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ACCESSIONPLANT NAMETAXONOMYORIGINGENEBANKIMAGEAVAILABILITYRECEIVEDSOURCE TYPESOURCE DATECOLLECTION SITECOORDINATESELEVATIONHABITATIMPROVEMENT LEVELNARRATIVE
0NA 88440MARSB-419Rosa virginiana Mill. New York, United StatesNASEED2019Wild material2097623NA 88440
1NA 890812024RJLPA-009Rosa carolina L. Pennsylvania, United StatesNA2024COLLECTED09/22/2024Lancaster and York Counties: outcrops along the Susquehanna River, accessed from the Historic Lock 12 parking lot off of Pennsylvania Road 372.39.81483500, -76.3276220034Plants are growing from part-sun to full sun in crevices of the outcrops and where organic debris has accumulated in between boulders along the Susquehanna River. The sites range from nearly xeric to dry mesic, at least on the surface. Plants are generally growing 4-10 m above the normal flow of the river; however, the Holtwood Dam is less than 1 kilometer upstream and debris found trapped in the boulders indicates that there is periodic flooding, at least, in the lower zone of 4+ meters or so above normal river flow. This habitat has a diverse assemblage of deciduous trees and shrubs as well as abundant herbaceous taxa. Slope: 0 to 60 percent. Aspect: Northeast (generally). Geology: The underlying geology of this area is probably of lower Paleozoic age and characterized as the Octoraro Formation. It includes albite-chlorite schist, phyllite, some hornblende gneiss, and granitized members. Soils: The area where this species occurs is right on the edge of two soil zones that transition from the river’s edge to mesic conditions upslope. The first is generally referred to as Rock Outcrop. This terrestrial matrix in which plants grow is largely exposed underlying rock geology with accumulated outwash, rock decomposition, and organic debris buildup. The second is Mt. Airy (80%) and Manor (20%) Series soils, 25 to 60 percent slopes, extremely stony (MRF). (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). EPA Ecoregion (Level III): Northern Piedmont (64). EPA Ecoregion (Level IV): Piedmont Uplands (64c).Wild material2169045NA 89081
2NA 88542RJLSEUS2022-014Rosa palustris Marshall Georgia, United StatesNA2023COLLECTED12/09/2022Plants growing around a pond and associated wetland on the property of Monica Williams north of Albany, Georgia. Common along the transitional edges from wet to dry.31.63723900, -84.1377620060Plants are growing in full sun mostly in the transitional edges of the pond where conditions are generally moist mesic. Even so, this species appears quite adaptable and can be found in quite moist as well as drier soil conditions.
Soils: The underlying geology of this area is of Eocene origin and characterized as Ocala Limestone. The Ocala Limestone consists of almost pure limestones with occasional dolomites. It can be subdivided into both lower and upper facies with the lower facies composed of a whitish to cream-colored, fine to medium grained, poorly to moderately hard, fossil rich grainstone and packstone. The upper Ocala is white and somewhat weak and poorly sorted. It is extremely fossil rich grainstone, packstone and wackestone and some chert is common in the upper facies.
Source: USGS Georgia Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=GANu%3B1)
The primary soil types in the collection area are classified as Herod and Muckalee Series soils. The Herod Series consists of poorly drained moderately permeable soils formed in loamy alluvium. These soils are on flood plains of streams in the Coastal Plain. Slopes range from 0 to 2 percent. The Muckalee Series consists of poorly drained moderately permeable soils formed in loamy and sandy alluvium. These soils are on flood plains of streams in the Coastal Plain. Slopes range from 0 to 2 percent.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)
Wild material2140817NA 88542
3NA 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
4NA 88439CBG-10597Rosa setigera Michx. Illinois, United StatesNA2021Wild materialPlant numbers sampled estimated.2120182NA 88439
5WLP 1686APS/RS/2019/067/396Rosa setigera Michx. Arkansas, United StatesNAFRUIT2019COLLECTED11/07/2019Located near intersection of Smith Mountain Road and Newton County 8828 Road approximately 6.00 miles north of Deer, Newton County35.91212000, -93.21112000636Roadside, upland with rocky soilsWild material2097789WLP 1686
6WLP 1685JDC/RS/2019/036/915Rosa setigera Michx. Iowa, United StatesNAFRUIT2019COLLECTED10/17/2019Ledges State Park located approximately 4.75 miles south of Boone, just south of the Oakwoods Shelter/Picnic area, T83N R26W NE1/4 NE1/4 and also NW1/4 NE1/4 Sec. 21, Boone County41.99262400, -93.87724800330Edges of woods (adjacent to prairie) and also within 20-25 yards from woods in prairie. Noted in east, west, and south-facing edges of woods (no specimens noted on north-facing woodland edges)Wild materialWoody shrub/vine stretching up to 12' in length. Alternate compound leaves usually consisting of five lealets. Leaf rachis and stipule margins glandular. Mature hypanthium and pedicel with stipitate glandular hairs. Mature hypanthium mostly bright to dark red in color with a few dark orange noted at time of harvest (17 October 2019). Leaves rather to somewhat glossy. This collection represents genetics from the northwestern edge of the species range, likely suggesting good cold-hardiness (USDA Zone 5a). 2097769WLP 1685
7NA 88443NV040-344Rosa woodsii Lindl. Nevada, United StatesNASEED2019Wild material2094595NA 88443
8NA 88434NEWFS-740Rosa palustris Marshall Massachusetts, United StatesNASEED2019Wild material1976342NA 88434
9PI 616950F. virginiana subsp. virginiana NC 98-14-2Fragaria virginiana Mill. subsp. virginiana Tennessee, United StatesCOROut of Season2000COLLECTED09/27/1998Ceders of Lebanon State Forest. 0.7 mile down State Forest road from the 'Pork'. Road edge on the right and 3 to 4 miles into a very large cedar glade. Wilson county.36.07361000, -86.31056000340Cedar glade with typical vegetation. Pimarily growing through a mat of mosses. Some plants suffering from severe drought. Rhus aromatica, Rosa sp. and Rhamus caroliniana occasional to scattered.Wild material1603162PI 616950
10PI 616833F. virginiana subsp. virginiana NC 96-45-1Fragaria virginiana Mill. subsp. virginiana South Carolina, United StatesCOROut of Season1996COLLECTED07/20/1996Left roadside both north and south of Little River, 6.3 miles south of Clinton on SC 72, Laurens county, South Carolina.34.38694000, -81.94444000Fragaria virginiana occasional on dry roadbanks over about 300 yards along road. Rosa carolina also associated with strawberry.Wild materialUSDA Sponsored plant collecting expedition, 19961535626PI 616833
11PI 616835F. virginiana subsp. virginiana NC 96-45-3Fragaria virginiana Mill. subsp. virginiana South Carolina, United StatesCOROut of Season1996COLLECTED07/20/1996Left roadside both north and south of Little River, 6.3 miles south of Clinton on SC 72, Laurens county, South Carolina.34.38694000, -81.94444000Fragaria virginiana occasional on dry roadbanks over about 300 yards along road. Rosa carolina also associated with strawberry.Wild materialUSDA Sponsored plant collecting expedition, 19961535628PI 616835
12PI 616836F. virginiana subsp. virginiana NC 96-45-4Fragaria virginiana Mill. subsp. virginiana South Carolina, United StatesCOROut of Season1996COLLECTED07/20/1996Left roadside both north and south of Little River, 6.3 miles south of Clinton on SC 72, Laurens county, South Carolina.34.38694000, -81.94444000Fragaria virginiana occasional on dry roadbanks over about 300 yards along road. Rosa carolina also associated with strawberry.Wild materialUSDA Sponsored plant collecting expedition, 19961535629PI 616836
13PI 616837F. virginiana subsp. virginiana NC 96-46-1Fragaria virginiana Mill. subsp. virginiana South Carolina, United StatesCOROut of Season1996COLLECTED07/20/1996Roadside on the right just above the Tyger River, 0.3 mile north of the town limits of Cross Anchor, on county road 56 , Spartonbury county, South Carolina.34.69167000, -81.83250000One scattered colony of Fragaria virginiana growing on the dry shoulder of the road. Rosa carolina also on the site. Climbing milkweed between the site and the river.Wild materialUSDA Sponsored plant collecting expedition, 19961535630PI 616837
14NA 88389NEWFS-739Juniperus virginiana L. var. virginiana Massachusetts, United StatesNA2021Wild materialSmall conical shrub with waxy blue green fruits and tight scale like leaves.2138832NA 88389
15NA 88081NEWFS-739Juniperus virginiana L. var. virginiana Massachusetts, United StatesNASEED2019Wild material1976341NA 88081
16GPRU 170NV030-1334Prunus virginiana L. California, United StatesGENSEED2018COLLECTED09/25/2017From US-395N from Reno, turn L onto CA-70W to Chilcoot. Turn R onto CA-284N towards Frenchman Lake, and continue 7 miles until Cornus patch.39.87549000, -120.183700001623Wild material1970658GPRU 170
17WLP 2435CBG-1797Prunus virginiana L. Wyoming, United StatesNASEED2013COLLECTED09/06/20111727Stream gulch with wetter soils within Western Rocky Mountain foothills.Wild material1908924WLP 2435
18WLP 2346NV030-220Prunus virginiana L. California, United StatesNASEED2009COLLECTED10/15/2008Bank of the Truckee River, from Floriston exit off 80W coming from Reno, Nevada.Riparian community along river; site is used for recreation; soil consists of rocks, gravel, and sandWild materialNo thorns present. Ht: 1-3 meters.1808200WLP 2346
19WLP 2120302025Juniperus virginiana L. Virginia, United StatesNASEED2008COLLECTED12/28/200589Slope: 0 Aspect: NE Soil: Clay-loam, Land form: Upland meadow. Mowed.Wild material1780179WLP 2120
