Search Accessions

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


Search
Search Clear All
Scientific name (any part, no hybrid symbols)

Plant name


Genebank
Country of Origin


Other search criteria:



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

Search
View Observation Data
Selected item(s) below:

ACCESSIONPLANT NAMETAXONOMYORIGINGENEBANKIMAGEAVAILABILITYRECEIVEDSOURCE TYPESOURCE DATECOLLECTION SITECOORDINATESELEVATIONHABITATIMPROVEMENT LEVELNARRATIVE
0PI 658651Ames 26838Rhus glabra L. Missouri, United StatesNC72002COLLECTED2001Shaw Nature Reserve, Gray Summit38.48972222, -90.81666667204Wild material1635682PI 658651
1PI 5185029031712Rhus glabra L. Michigan, United StatesNC71988COLLECTED12/12/1980T45N R30W, Marquette County, MLRA 9346.29005230, -88.05458820469Wild materialTillers/suckers abundant. Used for critical area stabilization on acid mine spoil in midwestern and northeastern U.S.1413438PI 518502
2PI 5185039031717Rhus glabra L. Illinois, United StatesNC71988COLLECTED09/17/1981T12S R2W Sec. 3, Calhoun County, MLRA 11539.04785350, -90.62647550243Wild materialTillers/suckers abundant. Vigor excellent. Used for critical area stabilization primarily on acid mine spoil in midwestern and northeastern U.S.1413439PI 518503
3PI 5185049031719Rhus glabra L. Indiana, United StatesNC71988COLLECTED09/22/1981R1E T10N Sec. 1, Brown County, MLRA 12039.33242680, -86.36666667274Wild materialSeed production heavy. Plants vigorous. Used for critical area stabilization primarily on acid mine spoil in midwestern and northeastern U.S.1413440PI 518504
4PI 5185069031748Rhus glabra L. Indiana, United StatesNC71988COLLECTED1981T4S R5E Sec. 34, Harrison County, MLRA 12238.12010350, -85.94921670243Wild materialGrowth uniform. Seed production heavy. Used for critical area stabilization primarily on acid mine spoil in midwestern and northeastern U.S.1413442PI 518506
5PI 5185079031759Rhus glabra L. Missouri, United StatesNC71988COLLECTED1981East side of I-29, .8km N of mile post 54, N of St. Joseph, Andrew County, MLRA 10739.86056100, -94.81421100304Wild materialTillers/suckers abundant. Plants vigorous. Used for critical area stabilization primarily on acid mine spoil in midwestern and northeastern U.S.1413443PI 518507
6PI 5185109031828Rhus glabra L. Missouri, United StatesNC71988COLLECTED1981T50N R16W Sec. 10, Howard County, MLRA 11539.15000000, -92.70000000216Wild materialPlants produce tillers/suckers. Seed production good. Used for critical area stabilization primarily on acid mine spoil in midwestern and northeastern U.S.1413446PI 518510
7Ames 35752#476-477Rhus glabra L. Iowa, United StatesNC7PLANT2021COLLECTED09/29/2021Upper Iowa River area near Bluffton, T99N R9W NE1/4 Sec. 9 and S1/2 Sec. 1043.40275000, -91.90494000299High bluffs, roadside and stream banksWild materialPlants sampled in nature (29 September 2021) during peak fall color displaying bright reds to maroonish colors while measuring approximately 12-15 feet in height. One clonal patch noted was estimated to have 1,000+ ramets. 2122093Ames 35752
8W6 57249MARSB-714Rhus glabra L. New York, United StatesW6SEED2019Wild material2097688W6 57249
9WLP 158NACPEC19-029Rhus glabra L. Kentucky, United StatesNA2019COLLECTED09/09/2019Madison County; Berea College Forest: Radio Tower Service Trail37.55289700, -84.28793400379Xeric shade knob, limestone shale conglomerate materialWild material2110470WLP 158
10W6 56179NEWFS-305Rhus glabra L. Massachusetts, United StatesW6SEED2019Wild material1976214W6 56179
11Ames 34794NCBG-739Rhus glabra L. North Carolina, United StatesNC7SEED2018COLLECTED10/07/2017Just north of Oswego.36.19391000, -78.1939100091Ruderal loblolly pine/sweetgum red maple forestWild material1966040Ames 34794
12Ames 34791CO150A-34Rhus glabra L. Colorado, United StatesNC7SEED2018COLLECTED09/10/2016Uncompahgre National Forest near East Fork Escalante Creek between MM 29 and MM 30.38.50333000, -108.460270002490Burned pinyon/juniperWild material1958166Ames 34791
13WLP 1704NA 83942Rhus glabra L. Kentucky, United StatesNA2016COLLECTED09/29/2016Kentenia State Forest, Pine Mountain, on Route 1679, south side.36.90500000, -83.29100000771Roadside.1953164WLP 1704
14Ames 32900JDC/RG/2015/017/673Rhus glabra L. Oklahoma, United StatesNC7Fruit2015COLLECTED03/17/2015Located approximately 10 miles west of Vici, T19N R21W N edge of Sec. 7, Ellis County36.14448500, -99.47983500701Roadside. Wild material1925366Ames 32900
15W6 42297NYCDPR-BBG-83Rhus glabra L. New York, United StatesW62011Wild material1889648W6 42297
16WLP 1618RL 08085Rhus glabra L. North Carolina, United StatesNA2008COLLECTEDNorth Carolina: Buncombe County, Along road leading to Elk Mountian summit ridge, east end, ca. 400 ft. from junction with Elk Mountain Scenic Hwy.1922675WLP 1618
17Ames 22092Index Seminum #88Rhus glabra L. Oklahoma, United StatesNC71994COLLECTED1993Greer County34.92309300, -99.55455000479Wild material1087573Ames 22092
18W6 52944NEWFS-127Rhus copallinum L. Connecticut, United StatesW6SEED2017Wild material1954687W6 52944
19Ames 33232Index Seminum 9Rhus typhina L. Michigan, United StatesNC72016COLLECTED10/23/2014Along Woodbury Road, Rose Lake State Wildlife Research Area, T5N R1E Sec. 20, Shiawassee County42.81640000, -84.35390000257Old flooded field.Wild material1936482Ames 33232
20Ames 32800JDC/RC/2014/085/587Rhus copallinum L. Mississippi, United StatesNC72014COLLECTED09/22/2014Near J.P. Coleman State Park, T1S, R10E NW 1/4 of NW 1/4 of NW 1/4 of Sec. 24, extreme northeast corner of Tishomingo County34.98550900, -88.20415100196Dry, pine-post oak woodsWild material1921811Ames 32800
21WLP 1619RL 08086Rhus ×pulvinata Greene North Carolina, United StatesNA2008COLLECTED09/11/2008North Carolina, Buncombe County, Along road leading to Elk Mountain summit ridge, east end, ca. 450 ft. from junction with Elk Mountain Scenic Hwy.Wild materialRhus glabra x typhina1898077WLP 1619
22Ames 29227JDC-0452007Rhus copallinum L. Missouri, United StatesNC7SEED2007COLLECTED10/04/2007Along trail to Mina Sauk Falls, Taum Sauk Mountain State Park, Iron County37.57250000, -90.72805556541Very dry, rocky soil. Very close to the highest elevation in MissouriWild materialReddish fall color.1743330Ames 29227
23WLP 1613RL 099Rhus ×pulvinata Greene North Carolina, United StatesNA2006COLLECTED07/01/2004North Carolina, Buncombe County, Elk Mountain; west of Bull Gap, and north of Vance Birthplace Road; along old road to ridgetop.Wild materialRhus glabra x typhina1898074WLP 1613
24PI 704861 sosR. pensilvanicus NCBG-442Rubus pensilvanicus Poir. North Carolina, United StatesCOR2021Wild materialhigh arching2116312PI 704861 sos
25PI 702722MARSB-400Schizachyrium scoparium (Michx.) Nash New York, United StatesS9SEED2019Wild material2097613PI 702722
26PI 710489MARSB-254Lespedeza capitata Michx. New York, United StatesS9SEED2018Wild material1964746PI 710489
27PI 710485CBG-7324Desmodium canadense (L.) DC. Wisconsin, United StatesS9SEED2017Wild material 1954800PI 710485
28PI 664805JDC/HX/2010/035/305Helianthus mollis Lam. Kansas, United StatesNC72010COLLECTED09/14/2010Roadside along Kansas Rd, west of Hwy 3 south of Uniontown, Bourbon County.37.81978000, -94.98685000325Uplands. Associated with Andropogon gerardii, Bidens polylepis, Chamaechrista fasciculata, Cornus, Diospyros virginiana, Gleditsia triacanthos, Juglans nigra, Maclura pomifera, Monarda, Pycnanthemum virginianum, Quercus, Rhus glabra, and Sorghastrum nutans.Wild material1848907PI 664805
29PI 664869JDC/HP/2008/030/100Hypericum prolificum L. Missouri, United StatesNC7SEED2008COLLECTED10/06/2008Rudolf Bennitt Conservation Area, NE 1/4 of NE 1/4 of Section 25, T52N, R14W, Renick Quad, Randolph County.39.27527778, -92.43388889256Wild material1788211PI 664869
30PI 653309R. occidentalis HDF-2007-094Rubus occidentalis L. Nebraska, United StatesCORHABITAT2007COLLECTED07/09/2007Cherry County, Valentine City Park and area along creek Roadside with Rhus glabra Opuntia nearby41.88500000, -100.54870000823roadside along Lake Shore Drive. Riparian Edge @ State Park Mennachadinga CreekWild materialMichael Dossett, Chad Finn collected from Nebraska.

