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ACCESSIONPLANT NAMETAXONOMYORIGINGENEBANKIMAGEAVAILABILITYRECEIVEDSOURCE TYPESOURCE DATECOLLECTION SITECOORDINATESELEVATIONHABITATIMPROVEMENT LEVELNARRATIVE
0OPGC 8600OR080-91Typha latifolia L. Oregon, United StatesOPGC2022Wild materialHuge, brown seed heads on top of grass-like leaves. Seed heads have a male terminus.2138308OPGC 8600
1OPGC 8491NCBG-235Typha latifolia L. North Carolina, United StatesOPGC2021Wild material2132858OPGC 8491
2OPGC 8492NCBG-237Typha latifolia L. North Carolina, United StatesOPGC2021Wild materialWider leaves than T angustifolia.2132859OPGC 8492
3OPGC 8493NCBG-239Typha latifolia L. North Carolina, United StatesOPGC2021Wild material2132860OPGC 8493
4OPGC 8494NCBG-242Typha latifolia L. North Carolina, United StatesOPGC2021Wild materialWide heads that are red brown in color.2132861OPGC 8494
5OPGC 8495NCBG-247Typha latifolia L. North Carolina, United StatesOPGC2021Wild material2132862OPGC 8495
6OPGC 8496NCBG-262Typha latifolia L. Virginia, United StatesOPGC2021Wild materialWide leaf blades.2132863OPGC 8496
7OPGC 8512NCBG-552Typha latifolia L. North Carolina, United StatesOPGC2021Wild material2132917OPGC 8512
8OPGC 8514NCBG-579Typha latifolia L. Maryland, United StatesOPGC2021Wild material2132928OPGC 8514
9OPGC 8429NV030-1517Typha latifolia L. Nevada, United StatesOPGC2021Wild material2120791OPGC 8429
10OPGC 8432NV030-1530Typha latifolia L. Nevada, United StatesOPGC2021Wild material2120802OPGC 8432
11OPGC 8207NEWFS-572Typha latifolia L. New Hampshire, United StatesOPGC2021Wild material2115706OPGC 8207
12OPGC 8148MARSB-496Typha latifolia L. New Jersey, United StatesOPGC2021Wild materialStem shape in cross-sectionûthe stem is round or oval in cross-sectionûLeaf blade widthû5–29 mmûLeaf blade cross-sectionûthe leaf blade is flat or rolled in at the edgesûInflorescence positionûthe inflorescence is at the tip of the plantûInflorescence branchingûthe inflorescence is on one or more stems with no branchesûFruit type (general)ûthe fruit is like a seed, and surrounded by hairsûFruit lengthû10–15 mmûLeaf position on plantûsome leaf attachment points are above the midpoint of the stemûPerianth compositionûthere are long, thin hairs attached at the base of the acheneûthere are three bristles and three scales on narrow stalks, attached at the base of the acheneûFruit cross-sectionûthe fruit is triangular to terete (circular) in cross-section2113541OPGC 8148
13OPGC 8152MARSB-608Typha latifolia L. New York, United StatesOPGC2021Wild materialRound stem, wide cylindrical infloresences at the tip of the stem2113570OPGC 8152
14OPGC 8153MARSB-645Typha latifolia L. Delaware, United StatesOPGC2021Wild materialTall green stem (reed-like) with long, thick, brown, cat-tail like inflorescence.2113578OPGC 8153
15OPGC 7957NEWFS-502Typha latifolia L. Massachusetts, United StatesOPGCSEED2019Wild material2098227OPGC 7957
16OPGC 7935NEWFS-173Typha latifolia L. Rhode Island, United StatesOPGCSEED2019Wild material2098146OPGC 7935
17OPGC 7353NV030-1341Typha latifolia L. Nevada, United StatesOPGCSEED2018Wild material1970665OPGC 7353
18OPGC 7360NV030-1361Typha latifolia L. Nevada, United StatesOPGCSEED2018Wild material1970685OPGC 7360
19OPGC 7187NV030-1151Typha latifolia L. Nevada, United StatesOPGCSEED2017Wild material1949776OPGC 7187
20OPGC 7158NM930N-164Typha latifolia L. New Mexico, United StatesOPGC2017Wild material1943612OPGC 7158
21OPGC 7112NV030-860Typha latifolia L. California, United StatesOPGCSEED2014Wild material1920691OPGC 7112
22OPGC 7063AK930-301Typha latifolia L. Alaska, United StatesOPGCSEED2012Wild material1900649OPGC 7063
23OPGC 7050WY040-75Typha latifolia L. Wyoming, United StatesOPGCSEED2012Wild material1897996OPGC 7050
24OPGC 7052WY040-82Typha latifolia L. Wyoming, United StatesOPGCSEED2012Wild material1897998OPGC 7052
25OPGC 7047MSB210579Typha latifolia L. Texas, United StatesOPGCSEED2011Wild material1895403OPGC 7047
26OPGC 8502NCBG-509Typha angustifolia L. North Carolina, United StatesOPGC2021Wild material2132892OPGC 8502
27OPGC 8503NCBG-513Typha angustifolia L. Maryland, United StatesOPGC2021Wild materialNarrow leaves and inflorescense.2132895OPGC 8503
28OPGC 8504NCBG-518Typha angustifolia L. Maryland, United StatesOPGC2021Wild material2132898OPGC 8504
29OPGC 8508NCBG-536Typha angustifolia L. Virginia, United StatesOPGC2021Wild material2132909OPGC 8508
30OPGC 8509NCBG-543Typha angustifolia L. Virginia, United StatesOPGC2021Wild material2132912OPGC 8509
31OPGC 8513NCBG-575Typha angustifolia L. Maryland, United StatesOPGC2021Wild material2132926OPGC 8513
32OPGC 7226NCBG-225Typha angustifolia L. North Carolina, United StatesOPGCSEED2018Wild material1965873OPGC 7226
33OPGC 7227NCBG-236Typha angustifolia L. North Carolina, United StatesOPGCSEED2018Wild material1965879OPGC 7227
34OPGC 7228NCBG-241Typha angustifolia L. North Carolina, United StatesOPGCSEED2018Wild material1965881OPGC 7228
35OPGC 7229NCBG-248Typha angustifolia L. North Carolina, United StatesOPGCSEED2018Wild material1965885OPGC 7229
36W6 59032NCBG-574Sagittaria latifolia Willd. Maryland, United StatesW62021Wild material2116349W6 59032
37W6 56635CBG-8953Sagittaria latifolia Willd. Nebraska, United StatesW6SEED2019Wild material2092734W6 56635
38PI 702717NCBG-648Sacciolepis striata (L.) Nash Virginia, United StatesS9SEED2019Wild material2098499PI 702717
39PI 710499NCBG-752Sesbania exaltata (Raf.) Rydb. North Carolina, United StatesS9SEED2018Wild material1966044PI 710499
40PI 698949CBG-7492Echinochloa walteri (Pursh) A. Heller Illinois, United StatesNC7SEED2017Wild material1954806PI 698949
