| 0 | Ames 32955 | JDC/BP/2015/042/699 | Betula pumila L. | Iowa, United States | NC7 |  | | 2015 | COLLECTED | 09/04/2015 | Private property approximately 7 miles northwest of Cedar Falls, T90N R14W SW 1/4 NW 1/4 SE 1/4 Sec. 18. | 42.60398800, -92.54284800 | 284 | High-quality remnant wetland/fen | Wild material | Specimens sampled averaged approximately 278 cm in height, ranging from 250 cm to 330 cm. Female catkins were both green and brown at time of harvest. Little to no fall color at time of seed collection (4 Sept. 2015) with approximately 75% of leaves already dropped. During growout in 2016, samples #699-3 and #699-5 resulted in seedlings that have petiolules (on small seedlings) that average 3-5 mm in length with the leaf apex being rather sharply acute, possibly indicating presence of hybrids. Other samples (#699-1, #699-2, #699-6, and #699-7) seem to exhibit characteristics of B. pumila with densely pubescent leaves and stems, with leaves having the apex usually broadly acute or obtuse to rounded, and essentially leaves being sessile or less than 1mm in length. | 1927397 | Ames 32955 |
| 1 | Ames 32761 | JDC/BP/2014/034/536 | Betula pumila L. | Iowa, United States | NC7 |  | | 2014 | COLLECTED | 09/03/2014 | Crossman Prairie State Preserve, approximately 5 miles northeast of Riceville, Howard County. | 43.40777300, -92.47500720 | 413 | Remnant tallgrass prairie. | Wild material | | 1921309 | Ames 32761 |
| 2 | Ames 32762 | JDC/BP/2014/044/546 | Betula pumila L. | Iowa, United States | NC7 |  | | 2014 | COLLECTED | 09/03/2014 | Private property, located approximately 2 miles south of Sumner, Bremer County. | 42.80952700, -92.10866400 | 328 | Remnant wet prairie. | Wild material | | 1921310 | Ames 32762 |
| 3 | NA 89173 | 2025RJLSEUS-14 | Chionanthus sp. | Florida, United States | NA | | | 2026 | COLLECTED | 10/03/2025 | Choctawhatchee National Forest: the collection site is reached by foot (~0.5 km) along a loose sand road/firebreak from Martin Luther King, Jr. Boulevard, just east of the boundary for Hurlburt Field in Hurlburt Field/Ft. Walton Beach, FL. Collected from 30 deg. 26.859', -86 deg. 39.577' to 30 deg. 27.137', -86 deg. 39.580'; latitude and longitude of record calculated at the midpoint of these coordinates. | 30.44996000, -86.65965000 | 10 | Dry to xeric conditions of well-drained, deep sandy soils on a relatively level area bordering a powerline in an open mixed mostly mixed evergreen and deciduous, somewhat disturbed habitat in sun to part shade. In areas “broadleaved scrub” vegetation is so dense, that it is almost impenetrable. Elevation: 9 to 11 meters. Slope: 0 to 3 percent. Aspect: Variable. Soil: The soils of this area are characterized as Foxworth Series (95 percent) sand, 0 to 5 percent slopes (8). Other soil series interbedded with the Foxworth Series, vary in percentages from 1-4 percent including Lakeland and Chipley. The Foxworth Series consists of very deep, moderately well to somewhat excessively drained, rapid to very rapid permeable soils on broad uplands and side slopes. They formed in sandy marine or eolian sediments in the Southern Coastal Plain (MLRA 133A), The Eastern Gulf Coast Flatwoods (MLRA 152A), The Atlantic Coast Flatwoods (153A) and the Tidewater Area (153B). Thickness of the grayish brown to light yellowish-brown sand exceeds 2 meters. Reaction ranges from very strongly acid to slightly acid throughout. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). Geology: The underlying geology of this area is characterized as undifferentiated Quaternary Sediments. Much of Florida's surface is covered by a varying thickness of undifferentiated sediments consisting of siliciclastics, organics and freshwater carbonates. Where these sediments exceed 6.1 meters thick, they were mapped as discrete units. To subdivide the undifferentiated sediments, those sediments occurring in flood plains were mapped as alluvial and flood plain deposits (Qal). Sediments showing surficial expression of beach ridges and dunes were mapped separately (Qbd) as were the sediments composing Trail Ridge (Qtr). Terrace sands were not mapped (refer to Healy [1975] for a discussion of the terraces in