Search Accessions

rows.  (Please note that results of more than 500 rows will not contain images.)


Search
Search Clear All
Scientific name (any part, no hybrid symbols)

Plant name


Genebank
Country of Origin


Other search criteria:



With genomic data With NCBI link With images Only non-Genetically Engineered

Search
View Observation Data
Selected item(s) below:

ACCESSIONPLANT NAMETAXONOMYORIGINGENEBANKIMAGEAVAILABILITYRECEIVEDSOURCE TYPESOURCE DATECOLLECTION SITECOORDINATESELEVATIONHABITATIMPROVEMENT LEVELNARRATIVE
0NA 88416NCBG-620Pinus taeda L. North Carolina, United StatesNA2021Wild material2116356NA 88416
1FSNS 9208FSNS 9208Pinus taeda L. NTSL2021Wild material2137624FSNS 9208
2FSNS 9209FSNS 9209Pinus taeda L. NTSL2021Wild material2137625FSNS 9209
3FSNS 9210FSNS 9210Pinus taeda L. NTSL2021Wild material2137626FSNS 9210
4FSNS 9211FSNS 9211Pinus taeda L. NTSL2021Wild material2137627FSNS 9211
5FSNS 9212FSNS 9212Pinus taeda L. NTSL2021Wild material2137628FSNS 9212
6FSNS 9213FSNS 9213Pinus taeda L. NTSL2021Wild material2137629FSNS 9213
7FSNS 9214FSNS 9214Pinus taeda L. NTSL2021Wild material2137633FSNS 9214
8FSNS 9215FSNS 9215Pinus taeda L. NTSL2021Wild material2137634FSNS 9215
9FSNS 9216FSNS 9216Pinus taeda L. NTSL2021Wild material2137635FSNS 9216
10FSNS 9217FSNS 9217Pinus taeda L. NTSL2021Wild material2137636FSNS 9217
11FSNS 9218FSNS 9218Pinus taeda L. NTSL2021Wild material2137637FSNS 9218
12FSNS 9219FSNS 9219Pinus taeda L. NTSL2021Wild material2137638FSNS 9219
13FSNS 9220FSNS 9220Pinus taeda L. NTSL2021Wild material2137639FSNS 9220
14FSNS 9221FSNS 9221Pinus taeda L. NTSL2021Wild material2137640FSNS 9221
15FSNS 9222FSNS 9222Pinus taeda L. NTSL2021Wild material2137641FSNS 9222
16FSNS 9223FSNS 9223Pinus taeda L. NTSL2021Wild material2137642FSNS 9223
17FSNS 9224FSNS 9224Pinus taeda L. NTSL2021Wild material2137643FSNS 9224
18FSNS 9225FSNS 9225Pinus taeda L. NTSL2021Wild material2137644FSNS 9225
19FSNS 9226FSNS 9226Pinus taeda L. NTSL2021Wild material2137645FSNS 9226
20FSNS 9227FSNS 9227Pinus taeda L. NTSL2021Wild material2137646FSNS 9227
21FSNS 9228FSNS 9228Pinus taeda L. NTSL2021Wild material2137647FSNS 9228
22FSNS 9229FSNS 9229Pinus taeda L. NTSL2021Wild material2137648FSNS 9229
23FSNS 9230FSNS 9230Pinus taeda L. NTSL2021Wild material2137649FSNS 9230
24FSNS 9231FSNS 9231Pinus taeda L. NTSL2021Wild material2137650FSNS 9231
25FSNS 9232FSNS 9232Pinus taeda L. NTSL2021Wild material2137651FSNS 9232
26FSNS 9233FSNS 9233Pinus taeda L. NTSL2021Wild material2137652FSNS 9233
27FSNS 9234FSNS 9234Pinus taeda L. NTSL2021Wild material2137653FSNS 9234
28FSNS 9235FSNS 9235Pinus taeda L. NTSL2021Wild material2137654FSNS 9235
29FSNS 9236FSNS 9236Pinus taeda L. NTSL2021Wild material2137655FSNS 9236
30FSNS 9237FSNS 9237Pinus taeda L. NTSL2021Wild material2137656FSNS 9237
31FSNS 9238FSNS 9238Pinus taeda L. NTSL2021Wild material2137657FSNS 9238
32FSNS 9239FSNS 9239Pinus taeda L. NTSL2021Wild material2137658FSNS 9239
33FSNS 9240FSNS 9240Pinus taeda L. NTSL2021Wild material2137659FSNS 9240
34FSNS 9241FSNS 9241Pinus taeda L. NTSL2021Wild material2137660FSNS 9241
35FSNS 9242FSNS 9242Pinus taeda L. NTSL2021Wild material2137661FSNS 9242
36FSNS 9243FSNS 9243Pinus taeda L. NTSL2021Wild material2137662FSNS 9243
37FSNS 9244FSNS 9244Pinus taeda L. NTSL2021Wild material2137663FSNS 9244
38FSNS 9245FSNS 9245Pinus taeda L. NTSL2021Wild material2137664FSNS 9245
39FSNS 9246FSNS 9246Pinus taeda L. NTSL2021Wild material2137665FSNS 9246
40FSNS 9247FSNS 9247Pinus taeda L. NTSL2021Wild material2137666FSNS 9247
41FSNS 9248FSNS 9248Pinus taeda L. NTSL2021Wild material2137667FSNS 9248
42FSNS 9249FSNS 9249Pinus taeda L. NTSL2021Wild material2137668FSNS 9249
43FSNS 9250FSNS 9250Pinus taeda L. NTSL2021Wild material2137669FSNS 9250
44FSNS 9251FSNS 9251Pinus taeda L. NTSL2021Wild material2137670FSNS 9251
45FSNS 9252FSNS 9252Pinus taeda L. NTSL2021Wild material2137671FSNS 9252
46FSNS 9253FSNS 9253Pinus taeda L. NTSL2021Wild material2137672FSNS 9253
47FSNS 9254FSNS 9254Pinus taeda L. NTSL2021Wild material2137673FSNS 9254
48FSNS 9255FSNS 9255Pinus taeda L. NTSL2021Wild material2137674FSNS 9255
49FSNS 9256FSNS 9256Pinus taeda L. NTSL2021Wild material2137675FSNS 9256
50FSNS 9257FSNS 9257Pinus taeda L. NTSL2021Wild material2137676FSNS 9257
51FSNS 9258FSNS 9258Pinus taeda L. NTSL2021Wild material2137677FSNS 9258
52FSNS 9259FSNS 9259Pinus taeda L. NTSL2021Wild material2137678FSNS 9259
53FSNS 9260FSNS 9260Pinus taeda L. NTSL2021Wild material2137679FSNS 9260
54FSNS 9261FSNS 9261Pinus taeda L. NTSL2021Wild material2137680FSNS 9261
55FSNS 9262FSNS 9262Pinus taeda L. NTSL2021Wild material2137681FSNS 9262
56FSNS 9263FSNS 9263Pinus taeda L. NTSL2021Wild material2137682FSNS 9263
57FSNS 9264FSNS 9264Pinus taeda L. NTSL2021Wild material2137683FSNS 9264
58FSNS 9265FSNS 9265Pinus taeda L. NTSL2021Wild material2137684FSNS 9265
59FSNS 9266FSNS 9266Pinus taeda L. NTSL2021Wild material2137685FSNS 9266
60FSNS 9267FSNS 9267Pinus taeda L. NTSL2021Wild material2137686FSNS 9267
61FSNS 9268FSNS 9268Pinus taeda L. NTSL2021Wild material2137687FSNS 9268
62FSNS 9269FSNS 9269Pinus taeda L. NTSL2021Wild material2137688FSNS 9269
63FSNS 9270FSNS 9270Pinus taeda L. NTSL2021Wild material2137689FSNS 9270
64FSNS 9271FSNS 9271Pinus taeda L. NTSL2021Wild material2137690FSNS 9271
65FSNS 9272FSNS 9272Pinus taeda L. NTSL2021Wild material2137691FSNS 9272
66FSNS 9273FSNS 9273Pinus taeda L. NTSL2021Wild material2137692FSNS 9273
67FSNS 9274FSNS 9274Pinus taeda L. NTSL2021Wild material2137693FSNS 9274
68FSNS 9275FSNS 9275Pinus taeda L. NTSL2021Wild material2137694FSNS 9275
69FSNS 9276FSNS 9276Pinus taeda L. NTSL2021Wild material2137695FSNS 9276
70FSNS 9277FSNS 9277Pinus taeda L. NTSL2021Wild material2137696FSNS 9277
71FSNS 9278FSNS 9278Pinus taeda L. NTSL2021Wild material2137697FSNS 9278
72FSNS 9279FSNS 9279Pinus taeda L. NTSL2021Wild material2137698FSNS 9279
73FSNS 9280FSNS 9280Pinus taeda L. NTSL2021Wild material2137699FSNS 9280
74FSNS 9281FSNS 9281Pinus taeda L. NTSL2021Wild material2137700FSNS 9281
75FSNS 9282FSNS 9282Pinus taeda L. NTSL2021Wild material2137701FSNS 9282
76FSNS 9283FSNS 9283Pinus taeda L. NTSL2021Wild material2137702FSNS 9283
77FSNS 9284FSNS 9284Pinus taeda L. NTSL2021Wild material2137703FSNS 9284
78FSNS 9285FSNS 9285Pinus taeda L. NTSL2021Wild material2137704FSNS 9285
79FSNS 9286FSNS 9286Pinus taeda L. NTSL2021Wild material2137705FSNS 9286
80FSNS 9287FSNS 9287Pinus taeda L. NTSL2021Wild material2137706FSNS 9287
81FSNS 9288FSNS 9288Pinus taeda L. NTSL2021Wild material2137707FSNS 9288
82FSNS 9289FSNS 9289Pinus taeda L. NTSL2021Wild material2137708FSNS 9289
83FSNS 9290FSNS 9290Pinus taeda L. NTSL2021Wild material2137709FSNS 9290
84FSNS 9291FSNS 9291Pinus taeda L. NTSL2021Wild material2137710FSNS 9291
85FSNS 9292FSNS 9292Pinus taeda L. NTSL2021Wild material2137711FSNS 9292
86FSNS 9293FSNS 9293Pinus taeda L. NTSL2021Wild material2137712FSNS 9293
87FSNS 9294FSNS 9294Pinus taeda L. NTSL2021Wild material2137713FSNS 9294
88FSNS 9295FSNS 9295Pinus taeda L. NTSL2021Wild material2137714FSNS 9295
89FSNS 9297FSNS 9297Pinus taeda L. NTSL2021Wild material2137716FSNS 9297
90FSNS 9298FSNS 9298Pinus taeda L. NTSL2021Wild material2137717FSNS 9298
91FSNS 9299FSNS 9299Pinus taeda L. NTSL2021Wild material2137718FSNS 9299
92FSNS 9300FSNS 9300Pinus taeda L. NTSL2021Wild material2137719FSNS 9300
93FSNS 9301FSNS 9301Pinus taeda L. NTSL2021Wild material2137720FSNS 9301
94FSNS 9302FSNS 9302Pinus taeda L. NTSL2021Wild material2137721FSNS 9302
95FSNS 9303FSNS 9303Pinus taeda L. NTSL2021Wild material2137722FSNS 9303
96FSNS 9304FSNS 9304Pinus taeda L. NTSL2021Wild material2137723FSNS 9304
97FSNS 9305FSNS 9305Pinus taeda L. NTSL2021Wild material2137724FSNS 9305
98FSNS 9306FSNS 9306Pinus taeda L. NTSL2021Wild material2137725FSNS 9306
99FSNS 9307FSNS 9307Pinus taeda L. NTSL2021Wild material2137726FSNS 9307
100FSNS 9308FSNS 9308Pinus taeda L. NTSL2021Wild material2137727FSNS 9308
101FSNS 9309FSNS 9309Pinus taeda L. NTSL2021Wild material2137728FSNS 9309
102FSNS 9310FSNS 9310Pinus taeda L. NTSL2021Wild material2137729FSNS 9310
103FSNS 9311FSNS 9311Pinus taeda L. NTSL2021Wild material2137730FSNS 9311
104FSNS 9312FSNS 9312Pinus taeda L. NTSL2021Wild material2137731FSNS 9312
105FSNS 9313FSNS 9313Pinus taeda L. NTSL2021Wild material2137732FSNS 9313
106FSNS 9314FSNS 9314Pinus taeda L. NTSL2021Wild material2137733FSNS 9314
107FSNS 9315FSNS 9315Pinus taeda L. NTSL2021Wild material2137734FSNS 9315
108FSNS 9316FSNS 9316Pinus taeda L. NTSL2021Wild material2137735FSNS 9316
109FSNS 9317FSNS 9317Pinus taeda L. NTSL2021Wild material2137736FSNS 9317
110FSNS 9318FSNS 9318Pinus taeda L. NTSL2021Wild material2137737FSNS 9318
111FSNS 9319FSNS 9319Pinus taeda L. NTSL2021Wild material2137738FSNS 9319
112FSNS 9320FSNS 9320Pinus taeda L. NTSL2021Wild material2137739FSNS 9320
113FSNS 9321FSNS 9321Pinus taeda L. NTSL2021Wild material2137740FSNS 9321
114FSNS 9322FSNS 9322Pinus taeda L. NTSL2021Wild material2137741FSNS 9322
115FSNS 9323FSNS 9323Pinus taeda L. NTSL2021Wild material2137742FSNS 9323
116FSNS 9324FSNS 9324Pinus taeda L. NTSL2021Wild material2137743FSNS 9324
117FSNS 9325FSNS 9325Pinus taeda L. NTSL2021Wild material2137744FSNS 9325
118FSNS 9326FSNS 9326Pinus taeda L. NTSL2021Wild material2137745FSNS 9326
119FSNS 9327FSNS 9327Pinus taeda L. NTSL2021Wild material2137746FSNS 9327
120FSNS 9328FSNS 9328Pinus taeda L. NTSL2021Wild material2137747FSNS 9328
121FSNS 9329FSNS 9329Pinus taeda L. NTSL2021Wild material2137748FSNS 9329
122FSNS 9330FSNS 9330Pinus taeda L. NTSL2021Wild material2137749FSNS 9330
123FSNS 9331FSNS 9331Pinus taeda L. NTSL2021Wild material2137750FSNS 9331
124FSNS 9332FSNS 9332Pinus taeda L. NTSL2021Wild material2137751FSNS 9332
125FSNS 9333FSNS 9333Pinus taeda L. NTSL2021Wild material2137752FSNS 9333
126FSNS 9334FSNS 9334Pinus taeda L. NTSL2021Wild material2137753FSNS 9334
127FSNS 9335FSNS 9335Pinus taeda L. NTSL2021Wild material2137754FSNS 9335
128FSNS 9336FSNS 9336Pinus taeda L. NTSL2021Wild material2137755FSNS 9336
129FSNS 9337FSNS 9337Pinus taeda L. NTSL2021Wild material2137756FSNS 9337
130FSNS 9338FSNS 9338Pinus taeda L. NTSL2021Wild material2137757FSNS 9338
131FSNS 9339FSNS 9339Pinus taeda L. NTSL2021Wild material2137758FSNS 9339
132FSNS 9340FSNS 9340Pinus taeda L. NTSL2021Wild material2137759FSNS 9340
133FSNS 9341FSNS 9341Pinus taeda L. NTSL2021Wild material2137760FSNS 9341
134FSNS 9342FSNS 9342Pinus taeda L. NTSL2021Wild material2137761FSNS 9342
135FSNS 9343FSNS 9343Pinus taeda L. NTSL2021Wild material2137762FSNS 9343
136FSNS 9344FSNS 9344Pinus taeda L. NTSL2021Wild material2137763FSNS 9344
137FSNS 9345FSNS 9345Pinus taeda L. NTSL2021Wild material2137764FSNS 9345
138FSNS 9346FSNS 9346Pinus taeda L. NTSL2021Wild material2137765FSNS 9346
139FSNS 9347FSNS 9347Pinus taeda L. NTSL2021Wild material2137766FSNS 9347
140FSNS 9348FSNS 9348Pinus taeda L. NTSL2021Wild material2137767FSNS 9348
141FSNS 9349FSNS 9349Pinus taeda L. NTSL2021Wild material2137768FSNS 9349
142FSNS 9350FSNS 9350Pinus taeda L. NTSL2021Wild material2137769FSNS 9350
143FSNS 9351FSNS 9351Pinus taeda L. NTSL2021Wild material2137770FSNS 9351
144FSNS 9352FSNS 9352Pinus taeda L. NTSL2021Wild material2137771FSNS 9352
145FSNS 9353FSNS 9353Pinus taeda L. NTSL2021Wild material2137772FSNS 9353
146FSNS 9354FSNS 9354Pinus taeda L. NTSL2021Wild material2137773FSNS 9354
147FSNS 9355FSNS 9355Pinus taeda L. NTSL2021Wild material2137774FSNS 9355
148FSNS 9356FSNS 9356Pinus taeda L. NTSL2021Wild material2137775FSNS 9356
149FSNS 9357FSNS 9357Pinus taeda L. NTSL2021Wild material2137776FSNS 9357
150FSNS 9358FSNS 9358Pinus taeda L. NTSL2021Wild material2137777FSNS 9358
151FSNS 9359FSNS 9359Pinus taeda L. NTSL2021Wild material2137778FSNS 9359
152FSNS 9360FSNS 9360Pinus taeda L. NTSL2021Wild material2137779FSNS 9360
153FSNS 9361FSNS 9361Pinus taeda L. NTSL2021Wild material2137780FSNS 9361
154FSNS 9362FSNS 9362Pinus taeda L. NTSL2021Wild material2137781FSNS 9362
155FSNS 9363FSNS 9363Pinus taeda L. NTSL2021Wild material2137782FSNS 9363
156FSNS 9364FSNS 9364Pinus taeda L. NTSL2021Wild material2137783FSNS 9364
157FSNS 9365FSNS 9365Pinus taeda L. NTSL2021Wild material2137784FSNS 9365
