Citation:

PANGAEA.933148

Name: Description of sampling sites in the NW America region
Published: 2023-05-23
License: https://creativecommons.org/licenses/by/4.0/
Keywords: fossil pollen; Neotoma; paleoecology; taxonomically harmonized

Always quote citation above when using data! You can download the citation in several formats below.

RIS Citation BibTeX Citation Text Citation Facebook TwitterShow Map Google Earth

Keyword(s):

fossil pollen; Neotoma; paleoecology; taxonomically harmonized

Further details:

Pollen taxa harmonisation table

Project(s):

Polar Terrestrial Environmental Systems @ AWI (AWI_Envi)

Coverage:

Median Latitude: 50.418674 * Median Longitude: -124.453395 * South-bound Latitude: 20.794290 * West-bound Longitude: -162.200000 * North-bound Latitude: 73.533333 * East-bound Longitude: -104.938605

Minimum ELEVATION: 0 m a.s.l. * Maximum ELEVATION: 3740 m a.s.l.

Event(s):

ABALONE (Abalone Rocks Marsh) * Latitude: 33.956389 * Longitude: -119.976667 * Location: Western North America

ANDYLAKE (Andy Lake) * Latitude: 64.650000 * Longitude: -128.083333 * Location: North America

ANGAL (Angal Lake) * Latitude: 67.133333 * Longitude: -153.900000 * Location: North America

Parameter(s):

#	Name	Short Name	Unit	Principal Investigator	Comment
1	Event label	Event		Herzschuh, Ulrike
2	Reference/source	Reference		Herzschuh, Ulrike	Event
3	Identification	ID		Herzschuh, Ulrike	Site
4	Identification	ID		Herzschuh, Ulrike	Dataset
5	Site	Site		Herzschuh, Ulrike
6	LONGITUDE	Longitude		Herzschuh, Ulrike	Geocode
7	LATITUDE	Latitude		Herzschuh, Ulrike	Geocode
8	Continent	Cont		Herzschuh, Ulrike
9	ELEVATION	Elevation	m a.s.l.	Herzschuh, Ulrike	Geocode
10	Type	Type		Herzschuh, Ulrike	of data
11	Location type	Loc type		Herzschuh, Ulrike
12	Sample amount	N	#	Herzschuh, Ulrike	Pollen samples in core
13	Reference/source	Reference		Herzschuh, Ulrike	AgeModel
14	Age, minimum/young	Age min	ka	Herzschuh, Ulrike
15	Age, maximum/old	Age max	ka	Herzschuh, Ulrike
16	Description	Description		Herzschuh, Ulrike	Site Description from Neotoma
17	Reference/source	Reference		Herzschuh, Ulrike	Literature source #1
18	Uniform resource locator/link to reference	URL ref		Herzschuh, Ulrike	Literature source #1
19	Reference/source	Reference		Herzschuh, Ulrike	Literature source #2
20	Uniform resource locator/link to reference	URL ref		Herzschuh, Ulrike	Literature source #2
21	Reference/source	Reference		Herzschuh, Ulrike	Literature source #3
22	Uniform resource locator/link to reference	URL ref		Herzschuh, Ulrike	Literature source #3
23	Reference/source	Reference		Herzschuh, Ulrike	Literature source #4
24	Uniform resource locator/link to reference	URL ref		Herzschuh, Ulrike	Literature source #4
25	Reference/source	Reference		Herzschuh, Ulrike	Literature source #5
26	Uniform resource locator/link to reference	URL ref		Herzschuh, Ulrike	Literature source #5

License:

Creative Commons Attribution 4.0 International (CC-BY-4.0)

Status:

Curation Level: Enhanced curation (CurationLevelC)

Size:

5217 data points

Data

Download dataset as tab-delimited text — use the following character encoding:

1 Event	2 Reference (Event)	3 ID (Site)	4 ID (Dataset)	5 Site	6 Longitude	7 Latitude	8 Cont	9 Elevation [m a.s.l.]	10 Type (of data)	11 Loc type	12 N [#] (Pollen samples in core)	13 Reference (AgeModel)	14 Age min [ka]	15 Age max [ka]	16 Description (Site Description from Neotoma)	17 Reference (Literature source #1)	18 URL ref (Literature source #1)	19 Reference (Literature source #2)	20 URL ref (Literature source #2)	21 Reference (Literature source #3)	22 URL ref (Literature source #3)	23 Reference (Literature source #4)	24 URL ref (Literature source #4)	25 Reference (Literature source #5)	26 URL ref (Literature source #5)
ABALONE	Neotoma	8	8	Abalone Rocks Marsh	-119.976667	33.956389	Western North America	0	Raw	Peat	32	AWI	-0.049	5.845	Small estuarine marsh. Physiography: Santa Rosa Island. Surrounding vegetation: coastal marsh and grassland.	Cole, K.L. and Liu, G.W., 1994. Holocene paleoecology of an estuary on Santa Rosa Island, California. Quaternary Research, 41(3), pp.326-335.	https://doi.org/10.1006/qres.1994.1037
ANDYLAKE	Neotoma	206	206	Andy Lake	-128.083333	64.650000	Western North America	1360	Raw	Lake	57	AWI	-0.066	13.049	Lake dammed by a Mountain River moraine. Physiography: Mackenzie Mountains. Surrounding vegetation: shrub tundra.	Szeicz, J.M., MacDonald, G.M. and Duk-Rodkin, A., 1995. Late Quaternary vegetation history of the central Mackenzie Mountains, Northwest Territories, Canada. Palaeogeography, Palaeoclimatology, Palaeoecology, 113(2-4), pp.351-371.	https://doi.org/10.1016/0031-0182(95)00070-3
ANGAL	Neotoma	207	208	Angal Lake	-153.900000	67.133333	Western North America	820	Raw	Lake	37	AWI	-0.051	17.051	Cirque lake. Physiography: mountainous. Surrounding vegetation: Betula shrub tundra.	Brubaker, L.B., Garfinkee, H.L. and Edwards, M.E., 1983. A late Wisconsin and Holocene vegetation history from the central Brooks Range: implications for Alaskan palaeoecology. Quaternary Research, 20(2), pp.194-214.	https://doi.org/10.1016/0033-5894(83)90077-7
ANTELOPE	Neotoma	209	210	Antelope Playa	-105.450000	43.500000	Western North America	1450	Raw	River	25	AWI	-0.054	16.494	Small playa. Physiography: Powder River Basin. Surrounding vegetation: Artemisia tridentata grassland.	Markgraf, V. and Lennon, T., 1986. Paleoenvironmental history of the last 13,000 years of the eastern Powder River Basin, Wyoming, and its implications for prehistoric cultural patterns. Plains Anthropologist, 31(111), pp.1-12.	https://doi.org/10.1080/2052546.1986.11909310
BARRETT	Neotoma	231	234	Barrett Lake	-119.008333	37.595833	Western North America	2816	Raw	Lake	38	AWI	-0.061	15.366	Glacial scour lake. Physiography: Sierra Nevada mountains. Surrounding vegetation: lodgepole/limber pine, mountain hemlock.	Anderson, R.S., 1987. Late-Quaternary environments of the Sierra Nevada, California. Doctoral dissertation. University of Arizona, Tucson, Arizona, USA.		Anderson, R.S., 1990. Holocene forest development and paleoclimates within the central Sierra Nevada, California. Journal of Ecology, 78(2), pp.470-489.	https://doi.org/10.2307/2261125
BATLGRND	Neotoma	236	239	Battle Ground Lake	-122.491667	45.800000	Western North America	155	Raw	Lake	105	AWI	-0.040	24.274	Volcanic crater. Physiography: Puget Trough. Surrounding vegetation: second-growth Pseudotsuga/decid forest.	Barnosky, C.W., 1983. Late-Quaternary vegetational and climatic history of southwestern Washington. Doctoral dissertation. University of Washington, Seattle, Washingtion, USA.		Barnosky, C.W., 1985. Late Quaternary vegetation near Battle Ground Lake, southern Puget Trough, Washington. Geological Society of America Bulletin, 96(2), pp.263-271.	https://doi.org/10.1130/0016-7606(1985)96%3C263:LQVNBG%3E2.0.CO;2	Whitlock, C., 1992. Vegetational and climatic history of the Pacific Northwest during the last 20,000 years: implications for understanding present-day biodiversity. Northwest Environmental Journal, 8, pp.5-28.
BEEFPAST	Neotoma	246	250	Beef Pasture	-108.160375	37.473105	Western North America	3060	Raw	Peat	91	AWI	-0.024	6.033	Open wet meadow and fen occupying a depression formed by a landslide ~5000 BP in the La Plata Mountains. Local upland vegetation dominated by Picea engelmannii, Pseudotsuga menziesii, Populus tremuloides, and Alnus tenuifolia. Salix brachycarpa lines the edges of the wet meadow.	Petersen, K.L., 1988. Climate and the Dolores River Anasazi: a paleoenvironmental reconstruction from a 10,000-year pollen record, La Plata Mountains, Southwestern Colorado. University of Utah, Anthropological Papers 113. University of Utah Pres, Salt Lake City, Utah, USA.		Petersen, K.L., 1985. Palynology in Montezuma County, southwestern Colorado: the local history of the Pinyon Pine (Pinus edulis). In: Late Quaternary Vegetation and Climates in the American Southwest. Contribution Series 16. ed. by B.F. Jacobs, P.L. Fall, and O.K. Davis (pp.47-62). American Association of Stratigraphic Palynologists, Dallas, Texas, USA.		Petersen, K.L., 1994. A warm and wet Little Climatic Optimum and a cold and dry Little Ice Age in the southern Rocky Mountains, USA. Climatic Change, 26(2), pp.243-269.	https://doi.org/10.1007/BF01092417
BELLS	Neotoma	248	253	Bell's Lake	-127.483333	65.016667	Western North America	580	Raw	Lake	53	AWI	-0.057	12.638	Ground moraine depression. Physiography: Mackenzie Mountains. Surrounding vegetation: open Picea muskeg and forest.	Szeicz, J.M., MacDonald, G.M. and Duk-Rodkin, A., 1995. Late Quaternary vegetation history of the central Mackenzie Mountains, Northwest Territories, Canada. Palaeogeography, Palaeoclimatology, Palaeoecology, 113(2-4), pp.351-371.	https://doi.org/10.1016/0031-0182(95)00070-3
BI74MS11	Neotoma	261	267	Banks Island 74MS11	-124.266667	71.750000	Western North America	30	Raw	Lake	55	AWI	-0.050	12.691	Small coastal kettle lake. Physiography: ice-contact sediments, Carpenter Till.	Gajewski, K., Mott, R.J., Ritchie, J.C. and Hadden, K., 2000. Holocene vegetation history of Banks Island, Northwest Territories, Canada. Canadian Journal of Botany, 78(4), pp.430-436.	https://doi.org/10.1139/b00-018
BI74MS12	Neotoma	262	268	Banks Island 74MS12	-119.833333	72.366667	Western North America	220	Raw	Lake	33	AWI	0.257	12.259	Small upland kettle lake. Physiography: morainal deposits of Jesse Till.	Gajewski, K., Mott, R.J., Ritchie, J.C. and Hadden, K., 2000. Holocene vegetation history of Banks Island, Northwest Territories, Canada. Canadian Journal of Botany, 78(4), pp.430-436.	https://doi.org/10.1139/b00-018
BI74MS15	Neotoma	263	269	Banks Island 74MS15	-120.216667	73.533333	Western North America	120	Raw	Lake	62	AWI	0.070	13.085	Small lake in depression in Baker Till. Physiography: morainal deposits of Baker Till.	Gajewski, K., Mott, R.J., Ritchie, J.C. and Hadden, K., 2000. Holocene vegetation history of Banks Island, Northwest Territories, Canada. Canadian Journal of Botany, 78(4), pp.430-436.	https://doi.org/10.1139/b00-018
BLAKTAIL	Neotoma	273	279	Blacktail Pond	-110.600710	44.956110	Western North America	2012	Raw	Lake	56	AWI	-0.022	16.816	Blacktail Pond is situated in a remnant late-Pleistocene meltwater channel; surrounding vegetation is Pseudotsuga menziesii (Douglas-fir) parkland, which includes grassland and steppe communities dominated by Artemisia tridentata (big sagebrush), Festuca idahoensis (Idaho fescue), and Ericameria nauseosa (rabbitbrush).	Gennett, J.A., 1977. Palynology and paleoecology of sediments from Blacktail Pond, northern Yellowstone Park, Wyoming. Master's thesis. University of Iowa, Iowa City, Iowa, USA.		Gennett, J.A. and Baker, R.G., 1986. A late quaternary pollen sequence from blacktail pond, Yellowstone national park, Wyoming, USA. Palynology, 10(1), pp.61-71.	https://doi.org/10.1080/01916122.1986.9989303
BOONE	Neotoma	296	302	Boone Lake	-119.433333	55.575000	Western North America	872	Raw	Lake	72	AWI	-0.025	13.961	Glacial montane lake. Physiography: glaciated mountain foothills. Surrounding vegetation: Picea mariana; Betula glandulosa, Salix.	White, J.M. and Mathewes, R.W., 1986. Postglacial vegetation and climatic change in the upper Peace River district, Alberta. Canadian Journal of Botany, 64(10), pp.2305-2318.	https://doi.org/10.1139/b86-302	White, J.M., Mathewes, R.W. and Mathews, W.H., 1979. Radiocarbon dates from Boone Lake and their relation to the'Ice-free Corridor'in the Peace River District of Alberta, Canada. Canadian Journal of Earth Sciences, 16(9), pp.1870-1874.	https://doi.org/10.1139/e79-171	White, J.M., Mathewes, R.W. and Mathews, W.H., 1985. Late Pleistocene chronology and environment of the \Ice-Free Corridor\ of northwestern Alberta. Quaternary Research, 24(2), pp.173-186.	https://doi.org/10.1016/0033-5894(85)90004-3
BUCKBEAN	Neotoma	311	318	Buckbean Fen	-110.260556	44.298611	Western North America	2362	Raw	Peat	59	AWI	-0.051	13.895	Fen 5 m above Yellowstone Lake. Physiography: within former Yellowstone Lake shorelines. Surrounding vegetation: Pinus contorta forest.	Baker, R.G., 1976. Late Quaternary vegetation history of the Yellowstone Lake basin, Wyoming. United States Geological Survey Professional Paper 729-E.
CANDELAB	Neotoma	329	336	Candelabra Lake	-130.650000	61.683333	Western North America	1040	Raw	Lake	58	AWI	-0.028	11.580	Small lake. Surrounding vegetation: Picea mariana, muskeg.	Cwynar, L.C. and Spear, R., 1995. Paleovegetation and paleoclimatic changes in the Yukon at 6 ka BP. Geographie physique et Quaternaire, 49(1), pp.29-35.	https://doi.org/10.7202/033027ar
CARPLAKE	Neotoma	336	343	Carp Lake	-120.880556	45.918056	Western North America	714	Raw	Lake	88	AWI	-0.051	35.994	Volcanic explosion crater. Physiography: hilly, local relief 100 m. Surrounding vegetation: open ponderosa pine forest.	Barnosky, C.W., 1983. Late-Quaternary vegetational and climatic history of southwestern Washington. Doctoral dissertation. University of Washington, Seattle, Washingtion, USA.		Barnosky, C.W., 1985. Late Quaternary vegetation in the southwestern Columbia basin, Washington. Quaternary Research, 23(1), pp.109-122.	https://doi.org/10.1016/0033-5894(85)90075-4
CIELBLAN	Neotoma	370	381	Lac Ciel Blanc	-122.166667	59.516667	Western North America	651	Raw	Lake	24	AWI	-0.027	13.073	NA	MacDonald, G.M. and Cwynar, L.C., 1985. A fossil pollen based reconstruction of the late Quaternary history of lodgepole pine (Pinus contorta ssp. latifolia) in the western interior of Canada. Canadian Journal of Forest Research, 15(6), pp.1039-1044.	https://doi.org/10.1139/x85-168	MacDonald, G.M. and Cwynar, L.C., 1991. Post-glacial population growth rates of Pinus contorta ssp. latifolia in western Canada. Journal of Ecology, 79(2), pp.417-429.	https://doi.org/10.2307/2260723
CLEARWTR	Neotoma	481	493	Clearwater Lake	-107.933333	50.873611	Western North America	686	Raw	Lake	34	AWI	-0.053	7.350	Closed depression, kettle lake. Physiography: Alberta high plains, moraine, kame. Surrounding vegetation: grassland lake bordered by Populus.	Mott, R.J., 1973. Palynological studies in central Saskatchewan: pollen stratigraphy from lake sediment sequences. Geological Survey of Canada, Ottawa, Ontario, Canada.		Ritchie, J.C., 1976. The late-Quaternary vegetational history of the western interior of Canada. Canadian Journal of Botany, 54(15), pp.1793-1818.	https://doi.org/10.1139/b76-194
COPLEY	Neotoma	494	506	Copley Lake	-107.083090	38.872130	Western North America	3250	Raw	Lake	60	AWI	-0.030	16.972	Montane glacial lake (water 1 m deep). Physiography: flat knoll on mountain slope. Surrounding vegetation: Picea engelmannii - Abies lasiocarpa.	Fall, P.L., 1988. Vegetation dynamics in the southern Rocky Mountains: late Pleistocene and Holocene timberline fluctuations. Doctoral dissertation. University of Arizona, Tucson, Arizona, USA.		Fall, P.L., 1997. Timberline fluctuations and late Quaternary paleoclimates in the Southern Rocky Mountains, Colorado. Geological Society of America Bulletin, 109(10), pp.1306-1320.	https://doi.org/10.1130/0016-7606(1997)109%3C1306:TFALQP%3E2.3.CO;2
COPPER	Neotoma	495	507	Coppermine Saddleback	-115.316667	67.833333	Western North America	43	Raw	Lake	47	AWI	-0.068	4.173	NA	Nichols, H., 1975. Palynological and paleoclimatic study of the late Quaternary displacements of the boreal forest-tundra ecotone in Keewatin and Mackenzie, N.W.T., Canada. Occasional Paper 15. Institute of Arctic and Alpine Research, University of Colorado, Boulder, Colorado, USA.
COTTPASS	Neotoma	501	514	Cottonwood Pass Pond	-106.410840	38.828730	Western North America	3670	Raw	Lake	33	AWI	-0.022	9.442	Alpine pond. Physiography: glaciated mountain pass. Surrounding vegetation: Salix, sedges and grasses.	Fall, P.L., 1988. Vegetation dynamics in the southern Rocky Mountains: late Pleistocene and Holocene timberline fluctuations. Doctoral dissertation. University of Arizona, Tucson, Arizona, USA.		Fall, P.L., 1997. Timberline fluctuations and late Quaternary paleoclimates in the Southern Rocky Mountains, Colorado. Geological Society of America Bulletin, 109(10), pp.1306-1320.	https://doi.org/10.1130/0016-7606(1997)109%3C1306:TFALQP%3E2.3.CO;2
CRANELAK	Neotoma	504	517	Crane Lake	-112.148895	36.529860	Western North America	2590	Raw	Lake	23	AWI	-0.029	13.995	Mature karst doline. Physiography: Kaibab Plateau. Surrounding vegetation: Pinus ponderosa, Pseudotsuga menziesii, with sparse Abies concolor. Picea engelmannii, P, pungens, and Populus tremuloides line the meadow edges.	Shafer, D.S., 1989. The timing of late Quaternary monsoon precipitation maxima in the southwest United States. Doctoral dissertation. University of Arizona, Tucson, Arizona, USA.
CROWFOOT	Neotoma	512	525	Crowfoot Lake	-116.416667	51.650000	Western North America	1940	Raw	Lake	47	AWI	-0.060	13.565	Lake in glacial valley. Physiography: Mountains, outside Crowfoot Moraine. Surrounding vegetation: Picea engelmanii, Abies lasiocarpa.	Osborn, G., Clapperton, C., Davis, P.T., Reasoner, M., Rodbell, D.T., Seltzer, G.O. and Zielinski, G., 1995. Potential glacial evidence for the Younger Dryas event in the cordillera of North and South America. Quaternary Science Reviews, 14(9), pp.823-832.	https://doi.org/10.1016/0277-3791(95)00064-X	Reasoner, M.A., 1996. Late Quaternary alpine and sub-alpine lacustrine records: Canadian and Colorado Rocky Mountains. Doctoral dissertation. University of Alberta, Edmonton, Alberta, Canada.		Reasoner, M.A., Osborn, G. and Rutter, N.W., 1994. Age of the Crowfoot advance in the Canadian Rocky Mountains: A glacial event coeval with the Younger Dryas oscillation. Geology, 22(5), pp.439-442.	https://doi.org/10.1130/0091-7613(1994)022%3C0439:AOTCAI%3E2.3.CO;2
CROWSNES	Neotoma	513	527	Crowsnest Lake	-146.483333	68.333333	Western North America	881	Raw	Lake	67	AWI	0.069	12.594	Morainally dammed lake. Physiography: high mountain valley. Surrounding vegetation: birch shrub tundra.
CUBID	Neotoma	520	534	Cub Lake	-111.183333	44.125000	Western North America	1840	Raw	Lake	26	AWI	-0.063	17.402	Shallow lake. Physiography: west slope Yellowstone Plateau. Surrounding vegetation: lodgepole pine, Douglas fir.	Baker, R.G., 1983. Holocene vegetational history of the western United States. In: Late-Quaternary environments of the United States. Volume 2. the Holocene ed. by Wright Jr, H.E. (pp.109-127). University of Minnesota Press. Minneapolis, USA.		Bender, M.M., Bryson, R.A. and Baerreis, D.A., 1971. University of Wisconsin radiocarbon dates IX. Radiocarbon, 13(2), pp.475-486.	https://doi.org/10.1017/S0033822200008584
CYGNET	Neotoma	528	543	Cygnet Lake Fen	-110.600000	44.650000	Western North America	2530	Raw	Peat	32	AWI	-0.057	18.016	Fen marginal to glacial scour lake. Physiography: Yellowstone Plateau. Surrounding vegetation: Pinus contorta forest.	Whitlock, C., 1993. Postglacial vegetation and climate of Grand Teton and southern Yellowstone National Parks. Ecological Monographs, 63(2), pp.173-198.	https://doi.org/10.2307/2937179	Whitlock, C. and Bartlein, P.J., 1993. Spatial variations of Holocene climatic change in the Yellowstone region. Quaternary Research, 39(2), pp.231-238.	https://doi.org/10.1006/qres.1993.1026
