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ACCESSIONPLANT NAMETAXONOMYORIGINGENEBANKIMAGEAVAILABILITYRECEIVEDSOURCE TYPESOURCE DATECOLLECTION SITECOORDINATESELEVATIONHABITATIMPROVEMENT LEVELNARRATIVE
0W6 62415DAK930-3Carex lenticularis Michx. Alaska, United StatesW62025Wild materialLikely var limnophila2172769W6 62415
1W6 62417DAK930-5Carex mertensii J. D. Prescott ex Bong. Alaska, United StatesW62025Wild materialNA2172771W6 62417
2W6 61268OR080-102Carex obnupta L. H. Bailey Oregon, United StatesW6SEED2023Wild materialSturdy gramminoid with large 2 inch spikes. Most often with 2 female spikes below 2-4 male spikes. Achenes are very round and firm.2142712W6 61268
3W6 61274OR080-107Carex lyngbyei Hornem. Oregon, United StatesW6SEED2023Wild materialGraminoid with leaves forming long sheathes. Strong central mid-vein. Two male heads are subtended by three females.2142718W6 61274
4W6 61358CBG- 10772Carex cephalophora Muhl. ex Willd. Wisconsin, United StatesW6SEED2023Wild material2142240W6 61358
5W6 61381CBG- 10804Carex eburnea Boott Wisconsin, United StatesW6SEED2023Wild material2142263W6 61381
6W6 60178NEWFS-701Carex crinita Lam. Massachusetts, United StatesW62021Wild materialSharp pointed perigynia that will prick upon contact in a spike about 24 long, dangling in groups of 15 from stem on long peduncle.2138804W6 60178
7W6 60180NEWFS-703Carex scoparia Schkuhr ex Willd. var. scoparia Massachusetts, United StatesW62021Wild materialReceived as: Carex scoparia var. scoparia. 0.5 inch long small rounded spikelets alterte in a densely packed cluster on stem, sometimes drooping.2138806W6 60180
8W6 60109NEWFS-338Carex lurida Wahlenb. Rhode Island, United StatesW62021Wild material2137194W6 60109
9W6 60155NEWFS-656Carex annectens (E. P. Bicknell) E. P. Bicknell Rhode Island, United StatesW62021Wild material2137240W6 60155
10W6 60171NEWFS-693Carex lurida Wahlenb. Rhode Island, United StatesW62021Wild material12 spikes with inflated perigynia pointed straight outward 15 spikes per stem.2137256W6 60171
11W6 60172NEWFS-694Carex intumescens Rudge Rhode Island, United StatesW62021Wild material0 5 1â rounded spikes with inflated perigynia pointed straight outward in radial pattern very large prominent inflated perigynia 2137257W6 60172
12W6 59935CBG-10658Carex bebbii (L. H. Bailey) Olney ex Fernald Illinois, United StatesW6SEED2021Wild material2132514W6 59935
13W6 59939CBG-10662Carex crus-corvi Shuttlew. Illinois, United StatesW6SEED2021Wild material2132518W6 59939
14W6 59088CBG-9705Carex haydenii Dewey Illinois, United StatesW62021Wild material2120018W6 59088
15W6 59092CBG-9709Carex sterilis Willd. Wisconsin, United StatesW62021Wild materialplant habit - grass, grasslike2120021W6 59092
16W6 59098CBG-9772Carex swanii (Fernald) Mack. Illinois, United StatesW62021Wild material2120027W6 59098
17W6 59226CBG-10533Carex bicknellii Britton Illinois, United StatesW62021Wild materialPlant numbers estimated.2120141W6 59226
18W6 59010NCBG-463Carex lurida Wahlenb. Virginia, United StatesW62021Wild material2116328W6 59010
19W6 58824AK930-859Carex aquatilis Wahlenb. Alaska, United StatesW62021Wild material2116007W6 58824
20W6 58857AK930-897Carex aquatilis Wahlenb. Alaska, United StatesW62021Wild material2116039W6 58857
21W6 58593MARSB-451Carex atlantica L. H. Bailey New Jersey, United StatesW62021Wild materialMultiple stellate seed heads per stem. Stems scabrous on the angles above. Perigynia greeen, usually several-nerved ventrally.2113523W6 58593
22W6 58600MARSB-466Carex lupulina Muhl. ex Willd. New Jersey, United StatesW62021Wild materialstems 2-13 dm, smooth, solitary or few together from long, dark, scaly, sympodial rhizomes.basal sheaths reddish to brownish. terminal spike staminate. pistillate spikes 2-5, ascending, ovoid to cylindric. perigynia smooth and shiny, strongly 13-22-nerved.2113530W6 58600
23W6 58630MARSB-560Carex crinita Lam. New York, United StatesW62021Wild materialTriangular stem with long, many-seeded, drooping infloresences2113560W6 58630
24W6 58518NV030-1466Carex athrostachya Olney California, United StatesW62020Wild materialLong bracts around fruit, stem with ridges.2110412W6 58518
25W6 58123OR090A-339Carex obnupta L. H. Bailey Oregon, United StatesW62020Wild material2107508W6 58123
26W6 57539NCBG-498Carex glaucescens Elliott North Carolina, United StatesW6SEED2019Wild material2098463W6 57539
27W6 57411NEWFS-370Carex crinita Lam. Massachusetts, United StatesW6SEED2019Wild material2098208W6 57411
28W6 57403NEWFS-334Carex crinita Lam. New Hampshire, United StatesW6SEED2019Wild material2098200W6 57403
29W6 57402NEWFS-330Carex annectens (E. P. Bicknell) E. P. Bicknell Rhode Island, United StatesW6SEED2019Wild material2098199W6 57402
30W6 57380NEWFS-256Carex scoparia Schkuhr ex Willd. Massachusetts, United StatesW6SEED2019Wild material2098177W6 57380
31W6 57084MARSB-216Carex annectens (E. P. Bicknell) E. P. Bicknell New York, United StatesW6SEED2019Wild material2097523W6 57084
32W6 57090MARSB-233Carex lurida Wahlenb. New York, United StatesW6SEED2019Wild material2097529W6 57090
33W6 56575CBG-8192Carex garberi Fernald Illinois, United StatesW6SEED2019Wild material2092674W6 56575
34W6 56584CBG-8203Carex brevior (Dewey) Mack. ex Lunell Wisconsin, United StatesW6SEED2019Wild material2092683W6 56584
35W6 56588CBG-8636Carex brevior (Dewey) Mack. ex Lunell Illinois, United StatesW6SEED2019Wild material2092687W6 56588
36W6 56646CBG-9068Carex hoodii Boott Wyoming, United StatesW6SEED2019Wild material2092745W6 56646
37W6 56173NEWFS-293Carex comosa Boott Massachusetts, United StatesW6SEED2019Wild material1976208W6 56173
38W6 56055AK930-644Carex atratiformis Britton Alaska, United StatesW6SEED2019Wild material1975853W6 56055
39W6 56106AK930-703Carex utriculata Boott Alaska, United StatesW6SEED2019Wild material1975847W6 56106
40W6 56090AK930-686Carex capillaris L. Alaska, United StatesW6SEED2019Wild material1975831W6 56090
41W6 56067AK930-659Carex saxatilis L. Alaska, United StatesW6SEED2019Wild material1975808W6 56067
42W6 55380OR050-263Carex douglasii Boott Oregon, United StatesW6SEED2018Wild materialCarex douglasii1967932W6 55380
43W6 54509AK930-727Carex aquatilis Wahlenb. Alaska, United StatesW6SEED2018Wild materialCarex aquatilis1965735W6 54509
44W6 54510AK930-728Carex membranacea Hook. Alaska, United StatesW6SEED2018Wild materialCarex membranacea1965736W6 54510
45W6 54511AK930-729Carex media R. Br. Alaska, United StatesW6SEED2018Wild materialCarex media1965737W6 54511
46W6 54521AK930-739Carex crawfordii Fernald Alaska, United StatesW6SEED2018Wild materialCarex crawfordii1965747W6 54521
47W6 54524AK930-742Carex utriculata Boott Alaska, United StatesW6SEED2018Wild materialCarex utriculata1965750W6 54524
48W6 54547AK930-765Carex aquatilis Wahlenb. Alaska, United StatesW6SEED2018Wild materialCarex aquatilis1965773W6 54547
49W6 54548AK930-766Carex saxatilis L. Alaska, United StatesW6SEED2018Wild materialCarex saxatilis1965774W6 54548
50W6 54549AK930-767Carex aquatilis Wahlenb. Alaska, United StatesW6SEED2018Wild materialCarex aquatilis1965775W6 54549
51W6 54582AK930-800Carex membranacea Hook. Alaska, United StatesW6SEED2018Wild materialCarex membranacea1965808W6 54582
52W6 54601AK930-819Carex membranacea Hook. Alaska, United StatesW6SEED2018Wild materialCarex membranacea1965827W6 54601
53W6 54603AK930-821Carex saxatilis L. Alaska, United StatesW6SEED2018Wild materialCarex saxatilis1965829W6 54603
54W6 54608AK930-826Carex aquatilis Wahlenb. Alaska, United StatesW6SEED2018Wild materialCarex aquatilis1965834W6 54608
55W6 54629NCBG-203Carex lurida Wahlenb. North Carolina, United StatesW62018Wild materialCarex lurida1965855W6 54629
56W6 54631NCBG-206Carex vulpinoidea Michx. North Carolina, United StatesW62018Wild materialCarex vulpinoidea1965857W6 54631
57W6 54639NCBG-214Carex lurida Wahlenb. North Carolina, United StatesW62018Wild materialCarex lurida1965865W6 54639
58W6 54724NCBG-456Carex lurida Wahlenb. Virginia, United StatesW6SEED2018Wild materialCarex lurida1965950W6 54724
59W6 54798NCBG-714Carex alata Torr. Virginia, United StatesW6SEED2018Wild materialCarex alata1966024W6 54798
60W6 54008MARSB-151Carex lurida Wahlenb. Delaware, United StatesW6SEED2018Wild materialCarex lurida1964724W6 54008
61W6 54028MARSB-234Carex comosa Boott New York, United StatesW6SEED2018Wild materialCarex comosa1964744W6 54028
62W6 54032MARSB-287Carex crinita Lam. New Jersey, United StatesW6SEED2018Wild materialCarex crinita1964748W6 54032
63W6 54033MARSB-288Carex lurida Wahlenb. New Jersey, United StatesW6SEED2018Wild materialCarex lurida1964749W6 54033
64W6 54216OR010-302Carex pellita Muhl. ex Willd. Oregon, United StatesW62018Wild materialCarex pellita1964933W6 54216
65W6 54340WY050-142Carex nebrascensis Dewey Wyoming, United StatesW6SEED2018Wild materialCarex nebrascensis1965057W6 54340
66W6 53275OR080-42Carex obnupta L. H. Bailey Oregon, United StatesW6SEED2018Wild material1957625W6 53275
67W6 53021CBG-6587Carex albicans Willd. ex Spreng. var. albicans Illinois, United StatesW6SEED2017Wild materialCarex albicans var. albicans1954772W6 53021
68W6 53022CBG-6586Carex cephalophora Muhl. ex Willd. Illinois, United StatesW6SEED2017Wild material1954773W6 53022
69W6 52969NEWFS-368Carex crinita Lam. Connecticut, United StatesW6SEED2017Wild material1954712W6 52969
70W6 51599CBG-4310Carex blanda Dewey Iowa, United StatesW62016Wild material1942729W6 51599
71W6 51600CBG-4311Carex brevior (Dewey) Mack. ex Lunell Nebraska, United StatesW62016Wild material1942730W6 51600
72W6 51638CBG-5283Carex gynandra Schwein. Wisconsin, United StatesW62016Wild material1942768W6 51638
73W6 49996NV030-1004Carex utriculata Boott Nevada, United StatesW6SEED2015Wild material1927019W6 49996
74W6 49997NV030-1007Carex leporinella Mack. Nevada, United StatesW6SEED2015Wild material1927020W6 49997
75W6 50027NV030-984Carex simulata Mack. Nevada, United StatesW6SEED2015Wild material1927049W6 50027
76W6 50033NV030-990Carex simulata Mack. Nevada, United StatesW6SEED2015Wild material1927054W6 50033
77W6 49515CBG-2446Carex sprengelii Dewey ex Spreng. Illinois, United StatesW6SEED2015Wild material1925995W6 49515
78W6 49522CBG-2457Carex muehlenbergii Schkuhr ex Willd. Illinois, United StatesW6SEED2015Wild material1926154W6 49522
79W6 49535CBG-2476Carex muehlenbergii Schkuhr ex Willd. Illinois, United StatesW6SEED2015Wild material1926160W6 49535
80W6 49542CBG-2484Carex vulpinoidea Michx. Illinois, United StatesW6SEED2015Wild material1926016W6 49542
81W6 49581CBG-2566Carex vulpinoidea Michx. Illinois, United StatesW6SEED2015Wild material1926052W6 49581
82W6 49608CBG-2609Carex hystericina Muhl. ex Willd. Colorado, United StatesW6SEED2015Wild material1926076W6 49608
83W6 48945AK930-470Carex podocarpa R. Br. Alaska, United StatesW6SEED2015Wild material1923860W6 48945
84W6 48822MARSB-46Carex atlantica L. H. Bailey New Jersey, United StatesW6SEED2015Wild material1922838W6 48822
85W6 48836MARSB-63Carex vulpinoidea Michx. West Virginia, United StatesW6SEED2015Wild material1922848W6 48836
86W6 36770UT931-99Carex simulata Mack. Utah, United StatesW6SEED2009Wild material1826924W6 36770
87W6 34204CABR2-SOSID-075-048-04Carex breweri Boott United StatesW6SEED2009Wild material1798478W6 34204
88W6 35191AZ930-206Carex senta Boott Arizona, United StatesW6SEED2009Wild material1802284W6 35191
89W6 26847GSENM-016Carex praegracilis W. Boott Utah, United StatesW6SEED2005Wild materialGrasslike 0.3 meters tall. 1673886W6 26847
90W6 26879GSENM-027Carex pellita Muhl. ex Willd. Utah, United StatesW6SEED2005Wild materialGrasslike .3-.45 meters tall. 1673918W6 26879
91W6 27132CA330-16Carex pansa L. H. Bailey California, United StatesW6SEED2005Wild materialGrasslike 0.45 meters tall. 1674167W6 27132
92W6 27133CA330-17Carex obnupta L. H. Bailey California, United StatesW6SEED2005Wild materialGrasslike 0.45-1.2 meters tall. 1674168W6 27133
93W6 27134CA330-18Carex cusickii Mack. ex Piper ex Beattie California, United StatesW6SEED2005Wild materialGrasslike 0.45-1.2 meters tall. 1674169W6 27134
94W6 27197CA330-27Carex obnupta L. H. Bailey California, United StatesW6SEED2005Wild materialGrasslike 0.45-1 meters tall. 1674232W6 27197
95W6 27254UT030-17Carex hystericina Muhl. ex Willd. Utah, United StatesW6SEED2005Wild materialGrasslike 0.15-0.3 meters tall. 1674288W6 27254
96PI 704863 sosV. angustifolium CBG-9706Vaccinium angustifolium Aiton Illinois, United StatesCOR2021Wild material2120019PI 704863 sos
97PI 704823 sosV. corymbosum MARSB-141Vaccinium corymbosum L. Delaware, United StatesCORSEED2019Wild material2097497PI 704823 sos
98PI 704821 sosF. virginiana CBG-8193Fragaria virginiana Mill. Illinois, United StatesCORSEED2019Wild material2092675PI 704821 sos
99PI 704817 sosV. uliginosum AK930-843Vaccinium uliginosum L. Alaska, United StatesCORSEED2018Wild materialVaccinium uliginosum1965851PI 704817 sos
100PI 710516NCBG-715Eleocharis obtusa (Willd.) Schult. Maryland, United StatesS9SEED2018Wild material1966025PI 710516
101PI 704814 sosV. ovatum OR080-53Vaccinium ovatum Pursh Oregon, United StatesCORSEED2018Wild material1957636PI 704814 sos
102PI 679702V. macrocarpon USFS-ONF-2015-1Vaccinium macrocarpon Aiton Michigan, United StatesCOR2016COLLECTED08/31/2015Gogebic County, Ottawa National Forest, Watersmeet Ranger District, T44N R41 W, Section 9, next to Cisco Lake Road, north side. 46.22302000, -89.43894000512Small, floating bog, surrounded by moat of open water in an area of mixed hardwoods, lakes and developed lots. Some parts of bog have a dense tangle of cranberry vines and some have only a few. Associated plants Sphagnum spp., Chamaedaphne calyculata, Eriophorum sp., Triadenum fraseri, and Iris versicolor. On one end there are more plants of Typha sp., Carex sp., and Scirpus cyperinus, with no V. macrocarpon present. No V. oxycoccos observed anywhere in bog. Wild material1933068PI 679702
103PI 710515OR010-265Eleocharis macrostachya Britton Oregon, United StatesS9SEED2015Wild material 1927502PI 710515
104PI 679661V. macrocarpon Sand Point Bog MIVaccinium macrocarpon Aiton Michigan, United StatesCOR2014COLLECTED08/06/2014Sand Point Bog, Keweenaw Bay Indian Community, Baraga County, near US 41, North of Baraga46.79693690, -88.46948284183Slope = 0; bog, 30 acres, associated plants: Sphagnum spp., V. oxycoccos, Carex lasiocarpa, Menyanthes trifoliata, Pogonia ophioglossoides, Plantanthera clavellata, Andromeda polifolia var. glaucophylla, Utricularia intermedia, small Lariz laricina, Xyris montana, Chamaedaphne calyculata, Drosera sp.Wild materialRobust population. Fruit randomly sampled.1921319PI 679661
105PI 679662V. oxycoccos Sand Point Bog MIVaccinium oxycoccos L. Michigan, United StatesCOR2014COLLECTED08/06/2014Sand Point Bog, Keweenaw Bay Indian Community, Baraga County, near US 41, North of Baraga46.79693690, -88.46948284183Slope = 0; bog, 30 acres, associated plants: Sphagnum spp., V. macrocarpon, Carex lasiocarpa, Menyanthes trifoliata, Pogonia ophioglossoides, Plantanthera clavellata, Andromeda polifolia var. glaucophylla, Utricularia intermedia, small Lariz laricina, Xyris montana, Chamaedaphne calyculata, Drosera sp.Wild materialMore common at the south end of the bog. Fruit randomly sampled.1921320PI 679662
106PI 679627V. macrocarpon Big Run Bog FR 18Vaccinium macrocarpon Aiton West Virginia, United StatesCOR2014COLLECTED04/22/2014Big Run Bog, Backbone Mountain, Monogahela National Forest, Tucker County. Next to Forest Road 1839.11812000, -79.58452000983Minerotrophic fen in a shallow basin. Many hummocks with standing water between. Fen dissected by many sloughs. A large area of open water within the fen has active beaver dams. Hummocks support small trees and shrubsWild materialPlants in fen include Spaghnum sp., Rubus hispidus, Solidago uliginosa, Eriphorum virginicum, Juncus sp., Carex spp., Scirpus sp. Gaultheria hispidula, Aronia melanocarpa, Sarracenia purpurea (introduced). Hummocks supported Picea rubens, Rhododendron maximum, Kalmia latifolia, and ferns including Osmundastrum cinnamomea. Vegetation on surrounding slopes includes Picea rubens, Tsuga canadensis, Amelanchier sp. and Pinus rigida.

Plant description: Reddish leaves. Prolific fruit production. Fruit shape, size and color typical for species. Voucher colleted. Type of propagule collected: seed

Collectors: Williams, KA; Garvey, E; Polgar, R. CRANBERRY IGRR PROJECT		1919345PI 679627
107PI 679628V. oxycoccos Big Run Bog FR 18Vaccinium oxycoccos L. West Virginia, United StatesCOR2014COLLECTED04/22/2014Big Run Bog, Backbone Mountain, Monogahela National Forest, Tucker County. Next to Forest Road 1839.11812000, -79.58452000983Minerotrophic fen in a shallow basin. Many hummocks with standing water between. Fen dissected by many sloughs. A large area of open water within the fen has active beaver dams. Hummocks support small trees and shrubsWild materialPlants in fen include Spaghnum sp., Rubus hispidus, Solidago uliginosa, Eriphorum virginicum, Juncus sp., Carex spp., Scirpus sp. Gaultheria hispidula, Aronia melanocarpa, Sarracenia purpurea (introduced). Hummocks supported Picea rubens, Rhododendron maximum, Kalmia latifolia, and ferns including Osmundastrum cinnamomea. Vegetation on surrounding slopes includes Picea rubens, Tsuga canadensis, Amelanchier sp. and Pinus rigida.

Plant description: Plant prostrate. Fruit shape, size and color typical for species. Voucher collected Type of propagule collected: seed

Collectors: Williams, KA; Garvey, E; Polgar, R. CRANBERRY IGRR PROJECT		1919346PI 679628
108PI 679629V. oxycoccos Red Run Bog FR 13Vaccinium oxycoccos L. West Virginia, United StatesCOR2014COLLECTED04/23/2014Red Run Bog, Monongahela National Forest. Tucker County. The bog is bisected by Canaan Loop Road (Forest Road 13)39.07228000, -79.473630001110Bog with two main areas (east and west) separated by forest which is interspersed with smaller boggy areas. Road runs through forested area. Gentle slope from 1115 m in the east to 1105 m in the west. The total area is approximately 100 acres.Wild materialPlants in bog include Spaghnum sp., Lycopodium sp., Rubus hispidus, Solidago uliginosa, Eriphorum virginicum, Pteridium aquilinum, Juncus sp., Carex spp., Aronia melanocarpa, and Vaccinium macrocarpon . Vegetation on surrounding slopes includes Picea rubens, Tsuga canadensis, Rhododendron maximum, Kalmia latifolia, Ilex montana, Gaultheria sp., and Viburnum prunifolium. Abies balsamea occurs on the edge of the bog.

Plant description: Abundant fruit. Fruit shape, size and color typical for species. Voucher collected Type of propagule collected: seed

Collectors: Williams, KA; Garvey, E; Polgar, R. CRANBERRY IGRR PROJECT		1919347PI 679629
109PI 679630V. macrocarpon Red Run Bog FR 13Vaccinium macrocarpon Aiton West Virginia, United StatesCOR2014COLLECTED04/23/2014Red Run Bog, Monongahela National Forest. Tucker County. The bog is bisected by Canaan Loop Road (Forest Road 13)39.07228000, -79.473630001110Bog with two main areas (east and west) separated by forest which is interspersed with smaller boggy areas. Road runs through forested area. Gentle slope from 1115 m in the east to 1105 m in the west. The total area is approximately 100 acres.Wild materialPlants in bog include Spaghnum sp., Lycopodium sp., Rubus hispidus, Solidago uliginosa, Eriphorum virginicum, Pteridium aquilinum, Juncus sp., Carex spp., Aronia melanocarpa, and Vaccinium oxycoccos . Vegetation on surrounding slopes includes Picea rubens, Tsuga canadensis, Rhododendron maximum, Kalmia latifolia, Ilex montana, Gaultheria sp., and Viburnum prunifolium. Abies balsamea occurs on the edge of the bog.

Plant description: Abundant fruit. Fruit shape, size and color typical for species. Voucher collected Type of propagule collected: seed

Collectors: Williams, KA; Garvey, E; Polgar, R. CRANBERRY IGRR PROJECT		1919348PI 679630
110PI 679631V. oxycoccos Bear Rocks Bog FR 75Vaccinium oxycoccos L. West Virginia, United StatesCOR2014COLLECTED04/23/2014Bear Rocks Bog, Dolly Sods Wilderness Area, Monongahela National Forest. Tucker County. Accessed from Forest Road 75.39.06700800, -79.304966001196Fen with spongy, saturated uneven survace and many hummocks. Water levelWild materialPlants in bog include Spaghnum sp., and other mosses. Lycopodium sp., Rubus hispidus, Eriphorum virginicum, Juncus sp., Carex spp., Gaultheria sp., and Vaccinium macrocarpon . Vegetation on surrounding slopes includes Picea rubens, Rhododendron maximum, Kalmia latifolia, and Vaccinium spp.

Plant description: Plants occasionally upright but mostly prostrate. Fruit shape, size, and color typical for species. Heavy fruit production. Voucher collected Type of propagule collected: seed

Collectors: Williams, KA; Garvey, E; Polgar, R. CRANBERRY IGRR PROJECT		1919349PI 679631
111PI 679632V. macrocarpon Bear Rocks Bog FR 75Vaccinium macrocarpon Aiton West Virginia, United StatesCOR2014COLLECTED04/23/2014Bear Rocks Bog, Dolly Sods Wilderness Area, Monongahela National Forest. Tucker County. Accessed from Forest Road 75.39.06700800, -79.304966001196Fen with spongy, saturated uneven survace and many hummocks. Water levelWild materialPlants in bog include Spaghnum sp., and other mosses. Lycopodium sp., Rubus hispidus, Eriphorum virginicum, Juncus sp., Carex spp., Gaultheria sp., and Vaccinium oxycoccos . Vegetation on surrounding slopes includes Picea rubens, Rhododendron maximum, Kalmia latifolia, and Vaccinium spp.

Plant description: Plants occasionally upright but mostly prostrate. Fruit shape, size, and color typical for species. Heavy fruit production. Voucher collected Type of propagule collected: seed