1733169PI 653309
31PI 664901JM20061003Teucrium canadense L. Missouri, United StatesNC72006COLLECTED09/25/2006Mile marker 222.1, Route 66 off of Interstate 44, southwest of Meramec State Park, West Sullivan, Crawford County.38.18194444, -91.20194444301Roadside prairie remnant (between railroad and state road). Ambrosia artemisiifolia, Andropogon gerardii, Celtis laevigata, Elaeagnus angustifolia, Eryngium, Helianthus mollus, Rhus glabra, Schrankia nuttallianum, and Sorghastrum nutans.Wild material1715759PI 664901
32PI 66201724Cornus drummondii C. A. Mey. Iowa, United StatesNC72003COLLECTED09/22/2003Eldon Wildlife Management Area, Floris, SW 1/4 of NW 1/4 of Section 9, T70N, R12W, Agency Quad, Davis County.40.88083333, -92.25222222235Near a pond. Sunny. Slight slope. Clay loam soil. Wild materialMedium sized, suckering shrubs. Good leaf quality and fruit production. 1649669PI 662017
33PI 64970212Physocarpus opulifolius (L.) Maxim. Iowa, United StatesNC72003COLLECTED09/14/2003100 meters south of campground at North Bear Creek, west side of Quandahl Road, Bear Creek Wildlife Area, Highlandville, NW 1/4 of SE 1/4 of Section 25, T100N, R7W, Dorchester Quad, Winneshiek County.43.44833333, -91.61861111265Limestone road cut. Mostly sunny. Steep slope with an eastern aspect. Thin soil with high stoniness, well drained. Wild materialMedium sized shrubs with arching stems. 1649462PI 649702
34PI 631302048Echinacea pallida (Nutt.) Nutt. Missouri, United StatesNC7HEAD1997COLLECTED08/25/1997Near Sleeper, Laclede County. Please contact curator for specific site location.37.75000000, -92.56666667390Roadside prairie remnant/disturbed area. Full exposure, ~15 degrees of slope with a southern aspect. Calcareous, dry soil with good drainage and high stoniness.Wild materialPlants were tall, occasional, and sometimes branched with pale pink flowers. Population had the "mixed pollen color" character (ie. most plants had white pollen, some had light yellow pollen). Part of site mowed, part of site previously harvested of seed: more of a "clear cut" than a random/scientific collection (probable collection for profit).1548372PI 631302
35PI 631264017Echinacea paradoxa (Norton) Britton var. neglecta McGregor Oklahoma, United StatesNC7HEAD1997COLLECTED08/10/1997Near Sulphur, Murray County. Please contact curator for specific site location.34.50000000, -96.96666667370Top of road bank adjacent to buffalo pasture. Full exposure on nearly level ground. Calcareous, well drained soil with high stoniness.Wild materialPlants were up to ~2.5 feet high, in relative abundance, and seldom branched with white and medium pink flowers. Endemic to Arbuckle Mountains.1547266PI 631264
36PI 64968615Monarda fistulosa L. Kansas, United StatesNC7Flower1985COLLECTED09/23/1985Chase County State Fishing Lake,T19S R8E W1/4 of SW 1/4 of Sec. 30, Cottonwood Falls Quad, Chase County38.36277600, -96.59551200402Southeast facing slope on limestone.Wild materialLemon-scented plants noted in this population.1028672PI 649686
37NA 89115TLM25-04aHamamelis ovalis S. W. Leonard Texas, United StatesNA2025COLLECTED07/10/2025State Highway 87 approximately 3.25 kilometers north of the crossroad junction with Texas Recreational Road 255 (RE 255); plants were growing in the narrow buffer woods along the east side of the highway.31.12051300, -93.72628100138The habitat is an upland mixed coniferous and deciduous woodlands in part to full shade and dry conditions, often under drought stress. Plants seem to always occur on the top of dry ridges or well-drained slopes. Slope: 0 to 1 percent. Aspect: N/A. Soils: The soils of this collection area are classified as Tehran-Letney Association, hilly (TLE) soils. The Tehran Series (55%) consists of deep, somewhat excessively drained, moderately rapidly permeable soils on uplands. They formed in thick loamy and sandy sediments on the Western Coastal Plain. These soils are on gently sloping to moderately steep uplands with slopes ranging from 1 to 20 percent. The Letney Series (30%) consists of deep, well drained, moderately rapidly permeable, upland soils. They formed in thick sandy and loamy sediments of the coastal plains. These soils are on gently sloping to moderately steep uplands with slopes ranging from 1 to 20 percent. Soil pH ranges from 4.5 to 6.0. The minor soil components include Doucette Series (10%) and Boykin Series (5%) soils. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). Geology: The underlying geology of this area is of Oligocene origin and characterized as Catahoula Formation. This formation is extensive and deep in Texas, up to 185 meters thick. In the area of the collection the Catahoula Formation is primarily mudstone and sand. The upper 90-150 meters is mudstone that is tuffaceous, and sandy; also, occasionally, with some bentonitic clay. (Source: USGS Texas Geologic Map Data).Wild material2191654NA 89115
38NA 885812024RJLFL-012Ilex ambigua Torr. Florida, United StatesNA2024COLLECTED11/13/2024Woodland edge along the south side of Bud Bass Road (DOF B48), 0.30 kilometers east of the junction with Norman Riley Road.30.75763200, -86.8018430032Woodland edge. Slope: 3 percent. Aspect: North. The underlying geology of this area is characterized as Citronelle Formation of the Pliocene period. The Citronelle Formation is widespread in the Gulf Coastal Plain. The type section for the Citronelle Formation, named by Matson (1916), is near Citronelle, Alabama. The Citronelle Formation grades laterally, through a broad facies transition, into the Miccosukee Formation of the eastern Florida panhandle. Coe (1979) investigated the Citronelle Formation in portions of the western Florida panhandle. The Citronelle Formation is a siliciclastic, deltaic deposit that is lithologically similar to, and time equivalent with, the Cypresshead Formation and, at least in part, the Long Key Formation (Cunningham et al., 1998) of the peninsula. In the western panhandle, some of the sediments mapped as Citronelle Formation may be reworked Citronelle. The lithologies are the same and there are few fossils present to document a possible younger age. The Citronelle Formation consists of gray to orange, often mottled, unconsolidated to poorly consolidated, very fine to very coarse, poorly sorted, clean to clayey sands. It contains significant amounts of clay, silt and gravel which may occur as beds and lenses and may vary considerably over short distances. Limonite nodules and limonite-cemented beds are common. Marine fossils are rare but fossil pollen, plant remains and occasional vertebrates are found. Much of the Citronelle Formation is highly permeable. It forms the Sand and Gravel Aquifer of the surficial aquifer system contain organics. The dominant fossils in the freshwater carbonates are mollusks. (Source: USGS Florida Geologic Map Data). The soils of this are characterized as Lakeland Series Sand, 0 to 5 percent slopes. The Lakeland series consists of very deep, excessively drained, rapid to very rapidly permeable soils on uplands. They formed in thick beds of eolian or marine and/or fluvio-marine sands in the Southern Coastal Plain MLRA (133A), the Carolina and Georgia Sandhills (MLRA 137), the Eastern Gulf Coast Flatwoods (MLRA 152A) and the Atlantic Coast Flatwoods (MLRA 153A). Slopes are dominantly from 0 to 12 percent but can range to 85 percent in dissected areas. Thickness of the sand exceeds 200 cm. Silt plus clay in the 25 to 100 cm control section ranges from 5 to 10 percent. Reaction ranges from very strongly acid to moderately acid throughout. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions).Wild material2169918NA 88581
39Ames 36284Oak Creek CanyonAlnus oblongifolia Torr. Arizona, United StatesNC7BARK2024COLLECTED10/18/2024Oak Creek Canyon, approximately five miles north-northeast of Sedona in the Coconino National Forest, T18N R6E Sec. 8 and Sec. 21 and also T19N R6E Sec. 22 and Sec. 27.35.01694800, -111.737559001538Creek beds in canyon bottom.Wild materialPlants sampled in nature had dark green, glossy leaves. Young bark is smooth and light grey, becoming dark and scaly with age. Approximately 50 feet in height.2169812Ames 36284
40NA 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