20PI 704849 sosR. flagellaris MARSB-128Rubus flagellaris Willd. New Jersey, United StatesCORSEED2019Wild material2097493PI 704849 sos
21PI 656821Ames 27283Physocarpus opulifolius (L.) Maxim. Iowa, United StatesNC72003COLLECTED09/06/2003Above Cedar River, along River Road, southeast of Mitchell, extreme SE corner of Section 8 and NE corner of Section 17, T98N, R17W, Osage Quad, Mitchell County.43.31277778, -92.87166667332Base of west-facing limestone bluff. Wild materialLarge, floriferous shrubs.1648679PI 656821
22PI 635465H. lupulus var. neomexicanus OCJ-42Humulus lupulus L. var. neomexicanus A. Nelson & Cockerell Colorado, United StatesCOR2002COLLECTED09/16/2002North of Poncha Springs along the Arkansas River on U.S.-285 Two miles north of Nathrop turn north on County Road 301 (C-301). Upstream from C-301 bridge, between C-301A and river.38.76778000, -106.097220002348Raparian; Salix sp., Prunus virginiana, Ribes aureum and Rosa sp.Wild material1642224PI 635465
23NA 890772024RJLPA-003Viburnum acerifolium L. Pennsylvania, United StatesNA2024COLLECTED09/19/2024Birdell Road, near parking lot to trail where the road ends at Chambers Lake, which is part of Hibernia County Park.40.03559500, -75.85708600187Plants are growing in deep shade of a dry deciduous forest dominated by Fagus grandifolia. Slope: 0 percent. Aspect: N/A. Geology: The underlying geology of this area is of Precambrian origin and characterized as Banded Mafic Gneiss. It is characterized as dark and fine to medium grained. This formation includes rocks of probable sedimentary origin; may be equivalent to "PZmgh." (Source: USGS Pennsylvania Geologic Map Data). Soils: The primary soil type in the area of this collection is classified as Neshaminy Series Silt Loam, very deep over mafic gneiss, 3 to 8 percent slopes (NvB). (Source: USDA-NRCS Official Soil Series Descriptions). EPA Ecoregion (Level III): Northern Piedmont (64). EPA Ecoregion (Level IV): Piedmont Uplands (64c).Wild material2169041NA 89077
24NA 890822024RJLPA-010Amorpha fruticosa L. Pennsylvania, United StatesNA2024COLLECTED09/22/2024Outcrops along the Susquehanna River, accessed from the Historic Lock 12 parking lot off of Pennsylvania Road 372.39.81481500, -76.3275790034Plants are growing from part-sun to full sun in crevices of the outcrops and where organic debris has accumulated in between boulders along the Susquehanna River. The sites range from nearly xeric to dry mesic, at least on the surface. Plants are generally growing 4-10 m above the normal flow of the river; however, the Holtwood Dam is less than 1 kilometer upstream and debris found trapped in the boulders indicates that there is periodic flooding, at least, in the lower zone of 4+ meters or so above normal river flow. This habitat has a diverse assemblage of deciduous trees and shrubs as well as abundant herbaceous taxa. Slope: 0 to 25 percent. Aspect: Northeast (generally). Geology: The underlying geology of this area is probably of lower Paleozoic age and characterized as the Octoraro Formation. It includes albite-chlorite schist, phyllite, some hornblende gneiss, and granitized members. Soils: The area where this species occurs is right on the edge of two soil zones that transition from the river’s edge to mesic conditions upslope. The first is generally referred to as Rock Outcrop. This terrestrial matrix in which plants grow is largely exposed underlying rock geology with accumulated outwash, rock decomposition, and organic debris buildup. The second is Mt. Airy (80%) and Manor (20%) Series soils, 25 to 60 percent slopes, extremely stony (MRF). (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). EPA Ecoregion (Level III): Northern Piedmont (64). EPA Ecoregion (Level IV): Piedmont Uplands (64c).Wild material2169046NA 89082
25NA 890832024RJLPA-012Rhododendron periclymenoides (Michx.) Shinners Pennsylvania, United StatesNA2024COLLECTED09/22/2024Outcrops along the Susquehanna River, accessed from the Historic Lock 12 parking lot off of Pennsylvania Road 372.39.81477400, -76.3280730035Plants are growing from shade to part-sun and occasionally full sun in crevices of the outcrops and where organic debris has accumulated in between boulders along the Susquehanna River. The sites range from nearly xeric to mesic, at least on the surface. Plants are generally growing 4-10 m above the normal flow of the river; however, the Holtwood Dam is less than 1 kilometer upstream and debris found trapped in the boulders indicates that there is periodic flooding, at least, in the lower zone of 4+ meters or so above normal river flow. This habitat has a diverse assemblage of deciduous trees and shrubs as well as abundant herbaceous taxa. Slope: 0 to 60 percent. Aspect: Northeast (generally). Geology: The underlying geology of this area is probably of lower Paleozoic age and characterized as the Octoraro Formation. It includes albite-chlorite schist, phyllite, some hornblende gneiss, and granitized members. Soils: The area where this species occurs is right on the edge of two soil zones that transition from the river’s edge to mesic conditions upslope. The first is generally referred to as Rock Outcrop. This terrestrial matrix in which plants grow is largely exposed underlying rock geology with accumulated outwash, rock decomposition, and organic debris buildup. The second is Mt. Airy (80%) and Manor (20%) Series soils, 25 to 60 percent slopes, extremely stony (MRF). (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). EPA Ecoregion (Level III): Northern Piedmont (64). EPA Ecoregion (Level IV): Piedmont Uplands (64c).Wild material2169047NA 89083
26NA 890842024RJLPA-013Physocarpus opulifolius (L.) Maxim. Pennsylvania, United StatesNA2024COLLECTED09/22/2024Outcrops along the Susquehanna River, accessed from the Historic Lock 12 parking lot off of Pennsylvania Road 372.39.81466300, -76.3283390036Plants are growing from shade to part-sun where organic debris has accumulated in between boulders as well as further upslope in deeper mesic soils along the Susquehanna River. This habitat has a diverse assemblage of deciduous trees and shrubs as well as abundant herbaceous taxa. Slope: 10 to 25 percent. Aspect: Northeast (generally). Geology: The underlying geology of this area is probably of lower Paleozoic age and characterized as the Octoraro Formation. It includes albite-chlorite schist, phyllite, some hornblende gneiss, and granitized members. Soils: The area where this species occurs is right on the edge of two soil zones that transition from the river’s edge to mesic conditions upslope. The first is generally referred to as Rock Outcrop. This terrestrial matrix in which plants grow is largely exposed underlying rock geology with accumulated outwash, rock decomposition, and organic debris buildup. The second is Mt. Airy (80%) and Manor (20%) Series soils, 25 to 60 percent slopes, extremely stony (MRF). (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). EPA Ecoregion (Level III): Northern Piedmont (64). EPA Ecoregion (Level IV): Piedmont Uplands (64c).Wild material2169048NA 89084
27NA 890852024RJLPA-014Rhododendron arborescens (Pursh) Torr. Pennsylvania, United StatesNA2024COLLECTED09/22/2024Outcrops along the Susquehanna River, accessed from the Historic Lock 12 parking lot off of Pennsylvania Road 372.39.81618100, -76.3306980038Plants are growing from shade to part-sun and occasionally full sun in crevices of the outcrops and where organic debris has accumulated in between boulders along the Susquehanna River. The sites range from nearly xeric to mesic, at least on the surface. Plants are generally growing 4-10 m above the normal flow of the river; however, the Holtwood Dam is less than 1 kilometer upstream and debris found trapped in the boulders indicates that there is periodic flooding, at least, in the lower zone of 4+ meters or so above normal river flow. This habitat has a diverse assemblage of deciduous trees and shrubs as well as abundant herbaceous taxa. Slope: 0 to 75 percent. Aspect: Northeast (generally). Geology: The underlying geology of this area is probably of lower Paleozoic age and characterized as the Octoraro Formation. It includes albite-chlorite schist, phyllite, some hornblende gneiss, and granitized members. Soils: The area where this species occurs is right on the edge of two soil zones that transition from the river’s edge to mesic conditions upslope. The first is generally referred to as Rock Outcrop. This terrestrial matrix in which plants grow is largely exposed underlying rock geology with accumulated outwash, rock decomposition, and organic debris buildup. The second is Mt. Airy (80%) and Manor (20%) Series soils, 25 to 60 percent slopes, extremely stony (MRF). (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). EPA Ecoregion (Level III): Northern Piedmont (64). EPA Ecoregion (Level IV): Piedmont Uplands (64c).Wild material2169049NA 89085
