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Your query included: All accessions taxonomy genus name like Ilex

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	ACCESSION	PLANT NAME	TAXONOMY	ORIGIN	GENEBANK	AVAILABILITY	RECEIVED	SOURCE TYPE	SOURCE DATE	COLLECTION SITE	COORDINATES	ELEVATION	HABITAT	IMPROVEMENT LEVEL	NARRATIVE
0	PI 691715	WLP 1260	Ilex mucronata (L.) M. Powell et al.	Maine, United States	NA		2014	COLLECTED			44.80087000, -67.12674000					1923674	PI 691715
1	PI 691727	WLP 1261	Ilex verticillata (L.) A. Gray	New York, United States	NA		2011	COLLECTED	09/12/2011	Hanging Bog Game Management Area, just west of Hanging Bog, Allegany County.	42.30500000, -78.25600000	632	Marsh. Associated with Aronia, Aster, Cornus amomum, Eutrochium, Salix, Solidago, Spiraea alba, Viburnum cassinoides, Viburnum dentatum, and Viburnum lentago.	Wild material		1891481	PI 691727
2	PI 691734	WLP 1262	Ilex opaca Aiton	North Carolina, United States	NA		2008	COLLECTED	11/05/2008			2106				1922752	PI 691734
3	PI 578191	'Scepter'	Ilex hybr.	District of Columbia, United States	NA	Not Available	1994	DONATED	03/23/1994					Cultivar	Red fruited evergreen tree to 30 feet with soft, spineless to weakly spined leaves	1473162	PI 578191
4	PI 560963	'Venus'	Ilex hybr.	District of Columbia, United States	NA	Not Available	1992	DEVELOPED						Cultivar	Large evergreen shrub to 18'. Numerous small spines on leaf margin. Female. Fruit red. Hardiness zone 7 on USDA Plant Hardiness Zone Map (1990). International Ilex cultivar registration 8-91. Selected and named by F.S. Santamour, Jr. and G.K. Eisenbeiss.	1455935	PI 560963
5	PI 560964	'Adonis'	Ilex hybr.	District of Columbia, United States	NA	Not Available	1992	DEVELOPED						Cultivar	Large evergreen shrub to 18'. Leaves large with numerous small spines on leaf margin. Male. Hardiness zone 7 on USDA Plant Hardiness Zone Map (1990). International Ilex cultivar registration 9-91. Selected and named by F.S. Santamour, Jr. and G.K. Eisenbeiss.	1455936	PI 560964
6	PI 560965	'Coronet'	Ilex hybr.	District of Columbia, United States	NA	Not Available	1992	DEVELOPED						Cultivar	Large evergreen shrub to 15'. Leaves soft, spiny. Female. Fruit red. Hardiness zone 7 on USDA Plant Hardiness Zone Map (1990). International Ilex cultivar registration 12-91. Selected by W.F. Kosar and named by G.K. Eisenbeiss.	1455937	PI 560965
7	PI 560966	'Miniature'	Ilex hybr.	District of Columbia, United States	NA	Not Available	1992	DEVELOPED						Cultivar	Evergreen shrub to 8'. Leaves small, strongly spined. Female. Fruit red. Hardiness zone 7 on USDA Plant Hardiness Zone Map (1990). International Ilex cultivar registration 13-91. Selected and named by W.F. Kosar.	1455938	PI 560966
8	PI 560967	'Sundrops'	Ilex serrata Thunb.	District of Columbia, United States	NA	Not Available	1992	DEVELOPED						Cultivar	Deciduous shrub to 8' tall and 15' wide. Female. Fruit yellow. Hardiness zone 5 on USDA Plant Hardiness Zone Map (1990). International Ilex cultivar registration 14-91.	1455939	PI 560967
9	PI 296109		Ilex fargesii Franch.	United Kingdom		Historic	1990	COLLECTED								1681379	PI 296109
10	PI 287736	'Golden Gem'	Ilex crenata Thunb.	British Columbia, Canada		Historic	1987	COLLECTED								1689796	PI 287736
11	PI 479432	NA 51056	Ilex crenata Thunb.	Japan	NA	Not Available	1982	COLLECTED	09/15/1982		44.88333333, 141.91666667			Wild material	Snow cover 1-2m per annum. Minimum temperature -17C. Shrub evergreen, 1.2m. Leaves lustrous above. Fruit black. Seed from one plant moved from wild.	1374368	PI 479432
12	PI 479433	JH-310-82	Ilex crenata Thunb. var. paludosa (Nakai) H. Hara	Japan		Historic	1982	COLLECTED	10/08/1982					Wild material	Snow 2-3m, 58 days of snow cover 50cm or deeper. Minimum temperature -20C. Cuttings collected from one male plant.	1374369	PI 479433
13	PI 479434	JH-305-82	Ilex crenata Thunb. var. paludosa (Nakai) H. Hara	Japan		Historic	1982	COLLECTED	10/08/1982		40.55000000, 140.96666667			Wild material	Snow 2-3m; 58 days covered by 50cm or deeper. Minimum temperature -20C. Shrub evergreen, 1.2-1.7m tall. Branches many, low spreading. Bark smooth, gray. Leaves lustrous above, pale beneath. Fruit nearly black. Growing in marsh on edge of small lake. Seed from several plants.	1374370	PI 479434
14	PI 479435	JH-267-82	Ilex leucoclada (Maxim.) Makino	Japan		Historic	1982	COLLECTED	10/05/1982		41.81666667, 140.80000000			Cultivated material	Snow cover for 2 days by snow 50cm or deeper. Minimum temperature -18C. Cuttings collected from a female plant moved from Kikonai-machi where it was native.	1374371	PI 479435
15	PI 479436	JH-312-82	Ilex leucoclada (Maxim.) Makino	Japan		Historic	1982	COLLECTED	10/08/1982		40.55000000, 140.96666667			Wild material	Snow cover 2-3m; 58 days covered by 50cm or deeper. Minimum temperature -20C. Cuttings collected from a male plant.	1374372	PI 479436
16	PI 479437	JH-326-82	Ilex leucoclada (Maxim.) Makino	Japan		Historic	1982	COLLECTED	10/09/1982		40.65000000, 140.83333333			Wild material	Snow 2-3m; 58 days covered by snow 50cm or deeper. Minimum temperature -20C. Growing in wooded area. Cuttings from 2 male plants.	1374373	PI 479437
17	PI 479438	JH-327-82	Ilex leucoclada (Maxim.) Makino	Japan		Historic	1982	COLLECTED	10/09/1982		40.65000000, 140.83333333			Wild material	Snow 2-3m; 58 days covered by snow 50cm or deeper. Minimum temperature -20C. Shrub evergreen, 60-90cm tall, erect habit, stems green. Leaves coriaceous deep green above, pale beneath. Fruit dark red, globose. Growing in Fagus crenata woodland. Cuttings from two female plants.	1374374	PI 479438
18	PI 479439	JH-390-82	Ilex macropoda Miq.	Japan		Historic	1982	COLLECTED	10/15/1982	Foot of Mt Nyokoo, near Zyakko Falls, Nikko, Tochigi-ken, Honshu				Wild material	Tree deciduous, 7.5m tall. Branches wide spreading. Bark smooth, whitish to gray. Leaves dark green above with impressed veins, pale beneath and lustrous. Fruit purplish red, sweet to taste. Growing in woodland on dry ridge.	1374375	PI 479439
19	PI 479440	JH-20-82	Ilex rugosa F. Schmidt	Japan		Historic	1982	COLLECTED	09/14/1982		45.08333333, 141.71666667			Wild material	Shrub evergreen, decumbent, 31-38.7cm. Branches rooting along, greenish. Leaves dark green aboe, rugose, light green green beneath. Fruits orange-red. Growing with Viburnum furcatum, Abies sacchalinensis, Magnolia, Quercus mongolica, Acanthopanax, Kalopanax. Seed from several plants.	1374376	PI 479440
20	PI 479441	JH-82-82	Ilex rugosa F. Schmidt	Japan		Historic	1982	COLLECTED	09/18/1982		44.05000000, 145.00000000			Wild material	Snow fall 2m per annum. Growing with trees similar to JH-75. Seed collected from several plants.	1374377	PI 479441
21	PI 479442	JH-112-82	Ilex rugosa F. Schmidt	Japan		Historic	1982	COLLECTED	09/21/1982		43.30000000, 145.60000000			Wild material	Snow cover 50cm or deeper for 30 days. Minimum temperature -23C. Shrub evergreen decumbent, 25-30cm tall. Stems declined. Twigs green. Leaves deep green above, lighter beneath. Fruit bright red. Growing in mixed woodland. Seed from several plants.	1374378	PI 479442
22	PI 479443	JH-102-82	Ilex sugerokii Maxim.	Japan		Historic	1982	COLLECTED	09/19/1982		44.05000000, 145.16666667			Wild material	Snow cover 1.5m per annum. Minimum temperature -20C. Shrub evergreen, 1-1.8m tall, multistemmed from base. Branches dense. Leaves subcoriaceous, lustrous above, light green beneath. Fruit red, lustrous. Growing in open woodland in sunny situation. Seed from several plants.	1374379	PI 479443
23	PI 479444	JH-347-82	Ilex sugerokii Maxim.	Japan		Historic	1982	COLLECTED	10/10/1982		40.61666667, 140.93333333			Wild material	Snow cover 2-3m, 58 days covered by 50cm or deeper. Minimum temperature -20C. Seed collected from several plants.	1374380	PI 479444
24	PI 479445	JH-348-82	Ilex sugerokii Maxim.	Japan		Historic	1982	COLLECTED	10/10/1982		40.61666667, 140.93333333			Wild material	Snow cover 2-3m, 58 days covered by snow 50 cm or deeper. Minimum temperature -20c. Cuttings taken from male plants.	1374381	PI 479445
25	PI 479446	JH-349-82	Ilex sugerokii Maxim.	Japan		Historic	1982	COLLECTED	10/10/1982		40.61666667, 140.93333333			Wild material	Snow cover 2-3m, 58 days covered by snow 50cm or deeper. Minimum temperature -20C. Cuttings taken from female plant.	1374382	PI 479446
26	PI 465978	'Sunny Foster'	Ilex ×attenuata Ashe	United States	NA	Not Available	1981	COLLECTED	1964	Discovered on grounds of National Arboretum in 1964 by W.F. Kosar				Cultivar	Tree evergreen with pale yellow variegated leaves. Similar in leaf shape, size, habit, hardiness, fruiting, and ease of culture to its parent clone 'Foster #2' except for slightly slower growth rate and the genetically stable variegated-leaf trait.	1360914	PI 465978
27	PI 452266	'Twiggy'	Ilex crenata Thunb.	District of Columbia, United States	NA	Not Available	1981	DONATED	01/1981					Cultivar	Plants compact, globe-shaped, densely branched. Shearing not required. Growth rate slow to moderate. Leaves small, elliptic, dark green.	1347202	PI 452266
28	PI 443301		Ilex verticillata (L.) A. Gray	United States		Historic	1980	COLLECTED	10/1978	Carbon Co., Pennsylvania					Collected by C. Heiney.	1338237	PI 443301
29	PI 443302		Ilex verticillata (L.) A. Gray	United States		Historic	1980	COLLECTED	10/1978	Crawford Co., Pennsylvania					Collected by K. Hinman.	1338238	PI 443302
30	PI 441093		Ilex decidua Walter	United States		Historic	1980	COLLECTED	12/1977	Bell Co., Texas					Collected by H. W. Everett.	1336029	PI 441093
31	PI 399369		Ilex aquifolium L.	Former Serbia and Montenegro		Historic	1975	COLLECTED								1300652	PI 399369
32	PI 399370		Ilex aquifolium L.	Former Serbia and Montenegro		Historic	1975	COLLECTED								1300653	PI 399370
33	PI 377678	Cacapon	Ilex verticillata (L.) A. Gray	West Virginia, United States		Historic	1972	DONATED	12/18/1972							1282955	PI 377678
34	PI 377680	'Jackson'	Ilex verticillata (L.) A. Gray		NA	Not Available	1972							Cultivar	From United States. Plants selected by O.M. Neal, Division of Plant Sciences, University of West Virginia, Morgantown, West Virginia. Received December 18, 1972. 'Jackson'. Origin same as P.I. 377678 ['Cacapon': Selected from several hundred mixed seedlings at Horticulture Farm]. Male plant, dark green foliage, produces abundant pollen. Ref: Plant Distribution List CR Form 7A. Comment: Selected from mixed seedlings from seed germination experiments.	2158608	PI 377680
35	PI 331202	'Alber Close'	Ilex hybr.		NA	Not Available	1969									2107845	PI 331202
36	PI 331204	'Howard Dorsett'	Ilex hybr.		NA	Not Available	1969	DEVELOPED							Considered a good companion plant to 'William Cowgill'. Selection made at the USPIS, Glenn Dale, MD	2107846	PI 331204
37	PI 331206	'Harry Gunning'	Ilex hybr.		NA	Not Available	1969	DEVELOPED							Selection made at USPIS, Glenn Dale, MD	2107847	PI 331206
38	PI 331203	'William Cowgill'	Ilex hybr.	Maryland, United States	NA	Not Available	1968	DONATED	06/25/1968					Cultivar		1246457	PI 331203
39	PI 378149	'Sparkleberry'	Ilex hybr.		NA	Not Available	1967									2107850	PI 378149
40	PI 422217	'Apollo'	Ilex hybr.		NA	Not Available	1967									2107853	PI 422217
41	PI 319168		Ilex aquifolium L.	Krym, Ukraine		Historic	1967	COLLECTED								1711101	PI 319168
42	PI 319169		Ilex colchica Pojark.	Krym, Ukraine		Historic	1967	COLLECTED								1711102	PI 319169
43	PI 319170		Ilex cornuta Lindl. & Paxton	Krym, Ukraine		Historic	1967	COLLECTED								1711103	PI 319170
44	PI 319171		Ilex latifolia Thunb.	Krym, Ukraine		Historic	1967	COLLECTED								1711104	PI 319171
45	PI 318660		Ilex insignis Hook. f.	India		Historic	1967	COLLECTED								1709553	PI 318660
46	PI 318661		Ilex wightiana Wall. ex Wight	India		Historic	1967	COLLECTED								1709554	PI 318661
47	PI 318652		Ilex aquifolium L.	Hordaland, Norway		Historic	1967	COLLECTED								1709547	PI 318652
48	PI 318549	Col. No. K-13	Ilex crenata Thunb.	Jeju-teukbyeoljachido, Korea, South		Historic	1967	COLLECTED		South slope, Mt. Halla, Cheju Island, moist open area		1200		Wild material	Small leaved, evergreen, dwarf shrub with small white flowers. Male plant. Plants. 10	1237106	PI 318549
49	PI 317234	Col. No. K-442	Ilex crenata Thunb.	Jeju-teukbyeoljachido, Korea, South		Historic	1966	COLLECTED		Open alpine meadow, Mt. Halla, Cheju Island		1400				1708746	PI 317234
50	PI 317235	Col. No. K-426	Ilex crenata Thunb.	Jeju-teukbyeoljachido, Korea, South		Historic	1966	COLLECTED		Along trail up Mt. Halla, Cheju Island		700				1708747	PI 317235
51	PI 317035	No. 733	Ilex canariensis Poir.	Canarias, Spain		Historic	1966	COLLECTED								1708358	PI 317035
52	PI 317040	No. 327	Ilex mitis (L.) Radlk.	South Africa		Historic	1966	COLLECTED								1708363	PI 317040
53	PI 316703	Col. No. K-249	Ilex macropoda Miq.	Korea, South		Historic	1966	COLLECTED		In open, along trail on Mt. Sok Ni		450				1708213	PI 316703
54	PI 316704	Col. No. K-274	Ilex macropoda Miq.	Korea, South		Historic	1966	COLLECTED		Along road to Mt. Tok-Yu, Ko Chun						1708214	PI 316704
55	PI 316603	Col. No. K-133	Ilex macropoda Miq.	Korea, South		Historic	1966	COLLECTED		Along trail up Mt. Chiri, Cholla Namdo		1100				1708088	PI 316603
56	PI 316588	'High Light'	Ilex crenata Thunb.	District of Columbia, United States		Historic	1966	COLLECTED								1708072	PI 316588
57	PI 315894		Ilex pedunculosa Miq.	Japan		Historic	1966	COLLECTED		Kaseda, Kyusiu Island						1707714	PI 315894
58	PI 315213		Ilex colchica Pojark.	Russian Federation		Historic	1966	COLLECTED								1707457	PI 315213
59	PI 329155	'Tanager'	Ilex hybr.		NA	Not Available	1966									2107844	PI 329155
60	PI 313116	'Mariesii'	Ilex crenata Thunb.	United Kingdom		Historic	1966	COLLECTED								1706182	PI 313116
61	PI 311717		Ilex sikkimensis Kurz	United Kingdom		Historic	1966	COLLECTED								1705494	PI 311717
62	PI 311301		Ilex intricata Hook. f.	India		Historic	1966	COLLECTED								1705293	PI 311301
63	PI 578192	'Geisha'	Ilex crenata Thunb.	District of Columbia, United States		Historic	1966	DONATED	03/23/1994					Cultivar	Donated by G. Eisenbeiss, USDA-ARS, National Arboretum, 3501 New York Ave., N.D., Washington, D.C. 20002, United States. Received [PI numbered] 3/23/1994. 'Geisha'. Female parent PI 231948, NA 10815 a yellow fruited plant from Japan. Male parent NA 10822 a F2 backcross of a male seedling of NA 10815, back crossed to 10815. Evergreen shrub with extremely small convex leaves and yellow fruit.	1473163	PI 578192
64	PI 308634		Ilex asprella (Hook. & Arn.) Champ. ex Benth.	Hong Kong		Historic	1965	COLLECTED								1704344	PI 308634
65	PI 308635		Ilex pubescens Hook. & Arn.	Hong Kong		Historic	1965	COLLECTED								1704345	PI 308635
66	PI 308636		Ilex viridis Champ. ex Benth.	Hong Kong		Historic	1965	COLLECTED								1704346	PI 308636
67	PI 307274	Col. No. 122	Ilex hookeri King	West Bengal, India		Historic	1965	COLLECTED		Between Phalut and Samanden		2860				1702786	PI 307274
68	PI 307275	Col. No. 208	Ilex insignis Hook. f.	West Bengal, India		Historic	1965	COLLECTED								1702787	PI 307275
69	PI 307276	Col. No. 176	Ilex intricata Hook. f.	West Bengal, India		Historic	1965	COLLECTED		Mt. Tonglu, along trail from Batasi		2408				1702788	PI 307276
70	PI 307277	Col. No. 209	Ilex wightiana Wall. ex Wight	West Bengal, India		Historic	1965	COLLECTED								1702789	PI 307277
71	PI 307278	Col. No. 282	Ilex wightiana Wall. ex Wight	West Bengal, India		Historic	1965	COLLECTED		Darjeeling						1702790	PI 307278
72	PI 306368	366, 499	Ilex aquifolium L.	Germany		Historic	1965	COLLECTED								1702235	PI 306368
73	PI 305310		Ilex aquifolium L.	Denmark		Historic	1965	COLLECTED								1701265	PI 305310
74	PI 305311		Ilex aquifolium L.	Denmark		Historic	1965	COLLECTED								1701266	PI 305311
75	PI 305312		Ilex aquifolium L.	Denmark		Historic	1965	COLLECTED								1701268	PI 305312
76	PI 305313	'Pyramidalis'	Ilex aquifolium L.	Denmark		Historic	1965	COLLECTED								1701267	PI 305313
77	PI 304944		Ilex crenata Thunb.	Hirosima, Japan		Historic	1965	COLLECTED								1701086	PI 304944
78	PI 304945		Ilex crenata Thunb.	Hirosima, Japan		Historic	1965	COLLECTED								1701087	PI 304945
79	PI 304946		Ilex purpurea Hassk.	Kagosima, Japan		Historic	1965	COLLECTED								1701088	PI 304946
80	PI 304947		Ilex rotunda Thunb.	Hirosima, Japan		Historic	1965	COLLECTED								1701089	PI 304947
81	PI 260386 NA 25704		Ilex crenata Thunb.	Honshu, Japan	NA	Not Available	1964	COLLECTED	PRE 09/09/1959	Aomori Prefecture: Mutsu-shi.				Wild material	Received as a single seedling, inocrrectly identified as I. crenata var. paludosa. From USDA Plant Inventory No. 167: "260384 to 260393. From Japan. Seeds presented by the Government Forest Experiment Station, Okidate, Aomori. Received September 9, 1959. [...] 260385 and 260386. Ilex crenata var. paludosa Thunb. Aquifoliaceae. [...] 260386. Province Mutsu." [This accession does not display the low and spreading (or low and creeping) habit of I. crenata var. paludosa found in other individuals. Instead, the habit is vertical, significantly taller than wide, yet open (not narrowly fastigiate). Both remaining plants of this accession have this appearance (which makes sense, since they belong to a single seedling clone). The closely-ranked foliage is also interesting, being more prominently and sharply toothed than typical Ilex crenata. Male.	2191651	PI 260386 NA 25704
82	PI 299436		Ilex asprella (Hook. & Arn.) Champ. ex Benth.	Hong Kong		Historic	1964	COLLECTED								1677912	PI 299436
83	PI 299437		Ilex cinerea Champ. ex Benth.	Hong Kong		Historic	1964	COLLECTED								1677913	PI 299437
84	PI 299438		Ilex graciliflora Champ. ex Benth.	Hong Kong		Historic	1964	COLLECTED								1677914	PI 299438
85	PI 299439		Ilex memecylifolia Champ. ex Benth.	Hong Kong		Historic	1964	COLLECTED								1677915	PI 299439
86	PI 299440		Ilex pubescens Hook. & Arn.	Hong Kong		Historic	1964	COLLECTED								1677916	PI 299440
87	PI 299441		Ilex rotunda Thunb.	Hong Kong		Historic	1964	COLLECTED								1677917	PI 299441
88	PI 299399		Ilex mitis (L.) Radlk.	South Africa		Historic	1964	COLLECTED								1677895	PI 299399
89	PI 298031		Ilex mitis (L.) Radlk.	South Africa		Historic	1964	COLLECTED								1682694	PI 298031
90	PI 296985	No. 1	Ilex centrochinensis S. Y. Hu	Japan		Historic	1964	COLLECTED								1681832	PI 296985
91	PI 296986	No. 2	Ilex centrochinensis S. Y. Hu	Japan		Historic	1964	COLLECTED								1681833	PI 296986
92	PI 296020		Ilex macropoda Miq.	Iwate, Japan		Historic	1964	COLLECTED								1681335	PI 296020
93	PI 292361	No. 372	Ilex mitis (L.) Radlk.	South Africa		Historic	1963	COLLECTED								1695403	PI 292361
94	PI 291938		Ilex verticillata (L.) A. Gray	Ontario, Canada		Historic	1963	COLLECTED		Hamilton						1694777	PI 291938
95	PI 291939		Ilex verticillata (L.) A. Gray	Canada		Historic	1963	COLLECTED		Northumberland County, Colborne						1694778	PI 291939
96	PI 291941	No. 12362	Ilex mucronata (L.) M. Powell et al.	Ontario, Canada		Historic	1963	COLLECTED		Borthwick Road, 6.4km east of Ramsayville						1694780	PI 291941
97	PI 289935		Ilex sp.	Nepal		Historic	1963	COLLECTED								1692350	PI 289935
98	PI 289743	'Golden Gem'	Ilex crenata Thunb.	Netherlands		Historic	1963	COLLECTED								1692248	PI 289743
99	PI 288703		Ilex aquifolium L.	Japan		Historic	1963	COLLECTED								1691441	PI 288703
100	PI 288704		Ilex centrochinensis S. Y. Hu	Japan		Historic	1963	COLLECTED								1691442	PI 288704
101	PI 286159		Ilex macropoda Miq.	Japan		Historic	1963	COLLECTED								1689099	PI 286159
102	PI 285365	Col. No. 1272	Ilex excelsa (Wall.) Hook. f.	Nepal		Historic	1962	COLLECTED		Along streambed above Godavari		1806				1688818	PI 285365
103	PI 285445	Col. No. 1154	Ilex dipyrena Wall.	Nepal		Historic	1962	COLLECTED		In forest with rhododendrons, Mt. Furkai		2559				1688895	PI 285445
104	PI 285469	Col. No. 1234	Ilex sp.	Nepal		Historic	1962	COLLECTED		Rhododendron forest above Mardi Khola		2408				1688918	PI 285469
105	PI 284783		Ilex paraguariensis A. St.-Hil.	Australia		Historic	1962	COLLECTED								1687948	PI 284783
106	PI 282697		Ilex asprella (Hook. & Arn.) Champ. ex Benth.	Hong Kong		Historic	1962	COLLECTED								1686697	PI 282697
107	PI 282698		Ilex hanceana Maxim.	Hong Kong		Historic	1962	COLLECTED								1686698	PI 282698
108	PI 282478		Ilex mitis (L.) Radlk.	South Africa		Historic	1962	COLLECTED								1686569	PI 282478
109	PI 282427	'Agena'	Ilex ×koehneana Loes.	District of Columbia, United States	NA	Not Available	1962	DEVELOPED						Cultivar	International Ilex cultivar registration 11-91.	1209826	PI 282427