DAVIS_neotoma	Neotoma	534	550	Davis Lake	-122.250000	46.591667	Western North America	282	Raw	Lake	75	AWI	0.037	29.406	Lake. Physiography: Puget Sound lowland. Surrounding vegetation: Psuedotsuga with Tsuga and Thuja.	Barnosky, C.W., 1981. A record of late Quaternary vegetation from Davis Lake, southern Puget Lowland, Washington. Quaternary Research, 16(2), pp.221-239.	https://doi.org/10.1016/0033-5894(81)90046-6
DEAD5826	Neotoma	655	671	Toadlena Lake [Dead Man Lake]	-108.952770	36.237195	Western North America	2759	Raw	Lake	66	AWI	24.497	32.816	Sandstone depression formed by piping. Physiography: crest of the Chuska Mountains. Surrounding vegetation: Pinus ponderosa forest.	Bent, A.M., 1960. Pollen analysis of Deadman Lake, Chuska Mountains, New Mexico. Master's thesis. University of Minnesota, Minneapolis, Minnesota, USA.		Wright Jr, H.E., 1964. Origin of the lakes in the Chuska Mountains, northwestern New Mexico. Geological Society of America Bulletin, 75(7), pp.589-598.	https://doi.org/10.1130/0016-7606(1964)75%5B589:OOTLIT%5D2.0.CO;2	Wright Jr, H.E., Bent, A.M., Spross Hansen, B. and Maher Jr, L.J., 1973. Present and past vegetation of the Chuska Mountains, northwestern New Mexico. Geological Society of America Bulletin, 84(4), pp.1155-1180.	https://doi.org/10.1130/0016-7606(1973)84%3C1155:PAPVOT%3E2.0.CO;2
DEMAIN	Neotoma	660	678	Lac Demain	-118.700000	62.050000	Western North America	745	Raw	Lake	23	AWI	-0.033	14.073	Depression in ground moraine. Physiography: ground moraine. Surrounding vegetation: Picea mariana-Sphagnum muskeg.	MacDonald, G.M., 1984. Postglacial plant migration and vegetation development in the western Canadian boreal forest. Doctoral dissertation. University of Toronto, Toronto, Ontario, Canada.		MacDonald, G.M., 1987. Postglacial vegetation history of the Mackenzie River Basin. Quaternary Research, 28(2), pp.245-262.	https://doi.org/10.1016/0033-5894(87)90063-9
DINKEY	Neotoma	673	693	Dinkey Meadow	-119.083333	37.000000	Western North America	1683	Raw	Meadow	15	AWI	-0.043	5.661	Small clearing along Dinkey Creek. Physiography: Sierra Nevada Mountain Range. Surrounding vegetation: Lodgepole Pine, White Fir, Sugar Pine.	Anderson, R.S., 1987. Late-Quaternary environments of the Sierra Nevada, California. Doctoral dissertation. University of Arizona, Tucson, Arizona, USA.		Davis, O.K. and Moratto, M.J., 1988. Evidence for a warm dry early Holocene in the western Sierra Nevada of California: Pollen and plant macrofossil analysis of Dinkey and Exchequer Meadows. Madrono, 35(2), pp.132-149.
DIVIDE	Neotoma	681	701	Divide Lake	-110.233333	43.933333	Western North America	2628	Raw	Lake	23	AWI	-0.049	14.591	Glacial scour lake. Physiography: Pinyon Peak Highlands. Surrounding vegetation: Picea-Abies-Pinus albicaulis forest.	Steventon, R.L. and Kutzbach, J.E., 1987. University of Wisconsin radiocarbon dates XXIV. Radiocarbon, 29(3), pp.397-415.	https://doi.org/10.1017/S0033822200043794	Steventon, R.L. and Kutzbach, J.E., 1988. University of Wisconsin radiocarbon dates XXV. Radiocarbon, 30(3), pp.367-383.	https://doi.org/10.1017/S0033822200044416	Whitlock, C., 1993. Postglacial vegetation and climate of Grand Teton and southern Yellowstone National Parks. Ecological Monographs, 63(2), pp.173-198.	https://doi.org/10.2307/2937179	Whitlock, C. and Bartlein, P.J., 1993. Spatial variations of Holocene climatic change in the Yellowstone region. Quaternary Research, 39(2), pp.231-238.	https://doi.org/10.1006/qres.1993.1026
DOME	Neotoma	699	719	Dome Creek Meadow	-107.050833	40.024167	Western North America	3165	Raw	Peat	29	AWI	0.065	12.690	Sedge meadow. Physiography: Colorado Front Range. Surrounding vegetation: Spruce/Betula/Salix/Ribes/Rosa/.	Feiler, E.J., Anderson, R.S. and Koehler, P.A., 1997. Late Quaternary Paleoenvironments of the White River Plateau, Colorado, U.S.A. Arctic and Alpine Research, 29(1), pp.53-62.
EAGLENES	Neotoma	759	778	Eaglenest Lake	-112.100000	57.766667	Western North America	725	Raw	Lake	52	AWI	-0.027	14.234	Large, flat-bottomed lake. Physiography: Birch Mountain Upland - rolling moraine. Surrounding vegetation: Picea mariana.	Vance, R.E., 1986. Pollen stratigraphy of Eaglenest Lake, northeastern Alberta. Canadian Journal of Earth Sciences, 23(1), pp.11-20.	https://doi.org/10.1139/e86-002
ELDORA	Neotoma	771	790	Eldora Fen	-105.580000	39.936667	Western North America	2848	Raw	Peat	44	AWI	0.004	8.786	Drained fen. Physiography: Ute Mountains.
EMERALD_neotoma	Neotoma	776	796	Emerald Lake	-110.300000	44.066667	Western North America	2634	Raw	Lake	32	AWI	0.488	14.953	Glacial scour lake. Physiography: Pinyon Peak Highlands. Surrounding vegetation: Picea-Abies-Pinus albicaulis forest.	Steventon, R.L. and Kutzbach, J.E., 1987. University of Wisconsin radiocarbon dates XXIV. Radiocarbon, 29(3), pp.397-415.	https://doi.org/10.1017/S0033822200043794	Steventon, R.L. and Kutzbach, J.E., 1988. University of Wisconsin radiocarbon dates XXV. Radiocarbon, 30(3), pp.367-383.	https://doi.org/10.1017/S0033822200044416	Whitlock, C., 1993. Postglacial vegetation and climate of Grand Teton and southern Yellowstone National Parks. Ecological Monographs, 63(2), pp.173-198.	https://doi.org/10.2307/2937179	Whitlock, C. and Bartlein, P.J., 1993. Spatial variations of Holocene climatic change in the Yellowstone region. Quaternary Research, 39(2), pp.231-238.	https://doi.org/10.1006/qres.1993.1026
ESOOKE	Neotoma	788	808	East Sooke Fen	-123.681667	48.351944	Western North America	155	Raw	Peat	93	AWI	0.180	13.681	Small fen basin. Physiography: rolling hills and flat plains. Surrounding vegetation: fir, cedar, pine, hemlock, alder.	Brown, K.J. and Hebda, R.J., 2002. Origin, development, and dynamics of coastal temperate conifer rainforests of southern Vancouver Island, Canada. Canadian Journal of Forest Research, 32(2), pp.353-372.	https://doi.org/10.1139/x01-197	Brown, K.J. and Hebda, R.J., 2003. Coastal rainforest connections disclosed through a Late Quaternary vegetation, climate, and fire history investigation from the Mountain Hemlock Zone on southern Vancouver Island, British Colombia, Canada. Review of Palaeobotany and Palynology, 123(3-4), pp.247-269.	https://doi.org/10.1016/S0034-6667(02)00195-1
ETIVLIK	Neotoma	790	811	Etivlik Lake	-156.033333	68.133333	Western North America	631	Raw	Lake	23	AWI	0.069	17.146	Morainally dammed lake. Physiography: low rolling hills. Surrounding vegetation: birch shrub tundra.
EXCHEQUE	Neotoma	794	816	Exchequer Meadow	-119.833333	37.000000	Western North America	2219	Raw	Peat	24	AWI	-0.053	15.840	Wet meadow. Physiography: Sierra Nevada Mountains. Surrounding vegetation: Pinus jeffreyi, Abies magnifica.	Davis, O.K. and Moratto, M.J., 1988. Evidence for a warm dry early Holocene in the western Sierra Nevada of California: Pollen and plant macrofossil analysis of Dinkey and Exchequer Meadows. Madrono, 35(2), pp.132-149.
FALLBACK	Neotoma	796	818	Fallback Lake	-110.433333	43.966667	Western North America	2597	Raw	Lake	31	AWI	10.105	19.103	Glacial scour lake. Physiography: Pinyon Peak Highlands. Surrounding vegetation: Picea-Abies-Pinus albicaulis forest.	Steventon, R.L. and Kutzbach, J.E., 1988. University of Wisconsin radiocarbon dates XXV. Radiocarbon, 30(3), pp.367-383.	https://doi.org/10.1017/S0033822200044416	Whitlock, C., 1993. Postglacial vegetation and climate of Grand Teton and southern Yellowstone National Parks. Ecological Monographs, 63(2), pp.173-198.	https://doi.org/10.2307/2937179
FIDDLERS	Neotoma	805	829	Fiddler's Pond	-121.420000	56.250000	Western North America	630	Raw	Lake	45	AWI	-0.032	7.894	Kettle pond. Physiography: glaciated plateau. Surrounding vegetation: Populus, Symphoricarpos; Carex, Rumex.	White, J.M. and Mathewes, R.W., 1982. Holocene vegetation and climatic change in the Peace River district, Canada. Canadian Journal of Earth Sciences, 19(3), pp.555-570.	https://doi.org/10.1139/e82-045
FLOATIL1	Neotoma	811	835	Floating Island Lake	-107.466667	44.550000	Western North America	2609	Raw	Lake	75	AWI	-0.009	10.603	Kettle lake with floating sedge mat. Physiography: Bighorn Mountains. Surrounding vegetation: lodgepole pine forest.	Burkart, M.R., 1976. Pollen biostratigraphy and late Quaternary vegetation history of the Bighorn Mountains, Wyoming. Doctoral dissertation. University of Iowa, Iowa City, Iowa, USA.
FOREST1	Neotoma	816	841	Forest Pond 1	-109.938889	43.471667	Western North America	2797	Raw	Lake	27	AWI	-0.066	9.718	Kettle pond. Physiography: high plateau in Wind River Range. Surrounding vegetation: clearcut in Pinus contorta.	Lynch, E.A., 1995. Origin of a park-forest vegetation mosaic in the Wind River Range, Wyoming. Doctoral dissertation. University of Minnesota, Minneapolis, Minnesota, USA.		Lynch, E.A., 1998. Origin of a park-forest vegetation mosaic in the Wind River Range, Wyoming. Ecology, 79(4), pp.1320-1338.	https://doi.org/10.1890/0012-9658(1998)079%5B1320:OOAPFV%5D2.0.CO;2
FOREST2	Neotoma	817	843	Forest Pond 2	-109.950000	43.438889	Western North America	2766	Raw	Lake	27	AWI	-0.065	9.773	Kettle pond. Physiography: high plateau in Wind River Range. Surrounding vegetation: Pinus contorta forest.	Lynch, E.A., 1995. Origin of a park-forest vegetation mosaic in the Wind River Range, Wyoming. Doctoral dissertation. University of Minnesota, Minneapolis, Minnesota, USA.		Lynch, E.A., 1998. Origin of a park-forest vegetation mosaic in the Wind River Range, Wyoming. Ecology, 79(4), pp.1320-1338.	https://doi.org/10.1890/0012-9658(1998)079%5B1320:OOAPFV%5D2.0.CO;2
FRYINGPN	Neotoma	827	853	Frying Pan Lake	-111.666667	38.616667	Western North America	2720	Raw	Lake	25	AWI	-0.054	10.334	Shallow lake behind Pleistocene moraine. Physiography: horst and graben plateau. Surrounding vegetation: Pinus/Pseudotsuga/Cercocarpus/Populus.	Shafer, D.S., 1989. The timing of late Quaternary monsoon precipitation maxima in the southwest United States. Doctoral dissertation. University of Arizona, Tucson, Arizona, USA.
GOLDLKBG	Neotoma	937	966	Gold Lake Bog	-122.041667	43.650000	Western North America	1465	Raw	Peat	24	AWI	-0.034	10.964	Sphagnum bog with trees and shrubs. Physiography: Cascade Range. Surrounding vegetation: Pseudotsuga/Tsuga mertensiana/Pinus.	Sea, D.S. and Whitlock, C., 1995. Postglacial vegetation and climate of the Cascade Range, central Oregon. Quaternary Research, 43(3), pp.370-381.	https://doi.org/10.1006/qres.1995.1043
HAFICHUK	Neotoma	969	1000	Hafichuk Site	-105.883889	50.320556	Western North America	740	Raw	Lake	34	AWI	11.805	13.476	Ephemeral prairie pothole pond. Physiography: disintegration moraine.	de Vries, B., 1964. An investigation of a late-glacial deposit from the Missouri Coteau in Saskatchewan. Master's thesis. University of Manitoba, Winnipeg, Manitoba, Canada.		Ritchie, J.C. and Vries, B.D., 1964. Contributions to the Holocene paleoecology of westcentral Canada: a late-glacial deposit from the Missouri Coteau. Canadian Journal of Botany, 42(6), pp.677-692.	https://doi.org/10.1139/b64-063
HAIL	Neotoma	970	1001	Hail Lake	-129.016667	60.033333	Western North America	690	Raw	Lake	84	AWI	0.000	11.809	Small lake. Surrounding vegetation: Picea mariana, P. glauca, Pinus contorta.	Cwynar, L. and Spear, R., 1995. Paleovegetation and paleoclimatic changes in the Yukon at 6 ka BP. Geographie physique et Quaternaire, 49(1), pp.29-35.	https://doi.org/10.7202/033027ar
HANGING	Neotoma	972	1003	Hanging Lake	-138.383333	68.383333	Western North America	500	Raw	Lake	133	AWI	-0.067	36.782	Small lake in broad basin. Physiography: undulating tundra surface. Surrounding vegetation: tussock tundra/wet sedge/heath/fellfield.	Cwynar, L.C., 1980. A Late-Quaternary vegetation history from Hanging Lake, northern Yukon. Doctoral dissertation. University of Toronto, Toronto, Ontario, Canada.		Cwynar, L.C., 1982. A Late-Quaternary Vegetation History from Hanging Lake, Northern Yukon. Ecological Monographs, 52(1), pp.1-24.	https://doi.org/10.2307/2937342
HARDING	Neotoma	975	1006	Harding Lake	-146.907500	64.444444	Western North America		Raw	Lake	41	AWI	0.037	24.182	Small lake. Physiography: glacial valley bottom.	Ager, T.A., 1982. Pollen studies of Quaternary-age sediments in the Tanana Valley (Alaska). In: United States Geological Survey in Alaska: Accomplishments during 1980 ed. by W. Conrad (pp.64-67). USGS Circular 844.		Ager, T.A. and Brubaker, L.B., 1985. Quaternary palynology and vegetational history of Alaska. In: Pollen records of late Quaternary North American sediments ed. by V.M. Bryant, Jr. and R.G. Holloway (pp.353-384). American Association of Stragigraphic Palynologists Foundation, Dallas, Texas, USA.		Ager, T.A., 1983. Holocene vegetational history of Alaska. In: Late-Quaternary Environments of the United States. Volume 2. The Holocene ed. by Wright Jr, H.E. (pp.128-141). University of Minnesota Press. Minneapolis, Minnesota, USA.		Nakao, K., La Perriere, J. and Ager, T.A., 1980. Climatic changes in interior Alaska. In: Climatic Changes in Interior Alaska ed. by K. Nakao (pp.16-23). Hokkaido Univesity, Department of Geophysics, Sapporo, Japan.
HAYLAKE	Neotoma	982	1013	Hay Lake	-109.425000	34.000000	Western North America	2780	Raw	Lake	46	AWI	0.019	48.502	Lake on basaltic bedrock. Physiography: White Mountains. Surrounding vegetation: Pinus-Pseudotsuga-Abies-Juniperus.	Jacobs, B.F., 1983. Past vegetation and climate of the Mogollon Rim Area, Arizona. Doctoral dissertation. University of Arizona, Tucson, Arizona, USA.		Jacobs, B.F., 1985. A middle Wisconsin pollen record from Hay Lake, Arizona. Quaternary Research, 24(1), pp.121-130.	https://doi.org/10.1016/0033-5894(85)90088-2
HEADWATR	Neotoma	992	1024	Headwaters Lake	-155.050000	67.933333	Western North America	820	Raw	Lake	30	AWI	-0.069	13.651	Kettle lake. Physiography: mountainous. Surrounding vegetation: birch shrub tundra.	Brubaker, L.B., Garfinkee, H.L. and Edwards, M.E., 1983. A late Wisconsin and Holocene vegetation history from the central Brooks Range: implications for Alaskan palaeoecology. Quaternary Research, 20(2), pp.194-214.
HEDRICK	Neotoma	997	1030	Hedrick Pond	-110.600000	43.750000	Western North America	2073	Raw	Lake	75	AWI	-0.059	20.882	Kettle lake. Physiography: stagnation moraine, Hedrick Pond Advance. Surrounding vegetation: open forest, Pinus contorta, Pseudotsuga.	Steventon, R.L. and Kutzbach, J.E., 1988. University of Wisconsin radiocarbon dates XXV. Radiocarbon, 30(3), pp.367-383.	https://doi.org/10.1017/S0033822200044416	Whitlock, C., 1993. Postglacial vegetation and climate of Grand Teton and southern Yellowstone National Parks. Ecological Monographs, 63(2), pp.173-198.	https://doi.org/10.2307/2937179	Whitlock, C. and Bartlein, P.J., 1993. Spatial variations of Holocene climatic change in the Yellowstone region. Quaternary Research, 39(2), pp.231-238.	https://doi.org/10.1006/qres.1993.1026
HIDDEN	Neotoma	1071	1104	Hidden Lake	-144.658333	63.940000	Western North America		Raw	Lake	33	AWI	-0.019	19.377	Morainally dammed glacial scour lake. Physiography: Kenai mountains. Surrounding vegetation: Picea/Tsuga/Betula/Populus/Alnus/Salix.	Ager, T.A., 1983. Holocene vegetational history of Alaska. In: Late-Quaternary Environments of the United States. Volume 2. The Holocene ed. by Wright Jr, H.E. (pp.128-141). University of Minnesota Press. Minneapolis, Minnesota, USA.		Ager, T.A. and Sims, J.D., 1984. Postglacial pollen and tephra records from lakes in the Cook Inlet region, southern Alaska. In: The United States Geological Survey in Alaska: Accomplishments During 1981 ed. by W.L. Conrad and R.L. Elliot (pp.103-105). U.S. Geological Survey Circular 868.		Ager, T.A. and Brubaker, L.B., 1985. Quaternary palynology and vegetational history of Alaska. In: Pollen records of late Quaternary North American sediments ed. by V.M. Bryant, Jr. and R.G. Holloway (pp.353-384). American Association of Stragigraphic Palynologists Foundation, Dallas, Texas, USA.		Rymer, M.J. and Sims, J.D., 1982. Lake-sediment evidence for the date of deglaciation of the Hidden Lake area, Kenai Peninsula, Alaska. Geology, 10(6), pp.314-316.	https://doi.org/10.1130/0091-7613(1982)10%3C314:LEFTDO%3E2.0.CO;2
