| 0 | NA 85961 | PCC15-SEUSA025 | Quercus boyntonii Beadle | Alabama, United States | NA | | | 2017 | COLLECTED | 10/28/2015 | Shelby County; Birmingham; Off parking lot of EBSCO Industries, Inc., located at 5724 US-280, Birmingham, Alabama. | 33.37888000, -86.67333000 | | Ridge of Appalachian forest. | Wild material | | 2109093 | NA 85961 |
| 1 | NA 88593 | 2024RJLNJ-001 | Ilex glabra (L.) A. Gray | New Jersey, United States | NA | | | 2024 | COLLECTED | 11/24/2024 | Mullica Township: Both sides of Duerer Street, approximately 0.37 kilometers southeast of 4th Avenue. | 39.55885000, -74.66442500 | 21 | 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. 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 material | | 2169930 | NA 88593 |
| 2 | NA 88852 | TJK2023FL-047 | Ilex glabra (L.) A. Gray | Florida, United States | NA | | | 2024 | COLLECTED | 12/26/2023 | South of Highway 98, west of Twine Road. Track has a very large powerline right-of-way to the east, and George Washington Swamp bottom to the west. | 29.77640000, -85.27410000 | 6 | Longleaf Pine-Saw Palmetto. This area appears to be declining in quality, as witnessed by the declining in Rhododendron stem/plant density. Possible contributing issues: lacking necessary fire regime, has not seen fire in 8-10 years, encroaching woody shrub layer, accumulating organic matter (pine needle), expanding tree canopy, Hurricane Michael. Slope: less than 7%. Aspect: West. Elevation: 20 feet. | Wild material | | 2165707 | NA 88852 |
| 3 | NA 88686 | TJK2023FL-033 | Ilex glabra (L.) A. Gray | Florida, United States | NA | | | 2023 | COLLECTED | 11/18/2023 | Navarre, Florida: Adams St. cul-de-sac, on nine-acre private property. Infrastructure development began and was terminated due to the lack of any engineering or environmental site planning (designated wetland status). It has remained idle for a number of years. | 30.40970000, -86.92980000 | 11 | Wet pine flatwood transitioning to a shrub bog habitat under fire suppression. Slope: 3.5%. Aspect: West. Elevation: 36 feet. | Wild material | | 2159098 | NA 88686 |
| 4 | NA 88538 | RJLSEUS2022-010 | Ilex glabra (L.) A. Gray | Georgia, United States | NA | | | 2023 | COLLECTED | 12/08/2022 | Junction of Old Whitley Rd & Irwinville Hwy (GA 125). | 31.64601300, -83.33625800 | 111 | Low woods, a remnant woodland/low moist habitat between agricultural fields. Growing in part shade to shade of a moist mesic (occasionally temporarily wet) mixed evergreen and deciduous woodland along the edge where light conditions are slightly higher. 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. This unit is characterized by in situ weathered feldspar and an abundance of quartzite gravel and cobbles. (Source: USGS Georgia Geologic Map Data). The primary soil types in the collection area are classified as Alapaha Loamy Sand soil (0 to 2 percent slopes, occasionally flooded). The Alapaha Series consists of very deep, poorly drained, moderately slow to slowly permeable soils in small drainageways, flats, seepage areas, and depressions. They formed in sandy and loamy marine deposits of the Southern Coastal Plain. Slopes range from 0 to 5 percent. This series consists of deep, somewhat poorly drained soils. Permeability is very slow. These nearly level to gently sloping soils formed in clayey alluvium on flood plains of streams that drain uplands of the Southern Coastal Plain. The water table ranges from 0-25 cm below the surface and the soils are strongly acid. (Source: NRCS Web Soil Survey). | Wild material | | 2140816 | NA 88538 |
| 5 | NA 88500 | RJL2022NJ-002 | Ilex glabra (L.) A. Gray | New Jersey, United States | NA | | | 2022 | COLLECTED | 10/24/2022 | Mullica Township: both sides of Duerer Street, approximately 0.37 kilometers southeast of 4th Avenue. | 39.55885000, -74.66442500 | 21 | Plants 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 material | | 2139663 | NA 88500 |
| 6 | Ames 35752 | #476-477 | Rhus glabra L. | Iowa, United States | NC7 |  | | 2021 | COLLECTED | 09/29/2021 | Upper Iowa River area near Bluffton, T99N R9W NE1/4 Sec. 9 and S1/2 Sec. 10 | 43.40275000, -91.90494000 | 299 | High bluffs, roadside and stream banks | Wild material | Plants sampled in nature (29 September 2021) during peak fall color displaying bright reds to maroonish colors while measuring approximately 12-15 feet in height. One clonal patch noted was estimated to have 1,000+ ramets. | 2122093 | Ames 35752 |
| 7 | NA 88096 | MARSB-258 | Ilex glabra (L.) A. Gray | New York, United States | NA |  | | 2019 | COLLECTED | 10/08/2015 | In Sag Harbor, park in Mashashimuet Park. Enter the Long Pond Greenbelt and walk along it until you reach Crooked Pond, the third pond on the left. The population is along pond edges. | 40.96283000, -72.29366000 | 5 | Central shrub & herb depression pond. | Wild material | | 2097545 | NA 88096 |
| 8 | NA 88110 | MARSB-426 | Ilex glabra (L.) A. Gray | New Jersey, United States | NA |  | | 2019 | COLLECTED | 11/04/2015 | Bass River State Forest: take Garden State Pkwy to E Greenbush Rd in Bass River. Take exit 52 from Garden State Pkwy toward New Gretna. Turn right onto Stage Rd and left onto Dump Rd. | 39.62786000, -74.43636000 | 5 | Pitch pine barrens. | Wild material | | 2097627 | NA 88110 |
| 9 | NA 88121 | MARSB-734 | Ilex glabra (L.) A. Gray | New York, United States | NA |  | | 2019 | COLLECTED | 10/27/2016 | Peasys Pond: drive down NY-25E past Brookhaven State Park. To your right is a hunter's parking area (across from Panamoka Trail). Park here and hike south on trail. Population is along edges of dry riverbeds and dry pond beds. | 40.90238000, -72.84072000 | 15 | Pine barren, pond edge. | Wild material | | 2097693 | NA 88121 |
| 10 | WLP 158 | NACPEC19-029 | Rhus glabra L. | Kentucky, United States | NA | | | 2019 | COLLECTED | 09/09/2019 | Madison County; Berea College Forest: Radio Tower Service Trail | 37.55289700, -84.28793400 | 379 | Xeric shade knob, limestone shale conglomerate material | Wild material | | 2110470 | WLP 158 |
| 11 | W6 56435 | CA190B-128 | Turritis glabra L. | California, United States | W6 |  | | 2019 | | | | | | | Wild material | | 2091938 | W6 56435 |
| 12 | WLP 1704 | NA 83942 | Rhus glabra L. | Kentucky, United States | NA | | | 2016 | COLLECTED | 09/29/2016 | Kentenia State Forest, Pine Mountain, on Route 1679, south side. | 36.90500000, -83.29100000 | 771 | Roadside. | | | 1953164 | WLP 1704 |
| 13 | PI 702720 | MARSB-360 | Schizachyrium scoparium (Michx.) Nash | New Jersey, United States | S9 |  | | 2019 | | | | | | | Wild material | | 2097597 | PI 702720 |
| 14 | PI 702722 | MARSB-400 | Schizachyrium scoparium (Michx.) Nash | New York, United States | S9 |  | | 2019 | | | | | | | Wild material | | 2097613 | PI 702722 |
| 15 | PI 704856 sos | V. corymbosum MARSB-569 | Vaccinium corymbosum L. | New York, United States | COR |  | | 2019 | | | | | | | Wild material | PI assigned before phyical inventory of W6 shipment and is missing. Maintain COR as site in case seeds are recovered. | 2097658 | PI 704856 sos |
| 16 | PI 710489 | MARSB-254 | Lespedeza capitata Michx. | New York, United States | S9 |  | | 2018 | | | | | | | Wild material | | 1964746 | PI 710489 |
| 17 | PI 664805 | JDC/HX/2010/035/305 | Helianthus mollis Lam. | Kansas, United States | NC7 | | | 2010 | COLLECTED | 09/14/2010 | Roadside along Kansas Rd, west of Hwy 3 south of Uniontown, Bourbon County. | 37.81978000, -94.98685000 | 325 | Uplands. Associated with Andropogon gerardii, Bidens polylepis, Chamaechrista fasciculata, Cornus, Diospyros virginiana, Gleditsia triacanthos, Juglans nigra, Maclura pomifera, Monarda, Pycnanthemum virginianum, Quercus, Rhus glabra, and Sorghastrum nutans. | Wild material | | 1848907 | PI 664805 |
| 18 | PI 664869 | JDC/HP/2008/030/100 | Hypericum prolificum L. | Missouri, United States | NC7 |  | | 2008 | COLLECTED | 10/06/2008 | Rudolf Bennitt Conservation Area, NE 1/4 of NE 1/4 of Section 25, T52N, R14W, Renick Quad, Randolph County. | 39.27527778, -92.43388889 | 256 | | Wild material | | 1788211 | PI 664869 |
| 19 | PI 649051 | C-H148 | Hypericum gentianoides (L.) Britton et al. | Florida, United States | NC7 | | | 2004 | COLLECTED | 11/03/2000 | Adjacent to a pine plantation, south side of Highway 231, 5 miles south Alford, Washington County. | 30.62054300, -85.39622500 | | | Wild material | Plant about 1 meter tall. | 1659755 | PI 649051 |
| 20 | PI 495604 | 8 | Cornus drummondii C. A. Mey. | Iowa, United States | NC7 |  | | 1984 | COLLECTED | 09/21/1984 | Along south end of parking area, Lake of Three Fires State Park, extreme NW corner of Section 7, T68N, R33W, Bedford Quad, Taylor County. | 40.71194444, -94.68583333 | 360 | | Wild material | Perennial woody. Plants in wide thicket to 2 meters tall, heavy fruiting. Very clean foliage with nice white fruits. | 1390540 | PI 495604 |
| 21 | NA 89180 | TJK | Rhododendron minus Michx. var. chapmanii (Alph. Wood) W. H. Duncan & Pullen | Florida, United States | NA | | Contact Site | 2026 | COLLECTED | 04/01/2025 | St. Joseph Bay State Buffer Preserve. Collected from 29.7187833056, -85.2683638611 to 29.7186610833, -85.2689666667 [Note: latitude and longitude of record is selected from the first set of coordinates rather than an average; see the additional field collection note regarding population concentrations.] | 29.71878331, -85.26836386 | 3 | This population is growing in full sun in an area that has been burned in recent years (time frame unknown) and possibly logged. There are scattered large pines, but little shade. This are has been heavily impacted by Category 4/5 hurricanes in recent years and some of the current conditions are undoubtedly a result of this. Soil: The soils of this site are classified as Leon fine sand, 0 to 2 percent slopes (22). 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 (MLRA 152A), the Atlantic Coast Flatwoods (MLRA 153A) and to a lesser extent in the Southern Coastal Plain (MLRA 133A) and the North-Central Florida Ridge (MLRA 138). Near the type location, the mean annual temperature is about 68 degrees F., and the mean annual precipitation is about 65 inches. Slopes range from 0 to 5 percent. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). Geology: The underlying geology of this area is characterized as Beach Ridge and Dune from the Pleistocene/Holocene which is 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. In an effort 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 material | Received as R. chapmanii | 2193314 | NA 89180 |
| 22 | NA 89174 | 2025RJLSEUS-16 | Kalmia hirsuta Walter | Florida, United States | NA | | | 2026 | COLLECTED | 10/04/2025 | Eglin Air Force Base: collected along Florida National Scenic Trail/Eglin AFB unnamed road. | 30.43936000, -86.84404500 | 7 | Growing in full sun in dry areas above stream. Slope: 0 percent. Aspect: N/A. Soil: The primary soil type in the collection area is classified as Pickney Loamy Sand soils. The Pickney Series consists of very deep, very poorly drained soils. Permeability is rapid. These nearly level soils have negligible runoff and were formed by marine or fluvial sediments in the lower coastal plain on flats, depressions, stream terraces, and flood plains. Slopes range from 0 to 2 percent. The soils of this series are loamy fine sand that is very friable and extremely acid in the upper 0-25 cm. The lower strata are similar, while the lower strata from 0.8-2 meters are comprised of fine sand. (Source: NRCS Web Soil Survey). Geology: 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). | Wild material | | 2193308 | NA 89174 |
| 23 | NA 89171 | 2025RJLSEUS-04 | Rhododendron catawbiense Michx. | Alabama, United States | NA | | | 2026 | COLLECTED | 09/30/2025 | Scarham Creek: southeast of the Pea Ridge Road bridge, approximately 50-80 meters on the south side of the creek. | 34.32559600, -86.16054600 | 266 | Growing near the base of the slopes above the riparian zone, generally on the exposed geology under very well-drained conditions. The woodlands are primarily deciduous with a few evergreens infrequently mixed. Slope: 15 to 30 percent. Aspect: Northeast. Soil: The primary soil type in the area of this collection is classified as Rockland Series sandstone (Rc). The Rockland series consists of well drained soils formed in loamy colluvium from rotational landslides on slopes of stream valleys and dissections of ground moraines. Saturated hydraulic conductivity is moderate in the upper part of the profile and moderately slow in the lower part. Slopes range from 18 to 70 percent. Some pedons have buried leaves, twigs, and moss. Mass soil movement has left random remnants of soil structure from prior upslope soil development and has buried tree branches, leaves and moss. The upper 0-2 cm of soil contains slightly decomposed organic matter while lower soils layers to a depth of 58 cm are comprised of dark reddish-brown to brown silt loam and are moderately acidic. Below 58 cm the soils are generally dark reddish-brown silt loam and strongly to moderately alkaline. (Source:California Soil Resource Lab/NRCS Official Soil Series Descriptions). Geology: The underlying geology of this area is of Pennsylvanian origin and characterized as Pottsville Formation. It is characterized by light-gray thin to thick-bedded quartzose sandstone and conglomerate containing interbedded dark-gray shale, siltstone, and coal. Mapped on Lookout Mountain, Blount and Chandler Mountains, and Sand Mountain northeast of Blount County, and on the mountains of Jackson, Marshall, and Madison Counties north and west of the TN river. (Source: USGS Alabama Geologic Map Data). | Wild material | Received as R. catawbiense vsr. insularis | 2193305 | NA 89171 |
| 24 | NA 89155 | 2025RJLSEUS-02 | Ilex longipes Chapm. ex Trel. | Alabama, United States | NA | | | 2025 | COLLECTED | 09/30/2025 | Scarham Creek: southeast of the Pea Ridge Road bridge, approximately 50-80 meters on the south side of the creek. | 34.32520700, -86.15967000 | 261 | Plants are growing on relatively steep woodland slopes in shade. The woodlands are primarily deciduous with a few evergreens infrequently mixed. Slope: 15 to 30 percent. Aspect: Northeast. Soil: The primary soil type in the area of this collection is classified as Rockland Series sandstone (Rc). The Rockland series consists of well drained soils formed in loamy colluvium from rotational landslides on slopes of stream valleys and dissections of ground moraines. Saturated hydraulic conductivity is moderate in the upper part of the profile and moderately slow in the lower part. Slopes range from 18 to 70 percent. Some pedons have buried leaves, twigs, and moss. Mass soil movement has left random remnants of soil structure from prior upslope soil development and has buried tree branches, leaves and moss. The upper 0-2 cm of soil contains slightly decomposed organic matter while lower soils layers to a depth of 58 cm are comprised of dark reddish-brown to brown silt loam and are moderately acidic. Below 58 cm the soils are generally dark reddish-brown silt loam and strongly to moderately alkaline. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). Geology: The underlying geology of this area is of Pennsylvanian origin and characterized as Pottsville Formation. It is characterized by light-gray thin to thick-bedded quartzose sandstone and conglomerate containing interbedded dark-gray shale, siltstone, and coal. Mapped on Lookout Mountain, Blount and Chandler Mountains, and Sand Mountain northeast of Blount County, and on the mountains of Jackson, Marshall, and Madison Counties north and west of the TN river. (Source: USGS Alabama Geologic Map Data). | Wild material | | 2193001 | NA 89155 |
| 25 | NA 89156 | 2025RJLSEUS-03 | Euonymus americanus L. | Alabama, United States | NA | | | 2025 | COLLECTED | 09/30/2025 | Scarham Creek: southeast of the Pea Ridge Road bridge, approximately 50-80 meters on the south side of the creek. | 34.32577600, -86.16071000 | 260 | Plants are growing on relatively steep woodland slopes in shade. The woodlands are primarily deciduous with a few evergreens infrequently mixed. Slope: 15 to 30 percent. Aspect: Northeast. Soil: The primary soil type in the area of this collection is classified as Rockland Series sandstone (Rc). The Rockland series consists of well drained soils formed in loamy colluvium from rotational landslides on slopes of stream valleys and dissections of ground moraines. Saturated hydraulic conductivity is moderate in the upper part of the profile and moderately slow in the lower part. Slopes range from 18 to 70 percent. Some pedons have buried leaves, twigs, and moss. Mass soil movement has left random remnants of soil structure from prior upslope soil development and has buried tree branches, leaves and moss. The upper 0-2 cm of soil contains slightly decomposed organic matter while lower soils layers to a depth of 58 cm are comprised of dark reddish-brown to brown silt loam and are moderately acidic. Below 58 cm the soils are generally dark reddish-brown silt loam and strongly to moderately alkaline. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). Geology: The underlying geology of this area is of Pennsylvanian origin and characterized as Pottsville Formation. It is characterized by light-gray thin to thick-bedded quartzose sandstone and conglomerate containing interbedded dark-gray shale, siltstone, and coal. Mapped on Lookout Mountain, Blount and Chandler Mountains, and Sand Mountain northeast of Blount County, and on the mountains of Jackson, Marshall, and Madison Counties north and west of the TN river. (Source: USGS Alabama Geologic Map Data). | Wild material | | 2193002 | NA 89156 |
| 26 | NA 89158 | 2025RJLSEUS-06 | Cornus florida L. | Alabama, United States | NA | | | 2025 | COLLECTED | 10/01/2025 | Coosa Wildlife Management Area: along the edge of gated dirt road on the west side of Coosa County Road 29, 0.3 kilometers north of Hatchet Creek. | 32.86402200, -86.33871400 | 108 | Plants are growing in part sun to shade on dry-mesic slopes above the road cut on the gated dirt road; most likely a road for access for fire control/forest management. The forest is a combination of deciduous and evergreen with evergreens primarily comprised of Pinus taeda. The habitat was quite dry during this time of year. Slope: 5 to 20 percent. Aspect: North. Soils: The primary soil in the area of this collection is classified as Madison-Louisa Series complex, 15 to 30 percent slopes, moderately eroded (MdE2). The Madison Series soils are very deep, well drained soils with medium runoff found on Piedmont uplands in interstream divides, ridges and side slopes. They are comprised of residuum weathered from felsic or intermediate, high-grade metamorphic or igneous rocks high in content of mica. Slopes range from 2 to 60 percent and soil is typically strongly acidic. Louisa Series soils The Louisa Series soils consist of shallow, somewhat excessively drained soils which formed over mica gneiss and schist bedrock. They occur on Piedmont uplands. Slopes are 6 to 80 percent. This soil is moderately acid. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). Geology: The underlying geology of this area is of Precambrian to Paleozoic origin and characterized as Hatchet Creek Group; Pinchoulee Gneiss Formation. It is characterized by medium to fine-grained migmatitic, locally garnetiferous biotite-feldspar gneiss, commonly saturated with granitic pods. (Source: USGS Alabama Geologic Map Data). | Wild material | | 2193004 | NA 89158 |
| 27 | NA 89161 | 2025RJLSEUS-10 | Stewartia malacodendron L. | Florida, United States | NA | | | 2025 | COLLECTED | 10/02/2025 | Eglin Air Force Base: woodlands along Weaver Creek accessed from unnamed dirt road, 0.82 kilometers west of junction with Eglin AFB 720; approximately 0.73 kilometers north of junction with Choctaw Nolf Airfield Road and Eglin AFB 720. | 30.51708000, -86.91515000 | 11 | Moist, well-drained, sandy soils above Weaver Creek in a mixed broadleaved evergreen and deciduous woodland habitat in part shade to shade of west facing slopes several meters above the wetland zone. A high-competition, richly diverse environment. Elevation: 7 to 15 meters. Slope: 1 to 15 percent. Aspect: West. Soils: The soils of this area are characterized as Lakeland Series which consist 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: USDA-NRCS Official Soil Series Descriptions). Geology: 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). | Wild material | | 2193007 | NA 89161 |
| 28 | NA 89115 | TLM25-04a | Hamamelis ovalis S. W. Leonard | Texas, United States | NA | | | 2025 | COLLECTED | 07/10/2025 | State 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, -93.72628100 | 138 | The 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 material | | 2191654 | NA 89115 |
| 29 | NA 88757 | 2025 TKRM-001 | Cyrilla racemiflora L. | Florida, United States | NA | | | 2025 | COLLECTED | 01/03/2025 | Area on the south side of an unnamed sand road, about 0.54 kilometers south of Florida State Highway 98 and accessed from Walton County Highway 283 S. The collecting site is accessed by going east 0.54 kilometers on the unnamed sand road from the junction with Walton County Highway 283 S. | 30.35374700, -86.15172700 | 12 | Mostly found in moist to dry flatwoods in mixed evergreen and deciduous forest. Slope: N/A. Aspect: various. 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. In an effort 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 in order to facilitate a better understanding of the State's geology. The siliciclastics are light gray, tan, brown to black, unconsolidated to poorly consolidated, clean to clayey, silty, unfossiliferous, variably organic-bearing sands to blue green to olive green, poorly to moderately consolidated, sandy, silty clays. Gravel is occasionally present in the panhandle. Organics occur as plant debris, roots, disseminated organic matrix and beds of peat. Freshwater carbonates, often referred to as marls in the literature, are scattered over much of the State. In southern Florida, freshwater carbonates are nearly ubiquitous in the Everglades. These sediments are buff colored to tan, unconsolidated to poorly consolidated, fossiliferous carbonate muds. Sand, silt and clay may be present in limited quantities. These carbonates often contain organics. The dominant fossils in the freshwater carbonates are mollusks. (Source: USGS Florida Geologic Map Data). The Hurricane Series consists of very deep, somewhat poorly drained, moderately rapid permeable soils on broad areas that are slightly higher than the adjacent flats in the Southern Coastal Plain (MLRA 133A), the Gulf Coast Flatwoods (MLRA 152A) and the Atlantic Coast Flatwoods (MLRA 153A). They formed in sandy marine sediments. Slopes range from 0 to 5 percent. Solum thickness is 1.5 meters or more. Reaction ranges from extremely acid to moderately acid throughout. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). | Wild material | Received as Cyrilla parvifolia. | 2171019 | NA 88757 |
| 30 | NA 88578 | 2024RJLFL-004 | Ilex vomitoria Aiton | Florida, United States | NA | | | 2024 | COLLECTED | 11/12/2024 | Collected along Florida National Scenic Trail/Eglin Air Force Base unnamed road. | 30.44526100, -86.86094700 | 4 | Mixed evergreen and deciduous forests in part shade to full sun. 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 Lakeland Series Sand, 5 to 12 percent slopes. The Lakeland series consists of very deep, excessively drained, rapid to very rapidly permeable soils on uplands. They formed in thick beds of eolian or marine and/or fluvio-marine sands in the Southern Coastal Plain MLRA (133A), the Carolina and Georgia Sandhills (MLRA 137), the Eastern Gulf Coast Flatwoods (MLRA 152A) and the Atlantic Coast Flatwoods (MLRA 153A). Slopes are dominantly from 0 to 12 percent but can range to 85 percent in dissected areas. Thickness of the sand exceeds 200 cm. Silt plus clay in the 25 to 100 cm control section ranges from 5 to 10 percent. Reaction ranges from very strongly acid to moderately acid throughout. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). | Wild material | | 2169915 | NA 88578 |
| 31 | NA 88579 | 2024RJLFL-007 | Ilex myrtifolia Walter | Florida, United States | NA | | | 2024 | COLLECTED | 11/13/2024 | Wetlands accessed from Miller Bluff Road. | 30.62251200, -86.86030700 | 8 | Open, wet areas and woodland edge slightly above permanently wet habitat in part shade to full sun. Slope: 0 percent. Aspect: N/A. | Wild material | | 2169916 | NA 88579 |
| 32 | NA 88580 | 2024RJLFL-009 | Ilex myrtifolia Walter | Florida, United States | NA | | | 2024 | COLLECTED | 11/13/2024 | Woodlands on the north side of Fisher Old Mill Road about 0.10 kilometers west of intersection with DOF Y12. | 30.62693800, -86.83962200 | 6 | Mixed evergreen and deciduous moist to wet forest in part shade to full sun. From the associated taxa, this site can be quite wet during the growing season; however, it was dry during this collection time; likely due to extended drought. Slope: 0 percent. Aspect: South. | Wild material | | 2169917 | NA 88580 |
| 33 | NA 88581 | 2024RJLFL-012 | Ilex ambigua Torr. | Florida, United States | NA | | | 2024 | COLLECTED | 11/13/2024 | Woodland edge along the south side of Bud Bass Road (DOF B48), 0.30 kilometers east of the junction with Norman Riley Road. | 30.75763200, -86.80184300 | 32 | Woodland edge. Slope: 3 percent. Aspect: North. The underlying geology of this area is characterized as Citronelle Formation of the Pliocene period. The Citronelle Formation is widespread in the Gulf Coastal Plain. The type section for the Citronelle Formation, named by Matson (1916), is near Citronelle, Alabama. The Citronelle Formation grades laterally, through a broad facies transition, into the Miccosukee Formation of the eastern Florida panhandle. Coe (1979) investigated the Citronelle Formation in portions of the western Florida panhandle. The Citronelle Formation is a siliciclastic, deltaic deposit that is lithologically similar to, and time equivalent with, the Cypresshead Formation and, at least in part, the Long Key Formation (Cunningham et al., 1998) of the peninsula. In the western panhandle, some of the sediments mapped as Citronelle Formation may be reworked Citronelle. The lithologies are the same and there are few fossils present to document a possible younger age. The Citronelle Formation consists of gray to orange, often mottled, unconsolidated to poorly consolidated, very fine to very coarse, poorly sorted, clean to clayey sands. It contains significant amounts of clay, silt and gravel which may occur as beds and lenses and may vary considerably over short distances. Limonite nodules and limonite-cemented beds are common. Marine fossils are rare but fossil pollen, plant remains and occasional vertebrates are found. Much of the Citronelle Formation is highly permeable. It forms the Sand and Gravel Aquifer of the surficial aquifer system contain organics. The dominant fossils in the freshwater carbonates are mollusks. (Source: USGS Florida Geologic Map Data). The soils of this are characterized as Lakeland Series Sand, 0 to 5 percent slopes. The Lakeland series consists of very deep, excessively drained, rapid to very rapidly permeable soils on uplands. They formed in thick beds of eolian or marine and/or fluvio-marine sands in the Southern Coastal Plain MLRA (133A), the Carolina and Georgia Sandhills (MLRA 137), the Eastern Gulf Coast Flatwoods (MLRA 152A) and the Atlantic Coast Flatwoods (MLRA 153A). Slopes are dominantly from 0 to 12 percent but can range to 85 percent in dissected areas. Thickness of the sand exceeds 200 cm. Silt plus clay in the 25 to 100 cm control section ranges from 5 to 10 percent. Reaction ranges from very strongly acid to moderately acid throughout. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). | Wild material | | 2169918 | NA 88581 |
