| 0 | NA 89158 | 2025RJLSEUS-06 | Cornus florida L. | Alabama, United States | NA | | | 2025 | COLLECTED | 10/01/2025 | Coosa Wildlife Management Area: along the edge of gated dirt road on the west side of Coosa County Road 29, 0.3 kilometers north of Hatchet Creek. | 32.86402200, -86.33871400 | 108 | Plants are growing in part sun to shade on dry-mesic slopes above the road cut on the gated dirt road; most likely a road for access for fire control/forest management. The forest is a combination of deciduous and evergreen with evergreens primarily comprised of Pinus taeda. The habitat was quite dry during this time of year. Slope: 5 to 20 percent. Aspect: North. Soils: The primary soil in the area of this collection is classified as Madison-Louisa Series complex, 15 to 30 percent slopes, moderately eroded (MdE2). The Madison Series soils are very deep, well drained soils with medium runoff found on Piedmont uplands in interstream divides, ridges and side slopes. They are comprised of residuum weathered from felsic or intermediate, high-grade metamorphic or igneous rocks high in content of mica. Slopes range from 2 to 60 percent and soil is typically strongly acidic. Louisa Series soils The Louisa Series soils consist of shallow, somewhat excessively drained soils which formed over mica gneiss and schist bedrock. They occur on Piedmont uplands. Slopes are 6 to 80 percent. This soil is moderately acid. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). Geology: The underlying geology of this area is of Precambrian to Paleozoic origin and characterized as Hatchet Creek Group; Pinchoulee Gneiss Formation. It is characterized by medium to fine-grained migmatitic, locally garnetiferous biotite-feldspar gneiss, commonly saturated with granitic pods. (Source: USGS Alabama Geologic Map Data). | Wild material | | 2193004 | NA 89158 |
| 1 | NA 89115 | TLM25-04a | Hamamelis ovalis S. W. Leonard | Texas, United States | NA | | | 2025 | COLLECTED | 07/10/2025 | State 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, -93.72628100 | 138 | The 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 material | | 2191654 | NA 89115 |
| 2 | NA 88981 | TXWL2025-031 | Ilex opaca Aiton | Texas, United States | NA | | | 2025 | COLLECTED | 01/07/2025 | South of Jericho community. | 31.67015000, -94.25641000 | | Western sandy lands; small grove of Ilex opaca in upland position above a baygall. Bare ground cover with Ilex opaca regeneration. Adjacent to a loblolly pine plantation and a new longleaf pine plantation. | Wild material | | 2170965 | NA 88981 |
| 3 | NA 88982 | TXWL2025-032 | Ilex opaca Aiton | Texas, United States | NA | | | 2025 | COLLECTED | 01/07/2025 | South of Jericho community. | 31.66973000, -94.25613000 | | Western sandy lands; edge of small grove of Ilex opaca with sun exposure in upland position above a baygall. Bare ground cover with Ilex opaca regeneration. Adjacent to a new longleaf pine plantation located on fireline. | Wild material | | 2170966 | NA 88982 |
| 4 | NA 88718 | RJL2023NCSC-023 | Ilex decidua Walter | South Carolina, United States | NA | | | 2023 | COLLECTED | 11/15/2023 | Waccamaw National Wildlife Refuge: U.S. Highway 701, Yauhannah Landing on the east side of the Great Pee Dee River. Plants growing in low woods on the north side of the landing. | 33.66208900, -79.15305000 | 2 | Plants growing in shade to part-shade of a moist to wet woodland habitat that is mostly deciduous and evergreen. Portions of the woodland have depressions with year-round standing water. Slope: N/A. Aspect: N/A. The underlying geology of this area is of Quaternary origin and characterized as Alluvial Valley Swamp. This formation is unconformable on all underlying units. It