Search Accessions


rows.  (Please note that results of more than 500 rows will not contain images.)

Scientific name (any part, no hybrid symbols)

Plant name


Genebank
Country of Origin


Other search criteria:



With genomic data With NCBI link With images Only non-Genetically Engineered

View Observation Data
Selected item(s) below:

ACCESSIONPLANT NAMETAXONOMYORIGINGENEBANKIMAGEAVAILABILITYRECEIVEDSOURCE TYPESOURCE DATECOLLECTION SITECOORDINATESELEVATIONHABITATIMPROVEMENT LEVELNARRATIVE
0PI 667427Lot # PM312VLiatris spicata (L.) Willd. Wisconsin, United StatesOPGC2006COLLECTED20041717146PI 667427
1W6 62532FWS0300-138Liatris spicata (L.) Willd. Michigan, United StatesW6SEED2025Wild materialThe above acreage is that of the large, dense patch near the road. The species occurs elsewhere in the sanctuary, but in low abundance.2192230W6 62532
2W6 62524FWS0300-120Liatris aspera Michx. Michigan, United StatesW6SEED2025Wild material2192222W6 62524
3W6 62539FWS0300-154Liatris cylindracea Michx. Michigan, United StatesW6SEED2025Wild materialThe vegetative part of the population is likely dormant, though it is not possible to discern dormant individuals. Consequently, the above population size may be an underestimate.2192237W6 62539
4OPGC 8278CBG-9870Lobelia spicata Lam. Wisconsin, United StatesOPGC2021Wild material2120028OPGC 8278
5PI 658641JM2004016Aronia arbutifolia (L.) Pers. South Carolina, United StatesNC7SEED2004COLLECTED10/06/2004Poe Creek outcrop, State Forest, Pickens County.34.92856600, -82.86763300314Granite flatrock/glade community. Above seepage fen hummock on edge of rock outcrop. 10 degrees of slope. Fen/bog. Wild materialAccession has good vigor with very open growth and minimal suckering. Specimens at original collection site in nature measured up to 10 feet tall.1667569PI 658641
6PI 664646CP39Helianthus occidentalis Riddell Ohio, United StatesNC7ACHENES2004COLLECTED10/07/2004Chaparral Prairie State Nature Preserve, 3 miles northwest of West Union, Adams County.38.83583333, -83.57361111Cedar barrens prairie. Sun. Slight slope. Site size 5 square meters; 67 acre total area. Associated with Baptisia australis, Coreopsis tripteris, Eryngium yuccafolium, Liatris spicata, Physostegia virginiana, Pycnanthemum tenuifolium, Ratibida pinnata, and Rudbeckia hirta.Wild material2-5 feet tall1690634PI 664646
7W6 62534FWS0300-144Solidago riddellii Frank Michigan, United StatesW6SEED2025Wild materialThe vegetative part of the population is likely dormant, though it is not possible to discern dormant individuals. Consequently, the above population size may be an underestimate.2192232W6 62534
8W6 62536FWS0300-150Solidago ohioensis Riddell Michigan, United StatesW6SEED2025Wild materialPoison sumac present2192234W6 62536
9W6 62540FWS0300-161Solidago riddellii Frank Michigan, United StatesW6SEED2025Wild materialThe vegetative part of the population is likely dormant, though it is not possible to discern dormant individuals. Consequently, the above population size may be an underestimate.2192238W6 62540
10Ames 36255Kothenbeutel PrairieDelphinium carolinianum Walter subsp. virescens (Nutt.) R. E. Brooks Iowa, United StatesNC7PLANT2024COLLECTED07/08/2024Kothenbeutel Prairie Preserve located approximately 4.24 miles east, southeast of Sheffield just north of 240th Street, T93 R19W SW 1/4 SE 1/4 Sec. 7.42.87887400, -93.13261500332Prairie remnant on south and southwestern aspects of 15-25 degree slopes.Wild materialPlants in nature measuring approximately 30-38" in height. 2168178Ames 36255
11NA 88834RJL-RM2023FLAL-008Rhododendron canescens (Michx.) Sweet Florida, United StatesNA2023COLLECTED12/06/2023Blackwater State Forest: plants are growing in wetlands accessed by foot from Buddy Hardy Road. The collection site is approximately 0.14 kilometers west and downhill from the road.30.80736700, -86.9578470053Growing in shade to part-shade of the well-drained moist mesic habitat about 1 m above the wetland which appears to be formed by a nearby hillside seepage area. In this zone there are numerous facultative wetland species as well as high competition from facultative upland plants. Slope: 5 to 10 percent. Aspect: