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ACCESSIONPLANT NAMETAXONOMYORIGINGENEBANKIMAGEAVAILABILITYRECEIVEDSOURCE TYPESOURCE DATECOLLECTION SITECOORDINATESELEVATIONHABITATIMPROVEMENT LEVELNARRATIVE
0DPRU 2937AM-2006-172Prunus incana (Pall.) Batsch ArmeniaDAV2006COLLECTED10/13/2006Near Khosrov Preserve, Ararat40.05576000, 44.782640001722Shrub with spiny branches. Fruit small, dried, adhering to stems. Seed from single plant.Wild materialShrub 1.5-2m. Glabrous fruit. Cherry?1713206DPRU 2937
1DPRU 2938AM-2006-173Prunus incana (Pall.) Batsch ArmeniaDAV2006COLLECTED10/04/2006Syunik40.06530000, 44.791960001664very dry hillside: Fruit redish-brown, dried flesh covering small pit. Seed collected from 6+ plants.Wild materialCollectors Note: Fruit redish-brown, dried flesh covering small pit. Seed collected from 6+ plants.1713207DPRU 2938
2NA 890912024RM-TK-004Prunus sp.Florida, United StatesNA2024COLLECTED09/05/2024Blackwater River Wildlife Management Area: on the south side of Boundary Line Road about 0.32 kilometers west of Deaton Bridge Road along an area edged by a barbed wire fence.30.68579800, -86.8796430045Plants are growing from part-sun to full sun. Plants are growing in an area that is frequently burned with a lot of [Prunus sp. (orig. listed as Prunus alabamensis)] scattered throughout. This habitat is a longleaf pine-wiregrass community with scattered turkey (Quercus laevis) and blackjack oaks (Quercus incana). There is a slight slope downward. The line of [Prunus sp.] goes along a semi-ditch on the side of a dirt road. The plants probably get a bit more water than the plants out in the open forest. The [Prunus sp.] are most often without any other close woody companions. Slope: 0 percent. Aspect: North. Geology: The underlying geology of this area is probably of lower Pliocene age and characterized as the Citronelle Formation. The Citronelle Formation is widespread in the Gulf Coastal Plain. The type section for the Citronelle Formation, named by Matson (1916), is near Citronelle, Alabama. The Citronelle Formation grades laterally, through a broad facies transition, into the Miccosukee Formation of the eastern Florida panhandle. Coe (1979) investigated the Citronelle Formation in portions of the western Florida panhandle. The Citronelle Formation is a siliciclastic, deltaic deposit that is lithologically similar to, and time equivalent with, the Cypresshead Formation and, at least in part, the Long Key Formation (Cunningham et al., 1998) of the peninsula. In the western panhandle, some of the sediments mapped as Citronelle Formation may be reworked Citronelle. The lithologies are the same and there are few fossils present to document a possible younger age. The Citronelle Formation consists of gray to orange, often mottled, unconsolidated to poorly consolidated, very fine to very coarse, poorly sorted, clean to clayey sands. It contains significant amounts of clay, silt and gravel which may occur as beds and lenses and may vary considerably over short distances. Limonite nodules and limonite-cemented beds are common. Marine fossils are rare but fossil pollen, plant remains and occasional vertebrates are found. Much of the Citronelle Formation is highly permeable. It forms the Sand and Gravel Aquifer of the surficial aquifer system. (Source: USGS Florida Geologic Map Data). Soils: The soil of this area is characterized as Lakeland Series Sand, 0 to 5 percent slopes (21). The Lakeland Series consists of very deep, excessively drained, rapid to very rapidly permeable soils on uplands. They formed in thick beds of eolian or marine and/or fluvio-marine sands in the Southern Coastal Plain MLRA (133A), the Carolina and Georgia Sandhills (MLRA 137), the Eastern Gulf Coast Flatwoods (MLRA 152A) and the Atlantic Coast Flatwoods (MLRA 153A). (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). EPA Ecoregion (Level III): Southeastern Plains (65). EPA Ecoregion (Level IV): Southern Pine Plains and Hills (65f).Wild materialReceived as Prunus alabamensis; other collections of this material have proven not to be Prunus serotina var. alabamensis, but actually a species of plum; this will likewise be treated as unidentified material until its species can be ascertained. Collectors' notes refer to the plant by the name under which it was collected.2169055NA 89091
