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ACCESSIONPLANT NAMETAXONOMYORIGINGENEBANKIMAGEAVAILABILITYRECEIVEDSOURCE TYPESOURCE DATECOLLECTION SITECOORDINATESELEVATIONHABITATIMPROVEMENT LEVELNARRATIVE
0NA 84666PCC17-TNKY-017Aesculus flava Sol. Kentucky, United StatesNA2017COLLECTED10/01/2017Brigadoon State Nature Preserve.36.89931000, -85.98720000198Mesic slope that drains into reservoir.Wild material2108768NA 84666
1NA 81520NA 81520Aesculus flava Sol. North Carolina, United StatesNA2013COLLECTED09/23/2012Bearpen Knob at Craggy Gardens in the picnic area on the north side of the Blue Ridge Parkway.35.69954000, -82.392580001591Growing in open woodlands and mown hillside areas from part shade to full sun.1950672NA 81520
2NA 81179RJLNC2012-001Aesculus flava Sol. North Carolina, United StatesNA2012COLLECTED10/15/2012Wild material1914204NA 81179
3NA 70437MWPCC 00-109Aesculus flava Sol. Georgia, United StatesNA2000COLLECTED09/18/2000Walker Co. GA, Pigeon Mountain, on trail at end of Pocket road.34.70888889, -85.37527778300Two plants above waterfall, one immediately by streambed, other more than 30 ft. up slole, on a limestone outcrop.Wild materialSlope 15 degrees, Aspect SW, half shaded, soil type thin grittysoil eroded limestone, thin organic layer.1606349NA 70437
4NA 61265NA 61265Aesculus flava Sol. Virginia, United StatesNA1989COLLECTED09/26/198938.00285700, -79.45777100212Wild material1495992NA 61265
5WLP 3433RM2023-002Clethra acuminata Michx. Georgia, United StatesNA2024COLLECTED10/21/2023Plants growing along Patterson Gap Road.34.97299200, -83.46003100789Plants growing in part shade in a very dry and rocky, mostly deciduous habitat. The site is steeply sloped, underlain by rock, with rocky outcrops. Slope: 15 percent. Aspect: Variable. The underlying geology of this area is Biotite Gneiss, primarily of Precambrian-Paleozoic origin. (Source: USGS North Carolina Geologic Map Data.) The primary soil type in the collection area is classified as Tusquitee loam, 10 to 25 percent slopes. The Tusquitee series consists of very deep, well drained soils on gently sloping to very steep benches, foot slopes, toe slopes, and fans in coves in the Southern Blue Ridge mountains, MLRA 130B. These soils formed in colluvium derived from materials weathered from igneous and high-grade metamorphic crystalline rocks such as granite, mica gneiss, hornblende gneiss, and schist. Slope ranges from 2 to 95 percent. The surface layer to 5cm deep is comprised of moderately decomposed organic matter and leaves, twigs, and roots. Layers to 2m deep range from very dark grayish brown to brown sandy loam with weak medium and coarse granular structure that is friable. A few fine flakes of mica can be found and these soils are very strongly acid. (Source: NRCS Web Soil Survey.)Wild material2166142WLP 3433
6WLP 157NACPEC19-026Carpinus caroliniana Walter Kentucky, United StatesNA2019COLLECTED09/09/2019Madison County; Berea College Forest: Gabertown Road, near junction of Gabertown Road (KY 1617) + Scaffold Cane (KY595)37.54309800, -84.27086000292Former Pinus taeda plantationWild material2110469WLP 157
7WLP 1220JDC/HA/2009/108/258Hydrangea arborescens L. Ohio, United StatesNA2009COLLECTED10/18/2009Along Old US 68, just northeast of Levanna, Russellville Quad, Brown County.38.78250000, -83.85222222265Steep, rocky north facing slope. Underground seep present. Associated with Aesculus flava, Fraxinus americana, Liriodendron tulipifera, and Quercus.Wild material1823928WLP 1220