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ACCESSIONPLANT NAMETAXONOMYORIGINGENEBANKIMAGEAVAILABILITYRECEIVEDSOURCE TYPESOURCE DATECOLLECTION SITECOORDINATESELEVATIONHABITATIMPROVEMENT LEVELNARRATIVE
0MIA 37265 OrnaMIA 37265 OrnaSabal palmetto (Walter) Lodd. ex Schult. & Schult. f. MIAPLANT20222170635MIA 37265 Orna
1MIA 25222Sabal palmetto (Walter) Lodd. ex Schult. & Schult. f. Florida, United StatesMIA1978COLLECTEDWild material1091123MIA 25222
2MIA 22925Sabal palmetto (Walter) Lodd. ex Schult. & Schult. f. MIAFlower1939S3-4-02-08^;1088426MIA 22925
3PI 108021Sabal causiarum (O. F. Cook) Becc. Cienfuegos, CubaMIAPlant1935DONATED10/09/19351128845PI 108021
4PI 105955Sabal causiarum (O. F. Cook) Becc. Puerto Rico, United StatesMIAPlant1934DONATED07/06/19341128405PI 105955
5PI 96489Sabal causiarum (O. F. Cook) Becc. Dominican RepublicMIAPlant1932COLLECTEDS3-4-02-07^;1127322PI 96489
6PI 87458 tarsInodes PalmettoSabal sp.Virgin Islands, U.S., United StatesMAY1930DONATED04/25/1930A fan-leaved palm said to have come from the island of St. Thomas - BPI Inventories No. 103-201908268PI 87458 tars
7PI 80551Sabal mexicana Mart. GuyanaMIAPlant1929DONATED06/05/19291118433PI 80551
8PI 80183Sabal causiarum (O. F. Cook) Becc. Trinidad, Trinidad and TobagoMIAPLANT1929DONATED04/10/19291118309PI 80183
9PI 77166Sabal causiarum (O. F. Cook) Becc. Cienfuegos, CubaMIAPlant1928DONATED06/22/19281117860PI 77166
10MIA 37250 OrnaMIA 37250 OrnaSabal miamiensis Zona MIAPLANT20232170620MIA 37250 Orna
11MIA 37251 OrnaMIA 37251 OrnaSabal miamiensis Zona MIAPLANT20232170621MIA 37251 Orna
12MIA 37281 OrnaMIA 37281 OrnaSabal minor (Jacq.) Pers. MIAPLANT20232170651MIA 37281 Orna
13MIA 37282 OrnaMIA 37282 OrnaSabal minor (Jacq.) Pers. MIAPLANT20232170652MIA 37282 Orna
14MIA 37283 OrnaMIA 37283 OrnaSabal minor (Jacq.) Pers. MIAPLANT20232170653MIA 37283 Orna
15MIA 37284 OrnaMIA 37284 OrnaSabal minor (Jacq.) Pers. MIAPLANT20232170654MIA 37284 Orna
16MIA 37280 OrnaMIA 37280 OrnaSabal minor (Jacq.) Pers. MIAPLANT20222170650MIA 37280 Orna
17MIA 8639Sabal mexicana Mart. MIAPlant19391044633MIA 8639
18MIA 9482Sabal mexicana Mart. MIAPLANT1939E3-2-02-01.5^;1048834MIA 9482
19PI 673213CDKHelianthus debilis Nutt. subsp. tardiflorus Heiser Florida, United StatesNC72011COLLECTED12/14/2010Along Highway 24, east of County Road 347, north of Cedar Key, Levy County.29.18320000, -83.01710000Roadside. Dry, sandy. Associated with Morella cerifera, Quercus, and Sabal palmetto.Wild material1887445PI 673213
20NA 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
21NA 87346TJK2022FL-001Cornus florida L. Florida, United StatesNA2023COLLECTED10/27/2022Okaloosa County: Duke Field AFS; Eglin Air Force Base, approximately 1.3 miles southeast of Military Rd 231, Juniper Creek Bayhead.30.62890000, -86.5000000042Rich evergreen and deciduous Bayhead Community. Extensive Quercus arkansana along the bluff top to mid-slope, with Magnolia ashei in steephead bottom to lower half of slope. Cornus at toe of slope on the first bench, off bottom.Wild material2141637NA 87346
22NA 88524RM-TK2022-012Hydrangea quercifolia W. Bartram Florida, United StatesNA2023COLLECTED10/20/2022Private property of Joann Palmer on Reservation Court30.23775000, -84.324100005Plants are abundant in this upland, dry, and arenaceous soil over karst.
Soils: The underlying geology of this area is the St. Michaels Formation of Miocene origin. The Lower Miocene St. Marks Formation, named by Finch (1823), is exposed in Wakulla, Leon and Jefferson Counties on the northwestern flank of the Ocala Platform. It is a white to yellowish gray, poorly to moderately indurated, sandy, fossiliferous (molds and casts) limestone (packstone to wackestone). Mollusk molds and casts are often abundant. The St. Marks Formation makes up the upper part of the FAS in part of the eastern panhandle.
Source: USGS Florida Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=FLMIsmk%3B0)
The surface soil profile found in this area is Otela limestone substratum-Ortega sands (0 to 5 percent slopes). The Otela Series consists of very deep, moderately well drained, moderately slowly to slowly permeable soils on broad uplands. They formed in sandy and loamy marine sediments over limestone on karst topography. Slopes range from 0 to 8 percent. 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. Ortega Series soils are generally strongly acid.
https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)
Wild material2140805NA 88524
23WLP 2518River Bluff Recreational AreaHydrangea quercifolia W. Bartram Georgia, United StatesNA2019COLLECTED11/12/2018River Bluff Recreation Area, Quitman County. Adjacent to Walter F. George Reservoir (eastern edge), across from Eufaula and approximately 0.9 miles north of Georgetown.31.89845700, -85.10882700Shady bluffs adjacent to reservoir.Wild materialMeasurements of sampled specimens taken in nature: Height 78 to 158 in.; width 57 to 157 in. Measurements for each specimen sampled may be provided upon request.2106228WLP 2518
24NA 71849NA 71849Torreya taxifolia Arn. Florida, United StatesNAContact Site2002COLLECTED11/1989Nature Conservancy Preserve. Travelers Flood Plain, between Sweetwater Creek and Long Branch. Slopes above the flood plain of the Appalachicola River. Taken from slopes 50-300 feet from waters edge. In general, many of these plants were further from the waters edge than usually seen, probably due to effects of flooding, from the river. Creek. Just southwest of the village of Sweetwater.30.53888000, 84.96666000Deciduous forest with Sabal palmetto understory1951019NA 71849