Collectors: Williams, KA; Garvey, E; Polgar, R. CRANBERRY IGRR PROJECT		1919350PI 679632
112PI 678498RU2012-5021Festuca arundinacea Schreb. Sakhalin, Russian FederationW62013COLLECTED09/04/2012Dolinsky Region, 10 km W of Dolinsk, near Oktyabrskoye Village47.34190000, 142.710200007Former collective farm yard, meadowWild material1909837PI 678498
113PI 678499RU2012-5022Poa pratensis L. Sakhalin, Russian FederationW62013COLLECTED09/04/2012Dolinsky Region, 10 km W of Dolinsk, near Oktyabrskoye Village47.34190000, 142.710200007Former collective farm yard, meadowWild material1909818PI 678499
114PI 678501RU2012-5033Elymus sibiricus L. Kabardino-Balkaria, Russian FederationW62013COLLECTED09/12/2012Nanayiskii area, along highway from Khabarovsk to Komsomolsk-na -Amure49.70060000, 137.0580000040Along highwayWild material1909827PI 678501
115PI 678900RU2012-5019Trifolium hybridum L. Sakhalin, Russian FederationW62013COLLECTED09/04/2012Dolinsky Region, 10 km W of Dolinsk, near Oktyabrskoye Village47.34190000, 142.710200007Former collective farm yard, meadowWild material1909816PI 678900
116PI 675216R10-02-006Phleum phleoides (L.) H. Karst. Stavropol, Russian FederationW6PLANT2011COLLECTED07/17/201010 km NW of Stavropol45.11500000, 41.86900000520Stony steppe surrounded by forest (Quercus robur, Q. calcarea, Fraxinus exelsior): moderate depth soils. Black A horizon, weathered limestone parent material: hay meadows: : seed collected from >100 plantsWild material1883108PI 675216
117PI 675304R10-01-005Bromus riparius Rehmann Stavropol, Russian FederationW62011COLLECTED07/17/201012 NW of Stavropol45.12900000, 41.85200000436Stony steppe surrounded by forest (Quercus robur, Q. calcarea, Fraxinus exelsior): margin of gravel pit area: scraped shallow soils. Shallow sandy black A horizon, very stony, weathered limestone parent material and outcroppings: seed collected from >100 plantsWild material1883107PI 675304
118PI 675306R10-05-023Phleum phleoides (L.) H. Karst. Stavropol, Russian FederationW62011COLLECTED07/17/2010Slope of Nedzemahnaya (never sleeping) Mountain 22 km S of Stavropol44.85100000, 41.91200000655Steppe. Shallow stony mollisol, weathered limestone: seed collected from >100 plantsWild material1883123PI 675306
119PI 675310R10-20-076Pseudoroegneria stipifolia (Czern. ex Nevski) Á. Löve Stavropol, Russian FederationW62011COLLECTED07/22/20109 km N of Kislovodsk; Borgustan Mountain Range43.98000000, 42.80000000697Mesic steppe meadow. 30% slope SW exposure, surrounded by Quercus petria forest and Fraxinus excelsior, limestone parent material: stony or pebbly soil: seed collected from >100 plantsWild material1883170PI 675310
120PI 676154R10-02-007Brachypodium rupestre (Host) Roem. & Schult. Stavropol, Russian FederationW62011COLLECTED07/17/201010 km NW of Stavropol45.11500000, 41.86900000520Stony steppe surrounded by forest (Quercus robur, Q. calcarea, Fraxinus exelsior): moderate depth soils. Black A horizon, weathered limestone parent material: hay meadows: : seed collected from >100 plantsWild material1883109PI 676154
121PI 676157R10-45-187Briza media L. subsp. elatior (Sm.) Rohlena Karačaevo-Čerkesskaja Respublika, Russian FederationW62011COLLECTED08/01/201020 km NW of Karachayevsk43.89200000, 41.87200000802Mesic steppe. Foot slopes of mountain range, N exposure, 30% slope, sandstone: seed collected from >100 plantsWild material1883274PI 676157
122PI 676206R10-45-190Poa pratensis L. subsp. angustifolia (L.) Arcang. Karačaevo-Čerkesskaja Respublika, Russian FederationW62011COLLECTED08/01/201020 km NW of Karachayevsk43.89200000, 41.87200000802Mesic steppe. Foot slopes of mountain range, N exposure, 30% slope, sandstone: seed collected from >100 plantsWild material1883277PI 676206
123PI 678468R10-01-004Lolium perenne L. Stavropol, Russian FederationW6SEED2011COLLECTED07/17/201012 NW of Stavropol45.12900000, 41.85200000436Stony steppe surrounded by forest (Quercus robur, Q. calcarea, Fraxinus exelsior): margin of gravel pit area: scraped shallow soils. Shallow sandy black A horizon, very stony, weathered limestone parent material and outcroppings: seed collected from >100 plantsWild material1883106PI 678468
124PI 678469R10-02-008Lolium perenne L. Stavropol, Russian FederationW6SEED2011COLLECTED07/17/201010 km NW of Stavropol45.11500000, 41.86900000520Stony steppe surrounded by forest (Quercus robur, Q. calcarea, Fraxinus exelsior): moderate depth soils. Black A horizon, weathered limestone parent material: hay meadows: : seed collected from >100 plantsWild material1883110PI 678469
125PI 678471R10-05-020Festuca valesiaca Schleich. ex Gaudin Stavropol, Russian FederationW62011COLLECTED07/17/2010Slope of Nedzemahnaya (never sleeping) Mountain 22 km S of Stavropol44.85100000, 41.91200000655Steppe. Shallow stony mollisol, weathered limestone: seed collected from >100 plantsWild material1883120PI 678471
126PI 678484R10-20-077Bromus riparius Rehmann Stavropol, Russian FederationW62011COLLECTED07/22/20109 km N of Kislovodsk; Borgustan Mountain Range43.98000000, 42.80000000697Mesic steppe meadow. 30% slope SW exposure, surrounded by Quercus petria forest and Fraxinus excelsior, limestone parent material: stony or pebbly soil: seed collected from >100 plantsWild material1883171PI 678484
127PI 678488R10-45-192Lolium perenne L. Karačaevo-Čerkesskaja Respublika, Russian FederationW6SEED2011COLLECTED08/01/201020 km NW of Karachayevsk43.89200000, 41.87200000802Mesic steppe. Foot slopes of mountain range, N exposure, 30% slope, sandstone: seed collected from >100 plantsWild material1883279PI 678488
128PI 685586R10-01-001Festuca rupicola Heuff. Stavropol, Russian FederationW62011COLLECTED07/17/201012 NW of Stavropol45.12900000, 41.85200000436Stony steppe surrounded by forest (Quercus robur, Q. calcarea, Fraxinus exelsior): margin of gravel pit area: scraped shallow soils. Shallow sandy black A horizon, very stony, weathered limestone parent material and outcroppings: seed collected from >100 plantsWild material1883103PI 685586
129PI 693818R10-01-002Poa compressa L. Stavropol, Russian FederationW62011COLLECTED07/17/201012 NW of Stavropol45.12900000, 41.85200000436Stony steppe surrounded by forest (Quercus robur, Q. calcarea, Fraxinus exelsior): margin of gravel pit area: scraped shallow soils. Shallow sandy black A horizon, very stony, weathered limestone parent material and outcroppings: seed collected from >100 plantsWild material1883104PI 693818
130PI 693819R10-01-003Poa pratensis L. subsp. angustifolia (L.) Arcang. Stavropol, Russian FederationW62011COLLECTED07/17/201012 NW of Stavropol45.12900000, 41.85200000436Stony steppe surrounded by forest (Quercus robur, Q. calcarea, Fraxinus exelsior): margin of gravel pit area: scraped shallow soils. Shallow sandy black A horizon, very stony, weathered limestone parent material and outcroppings: seed collected from >100 plantsWild material1883105PI 693819
131PI 693821R10-05-019Poa badensis Haenke ex Willd. Stavropol, Russian FederationW62011COLLECTED07/17/2010Slope of Nedzemahnaya (never sleeping) Mountain 22 km S of Stavropol44.85100000, 41.91200000655Steppe. Shallow stony mollisol, weathered limestone: seed collected from >100 plantsWild material1883119PI 693821
132PI 693822R10-05-022Koeleria pyramidata (Lam.) P. Beauv. Stavropol, Russian FederationW62011COLLECTED07/17/2010Slope of Nedzemahnaya (never sleeping) Mountain 22 km S of Stavropol44.85100000, 41.91200000655Steppe. Shallow stony mollisol, weathered limestone: seed collected from >100 plantsWild material1883122PI 693822
133PI 660961V. oxycoccos Dinger LakeVaccinium oxycoccos L. Oregon, United StatesCOR2009COLLECTED09/26/2009Clackamas County, Mount Hood National Forest, Dinger Lake.45.14563000, -121.846280001214Wet margins of lake (Seep) with Pinus contorta, Carex sp., Aulacomnium palustre and Vaccinium membranaceum.Wild materialDouglas Cook collection in Oregon.

1824093PI 660961
134PI 676214OR090-21Agrostis exarata Trin. Oregon, United StatesW6SEED2007Wild materialGrasslike, Height about: 1.06 m1727223PI 676214
135PI 664509194952Angelica lucida L. California, United StatesNC7SEED2005COLLECTED06/12/20033Coastal strand. Associated with Schrophularia sp, Juncus sp, Lupinus arboreus, Briza major, Tanacetum camphoratum, Carex panda, Calystegia sp and Baccharis pilularis.Wild materialForb 1.5-2 meters tall. 1674127PI 664509
136PI 699126F. vesca f. bracteata CA330-04Fragaria vesca L. California, United StatesCORSEED2005COLLECTED06/10/2003667Redwood-Douglas Fir. Associated with Rubus ursinus, Galium sp., Juncus sp., Carex sp., Rubus spectabilis and Rubus parviflorus. Slope: 0-5% SE. Soil: Clay.Wild materialSeeds of Success (SOS) program germplasm.1674126PI 699126
137PI 685559KAZ04-11-023Agropyron cristatum (L.) Gaertn. KazakhstanW6HABITAT2005COLLECTED2004Like Zhamschi, 45 km from Bektauata614Flat plain with clay and loamy soil, and no stones, somewhat poorly drained.Wild materialPopulation is occasional and pure.1668910PI 685559
138PI 693749KAZ04-10-017Poa versicolor Besser subsp. stepposa (Krylov) Tzvelev KazakhstanW6HABITAT2005COLLECTED2004Bektayata mountainains47.44722222, 74.81388889618Well-drained gray and light brown soil on 70-80 degree slope.Wild materialPopulation is frequent and uniform.1668905PI 693749
139PI 693635Jitnak tarbagataiskiAgropyron cristatum (L.) Gaertn. subsp. tarbagataicum (N. Plotn.) Tzvelev KazakhstanW62003COLLECTED08/08/2003East Kazakhstan, county Aygyz, 50 km from Ayagyz.47.59388889, 80.63750000747Near lowhills; Agropyron steppe; good drainage. Stipa capilata, Agropyron tarbagataicum, Elytrigia repens, Carex physoides, Limonium gmelinii, Salvia steposa, Trula britanica, Centaureea sp. Artemisia scoparia, Festuca gulcata.Wild materialPerennial; height 150 cm; rhizome shortly crouching; stem upright, naked, striated, under spikes short pubescent; leaf 5-8 cm long, 1.5-2 cm wide; spikelet sessile, 5-7 mm wide, spikelet glume with 3 veins, lanceolate, up to 5 mm long.1650190PI 693635
140PI 693636Pyrei polzuchiiElymus repens (L.) Gould subsp. repens KazakhstanW62003COLLECTED08/08/2003East Kazakhstan, county Aygyz, 50 km from Ayagyz.47.59388889, 80.63750000747Near lowhills; Agropyron steppe; good drainage. Stipa capilata, Agropyron tarbagataicum, Elytrigia repens, Carex physoides, Limonium gmelinii, Salvia steposa, Trula britanica, Centaureea sp. Artemisia scoparia, Festuca gulcata.Wild materialzprtrnnisl, up to 100 cm high; stem naked, leaf sheath naked; leaves plain or rolled, 5-10 mm wide, lilnear, smooth underneath, upper side is rough; spike erect, up 19 cm long, spiklets are a bit prominent.1650191PI 693636
141PI 636681TP00-37-127Elymus strictus (Keng) S. L. Chen Xizang Zizhiqu, ChinaW62001COLLECTED09/02/200028 km NW of Luhuo, Sichuan Province31.54777778, 100.465555563210Sub-alpine meadow, Picea spp. planted SOIL:Gravelly clay loam SLOPE:3% ASPECT:NEWild material1616541PI 636681
142PI 639856TP00-12-048Kengyilia melanthera (Keng) J. L. Yang et al. Xizang Zizhiqu, ChinaW62001COLLECTED08/25/20004 km S of Maqu, Gansu Province33.95750000, 102.063333333280Sand dune area south of Yellow River, sand dunes stabilized SOIL:Sandy loam SLOPE:0-5% ASPECT:VariousWild material1616090PI 639856
143PI 639860TP00-26-089Elymus dahuricus Turcz. ex Griseb. subsp. excelsus (Turcz. ex Griseb.) Tzvelev Xizang Zizhiqu, ChinaW62001COLLECTED08/30/200045 km SE of Longriba, Sichuan Province32.07861111, 102.572777783280Sub-alpine shrub, old logged forest SOIL:Gravelly loam SLOPE:30-40% ASPECT:SWWild material1616072PI 639860
144PI 639861TP00-38-134Deschampsia cespitosa (L.) P. Beauv. Xizang Zizhiqu, ChinaW62001COLLECTED09/03/200012 km E of Ganzi, Sichuan Province31.60305556, 100.153611113620Sub-alpine meadow, grass and shrub, ungrazed SOIL:Gravelly loam SLOPE:30-35% ASPECT:NWWild material1616548PI 639861
145PI 655191TP00-11-040Elymus burchan-buddae (Nevski) Tzvelev Xizang Zizhiqu, ChinaW62001COLLECTED08/25/200010 km NE of Maqu, Gansu Province34.07027778, 102.159444443660Sub-alpine meadow, upslope from road between Luqu and Maqu, not grazed SOIL:Silt loam SLOPE:40% ASPECT:SWild material1616131PI 655191
146PI 655192TP00-11-045Elymus nutans Griseb. Xizang Zizhiqu, ChinaW62001COLLECTED08/25/200010 km NE of Maqu, Gansu Province34.07027778, 102.159444443660Sub-alpine meadow, upslope from road between Luqu and Maqu, not grazed SOIL:Silt loam SLOPE:40% ASPECT:SWild material1616088PI 655192
147PI 655193TP00-12-051Elymus nutans Griseb. Xizang Zizhiqu, ChinaW62001COLLECTED08/25/20004 km S of Maqu, Gansu Province33.95750000, 102.063333333280Sand dune area south of Yellow River, sand dunes stabilized SOIL:Sandy loam SLOPE:0-5% ASPECT:VariousWild material1616091PI 655193
148PI 655194TP00-12-052Elymus burchan-buddae (Nevski) Tzvelev Xizang Zizhiqu, ChinaW62001COLLECTED08/25/20004 km S of Maqu, Gansu Province33.95750000, 102.063333333280Sand dune area south of Yellow River, sand dunes stabilized SOIL:Sandy loam SLOPE:0-5% ASPECT:VariousWild material1616092PI 655194
149PI 655195TP00-14-056Elymus nutans Griseb. Xizang Zizhiqu, ChinaW62001COLLECTED08/26/200055 km E of Maqu, Sichuan Province34.00805556, 102.750555563350Downslope from road to Zoige, winter grazing, sub-alpine meadow SOIL:Loam SLOPE:5% ASPECT:SWWild material1616095PI 655195
150PI 655196TP00-15-057Poa pratensis L. Xizang Zizhiqu, ChinaW62001COLLECTED08/26/200025 km N of Zoige, Sichuan Province33.80222222, 102.960000003300West side of road to Zoige, sub-alpine meadow SOIL:Loam SLOPE:3-5% ASPECT:WWild material1616096PI 655196
151PI 655199TP00-26-090Elymus sibiricus L. Xizang Zizhiqu, ChinaW62001COLLECTED08/30/200045 km SE of Longriba, Sichuan Province32.07861111, 102.572777783280Sub-alpine shrub, old logged forest SOIL:Gravelly loam SLOPE:30-40% ASPECT:SWWild material1616073PI 655199
152PI 655202TP00-32-108Elymus burchan-buddae (Nevski) Tzvelev Xizang Zizhiqu, ChinaW62001COLLECTED09/01/200064 km SE of Dafu, Sichuan Province30.54611111, 101.540555563550Sub-alpine meadow, oil saturated soils growing Carex. SOIL:Gravelly loam SLOPE:2-3% ASPECT:NEWild material1616576PI 655202
153PI 655206TP00-37-126Festuca ovina L. Xizang Zizhiqu, ChinaW62001COLLECTED09/02/200028 km NW of Luhuo, Sichuan Province31.54777778, 100.465555563210Sub-alpine meadow, Picea spp. planted SOIL:Gravelly clay loam SLOPE:60% ASPECT:NWild material1616569PI 655206
154PI 655207TP00-38-132Elymus burchan-buddae (Nevski) Tzvelev Xizang Zizhiqu, ChinaW62001COLLECTED09/03/200012 km E of Ganzi, Sichuan Province31.60305556, 100.153611113620Sub-alpine meadow, grass and shrub, ungrazed SOIL:Gravelly loam SLOPE:30-35% ASPECT:NWWild material1616546PI 655207
155PI 655210TP00-44-162Elymus burchan-buddae (Nevski) Tzvelev Xizang Zizhiqu, ChinaW62001COLLECTED09/07/20002 km SE of Horni Township, 45 km NE Litang, Sichuan Province30.22277778, 99.856111114000Fenced winter pasture, sub-alpine meadow SOIL:Loam SLOPE:0-5% ASPECT:SWild material1616599PI 655210
156PI 662329TP00-12-049Poa psilolepis Keng Xizang Zizhiqu, ChinaW62001COLLECTED08/25/20004 km S of Maqu, Gansu Province33.95750000, 102.063333333280Sand dune area south of Yellow River, sand dunes stabilized SOIL:Sandy loam SLOPE:0-5% ASPECT:VariousWild material1616175PI 662329
157PI 665516TP00-38-131Festuca rubra L. Xizang Zizhiqu, ChinaW62001COLLECTED09/03/200012 km E of Ganzi, Sichuan Province31.60305556, 100.153611113620Sub-alpine meadow, grass and shrub, ungrazed SOIL:Gravelly loam SLOPE:30-35% ASPECT:NWWild material1616545PI 665516
158PI 678460TP00-10-038Elymus nutans Griseb. Xizang Zizhiqu, ChinaW62001COLLECTED08/24/200035 km NE of Maqu, Gansu Province34.24694444, 102.3363888933305 km southwest of road junction to Maqu, sub-alpine meadow, winter pasture SOIL:Silt loam SLOPE:0-5% ASPECT:Flat-WWild material1616129PI 678460
159PI 693582TP00-14-055Elymus burchan-buddae (Nevski) Tzvelev Xizang Zizhiqu, ChinaW62001COLLECTED08/26/200055 km E of Maqu, Sichuan Province34.00805556, 102.750555563350Downslope from road to Zoige, winter grazing, sub-alpine meadow SOIL:Loam SLOPE:5% ASPECT:SWWild material1616094PI 693582
160PI 693588TP00-38-133Festuca ovina L. Xizang Zizhiqu, ChinaW62001COLLECTED09/03/200012 km E of Ganzi, Sichuan Province31.60305556, 100.153611113620Sub-alpine meadow, grass and shrub, ungrazed SOIL:Gravelly loam SLOPE:30-35% ASPECT:NWWild material1616547PI 693588
161PI 63409698HV-150Trifolium lupinaster L. MongoliaW6SEED1999COLLECTED09/1998Eguur Sum, Hovsgol Aimag, 3 km NE of Erdenebulgan50.12305556, 101.605000001204Egiyn River bottom, small open meadows in stands of birch and willow, Carex-grass-forb type, meadow brown soilWild materialAssociated vegetation:Galatella dahurica, Artemisia sp., Galium verum, Kobresia sibirica, Carex pediformis, Leymus chinensis, Schizonepeta multifida, Stipa sibirica, Heteropappus biennis1577917PI 634096
162PI 64155098HV-151Medicago platycarpos (L.) Trautv. MongoliaW61999COLLECTED09/1998Eguur Sum, Hovsgol Aimag, 3 km NE of Erdenebulgan50.12305556, 101.605000001204Egiyn River bottom, small open meadows in stands of birch and willow, Carex-grass-forb type, meadow brown soilWild materialAssociated vegetation:Galatella dahurica, Artemisia sp., Galium verum, Kobresia sibirica, Carex pediformis, Leymus chinensis, Schizonepeta multifida, Stipa sibirica, Heteropappus biennis1577918PI 641550
163PI 61876896S-149Poa pratensis L. MongoliaW61997COLLECTED09/1996Zavhan Aimag, Tes Sum, about 80 km east of sum center.49.50527778, 96.6350000017103% east slope. Rolling hills with rock outcrops along the hill crest. Soils are very gravelly brown sands and loamy soils. Conifers occur in protected areas.Wild materialDOMINANT VEG: Elymus secalinus + Poa pratensis, Artemisia sp., Carex sp.1543047PI 618768
164PI 641511D49Lotus corniculatus L. Chelyabinsk, Russian FederationW6SEED1996COLLECTED07/26/19955 km. south of Bekeshevskaya.44.07361111, 42.35666667823Past logged, now grazed. Slope 11-40%, aspect E. Open. Soil loam, pH 7.8-8.0. Seasonally dry, mid slope, high terrace. Vegetation closed, seasonal tall and short grass. Surrounding vegetation open deciduous forest with closed lower layers.Wild materialDominant shrub species Carpinus c., Q. petraea. Dominant herb/grass species Carex sp., Bothriochloa i., Festuca sp., Koeleria sp. Extensive regional climate data available in spreadsheet format or image maps in raster format suitable for GIS analysis. Contact Dr. Stephanie L. Greene (sgreene@ars-grin.gov).1531091PI 641511
165PI 593339OR-43Trifolium cyathiferum Lindl. Oregon, United StatesS91995COLLECTED08/09/1994Douglas Co., Tiller. South on Elk Creek Hw 1 to 1610 to 300 1/8 mile.990Small pond on east side of road at bottom of a slope. Assoc. with Madia gracilis, grasses, Menth sp, Carex sp.Wild materialCollected late in season. Much seed has been dispersed.1512577PI 593339
166PI 598831MO17.CPG94Festuca arundinacea Schreb. MoroccoW61994COLLECTED07/12/1994Near Taounate, 5 km northeast of Taounate, 1 km. east on road S304 from S302, Ketama-Taounate.34.57444444, -4.59277778380Grazed. Slope 11-40%, aspect E. Open. Soil loam,heavy calcareous,on dolomite bedrock,stony on surface,pH 8.5-9.0.Rainfall 800 mm.Moist,ravine watercourse.Vegetation closed, seasonal tall grass.Surrounding veg. seasonal tall and short grass.Wild materialPopulation distribution patchy, abundance occasional. Growth habit erect.1480208PI 598831
167PI 598879M118.CPG94Lolium perenne L. MoroccoW6SEED1994COLLECTED07/20/19942 km north of Ait-Oufella on P21, Azrou-Midelt; 52 km northwest of Midelt.33.95444444, -5.053888891880Grazed. Slope 6-10%, aspect SE. Area open. Soil loam-clay, hydromorphic on calcareous limestone type bedrock, pH 9.5-10.0. Rainfall 375 mm. Moist, ravine. Vegetation closed, evergreen tall grass. Surrounding veg. degraded evergreen forest.Wild materialPopulation abundance frequent, distribution patchy. Growth habit semi-erect.1480307PI 598879
168PI 598907M236.CPG94Lolium perenne L. MoroccoW6SEED1994COLLECTED07/29/19941 km upstream southwest of Setti Fatma off road S513 to Marrakech.31.22527778, -7.681111111375Grazed, hay. Slope 0-5%, aspect E. Open. Soil sandy, hydromorphic from granite alluvium, pH 6.5. Rainfall 700 mm. Moist, stream terrace. Veg. closed evergreen broad-leafed herb. Surrounding veg. evergreen open forest with closed lower layerWild materialPopulation abundant, distribution uniform. Growth habit erect.1480432PI 598907
169PI 598934S048.CPG94Festuca arundinacea Schreb. Sardegna, ItalyW61994COLLECTED07/06/1994Near Padru Mannu, 45 km south of Sassari and 2 km east of Hwy. 131, 1/2 km south of road to Bolotana.40.35500000, 8.79583333650Grazed. Slope 0-5%, aspect E. Area open. Soil loam, pH 6.0. Rainfall 960 mm. Seasonally dry, stream terrace. Vegetation closed, seasonal tall grass. Surrounding veg. evergreen open forest with closed lower layers.Wild materialPopulation abundance occasional, distribution patchy. Growth habit erect.1480137PI 598934
170PI 598937S057.CPG94Lolium perenne L. Sardegna, ItalyW6SEED1994COLLECTED07/06/19947 km west of Macomer to Bosa on road S121 bis.40.28805556, 8.70750000610Grazed. Slope 0-5%, aspect E. Area open. Soil loam, pH 4.0-4.5. Rainfall 1014 mm. Seasonally inundated, floodplain. Vegetation closed, seasonal tall grass. Surrounding veg. evergreen open forest with closed lower layers.Wild materialPopulation abundance frequent, distribution patchy. Growth habit semi-erect.1480146PI 598937
171PI 598938S058.CPG94Phalaris aquatica L. Sardegna, ItalyW61994COLLECTED07/06/19947 km west of Macomer to Bosa on road S121 bis.40.28805556, 8.70750000610Grazed. Slope 0-5%, aspect E. Area open. Soil loam, pH 4.0-4.5. Rainfall 1014 mm. Seasonally inundated, floodplain. Vegetation closed, seasonal tall grass. Surrounding veg. evergreen open forest wtih closed lower layers.Wild materialPopulation abundance occasional, distribution patchy. Growth habit erect.1480147PI 598938
172PI 598939S059.CPG94Lolium multiflorum Lam. Sardegna, ItalyW6SEED1994COLLECTED07/06/19947 km west of Macomer to Bosa on road S121 bis.40.28805556, 8.70750000610Grazed. Slope 0-5%, aspect E. Area open. Soil loam, pH 4.0-4.5. Rainfall 1014 mm. Seasonally inundated, floodplain. Vegetation closed, seasonal tall grass. Surrounding veg. evergreen open forest with closed lower layers.Wild materialPopulation abundance occasional, distribution patchy. Growth habit erect.1480148PI 598939
173PI 598943S076.CPG94Festuca arundinacea Schreb. Sardegna, ItalyW61994COLLECTED07/07/199411 km southeast of Fonni on road S38, Fonni-Lanusei.40.10361111, 9.316388891040Grazed. Slope 0-5%, aspect W. Area open. Soil loam, pH 6.0. Rainfall 1000 mm. Moist, stream terrace. Vegetation closed, seasonal tall grass. Surrounding veg. evergreen open forest with closed lower layers.Wild materialPopulation abundance occasional, distribution patchy. Growth habit erect.1480165PI 598943
174PI 598947S089.CPG94Phalaris aquatica L. Sardegna, ItalyW61994COLLECTED07/08/19942 km west of San Priamo, road SSN 125, San Priamo-Cagliari.39.35777778, 9.519722228Past grazed, now roadway. Slope 0-5%, aspect E. Area open. Soil loam, sandy, pH 7.0. Rainfall 660 mm. Seasonally inundated, ravine. Vegetation closed, seasonal short grass. Surrounding veg. open evergreen scrub with closed ground cover.Wild materialPopulation abundance occasional, distribution patchy. Growth habit erect.1480178PI 598947
175PI 598948S091.CPG94Festuca arundinacea Schreb. Sardegna, ItalyW61994COLLECTED07/08/199422 km west of San Priamo, road SSN 125, San Priamo-Cagliari.39.30888889, 9.39888889345Past cultivated, now grazed. Slope 0-5%, aspect E. 1/2 shade. Soil loam, alluvial-granitic, pH 7.0. Rainfall 860 mm. Seasonally inundated, stream terrace. Vegetation closed, evergreen open forest with closed lower layers.Cultivated materialPopulation abundance occasional, distribution patchy. Growth habit erect.1480180PI 598948
176PI 610906M119.CPG94Festuca arundinacea Schreb. MoroccoW61994COLLECTED07/20/1994Near Ait-Oufeua, 2 k north of Ait-Oufeua on P21, Azrou-Midelt, 52 k northwest of Midelt.33.95444444, -5.053888891880Grazed. Slope 6-10%, aspect SE. Area open. Soil loam, clay, heavy hydromorphic on calcareous limestone type bedrock, pH 9.5-10.0. Moist, ravine. Vegetation closed, evergreen tall grass. Surrounding veg. degraded evergreen forest and scrub.Wild materialPopulation abundance frequent, distribution patchy. Growth habit erect.1480308PI 610906
177PI 610928S078.CPG94Lolium perenne L. Sardegna, ItalyW6SEED1994COLLECTED07/07/199411 k southeast of Fonni on road S389, Fonni-Lanusei.40.10361111, 9.316388891040Grazed. Slope 11-40%, aspect W. 1/2 shade. Soil loam, granitic rock, pH 6.0. Rainfall 1000 mm. Seasonally dry, mid slope. Vegetation closed, seasonal tall grass. Surrounding veg. evergreen open forest with closed lower layers.Wild materialPopulation abundance frequent, distribution patchy. Growth habit semi-erect.1480167PI 610928
178PI 632473S051.CPG94Lolium perenne L. Sardegna, ItalyW6SEED1994COLLECTED07/06/1994Padru Mannu, 45 k south of Sassari, 2 k east of Hw.131, 1/2 k south of road to Bolotana.40.35500000, 8.79583333650Grazed. Slope 0-5%, aspect E. Area open. Soil loam, pH 6.0. Rainfall 960 mm. Seasonally dry, stream terrace, oak-grassland. Vegetation closed, seasonal tall grass. Surrounding veg. evergreen open forest with closed lower layers.Wild materialPopulation abundance frequent, distribution patchy. Growth habit semi-erect.1480140PI 632473
179PI 632474S019.CPG94Lolium perenne L. Sardegna, ItalyW6SEED1994COLLECTED07/04/1994Near Ozieri, 6 k east of Ozieri on road SS128bis, Ozieri-Battada.40.56861111, 9.04833333545Grazed. Slope 0-5%, aspect N. Area open. Soil clay, pH 7.0. Rainfall 670 mm. Moist, basin, swale zone. Vegetation closed, evergreen broad-leafed herb veg. Surrounding veg. dryland forage agri.Wild materialPopulation abundance frequent, distribution patchy. Growth habit semi-erect.1480108PI 632474
180PI 632592M122.CPG94Dactylis glomerata L. MoroccoW61994COLLECTED07/20/1994Near Ait-Oufeua, 2 k north of Ait-Oufeua on P21, Azrou-Midelt, 52 k northwest of Midelt.33.95444444, -5.053888891880Grazed. Slope 6-10%, aspect SE-SW. Open. Soil loam, heavy hydromorphic on calcareous limestone bedrock, pH 9.5-10.0. Seasonally dry, lower slope. Vegetation closed, evergreen tall grass. Surrounding veg. degraded evergreen forest and scrub.Wild materialPopulation abundance frequent, distribution patchy. Growth habit erect.1480311PI 632592
181PI 636537S063.CPG94Festuca arundinacea Schreb. Sardegna, ItalyW61994COLLECTED07/06/199416 k east of Macomer on road SS129 to Nuoro, 1 k south on dirt road.40.29083333, 8.94611111255Grazed. Slope 0-5%, aspect S. Area open. Soil loam, pH 6.0-6.5. Rainfall 755 mm. Moist, stream terrace. Vegetation closed, seasonal tall grass. Surrounding veg. seasonal short grass. Dominant herb/grass sp. couch, bermuda, tall fescue.Wild materialPopulation abundance frequent, distribution patchy. Growth habit erect.1480152PI 636537
182PI 636540S090.CPG94Festuca arundinacea Schreb. Sardegna, ItalyW61994COLLECTED07/08/19942 k west of San Priamo, road SSN 125, San Priamo-Cagliari.39.35777778, 9.519722228Past grazed, now roadway. Slope 0-5%, aspect E. Open. Soil sandy loam, pH 7.0. Rainfall 660 mm. Seasonally flooded, ravine, alluvial plain. Veg. closed, seasonal short grass. Surrounding veg. open evergreen scrub with closed ground cover.Wild materialPopulation abundance rare, distribution patchy. Growth habit erect.1480179PI 636540
183PI 641423M121.CPG94Lotus corniculatus L. MoroccoW61994COLLECTED07/20/1994Near Ait-Oufeua, 2 k north of Ait-Oufeua on P21, Azrou-Midelt, 52 k northwest of Midelt.33.95444444, -5.053888891880Grazed. Slope 6-10%, aspect SE. Area open. Soil loam, clay, heavy hydromorphic on calcareous limestone type bedrock, pH 9.5-10.0. Moist, ravine. Vegetation closed, evergreen tall grass. Surrounding veg. degraded evergreen forest and scrub.Wild materialPopulation abundance frequent, distribution patchy. Growth habit prostrate. Flower yellow.1480310PI 641423
184PI 641426S020.CPG94Trifolium pratense L. Sardegna, ItalyW61994COLLECTED07/04/1994Near Ozieri, 6 k east of Ozieri on road SS128bis, Ozieri-Battada.40.56861111, 9.04833333545Grazed. Slope 0-5%, aspect N. Area open. Soil clay, pH 7.0. Rainfall 670 mm. Moist, basin, swale zone. Vegetation closed, evergreen broad-leafed herb veg. Surrounding veg. dryland forage agri.Wild materialPopulation abundance frequent, distribution patchy. Growth habit semi-erect. Flower purple/red.1480109PI 641426
185PI 655711MO10.CPG94Trifolium repens L. MoroccoW61994COLLECTED07/12/1994Near Bab-Berred, 10 km. east of Bab-Berred on road P39, Chefchaouen to Al-Hoceima.34.99277778, -4.822777781330Grazed. Slope 0-5%, aspect N. Light open. Soil sandy loam on shale/schist bedrock, pH 5.0-5.5. Seasonally inundated, basin, spring bog. Assoc. spp. bracken ferns, Lotus palustris, tall fescue, Carex-Cyperns spp., perennial Poa sp.Wild materialPopulation distribution patchy, abundance frequent. Growth habit prostrate. Flower white.1480201PI 655711
186PI 655734M120.CPG94Trifolium fragiferum L. MoroccoW61994COLLECTED07/20/1994Near Ait-Oufeua, 2 k north of Ait-Oufeua on P21, Azrou-Midelt, 52 k northwest of Midelt.33.95444444, -5.053888891880Grazed. Slope 6-10%, aspect SE. Area open. Soil loam, clay, heavy hydromorphic on calcareous limestone type bedrock, pH 9.5-10.0. Moist, ravine. Vegetation closed, evergreen tall grass. Surrounding veg. degraded evergreen forest and scrub.Wild materialPopulation abundance frequent, distribution patchy. Growth habit prostrate. Flower color rose.1480309PI 655734
187PI 655764M235.CPG94Trifolium repens L. MoroccoW6SEED1994COLLECTED07/29/1994Near Setti Fatma, 1 k upstream southwest of Setti Fatma off road S513 to Marrakech.31.22527778, -7.681111111375Grazed, hay. Slope 0-5%, aspect E. Area open. Soil hydromorphic, sandy from granite alluvium, pH 6.5. Rainfall 700 mm. Seasonally inundated, alluvial fan, flood plain. Vegetation closed, evergreen broad-leafed herb veg.Wild materialPopulation abundance occasional, distribution patchy. Growth habit prostrate. Flower white.1480431PI 655764
188PI 613184V. macrocarpon MD Allen 11Vaccinium macrocarpon Aiton Maryland, United StatesCORImage1991COLLECTED10/29/1991Six to Eight acres of Sedge/Shrub minerotophic acidic fen on Snaggy Mountain rd, Garrett county, MD, Murley Run Bog, Potomic-Garrett State Forest39.47833000, -79.46083000813Associated vegatation, Carex Stricta, C. Folliculata, Gaultheria procumbens, Rubus hispicus, Arbutus spp., Calamogrostis canadensid, hypercum densiflorum, Sphagnum sp. Small streams flowing through outWild material(This accession was part of the PL,SD 'breakout' - 1992)1009965PI 613184
189PI 613185V. macrocarpon MD Allen 12Vaccinium macrocarpon Aiton Maryland, United StatesCORImage1991COLLECTED10/29/1991"The Glades" minerotrophic fen, near Grantsville, Garrett county, MD39.55767000, -79.27967000817greater than 100 acres, sedge/grass dominated minerotrophic fen, bordered by scattered white pine and spruce, also with Sphagnum spp., Solidago uliginosa, Glyceria canadensis, Calamogrostis canadensis, Carex Rostrata, C. Folliculata,Wild materialAssociated with Rubus Hispidus, Polytrichum sp., Alnus Rugosa. (This accession was part of the PL,SD 'breakout' - 1992)1009975PI 613185
190PI 613186V. oxycoccos Allen 19Vaccinium oxycoccos L. West Virginia, United StatesCOR1991COLLECTED10/30/1991Bear Rocks Bog, Dolly Sods, Monongahela National Forest, Tucker County, West Virginia39.06667000, -79.30433000115850A area minerotrophic fen, Pyrus spp., the only shrubs, the rest of vegeation is low growing, including Sphagnum sp., Eriophorium virginicium, (abundant) Carex sp., Scleria sp., Juncus sp.Wild materialV. oxycoccos abundant, plants dimunitive. 100 years ago, area was completely covered with spruce, then it was logged, then fire burned the area(This accession was part of the PL,SD 'breakout' - 1992)1010040PI 613186
191PI 618015V. macrocarpon WV Allen 7Vaccinium macrocarpon Aiton West Virginia, United StatesCORImage1991COLLECTED10/29/1991Oligotrophic fen near WV/MD border in Preston county, WV, owned by the nature conservancy, WV, known as Cranesville Swamp39.51950000, -79.482330007862 acres fen, bordered by Typha sp., Acer rubrum, Prunus serotina, Hemlock, Sotuhern most population of American Larch (Tamarack), also has Sphagnum spp., Rubus hispidus, Solidago uliginosa, Eripphorum virginicum, Pyrus melanocarpaWild materialSite holding moisture well in a regional drought, designated as a National Natural Landmark Additional plants are Hypericum densiflorum, Carex folliculata, Juncus effusus, J. canadensis, Bartonia virginica, Gaultheria procumbens1009919PI 618015
192PI 618017V. oxycoccos MD Allen 13Vaccinium oxycoccos L. Maryland, United StatesCORImage1991COLLECTED10/30/1991"The Glades" minerotrophic fen, near Grantsville, Garrett county, MD39.55767000, -79.27967000817greater than 100 acres, sedge/grass dominated minerotrophic fen, bordered by scattered white pine and spruce, also with Sphagnum spp., Solidago uliginosa, Glyceria canadensis, Calamogrostis canadensis, Carex Rostrata, C. Folliculata,Wild materialAssociated with Rubus Hispidus, Polytrichum sp., Alnus Rugosa. (This accession was part of the PL,SD 'breakout' - 1992)1009989PI 618017
193PI 618020V. macrocarpon WV Allen 16Vaccinium macrocarpon Aiton West Virginia, United StatesCORImage1991COLLECTED10/30/1991Minerotrophic fen in large basin between 2 ridges, Tucker Co Big Run Bog (A.K.A. Olson Bog), Monongahela National Forest39.11750000, -79.583330000associated plants Sphagnum sp., Rubus hispidus, Eripphorium virginicum, Carex sp., Juncus sp., Sarracenia purpurea (introduced), Ilex verticillataWild materialSite proposed as a research natural area. (This accession was part of the PL,SD 'breakout' - 1992)1010011PI 618020
194PI 618021V. oxycoccos Allen 17Vaccinium oxycoccos L. West Virginia, United StatesCOR1991COLLECTED10/30/1991Minerotrophic fen in large basin between 2 ridges, Tucker Co Big Run Bog (A.K.A. Olson Bog), Monongahela National Forest39.11750000, -79.583330000associated plants Sphagnum sp., Rubus hispidus, Eripphorium virginicum, Carex sp., Juncus sp., Sarracenia purpurea (introduced), Ilex verticillataWild materialSite proposed as a research natural area. (This accession was part of the PL,SD 'breakout' - 1992)1010027PI 618021
195PI 613182V. macrocarpon Site D Ogle 1Vaccinium macrocarpon Aiton Tennessee, United StatesCOR1991COLLECTED10/19/1991Side of Holston mountains above Shady Valley, Johnson county , Tennessee.36.51667000, -81.966670001120Habitat saturated stream bank at lower edge of secondary seep. Edged by dry deciduous woods. Carex sp., Scirpus cyperinus, Pinus strobus, Lyonia ligustrina, Rosa sp., Dulichium arundinaceum, et al.Wild materialD. W. Ogle collection

