| 0 | NA 88457 | NEWFS-934 | Smilax glauca Walter | Massachusetts, United States | NA | | | 2021 | | | | | | | Wild material | Leaves bluntly triangular and acumite with three prominent parallel veins and a glaucus bloom on abaxial surface. | 2138954 | NA 88457 |
| 1 | NA 88612 | KY23-015 | Smilax herbacea L. | Kentucky, United States | NA | | | 2023 | COLLECTED | 09/09/2023 | Black Mountain summit, along gas pipeline. | 36.91943000, -82.90633000 | 1220 | Along pipeline road. Elevation: 4003 feet. Aspect: Southwest. | Wild material | Received as Smilax glauca; reidentified by Tim Block, Morris Arboretum. | 2158704 | NA 88612 |
| 2 | NA 88026 | NCBG-337 | Smilax rotundifolia L. | Virginia, United States | NA |  | | 2018 | | | | | | | Wild material | | 1965915 | NA 88026 |
| 3 | Ames 36219 | Egyptian Tract | Salix sericea Marshall | Missouri, United States | NC7 |  | | 2024 | COLLECTED | 01/19/2024 | LAD Foundation Egyptian Tract Wet Hollow Seep/Fen Complex located 7.52 miles west, southwest of Annapolis just northwest of intersection of CR 338 and CR 334, T31N R2E SW 1/4 SE 1/4 SE 1/4 Sec. 21 (Lesterville SE Quad.). | 37.34429700, -90.83361600 | 217 | Perched wet fen/seep complex with standing water supporting both obligate calciphilic and obligate acidophilic plant species. | Wild material | The native range of Salix sericea is concentrated througout the northeastern and eastern central United States ranging from Maine south to South Carolina, west to Illinois with a relatively large disjunct area in southeastern Missouri (Little, E. L. Jr. 1977). This accession represents genetics from southeastern Missouri in Reynolds County. Shrubs noted at the collection site in nature ranging in height from 2-7 feet and typically twice as wide as tall. Multi-stemmed shrubs expanding vegetatively via layering. Dormant stem colors noted at collection site ranging from mostly greenish to occassionally brownish red and/or copper tones. Dormant buds rather red and often bright red in color. Salix sericea is native to areas of the northeastern U.S. and north into Canada, reaching its western extent in Missouri. Classified as an obligate wetland plant that typically occurs on wet seeps, sedge meadows, streambanks, fens, etc. that are usually slightly acidic. Known to have the potential to reach up to four meters in height, but always much wider than tall. Ornamental characteristics include dark green leaves that are hairless above with undersides that are densely minutely-hairy making them rather white in appearance. Flowering occurs before or during leaf expansion. This species is known to serve as a larval host plant for the Arcadian Hairstreak, Satyrium acadica. | 2165775 | Ames 36219 |
| 4 | NA 88686 | TJK2023FL-033 | Ilex glabra (L.) A. Gray | Florida, United States | NA | | | 2023 | COLLECTED | 11/18/2023 | Navarre, 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, -86.92980000 | 11 | Wet pine flatwood transitioning to a shrub bog habitat under fire suppression. Slope: 3.5%. Aspect: West. Elevation: 36 feet. | Wild material | | 2159098 | NA 88686 |
| 5 | NA 88687 | TJK2023FL-034 | Clethra alnifolia L. | Florida, United States | NA | | | 2023 | COLLECTED | 11/18/2023 | Navarre, 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, -86.92890000 | 11 | Wet Pine Flatwood transitioning to a shrub bog habitat under fire suppression. Slope: less than 2%. Aspect: North. Elevation: 36 feet. | Wild material | | 2159099 | NA 88687 |
| 6 | NA 88506 | RJL2022TX-001 | Itea virginica L. | Texas, United States | NA | | | 2022 | COLLECTED | 10/31/2022 | Plants growing at Shangri La Botanical Gardens and Nature Center, Orange, TX along Adams Bayou, accessed via internal service roads. Plant is infrequent at this site. | 30.10322000, -93.76271700 | 1 | Plants are growing in shade to part-shade of a Taxodium distichum-Nyssa aquatica dominated forested swampland associated with Adams Bayou in a wet low-lying area that is frequently inundated.
Soils: The underlying geology of this area is of Quaternary to Late Pleistocene origin and comprised of the Beaumont Formation. This formation is yellowish- to brownish-gray, locally reddish orange with very fine to fine quartz sand, silt, and minor fine gravel, intermixed and interbedded. It also includes stream channel, point-bar, cravasse-splay, and natural levee ridge deposits, and clayey fill in abandoned channels. Channel fill is dark brown to brownish-gray with laminated clay and silt that is organic-rich. Includes marine delta-front sand, lagoonal clay, and near-shore marine sand beneath and landward of bays along the coast. Depth of this unconsolidated outwash ranges from 3-100 meters thick.
Source: USGS Texas Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=TXQbs%3B0)
The primary soil types in the collection area are classified as Cowmarsh series. The Cowmarsh series consists of very deep, very poorly drained soils that formed in mucky silty clayey alluvial deposits of Holocene age. These depressional soils are oxbows and relict channels of rivers where flooding and ponding is frequent. Slope ranges from 0 to 1 percent but mainly less than 1 percent. very poorly drained. Runoff is negligible. Frequently flooded for very long periods from February through May and surface remains saturated for very long periods once flood waters have receded.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2139813 | NA 88506 |
| 7 | NA 88507 | RJL2022TX-002 | Fraxinus caroliniana Mill. | Texas, United States | NA | | | 2022 | COLLECTED | 10/31/2022 | Plants growing at Shangri La Botanical Gardens and Nature Center, Orange, TX along Adams Bayou, accessed via internal service roads. Plant is relatively common along Adams Bayou but scattered. | 30.09989400, -93.75239700 | 1 | Plants are growing in part-shade to sun of a Taxodium distichum-Nyssa aquatica dominated forested swampland associated with Adams Bayou in a wet low-lying area that is frequently inundated. While found as an occasional understory element, it is more common on the edge of the swampland forest where there are high light conditions.