41PI 710484CBG-7972Desmanthus illinoensis (Michx.) MacMill. ex B. L. Rob. & Fernald South Dakota, United StatesS9SEED2017Wild material 1954799PI 710484
42PI 693864AM-2014-01Spinacia tetrandra Steven ex M. Bieb. ArmeniaNC7HABITAT2014COLLECTED06/08/2014Kotajk region, vicinity of Nubarashen town.40.11836000, 44.548220001050Growing on red clay near a small spring. Water-marsh vegetation in the semi-desert belt. Edificators: Phragmites australis, Typha latifolia, and Mentha longifoliaWild materialAnnual, glabrous, 40-50 cm high, stems erect, simple, slightly branched. Seed-units falling together with leaves, spiny-corniculate, 1 cm in diameter.1922164PI 693864
43PI 693865AM-2014-02Spinacia tetrandra Steven ex M. Bieb. ArmeniaNC7HABITAT2014COLLECTED06/08/2014Ararat region, vicinity of Khor Virap monastery.39.88806000, 44.57167000860Growing near wet place along an irrigation channel. Water-marsh vegetation in the semi-desert belt. Edificators: Phragmites australis, Typha latifolia, and Salsola dendroides.Wild materialAnnual, glabrous, 40-60 cm high, stems erect, simple, slightly branched. Seed-units falling together with leaves, spiny-corniculate, 1 cm in diameter.1922165PI 693865
44PI 688898 sosM. arvensis 178143Mentha arvensis L. Utah, United StatesCORSEED2005COLLECTED09/19/20022058Herbaceous riparian meadow dominated by Stachys palustris, Carex nebrascensis, Agrostis stolonifera, Typha latifolia.Wild materialForb .15 meters tall. 1674029PI 688898 sos
45Ames 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
46Ames 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
47W6 61522CA180-292Eryngium castrense Jeps. California, United StatesW6SEED20242167621W6 61522
48W6 61524CA180-294Chlorogalum pomeridianum (DC.) Kunth California, United StatesW6SEED20242167623W6 61524
49W6 61562CA340-52Asclepias fascicularis Decne. California, United StatesW6SEED2024Wild material2168011W6 61562
50NA 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
51NA 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
52NA 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
53NA 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
54NA 88694RJL2023NJ-007Spiraea tomentosa 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.39.57318200, -74.9267370028Plants growing in part-shade to sun along the edges of McCarthys Lakes in moist-mesic to wet areas dominated by herbaceous plants. Slope: N/A. Aspect: N/A.Wild material2159122NA 88694
55NA 88695RJL2023NJ-008Aronia arbutifolia (L.) Pers. 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.39.57262400, -74.9260690028Plants growing in part-shade to sun along the edges of McCarthys Lakes and in the understory of a mixed deciduous and evergreen forest in moist-mesic to wet conditions. Slope: N/A. Aspect: N/A.Wild material2159123NA 88695
56NA 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
57Ames 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
58Ames 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
59W6 61261OR010-453Schoenoplectus acutus (Muhl. ex Bigelow) Á. Löve & D. Löve Oregon, United StatesW62023Wild materialTall round-stemmed wetland graminoid. Branching clusters of florets at top of stem. Floret scales pale grey-tan with distinct red-brown lines. Single bract that appears to be a continuation of the stem.2142216W6 61261
60W6 61267OR010-460Schoenoplectus acutus (Muhl. ex Bigelow) Á. Löve & D. Löve Oregon, United StatesW6SEED2023Wild materialTall round-stemmed wetland graminoid. Branching clusters of florets at top of stem. Floret scales pale grey-tan with distinct red-brown lines. Single bract that appears to be a continuation of the stem.2142222W6 61267
61OPGC 8848CBG- 10860Solidago riddellii Frank Illinois, United StatesOPGC2023Wild material2142306OPGC 8848
62OPGC 8849CBG- 10861Chelone glabra L. Illinois, United StatesOPGC2023Wild material2142307OPGC 8849
63W6 61417CBG- 10852Verbesina alternifolia (L.) Britton ex Kearney Illinois, United StatesW6SEED2023Wild material2142299W6 61417
64W6 61418CBG- 10853Agastache scrophulariifolia (Willd.) Kuntze Illinois, United StatesW6SEED2023Wild material2142300W6 61418
65Ames 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
66Ames 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
67Ames 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
68NA 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
69NA 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
70NA 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
71WLP 2677RJL2022NJ-008Lyonia ligustrina (L.) DC. New Jersey, United StatesNA2022COLLECTED10/24/2022Plants growing along Burlington County Road 563, Green Bank Chatsworth Road, on the west side of the road, 16.22 kilometers south of the intersection with New Jersey Hwy 72. Plants are common at this location. 39.73274000, -74.5344900015Plants growing in a depression wetland habitat in full sun. This location seems somewhat historically disturbed by development of cranberry bogs surrounding the wet site.
Soils: The underlying geology of this area is the Cohansey Formation of middle Miocene origin and comprised of sand, white to yellow with local gravel and clay. It is sometimes 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 it is interbedded with thin beds of ironstone. 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. Maximum thickness in the map area is about 60 meters; however, thickness is difficult to determine because of the irregular basal contact and extensive post-depositional erosion.
