| 0 | W6 60055 | NCBG-707 | Salvia lyrata L. | North Carolina, United States | W6 | | | 2021 | | | | | | | Wild material | | 2132936 | W6 60055 |
| 1 | W6 27648 | ODNR 11 | Salvia lyrata L. | Ohio, United States | W6 | | | 2004 | COLLECTED | 06/22/2004 | Shawnee State Forest | 38.72666667, -83.26277778 | 1058 | Associated vegetation: Thalictrum revolutum, Iris cristata and Phlox glaberrima | Wild material | | 1680750 | W6 27648 |
| 2 | W6 27662 | 'Purple Knockout' | Salvia lyrata L. | Ohio, United States | W6 | | | 2004 | DONATED | 08/12/2004 | | | | | Cultivar | | 1658737 | W6 27662 |
| 3 | PI 673987 | TX-07 | Coreopsis lanceolata L. | Texas, United States | OPGC | | | 2010 | COLLECTED | 05/26/2010 | Upper West Gulf Coastal Plain. Harrison County.SH 43 between Marshall and Karnack Texas. | 32.63652800, -94.18847200 | 90 | Maintained Roadside ROW adjacent to mixed pine forest. Land form: Rolling hills to flat. Land Use: Roadside ROW. Geology: Sandstone. Soil Texture: Sandy. Soil Color: Tan. | Wild material | Erect, clumped, glabrous to 70 cm tall. Flowers numerous, yellow ray florets. | 1897289 | PI 673987 |
| 4 | PI 673988 | TX-08 | Rudbeckia maxima Nutt. | Texas, United States | OPGC |  | | 2010 | COLLECTED | 05/26/2010 | Upper West Gulf Coastal Plain. Harrison County.SH 43 between Marshall and Karnack Texas. | 32.63652800, -94.18847200 | 90 | Maintained Roadside ROW adjacent to mixed pine forest. Land form: Rolling hills to flat. Land Use: Roadside ROW. Geology: Sandstone. Soil Texture: Sandy. Soil Color: Tan. | Wild material | Large blue-green leathery leaves mostly basal, plants to 2 m tall, yellow ray florets. | 1897290 | PI 673988 |
| 5 | NA 88582 | 2024RJLFL-013 | Cornus florida L. | Florida, United States | NA | | | 2024 | COLLECTED | 11/13/2024 | Woodland edge along the south side of Bud Bass Road (DOF B48), 0.30 kilometers east of the junction with Norman Riley Road. | 30.75753300, -86.80457600 | 39 | Mixed evergreen and deciduous forests in part shade in a mesic- to mesic-dry situation. Slope: 0 percent. Aspect: North. 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 Troup Series loamy sand, 0 to 5 percent slopes. The Troup series consists of very deep, somewhat excessively drained soils that formed in unconsolidated sandy and loamy marine sediments. Troup soils are on ridges and hillslopes. Slopes predominantly range from 0 to 15 percent but range to 45 percent. The soil pH is generally strongly acid. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). | Wild material | | 2169919 | NA 88582 |
| 6 | Ames 34315 | JDC/ML/2018/039/852 | Monarda luteola Singhurst & W. C. Holmes | Texas, United States | NC7 |  | | 2018 | COLLECTED | 07/18/2018 | Located 4.10 miles east of Mineola on west side of County Road 2650 just 0.88 miles north of intersection with FM 1801, Wood County | 32.66918400, -95.41726400 | 139 | Very diverse vegetation. Roadside. | Wild material | Plants with lemon scent, pubescent stems and leaves with faint yellow flowers measuring circa 1.0-2.5' in height. Plants likely reached peak flower on 15 May 2018. Seeds likely reached full maturity around first week in July (2018). | 1964622 | Ames 34315 |
| 7 | Ames 34205 | JDC/PV/2018/038/851 | Prunella vulgaris L. | Texas, United States | NC7 | _thumbnail.jpg) | | 2018 | COLLECTED | 05/23/2018 | Located 4.10 miles east of Mineola along County Road 2650 just 1.00 miles north of intersection with FM 1801, Wood County | 32.67184300, -95.41677700 | 142 | Roadside. Very diverse vegetation. | Wild material | Plants approximately 10" tall. Seeds collected right at peak maturity (23 May 2018). | 1963388 | Ames 34205 |