110	PI 279951		Ilex centrochinensis S. Y. Hu	Japan		Historic	1962	COLLECTED								1685028	PI 279951
111	PI 279952	DEIP No. 21.274	Ilex paraguariensis A. St.-Hil.	Argentina		Historic	1962	COLLECTED								1685029	PI 279952
112	PI 280057	'Madame Briot'	Ilex aquifolium L.	United Kingdom		Historic	1962	COLLECTED								1685065	PI 280057
113	PI 280058	'Longifolia'	Ilex aquifolium L.	United Kingdom		Historic	1962	COLLECTED								1685066	PI 280058
114	PI 279006	JC0461	Ilex crenata Thunb.	Japan		Historic	1962	COLLECTED								1700507	PI 279006
115	PI 276341	JC0461	Ilex rotunda Thunb.	Maryland, United States		Historic	1961	DONATED	08/17/1961							1206711	PI 276341
116	PI 272055		Ilex serrata Thunb.		NA	Not Available	1961							Cultivated material	From the record of NA 17022 at the U.S. National Arboretum: "From Japan. Seeds purchased from P. H. Kubota, Nikko Tochigi Prefecture. Received March 3, 1961. Collected from cultivated plants in Angyo, Saitama Prefecture. Comments: 9 seedlings flowered 3 males, 6 females; 1 female yellow-fruited; the remaining red-fruited. Only 3 listed in locations remain NA 17022-1 named 'Sundrops' 1991. NA 17022-1 reaccessioned to NA 62386 (3/91) to be named and released by G. Eisenbeiss. See NA 62386 'Sundrops' & HSA Reg. 1991. Name changed to Ilex serrata - not all seedlings bear white/yellow fruit so name is inappropriate, and according to Eisenbeiss's notes, only one NA 17022 seedling actually bore yellow fruit and became 'Sundrops', so presumably the remaining fraction are red-fruited or male. They should, however, at least carry the recessive gene for yellow/pale fruit. -SBL"	2158576	PI 272055
117	PI 269620	'Ajax'	Ilex ×koehneana Loes.	District of Columbia, United States	NA	Not Available	1960	DEVELOPED						Cultivar	International Ilex cultivar registration 10-91.	1202833	PI 269620
118	PI 267825	'John T. Morris'	Ilex hybr.	District of Columbia, United States	NA	Not Available	1960	DONATED	08/15/1960					Cultivar		1201580	PI 267825
119	PI 329153	'Elegance'	Ilex hybr.		NA	Not Available	1960									2107842	PI 329153
120	PI 329154	'Accent'	Ilex hybr.		NA	Not Available	1960									2107843	PI 329154
121	PI 371685	'Ruby'	Ilex ×koehneana Loes.		NA	Not Available	1960	DEVELOPED						Cultivar	P1 female = NA 3935 I. aquifolium (Whitney sel.) PP2 male = NA 7528-3 I. latifolia Vigorous, conical tree to 6.5m tall. More hardy and more tolerant to adverse exposure and soil than parent species. Lvs. evergreen, 15 to 18cm long, intermediate in number and legnth of spines between parent species. Frts. bright red, borne on short pedicels, intermediate in size between those of parents.	1278576	PI 371685
122	PI 371686	'Jade'	Ilex ×koehneana Loes.		NA	Not Available	1960	DEVELOPED						Cultivar	P1 female = NA 3935 I. aquifolium (Whitney sel.) P2 male = NA 7528-3 I. latifolia Male selection from F1 population hybrid and a brother seedling of PI 371685. Very similar to 'Ruby' in foliage, habit of growth, and hardiness and is being introduced as a pollinator for 'Ruby'.	1278577	PI 371686
123	PI 267253	'Media Picta'	Ilex aquifolium L.	Scotland, United Kingdom		Historic	1960	DEVELOPED						Cultivar		1201272	PI 267253
124	PI 267255	'Recurva'	Ilex aquifolium L.	Scotland, United Kingdom		Historic	1960	DEVELOPED						Cultivar		1201273	PI 267255
125	PI 267257	'Whittingtonensis'	Ilex aquifolium L.	Scotland, United Kingdom		Historic	1960	DEVELOPED						Cultivar		1201274	PI 267257
126	PI 267259	'Ferox Aurea'	Ilex aquifolium L.	Scotland, United Kingdom		Historic	1960	DONATED	06/14/1960					Cultivar		1201275	PI 267259
127	PI 267261	'Ferox'	Ilex aquifolium L.	Scotland, United Kingdom		Historic	1960	DEVELOPED						Cultivar		1201276	PI 267261
128	PI 267263	'Pendula'	Ilex aquifolium L.	Scotland, United Kingdom	NA	Not Available	1960	DEVELOPED						Cultivar		1201277	PI 267263
129	PI 267266	'Crassifolia'	Ilex aquifolium L.	Scotland, United Kingdom		Historic	1960	DONATED	06/14/1960					Cultivar		1201278	PI 267266
130	PI 267267	NA 15351	Ilex crenata Thunb.	Scotland, United Kingdom	NA	Not Available	1960	DONATED	06/14/1960					Cultivar	Received as Ilex crenata f. latifolia major. From the record of NA15351 at the U.S. National Arboretum: 9/86: T. R. Dudley changed name from f. latifolia major to cv. Major; 3/94: TR Dudley & G. Eisenbeiss noted that the cv. name Major has been applied to several clones. We are unsure of what we have, so we reduced the name to the species. (see Ilex crenata checklist).	1201279	PI 267267
131	PI 263648		Ilex crenata Thunb.	Hukuoka, Japan		Historic	1960	DONATED	02/18/1960							1568064	PI 263648
132	PI 263649	'Convexa'	Ilex crenata Thunb.	Hukuoka, Japan		Historic	1960	DONATED	02/18/1960							1568065	PI 263649
133	PI 263651		Ilex integra Thunb.	Hukuoka, Japan		Historic	1960	DONATED	02/18/1960							1568066	PI 263651
134	PI 263652		Ilex latifolia Thunb.	Hukuoka, Japan		Historic	1960	DONATED	02/18/1960							1568067	PI 263652
135	PI 263653		Ilex pedunculosa Miq.	Hukuoka, Japan		Historic	1960	DONATED	02/18/1960							1568068	PI 263653
136	PI 263654		Ilex rotunda Thunb.	Hukuoka, Japan		Historic	1960	DONATED	02/18/1960							1568069	PI 263654
137	PI 263655		Ilex serrata Thunb.	Hukuoka, Japan		Historic	1960	DONATED	02/18/1960							1568070	PI 263655
138	PI 262783		Ilex latifolia Thunb.	Saitama, Japan		Historic	1960	DONATED	01/06/1960							1567351	PI 262783
139	PI 261745	'Brevipedunclata'	Ilex sugerokii Maxim.	Tôkyô, Japan		Historic	1959	DONATED	12/09/1959							1566725	PI 261745
140	PI 261441		Ilex perado Aiton	Maryland, United States		Historic	1959	DONATED	11/25/1959							1565884	PI 261441
141	PI 261224	'Bicolor'	Ilex aquifolium L.	England, United Kingdom		Historic	1959	DONATED	11/12/1959							1565713	PI 261224
142	PI 261225	'Latispina Minor'	Ilex aquifolium L.	England, United Kingdom		Historic	1959	DONATED	11/12/1959							1565714	PI 261225
143	PI 261226	'N.E. Barnes'	Ilex aquifolium L.	England, United Kingdom		Historic	1959	DONATED	11/12/1959							1565715	PI 261226
144	PI 261227	'Recurva'	Ilex aquifolium L.	England, United Kingdom		Historic	1959	DONATED	11/12/1959							1565716	PI 261227
145	PI 261228	'Variegata'	Ilex aquifolium L.	England, United Kingdom		Historic	1959	DONATED	11/12/1959							1565717	PI 261228
146	PI 261229		Ilex cassine L.	England, United Kingdom		Historic	1959	DONATED	11/12/1959							1565718	PI 261229
147	PI 261230		Ilex corallina Franch.	England, United Kingdom		Historic	1959	DONATED	11/12/1959							1565719	PI 261230
148	PI 261231		Ilex dipyrena Wall.	England, United Kingdom		Historic	1959	DONATED	11/12/1959							1565720	PI 261231
149	PI 261233	'Sclerophylla'	Ilex fargesii Franch.	England, United Kingdom		Historic	1959	DONATED	11/12/1959							1565721	PI 261233
150	PI 261234		Ilex hookeri King	England, United Kingdom		Historic	1959	DONATED	11/12/1959							1565722	PI 261234
151	PI 261235		Ilex fargesii Franch. subsp. melanotricha (Merr.) S. Andrews	England, United Kingdom		Historic	1959	DONATED	11/12/1959							1565723	PI 261235
152	PI 261236		Ilex yunnanensis Franch.	England, United Kingdom		Historic	1959	DONATED	11/12/1959							1565724	PI 261236
153	PI 261237	'Forest 24826'	Ilex sp.	England, United Kingdom		Historic	1959	DONATED	11/12/1959							1565725	PI 261237
154	PI 261216		Ilex fargesii Franch. subsp. melanotricha (Merr.) S. Andrews	England, United Kingdom		Historic	1959	DONATED	11/10/1959							1565709	PI 261216
155	PI 260749		Ilex cornuta Lindl. & Paxton	Maryland, United States		Historic	1959	DONATED	10/13/1959							1563455	PI 260749
156	PI 260385		Ilex crenata Thunb. var. paludosa (Nakai) H. Hara	Honshu, Japan		Historic	1959	DONATED	09/09/1959							1563168	PI 260385
157	PI 260386		Ilex crenata Thunb.	Honshu, Japan	NA	Not Available	1959	COLLECTED	PRE 09/09/1959	Aomori Prefecture: Mutsu-shi.				Wild material	From the record of NA 25704 at the U.S. National Arboretum: From USDA Plant Inventory No. 167: "260384 to 260393. From Japan. Seeds presented by the Government Forest Experiment Station, Okidate, Aomori. Received September 9, 1959. [...] 260385 and 260386. Ilex crenata var. paludosa Thunb. Aquifoliaceae. [...] 260386. Province Mutsu." [This accession does not display the low and spreading (or low and creeping) habit of I. crenata var. paludosa found in other individuals. Instead, the habit is vertical, significantly taller than wide, yet open (not narrowly fastigiate). Both remaining plants of this accession have this appearance. -SBL	2158600	PI 260386
158	PI 260387		Ilex macropoda Miq.	Honshu, Japan		Historic	1959	DONATED	09/09/1959							1563169	PI 260387
159	PI 260388		Ilex leucoclada (Maxim.) Makino	Honshu, Japan		Historic	1959	DONATED	09/09/1959							1563170	PI 260388
160	PI 260389		Ilex sugerokii Maxim.	Honshu, Japan		Historic	1959	DONATED	09/09/1959							1563171	PI 260389
161	PI 255344		Ilex aquifolium L.	Slovenia		Historic	1959	DONATED	02/06/1959							1558166	PI 255344
162	PI 267824	'Lydia Morris'	Ilex hybr.		NA	Not Available	1959									2107833	PI 267824
163	PI 254592		Ilex cassine L.	England, United Kingdom		Historic	1958	DONATED	12/12/1958							1195485	PI 254592
164	PI 422216	'September Gem'	Ilex hybr.		NA	Not Available	1958									2107852	PI 422216
165	PI 237879		Ilex rotunda Thunb.	Japan		Historic	1957	COLLECTED						Wild material		1186374	PI 237879
166	PI 236233	Nakada	Ilex crenata Thunb.	Japan	NA	Not Available	1957	COLLECTED						Cultivar		1185655	PI 236233
167	PI 235574		Ilex triflora Blume var. kanehirae (Yamam.) S. Y. Hu		NA	Not Available	1956							Cultivated material		2158542	PI 235574
168	PI 231705	'Watereriana'	Ilex aquifolium L.	England, United Kingdom	NA	Not Available	1956	DONATED	03/14/1956					Cultivar		1184010	PI 231705
169	PI 231948		Ilex crenata Thunb.	District of Columbia, United States		Historic	1956	DEVELOPED	1968					Cultivar		1492198	PI 231948
170	PI 198275	B-43193	Ilex aquifolium L.	Maryland, United States		Historic	1951	COLLECTED								1675898	PI 198275
171	PI 198276	B-43194	Ilex aquifolium L.	Maryland, United States		Historic	1951	COLLECTED								1675899	PI 198276
172	PI 198277	B-43195	Ilex cornuta Lindl. & Paxton	Maryland, United States		Historic	1951	COLLECTED								1675900	PI 198277
173	PI 198278	B-10909	Ilex cornuta Lindl. & Paxton	Maryland, United States		Historic	1951	COLLECTED								1675901	PI 198278
174	PI 198279	B-10909A	Ilex cornuta Lindl. & Paxton	Maryland, United States		Historic	1951	COLLECTED								1675902	PI 198279
175	PI 198280		Ilex sp.	Maryland, United States		Historic	1951	COLLECTED								1675903	PI 198280
176	PI 195133		Ilex cornuta Lindl. & Paxton	Maryland, United States		Historic	1951	COLLECTED								1671868	PI 195133
177	PI 148016		Ilex sp.	Virginia, United States		Historic	1944	COLLECTED		Bennet's Creek						1881606	PI 148016
178	PI 148017		Ilex sp.	Virginia, United States		Historic	1944	COLLECTED		Bennet's Creek						1881607	PI 148017
179	PI 146599		Ilex sp.	Amazonas, Brazil		Historic	1943	COLLECTED	05/08/1943	Porto Velho						1879927	PI 146599
180	PI 143795	'Rotunda'	Ilex cornuta Lindl. & Paxton	Louisiana, United States	NA	Not Available	1942	COLLECTED						Cultivar		1869732	PI 143795
181	PI 141022	No. 6347	Ilex sp.	Māzandarān, Iran		Historic	1941	COLLECTED	07/23/1940	Dimalu						1865646	PI 141022
182	PI 139217	No. 5293	Ilex coriacea (Pursh) Chapm.	Georgia, United States		Historic	1940	COLLECTED	08/24/1940	Homerville						1862378	PI 139217
183	PI 207438	NA 25	Ilex aquifolium L.	Colombia		Historic	1938	DONATED	10/19/1938					Cultivated material		1173508	PI 207438
184	PI 207439	NA 26	Ilex aquifolium L.	Colombia		Historic	1938	DONATED	10/19/1938					Cultivated material		1173509	PI 207439
185	PI 207440	NA 27	Ilex aquifolium L.	Colombia		Historic	1938	DONATED	10/19/1938					Cultivated material		1173510	PI 207440
186	PI 130082	No. 7826	Ilex sp.	Yunnan Sheng, China		Historic	1938	COLLECTED		Dokerla, Atuntze		3000				1846009	PI 130082
187	PI 130083	No. 7831	Ilex sp.	Yunnan Sheng, China		Historic	1938	COLLECTED		Dokerla, Atuntze		3100				1846010	PI 130083
188	PI 130084	No. 10610	Ilex sp.	Yunnan Sheng, China		Historic	1938	COLLECTED		Mount Kaaperpu, Atuntze		3000				1846011	PI 130084
189	PI 130085	No. 13536	Ilex sp.	Yunnan Sheng, China		Historic	1938	COLLECTED		Haba, Chungtien		3400				1846012	PI 130085
190	PI 130086	No. 14283	Ilex sp.	Yunnan Sheng, China		Historic	1938	COLLECTED		Kulu, Muli		3200				1846013	PI 130086
191	PI 130087	No. 14921	Ilex sp.	Yunnan Sheng, China		Historic	1938	COLLECTED		Paitih, Chungtien		2700				1846014	PI 130087
192	PI 129234	No. 1278	Ilex sp.	Sichuan Sheng, China		Historic	1938	COLLECTED	10/1937	Mount Omei		600				1845272	PI 129234
193	PI 129235	No. 1285	Ilex sp.	Sichuan Sheng, China		Historic	1938	COLLECTED	10/1937	Mount Omei		6000				1845273	PI 129235
194	PI 129236	No. 1288	Ilex sp.	Sichuan Sheng, China		Historic	1938	COLLECTED	10/1937	Mount Omei between 900m and 1000m altitude						1845274	PI 129236
195	PI 129237	No. 1313	Ilex sp.	Sichuan Sheng, China		Historic	1938	COLLECTED	11/1937	Tien Chuan Hsien		2300				1845275	PI 129237
196	PI 129238	No. 1349	Ilex sp.	Sichuan Sheng, China		Historic	1938	COLLECTED	11/1937	O-pie Hsien		1700				1845276	PI 129238
197	PI 129239	No. 1373	Ilex sp.	Sichuan Sheng, China		Historic	1938	COLLECTED	10/1937	Mount Omei		1800				1845277	PI 129239
198	PI 129240	No. 1396	Ilex sp.	Sichuan Sheng, China		Historic	1938	COLLECTED	11/1937	Tien Chuan Hsien		500				1845278	PI 129240
199	PI 124708		Ilex pedunculosa Miq.	China		Historic	1937	COLLECTED								1839275	PI 124708
200	PI 124250		Ilex hookeri King	India		Historic	1937	COLLECTED								1838086	PI 124250
201	PI 124251		Ilex insignis Hook. f.	India		Historic	1937	COLLECTED								1838087	PI 124251
202	PI 122095	No. 1919	Ilex insignis Hook. f.	West Bengal, India		Historic	1937	COLLECTED	12/1936	Darjeeling						1833020	PI 122095
203	PI 122096	No. 1920	Ilex sp.	West Bengal, India		Historic	1937	COLLECTED	12/1936	Darjeeling						1833021	PI 122096
204	PI 122673	No. 2401	Ilex sp.	Trabzon, Turkey		Historic	1937	COLLECTED	08/12/1936	23km east of Trabzon						1834157	PI 122673
205	PI 117060		Ilex geniculata Maxim.	Japan		Historic	1936	COLLECTED								1826404	PI 117060
206	PI 116873	No. 439	Ilex sp.	Hunan Sheng, China		Historic	1936	COLLECTED	10/1935	Ma-Ling-Tung		564				1825132	PI 116873
207	PI 114757	No. 100	Ilex corallina Franch.	China		Historic	1936	COLLECTED								1813205	PI 114757
208	PI 114758	No. 101	Ilex dunniana H. Lév.	China		Historic	1936	COLLECTED								1813206	PI 114758
209	PI 114759	No. 102	Ilex pernyi Franch.	China		Historic	1936	COLLECTED								1813207	PI 114759
210	PI 111359	No. 18	Ilex micrococca Maxim.	Hubei Sheng, China		Historic	1935	COLLECTED		Western Hubei						1803744	PI 111359
211	PI 111360	No. 74	Ilex micrococca Maxim.	Hubei Sheng, China		Historic	1935	COLLECTED		Western Hubei						1803745	PI 111360
212	PI 111388	No. 21	Ilex purpurea Hassk.	Hubei Sheng, China		Historic	1935	COLLECTED		Western Hubei						1803772	PI 111388
213	PI 110867		Ilex cornuta Lindl. & Paxton	California, United States		Historic	1935	COLLECTED								1492168	PI 110867
214	PI 110289		Ilex pubescens Hook. & Arn.	Guangdong Sheng, China		Historic	1935	COLLECTED	11/1934	Chinchow on the North River		301				1801738	PI 110289
215	PI 108761		Ilex aquifolium L.	Bosnia and Herzegovina		Historic	1935	COLLECTED		Above Sarajevo						1798990	PI 108761
216	PI 109296	No. T-337	Ilex sp.	Bolu, Turkey		Historic	1935	COLLECTED	10/09/1934	About 14.4km west of Bolu						1568213	PI 109296
217	PI 107725		Ilex opaca Aiton	Unknown		Historic	1934	COLLECTED		Yugoslavia						1797459	PI 107725
218	PI 107436	'Argentea marginata'	Ilex aquifolium L.	New York, United States		Historic	1934	COLLECTED								1492678	PI 107436
219	PI 107437	'Argentea medio-picta'	Ilex aquifolium L.	New York, United States		Historic	1934	COLLECTED								1796805	PI 107437
220	PI 107438	(seed of 'Aurifodina')	Ilex aquifolium L.	New York, United States	NA	Not Available	1934	COLLECTED						Cultivated material		1796806	PI 107438
221	PI 107439	CamelliIfolia (seedling)	Ilex ×altaclerensis (Loudon) Dallim.	New York, United States		Historic	1934	COLLECTED								1796807	PI 107439
222	PI 107440	'Ciliata major'	Ilex aquifolium L.	New York, United States		Historic	1934	COLLECTED								1796808	PI 107440
223	PI 107441	'Cookii'	Ilex aquifolium L.	New York, United States		Historic	1934	COLLECTED								1796809	PI 107441
224	PI 107442	'Flavescens'	Ilex aquifolium L.	New York, United States		Historic	1934	COLLECTED								1796810	PI 107442
225	PI 107443	(seed of 'Fructu Luteo')	Ilex aquifolium L.	New York, United States	NA	Not Available	1934	COLLECTED						Cultivated material		1796811	PI 107443
226	PI 107444	'Integrifolia'	Ilex aquifolium L.	New York, United States		Historic	1934	COLLECTED								1796812	PI 107444
227	PI 107445	'Rubicaulis aurea'	Ilex aquifolium L.	New York, United States		Historic	1934	COLLECTED								1796813	PI 107445
228	PI 107446		Ilex sp.	New York, United States		Historic	1934	COLLECTED								1796814	PI 107446
229	PI 107447		Ilex sp.	New York, United States		Historic	1934	COLLECTED								1796815	PI 107447
230	PI 107448		Ilex perado Aiton subsp. platyphylla (Webb & Berthel.) S. Andrews	New York, United States		Historic	1934	COLLECTED								1796816	PI 107448
231	PI 107626		Ilex aquifolium L.	Bosnia and Herzegovina		Historic	1934	COLLECTED		Sarajevo						1797032	PI 107626
232	PI 105888		Ilex sp.	Uttar Pradesh, India		Historic	1934	COLLECTED		Sarahan						1793810	PI 105888
233	PI 105610	No. F. 87	Ilex sp.	Jiangsu Sheng, China		Historic	1934	COLLECTED	09/15/1933	Near Ta Tseh Tsuen, Yung Hsien		301				1794445	PI 105610
234	PI 112222	No. 47	Ilex sp.	China		Historic	1934	COLLECTED		Ta Tseh Tsuen, Yung Hsien						1491957	PI 112222
235	PI 105320		Ilex purpurea Hassk.	China		Historic	1934	COLLECTED								1793948	PI 105320
236	PI 105321		Ilex rotunda Thunb.	China		Historic	1934	COLLECTED								1793949	PI 105321
237	PI 105322		Ilex viridis Champ. ex Benth.	China		Historic	1934	COLLECTED								1793950	PI 105322
238	PI 105323		Ilex wilsonii Loes.	China		Historic	1934	COLLECTED								1793951	PI 105323
239	PI 103698		Ilex paraguariensis A. St.-Hil.	Paraguay		Historic	1933	COLLECTED								1493572	PI 103698
240	PI 103447	No. 24323	Ilex sp.	Sichuan Sheng, China		Historic	1933	COLLECTED		Mutirong, Muli Territory		3311				1791781	PI 103447
241	PI 103459	No. 22299	Ilex sp.	China		Historic	1933	COLLECTED		Solola, Tsarung Province		3763				1791795	PI 103459
242	PI 103460	No. 23654	Ilex sp.	China		Historic	1933	COLLECTED		Mountains of Kaakerbo, Tsarung Province		3010				1791796	PI 103460
243	PI 103427	No. D-335	Ilex corallina Franch.	China		Historic	1933	COLLECTED								1791763	PI 103427
244	PI 103221	No. 24556	Ilex pernyi Franch.	Sichuan Sheng, China		Historic	1933	COLLECTED		Between Muli and Kulu		2709				1791523	PI 103221
245	PI 102905		Ilex hookeri King	India		Historic	1933	COLLECTED								1791234	PI 102905
246	PI 102906		Ilex insignis Hook. f.	India		Historic	1933	COLLECTED								1791235	PI 102906
247	PI 102944	No. 5	Ilex sp.	Jiangxi Sheng, China		Historic	1933	COLLECTED		Huangyensze						1791273	PI 102944
248	PI 102945	No. 53	Ilex sp.	Jiangxi Sheng, China		Historic	1933	COLLECTED		Kuanyinchiao						1791274	PI 102945
249	PI 102946	No. 68	Ilex sp.	Jiangxi Sheng, China		Historic	1933	COLLECTED		Pailohtung						1791275	PI 102946
250	PI 105222		Ilex paraguariensis A. St.-Hil.	Argentina		Historic	1933	COLLECTED								1492422	PI 105222
251	PI 102299		Ilex pedunculosa Miq.	China		Historic	1933	COLLECTED		Manchuria						1790478	PI 102299
252	PI 102300		Ilex pedunculosa Miq.	China		Historic	1933	COLLECTED		Manchuria						1790480	PI 102300
253	PI 102301		Ilex pedunculosa Miq.	China		Historic	1933	COLLECTED		Manchuria						1790481	PI 102301
254	PI 102075		Ilex purpurea Hassk.	China		Historic	1933	COLLECTED								1789903	PI 102075
255	PI 101516		Ilex paraguariensis A. St.-Hil.	Argentina		Historic	1932	COLLECTED								1789025	PI 101516
256	PI 100561	F. 29908	Ilex micrococca Maxim.	China		Historic	1932	COLLECTED								1788166	PI 100561
257	PI 100562	F. 30561	Ilex sp.	China		Historic	1932	COLLECTED								1788167	PI 100562
258	PI 99876	F. 30479	Ilex venulosa Hook. f.	China		Historic	1932	COLLECTED								1787192	PI 99876
259	PI 99167	Pa Hua Mu	Ilex micrococca Maxim.	Guizhou Sheng, China		Historic	1932	COLLECTED	10/20/1931	Forest slope near Machaoho, Fangchingshan, Kiangkouhsien		1054				1786461	PI 99167
