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ACCESSIONPLANT NAMETAXONOMYORIGINGENEBANKIMAGEAVAILABILITYRECEIVEDSOURCE TYPESOURCE DATECOLLECTION SITECOORDINATESELEVATIONHABITATIMPROVEMENT LEVELNARRATIVE
0WLP 876AF2018-004Celtis laevigata Willd. Virginia, United StatesNA2018COLLECTED09/10/2018Suffolk County; ; Lone Star Lakes Park, ca 1 mile from entrance on a gravel road near parking for a Crane Lake boat ramp.36.86919000, -76.575500004Roadside near lake.Herbarium voucher collected (see barcode NA0103773).2108853WLP 876
1NA 79090MANOS05-06Celtis laevigata Willd. North Carolina, United StatesNA2010COLLECTEDPRE 07/01/2010Penny's Bend State Nature Preserve, on the Eno River near DurhamWild material1898065NA 79090
2WLP 775LA002-2006Celtis laevigata Willd. Louisiana, United StatesNA2006COLLECTED12/28/2006Louisiana: Terrebonne Parish, Shrimp Row south of Dulac along Grand Canal29.38176000, -90.715930005Coastal marsh, 0, Mixed shrubWild material1913887WLP 775
3NA 75357RL 091Celtis laevigata Willd. Georgia, United StatesNA2006COLLECTED07/01/2004Georgia, Walker County, Pigeon Mountain Wildlife Management Area; Pocket Branch, east side of barn at old homesite.Wild material1777635NA 75357
4DLEG 900440DLEG 900440Neltuma laevigata (Humb. & Bonpl. ex Willd.) Britton & Rose San Luis Potosí, Mexico SEEDHistoric1990COLLECTED08/17/1990Hwy 57, 4.6 mi. W of Ciudad del Maiz.Growing with Celtis pallida adjacent to fields.Wild materialSpreading trees to 30 ft. tall. M. Johnson 90-194. 1526455DLEG 900440
5PI 709491LBJWC-MM-794Setaria scheelei (Steud.) Hitchc. Texas, United StatesNC7GREENHOUSE2007COLLECTED11/19/2006Blanco Shoals Greenbelt, Interstate Highway 35 at the Blanco River.29.90241000, -97.89913000180Moist or mesic. Soil Texture: Sandy loam, light gray. Population size 400.Wild material1726927PI 709491
6PI 664901JM20061003Teucrium canadense L. Missouri, United StatesNC72006COLLECTED09/25/2006Mile marker 222.1, Route 66 off of Interstate 44, southwest of Meramec State Park, West Sullivan, Crawford County.38.18194444, -91.20194444301Roadside prairie remnant (between railroad and state road). Ambrosia artemisiifolia, Andropogon gerardii, Celtis laevigata, Elaeagnus angustifolia, Eryngium, Helianthus mollus, Rhus glabra, Schrankia nuttallianum, and Sorghastrum nutans.Wild material1715759PI 664901
7NA 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
8NA 89115TLM25-04aHamamelis ovalis S. W. Leonard Texas, United StatesNA2025COLLECTED07/10/2025State Highway 87 approximately 3.25 kilometers north of the crossroad junction with Texas Recreational Road 255 (RE 255); plants were growing in the narrow buffer woods along the east side of the highway.31.12051300, -93.72628100138The habitat is an upland mixed coniferous and deciduous woodlands in part to full shade and dry conditions, often under drought stress. Plants seem to always occur on the top of dry ridges or well-drained slopes. Slope: 0 to 1 percent. Aspect: N/A. Soils: The soils of this collection area are classified as Tehran-Letney Association, hilly (TLE) soils. The Tehran Series (55%) consists of deep, somewhat excessively drained, moderately rapidly permeable soils on uplands. They formed in thick loamy and sandy sediments on the Western Coastal Plain. These soils are on gently sloping to moderately steep uplands with slopes ranging from 1 to 20 percent. The Letney Series (30%) consists of deep, well drained, moderately rapidly permeable, upland soils. They formed in thick sandy and loamy sediments of the coastal plains. These soils are on gently sloping to moderately steep uplands with slopes ranging from 1 to 20 percent. Soil pH ranges from 4.5 to 6.0. The minor soil components include Doucette Series (10%) and Boykin Series (5%) soils. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). Geology: The underlying geology of this area is of Oligocene origin and characterized as Catahoula Formation. This formation is extensive and deep in Texas, up to 185 meters thick. In the area of the collection the Catahoula Formation is primarily mudstone and sand. The upper 90-150 meters is mudstone that is tuffaceous, and sandy; also, occasionally, with some bentonitic clay. (Source: USGS Texas Geologic Map Data).Wild material2191654NA 89115
