| 0 | WLP 3085 | RM2023-003 | Hibiscus laevis All. | Florida, United States | NA | | | 2023 | COLLECTED | 10/01/2022 | This species is growing along the Escambia River and accessed by boat. | 30.62930000, -87.25830000 | 1 | The plants were growing on stumps in full sun on the edge of a semi-alluvial area of the river.
Soils: The underlying geology of this area is classified as Alluvium, of Pleistocene/Holocene origin and consists of undifferentiated Quaternary sediments of varying thickness including siliciclastics, organics and freshwater carbonates. 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. 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.
Source: USGS Florida Geologic Map Data (https://mrdata.usgs.gov/geology/state/state.php?state=fl)
The surface soil profile of this area is primarily Chewacla-Wahee-Riverview Association. The Chewacla Series soils are dark yellowish brown silty clay loam soils, that are strongly acidic and somewhat poorly drained. They are soils of flood plains and streams subject to frequent flooding. The Wahee Series soils are dark gray clayey and loamy marine or fluviomarine sediments that are strongly acidic and somewhat poorly drained. 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.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2141439 | WLP 3085 |
| 1 | PI 671849 | FL2010WW-6 | Amphicarpaea bracteata (L.) Fernald | Florida, United States | W6 |  | | 2010 | COLLECTED | 11/09/2010 | Columbia County; Ichetucknee State Park; South entrance; 0.4 miles from entrance; immediately after kiosk, turn left into parking lot; parking lot near maintenance shed; lot perimeter about 15-25 m out | 29.95299000, -82.77148000 | 5 | sand hill; dry, well-drained soil; sunny, open location, edge of open forest dominated by Pinus palustris with an understory of Quercus laevis, Quercus stellata, invasive Quercus laurifolia, Vitis spp, Carya spp. and many annuals | Wild material | Very abundant; prostrate vines; very mature leaves; insect damage; no flowers; few green pods; dry and dehisced pods; small root tuber with fibrous roots extending; adventitious roots from tuber and from lower nodes, growing out to produce other daughter plants; small white ?nodule? on white adventitious roots with more white root growing from it; the main plant often has many satellite plants attached to it. Sample size 750 meters square. | 1854396 | PI 671849 |
| 2 | PI 664832 | L.K. 24 | Echinacea purpurea (L.) Moench | Ohio, United States | NC7 |  | | 2004 | COLLECTED | 11/15/2003 | State Route 161 West from Columbus, south on Rosedale Road, Bigelow Cemetery State Nature Preserve, Madison County. | 40.10972222, -83.41916667 | 301 | Full sun (except for shading from taller prairie plants) on flat ground. Dark, loamy soil with some gravel and a little clay, fair to good drainage. | Wild material | Somewhat clump forming. Toothed/serrated margin, long petioles, pubescent, impressed veins. 3-4 feet in height. Rays reddish purple. Flower heads 3-4 inches in diameter; bristly central disk. | 1655342 | PI 664832 |
| 3 | PI 633671 | SC 4 | Echinacea purpurea (L.) Moench | Ohio, United States | NC7 |  | | 2000 | COLLECTED | 09/30/2004 | | | | Site size 5 square meters; total land area approximately 300 feet x 300 feet. | Wild material | Plants noted in nature measuring 3-4 feet in height. Lanceolate lower leaves. Flower heads 3 inches in diameter, rays reddish purple, drooping. | 1606281 | PI 633671 |
| 4 | 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 |