Florida). The subdivisions of the Undifferentiated Quaternary Sediments (Qu) are not lithostratigraphic units but are utilized to facilitate a better understanding of the State's geology. The siliciclastics are light gray, tan, brown to black, unconsolidated to poorly consolidated, clean to clayey, silty, unfossiliferous, variably organic-bearing sands to blue green to olive green, poorly to moderately consolidated, sandy, silty clays. Gravel is occasionally present in the panhandle. Organics occur as plant debris, roots, disseminated organic matrix and beds of peat. Freshwater carbonates, often referred to as marls in the literature, are scattered over much of the State. In southern Florida, freshwater carbonates are nearly ubiquitous in the Everglades. These sediments are buff colored to tan, unconsolidated to poorly consolidated, fossiliferous carbonate muds. Sand, silt and clay may be present in limited quantities. These carbonates often contain organics. The dominant fossils in the freshwater carbonates are mollusks. (Source: USGS Florida Geologic Map Data). | Wild material | Received as C. cf. henryae | 2193307 | NA 89173 |
| 4 | W6 62512 | FWS0300-100 | Sporobolus cryptandrus (Torr.) A. Gray | Michigan, United States | W6 |  | | 2025 | | | | | | | Wild material | | 2192210 | W6 62512 |
| 5 | W6 62513 | FWS0300-102 | Sorghastrum nutans (L.) Nash | Michigan, United States | W6 |  | | 2025 | | | | | | | Wild material | Near active artillery range | 2192211 | W6 62513 |
| 6 | W6 62517 | FWS0300-107 | Hudsonia tomentosa Nutt. | Michigan, United States | W6 |  | | 2025 | | | | | | | Wild material | | 2192215 | W6 62517 |
| 7 | W6 62518 | FWS0300-108 | Anaphalis margaritacea (L.) Benth. & Hook. f. | Michigan, United States | W6 |  | | 2025 | | | | | | | Wild material | | 2192216 | W6 62518 |
| 8 | W6 62526 | FWS0300-127 | Bromus kalmii A. Gray | Michigan, United States | W6 |  | | 2025 | | | | | | | Wild material | Near active artillery range. The above population size does not include vegetative plants. | 2192224 | W6 62526 |
| 9 | W6 62541 | FWS0300-65 | Coreopsis lanceolata L. | Michigan, United States | W6 |  | | 2025 | | | | | | | Wild material | Only scouted the part of the population on USFWS property | 2192239 | W6 62541 |
| 10 | W6 62546 | FWS0300-97 | Schizachyrium scoparium (Michx.) Nash | Michigan, United States | W6 |  | | 2025 | | | | | | | Wild material | There is Solidago vossii in the area. | 2192244 | W6 62546 |
| 11 | W6 62547 | FWS0300-98 | Andropogon gerardi Vitman | Michigan, United States | W6 |  | | 2025 | | | | | | | Wild material | There is Solidago vossii in the area. | 2192245 | W6 62547 |
| 12 | W6 62548 | FWS0300-99 | Elymus canadensis L. | Michigan, United States | W6 |  | | 2025 | | | | | | | Wild material | | 2192246 | W6 62548 |
| 13 | NA 89115 | TLM25-04a | Hamamelis ovalis S. W. Leonard | Texas, United States | NA | | | 2025 | COLLECTED | 07/10/2025 | State Highway 87 approximately 3.25 kilometers north of the crossroad junction with Texas Recreational Road 255 (RE 255); plants were growing in the narrow buffer woods along the east side of the highway. | 31.12051300, -93.72628100 | 138 | The habitat is an upland mixed coniferous and deciduous woodlands in part to full shade and dry conditions, often under drought stress. Plants seem to always occur on the top of dry ridges or well-drained slopes. Slope: 0 to 1 percent. Aspect: N/A. Soils: The soils of this collection area are classified as Tehran-Letney Association, hilly (TLE) soils. The Tehran Series (55%) consists of deep, somewhat excessively drained, moderately rapidly permeable soils on uplands. They formed in thick loamy and sandy sediments on the Western Coastal Plain. These soils are on gently sloping to moderately steep uplands with slopes ranging from 1 to 20 percent. The Letney Series (30%) consists of deep, well drained, moderately rapidly permeable, upland soils. They formed in thick sandy and loamy sediments of the coastal plains. These soils are on gently sloping to moderately steep uplands with slopes ranging from 1 to 20 percent. Soil pH ranges from 4.5 to 6.0. The minor soil components include Doucette Series (10%) and Boykin Series (5%) soils. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). Geology: The underlying geology of this area is of Oligocene origin and characterized as Catahoula Formation. This formation is extensive and deep in Texas, up to 185 meters thick. In the area of the collection the Catahoula Formation is primarily mudstone and sand. The upper 90-150 meters is mudstone that is tuffaceous, and sandy; also, occasionally, with some bentonitic clay. (Source: USGS Texas Geologic Map Data). | Wild material | | 2191654 | NA 89115 |
