| 0 | 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 |
| 1 | NA 87844 | TRX241118-02GA | Ilex cassine L. | Georgia, United States | NA | | | 2024 | COLLECTED | 11/18/2024 | St. Simons Island: Frederica Park. | 31.23766000, -81.35638000 | 6 | | Wild material | | 2169897 | NA 87844 |
| 2 | WLP 3411 | TJK2023FL-044 | Cyrilla racemiflora L. | Florida, United States | NA |  | | 2024 | COLLECTED | 12/26/2023 | Forest Hill Cemetery, east fence line, 0.4 mi north of Hwy 98, off Twine Rd. | 29.78030000, -85.27160000 | 7 | Growing on the edge of a wet pine savanna/flatwood. Slope: flat. Aspect: Southeast. Elevation: 23 feet. | Wild material | | 2165704 | WLP 3411 |
| 3 | WLP 3412 | TJK2023FL-045 | Lyonia lucida (Lam.) K. Koch | Florida, United States | NA | | | 2024 | COLLECTED | 12/26/2023 | East backwoods adjacent to Forest Hill Cemetery, 0.4 mi north of Hwy 98, off Twine Rd. | 29.78030000, -85.27160000 | 7 | Edge of a wet pine savanna/flatwood. Slope: flat. Aspect: Southeast. Elevation: 23 feet. | Wild material | | 2165705 | WLP 3412 |
| 4 | 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 |