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ACCESSIONPLANT NAMETAXONOMYORIGINGENEBANKIMAGEAVAILABILITYRECEIVEDSOURCE TYPESOURCE DATECOLLECTION SITECOORDINATESELEVATIONHABITATIMPROVEMENT LEVELNARRATIVE
0PI 702720MARSB-360Schizachyrium scoparium (Michx.) Nash New Jersey, United StatesS9SEED2019Wild material2097597PI 702720
1PI 704845 sosV. parvifolium OR080-49Vaccinium parvifolium Sm. Oregon, United StatesCORSEED2018Wild material1957632PI 704845 sos
2PI 679629V. oxycoccos Red Run Bog FR 13Vaccinium oxycoccos L. West Virginia, United StatesCOR2014COLLECTED04/23/2014Red Run Bog, Monongahela National Forest. Tucker County. The bog is bisected by Canaan Loop Road (Forest Road 13)39.07228000, -79.473630001110Bog with two main areas (east and west) separated by forest which is interspersed with smaller boggy areas. Road runs through forested area. Gentle slope from 1115 m in the east to 1105 m in the west. The total area is approximately 100 acres.Wild materialPlants in bog include Spaghnum sp., Lycopodium sp., Rubus hispidus, Solidago uliginosa, Eriphorum virginicum, Pteridium aquilinum, Juncus sp., Carex spp., Aronia melanocarpa, and Vaccinium macrocarpon . Vegetation on surrounding slopes includes Picea rubens, Tsuga canadensis, Rhododendron maximum, Kalmia latifolia, Ilex montana, Gaultheria sp., and Viburnum prunifolium. Abies balsamea occurs on the edge of the bog.

Plant description: Abundant fruit. Fruit shape, size and color typical for species. Voucher collected Type of propagule collected: seed

Collectors: Williams, KA; Garvey, E; Polgar, R. CRANBERRY IGRR PROJECT		1919347PI 679629
3PI 679630V. macrocarpon Red Run Bog FR 13Vaccinium macrocarpon Aiton West Virginia, United StatesCOR2014COLLECTED04/23/2014Red Run Bog, Monongahela National Forest. Tucker County. The bog is bisected by Canaan Loop Road (Forest Road 13)39.07228000, -79.473630001110Bog with two main areas (east and west) separated by forest which is interspersed with smaller boggy areas. Road runs through forested area. Gentle slope from 1115 m in the east to 1105 m in the west. The total area is approximately 100 acres.Wild materialPlants in bog include Spaghnum sp., Lycopodium sp., Rubus hispidus, Solidago uliginosa, Eriphorum virginicum, Pteridium aquilinum, Juncus sp., Carex spp., Aronia melanocarpa, and Vaccinium oxycoccos . Vegetation on surrounding slopes includes Picea rubens, Tsuga canadensis, Rhododendron maximum, Kalmia latifolia, Ilex montana, Gaultheria sp., and Viburnum prunifolium. Abies balsamea occurs on the edge of the bog.

Plant description: Abundant fruit. Fruit shape, size and color typical for species. Voucher collected Type of propagule collected: seed

Collectors: Williams, KA; Garvey, E; Polgar, R. CRANBERRY IGRR PROJECT		1919348PI 679630
4PI 656860V. ovatum 178338Vaccinium ovatum Pursh Oregon, United StatesCORSEED2005COLLECTED09/30/2002506Generally closed canopy, douglas fir forest with Lithocarpus densiflora/Acer macrophylum understory. Dense shrub cover of Gaultheria shallon & others. Associated with Pteridium aquilinum, Mahonia aquilfolium, Rosa gymnocarpa.Wild materialSeeds of Success (SOS) program germplasm.1674047PI 656860
5PI 633672010Echinacea sanguinea Nutt. Louisiana, United StatesNC7HEAD1997COLLECTED08/08/1997Near Lucky, Bienville Parish. Please contact curator for specific site location.32.28333333, -93.05000000180Roadside at edge of pine woods. Full exposure with ~10 degrees of slope and a northern aspect. Sandy soil with low stoniness and fair drainage.Wild materialPlants were up to ~2.5 feet tall in relative abundance with rose colored flowers and some branching.1547201PI 633672
6PI 649044008Echinacea sanguinea Nutt. Louisiana, United StatesNC7HEAD1997COLLECTED08/07/1997Kisatchie National Forest, near Leesville, Vernon Parish. Please contact curator for specific site location.31.00000000, -93.16666667160Upland long-leaf pine. ~70% exposure on level ground. Sandy soil with no stones and fair drainage.Wild materialPlants were 2-2.5 feet tall in occasional abundance with light pink flowers and some branching.1547199PI 649044
7PI 604594Mapes 889Amaranthus hypochondriacus L. Puebla, MexicoNC7GREENHOUSE1995COLLECTED11/15/1993Jilotzingo, Municipal of Zacatlan.20.01666667, -97.900000001850Growing amoung stalks after Zea mays is harvested. Associated with Phaseolus, Sechim edule, Pteridium, Lopezia, Tagetes, Persea americana, Prunus domestica, Annona cherimola, Citrus aurantiifolia, Alnus, Yucca aloifolia, and Clethera.LandraceInflorescense very red.1505563PI 604594
8PI 561479Graham 1007Cuphea hookeriana Walp. Veracruz de Ignacio de la Llave, MexicoNC7SEED1988COLLECTED10/11/19884 km S of Tlilapan on Orizba-Zongolica road.1450Wild materialCommon on open, disturbed banks with Pteridium aquilinum; floral tube color varying from partly red to dark red; dorsal petals dark maroon, ventral petals absent; anthers pale purple.1456451PI 561479
9NA 891732025RJLSEUS-14Chionanthus sp.Florida, United StatesNA2026COLLECTED10/03/2025Choctawhatchee National Forest: the collection site is reached by foot (~0.5 km) along a loose sand road/firebreak from Martin Luther King, Jr. Boulevard, just east of the boundary for Hurlburt Field in Hurlburt Field/Ft. Walton Beach, FL. Collected from 30 deg. 26.859', -86 deg. 39.577' to 30 deg. 27.137', -86 deg. 39.580'; latitude and longitude of record calculated at the midpoint of these coordinates.30.44996000, -86.6596500010Dry to xeric conditions of well-drained, deep sandy soils on a relatively level area bordering a powerline in an open mixed mostly mixed evergreen and deciduous, somewhat disturbed habitat in sun to part shade. In areas “broadleaved scrub” vegetation is so dense, that it is almost impenetrable. Elevation: 9 to 11 meters. Slope: 0 to 3 percent. Aspect: Variable. Soil: The soils of this area are characterized as Foxworth Series (95 percent) sand, 0 to 5 percent slopes (8). Other soil series interbedded with the Foxworth Series, vary in percentages from 1-4 percent including Lakeland and Chipley. The Foxworth Series consists of very deep, moderately well to somewhat excessively drained, rapid to very rapid permeable soils on broad uplands and side slopes. They formed in sandy marine or eolian sediments in the Southern Coastal Plain (MLRA 133A), The Eastern Gulf Coast Flatwoods (MLRA 152A), The Atlantic Coast Flatwoods (153A) and the Tidewater Area (153B). Thickness of the grayish brown to light yellowish-brown sand exceeds 2 meters. Reaction ranges from very strongly acid to slightly acid throughout. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). Geology: The underlying geology of this area is characterized as 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 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).Wild materialReceived as C. cf. henryae2193307NA 89173
10W6 62512FWS0300-100Sporobolus cryptandrus (Torr.) A. Gray Michigan, United StatesW6SEED2025Wild material2192210W6 62512
11W6 62513FWS0300-102Sorghastrum nutans (L.) Nash Michigan, United StatesW6SEED2025Wild materialNear active artillery range2192211W6 62513
12W6 62521FWS0300-111Chamaenerion angustifolium (L.) Scop. subsp. angustifolium Michigan, United StatesW6SEED2025Wild material2192219W6 62521
13W6 62527FWS0300-130Solidago hispida Muhl. ex Willd. Michigan, United StatesW6SEED2025Wild materialReceived as: Solidago hispida2192225W6 62527
14W6 62528FWS0300-131Symphyotrichum urophyllum (Lindl.) G. L. Nesom Michigan, United StatesW6SEED2025Wild material2192226W6 62528
15W6 62541FWS0300-65Coreopsis lanceolata L. Michigan, United StatesW6SEED2025Wild materialOnly scouted the part of the population on USFWS property2192239W6 62541
16W6 62542FWS0300-66Danthonia spicata (L.) P. Beauv. ex Roem. & Schult. Michigan, United StatesW6SEED2025Wild material2192240W6 62542
17W6 62543FWS0300-67Avenella flexuosa (L.) Parl. Michigan, United StatesW6SEED2025Wild material2192241W6 62543
18W6 62546FWS0300-97Schizachyrium scoparium (Michx.) Nash Michigan, United StatesW6SEED2025Wild materialThere is Solidago vossii in the area.2192244W6 62546
19W6 62547FWS0300-98Andropogon gerardi Vitman Michigan, United StatesW6SEED2025Wild materialThere is Solidago vossii in the area.2192245W6 62547
20W6 62548FWS0300-99Elymus canadensis L. Michigan, United StatesW6SEED2025Wild material2192246W6 62548
21W6 62555FWS0502-51Scirpus cyperinus (L.) Kunth Pennsylvania, United StatesW6SEED2025Wild materialClear cut forest2192253W6 62555
22W6 62556FWS0502-52Carex lupulina Muhl. ex Willd. Pennsylvania, United StatesW6SEED2025Wild materialLogged forested wetland2192254W6 62556
23W6 62597TYT-3Achillea millefolium L. California, United StatesW6SEED2025Wild materialYarrow hidden amongst grasses and ferns.2192295W6 62597