41NA 890822024RJLPA-010Amorpha fruticosa L. Pennsylvania, United StatesNA2024COLLECTED09/22/2024Outcrops along the Susquehanna River, accessed from the Historic Lock 12 parking lot off of Pennsylvania Road 372.39.81481500, -76.3275790034Plants are growing from part-sun to full sun in crevices of the outcrops and where organic debris has accumulated in between boulders along the Susquehanna River. The sites range from nearly xeric to dry mesic, at least on the surface. Plants are generally growing 4-10 m above the normal flow of the river; however, the Holtwood Dam is less than 1 kilometer upstream and debris found trapped in the boulders indicates that there is periodic flooding, at least, in the lower zone of 4+ meters or so above normal river flow. This habitat has a diverse assemblage of deciduous trees and shrubs as well as abundant herbaceous taxa. Slope: 0 to 25 percent. Aspect: Northeast (generally). Geology: The underlying geology of this area is probably of lower Paleozoic age and characterized as the Octoraro Formation. It includes albite-chlorite schist, phyllite, some hornblende gneiss, and granitized members. Soils: The area where this species occurs is right on the edge of two soil zones that transition from the river’s edge to mesic conditions upslope. The first is generally referred to as Rock Outcrop. This terrestrial matrix in which plants grow is largely exposed underlying rock geology with accumulated outwash, rock decomposition, and organic debris buildup. The second is Mt. Airy (80%) and Manor (20%) Series soils, 25 to 60 percent slopes, extremely stony (MRF). (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). EPA Ecoregion (Level III): Northern Piedmont (64). EPA Ecoregion (Level IV): Piedmont Uplands (64c).Wild material2169046NA 89082
42NA 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
43NA 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
44NA 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
45NA 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
46NA 890912024RM-TK-004Prunus sp.Florida, United StatesNA2024COLLECTED09/05/2024Blackwater River Wildlife Management Area: on the south side of Boundary Line Road about 0.32 kilometers west of Deaton Bridge Road along an area edged by a barbed wire fence.30.68579800, -86.8796430045Plants are growing from part-sun to full sun. Plants are growing in an area that is frequently burned with a lot of [Prunus sp. (orig. listed as Prunus alabamensis)] scattered throughout. This habitat is a longleaf pine-wiregrass community with scattered turkey (Quercus laevis) and blackjack oaks (Quercus incana). There is a slight slope downward. The line of [Prunus sp.] goes along a semi-ditch on the side of a dirt road. The plants probably get a bit more water than the plants out in the open forest. The [Prunus sp.] are most often without any other close woody companions. Slope: 0 percent. Aspect: North. Geology: The underlying geology of this area is probably of lower Pliocene age and characterized as the Citronelle Formation. The Citronelle Formation is widespread in the Gulf Coastal Plain. The type section for the Citronelle Formation, named by Matson (1916), is near Citronelle, Alabama. The Citronelle Formation grades laterally, through a broad facies transition, into the Miccosukee Formation of the eastern Florida panhandle. Coe (1979) investigated the Citronelle Formation in portions of the western Florida panhandle. The Citronelle Formation is a siliciclastic, deltaic deposit that is lithologically similar to, and time equivalent with, the Cypresshead Formation and, at least in part, the Long Key Formation (Cunningham et al., 1998) of the peninsula. In the western panhandle, some of the sediments mapped as Citronelle Formation may be reworked Citronelle. The lithologies are the same and there are few fossils present to document a possible younger age. The Citronelle Formation consists of gray to orange, often mottled, unconsolidated to poorly consolidated, very fine to very coarse, poorly sorted, clean to clayey sands. It contains significant amounts of clay, silt and gravel which may occur as beds and lenses and may vary considerably over short distances. Limonite nodules and limonite-cemented beds are common. Marine fossils are rare but fossil pollen, plant remains and occasional vertebrates are found. Much of the Citronelle Formation is highly permeable. It forms the Sand and Gravel Aquifer of the surficial aquifer system. (Source: USGS Florida Geologic Map Data). Soils: The soil of this area is characterized as Lakeland Series Sand, 0 to 5 percent slopes (21). The Lakeland Series consists of very deep, excessively drained, rapid to very rapidly permeable soils on uplands. They formed in thick beds of eolian or marine and/or fluvio-marine sands in the Southern Coastal Plain MLRA (133A), the Carolina and Georgia Sandhills (MLRA 137), the Eastern Gulf Coast Flatwoods (MLRA 152A) and the Atlantic Coast Flatwoods (MLRA 153A). (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). EPA Ecoregion (Level III): Southeastern Plains (65). EPA Ecoregion (Level IV): Southern Pine Plains and Hills (65f).Wild materialReceived as Prunus alabamensis; other collections of this material have proven not to be Prunus serotina var. alabamensis, but actually a species of plum; this will likewise be treated as unidentified material until its species can be ascertained. Collectors' notes refer to the plant by the name under which it was collected.2169055NA 89091
47NA 890932024RM-TK-006Ilex ambigua Torr. Florida, United StatesNA2024COLLECTED09/29/2024Blackwater River Wildlife Management Area: growing on the south side of Bud Bass Road, approximately 0.3 kilometers east of Training Center R./Norma Riley Rd.30.75759720, -86.8018722029This plant is growing in part-shade under mesic conditions along the edge of a longleaf pine plantation. Slope: 0 percent. Aspect: North. Geology: The underlying geology of this area is probably of lower Pliocene age and characterized as the Citronelle Formation. The Citronelle Formation is widespread in the Gulf Coastal Plain. The type section for the Citronelle Formation, named by Matson (1916), is near Citronelle, Alabama. The Citronelle Formation grades laterally, through a broad facies transition, into the Miccosukee Formation of the eastern Florida panhandle. Coe (1979) investigated the Citronelle Formation in portions of the western Florida panhandle. The Citronelle Formation is a siliciclastic, deltaic deposit that is lithologically similar to, and time equivalent with, the Cypresshead Formation and, at least in part, the Long Key Formation (Cunningham et al., 1998) of the peninsula. In the western panhandle, some of the sediments mapped as Citronelle Formation may be reworked Citronelle. The lithologies are the same and there are few fossils present to document a possible younger age. The Citronelle Formation consists of gray to orange, often mottled, unconsolidated to poorly consolidated, very fine to very coarse, poorly sorted, clean to clayey sands. It contains significant amounts of clay, silt and gravel which may occur as beds and lenses and may vary considerably over short distances. Limonite nodules and limonite-cemented beds are common. Marine fossils are rare but fossil pollen, plant remains and occasional vertebrates are found. Much of the Citronelle Formation is highly permeable. It forms the Sand and Gravel Aquifer of the surficial aquifer system. (Source: USGS Florida Geologic Map Data). Soils: The soil of this area is characterized as Lakeland Series Sand, 0 to 5 percent slopes (21). The Lakeland Series consists of very deep, excessively drained, rapid to very rapidly permeable soils on uplands. They formed in thick beds of eolian or marine and/or fluvio-marine sands in the Southern Coastal Plain MLRA (133A), the Carolina and Georgia Sandhills (MLRA 137), the Eastern Gulf Coast Flatwoods (MLRA 152A) and the Atlantic Coast Flatwoods (MLRA 153A). (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). EPA Ecoregion (Level III): Southeastern Plains (65). EPA Ecoregion (Level IV): Southern Pine Plains and Hills (65f).Wild material2169057NA 89093
48NA 87823FL24-01Ilex cassine L. Florida, United StatesNA2024COLLECTED09/05/2024Matanzas State Forest.29.72143991, -81.28386478Boggy blackwater ditches along edge of dirt road. EPA Ecoregion III: Southern Coastal Plain (75). EPA Ecoregion IV: Eastern Florida Flatwoods (75d). Geology: Beach Ridge and Dune. Soil: Immokalee Series Fine Sand.Wild material2168973NA 87823
