| 0 | PI 132064 | | Pinckneya bracteata (W. Bartram) Raf. | Georgia, United States | | | Historic | 1939 | COLLECTED | 03/11/1937 | Sylvester, Worth County | | | | | | 1848169 | PI 132064 |
| 1 | NA 88841 | RJL-RM2023FLAL-015 | Pinckneya bracteata (W. Bartram) Raf. | Florida, United States | NA | | | 2023 | COLLECTED | 12/11/2023 | West side of Marville Drive on the edge of the woodlands just a few hundred feet south of Fairway Drive. | 30.60665300, -85.32572200 | 79 | Plants are growing on the edge of a wetland acid habitat in the transitional zone between the obligate and facultative zones. They are growing in part-shade to shade with lower woody competition due to the moist conditions. Slope: N/A. 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 surface soil profile of this area is primarily Pamlico-Pantego-Rutlege Association. 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 0.4-1.3 meters of organic material over dominantly sandy sediments. Reaction is extremely in the organic layers and ranges from extremely acid to strongly acid in the underlying mineral layers. The Pantego series consists of very deep, very poorly drained, moderately permeable soils that formed in thick loamy sediments on the Southern Coastal Plain and Atlantic Coast Flatwoods. Slopes are less than 2 percent. This soil is strongly acid. The Rutlege series comprises very deep, very poorly drained persistently wet soils on flats, depressions and floodplains where shallow ponding is common. They are of marine or fluvial sediment origin. Thickness of these loamy sandy soils is greater than 1.5 meters and a reaction from extremely acid to strongly acid. (Source: NRCS Web Soil Survey.) | Wild material | | 2165671 | NA 88841 |
| 2 | NA 88842 | RJL-RM2023FLAL-016 | Pinckneya bracteata (W. Bartram) Raf. | Florida, United States | NA | | | 2023 | COLLECTED | 12/11/2023 | West side of Scott Road in woodlands approximately 0.13 kilometers north of where the road crosses Ecofina Creek. As of 2023, this road appears permanently closed from previous hurricane damage. | 30.55633300, -85.43520000 | 38 | Plants are growing in the understory of a mixed evergreen and deciduous bottomland forest associated with the Ecofina Creek. Plans are growing mostly on hummocks in a very wet, acidic wetland habitat. Slope: N/A. Aspect: N/A. The underlying geology of this area is the Alum Bluff Group of Miocene origin. It includes the Chipola Formation, Oak Grove Sand, Shoal River Formation, Choctawhatchee Formation and the Jackson Bluff Formation. The formations included in this group are generally defined on the basis of their molluscan faunas and stratigraphic position. Puri (1953) described sediment facies as they relate to the formations of the Alum Bluff Group. These sediments are lithologically distinct as a group, not as individual units. The Alum Bluff Group crops out or is beneath a thin overburden in the western panhandle from river valleys in Okaloosa County eastward to western Jackson County. The Alum Bluff Group consists of clays, sands and shell beds which may vary from fossiliferous, sandy clays to unfossiliferous sands and clays and occasional carbonate beds. Mica is a common constituent and glauconite and phosphate occur sporadically. Induration varies from essentially nonindurated in sands to well indurated in carbonate lenses. Colors range from cream to olive gray with mottled reddish brown in weathered sections. Sand grain size varies from very fine to very coarse with sporadic occurrences of gravel. These sediments generally have low permeabilities and are part of the intermediate confining unit/aquifer system. (Source: USGS Florida Geologic Map Data.) The surface soil profile of this area is primarily Pamlico-Pantego-Rutlege Association. 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 0.4-1.3 meters of organic material over dominantly sandy sediments. Reaction is extremely in the organic layers and ranges from extremely acid to strongly acid in the underlying mineral layers. The Pantego series consists of very deep, very poorly drained, moderately permeable soils that formed in thick loamy sediments on the Southern Coastal Plain and Atlantic Coast Flatwoods. Slopes are less than 2 percent. This soil is strongly acid. The Rutlege series comprises very deep, very poorly drained persistently wet soils on flats, depressions and floodplains where shallow ponding is common. They are of marine or fluvial sediment origin. Thickness of these loamy sandy soils is greater than 1.5 meters and a reaction from extremely acid to strongly acid. (Source: NRCS Web Soil Survey.) | Wild material | | 2165672 | NA 88842 |
