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ACCESSIONPLANT NAMETAXONOMYORIGINGENEBANKIMAGEAVAILABILITYRECEIVEDSOURCE TYPESOURCE DATECOLLECTION SITECOORDINATESELEVATIONHABITATIMPROVEMENT LEVELNARRATIVE
0PI 662019Ames 27282Cornus racemosa Lam. Iowa, United StatesNC72003COLLECTED09/07/2003Along Wapsi Great Western Trail, Lake Hendricks County Park, NE corner of SW 1/4 of SW 1/4 of Section 19, T99N, R14W, Riceville Quad, Howard County.43.37694444, -92.55111111378Wild materialShrubs mostly 1.7 to 2 meters tall. Good leaf quality, some plants with striking red pedicels, heavy fruit production.1648678PI 662019
1PI 66201802-001Cornus racemosa Lam. Minnesota, United StatesNC72003COLLECTED2002North of collector's house, Hennepin County.44.95483330, -93.70646660Road bank.Wild material1644314PI 662018
2WLP 1125V18-03Cornus racemosa Lam. Vermont, United StatesNA2018COLLECTED10/02/2018Addison County; Middlebury; Otter View Park, in natural area near the parking lot.44.01924000, -73.18117000114Growing in a wet depression.2108865WLP 1125
3Ames 2699702-004Cornus racemosa Lam. Minnesota, United StatesNC72003COLLECTED2002One mile south of Backus, Cass County.46.81630000, -94.51701660Trail.Wild material1644315Ames 26997
4Ames 22080Ames 22080Cornus racemosa Lam. New Jersey, United StatesNC7FRUIT1994COLLECTEDBlawenburg.40.40750000, -74.7030555648Wild material1087560Ames 22080
5Ames 21980Ames 21980Cornus racemosa Lam. Michigan, United StatesNC71994COLLECTED1993East side of Bear Lake, Ingham County.42.70000000, -84.50000000Open old field. Wild material1087401Ames 21980
6Ames 20183No. 9Cornus racemosa Lam. New Jersey, United StatesNC7PLANT1993COLLECTEDMorris and Somerset Counties.40.78333333, -74.45000000Plants growing in their native stations.Wild material1084375Ames 20183
7Ames 1489718Cornus racemosa Lam. Illinois, United StatesNC71991COLLECTEDDupage County, Illinois.41.83024200, -88.05198800Wild materialCollected from natural populations, DuPage Co., Illinois.1069320Ames 14897
8NA 89036RJL2022KS-003Cornus drummondii C. A. Mey. Kansas, United StatesNA2022COLLECTED09/21/2022Coronado Heights Park, Smoky View, Kansas hillsides surrounding the historic WPA circa 1932 Coronado Heights Castle located about 91 meters above the surrounding land. This plant is common and abundant on the slopes of this site.38.61348400, -97.70343100475 Plants growing in part shade to full sun, under extreme exposure, rocky, dry and thin soils of this short grass prairie habitat on the slopes surrounding the summit of Coronado Heights Park. The underlying geology of this area is of Upper Cretaceous origin and comprised of Kiowa Shale or FM- light -gray to black illitic shale with thin coquinoidal limestone beds at the base; sandstone lenses are common. Cheyenne Sandstone-massive to cross-bedded, light-gray to buff fine-grained sandstone with lenses of gray sandy shale and conglomerate.
Source: USGS Kansas Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=KSKkc%3B0)
The surface soil profile of this area is Lancaster-Hedville complex, 3 to 20 percent slopes. The Lancaster series consists of moderately deep, well drained soils that formed in residuum from sandstone and sandy shales; it can be up to 200 cm deep. Slopes range from 1-20%. Hedville soils have bedrock within 50 centimeters of the surface and occur on similar hillslope positions.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)
Slope: 5-20% Aspect: all		Wild material2139601NA 89036
9Ames 34696MARSB-074Cornus amomum Mill. New Jersey, United StatesNC7SEED2015COLLECTED08/29/2013West Essex Park just southeast of Pine Brook.40.84291000, -74.3134100051Wild material1922850Ames 34696
10Ames 29506JDC-CA-2008-003Cornus alternifolia L. f. Iowa, United StatesNC7SEED2008COLLECTED07/20/2008Tower Rock Park, N edge of SE 1/4 of SW 1/4 of Section 28, T88N, R19W, Steamboat Roak Quad, Steamboat Rock, Hardin County.42.40111111, -93.07166667292Eroding (burnt orange) sandstone cliff, south side of Iowa River; mostly shaded; near base of slope with northern aspect; sand and organic matter above cliff; well drained. Wild material1782028Ames 29506
11PI 649023NY2Actaea racemosa L. New York, United StatesNC72005Wild material1698893PI 649023
12PI 664811DE2Actaea racemosa L. Delaware, United StatesNC72005Wild material1698885PI 664811
13PI 664813KY1Actaea racemosa L. Kentucky, United StatesNC72005Wild material1698887PI 664813
14PI 64902146Actaea racemosa L. Missouri, United StatesNC72004Wild material1 meter tall.1668177PI 649021
15Ames 27648JM2004009Actaea racemosa L. South Carolina, United StatesNC72004Wild material1667568Ames 27648
16PI 64970314Physocarpus opulifolius (L.) Maxim. Iowa, United StatesNC7PLANT2003COLLECTED09/14/2003Fish Farm Mounds, New Albin, SW 1/4 of SW 1/4 of NW 1/4 of Section 26, T100N, R4W, New Albin Quad, Allamakee County.43.45111111, -91.28222222280Sandstone ridge just above goat prairie. 1/2 sun. 30-50% slope w/ NW aspect. Sandy loam soil w/ some stoniness, well drainedWild materialMedium sized shrubs. 1649463PI 649703
17W6 62559FWS0502-94Epilobium ciliatum Raf. Pennsylvania, United StatesW6SEED2025Wild materialSeeds mostly ripe in reddish pods, before they split2192257W6 62559
18NA 885882024RM-001Hydrangea radiata Walter Georgia, United StatesNA2024COLLECTED10/24/2024Chattahoochee National Forest: Warwoman Wildlife Management Area: north side of Overflow Creek Road just west of the bridge over the Chattooga River.34.94956600, -83.20652000498Mixed evergreen and deciduous moist mesic forest in part shade. The underlying geology of this area is characterized as Metagraywacke/Mica Schist Formation of the Precambrian-Paleozoic period. (Source: USGS Georgia Geologic Map Data). The soils of this are characterized as Tusquitee Series Loam, 10 to 25 percent slopes. The Tusquitee Series consists of very deep, well drained soils on gently sloping to very steep benches, foot slopes, toe slopes, and fans in coves in the Southern Blue Ridge mountains, MLRA 130B. These soils formed in colluvium derived from materials weathered from igneous and high-grade metamorphic crystalline rocks such as granite, mica gneiss, hornblende gneiss, and schist. Slope ranges from 2 to 95 percent. Solum thickness ranges from 1 to 3+ meters. Reaction is very strongly acid to slightly acid, in the A horizon. The Bw and lower horizons are very strongly acid to moderately acid. In the upper 1 meter, content of rock fragments, dominantly of gravel to stone size, ranges up to 35 percent. Below 1 meter, rock fragment content may range up to 60 percent. Content of mica flakes ranges from few to common. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions).Wild material2169925NA 88588
