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ACCESSIONPLANT NAMETAXONOMYORIGINGENEBANKIMAGEAVAILABILITYRECEIVEDSOURCE TYPESOURCE DATECOLLECTION SITECOORDINATESELEVATIONHABITATIMPROVEMENT LEVELNARRATIVE
0MIA 25211Serenoa repens (W. Bartram) Small Florida, United StatesMIAPlant1978COLLECTEDWild materialE2-2 in front of Building 11091101MIA 25211
1PI 691215V. arboreum GN2018 Manatee Springs State Park1Vaccinium arboreum Marshall Florida, United StatesCOR2019COLLECTED12/06/2018Manatee Springs State Park29.49358600, -82.9733690023NNW exposure/aspect. Next to driving road by gate to the north trail.Vegetation nearby included; Crowngrass (Paspalum spp.), water oak (Quercus nigra), saw palmetto (Serenoa repens), longleaf pine (Pinus palustris), slash pine (pinus elliottii). Wild materialGerardo Nunez USDA plant collecting trip to Florida 2018, 20192094707PI 691215
2PI 691216V. arboreum GN2018 Manatee Springs State Park 2Vaccinium arboreum Marshall Florida, United StatesCOR2019COLLECTED12/06/2018Manatee Springs State Park29.49414000, -82.9734740019200 m past north trail gate. Evidence of recent fire. Fallen trees around. Flood prone area. Not flooded at the time of collection. Vegetation nearby included; Water oak (Quercus nigra), saw palmetto (Serenoa repens), dollarweed (Hydrocotyle spp.), crowngrass (Paspalum spp.), bald cypress (Taxodium distichum). Native soil pH = 5.41. NNW exposure/aspect. Wild materialGerardo Nunez USDA plant collecting trip to Florida 2018, 20192094708PI 691216
3PI 691217V. arboreum GN2018 Manatee Springs State Park 4Vaccinium arboreum Marshall Florida, United StatesCOR2019COLLECTED12/06/2018Manatee Springs State Park29.49653600, -82.9759570013Partially Shaded area. Side of the trail. North Exposure/aspect. Nearby vegetation included; Saw palmetto (Serenoa repens), bald cypress (Taxodium distichum). Native soil pH = 5.52Wild materialGerardo Nunez USDA plant collecting trip to Florida 2018, 20192094709PI 691217
4PI 691218V. arboreum GN2018 Manatee Springs State Park 6Vaccinium arboreum Marshall Florida, United StatesCOR2019COLLECTED12/06/2018Manatee Springs State Park29.49854500, -82.9745830018Partial sun. Side of the road. Broadleaf leaf litter. Nearby vegetation included; Laurel oak (Quercus laurifolia), bald cypress (Taxodium distichum), loblolly pine (Pinus taeda), Rhododendron spp., saw palmetto (Serenoa repens). Native soil pH = 5.03. NNE exposure/aspect.Wild materialGerardo Nunez USDA plant collecting trip to Florida 2018, 20192094710PI 691218
5PI 691219V. arboreum GN2018 Manatee Springs State Park 7Vaccinium arboreum Marshall Florida, United StatesCOR2019COLLECTED12/06/2019Manatee Springs State Park29.50007400, -82.9652620011Post #15 on shacklefoot trail. Partial shade. Vegetation nearby included; Hardwood forest, saw palmetto (Serenoa repens), slash pine (Pinus elliottii). Native soil pH = 5.71. SSW exposure/aspect Wild materialGerardo Nunez USDA plant collecting trip to Florida 2018, 20192094711PI 691219
6PI 691220V. arboreum GN2018 Manatee Springs State Park 8Vaccinium arboreum Marshall Florida, United StatesCOR2019COLLECTED12/06/2018Manatee Springs State Park29.49911800, -82.9662610018Partial Shade on trail. NNW exsposure/aspect. Near Wax myrtle (Myrica cerifera), saw palmettow (Serenoa repens). Native soil pH= 5.58 Wild materialGerardo Nunez USDA plant collecting trip to Florida 2018, 20192094712PI 691220
7PI 656829JM2005805Trichostema dichotomum L. South Carolina, United StatesNC72006COLLECTED09/28/2005Along Highway 17 to Bailey Island, 100 meters off Pine Landing Road, Charleston County.33.15000000, -80.435277783Barrier island; live oak community; weedy; sandy loam soil. Wild material1704277PI 656829
8NA 89180TJKRhododendron minus Michx. var. chapmanii (Alph. Wood) W. H. Duncan & Pullen Florida, United StatesNAContact Site2026COLLECTED04/01/2025St. 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, -85.268363863This 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 materialReceived as R. chapmanii2193314NA 89180
9NA 891742025RJLSEUS-16Kalmia hirsuta Walter Florida, United StatesNA2026COLLECTED10/04/2025Eglin Air Force Base: collected along Florida National Scenic Trail/Eglin AFB unnamed road.30.43936000, -86.844045007Growing 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 material2193308NA 89174