1009852PI 613182
196PI 638753V. macrocarpon Site D. Ogle 2Vaccinium macrocarpon Aiton Tennessee, United StatesCOR1991COLLECTED10/19/1991Side of Holston mountains above Shady Valley, Johnson county , Tennessee.36.51667000, -81.966670001120Habitat saturated stream bank at lower edge of secondary seep. Edged by dry deciduous woods. Carex sp., Scirpus cyperinus, Pinus strobus, Lyonia ligustrina, Rosa sp., Dulichium arundinaceum, et al.Wild materialD. W. Ogle collection

1009838PI 638753
197PI 618013V. macrocarpon Site IIVaccinium macrocarpon Aiton Virginia, United StatesCOR1991COLLECTED10/17/1991Nature area owend by the Nature Conservancy, near intersecti on of routes 785 and 613 across route 613 from stone quarry, 1/4 mile up dirt road, Big Spring Glade area36.66667000, -80.93333000786Soil Wehadkee silt loam, flora more varied than a typical bog, Sphagnum subsecundum Nees ex Strum, Pinus sp., Quercus sp., Acer sp., Lyondia sp., Sorbus., Ilex sp., Viola sp., Delphinium sp., Xanthorhiza, Phalaris, Carex, AletrisWild material'Poor fen' as descirbed by Ogle in paper and by Sjors (1959) cited by Ogle (p 144) Cranberry crop at this site very poor in 1991, leaves smaller that usual. 'something had been in and tramping but probably not human.' (This accession was part of the PL,SD 'breakout' - 1992)1009869PI 618013
198PI 560086MPW-WWR 215Cuphea viscosissima Jacq. Tennessee, United StatesNC71989COLLECTED09/12/1989Gravel rd edge, plts cut over, on N side or road with Eupatorium coelestinum, Carex sp, Euphorbia maculata, and Cercis. 0.1 mi NW TN 149 on Hematite Rd, Palmyra quad. Palmyra city, in Montgomery Cty.36.45000000, -87.45000000115Wild materialPopulation of over 100 plants.1455058PI 560086
199Ames 38800Camp MitigwaAmelanchier arborea (F. Michx.) Fernald Iowa, United StatesNC7FRUIT2026COLLECTED06/01/2026Mitigwa Scout Camp located on west side of Des Moines River watershed approximately 7.50 miles south, southwest of Boone, T82N R26W N 1/4 Sec. 5 and T83N R26W S 1/4 Sec. 32.41.94894500, -93.90537200310High-quality white oak - ironwood, mature woods.Wild materialThe native range of Amelanchier arborea is concentrated in the eastern half of the U.S. (Little, 1977). This accession represents a collection of A. arborea germplasm from the western edge of the species native range, specifically central Iowa. Specimens sampled at the collection site in nature were small to medium understory or woodland edge single and/or multi-trunked trees with a few trees getting close to being deemed as canopy specimens. Bark smooth and light grey in color. Specimens sampled in nature ranging 15-50' in height. Peak flowering occurred on 8 April 2026 with white flowers appearing prior to leaf expansion. Fall colors ranging from orange to orange-red peaking typically at the end of September (central Iowa). Fruits, dark-pink to red, maturing in early June (peak in 2026 occurred on 2 June) averaging 8 mm in diameter, except for mother tree #6 that had rather large fruits at 11 mm in diameter. 2197049Ames 38800
200NA 891732025RJLSEUS-14Chionanthus sp.Florida, United StatesNA2026COLLECTED10/03/2025Choctawhatchee 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, -86.6596500010Dry 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 materialReceived as C. cf. henryae2193307NA 89173
201NA 891712025RJLSEUS-04Rhododendron catawbiense Michx. Alabama, United StatesNA2026COLLECTED09/30/2025Scarham Creek: southeast of the Pea Ridge Road bridge, approximately 50-80 meters on the south side of the creek.34.32559600, -86.16054600266Growing near the base of the slopes above the riparian zone, generally on the exposed geology under very well-drained conditions. The woodlands are primarily deciduous with a few evergreens infrequently mixed. Slope: 15 to 30 percent. Aspect: Northeast. Soil: The primary soil type in the area of this collection is classified as Rockland Series sandstone (Rc). The Rockland series consists of well drained soils formed in loamy colluvium from rotational landslides on slopes of stream valleys and dissections of ground moraines. Saturated hydraulic conductivity is moderate in the upper part of the profile and moderately slow in the lower part. Slopes range from 18 to 70 percent. Some pedons have buried leaves, twigs, and moss. Mass soil movement has left random remnants of soil structure from prior upslope soil development and has buried tree branches, leaves and moss. The upper 0-2 cm of soil contains slightly decomposed organic matter while lower soils layers to a depth of 58 cm are comprised of dark reddish-brown to brown silt loam and are moderately acidic. Below 58 cm the soils are generally dark reddish-brown silt loam and strongly to moderately alkaline. (Source:California Soil Resource Lab/NRCS Official Soil Series Descriptions). Geology: The underlying geology of this area is of Pennsylvanian origin and characterized as Pottsville Formation. It is characterized by light-gray thin to thick-bedded quartzose sandstone and conglomerate containing interbedded dark-gray shale, siltstone, and coal. Mapped on Lookout Mountain, Blount and Chandler Mountains, and Sand Mountain northeast of Blount County, and on the mountains of Jackson, Marshall, and Madison Counties north and west of the TN river. (Source: USGS Alabama Geologic Map Data).Wild materialReceived as R. catawbiense vsr. insularis2193305NA 89171
202NA 891552025RJLSEUS-02Ilex longipes Chapm. ex Trel. Alabama, United StatesNA2025COLLECTED09/30/2025Scarham Creek: southeast of the Pea Ridge Road bridge, approximately 50-80 meters on the south side of the creek.34.32520700, -86.15967000261Plants are growing on relatively steep woodland slopes in shade. The woodlands are primarily deciduous with a few evergreens infrequently mixed. Slope: 15 to 30 percent. Aspect: Northeast. Soil: The primary soil type in the area of this collection is classified as Rockland Series sandstone (Rc). The Rockland series consists of well drained soils formed in loamy colluvium from rotational landslides on slopes of stream valleys and dissections of ground moraines. Saturated hydraulic conductivity is moderate in the upper part of the profile and moderately slow in the lower part. Slopes range from 18 to 70 percent. Some pedons have buried leaves, twigs, and moss. Mass soil movement has left random remnants of soil structure from prior upslope soil development and has buried tree branches, leaves and moss. The upper 0-2 cm of soil contains slightly decomposed organic matter while lower soils layers to a depth of 58 cm are comprised of dark reddish-brown to brown silt loam and are moderately acidic. Below 58 cm the soils are generally dark reddish-brown silt loam and strongly to moderately alkaline. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). Geology: The underlying geology of this area is of Pennsylvanian origin and characterized as Pottsville Formation. It is characterized by light-gray thin to thick-bedded quartzose sandstone and conglomerate containing interbedded dark-gray shale, siltstone, and coal. Mapped on Lookout Mountain, Blount and Chandler Mountains, and Sand Mountain northeast of Blount County, and on the mountains of Jackson, Marshall, and Madison Counties north and west of the TN river. (Source: USGS Alabama Geologic Map Data).Wild material2193001NA 89155
203NA 891562025RJLSEUS-03Euonymus americanus L. Alabama, United StatesNA2025COLLECTED09/30/2025Scarham Creek: southeast of the Pea Ridge Road bridge, approximately 50-80 meters on the south side of the creek.34.32577600, -86.16071000260Plants are growing on relatively steep woodland slopes in shade. The woodlands are primarily deciduous with a few evergreens infrequently mixed. Slope: 15 to 30 percent. Aspect: Northeast. Soil: The primary soil type in the area of this collection is classified as Rockland Series sandstone (Rc). The Rockland series consists of well drained soils formed in loamy colluvium from rotational landslides on slopes of stream valleys and dissections of ground moraines. Saturated hydraulic conductivity is moderate in the upper part of the profile and moderately slow in the lower part. Slopes range from 18 to 70 percent. Some pedons have buried leaves, twigs, and moss. Mass soil movement has left random remnants of soil structure from prior upslope soil development and has buried tree branches, leaves and moss. The upper 0-2 cm of soil contains slightly decomposed organic matter while lower soils layers to a depth of 58 cm are comprised of dark reddish-brown to brown silt loam and are moderately acidic. Below 58 cm the soils are generally dark reddish-brown silt loam and strongly to moderately alkaline. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). Geology: The underlying geology of this area is of Pennsylvanian origin and characterized as Pottsville Formation. It is characterized by light-gray thin to thick-bedded quartzose sandstone and conglomerate containing interbedded dark-gray shale, siltstone, and coal. Mapped on Lookout Mountain, Blount and Chandler Mountains, and Sand Mountain northeast of Blount County, and on the mountains of Jackson, Marshall, and Madison Counties north and west of the TN river. (Source: USGS Alabama Geologic Map Data).Wild material2193002NA 89156
204W6 62522FWS0300-112Eupatorium perfoliatum L. Michigan, United StatesW6SEED2025Wild material2192220W6 62522
205W6 62535FWS0300-145Verbena hastata L. Michigan, United StatesW6SEED2025Wild material2192233W6 62535
206W6 62539FWS0300-154Liatris cylindracea Michx. 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.2192237W6 62539
207W6 62544FWS0300-78Schoenoplectus tabernaemontani (C. C. Gmel.) Palla Michigan, United StatesW6SEED2025Wild materialPlants have variable phenology with mature achenes and fresh flowers often on a single individual2192242W6 62544
208NA 89194DLSP-WBHamamelis virginiana L. Wisconsin, United StatesNA2025COLLECTED08/21/2024Devil's Lake State Park: West Bluff.43.41418510, -89.73993600332Shade to part shade/sun to full sun in thin layer of clayey organic matter on boulder field. Slope: 60 degrees. Aspect: East. Red oak-sugar maple-linden vegetative community.Wild material2171015NA 89194
209NA 89196KVRHamamelis virginiana L. Wisconsin, United StatesNA2025COLLECTED08/22/2024Kickapoo Valley Reserve.43.62650770, -90.64627490299Shade in thick, clayey, organic soil with sand. Slope: 45 degrees. Aspect: Northeast. Silver maple-boxelder-elm vegetative community.Wild material2171017NA 89196
210NA 885792024RJLFL-007Ilex myrtifolia Walter Florida, United StatesNA2024COLLECTED11/13/2024Wetlands accessed from Miller Bluff Road.30.62251200, -86.860307008Open, wet areas and woodland edge slightly above permanently wet habitat in part shade to full sun. Slope: 0 percent. Aspect: N/A.Wild material2169916NA 88579
211NA 885802024RJLFL-009Ilex myrtifolia Walter Florida, United StatesNA2024COLLECTED11/13/2024Woodlands on the north side of Fisher Old Mill Road about 0.10 kilometers west of intersection with DOF Y12.30.62693800, -86.839622006Mixed evergreen and deciduous moist to wet forest in part shade to full sun. From the associated taxa, this site can be quite wet during the growing season; however, it was dry during this collection time; likely due to extended drought. Slope: 0 percent. Aspect: South.Wild material2169917NA 88580
212NA 885832024RJLFL-014Ilex amelanchier M. A. Curtis ex Chapm. Florida, United StatesNA2024COLLECTED11/13/2024Yellow River Water Management Area: found in an area where an unnamed unpaved road dead ends near the Yellow River. This unpaved road is accessed from Old River Road to the east near the junction with Shockley Springs Road. Individual plants for this collection were accessed by foot along the edge of the river and associated wetland depressions to the east of the road. The sampling for this portion of the population extends from the GPS coordinates listed above to the northeast where sampling ended at coordinates 30.871238 deg. N, 86.590170 deg. W.30.86989400, -86.5921850023Plants growing in seasonally inundated swamp habitats associated with the Yellow River and small tributaries. Plants are emergent during portions of the year, primarily during the growing season. During this time of collection, water had receded from the wetlands and the area was relatively dry. Slope: N/A. Aspect: N./A. The underlying geology of this area is the Alum Bluff Group of Miocene origin. It includes the Chipola Formation, Oak Grove Sand, Shoal River Formation, Choctawhatchee Formation and the Jackson Bluff Formation. The formations included in this group are generally defined based on their molluscan faunas and stratigraphic position. Puri (1953) described sediment facies as they relate to the formations of the Alum Bluff Group. These sediments are lithologically distinct as a group, not as individual units. The Alum Bluff Group crops out or is beneath a thin overburden in the western panhandle from river valleys in Okaloosa County eastward to western Jackson County. The Alum Bluff Group consists of clays, sands and shell beds which may vary from fossiliferous, sandy clays to unfossiliferous sands and clays and occasional carbonate beds. Mica is a common constituent and glauconite and phosphate occur sporadically. Induration varies from essentially nonindurated in sands to well indurated in carbonate lenses. Colors range from cream to olive gray with mottled reddish brown in weathered sections. Sand grain size varies from very fine to very coarse with sporadic occurrences of gravel. These sediments generally have low permeabilities and are part of the intermediate confining unit/aquifer system. (Source: USGS Florida Geologic Map Data). The surface soil profile of this area is primarily Kinston, Johnston, and Bibb soils, frequently flooded. Kinston Series soils are poorly drained, alluvial, fine-loamy, siliceous, and acid soils of flood plains. They are peaty to loamy friable, slightly sticky, and slightly plastic in the upper 0 to 7.5 cm of the strata with less sand and more silt-loam in progressively deeper strata. The Johnston Series consists of very deep, very poorly drained coarse-loamy, siliceous, active, acid, thermic Cumulic Humaquepts. The upper 0-75 cm is black, mucky loam that is friable and very strongly acid. The lower strata to 1.75 m are dark gray, loamy fine sand, single grained, loose and very strongly acid. (Source: NRCS Web Soil Survey).Wild material2169920NA 88583
213NA 885852024RJLFL-018Rhododendron canescens (Michx.) Sweet Florida, United StatesNA2024COLLECTED11/14/2024Woodlands in the riparian zone of a headwater spring and wetland leading to Panther Creek. The area is accessed from High Bridge Road by turning south on an unnamed dirt/sand road and driving about 0.27 kilometers to a pond. 30.90865300, -86.6910720049Mostly deciduous woodlands in the riparian zone of a headwater spring and wetland in shade to part shade. Slope: 5 to 8 percent. Aspect: N/A. The underlying geology of this area is characterized as Citronelle Formation of the Pliocene period. The Citronelle Formation is widespread in the Gulf Coastal Plain. The type section for the Citronelle Formation, named by Matson (1916), is near Citronelle, Alabama. The Citronelle Formation grades laterally, through a broad facies transition, into the Miccosukee Formation of the eastern Florida panhandle. Coe (1979) investigated the Citronelle Formation in portions of the western Florida panhandle. The Citronelle Formation is a siliciclastic, deltaic deposit that is lithologically similar to, and time equivalent with, the Cypresshead Formation and, at least in part, the Long Key Formation (Cunningham et al., 1998) of the peninsula. In the western panhandle, some of the sediments mapped as Citronelle Formation may be reworked Citronelle. The lithologies are the same and there are few fossils present to document a possible younger age. The Citronelle Formation consists of gray to orange, often mottled, unconsolidated to poorly consolidated, very fine to very coarse, poorly sorted, clean to clayey sands. It contains significant amounts of clay, silt and gravel which may occur as beds and lenses and may vary considerably over short distances. Limonite nodules and limonite-cemented beds are common. Marine fossils are rare but fossil pollen, plant remains and occasional vertebrates are found. Much of the Citronelle Formation is highly permeable. It forms the Sand and Gravel Aquifer of the surficial aquifer system contain organics. The dominant fossils in the freshwater carbonates are mollusks. (Source: USGS Florida Geologic Map Data). The surface soil profile is classified as Troup-Orangeburg-Cowarts complex, 5 to 12 percent slopes. The Troup series consists of very deep, somewhat excessively drained soils formed in unconsolidated sandy and loamy marine sediments. Troup soils are found on ridges and hillslopes. The Orangeburg series consists of very deep, well drained, moderately permeable soils on uplands of the Southern Coastal Plain. They formed in loamy and clayey marine sediments. 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. The reaction of all these soils ranges from very strongly acid to strongly acid. (Source: USDA-NRCS Official Soil Series Descriptions).Wild material2169922NA 88585
214NA 890752024RJLPA-001Rhododendron maximum L. Pennsylvania, United StatesNA2024COLLECTED09/18/2024Fieldstone Farm Tank Creek Nature Preserve (a property of the Pocono Heritage Land Trust): Collected along Tank Creek. The property is accessed from a parking area located on Devil's Hole Road.41.13862300, -75.34562700493Mostly found in mixed deciduous forest with occasional conifers and evergreen shrubs generally on steep slopes above Tank Creek in rocky well-drained soils in shade to part-shade. The slopes are abundant in decomposed organic matter and runoff soils. Slope: 5 to 30 percent. Aspect: various. Geology: The underlying geology of this area is of Devonian origin and characterized as the Long Run Member of Catskill Formation. It is comprised of gray and grayish-red sandstone and grayish-red siltstone and mudstone in fining-upward cycles. (Source: USGS Pennsylvania Geologic Map Data). Soils: The primary soil type found here is classified as Alluvial Land. In geology, alluvial land refers to areas of land that are formed by the deposition of sediments carried by rivers, or other surface water. EPA Ecoregion (Level III): North Central Appalachians (62). EPA Ecoregion (Level IV): Low Poconos (62b).Wild material2169039NA 89075
215NA 890762024RJLPA-002Kalmia latifolia L. Pennsylvania, United StatesNA2024COLLECTED09/18/2024Fieldstone Farm Tank Creek Nature Preserve (a property of the Pocono Heritage Land Trust): Collected along Tank Creek. The property is accessed from a parking area located on Devil's Hole Road.41.13862300, -75.34562700493Mostly found in mixed deciduous forest with occasional conifers and evergreen shrubs generally on sloping sites as an understory shrub in rocky well-drained soils in shade to part-shade. Slope: 5 to 15 percent. Aspect: various. Geology: The underlying geology of this area is of Devonian origin and characterized as the Long Run Member of Catskill Formation. It is comprised of gray and grayish-red sandstone and grayish-red siltstone and mudstone in fining-upward cycles. (Source: USGS Pennsylvania Geologic Map Data). Soils: The primary soil type found here is classified as Alluvial Land. In geology, alluvial land refers to areas of land that are formed by the deposition of sediments carried by rivers, or other surface water. EPA Ecoregion (Level III): North Central Appalachians (62). EPA Ecoregion (Level IV): Low Poconos (62b).Wild material2169040NA 89076
216NA 890772024RJLPA-003Viburnum acerifolium L. Pennsylvania, United StatesNA2024COLLECTED09/19/2024Birdell Road, near parking lot to trail where the road ends at Chambers Lake, which is part of Hibernia County Park.40.03559500, -75.85708600187Plants are growing in deep shade of a dry deciduous forest dominated by Fagus grandifolia. Slope: 0 percent. Aspect: N/A. Geology: The underlying geology of this area is of Precambrian origin and characterized as Banded Mafic Gneiss. It is characterized as dark and fine to medium grained. This formation includes rocks of probable sedimentary origin; may be equivalent to "PZmgh." (Source: USGS Pennsylvania Geologic Map Data). Soils: The primary soil type in the area of this collection is classified as Neshaminy Series Silt Loam, very deep over mafic gneiss, 3 to 8 percent slopes (NvB). (Source: USDA-NRCS Official Soil Series Descriptions). EPA Ecoregion (Level III): Northern Piedmont (64). EPA Ecoregion (Level IV): Piedmont Uplands (64c).Wild material2169041NA 89077
217NA 890782024RJLPA-004Staphylea trifolia L. Pennsylvania, United StatesNA2024COLLECTED09/20/2024Along gated road about 0.33 kilometers southwest of the Lake Ontelaunee Trail parking lot.40.49850800, -75.8912130094Plants 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 material2169042NA 89078
218NA 890802024RJLPA-006Ilex montana Torr. & A. Gray Pennsylvania, United StatesNA2024COLLECTED09/20/2024Berks and Schuylkill Counties: Hawk Mountain Sanctuary.40.64162200, -75.99122600418Plants are growing from shade to full sun on a dry-mesic to very dry, well-drained upland/montane habitat characterized by an upland mixed deciduous and evergreen forest that is very rocky. All the plants found in this habitat go through periods of drought during the growing season due to the limited litter/soil layer in which moisture can be held. Elevation: 405 to 430 meters. Slope: 5 to 25 percent. Aspect: various. Geology: The underlying geology of this area is of Silurian origin and comprised of Shawangunk Formation. This formation is primarily light- to dark-gray, fine- to very coarse-grained sandstone and conglomerate containing thin shale interbeds. (Source: USGS Pennsylvania Geologic Map Data). Soils: The surface soil profile of this area is characterized as the Hazleton Series which consists of deep and very deep, well drained soils formed in residuum of acid gray, brown or red sandstone on uplands. The matrix includes a considerable accumulation of thin, flat, coarse fragments of sandstone, limestone, or schist with diameters up to 15 cm. Slope ranges from 0-80%. Permeability is moderately rapid to rapid. (Source: USDA-NRCS Official Soil Series Descriptions). EPA Ecoregion (Level III): Ridge and Valley (67). EPA Ecoregion (Level IV): Northern Sandstone Ridges (67c).Wild material2169044NA 89080
219NA 890882024RM-TK-001Viburnum acerifolium L. Alabama, United StatesNA2024COLLECTED09/19/2024Haines Island Park. Follow Ferry Road to the top of the hill entering the park where a picnic shelter is located. Plants are growing along trails to the north of the picnic shelter.31.72132026, -87.4640891081Plants are growing from part-sun to full shade in the understory of a mixed deciduous and coniferous forest on very dry upland habitat. Slope: 10 to 20 percent. Aspect: North. Geology: The underlying geology of this area is probably of Eocene age and characterized as the Claiborne Group: Tallahatta Formation. It is comprised of white to very light-greenish-gray thin-bedded to massive siliceous claystone; interbedded with thin layers of fossiliferous clay, sandy clay, and glauconitic sand and sandstone. White to light-greenish-gray fine to coarse sand and fine gravel occur at the base of the formation in southwest Alabama (Meridian Sand Member). (Source: USGS Alabama Geologic Map Data). Soils: The area of this occurrence is characterized as Arundel Series Loam, 8 to 35 percent slopes (ArF). The Arundel series consists of moderately deep, well drained, very slowly permeable soils on dissected uplands of the Southern Coastal Plain Major Land Resource Area (MLRA 133A). They formed in marine deposits consisting of acid clays underlain by horizontally bedded sandstone, buhrstone and siltstone. Slopes range from 2 to 60 percent. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). EPA Ecoregion (Level III): Southeastern Plains (65). EPA Ecoregion (Level IV): Buhrstone/Lime Hills (65q).Wild material2169052NA 89088
220NA 890892024RM-TK-002Viburnum acerifolium L. Alabama, United StatesNA2024COLLECTED09/19/2024Woodland slopes around and below the hilltop parking area leading down to the Silver Creek Lake Campground off of Silver Creek Lake Road.31.66612294, -87.5756986049Plants are growing in shade of upland dry mesic, mature mixed deciduous and evergreen woodland. Generally, the overstory is thinner and there is less leaf litter cover, making the surface soil conditions drier. Slope: 5 to 10 percent. Aspect: Southeast. Geology: The underlying geology of this area is Claiborne Group, Tallahatta Formation, of Eocene origin, with white to very light-greenish-gray thin-bedded to massive siliceous claystone; interbedded with thin layers of fossiliferous clay, sandy clay, and glauconitic sand and sandstone. (Source: USGS Alabama Geologic Map Data). Soils: The primary soil types in the collection area are classified as Arundel-Cantuche Complex soils (15 to 35 percent slopes). The Arundel Series consists of moderately deep, well drained, very slowly permeable soils on dissected uplands of the Southern Coastal Plain. They formed in marine deposits consisting of acid clays underlain by horizontally bedded sandstone, buhrstone and siltstone. These soils are strongly acid. Slopes range from 2 to 60 percent. The Cantuche Series consists of shallow, well drained, moderately permeable soils that formed over horizontally bedded claystone. These soils are on narrow ridgetops and narrow benches on steep side-slopes of dissected landscapes in the Coastal Plain. They are strongly acid. Slopes range from 2 to 35 percent. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). EPA Ecoregion (Level III): Southeastern Plains (65). EPA Ecoregion (Level IV): Buhrstone/Lime Hills (65q).Wild material2169053NA 89089
221NA 890902024RM-TK-003Ilex longipes Chapm. ex Trel. Alabama, United StatesNA2024COLLECTED09/19/2024Woodland slopes around and below the hilltop parking area leading down to the Silver Creek Lake Campground off of Silver Creek Lake Road.31.66612294, -87.5756986039Plants are growing in part-shade to shade of a moist mesic deciduous and evergreen woodland on dry, well-drained soil to an area 1-2 meters above a small seasonally spring-fed creek at 31.664428°, -87.574614°. Slope: 5 to 10 percent. Aspect: Southeast. Geology: The underlying geology of this area is Claiborne Group, Tallahatta Formation, of Eocene origin, with white to very light-greenish-gray thin-bedded to massive siliceous claystone; interbedded with thin layers of fossiliferous clay, sandy clay, and glauconitic sand and sandstone. (Source: USGS Alabama Geologic Map Data). Soils: The primary soil types in the collection area are classified as Arundel-Cantuche Complex soils (15 to 35 percent slopes). The Arundel Series consists of moderately deep, well drained, very slowly permeable soils on dissected uplands of the Southern Coastal Plain. They formed in marine deposits consisting of acid clays underlain by horizontally bedded sandstone, buhrstone and siltstone. These soils are strongly acid. Slopes range from 2 to 60 percent. The Cantuche Series consists of shallow, well drained, moderately permeable soils that formed over horizontally bedded claystone. These soils are on narrow ridgetops and narrow benches on steep side-slopes of dissected landscapes in the Coastal Plain. They are strongly acid. Slopes range from 2 to 35 percent. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). EPA Ecoregion (Level III): Southeastern Plains (65). EPA Ecoregion (Level IV): Buhrstone/Lime Hills (65q).Wild material2169054NA 89090
222NA 890922024RM-TK-005Ilex amelanchier M. A. Curtis ex Chapm. Florida, United StatesNA2024COLLECTED09/29/2024Yellow River Water Management Area: found in an area where an unnamed, unpaved road dead ends near the Yellow River. This unpaved road is accessed from Old River Road to the east near the junction with Shockley Springs Road. Plants are accessed by foot along the edge of the river and associated wetland depressions to the west of the road.30.86946200, -86.5934900023Plants growing in seasonally inundated swamp habitats associated with the Yellow River. Plants are emergent during portions of the year, primarily during the growing season. During this time of collection, water had receded from the wetlands but the area was still quite wet with many tiny stream rivulets still draining. Slope: 0 percent. Aspect: N/A. Geology: The underlying geology of this area is the Alum Bluff Group of Miocene origin. It includes the Chipola Formation, Oak Grove Sand, Shoal River Formation, Choctawhatchee Formation and the Jackson Bluff Formation. The formations included in this group are generally defined based on their molluscan faunas and stratigraphic position. Puri (1953) described sediment facies as they relate to the formations of the Alum Bluff Group. These sediments are lithologically distinct as a group, not as individual units. The Alum Bluff Group crops out or is beneath a thin overburden in the western panhandle from river valleys in Okaloosa County eastward to western Jackson County. The Alum Bluff Group consists of clays, sands and shell beds which may vary from fossiliferous, sandy clays to unfossiliferous sands and clays and occasional carbonate beds. Mica is a common constituent and glauconite and phosphate occur sporadically. Induration varies from essentially nonindurated in sands to well indurated in carbonate lenses. Colors range from cream to olive gray with mottled reddish brown in weathered sections. Sand grain size varies from very fine to very coarse with sporadic occurrences of gravel. These sediments generally have low permeabilities and are part of the intermediate confining unit/aquifer system. (Source: USGS Florida Geologic Map Data). Soils: The surface soil profile of this area is primarily Kinston, Johnston, and Bibb soils, frequently flooded. Kinston Series soils are poorly drained, alluvial, fine-loamy, siliceous, and acid soils of flood plains. They are peaty to loamy friable, slightly sticky and slightly plastic in the upper 0 to 7.5 cm of the strata with less sand and more silt-loam in progressively deeper strata. The Johnston Series consists of very deep, very poorly drained coarse-loamy, siliceous, active, acid, thermic Cumulic Humaquepts. The upper 0-75 cm is black, mucky loam that is friable and very strongly acid. The lower strata to 1.75 m are dark gray, loamy fine sand, single grained, loose and very strongly a).id. The Bibb Series soils consist of very deep, poorly drained, moderately permeable soils on flood plains of streams in the Southern Coastal Plain (133A) Major Land Resource Area. They formed in stratified loamy and sandy alluvium that are commonly and frequently flooded and water runs off the surface very slowly. Slopes range from 0 to 2 percent. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). EPA Ecoregion (Level III): Southeastern Plains (65). EPA Ecoregion (Level IV): Southeastern Floodplains and Low Terraces (65p).Wild material2169056NA 89092
