| 0 | MIA 37281 Orna | MIA 37281 Orna | Sabal minor (Jacq.) Pers. | | MIA |  | | 2023 | | | | | | | | | 2170651 | MIA 37281 Orna |
| 1 | MIA 37282 Orna | MIA 37282 Orna | Sabal minor (Jacq.) Pers. | | MIA |  | | 2023 | | | | | | | | | 2170652 | MIA 37282 Orna |
| 2 | MIA 37283 Orna | MIA 37283 Orna | Sabal minor (Jacq.) Pers. | | MIA |  | | 2023 | | | | | | | | | 2170653 | MIA 37283 Orna |
| 3 | MIA 37284 Orna | MIA 37284 Orna | Sabal minor (Jacq.) Pers. | | MIA |  | | 2023 | | | | | | | | | 2170654 | MIA 37284 Orna |
| 4 | MIA 37280 Orna | MIA 37280 Orna | Sabal minor (Jacq.) Pers. | | MIA |  | | 2022 | | | | | | | | | 2170650 | MIA 37280 Orna |
| 5 | NA 88583 | 2024RJLFL-014 | Ilex amelanchier M. A. Curtis ex Chapm. | Florida, United States | NA | | | 2024 | COLLECTED | 11/13/2024 | Yellow River Water Management Area: found in an area where an unnamed unpaved road dead ends near the Yellow River. This unpaved road is accessed from Old River Road to the east near the junction with Shockley Springs Road. Individual plants for this collection were accessed by foot along the edge of the river and associated wetland depressions to the east of the road. The sampling for this portion of the population extends from the GPS coordinates listed above to the northeast where sampling ended at coordinates 30.871238 deg. N, 86.590170 deg. W. | 30.86989400, -86.59218500 | 23 | Plants growing in seasonally inundated swamp habitats associated with the Yellow River and small tributaries. Plants are emergent during portions of the year, primarily during the growing season. During this time of collection, water had receded from the wetlands and the area was relatively dry. Slope: N/A. Aspect: N./A. The underlying geology of this area is the Alum Bluff Group of Miocene origin. It includes the Chipola Formation, Oak Grove Sand, Shoal River Formation, Choctawhatchee Formation and the Jackson Bluff Formation. The formations included in this group are generally defined based on their molluscan faunas and stratigraphic position. Puri (1953) described sediment facies as they relate to the formations of the Alum Bluff Group. These sediments are lithologically distinct as a group, not as individual units. The Alum Bluff Group crops out or is beneath a thin overburden in the western panhandle from river valleys in Okaloosa County eastward to western Jackson County. The Alum Bluff Group consists of clays, sands and shell beds which may vary from fossiliferous, sandy clays to unfossiliferous sands and clays and occasional carbonate beds. Mica is a common constituent and glauconite and phosphate occur sporadically. Induration varies from essentially nonindurated in sands to well indurated in carbonate lenses. Colors range from cream to olive gray with mottled reddish brown in weathered sections. Sand grain size varies from very fine to very coarse with sporadic occurrences of gravel. These sediments generally have low permeabilities and are part of the intermediate confining unit/aquifer system. (Source: USGS Florida Geologic Map Data). The surface soil profile of this area is primarily Kinston, Johnston, and Bibb soils, frequently flooded. Kinston Series soils are poorly drained, alluvial, fine-loamy, siliceous, and acid soils of flood plains. They are peaty to loamy friable, slightly sticky, and slightly plastic in the upper 0 to 7.5 cm of the strata with less sand and more silt-loam in progressively deeper strata. The Johnston 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 strata to 1.75 m are dark gray, loamy fine sand, single grained, loose and very strongly acid. (Source: NRCS Web Soil Survey). | Wild material | | 2169920 | NA 88583 |
| 6 | NA 88477 | TXWL2024-027 | Ilex ambigua Torr. | Texas, United States | NA | | | 2024 | COLLECTED | 11/12/2024 | Sabine River at I-10 at the Texas/Louisiana state line; south side of bridge. | 30.12654000, -93.70258000 | | Bottomland. | Wild material | | 2169862 | NA 88477 |
| 7 | NA 89092 | 2024RM-TK-005 | Ilex amelanchier M. A. Curtis ex Chapm. | Florida, United States | NA | | | 2024 | COLLECTED | 09/29/2024 | Yellow River Water Management Area: found in an area where an unnamed, unpaved road dead ends near the Yellow River. This unpaved road is accessed from Old River Road to the east near the junction with Shockley Springs Road. Plants are accessed by foot along the edge of the river and associated wetland depressions to the west of the road. | 30.86946200, -86.59349000 | 23 | Plants growing in seasonally inundated swamp habitats associated with the Yellow River. Plants are emergent during portions of the year, primarily during the growing season. During this time of collection, water had receded from the wetlands but the area was still quite wet with many tiny stream rivulets still draining. Slope: 0 percent. Aspect: N/A. Geology: The underlying geology of this area is the Alum Bluff Group of Miocene origin. It includes the Chipola Formation, Oak Grove Sand, Shoal River Formation, Choctawhatchee Formation and the Jackson Bluff Formation. The formations included in this group are generally defined based on their molluscan faunas and stratigraphic position. Puri (1953) described sediment facies as they relate to the formations of the Alum Bluff Group. These sediments are lithologically distinct as a group, not as individual units. The Alum Bluff Group crops out or is beneath a thin overburden in the western panhandle from river valleys