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ACCESSIONPLANT NAMETAXONOMYORIGINGENEBANKIMAGEAVAILABILITYRECEIVEDSOURCE TYPESOURCE DATECOLLECTION SITECOORDINATESELEVATIONHABITATIMPROVEMENT LEVELNARRATIVE
0PI 662010JDC/CA/2008/013/083Cornus alternifolia L. f. Iowa, United StatesNC7SEED2003COLLECTED09/15/2003West side of Fortune Road, just north of 38558 Fortune, near entrance to Bixby State Park, north of Edgewood, SW corner of SE 1/4 of NW 1/4 of Section 26, T91N, R5W, Edgewood Quad, Clayton County.42.66694444, -91.40333333329Woodland. Steep bank along creek. 100% filtered shade. Soil consisted of organic matter and rock fill with many stones, well drained. Wild materialSmall tree. Very late fruiting. 1649455PI 662010
1Ames 36260Thomson Causeway Recreation AreaCornus drummondii C. A. Mey. Illinois, United StatesNC7HABITAT2024COLLECTED08/19/2024Thomson Causeway Recreation Area, approximately 1 mile southwest of Thomson. Scattered along Potter Road starting just east of the causeway heading west, and along the gravel service road to the south. T23N R3E SE 1/4 Sec. 26.41.94919700, -90.11822100179Floodplain of wetland complex along east bank of Mississippi River. Soils are moist and seasonally inundated with high organic matter content. Wild materialShrubs in nature measuring approximately 10 feet in height (to 15 feet) with varying degrees of red pigmentation on the pedicles. Peak fruit ripening occurred in late August 2024. Minor foliar disease noted at the time of collection. Growing as individual shrubs in shadier locations and forming thickets in sunnier sites.2168984Ames 36260
2NA 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
3W6 55946NV030-1333Cornus sericea L. subsp. occidentalis (Torr. & A. Gray) Fosberg California, United StatesW6SEED2018Wild materialCornus sericea subsp. occidentalis1970657W6 55946
4W6 55392OR050-275Cornus sericea L. subsp. occidentalis (Torr. & A. Gray) Fosberg Oregon, United StatesW6SEED2018Wild materialCornus sericea ssp. occidentalis1967944W6 55392
5WLP 1117NA 83967Cornus foemina Mill. Kentucky, United StatesNA2016COLLECTED09/30/2016[Locality data unparseable; GPS coordinates appear near a road of uncertain name off Howard Munsey Rd. north of Betsey, Kentucky. Original location was listed as: "At Edam Road?"; no road by this name was found in the county. -SBL]36.92000000, -84.73900000274Wet roadside couvee (ditch).1952406WLP 1117
6Ames 30552Ames 30552Cornus alternifolia L. f. Missouri, United StatesNC7SEED2010COLLECTED06/29/2010Along North River, Callaghan Mound Access Conservation Area, near Heather, SW 1/4 of Section 15, T58N, R8W, Emden Quad.39.82140000, -91.78680000190Northeast facing slope.Wild material1843106Ames 30552
7Ames 30366JDC/CA/2009/090/240Cornus amomum Mill. subsp. obliqua (Raf.) J. S. Wilson Ohio, United StatesNC7SEED2009COLLECTED10/16/2009Along Dicks Creek, Wayne National Forest, just southeast of Kitchen, NW 1/4 of NE 1/4 of Section 5, T6N, R17W, Gallia Quad, Jackson County.38.86166667, -82.53805556204Wet marsh. Wild material1823918Ames 30366
8WLP 1046JDC/CF/2009/091/241Cornus florida L. Ohio, United StatesNA2009COLLECTED10/16/2009Wayne National Forest, near Dirtyface Creek, SE 1/4 of SW 1/4 of Section 21, T6N, R17W, Gallia Quad, Jackson County.38.80750000, -82.53000000210Associated with Acer saccharum, Cephalanthus occidentalis, Eutrochium maculatum, Hypericum densiflorum, Liriodendron tulipifera, Monarda fistulosa, Penstemon digitalis, Pinus virginiana, Prunella vulgaris, Rhus copallinum, (continued below)Wild material1823920WLP 1046
9Ames 30133JDC/CD/2009/063/213Cornus drummondii C. A. Mey. Illinois, United StatesNC7SEED2009COLLECTED09/25/2009Four Corners Road, north from Illinois Highway 84, NW 1/4 of SW 1/4 of Section 36, T26N, R2E, Blackhawk (IL-IA) Quad, Jo Daviess County.42.20027778, -90.22944444194Roadside in fence row. Wild material1819714Ames 30133
10Ames 29523JDC/CA/2008/015/085Cornus alternifolia L. f. Illinois, United StatesNC7SEED2008COLLECTED08/06/2008Along trail heading towards lake, Crosby Road to parking lot, Morrisson-Rockwood State Park, approximately 2 miles north of Morrisson, Whiteside County.41.84222222, -89.96888889247Woodland area. 100% filtered shade. Wild material1782640Ames 29523
11NA 88710RJL2023NCSC-015Cephalanthus occidentalis L. South Carolina, United StatesNA2023COLLECTED11/14/2023Francis Marion National Forest: plants growing in wetlands/swamps on US Forest Service Road 223 approximately 0.57 kilometers southeast from the junction with Halfway Creek Road.33.06771000, -79.6776970020Plants are growing in part-shade to sun along the edges of the swamp in seasonally inundated acidic wetland habitat. Slope: N/A. Aspect: N/A. The underlying geology of this area is of Pleistocene origin and characterized as an Socastee Formation. This is a low coastal formation in the Carolinas like Penholoway but younger and lower in altitude. It is comprised primarily of unconsolidated, fine-detrital clay. It is described as variegated quartzose sands, argillaceous sands, and clays, 5 m thick at the type section near Socastee Swamp. (Source: USGS South Carolina Geologic Map Data.) The primary soil type in this collection area is classified as Rutlege Series loamy fine sand. Rutlege Series soils are very deep, very poorly drained soils that are sandy, siliceous, thermic Typic Humaquepts. Upper strata soils (0-38 cm) are black loamy sand with weak medium granular structure. They are loose and very strongly acid. Lower strata (38-175 cm) range from dark gray to dark brown sand that is single grained, loose, and very strongly acid. (Source: NRCS Web Soil Survey.)Wild material2159138NA 88710
12NA 88283NEWFS-554Cephalanthus occidentalis L. Massachusetts, United StatesNA2021Wild materialOpposite branches, balls of white flowers, seeds in balls.2115694NA 88283
13WLP 170NACPEC19-061Cephalanthus occidentalis L. Georgia, United StatesNA2019COLLECTED09/15/2019Walker County; Lula Lake Land Trust: Lula Lake Land Trust Falls: East Side of Falls34.93361200, -85.37187800427Ravine, slope forest, stream margin at Lula Lake FallsWild material2110482WLP 170
14NA 87967CBG-8082Cephalanthus occidentalis L. Illinois, United StatesNASEED2017Wild material1954783NA 87967
15NA 87968CBG-7597Thuja occidentalis L. Illinois, United StatesNASEED2017Wild material1954885NA 87968
16WLP 858APS/CO/2014/034/165Cephalanthus occidentalis L. Iowa, United StatesNA2014COLLECTED10/07/2014Lake Rathbun Wildlife Management Area (SW Unit), NE 1/4 of Section 16, T69N, R20W, Wayne County.40.77822200, -93.15527400306Bottomland/floodplaind overflow of South Fork Chariton River. Associated with Acer saccharinum, Carya cordiformis, C. laciniosa, Cornus amomum subsp. obliqua, and Tilia americana.Wild material1921815WLP 858
17WLP 856JDC/CO/2009/043/193Cephalanthus occidentalis L. Wisconsin, United StatesNA2009COLLECTED09/22/2009Wisconsin: Columbia County; Pine Island State Wildlife Area, Wisconsin River flood plain along Levee Road, SW 1/4 of NW 1/4 of Section 11, T12N, R8E, Pine Island Quad, Columbia County.43.53250000, -89.51555556242Wisconsin River watershed/floodplain. Associated with Acer saccharinum, Betula nigra, Cornus amomum subsp. obliqua, Fraxinus pennsylvanica, and Quercus bicolor.Wild material1819711WLP 856
18WLP 837RES019Cephalanthus occidentalis L. Michigan, United StatesNA2008COLLECTED10/16/2002Michigan: Ingham County; East side of Lake Lansing Road, west side of Lake Lansing, south of Lake Lansing South Park.42.75222222, -84.40416667259Marshy area along road. Associated vegetation: Cornus sericea.Wild material1775515WLP 837
19WLP 771NA 73814Cephalanthus occidentalis L. Iowa, United StatesNAPLANT2003COLLECTED10/21/2003Chichaqua Wildlife Habitat Park bottoms, Elkhart, T81N R22W, NW 1/4 of NW 1/4, Section 32, Loring Quad, Polk County.41.79000000, -93.43972222247Edge of oxbow ponds. Sunny. Flat. Alluvial soil. Associated with reed canary grass, Anemone canadensis, Quercus bicolor, Cornus drummondii, and Amorpha fruticosa.Wild materialLarge, well branched shrubs to 2.5 meters tall.1649920WLP 771
20PI 710486CBG-9082Desmodium canadense (L.) DC. Wisconsin, United StatesS9SEED2019Wild material 2092756PI 710486
21PI 664899JDC/PV/2009/092/242Prunella vulgaris L. Ohio, United StatesNC7SEED2009COLLECTED10/16/2009Wayne National Forest, near Dirtyface Creek, SE 1/4 of SW 1/4 of Section 21, T6N, R17W, Gallia Quad, Jackson County.38.80750000, -82.53000000210Open prairie. Variable soil types present. Wild material1823940PI 664899
22PI 64974544Symphoricarpos orbiculatus Moench Iowa, United StatesNC72003COLLECTED10/21/2003Chichaqua Wildlife Habitat Park bottoms, Elkhart, NW corner of SE 1/4 of SE 1/4 of Section 29, T81N, R22W, Loring Quad, Polk County.41.79472222, -93.42972222250Alluvial soil. Understory of green ash, Cornus drummondii, Rubus occidentalis, and Smilax.Wild materialLow, suckering shrubs to 1 meter tall. Good fruit and foliage quality.1649921PI 649745