158FSNS 9366FSNS 9366Pinus taeda L. NTSL2021Wild material2137785FSNS 9366
159FSNS 9367FSNS 9367Pinus taeda L. NTSL2021Wild material2137786FSNS 9367
160FSNS 9368FSNS 9368Pinus taeda L. NTSL2021Wild material2137787FSNS 9368
161FSNS 9369FSNS 9369Pinus taeda L. NTSL2021Wild material2137788FSNS 9369
162FSNS 9370FSNS 9370Pinus taeda L. NTSL2021Wild material2137789FSNS 9370
163FSNS 9371FSNS 9371Pinus taeda L. NTSL2021Wild material2137790FSNS 9371
164FSNS 9372FSNS 9372Pinus taeda L. NTSL2021Wild material2137791FSNS 9372
165FSNS 9373FSNS 9373Pinus taeda L. NTSL2021Wild material2137792FSNS 9373
166FSNS 9374FSNS 9374Pinus taeda L. NTSL2021Wild material2137793FSNS 9374
167FSNS 9375FSNS 9375Pinus taeda L. NTSL2021Wild material2137794FSNS 9375
168FSNS 9376FSNS 9376Pinus taeda L. NTSL2021Wild material2137795FSNS 9376
169FSNS 9377FSNS 9377Pinus taeda L. NTSL2021Wild material2137796FSNS 9377
170FSNS 9378FSNS 9378Pinus taeda L. NTSL2021Wild material2137797FSNS 9378
171FSNS 9379FSNS 9379Pinus taeda L. NTSL2021Wild material2137798FSNS 9379
172FSNS 9380FSNS 9380Pinus taeda L. NTSL2021Wild material2137799FSNS 9380
173FSNS 9381FSNS 9381Pinus taeda L. NTSL2021Wild material2137800FSNS 9381
174FSNS 9382FSNS 9382Pinus taeda L. NTSL2021Wild material2137801FSNS 9382
175FSNS 9383FSNS 9383Pinus taeda L. NTSL2021Wild material2137802FSNS 9383
176FSNS 9384FSNS 9384Pinus taeda L. NTSL2021Wild material2137803FSNS 9384
177FSNS 9385FSNS 9385Pinus taeda L. NTSL2021Wild material2137804FSNS 9385
178FSNS 9386FSNS 9386Pinus taeda L. NTSL2021Wild material2137805FSNS 9386
179FSNS 9387FSNS 9387Pinus taeda L. NTSL2021Wild material2137806FSNS 9387
180FSNS 9388FSNS 9388Pinus taeda L. NTSL2021Wild material2137807FSNS 9388
181FSNS 9389FSNS 9389Pinus taeda L. NTSL2021Wild material2137808FSNS 9389
182FSNS 9390FSNS 9390Pinus taeda L. NTSL2021Wild material2137809FSNS 9390
183FSNS 9391FSNS 9391Pinus taeda L. NTSL2021Wild material2137810FSNS 9391
184FSNS 9392FSNS 9392Pinus taeda L. NTSL2021Wild material2137811FSNS 9392
185FSNS 9393FSNS 9393Pinus taeda L. NTSL2021Wild material2137812FSNS 9393
186FSNS 9394FSNS 9394Pinus taeda L. NTSL2021Wild material2137813FSNS 9394
187FSNS 9395FSNS 9395Pinus taeda L. NTSL2021Wild material2137814FSNS 9395
188FSNS 9396FSNS 9396Pinus taeda L. NTSL2021Wild material2137815FSNS 9396
189FSNS 9397FSNS 9397Pinus taeda L. NTSL2021Wild material2137816FSNS 9397
190FSNS 9398FSNS 9398Pinus taeda L. NTSL2021Wild material2137817FSNS 9398
191FSNS 9399FSNS 9399Pinus taeda L. NTSL2021Wild material2137818FSNS 9399
192FSNS 9400FSNS 9400Pinus taeda L. NTSL2021Wild material2137819FSNS 9400
193FSNS 9401FSNS 9401Pinus taeda L. NTSL2021Wild material2137820FSNS 9401
194FSNS 9402FSNS 9402Pinus taeda L. NTSL2021Wild material2137821FSNS 9402
195FSNS 9403FSNS 9403Pinus taeda L. NTSL2021Wild material2137822FSNS 9403
196FSNS 9404FSNS 9404Pinus taeda L. NTSL2021Wild material2137823FSNS 9404
197FSNS 9405FSNS 9405Pinus taeda L. NTSL2021Wild material2137824FSNS 9405
198FSNS 9406FSNS 9406Pinus taeda L. NTSL2021Wild material2137825FSNS 9406
199FSNS 9407FSNS 9407Pinus taeda L. NTSL2021Wild material2137826FSNS 9407
200FSNS 9408FSNS 9408Pinus taeda L. NTSL2021Wild material2137827FSNS 9408
201FSNS 9409FSNS 9409Pinus taeda L. NTSL2021Wild material2137828FSNS 9409
202FSNS 9410FSNS 9410Pinus taeda L. NTSL2021Wild material2137829FSNS 9410
203FSNS 9411FSNS 9411Pinus taeda L. NTSL2021Wild material2137830FSNS 9411
204FSNS 9412FSNS 9412Pinus taeda L. NTSL2021Wild material2137831FSNS 9412
205FSNS 9413FSNS 9413Pinus taeda L. NTSL2021Wild material2137832FSNS 9413
206FSNS 9414FSNS 9414Pinus taeda L. NTSL2021Wild material2137833FSNS 9414
207FSNS 9415FSNS 9415Pinus taeda L. NTSL2021Wild material2137834FSNS 9415
208FSNS 9416FSNS 9416Pinus taeda L. NTSL2021Wild material2137835FSNS 9416
209FSNS 9417FSNS 9417Pinus taeda L. NTSL2021Wild material2137836FSNS 9417
210FSNS 9418FSNS 9418Pinus taeda L. NTSL2021Wild material2137837FSNS 9418
211FSNS 9419FSNS 9419Pinus taeda L. NTSL2021Wild material2137838FSNS 9419
212FSNS 9420FSNS 9420Pinus taeda L. NTSL2021Wild material2137839FSNS 9420
213FSNS 9421FSNS 9421Pinus taeda L. NTSL2021Wild material2137840FSNS 9421
214FSNS 9422FSNS 9422Pinus taeda L. NTSL2021Wild material2137841FSNS 9422
215FSNS 9423FSNS 9423Pinus taeda L. NTSL2021Wild material2137842FSNS 9423
216FSNS 9424FSNS 9424Pinus taeda L. NTSL2021Wild material2137843FSNS 9424
217FSNS 9425FSNS 9425Pinus taeda L. NTSL2021Wild material2137844FSNS 9425
218FSNS 9426FSNS 9426Pinus taeda L. NTSL2021Wild material2137845FSNS 9426
219FSNS 9427FSNS 9427Pinus taeda L. NTSL2021Wild material2137846FSNS 9427
220FSNS 9428FSNS 9428Pinus taeda L. NTSL2021Wild material2137847FSNS 9428
221FSNS 9429FSNS 9429Pinus taeda L. NTSL2021Wild material2137848FSNS 9429
222FSNS 9430FSNS 9430Pinus taeda L. NTSL2021Wild material2137849FSNS 9430
223FSNS 9431FSNS 9431Pinus taeda L. NTSL2021Wild material2137850FSNS 9431
224FSNS 9432FSNS 9432Pinus taeda L. NTSL2021Wild material2137851FSNS 9432
225FSNS 9433FSNS 9433Pinus taeda L. NTSL2021Wild material2137852FSNS 9433
226FSNS 9434FSNS 9434Pinus taeda L. NTSL2021Wild material2137853FSNS 9434
227FSNS 9435FSNS 9435Pinus taeda L. NTSL2021Wild material2137854FSNS 9435
228FSNS 9436FSNS 9436Pinus taeda L. NTSL2021Wild material2137855FSNS 9436
229FSNS 9437FSNS 9437Pinus taeda L. NTSL2021Wild material2137856FSNS 9437
230FSNS 9438FSNS 9438Pinus taeda L. NTSL2021Wild material2137857FSNS 9438
231FSNS 9439FSNS 9439Pinus taeda L. NTSL2021Wild material2137858FSNS 9439
232FSNS 9440FSNS 9440Pinus taeda L. NTSL2021Wild material2137859FSNS 9440
233FSNS 9441FSNS 9441Pinus taeda L. NTSL2021Wild material2137860FSNS 9441
234FSNS 9442FSNS 9442Pinus taeda L. NTSL2021Wild material2137861FSNS 9442
235FSNS 9443FSNS 9443Pinus taeda L. NTSL2021Wild material2137862FSNS 9443
236FSNS 9444FSNS 9444Pinus taeda L. NTSL2021Wild material2137863FSNS 9444
237FSNS 9445FSNS 9445Pinus taeda L. NTSL2021Wild material2137864FSNS 9445
238FSNS 9446FSNS 9446Pinus taeda L. NTSL2021Wild material2137865FSNS 9446
239FSNS 9447FSNS 9447Pinus taeda L. NTSL2021Wild material2137866FSNS 9447
240FSNS 9448FSNS 9448Pinus taeda L. NTSL2021Wild material2137867FSNS 9448
241FSNS 9449FSNS 9449Pinus taeda L. NTSL2021Wild material2137868FSNS 9449
242FSNS 9450FSNS 9450Pinus taeda L. NTSL2021Wild material2137869FSNS 9450
243FSNS 9451FSNS 9451Pinus taeda L. NTSL2021Wild material2137870FSNS 9451
244FSNS 9452FSNS 9452Pinus taeda L. NTSL2021Wild material2137871FSNS 9452
245FSNS 9453FSNS 9453Pinus taeda L. NTSL2021Wild material2137872FSNS 9453
246FSNS 9454FSNS 9454Pinus taeda L. NTSL2021Wild material2137873FSNS 9454
247FSNS 9455FSNS 9455Pinus taeda L. NTSL2021Wild material2137874FSNS 9455
248NA 88154NCBG-323Pinus taeda L. North Carolina, United StatesNASEED2019Wild material2098414NA 88154
249NA 88028NCBG-358Pinus taeda L. Virginia, United StatesNASEED2018Wild material1965927NA 88028
250PI 704859 sosV. fuscatum NCBG-440Vaccinium fuscatum Aiton North Carolina, United StatesCOR2021Wild materialPI assigned before phyical inventory of W6 shipment and is missing. Maintain COR as site in case seeds are recovered. Berries glaucous, calyx not oppressed2116310PI 704859 sos
251PI 704860 sosV. fuscatum NCBG-441Vaccinium fuscatum Aiton North Carolina, United StatesCOR2021Wild materialPI assigned before phyical inventory of W6 shipment and is missing. Maintain COR as site in case seeds are recovered. Berries black, glabrous2116311PI 704860 sos
252PI 702690MARSB-175Chasmanthium laxum (L.) H. O. Yates Delaware, United StatesS9SEED2019Wild material2097507PI 702690
253PI 704823 sosV. corymbosum MARSB-141Vaccinium corymbosum L. Delaware, United StatesCORSEED2019Wild material2097497PI 704823 sos
254PI 691218V. arboreum GN2018 Manatee Springs State Park 6Vaccinium arboreum Marshall Florida, United StatesCOR2019COLLECTED12/06/2018Manatee Springs State Park29.49854500, -82.9745830018Partial sun. Side of the road. Broadleaf leaf litter. Nearby vegetation included; Laurel oak (Quercus laurifolia), bald cypress (Taxodium distichum), loblolly pine (Pinus taeda), Rhododendron spp., saw palmetto (Serenoa repens). Native soil pH = 5.03. NNE exposure/aspect.Wild materialGerardo Nunez USDA plant collecting trip to Florida 2018, 20192094710PI 691218
255PI 710477NCBG-582Chamaecrista fasciculata (Michx.) Greene North Carolina, United StatesS9SEED2018Wild material1965981PI 710477
256PI 710478NCBG-750Chamaecrista fasciculata (Michx.) Greene Virginia, United StatesS9SEED2018Wild material1966043PI 710478
257PI 710481NCBG-748Chamaecrista nictitans (L.) Moench Virginia, United StatesS9SEED2018Wild material1966042PI 710481
258PI 710499NCBG-752Sesbania exaltata (Raf.) Rydb. North Carolina, United StatesS9SEED2018Wild material1966044PI 710499
259PI 710513NCBG-209Eleocharis fallax Weath. North Carolina, United StatesS92018Wild material1965860PI 710513
260PI 661254TX-027Daucus pusillus Michx. Texas, United StatesNC7SEED2011COLLECTED05/27/2010Along County Road 1090, Indian Hills area, approximately 0.5 mile south of Little Cow Creek, Newton County.31.04669000, -93.78282000122Roadside row/forest edge. Area primarily used for timber/tree farms. Full sun. Associated with Carya texana, Crataegus uniflora, Hamamelis virginiana, Pinus taeda, Trillium gracile, and Viburnum dentatum.Wild material1862436PI 661254
261PI 667471TX-25Rudbeckia hirta L. Texas, United StatesOPGC2010COLLECTED05/27/2010Upper West Gulf Coastal Plain. Newton County. CR 1090 Roadside approx. 0.25 miles south of Little Cow Creek. Collection made in Indian Hills area.31.04819400, -93.78247200116Roadside ROW/forest edge. Land form: Rolling hills. Land Use: Roadside ROW. Geology: Sandstone. Soil Texture: Sandy. Soil color: Reddish-tan.Wild materialPlant to 70 cm tall, gold-yellow ray petals.1897306PI 667471
262PI 673986TX-03Rudbeckia grandiflora (Sweet) C. C. Gmel. ex DC. Texas, United StatesOPGC2010COLLECTED05/26/2010Upper West Gulf Coastal Plain. Harrison County. South of Marshall Texas. East on 2625, cross 31, left onto CR 1111, Brad spann road veer right.32.47050000, -94.2159440097Meadow(Maintained ROW under power lines). Land form: Rolling hills. Land Use: Roadside ROW. Geology: Sandstone. Soil Texture: Sandy. Soil Color: Brown.Wild materialErect, clumped, glabrous to 60 cm tall. Flowers numerous, yellow ray florets.1897287PI 673986
263PI 673989TX-11Rudbeckia grandiflora (Sweet) C. C. Gmel. ex DC. Texas, United StatesOPGC2010COLLECTED05/26/2010Upper West Gulf Coastal Plain. Marion County. Smithland Cuttoff Road approx. 1 mile east of SH 43.32.76347200, -94.1815280053Roadside ROW/forest edge(tree farm/harvesting area). Land form: Flat. Land Use: Roadside ROW. Geology: Sandstone. Soil Texture: Sandy. Soil Color: Tan.Wild materialErect, coarse perennial to 125 cm tall; leaves mostly basal; ray flowers yellow and drooping.1897293PI 673989
264PI 673991TX-23Coreopsis lanceolata L. Texas, United StatesOPGC2010COLLECTED05/27/2010Upper West Gulf Coastal Plain. Jasper County. Roadside ROW along R255.31.05984000, -94.00301000135Roadside ROW/forest edge. Land form: Rolling hills. Land Use: Roadside ROW. Geology: Sandstone. Soil Texture: Sandy. Soil color: Reddish-orange.Wild materialErect, clumped, glabrous to 70 cm tall. Flowers numerous, yellow ray florets.1897304PI 673991
265PI 673992TX-30Coreopsis lanceolata L. Texas, United StatesOPGC2010COLLECTED05/27/2010Upper West Gulf Coastal Plain. Newton County. Roadside approx. 1.5 miles south of 1416 on SH 87.30.58986100, -93.7943060027Roadside ROW/forest edge. Land form: Flat. Land Use: Roadside ROW. Geology: Sandstone. Soil Texture: Sandy to clay. Soil color: Greyish-brown.Wild materialErect, clumped, glabrous to 70 cm tall. Flowers with yellow ray florets, mostly gone to seed.1897309PI 673992
266PI 653297R. argutus HD-2007-070Rubus argutus Link Mississippi, United StatesCOR2007COLLECTED06/09/2007Marshall County, northwest of Potts Camp off route 178 onto George Mann Road onto Lake Shore Drive at a drainage ditch in the community of Lake Center.34.69310000, -89.36150000120Open area in drainage ditch growing on the perimeter road of a lake. Associated Plants: Rhus typhina, Vitis rotundifolia, Pinus taeda, Salix sp., Lonicera japonica, Liquidambar styraciflua and Acer negundo.Wild materialKim Hummer, Michael Dossett collection from Mississippi.