3Ames 36263Chippewa National Forest (Itasca)Viburnum opulus L. var. americanum Aiton Minnesota, United StatesNC7FRUIT2024COLLECTED09/15/2024Chippewa National Forest between Alder and Suomi including Bowstring River, Turtle River, and Potato Creek watersheds.47.56968000, -93.68815400407Roadside edges with most samples near open water (creek/rivers).Wild materialFormerly known as Viburnum trilobum, American highbush cranberry (V. opulus var. americanum) is a North American native shrub that is utilized as an important ornamental and conservation plant that is also harvested as a minor fruit crop (jams/jellies). In nature, this variety is generally found in moist habitats typically along stream banks and swamps where ample moisture is readily available. The native range of V. opulus var. americana is concentrated in the northeastern United States and into Canada (Little, E. L. Jr. 1977). Attractive ornamental characteristics includes showy lacecap flowers in spring and bright red fruits and foliage in the fall. Fruits are tart with a hint of sweetness. The European highbush cranberry (V. opulus var. opulus) is nearly identical to American highbush cranberry other than small glands (<1 mm) on the petiole making the exact determination very challenging resulting in common misidentifications. A major difference between the American and European highbush cranberries is that the European variety produces unpalatable fruit. Recent research has shown that American and European highbush cranberries are genetically distinct and that plants of hybrid origin are uncommon (Tork et. al 2025). Genetics of this accession represents a very broad collection area stretching nearly 7.0 miles near Alder in central Itasca County of north central Minnesota. In August of 2022, a total of 23 leaf samples from this same area were sampled (OB001-OB012 and OB0015-OB025) and all samples were genetically confirmed as American highbush cranberry, V. opulus var. americanum (Tork et. al 2025). 2168987Ames 36263
4Ames 35923AS/FN/2022/072/203Fraxinus nigra Marshall Wisconsin, United StatesNC7SEED2022COLLECTED09/29/2022Chequamegon National Forest, approximately ten miles southeast of Park Falls. Collected along North Gates Lake Road, Sailor Lake Road and State Highway 70, T38N R2E and T39N R1E.45.81027500, -90.27504800483Saturated soils in northern hardwood forest.Wild materialAccession represents materials collected across a 15 x 15 square mile area sampled by Carstens, Sherwood, and Brandtner. Same area as where FSNS 5000 was collected.2139686Ames 35923
5Ames 31676GA12010001Fraxinus pennsylvanica Marshall Minnesota, United StatesNC7SEED2012COLLECTEDNEAR 09/24/2012Near Mashaug Creek just north of Twin Valley, Norman County.47.28851660, -96.26865000327Upland forest, dominated by Populus deltoides. Wild material1906587Ames 31676
6Ames 30132JDC/CA/2009/041/191Cornus amomum Mill. subsp. obliqua (Raf.) J. S. Wilson Wisconsin, United StatesNC7SEED2009COLLECTED09/22/2009Along Kent Road, near Poynette, NW 1/4 of NW 1/4 of Section 29, T11N, R9E, Poynette Quad, Columbia County.43.40638889, -89.45861111243Hinkson Creek Watershed. Wild material1819713Ames 30132
7NA 82193JDC/IV/2009/039/189Ilex verticillata (L.) A. Gray Wisconsin, United StatesNA2009COLLECTED09/22/2009Wisconsin: Columbia County; Along Kent Road, near Poynette, NW 1/4 of NW 1/4 of Section 29, T11N, R9E, Poynette Quad. Hinkson Creek watershed.43.40638889, -89.45861111243Hinkson Creek Watershed. Associated with Acer negundo, Alnus incana subsp. rugosa, Amelanchier, Aronia melanocarpa, Carpinus caroliniana, Cornus amomum subsp. obliqua, Fraxinus nigra, Helianthus strumosus, Juglans nigra, Populus tremuloides, Prunus virginiana, and Viburnum lentago.Wild material1819738NA 82193
8WLP 854JDC/CC/2009/038/188Carpinus caroliniana Walter Wisconsin, United StatesNA2009COLLECTED09/22/2009Wisconsin: Columbia County; Along Kent Road, near Poynette, NW 1/4 of NW 1/4 of Section 29, T11N, R9E, Poynette Quad. Hinkson Creek watershed.43.40638889, -89.45861111243Hinkson Creek Watershed. Associated with Acer negundo, Alnus incana subsp. rugosa, Amelanchier, Aronia melanocarpa, Cornus amomum subsp. obliqua, Fraxinus nigra, Helianthus strumosus, Ilex verticillata, Juglans nigra, Populus tremuloides, Prunus virginiana, and Viburnum lentago.Wild material1819709WLP 854