260	PI 99180	No. 48	Ilex sp.	Guizhou Sheng, China		Historic	1932	COLLECTED	10/25/1931	Roadside near Hweihsiangping		1595				1786474	PI 99180
261	PI 99181	No. 93	Ilex sp.	Guizhou Sheng, China		Historic	1932	COLLECTED	11/14/1931	Tahoyen, Kiangkouhsien		753				1786475	PI 99181
262	PI 99236	No. 55	Ilex purpurea Hassk.	Guizhou Sheng, China		Historic	1932	COLLECTED	10/25/1931	Rocky slopes near Soochiapo, Fangchingshan, Kiangkouhsien		903				1786530	PI 99236
263	PI 97994	'Camelliifolia'	Ilex ×altaclerensis (Loudon) Dallim.	Netherlands	NA	Not Available	1932	COLLECTED						Cultivar		1784624	PI 97994
264	PI 97995	'Pyramidalis'	Ilex aquifolium L.	Netherlands		Historic	1932	COLLECTED								1784625	PI 97995
265	PI 94775		Ilex paraguariensis A. St.-Hil.	Argentina		Historic	1931	COLLECTED								1781476	PI 94775
266	PI 94152	No. 7968	Ilex integra Thunb.	Tôkyô, Japan		Historic	1931	COLLECTED								1781241	PI 94152
267	PI 94004	No. 29054	Ilex delavayi Franch.	China		Historic	1931	COLLECTED								1781084	PI 94004
268	PI 93898	No. 28997	Ilex corallina Franch.	China		Historic	1931	COLLECTED								1780970	PI 93898
269	PI 93899	No. 29020	Ilex yunnanensis Franch.	China		Historic	1931	COLLECTED								1780971	PI 93899
270	PI 92775		Ilex ×altaclerensis (Loudon) Dallim.	France		Historic	1931	COLLECTED								1779529	PI 92775
271	PI 92776		Ilex pernyi Franch.	France		Historic	1931	COLLECTED								1779530	PI 92776
272	PI 92493		Ilex integra Thunb.	England, United Kingdom		Historic	1931	COLLECTED								1779337	PI 92493
273	PI 91960		Ilex latifolia Thunb.	Hyôgo, Japan		Historic	1931	COLLECTED								1778466	PI 91960
274	PI 91518		Ilex latifolia Thunb.	Kanagawa, Japan		Historic	1931	COLLECTED								1493915	PI 91518
275	PI 91252		Ilex pedunculosa Miq.	Hyôgo, Japan		Historic	1931	COLLECTED								1776062	PI 91252
276	PI 91253		Ilex integra Thunb.	Hyôgo, Japan		Historic	1931	COLLECTED								1776063	PI 91253
277	PI 91254		Ilex purpurea Hassk.	Hyôgo, Japan		Historic	1931	COLLECTED								1776064	PI 91254
278	PI 91255		Ilex sugerokii Maxim.	Hyôgo, Japan		Historic	1931	COLLECTED								1776065	PI 91255
279	PI 90792		Ilex macropoda Miq.	Unknown		Historic	1930	COLLECTED		Chosen						1775437	PI 90792
280	PI 88236		Ilex argentina Lillo	Tucumán, Argentina		Historic	1930	COLLECTED								1752000	PI 88236
281	PI 86677		Ilex fragilis Hook. f.	West Bengal, India		Historic	1930	COLLECTED								1750473	PI 86677
282	PI 86678		Ilex wightiana Wall. ex Wight	West Bengal, India		Historic	1930	COLLECTED								1750474	PI 86678
283	PI 85870	No. 3904	Ilex rotunda Thunb.	Sizuoka, Japan		Historic	1930	COLLECTED	01/24/1930							1749473	PI 85870
284	PI 83795	No. 3155	Ilex latifolia Thunb.	Tôkyô, Japan		Historic	1930	COLLECTED	12/13/1929							1747326	PI 83795
285	PI 85735	No. 1450	Ilex serrata Thunb.	Akita, Japan		Historic	1929	COLLECTED	10/11/1929							1749362	PI 85735
286	PI 80095		Ilex purpurea Hassk.	Georgia, United States		Historic	1929	COLLECTED								1496271	PI 80095
287	PI 80363	No. 17368	Ilex sp.	Sichuan Sheng, China		Historic	1929	COLLECTED	01/1929	In spruce forests, southern slopes ot Mount Gibbah, Muli		3462				1744209	PI 80363
288	PI 80083		Ilex insignis Hook. f.	West Bengal, India		Historic	1929	COLLECTED								1743973	PI 80083
289	PI 80403		Ilex pernyi Franch.	Île-de-France, France		Historic	1929	COLLECTED								1744245	PI 80403
290	PI 78144	NA 82707	Ilex ciliospinosa Loes.	Grand-Est, France	NA	Not Available	1928	COLLECTED								1733747	PI 78144
291	PI 78145		Ilex bioritsensis Hayata	Grand-Est, France		Historic	1928	COLLECTED								1733748	PI 78145
292	PI 78146		Ilex wilsonii Loes.	Grand-Est, France		Historic	1928	COLLECTED								1733749	PI 78146
293	PI 77832	No. 892-3	Ilex serrata Thunb.	Massachusetts, United States		Historic	1928	COLLECTED								1733382	PI 77832
294	PI 77583	'National'	Ilex cornuta Lindl. & Paxton	District of Columbia, United States	NA	Not Available	1928	COLLECTED						Cultivar		1495929	PI 77583
295	PI 77165		Ilex geniculata Maxim.	Cienfuegos, Cuba		Historic	1928	COLLECTED								1732756	PI 77165
296	PI 76119	No. 666	Ilex pedunculosa Miq.	Kyôto, Japan		Historic	1928	COLLECTED	02/1928	Mountain side of Higashi-yama						1497417	PI 76119
297	PI 75713	Soyogo	Ilex sp.	Kyôto, Japan		Historic	1927	COLLECTED	11/02/1927							1730404	PI 75713
298	PI 75716	Umemodoki	Ilex serrata Thunb.	Kyôto, Japan		Historic	1927	COLLECTED	11/12/1927	Old garden ath Golden Pavilion, Kyoto						1730410	PI 75716
299	PI 73278		Ilex aquifolium L.	Île-de-France, France		Historic	1927	COLLECTED								1728449	PI 73278
300	PI 73438		Ilex yunnanensis Franch.	England, United Kingdom		Historic	1927	COLLECTED								1728510	PI 73438
301	PI 70980	Hung tung tsing	Ilex cornuta Lindl. & Paxton	Jiangxi Sheng, China		Historic	1927	COLLECTED	12/1926	En route from Kian to Taihop						1725641	PI 70980
302	PI 70981	Lak kok	Ilex sp.	Jiangxi Sheng, China		Historic	1927	COLLECTED	12/1926	En route from Kian to Wanan						1725642	PI 70981
303	PI 70982	Hung tung tsing	Ilex sp.	Jiangxi Sheng, China		Historic	1927	COLLECTED	12/1926	En route from Kian to Wanan						1725643	PI 70982
304	PI 70983	Laap shue	Ilex sp.	Jiangxi Sheng, China		Historic	1927	COLLECTED	12/16/1926	Near Kanchow						1725644	PI 70983
305	PI 70979	Lak kok	Ilex cornuta Lindl. & Paxton	Jiangxi Sheng, China		Historic	1927	COLLECTED	12/08/1926	Near Kian						1116163	PI 70979
306	PI 71859	No. 931	Ilex canariensis Poir.	Canarias, Spain		Historic	1927	COLLECTED	12/23/1926	Orotava Botanic Gardens, Teneriffe						1726617	PI 71859
307	PI 72467	No. 6925	Ilex sp.	Myanmar		Historic	1927	COLLECTED								1727329	PI 72467
308	PI 69865		Ilex paraguariensis A. St.-Hil.	Asunción, Paraguay		Historic	1926	COLLECTED								1499661	PI 69865
309	PI 67361		Ilex integra Thunb.	England, United Kingdom		Historic	1926	COLLECTED								1719685	PI 67361
310	PI 67362		Ilex latifolia Thunb.	England, United Kingdom		Historic	1926	COLLECTED								1719686	PI 67362
311	PI 67363		Ilex sikkimensis Kurz	England, United Kingdom		Historic	1926	COLLECTED								1719687	PI 67363
312	PI 67032		Ilex pernyi Franch.	Île-de-France, France		Historic	1926	COLLECTED								1719405	PI 67032
313	PI 66028		Ilex purpurea Hassk.	Jiangsu Sheng, China		Historic	1926	COLLECTED								1499087	PI 66028
314	PI 65256		Ilex insignis Hook. f.	West Bengal, India		Historic	1925	COLLECTED								1716527	PI 65256
315	PI 64255	No. 6249	Ilex sp.	Xizang Zizhiqu, China		Historic	1925	COLLECTED								1665572	PI 64255
316	PI 63793	Chue t'in shue, Tsau peng shue	Ilex rotunda Thunb.	Guangdong Sheng, China		Historic	1925	COLLECTED								1665180	PI 63793
317	PI 63794	Pak lan heung	Ilex sp.	Guangdong Sheng, China		Historic	1925	COLLECTED	02/16/1925							1665181	PI 63794
318	PI 63626	Pak lan heung	Ilex rotunda Thunb.	Guangdong Sheng, China		Historic	1925	COLLECTED	01/02/1925							1664999	PI 63626
319	PI 62810		Ilex sikkimensis Kurz	West Bengal, India		Historic	1925	COLLECTED								1664091	PI 62810
320	PI 62723		Ilex ciliospinosa Loes.	England, United Kingdom		Historic	1925	COLLECTED								1664030	PI 62723
321	PI 60646		Ilex insignis Hook. f.	West Bengal, India		Historic	1924	COLLECTED								1662251	PI 60646
322	PI 59391		Ilex latifolia Thunb.	England, United Kingdom		Historic	1924	COLLECTED								1660681	PI 59391
323	PI 57770		Ilex paraguariensis A. St.-Hil.	Buenos Aires, Argentina		Historic	1923	COLLECTED								1502813	PI 57770
324	PI 57085		Ilex sp.	Hubei Sheng, China		Historic	1923	COLLECTED								1657455	PI 57085
325	PI 57086		Ilex sp.	Hubei Sheng, China		Historic	1923	COLLECTED								1657456	PI 57086
326	PI 65860		Ilex cornuta Lindl. & Paxton	Hubei Sheng, China		Historic	1923	COLLECTED								1499070	PI 65860
327	PI 56314	No. 6781	Ilex sp.	China		Historic	1923	COLLECTED	10/1922			3600				1656219	PI 56314
328	PI 66866		Ilex intricata Hook. f.	West Bengal, India		Historic	1923	COLLECTED		Darjilling						1499253	PI 66866
329	PI 55621		Ilex paraguariensis A. St.-Hil.	Buenos Aires, Argentina		Historic	1922	COLLECTED								1502278	PI 55621
330	PI 55682		Ilex insignis Hook. f.	West Bengal, India		Historic	1922	COLLECTED								1654984	PI 55682
331	PI 55566		Ilex paraguariensis A. St.-Hil.	Asunción, Paraguay		Historic	1922	COLLECTED								1502240	PI 55566
332	PI 55493		Ilex paraguariensis A. St.-Hil.	Île-de-France, France		Historic	1922	COLLECTED								1502204	PI 55493
333	PI 55489		Ilex paraguariensis A. St.-Hil.	Buenos Aires, Argentina		Historic	1922	COLLECTED								1502201	PI 55489
334	PI 53452		Ilex sp.	Uttar Pradesh, India		Historic	1921	COLLECTED								1500573	PI 53452
335	PI 52644		Ilex fargesii Franch.	England, United Kingdom		Historic	1921	COLLECTED								1624556	PI 52644
336	PI 50420	No. 1201	Ilex sp.	Massachusetts, United States		Historic	1920	COLLECTED								1618187	PI 50420
337	PI 47697		Ilex fragilis Hook. f.	West Bengal, India		Historic	1919	COLLECTED								1613255	PI 47697
338	PI 47698		Ilex insignis Hook. f.	West Bengal, India		Historic	1919	COLLECTED								1613249	PI 47698
339	PI 47699		Ilex intricata Hook. f.	West Bengal, India		Historic	1919	COLLECTED								1613250	PI 47699
340	PI 47309		Ilex paraguariensis A. St.-Hil.	Asunción, Paraguay		Historic	1919	COLLECTED								1508606	PI 47309
341	PI 46891		Ilex paraguariensis A. St.-Hil.	Al Qāhirah, Egypt		Historic	1918	COLLECTED								1508320	PI 46891
342	PI 46564		Ilex paraguariensis A. St.-Hil.	Al Qāhirah, Egypt		Historic	1918	COLLECTED								1508217	PI 46564
343	PI 44676	'Alba de Llamas'	Ilex paraguariensis A. St.-Hil.	Salta, Argentina		Historic	1917	COLLECTED								1506782	PI 44676
344	PI 44335		Ilex latifolia Thunb.	Toscana, Italy		Historic	1917	COLLECTED								1506700	PI 44335
345	PI 43598		Ilex paraguariensis A. St.-Hil.	Concepción, Paraguay		Historic	1916	COLLECTED								1506377	PI 43598
346	PI 43456		Ilex paraguariensis A. St.-Hil.	Argentina		Historic	1916	COLLECTED								1608180	PI 43456
347	PI 39667		Ilex fragilis Hook. f.	West Bengal, India		Historic	1914	COLLECTED								1604339	PI 39667
348	PI 39668		Ilex intricata Hook. f.	West Bengal, India		Historic	1914	COLLECTED								1604340	PI 39668
349	PI 38858		Ilex paraguariensis A. St.-Hil.	Asunción, Paraguay		Historic	1914	COLLECTED								1518227	PI 38858
350	PI 34836		Ilex corallina Franch.	Centre-Val de Loire, France		Historic	1913	COLLECTED								1515010	PI 34836
351	PI 34655		Ilex paraguariensis A. St.-Hil.	Buenos Aires, Argentina		Historic	1912	COLLECTED								1514936	PI 34655
352	PI 34525		Ilex fargesii Franch.	Massachusetts, United States		Historic	1912	COLLECTED	05/1907							1599886	PI 34525
353	PI 34527		Ilex pernyi Franch.	Massachusetts, United States		Historic	1912	COLLECTED								1599888	PI 34527
354	PI 34546		Ilex macrocarpa Oliv.	Massachusetts, United States		Historic	1912	COLLECTED	1907							1599908	PI 34546
355	PI 34152		Ilex paraguariensis A. St.-Hil.	Asunción, Paraguay		Historic	1912	COLLECTED								1521166	PI 34152
356	PI 32945		Ilex cornuta Lindl. & Paxton	Liguria, Italy		Historic	1912	COLLECTED								1598546	PI 32945
357	PI 31255		Ilex cornuta Lindl. & Paxton	Liguria, Italy		Historic	1911	COLLECTED								1597068	PI 31255
358	PI 29134		Ilex paraguariensis A. St.-Hil.	Paraguay		Historic	1910	COLLECTED								1518190	PI 29134
359	PI 29097	Yerba	Ilex paraguariensis A. St.-Hil.	Unknown		Historic	1910	COLLECTED								1518164	PI 29097
360	PI 25529	'Yerba'	Ilex paraguariensis A. St.-Hil.	Paraguay		Historic	1909	COLLECTED								1587524	PI 25529
361	PI 24638	Chinese holly	Ilex cornuta Lindl. & Paxton	Shanghai Shi, China		Historic	1909	COLLECTED								1522826	PI 24638
362	PI 24313		Ilex paraguariensis A. St.-Hil.	Buenos Aires, Argentina		Historic	1908	COLLECTED								1522683	PI 24313
363	PI 22979	Tu hu tse	Ilex cornuta Lindl. & Paxton	Jiangsu Sheng, China		Historic	1908	COLLECTED	04/26/1908							1585031	PI 22979
364	PI 19105	Yerba mate	Ilex paraguariensis A. St.-Hil.	Buenos Aires, Argentina		Historic	1906	COLLECTED								1532348	PI 19105
365	PI 10449		Ilex crenata Thunb.	Kanagawa, Japan		Historic	1904	COLLECTED								1524776	PI 10449
366	PI 8953		Ilex paraguariensis A. St.-Hil.	Buenos Aires, Argentina		Historic	1902	COLLECTED								1548251	PI 8953
367	PI 8664		Ilex wightiana Wall. ex Wight	Tamil Nadu, India		Historic	1902	COLLECTED								1547869	PI 8664
368	PI 7554		Ilex integra Thunb.	Île-de-France, France		Historic	1901	COLLECTED								1545978	PI 7554
369	PI 4594		Ilex decidua Walter	Missouri, United States		Historic	1900	COLLECTED								1539981	PI 4594
370	PI 4017		Ilex verticillata (L.) A. Gray	North Carolina, United States		Historic	1899	COLLECTED								1539121	PI 4017
371	PI 3035		Ilex paraguariensis A. St.-Hil.	France		Historic	1899	COLLECTED								1537220	PI 3035
372	PI 2173		Ilex integra Thunb.	France		Historic	1899	COLLECTED								1535863	PI 2173
373	PI 1698	'Ilex balearica'	Ilex aquifolium L.	France		Historic	1898	COLLECTED								1534738	PI 1698
374	NA 89129	TRx250809-01PA	Ilex mucronata (L.) M. Powell et al.	Pennsylvania, United States	NA	Not Available	2025	COLLECTED	07/09/2025	Hickory Run Boulder Field	41.04973900, -75.64300700	555	Gowing within ca 15 m of boulder field edge, most individuals occured on sun-exposed margin.	Wild material		2191815	NA 89129
375	NA 89112	NA 89112	Ilex crenata Thunb.		NA	Not Available	2025							Wild material	One plant long considered and mapped as an individual of NA 44889, Ilex crenata var. paludosa (at least as early as 1993) is very different in habit from the lower, spreading plant of NA 44889 next to it. It is unclear if this could have been another accession, or if seed collected from var. paludosa could have outcrossed with another taxon to result in this growth habit. Assigned a new number out of an abundance of caution; likely to have been collected from the wild in Japan in any case, since all of the plants in the bed AC-J-L planting were.The plant might be male or non-flowering in 2025, as there are no fruit present, and I did not see any floral remants.	2191658	NA 89112
376	NA 88915	TRx250318-01FL	Ilex vomitoria Aiton	Florida, United States	NA	Not Available	2025	COLLECTED	03/18/2025	Yellow River Wildlife Management Area: along dirt access road DOF Y15, in the vicinity fo Burnt Grocery Creek.	30.62922000, -86.84158000		Understory of dry pine forest.	Wild material	small leaved plant	2172685	NA 88915
377	NA 88747	TXWL2025-038	Ilex opaca Aiton	Texas, United States	NA		2025	COLLECTED	01/23/2025	Milam, Texas: On flat road, private land.	31.43288000, -93.88208000		Upland shortleaf pine stand with sandy loam; closed canopy.	Wild material		2171021	NA 88747
378	NA 88746	TXWL2025-039	Ilex verticillata (L.) A. Gray	Louisiana, United States	NA		2025	COLLECTED	01/24/2025	Kistachie National Forest: Compartment 49, Indian Creek.	31.09110000, -93.53333000		Slough/baygall area with standing water below a longleaf pine stand.	Wild material		2171020	NA 88746
379	NA 88981	TXWL2025-031	Ilex opaca Aiton	Texas, United States	NA		2025	COLLECTED	01/07/2025	South of Jericho community.	31.67015000, -94.25641000		Western 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 material		2170965	NA 88981
380	NA 88982	TXWL2025-032	Ilex opaca Aiton	Texas, United States	NA		2025	COLLECTED	01/07/2025	South of Jericho community.	31.66973000, -94.25613000		Western 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 material		2170966	NA 88982
381	NA 88983	TXWL2025-033	Ilex opaca Aiton	Texas, United States	NA		2025	COLLECTED	01/12/2025	Adjacent to Toledo Bend reservoir in Huxley Bay community, eastern Shelby County.	31.77133000, -93.85094000		Low area with heavy duff near reservoir.	Wild material		2170967	NA 88983
382	NA 88984	TXWL2025-034	Ilex opaca Aiton	Texas, United States	NA		2025	COLLECTED	01/13/2025	Fairmount Township: Sabine National Forest C-139: Foxhunters Hill.	31.18153000, -93.72368000		Baygall below a longleaf pine stand. Same system as 035 [NA 88985].	Wild material		2170968	NA 88984
383	NA 88985	TXWL2025-035	Ilex opaca Aiton	Texas, United States	NA		2025	COLLECTED	01/13/2025	Fairmount Township: Sabine National Forest C-139: Foxhunters Hill.	31.18220000, -93.72291000		Baygall below a longleaf pine stand. Same system as 034 [NA 88984].	Wild material		2170969	NA 88985
384	NA 88986	TXWL2025-036	Ilex opaca Aiton	Texas, United States	NA	Not Available	2025	COLLECTED	01/13/2025	Fairmount Township: Sabine National Forest C-139: Foxhunters Hill.	31.18440000, -93.72253000		Baygall below a longleaf pine stand.	Wild material		2170970	NA 88986
385	NA 88987	TXWL2025-037	Ilex opaca Aiton	Texas, United States	NA		2025	COLLECTED	01/13/2025	Fairmount Township: Sabine National Forest C-139: Foxhunters Hill.	31.18365000, -93.72211000		Baygall below a longleaf pine stand.	Wild material		2170971	NA 88987
386	NA 89095	SNR2024	Ilex decidua Walter	Missouri, United States	NA		2024	COLLECTED	12/03/2024	Shaw Nature Reserve: near Shaw Nature Reserve's Trail House.	38.46697200, -90.81925000		Upland site.	Wild material		2169943	NA 89095
387	NA 88577	2024RJLFL-001	Ilex myrtifolia Walter	Florida, United States	NA		2024	COLLECTED	11/12/2024	Yellow River Marsh Preserve State Park: collected along trail from the parking lot. The property is accessed from a parking area located on Dickerson City Road.	30.48472300, -87.07110400	5	Mostly found in moist flatwoods in mixed evergreen and deciduous forest. Slope: N/A. Aspect: Various. The underlying geology of this area is characterized as undifferentiated Quaternary Sediments. Much of Florida's surface is covered by a varying thickness of undifferentiated sediments consisting of siliciclastics, organics and freshwater carbonates. Where these sediments exceed 6.1 meters thick, they were mapped as discrete units. In an effort to subdivide the undifferentiated sediments, those sediments occurring in flood plains were mapped as alluvial and flood plain deposits (Qal). Sediments showing surficial expression of beach ridges and dunes were mapped separately (Qbd) as were the sediments composing Trail Ridge (Qtr). Terrace sands were not mapped (refer to Healy [1975] for a discussion of the terraces in Florida). The subdivisions of the Undifferentiated Quaternary Sediments (Qu) are not lithostratigraphic units but are utilized in order to facilitate a better understanding of the State's geology. The siliciclastics are light gray, tan, brown to black, unconsolidated to poorly consolidated, clean to clayey, silty, unfossiliferous, variably organic-bearing sands to blue green to olive green, poorly to moderately consolidated, sandy, silty clays. Gravel is occasionally present in the panhandle. Organics occur as plant debris, roots, disseminated organic matrix and beds of peat. Freshwater carbonates, often referred to as marls in the literature, are scattered over much of the State. In southern Florida, freshwater carbonates are nearly ubiquitous in the Everglades. These sediments are buff colored to tan, unconsolidated to poorly consolidated, fossiliferous carbonate muds. Sand, silt and clay may be present in limited quantities. These carbonates often contain organics. The dominant fossils in the freshwater carbonates are mollusks. (Source: USGS Florida Geologic Map Data). The Goldhead Series consists of poorly drained and very poorly drained soils on broad areas of the flatwoods and in depressions. They formed in thick beds of stratified unconsolidated loamy and sandy marine sediments. Slopes range from 0 to 5 percent. The solum thickness ranges from 35 to greater than 60 inches. Soil reaction ranges from very strongly acid to mildly alkaline in the A and E horizons, and very strongly acid to moderately alkaline in the B and C horizons. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions).	Wild material		2169914	NA 88577