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 885822024RJLFL-013Cornus florida L. Florida, United StatesNA2024COLLECTED11/13/2024Woodland edge along the south side of Bud Bass Road (DOF B48), 0.30 kilometers east of the junction with Norman Riley Road.30.75753300, -86.8045760039Mixed evergreen and deciduous forests in part shade in a mesic- to mesic-dry situation. Slope: 0 percent. Aspect: North. The underlying geology of this area is characterized as Citronelle Formation of the Pliocene period. The Citronelle Formation is widespread in the Gulf Coastal Plain. The type section for the Citronelle Formation, named by Matson (1916), is near Citronelle, Alabama. The Citronelle Formation grades laterally, through a broad facies transition, into the Miccosukee Formation of the eastern Florida panhandle. Coe (1979) investigated the Citronelle Formation in portions of the western Florida panhandle. The Citronelle Formation is a siliciclastic, deltaic deposit that is lithologically similar to, and time equivalent with, the Cypresshead Formation and, at least in part, the Long Key Formation (Cunningham et al., 1998) of the peninsula. In the western panhandle, some of the sediments mapped as Citronelle Formation may be reworked Citronelle. The lithologies are the same and there are few fossils present to document a possible younger age. The Citronelle Formation consists of gray to orange, often mottled, unconsolidated to poorly consolidated, very fine to very coarse, poorly sorted, clean to clayey sands. It contains significant amounts of clay, silt and gravel which may occur as beds and lenses and may vary considerably over short distances. Limonite nodules and limonite-cemented beds are common. Marine fossils are rare but fossil pollen, plant remains and occasional vertebrates are found. Much of the Citronelle Formation is highly permeable. It forms the Sand and Gravel Aquifer of the surficial aquifer system contain organics. The dominant fossils in the freshwater carbonates are mollusks. (Source: USGS Florida Geologic Map Data). The soils of this are characterized as Troup Series loamy sand, 0 to 5 percent slopes. The Troup series consists of very deep, somewhat excessively drained soils that formed in unconsolidated sandy and loamy marine sediments. Troup soils are on ridges and hillslopes. Slopes predominantly range from 0 to 15 percent but range to 45 percent. The soil pH is generally strongly acid. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions).Wild material2169919NA 88582
26NA 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
27NA 885862024RJLFL-020Vaccinium arboreum Marshall Florida, United StatesNA2024COLLECTED11/14/2024Woodland edge off of Ralf Laurant Road, above the wetland/headwaters of Danley Branch along the edge of a young longleaf pine plantation.30.90104300, -86.7887810061Edge of a mixed evergreen and deciduous forest in part shade to full sun on a mesic to mesic-dry slope, adjacent to a young longleaf pine plantation. Slope: 3 to 8 percent. Aspect: West. 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. The dominant fossils in the freshwater carbonates are mollusks. (Source: USGS Florida Geologic Map Data). The surface soil profile is classified as Troup Series loamy sand, 5 to 8 percent slopes. The Troup series consists of very deep, somewhat excessively drained soils formed in unconsolidated sandy and loamy marine sediments. Troup soils are found on ridges and hillslopes. These soils are very strongly acid to strongly acid. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions).Wild material2169923NA 88586
28NA 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
29NA 88731RonMiller2022-Old Land PlaceGordonia lasianthus (L.) J. Ellis Florida, United StatesNA2024COLLECTED04/2022Yellow River Marsh State Aquatic Preserve, "Old Land Place" along Weaver River, 1.47 miles south of the confluence with the Yellow River.30.55318000, -87.936560003Moist to wet areas in wetland adjacent to the river in association with a range of evergreen and deciduous forest elements.Wild materialFrom open-pollinated, but presumed isolated, seeds of NA 87342-H, -J, and -L (three young plants flowering in containers in production during 2024). Seed was harvested over a period roughly from October through December 2024 as fruits matured. From the record of the parent accession, NA 87342: Exact date of collection unknown.2170992NA 88731
30W6 61971OR930A-10Chamaenerion angustifolium (L.) Scop. subsp. angustifolium Oregon, United StatesW6SEED2024Wild materialThey are found in dry to moist disturbed areas Its leaves are lance shaped with rose to purple sepals and petals 2168424W6 61971
31W6 61974OR930A-15Chamaenerion angustifolium (L.) Scop. subsp. angustifolium Oregon, United StatesW6SEED2024Wild materialFlowers pink purple 4 lobed stigma 8 stamens2168375W6 61974
32W6 61975OR930A-16Prunella vulgaris L. Oregon, United StatesW6SEED2024Wild materialFlowers in bracteate terminal spike corolla purple2168427W6 61975
33W6 61976OR930A-17Chamaenerion angustifolium (L.) Scop. subsp. angustifolium Oregon, United StatesW6SEED2024Wild materialFlowers pink purple 4 lobed stigma 8 stamens2168428W6 61976
34W6 61977OR930A-19Chamaenerion angustifolium (L.) Scop. subsp. angustifolium Oregon, United StatesW6SEED2024Wild materialFlowers pink purple 4 lobed stigma 8 stamens2168376W6 61977
35W6 61978OR930A-20Prunella vulgaris L. Oregon, United StatesW6SEED2024Wild materialFlowers in bracteate terminal spikes corolla purple2168377W6 61978
36W6 61979OR930A-21Vaccinium parvifolium Sm. Oregon, United StatesW6SEED2024Wild materialMulti stemmed shrub current season twigs green2168378W6 61979
37NA 88827RJL-RM2023FLAL-001Ilex ambigua Torr. Florida, United StatesNA2023COLLECTED12/05/2023Yellow River Wildlife Management Area, along DOF [Department of Forestry] Y9 dirt road 0.08 kilometers east of Miller Bluff Road.30.65289100, -86.8760280044Growing in part shade to sun in very dry, highly competitive site still recovering from the logging of pines in the past decade. This young woodland is comprised of a combination of evergreen and deciduous species competing for available resources and light before the young sand pines begin to dominate the upper canopy. Slope: 0 percent. 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 primary soil type in the collection area is classified as Lakeland Sand soils (0 to 5 percent slopes). The surface soil profile of this area is primarily the Lakeland series which consists of very deep, excessively drained, rapid to very rapidly permeable soils on uplands. They formed in thick beds of eolian or marine and/or fluvio-marine sands. Thickness of the sand exceeds 2 meters. Silt plus clay in the upper meter ranges from 5-10 percent. Reaction ranges from very strongly acid to moderately acid throughout. (Source: NRCS Web Soil Survey.)Wild material2165657NA 88827
38NA 88828RJL-RM2023FLAL-002Vaccinium arboreum Marshall Florida, United StatesNA2023COLLECTED12/05/2023Yellow River Wildlife Management Area, along DOF [Department of Forestry] Y9 dirt road 0.08 kilometers east of Miller Bluff Road.30.65289100, -86.8760850044Growing in part shade to sun in very dry, highly competitive site still recovering from the logging of pines in the past decade. This young woodland is comprised of a combination of evergreen and deciduous species competing for available resources and light before the young sand pines begin to dominate the upper canopy. Slope: 0 percent. 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 primary soil type in the collection area is classified as Lakeland Sand soils (0 to 5 percent slopes). The surface soil profile of this area is primarily the Lakeland series which consists of very deep, excessively drained, rapid to very rapidly permeable soils on uplands. They formed in thick beds of eolian or marine and/or fluvio-marine sands. Thickness of the sand exceeds 2 meters. Silt plus clay in the upper meter ranges from 5-10 percent. Reaction ranges from very strongly acid to moderately acid throughout. (Source: NRCS Web Soil Survey.)Wild material2165658NA 88828
39NA 88829RJL-RM2023FLAL-003Oxydendrum arboreum (L.) DC. Florida, United StatesNA2023COLLECTED12/05/2023Yellow River Wildlife Management Area, along DOF [Department of Forestry] Y15 dirt road 0.06 kilometers north of Fisher Old Mill Road.30.62728600, -86.838246007Growing in part shade to sun in moist to wet flat woods of the longleaf pine forest. The woodland is comprised mostly of open habitat of longleaf pine and an understory tree and shrub layer of evergreen and deciduous species. There is also a wealth of herbaceous species in moist to wet conditions of the habitat where there is rich organic matter in the surface layer. Slope: 0 percent. Aspect: N/A. 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 primary soil types in the collection area are classified as Pactolus Loamy Sand soils (0 to 5 percent slopes). The Pactolus Series consists of very deep, moderately well to somewhat poorly drained soils. Permeability is rapid. These Coastal Plain soils, typically found with streams and marine terraces and were formed by loamy and sandy fluvial sediments and marine sediments. The strata is, generally, uniformly loamy sand that is very friable and strongly acid from the surface to a depth of 1.8 meters. (Source: NRCS Web Soil Survey.)Wild material2165659NA 88829