Source: USGS New Jersey Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=NJTch%3B1)
The primary soil type in the area of this collection is classified as Atsion sand, 0 to 2 percent slopes, Northern Tidewater Area. The area is close and probably overlapping with Lakehurst sand series soil. Atsion series soil is poor to slowly draining and comprised primarily of sandy marine sediments. Surface runoff is slow to very slow. This soil is strongly to extremely acid throughout the profile. This soil is generally 50-100 cm deep.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2139668WLP 2677
72WLP 2674RJL2022NJ-005Alnus serrulata (Aiton) Willd. New Jersey, United StatesNA2022COLLECTED10/24/2022Plants growing on the east side of Atlantic County Road 543, Green Bank Road, in wetlands of the Mullica River, approximately 1.01 kilometers southwest of the intersection with River Road in Green Bank, New Jersey. Plants are common but scattered on the east side of the road at this location. 39.60472300, -74.593781002Plants grow in full sun to light shade throughout this permanently wet to inundated habitat that is comprised mostly of emergent and obligate wetland herbaceous plants, deciduous shrubs, and Chamaecyparis thyoides, none reaching more than 5-10 meters tall. There are small elevation changes throughout this wetland, but the location is surrounded by water year-round.
Soils: The underlying geology of this area is the Cohansey Formation of middle Miocene origin and comprised of sand, white to yellow with local gravel and clay. It is sometimes 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 it is interbedded with thin beds of ironstone. 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. Maximum thickness in the map area is about 60 meters; however, thickness is difficult to determine because of the irregular basal contact and extensive post-depositional erosion.
Source: USGS New Jersey Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=NJTch%3B1)
The primary soil type in the area of this collection is classified as Manahawkin muck, 0 to 2 percent slopes, frequently flooded. This soil is moderately high to high in the organic layers and high in the mineral layers comprised of sandy or sandy-skeletal, siliceous, dysic, mesic terric haplosaprists. This soil is considered extremely acid or very strongly acid in the surface tier and very strongly acid or strongly acid in the lower tiers and in the mineral substratum. The mineral content of organic layers ranges from 5 to 80 percent. Organic layers consist of mostly sapric material. Some pedons have subhorizons or a surface horizon of hemic material up to 25 cm. Woody fragments range from 0 to 50 percent, by volume, in the organic layers. These fragments are mostly twigs, branches, or logs ranging in size from 3 mm to 51 cm in diameter and completely break down when rubbed or crushed. The depth of this soil ranges from 0.2-2 meters. This soil is considered wet to inundated year-round.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2139665WLP 2674
73NA 89047RJL2022PA-015Cephalanthus occidentalis L. Pennsylvania, United StatesNA2022COLLECTED10/09/2022Plants growing in the floodplain of Octoraro Creek near 698 Lees Bridge Road, West Nottingham Township, Pennsylvania on the south side of the road. Plants are locally common and spread out in the floodplain area along the Octoraro Creek. 39.73540700, -76.0922650060Plants of this species are growing in full sun to part shade of a moist to seasonally mucky and wide flood plain area adjacent to Octoraro Creek. The area is dominated by deciduous herbaceous plants, scrambling vines, shrubs and occasional small trees. Much of this wet “meadow” is dominated by aggressive stands of grasses and members of the sedge family.
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. Interestingly, this area is very close to and may interface with the adjacent formation of Ultramafic Rocks that includes serpentine, steatite, and other products of alteration of peridotites and pyroxenites.
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 Hatboro Silt Loam which consists of soils formed in alluvium derived from metamorphic and crystalline rock. They are on flood plains. Slopes range from 0 to 3 percent. Hatboro Silt Loam soils are poorly drained and have a high to very high surface runoff index. These soils are subject to periodic stream overflow, which usually occurs during the winter and spring months. The A and B horizons are moderately acidic to neutral, generally to a depth of 1-2 meters; the C horizon below ranges from a depth of 2-3 meters with uniformly acidic soils.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2139612NA 89047
74NA 89046RJL2022PA-014Alnus serrulata (Aiton) Willd. Pennsylvania, United StatesNA2022COLLECTED10/09/2022Plants growing in the floodplain of Octoraro Creek near 698 Lees Bridge Road, West Nottingham Township, Pennsylvania on the south side of the road. Plants are locally common and spread out in the floodplain area along the Octoraro Creek. 39.73579900, -76.0923830060Plants of this species are growing in full sun of a moist to seasonally mucky and wide flood plain area adjacent to Octoraro Creek. The area is dominated by deciduous herbaceous plants, scrambling vines, shrubs and occasional small trees. Much of this wet “meadow” is dominated by aggressive stands of grasses and members of the sedge family.
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. Interestingly, this area is very close to and may interface with the adjacent formation of Ultramafic Rocks that includes serpentine, steatite, and other products of alteration of peridotites and pyroxenites.
