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ACCESSIONPLANT NAMETAXONOMYORIGINGENEBANKIMAGEAVAILABILITYRECEIVEDSOURCE TYPESOURCE DATECOLLECTION SITECOORDINATESELEVATIONHABITATIMPROVEMENT LEVELNARRATIVE
0DVIT 2565'Rogers 638'Vitis shuttleworthii House Florida, United StatesDAV1995COLLECTED08/11/1995Breeding materialType = Species.1565317DVIT 2565
1DVIT 2366D'arpaVitis shuttleworthii House United StatesDAV1990COLLECTEDCultivated materialType = Species. Moderately resistant to PD, anthracnose, bitter rot (Melanconium fuligineum (Scrib. and Viala) Cav., Isariopsis leaf blight, and root-knot nematodes; medium vigor and moderately high productivity; of good quality for wild type. [Berry] fruit color red. Large berry, medium bunch.1019965DVIT 2366
2DVIT 2386Haines CityVitis shuttleworthii House United StatesDAV1990COLLECTEDCultivated materialType = Species. Highly resistant to PD, anthracnose, downy mildew, Isariopsis leaf blight, and root-knot nematodes; moderately resistant to bitter rot; great vigor, growing near Lake Hatchineha and medium productivity; proven breeding parent for rootstocks. [Berry] fruit color red. Medium berry, medium small bunch.1020109DVIT 2386
3DVIT 2387KissimmeeVitis shuttleworthii House United StatesDAV1990COLLECTEDCultivated materialType = Species. Highly resistant to PD, anthracnose, downy mildew, Isariopsis leaf blight, and root-knot nematodes; extremely vigorous, occurred naturally with roots entirely under water in Lake Kissimmee, but also fully drought resistant; proven breeder from roots.1020114DVIT 2387
4DVIT 2249DVIT 2249Vitis shuttleworthii House Florida, United StatesDAV1987COLLECTEDWild materialType = Species.1019168DVIT 2249
5DVIT 1719Olmo (U69-50)Vitis shuttleworthii House California, United StatesDAV1983DONATED01/01/1983Breeding materialType = species. Flower type = female.1015663DVIT 1719
6DVIT 1720Olmo (U69-45)Vitis shuttleworthii House California, United StatesDAV1983DONATED01/01/1983Breeding materialType = species. Flower type = hermaphrodite1015671DVIT 1720
7DVIT 2473'Largo'Vitis hybr.Florida, United StatesDAV1997DONATED08/18/1997Cultivated materialOriginally received 2/1/94, but it died. Type = Hybrid. Self-fertile. Cross of Fennell 105 (V. rufotomenstosa x Ribier) with Fennell 23 (a wild vine, apparently a natural cross between V. shuttleworthii and V. rofotomentosa), the seed parent. First fruited 1946 in Turrialba, Costa Rica. Clusters 8"-10", somewhat compound. Berries round, medium size, black. Skin medium thin, pulp tender and melting, flavor similar to vinifera. In Florida both size and quality of fruit have been inferior to what was seen in Costa Rica. Vine healthly and vigorous.1564130DVIT 2473
8DVIT 2474'Caribe'Vitis hybr.Florida, United StatesDAV1997DONATED08/18/1997Cultivated materialType = Hybrid. Sex = Female. Cross of "Fairchild" (Fennell 106) and "Tropico" (Fennell 240), the seed parent. First fruited in 1953 at Lady Lake, Florida. Large, compound clusters with good berry set if well pollinated. Berries are about 3/4" slightly ovoid, black, with thin skin, tender pulp, clear red juice. Flavor medium sweet throughout. Heavy fruit production. Vine very vigorous, sometimes susceptable to downy mildew, apparently free of black rot. {Note on parents: Fairchild is a cross of the vinifera variety Alphonse Lavelle (Ribier) with V. tileaefolia ("Agras") of Cental America, first fruited at Princeton, Florida, in 1940 and apparently held at the Davis Germplasm Repository as Accession No. 165. Tropico is a cross between Lomanto (V. champini-labrusca-vinifera) and the wild "Calloosa" grape (V. shuttleworthii) of south Florida, first fruited in 1943.}1564131DVIT 2474
9DVIT 166'Tamiami'Vitis hybr.Florida, United StatesDAV1995DEVELOPED03/15/1966Cultivated materialType = American hybrid. Per Brooks and Olmo (see citation): "Fruit: quality good; sugar content high; resembles a medium sized berry of Vitis vinifera; tend to recent tests (1967) at Watermelon and Grape Investigations Lab, Leesburg, Fla. Vine: extremely vigorous, with some canes 40-50 ft. long, large trunk and arms; resistant to downy and powdery mildew, susceptible to anthracnose and moderately susceptible to Pierce's disease." Fennell 6 was also called Prairie Creek. It was discovered in the wild by Dr. J. L. Fennell in 1936 near Punta Gorda, Florida. It is a natural hybrid of Vitis smalliana x Vitis shuttleworthii.1003828DVIT 166
10DVIT 2393ManteyVitis hybr. United StatesDAV1990COLLECTEDCultivated materialType = Hybrid. Resistant to PD, bitter rot, downy mildew; less resistant to anthracnose and root-knot nematodes; susceptible to drought; vine moderately vigorous and of medium productivity; parent of 'Stover'. [Berry] fruit color light red. Medium berry and moderately small bunch.1020143DVIT 2393
11DVIT 2381FLA CA 8-15Vitis hybr.Florida, United StatesDAV1990DONATED02/05/1990Breeding materialType = Hybrid. Highly resistant to PD, bitter rot, and downy mildew; moderately resistant to root-knot nematodes; fairly susceptible to anthracnose; medium vigor vine and medium productivity. Leaves like shuttleworthii. [Berry] fruit color purple. Medium berry on medium clusters.1020079DVIT 2381