| 34 | NA 88584 | 2024RJLFL-016 | Cornus florida L. | Florida, United States | NA | | | 2024 | COLLECTED | 11/14/2024 | Both sides of Kennedy Bridge Road approximately 0.27 kilometers west of the junction with Hurricane Lake South Entrance Road. | 30.93159700, -86.74928000 | 43 | Mesic 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 material | | 2169921 | NA 88584 |
| 35 | NA 88586 | 2024RJLFL-020 | Vaccinium arboreum Marshall | Florida, United States | NA | | | 2024 | COLLECTED | 11/14/2024 | Woodland edge off of Ralf Laurant Road, above the wetland/headwaters of Danley Branch along the edge of a young longleaf pine plantation. | 30.90104300, -86.78878100 | 61 | Edge 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 material | | 2169923 | NA 88586 |
| 36 | NA 88589 | 2024RM-002 | Lyonia ferruginea (Walter) Nutt. | Florida, United States | NA | | | 2024 | COLLECTED | 11/21/2024 | Eglin Air Force Base: collected along an unnamed sand road that leads to the former Flowers Boat Landing (now permanently closed) along the Yellow River. Accessed by boat. | 30.60823600, -86.83595500 | 6 | Mixed evergreen and deciduous open habitat in part shade to full sun. Slope: 0 to 1 percent. Aspect: N/A. The underlying geology of this area is characterized as Alluvium from undifferentiated Quaternary Sediments. Much of Florida's surface is covered by a varying thickness of undifferentiated sediments consisting of siliciclastics, organics and freshwater carbonates. Where these sediments exceed 20 feet (6.1 meters) thick, they were mapped as discrete units. To subdivide the undifferentiated sediments, those sediments occurring in flood plains were mapped as alluvial and flood plain deposits (Qal). Sediments showing surficial expression of beach ridges and dunes were mapped separately (Qbd) as were the sediments composing Trail Ridge (Qtr). Terrace sands were not mapped (refer to Healy [1975] for a discussion of the terraces in Florida). The subdivisions of the Undifferentiated Quaternary Sediments (Qu) are not lithostratigraphic units but are utilized to facilitate a better understanding of the State's geology. The siliciclastics are light gray, tan, brown to black, unconsolidated to poorly consolidated, clean to clayey, silty, unfossiliferous, variably organic-bearing sands to blue green to olive green, poorly to moderately consolidated, sandy, silty clays. Gravel is occasionally present in the panhandle. Organics occur as plant debris, roots, disseminated organic matrix and beds of peat. Freshwater carbonates, often referred to as marls in the literature, are scattered over much of the State. In southern Florida, freshwater carbonates are nearly ubiquitous in the Everglades. These sediments are buff colored to tan, unconsolidated to poorly consolidated, fossiliferous carbonate muds. Sand, silt and clay may be present in limited quantities. These carbonates often contain organics. The dominant fossils in the freshwater carbonates are mollusks. (Source: USGS Florida Geologic Map Data). The soils of this are characterized as Dorovan-Pamlico Series association. The Dorovan Series consists of very deep, very poorly drained, moderately permeable soils on densely forested flood plains, hardwood swamps, and depressions in the Atlantic Coast Flatwoods (153A), Eastern Gulf Coast Flatwoods (152A), and Southern Coastal Plain Major (133A) Land Resource Areas. They formed in highly decomposed acid-organic materials. Slopes are less than 1 percent. The organic material ranges from 1.3 to 2 meters or more thick. Reaction is extremely acid to very strongly acid in the organic layers and very strongly acid or strongly acid in the mineral layers. 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 to 1.3 meters of organic material over dominantly sandy sediments. Reaction is extremely acid (less than 4.5 in 0.01 M calcium chloride) in the organic layers, and ranges from extremely acid to strongly acid in the underlying mineral layers. | Wild material | | 2169926 | NA 88589 |
| 37 | NA 88590 | 2024RM-003 | Ilex verticillata (L.) A. Gray | Florida, United States | NA | | | 2024 | COLLECTED | 11/21/2024 | Along the west/north side of the Yellow River about 0.33 kilometers (as the crow flies) upstream from the channel that leads the Fisher Old Mill Road Boat Ramp. This site was accessed by boat. | 30.62868600, -86.80748000 | 4 | Plants are found growing primarily in permanently saturated to submersed conditions along the edge of the Yellow River in part shade. The riverine habitat is comprised of a wide array of deciduous and evergreen trees, shrubs, and perennial plant species. Most of the plants along the river are adapted to acidic conditions and, while the aquatic habitat is generally fresh water, there is occasionally tidal or hurricane-caused saltwater intrusions. Slope: 0 percent. Aspect: East-southeast. The underlying geology of this area is characterized as Alluvium from undifferentiated Quaternary Sediments. Much of Florida's surface is covered by a varying thickness of undifferentiated sediments consisting of siliciclastics, organics and freshwater carbonates. Where these sediments exceed 20 feet (6.1 meters) thick, they were mapped as discrete units. To subdivide the undifferentiated sediments, those sediments occurring in flood plains were mapped as alluvial and flood plain deposits (Qal). Sediments showing surficial expression of beach ridges and dunes were mapped separately (Qbd) as were the sediments composing Trail Ridge (Qtr). Terrace sands were not mapped (refer to Healy [1975] for a discussion of the terraces in Florida). The subdivisions of the Undifferentiated Quaternary Sediments (Qu) are not lithostratigraphic units but are utilized to facilitate a better understanding of the State's geology. The siliciclastics are light gray, tan, brown to black, unconsolidated to poorly consolidated, clean to clayey, silty, unfossiliferous, variably organic-bearing sands to blue green to olive green, poorly to moderately consolidated, sandy, silty clays. Gravel is occasionally present in the panhandle. Organics occur as plant debris, roots, disseminated organic matrix and beds of peat. Freshwater carbonates, often referred to as marls in the literature, are scattered over much of the State. In southern Florida, freshwater carbonates are nearly ubiquitous in the Everglades. These sediments are buff colored to tan, unconsolidated to poorly consolidated, fossiliferous carbonate muds. Sand, silt and clay may be present in limited quantities. These carbonates often contain organics. The dominant fossils in the freshwater carbonates are mollusks. (Source: USGS Florida Geologic Map Data). The soils of this are characterized as Bibb-Kinston Series association. The Bibb Series consists of very deep, poorly drained, moderately permeable soils on flood plains of streams in the Southern Coastal Plain (133A) Major Land Resource Area. They formed in stratified loamy and sandy alluvium that are commonly and frequently flooded and water runs off the surface very slowly. Slopes range from 0 to 2 percent. Reaction ranges from extremely acid to strongly acid throughout. Content of mica flakes ranges from none to common. Content of rounded gravel typically ranges from 0 to 10 percent throughout, but may range to 50 percent in thin strata below a depth of 1 meter. Buried soil horizons, present in many pedons have the same range in color and texture as the surface horizon which has iron and organic matter concentrations in shades of brown and yellow ranging from none to common. Texture is sand, loamy sand, loamy fine sand, fine sandy loam, sandy loam, loam or silt loam. The Kinston Series consists of very deep, poorly drained, moderately permeable soils found on flood plains. They were formed in alluvial depositions. Slopes range from 0 to 2 percent. Soil reaction ranges from strongly acid to very strongly acid. Typical texture across the pedons is loamy, gravelly loam, sandy loam, and clay loam with dark concretions often present. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). | Wild material | | 2169927 | NA 88590 |
| 38 | NA 88591 | 2024RM-004 | Ilex opaca Aiton | Florida, United States | NA | | | 2024 | COLLECTED | 11/21/2024 | Along the west/north side of the Yellow River about 5.5 kilometers upstream from the State Highway 87 boat ramp. This site was accessed by boat. | 30.59986000, -86.87936000 | 2 | Plants are found growing primarily in permanently saturated to submersed conditions along the edge of the Yellow River in part shade. The riverine habitat is comprised of a wide array of deciduous and evergreen trees, shrubs, and perennial plant species. Most of the plants along the river are adapted to acidic conditions and, while the aquatic habitat is generally fresh water, there is occasionally tidal or hurricane-caused saltwater intrusions. Slope: 0 percent. Aspect: East-southeast. The underlying geology of this area is characterized as Alluvium from undifferentiated Quaternary Sediments. Much of Florida's surface is covered by a varying thickness of undifferentiated sediments consisting of siliciclastics, organics and freshwater carbonates. Where these sediments exceed 20 feet (6.1 meters) thick, they were mapped as discrete units. To subdivide the undifferentiated sediments, those sediments occurring in flood plains were mapped as alluvial and flood plain deposits (Qal). Sediments showing surficial expression of beach ridges and dunes were mapped separately (Qbd) as were the sediments composing Trail Ridge (Qtr). Terrace sands were not mapped (refer to Healy [1975] for a discussion of the terraces in Florida). The subdivisions of the Undifferentiated Quaternary Sediments (Qu) are not lithostratigraphic units but are utilized to facilitate a better understanding of the State's geology. The siliciclastics are light gray, tan, brown to black, unconsolidated to poorly consolidated, clean to clayey, silty, unfossiliferous, variably organic-bearing sands to blue green to olive green, poorly to moderately consolidated, sandy, silty clays. Gravel is occasionally present in the panhandle. Organics occur as plant debris, roots, disseminated organic matrix and beds of peat. Freshwater carbonates, often referred to as marls in the literature, are scattered over much of the State. In southern Florida, freshwater carbonates are nearly ubiquitous in the Everglades. These sediments are buff colored to tan, unconsolidated to poorly consolidated, fossiliferous carbonate muds. Sand, silt and clay may be present in limited quantities. These carbonates often contain organics. The dominant fossils in the freshwater carbonates are mollusks. (Source: USGS Florida Geologic Map Data). The soils of this are characterized as Bibb-Kinston Series association. The Bibb Series consists of very deep, poorly drained, moderately permeable soils on flood plains of streams in the Southern Coastal Plain (133A) Major Land Resource Area. They formed in stratified loamy and sandy alluvium that are commonly and frequently flooded and water runs off the surface very slowly. Slopes range from 0 to 2 percent. Reaction ranges from extremely acid to strongly acid throughout. Content of mica flakes ranges from none to common. Content of rounded gravel typically ranges from 0 to 10 percent throughout, but may range to 50 percent in thin strata below a depth of 1 meter. Buried soil horizons, present in many pedons have the same range in color and texture as the surface horizon which has iron and organic matter concentrations in shades of brown and yellow ranging from none to common. Texture is sand, loamy sand, loamy fine sand, fine sandy loam, sandy loam, loam or silt loam. The Kinston Series consists of very deep, poorly drained, moderately permeable soils found on flood plains. They were formed in alluvial depositions. Slopes range from 0 to 2 percent. Soil reaction ranges from strongly acid to very strongly acid. Typical texture across the pedons is loamy, gravelly loam, sandy loam, and clay loam with dark concretions often present. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). | Wild material | | 2169928 | NA 88591 |
| 39 | NA 88592 | 2024RM-005 | Ilex sp. | Florida, United States | NA | | | 2024 | COLLECTED | 11/21/2024 | Along the west/north side of the Yellow River about 1.1 kilometers upstream from the State Highway 87 boat ramp. This site was accessed by boat. | 30.57956000, -86.91916400 | 1 | Plants are found growing primarily in permanently saturated to submersed conditions along the edge of the Yellow River in part shade. The riverine habitat is comprised of a wide array of deciduous and evergreen trees, shrubs, and perennial plant species. Most of the plants along the river are adapted to acidic conditions and, while the aquatic habitat is generally fresh water, there is occasionally tidal or hurricane-caused saltwater intrusions. Slope: 0 percent. Aspect: North. The underlying geology of this area is characterized as Alluvium from undifferentiated Quaternary Sediments. Much of Florida's surface is covered by a varying thickness of undifferentiated sediments consisting of siliciclastics, organics and freshwater carbonates. Where these sediments exceed 20 feet (6.1 meters) thick, they were mapped as discrete units. To subdivide the undifferentiated sediments, those sediments occurring in flood plains were mapped as alluvial and flood plain deposits (Qal). Sediments showing surficial expression of beach ridges and dunes were mapped separately (Qbd) as were the sediments composing Trail Ridge (Qtr). Terrace sands were not mapped (refer to Healy [1975] for a discussion of the terraces in Florida). The subdivisions of the Undifferentiated Quaternary Sediments (Qu) are not lithostratigraphic units but are utilized to facilitate a better understanding of the State's geology. The siliciclastics are light gray, tan, brown to black, unconsolidated to poorly consolidated, clean to clayey, silty, unfossiliferous, variably organic-bearing sands to blue green to olive green, poorly to moderately consolidated, sandy, silty clays. Gravel is occasionally present in the panhandle. Organics occur as plant debris, roots, disseminated organic matrix and beds of peat. Freshwater carbonates, often referred to as marls in the literature, are scattered over much of the State. In southern Florida, freshwater carbonates are nearly ubiquitous in the Everglades. These sediments are buff colored to tan, unconsolidated to poorly consolidated, fossiliferous carbonate muds. Sand, silt and clay may be present in limited quantities. These carbonates often contain organics. The dominant fossils in the freshwater carbonates are mollusks. (Source: USGS Florida Geologic Map Data). The soils of this are characterized as Bibb-Kinston Series association. The Bibb Series consists of very deep, poorly drained, moderately permeable soils on flood plains of streams in the Southern Coastal Plain (133A) Major Land Resource Area. They formed in stratified loamy and sandy alluvium that are commonly and frequently flooded and water runs off the surface very slowly. Slopes range from 0 to 2 percent. Reaction ranges from extremely acid to strongly acid throughout. Content of mica flakes ranges from none to common. Content of rounded gravel typically ranges from 0 to 10 percent throughout, but may range to 50 percent in thin strata below a depth of 1 meter. Buried soil horizons, present in many pedons have the same range in color and texture as the surface horizon which has iron and organic matter concentrations in shades of brown and yellow ranging from none to common. Texture is sand, loamy sand, loamy fine sand, fine sandy loam, sandy loam, loam or silt loam. The Kinston Series consists of very deep, poorly drained, moderately permeable soils found on flood plains. They were formed in alluvial depositions. Slopes range from 0 to 2 percent. Soil reaction ranges from strongly acid to very strongly acid. Typical texture across the pedons is loamy, gravelly loam, sandy loam, and clay loam with dark concretions often present. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). | Wild material | | 2169929 | NA 88592 |
| 40 | Ames 36284 | Oak Creek Canyon | Alnus oblongifolia Torr. | Arizona, United States | NC7 |  | | 2024 | COLLECTED | 10/18/2024 | Oak Creek Canyon, approximately five miles north-northeast of Sedona in the Coconino National Forest, T18N R6E Sec. 8 and Sec. 21 and also T19N R6E Sec. 22 and Sec. 27. | 35.01694800, -111.73755900 | 1538 | Creek beds in canyon bottom. | Wild material | Plants sampled in nature had dark green, glossy leaves. Young bark is smooth and light grey, becoming dark and scaly with age. Approximately 50 feet in height. | 2169812 | Ames 36284 |
| 41 | NA 89078 | 2024RJLPA-004 | Staphylea trifolia L. | Pennsylvania, United States | NA | | | 2024 | COLLECTED | 09/20/2024 | Along gated road about 0.33 kilometers southwest of the Lake Ontelaunee Trail parking lot. | 40.49850800, -75.89121300 | 94 | Plants are growing on well-drained steep slopes in shade to part shade of a deciduous forest. Slope: 35 to 50 percent. Aspect: East-southeast. Geology: The underlying geology of this area is of Ordovician origin and characterized as Shale and graywacke of Hamburg sequence. It is characterized by shale containing zones of conspicuous graywacke. (Source: USGS Pennsylvania Geologic Map Data). Soils: The primary soil type in the area of this collection is classified as Berks-Weikert Complex, 25 to 60% slopes (BkF). Dominantly sloping to very steep, moderately deep and shallow, well drained soils underlain by acid shale bedrock. (Source: UPenn State University Soil Info Website). EPA Ecoregion (Level III): Ridge and Valley (67). EPA Ecoregion (Level IV): Northern Shale Valleys (67b). | Wild material | | 2169042 | NA 89078 |
| 42 | NA 89081 | 2024RJLPA-009 | Rosa carolina L. | Pennsylvania, United States | NA | | | 2024 | COLLECTED | 09/22/2024 | Lancaster and York Counties: outcrops along the Susquehanna River, accessed from the Historic Lock 12 parking lot off of Pennsylvania Road 372. | 39.81483500, -76.32762200 | 34 | Plants are growing from part-sun to full sun in crevices of the outcrops and where organic debris has accumulated in between boulders along the Susquehanna River. The sites range from nearly xeric to dry mesic, at least on the surface. Plants are generally growing 4-10 m above the normal flow of the river; however, the Holtwood Dam is less than 1 kilometer upstream and debris found trapped in the boulders indicates that there is periodic flooding, at least, in the lower zone of 4+ meters or so above normal river flow. This habitat has a diverse assemblage of deciduous trees and shrubs as well as abundant herbaceous taxa. Slope: 0 to 60 percent. Aspect: Northeast (generally). Geology: The underlying geology of this area is probably of lower Paleozoic age and characterized as the Octoraro Formation. It includes albite-chlorite schist, phyllite, some hornblende gneiss, and granitized members. Soils: The area where this species occurs is right on the edge of two soil zones that transition from the river’s edge to mesic conditions upslope. The first is generally referred to as Rock Outcrop. This terrestrial matrix in which plants grow is largely exposed underlying rock geology with accumulated outwash, rock decomposition, and organic debris buildup. The second is Mt. Airy (80%) and Manor (20%) Series soils, 25 to 60 percent slopes, extremely stony (MRF). (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). EPA Ecoregion (Level III): Northern Piedmont (64). EPA Ecoregion (Level IV): Piedmont Uplands (64c). | Wild material | | 2169045 | NA 89081 |
| 43 | NA 89082 | 2024RJLPA-010 | Amorpha fruticosa L. | Pennsylvania, United States | NA | | | 2024 | COLLECTED | 09/22/2024 | Outcrops along the Susquehanna River, accessed from the Historic Lock 12 parking lot off of Pennsylvania Road 372. | 39.81481500, -76.32757900 | 34 | Plants are growing from part-sun to full sun in crevices of the outcrops and where organic debris has accumulated in between boulders along the Susquehanna River. The sites range from nearly xeric to dry mesic, at least on the surface. Plants are generally growing 4-10 m above the normal flow of the river; however, the Holtwood Dam is less than 1 kilometer upstream and debris found trapped in the boulders indicates that there is periodic flooding, at least, in the lower zone of 4+ meters or so above normal river flow. This habitat has a diverse assemblage of deciduous trees and shrubs as well as abundant herbaceous taxa. Slope: 0 to 25 percent. Aspect: Northeast (generally). Geology: The underlying geology of this area is probably of lower Paleozoic age and characterized as the Octoraro Formation. It includes albite-chlorite schist, phyllite, some hornblende gneiss, and granitized members. Soils: The area where this species occurs is right on the edge of two soil zones that transition from the river’s edge to mesic conditions upslope. The first is generally referred to as Rock Outcrop. This terrestrial matrix in which plants grow is largely exposed underlying rock geology with accumulated outwash, rock decomposition, and organic debris buildup. The second is Mt. Airy (80%) and Manor (20%) Series soils, 25 to 60 percent slopes, extremely stony (MRF). (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). EPA Ecoregion (Level III): Northern Piedmont (64). EPA Ecoregion (Level IV): Piedmont Uplands (64c). | Wild material | | 2169046 | NA 89082 |
| 44 | NA 89083 | 2024RJLPA-012 | Rhododendron periclymenoides (Michx.) Shinners | Pennsylvania, United States | NA | | | 2024 | COLLECTED | 09/22/2024 | Outcrops along the Susquehanna River, accessed from the Historic Lock 12 parking lot off of Pennsylvania Road 372. | 39.81477400, -76.32807300 | 35 | Plants are growing from shade to part-sun and occasionally full sun in crevices of the outcrops and where organic debris has accumulated in between boulders along the Susquehanna River. The sites range from nearly xeric to mesic, at least on the surface. Plants are generally growing 4-10 m above the normal flow of the river; however, the Holtwood Dam is less than 1 kilometer upstream and debris found trapped in the boulders indicates that there is periodic flooding, at least, in the lower zone of 4+ meters or so above normal river flow. This habitat has a diverse assemblage of deciduous trees and shrubs as well as abundant herbaceous taxa. Slope: 0 to 60 percent. Aspect: Northeast (generally). Geology: The underlying geology of this area is probably of lower Paleozoic age and characterized as the Octoraro Formation. It includes albite-chlorite schist, phyllite, some hornblende gneiss, and granitized members. Soils: The area where this species occurs is right on the edge of two soil zones that transition from the river’s edge to mesic conditions upslope. The first is generally referred to as Rock Outcrop. This terrestrial matrix in which plants grow is largely exposed underlying rock geology with accumulated outwash, rock decomposition, and organic debris buildup. The second is Mt. Airy (80%) and Manor (20%) Series soils, 25 to 60 percent slopes, extremely stony (MRF). (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). EPA Ecoregion (Level III): Northern Piedmont (64). EPA Ecoregion (Level IV): Piedmont Uplands (64c). | Wild material | | 2169047 | NA 89083 |
| 45 | NA 89084 | 2024RJLPA-013 | Physocarpus opulifolius (L.) Maxim. | Pennsylvania, United States | NA | | | 2024 | COLLECTED | 09/22/2024 | Outcrops along the Susquehanna River, accessed from the Historic Lock 12 parking lot off of Pennsylvania Road 372. | 39.81466300, -76.32833900 | 36 | Plants are growing from shade to part-sun where organic debris has accumulated in between boulders as well as further upslope in deeper mesic soils along the Susquehanna River. This habitat has a diverse assemblage of deciduous trees and shrubs as well as abundant herbaceous taxa. Slope: 10 to 25 percent. Aspect: Northeast (generally). Geology: The underlying geology of this area is probably of lower Paleozoic age and characterized as the Octoraro Formation. It includes albite-chlorite schist, phyllite, some hornblende gneiss, and granitized members. Soils: The area where this species occurs is right on the edge of two soil zones that transition from the river’s edge to mesic conditions upslope. The first is generally referred to as Rock Outcrop. This terrestrial matrix in which plants grow is largely exposed underlying rock geology with accumulated outwash, rock decomposition, and organic debris buildup. The second is Mt. Airy (80%) and Manor (20%) Series soils, 25 to 60 percent slopes, extremely stony (MRF). (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). EPA Ecoregion (Level III): Northern Piedmont (64). EPA Ecoregion (Level IV): Piedmont Uplands (64c). | Wild material | | 2169048 | NA 89084 |
| 46 | NA 89085 | 2024RJLPA-014 | Rhododendron arborescens (Pursh) Torr. | Pennsylvania, United States | NA | | | 2024 | COLLECTED | 09/22/2024 | Outcrops along the Susquehanna River, accessed from the Historic Lock 12 parking lot off of Pennsylvania Road 372. | 39.81618100, -76.33069800 | 38 | Plants are growing from shade to part-sun and occasionally full sun in crevices of the outcrops and where organic debris has accumulated in between boulders along the Susquehanna River. The sites range from nearly xeric to mesic, at least on the surface. Plants are generally growing 4-10 m above the normal flow of the river; however, the Holtwood Dam is less than 1 kilometer upstream and debris found trapped in the boulders indicates that there is periodic flooding, at least, in the lower zone of 4+ meters or so above normal river flow. This habitat has a diverse assemblage of deciduous trees and shrubs as well as abundant herbaceous taxa. Slope: 0 to 75 percent. Aspect: Northeast (generally). Geology: The underlying geology of this area is probably of lower Paleozoic age and characterized as the Octoraro Formation. It includes albite-chlorite schist, phyllite, some hornblende gneiss, and granitized members. Soils: The area where this species occurs is right on the edge of two soil zones that transition from the river’s edge to mesic conditions upslope. The first is generally referred to as Rock Outcrop. This terrestrial matrix in which plants grow is largely exposed underlying rock geology with accumulated outwash, rock decomposition, and organic debris buildup. The second is Mt. Airy (80%) and Manor (20%) Series soils, 25 to 60 percent slopes, extremely stony (MRF). (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). EPA Ecoregion (Level III): Northern Piedmont (64). EPA Ecoregion (Level IV): Piedmont Uplands (64c). | Wild material | | 2169049 | NA 89085 |