Soils: The underlying geology of this area is of Quaternary to Late Pleistocene origin and comprised of the Beaumont Formation. This formation is yellowish- to brownish-gray, locally reddish orange with very fine to fine quartz sand, silt, and minor fine gravel, intermixed and interbedded. It also includes stream channel, point-bar, cravasse-splay, and natural levee ridge deposits, and clayey fill in abandoned channels. Channel fill is dark brown to brownish-gray with laminated clay and silt that is organic-rich. Includes marine delta-front sand, lagoonal clay, and near-shore marine sand beneath and landward of bays along the coast. Depth of this unconsolidated outwash ranges from 3-100 meters thick.
Source: USGS Texas Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=TXQbs%3B0)
The primary soil types in the collection area are classified as Cowmarsh series. The Cowmarsh series consists of very deep, very poorly drained soils that formed in mucky silty clayey alluvial deposits of Holocene age. These depressional soils are oxbows and relict channels of rivers where flooding and ponding is frequent. Slope ranges from 0 to 1 percent but mainly less than 1 percent. very poorly drained. Runoff is negligible. Frequently flooded for very long periods from February through May and surface remains saturated for very long periods once flood waters have receded.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2139814 | NA 88507 |
| 8 | NA 88508 | RJL2022TX-003 | Morella cerifera (L.) Small | Texas, United States | NA | | | 2022 | COLLECTED | 10/31/2022 | Plants growing at Shangri La Botanical Gardens and Nature Center Orange, TX along Adams Bayou, accessed via internal service roads. Plant is relatively common along Adams Bayou but scattered in the understory. | 30.10035500, -93.75288700 | 1 | Plants are growing in part-shade to shade of a Taxodium distichum-Nyssa aquatica dominated forested swampland associated with Adams Bayou in a wet low-lying area that is frequently inundated.
Soils: The underlying geology of this area is of Quaternary to Late Pleistocene origin and comprised of the Beaumont Formation. This formation is yellowish- to brownish-gray, locally reddish orange with very fine to fine quartz sand, silt, and minor fine gravel, intermixed and interbedded. It also includes stream channel, point-bar, cravasse-splay, and natural levee ridge deposits, and clayey fill in abandoned channels. Channel fill is dark brown to brownish-gray with laminated clay and silt that is organic-rich. Includes marine delta-front sand, lagoonal clay, and near-shore marine sand beneath and landward of bays along the coast. Depth of this unconsolidated outwash ranges from 3-100 meters thick.
Source: USGS Texas Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=TXQbs%3B0)
The primary soil types in the collection area are classified as Cowmarsh series. The Cowmarsh series consists of very deep, very poorly drained soils that formed in mucky silty clayey alluvial deposits of Holocene age. These depressional soils are oxbows and relict channels of rivers where flooding and ponding is frequent. Slope ranges from 0 to 1 percent but mainly less than 1 percent. very poorly drained. Runoff is negligible. Frequently flooded for very long periods from February through May and surface remains saturated for very long periods once flood waters have receded.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2139815 | NA 88508 |
| 9 | W6 60329 | NEWFS-935 | Rhus typhina L. | Massachusetts, United States | W6 | | | 2021 | | | | | | | Wild material | Upper branches and stems velvety fruit, a drupe enclosed in red pubescence. Sap thick, milky and irritating to the skin. | 2138955 | W6 60329 |
| 10 | OPGC 8255 | NCBG-335 | Rhexia nashii Small | Virginia, United States | OPGC | | | 2021 | | | | | | | Wild material | Glandular, hairy petals on lower surface. Stem faces unequal. | 2116297 | OPGC 8255 |
| 11 | WLP 684 | NA 85860 | Amelanchier arborea (F. Michx.) Fernald | Kentucky, United States | NA | | | 2019 | COLLECTED | 06/15/2019 | Powell County; ; Red River Gorge (west), ridge west of Nada Tunnel Road, along about 200 m of sandstone cliffline. [GPS coordinates provided for four out of seven total separate collection sites, all within 200 m of one another; only the first represented in the primary record. The rest are provided later.] | 37.82341000, -83.66703000 | | Along sandstone cliffline; collections made from plants growing within 10 m of the edge of the cliff. | | Additional GPS coordinates provided for three other sites: 37.82342, -83.66722; 37.82331, -83.66708; 37.82303, -83.66656 [all sites within 200 m of one another.] | 2109076 | WLP 684 |
| 12 | WLP 685 | NA 85861 | Amelanchier arborea (F. Michx.) Fernald | Kentucky, United States | NA | | | 2019 | COLLECTED | 06/15/2019 | Powell County; ; Red River Gorge (south), southeast end of Gritter Ridge, near the edge of a dry sandstone cliff. [GPS coordinates provided for four out of seven total separate collection sites, all within 200 m of one another; only the first represented in the primary record. The rest are provided later.] | 37.76731000, -83.74755000 | | Located near the edge of a dry sandstone cliff. Growth location was exposed and in full sun for much of the day. | Wild material | The berries were harvested predominantly from one plant located near the edge of a dry sandstone cliff. | 2109077 | WLP 685 |
| 13 | NA 87958 | NEWFS-394 | Viburnum acerifolium L. | Connecticut, United States | NA |  | | 2017 | | | | | | | Wild material | | 1954670 | NA 87958 |