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ACCESSIONPLANT NAMETAXONOMYORIGINGENEBANKIMAGEAVAILABILITYRECEIVEDSOURCE TYPESOURCE DATECOLLECTION SITECOORDINATESELEVATIONHABITATIMPROVEMENT LEVELNARRATIVE
0NA 88149NCBG-313Liquidambar styraciflua L. North Carolina, United StatesNASEED2019Wild material2098409NA 88149
1NA 88152NCBG-320Liquidambar styraciflua L. North Carolina, United StatesNASEED2019Wild material2098412NA 88152
2NA 88034NCBG-430Liquidambar styraciflua L. North Carolina, United StatesNASEED2018Wild material1965947NA 88034
3PI 702725NCBG-428Schizachyrium scoparium (Michx.) Nash Maryland, United StatesS9SEED2019Wild material2098447PI 702725
4PI 702690MARSB-175Chasmanthium laxum (L.) H. O. Yates Delaware, United StatesS9SEED2019Wild material2097507PI 702690
5PI 702691MARSB-322Chasmanthium laxum (L.) H. O. Yates New Jersey, United StatesS9SEED2019Wild material2097574PI 702691
6PI 702692MARSB-332Chasmanthium laxum (L.) H. O. Yates New Jersey, United StatesS9SEED2019Wild material2097581PI 702692
7PI 702695MARSB-502Chasmanthium laxum (L.) H. O. Yates New Jersey, United StatesS9SEED2019Wild material2097639PI 702695
8PI 702709MARSB-655Panicum virgatum L. Delaware, United StatesS9SEED2019Wild material2097673PI 702709
9PI 704826 sosR. pensilvanicus MARSB-285Rubus pensilvanicus Poir. New Jersey, United StatesCORSEED2019Wild material2097556PI 704826 sos
10PI 704854 sosR. cuneifolius MARSB-462Rubus cuneifolius Pursh New Jersey, United StatesCORSEED2019Wild material2097633PI 704854 sos
11PI 710478NCBG-750Chamaecrista fasciculata (Michx.) Greene Virginia, United StatesS9SEED2018Wild material1966043PI 710478
12PI 710480NCBG-700Chamaecrista nictitans (L.) Moench North Carolina, United StatesS9SEED2018Wild material1966014PI 710480
13PI 710499NCBG-752Sesbania exaltata (Raf.) Rydb. North Carolina, United StatesS9SEED2018Wild material1966044PI 710499
14PI 710490MARSB-345Lespedeza capitata Michx. New Jersey, United StatesS9SEED2018Wild material1964765PI 710490
15PI 673986TX-03Rudbeckia grandiflora (Sweet) C. C. Gmel. ex DC. Texas, United StatesOPGC2010COLLECTED05/26/2010Upper West Gulf Coastal Plain. Harrison County. South of Marshall Texas. East on 2625, cross 31, left onto CR 1111, Brad spann road veer right.32.47050000, -94.2159440097Meadow(Maintained ROW under power lines). Land form: Rolling hills. Land Use: Roadside ROW. Geology: Sandstone. Soil Texture: Sandy. Soil Color: Brown.Wild materialErect, clumped, glabrous to 60 cm tall. Flowers numerous, yellow ray florets.1897287PI 673986
16PI 673989TX-11Rudbeckia grandiflora (Sweet) C. C. Gmel. ex DC. Texas, United StatesOPGC2010COLLECTED05/26/2010Upper West Gulf Coastal Plain. Marion County. Smithland Cuttoff Road approx. 1 mile east of SH 43.32.76347200, -94.1815280053Roadside ROW/forest edge(tree farm/harvesting area). Land form: Flat. Land Use: Roadside ROW. Geology: Sandstone. Soil Texture: Sandy. Soil Color: Tan.Wild materialErect, coarse perennial to 125 cm tall; leaves mostly basal; ray flowers yellow and drooping.1897293PI 673989
17PI 673992TX-30Coreopsis lanceolata L. Texas, United StatesOPGC2010COLLECTED05/27/2010Upper West Gulf Coastal Plain. Newton County. Roadside approx. 1.5 miles south of 1416 on SH 87.30.58986100, -93.7943060027Roadside ROW/forest edge. Land form: Flat. Land Use: Roadside ROW. Geology: Sandstone. Soil Texture: Sandy to clay. Soil color: Greyish-brown.Wild materialErect, clumped, glabrous to 70 cm tall. Flowers with yellow ray florets, mostly gone to seed.1897309PI 673992
18PI 653297R. argutus HD-2007-070Rubus argutus Link Mississippi, United StatesCOR2007COLLECTED06/09/2007Marshall County, northwest of Potts Camp off route 178 onto George Mann Road onto Lake Shore Drive at a drainage ditch in the community of Lake Center.34.69310000, -89.36150000120Open area in drainage ditch growing on the perimeter road of a lake. Associated Plants: Rhus typhina, Vitis rotundifolia, Pinus taeda, Salix sp., Lonicera japonica, Liquidambar styraciflua and Acer negundo.Wild materialKim Hummer, Michael Dossett collection from Mississippi.

1730104PI 653297
19PI 657221V. corymbosum ZebulonVaccinium corymbosum L. North Carolina, United StatesCORImage2007COLLECTED06/01/2007Zebulon, Wake County. Near sewer right of way on North Worth Hinton Road (SR 2369).35.82683000, -78.3311000090Organic duff over dark brown sandy soil. Associated with: Liquidambar styraciflua, Acer rubrum, Rhus typhina, Rubus argutus, Pinus palustris and Liriodentdron tulipfera. Near sewer right of way, at edge of dark hardwood forest.Wild materialKim Hummer, Michael Dossett collected from North Carolina.

1730106PI 657221
20PI 657223V. corymbosum HD-2007-016Vaccinium corymbosum L. South Carolina, United StatesCOR2007COLLECTED06/03/2007Northwest of Little Rock, Dillon County. Intersection of SR-57 and McLaurin Lake Circle. Growing in a drainage ditch west side of road.34.50649000, -79.4789200020Flat terrain. Associated with: Smilax, Acer rubrum, Liquidambar styraciflua, Quercus velutina, Sasafras albidum, Lonicera japonica, Pinus palustris and Campsus radicans.Wild materialKim Hummer, Michael Dossett collected from South Carolina. V. corymbosum diploid

1730114PI 657223
21PI 657235V. pallidum Scenic HWY HD 2007-59Vaccinium pallidum Aiton Alabama, United StatesCORImage2007COLLECTED06/08/2007East of Keener, Etwah County, Keener Gap. Woods at intersection of Keener Gap Road and Scenic Highway. On ridge above road.34.15484000, -85.93371000300Soil sandy brown red limestone, with a layer of oak-hickory leaf duff on top. Associated with: Carya, Quercus nigra, Vaccinium stamineum, Liriodendron tulipifera, Liquidambar styraciflua and Acer rubrum.Wild materialKim Hummer, Michael Dossett collected from Alabama.

1730127PI 657235
22PI 664811DE2Actaea racemosa L. Delaware, United StatesNC72005Wild material1698885PI 664811
23NA 891582025RJLSEUS-06Cornus florida L. Alabama, United StatesNA2025COLLECTED10/01/2025Coosa Wildlife Management Area: along the edge of gated dirt road on the west side of Coosa County Road 29, 0.3 kilometers north of Hatchet Creek.32.86402200, -86.33871400108Plants are growing in part sun to shade on dry-mesic slopes above the road cut on the gated dirt road; most likely a road for access for fire control/forest management. The forest is a combination of deciduous and evergreen with evergreens primarily comprised of Pinus taeda. The habitat was quite dry during this time of year. Slope: 5 to 20 percent. Aspect: North. Soils: The primary soil in the area of this collection is classified as Madison-Louisa Series complex, 15 to 30 percent slopes, moderately eroded (MdE2). The Madison Series soils are very deep, well drained soils with medium runoff found on Piedmont uplands in interstream divides, ridges and side slopes. They are comprised of residuum weathered from felsic or intermediate, high-grade metamorphic or igneous rocks high in content of mica. Slopes range from 2 to 60 percent and soil is typically strongly acidic. Louisa Series soils The Louisa Series soils consist of shallow, somewhat excessively drained soils which formed over mica gneiss and schist bedrock. They occur on Piedmont uplands. Slopes are 6 to 80 percent. This soil is moderately acid. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). Geology: The underlying geology of this area is of Precambrian to Paleozoic origin and characterized as Hatchet Creek Group; Pinchoulee Gneiss Formation. It is characterized by medium to fine-grained migmatitic, locally garnetiferous biotite-feldspar gneiss, commonly saturated with granitic pods. (Source: USGS Alabama Geologic Map Data).Wild material2193004NA 89158
24NA 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
25NA 8893124Flam27Rhododendron flammeum (Michx.) Sarg. Georgia, United StatesNA2025COLLECTED09/10/2024DeKalb County: Stone Mountain: Stone Mountain Park along Evergreen Trail by resort, growing within 40 feet of Venable Lake. GPS coordinates a general locality for population and each seed lot for 24Flam27-30 was collected progressively further west).33.79769000, -84.13420000291Dry, somewhat shady forest adjacent to lake, some plants hanging over edge. Primarily close to the water on flat ground, though some on slope. Growing in half shade. Slope: Flat to 30 degrees. Aspect: North.Wild materialNote: Seeds from three different lots collected at the same spot were bulked together in this accession; the lowest field collection number (24Flam27) has been chosen as the primary for this record.2172814NA 88931
26NA 8893324Flam40Agarista populifolia (Lam.) Judd South Carolina, United StatesNA2025COLLECTED09/12/2025Robertville, SC: Gillison Branch Road (plants on both sides of road).32.58673000, -81.1930000031Shady swamp forest with road running between Agarista population. Agarista was the predominant plant throughout. Soggy but solid ground, especially on northern side of road. Growing in 3/4 shade. Slope: Generally flat.Wild materialNote: Two field collections, 24Flam40 and 24Flam41, were combined together in this USNA accession, with the former identifier being used as the primary one.2172816NA 88933
27NA 8894024Flam60Rhododendron flammeum (Michx.) Sarg. South Carolina, United StatesNA2025COLLECTED09/13/2025Savannah River Site, near Tinker Creek. GPS coordinates represent a general location for the population.33.36802000, -81.5497100090Shady forest following Tinker Creek. Seed collected primarily on slopes and banks over the creek. Growing in half shade. Slope: Varying.Wild materialNote: Two field collections, 24Flam60 and 24Flam65, were combined together in this USNA accession, with the former identifier being used as the primary one. The collectors note the possibility that this contains hybrids because the plants were not observed in flower.2172823NA 88940
28NA 88746TXWL2025-039Ilex verticillata (L.) A. Gray Louisiana, United StatesNA2025COLLECTED01/24/2025Kistachie National Forest: Compartment 49, Indian Creek.31.09110000, -93.53333000Slough/baygall area with standing water below a longleaf pine stand.Wild material2171020NA 88746
29NA 88981TXWL2025-031Ilex opaca Aiton Texas, United StatesNA2025COLLECTED01/07/2025South of Jericho community.31.67015000, -94.25641000Western sandy lands; small grove of Ilex opaca in upland position above a baygall. Bare ground cover with Ilex opaca regeneration. Adjacent to a loblolly pine plantation and a new longleaf pine plantation.Wild material2170965NA 88981
30NA 88982TXWL2025-032Ilex opaca Aiton Texas, United StatesNA2025COLLECTED01/07/2025South of Jericho community.31.66973000, -94.25613000Western sandy lands; edge of small grove of Ilex opaca with sun exposure in upland position above a baygall. Bare ground cover with Ilex opaca regeneration. Adjacent to a new longleaf pine plantation located on fireline.Wild material2170966NA 88982
31NA 88983TXWL2025-033Ilex opaca Aiton Texas, United StatesNA2025COLLECTED01/12/2025Adjacent to Toledo Bend reservoir in Huxley Bay community, eastern Shelby County.31.77133000, -93.85094000Low area with heavy duff near reservoir.Wild material2170967NA 88983
32NA 885792024RJLFL-007Ilex myrtifolia Walter Florida, United StatesNA2024COLLECTED11/13/2024Wetlands accessed from Miller Bluff Road.30.62251200, -86.860307008Open, wet areas and woodland edge slightly above permanently wet habitat in part shade to full sun. Slope: 0 percent. Aspect: N/A.Wild material2169916NA 88579
33NA 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
34NA 885842024RJLFL-016Cornus florida L. Florida, United StatesNA2024COLLECTED11/14/2024Both sides of Kennedy Bridge Road approximately 0.27 kilometers west of the junction with Hurricane Lake South Entrance Road.30.93159700, -86.7492800043Mesic to mesic-moist conditions in a mixed and deciduous evergreen forest in part shade. Slope: 5 to 10 percent. Aspect: Various. 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 Dothan Series loamy sand, 5 to 8 percent slopes. 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. Slopes range from 0 to 15 percent. 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. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions).Wild material2169921NA 88584
35NA 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
36NA 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
37NA 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
38NA 885932024RJLNJ-001Ilex glabra (L.) A. Gray New Jersey, United StatesNA2024COLLECTED11/24/2024Mullica Township: Both sides of Duerer Street, approximately 0.37 kilometers southeast of 4th Avenue.39.55885000, -74.6644250021Shade to almost full sun on compacted seasonally moist to temporarily wet areas of a mixed evergreen and deciduous woodland dominated by Pinus rigida. Vegetation of this area is very much defined by small changes in elevation that go from wet to very dry. Ilex glabra remains abundant throughout, though. Slope: N/A. Aspect: N/A. The underlying geology of this area is the Cohansey Formation of middle Miocene origin and comprised of sand, white to yellow with local gravel and clay. It is sometimes locally stained red or orange brown by iron oxides and (or) cemented into large blocks of ironstone. Unweathered clay is typically dark gray, but commonly weathers white where it is interbedded with thin beds of ironstone. Sand is typically medium grained and moderately sorted although it ranges from fine to very coarse grained and from poorly to well sorted. Sand consists of quartz and siliceous rock fragments. Some beds are locally micaceous. Maximum thickness in the map area is about 60 meters; however, thickness is difficult to determine because of the irregular basal contact and extensive post-depositional erosion. (Source: USGS New Jersey Geologic Map Data). The primary soil type in the area of this collection is classified as Mullica Series sandy loam, 0 to 2 percent slopes. These soils are typically coarse-loamy, siliceous, semiactive, and mesic typic humaquepts that are strongly to extremely acidic throughout the profile. The typical solum thickness ranges from 50-150+ cm. These soils are generally considered to be poorly drained. (Source: NRCS Web Soil Survey).Wild material2169930NA 88593
39NA 88479TXWL2024-029Ilex longipes Chapm. ex Trel. Texas, United StatesNA2024COLLECTED11/20/2024Little Cow Creek.31.06221000, -93.79603000Upland position above perennial creek.Wild material2169906NA 88479
40NA 87842TRX241117-08SCIlex opaca Aiton South Carolina, United StatesNA2024COLLECTED11/17/2024Francis Marion National Forest.33.15167000, -79.6025300031Wild material2169895NA 87842
41NA 890882024RM-TK-001Viburnum acerifolium L. Alabama, United StatesNA2024COLLECTED09/19/2024Haines Island Park. Follow Ferry Road to the top of the hill entering the park where a picnic shelter is located. Plants are growing along trails to the north of the picnic shelter.31.72132026, -87.4640891081Plants are growing from part-sun to full shade in the understory of a mixed deciduous and coniferous forest on very dry upland habitat. Slope: 10 to 20 percent. Aspect: North. Geology: The underlying geology of this area is probably of Eocene age and characterized as the Claiborne Group: Tallahatta Formation. It is comprised of white to very light-greenish-gray thin-bedded to massive siliceous claystone; interbedded with thin layers of fossiliferous clay, sandy clay, and glauconitic sand and sandstone. White to light-greenish-gray fine to coarse sand and fine gravel occur at the base of the formation in southwest Alabama (Meridian Sand Member). (Source: USGS Alabama Geologic Map Data). Soils: The area of this occurrence is characterized as Arundel Series Loam, 8 to 35 percent slopes (ArF). The Arundel series consists of moderately deep, well drained, very slowly permeable soils on dissected uplands of the Southern Coastal Plain Major Land Resource Area (MLRA 133A). They formed in marine deposits consisting of acid clays underlain by horizontally bedded sandstone, buhrstone and siltstone. Slopes range from 2 to 60 percent. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). EPA Ecoregion (Level III): Southeastern Plains (65). EPA Ecoregion (Level IV): Buhrstone/Lime Hills (65q).Wild material2169052NA 89088
42NA 890892024RM-TK-002Viburnum acerifolium L. Alabama, United StatesNA2024COLLECTED09/19/2024Woodland slopes around and below the hilltop parking area leading down to the Silver Creek Lake Campground off of Silver Creek Lake Road.31.66612294, -87.5756986049Plants are growing in shade of upland dry mesic, mature mixed deciduous and evergreen woodland. Generally, the overstory is thinner and there is less leaf litter cover, making the surface soil conditions drier. Slope: 5 to 10 percent. Aspect: Southeast. Geology: The underlying geology of this area is Claiborne Group, Tallahatta Formation, of Eocene origin, with white to very light-greenish-gray thin-bedded to massive siliceous claystone; interbedded with thin layers of fossiliferous clay, sandy clay, and glauconitic sand and sandstone. (Source: USGS Alabama Geologic Map Data). Soils: The primary soil types in the collection area are classified as Arundel-Cantuche Complex soils (15 to 35 percent slopes). The Arundel Series consists of moderately deep, well drained, very slowly permeable soils on dissected uplands of the Southern Coastal Plain. They formed in marine deposits consisting of acid clays underlain by horizontally bedded sandstone, buhrstone and siltstone. These soils are strongly acid. Slopes range from 2 to 60 percent. The Cantuche Series consists of shallow, well drained, moderately permeable soils that formed over horizontally bedded claystone. These soils are on narrow ridgetops and narrow benches on steep side-slopes of dissected landscapes in the Coastal Plain. They are strongly acid. Slopes range from 2 to 35 percent. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). EPA Ecoregion (Level III): Southeastern Plains (65). EPA Ecoregion (Level IV): Buhrstone/Lime Hills (65q).Wild material2169053NA 89089
43NA 890902024RM-TK-003Ilex longipes Chapm. ex Trel. Alabama, United StatesNA2024COLLECTED09/19/2024Woodland slopes around and below the hilltop parking area leading down to the Silver Creek Lake Campground off of Silver Creek Lake Road.31.66612294, -87.5756986039Plants are growing in part-shade to shade of a moist mesic deciduous and evergreen woodland on dry, well-drained soil to an area 1-2 meters above a small seasonally spring-fed creek at 31.664428°, -87.574614°. Slope: 5 to 10 percent. Aspect: Southeast. Geology: The underlying geology of this area is Claiborne Group, Tallahatta Formation, of Eocene origin, with white to very light-greenish-gray thin-bedded to massive siliceous claystone; interbedded with thin layers of fossiliferous clay, sandy clay, and glauconitic sand and sandstone. (Source: USGS Alabama Geologic Map Data). Soils: The primary soil types in the collection area are classified as Arundel-Cantuche Complex soils (15 to 35 percent slopes). The Arundel Series consists of moderately deep, well drained, very slowly permeable soils on dissected uplands of the Southern Coastal Plain. They formed in marine deposits consisting of acid clays underlain by horizontally bedded sandstone, buhrstone and siltstone. These soils are strongly acid. Slopes range from 2 to 60 percent. The Cantuche Series consists of shallow, well drained, moderately permeable soils that formed over horizontally bedded claystone. These soils are on narrow ridgetops and narrow benches on steep side-slopes of dissected landscapes in the Coastal Plain. They are strongly acid. Slopes range from 2 to 35 percent. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). EPA Ecoregion (Level III): Southeastern Plains (65). EPA Ecoregion (Level IV): Buhrstone/Lime Hills (65q).Wild material2169054NA 89090
44NA 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
45NA 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
46NA 88838RJL-RM2023FLAL-012Ilex opaca Aiton Florida, United StatesNA2023COLLECTED12/08/2023North side of Sid Hayes Road approximately 65 m southeast of the junction with Watson Road.30.83277400, -87.2432450032Growing in shade, part shade and light shade in dry mesic to moist, occasionally wet, habitats along the edge of the road and in the woodland interior. This species is remarkably adaptable. The only drawback to the range of habitats is that in deep shade, very few fruit can be found, presumably because there is far less flower production and/or fewer pollinators. Slope: 0 to 3 percent. Aspect: South. 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 surface soil profile of this area is Dothan Series fine sandy loam soils (5 to 8 percent slopes). 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. (Source: NRCS Web Soil Survey.)Wild material2165668NA 88838
47NA 88839RJL-RM2023FLAL-013Rhododendron austrinum (Small) Rehder Florida, United StatesNA2023COLLECTED12/10/2023Along the Florida Trail, accessed from Miller Bluff Road. Plants were found infrequently but regularly along the trail over 1 kilometer or more.30.61991500, -86.865210004Plants are growing primarily in shade to dappled shade, above a small stream in moist mesic conditions along and below the Florida Trail. The mixed evergreen and deciduous forest is quite diverse with an excellent litter layer. Slope: 2 to 8 percent. Aspect: South. 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: NRCS Web Soil Survey.)Wild material2165669NA 88839
48NA 88841RJL-RM2023FLAL-015Pinckneya bracteata (W. Bartram) Raf. Florida, United StatesNA2023COLLECTED12/11/2023West side of Marville Drive on the edge of the woodlands just a few hundred feet south of Fairway Drive.30.60665300, -85.3257220079Plants are growing on the edge of a wetland acid habitat in the transitional zone between the obligate and facultative zones. They are growing in part-shade to shade with lower woody competition due to the moist conditions. Slope: N/A. Aspect: N/A. 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 surface soil profile of this area is primarily Pamlico-Pantego-Rutlege Association. The Pamlico series consists of very poorly drained soils that formed in decomposed organic material underlain by dominantly sandy sediment. The soils are on nearly level flood plains, bays, and depressions of the Coastal Plain. Slopes are less than 1 percent. Pamlico soils have 0.4-1.3 meters of organic material over dominantly sandy sediments. Reaction is extremely in the organic layers and ranges from extremely acid to strongly acid in the underlying mineral layers. The Pantego series consists of very deep, very poorly drained, moderately permeable soils that formed in thick loamy sediments on the Southern Coastal Plain and Atlantic Coast Flatwoods. Slopes are less than 2 percent. This soil is strongly acid. The Rutlege series comprises very deep, very poorly drained persistently wet soils on flats, depressions and floodplains where shallow ponding is common. They are of marine or fluvial sediment origin. Thickness of these loamy sandy soils is greater than 1.5 meters and a reaction from extremely acid to strongly acid. (Source: NRCS Web Soil Survey.)Wild material2165671NA 88841