| 5 | NA 88578 | 2024RJLFL-004 | Ilex vomitoria Aiton | Florida, United States | NA | | | 2024 | COLLECTED | 11/12/2024 | Collected along Florida National Scenic Trail/Eglin Air Force Base unnamed road. | 30.44526100, -86.86094700 | 4 | Mixed evergreen and deciduous forests in part shade to full sun. Slope: 5 to 10 percent. Aspect: Various. The underlying geology of this area is characterized as Citronelle Formation of the Pliocene period. 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 contain organics. The dominant fossils in the freshwater carbonates are mollusks. (Source: USGS Florida Geologic Map Data). The soils of this are characterized as Lakeland Series Sand, 5 to 12 percent slopes. 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). Slopes are dominantly from 0 to 12 percent but can range to 85 percent in dissected areas. Thickness of the sand exceeds 200 cm. Silt plus clay in the 25 to 100 cm control section ranges from 5 to 10 percent. Reaction ranges from very strongly acid to moderately acid throughout. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). | Wild material | | 2169915 | NA 88578 |
| 6 | 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 |
| 7 | NA 88827 | RJL-RM2023FLAL-001 | Ilex ambigua Torr. | Florida, United States | NA | | | 2023 | COLLECTED | 12/05/2023 | Yellow River Wildlife Management Area, along DOF [Department of Forestry] Y9 dirt road 0.08 kilometers east of Miller Bluff Road. | 30.65289100, -86.87602800 | 44 | Growing in part shade to sun in very dry, highly competitive site still recovering from the logging of pines in the past decade. This young woodland is comprised of a combination of evergreen and deciduous species competing for available resources and light before the young sand pines begin to dominate the upper canopy. Slope: 0 percent. Aspect: N/A. 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 (0 to 5 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 | | 2165657 | NA 88827 |
| 8 | NA 88828 | RJL-RM2023FLAL-002 | Vaccinium arboreum Marshall | Florida, United States | NA | | | 2023 | COLLECTED | 12/05/2023 | Yellow River Wildlife Management Area, along DOF [Department of Forestry] Y9 dirt road 0.08 kilometers east of Miller Bluff Road. | 30.65289100, -86.87608500 | 44 | Growing in part shade to sun in very dry, highly competitive site still recovering from the logging of pines in the past decade. This young woodland is comprised of a combination of evergreen and deciduous species competing for available resources and light before the young sand pines begin to dominate the upper canopy. Slope: 0 percent. Aspect: N/A. 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 (0 to 5 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 | | 2165658 | NA 88828 |
| 9 | NA 88683 | TJK2023FL-030 | Vaccinium arboreum Marshall | Florida, United States | NA | | | 2023 | COLLECTED | 11/16/2023 | Pensacola State College, Midway Campus, 1/8 mile south of Highway 98. | 30.39710000, -87.01040000 | 10 | Sand Pine Scrub, old remnant sand dune. Slope: flat. Aspect: West. Elevation: 32 feet. | Wild material | | 2159095 | NA 88683 |
| 10 | NA 88685 | TJK2023FL-032 | Lyonia ligustrina (L.) DC. | Florida, United States | NA | | | 2023 | COLLECTED | 11/18/2023 | Blackwater State Forest: Wolfe Creek. | 30.80844000, -86.96243000 | 55 | Drier ridge above seepage slope. Slope: less than 2%. Aspect: South. Elevation: 180 feet. | Wild material | | 2159097 | NA 88685 |
| 11 | NA 88688 | TJK2023FL-035 | Ilex decidua Walter | Florida, United States | NA | | | 2023 | COLLECTED | 11/19/2023 | Eglin Air Force Base, Choctaw West; Range Rd 813, approximately 0.3 miles north of Range Rd 213 - Choctaw Nolf Airport Rd. Growing in flat west of Weaver Creek. | 30.51790000, -86.93230000 | 34 | Damp (not wet) flat west of creek. Slope: less than 2%. Aspect: West. Elevation: 113 feet. | Wild material | | 2159100 | NA 88688 |
| 12 | NA 88662 | TJK2023FL-016 | Sideroxylon sp. | Florida, United States | NA | | | 2023 | COLLECTED | 09/16/2023 | East River Unit, Eglin Air Force Base. Near A-21 Rd. | 30.41250000, -86.77110000 | 7 | Xeric shrub, xeric sandhills community. Elevation: 26 feet. Slope: 2%. Aspect: South. | Wild material | | 2158796 | NA 88662 |