40NA 88834RJL-RM2023FLAL-008Rhododendron canescens (Michx.) Sweet Florida, United StatesNA2023COLLECTED12/06/2023Blackwater State Forest: plants are growing in wetlands accessed by foot from Buddy Hardy Road. The collection site is approximately 0.14 kilometers west and downhill from the road.30.80736700, -86.9578470053Growing in shade to part-shade of the well-drained moist mesic habitat about 1 m above the wetland which appears to be formed by a nearby hillside seepage area. In this zone there are numerous facultative wetland species as well as high competition from facultative upland plants. Slope: 5 to 10 percent. Aspect: Variable. 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 Troup Series (5 to 8% slopes) consists of very deep, somewhat excessively drained soil formed in unconsolidated sandy and loamy marine sediments. Troup soils are on ridges and hillslopes. The upper 0-13 cm is comprised primarily of decomposing sphagnum peat with a significant amount of fibrous root content. From 15-112 cm the soil is comprised primarily of fine-grained yellowish-brown sand with varying amounts of root content; this zone is strongly acid. From 112-203 cm the soil is comprised of light-red to red sandy clay loam that is discontinuous, generally friable, and strongly acid. (Source: NRCS Web Soil Survey.)Wild material2165664NA 88834
41NA 88835RJL-RM2023FLAL-009Rhododendron viscosum (L.) Torr. Florida, United StatesNA2023COLLECTED12/06/2023Blackwater State Forest: plants are growing in wetlands accessed by foot from Buddy Hardy Road. The collection site is approximately 0.14 kilometers west and downhill from the road.30.80841000, -86.9628330043Growing in part-shade of the well-drained moist-dry mesic habitat about 2-3 m above the wetland. In this zone there are numerous facultative wetland species as well as high competition from facultative upland plants. Slope: 5 to 10 percent. Aspect: Variable. 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 Troup Series (5 to 8% slopes) consists of very deep, somewhat excessively drained soil formed in unconsolidated sandy and loamy marine sediments. Troup soils are on ridges and hillslopes. The upper 0-13 cm is comprised primarily of decomposing sphagnum peat with a significant amount of fibrous root content. From 15-112 cm the soil is comprised primarily of fine-grained yellowish-brown sand with varying amounts of root content; this zone is strongly acid. From 112-203 cm the soil is comprised of light-red to red sandy clay loam that is discontinuous, generally friable, and strongly acid. (Source: NRCS Web Soil Survey.)Wild material2165665NA 88835
42NA 88840RJL-RM2023FLAL-014Rhododendron viscosum (L.) Torr. Florida, United StatesNA2023COLLECTED12/11/2023Property of Floyd Griffith off View Drive on the southwest side of McCormick Lake.30.63247000, -85.3371820056Plants are growing primarily in part shade a few meters above the lake, generally in areas that appear dry, but clearly are associated with hillside seeps. While much of the area has been cultivated, the remnant native flora are largely broadleaved evergreen shrub and deciduous shrub and tree species. Slope: 10 to 15 percent. Aspect: Northeast. The underlying geology of this area is the Citronelle Formation of Pliocene origin and consists of gray to orange, often mottled, unconsolidated to poorly consolidated, very fine to very coarse, poorly sorted, clean to clayey sands. It contains significant amounts of clay, silt and gravel which may occur as beds and lenses and may vary considerably over short distances. Limonite nodules and limonite-cemented beds are common. (Source: USGS Florida Geologic Map Data.) The 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 material2165670NA 88840
43NA 88844RJL-RM2023FLAL-018Clethra alnifolia L. Florida, United StatesNA2023COLLECTED12/13/2023Yellow River Water Management Area, accessed off of Old River Road by vehicle on an unmaintained sand road for approximately 1.68 kilometers. Upon reaching the destination, plants are accessed by foot along unmaintained trail to the east.30.83495500, -86.6200540027Plants are growing primarily in part shade as understory shrubs in mixed evergreen and deciduous, moist to wet, acidic woodlands. Plants form large colonies and appear to have been subjected to prescribed fire in recent years. Slope: 10 to 15 percent. Aspect: Northeast. The underlying geology of this area is the Citronelle Formation of Pliocene origin and consists of gray to orange, often mottled, unconsolidated to poorly consolidated, very fine to very coarse, poorly sorted, clean to clayey sands. It contains significant amounts of clay, silt and gravel which may occur as beds and lenses and may vary considerably over short distances. Limonite nodules and limonite-cemented beds are common. (Source: USGS Florida Geologic Map Data.) The soil profile for this area is classified as the Bonifay Soil Series. Bonifay soil consists of very deep, well drained, moderately slowly permeable soils on ridges and side slopes in the Southern Coastal Plain. They formed in thick beds of sandy and loamy marine sediments. Solum thickness ranges from 1.5-2.0 m. Soil reaction ranges from very strongly acid to moderately acid throughout, except where the surface has been limed. Ironstone pebbles, 2 to 15 mm in size, range from 0 to 5 percent, by volume. Depth to the plinthic horizon ranges from 1.1-1.7 m. Some horizons contain up to 25 percent plinthite by volume. (Source: NRCS Web Soil Survey.)Wild material2165674NA 88844
44NA 88689RJL2023NJ-002Kalmia latifolia 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.39.57400900, -74.9360240032Plants growing in shade to part-shade of a mesic to mesic-dry woodland habitat that is mostly deciduous, but also includes pine overstory. Slope: N/A. Aspect: N/A. Soils: 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 location of this collection is classified as Downer loamy sand, 0 to 5 percent slopes, Northern Coastal Plain. Downer Series soils are very deep, well-drained soils that are coarse-loamy, siliceous, semiactive, mesic Typic Hapludults. The upper strata 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 material2159117NA 88689
45NA 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
46NA 88698RJL2023NCSC-003Ilex laevigata (Pursh) A. Gray North Carolina, United StatesNA2023COLLECTED11/13/2023Sandhills Game Land: north side of Pulpwood Road approximately 0.11 km southwest of the junction with Tyner Road.34.95939500, -79.48676300114Plants growing in shade to part-shade of a spring fed wetland that is a mixed evergreen and deciduous woodland habitat. Slope: 3 to 10 percent. Aspect: Northeast. The underlying geology of this area is of Tertiary origin and characterized as Pinehurst Formation. It is comprised of sand that is medium- to coarse-grained, cross-bedding and rhythmic bands of clayey sand common, unconsolidated. (Source: USGS North Carolina Geologic Map Data.) The primary soil type in the area of this collection is classified as Pelion loamy sand, 6 to 10 percent slopes. Pelion Series soils are very deep, moderately well-drained soils with moderately slow to slow permeability. The upper 30 cm of the strata is sandy loam to sandy clay loam ranging from grayish brown to reddish yellow. This stratum has a weak fine granular structure and is very friable. It contains many fine roots and is moderately acid. Deeper strata to 2 m range from yellow to yellowish red sandy clay, often with masses of oxidized iron and few fine prominent light gray iron depletions; they are strongly acid. (Source: NRCS Web Soil Survey.)Wild material2159126NA 88698
47NA 88699RJL2023NCSC-004Lyonia ligustrina (L.) DC. North Carolina, United StatesNA2023COLLECTED11/13/2023Sandhills Game Land: north side of Pulpwood Road approximately 0.11 km southwest of the junction with Tyner Road.34.95949000, -79.48665600107Plants growing in part-shade to sun on the moist margins of a spring fed wetland that is a mixed evergreen and deciduous woodland habitat. The underlying soils are moist even during dry periods due to seepage from the wetland. Slope: 3 to 10 percent. Aspect: Northeast. The underlying geology of this area is of Tertiary origin and characterized as Pinehurst Formation. It is comprised of sand that is medium- to coarse-grained, cross-bedding and rhythmic bands of clayey sand common, unconsolidated. (Source: USGS North Carolina Geologic Map Data.) The primary soil type in the area of this collection is classified as Pelion loamy sand, 6 to 10 percent slopes. Pelion Series soils are very deep, moderately well-drained soils with moderately slow to slow permeability. The upper 30 cm of the strata is sandy loam to sandy clay loam ranging from grayish brown to reddish yellow. This stratum has a weak fine granular structure and is very friable. It contains many fine roots and is moderately acid. Deeper strata to 2 m range from yellow to yellowish red sandy clay, often with masses of oxidized iron and few fine prominent light gray iron depletions; they are strongly acid. (Source: NRCS Web Soil Survey.)Wild material2159127NA 88699
