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ACCESSIONPLANT NAMETAXONOMYORIGINGENEBANKIMAGEAVAILABILITYRECEIVEDSOURCE TYPESOURCE DATECOLLECTION SITECOORDINATESELEVATIONHABITATIMPROVEMENT LEVELNARRATIVE
0WLP 1686APS/RS/2019/067/396Rosa setigera Michx. Arkansas, United StatesNAFRUIT2019COLLECTED11/07/2019Located near intersection of Smith Mountain Road and Newton County 8828 Road approximately 6.00 miles north of Deer, Newton County35.91212000, -93.21112000636Roadside, upland with rocky soilsWild material2097789WLP 1686
1NA 89114TLM25-03Zanthoxylum clava-herculis L. Texas, United StatesNA2025COLLECTED07/09/2025Jackson County Road 113, Bergston Road, approximately 2.1 kilometers north of the junction with Jackson County Road 234; growing on the west side of the road along a fenceline running parallel to the road.29.00576600, -96.7629850024Plants are growing in full sun to light shade along a fence line near where cattle graze and the dirt road. The area is disturbed, but somewhat overgrown since there is very little traffic on the road that is primarily used by farmers and ranchers to access their fields. Slope: 0 to 1 percent. Aspect: N/A. Soils: The soils of this area sampled are classified as Laewest clay, 0 to 1 percent slopes (LaA). The Laewest Series consists of very deep, moderately well drained soils that formed in clayey flood basin deposits on alluvial plains or deltas of the Beaumont Formation of Pleistocene Age. These nearly level to gently sloping soils are on broad flat coastal plains. Slope ranges from 0 to 8 percent. The solum thickness is more than 200 cm and ranges from slightly acidic on the surface to neutral in deeper pedons. This is a cyclic soil and undisturbed areas have gilgai microrelief with microhighs 15 to 30 cm higher than microlows. Distance from the center of the microhighs to the center of the microlows ranges from about 1.2 to 4.9 m. The microhigh makes up about 20 percent, the intermediate, or area between the knoll and depression about 50 percent, and the microlow about 30 percent. The amplitude of waviness between mollic colored materials in the upper part of the solum and the higher value colors in the lower part ranges from about 30 to 150 cm. When dry, the soil has cracks 1 to 5 cm wide at the surface and commonly 1 cm wide cracks extend to a depth of 1.2 m during the summer. The cracks remain open for less than 90 cumulative days in most years. Some pedons have an overwash of calcareous clay or silty clay 20 to 51 cm thick. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). Geology: The underlying geology of this area is Lizzie Formation of Quaternary, Middle Pleistocene age. It is comprised of sand, silt, clay, and minor amount of gravel. Iron oxide and iron-manganese nodules are common in zones of weathering; locally calcareous. Surface is fairly flat and featureless except for many shallow depressions and pimple mounds. Moore and Wermund (1993a) mapped three units--(1) alluvium undifferentiated as to texture and origin--includes meander belt, levee, crevasse splay, and distributary sand, and flood-basin mud deposits, about 60 m thick, (2) fine-grained channel facies (alluvial sand, silt, and clay) about 10-25 m thick, thicker seaward, and (3) fine-grained overbank facies (alluvial silt and clay) about 55-65 m thick, thicker seaward. Together, these deposits form a deltaic plain that parallels the Gulf Coast. Unit contains Pleistocene vertebrate fauna, dips seaward beneath the Beaumont Fm. and disconformably overlies deposits of the Pliocene and early Pleistocene Willis Formation. The deltaic plain is entrenched as much as 7 m by streams. In Hidalgo County (southernmost part of Texas) the unit underlies a semiarid plain, widely irrigated and cultivated. Unit is locally veneered with thin, discontinuous stabilized eolian sand. (Source: USGS Texas Geologic Map Data).Wild material2191653NA 89114
2Ames 35951AS/ML/2022/020/151Monarda lindheimeri Engelm. & A. Gray Texas, United StatesNC7SHOOT2022COLLECTED08/07/2022Located northwest of Navasota approximately 5.60 miles along Old Highway 6.30.44628200, -96.1533320067Powerline cut.Wild materialAccession consisting of both white flowering specimens and multi-colored (pinkish) flowering specimens. Inventory 01 represented as rather robust plants up to 40" tall that display a rather to somewhat clump type growth habit (possibly due to growing in more of a prairie habitat/full sun), but also includes adjacent specimens that are rhizomatous. Inventory 02 represents a more rhizomatous growth habit and shorter in height (e.g. less than 20" tall). Plants sampled ranging from 1.0-4.5' in height. 2140541Ames 35951
3Ames 32892APS/GD/2015/014/196Gymnocladus dioicus (L.) K. Koch Oklahoma, United StatesNC7Fruit2015COLLECTED03/13/2015Wagoner County: Billy Creek watershed, T17N R17E NE 1/4 Sec. 22. McClellen-Kerr Wildlife Management Area (Billy Creek WDU) portion approximatley 4 miles west, southwest of Wagoner.35.94442000, -95.48112700171Floodplain.Wild material1925358Ames 32892