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ACCESSIONPLANT NAMETAXONOMYORIGINGENEBANKIMAGEAVAILABILITYRECEIVEDSOURCE TYPESOURCE DATECOLLECTION SITECOORDINATESELEVATIONHABITATIMPROVEMENT LEVELNARRATIVE
0W6 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
1OPGC 7577Marietta Sand PraireSolidago nemoralis Aiton Iowa, United StatesOPGCPlant2021COLLECTED10/06/2021Marietta Sand Prairie State Preserve located just northwest of Marshalltown, T84N R19W SW1/4 Sec. 1142.09830600, -93.03374300293Remnant sand prairieWild materialPlants in nature varied in height from approximately one to two feet, growing in tight clumps. Flower color was a fairly uniform light yellow, but peak flower timing varied among plants from late August to late September in 2021.2132831OPGC 7577
2OPGC 7578Marietta Sand PraireSolidago rigida L. Iowa, United StatesOPGCPlant2021COLLECTED10/06/2021Marietta Sand Prairie State Preserve located just northwest of Marshalltown, T84N R19W NW1/4 Sec. 1142.10422100, -93.03712300282Remnant sand prairieWild materialPlants in nature varied in height from approximately three to five feet and had a muted orange/red fall foliage color at the end of October 2021. Peak bloom occurred during the week of August 30 in 2021. Plants were generally growing as fairly open clumps with minimal spreading.2132832OPGC 7578
3PI 662362R07-01-002Agrostis gigantea Roth Novgorod, Russian FederationW62008COLLECTED08/08/200746 km NNE of Novgorod; Volhor River Bank. Malovishera district58.92166667, 31.5136111147Marshy meadowWild material1778048PI 662362
4PI 710731Doolittle PrairieDalea purpurea Vent. Iowa, United StatesNC7FLOWER2020COLLECTED08/26/2020Doolittle Prairie State Preserve located approximately 3 miles south of Story City. T85N, R24W, SW1/4 NE1/4 Sec. 25. Story County.42.14532900, -93.58960600299Prairie pothole wetland complex.Wild materialPlants sampled were 1-2' in height. Peak flowering and subsequent maturation of seeds at collection site peaked near 21 July and 26 August (2020), respectively. Flowers vibrant purple.2106729PI 710731
5PI 6746899106219Panicum virgatum L. New York, United StatesS92009COLLECTED10/04/2008South end of Island and along southwest edge of island; Graminoid dominated meadow immediately off of river, Saratoga County.42.77694444, -73.69000000Scattered trees at the base of steep cliffs; thin alluvial soils; also wrack from the Mohawk river. Associated vegetation: Andropogon gerardi, Cornusamomum, C. racemosa, Solidago gigantea, Sorghastrum nutans.Wild material1798152PI 674689
6PI 662361R07-01-001Phleum pratense L. Novgorod, Russian FederationW62008COLLECTED08/08/200746 km NNE of Novgorod; Volhor River Bank. Malovishera district58.92166667, 31.5136111147Marshy meadowWild material1778047PI 662361
7W6 62516FWS0300-106Rudbeckia hirta L. Michigan, United StatesW6SEED2025Wild material2192214W6 62516
8W6 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
9W6 62535FWS0300-145Verbena hastata L. Michigan, United StatesW6SEED2025Wild material2192233W6 62535
10W6 62558FWS0502-80Eutrochium fistulosum (Barratt) E. E. Lamont Pennsylvania, United StatesW6SEED2025Wild materialSCOUTING ID CHANGE. Ripe plants mostly withered but whorled leaves still hanging on2192256W6 62558
11W6 62560FWS0502-97Verbena hastata L. Pennsylvania, United StatesW6SEED2025Wild materialMixed in a dense stand of Fireweed2192258W6 62560
12OPGC 8857Marietta Sand PrairieVerbena stricta Vent. Iowa, United StatesOPGC2024COLLECTED09/04/2024Marietta Sand Prairie State Preserve located 7.5 miles northwest of Marshalltown on Knapp Avenue, T84N R19W SW ¼ Sec. 11.42.09711200, -93.03873400297Remnant sand prairie.Wild material2170474OPGC 8857
