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ACCESSIONPLANT NAMETAXONOMYORIGINGENEBANKIMAGEAVAILABILITYRECEIVEDSOURCE TYPESOURCE DATECOLLECTION SITECOORDINATESELEVATIONHABITATIMPROVEMENT LEVELNARRATIVE
0PI 691725BJP/CC/2014/003Cornus canadensis L. Maine, United StatesNA2014COLLECTED08/13/2014Edge of woods along west edge of Timber Cove Road, just northwest of intersection with Hwy. 189 and across the road from a cemetery. Approximately 13 km southwest of Lubec.44.80125000, -67.12708000Edge of woods along west edge of road.Wild material1923675PI 691725
1PI 691722BJP/CC/2014/001Cornus canadensis L. Maine, United StatesNA2014COLLECTED08/08/2014End of Lower Lyndon Street (public boat landing), immediately south of Caribou.46.84433000, -68.00089000Woods on the west side of the Aroostook River, immediately adjacent to the boat landing.Wild material1922793PI 691722
2PI 691726BJP/CC/2014/002Cornus canadensis L. Maine, United StatesNA2014COLLECTED08/11/2014Orono: University of Maine campus: along walking trail across a power line right-of-way.44.90100000, -68.65689000Rocky soils on both sides of a walking trail across a sunny power line right-of-way on campus.Wild material1922796PI 691726
3PI 691730WLP 1062Cornus florida L. United StatesNA2011COLLECTED09/15/2011Michigan: Van Buren County: Porter Township, Gravel Lake42.07840000, -85.85905000275Wild material1899522PI 691730
4PI 662012Ames 27964Cornus alternifolia L. f. Manitoba, CanadaNC72005COLLECTED08/2004Near the south end of Lake Manitoba, Portage la Prairie.50.19138889, -98.30333333245Wild material1700784PI 662012
5PI 662013Ames 27965Cornus alternifolia L. f. Minnesota, United StatesNC72005COLLECTED07/2004Stearns County.Wild material1700785PI 662013
6PI 649655002Cornus alternifolia L. f. Iowa, United StatesNC7SEED2005COLLECTED07/17/2005Adjacent to the Boone River on the south side, Tunnel Mill Wildlife Management Area, Hamilton County42.34972222, -93.85777778295Partial shade. 40% slope with a northern aspectWild material4 plants with approximately 3-5 inch caliper and approximately 15-20 feet in height. Foliage quality very clean with little to no leaf spots. Likely has some Septoria resistance.1685174PI 649655
7PI 656805001Cornus alternifolia L. f. Iowa, United StatesNC7SEED2005COLLECTED07/14/2005Ledges State Park, Boone County.41.99666667, -93.88166667328Mostly shaded, exposed over rock cliffs, next to small creek. 55% slope with a northern aspect. Well drained soil, predominately rock substrate. Wild materialPlants 6-10 feet in height, clean foliage, some canker.1685173PI 656805
8PI 66201103-01Cornus alternifolia L. f. Minnesota, United StatesNC7SEED2004COLLECTED2003Along a trail that was formerly a railroad track, southwest of Maple Plain, Hennepin County.44.98388889, -93.70250000295Wild material1655097PI 662011
9PI 66201724Cornus drummondii C. A. Mey. Iowa, United StatesNC72003COLLECTED09/22/2003Eldon Wildlife Management Area, Floris, SW 1/4 of NW 1/4 of Section 9, T70N, R12W, Agency Quad, Davis County.40.88083333, -92.25222222235Near a pond. Sunny. Slight slope. Clay loam soil. Wild materialMedium sized, suckering shrubs. Good leaf quality and fruit production. 1649669PI 662017
10PI 662010JDC/CA/2008/013/083Cornus alternifolia L. f. Iowa, United StatesNC7SEED2003COLLECTED09/15/2003West side of Fortune Road, just north of 38558 Fortune, near entrance to Bixby State Park, north of Edgewood, SW corner of SE 1/4 of NW 1/4 of Section 26, T91N, R5W, Edgewood Quad, Clayton County.42.66694444, -91.40333333329Woodland. Steep bank along creek. 100% filtered shade. Soil consisted of organic matter and rock fill with many stones, well drained. Wild materialSmall tree. Very late fruiting. 1649455PI 662010
11PI 662019Ames 27282Cornus racemosa Lam. Iowa, United StatesNC72003COLLECTED09/07/2003Along Wapsi Great Western Trail, Lake Hendricks County Park, NE corner of SW 1/4 of SW 1/4 of Section 19, T99N, R14W, Riceville Quad, Howard County.43.37694444, -92.55111111378Wild materialShrubs mostly 1.7 to 2 meters tall. Good leaf quality, some plants with striking red pedicels, heavy fruit production.1648678PI 662019
12PI 662016Ames 27280Cornus drummondii C. A. Mey. Iowa, United StatesNC72003COLLECTED09/02/2003South side of Skunk River, Oakland Mills County Park, SW 1/4 of SE 1/4 of Section 24, T71N, R7W, Mount Pleasant Quad, Henry County.40.93222222, -91.61055556184Limestone ridge along ravine. Wild materialLarge shrubs to small trees to 3.5 meters tall.1648648PI 662016
13PI 66201802-001Cornus racemosa Lam. Minnesota, United StatesNC72003COLLECTED2002North of collector's house, Hennepin County.44.95483330, -93.70646660Road bank.Wild material1644314PI 662018
14PI 649657WSYUS 16Cornus sanguinea L. Kiev, UkraineNC7PLANT1999COLLECTED09/09/1999Near the lake and across the street from the Dendrology Building, National Agricultural University campus, Kyiv.50.38305556, 30.50388889140Edge of road on a bank. Partial shade, 5-10% slope with a southwestern exposure. Sandy loam soil with good drainage. Wild materialLarge arching shrub to 16 feet.1586017PI 649657
15PI 649658WSYUS 47Cornus sanguinea L. Kharkiv, UkraineNC71999COLLECTED09/14/1999Krupchany.50.07222222, 35.81416667200Edge of forest/road. Typical edge of woods habit with foliage on open side. Partial shade, 0-1% slope with a western exposure. Clay loam soil with good drainage. Wild materialLarge shrub to 12 feet.1586018PI 649658
16PI 662015Ames 21660Cornus drummondii C. A. Mey. Oklahoma, United StatesNC71993COLLECTEDWichita Mountains, Kiowa County.Wild material1086897PI 662015
17PI 662014No. 23Cornus amomum Mill. subsp. obliqua (Raf.) J. S. Wilson Illinois, United StatesNC71993COLLECTEDWill County.Wild material1086114PI 662014
18PI 618691890414Cornus drummondii C. A. Mey. Ontario, CanadaNC71990COLLECTEDPRE 1990Pelee Island, Mosquito Bay, Essex County.41.73333333, -82.68333333175Shrub thicket.Wild material1064759PI 618691
19PI 631248890438Cornus drummondii C. A. Mey. Ontario, CanadaNC71990COLLECTEDSouth of Eagle (village), Aldborough Township, Elgin County.42.55000000, -81.56666667205Wild material1064756PI 631248
20PI 656804Ames 13718Cornus alba L. Russian FederationNC7BARK1990DONATED05/14/1990Uncertain improvement status1064554PI 656804
21PI 516476'Redstone'Cornus mas L. New York, United StatesNC71988COLLECTED1934Bureau of Parks, RochesterCultivarSmall tree to rounded bush reaching up to 8 meters in height, hardy to zone 5a. Flowers yellow (Feb.-Mar.), showy. Fruit abundant, scarlet, ripens August -Sept. Excellent survival rate, high vigor and growth habit. Potential conservation use in windbreaks, wildlife plantings, and landscaping. Selected for release by the USDA-NRCS, Plant Materials Center, Elsberry, MO. Selected on the basis of superior seedling vigor, dense growth form and glossy foliage. Demonstrated excellent survival and longevity with no apparent disease or insect problems after 44 years of evaluation. Cornelian cherry dogwood is a woody species native to central and southern Europe and western Asia. 1411412PI 516476
22PI 633649KSW 3653Cornus walteri Wangerin Jeollabuk-do, Korea, SouthNC71985COLLECTED10/03/1985Southeast side of village, Unho-ri, Chinso Myon, Puan Gun, Chollo Pukto (35 35 30 N, 126 34 E - original data)35.59166700, 126.5666670040Several trees in grove at edge of woods above rice field, rich moist soil, northeast-facing slopeWild materialSingle-trunked decid. tree ca 12 m tall, dbh 15 cm; lvs. dull medium green above, lighter beneath: infruct. rachis pink to rosy pink, frt. dull green, turning blue and falling, round, 5 mm diam.1064480PI 633649
23PI 649656NA 55219Cornus officinalis Siebold & Zucc. Seoul-teukbyeolsi, Korea, SouthNC71985COLLECTED10/24/1984Namdaemun Market, Seoul.Cultivated materialFruit yellow, turning red, 1.3 cm long, 7 mm diameter, juicy.1064475PI 649656
24PI 4956034Cornus drummondii C. A. Mey. Iowa, United StatesNC71984COLLECTED09/21/1984Pierce Creek County Recreation Area, Section 29, T70N, R39W, Page County.40.83709800, -95.35997900312Field near lakeshore. Growing in association with Solidago and Aster.Wild materialPlant to 3 meters. Perennial woody.1390539PI 495603
25PI 4956048Cornus drummondii C. A. Mey. Iowa, United StatesNC7FRUIT1984COLLECTED09/21/1984Along south end of parking area, Lake of Three Fires State Park, extreme NW corner of Section 7, T68N, R33W, Bedford Quad, Taylor County.40.71194444, -94.68583333360Wild materialPerennial woody. Plants in wide thicket to 2 meters tall, heavy fruiting. Very clean foliage with nice white fruits.1390540PI 495604
26PI 618692Ames 2812Cornus sericea L. subsp. sericea Manitoba, CanadaNC71984COLLECTEDHecla Islands.Cultivated materialShrub, fruit light blue.1022015PI 618692
27PI 468117'Indigo'Cornus amomum Mill. Michigan, United StatesNC71982COLLECTED1961Rose Lake Wildlife Experiment Station.42.79700600, -84.41192600254Wild material‘Indigo’ is a spreading shrub that can grow up to 10 feet tall. The stems are red when young but turn reddish brown and gray as they mature. ‘Indigo’ has yellowish white flowers that bloom in mid June. It produces an abundant crop of fruit, which ripens in September. The fruit is pale to dark blue and about ¼ inch in diameter. Multiple use conservation shrub for windbreaks and wildlife food and cover. 'Indigo' has been evaluated in 20 states, particularly in the Great Lake States, where it has performed well in moist soils. It is moderately shade tolerant but is not drought tolerant. Released in 1982 by the USDA-Natural Resource Conservation Service, Rose Lake Plant Materials Center and the Michigan Department of Natural Resources. 1363053PI 468117
28PI 443229'Ruby'Cornus sericea L. subsp. sericea New York, United StatesNC7STEM1980COLLECTED1975Near Painted Post.42.17257900, -77.13233500379Wild materialReleased in 1988 by the USDA-ARS Natural Resources Conservation Service, Big Flats Plant Materials Center, Corning, NY in cooperation with the New York State Department of Environmental Conservation. Evaluated at the Big Flats PMC alongside 42 other accessions from the northeastern United States. 'Ruby' was selected for its outstanding layering ability, geen stems in summer followed by bright red stems in fall/winter, white flowers and cream colored fruits and its uniform, rounded growth habit. Shrub to 6-10 feet with ascending outside stems. Useful for steambank protection due to the tendancy for side branches to root by layering. It preforms best on soils that are moist, somewhat poorly drained, moderately acidic to neutral, and in areas that have medium to coarse textured soils. It is tolerant to some shade but not to droughty conditions. Originally obtained in 1975 from a single, native plant growing near Painted Post, NY.1338165PI 443229
29PI 377803Cornus mas L. Krapinsko-zagorska županija, CroatiaNC71973COLLECTEDMt. Strahinjscica near Krapina, north Croatia.46.18132800, 15.88384400540Wild material1283018PI 377803
30PI 377804Cornus mas L. Ličko-senjska županija, CroatiaNC71973COLLECTEDNear Otocac, Svica-Krasno, Lika.44.87137900, 15.17703000490Wild material1283019PI 377804
31PI 3701582137Cornus mas L. Saraj, North MacedoniaNC71972COLLECTED07/01/1971Planina Zeden.42.03890000, 21.18860000650Wild material1277240PI 370158
32PI 3701592138Cornus mas L. Saraj, North MacedoniaNC71972COLLECTED07/01/1971Planina Zeden.42.03890000, 21.18860000650Wild material1277241PI 370159
33PI 3701602139Cornus mas L. Struga, North MacedoniaNC7FLOWER1972COLLECTED07/01/1971Modric.41.36690000, 20.57220000950Wild material1277242PI 370160
34PI 3701622141Cornus mas L. Ohrid, North MacedoniaNC71972COLLECTED07/01/1971Planina Galicica.40.94700000, 20.833300001250Wild material1277244PI 370162
35PI 323959B-140Cornus mas L. Stavropol'skij kraj, Russian FederationNC71967COLLECTED08/15/1967Pyatiborsk, Stavropol'skij kraj44.05871200, 43.02655500567Unknown, previous collection (PI323958. Col. No. B-121) was collected in a pasture. Possible this accession also represents a wild/naturalized source.Uncertain improvement statusAccession acquired in area where lowest winter temperature on average is -5 degrees C.1240618PI 323959
36PI 317223K-436Cornus kousa Bürger ex Hance Jeju-teukbyeoljachido, Korea, SouthNA1966COLLECTED1966Along trail up Hallasan [Mt. Halla].1000Wild material1708708PI 317223
37PI 293777ViridissimaCornus sanguinea L. Former, Soviet UnionNC71963COLLECTEDFrom swampy ares, Strashensky Forest, Kholorash Region Moldavia.300Wild materialSmall shrub in wild; stems reddish; fruit purple black.1222567PI 293777
38NA 891582025RJLSEUS-06Cornus florida L. Alabama, United StatesNA2025COLLECTED10/01/2025Coosa Wildlife Management Area: along the edge of gated dirt road on the west side of Coosa County Road 29, 0.3 kilometers north of Hatchet Creek.32.86402200, -86.33871400108Plants are growing in part sun to shade on dry-mesic slopes above the road cut on the gated dirt road; most likely a road for access for fire control/forest management. The forest is a combination of deciduous and evergreen with evergreens primarily comprised of Pinus taeda. The habitat was quite dry during this time of year. Slope: 5 to 20 percent. Aspect: North. Soils: The primary soil in the area of this collection is classified as Madison-Louisa Series complex, 15 to 30 percent slopes, moderately eroded (MdE2). The Madison Series soils are very deep, well drained soils with medium runoff found on Piedmont uplands in interstream divides, ridges and side slopes. They are comprised of residuum weathered from felsic or intermediate, high-grade metamorphic or igneous rocks high in content of mica. Slopes range from 2 to 60 percent and soil is typically strongly acidic. Louisa Series soils The Louisa Series soils consist of shallow, somewhat excessively drained soils which formed over mica gneiss and schist bedrock. They occur on Piedmont uplands. Slopes are 6 to 80 percent. This soil is moderately acid. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). Geology: The underlying geology of this area is of Precambrian to Paleozoic origin and characterized as Hatchet Creek Group; Pinchoulee Gneiss Formation. It is characterized by medium to fine-grained migmatitic, locally garnetiferous biotite-feldspar gneiss, commonly saturated with granitic pods. (Source: USGS Alabama Geologic Map Data).Wild material2193004NA 89158
39NA 885822024RJLFL-013Cornus florida L. Florida, United StatesNA2024COLLECTED11/13/2024Woodland edge along the south side of Bud Bass Road (DOF B48), 0.30 kilometers east of the junction with Norman Riley Road.30.75753300, -86.8045760039Mixed evergreen and deciduous forests in part shade in a mesic- to mesic-dry situation. Slope: 0 percent. Aspect: North. The underlying geology of this area is characterized as Citronelle Formation of the Pliocene period. The Citronelle Formation is widespread in the Gulf Coastal Plain. The type section for the Citronelle Formation, named by Matson (1916), is near Citronelle, Alabama. The Citronelle Formation grades laterally, through a broad facies transition, into the Miccosukee Formation of the eastern Florida panhandle. Coe (1979) investigated the Citronelle Formation in portions of the western Florida panhandle. The Citronelle Formation is a siliciclastic, deltaic deposit that is lithologically similar to, and time equivalent with, the Cypresshead Formation and, at least in part, the Long Key Formation (Cunningham et al., 1998) of the peninsula. In the western panhandle, some of the sediments mapped as Citronelle Formation may be reworked Citronelle. The lithologies are the same and there are few fossils present to document a possible younger age. The Citronelle Formation consists of gray to orange, often mottled, unconsolidated to poorly consolidated, very fine to very coarse, poorly sorted, clean to clayey sands. It contains significant amounts of clay, silt and gravel which may occur as beds and lenses and may vary considerably over short distances. Limonite nodules and limonite-cemented beds are common. Marine fossils are rare but fossil pollen, plant remains and occasional vertebrates are found. Much of the Citronelle Formation is highly permeable. It forms the Sand and Gravel Aquifer of the surficial aquifer system contain organics. The dominant fossils in the freshwater carbonates are mollusks. (Source: USGS Florida Geologic Map Data). The soils of this are characterized as Troup Series loamy sand, 0 to 5 percent slopes. The Troup series consists of very deep, somewhat excessively drained soils that formed in unconsolidated sandy and loamy marine sediments. Troup soils are on ridges and hillslopes. Slopes predominantly range from 0 to 15 percent but range to 45 percent. The soil pH is generally strongly acid. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions).Wild material2169919NA 88582
40NA 885842024RJLFL-016Cornus florida L. Florida, United StatesNA2024COLLECTED11/14/2024Both sides of Kennedy Bridge Road approximately 0.27 kilometers west of the junction with Hurricane Lake South Entrance Road.30.93159700, -86.7492800043Mesic to mesic-moist conditions in a mixed and deciduous evergreen forest in part shade. Slope: 5 to 10 percent. Aspect: Various. The underlying geology of this area is characterized as Citronelle Formation of the Pliocene period. The Citronelle Formation is widespread in the Gulf Coastal Plain. The type section for the Citronelle Formation, named by Matson (1916), is near Citronelle, Alabama. The Citronelle Formation grades laterally, through a broad facies transition, into the Miccosukee Formation of the eastern Florida panhandle. Coe (1979) investigated the Citronelle Formation in portions of the western Florida panhandle. The Citronelle Formation is a siliciclastic, deltaic deposit that is lithologically similar to, and time equivalent with, the Cypresshead Formation and, at least in part, the Long Key Formation (Cunningham et al., 1998) of the peninsula. In the western panhandle, some of the sediments mapped as Citronelle Formation may be reworked Citronelle. The lithologies are the same and there are few fossils present to document a possible younger age. The Citronelle Formation consists of gray to orange, often mottled, unconsolidated to poorly consolidated, very fine to very coarse, poorly sorted, clean to clayey sands. It contains significant amounts of clay, silt and gravel which may occur as beds and lenses and may vary considerably over short distances. Limonite nodules and limonite-cemented beds are common. Marine fossils are rare but fossil pollen, plant remains and occasional vertebrates are found. Much of the Citronelle Formation is highly permeable. It forms the Sand and Gravel Aquifer of the surficial aquifer system contain organics. The dominant fossils in the freshwater carbonates are mollusks. (Source: USGS Florida Geologic Map Data). The soils of this are characterized as Dothan Series loamy sand, 5 to 8 percent slopes. 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. Slopes range from 0 to 15 percent. 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. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions).Wild material2169921NA 88584
41Ames 36260Thomson Causeway Recreation AreaCornus drummondii C. A. Mey. Illinois, United StatesNC7HABITAT2024COLLECTED08/19/2024Thomson 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, -90.11822100179Floodplain of wetland complex along east bank of Mississippi River. Soils are moist and seasonally inundated with high organic matter content. Wild materialShrubs 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.2168984Ames 36260
42W6 62095CBG-10902Cornus amomum Mill. subsp. obliqua (Raf.) J. S. Wilson W6SEED20242168893W6 62095
43WLP 3137TJK2023AL-001Cornus alternifolia L. f. Alabama, United StatesNA2023COLLECTED08/15/2023Claiborne Bluffs, above the Alabama River.31.54883000, -87.5141700016Slope: 35%. Aspect: West-northwest. Elevation recorded as 52 feet.Wild materialWLPGR contract collection.2158469WLP 3137
44Ames 36172JDC/CR/2012/005/398Cornus rugosa Lam. Iowa, United StatesNC7FRUIT2023DEVELOPED08/23/2023Boone Forks Wildlife Area (Hamilton county), Dolliver Memorial State Park (Webster county), and Ledges State Park (Boone county).42.16369500, -93.96430100325Mesic deciduous woodsWild materialThis accession represents genetics originating from central Iowa developed through the combination of three separate, disjunct populations (Ames 31514; Ames 27276; and Ames 31515). Plants from each population were combined together in order to acheive a successful seed increase as the genetic diversity within each original accession was not sufficient (strong self-incompatibility). Round-leaf dogwood is typically noted as a woodland shrub that has a high tolerance to shading, but prefers well-drained yet moist soils. Round-leaf dogwood is native to most of the northeastern US west to the Minnesota/North Dakota border south to very rare, disjunct populations in central Iowa. Genetics of this accession would represent the extreme southwestern edge of the species native range. 2158817Ames 36172
45NA 87346TJK2022FL-001Cornus florida L. Florida, United StatesNA2023COLLECTED10/27/2022Okaloosa County: Duke Field AFS; Eglin Air Force Base, approximately 1.3 miles southeast of Military Rd 231, Juniper Creek Bayhead.30.62890000, -86.5000000042Rich evergreen and deciduous Bayhead Community. Extensive Quercus arkansana along the bluff top to mid-slope, with Magnolia ashei in steephead bottom to lower half of slope. Cornus at toe of slope on the first bench, off bottom.Wild material2141637NA 87346
46NA 87317NA 87317Cornus quinquenervis Franch. NA2022Wild materialFull name as recorded at U.S. National Arboretum: Cornus quinquenervis. Given to Dr. Richard Olsen by Dr. Donglin Zhang, University of Georgia, at the October 17-21 International Plant Propagators Society's Southern Region meeting in Athens, Georgia. See https://jcra.ncsu.edu/publications/travelogs/2017-china/index.php for more information about this expedition. Collected under permit number P37-17-01075. See also NA 885674 for earlier seedlings given by Scott McMahan, Atlanta Botanical Garden.2155316NA 87317
47NA 89036RJL2022KS-003Cornus drummondii C. A. Mey. Kansas, United StatesNA2022COLLECTED09/21/2022Coronado 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, -97.70343100475 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 material2139601NA 89036
48WLP 1140WLP 1140Cornus canadensis L. New Hampshire, United StatesNA2021Wild material2116602WLP 1140
49NA 88469F016Cornus florida L. Pennsylvania, United StatesNA2020COLLECTED09/24/2020J. Edward Mack Boy Scout Camp near Brickerville, PA.40.26000000, -76.31888000Near power lines.Wild material2109480NA 88469
50W6 57413NEWFS-373Cornus amomum Mill. Massachusetts, United StatesW6SEED2019Wild material2098210W6 57413
51WLP 1135F007Cornus florida L. Pennsylvania, United StatesNA2019COLLECTED09/12/2019Lebanon County; Newmanstown [to Brickerville?]; J Eward Mack Scout Reservation [and beyond]; collected across a five-mile radius [Locality given as J Edward Mack, Brickerville; coordinates provided are at J Edward Mack Scout Reservation in Newmanstown, with Brickerville some distance to the southeast. -SBL]40.25705000, -76.31936000Collected from several specimens in a five mile radius.2109114WLP 1135
52W6 55946NV030-1333Cornus sericea L. subsp. occidentalis (Torr. & A. Gray) Fosberg California, United StatesW6SEED2018Wild materialCornus sericea subsp. occidentalis1970657W6 55946
53W6 55392OR050-275Cornus sericea L. subsp. occidentalis (Torr. & A. Gray) Fosberg Oregon, United StatesW6SEED2018Wild materialCornus sericea ssp. occidentalis1967944W6 55392
54WLP 1125V18-03Cornus racemosa Lam. Vermont, United StatesNA2018COLLECTED10/02/2018Addison County; Middlebury; Otter View Park, in natural area near the parking lot.44.01924000, -73.18117000114Growing in a wet depression.2108865WLP 1125
55W6 54652NCBG-232Cornus amomum Mill. Virginia, United StatesW6SEED2018Wild materialCornus amomum1965878W6 54652
56W6 53278OR080-45Cornus sericea L. subsp. sericea Oregon, United StatesW6SEED2018Wild material1957628W6 53278
57Ames 34015Ames 34015Cornus rugosa Lam. Minnesota, United StatesNC72017COLLECTED08/23/2017Smoky Hills State Forest between Snellman and Osage, T139N R37W Sec. 2, 9, 11, and 14 and also T140N R37W Sec. 26 and 34.46.89278300, -95.35163300501Mixed pine and deciduous moist woods.Wild material1953929Ames 34015
58WLP 1116NA 83889Cornus florida L. Kentucky, United StatesNA2016COLLECTED09/27/2016Cumberland Falls State Park, Trail #6 (Cumberland Falls Trail).36.83700000, -84.340000003021951893WLP 1116
59WLP 1117NA 83967Cornus foemina Mill. Kentucky, United StatesNA2016COLLECTED09/30/2016[Locality data unparseable; GPS coordinates appear near a road of uncertain name off Howard Munsey Rd. north of Betsey, Kentucky. Original location was listed as: "At Edam Road?"; no road by this name was found in the county. -SBL]36.92000000, -84.73900000274Wet roadside couvee (ditch).1952406WLP 1117
60WLP 1119PCC16-GE112Cornus sanguinea L. subsp. australis (C. A. Mey.) Jáv. Kvemo Kartli, GeorgiaNA2016COLLECTED08/28/2016Trialeti [historical region], 100 m east of dead end of Samshvilde Complex Road, between Chivchara and Khrami Rivers. 1.3 air kilometers southeast of Samshvilde.41.50663000, 44.50285000796Open, mixed savanna. Flat ground.Common on trailside.2108740WLP 1119
61Ames 34698AK930-371Cornus sericea L. Alaska, United StatesNC7SEED2016COLLECTED08/15/2011Left bank Yukon River, between NPS/BLM headquarters and Eagle Bluff.64.79415000, -141.19875000259Regenerated scrubWild material1932565Ames 34698
62Ames 33039NA 82750Cornus alternifolia L. f. Alabama, United StatesNC7FRUIT2015COLLECTEDPRE 09/2014Butler County.31.75269200, -86.69006900Wild material1928686Ames 33039
63WLP 1105NA 82792Cornus florida L. Indiana, United StatesNA2015COLLECTED10/07/2015Grindstone Creek watershed, T22N R6W NW 1/4 SE 1/4 Sec. 20, just northeast of Attica, Fountain County.40.33643000, -87.11758400192Upland, gentle bluffs. Deciduous woods. Growing on west and southwest-facing slopes at approximately 0 to 45 degrees. Growing in association with Quercus alba, Quercus velutina, Quercus rubra, Acer saccharum, and Sassafras albidum.Wild materialBright red fruits approximately 10mm in length. One specimen close to 30' in height and 25' spread. Sampled three specimens all within a quarter mile.1927828WLP 1105
64NA 83149'Juanita'Cornus florida L. NA20151952074NA 83149
65NA 83150'Super'Cornus florida L. NA20151952075NA 83150
66Ames 34696MARSB-074Cornus amomum Mill. New Jersey, United StatesNC7SEED2015COLLECTED08/29/2013West Essex Park just southeast of Pine Brook.40.84291000, -74.3134100051Wild material1922850Ames 34696
67Ames 34697MARSB-080Cornus amomum Mill. Pennsylvania, United StatesNC7SEED2015COLLECTED09/11/2013Allegheny National Forest -Minister Creek watershed just south of Minister.41.61593000, -79.15109000369Wild material1922851Ames 34697
68Ames 32831RLD1401Cornus rugosa Lam. Minnesota, United StatesNC72014COLLECTED09/03/2014Becker County near Pine Island Lake.47.14710000, -95.43608330503Upland roadside near steep dropoff with lake below. Mixed deciduous and conifer forest. Growing in association with Fraxinus pennsylvanica, Quercus macrocarpa, Populus tremuloides, Betula papyrifera, Picea glauca, Pinus strobus, Sambucus sp., Acer spicatum, Rosa sp., Rubus sp., and Sanicula marilandica.Wild material1921824Ames 32831
69Ames 32829NA 82181Cornus amomum Mill. Maine, United StatesNC72014COLLECTED09/13/2014Along small gravel road heading north along Birch Stream from the Stillwater River boat landing on Southgate Road, Old Town, Penobscot County, Maine44.98842400, -68.6756140033Open, seasonally wet woods. Growing in association with Quercus rubra, Fraxinus pennsylvanica, Ilex verticillata, Viburnum nudum, Crataegus sp., Myrica gale, Rhodora canadense, Betula sp, and Acer saccharinum.Wild material1921789Ames 32829
70Ames 32830BJP/C.AM/2014/002Cornus amomum Mill. Maine, United StatesNC72014COLLECTED09/04/2014Field edge near Levant Elementary School, Levant, Penobscot County, Maine.44.86062400, -69.0006920071Wetland. Growing in association with Salix spp., Alnus incana, and Betula populifoliaWild material1921790Ames 32830
71WLP 1093JDC/CF/2014/097/599Cornus florida L. Alabama, United StatesNA2014COLLECTED09/23/2014Alabama: Winston County; William B. Bankhead National Forest along County Road 8.34.06143000, -87.31290200211 Growing in association with Quercus sp., Pinus sp., and Diospyros virginiana. Wild materialVariation in fruit size noticed across specimens sampled.1922368WLP 1093
72Ames 32755C-alt-01Cornus alternifolia L. f. Maine, United StatesNC72014COLLECTED08/08/2014East side of Bennoch Road, just north of where Pushaw Stream crosses Bennoch Road, approximately 3 miles northwest of Old Town, Penobscot County.44.96142300, -68.6954720041Roadside. Disturbed area on the upper portion of a west-facing slope. Specimens sampled were approximately 2.5-3.6 m tall and multi-stemmed. Most fruits on upper branches were dark blue, many fruits on lower branches were still white. Plants appeared to be in good health, without obvious insect or disease problems at the time of collection.Wild material1920148Ames 32755
73Ames 32756C-alt-02Cornus alternifolia L. f. Maine, United StatesNC72014COLLECTED08/08/2014End of Lower Lyndon Street (public boat landing), immediately south of Caribou, Aroostook County.46.84576900, -68.00155500121Specimens sampled in woods on flat terrain on the west side of the Aroostook River. Collection site is several (2-3) meters higher in elevation than the river below near a steep incline (45 degrees) at the edge of the river. Growing in association with Populus tremuloides, Pinus strobus, Acer negundo, Cornus sericea, Amelanchier sanguinea, Cornus canadensis, and Sorbus aucuparia.Wild material1920149Ames 32756
74NA 81638NA 81638Cornus wilsoniana Wangerin NA2013Cultivated material1940378NA 81638
75WLP 1079NA 81742Cornus florida L. Missouri, United StatesNA2013COLLECTED09/26/201338.41792000, -93.604330001922751WLP 1079
76NA 81762(golden selection)Cornus florida L. NA2013CloneReceived as grafted plants.1951169NA 81762
77Ames 31516JDC/CR/2012/014/407Cornus rugosa Lam. Iowa, United StatesNC7SEED2012COLLECTED07/13/2012Bluffton Fir State Preserve, SW 1/4 of Section 10, T99N, R9W, Bluffton Quad, near Bluffton, Winneshiek County.43.41080200, -91.93845200343Mixed hardwood forest. Very steep, northwest-facing slope. Wild material1903743Ames 31516
78Ames 31504Ames 31504Cornus alternifolia L. f. Ohio, United StatesNC7SEED2012COLLECTED07/13/2012Shawnee State Forest. Scioto County Ohio. Along Forest Road 1.38.69784000, -83.16209000235North-facing slope. Fairly localized population. Specimens ranging from 10-20 feet in height.Wild material1903497Ames 31504
79WLP 1075MSU Coll. No. 20120382Cornus florida L. Michigan, United StatesNA2012COLLECTED09/20/201242.38255000, -85.08531000Wild material1913908WLP 1075
80WLP 2199COFL2Cornus florida L. New York, United StatesNASEED2012COLLECTED09/23/2011375Wild material1900127WLP 2199
81Ames 31214Ames 31214Cornus rugosa Lam. Wisconsin, United StatesNC7SEED2011COLLECTED2011Along east side of County Road C, base of McCaslin Mountain, NW 1/4 of Section 26, T34N, R17E, Roaring Rapids Quad, Marinette County.45.39916660, -88.34111110371Hilly terrain. Sandy loam soil with a shallow humus layer, near surface of granite and scattered granite boulders. Soils must be near neutral due to abscence of Ericaceae plants. Wild material1894296Ames 31214
82Ames 31207ALB-2011-019Cornus mas L. Korçë, AlbaniaNC7SEED2011COLLECTED09/14/2011Northern side of Gjançi Reservoir between Gjanç and Ujëbardhë, Korçë approximately 1 km from ALB-2011-020 (Ames 31208).40.52677000, 20.658570001089Wild material1891851Ames 31207
83Ames 31208ALB-2011-020Cornus mas L. Korçë, AlbaniaNC7SEED2011COLLECTED09/14/2011Northern side of Gjançi Reservoir between Gjanç and Ujëbardhë, Korçë approximately 1 km from ALB-2011-019 (Ames 31207).40.52942000, 20.647100001079Wild material1891852Ames 31208
84Ames 31209ALB-2011-048Cornus mas L. Shkodër, AlbaniaNC7SEED2011COLLECTED09/17/2011Between Dedaj and Bzhete, Shkodër42.29936000, 19.54058000490Wild material1891860Ames 31209
85WLP 1054362Cornus florida L. New York, United StatesNAFRUIT2011COLLECTED09/11/2011Cameron-North Jasper Road, Steuben County.42.20100000, -77.43300000384Mixed, upland, hardwood forest. Associated with Carpinus caroliniana, Pinus strobus, Populus tremuloides, Prunus serotina, Rhus typhina, Quercus alba, Quercus velutina, Tilia americana, and Ulmus.Wild material1891448WLP 1054
86WLP 1055386Cornus florida L. Pennsylvania, United StatesNAFRUIT2011COLLECTED09/16/2011Along Highway 120, Cameron County.41.32400000, -78.12500000251Mixed hardwood forest. Steep (60 degree) west-facing slope. Associated with Carya, Cornus alternifolia, Fraxinus americana, Quercus alba, Quercus prinus, Quercus rubra, Rhododendron maximum, and Sassafras albidum.Wild material1891449WLP 1055
87WLP 1051AK-2011-007Cornus foemina Mill. Arkansas, United StatesNA2011COLLECTED09/19/201134.87842000, -90.56197000208Wild material1890984WLP 1051
88Ames 31028MPW/MSD 703Cornus alternifolia L. f. Pennsylvania, United StatesNC7FRUIT2011COLLECTED07/27/2011Along Martin Road, Warren County.41.98090000, -79.13630000385Rich woods. Wild material1886743Ames 31028
89Ames 31029MPW/MSD 710Cornus rugosa Lam. New York, United StatesNC7SEED2011COLLECTED07/29/2011Along Tannery Creek Road, Steuben County.42.04210000, -77.11640000378Rich woods, just above shale. Steep, north-facing slope. Wild material1886744Ames 31029
90NA 80068KNW 243Cornus kousa Bürger ex Hance Incheon-gwangyeoksi, Korea, SouthNA2011COLLECTED10/06/1984Ganghwa-gun, Hwado-myeon: Gangwhado (island): Sagi-ri village. [Originally listed as Kyong Gi Do, Kanghwa Gun, Hwado Myon, Sagiri village.]Occasional individuals in understory of mixed deciduous forest along a mountain stream.Wild material1896456NA 80068
91NA 80282RL 11004Cornus amomum Mill. North Carolina, United StatesNA2011COLLECTED08/14/2011Wild material1914115NA 80282