| 14 | NA 89078 | 2024RJLPA-004 | Staphylea trifolia L. | Pennsylvania, United States | NA | | | 2024 | COLLECTED | 09/20/2024 | Along gated road about 0.33 kilometers southwest of the Lake Ontelaunee Trail parking lot. | 40.49850800, -75.89121300 | 94 | Plants are growing on well-drained steep slopes in shade to part shade of a deciduous forest. Slope: 35 to 50 percent. Aspect: East-southeast. Geology: The underlying geology of this area is of Ordovician origin and characterized as Shale and graywacke of Hamburg sequence. It is characterized by shale containing zones of conspicuous graywacke. (Source: USGS Pennsylvania Geologic Map Data). Soils: The primary soil type in the area of this collection is classified as Berks-Weikert Complex, 25 to 60% slopes (BkF). Dominantly sloping to very steep, moderately deep and shallow, well drained soils underlain by acid shale bedrock. (Source: UPenn State University Soil Info Website). EPA Ecoregion (Level III): Ridge and Valley (67). EPA Ecoregion (Level IV): Northern Shale Valleys (67b). | Wild material | | 2169042 | NA 89078 |
| 15 | NA 88840 | RJL-RM2023FLAL-014 | Rhododendron viscosum (L.) Torr. | Florida, United States | NA | | | 2023 | COLLECTED | 12/11/2023 | Property of Floyd Griffith off View Drive on the southwest side of McCormick Lake. | 30.63247000, -85.33718200 | 56 | Plants are growing primarily in part shade a few meters above the lake, generally in areas that appear dry, but clearly are associated with hillside seeps. While much of the area has been cultivated, the remnant native flora are largely broadleaved evergreen shrub and deciduous shrub and tree species. Slope: 10 to 15 percent. Aspect: Northeast. The underlying geology of this area is the Citronelle Formation of Pliocene origin and consists of gray to orange, often mottled, unconsolidated to poorly consolidated, very fine to very coarse, poorly sorted, clean to clayey sands. It contains significant amounts of clay, silt and gravel which may occur as beds and lenses and may vary considerably over short distances. Limonite nodules and limonite-cemented beds are common. (Source: USGS Florida Geologic Map Data.) The surface soil profile of this area is primarily Pamlico-Pantego-Rutlege Association. The Pamlico series consists of very poorly drained soils that formed in decomposed organic material underlain by dominantly sandy sediment. The soils are on nearly level flood plains, bays, and depressions of the Coastal Plain. Slopes are less than 1 percent. Pamlico soils have 0.4-1.3 meters of organic material over dominantly sandy sediments. Reaction is extremely in the organic layers and ranges from extremely acid to strongly acid in the underlying mineral layers. The Pantego series consists of very deep, very poorly drained, moderately permeable soils that formed in thick loamy sediments on the Southern Coastal Plain and Atlantic Coast Flatwoods. Slopes are less than 2 percent. This soil is strongly acid. The Rutlege series comprises very deep, very poorly drained persistently wet soils on flats, depressions and floodplains where shallow ponding is common. They are of marine or fluvial sediment origin. Thickness of these loamy sandy soils is greater than 1.5 meters and a reaction from extremely acid to strongly acid. (Source: NRCS Web Soil Survey.) | Wild material | | 2165670 | NA 88840 |
| 16 | WLP 3377 | TXWL2023-024 | Viburnum dentatum L. | Texas, United States | NA | | | 2023 | COLLECTED | 12/13/2023 | Roadside between Big Cow Creek and Hardy Cemetery. | 31.03548900, -93.85086800 | | Roadside; mesic, mixed hardwood/pine forest. | Wild material | | 2165656 | WLP 3377 |