HONEYMOO	Neotoma	1074	1107	Honeymoon Pond	-138.400000	64.633333	Western North America	1160	Raw	Lake	71	AWI	-0.025	10.791	Just inside terminal moraines. Physiography: Southern Ogilvie Ranges. Surrounding vegetation: shrub tundra, isolated Picea groves.	Cwynar, L.C. and Spear, R.W., 1991. Reversion of forest to tundra in the central Yukon. Ecology, 72(1), pp.202-212.	https://doi.org/10.2307/1938915
INDIANPF	Neotoma	1114	1148	Indian Prairie Fen	-122.575000	44.633333	Western North America	988	Raw	Peat	50	AWI	0.330	15.822	Fen in cirque valley. Physiography: Cascade Range. Surrounding vegetation: 2nd growth Pseudotsuga and Abies procera.	Sea, D.S. and Whitlock, C., 1995. Postglacial vegetation and climate of the Cascade Range, central Oregon. Quaternary Research, 43(3), pp.370-381.	https://doi.org/10.1006/qres.1995.1043
IRONBOG	Neotoma	1118	1152	Keystone Iron Fen	-107.033333	38.865000	Western North America	2920	Raw	Peat	31	AWI	0.024	9.258	Iron oxide acid fen. Physiography: small basin behind moraine along creek. Surrounding vegetation: Carex, Sphagnum, Eriophorum, Betula glandulosa.	Fall, P.L., 1988. Vegetation dynamics in the southern Rocky Mountains: late Pleistocene and Holocene timberline fluctuations. Doctoral dissertation. University of Arizona, Tucson, Arizona, USA.		Fall, P.L., 1985. Holocene dynamics of the subalpine forest in central Colorado. American Association of Stratigraphic Palynologists Contribution Series, 16, pp.31-46.		Fall, P., 1997. Fire history and composition of the subalpine forest of western Colorado during the Holocene. Journal of Biogeography, 24(3), pp.309-325.	https://doi.org/10.1046/j.1365-2699.1997.00094.x
JACOB	Neotoma	1127	1162	Jacob Lake	-110.833333	34.333333	Western North America	2285	Raw	Lake	20	AWI	-0.022	24.587	Ephemeral lake/sinkhole in sandstone. Physiography: Mogollon Rim. Surrounding vegetation: ponderosa pine forest.	Jacobs, B.F., 1983. Past vegetation and climate of the Mogollon Rim Area, Arizona. Doctoral dissertation. University of Arizona, Tucson, Arizona, USA.
JOELAKE	Neotoma	1355	1390	Joe Lake	-157.216667	66.766667	Western North America	183	Raw	Lake	87	AWI	-0.049	50.044	Lake in glacial outwash. Physiography: rolling uplands. Surrounding vegetation: birch-alder shrub tundra.	Anderson, P.M., 1988. Late Quaternary pollen records from the Kobuk and Noatak River drainages, northwestern Alaska. Quaternary Research, 29(3), pp.263-276.	https://doi.org/10.1016/0033-5894(88)90035-X
KAIYAK	Neotoma	1396	1432	Kaiyak Lake	-161.416667	68.150000	Western North America	190	Raw	Lake	53	AWI	-0.065	43.302	Lake in glacial drift. Physiography: river terrace in broad mountain valley. Surrounding vegetation: birch-alder shrub tundra.	Anderson, P.M., 1985. Late Quaternary vegetational change in the Kotzebue Sound area, northwestern Alaska. Quaternary Research, 24(3), pp.307-321.	https://doi.org/10.1016/0033-5894(85)90053-5
KEELE	Neotoma	1408	1445	Keele Lake	-127.616667	64.166667	Western North America	1150	Raw	Lake	51	AWI	-0.049	13.757	Lake dammed by Mountain River moraine. Physiography: Mackenzie Mountains. Surrounding vegetation: tundra/scattered Picea glauca.	Szeicz, J.M., MacDonald, G.M. and Duk-Rodkin, A., 1995. Late Quaternary vegetation history of the central Mackenzie Mountains, Northwest Territories, Canada. Palaeogeography, Palaeoclimatology, Palaeoecology, 113(2-4), pp.351-371.	https://doi.org/10.1016/0031-0182(95)00070-3
KIRK	Neotoma	1485	1523	Kirk Lake	-121.616667	48.233333	Western North America	190	Raw	Lake	84	AWI	-0.022	14.031	Small lake. Physiography: North Cascade range mountains.	Cwynar, L.C., 1987. Fire and the forest history of the North Cascade Range. Ecology, 68(4), pp.791-802.	https://doi.org/10.2307/1938350
KOLLIOKS	Neotoma	1503	1541	Kollioksak	-156.450000	66.966667	Western North America	213	Raw	Lake	47	AWI	1.662	17.332	Morainally dammed lake. Physiography: mountain valley. Surrounding vegetation: birch shrub tundra/spruce forest.
LATPOND	Neotoma	1571	1617	Lateral Pond	-135.514167	65.942222	Western North America	470	Raw	Lake	105	AWI	-0.026	20.474	Lake between lateral moraine ridges. Physiography: valley moraine in Richardson Mountains. Surrounding vegetation: black Spruce, Sphagnum.	Ritchie, J.C., 1982. The modern and late-Quaternary vegetation of the Doll Creek area, north Yukon, Canada. New Phytologist, 90(3), pp.563-603.		Ritchie, J.C. and Cwynar, L.C., 1982. The Late Quaternary Vegetation of the North Yukon. In: Paleoecology of Beringia ed. by D.M. Hopkins, J.V. Matthews, Jr., C.E. Schweger, and S.B. Young (pp.113-126). Academic Press, New York, USA.
LILYAK	Neotoma	1585	1632	Lily Lake	-135.400000	59.200000	Western North America	230	Raw	Lake	62	AWI	-0.012	12.560	Headwaters lake between two low hills. Physiography: Chilkat Peninsula. Surrounding vegetation: Picea sitchensis, Tsuga heterophylla.	Cwynar, L.C., 1990. A late quaternary vegetation history from Lily Lake, Chilkat Peninsula, southeast Alaska. Canadian Journal of Botany, 68(5), pp.1106-1112.	https://doi.org/10.1139/b90-139
LILYLK	Neotoma	1587	1635	Lily Lake	-110.316667	43.766667	Western North America	2469	Raw	Lake	31	AWI	-0.053	9.224	Kettle Lake with marginal fen. Physiography: stagnation moraine. Surrounding vegetation: Pinus contorta, P. albicaulis, Pic, Abi.	Steventon, R.L. and Kutzbach, J.E., 1988. University of Wisconsin radiocarbon dates XXV. Radiocarbon, 30(3), pp.367-383.	https://doi.org/10.1017/S0033822200044416	Whitlock, C., 1993. Postglacial vegetation and climate of Grand Teton and southern Yellowstone National Parks. Ecological Monographs, 63(2), pp.173-198.	https://doi.org/10.2307/2937179	Whitlock, C. and Bartlein, P.J., 1993. Spatial variations of Holocene climatic change in the Yellowstone region. Quaternary Research, 39(2), pp.231-238.	https://doi.org/10.1006/qres.1993.1026
LILYLKFN	Neotoma	1588	1637	Lily Lake Fen	-110.316667	43.766667	Western North America	2469	Raw	Peat	31	AWI	7.217	15.152	Marginal fen along a kettle lake. Physiography: stagnation moraine. Surrounding vegetation: Pinus contorta, P. albicaulis, Pic, Abi.	Steventon, R.L. and Kutzbach, J.E., 1987. University of Wisconsin radiocarbon dates XXIV. Radiocarbon, 29(3), pp.397-415.	https://doi.org/10.1017/S0033822200043794
LITTLEOR	Neotoma	1592	1642	Little Lake	-123.583975	44.166580	Western North America	217	Raw	Lake	66	AWI	0.211	44.363	Fen margin on landslide dammed lake. Physiography: Coast Range. Surrounding vegetation: second growth Pseudotsuga forest.	Worona, M.A. and Whitlock, C., 1995. Late quaternary vegetation and climate history near Little Lake, central Coast Range, Oregon. Geological Society of America Bulletin, 107(7), pp.867-876.	https://doi.org/10.1130/0016-7606(1995)107%3C0867:LQVACH%3E2.3.CO;2
LOFTY	Neotoma	1605	1656	Lofty Lake	-112.480833	54.725278	Western North America	620	Raw	Lake	62	AWI	-0.016	13.437	Kettle lake. Physiography: gently rolling moraine. Surrounding vegetation: Populus, Betula, Picea, Pinus.	Lichti-Federovich, S., 1970. The pollen stratigraphy of a dated section of Late Pleistocene lake sediment from central Alberta. Canadian Journal of Earth Sciences, 7(3), pp.938-945.	https://doi.org/10.1139/e70-089
LONEFOX	Neotoma	1606	1657	Lone Fox Lake	-119.716667	56.716667	Western North America	1100	Raw	Lake	37	AWI	-0.030	12.259	Lake in ground morainal depression. Physiography: ground moraine in Clear Hills. Surrounding vegetation: Picea mariana, P. glauca, Pinus contorta.	MacDonald, G.M., 1984. Postglacial plant migration and vegetation development in the western Canadian boreal forest. Doctoral dissertation. University of Toronto, Toronto, Ontario, Canada.		MacDonald, G.M., 1987. Postglacial development of the subalpine-boreal transition forest of western Canada. Journal of Ecology, 75, pp.303-320.	https://doi.org/10.2307/2260420	MacDonald, G.M. and Cwynar, L.C., 1985. A fossil pollen based reconstruction of the late Quaternary history of lodgepole pine (Pinus contorta ssp. latifolia) in the western interior of Canada. Canadian Journal of Forest Research, 15(6), pp.1039-1044.	https://doi.org/10.1139/x85-168	MacDonald, G.M. and Cwynar, L.C., 1991. Post-glacial population growth rates of Pinus contorta ssp. latifolia in western Canada. The Journal of Ecology, 79(2), pp.417-429.	https://doi.org/10.2307/2260723
LOSTLKMT	Neotoma	1614	1666	Lost Lake	-110.484340	47.635160	Western North America	1019	Raw	Lake	43	AWI	-0.025	10.579	Lake in abandoned river channel. Physiography: base of Highwood Mountains. Surrounding vegetation: short-grass prairie.	Barnosky, C.W., 1989. Postglacial vegetation and climate in the northwestern Great Plains of Montana. Quaternary Research, 31(1), pp.57-73.	https://doi.org/10.1016/0033-5894(89)90085-9
LOUISEPD	Neotoma	1618	1670	Louise Pond	-131.764345	52.946430	Western North America	650	Raw	Lake	49	AWI	0.012	11.992	Glacial scour lake. Physiography: Queen Charlotte Ranges, Louise Island. Surrounding vegetation: Tsuga mertensiana, Pinus contorta.	Pellatt, M.G. and Mathewes, R.W., 1994. Paleoecology of postglacial tree line fluctuations on the Queen Charlotte Islands, Canada. Ecoscience, 1(1), pp.71-81.	https://doi.org/10.1080/11956860.1994.11682230	Pellatt, M.G. and Mathewes, R.W., 1997. Holocene tree line and climate change on the Queen Charlotte Islands, Canada. Quaternary Research, 48(1), pp.88-99.	https://doi.org/10.1006/qres.1997.1903
MARIA	Neotoma	1648	1704	M Lake	-133.466667	68.266667	Western North America	105	Raw	Lake	71	AWI	-0.030	14.351	Small deep lake in bedrock basin. Physiography: Campbell-Dolomite Uplands.	Ritchie, J.C., 1984. Past and present vegetation of the far northwest of Canada. University of Toronto Press, Toronto, Ontario, Canada.		Ritchie, J.C., 1977. The modern and late Quaternary vegetation of the Campbell-Dolomite uplands, near Inuvik, NWT, Canada. Ecological Monographs, 47(4), pp.401-423.	https://doi.org/10.2307/1942175
MARION	Neotoma	1649	1705	Marion Lake	-122.547222	49.308333	Western North America	305	Raw	Lake	116	AWI	-0.010	14.668	Lake in valley depression. Physiography: hilly and mountainous. Surrounding vegetation: western hemlock forest.	Mathewes, R.W., 1973. A palynological study of postglacial vegetation changes in the University Research Forest, southwestern British Columbia. Canadian Journal of Botany, 51(11), pp.2085-2103.	https://doi.org/10.1139/b73-271	Mathewes, R.W. and Heusser, L.E., 1981. A 12 000 year palynological record of temperature and precipitation trends in southwestern British Columbia. Canadian Journal of Botany, 59(5), pp.707-710.	https://doi.org/10.1139/b81-100
MARIPOSA	Neotoma	1651	1707	Mariposa Lake	-110.233333	44.150000	Western North America	2730	Raw	Lake	34	AWI	-0.062	15.245	Glacial scour lake. Physiography: Pinyon Peak Highlands. Surrounding vegetation: Pinus contorta forest in old burns.	Steventon, R.L. and Kutzbach, J.E., 1987. University of Wisconsin radiocarbon dates XXIV. Radiocarbon, 29(3), pp.397-415.	https://doi.org/10.1017/S0033822200043794	Steventon, R.L. and Kutzbach, J.E., 1988. University of Wisconsin radiocarbon dates XXV. Radiocarbon, 30(3), pp.367-383.	https://doi.org/10.1017/S0033822200044416	Whitlock, C., 1993. Postglacial vegetation and climate of Grand Teton and southern Yellowstone National Parks. Ecological Monographs, 63(2), pp.173-198.	https://doi.org/10.2307/2937179	Whitlock, C. and Bartlein, P.J., 1993. Spatial variations of Holocene climatic change in the Yellowstone region. Quaternary Research, 39(2), pp.231-238.	https://doi.org/10.1006/qres.1993.1026
MCMASTER	Neotoma	1668	1724	McMaster Lake	-110.583333	64.133333	Western North America	480	Raw	Lake	27	AWI	-0.054	7.350	Glacial lake. Physiography: Canadian shield, rolling terrain. Surrounding vegetation: Alnus crispa, Betula glandulosa tundra.	MacDonald, G.M., Edwards, T.W., Moser, K.A., Pienitz, R. and Smol, J.P., 1993. Rapid response of treeline vegetation and lakes to past climate warming. Nature, 361(6409), pp.243-246.	https://doi.org/10.1038/361243a0	Moser, K.A. and MacDonald, G.M., 1990. Holocene vegetation change at treeline north of Yellowknife, Northwest Territories, Canada. Quaternary Research, 34(2), pp.227-239.	https://doi.org/10.1016/0033-5894(90)90033-H
MELEZE	Neotoma	1677	1733	Lac Meleze	-126.116667	65.216667	Western North America	650	Raw	Lake	47	AWI	-0.032	13.206	Small lake, origin uncertain. Physiography: Franklin Mountains. Surrounding vegetation: Picea mariana-Sphagnum muskeg/Larix.	MacDonald, G.M., 1987. Postglacial vegetation history of the Mackenzie River Basin. Quaternary Research, 28(2), pp.245-262.	https://doi.org/10.1016/0033-5894(87)90063-9
MINAKOKO	Neotoma	1699	1755	Minakokosa Lake	-155.033333	66.916667	Western North America	122	Raw	Lake	55	AWI	0.455	22.383	Morainally dammed lake. Physiography: valley bordered by mountains. Surrounding vegetation: spruce forest-shrub tundra.
MOLASBOG	Neotoma	1706	1762	Molas Pass Bog	-107.697500	37.737778	Western North America	3220	Raw	Peat	29	AWI	0.070	10.859	Linear depression of limestone bedrock. Physiography: Animas Valley, San Juan Mountains. Surrounding vegetation: Picea, Abies, and grassland.	Maher Jr, L.J., 1961. Pollen analysis and postglacial vegetation history in the Animas Valley Region, Southern San Juan Mountains, Colorado. Doctoral dissertation. University of Minnesota, Minneapolis, Minnesota, USA.		Bender, M.M., Bryson, R.A. and Baerreis, D.A., 1970. University of Wisconsin radiocarbon dates VII. Radiocarbon, 12(1), pp.335-345.	https://doi.org/10.1017/S0033822200036377	Hubbs, C.L., Bien, G.S. and Suess, H.E., 1963. La Jolla Natural Radiocarbon Measurements III. Radiocarbon, 5, pp.254-272.	https://doi.org/10.1017/S0033822200036882	Maher Jr, L.J., 1963. Pollen analyses of surface materials from the southern San Juan Mountains, Colorado. Geological Society of America Bulletin, 74(12), pp.1485-1503.	https://doi.org/10.1130/0016-7606(1963)74%5B1485:PAOSMF%5D2.0.CO;2	Maher Jr, L.J., 1972. Nomograms for computing 0.95 confidence limits of pollen data. Review of Palaeobotany and Palynology, 13(2), pp.85-93.	https://doi.org/10.1016/0034-6667(72)90038-3
MONTEZUM	Neotoma	1710	1766	Montezuma Well	-111.752250	34.649200	Western North America	1081	Raw	Lake	70	Neotoma_SKOPE	-0.035	12.838	Thermal spring sinkhole, 16 m deep. Surrounding vegetation: desert scrub/semidesert grassland.	Shafer, D.S., 1989. The timing of late Quaternary monsoon precipitation maxima in the southwest United States. Doctoral dissertation. University of Arizona, Tucson, Arizona, USA.		Davis, O.K. and Shafer, D.S., 1992. A Holocene climatic record for the Sonoran Desert from pollen analysis of Montezuma Well, Arizona, USA. Palaeogeography, Palaeoclimatology, Palaeoecology, 92(1-2), pp.107-119.	https://doi.org/10.1016/0031-0182(92)90137-T
MOSQUIT3	Neotoma	1715	1772	Mosquito Lake Bog	-122.117778	48.769167	Western North America	198	Raw	Peat	59	AWI	2.387	17.159	Sphagnum bog. Physiography: Puget Sound Lowland. Surrounding vegetation: western hemlock-douglas fir.	Steventon, R.L. and Kutzbach, J.E., 1986. University of Wisconsin Radiocarbon Dates XXIII. Radiocarbon, 28(3), pp.1206-1223.	https://doi.org/10.1017/S003382220002021X	Hansen, B.S. and Easterbrook, D.J., 1974. Stratigraphy and palynology of late Quaternary sediments in the Puget Lowland, Washington. Geological Society of America Bulletin, 85(4), pp.587-602.	https://doi.org/10.1130/0016-7606(1974)85%3C587:SAPOLQ%3E2.0.CO;2
MUNDAY	Neotoma	1723	1780	Munday Creek	-141.966667	60.033333	Western North America	88	Raw	Peat	111	AWI	-0.027	11.052	Muskeg. Physiography: Coastal mountains. Surrounding vegetation: Picea, Tsuga het, Tsuga mer, Alnus.	Peteet, D.M., 1986. Modern pollen rain and vegetational history of the Malaspina Glacier District, Alaska. Quaternary Research, 25(1), pp.100-120.	https://doi.org/10.1016/0033-5894(86)90047-5