49NA 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
50NA 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
51NA 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
52WLP 3377TXWL2023-024Viburnum dentatum L. Texas, United StatesNA2023COLLECTED12/13/2023Roadside between Big Cow Creek and Hardy Cemetery.31.03548900, -93.85086800Roadside; mesic, mixed hardwood/pine forest.Wild material2165656WLP 3377
53NA 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
54NA 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
55NA 88812TXWL2023-018Ilex ambigua Torr. Texas, United StatesNA2023COLLECTED12/05/2023Davy Crockett National Forest: Forest Service Road 526 roadside.31.49017400, -95.22343300Roadside. Shortleaf mixed upland hardwood forest; dry-mesic.Wild material2165615NA 88812
56NA 88814TXWL2023-021Ilex ambigua Torr. Texas, United StatesNA2023COLLECTED12/09/2023Roadside between Big Cow Creek and Hardy Cemetery.31.03548900, -93.85086800Roadside; mesic, mixed hardwood/pine forest.Wild material2165618NA 88814
57NA 88815TXWL2023-022Ilex opaca Aiton Texas, United StatesNA2023COLLECTED12/10/2023Angelina National Forest: Upland Island Wilderness Area: Neches River bottom.31.03919400, -94.37937900Bottomland hardwood forest.Wild material2165619NA 88815
58NA 88816TXWL2023-023Ilex decidua Walter Texas, United StatesNA2023COLLECTED12/10/2023Angelina National Forest: Upland Island Wilderness Area: Neches River bottom.31.03478500, -94.38286600Bottomland hardwood forest.Wild material2165620NA 88816
59NA 88800TXWL2023-015Ilex longipes Chapm. ex Trel. Texas, United StatesNA2023COLLECTED11/15/2023Sabine National Forest: Compartment 65 along County Road 131 near White Rock, Texas.31.55793500, -94.01980900Upland; mixed hardwood and pine; sandy soil; rocky outcrops.Wild material2159157NA 88800
60NA 88690RJL2023NJ-003Ilex verticillata (L.) A. Gray New Jersey, United StatesNA2023COLLECTED11/10/2023Franklin Township: Piney Hollow Preservation Area (the site is owned by Franklin Township). This species was found below the dam at the far end of McCarthys Lakes. Plants accessed by foot along trails throughout property.39.57407200, -74.9251860028Plants growing in part-shade to sun of the moist to saturated areas below the McCarthys Lakes dam in the wetlands associated with the New Squankum Branch. The area appears to be inundated year-round with plants growing on low mounds surrounded by obligate wetland species. Slope: N/A. Aspect: N/A. The underlying geology of this area is of Middle Miocene, Serravallian origin and characterized as an Cohansey Formation. It is comprised of sand, white to yellow with local gravel and clay. Locally stained red or orange brown by iron oxides and (or) cemented into large blocks of ironstone. Unweathered clay is typically dark gray, but commonly weathers white where interbedded with thin beds of ironstone. Unit is a complex of interfingering marine and nonmarine facies. Sand is typically medium grained and moderately sorted although it ranges from fine to very coarse grained and from poorly to well sorted. Sand consists of quartz and siliceous rock fragments. Some beds are locally micaceous. In general, the sand is crossbedded, although the style of crossbedding varies significantly with the paleoenvironment. Trough crossbedding predominates, especially in the nonmarine channel fill deposits, and the scale of the crossbeds varies from small to large. Maximum thickness in the map area is about 60 m; however, thickness is difficult to determine because of the irregular basal contact and extensive post-depositional erosion. There is as much as 18 m of relief along the basal contact. The basal contact is sharp, undulatory, and directly overlain by a thin gravel bed. The Cohansey Formation unconformably overlies the Kirkwood Formation and is found in channels cut down into the Kirkwood. Where the Kirkwood consists of sandy, light-colored sediments, the basal contact of the Cohansey is drawn below crossbedded sediments. Where the Kirkwood consists of dark-colored silty beds, the basal contact is drawn between light-colored Cohansey sediments and the underlying dark-colored sediments. The Cohansey was markedly thinned because of erosion prior to deposition of overlying units in the western and southern parts of the southern sheet. The unit has been extensively eroded and stripped from large areas of the New Jersey Coastal Plain, particularly in the central sheet where outliers are common. In spite of its widespread nature, the Cohansey is poorly exposed because of its loose sandy composition, which causes it to erode easily. (Source: USGS New Jersey Geologic Map Data.) The primary soil type in the collection area is classified as Manahawkin Series muck, 0 to 2 percent slopes, frequently flooded, Northern Coastal Plain. Manahawkin Series soils are very deep, very poorly drained soils that are sandy or sandy-skeletal, siliceous, dysic, mesic Terric Haplosaprists high in organic deposits that are found in lake basins, back swamps, floodplains, and freshwater channels. The soils are classified in the dysic reaction class because pH in water dominantly ranges from 4.5 to 5.0. The zone from the soil surface to a depth of 200 cm is continuously saturated (endosaturation). The upper strata of Manahawkin Series from 0 to 76 cm is black broken face and rubbed muck; 10 percent fibers, less than 2 percent rubbed; moderate medium granular structure; mat of many fine roots; identifiable material is primarily herbaceous with a trace of woody fragments; 85-95 percent organic matter; extremely acid. Lower strata to 200 cm are gray sand, single grained and loose; strongly acid. (Source: NRCS Web Soil Survey.)Wild material2159118NA 88690
61NA 88691RJL2023NJ-004Ilex laevigata (Pursh) A. Gray New Jersey, United StatesNA2023COLLECTED11/10/2023Franklin Township: Piney Hollow Preservation Area (the site is owned by Franklin Township). This species was found below the dam at the far end of McCarthys Lakes. Plants accessed by foot along trails throughout property.39.57404200, -74.9252370028Plants growing in part-shade to sun of the moist to saturated areas below the McCarthys Lakes dam in the wetlands associated with the New Squankum Branch. The area appears to be inundated year-round with plants growing on low mounds surrounded by obligate wetland species. Slope: N/A. Aspect: N/A. The underlying geology of this area is of Middle Miocene, Serravallian origin and characterized as an Cohansey Formation. It is comprised of sand, white to yellow with local gravel and clay. Locally stained red or orange brown by iron oxides and (or) cemented into large blocks of ironstone. Unweathered clay is typically dark gray, but commonly weathers white where interbedded with thin beds of ironstone. Unit is a complex of interfingering marine and nonmarine facies. Sand is typically medium grained and moderately sorted although it ranges from fine to very coarse grained and from poorly to well sorted. Sand consists of quartz and siliceous rock fragments. Some beds are locally micaceous. In general, the sand is crossbedded, although the style of crossbedding varies significantly with the paleoenvironment. Trough crossbedding predominates, especially in the nonmarine channel fill deposits, and the scale of the crossbeds varies from small to large. Maximum thickness in the map area is about 60 m; however, thickness is difficult to determine because of the irregular basal contact and extensive post-depositional erosion. There is as much as 18 m of relief along the basal contact. The basal contact is sharp, undulatory, and directly overlain by a thin gravel bed. The Cohansey Formation unconformably overlies the Kirkwood Formation and is found in channels cut down into the Kirkwood. Where the Kirkwood consists of sandy, light-colored sediments, the basal contact of the Cohansey is drawn below crossbedded sediments. Where the Kirkwood consists of dark-colored silty beds, the basal contact is drawn between light-colored Cohansey sediments and the underlying dark-colored sediments. The Cohansey was markedly thinned because of erosion prior to deposition of overlying units in the western and southern parts of the southern sheet. The unit has been extensively eroded and stripped from large areas of the New Jersey Coastal Plain, particularly in the central sheet where outliers are common. In spite of its widespread nature, the Cohansey is poorly exposed because of its loose sandy composition, which causes it to erode easily. (Source: USGS New Jersey Geologic Map Data.) The primary soil type in the collection area is classified as Manahawkin Series muck, 0 to 2 percent slopes, frequently flooded, Northern Coastal Plain. Manahawkin Series soils are very deep, very poorly drained soils that are sandy or sandy-skeletal, siliceous, dysic, mesic Terric Haplosaprists high in organic deposits that are found in lake basins, back swamps, floodplains, and freshwater channels. The soils are classified in the dysic reaction class because pH in water dominantly ranges from 4.5 to 5.0. The zone from the soil surface to a depth of 200 cm is continuously saturated (endosaturation). The upper strata of Manahawkin Series from 0 to 76 cm is black broken face and rubbed muck; 10 percent fibers, less than 2 percent rubbed; moderate medium granular structure; mat of many fine roots; identifiable material is primarily herbaceous with a trace of woody fragments; 85-95 percent organic matter; extremely acid. Lower strata to 200 cm are gray sand, single grained and loose; strongly acid. (Source: NRCS Web Soil Survey.)Wild material2159119NA 88691
62NA 88692RJL2023NJ-005Ilex opaca Aiton New Jersey, United StatesNA2023COLLECTED11/10/2023Franklin Township: Piney Hollow Preservation Area (the site is owned by Franklin Township). This species was found on as well as below the dam at the far end of McCarthys Lakes. Plants accessed by foot along trails throughout property.39.57423200, -74.9252560029Plants growing in part-shade to sun of the moist to saturated areas below the McCarthys Lakes dam in the wetlands associated with the New Squankum Branch. Plants were also found growing on the slopes of the dam in well-drained mesic to dry-mesic conditions. This species is clearly adaptable to a variety of conditions. Slope: 0 to 15 percent. Aspect: East. Elevation: 28 to 30 meters. NOTE: In addition to the soil type described below, this species was also growing on the slopes of a constructed earthen dam of unknown soil origin. The underlying geology of this area is of Middle Miocene, Serravallian origin and characterized as an Cohansey Formation. It is comprised of sand, white to yellow with local gravel and clay. Locally stained red or orange brown by iron oxides and (or) cemented into large blocks of ironstone. Unweathered clay is typically dark gray, but commonly weathers white where interbedded with thin beds of ironstone. Unit is a complex of interfingering marine and nonmarine facies. Sand is typically medium grained and moderately sorted although it ranges from fine to very coarse grained and from poorly to well sorted. Sand consists of quartz and siliceous rock fragments. Some beds are locally micaceous. In general, the sand is crossbedded, although the style of crossbedding varies significantly with the paleoenvironment. Trough crossbedding predominates, especially in the nonmarine channel fill deposits, and the scale of the crossbeds varies from small to large. Maximum thickness in the map area is about 60 m; however, thickness is difficult to determine because of the irregular basal contact and extensive post-depositional erosion. There is as much as 18 m of relief along the basal contact. The basal contact is sharp, undulatory, and directly overlain by a thin gravel bed. The Cohansey Formation unconformably overlies the Kirkwood Formation and is found in channels cut down into the Kirkwood. Where the Kirkwood consists of sandy, light-colored sediments, the basal contact of the Cohansey is drawn below crossbedded sediments. Where the Kirkwood consists of dark-colored silty beds, the basal contact is drawn between light-colored Cohansey sediments and the underlying dark-colored sediments. The Cohansey was markedly thinned because of erosion prior to deposition of overlying units in the western and southern parts of the southern sheet. The unit has been extensively eroded and stripped from large areas of the New Jersey Coastal Plain, particularly in the central sheet where outliers are common. In spite of its widespread nature, the Cohansey is poorly exposed because of its loose sandy composition, which causes it to erode easily. (Source: USGS New Jersey Geologic Map Data.) The primary soil type in the collection area is classified as Manahawkin Series muck, 0 to 2 percent slopes, frequently flooded, Northern Coastal Plain. Manahawkin Series soils are very deep, very poorly drained soils that are sandy or sandy-skeletal, siliceous, dysic, mesic Terric Haplosaprists high in organic deposits that are found in lake basins, back swamps, floodplains, and freshwater channels. The soils are classified in the dysic reaction class because pH in water dominantly ranges from 4.5 to 5.0. The zone from the soil surface to a depth of 200 cm is continuously saturated (endosaturation). The upper strata of Manahawkin Series from 0 to 76 cm is black broken face and rubbed muck; 10 percent fibers, less than 2 percent rubbed; moderate medium granular structure; mat of many fine roots; identifiable material is primarily herbaceous with a trace of woody fragments; 85-95 percent organic matter; extremely acid. Lower strata to 200 cm are gray sand, single grained and loose; strongly acid. (Source: NRCS Web Soil Survey.)Wild material2159120NA 88692
63NA 88693RJL2023NJ-006Clethra alnifolia L. New Jersey, United StatesNA2023COLLECTED11/10/2023Franklin Township: Piney Hollow Preservation Area (the site is owned by Franklin Township). Plants accessed by foot along trails throughout property.39.57319800, -74.9290890029Plants growing in shade to part-shade over a wide range of habitats from mesic to mesic-dry as well as moist to wetland habitats. The woodlands are mostly deciduous, but also include occasional pine overstory. Slope: N/A. Aspect: N/A. The underlying geology of this area is of Middle Miocene, Serravallian origin and characterized as an Cohansey Formation. It is comprised of sand, white to yellow with local gravel and clay. Locally stained red or orange brown by iron oxides and (or) cemented into large blocks of ironstone. Unweathered clay is typically dark gray, but commonly weathers white where interbedded with thin beds of ironstone. Unit is a complex of interfingering marine and nonmarine facies. Sand is typically medium grained and moderately sorted although it ranges from fine to very coarse grained and from poorly to well sorted. Sand consists of quartz and siliceous rock fragments. Some beds are locally micaceous. In general, the sand is crossbedded, although the style of crossbedding varies significantly with the paleoenvironment. Trough crossbedding predominates, especially in the nonmarine channel fill deposits, and the scale of the crossbeds varies from small to large. Maximum thickness in the map area is about 60 m; however, thickness is difficult to determine because of the irregular basal contact and extensive post-depositional erosion. There is as much as 18 m of relief along the basal contact. The basal contact is sharp, undulatory, and directly overlain by a thin gravel bed. The Cohansey Formation unconformably overlies the Kirkwood Formation and is found in channels cut down into the Kirkwood. Where the Kirkwood consists of sandy, light-colored sediments, the basal contact of the Cohansey is drawn below crossbedded sediments. Where the Kirkwood consists of dark-colored silty beds, the basal contact is drawn between light-colored Cohansey sediments and the underlying dark-colored sediments. The Cohansey was markedly thinned because of erosion prior to deposition of overlying units in the western and southern parts of the southern sheet. The unit has been extensively eroded and stripped from large areas of the New Jersey Coastal Plain, particularly in the central sheet where outliers are common. In spite of its widespread nature, the Cohansey is poorly exposed because of its loose sandy composition, which causes it to erode easily. (Source: USGS New Jersey Geologic Map Data.) The primary soil types in the area of this collection is classified as Atsion sand, 0 to 2 percent slopes, Northern Tidewater Area and Downer loamy sand, 0 to 5 percent slopes, Northern Coastal Plain. Atsion Series soils are very deep, poorly drained with moderate to rapid permeability above 70 cm and slower beneath. They are classified as sandy, siliceous, mesic Aeric Alaquods. The upper stratum from 0 to 25 cm is dark gray sand, dry, single grained and lose with many fine roots. It is extremely acid. Lower strata are light gray to dark brown with small percentages of rounded quartzose pebbles and are extremely acid. Downer Series soils are very deep, well-drained soils that are coarse-loamy, siliceous, semiactive, mesic Typic Hapludults. The upper stratum of Downer Series from 0 to 25 cm is dark grayish brown, brown loamy sand that is dry with weak fine granular structure. It is very friable and strongly acid. Lower strata from 25 to 76 cm are yellowish brown single grain, loose loamy sand with few extremely weakly cemented masses of oxidized iron in the lower part. This layer is very strongly acid. (Source: NRCS Web Soil Survey.)Wild material2159121NA 88693
64NA 88694RJL2023NJ-007Spiraea tomentosa L. New Jersey, United StatesNA2023COLLECTED11/10/2023Franklin Township: Piney Hollow Preservation Area (the site is owned by Franklin Township). Plants accessed by foot along trails throughout property.39.57318200, -74.9267370028Plants growing in part-shade to sun along the edges of McCarthys Lakes in moist-mesic to wet areas dominated by herbaceous plants. Slope: N/A. Aspect: N/A.Wild material2159122NA 88694
65NA 88695RJL2023NJ-008Aronia arbutifolia (L.) Pers. New Jersey, United StatesNA2023COLLECTED11/10/2023Franklin Township: Piney Hollow Preservation Area (the site is owned by Franklin Township). Plants accessed by foot along trails throughout property.39.57262400, -74.9260690028Plants growing in part-shade to sun along the edges of McCarthys Lakes and in the understory of a mixed deciduous and evergreen forest in moist-mesic to wet conditions. Slope: N/A. Aspect: N/A.Wild material2159123NA 88695
66NA 88697RJL2023NCSC-002Ilex amelanchier M. A. Curtis ex Chapm. North Carolina, United StatesNA2023COLLECTED11/12/2023Goose Pond Bay (Nature Conservancy-owned site): wetlands on the south side of McNeil Road approximately 0.64 kilometers west of junction with McIntosh Road.34.88254100, -79.0991570060Plants are growing in part-shade to sun of a Carolina Bay habitat with seasonally moist to wet, acidic conditions. Slope: N/A. Aspect: N/A. The underlying geology of this area is of Cretaceous origin and characterized as Black Creek Formation. The formation is comprised of clay that is gray to black and lignitic. It contains thin beds and laminae of fine-grained micaceous sand and thick lenses of cross-bedded sand. This formation has glauconitic, fossiliferous clayey sand lenses in the upper part. (Source: USGS North Carolina Geologic Map Data.) The primary soil type in the collection area is classified as McColl loam soil. The McColl Series consists of poorly drained, slowly permeable soils that are shallow or moderately deep to a fragipan and very deep to bedrock. They formed in loamy sediments in oval depressions on the Coastal Plain. The soils are nearly level or concave. Runoff is frequently ponded. Slopes are less than 2 percent. These soils are strongly acid. (Source: NRCS Web Soil Survey.)Wild material2159125NA 88697
67NA 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
68NA 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
69NA 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
70NA 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
71NA 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
72NA 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
73NA 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
74NA 88716RJL2023NCSC-021Ilex myrtifolia Walter South Carolina, United StatesNA2023COLLECTED11/14/2023Francis Marion National Forest: plants growing in a pond cypress-water tupelo swamp on the west side of Thompson Branch Road just south of the junction with Round Pond Road B.33.15167800, -79.6025370031Plants are growing in part-shade to shade as understory trees among the pond cypress-water tupelo forest throughout the acid swamp which is seasonally inundated. The overstory is largely deciduous and comprised of pond cypress and water tupelo, while the understory is a mix of evergreen and deciduous broadleaved shrubs and understory trees. 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 Pickney Series loamy fine sand. The Pickney Series consists of very deep, very poorly drained, persistently wet, permeable soils that formed from marine or fluvial sediments. Slopes range from 0 to 2 percent. The upper strata soil, 0-75 cm, is black loamy fine sand that is very friable and extremely acid. The lower strata, 75-120 cm is dark gray fine sand with occasional white mottling, loose, and moderately acid. (Source: NRCS Web Soil Survey.)Wild material2159144NA 88716
75NA 88717RJL2023NCSC-022Ilex opaca Aiton South Carolina, United StatesNA2023COLLECTED11/14/2023Francis Marion National Forest: plants growing in a pond cypress-water tupelo swamp on the west side of Thompson Branch Road just south of the junction with Round Pond Road B.33.15161300, -79.6021790022Plants are growing in part-shade to shade as understory trees among the pond cypress-water tupelo forest, mostly along the edges of the acid swamp which is seasonally inundated. The overstory is largely deciduous and comprised of pond cypress and water tupelo, while the understory is a mix of evergreen and deciduous broadleaved shrubs and understory trees. 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 Pickney Series loamy fine sand. The Pickney Series consists of very deep, very poorly drained, persistently wet, permeable soils that formed from marine or fluvial sediments. Slopes range from 0 to 2 percent. The upper strata soil, 0-75 cm, is black loamy fine sand that is very friable and extremely acid. The lower strata, 75-120 cm is dark gray fine sand with occasional white mottling, loose, and moderately acid. (Source: NRCS Web Soil Survey.)Wild material2159145NA 88717