23NA 885832024RJLFL-014Ilex amelanchier M. A. Curtis ex Chapm. Florida, United StatesNA2024COLLECTED11/13/2024Yellow River Water Management Area: found in an area where an unnamed unpaved road dead ends near the Yellow River. This unpaved road is accessed from Old River Road to the east near the junction with Shockley Springs Road. Individual plants for this collection were accessed by foot along the edge of the river and associated wetland depressions to the east of the road. The sampling for this portion of the population extends from the GPS coordinates listed above to the northeast where sampling ended at coordinates 30.871238 deg. N, 86.590170 deg. W.30.86989400, -86.5921850023Plants growing in seasonally inundated swamp habitats associated with the Yellow River and small tributaries. Plants are emergent during portions of the year, primarily during the growing season. During this time of collection, water had receded from the wetlands and the area was relatively dry. Slope: N/A. Aspect: N./A. The underlying geology of this area is the Alum Bluff Group of Miocene origin. It includes the Chipola Formation, Oak Grove Sand, Shoal River Formation, Choctawhatchee Formation and the Jackson Bluff Formation. The formations included in this group are generally defined based on their molluscan faunas and stratigraphic position. Puri (1953) described sediment facies as they relate to the formations of the Alum Bluff Group. These sediments are lithologically distinct as a group, not as individual units. The Alum Bluff Group crops out or is beneath a thin overburden in the western panhandle from river valleys in Okaloosa County eastward to western Jackson County. The Alum Bluff Group consists of clays, sands and shell beds which may vary from fossiliferous, sandy clays to unfossiliferous sands and clays and occasional carbonate beds. Mica is a common constituent and glauconite and phosphate occur sporadically. Induration varies from essentially nonindurated in sands to well indurated in carbonate lenses. Colors range from cream to olive gray with mottled reddish brown in weathered sections. Sand grain size varies from very fine to very coarse with sporadic occurrences of gravel. These sediments generally have low permeabilities and are part of the intermediate confining unit/aquifer system. (Source: USGS Florida Geologic Map Data). The surface soil profile of this area is primarily Kinston, Johnston, and Bibb soils, frequently flooded. Kinston Series soils are poorly drained, alluvial, fine-loamy, siliceous, and acid soils of flood plains. They are peaty to loamy friable, slightly sticky, and slightly plastic in the upper 0 to 7.5 cm of the strata with less sand and more silt-loam in progressively deeper strata. The Johnston Series consists of very deep, very poorly drained coarse-loamy, siliceous, active, acid, thermic Cumulic Humaquepts. The upper 0-75 cm is black, mucky loam that is friable and very strongly acid. The lower strata to 1.75 m are dark gray, loamy fine sand, single grained, loose and very strongly acid. (Source: NRCS Web Soil Survey).Wild material2169920NA 88583
24NA 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
25NA 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
26NA 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
27NA 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
28NA 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
29NA 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
30NA 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
31NA 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
32NA 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
33NA 890922024RM-TK-005Ilex amelanchier M. A. Curtis ex Chapm. Florida, United StatesNA2024COLLECTED09/29/2024Yellow River Water Management Area: found in an area where an unnamed, unpaved road dead ends near the Yellow River. This unpaved road is accessed from Old River Road to the east near the junction with Shockley Springs Road. Plants are accessed by foot along the edge of the river and associated wetland depressions to the west of the road.30.86946200, -86.5934900023Plants growing in seasonally inundated swamp habitats associated with the Yellow River. Plants are emergent during portions of the year, primarily during the growing season. During this time of collection, water had receded from the wetlands but the area was still quite wet with many tiny stream rivulets still draining. Slope: 0 percent. Aspect: N/A. Geology: The underlying geology of this area is the Alum Bluff Group of Miocene origin. It includes the Chipola Formation, Oak Grove Sand, Shoal River Formation, Choctawhatchee Formation and the Jackson Bluff Formation. The formations included in this group are generally defined based on their molluscan faunas and stratigraphic position. Puri (1953) described sediment facies as they relate to the formations of the Alum Bluff Group. These sediments are lithologically distinct as a group, not as individual units. The Alum Bluff Group crops out or is beneath a thin overburden in the western panhandle from river valleys in Okaloosa County eastward to western Jackson County. The Alum Bluff Group consists of clays, sands and shell beds which may vary from fossiliferous, sandy clays to unfossiliferous sands and clays and occasional carbonate beds. Mica is a common constituent and glauconite and phosphate occur sporadically. Induration varies from essentially nonindurated in sands to well indurated in carbonate lenses. Colors range from cream to olive gray with mottled reddish brown in weathered sections. Sand grain size varies from very fine to very coarse with sporadic occurrences of gravel. These sediments generally have low permeabilities and are part of the intermediate confining unit/aquifer system. (Source: USGS Florida Geologic Map Data). Soils: The surface soil profile of this area is primarily Kinston, Johnston, and Bibb soils, frequently flooded. Kinston Series soils are poorly drained, alluvial, fine-loamy, siliceous, and acid soils of flood plains. They are peaty to loamy friable, slightly sticky and slightly plastic in the upper 0 to 7.5 cm of the strata with less sand and more silt-loam in progressively deeper strata. The Johnston Series consists of very deep, very poorly drained coarse-loamy, siliceous, active, acid, thermic Cumulic Humaquepts. The upper 0-75 cm is black, mucky loam that is friable and very strongly acid. The lower strata to 1.75 m are dark gray, loamy fine sand, single grained, loose and very strongly a).id. The Bibb Series soils consist 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. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). EPA Ecoregion (Level III): Southeastern Plains (65). EPA Ecoregion (Level IV): Southeastern Floodplains and Low Terraces (65p).Wild material2169056NA 89092
34Ames 36219Egyptian TractSalix sericea Marshall Missouri, United StatesNC7LEAF2024COLLECTED01/19/2024LAD Foundation Egyptian Tract Wet Hollow Seep/Fen Complex located 7.52 miles west, southwest of Annapolis just northwest of intersection of CR 338 and CR 334, T31N R2E SW 1/4 SE 1/4 SE 1/4 Sec. 21 (Lesterville SE Quad.).37.34429700, -90.83361600217Perched wet fen/seep complex with standing water supporting both obligate calciphilic and obligate acidophilic plant species.Wild materialThe native range of Salix sericea is concentrated througout the northeastern and eastern central United States ranging from Maine south to South Carolina, west to Illinois with a relatively large disjunct area in southeastern Missouri (Little, E. L. Jr. 1977). This accession represents genetics from southeastern Missouri in Reynolds County. Shrubs noted at the collection site in nature ranging in height from 2-7 feet and typically twice as wide as tall. Multi-stemmed shrubs expanding vegetatively via layering. Dormant stem colors noted at collection site ranging from mostly greenish to occassionally brownish red and/or copper tones. Dormant buds rather red and often bright red in color. Salix sericea is native to areas of the northeastern U.S. and north into Canada, reaching its western extent in Missouri. Classified as an obligate wetland plant that typically occurs on wet seeps, sedge meadows, streambanks, fens, etc. that are usually slightly acidic. Known to have the potential to reach up to four meters in height, but always much wider than tall. Ornamental characteristics include dark green leaves that are hairless above with undersides that are densely minutely-hairy making them rather white in appearance. Flowering occurs before or during leaf expansion. This species is known to serve as a larval host plant for the Arcadian Hairstreak, Satyrium acadica. 2165775Ames 36219
35NA 88845RJL-RM2023FLAL-019Ilex opaca Aiton Florida, United StatesNA2023COLLECTED12/13/2023Yellow River Water Management Area, found along an unnamed unpaved road leading down to the Yellow River. This unpaved road is accessed from Old River Road to the east near the junction with Shockley Springs Road.30.87382600, -86.6022130035Plants are growing along the road on the woodland edge on a small bluff above a creek in well-drained to dry habitat in part shade. They are also found sporadically in areas along the Yellow River where occasional inundation occurs. Slope: N/A. Aspect: N/A. The underlying geology of this area is the Alum Bluff Group of Miocene origin. It includes the Chipola Formation, Oak Grove Sand, Shoal River Formation, Choctawhatchee Formation and the Jackson Bluff Formation. The formations included in this group are generally defined on the basis of their molluscan faunas and stratigraphic position. Puri (1953) described sediment facies as they relate to the formations of the Alum Bluff Group. These sediments are lithologically distinct as a group, not as individual units. The Alum Bluff Group crops out or is beneath a thin overburden in the western panhandle from river valleys in Okaloosa County eastward to western Jackson County. The Alum Bluff Group consists of clays, sands and shell beds which may vary from fossiliferous, sandy clays to unfossiliferous sands and clays and occasional carbonate beds. Mica is a common constituent and glauconite and phosphate occur sporadically. Induration varies from essentially nonindurated in sands to well indurated in carbonate lenses. Colors range from cream to olive gray with mottled reddish brown in weathered sections. Sand grain size varies from very fine to very coarse with sporadic occurrences of gravel. These sediments generally have low permeabilities and are part of the intermediate confining unit/aquifer system. (Source: USGS Florida Geologic Map Data.) The surface soil profile of this area is primarily Bonifay-Dothan-Angie complex (5 to 12 percent slopes). Bonifay soil consists of very deep, well drained, moderately slowly permeable soils on ridges and side slopes in the Southern Coastal Plain. They formed in thick beds of sandy and loamy marine sediments. Solum thickness ranges from 1.5-2.0 m. Soil reaction ranges from very strongly acid to moderately acid throughout, except where the surface has been limed. Ironstone pebbles, 2 to 15 mm in size, range from 0 to 5 percent, by volume. Depth to the plinthic horizon ranges from 1.1-1.7 m. Some horizons contain up to 25 percent plinthite by volume. The Dothan Series consists of very deep, well drained soils that formed in thick beds of unconsolidated, medium to fine-textured marine sediments. Dothan soils are on interfluves. The surface 0-33 cm is characterized by sandy-loam, well-drained soils that are strongly acid. From 33-200 cm they are characterized by sandy clay loam soils that are more moisture retentive and strongly acid. The Angie series consists of very deep, moderately well drained, slowly permeable soils that formed in loamy and clayey sediment on Tertiary-aged uplands. These soils are on broad, level to strongly sloping coastal plains. Slope is dominantly 1 to 5 percent, but the range is 0 to 12 percent. (Source: NRCS Web Soil Survey.)Wild material2165675NA 88845