MUSKOX_neotoma	Neotoma	1726	1783	Muskox Lake	-122.666667	71.783333	Western North America	305	Raw	Lake	18	AWI	-0.061	16.078	Depression in morainal deposits. Physiography: morainal deposits of Kellett till.	Gajewski, K., Mott, R.J., Ritchie, J.C. and Hadden, K., 2000. Holocene vegetation history of Banks Island, Northwest Territories, Canada. Canadian Journal of Botany, 78(4), pp.430-436.	https://doi.org/10.1139/b00-018
NATLA_neotoma	Neotoma	1731	1788	Natla Bog	-128.800000	63.016667	Western North America	1380	Raw	Peat	22	AWI	-0.064	10.104	Bog dissected by Natla River. Physiography: intermontane basin. Surrounding vegetation: Betula, Cladonia, Carex, Sphagnum.	MacDonald, G.M., 1983. Holocene vegetation history of the upper Natla River area, Northwest Territories, Canada. Arctic and Alpine Research, 15(2), pp.169-180.	https://doi.org/10.2307/1550919
NILIQ	Neotoma	1748	1806	Niliq Lake	-160.433333	67.866667	Western North America	274	Raw	Lake	42	AWI	1.385	17.029	Lake of unknown origin, glac. topography. Physiography: low rolling hills. Surrounding vegetation: birch-alder shrub tundra.	Anderson, P.M., 1988. Late Quaternary pollen records from the Kobuk and Noatak River drainages, northwestern Alaska. Quaternary Research, 29(3), pp.263-276.	https://doi.org/10.1016/0033-5894(88)90035-X
PARK1	Neotoma	1792	1852	Park Pond 1	-109.959444	43.468056	Western North America	2705	Raw	Lake	23	AWI	0.151	5.173	Kettle pond. Physiography: high plateau in Wind River Range. Surrounding vegetation: Artemisia grassland (Fish Creek Park).	Lynch, E.A., 1995. Origin of a park-forest vegetation mosaic in the Wind River Range, Wyoming. Doctoral dissertation. University of Minnesota, Minneapolis, Minnesota, USA.		Lynch, E.A., 1998. Origin of a park-forest vegetation mosaic in the Wind River Range, Wyoming. Ecology, 79(4), pp.1320-1338.	https://doi.org/10.1890/0012-9658(1998)079%5B1320:OOAPFV%5D2.0.CO;2
PARK2	Neotoma	1793	1854	Park Pond 2	-109.940833	43.450000	Western North America	2714	Raw	Lake	30	AWI	-0.056	12.075	Kettle pond. Physiography: high plateau in Wind River Range. Surrounding vegetation: Artemisia grassland (Fish Creek Park).	Lynch, E.A., 1995. Origin of a park-forest vegetation mosaic in the Wind River Range, Wyoming. Doctoral dissertation. University of Minnesota, Minneapolis, Minnesota, USA.		Lynch, E.A., 1998. Origin of a park-forest vegetation mosaic in the Wind River Range, Wyoming. Ecology, 79(4), pp.1320-1338.	https://doi.org/10.1890/0012-9658(1998)079%5B1320:OOAPFV%5D2.0.CO;2
PARK3	Neotoma	1794	1856	Park Pond 3	-109.920000	43.459167	Western North America	2739	Raw	Lake	36	AWI	0.392	12.328	Kettle pond. Physiography: high plateau in Wind River Range. Surrounding vegetation: Artemisia grassland (Fish Creek Park).	Lynch, E.A., 1995. Origin of a park-forest vegetation mosaic in the Wind River Range, Wyoming. Doctoral dissertation. University of Minnesota, Minneapolis, Minnesota, USA.		Lynch, E.A., 1998. Origin of a park-forest vegetation mosaic in the Wind River Range, Wyoming. Ecology, 79(4), pp.1320-1338.	https://doi.org/10.1890/0012-9658(1998)079%5B1320:OOAPFV%5D2.0.CO;2
PEDPOND	Neotoma	1818	1882	Ped Pond	-142.066667	67.200000	Western North America	211	Raw	Lake	32	AWI	-0.064	14.819	Ancient flood channel. Physiography: river terraces. Surrounding vegetation: spruce forest.	Edwards, M.E. and Brubaker, L.B., 1986. Late quaternary vegetation history of the Fishhook Bend area, Porcupine River, Alaska. Canadian Journal of Earth Sciences, 23(11), pp.1765-1773.	https://doi.org/10.1139/e86-162
PIXIE	Neotoma	1842	1906	Pixie Lake	-124.196667	48.596389	Western North America	70	Raw	Lake	108	AWI	0.019	16.008	Kettle lake. Physiography: San Juan River floodplain. Surrounding vegetation: hemlock, cedar, fir.	Brown, K.J. and Hebda, R.J., 2002. Origin, development, and dynamics of coastal temperate conifer rainforests of southern Vancouver Island, Canada. Canadian Journal of Forest Research, 32(2), pp.353-372.	https://doi.org/10.1139/x01-197	Brown, K.J. and Hebda, R.J., 2003. Coastal rainforest connections disclosed through a Late Quaternary vegetation, climate, and fire history investigation from the Mountain Hemlock Zone on southern Vancouver Island, British Colombia, Canada. Review of Palaeobotany and Palynology, 123(3-4), pp.247-269.	https://doi.org/10.1016/S0034-6667(02)00195-1
PORPHYRY	Neotoma	1899	1964	Porphyry Lake	-123.833333	48.905556	Western North America	1100	Raw	Lake	59	AWI	0.271	15.699	Physiography: Nanaimo Lakes and Highlands region. Surrounding vegetation: shore bog, forests of hemlock and fir.	Brown, K.J. and Hebda, R.J., 2002. Origin, development, and dynamics of coastal temperate conifer rainforests of southern Vancouver Island, Canada. Canadian Journal of Forest Research, 32(2), pp.353-372.	https://doi.org/10.1139/x01-197	Brown, K.J. and Hebda, R.J., 2003. Coastal rainforest connections disclosed through a Late Quaternary vegetation, climate, and fire history investigation from the Mountain Hemlock Zone on southern Vancouver Island, British Colombia, Canada. Review of Palaeobotany and Palynology, 123(3-4), pp.247-269.	https://doi.org/10.1016/S0034-6667(02)00195-1
POSYLAKE	Neotoma	1905	1970	Posy Lake	-111.696035	37.937460	Western North America	2653	Raw	Lake	26	AWI	-0.032	9.109	Small lake on glacial deposits. Physiography: Aquarius plateau. Surrounding vegetation: transition zone between lower elevation pinyon-juniper forest and higher elevation Pinus ponderosa, Pseudotsuga menziesii, Populus tremuloides, and occasional Pinus edulis occur around the lake.	Shafer, D.S., 1989. The timing of late Quaternary monsoon precipitation maxima in the southwest United States. Doctoral dissertation. University of Arizona, Tucson, Arizona, USA.
PUYUK	Neotoma	1920	1987	Puyuk Lake	-162.200000	63.500000	Western North America	15	Raw	Lake	38	AWI	0.033	19.310	Maar crater on volcanic island. Physiography: subdued rounded hills and volcanic cones. Surrounding vegetation: mesic low-shrub tundra.	Ager, T.A., 1980. A 16,000 year pollen record from St. Michael Island, Norton Sound, western Alaska. In: American Quaternary Association, Sixth Biennial Meeting, Abstracts and Program, 18-20 August 1980 (p.3). Institute for Quaternary Studies, University of Maine, Orono, Maine, USA.		Ager, T.A., 1982. Vegetational history of western Alaska during the Wisconsin glacial interval and the Holocene. In: Paleoecology of Beringia ed. by D.M. Hopkins, J.V. Matthews, Jr., C.E. Schweger, and S.B. Young (pp. 75-93). Paleoecology of Beringia. Academic Press, New York, New York, USA.		Ager, T.A. and Bradbury, J.P., 1982. Quaternary history of vegetation and climate of the Yukon Delta-Norton Sound Area. In W.L. Conrad, editor. In: The United States Geological Survey in Alaska: Accomplishments during 1981. U.S. ed. by W.L. Conrad (pp.103-105). Geological Survey Circular 868.		Ager, T.A. and Brubaker, L.B., 1985. Quaternary palynology and vegetational history of Alaska. In: Pollen records of late-Quaternary North American sediments ed. by V.M. Bryant, Jr. and R.G. Holloway (pp.353-384). American Association of Stragigraphic Palynologists Foundation, Dallas, Texas, USA.
QUEENS	Neotoma	1937	2004	Queens Lake	-110.566667	64.116667	Western North America	480	Raw	Lake	33	AWI	-0.060	8.428	Glacial lake. Physiography: Canadian shield, rolling terrain. Surrounding vegetation: Alnus crispa, Betula glandulosa tundra.	MacDonald, G.M., Edwards, T.W., Moser, K.A., Pienitz, R. and Smol, J.P., 1993. Rapid response of treeline vegetation and lakes to past climate warming. Nature, 361(6409), pp.243-246.	https://doi.org/10.1038/361243a0	Moser, K.A. and MacDonald, G.M., 1990. Holocene vegetation change at treeline north of Yellowknife, Northwest Territories, Canada. Quaternary Research, 34(2), pp.227-239.	https://doi.org/10.1016/0033-5894(90)90033-H
RALAKE	Neotoma	1953	2022	Ra Lake	-126.416667	65.233333	Western North America	330	Raw	Lake	13	AWI	-0.034	13.048	Lake in Mackenzie River valley. Physiography: Franklin Mountains. Surrounding vegetation: Populus, Betula, Picea.	MacDonald, G.M., 1984. Postglacial plant migration and vegetation development in the western Canadian boreal forest. Doctoral dissertation. University of Toronto, Toronto, Ontario, Canada.
RANGER	Neotoma	1955	2025	Ranger Lake	-153.650000	67.147222	Western North America	820	Raw	Lake	60	AWI	-0.069	29.992	Cirque lake. Physiography: mountainous. Surrounding vegetation: birch shrub tundra.	Brubaker, L.B., Garfinkee, H.L. and Edwards, M.E., 1983. A late Wisconsin and Holocene vegetation history from the central Brooks Range: implications for Alaskan palaeoecology. Quaternary Research, 20(2), pp.194-214.	https://doi.org/10.1016/0033-5894(83)90077-7
RAPID	Neotoma	1956	2026	Rapid Lake	-109.193889	42.728889	Western North America	3134	Raw	Lake	46	AWI	-0.065	17.411	Subalpine lake w/ inlet and outlet streams. Physiography: glaciated mountains. Surrounding vegetation: Pinus albicaulis, Salix, sedges, grasses.	Fall, P.L., 1988. Vegetation dynamics in the southern Rocky Mountains: late Pleistocene and Holocene timberline fluctuations. Doctoral dissertation. University of Arizona, Tucson, Arizona, USA.		Fall, P.L., Davis, P.T. and Zielinski, G.A., 1995. Late quaternary vegetation and climate of the Wind River Range, Wyoming. Quaternary Research, 43(3), pp.393-404.	https://doi.org/10.1006/qres.1995.1045	Zielinski, G.A. and Thompson Davis, P., 1987. Late Pleistocene age of the type Temple Lake moraine, Wind River Range, Wyoming, USA. Geographie physique et Quaternaire, 41(3), pp.397-401.	https://doi.org/10.7202/032695ar
REBEL	Neotoma	1973	2045	Rebel Lake	-149.800000	67.416667	Western North America	914	Raw	Lake	45	AWI	-0.067	16.812	Kettle lake. Physiography: mountainous. Surrounding vegetation: birch-heath tundra.	Ager, T.A. and Brubaker, L.B., 1985. Quaternary palynology and vegetational history of Alaska. In: Pollen records of late-Quaternary North American sediments ed. by V.M. Bryant, Jr. and R.G. Holloway (pp.353-384). American Association of Stragigraphic Palynologists Foundation, Dallas, Texas, USA.		Edwards, M.E., Anderson, P.M., Garfinkel, H.L. and Brubaker, L.B., 1985. Late Wisconsin and Holocene vegetational history of the upper Koyukuk region, Brooks Range, Alaska. Canadian Journal of Botany, 63(3), pp.616-626.	https://doi.org/10.1139/b85-077
REDONDO	Neotoma	1974	2047	Redondo Lake	-155.033333	67.683333	Western North America	460	Raw	Lake	25	AWI	-0.064	6.723	Kettle lake. Physiography: mountain valley. Surrounding vegetation: birch tundra, alder thickets, spruce.	Brubaker, L.B., Garfinkee, H.L. and Edwards, M.E., 1983. A late Wisconsin and Holocene vegetation history from the central Brooks Range: implications for Alaskan palaeoecology. Quaternary Research, 20(2), pp.194-214.	https://doi.org/10.1016/0033-5894(83)90077-7
REDROCK	Neotoma	1976	2049	Redrock Lake	-105.541667	40.083333	Western North America	3095	Raw	Lake	41	AWI	-0.012	11.554	Depression in moraine (Mid Pindale age). Physiography: low morainic ridges in Front Range. Surrounding vegetation: Pinus, Populus, Juniperus, Ericaceae.	Maher Jr, L.J., 1973. Pollen evidence suggests that climatic changes in the Colorado Rockies during the last 5000 years were out of phase with those in the northeastern United States. In: Abstracts, Ninth Congress International Union for Quaternary Research, 2-10 December 1973, Christchurch, New Zealand (pp. 227-228).		Maher Jr, L.J., 1972. Absolute pollen diagram of Redrock Lake, Boulder County, Colorado. Quaternary Research, 2(4), pp.531-553.	https://doi.org/10.1016/0033-5894(72)90090-7
REDSTONE	Neotoma	1977	2050	Redstone Lake	-152.600000	67.250000	Western North America	914	Raw	Lake	50	AWI	-0.064	16.248	Cirque lake. Physiography: mountanous. Surrounding vegetation: birch shrub tundra.	Edwards, M.E., Anderson, P.M., Garfinkel, H.L. and Brubaker, L.B., 1985. Late Wisconsin and Holocene vegetational history of the upper Koyukuk region, Brooks Range, Alaska. Canadian Journal of Botany, 63(3), pp.616-626.	https://doi.org/10.1139/b85-077
REINDEER	Neotoma	1980	2054	Reindeer Lake	-132.166667	69.116667	Western North America		Raw	Lake	29	AWI	-0.052	18.693	Lake of glacial origin. Surrounding vegetation: dwarf Betula, Ericaceae, Salix, Alnus.	Spear, R.W., 1993. The palynological record of Late-Quaternary arctic tree-line in northwest Canada. Review of Palaeobotany and Palynology, 79(1-2), pp.99-111.	https://doi.org/10.1016/0034-6667(93)90040-2
RUPPERT	Neotoma	2232	2311	Ruppert Lake	-154.233333	67.066667	Western North America	210	Raw	Lake	55	AWI	0.566	15.533	Kettle lake on terminal moraine. Physiography: base of mountains. Surrounding vegetation: black spruce forest.	Brubaker, L.B., Garfinkee, H.L. and Edwards, M.E., 1983. A late Wisconsin and Holocene vegetation history from the central Brooks Range: implications for Alaskan palaeoecology. Quaternary Research, 20(2), pp.194-214.	https://doi.org/10.1016/0033-5894(83)90077-7
SAKANA	Neotoma	2245	2324	Sakana Lake	-147.850000	67.433333	Western North America	640	Raw	Lake	20	AWI	0.199	15.559	Kettle lake. Physiography: mountainous. Surrounding vegetation: open black spruce forest.
SANJOAQ	Neotoma	2258	2338	San Joaquin Marsh	-117.858333	33.658333	Western North America	2	Raw	Peat	47	AWI	-0.055	8.073	Salt marsh. Physiography: coastal. Surrounding vegetation: salt marsh, urban.	Davis, O.K., 1992. Rapid climatic change in coastal southern California inferred from pollen analysis of San Joaquin Marsh. Quaternary Research, 37(1), pp.89-100.	https://doi.org/10.1016/0033-5894(92)90008-7
SAPAUG	Neotoma	2260	2340	San Agustin Plains	-108.250000	33.866667	Western North America	2069	Raw	Lake	16	AWI	18.536	26.304	Playa lake. Physiography: Datil-Mogollon volcanic plateau. Surrounding vegetation: pinyon-juniper woodland.	Markgraf, V., Bradbury, J.P., Forester, R.M., Singh, G. and Sternberg, R.S., 1984. San Agustin Plains, New Mexico: age and paleoenvironmental potential reassessed. Quaternary Research, 22(3), pp.336-343.	https://doi.org/10.1016/0033-5894(84)90027-9
SC1POND	Neotoma	2268	2348	SC1 Pond	-131.906667	54.416667	Western North America	550	Raw	Lake	19	AWI	0.042	8.005	Small subalpine lake. Physiography: San Christoval Range, Moresby Island. Surrounding vegetation: Ts mert, Chamae noot, Pinus contorta.	Pellatt, M.G. and Mathewes, R.W., 1997. Holocene tree line and climate change on the Queen Charlotte Islands, Canada. Quaternary Research, 48(1), pp.88-99.	https://doi.org/10.1006/qres.1997.1903
SCREAMIN	Neotoma	2270	2351	Screaming Yellowlegs Pond	-151.416667	67.583333	Western North America	650	Raw	Lake	37	AWI	-0.068	17.744	Kettle lake. Physiography: mountainous. Surrounding vegetation: black spruce muskeg.	Edwards, M.E., Anderson, P.M., Garfinkel, H.L. and Brubaker, L.B., 1985. Late Wisconsin and Holocene vegetational history of the upper Koyukuk region, Brooks Range, Alaska. Canadian Journal of Botany, 63(3), pp.616-626.	https://doi.org/10.1139/b85-077
SEAGULL	Neotoma	2271	2352	Seagull Lake	-145.216667	68.266667	Western North America	637	Raw	Lake	36	AWI	0.074	16.174	Kettle lake. Physiography: low mountains. Surrounding vegetation: birch tundra, white spruce stands.
SHERD	Neotoma	2299	2381	Sherd Lake	-107.012370	44.269700	Western North America	2665	Raw	Lake	58	AWI	-0.051	15.914	Moraine dammed lake. Physiography: Bighorn Mountains. Surrounding vegetation: lodgepole pine forest.	Burkart, M.R., 1976. Pollen biostratigraphy and late Quaternary vegetation history of the Bighorn Mountains, Wyoming. Doctoral dissertation. University of Iowa, Iowa City, Iowa, USA.
SLEET	Neotoma	2392	2476	Sleet Lake	-133.583333	69.283333	Western North America		Raw	Lake	78	AWI	-0.051	14.959	Glacial origin lake. Physiography: rolling hills on Tuktoyaktuk Pininsula. Surrounding vegetation: dwarf Betula, Ericaceae, Salix.	Spear, R.W., 1983. Paleoecological approaches to a study of tree line fluctuation in the Mackenzie Delta Region, Northwest Territories: preliminary results. Nordicana, 47, pp.61-72.		Spear, R.W., 1993. The palynological record of Late-Quaternary arctic tree-line in northwest Canada. Review of Palaeobotany and Palynology, 79(1-2), pp.99-111.	https://doi.org/10.1016/0034-6667(93)90040-2