in Okaloosa County eastward to western Jackson County. The Alum Bluff Group consists of clays, sands and shell beds which may vary from fossiliferous, sandy clays to unfossiliferous sands and clays and occasional carbonate beds. Mica is a common constituent and glauconite and phosphate occur sporadically. Induration varies from essentially nonindurated in sands to well indurated in carbonate lenses. Colors range from cream to olive gray with mottled reddish brown in weathered sections. Sand grain size varies from very fine to very coarse with sporadic occurrences of gravel. These sediments generally have low permeabilities and are part of the intermediate confining unit/aquifer system. (Source: USGS Florida Geologic Map Data). Soils: The surface soil profile of this area is primarily Kinston, Johnston, and Bibb soils, frequently flooded. Kinston Series soils are poorly drained, alluvial, fine-loamy, siliceous, and acid soils of flood plains. They are peaty to loamy friable, slightly sticky and slightly plastic in the upper 0 to 7.5 cm of the strata with less sand and more silt-loam in progressively deeper strata. The Johnston 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 strata to 1.75 m are dark gray, loamy fine sand, single grained, loose and very strongly a).id. The Bibb Series soils consist of very deep, poorly drained, moderately permeable soils on flood plains of streams in the Southern Coastal Plain (133A) Major Land Resource Area. They formed in stratified loamy and sandy alluvium that are commonly and frequently flooded and water runs off the surface very slowly. Slopes range from 0 to 2 percent. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). EPA Ecoregion (Level III): Southeastern Plains (65). EPA Ecoregion (Level IV): Southeastern Floodplains and Low Terraces (65p). | Wild material | | 2169056 | NA 89092 |
| 8 | NA 88851 | TJK2023FL-046 | Aronia arbutifolia (L.) Pers. | Florida, United States | NA |  | | 2024 | COLLECTED | 12/26/2023 | George Washington Swamp, Highway 98, approximately 0.1 miles west of Twine Rd. | 29.77650000, -85.27540000 | 5 | Roadside. Wet wooded edge running along George Washington Swamp bottom. Slope: less than 4%. Aspect: South-southwest. Elevation: 16 feet. | Wild material | | 2165706 | NA 88851 |
| 9 | NA 88843 | RJL-RM2023FLAL-017 | Rhododendron austrinum (Small) Rehder | Florida, United States | NA | | | 2023 | COLLECTED | 12/11/2023 | Holmes Creek at Live Oak Landing: plants found on the low bluff along the south side of Holmes Creek accessed by foot from a parking lot on Live Oak Landing Road that dead ends into the creek. | 30.59043500, -85.83899800 | 7 | Plants are growing in part shade to shade on the top and slope of the low bluff overlooking Holmes Creek in a mixed deciduous and evergreen forest. The dry mesic habitat has relatively low competition and is quite acidic. Slope: 0 to 45 percent. Aspect: Northwest. 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.) The surface soil profile of this area is primarily Nankin-Cowarts-Lakeland Complex. The Nankin Series consists of very deep, well drained, moderately slowly permeable soils on uplands of the Coastal Plain. They formed in stratified loamy and clayey marine sediments. Slopes range from 0 to 60 percent. Soils are comprised of sandy loam in the upper 25 cm to sandy clay loam and sandy clay in lower strata to about 1.7 meters deep; these soils are strongly acid. The Cowarts Series consists of very deep, moderately well and well drained soils on ridge tops and side slopes on uplands of the Coastal Plain Major Land Resource Area. They formed in loamy marine sediments. Slopes range from 1 to 60 percent. 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. 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 | | 2165673 | NA 88843 |
| 10 | NA 88845 | RJL-RM2023FLAL-019 | Ilex opaca Aiton | Florida, United States | NA | | | 2023 | COLLECTED | 12/13/2023 | Yellow River Water Management Area, found along an unnamed unpaved road leading down to the Yellow River. This unpaved road is accessed from Old River Road to the east near the junction with Shockley Springs Road. | 30.87382600, -86.60221300 | 35 | Plants are growing along the road on the woodland edge on a small bluff above a creek in well-drained to dry habitat in part shade. They are also found sporadically in areas along the Yellow River where occasional inundation occurs. Slope: N/A. Aspect: N/A. The underlying geology of this area is the Alum Bluff Group of Miocene origin. It includes the Chipola Formation, Oak Grove Sand, Shoal River Formation, Choctawhatchee Formation and the Jackson Bluff Formation. The formations included in this group are generally defined on the basis of their molluscan faunas and stratigraphic position. Puri (1953) described sediment facies as they relate to the formations of the Alum Bluff Group. These sediments are lithologically distinct as a group, not as individual units. The Alum Bluff Group crops out or is beneath a thin overburden in the western panhandle from river valleys in Okaloosa County eastward to western Jackson County. The Alum Bluff Group consists of clays, sands and shell beds which may vary from fossiliferous, sandy clays to unfossiliferous sands and clays and occasional carbonate beds. Mica is a common constituent and glauconite and phosphate occur sporadically. Induration varies from essentially nonindurated in sands to well indurated