| 47 | NA 89086 | 2024RJLPA-015 | Ilex verticillata (L.) A. Gray | Pennsylvania, United States | NA | | | 2024 | COLLECTED | 09/22/2024 | Outcrops along the Susquehanna River, accessed from the Historic Lock 12 parking lot off of Pennsylvania Road 372. | 39.81656600, -76.33136600 | 38 | Plants are growing from part-sun to full sun in crevices of the outcrops and where organic debris has accumulated in between boulders along the Susquehanna River. The sites range from nearly xeric to dry mesic, at least on the surface. Plants are generally growing 4-10 m above the normal flow of the river; however, the Holtwood Dam is less than 1 kilometer upstream and debris found trapped in the boulders indicates that there is periodic flooding, at least, in the lower zone of 4+ meters or so above normal river flow. This habitat has a diverse assemblage of deciduous trees and shrubs as well as abundant herbaceous taxa. Slope: 0 to 10 percent. Aspect: Northeast (generally). Geology: The underlying geology of this area is probably of lower Paleozoic age and characterized as the Octoraro Formation. It includes albite-chlorite schist, phyllite, some hornblende gneiss, and granitized members. Soils: The area where this species occurs is right on the edge of two soil zones that transition from the river’s edge to mesic conditions upslope. The first is generally referred to as Rock Outcrop. This terrestrial matrix in which plants grow is largely exposed underlying rock geology with accumulated outwash, rock decomposition, and organic debris buildup. The second is Mt. Airy (80%) and Manor (20%) Series soils, 25 to 60 percent slopes, extremely stony (MRF). (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). EPA Ecoregion (Level III): Northern Piedmont (64). EPA Ecoregion (Level IV): Piedmont Uplands (64c). | Wild material | | 2169050 | NA 89086 |
| 48 | NA 89087 | 2024RJLPA-016 | Hydrangea arborescens L. | Pennsylvania, United States | NA | | | 2024 | COLLECTED | 09/22/2024 | Outcrops along the Susquehanna River, accessed from the Historic Lock 12 parking lot off of Pennsylvania Road 372. | 39.81489000, -76.32912200 | 43 | Plants are growing in deep shade of the deciduous woodlands on outcrops and the steep slopes where organic debris and detritus has accumulated. This habitat has a diverse assemblage of deciduous trees and shrubs as well as abundant herbaceous taxa. Slope: 30 to 90 percent. Aspect: Northeast (generally). Geology: The underlying geology of this area is probably of lower Paleozoic age and characterized as the Octoraro Formation. It includes albite-chlorite schist, phyllite, some hornblende gneiss, and granitized members. (Source: Source: USGS Pennsylvania Geologic Map Data). Soils: The area where this species occurs is right on the edge of two soil zones that transition from the river’s edge to mesic conditions upslope. The first is generally referred to as Rock Outcrop. This terrestrial matrix in which plants grow is largely exposed underlying rock geology with accumulated outwash, rock decomposition, and organic debris buildup. The second is Mt. Airy (80%) and Manor (20%) Series soils, 25 to 60 percent slopes, extremely stony (MRF). (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). EPA Ecoregion (Level III): Northern Piedmont (64). EPA Ecoregion (Level IV): Piedmont Uplands (64c). | Wild material | | 2169051 | NA 89087 |
| 49 | NA 89089 | 2024RM-TK-002 | Viburnum acerifolium L. | Alabama, United States | NA | | | 2024 | COLLECTED | 09/19/2024 | Woodland slopes around and below the hilltop parking area leading down to the Silver Creek Lake Campground off of Silver Creek Lake Road. | 31.66612294, -87.57569860 | 49 | Plants are growing in shade of upland dry mesic, mature mixed deciduous and evergreen woodland. Generally, the overstory is thinner and there is less leaf litter cover, making the surface soil conditions drier. Slope: 5 to 10 percent. Aspect: Southeast. Geology: The underlying geology of this area is Claiborne Group, Tallahatta Formation, of Eocene origin, with white to very light-greenish-gray thin-bedded to massive siliceous claystone; interbedded with thin layers of fossiliferous clay, sandy clay, and glauconitic sand and sandstone. (Source: USGS Alabama Geologic Map Data). Soils: The primary soil types in the collection area are classified as Arundel-Cantuche Complex soils (15 to 35 percent slopes). The Arundel Series consists of moderately deep, well drained, very slowly permeable soils on dissected uplands of the Southern Coastal Plain. They formed in marine deposits consisting of acid clays underlain by horizontally bedded sandstone, buhrstone and siltstone. These soils are strongly acid. Slopes range from 2 to 60 percent. The Cantuche Series consists of shallow, well drained, moderately permeable soils that formed over horizontally bedded claystone. These soils are on narrow ridgetops and narrow benches on steep side-slopes of dissected landscapes in the Coastal Plain. They are strongly acid. Slopes range from 2 to 35 percent. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). EPA Ecoregion (Level III): Southeastern Plains (65). EPA Ecoregion (Level IV): Buhrstone/Lime Hills (65q). | Wild material | | 2169053 | NA 89089 |
| 50 | NA 89090 | 2024RM-TK-003 | Ilex longipes Chapm. ex Trel. | Alabama, United States | NA | | | 2024 | COLLECTED | 09/19/2024 | Woodland slopes around and below the hilltop parking area leading down to the Silver Creek Lake Campground off of Silver Creek Lake Road. | 31.66612294, -87.57569860 | 39 | Plants are growing in part-shade to shade of a moist mesic deciduous and evergreen woodland on dry, well-drained soil to an area 1-2 meters above a small seasonally spring-fed creek at 31.664428°, -87.574614°. Slope: 5 to 10 percent. Aspect: Southeast. Geology: The underlying geology of this area is Claiborne Group, Tallahatta Formation, of Eocene origin, with white to very light-greenish-gray thin-bedded to massive siliceous claystone; interbedded with thin layers of fossiliferous clay, sandy clay, and glauconitic sand and sandstone. (Source: USGS Alabama Geologic Map Data). Soils: The primary soil types in the collection area are classified as Arundel-Cantuche Complex soils (15 to 35 percent slopes). The Arundel Series consists of moderately deep, well drained, very slowly permeable soils on dissected uplands of the Southern Coastal Plain. They formed in marine deposits consisting of acid clays underlain by horizontally bedded sandstone, buhrstone and siltstone. These soils are strongly acid. Slopes range from 2 to 60 percent. The Cantuche Series consists of shallow, well drained, moderately permeable soils that formed over horizontally bedded claystone. These soils are on narrow ridgetops and narrow benches on steep side-slopes of dissected landscapes in the Coastal Plain. They are strongly acid. Slopes range from 2 to 35 percent. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). EPA Ecoregion (Level III): Southeastern Plains (65). EPA Ecoregion (Level IV): Buhrstone/Lime Hills (65q). | Wild material | | 2169054 | NA 89090 |
| 51 | NA 89091 | 2024RM-TK-004 | Prunus sp. | Florida, United States | NA | | | 2024 | COLLECTED | 09/05/2024 | Blackwater River Wildlife Management Area: on the south side of Boundary Line Road about 0.32 kilometers west of Deaton Bridge Road along an area edged by a barbed wire fence. | 30.68579800, -86.87964300 | 45 | Plants are growing from part-sun to full sun. Plants are growing in an area that is frequently burned with a lot of [Prunus sp. (orig. listed as Prunus alabamensis)] scattered throughout. This habitat is a longleaf pine-wiregrass community with scattered turkey (Quercus laevis) and blackjack oaks (Quercus incana). There is a slight slope downward. The line of [Prunus sp.] goes along a semi-ditch on the side of a dirt road. The plants probably get a bit more water than the plants out in the open forest. The [Prunus sp.] are most often without any other close woody companions. Slope: 0 percent. Aspect: North. Geology: The underlying geology of this area is probably of lower Pliocene age and characterized as the Citronelle Formation. The Citronelle Formation is widespread in the Gulf Coastal Plain. The type section for the Citronelle Formation, named by Matson (1916), is near Citronelle, Alabama. The Citronelle Formation grades laterally, through a broad facies transition, into the Miccosukee Formation of the eastern Florida panhandle. Coe (1979) investigated the Citronelle Formation in portions of the western Florida panhandle. The Citronelle Formation is a siliciclastic, deltaic deposit that is lithologically similar to, and time equivalent with, the Cypresshead Formation and, at least in part, the Long Key Formation (Cunningham et al., 1998) of the peninsula. In the western panhandle, some of the sediments mapped as Citronelle Formation may be reworked Citronelle. The lithologies are the same and there are few fossils present to document a possible younger age. The Citronelle Formation consists of gray to orange, often mottled, unconsolidated to poorly consolidated, very fine to very coarse, poorly sorted, clean to clayey sands. It contains significant amounts of clay, silt and gravel which may occur as beds and lenses and may vary considerably over short distances. Limonite nodules and limonite-cemented beds are common. Marine fossils are rare but fossil pollen, plant remains and occasional vertebrates are found. Much of the Citronelle Formation is highly permeable. It forms the Sand and Gravel Aquifer of the surficial aquifer system. (Source: USGS Florida Geologic Map Data). Soils: The soil of this area is characterized as Lakeland Series Sand, 0 to 5 percent slopes (21). The Lakeland Series consists of very deep, excessively drained, rapid to very rapidly permeable soils on uplands. They formed in thick beds of eolian or marine and/or fluvio-marine sands in the Southern Coastal Plain MLRA (133A), the Carolina and Georgia Sandhills (MLRA 137), the Eastern Gulf Coast Flatwoods (MLRA 152A) and the Atlantic Coast Flatwoods (MLRA 153A). (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). EPA Ecoregion (Level III): Southeastern Plains (65). EPA Ecoregion (Level IV): Southern Pine Plains and Hills (65f). | Wild material | Received as Prunus alabamensis; other collections of this material have proven not to be Prunus serotina var. alabamensis, but actually a species of plum; this will likewise be treated as unidentified material until its species can be ascertained. Collectors' notes refer to the plant by the name under which it was collected. | 2169055 | NA 89091 |
| 52 | NA 89093 | 2024RM-TK-006 | Ilex ambigua Torr. | Florida, United States | NA | | | 2024 | COLLECTED | 09/29/2024 | Blackwater River Wildlife Management Area: growing on the south side of Bud Bass Road, approximately 0.3 kilometers east of Training Center R./Norma Riley Rd. | 30.75759720, -86.80187220 | 29 | This plant is growing in part-shade under mesic conditions along the edge of a longleaf pine plantation. Slope: 0 percent. Aspect: North. Geology: The underlying geology of this area is probably of lower Pliocene age and characterized as the Citronelle Formation. The Citronelle Formation is widespread in the Gulf Coastal Plain. The type section for the Citronelle Formation, named by Matson (1916), is near Citronelle, Alabama. The Citronelle Formation grades laterally, through a broad facies transition, into the Miccosukee Formation of the eastern Florida panhandle. Coe (1979) investigated the Citronelle Formation in portions of the western Florida panhandle. The Citronelle Formation is a siliciclastic, deltaic deposit that is lithologically similar to, and time equivalent with, the Cypresshead Formation and, at least in part, the Long Key Formation (Cunningham et al., 1998) of the peninsula. In the western panhandle, some of the sediments mapped as Citronelle Formation may be reworked Citronelle. The lithologies are the same and there are few fossils present to document a possible younger age. The Citronelle Formation consists of gray to orange, often mottled, unconsolidated to poorly consolidated, very fine to very coarse, poorly sorted, clean to clayey sands. It contains significant amounts of clay, silt and gravel which may occur as beds and lenses and may vary considerably over short distances. Limonite nodules and limonite-cemented beds are common. Marine fossils are rare but fossil pollen, plant remains and occasional vertebrates are found. Much of the Citronelle Formation is highly permeable. It forms the Sand and Gravel Aquifer of the surficial aquifer system. (Source: USGS Florida Geologic Map Data). Soils: The soil of this area is characterized as Lakeland Series Sand, 0 to 5 percent slopes (21). The Lakeland Series consists of very deep, excessively drained, rapid to very rapidly permeable soils on uplands. They formed in thick beds of eolian or marine and/or fluvio-marine sands in the Southern Coastal Plain MLRA (133A), the Carolina and Georgia Sandhills (MLRA 137), the Eastern Gulf Coast Flatwoods (MLRA 152A) and the Atlantic Coast Flatwoods (MLRA 153A). (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). EPA Ecoregion (Level III): Southeastern Plains (65). EPA Ecoregion (Level IV): Southern Pine Plains and Hills (65f). | Wild material | | 2169057 | NA 89093 |
| 53 | OPGC 8855 | JDC/RM/2024/019/1141 | Rudbeckia missouriensis Engelm. ex C. L. Boynton & Beadle | Missouri, United States | OPGC |  | | 2024 | COLLECTED | 09/28/2024 | Danville Glade Conservation Area located 3.60 miles south, southeast of Danville, T47N R5W SW 1/4 SW 1/4 Sec. 5. | 38.86583400, -91.50779400 | 222 | Remnant glade. | Wild material | | 2169019 | OPGC 8855 |
| 54 | NA 87823 | FL24-01 | Ilex cassine L. | Florida, United States | NA | | | 2024 | COLLECTED | 09/05/2024 | Matanzas State Forest. | 29.72143991, -81.28386478 | | Boggy blackwater ditches along edge of dirt road. EPA Ecoregion III: Southern Coastal Plain (75). EPA Ecoregion IV: Eastern Florida Flatwoods (75d). Geology: Beach Ridge and Dune. Soil: Immokalee Series Fine Sand. | Wild material | | 2168973 | NA 87823 |
| 55 | W6 61540 RE | CA190B-214 | Calochortus luteus Douglas ex Lindl. | California, United States | W6 |  | | 2024 | | | | | | | Wild material | Petal deep yellow Inflorescence umbel like perianth bell shaped nectary not depressed (Recollection of CA190B-109, W6 60820) | 2167989 | W6 61540 RE |
| 56 | W6 61577 | CA360-209 | Clarkia purpurea (Curtis) A. Nelson & J. F. Macbr. | California, United States | W6 |  | | 2024 | | | | | | | Wild material | | 2168025 | W6 61577 |
| 57 | WLP 3492 | St. Francois State Park | Hydrangea arborescens L. | Missouri, United States | NA |  | | 2024 | COLLECTED | 01/19/2024 | St. Francois State Park, 8920 US Highway 67 North, approximately 3.2 miles north-northeast of Bonne Terre. | 37.96381000, -90.53403000 | 202 | Rocky outcrops above Big River and rocky areas on bank of Big River. | Wild material | | 2166135 | WLP 3492 |
| 58 | NA 88853 | TJK2023FL-048 | Lyonia ferruginea (Walter) Nutt. | Florida, United States | NA | | | 2024 | COLLECTED | 12/26/2023 | South of Highway 98, west of Twine Road. Track has a very large powerline right-of-way to the east, and George Washington Swamp bottom to the west. | 29.77560000, -85.27400000 | 6 | Longleaf Pine-Saw Palmetto. This area appears to be declining in quality, as witnessed by the declining in Rhododendron stem/plant density. Possible contributing issues: lacking necessary fire regime, has not seen fire in 8-10 years, encroaching woody shrub layer, accumulating organic matter (pine needle), expanding tree canopy, Hurricane Michael. Slope: less than 2%. Aspect: Northeast. Elevation: 20 feet. | Wild material | | 2165708 | NA 88853 |
| 59 | NA 88829 | RJL-RM2023FLAL-003 | Oxydendrum arboreum (L.) DC. | Florida, United States | NA | | | 2023 | COLLECTED | 12/05/2023 | Yellow River Wildlife Management Area, along DOF [Department of Forestry] Y15 dirt road 0.06 kilometers north of Fisher Old Mill Road. | 30.62728600, -86.83824600 | 7 | Growing 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 material | | 2165659 | NA 88829 |
| 60 | NA 88834 | RJL-RM2023FLAL-008 | Rhododendron canescens (Michx.) Sweet | Florida, United States | NA | | | 2023 | COLLECTED | 12/06/2023 | Blackwater 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, -86.95784700 | 53 | Growing 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 material | | 2165664 | NA 88834 |
| 61 | NA 88835 | RJL-RM2023FLAL-009 | Rhododendron viscosum (L.) Torr. | Florida, United States | NA | | | 2023 | COLLECTED | 12/06/2023 | Blackwater 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, -86.96283300 | 43 | Growing 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 material | | 2165665 | NA 88835 |
| 62 | NA 88840 | RJL-RM2023FLAL-014 | Rhododendron viscosum (L.) Torr. | Florida, United States | NA | | | 2023 | COLLECTED | 12/11/2023 | Property of Floyd Griffith off View Drive on the southwest side of McCormick Lake. | 30.63247000, -85.33718200 | 56 | Plants 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 material | | 2165670 | NA 88840 |
| 63 | NA 88843 | RJL-RM2023FLAL-017 | Rhododendron austrinum (Small) Rehder | Florida, United States | NA | | | 2023 | COLLECTED | 12/11/2023 | Holmes Creek at Live Oak Landing: plants found on the low bluff along the south side of Holmes Creek accessed by foot from a parking lot on Live Oak Landing Road that dead ends into the creek. | 30.59043500, -85.83899800 | 7 | Plants are growing in part shade to shade on the top and slope of the low bluff overlooking Holmes Creek in a mixed deciduous and evergreen forest. The dry mesic habitat has relatively low competition and is quite acidic. Slope: 0 to 45 percent. Aspect: Northwest. The underlying geology of this area is classified as Alluvium, of Pleistocene/Holocene origin and consists of undifferentiated Quaternary sediments of varying thickness including siliciclastics, organics and freshwater carbonates. The siliciclastics are light gray, tan, brown to black, unconsolidated to poorly consolidated, clean to clayey, silty, unfossiliferous, variably organic-bearing sands to blue green to olive green, poorly to moderately consolidated, sandy, silty clays. Organics occur as plant debris, roots, disseminated organic matrix and beds of peat. Freshwater carbonates, often referred to as marls in the literature, are scattered. (Source: USGS Florida Geologic Map Data.) The surface soil profile of this area is primarily Nankin-Cowarts-Lakeland Complex. 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 Cowarts Series consists of very deep, moderately well and well drained soils on ridge tops and side slopes on uplands of the Coastal Plain Major Land Resource Area. They formed in loamy marine sediments. Slopes range from 1 to 60 percent. The Lakeland series consists of very deep, excessively drained, rapid to very rapidly permeable soils on uplands. They formed in thick beds of eolian or marine and/or fluvio-marine sands. 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 material | | 2165673 | NA 88843 |
| 64 | NA 88844 | RJL-RM2023FLAL-018 | Clethra alnifolia L. | Florida, United States | NA | | | 2023 | COLLECTED | 12/13/2023 | Yellow 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, -86.62005400 | 27 | Plants 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 material | | 2165674 | NA 88844 |
| 65 | NA 88850 | RJL-RM2023FLAL-024 | Rhododendron austrinum (Small) Rehder | Florida, United States | NA | | | 2023 | COLLECTED | 12/13/2023 | Yellow River Water Management Area, found in an area where an unnamed unpaved road winds along the edges of the Yellow River. This unpaved road is accessed from Old River Road to the east near the junction with Shockley Springs Road. Individuals are found along the roadside for at least 6 kilometers from the point where the unnamed road splits and turns south. | 30.82647700, -86.60892000 | 23 | Plants are growing primarily in part shade to shade in mesic conditions in a mixed evergreen and deciduous forest. Fruiting plants are more abundant where plants receive more sunlight. Slope: 0 to 2 percent. Aspect: Various. The underlying geology of this area is the Alum Bluff Group of Miocene origin. It includes the Chipola Formation, Oak Grove Sand, Shoal River Formation, Choctawhatchee Formation and the Jackson Bluff Formation. The formations included in this group are generally defined on the basis of their molluscan faunas and stratigraphic position. Puri (1953) described sediment facies as they relate to the formations of the Alum Bluff Group. These sediments are lithologically distinct as a group, not as individual units. The Alum Bluff Group crops out or is beneath a thin overburden in the western panhandle from river valleys in Okaloosa County eastward to western Jackson County. The Alum Bluff Group consists of clays, sands and shell beds which may vary from fossiliferous, sandy clays to unfossiliferous sands and clays and occasional carbonate beds. Mica is a common constituent and glauconite and phosphate occur sporadically. Induration varies from essentially nonindurated in sands to well indurated in carbonate lenses. Colors range from cream to olive gray with mottled reddish brown in weathered sections. Sand grain size varies from very fine to very coarse with sporadic occurrences of gravel. These sediments generally have low permeabilities and are part of the intermediate confining unit/aquifer system. (Source: USGS Florida Geologic Map Data.) The surface soil profile of this area is primarily Yemassee, Garcon, and Bigbee soils that are occasionally flooded. The Yemassee Series consists of very deep, somewhat poorly drained, moderately permeable, loamy soils that formed in marine sediments. These soils are on terraces and broad flats of the lower Coastal Plain and very strongly acid. Slopes range from 0 to 2 percent. The Garcon Series consists of very deep, somewhat poorly drained, moderately permeable soils on terraces and in the broad flats of the lower Coastal Plain. They formed in sandy and loamy marine sediments. This soil ranges from very strongly acid to extremely acid. The Bigbee series consists of very deep, excessively drained, rapidly permeable soils that are on natural levees and higher positions in flood plains along stream flood plains in the Southern Coastal Plain (MLRA 133A) and the Eastern Gulf Coast Flatwoods (MLRA 152A). They formed in thick sandy alluvial sediments. They range from strongly acid to very strongly acid. (Source: NRCS Web Soil Survey.) | Wild material | | 2165680 | NA 88850 |
| 66 | NA 88820 | TJK2023AL-005 | Hydrangea arborescens L. | Alabama, United States | NA | | | 2023 | COLLECTED | 12/07/2023 | Between Monroe County Route 1 and Tom Hayles Road. | 31.40575900, -87.54924000 | 22 | In woodlands on limestone outcrop. While the upper area of slopes is covered by a thin soil layer, the exposed limestone rock outcrop on the northwestern edge of this area is a low competition niche for plants like the Hydrangea to gain a foothold. Slope: 60% (plus). Aspect: Northwest. Elevation: 72 feet. | Wild material | | 2165649 | NA 88820 |
| 67 | NA 88821 | TJK2023AL-006 | Hydrangea quercifolia W. Bartram | Alabama, United States | NA | | | 2023 | COLLECTED | 12/07/2023 | Between Monroe County Route 1 and Tom Hayles Road. | 31.40580000, -87.54890000 | 22 | In woodlands on limestone outcrop. While the upper area of slopes is covered by a thin soil layer, the exposed limestone rock outcrop on the northwestern edge of this area is a low competition niche for plants like the Hydrangea to gain a foothold. Slope: 60% (plus). Aspect: Northwest. Elevation: 72 feet. | Wild material | | 2165650 | NA 88821 |
| 68 | NA 88689 | RJL2023NJ-002 | Kalmia latifolia L. | New Jersey, United States | NA | | | 2023 | COLLECTED | 11/10/2023 | Franklin Township: Piney Hollow Preservation Area (the site is owned by Franklin Township). Plants accessed by foot along trails throughout property. | 39.57400900, -74.93602400 | 32 | Plants 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 material | | 2159117 | NA 88689 |
| 69 | NA 88692 | RJL2023NJ-005 | Ilex opaca Aiton | New Jersey, United States | NA | | | 2023 | COLLECTED | 11/10/2023 | Franklin Township: Piney Hollow Preservation Area (the site is owned by Franklin Township). This species was found on as well as below the dam at the far end of McCarthys Lakes. Plants accessed by foot along trails throughout property. | 39.57423200, -74.92525600 | 29 | Plants growing in part-shade to sun of the moist to saturated areas below the McCarthys Lakes dam in the wetlands associated with the New Squankum Branch. Plants were also found growing on the slopes of the dam in well-drained mesic to dry-mesic conditions. This species is clearly adaptable to a variety of conditions. Slope: 0 to 15 percent. Aspect: East. Elevation: 28 to 30 meters. NOTE: In addition to the soil type described below, this species was also growing on the slopes of a constructed earthen dam of unknown soil origin. The underlying geology of this area is of Middle Miocene, Serravallian origin and characterized as an Cohansey Formation. It is comprised of sand, white to yellow with local gravel and clay. Locally stained red or orange brown by iron oxides and (or) cemented into large blocks of ironstone. Unweathered clay is typically dark gray, but commonly weathers white where interbedded with thin beds of ironstone. Unit is a complex of interfingering marine and nonmarine facies. Sand is typically medium grained and moderately sorted although it ranges from fine to very coarse grained and from poorly to well sorted. Sand consists of quartz and siliceous rock fragments. Some beds are locally micaceous. In general, the sand is crossbedded, although the style of crossbedding varies significantly with the paleoenvironment. Trough crossbedding predominates, especially in the nonmarine channel fill deposits, and the scale of the crossbeds varies from small to large. Maximum thickness in the map area is about 60 m; however, thickness is difficult to determine because of the irregular basal contact and extensive post-depositional erosion. There is as much as 18 m of relief along the basal contact. The basal contact is sharp, undulatory, and directly overlain by a thin gravel bed. The Cohansey Formation unconformably overlies the Kirkwood Formation and is found in channels cut down into the Kirkwood. Where the Kirkwood consists of sandy, light-colored sediments, the basal contact of the Cohansey is drawn below crossbedded sediments. Where the Kirkwood consists of dark-colored silty beds, the basal contact is drawn between light-colored Cohansey sediments and the underlying dark-colored sediments. The Cohansey was markedly thinned because of erosion prior to deposition of overlying units in the western and southern parts of the southern sheet. The unit has been extensively eroded and stripped from large areas of the New Jersey Coastal Plain, particularly in the central sheet where outliers are common. In spite of its widespread nature, the Cohansey is poorly exposed because of its loose sandy composition, which causes it to erode easily. (Source: USGS New Jersey Geologic Map Data.) The primary soil type in the collection area is classified as Manahawkin Series muck, 0 to 2 percent slopes, frequently flooded, Northern Coastal Plain. Manahawkin Series soils are very deep, very poorly drained soils that are sandy or sandy-skeletal, siliceous, dysic, mesic Terric Haplosaprists high in organic deposits that are found in lake basins, back swamps, floodplains, and freshwater channels. The soils are classified in the dysic reaction class because pH in water dominantly ranges from 4.5 to 5.0. The zone from the soil surface to a depth of 200 cm is continuously saturated (endosaturation). The upper strata of Manahawkin Series from 0 to 76 cm is black broken face and rubbed muck; 10 percent fibers, less than 2 percent rubbed; moderate medium granular structure; mat of many fine roots; identifiable material is primarily herbaceous with a trace of woody fragments; 85-95 percent organic matter; extremely acid. Lower strata to 200 cm are gray sand, single grained and loose; strongly acid. (Source: NRCS Web Soil Survey.) | Wild material | | 2159120 | NA 88692 |