| 17 | Ames 36184 | Ames 36184 | Quercus durandii Buckley var. breviloba (Torr.) E. J. Palmer | Oklahoma, United States | NC7 |  | | 2023 | COLLECTED | 2022 | Private property located 11.0 miles west of Clinton just northeast of intersection of Highway 73 and N2140 Road, T12N R19W NE 1/4 SW 1/4 SW 1/4 Sec. 13 | 35.51213100, -99.16652700 | 518 | Rocky knolls consisting of red Permian sandstone scree and red shale outcroppings with a high pH (estimated 8.0-8.5 pH). | Wild material | Accession represents genetics of a disjunct population that is approximately 150 miles northwest of the nearest population of this taxon. Estimated to reach a mature height at 18-20’ and spread at 12-15’. Leaves are rather persistent (strong marcescence) throughout winter. Specimens are shrubby, multi-stemmed and low-branching. Often referred to as Bigelow oak and typically found throughout most of central Texas and parts of southern Oklahoma. According to Lance (2022), “Bigelow oak is mostly allopatric from typical Durand Oak in its range. East of this range, errors in herbarium annotations of juvenile Durand Oak material, where leaf shapes may mimic Bigelow oak, have caused confusion and inaccurate range extensions.” | 2159016 | Ames 36184 |
| 18 | NA 88667 | RJL2023PA-004 | Viburnum acerifolium L. | Pennsylvania, United States | NA | | | 2023 | | | | | | | Wild material | | 2158816 | NA 88667 |
| 19 | WLP 3092 | RJLSEUS2022-021 | Rhododendron prunifolium (Small) Millais | Alabama, United States | NA | | | 2023 | COLLECTED | 12/10/2023 | Slopes along Poke Springs Branch inlet accessed by boat from Walter F. George Reservoir. Generally uncommon, but frequent at this site. | 31.72318400, -85.12907800 | 69 | Plants 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 material | | 2141446 | WLP 3092 |
| 20 | NA 88559 | RJLSEUS2022-032 | Rhododendron colemanii R. F. Mill. | Alabama, United States | NA | | | 2023 | COLLECTED | 12/12/2022 | Plants growing in bottomland mostly deciduous woodlands on the south side of Lena Landegger Hwy (Monroe County Road 39) about 0.5 kilometers south of the entrance to the Alabama River Cellulose plant. Common at this site. | 31.56879700, -87.49589500 | 10 | Plants are growing in shade of a moist mesic (occasionally temporarily wet) deciduous woodland less than 1 meter above wetland habitats associated with the nearby Alabama River.
Soils: The underlying geology of this area is of Holocene origin and characterized as Alluvial, coastal and low terrace deposits. Varicolored fine to coarse quartz sand containing clay lenses and gravel in places.
Source: USGS Alabama Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=ALHalt%3B0)
The primary soil types in the collection area are classified as Chrysler Silt Loam soils (0 to 5 percent slopes, occasionally flooded). The Chrysler Series consists of deep, moderately well drained, slowly permeable soils that formed in clayey fluvial or alluvial sediments. These soils are on stream terraces of the Coastal Plain. They are strongly acid. The rate at which water runs off the surface is medium to rapid. Slopes range from 0 to 5 percent.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2140784 | NA 88559 |
| 21 | NA 88481 | RJL2022MD-002 | Kalmia latifolia L. | Maryland, United States | NA | | | 2022 | COLLECTED | 09/04/2022 | Plants growing at Elkton State Forest along roads and woodlands over a distance of approximately 5 kilometers labelled as the address of 717 Irishtown Rd, North East, MD 21901. Kalmia is very common along the unnamed gravel road as well as the understory of the upland woodlands. | 39.58852900, -75.90452900 | 60 | Plants are growing in a mesic to dry, well-drained habitat of mixed deciduous and evergreen woodlands comprised primarily of acid-loving plants. Plants are growing in shade to part shade along the unnamed road as well as the woodlands. The soils in the collection area are generally described as a complex series of fluviomarine deposits. The soils range from a thin loam layer at the surface to varying levels of loam to sandy loam and/or extremely gravelly sandy clay loam strata, depending upon geographical location (ie. Hillslope summits, slopes, footslopes, swales, etc.). The primary soil types in the collection area are classified as Russett-Christiana-Hambrook Complex and/or Sassafras and Croom Soils; though, others may intersect and overlay in specific areas. | Wild material | | 2139360 | NA 88481 |