223Ames 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
224Ames 36250Liverpool Nature PreserveSalix myricoides Muhl. Indiana, United StatesNC7LEAF2024COLLECTED06/03/2024Liverpool Nature Preserve located just east of Liverpool, T36N R8W W 1/2 NW 1/4 SE 1/4 Sec. 24.41.55597400, -87.28701600189Savanna and prairie remnant with high water-table on sandy soils.Wild materialBayberry willow is native to areas of the northeastern U.S. and north into Canada, localized around the Great Lakes region. Known to occur on shorelines/dunes but also in swamps, fens, and on talus (Haines 2004) with the potential to reach six meters in height (Dorn 1995). Ornamental characteristics include glaucous lower leaf blades that appear chalky white. Staminate flowering occurs before or during leaf expansion with purple-turning-yellow anthers (Haines 2004). This accession represents a large amount of phenotypic variability observed at the time of collection. This included variation in leaf size, shape, margins and presence of stipules. All plants sampled have very glaucus undersides of the leaves. Winter stem colors vary widely from yellowish-orange; greenish-grey; mahogany; and reddish-brown. 2167952Ames 36250
225W6 61536CA190B-210Erythranthe guttata (DC.) G. L. Nesom California, United StatesW6SEED20242167635W6 61536
226WLP 3432RM2023-001Rhododendron minus Michx. Georgia, United StatesNA2024COLLECTED10/21/2023Plants growing along Patterson Gap Road.34.96995500, -83.477228001005Plants growing in part shade to sun in an upland, very dry and rocky, mostly deciduous habitat. The site is steeply sloped, underlain by rock, with rocky outcrops. Slope: 15 to 65 percent. Aspect: Variable. The underlying geology of this area is Quartzite/Mica Schist, primarily of Precambrian-Paleozoic origin. (Source: USGS North Carolina Geologic Map Data.) The primary soil type in the collection area is classified as Ashe Series that is stony and very steep. The Ashe series consists of moderately deep, somewhat excessively drained soils on gently sloping to very steep ridges and side slopes of the Blue Ridge. They formed in residuum that is affected by soil creep in the upper part, and weathered from felsic or mafic igneous and high-grade metamorphic rocks such as granite, hornblende gneiss, granodiorite, biotite gneiss, and high-grade metagraywacke. Slope ranges from 2 to 95 percent. The surface layer to 5cm deep is comprised of moderately decomposed organic matter and leaves, twigs, and roots. Layers to 70cm deep range from very dark grayish brown to brown sandy loam with weak medium and coarse granular structure that is friable. A few fine flakes of mica can be found and these soils are very strongly acid. (Source: NRCS Web Soil Survey.)Wild material2166141WLP 3432
227Ames 36219Egyptian TractSalix sericea Marshall Missouri, United StatesNC7LEAF2024COLLECTED01/19/2024LAD Foundation Egyptian Tract Wet Hollow Seep/Fen Complex located 7.52 miles west, southwest of Annapolis just northwest of intersection of CR 338 and CR 334, T31N R2E SW 1/4 SE 1/4 SE 1/4 Sec. 21 (Lesterville SE Quad.).37.34429700, -90.83361600217Perched wet fen/seep complex with standing water supporting both obligate calciphilic and obligate acidophilic plant species.Wild materialThe native range of Salix sericea is concentrated througout the northeastern and eastern central United States ranging from Maine south to South Carolina, west to Illinois with a relatively large disjunct area in southeastern Missouri (Little, E. L. Jr. 1977). This accession represents genetics from southeastern Missouri in Reynolds County. Shrubs noted at the collection site in nature ranging in height from 2-7 feet and typically twice as wide as tall. Multi-stemmed shrubs expanding vegetatively via layering. Dormant stem colors noted at collection site ranging from mostly greenish to occassionally brownish red and/or copper tones. Dormant buds rather red and often bright red in color. Salix sericea is native to areas of the northeastern U.S. and north into Canada, reaching its western extent in Missouri. Classified as an obligate wetland plant that typically occurs on wet seeps, sedge meadows, streambanks, fens, etc. that are usually slightly acidic. Known to have the potential to reach up to four meters in height, but always much wider than tall. Ornamental characteristics include dark green leaves that are hairless above with undersides that are densely minutely-hairy making them rather white in appearance. Flowering occurs before or during leaf expansion. This species is known to serve as a larval host plant for the Arcadian Hairstreak, Satyrium acadica. 2165775Ames 36219
228NA 88839RJL-RM2023FLAL-013Rhododendron austrinum (Small) Rehder Florida, United StatesNA2023COLLECTED12/10/2023Along the Florida Trail, accessed from Miller Bluff Road. Plants were found infrequently but regularly along the trail over 1 kilometer or more.30.61991500, -86.865210004Plants are growing primarily in shade to dappled shade, above a small stream in moist mesic conditions along and below the Florida Trail. The mixed evergreen and deciduous forest is quite diverse with an excellent litter layer. Slope: 2 to 8 percent. Aspect: South. The underlying geology of this area is classified as Alluvium, of Pleistocene/Holocene origin and consists of undifferentiated Quaternary sediments of varying thickness including siliciclastics, organics and freshwater carbonates. The siliciclastics are light gray, tan, brown to black, unconsolidated to poorly consolidated, clean to clayey, silty, unfossiliferous, variably organic-bearing sands to blue green to olive green, poorly to moderately consolidated, sandy, silty clays. Organics occur as plant debris, roots, disseminated organic matrix and beds of peat. Freshwater carbonates, often referred to as marls in the literature, are scattered. (Source: USGS Florida Geologic Map Data.) The surface soil profile of this area is primarily Bibb-Kinston Series Association. Bibb Series soils are coarse-loamy, sandy, acid soils that are poorly drained. They are soils of flood plains and streams subject to frequent flooding. These are found in association with Kinston Series soils that are fine-loamy, sandy, acid soils of flood plains and stream subject to frequent flooding. The Bibb-Kinston association ranges from 1-1.5 meters thick and is strongly acid. (Source: NRCS Web Soil Survey.)Wild material2165669NA 88839
229NA 88841RJL-RM2023FLAL-015Pinckneya bracteata (W. Bartram) Raf. Florida, United StatesNA2023COLLECTED12/11/2023West side of Marville Drive on the edge of the woodlands just a few hundred feet south of Fairway Drive.30.60665300, -85.3257220079Plants are growing on the edge of a wetland acid habitat in the transitional zone between the obligate and facultative zones. They are growing in part-shade to shade with lower woody competition due to the moist conditions. Slope: N/A. Aspect: N/A. 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 material2165671NA 88841
230NA 88844RJL-RM2023FLAL-018Clethra alnifolia L. Florida, United StatesNA2023COLLECTED12/13/2023Yellow River Water Management Area, accessed off of Old River Road by vehicle on an unmaintained sand road for approximately 1.68 kilometers. Upon reaching the destination, plants are accessed by foot along unmaintained trail to the east.30.83495500, -86.6200540027Plants are growing primarily in part shade as understory shrubs in mixed evergreen and deciduous, moist to wet, acidic woodlands. Plants form large colonies and appear to have been subjected to prescribed fire in recent years. 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 soil profile for this area is classified as the Bonifay Soil Series. Bonifay soil consists of very deep, well drained, moderately slowly permeable soils on ridges and side slopes in the Southern Coastal Plain. They formed in thick beds of sandy and loamy marine sediments. Solum thickness ranges from 1.5-2.0 m. Soil reaction ranges from very strongly acid to moderately acid throughout, except where the surface has been limed. Ironstone pebbles, 2 to 15 mm in size, range from 0 to 5 percent, by volume. Depth to the plinthic horizon ranges from 1.1-1.7 m. Some horizons contain up to 25 percent plinthite by volume. (Source: NRCS Web Soil Survey.)Wild material2165674NA 88844
231NA 88845RJL-RM2023FLAL-019Ilex opaca Aiton Florida, United StatesNA2023COLLECTED12/13/2023Yellow River Water Management Area, found along an unnamed unpaved road leading down to the Yellow River. This unpaved road is accessed from Old River Road to the east near the junction with Shockley Springs Road.30.87382600, -86.6022130035Plants are growing along the road on the woodland edge on a small bluff above a creek in well-drained to dry habitat in part shade. They are also found sporadically in areas along the Yellow River where occasional inundation occurs. Slope: N/A. Aspect: N/A. The underlying geology of this area is the Alum Bluff Group of Miocene origin. It includes the Chipola Formation, Oak Grove Sand, Shoal River Formation, Choctawhatchee Formation and the Jackson Bluff Formation. The formations included in this group are generally defined on the basis of their molluscan faunas and stratigraphic position. Puri (1953) described sediment facies as they relate to the formations of the Alum Bluff Group. These sediments are lithologically distinct as a group, not as individual units. The Alum Bluff Group crops out or is beneath a thin overburden in the western panhandle from river valleys in Okaloosa County eastward to western Jackson County. The Alum Bluff Group consists of clays, sands and shell beds which may vary from fossiliferous, sandy clays to unfossiliferous sands and clays and occasional carbonate beds. Mica is a common constituent and glauconite and phosphate occur sporadically. Induration varies from essentially nonindurated in sands to well indurated in carbonate lenses. Colors range from cream to olive gray with mottled reddish brown in weathered sections. Sand grain size varies from very fine to very coarse with sporadic occurrences of gravel. These sediments generally have low permeabilities and are part of the intermediate confining unit/aquifer system. (Source: USGS Florida Geologic Map Data.) The surface soil profile of this area is primarily Bonifay-Dothan-Angie complex (5 to 12 percent slopes). Bonifay soil consists of very deep, well drained, moderately slowly permeable soils on ridges and side slopes in the Southern Coastal Plain. They formed in thick beds of sandy and loamy marine sediments. Solum thickness ranges from 1.5-2.0 m. Soil reaction ranges from very strongly acid to moderately acid throughout, except where the surface has been limed. Ironstone pebbles, 2 to 15 mm in size, range from 0 to 5 percent, by volume. Depth to the plinthic horizon ranges from 1.1-1.7 m. Some horizons contain up to 25 percent plinthite by volume. The Dothan Series consists of very deep, well drained soils that formed in thick beds of unconsolidated, medium to fine-textured marine sediments. Dothan soils are on interfluves. The surface 0-33 cm is characterized by sandy-loam, well-drained soils that are strongly acid. From 33-200 cm they are characterized by sandy clay loam soils that are more moisture retentive and strongly acid. The Angie series consists of very deep, moderately well drained, slowly permeable soils that formed in loamy and clayey sediment on Tertiary-aged uplands. These soils are on broad, level to strongly sloping coastal plains. Slope is dominantly 1 to 5 percent, but the range is 0 to 12 percent. (Source: NRCS Web Soil Survey.)Wild material2165675NA 88845
232NA 88846RJL-RM2023FLAL-020Ilex decidua Walter Florida, United StatesNA2023COLLECTED12/13/2023Yellow River Water Management Area: found in an area where an unnamed unpaved road dead ends near the Yellow River. This unpaved road is accessed from Old River Road to the east near the junction with Shockley Springs Road.30.86973100, -86.5916870023Plants are growing primarily in part-shade to part-sun in low-lying moist habitats associated with the Yellow River. They are in the flood zone, but not regularly inundated. Slope: N/A. Aspect: N/A. The underlying geology of this area is the Alum Bluff Group of Miocene origin. It includes the Chipola Formation, Oak Grove Sand, Shoal River Formation, Choctawhatchee Formation and the Jackson Bluff Formation. The formations included in this group are generally defined on the basis of their molluscan faunas and stratigraphic position. Puri (1953) described sediment facies as they relate to the formations of the Alum Bluff Group. These sediments are lithologically distinct as a group, not as individual units. The Alum Bluff Group crops out or is beneath a thin overburden in the western panhandle from river valleys in Okaloosa County eastward to western Jackson County. The Alum Bluff Group consists of clays, sands and shell beds which may vary from fossiliferous, sandy clays to unfossiliferous sands and clays and occasional carbonate beds. Mica is a common constituent and glauconite and phosphate occur sporadically. Induration varies from essentially nonindurated in sands to well indurated in carbonate lenses. Colors range from cream to olive gray with mottled reddish brown in weathered sections. Sand grain size varies from very fine to very coarse with sporadic occurrences of gravel. These sediments generally have low permeabilities and are part of the intermediate confining unit/aquifer system. (Source: USGS Florida Geologic Map Data.) The surface soil profile of this area is primarily Kinston, Johnston, and Bibb soils, frequently flooded. Kinston Series soils are poorly drained, alluvial, fine-loamy, siliceous, and acid soils of flood plains. They are peaty to loamy friable, slightly sticky and slightly plastic in the upper 0 to 7.5 cm of the strata with less sand and more silt-loam in progressively deeper strata. The Johnston Series consists of very deep, very poorly drained coarse-loamy, siliceous, active, acid, thermic Cumulic Humaquepts. The upper 0-75 cm is black, mucky loam that is friable and very strongly acid. The lower strata to 1.75 m is dark gray, loamy fine sand, single grained, loose and very strongly acid. The Bibb Series soils consists of very deep, poorly drained, moderately permeable soils on flood plains of streams in the Southern Coastal Plain (133A) Major Land Resource Area. They formed in stratified loamy and sandy alluvium that are commonly and frequently flooded and water runs off the surface very slowly. Slopes range from 0 to 2 percent. (Source: NRCS Web Soil Survey.)Wild material2165676NA 88846
233NA 88847RJL-RM2023FLAL-021Ilex amelanchier M. A. Curtis ex Chapm. Florida, United StatesNA2023COLLECTED12/13/2023Yellow River Water Management Area, found in an area where an unnamed unpaved road dead ends near the Yellow River. This unpaved road is accessed from Old River Road to the east near the junction with Shockley Springs Road. Individuals are accessed by foot along the edge of the river and associated wetland depressions to the west of the road.30.86980100, -86.5921050023Plants growing in seasonally inundated swamp habitats associated with the Yellow River. Plants are emergent during portions of the year, primarily during the growing season. During this time of collection, water had receded from the wetlands but the area was still quite wet with many tiny stream rivulets still draining. Slope: N/A. Aspect: N/A. The underlying geology of this area is the Alum Bluff Group of Miocene origin. It includes the Chipola Formation, Oak Grove Sand, Shoal River Formation, Choctawhatchee Formation and the Jackson Bluff Formation. The formations included in this group are generally defined on the basis of their molluscan faunas and stratigraphic position. Puri (1953) described sediment facies as they relate to the formations of the Alum Bluff Group. These sediments are lithologically distinct as a group, not as individual units. The Alum Bluff Group crops out or is beneath a thin overburden in the western panhandle from river valleys in Okaloosa County eastward to western Jackson County. The Alum Bluff Group consists of clays, sands and shell beds which may vary from fossiliferous, sandy clays to unfossiliferous sands and clays and occasional carbonate beds. Mica is a common constituent and glauconite and phosphate occur sporadically. Induration varies from essentially nonindurated in sands to well indurated in carbonate lenses. Colors range from cream to olive gray with mottled reddish brown in weathered sections. Sand grain size varies from very fine to very coarse with sporadic occurrences of gravel. These sediments generally have low permeabilities and are part of the intermediate confining unit/aquifer system. (Source: USGS Florida Geologic Map Data.) The surface soil profile of this area is primarily Kinston, Johnston, and Bibb soils, frequently flooded. Kinston Series soils are poorly drained, alluvial, fine-loamy, siliceous, and acid soils of flood plains. They are peaty to loamy friable, slightly sticky and slightly plastic in the upper 0 to 7.5 cm of the strata with less sand and more silt-loam in progressively deeper strata. The Johnston Series consists of very deep, very poorly drained coarse-loamy, siliceous, active, acid, thermic Cumulic Humaquepts. The upper 0-75 cm is black, mucky loam that is friable and very strongly acid. The lower strata to 1.75 m is dark gray, loamy fine sand, single grained, loose and very strongly acid. The Bibb Series soils consists of very deep, poorly drained, moderately permeable soils on flood plains of streams in the Southern Coastal Plain (133A) Major Land Resource Area. They formed in stratified loamy and sandy alluvium that are commonly and frequently flooded and water runs off the surface very slowly. Slopes range from 0 to 2 percent. (Source: NRCS Web Soil Survey.)Wild material2165677NA 88847
234NA 88820TJK2023AL-005Hydrangea arborescens L. Alabama, United StatesNA2023COLLECTED12/07/2023Between Monroe County Route 1 and Tom Hayles Road.31.40575900, -87.5492400022In woodlands on limestone outcrop. While the upper area of slopes is covered by a thin soil layer, the exposed limestone rock outcrop on the northwestern edge of this area is a low competition niche for plants like the Hydrangea to gain a foothold. Slope: 60% (plus). Aspect: Northwest. Elevation: 72 feet.Wild material2165649NA 88820
235NA 88821TJK2023AL-006Hydrangea quercifolia W. Bartram Alabama, United StatesNA2023COLLECTED12/07/2023Between Monroe County Route 1 and Tom Hayles Road.31.40580000, -87.5489000022In woodlands on limestone outcrop. While the upper area of slopes is covered by a thin soil layer, the exposed limestone rock outcrop on the northwestern edge of this area is a low competition niche for plants like the Hydrangea to gain a foothold. Slope: 60% (plus). Aspect: Northwest. Elevation: 72 feet.Wild material2165650NA 88821
236NA 88801TJK2023LA/TX-001Cocculus carolinus (L.) DC. Louisiana, United StatesNA2023COLLECTED11/21/2023Interstate 20, westbound, approximately 13 miles west of Mississippi River, 9 miles east of U.S. Highway 65.32.33740000, -91.0632000024Damp low, wooded treeline. Slope: less than 2%. Aspect: Southwest. Elevation: 79 feet.Wild material2159184NA 88801
237NA 88802TJK2023LA/TX-002Ilex decidua Walter Louisiana, United StatesNA2023COLLECTED11/21/2023Interstate 20, westbound, approximately 6 miles west of U.S. Highway 65 and 7.5 miles east of Louisiana Highway 577. Tensas River watershed.32.41950000, -91.2967000021Damp wooded treeline. Slope: 12%. Aspect: West-southwest. Elevation: 69 feet.Wild material2159185NA 88802
238NA 88803TJK2023LA/TX-003Crataegus viridis L. Louisiana, United StatesNA2023COLLECTED11/21/2023Interstate 20, westbound, approximately 7 miles west of Louisiana Highway 17 and 8.5 miles east of U.S. Highway 425. Tensas River watershed.32.41940000, -91.2967000021Damp wooded treeline. Slope: 12%. Aspect: West-southwest. Elevation: 69 feet.Wild material2159186NA 88803
239NA 88804TJK2023LA/TX-004Crataegus viridis L. Louisiana, United StatesNA2023COLLECTED11/21/2023Walnut Bayou (Mississippi River bottom): Interstate 20, westbound, approximately 10 miles west of the Mississippi River and 8.25 miles east of U.S. Highway 65.32.34130000, -91.0717000026Damp wooded treeline. Slope: 10%. Aspect: North-northeast. Elevation: 84 feet.Wild material2159187NA 88804
240NA 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
241NA 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
242NA 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
243NA 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
244NA 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
245NA 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
246NA 88708RJL2023NCSC-013Zenobia pulverulenta (W. Bartram ex Willd.) Pollard North Carolina, United StatesNA2023COLLECTED11/13/2023Wetlands associated with Bones Fork and accessed from Nursery Lane onto unnamed road. From Derby Road (Scotland Co Road 1003), turn west onto Nursery Lane and go 3.11 kilometers to unnamed road and turn right. Travel north along Bones Fork on foot for 0.11 kilometers to the collecting site.35.05753000, -79.61873900108Plants growing in shade to part-shade of a moist to wet woodland habitat that is mostly evergreen and deciduous acidic habitat. Slope: N/A. Aspect: N/A. The underlying geology of this area is of Cretaceous origin and characterized as Middendorf Formation. It is composed of sand, sandstone, and mudstone, gray to pale gray with an orange cast, mottled; clay balls and iron-cemented concretions common, beds laterally discontinuous, cross-bedding common. (Source: USGS North Carolina Geologic Map Data.) The primary soil type in the collection area is classified as Ailey Series loamy sand, 8 to 15 percent slopes. The Ailey Series consists of moderately deep or deep to fragic soil properties and deep or very deep to densic materials. This soil is well drained or somewhat excessively drained. The upper layer (0-12.5 cm) of this soil is dark grayish brown loamy sand that is frequently dry. It has a weak fine granular structure, is very friable, non-sticky, non-plastic, and is strongly acid. The lower strata soils (12.5-90 cm) are yellowish brown loamy sand, with weak fine granular structure, very friable, non-sticky, non-plastic, and moderately acid. Deeper depths (below 90 cm) are characterized by slightly greater clay content that is slightly more plastic and strongly acid. (Source: NRCS Web Soil Survey.)Wild material2159136NA 88708
247NA 88710RJL2023NCSC-015Cephalanthus occidentalis L. South Carolina, United StatesNA2023COLLECTED11/14/2023Francis Marion National Forest: plants growing in wetlands/swamps on US Forest Service Road 223 approximately 0.57 kilometers southeast from the junction with Halfway Creek Road.33.06771000, -79.6776970020Plants are growing in part-shade to sun along the edges of the swamp in seasonally inundated acidic wetland habitat. Slope: N/A. Aspect: N/A. The underlying geology of this area is of Pleistocene origin and characterized as an Socastee Formation. This is a low coastal formation in the Carolinas like Penholoway but younger and lower in altitude. It is comprised primarily of unconsolidated, fine-detrital clay. It is described as variegated quartzose sands, argillaceous sands, and clays, 5 m thick at the type section near Socastee Swamp. (Source: USGS South Carolina Geologic Map Data.) The primary soil type in this collection area is classified as Rutlege Series loamy fine sand. Rutlege Series soils are very deep, very poorly drained soils that are sandy, siliceous, thermic Typic Humaquepts. Upper strata soils (0-38 cm) are black loamy sand with weak medium granular structure. They are loose and very strongly acid. Lower strata (38-175 cm) range from dark gray to dark brown sand that is single grained, loose, and very strongly acid. (Source: NRCS Web Soil Survey.)Wild material2159138NA 88710
248NA 88711RJL2023NCSC-016Ilex myrtifolia Walter South Carolina, United StatesNA2023COLLECTED11/14/2023Francis Marion National Forest: plants growing in wetlands/swamps on US Forest Service Road 223 approximately 0.57 kilometers southeast from the junction with Halfway Creek Road.33.06786200, -79.6776180011Plants are growing in shade to part-shade in the swamp in seasonally inundated acidic wetland habitat. Slope: N/A. Aspect: N/A. The underlying geology of this area is of Pleistocene origin and characterized as an Socastee Formation. This is a low coastal formation in the Carolinas like Penholoway but younger and lower in altitude. It is comprised primarily of unconsolidated, fine-detrital clay. It is described as variegated quartzose sands, argillaceous sands, and clays, 5 m thick at the type section near Socastee Swamp. (Source: USGS South Carolina Geologic Map Data.) The primary soil type in this collection area is classified as Rutlege Series loamy fine sand. Rutlege Series soils are very deep, very poorly drained soils that are sandy, siliceous, thermic Typic Humaquepts. Upper strata soils (0-38 cm) are black loamy sand with weak medium granular structure. They are loose and very strongly acid. Lower strata (38-175 cm) range from dark gray to dark brown sand that is single grained, loose, and very strongly acid. (Source: NRCS Web Soil Survey.)Wild material2159139NA 88711
249NA 88712RJL2023NCSC-017Itea virginica L. South Carolina, United StatesNA2023COLLECTED11/14/2023Francis Marion National Forest: plants growing in wetlands/swamps on US Forest Service Road 223 approximately 0.57 kilometers southeast from the junction with Halfway Creek Road.33.06755600, -79.6778910011Plants are growing in the understory of the acidic swamp that is seasonally inundated in shade. Slope: N/A. Aspect: N/A. The underlying geology of this area is of Pleistocene origin and characterized as an Socastee Formation. This is a low coastal formation in the Carolinas like Penholoway but younger and lower in altitude. It is comprised primarily of unconsolidated, fine-detrital clay. It is described as variegated quartzose sands, argillaceous sands, and clays, 5 m thick at the type section near Socastee Swamp. (Source: USGS South Carolina Geologic Map Data.) The primary soil type in this collection area is classified as Rutlege Series loamy fine sand. Rutlege Series soils are very deep, very poorly drained soils that are sandy, siliceous, thermic Typic Humaquepts. Upper strata soils (0-38 cm) are black loamy sand with weak medium granular structure. They are loose and very strongly acid. Lower strata (38-175 cm) range from dark gray to dark brown sand that is single grained, loose, and very strongly acid. (Source: NRCS Web Soil Survey.)Wild material2159140NA 88712
250NA 88713RJL2023NCSC-018Ilex opaca Aiton South Carolina, United StatesNA2023COLLECTED11/14/2023Francis Marion National Forest: plants growing in wetlands/swamps on US Forest Service Road 223 approximately 0.57 kilometers southeast from the junction with Halfway Creek Road.33.06783000, -79.6774910011Plants are growing in part shade to shade of a swamp in seasonally inundated acidic wetland habitat. Slope: N/A. Aspect: N/A. The underlying geology of this area is of Pleistocene origin and characterized as an Socastee Formation. This is a low coastal formation in the Carolinas like Penholoway but younger and lower in altitude. It is comprised primarily of unconsolidated, fine-detrital clay. It is described as variegated quartzose sands, argillaceous sands, and clays, 5 m thick at the type section near Socastee Swamp. (Source: USGS South Carolina Geologic Map Data.) The primary soil type in this collection area is classified as Rutlege Series loamy fine sand. Rutlege Series soils are very deep, very poorly drained soils that are sandy, siliceous, thermic Typic Humaquepts. Upper strata soils (0-38 cm) are black loamy sand with weak medium granular structure. They are loose and very strongly acid. Lower strata (38-175 cm) range from dark gray to dark brown sand that is single grained, loose, and very strongly acid. (Source: NRCS Web Soil Survey.)Wild material2159141NA 88713