49NA 88844RJL-RM2023FLAL-018Clethra alnifolia L. Florida, United StatesNA2023COLLECTED12/13/2023Yellow River Water Management Area, accessed off of Old River Road by vehicle on an unmaintained sand road for approximately 1.68 kilometers. Upon reaching the destination, plants are accessed by foot along unmaintained trail to the east.30.83495500, -86.6200540027Plants are growing primarily in part shade as understory shrubs in mixed evergreen and deciduous, moist to wet, acidic woodlands. Plants form large colonies and appear to have been subjected to prescribed fire in recent years. Slope: 10 to 15 percent. Aspect: Northeast. The underlying geology of this area is the Citronelle Formation of Pliocene origin and consists of gray to orange, often mottled, unconsolidated to poorly consolidated, very fine to very coarse, poorly sorted, clean to clayey sands. It contains significant amounts of clay, silt and gravel which may occur as beds and lenses and may vary considerably over short distances. Limonite nodules and limonite-cemented beds are common. (Source: USGS Florida Geologic Map Data.) The soil profile for this area is classified as the Bonifay Soil Series. 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. (Source: NRCS Web Soil Survey.)Wild material2165674NA 88844
50NA 88820TJK2023AL-005Hydrangea arborescens L. Alabama, United StatesNA2023COLLECTED12/07/2023Between Monroe County Route 1 and Tom Hayles Road.31.40575900, -87.5492400022In woodlands on limestone outcrop. While the upper area of slopes is covered by a thin soil layer, the exposed limestone rock outcrop on the northwestern edge of this area is a low competition niche for plants like the Hydrangea to gain a foothold. Slope: 60% (plus). Aspect: Northwest. Elevation: 72 feet.Wild material2165649NA 88820
51NA 88821TJK2023AL-006Hydrangea quercifolia W. Bartram Alabama, United StatesNA2023COLLECTED12/07/2023Between Monroe County Route 1 and Tom Hayles Road.31.40580000, -87.5489000022In woodlands on limestone outcrop. While the upper area of slopes is covered by a thin soil layer, the exposed limestone rock outcrop on the northwestern edge of this area is a low competition niche for plants like the Hydrangea to gain a foothold. Slope: 60% (plus). Aspect: Northwest. Elevation: 72 feet.Wild material2165650NA 88821
52NA 88704RJL2023NCSC-009Rhododendron viscosum (L.) Torr. North Carolina, United StatesNA2023COLLECTED11/13/2023Sandhills Game Land: wetlands and moist depressions along Hoffman Road, Scotland County Road 1328,34.95510000, -79.51769700112Plants are growing in sun in an acidic wetland habitat rich in sphagnum and other wetland species. The habitat is moist to wet year-round and periodically has surface runoff occurring; even so, this habitat can become quite dry during seasonal periods without rainfall. Slope: 2 to 3 percent. Aspect: Northeast. The underlying geology of this area is of Tertiary origin and characterized as Pinehurst Formation. It is comprised of medium- to coarse-grained sand as well as cross-bedding and rhythmic bands of clayey sand that are unconsolidated. (Source: USGS North Carolina Geologic Map Data.) The primary soil type in the collection area is classified as Pelion Loamy Sand (2 to 6 percent slopes). The Pelion Loamy Sand series consists of very deep, moderately well-drained marine deposits, fluviomarine deposits, and sand sheets. Permeability is moderately slow or slow. Surface layers 0-25 cm deep are comprised of loamy sand with a weak fine granular structure and are very friable. Deeper horizons are comprised of sandy loam, sandy clay loam, or clay loam in the upper part and includes sandy clay or clay in the deepest part. Soils are extremely acid to strongly acid. (Source: NRCS Web Soil Survey.)Wild material2159132NA 88704
53NA 88705RJL2023NCSC-010Zenobia pulverulenta (W. Bartram ex Willd.) Pollard North Carolina, United StatesNA2023COLLECTED11/13/2023Sandhills Game Land: wetlands and moist depressions along Hoffman Road, Scotland County Road 1328,34.95510000, -79.51769700112Plants are growing in part-shade to sun in an acidic wetland habitat rich in sphagnum and other obligate wetland species. The habitat is moist to wet year-round and periodically has surface runoff occurring; even so, this habitat can become quite dry during seasonal periods without rainfall. Slope: 2 to 3 percent. Aspect: Northeast. The underlying geology of this area is of Tertiary origin and characterized as Pinehurst Formation. It is comprised of medium- to coarse-grained sand as well as cross-bedding and rhythmic bands of clayey sand that are unconsolidated. (Source: USGS North Carolina Geologic Map Data.) The primary soil type in the collection area is classified as Pelion Loamy Sand (2 to 6 percent slopes). The Pelion Loamy Sand series consists of very deep, moderately well-drained marine deposits, fluviomarine deposits, and sand sheets. Permeability is moderately slow or slow. Surface layers 0-25 cm deep are comprised of loamy sand with a weak fine granular structure and are very friable. Deeper horizons are comprised of sandy loam, sandy clay loam, or clay loam in the upper part and includes sandy clay or clay in the deepest part. Soils are extremely acid to strongly acid. (Source: NRCS Web Soil Survey.)Wild material2159133NA 88705
54NA 88706RJL2023NCSC-011Smilax laurifolia L. North Carolina, United StatesNA2023COLLECTED11/13/2023Sandhills Game Land: wetland associated with the West Prong of Juniper Creek on the north side of Whisky Still Road approximately 0.63 kilometers northeast of Hoffman Road, Scotland County Road 1328.34.95683200, -79.51146200103Plants are growing in part-shade to sun in an acidic wetland habitat rich in sphagnum and other wetland species. The habitat is moist to wet year-round and periodically has surface runoff occurring; even so, this habitat can become quite dry during seasonal periods without rainfall. Slope: N/A. Aspect: N/A. The underlying geology of this area is of Tertiary origin and characterized as Pinehurst Formation. It is comprised of medium- to coarse-grained sand as well as cross-bedding and rhythmic bands of clayey sand that are unconsolidated. (Source: USGS North Carolina Geologic Map Data.) The primary soil type in the collection area is classified as Johnston Series soils, 0 to 2 percent slopes, frequently flooded. The Johnson 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. (Source: NRCS Web Soil Survey.)Wild material2159134NA 88706
55NA 88707RJL2023NCSC-012Rhododendron viscosum (L.) Torr. North Carolina, United StatesNA2023COLLECTED11/13/2023Sandhills Game Land: wetland associated with the West Prong of Juniper Creek on the north side of Whisky Still Road approximately 0.63 kilometers northeast of Hoffman Road, Scotland County Road 1328.34.95683200, -79.51146200103Plants are growing in part-shade to sun in an acidic wetland habitat rich in sphagnum and other wetland species. The habitat is moist to wet year-round and periodically has surface runoff occurring; even so, this habitat can become quite dry during seasonal periods without rainfall. Slope: N/A. Aspect: N/A. The underlying geology of this area is of Tertiary origin and characterized as Pinehurst Formation. It is comprised of medium- to coarse-grained sand as well as cross-bedding and rhythmic bands of clayey sand that are unconsolidated. (Source: USGS North Carolina Geologic Map Data.) The primary soil type in the collection area is classified as Johnston Series soils, 0 to 2 percent slopes, frequently flooded. The Johnson 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. (Source: NRCS Web Soil Survey.)Wild material2159135NA 88707
56Ames 36168Mount MagazinePtelea trifoliata L. Arkansas, United StatesNC7PLANT2023COLLECTED08/26/2023Mount Magazine State Park primarily localized to the northwest rim of the mountain along the trails heading west from Brown's Spring, T6N R25W Sec. 21.35.17130900, -93.65582200786Top of sky-island mountain. Localized along the rims just above steep cliffs on north facing slopes.Wild materialPlants in nature ranging from three to fifteen feet in height with peak bloom observed during the first week of May (2023). 2158787Ames 36168