92WLP 1052NA 80304Cornus florida L. NA2011COLLECTEDPRE 07/01/2011New York, Tompkins County, Two collection sites: one at Newfield, NY and another 5.74 miles away in Spencer, NY (given as West Danby, NY) [see GPS coordinates in Collection Miscellaneous]Wild material1896483WLP 1052
93W6 40418UT931-417Cornus sericea L. Utah, United StatesW6SEED2011Wild material1861182W6 40418
94NA 80805RL 10032Cornus drummondii C. A. Mey. Texas, United StatesNA2010COLLECTED11/15/2010Texas: Hill County, North of Carl's Corner along frontage road of I-35, north side, in ravine crossing.Wild material1914181NA 80805
95WLP 1065RL 10008Cornus asperifolia Michx. Georgia, United StatesNA2010COLLECTED11/15/2010Georgia: Decatur County: Faceville, Faceville Landing on Lake Seminole, between picnic area and campground.Wild material1914307WLP 1065
96WLP 1066RL 10019Cornus asperifolia Michx. Florida, United StatesNA2010COLLECTED11/15/2010Florida: Liberty County, Torreya State Park, in ravines SW of Gregory House.Wild material1914170WLP 1066
97Ames 30873G10-121Cornus mas L. South Ossetia, GeorgiaNC7SEED2010COLLECTED09/2010Gldani Market, Tbilisi.41.79222222, 44.81583333470Market.Cultivated material1850241Ames 30873
98WLP 1043JDC/CF/2010/044/314Cornus florida L. Missouri, United StatesNASEED2010COLLECTED09/15/2010Odin Access Conservation Area, Wright County.37.26709000, -92.61271000388South-southeast facing slope (50%). Associated with Hydrangea arborescens, Morus rubra, Quercus, Staphylea trifolia, and Viburnum prunifolium.Wild materialVery large flowering dogwoods, approximately 5-6 inches d.b.h. and 25-30 feet tall.1848889WLP 1043
99WLP 1037KC10-003Cornus florida L. NA2010COLLECTEDPRE 09/15/2010Virginia, Appomattox County, route 460, 1 mile east of town center near rest stopoak woodlandWild material1896373WLP 1037
100Ames 30552Ames 30552Cornus alternifolia L. f. Missouri, United StatesNC7SEED2010COLLECTED06/29/2010Along North River, Callaghan Mound Access Conservation Area, near Heather, SW 1/4 of Section 15, T58N, R8W, Emden Quad.39.82140000, -91.78680000190Northeast facing slope.Wild material1843106Ames 30552
101Ames 30496Ames 30496Cornus amomum Mill. Pennsylvania, United StatesNC7SEED2010COLLECTEDBrandywine Creek, Chadds Ford.39.86666600, -75.5933330076Creek banks.Cultivated material1831698Ames 30496
102WLP 2140COUN-SOS-OR931-33-08Cornus unalaschkensis Ledeb. Oregon, United StatesNASEED2009COLLECTED2008Wild material1827769WLP 2140
103WLP 2132418320Cornus nuttallii Audubon Oregon, United StatesNASEED2009COLLECTED10/09/2007650Old growth conifer forest (white fir- Douglas Fir climax type). Associated with Acer circinatum, Corycus cornuta var. californica, Tsuga heterophylla.Wild material1826931WLP 2132
104Ames 30366JDC/CA/2009/090/240Cornus amomum Mill. subsp. obliqua (Raf.) J. S. Wilson Ohio, United StatesNC7SEED2009COLLECTED10/16/2009Along Dicks Creek, Wayne National Forest, just southeast of Kitchen, NW 1/4 of NE 1/4 of Section 5, T6N, R17W, Gallia Quad, Jackson County.38.86166667, -82.53805556204Wet marsh. Wild material1823918Ames 30366
105WLP 1046JDC/CF/2009/091/241Cornus florida L. Ohio, United StatesNA2009COLLECTED10/16/2009Wayne National Forest, near Dirtyface Creek, SE 1/4 of SW 1/4 of Section 21, T6N, R17W, Gallia Quad, Jackson County.38.80750000, -82.53000000210Associated with Acer saccharum, Cephalanthus occidentalis, Eutrochium maculatum, Hypericum densiflorum, Liriodendron tulipifera, Monarda fistulosa, Penstemon digitalis, Pinus virginiana, Prunella vulgaris, Rhus copallinum, (continued below)Wild material1823920WLP 1046
106Ames 30132JDC/CA/2009/041/191Cornus amomum Mill. subsp. obliqua (Raf.) J. S. Wilson Wisconsin, United StatesNC7SEED2009COLLECTED09/22/2009Along Kent Road, near Poynette, NW 1/4 of NW 1/4 of Section 29, T11N, R9E, Poynette Quad, Columbia County.43.40638889, -89.45861111243Hinkson Creek Watershed. Wild material1819713Ames 30132
107Ames 30133JDC/CD/2009/063/213Cornus drummondii C. A. Mey. Illinois, United StatesNC7SEED2009COLLECTED09/25/2009Four Corners Road, north from Illinois Highway 84, NW 1/4 of SW 1/4 of Section 36, T26N, R2E, Blackhawk (IL-IA) Quad, Jo Daviess County.42.20027778, -90.22944444194Roadside in fence row. Wild material1819714Ames 30133
108Ames 300862Cornus alternifolia L. f. Connecticut, United StatesNC7SEED2009COLLECTEDNEAR 09/2009Mansfield Center.41.76111111, -72.1877777878Edge of woods along a powerline cut. Sandy, well-drained soil.Wild material1813033Ames 30086
109Ames 300873Cornus amomum Mill. Maine, United StatesNC7SEED2009COLLECTEDNEAR 09/2009Damariscotta Lake, Nobleboro.44.14777778, -69.4800000018Backwater area between dirt road and edge of water. Wild material1813034Ames 30087
110Ames 300885Cornus amomum Mill. Connecticut, United StatesNC7SEED2009COLLECTEDNEAR 09/2009Eagleville Lake, Mansfield.41.78472220, -72.2805555683Near the dam and spillway, growing in riprap stones places along the edge of the dam. Full sun.Wild material1813035Ames 30088
111Ames 300894Cornus rugosa Lam. Maine, United StatesNC7SEED2009COLLECTEDNEAR 09/2009Great Salt Bay Preserve Farm, Damariscotta.44.04722222, -69.518055563Along a thin line of small trees facing an open meadow; close to the edge of the Damariscotta River/Great Salt Bay.Wild material1813036Ames 30089
112Ames 30061JDC/CA/2009/015/165Cornus alternifolia L. f. Illinois, United StatesNC7SEED2009COLLECTED08/06/2009Southwest edge of Pierce Lake, Rock Cut State Park, SW 1/4 of SE 1/4 of Section 27, T45N, R2E, Caledonia Quad, Rockford, Winnebago County.42.34333333, -88.98638889259Rich woods. Wild materialUp to 20-30 feet in height.1812364Ames 30061
113Ames 30062JDC/CR/2009/011/161Cornus rugosa Lam. Wisconsin, United StatesNC7Flower2009COLLECTED08/03/2009Along Highway 133, Lower Wisconsin Riverway State Wildlife Area, SE 1/4 of NW 1/4 of Section 14, T7N, R4W, Wauzeka East Quad, Woodman, Grant County.43.08527778, -90.81638889201Wisconsin River watershed. Wild material1812365Ames 30062
114Ames 30063JDC/CR/2009/014/164Cornus rugosa Lam. Wisconsin, United StatesNC7SEED2009COLLECTED08/04/2009Along Fairfield Road east of Paschen Road, SW 1/4 of SW 1/4 of Section 16, T12N, R7E, Lewiston Quad, Baraboo, Sauk County.43.51083333, -89.67583333259Rich woods. North facing slopeWild material1812366Ames 30063
115WLP 1036KC09-007Cornus florida L. NA2009COLLECTEDPRE 07/01/2009Virginia, Appomattox County, Route 601 6 miles north of intersection of 601 and route 460roadside; wooded; oak-hickory-maple forestWild material1896365WLP 1036
116Ames 29982NA 76656Cornus foemina Mill. Georgia, United StatesNC7FRUIT2009COLLECTED09/2005Berry College Flatwoods, Rome, Floyd County.34.34191000, -85.27233600Cultivated materialCultivated plant of known (indirect) wild origin.1800369Ames 29982
117NA 79163NACPEC08028Cornus kousa Hance subsp. chinensis (Osborn) Q. Y. Xiang Shaanxi Sheng, ChinaNA2008COLLECTED09/23/2008Hong He Gu Forest Park; northeast-running stream valley.34.06216000, 107.748660001388cool, moist northeast-running stream valley; mesic, mixed deciduous forest; open clearing in woods.Wild material1950255NA 79163
118WLP 1025AZB-2008-027Cornus sanguinea L. NA2008COLLECTEDPRE 10/15/2008Guba District, Vladimirovka Nursery41.39835000, 48.53626000Wild material1896254WLP 1025
119WLP 1028AZB-2008-069Cornus sanguinea L. NA2008COLLECTEDPRE 10/15/2008Gusar District, Gara BulagWild material1896269WLP 1028
120Ames 29532JDC/CA/2008/008/078Cornus alternifolia L. f. Illinois, United StatesNC7SEED2008COLLECTED08/25/2008Black Hawk Forest Nature Preserve, Rock Island, Rock Island County.41.46583333, -90.57277778186Wooded understory. Essentially full shade. Generally located along north facing 40% slope. Wild materialMajority of specimens exhibited strong central leaders at time of collection. Tallest specimen was approximately 25 feet in height.1783446Ames 29532
121Ames 29520JDC/CA/2008/010/080Cornus alternifolia L. f. Iowa, United StatesNC7SEED2008COLLECTED08/04/2008Along Dorchester Drive, just west of Dorchester, Allamakee County.43.47000000, -91.51777778265High knoll. Dry, rocky area. 70% slope, northeastern aspect. 50% full sun (morning); 50% full shade (afternoon). Wild material1782637Ames 29520
122Ames 29521JDC/CA/2008/012/082Cornus alternifolia L. f. Iowa, United StatesNC7SEED2008COLLECTED08/04/2008North and south sides of Ivy Road, Volga River State Park, Fayette, Volga River watershed, Fayette County.42.88027778, -91.78472222264Wet woodland, high organic matter. 65% mostly full sun (morning); 35% full shade (afternoon).Wild material1782638Ames 29521
123Ames 29523JDC/CA/2008/015/085Cornus alternifolia L. f. Illinois, United StatesNC7SEED2008COLLECTED08/06/2008Along trail heading towards lake, Crosby Road to parking lot, Morrisson-Rockwood State Park, approximately 2 miles north of Morrisson, Whiteside County.41.84222222, -89.96888889247Woodland area. 100% filtered shade. Wild material1782640Ames 29523
124Ames 29524JDC/CA/2008/011/081Cornus rugosa Lam. Iowa, United StatesNC7SEED2008COLLECTED08/04/2008Along Dorchester Drive, just west of Dorcheste.43.47027778, -91.51861111267High knoll. Dry, rocky area. 70% slope, northeastern aspect. 50% full sun (morning); 50% full shade (afternoon). Wild material1782641Ames 29524
125Ames 29506JDC-CA-2008-003Cornus alternifolia L. f. Iowa, United StatesNC7SEED2008COLLECTED07/20/2008Tower Rock Park, N edge of SE 1/4 of SW 1/4 of Section 28, T88N, R19W, Steamboat Roak Quad, Steamboat Rock, Hardin County.42.40111111, -93.07166667292Eroding (burnt orange) sandstone cliff, south side of Iowa River; mostly shaded; near base of slope with northern aspect; sand and organic matter above cliff; well drained. Wild material1782028Ames 29506
126Ames 29407RES008Cornus alternifolia L. f. Michigan, United StatesNC7SEED2008COLLECTED09/26/2002Near depression on north side of Beckett Road, west of Gingell Road, Ostego County.45.01472222, -84.47444444391Along the road, partial shaded understory, moist soils. Wild material1775521Ames 29407
127WLP 1077RES012Cornus florida L. Michigan, United StatesNA2008COLLECTED09/29/2002Michigan: Eaton County: Eaton Rapids; Natural area behind playground, Northwestern Elementary School.42.52027778, -84.66472222273Forested area, sandy loam soils. Associated vegetation: Cornus florida, Acer, Pinus, and Rhus.Wild material1775524WLP 1077
128WLP 1078RES013Cornus florida L. Michigan, United StatesNA2008COLLECTED10/02/2002Michigan: Calhoun County; Interstate 69 South rest area, north of junction with Interstate 94.42.32000000, -84.99222222286Edge of forested area along a rest area, sandy loam soils. Associated vegetation: Acer, Lindera, and Rhus.Wild material1775525WLP 1078
129Ames 29272Ames 29272Cornus rugosa Lam. Minnesota, United StatesNC7BARK2007COLLECTEDAlong Highway 108 (intersection of east park boundary gravel road and Highway 108), northeast corner of Maplewood State Park, Otter Tail County.46.54470000, -95.92750000444Wild materialPlants grown from seed collected in the wild.1743776Ames 29272
130WLP 962CHCOMD01-07Cornus florida L. NA2007COLLECTEDPRE 10/29/2007Maryland, Charles County, Along Highway 638.46591000, -77.16308000Woodland edge understoryWild material1895944WLP 962
131WLP 961FREDERICK0107Cornus florida L. NA2007COLLECTEDPRE 10/15/2007Maryland, Frederick County, Poffenberger Road near Catoctin Creek in mixed forest39.37380000, -77.55690000Roadside, mixed forest along creekWild material1895938WLP 961
132WLP 957RL 07004Cornus foemina Mill. NA2007COLLECTEDPRE 09/15/2007Georgia, Floyd County, Berry College flatwoods, along road in clay flatwoods.Wild material1895879WLP 957
133WLP 959RL 07025Cornus foemina Mill. NA2007COLLECTEDPRE 09/15/2007Florida, Orange County, Along Wekiva River.Wild material1895893WLP 959
134Ames 35652AZ FALL06-8Cornus mas L. Lerik, AzerbaijanNC7SEED2007COLLECTED10/15/2006Lankaran-Astara, Lerik, Bobogil Village (24 km from Lankaran), Talish Mountains38.73506000, 48.63435000237Streambank of Lerik River. Woodland, with a 90 slolpe and a NW aspect.Wild material1890563Ames 35652
135Ames 28962GE-2006-033Cornus mas L. Tbilisi, GeorgiaNC7SEED2007COLLECTED09/19/2006Georgia Institute of Horticulture, Viticulture and Oenology: Tbilisi Province.41.75194444, 44.77111111423Research institute sample.Cultivated materialGIHVO (Georgia Institute of Horticulture, Viticulture and Oenology - Tbilisi, Georgia) Cornelian Cherry Selection No. 1: Characterstics: Fruit small, ovate, 2.0 cm long, 1.2 cm diameter, dark purple flesh, distinct, rich, pomegranate-like flavor.1719331Ames 28962
136Ames 28966GE-2006-132Cornus mas L. K'akheti, GeorgiaNC7SEED2007COLLECTED09/27/2006Dedoplis Tskaro, Kakheti Province.41.46527778, 46.09500000801Yard of private home. Specimen originally purchased from a grower.Cultivated materialFruit 2.0 cm long, 1.3 cm diameter, ovoid, dark purple, astringent.1719334Ames 28966
137NA 75365RL 249Cornus amomum Mill. North Carolina, United StatesNA2006COLLECTED07/01/2005North Carolina, Henderson County, McDowell Creek, near junction with Fanning Field Road.Wild material1777642NA 75365
138Ames 27966Ames 27966Cornus alternifolia L. f. Minnesota, United StatesNC7PLANT2005COLLECTED2003Maplewood State Park, Otter Tail County.46.51666670, -95.95861111424Wild material1700786Ames 27966
139Ames 29890172417Cornus sericea L. Colorado, United StatesNC7SEED2005COLLECTED08/08/2002Colorado Rocky Mountains. Grand County. Corral Creek.40.07750000, -106.185830002325Montane riparian community. Wild materialShrub 1.2-1.5 meters tall. 1673920Ames 29890
140WLP 2075178626Cornus nuttallii Audubon Oregon, United StatesNASEED2005COLLECTED10/07/2002386Moderately closed canopy Pseudotsuga menziesii/Acer macrophyllum dominated forest with Acer circinatum/Sambucus nigra understory. Shrub cover of Gaultheria shallon, Vaccinium parvifolium, Berberis nervosa, Rubus discolor, PteWild materialTree 4.5-15 meters tall. 1674069WLP 2075
141Ames 27382GE-2004-004Cornus mas L. K'akheti, GeorgiaNC72004COLLECTED09/21/2004Lagodekhi Preserve, Kakheti Province.41.84506000, 46.28223000607Riparian woods.Wild material1665041Ames 27382
142WLP 1048AG Number 443Cornus canadensis L. NA2004COLLECTEDPRE 10/29/2004Alaska, Pt. MacKenzieWild material1896473WLP 1048
143WLP 1049AG Number 441Cornus canadensis L. NA2004COLLECTEDPRE 10/29/2004Alaska, Peter HillsWild material1896474WLP 1049
144WLP 1050NA 80098Cornus canadensis L. NA2004COLLECTEDPRE 10/29/2004Alaska, Wolverine Creek BridgeWild material1896475WLP 1050
145NSL 439911'Jefferson'Cornus drummondii C. A. Mey. Iowa, United StatesNC7SEED2004COLLECTED09/15/1988Round Prairie Park near Fairfield, T71N R8W Sec. 32.40.91348600, -91.80467100192Slope 14 to 25%. 109 MLRA. Lindley loam soil.Wild materialRoughleaf dogwood is a small native tree (5-6m tall) that can form dense colonies by root suckers. Fruits are a white, berry-like drupe, globular (6-7mm) in shape that mature in the fall. Jefferson was selected out of an assembly of fivty-five collections planted at the Natural Resources Conservation Service Plant Materials Center, Elsberry, MO. This accession was selected based on fruit production, insect and disease resistance, form and seedling vigor. Jefferson was the best fruit producer of all the accessions included in the assembly that originated from the state of Iowa. 1694820NSL 439911
146NSL 439912'Corinth'Cornus drummondii C. A. Mey. Missouri, United StatesNC7SEED2004COLLECTED1999Along a gravel road that passes by Presley's Rock Quarry, north of Foley.39.05818700, -90.75841600168Wild materialRoughleaf dogwood is a small native tree (5-6m tall) that can form dense colonies by root suckers. Fruits are a white, berry-like drupe, globular (6-7mm) in shape that mature in the fall. Corinth was selected out of an assembly of fivty-five collections planted at the Natural Resources Conservation Service Plant Materials Center, Elsberry, MO. This accession was selected based on fruit production, insect and disease resistance, form and seedling vigor. Corinth was the best fruit producer of all the accessions included in the assembly that originated from the state of Missouri.1694821NSL 439912
147NSL 439913'Tazewell'Cornus drummondii C. A. Mey. Illinois, United StatesNC7SEED2004COLLECTED11/15/1988Near Pekin: T24N R5W Sec. 2.40.56194300, -89.63071600184Rozetta-Fagette soil.Wild materialRoughleaf dogwood is a small native tree (5-6m tall) that can form dense colonies by root suckers. Fruits are a white, berry-like drupe, globular (6-7mm) in shape that mature in the fall. Tazewell was selected out of an assembly of fivty-five collections planted at the Natural Resources Conservation Service Plant Materials Center, Elsberry, MO. This accession was selected based on fruit production, insect and disease resistance, form and seedling vigor. Tazewell was the best fruit producer of all the accessions included in the assembly that originated from the state of Illinois.1694822NSL 439913
148NSL 439914'Nicholson'Cornus drummondii C. A. Mey. Kansas, United StatesNC7SEED2004COLLECTED09/16/1987Native stand near Junction City.38.99444200, -96.779278003665% slope. 76 MRLA. 787.4 mL precipitation.Wild materialRoughleaf dogwood is a small native tree (5-6m tall) that can form dense colonies by root suckers. Fruits are a white, berry-like drupe, globular (6-7mm) in shape that mature in the fall. Nicholson was selected out of an assembly of fivty-five collections planted at the Natural Resources Conservation Service Plant Materials Center, Elsberry, MO. This accession was selected based on fruit production, insect and disease resistance, form and seedling vigor. 1694823NSL 439914
149Ames 275019023733Cornus sericea L. subsp. sericea Oregon, United StatesNC72004COLLECTEDMajor Land Resource Area E-43, Near Wallowa, Wallowa County.823Wild materialDeciduous shrub up to 4.5 feet in height and 7 feet in width. It produces numerous stems, leaves, and fruit. Plants are stoloniferous, producing roots where branches contact soil with adequate moisture. Plants tend to have a spreading growth form with numerous stems, attributes which were deemed desirable for riparian plantings. Single clone from six original plants. Selected from a Pullman PMC study of 71 Redosier dogwood accessions, 56 of which were planted in the field. The Redosier dogweed study was evaluated from 1983-1987. Rated excellent in vigor, number of basal stems, and very good in fruit production, foliage, and stem abundance. Grows well in moist well-drained sites. Tolerates flooding and partial shade. After establishment for several years, it will live with roots submerged in water for most of the growing season. The primary potential use is in bioengineering projects and riparian rehabilitation efforts in the Pacific Northwest. It is recognized as a plant which can be planted as cuttings direct into moist soil. It is an excellent plant for erosion control on streambanks, shorelines, and other sites with adequate moisture. Its spreading habit and extensive root system withstands action by waves and currents, aiding in holding soil. It is an attractive plant for landscaping as a screen or hedge. Stems and twigs are bright red, being especially attractive in winter after leaves drop. It is also a valuable wildlife plant as browse, cover, and food. Conservation practices that may use it include Critical Area Planting and Riparian Forest Buffer.1660420Ames 27501
150Ames 275039023758Cornus sericea L. subsp. sericea Washington, United StatesNC72004COLLECTEDLake Creek, Major Land Resource Area B-8 (Columbia Plateau), near Harrington, Lincoln County.600Wild materialDeciduous shrub up to 4.5 feet in height and 5 feet canopy width after 13 years on an upland site with average annual precipitation of 20 inches. It produces numerous stems, leaves, and fruit. Plants are stoloniferous, producing roots where branches contact soil with adequate moisture. Plants tend to have a spreading growth form with numerous stems, attributes which were deemed desirable for riparian plantings. Clonal selection from six original plants. Selected from a Pullman PMC study of 73 Redosier dogwood accessions, 67 of which were planted in the field. The Redosier dogweed study was evaluated from 1983-1987. Limited evaluations were made through 1995. Rated excellent in vigor and number of basal stems, and very good in fruit production, foliage, and stem abundance. Grows well in moist well-drained sites. Tolerates flooding and partial shade. After establishment for several years, it will live with roots submerged in water for most of the growing season. The primary potential use is in bioengineering projects and riparian rehabilitation efforts in the Pacific Northwest. It is recognized as a plant which can be planted as cuttings direct into moist soil. It is an excellent plant for erosion control on streambanks, shorelines, and other sites with adequate moisture. Its spreading habit and extensive root system withstands action by waves and currents, aiding in holding soil. It is an attractive plant for landscaping as a screen or hedge. Stems and twigs are bright red, being especially attractive in winter after leaves drop. It is also a valuable wildlife plant as browse, cover, and food. Conservation practices that may use it include Critical Area Planting and Riparian Forest Buffer.1660422Ames 27503
151Ames 27058Index Seminum 22Cornus amomum Mill. Tennessee, United StatesNC72003COLLECTED2002Morgan County. Lily Bridge Wild River Access to Clear Creek from Ridge Road, ca. 8.2km west-southwest of Wartburg.36.10288300, -84.71795000360River bank. Growing in association with Rhododendron arborescens, Leucothoe recurva, Aronia arbutifolia, Hypericum prolificum, Vaccinium arboreum, Conradina verticillata, and CalycanthusWild material1645452Ames 27058
152Ames 2699702-004Cornus racemosa Lam. Minnesota, United StatesNC72003COLLECTED2002One mile south of Backus, Cass County.46.81630000, -94.51701660Trail.Wild material1644315Ames 26997
153Ames 2699803-02Cornus rugosa Lam. Minnesota, United StatesNC7PLANT2003COLLECTED2002Collections made at three sites between Walker and Backus (14.3 mile stretch) at T141N R31W Sec. 15, T140N R30W Sec. 18, and T139N R30W Sec. 28, Cass County.46.95055550, -94.52972220400Wild material1644316Ames 26998
154Ames 2699902-010Cornus rugosa Lam. Minnesota, United StatesNC7PLANT2003COLLECTED2002Hennepin County.44.95472222, -93.70638889294Wild material1644317Ames 26999
155Ames 2693134-002Cornus alba L. Habarovskij kraj, Russian FederationNC7PLANT2002COLLECTED08/2002Burea River region.Wild material1641472Ames 26931
156Ames 26926ARM-02-127Cornus mas L. Tavuš, ArmeniaNC72002COLLECTED09/07/2002Dilijan National Park, Tavush Marz.40.70250000, 45.055555561116Edge of mature woodland.Wild materialSmall, multi-stemmed tree, 5 meters tall. Red fruits. In Armenia, fruits are sold locally for juice and jam, considered healthful. 1641467Ames 26926
157Ames 26927ARM-02-191Cornus mas L. Loṙi, ArmeniaNC7PLANT2002COLLECTED09/14/2002Near Alaverdi, Lorri Marz.40.99805556, 44.65222222834Disturbed rocky slope along river.Wild materialMulti-stemmed tree. Red, shiny fruit. In Armenia, fruits are sold locally for juice and jam, considered healthful. Specimens growing in cultivation at NCRPIS station in Ames, Iowa exhibited orange-red fall color on 31 Oct. 2013.1641468Ames 26927
158Ames 26928ARM-025-02Cornus sanguinea L. subsp. australis (C. A. Mey.) Jáv. ArmeniaNC72002COLLECTED09/01/2002Syunik Marz.39.14583333, 46.45555556994Edge of forest. Slope of 45 with a southern aspect. Wild materialTree, 5 meters tall. Blue-black fruit; 5 mm x 8 mm. 1641469Ames 26928
159WLP 94315-2002Cornus bretschneideri L. Henry Shaanxi Sheng, ChinaNA2002COLLECTEDPRE 03/14/2002Shanxi Province, Pangquangou National Preserve. Wild collected among shrubs habitat Green Corridor.Wild material1895789WLP 943
160Ames 261423.2Cornus mas L. Kiev, UkraineNC7PLANT2000COLLECTED10/2000Near Khodosovka (suburb of Kyiv), approximately 20 km south of Kyiv.50.26666667, 30.51666667100Small plantation.Cultivated material1606546Ames 26142
161Ames 26065Index Seminum 39Cornus rugosa Lam. Ontario, CanadaNC72000COLLECTEDPRE 12/1999Highland Creek valley, Toronto.43.76666667, -79.20000000138Upland mixed forest.Wild material1599819Ames 26065
162Ames 25499WSYUS 5Cornus mas L. Kiev, UkraineNC7FRUIT1999COLLECTED09/08/1999Botanical garden of the National Agricultural University, Kyiv.50.38305556, 30.50388889140Along trail through the botanical garden. Partial shade, 1% slope with a northwestern exposure. Sandy loam soil with good drainage. Two L-shaped rows of Cornus mas bordered by Fagus sylvatica and Acer.Cultivated materialTrees have an arching crown, no lower branches. 1586016Ames 25499
163Ames 24553'Bud's Yellow'Cornus sericea L. subsp. sericea Manitoba, CanadaNC7FLOWER1998DEVELOPEDPRE 1998CultivarBright yellow stems and improved disease resistance make it vastly superior to older, greener cultivars. Zone 3, 6-8 feet tall, good for cut flowers or foilage, full sun to partial shade. Growth rate: will produce 1 gallon container plant in 1 growing season.1556799Ames 24553
164NA 67878QLG246Cornus kousa Hance subsp. chinensis (Osborn) Q. Y. Xiang Gansu Sheng, ChinaNA1996COLLECTED10/18/1996Xiao Long Shan Forest Bureau, Guang Ying Forest Station, Wang Jia Gou34.18361111, 106.000277781550Along woodland edge in upper canopy in full sun; 35% NW slope; clay-loam soil; w/ Symplocos paniculata, Populus sp., Quercus sp., Lindera sp., Campylotropis sp., Corylus sp., Sorbaria sp., Lonicera japonica and numerous herbaceous sp.Wild material9 meters; single-stemmed deciduous tree with upright vase-shaped habit; absolutely loaded with fruit; D.B.H. 18 cm; bark gray-brown to tan and exfoliating; fruit red, globe-shaped, 2-3 cm diameter 1579681NA 67878
165NA 67880 NA 67880QLG248Cornus controversa Hemsl. Gansu Sheng, ChinaNA1996COLLECTED10/06/1996Qinling Mountains: Tianshui City: Xiaolongshan Forestry Experimental Bureau, Guangying Forest Station, Wangjiagou.34.18516000, 106.010520001540Growing one meter above the stream in open, full sun and heavily grazed area among boulders; growing in clay-loam soil. Slope: Less than 3 percent. Aspect: North.Wild material1951538NA 67880 NA 67880
166Ames 23203Al 072Cornus mas L. Korçë, AlbaniaNC7FRUIT1996COLLECTEDNEAR 08/27/1996Along road between Leskovik and Ersekel, Korçë40.18638889, 20.64916667840Many Cornus mas growing at edge of field. All but one had red fruits.Wild materialTree 6m tall. Fruits red.1531345Ames 23203
167Ames 22080Ames 22080Cornus racemosa Lam. New Jersey, United StatesNC7FRUIT1994COLLECTEDBlawenburg.40.40750000, -74.7030555648Wild material1087560Ames 22080
168Ames 21980Ames 21980Cornus racemosa Lam. Michigan, United StatesNC71994COLLECTED1993East side of Bear Lake, Ingham County.42.70000000, -84.50000000Open old field. Wild material1087401Ames 21980
169Ames 21899719-79ctCornus pumila Koehne Illinois, United StatesNC7Flower1994DONATED02/15/1994ADD_DATA1:: Minimal data entered 4/21/94.1087299Ames 21899
170Ames 20183No. 9Cornus racemosa Lam. New Jersey, United StatesNC7PLANT1993COLLECTEDMorris and Somerset Counties.40.78333333, -74.45000000Plants growing in their native stations.Wild material1084375Ames 20183
171WLP 930NA 64067Cornus florida L. Missouri, United StatesNA1992COLLECTEDMississippi, Clay CountyWild material1494386WLP 930
172NA 66345NA 66345Cornus florida L. NA19921951674NA 66345
173NA 63135(open-pollinated seed of Xanthocarpa Group)Cornus florida L. United StatesNA1991COLLECTEDNorth side of route 64 at junction with Morrison Grove Rd. Roanoke Island35.88266800, -75.65545700Wild material1496785NA 63135
174NA 63266NG 7Cornus florida L. Maryland, United StatesNA1991COLLECTED10/02/1991Maryland, Caroline County, Tuckahoe State Parkopen woodland edge of field.Wild materialFrom 10 trees in one area.1494716NA 63266
175Ames 1489718Cornus racemosa Lam. Illinois, United StatesNC71991COLLECTEDDupage County, Illinois.41.83024200, -88.05198800Wild materialCollected from natural populations, DuPage Co., Illinois.1069320Ames 14897
176WLP 924GU 130Cornus florida L. Virginia, United StatesNA1989COLLECTED09/28/1989George Washington National Forest, Forest Road 92, along Stony Creek.38.14103700, -79.09881600609Deciduous woodland. Elevation: 2000 feet.Wild material1112037WLP 924
177WLP 925GU 136Cornus florida L. Virginia, United StatesNA1989COLLECTED09/29/1989George Washington National Forest, Junction 273 & 758, Powell Mountain.Wild material1496023WLP 925
178Ames 5709Ames 5709Cornus mas L. New York, United StatesNC7FLOWER1986DONATEDPRE 1986Cultivated materialLarge deciduous shrub or small tree, red fruits and yellow flowers.1032999Ames 5709
179NA 56660KSW 3723Cornus kousa Bürger ex Hance Korea, SouthNA1985COLLECTED10/08/1985Yuyu Dong, Mapo-ri, Sannae Myon, Puan Gun, Cholla Pukto On cut-over NW-facing slope, in thicket, sun.35.61666667, 126.53333333150Wild materialSmall 2-trunked decid. tree ca 6 m tall, dbh 11 cm, with slightly ascending nearly horizontal branches; bark dark gray, lenticelate, exfoliating to reveal yellowish patches; lvs. dull med. yellow-green turning purple above, paler beneath; peduncles long, reddish; frt. ripe, soft, falling, dark dull purplish-red, pulp yellow, edible.1111156NA 56660
180NA 55081KNW 278Cornus kousa Bürger ex Hance Incheon-gwangyeoksi, Korea, SouthNA1984COLLECTED10/08/1984Ganghwa-gun, Hwado-myeon: Ganghwado (island): Sagi-ri: On path to Chongsu-sa [temple]. [Originally listed as Kyong Gi Do, Kanghwa Gun, Hwado Myon, Sagiri, on path to Chongsu Sa temple.]37.61749600, 126.46859700150In understory of mixed deciduous forest.Wild materialSingle-trunked deciduous tree 6m tall, DBH 15.5cm, vase shaped. Heavily-fruited, red frt. soft and ripe, falling. Voucher tree in adjacent valley.1109714NA 55081
181PI 704858 sosV. uliginosum AK930-900Vaccinium uliginosum L. Alaska, United StatesCOR2021Wild material2116042PI 704858 sos
182PI 702701MARSB-249Dichanthelium clandestinum (L.) Gould New York, United StatesS9SEED2019Wild material2097541PI 702701
183PI 691719WLP 1903Viburnum nudum L. Maine, United StatesNA2015COLLECTED08/23/2015Along west edge of Timber Cove Road, just northwest of intersection with Hwy. 189 and across the road from a cemetery. Approximately 13 km southwest of Lubec, Washington County, ME.44.80160000, -67.1270500032Edge of woods; roadside.1950395PI 691719
184PI 665769ALB-2011-078Pyrus spinosa Forssk. Tepelene, AlbaniaCOR2011COLLECTED09/22/2011Village of Lekdush40.23023000, 19.96202000980Small village in mountains SW of Tepelene. Terraced agricultural slopes, mostly small pastures separated by hedgerows of Cornus mas, Prunus mahaleb, blackberry, oak, pear.Wild material1891931PI 665769
185PI 691727WLP 1261Ilex verticillata (L.) A. Gray New York, United StatesNAFRUIT2011COLLECTED09/12/2011Hanging Bog Game Management Area, just west of Hanging Bog, Allegany County.42.30500000, -78.25600000632Marsh. Associated with Aronia, Aster, Cornus amomum, Eutrochium, Salix, Solidago, Spiraea alba, Viburnum cassinoides, Viburnum dentatum, and Viburnum lentago.Wild material1891481PI 691727
186PI 675309R10-15-060Brachypodium sylvaticum (Huds.) P. Beauv. Stavropol, Russian FederationW62011COLLECTED07/20/2010NE facing slope at foot of Mashuk Mountain near Pyatigorsk44.06300000, 43.09500000592Temperate deciduous forest understory. Limestone parent material, located in the forest and openings: seed collected from >100 plantsWild material1883155PI 675309
187PI 685593R10-18-070Poa nemoralis L. Stavropol, Russian FederationW62011COLLECTED07/21/2010Forest at mid-elevation of Mashuk Mountain near Pyatigorsk44.04600000, 43.08800000752Temperate deciduous forest understory. Deep black soils, 5-10% slope: seed collected from >100 plantsWild material1883165PI 685593
188PI 693827R10-15-058Dactylis glomerata L. subsp. lobata (Drejer) H. Lindb. Stavropol, Russian FederationW62011COLLECTED07/20/2010NE facing slope at foot of Mashuk Mountain near Pyatigorsk44.06300000, 43.09500000592Temperate deciduous forest understory. Limestone parent material, small statured <0.4m in height, fine, light green, soft, lax, basal leaves (diploid?): seed collected from >100 plantsWild material1883153PI 693827
189PI 699305R10-15-284Poa pratensis L. subsp. angustifolia (L.) Arcang. Stavropol, Russian FederationW62011COLLECTED07/20/2010NE facing slope at foot of Mashuk Mountain near Pyatigorsk44.06300000, 43.09500000592Temperate deciduous forest understory. Limestone parent material, dark-green collection: seed collected from >100 plantsWild material1883362PI 699305
190PI 664805JDC/HX/2010/035/305Helianthus mollis Lam. Kansas, United StatesNC72010COLLECTED09/14/2010Roadside along Kansas Rd, west of Hwy 3 south of Uniontown, Bourbon County.37.81978000, -94.98685000325Uplands. Associated with Andropogon gerardii, Bidens polylepis, Chamaechrista fasciculata, Cornus, Diospyros virginiana, Gleditsia triacanthos, Juglans nigra, Maclura pomifera, Monarda, Pycnanthemum virginianum, Quercus, Rhus glabra, and Sorghastrum nutans.Wild material1848907PI 664805
191PI 664899JDC/PV/2009/092/242Prunella vulgaris L. Ohio, United StatesNC7SEED2009COLLECTED10/16/2009Wayne National Forest, near Dirtyface Creek, SE 1/4 of SW 1/4 of Section 21, T6N, R17W, Gallia Quad, Jackson County.38.80750000, -82.53000000210Open prairie. Variable soil types present. Wild material1823940PI 664899
192PI 673984JDC/RL/2009/067/217Rudbeckia laciniata L. Illinois, United StatesOPGC2009COLLECTED09/25/2009Along Rush Road, NW 1/4 of NW 1/4 of NE 1/4 of Section 36, T26N, R2E, Blackhawk (IL-IA) Quad, Jo Daviess County.42.21000000, -90.22472222192Roadside. Associated with Clematis virginiana, Cornus amomum subsp. obliqua, C. drummondii, Juglans nigra, and Viburnum lentago.Wild material1819752PI 673984
193PI 657226V. pallidum Stumphouse HD-2007-025Vaccinium pallidum Aiton South Carolina, United StatesCORImage2007COLLECTED06/04/2007Stumphouse Mountain, Oconee County. Northwest of Walhalla off SR-107, Ross Mountain Road, near Gramling Drive, edge of trail.34.82217000, -83.10895000487Red sandy loam associated with: Liriodendron tulipifera, Oxydendron arboreum, Kalmia latifolia, Acer rubrum, Quercus nigra, Cornus florida and Prunus virginiana.Wild materialKim Hummer, Michael Dossett collected from South Carolina.

