| 0 | NA 88577 | 2024RJLFL-001 | Ilex myrtifolia Walter | Florida, United States | NA | | | 2024 | COLLECTED | 11/12/2024 | Yellow River Marsh Preserve State Park: collected along trail from the parking lot. The property is accessed from a parking area located on Dickerson City Road. | 30.48472300, -87.07110400 | 5 | Mostly found in moist 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 Goldhead Series consists of poorly drained and very poorly drained soils on broad areas of the flatwoods and in depressions. They formed in thick beds of stratified unconsolidated loamy and sandy marine sediments. Slopes range from 0 to 5 percent. The solum thickness ranges from 35 to greater than 60 inches. Soil reaction ranges from very strongly acid to mildly alkaline in the A and E horizons, and very strongly acid to moderately alkaline in the B and C horizons. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). | Wild material | | 2169914 | NA 88577 |
| 1 | NA 88725 | RJL2023NCSC-030 | Ilex myrtifolia Walter | North Carolina, United States | NA | | | 2023 | COLLECTED | 11/15/2023 | Boiling Spring Lakes, NC: Plants growing along unused road of potential new development on Baden Street, between Camden Street and Midwood Street. The site is accessed from North Carolina Highway 87 (George II Highway SE) by turning west onto Brunswick Road and right onto Baden Street at the first intersection. | 34.01935700, -78.06110500 | 16 | Plants growing in part-shade along the road, edges of ditches and managed edges of longleaf pine forest in well-drained, but seasonally moist habitat with very little organic litter layer. It seems that low competition and exposed sandy conditions allows this plant to thrive. 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 North Carolina Geologic Map Data.) The primary soil type in this collection area is classified as Leon Series fine sand. 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. The upper horizon (0-75 cm) is comprised of a high percent of blac and lower percentage of light gray sand that is very friable and very strongly acid. The lower horizon (75-270 cm) has a range of gray, dark brown and yellowish-brown sands that range from fine to coarse and are also very strongly acid. (Source: NRCS Web Soil Survey.) | Wild material | | 2159153 | NA 88725 |
| 2 | NA 88724 | RJL2023NCSC-029 | Kalmia buxifolia (P. J. Bergius) Gift & Kron | North Carolina, United States | NA | | | 2023 | COLLECTED | 11/15/2023 | Boiling Spring Lakes, NC: Plants growing along unused road of potential new development on Baden Street, between Camden Street and Midwood Street. The site is accessed from North Carolina Highway 87 (George II Highway SE) by turning west onto Brunswick Road and right onto Baden Street at the first intersection. | 34.01935700, -78.06110500 | 16 | Plants growing in part-shade to full sun along the road, edges of ditches and managed edges of longleaf pine forest in well-drained, but seasonally moist habitat with very little organic litter layer. It seems that low competition and exposed sandy conditions allows this plant to thrive. 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 North Carolina Geologic Map Data.) The primary soil type in this collection area is classified as Leon Series fine sand. 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. The upper horizon (0-75 cm) is comprised of a high percent of blac and lower percentage of light gray sand that is very friable and very strongly acid. The lower horizon (75-270 cm) has a range of gray, dark brown and yellowish-brown sands that range from fine to coarse and are also very strongly acid. (Source: NRCS Web Soil Survey.) | Wild material | | 2159152 | NA 88724 |
| 3 | NA 88726 | RJL2023NCSC-031 | Gordonia lasianthus (L.) J. Ellis | North Carolina, United States | NA | | | 2023 | COLLECTED | 11/15/2023 | Boiling Spring Lakes, NC: Plants growing along unused road of potential new development on Baden Street, between Camden Street and Midwood Street. The site is accessed from North Carolina Highway 87 (George II Highway SE) by turning west onto Brunswick Road and right onto Baden Street at the first intersection. Seeds were collected from plants growing along Baden Street. | 34.01909500, -78.06087300 | 15 | Plants growing in part-shade to sun along the road, edges of ditches and managed edges of longleaf pine forest in well-drained, but seasonally moist habitat with very little organic litter layer. In addition, large specimens are found in undisturbed lowland acid woodlands nearby. 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 North Carolina Geologic Map Data.) The primary soil type in this collection area is classified as Leon Series fine sand. 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. The upper horizon (0-75 cm) is comprised of a high percent of blac and lower percentage of light gray sand that is very friable and very strongly acid. The lower horizon (75-270 cm) has a range of gray, dark brown and yellowish-brown sands that range from fine to coarse and are also very strongly acid. (Source: NRCS Web Soil Survey.) | Wild material | | 2159154 | NA 88726 |