28NA 890862024RJLPA-015Ilex verticillata (L.) A. Gray Pennsylvania, United StatesNA2024COLLECTED09/22/2024Outcrops along the Susquehanna River, accessed from the Historic Lock 12 parking lot off of Pennsylvania Road 372.39.81656600, -76.3313660038Plants are growing from part-sun to full sun in crevices of the outcrops and where organic debris has accumulated in between boulders along the Susquehanna River. The sites range from nearly xeric to dry mesic, at least on the surface. Plants are generally growing 4-10 m above the normal flow of the river; however, the Holtwood Dam is less than 1 kilometer upstream and debris found trapped in the boulders indicates that there is periodic flooding, at least, in the lower zone of 4+ meters or so above normal river flow. This habitat has a diverse assemblage of deciduous trees and shrubs as well as abundant herbaceous taxa. Slope: 0 to 10 percent. Aspect: Northeast (generally). Geology: The underlying geology of this area is probably of lower Paleozoic age and characterized as the Octoraro Formation. It includes albite-chlorite schist, phyllite, some hornblende gneiss, and granitized members. Soils: The area where this species occurs is right on the edge of two soil zones that transition from the river’s edge to mesic conditions upslope. The first is generally referred to as Rock Outcrop. This terrestrial matrix in which plants grow is largely exposed underlying rock geology with accumulated outwash, rock decomposition, and organic debris buildup. The second is Mt. Airy (80%) and Manor (20%) Series soils, 25 to 60 percent slopes, extremely stony (MRF). (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). EPA Ecoregion (Level III): Northern Piedmont (64). EPA Ecoregion (Level IV): Piedmont Uplands (64c).Wild material2169050NA 89086
29Ames 36168Mount MagazinePtelea trifoliata L. Arkansas, United StatesNC7PLANT2023COLLECTED08/26/2023Mount Magazine State Park primarily localized to the northwest rim of the mountain along the trails heading west from Brown's Spring, T6N R25W Sec. 21.35.17130900, -93.65582200786Top of sky-island mountain. Localized along the rims just above steep cliffs on north facing slopes.Wild materialPlants in nature ranging from three to fifteen feet in height with peak bloom observed during the first week of May (2023). 2158787Ames 36168
30Ames 36153JDC/MM/2023/049/1081Monarda maxmedleyi J. J. N. Campb. & Floden Kentucky, United StatesNC7PLANT2023COLLECTED08/10/2023Lily Mountain Preserve located 6.92 miles west, southwest of South Irvine37.63661300, -84.09026400432Open dry, woods. Localized at highest elevations of preserve.Wild materialPlants measuring 12-18" in height. Spreading vegetatively via rhizomes. Majority of specimens with mostly white flowers. Peak flowering at collection site occurred near 26th of May (2023).2158358Ames 36153
31Ames 36154JDC/MM/2023/051/1083Monarda maxmedleyi J. J. N. Campb. & Floden Kentucky, United StatesNC7PLANT2023COLLECTED08/08/2023Located just east of highway 213 (Morris Creek Road) near Powell and Montgomery County line. Population in both counties.37.90554800, -83.86808700359Dry, steep hillside (roadside). Localized to south-facing slopes.Wild materialPlants measuring 12-18" in height. Peak flowering at collection site occurred near 24th of May (2023). Some specimens extremely vigorous forming dense clonal patches covering a 5' x 5' area. Majority of specimens with mostly white flowers.2158359Ames 36154
32Ames 36155JDC/MM/2023/052/1084Monarda maxmedleyi J. J. N. Campb. & Floden Kentucky, United StatesNC7PLANT2023COLLECTED08/09/2023Star Gap Road between Red River and Campton Road located 3.0 miles north, northwest of Slade37.83158300, -83.72674500265Edges of woods/roadsides. Localized to west and southeast facing slopes.Wild materialPlants measuring 12-18" in height. Spreading vegetatively via rhizomes. Most specimens had pale pink flowers with some having white flowers. Peak flowering at collection site occurred near 29th of May (2023).2158360Ames 36155
33Ames 36158JDC/MM/2023/058/1090Monarda maxmedleyi J. J. N. Campb. & Floden Kentucky, United StatesNC7PLANT2023COLLECTED08/09/2023South of Morehead approximately 5.8 miles on Pretty Ridge Road (highway 1274) just north of intersection with Road 80138.10409000, -83.42610600353Roadside. High-quality remnant prairie/open woods in immediate area.Wild materialPlants measuring 12-18" in height. Spreading vegetatively via rhizomes. Majority of specimens with light pink flowers but a few have white flowers. Peak flowering at collection site occurred near 25th of May (2023).2158363Ames 36158
34Ames 36159JDC/MM/2023/062/1094Monarda maxmedleyi J. J. N. Campb. & Floden Kentucky, United StatesNC7PLANT2023COLLECTED08/09/2023Daniel Boone National Forest on north and south sides along Zilpo Road with the highest abundance being across from intersection with Dogwood Lane.38.05551500, -83.53288600354Edges of woods/roadsides. Localized to west and southeast facing slopes.Wild materialPlants measuring 12-18" in height. Spreading vegetatively via rhizomes. Flower color varies within the population from white to pink. Peak flowering at collection site occurred near 27th of May (2023).2158364Ames 36159
35OPGC 8851AS/OF/2023/068/278Oenothera fruticosa L. subsp. glauca (Michx.) Straley Kentucky, United StatesOPGCFLOWER2023COLLECTED08/09/2023Star Gap Road between Red River and Campton Road located 3.0 miles north, northwest of Slade37.83158300, -83.72674500260Edges of woods/roadsides. Localized to west and southeast facing slopes.Wild materialPlants in nature measuring approximately 3.0' in height. Bright yellow flowers peaking in early June (central Kentucky) measuring approximately 1-2" across. 2158361OPGC 8851
36W6 61386CBG- 10811Parthenium integrifolium L. Illinois, United StatesW6SEED2023Wild material2142268W6 61386
37W6 61387CBG- 10812Chamaecrista fasciculata (Michx.) Greene Illinois, United StatesW6SEED2023Wild material2142269W6 61387
38WLP 3084RM2023-002Rhododendron viscosum (L.) Torr. Florida, United StatesNA2023COLLECTED09/15/2022This species is growing in the Blackwater River State Forest approximately 0.24 kilometers north of Wof W20 and approximately 0.93 kilometers west of the junction of 3 Notch Trail/Road. 30.84510000, -86.9494000038The plants were growing in part shade of a moist mesic transition slope between a dry upland habitat and a bog.
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 material2141438WLP 3084
39NA 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
40NA 88526RM-TK2022-014Oxydendrum arboreum (L.) DC. Florida, United StatesNA2023COLLECTED11/06/2022Growing along an unnamed dirt road leading to “Old Land Place” on the edge of Eglin AFB accessed from the Yellow River.30.55320000, -86.937300002The underlying geology of this area is classified as Alluvium of Pleistocene/Holocene origin and consists of undifferentiated Quaternary sediments of varying thickness including siliciclastics, organics and freshwater carbonates. The siliciclastics are light gray, tan, brown to black, unconsolidated to poorly consolidated, clean to clayey, silty, unfossiliferous, variably organic-bearing sands to blue green to olive green, poorly to moderately consolidated, sandy, silty clays. Organics occur as plant debris, roots, disseminated organic matrix and beds of peat. Freshwater carbonates, often referred to as marls in the literature, are scattered.
Source: USGS Florida Geologic Map Data (https://mrdata.usgs.gov/geology/state/state.php?state=fl)
The surface soil profile of this area is primarily Bibb-Kinston Series Association. Bibb Series soils are coarse-loamy, sandy, acid soils that are poorly drained. They are soils of flood plains and streams subject to frequent flooding. These are found in association with Kinston Series soils that are fine-loamy, sandy, acid soils of flood plains and stream subject to frequent flooding. The Bibb-Kinston association ranges from 1-1.5 meters thick and is strongly acid.
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 material2140807NA 88526
41NA 88541RJLSEUS2022-013Rhododendron viscosum (L.) Torr. Georgia, United StatesNA2023COLLECTED12/09/2022Plants growing around a pond and associated wetland on the property of Monica Williams north of Albany, Georgia. Common along the edges of the pond and wetland area. 31.63828300, -84.1382700062Plants are growing in part-shade to sun of a wetland habitat on the edge of a large pond. The habitat is comprised of numerous hummocks where this species grows, slightly above the permanently wet, inundated edges of the pond. Some plants are growing in more shade under moist mesic conditions as well.
Soils: The underlying geology of this area is of Eocene origin and characterized as Ocala Limestone. The Ocala Limestone consists of almost pure limestones with occasional dolomites. It can be subdivided into both lower and upper facies with the lower facies composed of a whitish to cream-colored, fine to medium grained, poorly to moderately hard, fossil rich grainstone and packstone. The upper Ocala is white and somewhat weak and poorly sorted. It is extremely fossil rich grainstone, packstone and wackestone and some chert is common in the upper facies.
Source: USGS Georgia Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=GANu%3B1)
The primary soil types in the collection area are classified as Herod and Muckalee Series soils. The Herod Series consists of poorly drained moderately permeable soils formed in loamy alluvium. These soils are on flood plains of streams in the Coastal Plain. Slopes range from 0 to 2 percent. The Muckalee Series consists of poorly drained moderately permeable soils formed in loamy and sandy alluvium. These soils are on flood plains of streams in the Coastal Plain. Slopes range from 0 to 2 percent.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)
Wild material2140768NA 88541
42NA 88544RJLSEUS2022-016Itea virginica L. Georgia, United StatesNA2023COLLECTED12/09/2022Plants growing around a pond and associated wetland on the property of Monica Williams north of Albany, Georgia as well as the edges of nearby Muckalee Creek. Common in the wetland habitat edges. 31.63834700, -84.1383560063Plants are growing in part-shade to sun in wet to inundated conditions along the edges of a pond as well as the edges of Muckalee Creek. This species is found in conditions of abundant, year-round moisture.