388	NA 88578	2024RJLFL-004	Ilex vomitoria Aiton	Florida, United States	NA		2024	COLLECTED	11/12/2024	Collected along Florida National Scenic Trail/Eglin Air Force Base unnamed road.	30.44526100, -86.86094700	4	Mixed evergreen and deciduous forests in part shade to full sun. Slope: 5 to 10 percent. Aspect: Various. The underlying geology of this area is characterized as Citronelle Formation of the Pliocene period. The Citronelle Formation is widespread in the Gulf Coastal Plain. The type section for the Citronelle Formation, named by Matson (1916), is near Citronelle, Alabama. The Citronelle Formation grades laterally, through a broad facies transition, into the Miccosukee Formation of the eastern Florida panhandle. Coe (1979) investigated the Citronelle Formation in portions of the western Florida panhandle. The Citronelle Formation is a siliciclastic, deltaic deposit that is lithologically similar to, and time equivalent with, the Cypresshead Formation and, at least in part, the Long Key Formation (Cunningham et al., 1998) of the peninsula. In the western panhandle, some of the sediments mapped as Citronelle Formation may be reworked Citronelle. The lithologies are the same and there are few fossils present to document a possible younger age. The Citronelle Formation consists of gray to orange, often mottled, unconsolidated to poorly consolidated, very fine to very coarse, poorly sorted, clean to clayey sands. It contains significant amounts of clay, silt and gravel which may occur as beds and lenses and may vary considerably over short distances. Limonite nodules and limonite-cemented beds are common. Marine fossils are rare but fossil pollen, plant remains and occasional vertebrates are found. Much of the Citronelle Formation is highly permeable. It forms the Sand and Gravel Aquifer of the surficial aquifer system contain organics. The dominant fossils in the freshwater carbonates are mollusks. (Source: USGS Florida Geologic Map Data). The soils of this are characterized as Lakeland Series Sand, 5 to 12 percent slopes. 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 in the Southern Coastal Plain MLRA (133A), the Carolina and Georgia Sandhills (MLRA 137), the Eastern Gulf Coast Flatwoods (MLRA 152A) and the Atlantic Coast Flatwoods (MLRA 153A). Slopes are dominantly from 0 to 12 percent but can range to 85 percent in dissected areas. Thickness of the sand exceeds 200 cm. Silt plus clay in the 25 to 100 cm control section ranges from 5 to 10 percent. Reaction ranges from very strongly acid to moderately acid throughout. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions).	Wild material		2169915	NA 88578
389	NA 88579	2024RJLFL-007	Ilex myrtifolia Walter	Florida, United States	NA		2024	COLLECTED	11/13/2024	Wetlands accessed from Miller Bluff Road.	30.62251200, -86.86030700	8	Open, wet areas and woodland edge slightly above permanently wet habitat in part shade to full sun. Slope: 0 percent. Aspect: N/A.	Wild material		2169916	NA 88579
390	NA 88580	2024RJLFL-009	Ilex myrtifolia Walter	Florida, United States	NA		2024	COLLECTED	11/13/2024	Woodlands on the north side of Fisher Old Mill Road about 0.10 kilometers west of intersection with DOF Y12.	30.62693800, -86.83962200	6	Mixed 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 material		2169917	NA 88580
391	NA 88581	2024RJLFL-012	Ilex ambigua Torr.	Florida, United States	NA		2024	COLLECTED	11/13/2024	Woodland edge along the south side of Bud Bass Road (DOF B48), 0.30 kilometers east of the junction with Norman Riley Road.	30.75763200, -86.80184300	32	Woodland edge. Slope: 3 percent. Aspect: North. The underlying geology of this area is characterized as Citronelle Formation of the Pliocene period. The Citronelle Formation is widespread in the Gulf Coastal Plain. The type section for the Citronelle Formation, named by Matson (1916), is near Citronelle, Alabama. The Citronelle Formation grades laterally, through a broad facies transition, into the Miccosukee Formation of the eastern Florida panhandle. Coe (1979) investigated the Citronelle Formation in portions of the western Florida panhandle. The Citronelle Formation is a siliciclastic, deltaic deposit that is lithologically similar to, and time equivalent with, the Cypresshead Formation and, at least in part, the Long Key Formation (Cunningham et al., 1998) of the peninsula. In the western panhandle, some of the sediments mapped as Citronelle Formation may be reworked Citronelle. The lithologies are the same and there are few fossils present to document a possible younger age. The Citronelle Formation consists of gray to orange, often mottled, unconsolidated to poorly consolidated, very fine to very coarse, poorly sorted, clean to clayey sands. It contains significant amounts of clay, silt and gravel which may occur as beds and lenses and may vary considerably over short distances. Limonite nodules and limonite-cemented beds are common. Marine fossils are rare but fossil pollen, plant remains and occasional vertebrates are found. Much of the Citronelle Formation is highly permeable. It forms the Sand and Gravel Aquifer of the surficial aquifer system contain organics. The dominant fossils in the freshwater carbonates are mollusks. (Source: USGS Florida Geologic Map Data). The soils of this are characterized as Lakeland Series Sand, 0 to 5 percent slopes. 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 in the Southern Coastal Plain MLRA (133A), the Carolina and Georgia Sandhills (MLRA 137), the Eastern Gulf Coast Flatwoods (MLRA 152A) and the Atlantic Coast Flatwoods (MLRA 153A). Slopes are dominantly from 0 to 12 percent but can range to 85 percent in dissected areas. Thickness of the sand exceeds 200 cm. Silt plus clay in the 25 to 100 cm control section ranges from 5 to 10 percent. Reaction ranges from very strongly acid to moderately acid throughout. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions).	Wild material		2169918	NA 88581
392	NA 88583	2024RJLFL-014	Ilex amelanchier M. A. Curtis ex Chapm.	Florida, United States	NA		2024	COLLECTED	11/13/2024	Yellow River Water Management Area: found in an area where an unnamed unpaved road dead ends near the Yellow River. This unpaved road is accessed from Old River Road to the east near the junction with Shockley Springs Road. Individual plants for this collection were accessed by foot along the edge of the river and associated wetland depressions to the east of the road. The sampling for this portion of the population extends from the GPS coordinates listed above to the northeast where sampling ended at coordinates 30.871238 deg. N, 86.590170 deg. W.	30.86989400, -86.59218500	23	Plants growing in seasonally inundated swamp habitats associated with the Yellow River and small tributaries. Plants are emergent during portions of the year, primarily during the growing season. During this time of collection, water had receded from the wetlands and the area was relatively dry. Slope: N/A. Aspect: N./A. The underlying geology of this area is the Alum Bluff Group of Miocene origin. It includes the Chipola Formation, Oak Grove Sand, Shoal River Formation, Choctawhatchee Formation and the Jackson Bluff Formation. The formations included in this group are generally defined based on their molluscan faunas and stratigraphic position. Puri (1953) described sediment facies as they relate to the formations of the Alum Bluff Group. These sediments are lithologically distinct as a group, not as individual units. The Alum Bluff Group crops out or is beneath a thin overburden in the western panhandle from river valleys in Okaloosa County eastward to western Jackson County. The Alum Bluff Group consists of clays, sands and shell beds which may vary from fossiliferous, sandy clays to unfossiliferous sands and clays and occasional carbonate beds. Mica is a common constituent and glauconite and phosphate occur sporadically. Induration varies from essentially nonindurated in sands to well indurated in carbonate lenses. Colors range from cream to olive gray with mottled reddish brown in weathered sections. Sand grain size varies from very fine to very coarse with sporadic occurrences of gravel. These sediments generally have low permeabilities and are part of the intermediate confining unit/aquifer system. (Source: USGS Florida Geologic Map Data). The surface soil profile of this area is primarily Kinston, Johnston, and Bibb soils, frequently flooded. Kinston Series soils are poorly drained, alluvial, fine-loamy, siliceous, and acid soils of flood plains. They are peaty to loamy friable, slightly sticky, and slightly plastic in the upper 0 to 7.5 cm of the strata with less sand and more silt-loam in progressively deeper strata. The Johnston Series consists of very deep, very poorly drained coarse-loamy, siliceous, active, acid, thermic Cumulic Humaquepts. The upper 0-75 cm is black, mucky loam that is friable and very strongly acid. The lower strata to 1.75 m are dark gray, loamy fine sand, single grained, loose and very strongly acid. (Source: NRCS Web Soil Survey).	Wild material		2169920	NA 88583
393	NA 88590	2024RM-003	Ilex verticillata (L.) A. Gray	Florida, United States	NA		2024	COLLECTED	11/21/2024	Along the west/north side of the Yellow River about 0.33 kilometers (as the crow flies) upstream from the channel that leads the Fisher Old Mill Road Boat Ramp. This site was accessed by boat.	30.62868600, -86.80748000	4	Plants are found growing primarily in permanently saturated to submersed conditions along the edge of the Yellow River in part shade. The riverine habitat is comprised of a wide array of deciduous and evergreen trees, shrubs, and perennial plant species. Most of the plants along the river are adapted to acidic conditions and, while the aquatic habitat is generally fresh water, there is occasionally tidal or hurricane-caused saltwater intrusions. Slope: 0 percent. Aspect: East-southeast. The underlying geology of this area is characterized as Alluvium from undifferentiated Quaternary Sediments. Much of Florida's surface is covered by a varying thickness of undifferentiated sediments consisting of siliciclastics, organics and freshwater carbonates. Where these sediments exceed 20 feet (6.1 meters) thick, they were mapped as discrete units. To subdivide the undifferentiated sediments, those sediments occurring in flood plains were mapped as alluvial and flood plain deposits (Qal). Sediments showing surficial expression of beach ridges and dunes were mapped separately (Qbd) as were the sediments composing Trail Ridge (Qtr). Terrace sands were not mapped (refer to Healy [1975] for a discussion of the terraces in Florida). The subdivisions of the Undifferentiated Quaternary Sediments (Qu) are not lithostratigraphic units but are utilized to facilitate a better understanding of the State's geology. The siliciclastics are light gray, tan, brown to black, unconsolidated to poorly consolidated, clean to clayey, silty, unfossiliferous, variably organic-bearing sands to blue green to olive green, poorly to moderately consolidated, sandy, silty clays. Gravel is occasionally present in the panhandle. Organics occur as plant debris, roots, disseminated organic matrix and beds of peat. Freshwater carbonates, often referred to as marls in the literature, are scattered over much of the State. In southern Florida, freshwater carbonates are nearly ubiquitous in the Everglades. These sediments are buff colored to tan, unconsolidated to poorly consolidated, fossiliferous carbonate muds. Sand, silt and clay may be present in limited quantities. These carbonates often contain organics. The dominant fossils in the freshwater carbonates are mollusks. (Source: USGS Florida Geologic Map Data). The soils of this are characterized as Bibb-Kinston Series association. The Bibb Series consists of very deep, poorly drained, moderately permeable soils on flood plains of streams in the Southern Coastal Plain (133A) Major Land Resource Area. They formed in stratified loamy and sandy alluvium that are commonly and frequently flooded and water runs off the surface very slowly. Slopes range from 0 to 2 percent. Reaction ranges from extremely acid to strongly acid throughout. Content of mica flakes ranges from none to common. Content of rounded gravel typically ranges from 0 to 10 percent throughout, but may range to 50 percent in thin strata below a depth of 1 meter. Buried soil horizons, present in many pedons have the same range in color and texture as the surface horizon which has iron and organic matter concentrations in shades of brown and yellow ranging from none to common. Texture is sand, loamy sand, loamy fine sand, fine sandy loam, sandy loam, loam or silt loam. The Kinston Series consists of very deep, poorly drained, moderately permeable soils found on flood plains. They were formed in alluvial depositions. Slopes range from 0 to 2 percent. Soil reaction ranges from strongly acid to very strongly acid. Typical texture across the pedons is loamy, gravelly loam, sandy loam, and clay loam with dark concretions often present. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions).	Wild material		2169927	NA 88590
394	NA 88591	2024RM-004	Ilex opaca Aiton	Florida, United States	NA		2024	COLLECTED	11/21/2024	Along the west/north side of the Yellow River about 5.5 kilometers upstream from the State Highway 87 boat ramp. This site was accessed by boat.	30.59986000, -86.87936000	2	Plants are found growing primarily in permanently saturated to submersed conditions along the edge of the Yellow River in part shade. The riverine habitat is comprised of a wide array of deciduous and evergreen trees, shrubs, and perennial plant species. Most of the plants along the river are adapted to acidic conditions and, while the aquatic habitat is generally fresh water, there is occasionally tidal or hurricane-caused saltwater intrusions. Slope: 0 percent. Aspect: East-southeast. The underlying geology of this area is characterized as Alluvium from undifferentiated Quaternary Sediments. Much of Florida's surface is covered by a varying thickness of undifferentiated sediments consisting of siliciclastics, organics and freshwater carbonates. Where these sediments exceed 20 feet (6.1 meters) thick, they were mapped as discrete units. To subdivide the undifferentiated sediments, those sediments occurring in flood plains were mapped as alluvial and flood plain deposits (Qal). Sediments showing surficial expression of beach ridges and dunes were mapped separately (Qbd) as were the sediments composing Trail Ridge (Qtr). Terrace sands were not mapped (refer to Healy [1975] for a discussion of the terraces in Florida). The subdivisions of the Undifferentiated Quaternary Sediments (Qu) are not lithostratigraphic units but are utilized to facilitate a better understanding of the State's geology. The siliciclastics are light gray, tan, brown to black, unconsolidated to poorly consolidated, clean to clayey, silty, unfossiliferous, variably organic-bearing sands to blue green to olive green, poorly to moderately consolidated, sandy, silty clays. Gravel is occasionally present in the panhandle. Organics occur as plant debris, roots, disseminated organic matrix and beds of peat. Freshwater carbonates, often referred to as marls in the literature, are scattered over much of the State. In southern Florida, freshwater carbonates are nearly ubiquitous in the Everglades. These sediments are buff colored to tan, unconsolidated to poorly consolidated, fossiliferous carbonate muds. Sand, silt and clay may be present in limited quantities. These carbonates often contain organics. The dominant fossils in the freshwater carbonates are mollusks. (Source: USGS Florida Geologic Map Data). The soils of this are characterized as Bibb-Kinston Series association. The Bibb Series consists of very deep, poorly drained, moderately permeable soils on flood plains of streams in the Southern Coastal Plain (133A) Major Land Resource Area. They formed in stratified loamy and sandy alluvium that are commonly and frequently flooded and water runs off the surface very slowly. Slopes range from 0 to 2 percent. Reaction ranges from extremely acid to strongly acid throughout. Content of mica flakes ranges from none to common. Content of rounded gravel typically ranges from 0 to 10 percent throughout, but may range to 50 percent in thin strata below a depth of 1 meter. Buried soil horizons, present in many pedons have the same range in color and texture as the surface horizon which has iron and organic matter concentrations in shades of brown and yellow ranging from none to common. Texture is sand, loamy sand, loamy fine sand, fine sandy loam, sandy loam, loam or silt loam. The Kinston Series consists of very deep, poorly drained, moderately permeable soils found on flood plains. They were formed in alluvial depositions. Slopes range from 0 to 2 percent. Soil reaction ranges from strongly acid to very strongly acid. Typical texture across the pedons is loamy, gravelly loam, sandy loam, and clay loam with dark concretions often present. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions).	Wild material		2169928	NA 88591
395	NA 88592	2024RM-005	Ilex sp.	Florida, United States	NA		2024	COLLECTED	11/21/2024	Along the west/north side of the Yellow River about 1.1 kilometers upstream from the State Highway 87 boat ramp. This site was accessed by boat.	30.57956000, -86.91916400	1	Plants are found growing primarily in permanently saturated to submersed conditions along the edge of the Yellow River in part shade. The riverine habitat is comprised of a wide array of deciduous and evergreen trees, shrubs, and perennial plant species. Most of the plants along the river are adapted to acidic conditions and, while the aquatic habitat is generally fresh water, there is occasionally tidal or hurricane-caused saltwater intrusions. Slope: 0 percent. Aspect: North. The underlying geology of this area is characterized as Alluvium from undifferentiated Quaternary Sediments. Much of Florida's surface is covered by a varying thickness of undifferentiated sediments consisting of siliciclastics, organics and freshwater carbonates. Where these sediments exceed 20 feet (6.1 meters) thick, they were mapped as discrete units. To subdivide the undifferentiated sediments, those sediments occurring in flood plains were mapped as alluvial and flood plain deposits (Qal). Sediments showing surficial expression of beach ridges and dunes were mapped separately (Qbd) as were the sediments composing Trail Ridge (Qtr). Terrace sands were not mapped (refer to Healy [1975] for a discussion of the terraces in Florida). The subdivisions of the Undifferentiated Quaternary Sediments (Qu) are not lithostratigraphic units but are utilized to facilitate a better understanding of the State's geology. The siliciclastics are light gray, tan, brown to black, unconsolidated to poorly consolidated, clean to clayey, silty, unfossiliferous, variably organic-bearing sands to blue green to olive green, poorly to moderately consolidated, sandy, silty clays. Gravel is occasionally present in the panhandle. Organics occur as plant debris, roots, disseminated organic matrix and beds of peat. Freshwater carbonates, often referred to as marls in the literature, are scattered over much of the State. In southern Florida, freshwater carbonates are nearly ubiquitous in the Everglades. These sediments are buff colored to tan, unconsolidated to poorly consolidated, fossiliferous carbonate muds. Sand, silt and clay may be present in limited quantities. These carbonates often contain organics. The dominant fossils in the freshwater carbonates are mollusks. (Source: USGS Florida Geologic Map Data). The soils of this are characterized as Bibb-Kinston Series association. The Bibb Series consists of very deep, poorly drained, moderately permeable soils on flood plains of streams in the Southern Coastal Plain (133A) Major Land Resource Area. They formed in stratified loamy and sandy alluvium that are commonly and frequently flooded and water runs off the surface very slowly. Slopes range from 0 to 2 percent. Reaction ranges from extremely acid to strongly acid throughout. Content of mica flakes ranges from none to common. Content of rounded gravel typically ranges from 0 to 10 percent throughout, but may range to 50 percent in thin strata below a depth of 1 meter. Buried soil horizons, present in many pedons have the same range in color and texture as the surface horizon which has iron and organic matter concentrations in shades of brown and yellow ranging from none to common. Texture is sand, loamy sand, loamy fine sand, fine sandy loam, sandy loam, loam or silt loam. The Kinston Series consists of very deep, poorly drained, moderately permeable soils found on flood plains. They were formed in alluvial depositions. Slopes range from 0 to 2 percent. Soil reaction ranges from strongly acid to very strongly acid. Typical texture across the pedons is loamy, gravelly loam, sandy loam, and clay loam with dark concretions often present. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions).	Wild material		2169929	NA 88592
