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taxonomy genus name like Agarista
| ACCESSION | PLANT NAME | TAXONOMY | ORIGIN | GENEBANK | IMAGE | AVAILABILITY | RECEIVED | SOURCE TYPE | SOURCE DATE | COLLECTION SITE | COORDINATES | ELEVATION | HABITAT | IMPROVEMENT LEVEL | NARRATIVE | | |
|---|
| 0 | PI 142293 | | Agarista populifolia (Lam.) Judd | Maryland, United States | | | Historic | 1941 | COLLECTED | | | | | | | | 1867122 | PI 142293 |
| 1 | NA 88933 | 24Flam40 | Agarista populifolia (Lam.) Judd | South Carolina, United States | NA | | | 2025 | COLLECTED | 09/12/2025 | Robertville, SC: Gillison Branch Road (plants on both sides of road). | 32.58673000, -81.19300000 | 31 | Shady swamp forest with road running between Agarista population. Agarista was the predominant plant throughout. Soggy but solid ground, especially on northern side of road. Growing in 3/4 shade. Slope: Generally flat. | Wild material | Note: Two field collections, 24Flam40 and 24Flam41, were combined together in this USNA accession, with the former identifier being used as the primary one. | 2172816 | NA 88933 |
| 2 | NA 88598 | RJL2023FL-002a | Agarista populifolia (Lam.) Judd | Florida, United States | NA | | | 2023 | COLLECTED | 02/14/2023 | Plants 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, -81.47205400 | 10 | Plants 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 material | | 2141479 | NA 88598 |
| 3 | NA 85027 | 'Taylor's Treasure' | Agarista populifolia (Lam.) Judd | | NA | | Not Available | 2010 | | | | | | | Cultivar | Full name as recorded at U.S. National Arboretum: Agarista populifolia 'Taylor's Treasure' LEPRECHAUN. | 2153970 | NA 85027 |
| 4 | NA 63191 | NA 63191 | Agarista populifolia (Lam.) Judd | | NA | | Not Available | 1991 | | | | | | | Cultivated material | Full name as recorded at U.S. National Arboretum: Agarista populifolia. | 2147079 | NA 63191 |
| 5 | NA 31294 | NA 31294 | Agarista populifolia (Lam.) Judd | | NA | | Not Available | 1969 | | | | | | | Cultivated material | Full name as recorded at U.S. National Arboretum: Agarista populifolia. Rec'd thru Mr. Wilburn H. Youngman, Silver Spring, MD. Journal of Arnold Arb. 65(3): p. 297. 1984. | 2144206 | NA 31294 |