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 Hatboro Silt Loam which consists of soils formed in alluvium derived from metamorphic and crystalline rock. They are on flood plains. Slopes range from 0 to 3 percent. Hatboro Silt Loam soils are poorly drained and have a high to very high surface runoff index. These soils are subject to periodic stream overflow, which usually occurs during the winter and spring months. The A and B horizons are moderately acidic to neutral, generally to a depth of 1-2 meters; the C horizon below ranges from a depth of 2-3 meters with uniformly acidic soils.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2139611NA 89046
75Ames 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
76W6 60371OR080-93Carex aquatilis Wahlenb. Oregon, United StatesW6SEED2022Wild materialGrass-like leaves with triangular stems. Seed heads 3-5 cm long with prominent, acute scales.2138309W6 60371
77OPGC 8536NEWFS-786Verbena hastata L. Massachusetts, United StatesOPGC2021Wild materialLeaves are simple, sometimes lobed and sometimes unlobed. Flowers purple with petals that are fused into a floral tube. Iinflorescence ranges from open, showy flowers at the base of the cone shaped inflorescence to smaller florets at the tip of the inflorescence.2138853OPGC 8536
78W6 60226NEWFS-785Scirpus cyperinus (L.) Kunth Massachusetts, United StatesW62021Wild materialBranching inflorescence with rounded, fluffy spikelets on long, drooping peduncles. Although the girdle has slightly anthocyanic pigments this is S. cyperinus.2138852W6 60226
79W6 60229NEWFS-789Bolboschoenus maritimus (L.) Palla Massachusetts, United StatesW62021Wild materialLong bract subtends axillary inflorescence.2138855W6 60229
80OPGC 8499NCBG-489Hibiscus moscheutos L. Maryland, United StatesOPGC2021Wild material2132887OPGC 8499
81OPGC 8520MARSB-607Symphyotrichum subulatum (Michx.) G. L. Nesom New York, United StatesOPGC2021Wild materialSimple, alternate leaves radiate heads with white pink rays.2137181OPGC 8520
82W6 60019NCBG-523Cyperus flavicomus Michx. Virginia, United StatesW62021Wild materialConspicuous hyaline margin on spikelets.2132901W6 60019
83W6 60040NCBG-563Pluchea odorata (L.) Cass. Virginia, United StatesW62021Wild material2132922W6 60040
84W6 60046NCBG-576Leersia oryzoides (L.) Sw. Maryland, United StatesW62021Wild material2132927W6 60046
85W6 60059NCBG-724Bolboschoenus robustus (Pursh) Soják Maryland, United StatesW62021Wild material2132940W6 60059
86W6 60093MARSB-486Rhynchospora capitellata (Michx.) Vahl New Jersey, United StatesW62021Wild materialThe stem is roughly triangular in cross section. Leaf blade width 1 5 3 mm Leaf blade cross section the leaf blade is flat or rolled in at the edges Inflorescence position the inflorescence emerges from an axil or most of its parts do so the inflorescence is at the tip of the plant Inflorescence branching the inflorescence is branched Fruit type general the fruit is like a seed and surrounded by scales Fruit length 2 3 mm Leaf position on plant some leaf attachment points are above the midpoint of the stem Perianth composition there are bristles attached at the base of the achene Fruit cross section the fruit is biconvex or elliptic widest in the middle and tapering to both ends in cross section.2137178W6 60093
87W6 60095MARSB-606Pluchea odorata (L.) Cass. New York, United StatesW62021Wild materialFragrant, pink, discoid heads. Simple alternate leaves. Received as: Pluchea odorata.2137180W6 60095
88W6 60097MARSB-610Triadenum virginicum (L.) Raf. New York, United StatesW62021Wild materialSimple opposite leaves flowers with 5 light pink petals and 9 stamens2137182W6 60097
89WLP 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
90Ames 35753#470Alnus incana (L.) Moench subsp. rugosa (Du Roi) R. T. Clausen Iowa, United StatesNC7HABITAT2021COLLECTED09/29/2021Freeport Marsh located on west side of Clay Hill Road adjacent to the Upper Iowa River just 0.75 miles north of Freeprort, T98N R8W NE1/4 NE1/4 NE1/4 Sec. 1443.31297000, -91.7438000077Wet marsh with running waterWild materialClump, multi-stemmed specimens noted in nature measuring approximately 15-20 feet in height.2122094Ames 35753
91OPGC 8433NV030-1531Euthamia occidentalis Nutt. Nevada, United StatesOPGC2021Wild material2120803OPGC 8433
92OPGC 8434NV030-1532Euthamia occidentalis Nutt. Nevada, United StatesOPGC2021Wild material2120804OPGC 8434
93OPGC 8365CA170-255Apocynum cannabinum L. California, United StatesOPGC2021Wild materialPerennial forb with white flowers and opposite petioled leaves; milky latex; fruits are pairs of long slender capsules that dehisce and release wind dispersed seeds at maturity.2120350OPGC 8365
94OPGC 8367CA170-259Solidago spectabilis (D. C. Eaton) A. Gray California, United StatesOPGC2021Wild materialPerennial forb with linear petioled leaves the largest toward the base of plant; inflorescence panicle-shaped; leaves and heads glabrous; phyllaries lanceolate2120354OPGC 8367
95NA 88330CBG-10583Hypericum mutilum L. Illinois, United StatesNA2021Wild materialPlant numbers sampled estimated.2120174NA 88330
96W6 59131CBG-10191Saururus cernuus L. Illinois, United StatesW62021Wild materialReceived as: Saururus cernuus2120193W6 59131
97W6 59168CBG-10452Carex scoparia Schkuhr ex Willd. Illinois, United StatesW62021Wild material2120090W6 59168
98W6 58984NCBG-394Sagittaria lancifolia L. subsp. media (Micheli) Bogin North Carolina, United StatesW62021Wild materialReceived as: Sagittaria lancifolia ssp. media2116419W6 58984