1730117PI 657226
194PI 664836Ames 28959Echinacea purpurea (L.) Moench Iowa, United StatesNC7HEAD2007COLLECTED2006Codfish Hollow Hill Prairie just east of Maquoketa (Southern Iowa Drift Plain) T84N R3E NE1/4 Sec. 23 and NE1/4 Sec. 2442.07419100, -90.56693400214Woodland-prairie edge. General land use light intermittent grazing. Cool and damp with northern exposure and tree/brush enclosure. Nordess silt loam at rocky dolomite outcrop junction with Fayette-Lamont-Chelsea complex silt loam soil. Wild materialThis population of Echinacea purpurea may represents one of the very few native sites and the most northern in Iowa. Plants show phenotypic variation within the population, consistent with native populations. Specimens are generally restricted to the cooler and damper (north-facing and tree/brush enclosed) areas of the prairie/savanna complex. 1717968PI 664836
195PI 649023NY2Actaea racemosa L. New York, United StatesNC72005Wild material1698893PI 649023
196PI 664811DE2Actaea racemosa L. Delaware, United StatesNC72005Wild material1698885PI 664811
197PI 664813KY1Actaea racemosa L. Kentucky, United StatesNC72005Wild material1698887PI 664813
198PI 64902146Actaea racemosa L. Missouri, United StatesNC72004Wild material1 meter tall.1668177PI 649021
199PI 656815JM2004010Monarda clinopodia L. South Carolina, United StatesNC7SEED2004COLLECTED10/05/2004Wadakoe Mountain, Pickens County.34.98055556, -82.84361111464Cove-hardwood community. Wild material1667582PI 656815
200PI 664873JM2004005Prunella vulgaris L. North Carolina, United StatesNC72004COLLECTED10/02/2004Highway 276 to East Fork Road, Pine Shore Lakes, Brevard, Transylvania County.35.12611111, -82.72944444851Pine-oak forest. Lakeside on private land. 15 degrees of slope with a northwestern aspect. Wild material15-40 cm tall.1667584PI 664873
201PI 649072Ames 27522Hypericum perforatum L. TurkeyNC7PLANT2004COLLECTEDNorth of Zigana Pass along E97 (Trabzon Gumushane Yolu) near Zigana Tunnel.40.66150000, 39.41410000Moist roadside. Wild material1660643PI 649072
202PI 64974544Symphoricarpos orbiculatus Moench Iowa, United StatesNC72003COLLECTED10/21/2003Chichaqua Wildlife Habitat Park bottoms, Elkhart, NW corner of SE 1/4 of SE 1/4 of Section 29, T81N, R22W, Loring Quad, Polk County.41.79472222, -93.42972222250Alluvial soil. Understory of green ash, Cornus drummondii, Rubus occidentalis, and Smilax.Wild materialLow, suckering shrubs to 1 meter tall. Good fruit and foliage quality.1649921PI 649745
203PI 64970314Physocarpus opulifolius (L.) Maxim. Iowa, United StatesNC7PLANT2003COLLECTED09/14/2003Fish Farm Mounds, New Albin, SW 1/4 of SW 1/4 of NW 1/4 of Section 26, T100N, R4W, New Albin Quad, Allamakee County.43.45111111, -91.28222222280Sandstone ridge just above goat prairie. 1/2 sun. 30-50% slope w/ NW aspect. Sandy loam soil w/ some stoniness, well drainedWild materialMedium sized shrubs. 1649463PI 649703
204PI 635435H. lupulus var. neomexicanus OCJ-09Humulus lupulus L. var. neomexicanus A. Nelson & Cockerell Colorado, United StatesCOR2002COLLECTED09/12/2002Four miles west of Milner on US-40 between milepost (MP) 117 and MP 118 at Little Butcherknife Gulch. On both sides of the road.40.48722000, -107.088890002063Aluvial road fill. Ribes aureum, Chrysothamnus nauseosus, Salix sp., Quercus gambelii and Cornus sericea subsp. sericea.Wild material1642194PI 635435
205PI 635438H. lupulus var. neomexicanus OCJ-12Humulus lupulus L. var. neomexicanus A. Nelson & Cockerell Colorado, United StatesCOR2002COLLECTED09/12/2002East of Hayden on US-40, north on County Road 70 for 100 meters. Between railroad tracks and river.40.48889000, -107.156110001964Raparian; among Cornus sericea subsp. sericea.Wild material1642197PI 635438
206PI 635439H. lupulus var. neomexicanus OCJ-13Humulus lupulus L. var. neomexicanus A. Nelson & Cockerell Colorado, United StatesCOR2002COLLECTED09/12/2002A mile west of Hayden on US-40. After crossing the Yampa River, plants are found in the low area between the road and the railroad tracks to the north.40.49194000, -107.298890001939Among Salix sp., Cornus sericea subsp. sericea and Populus sp.Wild material1642198PI 635439
207PI 635473H. lupulus var. neomexianus OCJ-50Humulus lupulus L. var. neomexicanus A. Nelson & Cockerell Colorado, United StatesCOR2002COLLECTED09/18/2002Travel 2.6 miles on State Highway 62 (S-62) north of S-145, between mileposts 2 and 3. West side of Leopard Creek, between road and creek.38.04861000, -108.034720002299Raparian; Populus sp., Rosa sp., Cornus sericea subsp. sericea and Salix sp.Wild material1642232PI 635473
208PI 635474H. lupulus var. neomexicanus OCJ-51Humulus lupulus L. var. neomexicanus A. Nelson & Cockerell Colorado, United StatesCOR2002COLLECTED09/18/2002Travel one-fourth mile on State Highway 62 (S-62) north of S-145. West side of Leopard Creek, between road and creek.38.02250000, -108.055000002228Raparian; Populus sp., Rosa sp., Cornus sericea subsp. sericea and Salix sp.Wild material1642233PI 635474
209PI 635485H. lupulus var. neomexicanus OCJ-64Humulus lupulus L. var. neomexicanus A. Nelson & Cockerell Colorado, United StatesCOR2002COLLECTED09/19/2002North of the Colorado and New Mexico boarder. Take Exit 2 off Interstate 25 and back south a short distance on an old road to Raton Creek where a railroad bridge crosses over the creek.37.01917000, -104.491390002201Raparian; Populus sp., Rosa sp., Cornus sericea subsp. sericea and Salix sp.Wild material1642245PI 635485
210PI 638194R. sachalinensis HVSC-068Rubus sachalinensis H. Lév. Habarovskij kraj, Russian FederationCORImage2001COLLECTED8 km from Aubovby Mbis edge of road, exposure was open, slope was flat soil texture was sandy49.00694000, 136.4719400043edge of road Associated vegetation: Cornus ceresia, Alnus, Betula platyphylla, SpireaWild materialSurname initials of collectors (Hummer, Vorsa, Sabitov and Cherbukin.)

1631186PI 638194
211PI 700070'Little Cherub'Viburnum nudum L. North Carolina, United StatesNA2000COLLECTED15/09/2000Buncombe County: Asheville: North Carolina Arboretum.35.49441000, -82.60726000667Plants growing well as understory shrub in dappled shade, mesic cove environment; multiple plants adjacent to dirt road in sandy soil.CloneU.S. National Arboretum introduction. One seedling formerly accessioned under NA 70426 (individual 70426-008, growing at South Farm in the 200 Field, Row 11), showing a distinctly compact, dense habit. Following evaluation, released in 2022 as 'Little Cherub' (PI-700070).1950336PI 700070
212PI 612499F. virginiana subsp. virginiana RH 30 MiFragaria virginiana Mill. subsp. virginiana Minnesota, United StatesCORImageOut of Season1999COLLECTED06/21/1986Cut Face Creek (Good Harbor Creek), Cook county, Minnesota47.73028000, -90.440000000Populus tremuloides, Cornus sp. and Picea marianaWild materialPartial hermaphrodite; cyclic flowering; resistant to black root rot, scorch and spot; representative of subsp. virginiana from the upper midwest (Minnesota).1588167PI 612499
213PI 612359RUS 98 02-01Malus orientalis Uglitzk. Caucasus, Soviet UnionGEN1998COLLECTED07/25/19985 km. south of Krymsk, near an ancient Greek village of Alevra.44.92000000, 38.00000000100Slight SE facing slope. The population area covered about 1 km. Associated species: Cornus mas, Pyrus sylvestris, Crataegus monogyna, Prunus spinosa. Rainfall: 640 mm. annuallyWild materialLeaves and seeds collected. 1563272PI 612359
214PI 612360RUS 98 02-02Malus orientalis Uglitzk. Caucasus, Soviet UnionGEN1998COLLECTED07/25/19985 km. south of Krymsk, near an ancient Greek village of Alevra.44.92000000, 38.00000000100Slight SE facing slope. The population area covered about 1 km. Associated species: Cornus mas, Pyrus sylvestris, Crataegus monogyna, Prunus spinosa. Rainfall: 640 mm. annuallyWild materialLeaves and seeds collected. 1563273PI 612360
215PI 612361RUS 98 02-03Malus orientalis Uglitzk. Caucasus, Soviet UnionGEN1998COLLECTED07/25/19985 km. south of Krymsk, near an ancient Greek village of Alevra.44.92000000, 38.00000000100Slight SE facing slope. The population area covered about 1 km. Associated species: Cornus mas, Pyrus sylvestris, Crataegus monogyna, Prunus spinosa. Rainfall: 640 mm. annuallyWild materialLeaves and seeds collected. 1563274PI 612361
216PI 612365RUS 98 03-01Malus orientalis Uglitzk. Caucasus, Soviet UnionGEN1998COLLECTED07/26/19983 km. southwest of Shuntuk, 1 km. from nearest commercial apples.44.43000000, 40.15000000400Slight NW facing slope along the edge of an open field. Trees were 35 to 80 years old. The population covered about 1 km. Associated species: Cornus mas, Pyurs sylvestris, Crataegus monogyna, Prunus spinosa. Rainfall: 800-1000 mm. annually.Wild materialLeaves and seeds collected. 1563276PI 612365
217PI 612366RUS 98 03-02Malus orientalis Uglitzk. Caucasus, Soviet UnionGEN1998COLLECTED07/26/19983 km. southwest of Shuntuk, 1 km. from nearest commercial apples.44.43000000, 40.15000000400Slight NW facing slope along the edge of an open field. Trees were 35 to 80 years old. The population covered about 1 km. Associated species: Cornus mas, Pyurs sylvestris, Crataegus monogyna, Prunus spinosa. Rainfall: 800-1000 mm. annually.Wild materialLeaves and seeds collected. 1563277PI 612366
218PI 612373RUS 98 04-01Malus orientalis Uglitzk. Caucasus, Soviet UnionGEN1998COLLECTED07/26/19987 km. southwest of Shuntuk, in the "Horse mound" area.44.41000000, 40.12000000500Trees were 35 to 100 years old. The population area covered about 3 km. Associated species: Cornus mas, Pyrus sylvestris, Crataegus monogyna, Prunus spinosa. Rainfall: 800-1000 mm. annually.Wild materialLeaves and seeds collected. 1563282PI 612373
219PI 612374RUS 98 04-02Malus orientalis Uglitzk. Caucasus, Soviet UnionGEN1998COLLECTED07/26/19987 km. southwest of Shuntuk, in the "Horse mound" area.44.41000000, 40.12000000500Trees were 35 to 100 years old. The population area covered about 3 km. Associated species: Cornus mas, Pyrus sylvestris, Crataegus monogyna, Prunus spinosa. Rainfall: 800-1000 mm. annually.Wild materialLeaves and seeds collected. 1563283PI 612374
220PI 612375RUS 98 04-03Malus orientalis Uglitzk. Caucasus, Soviet UnionGEN1998COLLECTED07/26/19987 km. southwest of Shuntuk, in the "Horse mound" area.44.41000000, 40.12000000500Trees were 35 to 100 years old. The population area covered about 3 km. Associated species: Cornus mas, Pyrus sylvestris, Crataegus monogyna, Prunus spinosa. Rainfall: 800-1000 mm. annually.Wild materialLeaves and seeds collected. 1563284PI 612375
221PI 612376RUS 98 04-04Malus orientalis Uglitzk. Caucasus, Soviet UnionGEN1998COLLECTED07/26/19987 km. southwest of Shuntuk, in the "Horse mound" area.44.41000000, 40.12000000500Trees were 35 to 100 years old. The population area covered about 3 km. Associated species: Cornus mas, Pyrus sylvestris, Crataegus monogyna, Prunus spinosa. Rainfall: 800-1000 mm. annually.Wild materialLeaves and seeds collected. 1563285PI 612376
222PI 612377RUS 98 04-05Malus orientalis Uglitzk. Caucasus, Soviet UnionGEN1998COLLECTED07/26/19987 km. southwest of Shuntuk, in the "Horse mound" area.44.41000000, 40.12000000500Trees were 35 to 100 years old. The population area covered about 3 km. Associated species: Cornus mas, Pyrus sylvestris, Crataegus monogyna, Prunus spinosa. Rainfall: 800-1000 mm. annually.Wild materialLeaves and seeds collected. 1563286PI 612377
223PI 612378RUS 98 04-06Malus orientalis Uglitzk. Caucasus, Soviet UnionGEN1998COLLECTED07/26/19987 km. southwest of Shuntuk, in the "Horse mound" area.44.41000000, 40.12000000500Trees were 35 to 100 years old. The population area covered about 3 km. Associated species: Cornus mas, Pyrus sylvestris, Crataegus monogyna, Prunus spinosa. Rainfall: 800-1000 mm. annually.Wild materialLeaves and seeds collected. 1563297PI 612378
224PI 612379RUS 98 05-01Malus orientalis Uglitzk. Caucasus, Soviet UnionGEN1998COLLECTED07/26/19983 km. east of Shuntuk, along the Bileyi river with the limestone cliffs on the opposite bank of the river.44.45000000, 40.21000000300Trees were 35 to 80 years old. The population area covered about 1 km. Associated species: Cornus mas, Pyrus sylvestris, Crataegus monogyna, Prunus spinosa. Rainfall: 800-1000 mm. annually.Wild materialLeaves and seeds collected. 1563287PI 612379
225PI 612380RUS 98 05-02Malus orientalis Uglitzk. Caucasus, Soviet UnionGEN1998COLLECTED07/26/19983 km. east of Shuntuk, along the Bileyi river with the limestone cliffs on the opposite bank of the river.44.45000000, 40.21000000300Trees were 35 to 80 years old. The population area covered about 1 km. Associated species: Cornus mas, Pyrus sylvestris, Crataegus monogyna, Prunus spinosa. Rainfall: 800-1000 mm. annually.Wild materialLeaves and seeds collected. 1563288PI 612380
226PI 612381RUS 98 05-03Malus orientalis Uglitzk. Caucasus, Soviet UnionGEN1998COLLECTED07/26/19983 km. east of Shuntuk, along the Bileyi river with the limestone cliffs on the opposite bank of the river.44.45000000, 40.21000000300Trees were 35 to 80 years old. The population area covered about 1 km. Associated species: Cornus mas, Pyrus sylvestris, Crataegus monogyna, Prunus spinosa. Rainfall: 800-1000 mm. annually.Wild materialLeaves and seeds collected. 1563289PI 612381
227PI 612382RUS 98 05-04Malus orientalis Uglitzk. Caucasus, Soviet UnionGEN1998COLLECTED07/26/19983 km. east of Shuntuk, along the Bileyi river with the limestone cliffs on the opposite bank of the river.44.45000000, 40.21000000300Trees were 35 to 80 years old. The population area covered about 1 km. Associated species: Cornus mas, Pyrus sylvestris, Crataegus monogyna, Prunus spinosa. Rainfall: 800-1000 mm. annually.Wild materialLeaves and seeds collected. 1563299PI 612382
228PI 612383RUS 98 05-05Malus orientalis Uglitzk. Caucasus, Soviet UnionGEN1998COLLECTED07/26/19983 km. east of Shuntuk, along the Bileyi river with the limestone cliffs on the opposite bank of the river.44.45000000, 40.21000000300Trees were 35 to 80 years old. The population area covered about 1 km. Associated species: Cornus mas, Pyrus sylvestris, Crataegus monogyna, Prunus spinosa. Rainfall: 800-1000 mm. annually.Wild materialLeaves and seeds collected. 1563290PI 612383
229PI 612384RUS 98 05-06Malus orientalis Uglitzk. Caucasus, Soviet UnionGEN1998COLLECTED07/26/19983 km. east of Shuntuk, along the Bileyi river with the limestone cliffs on the opposite bank of the river.44.45000000, 40.21000000300Trees were 35 to 80 years old. The population area covered about 1 km. Associated species: Cornus mas, Pyrus sylvestris, Crataegus monogyna, Prunus spinosa. Rainfall: 800-1000 mm. annually.Wild materialLeaves and seeds collected. 1563291PI 612384
230PI 612385RUS 98 07-01Malus orientalis Uglitzk. Caucasus, Soviet UnionGEN1998COLLECTED07/27/199825 km. south of Shuntuk, along mountain road.44.23000000, 40.18000000700Associated species: Cornus mas, Pyrus sylvestris, Crataegus monogyna, Prunus spinosa. Rainfall: 800-1000 mm. annually.Wild materialLeaves and seeds collected. 1563292PI 612385
231PI 612386RUS 98 07-02Malus orientalis Uglitzk. Caucasus, Soviet UnionGEN1998COLLECTED07/27/199825 km. south of Shuntuk, along mountain road.44.23000000, 40.18000000700Associated species: Cornus mas, Pyrus sylvestris, Crataegus monogyna, Prunus spinosa. Rainfall: 800-1000 mm. annually.Wild materialLeaves and seeds collected. 1563298PI 612386
232PI 633819RUS 98 02-01Malus orientalis Uglitzk. Caucasus, Soviet UnionGEN1998COLLECTED07/25/19985 km. south of Krymsk, near an ancient Greek village of Alevra.44.92000000, 38.00000000100Slight SE facing slope. The population area covered about 1 km. Associated species: Cornus mas, Pyrus sylvestris, Crataegus monogyna, Prunus spinosa. Rainfall: 640 mm. annuallyWild materialLeaves and seeds collected. 1652470PI 633819
233PI 633821RUS 98 04-02Malus orientalis Uglitzk. Caucasus, Soviet UnionGENFRUIT1998COLLECTED07/26/19987 km. southwest of Shuntuk, in the "Horse mound" area.44.41000000, 40.12000000500Trees were 35 to 100 years old. The population area covered about 3 km. Associated species: Cornus mas, Pyrus sylvestris, Crataegus monogyna, Prunus spinosa. Rainfall: 800-1000 mm. annually.Wild materialLeaves and seeds collected. 1652472PI 633821
234PI 633822RUS 98 05-05Malus orientalis Uglitzk. Caucasus, Soviet UnionGENFRUIT1998COLLECTED07/26/19983 km. east of Shuntuk, along the Bileyi river with the limestone cliffs on the opposite bank of the river.44.45000000, 40.21000000300Trees were 35 to 80 years old. The population area covered about 1 km. Associated species: Cornus mas, Pyrus sylvestris, Crataegus monogyna, Prunus spinosa. Rainfall: 800-1000 mm. annually.Wild materialLeaves and seeds collected. 1652473PI 633822
235PI 633823RUS 98 07-01Malus orientalis Uglitzk. Caucasus, Soviet UnionGENFRUIT1998COLLECTED07/27/199825 km. south of Shuntuk, along mountain road.44.23000000, 40.18000000700Associated species: Cornus mas, Pyrus sylvestris, Crataegus monogyna, Prunus spinosa. Rainfall: 800-1000 mm. annually.Wild materialLeaves and seeds collected. 1652474PI 633823
236PI 666155RUS 98 02-03Malus orientalis Uglitzk. Caucasus, Soviet UnionGEN1998COLLECTED07/25/19985 km. south of Krymsk, near an ancient Greek village of Alevra.44.92000000, 38.00000000100Slight SE facing slope. The population area covered about 1 km. Associated species: Cornus mas, Pyrus sylvestris, Crataegus monogyna, Prunus spinosa. Rainfall: 640 mm. annuallyWild materialLeaves and seeds collected. Ressitant to apple scab and cedar apple rust, susceptible to fire blight.1905467PI 666155
237PI 666156RUS 98 02-04Malus orientalis Uglitzk. Caucasus, Soviet UnionGEN1998COLLECTED07/25/19985 km. south of Krymsk, near an ancient Greek village of Alevra.44.92000000, 38.00000000100Slight SE facing slope. The population area covered about 1 km. Associated species: Cornus mas, Pyrus sylvestris, Crataegus monogyna, Prunus spinosa. Rainfall: 640 mm. annuallyWild materialLeaves and seeds collected.1905468PI 666156
238PI 666157RUS 98 02-06Malus orientalis Uglitzk. Caucasus, Soviet UnionGEN1998COLLECTED07/25/19985 km. south of Krymsk, near an ancient Greek village of Alevra.44.92000000, 38.00000000100Slight SE facing slope. The population area covered about 1 km. Associated species: Cornus mas, Pyrus sylvestris, Crataegus monogyna, Prunus spinosa. Rainfall: 640 mm. annuallyWild materialLeaves and seeds collected. Resistant to fire blight and cedar apple rust. Susceptible to apple scab.1905469PI 666157
239PI 666158RUS 98 03-01Malus orientalis Uglitzk. Caucasus, Soviet UnionGEN1998COLLECTED07/26/19983 km. southwest of Shuntuk, 1 km. from nearest commercial apples.44.43000000, 40.15000000400Slight NW facing slope along the edge of an open field. Trees were 35 to 80 years old. The population covered about 1 km. Associated species: Cornus mas, Pyurs sylvestris, Crataegus monogyna, Prunus spinosa. Rainfall: 800-1000 mm. annually.Wild materialLeaves and seeds collected. Susceptible to fire blight and cedar apple rust. Resistant to apple scab.1905470PI 666158
240PI 666162RUS 98 04-04Malus orientalis Uglitzk. Caucasus, Soviet UnionGEN1998COLLECTED07/26/19987 km. southwest of Shuntuk, in the "Horse mound" area.44.41000000, 40.12000000500Trees were 35 to 100 years old. The population area covered about 3 km. Associated species: Cornus mas, Pyrus sylvestris, Crataegus monogyna, Prunus spinosa. Rainfall: 800-1000 mm. annually.Wild materialLeaves and seeds collected. Susceptible to fire blight and cedar apple rust. Resistant to apple scab.1905474PI 666162
241PI 666163RUS 98 05-01Malus orientalis Uglitzk. Caucasus, Soviet UnionGEN1998COLLECTED07/26/19983 km. east of Shuntuk, along the Bileyi river with the limestone cliffs on the opposite bank of the river.44.45000000, 40.21000000300Trees were 35 to 80 years old. The population area covered about 1 km. Associated species: Cornus mas, Pyrus sylvestris, Crataegus monogyna, Prunus spinosa. Rainfall: 800-1000 mm. annually.Wild materialLeaves and seeds collected. Resistant to P. expansum.1905475PI 666163
242PI 666164RUS 98 05-02Malus orientalis Uglitzk. Caucasus, Soviet UnionGEN1998COLLECTED07/26/19983 km. east of Shuntuk, along the Bileyi river with the limestone cliffs on the opposite bank of the river.44.45000000, 40.21000000300Trees were 35 to 80 years old. The population area covered about 1 km. Associated species: Cornus mas, Pyrus sylvestris, Crataegus monogyna, Prunus spinosa. Rainfall: 800-1000 mm. annually.Wild materialLeaves and seeds collected. Resistant to apple scab and fire blight. Susceptible to cedar apple rust.1905476PI 666164
243PI 666165RUS 98 07-01Malus orientalis Uglitzk. Caucasus, Soviet UnionGEN1998COLLECTED07/27/199825 km. south of Shuntuk, along mountain road.44.23000000, 40.18000000700Associated species: Cornus mas, Pyrus sylvestris, Crataegus monogyna, Prunus spinosa. Rainfall: 800-1000 mm. annually.Wild materialLeaves and seeds collected. Resistant to apple scab, susceptible to cedar apple rust.1905477PI 666165
244PI 682806RUS 98 02-05Malus orientalis Uglitzk. Caucasus, Soviet UnionGEN1998COLLECTED07/25/19985 km. south of Krymsk, near an ancient Greek village of Alevra.44.92000000, 38.00000000100Slight SE facing slope. The population area covered about 1 km. Associated species: Cornus mas, Pyrus sylvestris, Crataegus monogyna, Prunus spinosa. Rainfall: 640 mm. annuallyWild materialLeaves and seeds collected. Susceptible to fire blight and cedar apple rust. Resistant to apple scab.1696118PI 682806
245PI 633807CH97 03-01Malus hupehensis (Pamp.) Rehder Sichuan Sheng, ChinaGEN1997COLLECTED09/21/1997Maerkang County, Dananzugou village. 5 km. northeast of Maerkang.31.95583333, 102.275555562930Aspect-South, partial canopy. Incline <5%, slight south, variable. Landform: Mountain valley. Assoc. sp: Sorbus, Fir, Pine Acer, Cornus, Willow, Betula. Shrub sp: Rosa, Pyracantha, Holly, Berberis, Cotoneaster, Rubus. Herb sp: Aster, Fern.Wild materialAdditional Weather Notes: Rainfall in concentrated from May to Sept. There are spring and summer droughts. Hail and frost damage occur. Additional Habitat Notes: Collection tree nearly defoilated, 5m. in height, located on minimal south facing slope. Name of gorge: Da Nan Zu Gou. Name of village: Cha Bei. Sampled 132 fruits from 23 trees. 1652458PI 633807
246PI 633808CH97 03-02Malus toringoides (Rehder) Hughes Sichuan Sheng, ChinaGENFRUIT1997COLLECTED09/21/1997Maerkang County, Dananzugou village. 5 km. northeast of Maerkang.31.95583333, 102.275555562930Aspect-South, partial canopy. Incline <5%, slight south, variable. Landform: Mountain valley. Assoc. sp: Sorbus, Fir, Pine Acer, Cornus, Willow, Betula. Shrub sp: Rosa, Pyracantha, Holly, Berberis, Cotoneaster, Rubus. Herb sp: Aster, Fern.Wild materialAdditional Weather Notes: Rainfall in concentrated from May to Sept. There are spring and summer droughts. Hail and frost damage occur. Sampled 132 fruits from each of the 23 trees. 1652459PI 633808
247PI 633810CH97 03-20Malus kansuensis (Batalin) C. K. Schneid. Sichuan Sheng, ChinaGEN1997COLLECTED09/21/1997Maerkang County, Dananzugou village. 5 km. northeast of Maerkang.31.94472222, 102.270000002930Aspect-South, partial canopy. Incline <5%, slight south, variable. Landform: Mountain valley. Assoc. sp: Sorbus, Fir, Pine Acer, Cornus, Willow, Betula. Shrub sp: Rosa, Pyracantha, Holly, Berberis, Cotoneaster, Rubus. Herb sp: Aster, Fern.Wild materialAdditional Weather Notes: Rainfall in concentrated from May to Sept. There are spring and summer droughts. Hail and frost damage occur. Additional Habitat Notes: Collection tree 4m. in height with 6 trunks copiced; located on a very rocky hillside. Sampled 132 fruits from 23 trees. Rust present; no scab. 1652461PI 633810
248PI 703093CH97 03-02Malus toringoides (Rehder) Hughes Sichuan Sheng, China Historic1997COLLECTED09/21/1997Maerkang County, Dananzugou village. 5 km. northeast of Maerkang.31.95583333, 102.275555562930Aspect-South, partial canopy. Incline <5%, slight south, variable. Landform: Mountain valley. Assoc. sp: Sorbus, Fir, Pine Acer, Cornus, Willow, Betula. Shrub sp: Rosa, Pyracantha, Holly, Berberis, Cotoneaster, Rubus. Herb sp: Aster, Fern.Wild materialAdditional Weather Notes: Rainfall in concentrated from May to Sept. There are spring and summer droughts. Hail and frost damage occur. Sampled 132 fruits from each of the 23 trees. 1695202PI 703093
249PI 703094CH97 03-02Malus toringoides (Rehder) Hughes Sichuan Sheng, China Historic1997COLLECTED09/21/1997Maerkang County, Dananzugou village. 5 km. northeast of Maerkang.31.95583333, 102.275555562930Aspect-South, partial canopy. Incline <5%, slight south, variable. Landform: Mountain valley. Assoc. sp: Sorbus, Fir, Pine Acer, Cornus, Willow, Betula. Shrub sp: Rosa, Pyracantha, Holly, Berberis, Cotoneaster, Rubus. Herb sp: Aster, Fern.Wild materialAdditional Weather Notes: Rainfall in concentrated from May to Sept. There are spring and summer droughts. Hail and frost damage occur. Sampled 132 fruits from each of the 23 trees. 1695203PI 703094
250PI 703095CH97 03-02Malus toringoides (Rehder) Hughes Sichuan Sheng, China Historic1997COLLECTED09/21/1997Maerkang County, Dananzugou village. 5 km. northeast of Maerkang.31.95583333, 102.275555562930Aspect-South, partial canopy. Incline <5%, slight south, variable. Landform: Mountain valley. Assoc. sp: Sorbus, Fir, Pine Acer, Cornus, Willow, Betula. Shrub sp: Rosa, Pyracantha, Holly, Berberis, Cotoneaster, Rubus. Herb sp: Aster, Fern.Wild materialAdditional Weather Notes: Rainfall in concentrated from May to Sept. There are spring and summer droughts. Hail and frost damage occur. Sampled 132 fruits from each of the 23 trees. 1695205PI 703095
251PI 703096CH97 03-03Malus toringoides (Rehder) Hughes Sichuan Sheng, China Historic1997COLLECTED09/21/1997Maerkang County, Dananzugou village. 5 km. northeast of Maerkang.31.95583333, 102.275555562930Aspect-South, partial canopy. Incline <5%, slight south, variable. Landform: Mountain valley. Assoc. sp: Sorbus, Fir, Pine Acer, Cornus, Willow, Betula. Shrub sp: Rosa, Pyracantha, Holly, Berberis, Cotoneaster, Rubus. Herb sp: Aster, Fern.Wild materialAdditional Weather Notes: Rainfall in concentrated from May to Sept. There are spring and summer droughts. Hail and frost damage occur. Additional Habitat Notes: Collection tree an older tree, 6m. in height, 40cm. diameter, good vigor; located on west facing slope; incline 30%. Sampled 132 fruits from 23 trees. No scab present; quite a lot of of leaf spotting. 1695209PI 703096
252PI 703097CH97 03-03Malus toringoides (Rehder) Hughes Sichuan Sheng, China Historic1997COLLECTED09/21/1997Maerkang County, Dananzugou village. 5 km. northeast of Maerkang.31.95583333, 102.275555562930Aspect-South, partial canopy. Incline <5%, slight south, variable. Landform: Mountain valley. Assoc. sp: Sorbus, Fir, Pine Acer, Cornus, Willow, Betula. Shrub sp: Rosa, Pyracantha, Holly, Berberis, Cotoneaster, Rubus. Herb sp: Aster, Fern.Wild materialAdditional Weather Notes: Rainfall in concentrated from May to Sept. There are spring and summer droughts. Hail and frost damage occur. Additional Habitat Notes: Collection tree an older tree, 6m. in height, 40cm. diameter, good vigor; located on west facing slope; incline 30%. Sampled 132 fruits from 23 trees. No scab present; quite a lot of of leaf spotting. 1695206PI 703097
253PI 703098CH97 03-04Malus toringoides (Rehder) Hughes Sichuan Sheng, China Historic1997COLLECTED09/21/1997Maerkang County, Dananzugou village. 5 km. northeast of Maerkang.31.95583333, 102.275555562930Aspect-South, partial canopy. Incline <5%, slight south, variable. Landform: Mountain valley. Assoc. sp: Sorbus, Fir, Pine Acer, Cornus, Willow, Betula. Shrub sp: Rosa, Pyracantha, Holly, Berberis, Cotoneaster, Rubus. Herb sp: Aster, Fern.Wild materialAdditional Weather Notes: Rainfall in concentrated from May to Sept. There are spring and summer droughts. Hail and frost damage occur. Additional Habitat Notes: Collection tree located on south facing slope, 20% incline. Sampled 132 fruits from 23 trees. 1695210PI 703098
254PI 703099CH97 03-05Malus hupehensis (Pamp.) Rehder Sichuan Sheng, China FRUITHistoric1997COLLECTED09/21/1997Maerkang County, Dananzugou village. 5 km. northeast of Maerkang.31.95583333, 102.275555562920Aspect-South, partial canopy. Incline <5%, slight south, variable. Landform: Mountain valley. Assoc. sp: Sorbus, Fir, Pine Acer, Cornus, Willow, Betula. Shrub sp: Rosa, Pyracantha, Holly, Berberis, Cotoneaster, Rubus. Herb sp: Aster, Fern.Wild materialAdditional Weather Notes: Rainfall in concentrated from May to Sept. There are spring and summer droughts. Hail and frost damage occur. Sampled 132 fruits from each of the 23 trees. Collection tree 15cm. in diameter. Fruit shows heavy disease. leaves are lanceolate. 1695218PI 703099
255PI 703100CH97 03-16Malus kansuensis (Batalin) C. K. Schneid. Sichuan Sheng, China Historic1997COLLECTED09/21/1997Maerkang County, Dananzugou village. 5 km. northeast of Maerkang.31.94472222, 102.270000002880Aspect-South, partial canopy. Incline <5%, slight south, variable. Landform: Mountain valley. Assoc. sp: Sorbus, Fir, Pine Acer, Cornus, Willow, Betula. Shrub sp: Rosa, Pyracantha, Holly, Berberis, Cotoneaster, Rubus. Herb sp: Aster, Fern.Wild materialAdditional Weather Notes: Rainfall in concentrated from May to Sept. There are spring and summer droughts. Hail and frost damage occur. Additional Habitat Notes: Collection tree 3m. in height, moderate vigor; located on a rocky river bank. Sampled 132 fruits from 23 trees. Leaf rust present. No scab. 1695245PI 703100
256PI 703101CH97 03-19Malus toringoides (Rehder) Hughes Sichuan Sheng, China Historic1997COLLECTED09/21/1997Maerkang County, Dananzugou village. 5 km. northeast of Maerkang.31.94472222, 102.270000002930Aspect-South, partial canopy. Incline <5%, slight south, variable. Landform: Mountain valley. Assoc. sp: Sorbus, Fir, Pine Acer, Cornus, Willow, Betula. Shrub sp: Rosa, Pyracantha, Holly, Berberis, Cotoneaster, Rubus. Herb sp: Aster, Fern.Wild materialAdditional Weather Notes: Rainfall in concentrated from May to Sept. There are spring and summer droughts. Hail and frost damage occur. Additional Habitat Notes: Collection tree older, 12m. in height, 40cm. diameter, 3 trunks, moderate vigor; located on a very rocky slope, near Acer and Holly. Sampled 132 fruits from 23 trees. Rust and leaf spotting present; no scab. 1695248PI 703101
257PI 635979BJG122Sorbus aucuparia L. subsp. pohuashanensis (Hance) McAll. Beijing Shi, ChinaNA1997COLLECTED09/25/1994Mentougou District: Baihua Shan Forest Preserve, Da Mu Chang (Big Trunk Field).39.83111000, 115.589170001690Growing on north facing slope in full sun in association with Syringa sp., Corylus mandshurica, Acer truncatum, Populus davidana, Betula davurica, Aquilegia sp., Lespedeza bicolor, Rhododendron mucronulatum and Cornus bretschneideriWild material1544556PI 635979
258PI 606511R. spectabilis KHCW 96-09-03Rubus spectabilis Pursh Alaska, United StatesCOR1996COLLECTED07/31/1996McKinley Lake Trail between 1 to 2.5 miles up from Copper River Road.60.45194000, -145.2033300052Along trail edge.Wild materialUSDA Plant Exploration Expedition, 1996. Associated plants: Cornus, Devil's Club, Rusty Menziesii, Lycopodium, Foam flower, Braken Fern.1536579PI 606511
259PI 613679V. uliginosum KHCW 96-04-01Vaccinium uliginosum L. Alaska, United StatesCOR1996COLLECTED07/30/1996Whitshed Road Extended, about 8 miles southwest of Cordova60.49139000, -145.8705600010Exposured Peat bog, a few scattered scrub spruce. Associated plants: Vaccinium uliginosum, Spiranthes romanzoa, Carex, Vaccinium oxycoccus, V. vitis-idaea, Rubus spectabilis, Drosera rotundifolia, Cornus canadensis, Salix and Alnus.Wild materialUSDA Sponsored plant collecting expedition, 1996. Typical Fragaria chiloensis subsp. pacifica with spreading hairs on pedioles. Fruit past ripe on 29 August 1996. One flower in bloom.1536523PI 613679
260PI 613680V. vitis-idaea KHCW 96-04-02Vaccinium vitis-idaea L. Alaska, United StatesCORImage1996COLLECTED07/30/1996Whitshed Road Extended, about 8 miles southwest of Cordova60.49139000, -145.8705600010Exposured Peat bog, a few scattered scrub spruce. Associated plants: Vaccinium uliginosum, Spiranthes romanzoa, Carex, Vaccinium oxycoccus, V. vitis-idaea, Rubus spectabilis, Drosera rotundifolia, Cornus canadensis, Salix and Alnus.Wild materialUSDA Sponsored plant collecting expedition, 1996.1536524PI 613680
261PI 613683V. ovalifolium KHCW 96-09-01Vaccinium ovalifolium Sm. Alaska, United StatesCOR1996COLLECTED07/31/1996McKinley Cabin Lake Trail about 1 mile north of Copper River Road towards McKinley Lake.60.45200000, -145.2033000052Pants growing on either side of the trail in shade. Associated plants: Cornus, Echinopanax, Menziesia, Tsuga mertensiana, Picea sitchensis, Lycopodium annotinum, foam flower and Dryopteris dilatata.Wild materialUSDA Sponsored plant collecting expedition, 1996.1536527PI 613683
262PI 613684V. ovalifolium KHCW 96-09-02Vaccinium ovalifolium Sm. Alaska, United StatesCOR1996COLLECTED07/30/1996McKinley Cabin Lake Trail about 1 mile north of Copper River Road towards McKinley Lake60.45200000, -145.2033000052Shaded by hemlock and spruce. Associated plants: Cornus, Echinopanax, Menziesia, Tsuga mertensiana, Picea sitchensis , Lycopodium annotinum, foam flower and Dryopteris dilatata.Wild materialUSDA Sponsored plant collecting expedition, 1996.1536528PI 613684
263PI 613685V. ovalifolium KHCW 96-09-06Vaccinium ovalifolium Sm. Alaska, United StatesCOR1996COLLECTED07/30/1996McKinley Cabin Lake Trail about 1 mile north of Copper River Road towards McKinley Lake. Pants growing about halfway to lake.60.45200000, -145.2033000052Shaded by hemlock and spruce. Associated plants: Cornus, Echinopanax, Menziesia, Tsuga mertensiana, Picea sitchensis , Lycopodium annotinum, foam flower and Dryopteris dilatata.Wild materialUSDA Sponsored plant collecting expedition, 1996.1536529PI 613685
264PI 613687V. vitis-idaea Muskeeg KHCW 96-12-01AVaccinium vitis-idaea L. Alaska, United StatesCORImage1996COLLECTED07/31/1996About 0.5 mile from Copper River Road on Muskeeg Meander Trail.60.49816000, -145.4673300045Associated plants:Salix alaxensis, Picea sitchensis, Festuca Rubus spectabilis, Cornus canadensis, Gentian, Epilobium angustifolium.Wild materialUSDA Sponsored plant collecting expedition, 1996.1536531PI 613687
265PI 613695V. vitis-idaea KHCW 96-21-01Vaccinium vitis-idaea L. Alaska, United StatesCOR1996COLLECTED08/03/1996Pillar Mountain, about 5 miles west of Kodiak, Kodiak Island.57.78867000, -152.43610000367Boggy basins at the top of mountain. Associated plants: Empetrum nigrum, Aconitum delphinifolium Epilobium angustifolium, Campanula, Polygonum, Aquillea Cornus canadiensis, Geranium, Solidago, Potentilla villosa.Wild materialUSDA Sponsored plant collecting expedition, 1996.1536539PI 613695
266PI 617856R. bracteosum KHCW 96-09-05Ribes bracteosum Douglas Alaska, United StatesCOR1996COLLECTED07/30/1996McKinley Cabin Trail to McKinley Lake about 2 miles from Copper River Road.60.46666667, -145.2000000030By stream, open edge of trail.Wild materialUSDA Sponsored plant collecting expedition, 1996. Associated plants: Cornus canadensis, Sanguisorba, Alnus, Arunkus, Pyrola, Potentilla Alnus, Tsuga mertensiana, Picea sitchensis, Lycopodium annotinum Dryopteris dilatata, Menziesia ferruginea1536487PI 617856
267PI 617858R. hudsonianum KHCW 96-14-02Ribes hudsonianum Richardson Alaska, United StatesCOR1996COLLECTED07/30/1996McKinley Cabin Trail to McKinley Lake about 2 miles from Copper River Road.60.46666667, -145.2000000030By stream, open edge of trail.Wild materialUSDA Sponsored plant collecting expedition, 1996. Associated plants: Cornus, Sanguisorba, Alnus, Tsuga Arunkus, Pyrola, Potentilla1536489PI 617858
268PI 617748R. cereum LIG-21Ribes cereum Douglas Washington, United StatesCOR1993COLLECTED08/12/199348.50000000, -120.500000001020T36N R20E Sec. 20 & 19; Okanogan Nat'l Forest, from FR 52 then west on FR 5225 approx. 1.6 km.Wild materialVery dry, overgrazed. Found near dry creekbed along with Cornus spp.1482812PI 617748
269PI 638760V. arboreumVaccinium arboreum Marshall Missouri, United StatesCOR1993COLLECTED10/1992T36N, R2E, Sec 9, E 1/2 (along east side of road) Site just north of Belgrade, Missouri, Washington County.37.00000000, -90.000000000As understory plants with Vaccinium stamineum and V. vacillans. Cornus florida present as understory tree. Highly orgnaic duff layer. Plants straggly and not in their prime due to poor light penetration.Wild materialFruits ripen at this site from late August until a hard freeze. Green fruits have been seen late October. Plants show only shrub habit. Fruiting plants typically approximately 1.2 m tall. Foliage glossy and dark green. Fruit glossy and black, about 0.6 cm in diameter. No visible winter injury or insect damage. Minimal disease problems: Ophiodothella spp., which doesn't appear to affect the plant; some fruit appeared to have mummyberry (Monilinia spp.). For best germination of dry seed, Ballington (NC State) and Lyrene (U. of Florida) suggest soaking the seeds for 24 hrs. in 500ppm GA4+7 prior to germination.1011314PI 638760
270PI 606455R. corchorifolius MT 92116Rubus corchorifolius L. f. Guizhou Sheng, ChinaCORImage1992COLLECTED05/31/1992Leigong Mt. Nature Preserve, Leishan County Road to Maoping26.40000000, 108.250000002000cool, subtropical, mountainous vegetation, mostly shrubby with scattered large trees , with Pinus massoniana, Prunus, Cornus, Acer, Salix,Wild materialAdditional information is forthcoming1015152PI 606455
271PI 650012Ames 10808Helianthus microcephalus Torr. & A. Gray Indiana, United StatesNC71989COLLECTED09/21/19891 mile NNE of I64 and Indiana 135 interchange. Corydon, Harrison Co., Indiana.38.25000000, -86.13333333206Growing on edge of black oak forest in acidic forest loam with Cornus florida, Nyssa sylvatica and Toxicodendron radicans.Wild material5 plants in the population, sample size was 18 seed, okay maturity, and no disease or insect damage.1053651PI 650012