36NA 88846RJL-RM2023FLAL-020Ilex decidua Walter Florida, United StatesNA2023COLLECTED12/13/2023Yellow River Water Management Area: found in an area where an unnamed unpaved road dead ends near the Yellow River. This unpaved road is accessed from Old River Road to the east near the junction with Shockley Springs Road.30.86973100, -86.5916870023Plants are growing primarily in part-shade to part-sun in low-lying moist habitats associated with the Yellow River. They are in the flood zone, but not regularly inundated. Slope: N/A. Aspect: N/A. The underlying geology of this area is the Alum Bluff Group of Miocene origin. It includes the Chipola Formation, Oak Grove Sand, Shoal River Formation, Choctawhatchee Formation and the Jackson Bluff Formation. The formations included in this group are generally defined on the basis of their molluscan faunas and stratigraphic position. Puri (1953) described sediment facies as they relate to the formations of the Alum Bluff Group. These sediments are lithologically distinct as a group, not as individual units. The Alum Bluff Group crops out or is beneath a thin overburden in the western panhandle from river valleys in Okaloosa County eastward to western Jackson County. The Alum Bluff Group consists of clays, sands and shell beds which may vary from fossiliferous, sandy clays to unfossiliferous sands and clays and occasional carbonate beds. Mica is a common constituent and glauconite and phosphate occur sporadically. Induration varies from essentially nonindurated in sands to well indurated in carbonate lenses. Colors range from cream to olive gray with mottled reddish brown in weathered sections. Sand grain size varies from very fine to very coarse with sporadic occurrences of gravel. These sediments generally have low permeabilities and are part of the intermediate confining unit/aquifer system. (Source: USGS Florida Geologic Map Data.) The surface soil profile of this area is primarily Kinston, Johnston, and Bibb soils, frequently flooded. Kinston Series soils are poorly drained, alluvial, fine-loamy, siliceous, and acid soils of flood plains. They are peaty to loamy friable, slightly sticky and slightly plastic in the upper 0 to 7.5 cm of the strata with less sand and more silt-loam in progressively deeper strata. The Johnston Series consists of very deep, very poorly drained coarse-loamy, siliceous, active, acid, thermic Cumulic Humaquepts. The upper 0-75 cm is black, mucky loam that is friable and very strongly acid. The lower strata to 1.75 m is dark gray, loamy fine sand, single grained, loose and very strongly acid. The Bibb Series soils 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. (Source: NRCS Web Soil Survey.)Wild material2165676NA 88846
37NA 88847RJL-RM2023FLAL-021Ilex amelanchier M. A. Curtis ex Chapm. Florida, United StatesNA2023COLLECTED12/13/2023Yellow River Water Management Area, found in an area where an unnamed unpaved road dead ends near the Yellow River. This unpaved road is accessed from Old River Road to the east near the junction with Shockley Springs Road. Individuals are accessed by foot along the edge of the river and associated wetland depressions to the west of the road.30.86980100, -86.5921050023Plants growing in seasonally inundated swamp habitats associated with the Yellow River. Plants are emergent during portions of the year, primarily during the growing season. During this time of collection, water had receded from the wetlands but the area was still quite wet with many tiny stream rivulets still draining. Slope: N/A. Aspect: N/A. The underlying geology of this area is the Alum Bluff Group of Miocene origin. It includes the Chipola Formation, Oak Grove Sand, Shoal River Formation, Choctawhatchee Formation and the Jackson Bluff Formation. The formations included in this group are generally defined on the basis of their molluscan faunas and stratigraphic position. Puri (1953) described sediment facies as they relate to the formations of the Alum Bluff Group. These sediments are lithologically distinct as a group, not as individual units. The Alum Bluff Group crops out or is beneath a thin overburden in the western panhandle from river valleys in Okaloosa County eastward to western Jackson County. The Alum Bluff Group consists of clays, sands and shell beds which may vary from fossiliferous, sandy clays to unfossiliferous sands and clays and occasional carbonate beds. Mica is a common constituent and glauconite and phosphate occur sporadically. Induration varies from essentially nonindurated in sands to well indurated in carbonate lenses. Colors range from cream to olive gray with mottled reddish brown in weathered sections. Sand grain size varies from very fine to very coarse with sporadic occurrences of gravel. These sediments generally have low permeabilities and are part of the intermediate confining unit/aquifer system. (Source: USGS Florida Geologic Map Data.) The surface soil profile of this area is primarily Kinston, Johnston, and Bibb soils, frequently flooded. Kinston Series soils are poorly drained, alluvial, fine-loamy, siliceous, and acid soils of flood plains. They are peaty to loamy friable, slightly sticky and slightly plastic in the upper 0 to 7.5 cm of the strata with less sand and more silt-loam in progressively deeper strata. The Johnston Series consists of very deep, very poorly drained coarse-loamy, siliceous, active, acid, thermic Cumulic Humaquepts. The upper 0-75 cm is black, mucky loam that is friable and very strongly acid. The lower strata to 1.75 m is dark gray, loamy fine sand, single grained, loose and very strongly acid. The Bibb Series soils 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. (Source: NRCS Web Soil Survey.)Wild material2165677NA 88847
38NA 88711RJL2023NCSC-016Ilex myrtifolia Walter South Carolina, United StatesNA2023COLLECTED11/14/2023Francis Marion National Forest: plants growing in wetlands/swamps on US Forest Service Road 223 approximately 0.57 kilometers southeast from the junction with Halfway Creek Road.33.06786200, -79.6776180011Plants are growing in shade to part-shade in the swamp in seasonally inundated acidic wetland habitat. Slope: N/A. Aspect: N/A. The underlying geology of this area is of Pleistocene origin and characterized as an Socastee Formation. This is a low coastal formation in the Carolinas like Penholoway but younger and lower in altitude. It is comprised primarily of unconsolidated, fine-detrital clay. It is described as variegated quartzose sands, argillaceous sands, and clays, 5 m thick at the type section near Socastee Swamp. (Source: USGS South Carolina Geologic Map Data.) The primary soil type in this collection area is classified as Rutlege Series loamy fine sand. Rutlege Series soils are very deep, very poorly drained soils that are sandy, siliceous, thermic Typic Humaquepts. Upper strata soils (0-38 cm) are black loamy sand with weak medium granular structure. They are loose and very strongly acid. Lower strata (38-175 cm) range from dark gray to dark brown sand that is single grained, loose, and very strongly acid. (Source: NRCS Web Soil Survey.)Wild material2159139NA 88711
39NA 88712RJL2023NCSC-017Itea virginica L. South Carolina, United StatesNA2023COLLECTED11/14/2023Francis Marion National Forest: plants growing in wetlands/swamps on US Forest Service Road 223 approximately 0.57 kilometers southeast from the junction with Halfway Creek Road.33.06755600, -79.6778910011Plants are growing in the understory of the acidic swamp that is seasonally inundated in shade. Slope: N/A. Aspect: N/A. The underlying geology of this area is of Pleistocene origin and characterized as an Socastee Formation. This is a low coastal formation in the Carolinas like Penholoway but younger and lower in altitude. It is comprised primarily of unconsolidated, fine-detrital clay. It is described as variegated quartzose sands, argillaceous sands, and clays, 5 m thick at the type section near Socastee Swamp. (Source: USGS South Carolina Geologic Map Data.) The primary soil type in this collection area is classified as Rutlege Series loamy fine sand. Rutlege Series soils are very deep, very poorly drained soils that are sandy, siliceous, thermic Typic Humaquepts. Upper strata soils (0-38 cm) are black loamy sand with weak medium granular structure. They are loose and very strongly acid. Lower strata (38-175 cm) range from dark gray to dark brown sand that is single grained, loose, and very strongly acid. (Source: NRCS Web Soil Survey.)Wild material2159140NA 88712