Soils: The underlying geology of this area is of Eocene origin and characterized as Ocala Limestone. The Ocala Limestone consists of almost pure limestones with occasional dolomites. It can be subdivided into both lower and upper facies with the lower facies composed of a whitish to cream-colored, fine to medium grained, poorly to moderately hard, fossil rich grainstone and packstone. The upper Ocala is white and somewhat weak and poorly sorted. It is extremely fossil rich grainstone, packstone and wackestone and some chert is common in the upper facies.
Source: USGS Georgia Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=GANu%3B1)
The primary soil types in the collection area are classified as Herod and Muckalee Series soils. The Herod Series consists of poorly drained moderately permeable soils formed in loamy alluvium. These soils are on flood plains of streams in the Coastal Plain. Slopes range from 0 to 2 percent. The Muckalee Series consists of poorly drained moderately permeable soils formed in loamy and sandy alluvium. These soils are on flood plains of streams in the Coastal Plain. Slopes range from 0 to 2 percent.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)
Wild material2140770NA 88544
43NA 88569RJLSEUS2022-042Ilex hybr.Florida, United StatesNA2023COLLECTED12/15/2022Yellow River: this plant is growing on the edge of the Yellow River and accessed by boat. This collection located approximately 0.4 kilometers north of the Yellow River Boat Ramp on the east side of Florida State Hwy 87.30.57317600, -86.923675001This plant was found growing in full sun in permanently saturated to submersed conditions along the edge of the Yellow River, growing in an open river edge with no overstory. Like most of the plants along the river, this collection is adapted to acidic conditions and while the aquatic habitats are generally fresh water, there can occasionally be tidal or hurricane-caused saltwater intrusions. The underlying geology of this area is classified as Alluvium, of Pleistocene/Holocene origin and consists of undifferentiated Quaternary sediments of varying thickness including siliciclastics, organics and freshwater carbonates. The siliciclastics are light gray, tan, brown to black, unconsolidated to poorly consolidated, clean to clayey, silty, unfossiliferous, variably organic-bearing sands to blue green to olive green, poorly to moderately consolidated, sandy, silty clays. Organics occur as plant debris, roots, disseminated organic matrix and beds of peat. Freshwater carbonates, often referred to as marls in the literature, are scattered. (Source: USGS Florida Geologic Map Data). The surface soil profile of this area is primarily Bibb-Kinston Series Association. Bibb Series soils are coarse-loamy, sandy, acid soils that are poorly drained. They are soils of flood plains and streams subject to frequent flooding. These are found in association with Kinston Series soils that are fine-loamy, sandy, acid soils of flood plains and stream subject to frequent flooding. The Bibb-Kinston association ranges from 1-1.5 meters thick and is strongly acid. (Source: Soil Survey of Santa Rosa County and NRCS Web Soil Survey).Wild materialIlex putative natural hybrid (I. myrtifolia x I. opaca)2140823NA 88569
44NA 88570RJLSEUS2022-043Ilex myrtifolia Walter Florida, United StatesNA2023COLLECTED12/15/2022Yellow River: plants are growing along a several mile stretch of the Yellow River and accessed by boat via the Yellow River Boat Ramp on the east side of Florida State Hwy 87.30.58148800, -86.911219001Plants are typically found growing in full sun to part shade in permanently saturated to submersed conditions along the edge of the Yellow River, growing in association with a wide array of deciduous and evergreen trees, shrubs and perennial plant species. Most of the plants along the river are adapted to acidic conditions and, while the aquatic habitats are generally fresh water, there is occasionally tidal or hurricane-caused saltwater intrusions. The underlying geology of this area is classified as Alluvium, of Pleistocene/Holocene origin and consists of undifferentiated Quaternary sediments of varying thickness including siliciclastics, organics and freshwater carbonates. The siliciclastics are light gray, tan, brown to black, unconsolidated to poorly consolidated, clean to clayey, silty, unfossiliferous, variably organic-bearing sands to blue green to olive green, poorly to moderately consolidated, sandy, silty clays. Organics occur as plant debris, roots, disseminated organic matrix and beds of peat. Freshwater carbonates, often referred to as marls in the literature, are scattered. (Source: USGS Florida Geologic Map Data). The surface soil profile of this area is primarily Bibb-Kinston Series association. Bibb Series soils are coarse-loamy, sandy, acid soils that are poorly drained. They are soils of flood plains and streams subject to frequent flooding. These are found in association with Kinston Series soils that are fine-loamy, sandy, acid soils of flood plains and stream subject to frequent flooding. The Bibb-Kinston association ranges from 1-1.5 meters thick and is strongly acid. (Source: Soil Survey of Santa Rosa County and NRCS Web Soil Survey).Wild material2140824NA 88570
45NA 88571RJLSEUS2022-044Itea virginica L. Florida, United StatesNA2023COLLECTED12/15/2022Plants are growing along a several mile stretch of the Yellow River and accessed by boat via the Yellow River Boat Ramp on the east side of Florida State Hwy 87. The species is common along several miles of the Yellow River.30.55805600, -86.935445001Plants are typically found growing in part-shade to sun in permanently saturated to submersed conditions along the edge of the Yellow River, growing in association with a wide array of deciduous and evergreen trees, shrubs and perennial plant species. Most of the plants along the river are adapted to acidic conditions and, while the aquatic habitats are generally fresh water, there is occasionally tidal or hurricane-caused saltwater intrusions.
Soils: The underlying geology of this area is classified as Alluvium, of Pleistocene/Holocene origin and consists of undifferentiated Quaternary sediments of varying thickness including siliciclastics, organics and freshwater carbonates. The siliciclastics are light gray, tan, brown to black, unconsolidated to poorly consolidated, clean to clayey, silty, unfossiliferous, variably organic-bearing sands to blue green to olive green, poorly to moderately consolidated, sandy, silty clays. Organics occur as plant debris, roots, disseminated organic matrix and beds of peat. Freshwater carbonates, often referred to as marls in the literature, are scattered.
Source: USGS Florida Geologic Map Data (https://mrdata.usgs.gov/geology/state/state.php?state=fl)
The surface soil profile of this area is primarily Bibb-Kinston Series association. Bibb Series soils are coarse-loamy, sandy, acid soils that are poorly drained. They are soils of flood plains and streams subject to frequent flooding. These are found in association with Kinston Series soils that are fine-loamy, sandy, acid soils of flood plains and stream subject to frequent flooding. The Bibb-Kinston Association ranges from 1-1.5 meters thick and is strongly acid.
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 material2140791NA 88571
46NA 88572RJLSEUS2022-045Ilex verticillata (L.) A. Gray Florida, United StatesNA2023COLLECTED12/15/2022Yellow River: plants are growing along a several mile stretch of the Yellow River and accessed by boat via the Yellow River Boat Ramp on the east side of Florida State Hwy 87.30.57947400, -86.919061001Plants are typically found growing in full sun to part shade in permanently saturated to submersed conditions along the edge of the Yellow River, growing in association with a wide array of deciduous and evergreen trees, shrubs and perennial plant species. Most of the plants along the river are adapted to acidic conditions and, while the aquatic habitats are generally fresh water, there is occasionally tidal or hurricane-caused saltwater intrusions. The underlying geology of this area is classified as Alluvium, of Pleistocene/Holocene origin and consists of undifferentiated Quaternary sediments of varying thickness including siliciclastics, organics and freshwater carbonates. The siliciclastics are light gray, tan, brown to black, unconsolidated to poorly consolidated, clean to clayey, silty, unfossiliferous, variably organic-bearing sands to blue green to olive green, poorly to moderately consolidated, sandy, silty clays. Organics occur as plant debris, roots, disseminated organic matrix and beds of peat. Freshwater carbonates, often referred to as marls in the literature, are scattered. (Source: USGS Florida Geologic Map Data). The surface soil profile of this area is primarily Bibb-Kinston Series association. Bibb Series soils are coarse-loamy, sandy, acid soils that are poorly drained. They are soils of flood plains and streams subject to frequent flooding. These are found in association with Kinston Series soils that are fine-loamy, sandy, acid soils of flood plains and stream subject to frequent flooding. The Bibb-Kinston association ranges from 1-1.5 meters thick and is strongly acid. (Source: Soil Survey of Santa Rosa County and NRCS Web Soil Survey).Wild material2140825NA 88572
47NA 88573RJLSEUS2022-046Ilex myrtifolia Walter Florida, United StatesNA2023COLLECTED12/15/2022Yellow River: this plant is growing on the edge of the Yellow River and accessed by boat. This collection is located approximately 3.2 kilometers by boat north and east of the Yellow River Boat Ramp on the east side of Florida State Hwy 87.30.58188200, -86.912205001This plant is growing in full sun in permanently saturated conditions along the edge of the Yellow River, growing in association with a wide array of deciduous and evergreen trees, shrubs and perennial plant species. Most of the plants along the river are adapted to acidic conditions and, while the aquatic habitats are generally fresh water, there is occasionally tidal or hurricane-caused saltwater intrusions. The underlying geology of this area is classified as Alluvium, of Pleistocene/Holocene origin and consists of undifferentiated Quaternary sediments of varying thickness including siliciclastics, organics and freshwater carbonates. The siliciclastics are light gray, tan, brown to black, unconsolidated to poorly consolidated, clean to clayey, silty, unfossiliferous, variably organic-bearing sands to blue green to olive green, poorly to moderately consolidated, sandy, silty clays. Organics occur as plant debris, roots, disseminated organic matrix and beds of peat. Freshwater carbonates, often referred to as marls in the literature, are scattered. (Source: USGS Florida Geologic Map Data). The surface soil profile of this area is primarily Bibb-Kinston Series Association. Bibb Series soils are coarse-loamy, sandy, acid soils that are poorly drained. They are soils of flood plains and streams subject to frequent flooding. These are found in association with Kinston Series soils that are fine-loamy, sandy, acid soils of flood plains and stream subject to frequent flooding. The Bibb-Kinston Association ranges from 1-1.5 meters thick and is strongly acid. (Source: Soil Survey of Santa Rosa County and NRCS Web Soil Survey).Wild materialorange-fruited form2140826NA 88573
48NA 88574RJLSEUS2022-047Rhododendron austrinum (Small) Rehder Florida, United StatesNA2023COLLECTED12/15/2022Plants are growing along a several mile stretch of the Yellow River and accessed by boat via the Yellow River Boat Ramp on the east side of Florida State Hwy 87. The species is found frequently along several miles of the Yellow River.30.58133600, -86.899539002Plants are found growing in part-shade to shade along areas of the river where natural levies, 1-3 meters tall, have formed, depositing sand and organic matter. The plants grow well-above normal flow of the river in well-drained to dry conditions. Even so, they are periodically subjected to inundation from floodwaters.