19NA 885902024RM-003Ilex verticillata (L.) A. Gray Florida, United StatesNA2024COLLECTED11/21/2024Along the west/north side of the Yellow River about 0.33 kilometers (as the crow flies) upstream from the channel that leads the Fisher Old Mill Road Boat Ramp. This site was accessed by boat.30.62868600, -86.807480004Plants are found growing primarily in permanently saturated to submersed conditions along the edge of the Yellow River in part shade. The riverine habitat is comprised of 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 habitat is generally fresh water, there is occasionally tidal or hurricane-caused saltwater intrusions. Slope: 0 percent. Aspect: East-southeast. The underlying geology of this area is characterized as Alluvium from undifferentiated Quaternary Sediments. Much of Florida's surface is covered by a varying thickness of undifferentiated sediments consisting of siliciclastics, organics and freshwater carbonates. Where these sediments exceed 20 feet (6.1 meters) thick, they were mapped as discrete units. To subdivide the undifferentiated sediments, those sediments occurring in flood plains were mapped as alluvial and flood plain deposits (Qal). Sediments showing surficial expression of beach ridges and dunes were mapped separately (Qbd) as were the sediments composing Trail Ridge (Qtr). Terrace sands were not mapped (refer to Healy [1975] for a discussion of the terraces in Florida). The subdivisions of the Undifferentiated Quaternary Sediments (Qu) are not lithostratigraphic units but are utilized to facilitate a better understanding of the State's geology. 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. Gravel is occasionally present in the panhandle. 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 over much of the State. In southern Florida, freshwater carbonates are nearly ubiquitous in the Everglades. These sediments are buff colored to tan, unconsolidated to poorly consolidated, fossiliferous carbonate muds. Sand, silt and clay may be present in limited quantities. These carbonates often contain organics. The dominant fossils in the freshwater carbonates are mollusks. (Source: USGS Florida Geologic Map Data). The soils of this are characterized as Bibb-Kinston Series association. The Bibb Series consists of very deep, poorly drained, moderately permeable soils on flood plains of streams in the Southern Coastal Plain (133A) Major Land Resource Area. They formed in stratified loamy and sandy alluvium that are commonly and frequently flooded and water runs off the surface very slowly. Slopes range from 0 to 2 percent. Reaction ranges from extremely acid to strongly acid throughout. Content of mica flakes ranges from none to common. Content of rounded gravel typically ranges from 0 to 10 percent throughout, but may range to 50 percent in thin strata below a depth of 1 meter. Buried soil horizons, present in many pedons have the same range in color and texture as the surface horizon which has iron and organic matter concentrations in shades of brown and yellow ranging from none to common. Texture is sand, loamy sand, loamy fine sand, fine sandy loam, sandy loam, loam or silt loam. The Kinston Series consists of very deep, poorly drained, moderately permeable soils found on flood plains. They were formed in alluvial depositions. Slopes range from 0 to 2 percent. Soil reaction ranges from strongly acid to very strongly acid. Typical texture across the pedons is loamy, gravelly loam, sandy loam, and clay loam with dark concretions often present. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions).Wild material2169927NA 88590
20NA 885912024RM-004Ilex opaca Aiton Florida, United StatesNA2024COLLECTED11/21/2024Along the west/north side of the Yellow River about 5.5 kilometers upstream from the State Highway 87 boat ramp. This site was accessed by boat.30.59986000, -86.879360002Plants are found growing primarily in permanently saturated to submersed conditions along the edge of the Yellow River in part shade. The riverine habitat is comprised of 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 habitat is generally fresh water, there is occasionally tidal or hurricane-caused saltwater intrusions. Slope: 0 percent. Aspect: East-southeast. The underlying geology of this area is characterized as Alluvium from undifferentiated Quaternary Sediments. Much of Florida's surface is covered by a varying thickness of undifferentiated sediments consisting of siliciclastics, organics and freshwater carbonates. Where these sediments exceed 20 feet (6.1 meters) thick, they were mapped as discrete units. To subdivide the undifferentiated sediments, those sediments occurring in flood plains were mapped as alluvial and flood plain deposits (Qal). Sediments showing surficial expression of beach ridges and dunes were mapped separately (Qbd) as were the sediments composing Trail Ridge (Qtr). Terrace sands were not mapped (refer to Healy [1975] for a discussion of the terraces in Florida). The subdivisions of the Undifferentiated Quaternary Sediments (Qu) are not lithostratigraphic units but are utilized to facilitate a better understanding of the State's geology. 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. Gravel is occasionally present in the panhandle. 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 over much of the State. In southern Florida, freshwater carbonates are nearly ubiquitous in the Everglades. These sediments are buff colored to tan, unconsolidated to poorly consolidated, fossiliferous carbonate muds. Sand, silt and clay may be present in limited quantities. These carbonates often contain organics. The dominant fossils in the freshwater carbonates are mollusks. (Source: USGS Florida Geologic Map Data). The soils of this are characterized as Bibb-Kinston Series association. The Bibb Series consists of very deep, poorly drained, moderately permeable soils on flood plains of streams in the Southern Coastal Plain (133A) Major Land Resource Area. They formed in stratified loamy and sandy alluvium that are commonly and frequently flooded and water runs off the surface very slowly. Slopes range from 0 to 2 percent. Reaction ranges from extremely acid to strongly acid throughout. Content of mica flakes ranges from none to common. Content of rounded gravel typically ranges from 0 to 10 percent throughout, but may range to 50 percent in thin strata below a depth of 1 meter. Buried soil horizons, present in many pedons have the same range in color and texture as the surface horizon which has iron and organic matter concentrations in shades of brown and yellow ranging from none to common. Texture is sand, loamy sand, loamy fine sand, fine sandy loam, sandy loam, loam or silt loam. The Kinston Series consists of very deep, poorly drained, moderately permeable soils found on flood plains. They were formed in alluvial depositions. Slopes range from 0 to 2 percent. Soil reaction ranges from strongly acid to very strongly acid. Typical texture across the pedons is loamy, gravelly loam, sandy loam, and clay loam with dark concretions often present. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions).Wild material2169928NA 88591