272PI 589766GMAL 2367Malus angustifolia (Aiton) Michx. Virginia, United StatesGEN1987COLLECTED08/27/1987Virginia, Shenandoah Co. 5.4 mi SE of junction US 11 and Co. 675 on Co. 675 at W. corner of unmarked dirt Rd to the W.Comments: 20 ft. tall, 6 cm diameter. Population of 6 large trees and 20+ smaller trees. Ostoya Virginia, Cornus, Pinus virginiana, Carya, Ovata, Carya cordiformis, Quercus.1019975PI 589766
273PI 495622 .d25Vitis riparia Michx. Nebraska, United StatesGEN1984COLLECTED09/23/1984Langdon Quadrant, Indian Cave State Park, Richardson County (T3N R17E sec 5, west edge of southwest quarter), Nebraska290Wild materialVine on Cornus, Ulmus, Acer, and Juglans. Fruit sweet. Heavily fruiting; free of disease. 1691655PI 495622 .d
274PI 495622 .e25Vitis riparia Michx. Nebraska, United StatesGEN1984COLLECTED09/23/1984Langdon Quadrant, Indian Cave State Park, Richardson County (T3N R17E sec 5, west edge of southwest quarter), Nebraska290Wild materialVine on Cornus, Ulmus, Acer, and Juglans. Fruit sweet. Heavily fruiting; free of disease. 1691656PI 495622 .e
275PI 495622 .f25Vitis riparia Michx. Nebraska, United StatesGEN1984COLLECTED09/23/1984Langdon Quadrant, Indian Cave State Park, Richardson County (T3N R17E sec 5, west edge of southwest quarter), Nebraska290Wild materialVine on Cornus, Ulmus, Acer, and Juglans. Fruit sweet. Heavily fruiting; free of disease. 1691652PI 495622 .f
276PI 495622 .i25Vitis riparia Michx. Nebraska, United StatesGEN1984COLLECTED09/23/1984Langdon Quadrant, Indian Cave State Park, Richardson County (T3N R17E sec 5, west edge of southwest quarter), Nebraska290Wild materialVine on Cornus, Ulmus, Acer, and Juglans. Fruit sweet. Heavily fruiting; free of disease. 1691657PI 495622 .i
277PI 495622 .v25Vitis riparia Michx. Nebraska, United StatesGEN1984COLLECTED09/23/1984Langdon Quadrant, Indian Cave State Park, Richardson County (T3N R17E sec 5, west edge of southwest quarter), Nebraska290Wild materialVine on Cornus, Ulmus, Acer, and Juglans. Fruit sweet. Heavily fruiting; free of disease. 1691670PI 495622 .v
278PI 49561518Quercus muehlenbergii Engelm. Nebraska, United StatesNC7PLANT1984COLLECTED09/23/1984Indian Cave State Park, T4N R16E Sec. 36 and T3N R17E NW 1/4 Sec. 6, Nemaha County.40.25376700, -95.55209100326Growing in association with an understory of Cornus, Asimina triloba, and Fraxinus.Wild materialPlants wide to 10 meters tall. Large trees approximately 2 feet in diameter and 40-45 feet in height.1390551PI 495615
279PI 495616Climbing RoseRosa setigera Michx. Nebraska, United StatesNA1984COLLECTED09/23/1984Indian Cave State Park (T4N R16E Sec 36)40.26190900, -95.56702400339In association with Rhus, Cornus, and Quercus borealis.Wild materialPlant shaped fountain-like, to 1 meter tall. Perennial woody.1390552PI 495616
280PI 49561921Staphylea trifolia L. Nebraska, United StatesNC7SEED1984COLLECTED09/23/1984Indian Cave State Park, T3N R17E NE 1/4 of NW 1/4 of Section 9, Richardson County40.24527778, -95.51527778265Base of bluff. Population of approximately 10Wild materialPlants to 3 meters tall. Heavy seed production.1390555PI 495619
281Ames 38800Camp MitigwaAmelanchier arborea (F. Michx.) Fernald Iowa, United StatesNC7FRUIT2026COLLECTED06/01/2026Mitigwa Scout Camp located on west side of Des Moines River watershed approximately 7.50 miles south, southwest of Boone, T82N R26W N 1/4 Sec. 5 and T83N R26W S 1/4 Sec. 32.41.94894500, -93.90537200310High-quality white oak - ironwood, mature woods.Wild materialThe native range of Amelanchier arborea is concentrated in the eastern half of the U.S. (Little, 1977). This accession represents a collection of A. arborea germplasm from the western edge of the species native range, specifically central Iowa. Specimens sampled at the collection site in nature were small to medium understory or woodland edge single and/or multi-trunked trees with a few trees getting close to being deemed as canopy specimens. Bark smooth and light grey in color. Specimens sampled in nature ranging 15-50' in height. Peak flowering occurred on 8 April 2026 with white flowers appearing prior to leaf expansion. Fall colors ranging from orange to orange-red peaking typically at the end of September (central Iowa). Fruits, dark-pink to red, maturing in early June (peak in 2026 occurred on 2 June) averaging 8 mm in diameter, except for mother tree #6 that had rather large fruits at 11 mm in diameter. 2197049Ames 38800
282Ames 36705State Line FenAgastache scrophulariifolia (Willd.) Kuntze Missouri, United StatesNC7INFLORESCENCE2025COLLECTED10/17/2025State Line Fen just east of the Chariton River approximately 2.75 miles west of Coatsville just south of the Missouri/Iowa border, T67N R16W SW 1/4 Sec. 2240.58924000, -92.68834100257Moist, mucky soils. Degraded fen near small creek.Wild materialPurple Giant Hyssop is a tall (e.g. up to 6') perennial forb native to the northeastern US. Blooms extend for several weeks in the fall typically August through September and are visited by many pollinators. This accession was collected in northern Missouri and thus represents genetics from the southwestern edge of the species native range. At the collection site, most specimens had white blooms, while some showed light lavender coloration with plants averaging 4.5-5.5' in height. In Missouri, the Natural Heritage Program currently tracks this species ranked as an S1 (Critically imperiled in the state because of extreme rarity or because of some factor(s) such as very steep declines making it especially vulnerable to extirpation from the state.) and has been documented in only six Missouri counties including Adair, Atchison, Clark, Harrison, Schuyler, and Worth. 2192996Ames 36705
283W6 62518FWS0300-108Anaphalis margaritacea (L.) Benth. & Hook. f. Michigan, United StatesW6SEED2025Wild material2192216W6 62518
284W6 62523FWS0300-116Doellingeria umbellata (Mill.) Nees Michigan, United StatesW6SEED2025Wild materialPoison sumac present2192221W6 62523
285W6 62525FWS0300-125Lysimachia quadriflora Sims Michigan, United StatesW6SEED2025Wild material2192223W6 62525
286W6 62531FWS0300-137Eutrochium maculatum (L.) E. E. Lamont Michigan, United StatesW6SEED2025Wild materialThe above acreage and population size are for the dense patch near the gate, including the portion of the patch not on sanctuary property.2192229W6 62531
287W6 62533FWS0300-143Helenium autumnale L. Michigan, United StatesW6SEED2025Wild materialThe vegetative part of the population is likely dormant, though it is not possible to discern dormant individuals. Consequently, the above population size may be an underestimate.2192231W6 62533
288W6 62534FWS0300-144Solidago riddellii Frank Michigan, United StatesW6SEED2025Wild materialThe vegetative part of the population is likely dormant, though it is not possible to discern dormant individuals. Consequently, the above population size may be an underestimate.2192232W6 62534
289W6 62535FWS0300-145Verbena hastata L. Michigan, United StatesW6SEED2025Wild material2192233W6 62535
290W6 62550FWS0502-102Eutrochium fistulosum (Barratt) E. E. Lamont Pennsylvania, United StatesW6SEED2025Wild materialStem hollow at base2192248W6 62550
291W6 62559FWS0502-94Epilobium ciliatum Raf. Pennsylvania, United StatesW6SEED2025Wild materialSeeds mostly ripe in reddish pods, before they split2192257W6 62559
292NA 89115TLM25-04aHamamelis ovalis S. W. Leonard Texas, United StatesNA2025COLLECTED07/10/2025State 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, -93.72628100138The 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 material2191654NA 89115
293WLP 3658TRx250704-01NYLonicera morrowii A. Gray New York, United StatesNA2025COLLECTED07/04/202543.31284000, -78.49509400Edge of disturbed forestWild material2191634WLP 3658
294NA 89051AFGN25-01Hydrangea barbara (L.) Bernd Schulz Alabama, United StatesNA2025COLLECTED05/31/2025Ebeneezer Swamp Ecological Preserve.33.16818000, -86.81243000148Swamp forest with slow moving water. Dominant canopy consisted of Nyssa aquatica, Magnolia virginiana, and Acer rubrum.Wild material2191418NA 89051
295NA 89070AFGN25-16Rubus odoratus L. North Carolina, United StatesNA2025COLLECTED06/03/2025Ball Creek Rd (83).35.03127000, -83.457860001334Mixed mesophytic Appalachian forest.Wild material2191433NA 89070
296Ames 36305Cook/St. Louis CountiesSalix pellita Andersson Minnesota, United StatesNC7LEAF2025Wild materialSatiny willow is a tall shrub that reaches its southern limits across the extreme northern and northeastern portions of the U.S. Plants can reach 4-5 meters in height and are identified by typically dense hairs on the lower surface of leaves that are straight and lie flat. Dormant twigs are noticeably yellowish. Leaf morphology is similar to that of S. candida and S. petiolaris. Satiny willow in nature tends to be restricted to wet habitats such as riverbanks and shorelines and its presence quickly disappates the greater the distance away from open/available surface water. This accession represents genetics from the northeastern portion of Minnesota. Satiny willow is tracked (listed Threatened in 2013) by the Minnesota Department of Natural Resources and has only been documented in three Minnesota counties in the extreme northeast corner of the state. After years of targeted surveys, only eight populations have been documented since 1996. 2172670Ames 36305
297NA 88748SOKO2024-001Viburnum dilatatum Thunb. Gangwon-do, Korea, SouthNA2025COLLECTED09/19/2024Yeongwol-gun: Yeongheung-ri: Jangneung Mulmurigol Marsh.37.20005000, 128.44996000244Boardwalk separating woodland edge and marsh in 50 percent shade. Organic soil [locally known for calcareous soils]. Slope: 5 to 10 degrees. Aspect: South-southwest.Wild material2172323NA 88748
298NA 8892924Flam8Rhododendron hybr.Georgia, United StatesNA2025COLLECTED09/09/2024Smyrna, GA: private residence.33.84871000, -84.51773000303Dry slope in backyard of residence, primarily open with some large oaks. Open conditions. Slope: 30 degrees. Aspect: Northwest.Wild material2172812NA 88929
299NA 8893024Flam16Rhododendron canescens (Michx.) Sweet Georgia, United StatesNA2025COLLECTED09/10/2024DeKalb County: Stone Mountain: Stone Mountain Park: slope near Robert E. Lee Boulevard.33.80238000, -84.15508000286Dry, shady slope. Growing in 3/4 shade. Slope: 30 to 45 degrees. Aspect: West-southwest.Wild materialNote: Seeds from three different plants collected at the same spot were bulked together in this accession; the lowest field collection number (24Flam16) has been chosen as the primary for this record. It appears from the notes that the identity is slightly uncertain; possibly not pure R. canescens.2172813NA 88930
300NA 89095SNR2024Ilex decidua Walter Missouri, United StatesNA2024COLLECTED12/03/2024Shaw Nature Reserve: near Shaw Nature Reserve's Trail House.38.46697200, -90.81925000Upland site.Wild material2169943NA 89095
301NA 885832024RJLFL-014Ilex amelanchier M. A. Curtis ex Chapm. Florida, United StatesNA2024COLLECTED11/13/2024Yellow 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, -86.5921850023Plants 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 material2169920NA 88583
302NA 885882024RM-001Hydrangea radiata Walter Georgia, United StatesNA2024COLLECTED10/24/2024Chattahoochee National Forest: Warwoman Wildlife Management Area: north side of Overflow Creek Road just west of the bridge over the Chattooga River.34.94956600, -83.20652000498Mixed evergreen and deciduous moist mesic forest in part shade. The underlying geology of this area is characterized as Metagraywacke/Mica Schist Formation of the Precambrian-Paleozoic period. (Source: USGS Georgia Geologic Map Data). The soils of this are characterized as Tusquitee Series Loam, 10 to 25 percent slopes. The Tusquitee Series consists of very deep, well drained soils on gently sloping to very steep benches, foot slopes, toe slopes, and fans in coves in the Southern Blue Ridge mountains, MLRA 130B. These soils formed in colluvium derived from materials weathered from igneous and high-grade metamorphic crystalline rocks such as granite, mica gneiss, hornblende gneiss, and schist. Slope ranges from 2 to 95 percent. Solum thickness ranges from 1 to 3+ meters. Reaction is very strongly acid to slightly acid, in the A horizon. The Bw and lower horizons are very strongly acid to moderately acid. In the upper 1 meter, content of rock fragments, dominantly of gravel to stone size, ranges up to 35 percent. Below 1 meter, rock fragment content may range up to 60 percent. Content of mica flakes ranges from few to common. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions).Wild material2169925NA 88588
303NA 885902024RM-003Ilex verticillata (L.) A. Gray Florida, United StatesNA2024COLLECTED11/21/2024Along the west/north side of the Yellow River about 0.33 kilometers (as the crow flies) upstream from the channel that leads the Fisher Old Mill Road Boat Ramp. This site was accessed by boat.30.62868600, -86.807480004Plants are found growing primarily in permanently saturated to submersed conditions along the edge of the Yellow River in part shade. The riverine habitat is comprised of a wide array of deciduous and evergreen trees, shrubs, and perennial plant species. Most of the plants along the river are adapted to acidic conditions and, while the aquatic habitat is generally fresh water, there is occasionally tidal or hurricane-caused saltwater intrusions. Slope: 0 percent. Aspect: East-southeast. The underlying geology of this area is characterized as Alluvium from undifferentiated Quaternary Sediments. Much of Florida's surface is covered by a varying thickness of undifferentiated sediments consisting of siliciclastics, organics and freshwater carbonates. Where these sediments exceed 20 feet (6.1 meters) thick, they were mapped as discrete units. To subdivide the undifferentiated sediments, those sediments occurring in flood plains were mapped as alluvial and flood plain deposits (Qal). Sediments showing surficial expression of beach ridges and dunes were mapped separately (Qbd) as were the sediments composing Trail Ridge (Qtr). Terrace sands were not mapped (refer to Healy [1975] for a discussion of the terraces in Florida). The subdivisions of the Undifferentiated Quaternary Sediments (Qu) are not lithostratigraphic units but are utilized to facilitate a better understanding of the State's geology. The siliciclastics are light gray, tan, brown to black, unconsolidated to poorly consolidated, clean to clayey, silty, unfossiliferous, variably organic-bearing sands to blue green to olive green, poorly to moderately consolidated, sandy, silty clays. Gravel is occasionally present in the panhandle. Organics occur as plant debris, roots, disseminated organic matrix and beds of peat. Freshwater carbonates, often referred to as marls in the literature, are scattered over much of the State. In southern Florida, freshwater carbonates are nearly ubiquitous in the Everglades. These sediments are buff colored to tan, unconsolidated to poorly consolidated, fossiliferous carbonate muds. Sand, silt and clay may be present in limited quantities. These carbonates often contain organics. The dominant fossils in the freshwater carbonates are mollusks. (Source: USGS Florida Geologic Map Data). The soils of this are characterized as Bibb-Kinston Series association. The Bibb Series 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. Reaction ranges from extremely acid to strongly acid throughout. Content of mica flakes ranges from none to common. Content of rounded gravel typically ranges from 0 to 10 percent throughout, but may range to 50 percent in thin strata below a depth of 1 meter. Buried soil horizons, present in many pedons have the same range in color and texture as the surface horizon which has iron and organic matter concentrations in shades of brown and yellow ranging from none to common. Texture is sand, loamy sand, loamy fine sand, fine sandy loam, sandy loam, loam or silt loam. The Kinston Series consists of very deep, poorly drained, moderately permeable soils found on flood plains. They were formed in alluvial depositions. Slopes range from 0 to 2 percent. Soil reaction ranges from strongly acid to very strongly acid. Typical texture across the pedons is loamy, gravelly loam, sandy loam, and clay loam with dark concretions often present. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions).Wild material2169927NA 88590
304NA 885912024RM-004Ilex opaca Aiton Florida, United StatesNA2024COLLECTED11/21/2024Along the west/north side of the Yellow River about 5.5 kilometers upstream from the State Highway 87 boat ramp. This site was accessed by boat.30.59986000, -86.879360002Plants are found growing primarily in permanently saturated to submersed conditions along the edge of the Yellow River in part shade. The riverine habitat is comprised of a wide array of deciduous and evergreen trees, shrubs, and perennial plant species. Most of the plants along the river are adapted to acidic conditions and, while the aquatic habitat is generally fresh water, there is occasionally tidal or hurricane-caused saltwater intrusions. Slope: 0 percent. Aspect: East-southeast. The underlying geology of this area is characterized as Alluvium from undifferentiated Quaternary Sediments. Much of Florida's surface is covered by a varying thickness of undifferentiated sediments consisting of siliciclastics, organics and freshwater carbonates. Where these sediments exceed 20 feet (6.1 meters) thick, they were mapped as discrete units. To subdivide the undifferentiated sediments, those sediments occurring in flood plains were mapped as alluvial and flood plain deposits (Qal). Sediments showing surficial expression of beach ridges and dunes were mapped separately (Qbd) as were the sediments composing Trail Ridge (Qtr). Terrace sands were not mapped (refer to Healy [1975] for a discussion of the terraces in Florida). The subdivisions of the Undifferentiated Quaternary Sediments (Qu) are not lithostratigraphic units but are utilized to facilitate a better understanding of the State's geology. The siliciclastics are light gray, tan, brown to black, unconsolidated to poorly consolidated, clean to clayey, silty, unfossiliferous, variably organic-bearing sands to blue green to olive green, poorly to moderately consolidated, sandy, silty clays. Gravel is occasionally present in the panhandle. Organics occur as plant debris, roots, disseminated organic matrix and beds of peat. Freshwater carbonates, often referred to as marls in the literature, are scattered over much of the State. In southern Florida, freshwater carbonates are nearly ubiquitous in the Everglades. These sediments are buff colored to tan, unconsolidated to poorly consolidated, fossiliferous carbonate muds. Sand, silt and clay may be present in limited quantities. These carbonates often contain organics. The dominant fossils in the freshwater carbonates are mollusks. (Source: USGS Florida Geologic Map Data). The soils of this are characterized as Bibb-Kinston Series association. The Bibb Series 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. Reaction ranges from extremely acid to strongly acid throughout. Content of mica flakes ranges from none to common. Content of rounded gravel typically ranges from 0 to 10 percent throughout, but may range to 50 percent in thin strata below a depth of 1 meter. Buried soil horizons, present in many pedons have the same range in color and texture as the surface horizon which has iron and organic matter concentrations in shades of brown and yellow ranging from none to common. Texture is sand, loamy sand, loamy fine sand, fine sandy loam, sandy loam, loam or silt loam. The Kinston Series consists of very deep, poorly drained, moderately permeable soils found on flood plains. They were formed in alluvial depositions. Slopes range from 0 to 2 percent. Soil reaction ranges from strongly acid to very strongly acid. Typical texture across the pedons is loamy, gravelly loam, sandy loam, and clay loam with dark concretions often present. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions).Wild material2169928NA 88591
305NA 885922024RM-005Ilex sp.Florida, United StatesNA2024COLLECTED11/21/2024Along the west/north side of the Yellow River about 1.1 kilometers upstream from the State Highway 87 boat ramp. This site was accessed by boat.30.57956000, -86.919164001Plants are found growing primarily in permanently saturated to submersed conditions along the edge of the Yellow River in part shade. The riverine habitat is comprised of a wide array of deciduous and evergreen trees, shrubs, and perennial plant species. Most of the plants along the river are adapted to acidic conditions and, while the aquatic habitat is generally fresh water, there is occasionally tidal or hurricane-caused saltwater intrusions. Slope: 0 percent. Aspect: North. The underlying geology of this area is characterized as Alluvium from undifferentiated Quaternary Sediments. Much of Florida's surface is covered by a varying thickness of undifferentiated sediments consisting of siliciclastics, organics and freshwater carbonates. Where these sediments exceed 20 feet (6.1 meters) thick, they were mapped as discrete units. To subdivide the undifferentiated sediments, those sediments occurring in flood plains were mapped as alluvial and flood plain deposits (Qal). Sediments showing surficial expression of beach ridges and dunes were mapped separately (Qbd) as were the sediments composing Trail Ridge (Qtr). Terrace sands were not mapped (refer to Healy [1975] for a discussion of the terraces in Florida). The subdivisions of the Undifferentiated Quaternary Sediments (Qu) are not lithostratigraphic units but are utilized to facilitate a better understanding of the State's geology. The siliciclastics are light gray, tan, brown to black, unconsolidated to poorly consolidated, clean to clayey, silty, unfossiliferous, variably organic-bearing sands to blue green to olive green, poorly to moderately consolidated, sandy, silty clays. Gravel is occasionally present in the panhandle. Organics occur as plant debris, roots, disseminated organic matrix and beds of peat. Freshwater carbonates, often referred to as marls in the literature, are scattered over much of the State. In southern Florida, freshwater carbonates are nearly ubiquitous in the Everglades. These sediments are buff colored to tan, unconsolidated to poorly consolidated, fossiliferous carbonate muds. Sand, silt and clay may be present in limited quantities. These carbonates often contain organics. The dominant fossils in the freshwater carbonates are mollusks. (Source: USGS Florida Geologic Map Data). The soils of this are characterized as Bibb-Kinston Series association. The Bibb Series 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. Reaction ranges from extremely acid to strongly acid throughout. Content of mica flakes ranges from none to common. Content of rounded gravel typically ranges from 0 to 10 percent throughout, but may range to 50 percent in thin strata below a depth of 1 meter. Buried soil horizons, present in many pedons have the same range in color and texture as the surface horizon which has iron and organic matter concentrations in shades of brown and yellow ranging from none to common. Texture is sand, loamy sand, loamy fine sand, fine sandy loam, sandy loam, loam or silt loam. The Kinston Series consists of very deep, poorly drained, moderately permeable soils found on flood plains. They were formed in alluvial depositions. Slopes range from 0 to 2 percent. Soil reaction ranges from strongly acid to very strongly acid. Typical texture across the pedons is loamy, gravelly loam, sandy loam, and clay loam with dark concretions often present. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions).Wild material2169929NA 88592
306NA 88479TXWL2024-029Ilex longipes Chapm. ex Trel. Texas, United StatesNA2024COLLECTED11/20/2024Little Cow Creek.31.06221000, -93.79603000Upland position above perennial creek.Wild material2169906NA 88479
307NA 890772024RJLPA-003Viburnum acerifolium L. Pennsylvania, United StatesNA2024COLLECTED09/19/2024Birdell Road, near parking lot to trail where the road ends at Chambers Lake, which is part of Hibernia County Park.40.03559500, -75.85708600187Plants are growing in deep shade of a dry deciduous forest dominated by Fagus grandifolia. Slope: 0 percent. Aspect: N/A. Geology: The underlying geology of this area is of Precambrian origin and characterized as Banded Mafic Gneiss. It is characterized as dark and fine to medium grained. This formation includes rocks of probable sedimentary origin; may be equivalent to "PZmgh." (Source: USGS Pennsylvania Geologic Map Data). Soils: The primary soil type in the area of this collection is classified as Neshaminy Series Silt Loam, very deep over mafic gneiss, 3 to 8 percent slopes (NvB). (Source: USDA-NRCS Official Soil Series Descriptions). EPA Ecoregion (Level III): Northern Piedmont (64). EPA Ecoregion (Level IV): Piedmont Uplands (64c).Wild material2169041NA 89077
308NA 890792024RJLPA-005Viburnum prunifolium L. Pennsylvania, United StatesNA2024COLLECTED09/20/2024Along gated road about 0.33 kilometers southwest of the Lake Ontelaunee Trail parking lot.40.50062600, -75.8900490094Plants are growing on moist, well-drained in part shade of a deciduous forest. Slope: 0 percent. Aspect: N/A. Geology: The underlying geology of this area is of Ordovician origin and characterized as Shale and graywacke of Hamburg sequence. It is characterized by shale containing zones of conspicuous graywacke. (Source: USGS Pennsylvania Geologic Map Data). Soils: The primary soil type in the area of this collection is classified as Holly Series Silt Loam (Ho). The Holly Series consists of very deep, very poorly and poorly drained soils formed in loamy alluvium on flood plains. Saturated hydraulic conductivity is moderately high through high in the mineral soil. Slope ranges from 0 through 3 percent. (Source: USDA-NRCS Official Soil Series Descriptions). EPA Ecoregion (Level III): Ridge and Valley (67). EPA Ecoregion (Level IV): Northern Shale Valleys (67b).Wild material2169043NA 89079
309NA 890802024RJLPA-006Ilex montana Torr. & A. Gray Pennsylvania, United StatesNA2024COLLECTED09/20/2024Berks and Schuylkill Counties: Hawk Mountain Sanctuary.40.64162200, -75.99122600418Plants are growing from shade to full sun on a dry-mesic to very dry, well-drained upland/montane habitat characterized by an upland mixed deciduous and evergreen forest that is very rocky. All the plants found in this habitat go through periods of drought during the growing season due to the limited litter/soil layer in which moisture can be held. Elevation: 405 to 430 meters. Slope: 5 to 25 percent. Aspect: various. Geology: The underlying geology of this area is of Silurian origin and comprised of Shawangunk Formation. This formation is primarily light- to dark-gray, fine- to very coarse-grained sandstone and conglomerate containing thin shale interbeds. (Source: USGS Pennsylvania Geologic Map Data). Soils: The surface soil profile of this area is characterized as the Hazleton Series which consists of deep and very deep, well drained soils formed in residuum of acid gray, brown or red sandstone on uplands. The matrix includes a considerable accumulation of thin, flat, coarse fragments of sandstone, limestone, or schist with diameters up to 15 cm. Slope ranges from 0-80%. Permeability is moderately rapid to rapid. (Source: USDA-NRCS Official Soil Series Descriptions). EPA Ecoregion (Level III): Ridge and Valley (67). EPA Ecoregion (Level IV): Northern Sandstone Ridges (67c).Wild material2169044NA 89080
310NA 890812024RJLPA-009Rosa carolina L. Pennsylvania, United StatesNA2024COLLECTED09/22/2024Lancaster and York Counties: outcrops along the Susquehanna River, accessed from the Historic Lock 12 parking lot off of Pennsylvania Road 372.39.81483500, -76.3276220034Plants are growing from part-sun to full sun in crevices of the outcrops and where organic debris has accumulated in between boulders along the Susquehanna River. The sites range from nearly xeric to dry mesic, at least on the surface. Plants are generally growing 4-10 m above the normal flow of the river; however, the Holtwood Dam is less than 1 kilometer upstream and debris found trapped in the boulders indicates that there is periodic flooding, at least, in the lower zone of 4+ meters or so above normal river flow. This habitat has a diverse assemblage of deciduous trees and shrubs as well as abundant herbaceous taxa. Slope: 0 to 60 percent. Aspect: Northeast (generally). Geology: The underlying geology of this area is probably of lower Paleozoic age and characterized as the Octoraro Formation. It includes albite-chlorite schist, phyllite, some hornblende gneiss, and granitized members. Soils: The area where this species occurs is right on the edge of two soil zones that transition from the river’s edge to mesic conditions upslope. The first is generally referred to as Rock Outcrop. This terrestrial matrix in which plants grow is largely exposed underlying rock geology with accumulated outwash, rock decomposition, and organic debris buildup. The second is Mt. Airy (80%) and Manor (20%) Series soils, 25 to 60 percent slopes, extremely stony (MRF). (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). EPA Ecoregion (Level III): Northern Piedmont (64). EPA Ecoregion (Level IV): Piedmont Uplands (64c).Wild material2169045NA 89081
311NA 890832024RJLPA-012Rhododendron periclymenoides (Michx.) Shinners Pennsylvania, United StatesNA2024COLLECTED09/22/2024Outcrops along the Susquehanna River, accessed from the Historic Lock 12 parking lot off of Pennsylvania Road 372.39.81477400, -76.3280730035Plants are growing from shade to part-sun and occasionally full sun in crevices of the outcrops and where organic debris has accumulated in between boulders along the Susquehanna River. The sites range from nearly xeric to mesic, at least on the surface. Plants are generally growing 4-10 m above the normal flow of the river; however, the Holtwood Dam is less than 1 kilometer upstream and debris found trapped in the boulders indicates that there is periodic flooding, at least, in the lower zone of 4+ meters or so above normal river flow. This habitat has a diverse assemblage of deciduous trees and shrubs as well as abundant herbaceous taxa. Slope: 0 to 60 percent. Aspect: Northeast (generally). Geology: The underlying geology of this area is probably of lower Paleozoic age and characterized as the Octoraro Formation. It includes albite-chlorite schist, phyllite, some hornblende gneiss, and granitized members. Soils: The area where this species occurs is right on the edge of two soil zones that transition from the river’s edge to mesic conditions upslope. The first is generally referred to as Rock Outcrop. This terrestrial matrix in which plants grow is largely exposed underlying rock geology with accumulated outwash, rock decomposition, and organic debris buildup. The second is Mt. Airy (80%) and Manor (20%) Series soils, 25 to 60 percent slopes, extremely stony (MRF). (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). EPA Ecoregion (Level III): Northern Piedmont (64). EPA Ecoregion (Level IV): Piedmont Uplands (64c).Wild material2169047NA 89083
312NA 890842024RJLPA-013Physocarpus opulifolius (L.) Maxim. Pennsylvania, United StatesNA2024COLLECTED09/22/2024Outcrops along the Susquehanna River, accessed from the Historic Lock 12 parking lot off of Pennsylvania Road 372.39.81466300, -76.3283390036Plants are growing from shade to part-sun where organic debris has accumulated in between boulders as well as further upslope in deeper mesic soils along the Susquehanna River. This habitat has a diverse assemblage of deciduous trees and shrubs as well as abundant herbaceous taxa. Slope: 10 to 25 percent. Aspect: Northeast (generally). Geology: The underlying geology of this area is probably of lower Paleozoic age and characterized as the Octoraro Formation. It includes albite-chlorite schist, phyllite, some hornblende gneiss, and granitized members. Soils: The area where this species occurs is right on the edge of two soil zones that transition from the river’s edge to mesic conditions upslope. The first is generally referred to as Rock Outcrop. This terrestrial matrix in which plants grow is largely exposed underlying rock geology with accumulated outwash, rock decomposition, and organic debris buildup. The second is Mt. Airy (80%) and Manor (20%) Series soils, 25 to 60 percent slopes, extremely stony (MRF). (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). EPA Ecoregion (Level III): Northern Piedmont (64). EPA Ecoregion (Level IV): Piedmont Uplands (64c).Wild material2169048NA 89084
313NA 890852024RJLPA-014Rhododendron arborescens (Pursh) Torr. Pennsylvania, United StatesNA2024COLLECTED09/22/2024Outcrops along the Susquehanna River, accessed from the Historic Lock 12 parking lot off of Pennsylvania Road 372.39.81618100, -76.3306980038Plants are growing from shade to part-sun and occasionally full sun in crevices of the outcrops and where organic debris has accumulated in between boulders along the Susquehanna River. The sites range from nearly xeric to mesic, at least on the surface. Plants are generally growing 4-10 m above the normal flow of the river; however, the Holtwood Dam is less than 1 kilometer upstream and debris found trapped in the boulders indicates that there is periodic flooding, at least, in the lower zone of 4+ meters or so above normal river flow. This habitat has a diverse assemblage of deciduous trees and shrubs as well as abundant herbaceous taxa. Slope: 0 to 75 percent. Aspect: Northeast (generally). Geology: The underlying geology of this area is probably of lower Paleozoic age and characterized as the Octoraro Formation. It includes albite-chlorite schist, phyllite, some hornblende gneiss, and granitized members. Soils: The area where this species occurs is right on the edge of two soil zones that transition from the river’s edge to mesic conditions upslope. The first is generally referred to as Rock Outcrop. This terrestrial matrix in which plants grow is largely exposed underlying rock geology with accumulated outwash, rock decomposition, and organic debris buildup. The second is Mt. Airy (80%) and Manor (20%) Series soils, 25 to 60 percent slopes, extremely stony (MRF). (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). EPA Ecoregion (Level III): Northern Piedmont (64). EPA Ecoregion (Level IV): Piedmont Uplands (64c).Wild material2169049NA 89085
314NA 890862024RJLPA-015Ilex verticillata (L.) A. Gray Pennsylvania, United StatesNA2024COLLECTED09/22/2024Outcrops along the Susquehanna River, accessed from the Historic Lock 12 parking lot off of Pennsylvania Road 372.39.81656600, -76.3313660038Plants are growing from part-sun to full sun in crevices of the outcrops and where organic debris has accumulated in between boulders along the Susquehanna River. The sites range from nearly xeric to dry mesic, at least on the surface. Plants are generally growing 4-10 m above the normal flow of the river; however, the Holtwood Dam is less than 1 kilometer upstream and debris found trapped in the boulders indicates that there is periodic flooding, at least, in the lower zone of 4+ meters or so above normal river flow. This habitat has a diverse assemblage of deciduous trees and shrubs as well as abundant herbaceous taxa. Slope: 0 to 10 percent. Aspect: Northeast (generally). Geology: The underlying geology of this area is probably of lower Paleozoic age and characterized as the Octoraro Formation. It includes albite-chlorite schist, phyllite, some hornblende gneiss, and granitized members. Soils: The area where this species occurs is right on the edge of two soil zones that transition from the river’s edge to mesic conditions upslope. The first is generally referred to as Rock Outcrop. This terrestrial matrix in which plants grow is largely exposed underlying rock geology with accumulated outwash, rock decomposition, and organic debris buildup. The second is Mt. Airy (80%) and Manor (20%) Series soils, 25 to 60 percent slopes, extremely stony (MRF). (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). EPA Ecoregion (Level III): Northern Piedmont (64). EPA Ecoregion (Level IV): Piedmont Uplands (64c).Wild material2169050NA 89086
315NA 890882024RM-TK-001Viburnum acerifolium L. Alabama, United StatesNA2024COLLECTED09/19/2024Haines Island Park. Follow Ferry Road to the top of the hill entering the park where a picnic shelter is located. Plants are growing along trails to the north of the picnic shelter.31.72132026, -87.4640891081Plants are growing from part-sun to full shade in the understory of a mixed deciduous and coniferous forest on very dry upland habitat. Slope: 10 to 20 percent. Aspect: North. Geology: The underlying geology of this area is probably of Eocene age and characterized as the Claiborne Group: Tallahatta Formation. It is comprised of white to very light-greenish-gray thin-bedded to massive siliceous claystone; interbedded with thin layers of fossiliferous clay, sandy clay, and glauconitic sand and sandstone. White to light-greenish-gray fine to coarse sand and fine gravel occur at the base of the formation in southwest Alabama (Meridian Sand Member). (Source: USGS Alabama Geologic Map Data). Soils: The area of this occurrence is characterized as Arundel Series Loam, 8 to 35 percent slopes (ArF). The Arundel series consists of moderately deep, well drained, very slowly permeable soils on dissected uplands of the Southern Coastal Plain Major Land Resource Area (MLRA 133A). They formed in marine deposits consisting of acid clays underlain by horizontally bedded sandstone, buhrstone and siltstone. Slopes range from 2 to 60 percent. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). EPA Ecoregion (Level III): Southeastern Plains (65). EPA Ecoregion (Level IV): Buhrstone/Lime Hills (65q).Wild material2169052NA 89088