| 70 | NA 88693 | RJL2023NJ-006 | Clethra alnifolia L. | New Jersey, United States | NA | | | 2023 | COLLECTED | 11/10/2023 | Franklin Township: Piney Hollow Preservation Area (the site is owned by Franklin Township). Plants accessed by foot along trails throughout property. | 39.57319800, -74.92908900 | 29 | Plants 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 material | | 2159121 | NA 88693 |
| 71 | NA 88694 | RJL2023NJ-007 | Spiraea tomentosa L. | New Jersey, United States | NA | | | 2023 | COLLECTED | 11/10/2023 | Franklin Township: Piney Hollow Preservation Area (the site is owned by Franklin Township). Plants accessed by foot along trails throughout property. | 39.57318200, -74.92673700 | 28 | Plants growing in part-shade to sun along the edges of McCarthys Lakes in moist-mesic to wet areas dominated by herbaceous plants. Slope: N/A. Aspect: N/A. | Wild material | | 2159122 | NA 88694 |
| 72 | NA 88695 | RJL2023NJ-008 | Aronia arbutifolia (L.) Pers. | New Jersey, United States | NA | | | 2023 | COLLECTED | 11/10/2023 | Franklin Township: Piney Hollow Preservation Area (the site is owned by Franklin Township). Plants accessed by foot along trails throughout property. | 39.57262400, -74.92606900 | 28 | Plants growing in part-shade to sun along the edges of McCarthys Lakes and in the understory of a mixed deciduous and evergreen forest in moist-mesic to wet conditions. Slope: N/A. Aspect: N/A. | Wild material | | 2159123 | NA 88695 |
| 73 | NA 88697 | RJL2023NCSC-002 | Ilex amelanchier M. A. Curtis ex Chapm. | North Carolina, United States | NA | | | 2023 | COLLECTED | 11/12/2023 | Goose Pond Bay (Nature Conservancy-owned site): wetlands on the south side of McNeil Road approximately 0.64 kilometers west of junction with McIntosh Road. | 34.88254100, -79.09915700 | 60 | Plants are growing in part-shade to sun of a Carolina Bay habitat with seasonally moist to wet, acidic conditions. Slope: N/A. Aspect: N/A. The underlying geology of this area is of Cretaceous origin and characterized as Black Creek Formation. The formation is comprised of clay that is gray to black and lignitic. It contains thin beds and laminae of fine-grained micaceous sand and thick lenses of cross-bedded sand. This formation has glauconitic, fossiliferous clayey sand lenses in the upper part. (Source: USGS North Carolina Geologic Map Data.) The primary soil type in the collection area is classified as McColl loam soil. The McColl Series consists of poorly drained, slowly permeable soils that are shallow or moderately deep to a fragipan and very deep to bedrock. They formed in loamy sediments in oval depressions on the Coastal Plain. The soils are nearly level or concave. Runoff is frequently ponded. Slopes are less than 2 percent. These soils are strongly acid. (Source: NRCS Web Soil Survey.) | Wild material | | 2159125 | NA 88697 |
| 74 | NA 88710 | RJL2023NCSC-015 | Cephalanthus occidentalis L. | South Carolina, United States | NA | | | 2023 | COLLECTED | 11/14/2023 | Francis Marion National Forest: plants growing in wetlands/swamps on US Forest Service Road 223 approximately 0.57 kilometers southeast from the junction with Halfway Creek Road. | 33.06771000, -79.67769700 | 20 | Plants are growing in part-shade to sun along the edges of the swamp in seasonally inundated acidic wetland habitat. Slope: N/A. Aspect: N/A. The underlying geology of this area is of Pleistocene origin and characterized as an Socastee Formation. This is a low coastal formation in the Carolinas like Penholoway but younger and lower in altitude. It is comprised primarily of unconsolidated, fine-detrital clay. It is described as variegated quartzose sands, argillaceous sands, and clays, 5 m thick at the type section near Socastee Swamp. (Source: USGS South Carolina Geologic Map Data.) The primary soil type in this collection area is classified as Rutlege Series loamy fine sand. Rutlege Series soils are very deep, very poorly drained soils that are sandy, siliceous, thermic Typic Humaquepts. Upper strata soils (0-38 cm) are black loamy sand with weak medium granular structure. They are loose and very strongly acid. Lower strata (38-175 cm) range from dark gray to dark brown sand that is single grained, loose, and very strongly acid. (Source: NRCS Web Soil Survey.) | Wild material | | 2159138 | NA 88710 |
| 75 | NA 88711 | RJL2023NCSC-016 | Ilex myrtifolia Walter | South Carolina, United States | NA | | | 2023 | COLLECTED | 11/14/2023 | Francis Marion National Forest: plants growing in wetlands/swamps on US Forest Service Road 223 approximately 0.57 kilometers southeast from the junction with Halfway Creek Road. | 33.06786200, -79.67761800 | 11 | Plants are growing in shade to part-shade in the swamp in seasonally inundated acidic wetland habitat. Slope: N/A. Aspect: N/A. The underlying geology of this area is of Pleistocene origin and characterized as an Socastee Formation. This is a low coastal formation in the Carolinas like Penholoway but younger and lower in altitude. It is comprised primarily of unconsolidated, fine-detrital clay. It is described as variegated quartzose sands, argillaceous sands, and clays, 5 m thick at the type section near Socastee Swamp. (Source: USGS South Carolina Geologic Map Data.) The primary soil type in this collection area is classified as Rutlege Series loamy fine sand. Rutlege Series soils are very deep, very poorly drained soils that are sandy, siliceous, thermic Typic Humaquepts. Upper strata soils (0-38 cm) are black loamy sand with weak medium granular structure. They are loose and very strongly acid. Lower strata (38-175 cm) range from dark gray to dark brown sand that is single grained, loose, and very strongly acid. (Source: NRCS Web Soil Survey.) | Wild material | | 2159139 | NA 88711 |
| 76 | NA 88712 | RJL2023NCSC-017 | Itea virginica L. | South Carolina, United States | NA | | | 2023 | COLLECTED | 11/14/2023 | Francis Marion National Forest: plants growing in wetlands/swamps on US Forest Service Road 223 approximately 0.57 kilometers southeast from the junction with Halfway Creek Road. | 33.06755600, -79.67789100 | 11 | Plants are growing in the understory of the acidic swamp that is seasonally inundated in shade. Slope: N/A. Aspect: N/A. The underlying geology of this area is of Pleistocene origin and characterized as an Socastee Formation. This is a low coastal formation in the Carolinas like Penholoway but younger and lower in altitude. It is comprised primarily of unconsolidated, fine-detrital clay. It is described as variegated quartzose sands, argillaceous sands, and clays, 5 m thick at the type section near Socastee Swamp. (Source: USGS South Carolina Geologic Map Data.) The primary soil type in this collection area is classified as Rutlege Series loamy fine sand. Rutlege Series soils are very deep, very poorly drained soils that are sandy, siliceous, thermic Typic Humaquepts. Upper strata soils (0-38 cm) are black loamy sand with weak medium granular structure. They are loose and very strongly acid. Lower strata (38-175 cm) range from dark gray to dark brown sand that is single grained, loose, and very strongly acid. (Source: NRCS Web Soil Survey.) | Wild material | | 2159140 | NA 88712 |
| 77 | NA 88713 | RJL2023NCSC-018 | Ilex opaca Aiton | South Carolina, United States | NA | | | 2023 | COLLECTED | 11/14/2023 | Francis Marion National Forest: plants growing in wetlands/swamps on US Forest Service Road 223 approximately 0.57 kilometers southeast from the junction with Halfway Creek Road. | 33.06783000, -79.67749100 | 11 | Plants are growing in part shade to shade of a swamp in seasonally inundated acidic wetland habitat. Slope: N/A. Aspect: N/A. The underlying geology of this area is of Pleistocene origin and characterized as an Socastee Formation. This is a low coastal formation in the Carolinas like Penholoway but younger and lower in altitude. It is comprised primarily of unconsolidated, fine-detrital clay. It is described as variegated quartzose sands, argillaceous sands, and clays, 5 m thick at the type section near Socastee Swamp. (Source: USGS South Carolina Geologic Map Data.) The primary soil type in this collection area is classified as Rutlege Series loamy fine sand. Rutlege Series soils are very deep, very poorly drained soils that are sandy, siliceous, thermic Typic Humaquepts. Upper strata soils (0-38 cm) are black loamy sand with weak medium granular structure. They are loose and very strongly acid. Lower strata (38-175 cm) range from dark gray to dark brown sand that is single grained, loose, and very strongly acid. (Source: NRCS Web Soil Survey.) | Wild material | | 2159141 | NA 88713 |
| 78 | NA 88714 | RJL2023NCSC-019 | Smilax walteri Pursh | South Carolina, United States | NA | | | 2023 | COLLECTED | 11/14/2023 | Francis Marion National Forest: plants growing in wetlands/swamps on US Forest Service Road 223 approximately 0.57 kilometers southeast from the junction with Halfway Creek Road. | 33.06757700, -79.67792800 | 11 | Plants are growing in shade, part-shade and sun in the acid soils of a swamp and along the edges of the swamp where the soils are seasonally inundated. Slope: N/A. Aspect: N/A. The underlying geology of this area is of Pleistocene origin and characterized as a Socastee Formation. This is a low coastal formation in the Carolinas like Penholoway but younger and lower in altitude. It is comprised primarily of unconsolidated, fine-detrital clay. It is described as variegated quartzose sands, argillaceous sands, and clays, 5 m thick at the type section near Socastee Swamp. (Source: USGS South Carolina Geologic Map Data.) The primary soil type in this collection area is classified as Rutlege Series loamy fine sand. Rutlege Series soils are very deep, very poorly drained soils that are sandy, siliceous, thermic Typic Humaquepts. Upper strata soils (0-38 cm) are black loamy sand with weak medium granular structure. They are loose and very strongly acid. Lower strata (38-175 cm) range from dark gray to dark brown sand that is single grained, loose, and very strongly acid. (Source: NRCS Web Soil Survey.) | Wild material | | 2159142 | NA 88714 |
| 79 | NA 88719 | RJL2023NCSC-024 | Ilex laevigata (Pursh) A. Gray | South Carolina, United States | NA | | | 2023 | COLLECTED | 11/15/2023 | Little Pee Dee Heritage Preserve/Wildlife Management Area (South Carolina Department of Natural Resources Public Lands, on South Carolina Highway 917). | 34.14123300, -79.19532100 | 13 | Plants growing in high understory shade to part-shade of a moist to relatively dry pine forest with occasional deciduous trees. The litter layer in the woodlands is very deep with longleaf pine needles, while the edges of the woodlands are much drier with exposed white sand and little to no litter layer. Slope: N/A. Aspect: N/A. The underlying geology of this area is of Pleistocene origin and characterized as Waccamaw Formation. This formation is another Carolina coastalized terrace that is deeply weathered. It is characterized by unconsolidated, coarse-detrital, soft sand limestones and loose gray to buff fine quartz sands in which occasional small quartz pebbles are present. It also includes sedimentary, carbonate, soft limestones. (Source: USGS South Carolina Geologic Map Data.) The primary soil type in this collection area is classified as Lynn Haven Series sand. The Lynn Haven Series consists of very deep, poorly and very poorly drained, moderate or moderately rapid, permeable soils in low areas and depressions in Atlantic Flatwoods and the Gulf. They formed in thick deposits of sandy marine sediments. Th Lynn Haven Series soil is approximately 2 m thick and ranges from black near the surface to yellow brown in the deepest strata. Most of the strata are comprised of fine sands that are friable with the deepest strata also including a small percentage of organic matter. Reaction ranges from extremely acid to strongly acid throughout the profile. The water table is at 0-15 cm for periods of 2 to 6 months annually and within a depth 1 m for more than 6 months during most years; during extended dry periods it is below 1 meter. Depressional areas are ponded for long duration in most years. (Source: NRCS Web Soil Survey.) | Wild material | | 2159147 | NA 88719 |
| 80 | NA 88720 | RJL2023NCSC-025 | Zenobia pulverulenta (W. Bartram ex Willd.) Pollard | South Carolina, United States | NA | | | 2023 | COLLECTED | 11/15/2023 | Little Pee Dee Heritage Preserve/Wildlife Management Area (South Carolina Department of Natural Resources Public Lands, on South Carolina Highway 917). | 34.13990000, -79.19691700 | 14 | Plants growing in high understory shade to part-shade of a moist to relatively dry pine forest with occasional deciduous trees. The litter layer in the woodlands is very deep with longleaf pine needles, while the edges of the woodland are much drier with exposed white sand and little to no litter layer. Slope: N/A. Aspect: N/A. The underlying geology of this area is of Pleistocene origin and characterized as Waccamaw Formation. This formation is another Carolina coastalized terrace that is deeply weathered. It is characterized by unconsolidated, coarse-detrital, soft sand limestones and loose gray to buff fine quartz sands in which occasional small quartz pebbles are present. It also includes sedimentary, carbonate, soft limestones. (Source: USGS South Carolina Geologic Map Data.) The primary soil type in this collection area is classified as Lynn Haven Series sand. The Lynn Haven Series consists of very deep, poorly and very poorly drained, moderate or moderately rapid, permeable soils in low areas and depressions in Atlantic Flatwoods and the Gulf. They formed in thick deposits of sandy marine sediments. Th Lynn Haven Series soil is approximately 2 m thick and ranges from black near the surface to yellow brown in the deepest strata. Most of the strata are comprised of fine sands that are friable with the deepest strata also including a small percentage of organic matter. Reaction ranges from extremely acid to strongly acid throughout the profile. The water table is at 0-15 cm for periods of 2 to 6 months annually and within a depth 1 m for more than 6 months during most years; during extended dry periods it is below 1 meter. Depressional areas are ponded for long duration in most years. (Source: NRCS Web Soil Survey.) | Wild material | | 2159148 | NA 88720 |
| 81 | NA 88721 | RJL2023NCSC-026 | Ilex opaca Aiton | South Carolina, United States | NA | | | 2023 | COLLECTED | 11/15/2023 | Little Pee Dee Heritage Preserve/Wildlife Management Area (South Carolina Department of Natural Resources Public Lands, on South Carolina Highway 917). | 34.14091500, -79.19555200 | 13 | Plants growing in high understory shade to part-shade of a moist to relatively dry pine forest with occasional deciduous trees. The litter layer in the woodlands is very deep with longleaf pine needles, while the edges of the woodlands are much drier with exposed white sand and little to no litter layer. Slope: N/A. Aspect: N/A. The underlying geology of this area is of Pleistocene origin and characterized as Waccamaw Formation. This formation is another Carolina coastalized terrace that is deeply weathered. It is characterized by unconsolidated, coarse-detrital, soft sand limestones and loose gray to buff fine quartz sands in which occasional small quartz pebbles are present. It also includes sedimentary, carbonate, soft limestones. (Source: USGS South Carolina Geologic Map Data.) The primary soil type in this collection area is classified as Lynn Haven Series sand. The Lynn Haven Series consists of very deep, poorly and very poorly drained, moderate or moderately rapid, permeable soils in low areas and depressions in Atlantic Flatwoods and the Gulf. They formed in thick deposits of sandy marine sediments. Th Lynn Haven Series soil is approximately 2 m thick and ranges from black near the surface to yellow brown in the deepest strata. Most of the strata are comprised of fine sands that are friable with the deepest strata also including a small percentage of organic matter. Reaction ranges from extremely acid to strongly acid throughout the profile. The water table is at 0-15 cm for periods of 2 to 6 months annually and within a depth 1 m for more than 6 months during most years; during extended dry periods it is below 1 meter. Depressional areas are ponded for long duration in most years. (Source: NRCS Web Soil Survey.) | Wild material | | 2159149 | NA 88721 |
| 82 | NA 88684 | TJK2023FL-031 | Smilax smallii Morong | Florida, United States | NA | | | 2023 | COLLECTED | 11/18/2023 | T. Kiphart residence, Navarre, Florida. | 30.40680000, -86.93090000 | 12 | Moist, urban woods. Slope: 3%. Aspect: South. Elevation: 39 feet. | Wild material | | 2159096 | NA 88684 |
| 83 | NA 88687 | TJK2023FL-034 | Clethra alnifolia L. | Florida, United States | NA | | | 2023 | COLLECTED | 11/18/2023 | Navarre, Florida: Adams St. cul-de-sac, on nine-acre private property. Infrastructure development began and was terminated due to the lack of any engineering or environmental site planning (designated wetland status). It has remained idle for a number of years. | 30.41000000, -86.92890000 | 11 | Wet Pine Flatwood transitioning to a shrub bog habitat under fire suppression. Slope: less than 2%. Aspect: North. Elevation: 36 feet. | Wild material | | 2159099 | NA 88687 |
| 84 | NA 88671 | RJL2023PA-005 | Rhododendron maximum L. | Pennsylvania, United States | NA | | | 2023 | COLLECTED | 10/16/2023 | Appalachian National Scenic Trail: Pulpit Rock and Pinnacle Loop. Rocky woodlands along Furnace Creek as well as steep rocky slopes above Pulpit Rock Reservoir associated with the Pulpit Rock and Pinnacle Loop Trail. | 40.59226100, -75.94588800 | 301 | Well-drained and very rocky dry deciduous woodlands in part shade to full shade. Slope: 0-30%. Aspect: variable. The underlying geology of this area is of Silurian origin and characterized as the Shawangunk Formation. It is characterized by light- to dark-gray, fine- to very coarse-grained sandstone and conglomerate containing thin shale interbeds. Includes four members, in descending order: Tammany--conglomerate and sandstone; Lizard Creek--sandstone and red or green shale; Minsi--sandstone and conglomerate; Weiders--conglomerate. Tammany and Lizard Creek Members together are approximately equivalent to Clinton Group to the west; Minsi and Weiders Members together are equivalent to Tuscarora Formation to the west. (Source: USGS Pennsylvania Geologic Map Data). The primary soil type in the collection area is classified as Hazleton Series. The Hazleton series consists of deep and very deep, well drained soils formed in residuum of acid gray, brown or red sandstone on uplands. Slope ranges from 0 to 80 percent. Permeability is moderately rapid to rapid. Solum thickness ranges from 60 to 120 centimeters. Depth to lithic contact ranges from 1 to 2 meters. Rock fragments of angular sandstone, dominantly less than 25 cm in size, range from 5 to 70 percent in individual horizons. Boulders, stones, flags and channers cover about 5 to 60 percent of the surface of some pedons. Reaction ranges from strongly acid through extremely acid throughout. (Source: NRCS Web Soil Survey). | Wild material | | 2159062 | NA 88671 |
| 85 | NA 88672 | RJL2023PA-006 | Rhododendron periclymenoides (Michx.) Shinners | Pennsylvania, United States | NA | | | 2023 | COLLECTED | 10/16/2023 | Appalachian National Scenic Trail: Pulpit Rock and Pinnacle Loop. Rocky woodland edges above Furnace Creek around Pulpit Rock and Pinnacle Loop Trail. | 40.58668200, -75.94269600 | 247 | Well-drained and very rocky dry deciduous woodlands in part shade to full shade. Slope: 10%. Aspect: East. The underlying geology of this area is of Silurian origin and characterized as the Shawangunk Formation. It is characterized by light- to dark-gray, fine- to very coarse-grained sandstone and conglomerate containing thin shale interbeds. Includes four members, in descending order: Tammany--conglomerate and sandstone; Lizard Creek--sandstone and red or green shale; Minsi--sandstone and conglomerate; Weiders--conglomerate. Tammany and Lizard Creek Members together are approximately equivalent to Clinton Group to the west; Minsi and Weiders Members together are equivalent to Tuscarora Formation to the west. (Source: USGS Pennsylvania Geologic Map Data). The primary soil type in the collection area is classified as Hazleton Series. The Hazleton series consists of deep and very deep, well drained soils formed in residuum of acid gray, brown or red sandstone on uplands. Slope ranges from 0 to 80 percent. Permeability is moderately rapid to rapid. Solum thickness ranges from 60 to 120 centimeters. Depth to lithic contact ranges from 1 to 2 meters. Rock fragments of angular sandstone, dominantly less than 25 cm in size, range from 5 to 70 percent in individual horizons. Boulders, stones, flags and channers cover about 5 to 60 percent of the surface of some pedons. Reaction ranges from strongly acid through extremely acid throughout. (Source: NRCS Web Soil Survey). | Wild material | | 2159063 | NA 88672 |
| 86 | NA 88673 | RJL2023PA-007 | Rhododendron pilosum (Michx.) Craven | Pennsylvania, United States | NA | | | 2023 | COLLECTED | 10/25/2023 | Ned Smith Center for Art and Nature. | 40.53367300, -76.92715700 | 147 | Well-drained and very rocky, dry slopes above 10-50 meters above Wiconisco Creek in mixed deciduous and evergreen woodlands in part shade to full shade. Slope: 10-40%. Aspect: North. The underlying geology of this area is of Mississippian origin and characterized as the Pocono Formation. It is comprised of light-gray to buff or light-olive-gray, medium-grained, crossbedded sandstone and minor siltstone; commonly conglomeratic at base and in middle; medial conglomerate, where present, is used to divide into Mount Carbon and Beckville Members; equivalent to Burgoon Sandstone of Allegheny Plateau. (Source: USGS Pennsylvania Geologic Map Data). The primary soil type in the collection area is classified as Laidig Series. The Laidig series consists of very deep, well drained soils formed in colluvium from sandstone, siltstone, and some shale. They are gently sloping to very steep soils on benches and foot slopes. Permeability is moderate or moderately rapid above the fragipan and moderately slow or slow in the fragipan. Slope ranges from 0 to 55 percent. Solum thickness ranges from 1.25 to 2.0 meters or more. Depth to the fragipan ranges from 0.75 to 1.25 meters. The particle-size control section averages less than 35 percent rock fragments. Rock fragments range from 5 to 50 percent in individual subhorizons of the A, E, BE, BA and Bt horizons; 15 to 70 percent in individual subhorizons of the Btx horizon; and 20 to 70 percent in the C horizon. Rock fragments are mostly sandstone but include siltstone and shale. Rock fragments include channers, cobbles, flagstones, and stones. Soils range from extremely acid through strongly acid throughout. (Source: NRCS Web Soil Survey). | Wild material | | 2159064 | NA 88673 |
| 87 | NA 88674 | RJL2023PA-008 | Kalmia latifolia L. | Pennsylvania, United States | NA | | | 2023 | COLLECTED | 10/25/2023 | Ned Smith Center for Art and Nature. | 40.53463500, -76.92616300 | 130 | Well-drained and very rocky, dry slopes above 10-50 meters above Wiconisco Creek in mixed deciduous and evergreen woodlands in part shade to full shade. Slope: 10-40%. Aspect: North. The underlying geology of this area is of Mississippian origin and characterized as the Pocono Formation. It is comprised of light-gray to buff or light-olive-gray, medium-grained, crossbedded sandstone and minor siltstone; commonly conglomeratic at base and in middle; medial conglomerate, where present, is used to divide into Mount Carbon and Beckville Members; equivalent to Burgoon Sandstone of Allegheny Plateau. (Source: USGS Pennsylvania Geologic Map Data). The primary soil type in the collection area is classified as Laidig Series. The Laidig series consists of very deep, well drained soils formed in colluvium from sandstone, siltstone, and some shale. They are gently sloping to very steep soils on benches and foot slopes. Permeability is moderate or moderately rapid above the fragipan and moderately slow or slow in the fragipan. Slope ranges from 0 to 55 percent. Solum thickness ranges from 1.25 to 2.0 meters or more. Depth to the fragipan ranges from 0.75 to 1.25 meters. The particle-size control section averages less than 35 percent rock fragments. Rock fragments range from 5 to 50 percent in individual subhorizons of the A, E, BE, BA and Bt horizons; 15 to 70 percent in individual subhorizons of the Btx horizon; and 20 to 70 percent in the C horizon. Rock fragments are mostly sandstone but include siltstone and shale. Rock fragments include channers, cobbles, flagstones, and stones. Soils range from extremely acid through strongly acid throughout. (Source: NRCS Web Soil Survey). | Wild material | | 2159065 | NA 88674 |