21NA 885922024RM-005Ilex sp.Florida, United StatesNA2024COLLECTED11/21/2024Along the west/north side of the Yellow River about 1.1 kilometers upstream from the State Highway 87 boat ramp. This site was accessed by boat.30.57956000, -86.919164001Plants are found growing primarily in permanently saturated to submersed conditions along the edge of the Yellow River in part shade. The riverine habitat is comprised of 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 habitat is generally fresh water, there is occasionally tidal or hurricane-caused saltwater intrusions. Slope: 0 percent. Aspect: North. The underlying geology of this area is characterized as Alluvium from undifferentiated Quaternary Sediments. Much of Florida's surface is covered by a varying thickness of undifferentiated sediments consisting of siliciclastics, organics and freshwater carbonates. Where these sediments exceed 20 feet (6.1 meters) thick, they were mapped as discrete units. To subdivide the undifferentiated sediments, those sediments occurring in flood plains were mapped as alluvial and flood plain deposits (Qal). Sediments showing surficial expression of beach ridges and dunes were mapped separately (Qbd) as were the sediments composing Trail Ridge (Qtr). Terrace sands were not mapped (refer to Healy [1975] for a discussion of the terraces in Florida). The subdivisions of the Undifferentiated Quaternary Sediments (Qu) are not lithostratigraphic units but are utilized to facilitate a better understanding of the State's geology. 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. Gravel is occasionally present in the panhandle. 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 over much of the State. In southern Florida, freshwater carbonates are nearly ubiquitous in the Everglades. These sediments are buff colored to tan, unconsolidated to poorly consolidated, fossiliferous carbonate muds. Sand, silt and clay may be present in limited quantities. These carbonates often contain organics. The dominant fossils in the freshwater carbonates are mollusks. (Source: USGS Florida Geologic Map Data). The soils of this are characterized as Bibb-Kinston Series association. The Bibb Series consists of very deep, poorly drained, moderately permeable soils on flood plains of streams in the Southern Coastal Plain (133A) Major Land Resource Area. They formed in stratified loamy and sandy alluvium that are commonly and frequently flooded and water runs off the surface very slowly. Slopes range from 0 to 2 percent. Reaction ranges from extremely acid to strongly acid throughout. Content of mica flakes ranges from none to common. Content of rounded gravel typically ranges from 0 to 10 percent throughout, but may range to 50 percent in thin strata below a depth of 1 meter. Buried soil horizons, present in many pedons have the same range in color and texture as the surface horizon which has iron and organic matter concentrations in shades of brown and yellow ranging from none to common. Texture is sand, loamy sand, loamy fine sand, fine sandy loam, sandy loam, loam or silt loam. The Kinston Series consists of very deep, poorly drained, moderately permeable soils found on flood plains. They were formed in alluvial depositions. Slopes range from 0 to 2 percent. Soil reaction ranges from strongly acid to very strongly acid. Typical texture across the pedons is loamy, gravelly loam, sandy loam, and clay loam with dark concretions often present. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions).Wild material2169929NA 88592
22NA 890792024RJLPA-005Viburnum prunifolium L. Pennsylvania, United StatesNA2024COLLECTED09/20/2024Along gated road about 0.33 kilometers southwest of the Lake Ontelaunee Trail parking lot.40.50062600, -75.8900490094Plants are growing on moist, well-drained in part shade of a deciduous forest. Slope: 0 percent. Aspect: N/A. Geology: The underlying geology of this area is of Ordovician origin and characterized as Shale and graywacke of Hamburg sequence. It is characterized by shale containing zones of conspicuous graywacke. (Source: USGS Pennsylvania Geologic Map Data). Soils: The primary soil type in the area of this collection is classified as Holly Series Silt Loam (Ho). The Holly Series consists of very deep, very poorly and poorly drained soils formed in loamy alluvium on flood plains. Saturated hydraulic conductivity is moderately high through high in the mineral soil. Slope ranges from 0 through 3 percent. (Source: USDA-NRCS Official Soil Series Descriptions). EPA Ecoregion (Level III): Ridge and Valley (67). EPA Ecoregion (Level IV): Northern Shale Valleys (67b).Wild material2169043NA 89079
23NA 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
24NA 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
25NA 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
26NA 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
27NA 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
28NA 88671RJL2023PA-005Rhododendron maximum L. Pennsylvania, United StatesNA2023COLLECTED10/16/2023Appalachian National Scenic Trail: Pulpit Rock and Pinnacle Loop. Rocky woodlands along Furnace Creek as well as steep rocky slopes above Pulpit Rock Reservoir associated with the Pulpit Rock and Pinnacle Loop Trail.40.59226100, -75.94588800301Well-drained and very rocky dry deciduous woodlands in part shade to full shade. Slope: 0-30%. Aspect: variable. The underlying geology of this area is of Silurian origin and characterized as the Shawangunk Formation. It is characterized by light- to dark-gray, fine- to very coarse-grained sandstone and conglomerate containing thin shale interbeds. Includes four members, in descending order: Tammany--conglomerate and sandstone; Lizard Creek--sandstone and red or green shale; Minsi--sandstone and conglomerate; Weiders--conglomerate. Tammany and Lizard Creek Members together are approximately equivalent to Clinton Group to the west; Minsi and Weiders Members together are equivalent to Tuscarora Formation to the west. (Source: USGS Pennsylvania Geologic Map Data). The primary soil type in the collection area is classified as Hazleton Series. The Hazleton series consists of deep and very deep, well drained soils formed in residuum of acid gray, brown or red sandstone on uplands. Slope ranges from 0 to 80 percent. Permeability is moderately rapid to rapid. Solum thickness ranges from 60 to 120 centimeters. Depth to lithic contact ranges from 1 to 2 meters. Rock fragments of angular sandstone, dominantly less than 25 cm in size, range from 5 to 70 percent in individual horizons. Boulders, stones, flags and channers cover about 5 to 60 percent of the surface of some pedons. Reaction ranges from strongly acid through extremely acid throughout. (Source: NRCS Web Soil Survey).Wild material2159062NA 88671
29Ames 36185APS/BP/2023/076/286Betula populifolia Marshall Indiana, United StatesNC7LEAF2023COLLECTED11/02/2023Indiana Dunes State Park just 3.40 miles northeast of Chesterton, T37N R5W NE 1/4 SE 1/4 SW 1/4 Sec. 1841.65352700, -87.03831500186Low depressions with some standing water. Woodland edge.Wild materialRepresents a disjunct population in northwest Indiana and the extreme western edge of the species native range. Trees sampled in nature averaging 30-45' in height with trunks ranging from 3" up to 8" DBH. Bark dull-white to grey. Typically multi-stemmed trunks. Leaves with acuminate tips and branches with typically one male catkin at terminal end of branches, but occassionally two male catkins. 2159042Ames 36185