is composed of fluvial sand and gravel at base, grading upwards into fine sands and silts, and local occasional peat. May be overrun with recent sediments from forest cutting and agriculture. (Source: USGS South Carolina Geologic Map Data.) The primary soil type in this collection area is classified as Johnston Series loam. The Johnson Series consists of very deep, very poorly drained coarse-loamy, siliceous, active, acid, thermic Cumulic Humaquepts. The upper 0-75 cm is black, mucky loam that is friable and very strongly acid. The lower stratum to 1.75 m is dark gray, loamy fine sand, single grained, loose and very strongly acid. (Source: NRCS Web Soil Survey.) | Wild material | | 2159146 | NA 88718 |
| 5 | Ames 36170 | Lake Catherine State Park | Ptelea trifoliata L. | Arkansas, United States | NC7 |  | | 2023 | COLLECTED | 08/27/2023 | Lake Catherine State Park approximately 10 miles southeast of Hot Springs. Localized to the ridge top of Dam Mountain on the south shore of the southeast arm of the reservior, starting approximately 0.25 miles southwest of the dam. T3S R18W Sec. 35. | 34.42452200, -92.90218400 | 199 | Dry ridge top. Predominantly on the north facing edge of ridge. | Wild material | A localized but very dense population. Ptelea is the dominant understory species in this location. | 2158789 | Ames 36170 |
| 6 | NA 88543 | RJLSEUS2022-015 | Rhododendron alabamense Rehder | Georgia, United States | NA | | | 2023 | COLLECTED | 12/09/2022 | Plants growing above a pond in drier upland conditions as well as along the banks of the Muckalee Creek on the property of Monica Williams north of Albany, Georgia. Infrequent, but occasionally seen in drier woods; more common along Muckalee Creek. | 31.63566400, -84.13379600 | 61 | Plants are growing in part-shade to shade of well-drained to drier understory conditions of a mixed evergreen and deciduous woodland, approximately 2 meters above Muckalee Creek, on sandy benches where occasional scouring has resulted in lower competition. Plants are occasionally impacted by flooding; however, they are not subjected to extended periods of high moisture on a regular basis.
Soils: The underlying geology of this area is of Eocene origin and characterized as Ocala Limestone. The Ocala Limestone consists of almost pure limestones with occasional dolomites. It can be subdivided into both lower and upper facies with the lower facies composed of a whitish to cream-colored, fine to medium grained, poorly to moderately hard, fossil rich grainstone and packstone. The upper Ocala is white and somewhat weak and poorly sorted. It is extremely fossil rich grainstone, packstone and wackestone and some chert is common in the upper facies.
Source: USGS Georgia Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=GANu%3B1)
The primary soil types in the collection area are classified as Herod and Muckalee Series soils. The Herod Series consists of poorly drained moderately permeable soils formed in loamy alluvium. These soils are on flood plains of streams in the Coastal Plain. Slopes range from 0 to 2 percent. The Muckalee Series consists of poorly drained moderately permeable soils formed in loamy and sandy alluvium. These soils are on flood plains of streams in the Coastal Plain. Slopes range from 0 to 2 percent.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2140769 | NA 88543 |
| 7 | NA 88552 | RJLSEUS2022-025 | Hydrangea quercifolia W. Bartram | Alabama, United States | NA | | | 2023 | COLLECTED | 12/12/2022 | Claiborne 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, -87.51416400 | 40 | Plants 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 material | | 2140779 | NA 88552 |