| 88 | NA 88675 | RJL2023PA-009 | Viburnum acerifolium L. | Pennsylvania, United States | NA | | | 2023 | COLLECTED | 10/25/2023 | Ned Smith Center for Art and Nature. | 40.53539200, -76.92313500 | 136 | Well-drained and very rocky dry deciduous woodlands in part shade to full shade. Slope: 10-30%. Aspect: North. The underlying geology of this area is of Mississippian origin and characterized as the Pocono Formation. It is comprised of light-gray to buff or light-olive-gray, medium-grained, crossbedded sandstone and minor siltstone; commonly conglomeratic at base and in middle; medial conglomerate, where present, is used to divide into Mount Carbon and Beckville Members; equivalent to Burgoon Sandstone of Allegheny Plateau. (Source: USGS Pennsylvania Geologic Map Data). The primary soil type in the collection area is classified as Laidig Series. The Laidig series consists of very deep, well drained soils formed in colluvium from sandstone, siltstone, and some shale. They are gently sloping to very steep soils on benches and foot slopes. Permeability is moderate or moderately rapid above the fragipan and moderately slow or slow in the fragipan. Slope ranges from 0 to 55 percent. Solum thickness ranges from 1.25 to 2.0 meters or more. Depth to the fragipan ranges from 0.75 to 1.25 meters. The particle-size control section averages less than 35 percent rock fragments. Rock fragments range from 5 to 50 percent in individual subhorizons of the A, E, BE, BA and Bt horizons; 15 to 70 percent in individual subhorizons of the Btx horizon; and 20 to 70 percent in the C horizon. Rock fragments are mostly sandstone but include siltstone and shale. Rock fragments include channers, cobbles, flagstones, and stones. Soils range from extremely acid through strongly acid throughout. (Source: NRCS Web Soil Survey). | Wild material | | 2159066 | NA 88675 |
| 89 | NA 88676 | RJL2023PA-010 | Staphylea trifolia L. | Pennsylvania, United States | NA | | | 2023 | COLLECTED | 10/25/2023 | Seed collected along the Appalachian National Scenic Trail, accessed from the Duncannon Entrance. | 40.38132600, -77.02965700 | 103 | Well-drained and very rocky deciduous woodlands where soil has accumulated in part shade to full shade. Slope: 0-30%. Aspect: variable. The underlying geology of this area is of Devonian origin and characterized as the Duncannon Member of Catskill Formation. It is characterized by grayish-red sandstone, siltstone, and mudstone in fining-upward cycles; conglomerate occurs at base of some cycles. The sandstones which comprise the Duncannon Member are fine to very coarse grained and grayish red to grayish red-purple in color. The Duncannon Member is known to be crossbedded to planar bedded in beds anywhere from 3 to 9 meters thick. Conglomerates have been spotted at the base of the Duncannon Member. The Duncannon Member is poorly exposed in most areas except along the Lehigh River. The conglomerate portion of this member has been known to form ridges and ledges with thicknesses approaching 228 meters. (Source: USGS Pennsylvania Geologic Map Data). The primary soil type in the collection area is classified as Hazleton Series. The Hazleton series consists of deep and very deep, well drained soils formed in residuum of acid gray, brown or red sandstone on uplands. Slope ranges from 0 to 80 percent. Permeability is moderately rapid to rapid. Solum thickness ranges from 60 to 120 centimeters. Depth to lithic contact ranges from 1 to 2 meters. Rock fragments of angular sandstone, dominantly less than 25 cm in size, range from 5 to 70 percent in individual horizons. Boulders, stones, flags and channers cover about 5 to 60 percent of the surface of some pedons. Reaction ranges from strongly acid through extremely acid throughout. (Source: NRCS Web Soil Survey). | Wild material | | 2159067 | NA 88676 |
| 90 | WLP 3280 | TJK2023FL-028 | Kalmia hirsuta Walter | Florida, United States | NA | | | 2023 | COLLECTED | 11/02/2023 | Navarre, Florida: Adams St. cul-de-sac, on nine-acre private property. Infrastructure development began and was terminated due to the lack of any engineering or environmental site planning (designated wetland status). It has remained idle for a number of years. | 30.41080000, -86.92840000 | 11 | Wet Pine Flatwood transitioning to a shrub bog habitat under fire suppression. Slope: flat. Aspect: East Elevation: 36 feet. | Wild material | | 2159060 | WLP 3280 |
| 91 | NA 89013 | TJK2023FL-021 | Smilax pumila Walter | Florida, United States | NA | | | 2023 | COLLECTED | 10/15/2023 | Collected at 1985 Reagan Rd in Navarre, Florida. | 30.40680000, -86.93090000 | 9 | Disturbed native residential woods. Elevation: 32 feet. Slope: 3%. Aspect: Southeast. | Wild material | | 2158906 | NA 89013 |
| 92 | NA 88667 | RJL2023PA-004 | Viburnum acerifolium L. | Pennsylvania, United States | NA | | | 2023 | | | | | | | Wild material | | 2158816 | NA 88667 |
| 93 | NA 88664 | RJL2023PA-001 | Viburnum acerifolium L. | Pennsylvania, United States | NA | | | 2023 | COLLECTED | 10/01/2023 | Seed collected from plants growing along a two-mile stretch of Harmonyville Road on the woodland edge next to the road. [Note: latitude and longitude were collected at the location of the largest seed collection.] | 40.18482200, -75.78145100 | 158 | Plants were growing in well-drained and rocky mesic-dry woodlands from part shade along the road edge to full shade in the understory of the woodlands. Slope: 2-10%. Aspect: Variable. The underlying geology of this area is of Triassic origin and characterized as the Stockton Formation. It is characterized by light-gray to buff, coarse-grained, arkosic sandstone; includes reddish-brown to grayish-purple sandstone, siltstone, and mudstone. (Source: USGS Pennsylvania Geologic Map Data.) The primary soil type in the area of this collection is classified as Edgemont Channery Sandy Loam Series (8 to 25 percent slopes), extremely stony. The Edgemont Series consists of deep and very deep, well drained soils formed in the weathered residuum of quartzitic rocks. They have moderately high to high saturated hydraulic conductivity. Slopes range from 0 to 70 percent. Solum thickness ranges from 50 to 10 cm. Depth to bedrock ranges from about 1.5 to 2.2 meters. Kaolinite is the dominant mineral in the clay fraction with detectable amounts of illite, vermiculite, montmorillonite, chlorite and interstratified clays. Gravel, channers, and stone size fragments of quartzite and quartz are present throughout the profile. Rock fragments range from 5 to 40 percent in the horizons of the solum and from 10 to 90 percent in the C horizon. Reaction ranges from extremely acid to strongly acid throughout. (Source: NRCS Web Soil Survey.) | Wild material | | 2158813 | NA 88664 |
| 94 | NA 88658 | TJK2023FL-012 | Ilex verticillata (L.) A. Gray | Florida, United States | NA | | | 2023 | COLLECTED | 09/10/2023 | Lower Yellow River. | 30.62868600, -86.80748000 | 3 | Beautiful riverine system. Elevation: 13 feet. Slope: 0 (none). Aspect: Northwest. | Wild material | | 2158792 | NA 88658 |
| 95 | NA 88659 | TJK2023FL-013 | Ilex sp. | Florida, United States | NA | | | 2023 | COLLECTED | 09/15/2023 | Lower Yellow River. | 30.58170000, -86.91770000 | 1 | Elevation: 3 feet. Slope: 0 percent. Aspect: North. | Wild material | | 2158793 | NA 88659 |
| 96 | NA 88660 | TJK2023FL-014 | Rhododendron austrinum (Small) Rehder | Florida, United States | NA | | | 2023 | COLLECTED | 09/15/2023 | Lower Yellow River, Grimes Lake. | 30.61930000, -86.81490000 | 3 | Elevation: 13 feet. Slope: 0 percent. Aspect: West-southwest. | Wild material | | 2158794 | NA 88660 |
| 97 | NA 88663 | TJK2023FL-017 | Rhododendron austrinum (Small) Rehder | Florida, United States | NA | | | 2023 | COLLECTED | 09/17/2023 | Lower Yellow River, below the Old Land Place. | 30.55513000, -86.94659000 | 0 | An area with very nice Pink R. austrinum. Elevation: 0. Slope: 0 percent. Aspect: South-southwest. | Wild material | | 2158797 | NA 88663 |
| 98 | WLP 3218 | TJK2023FL-011 | Stewartia malacodendron L. | Florida, United States | NA | | | 2023 | COLLECTED | 08/26/2023 | Weaver Creek Bayhead, Eglin Air Force Base. Common in scattered patches along both sides of Weaver Creek. | 30.51679000, -86.91493400 | 81 | Rich, loamy moist mesic slopes; mixed deciduous-evergreen woodlands. Elevation: 268 feet. Slope: 15%. Aspect: West. | Wild material | | 2158791 | WLP 3218 |
| 99 | Ames 36168 | Mount Magazine | Ptelea trifoliata L. | Arkansas, United States | NC7 |  | | 2023 | COLLECTED | 08/26/2023 | Mount Magazine State Park primarily localized to the northwest rim of the mountain along the trails heading west from Brown's Spring, T6N R25W Sec. 21. | 35.17130900, -93.65582200 | 786 | Top of sky-island mountain. Localized along the rims just above steep cliffs on north facing slopes. | Wild material | Plants in nature ranging from three to fifteen feet in height with peak bloom observed during the first week of May (2023). | 2158787 | Ames 36168 |
| 100 | NA 89233 | UK Arb. 2023-0059-A | Cladrastis kentukea (Dum. Cours.) Rudd | Kentucky, United States | NA | | | 2023 | COLLECTED | 08/22/2023 | Blue Sportsmen's League (land owner): trees growing on both sides of eroded dirt road from campground to Kentucky River. | 37.78777000, -84.65356000 | | Calcareous rocky woods, mid-slope. Slope: 20-30%. Aspect: Southwest. | Wild material | | 2158476 | NA 89233 |
| 101 | Ames 36159 | JDC/MM/2023/062/1094 | Monarda maxmedleyi J. J. N. Campb. & Floden | Kentucky, United States | NC7 |  | | 2023 | COLLECTED | 08/09/2023 | Daniel Boone National Forest on north and south sides along Zilpo Road with the highest abundance being across from intersection with Dogwood Lane. | 38.05551500, -83.53288600 | 354 | Edges of woods/roadsides. Localized to west and southeast facing slopes. | Wild material | Plants measuring 12-18" in height. Spreading vegetatively via rhizomes. Flower color varies within the population from white to pink. Peak flowering at collection site occurred near 27th of May (2023). | 2158364 | Ames 36159 |
| 102 | OPGC 8811 | CBG- 10775 | Penstemon pallidus Small | Illinois, United States | OPGC | | | 2023 | | | | | | | Wild material | | 2142242 | OPGC 8811 |
| 103 | NA 88598 | RJL2023FL-002a | Agarista populifolia (Lam.) Judd | Florida, United States | NA | | | 2023 | COLLECTED | 02/14/2023 | Plants 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, -81.47205400 | 10 | Plants 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 material | | 2141479 | NA 88598 |
| 104 | WLP 3084 | RM2023-002 | Rhododendron viscosum (L.) Torr. | Florida, United States | NA | | | 2023 | COLLECTED | 09/15/2022 | This 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, -86.94940000 | 38 | The 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 material | | 2141438 | WLP 3084 |
| 105 | WLP 3092 | RJLSEUS2022-021 | Rhododendron prunifolium (Small) Millais | Alabama, United States | NA | | | 2023 | COLLECTED | 12/10/2023 | Slopes along Poke Springs Branch inlet accessed by boat from Walter F. George Reservoir. Generally uncommon, but frequent at this site. | 31.72318400, -85.12907800 | 69 | Plants 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 material | | 2141446 | WLP 3092 |
| 106 | WLP 2795 | RJL2023NJ-001 | Rhododendron atlanticum (Ashe) Rehder | New Jersey, United States | NA | | | 2023 | COLLECTED | 01/16/2023 | Plants 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, -74.87482500 | 5 | Plants 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 material | | 2141140 | WLP 2795 |
| 107 | NA 87814 | RM-TK2022-003 | Nyssa ogeche W. Bartram ex Marshall | Florida, United States | NA | | | 2023 | COLLECTED | 09/06/2022 | Hightower Landing on Holmes Creek, off of Hightower Road. This location is off of Florida State Hwy. 79. | 30.60539000, -85.76513400 | 5 | Trees growing on the edge of the water along Holmes Creek.
Soils: The underlying geology of this area is classified as Alluvium of Pleistocene/Holocene origin and consists of undifferentiated Quaternary sediments of varying thickness including siliciclastics, organics and freshwater carbonates. The siliciclastics are light gray, tan, brown to black, unconsolidated to poorly consolidated, clean to clayey, silty, unfossiliferous, variably organic-bearing sands to blue green to olive green, poorly to moderately consolidated, sandy, silty clays. Organics occur as plant debris, roots, disseminated organic matrix and beds of peat. Freshwater carbonates, often referred to as marls in the literature, are scattered.
Source: USGS Florida Geologic Map Data (https://mrdata.usgs.gov/geology/state/state.php?state=fl)
The primary soil types in the collection area are classified as Rutlege, Pickney and Pamlico soils, frequently flooded. The Rutlege series comprises very deep, very poorly drained persistently wet soils on flats, depressions and floodplains where shallow ponding is common. They are of marine or fluvial sediment origin. Thickness of these loamy sandy soils is greater than 1.5 meters and a reaction from extremely acid to strongly acid. The Pickney Series consists of very deep, very poorly drained soils. Permeability is rapid. These nearly level soils have negligible runoff and were formed by marine or fluvial sediments in the lower coastal plain on flats, depressions, stream terraces, and flood plains. Slopes range from 0 to 2 percent. The soils of this series are loamy fine sand that is very friable and extremely acid in the upper 0-25 cm. The lower strata are similar, while the lower strata from 0.8-2 meters are comprised of fine sand. The Pamlico series consists of very poorly drained soils that formed in decomposed organic material underlain by dominantly sandy sediment. The soils are on nearly level flood plains, bays, and depressions of the Coastal Plain. Slopes are less than 1 percent. Pamlico soils have 0.4-1.3 meters of organic material over dominantly sandy sediments. Reaction is extremely in the organic layers and ranges from extremely acid to strongly acid in the underlying mineral layers.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2140796 | NA 87814 |
| 108 | NA 88525 | RM-TK2022-013 | Macranthera flammea (W. Bartram) Pennell | Florida, United States | NA | | | 2023 | COLLECTED | 11/04/2022 | Growing in wetland in Blackwater River State Forest. | 30.80870000, -86.96270000 | 42 | Plants are typically found growing in part shade to sun in saturated streamside wetland/seep areas at the base of the slope in sphagnum moss. This appears to be year-round wetland habitat.
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 material | | 2140806 | NA 88525 |
| 109 | NA 88549 | RJLSEUS2022-022 | Rhododendron minus Michx. var. minus | Georgia, United States | NA | | | 2023 | COLLECTED | 12/10/2022 | East side of Georgia State Hwy. 39, on the south side of Kolomoki Creek approximately 11 kilometers south of Fort Gaines, Georgia. Common on this site, but otherwise infrequent. This species is near the southernmost end of its natural range. | 31.52053400, -85.02351600 | 53 | Plants are growing in part-shade to shade of deciduous upland, dry, deciduous woodlands on steep slopes 10-15 meters above Kolomoki Creek.
Soils: The underlying geology of this area is of Paleocene origin and characterized as Tuscahoma Sand. As mapped this formation includes lower Eocene Bashi Marl Member of the Hatchetigbee Formation. This formation consists of light-gray to light-olive-gray laminated and thin-bedded carbonaceous silt and clay interbedded with fine sand; thin lignite beds occur locally. Lower part of the formation includes beds of fossiliferous, glauconitic fine quartz sand containing spheroidal sandstone concretions, gravel and clay pebbles.
Source: USGS Georgia Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=GANu%3B1)
The primary soil types in the collection area are classified as Ailey-Cowarts Complex Series soils (8 to 25 percent slopes). The Ailey Series consists of well drained or somewhat excessively drained soils formed by fluviomarine and marine deposits. These soils are found marine terraces and low hills of the upper coastal plain and sandhills; they are strongly acidic. The Cowarts Series consists of very deep, moderately well and well drained soils on ridge tops and side slopes on uplands of the Coastal Plain Major Land Resource Area. They formed in loamy marine sediments. Slopes range from 1 to 60 percent.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2140776 | NA 88549 |
| 110 | NA 88550 | RJLSEUS2022-023 | Kalmia latifolia L. | Georgia, United States | NA | | | 2023 | COLLECTED | 12/10/2022 | East side of Georgia State Hwy. 39, on the south side of Kolomoki Creek approximately 11 kilometers south of Fort Gaines, Georgia. Common on this site, but otherwise infrequent. This species is near the southernmost end of its natural range. | 31.52053400, -85.02351600 | 53 | Plants are growing in part-shade to shade of deciduous upland, dry, deciduous woodlands on steep slopes 10-15 meters above Kolomoki Creek.
Soils: The underlying geology of this area is of Paleocene origin and characterized as Tuscahoma Sand. As mapped this formation includes lower Eocene Bashi Marl Member of the Hatchetigbee Formation. This formation consists of light-gray to light-olive-gray laminated and thin-bedded carbonaceous silt and clay interbedded with fine sand; thin lignite beds occur locally. Lower part of the formation includes beds of fossiliferous, glauconitic fine quartz sand containing spheroidal sandstone concretions, gravel and clay pebbles.
Source: USGS Georgia Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=GANu%3B1)
The primary soil types in the collection area are classified as Ailey-Cowarts Complex Series soils (8 to 25 percent slopes). The Ailey Series consists of well drained or somewhat excessively drained soils formed by fluviomarine and marine deposits. These soils are found marine terraces and low hills of the upper coastal plain and sandhills; they are strongly acidic. The Cowarts Series consists of very deep, moderately well and well drained soils on ridge tops and side slopes on uplands of the Coastal Plain Major Land Resource Area. They formed in loamy marine sediments. Slopes range from 1 to 60 percent.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2140777 | NA 88550 |
| 111 | NA 88554 | RJLSEUS2022-027 | Rhododendron alabamense Rehder | Alabama, United States | NA | | | 2023 | COLLECTED | 12/12/2022 | Plants growing on woodland slopes around and below the hilltop parking area leading down to the Silver Creek Lake Campground off of Silver Creek Lake Road. Occasional in the upland woodlands. | 31.66613100, -87.57625700 | 49 | Plants are growing in shade of upland dry mesic mature mixed deciduous and evergreen woodland. Generally, the overstory is thinner and there is less leaf litter cover, making the surface soil conditions drier.
Soils: The underlying geology of this area is Claiborne Group, Tallahatta Formation, of Eocene origin, with white to very light-greenish-gray thin-bedded to massive siliceous claystone; interbedded with thin layers of fossiliferous clay, sandy clay, and glauconitic sand and sandstone.
Source: USGS Alabama Geological Map Data (https://mrdata.usgs.gov/geology/state/state.php?state=AL)
The primary soil types in the collection area are classified as Smithdale-Boykin Complex soils (2 to 5 percent slopes). The Smithdale Series consists of very deep, well drained, moderately permeable soils on ridge tops and hill slopes in dissected uplands of the Southern Coastal Plain and in the Western Coastal Plain. They formed in thick beds of loamy marine sediments and are strongly acid. Slopes range from 1 to 60 percent. The Boykin Series consists of deep, well drained, moderately permeable soils that formed in sandy and loamy coastal plain sediments of Pleistocene age. These soils are on gently sloping to moderately steep uplands. Slopes range from 1 to 20 percent.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2140781 | NA 88554 |
| 112 | NA 88555 | RJLSEUS2022-028 | Rhododendron canescens (Michx.) Sweet | Alabama, United States | NA | | | 2023 | COLLECTED | 12/12/2022 | Plants growing on woodland slopes below the hilltop parking area leading down to the Silver Creek Lake Campground off of Silver Creek Lake Road. Occasional in the woodlands. | 31.66549700, -87.57624500 | 45 | Plants are growing in shade of moist mesic deciduous and evergreen woodland, mid-slope between the upland dry mesic zone and the creekside habitat below.
Soils: The underlying geology of this area is Claiborne Group, Tallahatta Formation, of Eocene origin, with white to very light-greenish-gray thin-bedded to massive siliceous claystone; interbedded with thin layers of fossiliferous clay, sandy clay, and glauconitic sand and sandstone.
Source: USGS Alabama Geological Map Data (https://mrdata.usgs.gov/geology/state/state.php?state=AL)
The primary soil types in the collection area are classified as Luverne Sandy Loam soils (15 to 35 percent slopes). The Luverne Series consists of very deep, well drained, moderately slowly permeable soils on dissected uplands of the Southern Coastal Plain. They formed in stratified marine sediments and are strongly acid. The lower strata of this series are clay and clay loam. Slopes range from 1 to 45 percent.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2140782 | NA 88555 |
| 113 | NA 88556 | RJLSEUS2022-029 | Rhododendron colemanii R. F. Mill. | Alabama, United States | NA | | | 2023 | COLLECTED | 12/12/2022 | Plants growing on woodland slopes below the hilltop parking area leading down to the Silver Creek Lake Campground off of Silver Creek Lake Road. Occasional in the woodlands. | 31.66503300, -87.57468000 | 43 | Plants are growing in shade of moist mesic deciduous and evergreen woodland on rich slopes 1-3 meters above a small spring-fed creek.
Soils: The underlying geology of this area is Claiborne Group, Tallahatta Formation, of Eocene origin, with white to very light-greenish-gray thin-bedded to massive siliceous claystone; interbedded with thin layers of fossiliferous clay, sandy clay, and glauconitic sand and sandstone.
Source: USGS Alabama Geological Map Data (https://mrdata.usgs.gov/geology/state/state.php?state=AL)
The primary soil types in the collection area are classified as Smithdale-Boykin Complex soils (2 to 5 percent slopes). The Smithdale Series consists of very deep, well drained, moderately permeable soils on ridge tops and hill slopes in dissected uplands of the Southern Coastal Plain and in the Western Coastal Plain. They formed in thick beds of loamy marine sediments and are strongly acid. Slopes range from 1 to 60 percent. The Boykin Series consists of deep, well drained, moderately permeable soils that formed in sandy and loamy coastal plain sediments of Pleistocene age. These soils are on gently sloping to moderately steep uplands. Slopes range from 1 to 20 percent.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2140783 | NA 88556 |
| 114 | NA 88557 | RJLSEUS2022-030 | Ilex longipes Chapm. ex Trel. | Alabama, United States | NA | | | 2023 | COLLECTED | 12/12/2022 | Silver Creek Lake Campground off of Silver Creek Lake Road: woodland slopes below the hilltop parking lot leading down to the campground. | 31.66442800, -87.57461400 | 39 | Part shade of moist-mesic, mixed deciduous and evergreen woodland on dry, well-drained bank, 1-2 meters above a small spring-fed creek. The underlying geology of this area is Claiborne Group, Tallahatta Formation, of Eocene origin, with white to very light-greenish-gray thin-bedded to massive siliceous claystone; interbedded with thin layers of fossiliferous clay, sandy clay, and glauconitic sand and sandstone. (Source: USGS Alabama Geological Map Data). The primary soil types in the collection area are classified as Arundel-Cantuche Complex soils (15 to 35 percent slopes). The Arundel Series consists of moderately deep, well drained, very slowly permeable soils on dissected uplands of the Southern Coastal Plain. They formed in marine deposits consisting of acid clays underlain by horizontally bedded sandstone, buhrstone and siltstone. These soils are strongly acid. Slopes range from 2 to 60 percent. The Cantuche Series consists of shallow, well drained, moderately permeable soils that formed over horizontally bedded claystone. These soils are on narrow ridgetops and narrow benches on steep side-slopes of dissected landscapes in the Coastal Plain. They are strongly acid. Slopes range from 2 to 35 percent. (Source: NRCS Web Soil Survey). | Wild material | | 2140818 | NA 88557 |
| 115 | NA 88558 | RJLSEUS2022-031 | Ilex decidua Walter | Alabama, United States | NA | | | 2023 | COLLECTED | 12/12/2022 | Silver Creek Lake Campground off of Silver Creek Lake Road: Silver Creek Lake, at the edge of the campground. | 31.66344600, -87.57108400 | 16 | Part shade to sun along the eroding banks of Silver Creek Lake in moist-mesic, mixed deciduous and evergreen woodland, 2-3 meters above the water. The underlying geology of this area is Claiborne Group, Tallahatta Formation, of Eocene origin, with white to very light-greenish-gray thin-bedded to massive siliceous claystone; interbedded with thin layers of fossiliferous clay, sandy clay, and glauconitic sand and sandstone. (Source: USGS Alabama Geological Map Data). The primary soil types in the collection area are classified as Riverview Fine Sandy Loam soils (0 to 2 percent slopes, occasionally flooded). The Riverview Series consists of very deep, well drained, moderately permeable soils that formed in loamy alluvium on flood plains. Slopes range from 0 to 5 percent. Riverview soils fare on high parts of flood plains of rivers and streams draining the Coastal Plain and Southern Piedmont. Runoff is slow. Permeability is moderate. These soils flood for short periods mostly in winter or early spring months. (Source: NRCS Web Soil Survey). | Wild material | | 2140819 | NA 88558 |
| 116 | NA 88561 | RJLSEUS2022-034 | Hydrangea quercifolia W. Bartram | Alabama, United States | NA | | | 2023 | COLLECTED | 12/12/2022 | Plants growing in the woodlands at Haines Island Park at the foot of Tallahatta cuesta, accessed by foot via Ferry Road. Common at this site. | 31.72178200, -87.46589600 | 66 | Plants are growing in part-shade to shade of a moist mesic, well-drained conditions on rocks and in the eroding matrix of the Tallahatta Questa.
Soils: The underlying geology of this area is Claiborne Group, Tallahatta Formation, of Eocene origin, with white to very light-greenish-gray thin-bedded to massive siliceous claystone; interbedded with thin layers of fossiliferous clay, sandy clay, and glauconitic sand and sandstone.
Source: USGS Alabama Geological Map Data (https://mrdata.usgs.gov/geology/state/state.php?state=AL)
The primary soil type in the collection area is classified as Arundel Loam soil (8 to 35 percent slopes). The Arundel Series consists of moderately deep, well drained, very slowly permeable soils on dissected uplands of the Southern Coastal Plain. They formed in marine deposits consisting of acid clays underlain by horizontally bedded sandstone, buhrstone and siltstone. These soils are strongly acid. Slopes range from 2 to 60 percent.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2140786 | NA 88561 |
| 117 | NA 88562 | RJLSEUS2022-035 | Kalmia latifolia L. | Alabama, United States | NA | | | 2023 | COLLECTED | 12/12/2022 | Plants growing on both sides of River Ridge Road accessed from Alabama State Hwy 41 via Tin Cup Alley Road. Common at this site | 31.73823700, -87.35821100 | 132 | Plants are growing in part-shade to full sun on top of a very exposed ridge top under dry conditions.
Soils: The underlying geology of this area is of Eocene origin and characterized as Claiborne Group; Gosport Sand and Lisbon Formation Undifferentiated in part. Greenish-gray calcareous, glauconitic, fossiliferous clayey sand; marl; carbonaceous sand; carbonaceous silty clay; and coarse glauconitic, fossiliferous, quartz sand.