30NA 88666RJL2023PA-003Hamamelis virginiana L. Pennsylvania, United StatesNA2023COLLECTED10/01/2023Collected primarily along the woodland edge along Northside Road on Pennsylvania State Gamelands No. 43 as well as a few on nearby roads.40.17974200, -75.76790700176Plants were growing in mesic well-drained conditions on moderately sloping sites of a deciduous upland forest. This species grows well in shade to part-sun. Most abundant fruit development is found where plants are exposed to sunlight for a portion of the day. Slope: 15%. Aspect: North-northwest. The underlying geology of this area is of Precambrian origin and characterized as the Graphitic Felsic Gneiss. This includes Pickering Gneiss and small areas of marble; dominantly quartz and feldspar with varying amounts of graphite and various metamorphic minerals; medium grained, light to dark gray and greenish gray; sedimentary origin. (Source: USGS Pennsylvania Geologic Map Data.) The primary soil type in the area of this collection is classified as Gladstone Gravelly Loam Series (8 to 15 percent slopes). The Gladstone Series consists of very deep, well drained soils formed in residuum and colluvium from granitic gneiss. Saturated hydraulic conductivity is moderately high to high. Solum thickness ranges from 75 to 125 cm. Depth to granitic gneiss bedrock is 1.6 meters or more. The bedrock may be strongly weathered in the upper part. Gravel content ranges from 5 to 35 percent throughout the solum, and 10 to 40 percent in the C horizons. Fragments, larger than 3 inches in diameter, range from 0 to 20 percent by volume in the surface layer and 0 to 10 percent in the subsoil and substratum layers. Reaction is strongly or very strongly acid throughout the soil, unless limed. Areas that have been limed range to moderately acid in the upper part of the profile. (Source: NRCS Web Soil Survey.)Wild material2158815NA 88666
31NA 88664RJL2023PA-001Viburnum acerifolium L. Pennsylvania, United StatesNA2023COLLECTED10/01/2023Seed collected from plants growing along a two-mile stretch of Harmonyville Road on the woodland edge next to the road. [Note: latitude and longitude were collected at the location of the largest seed collection.]40.18482200, -75.78145100158Plants were growing in well-drained and rocky mesic-dry woodlands from part shade along the road edge to full shade in the understory of the woodlands. Slope: 2-10%. Aspect: Variable. The underlying geology of this area is of Triassic origin and characterized as the Stockton Formation. It is characterized by light-gray to buff, coarse-grained, arkosic sandstone; includes reddish-brown to grayish-purple sandstone, siltstone, and mudstone. (Source: USGS Pennsylvania Geologic Map Data.) The primary soil type in the area of this collection is classified as Edgemont Channery Sandy Loam Series (8 to 25 percent slopes), extremely stony. The Edgemont Series consists of deep and very deep, well drained soils formed in the weathered residuum of quartzitic rocks. They have moderately high to high saturated hydraulic conductivity. Slopes range from 0 to 70 percent. Solum thickness ranges from 50 to 10 cm. Depth to bedrock ranges from about 1.5 to 2.2 meters. Kaolinite is the dominant mineral in the clay fraction with detectable amounts of illite, vermiculite, montmorillonite, chlorite and interstratified clays. Gravel, channers, and stone size fragments of quartzite and quartz are present throughout the profile. Rock fragments range from 5 to 40 percent in the horizons of the solum and from 10 to 90 percent in the C horizon. Reaction ranges from extremely acid to strongly acid throughout. (Source: NRCS Web Soil Survey.)Wild material2158813NA 88664
32OPGC 8815CBG- 10787Maianthemum racemosum (L.) Link subsp. racemosum Wisconsin, United StatesOPGC2023Wild material2142251OPGC 8815
33W6 61417CBG- 10852Verbesina alternifolia (L.) Britton ex Kearney Illinois, United StatesW6SEED2023Wild material2142299W6 61417
34W6 61418CBG- 10853Agastache scrophulariifolia (Willd.) Kuntze Illinois, United StatesW6SEED2023Wild material2142300W6 61418
35WLP 2670RJL2022PA-016Acer negundo L. Pennsylvania, United StatesNA2022COLLECTED10/21/2022Plants 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. Plants are found regularly but scattered in the understory of the woodlands. 39.80426000, -75.82609300105Plants growing in a mesic, well-drained habitat of deciduous woodlands along streams and above the riparian zone that drains toward a small unnamed creek that feeds into the Middle Branch White Clay Creek. Plants generally grow in part shade to full sun, but perform best and fruit more heavily in full sun where there is abundant access to moisture. 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. Despite this fact, Acer negundo is highly competitive and competes well.
Soils: The underlying geology of this area is the Glenarm Wissahickon Formation of lower Paleozoic origin and lithologically similar to oligoclase-mica schist of the Wissahickon Formation (PZw), but also includes lenticular amphibolite bodies having ocean-floor basalt chemistry.
Source: USGS Pennsylvania Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=PAPZgw%3B0)
The primary soil type in the area of this collection is classified as Glenelg silt loam, 3 to 8 percent slopes. 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.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2139661WLP 2670
36NA 88483RJL2022MD-004Clethra alnifolia L. Maryland, United StatesNA2022COLLECTED09/04/2022Plants growing at Elkton State Forest along roads and woodlands over a distance of approximately 5 kilometers labelled as the address of 717 Irishtown Rd, North East, MD 21901. Plants are found regularly but scattered along the unnamed gravel road as well as in open understory of the upland woodlands. 39.58531200, -75.8956610047Plants are growing in a mesic to moist, well-drained habitat of mixed deciduous and evergreen woodlands comprised primarily of acid-loving plants. Plants are growing in part shade and open understory shade. The soils in the collection 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.). 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.Wild material2139362NA 88483
37NA 88488RJL2022PA-004Viburnum acerifolium L. Pennsylvania, United StatesNA2022COLLECTED09/03/2022Plants growing in woodlands on the east side of Shed Road in French Creek State Park. Plants are common and found scattered along the edges of the road and into the woodlands. 40.21969200, -75.77373600238Plants are growing in a mesic to dry, well-drained habitat of upland deciduous forest which is very rocky. The understory layer is generally not as rich due to the rock-laden ground layer. Plants are growing in part shade to shade. The underlying geology of this area is comprised of Hammer Creek Conglomerate, characterized by cobble and pebble quartz conglomerate interbedded with red sandstone.