396	NA 88593	2024RJLNJ-001	Ilex glabra (L.) A. Gray	New Jersey, United States	NA		2024	COLLECTED	11/24/2024	Mullica Township: Both sides of Duerer Street, approximately 0.37 kilometers southeast of 4th Avenue.	39.55885000, -74.66442500	21	Shade to almost full sun on compacted seasonally moist to temporarily wet areas of a mixed evergreen and deciduous woodland dominated by Pinus rigida. Vegetation of this area is very much defined by small changes in elevation that go from wet to very dry. Ilex glabra remains abundant throughout, though. Slope: N/A. Aspect: N/A. The underlying geology of this area is the Cohansey Formation of middle Miocene origin and comprised of sand, white to yellow with local gravel and clay. It is sometimes locally stained red or orange brown by iron oxides and (or) cemented into large blocks of ironstone. Unweathered clay is typically dark gray, but commonly weathers white where it is interbedded with thin beds of ironstone. Sand is typically medium grained and moderately sorted although it ranges from fine to very coarse grained and from poorly to well sorted. Sand consists of quartz and siliceous rock fragments. Some beds are locally micaceous. Maximum thickness in the map area is about 60 meters; however, thickness is difficult to determine because of the irregular basal contact and extensive post-depositional erosion. (Source: USGS New Jersey Geologic Map Data). The primary soil type in the area of this collection is classified as Mullica Series sandy loam, 0 to 2 percent slopes. These soils are typically coarse-loamy, siliceous, semiactive, and mesic typic humaquepts that are strongly to extremely acidic throughout the profile. The typical solum thickness ranges from 50-150+ cm. These soils are generally considered to be poorly drained. (Source: NRCS Web Soil Survey).	Wild material		2169930	NA 88593
397	NA 88479	TXWL2024-029	Ilex longipes Chapm. ex Trel.	Texas, United States	NA		2024	COLLECTED	11/20/2024	Little Cow Creek.	31.06221000, -93.79603000		Upland position above perennial creek.	Wild material		2169906	NA 88479
398	NA 88480	TXWL2024-030	Ilex coriacea (Pursh) Chapm.	Texas, United States	NA	Not Available	2024	COLLECTED	11/20/2024	Little Cow Creek.	31.06280000, -93.79610000		Upland position above perennial creek.	Wild material		2169907	NA 88480
399	NA 87836	TRX241117-01VA	Ilex vomitoria Aiton	Virginia, United States	NA		2024	COLLECTED	11/17/2024	Eastern Shore of Virginia National Wildlife Refuge.	37.13092000, -75.96253000	6		Wild material		2169889	NA 87836
400	NA 87838	TRX241117-03NC	Ilex coriacea (Pursh) Chapm.	North Carolina, United States	NA		2024	COLLECTED	11/17/2024	Boiling Spring Lakes Community Center nature trail.	34.02040000, -78.06469000	16		Wild material		2169891	NA 87838
401	NA 87839	TRX241117-04NC	Ilex cassine L.	North Carolina, United States	NA		2024	COLLECTED	11/17/2024	Boiling Spring Lakes Community Center nature trail.	34.02040000, -78.06469000	16		Wild material		2169892	NA 87839
402	NA 87840	TRX241117-05NC	Ilex cassine L.	North Carolina, United States	NA		2024	COLLECTED	11/17/2024	Boiling Spring Lakes Community Center nature trail.	34.02040000, -78.06469000	16		Wild material		2169893	NA 87840
403	NA 87842	TRX241117-08SC	Ilex opaca Aiton	South Carolina, United States	NA		2024	COLLECTED	11/17/2024	Francis Marion National Forest.	33.15167000, -79.60253000	31		Wild material		2169895	NA 87842
404	NA 87844	TRX241118-02GA	Ilex cassine L.	Georgia, United States	NA		2024	COLLECTED	11/18/2024	St. Simons Island: Frederica Park.	31.23766000, -81.35638000	6		Wild material		2169897	NA 87844
405	NA 87845	TRX241119-01GA	Ilex coriacea (Pursh) Chapm.	Georgia, United States	NA		2024	COLLECTED	11/19/2024	St. Simons Island: Guale Preserve.	31.21861000, -81.36872000	6		Wild material		2169898	NA 87845
406	NA 87848	TRX241119-04GA	Ilex vomitoria Aiton	Georgia, United States	NA		2024	COLLECTED	11/19/2024	Jekyll Island.	31.11344000, -81.40673000	4	The first vegetation occuring at the top of the beach, where high tide is actively eroding.	Wild material		2169901	NA 87848
407	NA 88476	TXWL2024-026	Ilex verticillata (L.) A. Gray	Texas, United States	NA	Not Available	2024	COLLECTED	11/12/2024	Sabine River at I-10 at the Texas/Louisiana state line; north side of bridge.	30.12830000, -93.70561000		Bottomland.	Wild material		2169861	NA 88476
408	NA 88477	TXWL2024-027	Ilex ambigua Torr.	Texas, United States	NA		2024	COLLECTED	11/12/2024	Sabine River at I-10 at the Texas/Louisiana state line; south side of bridge.	30.12654000, -93.70258000		Bottomland.	Wild material		2169862	NA 88477
409	NA 88478	TXWL2024-028	Ilex vomitoria Aiton	Texas, United States	NA		2024	COLLECTED	11/12/2024	Big Thicket National Preserve: Turkey Creek Unit.: Pitcher Plant Trail.	30.58602000, -94.34154000		Bog/wetland.	Wild material		2169863	NA 88478
410	NA 87820	'Blue Wave'	Ilex hybr.	Michigan, United States	NA	Not Available	2024	DONATED	PRE 2004					Cultivar	Holly Society of America test holly for 2024. Originated from the holly breeding program of the late Robert L. Tomayer (Wavecrest Nursery, Fennville, Michigan) and registered by his daughter, Carol T. Hop. The parent plant of this material was obtained by J. Resch directly from Mr. Tomayer at Wavecrest Nursery over 20 years ago.	2169671	NA 87820
411	NA 88474	JH2024NH	Ilex verticillata (L.) A. Gray	New Hampshire, United States	NA	Not Available	2024	COLLECTED	10/18/2024	North Conway, NH: near Saco River, river trail near Eastern Slope Camping Area [inferred; originally written, "River Trail Nr. East Slope."]				Wild material		2169440	NA 88474
412	NA 88475	TXWL2024-025	Ilex coriacea (Pursh) Chapm.	Texas, United States	NA		2024	COLLECTED	10/16/2024	Sabine National Forest C-142.			Baygall below longleaf [pine] forest.	Wild material		2169441	NA 88475
413	NA 89080	2024RJLPA-006	Ilex montana Torr. & A. Gray	Pennsylvania, United States	NA		2024	COLLECTED	09/20/2024	Berks and Schuylkill Counties: Hawk Mountain Sanctuary.	40.64162200, -75.99122600	418	Plants are growing from shade to full sun on a dry-mesic to very dry, well-drained upland/montane habitat characterized by an upland mixed deciduous and evergreen forest that is very rocky. All the plants found in this habitat go through periods of drought during the growing season due to the limited litter/soil layer in which moisture can be held. Elevation: 405 to 430 meters. Slope: 5 to 25 percent. Aspect: various. Geology: The underlying geology of this area is of Silurian origin and comprised of Shawangunk Formation. This formation is primarily light- to dark-gray, fine- to very coarse-grained sandstone and conglomerate containing thin shale interbeds. (Source: USGS Pennsylvania Geologic Map Data). Soils: The surface soil profile of this area is characterized as the Hazleton Series which consists of deep and very deep, well drained soils formed in residuum of acid gray, brown or red sandstone on uplands. The matrix includes a considerable accumulation of thin, flat, coarse fragments of sandstone, limestone, or schist with diameters up to 15 cm. Slope ranges from 0-80%. Permeability is moderately rapid to rapid. (Source: USDA-NRCS Official Soil Series Descriptions). EPA Ecoregion (Level III): Ridge and Valley (67). EPA Ecoregion (Level IV): Northern Sandstone Ridges (67c).	Wild material		2169044	NA 89080
414	NA 89086	2024RJLPA-015	Ilex verticillata (L.) A. Gray	Pennsylvania, United States	NA		2024	COLLECTED	09/22/2024	Outcrops along the Susquehanna River, accessed from the Historic Lock 12 parking lot off of Pennsylvania Road 372.	39.81656600, -76.33136600	38	Plants are growing from part-sun to full sun in crevices of the outcrops and where organic debris has accumulated in between boulders along the Susquehanna River. The sites range from nearly xeric to dry mesic, at least on the surface. Plants are generally growing 4-10 m above the normal flow of the river; however, the Holtwood Dam is less than 1 kilometer upstream and debris found trapped in the boulders indicates that there is periodic flooding, at least, in the lower zone of 4+ meters or so above normal river flow. This habitat has a diverse assemblage of deciduous trees and shrubs as well as abundant herbaceous taxa. Slope: 0 to 10 percent. Aspect: Northeast (generally). Geology: The underlying geology of this area is probably of lower Paleozoic age and characterized as the Octoraro Formation. It includes albite-chlorite schist, phyllite, some hornblende gneiss, and granitized members. Soils: The area where this species occurs is right on the edge of two soil zones that transition from the river’s edge to mesic conditions upslope. The first is generally referred to as Rock Outcrop. This terrestrial matrix in which plants grow is largely exposed underlying rock geology with accumulated outwash, rock decomposition, and organic debris buildup. The second is Mt. Airy (80%) and Manor (20%) Series soils, 25 to 60 percent slopes, extremely stony (MRF). (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). EPA Ecoregion (Level III): Northern Piedmont (64). EPA Ecoregion (Level IV): Piedmont Uplands (64c).	Wild material		2169050	NA 89086
415	NA 89090	2024RM-TK-003	Ilex longipes Chapm. ex Trel.	Alabama, United States	NA		2024	COLLECTED	09/19/2024	Woodland slopes around and below the hilltop parking area leading down to the Silver Creek Lake Campground off of Silver Creek Lake Road.	31.66612294, -87.57569860	39	Plants 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 material		2169054	NA 89090
416	NA 89092	2024RM-TK-005	Ilex amelanchier M. A. Curtis ex Chapm.	Florida, United States	NA		2024	COLLECTED	09/29/2024	Yellow River Water Management Area: found in an area where an unnamed, unpaved road dead ends near the Yellow River. This unpaved road is accessed from Old River Road to the east near the junction with Shockley Springs Road. Plants are accessed by foot along the edge of the river and associated wetland depressions to the west of the road.	30.86946200, -86.59349000	23	Plants growing in seasonally inundated swamp habitats associated with the Yellow River. Plants are emergent during portions of the year, primarily during the growing season. During this time of collection, water had receded from the wetlands but the area was still quite wet with many tiny stream rivulets still draining. Slope: 0 percent. Aspect: N/A. Geology: The underlying geology of this area is the Alum Bluff Group of Miocene origin. It includes the Chipola Formation, Oak Grove Sand, Shoal River Formation, Choctawhatchee Formation and the Jackson Bluff Formation. The formations included in this group are generally defined based on their molluscan faunas and stratigraphic position. Puri (1953) described sediment facies as they relate to the formations of the Alum Bluff Group. These sediments are lithologically distinct as a group, not as individual units. The Alum Bluff Group crops out or is beneath a thin overburden in the western panhandle from river valleys in Okaloosa County eastward to western Jackson County. The Alum Bluff Group consists of clays, sands and shell beds which may vary from fossiliferous, sandy clays to unfossiliferous sands and clays and occasional carbonate beds. Mica is a common constituent and glauconite and phosphate occur sporadically. Induration varies from essentially nonindurated in sands to well indurated in carbonate lenses. Colors range from cream to olive gray with mottled reddish brown in weathered sections. Sand grain size varies from very fine to very coarse with sporadic occurrences of gravel. These sediments generally have low permeabilities and are part of the intermediate confining unit/aquifer system. (Source: USGS Florida Geologic Map Data). Soils: The surface soil profile of this area is primarily Kinston, Johnston, and Bibb soils, frequently flooded. Kinston Series soils are poorly drained, alluvial, fine-loamy, siliceous, and acid soils of flood plains. They are peaty to loamy friable, slightly sticky and slightly plastic in the upper 0 to 7.5 cm of the strata with less sand and more silt-loam in progressively deeper strata. The Johnston Series consists of very deep, very poorly drained coarse-loamy, siliceous, active, acid, thermic Cumulic Humaquepts. The upper 0-75 cm is black, mucky loam that is friable and very strongly acid. The lower strata to 1.75 m are dark gray, loamy fine sand, single grained, loose and very strongly a).id. The Bibb Series soils consist of very deep, poorly drained, moderately permeable soils on flood plains of streams in the Southern Coastal Plain (133A) Major Land Resource Area. They formed in stratified loamy and sandy alluvium that are commonly and frequently flooded and water runs off the surface very slowly. Slopes range from 0 to 2 percent. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). EPA Ecoregion (Level III): Southeastern Plains (65). EPA Ecoregion (Level IV): Southeastern Floodplains and Low Terraces (65p).	Wild material		2169056	NA 89092
417	NA 89093	2024RM-TK-006	Ilex ambigua Torr.	Florida, United States	NA		2024	COLLECTED	09/29/2024	Blackwater River Wildlife Management Area: growing on the south side of Bud Bass Road, approximately 0.3 kilometers east of Training Center R./Norma Riley Rd.	30.75759720, -86.80187220	29	This plant is growing in part-shade under mesic conditions along the edge of a longleaf pine plantation. Slope: 0 percent. Aspect: North. Geology: The underlying geology of this area is probably of lower Pliocene age and characterized as the Citronelle Formation. The Citronelle Formation is widespread in the Gulf Coastal Plain. The type section for the Citronelle Formation, named by Matson (1916), is near Citronelle, Alabama. The Citronelle Formation grades laterally, through a broad facies transition, into the Miccosukee Formation of the eastern Florida panhandle. Coe (1979) investigated the Citronelle Formation in portions of the western Florida panhandle. The Citronelle Formation is a siliciclastic, deltaic deposit that is lithologically similar to, and time equivalent with, the Cypresshead Formation and, at least in part, the Long Key Formation (Cunningham et al., 1998) of the peninsula. In the western panhandle, some of the sediments mapped as Citronelle Formation may be reworked Citronelle. The lithologies are the same and there are few fossils present to document a possible younger age. The Citronelle Formation consists of gray to orange, often mottled, unconsolidated to poorly consolidated, very fine to very coarse, poorly sorted, clean to clayey sands. It contains significant amounts of clay, silt and gravel which may occur as beds and lenses and may vary considerably over short distances. Limonite nodules and limonite-cemented beds are common. Marine fossils are rare but fossil pollen, plant remains and occasional vertebrates are found. Much of the Citronelle Formation is highly permeable. It forms the Sand and Gravel Aquifer of the surficial aquifer system. (Source: USGS Florida Geologic Map Data). Soils: The soil of this area is characterized as Lakeland Series Sand, 0 to 5 percent slopes (21). 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 in the Southern Coastal Plain MLRA (133A), the Carolina and Georgia Sandhills (MLRA 137), the Eastern Gulf Coast Flatwoods (MLRA 152A) and the Atlantic Coast Flatwoods (MLRA 153A). (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). EPA Ecoregion (Level III): Southeastern Plains (65). EPA Ecoregion (Level IV): Southern Pine Plains and Hills (65f).	Wild material		2169057	NA 89093
418	NA 87823	FL24-01	Ilex cassine L.	Florida, United States	NA		2024	COLLECTED	09/05/2024	Matanzas State Forest.	29.72143991, -81.28386478		Boggy blackwater ditches along edge of dirt road. EPA Ecoregion III: Southern Coastal Plain (75). EPA Ecoregion IV: Eastern Florida Flatwoods (75d). Geology: Beach Ridge and Dune. Soil: Immokalee Series Fine Sand.	Wild material		2168973	NA 87823
419	NA 87824	FL24-02	Ilex cassine L.	Florida, United States	NA		2024	COLLECTED	09/05/2024	Wickham Park.	28.17068273, -80.66140942		A very open, sandy, and xeric forest that rapidly turns wet and boggy where P. palustris (and Ilex cassine) occurs. EPA Ecoregion III: Southern Coastal Plain (75). EPA Ecoregion IV: Eastern Florida Flatwoods (75d). Geology: Anastasia Formation. Soil: Myakka Series Sand, 0 to 2 percent slopes.	Wild material		2168974	NA 87824
420	NA 87825	FL24-03	Ilex ambigua Torr.	Florida, United States	NA		2024	COLLECTED	09/07/2024	Rye Preserve, along the Manatee River.	27.50951673, -82.35916675		Open scrub, xeric, sandy. EPA Ecoregion III: Southern Coastal Plain (75). EPA Ecoregion IV: Southwestern Florida Flatwood (75b). Geology: Hawthorn Group, Peace River Formation. Soil: Cassia Series Fine Sand, moderately well drained.	Wild material		2168975	NA 87825
421	NA 87828	GA24-01	Ilex glabra (L.) A. Gray	Georgia, United States	NA	Not Available	2024	COLLECTED	09/09/2024	Crooked River State Park.	30.83654580, -81.55628447		Longleaf Pine flatwoods, very wet. EPA Ecoregion III: Southern Coastal Plain (75). Geology: Princess Anne Shoreline Complex-Barrier Island Facies. EPA Ecoregion IV: Sea Islands/Coastal Marsh (75j). Soil: Mandarin Series Fine Sand, 0 to 2 percent slopes.	Wild material		2168978	NA 87828
422	NA 87834	TRX240901-02WV	Ilex montana Torr. & A. Gray	West Virginia, United States	NA		2024	COLLECTED	09/01/2024	Blackwater Falls State Park.	39.10665000, -79.48680000	967		Wild material		2168853	NA 87834
423	NA 87687	'Lacquerberry'	Ilex opaca Aiton		NA	Not Available	2024							Cultivar	One own root, potted plant received.	2167509	NA 87687
424	NA 88852	TJK2023FL-047	Ilex glabra (L.) A. Gray	Florida, United States	NA		2024	COLLECTED	12/26/2023	South of Highway 98, west of Twine Road. Track has a very large powerline right-of-way to the east, and George Washington Swamp bottom to the west.	29.77640000, -85.27410000	6	Longleaf Pine-Saw Palmetto. This area appears to be declining in quality, as witnessed by the declining in Rhododendron stem/plant density. Possible contributing issues: lacking necessary fire regime, has not seen fire in 8-10 years, encroaching woody shrub layer, accumulating organic matter (pine needle), expanding tree canopy, Hurricane Michael. Slope: less than 7%. Aspect: West. Elevation: 20 feet.	Wild material		2165707	NA 88852
425	NA 88827	RJL-RM2023FLAL-001	Ilex ambigua Torr.	Florida, United States	NA		2023	COLLECTED	12/05/2023	Yellow River Wildlife Management Area, along DOF [Department of Forestry] Y9 dirt road 0.08 kilometers east of Miller Bluff Road.	30.65289100, -86.87602800	44	Growing in part shade to sun in very dry, highly competitive site still recovering from the logging of pines in the past decade. This young woodland is comprised of a combination of evergreen and deciduous species competing for available resources and light before the young sand pines begin to dominate the upper canopy. Slope: 0 percent. 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 primary soil type in the collection area is classified as Lakeland Sand soils (0 to 5 percent slopes). The surface soil profile of this area is primarily the Lakeland series which 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 material		2165657	NA 88827
426	NA 88833	RJL-RM2023FLAL-007	Ilex decidua Walter	Florida, United States	NA	Not Available	2023	COLLECTED	12/06/2023	Plants are growing on the north side of Oil Plant Road between the road and Bray Mill Creek (which dumps into the nearby Escambia River), 0.37 kilometers east of McDavid Park.	30.97645800, -87.18562600	37	Growing in full sun to part shade in seasonally moist to wet areas associated with Bray Mill Creek; however, during low rainfall periods, plants are in dry soil. The habitat is heavily degraded due to logging of most of the area except a narrow woodland along the creek edge. The gravel road also causes significant run off and deposition of road debris. Despite this fact, the Ilex decidua is thriving. Slope: 0 to 5 percent. Aspect: North to northeast. 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 Chewacla-Wahee-Riverview Series Association. The Chewacla Series consists of very deep, somewhat poorly drained, fine loamy alluvial soils of flood plains that range from strongly to very strongly acid. These soils contain very little rock and can reach a thickness of 2 m. Wahee Series consists of very deep, somewhat poorly drained, clayey and loamy marine or fluviomarine sediments. These soils are strongly to very strongly acid. The Riverview Series consists of very deep, well drained, moderately permeable soils that formed in loamy alluvium on flood plains. These soils contain a slightly higher level of mica and iron deposits and range from slightly to strongly acid. (Source: NRCS Web Soil Survey.)	Wild material		2165663	NA 88833
