| 0 | NA 86666 | SE-2017-010A | Quercus sp. | Georgia, United States | NA | | | 2017 | COLLECTED | 10/13/2017 | Fall Line Sandhills Wildlife Management Area. | 32.57050000, -84.28230000 | 216 | Sandy old beach dune. | Wild material | Recorded at the U.S. National Arboretum as Quercus incana W. Bartram (non Q. incana Roxb., which is a synonym of Q. leucotrichophora; see the Flora of North America treatment for further information).This (along with NA 86667 and 86668) were missing from the other collection data used for initial accessioning; see NA 86648-86664 for the rest of the collections from this expedition. | 2141803 | NA 86666 |
| 1 | NA 89160 | 2025RJLSEUS-08 | Ilex hybr. | Florida, United States | NA | | | 2025 | COLLECTED | 10/02/2025 | Eglin Air Force Base: coastal dune ridge on Eglin AFB behind businesses located along Florida State Highway 98. The site is accessed through a now gated and permanently closed Eglin AFB, East River Unit, A-21 Road (now open to pedestrian traffic only with a valid Eglin user permit). After walking through the gated road, the site is to the west along 4-wheeling trails. | 30.41191000, -86.77315800 | 8 | Part shade in a primarily evergreen extremely dry dune community with a mixed understory of deciduous and evergreen plants. Slope: 0 to 2 percent. Soils: The soils of this are characterized as Kureb Series sand, 0 to 8 percent slopes. The Kureb series consists of very deep, excessively drained, gently sloping to moderately steep soils on Coastal Plain uplands and on side slopes along streams and bays. They have formed in marine, aeolian, or fluvial sands. Slopes range from 0 to 20 percent. The thickness of the sandy horizon is more than 2 meters. Soil reaction is neutral to extremely acid throughout. All horizons are fine sand, sand, or coarse sand. Silt plus clay content is less than 5 percent. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). Geology: The underlying geology of this area is characterized as undifferentiated Quaternary Sediments. Much of Florida's surface is covered by a varying thickness of undifferentiated sediments consisting of siliciclastics, organics and freshwater carbonates. Where these sediments exceed 6.1 meters thick, they were mapped as discrete units. To subdivide the undifferentiated sediments, those sediments occurring in flood plains were mapped as alluvial and flood plain deposits (Qal). Sediments showing surficial expression of beach ridges and dunes were mapped separately (Qbd) as were the sediments composing Trail Ridge (Qtr). Terrace sands were not mapped (refer to Healy [1975] for a discussion of the terraces in Florida). The subdivisions of the Undifferentiated Quaternary Sediments (Qu) are not lithostratigraphic units but are utilized to facilitate a better understanding of the State's geology. The siliciclastics are light gray, tan, brown to black, unconsolidated to poorly consolidated, clean to clayey, silty, unfossiliferous, variably organic-bearing sands to blue green to olive green, poorly to moderately consolidated, sandy, silty clays. Gravel is occasionally present in the panhandle. Organics occur as plant debris, roots, disseminated organic matrix and beds of peat. Freshwater carbonates, often referred to as marls in the literature, are scattered over much of the State. In southern Florida, freshwater carbonates are nearly ubiquitous in the Everglades. These sediments are buff colored to tan, unconsolidated to poorly consolidated, fossiliferous carbonate muds. Sand, silt and clay may be present in limited quantities. These carbonates often contain organics. The dominant fossils in the freshwater carbonates are mollusks. (Source: USGS Florida Geologic Map Data). | Wild material | | 2193006 | NA 89160 |