48NA 88700RJL2023NCSC-005Clethra alnifolia L. North Carolina, United StatesNA2023COLLECTED11/13/2023Sandhills Game Land: north side of Pulpwood Road approximately 0.11 km southwest of the junction with Tyner Road.34.96008500, -79.48751100108Plants growing in shade to part-shade as well as sun (when moisture is abundant) of a spring fed wetland that is comprised of a mixed evergreen and deciduous woodland habitat. Slope: 3 to 10 percent. Aspect: Various. : The underlying geology of this area is of Cretaceous origin and characterized as Middendorf Formation. It is characterized by sand, sandstone, and mudstone, gray to pale gray with an orange cast, mottled; clay balls and iron-cemented concretions common, beds laterally discontinuous, cross-bedding common. (Source: USGS North Carolina Geologic Map Data.) The primary soil type in the area of this collection is classified as Pelion loamy sand, 6 to 10 percent slopes. Pelion Series soils are very deep, moderately well-drained soils with moderately slow to slow permeability. The upper 30 cm of the strata is sandy loam to sandy clay loam ranging from grayish brown to reddish yellow. This stratum has a weak fine granular structure and is very friable. It contains many fine roots and is moderately acid. Deeper strata to 2 m range from yellow to yellowish red sandy clay, often with masses of oxidized iron and few fine prominent light gray iron depletions; they are strongly acid. (Source: NRCS Web Soil Survey.)Wild material2159128NA 88700
49NA 88701RJL2023NCSC-006Zenobia pulverulenta (W. Bartram ex Willd.) Pollard North Carolina, United StatesNA2023COLLECTED11/13/2023Sandhills Game Land: north side of Pulpwood Road approximately 0.11 km southwest of the junction with Tyner Road.34.96066900, -79.48735300111Plants growing in moist-mesic to seasonally saturated soils in part-shade of a spring fed wetland that is a mixed evergreen and deciduous woodland habitat. Slope: 0 to 5 percent. Aspect: Northeast. The underlying geology of this area is of Tertiary origin and characterized as Pinehurst Formation. It is comprised of sand that is medium- to coarse-grained, cross-bedding and rhythmic bands of clayey sand common, unconsolidated. (Source: USGS North Carolina Geologic Map Data.) The primary soil type in the area of this collection is classified as Pelion loamy sand, 6 to 10 percent slopes. Pelion Series soils are very deep, moderately well-drained soils with moderately slow to slow permeability. The upper 30 cm of the strata is sandy loam to sandy clay loam ranging from grayish brown to reddish yellow. This stratum has a weak fine granular structure and is very friable. It contains many fine roots and is moderately acid. Deeper strata to 2 m range from yellow to yellowish red sandy clay, often with masses of oxidized iron and few fine prominent light gray iron depletions; they are strongly acid. (Source: NRCS Web Soil Survey.)Wild material2159129NA 88701
50NA 88702RJL2023NCSC-007Rhododendron viscosum (L.) Torr. North Carolina, United StatesNA2023COLLECTED11/13/2023Sandhills Game Land: north side of Pulpwood Road approximately 0.11 km southwest of the junction with Tyner Road.34.96080300, -79.48730200113Plants growing in moist-mesic to seasonally saturated soils in shade to part-shade of a spring fed wetland that is a mixed evergreen and deciduous woodland habitat. Prescribed fires have burned a portion of the wetland edge where plants are resprouting vigorously. Slope: 0 to 5 percent. Aspect: Norhteast. The underlying geology of this area is of Tertiary origin and characterized as Pinehurst Formation. It is comprised of sand that is medium- to coarse-grained, cross-bedding and rhythmic bands of clayey sand common, unconsolidated. (Source: USGS North Carolina Geologic Map Data.) The primary soil type in the area of this collection is classified as Pelion loamy sand, 6 to 10 percent slopes. Pelion Series soils are very deep, moderately well-drained soils with moderately slow to slow permeability. The upper 30 cm of the strata is sandy loam to sandy clay loam ranging from grayish brown to reddish yellow. This stratum has a weak fine granular structure and is very friable. It contains many fine roots and is moderately acid. Deeper strata to 2 m range from yellow to yellowish red sandy clay, often with masses of oxidized iron and few fine prominent light gray iron depletions; they are strongly acid. (Source: NRCS Web Soil Survey.)Wild material2159130NA 88702
51NA 88703RJL2023NCSC-008Lyonia lucida (Lam.) K. Koch North Carolina, United StatesNA2023COLLECTED11/13/2023Sandhills Game Land: north side of Pulpwood Road approximately 0.11 km southwest of the junction with Tyner Road.34.95848900, -79.48618700101Plants growing in moist-mesic to seasonally saturated soils in shade to part-shade of a spring fed wetland that is a mixed evergreen and deciduous woodland habitat. Slope: 0 to 5 percent. Aspect: Various. The underlying geology of this area is of Tertiary origin and characterized as Pinehurst Formation. It is comprised of sand that is medium- to coarse-grained, cross-bedding and rhythmic bands of clayey sand common, unconsolidated. (Source: USGS North Carolina Geologic Map Data.) The primary soil type in the area of this collection is classified as Pelion loamy sand, 6 to 10 percent slopes. Pelion Series soils are very deep, moderately well-drained soils with moderately slow to slow permeability. The upper 30 cm of the strata is sandy loam to sandy clay loam ranging from grayish brown to reddish yellow. This stratum has a weak fine granular structure and is very friable. It contains many fine roots and is moderately acid. Deeper strata to 2 m range from yellow to yellowish red sandy clay, often with masses of oxidized iron and few fine prominent light gray iron depletions; they are strongly acid. (Source: NRCS Web Soil Survey.)Wild material2159131NA 88703
52NA 88704RJL2023NCSC-009Rhododendron viscosum (L.) Torr. North Carolina, United StatesNA2023COLLECTED11/13/2023Sandhills Game Land: wetlands and moist depressions along Hoffman Road, Scotland County Road 1328,34.95510000, -79.51769700112Plants are growing in sun in an acidic wetland habitat rich in sphagnum and other wetland species. The habitat is moist to wet year-round and periodically has surface runoff occurring; even so, this habitat can become quite dry during seasonal periods without rainfall. Slope: 2 to 3 percent. Aspect: Northeast. The underlying geology of this area is of Tertiary origin and characterized as Pinehurst Formation. It is comprised of medium- to coarse-grained sand as well as cross-bedding and rhythmic bands of clayey sand that are unconsolidated. (Source: USGS North Carolina Geologic Map Data.) The primary soil type in the collection area is classified as Pelion Loamy Sand (2 to 6 percent slopes). The Pelion Loamy Sand series consists of very deep, moderately well-drained marine deposits, fluviomarine deposits, and sand sheets. Permeability is moderately slow or slow. Surface layers 0-25 cm deep are comprised of loamy sand with a weak fine granular structure and are very friable. Deeper horizons are comprised of sandy loam, sandy clay loam, or clay loam in the upper part and includes sandy clay or clay in the deepest part. Soils are extremely acid to strongly acid. (Source: NRCS Web Soil Survey.)Wild material2159132NA 88704
53NA 88705RJL2023NCSC-010Zenobia pulverulenta (W. Bartram ex Willd.) Pollard North Carolina, United StatesNA2023COLLECTED11/13/2023Sandhills Game Land: wetlands and moist depressions along Hoffman Road, Scotland County Road 1328,34.95510000, -79.51769700112Plants are growing in part-shade to sun in an acidic wetland habitat rich in sphagnum and other obligate wetland species. The habitat is moist to wet year-round and periodically has surface runoff occurring; even so, this habitat can become quite dry during seasonal periods without rainfall. Slope: 2 to 3 percent. Aspect: Northeast. The underlying geology of this area is of Tertiary origin and characterized as Pinehurst Formation. It is comprised of medium- to coarse-grained sand as well as cross-bedding and rhythmic bands of clayey sand that are unconsolidated. (Source: USGS North Carolina Geologic Map Data.) The primary soil type in the collection area is classified as Pelion Loamy Sand (2 to 6 percent slopes). The Pelion Loamy Sand series consists of very deep, moderately well-drained marine deposits, fluviomarine deposits, and sand sheets. Permeability is moderately slow or slow. Surface layers 0-25 cm deep are comprised of loamy sand with a weak fine granular structure and are very friable. Deeper horizons are comprised of sandy loam, sandy clay loam, or clay loam in the upper part and includes sandy clay or clay in the deepest part. Soils are extremely acid to strongly acid. (Source: NRCS Web Soil Survey.)Wild material2159133NA 88705