57Ames 36153JDC/MM/2023/049/1081Monarda maxmedleyi J. J. N. Campb. & Floden Kentucky, United StatesNC7PLANT2023COLLECTED08/10/2023Lily Mountain Preserve located 6.92 miles west, southwest of South Irvine37.63661300, -84.09026400432Open dry, woods. Localized at highest elevations of preserve.Wild materialPlants measuring 12-18" in height. Spreading vegetatively via rhizomes. Majority of specimens with mostly white flowers. Peak flowering at collection site occurred near 26th of May (2023).2158358Ames 36153
58Ames 36159JDC/MM/2023/062/1094Monarda maxmedleyi J. J. N. Campb. & Floden Kentucky, United StatesNC7PLANT2023COLLECTED08/09/2023Daniel Boone National Forest on north and south sides along Zilpo Road with the highest abundance being across from intersection with Dogwood Lane.38.05551500, -83.53288600354Edges of woods/roadsides. Localized to west and southeast facing slopes.Wild materialPlants measuring 12-18" in height. Spreading vegetatively via rhizomes. Flower color varies within the population from white to pink. Peak flowering at collection site occurred near 27th of May (2023).2158364Ames 36159
59OPGC 8811CBG- 10775Penstemon pallidus Small Illinois, United StatesOPGC2023Wild material2142242OPGC 8811
60W6 61393CBG- 10818Linum sulcatum Riddell Illinois, United StatesW6SEED2023Wild material2142275W6 61393
61Ames 36016Sugar CreekPlatanus occidentalis L. Iowa, United StatesNC7FRUIT2023COLLECTED02/20/2023Scattered along Sugar Creek between 3.1 miles north and also 1.3 miles northeast of Franklin, T68N R6W Sections 2, 11, 12, 13 and 24.40.70277500, -91.51065900185River banks and floodplains.Wild materialThis accession of American sycamore includes the sampling from several very large specimens found in the state of Iowa including specimen #211-12 currently (2023) ranking 13th largest measuring 14' 9" circumference; 106' 8" in height; and a calculated spread of 114' 8" totalling 312.346 points (measured 23 April 2023 by Mark Rouw); specimen #211-10 currently (2023) ranking as the 9th largest measuring 16' 2" circumference; 97' 5" in height; and a calculated spread of 134' 3" totalling 322.983 points (measured 21 April 2020 by Mark Rouw); and specimen #211-6 currently (2023) ranking 2nd largest measuring 20' 2.5" circumference; 109' 6" in height; and a calculated spread of 148' 9" totalling 389.188 points (measured 23 April 2023 by Mark Rouw). Numerous specimens noted in nature with extremely white, superior, ornamental bark characteristics, specifically specimen #211-13. 2141476Ames 36016
62WLP 3092RJLSEUS2022-021Rhododendron prunifolium (Small) Millais Alabama, United StatesNA2023COLLECTED12/10/2023Slopes along Poke Springs Branch inlet accessed by boat from Walter F. George Reservoir. Generally uncommon, but frequent at this site. 31.72318400, -85.1290780069Plants are growing in part-shade to shade on the well-drained mostly deciduous woodland slopes approximately 3-6 meters above the inlet.
Soils: The underlying geology of this area is of Cretaceous origin and characterized as Selma Group; Providence Sand. The upper part of the profile consists of cross-bedded fine to coarse sand and white, dark-gray and pale-red-purple mottled clay containing lignite, sand, and kaolin. The lower part consists of dark-gray laminated to thin-bedded silty clay and abundantly micaceous, carbonaceous, fossiliferous very fine to fine sand.
Source: USGS Alabama Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=ALKp%3B1)
The primary soil types in the collection area are classified as Nankin-Lucy Complex soil (20 to 60 percent slopes). The Nankin Series consists of very deep, well drained, moderately slowly permeable soils on uplands of the Coastal Plain. They formed in stratified loamy and clayey marine sediments. Slopes range from 0 to 60 percent. Soils are comprised of sandy loam in the upper 25 cm to sandy clay loam and sandy clay in lower strata to about 1.7 meters deep; these soils are strongly acid. 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. Slopes vary from 0 to 45 percent. These soils are generally loamy to sandy loam in the upper 25 cm and sandy clay loam in the lower strata to 2 meters; these are strongly acid soils.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2141446WLP 3092
63NA 88549RJLSEUS2022-022Rhododendron minus Michx. var. minus Georgia, United StatesNA2023COLLECTED12/10/2022East side of Georgia State Hwy. 39, on the south side of Kolomoki Creek approximately 11 kilometers south of Fort Gaines, Georgia. Common on this site, but otherwise infrequent. This species is near the southernmost end of its natural range.31.52053400, -85.0235160053Plants are growing in part-shade to shade of deciduous upland, dry, deciduous woodlands on steep slopes 10-15 meters above Kolomoki Creek.
Soils: The underlying geology of this area is of Paleocene origin and characterized as Tuscahoma Sand. As mapped this formation includes lower Eocene Bashi Marl Member of the Hatchetigbee Formation. This formation consists of light-gray to light-olive-gray laminated and thin-bedded carbonaceous silt and clay interbedded with fine sand; thin lignite beds occur locally. Lower part of the formation includes beds of fossiliferous, glauconitic fine quartz sand containing spheroidal sandstone concretions, gravel and clay pebbles.
Source: USGS Georgia Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=GANu%3B1)
The primary soil types in the collection area are classified as Ailey-Cowarts Complex Series soils (8 to 25 percent slopes). The Ailey Series consists of well drained or somewhat excessively drained soils formed by fluviomarine and marine deposits. These soils are found marine terraces and low hills of the upper coastal plain and sandhills; they are strongly acidic. The Cowarts Series consists of very deep, moderately well and well drained soils on ridge tops and side slopes on uplands of the Coastal Plain Major Land Resource Area. They formed in loamy marine sediments. Slopes range from 1 to 60 percent.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2140776NA 88549
64NA 88550RJLSEUS2022-023Kalmia latifolia L. Georgia, United StatesNA2023COLLECTED12/10/2022East side of Georgia State Hwy. 39, on the south side of Kolomoki Creek approximately 11 kilometers south of Fort Gaines, Georgia. Common on this site, but otherwise infrequent. This species is near the southernmost end of its natural range. 31.52053400, -85.0235160053Plants are growing in part-shade to shade of deciduous upland, dry, deciduous woodlands on steep slopes 10-15 meters above Kolomoki Creek.
Soils: The underlying geology of this area is of Paleocene origin and characterized as Tuscahoma Sand. As mapped this formation includes lower Eocene Bashi Marl Member of the Hatchetigbee Formation. This formation consists of light-gray to light-olive-gray laminated and thin-bedded carbonaceous silt and clay interbedded with fine sand; thin lignite beds occur locally. Lower part of the formation includes beds of fossiliferous, glauconitic fine quartz sand containing spheroidal sandstone concretions, gravel and clay pebbles.
Source: USGS Georgia Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=GANu%3B1)
The primary soil types in the collection area are classified as Ailey-Cowarts Complex Series soils (8 to 25 percent slopes). The Ailey Series consists of well drained or somewhat excessively drained soils formed by fluviomarine and marine deposits. These soils are found marine terraces and low hills of the upper coastal plain and sandhills; they are strongly acidic. The Cowarts Series consists of very deep, moderately well and well drained soils on ridge tops and side slopes on uplands of the Coastal Plain Major Land Resource Area. They formed in loamy marine sediments. Slopes range from 1 to 60 percent.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2140777NA 88550
65NA 88562RJLSEUS2022-035Kalmia latifolia L. Alabama, United StatesNA2023COLLECTED12/12/2022Plants growing on both sides of River Ridge Road accessed from Alabama State Hwy 41 via Tin Cup Alley Road. Common at this site 31.73823700, -87.35821100132Plants are growing in part-shade to full sun on top of a very exposed ridge top under dry conditions.
Soils: The underlying geology of this area is of Eocene origin and characterized as Claiborne Group; Gosport Sand and Lisbon Formation Undifferentiated in part. Greenish-gray calcareous, glauconitic, fossiliferous clayey sand; marl; carbonaceous sand; carbonaceous silty clay; and coarse glauconitic, fossiliferous, quartz sand.