40NA 88713RJL2023NCSC-018Ilex opaca Aiton South Carolina, United StatesNA2023COLLECTED11/14/2023Francis Marion National Forest: plants growing in wetlands/swamps on US Forest Service Road 223 approximately 0.57 kilometers southeast from the junction with Halfway Creek Road.33.06783000, -79.6774910011Plants are growing in part shade to shade of a swamp in seasonally inundated acidic wetland habitat. Slope: N/A. Aspect: N/A. The underlying geology of this area is of Pleistocene origin and characterized as an Socastee Formation. This is a low coastal formation in the Carolinas like Penholoway but younger and lower in altitude. It is comprised primarily of unconsolidated, fine-detrital clay. It is described as variegated quartzose sands, argillaceous sands, and clays, 5 m thick at the type section near Socastee Swamp. (Source: USGS South Carolina Geologic Map Data.) The primary soil type in this collection area is classified as Rutlege Series loamy fine sand. Rutlege Series soils are very deep, very poorly drained soils that are sandy, siliceous, thermic Typic Humaquepts. Upper strata soils (0-38 cm) are black loamy sand with weak medium granular structure. They are loose and very strongly acid. Lower strata (38-175 cm) range from dark gray to dark brown sand that is single grained, loose, and very strongly acid. (Source: NRCS Web Soil Survey.)Wild material2159141NA 88713
41NA 88714RJL2023NCSC-019Smilax walteri Pursh South Carolina, United StatesNA2023COLLECTED11/14/2023Francis Marion National Forest: plants growing in wetlands/swamps on US Forest Service Road 223 approximately 0.57 kilometers southeast from the junction with Halfway Creek Road.33.06757700, -79.6779280011Plants are growing in shade, part-shade and sun in the acid soils of a swamp and along the edges of the swamp where the soils are seasonally inundated. Slope: N/A. Aspect: N/A. The underlying geology of this area is of Pleistocene origin and characterized as a Socastee Formation. This is a low coastal formation in the Carolinas like Penholoway but younger and lower in altitude. It is comprised primarily of unconsolidated, fine-detrital clay. It is described as variegated quartzose sands, argillaceous sands, and clays, 5 m thick at the type section near Socastee Swamp. (Source: USGS South Carolina Geologic Map Data.) The primary soil type in this collection area is classified as Rutlege Series loamy fine sand. Rutlege Series soils are very deep, very poorly drained soils that are sandy, siliceous, thermic Typic Humaquepts. Upper strata soils (0-38 cm) are black loamy sand with weak medium granular structure. They are loose and very strongly acid. Lower strata (38-175 cm) range from dark gray to dark brown sand that is single grained, loose, and very strongly acid. (Source: NRCS Web Soil Survey.)Wild material2159142NA 88714
42NA 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
43NA 88672RJL2023PA-006Rhododendron periclymenoides (Michx.) Shinners Pennsylvania, United StatesNA2023COLLECTED10/16/2023Appalachian National Scenic Trail: Pulpit Rock and Pinnacle Loop. Rocky woodland edges above Furnace Creek around Pulpit Rock and Pinnacle Loop Trail.40.58668200, -75.94269600247Well-drained and very rocky dry deciduous woodlands in part shade to full shade. Slope: 10%. Aspect: East. 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 material2159063NA 88672
44NA 88676RJL2023PA-010Staphylea trifolia L. Pennsylvania, United StatesNA2023COLLECTED10/25/2023Seed collected along the Appalachian National Scenic Trail, accessed from the Duncannon Entrance.40.38132600, -77.02965700103Well-drained and very rocky deciduous woodlands where soil has accumulated in part shade to full shade. Slope: 0-30%. Aspect: variable. The underlying geology of this area is of Devonian origin and characterized as the Duncannon Member of Catskill Formation. It is characterized by grayish-red sandstone, siltstone, and mudstone in fining-upward cycles; conglomerate occurs at base of some cycles. The sandstones which comprise the Duncannon Member are fine to very coarse grained and grayish red to grayish red-purple in color. The Duncannon Member is known to be crossbedded to planar bedded in beds anywhere from 3 to 9 meters thick. Conglomerates have been spotted at the base of the Duncannon Member. The Duncannon Member is poorly exposed in most areas except along the Lehigh River. The conglomerate portion of this member has been known to form ridges and ledges with thicknesses approaching 228 meters. (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 material2159067NA 88676
45NA 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
46NA 88639KY23-042Lyonia ligustrina (L.) DC. Kentucky, United StatesNA2023COLLECTED09/11/2023Daniel Boone National Forest: Bee Rock Loop Trail along Rockcastle River.37.04179000, -84.31805000233Riverscour grassland. Elevation: 765 feet. Aspect: East.Wild material2158731NA 88639
47NA 88640KY23-043Ilex verticillata (L.) A. Gray Kentucky, United StatesNA2023COLLECTED09/11/2023Daniel Boone National Forest: Bee Rock Loop Trail along Rockcastle River.37.04179000, -84.31805000233Riverscour grassland. Elevation: 765 feet. Aspect: East.Wild material2158732NA 88640
48NA 88641KY23-044Physocarpus opulifolius (L.) Maxim. Kentucky, United StatesNA2023COLLECTED09/11/2023Daniel Boone National Forest: Bee Rock Loop Trail along Rockcastle River.37.04179000, -84.31805000233Riverscour grassland. Elevation: 765 feet. Aspect: East.Wild material2158733NA 88641
49Ames 36138Muscatatuck NWRPopulus heterophylla L. Indiana, United StatesNC7PLANT2023COLLECTED05/30/2023Muscatatuck National Wildlife Refuge located 4.37 miles east, southeast of Seymour, T6N R6E SW 1/4 Sec. 2438.94292000, -85.81076600159Edge of stagnant swamp along road. Soils rather mucky/heavy clay.Wild materialNative to North America, this deciduous tree has a native range that covers the Atlantic coastal plain concentrated in the Carolinas and also along the Mississippi and Ohio Rivers along with various, tiny disjunct populations widely scattered across the southeast U.S. (Little, 1971). As an obligate wetland plant, the soils that this species inhabits is typically heavy clay (ranging 24 to 65%) and slightly acidic (soil pH ranges from 4.6 to 5.9) (Johnson 1990). Typical habitat is bottomlands/floodplains that generally have standing, shallow water. Sites that are often too wet for P. deltoides are suitable for P. heterophylla. Swamp Cottonwood can reach 10-20 meters in height and generally has an upright, rounded form. Broadly ovate leaves are rather large reaching up to 25 cm in length and nearly 15 cm wide with abaxial surfaces usually pubescent to partially glabrate. As with many other species in Salicaceae, P. heterophylla is dioecious with staminate and pistillate catkins appearing in early spring and reaching up to 10 and 15 cm in length, respectively. Seeds are dispersed in spring through early summer. Swamp Cottonwood is distinguishable from other Populus largely due to the distinctly cordate leaf bases and distinctive orange-brown pith in young twigs (McMaster 2003). Ornamental characteristics include golden yellow fall color. This taxon is essentially non-existent in the nursery trade and extremely rare in botanical garden and arboretum collections. Due to this species ability to grow in anaerobic, soils heavy in clay, this species may perform well in the typical urban landscape. Its potential to withstand extreme, drought despite being an obligate wetland plant may be similar to that found in Taxodium distichum. Genetics of this accession were collected in southern Indiana. Specimens sampled in nature were approximately 40-50' in height and were clonally (vegetative) spreading by rhizomes. 2158343Ames 36138
50W6 61417CBG- 10852Verbesina alternifolia (L.) Britton ex Kearney Illinois, United StatesW6SEED2023Wild material2142299W6 61417
51W6 61418CBG- 10853Agastache scrophulariifolia (Willd.) Kuntze Illinois, United StatesW6SEED2023Wild material2142300W6 61418
52Ames 36018AS/SL/2023/003/213Salix lucida Muhl. Wisconsin, United StatesNC7LEAF2023COLLECTED02/25/2023Located just west of Kempster approximately 4.65 miles along County Road J (floodplains of Sucker Creek and West Branch Eau Claire River), T33N R10E Sec. 32, 33, and 34 (extreme southern edges)45.29205000, -89.27304100479WetlandWild materialSalix lucida (shining willow) is referenced as a tall shrub or small tree with multiple trunks with the potential to reach 6 meters in height. Shining willow frequents wetland habitats such as swampy lakes, wet meadows and along rivers. Noted for it's extremely shiny, long (e.g. 7-14 cm) leaves with very elongated, acumiate leaf tips and conspicuous, enlarged glands clustered at the end of the petiole. First year branches are very glabrous and bright yellow to bright orange in color. Flowering tends to occur later in spring in comparison to other shrubby willows e.g. Salix discolor, Salix humilis, Salix petiolaris, and Salix eriocephala. Shining willow can often be confused with Salix serissima, but the presence of glands at the base of the petiole, the colorful first year stems (most noticeable in winter) of Salix lucida can be used to separate them. The native distribution of Salix lucida is concentrated in the northeastern U.S. with scattered disjuncts as far west as North Dakota and as far south as the northern tier of counties in Illinois, Indiana, and Ohio (Little, E. L. Jr. 1977). This accession represents genetics from northeastern Wisconsin. Specimens sampled in nature measuring approximately 6' in height with bright orange-yellowish stem colors on most recent year's growth.2141551Ames 36018
53Ames 36019AS/SD/2023/004/214Salix discolor Muhl. Wisconsin, United StatesNC7PLANT2023COLLECTED02/25/2023Located along County Road J west of Kempster and County Road T/County Road H west of Summit Lake.45.29210300, -89.27334900478WetlandWild 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 central Wisconsin. Plants in nature measuring approximately 8-10' in height occassionally up to 25' with brown to red-brown stem colors on most recent year's growth. Some genotypes with dense pubescence on stems while others are glabrous.2141552Ames 36019