9DPRU 3558CONS24-044Prunus minutiflora Engelm. ex A. Gray Texas, United StatesDAV2024COLLECTED06/17/202430.72248000, -98.00497000360Grassy scrub in railroad right-of way. Exposure open to 3/4 shadeWild materialOnly seed can be requested of this accession!! This donation is approximately half of a collection of 896 seeds from 76 maternal lines. An additional 137 seeds were collected in bulk for germination testing and grow out for a total collection size of 1,033 seeds. The population of over 200 plants covered an area of approximately 150m x 3m on thin, clay soil over limestone. Representative vegetation insluded Juniperus ashei, Celtis laevigata, Sideroxylon lanuginosum, Berberius trifoliolata, Rhus aromatica, Eriogonum longifolium, Krameria lanceolata, Gaillardia pulchella, Hedeoma acinoides, and Warnockia scutellarioides. Plant type is locally abundant, but uncommon throughout range.2170978DPRU 3558
10NA 88801TJK2023LA/TX-001Cocculus carolinus (L.) DC. Louisiana, United StatesNA2023COLLECTED11/21/2023Interstate 20, westbound, approximately 13 miles west of Mississippi River, 9 miles east of U.S. Highway 65.32.33740000, -91.0632000024Damp low, wooded treeline. Slope: less than 2%. Aspect: Southwest. Elevation: 79 feet.Wild material2159184NA 88801
11NA 88802TJK2023LA/TX-002Ilex decidua Walter Louisiana, United StatesNA2023COLLECTED11/21/2023Interstate 20, westbound, approximately 6 miles west of U.S. Highway 65 and 7.5 miles east of Louisiana Highway 577. Tensas River watershed.32.41950000, -91.2967000021Damp wooded treeline. Slope: 12%. Aspect: West-southwest. Elevation: 69 feet.Wild material2159185NA 88802
12NA 88803TJK2023LA/TX-003Crataegus viridis L. Louisiana, United StatesNA2023COLLECTED11/21/2023Interstate 20, westbound, approximately 7 miles west of Louisiana Highway 17 and 8.5 miles east of U.S. Highway 425. Tensas River watershed.32.41940000, -91.2967000021Damp wooded treeline. Slope: 12%. Aspect: West-southwest. Elevation: 69 feet.Wild material2159186NA 88803
13NA 88804TJK2023LA/TX-004Crataegus viridis L. Louisiana, United StatesNA2023COLLECTED11/21/2023Walnut Bayou (Mississippi River bottom): Interstate 20, westbound, approximately 10 miles west of the Mississippi River and 8.25 miles east of U.S. Highway 65.32.34130000, -91.0717000026Damp wooded treeline. Slope: 10%. Aspect: North-northeast. Elevation: 84 feet.Wild material2159187NA 88804
14NA 88805TJK2023LA/TX-005Carya aquatica (F. Michx.) Elliott Louisiana, United StatesNA2023COLLECTED11/21/2023Interstate 20, westbound, approximately 2 miles west of Louisiana Highway 609 and 0.75 miles east of Louisiana Highway 183.32.45620000, -91.6147000023Damp gallery woods, edge of palmetto flat. Slope: 5%. Aspect: North. Elevation: 76 feet.Wild material2159188NA 88805
15WLP 3217TJK2023TX-002Styphnolobium affine (Torr. & A. Gray) Walp. Texas, United StatesNA2023COLLECTED08/27/2023In the vicinity of Pilot Knob, an extinct cretaceous volcano situated about 8 miles south of Austin. Only exposed submarine volcano known in Texas. Onion Creek Watershed. Off Dee Gabriel Collins Rd/FM 812, approximately .38 of a mile east of McKinney Falls Pkwy and 1.5 miles west of Hwy 183.30.17484700, -97.71519000188Roadside environment. Highly modified ROW; trees growing in pushed up soil, gravel, road aggregate, caliche. Well established trees growing in a large motte - 20’ x 50’ area. Elevation: 617 feet. Slope: 7%. Aspect: South.Wild material2158761WLP 3217
16NA 87354TJK2022TX-002Ptelea trifoliata L. Texas, United StatesNA2023COLLECTED11/29/2022Blanco County: Little Blanco Road, upper slope off Little Blanco River; 330 feet west of Highway 281.30.00140000, -98.40650000390Shaded streamside slope between road and Little Blanco River.Wild material2141645NA 87354
17NA 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
18NA 88553RJLSEUS2022-026Hydrangea arborescens L. 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. Occasionally found in the woodlands. 31.54940700, -87.5136620025Plants are growing in part-shade to shade of mesic, well-drained, circum-neutral slopes mature mixed deciduous and evergreen woodlands where slopes are exposed and detritus does not build up.