| 2 | NA 88757 | 2025 TKRM-001 | Cyrilla racemiflora L. | Florida, United States | NA | | | 2025 | COLLECTED | 01/03/2025 | Area on the south side of an unnamed sand road, about 0.54 kilometers south of Florida State Highway 98 and accessed from Walton County Highway 283 S. The collecting site is accessed by going east 0.54 kilometers on the unnamed sand road from the junction with Walton County Highway 283 S. | 30.35374700, -86.15172700 | 12 | Mostly found in moist to dry flatwoods in mixed evergreen and deciduous forest. Slope: N/A. Aspect: various. The underlying geology of this area is characterized as undifferentiated Quaternary Sediments. Much of Florida's surface is covered by a varying thickness of undifferentiated sediments consisting of siliciclastics, organics and freshwater carbonates. Where these sediments exceed 6.1 meters thick, they were mapped as discrete units. In an effort to subdivide the undifferentiated sediments, those sediments occurring in flood plains were mapped as alluvial and flood plain deposits (Qal). Sediments showing surficial expression of beach ridges and dunes were mapped separately (Qbd) as were the sediments composing Trail Ridge (Qtr). Terrace sands were not mapped (refer to Healy [1975] for a discussion of the terraces in Florida). The subdivisions of the Undifferentiated Quaternary Sediments (Qu) are not lithostratigraphic units but are utilized in order to facilitate a better understanding of the State's geology. The siliciclastics are light gray, tan, brown to black, unconsolidated to poorly consolidated, clean to clayey, silty, unfossiliferous, variably organic-bearing sands to blue green to olive green, poorly to moderately consolidated, sandy, silty clays. Gravel is occasionally present in the panhandle. Organics occur as plant debris, roots, disseminated organic matrix and beds of peat. Freshwater carbonates, often referred to as marls in the literature, are scattered over much of the State. In southern Florida, freshwater carbonates are nearly ubiquitous in the Everglades. These sediments are buff colored to tan, unconsolidated to poorly consolidated, fossiliferous carbonate muds. Sand, silt and clay may be present in limited quantities. These carbonates often contain organics. The dominant fossils in the freshwater carbonates are mollusks. (Source: USGS Florida Geologic Map Data). The Hurricane Series consists of very deep, somewhat poorly drained, moderately rapid permeable soils on broad areas that are slightly higher than the adjacent flats in the Southern Coastal Plain (MLRA 133A), the Gulf Coast Flatwoods (MLRA 152A) and the Atlantic Coast Flatwoods (MLRA 153A). They formed in sandy marine sediments. Slopes range from 0 to 5 percent. Solum thickness is 1.5 meters or more. Reaction ranges from extremely acid to moderately acid throughout. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). | Wild material | Received as Cyrilla parvifolia. | 2171019 | NA 88757 |
| 3 | NA 89091 | 2024RM-TK-004 | Prunus sp. | Florida, United States | NA | | | 2024 | COLLECTED | 09/05/2024 | Blackwater River Wildlife Management Area: on the south side of Boundary Line Road about 0.32 kilometers west of Deaton Bridge Road along an area edged by a barbed wire fence. | 30.68579800, -86.87964300 | 45 | Plants are growing from part-sun to full sun. Plants are growing in an area that is frequently burned with a lot of [Prunus sp. (orig. listed as Prunus alabamensis)] scattered throughout. This habitat is a longleaf pine-wiregrass community with scattered turkey (Quercus laevis) and blackjack oaks (Quercus incana). There is a slight slope downward. The line of [Prunus sp.] goes along a semi-ditch on the side of a dirt road. The plants probably get a bit more water than the plants out in the open forest. The [Prunus sp.] are most often without any other close woody companions. Slope: 0 percent. Aspect: North. Geology: The underlying geology of this area is probably of lower Pliocene age and characterized as the Citronelle Formation. The Citronelle Formation is widespread in the Gulf Coastal Plain. The type section for the Citronelle Formation, named by Matson (1916), is near Citronelle, Alabama. The Citronelle Formation grades laterally, through a broad facies transition, into the Miccosukee Formation of the eastern Florida panhandle. Coe (1979) investigated the Citronelle