Source: USGS Pennsylvania Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=PATRhc%3B2) The surface soil profile of this area is Joanna Loam (JpD), 8 to 25 percent slopes which is extremely stony. It is represented by residuum weathered from sandstone and/or residuum weathered from conglomerate. Joanna Loam is moderately to well-drained and 1.8 meters to 2.5 meters to the lithic bedrock described above.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2139367NA 88488
38Ames 36026RJL2022FLAL-007Fraxinus caroliniana Mill. Florida, United StatesNC7SEED2022COLLECTED07/28/2022Growing along the Yellow River and reached by boat.30.58025000, -86.910528001Trees are typically found growing in full 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. This species requires acidic conditions. 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. Wild material2138696Ames 36026
39WLP 2584RJL2022FLAL-005Styrax americanus Lam. Florida, United StatesNA2022COLLECTED07/28/2022Growing along the Yellow River and reached by boat.30.57944000, -86.916898001Plants are typically found growing in shade to full 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. 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. Wild material2138694WLP 2584
40WLP 2585RJL2022FLAL-006Nyssa biflora Walter Florida, United StatesNA2022COLLECTED07/28/2022Growing along the Yellow River and reached by boat.30.58013800, -86.915568001Trees are typically found growing in full 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. This species requires acidic conditions. 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. Wild material2138695WLP 2585
41Ames 35881Reichelt UnitHeuchera richardsonii R. Br. Iowa, United StatesNC7FRUIT2022COLLECTED06/30/2022Reichelt Unit of Rock Creek State Park on south side of US highway 6 located 7.70 miles west, southwest of Grinnell, T80N R17W SE ¼ SE ¼ Sec. 30.41.70311300, -92.86569100274Prairie remnant. Hilltop/knoll.Wild materialPlants in nature measuring approximately six to eight inches in height with flowering stalks reaching up to three feet in height.2138180Ames 35881
42WLP 2576RJL2022-001Amelanchier arborea (F. Michx.) Fernald Maryland, United StatesNA2022COLLECTED05/25/2022Plants growing in open woodlands and part shade along unnamed Elkton State Forest gravel road over a distance of approximately 5 kilometers labelled as the address of 717 Irishtown Rd, North East, MD 21901.39.58089500, -75.9150590073Plants are found regularly but scattered along the unnamed gravel road as well as in open understory of the upland woodlands. Plants growing in a mesic to dry, well-drained habitat of mixed deciduous and evergreen woodlands comprised primarily of acid-loving plants. Plants are growing in part shade and open understory shade. The soils in the collection 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.). 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.Wild material2138095WLP 2576
43Ames 35807JDC/SD/2022/034/1014Salix discolor Muhl. Minnesota, United StatesNC7FRUIT2022COLLECTED06/06/2022Mud Lake and Amity Creek Watershed located just north of Duluth approximately 6.25 miles, T51N R14W Sec. 22, 26, 27, and 28. 46.87662300, -92.10040300418Floodplain, wetlands, drainages.Wild materialThe native range of Salix discolor is concentrated in the northeastern United States and also throughout southern Canada (Little, E. L. Jr. 1977). Generally adapted/tolerant to wet soils this species is often found in meadows, fens, swamps, and streambanks. Attractive ornamental characteristics includes early spring, showy flowers and yellow foliage in the fall. Salix discolor provides a critical source of pollen at the beginning of the growing season for a plethora of pollinators and also serves as a larval host to many insect species. Salix discolor are commonly used in the cut flower industry for both their showy catkins and colorful, dormant winter stems. This accession represents genetics from northeastern Minnesota. Specimens sampled in nature ranging from 6-22' in height. 2138039Ames 35807
44Ames 35806Reichelt PrairieSalix humilis Marshall var. tristis (Aiton) Griggs Iowa, United StatesNC7PLANT2022COLLECTED05/16/2022Reichelt Unit of Rock Creek State Park on south side of US highway 6 approximately 7.70 miles west, southwest of Grinnell, T80N R17W SE ¼ SE ¼ Sec. 30.41.70311300, -92.86569100274Xeric prairie remnant. Hilltop/knoll.Wild materialPlants sampled in nature measuring 2.0-4.0 feet in height. Specimens noted during peak flowering and seed dispersal on 21 April and 17 May (2022), respectively. Some plants upright and some rather prostrate. Site was mowed in winter 2020/2021 winter resulting in significant flowering in 2022. In cultivation (central Iowa), plants are extremely short and compact where after two field seasons plants are rather uniform and topping out at a height of 2.5'. Dense suckering immediately surrounding clump/base of plant. Peak fall color (central Iowa) occurring in mid-November. 2137912Ames 35806
45Ames 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
46OPGC 7585Pleggenkuhle PrairieLiatris pycnostachya Michx. Iowa, United StatesOPGC2022COLLECTED09/29/2021Pleggenkuhle Prairie located 2.11 miles northwest of Hawkeye, T94N R10W Sec. 14.42.95783800, -91.98405900341Wet-mesic prairie remnant on Clyde Silty Clay Loam and Floyd Loam soils.Wild material2133094OPGC 7585
47NA 86885RJL2021PA-004Ilex verticillata (L.) A. Gray Pennsylvania, United StatesNA2021COLLECTED11/16/2021Plants growing in woodlands along a small unnamed creek corridor dumping into the Middle Branch White Clay Creek in Goddard Park, West Grove Pennsylvania, off of Wickerton Road, Chester County.39.81063861, -75.82750806124Plants are growing in a range of habitats from mesic woodlands to saturated streamside settings of deciduous woodlands that drain toward the Middle Branch White Clay Creek. Plants grow in high understory shade with dappled to indirect sunlight. The only female (fruiting) plants were found in areas along the creek where soils are moist to saturated. Numerous male specimens were found in the areas described above. Soils: Soils found in the areas where this collection was made are comprised primarily of Baile silt loam (Ba), Hatboro silt loam (Ha), and Glenelg silt loam, 8 to 15 percent slopes (GgC). Baile silt loam consists of very deep, poorly drained, moderately low to moderately high saturated hydraulic conductivity, soils on upland depressions and footslopes that were formed in local alluvium over residuum from acid crystalline rocks, chiefly mica schist and granitized schist and gneiss; slope ranges from 0 to 8 percent. Hatboro silt loam consists of very deep and poorly drained soils formed in deposited alluvium derived from metamorphic and crystalline rock. They are on flood plains. Slopes range from 0 to 3 percent. Glenelg silt loam, 8 to 15 percent slopes consists of very deep, well drained soils formed in residuum weathered from micaceous schist on uplands of the Blue Ridge and the Northern Piedmont. This soil is undifferentiated, mostly poorly drained sandy bottomland soils intermingled with decomposing organic litter and eroded silts and clays due to erosion. Slope: 0 to 15% Aspect: Variable.Wild material2123125NA 86885