Source: USGS Alabama Geological Map Data (https://mrdata.usgs.gov/geology/state/state.php?state=AL)
The primary soil types in the collection area are classified as Saffell Very Gravelly Sandy Loam soil (5 to 8 percent slopes). The Saffell Series consists of very deep, well drained, moderately permeable soils that formed in loamy and gravelly marine sediments of the Tertiary Age and have acid reaction. These soils are found on the upper portion of the bluffs along the Alabama River.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2140787 | NA 88562 |
| 118 | NA 88563 | RJLSEUS2022-036 | Ilex myrtifolia Walter | Florida, United States | NA | | | 2023 | COLLECTED | 12/14/2022 | Eglin Air Forece Base: growing along the east side of Eglin AFB Choctaw Nolf Road northwest of Choctaw Navy Outlying Field. This road goes west and takes a circuitous route to the north around the Field en route to Escribano Point Wildlife Management Area. | 30.52650500, -86.96471100 | 10 | Part shade to sun in permanently wet areas of mixed evergreen and deciduous woodlands, mostly along the edges where higher light conditions prevail. 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 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 material | | 2140820 | NA 88563 |
| 119 | NA 88564 | RJLSEUS2022-037 | Aronia arbutifolia (L.) Pers. | Florida, United States | NA | | | 2023 | COLLECTED | 12/14/2022 | Plants growing along the west 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. Frequent in wet areas. | 30.52667900, -86.96485200 | 60 | Plants are growing in part-shade to full sun of moist to wet depressions in areas where wetland herbaceous plants dominate allowing for more light.
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 of this area is primarily Dorovan-Pamlico Series Association. The Dorovan Series consists of very deep, very poorly drained, moderately permeable soils on densely forested flood plains, hardwood swamps and Southern Coastal Plain Major Land Resource Areas. They were formed in highly decomposed acid-organic materials. Slopes are less than 1 percent. The organic material ranges from 1.3-2.1 meters thick. Reaction is extremely acid to very strongly acid in the organic layers and very strongly acid or strongly acid in the mineral layers. The Pamlico Series consists of very poorly drained soils that formed in decomposed organic material underlain by dominantly sandy sediment. The soils are on nearly level flood plains, bays, and depressions of the Coastal Plain. Slopes are less than 1 percent. Pamlico soils have 0.4-1.3 meters of organic material over dominantly sandy sediments. Reaction is extremely in the organic layers and ranges from extremely acid to strongly acid in the underlying mineral layers.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2140821 | NA 88564 |
| 120 | NA 88566 | RJLSEUS2022-039 | Rhododendron viscosum (L.) Torr. | Florida, United States | NA | | | 2023 | COLLECTED | 12/14/2022 | Plants growing in woodlands at Escribano Point Bayou Campground not far from the parking lot. Occasional. | 30.50990400, -87.00414900 | 1 | Plants 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 material | | 2140788 | NA 88566 |
| 121 | NA 88567 | RJLSEUS2022-040 | Chamaecyparis thyoides (L.) Britton et al. | Florida, United States | NA | | | 2023 | COLLECTED | 12/14/2022 | Plants growing in woodlands at Escribano Point Bayou Campground not far from the parking lot. Occasional. | 30.51018200, -87.00448800 | 1 | Plants 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 material | | 2140789 | NA 88567 |
| 122 | NA 88568 | RJLSEUS2022-041 | Oxydendrum arboreum (L.) DC. | Florida, United States | NA | | | 2023 | COLLECTED | 12/14/2022 | Plants 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, -87.00563800 | 2 | Trees 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 material | | 2140790 | NA 88568 |
| 123 | NA 88569 | RJLSEUS2022-042 | Ilex hybr. | Florida, United States | NA | | | 2023 | COLLECTED | 12/15/2022 | Yellow River: this plant is growing on the edge of the Yellow River and accessed by boat. This collection located approximately 0.4 kilometers north of the Yellow River Boat Ramp on the east side of Florida State Hwy 87. | 30.57317600, -86.92367500 | 1 | This plant was found growing in full sun in permanently saturated to submersed conditions along the edge of the Yellow River, growing in an open river edge with no overstory. Like most of the plants along the river, this collection is adapted to acidic conditions and while the aquatic habitats are generally fresh water, there can occasionally be tidal or hurricane-caused saltwater intrusions. The underlying geology of this area is classified as Alluvium, of Pleistocene/Holocene origin and consists of undifferentiated Quaternary sediments of varying thickness including siliciclastics, organics and freshwater carbonates. The siliciclastics are light gray, tan, brown to black, unconsolidated to poorly consolidated, clean to clayey, silty, unfossiliferous, variably organic-bearing sands to blue green to olive green, poorly to moderately consolidated, sandy, silty clays. Organics occur as plant debris, roots, disseminated organic matrix and beds of peat. Freshwater carbonates, often referred to as marls in the literature, are scattered. (Source: USGS Florida Geologic Map Data). The surface soil profile of this area is primarily Bibb-Kinston Series Association. Bibb Series soils are coarse-loamy, sandy, acid soils that are poorly drained. They are soils of flood plains and streams subject to frequent flooding. These are found in association with Kinston Series soils that are fine-loamy, sandy, acid soils of flood plains and stream subject to frequent flooding. The Bibb-Kinston association ranges from 1-1.5 meters thick and is strongly acid. (Source: Soil Survey of Santa Rosa County and NRCS Web Soil Survey). | Wild material | Ilex putative natural hybrid (I. myrtifolia x I. opaca) | 2140823 | NA 88569 |
| 124 | NA 88570 | RJLSEUS2022-043 | Ilex myrtifolia Walter | Florida, United States | NA | | | 2023 | COLLECTED | 12/15/2022 | Yellow River: plants are growing along a several mile stretch of the Yellow River and accessed by boat via the Yellow River Boat Ramp on the east side of Florida State Hwy 87. | 30.58148800, -86.91121900 | 1 | Plants are typically found growing in full sun to part shade in permanently saturated to submersed conditions along the edge of the Yellow River, growing in association with a wide array of deciduous and evergreen trees, shrubs and perennial plant species. Most of the plants along the river are adapted to acidic conditions and, while the aquatic habitats are generally fresh water, there is occasionally tidal or hurricane-caused saltwater intrusions. The underlying geology of this area is classified as Alluvium, of Pleistocene/Holocene origin and consists of undifferentiated Quaternary sediments of varying thickness including siliciclastics, organics and freshwater carbonates. The siliciclastics are light gray, tan, brown to black, unconsolidated to poorly consolidated, clean to clayey, silty, unfossiliferous, variably organic-bearing sands to blue green to olive green, poorly to moderately consolidated, sandy, silty clays. Organics occur as plant debris, roots, disseminated organic matrix and beds of peat. Freshwater carbonates, often referred to as marls in the literature, are scattered. (Source: USGS Florida Geologic Map Data). The surface soil profile of this area is primarily Bibb-Kinston Series association. Bibb Series soils are coarse-loamy, sandy, acid soils that are poorly drained. They are soils of flood plains and streams subject to frequent flooding. These are found in association with Kinston Series soils that are fine-loamy, sandy, acid soils of flood plains and stream subject to frequent flooding. The Bibb-Kinston association ranges from 1-1.5 meters thick and is strongly acid. (Source: Soil Survey of Santa Rosa County and NRCS Web Soil Survey). | Wild material | | 2140824 | NA 88570 |
| 125 | NA 88571 | RJLSEUS2022-044 | Itea virginica L. | Florida, United States | NA | | | 2023 | COLLECTED | 12/15/2022 | Plants are growing along a several mile stretch of the Yellow River and accessed by boat via the Yellow River Boat Ramp on the east side of Florida State Hwy 87. The species is common along several miles of the Yellow River. | 30.55805600, -86.93544500 | 1 | Plants are typically found growing in part-shade to sun in permanently saturated to submersed conditions along the edge of the Yellow River, growing in association with a wide array of deciduous and evergreen trees, shrubs and perennial plant species. Most of the plants along the river are adapted to acidic conditions and, while the aquatic habitats are generally fresh water, there is occasionally tidal or hurricane-caused saltwater intrusions.
Soils: The underlying geology of this area is classified as Alluvium, of Pleistocene/Holocene origin and consists of undifferentiated Quaternary sediments of varying thickness including siliciclastics, organics and freshwater carbonates. The siliciclastics are light gray, tan, brown to black, unconsolidated to poorly consolidated, clean to clayey, silty, unfossiliferous, variably organic-bearing sands to blue green to olive green, poorly to moderately consolidated, sandy, silty clays. Organics occur as plant debris, roots, disseminated organic matrix and beds of peat. Freshwater carbonates, often referred to as marls in the literature, are scattered.
Source: USGS Florida Geologic Map Data (https://mrdata.usgs.gov/geology/state/state.php?state=fl)
The surface soil profile of this area is primarily Bibb-Kinston Series association. Bibb Series soils are coarse-loamy, sandy, acid soils that are poorly drained. They are soils of flood plains and streams subject to frequent flooding. These are found in association with Kinston Series soils that are fine-loamy, sandy, acid soils of flood plains and stream subject to frequent flooding. The Bibb-Kinston Association ranges from 1-1.5 meters thick and is strongly acid.
Source: Soil Survey of Santa Rosa County and NRCS Web Soil Survey (https://www.nrcs.usda.gov/Internet/FSE_MANUSCRIPTS/florida/FL113/0/SantaRosa.pdf and https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2140791 | NA 88571 |
| 126 | NA 88572 | RJLSEUS2022-045 | Ilex verticillata (L.) A. Gray | Florida, United States | NA | | | 2023 | COLLECTED | 12/15/2022 | Yellow River: plants are growing along a several mile stretch of the Yellow River and accessed by boat via the Yellow River Boat Ramp on the east side of Florida State Hwy 87. | 30.57947400, -86.91906100 | 1 | Plants are typically found growing in full sun to part shade in permanently saturated to submersed conditions along the edge of the Yellow River, growing in association with a wide array of deciduous and evergreen trees, shrubs and perennial plant species. Most of the plants along the river are adapted to acidic conditions and, while the aquatic habitats are generally fresh water, there is occasionally tidal or hurricane-caused saltwater intrusions. The underlying geology of this area is classified as Alluvium, of Pleistocene/Holocene origin and consists of undifferentiated Quaternary sediments of varying thickness including siliciclastics, organics and freshwater carbonates. The siliciclastics are light gray, tan, brown to black, unconsolidated to poorly consolidated, clean to clayey, silty, unfossiliferous, variably organic-bearing sands to blue green to olive green, poorly to moderately consolidated, sandy, silty clays. Organics occur as plant debris, roots, disseminated organic matrix and beds of peat. Freshwater carbonates, often referred to as marls in the literature, are scattered. (Source: USGS Florida Geologic Map Data). The surface soil profile of this area is primarily Bibb-Kinston Series association. Bibb Series soils are coarse-loamy, sandy, acid soils that are poorly drained. They are soils of flood plains and streams subject to frequent flooding. These are found in association with Kinston Series soils that are fine-loamy, sandy, acid soils of flood plains and stream subject to frequent flooding. The Bibb-Kinston association ranges from 1-1.5 meters thick and is strongly acid. (Source: Soil Survey of Santa Rosa County and NRCS Web Soil Survey). | Wild material | | 2140825 | NA 88572 |
| 127 | NA 88573 | RJLSEUS2022-046 | Ilex myrtifolia Walter | Florida, United States | NA | | | 2023 | COLLECTED | 12/15/2022 | Yellow River: this plant is growing on the edge of the Yellow River and accessed by boat. This collection is located approximately 3.2 kilometers by boat north and east of the Yellow River Boat Ramp on the east side of Florida State Hwy 87. | 30.58188200, -86.91220500 | 1 | This plant is growing in full sun in permanently saturated conditions along the edge of the Yellow River, growing in association with a wide array of deciduous and evergreen trees, shrubs and perennial plant species. Most of the plants along the river are adapted to acidic conditions and, while the aquatic habitats are generally fresh water, there is occasionally tidal or hurricane-caused saltwater intrusions. The underlying geology of this area is classified as Alluvium, of Pleistocene/Holocene origin and consists of undifferentiated Quaternary sediments of varying thickness including siliciclastics, organics and freshwater carbonates. The siliciclastics are light gray, tan, brown to black, unconsolidated to poorly consolidated, clean to clayey, silty, unfossiliferous, variably organic-bearing sands to blue green to olive green, poorly to moderately consolidated, sandy, silty clays. Organics occur as plant debris, roots, disseminated organic matrix and beds of peat. Freshwater carbonates, often referred to as marls in the literature, are scattered. (Source: USGS Florida Geologic Map Data). The surface soil profile of this area is primarily Bibb-Kinston Series Association. Bibb Series soils are coarse-loamy, sandy, acid soils that are poorly drained. They are soils of flood plains and streams subject to frequent flooding. These are found in association with Kinston Series soils that are fine-loamy, sandy, acid soils of flood plains and stream subject to frequent flooding. The Bibb-Kinston Association ranges from 1-1.5 meters thick and is strongly acid. (Source: Soil Survey of Santa Rosa County and NRCS Web Soil Survey). | Wild material | orange-fruited form | 2140826 | NA 88573 |
| 128 | NA 88574 | RJLSEUS2022-047 | Rhododendron austrinum (Small) Rehder | Florida, United States | NA | | | 2023 | COLLECTED | 12/15/2022 | Plants are growing along a several mile stretch of the Yellow River and accessed by boat via the Yellow River Boat Ramp on the east side of Florida State Hwy 87. The species is found frequently along several miles of the Yellow River. | 30.58133600, -86.89953900 | 2 | Plants are found growing in part-shade to shade along areas of the river where natural levies, 1-3 meters tall, have formed, depositing sand and organic matter. The plants grow well-above normal flow of the river in well-drained to dry conditions. Even so, they are periodically subjected to inundation from floodwaters.
Soils: The underlying geology of this area is classified as Alluvium, of Pleistocene/Holocene origin and consists of undifferentiated Quaternary sediments of varying thickness including siliciclastics, organics and freshwater carbonates. The siliciclastics are light gray, tan, brown to black, unconsolidated to poorly consolidated, clean to clayey, silty, unfossiliferous, variably organic-bearing sands to blue green to olive green, poorly to moderately consolidated, sandy, silty clays. Organics occur as plant debris, roots, disseminated organic matrix and beds of peat. Freshwater carbonates, often referred to as marls in the literature, are scattered.
Source: USGS Florida Geologic Map Data (https://mrdata.usgs.gov/geology/state/state.php?state=fl)
The surface soil profile of this area is primarily Bibb-Kinston Series Association. Bibb Series soils are coarse-loamy, sandy, acid soils that are poorly drained. They are soils of flood plains and streams subject to frequent flooding. These are found in association with Kinston Series soils that are fine-loamy, sandy, acid soils of flood plains and stream subject to frequent flooding. The Bibb-Kinston Association ranges from 1-1.5 meters thick and is strongly acid.
Source: Soil Survey of Santa Rosa County and NRCS Web Soil Survey (https://www.nrcs.usda.gov/Internet/FSE_MANUSCRIPTS/florida/FL113/0/SantaRosa.pdf and https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | Yellow River Pink Austrinum | 2140792 | NA 88574 |
| 129 | NA 88576 | RJLSEUS2022-049 | Rhododendron atlanticum (Ashe) Rehder | South Carolina, United States | NA | | | 2023 | COLLECTED | 12/16/2022 | Plants growing in mixed evergreen and deciduous woods on the east side of Ip Canal Road approximately 0.33 kilometers south of Pleasant Hill Drive (Georgetown County Road 251). Frequent at this location. | 33.63226900, -79.25831700 | 8 | Plants are growing in part-shade to shade of a dry to periodically moist mesic woodland. Given some of the plant associates, there may be an impermeable subsurface soil layer to add moisture availability.
Soils: The underlying geology of this area is of Pleistocene origin and characterized as Socastee Formation. This is a low coastal formation in the Carolinas like Penholoway but younger and lower in altitude. The Socastee Formation lies seaward of the Penholoway and Canepatch Formations and is the next younger surficial unit. It is exposed in a belt approximately 25 km wide at elevations between 9 and 15 m above sea level. It is described as variegated quartzose sands, argillaceous sands, and clays, 5 m thick at the type section near Socastee Swamp. Unconformably overlies Canepatch Formation; unconformably underlies Waiter Island Formation and Ocean Forest Peat.
Source: USGS Texas Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=SCQso%3B1)
The primary soil type in the collection area is classified as Centenary Fine Sand. The Centenary Fine Sand Series consists of deep, well drained or somewhat excessively drained single-grained sand that is loose and moderately acid. The upper layer ranges from 7.5cm to 25cm thick. Deeper layers vary in percentage of single-grained sands and clay.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2140794 | NA 88576 |
| 130 | NA 88511 | RJL2022TX-006 | Persea palustris (Raf.) Sarg. | Texas, United States | NA | | | 2022 | COLLECTED | 11/01/2022 | Plants growing in a wetland on the north side of Clarktown Road approximately 1.5 kilometers west of Texas State Hwy 87 in Sabine National Forest. Plant is common in the moist-wet and mesic edges of the wetland habitat where it is best adapted. | 31.17114800, -93.75106200 | 71 | Plants are growing in part-shade in a depression wetland of a small upland valley stream area surrounded by upland Pinus palustris and Pinus taeda forests. While the region had a severe drought during 2022, this depression wetland remained mucky wet throughout. Higher light conditions that supported heavy fruit production on the Persea may have been due to nearby harvesting of forest sections adjacent to the wetland.
Soils: The underlying geology of this area is of Oligocene origin and characterized as Catahoula Formation. This formation is extensive and deep in Texas, up to 185 meters thick. In the area of the collection the Catahoula Formation is primarily mudstone and sand. The upper 90-150 meters is mudstone that is tuffaceous, and sandy; also, occasionally, with some bentonitic clay.
Source: USGS Texas Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=TXQbs%3B0
The primary soil types in the collection area are classified as Letney soils. These soils consist of deep, somewhat excessively drained, moderately rapidly permeable soils on uplands. They were formed in thick loamy and sandy sediments on the Western Coastal Plain. The Letney soils are on gently sloping uplands with slopes ranging from 1 to 5 percent. They are typically strongly acidic. It should be noted that the upper surface, to an unknown depth has a significant amount of decomposed and undecomposed organic litter, presumably from sphagnum, at least, in part.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2139818 | NA 88511 |
| 131 | NA 88512 | RJL2022TX-007 | Morella caroliniensis (Mill.) Small | Texas, United States | NA | | | 2022 | COLLECTED | 11/01/2022 | Plants growing in a wetland on the north side of Clarktown Road approximately 1.5 kilometers west of Texas State Hwy 87 in Sabine National Forest. Plant is relatively common in the moist-wet and mesic edges of the wetland habitat. | 31.17181200, -93.75118000 | 81 | Plants are growing in part-shade to part-sun in a depression wetland and slightly upslope of a small upland valley stream area surrounded by upland Pinus palustris and Pinus taeda forests. While the region had a severe drought during 2022, this depression wetland remained mucky wet throughout.
Soils: The underlying geology of this area is of Oligocene origin and characterized as Catahoula Formation. This formation is extensive and deep in Texas, up to 185 meters thick. In the area of the collection the Catahoula Formation is primarily mudstone and sand. The upper 90-150 meters is mudstone that is tuffaceous, and sandy; also, occasionally, with some bentonitic clay.
Source: USGS Texas Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=TXQbs%3B0
The primary soil types in the collection area are classified as Letney soils. These soils consist of deep, somewhat excessively drained, moderately rapidly permeable soils on uplands. They were formed in thick loamy and sandy sediments on the Western Coastal Plain. The Letney soils are on gently sloping uplands with slopes ranging from 1 to 5 percent. They are typically strongly acidic. It should be noted that the upper surface, to an unknown depth has a significant amount of decomposed and undecomposed organic litter, presumably from sphagnum, at least, in part.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2139819 | NA 88512 |
| 132 | WLP 2676 | RJL2022NJ-007 | Kalmia latifolia L. | New Jersey, United States | NA | | | 2022 | COLLECTED | 10/24/2022 | Plants growing along Hawkins Bridge Road in Wharton State Forest. Plants are common and frequent throughout the woodlands at this location. | 39.70292400, -74.56106800 | 16 | Plants 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 material | | 2139667 | WLP 2676 |
| 133 | WLP 2675 | RJL2022NJ-006 | Kalmia angustifolia L. | New Jersey, United States | NA | | | 2022 | COLLECTED | 10/24/2022 | Plants growing along Hawkins Bridge Road in Wharton State Forest. Plants are common and frequent throughout the woodlands at this location. | 39.70231900, -74.56084200 | 16 | Plants 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 material | | 2139666 | WLP 2675 |
| 134 | WLP 2673 | RJL2022NJ-004 | Lyonia mariana (L.) D. Don | New Jersey, United States | NA | | | 2022 | COLLECTED | 10/24/2022 | Plants growing on both sides of Duerer Street approximately 0.37 kilometers southeast of 4th Avenue, Mullica Township, New Jersey. Plants are common but scattered on both sides of the road at this site. | 39.55730700, -74.66376100 | 22 | Plants grow from part shade to full sun throughout the habit from the upper edges of the ditches through the herbaceous grass dominant buffer and all the way to the part shade of the woodland edge. Plants transition through moist/wet conditions in full sun to quite dry conditions in part shade and seem equally adapted.
Soils: The underlying geology of this area is the Cohansey Formation of middle Miocene origin and comprised of sand, white to yellow with local gravel and clay. It is sometimes locally stained red or orange brown by iron oxides and (or) cemented into large blocks of ironstone. Unweathered clay is typically dark gray, but commonly weathers white where it is interbedded with thin beds of ironstone. Sand is typically medium grained and moderately sorted although it ranges from fine to very coarse grained and from poorly to well sorted. Sand consists of quartz and siliceous rock fragments. Some beds are locally micaceous. Maximum thickness in the map area is about 60 meters; however, thickness is difficult to determine because of the irregular basal contact and extensive post-depositional erosion.
Source: USGS New Jersey Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=NJTch%3B1)
The primary soil type in the area of this collection is classified as Mullica sandy loam, 0 to 2 percent slopes. These soils are typically coarse-loamy, siliceous, semiactive, and mesic typic humaquepts that are strongly to extremely acidic throughout the profile. The typical solum thickness ranges from 50-150+ cm. These soils are generally considered to be poorly drained.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2139664 | WLP 2673 |
| 135 | NA 88499 | RJL2022MD-018 | Ilex opaca Aiton | Maryland, United States | NA | | | 2022 | COLLECTED | 10/22/2022 | Elk Neck State Park: woodlands along Maryland Hwy 272, Turkey Point Road. | 39.47706500, -75.98720900 | 35 | Plants growing in shade to full sun on well-drained slopes of a mixed evergreen and deciduous woodland. Soils: The underlying geology of this area is the characterized as Upland Deposits (Eastern Shore) of Quaternary origin. This formation is characterized by gravel, sand, silt, and clay. Mostly cross-bedded, poorly sorted, medium- to coarse-grained white to red sand and gravel; boulders near base; minor pink and yellow silts and clays. The thickness of this formation ranges from 0 to 90 feet, locally thicker in paleochannels. (Source: USGS Maryland Geologic Map Data). The primary soil type in the area of this collection is classified as Sassafras and Croom soils, 15 to 25 percent slopes. These soils are typically fine-loamy, siliceous, semiactive, mesic typic hapludults that are strongly to extremely acid. The typical solum thickness ranges from 60-130 cm. These soils are generally well-drained. (Source: NRCS Web Soil Survey). | Wild material | | 2139662 | NA 88499 |
| 136 | WLP 2670 | RJL2022PA-016 | Acer negundo L. | Pennsylvania, United States | NA | | | 2022 | COLLECTED | 10/21/2022 | Plants growing in woodlands above a small unnamed creek that dumps into the Middle Branch White Clay Creek in Goddard Park, West Grove Pennsylvania, off of Wickerton Road, Chester County. Plants are found regularly but scattered in the understory of the woodlands. | 39.80426000, -75.82609300 | 105 | Plants growing in a mesic, well-drained habitat of deciduous woodlands along streams and above the riparian zone that drains toward a small unnamed creek that feeds into the Middle Branch White Clay Creek. Plants generally grow in part shade to full sun, but perform best and fruit more heavily in full sun where there is abundant access to moisture. The remnant woodlands exist mostly along the steep slopes, wetlands and seeps of seasonal and year-round creeks flowing into the Middle Branch White Clay Creek. The woodlands are bordered by numerous housing developments and land converted to meadows; hence there is significant first order edge that is heavily impacted by invasive plant intrusion. Despite this fact, Acer negundo is highly competitive and competes well.
Soils: The underlying geology of this area is the Glenarm Wissahickon Formation of lower Paleozoic origin and lithologically similar to oligoclase-mica schist of the Wissahickon Formation (PZw), but also includes lenticular amphibolite bodies having ocean-floor basalt chemistry.
Source: USGS Pennsylvania Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=PAPZgw%3B0)
The primary soil type in the area of this collection is classified as Glenelg silt loam, 3 to 8 percent slopes. This series consists of very deep, well drained soils formed in residuum weathered from micaceous schist on uplands of the Blue Ridge and the Northern Piedmont. Saturated hydraulic conductivity is moderately high in the subsoil and moderately high to high in the substratum. This upper horizon of this soil is undifferentiated, mostly poorly drained sandy bottomland soils intermingled with decomposing organic litter and eroded silts and clays due to erosion.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2139661 | WLP 2670 |
| 137 | WLP 2669 | RJL2022NJ-001 | Rhododendron viscosum (L.) Torr. | New Jersey, United States | NA | | | 2022 | COLLECTED | 10/19/2022 | Plants 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, -74.67798200 | 7 | Plants 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 material | | 2139660 | WLP 2669 |
| 138 | NA 89045 | RJL2022PA-013 | Tsuga canadensis (L.) Carrière | Pennsylvania, United States | NA | | | 2022 | COLLECTED | 10/07/2022 | Plants growing on the steep banks along Octoraro Creek accessed by canoe. Plants are locally common but generally infrequent along the Octoraro Creek. | 39.74442700, -76.08856400 | 66 | Plants are growing in part-shade to sun of mixed deciduous and evergreen forests on steep rocky habitats overlain by relatively deep soil over occasionally exposed geology along the Octoraro Creek.