Source: USGS Alabama Geological Map Data (https://mrdata.usgs.gov/geology/state/state.php?state=AL)
The primary soil types in the collection area are classified as Saffell Very Gravelly Sandy Loam soil (5 to 8 percent slopes). 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.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2140787NA 88562
66NA 88568RJLSEUS2022-041Oxydendrum arboreum (L.) DC. Florida, United StatesNA2023COLLECTED12/14/2022Plants growing along the south side of Eglin AFB Choctaw Nolf Road northwest of Choctaw Navy Outlying Field. This road goes west and takes circuitous route to the north around the Field enroute to Escribano Point Wildlife Management Area. Common at the location; infrequent, otherwise. 30.51525300, -87.005638002Trees are growing in full sun to part-shade in mesic habitat associate with a nearby wet depression, less than 0.2 meters above the high moisture zone. The trees also extend into slightly drier mesic to the marginally xeric zone.
Soils: The underlying geology of this area is classified as Alluvium, of Pleistocene/Holocene origin and consists of undifferentiated Quaternary sediments of varying thickness including siliciclastics, organics and freshwater carbonates. The siliciclastics are light gray, tan, brown to black, unconsolidated to poorly consolidated, clean to clayey, silty, unfossiliferous, variably organic-bearing sands to blue green to olive green, poorly to moderately consolidated, sandy, silty clays. Organics occur as plant debris, roots, disseminated organic matrix and beds of peat. Freshwater carbonates, often referred to as marls in the literature, are scattered.
The primary soil types in the collection area are classified as Leon Sand soils (0 to 2 percent slopes). The Leon Series consists of very deep, very poorly and poorly drained, moderately rapid to moderately slowly permeable soils on upland flats, depressions, stream terraces and tidal areas. They formed in sandy marine sediments of the Eastern Gulf Coast Flatwoods, the Atlantic Coast Flatwoods, and to a lesser extent in the Southern Coastal Plain, and the North-Central Florida Ridge. Slopes range from 0 to 5 percent. Leon series is comprised of 95%+ sand in the strata to 3+ meters deep.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2140790NA 88568
67NA 88574RJLSEUS2022-047Rhododendron austrinum (Small) Rehder Florida, United StatesNA2023COLLECTED12/15/2022Plants are growing along a several mile stretch of the Yellow River and accessed by boat via the Yellow River Boat Ramp on the east side of Florida State Hwy 87. The species is found frequently along several miles of the Yellow River.30.58133600, -86.899539002Plants are found growing in part-shade to shade along areas of the river where natural levies, 1-3 meters tall, have formed, depositing sand and organic matter. The plants grow well-above normal flow of the river in well-drained to dry conditions. Even so, they are periodically subjected to inundation from floodwaters.
Soils: The underlying geology of this area is classified as Alluvium, of Pleistocene/Holocene origin and consists of undifferentiated Quaternary sediments of varying thickness including siliciclastics, organics and freshwater carbonates. The siliciclastics are light gray, tan, brown to black, unconsolidated to poorly consolidated, clean to clayey, silty, unfossiliferous, variably organic-bearing sands to blue green to olive green, poorly to moderately consolidated, sandy, silty clays. Organics occur as plant debris, roots, disseminated organic matrix and beds of peat. Freshwater carbonates, often referred to as marls in the literature, are scattered.
Source: USGS Florida Geologic Map Data (https://mrdata.usgs.gov/geology/state/state.php?state=fl)
The surface soil profile of this area is primarily Bibb-Kinston Series Association. Bibb Series soils are coarse-loamy, sandy, acid soils that are poorly drained. They are soils of flood plains and streams subject to frequent flooding. These are found in association with Kinston Series soils that are fine-loamy, sandy, acid soils of flood plains and stream subject to frequent flooding. The Bibb-Kinston Association ranges from 1-1.5 meters thick and is strongly acid.
Source: Soil Survey of Santa Rosa County and NRCS Web Soil Survey (https://www.nrcs.usda.gov/Internet/FSE_MANUSCRIPTS/florida/FL113/0/SantaRosa.pdf and https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild materialYellow River Pink Austrinum2140792NA 88574
68NA 89039RJL2022IL-001Ptelea trifoliata L. Illinois, United StatesNA2022COLLECTED09/28/2022Site of plant habitat is located at 823 E Co Rd 1220, Hamilton, IL 62341 which is the property where Jacob's Geode Shop and Mine is located. This species is scattered and relatively common throughout the woodlands on this site.40.37848400, -91.35390200175Plants growing in shade to part-shade of deciduous woodlands above a small creek.
Soils: The underlying geology of this area is of Mississippian origin and comprised of Warsaw Formation and Salem Limestone. Major lithological components include limestone that can be shaly, oolitic, bioclastic, or cherty. Minor lithological components include siltstone that can contain geodes or drusy quartz and can be calcareous.
Source: USGS Illinois Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=ILMws%3B0)
The surface soil profile of this area is Coffeen silt loam, 0 to 2 percent slopes, that are frequently flooded. The Coffeen series consists of very deep, somewhat poorly drained, moderately permeable soils on flood plains, low terraces or benches, toe slopes, and alluvial fans. They formed in silty alluvium. Much of the alluvium is of local origin derived from the nearby loess-covered uplands.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2139604NA 89039
69NA 89037RJL2022KS-004 Fraxinus pennsylvanica Marshall Kansas, United StatesNAImage2022COLLECTED09/21/2022 Coronado Heights Park, Smoky View, Kansas hillsides surrounding the historic WPA circa 1932 Coronado Heights Castle located about 91 meters above the surrounding land. This plant is scattered and infrequent on the slopes of this site.38.61065700, -97.70408300448Plants growing in full sun, under extreme exposure, rocky, dry and thin soils of this short grass prairie habitat on the slopes surrounding the summit of Coronado Heights Park. Plants tend
Soils: The underlying geology of this area is of Upper Cretaceous origin and comprised of Kiowa Shale or FM- light -gray to black illitic shale with thin coquinoidal limestone beds at the base; sandstone lenses are common. Cheyenne Sandstone-massive to cross-bedded, light-gray to buff fine-grained sandstone with lenses to be found in runoff zones where moisture is temporarily more abundant.of gray sandy shale and conglomerate.
Source: USGS Kansas Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=KSKkc%3B0)
The surface soil profile of this area is Lancaster-Hedville complex, 3 to 20 percent slopes. The Lancaster series consists of moderately deep, well drained soils that formed in residuum from sandstone and sandy shales; it can be up to 200 cm deep. Slopes range from 1-20%. Hedville soils have bedrock within 50 centimeters of the surface and occur on similar hillslope positions.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2139602NA 89037
70NA 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
71NA 89035RJL2022KS-002Rosa arkansana Porter Kansas, United StatesNA2022COLLECTED09/20/2022Coronado Heights Park, Smoky View, Kansas hillsides surrounding the historic WPA circa 1932 Coronado Heights Castle located about 91 meters above the surrounding land. This plant is quite abundant on the slopes of this site and highly competitive.38.61158800, -97.70427000475Plants growing in part-sun to full sun, under extreme exposure, rocky, dry and thin soils of this short grass prairie habitat on the slopes surrounding the summit of Coronado Heights Park.
The underlying geology of this area is of Upper Cretaceous origin and comprised of Kiowa Shale or FM- light -gray to black illitic shale with thin coquinoidal limestone beds at the base; sandstone lenses are common. Cheyenne Sandstone-massive to cross-bedded, light-gray to buff fine-grained sandstone with lenses of gray sandy shale and conglomerate.
Source: USGS Kansas Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=KSKkc%3B0)
The surface soil profile of this area is Lancaster-Hedville complex, 3 to 20 percent slopes. The Lancaster series consists of moderately deep, well drained soils that formed in residuum from sandstone and sandy shales; it can be up to 200 cm deep. Slopes range from 1-20%. Hedville soils have bedrock within 50 centimeters of the surface and occur on similar hillslope positions.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2139600NA 89035
72NA 89034RJL2022KS-001Baptisia australis (L.) R. Br. var. minor (Lehm.) Fernald Kansas, United StatesNA2022COLLECTED09/20/2022Coronado Heights Park, Smoky View, Kansas hillsides surrounding the historic WPA circa 1932 Coronado Heights Castle located about 91 meters above the surrounding land. This plant is sporadic to common on the slopes of this site.38.61349700, -97.70303900487This plant is sporadic to common on the slopes of this site.
Habitat Notes: Plants growing in full sun, under extreme exposure, rocky, dry and thin soils of this short grass prairie habitat on the slopes surrounding the summit of Coronado Heights Park.
The underlying geology of this area is of Upper Cretaceous origin and comprised of Kiowa Shale or FM- light -gray to black illitic shale with thin coquinoidal limestone beds at the base; sandstone lenses are common. Cheyenne Sandstone-massive to cross-bedded, light-gray to buff fine-grained sandstone with lenses of gray sandy shale and conglomerate.