48WLP 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
49WLP 1732RJL2021PA-002Viburnum prunifolium L. Pennsylvania, United StatesNA2021COLLECTED11/05/2021Plants growing in woodlands along a small unnamed creek corridor dumping into the Middle Branch White Clay Creek in Goddard Park, West Grove Pennsylvania, off of Wickerton Road, Chester County.39.80462083, -75.82888750102Plants are growing in a range of habitats from drier upland woods to moist creekside settings of deciduous woodlands that drain toward the Middle Branch White Clay Creek. Plants grow in part shade to high understory shade with dappled to indirect direct sunlight. Plants achieve their largest size and fruiting potential in part sun of the riparian zone of the creek where woodland canopy is thinner. Soils: Soils found in the areas where this collection was made are comprised primarily of flood plain Hatboro silt loam (Ha) and well-drained, upland Glenelg silt loam, 8 to 15 percent slopes (GgC). Hatboro silt loam consists of very deep and poorly drained soils formed in deposited alluvium derived from metamorphic and crystalline rock. They are on flood plains. Slopes range from 0 to 3 percent. Glenelg silt loam, 8 to 15 percent slopes consists of very deep, well drained soils formed in residuum weathered from micaceous schist on uplands of the Blue Ridge and the Northern Piedmont. This soil is undifferentiated, mostly poorly drained sandy bottomland soils intermingled with decomposing organic litter and eroded silts and clays due to erosion. Slope: 0 to 15% Aspect: Variable.Wild material2123098WLP 1732
50WLP 1733RJL2021PA-003Viburnum dentatum L. Pennsylvania, United StatesNA2021COLLECTED11/05/2021Plants growing in woodlands along a small unnamed creek corridor dumping into the Middle Branch White Clay Creek in Goddard Park, West Grove Pennsylvania, off of Wickerton Road, Chester County.39.80522167, -75.82928139107Plants are growing in a range of habitats from mesic woodland to moist creekside settings of deciduous woodlands that drain toward the Middle Branch White Clay Creek. Plants grow in high understory shade with dappled to indirect sunlight. Soils: Soils found in the areas where this collection was made are comprised primarily of flood plain Hatboro silt loam (Ha) and well-drained, upland Glenelg silt loam, 8 to 15 percent slopes (GgC). Hatboro silt loam consists of very deep and poorly drained soils formed in deposited alluvium derived from metamorphic and crystalline rock. They are on flood plains. Slopes range from 0 to 3 percent. Glenelg silt loam, 8 to 15 percent slopes consists of very deep, well drained soils formed in residuum weathered from micaceous schist on uplands of the Blue Ridge and the Northern Piedmont. This soil is undifferentiated, mostly poorly drained sandy bottomland soils intermingled with decomposing organic litter and eroded silts and clays due to erosion. Slope: 0 to 15% Aspect: Variable.Wild material2123124WLP 1733
51W6 59938CBG-10661Poa palustris L. Illinois, United StatesW6SEED2021Wild material2132517W6 59938
52Ames 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
53W6 59182CBG-10473Echinacea pallida (Nutt.) Nutt. Illinois, United StatesW62021Wild material2120103W6 59182
54Ames 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
55OPGC 7553Williams PrairieLiatris pycnostachya Michx. Iowa, United StatesOPGCHABITAT2020COLLECTED09/25/2020Williams Prairie State Preserve approximately 3 miles north of Oxford, T80N R8W SW1/4 NE1/4 Sec. 5, Johnson County41.76811400, -91.80062300226Dry, upland portions of a remnant wet prairie.Wild materialPlants sampled in nature were 1.5 to 3 feet in height. At time of collection (25 September 2020), approximately 20% of the seed had begun to disperse. Some plants still had green leaves, while most were entirely senesced. 2107740OPGC 7553
56WLP 2018MARSB-976Viburnum opulus L. var. americanum Aiton New York, United StatesNA2019COLLECTED08/01/2019Dutchess County; Tivoli; Bard College campus.200Open marsh (tidal marsh), full sun, red maple swamp; growing in moist loamy sand.Seed collected from 20 plants; population scattered in distribution, found over a 1 mile by 1 mile area. Seed maturation early, middle.2109167WLP 2018
57WLP 2036MARSB-1003Viburnum opulus L. var. americanum Aiton New York, United StatesNA2019COLLECTED08/30/2019Columbia County; Germantown; Rt. 9 (9G?)/Main St. right-of-way, Germantown.183Roadside right-of-way in full sun; growing in moist loamy sand.Seeds collected from 40 individuals in a population of 50+ plants occurring over an area 300 meters by 500 meters in size; common. Seed maturation: middle.2109185WLP 2036
58WLP 2038MARSB-1005Viburnum lentago L. New York, United StatesNA2019COLLECTED09/19/2019Columbia County; Germantown; Rt. 6, Germantown. [This appears to be south of Germantown. -SBL]183Marsh.Seeds collected from 20 individuals in a population of 25+ plants; scattered distribution. Seed maturation: middle. Birds, low fruit set noted.2109187WLP 2038
59WLP 2003MARSB-968Viburnum dentatum L. New York, United StatesNA2019COLLECTED08/04/2019Ulster County; Gardiner; Private residence at 844 Route 208, Gardiner, New York 12525.41.65848000, -74.14236000122Forest, marsh/pond shore in partial to full shade; poorly drained, clay loam soil, seasonally wet/moist.Seeds collected from plant. Many seeds had already dropped or been eaten; seeds collected from an approximately 1 acre (or 4000 square meters) area with Viburnum dentatum growing in several dense patches and sparsely between. Species common, scattered in area; 100-plus individuals estimated in approximately 4000 square meters.2109099WLP 2003
60WLP 2004MARSB-969Viburnum dentatum L. New York, United StatesNA2019COLLECTED07/31/2019Onondaga County; Liverpool; Hamlin Swamp (two sets of coordinates and data collected over two days at this site; the earlier data is noted first. The second set of coordinates given is 43.150864 deg. N, 76.175374 deg. W.)43.15140000, -76.17474000Edge of wetland. Marsh/pond shore in full sun; moist to wet, clay loam to clay soil.Seeds collected directly from plants. Collected in two partial collections, one on 7/31/2019 and the second on 8/8/2019; Species common to scattered in area; 50+ individuals in population visited on 7/31/2019, and 30+ individuals in the population visited on 8/8/2019 (five individuals sampled from the second site; number of individuals sampled at first site not recorded.) Seed quality good.2109100WLP 2004
61WLP 2008MARSB-974Viburnum dentatum L. New York, United StatesNA2019COLLECTED07/29/2019Columbia County; Clermont; Church Avenue, Clermont, New York; privately owned agricultural land.0.00000000, 0.00000000183Edge of oak-hickory woodland in partial shade; growing in dry clay-loam soil.Seeds collected directly from plants. Species common in area; 50+ individuals in population, 50+ individuals sampled, with population area 1/4 mile (linear).2109104WLP 2008