13Ames 36193Mounds SPMonarda sp.Indiana, United StatesNC7LEAF2023COLLECTED09/17/2023Mounds State Park located approximately 3.15 miles east of Anderson, T19N R8E NE 1/4 Sec. 16.40.10142600, -85.62065300258Floodplain.Wild materialThis taxa is currently undescribed and according to Campbell and Medley in The atlas of vascular plants in Kentucky (Accessed 06 September 2019) was provisionally named Monarda serotina by R.T. Simmers. Described as a broad-leaved form of M. fistulosa, generally intermediate between M. fistulosa and M. clinopodia, with probable hybrid origin. Typcial habitat is mesic woods and edges on lowlands. In contrast to M. fistulosa, this taxon has longer petioles (usually 2-3 cm versus 0.5-2.0 cm), lower leaf surfaces with scattered spreading hairs, and corollas are paler pink at tips to almost white with peak flowering occurring prior to M. fistulosa by approximately 1-2 weeks. Leaves are rather rugose, where upper leaf tissue between veins is visibly raised. This accession represents genetics from central Indiana (Mounds State Park). Plants at the collection site in nature peaked flower 8 July (2023). Plants in nature generally reaching 1.0-1.3 meters in height with about 10 percent having stacked heads. Majority of plants unbranched. 2159165Ames 36193
14W6 61387CBG- 10812Chamaecrista fasciculata (Michx.) Greene Illinois, United StatesW6SEED2023Wild material2142269W6 61387
15Ames 36027Marietta Sand PrairieSalix petiolaris Sm. Iowa, United StatesNC7PLANT2023COLLECTED03/15/2023Marietta Sand Prairie State Preserve approximately 7.5 miles northwest of Marshalltown on east side of Knapp Avenue, T84N R19W W 1/2 Sec. 11.42.09951000, -93.03668800299Remnant sand prairie in areas with likely high water table.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 central Iowa and thus the southwestern edge of the species native range. Plants sampled in nature measuring at most 5' in height. Clump-type growth habit with minimal branching, but dense suckering (e.g. 50+ ramets per genet - typically encompassing 5' x 5' area) with winter stem colors ranging from red, orange-red, yellow, dark-green, green-brown, and yellow-green. Stems glabrous. Dormant buds occassionally black, but often reddish.2141651Ames 36027
16NA 88598RJL2023FL-002aAgarista populifolia (Lam.) Judd Florida, United StatesNA2023COLLECTED02/14/2023Plants growing in woodlands of Wekiwa Springs State Park along trails accessed from the Sand Lake parking lot at the end of Palmetto Avenue. From the parking lot, take the main trail south for about 18 meters and immediately take a cut-through trail on the left to the location of this population.28.72398600, -81.4720540010Plants were growing in shade to part-shade of moist mesic hammocks of lowland transitional woodlands eventually becoming wetland habitats that are comprised primarily of evergreen plants with fewer deciduous plants. The underlying geology of this area is of Pliocene origin and characterized as the Cypresshead Formation. The Cypresshead Formation named by Huddlestun (1988), is composed of siliciclastics and occurs only in the peninsula and eastern Georgia. It is at or near the surface from northern Nassau County southward to Highlands County forming the peninsular highlands. It appears that the Cypresshead Formation occurs in the subsurface southward from the outcrop region and similar sediments, the Long Key Formation, underlie the Florida Keys. The Cypresshead Formation is a shallow marine, near shore deposit equivalent to the Citronelle Formation deltaic sediments and the Miccosukee Formation prodeltaic sediments. The Cypresshead Formation consists of reddish brown to reddish orange, unconsolidated to poorly consolidated, fine to very coarse grained, clean to clayey sands. Cross bedded sands are common within the formation. Discoid quartzite pebbles and mica are often present. Clay beds are scattered and not areally extensive. In general, the Cypresshead Formation in exposure occurs above 100 feet (30 meters) above mean sea level (msl). Original fossil material is not present in the sediments although poorly preserved molds and casts of mollusks and burrow structures are occasionally present. The presence of these fossil "ghosts" and trace fossils documents marine influence on deposition of the Cypresshead sediments. The permeable sands of the Cypresshead Formation form part of the surficial aquifer system.Wild material2141479NA 88598
17WLP 3092RJLSEUS2022-021Rhododendron prunifolium (Small) Millais Alabama, United StatesNA2023COLLECTED12/10/2023Slopes along Poke Springs Branch inlet accessed by boat from Walter F. George Reservoir. Generally uncommon, but frequent at this site. 31.72318400, -85.1290780069Plants are growing in part-shade to shade on the well-drained mostly deciduous woodland slopes approximately 3-6 meters above the inlet.