| 8 | NA 88553 | RJLSEUS2022-026 | Hydrangea arborescens L. | Alabama, United States | NA | | | 2023 | COLLECTED | 12/12/2022 | Claiborne 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, -87.51366200 | 25 | Plants 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 material | | 2140780 | NA 88553 |
| 9 | Ames 35948 | AS/ML/2022/017/147 | Monarda lindheimeri Engelm. & A. Gray | Texas, United States | NC7 |  | | 2022 | COLLECTED | 08/06/2022 | Located near Grimes County line along highway 6 approximately 6.5 miles north of Hempstead. | 30.22891300, -96.05532600 | 68 | Woodland edge. | Wild material | Plants in nature measuring up to approximately 3.0-3.5' in height with very long internodes. Extreme variation noted on stem color from green, to purple to green with purple edges. | 2140538 | Ames 35948 |
| 10 | Ames 35949 | AS/ML/2022/018/149 | Monarda lindheimeri Engelm. & A. Gray | Texas, United States | NC7 |  | | 2022 | COLLECTED | 08/06/2022 | Located approximately 5.47 miles southeast of Navasota on County Road 314 just south of highway 105 (0.4-0.8 miles). | 30.35463000, -96.00678200 | 83 | Fenceline, grazed pasture and woodland edges. | Wild material | Plants in nature measuring up to approximately 32" in height with average height at 24". | 2140539 | Ames 35949 |
| 11 | Ames 35951 | AS/ML/2022/020/151 | Monarda lindheimeri Engelm. & A. Gray | Texas, United States | NC7 |  | | 2022 | COLLECTED | 08/07/2022 | Located northwest of Navasota approximately 5.60 miles along Old Highway 6. | 30.44628200, -96.15333200 | 67 | Powerline cut. | Wild material | Accession 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. | 2140541 | Ames 35951 |
| 12 | Ames 35954 | AS/ML/2022/023/154 | Monarda lindheimeri Engelm. & A. Gray | Texas, United States | NC7 |  | | 2022 | COLLECTED | 08/07/2022 | Located just southwest of College Station on both Los Robles Dr and White Creek Rd. | 30.57630900, -96.38686600 | 91 | Roadside, woodland edge and savannah. | Wild material | Very rhizamatous specimens noted in nature. 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. | 2140544 | Ames 35954 |
| 13 | Ames 35955 | AS/ML/2022/024/155 | Monarda lindheimeri Engelm. & A. Gray | Texas, United States | NC7 |  | | 2022 | COLLECTED | 08/05/2022 | Located just north of Roans Prairie approximately 1.27 miles on highway 90 N. | 30.60214700, -95.94961100 | 116 | Roadside, woodland edge. | Wild material | | 2140545 | Ames 35955 |
| 14 | Ames 35956 | AS/ML/2022/025/156 | Monarda lindheimeri Engelm. & A. Gray | Texas, United States | NC7 |  | | 2022 | COLLECTED | 08/05/2022 | Located just south of Bedias approximately 4.34 miles on highway 90 N (east side). | 30.71054100, -95.96554500 | 98 | Roadside, woodland edge. | Wild material | | 2140546 | Ames 35956 |
| 15 | Ames 35957 | AS/ML/2022/026/157 | Monarda luteola Singhurst & W. C. Holmes | Texas, United States | NC7 |  | | 2022 | COLLECTED | 08/05/2022 | Located north of Palestine approximately 3.60 miles on AN Country Road 404 (west side) just 0.7 miles north from intersection with AN Country Road 403 | 31.81051200, -95.63928400 | 185 | Roadside, woodland edge. | Wild material | Lemon-scented foliage when crushed. Population in nature noted slightly prior to peak flowering on 28 April (2022) at collection site. | 2140547 | Ames 35957 |
| 16 | Ames 35792 | APS/ID/2022/027/489 | Ilex decidua Walter | Arkansas, United States | NC7 |  | | 2022 | COLLECTED | 03/15/2022 | Located approximately 3.75 miles east of Allison just off Round Bottom Road. | 35.93670000, -92.04891000 | 133 | Dry west facing slope in a pine, oak, and hickory forest. | Wild material | Plants sampled in nature with bright red fruits measuring 7-9 mm in diameter. | 2137431 | Ames 35792 |
