| 0 | NA 89173 | 2025RJLSEUS-14 | Chionanthus sp. | Florida, United States | NA | | | 2026 | COLLECTED | 10/03/2025 | Choctawhatchee National Forest: the collection site is reached by foot (~0.5 km) along a loose sand road/firebreak from Martin Luther King, Jr. Boulevard, just east of the boundary for Hurlburt Field in Hurlburt Field/Ft. Walton Beach, FL. Collected from 30 deg. 26.859', -86 deg. 39.577' to 30 deg. 27.137', -86 deg. 39.580'; latitude and longitude of record calculated at the midpoint of these coordinates. | 30.44996000, -86.65965000 | 10 | Dry to xeric conditions of well-drained, deep sandy soils on a relatively level area bordering a powerline in an open mixed mostly mixed evergreen and deciduous, somewhat disturbed habitat in sun to part shade. In areas “broadleaved scrub” vegetation is so dense, that it is almost impenetrable. Elevation: 9 to 11 meters. Slope: 0 to 3 percent. Aspect: Variable. Soil: The soils of this area are characterized as Foxworth Series (95 percent) sand, 0 to 5 percent slopes (8). Other soil series interbedded with the Foxworth Series, vary in percentages from 1-4 percent including Lakeland and Chipley. The Foxworth Series consists of very deep, moderately well to somewhat excessively drained, rapid to very rapid permeable soils on broad uplands and side slopes. They formed in sandy marine or eolian sediments in the Southern Coastal Plain (MLRA 133A), The Eastern Gulf Coast Flatwoods (MLRA 152A), The Atlantic Coast Flatwoods (153A) and the Tidewater Area (153B). Thickness of the grayish brown to light yellowish-brown sand exceeds 2 meters. Reaction ranges from very strongly acid to slightly acid throughout. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). Geology: The underlying geology of this area is characterized as undifferentiated Quaternary Sediments. Much of Florida's surface is covered by a varying thickness of undifferentiated sediments consisting of siliciclastics, organics and freshwater carbonates. Where these sediments exceed 6.1 meters thick, they were mapped as discrete units. To subdivide the undifferentiated sediments, those sediments occurring in flood plains were mapped as alluvial and flood plain deposits (Qal). Sediments showing surficial expression of beach ridges and dunes were mapped separately (Qbd) as were the sediments composing Trail Ridge (Qtr). Terrace sands were not mapped (refer to Healy [1975] for a discussion of the terraces in Florida). The subdivisions of the Undifferentiated Quaternary Sediments (Qu) are not lithostratigraphic units but are utilized to facilitate a better understanding of the State's geology. The siliciclastics are light gray, tan, brown to black, unconsolidated to poorly consolidated, clean to clayey, silty, unfossiliferous, variably organic-bearing sands to blue green to olive green, poorly to moderately consolidated, sandy, silty clays. Gravel is occasionally present in the panhandle. Organics occur as plant debris, roots, disseminated organic matrix and beds of peat. Freshwater carbonates, often referred to as marls in the literature, are scattered over much of the State. In southern Florida, freshwater carbonates are nearly ubiquitous in the Everglades. These sediments are buff colored to tan, unconsolidated to poorly consolidated, fossiliferous carbonate muds. Sand, silt and clay may be present in limited quantities. These carbonates often contain organics. The dominant fossils in the freshwater carbonates are mollusks. (Source: USGS Florida Geologic Map Data). | Wild material | Received as C. cf. henryae | 2193307 | NA 89173 |