Variable. The underlying geology of this area is the Citronelle Formation of Pliocene origin and 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. (Source: USGS Florida Geologic Map Data.) The Troup Series (5 to 8% slopes) consists of very deep, somewhat excessively drained soil formed in unconsolidated sandy and loamy marine sediments. Troup soils are on ridges and hillslopes. The upper 0-13 cm is comprised primarily of decomposing sphagnum peat with a significant amount of fibrous root content. From 15-112 cm the soil is comprised primarily of fine-grained yellowish-brown sand with varying amounts of root content; this zone is strongly acid. From 112-203 cm the soil is comprised of light-red to red sandy clay loam that is discontinuous, generally friable, and strongly acid. (Source: NRCS Web Soil Survey.)Wild material2165664NA 88834
12NA 88835RJL-RM2023FLAL-009Rhododendron viscosum (L.) Torr. Florida, United StatesNA2023COLLECTED12/06/2023Blackwater State Forest: plants are growing in wetlands accessed by foot from Buddy Hardy Road. The collection site is approximately 0.14 kilometers west and downhill from the road.30.80841000, -86.9628330043Growing in part-shade of the well-drained moist-dry mesic habitat about 2-3 m above the wetland. In this zone there are numerous facultative wetland species as well as high competition from facultative upland plants. Slope: 5 to 10 percent. Aspect: Variable. The underlying geology of this area is the Citronelle Formation of Pliocene origin and 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. (Source: USGS Florida Geologic Map Data.) The Troup Series (5 to 8% slopes) consists of very deep, somewhat excessively drained soil formed in unconsolidated sandy and loamy marine sediments. Troup soils are on ridges and hillslopes. The upper 0-13 cm is comprised primarily of decomposing sphagnum peat with a significant amount of fibrous root content. From 15-112 cm the soil is comprised primarily of fine-grained yellowish-brown sand with varying amounts of root content; this zone is strongly acid. From 112-203 cm the soil is comprised of light-red to red sandy clay loam that is discontinuous, generally friable, and strongly acid. (Source: NRCS Web Soil Survey.)Wild material2165665NA 88835
13OPGC 8810CBG- 10773Penstemon pallidus Small Illinois, United StatesOPGC2023Wild material2142241OPGC 8810
14OPGC 8823CBG- 10813Physostegia virginiana (L.) Benth. Illinois, United StatesOPGC2023Wild material2142270OPGC 8823
15OPGC 8830CBG- 10835Solidago riddellii Frank Illinois, United StatesOPGC2023Wild material2142284OPGC 8830
16NA 88525RM-TK2022-013Macranthera flammea (W. Bartram) Pennell Florida, United StatesNA2023COLLECTED11/04/2022Growing in wetland in Blackwater River State Forest.30.80870000, -86.9627000042Plants are typically found growing in part shade to sun in saturated streamside wetland/seep areas at the base of the slope in sphagnum moss. This appears to be year-round wetland habitat.
Soils: The underlying geology of this area is the Citronelle Formation of Pliocene origin and 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. Source: USGS Florida Geologic Map Data (https://mrdata.usgs.gov/geology/state/state.php?state=fl)
The surface soil profile found in this area is primarily Troup Series. These soils are sandy and loamy marine deposits. They are well drained and typically on the tops and sides of broad and narrow ridges on uplands typically with 0-12% slopes. These soils are very strongly acid with a depth of 2-3 meters. Pactolus Series soils comprise a minor, but important percentage of the lower slopes that are nearly level to gently sloping and account for the somewhat poorly drained, yet, sandy conditions. These soils are also strongly acid with very dark gray loamy sands.
Source: Soil Survey of Santa Rosa County and NRCS Web Soil Survey (https://www.nrcs.usda.gov/Internet/FSE_MANUSCRIPTS/florida/FL113/0/SantaRosa.pdf and https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)
Wild material2140806NA 88525
