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ACCESSIONPLANT NAMETAXONOMYORIGINGENEBANKIMAGEAVAILABILITYRECEIVEDSOURCE TYPESOURCE DATECOLLECTION SITECOORDINATESELEVATIONHABITATIMPROVEMENT LEVELNARRATIVE
0W6 62531FWS0300-137Eutrochium maculatum (L.) E. E. Lamont Michigan, United StatesW6SEED2025Wild materialThe above acreage and population size are for the dense patch near the gate, including the portion of the patch not on sanctuary property.2192229W6 62531
1WLP 3137TJK2023AL-001Cornus alternifolia L. f. Alabama, United StatesNA2023COLLECTED08/15/2023Claiborne Bluffs, above the Alabama River.31.54883000, -87.5141700016Slope: 35%. Aspect: West-northwest. Elevation recorded as 52 feet.Wild materialWLPGR contract collection.2158469WLP 3137
2OPGC 8848CBG- 10860Solidago riddellii Frank Illinois, United StatesOPGC2023Wild material2142306OPGC 8848
3OPGC 8849CBG- 10861Chelone glabra L. Illinois, United StatesOPGC2023Wild material2142307OPGC 8849
4WLP 2668RJL2022MD-014Aronia arbutifolia (L.) Pers. Maryland, United StatesNA2022COLLECTED10/05/2022Plant growing at Elkton State Forest along road in wet woodlands near the Elk Neck State Forest Shooting Range labelled as the address of 717 Irishtown Rd, North East, MD 21901. Plant is uncommon at this site. 39.58716100, -75.9141900055Plants are growing in part-shade to part sun of a deciduous forest on hummocks in a very moist to wet low-lying area along a seasonal or year-round flowing seep.
Soils: The underlying geology of this area is of Cretaceous origin and comprised of Potomac Group, including Raritan and Patapsco Formations, and Patuxent Formation. The Potomac Group includes: interbedded quartzose gravels; proto-quartzitic to orthoquartzitic argillaceous sands; and white, dark gray, and multicolored silts and clays. Included withing this zone are Raritan and Patapsco Formations comprised of gray, brown, and red variegated silts and clays; lenticular, cross-bedded, argillaceous, subrounded sands; minor gravels; thickness. The Patuxent Formation is also interbedded in this zone and comprised of white or light gray to orange-brown, moderately sorted, cross-bedded, argillaceous, angular sands and subrounded quartz gravels; silts and clays subordinate that are predominantly pale gray.
Source: USGS Maryland Geologic Map Data https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=MDKp%3B5
The primary soil types in the collection area are classified as Russett-Christiana-Hambrook Complex and/or Sassafras and Croom Soils; though, others may intersect and overlay in specific areas. The soils in the collecting area are generally described as a complex series of fluviomarine deposits. The soils range from a thin loam layer at the surface to varying levels of loam to sandy loam and/or extremely gravelly sandy clay loam strata, depending upon geographical location (ie. Hillslope summits, slopes, footslopes, swales, etc.).
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)
Wild material2139659WLP 2668
5NA 89043RJL2022MD-017Cephalanthus occidentalis L. Maryland, United StatesNA2022COLLECTED10/05/2022Plants growing at Elkton State Forest along road and in wet woodlands near the Elk Neck State Forest Shooting Range labelled as the address of 717 Irishtown Rd, North East, MD 21901. Plants are locally common but restricted to the low-lying wet woodlands. 39.58727700, -75.9140390055Plants are growing in part-shade to part-sun of deciduous forests on hummocks in very moist to wet low-lying areas along seasonal or year-round flowing seeps.
Soils: The underlying geology of this area is of Cretaceous origin and comprised of Potomac Group, including Raritan and Patapsco Formations, and Patuxent Formation. The Potomac Group includes: interbedded quartzose gravels; proto-quartzitic to orthoquartzitic argillaceous sands; and white, dark gray, and multicolored silts and clays. Included withing this zone are Raritan and Patapsco Formations comprised of gray, brown, and red variegated silts and clays; lenticular, cross-bedded, argillaceous, subrounded sands; minor gravels; thickness. The Patuxent Formation is also interbedded in this zone and comprised of white or light gray to orange-brown, moderately sorted, cross-bedded, argillaceous, angular sands and subrounded quartz gravels; silts and clays subordinate that are predominantly pale gray.
Source: USGS Maryland Geologic Map Data https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=MDKp%3B5
The primary soil types in the collection area are classified as Russett-Christiana-Hambrook Complex and/or Sassafras and Croom Soils; though, others may intersect and overlay in specific areas. The soils in the collecting area are generally described as a complex series of fluviomarine deposits. The soils range from a thin loam layer at the surface to varying levels of loam to sandy loam and/or extremely gravelly sandy clay loam strata, depending upon geographical location (ie. Hillslope summits, slopes, footslopes, swales, etc.).
