| 0 | PI 341750 | 'Hoerscholmiensis' | Ulmus minor Mill. | Netherlands | NC7 | | | 1969 | DONATED | 03/20/1969 | | | | | Cultivar | Crown dense, narrow at base to nearly globose above. Leaves narrow. Resistance moderate. Wind resistant, cold hardy. Progeny nearly homogenous. | 1254934 | PI 341750 |
| 1 | PI 313550 | 'Christine Buisman' | Ulmus minor Mill. | Netherlands | NC7 | | | 1966 | COLLECTED | | | | | | Cultivar | Tree uniform, very erect, medium leafy, much branched. Excellent winter hardiness and spring vigor. | 1234072 | PI 313550 |
| 2 | NA 85690 | 'Sarniensis' | Ulmus minor Mill. | | NA | | | 2011 | | | | | | | Cultivar | From branch segments collected from a mature specimen growing as part of the NCCPG National Elm Collection, Brighton & Hove, UK. A tall, fastigiate, tree ideal for street planting. The tree has no resistance to Dutch elm disease. It is commonly known in the UK as the Guernsey Elm, Jersey Elm, Southampton Elm, and Wheatley Elm. Released to USNA from APHIS quarantine in December 2014 | 2115952 | NA 85690 |
| 3 | PI 675218 | R10-22-094 | Festuca valesiaca Schleich. ex Gaudin | Stavropol, Russian Federation | W6 | | | 2011 | COLLECTED | 07/24/2010 | | | | Temperate deciduous forest understory. Granitic parent material, NW facing slope to flat meadow, 0-45% slope: seed collected from >100 plants | Wild material | | 1883187 | PI 675218 |
| 4 | PI 675309 | R10-15-060 | Brachypodium sylvaticum (Huds.) P. Beauv. | Stavropol, Russian Federation | W6 | | | 2011 | COLLECTED | 07/20/2010 | NE facing slope at foot of Mashuk Mountain near Pyatigorsk | 44.06300000, 43.09500000 | 592 | Temperate deciduous forest understory. Limestone parent material, located in the forest and openings: seed collected from >100 plants | Wild material | | 1883155 | PI 675309 |
| 5 | PI 675313 | R10-22-087 | Brachypodium rupestre (Host) Roem. & Schult. | Stavropol, Russian Federation | W6 |  | | 2011 | COLLECTED | 07/24/2010 | | | | Temperate deciduous forest understory. Granitic parent material, NW facing slope to flat meadow, 0-45% slope: seed collected from >100 plants | Wild material | | 1883180 | PI 675313 |
| 6 | PI 675314 | R10-22-089 | Bromus erectus Huds. | Stavropol, Russian Federation | W6 | | | 2011 | COLLECTED | 07/24/2010 | | | | Temperate deciduous forest understory. Granitic parent material, NW facing slope to flat meadow, 0-45% slope: seed collected from >100 plants | Wild material | | 1883182 | PI 675314 |
| 7 | PI 675315 | R10-22-091 | Poa nemoralis L. | Stavropol, Russian Federation | W6 | | | 2011 | COLLECTED | 07/24/2010 | | | | Temperate deciduous forest understory. Granitic parent material, NW facing slope to flat meadow, 0-45% slope: seed collected from >100 plants | Wild material | | 1883184 | PI 675315 |
| 8 | PI 675316 | R10-22-095 | Dactylis glomerata L. | Stavropol, Russian Federation | W6 | | | 2011 | COLLECTED | 07/24/2010 | | | | Temperate deciduous forest understory. Granitic parent material, NW facing slope to flat meadow, 0-45% slope: seed collected from >100 plants | Wild material | | 1883188 | PI 675316 |
| 9 | PI 676173 | R10-53-224 | Festuca drymeja Mert. & W. D. J. Koch | Adygeja, Russian Federation | W6 | | | 2011 | COLLECTED | 08/03/2010 | West side of Belaya River, 10 km S of Khanyshki | 44.06400000, 41.55000000 | 633 | Forest opening and disturbed roadside. Shale substrate, high bench and slopes above Balia River: seed collected from >100 plants | Wild material | | 1883412 | PI 676173 |
| 10 | PI 676199 | R10-03-010 | Poa nemoralis L. | Stavropol, Russian Federation | W6 | | | 2011 | COLLECTED | 07/17/2010 | 10 km NW of Stavropol | 45.09100000, 41.89300000 | 571 | Forest understory. Rich organic O horizon: seed collected from >100 plants | Wild material | | 1883111 | PI 676199 |
| 11 | PI 676241 | R10-22-097 | Lolium perenne L. | Stavropol, Russian Federation | W6 |  | | 2011 | COLLECTED | 07/24/2010 | | | | Temperate deciduous forest understory. Granitic parent material, NW facing slope to flat meadow, 0-45% slope: seed collected from >100 plants | Wild material | | 1883190 | PI 676241 |
| 12 | PI 693827 | R10-15-058 | Dactylis glomerata L. subsp. lobata (Drejer) H. Lindb. | Stavropol, Russian Federation | W6 | | | 2011 | COLLECTED | 07/20/2010 | NE facing slope at foot of Mashuk Mountain near Pyatigorsk | 44.06300000, 43.09500000 | 592 | Temperate deciduous forest understory. Limestone parent material, small statured <0.4m in height, fine, light green, soft, lax, basal leaves (diploid?): seed collected from >100 plants | Wild material | | 1883153 | PI 693827 |