| 13 | 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 |
| 14 | 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 |
| 15 | 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 |
| 16 | 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 |
| 17 | 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 |
| 18 | NA 89271 | TJK2023FL-009 | Vaccinium stamineum L. | Florida, United States | NA | | | 2023 | COLLECTED | 07/16/2023 | Eglin Air Force Base: Weaver Creek area west of Highway 87, north of Choctaw Nolf Airfield Road (Escrobano Point). | 30.50710000, -86.91220000 | 33 | Xeric oak-pine uplands above Weaver Creek Bayhead. Slope: 5%. Aspect: Northwest. Elevation recorded as 107 feet. | Wild material | WLPGR contract collection. | 2158254 | NA 89271 |
| 19 | W6 61050 | CA930-1010 | Bouteloua barbata Lag. var. barbata | California, United States | W6 |  | | 2023 | | | | | | | Wild material | | 2142689 | W6 61050 |
| 20 | WLP 3084 | RM2023-002 | Rhododendron viscosum (L.) Torr. | Florida, United States | NA | | | 2023 | COLLECTED | 09/15/2022 | This species is growing in the Blackwater River State Forest approximately 0.24 kilometers north of Wof W20 and approximately 0.93 kilometers west of the junction of 3 Notch Trail/Road. | 30.84510000, -86.94940000 | 38 | The plants were growing in part shade of a moist mesic transition slope between a dry upland habitat and a bog.
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 (https://mrdata.usgs.gov/geology/state/state.php?state=fl)
The surface soil profile found in this area is primarily Troup Series. These soils are sandy and loamy marine deposits. They are well drained and typically on the tops and sides of broad and narrow ridges on uplands typically with 0-12% slopes. These soils are very strongly acid with a depth of 2-3 meters. Pactolus Series soils comprise a minor, but important percentage of the lower slopes that are nearly level to gently sloping and account for the somewhat poorly drained, yet, sandy conditions. These soils are also strongly acid with very dark gray loamy sands.
Source: Soil Survey of Santa Rosa County and NRCS Web Soil Survey (https://www.nrcs.usda.gov/Internet/FSE_MANUSCRIPTS/florida/FL113/0/SantaRosa.pdf and https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2141438 | WLP 3084 |
| 21 | NA 87350 | TJK2022FL-005 | Ilex ambigua Torr. | Florida, United States | NA | | | 2023 | COLLECTED | 11/02/2022 | Okaloosa County: Eglin Air Force Base: East River Unit H-3, Range Road 259, north of Highway 98. | 30.41190000, -86.77320000 | 0 | Xeric Scrub/Upland Sandhill community. | Wild material | | 2141641 | NA 87350 |
| 22 | 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 |
| 23 | NA 88565 | RJLSEUS2022-038 | Ilex ambigua Torr. | Florida, United States | NA | | | 2023 | COLLECTED | 12/14/2022 | Eglin Air Force Base: growing along the east side of Eglin AFB Choctaw Nolf Road northwest of Choctaw Navy Outlying Field. This road goes west and takes circuitous route to the north around the Field en route to Escribano Point Wildlife Management Area. | 30.51507900, -86.96767100 | 14 | Full sun on the top of the roadside slope in well-drained to dry conditions, 1-2 meters above surrounding lower, moist area. 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 | | 2140822 | NA 88565 |
| 24 | NA 88281 | MARSB-497 | Cephalanthus occidentalis L. | New Jersey, United States | NA | | | 2021 | | | | | | | Wild material | Growth formûthe plant is a shrub (i.e., a woody plant with several stems growing from the base)ûLeaf typeûthe leaf blade is simple (i.e., lobed or unlobed but not separated into leaflets)ûLeaves per nodeûthere are three leaves per node along the stemûthere are two leaves per node along the stemûLeaf blade edgesûthe edge of the leaf blade has teethûLeaf durationûthe leaves drop off in winter (or they wither but persist on the plant)ûarmature on plantûthe plant does not have spines, prickles, or thornsûLeaf blade lengthû80–150 mmûLeaf blade widthû23–150 mmûLeaf stalkûthe leaves have leaf stalksûFruit type (general)ûthe fruit is dry but does not split open when ripeûBark textureûthe bark of an adult plant is ridged or platedûthe bark of an adult plant is thin and smoothûTwig winter colorûbrownûgrayûredûBud scale numberûthere are no scales on the winter buds | 2113542 | NA 88281 |