Soils: The underlying geology of this area is classified as Alluvium, of Pleistocene/Holocene origin and consists of undifferentiated Quaternary sediments of varying thickness including siliciclastics, organics and freshwater carbonates. The siliciclastics are light gray, tan, brown to black, unconsolidated to poorly consolidated, clean to clayey, silty, unfossiliferous, variably organic-bearing sands to blue green to olive green, poorly to moderately consolidated, sandy, silty clays. Organics occur as plant debris, roots, disseminated organic matrix and beds of peat. Freshwater carbonates, often referred to as marls in the literature, are scattered.
Source: USGS Florida Geologic Map Data (https://mrdata.usgs.gov/geology/state/state.php?state=fl)
The surface soil profile of this area is primarily Bibb-Kinston Series Association. Bibb Series soils are coarse-loamy, sandy, acid soils that are poorly drained. They are soils of flood plains and streams subject to frequent flooding. These are found in association with Kinston Series soils that are fine-loamy, sandy, acid soils of flood plains and stream subject to frequent flooding. The Bibb-Kinston Association ranges from 1-1.5 meters thick and is strongly acid.
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 materialYellow River Pink Austrinum2140792NA 88574
49WLP 2674RJL2022NJ-005Alnus serrulata (Aiton) Willd. New Jersey, United StatesNA2022COLLECTED10/24/2022Plants growing on the east side of Atlantic County Road 543, Green Bank Road, in wetlands of the Mullica River, approximately 1.01 kilometers southwest of the intersection with River Road in Green Bank, New Jersey. Plants are common but scattered on the east side of the road at this location. 39.60472300, -74.593781002Plants grow in full sun to light shade throughout this permanently wet to inundated habitat that is comprised mostly of emergent and obligate wetland herbaceous plants, deciduous shrubs, and Chamaecyparis thyoides, none reaching more than 5-10 meters tall. There are small elevation changes throughout this wetland, but the location is surrounded by water year-round.
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 Manahawkin muck, 0 to 2 percent slopes, frequently flooded. This soil is moderately high to high in the organic layers and high in the mineral layers comprised of sandy or sandy-skeletal, siliceous, dysic, mesic terric haplosaprists. This soil is considered extremely acid or very strongly acid in the surface tier and very strongly acid or strongly acid in the lower tiers and in the mineral substratum. The mineral content of organic layers ranges from 5 to 80 percent. Organic layers consist of mostly sapric material. Some pedons have subhorizons or a surface horizon of hemic material up to 25 cm. Woody fragments range from 0 to 50 percent, by volume, in the organic layers. These fragments are mostly twigs, branches, or logs ranging in size from 3 mm to 51 cm in diameter and completely break down when rubbed or crushed. The depth of this soil ranges from 0.2-2 meters. This soil is considered wet to inundated year-round.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)
Wild material2139665WLP 2674
50NA 89039RJL2022IL-001Ptelea trifoliata L. Illinois, United StatesNA2022COLLECTED09/28/2022Site of plant habitat is located at 823 E Co Rd 1220, Hamilton, IL 62341 which is the property where Jacob's Geode Shop and Mine is located. This species is scattered and relatively common throughout the woodlands on this site.40.37848400, -91.35390200175Plants growing in shade to part-shade of deciduous woodlands above a small creek.
Soils: The underlying geology of this area is of Mississippian origin and comprised of Warsaw Formation and Salem Limestone. Major lithological components include limestone that can be shaly, oolitic, bioclastic, or cherty. Minor lithological components include siltstone that can contain geodes or drusy quartz and can be calcareous.
Source: USGS Illinois Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=ILMws%3B0)
The surface soil profile of this area is Coffeen silt loam, 0 to 2 percent slopes, that are frequently flooded. The Coffeen series consists of very deep, somewhat poorly drained, moderately permeable soils on flood plains, low terraces or benches, toe slopes, and alluvial fans. They formed in silty alluvium. Much of the alluvium is of local origin derived from the nearby loess-covered uplands.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)
Wild material2139604NA 89039
51NA 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
52NA 89033RJL2022MD-010Clethra alnifolia L. Maryland, United StatesNA2022COLLECTED09/15/2022Plants growing in low woodlands at the end of Greenway Avenue near a boat dock that leads to the Pocomoke River, adjacent to Winter Quarters Golf Course, Pocomoke City. Plants common throughout the wetland area as well as mesic edges of the woodlands.38.08305100, -75.56527800Plants growing in the flood plain of the Pocomoke River in shade to part sun of a mixed deciduous and evergreen bottomland habitat about 10 meters from the edge of the golf course fairway. The habitat is a mucky swamp edge habitat next to the Pocomoke River, most of which seems wet year-round and grades slightly upslope to more mesic conditions.
The underlying geology of this area is comprised of Quaternary Deposits of Wisconsin to Holocene origin. The composition is primarily undifferentiated gray to buff sand and gravel, gray to brown lignitic silt and clay, occasional boulders, and rare shell beds. Surficial deposits occur as shell-bearing estuarine clays and silts.
Source: USGS Maryland Geologic Map Data https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=MDQdu%3B5
The surface soil profile of this habitat is classified as Puckum Muck which is frequently flooded. These highly saturated soils are found in flats, depressions and swales. The soil reaction of Puckum Muck is extremely acid to strongly acid throughout the profile. The depth to bedrock is generally greater than 150 cm. Wood fragments comprise 0-25%, by volume of the Puckum Muck throughout the profile which includes mostly twigs, branches, logs, or stumps and are 1.5-30 cm in diameter. The composition of these highly saturated soils, are classified as muck (sapric soil material) or mucky peat (hemic soil material) throughout most of the upper 150 cm and may contain thin layers of mucky silt loam, silty clay loam, sandy loam and/or sand.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)
Wild material2139598NA 89033
53NA 89032RJL2022MD-009Rhododendron viscosum (L.) Torr. Maryland, United StatesNA2022COLLECTED09/15/2022Plants growing in low woodlands at the end of Greenway Avenue near a boat dock that leads to the Pocomoke River, adjacent to Winter Quarters Golf Course, Pocomoke City. Plants scattered throughout the wetland area. Infrequent, but regularly found. 38.08235200, -75.565665001Plants growing in the flood plain of the Pocomoke River in part shade to shade of a mixed deciduous and evergreen bottomland habitat about 10 meters from the edge of the golf course fairway. The habitat is a mucky swamp edge habitat next to the Pocomoke River, most of which seems wet year-round.
The underlying geology of this area is comprised of Quaternary Deposits of Wisconsin to Holocene origin. The composition is primarily undifferentiated gray to buff sand and gravel, gray to brown lignitic silt and clay, occasional boulders, and rare shell beds. Surficial deposits occur as shell-bearing estuarine clays and silts.