1730104PI 653297
267PI 657239V. fuscatum HD-2007-056Vaccinium fuscatum Aiton Alabama, United StatesCOR2007COLLECTED06/07/2007Calhoun County, Anniston Museum of Natural History grounds. Woodland trail 0.5 mile from visitors center. Found in the moister areas, such as dried up stream beds.33.69411000, -85.82097000230Grey loam - from sandstone. South slope 20 percent. Open woods. Associated with: Quercus nigra, Q. stellata, Q. prinus, Vaccinium arboreum, Pinus taeda and Carya.Wild materialKim Hummer, Michael Dossett collected from Alabama.

1730134PI 657239
268PI 649044008Echinacea sanguinea Nutt. Louisiana, United StatesNC7HEAD1997COLLECTED08/07/1997Kisatchie National Forest, near Leesville, Vernon Parish. Please contact curator for specific site location.31.00000000, -93.16666667160Upland long-leaf pine. ~70% exposure on level ground. Sandy soil with no stones and fair drainage.Wild materialPlants were 2-2.5 feet tall in occasional abundance with light pink flowers and some branching.1547199PI 649044
269NA 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
270NA 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
271NA 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
272NA 891582025RJLSEUS-06Cornus florida L. Alabama, United StatesNA2025COLLECTED10/01/2025Coosa Wildlife Management Area: along the edge of gated dirt road on the west side of Coosa County Road 29, 0.3 kilometers north of Hatchet Creek.32.86402200, -86.33871400108Plants are growing in part sun to shade on dry-mesic slopes above the road cut on the gated dirt road; most likely a road for access for fire control/forest management. The forest is a combination of deciduous and evergreen with evergreens primarily comprised of Pinus taeda. The habitat was quite dry during this time of year. Slope: 5 to 20 percent. Aspect: North. Soils: The primary soil in the area of this collection is classified as Madison-Louisa Series complex, 15 to 30 percent slopes, moderately eroded (MdE2). The Madison Series soils are very deep, well drained soils with medium runoff found on Piedmont uplands in interstream divides, ridges and side slopes. They are comprised of residuum weathered from felsic or intermediate, high-grade metamorphic or igneous rocks high in content of mica. Slopes range from 2 to 60 percent and soil is typically strongly acidic. Louisa Series soils The Louisa Series soils consist of shallow, somewhat excessively drained soils which formed over mica gneiss and schist bedrock. They occur on Piedmont uplands. Slopes are 6 to 80 percent. This soil is moderately acid. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). Geology: The underlying geology of this area is of Precambrian to Paleozoic origin and characterized as Hatchet Creek Group; Pinchoulee Gneiss Formation. It is characterized by medium to fine-grained migmatitic, locally garnetiferous biotite-feldspar gneiss, commonly saturated with granitic pods. (Source: USGS Alabama Geologic Map Data).Wild material2193004NA 89158
273NA 89115TLM25-04aHamamelis ovalis S. W. Leonard Texas, United StatesNA2025COLLECTED07/10/2025State Highway 87 approximately 3.25 kilometers north of the crossroad junction with Texas Recreational Road 255 (RE 255); plants were growing in the narrow buffer woods along the east side of the highway.31.12051300, -93.72628100138The habitat is an upland mixed coniferous and deciduous woodlands in part to full shade and dry conditions, often under drought stress. Plants seem to always occur on the top of dry ridges or well-drained slopes. Slope: 0 to 1 percent. Aspect: N/A. Soils: The soils of this collection area are classified as Tehran-Letney Association, hilly (TLE) soils. The Tehran Series (55%) consists of deep, somewhat excessively drained, moderately rapidly permeable soils on uplands. They formed in thick loamy and sandy sediments on the Western Coastal Plain. These soils are on gently sloping to moderately steep uplands with slopes ranging from 1 to 20 percent. The Letney Series (30%) consists of deep, well drained, moderately rapidly permeable, upland soils. They formed in thick sandy and loamy sediments of the coastal plains. These soils are on gently sloping to moderately steep uplands with slopes ranging from 1 to 20 percent. Soil pH ranges from 4.5 to 6.0. The minor soil components include Doucette Series (10%) and Boykin Series (5%) soils. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). Geology: The underlying geology of this area is of Oligocene origin and characterized as Catahoula Formation. This formation is extensive and deep in Texas, up to 185 meters thick. In the area of the collection the Catahoula Formation is primarily mudstone and sand. The upper 90-150 meters is mudstone that is tuffaceous, and sandy; also, occasionally, with some bentonitic clay. (Source: USGS Texas Geologic Map Data).Wild material2191654NA 89115
274NA 8893024Flam16Rhododendron canescens (Michx.) Sweet Georgia, United StatesNA2025COLLECTED09/10/2024DeKalb County: Stone Mountain: Stone Mountain Park: slope near Robert E. Lee Boulevard.33.80238000, -84.15508000286Dry, shady slope. Growing in 3/4 shade. Slope: 30 to 45 degrees. Aspect: West-southwest.Wild materialNote: Seeds from three different plants collected at the same spot were bulked together in this accession; the lowest field collection number (24Flam16) has been chosen as the primary for this record. It appears from the notes that the identity is slightly uncertain; possibly not pure R. canescens.2172813NA 88930
275NA 8893324Flam40Agarista populifolia (Lam.) Judd South Carolina, United StatesNA2025COLLECTED09/12/2025Robertville, SC: Gillison Branch Road (plants on both sides of road).32.58673000, -81.1930000031Shady swamp forest with road running between Agarista population. Agarista was the predominant plant throughout. Soggy but solid ground, especially on northern side of road. Growing in 3/4 shade. Slope: Generally flat.Wild materialNote: Two field collections, 24Flam40 and 24Flam41, were combined together in this USNA accession, with the former identifier being used as the primary one.2172816NA 88933
276NA 88747TXWL2025-038Ilex opaca Aiton Texas, United StatesNA2025COLLECTED01/23/2025Milam, Texas: On flat road, private land.31.43288000, -93.88208000Upland shortleaf pine stand with sandy loam; closed canopy.Wild material2171021NA 88747
277NA 88981TXWL2025-031Ilex opaca Aiton Texas, United StatesNA2025COLLECTED01/07/2025South of Jericho community.31.67015000, -94.25641000Western sandy lands; small grove of Ilex opaca in upland position above a baygall. Bare ground cover with Ilex opaca regeneration. Adjacent to a loblolly pine plantation and a new longleaf pine plantation.Wild material2170965NA 88981
278NA 88982TXWL2025-032Ilex opaca Aiton Texas, United StatesNA2025COLLECTED01/07/2025South of Jericho community.31.66973000, -94.25613000Western sandy lands; edge of small grove of Ilex opaca with sun exposure in upland position above a baygall. Bare ground cover with Ilex opaca regeneration. Adjacent to a new longleaf pine plantation located on fireline.Wild material2170966NA 88982
279NA 88983TXWL2025-033Ilex opaca Aiton Texas, United StatesNA2025COLLECTED01/12/2025Adjacent to Toledo Bend reservoir in Huxley Bay community, eastern Shelby County.31.77133000, -93.85094000Low area with heavy duff near reservoir.Wild material2170967NA 88983
280NA 88987TXWL2025-037Ilex opaca Aiton Texas, United StatesNA2025COLLECTED01/13/2025Fairmount Township: Sabine National Forest C-139: Foxhunters Hill.31.18365000, -93.72211000Baygall below a longleaf pine stand.Wild material2170971NA 88987
281NA 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
282NA 88479TXWL2024-029Ilex longipes Chapm. ex Trel. Texas, United StatesNA2024COLLECTED11/20/2024Little Cow Creek.31.06221000, -93.79603000Upland position above perennial creek.Wild material2169906NA 88479
283NA 87842TRX241117-08SCIlex opaca Aiton South Carolina, United StatesNA2024COLLECTED11/17/2024Francis Marion National Forest.33.15167000, -79.6025300031Wild material2169895NA 87842
284NA 87845TRX241119-01GAIlex coriacea (Pursh) Chapm. Georgia, United StatesNA2024COLLECTED11/19/2024St. Simons Island: Guale Preserve.31.21861000, -81.368720006Wild material2169898NA 87845
285NA 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
286NA 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
287NA 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
288NA 88838RJL-RM2023FLAL-012Ilex opaca Aiton Florida, United StatesNA2023COLLECTED12/08/2023North side of Sid Hayes Road approximately 65 m southeast of the junction with Watson Road.30.83277400, -87.2432450032Growing in shade, part shade and light shade in dry mesic to moist, occasionally wet, habitats along the edge of the road and in the woodland interior. This species is remarkably adaptable. The only drawback to the range of habitats is that in deep shade, very few fruit can be found, presumably because there is far less flower production and/or fewer pollinators. Slope: 0 to 3 percent. Aspect: South. 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 Dothan Series fine sandy loam soils (5 to 8 percent slopes). The Dothan Series consists of very deep, well drained soils that formed in thick beds of unconsolidated, medium to fine-textured marine sediments. Dothan soils are on interfluves. The surface 0-33 cm is characterized by sandy-loam, well-drained soils that are strongly acid. From 33-200 cm they are characterized by sandy clay loam soils that are more moisture retentive and strongly acid. (Source: NRCS Web Soil Survey.)Wild material2165668NA 88838
289NA 88840RJL-RM2023FLAL-014Rhododendron viscosum (L.) Torr. Florida, United StatesNA2023COLLECTED12/11/2023Property of Floyd Griffith off View Drive on the southwest side of McCormick Lake.30.63247000, -85.3371820056Plants are growing primarily in part shade a few meters above the lake, generally in areas that appear dry, but clearly are associated with hillside seeps. While much of the area has been cultivated, the remnant native flora are largely broadleaved evergreen shrub and deciduous shrub and tree species. Slope: 10 to 15 percent. Aspect: Northeast. The underlying geology of this area is the Citronelle Formation of Pliocene origin and consists of gray to orange, often mottled, unconsolidated to poorly consolidated, very fine to very coarse, poorly sorted, clean to clayey sands. It contains significant amounts of clay, silt and gravel which may occur as beds and lenses and may vary considerably over short distances. Limonite nodules and limonite-cemented beds are common. (Source: USGS Florida Geologic Map Data.) The surface soil profile of this area is primarily Pamlico-Pantego-Rutlege Association. The Pamlico series consists of very poorly drained soils that formed in decomposed organic material underlain by dominantly sandy sediment. The soils are on nearly level flood plains, bays, and depressions of the Coastal Plain. Slopes are less than 1 percent. Pamlico soils have 0.4-1.3 meters of organic material over dominantly sandy sediments. Reaction is extremely in the organic layers and ranges from extremely acid to strongly acid in the underlying mineral layers. The Pantego series consists of very deep, very poorly drained, moderately permeable soils that formed in thick loamy sediments on the Southern Coastal Plain and Atlantic Coast Flatwoods. Slopes are less than 2 percent. This soil is strongly acid. The Rutlege series comprises very deep, very poorly drained persistently wet soils on flats, depressions and floodplains where shallow ponding is common. They are of marine or fluvial sediment origin. Thickness of these loamy sandy soils is greater than 1.5 meters and a reaction from extremely acid to strongly acid. (Source: NRCS Web Soil Survey.)Wild material2165670NA 88840
290NA 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