Formation in portions of the western Florida panhandle. The Citronelle Formation is a siliciclastic, deltaic deposit that is lithologically similar to, and time equivalent with, the Cypresshead Formation and, at least in part, the Long Key Formation (Cunningham et al., 1998) of the peninsula. In the western panhandle, some of the sediments mapped as Citronelle Formation may be reworked Citronelle. The lithologies are the same and there are few fossils present to document a possible younger age. The Citronelle Formation consists of gray to orange, often mottled, unconsolidated to poorly consolidated, very fine to very coarse, poorly sorted, clean to clayey sands. It contains significant amounts of clay, silt and gravel which may occur as beds and lenses and may vary considerably over short distances. Limonite nodules and limonite-cemented beds are common. Marine fossils are rare but fossil pollen, plant remains and occasional vertebrates are found. Much of the Citronelle Formation is highly permeable. It forms the Sand and Gravel Aquifer of the surficial aquifer system. (Source: USGS Florida Geologic Map Data). Soils: The soil of this area is characterized as Lakeland Series Sand, 0 to 5 percent slopes (21). The Lakeland Series consists of very deep, excessively drained, rapid to very rapidly permeable soils on uplands. They formed in thick beds of eolian or marine and/or fluvio-marine sands in the Southern Coastal Plain MLRA (133A), the Carolina and Georgia Sandhills (MLRA 137), the Eastern Gulf Coast Flatwoods (MLRA 152A) and the Atlantic Coast Flatwoods (MLRA 153A). (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). EPA Ecoregion (Level III): Southeastern Plains (65). EPA Ecoregion (Level IV): Southern Pine Plains and Hills (65f). | Wild material | Received as Prunus alabamensis; other collections of this material have proven not to be Prunus serotina var. alabamensis, but actually a species of plum; this will likewise be treated as unidentified material until its species can be ascertained. Collectors' notes refer to the plant by the name under which it was collected. | 2169055 | NA 89091 |
| 4 | Ames 36185 | APS/BP/2023/076/286 | Betula populifolia Marshall | Indiana, United States | NC7 |  | | 2023 | COLLECTED | 11/02/2023 | Indiana Dunes State Park just 3.40 miles northeast of Chesterton, T37N R5W NE 1/4 SE 1/4 SW 1/4 Sec. 18 | 41.65352700, -87.03831500 | 186 | Low depressions with some standing water. Woodland edge. | Wild material | Represents a disjunct population in northwest Indiana and the extreme western edge of the species native range. Trees sampled in nature averaging 30-45' in height with trunks ranging from 3" up to 8" DBH. Bark dull-white to grey. Typically multi-stemmed trunks. Leaves with acuminate tips and branches with typically one male catkin at terminal end of branches, but occassionally two male catkins. | 2159042 | Ames 36185 |
| 5 | WLP 3213 | TXWL2023-001 | Lyonia mariana (L.) D. Don | Texas, United States | NA | | | 2023 | COLLECTED | 08/22/2023 | Angelina National Forest. | 31.05522100, -94.26205200 | | Baygall below longleaf [pine] stand. | Wild material | | 2158757 | WLP 3213 |
| 6 | WLP 3136 | TJK2023FL-010 | Morella cerifera (L.) Small | Florida, United States | NA | | | 2023 | COLLECTED | 08/18/2023 | Blackwater State Forest: Wolfe Creek. | 30.80751000, -86.95774000 | 52 | Beautiful xeric pine-oak upland community. Transitions to mesic slopes and then to seepage bottom, stringer wetland community adjacent to the Wolfe Creek. Area is on a regular 2-4[-year] burn cycle. Slope: 10%. Aspect: South. Elevation recorded as 172 feet. | Wild material | Received as Morella pumila (Morella cerifera var. pumila). Treated tentatively as Morella cerifera Pumila Group. WLPGR contract collection. | 2158468 | WLP 3136 |