Soils: The underlying geology of this area is estimated to be of lower Paleozoic origin and comprised of Peters Creek Schist. This is comprised of chlorite-sericite schist containing interbedded quartzite.
Source: USGS Pennsylvania Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=PAPZpc%3B0)
The primary soil types in the collection area are classified as Manor loam, 25 to 35 percent slopes, very stony. The soils in the collecting area originated as residuum, weathered from the micaceous schist exposed geology and are generally considered coarse-loamy, micaceous, mesic typic dystrudepts that are very acidic and well-drained. There is a variable depth of soil depending upon the steepness of slopes. Some areas contain significant exposed Peters Creek Schist overlain by a highly decomposed organic mat intermingled with a dense root mat of woody and herbaceous plants.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2139610 | NA 89045 |
| 139 | NA 89039 | RJL2022IL-001 | Ptelea trifoliata L. | Illinois, United States | NA | | | 2022 | COLLECTED | 09/28/2022 | Site of plant habitat is located at 823 E Co Rd 1220, Hamilton, IL 62341 which is the property where Jacob's Geode Shop and Mine is located. This species is scattered and relatively common throughout the woodlands on this site. | 40.37848400, -91.35390200 | 175 | Plants growing in shade to part-shade of deciduous woodlands above a small creek.
Soils: The underlying geology of this area is of Mississippian origin and comprised of Warsaw Formation and Salem Limestone. Major lithological components include limestone that can be shaly, oolitic, bioclastic, or cherty. Minor lithological components include siltstone that can contain geodes or drusy quartz and can be calcareous.
Source: USGS Illinois Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=ILMws%3B0)
The surface soil profile of this area is Coffeen silt loam, 0 to 2 percent slopes, that are frequently flooded. The Coffeen series consists of very deep, somewhat poorly drained, moderately permeable soils on flood plains, low terraces or benches, toe slopes, and alluvial fans. They formed in silty alluvium. Much of the alluvium is of local origin derived from the nearby loess-covered uplands.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2139604 | NA 89039 |
| 140 | NA 89033 | RJL2022MD-010 | Clethra alnifolia L. | Maryland, United States | NA | | | 2022 | COLLECTED | 09/15/2022 | Plants growing in low woodlands at the end of Greenway Avenue near a boat dock that leads to the Pocomoke River, adjacent to Winter Quarters Golf Course, Pocomoke City. Plants common throughout the wetland area as well as mesic edges of the woodlands. | 38.08305100, -75.56527800 | | Plants growing in the flood plain of the Pocomoke River in shade to part sun of a mixed deciduous and evergreen bottomland habitat about 10 meters from the edge of the golf course fairway. The habitat is a mucky swamp edge habitat next to the Pocomoke River, most of which seems wet year-round and grades slightly upslope to more mesic conditions.
The underlying geology of this area is comprised of Quaternary Deposits of Wisconsin to Holocene origin. The composition is primarily undifferentiated gray to buff sand and gravel, gray to brown lignitic silt and clay, occasional boulders, and rare shell beds. Surficial deposits occur as shell-bearing estuarine clays and silts.
Source: USGS Maryland Geologic Map Data https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=MDQdu%3B5
The surface soil profile of this habitat is classified as Puckum Muck which is frequently flooded. These highly saturated soils are found in flats, depressions and swales. The soil reaction of Puckum Muck is extremely acid to strongly acid throughout the profile. The depth to bedrock is generally greater than 150 cm. Wood fragments comprise 0-25%, by volume of the Puckum Muck throughout the profile which includes mostly twigs, branches, logs, or stumps and are 1.5-30 cm in diameter. The composition of these highly saturated soils, are classified as muck (sapric soil material) or mucky peat (hemic soil material) throughout most of the upper 150 cm and may contain thin layers of mucky silt loam, silty clay loam, sandy loam and/or sand.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2139598 | NA 89033 |
| 141 | NA 89032 | RJL2022MD-009 | Rhododendron viscosum (L.) Torr. | Maryland, United States | NA | | | 2022 | COLLECTED | 09/15/2022 | Plants growing in low woodlands at the end of Greenway Avenue near a boat dock that leads to the Pocomoke River, adjacent to Winter Quarters Golf Course, Pocomoke City. Plants scattered throughout the wetland area. Infrequent, but regularly found. | 38.08235200, -75.56566500 | 1 | Plants growing in the flood plain of the Pocomoke River in part shade to shade of a mixed deciduous and evergreen bottomland habitat about 10 meters from the edge of the golf course fairway. The habitat is a mucky swamp edge habitat next to the Pocomoke River, most of which seems wet year-round.
The underlying geology of this area is comprised of Quaternary Deposits of Wisconsin to Holocene origin. The composition is primarily undifferentiated gray to buff sand and gravel, gray to brown lignitic silt and clay, occasional boulders, and rare shell beds. Surficial deposits occur as shell-bearing estuarine clays and silts.
Source: USGS Maryland Geologic Map Data https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=MDQdu%3B5
The surface soil profile of this habitat is classified as Puckum Muck which is frequently flooded. These highly saturated soils are found in flats, depressions and swales. The soil reaction of Puckum Muck is extremely acid to strongly acid throughout the profile. The depth to bedrock is generally greater than 150 cm. Wood fragments comprise 0-25%, by volume of the Puckum Muck throughout the profile which includes mostly twigs, branches, logs, or stumps and are 1.5-30 cm in diameter. The composition of these highly saturated soils, are classified as muck (sapric soil material) or mucky peat (hemic soil material) throughout most of the upper 150 cm and may contain thin layers of mucky silt loam, silty clay loam, sandy loam and/or sand.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2139597 | NA 89032 |
| 142 | WLP 2610 | 2022VA-01 | Stewartia malacodendron L. | Virginia, United States | NA | | | 2022 | COLLECTED | 09/12/2022 | Woodlands adjacent to and bounded by the interchange of Business Route 168 (N. Battlefield Avenue) and Route 168, next to a detention basin and shopping plaza on the west side of Battlefield Avenue. Accessed by parking in the cul-de-sac at the south end of Kingsborough Square Street. This plant is a very common and abundant component of this woodland with significant recruitment continuing | 36.73888200, -76.24327700 | 9 | Plants growing in rich mesic, moist but well-drained conditions in the high understory shade of a mixed deciduous and evergreen woodland, primarily comprised of deciduous trees in the over-story and a mixture of deciduous and evergreen species in the sub-canopy.
Soils: The underlying geology of this area is the Tabb Formation of Quaternary origin which is comprised of undifferentiated sand, silt, and peat and subdivided into three members. Within the Tabb Formation lies the Sedgefield Member, a pebbly to bouldery, clayey sand and fine to medium, shell-rich sand that grades upward into sandy and clayey silt; locally, channel fill at the base of unit includes as much as 15 meters of fine to coarse, cross-bedded sand and clayey silt and peat containing in-situ tree stumps. Sandy bay facies commonly contain numerous mollusks as well as coral. Thickness is 0 to 15.8 meters.
Source: USGS Virginia Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=VAQts%3B0)
The surface soil profile of this area is Tetotum fine sandy loam, 0 to 2 percent slopes. Forming primarily terraces, these soils are moderately well-drained and highly acidic. They are generally 100-150 cm thick, the upper 20 inches of the horizon averages more than 30 percent silt or more than 40 percent silt plus very fine sand.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2139348 | WLP 2610 |
| 143 | WLP 2612 | 2022VA-03 | Styrax grandifolius Aiton | Virginia, United States | NA | | | 2022 | COLLECTED | 09/12/2022 | Northwest River Park on the south side of Indian Springs Road behind the Equestrian Center along a bridle trail. This plant is a common in the mesic woodlands at this location. | 36.58361100, -76.16277800 | 21 | Plants growing in shade to part-shade of the mixed deciduous and evergreen mesic woodland about 1 to 2 meters above a nearby wetland area.
The underlying geology of this area is the Tabb Formation of Quaternary origin which is comprised of undifferentiated sand, silt, and peat and subdivided into three members. Within the Tabb Formation lies the Lynnhaven Member with pebbly and cobbly, fine to coarse gray sand grades upward into clayey and silty fine sand and sandy silt. Extensive low lands bounded on the landward side by river-, bay-, and ocean-facing scarps having toe altitudes of 5-6 meters. Thickness is 0 to 6.5 meters.
Source: USGS Virginia Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=VAQtl%3B0)
The surface soil profile of this area is Chapanoke-Yeopim complex, 0 to 3 percent slopes. These soil as somewhat poorly to moderately drained, acidic, and found on marine terraces and summits of low elevation coastal plain areas. They are comprised of silt loam, silty clay loam, sandy clay loam and loam in varying quantities across the profile; the depth to parent geology is approximately 200 cm.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx | Wild material | | 2139350 | WLP 2612 |
| 144 | WLP 2614 | 2022VA-05 | Euonymus americanus L. | Virginia, United States | NA | | | 2022 | COLLECTED | 09/12/2022 | In Colonial Williamsburg, park in the Providence Hall Directors Wing parking lot and enter the Bassett Trace Nature Trail; this species is found in the woodlands on either side of the trail and over a bridge until the it turns right. This plant is infrequent, but occasionally found in the mesic woodlands throughout this location. | 37.26681600, -76.69252800 | 21 | Plants growing in shade to part-shade of the mixed deciduous and evergreen mesic woodland. This species is generally growing in areas with an abundant organic, mature woodland that is relatively undisturbed.
The underlying geology of this area is Windsor Formation of Tertiary-Quaternary origin (lower Pleistocene or upper Pliocene). It is comprised of gray and yellowish- to reddish-brown sand, gravel, silt, and clay. It constitutes surficial deposits of extensive plain and fluvial-estuarine terraces above elevations of 10 meters. The thickness of the Windsor Formation is 0 to 12.5 meters.
Source: USGS Virginia Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=VAQTw%3B0)
The surface soil profile of this area is Emporia Complex, 15 to 25 percent slopes. This soil as moderately well-drained, acidic, and found on sloping and elevated terraces. They are comprised of fine sandy loam, loam, and sandy clay loam in varying quantities across the profile; the depth to parent geology is approximately 200 cm.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2139352 | WLP 2614 |
| 145 | Ames 35907 | Oak Creek Canyon | Fraxinus velutina Torr. | Arizona, United States | NC7 |  | | 2022 | COLLECTED | 09/02/2022 | Oak Creek Canyon, approximately five miles north-northeast of Sedona in the Coconino National Forest. T18N R6E NE 1/4 NW 1/4 Sec. 21 . | 34.93600300, -111.74436900 | 1464 | Floodplain and riverbanks, growing in gravely soil. | Wild material | Most of the velvet ash in this population are small trees (10-25 feet in height and approximately 5 inches DBH). Variation was noted for leaflet pubescence but with the petioles of all trees in the population being pubescent. | 2139669 | Ames 35907 |
| 146 | WLP 2599 | RJL2022FLAL-028 | Viburnum nitidum Aiton | Florida, United States | NA | | | 2022 | COLLECTED | 08/07/2022 | Eglin AFB, in woodlands along Weaver Creek accessed from unnamed dirt road, 0.82 kilometers west of junction with Eglin AFB 720; approximately 0.73 kilometers north of junction with Choctaw Nolf Airfield Road and Eglin AFB 720. | 30.51753300, -86.91490000 | 13 | Plants are found growing in part shade to nearly full sun of a mixed deciduous and broadleaved evergreen woodland along Weaver Creek where there is a wider stream edge with low to flat slopes above the normal creek flow. 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. | Wild material | | 2138709 | WLP 2599 |
| 147 | WLP 2600 | RJL2022FLAL-029 | Stewartia malacodendron L. | Florida, United States | NA | | | 2022 | COLLECTED | 08/07/2022 | Eglin AFB, in woodlands along Weaver Creek accessed from unnamed dirt road, 0.82 kilometers west of junction with Eglin AFB 720; approximately 0.73 kilometers north of junction with Choctaw Nolf Airfield Road and Eglin AFB 720. | 30.51680000, -86.91469400 | 15 | Growing in moist, well-drained sandy soils above Weaver Creek in mixed broadleaved evergreen and deciduous woodland habitat in part shade to shade of west facing slopes several meters above the wetland zone. The Stewartia is growing in a high competition habitat. 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. | Wild material | | 2138710 | WLP 2600 |
| 148 | NA 87204 | RJL2022FLAL-019 | Ilex coriacea (Pursh) Chapm. | Florida, United States | NA | | | 2022 | COLLECTED | 08/02/2022 | Corner of San Jose Street and South 28th Avenue just east of Avalon Beach, FL. | 30.53172700, -87.09058900 | 3 | Growing in full sun to part shade in moist to wet areas, often with sphagnum moss along the edges, just above the water in ditches and waterways. Population is so dense that plants are crowding out other species. The underlying geology of this area is classified as Alluvium, of Pleistocene/Holocene origin and consists of undifferentiated Quaternary sediments of varying thickness including siliciclastics, organics and freshwater carbonates. The siliciclastics are light gray, tan, brown to black, unconsolidated to poorly consolidated, clean to clayey, silty, unfossiliferous, variably organic-bearing sands to blue green to olive green, poorly to moderately consolidated, sandy, silty clays. Organics occur as plant debris, roots, disseminated organic matrix and beds of peat. Freshwater carbonates, often referred to as marls in the literature, are scattered. | Wild material | | 2138707 | NA 87204 |
| 149 | NA 88414 | MARSB-446 | Pinus rigida Mill. | New Jersey, United States | NA | | | 2021 | | | | | | | Wild material | | 2137177 | NA 88414 |
| 150 | NA 86885 | RJL2021PA-004 | Ilex verticillata (L.) A. Gray | Pennsylvania, United States | NA | | | 2021 | COLLECTED | 11/16/2021 | Plants growing in woodlands along a small unnamed creek corridor dumping into the Middle Branch White Clay Creek in Goddard Park, West Grove Pennsylvania, off of Wickerton Road, Chester County. | 39.81063861, -75.82750806 | 124 | Plants are growing in a range of habitats from mesic woodlands to saturated streamside settings of deciduous woodlands that drain toward the Middle Branch White Clay Creek. Plants grow in high understory shade with dappled to indirect sunlight. The only female (fruiting) plants were found in areas along the creek where soils are moist to saturated. Numerous male specimens were found in the areas described above. Soils: Soils found in the areas where this collection was made are comprised primarily of Baile silt loam (Ba), Hatboro silt loam (Ha), and Glenelg silt loam, 8 to 15 percent slopes (GgC). Baile silt loam consists of very deep, poorly drained, moderately low to moderately high saturated hydraulic conductivity, soils on upland depressions and footslopes that were formed in local alluvium over residuum from acid crystalline rocks, chiefly mica schist and granitized schist and gneiss; slope ranges from 0 to 8 percent. Hatboro silt loam consists of very deep and poorly drained soils formed in deposited alluvium derived from metamorphic and crystalline rock. They are on flood plains. Slopes range from 0 to 3 percent. Glenelg silt loam, 8 to 15 percent slopes consists of very deep, well drained soils formed in residuum weathered from micaceous schist on uplands of the Blue Ridge and the Northern Piedmont. This soil is undifferentiated, mostly poorly drained sandy bottomland soils intermingled with decomposing organic litter and eroded silts and clays due to erosion. Slope: 0 to 15% Aspect: Variable. | Wild material | | 2123125 | NA 86885 |
| 151 | WLP 1731 | RJL2021PA-001 | Viburnum acerifolium L. | Pennsylvania, United States | NA | | | 2021 | COLLECTED | 11/05/2021 | Plants growing in woodlands above a small unnamed creek that dumps into the Middle Branch White Clay Creek in Goddard Park, West Grove Pennsylvania, off of Wickerton Road, Chester County. | 39.80462083, -75.82888750 | 103 | Plants growing in a mesic, well-drained habitat of deciduous woodlands, for the most part, above the riparian zone that drains toward a small unnamed creek that feeds into the Middle Branch White Clay Creek. Plants are growing in high understory shade with very little direct sun during most of the day. The remnant woodlands exist mostly along the steep slopes, wetlands and seeps of seasonal and year-round creeks flowing into the Middle Branch White Clay Creek. The woodlands are bordered by numerous housing developments and land converted to meadows; hence there is significant first order edge that is heavily impacted by invasive plant intrusion. Soils: Soils are classified as Glenelg silt loam, 8 to 15% slopes (GgC); this series consists of very deep, well drained soils formed in residuum weathered from micaceous schist on uplands of the Blue Ridge and the Northern Piedmont. Saturated hydraulic conductivity is moderately high in the subsoil and moderately high to high in the substratum. This upper horizon of this soil is undifferentiated, mostly poorly drained sandy bottomland soils intermingled with decomposing organic litter and eroded silts and clays due to erosion. Slope: 8 to 15% Aspect: West. | Wild material | | 2123080 | WLP 1731 |
| 152 | WLP 1732 | RJL2021PA-002 | Viburnum prunifolium L. | Pennsylvania, United States | NA | | | 2021 | COLLECTED | 11/05/2021 | Plants growing in woodlands along a small unnamed creek corridor dumping into the Middle Branch White Clay Creek in Goddard Park, West Grove Pennsylvania, off of Wickerton Road, Chester County. | 39.80462083, -75.82888750 | 102 | Plants are growing in a range of habitats from drier upland woods to moist creekside settings of deciduous woodlands that drain toward the Middle Branch White Clay Creek. Plants grow in part shade to high understory shade with dappled to indirect direct sunlight. Plants achieve their largest size and fruiting potential in part sun of the riparian zone of the creek where woodland canopy is thinner. Soils: Soils found in the areas where this collection was made are comprised primarily of flood plain Hatboro silt loam (Ha) and well-drained, upland Glenelg silt loam, 8 to 15 percent slopes (GgC). Hatboro silt loam consists of very deep and poorly drained soils formed in deposited alluvium derived from metamorphic and crystalline rock. They are on flood plains. Slopes range from 0 to 3 percent. Glenelg silt loam, 8 to 15 percent slopes consists of very deep, well drained soils formed in residuum weathered from micaceous schist on uplands of the Blue Ridge and the Northern Piedmont. This soil is undifferentiated, mostly poorly drained sandy bottomland soils intermingled with decomposing organic litter and eroded silts and clays due to erosion. Slope: 0 to 15% Aspect: Variable. | Wild material | | 2123098 | WLP 1732 |
| 153 | WLP 1733 | RJL2021PA-003 | Viburnum dentatum L. | Pennsylvania, United States | NA | | | 2021 | COLLECTED | 11/05/2021 | Plants growing in woodlands along a small unnamed creek corridor dumping into the Middle Branch White Clay Creek in Goddard Park, West Grove Pennsylvania, off of Wickerton Road, Chester County. | 39.80522167, -75.82928139 | 107 | Plants are growing in a range of habitats from mesic woodland to moist creekside settings of deciduous woodlands that drain toward the Middle Branch White Clay Creek. Plants grow in high understory shade with dappled to indirect sunlight. Soils: Soils found in the areas where this collection was made are comprised primarily of flood plain Hatboro silt loam (Ha) and well-drained, upland Glenelg silt loam, 8 to 15 percent slopes (GgC). Hatboro silt loam consists of very deep and poorly drained soils formed in deposited alluvium derived from metamorphic and crystalline rock. They are on flood plains. Slopes range from 0 to 3 percent. Glenelg silt loam, 8 to 15 percent slopes consists of very deep, well drained soils formed in residuum weathered from micaceous schist on uplands of the Blue Ridge and the Northern Piedmont. This soil is undifferentiated, mostly poorly drained sandy bottomland soils intermingled with decomposing organic litter and eroded silts and clays due to erosion. Slope: 0 to 15% Aspect: Variable. | Wild material | | 2123124 | WLP 1733 |
| 154 | Ames 35750 | Ames 35750 | Blephilia ciliata (L.) Benth. | Iowa, United States | NC7 |  | | 2021 | COLLECTED | 09/27/2021 | Located approximately 3 miles south, southeast of Fairfield, T71N R9W SW1/4 Sec. 7 | 40.96338000, -91.94686900 | 223 | Woodland openings/edges, disturbed areas | Wild material | | 2122068 | Ames 35750 |
| 155 | Ames 35746 | Guye Woods | Acer saccharum Marshall subsp. nigrum (F. Michx.) Desmarais | Iowa, United States | NC7 |  | | 2021 | COLLECTED | 09/08/2021 | Guye Woods County Park located 6.0 miles northeast of Winterset, T76N R27W NE1/4 Sec. 4 | 41.41235000, -93.96373000 | 278 | Moist deciduous maple, oak, hickory forest, northwest facing slope above the North River. | Wild material | Multiple specimens in this population were observed to be 24" diameter at breast height (DBH) or larger with the largest specimen encountered at the time of collection measuring 36.5" DBH.
Morphological traits of leaves suggests sampled specimens are true to type of Acer saccharum subsp. nigrum including leaves with three distinct points, leathery/thick, and drooping in appearance. On September 25, 2020 (Schmitz, A., personal communication, 31 January 2022), peak fall color on Acer saccharum subsp. nigrum at Guye Woods was observed with specimens having a clean yellow fall color, also indicative of Acer saccharum subsp. nigrum.