in carbonate lenses. Colors range from cream to olive gray with mottled reddish brown in weathered sections. Sand grain size varies from very fine to very coarse with sporadic occurrences of gravel. These sediments generally have low permeabilities and are part of the intermediate confining unit/aquifer system. (Source: USGS Florida Geologic Map Data.) The surface soil profile of this area is primarily Bonifay-Dothan-Angie complex (5 to 12 percent slopes). Bonifay soil consists of very deep, well drained, moderately slowly permeable soils on ridges and side slopes in the Southern Coastal Plain. They formed in thick beds of sandy and loamy marine sediments. Solum thickness ranges from 1.5-2.0 m. Soil reaction ranges from very strongly acid to moderately acid throughout, except where the surface has been limed. Ironstone pebbles, 2 to 15 mm in size, range from 0 to 5 percent, by volume. Depth to the plinthic horizon ranges from 1.1-1.7 m. Some horizons contain up to 25 percent plinthite by volume. The Dothan Series consists of very deep, well drained soils that formed in thick beds of unconsolidated, medium to fine-textured marine sediments. Dothan soils are on interfluves. The surface 0-33 cm is characterized by sandy-loam, well-drained soils that are strongly acid. From 33-200 cm they are characterized by sandy clay loam soils that are more moisture retentive and strongly acid. The Angie series consists of very deep, moderately well drained, slowly permeable soils that formed in loamy and clayey sediment on Tertiary-aged uplands. These soils are on broad, level to strongly sloping coastal plains. Slope is dominantly 1 to 5 percent, but the range is 0 to 12 percent. (Source: NRCS Web Soil Survey.) | Wild material | | 2165675 | NA 88845 |
| 11 | NA 88846 | RJL-RM2023FLAL-020 | Ilex decidua Walter | Florida, United States | NA | | | 2023 | COLLECTED | 12/13/2023 | Yellow River Water Management Area: found in an area where an unnamed unpaved road dead ends near the Yellow River. This unpaved road is accessed from Old River Road to the east near the junction with Shockley Springs Road. | 30.86973100, -86.59168700 | 23 | Plants are growing primarily in part-shade to part-sun in low-lying moist habitats associated with the Yellow River. They are in the flood zone, but not regularly inundated. Slope: N/A. Aspect: N/A. The underlying geology of this area is the Alum Bluff Group of Miocene origin. It includes the Chipola Formation, Oak Grove Sand, Shoal River Formation, Choctawhatchee Formation and the Jackson Bluff Formation. The formations included in this group are generally defined on the basis of their molluscan faunas and stratigraphic position. Puri (1953) described sediment facies as they relate to the formations of the Alum Bluff Group. These sediments are lithologically distinct as a group, not as individual units. The Alum Bluff Group crops out or is beneath a thin overburden in the western panhandle from river valleys in Okaloosa County eastward to western Jackson County. The Alum Bluff Group consists of clays, sands and shell beds which may vary from fossiliferous, sandy clays to unfossiliferous sands and clays and occasional carbonate beds. Mica is a common constituent and glauconite and phosphate occur sporadically. Induration varies from essentially nonindurated in sands to well indurated in carbonate lenses. Colors range from cream to olive gray with mottled reddish brown in weathered sections. Sand grain size varies from very fine to very coarse with sporadic occurrences of gravel. These sediments generally have low permeabilities and are part of the intermediate confining unit/aquifer system. (Source: USGS Florida Geologic Map Data.) The surface soil profile of this area is primarily Kinston, Johnston, and Bibb soils, frequently flooded. Kinston Series soils are poorly drained, alluvial, fine-loamy, siliceous, and acid soils of flood plains. They are peaty to loamy friable, slightly sticky and slightly plastic in the upper 0 to 7.5 cm of the strata with less sand and more silt-loam in progressively deeper strata. The Johnston 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 strata to 1.75 m is dark gray, loamy fine sand, single grained, loose and very strongly acid. The Bibb Series soils consists of very deep, poorly drained, moderately permeable soils on flood plains of streams in the Southern Coastal Plain (133A) Major Land Resource Area. They formed in stratified loamy and sandy alluvium that are commonly and frequently flooded and water runs off the surface very slowly. Slopes range from 0 to 2 percent. (Source: NRCS Web Soil Survey.) | Wild material | | 2165676 | NA 88846 |