62WLP 2009MARSB-975Viburnum dentatum L. New York, United StatesNA2019COLLECTED08/01/2019Columbia County; Germantown; Eastern Parkway, Germantown, New York; privately owned agricultural land.0.00000000, 0.00000000183Field edge, shrubland, in full sun; moist, well-drained, loamy sand soil.Seeds collected directly from plants. Species common in area; 50+ individuals in population, 50 individuals sampled, with population area 1 mile (linear).2109105WLP 2009
63WLP 2010MARSB-977Viburnum dentatum L. New York, United StatesNA2019COLLECTED08/02/2019Greene County; Catskill; Scenic Hudson plot (land in conservation use) on Kukuk Rd in Catskill, New York [Note: location could not be found on maps, and no latitude and longitude were supplied; possibly Kukuk Lane in Kingston, New York, which is a bit south of Catskill. -SBL]0.00000000, 0.0000000091Edge of oak-hickory woodland; growing in full sun in loamy sand soil.Seeds collected directly from plants. Sparse seed set noted. Species scattered in area; 30+ individuals in population, 32 individuals sampled, with population area 1 mile x 1 mile.2109106WLP 2010
64OPGC 7460CBG-8191Pedicularis canadensis L. Wisconsin, United StatesOPGCSEED2019Wild material2092673OPGC 7460
65OPGC 7464CBG-8630Heuchera richardsonii R. Br. Wisconsin, United StatesOPGCSEED2019Wild material2092685OPGC 7464
66W6 56648CBG-9070Amorpha canescens Pursh Wisconsin, United StatesW6SEED2019Wild material2092747W6 56648
67Ames 34337Doolittle PrairieDrymocallis arguta (Pursh) Rydb. Iowa, United StatesNC7SEED2018COLLECTED08/17/2018Doolittle Prairie State Preserve located approximately 2.5 miles south of Story City, T85N R24W NW 1/4 NE 1/4 Sec. 25, Story County42.15048400, -93.58989700303Prairie remnant.Wild material1967539Ames 34337
68Ames 34200Ellsworth Clear LakeTownship CemeterySalix humilis Marshall var. tristis (Aiton) Griggs Iowa, United StatesNC7FLOWER2018COLLECTED05/17/2018Ellsworth Clear Lake Township Cemetery located approximately 4.68 miles west, southwest of Randall just east of Olsen Ave., off 390th Street, T86N R24W NW ¼ SE ¼ SW ¼ Sec. 30.42.22720200, -93.69239400325Dry ridge top. Remnant prairieWild materialSpecimens at collection site in nature measuring approximately 2.5 feet in height with significant suckering and minimal branching. Stem color (variable) at time of collection (17 May 2018) with mostly dark yellow, greenish or brownish-orange. Female catkins measuring 1.25-2.00 cm. Pubescent leaves, rounded at tips. Plants with severe dieback (e.g. 1-2' on stems), but are respouting. Unknown if dieback at collection site is due to herbicide or environmental conditions. According to local botanist and author of the Vascular Flora of Hamilton County, Iowa (Thompson 2007), Thompson indicated this was the largest population observed (Thompson pers. comm., 16 May 2018) in Hamilton County. During a growout via seed executed in 2018 at NCRPIS, a total of 64 plants generated 19 males and 45 females.1963307Ames 34200
69Ames 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
70Ames 34031JDC/MF/2017/058/812Monarda fistulosa L. Iowa, United StatesNC7SEED2017COLLECTED10/12/2017Doolittle Prairie State Preserve located approximately 2.5 miles south of Story City, T85N R24W NW 1/4 NE 1/4 Sec. 25, Story County42.15048400, -93.58989700303Prairie pothole wetland complex.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 (10/12/2017). Plants sampled generally 3' in height.1954320Ames 34031
71Ames 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
72Ames 34023Ames 34023Viburnum prunifolium L. Iowa, United StatesNC7FRUIT2017COLLECTED09/27/2017Shimek State Forest, Donnellson Unit, approximately 6.0 miles west of Donnellson.40.64796000, -91.67764000219Oak-hickory upland forest.Wild materialPlants at collection site ranging between 10-15' tall. Fruits dark purple, leaves on some stems were turning red fall color at time of collection (09/27/2017).1953995Ames 34023
73Ames 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
74Ames 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
75Ames 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
76Ames 32957JDC/BP/2015/044/701Betula pumila L. Iowa, United StatesNC7PLANT2015COLLECTED09/04/2015Private property approximately 1.5 miles northwest of Lawler. T96N R11W SW 1/4 SW 1/4 Sec. 32 Chickasaw County.43.08335400, -92.17787800349High-quality remnant wetland/fen. Growing in Plams muck soils in association with Salix spp., Cornus racemosa, Oncolea sensibilis, Spiraea alba, Gentiana spp., Carex spp., Populus tremuloides, and Ambrosia trifida. Noted four specimens likely B. x sandbergii that were approximately 30-35' in height.Wild materialB. pumila could be considered a dominant species in portions of this site. Female catkins were both green and brown at time of harvest. Specimens average approximately 275 cm in height. Little to no fall color. Approximately 75% of leaves were already dropped. 1927399Ames 32957
77Ames 32820APS/EA/2013/041/126Euonymus atropurpureus Jacq. Iowa, United StatesNC7SEED2014COLLECTED10/10/2014Midland Trail Road near North Racoon River watershed. Dallas County T80N R27W SW 1/4 NW 1/4 Sec. 3041.71142000, -94.04538000299Wooded roadside.Wild material1921780Ames 32820
78Ames 32801JDC/SA/2014/046/548Spiraea alba Du Roi Iowa, United StatesNC72014COLLECTED09/19/2014Pike Run Wildlife Management Area located near intersection of Iron City Avenue and 170th Street, T77N R3W NW 1/4 of NW 1/4 of Sec. 9.41.49354000, -91.21225800187Remanant, wet prairie. Aquolls (0-2 percent slopes) depth to water table: about 0-12 inches, 0-24 inches: variable soil types, very poorly drained; and Intermittent waterWild material1921812Ames 32801
79Ames 32761JDC/BP/2014/034/536Betula pumila L. Iowa, United StatesNC7MISCELLANEOUS2014COLLECTED09/03/2014Crossman Prairie State Preserve, approximately 5 miles northeast of Riceville, Howard County.43.40777300, -92.47500720413Remnant tallgrass prairie. Wild material1921309Ames 32761
80Ames 32762JDC/BP/2014/044/546Betula pumila L. Iowa, United StatesNC7Fruit2014COLLECTED09/03/2014Private property, located approximately 2 miles south of Sumner, Bremer County.42.80952700, -92.10866400328Remnant wet prairie. Wild material1921310Ames 32762
81Ames 32766JDC/MF/2014/042/544Monarda fistulosa L. Iowa, United StatesNC72014COLLECTED09/03/2014Private property, located approximately 2 miles south of Sumner, Bremer County.42.80924300, -92.10579900324Remnant wet prairie. Wild material1921314Ames 32766
82Ames 32767JDC/PV/2014/036/538Prunella vulgaris L. Iowa, United StatesNC7PLANT2014COLLECTED09/03/2014Crossman Prairie State Preserve, approximately 5 miles northeast of Riceville, Howard County.43.40777300, -92.47500720413Remnant tallgrass prairie. Wild material1921315Ames 32767
83Ames 32769JDC/SA/2014/033/535Spiraea alba Du Roi Iowa, United StatesNC7MISCELLANEOUS2014COLLECTED09/03/2014Crossman Prairie State Preserve, approximately 5 miles northeast of Riceville.43.40777300, -92.47500720413Remnant tallgrass prairie. Clyde-Floyd complex (1-4 percent slopes) depth to water table: 12-42 inches, 0-17 inches silty clay loam, somewhat poorly drainedWild material1921317Ames 32769
