| 0 | PI 418774 | 37 | Fraxinus angustifolia Vahl subsp. oxycarpa (M. Bieb. ex Willd.) Franco & Rocha Afonso | Afghanistan | NC7 |  | | 1977 | COLLECTED | | Somakond. | | | | Uncertain improvement status | | 1316202 | PI 418774 |
| 1 | PI 377819 | | Fraxinus angustifolia Vahl subsp. oxycarpa (M. Bieb. ex Willd.) Franco & Rocha Afonso | Bosnia and Herzegovina | NC7 | | | 1973 | COLLECTED | | Kravica village near Capljina, Bosnia and Herzegovina. | | | | Uncertain improvement status | | 1283031 | PI 377819 |
| 2 | NA 89037 | RJL2022KS-004 | Fraxinus pennsylvanica Marshall | Kansas, United States | NA | ![Image]( "Click for 1 image(s) for this accession.") | | 2022 | COLLECTED | 09/21/2022 | Coronado Heights Park, Smoky View, Kansas hillsides surrounding the historic WPA circa 1932 Coronado Heights Castle located about 91 meters above the surrounding land. This plant is scattered and infrequent on the slopes of this site. | 38.61065700, -97.70408300 | 448 | Plants growing in full sun, under extreme exposure, rocky, dry and thin soils of this short grass prairie habitat on the slopes surrounding the summit of Coronado Heights Park. Plants tend
Soils: The underlying geology of this area is of Upper Cretaceous origin and comprised of Kiowa Shale or FM- light -gray to black illitic shale with thin coquinoidal limestone beds at the base; sandstone lenses are common. Cheyenne Sandstone-massive to cross-bedded, light-gray to buff fine-grained sandstone with lenses to be found in runoff zones where moisture is temporarily more abundant.of gray sandy shale and conglomerate.
Source: USGS Kansas Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=KSKkc%3B0)
The surface soil profile of this area is Lancaster-Hedville complex, 3 to 20 percent slopes. The Lancaster series consists of moderately deep, well drained soils that formed in residuum from sandstone and sandy shales; it can be up to 200 cm deep. Slopes range from 1-20%. Hedville soils have bedrock within 50 centimeters of the surface and occur on similar hillslope positions.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2139602 | NA 89037 |
| 3 | PI 693187 | R10-55-226 | Poa pratensis L. subsp. angustifolia (L.) Arcang. | Adygeja, Russian Federation | W6 | | | 2011 | COLLECTED | 08/03/2010 | Belaya River Bridge, 2 km SW of Dakhovskya | 44.36200000, 40.19400000 | 360 | Mesic steppe bench above river. Mollisol, disturbed site: seed collected from >100 plants | Wild material | | 1883311 | PI 693187 |
| 4 | PI 693819 | R10-01-003 | Poa pratensis L. subsp. angustifolia (L.) Arcang. | Stavropol, Russian Federation | W6 | | | 2011 | COLLECTED | 07/17/2010 | 12 NW of Stavropol | 45.12900000, 41.85200000 | 436 | Stony steppe surrounded by forest (Quercus robur, Q. calcarea, Fraxinus exelsior): margin of gravel pit area: scraped shallow soils. Shallow sandy black A horizon, very stony, weathered limestone parent material and outcroppings: seed collected from >100 plants | Wild material | | 1883105 | PI 693819 |
| 5 | 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 |
| 6 | 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 |
| 7 | PI 638000 | ARM-02-067 | Pyrus salicifolia Pall. | Armenia | COR |  | | 2002 | COLLECTED | 09/03/2002 | Arpa Gorge in Vayotz Dzor Marz (province). | 39.71861000, 45.58194000 | 1398 | angustifolia, Fraxinus excelsior and Salix sp. angustifolia, Fraxinus excelsior and Salix sp. | Wild material | | 1642263 | PI 638000 |
| 8 | W6 61945 | OR090B-334 | Potentilla gracilis Douglas ex Hook. | Oregon, United States | W6 |  | | 2024 | | | | | | | Wild material | NA | 2168350 | W6 61945 |
| 9 | W6 61287 | OR090B-322 | Danthonia californica Bol. | Oregon, United States | W6 |  | | 2023 | | | | | | | Wild material | Plants 30-130 cm tall; cespitose, with short rhizomes. Leaf blades spread stiffly sideways or down. Inflorescences with sparse appearance: few large spikelets held out at stiff angles by panicle branches, branches strongly divergent to reflexed at maturity, and pedicels equal to or longer than the spikelets. Spikelets with 3-6 florets. Glumes with 4-7 veins. | 2142731 | W6 61287 |