316NA 890892024RM-TK-002Viburnum acerifolium L. Alabama, United StatesNA2024COLLECTED09/19/2024Woodland slopes around and below the hilltop parking area leading down to the Silver Creek Lake Campground off of Silver Creek Lake Road.31.66612294, -87.5756986049Plants are growing in shade of upland dry mesic, mature mixed deciduous and evergreen woodland. Generally, the overstory is thinner and there is less leaf litter cover, making the surface soil conditions drier. Slope: 5 to 10 percent. Aspect: Southeast. Geology: The underlying geology of this area is Claiborne Group, Tallahatta Formation, of Eocene origin, with white to very light-greenish-gray thin-bedded to massive siliceous claystone; interbedded with thin layers of fossiliferous clay, sandy clay, and glauconitic sand and sandstone. (Source: USGS Alabama Geologic Map Data). Soils: The primary soil types in the collection area are classified as Arundel-Cantuche Complex soils (15 to 35 percent slopes). The Arundel Series consists of moderately deep, well drained, very slowly permeable soils on dissected uplands of the Southern Coastal Plain. They formed in marine deposits consisting of acid clays underlain by horizontally bedded sandstone, buhrstone and siltstone. These soils are strongly acid. Slopes range from 2 to 60 percent. The Cantuche Series consists of shallow, well drained, moderately permeable soils that formed over horizontally bedded claystone. These soils are on narrow ridgetops and narrow benches on steep side-slopes of dissected landscapes in the Coastal Plain. They are strongly acid. Slopes range from 2 to 35 percent. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). EPA Ecoregion (Level III): Southeastern Plains (65). EPA Ecoregion (Level IV): Buhrstone/Lime Hills (65q).Wild material2169053NA 89089
317NA 890902024RM-TK-003Ilex longipes Chapm. ex Trel. Alabama, United StatesNA2024COLLECTED09/19/2024Woodland slopes around and below the hilltop parking area leading down to the Silver Creek Lake Campground off of Silver Creek Lake Road.31.66612294, -87.5756986039Plants are growing in part-shade to shade of a moist mesic deciduous and evergreen woodland on dry, well-drained soil to an area 1-2 meters above a small seasonally spring-fed creek at 31.664428°, -87.574614°. Slope: 5 to 10 percent. Aspect: Southeast. Geology: The underlying geology of this area is Claiborne Group, Tallahatta Formation, of Eocene origin, with white to very light-greenish-gray thin-bedded to massive siliceous claystone; interbedded with thin layers of fossiliferous clay, sandy clay, and glauconitic sand and sandstone. (Source: USGS Alabama Geologic Map Data). Soils: The primary soil types in the collection area are classified as Arundel-Cantuche Complex soils (15 to 35 percent slopes). The Arundel Series consists of moderately deep, well drained, very slowly permeable soils on dissected uplands of the Southern Coastal Plain. They formed in marine deposits consisting of acid clays underlain by horizontally bedded sandstone, buhrstone and siltstone. These soils are strongly acid. Slopes range from 2 to 60 percent. The Cantuche Series consists of shallow, well drained, moderately permeable soils that formed over horizontally bedded claystone. These soils are on narrow ridgetops and narrow benches on steep side-slopes of dissected landscapes in the Coastal Plain. They are strongly acid. Slopes range from 2 to 35 percent. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). EPA Ecoregion (Level III): Southeastern Plains (65). EPA Ecoregion (Level IV): Buhrstone/Lime Hills (65q).Wild material2169054NA 89090
318NA 890922024RM-TK-005Ilex amelanchier M. A. Curtis ex Chapm. Florida, United StatesNA2024COLLECTED09/29/2024Yellow 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, -86.5934900023Plants 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 material2169056NA 89092
319OPGC 8855JDC/RM/2024/019/1141Rudbeckia missouriensis Engelm. ex C. L. Boynton & Beadle Missouri, United StatesOPGCHABITAT2024COLLECTED09/28/2024Danville Glade Conservation Area located 3.60 miles south, southeast of Danville, T47N R5W SW 1/4 SW 1/4 Sec. 5.38.86583400, -91.50779400222Remnant glade.Wild material2169019OPGC 8855
320Ames 36263Chippewa National Forest (Itasca)Viburnum opulus L. var. americanum Aiton Minnesota, United StatesNC7FRUIT2024COLLECTED09/15/2024Chippewa National Forest between Alder and Suomi including Bowstring River, Turtle River, and Potato Creek watersheds.47.56968000, -93.68815400407Roadside edges with most samples near open water (creek/rivers).Wild materialFormerly 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). Genetics of this accession represents a very broad collection area stretching nearly 7.0 miles near Alder in central Itasca County of north central Minnesota. In August of 2022, a total of 23 leaf samples from this same area were sampled (OB001-OB012 and OB0015-OB025) and all samples were genetically confirmed as American highbush cranberry, V. opulus var. americanum (Tork et. al 2025). 2168987Ames 36263
321Ames 36292Faith-Moccasin WMASalix petiolaris Sm. Minnesota, United StatesNC7LEAF2024COLLECTED09/07/2024Faith Wildlife Management Area and Moccassin State Wildlife Management Area east of Twin Valley approximately 8.25 miles.47.26010700, -96.09171700351Wetland, shrub-carr complex.Wild materialSlender-leaved willow, Salix petiolaris, is a somewhat dense suckering shrub that can reach up to 10' in height with slender stems that branch minimally, but typically maintains a height of 5-8'. Native to North America, the native range covers mostly the northeastern US stretching from Maine to western North Dakota and Canada south to central Iowa (Little, E. L. Jr. 1977). Salix petiolaris typically dominates wetland areas including sedge meadows, marshes, riverbanks, and lake shores. Despite favoring wet habitats, it can also be found in dry, upland areas, especially those with high-water tables. However, longevity is generally limited in upland habitats. S. petiolaris, similar to other willow species, responds well to fire, coppicing, or heavy browsing (highly favored by deer) by sprouting new stems close to the crown. In cultivation, plants after five years will encompass a 5' x 5' area due to stems that arch from the main base of the plant. Coppicing of plants to ground level is highly recommended either annually or once every 3-5 years to maintain vigorous growth and plant health. This species requires substantial to full sun exposure and is an excellent choice for streambank stabilizations and windbreaks to reduce soil erosion and drifting snow, respectively. This accession represents genetics from northwestern Minnesota. Plants sampled in nature averaging 6-8' in height. Clump-type growth habit with minimal branching, but dense suckering (e.g. 50+ ramets per genet - typically encompassing 5' x 5' area). Dormant, winter stem are rather uniform/consistent orange-brown/mahogany colors.2169827Ames 36292
322Ames 36248Robert's CreekSalix bebbiana Sarg. Iowa, United StatesNC7PLANT2024COLLECTED05/15/2024Robert’s Creek Preserve just north of Forest Road approximately 4.2 miles north, northeast of Elkader, T94N R5W near center of Sec. 36.42.91366500, -91.37990600260Mixed hardwood forest. Very steep, moist, north-facing slope. Wild materialBebb's willow, Salix bebbiana, is a tight, clump forming, multi-stemmed shrub that can reach up to 25' in height that forms a rather distinct, mounded growth habit. Native to North America, the native range covers mostly Canada, but extending south into the northeastern US and also the Rocky Mountains range stretching as far south as New Mexico and Arizona (Little, E. L. Jr. 1977). In Iowa, this species seems to only be known from northeastern Iowa. Salix bebbiana can be found in a variety of habitats from pond margins/swamps to even moderately well-drained open fields. The female capsules are long (5-9 mm) with a very slender beak held on the longest stalk of any N. American Salix. This accession represents genetics from northeastern Iowa at the southern edge of its range in northeastern N. America. Specimens sampled were estimated at 30' in height. Some of the oldest, largest specimens sampled measuring approximately 8" DBH were showing signs of decline. Immature leaves are reddish or yellow green and rather rugose. 2167645Ames 36248
323WLP 3433RM2023-002Clethra acuminata Michx. Georgia, United StatesNA2024COLLECTED10/21/2023Plants growing along Patterson Gap Road.34.97299200, -83.46003100789Plants growing in part shade in a very dry and rocky, mostly deciduous habitat. The site is steeply sloped, underlain by rock, with rocky outcrops. Slope: 15 percent. Aspect: Variable. The underlying geology of this area is Biotite Gneiss, primarily of Precambrian-Paleozoic origin. (Source: USGS North Carolina Geologic Map Data.) The primary soil type in the collection area is classified as Tusquitee loam, 10 to 25 percent slopes. The Tusquitee series consists of very deep, well drained soils on gently sloping to very steep benches, foot slopes, toe slopes, and fans in coves in the Southern Blue Ridge mountains, MLRA 130B. These soils formed in colluvium derived from materials weathered from igneous and high-grade metamorphic crystalline rocks such as granite, mica gneiss, hornblende gneiss, and schist. Slope ranges from 2 to 95 percent. The surface layer to 5cm deep is comprised of moderately decomposed organic matter and leaves, twigs, and roots. Layers to 2m deep range from very dark grayish brown to brown sandy loam with weak medium and coarse granular structure that is friable. A few fine flakes of mica can be found and these soils are very strongly acid. (Source: NRCS Web Soil Survey.)Wild material2166142WLP 3433
324Ames 36219Egyptian TractSalix sericea Marshall Missouri, United StatesNC7LEAF2024COLLECTED01/19/2024LAD Foundation Egyptian Tract Wet Hollow Seep/Fen Complex located 7.52 miles west, southwest of Annapolis just northwest of intersection of CR 338 and CR 334, T31N R2E SW 1/4 SE 1/4 SE 1/4 Sec. 21 (Lesterville SE Quad.).37.34429700, -90.83361600217Perched wet fen/seep complex with standing water supporting both obligate calciphilic and obligate acidophilic plant species.Wild materialThe native range of Salix sericea is concentrated througout the northeastern and eastern central United States ranging from Maine south to South Carolina, west to Illinois with a relatively large disjunct area in southeastern Missouri (Little, E. L. Jr. 1977). This accession represents genetics from southeastern Missouri in Reynolds County. Shrubs noted at the collection site in nature ranging in height from 2-7 feet and typically twice as wide as tall. Multi-stemmed shrubs expanding vegetatively via layering. Dormant stem colors noted at collection site ranging from mostly greenish to occassionally brownish red and/or copper tones. Dormant buds rather red and often bright red in color. Salix sericea is native to areas of the northeastern U.S. and north into Canada, reaching its western extent in Missouri. Classified as an obligate wetland plant that typically occurs on wet seeps, sedge meadows, streambanks, fens, etc. that are usually slightly acidic. Known to have the potential to reach up to four meters in height, but always much wider than tall. Ornamental characteristics include dark green leaves that are hairless above with undersides that are densely minutely-hairy making them rather white in appearance. Flowering occurs before or during leaf expansion. This species is known to serve as a larval host plant for the Arcadian Hairstreak, Satyrium acadica. 2165775Ames 36219
325WLP 3418HOKY23-13Acer tataricum L. subsp. aidzuense (Franch.) P. C. DeJong Honshu, JapanNA2024COLLECTED09/22/2023Tochigi Prefecture: Moka-shi: Utsunomiya University Farm.36.50005000, 139.98623330108Mesic woodland-farmfield edges above small stream. Growing in open to quarter-shade. Soil: Rich, organic-rich loam. Slope: 10°. Aspect: West. Elevation: 353 feet.Wild material2165756WLP 3418
326NA 88845RJL-RM2023FLAL-019Ilex opaca Aiton Florida, United StatesNA2023COLLECTED12/13/2023Yellow 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, -86.6022130035Plants 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 material2165675NA 88845
327NA 88846RJL-RM2023FLAL-020Ilex decidua Walter Florida, United StatesNA2023COLLECTED12/13/2023Yellow 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, -86.5916870023Plants 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 material2165676NA 88846
328NA 88847RJL-RM2023FLAL-021Ilex amelanchier M. A. Curtis ex Chapm. Florida, United StatesNA2023COLLECTED12/13/2023Yellow 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, -86.5921050023Plants 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 material2165677NA 88847
329WLP 3377TXWL2023-024Viburnum dentatum L. Texas, United StatesNA2023COLLECTED12/13/2023Roadside between Big Cow Creek and Hardy Cemetery.31.03548900, -93.85086800Roadside; mesic, mixed hardwood/pine forest.Wild material2165656WLP 3377
330NA 88814TXWL2023-021Ilex ambigua Torr. Texas, United StatesNA2023COLLECTED12/09/2023Roadside between Big Cow Creek and Hardy Cemetery.31.03548900, -93.85086800Roadside; mesic, mixed hardwood/pine forest.Wild material2165618NA 88814
331NA 88801TJK2023LA/TX-001Cocculus carolinus (L.) DC. Louisiana, United StatesNA2023COLLECTED11/21/2023Interstate 20, westbound, approximately 13 miles west of Mississippi River, 9 miles east of U.S. Highway 65.32.33740000, -91.0632000024Damp low, wooded treeline. Slope: less than 2%. Aspect: Southwest. Elevation: 79 feet.Wild material2159184NA 88801
332NA 88802TJK2023LA/TX-002Ilex decidua Walter Louisiana, United StatesNA2023COLLECTED11/21/2023Interstate 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, -91.2967000021Damp wooded treeline. Slope: 12%. Aspect: West-southwest. Elevation: 69 feet.Wild material2159185NA 88802
333NA 88803TJK2023LA/TX-003Crataegus viridis L. Louisiana, United StatesNA2023COLLECTED11/21/2023Interstate 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, -91.2967000021Damp wooded treeline. Slope: 12%. Aspect: West-southwest. Elevation: 69 feet.Wild material2159186NA 88803
334NA 88804TJK2023LA/TX-004Crataegus viridis L. Louisiana, United StatesNA2023COLLECTED11/21/2023Walnut 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, -91.0717000026Damp wooded treeline. Slope: 10%. Aspect: North-northeast. Elevation: 84 feet.Wild material2159187NA 88804
335NA 88689RJL2023NJ-002Kalmia latifolia L. New Jersey, United StatesNA2023COLLECTED11/10/2023Franklin Township: Piney Hollow Preservation Area (the site is owned by Franklin Township). Plants accessed by foot along trails throughout property.39.57400900, -74.9360240032Plants growing in shade to part-shade of a mesic to mesic-dry woodland habitat that is mostly deciduous, but also includes pine overstory. Slope: N/A. Aspect: N/A. Soils: The underlying geology of this area is of Middle Miocene, Serravallian origin and characterized as an Cohansey Formation. It is comprised of sand, white to yellow with local gravel and clay. Locally stained red or orange brown by iron oxides and (or) cemented into large blocks of ironstone. Unweathered clay is typically dark gray, but commonly weathers white where interbedded with thin beds of ironstone. Unit is a complex of interfingering marine and nonmarine facies. Sand is typically medium grained and moderately sorted although it ranges from fine to very coarse grained and from poorly to well sorted. Sand consists of quartz and siliceous rock fragments. Some beds are locally micaceous. In general, the sand is crossbedded, although the style of crossbedding varies significantly with the paleoenvironment. Trough crossbedding predominates, especially in the nonmarine channel fill deposits, and the scale of the crossbeds varies from small to large. Maximum thickness in the map area is about 60 m; however, thickness is difficult to determine because of the irregular basal contact and extensive post-depositional erosion. There is as much as 18 m of relief along the basal contact. The basal contact is sharp, undulatory, and directly overlain by a thin gravel bed. The Cohansey Formation unconformably overlies the Kirkwood Formation and is found in channels cut down into the Kirkwood. Where the Kirkwood consists of sandy, light-colored sediments, the basal contact of the Cohansey is drawn below crossbedded sediments. Where the Kirkwood consists of dark-colored silty beds, the basal contact is drawn between light-colored Cohansey sediments and the underlying dark-colored sediments. The Cohansey was markedly thinned because of erosion prior to deposition of overlying units in the western and southern parts of the southern sheet. The unit has been extensively eroded and stripped from large areas of the New Jersey Coastal Plain, particularly in the central sheet where outliers are common. In spite of its widespread nature, the Cohansey is poorly exposed because of its loose sandy composition, which causes it to erode easily. (Source: USGS New Jersey Geologic Map Data.) The primary soil type in the location of this collection is classified as Downer loamy sand, 0 to 5 percent slopes, Northern Coastal Plain. Downer Series soils are very deep, well-drained soils that are coarse-loamy, siliceous, semiactive, mesic Typic Hapludults. The upper strata of Downer Series from 0 to 25 cm is dark grayish brown, brown loamy sand that is dry with weak fine granular structure. It is very friable and strongly acid. Lower strata from 25 to 76 cm are yellowish brown single grain, loose loamy sand with few extremely weakly cemented masses of oxidized iron in the lower part. This layer is very strongly acid. (Source: NRCS Web Soil Survey.)Wild material2159117NA 88689
336NA 88690RJL2023NJ-003Ilex verticillata (L.) A. Gray New Jersey, United StatesNA2023COLLECTED11/10/2023Franklin Township: Piney Hollow Preservation Area (the site is owned by Franklin Township). This species was found below the dam at the far end of McCarthys Lakes. Plants accessed by foot along trails throughout property.39.57407200, -74.9251860028Plants growing in part-shade to sun of the moist to saturated areas below the McCarthys Lakes dam in the wetlands associated with the New Squankum Branch. The area appears to be inundated year-round with plants growing on low mounds surrounded by obligate wetland species. Slope: N/A. Aspect: N/A. The underlying geology of this area is of Middle Miocene, Serravallian origin and characterized as an Cohansey Formation. It is comprised of sand, white to yellow with local gravel and clay. Locally stained red or orange brown by iron oxides and (or) cemented into large blocks of ironstone. Unweathered clay is typically dark gray, but commonly weathers white where interbedded with thin beds of ironstone. Unit is a complex of interfingering marine and nonmarine facies. Sand is typically medium grained and moderately sorted although it ranges from fine to very coarse grained and from poorly to well sorted. Sand consists of quartz and siliceous rock fragments. Some beds are locally micaceous. In general, the sand is crossbedded, although the style of crossbedding varies significantly with the paleoenvironment. Trough crossbedding predominates, especially in the nonmarine channel fill deposits, and the scale of the crossbeds varies from small to large. Maximum thickness in the map area is about 60 m; however, thickness is difficult to determine because of the irregular basal contact and extensive post-depositional erosion. There is as much as 18 m of relief along the basal contact. The basal contact is sharp, undulatory, and directly overlain by a thin gravel bed. The Cohansey Formation unconformably overlies the Kirkwood Formation and is found in channels cut down into the Kirkwood. Where the Kirkwood consists of sandy, light-colored sediments, the basal contact of the Cohansey is drawn below crossbedded sediments. Where the Kirkwood consists of dark-colored silty beds, the basal contact is drawn between light-colored Cohansey sediments and the underlying dark-colored sediments. The Cohansey was markedly thinned because of erosion prior to deposition of overlying units in the western and southern parts of the southern sheet. The unit has been extensively eroded and stripped from large areas of the New Jersey Coastal Plain, particularly in the central sheet where outliers are common. In spite of its widespread nature, the Cohansey is poorly exposed because of its loose sandy composition, which causes it to erode easily. (Source: USGS New Jersey Geologic Map Data.) The primary soil type in the collection area is classified as Manahawkin Series muck, 0 to 2 percent slopes, frequently flooded, Northern Coastal Plain. Manahawkin Series soils are very deep, very poorly drained soils that are sandy or sandy-skeletal, siliceous, dysic, mesic Terric Haplosaprists high in organic deposits that are found in lake basins, back swamps, floodplains, and freshwater channels. The soils are classified in the dysic reaction class because pH in water dominantly ranges from 4.5 to 5.0. The zone from the soil surface to a depth of 200 cm is continuously saturated (endosaturation). The upper strata of Manahawkin Series from 0 to 76 cm is black broken face and rubbed muck; 10 percent fibers, less than 2 percent rubbed; moderate medium granular structure; mat of many fine roots; identifiable material is primarily herbaceous with a trace of woody fragments; 85-95 percent organic matter; extremely acid. Lower strata to 200 cm are gray sand, single grained and loose; strongly acid. (Source: NRCS Web Soil Survey.)Wild material2159118NA 88690
337NA 88691RJL2023NJ-004Ilex laevigata (Pursh) A. Gray New Jersey, United StatesNA2023COLLECTED11/10/2023Franklin Township: Piney Hollow Preservation Area (the site is owned by Franklin Township). This species was found below the dam at the far end of McCarthys Lakes. Plants accessed by foot along trails throughout property.39.57404200, -74.9252370028Plants growing in part-shade to sun of the moist to saturated areas below the McCarthys Lakes dam in the wetlands associated with the New Squankum Branch. The area appears to be inundated year-round with plants growing on low mounds surrounded by obligate wetland species. Slope: N/A. Aspect: N/A. The underlying geology of this area is of Middle Miocene, Serravallian origin and characterized as an Cohansey Formation. It is comprised of sand, white to yellow with local gravel and clay. Locally stained red or orange brown by iron oxides and (or) cemented into large blocks of ironstone. Unweathered clay is typically dark gray, but commonly weathers white where interbedded with thin beds of ironstone. Unit is a complex of interfingering marine and nonmarine facies. Sand is typically medium grained and moderately sorted although it ranges from fine to very coarse grained and from poorly to well sorted. Sand consists of quartz and siliceous rock fragments. Some beds are locally micaceous. In general, the sand is crossbedded, although the style of crossbedding varies significantly with the paleoenvironment. Trough crossbedding predominates, especially in the nonmarine channel fill deposits, and the scale of the crossbeds varies from small to large. Maximum thickness in the map area is about 60 m; however, thickness is difficult to determine because of the irregular basal contact and extensive post-depositional erosion. There is as much as 18 m of relief along the basal contact. The basal contact is sharp, undulatory, and directly overlain by a thin gravel bed. The Cohansey Formation unconformably overlies the Kirkwood Formation and is found in channels cut down into the Kirkwood. Where the Kirkwood consists of sandy, light-colored sediments, the basal contact of the Cohansey is drawn below crossbedded sediments. Where the Kirkwood consists of dark-colored silty beds, the basal contact is drawn between light-colored Cohansey sediments and the underlying dark-colored sediments. The Cohansey was markedly thinned because of erosion prior to deposition of overlying units in the western and southern parts of the southern sheet. The unit has been extensively eroded and stripped from large areas of the New Jersey Coastal Plain, particularly in the central sheet where outliers are common. In spite of its widespread nature, the Cohansey is poorly exposed because of its loose sandy composition, which causes it to erode easily. (Source: USGS New Jersey Geologic Map Data.) The primary soil type in the collection area is classified as Manahawkin Series muck, 0 to 2 percent slopes, frequently flooded, Northern Coastal Plain. Manahawkin Series soils are very deep, very poorly drained soils that are sandy or sandy-skeletal, siliceous, dysic, mesic Terric Haplosaprists high in organic deposits that are found in lake basins, back swamps, floodplains, and freshwater channels. The soils are classified in the dysic reaction class because pH in water dominantly ranges from 4.5 to 5.0. The zone from the soil surface to a depth of 200 cm is continuously saturated (endosaturation). The upper strata of Manahawkin Series from 0 to 76 cm is black broken face and rubbed muck; 10 percent fibers, less than 2 percent rubbed; moderate medium granular structure; mat of many fine roots; identifiable material is primarily herbaceous with a trace of woody fragments; 85-95 percent organic matter; extremely acid. Lower strata to 200 cm are gray sand, single grained and loose; strongly acid. (Source: NRCS Web Soil Survey.)Wild material2159119NA 88691
338NA 88692RJL2023NJ-005Ilex opaca Aiton New Jersey, United StatesNA2023COLLECTED11/10/2023Franklin Township: Piney Hollow Preservation Area (the site is owned by Franklin Township). This species was found on as well as below the dam at the far end of McCarthys Lakes. Plants accessed by foot along trails throughout property.39.57423200, -74.9252560029Plants growing in part-shade to sun of the moist to saturated areas below the McCarthys Lakes dam in the wetlands associated with the New Squankum Branch. Plants were also found growing on the slopes of the dam in well-drained mesic to dry-mesic conditions. This species is clearly adaptable to a variety of conditions. Slope: 0 to 15 percent. Aspect: East. Elevation: 28 to 30 meters. NOTE: In addition to the soil type described below, this species was also growing on the slopes of a constructed earthen dam of unknown soil origin. The underlying geology of this area is of Middle Miocene, Serravallian origin and characterized as an Cohansey Formation. It is comprised of sand, white to yellow with local gravel and clay. Locally stained red or orange brown by iron oxides and (or) cemented into large blocks of ironstone. Unweathered clay is typically dark gray, but commonly weathers white where interbedded with thin beds of ironstone. Unit is a complex of interfingering marine and nonmarine facies. Sand is typically medium grained and moderately sorted although it ranges from fine to very coarse grained and from poorly to well sorted. Sand consists of quartz and siliceous rock fragments. Some beds are locally micaceous. In general, the sand is crossbedded, although the style of crossbedding varies significantly with the paleoenvironment. Trough crossbedding predominates, especially in the nonmarine channel fill deposits, and the scale of the crossbeds varies from small to large. Maximum thickness in the map area is about 60 m; however, thickness is difficult to determine because of the irregular basal contact and extensive post-depositional erosion. There is as much as 18 m of relief along the basal contact. The basal contact is sharp, undulatory, and directly overlain by a thin gravel bed. The Cohansey Formation unconformably overlies the Kirkwood Formation and is found in channels cut down into the Kirkwood. Where the Kirkwood consists of sandy, light-colored sediments, the basal contact of the Cohansey is drawn below crossbedded sediments. Where the Kirkwood consists of dark-colored silty beds, the basal contact is drawn between light-colored Cohansey sediments and the underlying dark-colored sediments. The Cohansey was markedly thinned because of erosion prior to deposition of overlying units in the western and southern parts of the southern sheet. The unit has been extensively eroded and stripped from large areas of the New Jersey Coastal Plain, particularly in the central sheet where outliers are common. In spite of its widespread nature, the Cohansey is poorly exposed because of its loose sandy composition, which causes it to erode easily. (Source: USGS New Jersey Geologic Map Data.) The primary soil type in the collection area is classified as Manahawkin Series muck, 0 to 2 percent slopes, frequently flooded, Northern Coastal Plain. Manahawkin Series soils are very deep, very poorly drained soils that are sandy or sandy-skeletal, siliceous, dysic, mesic Terric Haplosaprists high in organic deposits that are found in lake basins, back swamps, floodplains, and freshwater channels. The soils are classified in the dysic reaction class because pH in water dominantly ranges from 4.5 to 5.0. The zone from the soil surface to a depth of 200 cm is continuously saturated (endosaturation). The upper strata of Manahawkin Series from 0 to 76 cm is black broken face and rubbed muck; 10 percent fibers, less than 2 percent rubbed; moderate medium granular structure; mat of many fine roots; identifiable material is primarily herbaceous with a trace of woody fragments; 85-95 percent organic matter; extremely acid. Lower strata to 200 cm are gray sand, single grained and loose; strongly acid. (Source: NRCS Web Soil Survey.)Wild material2159120NA 88692
339NA 88693RJL2023NJ-006Clethra alnifolia L. New Jersey, United StatesNA2023COLLECTED11/10/2023Franklin Township: Piney Hollow Preservation Area (the site is owned by Franklin Township). Plants accessed by foot along trails throughout property.39.57319800, -74.9290890029Plants growing in shade to part-shade over a wide range of habitats from mesic to mesic-dry as well as moist to wetland habitats. The woodlands are mostly deciduous, but also include occasional pine overstory. Slope: N/A. Aspect: N/A. The underlying geology of this area is of Middle Miocene, Serravallian origin and characterized as an Cohansey Formation. It is comprised of sand, white to yellow with local gravel and clay. Locally stained red or orange brown by iron oxides and (or) cemented into large blocks of ironstone. Unweathered clay is typically dark gray, but commonly weathers white where interbedded with thin beds of ironstone. Unit is a complex of interfingering marine and nonmarine facies. Sand is typically medium grained and moderately sorted although it ranges from fine to very coarse grained and from poorly to well sorted. Sand consists of quartz and siliceous rock fragments. Some beds are locally micaceous. In general, the sand is crossbedded, although the style of crossbedding varies significantly with the paleoenvironment. Trough crossbedding predominates, especially in the nonmarine channel fill deposits, and the scale of the crossbeds varies from small to large. Maximum thickness in the map area is about 60 m; however, thickness is difficult to determine because of the irregular basal contact and extensive post-depositional erosion. There is as much as 18 m of relief along the basal contact. The basal contact is sharp, undulatory, and directly overlain by a thin gravel bed. The Cohansey Formation unconformably overlies the Kirkwood Formation and is found in channels cut down into the Kirkwood. Where the Kirkwood consists of sandy, light-colored sediments, the basal contact of the Cohansey is drawn below crossbedded sediments. Where the Kirkwood consists of dark-colored silty beds, the basal contact is drawn between light-colored Cohansey sediments and the underlying dark-colored sediments. The Cohansey was markedly thinned because of erosion prior to deposition of overlying units in the western and southern parts of the southern sheet. The unit has been extensively eroded and stripped from large areas of the New Jersey Coastal Plain, particularly in the central sheet where outliers are common. In spite of its widespread nature, the Cohansey is poorly exposed because of its loose sandy composition, which causes it to erode easily. (Source: USGS New Jersey Geologic Map Data.) The primary soil types in the area of this collection is classified as Atsion sand, 0 to 2 percent slopes, Northern Tidewater Area and Downer loamy sand, 0 to 5 percent slopes, Northern Coastal Plain. Atsion Series soils are very deep, poorly drained with moderate to rapid permeability above 70 cm and slower beneath. They are classified as sandy, siliceous, mesic Aeric Alaquods. The upper stratum from 0 to 25 cm is dark gray sand, dry, single grained and lose with many fine roots. It is extremely acid. Lower strata are light gray to dark brown with small percentages of rounded quartzose pebbles and are extremely acid. Downer Series soils are very deep, well-drained soils that are coarse-loamy, siliceous, semiactive, mesic Typic Hapludults. The upper stratum of Downer Series from 0 to 25 cm is dark grayish brown, brown loamy sand that is dry with weak fine granular structure. It is very friable and strongly acid. Lower strata from 25 to 76 cm are yellowish brown single grain, loose loamy sand with few extremely weakly cemented masses of oxidized iron in the lower part. This layer is very strongly acid. (Source: NRCS Web Soil Survey.)Wild material2159121NA 88693
340NA 88696RJL2023NCSC-001Rhododendron catawbiense Michx. North Carolina, United StatesNA2023COLLECTED11/12/2023Duke Forest property along New Hope Creek. The collection site is accesses by foot along trails.35.98317700, -79.01856200103Plants growing in shade to part-shade of an upland very dry woodland habitat that is mostly deciduous. The site is steeply sloped underlain by rocky outcrop. Slope: 15 to 25 percent. Aspect: Northwest. The underlying geology of this area is of Cambrian/Late Proterozoic origin and characterized as a Metamorphosed Granitic Rock. It is megacrystic and well foliated; locally contains hornblende. Chapel Hill, Chatham, Farrington, Meadow Flats, Mt. Moriah, Parks Crossroads plutons, and Roxboro and Vance County suites. (Source: USGS North Carolina Geologic Map Data.) The primary soil type in the collection area is classified as Wedowee sandy loam, 15 to 25 percent slopes. Wedowee Series consists of very deep, well drained, moderately permeable soils that formed in residuum weathered from felsic igneous and metamorphic rocks of the Piedmont uplands. These soils are on narrow ridges and on side slopes of uplands. Slopes are dominantly 6 to 25 percent but ranges from 0 to 60 percent. The strata range from dark brown and brownish yellow to strong brown. They are mostly sandy loam; moderate fine granular structure; very friable; strongly acid. (Source: NRCS Web Soil Survey.) Wild material2159124NA 88696
341NA 88710RJL2023NCSC-015Cephalanthus occidentalis L. South Carolina, United StatesNA2023COLLECTED11/14/2023Francis Marion National Forest: plants growing in wetlands/swamps on US Forest Service Road 223 approximately 0.57 kilometers southeast from the junction with Halfway Creek Road.33.06771000, -79.6776970020Plants are growing in part-shade to sun along the edges of the swamp in seasonally inundated acidic wetland habitat. Slope: N/A. Aspect: N/A. The underlying geology of this area is of Pleistocene origin and characterized as an Socastee Formation. This is a low coastal formation in the Carolinas like Penholoway but younger and lower in altitude. It is comprised primarily of unconsolidated, fine-detrital clay. It is described as variegated quartzose sands, argillaceous sands, and clays, 5 m thick at the type section near Socastee Swamp. (Source: USGS South Carolina Geologic Map Data.) The primary soil type in this collection area is classified as Rutlege Series loamy fine sand. Rutlege Series soils are very deep, very poorly drained soils that are sandy, siliceous, thermic Typic Humaquepts. Upper strata soils (0-38 cm) are black loamy sand with weak medium granular structure. They are loose and very strongly acid. Lower strata (38-175 cm) range from dark gray to dark brown sand that is single grained, loose, and very strongly acid. (Source: NRCS Web Soil Survey.)Wild material2159138NA 88710
342NA 88711RJL2023NCSC-016Ilex myrtifolia Walter South Carolina, United StatesNA2023COLLECTED11/14/2023Francis Marion National Forest: plants growing in wetlands/swamps on US Forest Service Road 223 approximately 0.57 kilometers southeast from the junction with Halfway Creek Road.33.06786200, -79.6776180011Plants are growing in shade to part-shade in the swamp in seasonally inundated acidic wetland habitat. Slope: N/A. Aspect: N/A. The underlying geology of this area is of Pleistocene origin and characterized as an Socastee Formation. This is a low coastal formation in the Carolinas like Penholoway but younger and lower in altitude. It is comprised primarily of unconsolidated, fine-detrital clay. It is described as variegated quartzose sands, argillaceous sands, and clays, 5 m thick at the type section near Socastee Swamp. (Source: USGS South Carolina Geologic Map Data.) The primary soil type in this collection area is classified as Rutlege Series loamy fine sand. Rutlege Series soils are very deep, very poorly drained soils that are sandy, siliceous, thermic Typic Humaquepts. Upper strata soils (0-38 cm) are black loamy sand with weak medium granular structure. They are loose and very strongly acid. Lower strata (38-175 cm) range from dark gray to dark brown sand that is single grained, loose, and very strongly acid. (Source: NRCS Web Soil Survey.)Wild material2159139NA 88711