| 1 | NA 89159 | 2025RJLSEUS-07 | Persea borbonia (L.) Spreng. | Florida, United States | NA | | | 2025 | COLLECTED | 10/02/2025 | Eglin Air Force Base: Plants are found on a coastal dune ridge and surrounding xeric habitats on Eglin AFB behind businesses located along Florida State Highway 98. The site is accessed through a now gated and permanently closed Eglin AFB, East River Unit, A-21 Road (now open to pedestrian traffic only with a valid Eglin user permit). After walking through the gated road, the site is to the west along 4-wheeling trails. | 30.41249300, -86.77374700 | 9 | Shade to full sun in a primarily evergreen extremely dry dune community with a mixed understory of deciduous and evergreen plants. Slope: 0 to 2 percent. Aspect: Various. Soils: The soils of this are characterized as Kureb Series sand, 0 to 8 percent slopes. The Kureb series consists of very deep, excessively drained, gently sloping to moderately steep soils on Coastal Plain uplands and on side slopes along streams and bays. They have formed in marine, aeolian, or fluvial sands. Slopes range from 0 to 20 percent. The thickness of the sandy horizon is more than 2 meters. Soil reaction is neutral to extremely acid throughout. All horizons are fine sand, sand, or coarse sand. Silt plus clay content is less than 5 percent. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). Geology: The underlying geology of this area is characterized as undifferentiated Quaternary Sediments. Much of Florida's surface is covered by a varying thickness of undifferentiated sediments consisting of siliciclastics, organics and freshwater carbonates. Where these sediments exceed 6.1 meters thick, they were mapped as discrete units. To subdivide the undifferentiated sediments, those sediments occurring in flood plains were mapped as alluvial and flood plain deposits (Qal). Sediments showing surficial expression of beach ridges and dunes were mapped separately (Qbd) as were the sediments composing Trail Ridge (Qtr). Terrace sands were not mapped (refer to Healy [1975] for a discussion of the terraces in Florida). The subdivisions of the Undifferentiated Quaternary Sediments (Qu) are not lithostratigraphic units but are utilized to facilitate a better understanding of the State's geology. The siliciclastics are light gray, tan, brown to black, unconsolidated to poorly consolidated, clean to clayey, silty, unfossiliferous, variably organic-bearing sands to blue green to olive green, poorly to moderately consolidated, sandy, silty clays. Gravel is occasionally present in the panhandle. Organics occur as plant debris, roots, disseminated organic matrix and beds of peat. Freshwater carbonates, often referred to as marls in the literature, are scattered over much of the State. In southern Florida, freshwater carbonates are nearly ubiquitous in the Everglades. These sediments are buff colored to tan, unconsolidated to poorly consolidated, fossiliferous carbonate muds. Sand, silt and clay may be present in limited quantities. These carbonates often contain organics. The dominant fossils in the freshwater carbonates are mollusks. (Source: USGS Florida Geologic Map Data). | Wild material | | 2193005 | NA 89159 |
| 2 | NA 89160 | 2025RJLSEUS-08 | Ilex hybr. | Florida, United States | NA | | | 2025 | COLLECTED | 10/02/2025 | Eglin Air Force Base: coastal dune ridge on Eglin AFB behind businesses located along Florida State Highway 98. The site is accessed through a now gated and permanently closed Eglin AFB, East River Unit, A-21 Road (now open to pedestrian traffic only with a valid Eglin user permit). After walking through the gated road, the site is to the west along 4-wheeling trails. | 30.41191000, -86.77315800 | 8 | Part shade in a primarily evergreen extremely dry dune community with a mixed understory of deciduous and evergreen plants. Slope: 0 to 2 percent. Soils: The soils of this are characterized as Kureb Series sand, 0 to 8 percent slopes. The Kureb series consists of very deep, excessively drained, gently sloping to moderately steep soils on Coastal Plain uplands and on side slopes along streams and bays. They have formed in marine, aeolian, or fluvial sands. Slopes range from 0 to 20 percent. The thickness of the sandy horizon is more than 2 meters. Soil reaction is neutral to extremely acid throughout. All horizons are fine sand, sand, or coarse sand. Silt plus clay content is less than 5 percent. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). Geology: The underlying geology of this area is characterized as undifferentiated Quaternary Sediments. Much of Florida's surface is covered by a varying thickness of undifferentiated sediments consisting of siliciclastics, organics and freshwater carbonates. Where these sediments exceed 6.1 meters thick, they were mapped as discrete units. To subdivide the undifferentiated sediments, those sediments occurring in flood plains were mapped as alluvial and flood plain deposits (Qal). Sediments showing surficial expression of beach ridges and dunes were mapped separately (Qbd) as were the sediments composing Trail Ridge (Qtr). Terrace sands were not mapped (refer to Healy [1975] for a discussion of the terraces in Florida). The subdivisions of the Undifferentiated Quaternary Sediments (Qu) are not lithostratigraphic units but are utilized to facilitate a better understanding of the State's geology. The siliciclastics are light gray, tan, brown to black, unconsolidated to poorly consolidated, clean to clayey, silty, unfossiliferous, variably organic-bearing sands to blue green to olive green, poorly to moderately consolidated, sandy, silty clays. Gravel is occasionally present in the panhandle. Organics occur as plant debris, roots, disseminated organic matrix and beds of peat. Freshwater carbonates, often referred to as marls in the literature, are scattered over much of the State. In southern Florida, freshwater carbonates are nearly ubiquitous in the Everglades. These sediments are buff colored to tan, unconsolidated to poorly consolidated, fossiliferous carbonate muds. Sand, silt and clay may be present in limited quantities. These carbonates often contain organics. The dominant fossils in the freshwater carbonates are mollusks. (Source: USGS Florida Geologic Map Data). | Wild material | | 2193006 | NA 89160 |
| 3 | NA 89164 | 2025RJLSEUS-25 | Persea humilis Nash | Florida, United States | NA | | | 2025 | COLLECTED | 10/10/2025 | Hickory Lake Scrub Preserve, 1658 Scenic Highway Frostproof, FL 33843. The Hickory Lake Scrub Preserve was purchased in August 1997 from the Green Horizon Land Trust, a local nonprofit organization dedicated to preserving environmentally significant land. This property is now managed by Polk County’s Environmental Lands Program. | 27.69758800, -81.53739600 | 32 | Growing on sugar sand in full sun and extremely dry, xeric Lake Wales Ridge habitat comprised of a remarkably rich evergreen and deciduous plant community. The habitat is subjected to periodic prescribed fire (most recent estimated to be 2-3 years ago). Slope: 0 percent. Aspect: N/A. Soil: The soil of this site is characterized as St. Lucie Series fine sand, 0 to 5 percent slopes; with other minor contributions from Archbold, Myakka, and Cassia not described here. The St. Lucie Series consists of very deep, excessively drained soils that formed in sandy marine and/or eolian deposits. St. Lucie soils are on dunes, ridges, and knolls on marine terraces. Slopes range from linear to convex and range from 0 to 20 percent. This soil is strongly to extremely acid in the upper 200 cm of the horizon but can have neutral to alkaline components as well. The genesis of the St. Lucie soils is not clearly understood. No subsurface diagnostic horizons are within depths of 2 meters, but the uncoated sand grains suggest an albic horizon. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). Geology: The underlying geology of this area is characterized as Reworked Cypresshead Sediments from the Pliocene/Pleistocene. This unit is the result of post depositional reworking of the Cypresshead siliciclastics. The sediments are fine to coarse quartz sands with scattered quartz gravel and varying percentages of clay matrix that is undifferentiated. (Source: USGS Florida Geologic Map Data). | Wild material | | 2193010 | NA 89164 |