SLOUGHCK	Neotoma	2492	2576	Slough Creek Pond	-110.350000	44.933333	Western North America	1884	Raw	Lake	49	AWI	-0.043	15.247	Kettle lake. Physiography: Lamar River Valley, mountainous. Surrounding vegetation: Pseudotsuga parkland.	Whitlock, C. and Bartlein, P.J., 1993. Spatial variations of Holocene climatic change in the Yellowstone region. Quaternary Research, 39(2), pp.231-238.	https://doi.org/10.1006/qres.1993.1026
SNOWSHOE	Neotoma	2496	2580	Snowshoe Lake	-120.666667	57.450000	Western North America	900	Raw	Lake	28	AWI	-0.029	12.720	Lake among oriented glacial features. Physiography: Milligan Hills, rolling uplands. Surrounding vegetation: Picea glauca, P. mariana, Pinus contorta.	MacDonald, G.M., 1984. Postglacial plant migration and vegetation development in the western Canadian boreal forest. Doctoral dissertation. University of Toronto, Toronto, Ontario, Canada.		MacDonald, G.M., 1987. Postglacial development of the subalpine-boreal transition forest of western Canada. Journal of Ecology, 75(2), pp.303-320.	https://doi.org/10.2307/2260420	MacDonald, G.M. and Cwynar, L.C., 1985. A fossil pollen based reconstruction of the late Quaternary history of lodgepole pine (Pinus contorta ssp. latifolia) in the western interior of Canada. Canadian Journal of Forest Research, 15(6), pp.1039-1044.	https://doi.org/10.1139/x85-168	MacDonald, G.M. and Cwynar, L.C., 1991. Post-glacial population growth rates of Pinus contorta ssp. latifolia in western Canada. Journal of Ecology, 79(2), pp.417-429.	https://doi.org/10.2307/2260723
SPLAINSG	Neotoma	2503	2587	Splains Gulch	-107.068889	38.832778	Western North America	3150	Raw	Peat	19	AWI	3.401	16.623	Sedge peat fen bisected by small stream. Physiography: small basin in glaciated mountains. Surrounding vegetation: Picea engelmannii-Abies lasiocarpa.	Fall, P.L., 1988. Vegetation dynamics in the southern Rocky Mountains: late Pleistocene and Holocene timberline fluctuations. Doctoral dissertation. University of Arizona, Tucson, Arizona, USA.		Fall, P.L., 1997. Timberline fluctuations and late Quaternary paleoclimates in the Southern Rocky Mountains, Colorado. Geological Society of America Bulletin, 109(10), pp.1306-1320.	https://doi.org/10.1130/0016-7606(1997)109%3C1306:TFALQP%3E2.3.CO;2
SPLAINSL	Neotoma	2504	2588	Splains Lake	-107.078195	38.831640	Western North America	3165	Raw	Lake	30	AWI	-0.027	18.700	Montane glacial lake (water 1.7 m deep). Physiography: small basin in glaciated mountains. Surrounding vegetation: Picea engelmannii-Abies lasiocarpa.	Fall, P.L., 1988. Vegetation dynamics in the southern Rocky Mountains: late Pleistocene and Holocene timberline fluctuations. Doctoral dissertation. University of Arizona, Tucson, Arizona, USA.		Fall, P.L., 1997. Timberline fluctuations and late Quaternary paleoclimates in the Southern Rocky Mountains, Colorado. Geological Society of America Bulletin, 109(10), pp.1306-1320.	https://doi.org/10.1130/0016-7606(1997)109%3C1306:TFALQP%3E2.3.CO;2
SPRINGBC	Neotoma	2506	2590	Spring Lake	-119.583333	55.511389	Western North America	835	Raw	Lake	44	AWI	0.000	14.534	Glacial montane lake. Physiography: glaciated mountain foothills. Surrounding vegetation: Populus,Pinus,Picea;Salix,Betula glndlsa.	White, J.M. and Mathewes, R.W., 1986. Postglacial vegetation and climatic change in the upper Peace River district, Alberta. Canadian Journal of Botany, 64(10), pp.2305-2318.	https://doi.org/10.1139/b86-302	White, J.M., Mathewes, R.W. and Mathews, W.H., 1985. Late Pleistocene chronology and environment of the \Ice-Free Corridor\ of northwestern Alberta. Quaternary Research, 24(2), pp.173-186.	https://doi.org/10.1016/0033-5894(85)90004-3
SULPHUR	Neotoma	2522	2611	Sulphur Lake	-137.957778	60.950000	Western North America	847	Raw	Lake	92	AWI	-0.054	13.515	Large two basined lake. Physiography: Shakwak Trench b Kluane Hills/Ruby Range. Surrounding vegetation: Picea glauca dominated forest.	Lacourse, T. and Gajewski, K., 2000. Late Quaternary vegetation history of Sulphur Lake, southwest Yukon Territory, Canada. Arctic, 53(1), pp.27-35.		Lacourse, T., 1998. Late Quaternary vegetation history of Sulphur Lake, southwest Yukon Territory, Canada. Master's thesis. University of Ottawa, Ottawa, Ontario, Canada.
SURPRISE	Neotoma	2526	2615	Surprise Lake	-122.562125	49.319690	Western North America	540	Raw	Lake	67	AWI	0.040	13.202	Small, boggy pond. Physiography: hilly to mountainous. Surrounding vegetation: western hemlock/red cedar/ericaceous shb.	Mathewes, R.W., 1973. A palynological study of postglacial vegetation changes in the University Research Forest, southwestern British Columbia. Canadian Journal of Botany, 51(11), pp.2085-2103.	https://doi.org/10.1139/b73-271
SWAMPLK	Neotoma	2529	2619	Swamp Lake	-119.816667	37.950000	Western North America	1554	Raw	Lake	60	AWI	-0.014	18.238	Small lake. Physiography: Sierra Nevada Mountain Range. Surrounding vegetation: Pinus ponderosa, Pinus jeffreyi.	Smith, S.J., 1989. Pollen and microscopic charcoal analysis of a sediment core from Swamp Lake, Yosemite National Park, California. Doctoral dissertation. Northern Arizona University, Flagstaff, Arizona, U.S.A.		Smith, S.J. and Anderson, R.S., 1992. Late Wisconsin paleoecologic record from Swamp Lake, Yosemite National Park, California. Quaternary Research, 38(1), pp.91-102.	https://doi.org/10.1016/0033-5894(92)90032-E
SWEETLIT	Neotoma	2532	2622	Sweet Little Lake	-132.016667	67.650000	Western North America		Raw	Lake	67	AWI	-0.052	11.864	Small lake. Physiography: rolling hummocky complex of kame and kettl. Surrounding vegetation: Picea/Betula/Salix/Alnus.	Ritchie, J.C., 1984. A Holocene pollen record of boreal forest history from the Travaillant Lake area, Lower Mackenzie River Basin. Canadian Journal of Botany, 62(7), pp.1385-1392.	https://doi.org/10.1139/b84-188
TANGLE	Neotoma	2535	2625	Tangle Lakes	-146.063333	63.029444	Western North America		Raw	Lake	27	AWI	0.168	5.320	Small lake. Physiography: Gulkana Upland. Surrounding vegetation: Betula/Ericales/Spirea/Picea/Populus.	Ager, T.A. and Sims, J.D., 1981. Holocene pollen and sediment record from the Tangle Lakes area, central Alaska. Palynology, 5(1), pp.85-98.	https://doi.org/10.1080/01916122.1981.9989220	Schweger, C.E., 1981. Chronology of late glacial events from the Tangle Lakes, Alaska Range, Alaska. Arctic Anthropology, 18, pp.97-101.		Ager, T.A. and Brubaker, L., 1985. Quaternary palynology and vegetational history of Alaska. In: Pollen records of late-Quaternary North American sediments ed. by V.M. Bryant Jr. and R.G. Holloway (pp.353-384). American Association of Stragigraphic Palynologists Foundation, Dallas, Texas, USA.
TAYLOR	Neotoma	2541	2631	Taylor Lake	-123.906667	46.100556	Western North America	4	Raw	Lake	35	AWI	-0.061	4.705	Dune dammed lake. Physiography: Clatsop Plain. Surrounding vegetation: conifers, understory ferns/berries.	Long, C.J. and Whitlock, C., 2002. Fire and vegetation history from the coastal rain forest of the western Oregon Coast Range. Quaternary Research, 58(3), pp.215-225.	https://doi.org/10.1006/qres.2002.2378
TENMILE	Neotoma	2547	2637	Ten Mile Lake	-145.700000	63.066667	Western North America	1000	Raw	Lake	37	AWI	-0.068	13.825	Lake in glacial outwash. Physiography: rolling hills to south of Alaska Range. Surrounding vegetation: birch-willow shrub tundra.	Anderson, P.M., Lozhkin, A.V., Eisner, W.R., Hopkins, D.M., Brubaker, L.B. and Colinvaux, P.A., 1994. Pollen records from ten mile and Wonder Lake, Alaska. Geographie Physique et Quaternaire, 48(2), pp.131-141.
TIINKDHU	Neotoma	2551	2642	Tiinkdhul Lake	-143.150000	66.583333	Western North America	189	Raw	Lake	56	AWI	0.001	22.008	Maar lake. Physiography: rolling hills of uplands. Surrounding vegetation: spruce forest.	Anderson, P.M., Reanier, R.E. and Brubaker, L.B., 1988. Late Quaternary vegetational history of the Black River region in northeastern Alaska. Canadian Journal of Earth Sciences, 25(1), pp.84-94.	https://doi.org/10.1139/e88-009
TIOGA	Neotoma	2553	2644	Tioga Pass Pond	-119.258333	37.908333	Western North America	3018	Raw	Lake	34	AWI	-0.050	10.497	Kettle pond. Physiography: Sierra Nevada mountains. Surrounding vegetation: Pinus contorta, P. albicaulis.	Anderson, R.S., 1987. Late-Quaternary environments of the Sierra Nevada, California. Doctoral dissertation. University of Arizona, Tucson, Arizona, USA.		Anderson, R.S., 1990. Holocene forest development and paleoclimates within the central Sierra Nevada, California. Journal of Ecology, 78, pp.470-489.	https://doi.org/10.2307/2261125
TLANDING	Neotoma	2555	2646	Thompson Landing	-110.791667	63.066667	Western North America	180	Raw	Peat	65	AWI	3.058	7.062	Peat cliff on edge of unnamed lake. Physiography: low relief. Surrounding vegetation: tundra.	Nichols, H., 1975. Palynological and paleoclimatic study of the late Quaternary displacements of the boreal forest-tundra ecotone in Keewatin and Mackenzie, N.W.T., Canada. Occasional Paper 15. Institute of Arctic and Alpine Research, University of Colorado, Boulder, Colorado, USA.
TOBOGGAN	Neotoma	2556	2647	Toboggan Lake	-114.599460	50.815305	Western North America	1480	Raw	Lake	54	AWI	-0.034	11.401	Kettle lake in glacio-fluvial gravels. Physiography: Rocky Mountain foothills. Surrounding vegetation: Picea glauca, Pinus contorta, Populus tremuloides.	MacDonald, G.M., 1989. Postglacial palaeoecology of the subalpine forest-grassland ecotone of southwestern Alberta: New insights on vegetation and climate change in the Canadian Rocky Mountains and adjacent foothills. Palaeogeography, Palaeoclimatology, Palaeoecology, 73(3-4), pp.155-173.	https://doi.org/10.1016/0031-0182(89)90001-1	MacDonald, G.M., Beukens, R.P. and Kieser, W.E., 1991. Radiocarbon dating of limnic sediments: a comparative analysis and discussion. Ecology, 72(3), pp.1150-1155.	https://doi.org/10.2307/1940612	MacDonald, G.M., Beukens, R.P., Kieser, W.E. and Vitt, D.H., 1987. Comparative radiocarbon dating of terrestrial plant macrofossils and aquatic moss from the \ice-free corridor\ of western Canada. Geology, 15(9), pp.837-840.	https://doi.org/10.1130/0091-7613(1987)15%3C837:CRDOTP%3E2.0.CO;2
TONQUIN	Neotoma	2561	2652	Tonquin Creek	-118.366667	52.733333	Western North America	1935	Raw	Peat	25	AWI	0.306	11.550	Small depression. Physiography: rugged valley with kame and esker features. Surrounding vegetation: Picea Abies.	Kearney, M.S., 1981. Late Quaternary vegetational and environmental history of Jasper National Park, Alberta. Doctoral dissertation. University of Western Ontario, London, Ontario, Canada.		Kearney, M.S. and Luckman, B.H., 1983. Postglacial vegetational history of Tonquin Pass, British Columbia. Canadian Journal of Earth Sciences, 20(5), pp.776-786.	https://doi.org/10.1139/e83-069	Luckman, B.H., Kearney, M.S., King, R.H. and Beaudoin, A.B., 1986. Revised 14C age for St. Helens Y tephra at Tonquin Pass, British Columbia. Canadian Journal of Earth Sciences, 23(5), pp.734-736.	https://doi.org/10.1139/e86-072
TUK5	Neotoma	2569	2661	Tuktoyaktuk 5	-133.450000	69.050000	Western North America	60	Raw	Lake	51	AWI	-0.018	16.854	Kettle lake. Physiography: rolling morainic terrain.	Ritchie, J.C. and Hare, F.K., 1971. Late-Quaternary vegetation and climate near the arctic tree line of northwestern North America. Quaternary Research, 1(3), pp.331-342.	https://doi.org/10.1016/0033-5894(71)90069-X
TWINLAKE	Neotoma	2785	2880	Twin Lakes	-108.102560	37.469060	Western North America	3290	Raw	Lake	93	AWI	-0.016	11.252	Depression in headward end of landslide. Physiography: La Plata Mountains. Surrounding vegetation: engelmann spruce/subalpine fir.	Petersen, K.L., Clay, V.L., Matthews, M.H. and Neusius, S.W., 1985. Dolores Archaeological Program: Studies in Environmental Archaeology. U.S. Department of the Interior, Bureau of Reclamation, Engineering and Research Center, Denver, Colorado, USA.		Petersen, K.L., 1994. A warm and wet little climatic optimum and a cold and dry little ice age in the southern rocky mountains, U.S.A. Climatic Change, 26(2), pp.243-269.	https://doi.org/10.1007/BF01092417	Petersen, K.L. and Mehringer Jr, P.J., 1976. Postglacial timberline fluctuations, La Plata Mountains, southwestern Colorado. Arctic and Alpine Research, 8(3), pp.275-288.	https://doi.org/10.2307/1550475
TYRRELL	Neotoma	2787	2882	Tyrrell Lake	-135.655556	66.050000	Western North America	660	Raw	Lake	20	AWI	-0.024	13.500	Lk in ungl.val lateral to central gl.val. Physiography: Richardson Mountains. Surrounding vegetation: spruce forest, shrub-birch tundra.	Ritchie, J.C., 1982. The modern and late-Quaternary vegetation of the Doll Creek area, north Yukon, Canada. New Phytologist, 90, pp.563-603.
WALKER	Neotoma	2825	2922	Walker Lake	-124.002222	48.529167	Western North America	950	Raw	Lake	53	AWI	0.035	14.858	Physiography: San Juan Ridge, S. Vancouver Is. Ranges. Surrounding vegetation: sedges, hemlock, fir, cedar.	Brown, K.J. and Hebda, R.J., 2002. Origin, development, and dynamics of coastal temperate conifer rainforests of southern Vancouver Island, Canada. Canadian Journal of Forest Research, 32(2), pp.353-372.	https://doi.org/10.1139/x01-197	Brown, K.J. and Hebda, R.J., 2003. Coastal rainforest connections disclosed through a Late Quaternary vegetation, climate, and fire history investigation from the Mountain Hemlock Zone on southern Vancouver Island, British Colombia, Canada. Review of Palaeobotany and Palynology, 123(3-4), pp.247-269.	https://doi.org/10.1016/S0034-6667(02)00195-1
WATCHTWR	Neotoma	2828	2925	Watchtower Basin	-117.083333	52.783333	Western North America		Raw	Peat	35	AWI	-0.050	9.336	Small bog in bedrock depression. Physiography: Maligne range Rocky Mountains. Surrounding vegetation: Abies/Picea/Salix/Potentilla.	Kearney, M.S., 1981. Late Quaternary vegetational and environmental history of Jasper National Park, Alberta. Doctoral dissertation. University of Western Ontario, London, Ontario, Canada.		Kearney, M.S. and Luckman, B.H., 1983. Holocene timberline fluctuations in Jasper National Park, Alberta. Science, 221(4607), pp.261-263.	https://doi.org/10.1126/science.221.4607.261	Luckman, B.H. and Kearney, M.S., 1986. Reconstruction of Holocene changes in alpine vegetation and climate in the Maligne Range, Jasper National Park, Alberta. Quaternary Research, 26(2), pp.244-261.	https://doi.org/10.1016/0033-5894(86)90108-0
WHYAC	Neotoma	2856	2953	Whyac Lake	-124.844444	48.672222	Western North America	15	Raw	Lake	45	AWI	0.243	16.944	Kettle lake. Physiography: glacially scoured landscape. Surrounding vegetation: hemlock, cedar, spruce, myrica, bog.	Brown, K.J. and Hebda, R.J., 2002. Origin, development, and dynamics of coastal temperate conifer rainforests of southern Vancouver Island, Canada. Canadian Journal of Forest Research, 32(2), pp.353-372.	https://doi.org/10.1139/x01-197
WIENLAKE	Neotoma	2857	2954	Wien Lake	-151.266667	64.333333	Western North America	305	Raw	Lake	43	AWI	-0.061	14.423	Lake of unknown origin. Physiography: gentlly rolling hills. Surrounding vegetation: spruce forest.	Hu, F.S., Brubaker, L.B. and Anderson, P.M., 1993. A 12 000 year record of vegetation change and soil development from Wien Lake, central Alaska. Canadian Journal of Botany, 71(9), pp.1133-1142.	https://doi.org/10.1139/b93-133
WILCOX	Neotoma	2858	2955	Wilcox Pass	-117.216667	52.241667	Western North America	2355	Raw	Bog	31	AWI	-0.004	12.627	Small bog in shallow bedrock basin. Physiography: mountainous. Surrounding vegetation: alpine tundra, esp. Salix, Dryas.	Beaudoin, A.B., 1984. Holocene environmental change in the Sunwapta Pass Area, Jasper National Park. Doctoral dissertation. University of Western Ontario, London, Ontario, Canada.		Beaudoin, A.B. and King, R.H., 1986. Using discriminant function analysis to identify Holocene tephras based on magnetite composition: a case study from the Sunwapta Pass area, Jasper National Park. Canadian journal of earth sciences, 23(6), pp.804-812.	https://doi.org/10.1139/e86-082	Beaudoin, A.B. and King, R.H., 1990. Late Quaternary vegetation history of Wilcox Pass, Jasper National Park, Alberta. Palaeogeography, Palaeoclimatology, Palaeoecology, 80(2), pp.129-144.	https://doi.org/10.1016/0031-0182(90)90125-Q