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 (https://mrdata.usgs.gov/geology/state/state.php?state=AL)
The surface soil profile of this portion of the bluffs along the Alabama River are characterized by 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 (https://soilseries.sc.egov.usda.gov/osdname.aspx)
Wild material2140780NA 88553
19NA 88558RJLSEUS2022-031Ilex decidua Walter Alabama, United StatesNA2023COLLECTED12/12/2022Silver Creek Lake Campground off of Silver Creek Lake Road: Silver Creek Lake, at the edge of the campground.31.66344600, -87.5710840016Part shade to sun along the eroding banks of Silver Creek Lake in moist-mesic, mixed deciduous and evergreen woodland, 2-3 meters above the water. The underlying geology of this area is Claiborne Group, Tallahatta Formation, of Eocene origin, with white to very light-greenish-gray thin-bedded to massive siliceous claystone; interbedded with thin layers of fossiliferous clay, sandy clay, and glauconitic sand and sandstone. (Source: USGS Alabama Geological Map Data). The primary soil types in the collection area are classified as Riverview Fine Sandy Loam soils (0 to 2 percent slopes, occasionally flooded). The Riverview Series consists of very deep, well drained, moderately permeable soils that formed in loamy alluvium on flood plains. Slopes range from 0 to 5 percent. Riverview soils fare on high parts of flood plains of rivers and streams draining the Coastal Plain and Southern Piedmont. Runoff is slow. Permeability is moderate. These soils flood for short periods mostly in winter or early spring months. (Source: NRCS Web Soil Survey).Wild material2140819NA 88558
20Ames 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
21Ames 35953AS/ML/2022/022/153Monarda lindheimeri Engelm. & A. Gray Texas, United StatesNC7FLOWER2022COLLECTED08/07/2022Located 4.98 miles west of Millican on the south side of FM 2154 Rd.30.50280100, -96.2848380094Roadside, railroad right-of-way.Wild materialPopulation extending just over 2.00 miles represented as very vigorous, rhizamatous specimens. In comparison to other M. lindheimeri noted in Texas in 2022, this population is one of the earliest flowering populations, nearly 2-3 weeks earlier typically peaking in mid-April. In 2022, population peaked flower on 18 April. 2140543Ames 35953
22Ames 35956AS/ML/2022/025/156Monarda lindheimeri Engelm. & A. Gray Texas, United StatesNC7SHOOT2022COLLECTED08/05/2022Located just south of Bedias approximately 4.34 miles on highway 90 N (east side).30.71054100, -95.9655450098Roadside, woodland edge.Wild material2140546Ames 35956
23WLP 2568APS/HA/2022/028/490Hydrangea arborescens L. Arkansas, United StatesNAHABITAT2022COLLECTED03/15/2022Located approximately 3.75 miles east of Allison just off Round Bottom Road.35.93357000, -92.05110000144Moist, low deciduous forest with scattered rock outcrops, growing along base of hill and bank of seasonal stream. Wild material2137430WLP 2568
24OPGC 8394NM080-272Ratibida columnifera (Nutt.) Wooton & Standl. New Mexico, United StatesOPGC2021Wild materialInflorescence columniferous 1/2-1 inch, composite flower with yellow/maroon ray flowers2120648OPGC 8394
25WLP 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
26OPGC 7309AZ930-361Polanisia dodecandra (L.) DC. Arizona, United StatesOPGCSEED2018Wild material1970377OPGC 7309
27W6 55556NM030-99Sporobolus contractus Hitchc. New Mexico, United StatesW6SEED2018Wild material1970267W6 55556
28W6 55665AZ930-360Neltuma velutina (Wooton) Britton & Rose Arizona, United StatesW6SEED2018Wild materialProsopis velutina1970376W6 55665