Source: USGS Maryland Geologic Map Data https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=MDQdu%3B5
The surface soil profile of this habitat is classified as Puckum Muck which is frequently flooded. These highly saturated soils are found in flats, depressions and swales. The soil reaction of Puckum Muck is extremely acid to strongly acid throughout the profile. The depth to bedrock is generally greater than 150 cm. Wood fragments comprise 0-25%, by volume of the Puckum Muck throughout the profile which includes mostly twigs, branches, logs, or stumps and are 1.5-30 cm in diameter. The composition of these highly saturated soils, are classified as muck (sapric soil material) or mucky peat (hemic soil material) throughout most of the upper 150 cm and may contain thin layers of mucky silt loam, silty clay loam, sandy loam and/or sand.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)
Wild material2139597NA 89032
54Ames 35951AS/ML/2022/020/151Monarda lindheimeri Engelm. & A. Gray Texas, United StatesNC7SHOOT2022COLLECTED08/07/2022Located northwest of Navasota approximately 5.60 miles along Old Highway 6.30.44628200, -96.1533320067Powerline cut.Wild materialAccession consisting of both white flowering specimens and multi-colored (pinkish) flowering specimens. Inventory 01 represented as rather robust plants up to 40" tall that display a rather to somewhat clump type growth habit (possibly due to growing in more of a prairie habitat/full sun), but also includes adjacent specimens that are rhizomatous. Inventory 02 represents a more rhizomatous growth habit and shorter in height (e.g. less than 20" tall). Plants sampled ranging from 1.0-4.5' in height. 2140541Ames 35951
55Ames 35804Kuehn PrairieSalix humilis Marshall var. tristis (Aiton) Griggs Iowa, United StatesNC7BUD2022COLLECTED05/12/2022Kuehn Conservation Area located 4.90 miles north of Earlham on east side of Houston Trail Road, T78N R29W SE ¼ SE ¼ Sec. 12.41.56328500, -94.12929100313Xeric prairie remnant. Hilltop/knoll.Wild materialPlants in nature measuring approximately 2.0-2.5' in height. Specimens noted during peak flowering and seed dispersal on 9 April and 1 May (2021), respectively. Normally for central Iowa peak flowering and fruiting occurs in late April and mid-May, respectively.2137910Ames 35804
56Ames 35805Rippey RR ROWSalix humilis Marshall var. tristis (Aiton) Griggs Iowa, United StatesNC7FRUIT2022COLLECTED05/12/2022Located 3.27 miles southeast of Rippey along east side of highway 144, T82N R28W NW ¼ SW ¼ Sec. 19.41.89609800, -94.16247600284Xeric prairie remnant. Railroad right of way.Wild materialPlants in nature measuring approximately 3.0-3.5' in height. Specimens noted during peak flowering and seed dispersal on 12 April and 3 May (2021), respectively. Normally for central Iowa peak flowering and fruiting occurs in late April and mid-May, respectively.2137911Ames 35805
57W6 60090MARSB-410Tridens flavus (L.) Hitchc. New York, United StatesW62021Wild material2137175W6 60090
58WLP 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
59OPGC 7574Ledges State ParkSolidago ulmifolia Muhl. ex Willd. Iowa, United StatesOPGCFlower2021COLLECTED09/15/2021Ledges State Park, approximately 4.5 miles south of Boone, T83N R26W Sec. 2041.98266200, -93.89314800287Understory of hardwood forest.Wild materialPlants in nature were generally two to three feet in height, growing in sparsely spreading colonies. This population has a large amount of diversity for flowering time with the first plants in the population beginning to flower on 22 July 2021 and the last plants to flower were still blooming at the end of September. Some plants in the population had a muted red fall foliage color at the end of October 2021. This accession represents genetics from near the northwest edge of the species range of occurence.2132828OPGC 7574
60OPGC 7575Ledges State ParkSolidago flexicaulis L. Iowa, United StatesOPGCFlower2021COLLECTED10/03/2021Ledges State Park, approximately 4.5 miles south of Boone, T83N R26W Sec. 2141.98338100, -93.89052800288Understory of hardwood forest.Wild materialPlants in nature ranged in height from approximately one to three feet, growing in sparsely spreading colonies. Peak bloom in 2021 occurred near 15 September. Several specimens had branched inflorescences.2132829OPGC 7575
61Ames 35750Ames 35750Blephilia ciliata (L.) Benth. Iowa, United StatesNC7FLOWER2021COLLECTED09/27/2021Located approximately 3 miles south, southeast of Fairfield, T71N R9W SW1/4 Sec. 740.96338000, -91.94686900223Woodland openings/edges, disturbed areasWild material2122068Ames 35750
62W6 59340CA360-188Grindelia camporum Greene California, United StatesW62021Wild materialYellow flowers. Glandular bracts, stem, leaves. Pungent scent.2120393W6 59340
63Ames 35746Guye WoodsAcer saccharum Marshall subsp. nigrum (F. Michx.) Desmarais Iowa, United StatesNC7Shoot2021COLLECTED09/08/2021Guye Woods County Park located 6.0 miles northeast of Winterset, T76N R27W NE1/4 Sec. 441.41235000, -93.96373000278Moist deciduous maple, oak, hickory forest, northwest facing slope above the North River. Wild materialMultiple specimens in this population were observed to be 24" diameter at breast height (DBH) or larger with the largest specimen encountered at the time of collection measuring 36.5" DBH. Morphological traits of leaves suggests sampled specimens are true to type of Acer saccharum subsp. nigrum including leaves with three distinct points, leathery/thick, and drooping in appearance. On September 25, 2020 (Schmitz, A., personal communication, 31 January 2022), peak fall color on Acer saccharum subsp. nigrum at Guye Woods was observed with specimens having a clean yellow fall color, also indicative of Acer saccharum subsp. nigrum. 2122010Ames 35746
64Ames 35734Ledges State ParkTeucrium canadense L. Iowa, United StatesNC7SEED2021COLLECTED08/23/2021Ledges State Park located approximately 4.75 miles south of Boone T83N R26W Sec. 16 & 2141.99262400, -93.87724800330Edges of woodsWild material 2120338Ames 35734
65W6 59175CBG-10462Scirpus pendulus Muhl. Illinois, United StatesW62021Wild material2120097W6 59175
66W6 59183CBG-10474Leersia virginica Willd. Illinois, United StatesW62021Wild material2120104W6 59183
67Ames 35667Kankakee Sands PreserveAronia ×prunifolia (Marshall) Rehder Illinois, United StatesNC7Flower2021COLLECTED05/04/2021Kankakee Sands Preserve located approximately 2.3 miles southwest of Wilmington in Custer Township, T32N R9E NE 1/4 Sec. 1141.27166000, -88.15701800170Sand shrub prairieWild materialGenotypes noted in nature were averaging 5.0-6.0' in height, relatively upright in growth habit and extremely dense suckering. Numerous clones noted covering expansive areas (e.g. 30 yards by 20 yards, etc.). Variation in branching and glossiness of leaves noted across genotypes present in nature.2115976Ames 35667
68Ames 35668Iroquois County Conservation AreaAronia ×prunifolia (Marshall) Rehder Illinois, United StatesNC7Flower2021COLLECTED05/05/2021Iroquois County Conservation Area located approximately 4.5 miles northeast of Beaverville in Beaverville Township, T29N R11W NE1/4 Sec. 2240.99154700, -87.58073200198Woodland edge of wet sand prairieWild materialWide variety of genotypes noted in nature averaging 3.5-7' in height. Some growing in shade of oak forest were sparse suckering and open branching compared to open grown specimens that were extremely dense with suckers. 2115977Ames 35668
69NA 88190MARSB-749Baccharis halimifolia L. New York, United StatesNA2021Wild materialSimple, alternate, toothed leaves. White flowers that become conscpicuously fluffy when ripe.2113604NA 88190
70W6 58577MARSB-275Schizachyrium scoparium (Michx.) Nash subsp. littorale (Nash) Gandhi & Smeins New York, United StatesW62021Wild material2113507W6 58577
71WLP 2024MARSB-988Viburnum acerifolium L. New York, United StatesNA2019COLLECTED08/30/2019Onondaga County; Geddes; Long Branch County Park.43.11757000, -76.25210000Growing in full shade in forest, in moist to dry, well-drained silt/sand soil.Seed harvested from 35+ individuals in a population of 100+. Common. Seed 100 percent healthy; seed maturation middle.2109173WLP 2024
72OPGC 7903MARSB-411Asclepias tuberosa L. New York, United StatesOPGCSEED2019Wild material2097619OPGC 7903
73W6 57141MARSB-331Parthenocissus quinquefolia (L.) Planch. New Jersey, United StatesW6SEED2019Wild material2097580W6 57141
74W6 57179MARSB-409Eupatorium hyssopifolium L. New York, United StatesW6SEED2019Wild material2097618W6 57179
75W6 57287MARSB-840Schizachyrium scoparium (Michx.) Nash subsp. littorale (Nash) Gandhi & Smeins New York, United StatesW6SEED2019Wild material2097726W6 57287