Soils: The underlying geology of this area is of Cretaceous origin and characterized as Selma Group; Providence Sand. The upper part of the profile consists of cross-bedded fine to coarse sand and white, dark-gray and pale-red-purple mottled clay containing lignite, sand, and kaolin. The lower part consists of dark-gray laminated to thin-bedded silty clay and abundantly micaceous, carbonaceous, fossiliferous very fine to fine sand.
Source: USGS Alabama Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=ALKp%3B1)
The primary soil types in the collection area are classified as Nankin-Lucy Complex soil (20 to 60 percent slopes). The Nankin Series consists of very deep, well drained, moderately slowly permeable soils on uplands of the Coastal Plain. They formed in stratified loamy and clayey marine sediments. Slopes range from 0 to 60 percent. Soils are comprised of sandy loam in the upper 25 cm to sandy clay loam and sandy clay in lower strata to about 1.7 meters deep; these soils are strongly acid. 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. Slopes vary from 0 to 45 percent. These soils are generally loamy to sandy loam in the upper 25 cm and sandy clay loam in the lower strata to 2 meters; these are strongly acid soils.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2141446WLP 3092
18NA 88543RJLSEUS2022-015Rhododendron alabamense Rehder Georgia, United StatesNA2023COLLECTED12/09/2022Plants growing above a pond in drier upland conditions as well as along the banks of the Muckalee Creek on the property of Monica Williams north of Albany, Georgia. Infrequent, but occasionally seen in drier woods; more common along Muckalee Creek. 31.63566400, -84.1337960061Plants are growing in part-shade to shade of well-drained to drier understory conditions of a mixed evergreen and deciduous woodland, approximately 2 meters above Muckalee Creek, on sandy benches where occasional scouring has resulted in lower competition. Plants are occasionally impacted by flooding; however, they are not subjected to extended periods of high moisture on a regular basis.
Soils: The underlying geology of this area is of Eocene origin and characterized as Ocala Limestone. The Ocala Limestone consists of almost pure limestones with occasional dolomites. It can be subdivided into both lower and upper facies with the lower facies composed of a whitish to cream-colored, fine to medium grained, poorly to moderately hard, fossil rich grainstone and packstone. The upper Ocala is white and somewhat weak and poorly sorted. It is extremely fossil rich grainstone, packstone and wackestone and some chert is common in the upper facies.
Source: USGS Georgia Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=GANu%3B1)
The primary soil types in the collection area are classified as Herod and Muckalee Series soils. The Herod Series consists of poorly drained moderately permeable soils formed in loamy alluvium. These soils are on flood plains of streams in the Coastal Plain. Slopes range from 0 to 2 percent. The Muckalee Series consists of poorly drained moderately permeable soils formed in loamy and sandy alluvium. These soils are on flood plains of streams in the Coastal Plain. Slopes range from 0 to 2 percent.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2140769NA 88543
19NA 88549RJLSEUS2022-022Rhododendron minus Michx. var. minus Georgia, United StatesNA2023COLLECTED12/10/2022East side of Georgia State Hwy. 39, on the south side of Kolomoki Creek approximately 11 kilometers south of Fort Gaines, Georgia. Common on this site, but otherwise infrequent. This species is near the southernmost end of its natural range.31.52053400, -85.0235160053Plants are growing in part-shade to shade of deciduous upland, dry, deciduous woodlands on steep slopes 10-15 meters above Kolomoki Creek.