| 10 | WLP 2670 | RJL2022PA-016 | Acer negundo L. | Pennsylvania, United States | NA | | | 2022 | COLLECTED | 10/21/2022 | Plants growing in woodlands above a small unnamed creek that dumps into the Middle Branch White Clay Creek in Goddard Park, West Grove Pennsylvania, off of Wickerton Road, Chester County. Plants are found regularly but scattered in the understory of the woodlands. | 39.80426000, -75.82609300 | 105 | Plants growing in a mesic, well-drained habitat of deciduous woodlands along streams and above the riparian zone that drains toward a small unnamed creek that feeds into the Middle Branch White Clay Creek. Plants generally grow in part shade to full sun, but perform best and fruit more heavily in full sun where there is abundant access to moisture. The remnant woodlands exist mostly along the steep slopes, wetlands and seeps of seasonal and year-round creeks flowing into the Middle Branch White Clay Creek. The woodlands are bordered by numerous housing developments and land converted to meadows; hence there is significant first order edge that is heavily impacted by invasive plant intrusion. Despite this fact, Acer negundo is highly competitive and competes well.
Soils: The underlying geology of this area is the Glenarm Wissahickon Formation of lower Paleozoic origin and lithologically similar to oligoclase-mica schist of the Wissahickon Formation (PZw), but also includes lenticular amphibolite bodies having ocean-floor basalt chemistry.
Source: USGS Pennsylvania Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=PAPZgw%3B0)
The primary soil type in the area of this collection is classified as Glenelg silt loam, 3 to 8 percent slopes. This series consists of very deep, well drained soils formed in residuum weathered from micaceous schist on uplands of the Blue Ridge and the Northern Piedmont. Saturated hydraulic conductivity is moderately high in the subsoil and moderately high to high in the substratum. This upper horizon of this soil is undifferentiated, mostly poorly drained sandy bottomland soils intermingled with decomposing organic litter and eroded silts and clays due to erosion.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2139661 | WLP 2670 |
| 11 | NA 89036 | RJL2022KS-003 | Cornus drummondii C. A. Mey. | Kansas, United States | NA | | | 2022 | COLLECTED | 09/21/2022 | Coronado Heights Park, Smoky View, Kansas hillsides surrounding the historic WPA circa 1932 Coronado Heights Castle located about 91 meters above the surrounding land. This plant is common and abundant on the slopes of this site. | 38.61348400, -97.70343100 | 475 | Plants growing in part shade to full sun, under extreme exposure, rocky, dry and thin soils of this short grass prairie habitat on the slopes surrounding the summit of Coronado Heights Park. The underlying geology of this area is of Upper Cretaceous origin and comprised of Kiowa Shale or FM- light -gray to black illitic shale with thin coquinoidal limestone beds at the base; sandstone lenses are common. Cheyenne Sandstone-massive to cross-bedded, light-gray to buff fine-grained sandstone with lenses of gray sandy shale and conglomerate.
Source: USGS Kansas Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=KSKkc%3B0)
The surface soil profile of this area is Lancaster-Hedville complex, 3 to 20 percent slopes. The Lancaster series consists of moderately deep, well drained soils that formed in residuum from sandstone and sandy shales; it can be up to 200 cm deep. Slopes range from 1-20%. Hedville soils have bedrock within 50 centimeters of the surface and occur on similar hillslope positions.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)
Slope: 5-20% Aspect: all | Wild material | | 2139601 | NA 89036 |
| 12 | NA 89035 | RJL2022KS-002 | Rosa arkansana Porter | Kansas, United States | NA | | | 2022 | COLLECTED | 09/20/2022 | Coronado Heights Park, Smoky View, Kansas hillsides surrounding the historic WPA circa 1932 Coronado Heights Castle located about 91 meters above the surrounding land. This plant is quite abundant on the slopes of this site and highly competitive. | 38.61158800, -97.70427000 | 475 | Plants growing in part-sun to full sun, under extreme exposure, rocky, dry and thin soils of this short grass prairie habitat on the slopes surrounding the summit of Coronado Heights Park.