54NA 88709RJL2023NCSC-014Rhododendron minus Michx. South Carolina, United StatesNA2023COLLECTED11/13/2023Northwest side of the junction of Wire Road and Prichard Horse Road.34.49925200, -80.27470600146Plants growing in shade to part-shade of dry steep slope woodland habitat that is primarily composed of Pinus palustris. Slope: 2 to 20 percent. Aspect: North. The underlying geology of this area is of Cretaceous origin and characterized as Peedee Formation - Black Creek Group, undivided. The Peedee Formation is primarily unconsolidated, coarse-detrital, sand that is dark-green or gray, finely micaceous, more or less glauconitic and argillitic sand, many layers of which are calcareous (impure limestone). Irregular concretionary masses of impure calcium carbonate occur in places. Dark marine clays are interstratified with sand. The Black Creek Group consists of irregularly bedded, laminated, carbonaceous clays and thin laminae and lenses of sand; lignite and pyrite present; glauconitic in places; massive interbedded layers of glauconitic sand present toward top of unit. Light-colored clays and coarse arkosic sands also found. (Source: USGS South Carolina Geologic Map Data.) The primary soil type in the collection area is classified as Ailey Series sand, moderately wet, 2 to 6 percent slopes. The Ailey Series consists of moderately deep or deep to fragic soil properties and deep or very deep to densic materials. This soil is well drained or somewhat excessively drained. The upper layer (0-12.5 cm) of this soil is dark grayish brown loamy sand that is frequently dry. It has a weak fine granular structure, is very friable, non-sticky, non-plastic, and is strongly acid. The lower strata soils (12.5-90 cm) are yellowish brown loamy sand, with weak fine granular structure, very friable, non-sticky, non-plastic, and moderately acid. Deeper depths (below 90 cm) are characterized by slightly greater clay content that is slightly more plastic and strongly acid. (Source: NRCS Web Soil Survey.)Wild material2159137NA 88709
55NA 88715RJL2023NCSC-020Zenobia pulverulenta (W. Bartram ex Willd.) Pollard South Carolina, United StatesNA2023COLLECTED11/14/2023Francis Marion National Forest: plants growing in open wetlands/swamps on the south side of US Forest Service Road 5097 approximately 0.07 kilometers southwest of the junction with US Forest Service Road 223.33.06791000, -79.6721340011Plants are growing in full sun to part-shade along the edges of an extensive acid wetland in seasonally inundated habitat. The vegetation, is a mix of evergreen and deciduous species; it is so dense that it is almost impenetrable. 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 Seewee Complex soils. The Seewee series consists of very deep, somewhat poorly drained, moderately rapidly permeable soils that formed in sandy marine sediments. Slopes range from 0 to 2 percent. The upper strata soil, 0-38 cm, is black, loamy fine sand, friable, and extremely acid. The lower strata soil, 38-75 cm, is fine sand, commonly mottled with shades of brown or yellow and very strongly acid to moderately acid. (Source: NRCS Web Soil Survey.)Wild material2159143NA 88715
56WLP 3136TJK2023FL-010 Morella cerifera (L.) Small Florida, United StatesNA2023COLLECTED08/18/2023Blackwater State Forest: Wolfe Creek.30.80751000, -86.9577400052Beautiful xeric pine-oak upland community. Transitions to mesic slopes and then to seepage bottom, stringer wetland community adjacent to the Wolfe Creek. Area is on a regular 2-4[-year] burn cycle. Slope: 10%. Aspect: South. Elevation recorded as 172 feet.Wild materialReceived as Morella pumila (Morella cerifera var. pumila). Treated tentatively as Morella cerifera Pumila Group. WLPGR contract collection.2158468WLP 3136
57OPGC 8793OR110-1114Anaphalis margaritacea (L.) Benth. & Hook. f. Oregon, United StatesOPGC2023Wild material2142745OPGC 8793
58W6 61027CA360-198Elymus glaucus Buckley California, United StatesW6SEED2023Wild materialSeeds Grow in Pairs, Spiraling up the head2142666W6 61027
59OPGC 8813CBG- 10781Hieracium scabrum Michx. Illinois, United StatesOPGC2023Wild material2142247OPGC 8813
60NA 88598RJL2023FL-002aAgarista populifolia (Lam.) Judd Florida, United StatesNA2023COLLECTED02/14/2023Plants growing in woodlands of Wekiwa Springs State Park along trails accessed from the Sand Lake parking lot at the end of Palmetto Avenue. From the parking lot, take the main trail south for about 18 meters and immediately take a cut-through trail on the left to the location of this population.28.72398600, -81.4720540010Plants were growing in shade to part-shade of moist mesic hammocks of lowland transitional woodlands eventually becoming wetland habitats that are comprised primarily of evergreen plants with fewer deciduous plants. The underlying geology of this area is of Pliocene origin and characterized as the Cypresshead Formation. The Cypresshead Formation named by Huddlestun (1988), is composed of siliciclastics and occurs only in the peninsula and eastern Georgia. It is at or near the surface from northern Nassau County southward to Highlands County forming the peninsular highlands. It appears that the Cypresshead Formation occurs in the subsurface southward from the outcrop region and similar sediments, the Long Key Formation, underlie the Florida Keys. The Cypresshead Formation is a shallow marine, near shore deposit equivalent to the Citronelle Formation deltaic sediments and the Miccosukee Formation prodeltaic sediments. The Cypresshead Formation consists of reddish brown to reddish orange, unconsolidated to poorly consolidated, fine to very coarse grained, clean to clayey sands. Cross bedded sands are common within the formation. Discoid quartzite pebbles and mica are often present. Clay beds are scattered and not areally extensive. In general, the Cypresshead Formation in exposure occurs above 100 feet (30 meters) above mean sea level (msl). Original fossil material is not present in the sediments although poorly preserved molds and casts of mollusks and burrow structures are occasionally present. The presence of these fossil "ghosts" and trace fossils documents marine influence on deposition of the Cypresshead sediments. The permeable sands of the Cypresshead Formation form part of the surficial aquifer system.Wild material2141479NA 88598
61WLP 3084RM2023-002Rhododendron viscosum (L.) Torr. Florida, United StatesNA2023COLLECTED09/15/2022This species is growing in the Blackwater River State Forest approximately 0.24 kilometers north of Wof W20 and approximately 0.93 kilometers west of the junction of 3 Notch Trail/Road. 30.84510000, -86.9494000038The plants were growing in part shade of a moist mesic transition slope between a dry upland habitat and a bog.
Soils: The underlying geology of this area is the Citronelle Formation, of Pliocene origin, and consists of gray to orange, often mottled, unconsolidated to poorly consolidated, very fine to very coarse, poorly sorted, clean to clayey sands. It contains significant amounts of clay, silt and gravel which may occur as beds and lenses and may vary considerably over short distances. Limonite nodules and limonite-cemented beds are common. Source: USGS Florida Geologic Map Data (https://mrdata.usgs.gov/geology/state/state.php?state=fl)
The surface soil profile found in this area is primarily Troup Series. These soils are sandy and loamy marine deposits. They are well drained and typically on the tops and sides of broad and narrow ridges on uplands typically with 0-12% slopes. These soils are very strongly acid with a depth of 2-3 meters. Pactolus Series soils comprise a minor, but important percentage of the lower slopes that are nearly level to gently sloping and account for the somewhat poorly drained, yet, sandy conditions. These soils are also strongly acid with very dark gray loamy sands.
Source: Soil Survey of Santa Rosa County and NRCS Web Soil Survey (https://www.nrcs.usda.gov/Internet/FSE_MANUSCRIPTS/florida/FL113/0/SantaRosa.pdf and https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2141438WLP 3084
62WLP 3087RM2023-005Rhododendron minus Michx. var. minus Alabama, United StatesNA2023COLLECTED12/29/2022This plant is growing along the edges of Gantt Lake, accessed by boat. Occasional in shaded areas around Gantt Lake.31.40780000, -86.4677000068The plants were growing in open conditions on a steep north-facing bluff above Gantt Lake.