251NA 88714RJL2023NCSC-019Smilax walteri Pursh South Carolina, United StatesNA2023COLLECTED11/14/2023Francis Marion National Forest: plants growing in wetlands/swamps on US Forest Service Road 223 approximately 0.57 kilometers southeast from the junction with Halfway Creek Road.33.06757700, -79.6779280011Plants are growing in shade, part-shade and sun in the acid soils of a swamp and along the edges of the swamp where the soils are seasonally inundated. Slope: N/A. Aspect: N/A. The underlying geology of this area is of Pleistocene origin and characterized as a Socastee Formation. This is a low coastal formation in the Carolinas like Penholoway but younger and lower in altitude. It is comprised primarily of unconsolidated, fine-detrital clay. It is described as variegated quartzose sands, argillaceous sands, and clays, 5 m thick at the type section near Socastee Swamp. (Source: USGS South Carolina Geologic Map Data.) The primary soil type in this collection area is classified as Rutlege Series loamy fine sand. Rutlege Series soils are very deep, very poorly drained soils that are sandy, siliceous, thermic Typic Humaquepts. Upper strata soils (0-38 cm) are black loamy sand with weak medium granular structure. They are loose and very strongly acid. Lower strata (38-175 cm) range from dark gray to dark brown sand that is single grained, loose, and very strongly acid. (Source: NRCS Web Soil Survey.)Wild material2159142NA 88714
252NA 88718RJL2023NCSC-023Ilex decidua Walter South Carolina, United StatesNA2023COLLECTED11/15/2023Waccamaw National Wildlife Refuge: U.S. Highway 701, Yauhannah Landing on the east side of the Great Pee Dee River. Plants growing in low woods on the north side of the landing.33.66208900, -79.153050002Plants growing in shade to part-shade of a moist to wet woodland habitat that is mostly deciduous and evergreen. Portions of the woodland have depressions with year-round standing water. Slope: N/A. Aspect: N/A. The underlying geology of this area is of Quaternary origin and characterized as Alluvial Valley Swamp. This formation is unconformable on all underlying units. It is composed of fluvial sand and gravel at base, grading upwards into fine sands and silts, and local occasional peat. May be overrun with recent sediments from forest cutting and agriculture. (Source: USGS South Carolina Geologic Map Data.) The primary soil type in this collection area is classified as Johnston Series loam. The Johnson Series consists of very deep, very poorly drained coarse-loamy, siliceous, active, acid, thermic Cumulic Humaquepts. The upper 0-75 cm is black, mucky loam that is friable and very strongly acid. The lower stratum to 1.75 m is dark gray, loamy fine sand, single grained, loose and very strongly acid. (Source: NRCS Web Soil Survey.)Wild material2159146NA 88718
253NA 88723RJL2023NCSC-028Ilex myrtifolia Walter North Carolina, United StatesNA2023COLLECTED11/15/2023Juniper Creek State Game Lands (along Brunswick County Road 1340): swamps/wetlands associated with Juniper Creek.34.12438700, -78.3931070013Plants growing in shade to part-shade of a swamp habitat along Juniper Creek. At the time of collection, the swamp was relatively dry with water found only in deep depressions. Slope: N/A. Aspect: N/A. The underlying geology of this area is of Cretaceous origin and characterized as Peedee Formation - Black Creek Group, undivided. The Peedee Formation is primarily unconsolidated, coarse-detrital, sand that is dark-green or gray, finely micaceous, more or less glauconitic, and argillitic sand, many layers of which are calcareous (impure limestone). Irregular concretionary masses of impure calcium carbonate occur in places. Dark marine clays are interstratified with sand. The Black Creek Group consists of irregularly bedded, laminated, carbonaceous clays and thin laminae and lenses of sand; lignite and pyrite present; glauconitic in places; massive interbedded layers of glauconitic sand present toward top of unit. Light-colored clays and coarse arkosic sands also found. (Source: USGS North Carolina Geologic Map Data.) The primary soil type in this collection area is classified as Dorovan Series muck. The Dorovan Series consists of very deep, very poorly drained, moderately permeable soils on densely forested flood plains, hardwood swamps, and depressions in the Atlantic Coast Flatwoods, Eastern Gulf Coast Flatwoods, and Southern Coastal Plain Major Land Resource Areas. They formed in highly decomposed acid-organic materials and have slopes that are less than 1 percent. (Source: NRCS Web Soil Survey.)Wild material2159151NA 88723
254NA 88671RJL2023PA-005Rhododendron maximum L. Pennsylvania, United StatesNA2023COLLECTED10/16/2023Appalachian National Scenic Trail: Pulpit Rock and Pinnacle Loop. Rocky woodlands along Furnace Creek as well as steep rocky slopes above Pulpit Rock Reservoir associated with the Pulpit Rock and Pinnacle Loop Trail.40.59226100, -75.94588800301Well-drained and very rocky dry deciduous woodlands in part shade to full shade. Slope: 0-30%. Aspect: variable. The underlying geology of this area is of Silurian origin and characterized as the Shawangunk Formation. It is characterized by light- to dark-gray, fine- to very coarse-grained sandstone and conglomerate containing thin shale interbeds. Includes four members, in descending order: Tammany--conglomerate and sandstone; Lizard Creek--sandstone and red or green shale; Minsi--sandstone and conglomerate; Weiders--conglomerate. Tammany and Lizard Creek Members together are approximately equivalent to Clinton Group to the west; Minsi and Weiders Members together are equivalent to Tuscarora Formation to the west. (Source: USGS Pennsylvania Geologic Map Data). The primary soil type in the collection area is classified as Hazleton Series. The Hazleton series consists of deep and very deep, well drained soils formed in residuum of acid gray, brown or red sandstone on uplands. Slope ranges from 0 to 80 percent. Permeability is moderately rapid to rapid. Solum thickness ranges from 60 to 120 centimeters. Depth to lithic contact ranges from 1 to 2 meters. Rock fragments of angular sandstone, dominantly less than 25 cm in size, range from 5 to 70 percent in individual horizons. Boulders, stones, flags and channers cover about 5 to 60 percent of the surface of some pedons. Reaction ranges from strongly acid through extremely acid throughout. (Source: NRCS Web Soil Survey).Wild material2159062NA 88671
255NA 88672RJL2023PA-006Rhododendron periclymenoides (Michx.) Shinners Pennsylvania, United StatesNA2023COLLECTED10/16/2023Appalachian National Scenic Trail: Pulpit Rock and Pinnacle Loop. Rocky woodland edges above Furnace Creek around Pulpit Rock and Pinnacle Loop Trail.40.58668200, -75.94269600247Well-drained and very rocky dry deciduous woodlands in part shade to full shade. Slope: 10%. Aspect: East. The underlying geology of this area is of Silurian origin and characterized as the Shawangunk Formation. It is characterized by light- to dark-gray, fine- to very coarse-grained sandstone and conglomerate containing thin shale interbeds. Includes four members, in descending order: Tammany--conglomerate and sandstone; Lizard Creek--sandstone and red or green shale; Minsi--sandstone and conglomerate; Weiders--conglomerate. Tammany and Lizard Creek Members together are approximately equivalent to Clinton Group to the west; Minsi and Weiders Members together are equivalent to Tuscarora Formation to the west. (Source: USGS Pennsylvania Geologic Map Data). The primary soil type in the collection area is classified as Hazleton Series. The Hazleton series consists of deep and very deep, well drained soils formed in residuum of acid gray, brown or red sandstone on uplands. Slope ranges from 0 to 80 percent. Permeability is moderately rapid to rapid. Solum thickness ranges from 60 to 120 centimeters. Depth to lithic contact ranges from 1 to 2 meters. Rock fragments of angular sandstone, dominantly less than 25 cm in size, range from 5 to 70 percent in individual horizons. Boulders, stones, flags and channers cover about 5 to 60 percent of the surface of some pedons. Reaction ranges from strongly acid through extremely acid throughout. (Source: NRCS Web Soil Survey).Wild material2159063NA 88672
256NA 88677RJL2023PA-011Hydrangea arborescens L. Pennsylvania, United StatesNA2023COLLECTED10/25/2023Seed collected along the Appalachian National Scenic Trail, accessed from the Duncannon Entrance.40.37735300, -77.03997300239Well-drained and very rocky dry deciduous woodlands in part shade to full shade. Slope: 20-50%. Aspect: Northwest. The underlying geology of this area is of Devonian origin and characterized as the Duncannon Member of Catskill Formation. It is characterized by grayish-red sandstone, siltstone, and mudstone in fining-upward cycles; conglomerate occurs at base of some cycles. The sandstones which comprise the Duncannon Member are fine to very coarse grained and grayish red to grayish red-purple in color. The Duncannon Member is known to be crossbedded to planar bedded in beds anywhere from 3 to 9 meters thick. Conglomerates have been spotted at the base of the Duncannon Member. The Duncannon Member is poorly exposed in most areas except along the Lehigh River. The conglomerate portion of this member has been known to form ridges and ledges with thicknesses approaching 228 meters. (Source: USGS Pennsylvania Geologic Map Data). The primary soil type in the collection area is classified as Dystrochrepts, boulder soils. These soils are characterized by coarse-silty loess over residuum weathered from sedimentary rock and located on steep ridges along the upper third of the mountainflank. These soils are comprised of cobbles, stones or boulders (9%), well-drained, and approximately 1 meter or less to lithic bedrock. (Source: NRCS Web Soil Survey).Wild material2159068NA 88677
257NA 88678RJL2023PA-012Viburnum acerifolium L. Pennsylvania, United StatesNA2023COLLECTED10/27/2023Slopes on the east side of Creek Road above the North Branch of White Clay Creek.39.78552600, -75.8025190090Well-drained mesic-dry to rocky dry deciduous woodlands in part shade to full shade. Slope: 15-35%. Aspect: West to northwest. The underlying geology of this area includes two formations. The first and primary formation is Lower Paleozoic Glenarm Wissahickon Formation, lithologically similar to oligoclase-mica schist of the Wissahickon Formation, but also includes lenticular amphibolite bodies having ocean-floor basalt chemistry. The second formation is Lower Paleozoic Mafic Gneiss Formation that is dark and medium grained. It includes rocks of probable sedimentary origin. (Sources: USGS Pennsylvania Geologic Map Data). The primary soil type in the collection area is classified as Manor Series. The Manor Series consists of well-drained residuum weathered from micaceous schist. Soils in the upper pedon (0-33 cm) are very dark grayish brown loam with strong fine granular structure; also, very friable with fine mica flakes and strongly acid. Lower pedon soils (34-56 cm) are strong brown, sandy loams. They have weak medium sub-angular blocky structure, are friable with many fine and a few medium mica flakes; this pedon is very strongly acid. (Source: NRCS Web Soil Survey).Wild material2159069NA 88678
258NA 88679RJL2023PA-013Rhododendron prinophyllum (Small) Millais Pennsylvania, United StatesNA2023COLLECTED10/30/2023Southwest side of Dutch Mountain Road north of Pine Marsh Creek in Pennsylvania State Game Lands Number 66.41.48201500, -76.27286000602Moist, well-drained habitat with good organic matter in part shade on a wooded slope next to the road. Slope: 5-10%. Aspect: East. The underlying geology of this area is of Mississippian origin and characterized as the Burgoon Formation. It is comprised of buff, medium-grained, cross bedded sandstone that includes shale and coal. In some places, it contains conglomerate at base as well as occasionally contains plant fossils; equivalent to Pocono Formation of Ridge and Valley province. (Source: USGS Pennsylvania Geologic Map Data). The primary soil type in the collection area is classified as Wellsboro Series. The Wellsboro Series consists of very deep, moderately well- and somewhat poorly-drained soils formed in till derived from red sandstone, siltstone, and shale. Slope ranges from 0 to 50 percent. Saturated hydraulic conductivity is moderately high or high in the mineral surface layer, subsurface layer, and upper part of the subsoil; and low or moderately low in the lower part of the subsoil (fragipan) and the substratum. Solum thickness is greater than 102 cm. Depth to the fragipan ranges from 36 to 76 cm. Depth to bedrock is 152 cm or more. Rock fragments of subangular and rounded sandstone, siltstone or shale range from 5 to 40 percent in the A and B horizons, and from 15 to 50 percent in the Bx and C horizons. Typically, rock fragments average about 5 to 25 percent by volume above the fragipan and 15 to 40 percent by volume in and below the fragipan. Reaction commonly ranges from very strongly acid through moderately acid. (Source: NRCS Web Soil Survey).Wild material2159070NA 88679
259NA 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
260Ames 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
261NA 88667RJL2023PA-004Viburnum acerifolium L. Pennsylvania, United StatesNA2023Wild material2158816NA 88667
262NA 88666RJL2023PA-003Hamamelis virginiana L. Pennsylvania, United StatesNA2023COLLECTED10/01/2023Collected primarily along the woodland edge along Northside Road on Pennsylvania State Gamelands No. 43 as well as a few on nearby roads.40.17974200, -75.76790700176Plants were growing in mesic well-drained conditions on moderately sloping sites of a deciduous upland forest. This species grows well in shade to part-sun. Most abundant fruit development is found where plants are exposed to sunlight for a portion of the day. Slope: 15%. Aspect: North-northwest. The underlying geology of this area is of Precambrian origin and characterized as the Graphitic Felsic Gneiss. This includes Pickering Gneiss and small areas of marble; dominantly quartz and feldspar with varying amounts of graphite and various metamorphic minerals; medium grained, light to dark gray and greenish gray; sedimentary origin. (Source: USGS Pennsylvania Geologic Map Data.) The primary soil type in the area of this collection is classified as Gladstone Gravelly Loam Series (8 to 15 percent slopes). The Gladstone Series consists of very deep, well drained soils formed in residuum and colluvium from granitic gneiss. Saturated hydraulic conductivity is moderately high to high. Solum thickness ranges from 75 to 125 cm. Depth to granitic gneiss bedrock is 1.6 meters or more. The bedrock may be strongly weathered in the upper part. Gravel content ranges from 5 to 35 percent throughout the solum, and 10 to 40 percent in the C horizons. Fragments, larger than 3 inches in diameter, range from 0 to 20 percent by volume in the surface layer and 0 to 10 percent in the subsoil and substratum layers. Reaction is strongly or very strongly acid throughout the soil, unless limed. Areas that have been limed range to moderately acid in the upper part of the profile. (Source: NRCS Web Soil Survey.)Wild material2158815NA 88666
263NA 88665RJL2023PA-002Ilex verticillata (L.) A. Gray Pennsylvania, United StatesNA2023COLLECTED10/01/2023Woodlands along Pine Creek near the Harmonyville Road bridge.40.18764500, -75.76732200141Moist to mucky, wet woodland conditions along Pine Creek. Much of the site is very wet due to recent rains; though, earlier in the year, the soils were only moist. Plants grow in both well-drained mesic conditions as well as seasonally wet conditions. They do not grow in standing water anywhere in this location. Plants in this population are found mostly in the shade and partial shade of deciduous trees; there are occasional gaps that offer higher light conditions as well. Slope: 0-2%. Aspect: N/A. The underlying geology of this area is of Precambrian origin and characterized as the Graphitic Felsic Gneiss. This includes Pickering Gneiss and small areas of marble; dominantly quartz and feldspar with varying amounts of graphite and various metamorphic minerals; medium grained, light to dark gray and greenish gray; sedimentary origin. (Source: USGS Pennsylvania Geologic Map Data). The primary soil type in the area of this collection is classified as Hatboro Silt Loam Series. The Hatboro Series consists of very deep and poorly drained soils formed in alluvium derived from metamorphic and crystalline rock. They are on flood plains. Slopes range from 0 to 3 percent. Saturated hydraulic conductivity is moderately high to high. Solum thickness ranges from 50 to 150 cm. Depth to bedrock ranges from 1.5 to 3 meters or more. Organic carbon decreases irregularly with depth or is greater than 0.2 percent directly above any strongly contrasting C horizon. The depth to strongly contrasting sand and gravel is more than 100 cm or the transition is greater than 12.5 cm. Content of gravel ranges from 0 to 10 percent in the solum and from 0 to 80 percent in the C horizon. Mica flakes are common in the solum, and the C horizon contains thin lenses of mica. Reaction ranges from very strongly acid through neutral to a depth of 75 cm and from moderately acid through slightly acid below 75 cm. (Source: NRCS Web Soil Survey.)Wild material2158814NA 88665
264NA 88664RJL2023PA-001Viburnum acerifolium L. Pennsylvania, United StatesNA2023COLLECTED10/01/2023Seed collected from plants growing along a two-mile stretch of Harmonyville Road on the woodland edge next to the road. [Note: latitude and longitude were collected at the location of the largest seed collection.]40.18482200, -75.78145100158Plants were growing in well-drained and rocky mesic-dry woodlands from part shade along the road edge to full shade in the understory of the woodlands. Slope: 2-10%. Aspect: Variable. The underlying geology of this area is of Triassic origin and characterized as the Stockton Formation. It is characterized by light-gray to buff, coarse-grained, arkosic sandstone; includes reddish-brown to grayish-purple sandstone, siltstone, and mudstone. (Source: USGS Pennsylvania Geologic Map Data.) The primary soil type in the area of this collection is classified as Edgemont Channery Sandy Loam Series (8 to 25 percent slopes), extremely stony. The Edgemont Series consists of deep and very deep, well drained soils formed in the weathered residuum of quartzitic rocks. They have moderately high to high saturated hydraulic conductivity. Slopes range from 0 to 70 percent. Solum thickness ranges from 50 to 10 cm. Depth to bedrock ranges from about 1.5 to 2.2 meters. Kaolinite is the dominant mineral in the clay fraction with detectable amounts of illite, vermiculite, montmorillonite, chlorite and interstratified clays. Gravel, channers, and stone size fragments of quartzite and quartz are present throughout the profile. Rock fragments range from 5 to 40 percent in the horizons of the solum and from 10 to 90 percent in the C horizon. Reaction ranges from extremely acid to strongly acid throughout. (Source: NRCS Web Soil Survey.)Wild material2158813NA 88664
265Ames 36132Prairie Valley PreserveDelphinium carolinianum Walter subsp. virescens (Nutt.) R. E. Brooks Iowa, United StatesNC7FLOWER2023COLLECTED07/14/2023Prairie Valley Preserve located 2.5 miles west of Gilbert on the southeast corner of Y Avenue and 170th, T84N R24W NW ¼ NW ¼ Sec. 7.42.10528000, -93.69776000288Prairie remnant. Historically grazed for estimated 75 years. Mid-upper slopes on slightly north, northwest-facing slopes. Wild materialPlants in nature reaching (max) up to 75 cm in height. 2158217Ames 36132
266Ames 36073JDC/UT/2022/028/1009Ulmus thomasii Sarg. Iowa, United StatesNC7SHOOT2023COLLECTED06/05/2023Ledges State Park approximately 4.75 miles south of Boone, T83N R26W (Madrid NW Quad.) near center of SE ¼ Sec. 16 and also NW ¼ SW ¼ Sec. 21.41.99780200, -93.87967900288Moist deciduous woods typically on mid-slopes to base of slopes and also well-drained floodplains.Wild materialUlmus thomasii (Rock elm) is an underutilized tree species both in conservation and in the urban landscape. Charles Sprague Sargent (first director of the Arnold Arboretum of Harvard University, Boston, MA) described the wood of Rock Elm as "heavy, hard, very strong and tough, closely grained, and susceptible of receiving a beautiful polish". Historically noted for a variety of uses in woodworking including furniture, heavy agricultural implements, timber frame buildings, pianos, hockey sticks, and hand tools. U. thomasii is extremely drought tolerant, adaptable to very calcareous soils, and compared to U. americana or U. rubra has a very conservative growth rate requiring minimal attention in regards to pruning. Rock elm naturally tends to develop into a nice structural specimen in the landscape, unlike other fast growing U. americana cultivars in the nursery trade needing frequent attention. Rock elm has very fissured bark and is well known for maintaining a strong central leader resulting in a very attractive, pyramidal form. Despite many literature sources stating that "wings" on the stems are a key identifiying characteristic, this trait is not reliable and many genotypes may completely lack "wings" on the stems. While growth habit and morphology of dormant buds (very pointy) are good traits to help aid in identification, fruits are the best way to confirm identity. Fruits are densly pubescent, often described as "inflated" and generally reach maturity a couple weeks after U. rubra and U. americana. U. thomasii flowering in central Iowa typically occurs the last week in April into the first week in May and are rather distinguishable from other Ulmus in being pendulous. Fruits are extremely prized treats for many birds, where fruits are often "robbed" prior to full maturity. Fruits are also highly prized by many other animals such as mice, squirrels, chipmunks, turkeys, etc. and are generally consumed within hours after fruit abscission. The native range of U. thomasii is concentrated in the northeastern United States and into Canada with disjunct populations documented in northwestern Missouri and northwestern Arkansas (Little, E. L. Jr. 1971). In the 1895 Silva of North America (vol. 7) it was stated that, “The value of the wood of the Rock Elm threatens its extinction and most of the large trees have already been cut.” Today, since rock elm is rather rare, especially in areas near the edges of its range, many states list the species as endangered or threatened warranting preservation efforts. Genetics of this accession would be representative of the species southwestern edge of its native range. At the collection site in nature (Ledges State Park), out of approximately 100 specimens noted only 1-2% of specimens had characteristic "wings" on the stems. Research was executed (Moore, P., 2024) involving the core sampling of U. thomasii and U. americana specimens in Ledges State Park to make growth ring widths and basal area increment comparisons. Results determined that the average age of cored trees U. thomasii (n=4) and U. americana (n=4) of both species was roughly 80 years, excluding the exceptional case of tree #007 (Ames 36073 23ncao02 SD). Tree #007 was aged at 300 years of age and currently (2025) ranks as the 14th largest U. thomasii in Iowa measuring 21" DBH with a height of 75' 5" and a spread of 43' 5" totalling 152.21 points (Rouw, M., personal communication, 4 May 2022). The computed mean density at 𝑀𝑀 = 12% for U. thomasii was 0.80 g/cm3, and for U. americana was 0.672 g/cm3. These values are both higher than the representative values inferred from the Woods Database which are 0.755 g/cm3 for U. thomasii and 0.56 g/cm3 for U. americana. To date, there is little to no information regarding U. thomasii resistance to Dutch Elm Disease. Collections of U. thomasii at the Arnold Arboretum have over-time succumbed to DED (Pruka, B., 2016). However, data recorded by Moore (2024) indicates that U. thomasii growing in central Iowa can surpass 300 years in age verifying it's long-term utilization in the landscape. 2142915Ames 36073
267OPGC 8750ID120-25Symphyotrichum spathulatum (Lindl.) G. L. Nesom Idaho, United StatesOPGC2023Wild material2142071OPGC 8750
268OPGC 8755ID130-47Symphyotrichum spathulatum (Lindl.) G. L. Nesom Idaho, United StatesOPGC2023Wild material2142082OPGC 8755
269W6 60993CA340-23Wyethia angustifolia (DC.) Nutt. California, United StatesW62023Wild materialAll along lost valley where shrubs are not present. Low to ground but distinct leaves .2142632W6 60993
270W6 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
271W6 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
272OPGC 8803CBG- 10754Aquilegia canadensis L. Illinois, United StatesOPGC2023Wild material2142225OPGC 8803
273OPGC 8810CBG- 10773Penstemon pallidus Small Illinois, United StatesOPGC2023Wild material2142241OPGC 8810
274OPGC 8813CBG- 10781Hieracium scabrum Michx. Illinois, United StatesOPGC2023Wild material2142247OPGC 8813
275OPGC 8815CBG- 10787Maianthemum racemosum (L.) Link subsp. racemosum Wisconsin, United StatesOPGC2023Wild material2142251OPGC 8815
276OPGC 8818CBG- 10797Ludwigia alternifolia L. Illinois, United StatesOPGC2023Wild material2142256OPGC 8818
277OPGC 8821CBG- 10803Rhexia virginica L. Illinois, United StatesOPGC2023Wild material2142262OPGC 8821
278OPGC 8831CBG- 10837Solidago sciaphila E. Steele Wisconsin, United StatesOPGC2023Wild material2142286OPGC 8831
279OPGC 8833CBG- 10839Verbena hastata L. South Dakota, United StatesOPGC2023Wild material2142288OPGC 8833
280OPGC 8840CBG- 10848Symphyotrichum shortii (Lindl.) G. L. Nesom Illinois, United StatesOPGC2023Wild material2142296OPGC 8840
281OPGC 8848CBG- 10860Solidago riddellii Frank Illinois, United StatesOPGC2023Wild material2142306OPGC 8848
282OPGC 8849CBG- 10861Chelone glabra L. Illinois, United StatesOPGC2023Wild material2142307OPGC 8849
283W6 61366CBG- 10782Paronychia canadensis (L.) Alph. Wood Illinois, United StatesW6SEED2023Wild material2142248W6 61366
284W6 61370CBG- 10788Drymocallis arguta (Pursh) Rydb. Wisconsin, United StatesW6SEED2023Wild material2142252W6 61370
285W6 61379CBG- 10802Triadenum fraseri (Spach) Gleason Illinois, United StatesW6SEED2023Wild material2142261W6 61379
286W6 61403CBG- 10836Triosteum aurantiacum E. P. Bicknell Wisconsin, United StatesW6SEED2023Wild material2142285W6 61403
287NA 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
288WLP 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
289NA 88536RJLSEUS2022-007Leucothoe axillaris (Lam.) D. Don South Carolina, United StatesNA2023COLLECTED12/07/2022Plants growing along the margin of Sandy Run and its associated wetland on the north side of Paradise Rd. (State Rd. S-15-403). Common at this site and throughout the drainage of Sandy Run and its associated wetland. 32.83900000, -80.8101440027Plants are growing in part-shade to shade of a moist mesic woodland habitat along a small wetland associated with Sandy Run. Plants are located in an area that occasionally floods, but is not permanently wet.
Soils: The underlying geology of this area is of Pliocene origin and characterized as Bear Bluff Formation. This formation is considered one of the older coastal terrace sequences in the Carolinas. Bear Bluff Formation consists of gray to cream, fossiliferous, coarse-grained calcareous sand, and sandy limestone. It is typically 3-40 meters thick.
Source: USGS South Carolina Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=SCTbb%3B1)
The primary soil type in the collection area is classified as Pickney Loamy Sand soils. The Pickney Series consists of very deep, very poorly drained soils. Permeability is rapid. These nearly level soils have negligible runoff and were formed by marine or fluvial sediments in the lower coastal plain on flats, depressions, stream terraces, and flood plains. Slopes range from 0 to 2 percent. The soils of this series are loamy fine sand that is very friable and extremely acid in the upper 0-25 cm. The lower strata are similar, while the lower strata from 0.8-2 meters are comprised of fine sand.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild materialLeucothoe axillaris/fontanesiana2140764NA 88536
290NA 88537RJLSEUS2022-009Rhododendron canescens (Michx.) Sweet South Carolina, United StatesNA2023COLLECTED12/07/2022Plants growing along the upper margin of a small stream and associated wetland on the northwest side of Paradise Rd. (State Rd. S-15-403). Common at this site and throughout the drainage of the stream and associated wetland.32.83868100, -80.8109920028Plants are growing in part-shade to shade of a moist mesic woodland habitat along a small wetland associated with a creek. Plants are located in an area that occasionally floods, but is not permanently wet.
Soils: The underlying geology of this area is of Pliocene origin and characterized as Bear Bluff Formation. This formation is considered one of the older coastal terrace sequences in the Carolinas. Bear Bluff Formation consists of gray to cream, fossiliferous, coarse-grained calcareous sand, and sandy limestone. It is typically 3-4 meters thick.
Source: USGS South Carolina Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=SCTbb%3B1)
The primary soil type in the collection area is classified as Pickney Loamy Sand soils. The Pickney Series consists of very deep, very poorly drained soils. Permeability is rapid. These nearly level soils have negligible runoff and were formed by marine or fluvial sediments in the lower coastal plain on flats, depressions, stream terraces, and flood plains. Slopes range from 0 to 2 percent. The soils of this series are loamy fine sand that is very friable and extremely acid in the upper 0-25 cm. The lower strata are similar, while the lower strata from 0.8-2 meters are comprised of fine sand.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2140765NA 88537