76NA 88718RJL2023NCSC-023Ilex decidua Walter South Carolina, United StatesNA2023COLLECTED11/15/2023Waccamaw National Wildlife Refuge: U.S. Highway 701, Yauhannah Landing on the east side of the Great Pee Dee River. Plants growing in low woods on the north side of the landing.33.66208900, -79.153050002Plants growing in shade to part-shade of a moist to wet woodland habitat that is mostly deciduous and evergreen. Portions of the woodland have depressions with year-round standing water. Slope: N/A. Aspect: N/A. The underlying geology of this area is of Quaternary origin and characterized as Alluvial Valley Swamp. This formation is unconformable on all underlying units. It is composed of fluvial sand and gravel at base, grading upwards into fine sands and silts, and local occasional peat. May be overrun with recent sediments from forest cutting and agriculture. (Source: USGS South Carolina Geologic Map Data.) The primary soil type in this collection area is classified as Johnston Series loam. 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 stratum to 1.75 m is dark gray, loamy fine sand, single grained, loose and very strongly acid. (Source: NRCS Web Soil Survey.)Wild material2159146NA 88718
77NA 88668TXWL2023-011Amorpha paniculata Torr. & A. Gray Texas, United StatesNA2023COLLECTED10/02/2023Angelina National Forest: Forest Service Road 302A roadside [Note: GPS coordinates are west of FS Road 302A, closer to County Road 348B.]31.09190000, -94.29072400Roadside.Wild material2159043NA 88668
78NA 88660TJK2023FL-014Rhododendron austrinum (Small) Rehder Florida, United StatesNA2023COLLECTED09/15/2023Lower Yellow River, Grimes Lake.30.61930000, -86.814900003Elevation: 13 feet. Slope: 0 percent. Aspect: West-southwest.Wild material2158794NA 88660
79NA 88663TJK2023FL-017Rhododendron austrinum (Small) Rehder Florida, United StatesNA2023COLLECTED09/17/2023Lower Yellow River, below the Old Land Place.30.55513000, -86.946590000An area with very nice Pink R. austrinum. Elevation: 0. Slope: 0 percent. Aspect: South-southwest.Wild material2158797NA 88663
80NA 88628KY23-031Rhododendron arborescens (Pursh) Torr. Kentucky, United StatesNA2023COLLECTED09/11/2023Daniel Boone National Forest: Bee Rock Loop Trail along Rockcastle River.37.03497974, -84.30580649229Riverscour grassland, edge of river, river scour/boulder pile. Elevation: 750 feet. Aspect: Southeast.Wild material2158720NA 88628
81NA 88630KY23-033Rhododendron periclymenoides (Michx.) Shinners Kentucky, United StatesNA2023COLLECTED09/11/2023Daniel Boone National Forest: Bee Rock Loop Trail along Rockcastle River.37.03537000, -84.30551000229Riverscour grassland, edge of river, river scour/boulder pile. Elevation: 750 feet. Aspect: Southeast.Wild materialInitial identification: Rhododendron periclymenoides aff. 2158722NA 88630
82NA 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
83NA 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
84NA 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
85NA 88644KY23-047Stewartia ovata (Cav.) Weath. Kentucky, United StatesNA2023COLLECTED09/12/2023Cumberland Falls Trail #2.36.83847000, -84.33115000271Elevation: 889 feet. Aspect: South.Wild material2158736NA 88644
86WLP 3214TXWL2023-002Stewartia malacodendron L. Texas, United StatesNA2023COLLECTED08/27/2023Little Cow Creek.31.06090300, -93.79570300Mesic mixed hardwood-pine forest adjacent to riparian area. Some blowdown evident.Wild material2158758WLP 3214
87WLP 3215TXWL2023-003Stewartia malacodendron L. Texas, United StatesNA2023COLLECTED08/27/2023Little Cow Creek.31.06228800, -93.79734300Mesic mixed hardwood-pine forest adjacent to riparian area. Some blowdown evident.Wild material2158759WLP 3215
88WLP 3345AS/SG/2023/025/235Styrax grandifolius Aiton Arkansas, United StatesNAFLOWER2023COLLECTED08/27/2023Ouachita National Forest - Winona Wildlife Management Area/South Fourche Botanical Area. Approximately 20 miles southwest of Danville, along County Road 362, east of Scenic Highway 7. T3N R20W Sec. 23.34.89619000, -93.10769400275Uplands and on bluffs; understory of pine-hardwood forest.Wild materialPlants in nature are large, clonally spreading colonies to 20 feet in height and similar width. Peak bloom occurred the last week of April (2023).2158786WLP 3345
89WLP 3140TJK2023AL-004Viburnum acerifolium L. Alabama, United StatesNA2023COLLECTED08/15/2023Haines Island Park; overlooks the Alabama River.31.72057000, -87.4654300086Beautiful Pine-Oak forest sits atop the Buhrstone Questa, an escarpment that rises over 350 feet. Southern Red Hills Region. Slope: 10%. Aspect: North. Elevation recorded as 281 feet.Wild materialWLPGR contract collection.2158472WLP 3140
90WLP 3138TJK2023AL-002Hamamelis virginiana L. Alabama, United StatesNA2023COLLECTED08/15/2023Haines Island Park; overlooks the Alabama River.31.72074000, -87.4636200094Beautiful Pine-Oak forest sits atop the Buhrstone Questa, an escarpment that rises over 350 feet. Southern Red Hills Region. Slope: 12%. Aspect: West. Elevation recorded as 308 feet.Wild materialWLPGR contract collection.2158470WLP 3138
91WLP 3137TJK2023AL-001Cornus alternifolia L. f. Alabama, United StatesNA2023COLLECTED08/15/2023Claiborne Bluffs, above the Alabama River.31.54883000, -87.5141700016Slope: 35%. Aspect: West-northwest. Elevation recorded as 52 feet.Wild materialWLPGR contract collection.2158469WLP 3137
92NA 89008WLP 3120Morus rubra L. Kentucky, United StatesNA2023COLLECTED06/05/2023Swan Pond Bottom. Riparian buffer and historic floodplain of Cumberland River, approximately 4 river miles downstream of Wolf Creek Dam.36.90259500, -85.13557900Riparian buffer and historic river floodplain. Slope: <5%. Aspect: North.Wild material2158092NA 89008
93NA 88599RJL2023NC-001Ilex decidua Walter North Carolina, United StatesNA2023COLLECTED02/18/2023Plants growing along a fenceline on a hillside about 10 meters from Interstate 85 (south bound) and approximately 0.65 kilometers south of the North Carolina-Virginia border.36.53904800, -78.1882250086The plant was growing on the upper shoulder of a slope about 7 meters above the highway in part-shade to sun of an upland, well-drained, dry mesic somewhat disturbed site on the fenceline boundary of Interstate 85 (south bound). The area was originally cleared of all vegetation and now, many years later, native and non-native plant species have aggressively recolonized the area. This early successional habitat is dominated by Juniperus virginiana and Liquidambar styraciflua, as well as, non-native species such as Ligustrum sinense, Lonicera japonica, and Ailanthus altissima. The underlying geology of this area is of Permian/Pennsylvanian origin and characterized as the Granitic Rock Formation. It is characterized by megacrystic to equigranular components and includs Castalia and Wilton intrusives.Wild material2141480NA 88599
94WLP 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
95WLP 2795RJL2023NJ-001Rhododendron atlanticum (Ashe) Rehder New Jersey, United StatesNA2023COLLECTED01/16/2023Plants growing in woodlands on the south side of a powerline right-of-way approximately 0.72 kilometers southwest of Indian Trail Road. The site was accessed by foot. Plants are infrequent at this site and considered rare in New Jersey. 39.05653200, -74.874825005Plants growing in shade to part-shade of a dry woodland habitat that is mostly deciduous. Nearby, as the elevation changes slightly, there is more abundant soil moisture, becoming a bit more mesic. Soils: The underlying geology of this area is of Upper Pliocene origin and characterized as an Unnamed Formation at Cape May. It is comprised of interbedded gravel, sand, and clay, massive to thickly-bedded. This is an informal unit described from a core hole at the Cape May Airport. The lower 18.3 meters consists of interbedded gravel; medium- to very coarse grained, poorly sorted sand; and thin to thick beds of medium- to dark-gray, very woody clay. Gravel clasts are typically less than 0.64 mm in diameter. The upper 12.2 meters consists of a thick-bedded, medium-gray, extensively bioturbated clay-silt, which is overlain by an extensively burrowed, fine- to medium-grained glauconitic (about 5 percent) quartz sand. Quartz and siliceous rock fragments compose most sand grains. Feldspar is present in most samples but usually constitutes less than 10 percent of the sand fraction. No calcareous macrofossils were found in the burrowed intervals. This unit is known only to occur on the Cape May peninsula where it lies within a large channel. The unit is about 60 m in maximum thickness. The contact with the underlying Belleplain Member of the Kirkwood Formation is sharp and unconformable; a basal gravel bed as much as 1 m thick is present along the contact. The pollen assemblage in the lower part of the unit is dominated by pine and oak with somewhat lesser amounts of hickory and basswood. Spruce, hemlock, beech, alder, and black gum are minor constituents. Traces of fir, willow, birch, and sweet gum are present, as is exotic Engelhardia. The non-arboreal pollen are a Multisia-type composite of the present-day Andean provenance which indicate an exotic cool climate. The lower assemblage suggests a cool-temperate climatic regimen. The pollen assemblage in the upper beds is dominated by oak and hickory with minor amounts of basswood, sweet gum, pine, and Multisia-type composite. Traces of cedar, willow, birch, alder, grass, and Sphagnum spores also are present. This assemblage probably represents a temperate climatic regimen (Les Sirkin, Adelphi University, written commun., 1991). The low percentage of exotic species is characteristic of the late Pliocene, and therefore, the unnamed unit at Cape May could be equivalent to the Beaverdam Formation of the Delmarva Peninsula of Delaware, Maryland, and Virginia. Source: USGS New Jersey Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=NJTc%3B1) The primary soil type in the area of this collection is classified as Berryland and Mullica soils (0 to 2 percent slopes, occasionally flooded). Berryland Series soils are very deep, very poorly drained soils of the Coastal Plains formed by sandy eolian deposits and/or fluviomarine sediments. Th upper 30 cm of the strata is sandy, dry, very friable and extremely acid. The lower strata to 1.8 meters contains loamy sand coated with organic matter, weakly cemented organ nodules and additional layers of sand occasionally containing rounded quartzose pebbles. The Mullica Series soils are typically coarse-loamy, siliceous, semiactive, and mesic typic humaquepts that are strongly to extremely acidic throughout the profile. The typical solum thickness ranges from 50-150+ cm. These soils are generally considered to be poorly drained. Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)Wild material2141140WLP 2795
96NA 87814RM-TK2022-003Nyssa ogeche W. Bartram ex Marshall Florida, United StatesNA2023COLLECTED09/06/2022Hightower Landing on Holmes Creek, off of Hightower Road. This location is off of Florida State Hwy. 79.30.60539000, -85.765134005Trees growing on the edge of the water along Holmes Creek.
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 primary soil types in the collection area are classified as Rutlege, Pickney and Pamlico soils, frequently flooded. The Rutlege series comprises very deep, very poorly drained persistently wet soils on flats, depressions and floodplains where shallow ponding is common. They are of marine or fluvial sediment origin. Thickness of these loamy sandy soils is greater than 1.5 meters and a reaction from extremely acid to strongly acid. The Pickney Series consists of very deep, very poorly drained soils. Permeability is rapid. These nearly level soils have negligible runoff and were formed by marine or fluvial sediments in the lower coastal plain on flats, depressions, stream terraces, and flood plains. Slopes range from 0 to 2 percent. The soils of this series are loamy fine sand that is very friable and extremely acid in the upper 0-25 cm. The lower strata are similar, while the lower strata from 0.8-2 meters are comprised of fine sand. The Pamlico series consists of very poorly drained soils that formed in decomposed organic material underlain by dominantly sandy sediment. The soils are on nearly level flood plains, bays, and depressions of the Coastal Plain. Slopes are less than 1 percent. Pamlico soils have 0.4-1.3 meters of organic material over dominantly sandy sediments. Reaction is extremely in the organic layers and ranges from extremely acid to strongly acid in the underlying mineral layers.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2140796NA 87814
97NA 88522RM-TK2022-010Viburnum dentatum L. var. scabrellum Torr. & A. Gray Florida, United StatesNA2023COLLECTED10/10/2022Plants growing in woodlands via an unnamed dirt road accessed from Old Ferry Road.30.91880000, -87.2599000043Plants are growing in an upland habitat on the edge of south-facing woodland in part-shade.
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/sgmc-unit.php?unit=FLPSHal%3B0)
The primary soil type in the collection area is classified as Orangeburg sandy loam soil (2 to 5 percent slopes). The Orangeburg Series consists of very deep, well drained, moderately permeable soils on uplands of the Southern Coastal Plain. They formed in loamy and clayey marine sediments. The reaction of all this soil ranges from very strongly acid to strongly acid.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2140803NA 88522
98NA 88534RJLSEUS2022-005Leucothoe axillaris (Lam.) D. Don North Carolina, United StatesNA2023COLLECTED12/06/2022Plants growing in the wetlands and other moist depressions along Scotland Co. Road 1328 in the Sandhills Game Lands. Common at this site This plant is somewhat sporadic in its distribution, but abundant in places where it is found in moist to wet habitats of bottomlands in this area. 34.88545200, -79.4459750071Plants are growing in shade of acid bottomland wet woodlands along streams or adjoining wetlands with constant sub-surface moisture. It prefers areas above the permanently wet conditions and can go through periods of drought.
Soils: The underlying geology of this area is of Cretaceous origin and characterized as Mittendorf Formation. The formation is comprised of sand, sandstone, and mudstone, gray to pale gray with an orange cast, and mottled. Clay balls and iron-cemented concretions are common, beds are laterally discontinuous, and cross-bedding is common.
Source: USGS North Carolina Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=NCKm%3B11)
The primary soil type in the collection area is classified as Paxville loam soil (0 to 1 percent slopes, rarely flooded). The Paxville Series consists of very deep, very poorly drained soils. Permeability is moderate. These nearly level soils formed from marine deposits, fluviomarine deposits, and alluvium. They range from 0 to 2 percent slopes. The frequency of flooding is typically very rare to brief periods. The upper strata, 0-1.2 meters, is comprised of fine sandy loam that is friable, non-sticky and non-plastic; it does contain small amounts clean quartz grains and is strongly acid. Lower strata to a depth of 2.5 meters are similar with fine sandy loam in the upper portions and progressively more sandy loam to fine sand in the deepest strata.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2140763NA 88534
99NA 88536RJLSEUS2022-007Leucothoe axillaris (Lam.) D. Don South Carolina, United StatesNA2023COLLECTED12/07/2022Plants growing along the margin of Sandy Run and its associated wetland on the north side of Paradise Rd. (State Rd. S-15-403). Common at this site and throughout the drainage of Sandy Run and its associated wetland. 32.83900000, -80.8101440027Plants are growing in part-shade to shade of a moist mesic woodland habitat along a small wetland associated with Sandy Run. Plants are located in an area that occasionally floods, but is not permanently wet.
Soils: The underlying geology of this area is of Pliocene origin and characterized as Bear Bluff Formation. This formation is considered one of the older coastal terrace sequences in the Carolinas. Bear Bluff Formation consists of gray to cream, fossiliferous, coarse-grained calcareous sand, and sandy limestone. It is typically 3-40 meters thick.
Source: USGS South Carolina Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=SCTbb%3B1)
The primary soil type in the collection area is classified as Pickney Loamy Sand soils. The Pickney Series consists of very deep, very poorly drained soils. Permeability is rapid. These nearly level soils have negligible runoff and were formed by marine or fluvial sediments in the lower coastal plain on flats, depressions, stream terraces, and flood plains. Slopes range from 0 to 2 percent. The soils of this series are loamy fine sand that is very friable and extremely acid in the upper 0-25 cm. The lower strata are similar, while the lower strata from 0.8-2 meters are comprised of fine sand.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild materialLeucothoe axillaris/fontanesiana2140764NA 88536
100NA 88537RJLSEUS2022-009Rhododendron canescens (Michx.) Sweet South Carolina, United StatesNA2023COLLECTED12/07/2022Plants growing along the upper margin of a small stream and associated wetland on the northwest side of Paradise Rd. (State Rd. S-15-403). Common at this site and throughout the drainage of the stream and associated wetland.32.83868100, -80.8109920028Plants are growing in part-shade to shade of a moist mesic woodland habitat along a small wetland associated with a creek. Plants are located in an area that occasionally floods, but is not permanently wet.
Soils: The underlying geology of this area is of Pliocene origin and characterized as Bear Bluff Formation. This formation is considered one of the older coastal terrace sequences in the Carolinas. Bear Bluff Formation consists of gray to cream, fossiliferous, coarse-grained calcareous sand, and sandy limestone. It is typically 3-4 meters thick.
Source: USGS South Carolina Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=SCTbb%3B1)
The primary soil type in the collection area is classified as Pickney Loamy Sand soils. The Pickney Series consists of very deep, very poorly drained soils. Permeability is rapid. These nearly level soils have negligible runoff and were formed by marine or fluvial sediments in the lower coastal plain on flats, depressions, stream terraces, and flood plains. Slopes range from 0 to 2 percent. The soils of this series are loamy fine sand that is very friable and extremely acid in the upper 0-25 cm. The lower strata are similar, while the lower strata from 0.8-2 meters are comprised of fine sand.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2140765NA 88537
101NA 88540RJLSEUS2022-012Rhododendron austrinum (Small) Rehder Georgia, United StatesNA2023COLLECTED12/09/2022Plants growing along the edge of a moist woodland habitat on the property at the end of the Lavender Lane cul-de-sac adjoining that of Monica Williams, in Albany, Georgia. Infrequent on the woodland edge at this site.31.63812300, -84.1406650064Plants are growing in part-shade of a moist mesic, mostly deciduous, woodland along the upper fringes of seasonally moist to wet drainage area leading to a large pond and wetland habitat further downstream.
Soils: The underlying geology of this area is of Eocene origin and characterized as Ocala Limestone. The Ocala Limestone consists of almost pure limestones with occasional dolomites. It can be subdivided into both lower and upper facies with the lower facies composed of a whitish to cream-colored, fine to medium grained, poorly to moderately hard, fossil rich grainstone and packstone. The upper Ocala is white and somewhat weak and poorly sorted. It is extremely fossil rich grainstone, packstone and wackestone and some chert is common in the upper facies.
Source: USGS Georgia Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=GANu%3B1)
The primary soil types in the collection area are classified as Herod and Muckalee Series soils. The Herod Series consists of poorly drained moderately permeable soils formed in loamy alluvium. These soils are on flood plains of streams in the Coastal Plain. Slopes range from 0 to 2 percent. The Muckalee Series consists of poorly drained moderately permeable soils formed in loamy and sandy alluvium. These soils are on flood plains of streams in the Coastal Plain. Slopes range from 0 to 2 percent.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2140767NA 88540
102NA 88541RJLSEUS2022-013Rhododendron viscosum (L.) Torr. Georgia, United StatesNA2023COLLECTED12/09/2022Plants growing around a pond and associated wetland on the property of Monica Williams north of Albany, Georgia. Common along the edges of the pond and wetland area. 31.63828300, -84.1382700062Plants are growing in part-shade to sun of a wetland habitat on the edge of a large pond. The habitat is comprised of numerous hummocks where this species grows, slightly above the permanently wet, inundated edges of the pond. Some plants are growing in more shade under moist mesic conditions as well.
Soils: The underlying geology of this area is of Eocene origin and characterized as Ocala Limestone. The Ocala Limestone consists of almost pure limestones with occasional dolomites. It can be subdivided into both lower and upper facies with the lower facies composed of a whitish to cream-colored, fine to medium grained, poorly to moderately hard, fossil rich grainstone and packstone. The upper Ocala is white and somewhat weak and poorly sorted. It is extremely fossil rich grainstone, packstone and wackestone and some chert is common in the upper facies.
Source: USGS Georgia Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=GANu%3B1)
The primary soil types in the collection area are classified as Herod and Muckalee Series soils. The Herod Series consists of poorly drained moderately permeable soils formed in loamy alluvium. These soils are on flood plains of streams in the Coastal Plain. Slopes range from 0 to 2 percent. The Muckalee Series consists of poorly drained moderately permeable soils formed in loamy and sandy alluvium. These soils are on flood plains of streams in the Coastal Plain. Slopes range from 0 to 2 percent.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2140768NA 88541
103NA 88542RJLSEUS2022-014Rosa palustris Marshall Georgia, United StatesNA2023COLLECTED12/09/2022Plants growing around a pond and associated wetland on the property of Monica Williams north of Albany, Georgia. Common along the transitional edges from wet to dry.31.63723900, -84.1377620060Plants are growing in full sun mostly in the transitional edges of the pond where conditions are generally moist mesic. Even so, this species appears quite adaptable and can be found in quite moist as well as drier soil conditions.
Soils: The underlying geology of this area is of Eocene origin and characterized as Ocala Limestone. The Ocala Limestone consists of almost pure limestones with occasional dolomites. It can be subdivided into both lower and upper facies with the lower facies composed of a whitish to cream-colored, fine to medium grained, poorly to moderately hard, fossil rich grainstone and packstone. The upper Ocala is white and somewhat weak and poorly sorted. It is extremely fossil rich grainstone, packstone and wackestone and some chert is common in the upper facies.