99W6 58995NCBG-443Juncus roemerianus Scheele Virginia, United StatesW62021Wild materialsharply pointed culm2116313W6 58995
100W6 58997NCBG-445Glyceria striata (Lam.) Hitchc. Maryland, United StatesW62021Wild materialdrooping inflorescence2116315W6 58997
101W6 59014NCBG-470Cladium mariscoides (Muhl.) Torr. North Carolina, United StatesW62021Wild material2116332W6 59014
102W6 59016NCBG-472Schoenoplectus pungens (Vahl) Palla North Carolina, United StatesW62021Wild material2116334W6 59016
103W6 58706NEWFS-403Glyceria canadensis (Michx.) Trin. New Hampshire, United StatesW62021Wild material2115645W6 58706
104W6 58792NEWFS-790Schoenoplectus americanus (Pers.) Volkart ex Schinz & R. Keller Massachusetts, United StatesW62021Wild materialThere is an awn present that subtends the scales/ bracts of the cone; also differs from S. pungens by a nook or divot at the tip of the bract where the awn resides.2115731W6 58792
105NA 88281MARSB-497Cephalanthus occidentalis L. New Jersey, United StatesNA2021Wild materialGrowth formûthe plant is a shrub (i.e., a woody plant with several stems growing from the base)ûLeaf typeûthe leaf blade is simple (i.e., lobed or unlobed but not separated into leaflets)ûLeaves per nodeûthere are three leaves per node along the stemûthere are two leaves per node along the stemûLeaf blade edgesûthe edge of the leaf blade has teethûLeaf durationûthe leaves drop off in winter (or they wither but persist on the plant)ûarmature on plantûthe plant does not have spines, prickles, or thornsûLeaf blade lengthû80–150 mmûLeaf blade widthû23–150 mmûLeaf stalkûthe leaves have leaf stalksûFruit type (general)ûthe fruit is dry but does not split open when ripeûBark textureûthe bark of an adult plant is ridged or platedûthe bark of an adult plant is thin and smoothûTwig winter colorûbrownûgrayûredûBud scale numberûthere are no scales on the winter buds2113542NA 88281
106NA 88285MARSB-766Cephalanthus occidentalis L. New Jersey, United StatesNA2021Wild materialGrowth formûthe plant is a shrub (i.e., a woody plant with several stems growing from the base)ûLeaf typeûthe leaf blade is simple (i.e., lobed or unlobed but not separated into leaflets)ûLeaves per nodeûthere are three leaves per node along the stemûthere are two leaves per node along the stemûLeaf blade edgesûthe edge of the leaf blade has teethûLeaf durationûthe leaves drop off in winter (or they wither but persist on the plant)ûarmature on plantûthe plant does not have spines, prickles, or thornsûLeaf blade lengthû80–150 mmûLeaf blade widthû23–150 mmûLeaf stalkûthe leaves have leaf stalksûFruit type (general)ûthe fruit is dry but does not split open when ripeûBark textureûthe bark of an adult plant is ridged or platedûthe bark of an adult plant is thin and smoothûTwig winter colorûbrownûgrayûredûBud scale numberûthere are no scales on the winter buds2113612NA 88285
107OPGC 8147MARSB-487Rhexia mariana L. New Jersey, United StatesOPGC2021Wild materialFlower petal colorûblue to purpleûwhiteûLeaf typeûthe leaves are simple (i.e., lobed or unlobed but not separated into leaflets)ûLeaf arrangementûopposite: there are two leaves per node along the stemûLeaf blade edgesûthe edge of the leaf blade is entire (has no teeth or lobes)ûFlower symmetryûthere are two or more ways to evenly divide the flower (the flower is radially symmetrical)ûthere is only one way to evenly divide the flower (the flower is bilaterally symmetrical)ûNumber of sepals, petals or tepalsûthere are four petals, sepals, or tepals in the flowerûFusion of sepals and petalsûboth the petals and sepals are separate and not fusedûthe petals or the sepals are fused into a cup or tubeûStamen numberû8ûFruit type (general)ûthe fruit is dry and splits open when ripe2113538OPGC 8147
108W6 58602MARSB-471Elymus virginicus L. var. virginicus New Jersey, United StatesW62021Wild materialTufted perennial 5-12 dm, lvs mostly 6-10 per stem, scabrous on both sides. spikes rigidly erect. spikelets mostly paired, disarticulating below the glumes. glumes subequal, 10-30 mm, firm, bowed-out at the base. long awned up to 4 cm.2113532W6 58602
109W6 58606MARSB-484Scirpus cyperinus (L.) Kunth New Jersey, United StatesW62021Wild materialforms dense tussocks on short rhizomes. leaf blades dark green, 3-10mm wide. glomerular inflorescence of orange, wooly spikelets. seeds very small, white.2113536W6 58606
110W6 58607MARSB-485Chasmanthium laxum (L.) H. O. Yates New Jersey, United StatesW62021Wild materialtufted on short rhizomes. sheaths glabrous with ciliate margins. virgate inflorescence. spikelets v-shaped. widely spreading lemmas and paleas at maturity.2113537W6 58607
111W6 58613MARSB-498Scirpus cyperinus (L.) Kunth New Jersey, United StatesW62021Wild materialStem shape in cross-sectionûthe stem is roughly triangular in cross-sectionûthe stem is round or oval in cross-sectionûLeaf blade widthû3–10 mmûLeaf blade cross-sectionûthe leaf blade is flat or rolled in at the edgesûInflorescence positionûthe inflorescence is at the tip of the plantûInflorescence branchingûthe inflorescence is branchedûFruit type (general)ûthe fruit is like a seed, and surrounded by hairsûthe fruit is like a seed, and surrounded by scalesûFruit lengthû0.6–0.9 mmûLeaf position on plantûsome leaf attachment points are above the midpoint of the stemûthe attachment points of all the leaves are at or near the base of the plantûPerianth compositionûthere are bristles attached at the base of the acheneûFruit cross-sectionûthe fruit is lenticular (lens-shaped) in cross-sectionûthe fruit is triangular to terete (circular) in cross-section2113543W6 58613