54Ames 36021AS/SP/2023/006/216Salix petiolaris Sm. Wisconsin, United StatesNC7PLANT2023COLLECTED02/25/2023Located just west of Kempster approximately 5.25 miles along County Road J (floodplain between Sucker Creek and West Branch Eau Claire River), T33N R10E Sec. 32 and 33 (extreme southern edges).45.29239600, -89.27583700478WetlandWild materialSlender-leaved willow, Salix petiolaris, is a somewhat dense suckering shrub that can reach up to 10' in height with slender stems that branch minimally, but typically maintains a height of 5-8'. Native to North America, the native range covers mostly the northeastern US stretching from Maine to western North Dakota and Canada south to central Iowa (Little, E. L. Jr. 1977). Salix petiolaris typically dominates wetland areas including sedge meadows, marshes, riverbanks, and lake shores. Despite favoring wet habitats, it can also be found in dry, upland areas, especially those with high-water tables. However, longevity is generally limited in upland habitats. S. petiolaris, similar to other willow species, responds well to fire, coppicing, or heavy browsing (highly favored by deer) by sprouting new stems close to the crown. In cultivation, plants after five years will encompass a 5' x 5' area due to stems that arch from the main base of the plant. Coppicing of plants to ground level is highly recommended either annually or once every 3-5 years to maintain vigorous growth and plant health. This species requires substantial to full sun exposure and is an excellent choice for streambank stabilizations and windbreaks to reduce soil erosion and drifting snow, respectively. This accession represents genetics from central Wisconsin. Plants noted in nature measuring up to 6' in height. Very densely suckering clumps occassionally reaching up to 10' in diameter. Stem colors on most recent year's growth varied from orange-yellow, red (predominate), to yellow. Petioles are minutely hairy.2141554Ames 36021
55Ames 36024AS/FN/2023/011/221Fraxinus nigra Marshall Wisconsin, United StatesNC7PLANT2023COLLECTED02/26/2023Located just north of Leland approximately 0.70 miles along Hemlock Road, T10N R5E SW 1/4 NW 1/4 Sec. 1843.34472800, -89.95099700242FloodplainWild materialSingle mother tree sample with signs of wood pecker damage on trunk.2141557Ames 36024
56NA 88552RJLSEUS2022-025Hydrangea quercifolia W. Bartram Alabama, United StatesNA2023COLLECTED12/12/2022Claiborne Bluffs area along unnamed road to boat ramp on the east side of the Alabama River at the U.S. Highway 84 bridge over the river. Common at this location and along the nearby Alabama River.31.54879700, -87.5141640040Plants are growing in part-shade to shade of mesic, well-drained, circum-neutral slopes and benches in mature mixed deciduous and evergreen woodlands with good litter layer. Soils: The underlying geology of this area is the Jackson Group Undifferentiated. The units of the Jackson Group are the Yazoo Clay and Crystal River and Moodys Branch Formations. Descriptions of the members of the Yazoo Clay follow in descending order. Shubuta Member - in western Alabama consists of light-greenish-gray to white plastic fossiliferous, calcareous clay containing irregular calcareous nodules. From the Tombigbee River eastward, the Shubuta becomes more calcareous and grades into massive clayey glauconitic limestone. Eastward from the Alabama River, equivalent beds grade into the Crystal River Formation. Pachuta Marl Member - light-greenish-grey glauconitic, fossiliferous clayey sand and sandy limestone traceable from western Alabama eastward to Covington County where it grades into the Crystal River Formation. Cocoa Sand Member - yellowish-gray firm calcareous, fossiliferous fine to medium sand or sandy limestone or greenish-grey micaceous, calcareous, very clayey sand. Calcareous and clayey sand equivalent to the Cocoa is traceable from western Alabama to the Conecuh River area. (Source: USGS Alabama Geological Map Data). The surface soil profile of this portion of the bluffs along the Alabama River are characterized as Saffell-Lucy (Flomaton) Series Complex soils. The Saffell Series consists of very deep, well drained, moderately permeable soils that formed in loamy and gravelly marine sediments of the Tertiary Age and have acid reaction. These soils are found on the upper portion of the bluffs along the Alabama River. The Lucy Series consists of very deep, well drained, moderately permeable soils on uplands. They formed in sandy and loamy marine and fluvial sediments of the Southern Coastal Plain Major Land Resource Area. Soil reaction runs from strongly to moderately acid. The Flomaton Series consists of very deep, excessively drained, rapidly permeable soils on uplands of the Southern Coastal Plain Major Land Resource Area. They formed in gravelly sandy marine sediments and also have an acid reaction. The remainder of soils are of miscellaneous origin. (Source: USDA-NRCS Official Soil Series Descriptions).Wild material2140779NA 88552
57NA 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
58NA 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
59NA 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
60NA 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
61NA 88506RJL2022TX-001Itea virginica L. Texas, United StatesNA2022COLLECTED10/31/2022Plants growing at Shangri La Botanical Gardens and Nature Center, Orange, TX along Adams Bayou, accessed via internal service roads. Plant is infrequent at this site.30.10322000, -93.762717001Plants are growing in shade to part-shade of a Taxodium distichum-Nyssa aquatica dominated forested swampland associated with Adams Bayou in a wet low-lying area that is frequently inundated.
Soils: The underlying geology of this area is of Quaternary to Late Pleistocene origin and comprised of the Beaumont Formation. This formation is yellowish- to brownish-gray, locally reddish orange with very fine to fine quartz sand, silt, and minor fine gravel, intermixed and interbedded. It also includes stream channel, point-bar, cravasse-splay, and natural levee ridge deposits, and clayey fill in abandoned channels. Channel fill is dark brown to brownish-gray with laminated clay and silt that is organic-rich. Includes marine delta-front sand, lagoonal clay, and near-shore marine sand beneath and landward of bays along the coast. Depth of this unconsolidated outwash ranges from 3-100 meters thick.
Source: USGS Texas Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=TXQbs%3B0)
The primary soil types in the collection area are classified as Cowmarsh series. The Cowmarsh series consists of very deep, very poorly drained soils that formed in mucky silty clayey alluvial deposits of Holocene age. These depressional soils are oxbows and relict channels of rivers where flooding and ponding is frequent. Slope ranges from 0 to 1 percent but mainly less than 1 percent. very poorly drained. Runoff is negligible. Frequently flooded for very long periods from February through May and surface remains saturated for very long periods once flood waters have receded.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2139813NA 88506
62NA 88507RJL2022TX-002Fraxinus caroliniana Mill. Texas, United StatesNA2022COLLECTED10/31/2022Plants growing at Shangri La Botanical Gardens and Nature Center, Orange, TX along Adams Bayou, accessed via internal service roads. Plant is relatively common along Adams Bayou but scattered.30.09989400, -93.752397001Plants are growing in part-shade to sun of a Taxodium distichum-Nyssa aquatica dominated forested swampland associated with Adams Bayou in a wet low-lying area that is frequently inundated. While found as an occasional understory element, it is more common on the edge of the swampland forest where there are high light conditions.
Soils: The underlying geology of this area is of Quaternary to Late Pleistocene origin and comprised of the Beaumont Formation. This formation is yellowish- to brownish-gray, locally reddish orange with very fine to fine quartz sand, silt, and minor fine gravel, intermixed and interbedded. It also includes stream channel, point-bar, cravasse-splay, and natural levee ridge deposits, and clayey fill in abandoned channels. Channel fill is dark brown to brownish-gray with laminated clay and silt that is organic-rich. Includes marine delta-front sand, lagoonal clay, and near-shore marine sand beneath and landward of bays along the coast. Depth of this unconsolidated outwash ranges from 3-100 meters thick.
Source: USGS Texas Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=TXQbs%3B0)
The primary soil types in the collection area are classified as Cowmarsh series. The Cowmarsh series consists of very deep, very poorly drained soils that formed in mucky silty clayey alluvial deposits of Holocene age. These depressional soils are oxbows and relict channels of rivers where flooding and ponding is frequent. Slope ranges from 0 to 1 percent but mainly less than 1 percent. very poorly drained. Runoff is negligible. Frequently flooded for very long periods from February through May and surface remains saturated for very long periods once flood waters have receded.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2139814NA 88507
63NA 88508RJL2022TX-003Morella cerifera (L.) Small Texas, United StatesNA2022COLLECTED10/31/2022Plants growing at Shangri La Botanical Gardens and Nature Center Orange, TX along Adams Bayou, accessed via internal service roads. Plant is relatively common along Adams Bayou but scattered in the understory. 30.10035500, -93.752887001Plants are growing in part-shade to shade of a Taxodium distichum-Nyssa aquatica dominated forested swampland associated with Adams Bayou in a wet low-lying area that is frequently inundated.
Soils: The underlying geology of this area is of Quaternary to Late Pleistocene origin and comprised of the Beaumont Formation. This formation is yellowish- to brownish-gray, locally reddish orange with very fine to fine quartz sand, silt, and minor fine gravel, intermixed and interbedded. It also includes stream channel, point-bar, cravasse-splay, and natural levee ridge deposits, and clayey fill in abandoned channels. Channel fill is dark brown to brownish-gray with laminated clay and silt that is organic-rich. Includes marine delta-front sand, lagoonal clay, and near-shore marine sand beneath and landward of bays along the coast. Depth of this unconsolidated outwash ranges from 3-100 meters thick.