10NA 891732025RJLSEUS-14Chionanthus sp.Florida, United StatesNA2026COLLECTED10/03/2025Choctawhatchee 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, -86.6596500010Dry 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 materialReceived as C. cf. henryae2193307NA 89173
11NA 891602025RJLSEUS-08Ilex hybr.Florida, United StatesNA2025COLLECTED10/02/2025Eglin 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, -86.773158008Part 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 material2193006NA 89160
12NA 885782024RJLFL-004Ilex vomitoria Aiton Florida, United StatesNA2024COLLECTED11/12/2024Collected along Florida National Scenic Trail/Eglin Air Force Base unnamed road.30.44526100, -86.860947004Mixed 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 material2169915NA 88578
13NA 885892024RM-002Lyonia ferruginea (Walter) Nutt. Florida, United StatesNA2024COLLECTED11/21/2024Eglin 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, -86.835955006Mixed 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 material2169926NA 88589
14NA 88731RonMiller2022-Old Land PlaceGordonia lasianthus (L.) J. Ellis Florida, United StatesNA2024COLLECTED04/2022Yellow River Marsh State Aquatic Preserve, "Old Land Place" along Weaver River, 1.47 miles south of the confluence with the Yellow River.30.55318000, -87.936560003Moist to wet areas in wetland adjacent to the river in association with a range of evergreen and deciduous forest elements.Wild materialFrom open-pollinated, but presumed isolated, seeds of NA 87342-H, -J, and -L (three young plants flowering in containers in production during 2024). Seed was harvested over a period roughly from October through December 2024 as fruits matured. From the record of the parent accession, NA 87342: Exact date of collection unknown.2170992NA 88731
15NA 87844TRX241118-02GAIlex cassine L. Georgia, United StatesNA2024COLLECTED11/18/2024St. Simons Island: Frederica Park.31.23766000, -81.356380006Wild material2169897NA 87844
16NA 87825FL24-03Ilex ambigua Torr. Florida, United StatesNA2024COLLECTED09/07/2024Rye Preserve, along the Manatee River.27.50951673, -82.35916675Open scrub, xeric, sandy. EPA Ecoregion III: Southern Coastal Plain (75). EPA Ecoregion IV: Southwestern Florida Flatwood (75b). Geology: Hawthorn Group, Peace River Formation. Soil: Cassia Series Fine Sand, moderately well drained.Wild material2168975NA 87825
17NA 88852TJK2023FL-047Ilex glabra (L.) A. Gray Florida, United StatesNA2024COLLECTED12/26/2023South 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, -85.274100006Longleaf 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 material2165707NA 88852
18NA 88853TJK2023FL-048Lyonia ferruginea (Walter) Nutt. Florida, United StatesNA2024COLLECTED12/26/2023South 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, -85.274000006Longleaf 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 material2165708NA 88853
19WLP 3411TJK2023FL-044Cyrilla racemiflora L. Florida, United StatesNAPLANT2024COLLECTED12/26/2023Forest Hill Cemetery, east fence line, 0.4 mi north of Hwy 98, off Twine Rd.29.78030000, -85.271600007Growing on the edge of a wet pine savanna/flatwood. Slope: flat. Aspect: Southeast. Elevation: 23 feet.Wild material2165704WLP 3411
20WLP 3412TJK2023FL-045Lyonia lucida (Lam.) K. Koch Florida, United StatesNA2024COLLECTED12/26/2023East backwoods adjacent to Forest Hill Cemetery, 0.4 mi north of Hwy 98, off Twine Rd.29.78030000, -85.271600007Edge of a wet pine savanna/flatwood. Slope: flat. Aspect: Southeast. Elevation: 23 feet.Wild material2165705WLP 3412
21NA 88827RJL-RM2023FLAL-001Ilex ambigua Torr. Florida, United StatesNA2023COLLECTED12/05/2023Yellow River Wildlife Management Area, along DOF [Department of Forestry] Y9 dirt road 0.08 kilometers east of Miller Bluff Road.30.65289100, -86.8760280044Growing in part shade to sun in very dry, highly competitive site still recovering from the logging of pines in the past decade. This young woodland is comprised of a combination of evergreen and deciduous species competing for available resources and light before the young sand pines begin to dominate the upper canopy. Slope: 0 percent. Aspect: N/A. 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 type in the collection area is classified as Lakeland Sand soils (0 to 5 percent slopes). The surface soil profile of this area is primarily the Lakeland series which 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 material2165657NA 88827