| 12 | NA 88847 | RJL-RM2023FLAL-021 | Ilex amelanchier M. A. Curtis ex Chapm. | Florida, United States | NA | | | 2023 | COLLECTED | 12/13/2023 | Yellow River Water Management Area, found in an area where an unnamed unpaved road dead ends near the Yellow River. This unpaved road is accessed from Old River Road to the east near the junction with Shockley Springs Road. Individuals are accessed by foot along the edge of the river and associated wetland depressions to the west of the road. | 30.86980100, -86.59210500 | 23 | Plants growing in seasonally inundated swamp habitats associated with the Yellow River. Plants are emergent during portions of the year, primarily during the growing season. During this time of collection, water had receded from the wetlands but the area was still quite wet with many tiny stream rivulets still draining. Slope: N/A. Aspect: N/A. The underlying geology of this area is the Alum Bluff Group of Miocene origin. It includes the Chipola Formation, Oak Grove Sand, Shoal River Formation, Choctawhatchee Formation and the Jackson Bluff Formation. The formations included in this group are generally defined on the basis of their molluscan faunas and stratigraphic position. Puri (1953) described sediment facies as they relate to the formations of the Alum Bluff Group. These sediments are lithologically distinct as a group, not as individual units. The Alum Bluff Group crops out or is beneath a thin overburden in the western panhandle from river valleys in Okaloosa County eastward to western Jackson County. The Alum Bluff Group consists of clays, sands and shell beds which may vary from fossiliferous, sandy clays to unfossiliferous sands and clays and occasional carbonate beds. Mica is a common constituent and glauconite and phosphate occur sporadically. Induration varies from essentially nonindurated in sands to well indurated in carbonate lenses. Colors range from cream to olive gray with mottled reddish brown in weathered sections. Sand grain size varies from very fine to very coarse with sporadic occurrences of gravel. These sediments generally have low permeabilities and are part of the intermediate confining unit/aquifer system. (Source: USGS Florida Geologic Map Data.) The surface soil profile of this area is primarily Kinston, Johnston, and Bibb soils, frequently flooded. Kinston Series soils are poorly drained, alluvial, fine-loamy, siliceous, and acid soils of flood plains. They are peaty to loamy friable, slightly sticky and slightly plastic in the upper 0 to 7.5 cm of the strata with less sand and more silt-loam in progressively deeper strata. The Johnston 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 strata to 1.75 m is dark gray, loamy fine sand, single grained, loose and very strongly acid. The Bibb Series soils consists of very deep, poorly drained, moderately permeable soils on flood plains of streams in the Southern Coastal Plain (133A) Major Land Resource Area. They formed in stratified loamy and sandy alluvium that are commonly and frequently flooded and water runs off the surface very slowly. Slopes range from 0 to 2 percent. (Source: NRCS Web Soil Survey.) | Wild material | | 2165677 | NA 88847 |
| 13 | NA 88822 | TJK2023FL-039 | Viburnum obovatum Walter | Florida, United States | NA | | | 2023 | COLLECTED | 12/09/2023 | Freeport, Florida: Nokuse Plantation, E.O. Wilson Biophilia Center, State Highway 20. | 30.47615000, -86.05373000 | 15 | Edge of wet woods. Slope: 5%. Aspect: East. Elevation: 48 feet. | Wild material | | 2165651 | NA 88822 |
| 14 | NA 88824 | TJK2023FL-041 | Ilex opaca Aiton | Florida, United States | NA | | | 2023 | COLLECTED | 12/11/2023 | Holmes Creek, Live Oak Landing. | 30.60450000, -85.76670000 | 6 | Bottomland floodpain of Holmes Creek. Slope: flat. Aspect: Southwest. Elevation: 20 feet. | Wild material | | 2165653 | NA 88824 |
| 15 | NA 88825 | TJK2023FL-042 | Ilex verticillata (L.) A. Gray | Florida, United States | NA | | | 2023 | COLLECTED | 12/11/2023 | Holmes Creek, Live Oak Landing. | 30.60450000, -85.76670000 | 6 | Bottomland floodpain of Holmes Creek. Slope: flat. Aspect: Southwest. Elevation: 20 feet. | Wild material | | 2165654 | NA 88825 |
| 16 | NA 88826 | TJK2023FL-043 | Ilex decidua Walter | Florida, United States | NA | | | 2023 | COLLECTED | 12/14/2023 | Upper Escambia River. | 30.87870000, -87.29120000 | 9 | Hammock, bench-like river floodplain/bottomland. Slope: flat. Aspect: East-southeast. Elevation: 30 feet. | Wild material | | 2165655 | NA 88826 |
| 17 | NA 88815 | TXWL2023-022 | Ilex opaca Aiton | Texas, United States | NA | | | 2023 | COLLECTED | 12/10/2023 | Angelina National Forest: Upland Island Wilderness Area: Neches River bottom. | 31.03919400, -94.37937900 | | Bottomland hardwood forest. | Wild material | | 2165619 | NA 88815 |
| 18 | NA 88816 | TXWL2023-023 | Ilex decidua Walter | Texas, United States | NA | | | 2023 | COLLECTED | 12/10/2023 | Angelina National Forest: Upland Island Wilderness Area: Neches River bottom. | 31.03478500, -94.38286600 | | Bottomland hardwood forest. | Wild material | | 2165620 | NA 88816 |
| 19 | NA 88801 | TJK2023LA/TX-001 | Cocculus carolinus (L.) DC. | Louisiana, United States | NA | | | 2023 | COLLECTED | 11/21/2023 | Interstate 20, westbound, approximately 13 miles west of Mississippi River, 9 miles east of U.S. Highway 65. | 32.33740000, -91.06320000 | 24 | Damp low, wooded treeline. Slope: less than 2%. Aspect: Southwest. Elevation: 79 feet. | Wild material | | 2159184 | NA 88801 |
| 20 | NA 88802 | TJK2023LA/TX-002 | Ilex decidua Walter | Louisiana, United States | NA | | | 2023 | COLLECTED | 11/21/2023 | Interstate 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, -91.29670000 | 21 | Damp wooded treeline. Slope: 12%. Aspect: West-southwest. Elevation: 69 feet. | Wild material | | 2159185 | NA 88802 |
| 21 | NA 88803 | TJK2023LA/TX-003 | Crataegus viridis L. | Louisiana, United States | NA | | | 2023 | COLLECTED | 11/21/2023 | Interstate 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, -91.29670000 | 21 | Damp wooded treeline. Slope: 12%. Aspect: West-southwest. Elevation: 69 feet. | Wild material | | 2159186 | NA 88803 |