| 17 | NA 86885 | RJL2021PA-004 | Ilex verticillata (L.) A. Gray | Pennsylvania, United States | NA | | | 2021 | COLLECTED | 11/16/2021 | Plants growing in woodlands along a small unnamed creek corridor dumping into the Middle Branch White Clay Creek in Goddard Park, West Grove Pennsylvania, off of Wickerton Road, Chester County. | 39.81063861, -75.82750806 | 124 | Plants are growing in a range of habitats from mesic woodlands to saturated streamside settings of deciduous woodlands that drain toward the Middle Branch White Clay Creek. Plants grow in high understory shade with dappled to indirect sunlight. The only female (fruiting) plants were found in areas along the creek where soils are moist to saturated. Numerous male specimens were found in the areas described above. Soils: Soils found in the areas where this collection was made are comprised primarily of Baile silt loam (Ba), Hatboro silt loam (Ha), and Glenelg silt loam, 8 to 15 percent slopes (GgC). Baile silt loam consists of very deep, poorly drained, moderately low to moderately high saturated hydraulic conductivity, soils on upland depressions and footslopes that were formed in local alluvium over residuum from acid crystalline rocks, chiefly mica schist and granitized schist and gneiss; slope ranges from 0 to 8 percent. Hatboro silt loam consists of very deep and poorly drained soils formed in deposited alluvium derived from metamorphic and crystalline rock. They are on flood plains. Slopes range from 0 to 3 percent. Glenelg silt loam, 8 to 15 percent slopes consists of very deep, well drained soils formed in residuum weathered from micaceous schist on uplands of the Blue Ridge and the Northern Piedmont. This soil is undifferentiated, mostly poorly drained sandy bottomland soils intermingled with decomposing organic litter and eroded silts and clays due to erosion. Slope: 0 to 15% Aspect: Variable. | Wild material | | 2123125 | NA 86885 |
| 18 | WLP 1731 | RJL2021PA-001 | Viburnum acerifolium L. | Pennsylvania, United States | NA | | | 2021 | COLLECTED | 11/05/2021 | Plants growing in woodlands above a small unnamed creek that dumps into the Middle Branch White Clay Creek in Goddard Park, West Grove Pennsylvania, off of Wickerton Road, Chester County. | 39.80462083, -75.82888750 | 103 | Plants growing in a mesic, well-drained habitat of deciduous woodlands, for the most part, above the riparian zone that drains toward a small unnamed creek that feeds into the Middle Branch White Clay Creek. Plants are growing in high understory shade with very little direct sun during most of the day. The remnant woodlands exist mostly along the steep slopes, wetlands and seeps of seasonal and year-round creeks flowing into the Middle Branch White Clay Creek. The woodlands are bordered by numerous housing developments and land converted to meadows; hence there is significant first order edge that is heavily impacted by invasive plant intrusion. Soils: Soils are classified as Glenelg silt loam, 8 to 15% slopes (GgC); this series consists of very deep, well drained soils formed in residuum weathered from micaceous schist on uplands of the Blue Ridge and the Northern Piedmont. Saturated hydraulic conductivity is moderately high in the subsoil and moderately high to high in the substratum. This upper horizon of this soil is undifferentiated, mostly poorly drained sandy bottomland soils intermingled with decomposing organic litter and eroded silts and clays due to erosion. Slope: 8 to 15% Aspect: West. | Wild material | | 2123080 | WLP 1731 |