Source: USGS Georgia Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=GANu%3B1)
The primary soil types in the collection area are classified as Herod and Muckalee Series soils. The Herod Series consists of poorly drained moderately permeable soils formed in loamy alluvium. These soils are on flood plains of streams in the Coastal Plain. Slopes range from 0 to 2 percent. The Muckalee Series consists of poorly drained moderately permeable soils formed in loamy and sandy alluvium. These soils are on flood plains of streams in the Coastal Plain. Slopes range from 0 to 2 percent.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2140817NA 88542
104NA 88544RJLSEUS2022-016Itea virginica L. Georgia, United StatesNA2023COLLECTED12/09/2022Plants growing around a pond and associated wetland on the property of Monica Williams north of Albany, Georgia as well as the edges of nearby Muckalee Creek. Common in the wetland habitat edges. 31.63834700, -84.1383560063Plants are growing in part-shade to sun in wet to inundated conditions along the edges of a pond as well as the edges of Muckalee Creek. This species is found in conditions of abundant, year-round moisture.
Soils: The underlying geology of this area is of Eocene origin and characterized as Ocala Limestone. The Ocala Limestone consists of almost pure limestones with occasional dolomites. It can be subdivided into both lower and upper facies with the lower facies composed of a whitish to cream-colored, fine to medium grained, poorly to moderately hard, fossil rich grainstone and packstone. The upper Ocala is white and somewhat weak and poorly sorted. It is extremely fossil rich grainstone, packstone and wackestone and some chert is common in the upper facies.
Source: USGS Georgia Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=GANu%3B1)
The primary soil types in the collection area are classified as Herod and Muckalee Series soils. The Herod Series consists of poorly drained moderately permeable soils formed in loamy alluvium. These soils are on flood plains of streams in the Coastal Plain. Slopes range from 0 to 2 percent. The Muckalee Series consists of poorly drained moderately permeable soils formed in loamy and sandy alluvium. These soils are on flood plains of streams in the Coastal Plain. Slopes range from 0 to 2 percent.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2140770NA 88544
105NA 88545RJLSEUS2022-017Cephalanthus occidentalis L. Georgia, United StatesNA2023COLLECTED12/09/2022Plants growing around a pond and associated wetland on the property of Monica Williams north of Albany, Georgia. Infrequent frequency.31.63802000, -84.1349900059Plants are growing in part-shade to sun in the wetland associated with a large pond. This area is frequently wet during the growing season, but drier during the winter months.
Soils: The underlying geology of this area is of Eocene origin and characterized as Ocala Limestone. The Ocala Limestone consists of almost pure limestones with occasional dolomites. It can be subdivided into both lower and upper facies with the lower facies composed of a whitish to cream-colored, fine to medium grained, poorly to moderately hard, fossil rich grainstone and packstone. The upper Ocala is white and somewhat weak and poorly sorted. It is extremely fossil rich grainstone, packstone and wackestone and some chert is common in the upper facies.
Source: USGS Georgia Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=GANu%3B1)
The primary soil types in the collection area are classified as Herod and Muckalee Series soils. The Herod Series consists of poorly drained moderately permeable soils formed in loamy alluvium. These soils are on flood plains of streams in the Coastal Plain. Slopes range from 0 to 2 percent. The Muckalee Series consists of poorly drained moderately permeable soils formed in loamy and sandy alluvium. These soils are on flood plains of streams in the Coastal Plain. Slopes range from 0 to 2 percent.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2140771NA 88545
106NA 88547RJLSEUS2022-019Alnus serrulata (Aiton) Willd. Alabama, United StatesNA2023COLLECTED12/10/2022Poke Springs Branch inlet accessed by boat from Walter F. George Reservoir. Frequent plants.31.72236600, -85.1279370063Plants are growing in full sun on the eroded bank of the lake. The plants have access to abundant moisture with root systems extended into the lake.
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 soils (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 material2140773NA 88547
107NA 88548RJLSEUS2022-020Morella cerifera (L.) Small Alabama, United StatesNA2023COLLECTED12/10/2022Poke Springs Branch inlet accessed by boat from Walter F. George Reservoir. Common frequency.31.72236600, -85.1279370063Plants are growing in full sun on the eroded bank of the lake. The plants have access to abundant moisture with root systems extended into the lake.
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 soils (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 material2140774NA 88548
108NA 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
109NA 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
110NA 88551RJLSEUS2022-024Rhododendron minus Michx. var. minus Alabama, United StatesNA2023COLLECTED12/10/2022Plants growing on the west side of George H. Grimsley Highway (Alabama State Hwy. 95) on the bluffs above the south side of Abbie Creek. Common on this site, but otherwise infrequent. This species is near the southernmost end of its natural range. 31.47254800, -85.1630480067Plants are growing in part-shade to shade of a mixed evergreen and deciduous woodland on the dry well-drained bluffs 4-5 meters above Abbie Creek.
Soils: The underlying geology of this area is of Holocene origin and characterized as Alluvial, coastal and low terrace deposits. Varicolored fine to coarse quartz sand containing clay lenses and gravel in places.
Source: USGS Alabama Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=ALHalt%3B0)
The primary soil types in the collection area are classified as Bonneau Loamy Fine Sand soil (0 to 2 percent slopes). The Bonneau Series consists of very deep, well drained, moderately permeable soils on the middle and upper coastal plain. They were formed by marine and fluviomarine deposits. Slopes range from 0 to 12 percent. Soils are comprised of very friable loamy sand that is strongly acid in the upper 0.7 meters. The lower strata to 2 meters are comprised of sandy clay loam that is friable, sometimes with oxidized iron, and strongly acid.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2140778NA 88551
111NA 88554RJLSEUS2022-027Rhododendron alabamense Rehder Alabama, United StatesNA2023COLLECTED12/12/2022Plants growing on woodland slopes around and below the hilltop parking area leading down to the Silver Creek Lake Campground off of Silver Creek Lake Road. Occasional in the upland woodlands. 31.66613100, -87.5762570049Plants are growing in shade of upland dry mesic mature mixed deciduous and evergreen woodland. Generally, the overstory is thinner and there is less leaf litter cover, making the surface soil conditions drier.
Soils: The underlying geology of this area is Claiborne Group, Tallahatta Formation, of Eocene origin, with white to very light-greenish-gray thin-bedded to massive siliceous claystone; interbedded with thin layers of fossiliferous clay, sandy clay, and glauconitic sand and sandstone.
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 Smithdale-Boykin Complex soils (2 to 5 percent slopes). The Smithdale Series consists of very deep, well drained, moderately permeable soils on ridge tops and hill slopes in dissected uplands of the Southern Coastal Plain and in the Western Coastal Plain. They formed in thick beds of loamy marine sediments and are strongly acid. Slopes range from 1 to 60 percent. The Boykin Series consists of deep, well drained, moderately permeable soils that formed in sandy and loamy coastal plain sediments of Pleistocene age. These soils are on gently sloping to moderately steep uplands. Slopes range from 1 to 20 percent.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2140781NA 88554
112NA 88555RJLSEUS2022-028Rhododendron canescens (Michx.) Sweet Alabama, United StatesNA2023COLLECTED12/12/2022Plants growing on woodland slopes below the hilltop parking area leading down to the Silver Creek Lake Campground off of Silver Creek Lake Road. Occasional in the woodlands. 31.66549700, -87.5762450045Plants are growing in shade of moist mesic deciduous and evergreen woodland, mid-slope between the upland dry mesic zone and the creekside habitat below.
Soils: The underlying geology of this area is Claiborne Group, Tallahatta Formation, of Eocene origin, with white to very light-greenish-gray thin-bedded to massive siliceous claystone; interbedded with thin layers of fossiliferous clay, sandy clay, and glauconitic sand and sandstone.
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 Luverne Sandy Loam soils (15 to 35 percent slopes). The Luverne Series consists of very deep, well drained, moderately slowly permeable soils on dissected uplands of the Southern Coastal Plain. They formed in stratified marine sediments and are strongly acid. The lower strata of this series are clay and clay loam. Slopes range from 1 to 45 percent.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2140782NA 88555
113NA 88556RJLSEUS2022-029Rhododendron colemanii R. F. Mill. Alabama, United StatesNA2023COLLECTED12/12/2022Plants growing on woodland slopes below the hilltop parking area leading down to the Silver Creek Lake Campground off of Silver Creek Lake Road. Occasional in the woodlands. 31.66503300, -87.5746800043Plants are growing in shade of moist mesic deciduous and evergreen woodland on rich slopes 1-3 meters above a small spring-fed creek.
Soils: The underlying geology of this area is Claiborne Group, Tallahatta Formation, of Eocene origin, with white to very light-greenish-gray thin-bedded to massive siliceous claystone; interbedded with thin layers of fossiliferous clay, sandy clay, and glauconitic sand and sandstone.
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 Smithdale-Boykin Complex soils (2 to 5 percent slopes). The Smithdale Series consists of very deep, well drained, moderately permeable soils on ridge tops and hill slopes in dissected uplands of the Southern Coastal Plain and in the Western Coastal Plain. They formed in thick beds of loamy marine sediments and are strongly acid. Slopes range from 1 to 60 percent. The Boykin Series consists of deep, well drained, moderately permeable soils that formed in sandy and loamy coastal plain sediments of Pleistocene age. These soils are on gently sloping to moderately steep uplands. Slopes range from 1 to 20 percent.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2140783NA 88556
114NA 88557RJLSEUS2022-030Ilex longipes Chapm. ex Trel. Alabama, United StatesNA2023COLLECTED12/12/2022Silver Creek Lake Campground off of Silver Creek Lake Road: woodland slopes below the hilltop parking lot leading down to the campground.31.66442800, -87.5746140039Part shade of moist-mesic, mixed deciduous and evergreen woodland on dry, well-drained bank, 1-2 meters above a small spring-fed creek. The underlying geology of this area is Claiborne Group, Tallahatta Formation, of Eocene origin, with white to very light-greenish-gray thin-bedded to massive siliceous claystone; interbedded with thin layers of fossiliferous clay, sandy clay, and glauconitic sand and sandstone. (Source: USGS Alabama Geological Map Data). The primary soil types in the collection area are classified as Arundel-Cantuche Complex soils (15 to 35 percent slopes). The Arundel Series consists of moderately deep, well drained, very slowly permeable soils on dissected uplands of the Southern Coastal Plain. They formed in marine deposits consisting of acid clays underlain by horizontally bedded sandstone, buhrstone and siltstone. These soils are strongly acid. Slopes range from 2 to 60 percent. The Cantuche Series consists of shallow, well drained, moderately permeable soils that formed over horizontally bedded claystone. These soils are on narrow ridgetops and narrow benches on steep side-slopes of dissected landscapes in the Coastal Plain. They are strongly acid. Slopes range from 2 to 35 percent. (Source: NRCS Web Soil Survey).Wild material2140818NA 88557
115NA 88558RJLSEUS2022-031Ilex decidua Walter Alabama, United StatesNA2023COLLECTED12/12/2022Silver Creek Lake Campground off of Silver Creek Lake Road: Silver Creek Lake, at the edge of the campground.31.66344600, -87.5710840016Part shade to sun along the eroding banks of Silver Creek Lake in moist-mesic, mixed deciduous and evergreen woodland, 2-3 meters above the water. The underlying geology of this area is Claiborne Group, Tallahatta Formation, of Eocene origin, with white to very light-greenish-gray thin-bedded to massive siliceous claystone; interbedded with thin layers of fossiliferous clay, sandy clay, and glauconitic sand and sandstone. (Source: USGS Alabama Geological Map Data). The primary soil types in the collection area are classified as Riverview Fine Sandy Loam soils (0 to 2 percent slopes, occasionally flooded). The Riverview Series consists of very deep, well drained, moderately permeable soils that formed in loamy alluvium on flood plains. Slopes range from 0 to 5 percent. Riverview soils fare on high parts of flood plains of rivers and streams draining the Coastal Plain and Southern Piedmont. Runoff is slow. Permeability is moderate. These soils flood for short periods mostly in winter or early spring months. (Source: NRCS Web Soil Survey).Wild material2140819NA 88558
116NA 88559RJLSEUS2022-032Rhododendron colemanii R. F. Mill. Alabama, United StatesNA2023COLLECTED12/12/2022Plants growing in bottomland mostly deciduous woodlands on the south side of Lena Landegger Hwy (Monroe County Road 39) about 0.5 kilometers south of the entrance to the Alabama River Cellulose plant. Common at this site. 31.56879700, -87.4958950010Plants are growing in shade of a moist mesic (occasionally temporarily wet) deciduous woodland less than 1 meter above wetland habitats associated with the nearby Alabama River.
Soils: The underlying geology of this area is of Holocene origin and characterized as Alluvial, coastal and low terrace deposits. Varicolored fine to coarse quartz sand containing clay lenses and gravel in places.
Source: USGS Alabama Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=ALHalt%3B0)
The primary soil types in the collection area are classified as Chrysler Silt Loam soils (0 to 5 percent slopes, occasionally flooded). The Chrysler Series consists of deep, moderately well drained, slowly permeable soils that formed in clayey fluvial or alluvial sediments. These soils are on stream terraces of the Coastal Plain. They are strongly acid. The rate at which water runs off the surface is medium to rapid. Slopes range from 0 to 5 percent.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2140784NA 88559
117NA 88560RJLSEUS2022-033Hydrangea arborescens L. Alabama, United StatesNA2023COLLECTED12/12/2022Plants growing along the west side of Ferry Road at Haines Island Park leading down to the Alabama River.31.72299700, -87.4679820046Plants are growing in part-shade in the scoured ditch and slope alongside Ferry Road; occasionally in moss where seed undoubtedly germinated.
Soils: The underlying geology of this area is Claiborne Group, Tallahatta Formation, of Eocene origin, with white to very light-greenish-gray thin-bedded to massive siliceous claystone; interbedded with thin layers of fossiliferous clay, sandy clay, and glauconitic sand and sandstone.
Source: USGS Alabama Geological Map Data (https://mrdata.usgs.gov/geology/state/state.php?state=AL)
The primary soil type in the collection area is classified as Arundel Loam soil (8 to 35 percent slopes). The Arundel Series consists of moderately deep, well drained, very slowly permeable soils on dissected uplands of the Southern Coastal Plain. They formed in marine deposits consisting of acid clays underlain by horizontally bedded sandstone, buhrstone and siltstone. These soils are strongly acid. Slopes range from 2 to 60 percent.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2140785NA 88560
118NA 88561RJLSEUS2022-034Hydrangea quercifolia W. Bartram Alabama, United StatesNA2023COLLECTED12/12/2022Plants growing in the woodlands at Haines Island Park at the foot of Tallahatta cuesta, accessed by foot via Ferry Road. Common at this site. 31.72178200, -87.4658960066Plants are growing in part-shade to shade of a moist mesic, well-drained conditions on rocks and in the eroding matrix of the Tallahatta Questa.
Soils: The underlying geology of this area is Claiborne Group, Tallahatta Formation, of Eocene origin, with white to very light-greenish-gray thin-bedded to massive siliceous claystone; interbedded with thin layers of fossiliferous clay, sandy clay, and glauconitic sand and sandstone.
Source: USGS Alabama Geological Map Data (https://mrdata.usgs.gov/geology/state/state.php?state=AL)
The primary soil type in the collection area is classified as Arundel Loam soil (8 to 35 percent slopes). The Arundel Series consists of moderately deep, well drained, very slowly permeable soils on dissected uplands of the Southern Coastal Plain. They formed in marine deposits consisting of acid clays underlain by horizontally bedded sandstone, buhrstone and siltstone. These soils are strongly acid. Slopes range from 2 to 60 percent.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2140786NA 88561
119NA 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
120NA 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
121NA 88571RJLSEUS2022-044Itea virginica L. Florida, United StatesNA2023COLLECTED12/15/2022Plants are growing along a several mile stretch of the Yellow River and accessed by boat via the Yellow River Boat Ramp on the east side of Florida State Hwy 87. The species is common along several miles of the Yellow River.30.55805600, -86.935445001Plants are typically found growing in part-shade to sun in permanently saturated to submersed conditions along the edge of the Yellow River, growing in association with a wide array of deciduous and evergreen trees, shrubs and perennial plant species. Most of the plants along the river are adapted to acidic conditions and, while the aquatic habitats are generally fresh water, there is occasionally tidal or hurricane-caused saltwater intrusions.
Soils: The underlying geology of this area is classified as Alluvium, of Pleistocene/Holocene origin and consists of undifferentiated Quaternary sediments of varying thickness including siliciclastics, organics and freshwater carbonates. The siliciclastics are light gray, tan, brown to black, unconsolidated to poorly consolidated, clean to clayey, silty, unfossiliferous, variably organic-bearing sands to blue green to olive green, poorly to moderately consolidated, sandy, silty clays. Organics occur as plant debris, roots, disseminated organic matrix and beds of peat. Freshwater carbonates, often referred to as marls in the literature, are scattered.
Source: USGS Florida Geologic Map Data (https://mrdata.usgs.gov/geology/state/state.php?state=fl)
The surface soil profile of this area is primarily Bibb-Kinston Series association. Bibb Series soils are coarse-loamy, sandy, acid soils that are poorly drained. They are soils of flood plains and streams subject to frequent flooding. These are found in association with Kinston Series soils that are fine-loamy, sandy, acid soils of flood plains and stream subject to frequent flooding. The Bibb-Kinston Association ranges from 1-1.5 meters thick and is strongly acid.
Source: Soil Survey of Santa Rosa County and NRCS Web Soil Survey (https://www.nrcs.usda.gov/Internet/FSE_MANUSCRIPTS/florida/FL113/0/SantaRosa.pdf and https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2140791NA 88571
122NA 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
123NA 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
124NA 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
125NA 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
126NA 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
127NA 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
128NA 88509RJL2022TX-004Ilex decidua Walter Texas, United StatesNA2022COLLECTED11/01/2022Low woodlands along the north side of Texas State Hwy 190 between the highway and an unnamed paved service road that leads down to the Sabine River; the turn for the service road is approximately 0.62 kilometers west of the Sabine River. Near the bridge over the Sabine River.30.74730000, -93.6156890020Plants are growing in part-shade to shade of a moist mesic (occasionally temporarily wet) woodland. Ilex decidua can be in the low woods most of the way down to the river. Plant is a common understory shrub in the moist woodland habitat not far from the Sabine River. Soils: The underlying geology of this area is of Holocene origin and characterized as Alluvium. The alluvium and low terrace deposits along streams include sand, silt, clay, and gravel. Thickness is variable. In this case alluvium is from the Sabine River. (Source: USGS Texas Geologic Map Data). The primary soil types in the collection area are classified as Urbo and Mantachie soils. The Urbo series consists of deep, somewhat poorly drained soils. Permeability is very slow. These nearly level to gently sloping soils formed in clayey alluvium on flood plains of streams that drain uplands of the Southern Coastal Plain. Slopes range from 0 to 3 percent. In wet seasons late in winter and early in spring, the water table is at a depth of 1 to 2 feet and most areas of Urbo soils are subject to either occasional or frequent flooding of brief to long duration. The Mantachie series consists of very deep, somewhat poorly drained, moderately permeable soils on flood plains of the Southern Coastal Plain. They formed in loamy alluvium and considered acidic. Mantachie soils are subject to rare to frequent flooding in the winter and early spring for brief to long duration, unless protected. The seasonal high water table ranges from 1.0 to 1.5 feet of the surface during periods of high rainfall. (Source: NRCS Web Soil Survey).Wild material2139816NA 88509
129NA 88510RJL2022TX-005Crataegus marshallii Eggl. Texas, United StatesNA2022COLLECTED11/01/2022Plants growing along the west side of Texas State Hwy 87 on the edge of the woodlands. Plant is infrequently found, but a regular member of the woodlands as well as forest edge communities along the highway. 31.15847300, -93.73852000115Plants are growing in part-shade to sun on upland dry hills. In shade they survive, but in part-shade to sun they develop excellent flowering and fruiting.
Soils: 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 (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=TXQbs%3B0
The primary soil types in the collection area are classified as Letney-Tehran soils. These soils consist of deep, somewhat excessively drained, moderately rapidly permeable soils on uplands. They were formed in thick loamy and sandy sediments on the Western Coastal Plain. The Letney-Tehran soils are on gently sloping to moderately steep uplands with slopes ranging from 1 to 20 percent. They are typically strongly acidic.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2139817NA 88510
130NA 88511RJL2022TX-006Persea palustris (Raf.) Sarg. Texas, United StatesNA2022COLLECTED11/01/2022Plants growing in a wetland on the north side of Clarktown Road approximately 1.5 kilometers west of Texas State Hwy 87 in Sabine National Forest. Plant is common in the moist-wet and mesic edges of the wetland habitat where it is best adapted. 31.17114800, -93.7510620071Plants are growing in part-shade in a depression wetland of a small upland valley stream area surrounded by upland Pinus palustris and Pinus taeda forests. While the region had a severe drought during 2022, this depression wetland remained mucky wet throughout. Higher light conditions that supported heavy fruit production on the Persea may have been due to nearby harvesting of forest sections adjacent to the wetland.