| 22 | NA 88804 | TJK2023LA/TX-004 | Crataegus viridis L. | Louisiana, United States | NA | | | 2023 | COLLECTED | 11/21/2023 | Walnut 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, -91.07170000 | 26 | Damp wooded treeline. Slope: 10%. Aspect: North-northeast. Elevation: 84 feet. | Wild material | | 2159187 | NA 88804 |
| 23 | 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 |
| 24 | NA 88660 | TJK2023FL-014 | Rhododendron austrinum (Small) Rehder | Florida, United States | NA | | | 2023 | COLLECTED | 09/15/2023 | Lower Yellow River, Grimes Lake. | 30.61930000, -86.81490000 | 3 | Elevation: 13 feet. Slope: 0 percent. Aspect: West-southwest. | Wild material | | 2158794 | NA 88660 |
| 25 | NA 88663 | TJK2023FL-017 | Rhododendron austrinum (Small) Rehder | Florida, United States | NA | | | 2023 | COLLECTED | 09/17/2023 | Lower Yellow River, below the Old Land Place. | 30.55513000, -86.94659000 | 0 | An area with very nice Pink R. austrinum. Elevation: 0. Slope: 0 percent. Aspect: South-southwest. | Wild material | | 2158797 | NA 88663 |
| 26 | NA 88598 | RJL2023FL-002a | Agarista populifolia (Lam.) Judd | Florida, United States | NA | | | 2023 | COLLECTED | 02/14/2023 | Plants growing in woodlands of Wekiwa Springs State Park along trails accessed from the Sand Lake parking lot at the end of Palmetto Avenue. From the parking lot, take the main trail south for about 18 meters and immediately take a cut-through trail on the left to the location of this population. | 28.72398600, -81.47205400 | 10 | Plants were growing in shade to part-shade of moist mesic hammocks of lowland transitional woodlands eventually becoming wetland habitats that are comprised primarily of evergreen plants with fewer deciduous plants. The underlying geology of this area is of Pliocene origin and characterized as the Cypresshead Formation. The Cypresshead Formation named by Huddlestun (1988), is composed of siliciclastics and occurs only in the peninsula and eastern Georgia. It is at or near the surface from northern Nassau County southward to Highlands County forming the peninsular highlands. It appears that the Cypresshead Formation occurs in the subsurface southward from the outcrop region and similar sediments, the Long Key Formation, underlie the Florida Keys. The Cypresshead Formation is a shallow marine, near shore deposit equivalent to the Citronelle Formation deltaic sediments and the Miccosukee Formation prodeltaic sediments. The Cypresshead Formation consists of reddish brown to reddish orange, unconsolidated to poorly consolidated, fine to very coarse grained, clean to clayey sands. Cross bedded sands are common within the formation. Discoid quartzite pebbles and mica are often present. Clay beds are scattered and not areally extensive. In general, the Cypresshead Formation in exposure occurs above 100 feet (30 meters) above mean sea level (msl). Original fossil material is not present in the sediments although poorly preserved molds and casts of mollusks and burrow structures are occasionally present. The presence of these fossil "ghosts" and trace fossils documents marine influence on deposition of the Cypresshead sediments. The permeable sands of the Cypresshead Formation form part of the surficial aquifer system. | Wild material | | 2141479 | NA 88598 |
| 27 | NA 88524 | RM-TK2022-012 | Hydrangea quercifolia W. Bartram | Florida, United States | NA | | | 2023 | COLLECTED | 10/20/2022 | Private property of Joann Palmer on Reservation Court | 30.23775000, -84.32410000 | 5 | Plants are abundant in this upland, dry, and arenaceous soil over karst.
Soils: The underlying geology of this area is the St. Michaels Formation of Miocene origin. The Lower Miocene St. Marks Formation, named by Finch (1823), is exposed in Wakulla, Leon and Jefferson Counties on the northwestern flank of the Ocala Platform. It is a white to yellowish gray, poorly to moderately indurated, sandy, fossiliferous (molds and casts) limestone (packstone to wackestone). Mollusk molds and casts are often abundant. The St. Marks Formation makes up the upper part of the FAS in part of the eastern panhandle.
Source: USGS Florida Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=FLMIsmk%3B0)
The surface soil profile found in this area is Otela limestone substratum-Ortega sands (0 to 5 percent slopes). The Otela Series consists of very deep, moderately well drained, moderately slowly to slowly permeable soils on broad uplands. They formed in sandy and loamy marine sediments over limestone on karst topography. Slopes range from 0 to 8 percent. The Ortega series consists of very deep, moderately well drained soils that formed in a sandy deposit on marine terraces. These soils are on nearly level to strongly sloping upland landscapes. Slopes range from 0 to 12 percent. Ortega Series soils are generally strongly acid.
https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2140805 | NA 88524 |
| 28 | NA 88542 | RJLSEUS2022-014 | Rosa palustris Marshall | Georgia, United States | NA | | | 2023 | COLLECTED | 12/09/2022 | Plants growing around a pond and associated wetland on the property of Monica Williams north of Albany, Georgia. Common along the transitional edges from wet to dry. | 31.63723900, -84.13776200 | 60 | Plants are growing in full sun mostly in the transitional edges of the pond where conditions are generally moist mesic. Even so, this species appears quite adaptable and can be found in quite moist as well as drier soil conditions.