291NA 88842RJL-RM2023FLAL-016Pinckneya bracteata (W. Bartram) Raf. Florida, United StatesNA2023COLLECTED12/11/2023West side of Scott Road in woodlands approximately 0.13 kilometers north of where the road crosses Ecofina Creek. As of 2023, this road appears permanently closed from previous hurricane damage.30.55633300, -85.4352000038Plants are growing in the understory of a mixed evergreen and deciduous bottomland forest associated with the Ecofina Creek. Plans are growing mostly on hummocks in a very wet, acidic wetland habitat. 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 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 material2165672NA 88842
292NA 88843RJL-RM2023FLAL-017Rhododendron austrinum (Small) Rehder Florida, United StatesNA2023COLLECTED12/11/2023Holmes Creek at Live Oak Landing: plants found on the low bluff along the south side of Holmes Creek accessed by foot from a parking lot on Live Oak Landing Road that dead ends into the creek.30.59043500, -85.838998007Plants are growing in part shade to shade on the top and slope of the low bluff overlooking Holmes Creek in a mixed deciduous and evergreen forest. The dry mesic habitat has relatively low competition and is quite acidic. Slope: 0 to 45 percent. Aspect: Northwest. 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 Nankin-Cowarts-Lakeland Complex. 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 Cowarts Series consists of very deep, moderately well and well drained soils on ridge tops and side slopes on uplands of the Coastal Plain Major Land Resource Area. They formed in loamy marine sediments. Slopes range from 1 to 60 percent. The Lakeland series consists of very deep, excessively drained, rapid to very rapidly permeable soils on uplands. They formed in thick beds of eolian or marine and/or fluvio-marine sands. Thickness of the sand exceeds 2 meters. Silt plus clay in the upper meter ranges from 5-10 percent. Reaction ranges from very strongly acid to moderately acid throughout. (Source: NRCS Web Soil Survey.)Wild material2165673NA 88843
293NA 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
294WLP 3377TXWL2023-024Viburnum dentatum L. Texas, United StatesNA2023COLLECTED12/13/2023Roadside between Big Cow Creek and Hardy Cemetery.31.03548900, -93.85086800Roadside; mesic, mixed hardwood/pine forest.Wild material2165656WLP 3377
295NA 88812TXWL2023-018Ilex ambigua Torr. Texas, United StatesNA2023COLLECTED12/05/2023Davy Crockett National Forest: Forest Service Road 526 roadside.31.49017400, -95.22343300Roadside. Shortleaf mixed upland hardwood forest; dry-mesic.Wild material2165615NA 88812
296NA 88814TXWL2023-021Ilex ambigua Torr. Texas, United StatesNA2023COLLECTED12/09/2023Roadside between Big Cow Creek and Hardy Cemetery.31.03548900, -93.85086800Roadside; mesic, mixed hardwood/pine forest.Wild material2165618NA 88814
297NA 88815TXWL2023-022Ilex opaca Aiton Texas, United StatesNA2023COLLECTED12/10/2023Angelina National Forest: Upland Island Wilderness Area: Neches River bottom.31.03919400, -94.37937900Bottomland hardwood forest.Wild material2165619NA 88815
298NA 88816TXWL2023-023Ilex decidua Walter Texas, United StatesNA2023COLLECTED12/10/2023Angelina National Forest: Upland Island Wilderness Area: Neches River bottom.31.03478500, -94.38286600Bottomland hardwood forest.Wild material2165620NA 88816
299NA 88800TXWL2023-015Ilex longipes Chapm. ex Trel. Texas, United StatesNA2023COLLECTED11/15/2023Sabine National Forest: Compartment 65 along County Road 131 near White Rock, Texas.31.55793500, -94.01980900Upland; mixed hardwood and pine; sandy soil; rocky outcrops.Wild material2159157NA 88800
300WLP 3343TXWL2023-014Croton michauxii G. L. Webster Texas, United StatesNA2023COLLECTED11/07/2023Angelina National Forest: Compartment 84 Black Branch Area.31.03849000, -94.18679000Glade area on the Catahould/Fleming formation.Wild material2159156WLP 3343
301NA 88696RJL2023NCSC-001Rhododendron catawbiense Michx. North Carolina, United StatesNA2023COLLECTED11/12/2023Duke Forest property along New Hope Creek. The collection site is accesses by foot along trails.35.98317700, -79.01856200103Plants growing in shade to part-shade of an upland very dry woodland habitat that is mostly deciduous. The site is steeply sloped underlain by rocky outcrop. Slope: 15 to 25 percent. Aspect: Northwest. The underlying geology of this area is of Cambrian/Late Proterozoic origin and characterized as a Metamorphosed Granitic Rock. It is megacrystic and well foliated; locally contains hornblende. Chapel Hill, Chatham, Farrington, Meadow Flats, Mt. Moriah, Parks Crossroads plutons, and Roxboro and Vance County suites. (Source: USGS North Carolina Geologic Map Data.) The primary soil type in the collection area is classified as Wedowee sandy loam, 15 to 25 percent slopes. Wedowee Series consists of very deep, well drained, moderately permeable soils that formed in residuum weathered from felsic igneous and metamorphic rocks of the Piedmont uplands. These soils are on narrow ridges and on side slopes of uplands. Slopes are dominantly 6 to 25 percent but ranges from 0 to 60 percent. The strata range from dark brown and brownish yellow to strong brown. They are mostly sandy loam; moderate fine granular structure; very friable; strongly acid. (Source: NRCS Web Soil Survey.) Wild material2159124NA 88696
302NA 88697RJL2023NCSC-002Ilex amelanchier M. A. Curtis ex Chapm. North Carolina, United StatesNA2023COLLECTED11/12/2023Goose Pond Bay (Nature Conservancy-owned site): wetlands on the south side of McNeil Road approximately 0.64 kilometers west of junction with McIntosh Road.34.88254100, -79.0991570060Plants are growing in part-shade to sun of a Carolina Bay habitat with seasonally moist to wet, acidic conditions. Slope: N/A. Aspect: N/A. The underlying geology of this area is of Cretaceous origin and characterized as Black Creek Formation. The formation is comprised of clay that is gray to black and lignitic. It contains thin beds and laminae of fine-grained micaceous sand and thick lenses of cross-bedded sand. This formation has glauconitic, fossiliferous clayey sand lenses in the upper part. (Source: USGS North Carolina Geologic Map Data.) The primary soil type in the collection area is classified as McColl loam soil. The McColl Series consists of poorly drained, slowly permeable soils that are shallow or moderately deep to a fragipan and very deep to bedrock. They formed in loamy sediments in oval depressions on the Coastal Plain. The soils are nearly level or concave. Runoff is frequently ponded. Slopes are less than 2 percent. These soils are strongly acid. (Source: NRCS Web Soil Survey.)Wild material2159125NA 88697
303NA 88698RJL2023NCSC-003Ilex laevigata (Pursh) A. Gray North Carolina, United StatesNA2023COLLECTED11/13/2023Sandhills Game Land: north side of Pulpwood Road approximately 0.11 km southwest of the junction with Tyner Road.34.95939500, -79.48676300114Plants growing in shade to part-shade of a spring fed wetland that is a mixed evergreen and deciduous woodland habitat. Slope: 3 to 10 percent. Aspect: Northeast. The underlying geology of this area is of Tertiary origin and characterized as Pinehurst Formation. It is comprised of sand that is medium- to coarse-grained, cross-bedding and rhythmic bands of clayey sand common, unconsolidated. (Source: USGS North Carolina Geologic Map Data.) The primary soil type in the area of this collection is classified as Pelion loamy sand, 6 to 10 percent slopes. Pelion Series soils are very deep, moderately well-drained soils with moderately slow to slow permeability. The upper 30 cm of the strata is sandy loam to sandy clay loam ranging from grayish brown to reddish yellow. This stratum has a weak fine granular structure and is very friable. It contains many fine roots and is moderately acid. Deeper strata to 2 m range from yellow to yellowish red sandy clay, often with masses of oxidized iron and few fine prominent light gray iron depletions; they are strongly acid. (Source: NRCS Web Soil Survey.)Wild material2159126NA 88698
304NA 88699RJL2023NCSC-004Lyonia ligustrina (L.) DC. North Carolina, United StatesNA2023COLLECTED11/13/2023Sandhills Game Land: north side of Pulpwood Road approximately 0.11 km southwest of the junction with Tyner Road.34.95949000, -79.48665600107Plants growing in part-shade to sun on the moist margins of a spring fed wetland that is a mixed evergreen and deciduous woodland habitat. The underlying soils are moist even during dry periods due to seepage from the wetland. Slope: 3 to 10 percent. Aspect: Northeast. The underlying geology of this area is of Tertiary origin and characterized as Pinehurst Formation. It is comprised of sand that is medium- to coarse-grained, cross-bedding and rhythmic bands of clayey sand common, unconsolidated. (Source: USGS North Carolina Geologic Map Data.) The primary soil type in the area of this collection is classified as Pelion loamy sand, 6 to 10 percent slopes. Pelion Series soils are very deep, moderately well-drained soils with moderately slow to slow permeability. The upper 30 cm of the strata is sandy loam to sandy clay loam ranging from grayish brown to reddish yellow. This stratum has a weak fine granular structure and is very friable. It contains many fine roots and is moderately acid. Deeper strata to 2 m range from yellow to yellowish red sandy clay, often with masses of oxidized iron and few fine prominent light gray iron depletions; they are strongly acid. (Source: NRCS Web Soil Survey.)Wild material2159127NA 88699
305NA 88700RJL2023NCSC-005Clethra alnifolia L. North Carolina, United StatesNA2023COLLECTED11/13/2023Sandhills Game Land: north side of Pulpwood Road approximately 0.11 km southwest of the junction with Tyner Road.34.96008500, -79.48751100108Plants growing in shade to part-shade as well as sun (when moisture is abundant) of a spring fed wetland that is comprised of a mixed evergreen and deciduous woodland habitat. Slope: 3 to 10 percent. Aspect: Various. : The underlying geology of this area is of Cretaceous origin and characterized as Middendorf Formation. It is characterized by 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 area of this collection is classified as Pelion loamy sand, 6 to 10 percent slopes. Pelion Series soils are very deep, moderately well-drained soils with moderately slow to slow permeability. The upper 30 cm of the strata is sandy loam to sandy clay loam ranging from grayish brown to reddish yellow. This stratum has a weak fine granular structure and is very friable. It contains many fine roots and is moderately acid. Deeper strata to 2 m range from yellow to yellowish red sandy clay, often with masses of oxidized iron and few fine prominent light gray iron depletions; they are strongly acid. (Source: NRCS Web Soil Survey.)Wild material2159128NA 88700
306NA 88701RJL2023NCSC-006Zenobia pulverulenta (W. Bartram ex Willd.) Pollard North Carolina, United StatesNA2023COLLECTED11/13/2023Sandhills Game Land: north side of Pulpwood Road approximately 0.11 km southwest of the junction with Tyner Road.34.96066900, -79.48735300111Plants growing in moist-mesic to seasonally saturated soils in part-shade of a spring fed wetland that is a mixed evergreen and deciduous woodland habitat. Slope: 0 to 5 percent. Aspect: Northeast. The underlying geology of this area is of Tertiary origin and characterized as Pinehurst Formation. It is comprised of sand that is medium- to coarse-grained, cross-bedding and rhythmic bands of clayey sand common, unconsolidated. (Source: USGS North Carolina Geologic Map Data.) The primary soil type in the area of this collection is classified as Pelion loamy sand, 6 to 10 percent slopes. Pelion Series soils are very deep, moderately well-drained soils with moderately slow to slow permeability. The upper 30 cm of the strata is sandy loam to sandy clay loam ranging from grayish brown to reddish yellow. This stratum has a weak fine granular structure and is very friable. It contains many fine roots and is moderately acid. Deeper strata to 2 m range from yellow to yellowish red sandy clay, often with masses of oxidized iron and few fine prominent light gray iron depletions; they are strongly acid. (Source: NRCS Web Soil Survey.)Wild material2159129NA 88701