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 surface soil profile of this area is primarily Eunola Series Loamy Fine Sand (0 to 2 percent slopes, rarely flooded). The Eunola series consists of very deep, moderately well drained, moderately permeable loamy soils that formed in fluvial or marine sediments. They are on low stream or marine terraces of the Southern Coastal Plain. They are strongly acid. Slopes are dominantly 0 to 3 percent but range up to 6 percent.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2141441WLP 3087
63WLP 3088RM2023-006Kalmia latifolia L. Alabama, United StatesNA2023COLLECTED12/29/2022This plant is growing along the edges of Gantt Lake, accessed by boat. Occasional in shaded areas around Gantt Lake.31.40780000, -86.4677000068The plants were growing in open conditions on a steep north-facing bluff above Gantt Lake.
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 surface soil profile of this area is primarily Eunola Series Loamy Fine Sand (0 to 2 percent slopes, rarely flooded). The Eunola series consists of very deep, moderately well drained, moderately permeable loamy soils that formed in fluvial or marine sediments. They are on low stream or marine terraces of the Southern Coastal Plain. They are strongly acid. Slopes are dominantly 0 to 3 percent but range up to 6 percent.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2141442WLP 3088
64WLP 3089RM2023-007Oxydendrum arboreum (L.) DC. Alabama, United StatesNA2023COLLECTED12/29/2022This plant is growing along the edges of Gantt Lake, accessed by boat. Occasional around Gantt Lake.31.41156000, -86.4692000070The plants were growing in open sunny conditions on a steep east-facing bluff above Gantt Lake.
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 surface soil profile of this area is primarily Eunola Series Loamy Fine Sand (0 to 2 percent slopes, rarely flooded). The Eunola series consists of very deep, moderately well drained, moderately permeable loamy soils that formed in fluvial or marine sediments. They are on low stream or marine terraces of the Southern Coastal Plain. They are strongly acid. Slopes are dominantly 0 to 3 percent but range up to 6 percent.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2141443WLP 3089
65WLP 3090RM2023-008Lyonia lucida (Lam.) K. Koch Alabama, United StatesNA2023COLLECTED12/29/2022This plant is growing along the steep edges of Gantt Lake, accessed by boat. Occasional in shaded areas around Gantt Lake.31.40780000, -86.4677000068The plants were growing in open conditions on a steep north-facing bluff above Gantt Lake.
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 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 material2141444WLP 3090
66WLP 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
67WLP 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
68NA 88523RM-TK2022-011Ilex ambigua Torr. Florida, United StatesNA2023COLLECTED10/16/2022Blackwater River State Park: growing along unnamed dirt road approximately 0.26 kilometers north of the intersection with Boundary Line Road.30.68790000, -86.8623000056Plants are growing in hot, dry, full sun conditions. Soils: The underlying geology of this area is the Citronelle Formation of Pliocene origin and consists of gray to orange, often mottled, unconsolidated to poorly consolidated, very fine to very coarse, poorly sorted, clean to clayey sands. It contains significant amounts of clay, silt and gravel which may occur as beds and lenses and may vary considerably over short distances. Limonite nodules and limonite-cemented beds are common. (Source: USGS Florida Geologic Map Data). The primary soil type in the collection area is classified as Lakeland Sand soils (5 to 12 percent slopes). The surface soil profile of this area is primarily the Lakeland series which consists of very deep, excessively drained, rapid to very rapidly permeable soils on uplands. They formed in thick beds of eolian or marine and/or fluvio-marine sands. Thickness of the sand exceeds 2 meters. Silt plus clay in the upper meter ranges from 5-10 percent. Reaction ranges from very strongly acid to moderately acid throughout. (Source: NRCS Web Soil Survey).Wild material2140804NA 88523
69NA 88526RM-TK2022-014Oxydendrum arboreum (L.) DC. Florida, United StatesNA2023COLLECTED11/06/2022Growing along an unnamed dirt road leading to “Old Land Place” on the edge of Eglin AFB accessed from the Yellow River.30.55320000, -86.937300002The underlying geology of this area is classified as Alluvium of Pleistocene/Holocene origin and consists of undifferentiated Quaternary sediments of varying thickness including siliciclastics, organics and freshwater carbonates. The siliciclastics are light gray, tan, brown to black, unconsolidated to poorly consolidated, clean to clayey, silty, unfossiliferous, variably organic-bearing sands to blue green to olive green, poorly to moderately consolidated, sandy, silty clays. Organics occur as plant debris, roots, disseminated organic matrix and beds of peat. Freshwater carbonates, often referred to as marls in the literature, are scattered.
Source: USGS Florida Geologic Map Data (https://mrdata.usgs.gov/geology/state/state.php?state=fl)
The surface soil profile of this area is primarily Bibb-Kinston Series Association. Bibb Series soils are coarse-loamy, sandy, acid soils that are poorly drained. They are soils of flood plains and streams subject to frequent flooding. These are found in association with Kinston Series soils that are fine-loamy, sandy, acid soils of flood plains and stream subject to frequent flooding. The Bibb-Kinston association ranges from 1-1.5 meters thick and is strongly acid.
Source: Soil Survey of Santa Rosa County and NRCS Web Soil Survey (https://www.nrcs.usda.gov/Internet/FSE_MANUSCRIPTS/florida/FL113/0/SantaRosa.pdf and https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2140807NA 88526
70NA 88530RJLSEUS2022-001Oxydendrum arboreum (L.) DC. North Carolina, United StatesNA2023COLLECTED12/06/2022Plants growing around a wetland on both sides of Scotland Lake Road, approximately 1.1 kilometers southwest of the junction with Hoffman Road (Scotland Co. Road 1328) in the Sandhills Game Lands. This plant is a common component along the mesic/moist boundary on the upper edge of the understory shrub in the moist woodland habitat not far from the wetland. 34.98402000, -79.54267200116Plants are growing in full sun to part-shade in the moist, well-drained, mesic conditions just above a wetland area occupied by obligate wetland species. The underlying geology of this area is of Tertiary origin and characterized as Pinehurst Formation. It is composed 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 (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=NCTp%3B11)
The primary soil type in the collection area is Pelion Loamy Sand soil (6 to 10 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 include sandy clay or clay in the deepest strata. Soils are extremely acid to strongly acid.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2140759NA 88530
71NA 88531RJLSEUS2022-002Cyrilla racemiflora L. North Carolina, United StatesNA2023COLLECTED12/06/2022Plants growing around a wetland on both sides of Scotland Lake Road, approximately 1.1 kilometers southwest of the junction with Hoffman Road (Scotland Co. Road 1328) in the Sandhills Game Lands. This plant is a common component of moist to wet areas of the wetland habitats in this area. 34.98418000, -79.54079800120Plants are growing in part-shade to sun in a wetland habitat as well as nearby seasonally drier mesic habitat.
Soils: 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 (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=NCTp%3B11)
The primary soil type in the collection area is classified as Johnston Series soils (0 to 2 percent slopes, frequently flooded). The Johnston series consists of very deep, very poorly drained soils that are occasionally to frequently flooded for short to extended periods. Permeability is moderate to rapid. These nearly level soils are alluvial in origin and typical of floodplains and swamp. Slopes range from 0 to 2 percent. Johnston Series soils are comprised of mucky loam that is friable with siliceous elements in the upper 0-75 cm. Lower strata range in percentages of mucky loam and loamy fine sand.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2140760NA 88531
72NA 88532RJLSEUS2022-003Alnus serrulata (Aiton) Willd. North Carolina, United StatesNA2023COLLECTED12/06/2022Plants growing around a wetland on both sides of Scotland Lake Road, approximately 1.1 kilometers southwest of the junction with Hoffman Road (Scotland Co. Road 1328) in the Sandhills Game Lands. This plant is a common component of the moist to wet areas of the wetland habitats in this area. 34.98413200, -79.54196300118Plants are growing in part-shade to sun in a wet to inundated habitat that contains standing water and/or significant moisture year-round.
Soils: 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 (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=NCTp%3B11)
The primary soil type in the collection area is classified as Johnston Series soils (0 to 2 percent slopes, frequently flooded). The Johnston series consists of very deep, very poorly drained soils that are occasionally to frequently flooded for short to extended periods. Permeability is moderate to rapid. These nearly level soils are alluvial in origin and typical of floodplains and swamp. Slopes range from 0 to 2 percent. Johnston Series soils are comprised of mucky loam that is friable with siliceous elements in the upper 0-75 cm. Lower strata range in percentages of mucky loam and loamy fine sand.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2140761NA 88532
73NA 88533RJLSEUS2022-004Zenobia pulverulenta (W. Bartram ex Willd.) Pollard North Carolina, United StatesNA2023COLLECTED12/06/2022Plants growing in the wetlands and moist depressions along Scotland Co. Road 1328 in the Sandhills Game Lands. This plant is somewhat infrequent and sporadic, but abundant in places with moist to wet habitats in this area. 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.