427	NA 88838	RJL-RM2023FLAL-012	Ilex opaca Aiton	Florida, United States	NA		2023	COLLECTED	12/08/2023	North side of Sid Hayes Road approximately 65 m southeast of the junction with Watson Road.	30.83277400, -87.24324500	32	Growing 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 material		2165668	NA 88838
428	NA 88845	RJL-RM2023FLAL-019	Ilex opaca Aiton	Florida, United States	NA		2023	COLLECTED	12/13/2023	Yellow River Water Management Area, found along an unnamed unpaved road leading down to the Yellow River. This unpaved road is accessed from Old River Road to the east near the junction with Shockley Springs Road.	30.87382600, -86.60221300	35	Plants are growing along the road on the woodland edge on a small bluff above a creek in well-drained to dry habitat in part shade. They are also found sporadically in areas along the Yellow River where occasional inundation occurs. Slope: N/A. Aspect: N/A. The underlying geology of this area is the Alum Bluff Group of Miocene origin. It includes the Chipola Formation, Oak Grove Sand, Shoal River Formation, Choctawhatchee Formation and the Jackson Bluff Formation. The formations included in this group are generally defined on the basis of their molluscan faunas and stratigraphic position. Puri (1953) described sediment facies as they relate to the formations of the Alum Bluff Group. These sediments are lithologically distinct as a group, not as individual units. The Alum Bluff Group crops out or is beneath a thin overburden in the western panhandle from river valleys in Okaloosa County eastward to western Jackson County. The Alum Bluff Group consists of clays, sands and shell beds which may vary from fossiliferous, sandy clays to unfossiliferous sands and clays and occasional carbonate beds. Mica is a common constituent and glauconite and phosphate occur sporadically. Induration varies from essentially nonindurated in sands to well indurated in carbonate lenses. Colors range from cream to olive gray with mottled reddish brown in weathered sections. Sand grain size varies from very fine to very coarse with sporadic occurrences of gravel. These sediments generally have low permeabilities and are part of the intermediate confining unit/aquifer system. (Source: USGS Florida Geologic Map Data.) The surface soil profile of this area is primarily Bonifay-Dothan-Angie complex (5 to 12 percent slopes). Bonifay soil consists of very deep, well drained, moderately slowly permeable soils on ridges and side slopes in the Southern Coastal Plain. They formed in thick beds of sandy and loamy marine sediments. Solum thickness ranges from 1.5-2.0 m. Soil reaction ranges from very strongly acid to moderately acid throughout, except where the surface has been limed. Ironstone pebbles, 2 to 15 mm in size, range from 0 to 5 percent, by volume. Depth to the plinthic horizon ranges from 1.1-1.7 m. Some horizons contain up to 25 percent plinthite by volume. The Dothan Series consists of very deep, well drained soils that formed in thick beds of unconsolidated, medium to fine-textured marine sediments. Dothan soils are on interfluves. The surface 0-33 cm is characterized by sandy-loam, well-drained soils that are strongly acid. From 33-200 cm they are characterized by sandy clay loam soils that are more moisture retentive and strongly acid. The Angie series consists of very deep, moderately well drained, slowly permeable soils that formed in loamy and clayey sediment on Tertiary-aged uplands. These soils are on broad, level to strongly sloping coastal plains. Slope is dominantly 1 to 5 percent, but the range is 0 to 12 percent. (Source: NRCS Web Soil Survey.)	Wild material		2165675	NA 88845
429	NA 88846	RJL-RM2023FLAL-020	Ilex decidua Walter	Florida, United States	NA		2023	COLLECTED	12/13/2023	Yellow River Water Management Area: found in an area where an unnamed unpaved road dead ends near the Yellow River. This unpaved road is accessed from Old River Road to the east near the junction with Shockley Springs Road.	30.86973100, -86.59168700	23	Plants are growing primarily in part-shade to part-sun in low-lying moist habitats associated with the Yellow River. They are in the flood zone, but not regularly inundated. Slope: N/A. Aspect: N/A. The underlying geology of this area is the Alum Bluff Group of Miocene origin. It includes the Chipola Formation, Oak Grove Sand, Shoal River Formation, Choctawhatchee Formation and the Jackson Bluff Formation. The formations included in this group are generally defined on the basis of their molluscan faunas and stratigraphic position. Puri (1953) described sediment facies as they relate to the formations of the Alum Bluff Group. These sediments are lithologically distinct as a group, not as individual units. The Alum Bluff Group crops out or is beneath a thin overburden in the western panhandle from river valleys in Okaloosa County eastward to western Jackson County. The Alum Bluff Group consists of clays, sands and shell beds which may vary from fossiliferous, sandy clays to unfossiliferous sands and clays and occasional carbonate beds. Mica is a common constituent and glauconite and phosphate occur sporadically. Induration varies from essentially nonindurated in sands to well indurated in carbonate lenses. Colors range from cream to olive gray with mottled reddish brown in weathered sections. Sand grain size varies from very fine to very coarse with sporadic occurrences of gravel. These sediments generally have low permeabilities and are part of the intermediate confining unit/aquifer system. (Source: USGS Florida Geologic Map Data.) The surface soil profile of this area is primarily Kinston, Johnston, and Bibb soils, frequently flooded. Kinston Series soils are poorly drained, alluvial, fine-loamy, siliceous, and acid soils of flood plains. They are peaty to loamy friable, slightly sticky and slightly plastic in the upper 0 to 7.5 cm of the strata with less sand and more silt-loam in progressively deeper strata. The Johnston Series consists of very deep, very poorly drained coarse-loamy, siliceous, active, acid, thermic Cumulic Humaquepts. The upper 0-75 cm is black, mucky loam that is friable and very strongly acid. The lower strata to 1.75 m is dark gray, loamy fine sand, single grained, loose and very strongly acid. The Bibb Series soils consists of very deep, poorly drained, moderately permeable soils on flood plains of streams in the Southern Coastal Plain (133A) Major Land Resource Area. They formed in stratified loamy and sandy alluvium that are commonly and frequently flooded and water runs off the surface very slowly. Slopes range from 0 to 2 percent. (Source: NRCS Web Soil Survey.)	Wild material		2165676	NA 88846
430	NA 88847	RJL-RM2023FLAL-021	Ilex amelanchier M. A. Curtis ex Chapm.	Florida, United States	NA		2023	COLLECTED	12/13/2023	Yellow River Water Management Area, found in an area where an unnamed unpaved road dead ends near the Yellow River. This unpaved road is accessed from Old River Road to the east near the junction with Shockley Springs Road. Individuals are accessed by foot along the edge of the river and associated wetland depressions to the west of the road.	30.86980100, -86.59210500	23	Plants growing in seasonally inundated swamp habitats associated with the Yellow River. Plants are emergent during portions of the year, primarily during the growing season. During this time of collection, water had receded from the wetlands but the area was still quite wet with many tiny stream rivulets still draining. Slope: N/A. Aspect: N/A. The underlying geology of this area is the Alum Bluff Group of Miocene origin. It includes the Chipola Formation, Oak Grove Sand, Shoal River Formation, Choctawhatchee Formation and the Jackson Bluff Formation. The formations included in this group are generally defined on the basis of their molluscan faunas and stratigraphic position. Puri (1953) described sediment facies as they relate to the formations of the Alum Bluff Group. These sediments are lithologically distinct as a group, not as individual units. The Alum Bluff Group crops out or is beneath a thin overburden in the western panhandle from river valleys in Okaloosa County eastward to western Jackson County. The Alum Bluff Group consists of clays, sands and shell beds which may vary from fossiliferous, sandy clays to unfossiliferous sands and clays and occasional carbonate beds. Mica is a common constituent and glauconite and phosphate occur sporadically. Induration varies from essentially nonindurated in sands to well indurated in carbonate lenses. Colors range from cream to olive gray with mottled reddish brown in weathered sections. Sand grain size varies from very fine to very coarse with sporadic occurrences of gravel. These sediments generally have low permeabilities and are part of the intermediate confining unit/aquifer system. (Source: USGS Florida Geologic Map Data.) The surface soil profile of this area is primarily Kinston, Johnston, and Bibb soils, frequently flooded. Kinston Series soils are poorly drained, alluvial, fine-loamy, siliceous, and acid soils of flood plains. They are peaty to loamy friable, slightly sticky and slightly plastic in the upper 0 to 7.5 cm of the strata with less sand and more silt-loam in progressively deeper strata. The Johnston Series consists of very deep, very poorly drained coarse-loamy, siliceous, active, acid, thermic Cumulic Humaquepts. The upper 0-75 cm is black, mucky loam that is friable and very strongly acid. The lower strata to 1.75 m is dark gray, loamy fine sand, single grained, loose and very strongly acid. The Bibb Series soils consists of very deep, poorly drained, moderately permeable soils on flood plains of streams in the Southern Coastal Plain (133A) Major Land Resource Area. They formed in stratified loamy and sandy alluvium that are commonly and frequently flooded and water runs off the surface very slowly. Slopes range from 0 to 2 percent. (Source: NRCS Web Soil Survey.)	Wild material		2165677	NA 88847
431	NA 88848	RJL-RM2023FLAL-022	Ilex amelanchier M. A. Curtis ex Chapm.	Florida, United States	NA	Not Available	2023	COLLECTED	12/13/2023	Yellow River Water Management Area, found in an area where an unnamed unpaved road dead ends near the Yellow River. This unpaved road is accessed from Old River Road to the east near the junction with Shockley Springs Road. Individuals are accessed by foot along the edge of the river and associated wetland depressions to the west of the road.	30.86945000, -86.59348800	23	Plants growing in seasonally inundated swamp habitats associated with the Yellow River. Plants are emergent during portions of the year, primarily during the growing season. During this time of collection, water had receded from the wetlands but the area was still quite wet with many tiny stream rivulets still draining. Slope: N/A. Aspect: N/A. The underlying geology of this area is the Alum Bluff Group of Miocene origin. It includes the Chipola Formation, Oak Grove Sand, Shoal River Formation, Choctawhatchee Formation and the Jackson Bluff Formation. The formations included in this group are generally defined on the basis of their molluscan faunas and stratigraphic position. Puri (1953) described sediment facies as they relate to the formations of the Alum Bluff Group. These sediments are lithologically distinct as a group, not as individual units. The Alum Bluff Group crops out or is beneath a thin overburden in the western panhandle from river valleys in Okaloosa County eastward to western Jackson County. The Alum Bluff Group consists of clays, sands and shell beds which may vary from fossiliferous, sandy clays to unfossiliferous sands and clays and occasional carbonate beds. Mica is a common constituent and glauconite and phosphate occur sporadically. Induration varies from essentially nonindurated in sands to well indurated in carbonate lenses. Colors range from cream to olive gray with mottled reddish brown in weathered sections. Sand grain size varies from very fine to very coarse with sporadic occurrences of gravel. These sediments generally have low permeabilities and are part of the intermediate confining unit/aquifer system. (Source: USGS Florida Geologic Map Data.) The surface soil profile of this area is primarily Kinston, Johnston, and Bibb soils, frequently flooded. Kinston Series soils are poorly drained, alluvial, fine-loamy, siliceous, and acid soils of flood plains. They are peaty to loamy friable, slightly sticky and slightly plastic in the upper 0 to 7.5 cm of the strata with less sand and more silt-loam in progressively deeper strata. The Johnston Series consists of very deep, very poorly drained coarse-loamy, siliceous, active, acid, thermic Cumulic Humaquepts. The upper 0-75 cm is black, mucky loam that is friable and very strongly acid. The lower strata to 1.75 m is dark gray, loamy fine sand, single grained, loose and very strongly acid. The Bibb Series soils consists of very deep, poorly drained, moderately permeable soils on flood plains of streams in the Southern Coastal Plain (133A) Major Land Resource Area. They formed in stratified loamy and sandy alluvium that are commonly and frequently flooded and water runs off the surface very slowly. Slopes range from 0 to 2 percent. (Source: NRCS Web Soil Survey.)	Wild material		2165678	NA 88848
432	NA 88849	RJL-RM2023FLAL-023	Ilex amelanchier M. A. Curtis ex Chapm.	Florida, United States	NA	Not Available	2023	COLLECTED	12/13/2023	Yellow River Water Management Area, found in an area where an unnamed unpaved road dead ends near the Yellow River. This unpaved road is accessed from Old River Road to the east near the junction with Shockley Springs Road. Individuals are accessed by foot along the edge of the river and associated wetland depressions to the west of the road.	30.86982300, -86.59378300	23	Plants growing in seasonally inundated swamp habitats associated with the Yellow River. Plants are emergent during portions of the year, primarily during the growing season. During this time of collection, water had receded from the wetlands but the area was still quite wet with many tiny stream rivulets still draining. Slope: N/A. Aspect: N/A. The underlying geology of this area is the Alum Bluff Group of Miocene origin. It includes the Chipola Formation, Oak Grove Sand, Shoal River Formation, Choctawhatchee Formation and the Jackson Bluff Formation. The formations included in this group are generally defined on the basis of their molluscan faunas and stratigraphic position. Puri (1953) described sediment facies as they relate to the formations of the Alum Bluff Group. These sediments are lithologically distinct as a group, not as individual units. The Alum Bluff Group crops out or is beneath a thin overburden in the western panhandle from river valleys in Okaloosa County eastward to western Jackson County. The Alum Bluff Group consists of clays, sands and shell beds which may vary from fossiliferous, sandy clays to unfossiliferous sands and clays and occasional carbonate beds. Mica is a common constituent and glauconite and phosphate occur sporadically. Induration varies from essentially nonindurated in sands to well indurated in carbonate lenses. Colors range from cream to olive gray with mottled reddish brown in weathered sections. Sand grain size varies from very fine to very coarse with sporadic occurrences of gravel. These sediments generally have low permeabilities and are part of the intermediate confining unit/aquifer system. (Source: USGS Florida Geologic Map Data.) The surface soil profile of this area is primarily Kinston, Johnston, and Bibb soils, frequently flooded. Kinston Series soils are poorly drained, alluvial, fine-loamy, siliceous, and acid soils of flood plains. They are peaty to loamy friable, slightly sticky and slightly plastic in the upper 0 to 7.5 cm of the strata with less sand and more silt-loam in progressively deeper strata. The Johnston Series consists of very deep, very poorly drained coarse-loamy, siliceous, active, acid, thermic Cumulic Humaquepts. The upper 0-75 cm is black, mucky loam that is friable and very strongly acid. The lower strata to 1.75 m is dark gray, loamy fine sand, single grained, loose and very strongly acid. The Bibb Series soils consists of very deep, poorly drained, moderately permeable soils on flood plains of streams in the Southern Coastal Plain (133A) Major Land Resource Area. They formed in stratified loamy and sandy alluvium that are commonly and frequently flooded and water runs off the surface very slowly. Slopes range from 0 to 2 percent. (Source: NRCS Web Soil Survey.)	Wild material		2165679	NA 88849
433	NA 88818	TJK2023FL-037	Ilex opaca Aiton var. arenicola (Ashe) Ashe	Florida, United States	NA	Not Available	2023	COLLECTED	12/05/2023	Lake Wales Ridge State Forest.	27.68579700, -81.41422500	27	Xeric scrub. Slope: flat. Aspect: Southeast. Elevation: 89 feet.	Wild material		2165647	NA 88818
434	NA 88824	TJK2023FL-041	Ilex opaca Aiton	Florida, United States	NA		2023	COLLECTED	12/11/2023	Holmes Creek, Live Oak Landing.	30.60450000, -85.76670000	6	Bottomland floodpain of Holmes Creek. Slope: flat. Aspect: Southwest. Elevation: 20 feet.	Wild material		2165653	NA 88824
435	NA 88825	TJK2023FL-042	Ilex verticillata (L.) A. Gray	Florida, United States	NA		2023	COLLECTED	12/11/2023	Holmes Creek, Live Oak Landing.	30.60450000, -85.76670000	6	Bottomland floodpain of Holmes Creek. Slope: flat. Aspect: Southwest. Elevation: 20 feet.	Wild material		2165654	NA 88825
436	NA 88826	TJK2023FL-043	Ilex decidua Walter	Florida, United States	NA		2023	COLLECTED	12/14/2023	Upper Escambia River.	30.87870000, -87.29120000	9	Hammock, bench-like river floodplain/bottomland. Slope: flat. Aspect: East-southeast. Elevation: 30 feet.	Wild material		2165655	NA 88826
437	NA 88811	TXWL2023-017	Ilex longipes Chapm. ex Trel.	Texas, United States	NA	Not Available	2023	COLLECTED	12/04/2023	Indian Hills Community/Wiergate: County Road 1089 roadside.	31.00317700, -93.72888600		Roadside. Upland; sandy loam soil.	Wild material		2165614	NA 88811
438	NA 88812	TXWL2023-018	Ilex ambigua Torr.	Texas, United States	NA		2023	COLLECTED	12/05/2023	Davy Crockett National Forest: Forest Service Road 526 roadside.	31.49017400, -95.22343300		Roadside. Shortleaf mixed upland hardwood forest; dry-mesic.	Wild material		2165615	NA 88812
439	NA 88813	TXWL2023-020	Ilex vomitoria Aiton	Texas, United States	NA		2023	COLLECTED	12/06/2023	Private property (Bayou Bleu Farm).	31.66376880, -94.01070880		Road edge of wooded road; mixed pine-hardwood stand.	Wild material		2165617	NA 88813
440	NA 88814	TXWL2023-021	Ilex ambigua Torr.	Texas, United States	NA		2023	COLLECTED	12/09/2023	Roadside between Big Cow Creek and Hardy Cemetery.	31.03548900, -93.85086800		Roadside; mesic, mixed hardwood/pine forest.	Wild material		2165618	NA 88814
441	NA 88815	TXWL2023-022	Ilex opaca Aiton	Texas, United States	NA		2023	COLLECTED	12/10/2023	Angelina National Forest: Upland Island Wilderness Area: Neches River bottom.	31.03919400, -94.37937900		Bottomland hardwood forest.	Wild material		2165619	NA 88815
442	NA 88816	TXWL2023-023	Ilex decidua Walter	Texas, United States	NA		2023	COLLECTED	12/10/2023	Angelina National Forest: Upland Island Wilderness Area: Neches River bottom.	31.03478500, -94.38286600		Bottomland hardwood forest.	Wild material		2165620	NA 88816
443	NA 88802	TJK2023LA/TX-002	Ilex decidua Walter	Louisiana, United States	NA		2023	COLLECTED	11/21/2023	Interstate 20, westbound, approximately 6 miles west of U.S. Highway 65 and 7.5 miles east of Louisiana Highway 577. Tensas River watershed.	32.41950000, -91.29670000	21	Damp wooded treeline. Slope: 12%. Aspect: West-southwest. Elevation: 69 feet.	Wild material		2159185	NA 88802
444	NA 88809	TJK2023LA/TX-009	Ilex decidua Walter	Texas, United States	NA		2023	COLLECTED	11/27/2023	Southbound Highway 281, west side of road, approximately 13 miles south of Highway 290 and 1 mile north of RR [rural route] 473 East.	30.01610000, -98.40610000	407	Roadside, brushy fencerow. Slope: 10%. Aspect: East-northeast. Elevation: 1336 feet.	Wild material		2159192	NA 88809