| 3 | WLP 3242 | RM2023-009 | Pinckneya bracteata (W. Bartram) Raf. | Florida, United States | NA | | Not Available | 2023 | COLLECTED | 01/09/2023 | This plant is growing in a bog to the west and south of the junction of Marville Drive and Fairway Drive. | 30.60688400, -85.32575300 | 79 | The plants were growing in part shade in a bog with gray muck and running clear tea-colored water. Slope: N/A. 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 surface soil profile of this area is primarily Pamlico-Pantego-Rutlege Association. 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 0.4-1.3 meters of organic material over dominantly sandy sediments. Reaction is extremely in the organic layers and ranges from extremely acid to strongly acid in the underlying mineral layers. The Pantego series consists of very deep, very poorly drained, moderately permeable soils that formed in thick loamy sediments on the Southern Coastal Plain and Atlantic Coast Flatwoods. Slopes are less than 2 percent. This soil is strongly acid. The Rutlege series comprises very deep, very poorly drained persistently wet soils on flats, depressions and floodplains where shallow ponding is common. They are of marine or fluvial sediment origin. Thickness of these loamy sandy soils is greater than 1.5 meters and a reaction from extremely acid to strongly acid. (Source: NRCS Web Soil Survey.) | Wild material | Received as seedlings. | 2158833 | WLP 3242 |
| 4 | WLP 3091 | RM2023-009 | Pinckneya bracteata (W. Bartram) Raf. | Florida, United States | NA | | | 2023 | COLLECTED | 01/09/2023 | This plant is growing in a bog to the west and south of the junction of Marville Drive and Fairway Drive. | 30.60688400, -85.32575300 | 79 | The plants were growing in part shade in a bog with gray muck and running clear tea-colored water.
Soils: 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 (https://mrdata.usgs.gov/geology/state/state.php?state=fl)
The surface soil profile of this area is primarily Pamlico-Pantego-Rutlege Association. 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 0.4-1.3 meters of organic material over dominantly sandy sediments. Reaction is extremely in the organic layers and ranges from extremely acid to strongly acid in the underlying mineral layers. The Pantego series consists of very deep, very poorly drained, moderately permeable soils that formed in thick loamy sediments on the Southern Coastal Plain and Atlantic Coast Flatwoods. Slopes are less than 2 percent. This soil is strongly acid. The Rutlege series comprises very deep, very poorly drained persistently wet soils on flats, depressions and floodplains where shallow ponding is common. They are of marine or fluvial sediment origin. Thickness of these loamy sandy soils is greater than 1.5 meters and a reaction from extremely acid to strongly acid.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2141445 | WLP 3091 |
| 5 | NA 85370 | NA 85370 | Pinckneya bracteata (W. Bartram) Raf. | | NA | | Not Available | 2018 | | | | | | | Wild material | Full name as recorded at U.S. National Arboretum: Pinckneya bracteata. | 2154193 | NA 85370 |
| 6 | WLP 1536 | GF2018-04 | Pinckneya bracteata (W. Bartram) Raf. | Georgia, United States | NA | | | 2018 | COLLECTED | 11/06/2018 | Screven County; ; Along the side of Oliver Hwy, 230 ft. north of Nancy Branch Creek. | 32.54847000, -81.52067000 | 38 | In swampy thicket near a pond. | | It looks like the area was cleared in the last 5-6 years with many other small trees about the same height. | 2108886 | WLP 1536 |
| 7 | NA 87220 | NA 87220 | Pinckneya bracteata (W. Bartram) Raf. | | NA | | Not Available | 2017 | | | | | | | Cultivated material | Full name as recorded at U.S. National Arboretum: Pinckneya bracteata. Seeds brought to USNA by Nick Lazio from the JC Raulston Arboretum for germination. Nick was also attempting crosses with Emmenopterys henryi at Raulston. One seedling was later given to the National Herb Garden curator for planting. | 2155237 | NA 87220 |
| 8 | NA 56808 | TD 481 | Pinckneya bracteata (W. Bartram) Raf. | Florida, United States | NA | | Not Available | 1985 | COLLECTED | | Liberty County; ; North of Bristol along the Apalachicola River, UNCC Station. | | | | | Original propagations from the wild. | 2108362 | NA 56808 |