Soils: 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 (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=NCTp%3B11)
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 (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2140762NA 88533
74NA 88539RJLSEUS2022-011Clethra tomentosa Lam. Georgia, United StatesNA2023COLLECTED12/08/2022Plants growing in the upper edges of a wetland in Longleaf pine forest on the north side of Old GA State Route 33, approximately 2.11 kilometers southwest of the junction with GA Hwy 33. Common at this site on the margins of the wetland community.31.42763000, -83.85190700108Plants are growing in part-shade of a Longleaf pine forest along the upper edges of a wetland community. Soils range seasonally from moist to mucky with occasional standing water in depressions.
Soils: The underlying geology of this area is of Neogene origin and characterized as Neogene Undifferentiated. It includes poorly sorted clayey sand and gravel deposited in a fluvial environment in South Carolina but becoming more fluvio-marine in Georgia. Unit is characterized by in situ weathered feldspar and an abundance of quartzite gravel and cobbles.
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 Pelham Loamy Sand soil (0 to 2 percent slopes). The Pelham Series consists of very deep, poorly drained, moderately permeable soils that formed in unconsolidated Coastal Plain sediments. These soils are on nearly level broad flats, toe slopes, depressions and drainageways. Slopes range from 0 to 5 percent. These soils are comprised of loamy sands that are friable to a depth of approximately 1 meter and sandy clay loam to a depth in the lower strata to about 2 meters. They are also strongly acid.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2140766NA 88539
75NA 88566RJLSEUS2022-039Rhododendron viscosum (L.) Torr. Florida, United StatesNA2023COLLECTED12/14/2022Plants growing in woodlands at Escribano Point Bayou Campground not far from the parking lot. Occasional.30.50990400, -87.004149001Plants are growing in shade to part-shade of dense mesic vegetation only a few meters from the edge of mixed evergreen and deciduous woodland associated with the Yellow River Marsh Aquatic Preserve. While this habitat is typical mesic and well-drained, it is clearly subject to periods of inundation from high tides or storms as it is a meter or less above the marsh habitat. Additionally, it seems likely that there is plentiful moisture further down in the soil profile based on some of the plant associates.
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 FL Map Data (https://mrdata.usgs.gov/geology/state/state.php?state=fl)
The primary soil types in the collection area are classified as Ortega Sand soils (0 to 5 percent slopes). The Ortega Series consists of very deep, moderately well drained soils that formed in a sandy deposit on marine terraces. These soils are on nearly level to strongly sloping upland landscapes. Slopes range from 0 to 12 percent. They are extremely acid to slightly acid throughout. They are fine sand or sand to depths of more than 2 meters. Silt plus clay totals less than 5 percent between 25 cm and 1 meter depth.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2140788NA 88566
76NA 88567RJLSEUS2022-040Chamaecyparis thyoides (L.) Britton et al. Florida, United StatesNA2023COLLECTED12/14/2022Plants growing in woodlands at Escribano Point Bayou Campground not far from the parking lot. Occasional.30.51018200, -87.004488001Plants are growing in part-shade of dense mesic vegetation only a few meters from the edge of mixed evergreen and deciduous woodland associated with the Yellow River Marsh Aquatic Preserve. While this habitat surface is typical mesic and well-drained, it is clearly subject to periods of inundation from high tides or storms as it is a meter or less above the marsh habitat. Additionally, it seems likely that there is plentiful moisture further down in the soil profile based on some of the plant associates.
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 FL Map Data (https://mrdata.usgs.gov/geology/state/state.php?state=fl)
The primary soil types in the collection area are classified as Ortega Sand soils (0 to 5 percent slopes). The Ortega Series consists of very deep, moderately well drained soils that formed in a sandy deposit on marine terraces. These soils are on nearly level to strongly sloping upland landscapes. Slopes range from 0 to 12 percent. They are extremely acid to slightly acid throughout. They are fine sand or sand to depths of more than 2 meters. Silt plus clay totals less than 5 percent between 25 cm and 1 meter depth.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2140789NA 88567
77NA 88568RJLSEUS2022-041Oxydendrum arboreum (L.) DC. Florida, United StatesNA2023COLLECTED12/14/2022Plants growing along the south side of Eglin AFB Choctaw Nolf Road northwest of Choctaw Navy Outlying Field. This road goes west and takes circuitous route to the north around the Field enroute to Escribano Point Wildlife Management Area. Common at the location; infrequent, otherwise. 30.51525300, -87.005638002Trees are growing in full sun to part-shade in mesic habitat associate with a nearby wet depression, less than 0.2 meters above the high moisture zone. The trees also extend into slightly drier mesic to the marginally xeric zone.
Soils: The underlying geology of this area is classified as Alluvium, of Pleistocene/Holocene origin and consists of undifferentiated Quaternary sediments of varying thickness including siliciclastics, organics and freshwater carbonates. The siliciclastics are light gray, tan, brown to black, unconsolidated to poorly consolidated, clean to clayey, silty, unfossiliferous, variably organic-bearing sands to blue green to olive green, poorly to moderately consolidated, sandy, silty clays. Organics occur as plant debris, roots, disseminated organic matrix and beds of peat. Freshwater carbonates, often referred to as marls in the literature, are scattered.
The primary soil types in the collection area are classified as Leon Sand soils (0 to 2 percent slopes). The Leon Series consists of very deep, very poorly and poorly drained, moderately rapid to moderately slowly permeable soils on upland flats, depressions, stream terraces and tidal areas. They formed in sandy marine sediments of the Eastern Gulf Coast Flatwoods, the Atlantic Coast Flatwoods, and to a lesser extent in the Southern Coastal Plain, and the North-Central Florida Ridge. Slopes range from 0 to 5 percent. Leon series is comprised of 95%+ sand in the strata to 3+ meters deep.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2140790NA 88568
78WLP 2676RJL2022NJ-007Kalmia latifolia L. New Jersey, United StatesNA2022COLLECTED10/24/2022Plants growing along Hawkins Bridge Road in Wharton State Forest. Plants are common and frequent throughout the woodlands at this location. 39.70292400, -74.5610680016Plants growing in a mixed Conifer-Broadleaved Evergreen-Deciduous dry to xeric forest habitat in part shade to shade.
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 Lakehurst sand, 0 to 5 percent slopes. Other related soils are found along the collection area; even so, this is the dominant soil in the collecting area of this species. This soil is primarily sandy coastal plain deposition that is moderately well-drained with limited organic matter in the upper horizon. This soil ranges in depth from 0.1-1.5 meters. It is very strongly acidic throughout. It is subject to periods of extreme drought.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2139667WLP 2676
79WLP 2675RJL2022NJ-006Kalmia angustifolia L. New Jersey, United StatesNA2022COLLECTED10/24/2022Plants growing along Hawkins Bridge Road in Wharton State Forest. Plants are common and frequent throughout the woodlands at this location. 39.70231900, -74.5608420016Plants growing in a mixed Conifer-Broadleaved Evergreen-Deciduous dry to xeric forest habitat in part shade to part sun.
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 Lakehurst sand, 0 to 5 percent slopes. Other related soils are found along the collection area; even so, this is the dominant soil in the collecting area of this species. This soil is primarily sandy coastal plain deposition that is moderately well-drained with limited organic matter in the upper horizon. This soil ranges in depth from 0.1-1.5 meters. It is very strongly acidic throughout. It is subject to periods of extreme drought.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2139666WLP 2675
80NA 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
81WLP 2669RJL2022NJ-001Rhododendron viscosum (L.) Torr. New Jersey, United StatesNA2022COLLECTED10/19/2022Plants growing near the confluence of Springers Brook and Mullica River in Wharton State Forest around wetlands and associated woodlands accessed off of an unnamed road from Stokes Road. Plants are common but scattered on the edges and in the understory of low-lying wet woodlands. 39.72857100, -74.677982007Plants are growing in part-shade to shade of mixed deciduous and evergreen forests on moist slopes to occasionally wet low-lying areas fed by Springers Brook.