307NA 88702RJL2023NCSC-007Rhododendron viscosum (L.) Torr. North Carolina, United StatesNA2023COLLECTED11/13/2023Sandhills Game Land: north side of Pulpwood Road approximately 0.11 km southwest of the junction with Tyner Road.34.96080300, -79.48730200113Plants growing in moist-mesic to seasonally saturated soils in shade to part-shade of a spring fed wetland that is a mixed evergreen and deciduous woodland habitat. Prescribed fires have burned a portion of the wetland edge where plants are resprouting vigorously. Slope: 0 to 5 percent. Aspect: Norhteast. The underlying geology of this area is of Tertiary origin and characterized as Pinehurst Formation. It is comprised of sand that is medium- to coarse-grained, cross-bedding and rhythmic bands of clayey sand common, unconsolidated. (Source: USGS North Carolina Geologic Map Data.) The primary soil type in the area of this collection is classified as Pelion loamy sand, 6 to 10 percent slopes. Pelion Series soils are very deep, moderately well-drained soils with moderately slow to slow permeability. The upper 30 cm of the strata is sandy loam to sandy clay loam ranging from grayish brown to reddish yellow. This stratum has a weak fine granular structure and is very friable. It contains many fine roots and is moderately acid. Deeper strata to 2 m range from yellow to yellowish red sandy clay, often with masses of oxidized iron and few fine prominent light gray iron depletions; they are strongly acid. (Source: NRCS Web Soil Survey.)Wild material2159130NA 88702
308NA 88703RJL2023NCSC-008Lyonia lucida (Lam.) K. Koch North Carolina, United StatesNA2023COLLECTED11/13/2023Sandhills Game Land: north side of Pulpwood Road approximately 0.11 km southwest of the junction with Tyner Road.34.95848900, -79.48618700101Plants growing in moist-mesic to seasonally saturated soils in shade to part-shade of a spring fed wetland that is a mixed evergreen and deciduous woodland habitat. Slope: 0 to 5 percent. Aspect: Various. The underlying geology of this area is of Tertiary origin and characterized as Pinehurst Formation. It is comprised of sand that is medium- to coarse-grained, cross-bedding and rhythmic bands of clayey sand common, unconsolidated. (Source: USGS North Carolina Geologic Map Data.) The primary soil type in the area of this collection is classified as Pelion loamy sand, 6 to 10 percent slopes. Pelion Series soils are very deep, moderately well-drained soils with moderately slow to slow permeability. The upper 30 cm of the strata is sandy loam to sandy clay loam ranging from grayish brown to reddish yellow. This stratum has a weak fine granular structure and is very friable. It contains many fine roots and is moderately acid. Deeper strata to 2 m range from yellow to yellowish red sandy clay, often with masses of oxidized iron and few fine prominent light gray iron depletions; they are strongly acid. (Source: NRCS Web Soil Survey.)Wild material2159131NA 88703
309NA 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
310NA 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
311NA 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
312NA 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
313NA 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
314NA 88716RJL2023NCSC-021Ilex myrtifolia Walter South Carolina, United StatesNA2023COLLECTED11/14/2023Francis Marion National Forest: plants growing in a pond cypress-water tupelo swamp on the west side of Thompson Branch Road just south of the junction with Round Pond Road B.33.15167800, -79.6025370031Plants are growing in part-shade to shade as understory trees among the pond cypress-water tupelo forest throughout the acid swamp which is seasonally inundated. The overstory is largely deciduous and comprised of pond cypress and water tupelo, while the understory is a mix of evergreen and deciduous broadleaved shrubs and understory trees. 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 Pickney Series loamy fine sand. The Pickney Series consists of very deep, very poorly drained, persistently wet, permeable soils that formed from marine or fluvial sediments. Slopes range from 0 to 2 percent. The upper strata soil, 0-75 cm, is black loamy fine sand that is very friable and extremely acid. The lower strata, 75-120 cm is dark gray fine sand with occasional white mottling, loose, and moderately acid. (Source: NRCS Web Soil Survey.)Wild material2159144NA 88716
315NA 88717RJL2023NCSC-022Ilex opaca Aiton South Carolina, United StatesNA2023COLLECTED11/14/2023Francis Marion National Forest: plants growing in a pond cypress-water tupelo swamp on the west side of Thompson Branch Road just south of the junction with Round Pond Road B.33.15161300, -79.6021790022Plants are growing in part-shade to shade as understory trees among the pond cypress-water tupelo forest, mostly along the edges of the acid swamp which is seasonally inundated. The overstory is largely deciduous and comprised of pond cypress and water tupelo, while the understory is a mix of evergreen and deciduous broadleaved shrubs and understory trees. 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 Pickney Series loamy fine sand. The Pickney Series consists of very deep, very poorly drained, persistently wet, permeable soils that formed from marine or fluvial sediments. Slopes range from 0 to 2 percent. The upper strata soil, 0-75 cm, is black loamy fine sand that is very friable and extremely acid. The lower strata, 75-120 cm is dark gray fine sand with occasional white mottling, loose, and moderately acid. (Source: NRCS Web Soil Survey.)Wild material2159145NA 88717
316NA 88668TXWL2023-011Amorpha paniculata Torr. & A. Gray Texas, United StatesNA2023COLLECTED10/02/2023Angelina National Forest: Forest Service Road 302A roadside [Note: GPS coordinates are west of FS Road 302A, closer to County Road 348B.]31.09190000, -94.29072400Roadside.Wild material2159043NA 88668
317WLP 3213TXWL2023-001Lyonia mariana (L.) D. Don Texas, United StatesNA2023COLLECTED08/22/2023Angelina National Forest.31.05522100, -94.26205200Baygall below longleaf [pine] stand.Wild material2158757WLP 3213
318WLP 3214TXWL2023-002Stewartia malacodendron L. Texas, United StatesNA2023COLLECTED08/27/2023Little Cow Creek.31.06090300, -93.79570300Mesic mixed hardwood-pine forest adjacent to riparian area. Some blowdown evident.Wild material2158758WLP 3214
319WLP 3215TXWL2023-003Stewartia malacodendron L. Texas, United StatesNA2023COLLECTED08/27/2023Little Cow Creek.31.06228800, -93.79734300Mesic mixed hardwood-pine forest adjacent to riparian area. Some blowdown evident.Wild material2158759WLP 3215
320WLP 3216TXWL2023-004Chionanthus virginicus L. Texas, United StatesNA2023COLLECTED09/09/2023Davy Crockett National Forest.Pine stand with mixed hardwood. Heavy midstory and [notes cut off here.]Wild material2158760WLP 3216
321WLP 3345AS/SG/2023/025/235Styrax grandifolius Aiton Arkansas, United StatesNAFLOWER2023COLLECTED08/27/2023Ouachita National Forest - Winona Wildlife Management Area/South Fourche Botanical Area. Approximately 20 miles southwest of Danville, along County Road 362, east of Scenic Highway 7. T3N R20W Sec. 23.34.89619000, -93.10769400275Uplands and on bluffs; understory of pine-hardwood forest.Wild materialPlants in nature are large, clonally spreading colonies to 20 feet in height and similar width. Peak bloom occurred the last week of April (2023).2158786WLP 3345
322NA 88599RJL2023NC-001Ilex decidua Walter North Carolina, United StatesNA2023COLLECTED02/18/2023Plants growing along a fenceline on a hillside about 10 meters from Interstate 85 (south bound) and approximately 0.65 kilometers south of the North Carolina-Virginia border.36.53904800, -78.1882250086The plant was growing on the upper shoulder of a slope about 7 meters above the highway in part-shade to sun of an upland, well-drained, dry mesic somewhat disturbed site on the fenceline boundary of Interstate 85 (south bound). The area was originally cleared of all vegetation and now, many years later, native and non-native plant species have aggressively recolonized the area. This early successional habitat is dominated by Juniperus virginiana and Liquidambar styraciflua, as well as, non-native species such as Ligustrum sinense, Lonicera japonica, and Ailanthus altissima. The underlying geology of this area is of Permian/Pennsylvanian origin and characterized as the Granitic Rock Formation. It is characterized by megacrystic to equigranular components and includs Castalia and Wilton intrusives.Wild material2141480NA 88599
323WLP 3087RM2023-005Rhododendron minus Michx. var. minus Alabama, United StatesNA2023COLLECTED12/29/2022This plant is growing along the edges of Gantt Lake, accessed by boat. Occasional in shaded areas around Gantt Lake.31.40780000, -86.4677000068The plants were growing in open conditions on a steep north-facing bluff above Gantt Lake.
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 surface soil profile of this area is primarily Eunola Series Loamy Fine Sand (0 to 2 percent slopes, rarely flooded). The Eunola series consists of very deep, moderately well drained, moderately permeable loamy soils that formed in fluvial or marine sediments. They are on low stream or marine terraces of the Southern Coastal Plain. They are strongly acid. Slopes are dominantly 0 to 3 percent but range up to 6 percent.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2141441WLP 3087
324WLP 3088RM2023-006Kalmia latifolia L. Alabama, United StatesNA2023COLLECTED12/29/2022This plant is growing along the edges of Gantt Lake, accessed by boat. Occasional in shaded areas around Gantt Lake.31.40780000, -86.4677000068The plants were growing in open conditions on a steep north-facing bluff above Gantt Lake.
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 surface soil profile of this area is primarily Eunola Series Loamy Fine Sand (0 to 2 percent slopes, rarely flooded). The Eunola series consists of very deep, moderately well drained, moderately permeable loamy soils that formed in fluvial or marine sediments. They are on low stream or marine terraces of the Southern Coastal Plain. They are strongly acid. Slopes are dominantly 0 to 3 percent but range up to 6 percent.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2141442WLP 3088
325WLP 3089RM2023-007Oxydendrum arboreum (L.) DC. Alabama, United StatesNA2023COLLECTED12/29/2022This plant is growing along the edges of Gantt Lake, accessed by boat. Occasional around Gantt Lake.31.41156000, -86.4692000070The plants were growing in open sunny conditions on a steep east-facing bluff above Gantt Lake.
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 surface soil profile of this area is primarily Eunola Series Loamy Fine Sand (0 to 2 percent slopes, rarely flooded). The Eunola series consists of very deep, moderately well drained, moderately permeable loamy soils that formed in fluvial or marine sediments. They are on low stream or marine terraces of the Southern Coastal Plain. They are strongly acid. Slopes are dominantly 0 to 3 percent but range up to 6 percent.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2141443WLP 3089
326WLP 3090RM2023-008Lyonia lucida (Lam.) K. Koch Alabama, United StatesNA2023COLLECTED12/29/2022This plant is growing along the steep edges of Gantt Lake, accessed by boat. Occasional in shaded areas around Gantt Lake.31.40780000, -86.4677000068The plants were growing in open conditions on a steep north-facing bluff above Gantt Lake.
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 surface soil profile of this area is primarily Bibb-Kinston Series Association. Bibb Series soils are coarse-loamy, sandy, acid soils that are poorly drained. They are soils of flood plains and streams subject to frequent flooding. These are found in association with Kinston Series soils that are fine-loamy, sandy, acid soils of flood plains and stream subject to frequent flooding. The Bibb-Kinston association ranges from 1-1.5 meters thick and is strongly acid.