Soils: 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 (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=TXQbs%3B0
The primary soil types in the collection area are classified as Letney soils. These soils consist of deep, somewhat excessively drained, moderately rapidly permeable soils on uplands. They were formed in thick loamy and sandy sediments on the Western Coastal Plain. The Letney soils are on gently sloping uplands with slopes ranging from 1 to 5 percent. They are typically strongly acidic. It should be noted that the upper surface, to an unknown depth has a significant amount of decomposed and undecomposed organic litter, presumably from sphagnum, at least, in part.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2139818NA 88511
131NA 88512RJL2022TX-007Morella caroliniensis (Mill.) Small Texas, United StatesNA2022COLLECTED11/01/2022Plants growing in a wetland on the north side of Clarktown Road approximately 1.5 kilometers west of Texas State Hwy 87 in Sabine National Forest. Plant is relatively common in the moist-wet and mesic edges of the wetland habitat.31.17181200, -93.7511800081Plants are growing in part-shade to part-sun in a depression wetland and slightly upslope of a small upland valley stream area surrounded by upland Pinus palustris and Pinus taeda forests. While the region had a severe drought during 2022, this depression wetland remained mucky wet throughout.
Soils: 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 (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=TXQbs%3B0
The primary soil types in the collection area are classified as Letney soils. These soils consist of deep, somewhat excessively drained, moderately rapidly permeable soils on uplands. They were formed in thick loamy and sandy sediments on the Western Coastal Plain. The Letney soils are on gently sloping uplands with slopes ranging from 1 to 5 percent. They are typically strongly acidic. It should be noted that the upper surface, to an unknown depth has a significant amount of decomposed and undecomposed organic litter, presumably from sphagnum, at least, in part.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2139819NA 88512
132NA 88513RJL2022TX-008Cephalanthus occidentalis L. Texas, United StatesNA2022COLLECTED11/01/2022Plants growing in moist sites on the north and south side of Clarktown Road approximately 0.5 kilometers west of Texas State Hwy 87 in Sabine National Forest. Plant is relatively common in the moist-wet and seasonally wet locations; absent elsewhere.31.17294500, -93.7413390092Plants are growing in part-shade to part-sun in moist-wet areas with low competition. The area generally retains moisture throughout the growing season.
Soils: 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 (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=TXQbs%3B0
The primary soil types in the collection area are classified as Mattex-Iulus complex soils. The Mattex series consists of very deep, somewhat poorly drained, slowly permeable, acidic loamy soils. They formed in loamy and clayey alluvium. These are nearly level soils on flood plains. Slopes range from 0 to 1 percent. The Iulus series consists of very deep, moderately well drained, moderately permeable, soils on flood plains. These soils formed in recent alluvium derived from coastal plain sediments, often containing fine sandy elements and are extremely acidic. The slope ranges from 0 to 1 percent.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2139820NA 88513
133WLP 2673RJL2022NJ-004Lyonia mariana (L.) D. Don New Jersey, United StatesNA2022COLLECTED10/24/2022Plants growing on both sides of Duerer Street approximately 0.37 kilometers southeast of 4th Avenue, Mullica Township, New Jersey. Plants are common but scattered on both sides of the road at this site. 39.55730700, -74.6637610022Plants grow from part shade to full sun throughout the habit from the upper edges of the ditches through the herbaceous grass dominant buffer and all the way to the part shade of the woodland edge. Plants transition through moist/wet conditions in full sun to quite dry conditions in part shade and seem equally adapted.
Soils: The underlying geology of this area is the Cohansey Formation of middle Miocene origin and comprised of sand, white to yellow with local gravel and clay. It is sometimes locally stained red or orange brown by iron oxides and (or) cemented into large blocks of ironstone. Unweathered clay is typically dark gray, but commonly weathers white where it is interbedded with thin beds of ironstone. Sand is typically medium grained and moderately sorted although it ranges from fine to very coarse grained and from poorly to well sorted. Sand consists of quartz and siliceous rock fragments. Some beds are locally micaceous. Maximum thickness in the map area is about 60 meters; however, thickness is difficult to determine because of the irregular basal contact and extensive post-depositional erosion.
Source: USGS New Jersey Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=NJTch%3B1)
The primary soil type in the area of this collection is classified as Mullica sandy loam, 0 to 2 percent slopes. These soils are typically coarse-loamy, siliceous, semiactive, and mesic typic humaquepts that are strongly to extremely acidic throughout the profile. The typical solum thickness ranges from 50-150+ cm. These soils are generally considered to be poorly drained.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2139664WLP 2673
134NA 88500RJL2022NJ-002Ilex glabra (L.) A. Gray New Jersey, United StatesNA2022COLLECTED10/24/2022Mullica Township: both sides of Duerer Street, approximately 0.37 kilometers southeast of 4th Avenue.39.55885000, -74.6644250021Plants growing in shade to almost full sun on compacted seasonally moist to temporarily wet areas of a mixed evergreen and deciduous woodland dominated by Pinus rigida. Vegetation of this area is very much defined by small changes in elevation that go from wet to very dry. Ilex glabra remains abundant throughout, though. Plants are abundant on the edge of the woodlands as well as the understory of the woodlands. Soils: The underlying geology of this area is the Cohansey Formation of middle Miocene origin and comprised of sand, white to yellow with local gravel and clay. It is sometimes locally stained red or orange brown by iron oxides and (or) cemented into large blocks of ironstone. Unweathered clay is typically dark gray, but commonly weathers white where it is interbedded with thin beds of ironstone. Sand is typically medium grained and moderately sorted although it ranges from fine to very coarse grained and from poorly to well sorted. Sand consists of quartz and siliceous rock fragments. Some beds are locally micaceous. Maximum thickness in the map area is about 60 meters; however, thickness is difficult to determine because of the irregular basal contact and extensive post-depositional erosion. (Source: USGS New Jersey Geologic Map Data). The primary soil type in the area of this collection is classified as Mullica sandy loam, 0 to 2 percent slopes. These soils are typically coarse-loamy, siliceous, semiactive, and mesic typic humaquepts that are strongly to extremely acidic throughout the profile. The typical solum thickness ranges from 50-150+ cm. These soils are generally considered to be poorly drained. (Source: NRCS Web Soil Survey).Wild material2139663NA 88500
135NA 88499RJL2022MD-018Ilex opaca Aiton Maryland, United StatesNA2022COLLECTED10/22/2022Elk Neck State Park: woodlands along Maryland Hwy 272, Turkey Point Road.39.47706500, -75.9872090035Plants growing in shade to full sun on well-drained slopes of a mixed evergreen and deciduous woodland. Soils: The underlying geology of this area is the characterized as Upland Deposits (Eastern Shore) of Quaternary origin. This formation is characterized by gravel, sand, silt, and clay. Mostly cross-bedded, poorly sorted, medium- to coarse-grained white to red sand and gravel; boulders near base; minor pink and yellow silts and clays. The thickness of this formation ranges from 0 to 90 feet, locally thicker in paleochannels. (Source: USGS Maryland Geologic Map Data). The primary soil type in the area of this collection is classified as Sassafras and Croom soils, 15 to 25 percent slopes. These soils are typically fine-loamy, siliceous, semiactive, mesic typic hapludults that are strongly to extremely acid. The typical solum thickness ranges from 60-130 cm. These soils are generally well-drained. (Source: NRCS Web Soil Survey).Wild material2139662NA 88499
136WLP 2668RJL2022MD-014Aronia arbutifolia (L.) Pers. Maryland, United StatesNA2022COLLECTED10/05/2022Plant growing at Elkton State Forest along road in wet woodlands near the Elk Neck State Forest Shooting Range labelled as the address of 717 Irishtown Rd, North East, MD 21901. Plant is uncommon at this site. 39.58716100, -75.9141900055Plants are growing in part-shade to part sun of a deciduous forest on hummocks in a very moist to wet low-lying area along a seasonal or year-round flowing seep.
Soils: The underlying geology of this area is of Cretaceous origin and comprised of Potomac Group, including Raritan and Patapsco Formations, and Patuxent Formation. The Potomac Group includes: interbedded quartzose gravels; proto-quartzitic to orthoquartzitic argillaceous sands; and white, dark gray, and multicolored silts and clays. Included withing this zone are Raritan and Patapsco Formations comprised of gray, brown, and red variegated silts and clays; lenticular, cross-bedded, argillaceous, subrounded sands; minor gravels; thickness. The Patuxent Formation is also interbedded in this zone and comprised of white or light gray to orange-brown, moderately sorted, cross-bedded, argillaceous, angular sands and subrounded quartz gravels; silts and clays subordinate that are predominantly pale gray.
Source: USGS Maryland Geologic Map Data https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=MDKp%3B5
The primary soil types in the collection area are classified as Russett-Christiana-Hambrook Complex and/or Sassafras and Croom Soils; though, others may intersect and overlay in specific areas. The soils in the collecting area are generally described as a complex series of fluviomarine deposits. The soils range from a thin loam layer at the surface to varying levels of loam to sandy loam and/or extremely gravelly sandy clay loam strata, depending upon geographical location (ie. Hillslope summits, slopes, footslopes, swales, etc.).
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2139659WLP 2668
137NA 89043RJL2022MD-017Cephalanthus occidentalis L. Maryland, United StatesNA2022COLLECTED10/05/2022Plants growing at Elkton State Forest along road and in wet woodlands near the Elk Neck State Forest Shooting Range labelled as the address of 717 Irishtown Rd, North East, MD 21901. Plants are locally common but restricted to the low-lying wet woodlands. 39.58727700, -75.9140390055Plants are growing in part-shade to part-sun of deciduous forests on hummocks in very moist to wet low-lying areas along seasonal or year-round flowing seeps.
Soils: The underlying geology of this area is of Cretaceous origin and comprised of Potomac Group, including Raritan and Patapsco Formations, and Patuxent Formation. The Potomac Group includes: interbedded quartzose gravels; proto-quartzitic to orthoquartzitic argillaceous sands; and white, dark gray, and multicolored silts and clays. Included withing this zone are Raritan and Patapsco Formations comprised of gray, brown, and red variegated silts and clays; lenticular, cross-bedded, argillaceous, subrounded sands; minor gravels; thickness. The Patuxent Formation is also interbedded in this zone and comprised of white or light gray to orange-brown, moderately sorted, cross-bedded, argillaceous, angular sands and subrounded quartz gravels; silts and clays subordinate that are predominantly pale gray.
Source: USGS Maryland Geologic Map Data https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=MDKp%3B5
The primary soil types in the collection area are classified as Russett-Christiana-Hambrook Complex and/or Sassafras and Croom Soils; though, others may intersect and overlay in specific areas. The soils in the collecting area are generally described as a complex series of fluviomarine deposits. The soils range from a thin loam layer at the surface to varying levels of loam to sandy loam and/or extremely gravelly sandy clay loam strata, depending upon geographical location (ie. Hillslope summits, slopes, footslopes, swales, etc.).
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2139608NA 89043
138NA 89042RJL2022MD-016Aronia ×prunifolia (Marshall) Rehder Maryland, United StatesNA2022COLLECTED10/05/2022Plants growing at Elkton State Forest along road and in wet woodlands near the Elk Neck State Forest Shooting Range labelled as the address of 717 Irishtown Rd, North East, MD 21901. Plants are infrequent and were found in this one area of low-lying wet woodlands. Perhaps others would have been found upon investigation of other similar habitats.39.58730200, -75.9141580055Plants are growing in part-sun to part-shade of deciduous forests on moist slopes and on hummocks in very moist to wet low-lying areas along seasonal or year-round flowing seeps.
Soils: The underlying geology of this area is of Cretaceous origin and comprised of Potomac Group, including Raritan and Patapsco Formations, and Patuxent Formation. The Potomac Group includes: interbedded quartzose gravels; proto-quartzitic to orthoquartzitic argillaceous sands; and white, dark gray, and multicolored silts and clays. Included withing this zone are Raritan and Patapsco Formations comprised of gray, brown, and red variegated silts and clays; lenticular, cross-bedded, argillaceous, subrounded sands; minor gravels; thickness. The Patuxent Formation is also interbedded in this zone and comprised of white or light gray to orange-brown, moderately sorted, cross-bedded, argillaceous, angular sands and subrounded quartz gravels; silts and clays subordinate that are predominantly pale gray.
Source: USGS Maryland Geologic Map Data https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=MDKp%3B5
The primary soil types in the collection area are classified as Russett-Christiana-Hambrook Complex and/or Sassafras and Croom Soils; though, others may intersect and overlay in specific areas. The soils in the collecting area are generally described as a complex series of fluviomarine deposits. The soils range from a thin loam layer at the surface to varying levels of loam to sandy loam and/or extremely gravelly sandy clay loam strata, depending upon geographical location (ie. Hillslope summits, slopes, footslopes, swales, etc.).
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2139607NA 89042
139NA 89041RJL2022MD-015Lyonia ligustrina (L.) DC. Maryland, United StatesNA2022COLLECTED10/05/2022Plants growing at Elkton State Forest along road and in wet woodlands near the Elk Neck State Forest Shooting Range labelled as the address of 717 Irishtown Rd, North East, MD 21901. Plants are common but scattered on the edges and in the understory of low-lying wet woodlands. 39.58716100, -75.9141900055Plants are growing in part-shade to shade of deciduous forests on moist slopes and on hummocks in very moist to wet low-lying areas along seasonal or year-round flowing seeps.
Soils: The underlying geology of this area is of Cretaceous origin and comprised of Potomac Group, including Raritan and Patapsco Formations, and Patuxent Formation. The Potomac Group includes: interbedded quartzose gravels; proto-quartzitic to orthoquartzitic argillaceous sands; and white, dark gray, and multicolored silts and clays. Included withing this zone are Raritan and Patapsco Formations comprised of gray, brown, and red variegated silts and clays; lenticular, cross-bedded, argillaceous, subrounded sands; minor gravels; thickness. The Patuxent Formation is also interbedded in this zone and comprised of white or light gray to orange-brown, moderately sorted, cross-bedded, argillaceous, angular sands and subrounded quartz gravels; silts and clays subordinate that are predominantly pale gray.
Source: USGS Maryland Geologic Map Data https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=MDKp%3B5
The primary soil types in the collection area are classified as Russett-Christiana-Hambrook Complex and/or Sassafras and Croom Soils; though, others may intersect and overlay in specific areas. The soils in the collecting area are generally described as a complex series of fluviomarine deposits. The soils range from a thin loam layer at the surface to varying levels of loam to sandy loam and/or extremely gravelly sandy clay loam strata, depending upon geographical location (ie. Hillslope summits, slopes, footslopes, swales, etc.).
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2139606NA 89041
140NA 89040RJL2022MD-013Eubotrys racemosus (L.) Nutt. Maryland, United StatesNA2022COLLECTED10/05/2022Plants growing at Elkton State Forest along road and in wet woodlands over a distance of about 0.55 kilometers near the Elk Neck State Forest Shooting Range labelled as the address of 717 Irishtown Rd, North East, MD 21901. Plants are common but scattered on the edges and in the understory of low-lying wet woodlands. 39.58227200, -75.9132880057Plants are growing in part-shade to shade of deciduous forests on moist slopes and on hummocks in very moist to wet low-lying areas along seasonal or year-round flowing seeps.
Soils: The underlying geology of this area is of Cretaceous origin and comprised of Potomac Group, including Raritan and Patapsco Formations, and Patuxent Formation. The Potomac Group includes: interbedded quartzose gravels; proto-quartzitic to orthoquartzitic argillaceous sands; and white, dark gray, and multicolored silts and clays. Included withing this zone are Raritan and Patapsco Formations comprised of gray, brown, and red variegated silts and clays; lenticular, cross-bedded, argillaceous, subrounded sands; minor gravels; thickness. The Patuxent Formation is also interbedded in this zone and comprised of white or light gray to orange-brown, moderately sorted, cross-bedded, argillaceous, angular sands and subrounded quartz gravels; silts and clays subordinate that are predominantly pale gray.
Source: USGS Maryland Geologic Map Data https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=MDKp%3B5
The primary soil types in the collection area are classified as Russett-Christiana-Hambrook Complex and/or Sassafras and Croom Soils; though, others may intersect and overlay in specific areas. The soils in the collecting area are generally described as a complex series of fluviomarine deposits. The soils range from a thin loam layer at the surface to varying levels of loam to sandy loam and/or extremely gravelly sandy clay loam strata, depending upon geographical location (ie. Hillslope summits, slopes, footslopes, swales, etc.).
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2139605NA 89040
141NA 89033RJL2022MD-010Clethra alnifolia L. Maryland, United StatesNA2022COLLECTED09/15/2022Plants growing in low woodlands at the end of Greenway Avenue near a boat dock that leads to the Pocomoke River, adjacent to Winter Quarters Golf Course, Pocomoke City. Plants common throughout the wetland area as well as mesic edges of the woodlands.38.08305100, -75.56527800Plants growing in the flood plain of the Pocomoke River in shade to part sun of a mixed deciduous and evergreen bottomland habitat about 10 meters from the edge of the golf course fairway. The habitat is a mucky swamp edge habitat next to the Pocomoke River, most of which seems wet year-round and grades slightly upslope to more mesic conditions.
The underlying geology of this area is comprised of Quaternary Deposits of Wisconsin to Holocene origin. The composition is primarily undifferentiated gray to buff sand and gravel, gray to brown lignitic silt and clay, occasional boulders, and rare shell beds. Surficial deposits occur as shell-bearing estuarine clays and silts.
Source: USGS Maryland Geologic Map Data https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=MDQdu%3B5
The surface soil profile of this habitat is classified as Puckum Muck which is frequently flooded. These highly saturated soils are found in flats, depressions and swales. The soil reaction of Puckum Muck is extremely acid to strongly acid throughout the profile. The depth to bedrock is generally greater than 150 cm. Wood fragments comprise 0-25%, by volume of the Puckum Muck throughout the profile which includes mostly twigs, branches, logs, or stumps and are 1.5-30 cm in diameter. The composition of these highly saturated soils, are classified as muck (sapric soil material) or mucky peat (hemic soil material) throughout most of the upper 150 cm and may contain thin layers of mucky silt loam, silty clay loam, sandy loam and/or sand.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2139598NA 89033
142NA 89032RJL2022MD-009Rhododendron viscosum (L.) Torr. Maryland, United StatesNA2022COLLECTED09/15/2022Plants growing in low woodlands at the end of Greenway Avenue near a boat dock that leads to the Pocomoke River, adjacent to Winter Quarters Golf Course, Pocomoke City. Plants scattered throughout the wetland area. Infrequent, but regularly found. 38.08235200, -75.565665001Plants growing in the flood plain of the Pocomoke River in part shade to shade of a mixed deciduous and evergreen bottomland habitat about 10 meters from the edge of the golf course fairway. The habitat is a mucky swamp edge habitat next to the Pocomoke River, most of which seems wet year-round.
The underlying geology of this area is comprised of Quaternary Deposits of Wisconsin to Holocene origin. The composition is primarily undifferentiated gray to buff sand and gravel, gray to brown lignitic silt and clay, occasional boulders, and rare shell beds. Surficial deposits occur as shell-bearing estuarine clays and silts.