Source: USGS Kansas Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=KSKkc%3B0)
The surface soil profile of this area is Lancaster-Hedville complex, 3 to 20 percent slopes. The Lancaster series consists of moderately deep, well drained soils that formed in residuum from sandstone and sandy shales; it can be up to 200 cm deep. Slopes range from 1-20%. Hedville soils have bedrock within 50 centimeters of the surface and occur on similar hillslope positions.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild materialreceived as Baptisia minor2139599NA 89034
73Ames 35907Oak Creek CanyonFraxinus velutina Torr. Arizona, United StatesNC7SHOOT2022COLLECTED09/02/2022Oak Creek Canyon, approximately five miles north-northeast of Sedona in the Coconino National Forest. T18N R6E NE 1/4 NW 1/4 Sec. 21 .34.93600300, -111.744369001464Floodplain and riverbanks, growing in gravely soil.Wild materialMost of the velvet ash in this population are small trees (10-25 feet in height and approximately 5 inches DBH). Variation was noted for leaflet pubescence but with the petioles of all trees in the population being pubescent. 2139669Ames 35907
74W6 60214NEWFS-754Lespedeza capitata Michx. Rhode Island, United StatesW62021Wild materialDrooping because top heavy.2138840W6 60214
75NA 88421CBG-10737Prunus americana Marshall NASEED2021Wild materialSpatially discreet collection for a clonal species. Counts made approximately every 6 feet. Fruits collected from the plant and the ground.2137989NA 88421
76NA 88320CBG-10190Hydrangea arborescens L. Illinois, United StatesNA2021Wild material2120058NA 88320
77NA 88332CBG-10580Hypericum prolificum L. Illinois, United StatesNA2021Wild materialPlant numbers sampled estimated.2120171NA 88332
78OPGC 8343CBG-10575Euthamia graminifolia (L.) Nutt. Illinois, United StatesOPGC2021Wild materialPlant numbers sampled estimated.2120166OPGC 8343
79W6 59243CBG-10560Cinna arundinacea L. Illinois, United StatesW62021Wild materialPlant numbers estimated.2120155W6 59243
80W6 59266CBG-10588Muhlenbergia sobolifera (Muhl. ex Willd.) Trin. Illinois, United StatesW62021Wild material2120209W6 59266
81W6 59267CBG-10590Muhlenbergia glabrifloris Scribn. Illinois, United StatesW62021Wild materialReceived as: Muhlenbergia glabriflora. Plant numbers sampled estimated.2120210W6 59267
82Ames 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
83Ames 35541NAO/MB/2020/01/53Monarda bradburiana L. C. Beck Illinois, United StatesNC7SEED2020COLLECTED07/16/2020Eagle Point Bay area located at southwest portion of Lake of Egypt, T11S R2E NE1/4 Sec. 1 and T11S R2E NW1/4 Sec. 6, Johnson County37.59183900, -88.93008100168Roadside, wooded rocky hillside.Wild material2106720Ames 35541
84WLP 1686APS/RS/2019/067/396Rosa setigera Michx. Arkansas, United StatesNAFRUIT2019COLLECTED11/07/2019Located near intersection of Smith Mountain Road and Newton County 8828 Road approximately 6.00 miles north of Deer, Newton County35.91212000, -93.21112000636Roadside, upland with rocky soilsWild material2097789WLP 1686
85Ames 34433Bryantsburg Prairie Salix humilis Marshall Iowa, United StatesNC7Fruit2019COLLECTED05/17/2019Bryantsburg Prairie located 2.75 miles south of Hazelton, T90N R9W SE ¼ SE ¼ NE ¼ Sec. 28.42.57794200, -91.90508100298Native prairie remnant.Wild materialPlants averaging 4.0-4.5 feet in height with extremely vigorous and densly flowered stems (no branching), perhaps a response due to management (e.g. burning and/or mowing). Estimated 25 ramets per genet. Some with pinkish/red fruiting capsules.2091749Ames 34433
86Ames 343483247Monarda punctata L. Missouri, United StatesNC72018COLLECTED09/13/2018Illiniwek Village State Historic Site located approximately 2.90 miles northeast of Wayland, T65N R6W SE ¼ Sec. 16, Clark County.40.42887800, -91.55410100161On flat open sand terrace.Wild material1967550Ames 34348
87NA 88425NCBG-738Rosa carolina L. North Carolina, United StatesNASEED2018Wild materialRosa carolina1966039NA 88425
88W6 54767NCBG-624Tridens flavus (L.) Hitchc. North Carolina, United StatesW6SEED2018Wild materialTridens flavus1965993W6 54767
89W6 54820NCBG-759Verbesina occidentalis (L.) Walter Maryland, United StatesW6SEED2018Wild materialVerbesina occidentalis1966046W6 54820
90NA 88001MARSB-595Morella pensylvanica (Mirb.) Kartesz New York, United StatesNASEED2018Wild material1964805NA 88001
91NA 85021JDC/SS/2018/004/817Sapindus saponaria L. var. drummondii (Hook. & Arn.) L. D. Benson Oklahoma, United StatesNAImage2018COLLECTED03/12/2018Private property approximately 4.8 miles southeast of Mulhall, north side of Cimarron River, T18N R2W, Logan County35.99972000, -97.39735900210Transition zone between higher elevations and bottomlands.Wild material1957958NA 85021
92NA 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
93NA 85024JDC/SS/2018/020/833Sapindus saponaria L. var. drummondii (Hook. & Arn.) L. D. Benson Kansas, United StatesNAImage2018COLLECTED03/15/2018Private property approximately 3.65 miles north of Lake City on Cottonwood Creek and Sand Creek watersheds, T30S R14W, Barber County37.39995200, -98.84153900593Cedar and elm woods.Wild material1957961NA 85024
94Ames 34038Ames 34038Monarda punctata L. Illinois, United StatesNC7SEED2017COLLECTED10/29/2017Nachusa Grasslands located approximately 4.17 miles northwest of Franklin Grove just west of Lowden Road, T22N R10E NW 1/4 NW 1/4 SE 1/4 Sec. 16, Ogle County.41.89120000, -89.34490000225Newly disturbed ground (fenceline installation 2015) consisting of almost level sandy soil with a very slight slope.Wild materialPlants ranging between 16-22" in height, branched with numerous seed heads.1954327Ames 34038
95Ames 34024Ames 34024Monarda fistulosa L. New Mexico, United StatesNC7Flower2017COLLECTED09/19/2017North of Cherry Creek Campground in the Gila National Forest along highway NM-15 (west side of road), T16S R13W Sec. 17, Grant County.32.91992700, -108.219019002105Roadside. Mixed habitat including woody and herbaceous vegetation.Wild material1953996Ames 34024
96Ames 34007JDC/PP/2017/052/806Pinus ponderosa P. Lawson & C. Lawson Nebraska, United StatesNC7FRUIT2017COLLECTED08/29/2017Areas on both north and south sides of the Niobrara River between Long Pine and Springview, T32N R21W; T32N R20W; and T31N R21W in Brown and Keya Paha Counties.42.75716800, -99.74657300685Dry, rocky ridgetops.Wild materialGenetics represent the extreme eastern edgeo of the species native range.1953921Ames 34007
97WLP 2602JDC/TA/2017/053/807Tilia americana L. Nebraska, United StatesNAPLANT2017COLLECTED08/29/2017Niobrara River Valley just 25.9 miles east, southeast of Valentine, T33N R23W Sec. 32 and Sec. 33.42.78284200, -100.05716700658Floodplain and also base of adjacent bluffs/slopes (north-facing).Wild materialGenetics represent the extreme western edge of the species native range.1953922WLP 2602
98Ames 34015Ames 34015Cornus rugosa Lam. Minnesota, United StatesNC72017COLLECTED08/23/2017Smoky Hills State Forest between Snellman and Osage, T139N R37W Sec. 2, 9, 11, and 14 and also T140N R37W Sec. 26 and 34.46.89278300, -95.35163300501Mixed pine and deciduous moist woods.Wild material1953929Ames 34015