Source: Soil Survey of Santa Rosa County and NRCS Web Soil Survey (https://www.nrcs.usda.gov/Internet/FSE_MANUSCRIPTS/florida/FL113/0/SantaRosa.pdf and https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2141444WLP 3090
327WLP 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
328NA 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
329NA 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
330NA 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
331NA 88542RJLSEUS2022-014Rosa palustris Marshall 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 transitional edges from wet to dry.31.63723900, -84.1377620060Plants are growing in full sun mostly in the transitional edges of the pond where conditions are generally moist mesic. Even so, this species appears quite adaptable and can be found in quite moist as well as drier soil conditions.
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 material2140817NA 88542
332NA 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
333NA 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
334NA 88549RJLSEUS2022-022Rhododendron minus Michx. var. minus Georgia, United StatesNA2023COLLECTED12/10/2022East side of Georgia State Hwy. 39, on the south side of Kolomoki Creek approximately 11 kilometers south of Fort Gaines, Georgia. Common on this site, but otherwise infrequent. This species is near the southernmost end of its natural range.31.52053400, -85.0235160053Plants are growing in part-shade to shade of deciduous upland, dry, deciduous woodlands on steep slopes 10-15 meters above Kolomoki Creek.
Soils: The underlying geology of this area is of Paleocene origin and characterized as Tuscahoma Sand. As mapped this formation includes lower Eocene Bashi Marl Member of the Hatchetigbee Formation. This formation consists of light-gray to light-olive-gray laminated and thin-bedded carbonaceous silt and clay interbedded with fine sand; thin lignite beds occur locally. Lower part of the formation includes beds of fossiliferous, glauconitic fine quartz sand containing spheroidal sandstone concretions, gravel and clay pebbles.
Source: USGS Georgia Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=GANu%3B1)
The primary soil types in the collection area are classified as Ailey-Cowarts Complex Series soils (8 to 25 percent slopes). The Ailey Series consists of well drained or somewhat excessively drained soils formed by fluviomarine and marine deposits. These soils are found marine terraces and low hills of the upper coastal plain and sandhills; they are strongly acidic. The Cowarts Series consists of very deep, moderately well and well drained soils on ridge tops and side slopes on uplands of the Coastal Plain Major Land Resource Area. They formed in loamy marine sediments. Slopes range from 1 to 60 percent.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2140776NA 88549
335NA 88550RJLSEUS2022-023Kalmia latifolia L. Georgia, United StatesNA2023COLLECTED12/10/2022East side of Georgia State Hwy. 39, on the south side of Kolomoki Creek approximately 11 kilometers south of Fort Gaines, Georgia. Common on this site, but otherwise infrequent. This species is near the southernmost end of its natural range. 31.52053400, -85.0235160053Plants are growing in part-shade to shade of deciduous upland, dry, deciduous woodlands on steep slopes 10-15 meters above Kolomoki Creek.
Soils: The underlying geology of this area is of Paleocene origin and characterized as Tuscahoma Sand. As mapped this formation includes lower Eocene Bashi Marl Member of the Hatchetigbee Formation. This formation consists of light-gray to light-olive-gray laminated and thin-bedded carbonaceous silt and clay interbedded with fine sand; thin lignite beds occur locally. Lower part of the formation includes beds of fossiliferous, glauconitic fine quartz sand containing spheroidal sandstone concretions, gravel and clay pebbles.
Source: USGS Georgia Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=GANu%3B1)
The primary soil types in the collection area are classified as Ailey-Cowarts Complex Series soils (8 to 25 percent slopes). The Ailey Series consists of well drained or somewhat excessively drained soils formed by fluviomarine and marine deposits. These soils are found marine terraces and low hills of the upper coastal plain and sandhills; they are strongly acidic. The Cowarts Series consists of very deep, moderately well and well drained soils on ridge tops and side slopes on uplands of the Coastal Plain Major Land Resource Area. They formed in loamy marine sediments. Slopes range from 1 to 60 percent.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2140777NA 88550
336NA 88551RJLSEUS2022-024Rhododendron minus Michx. var. minus Alabama, United StatesNA2023COLLECTED12/10/2022Plants growing on the west side of George H. Grimsley Highway (Alabama State Hwy. 95) on the bluffs above the south side of Abbie Creek. Common on this site, but otherwise infrequent. This species is near the southernmost end of its natural range. 31.47254800, -85.1630480067Plants are growing in part-shade to shade of a mixed evergreen and deciduous woodland on the dry well-drained bluffs 4-5 meters above Abbie Creek.
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 Bonneau Loamy Fine Sand soil (0 to 2 percent slopes). The Bonneau Series consists of very deep, well drained, moderately permeable soils on the middle and upper coastal plain. They were formed by marine and fluviomarine deposits. Slopes range from 0 to 12 percent. Soils are comprised of very friable loamy sand that is strongly acid in the upper 0.7 meters. The lower strata to 2 meters are comprised of sandy clay loam that is friable, sometimes with oxidized iron, and strongly acid.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2140778NA 88551
337NA 88552RJLSEUS2022-025Hydrangea quercifolia W. Bartram Alabama, United StatesNA2023COLLECTED12/12/2022Claiborne Bluffs area along unnamed road to boat ramp on the east side of the Alabama River at the U.S. Highway 84 bridge over the river. Common at this location and along the nearby Alabama River.31.54879700, -87.5141640040Plants are growing in part-shade to shade of mesic, well-drained, circum-neutral slopes and benches in mature mixed deciduous and evergreen woodlands with good litter layer. Soils: The underlying geology of this area is the Jackson Group Undifferentiated. The units of the Jackson Group are the Yazoo Clay and Crystal River and Moodys Branch Formations. Descriptions of the members of the Yazoo Clay follow in descending order. Shubuta Member - in western Alabama consists of light-greenish-gray to white plastic fossiliferous, calcareous clay containing irregular calcareous nodules. From the Tombigbee River eastward, the Shubuta becomes more calcareous and grades into massive clayey glauconitic limestone. Eastward from the Alabama River, equivalent beds grade into the Crystal River Formation. Pachuta Marl Member - light-greenish-grey glauconitic, fossiliferous clayey sand and sandy limestone traceable from western Alabama eastward to Covington County where it grades into the Crystal River Formation. Cocoa Sand Member - yellowish-gray firm calcareous, fossiliferous fine to medium sand or sandy limestone or greenish-grey micaceous, calcareous, very clayey sand. Calcareous and clayey sand equivalent to the Cocoa is traceable from western Alabama to the Conecuh River area. (Source: USGS Alabama Geological Map Data). The surface soil profile of this portion of the bluffs along the Alabama River are characterized as Saffell-Lucy (Flomaton) Series Complex soils. The Saffell Series consists of very deep, well drained, moderately permeable soils that formed in loamy and gravelly marine sediments of the Tertiary Age and have acid reaction. These soils are found on the upper portion of the bluffs along the Alabama River. The Lucy Series consists of very deep, well drained, moderately permeable soils on uplands. They formed in sandy and loamy marine and fluvial sediments of the Southern Coastal Plain Major Land Resource Area. Soil reaction runs from strongly to moderately acid. The Flomaton Series consists of very deep, excessively drained, rapidly permeable soils on uplands of the Southern Coastal Plain Major Land Resource Area. They formed in gravelly sandy marine sediments and also have an acid reaction. The remainder of soils are of miscellaneous origin. (Source: USDA-NRCS Official Soil Series Descriptions).Wild material2140779NA 88552
338NA 88553RJLSEUS2022-026Hydrangea arborescens L. Alabama, United StatesNA2023COLLECTED12/12/2022Claiborne Bluffs area along unnamed road to boat ramp on the east side of the Alabama River at the U.S. Highway 84 bridge over the river. Occasionally found in the woodlands. 31.54940700, -87.5136620025Plants are growing in part-shade to shade of mesic, well-drained, circum-neutral slopes mature mixed deciduous and evergreen woodlands where slopes are exposed and detritus does not build up.
Soils: The underlying geology of this area is the Jackson Group Undifferentiated. The units of the Jackson Group are the Yazoo Clay and Crystal River and Moodys Branch Formations. Descriptions of the members of the Yazoo Clay follow in descending order. Shubuta Member - in western Alabama consists of light-greenish-gray to white plastic fossiliferous, calcareous clay containing irregular calcareous nodules. From the Tombigbee River eastward, the Shubuta becomes more calcareous and grades into massive clayey glauconitic limestone. Eastward from the Alabama River, equivalent beds grade into the Crystal River Formation. Pachuta Marl Member - light-greenish-grey glauconitic, fossiliferous clayey sand and sandy limestone traceable from western Alabama eastward to Covington County where it grades into the Crystal River Formation. Cocoa Sand Member - yellowish-gray firm calcareous, fossiliferous fine to medium sand or sandy limestone or greenish-grey micaceous, calcareous, very clayey sand. Calcareous and clayey sand equivalent to the Cocoa is traceable from western Alabama to the Conecuh River area.
Source: USGS Alabama Geological Map Data (https://mrdata.usgs.gov/geology/state/state.php?state=AL)
The surface soil profile of this portion of the bluffs along the Alabama River are characterized by Saffell-Lucy (Flomaton) Series Complex soils. The Saffell Series consists of very deep, well drained, moderately permeable soils that formed in loamy and gravelly marine sediments of the Tertiary Age and have acid reaction. These soils are found on the upper portion of the bluffs along the Alabama River. The Lucy Series consists of very deep, well drained, moderately permeable soils on uplands. They formed in sandy and loamy marine and fluvial sediments of the Southern Coastal Plain Major Land Resource Area. Soil reaction runs from strongly to moderately acid. The Flomaton Series consists of very deep, excessively drained, rapidly permeable soils on uplands of the Southern Coastal Plain Major Land Resource Area. They formed in gravelly sandy marine sediments and also have an acid reaction. The remainder of soils are of miscellaneous origin.
Source: USDA-NRCS Official Soil Series Descriptions (https://soilseries.sc.egov.usda.gov/osdname.aspx)		Wild material2140780NA 88553
339NA 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
340NA 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
341NA 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
342NA 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
343NA 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
344NA 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
345NA 88562RJLSEUS2022-035Kalmia latifolia L. Alabama, United StatesNA2023COLLECTED12/12/2022Plants growing on both sides of River Ridge Road accessed from Alabama State Hwy 41 via Tin Cup Alley Road. Common at this site 31.73823700, -87.35821100132Plants are growing in part-shade to full sun on top of a very exposed ridge top under dry conditions.
Soils: The underlying geology of this area is of Eocene origin and characterized as Claiborne Group; Gosport Sand and Lisbon Formation Undifferentiated in part. Greenish-gray calcareous, glauconitic, fossiliferous clayey sand; marl; carbonaceous sand; carbonaceous silty clay; and coarse glauconitic, fossiliferous, quartz sand.
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 Saffell Very Gravelly Sandy Loam soil (5 to 8 percent slopes). The Saffell Series consists of very deep, well drained, moderately permeable soils that formed in loamy and gravelly marine sediments of the Tertiary Age and have acid reaction. These soils are found on the upper portion of the bluffs along the Alabama River.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2140787NA 88562
346NA 88576RJLSEUS2022-049Rhododendron atlanticum (Ashe) Rehder South Carolina, United StatesNA2023COLLECTED12/16/2022Plants growing in mixed evergreen and deciduous woods on the east side of Ip Canal Road approximately 0.33 kilometers south of Pleasant Hill Drive (Georgetown County Road 251). Frequent at this location. 33.63226900, -79.258317008Plants are growing in part-shade to shade of a dry to periodically moist mesic woodland. Given some of the plant associates, there may be an impermeable subsurface soil layer to add moisture availability.
Soils: The underlying geology of this area is of Pleistocene origin and characterized as Socastee Formation. This is a low coastal formation in the Carolinas like Penholoway but younger and lower in altitude. The Socastee Formation lies seaward of the Penholoway and Canepatch Formations and is the next younger surficial unit. It is exposed in a belt approximately 25 km wide at elevations between 9 and 15 m above sea level. It is described as variegated quartzose sands, argillaceous sands, and clays, 5 m thick at the type section near Socastee Swamp. Unconformably overlies Canepatch Formation; unconformably underlies Waiter Island Formation and Ocean Forest Peat.
Source: USGS Texas Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=SCQso%3B1)
The primary soil type in the collection area is classified as Centenary Fine Sand. The Centenary Fine Sand Series consists of deep, well drained or somewhat excessively drained single-grained sand that is loose and moderately acid. The upper layer ranges from 7.5cm to 25cm thick. Deeper layers vary in percentage of single-grained sands and clay.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2140794NA 88576
347NA 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
348NA 88510RJL2022TX-005Crataegus marshallii Eggl. Texas, United StatesNA2022COLLECTED11/01/2022Plants growing along the west side of Texas State Hwy 87 on the edge of the woodlands. Plant is infrequently found, but a regular member of the woodlands as well as forest edge communities along the highway. 31.15847300, -93.73852000115Plants are growing in part-shade to sun on upland dry hills. In shade they survive, but in part-shade to sun they develop excellent flowering and fruiting.