112W6 58641MARSB-609Scirpus cyperinus (L.) Kunth New York, United StatesW62021Wild materialVaguely triangular stem, branches radiate from one point at the top of the stem, flowers are in three-dimensional, woolly egg-shaped clusters. The end stalks of the flower clusters droop and the inflorescence has long leafy bracts.2113571W6 58641
113W6 58678MARSB-762Mikania scandens (L.) Willd. New Jersey, United StatesW62021Wild materialLeaf typeûleaves are simple (i.e., lobed or unlobed but not separated into leaflets)ûLeaf arrangementûopposite: there are two leaves per node along the stemûLeaf blade edgesûthe edge of the leaf blade has no teeth or lobesûthe edge of the leaf blade has teethûFlower type in flower headsûthe flower head has disk flowers only, and lacks the strap-shaped flowersûRay flower colorûNAûTuft or plume on fruitûat least a part of the plume is made up of fine bristlesûSpines on plantûthe plant has no spinesûLeaf blade lengthû30–150 mmûDisk flower numberû1-52113608W6 58678
114WLP 2054MARSB-1023Viburnum nudum L. New York, United StatesNA2020COLLECTED12/19/2019Orange County; Warwick; West St, on residential property.61Wet meadow in full sun; growing in moist loamy sand.Seeds collected from 35+ individuals in a population of 50+ individuals, growing over an area 500 meters by 500 meters in size. Common. Seed maturation: late.2109215WLP 2054
115NA 88138NCBG-253Juniperus virginiana L. North Carolina, United StatesNASEED2019Wild material2098380NA 88138
116W6 57451NCBG-227Mikania scandens (L.) Willd. North Carolina, United StatesW6SEED2019Wild material2098375W6 57451
117W6 57455NCBG-240Mikania scandens (L.) Willd. North Carolina, United StatesW6SEED2019Wild material2098379W6 57455
118W6 57474NCBG-294Mikania scandens (L.) Willd. Maryland, United StatesW6SEED2019Wild material2098398W6 57474
119W6 57537NCBG-496Eleocharis tuberculosa (Michx.) Roem. & Schult. North Carolina, United StatesW6SEED2019Wild material2098461W6 57537
120W6 57539NCBG-498Carex glaucescens Elliott North Carolina, United StatesW6SEED2019Wild material2098463W6 57539
121W6 57547NCBG-557Cyperus haspan L. North Carolina, United StatesW6SEED2019Wild material2098471W6 57547
122W6 57551NCBG-578Saururus cernuus L. Maryland, United StatesW6SEED2019Wild material2098475W6 57551
123W6 57554NCBG-590Sparganium americanum Nutt. Maryland, United StatesW6SEED2019Wild material2098478W6 57554
124W6 57586NCBG-678Saccharum giganteum (Walter) Pers. North Carolina, United StatesW6SEED2019Wild material2098510W6 57586
125WLP 3096NCBG-435Acer rubrum L. North Carolina, United StatesNASEED2019Wild material2098450WLP 3096
126OPGC 7963NEWFS-791Solidago sempervirens L. Massachusetts, United StatesOPGCSEED2019Wild material2098245OPGC 7963
127W6 57413NEWFS-373Cornus amomum Mill. Massachusetts, United StatesW6SEED2019Wild material2098210W6 57413
128W6 57409NEWFS-350Juncus effusus L. New Hampshire, United StatesW6SEED2019Wild material2098206W6 57409
129W6 57408NEWFS-348Glyceria canadensis (Michx.) Trin. New Hampshire, United StatesW6SEED2019Wild material2098205W6 57408
130W6 57385NEWFS-281Juncus gerardi Loisel. Maine, United StatesW62019Wild material2098182W6 57385
131W6 57380NEWFS-256Carex scoparia Schkuhr ex Willd. Massachusetts, United StatesW6SEED2019Wild material2098177W6 57380
132W6 57376NEWFS-245Elymus virginicus L. Massachusetts, United StatesW6SEED2019Wild material2098173W6 57376
133W6 57113MARSB-279Eupatorium perfoliatum L. New York, United StatesW6SEED2019Wild material2097552W6 57113
134W6 57163MARSB-377Eupatorium perfoliatum L. New Jersey, United StatesW62019Wild material2097602W6 57163
135WLP 1553TK2019-02Populus ×canescens (Aiton) Sm. Mtskheta-Mtianeti, GeorgiaNA2019COLLECTED05/08/2019Mtskheta (municipality/district); ; Armazi gorge to the west of Dzegvi village.41.83866000, 44.68065000466Fragmented riparian woodland.3000+ seeds collected from 13 individuals.2109130WLP 1553
136OPGC 7472CBG-9061Verbena hastata L. Nebraska, United StatesOPGCSEED2019Wild material2092740OPGC 7472
137W6 56634CBG-8952Schoenoplectus acutus (Muhl. ex Bigelow) Á. Löve & D. Löve South Dakota, United StatesW6SEED2019Wild material2092733W6 56634
138W6 56639CBG-9059Schoenoplectus tabernaemontani (C. C. Gmel.) Palla Nebraska, United StatesW6SEED2019Wild material2092738W6 56639
139W6 56640CBG-9060Sagittaria cuneata E. Sheld. South Dakota, United StatesW6SEED2019Wild material2092739W6 56640
140NA 88433NEWFS-237Rosa palustris Marshall Connecticut, United StatesNASEED2019Wild material1976186NA 88433
141W6 56194NEWFS-347Carex comosa Boott New Hampshire, United StatesW6SEED2019Wild material1976229W6 56194
142Ames 34360Ames 34360Salix serissima (L. H. Bailey) Fernald Minnesota, United StatesNC7FLOWER2018COLLECTED11/12/2018Kunkel State Wildlife Management Area located just west of Princeton approximately 4.75 miles off 160th St. NW along south side of a tributary that runs northeast into Battle Brook Creek, T36N R27W SE 1/4 SE 1/4 Sec. 34.45.56065600, -93.67933500301MarshWild materialSalix serissima (autumn willow) is a boreal willow and an obligate wetland species whose distribution is concentrated in the northeastern United States and in Canada from Newfoundland to British Columbia. A deciduous shrub that grows from 1 to 5 m tall. Bark color ranges from olive-brown or gray in older branches to yellowish-brown in younger branches, and the youngest twigs are glossy red-brown. The leaves of mature branches are dark green and shining on the top surface with a broad whitish midrib, and paler on the bottom surface. Leaves are elliptic or lanceolate with minutely toothed margins and the distinguishing presence of glands on the petiole near the base of the leaf blade. S. serissima flowers from May to July, and fruits mature from June to September (Decker 2006). Staminate flowers are rather showy and stout measuring approximately 45-55 mm in length and 15 mm in width that peak well after leaves have emerged; anthers yellow and dense. Pistillate catkins are rather loosely flowered and slightly shorter (e.g. 25-30 mm in length) in comparison to staminate flowers; green and inconspicuous. 1968259Ames 34360