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 | | 2140817 | NA 88542 |
| 29 | 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 |
| 30 | 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 |
| 31 | NA 88559 | RJLSEUS2022-032 | Rhododendron colemanii R. F. Mill. | Alabama, United States | NA | | | 2023 | COLLECTED | 12/12/2022 | Plants growing in bottomland mostly deciduous woodlands on the south side of Lena Landegger Hwy (Monroe County Road 39) about 0.5 kilometers south of the entrance to the Alabama River Cellulose plant. Common at this site. | 31.56879700, -87.49589500 | 10 | Plants are growing in shade of a moist mesic (occasionally temporarily wet) deciduous woodland less than 1 meter above wetland habitats associated with the nearby Alabama River.
Soils: The underlying geology of this area is of Holocene origin and characterized as Alluvial, coastal and low terrace deposits. Varicolored fine to coarse quartz sand containing clay lenses and gravel in places.
Source: USGS Alabama Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=ALHalt%3B0)
The primary soil types in the collection area are classified as Chrysler Silt Loam soils (0 to 5 percent slopes, occasionally flooded). The Chrysler Series consists of deep, moderately well drained, slowly permeable soils that formed in clayey fluvial or alluvial sediments. These soils are on stream terraces of the Coastal Plain. They are strongly acid. The rate at which water runs off the surface is medium to rapid. Slopes range from 0 to 5 percent.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2140784 | NA 88559 |
| 32 | NA 88566 | RJLSEUS2022-039 | Rhododendron viscosum (L.) Torr. | Florida, United States | NA | | | 2023 | COLLECTED | 12/14/2022 | Plants growing in woodlands at Escribano Point Bayou Campground not far from the parking lot. Occasional. | 30.50990400, -87.00414900 | 1 | Plants are growing in shade to part-shade of dense mesic vegetation only a few meters from the edge of mixed evergreen and deciduous woodland associated with the Yellow River Marsh Aquatic Preserve. While this habitat is typical mesic and well-drained, it is clearly subject to periods of inundation from high tides or storms as it is a meter or less above the marsh habitat. Additionally, it seems likely that there is plentiful moisture further down in the soil profile based on some of the plant associates.
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 FL Map Data (https://mrdata.usgs.gov/geology/state/state.php?state=fl)
The primary soil types in the collection area are classified as Ortega Sand soils (0 to 5 percent slopes). The Ortega Series consists of very deep, moderately well drained soils that formed in a sandy deposit on marine terraces. These soils are on nearly level to strongly sloping upland landscapes. Slopes range from 0 to 12 percent. They are extremely acid to slightly acid throughout. They are fine sand or sand to depths of more than 2 meters. Silt plus clay totals less than 5 percent between 25 cm and 1 meter depth.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2140788 | NA 88566 |
| 33 | NA 88567 | RJLSEUS2022-040 | Chamaecyparis thyoides (L.) Britton et al. | Florida, United States | NA | | | 2023 | COLLECTED | 12/14/2022 | Plants growing in woodlands at Escribano Point Bayou Campground not far from the parking lot. Occasional. | 30.51018200, -87.00448800 | 1 | Plants are growing in part-shade of dense mesic vegetation only a few meters from the edge of mixed evergreen and deciduous woodland associated with the Yellow River Marsh Aquatic Preserve. While this habitat surface is typical mesic and well-drained, it is clearly subject to periods of inundation from high tides or storms as it is a meter or less above the marsh habitat. Additionally, it seems likely that there is plentiful moisture further down in the soil profile based on some of the plant associates.
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 FL Map Data (https://mrdata.usgs.gov/geology/state/state.php?state=fl)
The primary soil types in the collection area are classified as Ortega Sand soils (0 to 5 percent slopes). The Ortega Series consists of very deep, moderately well drained soils that formed in a sandy deposit on marine terraces. These soils are on nearly level to strongly sloping upland landscapes. Slopes range from 0 to 12 percent. They are extremely acid to slightly acid throughout. They are fine sand or sand to depths of more than 2 meters. Silt plus clay totals less than 5 percent between 25 cm and 1 meter depth.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2140789 | NA 88567 |
| 34 | NA 88574 | RJLSEUS2022-047 | Rhododendron austrinum (Small) Rehder | Florida, United States | NA | | | 2023 | COLLECTED | 12/15/2022 | Plants are growing along a several mile stretch of the Yellow River and accessed by boat via the Yellow River Boat Ramp on the east side of Florida State Hwy 87. The species is found frequently along several miles of the Yellow River. | 30.58133600, -86.89953900 | 2 | Plants are found growing in part-shade to shade along areas of the river where natural levies, 1-3 meters tall, have formed, depositing sand and organic matter. The plants grow well-above normal flow of the river in well-drained to dry conditions. Even so, they are periodically subjected to inundation from floodwaters.
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 Bibb-Kinston Series Association. Bibb Series soils are coarse-loamy, sandy, acid soils that are poorly drained. They are soils of flood plains and streams subject to frequent flooding. These are found in association with Kinston Series soils that are fine-loamy, sandy, acid soils of flood plains and stream subject to frequent flooding. The Bibb-Kinston Association ranges from 1-1.5 meters thick and is strongly acid.
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 | Yellow River Pink Austrinum | 2140792 | NA 88574 |
| 35 | NA 88506 | RJL2022TX-001 | Itea virginica L. | Texas, United States | NA | | | 2022 | COLLECTED | 10/31/2022 | Plants growing at Shangri La Botanical Gardens and Nature Center, Orange, TX along Adams Bayou, accessed via internal service roads. Plant is infrequent at this site. | 30.10322000, -93.76271700 | 1 | Plants are growing in shade to part-shade of a Taxodium distichum-Nyssa aquatica dominated forested swampland associated with Adams Bayou in a wet low-lying area that is frequently inundated.
