesW62021Wild materialInflorescence looks like fireworks, bulbous root growths. Grows in clumps.2113504W6 58574
13W6 54272OR050-254Lomatium nudicaule (Pursh) J. M. Coult. & Rose Oregon, United StatesW62018Wild materialLomatium nudicaule1964989W6 54272
14W6 53346CA930A-596Descurainia pinnata (Walter) Britton subsp. glabra (Wooton & Standl.) Detling California, United StatesW62018Wild material1958081W6 53346
15W6 53362CA930A-613Chaenactis fremontii A. Gray California, United StatesW62018Wild material1958097W6 53362
16W6 53368CA930A-619Achnatherum speciosum (Trin. & Rupr.) Barkworth California, United StatesW62018Wild material1958103W6 53368
17W6 53369CA930A-620Ericameria linearifolia (DC.) Urbatsch & Wussow California, United StatesW62018Wild material1958104W6 53369
18W6 53370CA930A-621Eriocoma hymenoides (Roem. & Schult.) Rydb. California, United StatesW62018Wild material1958105W6 53370
19W6 53372CA930A-623Ambrosia salsola (Torr. & A. Gray) Strother & B. G. Baldwin var. salsola California, United StatesW62018Wild material1958107W6 53372
20W6 53378CA930A-629Encelia actoni Elmer California, United StatesW62018Wild material1958113W6 53378
21W6 53379CA930A-630Acamptopappus sphaerocephalus (Harv. & A. Gray) A. Gray var. sphaerocephalus California, United StatesW62018Wild material1958114W6 53379
22W6 53380CA930A-631Acmispon rigidus (Benth.) Brouillet California, United StatesW62018Wild material SOS 7th transfer.1958115W6 53380
23W6 53382CA930A-633Sphaeralcea ambigua A. Gray var. ambigua California, United StatesW62018Wild material1958117W6 53382
24W6 53387CA930A-638Eriogonum fasciculatum Benth. var. polifolium (Benth.) Torr. & A. Gray California, United StatesW62018Wild material1958122W6 53387
25W6 52179OR050-208Lomatium nudicaule (Pursh) J. M. Coult. & Rose Oregon, United StatesW62017Wild material1947314W6 52179
26OPGC 4286195373Olsynium douglasii (A. Dietr.) E. P. Bicknell var. inflatum (Suksd.) Cholewa & Douglass M. Hend. Oregon, United StatesOPGCSEED2005COLLECTED06/30/20031362Light cover of Juniperus occidentalis near a small stand of Pinus ponderosa. Associated with Artemisia rigida, Pseudoroegneria spicata, Balsamorhiza serrata, Lomatium cous and Epilobium minutum.Wild materialForb 0.3-0.6 meters tall. 1674156OPGC 4286
27OPGC 4303204439Linanthus pungens (Torr.) J. M. Porter & L. A. Johnson Oregon, United StatesOPGCSEED2005COLLECTED08/31/20031120Growing on mostly rocky outcrops in pumice flat. Associated with Juniperus occidentalis, Chrysothamnus nauseosus, Artemisia rigida, Elymus elymoides, Phacelia linearis, Pseudoroegneria spicata, Bromus tectorum and Poa secundaWild materialForb 0.38 meters tall. 1674364OPGC 4303
28NA 61753NA 61753Quercus dentata Thunb. Korea, SouthNA1989COLLECTED10/06/1989Maepo, Chungchong Pukto, Tanyang Gun, Myon. Just off Route 537.00000000, 128.00000000Open west facing limestone slope with Broussonetia, Quercus dentata, Juniperus rigida, Buxus sinica var. insularis.Wild material1498814NA 61753
29WLP 1581NEKG 166Rhododendron mucronulatum Turcz. Gangwon-do, Korea, SouthNA1989COLLECTED10/14/1989Sokcho-si: Seorak-dong: Seoraksan [mountain], on trail to Daecheongbong [peak], above Hangyeryeong [pass/ridge]. [Originally listed as Kang-won Do, Sorak San. On trail to Tae-chong Bong, above Han-gyae-Ryong.]38.10000000, 128.409722221000Rocky outcroppings - open.Wild material1506693WLP 1581