| 7 | NA 89264 | TJK2023FL-002 | Gaylussacia frondosa (L.) Torr. & A. Gray var. nana A. Gray | Florida, United States | NA | | | 2023 | COLLECTED | 05/19/2023 | Blackwater State Forest: Wolfe Creek. | 30.80760000, -86.96250000 | 49 | Beautiful xeric pine-oak upland community. Transitions to mesic slopes and then to seepage bottom, stringer wetland community adjacent to the Wolfe Creek. Area is on a regular 2-4[-year] burn cycle. Slope: 5%. Aspect: Northwest. Elevation recorded as 161 feet. | Wild material | WLPGR contract collection. Received as Gaylussacia tomentosa (nana). | 2158247 | NA 89264 |
| 8 | NA 89265 | TJK2023FL-003 | Ceanothus sp. | Florida, United States | NA | | | 2023 | COLLECTED | 05/19/2023 | Blackwater State Forest: Wolfe Creek. | 30.80650000, -86.95840000 | 49 | Beautiful xeric pine-oak upland community. Transitions to mesic slopes and then to seepage bottom, stringer wetland community adjacent to the Wolfe Creek. Slope: 20%. Aspect: Northwest. Elevation recorded as 162 feet. | Wild material | WLPGR contract collection. Received as Ceanothus microphyllus. | 2158248 | NA 89265 |
| 9 | NA 89266 | TJK2023FL-004 | Gaylussacia dumosa (Andrews) Torr. & A. Gray | Florida, United States | NA | | | 2023 | COLLECTED | 05/31/2023 | Blackwater State Forest: Wolfe Creek. | 30.80560000, -86.95890000 | 49 | Beautiful xeric pine-oak upland community. Transitions to mesic slopes and then to seepage bottom, stringer wetland community adjacent to the Wolfe Creek. Slope: 15%. Aspect: Northwest. Elevation recorded as 160 feet. | Wild material | WLPGR contract collection. | 2158249 | NA 89266 |
| 10 | NA 89267 | TJK2023FL-005 | Ceanothus americanus L. | Florida, United States | NA | | | 2023 | COLLECTED | 06/10/2023 | Blackwater State Forest: Wolfe Creek. | 30.80760000, -86.96250000 | 49 | Beautiful xeric pine-oak upland community. Transitions to mesic slopes and then to seepage bottom, stringer wetland community adjacent to the Wolfe Creek. Area is on a regular 2-4[-year] burn cycle. Slope: 5%. Aspect: Northwest. Elevation recorded as 161 feet. | Wild material | WLPGR contract collection. | 2158250 | NA 89267 |
| 11 | NA 89269 | TJK2023FL-007 | Vaccinium darrowii Camp | Florida, United States | NA | | | 2023 | COLLECTED | 06/10/2023 | Blackwater State Forest: Wolfe Creek. | 30.80560000, -86.95770000 | 60 | Beautiful xeric pine-oak upland community. Transitions to mesic slopes and then to seepage bottom, stringer wetland community adjacent to the Wolfe Creek. Area is on a regular 2-4[-year] burn cycle. Slope: 2%. Aspect: West-northwest. Elevation recorded as 197 feet. | Wild material | WLPGR contract collection. | 2158252 | NA 89269 |
| 12 | W6 61029 | CA360-200 | Schoenoplectus californicus (C. A. Mey.) Soják | California, United States | W6 |  | | 2023 | | | | | | | Wild material | Seed head shape and stem shape near base and tip. | 2142668 | W6 61029 |
| 13 | Ames 36024 | AS/FN/2023/011/221 | Fraxinus nigra Marshall | Wisconsin, United States | NC7 |  | | 2023 | COLLECTED | 02/26/2023 | Located just north of Leland approximately 0.70 miles along Hemlock Road, T10N R5E SW 1/4 NW 1/4 Sec. 18 | 43.34472800, -89.95099700 | 242 | Floodplain | Wild material | Single mother tree sample with signs of wood pecker damage on trunk. | 2141557 | Ames 36024 |
| 14 | NA 88523 | RM-TK2022-011 | Ilex ambigua Torr. | Florida, United States | NA | | | 2023 | COLLECTED | 10/16/2022 | Blackwater River State Park: growing along unnamed dirt road approximately 0.26 kilometers north of the intersection with Boundary Line Road. | 30.68790000, -86.86230000 | 56 | Plants are growing in hot, dry, full sun conditions. Soils: The underlying geology of this area is the Citronelle Formation of Pliocene origin and consists of gray to orange, often mottled, unconsolidated to poorly consolidated, very fine to very coarse, poorly sorted, clean to clayey sands. It contains significant amounts of clay, silt and gravel which may occur as beds and lenses and may vary considerably over short distances. Limonite nodules and limonite-cemented beds are common. (Source: USGS Florida Geologic Map Data). The primary soil type in the collection area is classified as Lakeland Sand soils (5 to 12 percent slopes). The surface soil profile of this area is primarily the Lakeland series which consists of very deep, excessively drained, rapid to very rapidly permeable soils on uplands. They formed in thick beds of eolian or marine and/or fluvio-marine sands. Thickness of the sand exceeds 2 meters. Silt plus clay in the upper meter ranges from 5-10 percent. Reaction ranges from very strongly acid to moderately acid throughout. (Source: NRCS Web Soil Survey). | Wild material | | 2140804 | NA 88523 |