99Ames 33918APS/GD/2017/008/267Gymnocladus dioicus (L.) K. Koch Minnesota, United StatesNC7Fruit2017COLLECTED03/16/2017Minnesota River watershed covering approximately 9.0 river miles between Redwood Falls and Vicksburg Park, Renville County44.61447700, -95.14878600254Mixed habitats, both upland dry sites, wet sites, and rocky sites. Wild material1946985Ames 33918
100WLP 1437NA 84027Oxydendrum arboreum (L.) DC. Florida, United StatesNA2016COLLECTED11/11/2016Woodlands associated with Miller Bayou, south of housing subdivision off of Pearl Court.30.46413000, -86.928040002Full sun to partial shade in mixed coniferous/broadleaved evergreen woodlands, with a mixture of deciduous plants in highly acidic sandy soils approximately 100-300 ft. from the salt marsh edge associated with Miller Bayou.1950372WLP 1437
101WLP 1181NA 83958Diospyros virginiana L. Kentucky, United StatesNA2016COLLECTED09/30/2016Daniel Boone National Forest, Natural Arch Scenic Area.36.84100000, -84.51200000408Natural area park.1951334WLP 1181
102Ames 33229JDC/SO/2016/001/716Symphoricarpos orbiculatus Moench Missouri, United StatesNC72016COLLECTED01/13/2016Access road near Scobee Lake, NE 1/4 of NE 1/4 of Section 32, T64N R16W, approximately 10.5 miles northwest of Kirksville, Adair County.40.30655000, -92.71615200Wild materialPlants approximately 4 feet in height. Fruits red in color. Variation noted in fruits ranging from bright red to dark red in color.1936479Ames 33229
103WLP 1098JDC/CO/2015/030/686Cotinus obovatus Raf. Arkansas, United StatesNAPLANT2015COLLECTED05/20/2015T18N R15W NW 1/4 Sec. 15 and SE 1/4 Sec. 10 Marion County. Hall Mountain area along County Road 6074.36.20574400, -92.56150900239Rocky, very shallow soils. Growing in association with Quercus muehlenbergii, Juniperus virginiana, Acer saccharum, Cercis canadensis, Lindera benzoin, Diospyros virginiana, Silphium terebinthinaceum, Baptisia sp., Rudbeckia sp., and Rhus glabra.Wild material1926260WLP 1098
104NA 82643NA 82643Lonicera sempervirens L. Texas, United StatesNA2015COLLECTED07/20/2014East side of Texas Route 87 approximately 0.52 miles south of Trout Creek, Texas.30.61156000, -93.8050600021Southwest-facing edge of mature woodland in part to full sun; well-drained, seasonally moist soils that are sandy loam; surface has an excellent organic litter layer.1952603NA 82643
105W6 48905MARSB-99Tridens flavus (L.) Hitchc. Virginia, United StatesW6SEED2015Wild material1922891W6 48905
106WLP 1253JDC/HQ/2014/090/592Hydrangea quercifolia W. Bartram Alabama, United StatesNAPLANT2014COLLECTED09/23/2014Alabama: Lawrence County; Near Franklin and Lawrence County line off County Road 303.34.33701600, -87.52906200332 Growing in association with Quercus alba, Quercus montana, Cornus florida, Rhus glabra, Liriodendron tulipifera, Pinus virginiana, Pinus sp., Acer rubrum, and Frangula alnus.Wild materialSome specimens with infructescences averaging 12" in length.1922364WLP 1253
107Ames 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
108Ames 30599JDC/FA/2010/031/301Fraxinus americana L. Kansas, United StatesNC7SEED2010COLLECTED09/13/2010Near Big Sugar Creek watershed, east of Centerville, Linn County.38.21145000, -94.93801000294Upland areas. Variable aspects. Wild material1848894Ames 30599
109WLP 809JDC/CS/2010/033/303Celastrus scandens L. Kansas, United StatesNAFRUIT2010COLLECTED09/14/2010Along Marshall Road, just north of Shaw, Neosho County.37.66917000, -95.31584000295Associated with Cornus drummondii, Juniperus virginiana, Liatris aspera, Maclura pomifera, Prunus serotina, Rhus glabra, and Ulmus.Wild material1848888WLP 809
110Ames 30481APS/GD/2010/001/036Gymnocladus dioicus (L.) K. Koch Missouri, United StatesNC7FRUIT2010COLLECTED02/17/2010Mark Twain Lake Project (Army Corp of Engineers), Mark Twain Lake, T54N R8W SE 1/4 of NW 1/4 of Section 2 and west 1/2 of Sec. 11, Florida Quad, Monroe County.39.49270000, -91.76510000199Northwest-facing bluff; woods.Wild material#106 measured 14.5" d.b.h and 70-80'; #107 measured 9.5" and 70-80'; #108 measured 11" d.b.h. and 60-70'; #109 measured 9.5" d.b.h. and 40-50'; #110 measured 11" d.b.h. at 30-40'; and #111 measured 6" d.b.h. and 30'.1831340Ames 30481
111Ames 30489APS/GD/2010/010/045Gymnocladus dioicus (L.) K. Koch Kentucky, United StatesNC7FRUIT2010COLLECTED02/22/2010Yellowbank Wildlife Management Area, near Lick Run Creek, on Ammons Church Road and slope on Jays Lane, north of Ammons, Breckinridge County.37.96060000, -86.49880000130Northeast-facing slope.Wild material#148 measured 16.5" d.b.h. and 100', #149 measured 14.5" d.b.h. and 90', #150 measured 16" d.b.h. and 90', and #151 measured 18" d.b.h. and 80'.1831348Ames 30489
112Ames 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
113Ames 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
114Ames 30167JDC/PT/2009/061/211Ptelea trifoliata L. Illinois, United StatesNC7SEED2009COLLECTED09/24/2009Rock Cut State Park along Hart Road; SE 1/4 of SE 1/4 of Section 21, T45N, R2E, Rockford North Quad.42.35500000, -89.00083333254Roadside.Wild material1819748Ames 30167
115Ames 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
116Ames 29628JDC/FA/2008/029/099Fraxinus americana L. Missouri, United StatesNC7SEED2008COLLECTED10/06/2008Rudolf Bennitt Conservation Area, NE 1/4 of NE 1/4 of Section 25, T52N, R14W, Renick Quad, Randolph County.39.27527778, -92.43388889256Wild materialOriginal specimens ranged from 6-10 inches d.b.h. and 30-50 feet in height. Reddish-orange fall color more apparent in males.1788183Ames 29628
117Ames 29885174525Cercocarpus montanus Raf. Colorado, United StatesNC7SEED2005COLLECTED08/19/2002Central shortgrass prairie. Jefferson County. Apex Gulch, US Highway 40 at County Road 93. Jefferson County Open Space.39.71361000, -105.217220001982Foothills. Wild materialShrub 1.5-1.8 meters tall. 1673952Ames 29885
118WLP 77025Celastrus scandens L. Iowa, United StatesNA2003COLLECTED09/22/2003Along Gate House Trail, Lacey-Keosauqua State Park, Keosauqua, T68N R10W, S edge of NE 1/4 of NW 1/4, Section 3, Keosauqua Quad, Van Buren County.40.72194444, -91.99861111203Woody invaders to old field setting. 2/3 sunny. Slight slope. Associated with Cornus drummondii, Viburnum lentago, Prunus serotina, Aster pilosus, Rhus glabra, and Rosa multiflora.Wild materialClimbing vine. 1649666WLP 770
119WLP 13329Lonicera reticulata Raf. Iowa, United StatesNAPLANT2003COLLECTED09/14/2003Parking area for ford, South Bear Creek Wildlife Area, Highlandville, T100N R7W, NE 1/4 of NE 1/4, Section 35, Highlandville Quad, Winneshiek County.43.44083333, -91.64722222274Edge of parking area, floodplain. Half sunny. No slope with an eastern aspect. Alluvial soil. Associated with Juglans nigra, Ulmus, Acer negundo, Xanthoxylum, and Rhus glabra.Wild materialOne large, very attractive vine ~14 feet tall, climbing up a Juglans nigra tree. 1649461WLP 1332
120WLP 769NA 73812Celastrus scandens L. Iowa, United StatesNAFRUIT2003COLLECTED09/14/2003Quandahl Road, Bear Creek Wildlife Area, Highlandville, T100N R7W, NE 1/4 of NW 1/4, Section 36, Dorchester Quad, Winneshiek County.43.44055556, -91.62388889268Mostly sunny. Steep slope with a southeastern aspect. Thin soil over limestone with high stoniness, well drained. Associated with Juniperus communis, J. virginiana, Ulmus rubra, Lespedeza capitata, Monarda fistulosa, and Rhus glabra.Wild materialVine to 4 meters tall. 1649454WLP 769