The underlying geology of this area is of Upper Cretaceous origin and comprised of Kiowa Shale or FM- light -gray to black illitic shale with thin coquinoidal limestone beds at the base; sandstone lenses are common. Cheyenne Sandstone-massive to cross-bedded, light-gray to buff fine-grained sandstone with lenses of gray sandy shale and conglomerate.
Source: USGS Kansas Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=KSKkc%3B0)
The surface soil profile of this area is Lancaster-Hedville complex, 3 to 20 percent slopes. The Lancaster series consists of moderately deep, well drained soils that formed in residuum from sandstone and sandy shales; it can be up to 200 cm deep. Slopes range from 1-20%. Hedville soils have bedrock within 50 centimeters of the surface and occur on similar hillslope positions.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2139600 | NA 89035 |
| 13 | NA 86885 | RJL2021PA-004 | Ilex verticillata (L.) A. Gray | Pennsylvania, United States | NA | | | 2021 | COLLECTED | 11/16/2021 | Plants growing in woodlands along a small unnamed creek corridor dumping into the Middle Branch White Clay Creek in Goddard Park, West Grove Pennsylvania, off of Wickerton Road, Chester County. | 39.81063861, -75.82750806 | 124 | Plants are growing in a range of habitats from mesic woodlands to saturated streamside settings of deciduous woodlands that drain toward the Middle Branch White Clay Creek. Plants grow in high understory shade with dappled to indirect sunlight. The only female (fruiting) plants were found in areas along the creek where soils are moist to saturated. Numerous male specimens were found in the areas described above. Soils: Soils found in the areas where this collection was made are comprised primarily of Baile silt loam (Ba), Hatboro silt loam (Ha), and Glenelg silt loam, 8 to 15 percent slopes (GgC). Baile silt loam consists of very deep, poorly drained, moderately low to moderately high saturated hydraulic conductivity, soils on upland depressions and footslopes that were formed in local alluvium over residuum from acid crystalline rocks, chiefly mica schist and granitized schist and gneiss; slope ranges from 0 to 8 percent. Hatboro silt loam consists of very deep and poorly drained soils formed in deposited alluvium derived from metamorphic and crystalline rock. They are on flood plains. Slopes range from 0 to 3 percent. Glenelg silt loam, 8 to 15 percent slopes consists of very deep, well drained soils formed in residuum weathered from micaceous schist on uplands of the Blue Ridge and the Northern Piedmont. This soil is undifferentiated, mostly poorly drained sandy bottomland soils intermingled with decomposing organic litter and eroded silts and clays due to erosion. Slope: 0 to 15% Aspect: Variable. | Wild material | | 2123125 | NA 86885 |
| 14 | WLP 1731 | RJL2021PA-001 | Viburnum acerifolium L. | Pennsylvania, United States | NA | | | 2021 | COLLECTED | 11/05/2021 | Plants growing in woodlands above a small unnamed creek that dumps into the Middle Branch White Clay Creek in Goddard Park, West Grove Pennsylvania, off of Wickerton Road, Chester County. | 39.80462083, -75.82888750 | 103 | Plants growing in a mesic, well-drained habitat of deciduous woodlands, for the most part, above the riparian zone that drains toward a small unnamed creek that feeds into the Middle Branch White Clay Creek. Plants are growing in high understory shade with very little direct sun during most of the day. The remnant woodlands exist mostly along the steep slopes, wetlands and seeps of seasonal and year-round creeks flowing into the Middle Branch White Clay Creek. The woodlands are bordered by numerous housing developments and land converted to meadows; hence there is significant first order edge that is heavily impacted by invasive plant intrusion. Soils: Soils are classified as Glenelg silt loam, 8 to 15% slopes (GgC); this series consists of very deep, well drained soils formed in residuum weathered from micaceous schist on uplands of the Blue Ridge and the Northern Piedmont. Saturated hydraulic conductivity is moderately high in the subsoil and moderately high to high in the substratum. This upper horizon of this soil is undifferentiated, mostly poorly drained sandy bottomland soils intermingled with decomposing organic litter and eroded silts and clays due to erosion. Slope: 8 to 15% Aspect: West. | Wild material | | 2123080 | WLP 1731 |