Source: USGS Texas Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=TXQbs%3B0)
The primary soil types in the collection area are classified as Cowmarsh series. The Cowmarsh series consists of very deep, very poorly drained soils that formed in mucky silty clayey alluvial deposits of Holocene age. These depressional soils are oxbows and relict channels of rivers where flooding and ponding is frequent. Slope ranges from 0 to 1 percent but mainly less than 1 percent. very poorly drained. Runoff is negligible. Frequently flooded for very long periods from February through May and surface remains saturated for very long periods once flood waters have receded.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2139815NA 88508
64NA 88514RJL2022MD-019Kalmia latifolia L. Maryland, United StatesNA2022COLLECTED11/04/2022Plants are growing on both sides of a fire road on Maryland Heights along the edge with Harpers Ferry National Historic Park. This location was accessed from the east where Miller Avenue meets the fire road, approximately 2 kilometers away. There is no vehicular access to the collecting area. Becoming locally uncommon. This local population is likely to be extirpated in the next 20-30 years. This collector has hiked through this area for more than 35 years and seen dramatic changes in the population. When first observed, Kalmia latifolia was a dominant understory shrub on south- to west-facing slopes beneath a mature forest canopy. Over the years, at least one forest fire has significantly reduced the population, along with a continuing increase in deer populations, resulting in catastrophic browse damage. The absence of a mature forest canopy and periods of drought have almost certainly also resulted in decline of this population. While collecting seed from scattered mature plants well above deer browse levels, this collector also noted that there was virtually no recruitment taking place.39.32811200, -77.72242400287Plants are growing in part-shade to shade of a deciduous upland, very rocky, and dry forest community. Plants are frequently found growing among boulders, rock outcrops, and steep-slope erosional areas, although, not exclusively.
Soils: The underlying geology of this area is of Late Cambrian to Cambrian origin and comprised of Chilhowee Group; Weverton Formation. This includes interbedded white to dark gray, thin-bedded, micaceous, ferruginous, and sericitic quartzites, phyllites, and white, thick-bedded, ledge-making quartzites; some gray to brown ferruginous quartz conglomerate and purple-banded phyllite.
Source: USGS Maryland Geologic Map Data https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=MDKp%3B5
The primary soil types in the collection area are classified as Dekalb-Bagtown-Rock outcrop complex, 25 to 65 percent slopes. The Dekalb series consists of moderately deep, excessively drained soils formed in material weathered from gray and brown acid sandstone in places interbedded with shale and graywacke. Slope ranges from 0 to 80 percent. Permeability is rapid. Solum thickness and depth to bedrock range from 50 to 100 cm. Flat, subangular or angular, sandstone fragments, 2.5-25 cm across increase with depth and range from 10-60 percent in individual horizons of the solum and from 50-90 percent or more in the C horizon. The amount of rock fragments typically increases with depth. Cobbly, channery, and very stony phases are common. Reaction ranges from extremely through strongly acid.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2139821NA 88514
65Ames 35924AS/FN/2022/073/204Fraxinus nigra Marshall Wisconsin, United StatesNC7SEED2022COLLECTED09/29/2022Chequamegon National Forest, approximately 4.5 miles south-southeast of Clam Lake along County Highway GG and adjacent Forest Service roads, T42N R4W Sec. 21.46.10020200, -90.87459600431Wet to saturated soils in northern hardwood forest.Wild material2139687Ames 35924
66Ames 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
67WLP 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
68WLP 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
69Ames 35792APS/ID/2022/027/489Ilex decidua Walter Arkansas, United StatesNC7FRUIT2022COLLECTED03/15/2022Located approximately 3.75 miles east of Allison just off Round Bottom Road.35.93670000, -92.04891000133Dry west facing slope in a pine, oak, and hickory forest.Wild materialPlants sampled in nature with bright red fruits measuring 7-9 mm in diameter.2137431Ames 35792
70NA 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
71WLP 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
72WLP 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
73WLP 1747RJL2021PA-005Rosa palustris Marshall Pennsylvania, United StatesNA2021COLLECTED11/20/2021Plants growing in wetland seeps surrounded by mown hayfields just west of the Middle Branch White Clay Creek in Goddard Park, West Grove Pennsylvania, off of Wickerton Road, Chester County.39.80090528, -75.82383250100Habitat Notes: Plants are growing in permanently saturated to moist soils in wetland habitats. Plants appear to be obligate wetland plants and are found only in permanent to nearly permanent wet habitats observed. Generally, the shrubs are found in part shade to full sun. Soils: Soils found in the areas where this collection was made are comprised primarily of Hatboro silt loam (Ha). 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. Slope: 0 to 3% Aspect: Variable.Wild material2123715WLP 1747
74OPGC 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
75OPGC 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
76Ames 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
77Ames 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
78Ames 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
79Ames 35615Ames 35615Aronia arbutifolia (L.) Pers. Michigan, United StatesNC7SEED2020COLLECTED11/03/2020Warren Townsend Park located just northeast of Cannonsburg southwest of Ramsdell Dr. and Six Mile Rd. intersection, T8N R10W NE ¼ NW ¼ Sec. 26, Cannon Twp., Kent County43.05606700, -85.46435100239Shrubby edge of old stream (Bear Creek) oxbow, adjacent to wet meadow with groundwater upwelling. Muck soils.Wild materialPlants in nature measuring approximately six meters in height; elongate shrubs mostly unbranched; bright-red fruits measuring between 4-7 mm in diameter; tomentose leaves underneath; scarlet fall color. This collection was discovered in 2011 and represents the first report of the species for the state of Michigan (Ryskamp and Warners 2012) and thus represents a widely disjunct population where the next nearest documented population is in southern Ohio (Clermont County). 2110277Ames 35615
80OPGC 8059ID310-42Asclepias speciosa Torr. Idaho, United StatesOPGC2020Wild materialPetiolate leaves, oblong-lanceolate leaves.2107488OPGC 8059
81NA 88438MARSB-202Rosa palustris Marshall Delaware, United StatesNA2020Wild materialWoody plant with stems covered in recurved thorns. Mature fruit a scarlet hip.2106461NA 88438
82NA 86434Pulverulentus GroupStyrax americanus Lam. Texas, United StatesNA2020COLLECTED09/08/2018Near Gum Slough, on the edges of woodlands along the north side of road FM 2246.30.33332000, -93.9470400015Plants are found along the edges and moist to wet areas of Gum Slough in part shade to full sun of a mixed deciduous and broadleaved evergreen woodlands. Soils are generally acidic with loamy to clayey sediments, but with some areas consisting of deep, nearly level loamy, poorly drained soil.Wild materialSpecies occurrence is infrequent at this location. Collector's note on the name under which this material was gathered, Styrax americanus var. pulverulentus: "In general, the var. pulverulentus is considered "taxonomically inconsequential" by many botanists. Even so, this densely pubescent characteristic is highly uniform across every plant I observed in the sampled population. Weakley notes that "true" var. pulverulentus can be found as far west as East Texas and, in my humble opinion, the population sampled herein represents this "taxon". Regardless, for the purposes of drawing distinction between "typical" Styrax americanus and the densely pubescent form, I've chosen to use this varietal name. It will be interesting to observe whether the seedling progeny are uniformly similar to their parents when they germinate." [Actual altitude recorded was 14.8 m, but decimals can't be used in the database, so the number was rounded.]2109219NA 86434
83Ames 35288APS/MF/2020/003/406Monarda fistulosa L. Kansas, United StatesNC7HABITAT2020COLLECTED02/05/2020Eisenhower State Park on north side of Melvern Lake approximately 5.25 miles west, northwest of Melvern, T18S R15E NE1/4 Sec. 3, Osage County38.51966000, -95.73352000323Edge of woods with limestone substrate.Wild material2101394Ames 35288
84WLP 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
85WLP 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