291NA 88538RJLSEUS2022-010Ilex glabra (L.) A. Gray Georgia, United StatesNA2023COLLECTED12/08/2022Junction of Old Whitley Rd & Irwinville Hwy (GA 125).31.64601300, -83.33625800111Low woods, a remnant woodland/low moist habitat between agricultural fields. Growing in part shade to shade of a moist mesic (occasionally temporarily wet) mixed evergreen and deciduous woodland along the edge where light conditions are slightly higher. The underlying geology of this area is of Neogene origin and characterized as Neogene Undifferentiated. It includes poorly sorted clayey sand and gravel deposited in a fluvial environment in South Carolina but becoming more fluvio-marine in Georgia. This unit is characterized by in situ weathered feldspar and an abundance of quartzite gravel and cobbles. (Source: USGS Georgia Geologic Map Data). The primary soil types in the collection area are classified as Alapaha Loamy Sand soil (0 to 2 percent slopes, occasionally flooded). The Alapaha Series consists of very deep, poorly drained, moderately slow to slowly permeable soils in small drainageways, flats, seepage areas, and depressions. They formed in sandy and loamy marine deposits of the Southern Coastal Plain. Slopes range from 0 to 5 percent. This series consists of deep, somewhat poorly drained soils. Permeability is very slow. These nearly level to gently sloping soils formed in clayey alluvium on flood plains of streams that drain uplands of the Southern Coastal Plain. The water table ranges from 0-25 cm below the surface and the soils are strongly acid. (Source: NRCS Web Soil Survey).Wild material2140816NA 88538
292NA 88541RJLSEUS2022-013Rhododendron viscosum (L.) Torr. Georgia, United StatesNA2023COLLECTED12/09/2022Plants growing around a pond and associated wetland on the property of Monica Williams north of Albany, Georgia. Common along the edges of the pond and wetland area. 31.63828300, -84.1382700062Plants are growing in part-shade to sun of a wetland habitat on the edge of a large pond. The habitat is comprised of numerous hummocks where this species grows, slightly above the permanently wet, inundated edges of the pond. Some plants are growing in more shade under moist mesic conditions as well.
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 material2140768NA 88541
293NA 88544RJLSEUS2022-016Itea virginica L. Georgia, United StatesNA2023COLLECTED12/09/2022Plants growing around a pond and associated wetland on the property of Monica Williams north of Albany, Georgia as well as the edges of nearby Muckalee Creek. Common in the wetland habitat edges. 31.63834700, -84.1383560063Plants are growing in part-shade to sun in wet to inundated conditions along the edges of a pond as well as the edges of Muckalee Creek. This species is found in conditions of abundant, year-round moisture.
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 material2140770NA 88544
294NA 88545RJLSEUS2022-017Cephalanthus occidentalis L. Georgia, United StatesNA2023COLLECTED12/09/2022Plants growing around a pond and associated wetland on the property of Monica Williams north of Albany, Georgia. Infrequent frequency.31.63802000, -84.1349900059Plants are growing in part-shade to sun in the wetland associated with a large pond. This area is frequently wet during the growing season, but drier during the winter months.
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 material2140771NA 88545
295NA 88547RJLSEUS2022-019Alnus serrulata (Aiton) Willd. Alabama, United StatesNA2023COLLECTED12/10/2022Poke Springs Branch inlet accessed by boat from Walter F. George Reservoir. Frequent plants.31.72236600, -85.1279370063Plants are growing in full sun on the eroded bank of the lake. The plants have access to abundant moisture with root systems extended into the lake.
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 soils (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 material2140773NA 88547
296NA 88548RJLSEUS2022-020Morella cerifera (L.) Small Alabama, United StatesNA2023COLLECTED12/10/2022Poke Springs Branch inlet accessed by boat from Walter F. George Reservoir. Common frequency.31.72236600, -85.1279370063Plants are growing in full sun on the eroded bank of the lake. The plants have access to abundant moisture with root systems extended into the lake.
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 soils (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 material2140774NA 88548
297NA 88554RJLSEUS2022-027Rhododendron alabamense Rehder Alabama, United StatesNA2023COLLECTED12/12/2022Plants growing on woodland slopes around and below the hilltop parking area leading down to the Silver Creek Lake Campground off of Silver Creek Lake Road. Occasional in the upland woodlands. 31.66613100, -87.5762570049Plants are growing in shade of upland dry mesic mature mixed deciduous and evergreen woodland. Generally, the overstory is thinner and there is less leaf litter cover, making the surface soil conditions drier.
Soils: 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 (https://mrdata.usgs.gov/geology/state/state.php?state=AL)
The primary soil types in the collection area are classified as Smithdale-Boykin Complex soils (2 to 5 percent slopes). The Smithdale Series consists of very deep, well drained, moderately permeable soils on ridge tops and hill slopes in dissected uplands of the Southern Coastal Plain and in the Western Coastal Plain. They formed in thick beds of loamy marine sediments and are strongly acid. Slopes range from 1 to 60 percent. The Boykin Series consists of deep, well drained, moderately permeable soils that formed in sandy and loamy coastal plain sediments of Pleistocene age. These soils are on gently sloping to moderately steep uplands. Slopes range from 1 to 20 percent.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2140781NA 88554
298NA 88555RJLSEUS2022-028Rhododendron canescens (Michx.) Sweet Alabama, United StatesNA2023COLLECTED12/12/2022Plants growing on woodland slopes below the hilltop parking area leading down to the Silver Creek Lake Campground off of Silver Creek Lake Road. Occasional in the woodlands. 31.66549700, -87.5762450045Plants are growing in shade of moist mesic deciduous and evergreen woodland, mid-slope between the upland dry mesic zone and the creekside habitat below.
Soils: 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 (https://mrdata.usgs.gov/geology/state/state.php?state=AL)
The primary soil types in the collection area are classified as Luverne Sandy Loam soils (15 to 35 percent slopes). The Luverne Series consists of very deep, well drained, moderately slowly permeable soils on dissected uplands of the Southern Coastal Plain. They formed in stratified marine sediments and are strongly acid. The lower strata of this series are clay and clay loam. Slopes range from 1 to 45 percent.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2140782NA 88555
299NA 88556RJLSEUS2022-029Rhododendron colemanii R. F. Mill. Alabama, United StatesNA2023COLLECTED12/12/2022Plants growing on woodland slopes below the hilltop parking area leading down to the Silver Creek Lake Campground off of Silver Creek Lake Road. Occasional in the woodlands. 31.66503300, -87.5746800043Plants are growing in shade of moist mesic deciduous and evergreen woodland on rich slopes 1-3 meters above a small spring-fed creek.
Soils: 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 (https://mrdata.usgs.gov/geology/state/state.php?state=AL)
The primary soil types in the collection area are classified as Smithdale-Boykin Complex soils (2 to 5 percent slopes). The Smithdale Series consists of very deep, well drained, moderately permeable soils on ridge tops and hill slopes in dissected uplands of the Southern Coastal Plain and in the Western Coastal Plain. They formed in thick beds of loamy marine sediments and are strongly acid. Slopes range from 1 to 60 percent. The Boykin Series consists of deep, well drained, moderately permeable soils that formed in sandy and loamy coastal plain sediments of Pleistocene age. These soils are on gently sloping to moderately steep uplands. Slopes range from 1 to 20 percent.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2140783NA 88556
300NA 88557RJLSEUS2022-030Ilex longipes Chapm. ex Trel. Alabama, United StatesNA2023COLLECTED12/12/2022Silver Creek Lake Campground off of Silver Creek Lake Road: woodland slopes below the hilltop parking lot leading down to the campground.31.66442800, -87.5746140039Part shade of moist-mesic, mixed deciduous and evergreen woodland on dry, well-drained bank, 1-2 meters above a small spring-fed creek. The underlying geology of this area is Claiborne Group, Tallahatta Formation, of Eocene origin, with white to very light-greenish-gray thin-bedded to massive siliceous claystone; interbedded with thin layers of fossiliferous clay, sandy clay, and glauconitic sand and sandstone. (Source: USGS Alabama Geological Map Data). The primary soil types in the collection area are classified as Arundel-Cantuche Complex soils (15 to 35 percent slopes). The Arundel Series consists of moderately deep, well drained, very slowly permeable soils on dissected uplands of the Southern Coastal Plain. They formed in marine deposits consisting of acid clays underlain by horizontally bedded sandstone, buhrstone and siltstone. These soils are strongly acid. Slopes range from 2 to 60 percent. The Cantuche Series consists of shallow, well drained, moderately permeable soils that formed over horizontally bedded claystone. These soils are on narrow ridgetops and narrow benches on steep side-slopes of dissected landscapes in the Coastal Plain. They are strongly acid. Slopes range from 2 to 35 percent. (Source: NRCS Web Soil Survey).Wild material2140818NA 88557
301NA 88559RJLSEUS2022-032Rhododendron colemanii R. F. Mill. Alabama, United StatesNA2023COLLECTED12/12/2022Plants 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, -87.4958950010Plants 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 material2140784NA 88559
302NA 88560RJLSEUS2022-033Hydrangea arborescens L. Alabama, United StatesNA2023COLLECTED12/12/2022Plants growing along the west side of Ferry Road at Haines Island Park leading down to the Alabama River.31.72299700, -87.4679820046Plants are growing in part-shade in the scoured ditch and slope alongside Ferry Road; occasionally in moss where seed undoubtedly germinated.
Soils: 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 (https://mrdata.usgs.gov/geology/state/state.php?state=AL)
The primary soil type in the collection area is classified as Arundel Loam soil (8 to 35 percent slopes). The Arundel Series consists of moderately deep, well drained, very slowly permeable soils on dissected uplands of the Southern Coastal Plain. They formed in marine deposits consisting of acid clays underlain by horizontally bedded sandstone, buhrstone and siltstone. These soils are strongly acid. Slopes range from 2 to 60 percent.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2140785NA 88560
303NA 88561RJLSEUS2022-034Hydrangea quercifolia W. Bartram Alabama, United StatesNA2023COLLECTED12/12/2022Plants growing in the woodlands at Haines Island Park at the foot of Tallahatta cuesta, accessed by foot via Ferry Road. Common at this site. 31.72178200, -87.4658960066Plants are growing in part-shade to shade of a moist mesic, well-drained conditions on rocks and in the eroding matrix of the Tallahatta Questa.
Soils: 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 (https://mrdata.usgs.gov/geology/state/state.php?state=AL)
The primary soil type in the collection area is classified as Arundel Loam soil (8 to 35 percent slopes). The Arundel Series consists of moderately deep, well drained, very slowly permeable soils on dissected uplands of the Southern Coastal Plain. They formed in marine deposits consisting of acid clays underlain by horizontally bedded sandstone, buhrstone and siltstone. These soils are strongly acid. Slopes range from 2 to 60 percent.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2140786NA 88561
304NA 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
305NA 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
306NA 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
307NA 88509RJL2022TX-004Ilex decidua Walter Texas, United StatesNA2022COLLECTED11/01/2022Low woodlands along the north side of Texas State Hwy 190 between the highway and an unnamed paved service road that leads down to the Sabine River; the turn for the service road is approximately 0.62 kilometers west of the Sabine River. Near the bridge over the Sabine River.30.74730000, -93.6156890020Plants are growing in part-shade to shade of a moist mesic (occasionally temporarily wet) woodland. Ilex decidua can be in the low woods most of the way down to the river. Plant is a common understory shrub in the moist woodland habitat not far from the Sabine River. Soils: The underlying geology of this area is of Holocene origin and characterized as Alluvium. The alluvium and low terrace deposits along streams include sand, silt, clay, and gravel. Thickness is variable. In this case alluvium is from the Sabine River. (Source: USGS Texas Geologic Map Data). The primary soil types in the collection area are classified as Urbo and Mantachie soils. The Urbo series consists of deep, somewhat poorly drained soils. Permeability is very slow. These nearly level to gently sloping soils formed in clayey alluvium on flood plains of streams that drain uplands of the Southern Coastal Plain. Slopes range from 0 to 3 percent. In wet seasons late in winter and early in spring, the water table is at a depth of 1 to 2 feet and most areas of Urbo soils are subject to either occasional or frequent flooding of brief to long duration. The Mantachie series consists of very deep, somewhat poorly drained, moderately permeable soils on flood plains of the Southern Coastal Plain. They formed in loamy alluvium and considered acidic. Mantachie soils are subject to rare to frequent flooding in the winter and early spring for brief to long duration, unless protected. The seasonal high water table ranges from 1.0 to 1.5 feet of the surface during periods of high rainfall. (Source: NRCS Web Soil Survey).Wild material2139816NA 88509
308NA 88511RJL2022TX-006Persea palustris (Raf.) Sarg. Texas, United StatesNA2022COLLECTED11/01/2022Plants growing in a wetland on the north side of Clarktown Road approximately 1.5 kilometers west of Texas State Hwy 87 in Sabine National Forest. Plant is common in the moist-wet and mesic edges of the wetland habitat where it is best adapted. 31.17114800, -93.7510620071Plants are growing in part-shade in a depression wetland of a small upland valley stream area surrounded by upland Pinus palustris and Pinus taeda forests. While the region had a severe drought during 2022, this depression wetland remained mucky wet throughout. Higher light conditions that supported heavy fruit production on the Persea may have been due to nearby harvesting of forest sections adjacent to the wetland.
Soils: 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 (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=TXQbs%3B0
The primary soil types in the collection area are classified as Letney soils. These soils consist of deep, somewhat excessively drained, moderately rapidly permeable soils on uplands. They were formed in thick loamy and sandy sediments on the Western Coastal Plain. The Letney soils are on gently sloping uplands with slopes ranging from 1 to 5 percent. They are typically strongly acidic. It should be noted that the upper surface, to an unknown depth has a significant amount of decomposed and undecomposed organic litter, presumably from sphagnum, at least, in part.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2139818NA 88511
309NA 88512RJL2022TX-007Morella caroliniensis (Mill.) Small Texas, United StatesNA2022COLLECTED11/01/2022Plants growing in a wetland on the north side of Clarktown Road approximately 1.5 kilometers west of Texas State Hwy 87 in Sabine National Forest. Plant is relatively common in the moist-wet and mesic edges of the wetland habitat.31.17181200, -93.7511800081Plants are growing in part-shade to part-sun in a depression wetland and slightly upslope of a small upland valley stream area surrounded by upland Pinus palustris and Pinus taeda forests. While the region had a severe drought during 2022, this depression wetland remained mucky wet throughout.
Soils: 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 (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=TXQbs%3B0
The primary soil types in the collection area are classified as Letney soils. These soils consist of deep, somewhat excessively drained, moderately rapidly permeable soils on uplands. They were formed in thick loamy and sandy sediments on the Western Coastal Plain. The Letney soils are on gently sloping uplands with slopes ranging from 1 to 5 percent. They are typically strongly acidic. It should be noted that the upper surface, to an unknown depth has a significant amount of decomposed and undecomposed organic litter, presumably from sphagnum, at least, in part.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2139819NA 88512
310NA 88513RJL2022TX-008Cephalanthus occidentalis L. Texas, United StatesNA2022COLLECTED11/01/2022Plants growing in moist sites on the north and south side of Clarktown Road approximately 0.5 kilometers west of Texas State Hwy 87 in Sabine National Forest. Plant is relatively common in the moist-wet and seasonally wet locations; absent elsewhere.31.17294500, -93.7413390092Plants are growing in part-shade to part-sun in moist-wet areas with low competition. The area generally retains moisture throughout the growing season.
Soils: 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 (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=TXQbs%3B0
The primary soil types in the collection area are classified as Mattex-Iulus complex soils. The Mattex series consists of very deep, somewhat poorly drained, slowly permeable, acidic loamy soils. They formed in loamy and clayey alluvium. These are nearly level soils on flood plains. Slopes range from 0 to 1 percent. The Iulus series consists of very deep, moderately well drained, moderately permeable, soils on flood plains. These soils formed in recent alluvium derived from coastal plain sediments, often containing fine sandy elements and are extremely acidic. The slope ranges from 0 to 1 percent.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2139820NA 88513
311NA 88514RJL2022MD-019Kalmia latifolia L. Maryland, United StatesNA2022COLLECTED11/04/2022Plants are growing on both sides of a fire road on Maryland Heights along the edge with Harpers Ferry National Historic Park. This location was accessed from the east where Miller Avenue meets the fire road, approximately 2 kilometers away. There is no vehicular access to the collecting area. Becoming locally uncommon. This local population is likely to be extirpated in the next 20-30 years. This collector has hiked through this area for more than 35 years and seen dramatic changes in the population. When first observed, Kalmia latifolia was a dominant understory shrub on south- to west-facing slopes beneath a mature forest canopy. Over the years, at least one forest fire has significantly reduced the population, along with a continuing increase in deer populations, resulting in catastrophic browse damage. The absence of a mature forest canopy and periods of drought have almost certainly also resulted in decline of this population. While collecting seed from scattered mature plants well above deer browse levels, this collector also noted that there was virtually no recruitment taking place.39.32811200, -77.72242400287Plants are growing in part-shade to shade of a deciduous upland, very rocky, and dry forest community. Plants are frequently found growing among boulders, rock outcrops, and steep-slope erosional areas, although, not exclusively.
Soils: The underlying geology of this area is of Late Cambrian to Cambrian origin and comprised of Chilhowee Group; Weverton Formation. This includes interbedded white to dark gray, thin-bedded, micaceous, ferruginous, and sericitic quartzites, phyllites, and white, thick-bedded, ledge-making quartzites; some gray to brown ferruginous quartz conglomerate and purple-banded phyllite.
Source: USGS Maryland Geologic Map Data https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=MDKp%3B5
The primary soil types in the collection area are classified as Dekalb-Bagtown-Rock outcrop complex, 25 to 65 percent slopes. The Dekalb series consists of moderately deep, excessively drained soils formed in material weathered from gray and brown acid sandstone in places interbedded with shale and graywacke. Slope ranges from 0 to 80 percent. Permeability is rapid. Solum thickness and depth to bedrock range from 50 to 100 cm. Flat, subangular or angular, sandstone fragments, 2.5-25 cm across increase with depth and range from 10-60 percent in individual horizons of the solum and from 50-90 percent or more in the C horizon. The amount of rock fragments typically increases with depth. Cobbly, channery, and very stony phases are common. Reaction ranges from extremely through strongly acid.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2139821NA 88514
312WLP 2676RJL2022NJ-007Kalmia latifolia L. New Jersey, United StatesNA2022COLLECTED10/24/2022Plants growing along Hawkins Bridge Road in Wharton State Forest. Plants are common and frequent throughout the woodlands at this location. 39.70292400, -74.5610680016Plants growing in a mixed Conifer-Broadleaved Evergreen-Deciduous dry to xeric forest habitat in part shade to shade.
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 Lakehurst sand, 0 to 5 percent slopes. Other related soils are found along the collection area; even so, this is the dominant soil in the collecting area of this species. This soil is primarily sandy coastal plain deposition that is moderately well-drained with limited organic matter in the upper horizon. This soil ranges in depth from 0.1-1.5 meters. It is very strongly acidic throughout. It is subject to periods of extreme drought.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2139667WLP 2676
313WLP 2675RJL2022NJ-006Kalmia angustifolia L. New Jersey, United StatesNA2022COLLECTED10/24/2022Plants growing along Hawkins Bridge Road in Wharton State Forest. Plants are common and frequent throughout the woodlands at this location. 39.70231900, -74.5608420016Plants growing in a mixed Conifer-Broadleaved Evergreen-Deciduous dry to xeric forest habitat in part shade to part sun.
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 Lakehurst sand, 0 to 5 percent slopes. Other related soils are found along the collection area; even so, this is the dominant soil in the collecting area of this species. This soil is primarily sandy coastal plain deposition that is moderately well-drained with limited organic matter in the upper horizon. This soil ranges in depth from 0.1-1.5 meters. It is very strongly acidic throughout. It is subject to periods of extreme drought.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2139666WLP 2675
314WLP 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
315NA 88499RJL2022MD-018Ilex opaca Aiton Maryland, United StatesNA2022COLLECTED10/22/2022Elk Neck State Park: woodlands along Maryland Hwy 272, Turkey Point Road.39.47706500, -75.9872090035Plants growing in shade to full sun on well-drained slopes of a mixed evergreen and deciduous woodland. Soils: The underlying geology of this area is the characterized as Upland Deposits (Eastern Shore) of Quaternary origin. This formation is characterized by gravel, sand, silt, and clay. Mostly cross-bedded, poorly sorted, medium- to coarse-grained white to red sand and gravel; boulders near base; minor pink and yellow silts and clays. The thickness of this formation ranges from 0 to 90 feet, locally thicker in paleochannels. (Source: USGS Maryland Geologic Map Data). The primary soil type in the area of this collection is classified as Sassafras and Croom soils, 15 to 25 percent slopes. These soils are typically fine-loamy, siliceous, semiactive, mesic typic hapludults that are strongly to extremely acid. The typical solum thickness ranges from 60-130 cm. These soils are generally well-drained. (Source: NRCS Web Soil Survey).Wild material2139662NA 88499
316WLP 2670RJL2022PA-016Acer negundo L. Pennsylvania, United StatesNA2022COLLECTED10/21/2022Plants growing in woodlands above a small unnamed creek that dumps into the Middle Branch White Clay Creek in Goddard Park, West Grove Pennsylvania, off of Wickerton Road, Chester County. Plants are found regularly but scattered in the understory of the woodlands. 39.80426000, -75.82609300105Plants growing in a mesic, well-drained habitat of deciduous woodlands along streams and above the riparian zone that drains toward a small unnamed creek that feeds into the Middle Branch White Clay Creek. Plants generally grow in part shade to full sun, but perform best and fruit more heavily in full sun where there is abundant access to moisture. The remnant woodlands exist mostly along the steep slopes, wetlands and seeps of seasonal and year-round creeks flowing into the Middle Branch White Clay Creek. The woodlands are bordered by numerous housing developments and land converted to meadows; hence there is significant first order edge that is heavily impacted by invasive plant intrusion. Despite this fact, Acer negundo is highly competitive and competes well.
Soils: The underlying geology of this area is the Glenarm Wissahickon Formation of lower Paleozoic origin and lithologically similar to oligoclase-mica schist of the Wissahickon Formation (PZw), but also includes lenticular amphibolite bodies having ocean-floor basalt chemistry.
Source: USGS Pennsylvania Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=PAPZgw%3B0)
The primary soil type in the area of this collection is classified as Glenelg silt loam, 3 to 8 percent slopes. This series consists of very deep, well drained soils formed in residuum weathered from micaceous schist on uplands of the Blue Ridge and the Northern Piedmont. Saturated hydraulic conductivity is moderately high in the subsoil and moderately high to high in the substratum. This upper horizon of this soil is undifferentiated, mostly poorly drained sandy bottomland soils intermingled with decomposing organic litter and eroded silts and clays due to erosion.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2139661WLP 2670
317WLP 2669RJL2022NJ-001Rhododendron viscosum (L.) Torr. New Jersey, United StatesNA2022COLLECTED10/19/2022Plants growing near the confluence of Springers Brook and Mullica River in Wharton State Forest around wetlands and associated woodlands accessed off of an unnamed road from Stokes Road. Plants are common but scattered on the edges and in the understory of low-lying wet woodlands. 39.72857100, -74.677982007Plants are growing in part-shade to shade of mixed deciduous and evergreen forests on moist slopes to occasionally wet low-lying areas fed by Springers Brook.
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 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 Fluvaquents, sandy, 0 to 3 percent slopes, frequently flooded. This soil is primarily stratified, wet soils on flood plains and deltas of middle and low latitudes. The stratification reflects deposition of sediments under changing currents and in shifting channels. The depth of this soil is approximately 5 meters and are consider very poorly drained; they are considered wet to inundated year-round.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2139660WLP 2669
318WLP 2668RJL2022MD-014Aronia arbutifolia (L.) Pers. Maryland, United StatesNA2022COLLECTED10/05/2022Plant growing at Elkton State Forest along road in wet woodlands near the Elk Neck State Forest Shooting Range labelled as the address of 717 Irishtown Rd, North East, MD 21901. Plant is uncommon at this site. 39.58716100, -75.9141900055Plants are growing in part-shade to part sun of a deciduous forest on hummocks in a very moist to wet low-lying area along a seasonal or year-round flowing seep.
Soils: The underlying geology of this area is of Cretaceous origin and comprised of Potomac Group, including Raritan and Patapsco Formations, and Patuxent Formation. The Potomac Group includes: interbedded quartzose gravels; proto-quartzitic to orthoquartzitic argillaceous sands; and white, dark gray, and multicolored silts and clays. Included withing this zone are Raritan and Patapsco Formations comprised of gray, brown, and red variegated silts and clays; lenticular, cross-bedded, argillaceous, subrounded sands; minor gravels; thickness. The Patuxent Formation is also interbedded in this zone and comprised of white or light gray to orange-brown, moderately sorted, cross-bedded, argillaceous, angular sands and subrounded quartz gravels; silts and clays subordinate that are predominantly pale gray.
Source: USGS Maryland Geologic Map Data https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=MDKp%3B5
The primary soil types in the collection area are classified as Russett-Christiana-Hambrook Complex and/or Sassafras and Croom Soils; though, others may intersect and overlay in specific areas. The soils in the collecting 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.).
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2139659WLP 2668
319NA 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
320NA 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
321NA 89043RJL2022MD-017Cephalanthus occidentalis L. Maryland, United StatesNA2022COLLECTED10/05/2022Plants growing at Elkton State Forest along road and in wet woodlands near the Elk Neck State Forest Shooting Range labelled as the address of 717 Irishtown Rd, North East, MD 21901. Plants are locally common but restricted to the low-lying wet woodlands. 39.58727700, -75.9140390055Plants are growing in part-shade to part-sun of deciduous forests on hummocks in very moist to wet low-lying areas along seasonal or year-round flowing seeps.