Soils: The underlying geology of this area is of Paleocene origin and characterized as Tuscahoma Sand. As mapped this formation includes lower Eocene Bashi Marl Member of the Hatchetigbee Formation. This formation consists of light-gray to light-olive-gray laminated and thin-bedded carbonaceous silt and clay interbedded with fine sand; thin lignite beds occur locally. Lower part of the formation includes beds of fossiliferous, glauconitic fine quartz sand containing spheroidal sandstone concretions, gravel and clay pebbles.
Source: USGS Georgia Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=GANu%3B1)
The primary soil types in the collection area are classified as Ailey-Cowarts Complex Series soils (8 to 25 percent slopes). The Ailey Series consists of well drained or somewhat excessively drained soils formed by fluviomarine and marine deposits. These soils are found marine terraces and low hills of the upper coastal plain and sandhills; they are strongly acidic. The Cowarts Series consists of very deep, moderately well and well drained soils on ridge tops and side slopes on uplands of the Coastal Plain Major Land Resource Area. They formed in loamy marine sediments. Slopes range from 1 to 60 percent.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2140776NA 88549
20NA 88550RJLSEUS2022-023Kalmia latifolia L. Georgia, United StatesNA2023COLLECTED12/10/2022East side of Georgia State Hwy. 39, on the south side of Kolomoki Creek approximately 11 kilometers south of Fort Gaines, Georgia. Common on this site, but otherwise infrequent. This species is near the southernmost end of its natural range. 31.52053400, -85.0235160053Plants are growing in part-shade to shade of deciduous upland, dry, deciduous woodlands on steep slopes 10-15 meters above Kolomoki Creek.
Soils: The underlying geology of this area is of Paleocene origin and characterized as Tuscahoma Sand. As mapped this formation includes lower Eocene Bashi Marl Member of the Hatchetigbee Formation. This formation consists of light-gray to light-olive-gray laminated and thin-bedded carbonaceous silt and clay interbedded with fine sand; thin lignite beds occur locally. Lower part of the formation includes beds of fossiliferous, glauconitic fine quartz sand containing spheroidal sandstone concretions, gravel and clay pebbles.
Source: USGS Georgia Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=GANu%3B1)
The primary soil types in the collection area are classified as Ailey-Cowarts Complex Series soils (8 to 25 percent slopes). The Ailey Series consists of well drained or somewhat excessively drained soils formed by fluviomarine and marine deposits. These soils are found marine terraces and low hills of the upper coastal plain and sandhills; they are strongly acidic. The Cowarts Series consists of very deep, moderately well and well drained soils on ridge tops and side slopes on uplands of the Coastal Plain Major Land Resource Area. They formed in loamy marine sediments. Slopes range from 1 to 60 percent.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2140777NA 88550
21NA 88558RJLSEUS2022-031Ilex decidua Walter Alabama, United StatesNA2023COLLECTED12/12/2022Silver Creek Lake Campground off of Silver Creek Lake Road: Silver Creek Lake, at the edge of the campground.31.66344600, -87.5710840016Part shade to sun along the eroding banks of Silver Creek Lake in moist-mesic, mixed deciduous and evergreen woodland, 2-3 meters above the water. 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 Riverview Fine Sandy Loam soils (0 to 2 percent slopes, occasionally flooded). 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. Riverview soils fare on high parts of flood plains of rivers and streams draining the Coastal Plain and Southern Piedmont. Runoff is slow. Permeability is moderate. These soils flood for short periods mostly in winter or early spring months. (Source: NRCS Web Soil Survey).Wild material2140819NA 88558
22NA 88574RJLSEUS2022-047Rhododendron austrinum (Small) Rehder Florida, United StatesNA2023COLLECTED12/15/2022Plants 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. The species is found frequently along several miles of the Yellow River.30.58133600, -86.899539002Plants are found growing in part-shade to shade along areas of the river where natural levies, 1-3 meters tall, have formed, depositing sand and organic matter. The plants grow well-above normal flow of the river in well-drained to dry conditions. Even so, they are periodically subjected to inundation from floodwaters.