| 22 | WLP 2600 | RJL2022FLAL-029 | Stewartia malacodendron L. | Florida, United States | NA | | | 2022 | COLLECTED | 08/07/2022 | Eglin AFB, in woodlands along Weaver Creek accessed from unnamed dirt road, 0.82 kilometers west of junction with Eglin AFB 720; approximately 0.73 kilometers north of junction with Choctaw Nolf Airfield Road and Eglin AFB 720. | 30.51680000, -86.91469400 | 15 | Growing in moist, well-drained sandy soils above Weaver Creek in mixed broadleaved evergreen and deciduous woodland habitat in part shade to shade of west facing slopes several meters above the wetland zone. The Stewartia is growing in a high competition habitat. The underlying geology of this area is the Citronelle Formation, of Pliocene origin, and consists of gray to orange, often mottled, unconsolidated to poorly consolidated, very fine to very coarse, poorly sorted, clean to clayey sands. It contains significant amounts of clay, silt and gravel which may occur as beds and lenses and may vary considerably over short distances. Limonite nodules and limonite-cemented beds are common. | Wild material | | 2138710 | WLP 2600 |
| 23 | WLP 2576 | RJL2022-001 | Amelanchier arborea (F. Michx.) Fernald | Maryland, United States | NA | | | 2022 | COLLECTED | 05/25/2022 | Plants growing in open woodlands and part shade along unnamed Elkton State Forest gravel road over a distance of approximately 5 kilometers labelled as the address of 717 Irishtown Rd, North East, MD 21901. | 39.58089500, -75.91505900 | 73 | Plants are found regularly but scattered along the unnamed gravel road as well as in open understory of the upland woodlands. Plants growing in a mesic to dry, well-drained habitat of mixed deciduous and evergreen woodlands comprised primarily of acid-loving plants. Plants are growing in part shade and open understory shade. The soils in the collection area are generally described as a complex series of fluviomarine deposits. The soils range from a thin loam layer at the surface to varying levels of loam to sandy loam and/or extremely gravelly sandy clay loam strata, depending upon geographical location (ie. Hillslope summits, slopes, footslopes, swales, etc.). The primary soil types in the collection area are classified as Russett-Christiana-Hambrook Complex and/or Sassafras and Croom Soils; though, others may intersect and overlay in specific areas. | Wild material | | 2138095 | WLP 2576 |
| 24 | Ames 35566 | SF_ID:34320/EO-ID:24816 | Agastache foeniculum (Pursh) Kuntze | Nebraska, United States | NC7 |  | | 2020 | | | | | | | Wild material | Plants measuring approximately 60-90 cm in height. Infructescences (purple) still flowering at time of harvest (19 August 2020). Population (EC-ID: 19112) at Metcalf Wildlife Management Area was originally documented by Elray S. Nixon on 15 July 1964 (Voucher #164) and later by Steven B. Rolfsmeier on 30 June 1991 (Vouchers #9127 and #9134). A. foeniculum in Nebraska is currently tracked by the Nebraska Natural Heritage Program and is listed (6 November 2019) as a S1 (Critically Imperiled - at very high risk of extirpation in the state due to very restricted range, few populations or occurrences, steep declines, severe threats or other factors) and Tier 2 species (Tier 2 - species are typically those that are not at-risk from a global or national perspective but are rare or imperiled within Nebraska). | 2107729 | Ames 35566 |
| 25 | W6 56791 | NV040-346 | Hackelia patens (Nutt.) I. M. Johnst. | Nevada, United States | W6 |  | | 2019 | | | | | | | Wild material | | 2094597 | W6 56791 |
| 26 | NA 84578 | RJL-RM002 | Magnolia pyramidata W. Bartram | Texas, United States | NA | | | 2017 | COLLECTED | 07/22/2017 | Newton County Road 425, about 2.8 miles south of Texas Recreational Road 255. | 30.85996000, -93.89596000 | 105 | Along roadsides and among young loblolly pines in forestry plantation. Plants growing in part shade to full sun in heavily regenerating roadside woodlands associated with loblolly pine plantations. Plants are growing in well drained, highly sandy soils. | Wild material | | 1953814 | NA 84578 |