WLDSPEAR	Neotoma	2865	2962	Wild Spear Lake	-114.150000	59.250000	Western North America	880	Raw	Lake	34	AWI	-0.021	13.919	Depression in ground moraine. Physiography: ground moraine. Surrounding vegetation: Picea mariana/Sphagnum muskeg.	MacDonald, G.M., 1984. Postglacial plant migration and vegetation development in the western Canadian boreal forest. Doctoral dissertation. University of Toronto, Toronto, Ontario, Canada.		MacDonald, G.M., 1987. Postglacial vegetation history of the Mackenzie River Basin. Quaternary Research, 28(2), pp.245-262.	https://doi.org/10.1016/0033-5894(87)90063-9	MacDonald, G.M. and Cwynar, L.C., 1985. A fossil pollen based reconstruction of the late Quaternary history of lodgepole pine (Pinus contorta ssp. latifolia) in the western interior of Canada. Canadian Journal of Forest Research, 15(6), pp.1039-1044.	https://doi.org/10.1139/x85-168
WONDER	Neotoma	2935	3033	Wonder Lake	-151.083333	63.483333	Western North America	610	Raw	Lake	34	AWI	0.013	19.712	Morainally dammed lake. Physiography: valley lowland in Alaska Range. Surrounding vegetation: spruce forest with tundra in mountains.	Anderson, P.M., Lozhkin, A.V., Eisner, W.R., Hopkins, D.M., Brubaker, L.B. and Colinvaux, P.A., 1994. Pollen records from Ten Mile and Wonder Lake, Alaska. Geographie Physique et Quaternaire, 48(2), pp.131-141.
WOSKI	Neotoma	2941	3039	Woski Pond	-119.625000	37.725000	Western North America	1212	Raw	Lake	20	AWI	-0.016	1.286	Cutoff meander of Merced River. Physiography: glacial valley bottom. Surrounding vegetation: Pinus/Calocedrus/Quercus/Alnus/Rubus.	Anderson, R.S., 1987. Late-Quaternary environments of the Sierra Nevada, California. Doctoral dissertation. University of Arizona, Tucson, Arizona, USA.		Anderson, R.S. and Carpenter, S.L., 1991. Vegetation change in Yosemite Valley, Yosemite National Park, California, during the protohistoric period. Madrono, 38, pp.1-13.
YESTERDY	Neotoma	2949	3048	Yesterday Lake	-119.483333	56.766667	Western North America	1050	Raw	Lake	10	AWI	-0.029	12.472	Lake in ground moraine depression. Physiography: Clear Hills. Surrounding vegetation: Picea mariana, P. glauca, Pinus contorta.	MacDonald, G.M., 1984. Postglacial plant migration and vegetation development in the western Canadian boreal forest. Doctoral dissertation. University of Toronto, Toronto, Ontario, Canada.		MacDonald, G.M., 1987. Postglacial development of the subalpine-boreal transition forest of western Canada. Journal of Ecology, 75, pp.303-320.	https://doi.org/10.2307/2260420	MacDonald, G.M. and Cwynar, L.C., 1985. A fossil pollen based reconstruction of the late Quaternary history of lodgepole pine (Pinus contorta ssp. latifolia) in the western interior of Canada. Canadian Journal of Forest Research, 15(6), pp.1039-1044.	https://doi.org/10.1139/x85-168
HEADLAKE	Neotoma	2955	3054	Head Lake	-105.740635	37.711090	Western North America	2300	Raw	Lake	32	AWI	-0.042	11.864	Playa lake in a blowout depression in the San Luis Valley. Surrounding vegetation: Sarcobatus/Atriplex/Chysothamnus steppe.	Jodry, M.A., Shafer, D.S., Stanford, D.J. and Davis, O.K., 1989. Late Quaternary environments and human adaptation in the San Luis Valley, south-central Colorado. In: Water in the valley: a 1989 perspective on water supplies, issues, and solutions in the San Luis Valley, Colorado ed. by E.J. Harmon (pp.189-208). Colorado Ground-Water Association Guidebook, Eighth Annual Field Trip, August 19-20, 1989.		Shafer, D.S., 1989. The timing of late Quaternary monsoon precipitation maxima in the southwest United States. Doctoral dissertation. University of Arizona, Tucson, Arizona, USA.
COMOLAKE	Neotoma	2957	3056	Como Lake	-105.514165	37.569525	Western North America	3523	Raw	Lake	31	AWI	-0.029	14.234	Glacial scour lake. Physiography: Sangre de Cristo Mountains. Surrounding vegetation: open Picea, Abies, Pinus aristata.	Jodry, M.A., Shafer, D.S., Stanford, D.J. and Davis, O.K., 1989. Late Quaternary environments and human adaptation in the San Luis Valley, south-central Colorado. In: Water in the valley: a 1989 perspective on water supplies, issues, and solutions in the San Luis Valley, Colorado ed. by E.J. Harmon (pp.189-208). Colorado Ground-Water Association Guidebook, Eighth Annual Field Trip, August 19-20, 1989.		Shafer, D.S., 1989. The timing of late Quaternary monsoon precipitation maxima in the southwest United States. Doctoral dissertation. University of Arizona, Tucson, Arizona, USA.
BECHAN2M	Neotoma	244	3060	Bechan Cave	-110.866667	37.366667	Western North America	1280	Raw	Cave	23	AWI	0.375	17.895	Large sandstone cave. Physiography: canyon lands. Surrounding vegetation: open juniper woodland.	Davis, O.K., 1990. Caves as sources of biotic remains in arid western North America. Palaeogeography, Palaeoclimatology, Palaeoecology, 76(3-4), pp.331-348.	https://doi.org/10.1016/0031-0182(90)90119-R	Davis, O.K., Agenbroad, L., Martin, P.S. and Mead, J.I., 1984. The Pleistocene dung blanket of Bechan Cave, Utah. In: Contributions in Quaternary vertebrate paleontology: a volume in memorial to John E. Guilday ed. by H.H. Genoways and M.R. Dawson (pp.267-282). Special Publication of Carnegie Museum of Natural History 8, Pittsburgh, Pennsylvania, USA.
DEAD6101	Neotoma	655	3076	Toadlena Lake [Dead Man Lake]	-108.952770	36.237195	Western North America	2759	Raw	Lake	22	AWI	36.131	45.058	Sandstone depression formed by piping. Physiography: crest of the Chuska Mountains. Surrounding vegetation: Pinus ponderosa forest.	Wright Jr, H.E., 1964. Origin of the lakes in the Chuska Mountains, northwestern New Mexico. Geological Society of America Bulletin, 75(7), pp.589-598.	https://doi.org/10.1130/0016-7606(1964)75%5B589:OOTLIT%5D2.0.CO;2	Wright Jr, H.E., Bent, A.M., Spross Hansen, B. and Maher Jr, L.J., 1973. Present and past vegetation of the Chuska Mountains, northwestern New Mexico. Geological Society of America Bulletin, 84(4), pp.1155-1180.	https://doi.org/10.1130/0016-7606(1973)84%3C1155:PAPVOT%3E2.0.CO;2
JOHNKLON	Neotoma	814	3149	John Klondike Bog	-123.646667	60.356667	Western North America	460	Raw	Peat	43	AWI	-0.019	11.031	The fossils come from a 4.65m section of peats collected from a raised frozen bog in the Fisherman Valley in the Liard Range. . The surrounding vegetation is Populus tremuloides and Picea glauca.	Matthews Jr, J.V., 1980. Paleoecology of John Klondike Bog, Fisherman Lake region, southwest district of Mackenzie. Geological Survey of Canada Paper 80-22.
POTATO2	Neotoma	1906	3561	Potato Lake	-111.345278	34.462222	Western North America	2205	Raw	Lake	61	AWI	0.222	39.944	Solution basin in Coconino Sandstone. Physiography: Mogollon Rim. Surrounding vegetation: open Pinus ponderosa forest.	Anderson, R.S., 1989. Development of the southwestern ponderosa pine forests: what do we really know. Multiresource management of ponderosa pine forests. US Forest Service General Technical Report RM-185, pp.15-22.		Anderson, R.S., 1993. A 35,000 year vegetation and climate history from Potato Lake, Mogollon Rim, Arizona. Quaternary Research, 40(3), pp.351-359.	https://doi.org/10.1006/qres.1993.1088	Anderson, R.S., Smith, S., Rothstein, D., Murray, L., Hadly, E., Force, C. and Diveley-White, S., 1989. The mid-and late-Wisconsin pollen stratigraphy of Potato Lake, Coconino County, Arizona. Current Research in the Pleistocene, 6, pp.51-54.		Whiteside, M.C., 1965. Paleoecological studies of Potato Lake and its environs. Ecology, 46(6), pp.807-816.	https://doi.org/10.2307/1934013
SAPBHM	Neotoma	2260	3611	San Agustin Plains	-108.250000	33.866667	Western North America	2069	Raw	Lake	81	AWI	-0.067	31.116	Playa lake. Physiography: Datil-Mogollon volcanic plateau. Surrounding vegetation: pinyon-juniper woodland.	Clisby, K.H., Foreman, F. and Sears, P.B., 1956. Pleistocene climatic changes in New Mexico. U.S.A. Veroffentlichungen des Geobotanisches Institutes Rubel der Eidgenossischen Technischen Hochschule, Stiftung Rubel, Zurich, 34, pp.22-26 (in German).		Clisby, K.H. and Foreman, F., 1962. Palynology - diastrophism - erosion. Field excursion guide, 1st International Pollen Conference, Tucson, Arizona, USA.		Markgraf, V., Bradbury, J.P., Forester, R.M., Singh, G. and Sternberg, R.S., 1984. San Agustin Plains, New Mexico: age and paleoenvironmental potential reassessed. Quaternary Research, 22(3), pp.336-343.	https://doi.org/10.1016/0033-5894(84)90027-9
BROWNS	Neotoma	9795	14491	Browns Island	-121.867950	38.042170	Western North America	0	Raw	Peat	28	AWI	-0.032	2.533	Browns Island is a 2.8 sq km tidal wetland located in the San Francisco Estuary at the confluence of the Sacramento and San Joaquin Rivers. Surrounding Vegetation: Schoenoplectus, Bolboschoenus, Distichlis spicata, Salicornia virginica, Juncus, Triglochin maritima.	Malamud-Roam, F. and Ingram, B.L., 2004. Late Holocene 13C and pollen records of paleosalinity from tidal marshes in the San Francisco Bay estuary, California. Quaternary Research, 62(2), pp.134-145.	https://doi.org/10.1016/j.yqres.2004.02.011	May, M.D., 1999. Vegetation and salinity changes over the last 2000 years at two islands in the northern San Francisco Estuary, California. Master's thesis. University of California Berkeley, Berkeley, California, USA.
ROEISLND	Neotoma	9796	14494	Roe Island	-122.032935	38.072300	Western North America	0	Raw	Marsh	31	AWI	-0.043	2.104	Tidal marsh located on an island in the San Francisco Estuary. Surrounding vegetation: Distichlis spicata and Salicornia virginica.	Malamud-Roam, F. and Ingram, B.L., 2004. Late Holocene 13C and pollen records of paleosalinity from tidal marshes in the San Francisco Bay estuary, California. Quaternary Research, 62(2), pp.134-145.	https://doi.org/10.1016/j.yqres.2004.02.011	May, M.D., 1999. Vegetation and salinity changes over the last 2000 years at two islands in the northern San Francisco Estuary, California. Master's thesis. University of California Berkeley, Berkeley, California, USA.
DOGLKBC	Neotoma	9798	14498	Dog Lake	-115.929770	50.780545	Western North America	1183	Raw	Lake	121	AWI	0.033	10.139	Dog Lake is a glacial origin lake located in the Kootenay Valley. Surrounding vegetation: Mixed stands of Pinus contorta and Pseudotsuga menziesii grow on xeric sites, while Picea glauca, Populus tremuloides, and Betula papyrifera are found on mesic sites. Dog Lake represents the northernmost extent of Larix occidentalis in the Rocky Mountains.	Hallett, D.J. and Hills, L.V., 2006. Holocene vegetation dynamics, fire history, lake level and climate change in the Kootenay Valley, southeastern British Columbia, Canada. Journal of Paleolimnology, 35(2), pp.351-371.	https://doi.org/10.1007/s10933-005-1335-6
LOWDER	Neotoma	9830	14549	Lowder Creek Bog	-112.792245	37.672140	Western North America	3127	Raw	Bog	37	AWI	-0.045	15.422	Fen sediments accumulated behind a well-developed Late Wisconsin moraine complex. Surrounding vegetation: Picea engelmannii - Abies lasiocarpa forest with Populus tremuloides. Members of the Cyperaceae family cover the bog surface. Dodecatheon pulchellum, Pedicularis groenlandica, and Gentiana are common.	Anderson, R.S., Hasbargen, J., Koehler, P.A. and Feiler, E.J., 1999. Late Wisconsin and Holocene subalpine forests of the Markagunt Plateau of Utah, southwestern Colorado Plateau, USA. Arctic, Antarctic, and Alpine Research, 31(4), pp.366-378.	https://doi.org/10.1080/15230430.1999.12003321
SANLUIS	Neotoma	9878	14650	San Luis Lake	-105.724665	37.677730	Western North America	2293	Raw	Lake	24	AWI	-0.044	1.552	Playa lake subject to drying out. Aeolian landscape with blowout depressions, parabolic dunes, and alkaline flats. Upland vegetation: saline bottom land shrublands, cold desert shrublands, and salt meadows, with Sarcobatus, Salsola, Atriplex, Sueda, Artemisia, and Poaceae.	de Lanois, J.L., 1993. Climatic change during the late Holocene from a south central Colorado lake. Master's thesis. University of Arizona, Tuscon, Arizona, USA.
YAHOO	Neotoma	9942	14792	Yahoo Lake	-124.018585	47.676915	Western North America	709	Raw	Lake	50	AWI	0.032	13.876	Yahoo Lake was formed by a small cirque glacier. Surrounding vegetation: The lake is located within the Pacific Silver Fir forest zone. North facing slopes are dominated by Abies amabilis and Tsuga heterophylla, while Thuja plicata is limited to flat areas or south aspects. The lake is near the upper elevation limits of Tsuga heterophylla and Thuja plicata.	Gavin, D.G. and Brubaker, L.B., 2015. Late Quaternary Vegetation and Fire History of the Olympic Peninsula. In: Late Pleistocene and Holocene Environmental Change on the Olympic Peninsula. Ecological Studies 222. ed. by D.G. Gavin and L.B. Brubaker (pp.61-106). Springer International Publishing, Cham, Switzerland.	https://doi.org/10.1007/978-3-319-11014-1_4	Gavin, D.G., Brubaker, L.B. and Greenwald, D.N., 2013. Postglacial climate and fire-mediated vegetation change on the western Olympic Peninsula, Washington (USA). Ecological Monographs, 83(4), pp.471-489.	https://doi.org/10.1890/12-1742.1
TWOFROG	Neotoma	9943	14794	Two Frog Lake	-127.534035	51.106595	Western North America	4	Raw	Lake	57	AWI	-0.051	14.270	Two Frog Lake is a small single basin unstratified freshwater lake. It is located in the Seymour-Belize Inlet Complex, situated in the central coastal mainland of British Columbia. Surrounding vegetation: The vegetation in this region is dominated by Tsuga heterophylla and Tsuga plicata.	Galloway, J.M., Patterson, R.T., Doherty, C.T. and Roe, H.M., 2007. Multi-proxy evidence of postglacial climate and environmental change at Two Frog Lake, central mainland coast of British Columbia, Canada. Journal of Paleolimnology, 38(4), pp.569-588.	https://doi.org/10.1007/s10933-007-9091-4
SIESTA	Neotoma	9945	14799	Siesta Lake	-119.659945	37.850500	Western North America	2430	Raw	Lake	26	AWI	0.005	12.419	Small morainally dammed lake in the Sierra Nevada mountains. Surrounding vegetation: Pinus contorta forest with Abies magnifica and an occasional Pinus monticola. There are very few herbaceous and shrubby understorey species. Occasional openings within the forest allow species such as Quercus vaccinifolia, Arctostaphylos nevadensis, Ribes montigenum, and Phyllodoce breweri to thrive.	Brunelle, A. and Anderson, R.S., 2003. Sedimentary charcoal as an indicator of late-Holocene drought in the Sierra Nevada, California, and its relevance to the future. The Holocene, 13(1), pp.21-28.	https://doi.org/10.1191/0959683603hl591rp
BURNTKNB	Neotoma	9947	14803	Burnt Knob Lake	-114.982900	45.706945	Western North America	2250	Raw	Lake	36	AWI	-0.043	14.955	Late-Pleistocene cirque basin. Physiography: Clearwater mountain range. Surrounding vegetation: Abies bifolia and Pinus albicaulis.	Brunelle-Daines, A.R., 2002. Holocene changes in fire, climate and vegetation in the northern Rocky Mountains of Idaho and western Montana. Doctoral dissertation. University of Oregon, Eugene, Oregon, USA.		Brunelle, A. and Whitlock, C., 2003. Postglacial fire, vegetation, and climate history in the Clearwater Range, Northern Idaho, USA. Quaternary Research, 60(3), pp.307-318.	https://doi.org/10.1016/j.yqres.2003.07.009