| 4 | NA 89023 | 2025RJL-001 | Persea humilis Nash | Florida, United States | NA | | | 2025 | COLLECTED | 05/09/2025 | Lake Wales Ridge Wildlife Refuge: Hiking Area, 5339 Placid View Drive, Lake Placid, FL 33852. Convenient parking and access to the area is located on east side of Placid View Drive, 1.23 kilometers north of Florida State Road 70. | 27.21871700, -81.37911000 | 37 | Growing in full sun on the upper portion of a relatively hilly sugar sand, extremely dry, xeric Lake Wales Ridge habitat comprised of a diverse evergreen and deciduous plant community. The habitat is subjected to periodic prescribed fire; the last fire seems to have been more than 4 years ago. This site is a bit more complex with intergradation xeric, dry-mesic, moist-mesic habitats on the lower portion of slopes that lead to a small stream. As a result, there is more overlap in plant species where plant communities intersect. Slope: 0 to 5 percent. Aspect: Various. Soil: The soils here, where Tamala humilis grows and thrives, are primarily Archbold Series sand, 0 to 5 percent slopes and Satellite Series sand, 0 to 2 percent slopes with occasional intrusions of St. Lucie Series sand, 0 to 8 percent slopes. The Archbold Series consists of deep, well drained, very rapidly permeable sandy soils that formed in marine or eolian deposits. These droughty soils are on low ridges in central Florida. Slopes are typically 0 to 5 percent. The soil reaction is slightly to extremely acid. The soil is sand or fine sand throughout. The silt plus clay content in the 25-100 depth is less than 2 percent; even so, they contain slightly more moisture in times of abundant rainfall. The Satellite Series consists of very deep, somewhat poorly drained, rapidly permeable soils on low knolls and ridges of the Southern Florida Flatwoods and less commonly on the South-Central Florida Ridge They formed in thick beds of marine sand. Soil reaction ranges from very strongly acid to slightly alkaline in all horizon. This soil can become saturated 25-100 cm below the surface during the summer rainy season. The St. Lucie Series consists of very deep, excessively drained soils that formed in sandy marine and/or eolian deposits. St. Lucie Series soils are on dunes, ridges, and knolls on marine terraces. Slopes range from linear to convex and range from 0 to 20 percent. This soil is strongly to extremely acid in the upper 200 cm of the horizon but can have neutral to alkaline components as well. The genesis of the St. Lucie Series soil is not clearly understood. No subsurface diagnostic horizons are within depths of 2 meters, but the uncoated sand grains suggest an albic horizon. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). Geology: The underlying geology of this area is characterized as Reworked Cypresshead Sediments from the Pliocene/Pleistocene. This unit is the result of post depositional reworking of the Cypresshead siliciclastics. The sediments are fine to coarse quartz sands with scattered quartz gravel and varying percentages of clay matrix and undifferentiated. (Source: USGS Florida Geologic Map Data). | Wild material | | 2191358 | NA 89023 |
| 5 | NA 89024 | 2025RJL-002 | Persea humilis Nash | Florida, United States | NA | | | 2025 | COLLECTED | 05/09/2025 | Hickory Lake Scrub Preserve, 1658 Scenic Highway Frostproof, FL 33843. | 27.69686700, -81.53802300 | 34 | Growing on sugar sand in full sun and extremely dry, xeric Lake Wales Ridge habitat comprised of a remarkably rich evergreen and deciduous plant community. The habitat is subjected to periodic prescribed fire (estimated to be 2-3 years ago). Slope: N/A. Aspect: N/A. Soil: The soil of this site is characterized as St. Lucie Series fine sand, 0 to 5 percent slopes; with other minor contributions from Archbold, Myakka, and Cassia not described here. The St. Lucie Series consists of very deep, excessively drained soils that formed in sandy marine and/or eolian deposits. St. Lucie soils are on dunes, ridges, and knolls on marine terraces. Slopes range from linear to convex and range from 0 to 20 percent. This soil is strongly to extremely acid in the upper 200 cm of the horizon but can have neutral to alkaline components as well. The genesis of the St. Lucie soils is not clearly understood. No subsurface diagnostic horizons are within depths of 2 meters, but the uncoated sand grains suggest an albic horizon. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). Geology: The underlying geology of this area is characterized as Reworked Cypresshead Sediments from the Pliocene/Pleistocene. This unit is the result of post depositional reworking of the Cypresshead siliciclastics. The sediments are fine to coarse quartz sands with scattered quartz gravel and varying percentages of clay matrix and undifferentiated. (Source: USGS Florida Geologic Map Data). | Wild material | | 2191359 | NA 89024 |