| 25 | OPGC 8148 | MARSB-496 | Typha latifolia L. | New Jersey, United States | OPGC | | | 2021 | | | | | | | Wild material | Stem shape in cross-sectionûthe stem is round or oval in cross-sectionûLeaf blade widthû5–29 mmûLeaf blade cross-sectionûthe leaf blade is flat or rolled in at the edgesûInflorescence positionûthe inflorescence is at the tip of the plantûInflorescence branchingûthe inflorescence is on one or more stems with no branchesûFruit type (general)ûthe fruit is like a seed, and surrounded by hairsûFruit lengthû10–15 mmûLeaf position on plantûsome leaf attachment points are above the midpoint of the stemûPerianth compositionûthere are long, thin hairs attached at the base of the acheneûthere are three bristles and three scales on narrow stalks, attached at the base of the acheneûFruit cross-sectionûthe fruit is triangular to terete (circular) in cross-section | 2113541 | OPGC 8148 |
| 26 | W6 58613 | MARSB-498 | Scirpus cyperinus (L.) Kunth | New Jersey, United States | W6 | | | 2021 | | | | | | | Wild material | Stem shape in cross-sectionûthe stem is roughly triangular in cross-sectionûthe stem is round or oval in cross-sectionûLeaf blade widthû3–10 mmûLeaf blade cross-sectionûthe leaf blade is flat or rolled in at the edgesûInflorescence positionûthe inflorescence is at the tip of the plantûInflorescence branchingûthe inflorescence is branchedûFruit type (general)ûthe fruit is like a seed, and surrounded by hairsûthe fruit is like a seed, and surrounded by scalesûFruit lengthû0.6–0.9 mmûLeaf position on plantûsome leaf attachment points are above the midpoint of the stemûthe attachment points of all the leaves are at or near the base of the plantûPerianth compositionûthere are bristles attached at the base of the acheneûFruit cross-sectionûthe fruit is lenticular (lens-shaped) in cross-sectionûthe fruit is triangular to terete (circular) in cross-section | 2113543 | W6 58613 |
| 27 | WLP 175 | NACPEC19-084 | Crataegus sp. | North Carolina, United States | NA | | | 2019 | COLLECTED | 09/18/2019 | Clay County; Nantahala National Forest: Forest Road 6269: Buck Creek Serpentine Barrens: main trail | 35.08578100, -83.61498800 | 1036 | Pinus rigida-Quercus alba / Sporobulus heterolepis-Andropogon gerardii Woodland OR Southern Blue Ridge Ultramafic Outcrop Barren | Wild material | | 2110489 | WLP 175 |
| 28 | WLP 176 | NACPEC19-085 | Viburnum cassinoides L. | North Carolina, United States | NA | | | 2019 | COLLECTED | 09/18/2019 | Clay County; Nantahala National Forest: Forest Road 6269: Buck Creek Serpentine Barrens: main trail | 35.08593700, -83.61539800 | 1057 | Pinus rigida-Quercus alba / Sporobulus heterolepis-Andropogon gerardii Woodland OR Southern Blue Ridge Ultramafic Outcrop Barren | Wild material | | 2110490 | WLP 176 |
| 29 | Ames 28264 | SC 3 | Monarda fistulosa L. | Ohio, United States | NC7 |  | | 2004 | COLLECTED | 09/30/2004 | West of Columbus on State Route 161, south on Kramer Road, west on Boyd Road, Smith Cemetery State Nature Preserve, Madison County. | 40.10305556, -83.32416667 | 294 | Small prairie remnant in pioneer cemetery; surrounded by farm fields. Full sun. Slight slope, south facing. Fair drainage. Site size 5 square meters; total land area approximately 300 feet x 300 feet. | Wild material | 2-3 feet in height. Pink/lilac flowers, foliage scented. | 1690523 | Ames 28264 |