22NA 88828RJL-RM2023FLAL-002Vaccinium arboreum Marshall Florida, United StatesNA2023COLLECTED12/05/2023Yellow River Wildlife Management Area, along DOF [Department of Forestry] Y9 dirt road 0.08 kilometers east of Miller Bluff Road.30.65289100, -86.8760850044Growing in part shade to sun in very dry, highly competitive site still recovering from the logging of pines in the past decade. This young woodland is comprised of a combination of evergreen and deciduous species competing for available resources and light before the young sand pines begin to dominate the upper canopy. Slope: 0 percent. Aspect: N/A. 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 type in the collection area is classified as Lakeland Sand soils (0 to 5 percent slopes). The surface soil profile of this area is primarily the Lakeland series which 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 material2165658NA 88828
23NA 88683TJK2023FL-030Vaccinium arboreum Marshall Florida, United StatesNA2023COLLECTED11/16/2023Pensacola State College, Midway Campus, 1/8 mile south of Highway 98.30.39710000, -87.0104000010Sand Pine Scrub, old remnant sand dune. Slope: flat. Aspect: West. Elevation: 32 feet.Wild material2159095NA 88683
24NA 88684TJK2023FL-031Smilax smallii Morong Florida, United StatesNA2023COLLECTED11/18/2023T. Kiphart residence, Navarre, Florida.30.40680000, -86.9309000012Moist, urban woods. Slope: 3%. Aspect: South. Elevation: 39 feet.Wild material2159096NA 88684
25NA 88686TJK2023FL-033Ilex glabra (L.) A. Gray Florida, United StatesNA2023COLLECTED11/18/2023Navarre, 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, -86.9298000011Wet pine flatwood transitioning to a shrub bog habitat under fire suppression. Slope: 3.5%. Aspect: West. Elevation: 36 feet.Wild material2159098NA 88686
26NA 88687TJK2023FL-034Clethra alnifolia L. Florida, United StatesNA2023COLLECTED11/18/2023Navarre, 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, -86.9289000011Wet Pine Flatwood transitioning to a shrub bog habitat under fire suppression. Slope: less than 2%. Aspect: North. Elevation: 36 feet.Wild material2159099NA 88687
27WLP 3280TJK2023FL-028Kalmia hirsuta Walter Florida, United StatesNA2023COLLECTED11/02/2023Navarre, 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, -86.9284000011Wet Pine Flatwood transitioning to a shrub bog habitat under fire suppression. Slope: flat. Aspect: East Elevation: 36 feet.Wild material2159060WLP 3280
28NA 89011TJK2023FL-019Kalmia hirsuta Walter Florida, United StatesNA2023COLLECTED10/10/2023Blackwater State Forest, a few hundred yards from Juniper Creek.30.80110600, -86.8910750015Elevation: 52 feet. Slope: 0%. Aspect: Southeast.Wild material2158904NA 89011
29NA 88662TJK2023FL-016Sideroxylon sp.Florida, United StatesNA2023COLLECTED09/16/2023East River Unit, Eglin Air Force Base. Near A-21 Rd.30.41250000, -86.771100007Xeric shrub, xeric sandhills community. Elevation: 26 feet. Slope: 2%. Aspect: South.Wild material2158796NA 88662
30NA 89271TJK2023FL-009Vaccinium stamineum L. Florida, United StatesNA2023COLLECTED07/16/2023Eglin Air Force Base: Weaver Creek area west of Highway 87, north of Choctaw Nolf Airfield Road (Escrobano Point).30.50710000, -86.9122000033Xeric oak-pine uplands above Weaver Creek Bayhead. Slope: 5%. Aspect: Northwest. Elevation recorded as 107 feet.Wild materialWLPGR contract collection.2158254NA 89271
31NA 88598RJL2023FL-002aAgarista populifolia (Lam.) Judd Florida, United StatesNA2023COLLECTED02/14/2023Plants 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, -81.4720540010Plants 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 material2141479NA 88598
32NA 87349TJK2022FL-004Cartrema americana (L.) G. L. Nesom Florida, United StatesNA2023COLLECTED11/02/2022Okaloosa County: Eglin Air Force Base: East River Unit H-3, Range Road 259, north of Highway 98.30.41300000, -86.774800000A wet stringer surrounded by Xeric Scrub/Upland Sandhill community.Wild material2141640NA 87349
33NA 87350TJK2022FL-005Ilex ambigua Torr. Florida, United StatesNA2023COLLECTED11/02/2022Okaloosa County: Eglin Air Force Base: East River Unit H-3, Range Road 259, north of Highway 98.30.41190000, -86.773200000Xeric Scrub/Upland Sandhill community.Wild material2141641NA 87350