Source: USGS Maryland Geologic Map Data https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=MDQdu%3B5
The surface soil profile of this habitat is classified as Puckum Muck which is frequently flooded. These highly saturated soils are found in flats, depressions and swales. The soil reaction of Puckum Muck is extremely acid to strongly acid throughout the profile. The depth to bedrock is generally greater than 150 cm. Wood fragments comprise 0-25%, by volume of the Puckum Muck throughout the profile which includes mostly twigs, branches, logs, or stumps and are 1.5-30 cm in diameter. The composition of these highly saturated soils, are classified as muck (sapric soil material) or mucky peat (hemic soil material) throughout most of the upper 150 cm and may contain thin layers of mucky silt loam, silty clay loam, sandy loam and/or sand.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2139597NA 89032
143NA 88481RJL2022MD-002Kalmia latifolia L. Maryland, United StatesNA2022COLLECTED09/04/2022Plants growing at Elkton State Forest along roads and woodlands over a distance of approximately 5 kilometers labelled as the address of 717 Irishtown Rd, North East, MD 21901. Kalmia is very common along the unnamed gravel road as well as the understory of the upland woodlands.39.58852900, -75.9045290060Plants are growing in a mesic to dry, well-drained habitat of mixed deciduous and evergreen woodlands comprised primarily of acid-loving plants. Plants are growing in shade to part shade along the unnamed road as well as the woodlands. The soils in the collection area are generally described as a complex series of fluviomarine deposits. The soils range from a thin loam layer at the surface to varying levels of loam to sandy loam and/or extremely gravelly sandy clay loam strata, depending upon geographical location (ie. Hillslope summits, slopes, footslopes, swales, etc.). The primary soil types in the collection area are classified as Russett-Christiana-Hambrook Complex and/or Sassafras and Croom Soils; though, others may intersect and overlay in specific areas.Wild material2139360NA 88481
144NA 88482RJL2022MD-003Rhododendron periclymenoides (Michx.) Shinners Maryland, United StatesNA2022COLLECTED09/04/2022Plants growing at Elkton State Forest along roads and woodlands over a distance of approximately 5 kilometers labelled as the address of 717 Irishtown Rd, North East, MD 21901. Plants are found infrequently and scattered along the unnamed gravel road39.58852900, -75.9045290051Plants are growing in a mesic to dry, well-drained habitat of mixed deciduous and evergreen woodlands comprised primarily of acid-loving plants. Plants are growing in part shade. The soils in the collection area are generally described as a complex series of fluviomarine deposits. The soils range from a thin loam layer at the surface to varying levels of loam to sandy loam and/or extremely gravelly sandy clay loam strata, depending upon geographical location (ie. Hillslope summits, slopes, footslopes, swales, etc.). The primary soil types in the collection area are classified as Russett-Christiana-Hambrook Complex and/or Sassafras and Croom Soils; though, others may intersect and overlay in specific areas.Wild material2139361NA 88482
145NA 88483RJL2022MD-004Clethra alnifolia L. Maryland, United StatesNA2022COLLECTED09/04/2022Plants growing at Elkton State Forest along roads and woodlands over a distance of approximately 5 kilometers labelled as the address of 717 Irishtown Rd, North East, MD 21901. Plants are found regularly but scattered along the unnamed gravel road as well as in open understory of the upland woodlands. 39.58531200, -75.8956610047Plants are growing in a mesic to moist, well-drained habitat of mixed deciduous and evergreen woodlands comprised primarily of acid-loving plants. Plants are growing in part shade and open understory shade. The soils in the collection area are generally described as a complex series of fluviomarine deposits. The soils range from a thin loam layer at the surface to varying levels of loam to sandy loam and/or extremely gravelly sandy clay loam strata, depending upon geographical location (ie. Hillslope summits, slopes, footslopes, swales, etc.). The primary soil types in the collection area are classified as Russett-Christiana-Hambrook Complex and/or Sassafras and Croom Soils; though, others may intersect and overlay in specific areas.Wild material2139362NA 88483
146NA 88484RJL2022MD-005Aronia melanocarpa (Michx.) Elliott Maryland, United StatesNA2022COLLECTED09/04/2022Plants growing at Elkton State Forest on Elk Neck Trail #3 (Starkey Lane) labelled as the address of 717 Irishtown Rd, North East, MD 21901. This was the only plant observed during several visits to Elk Neck State Forest during early and mid-summer39.58531200, -75.8956610055Plants are growing in a mesic to dry, well-drained habitat of mixed deciduous and evergreen woodlands comprised primarily of acid-loving plants. Plants are growing in part shade to part-sun. The soils in the collection area are generally described as a complex series of fluviomarine deposits. The soils range from a thin loam layer at the surface to varying levels of loam to sandy loam and/or extremely gravelly sandy clay loam strata, depending upon geographical location (ie. Hillslope summits, slopes, footslopes, swales, etc.). The primary soil types in the collection area are classified as Russett-Christiana-Hambrook Complex and/or Sassafras and Croom Soils; though, others may intersect and overlay in specific areas.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild materialreceived as A. prunifolia, on further examination by collector it was determined to be A. melanocarpa2139363NA 88484
147NA 88485RJL2022MD-006Hamamelis virginiana L. Maryland, United StatesNA2022COLLECTED09/04/2022Plants growing at Elkton State Forest on Elk Neck Trail #3 (Starkey Lane) labelled as the address of 717 Irishtown Rd, North East, MD 21901. This species was infrequent throughout most of Elk Neck State Park, but relatively common.39.58790000, -75.8885310054Plants are growing in a mesic to dry, well-drained habitat of mixed deciduous and evergreen woodlands comprised primarily of acid-loving plants. Plants are growing in part shade to shade. The soils in the collection area are generally described as a complex series of fluviomarine deposits. The soils range from a thin loam layer at the surface to varying levels of loam to sandy loam and/or extremely gravelly sandy clay loam strata, depending upon geographical location (ie. Hillslope summits, slopes, footslopes, swales, etc.). The primary soil types in the collection area are classified as Russett-Christiana-Hambrook Complex and/or Sassafras and Croom Soils; though, others may intersect and overlay in specific areas.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2139364NA 88485
148WLP 26102022VA-01Stewartia malacodendron L. Virginia, United StatesNA2022COLLECTED09/12/2022Woodlands adjacent to and bounded by the interchange of Business Route 168 (N. Battlefield Avenue) and Route 168, next to a detention basin and shopping plaza on the west side of Battlefield Avenue. Accessed by parking in the cul-de-sac at the south end of Kingsborough Square Street. This plant is a very common and abundant component of this woodland with significant recruitment continuing36.73888200, -76.243277009Plants growing in rich mesic, moist but well-drained conditions in the high understory shade of a mixed deciduous and evergreen woodland, primarily comprised of deciduous trees in the over-story and a mixture of deciduous and evergreen species in the sub-canopy.
Soils: The underlying geology of this area is the Tabb Formation of Quaternary origin which is comprised of undifferentiated sand, silt, and peat and subdivided into three members. Within the Tabb Formation lies the Sedgefield Member, a pebbly to bouldery, clayey sand and fine to medium, shell-rich sand that grades upward into sandy and clayey silt; locally, channel fill at the base of unit includes as much as 15 meters of fine to coarse, cross-bedded sand and clayey silt and peat containing in-situ tree stumps. Sandy bay facies commonly contain numerous mollusks as well as coral. Thickness is 0 to 15.8 meters.
Source: USGS Virginia Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=VAQts%3B0)
The surface soil profile of this area is Tetotum fine sandy loam, 0 to 2 percent slopes. Forming primarily terraces, these soils are moderately well-drained and highly acidic. They are generally 100-150 cm thick, the upper 20 inches of the horizon averages more than 30 percent silt or more than 40 percent silt plus very fine sand.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2139348WLP 2610
149WLP 26122022VA-03Styrax grandifolius Aiton Virginia, United StatesNA2022COLLECTED09/12/2022Northwest River Park on the south side of Indian Springs Road behind the Equestrian Center along a bridle trail. This plant is a common in the mesic woodlands at this location.36.58361100, -76.1627780021Plants growing in shade to part-shade of the mixed deciduous and evergreen mesic woodland about 1 to 2 meters above a nearby wetland area.
The underlying geology of this area is the Tabb Formation of Quaternary origin which is comprised of undifferentiated sand, silt, and peat and subdivided into three members. Within the Tabb Formation lies the Lynnhaven Member with pebbly and cobbly, fine to coarse gray sand grades upward into clayey and silty fine sand and sandy silt. Extensive low lands bounded on the landward side by river-, bay-, and ocean-facing scarps having toe altitudes of 5-6 meters. Thickness is 0 to 6.5 meters.
Source: USGS Virginia Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=VAQtl%3B0)
The surface soil profile of this area is Chapanoke-Yeopim complex, 0 to 3 percent slopes. These soil as somewhat poorly to moderately drained, acidic, and found on marine terraces and summits of low elevation coastal plain areas. They are comprised of silt loam, silty clay loam, sandy clay loam and loam in varying quantities across the profile; the depth to parent geology is approximately 200 cm.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx		Wild material2139350WLP 2612
150WLP 26142022VA-05Euonymus americanus L. Virginia, United StatesNA2022COLLECTED09/12/2022In Colonial Williamsburg, park in the Providence Hall Directors Wing parking lot and enter the Bassett Trace Nature Trail; this species is found in the woodlands on either side of the trail and over a bridge until the it turns right. This plant is infrequent, but occasionally found in the mesic woodlands throughout this location.37.26681600, -76.6925280021Plants growing in shade to part-shade of the mixed deciduous and evergreen mesic woodland. This species is generally growing in areas with an abundant organic, mature woodland that is relatively undisturbed.
The underlying geology of this area is Windsor Formation of Tertiary-Quaternary origin (lower Pleistocene or upper Pliocene). It is comprised of gray and yellowish- to reddish-brown sand, gravel, silt, and clay. It constitutes surficial deposits of extensive plain and fluvial-estuarine terraces above elevations of 10 meters. The thickness of the Windsor Formation is 0 to 12.5 meters.
Source: USGS Virginia Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=VAQTw%3B0)
The surface soil profile of this area is Emporia Complex, 15 to 25 percent slopes. This soil as moderately well-drained, acidic, and found on sloping and elevated terraces. They are comprised of fine sandy loam, loam, and sandy clay loam in varying quantities across the profile; the depth to parent geology is approximately 200 cm.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2139352WLP 2614
151Ames 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
152NA 87204RJL2022FLAL-019Ilex coriacea (Pursh) Chapm. Florida, United StatesNA2022COLLECTED08/02/2022Corner of San Jose Street and South 28th Avenue just east of Avalon Beach, FL.30.53172700, -87.090589003Growing in full sun to part shade in moist to wet areas, often with sphagnum moss along the edges, just above the water in ditches and waterways. Population is so dense that plants are crowding out other species. 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 material2138707NA 87204
153WLP 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
154WLP 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
155WLP 2576RJL2022-001Amelanchier arborea (F. Michx.) Fernald Maryland, United StatesNA2022COLLECTED05/25/2022Plants growing in open woodlands and part shade along unnamed Elkton State Forest gravel road over a distance of approximately 5 kilometers labelled as the address of 717 Irishtown Rd, North East, MD 21901.39.58089500, -75.9150590073Plants are found regularly but scattered along the unnamed gravel road as well as in open understory of the upland woodlands. Plants growing in a mesic to dry, well-drained habitat of mixed deciduous and evergreen woodlands comprised primarily of acid-loving plants. Plants are growing in part shade and open understory shade. The soils in the collection area are generally described as a complex series of fluviomarine deposits. The soils range from a thin loam layer at the surface to varying levels of loam to sandy loam and/or extremely gravelly sandy clay loam strata, depending upon geographical location (ie. Hillslope summits, slopes, footslopes, swales, etc.). The primary soil types in the collection area are classified as Russett-Christiana-Hambrook Complex and/or Sassafras and Croom Soils; though, others may intersect and overlay in specific areas.Wild material2138095WLP 2576
156Ames 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
157NA 88189NCBG-384Baccharis halimifolia L. Virginia, United StatesNA2021Wild material2132875NA 88189
158NA 88200NCBG-371Carpinus caroliniana Walter Virginia, United StatesNA2021Wild material2132869NA 88200
159NA 88334NCBG-390Ilex opaca Aiton Virginia, United StatesNA2021COLLECTED10/22/2015Caledon State Park: Caledon Marsh Trail: from visitors center, follow Boyd's Hole Trail northwest, continue left at triangle field and follw the Caledon Marsh trail. Population located at the end of trail along Caledo marsh edge and hillslope to the north.38.34408000, -77.168300002Marsh edge and slope.Wild material2132877NA 88334
160NA 88337NCBG-565Ilex verticillata (L.) A. Gray Maryland, United StatesNA2021COLLECTED10/03/2016Gunpowder Falls State Park: wetland near Hammerman Beach beach house: from Chase, MD, turn left onto Harewood Rd, then right onto Ebenezer Rd. Continue onto Grace's Quarters Rd for 0.5 miles, turn left onto Park Dr. Follow loop to Hammerman Beach. Population in woods opposite beach house.39.36469000, -76.342160000Flooded.Wild material2132923NA 88337
161NA 88415NCBG-424Pinus serotina Michx. North Carolina, United StatesNA2021Wild material2132885NA 88415
162NA 88464NCBG-372Viburnum nudum L. Virginia, United StatesNA2021Wild materialBRIGHT BLUE DRUPES2132870NA 88464
163OPGC 8492NCBG-237Typha latifolia L. North Carolina, United StatesOPGC2021Wild materialWider leaves than T angustifolia.2132859OPGC 8492
164OPGC 8493NCBG-239Typha latifolia L. North Carolina, United StatesOPGC2021Wild material2132860OPGC 8493
165OPGC 8506NCBG-526Xyris difformis Chapm. Maryland, United StatesOPGC2021Wild material2132902OPGC 8506
166OPGC 8508NCBG-536Typha angustifolia L. Virginia, United StatesOPGC2021Wild material2132909OPGC 8508
167W6 59984NCBG-315Eupatorium hyssopifolium L. North Carolina, United StatesW62021Wild material2132866W6 59984
168W6 59989NCBG-373Diospyros virginiana L. Virginia, United StatesW62021Wild material2132871W6 59989
169W6 59996NCBG-391Sorghastrum nutans (L.) Nash North Carolina, United StatesW62021Wild material2132878W6 59996
170W6 59998NCBG-395Eupatorium hyssopifolium L. Maryland, United StatesW62021Wild material2132880W6 59998
171W6 60001NCBG-399Sorghastrum nutans (L.) Nash Virginia, United StatesW62021Wild material2132883W6 60001
172W6 60002NCBG-405Andropogon gerardi Vitman Virginia, United StatesW62021Wild materialReceived as: Adropogon gerardii2132884W6 60002
173W6 60022NCBG-528Rhynchospora capitellata (Michx.) Vahl Maryland, United StatesW62021Wild material2132904W6 60022
174W6 60042NCBG-568Tridens flavus (L.) Hitchc. Maryland, United StatesW62021Wild material2132924W6 60042
175W6 60043NCBG-571Eleocharis quadrangulata (Michx.) Roem. Maryland, United StatesW62021Wild material2132925W6 60043
176W6 60044NCBG-572Aristida purpurascens Poir. var. virgata (Trin.) Allred Maryland, United StatesW62021Wild material2132952W6 60044
177W6 60048NCBG-580Schizachyrium scoparium (Michx.) Nash Maryland, United StatesW62021Wild material2132929W6 60048
178W6 60054NCBG-703Piptochaetium avenaceum (L.) Parodi North Carolina, United StatesW62021Wild material2132935W6 60054
179W6 60075NCBG-527Fimbristylis autumnalis (L.) Roem. & Schult. Maryland, United StatesW62021Wild material2132903W6 60075
180W6 60085MARSB-375Eupatorium serotinum Michx. New Jersey, United StatesW62021Wild material2137170W6 60085
181W6 60098MARSB-635Carex lurida Wahlenb. Delaware, United StatesW62021Wild materialThick green test tubed cleaner shaped inflorescence with long bracts extending beyond inflorescence.2137183W6 60098
182W6 60099MARSB-636Dichanthelium scoparium (Lam.) Gould Delaware, United StatesW62021Wild materialGrass with fuzzy, velvet like stem, green clasping leaves tannish green terminal seed head.2137184W6 60099
183NA 88402NCBG-633Lyonia ligustrina (L.) DC. Maryland, United StatesNA2021Wild material2116359NA 88402
184W6 58990NCBG-437Glyceria striata (Lam.) Hitchc. North Carolina, United StatesW62021Wild materialDrooping inflorescence; dark brown seeds2116308W6 58990
185W6 58997NCBG-445Glyceria striata (Lam.) Hitchc. Maryland, United StatesW62021Wild materialdrooping inflorescence2116315W6 58997
186W6 59000NCBG-448Schoenoplectus tabernaemontani (C. C. Gmel.) Palla Virginia, United StatesW62021Wild materialround culm2116318W6 59000
187W6 59005NCBG-455Avenella flexuosa (L.) Parl. Virginia, United StatesW62021Wild materialinflorescence drooping/nodding2116323W6 59005
188W6 59017NCBG-480Teucrium canadense L. North Carolina, United StatesW62021Wild material2116335W6 59017
189W6 59026NCBG-550Panicum virgatum L. North Carolina, United StatesW62021Wild material2116343W6 59026
190W6 59035NCBG-589Sorghastrum nutans (L.) Nash Virginia, United StatesW62021Wild material2116351W6 59035
191W6 59041NCBG-623Sorghastrum nutans (L.) Nash North Carolina, United StatesW62021Wild material2116357W6 59041
192W6 59062NCBG-676Andropogon gerardi Vitman Virginia, United StatesW62021Wild material2116376W6 59062
193NA 88281MARSB-497Cephalanthus occidentalis L. New Jersey, United StatesNA2021Wild materialGrowth formûthe plant is a shrub (i.e., a woody plant with several stems growing from the base)ûLeaf typeûthe leaf blade is simple (i.e., lobed or unlobed but not separated into leaflets)ûLeaves per nodeûthere are three leaves per node along the stemûthere are two leaves per node along the stemûLeaf blade edgesûthe edge of the leaf blade has teethûLeaf durationûthe leaves drop off in winter (or they wither but persist on the plant)ûarmature on plantûthe plant does not have spines, prickles, or thornsûLeaf blade lengthû80–150 mmûLeaf blade widthû23–150 mmûLeaf stalkûthe leaves have leaf stalksûFruit type (general)ûthe fruit is dry but does not split open when ripeûBark textureûthe bark of an adult plant is ridged or platedûthe bark of an adult plant is thin and smoothûTwig winter colorûbrownûgrayûredûBud scale numberûthere are no scales on the winter buds2113542NA 88281
194OPGC 8148MARSB-496Typha latifolia L. New Jersey, United StatesOPGC2021Wild materialStem shape in cross-sectionûthe stem is round or oval in cross-sectionûLeaf blade widthû5–29 mmûLeaf blade cross-sectionûthe leaf blade is flat or rolled in at the edgesûInflorescence positionûthe inflorescence is at the tip of the plantûInflorescence branchingûthe inflorescence is on one or more stems with no branchesûFruit type (general)ûthe fruit is like a seed, and surrounded by hairsûFruit lengthû10–15 mmûLeaf position on plantûsome leaf attachment points are above the midpoint of the stemûPerianth compositionûthere are long, thin hairs attached at the base of the acheneûthere are three bristles and three scales on narrow stalks, attached at the base of the acheneûFruit cross-sectionûthe fruit is triangular to terete (circular) in cross-section2113541OPGC 8148
195W6 58593MARSB-451Carex atlantica L. H. Bailey New Jersey, United StatesW62021Wild materialMultiple stellate seed heads per stem. Stems scabrous on the angles above. Perigynia greeen, usually several-nerved ventrally.2113523W6 58593
196W6 58613MARSB-498Scirpus cyperinus (L.) Kunth New Jersey, United StatesW62021Wild materialStem shape in cross-sectionûthe stem is roughly triangular in cross-sectionûthe stem is round or oval in cross-sectionûLeaf blade widthû3–10 mmûLeaf blade cross-sectionûthe leaf blade is flat or rolled in at the edgesûInflorescence positionûthe inflorescence is at the tip of the plantûInflorescence branchingûthe inflorescence is branchedûFruit type (general)ûthe fruit is like a seed, and surrounded by hairsûthe fruit is like a seed, and surrounded by scalesûFruit lengthû0.6–0.9 mmûLeaf position on plantûsome leaf attachment points are above the midpoint of the stemûthe attachment points of all the leaves are at or near the base of the plantûPerianth compositionûthere are bristles attached at the base of the acheneûFruit cross-sectionûthe fruit is lenticular (lens-shaped) in cross-sectionûthe fruit is triangular to terete (circular) in cross-section2113543W6 58613