17NA 88530RJLSEUS2022-001Oxydendrum arboreum (L.) DC. North Carolina, United StatesNA2023COLLECTED12/06/2022Plants growing around a wetland on both sides of Scotland Lake Road, approximately 1.1 kilometers southwest of the junction with Hoffman Road (Scotland Co. Road 1328) in the Sandhills Game Lands. This plant is a common component along the mesic/moist boundary on the upper edge of the understory shrub in the moist woodland habitat not far from the wetland. 34.98402000, -79.54267200116Plants are growing in full sun to part-shade in the moist, well-drained, mesic conditions just above a wetland area occupied by obligate wetland species. The underlying geology of this area is of Tertiary origin and characterized as Pinehurst Formation. It is composed of medium- to coarse-grained sand as well as cross-bedding and rhythmic bands of clayey sand that are unconsolidated.
Source: USGS North Carolina Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=NCTp%3B11)
The primary soil type in the collection area is Pelion Loamy Sand soil (6 to 10 percent slopes). The Pelion Loamy Sand series consists of very deep, moderately well-drained marine deposits, fluviomarine deposits, and sand sheets. Permeability is moderately slow or slow. Surface layers 0-25 cm deep are comprised of loamy sand with a weak fine granular structure and are very friable. Deeper horizons are comprised of sandy loam, sandy clay loam, or clay loam in the upper part and include sandy clay or clay in the deepest strata. Soils are extremely acid to strongly acid.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)
Wild material2140759NA 88530
18NA 88531RJLSEUS2022-002Cyrilla racemiflora L. North Carolina, United StatesNA2023COLLECTED12/06/2022Plants growing around a wetland on both sides of Scotland Lake Road, approximately 1.1 kilometers southwest of the junction with Hoffman Road (Scotland Co. Road 1328) in the Sandhills Game Lands. This plant is a common component of moist to wet areas of the wetland habitats in this area. 34.98418000, -79.54079800120Plants are growing in part-shade to sun in a wetland habitat as well as nearby seasonally drier mesic habitat.
Soils: The underlying geology of this area is of Tertiary origin and characterized as Pinehurst Formation. It is comprised of medium- to coarse-grained sand as well as cross-bedding and rhythmic bands of clayey sand that are unconsolidated.
Source: USGS North Carolina Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=NCTp%3B11)
The primary soil type in the collection area is classified as Johnston Series soils (0 to 2 percent slopes, frequently flooded). The Johnston series consists of very deep, very poorly drained soils that are occasionally to frequently flooded for short to extended periods. Permeability is moderate to rapid. These nearly level soils are alluvial in origin and typical of floodplains and swamp. Slopes range from 0 to 2 percent. Johnston Series soils are comprised of mucky loam that is friable with siliceous elements in the upper 0-75 cm. Lower strata range in percentages of mucky loam and loamy fine sand.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)
Wild material2140760NA 88531
19NA 88532RJLSEUS2022-003Alnus serrulata (Aiton) Willd. North Carolina, United StatesNA2023COLLECTED12/06/2022Plants growing around a wetland on both sides of Scotland Lake Road, approximately 1.1 kilometers southwest of the junction with Hoffman Road (Scotland Co. Road 1328) in the Sandhills Game Lands. This plant is a common component of the moist to wet areas of the wetland habitats in this area. 34.98413200, -79.54196300118Plants are growing in part-shade to sun in a wet to inundated habitat that contains standing water and/or significant moisture year-round.
Soils: The underlying geology of this area is of Tertiary origin and characterized as Pinehurst Formation. It is comprised of medium- to coarse-grained sand as well as cross-bedding and rhythmic bands of clayey sand that are unconsolidated.
Source: USGS North Carolina Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=NCTp%3B11)