143W6 54633NCBG-208Bolboschoenus robustus (Pursh) Soják North Carolina, United StatesW62018Wild materialBolboschoenus robustus1965859W6 54633
144W6 54639NCBG-214Carex lurida Wahlenb. North Carolina, United StatesW62018Wild materialCarex lurida1965865W6 54639
145W6 54666NCBG-258Schoenoplectus pungens (Vahl) Palla North Carolina, United StatesW6SEED2018Wild materialSchoenoplectus pungens1965892W6 54666
146W6 54704NCBG-362Alnus serrulata (Aiton) Willd. Virginia, United StatesW6SEED2018Wild materialAlnus serrulata1965930W6 54704
147W6 54725NCBG-457Bolboschoenus robustus (Pursh) Soják Virginia, United StatesW6SEED2018Wild materialBolboschoenus robustus1965951W6 54725
148W6 54730NCBG-476Schoenoplectus pungens (Vahl) Palla North Carolina, United StatesW6SEED2018Wild materialSchoenoplectus pungens1965956W6 54730
149W6 54731NCBG-477Bolboschoenus robustus (Pursh) Soják North Carolina, United StatesW6SEED2018Wild materialBolboschoenus robustus1965957W6 54731
150W6 54732NCBG-478Schoenoplectus pungens (Vahl) Palla North Carolina, United StatesW6SEED2018Wild materialSchoenoplectus pungens1965958W6 54732
151W6 54737NCBG-491Bolboschoenus robustus (Pursh) Soják Virginia, United StatesW6SEED2018Wild materialBolboschoenus robustus1965963W6 54737
152W6 54738NCBG-495Bolboschoenus robustus (Pursh) Soják North Carolina, United StatesW6SEED2018Wild materialBolboschoenus robustus1965964W6 54738
153W6 54740NCBG-502Pluchea odorata (L.) Cass. North Carolina, United StatesW6SEED2018Wild materialPluchea odorata1965966W6 54740
154W6 54803NCBG-720Cakile edentula (Bigelow) Hook. Virginia, United StatesW6SEED2018Wild materialCakile edentula1966029W6 54803
155W6 54006MARSB-131Juncus effusus L. Delaware, United StatesW6SEED2018Wild materialJuncus effusus1964722W6 54006
156W6 54024MARSB-221Bolboschoenus robustus (Pursh) Soják New York, United StatesW6SEED2018Wild materialSchoenoplectus robustus1964740W6 54024
157W6 54052MARSB-378Scirpus cyperinus (L.) Kunth New Jersey, United StatesW6SEED2018Wild materialScirpus cyperinus1964768W6 54052
158W6 54072MARSB-530Pluchea odorata (L.) Cass. New Jersey, United StatesW6SEED2018Wild materialPluchea odorata1964788W6 54072
159W6 54099MARSB-644Schoenoplectus tabernaemontani (C. C. Gmel.) Palla Delaware, United StatesW6SEED2018Wild materialSchoenoplectus tabernaemontani1964815W6 54099
160W6 54116MARSB-706Bolboschoenus robustus (Pursh) Soják Delaware, United StatesW6SEED2018Wild materialBolboschoenus robustus1964832W6 54116
161W6 54139MARSB-807Bolboschoenus robustus (Pursh) Soják Delaware, United StatesW6SEED2018Wild materialBolboschoenus robustus1964855W6 54139
162OPGC 6506UT030-274Asclepias speciosa Torr. Utah, United StatesOPGCSEED2018Wild material1964416OPGC 6506
163OPGC 7191CBG-7464Epilobium ciliatum Raf. Colorado, United StatesOPGCSEED2017Wild material1954807OPGC 7191
164W6 53111CBG-7103Schoenoplectus acutus (Muhl. ex Bigelow) Á. Löve & D. Löve South Dakota, United StatesW6SEED2017Wild material1954862W6 53111
165W6 53112CBG-7288Schoenoplectus acutus (Muhl. ex Bigelow) Á. Löve & D. Löve var. acutus Iowa, United StatesW6SEED2017Wild material1954863W6 53112
166W6 52960NEWFS-236Triadenum virginicum (L.) Raf. Connecticut, United StatesW6SEED2017Wild material1954703W6 52960
167WLP 2057NEWFS-270Viburnum dentatum L. Maine, United StatesNASEED2017COLLECTED08/11/2015Scarborough Marsh WMA just off Pine Point Road along trail across from Audubon Center, Cumberland County43.56536400, -70.374827001SaltmarshWild material1954666WLP 2057
168OPGC 5075JDC/PP/2017/022/776Phlox pilosa L. subsp. fulgida (Wherry) Wherry Iowa, United StatesOPGC2017COLLECTED06/24/2017Located approximately 3.52 miles east of Boone, T84N R26W Sec. 25, Sec. 29, and Sec. 30. 42.05267600, -93.82164600350High-quality wet and dry prairie, railroad right-of-way remnant. Biologically diverse. Growing in association with Asclepias incarnata, Asclepia syriaca, Asclepias sullivantii, Coreopsis palmata (rare), Eryngium yuccafolium, Helianthus spp., Echinacea pallida, Liatris pcynostachya, Apocynum cannabinum, Toxicodendron radicans, Carex sartwellii, Cares spp., Salix humilis, Iris virginica, Rosa sp., Astragulus sp., Bromus inermis, Typha latifolia, Pastinaca sativa, Silphium laciniatum, Anemone canadensis, Cicuta maculata, and Schizachyrium scoparium. Wild materialFlower color for population is dark purple (90%) or white with purple/pink centers (10%).1950051OPGC 5075
169W6 51905OR010-294Leymus triticoides (Buckley) Pilg. Ohio, United StatesW62017Wild material1947038W6 51905
170Ames 33900JDC/SA/2017/001/755Spiraea alba Du Roi Minnesota, United StatesNC7SEED2017COLLECTED02/17/2017Located approximately 5.88 miles east of Bethel along Fawn Lake Drive just east of Fish Lake, T34N R23W SE 1/4 NE 1/4 and also NE 1/4 SE 1/4 Sec. 25, Anoka County45.40641500, -93.14546800275WetlandWild material1946796Ames 33900