34NA 87351TJK2022FL-006Aronia arbutifolia (L.) Pers. Florida, United StatesNA2023COLLECTED12/31/2022Santa Rosa County: Midway: Pensacola State College, South Santa Rosa Center (Santa Rosa County School District), 1/4 mile south of Highway 98.30.39570000, -87.013000000Very interesting site. Interior flooded wetland dominated by Ilex cassine and Ilex myrtifolia. Xeric ridges in wetland have both Cladonia cristella and Cladonia perforata, xeric edges dominated by Pinus clausa. Cyrilla, in seed, consistently dwarfed 16 inches to 6 feet tall, probably due to hydrological and edaphic factors.Wild material2141642NA 87351
35NA 87352(open-pollinated seed of Lowei Group)Ilex myrtifolia Walter Florida, United StatesNA2023COLLECTED12/31/2022Santa Rosa County: Midway: Pensacola State College, South Santa Rosa Center (Santa Rosa County School District), 1/4 mile south of Highway 98. Coordinates for two plants given; second plant's coordinates are 30.3959 deg. N, 87.0097 deg. W.30.39570000, -87.012900000Very interesting site. Interior flooded wetland dominated by Ilex cassine and Ilex myrtifolia. Xeric ridges in wetland have both Cladonia cristella and Cladonia perforata, xeric edges dominated by Pinus clausa. Cyrilla, in seed, consistently dwarfed 16 inches to 6 feet tall, probably due to hydrological and edaphic factors.Wild materialReceived as Ilex myrtifolia (yellow fruit); accessioned at USNA as Ilex myrtifolia (open-pollinated seed of Lowei Group). Note: while these seeds were collected from yellow-fruited individuals, the parent plants were open-pollinated. The yellow fruit trait is likely to be recessive, so some seedlings may be only heterogeneous for yellow fruit. -SBL [As of late November 2025, all three female seedlings at USNA that have borne fruit are red-fruited; one might be a lighter, more orange-red tone than the other two.]2141643NA 87352
36NA 88526RM-TK2022-014Oxydendrum arboreum (L.) DC. Florida, United StatesNA2023COLLECTED11/06/2022Growing along an unnamed dirt road leading to “Old Land Place” on the edge of Eglin AFB accessed from the Yellow River.30.55320000, -86.937300002The 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 material2140807NA 88526
37NA 88565RJLSEUS2022-038Ilex ambigua Torr. Florida, United StatesNA2023COLLECTED12/14/2022Eglin Air Force Base: growing along the east 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 en route to Escribano Point Wildlife Management Area.30.51507900, -86.9676710014Full sun on the top of the roadside slope in well-drained to dry conditions, 1-2 meters above surrounding lower, moist area. 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 type in the collection area is classified as Lakeland Sand soils (5 to 12 percent slopes). The surface soil profile of this area is primarily the Lakeland series which 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 material2140822NA 88565
38NA 88566RJLSEUS2022-039Rhododendron viscosum (L.) Torr. Florida, United StatesNA2023COLLECTED12/14/2022Plants growing in woodlands at Escribano Point Bayou Campground not far from the parking lot. Occasional.30.50990400, -87.004149001Plants 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 material2140788NA 88566
39NA 88567RJLSEUS2022-040Chamaecyparis thyoides (L.) Britton et al. Florida, United StatesNA2023COLLECTED12/14/2022Plants growing in woodlands at Escribano Point Bayou Campground not far from the parking lot. Occasional.30.51018200, -87.004488001Plants 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 material2140789NA 88567
40NA 88568RJLSEUS2022-041Oxydendrum arboreum (L.) DC. Florida, United StatesNA2023COLLECTED12/14/2022Plants 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, -87.005638002Trees 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 material2140790NA 88568
41WLP 2600RJL2022FLAL-029Stewartia malacodendron L. Florida, United StatesNA2022COLLECTED08/07/2022Eglin 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, -86.9146940015Growing 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 material2138710WLP 2600
42WLP 1437NA 84027Oxydendrum arboreum (L.) DC. Florida, United StatesNA2016COLLECTED11/11/2016Woodlands associated with Miller Bayou, south of housing subdivision off of Pearl Court.30.46413000, -86.928040002Full 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.1950372WLP 1437