76Ames 35237Ames 35237Monarda fistulosa L. New Mexico, United StatesNC7Flower2019COLLECTED10/03/2019Railroad Canyon located approximately 6.38 miles west of Kingston just north of highway 152, T16S R10W Grant County32.91279900, -107.816403002173Sparsely wooded canyon with small creek.Wild material2097773Ames 35237
77Ames 35216Potato Creek SPMonarda sp.Indiana, United StatesNC7Flower2019COLLECTED09/02/2019Potato Creek State Park located approximately 2.6 miles northeast of North Liberty, T36N R1E extreme eastern edge of NW 1/4 SW 1/4 Sec. 23.41.55439400, -86.38375900222Degraded floodplain, along sides of elevated road bed.Wild materialThis taxa is currently undescribed and according to Campbell and Medley in The atlas of vascular plants in Kentucky (Accessed 06 September 2019) was provisionally named Monarda serotina by R.T. Simmers. Described as a broad-leaved form of M. fistulosa, generally intermediate between M. fistulosa and M. clinopodia, with probable hybrid origin. Typcial habitat is mesic woods and edges on lowlands. In contrast to M. fistulosa, this taxon has longer petioles (usually 2-3 cm versus 0.5-2.0 cm), lower leaf surfaces with scattered spreading hairs, and corollas are paler pink at tips to almost white with peak flowering occurring prior to M. fistulosa by approximately 1-2 weeks. Leaves are rather rugose, where upper leaf tissue between veins is visibly raised. This accession represents genetics from northern Indiana (Potato Creek State Park). Plants at the collection site in nature peaked flowering near 8 July 2019 where flower colors were more lavender in sun but pale in shade (Namestnik, S., personal communication, 15 July 2020). Peak fruiting occurs mid-August. Average height of plants sampled in nature estimated at 4.5' in height.2097752Ames 35216
78OPGC 7865NV040-348Dieteria canescens (Pursh) Nutt. var. canescens Nevada, United StatesOPGCSEED2019Wild material2094599OPGC 7865
79W6 56656CBG-9081Zizia aptera (A. Gray) Fernald Wisconsin, United StatesW6SEED2019Wild material2092755W6 56656
80Ames 34606JDC/MB/2019/011/890Monarda brevis (Fosberg & Artz) Floden West Virginia, United StatesNC72019Wild materialVariation in flower color present from near white, faint pink to faint "smoky" purple. Majority of specimens noted at collection site in nature were approximately 3-5 days past peak flower on 10 June 2019 with seeds reaching maturity approximately 55 days later. Majority of specimens observed were approximately 10" in height. Very healthy, dark-green leaves that maintained quality throughout the season (observed mid-August 2019). Some specimens consisting of 25-30 flowering stems encompassing a 1.5 sq. ft. area. 2092642Ames 34606
81Ames 34607JDC/MB/2019/012/891Monarda brevis (Fosberg & Artz) Floden West Virginia, United StatesNC7SHOOT2019Wild materialThis accession likely represents the holotype for Monarda brevis that was vouchered by Lena Artz in 1953 (Catalog No. 2097485). Variation in flower color present from near white, faint pink to faint "smoky" purple. Majority of specimens noted at collection site in nature were approximately 3-5 days past peak flower on 10 June 2019 with seeds reaching maturity approximately 55 days later. Majority of specimens observed were apprxoimately 10" in height. Very healthy, dark-green leaves that maintained quality throughout the season (observed mid-August 2019). 2092643Ames 34607
82Ames 34609JDC/MB/2019/014/893Monarda brevis (Fosberg & Artz) Floden West Virginia, United StatesNC7SHOOT2019Wild materialVariation in flower color present from near white, faint pink to faint "smoky" purple. Majority of specimens noted at collection site in nature were approximately 3-5 days past peak flower on 10 June 2019 with seeds reaching maturity approximately 55 days later. Majority of specimens observed were approximately 10" in height. Very healthy, dark-green leaves that maintained quality throughout the season (observed mid-August 2019). 2092645Ames 34609
83W6 55946NV030-1333Cornus sericea L. subsp. occidentalis (Torr. & A. Gray) Fosberg California, United StatesW6SEED2018Wild materialCornus sericea subsp. occidentalis1970657W6 55946
84OPGC 6539MARSB-445Solidago sempervirens L. New Jersey, United StatesOPGCSEED2018Wild materialSolidago sempervirens1964772OPGC 6539
85W6 54032MARSB-287Carex crinita Lam. New Jersey, United StatesW6SEED2018Wild materialCarex crinita1964748W6 54032
86W6 54033MARSB-288Carex lurida Wahlenb. New Jersey, United StatesW6SEED2018Wild materialCarex lurida1964749W6 54033
87W6 53039CBG-8026Dysphania atriplicifolia (Spreng.) G. Kadereit et al. Nebraska, United StatesW6SEED2017Wild material1954790W6 53039
88NA 87963NEWFS-365Morella caroliniensis (Mill.) Small Connecticut, United StatesNASEED2017Wild material1954710NA 87963
89Ames 34037JDC/MF/2017/059/813Monarda fistulosa L. Iowa, United StatesNC7Flower2017COLLECTED10/26/2017Private property located approximately 6.2 miles west, southwest of Grinnell, T80N R17W SE 1/4 NE 1/4 NW 1/4 Sec. 21, Jasper County41.72810000, -92.83508100285Prairie remnant, never plowed. Small (e.g. less than 1 acre), localized area of mixed woody (tree/shrub), grass, and forbs. Wild materialPopulation sampled at collection site consisted of approximately half of the specimens being void of foliage likely due to susceptibility to mildew, while the remaining half still had some green foliage at time of sampling (10/26/2017). Plants sampled varied in height, typically 3' in height, but a few specimens measuring 5' in height.1954326Ames 34037
90Ames 34052PB1701Betula papyrifera Marshall Minnesota, United StatesNC7SEED2017COLLECTED09/16/2017Detroit Mountain area just east of Detroit Lakes approximately 2.9 miles, T139N R40W SW 1/4 NE 1/4 and NE 1/4 NE 1/4 NW 1/4 Sec. 21, Becker County46.81210900, -95.78208300457Mixed deciduous woods.Wild material1954341Ames 34052
91Ames 34015Ames 34015Cornus rugosa Lam. Minnesota, United StatesNC72017COLLECTED08/23/2017Smoky Hills State Forest between Snellman and Osage, T139N R37W Sec. 2, 9, 11, and 14 and also T140N R37W Sec. 26 and 34.46.89278300, -95.35163300501Mixed pine and deciduous moist woods.Wild material1953929Ames 34015
92Ames 33921APS/GD/2016/001/236Gymnocladus dioicus (L.) K. Koch Minnesota, United StatesNC7Fruit2017COLLECTED03/17/2017Blue Earth River watershed covering approximately 9.0 river miles from Vernon Center south to the county line, Blue Earth and Faribault Counties43.87215300, -94.17375800316Mixed habitats, both upland dry and wet sites. Wild material1946988Ames 33921
93Ames 33866JDC/MP/2016/033/748Monarda punctata L. Iowa, United StatesNC7SEED2016COLLECTED11/01/2016Shields Prairie located appproximately 5.85 miles northwest of Muscatine, T77N R2W SW1/4 SE 1/4 Sec. 7 Muscatine County.41.48253000, -91.12427000217Native prairie remnant. Wild material1943208Ames 33866
94Ames 33867JDC/PT/2016/034/749Ptelea trifoliata L. Iowa, United StatesNC72016COLLECTED11/01/2016Shields Prairie located approximately 5.85 miles northwest of Muscatine, T77N R2W SW1/4 SE1/4 Sec. 741.48239000, -91.12428000222Native prairie remnantWild material1943209Ames 33867
95Ames 33289APS/GD/2016/010/245Gymnocladus dioicus (L.) K. Koch Michigan, United StatesNC7Fruit2016COLLECTED04/05/2016Ionia County: T5N R5W SW 1/4 SW 1/4 SE 1/4 Sec. 21; T5N R5W NE 1/4 NW 1/4 NW 1/4 Sec. 20; and T5N R5W SW 1/4 SW 1/4 SE 1/4 Sec. 20 along Grand River approximately 4.80 miles south and slightly west of Portland.42.80296200, -84.91275400231Floodplain. Wild material1940346Ames 33289
96W6 50196NV040-223Elymus elymoides (Raf.) Swezey Nevada, United StatesW6SEED2015Wild material1927505W6 50196
97Ames 32963JDC/BA/2015/049/706Betula alleghaniensis Britton Iowa, United StatesNC72015COLLECTED09/14/2015Bixby State Preserve, T91N R5W extreme southern edge of Sec. 23 basically restricted to W 1/2 of Sec. 23.42.67470300, -91.39917300308North-facing algific talus slope (45-60 degrees) adjacent to Bear Creek. Moist deciduous woods. Growing in association with Diervilla lonicera, Hamamelis virginiana, Corylus sp., Viburnum opulus var. americanum, Cornus rugosa (few), Cornus alternifolia, Fraxinus nigra, Quercus rubra, Viburnum lentago, Ribes sp., Rubus idaeus subsp. strigosus, Rhamnus alnifolia (few), Rosa sp., Taxus canadensis, Prunus virginiana, Impatiens sp., Dirca palustris, and Pinus strobus (few).Wild material1927433Ames 32963