197W6 58617MARSB-523Anatherum glomeratum (Walter) Voronts. & E. A. Kellogg New Jersey, United StatesW62021Wild materialLeaf blade widthû2.9–9.5 mmûInflorescence branchesûthe flowers are attached to branches rather than to the main axis of the inflorescenceûSpikelet lengthû3–5 mmûGlume relative lengthûboth glumes are as long or longer than all of the floretsûAwn on glumeûthe glume has no awnûOne or more floretsûthere is one floret per spikeletûLemma awn lengthû6–19 mmûLeaf ligule lengthû0.6–2.2 mmûAnther lengthû0.5–1.5 mm2113547W6 58617
198W6 58644MARSB-632Juncus effusus L. Delaware, United StatesW62021Wild materialRound stemmed rush with flower head sticking out from the side of the stem. Circular seeds/ seed heads.2113574W6 58644
199W6 58646MARSB-641Scirpus atrovirens Willd. Delaware, United StatesW62021Wild materialGrass with branching, drooping, inflorescence. Brown inflorescence with white seeds.2113576W6 58646
200W6 58649MARSB-647Scirpus atrovirens Willd. Delaware, United StatesW62021Wild materialGreen, glabrous culm. Up to 8 alternate leaves along culm, yellowish green to dark green. Inflorescence composed of 1-3 compound umbels of spiklets. 3 more more leafy bracts under inflorescence. Inflorescence, reddish brown.2113579W6 58649
201W6 58650MARSB-653Scirpus cyperinus (L.) Kunth Delaware, United StatesW62021Wild materialPerennial sedge with attractive, copper-colored, woolly inflorescences. It grows in dense tussocks and has white flowers. When seeds are ready, inflorescences turn dark and woolly, with small orange seeds.2113580W6 58650
202W6 58651MARSB-654Chasmanthium laxum (L.) H. O. Yates Delaware, United StatesW62021Wild materialSmall grass that has triangle shaped seed heads lining the upper stem.2113581W6 58651
203W6 58652MARSB-664Coleataenia anceps (Michx.) Soreng subsp. anceps Delaware, United StatesW62021Wild materialRhizomatous perennial grass, stems up to 4 feet tall, blades are erect, inflorescence is a panicle bearing pale green or yellowish spikelets.2113582W6 58652
204W6 58653MARSB-665Tridens flavus (L.) Hitchc. Delaware, United StatesW62021Wild materialBunchgrass with purple/ reddish panicle inflorescence.2113583W6 58653
205NA 87611ZARKS-030Rhododendron prinophyllum (Small) Millais Arkansas, United StatesNA2020COLLECTED10/05/2014King's River Falls Natural Area; King's River, downstream of junction of county roads 3415 and 3500 along trail leading from parking area and trail sign.35.90106000, -93.57456000514Mesic, mixed deciduous forest; growing on ledge along river, in rocky soil.Wild materialSee NA 84645 for material received from the Arnold Arboretum in 2017.2115796NA 87611
206W6 57966NCBG-306Rhus copallinum L. Virginia, United StatesW62020Wild material 2106478W6 57966
207NA 86848ZARKS-025Acer saccharum Marshall subsp. leucoderme (Small) Desmarais Arkansas, United StatesNA2020COLLECTED10/09/2014Cedar Fourche Creek; Harper Grocery Rd. at Rock Springs Rd.34.66470800, -93.26778900209Mesic, mixed deciduous forest; growing on the bank just above a small streamWild material2115797NA 86848
208NA 87036Site 3A/Live Oak Landing/Holmes Creek SiteMagnolia ashei Weath. Florida, United StatesNA2020COLLECTED07/15/2020Along Holmes Creek at Live Oak Landing.30.59208000, -85.8375000011Shade to partial shade of bluffs above the creek in well-drained mesic to dry deciduous woodlands with a few broadleaved and coniferous evergreens.Wild materialAlthough these were collected without any field collection number, seeds from individual trees were separated with letter identifiers that will be maintained with the qualifier (seedling) records. The relationships are as follows: 1. Maternal letter G, NA 87036-J, L, P, and T; maternal letter H, NA 87036-V; maternal letter K, NA 87036-X, Z, and H1; maternal letter N, NA 87036-H2. In addition, three seedlings' maternal letters were lost, and these will be NA 87036-H3, H4, and H5. See the following accessions for earlier collections from this same site/population, listed in our records as "Site 3A/Live Oak Landing/Holmes Creek Site": NA 81555 (2013), NA 82745 (2015), and NA 82745.01 (2019).2109403NA 87036
209NA 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
210NA 86519P, Thompson 18Quercus oglethorpensis W. H. Duncan Alabama, United StatesNA2020COLLECTED10/15/2015Between timber and hunting properties on a side of County Road 14, ca 3.5 air miles west of Catherine, Alabama. [The GPS coordinates provided, 32.177130 deg. N, 87.522820 deg. W, appear to be slightly east of the collecting site in neighboring Wilcox County. -SBL]32.17712000, -87.52281000Mesic roadside.Wild materialFor more information about the project for which this material was collected, see M. Lobdell and P. Thompson, Ex-situ Conservation of _Quercus oglethorpensis_ in Living Collections of Arboreta and Botanical Gardens in _Proceedings of Workshop on Gene Conservation of Tree Species--Banking on the Future_.2109228NA 86519
211WLP 2019MARSB-978Viburnum dentatum L. New York, United StatesNA2019COLLECTED08/09/2019Richmond County; Staten Island; William T. Davis Wildlife Refuge.40.59320000, -74.16770000Red maple/sweetgum swamp forest in partial shade; growing in moist, poorly drained sand/loam soil.Seed collected from 25 plants in a population of 40, found over a 500 m by 200 m area. Seed maturation: middle.2109168WLP 2019
212WLP 2021MARSB-980Viburnum dentatum L. New York, United StatesNA2019COLLECTED08/16/2019Richmond County; Staten Island; Blue Heron Park.Red maple forest in full shade; growing in moist, poorly drained silt/sand soil.Seed collected from 3 plants in population of 25, over an area of 20 square meters; population shaded out, very little seed/flower. Deer browse also heavy throughout park. Seed maturation: middle.2109170WLP 2021
213Ames 35688NCBG-553Monarda punctata L. North Carolina, United StatesNC7SEED2019Wild material2098470Ames 35688
214NA 88140NCBG-280Aralia spinosa L. North Carolina, United StatesNASEED2019Wild material2098388NA 88140
215NA 88146NCBG-309Aralia spinosa L. Virginia, United StatesNASEED2019Wild material2098406NA 88146
216NA 88150NCBG-317Aralia spinosa L. Virginia, United StatesNASEED2019Wild material2098410NA 88150
217NA 88154NCBG-323Pinus taeda L. North Carolina, United StatesNASEED2019Wild material2098414NA 88154
218NA 88155NCBG-324Clethra alnifolia L. North Carolina, United StatesNASEED2019Wild material2098415NA 88155
219NA 88156NCBG-326Cephalanthus occidentalis L. North Carolina, United StatesNASEED2019Wild material2098416NA 88156
220NA 88161NCBG-354Ilex opaca Aiton Virginia, United StatesNASEED2019COLLECTED10/14/2015Belle Isle State Park (Rappahanock River): from park entrance, continue on State Rte. 683/Belle Isle Rd. Turn right onto Creek Landing Road. Park at end of road, follow Mulberry Trail. Population along boardwalk as you walk toward the canoe launch.37.78222000, -76.604190002Riverside forest.Wild material2098425NA 88161
221NA 88165NCBG-450Viburnum dentatum L. Virginia, United StatesNASEED2019Wild material2098452NA 88165
222NA 88169NCBG-665Kalmia latifolia L. Virginia, United StatesNASEED2019Wild material2098504NA 88169
223NA 88171NCBG-667Kalmia latifolia L. Maryland, United StatesNASEED2019Wild material2098506NA 88171
224OPGC 7982NCBG-599Rhexia mariana L. Maryland, United StatesOPGCSEED2019Wild material2098480OPGC 7982
225W6 57468NCBG-285Parthenocissus quinquefolia (L.) Planch. Virginia, United StatesW6SEED2019Wild material2098392W6 57468
226W6 57538NCBG-497Cyperus strigosus L. North Carolina, United StatesW6SEED2019Wild material2098462W6 57538
227W6 57549NCBG-566Parthenocissus quinquefolia (L.) Planch. Maryland, United StatesW6SEED2019Wild material2098473W6 57549
228W6 57562NCBG-611Alnus serrulata (Aiton) Willd. Virginia, United StatesW6SEED2019Wild material2098486W6 57562
229W6 57570NCBG-631Alnus serrulata (Aiton) Willd. Maryland, United StatesW6SEED2019Wild material2098494W6 57570
230W6 57572NCBG-635Alnus serrulata (Aiton) Willd. Maryland, United StatesW6SEED2019Wild material2098496W6 57572
231W6 57584NCBG-671Ageratina altissima (L.) R. M. King & H. Rob. var. altissima Maryland, United StatesW6SEED2019Wild material2098508W6 57584
232W6 57586NCBG-678Saccharum giganteum (Walter) Pers. North Carolina, United StatesW6SEED2019Wild material2098510W6 57586
233WLP 3096NCBG-435Acer rubrum L. North Carolina, United StatesNASEED2019Wild material2098450WLP 3096
234WLP 2505Old U.S. 84Hydrangea quercifolia W. Bartram Mississippi, United StatesNA2019COLLECTED12/17/2017Along Old U.S. 84, approximately 4 miles west of Mississippi/Alabama state border and 300 m west of the Chickasawhay River. 31.74537000, -88.52251300Limestone cliff along road.Wild materialSpecimens in nature represented as fairly small plants with abundant flowering (2017). 2106215WLP 2505
235WLP 2506Cat's Cove Nature PreserveHydrangea quercifolia W. Bartram Mississippi, United StatesNAFLOWER2019COLLECTED12/17/2017Cat's Cove Nature Preserve, Smith County. Approximately 4 mi northwest of Bay Springs and 500 ft east of bridge where Highway 18 crosses Tallahala Creek.31.99742000, -89.35637200Limestone cliff and steep bluff above creek.Wild materialFlower profusion was variable in the wild population. The plants growing in sunnier locations had more flowers than those growing further into the forest.2106216WLP 2506
236WLP 2507LeFleur's Bluff State ParkHydrangea quercifolia W. Bartram Mississippi, United StatesNAFLOWER2019COLLECTED12/18/2017LeFleur's Bluff State Park, Jackson, Hinds County, MS. Approximately 400 m north-northwest of the Pearl River and 150 m east of the Mississippi Museum of Natural Science. On bluff along trail near stairs and in ravine west of trail.32.32533000, -90.15570500Bluff and ravine above cypress swamp.Wild materialMajority of specimens noted in nature did not flower in 2017. Some of the individuals had persistent leaves on 18 December 2017.2106217WLP 2507
237WLP 2526Franklin D. Roosevelt State ParkHydrangea quercifolia W. Bartram Georgia, United StatesNAFLOWER2019COLLECTED11/28/2018Franklin D. Roosevelt State Park, Harris County. Approximately 1.9 miles southeast of Pine Mountain along Mountain Creek.32.84099500, -84.83899300Shady streambank.Wild materialMeasurements of sampled specimen taken in nature: Height 47 to 101 in.; width 27 to 99 in.2106236WLP 2526
238WLP 2535Little River CanyonHydrangea quercifolia W. Bartram Alabama, United StatesNAFLOWER2019COLLECTED12/12/2018Little River Canyon National Park, DeKalb and Cherokee Counties. North end of population is 6.5 miles southeast of Fort Payne on the trail to the Little River Falls Overlook. Most of the sampled hydrangeas are along Cherokee County 275 and Little River Canyon Rim Parkway.34.39263100, -85.62385700Shady rim of canyon.Wild materialMeasurements of sampled speciimen taken in nature: Height 48 to 119 in.; width 26 to 115 in. Measurements for each specimen sampled may be provided upon request.2106245WLP 2535
239WLP 2540Cheaha MountainHydrangea quercifolia W. Bartram Alabama, United StatesNA2019COLLECTED12/01/2018Cheaha Mountain (Cheaha State Park and Talladega National Forest), Cleburne County. Approximately 9 miles south of Oxford. Hydrangeas are along Cheaha Road, Highway 281 and Skyway Mountainway.33.52890000, -85.74647800Rocky mountainside.Wild materialMeasurements of sampled specimens taken in nature: Height 55 to 106 in.; width 31 to 132 in. Measurements for each specimen sampled may be provided upon request.2106250WLP 2540
240GPRU 167MARSB-281Prunus serotina Ehrh. New Jersey, United StatesGENSEED2019Wild material2097554GPRU 167
241NA 88109MARSB-425Ilex opaca Aiton New Jersey, United StatesNASEED2019COLLECTED11/03/2015Tuckahoe Wildlife Management Area: take exit 20 off Garden State Parkway, route 50 north. Turn right onto Tuckahoe Road, left on Woods Road, right onto Washington Ave, and follow to Tuckahoe Lake.39.27769000, -74.731110000Pitch pine lowland swamp forest.Wild material2097626NA 88109
242NA 88111MARSB-428Lyonia ligustrina (L.) DC. New Jersey, United StatesNASEED2019Wild material2097629NA 88111
243NA 88114MARSB-533Ilex glabra (L.) A. Gray New Jersey, United StatesNASEED2019COLLECTED10/28/2016Tuckahoe Wildlife Management Area: from Tuckahoe, take route 50 north to Mosquito Landing Rd. Drive down Mosq. Landing Rd. to Middle Town Rd. Make right onto Meadow Rd. Population is in power line cut.39.28080000, -74.737330003Seasonal fresh water meadow.Wild material2097648NA 88114
244NA 88119MARSB-650Viburnum dentatum L. Delaware, United StatesNASEED2019Wild material2097671NA 88119
245NA 88120MARSB-651Lindera benzoin (L.) Blume Delaware, United StatesNA2019Wild material2097672NA 88120
246OPGC 7909MARSB-712Rhexia mariana L. New Jersey, United StatesOPGCSEED2019Wild material2097687OPGC 7909
247W6 57085MARSB-218Scirpus atrovirens Willd. New York, United StatesW6SEED2019Wild material2097524W6 57085
248W6 57143MARSB-333Eupatorium hyssopifolium L. New Jersey, United StatesW6SEED2019Wild material2097582W6 57143
249W6 57144MARSB-334Tridens flavus (L.) Hitchc. New Jersey, United StatesW6SEED2019Wild material2097583W6 57144
250W6 57162MARSB-376Tridens flavus (L.) Hitchc. New Jersey, United StatesW6SEED2019Wild material2097601W6 57162
251W6 57189MARSB-427Alnus serrulata (Aiton) Willd. New Jersey, United StatesW6SEED2019Wild material2097628W6 57189
252W6 57237MARSB-669Scirpus cyperinus (L.) Kunth Delaware, United StatesW6SEED2019Wild material2097676W6 57237
253W6 57244MARSB-689Andropogon gerardi Vitman Delaware, United StatesW6SEED2019Wild material2097683W6 57244
254WLP 157NACPEC19-026Carpinus caroliniana Walter Kentucky, United StatesNA2019COLLECTED09/09/2019Madison County; Berea College Forest: Gabertown Road, near junction of Gabertown Road (KY 1617) + Scaffold Cane (KY595)37.54309800, -84.27086000292Former Pinus taeda plantationWild material2110469WLP 157
255WLP 163NACPEC19-046BHydrangea cinerea Small Georgia, United StatesNA2019COLLECTED09/14/2019Walker County; Lula Lake Land Trust: Bridge from parking lot to South Creek Trail34.92114500, -85.38035700373Limestone bluffs surrounding dry creek bed in mixed mesophytic forestWild material2110475WLP 163
256WLP 164NACPEC19-047Kalmia latifolia L. Georgia, United StatesNA2019COLLECTED09/14/2019Walker County; Lula Lake Land Trust: Off of South Creek trail on North side of bridge from parking lot34.92134100, -85.38051100373Riparian zone, wet slope of creek, moist, sandy banksWild material2110476WLP 164
257WLP 167NACPEC19-053Mitchella repens L. Georgia, United StatesNA2019COLLECTED09/14/2019Walker County; Lula Lake Land Trust: Middle Trail near top, also collected along Connector Trail to Middle Trail from parking lot.34.93141800, -85.36991400469Mesic, sandy, rocky Oak-Hickory woodland slope - likely acidicWild material2110479WLP 167
258WLP 168NACPEC19-054Viburnum acerifolium L. Georgia, United StatesNA2019COLLECTED09/14/2019Walker County; Lula Lake Land Trust: Middle Trail near top.34.93146200, -85.37018800449Mesic, sandy, rocky Oak-Hickory woodland slope - likely acidicWild material2110480WLP 168
259WLP 1201AOK027Diospyros virginiana L. Arkansas, United StatesNA2019COLLECTED10/07/2018Franklin County; White Rock; Ozark National Forest: Shores Lake Recreation Area at the edge of Shores Lake and pavilion.35.63916000, -93.95958000206In maintained area at forest edge; 25 percent shade.50 seeds collected from many individuals [or rather, more than one; exact number not specified or estimated]. Species occasional, with patchy distribution.2109071WLP 1201
260WLP 1552AOK018Platanus occidentalis L. Arkansas, United StatesNA2019COLLECTED10/06/2018Madison County; Venus; Kings River Falls Natural Area (Arkansas Natural Heritage Commission property).35.89573000, -93.58238000521East side of hiking trail, near agricultural field; stream on opposite side of trail; open [full sun].600 seeds collected from one individual. Species occasional, with patchy distribution.2109070WLP 1552
261WLP 888AOK014Callicarpa americana L. Arkansas, United StatesNA2019COLLECTED10/05/2018Johnson County; Hagarville; Ozark National Forest: Little Sulphur Creek, along an unmarked trail off of Forest Service Road 1826.35.57135000, -93.28193000207Mixed hardwood forest; 50 percent shade.This specimen appears to be the uncommon white-fruited form [=C. americana Lactea Group]. 300 seeds collected from one individual. Species frequent, with patchy distribution.2109069WLP 888
262WLP 307AF2018-001Acer saccharum Marshall subsp. floridanum (Chapm.) Desmarais Virginia, United StatesNA2018COLLECTED09/10/2018James City County; ; Near Grove Creek, near the roadside in front of the wastewater plant at the end of Log Cabin Beach Rd.37.21613000, -76.6334800047Roadside near creek.Several large trees along roadside, fairly common. Herbarium voucher collected (see barcode NA0103770).2108850WLP 307
263NA 88024NCBG-316Lindera benzoin (L.) Blume Virginia, United StatesNASEED2018Wild material1965909NA 88024
264NA 88035NCBG-622Ilex glabra (L.) A. Gray North Carolina, United StatesNASEED2018COLLECTED10/27/2016From Roanoke Island, head SW on US-64 W, turn left onto US-264 W, population on left for approximately 12 miles.35.71316000, -75.768190001Pine-inkberry swamp.Wild material1965992NA 88035
265NA 88036NCBG-632Clethra alnifolia L. Maryland, United StatesNASEED2018Wild material1965997NA 88036
266NA 88208NCBG-721Ceanothus americanus L. North Carolina, United StatesNASEED2018Wild materialCeanothus americanus1966030NA 88208
267OPGC 7227NCBG-236Typha angustifolia L. North Carolina, United StatesOPGCSEED2018Wild material1965879OPGC 7227
268OPGC 7801NCBG-737Aletris farinosa L. North Carolina, United StatesOPGCSEED2018Wild materialAletris farinosa1966038OPGC 7801
269W6 54628NCBG-202Juncus effusus L. North Carolina, United StatesW62018Wild materialJuncus effusus1965854W6 54628
270W6 54629NCBG-203Carex lurida Wahlenb. North Carolina, United StatesW62018Wild materialCarex lurida1965855W6 54629
271W6 54630NCBG-204Juncus effusus L. Virginia, United StatesW62018Wild materialJuncus effusus1965856W6 54630
272W6 54631NCBG-206Carex vulpinoidea Michx. North Carolina, United StatesW62018Wild materialCarex vulpinoidea1965857W6 54631
273W6 54724NCBG-456Carex lurida Wahlenb. Virginia, United StatesW6SEED2018Wild materialCarex lurida1965950W6 54724
274W6 54775NCBG-652Pluchea odorata (L.) Cass. Virginia, United StatesW6SEED2018Wild materialPluchea odorata1966001W6 54775
275W6 54787NCBG-699Chrysopsis mariana (L.) Elliott North Carolina, United StatesW6SEED2018Wild materialChrysopsis mariana1966013W6 54787
276W6 54791NCBG-704Danthonia sericea Nutt. North Carolina, United StatesW6SEED2018Wild materialDanthonia sericea1966017W6 54791
277W6 54793NCBG-708Marshallia obovata (Walter) Beadle & F. E. Boynton North Carolina, United StatesW6SEED2018Wild materialMarshallia obovata1966019W6 54793
278W6 54800NCBG-716Juncus gerardi Loisel. Maryland, United StatesW6SEED2018Wild materialJuncus gerardii var. gerardii1966026W6 54800
279Ames 34782MARSB-656Rhus copallinum L. Delaware, United StatesNC7SEED2018COLLECTED09/25/2016Milford Neck Wildlife Area along Milford Neck Road just west of Thompsonville.38.99494000, -75.423380007MeadowWild material1964819Ames 34782
280NA 88009MARSB-761Baccharis halimifolia L. Delaware, United StatesNASEED2018Wild material1964846NA 88009
281W6 54006MARSB-131Juncus effusus L. Delaware, United StatesW6SEED2018Wild materialJuncus effusus1964722W6 54006
282W6 54009MARSB-152Carex crinita Lam. Delaware, United StatesW6SEED2018Wild materialCarex crinita1964725W6 54009
283W6 54021MARSB-217Scirpus cyperinus (L.) Kunth New York, United StatesW6SEED2018Wild materialScirpus cyperinus1964737W6 54021
284W6 54032MARSB-287Carex crinita Lam. New Jersey, United StatesW6SEED2018Wild materialCarex crinita1964748W6 54032
285W6 54033MARSB-288Carex lurida Wahlenb. New Jersey, United StatesW6SEED2018Wild materialCarex lurida1964749W6 54033
286OPGC 5470JDC/BN/2018/056/869Baptisia nuttalliana Small Arkansas, United StatesOPGCFRUIT2018COLLECTED07/17/2018Located circa 2.60 miles northwest of Brightstar off Miller Road 159, Miller Road 74, Miller Road 75, Miller Road 154 and highway 237, Miller County33.14091000, -94.02229000109Roadside. Edges of woods.Wild materialPlants essentially all black with seeds past maturity by approximately 2-3 weeks, plants starting to break off at ground level and fruiting capsules starting to split at time of collection (17 July 2018). Seed quality rather poor at time of collection largely due to weevils. 1964612OPGC 5470
287Ames 34204JDC/ML/2018/030/843Monarda luteola Singhurst & W. C. Holmes Arkansas, United StatesNC7Image2018COLLECTED05/22/2018Located 2.62 miles northwest of Brightstar off Miller Road 159 just 0.54 miles north of junction with state highway 160, Miller County33.14091000, -94.02229000109Roadside. Open woods.Wild materialPlants with lemon scent, pubescent stems and leaves with faint yellow flowers measuring circa 2.0' in height. Leaves longer than internodes. Plants likely reached peaked flower around 16 May 2018. Seeds likely reached full maturity around first week in July (2018).1963387Ames 34204