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 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 (https://www.nrcs.usda.gov/Internet/FSE_MANUSCRIPTS/florida/FL113/0/SantaRosa.pdf and https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild materialYellow River Pink Austrinum2140792NA 88574
23Ames 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
24Ames 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
25OPGC 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
26OPGC 7587Marietta Sand PrairiePackera plattensis (Nutt.) W. A. Weber & Á. Löve Iowa, United StatesOPGCFLOWER2022COLLECTED06/03/2022Marietta Sand Prairie State Preserve located 12.0 km northwest of Marshalltown and 10.0 km north of Highway 30 on Knapp Avenue, T84N R19W W ½ Sec. 11.42.09835700, -93.03457900299Remnant sand prairie.Wild materialPlants in nature are approximately one to two feet in height. Peak flower and fruiting in 2022 occurred on 26 May and 3 June, respectively.2138177OPGC 7587
27W6 59935CBG-10658Carex bebbii (L. H. Bailey) Olney ex Fernald Illinois, United StatesW6SEED2021Wild material2132514W6 59935
28Ames 36049CBG-9991Helianthus mollis Lam. Illinois, United StatesNC72021Wild material2120041Ames 36049
29W6 59183CBG-10474Leersia virginica Willd. Illinois, United StatesW62021Wild material2120104W6 59183
30OPGC 7559AS/VH/2020/023/098Verbena hastata L. Iowa, United StatesOPGCHABITAT2020COLLECTED10/07/2020Private property adjacent to (east of) Cedar Hills Sand Prairie, 7 miles northwest of Cedar Falls, Black Hawk County42.59408000, -92.54784000288Former cattle pasture, restored via natural succession with seed from adjacent remnant prairie.Wild materialPlants sampled in nature were approximately 2.5 to 4 feet in height.2107746OPGC 7559
31OPGC 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
32OPGC 7551Doolittle PrairieLiatris pycnostachya Michx. Iowa, United StatesOPGCHABITAT2020COLLECTED09/21/2020Doolittle Prairie State Preserve located approximately 3 miles south of Story City. T85N, R24W, SW1/4 NE1/4 Sec. 25, Story County42.14532900, -93.58960600299Prairie pothole wetland complex.Wild materialPlants sampled in nature mesaured approximately 1.5 to 3 feet in height. At time of collection (21 September 2020), approximately 10% of the seed had begun to disperse. Some plants still had green leaves, while others were entirely senesced. 2107731OPGC 7551
33OPGC 7558Doolittle PrairieVerbena hastata L. Iowa, United StatesOPGC2020COLLECTED09/21/2020Doolittle Prairie State Preserve located approximately 3.0 miles south of Story City, T85N, R24W, SW1/4 NE1/4 Sec. 25, Story County42.14849700, -93.58971400299Prairie pothole wetland complex.Wild material2107733OPGC 7558
34Ames 35688NCBG-553Monarda punctata L. North Carolina, United StatesNC7SEED2019Wild material2098470Ames 35688
35WLP 2526Franklin D. Roosevelt State ParkHydrangea quercifolia W. Bartram Georgia, United StatesNAFLOWER2019COLLECTED11/28/2018Franklin D. Roosevelt State Park, Harris County. Approximately 1.9 miles southeast of Pine Mountain along Mountain Creek.32.84099500, -84.83899300Shady streambank.Wild materialMeasurements of sampled specimen taken in nature: Height 47 to 101 in.; width 27 to 99 in.2106236WLP 2526
36W6 57113MARSB-279Eupatorium perfoliatum L. New York, United StatesW6SEED2019Wild material2097552W6 57113