98WLP 683JDC/AA/2015/040/697Amelanchier arborea (F. Michx.) Fernald Iowa, United StatesNAHABITAT2015COLLECTED06/16/2015Elk Rock State Park approximately 6.25 miles north of Knoxville. Extreme northern point of park. T76N R19W SW 1/4 SW 1/4 Sec. 5 Marion County41.40879000, -93.07958000219Relatively steep, north-facing slopes (55 degrees). Growing in association with Diervilla lonicera (rare), Tilia americana (large and abundant), Rosa multiflora, Lonicera maackia, Eleagnus umbellata, Quercus rubra, Viburnum rafinesqueanum, Sanguinaria canadensis, Staphylea trifolia, and Ostrya virginiana.Wild materialFruits harvested at peak maturity. Numerous fruits were soft and/or dropped when distrurbed. Fruit color ranged from dark red with tinge of blue/purple to light red. Fruit diameter averaged 10.28 mm (0.83 stdev), range min 9.00 mm to max 12.00 mm (random sample of 20 fruits). Stalk length (fruits) averaged 22.08 mm (5.28 stdev), range min 13.89 mm to max 35.00 mm (random sample of 20 fruits with intact stalks).1926845WLP 683
99Ames 32903APS/GD/2015/031/213Gymnocladus dioicus (L.) K. Koch Oklahoma, United StatesNC7Fruit2015COLLECTED03/19/2015Osage County: Arkansas River watershed area known as Souters Bend, T21N R7E. Keystone Wildlife Management Area (John Lowery Unit) approximatley 3 miles west of Cleveland.36.30185300, -96.53051000222Floodplain, but one specimen sampled was located on dry, rocky (large boulders) bluff. Wild material1925369Ames 32903
100NA 82391JDC/SD/2015/022/678Sapindus saponaria L. var. drummondii (Hook. & Arn.) L. D. Benson Kansas, United StatesNAImage2015COLLECTED03/20/2015Elk City State Park between Elk City and Independence, T32S R15E, northwest 1/4 of southwest 1/4 of Section 7.37.27647400, -95.81521600288Short grass prairie area.Wild material1925374NA 82391
101Ames 32886APS/GD/2015/002/184Gymnocladus dioicus (L.) K. Koch Missouri, United StatesNC7Fruit2015COLLECTED03/03/2015Douglas County: North Fork River watershed, T26N R12W Sec. 13. Private property approximately 5.3 miles east, southeast of Vanzant.36.93971400, -92.21469500264Floodplain. Riverbank in pure sand.Wild material1924364Ames 32886
102Ames 34289MARSB-090Rhus copallinum L. New York, United StatesNC7SEED2015COLLECTED09/26/2013Great Kills Park near Oakwood Beach.40.55428000, -74.107380003Wild material1922928Ames 34289
103Ames 32833GA14005001Fraxinus pennsylvanica Marshall North Dakota, United StatesNC7SEED2014COLLECTED09/25/2014Billings County, Southern Badlands area.46.42000000, -103.40000000753Growing in association with Arctium majus, Shepherdia argentea, Prunus virginiana, Rosa sp., and Symphoricarpos spp.Wild material1921826Ames 32833
104Ames 32835GA14014001Fraxinus pennsylvanica Marshall North Dakota, United StatesNC7SEED2014COLLECTED10/30/2014Bottineau County, Turtle Mountains.48.97000000, -100.45000000737Mixed oak-aspen forestWild material1921828Ames 32835
105WLP 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
106WLP 1967HBC1401Viburnum opulus L. var. americanum Aiton North Dakota, United StatesNA2014COLLECTED09/29/2014Jay Wessels Wildlife Management Area located in Pembina County.48.80000000, -97.83000000312Diverse habitats including edge of swamp and also upland sandy soils. Growing in association Fraxinus pennsylvanica, Fraxinus nigra, Quercus macrocarpa, Acer negundo, Ulmus americana, Populus tremuloides, Populus balsamifera, Toxicodendron radicans, Cornus sericea, Rosa sp., Corylus sp., Prunus virginiana, Ribes sp., Equisetum sp., Rubus sp., IMpatiens capensis, Thalictrum dasycarpum, Fragaria virginiana, Asarum canadense, Calamagrostis canadensis, Sium suave, Solidago gigantea, Poa pratensis, and Bromus inermis.Wild material1921830WLP 1967
107Ames 32826JDC/DL/2014/148/651Diervilla lonicera Mill. Iowa, United StatesNC7MISCELLANEOUS2014COLLECTED11/04/2014Elk Rock State Park (extreme northern point of park) approximately 6.25 miles north of Knoxville, T76N R19W SW 1/4 SW 1/4 Sec. 541.40879000, -93.07958000219Extremely steep, north-facing slopes. Wild material1921786Ames 32826
108WLP 689BJP/AI/2014/001Amelanchier intermedia Spach Maine, United StatesNA2014COLLECTED07/17/2014Woods at the edge of a small cemetery on Pigeon Hill Road, just east of its intersection with Main Street (Hwy. 1), approximately .2.5 miles southwest of Milbridge.44.51051000, -67.91188000Woods at the edge of a small cemetery.Wild material1922791WLP 689
109Ames 32386JDC/BN/2014/013/515Betula nigra L. Iowa, United StatesNC7SEED2014COLLECTED06/05/2014Bearbower Sand Prairie, T87N R9W SW 1/4 of SW 1/4 Sec. 32.42.29814100, -91.92822800289Sand prairie with likely high water table.Wild material1919307Ames 32386
110Ames 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
111Ames 32585CBG-1842Monarda fistulosa L. var. fistulosa Wyoming, United StatesNC7SEED2013COLLECTED09/07/2011Moiser Gulch Recreational picnic area, located approximately 5.5 miles west of Buffalo on highway 16 (Cloud Peak Scenic Byway) in northern Wyoming 44.33220000, -106.816600001727Stream gulch with wetter soils within Western Rocky Mountain foothills. Wild material1909018Ames 32585
112Ames 31679GA12011001Fraxinus pennsylvanica Marshall North Dakota, United StatesNC7SEED2012COLLECTEDNEAR 09/27/2012Sheyenne National Grassland along the Sheyenne River just east of Lisbon near Richland and Ransom County line.46.53246660, -97.26656660302Riverbank and transition area of tallgrass prairie and riparian forest. Sandy-silt soil with good drainage and ph of ~7Wild materialPopulation located close to windbreak planted with Fraxinus.1906590Ames 31679
113Ames 31529JDC/FQ/2012/038/431Fraxinus quadrangulata Michx. Indiana, United StatesNC7SEED2012COLLECTED07/24/2012Lick Creek Summit Nature Preserve, NW 1/4 of Section 23, T13N, R2W, Richmond Quad, near Richmond, Wayne County.39.78453000, -84.95276400267Dry woods. Bluffs. Shallow soils. Wild material1903756Ames 31529
114Ames 31217GA15004001Fraxinus pennsylvanica Marshall North Dakota, United StatesNC7SEED2011COLLECTED09/24/2011Along Forest Service Road 842, SW 1/4 of Section 2, T147N, R99W, Long X Divide Quad, Badlands, Little Missouri National Grasslands, McKenzie County.47.57730000, -103.26760000674Clay substrate. Wild materialRequests will be filled using inventory sample 11ncao02 (JDZ/2011/004/002) unless otherwise noted.1896696Ames 31217
115Ames 31218GA15005001Fraxinus pennsylvanica Marshall North Dakota, United StatesNC7SEED2011COLLECTED09/24/2011Along East River and Tracy Mountain Roads, Burning Coal Vein Campground, T139N, R102W, Chimney Butte Quad, Badlands, Little Missouri National Grasslands, Billings and Slope County. Area following along Little Missouri River and including small tributaries from approximately 4.5 miles south of Medora, ND to approximately 2.5 miles south of Billings/Slope County line. Material sampled along an 18 mile stretch.46.81270000, -103.50900000780Clay substrate. Wild materialRequests will be filled using inventory sample 11ncao02 (JDZ/2011/005/002) unless otherwise noted.1896697Ames 31218
116Ames 31087692Fraxinus pennsylvanica Marshall New York, United StatesNC7SEED2011COLLECTED09/11/2011McMaster at Jasper-North Cameron Road, Steuben County.42.20400000, -77.41500000349Edge of Canisteo River, adjacent farmland. Wild material1891473Ames 31087
117WLP 830381Carpinus caroliniana Walter Pennsylvania, United StatesNA2011COLLECTED09/15/2011Along Valentine Run Road, near small tributary to Rhine Run Creek, Warren County.41.92500000, -79.18800000475Roadside. Mixed hardwood forest and open rangeland (Solidago). Associated with Acer, Carya ovata, Cornus racemosa, Fagus grandifolia, Hamamelis virginiana, Quercus, Rosa, Rubus, and Tsuga canadensis.Wild material1891442WLP 830
118OPGC 4292198341Heuchera cylindrica Douglas Washington, United StatesOPGCSEED2005COLLECTED07/28/2003640Associated with Artemisia tripartita, Festuca idahoensis, Pseudoroegneria spicata, Artemisia tridentata, Amelanchier alniflolia, Rosa woodsii, Prunus virginiana, Lomatium dissectum, Lupinus sericeus, Gaillardia aristata and SWild materialForb 0.6 meters tall. 1674223OPGC 4292
119Ames 27962Quercus Wilderness AreaAmelanchier arborea (F. Michx.) Fernald Iowa, United StatesNC7FLOWER2003COLLECTED05/26/2003Quercus Wilderness Area located 6.75 miles south, southwest of Oskaloosa, T74N R16W SE ¼ NE ¼ of Sec. 23.41.19888889, -92.66111111244Mature woods on very sandy soils. Typically restricted to east, west or south facing slopes at either summits or mid-slopes.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 the southern portion of Iowa. As of 2025, the top ten largest specimens in the state of Iowa are located at Quercus Wilderness where this accession was collected. Iowa’s largest specimen of A. arborea specimen at Quercus Wilderness was measured at 14.17" DBH, 51.83’ in height, and 27.00’ average crown spread for a total of 102.955 points (Rouw, M., personal communication, 12 December 2023). Fall color (orange-red) tends to peak in the middle of September (Iowa) with peak fruiting occurring in early May. Bark smooth, grey.1700483Ames 27962