| 27 | WLP 699 | NA 82755 | Amelanchier spicata (Lam.) K. Koch | Maine, United States | NA | | | 2015 | COLLECTED | 07/07/2015 | Roadside near the parking area for Bluberry Barrens (also known as Kennebunk Plains), ca. 4.5 miles west of Kennebunk. | 43.40231000, -70.62462000 | | Roadside, along shoulder of road. | | | 1952492 | WLP 699 |
| 28 | NA 82643 | NA 82643 | Lonicera sempervirens L. | Texas, United States | NA | | | 2015 | COLLECTED | 07/20/2014 | East side of Texas Route 87 approximately 0.52 miles south of Trout Creek, Texas. | 30.61156000, -93.80506000 | 21 | Southwest-facing edge of mature woodland in part to full sun; well-drained, seasonally moist soils that are sandy loam; surface has an excellent organic litter layer. | | | 1952603 | NA 82643 |
| 29 | Ames 32894 | APS/GD/2015/017/199 | Gymnocladus dioicus (L.) K. Koch | Oklahoma, United States | NC7 |  | | 2015 | COLLECTED | 03/14/2015 | Cleveland County: T10N R5W SW 1/4 SW 1/4 Sec. 7. John Nichols Camp located on north side of Canadian River approxiamtely 4.25 miles south and southeast of Mustang. | 35.35029600, -97.66952200 | 395 | Higher elevations. Dry, relatively thin soils. | Wild material | | 1925360 | Ames 32894 |
| 30 | Ames 32898 | APS/GD/2015/025/207 | Gymnocladus dioicus (L.) K. Koch | Oklahoma, United States | NC7 |  | | 2015 | COLLECTED | 03/17/2015 | Ellis County: West Creek confluence with the Canadian River, T16N R24W E 1/4 Sec. 10. Packsaddle Wildlife Management Area approximately 18 miles north of Cheyenne. | 35.87199300, -99.72757700 | 608 | Bottomlands. | Wild material | | 1925364 | Ames 32898 |
| 31 | WLP 700 | BJP/AS/2014/002 | Amelanchier spicata (Lam.) K. Koch | New Hampshire, United States | NA | | | 2014 | COLLECTED | 07/03/2014 | Rye: West side of Ocean Boulevard in Rye, on shoulder of road. | 43.01886000, -70.73382000 | | Plants on shoulder of road adjacent to marshy field. | Wild material | Full name as recorded at the U.S. National Arboretum: Amelanchier spicata (''maritima''). Received as Amelanchier spicata ''maritima.'' | 1922824 | WLP 700 |
| 32 | Ames 32767 | JDC/PV/2014/036/538 | Prunella vulgaris L. | Iowa, United States | NC7 |  | | 2014 | COLLECTED | 09/03/2014 | Crossman Prairie State Preserve, approximately 5 miles northeast of Riceville, Howard County. | 43.40777300, -92.47500720 | 413 | Remnant tallgrass prairie. | Wild material | | 1921315 | Ames 32767 |
| 33 | Ames 32769 | JDC/SA/2014/033/535 | Spiraea alba Du Roi | Iowa, United States | NC7 |  | | 2014 | COLLECTED | 09/03/2014 | Crossman Prairie State Preserve, approximately 5 miles northeast of Riceville. | 43.40777300, -92.47500720 | 413 | Remnant tallgrass prairie. Clyde-Floyd complex (1-4 percent slopes) depth to water table: 12-42 inches, 0-17 inches silty clay loam, somewhat poorly drained | Wild material | | 1921317 | Ames 32769 |
| 34 | Ames 32770 | JDC/SA/2014/043/545 | Spiraea alba Du Roi | Iowa, United States | NC7 |  | | 2014 | COLLECTED | 09/03/2014 | Brayton-Horsley Prairie located approximately 2 miles south of Sumner, T92N R11W NE 1/4 NW 1/4 SE 1/4 Sec. 2. | 42.80957200, -92.10705300 | 323 | Remnant wet prairie. Klossner muck (1-3 percent slopes) depth to water table: about 0 inches, 0-10 inches: muck, very poorly drained | Wild material | | 1921318 | Ames 32770 |
| 35 | OPGC 4196 | JDC/LP/2014/035/537 | Liatris pycnostachya Michx. | Iowa, United States | OPGC | | | 2014 | COLLECTED | 09/03/2014 | Crossman Prairie State Preserve, approximately 5 miles northeast of Riceville, Howard County. | 43.40777300, -92.47500720 | 413 | Remnant tallgrass prairie. Associated with Aesclepias, Amorpha canescens, Andropogon gerardi, Baptisia, Betula pumila, Cornus amomum, C. racemosa, Dalea purpurea, Eryngium yuccifolium, Gentiana andrewsii, Helianthus grosseserratus, Hypericum ascyron subsp. pyramidatum, Liatris pcynostachya, Monarda fistulosa, Populus tremuloides, Prunella vulgaris, Prunus americana, Salix, Silphium laciniatum, Solidago, and Spiraea alba. | Wild material | | 1921312 | OPGC 4196 |