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-Tehran 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-Tehran soils are on gently sloping to moderately steep uplands with slopes ranging from 1 to 20 percent. They are typically strongly acidic.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2139817NA 88510
349NA 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
350NA 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
351NA 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
352NA 87267(female selection)Ilex vomitoria Sol. ex Aiton f. pendula Foret & SolymosyTexas, United StatesNA2022COLLECTED01/27/2020Plants growing on the north side of the unpaved Private Road 6061, approximately 0.4 kilometers east of Texas State Hwy 87.31.16207000, -93.72862000132Growing in almost full sun on a south-facing roadside slope in very dry upland conditions. Soils are deep, somewhat excessively well-drained, and typically strongly acidic. Slope: 8 percent. Aspect: South. 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. The primary soil types in the collection area are classified as Letney-Tehran 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-Tehran soils are on gently sloping to moderately steep uplands with slopes ranging from 1 to 20 percent. They are typically strongly acidic.Wild materialFull name as recorded at U.S. National Arboretum: Ilex vomitoria forma pendula (female selection). Six plants of a selection of weeping yaupon holly sent from Shangri La Botanical Gardens & Nature Center (Rick Lewandowski facilitated the distribution in retirement). It is evidently from a selection discovered growing in Newton County, Texas, presumably from the wild. A date of 11/25/2020 is on the plant's tag from the source, but it is unknown if this is a propagation date or an accession date. Form received: rooted cutting.2158071NA 87267
353NA 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
354NA 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
355WLP 26102022VA-01Stewartia malacodendron L. Virginia, United StatesNA2022COLLECTED09/12/2022Woodlands adjacent to and bounded by the interchange of Business Route 168 (N. Battlefield Avenue) and Route 168, next to a detention basin and shopping plaza on the west side of Battlefield Avenue. Accessed by parking in the cul-de-sac at the south end of Kingsborough Square Street. This plant is a very common and abundant component of this woodland with significant recruitment continuing36.73888200, -76.243277009Plants growing in rich mesic, moist but well-drained conditions in the high understory shade of a mixed deciduous and evergreen woodland, primarily comprised of deciduous trees in the over-story and a mixture of deciduous and evergreen species in the sub-canopy.
Soils: The underlying geology of this area is the Tabb Formation of Quaternary origin which is comprised of undifferentiated sand, silt, and peat and subdivided into three members. Within the Tabb Formation lies the Sedgefield Member, a pebbly to bouldery, clayey sand and fine to medium, shell-rich sand that grades upward into sandy and clayey silt; locally, channel fill at the base of unit includes as much as 15 meters of fine to coarse, cross-bedded sand and clayey silt and peat containing in-situ tree stumps. Sandy bay facies commonly contain numerous mollusks as well as coral. Thickness is 0 to 15.8 meters.
Source: USGS Virginia Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=VAQts%3B0)
The surface soil profile of this area is Tetotum fine sandy loam, 0 to 2 percent slopes. Forming primarily terraces, these soils are moderately well-drained and highly acidic. They are generally 100-150 cm thick, the upper 20 inches of the horizon averages more than 30 percent silt or more than 40 percent silt plus very fine sand.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2139348WLP 2610
356WLP 26122022VA-03Styrax grandifolius Aiton Virginia, United StatesNA2022COLLECTED09/12/2022Northwest River Park on the south side of Indian Springs Road behind the Equestrian Center along a bridle trail. This plant is a common in the mesic woodlands at this location.36.58361100, -76.1627780021Plants growing in shade to part-shade of the mixed deciduous and evergreen mesic woodland about 1 to 2 meters above a nearby wetland area.
The underlying geology of this area is the Tabb Formation of Quaternary origin which is comprised of undifferentiated sand, silt, and peat and subdivided into three members. Within the Tabb Formation lies the Lynnhaven Member with pebbly and cobbly, fine to coarse gray sand grades upward into clayey and silty fine sand and sandy silt. Extensive low lands bounded on the landward side by river-, bay-, and ocean-facing scarps having toe altitudes of 5-6 meters. Thickness is 0 to 6.5 meters.
Source: USGS Virginia Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=VAQtl%3B0)
The surface soil profile of this area is Chapanoke-Yeopim complex, 0 to 3 percent slopes. These soil as somewhat poorly to moderately drained, acidic, and found on marine terraces and summits of low elevation coastal plain areas. They are comprised of silt loam, silty clay loam, sandy clay loam and loam in varying quantities across the profile; the depth to parent geology is approximately 200 cm.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx		Wild material2139350WLP 2612
357WLP 26142022VA-05Euonymus americanus L. Virginia, United StatesNA2022COLLECTED09/12/2022In Colonial Williamsburg, park in the Providence Hall Directors Wing parking lot and enter the Bassett Trace Nature Trail; this species is found in the woodlands on either side of the trail and over a bridge until the it turns right. This plant is infrequent, but occasionally found in the mesic woodlands throughout this location.37.26681600, -76.6925280021Plants growing in shade to part-shade of the mixed deciduous and evergreen mesic woodland. This species is generally growing in areas with an abundant organic, mature woodland that is relatively undisturbed.
The underlying geology of this area is Windsor Formation of Tertiary-Quaternary origin (lower Pleistocene or upper Pliocene). It is comprised of gray and yellowish- to reddish-brown sand, gravel, silt, and clay. It constitutes surficial deposits of extensive plain and fluvial-estuarine terraces above elevations of 10 meters. The thickness of the Windsor Formation is 0 to 12.5 meters.
Source: USGS Virginia Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=VAQTw%3B0)
The surface soil profile of this area is Emporia Complex, 15 to 25 percent slopes. This soil as moderately well-drained, acidic, and found on sloping and elevated terraces. They are comprised of fine sandy loam, loam, and sandy clay loam in varying quantities across the profile; the depth to parent geology is approximately 200 cm.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2139352WLP 2614
358WLP 2600RJL2022FLAL-029Stewartia malacodendron L. Florida, United StatesNA2022COLLECTED08/07/2022Eglin AFB, in woodlands along Weaver Creek accessed from unnamed dirt road, 0.82 kilometers west of junction with Eglin AFB 720; approximately 0.73 kilometers north of junction with Choctaw Nolf Airfield Road and Eglin AFB 720.30.51680000, -86.9146940015Growing in moist, well-drained sandy soils above Weaver Creek in mixed broadleaved evergreen and deciduous woodland habitat in part shade to shade of west facing slopes several meters above the wetland zone. The Stewartia is growing in a high competition habitat. The underlying geology of this area is the Citronelle Formation, of Pliocene origin, and consists of gray to orange, often mottled, unconsolidated to poorly consolidated, very fine to very coarse, poorly sorted, clean to clayey sands. It contains significant amounts of clay, silt and gravel which may occur as beds and lenses and may vary considerably over short distances. Limonite nodules and limonite-cemented beds are common. Wild material2138710WLP 2600
359Ames 35939AS/ML/2022/008/139Monarda lindheimeri Engelm. & A. Gray Texas, United StatesNC7PLANT2022COLLECTED04/26/2022Located approximately 4.00 miles west, southwest of Huntsville near intersection of Gazebo Street and FM 1791 Rd.30.69714300, -95.61197300121Recently disturbed woodland edge.Wild material2140529Ames 35939
360NA 88335NCBG-425Ilex opaca Aiton Maryland, United StatesNA2021COLLECTED11/11/2015Robinson Neck: Nature Trai: from MD-16W, make a slight left onto Robinson Neck Rd. In about 2.7 miles, park where the nature trail starts off on the left as an old loggin road with a gate across it. Walk down the trail to the east. Seed collected along the trail and on the forest edge to the north of where the trail ends at the salt marsh.38.44180000, -76.262660003Forest edge and along trail.Wild material2132886NA 88335
361OPGC 8501NCBG-507Xyris difformis Chapm. North Carolina, United StatesOPGC2021Wild material2132891OPGC 8501
362OPGC 8506NCBG-526Xyris difformis Chapm. Maryland, United StatesOPGC2021Wild material2132902OPGC 8506
363OPGC 8510NCBG-547Typha angustifolia L. Virginia, United StatesOPGC2021Wild material2132914OPGC 8510
364W6 59984NCBG-315Eupatorium hyssopifolium L. North Carolina, United StatesW62021Wild material2132866W6 59984
365W6 59986NCBG-347Schizachyrium scoparium (Michx.) Nash Virginia, United StatesW62021Wild material2132868W6 59986
366W6 59989NCBG-373Diospyros virginiana L. Virginia, United StatesW62021Wild material2132871W6 59989
367W6 60006NCBG-504Cyperus grayi Torr. North Carolina, United StatesW62021Wild material2132888W6 60006
368W6 60008NCBG-506Eleocharis quadrangulata (Michx.) Roem. North Carolina, United StatesW62021Wild material2132890W6 60008
369W6 60012NCBG-512Cyperus strigosus L. North Carolina, United StatesW62021Wild material2132894W6 60012
370W6 60017NCBG-520Fimbristylis castanea (Michx.) Vahl Virginia, United StatesW62021Wild material2132899W6 60017
371W6 60024NCBG-530Panicum virgatum L. Maryland, United StatesW62021Wild material2132906W6 60024
372W6 60031NCBG-546Fimbristylis castanea (Michx.) Vahl Virginia, United StatesW62021Wild material2132913W6 60031
373W6 60033NCBG-548Fimbristylis castanea (Michx.) Vahl Virginia, United StatesW62021Wild material2132915W6 60033
374W6 60040NCBG-563Pluchea odorata (L.) Cass. Virginia, United StatesW62021Wild material2132922W6 60040
375W6 60051NCBG-596Panicum virgatum L. Virginia, United StatesW62021Wild material2132932W6 60051
376W6 60052NCBG-597Schizachyrium scoparium (Michx.) Nash Virginia, United StatesW62021Wild material2132933W6 60052
377W6 60059NCBG-724Bolboschoenus robustus (Pursh) Soják Maryland, United StatesW62021Wild material2132940W6 60059
378Ames 35728F-11Echinacea laevigata (C. L. Boynton & Beadle) S. F. Blake Georgia, United StatesNC7FruitContact Site2021COLLECTED07/06/2021Fort Stewart Training Area F-1132.11108600, -81.78672200Pine woodland situated on Fuquay loamy sand that slopes down to Osier soils.Wild materialSpecimens in nature reaching approximately 33 inches in height. Peak flowering occurred 10 June 2021. 2116603Ames 35728
379NA 86881ASA-009AIlex vomitoria Aiton Virginia, United StatesNA2021COLLECTED01/13/2020Virginia Beach: First Landing State Park. Collected in the park campground, near the location of VIRG-015. One plant at campsite #166, the other near site #7336.91886900, -76.05188900215 deg slope; SE-facing; sand. Dunes with live oaksWild material2116470NA 86881
380NA 88460NCBG-414Smilax rotundifolia L. Virginia, United StatesNA2021Wild material2116305NA 88460
381OPGC 8271NCBG-661Solidago sempervirens L. Virginia, United StatesOPGC2021Wild material2116371OPGC 8271
382OPGC 8274NCBG-755Heterotheca subaxillaris (Lam.) Britton & Rusby North Carolina, United StatesOPGC2021Wild material2116387OPGC 8274
383OPGC 8275NCBG-760Lythrum lineare L. Maryland, United StatesOPGC2021Wild material2116429OPGC 8275
384W6 59017NCBG-480Teucrium canadense L. North Carolina, United StatesW62021Wild material2116335W6 59017
385W6 59041NCBG-623Sorghastrum nutans (L.) Nash North Carolina, United StatesW62021Wild material2116357W6 59041
386W6 59063NCBG-681Pityopsis graminifolia (Michx.) Nutt. var. latifolia (Fernald) Semple & F. D. Bowers Virginia, United StatesW62021Wild material2116425W6 59063
387W6 59064NCBG-682Chasmanthium laxum (L.) H. O. Yates Virginia, United StatesW62021Wild material2116377W6 59064
388W6 59071NCBG-705Danthonia spicata (L.) P. Beauv. ex Roem. & Schult. North Carolina, United StatesW62021Wild material2116382W6 59071
389NA 87036Site 3A/Live Oak Landing/Holmes Creek SiteMagnolia ashei Weath. Florida, United StatesNA2020COLLECTED07/15/2020Along Holmes Creek at Live Oak Landing.30.59208000, -85.8375000011Shade to partial shade of bluffs above the creek in well-drained mesic to dry deciduous woodlands with a few broadleaved and coniferous evergreens.Wild materialAlthough these were collected without any field collection number, seeds from individual trees were separated with letter identifiers that will be maintained with the qualifier (seedling) records. The relationships are as follows: 1. Maternal letter G, NA 87036-J, L, P, and T; maternal letter H, NA 87036-V; maternal letter K, NA 87036-X, Z, and H1; maternal letter N, NA 87036-H2. In addition, three seedlings' maternal letters were lost, and these will be NA 87036-H3, H4, and H5. See the following accessions for earlier collections from this same site/population, listed in our records as "Site 3A/Live Oak Landing/Holmes Creek Site": NA 81555 (2013), NA 82745 (2015), and NA 82745.01 (2019).2109403NA 87036