29NA 85021JDC/SS/2018/004/817Sapindus saponaria L. var. drummondii (Hook. & Arn.) L. D. Benson Oklahoma, United StatesNAImage2018COLLECTED03/12/2018Private property approximately 4.8 miles southeast of Mulhall, north side of Cimarron River, T18N R2W, Logan County35.99972000, -97.39735900210Transition zone between higher elevations and bottomlands.Wild material1957958NA 85021
30Ames 32891APS/GD/2015/010/192Gymnocladus dioicus (L.) K. Koch Oklahoma, United StatesNC7Fruit2015COLLECTED03/12/2015Nowata County: T25N R16E NW 1/4 NE 1/4 Sec. 3. Oologah Wildlife Management Area approximately 3 miles east of Nowata.36.68401000, -95.58207800208Transition zone between higher elevations and bottomlands. Wild material1925357Ames 32891
31Ames 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
32Ames 32894APS/GD/2015/017/199Gymnocladus dioicus (L.) K. Koch Oklahoma, United StatesNC7Fruit2015COLLECTED03/14/2015Cleveland County: T10N R5W SW 1/4 SW 1/4 Sec. 7. John Nichols Camp located on north side of Canadian River approxiamtely 4.25 miles south and southeast of Mustang.35.35029600, -97.66952200395Higher elevations. Dry, relatively thin soils. Wild material1925360Ames 32894
33Ames 32887APS/GD/2015/003/185Gymnocladus dioicus (L.) K. Koch Arkansas, United StatesNC7Fruit2015COLLECTED03/04/2015Stone and Izard Counties: White River watershed, Ozark National Forest, Sylamore State Wildlife Management Area near Allison.35.95017300, -92.11129600126Floodplain, base of slopes.Wild material1924365Ames 32887
34NA 88308MSB210535Cocculus carolinus (L.) DC. Texas, United StatesNASEED2011Wild material1895239NA 88308
35W6 42878MSB231372Phacelia congesta Hook. Texas, United StatesW6SEED2011Wild material1895336W6 42878
36W6 42885MSB210513Pluchea odorata (L.) Cass. Texas, United StatesW6SEED2011Wild material1895343W6 42885
37W6 42888MSB203018Polytaenia nuttallii DC. Texas, United StatesW6SEED2011Wild material1895346W6 42888
38W6 42008RMRS-1257Hesperostipa comata (Trin. & Rupr.) Barkworth Oregon, United StatesW6SEED2011Wild material1887321W6 42008
39WLP 2124NM930-034Fallugia paradoxa (D. Don) Endl. ex Torr. New Mexico, United StatesNASEED2009COLLECTED07/01/2007Ice Canyon, half way up hiking trail to Dripping Springs. Arroyo at part of Oregon Mountains.32.32297000, -106.582580001800Arroyo. Land used as recreation natural area. Soil is very gravelly sand loam; color 10YR 4/3 brown.Wild material1802217WLP 2124
40Ames 29649JDC/FP/2008/049/119Fraxinus pennsylvanica Marshall Illinois, United StatesNC7HABITAT2008COLLECTED10/10/2008Horseshoe Lake Conservation Area, SW 1/4 of NW 1/4 of Section 4, T16S, R2W, Tamms Quad, Alexander County.37.15333333, -89.34277778100Wild material1788204Ames 29649
41Ames 29654JDC/FP/2008/038/108Fraxinus pennsylvanica Marshall Missouri, United StatesNC7SEED2008COLLECTED10/08/2008Along White Sands Road, near Magnolia Hollow Conservation Area, T38N, R8E, Bloomsdale Quad, Ste. Genevieve County.38.01277778, -90.18888889119Along bankside of creek. Wild materialA couple of original specimens were very tall (80 feet).1788209Ames 29654
42WLP 1112LBJWC-1141Crataegus viridis L. Texas, United StatesNA2008COLLECTED11/16/2007Mann Tract, Trinity River National Wildlife Refuge, southwest of the City of Hardin.30.13738000, -94.775050000Fencerow/bottomland hardwood mixed forest, flat, clayey soil.Wild material1781868WLP 1112
43WLP 2304LBJWC-MM-755Zanthoxylum hirsutum Buckley Texas, United StatesNA2006COLLECTED07/19/2006Stevenson Nature Preserve.30.03711000, -97.82372000245Arid; brown, sandy clay loam soil over Cretaceous limestone.Wild material1719704WLP 2304
44Ames 10332MPW207Torilis arvensis (Huds.) Link Oklahoma, United StatesNC71989COLLECTED07/31/1989Scrubby edge along road with Vitis, Celtis laevigata, and Ambrosia trifida.36.23333333, -95.86666667179Wild materialCollection site Mohawk Park, Tulsa, Tulsa Co., Oklahoma.1052355Ames 10332