| 13 | PI 693829 | R10-22-093 | Poa pratensis L. subsp. angustifolia (L.) Arcang. | Stavropol, Russian Federation | W6 | | | 2011 | COLLECTED | 07/24/2010 | | | | Temperate deciduous forest understory. Granitic parent material, NW facing slope to flat meadow, 0-45% slope: seed collected from >100 plants | Wild material | | 1883186 | PI 693829 |
| 14 | PI 693844 | R10-37-153 | Poa pratensis L. subsp. angustifolia (L.) Arcang. | Karačaevo-Čerkesskaja Respublika, Russian Federation | W6 | | | 2011 | COLLECTED | 07/30/2010 | Jamagat Valley near Teberda | 43.45900000, 41.79600000 | 1573 | Mountain meadow and forest understory. Seed collected from >100 plants | Wild material | | 1883243 | PI 693844 |
| 15 | PI 693845 | R10-37-154 | Agrostis capillaris L. | Karačaevo-Čerkesskaja Respublika, Russian Federation | W6 | | | 2011 | COLLECTED | 07/30/2010 | Jamagat Valley near Teberda | 43.45900000, 41.79600000 | 1573 | Mountain meadow and forest understory. Seed collected from >100 plants | Wild material | | 1883244 | PI 693845 |
| 16 | PI 693846 | R10-37-155 | Poa trivialis L. subsp. sylvicola (Guss.) H. Lindb. | Karačaevo-Čerkesskaja Respublika, Russian Federation | W6 | | | 2011 | COLLECTED | 07/30/2010 | Jamagat Valley near Teberda | 43.45900000, 41.79600000 | 1573 | Mountain meadow and forest understory. Seed collected from >100 plants | Wild material | | 1883245 | PI 693846 |
| 17 | PI 699305 | R10-15-284 | Poa pratensis L. subsp. angustifolia (L.) Arcang. | Stavropol, Russian Federation | W6 | | | 2011 | COLLECTED | 07/20/2010 | NE facing slope at foot of Mashuk Mountain near Pyatigorsk | 44.06300000, 43.09500000 | 592 | Temperate deciduous forest understory. Limestone parent material, dark-green collection: seed collected from >100 plants | Wild material | | 1883362 | PI 699305 |
| 18 | NA 89115 | TLM25-04a | Hamamelis ovalis S. W. Leonard | Texas, United States | NA | | | 2025 | COLLECTED | 07/10/2025 | State Highway 87 approximately 3.25 kilometers north of the crossroad junction with Texas Recreational Road 255 (RE 255); plants were growing in the narrow buffer woods along the east side of the highway. | 31.12051300, -93.72628100 | 138 | The habitat is an upland mixed coniferous and deciduous woodlands in part to full shade and dry conditions, often under drought stress. Plants seem to always occur on the top of dry ridges or well-drained slopes. Slope: 0 to 1 percent. Aspect: N/A. Soils: The soils of this collection area are classified as Tehran-Letney Association, hilly (TLE) soils. The Tehran Series (55%) consists of deep, somewhat excessively drained, moderately rapidly permeable soils on uplands. They formed in thick loamy and sandy sediments on the Western Coastal Plain. These soils are on gently sloping to moderately steep uplands with slopes ranging from 1 to 20 percent. The Letney Series (30%) consists of deep, well drained, moderately rapidly permeable, upland soils. They formed in thick sandy and loamy sediments of the coastal plains. These soils are on gently sloping to moderately steep uplands with slopes ranging from 1 to 20 percent. Soil pH ranges from 4.5 to 6.0. The minor soil components include Doucette Series (10%) and Boykin Series (5%) soils. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). Geology: The underlying geology of this area is of Oligocene origin and characterized as Catahoula Formation. This formation is extensive and deep in Texas, up to 185 meters thick. In the area of the collection the Catahoula Formation is primarily mudstone and sand. The upper 90-150 meters is mudstone that is tuffaceous, and sandy; also, occasionally, with some bentonitic clay. (Source: USGS Texas Geologic Map Data). | Wild material | | 2191654 | NA 89115 |
| 19 | Ames 36260 | Thomson Causeway Recreation Area | Cornus drummondii C. A. Mey. | Illinois, United States | NC7 |  | | 2024 | COLLECTED | 08/19/2024 | Thomson Causeway Recreation Area, approximately 1 mile southwest of Thomson. Scattered along Potter Road starting just east of the causeway heading west, and along the gravel service road to the south. T23N R3E SE 1/4 Sec. 26. | 41.94919700, -90.11822100 | 179 | Floodplain of wetland complex along east bank of Mississippi River. Soils are moist and seasonally inundated with high organic matter content. | Wild material | Shrubs in nature measuring approximately 10 feet in height (to 15 feet) with varying degrees of red pigmentation on the pedicles. Peak fruit ripening occurred in late August 2024. Minor foliar disease noted at the time of collection. Growing as individual shrubs in shadier locations and forming thickets in sunnier sites. | 2168984 | Ames 36260 |