| 15 | NA 87267 | (female selection) | Ilex vomitoria Sol. ex Aiton f. pendula Foret & Solymosy | Texas, United States | NA | | | 2022 | COLLECTED | 01/27/2020 | Plants growing on the north side of the unpaved Private Road 6061, approximately 0.4 kilometers east of Texas State Hwy 87. | 31.16207000, -93.72862000 | 132 | Growing in almost full sun on a south-facing roadside slope in very dry upland conditions. Soils are deep, somewhat excessively well-drained, and typically strongly acidic. Slope: 8 percent. Aspect: South. 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. The primary soil types in the collection area are classified as Letney-Tehran soils. These soils consist of deep, somewhat excessively drained, moderately rapidly permeable soils on uplands. They were formed in thick loamy and sandy sediments on the Western Coastal Plain. The Letney-Tehran soils are on gently sloping to moderately steep uplands with slopes ranging from 1 to 20 percent. They are typically strongly acidic. | Wild material | Full name as recorded at U.S. National Arboretum: Ilex vomitoria forma pendula (female selection). Six plants of a selection of weeping yaupon holly sent from Shangri La Botanical Gardens & Nature Center (Rick Lewandowski facilitated the distribution in retirement). It is evidently from a selection discovered growing in Newton County, Texas, presumably from the wild. A date of 11/25/2020 is on the plant's tag from the source, but it is unknown if this is a propagation date or an accession date. Form received: rooted cutting. | 2158071 | NA 87267 |
| 16 | NA 86881 | ASA-009A | Ilex vomitoria Aiton | Virginia, United States | NA | | | 2021 | COLLECTED | 01/13/2020 | Virginia Beach: First Landing State Park. Collected in the park campground, near the location of VIRG-015. One plant at campsite #166, the other near site #73 | 36.91886900, -76.05188900 | 2 | 15 deg slope; SE-facing; sand. Dunes with live oaks | Wild material | | 2116470 | NA 86881 |
| 17 | Ames 34728 | UT060-56 | Helianthus anomalus S. F. Blake | Utah, United States | NC7 | | | 2018 | | | | | | | Wild material | Helianthus anomalus | 1965083 | Ames 34728 |
| 18 | W6 53346 | CA930A-596 | Descurainia pinnata (Walter) Britton subsp. glabra (Wooton & Standl.) Detling | California, United States | W6 | | | 2018 | | | | | | | Wild material | | 1958081 | W6 53346 |
| 19 | W6 53387 | CA930A-638 | Eriogonum fasciculatum Benth. var. polifolium (Benth.) Torr. & A. Gray | California, United States | W6 | | | 2018 | | | | | | | Wild material | | 1958122 | W6 53387 |
| 20 | NA 81984 | Lactea Group | Callicarpa americana L. | Texas, United States | NA | | | 2014 | COLLECTED | 08/30/2013 | Woodlands above Boykin Spring Lake. | 31.06266000, -94.27565000 | 56 | Growing in partial shade of mixed deciduous and evergreen woodlands in well-drained to dry conditions. | | | 1951711 | NA 81984 |
| 21 | Ames 31676 | GA12010001 | Fraxinus pennsylvanica Marshall | Minnesota, United States | NC7 |  | | 2012 | COLLECTED | NEAR 09/24/2012 | Near Mashaug Creek just north of Twin Valley, Norman County. | 47.28851660, -96.26865000 | 327 | Upland forest, dominated by Populus deltoides. | Wild material | | 1906587 | Ames 31676 |
| 22 | Ames 30145 | JDC/FP/2009/031/181 | Fraxinus pennsylvanica Marshall | Wisconsin, United States | NC7 |  | | 2009 | COLLECTED | 09/22/2009 | Tower Hill State Park and Lower Wisconsin State Riverway (Helena Unit), SW 1/4 of SE 1/4 of Section 20 and SW 1/4 of NE 1/4 of Section 17, T8N, R4E, Spring Green Quad, Iowa County. | 43.15055556, -90.04166667 | 237 | Wisconsin River watershed/floodplain | Wild material | | 1819726 | Ames 30145 |