390NA 88149NCBG-313Liquidambar styraciflua L. North Carolina, United StatesNASEED2019Wild material2098409NA 88149
391NA 88150NCBG-317Aralia spinosa L. Virginia, United StatesNASEED2019Wild material2098410NA 88150
392NA 88153NCBG-321Morella cerifera (L.) Small North Carolina, United StatesNASEED2019Wild material2098413NA 88153
393NA 88156NCBG-326Cephalanthus occidentalis L. North Carolina, United StatesNASEED2019Wild material2098416NA 88156
394NA 88163NCBG-423Chamaecyparis thyoides (L.) Britton et al. North Carolina, United StatesNASEED2019Wild material2098444NA 88163
395NA 88166NCBG-558Chamaecyparis thyoides (L.) Britton et al. North Carolina, United StatesNASEED2019Wild material2098472NA 88166
396NA 88170NCBG-666Baccharis halimifolia L. Maryland, United StatesNASEED2019Wild material2098505NA 88170
397NA 88381NCBG-327Iva frutescens L. Virginia, United StatesNASEED2019Wild material2098417NA 88381
398OPGC 7972NCBG-411Oenothera biennis L. Virginia, United StatesOPGCSEED2019Wild material2098436OPGC 7972
399OPGC 7974NCBG-413Rhexia nashii Small Virginia, United StatesOPGCSEED2019Wild material2098438OPGC 7974
400OPGC 7975NCBG-416Lechea maritima Legg. ex Britton North Carolina, United StatesOPGCSEED2019Wild material2098440OPGC 7975
401OPGC 7983NCBG-601Rhexia mariana L. North Carolina, United StatesOPGCSEED2019Wild material2098481OPGC 7983
402OPGC 7985NCBG-609Lechea maritima Legg. ex Britton North Carolina, United StatesOPGCSEED2019Wild material2098485OPGC 7985
403W6 57458NCBG-269Mikania scandens (L.) Willd. Virginia, United StatesW6SEED2019Wild material2098382W6 57458
404W6 57535NCBG-488Teucrium canadense L. Maryland, United StatesW6SEED2019Wild material2098459W6 57535
405W6 57538NCBG-497Cyperus strigosus L. North Carolina, United StatesW6SEED2019Wild material2098462W6 57538
406W6 57555NCBG-598Andropogon gerardi Vitman Virginia, United StatesW6SEED2019Wild material2098479W6 57555
407W6 57560NCBG-608Chrysopsis gossypina (Michx.) Elliott subsp. gossypina North Carolina, United StatesW6SEED2019Wild material2098484W6 57560
408W6 57562NCBG-611Alnus serrulata (Aiton) Willd. Virginia, United StatesW6SEED2019Wild material2098486W6 57562
409W6 57568NCBG-619Saccharum giganteum (Walter) Pers. North Carolina, United StatesW6SEED2019Wild material2098492W6 57568
410W6 57585NCBG-677Schizachyrium scoparium (Michx.) Nash subsp. littorale (Nash) Gandhi & Smeins North Carolina, United StatesW6SEED2019Wild material2098509W6 57585
411W6 57586NCBG-678Saccharum giganteum (Walter) Pers. North Carolina, United StatesW6SEED2019Wild material2098510W6 57586
412W6 57590NCBG-693Saccharum giganteum (Walter) Pers. Virginia, United StatesW6SEED2019Wild material2098514W6 57590
413NA 88103MARSB-390Ilex opaca Aiton Delaware, United StatesNASEED2019COLLECTED11/03/2015Prime Hook National Wildlife Refuge: follow Broadkill Road towards Broadkill Beach. Almost immediately after the first bridge take the gated gravel road before a sharp right turn. Follow the gravel road until a right towards tree stand 9 (there is a sign). The population extends along the road.38.81797000, -75.203720007North Atlantic maritime scrub forest.Wild material2097608NA 88103
414W6 57082MARSB-210Teucrium canadense L. Delaware, United StatesW6SEED2019Wild material2097521W6 57082
415WLP 157NACPEC19-026Carpinus caroliniana Walter Kentucky, United StatesNA2019COLLECTED09/09/2019Madison County; Berea College Forest: Gabertown Road, near junction of Gabertown Road (KY 1617) + Scaffold Cane (KY595)37.54309800, -84.27086000292Former Pinus taeda plantationWild material2110469WLP 157
416WLP 163NACPEC19-046BHydrangea cinerea Small Georgia, United StatesNA2019COLLECTED09/14/2019Walker County; Lula Lake Land Trust: Bridge from parking lot to South Creek Trail34.92114500, -85.38035700373Limestone bluffs surrounding dry creek bed in mixed mesophytic forestWild material2110475WLP 163
417WLP 164NACPEC19-047Kalmia latifolia L. Georgia, United StatesNA2019COLLECTED09/14/2019Walker County; Lula Lake Land Trust: Off of South Creek trail on North side of bridge from parking lot34.92134100, -85.38051100373Riparian zone, wet slope of creek, moist, sandy banksWild material2110476WLP 164
418WLP 167NACPEC19-053Mitchella repens L. Georgia, United StatesNA2019COLLECTED09/14/2019Walker County; Lula Lake Land Trust: Middle Trail near top, also collected along Connector Trail to Middle Trail from parking lot.34.93141800, -85.36991400469Mesic, sandy, rocky Oak-Hickory woodland slope - likely acidicWild material2110479WLP 167
419WLP 168NACPEC19-054Viburnum acerifolium L. Georgia, United StatesNA2019COLLECTED09/14/2019Walker County; Lula Lake Land Trust: Middle Trail near top.34.93146200, -85.37018800449Mesic, sandy, rocky Oak-Hickory woodland slope - likely acidicWild material2110480WLP 168
420Ames 34783NCBG-274Rhus copallinum L. North Carolina, United StatesNC7SEED2018COLLECTED09/09/2015Cape Hatteras National Seashhore on Hatteras Island along Water Association Road.35.25722000, -75.586130001Maritime evergreen forest edges next to interdune swalesWild material1965902Ames 34783
421Ames 34788NCBG-385Rhus copallinum L. Virginia, United StatesNC7SEED2018COLLECTED10/19/2015Eastern Shore National Wildlife Refuge (Cape Charles) along Hallet Circle and Fitchetts Road.37.13108000, -75.958690005Mesic MeadowWild material1965941Ames 34788
422Ames 34794NCBG-739Rhus glabra L. North Carolina, United StatesNC7SEED2018COLLECTED10/07/2017Just north of Oswego.36.19391000, -78.1939100091Ruderal loblolly pine/sweetgum red maple forestWild material1966040Ames 34794
423NA 88035NCBG-622Ilex glabra (L.) A. Gray North Carolina, United StatesNASEED2018COLLECTED10/27/2016From Roanoke Island, head SW on US-64 W, turn left onto US-264 W, population on left for approximately 12 miles.35.71316000, -75.768190001Pine-inkberry swamp.Wild material1965992NA 88035
424NA 88349NCBG-593Iva frutescens L. Maryland, United StatesNASEED2018Wild materialIva frutescens1965985NA 88349
425NA 88425NCBG-738Rosa carolina L. North Carolina, United StatesNASEED2018Wild materialRosa carolina1966039NA 88425
426OPGC 7231NCBG-728Lachnanthes caroliana (Lam.) Dandy North Carolina, United StatesOPGCSEED2018Wild material1966033OPGC 7231
427W6 54630NCBG-204Juncus effusus L. Virginia, United StatesW62018Wild materialJuncus effusus1965856W6 54630
428W6 54633NCBG-208Bolboschoenus robustus (Pursh) Soják North Carolina, United StatesW62018Wild materialBolboschoenus robustus1965859W6 54633
429W6 54635NCBG-210Schoenoplectus pungens (Vahl) Palla North Carolina, United StatesW62018Wild materialSchoenoplectus pungens1965861W6 54635
430W6 54641NCBG-217Juncus effusus L. North Carolina, United StatesW62018Wild materialJuncus effusus1965867W6 54641
431W6 54702NCBG-359Distichlis spicata (L.) Greene Virginia, United StatesW6SEED2018Wild materialDistichlis spicata1965928W6 54702
432W6 54730NCBG-476Schoenoplectus pungens (Vahl) Palla North Carolina, United StatesW6SEED2018Wild materialSchoenoplectus pungens1965956W6 54730
433W6 54740NCBG-502Pluchea odorata (L.) Cass. North Carolina, United StatesW6SEED2018Wild materialPluchea odorata1965966W6 54740
434W6 54758NCBG-592Distichlis spicata (L.) Greene Maryland, United StatesW6SEED2018Wild materialDistichlis spicata1965984W6 54758
435W6 54765NCBG-621Trichostema dichotomum L. North Carolina, United StatesW6SEED2018Wild materialTrichostema dichotomum1965991W6 54765
436W6 54767NCBG-624Tridens flavus (L.) Hitchc. North Carolina, United StatesW6SEED2018Wild materialTridens flavus1965993W6 54767
437W6 54775NCBG-652Pluchea odorata (L.) Cass. Virginia, United StatesW6SEED2018Wild materialPluchea odorata1966001W6 54775
438W6 54776NCBG-654Tridens flavus (L.) Hitchc. Virginia, United StatesW6SEED2018Wild materialTridens flavus1966002W6 54776
439W6 54800NCBG-716Juncus gerardi Loisel. Maryland, United StatesW6SEED2018Wild materialJuncus gerardii var. gerardii1966026W6 54800
440NA 87992MARSB-205Juniperus virginiana L. Delaware, United StatesNASEED2018Wild material1964733NA 87992
441NA 87993MARSB-206Morella cerifera (L.) Small Delaware, United StatesNASEED2018Wild material1964734NA 87993
442NA 88002MARSB-637Morella cerifera (L.) Small Delaware, United StatesNASEED2018Wild material1964812NA 88002
443W6 54019MARSB-209Elymus virginicus L. Delaware, United StatesW6SEED2018Wild materialElymus virginicus1964735W6 54019
444W6 54101MARSB-648Bolboschoenus maritimus (L.) Palla Delaware, United StatesW6SEED2018Wild materialBolboschoenus maritimus1964817W6 54101
445NA 85961PCC15-SEUSA025Quercus boyntonii Beadle Alabama, United StatesNA2017COLLECTED10/28/2015Shelby County; Birmingham; Off parking lot of EBSCO Industries, Inc., located at 5724 US-280, Birmingham, Alabama.33.37888000, -86.67333000Ridge of Appalachian forest.Wild material2109093NA 85961
446NA 85963PCC15-SEUSA045Quercus arkansana Sarg. Alabama, United StatesNA2017COLLECTED10/30/2015Sumter County; ; Roadside, unincorporated area of Sumter County.32.56277000, -88.02721000Prairie woods, roadside.Seed from plant. Ground, vouchered. [Seed from plant and ground?] Ca five plants in area. No threats observed.2109095NA 85963
447NA 84577RJL-RM001Halesia diptera J. Ellis Texas, United StatesNA2017COLLECTED07/22/2017Along either side of a clear creek on private property approximately 1.42 kilometers north of Texas Recreational Road 255 in northeastern Jasper County.31.07135000, -93.94985000107Plants growing along the embankments of the clear creek just above normal flood stage in primarily deciduous woodlands with some broadleaved evergreens and conifers. Plants are growing in part shade; some direct sunlight occurs during mid-day hours for 1-2 hours. Soils sandy and topped with a generous undisturbed decomposed litter layer. Slope: 10 percent. Aspect: variable.Wild material1953812NA 84577
448NA 84578RJL-RM002Magnolia pyramidata W. Bartram Texas, United StatesNA2017COLLECTED07/22/2017Newton County Road 425, about 2.8 miles south of Texas Recreational Road 255.30.85996000, -93.89596000105Along roadsides and among young loblolly pines in forestry plantation. Plants growing in part shade to full sun in heavily regenerating roadside woodlands associated with loblolly pine plantations. Plants are growing in well drained, highly sandy soils.Wild material1953814NA 84578
449NA 82643NA 82643Lonicera sempervirens L. Texas, United StatesNA2015COLLECTED07/20/2014East side of Texas Route 87 approximately 0.52 miles south of Trout Creek, Texas.30.61156000, -93.8050600021Southwest-facing edge of mature woodland in part to full sun; well-drained, seasonally moist soils that are sandy loam; surface has an excellent organic litter layer.1952603NA 82643
450NA 81603(seedling of pink form)Rhododendron austrinum (Small) Rehder Florida, United StatesNA2013COLLECTED2013On the Escambia river near the mouth of the Yellow River. [GPS coordinates are actually at the confluence of the White River, the Little Simpson River, and the Buzzard Lake River (and gas line canal). -SBL]30.59699000, -87.22295000Plants were collected along along the sandy berms along river delta.1950972NA 81603
451Ames 32729286187Triadenum walteri (J. F. Gmel.) Gleason Texas, United StatesNC7SEED2011COLLECTED11/25/20052.4 km west of Interstate 45, south of FM 1488, Montgomery County.30.22427000, -95.49622000Above coastal mud flat. Sandy soil. Wild material1895385Ames 32729
452OPGC 7630MSB286693Xyris ambigua Beyr. ex Kunth Texas, United StatesOPGCSEED2011Wild material1895400OPGC 7630
453W6 42836MSB286523Juncus coriaceus Mack. Texas, United StatesW6SEED2011Wild material1895299W6 42836
454W6 42884MSB286224Pluchea foetida (L.) DC. Texas, United StatesW6SEED2011Wild material1895342W6 42884
455W6 42897MSB286615Rhynchospora inexpansa (Michx.) Vahl Texas, United StatesW6SEED2011Wild material1895355W6 42897
456OPGC 3957PZSH2011-34Phlox pilosa L. subsp. pulcherrima Lundell Texas, United StatesOPGC2011COLLECTED04/11/2011Shelby County; Approx 3.5 miles E of the juncture of State Route 87 and FM 2261, on S side of the road.31.61409000, -93.9122000087Roadside ditch, bordering Slash Pine plantations; Baptisia nuttalliana, Quercus spp., Pinus taeda, Carya texana, Smilax spp.Wild materialPlants erect, slender, to 45 cam tall; Flowers dull lavender-pink, with lavender-purple striae; leaves narrow-lanceolate, pilose abaxially.1907091OPGC 3957
457OPGC 3200TX-19Rudbeckia texana (Perdue) P. B. Cox & Urbatsch Texas, United StatesOPGC2010COLLECTED05/27/2010Upper West Gulf Coastal Plain. Jasper County. Roadside north of R255 between CR 61 and 60.31.04313900, -94.1583330048Roadside ROW/forest edge(adjacent to U.S. National Forest). Land form: Flat. Land Use: Roadside ROW. Geology: Sandstone. Soil Texture: Sandy. Soil Color: Tan.Wild materialPlants to 2 m tall, leathery leaves, rhizomatous; ray petals yellow.1897300OPGC 3200
458NA 78035AL #44Philadelphus inodorus L. Alabama, United StatesNA2008COLLECTED09/17/2008Just above the Cahaba River, near end of road and Caffee Creek.Wild material1913895NA 78035
459NA 78039ANN #3Frangula sp.Alabama, United StatesNA2008COLLECTED09/18/2008Calhoun County; ; Anniston Army Depot, woodland edge near roadWoodland edge near road.2108701NA 78039
460Ames 27660JM2004013Hypericum hypericoides (L.) Crantz South Carolina, United StatesNC7SEED2004COLLECTED10/06/2004Poe Creek outcrop, state forest, Pickens County.34.93055556, -82.86805556241Granite flatrock/glade community. Roadside. 10 degrees of slope. Calcareous soil. Wild material0.5-1 meter tall.1667580Ames 27660