445	NA 88800	TXWL2023-015	Ilex longipes Chapm. ex Trel.	Texas, United States	NA		2023	COLLECTED	11/15/2023	Sabine National Forest: Compartment 65 along County Road 131 near White Rock, Texas.	31.55793500, -94.01980900		Upland; mixed hardwood and pine; sandy soil; rocky outcrops.	Wild material		2159157	NA 88800
446	NA 88690	RJL2023NJ-003	Ilex verticillata (L.) A. Gray	New Jersey, United States	NA		2023	COLLECTED	11/10/2023	Franklin Township: Piney Hollow Preservation Area (the site is owned by Franklin Township). This species was found below the dam at the far end of McCarthys Lakes. Plants accessed by foot along trails throughout property.	39.57407200, -74.92518600	28	Plants growing in part-shade to sun of the moist to saturated areas below the McCarthys Lakes dam in the wetlands associated with the New Squankum Branch. The area appears to be inundated year-round with plants growing on low mounds surrounded by obligate wetland species. Slope: N/A. Aspect: N/A. The underlying geology of this area is of Middle Miocene, Serravallian origin and characterized as an Cohansey Formation. It is comprised of sand, white to yellow with local gravel and clay. Locally stained red or orange brown by iron oxides and (or) cemented into large blocks of ironstone. Unweathered clay is typically dark gray, but commonly weathers white where interbedded with thin beds of ironstone. Unit is a complex of interfingering marine and nonmarine facies. Sand is typically medium grained and moderately sorted although it ranges from fine to very coarse grained and from poorly to well sorted. Sand consists of quartz and siliceous rock fragments. Some beds are locally micaceous. In general, the sand is crossbedded, although the style of crossbedding varies significantly with the paleoenvironment. Trough crossbedding predominates, especially in the nonmarine channel fill deposits, and the scale of the crossbeds varies from small to large. Maximum thickness in the map area is about 60 m; however, thickness is difficult to determine because of the irregular basal contact and extensive post-depositional erosion. There is as much as 18 m of relief along the basal contact. The basal contact is sharp, undulatory, and directly overlain by a thin gravel bed. The Cohansey Formation unconformably overlies the Kirkwood Formation and is found in channels cut down into the Kirkwood. Where the Kirkwood consists of sandy, light-colored sediments, the basal contact of the Cohansey is drawn below crossbedded sediments. Where the Kirkwood consists of dark-colored silty beds, the basal contact is drawn between light-colored Cohansey sediments and the underlying dark-colored sediments. The Cohansey was markedly thinned because of erosion prior to deposition of overlying units in the western and southern parts of the southern sheet. The unit has been extensively eroded and stripped from large areas of the New Jersey Coastal Plain, particularly in the central sheet where outliers are common. In spite of its widespread nature, the Cohansey is poorly exposed because of its loose sandy composition, which causes it to erode easily. (Source: USGS New Jersey Geologic Map Data.) The primary soil type in the collection area is classified as Manahawkin Series muck, 0 to 2 percent slopes, frequently flooded, Northern Coastal Plain. Manahawkin Series soils are very deep, very poorly drained soils that are sandy or sandy-skeletal, siliceous, dysic, mesic Terric Haplosaprists high in organic deposits that are found in lake basins, back swamps, floodplains, and freshwater channels. The soils are classified in the dysic reaction class because pH in water dominantly ranges from 4.5 to 5.0. The zone from the soil surface to a depth of 200 cm is continuously saturated (endosaturation). The upper strata of Manahawkin Series from 0 to 76 cm is black broken face and rubbed muck; 10 percent fibers, less than 2 percent rubbed; moderate medium granular structure; mat of many fine roots; identifiable material is primarily herbaceous with a trace of woody fragments; 85-95 percent organic matter; extremely acid. Lower strata to 200 cm are gray sand, single grained and loose; strongly acid. (Source: NRCS Web Soil Survey.)	Wild material		2159118	NA 88690
447	NA 88691	RJL2023NJ-004	Ilex laevigata (Pursh) A. Gray	New Jersey, United States	NA		2023	COLLECTED	11/10/2023	Franklin Township: Piney Hollow Preservation Area (the site is owned by Franklin Township). This species was found below the dam at the far end of McCarthys Lakes. Plants accessed by foot along trails throughout property.	39.57404200, -74.92523700	28	Plants growing in part-shade to sun of the moist to saturated areas below the McCarthys Lakes dam in the wetlands associated with the New Squankum Branch. The area appears to be inundated year-round with plants growing on low mounds surrounded by obligate wetland species. Slope: N/A. Aspect: N/A. The underlying geology of this area is of Middle Miocene, Serravallian origin and characterized as an Cohansey Formation. It is comprised of sand, white to yellow with local gravel and clay. Locally stained red or orange brown by iron oxides and (or) cemented into large blocks of ironstone. Unweathered clay is typically dark gray, but commonly weathers white where interbedded with thin beds of ironstone. Unit is a complex of interfingering marine and nonmarine facies. Sand is typically medium grained and moderately sorted although it ranges from fine to very coarse grained and from poorly to well sorted. Sand consists of quartz and siliceous rock fragments. Some beds are locally micaceous. In general, the sand is crossbedded, although the style of crossbedding varies significantly with the paleoenvironment. Trough crossbedding predominates, especially in the nonmarine channel fill deposits, and the scale of the crossbeds varies from small to large. Maximum thickness in the map area is about 60 m; however, thickness is difficult to determine because of the irregular basal contact and extensive post-depositional erosion. There is as much as 18 m of relief along the basal contact. The basal contact is sharp, undulatory, and directly overlain by a thin gravel bed. The Cohansey Formation unconformably overlies the Kirkwood Formation and is found in channels cut down into the Kirkwood. Where the Kirkwood consists of sandy, light-colored sediments, the basal contact of the Cohansey is drawn below crossbedded sediments. Where the Kirkwood consists of dark-colored silty beds, the basal contact is drawn between light-colored Cohansey sediments and the underlying dark-colored sediments. The Cohansey was markedly thinned because of erosion prior to deposition of overlying units in the western and southern parts of the southern sheet. The unit has been extensively eroded and stripped from large areas of the New Jersey Coastal Plain, particularly in the central sheet where outliers are common. In spite of its widespread nature, the Cohansey is poorly exposed because of its loose sandy composition, which causes it to erode easily. (Source: USGS New Jersey Geologic Map Data.) The primary soil type in the collection area is classified as Manahawkin Series muck, 0 to 2 percent slopes, frequently flooded, Northern Coastal Plain. Manahawkin Series soils are very deep, very poorly drained soils that are sandy or sandy-skeletal, siliceous, dysic, mesic Terric Haplosaprists high in organic deposits that are found in lake basins, back swamps, floodplains, and freshwater channels. The soils are classified in the dysic reaction class because pH in water dominantly ranges from 4.5 to 5.0. The zone from the soil surface to a depth of 200 cm is continuously saturated (endosaturation). The upper strata of Manahawkin Series from 0 to 76 cm is black broken face and rubbed muck; 10 percent fibers, less than 2 percent rubbed; moderate medium granular structure; mat of many fine roots; identifiable material is primarily herbaceous with a trace of woody fragments; 85-95 percent organic matter; extremely acid. Lower strata to 200 cm are gray sand, single grained and loose; strongly acid. (Source: NRCS Web Soil Survey.)	Wild material		2159119	NA 88691
448	NA 88692	RJL2023NJ-005	Ilex opaca Aiton	New Jersey, United States	NA		2023	COLLECTED	11/10/2023	Franklin Township: Piney Hollow Preservation Area (the site is owned by Franklin Township). This species was found on as well as below the dam at the far end of McCarthys Lakes. Plants accessed by foot along trails throughout property.	39.57423200, -74.92525600	29	Plants growing in part-shade to sun of the moist to saturated areas below the McCarthys Lakes dam in the wetlands associated with the New Squankum Branch. Plants were also found growing on the slopes of the dam in well-drained mesic to dry-mesic conditions. This species is clearly adaptable to a variety of conditions. Slope: 0 to 15 percent. Aspect: East. Elevation: 28 to 30 meters. NOTE: In addition to the soil type described below, this species was also growing on the slopes of a constructed earthen dam of unknown soil origin. The underlying geology of this area is of Middle Miocene, Serravallian origin and characterized as an Cohansey Formation. It is comprised of sand, white to yellow with local gravel and clay. Locally stained red or orange brown by iron oxides and (or) cemented into large blocks of ironstone. Unweathered clay is typically dark gray, but commonly weathers white where interbedded with thin beds of ironstone. Unit is a complex of interfingering marine and nonmarine facies. Sand is typically medium grained and moderately sorted although it ranges from fine to very coarse grained and from poorly to well sorted. Sand consists of quartz and siliceous rock fragments. Some beds are locally micaceous. In general, the sand is crossbedded, although the style of crossbedding varies significantly with the paleoenvironment. Trough crossbedding predominates, especially in the nonmarine channel fill deposits, and the scale of the crossbeds varies from small to large. Maximum thickness in the map area is about 60 m; however, thickness is difficult to determine because of the irregular basal contact and extensive post-depositional erosion. There is as much as 18 m of relief along the basal contact. The basal contact is sharp, undulatory, and directly overlain by a thin gravel bed. The Cohansey Formation unconformably overlies the Kirkwood Formation and is found in channels cut down into the Kirkwood. Where the Kirkwood consists of sandy, light-colored sediments, the basal contact of the Cohansey is drawn below crossbedded sediments. Where the Kirkwood consists of dark-colored silty beds, the basal contact is drawn between light-colored Cohansey sediments and the underlying dark-colored sediments. The Cohansey was markedly thinned because of erosion prior to deposition of overlying units in the western and southern parts of the southern sheet. The unit has been extensively eroded and stripped from large areas of the New Jersey Coastal Plain, particularly in the central sheet where outliers are common. In spite of its widespread nature, the Cohansey is poorly exposed because of its loose sandy composition, which causes it to erode easily. (Source: USGS New Jersey Geologic Map Data.) The primary soil type in the collection area is classified as Manahawkin Series muck, 0 to 2 percent slopes, frequently flooded, Northern Coastal Plain. Manahawkin Series soils are very deep, very poorly drained soils that are sandy or sandy-skeletal, siliceous, dysic, mesic Terric Haplosaprists high in organic deposits that are found in lake basins, back swamps, floodplains, and freshwater channels. The soils are classified in the dysic reaction class because pH in water dominantly ranges from 4.5 to 5.0. The zone from the soil surface to a depth of 200 cm is continuously saturated (endosaturation). The upper strata of Manahawkin Series from 0 to 76 cm is black broken face and rubbed muck; 10 percent fibers, less than 2 percent rubbed; moderate medium granular structure; mat of many fine roots; identifiable material is primarily herbaceous with a trace of woody fragments; 85-95 percent organic matter; extremely acid. Lower strata to 200 cm are gray sand, single grained and loose; strongly acid. (Source: NRCS Web Soil Survey.)	Wild material		2159120	NA 88692
449	NA 88697	RJL2023NCSC-002	Ilex amelanchier M. A. Curtis ex Chapm.	North Carolina, United States	NA		2023	COLLECTED	11/12/2023	Goose 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, -79.09915700	60	Plants 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 material		2159125	NA 88697
450	NA 88698	RJL2023NCSC-003	Ilex laevigata (Pursh) A. Gray	North Carolina, United States	NA		2023	COLLECTED	11/13/2023	Sandhills Game Land: north side of Pulpwood Road approximately 0.11 km southwest of the junction with Tyner Road.	34.95939500, -79.48676300	114	Plants 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 material		2159126	NA 88698
451	NA 88711	RJL2023NCSC-016	Ilex myrtifolia Walter	South Carolina, United States	NA		2023	COLLECTED	11/14/2023	Francis 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, -79.67761800	11	Plants 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 material		2159139	NA 88711
452	NA 88713	RJL2023NCSC-018	Ilex opaca Aiton	South Carolina, United States	NA		2023	COLLECTED	11/14/2023	Francis 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, -79.67749100	11	Plants 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 material		2159141	NA 88713
453	NA 88716	RJL2023NCSC-021	Ilex myrtifolia Walter	South Carolina, United States	NA		2023	COLLECTED	11/14/2023	Francis 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, -79.60253700	31	Plants 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 material		2159144	NA 88716
454	NA 88717	RJL2023NCSC-022	Ilex opaca Aiton	South Carolina, United States	NA		2023	COLLECTED	11/14/2023	Francis 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, -79.60217900	22	Plants 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 material		2159145	NA 88717
455	NA 88718	RJL2023NCSC-023	Ilex decidua Walter	South Carolina, United States	NA		2023	COLLECTED	11/15/2023	Waccamaw National Wildlife Refuge: U.S. Highway 701, Yauhannah Landing on the east side of the Great Pee Dee River. Plants growing in low woods on the north side of the landing.	33.66208900, -79.15305000	2	Plants growing in shade to part-shade of a moist to wet woodland habitat that is mostly deciduous and evergreen. Portions of the woodland have depressions with year-round standing water. Slope: N/A. Aspect: N/A. The underlying geology of this area is of Quaternary origin and characterized as Alluvial Valley Swamp. This formation is unconformable on all underlying units. It is composed of fluvial sand and gravel at base, grading upwards into fine sands and silts, and local occasional peat. May be overrun with recent sediments from forest cutting and agriculture. (Source: USGS South Carolina Geologic Map Data.) The primary soil type in this collection area is classified as Johnston Series loam. The Johnson Series consists of very deep, very poorly drained coarse-loamy, siliceous, active, acid, thermic Cumulic Humaquepts. The upper 0-75 cm is black, mucky loam that is friable and very strongly acid. The lower stratum to 1.75 m is dark gray, loamy fine sand, single grained, loose and very strongly acid. (Source: NRCS Web Soil Survey.)	Wild material		2159146	NA 88718
456	NA 88719	RJL2023NCSC-024	Ilex laevigata (Pursh) A. Gray	South Carolina, United States	NA		2023	COLLECTED	11/15/2023	Little Pee Dee Heritage Preserve/Wildlife Management Area (South Carolina Department of Natural Resources Public Lands, on South Carolina Highway 917).	34.14123300, -79.19532100	13	Plants growing in high understory shade to part-shade of a moist to relatively dry pine forest with occasional deciduous trees. The litter layer in the woodlands is very deep with longleaf pine needles, while the edges of the woodlands are much drier with exposed white sand and little to no litter layer. Slope: N/A. Aspect: N/A. The underlying geology of this area is of Pleistocene origin and characterized as Waccamaw Formation. This formation is another Carolina coastalized terrace that is deeply weathered. It is characterized by unconsolidated, coarse-detrital, soft sand limestones and loose gray to buff fine quartz sands in which occasional small quartz pebbles are present. It also includes sedimentary, carbonate, soft limestones. (Source: USGS South Carolina Geologic Map Data.) The primary soil type in this collection area is classified as Lynn Haven Series sand. The Lynn Haven Series consists of very deep, poorly and very poorly drained, moderate or moderately rapid, permeable soils in low areas and depressions in Atlantic Flatwoods and the Gulf. They formed in thick deposits of sandy marine sediments. Th Lynn Haven Series soil is approximately 2 m thick and ranges from black near the surface to yellow brown in the deepest strata. Most of the strata are comprised of fine sands that are friable with the deepest strata also including a small percentage of organic matter. Reaction ranges from extremely acid to strongly acid throughout the profile. The water table is at 0-15 cm for periods of 2 to 6 months annually and within a depth 1 m for more than 6 months during most years; during extended dry periods it is below 1 meter. Depressional areas are ponded for long duration in most years. (Source: NRCS Web Soil Survey.)	Wild material		2159147	NA 88719
457	NA 88721	RJL2023NCSC-026	Ilex opaca Aiton	South Carolina, United States	NA		2023	COLLECTED	11/15/2023	Little Pee Dee Heritage Preserve/Wildlife Management Area (South Carolina Department of Natural Resources Public Lands, on South Carolina Highway 917).	34.14091500, -79.19555200	13	Plants growing in high understory shade to part-shade of a moist to relatively dry pine forest with occasional deciduous trees. The litter layer in the woodlands is very deep with longleaf pine needles, while the edges of the woodlands are much drier with exposed white sand and little to no litter layer. Slope: N/A. Aspect: N/A. The underlying geology of this area is of Pleistocene origin and characterized as Waccamaw Formation. This formation is another Carolina coastalized terrace that is deeply weathered. It is characterized by unconsolidated, coarse-detrital, soft sand limestones and loose gray to buff fine quartz sands in which occasional small quartz pebbles are present. It also includes sedimentary, carbonate, soft limestones. (Source: USGS South Carolina Geologic Map Data.) The primary soil type in this collection area is classified as Lynn Haven Series sand. The Lynn Haven Series consists of very deep, poorly and very poorly drained, moderate or moderately rapid, permeable soils in low areas and depressions in Atlantic Flatwoods and the Gulf. They formed in thick deposits of sandy marine sediments. Th Lynn Haven Series soil is approximately 2 m thick and ranges from black near the surface to yellow brown in the deepest strata. Most of the strata are comprised of fine sands that are friable with the deepest strata also including a small percentage of organic matter. Reaction ranges from extremely acid to strongly acid throughout the profile. The water table is at 0-15 cm for periods of 2 to 6 months annually and within a depth 1 m for more than 6 months during most years; during extended dry periods it is below 1 meter. Depressional areas are ponded for long duration in most years. (Source: NRCS Web Soil Survey.)	Wild material		2159149	NA 88721