343NA 88712RJL2023NCSC-017Itea virginica L. South Carolina, United StatesNA2023COLLECTED11/14/2023Francis Marion National Forest: plants growing in wetlands/swamps on US Forest Service Road 223 approximately 0.57 kilometers southeast from the junction with Halfway Creek Road.33.06755600, -79.6778910011Plants are growing in the understory of the acidic swamp that is seasonally inundated in shade. Slope: N/A. Aspect: N/A. The underlying geology of this area is of Pleistocene origin and characterized as an Socastee Formation. This is a low coastal formation in the Carolinas like Penholoway but younger and lower in altitude. It is comprised primarily of unconsolidated, fine-detrital clay. It is described as variegated quartzose sands, argillaceous sands, and clays, 5 m thick at the type section near Socastee Swamp. (Source: USGS South Carolina Geologic Map Data.) The primary soil type in this collection area is classified as Rutlege Series loamy fine sand. Rutlege Series soils are very deep, very poorly drained soils that are sandy, siliceous, thermic Typic Humaquepts. Upper strata soils (0-38 cm) are black loamy sand with weak medium granular structure. They are loose and very strongly acid. Lower strata (38-175 cm) range from dark gray to dark brown sand that is single grained, loose, and very strongly acid. (Source: NRCS Web Soil Survey.)Wild material2159140NA 88712
344NA 88713RJL2023NCSC-018Ilex opaca Aiton South Carolina, United StatesNA2023COLLECTED11/14/2023Francis Marion National Forest: plants growing in wetlands/swamps on US Forest Service Road 223 approximately 0.57 kilometers southeast from the junction with Halfway Creek Road.33.06783000, -79.6774910011Plants are growing in part shade to shade of a swamp in seasonally inundated acidic wetland habitat. Slope: N/A. Aspect: N/A. The underlying geology of this area is of Pleistocene origin and characterized as an Socastee Formation. This is a low coastal formation in the Carolinas like Penholoway but younger and lower in altitude. It is comprised primarily of unconsolidated, fine-detrital clay. It is described as variegated quartzose sands, argillaceous sands, and clays, 5 m thick at the type section near Socastee Swamp. (Source: USGS South Carolina Geologic Map Data.) The primary soil type in this collection area is classified as Rutlege Series loamy fine sand. Rutlege Series soils are very deep, very poorly drained soils that are sandy, siliceous, thermic Typic Humaquepts. Upper strata soils (0-38 cm) are black loamy sand with weak medium granular structure. They are loose and very strongly acid. Lower strata (38-175 cm) range from dark gray to dark brown sand that is single grained, loose, and very strongly acid. (Source: NRCS Web Soil Survey.)Wild material2159141NA 88713
345NA 88714RJL2023NCSC-019Smilax walteri Pursh South Carolina, United StatesNA2023COLLECTED11/14/2023Francis Marion National Forest: plants growing in wetlands/swamps on US Forest Service Road 223 approximately 0.57 kilometers southeast from the junction with Halfway Creek Road.33.06757700, -79.6779280011Plants are growing in shade, part-shade and sun in the acid soils of a swamp and along the edges of the swamp where the soils are seasonally inundated. Slope: N/A. Aspect: N/A. The underlying geology of this area is of Pleistocene origin and characterized as a Socastee Formation. This is a low coastal formation in the Carolinas like Penholoway but younger and lower in altitude. It is comprised primarily of unconsolidated, fine-detrital clay. It is described as variegated quartzose sands, argillaceous sands, and clays, 5 m thick at the type section near Socastee Swamp. (Source: USGS South Carolina Geologic Map Data.) The primary soil type in this collection area is classified as Rutlege Series loamy fine sand. Rutlege Series soils are very deep, very poorly drained soils that are sandy, siliceous, thermic Typic Humaquepts. Upper strata soils (0-38 cm) are black loamy sand with weak medium granular structure. They are loose and very strongly acid. Lower strata (38-175 cm) range from dark gray to dark brown sand that is single grained, loose, and very strongly acid. (Source: NRCS Web Soil Survey.)Wild material2159142NA 88714
346NA 88671RJL2023PA-005Rhododendron maximum L. Pennsylvania, United StatesNA2023COLLECTED10/16/2023Appalachian National Scenic Trail: Pulpit Rock and Pinnacle Loop. Rocky woodlands along Furnace Creek as well as steep rocky slopes above Pulpit Rock Reservoir associated with the Pulpit Rock and Pinnacle Loop Trail.40.59226100, -75.94588800301Well-drained and very rocky dry deciduous woodlands in part shade to full shade. Slope: 0-30%. Aspect: variable. The underlying geology of this area is of Silurian origin and characterized as the Shawangunk Formation. It is characterized by light- to dark-gray, fine- to very coarse-grained sandstone and conglomerate containing thin shale interbeds. Includes four members, in descending order: Tammany--conglomerate and sandstone; Lizard Creek--sandstone and red or green shale; Minsi--sandstone and conglomerate; Weiders--conglomerate. Tammany and Lizard Creek Members together are approximately equivalent to Clinton Group to the west; Minsi and Weiders Members together are equivalent to Tuscarora Formation to the west. (Source: USGS Pennsylvania Geologic Map Data). The primary soil type in the collection area is classified as Hazleton Series. The Hazleton series consists of deep and very deep, well drained soils formed in residuum of acid gray, brown or red sandstone on uplands. Slope ranges from 0 to 80 percent. Permeability is moderately rapid to rapid. Solum thickness ranges from 60 to 120 centimeters. Depth to lithic contact ranges from 1 to 2 meters. Rock fragments of angular sandstone, dominantly less than 25 cm in size, range from 5 to 70 percent in individual horizons. Boulders, stones, flags and channers cover about 5 to 60 percent of the surface of some pedons. Reaction ranges from strongly acid through extremely acid throughout. (Source: NRCS Web Soil Survey).Wild material2159062NA 88671
347NA 88672RJL2023PA-006Rhododendron periclymenoides (Michx.) Shinners Pennsylvania, United StatesNA2023COLLECTED10/16/2023Appalachian National Scenic Trail: Pulpit Rock and Pinnacle Loop. Rocky woodland edges above Furnace Creek around Pulpit Rock and Pinnacle Loop Trail.40.58668200, -75.94269600247Well-drained and very rocky dry deciduous woodlands in part shade to full shade. Slope: 10%. Aspect: East. The underlying geology of this area is of Silurian origin and characterized as the Shawangunk Formation. It is characterized by light- to dark-gray, fine- to very coarse-grained sandstone and conglomerate containing thin shale interbeds. Includes four members, in descending order: Tammany--conglomerate and sandstone; Lizard Creek--sandstone and red or green shale; Minsi--sandstone and conglomerate; Weiders--conglomerate. Tammany and Lizard Creek Members together are approximately equivalent to Clinton Group to the west; Minsi and Weiders Members together are equivalent to Tuscarora Formation to the west. (Source: USGS Pennsylvania Geologic Map Data). The primary soil type in the collection area is classified as Hazleton Series. The Hazleton series consists of deep and very deep, well drained soils formed in residuum of acid gray, brown or red sandstone on uplands. Slope ranges from 0 to 80 percent. Permeability is moderately rapid to rapid. Solum thickness ranges from 60 to 120 centimeters. Depth to lithic contact ranges from 1 to 2 meters. Rock fragments of angular sandstone, dominantly less than 25 cm in size, range from 5 to 70 percent in individual horizons. Boulders, stones, flags and channers cover about 5 to 60 percent of the surface of some pedons. Reaction ranges from strongly acid through extremely acid throughout. (Source: NRCS Web Soil Survey).Wild material2159063NA 88672
348NA 88676RJL2023PA-010Staphylea trifolia L. Pennsylvania, United StatesNA2023COLLECTED10/25/2023Seed collected along the Appalachian National Scenic Trail, accessed from the Duncannon Entrance.40.38132600, -77.02965700103Well-drained and very rocky deciduous woodlands where soil has accumulated in part shade to full shade. Slope: 0-30%. Aspect: variable. The underlying geology of this area is of Devonian origin and characterized as the Duncannon Member of Catskill Formation. It is characterized by grayish-red sandstone, siltstone, and mudstone in fining-upward cycles; conglomerate occurs at base of some cycles. The sandstones which comprise the Duncannon Member are fine to very coarse grained and grayish red to grayish red-purple in color. The Duncannon Member is known to be crossbedded to planar bedded in beds anywhere from 3 to 9 meters thick. Conglomerates have been spotted at the base of the Duncannon Member. The Duncannon Member is poorly exposed in most areas except along the Lehigh River. The conglomerate portion of this member has been known to form ridges and ledges with thicknesses approaching 228 meters. (Source: USGS Pennsylvania Geologic Map Data). The primary soil type in the collection area is classified as Hazleton Series. The Hazleton series consists of deep and very deep, well drained soils formed in residuum of acid gray, brown or red sandstone on uplands. Slope ranges from 0 to 80 percent. Permeability is moderately rapid to rapid. Solum thickness ranges from 60 to 120 centimeters. Depth to lithic contact ranges from 1 to 2 meters. Rock fragments of angular sandstone, dominantly less than 25 cm in size, range from 5 to 70 percent in individual horizons. Boulders, stones, flags and channers cover about 5 to 60 percent of the surface of some pedons. Reaction ranges from strongly acid through extremely acid throughout. (Source: NRCS Web Soil Survey).Wild material2159067NA 88676
349NA 88678RJL2023PA-012Viburnum acerifolium L. Pennsylvania, United StatesNA2023COLLECTED10/27/2023Slopes on the east side of Creek Road above the North Branch of White Clay Creek.39.78552600, -75.8025190090Well-drained mesic-dry to rocky dry deciduous woodlands in part shade to full shade. Slope: 15-35%. Aspect: West to northwest. The underlying geology of this area includes two formations. The first and primary formation is Lower Paleozoic Glenarm Wissahickon Formation, lithologically similar to oligoclase-mica schist of the Wissahickon Formation, but also includes lenticular amphibolite bodies having ocean-floor basalt chemistry. The second formation is Lower Paleozoic Mafic Gneiss Formation that is dark and medium grained. It includes rocks of probable sedimentary origin. (Sources: USGS Pennsylvania Geologic Map Data). The primary soil type in the collection area is classified as Manor Series. The Manor Series consists of well-drained residuum weathered from micaceous schist. Soils in the upper pedon (0-33 cm) are very dark grayish brown loam with strong fine granular structure; also, very friable with fine mica flakes and strongly acid. Lower pedon soils (34-56 cm) are strong brown, sandy loams. They have weak medium sub-angular blocky structure, are friable with many fine and a few medium mica flakes; this pedon is very strongly acid. (Source: NRCS Web Soil Survey).Wild material2159069NA 88678
350NA 88679RJL2023PA-013Rhododendron prinophyllum (Small) Millais Pennsylvania, United StatesNA2023COLLECTED10/30/2023Southwest side of Dutch Mountain Road north of Pine Marsh Creek in Pennsylvania State Game Lands Number 66.41.48201500, -76.27286000602Moist, well-drained habitat with good organic matter in part shade on a wooded slope next to the road. Slope: 5-10%. Aspect: East. The underlying geology of this area is of Mississippian origin and characterized as the Burgoon Formation. It is comprised of buff, medium-grained, cross bedded sandstone that includes shale and coal. In some places, it contains conglomerate at base as well as occasionally contains plant fossils; equivalent to Pocono Formation of Ridge and Valley province. (Source: USGS Pennsylvania Geologic Map Data). The primary soil type in the collection area is classified as Wellsboro Series. The Wellsboro Series consists of very deep, moderately well- and somewhat poorly-drained soils formed in till derived from red sandstone, siltstone, and shale. Slope ranges from 0 to 50 percent. Saturated hydraulic conductivity is moderately high or high in the mineral surface layer, subsurface layer, and upper part of the subsoil; and low or moderately low in the lower part of the subsoil (fragipan) and the substratum. Solum thickness is greater than 102 cm. Depth to the fragipan ranges from 36 to 76 cm. Depth to bedrock is 152 cm or more. Rock fragments of subangular and rounded sandstone, siltstone or shale range from 5 to 40 percent in the A and B horizons, and from 15 to 50 percent in the Bx and C horizons. Typically, rock fragments average about 5 to 25 percent by volume above the fragipan and 15 to 40 percent by volume in and below the fragipan. Reaction commonly ranges from very strongly acid through moderately acid. (Source: NRCS Web Soil Survey).Wild material2159070NA 88679
351NA 88681RJL2023PA-015Ilex verticillata (L.) A. Gray Pennsylvania, United StatesNA2023COLLECTED10/30/2023Wetlands near Phillips Creek: seed collected from plants on the north and south (further east) side of Pennsylvania Route 188 approximately 6.9 kilometers east of the junction with Pennsylvania Route 487.41.30353100, -76.22452800381Boggy to moist habitats associated with wetlands of Phillips Creek in shade to full sun next to the road. Slope: 0%. Aspect: various. The underlying geology of this area is of Devonian origin and characterized as the Catskill Formation. It is comprised of grayish-red sandstone, siltstone, shale, and mudstone; units of gray sandstone occur in upper part; lithologies in upper part arranged in fining-upward cycles. In the Altoona area, the Catskill Formation is mapped as the Duncannon, Sherman Creek, and Irish Valley Members, which are described under "Central and Eastern Pennsylvania" provinces. (Source: USGS Pennsylvania Geologic Map Data). The primary soil type in the collection area is classified as Wellsboro Series. The Wellsboro Series consists of very deep, moderately well- and somewhat poorly-drained soils formed in till derived from red sandstone, siltstone, and shale. Slope ranges from 0 to 50 percent. Saturated hydraulic conductivity is moderately high or high in the mineral surface layer, subsurface layer, and upper part of the subsoil; and low or moderately low in the lower part of the subsoil (fragipan) and the substratum. Solum thickness is greater than 102 cm. Depth to the fragipan ranges from 36 to 76 cm. Depth to bedrock is 152 cm or more. Rock fragments of subangular and rounded sandstone, siltstone or shale range from 5 to 40 percent in the A and B horizons, and from 15 to 50 percent in the Bx and C horizons. Typically, rock fragments average about 5 to 25 percent by volume above the fragipan and 15 to 40 percent by volume in and below the fragipan. Reaction commonly ranges from very strongly acid through moderately acid. (Source: NRCS Web Soil Survey).Wild material2159072NA 88681
352Ames 36185APS/BP/2023/076/286Betula populifolia Marshall Indiana, United StatesNC7LEAF2023COLLECTED11/02/2023Indiana Dunes State Park just 3.40 miles northeast of Chesterton, T37N R5W NE 1/4 SE 1/4 SW 1/4 Sec. 1841.65352700, -87.03831500186Low depressions with some standing water. Woodland edge.Wild materialRepresents a disjunct population in northwest Indiana and the extreme western edge of the species native range. Trees sampled in nature averaging 30-45' in height with trunks ranging from 3" up to 8" DBH. Bark dull-white to grey. Typically multi-stemmed trunks. Leaves with acuminate tips and branches with typically one male catkin at terminal end of branches, but occassionally two male catkins. 2159042Ames 36185
353Ames 36209JDC/EM/2023/089/1121Eutrochium maculatum (L.) E. E. Lamont Iowa, United StatesNC72023COLLECTED10/19/2023Located approximately 3.15 miles west of Grinnell, T80N R17W SE 1/4 SE 1/4 NE 1/4 Sec. 14.41.73894000, -92.78670000271Wet, remnant prairie.Wild materialPlants in nature at collection site measuring approximately 3.5-5.0 feet in height. 2165627Ames 36209
354NA 88667RJL2023PA-004Viburnum acerifolium L. Pennsylvania, United StatesNA2023Wild material2158816NA 88667
355NA 88666RJL2023PA-003Hamamelis virginiana L. Pennsylvania, United StatesNA2023COLLECTED10/01/2023Collected primarily along the woodland edge along Northside Road on Pennsylvania State Gamelands No. 43 as well as a few on nearby roads.40.17974200, -75.76790700176Plants were growing in mesic well-drained conditions on moderately sloping sites of a deciduous upland forest. This species grows well in shade to part-sun. Most abundant fruit development is found where plants are exposed to sunlight for a portion of the day. Slope: 15%. Aspect: North-northwest. The underlying geology of this area is of Precambrian origin and characterized as the Graphitic Felsic Gneiss. This includes Pickering Gneiss and small areas of marble; dominantly quartz and feldspar with varying amounts of graphite and various metamorphic minerals; medium grained, light to dark gray and greenish gray; sedimentary origin. (Source: USGS Pennsylvania Geologic Map Data.) The primary soil type in the area of this collection is classified as Gladstone Gravelly Loam Series (8 to 15 percent slopes). The Gladstone Series consists of very deep, well drained soils formed in residuum and colluvium from granitic gneiss. Saturated hydraulic conductivity is moderately high to high. Solum thickness ranges from 75 to 125 cm. Depth to granitic gneiss bedrock is 1.6 meters or more. The bedrock may be strongly weathered in the upper part. Gravel content ranges from 5 to 35 percent throughout the solum, and 10 to 40 percent in the C horizons. Fragments, larger than 3 inches in diameter, range from 0 to 20 percent by volume in the surface layer and 0 to 10 percent in the subsoil and substratum layers. Reaction is strongly or very strongly acid throughout the soil, unless limed. Areas that have been limed range to moderately acid in the upper part of the profile. (Source: NRCS Web Soil Survey.)Wild material2158815NA 88666
356NA 88665RJL2023PA-002Ilex verticillata (L.) A. Gray Pennsylvania, United StatesNA2023COLLECTED10/01/2023Woodlands along Pine Creek near the Harmonyville Road bridge.40.18764500, -75.76732200141Moist to mucky, wet woodland conditions along Pine Creek. Much of the site is very wet due to recent rains; though, earlier in the year, the soils were only moist. Plants grow in both well-drained mesic conditions as well as seasonally wet conditions. They do not grow in standing water anywhere in this location. Plants in this population are found mostly in the shade and partial shade of deciduous trees; there are occasional gaps that offer higher light conditions as well. Slope: 0-2%. Aspect: N/A. The underlying geology of this area is of Precambrian origin and characterized as the Graphitic Felsic Gneiss. This includes Pickering Gneiss and small areas of marble; dominantly quartz and feldspar with varying amounts of graphite and various metamorphic minerals; medium grained, light to dark gray and greenish gray; sedimentary origin. (Source: USGS Pennsylvania Geologic Map Data). The primary soil type in the area of this collection is classified as Hatboro Silt Loam Series. The Hatboro Series consists of very deep and poorly drained soils formed in alluvium derived from metamorphic and crystalline rock. They are on flood plains. Slopes range from 0 to 3 percent. Saturated hydraulic conductivity is moderately high to high. Solum thickness ranges from 50 to 150 cm. Depth to bedrock ranges from 1.5 to 3 meters or more. Organic carbon decreases irregularly with depth or is greater than 0.2 percent directly above any strongly contrasting C horizon. The depth to strongly contrasting sand and gravel is more than 100 cm or the transition is greater than 12.5 cm. Content of gravel ranges from 0 to 10 percent in the solum and from 0 to 80 percent in the C horizon. Mica flakes are common in the solum, and the C horizon contains thin lenses of mica. Reaction ranges from very strongly acid through neutral to a depth of 75 cm and from moderately acid through slightly acid below 75 cm. (Source: NRCS Web Soil Survey.)Wild material2158814NA 88665
357NA 88664RJL2023PA-001Viburnum acerifolium L. Pennsylvania, United StatesNA2023COLLECTED10/01/2023Seed collected from plants growing along a two-mile stretch of Harmonyville Road on the woodland edge next to the road. [Note: latitude and longitude were collected at the location of the largest seed collection.]40.18482200, -75.78145100158Plants were growing in well-drained and rocky mesic-dry woodlands from part shade along the road edge to full shade in the understory of the woodlands. Slope: 2-10%. Aspect: Variable. The underlying geology of this area is of Triassic origin and characterized as the Stockton Formation. It is characterized by light-gray to buff, coarse-grained, arkosic sandstone; includes reddish-brown to grayish-purple sandstone, siltstone, and mudstone. (Source: USGS Pennsylvania Geologic Map Data.) The primary soil type in the area of this collection is classified as Edgemont Channery Sandy Loam Series (8 to 25 percent slopes), extremely stony. The Edgemont Series consists of deep and very deep, well drained soils formed in the weathered residuum of quartzitic rocks. They have moderately high to high saturated hydraulic conductivity. Slopes range from 0 to 70 percent. Solum thickness ranges from 50 to 10 cm. Depth to bedrock ranges from about 1.5 to 2.2 meters. Kaolinite is the dominant mineral in the clay fraction with detectable amounts of illite, vermiculite, montmorillonite, chlorite and interstratified clays. Gravel, channers, and stone size fragments of quartzite and quartz are present throughout the profile. Rock fragments range from 5 to 40 percent in the horizons of the solum and from 10 to 90 percent in the C horizon. Reaction ranges from extremely acid to strongly acid throughout. (Source: NRCS Web Soil Survey.)Wild material2158813NA 88664
358Ames 36181Turtlehead FenEutrochium maculatum (L.) E. E. Lamont Iowa, United StatesNC72023COLLECTED09/29/2023Turtlehead Fen (Chichaqua Bottoms Greenbelt) located 1.75 miles southeast of Farrar just north of highway 65, T81N R21W SW ¼ NW ¼ Sec. 31.41.78610000, -93.34730000290Remnant fen with extremely wet, spongy soils and surface water visible at time of collection.Wild materialPlants in nature ranged in height from three to eight feet. Variation was also noted for phenology with some plants mostly dispersed and some just ripening at the time of collection.2159013Ames 36181
359WLP 3348AS/VO/2023/074/284Viburnum opulus L. var. americanum Aiton Minnesota, United StatesNAFRUIT2023COLLECTED09/23/2023Between Itasca State Park and White Earth State Forest, from 0.75 to 2.5 miles north of State Highway 113. Along McKenzie Road and Anchor Hill Road, T143N R37W Sections 22, 28, 30 and 31.47.16689300, -95.42134000515Understory of mixed forest in wetland complex. Near southern edge of transition zone from temperate to boreal forest.Wild materialVariation was noted for timing of fall color with some plants still green and others nearing peak display.2159012WLP 3348
360NA 88609KY23-011Hamamelis virginiana L. Kentucky, United StatesNA2023COLLECTED09/09/2023Black Mountain summit: along roadside on Black Mountain (Lynch property). (Second location, bulked with first: Black Mountain summit.)36.91584000, -82.894790001241Along roadside. Elevation: 4072 feet. Aspect: Northwest. (Second location, bulked with first: Elevation: 4120 feet. Aspect: North.)Wild material2158701NA 88609
361NA 88611KY23-013Acer pensylvanicum L. Kentucky, United StatesNA2023COLLECTED09/09/2023Black Mountain summit, along gas pipeline road.36.91742000, -82.902790001237Along gas line trail. Elevation: 4058 feet. Aspect: Southwest.Wild material2158703NA 88611
362NA 88639KY23-042Lyonia ligustrina (L.) DC. Kentucky, United StatesNA2023COLLECTED09/11/2023Daniel Boone National Forest: Bee Rock Loop Trail along Rockcastle River.37.04179000, -84.31805000233Riverscour grassland. Elevation: 765 feet. Aspect: East.Wild material2158731NA 88639
363NA 88640KY23-043Ilex verticillata (L.) A. Gray Kentucky, United StatesNA2023COLLECTED09/11/2023Daniel Boone National Forest: Bee Rock Loop Trail along Rockcastle River.37.04179000, -84.31805000233Riverscour grassland. Elevation: 765 feet. Aspect: East.Wild material2158732NA 88640
364NA 88641KY23-044Physocarpus opulifolius (L.) Maxim. Kentucky, United StatesNA2023COLLECTED09/11/2023Daniel Boone National Forest: Bee Rock Loop Trail along Rockcastle River.37.04179000, -84.31805000233Riverscour grassland. Elevation: 765 feet. Aspect: East.Wild material2158733NA 88641
365NA 88647KY23-051Stewartia ovata (Cav.) Weath. Kentucky, United StatesNA2023COLLECTED09/12/2023Daniel Boone National Forest: Marsh Creek south of KY-478.36.71494000, -84.35537000319Right off the road at bridge, along stream edge of Coddle branch of Marsh Creek, west side [is part of] Daniel Boone National Forest. Elevation: 1045 feet. Aspect: East.Wild material2158740NA 88647
366WLP 3214TXWL2023-002Stewartia malacodendron L. Texas, United StatesNA2023COLLECTED08/27/2023Little Cow Creek.31.06090300, -93.79570300Mesic mixed hardwood-pine forest adjacent to riparian area. Some blowdown evident.Wild material2158758WLP 3214
367WLP 3215TXWL2023-003Stewartia malacodendron L. Texas, United StatesNA2023COLLECTED08/27/2023Little Cow Creek.31.06228800, -93.79734300Mesic mixed hardwood-pine forest adjacent to riparian area. Some blowdown evident.Wild material2158759WLP 3215
368WLP 3345AS/SG/2023/025/235Styrax grandifolius Aiton Arkansas, United StatesNAFLOWER2023COLLECTED08/27/2023Ouachita National Forest - Winona Wildlife Management Area/South Fourche Botanical Area. Approximately 20 miles southwest of Danville, along County Road 362, east of Scenic Highway 7. T3N R20W Sec. 23.34.89619000, -93.10769400275Uplands and on bluffs; understory of pine-hardwood forest.Wild materialPlants in nature are large, clonally spreading colonies to 20 feet in height and similar width. Peak bloom occurred the last week of April (2023).2158786WLP 3345
369Ames 36138Muscatatuck NWRPopulus heterophylla L. Indiana, United StatesNC7PLANT2023COLLECTED05/30/2023Muscatatuck National Wildlife Refuge located 4.37 miles east, southeast of Seymour, T6N R6E SW 1/4 Sec. 2438.94292000, -85.81076600159Edge of stagnant swamp along road. Soils rather mucky/heavy clay.Wild materialNative to North America, this deciduous tree has a native range that covers the Atlantic coastal plain concentrated in the Carolinas and also along the Mississippi and Ohio Rivers along with various, tiny disjunct populations widely scattered across the southeast U.S. (Little, 1971). As an obligate wetland plant, the soils that this species inhabits is typically heavy clay (ranging 24 to 65%) and slightly acidic (soil pH ranges from 4.6 to 5.9) (Johnson 1990). Typical habitat is bottomlands/floodplains that generally have standing, shallow water. Sites that are often too wet for P. deltoides are suitable for P. heterophylla. Swamp Cottonwood can reach 10-20 meters in height and generally has an upright, rounded form. Broadly ovate leaves are rather large reaching up to 25 cm in length and nearly 15 cm wide with abaxial surfaces usually pubescent to partially glabrate. As with many other species in Salicaceae, P. heterophylla is dioecious with staminate and pistillate catkins appearing in early spring and reaching up to 10 and 15 cm in length, respectively. Seeds are dispersed in spring through early summer. Swamp Cottonwood is distinguishable from other Populus largely due to the distinctly cordate leaf bases and distinctive orange-brown pith in young twigs (McMaster 2003). Ornamental characteristics include golden yellow fall color. This taxon is essentially non-existent in the nursery trade and extremely rare in botanical garden and arboretum collections. Due to this species ability to grow in anaerobic, soils heavy in clay, this species may perform well in the typical urban landscape. Its potential to withstand extreme, drought despite being an obligate wetland plant may be similar to that found in Taxodium distichum. Genetics of this accession were collected in southern Indiana. Specimens sampled in nature were approximately 40-50' in height and were clonally (vegetative) spreading by rhizomes. 2158343Ames 36138
370OPGC 8815CBG- 10787Maianthemum racemosum (L.) Link subsp. racemosum Wisconsin, United StatesOPGC2023Wild material2142251OPGC 8815
371W6 61417CBG- 10852Verbesina alternifolia (L.) Britton ex Kearney Illinois, United StatesW6SEED2023Wild material2142299W6 61417
372W6 61418CBG- 10853Agastache scrophulariifolia (Willd.) Kuntze Illinois, United StatesW6SEED2023Wild material2142300W6 61418
373Ames 36018AS/SL/2023/003/213Salix lucida Muhl. Wisconsin, United StatesNC7LEAF2023COLLECTED02/25/2023Located just west of Kempster approximately 4.65 miles along County Road J (floodplains of Sucker Creek and West Branch Eau Claire River), T33N R10E Sec. 32, 33, and 34 (extreme southern edges)45.29205000, -89.27304100479WetlandWild materialSalix lucida (shining willow) is referenced as a tall shrub or small tree with multiple trunks with the potential to reach 6 meters in height. Shining willow frequents wetland habitats such as swampy lakes, wet meadows and along rivers. Noted for it's extremely shiny, long (e.g. 7-14 cm) leaves with very elongated, acumiate leaf tips and conspicuous, enlarged glands clustered at the end of the petiole. First year branches are very glabrous and bright yellow to bright orange in color. Flowering tends to occur later in spring in comparison to other shrubby willows e.g. Salix discolor, Salix humilis, Salix petiolaris, and Salix eriocephala. Shining willow can often be confused with Salix serissima, but the presence of glands at the base of the petiole, the colorful first year stems (most noticeable in winter) of Salix lucida can be used to separate them. The native distribution of Salix lucida is concentrated in the northeastern U.S. with scattered disjuncts as far west as North Dakota and as far south as the northern tier of counties in Illinois, Indiana, and Ohio (Little, E. L. Jr. 1977). This accession represents genetics from northeastern Wisconsin. Specimens sampled in nature measuring approximately 6' in height with bright orange-yellowish stem colors on most recent year's growth.2141551Ames 36018
374Ames 36019AS/SD/2023/004/214Salix discolor Muhl. Wisconsin, United StatesNC7PLANT2023COLLECTED02/25/2023Located along County Road J west of Kempster and County Road T/County Road H west of Summit Lake.45.29210300, -89.27334900478WetlandWild materialThe native range of Salix discolor is concentrated in the northeastern United States and also throughout southern Canada (Little, E. L. Jr. 1977). Generally adapted/tolerant to wet soils this species is often found in meadows, fens, swamps, and streambanks. Attractive ornamental characteristics includes early spring, showy flowers and yellow foliage in the fall. Salix discolor provides a critical source of pollen at the beginning of the growing season for a plethora of pollinators and also serves as a larval host to many insect species. Salix discolor are commonly used in the cut flower industry for both their showy catkins and colorful, dormant winter stems. This accession represents genetics from central Wisconsin. Plants in nature measuring approximately 8-10' in height occassionally up to 25' with brown to red-brown stem colors on most recent year's growth. Some genotypes with dense pubescence on stems while others are glabrous.2141552Ames 36019
375Ames 36021AS/SP/2023/006/216Salix petiolaris Sm. Wisconsin, United StatesNC7PLANT2023COLLECTED02/25/2023Located just west of Kempster approximately 5.25 miles along County Road J (floodplain between Sucker Creek and West Branch Eau Claire River), T33N R10E Sec. 32 and 33 (extreme southern edges).45.29239600, -89.27583700478WetlandWild materialSlender-leaved willow, Salix petiolaris, is a somewhat dense suckering shrub that can reach up to 10' in height with slender stems that branch minimally, but typically maintains a height of 5-8'. Native to North America, the native range covers mostly the northeastern US stretching from Maine to western North Dakota and Canada south to central Iowa (Little, E. L. Jr. 1977). Salix petiolaris typically dominates wetland areas including sedge meadows, marshes, riverbanks, and lake shores. Despite favoring wet habitats, it can also be found in dry, upland areas, especially those with high-water tables. However, longevity is generally limited in upland habitats. S. petiolaris, similar to other willow species, responds well to fire, coppicing, or heavy browsing (highly favored by deer) by sprouting new stems close to the crown. In cultivation, plants after five years will encompass a 5' x 5' area due to stems that arch from the main base of the plant. Coppicing of plants to ground level is highly recommended either annually or once every 3-5 years to maintain vigorous growth and plant health. This species requires substantial to full sun exposure and is an excellent choice for streambank stabilizations and windbreaks to reduce soil erosion and drifting snow, respectively. This accession represents genetics from central Wisconsin. Plants noted in nature measuring up to 6' in height. Very densely suckering clumps occassionally reaching up to 10' in diameter. Stem colors on most recent year's growth varied from orange-yellow, red (predominate), to yellow. Petioles are minutely hairy.2141554Ames 36021
376Ames 36022AS/SA/2023/007/217Spiraea alba Du Roi Wisconsin, United StatesNC7PLANT2023COLLECTED02/25/2023Located on the northeastern edge of Monico (Monico Creek floodplain) on east side of State Highway 45, T36N R11E NW 1/4 Sec. 2945.57830700, -89.14922800491WetlandWild materialPlants in nature measuring up to 6' in height with a clump forming habit.2141555Ames 36022
377Ames 36023AS/VO/2023/008/218Viburnum opulus L. var. americanum Aiton Wisconsin, United StatesNC7FRUIT2023COLLECTED02/25/2023Two areas sampled including (#1) located just northeast of Pelican Lake on east side of State Highway 45, T35N R11E NW ¼ NE ¼ Sec. 18 and (#2) located on the northeastern edge of Monico (Monico Creek floodplain) on east side of State Highway 45, T36N R11E NW ¼ Sec. 29.45.52491900, -89.16179900488WetlandWild materialFormerly 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). This accession represents genetics from northeastern Wisconsin. Specimens sampled in nature noted as having bright red fruits with slight sweet taste. Based on fruit taste, this accession is currently (2026) being listed as V. opulus var. americanum. 2141556Ames 36023
378Ames 36024AS/FN/2023/011/221Fraxinus nigra Marshall Wisconsin, United StatesNC7PLANT2023COLLECTED02/26/2023Located just north of Leland approximately 0.70 miles along Hemlock Road, T10N R5E SW 1/4 NW 1/4 Sec. 1843.34472800, -89.95099700242FloodplainWild materialSingle mother tree sample with signs of wood pecker damage on trunk.2141557Ames 36024
379Ames 35995Kauten FenSalix discolor Muhl. Iowa, United StatesNC7PLANT2023COLLECTED02/06/2023Kauten Fen, T92N R8W NE 1/4 of SW 1/4 of NE 1/4 Sec.16.42.78400000, -91.79050000345Closely followed gradient of drainage creek, approximately 10 yards to the west of the small drainage creek. 1 to 4 percent slope. Clyde-Floyd complex (clay loam); poorly drained soils. Water table at approximately 12 inches. Wild materialThe native range of Salix discolor is concentrated in the northeastern United States and also throughout southern Canada (Little, E. L. Jr. 1977). Generally adapted/tolerant to wet soils this species is often found in meadows, fens, swamps, and streambanks. Attractive ornamental characteristics includes early spring, showy flowers and yellow foliage in the fall. Salix discolor provides a critical source of pollen at the beginning of the growing season for a plethora of pollinators and also serves as a larval host to many insect species. Salix discolor are commonly used in the cut flower industry for both their showy catkins and colorful, dormant winter stems. This germplasm was collected as dormant cuttings from a northeastern Iowa site, Kauten Fen, which is a site boasting with Salix diversity. One could likely find just about any hybrid combination possible and observe a wide-diversity of morphology across hybrids and within species. Acquisition specifically targeted characters that were most characterstic of Salix discolor. Field observations of this accession grown in cultivation has shown this accession to be extremely vigorous. Established specimens coppiced at grown level generates very thick shoots reaching 7-8' in height in a single growing season. 2141279Ames 35995
380WLP 3085RM2023-003Hibiscus laevis All. Florida, United StatesNA2023COLLECTED10/01/2022This species is growing along the Escambia River and accessed by boat. 30.62930000, -87.258300001The plants were growing on stumps in full sun on the edge of a semi-alluvial area of the river.