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)
Wild material2139608NA 89043
6NA 89042RJL2022MD-016Aronia ×prunifolia (Marshall) Rehder Maryland, United StatesNA2022COLLECTED10/05/2022Plants growing at Elkton State Forest along road and in wet woodlands near the Elk Neck State Forest Shooting Range labelled as the address of 717 Irishtown Rd, North East, MD 21901. Plants are infrequent and were found in this one area of low-lying wet woodlands. Perhaps others would have been found upon investigation of other similar habitats.39.58730200, -75.9141580055Plants are growing in part-sun to part-shade of deciduous forests on moist slopes and on hummocks in very moist to wet low-lying areas along seasonal or year-round flowing seeps.
Soils: The underlying geology of this area is of Cretaceous origin and comprised of Potomac Group, including Raritan and Patapsco Formations, and Patuxent Formation. The Potomac Group includes: interbedded quartzose gravels; proto-quartzitic to orthoquartzitic argillaceous sands; and white, dark gray, and multicolored silts and clays. Included withing this zone are Raritan and Patapsco Formations comprised of gray, brown, and red variegated silts and clays; lenticular, cross-bedded, argillaceous, subrounded sands; minor gravels; thickness. The Patuxent Formation is also interbedded in this zone and comprised of white or light gray to orange-brown, moderately sorted, cross-bedded, argillaceous, angular sands and subrounded quartz gravels; silts and clays subordinate that are predominantly pale gray.
Source: USGS Maryland Geologic Map Data https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=MDKp%3B5
The primary soil types in the collection area are classified as Russett-Christiana-Hambrook Complex and/or Sassafras and Croom Soils; though, others may intersect and overlay in specific areas. The soils in the collecting area are generally described as a complex series of fluviomarine deposits. The soils range from a thin loam layer at the surface to varying levels of loam to sandy loam and/or extremely gravelly sandy clay loam strata, depending upon geographical location (ie. Hillslope summits, slopes, footslopes, swales, etc.).
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)
Wild material2139607NA 89042
7NA 89041RJL2022MD-015Lyonia ligustrina (L.) DC. Maryland, United StatesNA2022COLLECTED10/05/2022Plants growing at Elkton State Forest along road and in wet woodlands near the Elk Neck State Forest Shooting Range labelled as the address of 717 Irishtown Rd, North East, MD 21901. Plants are common but scattered on the edges and in the understory of low-lying wet woodlands. 39.58716100, -75.9141900055Plants are growing in part-shade to shade of deciduous forests on moist slopes and on hummocks in very moist to wet low-lying areas along seasonal or year-round flowing seeps.
Soils: The underlying geology of this area is of Cretaceous origin and comprised of Potomac Group, including Raritan and Patapsco Formations, and Patuxent Formation. The Potomac Group includes: interbedded quartzose gravels; proto-quartzitic to orthoquartzitic argillaceous sands; and white, dark gray, and multicolored silts and clays. Included withing this zone are Raritan and Patapsco Formations comprised of gray, brown, and red variegated silts and clays; lenticular, cross-bedded, argillaceous, subrounded sands; minor gravels; thickness. The Patuxent Formation is also interbedded in this zone and comprised of white or light gray to orange-brown, moderately sorted, cross-bedded, argillaceous, angular sands and subrounded quartz gravels; silts and clays subordinate that are predominantly pale gray.
Source: USGS Maryland Geologic Map Data https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=MDKp%3B5
The primary soil types in the collection area are classified as Russett-Christiana-Hambrook Complex and/or Sassafras and Croom Soils; though, others may intersect and overlay in specific areas. The soils in the collecting area are generally described as a complex series of fluviomarine deposits. The soils range from a thin loam layer at the surface to varying levels of loam to sandy loam and/or extremely gravelly sandy clay loam strata, depending upon geographical location (ie. Hillslope summits, slopes, footslopes, swales, etc.).
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)
Wild material2139606NA 89041
8NA 89040RJL2022MD-013Eubotrys racemosus (L.) Nutt. Maryland, United StatesNA2022COLLECTED10/05/2022Plants growing at Elkton State Forest along road and in wet woodlands over a distance of about 0.55 kilometers near the Elk Neck State Forest Shooting Range labelled as the address of 717 Irishtown Rd, North East, MD 21901. Plants are common but scattered on the edges and in the understory of low-lying wet woodlands. 39.58227200, -75.9132880057Plants are growing in part-shade to shade of deciduous forests on moist slopes and on hummocks in very moist to wet low-lying areas along seasonal or year-round flowing seeps.