Soils: The underlying geology of this area is of Quaternary to Late Pleistocene origin and comprised of the Beaumont Formation. This formation is yellowish- to brownish-gray, locally reddish orange with very fine to fine quartz sand, silt, and minor fine gravel, intermixed and interbedded. It also includes stream channel, point-bar, cravasse-splay, and natural levee ridge deposits, and clayey fill in abandoned channels. Channel fill is dark brown to brownish-gray with laminated clay and silt that is organic-rich. Includes marine delta-front sand, lagoonal clay, and near-shore marine sand beneath and landward of bays along the coast. Depth of this unconsolidated outwash ranges from 3-100 meters thick.
Source: USGS Texas Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=TXQbs%3B0)
The primary soil types in the collection area are classified as Cowmarsh series. The Cowmarsh series consists of very deep, very poorly drained soils that formed in mucky silty clayey alluvial deposits of Holocene age. These depressional soils are oxbows and relict channels of rivers where flooding and ponding is frequent. Slope ranges from 0 to 1 percent but mainly less than 1 percent. very poorly drained. Runoff is negligible. Frequently flooded for very long periods from February through May and surface remains saturated for very long periods once flood waters have receded.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2139813 | NA 88506 |
| 36 | NA 88507 | RJL2022TX-002 | Fraxinus caroliniana Mill. | Texas, United States | NA | | | 2022 | COLLECTED | 10/31/2022 | Plants growing at Shangri La Botanical Gardens and Nature Center, Orange, TX along Adams Bayou, accessed via internal service roads. Plant is relatively common along Adams Bayou but scattered. | 30.09989400, -93.75239700 | 1 | Plants are growing in part-shade to sun of a Taxodium distichum-Nyssa aquatica dominated forested swampland associated with Adams Bayou in a wet low-lying area that is frequently inundated. While found as an occasional understory element, it is more common on the edge of the swampland forest where there are high light conditions.
Soils: The underlying geology of this area is of Quaternary to Late Pleistocene origin and comprised of the Beaumont Formation. This formation is yellowish- to brownish-gray, locally reddish orange with very fine to fine quartz sand, silt, and minor fine gravel, intermixed and interbedded. It also includes stream channel, point-bar, cravasse-splay, and natural levee ridge deposits, and clayey fill in abandoned channels. Channel fill is dark brown to brownish-gray with laminated clay and silt that is organic-rich. Includes marine delta-front sand, lagoonal clay, and near-shore marine sand beneath and landward of bays along the coast. Depth of this unconsolidated outwash ranges from 3-100 meters thick.
Source: USGS Texas Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=TXQbs%3B0)
The primary soil types in the collection area are classified as Cowmarsh series. The Cowmarsh series consists of very deep, very poorly drained soils that formed in mucky silty clayey alluvial deposits of Holocene age. These depressional soils are oxbows and relict channels of rivers where flooding and ponding is frequent. Slope ranges from 0 to 1 percent but mainly less than 1 percent. very poorly drained. Runoff is negligible. Frequently flooded for very long periods from February through May and surface remains saturated for very long periods once flood waters have receded.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2139814 | NA 88507 |
| 37 | NA 88508 | RJL2022TX-003 | Morella cerifera (L.) Small | Texas, United States | NA | | | 2022 | COLLECTED | 10/31/2022 | Plants growing at Shangri La Botanical Gardens and Nature Center Orange, TX along Adams Bayou, accessed via internal service roads. Plant is relatively common along Adams Bayou but scattered in the understory. | 30.10035500, -93.75288700 | 1 | Plants are growing in part-shade to shade of a Taxodium distichum-Nyssa aquatica dominated forested swampland associated with Adams Bayou in a wet low-lying area that is frequently inundated.
Soils: The underlying geology of this area is of Quaternary to Late Pleistocene origin and comprised of the Beaumont Formation. This formation is yellowish- to brownish-gray, locally reddish orange with very fine to fine quartz sand, silt, and minor fine gravel, intermixed and interbedded. It also includes stream channel, point-bar, cravasse-splay, and natural levee ridge deposits, and clayey fill in abandoned channels. Channel fill is dark brown to brownish-gray with laminated clay and silt that is organic-rich. Includes marine delta-front sand, lagoonal clay, and near-shore marine sand beneath and landward of bays along the coast. Depth of this unconsolidated outwash ranges from 3-100 meters thick.