Soils: The underlying geology of this area is classified as Alluvium, of Pleistocene/Holocene origin and consists of undifferentiated Quaternary sediments of varying thickness including siliciclastics, organics and freshwater carbonates. The siliciclastics are light gray, tan, brown to black, unconsolidated to poorly consolidated, clean to clayey, silty, unfossiliferous, variably organic-bearing sands to blue green to olive green, poorly to moderately consolidated, sandy, silty clays. Organics occur as plant debris, roots, disseminated organic matrix and beds of peat. Freshwater carbonates, often referred to as marls in the literature, are scattered.
Source: USGS Florida Geologic Map Data (https://mrdata.usgs.gov/geology/state/state.php?state=fl)
The surface soil profile of this area is primarily Chewacla-Wahee-Riverview Association. The Chewacla Series soils are dark yellowish brown silty clay loam soils, that are strongly acidic and somewhat poorly drained. They are soils of flood plains and streams subject to frequent flooding. The Wahee Series soils are dark gray clayey and loamy marine or fluviomarine sediments that are strongly acidic and somewhat poorly drained. The Riverview series consists of very deep, well drained, moderately permeable soils that formed in loamy alluvium on flood plains. Slopes range from 0 to 5 percent.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2141439WLP 3085
381NA 88524RM-TK2022-012Hydrangea quercifolia W. Bartram Florida, United StatesNA2023COLLECTED10/20/2022Private property of Joann Palmer on Reservation Court30.23775000, -84.324100005Plants 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 material2140805NA 88524
382NA 88552RJLSEUS2022-025Hydrangea quercifolia W. Bartram Alabama, United StatesNA2023COLLECTED12/12/2022Claiborne 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, -87.5141640040Plants 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 material2140779NA 88552
383NA 88557RJLSEUS2022-030Ilex longipes Chapm. ex Trel. Alabama, United StatesNA2023COLLECTED12/12/2022Silver Creek Lake Campground off of Silver Creek Lake Road: woodland slopes below the hilltop parking lot leading down to the campground.31.66442800, -87.5746140039Part shade of moist-mesic, mixed deciduous and evergreen woodland on dry, well-drained bank, 1-2 meters above a small spring-fed creek. The underlying geology of this area is Claiborne Group, Tallahatta Formation, of Eocene origin, with white to very light-greenish-gray thin-bedded to massive siliceous claystone; interbedded with thin layers of fossiliferous clay, sandy clay, and glauconitic sand and sandstone. (Source: USGS Alabama Geological Map Data). The primary soil types in the collection area are classified as Arundel-Cantuche Complex soils (15 to 35 percent slopes). The Arundel Series consists of moderately deep, well drained, very slowly permeable soils on dissected uplands of the Southern Coastal Plain. They formed in marine deposits consisting of acid clays underlain by horizontally bedded sandstone, buhrstone and siltstone. These soils are strongly acid. Slopes range from 2 to 60 percent. The Cantuche Series consists of shallow, well drained, moderately permeable soils that formed over horizontally bedded claystone. These soils are on narrow ridgetops and narrow benches on steep side-slopes of dissected landscapes in the Coastal Plain. They are strongly acid. Slopes range from 2 to 35 percent. (Source: NRCS Web Soil Survey).Wild material2140818NA 88557
384NA 88569RJLSEUS2022-042Ilex hybr.Florida, United StatesNA2023COLLECTED12/15/2022Yellow River: this plant is growing on the edge of the Yellow River and accessed by boat. This collection located approximately 0.4 kilometers north of the Yellow River Boat Ramp on the east side of Florida State Hwy 87.30.57317600, -86.923675001This plant was found growing in full sun in permanently saturated to submersed conditions along the edge of the Yellow River, growing in an open river edge with no overstory. Like most of the plants along the river, this collection is adapted to acidic conditions and while the aquatic habitats are generally fresh water, there can occasionally be tidal or hurricane-caused saltwater intrusions. 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 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).Wild materialIlex putative natural hybrid (I. myrtifolia x I. opaca)2140823NA 88569
385NA 88570RJLSEUS2022-043Ilex myrtifolia Walter Florida, United StatesNA2023COLLECTED12/15/2022Yellow River: 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 87.30.58148800, -86.911219001Plants are typically found growing in full sun to part shade in permanently saturated to submersed conditions along the edge of the Yellow River, growing in association with a wide array of deciduous and evergreen trees, shrubs and perennial plant species. Most of the plants along the river are adapted to acidic conditions and, while the aquatic habitats are generally fresh water, there is occasionally tidal or hurricane-caused saltwater intrusions. 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 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).Wild material2140824NA 88570
386NA 88572RJLSEUS2022-045Ilex verticillata (L.) A. Gray Florida, United StatesNA2023COLLECTED12/15/2022Yellow River: 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 87.30.57947400, -86.919061001Plants are typically found growing in full sun to part shade in permanently saturated to submersed conditions along the edge of the Yellow River, growing in association with a wide array of deciduous and evergreen trees, shrubs and perennial plant species. Most of the plants along the river are adapted to acidic conditions and, while the aquatic habitats are generally fresh water, there is occasionally tidal or hurricane-caused saltwater intrusions. 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 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).Wild material2140825NA 88572
387NA 88573RJLSEUS2022-046Ilex myrtifolia Walter Florida, United StatesNA2023COLLECTED12/15/2022Yellow River: this plant is growing on the edge of the Yellow River and accessed by boat. This collection is located approximately 3.2 kilometers by boat north and east of the Yellow River Boat Ramp on the east side of Florida State Hwy 87.30.58188200, -86.912205001This plant is growing in full sun in permanently saturated conditions along the edge of the Yellow River, growing in association with a wide array of deciduous and evergreen trees, shrubs and perennial plant species. Most of the plants along the river are adapted to acidic conditions and, while the aquatic habitats are generally fresh water, there is occasionally tidal or hurricane-caused saltwater intrusions. 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 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).Wild materialorange-fruited form2140826NA 88573
388NA 88506RJL2022TX-001Itea virginica L. Texas, United StatesNA2022COLLECTED10/31/2022Plants 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, -93.762717001Plants 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 material2139813NA 88506
389NA 88507RJL2022TX-002Fraxinus caroliniana Mill. Texas, United StatesNA2022COLLECTED10/31/2022Plants 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, -93.752397001Plants 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 material2139814NA 88507
390NA 88508RJL2022TX-003Morella cerifera (L.) Small Texas, United StatesNA2022COLLECTED10/31/2022Plants 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, -93.752887001Plants 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 material2139815NA 88508
391NA 88514RJL2022MD-019Kalmia latifolia L. Maryland, United StatesNA2022COLLECTED11/04/2022Plants are growing on both sides of a fire road on Maryland Heights along the edge with Harpers Ferry National Historic Park. This location was accessed from the east where Miller Avenue meets the fire road, approximately 2 kilometers away. There is no vehicular access to the collecting area. Becoming locally uncommon. This local population is likely to be extirpated in the next 20-30 years. This collector has hiked through this area for more than 35 years and seen dramatic changes in the population. When first observed, Kalmia latifolia was a dominant understory shrub on south- to west-facing slopes beneath a mature forest canopy. Over the years, at least one forest fire has significantly reduced the population, along with a continuing increase in deer populations, resulting in catastrophic browse damage. The absence of a mature forest canopy and periods of drought have almost certainly also resulted in decline of this population. While collecting seed from scattered mature plants well above deer browse levels, this collector also noted that there was virtually no recruitment taking place.39.32811200, -77.72242400287Plants are growing in part-shade to shade of a deciduous upland, very rocky, and dry forest community. Plants are frequently found growing among boulders, rock outcrops, and steep-slope erosional areas, although, not exclusively.
Soils: The underlying geology of this area is of Late Cambrian to Cambrian origin and comprised of Chilhowee Group; Weverton Formation. This includes interbedded white to dark gray, thin-bedded, micaceous, ferruginous, and sericitic quartzites, phyllites, and white, thick-bedded, ledge-making quartzites; some gray to brown ferruginous quartz conglomerate and purple-banded phyllite.
Source: USGS Maryland Geologic Map Data https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=MDKp%3B5
The primary soil types in the collection area are classified as Dekalb-Bagtown-Rock outcrop complex, 25 to 65 percent slopes. The Dekalb series consists of moderately deep, excessively drained soils formed in material weathered from gray and brown acid sandstone in places interbedded with shale and graywacke. Slope ranges from 0 to 80 percent. Permeability is rapid. Solum thickness and depth to bedrock range from 50 to 100 cm. Flat, subangular or angular, sandstone fragments, 2.5-25 cm across increase with depth and range from 10-60 percent in individual horizons of the solum and from 50-90 percent or more in the C horizon. The amount of rock fragments typically increases with depth. Cobbly, channery, and very stony phases are common. Reaction ranges from extremely through strongly acid.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2139821NA 88514
392Ames 35934Powers LakeBetula pumila L. Minnesota, United StatesNC7SEED2022COLLECTED10/24/2022North of Powers Lake (Three Rivers Park District) located 6.25 miles southeast of Dayton, T120N R22W SW1/4 SE1/4 Sec. 27 and NE 1/4 Sec. 3445.16800600, -93.44795900261WetlandWild material2139697Ames 35934
393WLP 2670RJL2022PA-016Acer negundo L. Pennsylvania, United StatesNA2022COLLECTED10/21/2022Plants 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, -75.82609300105Plants 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 material2139661WLP 2670
394NA 89045RJL2022PA-013Tsuga canadensis (L.) Carrière Pennsylvania, United StatesNA2022COLLECTED10/07/2022Plants growing on the steep banks along Octoraro Creek accessed by canoe. Plants are locally common but generally infrequent along the Octoraro Creek. 39.74442700, -76.0885640066Plants are growing in part-shade to sun of mixed deciduous and evergreen forests on steep rocky habitats overlain by relatively deep soil over occasionally exposed geology along the Octoraro Creek.
Soils: The underlying geology of this area is estimated to be of lower Paleozoic origin and comprised of Peters Creek Schist. This is comprised of chlorite-sericite schist containing interbedded quartzite.
Source: USGS Pennsylvania Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=PAPZpc%3B0)
The primary soil types in the collection area are classified as Manor loam, 25 to 35 percent slopes, very stony. The soils in the collecting area originated as residuum, weathered from the micaceous schist exposed geology and are generally considered coarse-loamy, micaceous, mesic typic dystrudepts that are very acidic and well-drained. There is a variable depth of soil depending upon the steepness of slopes. Some areas contain significant exposed Peters Creek Schist overlain by a highly decomposed organic mat intermingled with a dense root mat of woody and herbaceous plants.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2139610NA 89045
395NA 89044RJL2022PA-012Rhododendron maximum L. Pennsylvania, United StatesNA2022COLLECTED10/07/2022Plants growing on the steep banks along Octoraro Creek accessed by canoe. Plants are locally common but generally uncommon along the Octoraro Creek. 39.75272200, -76.0827150063Plants are growing in part-shade to part-sun of mixed deciduous and evergreen forests on steep rocky habitats along the Octoraro Creek.
Soils: The underlying geology of this area is estimated to be of lower Paleozoic origin and comprised of Peters Creek Schist. This is comprised of chlorite-sericite schist containing interbedded quartzite.
Source: USGS Pennsylvania Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=PAPZpc%3B0)
The primary soil types in the collection area are classified as Manor loam, 25 to 60 percent slopes, very stony. The soils in the collecting area originated as residuum, weathered from the micaceous schist exposed geology and are generally considered coarse-loamy, micaceous, mesic typic dystrudepts that are very acidic and well-drained. There is a variable depth of soil depending upon the steepness of slopes. Some areas contain significant exposed Peters Creek Schist overlain by a highly decomposed organic mat intermingled with a dense root mat of woody and herbaceous plants.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2139609NA 89044
396Ames 35921Bear Creek Hemlocks State Natural AreaFraxinus nigra Marshall Wisconsin, United StatesNC7SEED2022COLLECTED09/28/2022Chequamegon National Forest, approximately 14 miles west of Medford. Along Winter Sports Road, north from intersection with State Highway 64, T31N R2W East edge of Sec. 32.45.11911600, -90.64690200403Edges of swamps; wet peat soil.Wild material2139684Ames 35921
397Ames 35922AS/BA/2022/071/202Betula alleghaniensis Britton Wisconsin, United StatesNC7PLANT2022COLLECTED09/29/2022Chequamegon National Forest, approximately nine miles southeast of Park Falls. Collected along North Gates Lake Road (one sample), Sailor Lake Road (two samples) and State Highway 70 (one sample), T38N R2E and T39N R1E.45.80979200, -90.27513800486Northern hardwood forest.Wild material2139685Ames 35922
398Ames 35924AS/FN/2022/073/204Fraxinus nigra Marshall Wisconsin, United StatesNC7SEED2022COLLECTED09/29/2022Chequamegon National Forest, approximately 4.5 miles south-southeast of Clam Lake along County Highway GG and adjacent Forest Service roads, T42N R4W Sec. 21.46.10020200, -90.87459600431Wet to saturated soils in northern hardwood forest.Wild material2139687Ames 35924
399Ames 35925AS/FN/2022/075/206Fraxinus nigra Marshall Wisconsin, United StatesNC7MISCELLANEOUS2022COLLECTED09/30/2022Approximately 9.3 miles north-northwest of Hayward along State Road 27, Wozny Road, John Waggoner Road and State Road 77. Collected in both Washburn and Sawyer Counties. Coordinates listed refer to the first plant sampled; coordinates for each specimen may be provided upon request. T42N R9W SW 1/4 SW 1/4 Sec. 5. 46.14354200, -91.52893600384Bogs and saturated soils in northern hardwood forest.Wild material2139688Ames 35925
400NA 88481RJL2022MD-002Kalmia latifolia L. Maryland, United StatesNA2022COLLECTED09/04/2022Plants growing at Elkton State Forest along roads and woodlands over a distance of approximately 5 kilometers labelled as the address of 717 Irishtown Rd, North East, MD 21901. Kalmia is very common along the unnamed gravel road as well as the understory of the upland woodlands.39.58852900, -75.9045290060Plants are growing in a mesic to dry, well-drained habitat of mixed deciduous and evergreen woodlands comprised primarily of acid-loving plants. Plants are growing in shade to part shade along the unnamed road as well as the woodlands. The soils in the collection area are generally described as a complex series of fluviomarine deposits. The soils range from a thin loam layer at the surface to varying levels of loam to sandy loam and/or extremely gravelly sandy clay loam strata, depending upon geographical location (ie. Hillslope summits, slopes, footslopes, swales, etc.). The primary soil types in the collection area are classified as Russett-Christiana-Hambrook Complex and/or Sassafras and Croom Soils; though, others may intersect and overlay in specific areas.Wild material2139360NA 88481
401NA 88482RJL2022MD-003Rhododendron periclymenoides (Michx.) Shinners Maryland, United StatesNA2022COLLECTED09/04/2022Plants growing at Elkton State Forest along roads and woodlands over a distance of approximately 5 kilometers labelled as the address of 717 Irishtown Rd, North East, MD 21901. Plants are found infrequently and scattered along the unnamed gravel road39.58852900, -75.9045290051Plants are growing in a mesic to dry, well-drained habitat of mixed deciduous and evergreen woodlands comprised primarily of acid-loving plants. Plants are growing in part shade. The soils in the collection area are generally described as a complex series of fluviomarine deposits. The soils range from a thin loam layer at the surface to varying levels of loam to sandy loam and/or extremely gravelly sandy clay loam strata, depending upon geographical location (ie. Hillslope summits, slopes, footslopes, swales, etc.). The primary soil types in the collection area are classified as Russett-Christiana-Hambrook Complex and/or Sassafras and Croom Soils; though, others may intersect and overlay in specific areas.Wild material2139361NA 88482
402NA 88483RJL2022MD-004Clethra alnifolia L. Maryland, United StatesNA2022COLLECTED09/04/2022Plants growing at Elkton State Forest along roads and woodlands over a distance of approximately 5 kilometers labelled as the address of 717 Irishtown Rd, North East, MD 21901. Plants are found regularly but scattered along the unnamed gravel road as well as in open understory of the upland woodlands. 39.58531200, -75.8956610047Plants are growing in a mesic to moist, well-drained habitat of mixed deciduous and evergreen woodlands comprised primarily of acid-loving plants. Plants are growing in part shade and open understory shade. The soils in the collection area are generally described as a complex series of fluviomarine deposits. The soils range from a thin loam layer at the surface to varying levels of loam to sandy loam and/or extremely gravelly sandy clay loam strata, depending upon geographical location (ie. Hillslope summits, slopes, footslopes, swales, etc.). The primary soil types in the collection area are classified as Russett-Christiana-Hambrook Complex and/or Sassafras and Croom Soils; though, others may intersect and overlay in specific areas.Wild material2139362NA 88483
403NA 88484RJL2022MD-005Aronia melanocarpa (Michx.) Elliott Maryland, United StatesNA2022COLLECTED09/04/2022Plants growing at Elkton State Forest on Elk Neck Trail #3 (Starkey Lane) labelled as the address of 717 Irishtown Rd, North East, MD 21901. This was the only plant observed during several visits to Elk Neck State Forest during early and mid-summer39.58531200, -75.8956610055Plants are growing in a mesic to dry, well-drained habitat of mixed deciduous and evergreen woodlands comprised primarily of acid-loving plants. Plants are growing in part shade to part-sun. The soils in the collection area are generally described as a complex series of fluviomarine deposits. The soils range from a thin loam layer at the surface to varying levels of loam to sandy loam and/or extremely gravelly sandy clay loam strata, depending upon geographical location (ie. Hillslope summits, slopes, footslopes, swales, etc.). The primary soil types in the collection area are classified as Russett-Christiana-Hambrook Complex and/or Sassafras and Croom Soils; though, others may intersect and overlay in specific areas.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild materialreceived as A. prunifolia, on further examination by collector it was determined to be A. melanocarpa2139363NA 88484
404NA 88485RJL2022MD-006Hamamelis virginiana L. Maryland, United StatesNA2022COLLECTED09/04/2022Plants growing at Elkton State Forest on Elk Neck Trail #3 (Starkey Lane) labelled as the address of 717 Irishtown Rd, North East, MD 21901. This species was infrequent throughout most of Elk Neck State Park, but relatively common.39.58790000, -75.8885310054Plants are growing in a mesic to dry, well-drained habitat of mixed deciduous and evergreen woodlands comprised primarily of acid-loving plants. Plants are growing in part shade to shade. The soils in the collection area are generally described as a complex series of fluviomarine deposits. The soils range from a thin loam layer at the surface to varying levels of loam to sandy loam and/or extremely gravelly sandy clay loam strata, depending upon geographical location (ie. Hillslope summits, slopes, footslopes, swales, etc.). The primary soil types in the collection area are classified as Russett-Christiana-Hambrook Complex and/or Sassafras and Croom Soils; though, others may intersect and overlay in specific areas.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2139364NA 88485
405NA 88488RJL2022PA-004Viburnum acerifolium L. Pennsylvania, United StatesNA2022COLLECTED09/03/2022Plants growing in woodlands on the east side of Shed Road in French Creek State Park. Plants are common and found scattered along the edges of the road and into the woodlands. 40.21969200, -75.77373600238Plants are growing in a mesic to dry, well-drained habitat of upland deciduous forest which is very rocky. The understory layer is generally not as rich due to the rock-laden ground layer. Plants are growing in part shade to shade. The underlying geology of this area is comprised of Hammer Creek Conglomerate, characterized by cobble and pebble quartz conglomerate interbedded with red sandstone.
Source: USGS Pennsylvania Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=PATRhc%3B2) The surface soil profile of this area is Joanna Loam (JpD), 8 to 25 percent slopes which is extremely stony. It is represented by residuum weathered from sandstone and/or residuum weathered from conglomerate. Joanna Loam is moderately to well-drained and 1.8 meters to 2.5 meters to the lithic bedrock described above.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2139367NA 88488
406NA 88489RJL2022PA-005Kalmia latifolia L. Pennsylvania, United StatesNA2022COLLECTED09/10/2022Plants are growing on the lands of Hawk Mountain Sanctuary. This species is very common and abundant. It is one of the most dominant understory plants in woodlands. This species is a common understory shrub throughout the entire region in upland dry woodland habitats.40.63862000, -75.99071200430Plants are growing primarily in shade to part-shade on a dry-mesic to very dry, well-drained upland/montane habitat characterized by upland mixed deciduous and evergreen forest that is very rocky. All of the plants found in this habitat go through periods of drought during the growing season due to the limited litter/soil layer in which moisture can be held. The underlying geology of this area is of Silurian origin and comprised of Shawangunk Formation. This formation is primarily light- to dark-gray, fine- to very coarse-grained sandstone and conglomerate containing thin shale interbeds.
Source: USGS Pennsylvania Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=PASs%3B14)
The surface soil profile of this area is the Hazleton series consists of deep and very deep, well drained soils formed in residuum of acid gray, brown or red sandstone on uplands. The matrix includes a considerable accumulation of thin, flat, coarse fragments of sandstone, limestone, or schist with diameters up to 15 cm. Slope ranges from 0-80%. Permeability is moderately rapid to rapid.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2139368NA 88489
407NA 88490RJL2022PA-006Ilex montana Torr. & A. Gray Pennsylvania, United StatesNA2022COLLECTED09/10/2022Hawk Mountain Sanctuary.40.64162200, -75.99122600420Plants are growing from shade to full sun on a dry-mesic to very dry, well-drained upland/montane habitat characterized by an upland mixed deciduous and evergreen forest that is very rocky. All of the plants found in this habitat go through periods of drought during the growing season due to the limited litter/soil layer in which moisture can be held. The underlying geology of this area is of Silurian origin and comprised of Shawangunk Formation. This formation is primarily light- to dark-gray, fine- to very coarse-grained sandstone and conglomerate containing thin shale interbeds. (Source: USGS Pennsylvania Geologic Map Data). The surface soil profile of this area is the Hazleton series consists of deep and very deep, well drained soils formed in residuum of acid gray, brown or red sandstone on uplands. The matrix includes a considerable accumulation of thin, flat, coarse fragments of sandstone, limestone, or schist with diameters up to 15 cm. Slope ranges from 0-80%. Permeability is moderately rapid to rapid. (Source: NRCS Web Soil Survey).Wild material2139369NA 88490
408NA 88491RJL2022PA-007Rhododendron maximum L. Pennsylvania, United StatesNA2022COLLECTED09/10/2022Plants are growing on the lands of Hawk Mountain Sanctuary. This species was common, but generally restricted to steep rocky outcrops.40.63813900, -75.98835200420Plants are growing from shade to full sun on a dry-mesic to very dry, well-drained upland/montane habitat characterized by an upland mixed deciduous and evergreen forest that is very rocky. Even so, most heavily fruited plants were growing in part shade to almost full sun. All of the plants found in this habitat go through periods of drought during the growing season due to the limited litter/soil layer in which moisture can be held. The underlying geology of this area is of Silurian origin and comprised of Shawangunk Formation. This formation is primarily light- to dark-gray, fine- to very coarse-grained sandstone and conglomerate containing thin shale interbeds.
Source: USGS Pennsylvania Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=PASs%3B14)
The surface soil profile of this area is the Hazleton series consists of deep and very deep, well drained soils formed in residuum of acid gray, brown or red sandstone on uplands. The matrix includes a considerable accumulation of thin, flat, coarse fragments of sandstone, limestone, or schist with diameters up to 15 cm. Slope ranges from 0-80%. Permeability is moderately rapid to rapid.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2139370NA 88491
409WLP 26122022VA-03Styrax grandifolius Aiton Virginia, United StatesNA2022COLLECTED09/12/2022Northwest River Park on the south side of Indian Springs Road behind the Equestrian Center along a bridle trail. This plant is a common in the mesic woodlands at this location.36.58361100, -76.1627780021Plants growing in shade to part-shade of the mixed deciduous and evergreen mesic woodland about 1 to 2 meters above a nearby wetland area.
The underlying geology of this area is the Tabb Formation of Quaternary origin which is comprised of undifferentiated sand, silt, and peat and subdivided into three members. Within the Tabb Formation lies the Lynnhaven Member with pebbly and cobbly, fine to coarse gray sand grades upward into clayey and silty fine sand and sandy silt. Extensive low lands bounded on the landward side by river-, bay-, and ocean-facing scarps having toe altitudes of 5-6 meters. Thickness is 0 to 6.5 meters.
Source: USGS Virginia Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=VAQtl%3B0)
The surface soil profile of this area is Chapanoke-Yeopim complex, 0 to 3 percent slopes. These soil as somewhat poorly to moderately drained, acidic, and found on marine terraces and summits of low elevation coastal plain areas. They are comprised of silt loam, silty clay loam, sandy clay loam and loam in varying quantities across the profile; the depth to parent geology is approximately 200 cm.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx		Wild material2139350WLP 2612
410WLP 26142022VA-05Euonymus americanus L. Virginia, United StatesNA2022COLLECTED09/12/2022In Colonial Williamsburg, park in the Providence Hall Directors Wing parking lot and enter the Bassett Trace Nature Trail; this species is found in the woodlands on either side of the trail and over a bridge until the it turns right. This plant is infrequent, but occasionally found in the mesic woodlands throughout this location.37.26681600, -76.6925280021Plants growing in shade to part-shade of the mixed deciduous and evergreen mesic woodland. This species is generally growing in areas with an abundant organic, mature woodland that is relatively undisturbed.
The underlying geology of this area is Windsor Formation of Tertiary-Quaternary origin (lower Pleistocene or upper Pliocene). It is comprised of gray and yellowish- to reddish-brown sand, gravel, silt, and clay. It constitutes surficial deposits of extensive plain and fluvial-estuarine terraces above elevations of 10 meters. The thickness of the Windsor Formation is 0 to 12.5 meters.