84Ames 32770JDC/SA/2014/043/545Spiraea alba Du Roi Iowa, United StatesNC7MISCELLANEOUS2014COLLECTED09/03/2014Brayton-Horsley Prairie located approximately 2 miles south of Sumner, T92N R11W NE 1/4 NW 1/4 SE 1/4 Sec. 2.42.80957200, -92.10705300323Remnant wet prairie. Klossner muck (1-3 percent slopes) depth to water table: about 0 inches, 0-10 inches: muck, very poorly drainedWild material1921318Ames 32770
85OPGC 4196JDC/LP/2014/035/537Liatris pycnostachya Michx. Iowa, United StatesOPGC2014COLLECTED09/03/2014Crossman Prairie State Preserve, approximately 5 miles northeast of Riceville, Howard County.43.40777300, -92.47500720413Remnant tallgrass prairie. Associated with Aesclepias, Amorpha canescens, Andropogon gerardi, Baptisia, Betula pumila, Cornus amomum, C. racemosa, Dalea purpurea, Eryngium yuccifolium, Gentiana andrewsii, Helianthus grosseserratus, Hypericum ascyron subsp. pyramidatum, Liatris pcynostachya, Monarda fistulosa, Populus tremuloides, Prunella vulgaris, Prunus americana, Salix, Silphium laciniatum, Solidago, and Spiraea alba.Wild material1921312OPGC 4196
86Ames 32095JDC/SA/2013/049/493Spiraea alba Du Roi Iowa, United StatesNC72013COLLECTED11/01/2013Floodplain of South Skunk River near Bondurant, Chichaqua Bottoms Greenbelt, T80N R22W SW 1/4 of SW 1/4 of NW 1/4 of Sec.13, NW 1/4 of SE 1/4 of Sec. 10, and SW 1/4 of SW 1/4 of NE 1/4 of Sec. 24, Mitchellville Quad.41.73534400, -93.36737800245Spillville loam (0-2 percent slope) depth to water table: 48-72 inches, 0-44 inches: loam, moderately well drained; and Coland clay-loam soil (0-2 percent slope) depth to water table: 0-12 inches, 0-8 inches: clay loam, poorly drained/occasionally floddedWild material1914039Ames 32095
87Ames 31982APS/GD/2013/004/089Gymnocladus dioicus (L.) K. Koch Kansas, United StatesNC7FRUIT2013COLLECTED02/18/2013Walnut Creek watershed, southwest of Marysville, Sections 5, 8, and 17, T3S R6E, Marshall County.39.79300943, -96.78506600382Dry floodplain.Wild material1907535Ames 31982
88Ames 31983APS/GD/2013/006/091Gymnocladus dioicus (L.) K. Koch Kansas, United StatesNC7FRUIT2013COLLECTED02/19/2013Beaver Creek, south of Scandia, Sections 7, 12, and extreme NW 1/4 of NW 1/4 of Section 8, T4S R5W, Republic County.39.72143025, -97.81205050432Dry floodplain.Wild material1907536Ames 31983
89Ames 31987APS/GD/2013/011/096Gymnocladus dioicus (L.) K. Koch Kansas, United StatesNC7FRUIT2013COLLECTED02/20/2013Camp Wood, near Cottonwood River, south of Elmdale, NW 1/4 of Section 3, T20S R7E, Chase County.38.34698100, -96.65080500377Samples obtained from both upland, rocky and floodplain habitat.Wild material1907540Ames 31987
90Ames 31519JDC/FQ/2012/028/421Fraxinus quadrangulata Michx. Iowa, United StatesNC7SEED2012COLLECTED07/20/2012Along Twin Rivers Drive, NE 1/4 of Section 34, T65N, R5W, Keokuk Quad, just southwest of Keokuk, Des Moines County.40.38649700, -91.42619300182Dry woods. Steep south and southwest-facing slopes. Wild material1903746Ames 31519
91Ames 31528JDC/FQ/2012/037/430Fraxinus quadrangulata Michx. Indiana, United StatesNC7SEED2012COLLECTED07/24/2012Along Highway 52, N 1/2 of Section 19, T9N, R2W, Brookville Quad, approximately 0.5 to 1 mile west of Brookville, Franklin County.39.43205200, -85.02163400209Roadside collection. South and southeast-facing slopes. Wild material1903755Ames 31528
92Ames 31054359Betula lenta L. New York, United StatesNC7SEED2011COLLECTED09/11/2011Hurd Cross Road, Steuben County.42.04000000, -77.07900000443Roadside. Wild material1891440Ames 31054
93Ames 31072693Fraxinus americana L. New York, United StatesNC7SEED2011COLLECTED09/12/2011840 to 1150 Turnpike Road, Allegany County.42.30200000, -77.79000000570Roadside and field edges. Southwest-facing slope (10-15 degrees). Wild material1891458Ames 31072
94Ames 31081711Fraxinus americana L. New York, United StatesNC7SEED2011COLLECTED09/11/2011Harrison Road, Steuben County.42.04500000, -77.06900000461Roadside of dry woods. Wild material1891467Ames 31081
95Ames 31082712Fraxinus americana L. New York, United StatesNC7SEED2011COLLECTED09/11/2011Federal Road, south of Marsh Road (Co. 4), Chemung County.42.15600000, -76.65500000466Roadside and woodland edges. Wild material1891468Ames 31082
96WLP 1955360Viburnum lentago L. New York, United StatesNAFLOWER2011COLLECTED09/11/2011Hurd Cross Road, Steuben County.42.03600000, -77.07600000470Upland roadside. Mixed forest. Slight slope with west facing aspect. Associated with Acer saccharum, Betula papyrifera, Cornus florida (few), Cornus racemosa, Fraxinus americana, and Vitis riparia.Wild material1891493WLP 1955
97WLP 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
98Ames 30685JDC/FP/2010/075/345Fraxinus pennsylvanica Marshall Wisconsin, United StatesNC7SEED2010COLLECTED09/30/2010Parking area for Richter Lane boat ramp, north side of Trauba Road, near northeast shore of Lake Poygan, SE 1/4 of NE 1/4 of Section 36, T20N R14E, Lake Poygan Quad, Winnebago County.44.16382000, -88.76668000230Wild material1853843Ames 30685
99Ames 30148JDC/FP/2009/045/195Fraxinus pennsylvanica Marshall Wisconsin, United StatesNC7SEED2009COLLECTED09/23/2009South side of Chub Lake, SE 1/4 of NE 1/4 of Section 25, T9N, R13E, Waterloo Quad, Dodge County.43.21944444, -88.89388889239Crawfish River watershed. Wet, open woodland. Wild material1819729Ames 30148
100Ames 30164LQ/PV/2009/004/004Prunella vulgaris L. Wisconsin, United StatesNC7SEED2009COLLECTED09/23/2009South side of Chub Lake, SE 1/4 of NE 1/4 of Section 25, T9N, R13E, Waterloo Quad, Dodge County.43.21944444, -88.89388889239Crawfish River watershed. Wet, open woodland. Wild material1819745Ames 30164
101WLP 2486JDC/VL/2009/023/173Viburnum lentago L. Wisconsin, United StatesNAFLOWER2009COLLECTED09/21/2009Along Bowers Road west of Snow Bottoms State Natural Area, Highland West Quad. T7N R1W SW1/4 SW /4 SE1/4 Sec. 3443.03200000, -90.47680000267RoadsideWild materialVariation in leaf thickness, fall color (mostly reddish tones) and degree of powdery mildew was noted across population sampled in nature. At time of collection (12 September) fruits were at various stages of maturity including green, red, blue/black. 1819759WLP 2486
102Ames 2731118Rhus typhina L. Iowa, United StatesNC72003COLLECTED09/15/2003Edge of road, north side of creek, Bixby State Park, Edgewood, T91N R5W SE 1/4 of SW 1/4 of Sec. 23, Edgewood Quad, Clayton County42.67527778, -91.40111111303Road edge. Mostly sunny. Slight slope with a southern aspect. Wild materialTall shrubs to 5 meters tall. 1649468Ames 27311
103WLP 1931Ames 27284Viburnum lentago L. Iowa, United StatesNA2003COLLECTED09/07/2003Along Wapsi Great Western Trail, Lake Hendricks County Park, T99N R14W, NE corner of SW 1/4 of SW 1/4, Section 19, Riceville Quad, Howard County.43.37694444, -92.55111111378Associated with Acer negundo, Parthenocissus, Rhamnus cathartica, Cornus racemosa, and Solidago altissima.Wild materialSmall trees to 4 meters tall.1648680WLP 1931