Source: USGS Texas Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=TXQbs%3B0)
The primary soil types in the collection area are classified as Cowmarsh series. The Cowmarsh series consists of very deep, very poorly drained soils that formed in mucky silty clayey alluvial deposits of Holocene age. These depressional soils are oxbows and relict channels of rivers where flooding and ponding is frequent. Slope ranges from 0 to 1 percent but mainly less than 1 percent. very poorly drained. Runoff is negligible. Frequently flooded for very long periods from February through May and surface remains saturated for very long periods once flood waters have receded.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2139815 | NA 88508 |
| 38 | OPGC 8032 | NV020-10 | Asclepias fascicularis Decne. | Nevada, United States | OPGC | | | 2020 | | | | | | | Wild material | | 2106482 | OPGC 8032 |
| 39 | NA 87036 | Site 3A/Live Oak Landing/Holmes Creek Site | Magnolia ashei Weath. | Florida, United States | NA | | | 2020 | COLLECTED | 07/15/2020 | Along Holmes Creek at Live Oak Landing. | 30.59208000, -85.83750000 | 11 | Shade to partial shade of bluffs above the creek in well-drained mesic to dry deciduous woodlands with a few broadleaved and coniferous evergreens. | Wild material | Although these were collected without any field collection number, seeds from individual trees were separated with letter identifiers that will be maintained with the qualifier (seedling) records. The relationships are as follows: 1. Maternal letter G, NA 87036-J, L, P, and T; maternal letter H, NA 87036-V; maternal letter K, NA 87036-X, Z, and H1; maternal letter N, NA 87036-H2. In addition, three seedlings' maternal letters were lost, and these will be NA 87036-H3, H4, and H5. See the following accessions for earlier collections from this same site/population, listed in our records as "Site 3A/Live Oak Landing/Holmes Creek Site": NA 81555 (2013), NA 82745 (2015), and NA 82745.01 (2019). | 2109403 | NA 87036 |
| 40 | WLP 2491 | Florida Caverns State Park | Hydrangea quercifolia W. Bartram | Florida, United States | NA |  | | 2019 | COLLECTED | 10/26/2017 | Florida Caverns State Park, Jackson County. Large population growing in two disjunct groups. Larger group is growing on the outcrops along Bluff Trail near the mouth of the cave. The smaller group is growing ca. 40 m north (This group is most accessible from the road to the campground, approximately 50 m east of the Chipola River). | 30.81017000, -85.22830000 | | Limestone outcrops above Taxodium distichum dominated swamp. | Wild material | Measurements of sampled specimens taken in nature: Height 53 to 168 in.; width 40 to 196 in. Measurements for each specimen sampled may be provided upon request (NA 86152.01 through 86152.27.) Most of the specimens in this population noted in nature (16 October 2017) had powdery mildew and/or bacterial leaf spot. | 2106201 | WLP 2491 |
| 41 | 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 |
| 42 | NA 82746 | Site 3B/Hightower Road at Holmes Creek | Magnolia ashei Weath. | Florida, United States | NA | | | 2015 | COLLECTED | 07/31/2015 | Along Holmes Creek 0.2 miles west-southwest of Hard Castle Landing boat ramp at hte end of Hightower Road. | 30.60401000, -85.76883000 | 11 | Shade to partial shade of deciduous woodlands 10 to 15 feet above the creek, surrounded by low lying swampy area. | Wild material | Originally just called Site 3, but the "A/B" has been added to distinguish the Live Oak Landing (3A) and Hightower Road (3B) material. For previous collections of this population, see NA 81556 (2013); for later collection, see NA 82746.01 (2019). | 1950860 | NA 82746 |
| 43 | Ames 32797 | JDC/FP/2014/113/615 | Fraxinus pennsylvanica Marshall | Mississippi, United States | NC7 |  | | 2014 | COLLECTED | 09/27/2014 | Delta National Forest, T12N, R6W, Sharkey County. | 32.81010300, -90.78898200 | 30 | Bottomlands. | Wild material | | 1921808 | Ames 32797 |
| 44 | NA 81566 | NA 81566 | Rhododendron austrinum (Small) Rehder | Florida, United States | NA | | | 2013 | COLLECTED | 03/31/2013 | White River approximately 0.92 miles north of the confluence with the Escambia River in the Escambia River State Wildlife Management Area. [Originally listed as: "Buzzard�s Lake River approximately 0.92 miles north of the confluence with the Escambia River..."; GPS coordinates are along the White River, and well south of the confluence with Buzzards Lake River. -SBL] | 30.58168000, -87.22233000 | 2 | Partial shade along the river on small sand berm above the stream in mixed deciduous and broadleaved evergreen maritime forest occasionally inundated by tidal salt water. | Wild material | | 1953003 | NA 81566 |
| 45 | NA 81570 | (orange suffused with rose) | Rhododendron austrinum (Small) Rehder | Florida, United States | NA | | | 2013 | COLLECTED | 03/31/2013 | Little Simpson River approximately 0.53 miles southeast of the confluence with Buzzards Lake River [and White River] in the Escambia River State Wildlife Management Area. | 30.59421000, -87.21575000 | 2 | Light shade along the river on a small sandy berm above the stream in mixed deciduous and broadleaved evergreen maritime forest occasionally inundated by tidal salt water. | Wild material | | 1951291 | NA 81570 |
| 46 | NA 81571 | (clear light pink) | Rhododendron austrinum (Small) Rehder | Florida, United States | NA | | | 2013 | COLLECTED | 03/31/2013 | White River approximately 1.1 miles north of the confluence with Buzzard�s Lake River in the Escambia River State Wildlife Management Area. | 30.60490000, -87.22261000 | 2 | Part shade along the river on a small sandy berm above the stream in mixed deciduous and broadleaved evergreen maritime forest occasionally inundated by tidal salt water. | Wild material | | 1952627 | NA 81571 |
| 47 | NA 81603 | (seedling of pink form) | Rhododendron austrinum (Small) Rehder | Florida, United States | NA | | | 2013 | COLLECTED | 2013 | On the Escambia river near the mouth of the Yellow River. [GPS coordinates are actually at the confluence of the White River, the Little Simpson River, and the Buzzard Lake River (and gas line canal). -SBL] | 30.59699000, -87.22295000 | | Plants were collected along along the sandy berms along river delta. | | | 1950972 | NA 81603 |