12NA 891712025RJLSEUS-04Rhododendron catawbiense Michx. Alabama, United StatesNA2026COLLECTED09/30/2025Scarham Creek: southeast of the Pea Ridge Road bridge, approximately 50-80 meters on the south side of the creek.34.32559600, -86.16054600266Growing near the base of the slopes above the riparian zone, generally on the exposed geology under very well-drained conditions. The woodlands are primarily deciduous with a few evergreens infrequently mixed. Slope: 15 to 30 percent. Aspect: Northeast. Soil: The primary soil type in the area of this collection is classified as Rockland Series sandstone (Rc). The Rockland series consists of well drained soils formed in loamy colluvium from rotational landslides on slopes of stream valleys and dissections of ground moraines. Saturated hydraulic conductivity is moderate in the upper part of the profile and moderately slow in the lower part. Slopes range from 18 to 70 percent. Some pedons have buried leaves, twigs, and moss. Mass soil movement has left random remnants of soil structure from prior upslope soil development and has buried tree branches, leaves and moss. The upper 0-2 cm of soil contains slightly decomposed organic matter while lower soils layers to a depth of 58 cm are comprised of dark reddish-brown to brown silt loam and are moderately acidic. Below 58 cm the soils are generally dark reddish-brown silt loam and strongly to moderately alkaline. (Source:California Soil Resource Lab/NRCS Official Soil Series Descriptions). Geology: The underlying geology of this area is of Pennsylvanian origin and characterized as Pottsville Formation. It is characterized by light-gray thin to thick-bedded quartzose sandstone and conglomerate containing interbedded dark-gray shale, siltstone, and coal. Mapped on Lookout Mountain, Blount and Chandler Mountains, and Sand Mountain northeast of Blount County, and on the mountains of Jackson, Marshall, and Madison Counties north and west of the TN river. (Source: USGS Alabama Geologic Map Data).Wild materialReceived as R. catawbiense vsr. insularis2193305NA 89171
13NA 891552025RJLSEUS-02Ilex longipes Chapm. ex Trel. Alabama, United StatesNA2025COLLECTED09/30/2025Scarham Creek: southeast of the Pea Ridge Road bridge, approximately 50-80 meters on the south side of the creek.34.32520700, -86.15967000261Plants are growing on relatively steep woodland slopes in shade. The woodlands are primarily deciduous with a few evergreens infrequently mixed. Slope: 15 to 30 percent. Aspect: Northeast. Soil: The primary soil type in the area of this collection is classified as Rockland Series sandstone (Rc). The Rockland series consists of well drained soils formed in loamy colluvium from rotational landslides on slopes of stream valleys and dissections of ground moraines. Saturated hydraulic conductivity is moderate in the upper part of the profile and moderately slow in the lower part. Slopes range from 18 to 70 percent. Some pedons have buried leaves, twigs, and moss. Mass soil movement has left random remnants of soil structure from prior upslope soil development and has buried tree branches, leaves and moss. The upper 0-2 cm of soil contains slightly decomposed organic matter while lower soils layers to a depth of 58 cm are comprised of dark reddish-brown to brown silt loam and are moderately acidic. Below 58 cm the soils are generally dark reddish-brown silt loam and strongly to moderately alkaline. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). Geology: The underlying geology of this area is of Pennsylvanian origin and characterized as Pottsville Formation. It is characterized by light-gray thin to thick-bedded quartzose sandstone and conglomerate containing interbedded dark-gray shale, siltstone, and coal. Mapped on Lookout Mountain, Blount and Chandler Mountains, and Sand Mountain northeast of Blount County, and on the mountains of Jackson, Marshall, and Madison Counties north and west of the TN river. (Source: USGS Alabama Geologic Map Data).Wild material2193001NA 89155
14NA 891562025RJLSEUS-03Euonymus americanus L. Alabama, United StatesNA2025COLLECTED09/30/2025Scarham Creek: southeast of the Pea Ridge Road bridge, approximately 50-80 meters on the south side of the creek.34.32577600, -86.16071000260Plants are growing on relatively steep woodland slopes in shade. The woodlands are primarily deciduous with a few evergreens infrequently mixed. Slope: 15 to 30 percent. Aspect: Northeast. Soil: The primary soil type in the area of this collection is classified as Rockland Series sandstone (Rc). The Rockland series consists of well drained soils formed in loamy colluvium from rotational landslides on slopes of stream valleys and dissections of ground moraines. Saturated hydraulic conductivity is moderate in the upper part of the profile and moderately slow in the lower part. Slopes range from 18 to 70 percent. Some pedons have buried leaves, twigs, and moss. Mass soil movement has left random remnants of soil structure from prior upslope soil development and has buried tree branches, leaves and moss. The upper 0-2 cm of soil contains slightly decomposed organic matter while lower soils layers to a depth of 58 cm are comprised of dark reddish-brown to brown silt loam and are moderately acidic. Below 58 cm the soils are generally dark reddish-brown silt loam and strongly to moderately alkaline. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). Geology: The underlying geology of this area is of Pennsylvanian origin and characterized as Pottsville Formation. It is characterized by light-gray thin to thick-bedded quartzose sandstone and conglomerate containing interbedded dark-gray shale, siltstone, and coal. Mapped on Lookout Mountain, Blount and Chandler Mountains, and Sand Mountain northeast of Blount County, and on the mountains of Jackson, Marshall, and Madison Counties north and west of the TN river. (Source: USGS Alabama Geologic Map Data).Wild material2193002NA 89156