Soils: The underlying geology of this area is of Cretaceous origin and comprised of Potomac Group, including Raritan and Patapsco Formations, and Patuxent Formation. The Potomac Group includes: interbedded quartzose gravels; proto-quartzitic to orthoquartzitic argillaceous sands; and white, dark gray, and multicolored silts and clays. Included withing this zone are Raritan and Patapsco Formations comprised of gray, brown, and red variegated silts and clays; lenticular, cross-bedded, argillaceous, subrounded sands; minor gravels; thickness. The Patuxent Formation is also interbedded in this zone and comprised of white or light gray to orange-brown, moderately sorted, cross-bedded, argillaceous, angular sands and subrounded quartz gravels; silts and clays subordinate that are predominantly pale gray.
Source: USGS Maryland Geologic Map Data https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=MDKp%3B5
The primary soil types in the collection area are classified as Russett-Christiana-Hambrook Complex and/or Sassafras and Croom Soils; though, others may intersect and overlay in specific areas. The soils in the collecting 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.).
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2139608NA 89043
322NA 89042RJL2022MD-016Aronia ×prunifolia (Marshall) Rehder Maryland, United StatesNA2022COLLECTED10/05/2022Plants growing at Elkton State Forest along road and in wet woodlands near the Elk Neck State Forest Shooting Range labelled as the address of 717 Irishtown Rd, North East, MD 21901. Plants are infrequent and were found in this one area of low-lying wet woodlands. Perhaps others would have been found upon investigation of other similar habitats.39.58730200, -75.9141580055Plants are growing in part-sun to part-shade of deciduous forests on moist slopes and on hummocks in very moist to wet low-lying areas along seasonal or year-round flowing seeps.
Soils: The underlying geology of this area is of Cretaceous origin and comprised of Potomac Group, including Raritan and Patapsco Formations, and Patuxent Formation. The Potomac Group includes: interbedded quartzose gravels; proto-quartzitic to orthoquartzitic argillaceous sands; and white, dark gray, and multicolored silts and clays. Included withing this zone are Raritan and Patapsco Formations comprised of gray, brown, and red variegated silts and clays; lenticular, cross-bedded, argillaceous, subrounded sands; minor gravels; thickness. The Patuxent Formation is also interbedded in this zone and comprised of white or light gray to orange-brown, moderately sorted, cross-bedded, argillaceous, angular sands and subrounded quartz gravels; silts and clays subordinate that are predominantly pale gray.
Source: USGS Maryland Geologic Map Data https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=MDKp%3B5
The primary soil types in the collection area are classified as Russett-Christiana-Hambrook Complex and/or Sassafras and Croom Soils; though, others may intersect and overlay in specific areas. The soils in the collecting 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.).
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2139607NA 89042
323NA 89041RJL2022MD-015Lyonia ligustrina (L.) DC. Maryland, United StatesNA2022COLLECTED10/05/2022Plants growing at Elkton State Forest along road and in wet woodlands near the Elk Neck State Forest Shooting Range labelled as the address of 717 Irishtown Rd, North East, MD 21901. Plants are common but scattered on the edges and in the understory of low-lying wet woodlands. 39.58716100, -75.9141900055Plants are growing in part-shade to shade of deciduous forests on moist slopes and on hummocks in very moist to wet low-lying areas along seasonal or year-round flowing seeps.
Soils: The underlying geology of this area is of Cretaceous origin and comprised of Potomac Group, including Raritan and Patapsco Formations, and Patuxent Formation. The Potomac Group includes: interbedded quartzose gravels; proto-quartzitic to orthoquartzitic argillaceous sands; and white, dark gray, and multicolored silts and clays. Included withing this zone are Raritan and Patapsco Formations comprised of gray, brown, and red variegated silts and clays; lenticular, cross-bedded, argillaceous, subrounded sands; minor gravels; thickness. The Patuxent Formation is also interbedded in this zone and comprised of white or light gray to orange-brown, moderately sorted, cross-bedded, argillaceous, angular sands and subrounded quartz gravels; silts and clays subordinate that are predominantly pale gray.
Source: USGS Maryland Geologic Map Data https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=MDKp%3B5
The primary soil types in the collection area are classified as Russett-Christiana-Hambrook Complex and/or Sassafras and Croom Soils; though, others may intersect and overlay in specific areas. The soils in the collecting 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.).
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2139606NA 89041
324NA 89040RJL2022MD-013Eubotrys racemosus (L.) Nutt. Maryland, United StatesNA2022COLLECTED10/05/2022Plants growing at Elkton State Forest along road and in wet woodlands over a distance of about 0.55 kilometers near the Elk Neck State Forest Shooting Range labelled as the address of 717 Irishtown Rd, North East, MD 21901. Plants are common but scattered on the edges and in the understory of low-lying wet woodlands. 39.58227200, -75.9132880057Plants are growing in part-shade to shade of deciduous forests on moist slopes and on hummocks in very moist to wet low-lying areas along seasonal or year-round flowing seeps.
Soils: The underlying geology of this area is of Cretaceous origin and comprised of Potomac Group, including Raritan and Patapsco Formations, and Patuxent Formation. The Potomac Group includes: interbedded quartzose gravels; proto-quartzitic to orthoquartzitic argillaceous sands; and white, dark gray, and multicolored silts and clays. Included withing this zone are Raritan and Patapsco Formations comprised of gray, brown, and red variegated silts and clays; lenticular, cross-bedded, argillaceous, subrounded sands; minor gravels; thickness. The Patuxent Formation is also interbedded in this zone and comprised of white or light gray to orange-brown, moderately sorted, cross-bedded, argillaceous, angular sands and subrounded quartz gravels; silts and clays subordinate that are predominantly pale gray.
Source: USGS Maryland Geologic Map Data https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=MDKp%3B5
The primary soil types in the collection area are classified as Russett-Christiana-Hambrook Complex and/or Sassafras and Croom Soils; though, others may intersect and overlay in specific areas. The soils in the collecting 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.).
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2139605NA 89040
325NA 89033RJL2022MD-010Clethra alnifolia L. Maryland, United StatesNA2022COLLECTED09/15/2022Plants growing in low woodlands at the end of Greenway Avenue near a boat dock that leads to the Pocomoke River, adjacent to Winter Quarters Golf Course, Pocomoke City. Plants common throughout the wetland area as well as mesic edges of the woodlands.38.08305100, -75.56527800Plants growing in the flood plain of the Pocomoke River in shade to part sun of a mixed deciduous and evergreen bottomland habitat about 10 meters from the edge of the golf course fairway. The habitat is a mucky swamp edge habitat next to the Pocomoke River, most of which seems wet year-round and grades slightly upslope to more mesic conditions.
The underlying geology of this area is comprised of Quaternary Deposits of Wisconsin to Holocene origin. The composition is primarily undifferentiated gray to buff sand and gravel, gray to brown lignitic silt and clay, occasional boulders, and rare shell beds. Surficial deposits occur as shell-bearing estuarine clays and silts.
Source: USGS Maryland Geologic Map Data https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=MDQdu%3B5
The surface soil profile of this habitat is classified as Puckum Muck which is frequently flooded. These highly saturated soils are found in flats, depressions and swales. The soil reaction of Puckum Muck is extremely acid to strongly acid throughout the profile. The depth to bedrock is generally greater than 150 cm. Wood fragments comprise 0-25%, by volume of the Puckum Muck throughout the profile which includes mostly twigs, branches, logs, or stumps and are 1.5-30 cm in diameter. The composition of these highly saturated soils, are classified as muck (sapric soil material) or mucky peat (hemic soil material) throughout most of the upper 150 cm and may contain thin layers of mucky silt loam, silty clay loam, sandy loam and/or sand.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2139598NA 89033
326NA 89032RJL2022MD-009Rhododendron viscosum (L.) Torr. Maryland, United StatesNA2022COLLECTED09/15/2022Plants growing in low woodlands at the end of Greenway Avenue near a boat dock that leads to the Pocomoke River, adjacent to Winter Quarters Golf Course, Pocomoke City. Plants scattered throughout the wetland area. Infrequent, but regularly found. 38.08235200, -75.565665001Plants growing in the flood plain of the Pocomoke River in part shade to shade of a mixed deciduous and evergreen bottomland habitat about 10 meters from the edge of the golf course fairway. The habitat is a mucky swamp edge habitat next to the Pocomoke River, most of which seems wet year-round.
The underlying geology of this area is comprised of Quaternary Deposits of Wisconsin to Holocene origin. The composition is primarily undifferentiated gray to buff sand and gravel, gray to brown lignitic silt and clay, occasional boulders, and rare shell beds. Surficial deposits occur as shell-bearing estuarine clays and silts.
Source: USGS Maryland Geologic Map Data https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=MDQdu%3B5
The surface soil profile of this habitat is classified as Puckum Muck which is frequently flooded. These highly saturated soils are found in flats, depressions and swales. The soil reaction of Puckum Muck is extremely acid to strongly acid throughout the profile. The depth to bedrock is generally greater than 150 cm. Wood fragments comprise 0-25%, by volume of the Puckum Muck throughout the profile which includes mostly twigs, branches, logs, or stumps and are 1.5-30 cm in diameter. The composition of these highly saturated soils, are classified as muck (sapric soil material) or mucky peat (hemic soil material) throughout most of the upper 150 cm and may contain thin layers of mucky silt loam, silty clay loam, sandy loam and/or sand.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2139597NA 89032
327W6 60826W6 60826Microseris nutans (Hook.) Sch. Bip. Idaho, United StatesW6SEED2022Wild materialPetals yellow Young flower buds nodding 2139401W6 60826
328NA 88481RJL2022MD-002Kalmia latifolia L. Maryland, United StatesNA2022COLLECTED09/04/2022Plants growing at Elkton State Forest along roads and woodlands over a distance of approximately 5 kilometers labelled as the address of 717 Irishtown Rd, North East, MD 21901. Kalmia is very common along the unnamed gravel road as well as the understory of the upland woodlands.39.58852900, -75.9045290060Plants are growing in a mesic to dry, well-drained habitat of mixed deciduous and evergreen woodlands comprised primarily of acid-loving plants. Plants are growing in shade to part shade along the unnamed road as well as the woodlands. The soils in the collection area are generally described as a complex series of fluviomarine deposits. The soils range from a thin loam layer at the surface to varying levels of loam to sandy loam and/or extremely gravelly sandy clay loam strata, depending upon geographical location (ie. Hillslope summits, slopes, footslopes, swales, etc.). The primary soil types in the collection area are classified as Russett-Christiana-Hambrook Complex and/or Sassafras and Croom Soils; though, others may intersect and overlay in specific areas.Wild material2139360NA 88481
329NA 88482RJL2022MD-003Rhododendron periclymenoides (Michx.) Shinners Maryland, United StatesNA2022COLLECTED09/04/2022Plants growing at Elkton State Forest along roads and woodlands over a distance of approximately 5 kilometers labelled as the address of 717 Irishtown Rd, North East, MD 21901. Plants are found infrequently and scattered along the unnamed gravel road39.58852900, -75.9045290051Plants are growing in a mesic to dry, well-drained habitat of mixed deciduous and evergreen woodlands comprised primarily of acid-loving plants. Plants are growing in part shade. The soils in the collection area are generally described as a complex series of fluviomarine deposits. The soils range from a thin loam layer at the surface to varying levels of loam to sandy loam and/or extremely gravelly sandy clay loam strata, depending upon geographical location (ie. Hillslope summits, slopes, footslopes, swales, etc.). The primary soil types in the collection area are classified as Russett-Christiana-Hambrook Complex and/or Sassafras and Croom Soils; though, others may intersect and overlay in specific areas.Wild material2139361NA 88482
330NA 88483RJL2022MD-004Clethra alnifolia L. Maryland, United StatesNA2022COLLECTED09/04/2022Plants growing at Elkton State Forest along roads and woodlands over a distance of approximately 5 kilometers labelled as the address of 717 Irishtown Rd, North East, MD 21901. Plants are found regularly but scattered along the unnamed gravel road as well as in open understory of the upland woodlands. 39.58531200, -75.8956610047Plants are growing in a mesic to moist, well-drained habitat of mixed deciduous and evergreen woodlands comprised primarily of acid-loving plants. Plants are growing in part shade and open understory shade. The soils in the collection area are generally described as a complex series of fluviomarine deposits. The soils range from a thin loam layer at the surface to varying levels of loam to sandy loam and/or extremely gravelly sandy clay loam strata, depending upon geographical location (ie. Hillslope summits, slopes, footslopes, swales, etc.). The primary soil types in the collection area are classified as Russett-Christiana-Hambrook Complex and/or Sassafras and Croom Soils; though, others may intersect and overlay in specific areas.Wild material2139362NA 88483
331NA 88484RJL2022MD-005Aronia melanocarpa (Michx.) Elliott Maryland, United StatesNA2022COLLECTED09/04/2022Plants growing at Elkton State Forest on Elk Neck Trail #3 (Starkey Lane) labelled as the address of 717 Irishtown Rd, North East, MD 21901. This was the only plant observed during several visits to Elk Neck State Forest during early and mid-summer39.58531200, -75.8956610055Plants are growing in a mesic to dry, well-drained habitat of mixed deciduous and evergreen woodlands comprised primarily of acid-loving plants. Plants are growing in part shade to part-sun. The soils in the collection area are generally described as a complex series of fluviomarine deposits. The soils range from a thin loam layer at the surface to varying levels of loam to sandy loam and/or extremely gravelly sandy clay loam strata, depending upon geographical location (ie. Hillslope summits, slopes, footslopes, swales, etc.). The primary soil types in the collection area are classified as Russett-Christiana-Hambrook Complex and/or Sassafras and Croom Soils; though, others may intersect and overlay in specific areas.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild materialreceived as A. prunifolia, on further examination by collector it was determined to be A. melanocarpa2139363NA 88484
332NA 88485RJL2022MD-006Hamamelis virginiana L. Maryland, United StatesNA2022COLLECTED09/04/2022Plants growing at Elkton State Forest on Elk Neck Trail #3 (Starkey Lane) labelled as the address of 717 Irishtown Rd, North East, MD 21901. This species was infrequent throughout most of Elk Neck State Park, but relatively common.39.58790000, -75.8885310054Plants are growing in a mesic to dry, well-drained habitat of mixed deciduous and evergreen woodlands comprised primarily of acid-loving plants. Plants are growing in part shade to shade. The soils in the collection area are generally described as a complex series of fluviomarine deposits. The soils range from a thin loam layer at the surface to varying levels of loam to sandy loam and/or extremely gravelly sandy clay loam strata, depending upon geographical location (ie. Hillslope summits, slopes, footslopes, swales, etc.). The primary soil types in the collection area are classified as Russett-Christiana-Hambrook Complex and/or Sassafras and Croom Soils; though, others may intersect and overlay in specific areas.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2139364NA 88485
333NA 88488RJL2022PA-004Viburnum acerifolium L. Pennsylvania, United StatesNA2022COLLECTED09/03/2022Plants growing in woodlands on the east side of Shed Road in French Creek State Park. Plants are common and found scattered along the edges of the road and into the woodlands. 40.21969200, -75.77373600238Plants are growing in a mesic to dry, well-drained habitat of upland deciduous forest which is very rocky. The understory layer is generally not as rich due to the rock-laden ground layer. Plants are growing in part shade to shade. The underlying geology of this area is comprised of Hammer Creek Conglomerate, characterized by cobble and pebble quartz conglomerate interbedded with red sandstone.
Source: USGS Pennsylvania Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=PATRhc%3B2) The surface soil profile of this area is Joanna Loam (JpD), 8 to 25 percent slopes which is extremely stony. It is represented by residuum weathered from sandstone and/or residuum weathered from conglomerate. Joanna Loam is moderately to well-drained and 1.8 meters to 2.5 meters to the lithic bedrock described above.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2139367NA 88488
334NA 88489RJL2022PA-005Kalmia latifolia L. Pennsylvania, United StatesNA2022COLLECTED09/10/2022Plants are growing on the lands of Hawk Mountain Sanctuary. This species is very common and abundant. It is one of the most dominant understory plants in woodlands. This species is a common understory shrub throughout the entire region in upland dry woodland habitats.40.63862000, -75.99071200430Plants are growing primarily in shade to part-shade on a dry-mesic to very dry, well-drained upland/montane habitat characterized by upland mixed deciduous and evergreen forest that is very rocky. All of the plants found in this habitat go through periods of drought during the growing season due to the limited litter/soil layer in which moisture can be held. The underlying geology of this area is of Silurian origin and comprised of Shawangunk Formation. This formation is primarily light- to dark-gray, fine- to very coarse-grained sandstone and conglomerate containing thin shale interbeds.
Source: USGS Pennsylvania Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=PASs%3B14)
The surface soil profile of this area is the Hazleton series consists of deep and very deep, well drained soils formed in residuum of acid gray, brown or red sandstone on uplands. The matrix includes a considerable accumulation of thin, flat, coarse fragments of sandstone, limestone, or schist with diameters up to 15 cm. Slope ranges from 0-80%. Permeability is moderately rapid to rapid.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2139368NA 88489
335NA 88490RJL2022PA-006Ilex montana Torr. & A. Gray Pennsylvania, United StatesNA2022COLLECTED09/10/2022Hawk Mountain Sanctuary.40.64162200, -75.99122600420Plants are growing from shade to full sun on a dry-mesic to very dry, well-drained upland/montane habitat characterized by an upland mixed deciduous and evergreen forest that is very rocky. All of the plants found in this habitat go through periods of drought during the growing season due to the limited litter/soil layer in which moisture can be held. The underlying geology of this area is of Silurian origin and comprised of Shawangunk Formation. This formation is primarily light- to dark-gray, fine- to very coarse-grained sandstone and conglomerate containing thin shale interbeds. (Source: USGS Pennsylvania Geologic Map Data). The surface soil profile of this area is the Hazleton series consists of deep and very deep, well drained soils formed in residuum of acid gray, brown or red sandstone on uplands. The matrix includes a considerable accumulation of thin, flat, coarse fragments of sandstone, limestone, or schist with diameters up to 15 cm. Slope ranges from 0-80%. Permeability is moderately rapid to rapid. (Source: NRCS Web Soil Survey).Wild material2139369NA 88490
336NA 88491RJL2022PA-007Rhododendron maximum L. Pennsylvania, United StatesNA2022COLLECTED09/10/2022Plants are growing on the lands of Hawk Mountain Sanctuary. This species was common, but generally restricted to steep rocky outcrops.40.63813900, -75.98835200420Plants are growing from shade to full sun on a dry-mesic to very dry, well-drained upland/montane habitat characterized by an upland mixed deciduous and evergreen forest that is very rocky. Even so, most heavily fruited plants were growing in part shade to almost full sun. All of the plants found in this habitat go through periods of drought during the growing season due to the limited litter/soil layer in which moisture can be held. The underlying geology of this area is of Silurian origin and comprised of Shawangunk Formation. This formation is primarily light- to dark-gray, fine- to very coarse-grained sandstone and conglomerate containing thin shale interbeds.
Source: USGS Pennsylvania Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=PASs%3B14)
The surface soil profile of this area is the Hazleton series consists of deep and very deep, well drained soils formed in residuum of acid gray, brown or red sandstone on uplands. The matrix includes a considerable accumulation of thin, flat, coarse fragments of sandstone, limestone, or schist with diameters up to 15 cm. Slope ranges from 0-80%. Permeability is moderately rapid to rapid.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2139370NA 88491
337Ames 35877Gallagher FenSalix myricoides Muhl. Ohio, United StatesNC7LEAF2022COLLECTED06/28/2022Gallagher Fen State Nature Preserve located just east, northeast of Springfield approximately 4.5 miles, T5E R9N NE 1/4 NE 1/4 Sec. 1139.93209100, -83.72390500307Remnant wetland occurring primarily where the marl meadow meets the stream and marl mud flats.Wild materialBayberry willow is native to areas of the northeastern U.S. and north into Canada, localized around the Great Lakes region. Known to occur on shorelines/dunes but also in swamps, fens, and on talus (Haines 2004) with the potential to reach six meters in height (Dorn 1995). Ornamental characteristics include glaucous lower leaf blades that appear chalky white. This disjunct population was sampled in southwestern Ohio (Gallagher Fen) where the species is currently (2022) designated as a potentially threatened species in the state. Specimens observed in nature were low, mounding shrubs measuruing 16-24" (40-60 cm) tall; stems were slender, red and glossy with prominent lenticles; bud scales red, darkening following opening; flowers on staminate individuals with dense whitish bracts opening to reveal stamens tipped with bright yellow anthers and pistillate flowers with pale green pistils tipped with paler stigmas. 2138175Ames 35877
338WLP 2576RJL2022-001Amelanchier arborea (F. Michx.) Fernald Maryland, United StatesNA2022COLLECTED05/25/2022Plants growing in open woodlands and part shade along unnamed Elkton State Forest gravel road over a distance of approximately 5 kilometers labelled as the address of 717 Irishtown Rd, North East, MD 21901.39.58089500, -75.9150590073Plants are found regularly but scattered along the unnamed gravel road as well as in open understory of the upland woodlands. Plants growing in a mesic to dry, well-drained habitat of mixed deciduous and evergreen woodlands comprised primarily of acid-loving plants. Plants are growing in part shade and open understory shade. The soils in the collection area are generally described as a complex series of fluviomarine deposits. The soils range from a thin loam layer at the surface to varying levels of loam to sandy loam and/or extremely gravelly sandy clay loam strata, depending upon geographical location (ie. Hillslope summits, slopes, footslopes, swales, etc.). The primary soil types in the collection area are classified as Russett-Christiana-Hambrook Complex and/or Sassafras and Croom Soils; though, others may intersect and overlay in specific areas.Wild material2138095WLP 2576
339OPGC 8607FS0417-18Arnica chamissonis Less. Nevada, United StatesOPGC2022Wild materialMost plants in population done flowering (~90% done). Green, lightly fuzzy leaves and stems. Leaves opposite and alternate with a deep midvein. Usually 1-4 flowers per plant.2138336OPGC 8607
340W6 60651NV030-1548Poa palustris L. California, United StatesW6SEED2022Wild materialLeaf blades are in-rolled, 1--2 mm wide when flat. Inflorescence are 2-10 cm, spikelet stalk scabrous, with lemma tip acute, margin near tip entire, lowest lemma 2 mm.2138770W6 60651
341W6 60652NV030-1549Poa compressa L. California, United StatesW6SEED2022Wild materialPerennial grass, 1-2 ft. tall. Flattened stem, spikelets short stalked and oblong. Strongly keeled with lemma webbed at base.2138771W6 60652
342Ames 35805Rippey RR ROWSalix humilis Marshall var. tristis (Aiton) Griggs Iowa, United StatesNC7FRUIT2022COLLECTED05/12/2022Located 3.27 miles southeast of Rippey along east side of highway 144, T82N R28W NW ¼ SW ¼ Sec. 19.41.89609800, -94.16247600284Xeric prairie remnant. Railroad right of way.Wild materialPlants in nature measuring approximately 3.0-3.5' in height. Specimens noted during peak flowering and seed dispersal on 12 April and 3 May (2021), respectively. Normally for central Iowa peak flowering and fruiting occurs in late April and mid-May, respectively.2137911Ames 35805
343Ames 35803Turtlehead FenSalix eriocephala Michx. Iowa, United StatesNC7FRUIT2022COLLECTED04/21/2022Turtlehead Fen (Chichaqua Bottoms Greenbelt) located 1.75 miles southeast of Farrar just north of highway 65, T81N R21W SW ¼ NW ¼ Sec. 31.41.78612100, -93.34726000290Extremely high-quality remnant fen. Extremely wet, spongy soils with surface water visible at time of collection.Wild materialPlants in nature averaging 20' in height. Bright red buds on nearly all genotypes with stem colors ranging from yellow/bronze, brownish-green, brown and green at time of sampling (21 April 2022). Some specimens are rather open, wide spreading and some are rather upright. Salix eriocephala at this site is one of the more dominant species of willow.2137909Ames 35803
344OPGC 8529NEWFS-728Persicaria sagittata (L.) H. Gross New Hampshire, United StatesOPGC2021Wild materialWhite, pink, globular inflorescences at termil end of stem. Arrow head shaped leaves, small sharp rows of spines on underside of stem.2138822OPGC 8529
345OPGC 8559NEWFS-891Verbena hastata L. Massachusetts, United StatesOPGC2021Wild materialSquare stem. upright plant with long dense pencil shaped spikes, tubular flowers purple and characteristically blooming in a ring from bottom to top toothed lanceolate leaves.2138914OPGC 8559
346W6 60179NEWFS-702Juncus effusus L. Massachusetts, United StatesW62021Wild materialRounded stem like bract rising above inflorescence of multiple peduncled capsules holding tiny achenes.2138805W6 60179
347W6 60193NEWFS-725Rhynchospora alba (L.) Vahl New Hampshire, United StatesW62021Wild materialBrown, termil inflorescence in spiky, rounded bulb.2138819W6 60193
348W6 60194NEWFS-726Triadenum virginicum (L.) Raf. New Hampshire, United StatesW62021Wild materialRed burgundy to brown seed capsule with three locules, each filled with numerous tiny brown seeds white when immature, leaves round opposite and sessile.2138820W6 60194
349W6 60195NEWFS-727Dulichium arundinaceum (L.) Britton New Hampshire, United StatesW62021Wild materialReceived as: Dulichium arundiceum. 3 ranked leaves with the inflorescences fruits branching from the axil.2138821W6 60195
350W6 60197NEWFS-729Scirpus atrovirens Willd. New Hampshire, United StatesW62021Wild materialTightly clumped termil inflorescences.2138823W6 60197
351W6 60290NEWFS-893Lycopus americanus Muhl. ex W. P. C. Barton Massachusetts, United StatesW62021Wild materialDistinctly and irregularly lobed opposite leaves, white tubular flowers clustered around the axil.2138916W6 60290
352W6 60173NEWFS-695Juncus effusus L. Rhode Island, United StatesW62021Wild materialRounded stem like bract rising above inflorescence of multiple peduncled capsules holding tiny achenes 2137258W6 60173
353OPGC 8496NCBG-262Typha latifolia L. Virginia, United StatesOPGC2021Wild materialWide leaf blades.2132863OPGC 8496
354W6 60049NCBG-591Paspalum boscianum Flüggé Maryland, United StatesW62021Wild material2132930W6 60049
355W6 60081MARSB-137Hudsonia tomentosa Nutt. New York, United StatesW62021Wild materialFlowers yellow remain folded into stem. Seed heads light brown. Leaves light bluish green, are also folded into stem.2137166W6 60081
356W6 60107NEWFS-336Scirpus atrovirens Willd. Rhode Island, United StatesW62021Wild material2137192W6 60107
357W6 60108NEWFS-337Juncus effusus L. Rhode Island, United StatesW62021Wild material2137193W6 60108
358W6 60129NEWFS-452Eriophorum virginicum L. Maine, United StatesW62021Wild material2137214W6 60129
359WLP 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
360NA 88328CBG-10698Hypericum kalmianum L. Illinois, United StatesNA2021Wild material2132546NA 88328
361OPGC 8486CBG-10697Lysimachia quadriflora Sims Illinois, United StatesOPGC2021Wild material2132545OPGC 8486
362W6 59934CBG-10657Calamagrostis canadensis (Michx.) P. Beauv. Illinois, United StatesW62021Wild material2132513W6 59934
363W6 59949CBG-10674Triglochin maritima L. Illinois, United StatesW6SEED2021Wild material2132527W6 59949