86Ames 35236SF_ID:24690/EO-ID:17843Agastache foeniculum (Pursh) Kuntze Nebraska, United StatesNC7FLOWER2019Wild materialPlants measuring approximately 60 cm in height. Infructescences fully mature at time of collection (23 October 2019), likely past peak maturity by approximately 4 weeks. Population (EC-ID: 17843) was originally documented by Steven B. Rolfsmeier on 8 June 2015 (Nebraska Pine Ridge Plant Resurvey, 2015: Report submitted to the Nebraska Natural Heritage Program) noting “ Agastache foeniculum was located in a ravine bottom that burned in 2012. Estimated population size: 200-300 stems covering approximately 125 sq. meters”. A. foeniculum in Nebraska is currently tracked by the Nebraska Natural Heritage Program and is listed (6 November 2019) as a S1 (Critically Imperiled - at very high risk of extirpation in the state due to very restricted range, few populations or occurrences, steep declines, severe threats or other factors) and Tier 2 species (Tier 2 - species are typically those that are not at-risk from a global or national perspective but are rare or imperiled within Nebraska). 2097772Ames 35236
87WLP 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
88WLP 171NACPEC19-063Itea virginica L. Georgia, United StatesNA2019COLLECTED09/15/2019Walker County; Lula Lake Land Trust: Lula Lake Land Trust Falls: West Side of Falls34.93319200, -85.37178900477Stream bank, mesic wood forestWild material2110485WLP 171
89WLP 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
90WLP 2014MARSB-985Viburnum dentatum L. New York, United StatesNA2019COLLECTED08/20/2019Oswego County; Williamstown; Private recreational land at 319 Stone Hill Rd.43.41583000, -75.96805000186Edge of open pond with edge trail lined with shrubs and trees, dam; growing in full sun in wet sand loam soil.Seeds collected directly from plants. Species scattered in area; 30 individuals in population, 500 seeds collected [presumably all individuals sampled]. Seed quality good, 95 percent healthy seed. Beaver activity in pond.2109110WLP 2014
91NA 88454OR050-274Rosa woodsii Lindl. var. ultramontana (S. Watson) Jeps. Oregon, United StatesNASEED2018Wild materialRosa woodsii var. ultramontana1967943NA 88454
92NA 88031NCBG-382Juniperus virginiana L. Virginia, United StatesNASEED2018Wild material1965940NA 88031
93NA 85007JDC/QB/2008/079/149 [related collection number]Quercus bicolor Willd. Iowa, United StatesNA2018COLLECTED09/24/2015Chichaqua Wildlife Habitat Park bottoms, near Elkhart, NW 1/4 of NW 1/4 of Section 32, T81N, R22W, Loring Quad.41.79000000, -93.43972222247Wild materialSeedlings from seed collected at the same site as NA 81010, which was received in 2012 under collection number JDC/QB/2008/079/149, and also as Ames 29670. GRIN narrative: "A small proportion of seedlings during growout were noted to be Q. bicolor x Q. macrocarpa hybrids." Digital photographs of source trees available in GRIN under NA 85010/Ames 29670.2141805NA 85007
94NA 85022JDC/SS/2018/008/821Sapindus saponaria L. var. drummondii (Hook. & Arn.) L. D. Benson Oklahoma, United StatesNAImage2018COLLECTED03/13/2018Thurmond Ranch approximately 3.80 miles southwest of Cheyenne, T13N R24W, Roger Mills County35.59226100, -99.69600600554Bottomlands and immediate higher elevations of Sergeant Major Creek and surrounding tributaries.Wild material1957959NA 85022
95OPGC 6411CBG-8084Solidago patula Muhl. ex Willd. Illinois, United StatesOPGCSEED2017Wild material1954874OPGC 6411
96Ames 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
97Ames 33985JDC/FQ/2017/041/795Fraxinus quadrangulata Michx. Kentucky, United StatesNC7SEED2017COLLECTED07/12/2017Carter Caves State Resort Park near Smoky Valley Lake just 4.46 miles south of Carter, Carter County38.36772700, -83.12512200230Deciduous woods.Wild material1950068Ames 33985
98NA 83897PCCKY16-024Xanthorhiza simplicissima Marshall Kentucky, United StatesNA2016COLLECTED09/27/2016Cumberland Falls State Park, Cumberland Falls Visitor Center. Beach north of visitor center outlook trail, boulders north of large sycamore with exposed root flare and hole in trunk base.36.84200000, -84.34200000252Beach, with boulders.Wild material1952452NA 83897
99WLP 1209NA 83966Hibiscus moscheutos L. Kentucky, United StatesNA2016COLLECTED09/30/2016[Locality data unparseable; GPS coordinates appear near a road of uncertain name off Howard Munsey Rd. north of Betsey, Kentucky. Original location was listed as: "At Edam Road?"; no road by this name was found in the county. -SBL]36.91900000, -84.73800000277Wet roadside couvee (ditch).1950957WLP 1209
100WLP 704NA 83896Amorpha fruticosa L. Kentucky, United StatesNA2016COLLECTED09/27/2016Cumberland Falls State Park, Cumberland Falls Visitor Center. Beach north of visitor center outlook trail, boulders north of large sycamore with exposed root flare and hole in trunk base.36.84200000, -84.34200000245Beach, with boulders.1950955WLP 704
101Ames 33752Ames 33752Maclura pomifera (Raf.) C. K. Schneid. Iowa, United StatesNC7SEED2016COLLECTED10/05/2016Deer Creek watershed, T80N R23W E1/2 Sec. 18.41.73813000, -93.56296400295Mixed deciduous woods, distrubed areas and also managed areas. Gentle slopes and wetlandsUncertain improvement statusThe native range for Osage-orange is reported from eastern Texas, southeastern Oklahoma, southwestern Arkansas, and the northwestern corner of Louisiana (Little, 1971). Historically and presently known for its extreme value as bow-wood and fence posts, Osage-orange represents one of the most widely planted tree species in the lower 48 US states as a living fence starting in the mid-1800's, in the late 1900's as a landscape tree for difficult sites, and most recently its chemical properties. Detailed history of Osage-orange and it's economic uses are well documented (Smith and Perino, 1981 and J. T. Winberry 1979). Osage wood is highly-prized for its use as fence posts (both living and non-living) and durable wood for wood working. Osage is an extremely drought and heat tolerant tree and is recommended for use in USDA cold-hardiness zones 5b or warmer. Although the species is commonly known for its stout thorns and large, globular fruits, the species is dioecious and the degree of thorns on individual genotypes can be extremely variable. This accession represents germplasm from a naturalizing, reproductive population collected in central Iowa (Polk County). Majority of specimens averaged approximately 40-50’ in height with multiple (e.g. 4-5) trunks. Specimens 03-1 and 03-2 were upright in form with tighter branch angles, while 03-10 was the widest spreading of all trees. Some yellow fall color (yellow) was apparent at time of fruit collection (10/05/2016). Size of fruits ranged from 9.00 to 10.75 inches circumference except for tree 03-5 with fruits averaging 7.33 inches circumference. 1942949Ames 33752
102OPGC 7157CBG-5314Geum aleppicum Jacq. Wisconsin, United StatesOPGC2016Wild material1942769OPGC 7157
103W6 51634CBG-5267Chamaenerion angustifolium (L.) Scop. subsp. circumvagum (Mosquin) Moldenke Wisconsin, United StatesW62016Wild material1942764W6 51634
104Ames 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
105WLP 1101JDC/CO/2015/036/692Cotinus obovatus Raf. Oklahoma, United StatesNAPLANT2015COLLECTED05/21/2015T16N R20E W 1/2 Sec. 18 Wagoner and Cherokee Counties. Fort Gibson Lake Dam.35.86228100, -95.22575600170Growing on shallow, rocky soils in association with Carya illinoinensis, Quercus muehlenbergii, Cornus sp., Cercis canadensis, Fraxinus americana, Platanus occidentalis, Ulmus sp., Diospyros virginiana, Sapindus saponaria var. drummondii, Lonicera sempervirens, Smilax sp., Toxicodendron radicans, and Robinia pseudoacacia.Wild material1926263WLP 1101
106Ames 32891APS/GD/2015/010/192Gymnocladus dioicus (L.) K. Koch Oklahoma, United StatesNC7Fruit2015COLLECTED03/12/2015Nowata County: T25N R16E NW 1/4 NE 1/4 Sec. 3. Oologah Wildlife Management Area approximately 3 miles east of Nowata.36.68401000, -95.58207800208Transition zone between higher elevations and bottomlands. Wild material1925357Ames 32891
107Ames 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
108NA 83061ZARKS-005Gymnocladus dioicus (L.) K. Koch Arkansas, United StatesNA2015COLLECTED10/02/2014Frog Valley (private property). West bank of North Fork of Saline River.34.76276000, -92.71386000133Alluvial low floodplain, in sandy clay soil. Slope: 0 degrees. Elevation: 435 feet.Wild material1950627NA 83061
109NA 83062NA 83062Taxodium distichum (L.) Rich. Arkansas, United StatesNA2015COLLECTED10/02/2014Frog Valley (private property). Banks of North Fork of Saline River.34.76443000, -92.71338000135Alluvial low floodplain, in gravel bank.1951432NA 83062
110NA 83063NA 83063Hamamelis vernalis Sarg. Arkansas, United StatesNA2015COLLECTED10/02/2014Frog Valley (private property). Gravel bar along North Fork of Saline River.34.76543000, -92.71353000134Alluvial low floodplain; gravel bar.1950887NA 83063
111Ames 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
112Ames 32812Ames 32812Euonymus atropurpureus Jacq. Iowa, United StatesNC7PLANT2014COLLECTED10/22/2014Chichaqua Bottoms Greenbelt, Polk County.41.77483000, -93.43145600250Bottomland/floodplain forest of Skunk River watershed.Wild materialOne specimen sampled in nature was approximately 20 feet in height. In cultivation at NCRPIS, plants display attractive fall foliage colors ranging from pale pink to deep red. Fruits are ornamentally significant, varying in color from pale to bright pink.1921817Ames 32812