Source: USGS Virginia Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=VAQTw%3B0)
The surface soil profile of this area is Emporia Complex, 15 to 25 percent slopes. This soil as moderately well-drained, acidic, and found on sloping and elevated terraces. They are comprised of fine sandy loam, loam, and sandy clay loam in varying quantities across the profile; the depth to parent geology is approximately 200 cm.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2139352WLP 2614
411WLP 2600RJL2022FLAL-029Stewartia malacodendron L. Florida, United StatesNA2022COLLECTED08/07/2022Eglin AFB, in woodlands along Weaver Creek accessed from unnamed dirt road, 0.82 kilometers west of junction with Eglin AFB 720; approximately 0.73 kilometers north of junction with Choctaw Nolf Airfield Road and Eglin AFB 720.30.51680000, -86.9146940015Growing in moist, well-drained sandy soils above Weaver Creek in mixed broadleaved evergreen and deciduous woodland habitat in part shade to shade of west facing slopes several meters above the wetland zone. The Stewartia is growing in a high competition habitat. The underlying geology of this area is the Citronelle Formation, of Pliocene origin, and consists of gray to orange, often mottled, unconsolidated to poorly consolidated, very fine to very coarse, poorly sorted, clean to clayey sands. It contains significant amounts of clay, silt and gravel which may occur as beds and lenses and may vary considerably over short distances. Limonite nodules and limonite-cemented beds are common. Wild material2138710WLP 2600
412Ames 36026RJL2022FLAL-007Fraxinus caroliniana Mill. Florida, United StatesNC7SEED2022COLLECTED07/28/2022Growing along the Yellow River and reached by boat.30.58025000, -86.910528001Trees are typically found growing in full sun in permanently saturated to submersed conditions along the edge of the Yellow River, growing in association with a wide array of deciduous and evergreen trees, shrubs and perennial plant species. This species requires acidic conditions. While the aquatic habitats are generally fresh water, there is occasionally tidal or hurricane-caused saltwater intrusions. 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. Wild material2138696Ames 36026
413WLP 2584RJL2022FLAL-005Styrax americanus Lam. Florida, United StatesNA2022COLLECTED07/28/2022Growing along the Yellow River and reached by boat.30.57944000, -86.916898001Plants are typically found growing in shade to full sun in permanently saturated to submersed conditions along the edge of the Yellow River, growing in association with a wide array of deciduous and evergreen trees, shrubs and perennial plant species. Most of the plants along the river are adapted to acidic conditions and while the aquatic habitats are generally fresh water, there is occasionally tidal or hurricane-caused saltwater intrusions. 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. Wild material2138694WLP 2584
414WLP 2585RJL2022FLAL-006Nyssa biflora Walter Florida, United StatesNA2022COLLECTED07/28/2022Growing along the Yellow River and reached by boat.30.58013800, -86.915568001Trees are typically found growing in full sun in permanently saturated to submersed conditions along the edge of the Yellow River, growing in association with a wide array of deciduous and evergreen trees, shrubs and perennial plant species. This species requires acidic conditions. While the aquatic habitats are generally fresh water, there is occasionally tidal or hurricane-caused saltwater intrusions. 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. Wild material2138695WLP 2585
415Ames 35901Blazing Star PrairieStachys pilosa Nutt. Iowa, United StatesNC7FLOWER2022COLLECTED07/29/2022Blazing Star Prairie located 2.00 miles southeast of Rowley, T87N R8W S ¼ NW ¼ NW ¼ Sec. 17.42.35365800, -91.81099000286Mesic prairie remnant.Wild materialPlants sampled in nature varied substantially in height and leaf size, where this variation could possibly be due to multiple ploidy levels existing in the population. Species is extremely vigorous and can aggressively spread via rhizomes especially under moist, wet soil conditions. Plants averaging 50-60 cm in height with minimal to no branching. Foliage and stems are densely covered in hairs. Flowers are faint pinkish-white in color with pink-light purple spots/splotches. Peak flowering generally occurs in mid-June (central Iowa) and can extend for almost four weeks. Genetics of this accession originated from eastern-central Iowa. Species is frequently visited by a plethora of pollinators, especially bumblebees. 2138298Ames 35901
416OPGC 7588Blazing Star PrairiePhlox maculata L. Iowa, United StatesOPGCFLOWER2022COLLECTED07/29/2022Blazing Star Prairie located 2.00 miles southeast of Rowley, T87N R8W S ¼ NW ¼ NW ¼ Sec. 17.42.35365800, -91.81099000286Mesic prairie remnant.Wild materialPlants in nature ranged in height from two to three feet. Some variation was noted for degree of branching in the inflorescence with a small number of plants having highly branched inflorescences. Peak flowering and fruiting in nature at collection site peaked 20 June and 26 July, respectively.2138297OPGC 7588
417NA 87148PCC18-GE029Punica granatum L. K'akheti, GeorgiaNA2022COLLECTED04/27/2018Sighnaghi (municipality/district); On the south side of April Street, approximately 0.83 air miles northeast of Signagi.41.62070000, 45.93503000506Growing on dry, north-facing slope in disturbed dry forest near the base of the main slope.Wild material2138737NA 87148
418Ames 35881Reichelt UnitHeuchera richardsonii R. Br. Iowa, United StatesNC7FRUIT2022COLLECTED06/30/2022Reichelt Unit of Rock Creek State Park on south side of US highway 6 located 7.70 miles west, southwest of Grinnell, T80N R17W SE ¼ SE ¼ Sec. 30.41.70311300, -92.86569100274Prairie remnant. Hilltop/knoll.Wild materialPlants in nature measuring approximately six to eight inches in height with flowering stalks reaching up to three feet in height.2138180Ames 35881
419WLP 2576RJL2022-001Amelanchier arborea (F. Michx.) Fernald Maryland, United StatesNA2022COLLECTED05/25/2022Plants growing in open woodlands and part shade along unnamed Elkton State Forest gravel road over a distance of approximately 5 kilometers labelled as the address of 717 Irishtown Rd, North East, MD 21901.39.58089500, -75.9150590073Plants are found regularly but scattered along the unnamed gravel road as well as in open understory of the upland woodlands. Plants growing in a mesic to dry, well-drained habitat of mixed deciduous and evergreen woodlands comprised primarily of acid-loving plants. Plants are growing in part shade and open understory shade. The soils in the collection area are generally described as a complex series of fluviomarine deposits. The soils range from a thin loam layer at the surface to varying levels of loam to sandy loam and/or extremely gravelly sandy clay loam strata, depending upon geographical location (ie. Hillslope summits, slopes, footslopes, swales, etc.). The primary soil types in the collection area are classified as Russett-Christiana-Hambrook Complex and/or Sassafras and Croom Soils; though, others may intersect and overlay in specific areas.Wild material2138095WLP 2576
420Ames 35807JDC/SD/2022/034/1014Salix discolor Muhl. Minnesota, United StatesNC7FRUIT2022COLLECTED06/06/2022Mud Lake and Amity Creek Watershed located just north of Duluth approximately 6.25 miles, T51N R14W Sec. 22, 26, 27, and 28. 46.87662300, -92.10040300418Floodplain, wetlands, drainages.Wild materialThe native range of Salix discolor is concentrated in the northeastern United States and also throughout southern Canada (Little, E. L. Jr. 1977). Generally adapted/tolerant to wet soils this species is often found in meadows, fens, swamps, and streambanks. Attractive ornamental characteristics includes early spring, showy flowers and yellow foliage in the fall. Salix discolor provides a critical source of pollen at the beginning of the growing season for a plethora of pollinators and also serves as a larval host to many insect species. Salix discolor are commonly used in the cut flower industry for both their showy catkins and colorful, dormant winter stems. This accession represents genetics from northeastern Minnesota. Specimens sampled in nature ranging from 6-22' in height. 2138039Ames 35807
421Ames 35806Reichelt PrairieSalix humilis Marshall var. tristis (Aiton) Griggs Iowa, United StatesNC7PLANT2022COLLECTED05/16/2022Reichelt Unit of Rock Creek State Park on south side of US highway 6 approximately 7.70 miles west, southwest of Grinnell, T80N R17W SE ¼ SE ¼ Sec. 30.41.70311300, -92.86569100274Xeric prairie remnant. Hilltop/knoll.Wild materialPlants sampled in nature measuring 2.0-4.0 feet in height. Specimens noted during peak flowering and seed dispersal on 21 April and 17 May (2022), respectively. Some plants upright and some rather prostrate. Site was mowed in winter 2020/2021 winter resulting in significant flowering in 2022. In cultivation (central Iowa), plants are extremely short and compact where after two field seasons plants are rather uniform and topping out at a height of 2.5'. Dense suckering immediately surrounding clump/base of plant. Peak fall color (central Iowa) occurring in mid-November. 2137912Ames 35806
422Ames 35805Rippey RR ROWSalix humilis Marshall var. tristis (Aiton) Griggs Iowa, United StatesNC7FRUIT2022COLLECTED05/12/2022Located 3.27 miles southeast of Rippey along east side of highway 144, T82N R28W NW ¼ SW ¼ Sec. 19.41.89609800, -94.16247600284Xeric prairie remnant. Railroad right of way.Wild materialPlants in nature measuring approximately 3.0-3.5' in height. Specimens noted during peak flowering and seed dispersal on 12 April and 3 May (2021), respectively. Normally for central Iowa peak flowering and fruiting occurs in late April and mid-May, respectively.2137911Ames 35805
423Ames 35803Turtlehead FenSalix eriocephala Michx. Iowa, United StatesNC7FRUIT2022COLLECTED04/21/2022Turtlehead Fen (Chichaqua Bottoms Greenbelt) located 1.75 miles southeast of Farrar just north of highway 65, T81N R21W SW ¼ NW ¼ Sec. 31.41.78612100, -93.34726000290Extremely high-quality remnant fen. Extremely wet, spongy soils with surface water visible at time of collection.Wild materialPlants in nature averaging 20' in height. Bright red buds on nearly all genotypes with stem colors ranging from yellow/bronze, brownish-green, brown and green at time of sampling (21 April 2022). Some specimens are rather open, wide spreading and some are rather upright. Salix eriocephala at this site is one of the more dominant species of willow.2137909Ames 35803
424Ames 35792APS/ID/2022/027/489Ilex decidua Walter Arkansas, United StatesNC7FRUIT2022COLLECTED03/15/2022Located approximately 3.75 miles east of Allison just off Round Bottom Road.35.93670000, -92.04891000133Dry west facing slope in a pine, oak, and hickory forest.Wild materialPlants sampled in nature with bright red fruits measuring 7-9 mm in diameter.2137431Ames 35792
425OPGC 7585Pleggenkuhle PrairieLiatris pycnostachya Michx. Iowa, United StatesOPGC2022COLLECTED09/29/2021Pleggenkuhle Prairie located 2.11 miles northwest of Hawkeye, T94N R10W Sec. 14.42.95783800, -91.98405900341Wet-mesic prairie remnant on Clyde Silty Clay Loam and Floyd Loam soils.Wild material2133094OPGC 7585
426OPGC 8523NEWFS-412Erechtites hieraciifolius (L.) Raf. ex DC. Massachusetts, United StatesOPGC2021Wild materialReceived as: Erechtites hieracifolia.2137209OPGC 8523
427W6 60025NCBG-532Decodon verticillatus (L.) Elliott Maryland, United StatesW62021Wild material2132907W6 60025
428NA 86885RJL2021PA-004Ilex verticillata (L.) A. Gray Pennsylvania, United StatesNA2021COLLECTED11/16/2021Plants 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, -75.82750806124Plants 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 material2123125NA 86885
429WLP 1731RJL2021PA-001Viburnum acerifolium L. Pennsylvania, United StatesNA2021COLLECTED11/05/2021Plants 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, -75.82888750103Plants 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 material2123080WLP 1731
430WLP 1732RJL2021PA-002Viburnum prunifolium L. Pennsylvania, United StatesNA2021COLLECTED11/05/2021Plants 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, -75.82888750102Plants 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 material2123098WLP 1732
431WLP 1733RJL2021PA-003Viburnum dentatum L. Pennsylvania, United StatesNA2021COLLECTED11/05/2021Plants 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, -75.82928139107Plants 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 material2123124WLP 1733
432WLP 1747RJL2021PA-005Rosa palustris Marshall Pennsylvania, United StatesNA2021COLLECTED11/20/2021Plants 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, -75.82383250100Habitat 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 material2123715WLP 1747
433OPGC 8486CBG-10697Lysimachia quadriflora Sims Illinois, United StatesOPGC2021Wild material2132545OPGC 8486
434W6 59938CBG-10661Poa palustris L. Illinois, United StatesW6SEED2021Wild material2132517W6 59938
435OPGC 7574Ledges State ParkSolidago ulmifolia Muhl. ex Willd. Iowa, United StatesOPGCFlower2021COLLECTED09/15/2021Ledges State Park, approximately 4.5 miles south of Boone, T83N R26W Sec. 2041.98266200, -93.89314800287Understory of hardwood forest.Wild materialPlants in nature were generally two to three feet in height, growing in sparsely spreading colonies. This population has a large amount of diversity for flowering time with the first plants in the population beginning to flower on 22 July 2021 and the last plants to flower were still blooming at the end of September. Some plants in the population had a muted red fall foliage color at the end of October 2021. This accession represents genetics from near the northwest edge of the species range of occurence.2132828OPGC 7574
436OPGC 7575Ledges State ParkSolidago flexicaulis L. Iowa, United StatesOPGCFlower2021COLLECTED10/03/2021Ledges State Park, approximately 4.5 miles south of Boone, T83N R26W Sec. 2141.98338100, -93.89052800288Understory of hardwood forest.Wild materialPlants in nature ranged in height from approximately one to three feet, growing in sparsely spreading colonies. Peak bloom in 2021 occurred near 15 September. Several specimens had branched inflorescences.2132829OPGC 7575
437Ames 35750Ames 35750Blephilia ciliata (L.) Benth. Iowa, United StatesNC7FLOWER2021COLLECTED09/27/2021Located approximately 3 miles south, southeast of Fairfield, T71N R9W SW1/4 Sec. 740.96338000, -91.94686900223Woodland openings/edges, disturbed areasWild material2122068Ames 35750
438Ames 35748Clay PrairieCeanothus americanus L. Iowa, United StatesNC7SEED2021COLLECTED09/01/2021Clay Prairie State Preserve located approximately 4 miles south of Allison, T91 R16W NE 1/4 NE 1/4 NE 1/4 Sec. 1842.70041000, -92.77174000307Mesic prairie remnant.Wild material2122066Ames 35748
439WLP 1446WLP 1446Rhododendron maximum L. New Hampshire, United StatesNA2021Wild material2120504WLP 1446
440Ames 35734Ledges State ParkTeucrium canadense L. Iowa, United StatesNC7SEED2021COLLECTED08/23/2021Ledges State Park located approximately 4.75 miles south of Boone T83N R26W Sec. 16 & 2141.99262400, -93.87724800330Edges of woodsWild material 2120338Ames 35734
441Ames 36062CBG-10584Linum sulcatum Riddell Illinois, United StatesNC72021Wild materialPlant numbers sampled estimated.2120175Ames 36062
442NA 88332CBG-10580Hypericum prolificum L. Illinois, United StatesNA2021Wild materialPlant numbers sampled estimated.2120171NA 88332
443W6 59136CBG-10266Dasiphora fruticosa (L.) Rydb. Wisconsin, United StatesW62021Wild material2120062W6 59136
444W6 59137CBG-10267Muhlenbergia glomerata (Willd.) Trin. Wisconsin, United StatesW62021Wild material2120195W6 59137
445W6 59182CBG-10473Echinacea pallida (Nutt.) Nutt. Illinois, United StatesW62021Wild material2120103W6 59182
446Ames 35667Kankakee Sands PreserveAronia ×prunifolia (Marshall) Rehder Illinois, United StatesNC7Flower2021COLLECTED05/04/2021Kankakee Sands Preserve located approximately 2.3 miles southwest of Wilmington in Custer Township, T32N R9E NE 1/4 Sec. 1141.27166000, -88.15701800170Sand shrub prairieWild materialGenotypes noted in nature were averaging 5.0-6.0' in height, relatively upright in growth habit and extremely dense suckering. Numerous clones noted covering expansive areas (e.g. 30 yards by 20 yards, etc.). Variation in branching and glossiness of leaves noted across genotypes present in nature.2115976Ames 35667
447NA 88283NEWFS-554Cephalanthus occidentalis L. Massachusetts, United StatesNA2021Wild materialOpposite branches, balls of white flowers, seeds in balls.2115694NA 88283
448Ames 35615Ames 35615Aronia arbutifolia (L.) Pers. Michigan, United StatesNC7SEED2020COLLECTED11/03/2020Warren Townsend Park located just northeast of Cannonsburg southwest of Ramsdell Dr. and Six Mile Rd. intersection, T8N R10W NE ¼ NW ¼ Sec. 26, Cannon Twp., Kent County43.05606700, -85.46435100239Shrubby edge of old stream (Bear Creek) oxbow, adjacent to wet meadow with groundwater upwelling. Muck soils.Wild materialPlants in nature measuring approximately six meters in height; elongate shrubs mostly unbranched; bright-red fruits measuring between 4-7 mm in diameter; tomentose leaves underneath; scarlet fall color. This collection was discovered in 2011 and represents the first report of the species for the state of Michigan (Ryskamp and Warners 2012) and thus represents a widely disjunct population where the next nearest documented population is in southern Ohio (Clermont County). 2110277Ames 35615
449OPGC 8123NV030-1451Asclepias speciosa Torr. Nevada, United StatesOPGC2020Wild materialErect stems, whorled leaf arrangement, pointed leaf tips, hairy leaves.2110398OPGC 8123
450NA 88465F012Viburnum dentatum L. Pennsylvania, United StatesNA2020COLLECTED09/06/2020J. Edward Mack Boy Scout Camp near Brickerville, PA: located between old logging road and power lines. [Longitude was entered incorrectly and has been estimated; it needs to be confirmed with original data.]40.26002778, -76.32097200Wild material2109476NA 88465
451NA 88466F013Viburnum dentatum L. Pennsylvania, United StatesNA2020COLLECTED09/09/2020Schaefferstown, PA: Middle Creek Wildlife Management Area, along the Middle Creek power lines on the southern side, starting near Laurel Drive and hiking east to Middle Creek.40.26400000, -76.25333000Wild material2109477NA 88466
452NA 88467F014Viburnum prunifolium L. Pennsylvania, United StatesNA2020COLLECTED09/24/2020J. Edward Mack Boy Scout Camp near Brickerville, PA.40.25944000, -76.32416600Near power lines, mostly on western slopes.Wild material2109478NA 88467
453NA 88468F015Ilex verticillata (L.) A. Gray Pennsylvania, United StatesNA2020COLLECTED10/04/2020J. Edward Mack Boy Scout Camp near Brickerville, PA.40.26000000, -76.31888000On south side of hill top.Wild material2109479NA 88468
454OPGC 7553Williams PrairieLiatris pycnostachya Michx. Iowa, United StatesOPGCHABITAT2020COLLECTED09/25/2020Williams Prairie State Preserve approximately 3 miles north of Oxford, T80N R8W SW1/4 NE1/4 Sec. 5, Johnson County41.76811400, -91.80062300226Dry, upland portions of a remnant wet prairie.Wild materialPlants sampled in nature were 1.5 to 3 feet in height. At time of collection (25 September 2020), approximately 20% of the seed had begun to disperse. Some plants still had green leaves, while most were entirely senesced. 2107740OPGC 7553
455Ames 35550Scuppernong PrairieSalix myricoides Muhl. Wisconsin, United StatesNC7LEAF2020COLLECTED09/04/2020Two areas of Salix myricoides were identified approximately 2.5 miles apart. The northern area is located along the Scuppernong Springs Nature Trail (intersection of State Highway 67 and County Highway ZZ) and the adjacent marsh prairie to the south. The southern area is located in the Scuppernong Prairie State Natural Area, at the intersection of Wilton Road and County Highway N. Kettle Moraine State Forest - Southern Unit, Waukesha County42.93363600, -88.47242400260Marsh, riverbank, prairie and woodland.Wild materialBayberry willow is native to areas of the northeastern U.S. and north into Canada, localized around the Great Lakes region. Known to occur on shorelines/dunes but also in swamps, fens, and on talus (Haines 2004) with the potential to reach six meters in height (Dorn 1995). Ornamental characteristics include glaucous lower leaf blades that appear chalky white. Staminate flowering occurs before or during leaf expansion with purple-turning-yellow anthers (Haines 2004). This accession was sampled on wet, slightly above neutral pH soils (6.0-7.3) which may result in superior performance in the urban landscape. Under cultivation, the plants grow in a widely spreading growth habit (some are nearly prostrate); however, this trait was not noticed at the time of collection from nature. Shrubs noted in nature measuring 0.5 to 2 m tall. The two areas sampled contained both Salix myricoides and Salix discolor, and likely hybrids between the two species. Attempts were made to collect only Salix myricoides based on the following characteristics: white undersides of the leaves, large stipules and finely serrated leaf margins. During collection on 6 April 2021, S. discolor was in flower while S. myricoides was not yet flowering. 2107011Ames 35550
456OPGC 8059ID310-42Asclepias speciosa Torr. Idaho, United StatesOPGC2020Wild materialPetiolate leaves, oblong-lanceolate leaves.2107488OPGC 8059
457NA 88438MARSB-202Rosa palustris Marshall Delaware, United StatesNA2020Wild materialWoody plant with stems covered in recurved thorns. Mature fruit a scarlet hip.2106461NA 88438
458NA 86434Pulverulentus GroupStyrax americanus Lam. Texas, United StatesNA2020COLLECTED09/08/2018Near Gum Slough, on the edges of woodlands along the north side of road FM 2246.30.33332000, -93.9470400015Plants are found along the edges and moist to wet areas of Gum Slough in part shade to full sun of a mixed deciduous and broadleaved evergreen woodlands. Soils are generally acidic with loamy to clayey sediments, but with some areas consisting of deep, nearly level loamy, poorly drained soil.Wild materialSpecies occurrence is infrequent at this location. Collector's note on the name under which this material was gathered, Styrax americanus var. pulverulentus: "In general, the var. pulverulentus is considered "taxonomically inconsequential" by many botanists. Even so, this densely pubescent characteristic is highly uniform across every plant I observed in the sampled population. Weakley notes that "true" var. pulverulentus can be found as far west as East Texas and, in my humble opinion, the population sampled herein represents this "taxon". Regardless, for the purposes of drawing distinction between "typical" Styrax americanus and the densely pubescent form, I've chosen to use this varietal name. It will be interesting to observe whether the seedling progeny are uniformly similar to their parents when they germinate." [Actual altitude recorded was 14.8 m, but decimals can't be used in the database, so the number was rounded.]2109219NA 86434
459Ames 35288APS/MF/2020/003/406Monarda fistulosa L. Kansas, United StatesNC7HABITAT2020COLLECTED02/05/2020Eisenhower State Park on north side of Melvern Lake approximately 5.25 miles west, northwest of Melvern, T18S R15E NE1/4 Sec. 3, Osage County38.51966000, -95.73352000323Edge of woods with limestone substrate.Wild material2101394Ames 35288
460WLP 2017MARSB-970Viburnum dentatum L. New York, United StatesNA2019COLLECTED08/29/2019Richmond County; Staten Island; Wolfes Pond Park, Staten Island's south shore.40.51800000, -74.19180000Forest, marsh shore in full sun; growing in wet, well-drained sand/loam.Good seed quality; 100 percent healthy seed. Seed maturation: middle. [Number of individuals harvested and population size not recorded.]2109166WLP 2017
461WLP 2018MARSB-976Viburnum opulus L. var. americanum Aiton New York, United StatesNA2019COLLECTED08/01/2019Dutchess County; Tivoli; Bard College campus.200Open marsh (tidal marsh), full sun, red maple swamp; growing in moist loamy sand.Seed collected from 20 plants; population scattered in distribution, found over a 1 mile by 1 mile area. Seed maturation early, middle.2109167WLP 2018
462WLP 2023MARSB-987Viburnum dentatum L. New York, United StatesNA2019COLLECTED08/21/2019Cattaraugus County; Red House; Public park land; wetland/lake shore.42.10720000, -78.75137000Wetland/lake shore, in full sun; growing in wet sand/clay soil.Seed harvested from 10 individuals in a population of 25+. Scattered distribution. Seed 95 percent healthy; seed maturation late.2109172WLP 2023
463WLP 2036MARSB-1003Viburnum opulus L. var. americanum Aiton New York, United StatesNA2019COLLECTED08/30/2019Columbia County; Germantown; Rt. 9 (9G?)/Main St. right-of-way, Germantown.183Roadside right-of-way in full sun; growing in moist loamy sand.Seeds collected from 40 individuals in a population of 50+ plants occurring over an area 300 meters by 500 meters in size; common. Seed maturation: middle.2109185WLP 2036
464WLP 2038MARSB-1005Viburnum lentago L. New York, United StatesNA2019COLLECTED09/19/2019Columbia County; Germantown; Rt. 6, Germantown. [This appears to be south of Germantown. -SBL]183Marsh.Seeds collected from 20 individuals in a population of 25+ plants; scattered distribution. Seed maturation: middle. Birds, low fruit set noted.2109187WLP 2038
465WLP 2051MARSB-1020Viburnum lentago L. New York, United StatesNA2019COLLECTED09/27/2019Onondaga County; Liverpool; Hamlin Marsh, Old Wetzel Rd.43.15000000, -76.17291000Forestd wetland/marsh edge in full sun to partial shade; growing in moist to wet, well-drained silt/clay/loam soilSeeds collected from 15+ individuals in a population of 50+ plants; common. 80 percent healthy seed. Seed maturation: late. End of ripening period.2109200WLP 2051
466NA 88146NCBG-309Aralia spinosa L. Virginia, United StatesNASEED2019Wild material2098406NA 88146
467NA 88152NCBG-320Liquidambar styraciflua L. North Carolina, United StatesNASEED2019Wild material2098412NA 88152
468NA 88165NCBG-450Viburnum dentatum L. Virginia, United StatesNASEED2019Wild material2098452NA 88165
469OPGC 7951NEWFS-413Oenothera biennis L. Massachusetts, United StatesOPGCSEED2019Wild material2098217OPGC 7951
470W6 57390NEWFS-297Phytolacca americana L. Massachusetts, United StatesW6SEED2019Wild material2098187W6 57390
471W6 57383NEWFS-272Carex crinita Lam. Massachusetts, United StatesW6SEED2019Wild material2098180W6 57383
472W6 57376NEWFS-245Elymus virginicus L. Massachusetts, United StatesW6SEED2019Wild material2098173W6 57376
473WLP 889PCC19-RO-01Carpinus orientalis Mill. Iași, RomaniaNA2019COLLECTED09/23/2019Roscani; ; Roscani Forest [Padurea Roscani]; in historic Moldavia region.47.43375000, 27.41406000141Mixed woodland in silty hills.20 trees visible from collection site, population likely much larger.2109159WLP 889
474W6 57099MARSB-246Tridens flavus (L.) Hitchc. New York, United StatesW6SEED2019Wild material2097538W6 57099
475Ames 35236SF_ID:24690/EO-ID:17843Agastache foeniculum (Pursh) Kuntze Nebraska, United StatesNC7FLOWER2019Wild materialPlants measuring approximately 60 cm in height. Infructescences fully mature at time of collection (23 October 2019), likely past peak maturity by approximately 4 weeks. Population (EC-ID: 17843) was originally documented by Steven B. Rolfsmeier on 8 June 2015 (Nebraska Pine Ridge Plant Resurvey, 2015: Report submitted to the Nebraska Natural Heritage Program) noting “ Agastache foeniculum was located in a ravine bottom that burned in 2012. Estimated population size: 200-300 stems covering approximately 125 sq. meters”. A. foeniculum in Nebraska is currently tracked by the Nebraska Natural Heritage Program and is listed (6 November 2019) as a S1 (Critically Imperiled - at very high risk of extirpation in the state due to very restricted range, few populations or occurrences, steep declines, severe threats or other factors) and Tier 2 species (Tier 2 - species are typically those that are not at-risk from a global or national perspective but are rare or imperiled within Nebraska). 2097772Ames 35236
476WLP 1685JDC/RS/2019/036/915Rosa setigera Michx. Iowa, United StatesNAFRUIT2019COLLECTED10/17/2019Ledges State Park located approximately 4.75 miles south of Boone, just south of the Oakwoods Shelter/Picnic area, T83N R26W NE1/4 NE1/4 and also NW1/4 NE1/4 Sec. 21, Boone County41.99262400, -93.87724800330Edges of woods (adjacent to prairie) and also within 20-25 yards from woods in prairie. Noted in east, west, and south-facing edges of woods (no specimens noted on north-facing woodland edges)Wild materialWoody shrub/vine stretching up to 12' in length. Alternate compound leaves usually consisting of five lealets. Leaf rachis and stipule margins glandular. Mature hypanthium and pedicel with stipitate glandular hairs. Mature hypanthium mostly bright to dark red in color with a few dark orange noted at time of harvest (17 October 2019). Leaves rather to somewhat glossy. This collection represents genetics from the northwestern edge of the species range, likely suggesting good cold-hardiness (USDA Zone 5a). 2097769WLP 1685
477NA 86027PCC19-RO-02Quercus dalechampii Ten. Iași, RomaniaNA2019COLLECTED09/23/2019Roscani; ; Roscani Forest [Padurea Roscani]; in historic Moldavia region.47.43369000, 27.41383000152Mixed woodland in silty hills.Wild materialCollected from two trees, one fruiting on the roadside. At least 15 trees visible.2109115NA 86027
478WLP 170NACPEC19-061Cephalanthus occidentalis L. Georgia, United StatesNA2019COLLECTED09/15/2019Walker County; Lula Lake Land Trust: Lula Lake Land Trust Falls: East Side of Falls34.93361200, -85.37187800427Ravine, slope forest, stream margin at Lula Lake FallsWild material2110482WLP 170
479WLP 171NACPEC19-063Itea virginica L. Georgia, United StatesNA2019COLLECTED09/15/2019Walker County; Lula Lake Land Trust: Lula Lake Land Trust Falls: West Side of Falls34.93319200, -85.37178900477Stream bank, mesic wood forestWild material2110485WLP 171
480WLP 178NACPEC19-098Sorbus americana Marshall Tennessee, United StatesNA2019COLLECTED09/19/2019Carter County; Cherokee National Forest: Appalachian Trail South to Carver's Gap from parking area36.10430400, -82.128437001854High elevation spruce fir mixed woodland prairieWild material2110492WLP 178
481WLP 179NACPEC19-099Alnus viridis (Chaix) DC. Tennessee, United StatesNA2019COLLECTED09/19/2019Carter County; Cherokee National Forest: Appalachian Trail South to Carver's Gap from parking area36.10416600, -82.128445001860High elevation spruce fir mixed woodland prairieWild material2110493WLP 179
482WLP 180NACPEC19-011Clematis virginiana L. Ohio, United StatesNA2019COLLECTED09/07/2019Adams County; Edge of Appalachia Preserve System: The Charles Eulett Wilderness Preserve38.78128800, -83.41623900263Managed old homestead site border: Xeric limestone prairie; managed turfgrassWild material2110494WLP 180
483Ames 35230Gabel #7103Agastache foeniculum (Pursh) Kuntze South Dakota, United StatesNC7Flower2019COLLECTED09/22/2019Black Hills National Forest known as Ranger Draw located approximately 10.3 miles west, southwest of Lead on south side of Roughlock Falls Road, T4N R1E SE1/4 NE1/4 NE1/4 Sec. 10 and T4N R1E NW1/4 NW1/4 Sec. 11 (circa 3.9 miles from Wyoming border), Lawrence County44.32706700, -103.973983001703Mixed spruce/pine forest.Wild materialPlants ranging in height from 0.5 to 1 m tall. Flower color mostly lavender, with some specimens having very dark, vibrant purple (e.g. samples 45, 45, 49 and 53) and some rather blue in color (samples 41 and 46). Terminal flower spikes averaged 6 cm in length (average 60 specimens) ranging from 0.6 to 13.3 cm. 2097766Ames 35230
484WLP 2003MARSB-968Viburnum dentatum L. New York, United StatesNA2019COLLECTED08/04/2019Ulster County; Gardiner; Private residence at 844 Route 208, Gardiner, New York 12525.41.65848000, -74.14236000122Forest, marsh/pond shore in partial to full shade; poorly drained, clay loam soil, seasonally wet/moist.Seeds collected from plant. Many seeds had already dropped or been eaten; seeds collected from an approximately 1 acre (or 4000 square meters) area with Viburnum dentatum growing in several dense patches and sparsely between. Species common, scattered in area; 100-plus individuals estimated in approximately 4000 square meters.2109099WLP 2003
485WLP 2004MARSB-969Viburnum dentatum L. New York, United StatesNA2019COLLECTED07/31/2019Onondaga County; Liverpool; Hamlin Swamp (two sets of coordinates and data collected over two days at this site; the earlier data is noted first. The second set of coordinates given is 43.150864 deg. N, 76.175374 deg. W.)43.15140000, -76.17474000Edge of wetland. Marsh/pond shore in full sun; moist to wet, clay loam to clay soil.Seeds collected directly from plants. Collected in two partial collections, one on 7/31/2019 and the second on 8/8/2019; Species common to scattered in area; 50+ individuals in population visited on 7/31/2019, and 30+ individuals in the population visited on 8/8/2019 (five individuals sampled from the second site; number of individuals sampled at first site not recorded.) Seed quality good.2109100WLP 2004
486WLP 2008MARSB-974Viburnum dentatum L. New York, United StatesNA2019COLLECTED07/29/2019Columbia County; Clermont; Church Avenue, Clermont, New York; privately owned agricultural land.0.00000000, 0.00000000183Edge of oak-hickory woodland in partial shade; growing in dry clay-loam soil.Seeds collected directly from plants. Species common in area; 50+ individuals in population, 50+ individuals sampled, with population area 1/4 mile (linear).2109104WLP 2008
487WLP 2009MARSB-975Viburnum dentatum L. New York, United StatesNA2019COLLECTED08/01/2019Columbia County; Germantown; Eastern Parkway, Germantown, New York; privately owned agricultural land.0.00000000, 0.00000000183Field edge, shrubland, in full sun; moist, well-drained, loamy sand soil.Seeds collected directly from plants. Species common in area; 50+ individuals in population, 50 individuals sampled, with population area 1 mile (linear).2109105WLP 2009
488WLP 2010MARSB-977Viburnum dentatum L. New York, United StatesNA2019COLLECTED08/02/2019Greene County; Catskill; Scenic Hudson plot (land in conservation use) on Kukuk Rd in Catskill, New York [Note: location could not be found on maps, and no latitude and longitude were supplied; possibly Kukuk Lane in Kingston, New York, which is a bit south of Catskill. -SBL]0.00000000, 0.0000000091Edge of oak-hickory woodland; growing in full sun in loamy sand soil.Seeds collected directly from plants. Sparse seed set noted. Species scattered in area; 30+ individuals in population, 32 individuals sampled, with population area 1 mile x 1 mile.2109106WLP 2010
489WLP 2011MARSB-981Viburnum dentatum L. New York, United StatesNA2019COLLECTED08/08/2019Onondaga County; Phoenix; Three Rivers Wildlife Management Area.43.19781000, -76.33312000Shrubland and meadow/grassland in moist to dry, well-drained, clay loam soil.Seeds collected directly from plants. Species common in area; 100+ individuals in population, 30+ individuals sampled. Seed quality good, 100 percent healthy seed. The first of two separate collections made in two areas of the WMA [see NA 86005, MARSB-982/MARSB_IL_007 for the second collection] since the area is very large.2109107WLP 2011
490WLP 2013MARSB-983Viburnum dentatum L. New York, United StatesNA2019COLLECTED08/08/2019Oswego County; Phoenix; Peter Scott Swamp.43.24977000, -76.26445000Edge of wetland in full sun, growing in moist to wet clay loam soil.Seeds collected directly from plants. Species scattered in area; 20+ individuals in population, five individuals sampled. Seed quality good, 75 percent healthy seed.2109109WLP 2013
491WLP 2014MARSB-985Viburnum dentatum L. New York, United StatesNA2019COLLECTED08/20/2019Oswego County; Williamstown; Private recreational land at 319 Stone Hill Rd.43.41583000, -75.96805000186Edge of open pond with edge trail lined with shrubs and trees, dam; growing in full sun in wet sand loam soil.Seeds collected directly from plants. Species scattered in area; 30 individuals in population, 500 seeds collected [presumably all individuals sampled]. Seed quality good, 95 percent healthy seed. Beaver activity in pond.2109110WLP 2014
492WLP 154NACPEC19-010Rhus copallinum L. Ohio, United StatesNA2019COLLECTED09/07/2019Adams County; Lynx Township; Edge of Appalachia Preserve System: The Charles A. Eulett Wilderness Preserve.38.78140000, -83.41647000254Managed old homestead site border: xeric limestone prairie; managed turfgrass, over Dolomitic limestone (dolostone), acidic edge.Seeds collected from one plant. Four herbarium specimens collected; photographed. DNA sample collection number: DENG8032.2109140WLP 154
493OPGC 7460CBG-8191Pedicularis canadensis L. Wisconsin, United StatesOPGCSEED2019Wild material2092673OPGC 7460
494OPGC 7464CBG-8630Heuchera richardsonii R. Br. Wisconsin, United StatesOPGCSEED2019Wild material2092685OPGC 7464
495OPGC 7471CBG-8944Anemone canadensis L. Iowa, United StatesOPGCSEED2019Wild material2092726OPGC 7471
496OPGC 7474CBG-9084Liatris pycnostachya Michx. Wisconsin, United StatesOPGCSEED2019Wild material2092758OPGC 7474
497W6 56648CBG-9070Amorpha canescens Pursh Wisconsin, United StatesW6SEED2019Wild material2092747W6 56648
498W6 56688CBG-9357Ageratina altissima (L.) R. M. King & H. Rob. var. altissima Iowa, United StatesW6SEED2019Wild material2092787W6 56688
499OPGC 7845CBG-8187Polemonium reptans L. Wisconsin, United StatesOPGCSEED2019Wild material SOS 7th transfer.2092671OPGC 7845