364W6 59951CBG-10677Juncus canadensis J. Gay ex Laharpe Illinois, United StatesW62021Wild material2132529W6 59951
365W6 59962CBG-10692Juncus alpinoarticulatus Chaix Illinois, United StatesW62021Wild material2132540W6 59962
366W6 59940CBG-10663Eleocharis elliptica Kunth Illinois, United StatesW6SEED2021Wild material2132813W6 59940
367OPGC 7576McFarland ParkSolidago flexicaulis L. Iowa, United StatesOPGCFlower2021COLLECTED09/26/2021McFarland Park just north, northeast of Ames, T84N R23W Sec. 742.09667500, -93.57083500288Moist areas near streambanks and bottomlands in hardwood forest understory.Wild materialPlants in nature ranged in height from approximately one to three feet, growing as spreading clumps. Peak flowering in 2021 occurred near 18 September.2132830OPGC 7576
368W6 59598CO932-406Elymus elymoides (Raf.) Swezey Colorado, United StatesW62021Wild materialinflorescence: purple at tips, green at base, culms erect to spreading; blades: flat to slightly rolled2120764W6 59598
369W6 59607CO932-415Elymus elymoides (Raf.) Swezey Colorado, United StatesW62021Wild materialCulms erect to spreading, sheaths open, glabrous to pubescent, purplish, blades flat to folded to in-rolled, ascending, inflorescence compact to open, entire rachis disarticulate, fading to straw2120773W6 59607
370W6 59649UT020-91Poa secunda J. Presl Utah, United StatesW62021Wild materialPerennial bunchgrass with narrow panicle inflorescence, growing in tufts with a reddish tint or golden hue to stems. Plants in this population were relatively tall for Sandberg Bluegrass in the West Desert of Utah, since they were growing in a wet mountain meadow. Poa secunda was the dominant grass in the small area where we collected.2120814W6 59649
371Ames 36061CBG-10739Linum medium (Planch.) Britton Illinois, United StatesNC7SEED2021Wild material2137990Ames 36061
372Ames 35736Horn Prairie Early BloomingMonarda fistulosa L. Illinois, United StatesNC7FLOWER2021COLLECTED08/27/2021Horn Prairie Grove located 3.91 miles east, southeast of Ramsey, T8N R1E SE ¼ SW ¼ Sec. 1339.12960100, -89.03759800166Very diverse remnant prairie.Wild materialAccession represents an “early” flowering variant of Monarda fistulosa. Majority of specimens noted have pubescent stems and leaves; peaking flower on 6 June (2021); and measuring 34-36" in height. Generally found in more open, drier habitats in comparison to the “late” flowering more typical form of Monarda fistulosa. Majority of the “late” variants noted at the same locality (Ames 35737) have glabrous stems and leaves; measuring 4-4.5’ in height; peaking flower approximately five weeks later; and typically found in slightly wetter habitats. 2120340Ames 35736
373Ames 35737Horn Prairie Late BloomingMonarda fistulosa L. Illinois, United StatesNC7Shoot2021COLLECTED08/27/2021Horn Prairie Grove located 3.91 miles east, southeast of Ramsey, T8N R1E SE ¼ SW ¼ Sec. 1339.12913900, -89.03924000166Very diverse remnant prairie.Wild materialAccession represents genetics from the typical form of M. fistulosa at the collection site. Majority of the specimens sampled display the typical morphological characters of the species including glabrous stems and leaves; measuring 4-4.5’ in height; peaking flower approximately 10 July (2021); and at the collection site typically, in slightly wetter habitats. Majority of the “early” variants noted at the same locality (Ames 35736) have pubescent stems and leaves; peaking flower on 6 June (2021); measuring 3’ in height or less; and are typically found in more open, drier habitats. 2120341Ames 35737
374W6 60355CBG-10735Juncus nodosus L. Illinois, United StatesW6SEED2021Wild material2137987W6 60355
375Ames 36062CBG-10584Linum sulcatum Riddell Illinois, United StatesNC72021Wild materialPlant numbers sampled estimated.2120175Ames 36062
376NA 88287CBG-10561Cephalanthus occidentalis L. Illinois, United StatesNA2021Wild materialPlant numbers sampled estimated.2120156NA 88287
377NA 88326CBG-10490Hypericum gentianoides (L.) Britton et al. Illinois, United StatesNA2021Wild material2120115NA 88326
378NA 88327CBG-10491Hypericum gentianoides (L.) Britton et al. Illinois, United StatesNA2021Wild material2120116NA 88327
379NA 88330CBG-10583Hypericum mutilum L. Illinois, United StatesNA2021Wild materialPlant numbers sampled estimated.2120174NA 88330
380NA 88439CBG-10597Rosa setigera Michx. Illinois, United StatesNA2021Wild materialPlant numbers sampled estimated.2120182NA 88439
381OPGC 8277CBG-9703Pedicularis canadensis L. Illinois, United StatesOPGC2021Wild materialplant habit: forb2120016OPGC 8277
382OPGC 8281CBG-9970Mitella pentandra Hook. Colorado, United StatesOPGC2021Wild material2120033OPGC 8281
383OPGC 8308CBG-10449Krigia biflora (Walter) S. F. Blake Wisconsin, United StatesOPGC2021Wild material2120088OPGC 8308
384OPGC 8320CBG-10493Vernonia missurica Raf. Illinois, United StatesOPGC2021Wild material2120118OPGC 8320
385OPGC 8321CBG-10498Euthamia gymnospermoides Greene Illinois, United StatesOPGC2021Wild material2120121OPGC 8321
386OPGC 8324CBG-10510Agalinis gattingeri (Small) Small Wisconsin, United StatesOPGC2021Wild materialforb2120202OPGC 8324
387OPGC 8342CBG-10574Euthamia gymnospermoides Greene Illinois, United StatesOPGC2021Wild materialPlant numbers sampled estimated.2120165OPGC 8342
388OPGC 8343CBG-10575Euthamia graminifolia (L.) Nutt. Illinois, United StatesOPGC2021Wild materialPlant numbers sampled estimated.2120166OPGC 8343
389OPGC 8344CBG-10576Gillenia stipulata (Muhl. ex Willd.) Nutt. Illinois, United StatesOPGC2021Wild materialplant numbers sampled estimated.2120167OPGC 8344
390OPGC 8348CBG-10581Hieracium scabrum Michx. Illinois, United StatesOPGC2021Wild materialPlant numbers sampled estimated.2120172OPGC 8348
391OPGC 8352CBG-10600Scutellaria lateriflora L. Illinois, United StatesOPGC2021Wild materialReceived as Scutellaria lateriflora var. lateriflora.2120185OPGC 8352
392OPGC 8355CBG-10605Solidago nemoralis Aiton Illinois, United StatesOPGC2021Wild materialAlso collected elsewhere in SCCA. Plant numbers sampled estimated.2120226OPGC 8355
393OPGC 8356CBG-10606Solidago ulmifolia Muhl. ex Willd. Illinois, United StatesOPGC2021Wild materialPlant numbers sampled estimated.2120227OPGC 8356
394W6 59105CBG-9971Luzula parviflora (Ehrh.) Desv. Colorado, United StatesW62021Wild material2120034W6 59105
395W6 59136CBG-10266Dasiphora fruticosa (L.) Rydb. Wisconsin, United StatesW62021Wild material2120062W6 59136
396W6 59137CBG-10267Muhlenbergia glomerata (Willd.) Trin. Wisconsin, United StatesW62021Wild material2120195W6 59137
397W6 59143CBG-10373Juncus interior Wiegand Iowa, United StatesW62021Wild material2120068W6 59143
398W6 59164CBG-10445Lycopus virginicus L. Kansas, United StatesW62021Wild material2120087W6 59164
399W6 59174CBG-10461Juncus bufonius L. Illinois, United StatesW62021Wild material2120096W6 59174
400W6 59186CBG-10477Juncus greenei Oakes & Tuck. Illinois, United StatesW62021Wild material2120105W6 59186
401W6 59200CBG-10494Cinna arundinacea L. Illinois, United StatesW62021Wild material2120119W6 59200
402W6 59201CBG-10497Lespedeza hirta (L.) Hornem. Illinois, United StatesW62021Wild material2120120W6 59201
403W6 59222CBG-10529Gratiola neglecta Torr. Illinois, United StatesW62021Wild materialPlant numbers estimated.2120137W6 59222
404W6 59234CBG-10548Dasistoma macrophyllum (Nutt.) Raf. Illinois, United StatesW62021Wild materialReceived as Dasistoma macrophylla. Plant numbers estimated. Few this year; abundant other years in numerous locations.2120206W6 59234
405W6 59241CBG-10557Boehmeria cylindrica (L.) Sw. Illinois, United StatesW62021Wild material2120153W6 59241
406W6 59243CBG-10560Cinna arundinacea L. Illinois, United StatesW62021Wild materialPlant numbers estimated.2120155W6 59243
407W6 59267CBG-10590Muhlenbergia glabrifloris Scribn. Illinois, United StatesW62021Wild materialReceived as: Muhlenbergia glabriflora. Plant numbers sampled estimated.2120210W6 59267
408W6 59284CBG-10609Sporobolus compositus (Poir.) Merr. Illinois, United StatesW62021Wild materialPlant numbers sampled estimated.2120229W6 59284
409W6 58997NCBG-445Glyceria striata (Lam.) Hitchc. Maryland, United StatesW62021Wild materialdrooping inflorescence2116315W6 58997
410W6 59009NCBG-462Eleocharis quadrangulata (Michx.) Roem. Virginia, United StatesW62021Wild material2116327W6 59009
411Ames 35729Woodside PrairieCeanothus americanus L. Iowa, United StatesNC72021COLLECTED08/31/2020Woodside Praire located 8.0 miles south and 2.0 miles west of Fontanelle41.17130000, -94.60140000380Remnant prairie.Wild material2120333Ames 35729
412Ames 35660Kiamichi MountainsPtelea trifoliata L. Oklahoma, United StatesNC72021COLLECTED07/19/2018Kiamichi Mountains of Ouachita National Forest along Road 6025 just west of State Highway 259, T2N R25E SW 1/4 NE 1/4 SW 1/4 Sec. 2734.61314900, -94.67035700651Open, dry ridgetop, rocky roadside.Wild materialSpecimens sampled measuring approximately 20-25' in height. 2114985Ames 35660
413NA 88284NEWFS-557Cephalanthus occidentalis L. Massachusetts, United StatesNA2021Wild material2115697NA 88284
414OPGC 8180NEWFS-473Solidago rugosa Mill. Massachusetts, United StatesOPGC2021Wild material2115663OPGC 8180
415OPGC 8181NEWFS-474Solidago altissima L. Massachusetts, United StatesOPGC2021Wild materialLeaves primarily three-veined, toothing infrequent and not flared. Plants often tall.2115664OPGC 8181
416OPGC 8182NEWFS-475Solidago canadensis L. Massachusetts, United StatesOPGC2021Wild materialThree-veined leaves with frequent, flared teeth.2115665OPGC 8182
417OPGC 8207NEWFS-572Typha latifolia L. New Hampshire, United StatesOPGC2021Wild material2115706OPGC 8207
418W6 58703NEWFS-371Scirpus atrovirens Willd. Massachusetts, United StatesW62021Wild material2115642W6 58703
419W6 58757NEWFS-556Scirpus cyperinus (L.) Kunth Massachusetts, United StatesW62021Wild material2115696W6 58757
420W6 58800NEWFS-830Juncus canadensis J. Gay ex Laharpe Massachusetts, United StatesW62021Wild materialDensely clustered spikelets on forking stem - superficially resembles Rhynchospora sp., miniscule seeds.2115739W6 58800
421W6 58801NEWFS-831Triadenum virginicum (L.) Raf. Massachusetts, United StatesW62021Wild materialOpposite leaves with pink bulbous fruits.2115740W6 58801
422Ames 35615Ames 35615Aronia arbutifolia (L.) Pers. Michigan, United StatesNC7SEED2020COLLECTED11/03/2020Warren Townsend Park located just northeast of Cannonsburg southwest of Ramsdell Dr. and Six Mile Rd. intersection, T8N R10W NE ¼ NW ¼ Sec. 26, Cannon Twp., Kent County43.05606700, -85.46435100239Shrubby edge of old stream (Bear Creek) oxbow, adjacent to wet meadow with groundwater upwelling. Muck soils.Wild materialPlants in nature measuring approximately six meters in height; elongate shrubs mostly unbranched; bright-red fruits measuring between 4-7 mm in diameter; tomentose leaves underneath; scarlet fall color. This collection was discovered in 2011 and represents the first report of the species for the state of Michigan (Ryskamp and Warners 2012) and thus represents a widely disjunct population where the next nearest documented population is in southern Ohio (Clermont County). 2110277Ames 35615
423NA 88297NV030-1484Clematis ligusticifolia Nutt. Nevada, United StatesNA2020Wild materialepiphytic vine, achene fr, achene attached to pubescent tail, compound lvs.2110425NA 88297
424NA 88449NV030-1465Rosa woodsii Lindl. Nevada, United StatesNA2020Wild materialBright red rose hips, margins of lvs serrated, opposite lvs.2110411NA 88449
425OPGC 8123NV030-1451Asclepias speciosa Torr. Nevada, United StatesOPGC2020Wild materialErect stems, whorled leaf arrangement, pointed leaf tips, hairy leaves.2110398OPGC 8123
426OPGC 8128NV030-1462Iris missouriensis Nutt. Nevada, United StatesOPGC2020Wild materialLinear lvs, elongated capsule - erect, lvs are basal.2110408OPGC 8128
427OPGC 8129NV030-1464Iris missouriensis Nutt. Nevada, United StatesOPGC2020Wild materialLinear lvs, lvs are basal, elongated erect capsule.2110410OPGC 8129
428OPGC 8130NV030-1467Navarretia divaricata Greene California, United StatesOPGC2020Wild materialHairy+glandular, prickly fr, rounded fr head2110413OPGC 8130
429OPGC 8132NV030-1485Solidago spectabilis (D. C. Eaton) A. Gray Nevada, United StatesOPGC2020Wild materialLance shaped lvs, aster inflor, basal rosette, erect/tall.2110426OPGC 8132
430W6 58501NV030-1446Leymus cinereus (Scribn. & Merr.) Á. Löve California, United StatesW62020Wild materialBunchgrass, elongated lvs, large plant size.2110395W6 58501
431W6 58515NV030-1463Leymus cinereus (Scribn. & Merr.) Á. Löve Nevada, United StatesW62020Wild materialBunchgrass, large pl size, elongated/linear lvs.2110409W6 58515
432W6 58520NV030-1468Juncus balticus Willd. subsp. littoralis (Engelm.) Snogerup California, United StatesW62020Wild materialBracts subtend and extend beyond inflorescence, clusters of fr in a panicle not bunched, rhizomatous.2110414W6 58520
433OPGC 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
434W6 58076ID230-42Erigeron pumilus Nutt. var. intermedius (Cronquist) S. L. Welsh Idaho, United StatesW62020Wild materialPubescent forb with ray and disk flowers. Rays white and disks yellow.2107682W6 58076
435OPGC 8031MT050-21Penstemon procerus Douglas ex Graham Montana, United StatesOPGC2020Wild material 2106477OPGC 8031
436OPGC 8039WY050-117Chrysothamnus viscidiflorus (Hook.) Nutt. Wyoming, United StatesOPGC2020Wild material2106502OPGC 8039
437OPGC 7556JDC/PM/2020/006/927 Phlox maculata L. Iowa, United StatesOPGCFLOWER2020COLLECTED07/18/2020Located approximately 3.0 miles southwest of Roland and just 330 yards west of 150h Street and 580th Avenue intersection, T85N R23W NE1/4 NE1/4 Sec. 32, Story County42.13724800, -93.54455800305Roadside restoration. Locallized in wetter soils/drainage.Wild materialPhlox maculata is rather rare in central Iowa, more common to northeastern parts of the state. This accession sampled in nature had purple-pink flowers on plants measuring circa 2-2.5’ in height with glabrous stems. Panicles measuring approximately 4-5” in length and 2” wide. Peak flowering and fruiting occurred 25 June and 18 July, respectively in central Iowa (2020). 2106130OPGC 7556
438Ames 35337JDC/SP/2020/002/923Salix pedicellaris Pursh Iowa, United StatesNC7FLOWER2020COLLECTED06/05/2020Pilot Knob State Preserve (Floating Bog) located approximately 3.66 miles east, southeast of Forest City, area just west of Dead Mans Lake, T97N R23W NW1/4 NW1/4 SE1/4 Sec. 4, Hancock County43.24868300, -93.56644900406Extremely high-quality remnant floating bog that has never been hydrologically altered. Very diverse habitat.Wild materialSalix pedicellaris is extremely rare in Iowa only found in the northern tiers of counties. Currently listed as a state threatened plant species and thus tracked via the Iowa Natural Areas Inventory Program (Iowa Department of Natural Resources). Only 15 sites throughout Iowa representing 13 counties have documented S. pedicellaris. Since the year 2000, only two reports (observation/herbarium specimen) have documented the species presence in Iowa. Bog willow is a small shrub (<2 meters) typically with few, short stems often hidden amongst sedges. Spreads clonally via suckering and/or layering lending it to be found in stable fen habitats with ample supply of water that see little to no distrurbance. Spring flowering typically occurring in mid-May to early June with fruiting occurring in early June in Iowa. Little to no existance in cultivation. Leaves are rather waxy and repel water significantly. During a growout of original plant material (sampled as cuttings from collection site in nature) at NCRPIS, a total of 45 genets were determined to be female (14 count) and male (31 count) during peak flowering on 4 May 2022. 2105808Ames 35337
439NA 88174CA180-204Cupressus macnabiana A. Murray bis California, United StatesNA2020Wild material2104955NA 88174
440W6 57661CA180-208Prunella vulgaris L. California, United StatesW62020Wild materialSOS 92nd Shipment2104959W6 57661
441W6 57723ID210-11Eriogonum umbellatum Torr. Idaho, United StatesW62020Wild materialSOS 92nd Shipment2105021W6 57723
442W6 57434NEWFS-573Sparganium americanum Nutt. New Hampshire, United StatesW6SEED2019Wild material2098231W6 57434
443OPGC 7946NEWFS-246Lobelia cardinalis L. Massachusetts, United StatesOPGCSEED2019Wild material2098174OPGC 7946
444W6 57374NEWFS-243Spiraea tomentosa L. Massachusetts, United StatesW6SEED2019Wild material2098171W6 57374
445W6 57371NEWFS-232Scirpus cyperinus (L.) Kunth Massachusetts, United StatesW6SEED2019Wild material2098168W6 57371
446W6 57347NEWFS-170Eriophorum virginicum L. Massachusetts, United StatesW6SEED2019Wild material2098144W6 57347
447W6 57630958097Pisum sativum L. subsp. elatius (M. Bieb.) Asch. & Graebn. Masallı, AzerbaijanW62019COLLECTED06/16/2017Masalli, vill.Gizilaghaj.39.03788889, 48.7921111116Meadow. Soil Texture: Silt-sand; Without drainage. Aspect: Flat.Wild material2098627W6 57630
448NA 88095MARSB-256Ilex verticillata (L.) A. Gray New York, United StatesNASEED2019COLLECTED10/07/2015In Sag Harbor, NY, park in Mashashimuet Park. Walk along the Long Pond Greenbelt Trail. The population is along the edges of Long Pond and Crooked Pond, the first and third ponds on the left, respectively.40.96283000, -72.293660005Central shrub & herb depression pond.Wild material2097543NA 88095
449NA 88096MARSB-258Ilex glabra (L.) A. Gray New York, United StatesNASEED2019COLLECTED10/08/2015In Sag Harbor, park in Mashashimuet Park. Enter the Long Pond Greenbelt and walk along it until you reach Crooked Pond, the third pond on the left. The population is along pond edges.40.96283000, -72.293660005Central shrub & herb depression pond.Wild material2097545NA 88096
450NA 88111MARSB-428Lyonia ligustrina (L.) DC. New Jersey, United StatesNASEED2019Wild material2097629NA 88111
451NA 88435MARSB-255Rosa palustris Marshall New York, United StatesNASEED2019Wild material2097542NA 88435
452OPGC 7884MARSB-259Rhexia virginica L. New York, United StatesOPGCSEED2019Wild material2097546OPGC 7884
453W6 57189MARSB-427Alnus serrulata (Aiton) Willd. New Jersey, United StatesW6SEED2019Wild material2097628W6 57189
454Ames 35237Ames 35237Monarda fistulosa L. New Mexico, United StatesNC7Flower2019COLLECTED10/03/2019Railroad Canyon located approximately 6.38 miles west of Kingston just north of highway 152, T16S R10W Grant County32.91279900, -107.816403002173Sparsely wooded canyon with small creek.Wild material2097773Ames 35237
455Ames 35236SF_ID:24690/EO-ID:17843Agastache foeniculum (Pursh) Kuntze Nebraska, United StatesNC7FLOWER2019Wild materialPlants measuring approximately 60 cm in height. Infructescences fully mature at time of collection (23 October 2019), likely past peak maturity by approximately 4 weeks. Population (EC-ID: 17843) was originally documented by Steven B. Rolfsmeier on 8 June 2015 (Nebraska Pine Ridge Plant Resurvey, 2015: Report submitted to the Nebraska Natural Heritage Program) noting “ Agastache foeniculum was located in a ravine bottom that burned in 2012. Estimated population size: 200-300 stems covering approximately 125 sq. meters”. A. foeniculum in Nebraska is currently tracked by the Nebraska Natural Heritage Program and is listed (6 November 2019) as a S1 (Critically Imperiled - at very high risk of extirpation in the state due to very restricted range, few populations or occurrences, steep declines, severe threats or other factors) and Tier 2 species (Tier 2 - species are typically those that are not at-risk from a global or national perspective but are rare or imperiled within Nebraska). 2097772Ames 35236
456Ames 35229JDC/AS/2019/020/899Agastache scrophulariifolia (Willd.) Kuntze Iowa, United StatesNC7PLANT2019COLLECTED10/01/2019Hertz Family Woods & Nature Preserve just 2.25 miles south of Nevada (T83N R22W NW1/4 NW1/4 Sec. 20) and Robison Wildlife Acres just 6.75 miles south of Nevada (T82N R22W NE1/4 SW1/4 Sec. 8), Story County41.99070000, -93.44186700285Moist, semi-shaded, deciduous woods.Wild materialPlants measuring approximately 6' in height with somewhat short (perhaps due to dense shade) 2-3" spikes rather white or extremely pale pink in color. Peak flowering occurred circa 26 August 2019 in nature.2097765Ames 35229
457OPGC 7546WY050-201Lysimachia maritima (L.) Galasso et al. Wyoming, United StatesOPGCSEED2019Wild material2096999OPGC 7546
458Ames 35224JDC/AP/2019/034/913Aronia ×prunifolia (Marshall) Rehder Wisconsin, United StatesNC7PLANT2019COLLECTED09/17/2019Crex Meadows Wildlife Management Area located along Buggerts Lake Road approximately 7.0 miles north of Grantsburg, T39N R19W NW1/4 NE1/4 Sec. 12, Burnett County45.88743300, -92.65832600284Wet, swampy areas.Wild materialPlants in nature with some orange fall color and black fruits (a few fruits shriveled) at time of harvest (17 September). Average height approximately 3.5-4.0'. 2097760Ames 35224
459Ames 35225JDC/MF/2019/035/914Monarda fistulosa L. Minnesota, United StatesNC7SEED2019COLLECTED09/17/2019Iron Horse Prairie Scientific Natural Area located approximately 1.5 miles south of Hayfield, T105N R17W NW1/4 SE1/4 and NE1/4 SW1/4 Sec. 27, Dodge County43.86750030, -92.84861000399High-quality prairie remnant with various habitats from dry, short-grass type vegetation to rather wet, thick vegetation.Wild materialPlants in nature ranging from 2' to 4.5' in height. Variability in mildew resistance noted at time of harvest (17 September) ranging from plants with no leaves to plants with persistent leaves with minimal to substantial mildew.2097761Ames 35225
460Ames 35251TK2019-18Salix armenorossica A. K. Skvortsov Samtskhe-Javakheti, GeorgiaNC7PLANT2019COLLECTED06/12/2019Near village of Tsikhisjvari, Borjomi municipality.41.72661700, 43.457933001602Riparian, banks of Oshora River.Wild materialDeciduous tree, 10-15 meters2097803Ames 35251
461NA 86438JDC/IV/2019/033/912Ilex verticillata (L.) A. Gray Wisconsin, United StatesNAPLANT2019COLLECTED09/17/2019Crex Meadows Wildlife Management Area located approximately 7.0 miles north of Grantsburg, Burnett County45.86773900, -92.63055500285Wet, swampy areasWild materialAverage height noted of plants in nature was circa 8' in height. Fruits bright red and persistent at time of harvest (17 September). Foliage green, signs of chlorosis noted on most specimens.2097759NA 86438
462WLP 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
463Ames 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
464NA 88443NV040-344Rosa woodsii Lindl. Nevada, United StatesNASEED2019Wild material2094595NA 88443
465W6 56735WY030-263Artemisia nova A. Nelson Wyoming, United StatesW6SEED2019Wild material2094541W6 56735
466W6 56772NV040-326Leymus cinereus (Scribn. & Merr.) Á. Löve Nevada, United StatesW6SEED2019Wild material2094578W6 56772
467W6 56782NV040-337Leymus cinereus (Scribn. & Merr.) Á. Löve Nevada, United StatesW6SEED2019Wild material2094588W6 56782
468W6 56787NV040-342Hymenoxys lemmonii (Greene) Cockerell Nevada, United StatesW6SEED2019Wild material2094593W6 56787
469OPGC 7472CBG-9061Verbena hastata L. Nebraska, United StatesOPGCSEED2019Wild material2092740OPGC 7472
470W6 56635CBG-8953Sagittaria latifolia Willd. Nebraska, United StatesW6SEED2019Wild material2092734W6 56635
471W6 56639CBG-9059Schoenoplectus tabernaemontani (C. C. Gmel.) Palla Nebraska, United StatesW6SEED2019Wild material2092738W6 56639
472W6 56643CBG-9064Trisetum spicatum (L.) K. Richt. Wyoming, United StatesW6SEED2019Wild material2092742W6 56643
473OPGC 7845CBG-8187Polemonium reptans L. Wisconsin, United StatesOPGCSEED2019Wild material SOS 7th transfer.2092671OPGC 7845
474Ames 34431JDC/SC/2019/001/880Salix candida Flüggé ex Willd. Iowa, United StatesNC7FRUIT2019COLLECTED05/17/2019Private property approximately 2.2 miles southwest of Oelwein, T91N R9W SW 1/4 SE 1/4 Sec. 30.42.65929300, -91.94916200311High-qulity fen, remnant.Wild materialPlants at collection site in nature averaging 2.0-2.5' in height with minimal branching. Pubescent stems mostly near apical ends. Most plants estimated at 25 ramets per genet. Estimated number of ramets per genet is difficult to separate/distinguish. This petite, shrubby willow is essentially restricted to cold bogs/fen communities and is rare in Iowa (Nekola 1990). It is easily recognized by its narrowly and extremely pubescent leaves. Salix candida was considered extirpated from Iowa by Spence (1959) and Roosa and Eilers (1978). Since discovery of eastern Iowa fen communities in 1984 it has been observed extant at 26 sites (Nekola 1988) and is tracked as a species of special concern by the Iowa Department of Natural Resources Natural Areas Inventory (2021). 2091747Ames 34431
475Ames 34432Kauten FenSalix candida Flüggé ex Willd. Iowa, United StatesNC7FRUIT2019COLLECTED05/17/2019Kauten Fen located 12.4 miles south of West Union, T92N R8W NE 1/4 SW 1/4 NE 1/4 Sec.16.42.78232200, -91.78865600351High-qulity fen, remnant.Wild materialPlants at collection site in nature averaging 2.0' in height with little to no branching (e.g. estimated 1-3 ramets per genet which are difficult to separate/distinguish due to the clonal nature of the species). Suspected possible suckering via rhizomes. Very pubescent stems mostly near apical ends. This petite, shrubby willow is essentially restricted to cold bogs/fen communities and is rare in Iowa (Nekola 1990). It is easily recognized by its narrowly and extremely pubescent leaves. The undersides are extremely white in appearance resulting in a very attractive ornamental characteristic. Salix candida was considered extirpated from Iowa by Spence (1959) and Roosa and Eilers (1978). Since discovery of eastern Iowa fen communities in 1984 it has been observed extant at 26 sites (Nekola 1988) and is tracked as a species of special concern by the Iowa Department of Natural Resources Natural Areas Inventory (2021). Plants in cultivation reached heights to 4.0-4.5'. Variation in degree of pubescence on apical portions of stems noted across genotypes with majority being rather to extremely pubescent. 2091748Ames 34432
476NA 88062NEWFS-233Clethra alnifolia L. Massachusetts, United StatesNASEED2019Wild material1976185NA 88062
477NA 88071NEWFS-610Clethra alnifolia L. Connecticut, United StatesNASEED2019Wild material1976301NA 88071
478NA 88074NEWFS-628Ilex verticillata (L.) A. Gray Maine, United StatesNASEED2019COLLECTED11/16/2016Wells Reserve: from Boston, take 93N to 95N to ME-109S. Left on US-1N. Right on Laudholm Farm Rd. Left on Skinner Mill Rd. Park at the reserve paring lot, walk across field to trails and boardwalk through bog. (Ref: NEWFS-452)43.33672000, -70.554880009Bog, bog/woodland edge, and wet meadow.Wild material1976304NA 88074
479NA 88433NEWFS-237Rosa palustris Marshall Connecticut, United StatesNASEED2019Wild material1976186NA 88433
480OPGC 7398NEWFS-431Rhexia virginica L. Massachusetts, United StatesOPGCSEED2019Wild material1976259OPGC 7398
481OPGC 7376AK930-682Saxifraga tricuspidata Rottb. Alaska, United StatesOPGCSEED2019Wild material1975827OPGC 7376
482W6 56066AK930-658Calamagrostis canadensis (Michx.) P. Beauv. Alaska, United StatesW6SEED2019Wild material1975807W6 56066
483OPGC 7311AZ930-363Aquilegia chrysantha A. Gray Arizona, United StatesOPGCSEED2018Wild material1970379OPGC 7311
484OPGC 7350NV030-1336Solidago spectabilis (D. C. Eaton) A. Gray Nevada, United StatesOPGCSEED2018Wild material1970660OPGC 7350
485W6 55616WY050-154Astragalus purshii Douglas var. purshii Wyoming, United StatesW6SEED2018Wild material1970327W6 55616
486W6 55618WY050-156Townsendia incana Nutt. Wyoming, United StatesW6SEED2018Wild material1970329W6 55618
487W6 55622WY050-160Allium textile A. Nelson & J. F. Macbr. Wyoming, United StatesW6SEED2018Wild material1970333W6 55622
488W6 55627WY050-165Oxytropis besseyi (Rydb.) Blank. var. fallax Barneby Wyoming, United StatesW6SEED2018Wild material1970338W6 55627
489W6 55708CA190C-14Juncus patens E. Mey. California, United StatesW6SEED2018Wild materialJuncus patens1970419W6 55708
490WLP 1545NACPEC18-090Photinia davidiana (Decne.) Cardot Hubei Sheng, ChinaNA2018COLLECTED09/21/2018Shennongjia Forest District; Muyuping; Guanmenshan.31.44033000, 110.385730001311Near footpath/boardwalk in rich gallery forest along river, in heavy shade. Growing in moss-covered humus.Seeds and three herbarium specimens collected from two plants. Photographed. In addition to the listed associated taxa, found growing in association with numerous ferns.2108988WLP 1545
491NA 88454OR050-274Rosa woodsii Lindl. var. ultramontana (S. Watson) Jeps. Oregon, United StatesNASEED2018Wild materialRosa woodsii var. ultramontana1967943NA 88454
492OPGC 6742MT050-63Platanthera dilatata (Pursh) Lindl. ex L. C. Beck var. albiflora (Cham.) Ledeb. Montana, United StatesOPGCSEEDContact Site2018Wild materialPlatanthera dilatata var. albiflora1967915OPGC 6742
493OPGC 7248OR050-271Epilobium brachycarpum C. Presl Oregon, United StatesOPGCSEED2018Wild material1967940OPGC 7248
494W6 55304WY030-232Leymus cinereus (Scribn. & Merr.) Á. Löve Wyoming, United StatesW6SEED2018Wild materialLeymus cinereus1967856W6 55304
495W6 55356MT050-56Wyethia helianthoides Nutt. Montana, United StatesW6SEED2018Wild material1967908W6 55356
496W6 55357MT050-57Stenotus lanuginosus (A. Gray) Greene Montana, United StatesW6SEED2018Wild materialStenotus lanuginosus1967909W6 55357
497W6 55392OR050-275Cornus sericea L. subsp. occidentalis (Torr. & A. Gray) Fosberg Oregon, United StatesW6SEED2018Wild materialCornus sericea ssp. occidentalis1967944W6 55392
498NA 86521NACPEC18-091Quercus engleriana Seemen Hubei Sheng, ChinaNA2018COLLECTED09/21/2018Shennongjia Forest District; Muyuping; Guanmenshan.31.43976000, 110.384060001315Vertical cliff along road. Growing in humus over rocks.Wild materialSeeds and four herbarium specimens collected from one plant. Photographed. In addition to the listed associated taxa, found growing in association with numerous ferns.2109230NA 86521
499OPGC 6656NM930-413Rudbeckia laciniata L. New Mexico, United StatesOPGCSEED2018Wild materialRudbeckia laciniata1966142OPGC 6656