113WLP 218JDC/TC/2014/089/591ATsuga canadensis (L.) Carrière Alabama, United StatesNA2014COLLECTED09/23/2014Alabama: Franklin County; William B. Bankhead National Forest, north-facing banks of Bear Creek watershed.34.33924600, -87.54771500285 Growing in association with Quercus alba, Cornus florida, Pueraria montana var. lobata, Magnolia macrophylla, Platanus occidentalis, Liquidambar styraciflua, and Fagus grandifolia. Wild materialExcellent cone production. Optimum timing for harvest. Species infrequent to locally abundant across a 12 mile linear stretch of the southeast corner of Franklin County to north-central Winston County.1922361WLP 218
114Ames 32388JDC/BN/2014/015/517Betula nigra L. Iowa, United StatesNC7SEED2014COLLECTED06/05/2014Princeton Wildlife Management Area, T80N R5E NE 1/4 Sec. 35.41.69417800, -90.34158400177Wet, heavy soil floodplain.Wild material1919309Ames 32388
115Ames 32226APS/GD/2014/010/141Gymnocladus dioicus (L.) K. Koch Indiana, United StatesNC72014COLLECTED03/22/2014Cabin Creek watershed, Sections 6 and 36, T20N, R13E, and Sections 22 and 23, T20N, R12E, just southwest of Farmland, Randolph County.40.15779200, -85.14474100304Moist woods.Wild material1917830Ames 32226
116Ames 32082JDC/FQ/2013/041/485Fraxinus quadrangulata Michx. Ohio, United StatesNC7SEED2013COLLECTED08/17/2013South Bass Island, Put-In-Bay Quad, Ottawa County.41.63639900, -82.83680200197Shallow, rocky soils. Wild material1913268Ames 32082
117Ames 32069APS/PO/2013/034/119Physocarpus opulifolius (L.) Maxim. Wisconsin, United StatesNC72013COLLECTED06/17/2013Cana Island, Door County.45.08814100, -87.04772000Wild material1912291Ames 32069
118Ames 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
119Ames 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
120Ames 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
121Ames 31677GA12001001Fraxinus pennsylvanica Marshall Minnesota, United StatesNC7SEED2012COLLECTED09/24/2012Southwest Becker County near Lake Cormorant and Lake Maud..46.73903330, -95.97883330415Edge of slough and forest. Wild material1906588Ames 31677
122Ames 31532JDC/FQ/2012/042/435Fraxinus quadrangulata Michx. Illinois, United StatesNC7SEED2012COLLECTED07/26/2012Trout Park Nature Preserve, Section 1, T41N, R83, Elgin Quad, near Elgin, Kane County.42.06258500, -88.27131500240Variable habitats: dry, rocky slopes and also near small creek in gravelly soils. Wild material1903759Ames 31532
123Ames 31086691Fraxinus pennsylvanica Marshall New York, United StatesNC7SEED2011COLLECTED09/10/2011Winters Road, south of Main Street, Chemung County.42.13200000, -76.92800000275Floodplain of Cuthrie RunWild material1891472Ames 31086
124Ames 30603JDC/FP/2010/055/325Fraxinus pennsylvanica Marshall Kansas, United StatesNC7SEED2010COLLECTED09/19/2010Along highway 160, Mouse Creek watershed, just east of Independence, Montgomery County.37.22496000, -95.66045000233Shallow soils in bedrock with seeps. Wild material1848898Ames 30603
125WLP 1949JDC/VM/2010/022/292Viburnum molle Michx. Illinois, United StatesNASEED2010COLLECTED09/06/2010Along Senachwine Creek, SE 1/4 of Section 12, Rome Quad, Peoria County.40.94680000, -89.52970000183Along steep (75%) west-northwest facing slope. Associated with Cornus, Fraxinus, Ostrya virginiana, Platanus occidentalis, Quercus rubra, Staphylea trifolia, Tilia americana, and Vitis riparia.Wild materialPlants up to 15 feet in height. Reddish fall color on apical stems. Peeling bark on older stems.1847248WLP 1949
126Ames 30491APS/GD/2010/013/048Gymnocladus dioicus (L.) K. Koch Illinois, United StatesNC7FRUIT2010COLLECTED02/23/2010Near Deans Hills State Nature Preserve, approximately 7 miles east of Ramsey, T8N R2E Sec. 10 and NE 1/4 of Sec. 16, Fayette County.39.13970000, -88.97490000172Gentle rolling hills of deciduous woods.Wild material#157 measured 9.5" and 50', #158 measured 11.5" d.b.h. and 50', #159 measured 16" and 60', #160 measured 15" and 80', and #161 measured 16.5" and 90'.1831350Ames 30491
127Ames 30381JDC/MF/2009/093/243Monarda fistulosa L. Ohio, United StatesNC7Flower2009COLLECTED10/16/2009Wayne National Forest, near Dirtyface Creek, SE 1/4 of SW 1/4 of Section 21, T6N, R17W, Gallia Quad, Jackson County.38.80750000, -82.53000000210Open prairie. Variable soil types present.Wild materialDuring an observation trial of 19 Monarda accessions at NCRPIS, this accession was found to be unique in having an extremely high number of inflorescences on each flowering stem.1823933Ames 30381
128WLP 1951JDC/VR/2009/110/260Viburnum rufidulum Raf. Ohio, United StatesNA2009COLLECTED10/18/2009Along Ohio County Highway 106 (Suck Run Road), just south of Neel, Decatur Quad, Brown County.39.00000000, -84.0000000022445% slope, southeast and east facing. Associated with Acer saccharum, Celtis occidentalis, Cercis canadensis, Cornus florida, Fraxinus quadrangulata, Quercus, Staphylea trifolia, Viburnum molle, and V. prunifolium.Wild material1823957WLP 1951
129WLP 814JDC/CC/2009/086/236Carpinus caroliniana Walter Ohio, United StatesNA2009COLLECTED10/15/2009Along Clear Creek, near Revenge, SE 1/4 of SE 1/4 of Section 13, T13N, R19W, Rockbridge Quad, Hocking County.39.59361111, -82.61944444246Creekbed. Associated with Acer rubra, Asimina triloba, Carya, Cephalanthus occidentalis, Cornus florida, Hamamelis virginiana, Nyssa sylvatica, Oxydendrum arboreum, and Quercus.Wild material1823913WLP 814
130Ames 30147JDC/FP/2009/042/192Fraxinus pennsylvanica Marshall Wisconsin, United StatesNC7SEED2009COLLECTED09/22/2009Along Levee Road, Pine Island State Wildlife Area, SW 1/4 of NW 1/4 of Section 11, T12N, R8E, Pine Island Quad, Columbia County.43.53250000, -89.51555556242Wisconsin River watershed/floodplain. Wild material1819728Ames 30147
131Ames 30153JDC/FP/2009/062/212Fraxinus pennsylvanica Marshall Illinois, United StatesNC7SEED2009COLLECTED09/25/2009Four Corners Road, north from Illinois Highway 84, NW 1/4 of SW 1/4 of Section 36, T26N, R2E, Blackhawk (IL-IA) Quad, Jo Daviess County.42.20027778, -90.22944444194Roadside in fence row. Wild material1819734Ames 30153
132Ames 29981APS/GD/2009/019/028Gymnocladus dioicus (L.) K. Koch Iowa, United StatesNC7HABITAT2009COLLECTED04/04/2009Near the confluence of the West Fork Cedar River and Shell Rock River, approximatley 2 miles east of Finchford, T90N R14W SE 1/4 SE 1/4 SE 1/4 and also SE 1/4 SW 1/4 Sec. 4 Shell Rock Quad., Black Hawk County.42.62888889, -92.49666667272Gentle, east-facing slopes and also floodplain.Wild materialTrees ranging from 13.5 to 18 inches DBH and 50 to 70 feet in height.1799101Ames 29981
133NA 78098J. Griffin S.N.Celastrus scandens L. Kansas, United StatesNA2009COLLECTED03/26/2009Approx. 5 miles NE of Leon, KS along SE Price Rd.37.73861111, -96.715833331371Relatively natural/undisturbed, first grade above flood plain. Reasonably well protected, direct sunlight probably only a couple of hours per day.Wild material1800361NA 78098
134Ames 29974JDC/GD/2009/003/153Gymnocladus dioicus (L.) K. Koch Iowa, United StatesNC7HABITAT2009COLLECTED03/19/2009Stone State Park, just northwest of Sioux City, T89N R48W west 1/2 of Sec. 1 and east 1/2 of Sec. 2 Sioux City Quad., extreme northwest corner of Woodbury County.42.55805556, -96.46861111390Variable-wet bottomland and dry slopes; a few small creeks with running water. Variable exposure. 0-45 degrees of slope with southern and eastern aspects.Wild materialPlants between 40 and 65 feet in height and 6 to 17 inches DBH. 1798766Ames 29974
135Ames 29975JDC/GD/2009/004/154Gymnocladus dioicus (L.) K. Koch Nebraska, United StatesNC7HABITAT2009COLLECTED03/20/2009Ponca State Park, approximately 2 miles north of Ponca, T30N R6E Sec. 3 Ponca Quad., Dixon County.42.60166667, -96.71444444365Variable from mid-level elevation sloped area to bottomland type. Variable exposure. 0-60 degrees of slope with variable aspects.Wild materialPlants between 40 and 75 feet in height and 8 to 26 inches DBH.1798767Ames 29975
136NA 81010JDC/QB/2008/079/149Quercus bicolor Willd. Iowa, United StatesNALEAF2008COLLECTED10/21/2008Chichaqua Wildlife Habitat Park bottoms, near Elkhart, NW 1/4 of NW 1/4 of Section 32, T81N, R22W, Loring Quad, Polk County.41.79000000, -93.43972222247Wild materialA couple of specimens are approximately 300 years in age. Very large mature specimens, approximately 70-90 feet in height and 4-5 feet d.b.h. Largest specimen sampled was 54.5" d.b.h. A small proportion of seedlings during grow out were noted to be Q. bicolor x Q. macrocarpa hybrids.1788225NA 81010
137Ames 2733241Staphylea trifolia L. Iowa, United StatesNC7PLANT2003COLLECTED09/24/2003Stoney Hollow, halfway between Burlington and Kingston, T71N R2W NW corner of NE 1/4 of SW 1/4 of Sec. 35, Des Moines County40.90611111, -91.05972222186Along creek. Shady. Steep banks with various aspects. Rocky, just above shale layer on limestone and alluviumWild materialLarge shrubs to 4 meters tall. 1649678Ames 27332
138WLP 76719Carpinus caroliniana Walter Iowa, United StatesNA2003COLLECTED09/15/2003Bixby State Park, Edgewood, T91N R5W, SW corner of SE 1/4 of NW 1/4, Section 26, Edgewood Quad, Clayton County.42.66694444, -91.40333333329Forest edge. Half shaded. 20% slope with a western aspect. Associated with Acer nigrum, Cornus alternifolia, Quercus rubra, and Rubus occidentalis.Wild materialSmall tree. 1649453WLP 767