| 19 | WLP 1732 | RJL2021PA-002 | Viburnum prunifolium L. | Pennsylvania, United States | NA | | | 2021 | COLLECTED | 11/05/2021 | Plants growing in woodlands along a small unnamed creek corridor dumping into the Middle Branch White Clay Creek in Goddard Park, West Grove Pennsylvania, off of Wickerton Road, Chester County. | 39.80462083, -75.82888750 | 102 | Plants are growing in a range of habitats from drier upland woods to moist creekside settings of deciduous woodlands that drain toward the Middle Branch White Clay Creek. Plants grow in part shade to high understory shade with dappled to indirect direct sunlight. Plants achieve their largest size and fruiting potential in part sun of the riparian zone of the creek where woodland canopy is thinner. Soils: Soils found in the areas where this collection was made are comprised primarily of flood plain Hatboro silt loam (Ha) and well-drained, upland Glenelg silt loam, 8 to 15 percent slopes (GgC). Hatboro silt loam consists of very deep and poorly drained soils formed in deposited alluvium derived from metamorphic and crystalline rock. They are on flood plains. Slopes range from 0 to 3 percent. Glenelg silt loam, 8 to 15 percent slopes consists of very deep, well drained soils formed in residuum weathered from micaceous schist on uplands of the Blue Ridge and the Northern Piedmont. This soil is undifferentiated, mostly poorly drained sandy bottomland soils intermingled with decomposing organic litter and eroded silts and clays due to erosion. Slope: 0 to 15% Aspect: Variable. | Wild material | | 2123098 | WLP 1732 |
| 20 | WLP 1733 | RJL2021PA-003 | Viburnum dentatum L. | Pennsylvania, United States | NA | | | 2021 | COLLECTED | 11/05/2021 | Plants growing in woodlands along a small unnamed creek corridor dumping into the Middle Branch White Clay Creek in Goddard Park, West Grove Pennsylvania, off of Wickerton Road, Chester County. | 39.80522167, -75.82928139 | 107 | Plants are growing in a range of habitats from mesic woodland to moist creekside settings of deciduous woodlands that drain toward the Middle Branch White Clay Creek. Plants grow in high understory shade with dappled to indirect sunlight. Soils: Soils found in the areas where this collection was made are comprised primarily of flood plain Hatboro silt loam (Ha) and well-drained, upland Glenelg silt loam, 8 to 15 percent slopes (GgC). Hatboro silt loam consists of very deep and poorly drained soils formed in deposited alluvium derived from metamorphic and crystalline rock. They are on flood plains. Slopes range from 0 to 3 percent. Glenelg silt loam, 8 to 15 percent slopes consists of very deep, well drained soils formed in residuum weathered from micaceous schist on uplands of the Blue Ridge and the Northern Piedmont. This soil is undifferentiated, mostly poorly drained sandy bottomland soils intermingled with decomposing organic litter and eroded silts and clays due to erosion. Slope: 0 to 15% Aspect: Variable. | Wild material | | 2123124 | WLP 1733 |
| 21 | NA 86848 | ZARKS-025 | Acer saccharum Marshall subsp. leucoderme (Small) Desmarais | Arkansas, United States | NA | | | 2020 | COLLECTED | 10/09/2014 | Cedar Fourche Creek; Harper Grocery Rd. at Rock Springs Rd. | 34.66470800, -93.26778900 | 209 | Mesic, mixed deciduous forest; growing on the bank just above a small stream | Wild material | | 2115797 | NA 86848 |
| 22 | Ames 35226 | Ocoee Gorge | Monarda austroappalachiana Floden | Tennessee, United States | NC7 |  | | 2019 | COLLECTED | 09/12/2019 | Located just east of Lake Ocoee along highway 74 approximately 9.8 miles east, southeast of Ocoee, Polk County | 35.09659000, -84.54762000 | 269 | Steep (some vertical) rocky cliffs and bluffs, predominately shale. | Wild material | Described by Aaron Floden (2015) as an erect perennial (30-50 cm tall) with a strong Oregano (thymol) scent, minute retrorse to spreading trichomes at internodes and large, emaculate, white corollas. Typically flowers in late May into early June, which is earlier than both M. fistulosa and M. clinopodia where sympatric. Species is endemic to the Southern Appalachians (northern Georgia, southwest North Carolina, and southeast Tennessee) and limited to calcareous phyllite and limestone, glade-like/talus slope habitats. | 2097762 | Ames 35226 |