| 2122010 | Ames 35746 |
| 156 | NA 88332 | CBG-10580 | Hypericum prolificum L. | Illinois, United States | NA | | | 2021 | | | | | | | Wild material | Plant numbers sampled estimated. | 2120171 | NA 88332 |
| 157 | OPGC 8343 | CBG-10575 | Euthamia graminifolia (L.) Nutt. | Illinois, United States | OPGC | | | 2021 | | | | | | | Wild material | Plant numbers sampled estimated. | 2120166 | OPGC 8343 |
| 158 | OPGC 8356 | CBG-10606 | Solidago ulmifolia Muhl. ex Willd. | Illinois, United States | OPGC | | | 2021 | | | | | | | Wild material | Plant numbers sampled estimated. | 2120227 | OPGC 8356 |
| 159 | W6 59206 | CBG-10504 | Muhlenbergia sobolifera (Muhl. ex Willd.) Trin. | Illinois, United States | W6 | | | 2021 | | | | | | | Wild material | | 2120201 | W6 59206 |
| 160 | W6 59243 | CBG-10560 | Cinna arundinacea L. | Illinois, United States | W6 | | | 2021 | | | | | | | Wild material | Plant numbers estimated. | 2120155 | W6 59243 |
| 161 | W6 59266 | CBG-10588 | Muhlenbergia sobolifera (Muhl. ex Willd.) Trin. | Illinois, United States | W6 | | | 2021 | | | | | | | Wild material | | 2120209 | W6 59266 |
| 162 | W6 59267 | CBG-10590 | Muhlenbergia glabrifloris Scribn. | Illinois, United States | W6 | | | 2021 | | | | | | | Wild material | Received as: Muhlenbergia glabriflora. Plant numbers sampled estimated. | 2120210 | W6 59267 |
| 163 | Ames 35667 | Kankakee Sands Preserve | Aronia ×prunifolia (Marshall) Rehder | Illinois, United States | NC7 |  | | 2021 | COLLECTED | 05/04/2021 | Kankakee Sands Preserve located approximately 2.3 miles southwest of Wilmington in Custer Township, T32N R9E NE 1/4 Sec. 11 | 41.27166000, -88.15701800 | 170 | Sand shrub prairie | Wild material | Genotypes noted in nature were averaging 5.0-6.0' in height, relatively upright in growth habit and extremely dense suckering. Numerous clones noted covering expansive areas (e.g. 30 yards by 20 yards, etc.). Variation in branching and glossiness of leaves noted across genotypes present in nature. | 2115976 | Ames 35667 |
| 164 | W6 58576 | MARSB-240 | Pityopsis falcata (Pursh) Nutt. | New York, United States | W6 | | | 2021 | | | | | | | Wild material | Yellow flowers, thin sickle-shaped leaves | 2113506 | W6 58576 |
| 165 | NA 88223 | CA190B-151 | Ceanothus cuneatus (Hook.) Nutt. var. rigidus (Nutt.) Hoover | California, United States | NA | | | 2020 | | | | | | | Wild material | Ceanothus 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. | 2110333 | NA 88223 |
| 166 | NA 87611 | ZARKS-030 | Rhododendron prinophyllum (Small) Millais | Arkansas, United States | NA | | | 2020 | COLLECTED | 10/05/2014 | King's River Falls Natural Area; King's River, downstream of junction of county roads 3415 and 3500 along trail leading from parking area and trail sign. | 35.90106000, -93.57456000 | 514 | Mesic, mixed deciduous forest; growing on ledge along river, in rocky soil. | Wild material | See NA 84645 for material received from the Arnold Arboretum in 2017. | 2115796 | NA 87611 |
| 167 | Ames 35541 | NAO/MB/2020/01/53 | Monarda bradburiana L. C. Beck | Illinois, United States | NC7 |  | | 2020 | COLLECTED | 07/16/2020 | Eagle Point Bay area located at southwest portion of Lake of Egypt, T11S R2E NE1/4 Sec. 1 and T11S R2E NW1/4 Sec. 6, Johnson County | 37.59183900, -88.93008100 | 168 | Roadside, wooded rocky hillside. | Wild material | | 2106720 | Ames 35541 |
| 168 | NA 87036 | Site 3A/Live Oak Landing/Holmes Creek Site | Magnolia ashei Weath. | Florida, United States | NA | | | 2020 | COLLECTED | 07/15/2020 | Along Holmes Creek at Live Oak Landing. | 30.59208000, -85.83750000 | 11 | Shade to partial shade of bluffs above the creek in well-drained mesic to dry deciduous woodlands with a few broadleaved and coniferous evergreens. | Wild material | Although these were collected without any field collection number, seeds from individual trees were separated with letter identifiers that will be maintained with the qualifier (seedling) records. The relationships are as follows: 1. Maternal letter G, NA 87036-J, L, P, and T; maternal letter H, NA 87036-V; maternal letter K, NA 87036-X, Z, and H1; maternal letter N, NA 87036-H2. In addition, three seedlings' maternal letters were lost, and these will be NA 87036-H3, H4, and H5. See the following accessions for earlier collections from this same site/population, listed in our records as "Site 3A/Live Oak Landing/Holmes Creek Site": NA 81555 (2013), NA 82745 (2015), and NA 82745.01 (2019). | 2109403 | NA 87036 |
| 169 | W6 57591 | NCBG-694 | Juncus scirpoides Lam. | Virginia, United States | W6 |  | | 2019 | | | | | | | Wild material | | 2098515 | W6 57591 |
| 170 | NA 88094 | MARSB-241 | Lyonia mariana (L.) D. Don | New York, United States | NA |  | | 2019 | | | | | | | Wild material | | 2097533 | NA 88094 |
| 171 | NA 88095 | MARSB-256 | Ilex verticillata (L.) A. Gray | New York, United States | NA |  | | 2019 | COLLECTED | 10/07/2015 | In Sag Harbor, NY, park in Mashashimuet Park. Walk along the Long Pond Greenbelt Trail. The population is along the edges of Long Pond and Crooked Pond, the first and third ponds on the left, respectively. | 40.96283000, -72.29366000 | 5 | Central shrub & herb depression pond. | Wild material | | 2097543 | NA 88095 |
| 172 | NA 88099 | MARSB-295 | Lyonia mariana (L.) D. Don | New Jersey, United States | NA |  | | 2019 | | | | | | | Wild material | | 2097562 | NA 88099 |
| 173 | NA 88107 | MARSB-421 | Chamaecyparis thyoides (L.) Britton et al. | New Jersey, United States | NA |  | | 2019 | | | | | | | Wild material | | 2097624 | NA 88107 |
| 174 | NA 88108 | MARSB-422 | Clethra alnifolia L. | New Jersey, United States | NA |  | | 2019 | | | | | | | Wild material | | 2097625 | NA 88108 |
| 175 | NA 88435 | MARSB-255 | Rosa palustris Marshall | New York, United States | NA |  | | 2019 | | | | | | | Wild material | | 2097542 | NA 88435 |
| 176 | OPGC 7884 | MARSB-259 | Rhexia virginica L. | New York, United States | OPGC |  | | 2019 | | | | | | | Wild material | | 2097546 | OPGC 7884 |
| 177 | WLP 1686 | APS/RS/2019/067/396 | Rosa setigera Michx. | Arkansas, United States | NA |  | | 2019 | COLLECTED | 11/07/2019 | Located near intersection of Smith Mountain Road and Newton County 8828 Road approximately 6.00 miles north of Deer, Newton County | 35.91212000, -93.21112000 | 636 | Roadside, upland with rocky soils | Wild material | | 2097789 | WLP 1686 |
| 178 | OPGC 7855 | CBG-9538 | Eutrochium purpureum (L.) E. E. Lamont | Illinois, United States | OPGC |  | | 2019 | | | | | | | Wild material | | 2092807 | OPGC 7855 |
| 179 | W6 56710 | CBG-9540 | Scrophularia marilandica L. | Illinois, United States | W6 |  | | 2019 | | | | | | | Wild material | | 2092809 | W6 56710 |
| 180 | W6 53346 | CA930A-596 | Descurainia pinnata (Walter) Britton subsp. glabra (Wooton & Standl.) Detling | California, United States | W6 | | | 2018 | | | | | | | Wild material | | 1958081 | W6 53346 |
| 181 | Ames 34024 | Ames 34024 | Monarda fistulosa L. | New Mexico, United States | NC7 |  | | 2017 | COLLECTED | 09/19/2017 | North of Cherry Creek Campground in the Gila National Forest along highway NM-15 (west side of road), T16S R13W Sec. 17, Grant County. | 32.91992700, -108.21901900 | 2105 | Roadside. Mixed habitat including woody and herbaceous vegetation. | Wild material | | 1953996 | Ames 34024 |
| 182 | Ames 34007 | JDC/PP/2017/052/806 | Pinus ponderosa P. Lawson & C. Lawson | Nebraska, United States | NC7 |  | | 2017 | COLLECTED | 08/29/2017 | Areas on both north and south sides of the Niobrara River between Long Pine and Springview, T32N R21W; T32N R20W; and T31N R21W in Brown and Keya Paha Counties. | 42.75716800, -99.74657300 | 685 | Dry, rocky ridgetops. | Wild material | Genetics represent the extreme eastern edgeo of the species native range. | 1953921 | Ames 34007 |
| 183 | WLP 2602 | JDC/TA/2017/053/807 | Tilia americana L. | Nebraska, United States | NA |  | | 2017 | COLLECTED | 08/29/2017 | Niobrara River Valley just 25.9 miles east, southeast of Valentine, T33N R23W Sec. 32 and Sec. 33. | 42.78284200, -100.05716700 | 658 | Floodplain and also base of adjacent bluffs/slopes (north-facing). | Wild material | Genetics represent the extreme western edge of the species native range. | 1953922 | WLP 2602 |
| 184 | Ames 34015 | Ames 34015 | Cornus rugosa Lam. | Minnesota, United States | NC7 | | | 2017 | COLLECTED | 08/23/2017 | Smoky Hills State Forest between Snellman and Osage, T139N R37W Sec. 2, 9, 11, and 14 and also T140N R37W Sec. 26 and 34. | 46.89278300, -95.35163300 | 501 | Mixed pine and deciduous moist woods. | Wild material | | 1953929 | Ames 34015 |
| 185 | NA 84645 | ZARKS-030 | Rhododendron prinophyllum (Small) Millais | Arkansas, United States | NA | | | 2017 | COLLECTED | 10/05/2014 | King's River Falls Natural Area; King's River, downstream of junction of county roads 3415 and 3500 along trail leading from parking area and trail sign. | 35.90106000, -93.57456000 | 514 | Mesic, mixed deciduous forest; growing on ledge along river, in rocky soil. | Wild material | See NA 87611 for plants of the same collection received from Morris Arboretum in 2020. | 2108758 | NA 84645 |
| 186 | Ames 33918 | APS/GD/2017/008/267 | Gymnocladus dioicus (L.) K. Koch | Minnesota, United States | NC7 |  | | 2017 | COLLECTED | 03/16/2017 | Minnesota River watershed covering approximately 9.0 river miles between Redwood Falls and Vicksburg Park, Renville County | 44.61447700, -95.14878600 | 254 | Mixed habitats, both upland dry sites, wet sites, and rocky sites. | Wild material | | 1946985 | Ames 33918 |
| 187 | WLP 1437 | NA 84027 | Oxydendrum arboreum (L.) DC. | Florida, United States | NA | | | 2016 | COLLECTED | 11/11/2016 | Woodlands associated with Miller Bayou, south of housing subdivision off of Pearl Court. | 30.46413000, -86.92804000 | 2 | Full sun to partial shade in mixed coniferous/broadleaved evergreen woodlands, with a mixture of deciduous plants in highly acidic sandy soils approximately 100-300 ft. from the salt marsh edge associated with Miller Bayou. | | | 1950372 | WLP 1437 |
| 188 | Ames 33229 | JDC/SO/2016/001/716 | Symphoricarpos orbiculatus Moench | Missouri, United States | NC7 | | | 2016 | COLLECTED | 01/13/2016 | Access road near Scobee Lake, NE 1/4 of NE 1/4 of Section 32, T64N R16W, approximately 10.5 miles northwest of Kirksville, Adair County. | 40.30655000, -92.71615200 | | | Wild material | Plants approximately 4 feet in height. Fruits red in color. Variation noted in fruits ranging from bright red to dark red in color. | 1936479 | Ames 33229 |
| 189 | NA 82746 | Site 3B/Hightower Road at Holmes Creek | Magnolia ashei Weath. | Florida, United States | NA | | | 2015 | COLLECTED | 07/31/2015 | Along Holmes Creek 0.2 miles west-southwest of Hard Castle Landing boat ramp at hte end of Hightower Road. | 30.60401000, -85.76883000 | 11 | Shade to partial shade of deciduous woodlands 10 to 15 feet above the creek, surrounded by low lying swampy area. | Wild material | Originally just called Site 3, but the "A/B" has been added to distinguish the Live Oak Landing (3A) and Hightower Road (3B) material. For previous collections of this population, see NA 81556 (2013); for later collection, see NA 82746.01 (2019). | 1950860 | NA 82746 |
| 190 | WLP 1098 | JDC/CO/2015/030/686 | Cotinus obovatus Raf. | Arkansas, United States | NA |  | | 2015 | COLLECTED | 05/20/2015 | T18N R15W NW 1/4 Sec. 15 and SE 1/4 Sec. 10 Marion County. Hall Mountain area along County Road 6074. | 36.20574400, -92.56150900 | 239 | Rocky, very shallow soils. Growing in association with Quercus muehlenbergii, Juniperus virginiana, Acer saccharum, Cercis canadensis, Lindera benzoin, Diospyros virginiana, Silphium terebinthinaceum, Baptisia sp., Rudbeckia sp., and Rhus glabra. | Wild material | | 1926260 | WLP 1098 |
| 191 | NA 82643 | NA 82643 | Lonicera sempervirens L. | Texas, United States | NA | | | 2015 | COLLECTED | 07/20/2014 | East side of Texas Route 87 approximately 0.52 miles south of Trout Creek, Texas. | 30.61156000, -93.80506000 | 21 | Southwest-facing edge of mature woodland in part to full sun; well-drained, seasonally moist soils that are sandy loam; surface has an excellent organic litter layer. | | | 1952603 | NA 82643 |
| 192 | NA 83068 | NA 83068 | Philadelphus pubescens Loisel. | Arkansas, United States | NA | | | 2015 | COLLECTED | 10/06/2014 | Mount Magazine State Park; Brown's Spring Picnic Area trail. | 36.16768000, -93.66583000 | 796 | Moist bluff line community, growing in moist organic soil layer over rocks. | | | 1952927 | NA 83068 |
| 193 | Ames 32849 | JDC/DL/2014/151/654 | Diervilla lonicera Mill. | Iowa, United States | NC7 | | | 2014 | COLLECTED | 11/23/2014 | Fern Cliff County Park located approximatley 3.75 miles west, southwest of Crawfordsville, T74N R7W southern edge of N 1/2 Sec. 24 | 41.19958700, -91.60874700 | 208 | Steep north-facing slopes on loose soils. | Wild material | | 1921870 | Ames 32849 |
| 194 | WLP 1253 | JDC/HQ/2014/090/592 | Hydrangea quercifolia W. Bartram | Alabama, United States | NA |  | | 2014 | COLLECTED | 09/23/2014 | Alabama: Lawrence County; Near Franklin and Lawrence County line off County Road 303. | 34.33701600, -87.52906200 | 332 | Growing in association with Quercus alba, Quercus montana, Cornus florida, Rhus glabra, Liriodendron tulipifera, Pinus virginiana, Pinus sp., Acer rubrum, and Frangula alnus. | Wild material | Some specimens with infructescences averaging 12" in length. | 1922364 | WLP 1253 |
| 195 | Ames 32800 | JDC/RC/2014/085/587 | Rhus copallinum L. | Mississippi, United States | NC7 | | | 2014 | COLLECTED | 09/22/2014 | Near J.P. Coleman State Park, T1S, R10E NW 1/4 of NW 1/4 of NW 1/4 of Sec. 24, extreme northeast corner of Tishomingo County | 34.98550900, -88.20415100 | 196 | Dry, pine-post oak woods | Wild material | | 1921811 | Ames 32800 |
| 196 | Ames 32223 | APS/GD/2014/002/133 | Gymnocladus dioicus (L.) K. Koch | Illinois, United States | NC7 | | | 2014 | COLLECTED | 03/20/2014 | Vermilion River watershed, N 1/2 of Section 11, T21N, R13W, just southeast of Potomac, Vermilion County. | 40.29257800, -87.78582500 | 202 | Floodplain. | Wild material | | 1917827 | Ames 32223 |
| 197 | NA 81603 | (seedling of pink form) | Rhododendron austrinum (Small) Rehder | Florida, United States | NA | | | 2013 | COLLECTED | 2013 | On the Escambia river near the mouth of the Yellow River. [GPS coordinates are actually at the confluence of the White River, the Little Simpson River, and the Buzzard Lake River (and gas line canal). -SBL] | 30.59699000, -87.22295000 | | Plants were collected along along the sandy berms along river delta. | | | 1950972 | NA 81603 |
| 198 | Ames 31987 | APS/GD/2013/011/096 | Gymnocladus dioicus (L.) K. Koch | Kansas, United States | NC7 |  | | 2013 | COLLECTED | 02/20/2013 | Camp Wood, near Cottonwood River, south of Elmdale, NW 1/4 of Section 3, T20S R7E, Chase County. | 38.34698100, -96.65080500 | 377 | Samples obtained from both upland, rocky and floodplain habitat. | Wild material | | 1907540 | Ames 31987 |
| 199 | Ames 31989 | APS/GD/2009/001/010 | Gymnocladus dioicus (L.) K. Koch | Kansas, United States | NC7 |  | | 2013 | COLLECTED | 02/21/2013 | Clinton State Park, west of Lawrence, Section 12, T13S R18E, Douglas County. | 38.93730038, -95.36213950 | 282 | Fairly dry, upland site. Majority of specimens found on upland areas. | Wild material | | 1907542 | Ames 31989 |
| 200 | Ames 31990 | APS/GD/2013/013/098 | Gymnocladus dioicus (L.) K. Koch | Missouri, United States | NC7 |  | | 2013 | COLLECTED | 02/22/2013 | Peavine Creek, south of Concordia, SW 1/4 of SE 1/4 of Section 20, SW 1/4 of NW 1/4 of Section 21, and NE 1/4 of NW 1/4 of Section 28, T48N R24W, Lafayette and Johnson Counties. | 38.93429000, -93.57204500 | 205 | Floodplain. | Wild material | | 1907543 | Ames 31990 |
| 201 | Ames 31520 | JDC/FQ/2012/029/422 | Fraxinus quadrangulata Michx. | Illinois, United States | NC7 |  | | 2012 | COLLECTED | 07/21/2012 | Funks Grove Nature Preserve, Section 17, T22N, R1E, McLean Quad, just southwest of Bloomington | 40.35954400, -89.12965500 | 229 | Mature, moist woods. Very flat terrain. | Wild material | Quite large, averaging 3-4 feet d.b.h. and 100-130 feet in height. | 1903747 | Ames 31520 |
| 202 | Ames 31521 | JDC/FQ/2012/030/423 | Fraxinus quadrangulata Michx. | Illinois, United States | NC7 |  | | 2012 | COLLECTED | 07/21/2012 | Trelease and Brownfield Woods, SE 1/4 of Section 34, T20N, R9E, and SW 1/4 of Section 1, T19N, R9E, Thomasboro Quad, near Urbana, Champaign County. | 40.14687500, -88.16305800 | 229 | Mature, moist woods. Very flat terrain. | Wild material | Relatively large, averaging 1-2 feet d.b.h. and 80-100 feet in height. | 1903748 | Ames 31521 |
| 203 | Ames 31527 | JDC/FQ/2012/036/429 | Fraxinus quadrangulata Michx. | Indiana, United States | NC7 |  | | 2012 | COLLECTED | 07/24/2012 | Versailles State Park, S 1/2 of Section 7, T7N, R12E, Milan Quad, near Versailles, Ripley County. | 39.07495100, -85.23553200 | 280 | Mature forest near southwestern portion of park. Shallow soils. West-facing slope. | Wild material | Fairly large, averaging 3 feet d.b.h. and 100 feet in height. | 1903754 | Ames 31527 |
| 204 | Ames 31529 | JDC/FQ/2012/038/431 | Fraxinus quadrangulata Michx. | Indiana, United States | NC7 |  | | 2012 | COLLECTED | 07/24/2012 | Lick Creek Summit Nature Preserve, NW 1/4 of Section 23, T13N, R2W, Richmond Quad, near Richmond, Wayne County. | 39.78453000, -84.95276400 | 267 | Dry woods. Bluffs. Shallow soils. | Wild material | | 1903756 | Ames 31529 |
| 205 | W6 43740 | NYCPDR-BBG-096 | Avenella flexuosa (L.) Parl. | New York, United States | W6 |  | | 2012 | | | | | | | Wild material | | 1900131 | W6 43740 |
| 206 | Ames 30599 | JDC/FA/2010/031/301 | Fraxinus americana L. | Kansas, United States | NC7 |  | | 2010 | COLLECTED | 09/13/2010 | Near Big Sugar Creek watershed, east of Centerville, Linn County. | 38.21145000, -94.93801000 | 294 | Upland areas. Variable aspects. | Wild material | | 1848894 | Ames 30599 |
| 207 | Ames 30589 | JDC/FQ/2010/025/295 | Fraxinus quadrangulata Michx. | Illinois, United States | NC7 |  | | 2010 | COLLECTED | 09/06/2010 | Along Burton Creek, middle of Section 27, Marblehead Quad, Adams County. | 39.86690000, -91.31220000 | 174 | Along very steep (90%) south facing slope. | Wild material | Approximately 8 inches d.b.h. | 1847246 | Ames 30589 |
| 208 | Ames 30541 | UC 105 | Aronia arbutifolia (L.) Pers. | North Carolina, United States | NC7 |  | | 2010 | COLLECTED | 10/21/2009 | Near West End, Moore County | 35.25260000, -79.49096700 | 149 | Powerline easement. Mixed hardwood woods. Sandy soil overlaying a moist seep. | Wild material | Received as plants grown from seed collected from native/wild population. Accession is extremely vigorous with an upright growth habit. Low fruit/seed production in cultivation in central Iowa. | 1843095 | Ames 30541 |
| 209 | Ames 30542 | UC 106 | Aronia arbutifolia (L.) Pers. | North Carolina, United States | NC7 |  | | 2010 | COLLECTED | 10/21/2009 | Near Hoffman Road, Jackson Springs | 35.21046700, -79.57120000 | 140 | Re-established longleaf pine ecosystem. Sandy soil overlaying moist seeps. | Wild material | Received as plants grown from seed collected from native/wild population. Accession is extremely vigorous and uniform displaying a very prostrate growth habit. Foliage is dense with leaves that are larger than the average A. arbutifolia. | 1843096 | Ames 30542 |
| 210 | Ames 32070 | UC 105 | Aronia arbutifolia (L.) Pers. | North Carolina, United States | NC7 |  | | 2010 | COLLECTED | 10/21/2009 | Near West End, Moore County | 35.25260000, -79.49096700 | 149 | Powerline easement. Mixed hardwood woods. Sandy soil overlaying a moist seep. | Wild material | Separated from Ames 30541 due to its extremely tight, upright growth habit. This new accession will be maintained as a uniform accession. | 1912823 | Ames 32070 |
| 211 | Ames 32072 | UC 106 | Aronia arbutifolia (L.) Pers. | North Carolina, United States | NC7 |  | | 2010 | COLLECTED | 10/21/2009 | Near Hoffman Road, Jackson Springs | 35.21046700, -79.57120000 | 140 | Re-established longleaf pine ecosystem. Sandy soil overlaying moist seeps. | Wild material | Separated from Ames 30542 due to open, spreading growth habit. This accession will be maintained as a uniform accession. | 1912825 | Ames 32072 |
| 212 | Ames 30481 | APS/GD/2010/001/036 | Gymnocladus dioicus (L.) K. Koch | Missouri, United States | NC7 |  | | 2010 | COLLECTED | 02/17/2010 | Mark Twain Lake Project (Army Corp of Engineers), Mark Twain Lake, T54N R8W SE 1/4 of NW 1/4 of Section 2 and west 1/2 of Sec. 11, Florida Quad, Monroe County. | 39.49270000, -91.76510000 | 199 | Northwest-facing bluff; woods. | Wild material | #106 measured 14.5" d.b.h and 70-80'; #107 measured 9.5" and 70-80'; #108 measured 11" d.b.h. and 60-70'; #109 measured 9.5" d.b.h. and 40-50'; #110 measured 11" d.b.h. at 30-40'; and #111 measured 6" d.b.h. and 30'. | 1831340 | Ames 30481 |
| 213 | Ames 30482 | APS/GD/2010/002/037 | Gymnocladus dioicus (L.) K. Koch | Missouri, United States | NC7 |  | | 2010 | COLLECTED | 02/17/2010 | Lake of the Ozarks, Grandglaize Creek Watershed, T39N R15W NW 1/4 Sec. 36 and NE 1/4 of SE 1/4 Sec. 35, Toronto Quad, Miller County. | 38.07386700, -92.52686700 | 207 | Mixed deciduous woods. | Wild material | | 1831341 | Ames 30482 |
| 214 | Ames 30488 | APS/GD/2010/009/044 | Gymnocladus dioicus (L.) K. Koch | Kentucky, United States | NC7 |  | | 2010 | COLLECTED | 02/21/2010 | Alum Hill and Big Slough Creek, near Hites Falls, Grayson County. | 37.53600000, -86.59630000 | 159 | Floodplain of Big Slough and base of bluffs on northeast-facing slope of Alum Hill. | Wild material | #140 measured 12" d.b.h. at 70', #141 measured 8.5" d.b.h. and 40', #142 measured 12" and 80', #143 measured 9.5" and 60', #144 measured 7.5" d.b.h. and 40', #145 measured 12" d.b.h. and 40', #146 measured 7.3" d.b.h. and 50', and #147 measured 14.25" d.b.h. and 75'. | 1831347 | Ames 30488 |
| 215 | Ames 30489 | APS/GD/2010/010/045 | Gymnocladus dioicus (L.) K. Koch | Kentucky, United States | NC7 |  | | 2010 | COLLECTED | 02/22/2010 | Yellowbank Wildlife Management Area, near Lick Run Creek, on Ammons Church Road and slope on Jays Lane, north of Ammons, Breckinridge County. | 37.96060000, -86.49880000 | 130 | Northeast-facing slope. | Wild material | #148 measured 16.5" d.b.h. and 100', #149 measured 14.5" d.b.h. and 90', #150 measured 16" d.b.h. and 90', and #151 measured 18" d.b.h. and 80'. | 1831348 | Ames 30489 |
| 216 | Ames 30133 | JDC/CD/2009/063/213 | Cornus drummondii C. A. Mey. | Illinois, United States | NC7 |  | | 2009 | COLLECTED | 09/25/2009 | Four Corners Road, north from Illinois Highway 84, NW 1/4 of SW 1/4 of Section 36, T26N, R2E, Blackhawk (IL-IA) Quad, Jo Daviess County. | 42.20027778, -90.22944444 | 194 | Roadside in fence row. | Wild material | | 1819714 | Ames 30133 |
| 217 | Ames 30153 | JDC/FP/2009/062/212 | Fraxinus pennsylvanica Marshall | Illinois, United States | NC7 |  | | 2009 | COLLECTED | 09/25/2009 | Four Corners Road, north from Illinois Highway 84, NW 1/4 of SW 1/4 of Section 36, T26N, R2E, Blackhawk (IL-IA) Quad, Jo Daviess County. | 42.20027778, -90.22944444 | 194 | Roadside in fence row. | Wild material | | 1819734 | Ames 30153 |
| 218 | Ames 29974 | JDC/GD/2009/003/153 | Gymnocladus dioicus (L.) K. Koch | Iowa, United States | NC7 |  | | 2009 | COLLECTED | 03/19/2009 | Stone State Park, just northwest of Sioux City, T89N R48W west 1/2 of Sec. 1 and east 1/2 of Sec. 2 Sioux City Quad., extreme northwest corner of Woodbury County. | 42.55805556, -96.46861111 | 390 | Variable-wet bottomland and dry slopes; a few small creeks with running water. Variable exposure. 0-45 degrees of slope with southern and eastern aspects. | Wild material | Plants between 40 and 65 feet in height and 6 to 17 inches DBH. | 1798766 | Ames 29974 |
| 219 | Ames 29628 | JDC/FA/2008/029/099 | Fraxinus americana L. | Missouri, United States | NC7 |  | | 2008 | COLLECTED | 10/06/2008 | Rudolf Bennitt Conservation Area, NE 1/4 of NE 1/4 of Section 25, T52N, R14W, Renick Quad, Randolph County. | 39.27527778, -92.43388889 | 256 | | Wild material | Original specimens ranged from 6-10 inches d.b.h. and 30-50 feet in height. Reddish-orange fall color more apparent in males. | 1788183 | Ames 29628 |
| 220 | Ames 29227 | JDC-0452007 | Rhus copallinum L. | Missouri, United States | NC7 |  | | 2007 | COLLECTED | 10/04/2007 | Along trail to Mina Sauk Falls, Taum Sauk Mountain State Park, Iron County | 37.57250000, -90.72805556 | 541 | Very dry, rocky soil. Very close to the highest elevation in Missouri | Wild material | Reddish fall color. | 1743330 | Ames 29227 |
| 221 | WLP 2487 | JDC-0112006 | Viburnum prunifolium L. | Iowa, United States | NA |  | | 2006 | COLLECTED | 09/12/2006 | Lake of Three Fires State Park, Bedford Quad.T68N R33W extreme NW corner of Sec. 7 | 40.71194444, -94.68583333 | 360 | Moderately shaded deciduous woods. | Wild material | Noted in nature as small understory trees, approximately 15-20 feet in height with clean foliage under moderate to heavy shade. In cultivation, fall color seems to vary from year to year ranging from dark purplish to bright red with peak fall color occurring around the later part of October (central Iowa). Flowers are white with peak flowering occurring in early-mid May. The range of this North American native is noted throughout the eastern and southeastern U.S. This accession represents genetics from the extreme northwestern corner of the species native range. Viburnum prunifolium in Iowa is rather rare and generally restricted and more commonly found in the extreme southeast corner of the state. This disjunct population in Taylor County (southwest Iowa) has been questioned as to whether it is a true native population or a naturalized escape. Additional V. prunifolium elsewhere in southwest Iowa has not been reported/documented. Immediately to the south of Taylor County, V. prunifolium is documented throughout most of Missouri and thus it is suspected that these genetics do represent a true native population. | 1708694 | WLP 2487 |