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ACCESSIONPLANT NAMETAXONOMYORIGINGENEBANKIMAGEAVAILABILITYRECEIVEDSOURCE TYPESOURCE DATECOLLECTION SITECOORDINATESELEVATIONHABITATIMPROVEMENT LEVELNARRATIVE
0PI 702712NCBG-287Panicum virgatum L. Virginia, United StatesS9SEED2019Wild material2098394PI 702712
1PI 710478NCBG-750Chamaecrista fasciculata (Michx.) Greene Virginia, United StatesS9SEED2018Wild material1966043PI 710478
2PI 710479NCBG-647Chamaecrista nictitans (L.) Moench Virginia, United StatesS9SEED2018Wild material1966000PI 710479
3NA 88982TXWL2025-032Ilex opaca Aiton Texas, United StatesNA2025COLLECTED01/07/2025South of Jericho community.31.66973000, -94.25613000Western sandy lands; edge of small grove of Ilex opaca with sun exposure in upland position above a baygall. Bare ground cover with Ilex opaca regeneration. Adjacent to a new longleaf pine plantation located on fireline.Wild material2170966NA 88982
4NA 885812024RJLFL-012Ilex ambigua Torr. Florida, United StatesNA2024COLLECTED11/13/2024Woodland edge along the south side of Bud Bass Road (DOF B48), 0.30 kilometers east of the junction with Norman Riley Road.30.75763200, -86.8018430032Woodland 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 material2169918NA 88581
5NA 890932024RM-TK-006Ilex ambigua Torr. Florida, United StatesNA2024COLLECTED09/29/2024Blackwater 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, -86.8018722029This 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 material2169057NA 89093
6WLP 3275TJK2023FL-023Morella cerifera (L.) Small Florida, United StatesNA2023COLLECTED10/20/2023Santa Rosa Island: White Sands Blvd, Navarre Beach at Santa Rosa Sound, soundside.30.37880000, -86.897700002Woody transition belt between sound-side marsh vegetation and fore dune vegetation. Plants experience saltwater intrusion. Slope: 7%. Aspect: Northwest. Elevation: 5 feet.Wild material2159055WLP 3275
7Ames 35688NCBG-553Monarda punctata L. North Carolina, United StatesNC7SEED2019Wild material2098470Ames 35688
8OPGC 6611NCBG-500Hibiscus moscheutos L. North Carolina, United StatesOPGCSEED2018Wild materialHibiscus moscheutos1965965OPGC 6611
9W6 54726NCBG-464Schoenoplectus pungens (Vahl) Palla Virginia, United StatesW6SEED2018Wild materialSchoenoplectus pungens1965952W6 54726
10W6 54770NCBG-630Trichostema dichotomum L. North Carolina, United StatesW6SEED2018Wild materialTrichostema dichotomum1965996W6 54770
11W6 54819NCBG-757Eragrostis hirsuta (Michx.) Nees North Carolina, United StatesW6SEED2018Wild materialEragrostis hirsuta1966045W6 54819