| 23 | Ames 34311 | JDC/ML/2018/029/842-A | Monarda luteola Singhurst & W. C. Holmes | Arkansas, United States | NC7 |  | | 2018 | COLLECTED | 07/17/2018 | Washburn Mountain Range located 8.10 miles south, southwest of Charleston on Fort Chaffee Military Base, T6N R29W NE 1/4 SW 1/4 Sec. 16, Sebastian County | 35.19071800, -94.09287200 | 290 | Open, dry woods. | Wild material | Plants with lemon scent, pubescent stems and leaves with faint yellow flowers measuring circa 2.0-2.5' in height. Plants likely reached peak flower on 18 May 2018. Seeds likely reached full maturity around first week in July (2018). | 1964618 | Ames 34311 |
| 24 | Ames 34312 | JDC/ML/2018/029/842-B | Monarda luteola Singhurst & W. C. Holmes | Arkansas, United States | NC7 |  | | 2018 | COLLECTED | 07/17/2018 | Washburn Mountain Range located 5.30 miles south of Charleston on Fort Chaffee Military Base on ridge near Rattlesnake Creek on the west side of S Rattlesnake Road, T6N R29W NE 1/4 SW 1/4 Sec. 1, Franklin County | 35.22206500, -94.03779700 | 229 | Open, dry woods. | Wild material | Plants with lemon scent, pubescent stems and leaves with faint yellow flowers measuring circa 1.5-2.0' in height. Plants likely reached peak flower on 18 May 2018. Seeds likely reached full maturity around first week in July (2018). | 1964619 | Ames 34312 |
| 25 | Ames 34321 | JDC/MR/2018/061/874 | Monarda russeliana Nutt. ex Sims | Oklahoma, United States | NC7 |  | | 2018 | COLLECTED | 07/19/2018 | On the northwest side of Wister Lake along the north side of Wister Lake MGMT Road, T5N R24E NW 1/4 NW 1/4 and NE 1/4 NW 1/4 Sec. 6, Le Flore County. | 34.93915700, -94.81967400 | 160 | Open, dry, rocky woods. | Wild material | Petite plants with only 1-3 stems per plant ranging from 1.0-1.5' in height. At time of collection (19 July 2018) peduncle showing 1-2" of dead/brown tissue. Leaves twice as long (or more) as wide. Generally three pairs of opposite leaves per stem. Slight pubescence on leaves with 1-2 mm petiole. Leaves rather flat. Seeds likely reached peak maturity around first week in July. | 1964628 | Ames 34321 |
| 26 | NA 86662 | SE-2017-016 | Quercus shumardii Buckley | Georgia, United States | NA | | | 2017 | COLLECTED | 10/14/2017 | Oconee National Forest: Monticello Glades. | 33.25416000, -83.68386000 | 185 | Moist woods. | Wild material | On the original collection notes, this was assigned the field collection number SE-2017-017, but it was corrected to SE-2017-016 later. | 2141807 | NA 86662 |
| 27 | WLP 1311 | NA 83922 | Itea virginica L. | Kentucky, United States | NA | | | 2016 | COLLECTED | 09/28/2016 | Cumberland Falls State Park; Cumberland Falls Trail #2 (Cumberland River Trail) at river's edge. | 36.83800000, -84.33200000 | 276 | River's edge below rocks. | | | 1953510 | WLP 1311 |
| 28 | WLP 1411 | JDC/OV/2010/049/319 | Ostrya virginiana (Mill.) K. Koch | Arkansas, United States | NA |  | | 2010 | COLLECTED | 09/16/2010 | Gamaliel Recreation Area, along Norfork Lake, Baxter County. | 36.42831000, -92.21806000 | 216 | Rock outcrop with underground seep. East facing slope (65%). Associated with Cotinus obovatus, Acer saccharum, Juniperus virginiana, Viburnum sp., Quercus muehlenbergii, Frangula caroliniana, Hydrangea arborescens, Cornus florida, Smilax sp., and Ulmus sp. (likely U. alata). | Wild material | | 1848910 | WLP 1411 |