37Ames 35234JDC/AS/2019/041/920Agastache scrophulariifolia (Willd.) Kuntze Minnesota, United StatesNC7HABITAT2019COLLECTED10/24/2019Private property approximately 4.94 miles south, southwest of Cannon Falls, T111N R18W NW1/4 Sec. 13, Goodhue County44.42498900, -92.93729200346Woodland edges, slightly disturbed.Wild materialPlants measuring approximately 5-6' in height with 4-5" spikes pale pink in color. Stems and petioles tomentose. Peak flowering occurred circa 1 September 2019 and fruiting circa 1 October 2019 in nature.2097770Ames 35234
38Ames 35227Castor River FloodplainMonarda sp.Missouri, United StatesNC72019COLLECTED09/10/2019Castor River floodplain (private property) located approximately 5.2 miles southwest of Grassy, T29N R8E NW 1/4 Sec. 5.37.21733000, -90.20170000128Floodplain. Deep sandy top of natural levee in open-partial shade.Wild materialThis taxa is currently undescribed and according to Campbell and Medley in The atlas of vascular plants in Kentucky (Accessed 06 September 2019) was provisionally named Monarda serotina by R.T. Simmers. Described as a broad-leaved form of M. fistulosa, generally intermediate between M. fistulosa and M. clinopodia, with probable hybrid origin. Typcial habitat is mesic woods and edges on lowlands. In contrast to M. fistulosa, this taxon has longer petioles (usually 2-3 cm versus 0.5-2.0 cm), lower leaf surfaces with scattered spreading hairs, and corollas are paler pink at tips to almost white with peak flowering occurring prior to M. fistulosa by approximately 1-2 weeks. Leaves are rather rugose, where upper leaf tissue between veins is visibly raised. This accession represents genetics from southeastern Missouri (Castor River watershed). Plants at the collection site in nature encompassed a 10 m x 10 m area and exhibited pink-purple corollas and darker spots on plants measuring approximately 1.5 m tall. In cultivation, this accession is extremely vigorous (rhizomatous) spreading to approximately two meters wide within one year after planting.2097763Ames 35227
39Ames 35226Ocoee GorgeMonarda austroappalachiana Floden Tennessee, United StatesNC7Flower2019COLLECTED09/12/2019Located just east of Lake Ocoee along highway 74 approximately 9.8 miles east, southeast of Ocoee, Polk County35.09659000, -84.54762000269Steep (some vertical) rocky cliffs and bluffs, predominately shale. Wild materialDescribed by Aaron Floden (2015) as an erect perennial (30-50 cm tall) with a strong Oregano (thymol) scent, minute retrorse to spreading trichomes at internodes and large, emaculate, white corollas. Typically flowers in late May into early June, which is earlier than both M. fistulosa and M. clinopodia where sympatric. Species is endemic to the Southern Appalachians (northern Georgia, southwest North Carolina, and southeast Tennessee) and limited to calcareous phyllite and limestone, glade-like/talus slope habitats. 2097762Ames 35226