288WLP 1983MARSB-806Viburnum dentatum L. Delaware, United StatesNA2017COLLECTED08/16/2017Sussex County; ; Bombay Hook National Wildlife Refuge: Marshtown Road.39.18963000, -75.440880003Mixed hardwood swamp; swales/terraces. Sand soil (Pineyneck series). Land used for conservation and recreation.Wild materialSeeds collected from 60 plants; 100 plants found in an area of two acres. Two herbarium vouchers collected on 16 Aug. 2017; held at Smithsonian and MARSB. Material identified in field by Clara Holmes on 16 Nov. 2017. Ecoregion: 63E -- Middle Atlantic Coastal Plains (Omernik).2108827WLP 1983
289NA 84645ZARKS-030Rhododendron prinophyllum (Small) Millais Arkansas, United StatesNA2017COLLECTED10/05/2014King's River Falls Natural Area; King's River, downstream of junction of county roads 3415 and 3500 along trail leading from parking area and trail sign.35.90106000, -93.57456000514Mesic, mixed deciduous forest; growing on ledge along river, in rocky soil.Wild materialSee NA 87611 for plants of the same collection received from Morris Arboretum in 2020.2108758NA 84645
290NA 84577RJL-RM001Halesia diptera J. Ellis Texas, United StatesNA2017COLLECTED07/22/2017Along either side of a clear creek on private property approximately 1.42 kilometers north of Texas Recreational Road 255 in northeastern Jasper County.31.07135000, -93.94985000107Plants growing along the embankments of the clear creek just above normal flood stage in primarily deciduous woodlands with some broadleaved evergreens and conifers. Plants are growing in part shade; some direct sunlight occurs during mid-day hours for 1-2 hours. Soils sandy and topped with a generous undisturbed decomposed litter layer. Slope: 10 percent. Aspect: variable.Wild material1953812NA 84577
291NA 84578RJL-RM002Magnolia pyramidata W. Bartram Texas, United StatesNA2017COLLECTED07/22/2017Newton County Road 425, about 2.8 miles south of Texas Recreational Road 255.30.85996000, -93.89596000105Along roadsides and among young loblolly pines in forestry plantation. Plants growing in part shade to full sun in heavily regenerating roadside woodlands associated with loblolly pine plantations. Plants are growing in well drained, highly sandy soils.Wild material1953814NA 84578
292NA 84158P. Thompson 19Quercus oglethorpensis W. H. Duncan Alabama, United StatesNA2017COLLECTED10/15/2015On side of CR 14, ca 3.5 air miles west of Catherine, Alabama.32.17725000, -87.51492000Growing on moist roadside between timber and hunting properties.Wild material2132959NA 84158
293NA 86662SE-2017-016Quercus shumardii Buckley Georgia, United StatesNA2017COLLECTED10/14/2017Oconee National Forest: Monticello Glades.33.25416000, -83.68386000185Moist woods.Wild materialOn the original collection notes, this was assigned the field collection number SE-2017-017, but it was corrected to SE-2017-016 later.2141807NA 86662
294NA 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
295WLP 1180NA 83893Euonymus americanus L. Kentucky, United StatesNA2016COLLECTED09/27/2016Cumberland Falls State Park, Trail #6 (Cumberland Falls Trail). Stairs above visitor center entrance at Trail #6 trailhead.36.83700000, -84.343000002731951485WLP 1180
296WLP 1375NA 83887Kalmia latifolia L. Kentucky, United StatesNA2016COLLECTED09/27/2016Cumberland Falls State Park, Trail #6 (Cumberland Falls Trail).36.83700000, -84.34000000302Break in canopy along trail near telephone pole.1953494WLP 1375
297WLP 1432NA 83894Ostrya virginiana (Mill.) K. Koch Kentucky, United StatesNA2016COLLECTED09/27/2016Cumberland Falls State Park, Cumberland Falls Visitor Center.36.84000000, -84.343000002581952033WLP 1432
298WLP 1434NA 83915Nyssa sylvatica Marshall Kentucky, United StatesNA2016COLLECTED09/28/2016Cumberland Falls State Park; Cumberland Falls Visitor Center parking lot en route to Trail #2 trailhead. Overhanging road beyond water treatment plant and beyond shelter with fireplace, before circle of picnic tables.36.83800000, -84.337000002761952017WLP 1434
299WLP 147NA 83890Mitchella repens L. Kentucky, United StatesNA2016COLLECTED09/27/2016Whitley County; Cumberland Falls State Park, Trail #636.83700000, -84.34000000301Wild material2110320WLP 147
300WLP 1702NA 83914Rhus copallinum L. Kentucky, United StatesNA2016COLLECTED09/28/2016Cumberland Falls State Park; Cumberland Falls Visitor Center parking lot en route to Trail #2 trailhead. Left of roadside beyond water treatment plant and beyond shelter with fireplace, before circle of picnic tables.36.83700000, -84.338000001951563WLP 1702
301WLP 1703NA 83921Rhododendron maximum L. Kentucky, United StatesNA2016COLLECTED09/28/2016Cumberland Falls State Park; Cumberland Falls Trail #2 (Cumberland River Trail) at river's edge.36.83800000, -84.33200000302River's edge on uphill side.1952964WLP 1703
302WLP 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
303Ames 33745UC 108Aronia melanocarpa (Michx.) Elliott Tennessee, United StatesNC7Flower2016COLLECTED10/01/2009Near Caryville, Campbell County36.35786670, -84.21851670532Powerline cut and surrounding area of dry and wet woods. Wild materialThis accession is rather unique as it seems to morphologically/phenologically (NCRPIS field plots) represent the "southern form" of A. melanocarpa, a potentially a new Aronia species. This southern form was originally discovered by Brand et al. 2022 (Ploidy, genetic diversity and speciation of the genus Aronia) and is known for having glabrous stems and leaves and a distinct phyllotaxy than other Aronia species. However, this accession based on Brand et al. 2022 AFLP dendogram fits with diploid A. melanocarpa, but flow cytometry indicates it is tetraploid. Fruits tend to ripen the same time as diploid A. melanocarpa and three weeks ahead of tetraploid A. melanocarpa. 1942831Ames 33745
304Ames 33746UC 110aAronia melanocarpa (Michx.) Elliott Tennessee, United StatesNC7FRUIT2016COLLECTED10/01/2009Near Newcomb, Campbell County36.53751670, -84.15580000541Very dry, exposed rock spine with primarily organic soil and plants growing in cracks and pockets. Growing in association with Pinus virginiana, Quercus, Vaccinium, Gaylussacia, Castanea, Amelanchier, Magnolia ashei, Magnolia tripetala, Oxydendrum, Nyssa, Liquidambar styraciflua.Wild materialThis accession has been confirmed to represent the "southern form" of A. melanocarpa, potentially a new Aronia species. This southern form was originally discovered by Brand et al. 2022 (Ploidy, genetic diversity and speciation of the genus Aronia) and is known for having glabrous stems and leaves and a distinct phyllotaxy than other Aronia species. In addition, plants tend to bloom approximately two weeks later than all other Aronia taxonomic groups and the inflorescences/infructescences are more spreading and extended due to longer peduncles and pedicels within the cyme. Fruit maturity tends to occur 2 to 4 weeks later than tetraploid A. melanocarpa and 4 to 6 weeks later than diploid A. melanocarpa. Phenolic levels are much higher in comparison to other A. melanocarpa accessions (Brand et al., 2017 - Anthocyanins, total phenolics, ORAC and moisture content of wild and cultivated dark-fruited Aronia species.)1942832Ames 33746
305NA 82746Site 3B/Hightower Road at Holmes CreekMagnolia ashei Weath. Florida, United StatesNA2015COLLECTED07/31/2015Along Holmes Creek 0.2 miles west-southwest of Hard Castle Landing boat ramp at hte end of Hightower Road.30.60401000, -85.7688300011Shade to partial shade of deciduous woodlands 10 to 15 feet above the creek, surrounded by low lying swampy area.Wild materialOriginally just called Site 3, but the "A/B" has been added to distinguish the Live Oak Landing (3A) and Hightower Road (3B) material. For previous collections of this population, see NA 81556 (2013); for later collection, see NA 82746.01 (2019).1950860NA 82746
306NA 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
307NA 83066NA 83066Hamamelis vernalis Sarg. Arkansas, United StatesNA2015COLLECTED10/04/2014King's River Falls Natural Area; upstream of the junction of County Rds 3415 and 3500 and the bridge over Mink Creek branch of King's River; at the Dripping Springs Schoolhouse (1921).35.88946000, -93.58091000528Mesic, mixed deciduous forest; north-northeast running stream valley; gravel bank along seasonal stream in sandy/gravelly soil.Wild material1953405NA 83066
308W6 48814MARSB-115Aristida purpurascens Poir. New Jersey, United StatesW6SEED2015Wild material1922907W6 48814
309W6 48819MARSB-101Boehmeria cylindrica (L.) Sw. Maryland, United StatesW6SEED2015Wild material1922836W6 48819
310W6 48822MARSB-46Carex atlantica L. H. Bailey New Jersey, United StatesW6SEED2015Wild material1922838W6 48822
311W6 48853MARSB-102Eragrostis spectabilis (Pursh) Steud. Maryland, United StatesW6SEED2015Wild material1922857W6 48853
312W6 48903MARSB-116Tridens flavus (L.) Hitchc. Delaware, United StatesW6SEED2015Wild material1922889W6 48903
313W6 48850MARSB-085Hexasepalum teres (Walter) J. H. Kirkbr. New Jersey, United StatesW6SEED2015Wild material1922915W6 48850
314W6 48854MARSB-106Eragrostis spectabilis (Pursh) Steud. New Jersey, United StatesW6SEED2015Wild material1922916W6 48854
315W6 48867MARSB-59Juncus tenuis Willd. New York, United StatesW6SEED2015Wild material1922918W6 48867
316W6 48902MARSB-114Tridens flavus (L.) Hitchc. New Jersey, United StatesW6SEED2015Wild material1922931W6 48902
317NA 82038JDC/QM/2014/052/554Quercus michauxii Nutt. Missouri, United StatesNANUT2014COLLECTED09/19/2014Missouri: Mississippi County; Big Oak Tree State Park.36.64463600, -89.28721300108Native, wet woods. Growing in association with Fraxinus sp., Liquidambar styraciflua, Carya laciniosa, Quercus macrocarpa, and Ulmus sp.Wild materialAcorns rather green approximately 2-3 weeks away from peak maturity. Specimen sampled approximatley 100' in height.1922339NA 82038
318NA 82052JDC/MV/2014/078/580Magnolia virginiana L. Mississippi, United StatesNA2014COLLECTED09/22/2014Mississippi: Tishomingo County; Bottomlands of Foote Branch Creek off Highway 982.34.87692100, -88.28330100150Deciduous woods. Growing in association with Quercus michauxii, Acer rubrum, Alnus sp., Liquidambar styraciflua, Toxicodendron radicans, Pinus sp., Nyssa sylvatica, and Vaccinum sp.Wild materialImpressive specimens. Optimum timing of harvest. Largest specimen measuring 19" d.b.h. and approximately 80' in height.1922353NA 82052
319NA 82059JDC/MM/2014/088/590Magnolia macrophylla Michx. Alabama, United StatesNA2014COLLECTED09/23/2014Franklin County and Lawrence County; Small tributary to Little Bear Creek (Frankllin County) and also William B. Bankhead National Forest (Lawrence County).34.43544700, -87.58959100293Wild material1922360NA 82059
320NA 82071JDC/QM/2014/103/605Quercus michauxii Nutt. Mississippi, United StatesNA2014COLLECTED09/25/2014Chinchahoma Creek watershed near Ennis Road.33.38574900, -88.9225560098Wet, deciduous woods.Wild materialSpecimen sampled measured 26.75" d.b.h. and approximately 110' in height. Fruits still green.1922372NA 82071
321WLP 1251JDC/HQ/2014/067/569Hydrangea quercifolia W. Bartram Mississippi, United StatesNAPLANT2014COLLECTED09/21/2014Mississippi: Lafayette County; Holly Springs National Forest along County Road 244.34.51468900, -89.45669300132Deciduous woods. Higher elevation than surrounding area. East, northeast-facing 45 degree slope. Growing in association with Cornus florida, Nyssa sylvatica, Quercus alba, Pinus sp., Liquidambar styraciflua, Juniperus virginiana, Carya tomentosa, and Rhus typhina.Wild materialNumerous specimens. Attractive peeling bark and large (10" long) infructescences.1922345WLP 1251
322WLP 1422JDC/NS/2014/068/570Nyssa sylvatica Marshall Mississippi, United StatesNA2014COLLECTED09/21/2014Mississippi: Lafayette County; Holly Springs National Forest along County Road 244.34.50982900, -89.3571680095Floodplain. Wet woods. Growing in association with Liquidambar styraciflua, Acer negundo, Cetlis sp., Juniperus virginiana, Carya illinoinensis, Quercus nigra, and Quercus phellos.Wild materialFruits rather green. 1922346WLP 1422
323WLP 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
324DPRU 3200JDC/PA/2014/082/584Prunus americana Marshall Mississippi, United StatesDAV2014COLLECTED09/22/2014Tishomingo County, Mississippi - Extreme northeast corner of Tishomingo County near J.P. Coleman S.P.34.98170000, -88.20449700202Dry, pine-oak-hickory woods. Growing in association with Pinus sp., Liquidambar styraciflua, Fraxinus americana, Rhus typhina, Acer rubrum, Quercus stellata, and Carya sp.Wild materialFruits perfectly round, very ripe, and pinkish-red in color. Actively dropping at time of collection. The only specimens of this species noted during entire trip throughout northern Mississippi, parts of Arkansas, and northwest Alabama. There were two specimens a few feet from each other, but I suspect they were not genetically unique from each other due to the suckering nature of the species. Considering there was decent fruit production there must have been another Prunus sp. nearby.1921307DPRU 3200
325Ames 32794JDC/FP/2014/106/608Fraxinus pennsylvanica Marshall Mississippi, United StatesNC7SEED2014COLLECTED09/25/2014Along Sanders Road, Cypress Creek watershed, NW 1/4 of SW 1/4 of SW1/4 of Section 10, T17N, R13E, Oktibbeha County.33.34662400, -88.93148200115Wild material1921805Ames 32794
326NA 81984Lactea GroupCallicarpa americana L. Texas, United StatesNA2014COLLECTED08/30/2013Woodlands above Boykin Spring Lake.31.06266000, -94.2756500056Growing in partial shade of mixed deciduous and evergreen woodlands in well-drained to dry conditions.1951711NA 81984
327NA 81696SOIL-014Crataegus phaenopyrum (L. f.) Medik. Illinois, United StatesNA2014COLLECTED10/2013Horseshoe Lake Nature Preserve. Roadside edge of wildlife management area.37.13025000, -89.2895300099Mesic forest, growing in 1/2 shade in highly organic soil.Wild material1953201NA 81696
328NA 81709CSF-13-22Cephalanthus occidentalis L. Maryland, United StatesNA2013COLLECTED11/04/2013Cedarville State Forest near Brandywine/Waldorf, MD, at power transmission line corridor along small stream.38.64824000, -76.8349300061Growing along small stream that crossed the transmission line right-of-way.Wild material1951113NA 81709
329NA 81566NA 81566Rhododendron austrinum (Small) Rehder Florida, United StatesNA2013COLLECTED03/31/2013White River approximately 0.92 miles north of the confluence with the Escambia River in the Escambia River State Wildlife Management Area. [Originally listed as: "Buzzard�s Lake River approximately 0.92 miles north of the confluence with the Escambia River..."; GPS coordinates are along the White River, and well south of the confluence with Buzzards Lake River. -SBL]30.58168000, -87.222330002Partial shade along the river on small sand berm above the stream in mixed deciduous and broadleaved evergreen maritime forest occasionally inundated by tidal salt water.Wild material1953003NA 81566
330OPGC 3928PZSH2011-5Phlox carolina L. Florida, United StatesOPGC2011COLLECTED04/03/2011Gadsden County, In forested areas along a single unnnamed tributary of the Apalachicola river, immediately south of Woodruff Dam Road, approx 0.30 miles W of Chattahoochee.30.42345000, -84.5126900022In floodplain hardwood forest; Acer barbatum, Rapidophyllum hystrix, Parthenocissus quinquefolia, Bignonia capreolata, Liquidambar styraciflua, Phlox divaricata.Wild materialPlants 15-20 cm tall; Leaves elliptical-lanceolate, lustrous, dark adaxially, light green abaxially.1907062OPGC 3928
331OPGC 3457PZ10-209Phlox paniculata L. Ohio, United StatesOPGC2010COLLECTED09/01/2010Scioto Co. Just S of juncture of Rocky Fork Rd. (Co. Rd. 40) and Tick Hill-Koenig Rd. On W side of road.38.49520000, -83.14058000191Roadsie ditch; Impatiens pallida, Eupatorium purpureum, Aplectrum hyemale, Trillium grandiflorum, Polystichum acrostichoides, Magnolia tripetala, Liquidambar styracifluaWild materialErect, slender perennial to 1 m tall; flowers magenta-pink; leaves ovate-lanceolate with areolate veins, glabrous1897773OPGC 3457
332Ames 30541UC 105Aronia arbutifolia (L.) Pers. North Carolina, United StatesNC7PLANT2010COLLECTED10/21/2009Near West End, Moore County35.25260000, -79.49096700149Powerline easement. Mixed hardwood woods. Sandy soil overlaying a moist seep. Wild materialReceived as plants grown from seed collected from native/wild population. Accession is extremely vigorous with an upright growth habit. Low fruit/seed production in cultivation in central Iowa.1843095Ames 30541
333Ames 30542UC 106Aronia arbutifolia (L.) Pers. North Carolina, United StatesNC7PLANT2010COLLECTED10/21/2009Near Hoffman Road, Jackson Springs35.21046700, -79.57120000140Re-established longleaf pine ecosystem. Sandy soil overlaying moist seeps. Wild materialReceived as plants grown from seed collected from native/wild population. Accession is extremely vigorous and uniform displaying a very prostrate growth habit. Foliage is dense with leaves that are larger than the average A. arbutifolia.1843096Ames 30542
334Ames 30543UC 109Aronia arbutifolia (L.) Pers. Tennessee, United StatesNC7PLANT2010COLLECTED10/22/2009Near Rock Quarry Road, Newcomb, Campbell County36.53751700, -84.15580000541Very dry, exposed rock spine with primarily organic soil and plants growing in cracks and pockets. Wild materialReceived as plants grown from seed collected from native/wild population. Accession is extremely vigorous and dense, with a relatively upright growth habit that is broad. Leaves are larger than the average A. arbutifolia.1843097Ames 30543
335Ames 32070UC 105Aronia arbutifolia (L.) Pers. North Carolina, United StatesNC7FRUIT2010COLLECTED10/21/2009Near West End, Moore County35.25260000, -79.49096700149Powerline easement. Mixed hardwood woods. Sandy soil overlaying a moist seep. Wild materialSeparated from Ames 30541 due to its extremely tight, upright growth habit. This new accession will be maintained as a uniform accession.1912823Ames 32070
336Ames 32072UC 106Aronia arbutifolia (L.) Pers. North Carolina, United StatesNC7PLANT2010COLLECTED10/21/2009Near Hoffman Road, Jackson Springs35.21046700, -79.57120000140Re-established longleaf pine ecosystem. Sandy soil overlaying moist seeps. Wild materialSeparated from Ames 30542 due to open, spreading growth habit. This accession will be maintained as a uniform accession.1912825Ames 32072
337OPGC 3200TX-19Rudbeckia texana (Perdue) P. B. Cox & Urbatsch Texas, United StatesOPGC2010COLLECTED05/27/2010Upper West Gulf Coastal Plain. Jasper County. Roadside north of R255 between CR 61 and 60.31.04313900, -94.1583330048Roadside ROW/forest edge(adjacent to U.S. National Forest). Land form: Flat. Land Use: Roadside ROW. Geology: Sandstone. Soil Texture: Sandy. Soil Color: Tan.Wild materialPlants to 2 m tall, leathery leaves, rhizomatous; ray petals yellow.1897300OPGC 3200
338Ames 30485APS/GD/2010/006/041Gymnocladus dioicus (L.) K. Koch Arkansas, United StatesNC7FRUIT2010COLLECTED02/19/2010Alum Fork Saline River, 4.5 miles northeast of Lake Balboa, Saline County.34.68933400, -92.84397400153Floodplain. Rich, high organic matter substrate.Wild materialSpecimen measured 12.5" d.b.h. and 80-90'.1831344Ames 30485
339NA 78035AL #44Philadelphus inodorus L. Alabama, United StatesNA2008COLLECTED09/17/2008Just above the Cahaba River, near end of road and Caffee Creek.Wild material1913895NA 78035
340NA 78052NA 78052Ilex longipes Chapm. ex Trel. Alabama, United StatesNA2008COLLECTED09/19/2008Little River Canyon National Preserve, Little River Canyon, on trail near Lynn Overlook tributary.Rocky woodland on trail near Lynn Overlook tributary.1950410NA 78052
341WLP 1112LBJWC-1141Crataegus viridis L. Texas, United StatesNA2008COLLECTED11/16/2007Mann Tract, Trinity River National Wildlife Refuge, southwest of the City of Hardin.30.13738000, -94.775050000Fencerow/bottomland hardwood mixed forest, flat, clayey soil.Wild material1781868WLP 1112
342WLP 2307LBJWC-MLE-036Ostrya virginiana (Mill.) K. Koch Texas, United StatesNA2008COLLECTED09/28/2006Approximately 7 miles south of Alto, Texas on 294.31.63803000, -95.2131600094Mixed hardwood and pine/forest roadside; rolling hills. Reddish tan colored, sandy soil over sandstone.Wild material1781863WLP 2307
343NA 76035DE.001-2006Clethra alnifolia L. Delaware, United StatesNA2006COLLECTED10/18/2006Thompson's Island State Park.38.70111000, -75.089020005Woodland coastal. Elevation: 17 feet.Wild material1716201NA 76035
344DVIT 3151RJL VA2003-005Vitis rotundifolia Michx. Virginia, United StatesDAV2003COLLECTED09/05/2003Collected from Chesapeake, VA at the interchange of Business Route 168 (Battlefield Ave) and Route 168, next to a detention basin and shopping plaza on the west side of Battlefield Ave.36.73861111, -76.242500005Mixed deciduous and evergreen woodland, primarily comprised of deciduous trees in the over-story and a mixture of deciduous and evergreen species in the sub-canopy. Plants growing in part-shade to full sun where they produce abundant fruit.Breeding materialSeed collected from many individuals and massed. Associated plants: Acer rubrum, Carpinus caroliniana, Clethra alnifolia, fagus grandifolia, gelsemium nudiflorum, Hamamelis virginiana, Ilex opaca, Leucothoe racemosa, liquidambar styraciflua, Liriodendron tulipfera, Nyssa sylvatica, Oxydendrum arboreum, Persea borbonia, Quercus falcata, Quercus michauxii, Smilax sp., Stewartia malacodendron, Symplocos tinctoria and Vaccinium sp.1651338DVIT 3151