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ACCESSIONPLANT NAMETAXONOMYORIGINGENEBANKIMAGEAVAILABILITYRECEIVEDSOURCE TYPESOURCE DATECOLLECTION SITECOORDINATESELEVATIONHABITATIMPROVEMENT LEVELNARRATIVE
0PI 667542TINKER BELLS OF CANTERBURYCampanula medium L. New York, United StatesOPGC1968DONATED19681113907PI 667542
1NSL 15499ANNUAL CHOICE MIXED COLORSCampanula medium L. California, United StatesOPGC1962DONATED19621071941NSL 15499
2PI 655899ARM 104Trifolium medium L. ArmeniaW6SEED2002COLLECTED08/10/2001Koshabulakh region.40.37694444, 44.263611112025Viburnum sp. bush, but also found wild Thymus, Trifolium, Dianthus, Campanula.Wild material1638597PI 655899
3NA 88552RJLSEUS2022-025Hydrangea quercifolia W. Bartram Alabama, United StatesNA2023COLLECTED12/12/2022Claiborne Bluffs area along unnamed road to boat ramp on the east side of the Alabama River at the U.S. Highway 84 bridge over the river. Common at this location and along the nearby Alabama River.31.54879700, -87.5141640040Plants are growing in part-shade to shade of mesic, well-drained, circum-neutral slopes and benches in mature mixed deciduous and evergreen woodlands with good litter layer. Soils: The underlying geology of this area is the Jackson Group Undifferentiated. The units of the Jackson Group are the Yazoo Clay and Crystal River and Moodys Branch Formations. Descriptions of the members of the Yazoo Clay follow in descending order. Shubuta Member - in western Alabama consists of light-greenish-gray to white plastic fossiliferous, calcareous clay containing irregular calcareous nodules. From the Tombigbee River eastward, the Shubuta becomes more calcareous and grades into massive clayey glauconitic limestone. Eastward from the Alabama River, equivalent beds grade into the Crystal River Formation. Pachuta Marl Member - light-greenish-grey glauconitic, fossiliferous clayey sand and sandy limestone traceable from western Alabama eastward to Covington County where it grades into the Crystal River Formation. Cocoa Sand Member - yellowish-gray firm calcareous, fossiliferous fine to medium sand or sandy limestone or greenish-grey micaceous, calcareous, very clayey sand. Calcareous and clayey sand equivalent to the Cocoa is traceable from western Alabama to the Conecuh River area. (Source: USGS Alabama Geological Map Data). The surface soil profile of this portion of the bluffs along the Alabama River are characterized as Saffell-Lucy (Flomaton) Series Complex soils. The Saffell Series consists of very deep, well drained, moderately permeable soils that formed in loamy and gravelly marine sediments of the Tertiary Age and have acid reaction. These soils are found on the upper portion of the bluffs along the Alabama River. The Lucy Series consists of very deep, well drained, moderately permeable soils on uplands. They formed in sandy and loamy marine and fluvial sediments of the Southern Coastal Plain Major Land Resource Area. Soil reaction runs from strongly to moderately acid. The Flomaton Series consists of very deep, excessively drained, rapidly permeable soils on uplands of the Southern Coastal Plain Major Land Resource Area. They formed in gravelly sandy marine sediments and also have an acid reaction. The remainder of soils are of miscellaneous origin. (Source: USDA-NRCS Official Soil Series Descriptions).Wild material2140779NA 88552