The primary soil type in the collection area is classified as Johnston Series soils (0 to 2 percent slopes, frequently flooded). The Johnston series consists of very deep, very poorly drained soils that are occasionally to frequently flooded for short to extended periods. Permeability is moderate to rapid. These nearly level soils are alluvial in origin and typical of floodplains and swamp. Slopes range from 0 to 2 percent. Johnston Series soils are comprised of mucky loam that is friable with siliceous elements in the upper 0-75 cm. Lower strata range in percentages of mucky loam and loamy fine sand.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)
Wild material2140761NA 88532
20NA 88533RJLSEUS2022-004Zenobia pulverulenta (W. Bartram ex Willd.) Pollard North Carolina, United StatesNA2023COLLECTED12/06/2022Plants growing in the wetlands and moist depressions along Scotland Co. Road 1328 in the Sandhills Game Lands. This plant is somewhat infrequent and sporadic, but abundant in places with moist to wet habitats in this area. 34.95510000, -79.51769700112Plants are growing in part-shade to sun in an acidic wetland habitat rich in sphagnum and other obligate wetland species. The habitat is moist to wet year-round and periodically has surface runoff occurring; even so, this habitat can become quite dry during seasonal periods without rainfall.
Soils: The underlying geology of this area is of Tertiary origin and characterized as Pinehurst Formation. It is comprised of medium- to coarse-grained sand as well as cross-bedding and rhythmic bands of clayey sand that are unconsolidated.
Source: USGS North Carolina Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=NCTp%3B11)
The primary soil type in the collection area is classified as Pelion Loamy Sand (2 to 6 percent slopes). The Pelion Loamy Sand series consists of very deep, moderately well-drained marine deposits, fluviomarine deposits, and sand sheets. Permeability is moderately slow or slow. Surface layers 0-25 cm deep are comprised of loamy sand with a weak fine granular structure and are very friable. Deeper horizons are comprised of sandy loam, sandy clay loam, or clay loam in the upper part and includes sandy clay or clay in the deepest part. Soils are extremely acid to strongly acid.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)
Wild material2140762NA 88533
21Ames 35906Turkey Mounds State PreserveHeuchera richardsonii R. Br. Iowa, United StatesNC72022COLLECTED07/30/2022Turkey River Mounds State Preserve located 5.50 miles south, southeast of Guttenberg, T91N R2W SE ¼ NE ¼ Sec. 11.42.71399000, -91.03844000228Narrow ridge with precipitous bluffs rising 250 feet above the Mississippi River floodplainWild material2139635Ames 35906
22OPGC 8308CBG-10449Krigia biflora (Walter) S. F. Blake Wisconsin, United StatesOPGC2021Wild material2120088OPGC 8308
23W6 59136CBG-10266Dasiphora fruticosa (L.) Rydb. Wisconsin, United StatesW62021Wild material2120062W6 59136
24W6 59171CBG-10456Carex annectens (E. P. Bicknell) E. P. Bicknell Illinois, United StatesW62021Wild material2120093W6 59171
25W6 59175CBG-10462Scirpus pendulus Muhl. Illinois, United StatesW62021Wild material2120097W6 59175
26W6 59278CBG-10602Schizachyrium scoparium (Michx.) Nash Illinois, United StatesW62021Wild materialPlant numbers sampled estimated.2120187W6 59278
27OPGC 8595CBG-10732Castilleja coccinea (L.) Spreng. OPGCSEED2021Wild materialYellow flower form.2137984OPGC 8595
28Ames 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
29W6 52029WY070-73Dalea candida Willd. Wyoming, United StatesW62017Wild material1947162W6 52029
30Ames 29940196532Sphaeralcea coccinea (Nutt.) Rydb. Colorado, United StatesNC7SEED2005COLLECTED07/22/2003Hayden Park (Ecoregion 20), West Alameda Parkway, park trailhead on the right.39.69333000, -105.155000001944Foothills.Wild materialForb 0.07 meters tall. 1674186Ames 29940
31Ames 28230CP12Helenium autumnale L. Ohio, United StatesNC72004COLLECTED10/07/2004Chaparral Prairie State Nature Preserve, 3 miles northwest of West Union, Adams County.38.83583333, -83.57361111Cedar barrens prairie; along pond edge. Site size 10 square meters; 67 acre total area. Associated with Baptisia australis, Coreopsis tripteris, Eryngium yuccafolium, Liatris spicata, Physostegia virginiana, Pycnanthemum tenuifolium, Ratibida pinnata, and Rudbeckia hirta.Wild material2-3 feet in height.1690609Ames 28230