| 20 | 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 |
| 21 | 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 |
| 22 | 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 |
| 23 | 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 |
| 24 | 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 |
| 25 | 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 |
| 26 | NA 89039 | RJL2022IL-001 | Ptelea trifoliata L. | Illinois, United States | NA | | | 2022 | COLLECTED | 09/28/2022 | Site of plant habitat is located at 823 E Co Rd 1220, Hamilton, IL 62341 which is the property where Jacob's Geode Shop and Mine is located. This species is scattered and relatively common throughout the woodlands on this site. | 40.37848400, -91.35390200 | 175 | Plants growing in shade to part-shade of deciduous woodlands above a small creek.
Soils: The underlying geology of this area is of Mississippian origin and comprised of Warsaw Formation and Salem Limestone. Major lithological components include limestone that can be shaly, oolitic, bioclastic, or cherty. Minor lithological components include siltstone that can contain geodes or drusy quartz and can be calcareous.
Source: USGS Illinois Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=ILMws%3B0)
The surface soil profile of this area is Coffeen silt loam, 0 to 2 percent slopes, that are frequently flooded. The Coffeen series consists of very deep, somewhat poorly drained, moderately permeable soils on flood plains, low terraces or benches, toe slopes, and alluvial fans. They formed in silty alluvium. Much of the alluvium is of local origin derived from the nearby loess-covered uplands.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2139604 | NA 89039 |
| 27 | 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 |
| 28 | WLP 1118 | NA 84103 | Crataegus caucasica K. Koch | Georgia | NA | | | 2016 | COLLECTED | 10/02/2016 | West of the town of Tetritskaro. | 41.53806000, 44.42435000 | 1148 | Forest clearings and post-forest meadows. | | | 1952624 | WLP 1118 |
| 29 | Ames 32966 | JDC/VA/2015/052/709 | Viburnum opulus L. var. americanum Aiton | Iowa, United States | NC7 |  | | 2015 | COLLECTED | 09/15/2015 | Yellow River State Forest, T97N R4W northern edge of SW ¼ NW ¼ Sec. 36. | 43.17778200, -91.26642800 | 239 | North-facing algific talus slope (45-60 degrees) adjacent to Paint Creek. Moist deciduous woods. | Wild material | Formerly known as Viburnum trilobum, American highbush cranberry (V. opulus var. americanum) is a North American native shrub that is utilized as an important ornamental and conservation plant that is also harvested as a minor fruit crop (jams/jellies). In nature, this variety is generally found in moist habitats typically along stream banks and swamps where ample moisture is readily available. The native range of V. opulus var. americana is concentrated in the northeastern United States and into Canada (Little, E. L. Jr. 1977). Attractive ornamental characteristics includes showy lacecap flowers in spring and bright red fruits and foliage in the fall. Fruits are tart with a hint of sweetness. The European highbush cranberry (V. opulus var. opulus) is nearly identical to American highbush cranberry other than small glands (<1 mm) on the petiole making the exact determination very challenging resulting in common misidentifications. A major difference between the American and European highbush cranberries is that the European variety produces unpalatable fruit. Recent research has shown that American and European highbush cranberries are genetically distinct and that plants of hybrid origin are uncommon (Tork et al. 2025). Vigorous early spring growth and good tolerance to late spring frosts. Genetic analysis from Tork et al. 2025 confirmed that genetics of this accession represents American highbush Cranberry (Viburnum opulus var. americanum). This accession represents genetics from northeast Iowa and thus the extreme western edge of the species native range. | 1927436 | Ames 32966 |
| 30 | 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 |
| 31 | W6 41658 | R10-22-092 | Trifolium alpestre L. | Stavropol, Russian Federation | W6 | | | 2011 | COLLECTED | 07/24/2010 | | | | Temperate deciduous forest understory. Granitic parent material, NW facing slope to flat meadow, 0-45% slope: seed collected from >100 plants | Wild material | | 1883185 | W6 41658 |