| 15 | WLP 1732 | RJL2021PA-002 | Viburnum prunifolium L. | Pennsylvania, United States | NA | | | 2021 | COLLECTED | 11/05/2021 | Plants growing in woodlands along a small unnamed creek corridor dumping into the Middle Branch White Clay Creek in Goddard Park, West Grove Pennsylvania, off of Wickerton Road, Chester County. | 39.80462083, -75.82888750 | 102 | Plants are growing in a range of habitats from drier upland woods to moist creekside settings of deciduous woodlands that drain toward the Middle Branch White Clay Creek. Plants grow in part shade to high understory shade with dappled to indirect direct sunlight. Plants achieve their largest size and fruiting potential in part sun of the riparian zone of the creek where woodland canopy is thinner. Soils: Soils found in the areas where this collection was made are comprised primarily of flood plain Hatboro silt loam (Ha) and well-drained, upland Glenelg silt loam, 8 to 15 percent slopes (GgC). Hatboro silt loam consists of very deep and poorly drained soils formed in deposited alluvium derived from metamorphic and crystalline rock. They are on flood plains. Slopes range from 0 to 3 percent. Glenelg silt loam, 8 to 15 percent slopes consists of very deep, well drained soils formed in residuum weathered from micaceous schist on uplands of the Blue Ridge and the Northern Piedmont. This soil is undifferentiated, mostly poorly drained sandy bottomland soils intermingled with decomposing organic litter and eroded silts and clays due to erosion. Slope: 0 to 15% Aspect: Variable. | Wild material | | 2123098 | WLP 1732 |
| 16 | WLP 1733 | RJL2021PA-003 | Viburnum dentatum L. | Pennsylvania, United States | NA | | | 2021 | COLLECTED | 11/05/2021 | Plants growing in woodlands along a small unnamed creek corridor dumping into the Middle Branch White Clay Creek in Goddard Park, West Grove Pennsylvania, off of Wickerton Road, Chester County. | 39.80522167, -75.82928139 | 107 | Plants are growing in a range of habitats from mesic woodland to moist creekside settings of deciduous woodlands that drain toward the Middle Branch White Clay Creek. Plants grow in high understory shade with dappled to indirect sunlight. Soils: Soils found in the areas where this collection was made are comprised primarily of flood plain Hatboro silt loam (Ha) and well-drained, upland Glenelg silt loam, 8 to 15 percent slopes (GgC). Hatboro silt loam consists of very deep and poorly drained soils formed in deposited alluvium derived from metamorphic and crystalline rock. They are on flood plains. Slopes range from 0 to 3 percent. Glenelg silt loam, 8 to 15 percent slopes consists of very deep, well drained soils formed in residuum weathered from micaceous schist on uplands of the Blue Ridge and the Northern Piedmont. This soil is undifferentiated, mostly poorly drained sandy bottomland soils intermingled with decomposing organic litter and eroded silts and clays due to erosion. Slope: 0 to 15% Aspect: Variable. | Wild material | | 2123124 | WLP 1733 |
| 17 | WLP 1747 | RJL2021PA-005 | Rosa palustris Marshall | Pennsylvania, United States | NA | | | 2021 | COLLECTED | 11/20/2021 | Plants growing in wetland seeps surrounded by mown hayfields just west of the Middle Branch White Clay Creek in Goddard Park, West Grove Pennsylvania, off of Wickerton Road, Chester County. | 39.80090528, -75.82383250 | 100 | Habitat Notes: Plants are growing in permanently saturated to moist soils in wetland habitats. Plants appear to be obligate wetland plants and are found only in permanent to nearly permanent wet habitats observed. Generally, the shrubs are found in part shade to full sun. Soils: Soils found in the areas where this collection was made are comprised primarily of Hatboro silt loam (Ha). Hatboro silt loam consists of very deep and poorly drained soils formed in deposited alluvium derived from metamorphic and crystalline rock. They are on flood plains. Slopes range from 0 to 3 percent. Slope: 0 to 3% Aspect: Variable. | Wild material | | 2123715 | WLP 1747 |
| 18 | Ames 34007 | JDC/PP/2017/052/806 | Pinus ponderosa P. Lawson & C. Lawson | Nebraska, United States | NC7 |  | | 2017 | COLLECTED | 08/29/2017 | Areas on both north and south sides of the Niobrara River between Long Pine and Springview, T32N R21W; T32N R20W; and T31N R21W in Brown and Keya Paha Counties. | 42.75716800, -99.74657300 | 685 | Dry, rocky ridgetops. | Wild material | Genetics represent the extreme eastern edgeo of the species native range. | 1953921 | Ames 34007 |