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 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 Fluvaquents, sandy, 0 to 3 percent slopes, frequently flooded. This soil is primarily stratified, wet soils on flood plains and deltas of middle and low latitudes. The stratification reflects deposition of sediments under changing currents and in shifting channels. The depth of this soil is approximately 5 meters and are consider very poorly drained; they are considered wet to inundated year-round.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2139660WLP 2669
82NA 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
83NA 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
84NA 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
85WLP 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
86W6 60625CA930E-17Camassia quamash (Pursh) Greene California, United StatesW6SEED2022Wild materialFlowers purple.2138744W6 60625
87NA 88414MARSB-446Pinus rigida Mill. New Jersey, United StatesNA2021Wild material2137177NA 88414
88W6 60080MARSB-134Hudsonia ericoides L. New Jersey, United StatesW62021Wild material2137165W6 60080
89NA 88426OR080-78Rosa nutkana C. Presl Oregon, United StatesNA2021Wild materialNative Rose w/ large pink flower and smaller leaves made from 7 serrated leaflets. The stems range from green-red-gray and the branches are mostly red-green in color. The thorns are mostly gray with a wide 1 cm diameter.2120737NA 88426
90NA 88223CA190B-151Ceanothus cuneatus (Hook.) Nutt. var. rigidus (Nutt.) Hoover California, United StatesNA2020Wild materialCeanothus rigidus is now recognized as species in new CA Jepson manual is simply Ceanothus rigidus. ûLeaves and branches are opposite; growing in the same vicinity as Ceanothus dentatus.2110333NA 88223
91NA 88240CA190B-159Ceanothus incanus Torr. & A. Gray California, United StatesNA2020Wild materialLeaves are larger than other Ft. Ord species and more supple.2110340NA 88240
92OPGC 7909MARSB-712Rhexia mariana L. New Jersey, United StatesOPGCSEED2019Wild material2097687OPGC 7909
93W6 56432CA190B-124Festuca octoflora Walter California, United StatesW6SEED2019Wild material2091935W6 56432
94W6 56435CA190B-128Turritis glabra L. California, United StatesW6SEED2019Wild material2091938W6 56435
95NA 88412OR110-1058Philadelphus lewisii Pursh Oregon, United StatesNASEED2018Wild materialPhiladelphus lewisii1970529NA 88412
96W6 55800OR110-1037Drymocallis glandulosa (Lindl.) Rydb. var. glandulosa Oregon, United StatesW62018Wild materialPotentilla glandulosa1970511W6 55800
97W6 55802OR110-1039Boykinia occidentalis Torr. & A. Gray Oregon, United StatesW6SEED2018Wild materialBoykinia occidentalis1970513W6 55802
98W6 55803OR110-1040Hosackia crassifolia Benth. Oregon, United StatesW6SEED2018Wild materialLotus crassifolius. SOS 7th transfer.1970514W6 55803
99W6 55819OR110-1059Physocarpus capitatus (Pursh) Kuntze Oregon, United StatesW6SEED2018Wild materialPhysocarpus capitatus1970530W6 55819
100W6 55850AZ040-291Hymenoxys hoopesii (A. Gray) Bierner Arizona, United StatesW6SEED2018Wild materialHymenoxys hoopesii1970561W6 55850
101NA 85524NACPEC18-071Pteroceltis tatarinowii Maxim. Hubei Sheng, ChinaNA2018COLLECTED09/19/2018Shennongjia Forest District; Mawan; Mawan.31.82953000, 110.64051000969Mixed mesophytic forest on moderate slope above small stream. Growing in leafy humus over clay/rocks.Seeds and four herbarium specimens collected from one plant. Photographed.2108983NA 85524
102W6 54050MARSB-352Juncus effusus L. New York, United StatesW6SEED2018Wild materialJuncus effusus1964766W6 54050
103W6 53688OR110-1007Hosackia crassifolia Benth. Oregon, United StatesW6SEED2018Wild material SOS 7th transfer.1964266W6 53688
104W6 53693OR110-1013Chamaenerion angustifolium (L.) Scop. subsp. angustifolium Oregon, United StatesW6SEED2018Wild material1964271W6 53693
105W6 53466NM030-64Chamaenerion angustifolium (L.) Scop. subsp. angustifolium New Mexico, United StatesW62018Wild material1958201W6 53466
106NA 87975OR080-54Rhododendron macrophyllum D. Don ex G. Don Oregon, United StatesNASEED2018Wild material1957637NA 87975
107NA 88204CBG-7297Ceanothus americanus L. Wisconsin, United StatesNASEED2017Wild material1954781NA 88204
108OPGC 6286OR130-100Eriophyllum lanatum (Pursh) J. Forbes Washington, United StatesOPGC2017Wild material1947329OPGC 6286
109W6 51918OR130-106Lomatium nudicaule (Pursh) J. M. Coult. & Rose Washington, United StatesW62017Wild material1947051W6 51918
110W6 51919OR130-107Allium cernuum Roth Washington, United StatesW62017Wild material1947052W6 51919
111W6 51923OR130-94Lomatium utriculatum (Nutt.) J. M. Coult. & Rose Washington, United StatesW62017Wild material1947056W6 51923
112W6 51925OR130-96Sisyrinchium idahoense E. P. Bicknell Washington, United StatesW62017Wild material1947058W6 51925
113W6 51927OR130-98Anisocarpus madioides Nutt. Washington, United StatesW62017Wild material1947060W6 51927
114OPGC 7157CBG-5314Geum aleppicum Jacq. Wisconsin, United StatesOPGC2016Wild material1942769OPGC 7157
115W6 51638CBG-5283Carex gynandra Schwein. Wisconsin, United StatesW62016Wild material1942768W6 51638
116W6 48844MARSB-64Danthonia compressa Austin West Virginia, United StatesW6SEED2015Wild material1922853W6 48844
117NA 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
118NA 81936NA 81936Magnolia virginiana L. Texas, United StatesNA2013COLLECTED04/11/2011On S side of County Road 59 ca. 1000 ft. W of it's juncture with Private Road 335 and ca. 0.25 miles N of Highway 255.31.05566000, -94.15485000Growing in seepage areas of otherwise dry Pinus palustris forest.1951206NA 81936
119OPGC 4421412823Ranunculus occidentalis Nutt. Washington, United StatesOPGCSEED2009COLLECTED06/02/200750Dry meadow, mounded prairie. Associated with Pteridium aquifolium, Hypochaeris radicata, Campanula rotundifolia, Festuca roemeri, Festuca rubra, Brodiaea coronaria, Chrysanthemum leucanthemum, Agrostis tenuis, Holcus lanatus etc.Wild material1826919OPGC 4421
120W6 35271RC32Microseris laciniata (Hook.) Sch. Bip. Washington, United StatesW6SEED2009Wild material1802247W6 35271
121NA 78035AL #44Philadelphus inodorus L. Alabama, United StatesNA2008COLLECTED09/17/2008Just above the Cahaba River, near end of road and Caffee Creek.Wild material1913895NA 78035
122Ames 29125JM200709111Hypericum androsaemum L. Ajaria, GeorgiaNC7HABITAT2007COLLECTED09/10/2007Chakuistskali River Valley Gorge, Mtrila National Forest, Ajara Region.41.70333333, 41.8077777840Colchic forest. Wet rock face beside road and above river.Wild material1744161Ames 29125
123Ames 29142JM200709112Hypericum perforatum L. Ajaria, GeorgiaNC7HABITAT2007COLLECTED09/10/2007Chakuistskali River Valley Gorge, Mtrila National Forest, Ajara Region.41.70333333, 41.8077777840Colchic forest. Wet rock face beside road and above river.Wild material1744178Ames 29142
124Ames 29149JM200709113Hypericum ×inodorum Mill. Ajaria, GeorgiaNC7HABITAT2007COLLECTED09/10/2007Chakuistskali River Valley Gorge, Mtrila National Forest, Ajara Region.41.70333333, 41.8077777840Colchic forest. Wet rock face beside road and above river.Wild material1744185Ames 29149
125Ames 31396271767Monardella villosa Benth. subsp. villosa California, United StatesNC7SEED2007COLLECTED08/02/2005Monterey County: At the junction of Pilarcitos Road and Jacks' Road and also on Engineer Canyon Road.36.61889000, -121.7225000060Oak woodland. Aspect: N-NE-NW. Light brown/greyish brown soil.Wild materialForb, Height about: 0.3 m1728075Ames 31396
126W6 30208CA330-50Elymus multisetus (J. G. Sm.) Burtt Davy California, United StatesW6SEED2007Wild material1719004W6 30208
127W6 26858ROSE-9Danthonia californica Bol. Oregon, United StatesW6SEED2005Wild materialGrasslike 0.07 meters tall. 1673897W6 26858
128W6 27009ROSE-32Scirpus microcarpus J. Presl & C. Presl Oregon, United StatesW6SEED2005Wild materialGrasslike 0.9-1.6 meters tall. 1674046W6 27009
129NA 70425MWPCC00-081Nyssa sylvatica Marshall North Carolina, United StatesNA2000COLLECTED09/15/2000Buncombe Co. Asheville NC. North Carolina Arboretum35.49611111, -82.60972222713near the top of a slope, native vegetation, adfacent to a service road and mowed roadside; associates; Oxydendrum, Rhus radicans, Kalmia latifolia, Acer rubrum, Quercus prinus, Quercus marilandica, Pteridium.Wild materialDry site for species, defoliation from stress? Ron Lance mentioned plants like this one from drier sites tend to have larger leaves.1608271NA 70425