40Ames 35216Potato Creek SPMonarda sp.Indiana, United StatesNC7Flower2019COLLECTED09/02/2019Potato Creek State Park located approximately 2.6 miles northeast of North Liberty, T36N R1E extreme eastern edge of NW 1/4 SW 1/4 Sec. 23.41.55439400, -86.38375900222Degraded floodplain, along sides of elevated road bed.Wild materialThis taxa is currently undescribed and according to Campbell and Medley in The atlas of vascular plants in Kentucky (Accessed 06 September 2019) was provisionally named Monarda serotina by R.T. Simmers. Described as a broad-leaved form of M. fistulosa, generally intermediate between M. fistulosa and M. clinopodia, with probable hybrid origin. Typcial habitat is mesic woods and edges on lowlands. In contrast to M. fistulosa, this taxon has longer petioles (usually 2-3 cm versus 0.5-2.0 cm), lower leaf surfaces with scattered spreading hairs, and corollas are paler pink at tips to almost white with peak flowering occurring prior to M. fistulosa by approximately 1-2 weeks. Leaves are rather rugose, where upper leaf tissue between veins is visibly raised. This accession represents genetics from northern Indiana (Potato Creek State Park). Plants at the collection site in nature peaked flowering near 8 July 2019 where flower colors were more lavender in sun but pale in shade (Namestnik, S., personal communication, 15 July 2020). Peak fruiting occurs mid-August. Average height of plants sampled in nature estimated at 4.5' in height.2097752Ames 35216
41W6 56643CBG-9064Trisetum spicatum (L.) K. Richt. Wyoming, United StatesW6SEED2019Wild material2092742W6 56643
42W6 56661CBG-9087Iodanthus pinnatifidus (Michx.) Steud. Kansas, United StatesW6SEED2019Wild material2092760W6 56661
43OPGC 7845CBG-8187Polemonium reptans L. Wisconsin, United StatesOPGCSEED2019Wild material SOS 7th transfer.2092671OPGC 7845
44OPGC 7773CBG-7497Eutrochium maculatum (L.) E. E. Lamont Wisconsin, United StatesOPGCSEED2017Wild material1954809OPGC 7773
45OPGC 7774CBG-7496Senecio suaveolens (L.) Elliott Wisconsin, United StatesOPGCSEED2017Wild material1954811OPGC 7774
46WLP 147NA 83890Mitchella repens L. Kentucky, United StatesNA2016COLLECTED09/27/2016Whitley County; Cumberland Falls State Park, Trail #636.83700000, -84.34000000301Wild material2110320WLP 147
47Ames 34803CBG-5442Spiraea tomentosa L. Illinois, United StatesNC7SEED2016COLLECTED09/30/2015Iroquois County Conservation Area40.99082000, -87.56577000199Wet prairie, sedge meadow.Wild material1942778Ames 34803
48OPGC 7156CBG-4795Geum aleppicum Jacq. Colorado, United StatesOPGC2016Wild material1942751OPGC 7156
49OPGC 6156CBG-2639Doellingeria umbellata (Mill.) Nees Illinois, United StatesOPGCSEED2015Wild material1926091OPGC 6156
50W6 49551CBG-2498Juncus articulatus L. Illinois, United StatesW6SEED2015Wild material1926024W6 49551
51W6 49585CBG-2571Scirpus cyperinus (L.) Kunth Illinois, United StatesW6SEED2015Wild material1926056W6 49585
52W6 49643CBG-2667Lycopus americanus Muhl. ex W. P. C. Barton Illinois, United StatesW6SEED2015Wild material1926108W6 49643
53WLP 1967HBC1401Viburnum opulus L. var. americanum Aiton North Dakota, United StatesNA2014COLLECTED09/29/2014Jay Wessels Wildlife Management Area located in Pembina County.48.80000000, -97.83000000312Diverse habitats including edge of swamp and also upland sandy soils. Growing in association Fraxinus pennsylvanica, Fraxinus nigra, Quercus macrocarpa, Acer negundo, Ulmus americana, Populus tremuloides, Populus balsamifera, Toxicodendron radicans, Cornus sericea, Rosa sp., Corylus sp., Prunus virginiana, Ribes sp., Equisetum sp., Rubus sp., IMpatiens capensis, Thalictrum dasycarpum, Fragaria virginiana, Asarum canadense, Calamagrostis canadensis, Sium suave, Solidago gigantea, Poa pratensis, and Bromus inermis.Wild material1921830WLP 1967