| 6 | NA 89025 | 2025RJL-003 | Ximenia americana L. | Florida, United States | NA | | | 2025 | COLLECTED | 05/09/2025 | Hickory Lake Scrub Preserve, 1658 Scenic Highway Frostproof, FL 33843. | 27.69744200, -81.53888700 | 32 | Growing on sugar sand in full sun and extremely dry, xeric Lake Wales Ridge habitat comprised of a remarkably rich evergreen and deciduous plant community. The habitat is subjected to prescribed fire periodically (estimated to be 2-3 years ago). Interestingly, this species was also found on dry-mesic edges of the habitat only 10-15 meters from the last, mostly in full sun, but occasionally in light shade; plants were flowering and fruiting. Slope: N/A. Aspect: N/A Soil: The soil of this site is characterized as St. Lucie Series fine sand, 0 to 5 percent slopes; with other minor contributions from Archbold, Myakka, and Cassia not described here. The St. Lucie Series consists of very deep, excessively drained soils that formed in sandy marine and/or eolian deposits. St. Lucie soils are on dunes, ridges, and knolls on marine terraces. Slopes range from linear to convex and range from 0 to 20 percent. This soil is strongly to extremely acid in the upper 200 cm of the horizon but can have neutral to alkaline components as well. The genesis of the St. Lucie soils is not clearly understood. No subsurface diagnostic horizons are within depths of 2 meters, but the uncoated sand grains suggest an albic horizon. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). Geology: The underlying geology of this area is characterized as Reworked Cypresshead Sediments from the Pliocene/Pleistocene. This unit is the result of post depositional reworking of the Cypresshead siliciclastics. The sediments are fine to coarse quartz sands with scattered quartz gravel and varying percentages of clay matrix and undifferentiated. (Source: USGS Florida Geologic Map Data). | Wild material | | 2191360 | NA 89025 |
| 7 | NA 88587 | 2024RJLFL-023 | Persea borbonia (L.) Spreng. | Florida, United States | NA | | | 2024 | COLLECTED | 11/15/2024 | Dune ridge behind businesses located along Florida State Highway 98. Site was accessed through a now pedestrian-only (gated) Eglin Air Force Base, East River Unit, A-21 Road. After walking through the gated road, the site is to the west along four-wheeling vehicle trails. | 30.41249300, -86.77374700 | 9 | Primarily evergreen, extremely dry dune community with a mixed understory of deciduous and evergreen plants in part shade to full sun. Slope: 0 to 2 percent. 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. 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 Kureb Series sand, 0 to 8 percent slopes. The Kureb series consists of very deep, excessively drained, gently sloping to moderately steep soils on Coastal Plain uplands and on side slopes along streams and bays. They have formed in marine, aeolian, or fluvial sands. Slopes range from 0 to 20 percent. The thickness of the sandy horizon is more than 2 meters. Soil reaction is neutral to extremely acid throughout. All horizons are fine sand, sand, or coarse sand. Silt plus clay content is less than 5 percent. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). | Wild material | | 2169924 | NA 88587 |
| 8 | NA 88806 | TJK2023LA/TX-006 | Vaccinium arboreum Marshall | Texas, United States | NA | | | 2023 | COLLECTED | 11/21/2023 | Interstate 20, westbound, approximately 2.2 miles west of FM (farm-to-market road) 2015 and 0.8 miles east of FM 14. | 32.45250000, -95.26960000 | 10 | Xeric shortleaf pine-post oak-blackjack oak uplands. Slope: flat. Aspect: West. Elevation: 32 feet. | Wild material | | 2159189 | NA 88806 |