458	NA 88723	RJL2023NCSC-028	Ilex myrtifolia Walter	North Carolina, United States	NA		2023	COLLECTED	11/15/2023	Juniper Creek State Game Lands (along Brunswick County Road 1340): swamps/wetlands associated with Juniper Creek.	34.12438700, -78.39310700	13	Plants growing in shade to part-shade of a swamp habitat along Juniper Creek. At the time of collection, the swamp was relatively dry with water found only in deep depressions. Slope: N/A. Aspect: N/A. The underlying geology of this area is of Cretaceous origin and characterized as Peedee Formation - Black Creek Group, undivided. The Peedee Formation is primarily unconsolidated, coarse-detrital, sand that is dark-green or gray, finely micaceous, more or less glauconitic, and argillitic sand, many layers of which are calcareous (impure limestone). Irregular concretionary masses of impure calcium carbonate occur in places. Dark marine clays are interstratified with sand. The Black Creek Group consists of irregularly bedded, laminated, carbonaceous clays and thin laminae and lenses of sand; lignite and pyrite present; glauconitic in places; massive interbedded layers of glauconitic sand present toward top of unit. Light-colored clays and coarse arkosic sands also found. (Source: USGS North Carolina Geologic Map Data.) The primary soil type in this collection area is classified as Dorovan Series muck. The Dorovan Series consists of very deep, very poorly drained, moderately permeable soils on densely forested flood plains, hardwood swamps, and depressions in the Atlantic Coast Flatwoods, Eastern Gulf Coast Flatwoods, and Southern Coastal Plain Major Land Resource Areas. They formed in highly decomposed acid-organic materials and have slopes that are less than 1 percent. (Source: NRCS Web Soil Survey.)	Wild material		2159151	NA 88723
459	NA 88725	RJL2023NCSC-030	Ilex myrtifolia Walter	North Carolina, United States	NA		2023	COLLECTED	11/15/2023	Boiling Spring Lakes, NC: Plants growing along unused road of potential new development on Baden Street, between Camden Street and Midwood Street. The site is accessed from North Carolina Highway 87 (George II Highway SE) by turning west onto Brunswick Road and right onto Baden Street at the first intersection.	34.01935700, -78.06110500	16	Plants growing in part-shade along the road, edges of ditches and managed edges of longleaf pine forest in well-drained, but seasonally moist habitat with very little organic litter layer. It seems that low competition and exposed sandy conditions allows this plant to thrive. Slope: N/A. Aspect: N/A. The underlying geology of this area is of Pleistocene origin and characterized as Waccamaw Formation. This formation is another Carolina coastalized terrace that is deeply weathered. It is characterized by unconsolidated, coarse-detrital, soft sand limestones and loose gray to buff fine quartz sands in which occasional small quartz pebbles are present. It also includes sedimentary, carbonate, soft limestones. (Source: USGS North Carolina Geologic Map Data.) The primary soil type in this collection area is classified as Leon Series fine sand. The Leon series consists of very deep, very poorly and poorly drained, moderately rapid to moderately slowly permeable soils on upland flats, depressions, stream terraces and tidal areas. They formed in sandy marine sediments of the Eastern Gulf Coast Flatwoods, the Atlantic Coast Flatwoods and to a lesser extent in the Southern Coastal Plain. The upper horizon (0-75 cm) is comprised of a high percent of blac and lower percentage of light gray sand that is very friable and very strongly acid. The lower horizon (75-270 cm) has a range of gray, dark brown and yellowish-brown sands that range from fine to coarse and are also very strongly acid. (Source: NRCS Web Soil Survey.)	Wild material		2159153	NA 88725
460	NA 88686	TJK2023FL-033	Ilex glabra (L.) A. Gray	Florida, United States	NA		2023	COLLECTED	11/18/2023	Navarre, Florida: Adams St. cul-de-sac, on nine-acre private property. Infrastructure development began and was terminated due to the lack of any engineering or environmental site planning (designated wetland status). It has remained idle for a number of years.	30.40970000, -86.92980000	11	Wet pine flatwood transitioning to a shrub bog habitat under fire suppression. Slope: 3.5%. Aspect: West. Elevation: 36 feet.	Wild material		2159098	NA 88686
461	NA 88688	TJK2023FL-035	Ilex decidua Walter	Florida, United States	NA		2023	COLLECTED	11/19/2023	Eglin Air Force Base, Choctaw West; Range Rd 813, approximately 0.3 miles north of Range Rd 213 - Choctaw Nolf Airport Rd. Growing in flat west of Weaver Creek.	30.51790000, -86.93230000	34	Damp (not wet) flat west of creek. Slope: less than 2%. Aspect: West. Elevation: 113 feet.	Wild material		2159100	NA 88688
462	NA 87576	'Golden Nellie'	Ilex hybr.		NA	Not Available	2023							Cultivar	Recorded at the U.S. National Arboretum as Ilex 'Golden Nellie'. Received as Ilex 'Whoa Nellie'. Rooted cutting. Holly Society of America test holly for 2024.	2165744	NA 87576
463	NA 88858	TRx231112-01MD	Ilex opaca Aiton	Maryland, United States	NA		2023	COLLECTED	11/12/2023		38.98349100, -76.91714400	22		Wild material		2159075	NA 88858
464	NA 88681	RJL2023PA-015	Ilex verticillata (L.) A. Gray	Pennsylvania, United States	NA		2023	COLLECTED	10/30/2023	Wetlands near Phillips Creek: seed collected from plants on the north and south (further east) side of Pennsylvania Route 188 approximately 6.9 kilometers east of the junction with Pennsylvania Route 487.	41.30353100, -76.22452800	381	Boggy to moist habitats associated with wetlands of Phillips Creek in shade to full sun next to the road. Slope: 0%. Aspect: various. The underlying geology of this area is of Devonian origin and characterized as the Catskill Formation. It is comprised of grayish-red sandstone, siltstone, shale, and mudstone; units of gray sandstone occur in upper part; lithologies in upper part arranged in fining-upward cycles. In the Altoona area, the Catskill Formation is mapped as the Duncannon, Sherman Creek, and Irish Valley Members, which are described under "Central and Eastern Pennsylvania" provinces. (Source: USGS Pennsylvania Geologic Map Data). The primary soil type in the collection area is classified as Wellsboro Series. The Wellsboro Series consists of very deep, moderately well- and somewhat poorly-drained soils formed in till derived from red sandstone, siltstone, and shale. Slope ranges from 0 to 50 percent. Saturated hydraulic conductivity is moderately high or high in the mineral surface layer, subsurface layer, and upper part of the subsoil; and low or moderately low in the lower part of the subsoil (fragipan) and the substratum. Solum thickness is greater than 102 cm. Depth to the fragipan ranges from 36 to 76 cm. Depth to bedrock is 152 cm or more. Rock fragments of subangular and rounded sandstone, siltstone or shale range from 5 to 40 percent in the A and B horizons, and from 15 to 50 percent in the Bx and C horizons. Typically, rock fragments average about 5 to 25 percent by volume above the fragipan and 15 to 40 percent by volume in and below the fragipan. Reaction commonly ranges from very strongly acid through moderately acid. (Source: NRCS Web Soil Survey).	Wild material		2159072	NA 88681
465	NA 88669	TXWL2023-012	Ilex decidua Walter	Texas, United States	NA		2023	COLLECTED	10/21/2023	County Road 3218 en route to Camp Wohaleta, north of Caddo National Grasslands.	33.75626700, -95.97888900		Roadside.	Wild material		2159044	NA 88669
466	NA 88665	RJL2023PA-002	Ilex verticillata (L.) A. Gray	Pennsylvania, United States	NA		2023	COLLECTED	10/01/2023	Woodlands along Pine Creek near the Harmonyville Road bridge.	40.18764500, -75.76732200	141	Moist to mucky, wet woodland conditions along Pine Creek. Much of the site is very wet due to recent rains; though, earlier in the year, the soils were only moist. Plants grow in both well-drained mesic conditions as well as seasonally wet conditions. They do not grow in standing water anywhere in this location. Plants in this population are found mostly in the shade and partial shade of deciduous trees; there are occasional gaps that offer higher light conditions as well. Slope: 0-2%. Aspect: N/A. The underlying geology of this area is of Precambrian origin and characterized as the Graphitic Felsic Gneiss. This includes Pickering Gneiss and small areas of marble; dominantly quartz and feldspar with varying amounts of graphite and various metamorphic minerals; medium grained, light to dark gray and greenish gray; sedimentary origin. (Source: USGS Pennsylvania Geologic Map Data). The primary soil type in the area of this collection is classified as Hatboro Silt Loam Series. The Hatboro Series consists of very deep and poorly drained soils formed in alluvium derived from metamorphic and crystalline rock. They are on flood plains. Slopes range from 0 to 3 percent. Saturated hydraulic conductivity is moderately high to high. Solum thickness ranges from 50 to 150 cm. Depth to bedrock ranges from 1.5 to 3 meters or more. Organic carbon decreases irregularly with depth or is greater than 0.2 percent directly above any strongly contrasting C horizon. The depth to strongly contrasting sand and gravel is more than 100 cm or the transition is greater than 12.5 cm. Content of gravel ranges from 0 to 10 percent in the solum and from 0 to 80 percent in the C horizon. Mica flakes are common in the solum, and the C horizon contains thin lenses of mica. Reaction ranges from very strongly acid through neutral to a depth of 75 cm and from moderately acid through slightly acid below 75 cm. (Source: NRCS Web Soil Survey.)	Wild material		2158814	NA 88665
467	NA 88658	TJK2023FL-012	Ilex verticillata (L.) A. Gray	Florida, United States	NA		2023	COLLECTED	09/10/2023	Lower Yellow River.	30.62868600, -86.80748000	3	Beautiful riverine system. Elevation: 13 feet. Slope: 0 (none). Aspect: Northwest.	Wild material		2158792	NA 88658
468	NA 88659	TJK2023FL-013	Ilex sp.	Florida, United States	NA		2023	COLLECTED	09/15/2023	Lower Yellow River.	30.58170000, -86.91770000	1	Elevation: 3 feet. Slope: 0 percent. Aspect: North.	Wild material		2158793	NA 88659
469	NA 88606	KY23-008	Ilex montana Torr. & A. Gray	Kentucky, United States	NA		2023	COLLECTED	09/09/2023	Black Mountain summit (second location, bulked with the first: Black Mountain; lat/long 36. 91614, -82. 89873)	36.91434000, -82.89463000	1261	Moist woods. Elevation: 4138 feet. Aspect: West. (Second location, bulked with first: Elevation: 4071 feet. Aspect: West.)	Wild material		2158698	NA 88606
470	NA 88621	KY23-025a	Ilex ambigua Torr.	Kentucky, United States	NA		2023	COLLECTED	09/10/2023	The Gulf - Natural Arch Scenic Area Panoramic Trail.	36.84417000, -84.52833000	395	Ridgeline. Elevation: 1295 feet. Aspect: South.	Wild material		2158713	NA 88621
471	NA 88622	KY23-025b	Ilex ambigua Torr.	Kentucky, United States	NA		2023	COLLECTED	09/10/2023	The Gulf - Natural Arch Scenic Area Panoramic Trail.	36.84417000, -84.52833000	395	Ridgeline. Elevation: 1295 feet. Aspect: South.	Wild material		2158714	NA 88622
472	NA 88640	KY23-043	Ilex verticillata (L.) A. Gray	Kentucky, United States	NA		2023	COLLECTED	09/11/2023	Daniel Boone National Forest: Bee Rock Loop Trail along Rockcastle River.	37.04179000, -84.31805000	233	Riverscour grassland. Elevation: 765 feet. Aspect: East.	Wild material		2158732	NA 88640
473	NA 87339	NA 87339	Ilex pedunculosa Miq.		NA	Not Available	2023							Uncertain improvement status	Presumed spontaneous seedling at the edge of the woodland in bed HM-C, likely from NA 158 [PI 102300] (which was growing very close to this plant for many years), although it could be a resprouting individual of NA 158 itself that was previously undocumented.	2158686	NA 87339
474	NA 87415	NA 87415	Ilex opaca Aiton		NA	Not Available	2023							Uncertain improvement status	Full name as recorded at U.S. National Arboretum: Ilex opaca. Prominent old specimen growing near Springhouse Run in the far eastern edge of the Hillside Nursery. Possibly native, but may have been planted. No records could be found. Form received: unknown propagule type.	2155350	NA 87415
475	NA 87340	(undetermined cultivar)	Ilex opaca Aiton		NA	Not Available	2023							Uncertain improvement status	Full name as recorded at U.S. National Arboretum: Ilex opaca (undetermined cultivar). An attractive, clearly planted American holly (cultivar unknown at this time) growing along the Kingman Lake Overloop on the Anacostia River side without any known documentation. Form received: unknown propagule type.	2155332	NA 87340
476	NA 87338	NA 87338	Ilex purpurea Hassk.		NA	Not Available	2023							Uncertain improvement status	Full name as recorded at U.S. National Arboretum: Ilex purpurea. Seedling (at least several years old) that appeared just north of the Kingman Lake Overlook loop guard rail amid invasive vines and shrubs, near some old Ilex opaca. Probably deposited from seed of NA 42133 from the other side of the collection, or maybe less likely from NA 69765 on the Anacostia River Flood Plain, if it is able to produce viable seed (no males are nearby). Since we have few plants of this taxon and parents are fairly likely to be of wild origin, this might be worth keeping and observing further. -SBL	2155331	NA 87338
477	NA 87334	NA 87334	Ilex pedunculosa Miq.		NA	Not Available	2023							Uncertain improvement status	Full name as recorded at U.S. National Arboretum: Ilex pedunculosa. Large, sparsely fruited (at the time of accessioning), upright-growing female with small fruit on long stalks growing near the southwestern corner of Korean Hillside bed AC-K-01; I suspect that this may have been transplanted from the old Holly Breeding Nursery in 1999 without being properly recorded. If that is the case, it is likely to be one of the following: NA 44884-J, L, or P (all females); NA 44910-H or V (females), or NA 45205-J (a small-fruited female, which this is). All of these were wild-collected, and there is a good chance that this was, too. -SBL Form received: unknown propagule type.	2155329	NA 87334
478	NA 87292	(hybrid selection)	Ilex hybr.		NA	Not Available	2023							Clone	Full name as recorded at U.S. National Arboretum: Ilex (hybrid selection). Mass of some uncertain female hybrid selection (appearing likely to be identical, although it is difficult to be completely sure) growing along the upper Mt Hamilton Trail in Azaleas; they probably represent an existing accession and are clearly hybrids, but little else is known about them at present. The former curator was friends with Gene Eisenbeiss and was given hollies to plant, so this material likely came from him. Shady conditions and inadequate pollination (stemming from isolation) will somewhat complicate attempts to identify these further. They do not appear to exactly match any USNA introductions, but clearly have Ilex aquifolium and eastern Asian background (such as I. cornuta). Form received: rooted cutting.	2155299	NA 87292
479	NA 87165	NA 87165	Ilex opaca Aiton		NA	Not Available	2023							Uncertain improvement status	Full name as recorded at U.S. National Arboretum: Ilex opaca. Two attractive, single-trunked, old specimens of this species growing in bed AC-CA-03 behind the Asian Collections restrooms; they could be cultivars or they could be well-tended natives from the grounds. -SBL Form received: unknown propagule type.	2155203	NA 87165
480	NA 80719	(male)	Ilex verticillata (L.) A. Gray		NA	Not Available	2023							Uncertain improvement status	Full name as recorded at U.S. National Arboretum: Ilex verticillata (male). Old Eisenbeiss map from March of 1965 show several male I. verticillata cultivars in this area; NA 9151, 24792 and one labeled I. verticillata 'Triton' that has no number associated with it. Form received: unknown propagule type.	2152224	NA 80719
481	NA 80718	(male)	Ilex verticillata (L.) A. Gray		NA	Not Available	2023							Uncertain improvement status	Full name as recorded at U.S. National Arboretum: Ilex verticillata (male). Single plant in HM-A10, near drain pipe. Form received: unknown propagule type.	2152223	NA 80718
482	NA 80189	NA 80189	Ilex opaca Aiton		NA	Not Available	2023							Uncertain improvement status	Full name as recorded at U.S. National Arboretum: Ilex opaca. Prior source unknown at this time--Bell number 53661 and location #26 P3 are only clues. -SBL	2152078	NA 80189
483	NA 76317	'William Hawkins'	Ilex opaca Aiton		NA	Not Available	2023							Cultivar	Full name as recorded at U.S. National Arboretum: Ilex opaca 'William Hawkins'.	2150665	NA 76317
484	NA 76096	'Burfordii'	Ilex cornuta Lindl. & Paxton		NA	Not Available	2023							Cultivar	Full name as recorded at U.S. National Arboretum: Ilex cornuta 'Burfordii'. Form received: unknown propagule type.	2150587	NA 76096
485	NA 76027	(undetermined cultivar)	Ilex crenata Thunb.		NA	Not Available	2023							Uncertain improvement status	Full name as recorded at U.S. National Arboretum: Ilex crenata (undetermined cultivar).	2150578	NA 76027
486	NA 74887	NA 74887	Ilex ×koehneana Loes.		NA	Not Available	2023							Uncertain improvement status	Full name as recorded at U.S. National Arboretum: Ilex x koehneana. Looks like latifolia. [Actually, it appears to be I. x koehneana, but does not quite match any cultivars in our collections as of 2025; it could be an unnamed seedling selection, or a cultivar otherwise absent from USNA at this time.]	2150193	NA 74887
487	NA 73322	NA 73322	Ilex opaca Aiton		NA	Not Available	2023							Uncertain improvement status	Full name as recorded at U.S. National Arboretum: Ilex opaca. Old USNA plant. Form received: unknown propagule type.	2149598	NA 73322
488	NA 73320	NA 73320	Ilex sp.		NA	Not Available	2023							Uncertain improvement status	Full name as recorded at U.S. National Arboretum: Ilex sp.. Old USNA plant. Form received: unknown propagule type.	2149596	NA 73320
489	NA 73313	NA 73313	Ilex glabra (L.) A. Gray		NA	Not Available	2023							Uncertain improvement status	Full name as recorded at U.S. National Arboretum: Ilex glabra. Form received: unknown propagule type.	2149590	NA 73313
490	NA 72598	NA 72598	Ilex sp.		NA	Not Available	2023							Uncertain improvement status	Full name as recorded at U.S. National Arboretum: Ilex sp.. Form received: unknown propagule type.	2149338	NA 72598
491	NA 70264	'Steward's Silver Crown'	Ilex opaca Aiton		NA	Not Available	2023							Cultivar	Full name as recorded at U.S. National Arboretum: Ilex opaca 'Steward's Silver Crown'. On Gene K. Eisenbeiss Ilex Inventory July 23, 1984 1 pt. 2 feet tall in greenhouse	2148622	NA 70264
492	NA 55314	'Beehive'	Ilex crenata Thunb.		NA	Not Available	2023							Cultivar	Full name as recorded at U.S. National Arboretum: Ilex crenata 'Beehive'. Holly Soc. Am. Reg. No. 11-84.	2146072	NA 55314
493	NA 32980	NA 32980	Ilex opaca Aiton		NA	Not Available	2023							Uncertain improvement status	Full name as recorded at U.S. National Arboretum: Ilex opaca. Accessioned 11/24/70. Selected from specimen growing across from Perkins-de Wilde Nursery, Shiloh, N.J.	2144342	NA 32980
494	NA 28318	(entire leaf, female)	Ilex cornuta Lindl. & Paxton		NA	Not Available	2023							Clone	Full name as recorded at U.S. National Arboretum: Ilex cornuta (entire leaf, female). Foliage similar to I. cornuta 'Burfordi' (male). Excellent landscape pollinator for I. cornuta specimens. Form received: unknown propagule type.	2144097	NA 28318
495	NA 27235	NA 27235	Ilex vomitoria Aiton		NA	Not Available	2023							Uncertain improvement status	Full name as recorded at U.S. National Arboretum: Ilex vomitoria.	2144058	NA 27235
496	NA 17789	NA 17789	Ilex opaca Aiton		NA	Not Available	2023							Uncertain improvement status	Full name as recorded at U.S. National Arboretum: Ilex opaca.	2143625	NA 17789
497	NA 17770	'Burfordii'	Ilex cornuta Lindl. & Paxton		NA	Not Available	2023							Cultivar	Full name as recorded at U.S. National Arboretum: Ilex cornuta aff. 'Burfordii'. Male clone, similar to 'Burford' in other respects. [This accession had been mistakenly tagged with PI number 3712, but this is not a valid PI number for an Ilex; it appears from the card that it may have been intended as a PO or PQ number instead. Evidently this and the numbers following were renumbered from NA 58, presumably an accession received as seed but with little information remaining. Each individual of former NA 58 received a separate new accession number. -SBL]	2143623	NA 17770
498	NA 7528	NA 7528	Ilex latifolia Thunb.		NA	Not Available	2023							Uncertain improvement status	Full name as recorded at U.S. National Arboretum: Ilex latifolia. Accession numbers assigned and cards made 8/10/55, NA#'s 7519 - 7529 were assigned to the Ilex listing of crosses & misc. old plants found at the arboretum 8/10/55. Form received: unknown propagule type.	2143235	NA 7528
499	NA 7520	'East Palatka'	Ilex ×attenuata Ashe		NA	Not Available	2023							Cultivar	Full name as recorded at U.S. National Arboretum: Ilex x attenuata 'East Palatka'. Accession numbers assigned and cards made 8/10/55, NA#'s 7519 - 7529 were assigned to the Ilex listing of crosses & misc. old plants found at the arboretum 8/10/55. Form received: unknown propagule type.	2143233	NA 7520

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