171W6 51676CBG-6228Lycopus americanus Muhl. ex W. P. C. Barton Iowa, United StatesW62016Wild material1942806W6 51676
172W6 51687CBG-6303Lycopus uniflorus Michx. Colorado, United StatesW62016Wild material1942817W6 51687
173W6 51688CBG-6304Carex scoparia Schkuhr ex Willd. Colorado, United StatesW62016Wild material1942818W6 51688
174NA 82794JDC/QE/2014/132/635Quercus ellipsoidalis E. J. Hill Iowa, United StatesNA2015COLLECTED10/21/2014Pilot Knob State Park just east of Forest City. T97N R23W Ellington Township SW 1/4 SW 1/4 NE 1/4 Sec. 4 Hancock County.43.24931400, -93.56681800399Near floating bog, transition area from edge of floating bog and incline to upland habitat. Growing in association with Cephalanthus occidentalis, Salix sp., Asclepias incarnata, Typha latifolia, Spiraea alba, Populus tremuloides, Quercus rubra, Rhamnus cathartica, Carex lacustris, Carex lupulina, and Carex spp.Wild materialAcorns harvested from forest floor. Attractive, red fall color noted (peak - October 21, 2014).1928362NA 82794
175W6 50141CA650-70Anemopsis californica (Nutt.) Hook. & Arn. California, United StatesW6SEED2015Wild material1927453W6 50141
176W6 50001NV030-1022Schoenoplectus acutus (Muhl. ex Bigelow) Á. Löve & D. Löve Nevada, United StatesW6SEED2015Wild material1927024W6 50001
177W6 49577CBG-2562Sparganium eurycarpum Engelm. Illinois, United StatesW6SEED2015Wild material1926048W6 49577
178Ames 34696MARSB-074Cornus amomum Mill. New Jersey, United StatesNC7SEED2015COLLECTED08/29/2013West Essex Park just southeast of Pine Brook.40.84291000, -74.3134100051Wild material1922850Ames 34696
179WLP 1746Ames 32838Viburnum opulus L. var. americanum Aiton North Dakota, United StatesNA2014COLLECTED10/31/2014Turtle Mountains - Bottineau County.48.95000000, -100.43000000692Wet, aspen forest. Growing in association with Sanicula marilandica, Fragaria virginiana, Trifolium repens, Rubus sp., Typha latifolia, Prunus pensylvanica, Prunus virginiana, Corylus sp., Crataegus sp., Viburnum lentago, Rosa sp., Cornus sericea, Amelanchier sp., Symphoricarpos sp., Salix sp., Betula papyrifera, Populus tremuloides, Ulmus americana, Acer negundo, Quercus macrocarpa, and Fraxinus pennsylvanica.Wild material1921831WLP 1746
180Ames 32811JDC/SA/2014/130/633Spiraea alba Du Roi Iowa, United StatesNC7MISCELLANEOUS2014COLLECTED10/21/2014Pilot Knob State Park located just east of Forest City, T97N R23W SW 1/4 of SW 1/4 of NE 1/4 of Sec. 4, Ellington Township.43.24931400, -93.56681800400Floating bog. Palms muck, ponded (0-1 percent slopes) depth to water table: 0-12 inches, 0-35 inches: muck, Very poorly drainedWild material1921821Ames 32811
181WLP 859JDC/CO/2014/133/636Cephalanthus occidentalis L. Iowa, United StatesNA2014COLLECTED10/21/2014Pilot Knob State Park, SW 1/4 of SW 1/4 of NE 1/4 of Section 4, T97N, R23W, Ellington Township, just east of Forest City, Hancock County.43.24930800, -93.56627600400Floating bog. Growing in association with Asclepias incarnata, Carex lacustris, Salix, Spiraea alba, and Typha latifolia.Wild material1921818WLP 859
182W6 46120CBG-1874Scirpus cyperinus (L.) Kunth Missouri, United StatesW6SEED2013Wild material1908952W6 46120
183W6 44475UT080-69Sporobolus airoides (Torr.) Torr. Utah, United StatesW6SEED2012Wild material1901264W6 44475
184W6 42805MSB245692Fuirena simplex Vahl Texas, United StatesW6SEED2011Wild material1895269W6 42805
185Ames 31101373Spiraea alba Du Roi New York, United StatesNC7HABITAT2011COLLECTED09/14/2011Beaver Meadow Brook Watershed, along Route 426, Chautauqua County42.03600000, -79.69900000418MarshWild material1891487Ames 31101
186W6 33741UJO 53176Medicago minima (L.) Bartal. Krym, UkraineW62008COLLECTED06/28/20081.59 Km W of Teplivka village,45.02263400, 33.70138100Depression adjacent to a small earthen dam and pond, along a road way; Associated Species: Elaeagnus angustifolia, Phragmites communis, Typha latifolia, Scirpus lacustris, various sedges, grasses, clover; Land Element: open depression; Aspect: unknown; Exposure: open; Slope: 0-5%; Soil pH: unknown; Soil Moisture: moist; Soil Texture: silt loamWild material1790379W6 33741
187OPGC 2888177434Asclepias speciosa Torr. Idaho, United StatesOPGCSEED2005COLLECTED09/13/2002700Pond edge. Associated with Typha latifolia, Helianthus annuus, Kochia scoparia, Melilotus alba, Setaria viridis.Wild materialForb .3-1.2 meters tall. 1674001OPGC 2888
188W6 26840ID BFO 33Juncus balticus Willd. Idaho, United StatesW6SEED2005Wild materialGrasslike .45 meters tall. 1673879W6 26840
189W6 26848GSENM-017Schoenoplectus pungens (Vahl) Palla var. longispicatus (Britton) S. G. Sm. Utah, United StatesW6SEED2005Wild materialGrasslike 0.3-0.6 meters tall. 1673887W6 26848
190W6 26916GSENM-040Juncus alpinoarticulatus Chaix Utah, United StatesW6SEED2005Wild materialGrasslike 0.15-0.3 meters tall. 1673955W6 26916
191W6 26927GSENM-042Schoenoplectus lacustris (L.) Palla United StatesW6SEED2005Wild materialGrasslike 1.2-1.8 meters tall. 1673966W6 26927
192W6 27158OR090-13Juncus bolanderi Engelm. Oregon, United StatesW6SEED2005Wild materialGrasslike 0.45 meters tall. 1674193W6 27158
193DLEG 900380DLEG 900380Mimosa asperata L. Texas, United States SEEDHistoric1990COLLECTED07/09/1990Hidalgo Co., Along road at Boundry of Santa Ana National Wildlife Refuge.Moist soil at base of levee. Disturbed vegetation including grasses, Typha latifolia, Salix sp., Parkinsonia aculeata.Wild materialSpiny shrubs to 3 m tall; prickly stems; pink flowers in round heads. M. Johnson 90-106. Accession has been regenerated.1526467DLEG 900380