Soils: The underlying geology of this area is of Cretaceous origin and comprised of Potomac Group, including Raritan and Patapsco Formations, and Patuxent Formation. The Potomac Group includes: interbedded quartzose gravels; proto-quartzitic to orthoquartzitic argillaceous sands; and white, dark gray, and multicolored silts and clays. Included withing this zone are Raritan and Patapsco Formations comprised of gray, brown, and red variegated silts and clays; lenticular, cross-bedded, argillaceous, subrounded sands; minor gravels; thickness. The Patuxent Formation is also interbedded in this zone and comprised of white or light gray to orange-brown, moderately sorted, cross-bedded, argillaceous, angular sands and subrounded quartz gravels; silts and clays subordinate that are predominantly pale gray.
Source: USGS Maryland Geologic Map Data https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=MDKp%3B5
The primary soil types in the collection area are classified as Russett-Christiana-Hambrook Complex and/or Sassafras and Croom Soils; though, others may intersect and overlay in specific areas. The soils in the collecting area are generally described as a complex series of fluviomarine deposits. The soils range from a thin loam layer at the surface to varying levels of loam to sandy loam and/or extremely gravelly sandy clay loam strata, depending upon geographical location (ie. Hillslope summits, slopes, footslopes, swales, etc.).
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)
Wild material2139605NA 89040
9Ames 36049CBG-9991Helianthus mollis Lam. Illinois, United StatesNC72021Wild material2120041Ames 36049
10W6 59136CBG-10266Dasiphora fruticosa (L.) Rydb. Wisconsin, United StatesW62021Wild material2120062W6 59136
11W6 59137CBG-10267Muhlenbergia glomerata (Willd.) Trin. Wisconsin, United StatesW62021Wild material2120195W6 59137
12OPGC 8180NEWFS-473Solidago rugosa Mill. Massachusetts, United StatesOPGC2021Wild material2115663OPGC 8180
13OPGC 8181NEWFS-474Solidago altissima L. Massachusetts, United StatesOPGC2021Wild materialLeaves primarily three-veined, toothing infrequent and not flared. Plants often tall.2115664OPGC 8181
14OPGC 8182NEWFS-475Solidago canadensis L. Massachusetts, United StatesOPGC2021Wild materialThree-veined leaves with frequent, flared teeth.2115665OPGC 8182
15Ames 35337JDC/SP/2020/002/923Salix pedicellaris Pursh Iowa, United StatesNC7FLOWER2020COLLECTED06/05/2020Pilot Knob State Preserve (Floating Bog) located approximately 3.66 miles east, southeast of Forest City, area just west of Dead Mans Lake, T97N R23W NW1/4 NW1/4 SE1/4 Sec. 4, Hancock County43.24868300, -93.56644900406Extremely high-quality remnant floating bog that has never been hydrologically altered. Very diverse habitat.Wild materialSalix pedicellaris is extremely rare in Iowa only found in the northern tiers of counties. Currently listed as a state threatened plant species and thus tracked via the Iowa Natural Areas Inventory Program (Iowa Department of Natural Resources). Only 15 sites throughout Iowa representing 13 counties have documented S. pedicellaris. Since the year 2000, only two reports (observation/herbarium specimen) have documented the species presence in Iowa. Bog willow is a small shrub (<2 meters) typically with few, short stems often hidden amongst sedges. Spreads clonally via suckering and/or layering lending it to be found in stable fen habitats with ample supply of water that see little to no distrurbance. Spring flowering typically occurring in mid-May to early June with fruiting occurring in early June in Iowa. Little to no existance in cultivation. Leaves are rather waxy and repel water significantly. During a growout of original plant material (sampled as cuttings from collection site in nature) at NCRPIS, a total of 45 genets were determined to be female (14 count) and male (31 count) during peak flowering on 4 May 2022. 2105808Ames 35337
16W6 57090MARSB-233Carex lurida Wahlenb. New York, United StatesW6SEED2019Wild material2097529W6 57090
17W6 54027MARSB-232Schoenoplectus pungens (Vahl) Palla New York, United StatesW6SEED2018Wild materialSchoenoplectus pungens1964743W6 54027
18Ames 32955JDC/BP/2015/042/699Betula pumila L. Iowa, United StatesNC72015COLLECTED09/04/2015Private property approximately 7 miles northwest of Cedar Falls, T90N R14W SW 1/4 NW 1/4 SE 1/4 Sec. 18.42.60398800, -92.54284800284High-quality remnant wetland/fenWild materialSpecimens sampled averaged approximately 278 cm in height, ranging from 250 cm to 330 cm. Female catkins were both green and brown at time of harvest. Little to no fall color at time of seed collection (4 Sept. 2015) with approximately 75% of leaves already dropped. During growout in 2016, samples #699-3 and #699-5 resulted in seedlings that have petiolules (on small seedlings) that average 3-5 mm in length with the leaf apex being rather sharply acute, possibly indicating presence of hybrids. Other samples (#699-1, #699-2, #699-6, and #699-7) seem to exhibit characteristics of B. pumila with densely pubescent leaves and stems, with leaves having the apex usually broadly acute or obtuse to rounded, and essentially leaves being sessile or less than 1mm in length. 1927397Ames 32955