BAKER	Neotoma	9974	14884	Baker Lake	-114.263205	45.891725	Western North America	2300	Raw	Lake	40	AWI	-0.044	13.903	Baker Lake is on the east side of the Bitterroot Range. It is a late-Pleistocene cirque basin. Surrounding vegetation is dominated by Pinus albicaulis and Larix lyallii on dry slopes, and Abies bifolia on wet slopes. Pinus contorta and Picea engelmannii also grow in the watershed. Dominant understory species include Vaccinium scoparium, Vaccinium membranaceum, Xerophyllum tenax, and Phyllodoce empetriformis.	Brunelle-Daines, A.R., 2002. Holocene changes in fire, climate and vegetation in the northern Rocky Mountains of Idaho and western Montana. Doctoral dissertation. University of Oregon, Eugene, Oregon, USA.		Brunelle, A., Rehfeldt, G.E., Bentz, B. and Munson, A.S., 2008. Holocene records of Dendroctonus bark beetles in high elevation pine forests of Idaho and Montana, USA. Forest Ecology and Management, 255(3-4), pp.836-846.	https://doi.org/10.1016/j.foreco.2007.10.008
HOODOO	Neotoma	9985	14911	Hoodoo Lake	-114.651530	46.320235	Western North America	1787	Raw	Lake	53	AWI	-0.047	10.055	Cutoff stream channel located on the west side of the Bitterroot Range. The subalpine forest surrounding Hoodo Lake is dominated by Picea engelmannii and Abies bifolia on the wet slopes, and Pinus contorta on the southern dry slopes. Salix and Scirpus are in seeps or moister areas. Dominant understory species include Vaccinium scoparium, Xerophyllum tenax, and Phyllodoce empetriformis. Various members of Poaceae and Asteraceae are also present in the watershed.	Brunelle-Daines, A.R., 2002. Holocene changes in fire, climate and vegetation in the northern Rocky Mountains of Idaho and western Montana. Doctoral dissertation. University of Oregon, Eugene, Oregon, USA.		Brunelle, A., Rehfeldt, G.E., Bentz, B. and Munson, A.S., 2008. Holocene records of Dendroctonus bark beetles in high elevation pine forests of Idaho and Montana, USA. Forest Ecology and Management, 255(3-4), pp.836-846.	https://doi.org/10.1016/j.foreco.2007.10.008
PINTLER	Neotoma	9989	14923	Pintler Lake	-113.439865	45.840555	Western North America	1921	Raw	Lake	36	AWI	-0.008	16.690	Pintler Lake is dammed behind a late-Pleistocene end moraine. The montane forest surrounding the lake is dominated by Pinus contorta with Pseudotsuga menziesii and Picea engelmannii as minor components. Dominant understory species include Arctostaphylos uva-ursi, Artemisia tridentata, Linnea borealis, and Ribes.	Brunelle-Daines, A.R., 2002. Holocene changes in fire, climate and vegetation in the northern Rocky Mountains of Idaho and western Montana. Doctoral dissertation. University of Oregon, Eugene, Oregon, USA.
MOOSE_neotoma	Neotoma	9994	14935	Moose Lake	-123.350930	47.883685	Western North America	1544	Raw	Lake	42	AWI	-0.018	15.822	Alpine lake located in the Grand Valley. Surrounding vegetation: Subalpine forest parkland dominated by Abies lasiocarpa. Tsuga heterophylla and Pseudotsuga menziesii reach their upper elevational limit near Moose Lake.	Gavin, D.G., McLachlan, J.S., Brubaker, L.B. and Young, K.A., 2001. Postglacial history of subalpine forests, Olympic Peninsula, Washington, USA. The Holocene, 11(2), pp.177-188.	https://doi.org/10.1191/095968301670879949
MARTINS	Neotoma	9995	14938	Martins Lake	-123.532590	47.712915	Western North America	1415	Raw	Lake	47	AWI	0.090	14.228	Martins Lake is a closed basin located on an alpine ridge. Surrounding vegetation: small meadows, scree slopes, and patchy Tsuga mertenisana forest. Phyllodoce empetriformis, Vaccinium deliciosum, Cassiope mertensiana, Carex, Erythronium montanum, and Polygonum bistortoides are common in meadows.	Gavin, D.G. and Brubaker, L.B., 2015. Late Quaternary Vegetation and Fire History of the Olympic Peninsula. In: Late Pleistocene and Holocene Environmental Change on the Olympic Peninsula. Ecological Studies 222. ed. by D.G. Gavin and L.B. Brubaker (pp.61-106). Springer International Publishing, Cham, Switzerland.	https://doi.org/10.1007/978-3-319-11014-1_4	Gavin, D.G., McLachlan, J.S., Brubaker, L.B. and Young, K.A., 2001. Postglacial history of subalpine forests, Olympic Peninsula, Washington, USA. The Holocene, 11(2), pp.177-188.	https://doi.org/10.1191/095968301670879949
FRACAS	Neotoma	9997	14944	Fracas Lake	-112.238595	36.630700	Western North America	2512	Raw	Lake	28	AWI	0.055	13.653	Small solution basin on the Kaibab Plateau. Pond has a central floating mat of Carex, Schoenoplectus acutus, and Poaceae. Surrounded by mixed conifer forest of Abies concolor, Picea pungens, Pinus ponderosa, and Pseudotsuga menziesii.	Weng, C. and Jackson, S.T., 1999. Late Glacial and Holocene vegetation history and paleoclimate of the Kaibab Plateau, Arizona. Palaeogeography, Palaeoclimatology, Palaeoecology, 153(1-4), pp.179-201.	https://doi.org/10.1016/S0031-0182(99)00070-X
BEARAZ	Neotoma	10000	14951	Bear Lake	-112.147175	36.371125	Western North America	2778	Raw	Lake	45	AWI	0.136	13.470	Bear Lake occurs in a limestone sinkhole and is located near the highest portion of the Kaibab Plateau. A sedge floating mat covers about two thirds of the water surface. Aquatic plants in the open water area are Glyceria borealis, Eleocharis, Sparganium, and Potamogeton. Surrounding vegetation: Forest dominated by Picea engelmannii and Abies lasiocarpa. Scattered Abies concolor and Pinus ponderosa also occur. Several Populus tremuloides trees grow on the west shore of the pond.	Weng, C. and Jackson, S.T., 1999. Late Glacial and Holocene vegetation history and paleoclimate of the Kaibab Plateau, Arizona. Palaeogeography, Palaeoclimatology, Palaeoecology, 153(1-4), pp.179-201.	https://doi.org/10.1016/S0031-0182(99)00070-X
MEADERVR	Neotoma	10019	14995	Meade River bluff	-157.342070	70.475005	Western North America	2	Raw	River	12	AWI	0.268	10.598	Tundra ice-wedge polygon on the Meade River bluffs. Sandy surface sediments are Pleistocene/Holocene eolian dunes. Surrounding vegetation: Carex, Sphagnum, Salix, Dryas, Polygonum. Sedge tundra.	Eisner, W.R. and Peterson, K.M., 1998. High-resolution pollen analysis of tundra polygons from the North Slope of Alaska. Journal of Geophysical Research: Atmospheres, 103(D22), pp.28929-28937.	https://doi.org/10.1029/98JD01462
MUMBO	Neotoma	10053	15074	Mumbo Lake	-122.510539	41.190975	Western North America	1860	Raw	Lake	34	AWI	-0.035	14.466	Lake is in a small cirque basin in the Trinity Mountains. Principal trees at Mumbo Lake include Pinus contorta, Abies concolor, A. magnifica, Pinus monticola, and Tsuga mertensiana. Forest canopy around the lake is closed, although montane chaparral (Quercus vaccinifolia, Arctostaphylos, and rosaceous taxa) and bare rock cover much of the surrounding slopes.	Daniels, M.L., Anderson, S. and Whitlock, C., 2005. Vegetation and fire history since the Late Pleistocene from the Trinity Mountains, northwestern California, USA. The Holocene, 15(7), pp.1062-1071.	https://doi.org/10.1191/0959683605hl878ra
EMMASEC1	Neotoma	10061	15106	Lake Emma	-107.615370	37.902105	Western North America	3740	Raw	Lake	52	AWI	-0.067	19.165	Glacial tarn in a south-facing cirque at the head of Eureka Gulch near the headwaterso of the Animas River. On 4 June 1978, it was suddenly and completely drained by the collapse of underground mine workings. Site is above timberline in alpine tundra.	Carrara, P.E., Trimble, D.A. and Rubin, M., 1991. Holocene treeline fluctuations in the northern San Juan Mountains, Colorado, USA, as indicated by radiocarbon-dated conifer wood. Arctic and Alpine Research, 23(3), pp.233-246.	https://doi.org/10.2307/1551601	Carrara, P.E., Mode, W.N., Rubin, M. and Robinson, S.W., 1984. Deglaciation and postglacial timberline in the San Juan Mountains, Colorado. Quaternary Research, 21(1), pp.42-55.	https://doi.org/10.1016/0033-5894(84)90088-7
CODE	Neotoma	10083	15157	Code Lake	-151.859995	67.157920	Western North America	250	Raw	Lake	25	AWI	-0.028	7.382	Physiography: Foothills of the southcentral Brooks Range, within the Kobuk Ridges and Valleys Ecoregion. Underlain by alluvial and glacial sediments. Surrounding Vegetation: Picea mariana, Picea glauca, Populus balsamifera, Populus tremuloides, Betula papyrifera, Salix glandulosa, Alnus.	Higuera, P.E., 2006. Late glacial and Holocene fire history in the southcentral Brooks Range, Alaska: Direct and indirect impacts of climate change on fire regimes. Doctoral dissertation. University of Washington, Seattle, Washington, USA.
LASTCHAN	Neotoma	10094	15175	Last Chance Lake	-150.745125	67.124060	Western North America	250	Raw	Lake	12	AWI	0.295	1.992	Physiography: Foothills of the southcentral Brooks Range, within the Kobuk Ridges and Valleys Ecoregion. Underlain by alluvial and glacial sediments. Surrounding Vegetation: Picea mariana, Picea glauca, Populus balsamifera, Populus tremuloides, Betula papyrifera, Salix glandulosa, Alnus.	Higuera, P.E., 2006. Late glacial and Holocene fire history in the southcentral Brooks Range, Alaska: Direct and indirect impacts of climate change on fire regimes. Doctoral dissertation. University of Washington, Seattle, Washington, USA.
RUPPERT1	Neotoma	10100	15185	Ruppert Lake	-154.244985	67.070840	Western North America	230	Raw	Lake	121	AWI	0.180	14.443	Kettle lake on a terminal moraine. Physiography: Foothills of the south central Brooks Range, within the Kobuk Ridges and Valleys Ecoregion. Underlain by alluvial and glacial sediments. Surrounding Vegetation: Picea mariana, Picea glauca, Populus balsamifera, Populus tremuloides, Betula papyrifera, Salix glandulosa, Alnus.	Higuera, P.E., 2006. Late glacial and Holocene fire history in the southcentral Brooks Range, Alaska: Direct and indirect impacts of climate change on fire regimes. Doctoral dissertation. University of Washington, Seattle, Washington, USA.
TUSSOCK	Neotoma	10101	15187	Wild Tussock Lake	-151.383615	67.126480	Western North America	290	Raw	Lake	27	AWI	0.558	7.240	Physiography: Foothills of the south central Brooks Range, within the Kobuk Ridges and Valleys Ecoregion. Underlain by alluvial and glacial sediments. Surrounding Vegetation: Picea mariana, Picea glauca, Populus balsamifera, Populus tremuloides, Betula papyrifera, Salix glandulosa, Alnus.	Higuera, P.E., 2006. Late glacial and Holocene fire history in the southcentral Brooks Range, Alaska: Direct and indirect impacts of climate change on fire regimes. Doctoral dissertation. University of Washington, Seattle, Washington, USA.
XINDI	Neotoma	10102	15189	Xindi Lake	-152.491385	67.111235	Western North America	240	Raw	Lake	64	AWI	-0.047	18.244	Physiography: Foothills of the south central Brooks Range, within the Kobuk Ridges and Valleys Ecoregion. Underlain by alluvial and glacial sediments. Surrounding Vegetation: Picea mariana, Picea glauca, Populus balsamifera, Populus tremuloides, Betula papyrifera, Salix glandulosa, Alnus.	Higuera, P.E., 2006. Late glacial and Holocene fire history in the southcentral Brooks Range, Alaska: Direct and indirect impacts of climate change on fire regimes. Doctoral dissertation. University of Washington, Seattle, Washington, USA.
LOSTPARK	Neotoma	10107	15201	Lost Park	-105.538300	39.294900	Western North America	3079	Raw	Peat	50	AWI	-0.047	13.791	Lost Park wet meadow occurs along the South Fork of Lost Creek, immediately northeast of the Tarryall Mountains. Surrounding vegetation: The forest vegetation of the area contains Juniperus communis as an understory shrub. Picea pungens and Pinus contorta grow on a knoll that extends into the valley near the coring site. Pinus contorta, Pinus aristata, and Picea engelmannii all occur on the forested valley slopes flanking Lost Park. Populus tremulouides commonly occurs in dry disturbed areas. The wet meadow vegetation consists of many herbaceous plant taxa such as Clementsia rhodantha, Potentilla, Gentiana calycosa, and members of the Poaceae, Cyperaceae, and Caryophyllaceae families. Occasional Salix shrubs also dot the wet meadow. In dry nonforested areas along the valley floor adjacent to the wet meadow, abundant taxa include Fragaria virginiana, Taraxacum officinale, Aster, Penstemon, Achillea lanulosa, A. frigida, Pentaphylloides floribunda, and members of the Chenopodiaceae and Poaceae families.	Vierling, L.A., 1998. Palynological evidence for late-and postglacial environmental change in central Colorado. Quaternary Research, 49(2), pp.222-232.	https://doi.org/10.1006/qres.1997.1960
BIGLAKE	Neotoma	10114	15214	Big Lake	-121.454395	51.668615	Western North America	1029	Raw	Lake	32	AWI	-0.022	12.006	Big Lake is situated in a topographically closed basin on the Cariboo Plateau. Surrounding vegetation: Pseudotsuga menziesii, Pinus contorta, and scattered grasslands.	Bennett, J.R., Cumming, B.F., Leavitt, P.R., Chiu, M., Smol, J.P. and Szeicz, J., 2001. Diatom, pollen, and chemical evidence of postglacial climatic change at Big Lake, south-central British Columbia, Canada. Quaternary Research, 55(3), pp.332-343.	https://doi.org/10.1006/qres.2001.2227
CASSIOPE	Neotoma	10145	15276	Cassiope Pond	-127.752025	50.166625	Western North America	550	Raw	Lake	53	AWI	0.092	12.771	Pond on the Brooks Peninsula, Vancouver Island.	Hebda, R.J. and Allen, G.B., 1997. Late Quaternary paleoecology of Brooks Peninsula. In: Brooks Peninsula: An Ice Age Refugium on Vancouver Island ed. by R.J. Hebda and J.C. Haggarty. Occasional Paper No 5. B.C. Parks.
TINY	Neotoma	10151	15284	Tiny Lake	-127.381880	51.194380	Western North America	6	Raw	Lake	45	AWI	-0.044	13.985	Tiny Lake is a coastal isolation basin separated from Mereworth Sound by a 3.28 m sill. Surrounding vegetation: Tsuga heterophylla dominates the forests. Thuja plicata is also common. Deciduous taxa include Acer glabrum and Alnus. There is an understory of ferns, bryophytes, and shrubs, namely Gaultheria shallon.	Galloway, J.M., 2006. Post-glacial climate and vegetation change in the Seymour-Belize Inlet complex, central coastal British Columbia, Canada. Doctoral dissertation. Carleton University, Ottawa, Ontario, Canada.
PYROLA	Neotoma	10153	15288	Pyrola Lake	-127.697995	50.183195	Western North America	506	Raw	Lake	49	AWI	0.072	16.329	NA	Hebda, R.J., 1997. Impact of climate change on biogeoclimatic zones of British Columbia and Yukon. Responding to global climate change in British Columbia and Yukon, 1, p.363.
DEVLINS	Neotoma	10158	15298	Devlins Park	-105.561560	40.000760	Western North America	2953	Raw	Lake	51	AWI	16.826	28.433	Former proglacial lake of Pinedale age on Caribou Creek that formed when glacial ice from North Boulder Creek downstream advanced across the valley of Caribou Creek. The lake floor is 14-20 m above present Caribou Creek. Surrounding vegetation: Slopes near the coring site are covered by Pinus contorta forest with Abies bifolia and Picea engelmannii. Populus tremuloides and Pinus flexilis are also present. The basin itself is dominated by Salix, Cyperaceae, and Poaceae.	Lego, T.E. and Bakrr, R.G., 1980. Palynology of Pinedale sediments, Devlins Park, Boulder County, Colorado. Arctic and Alpine Research, 12(3), pp.319-333.	https://doi.org/10.2307/1550718
BERENDON	Neotoma	10171	15323	Berendon Fen	-130.055465	56.242780	Western North America	794	Raw	Fen	23	AWI	-0.028	7.090	Fen near the terminal moraine of Berendon Glacier. Surrounding vegetation: predominantly sedges and willows on the fen surface. Wetland herbs (Sanguisorba and Caltha leptosepala) are less common. Young subalpine firs are present where mineral soil is available.	Clague, J.J. and Mathewes, R.W., 1996. Neoglaciation, glacier-dammed lakes, and vegetation change in northwestern British Columbia, Canada. Arctic and Alpine Research, 28(1), pp.10-24.	https://doi.org/10.2307/1552081	Clague, J.J., Wohlfarth, B., Ayotte, J., Eriksson, M., Hutchinson, I., Mathewes, R.W., Walker, I.R. and Walker, L., 2004. Late Holocene environmental change at treeline in the northern Coast Mountains, British Columbia, Canada. Quaternary Science Reviews, 23(23-24), pp.2413-2431.	https://doi.org/10.1016/j.quascirev.2004.01.009
SKINNY	Neotoma	10183	15342	Skinny Lake	-130.095975	57.594980	Western North America	899	Raw	Lake	41	AWI	0.300	14.143	Skinny Lake is located at an expansion in the Todagin River valley. Surrounding vegetation: Picea glauca, Pinus contorta, Picea mariana on poorly drained soils, Populus tremuloides on south facing slopes. Also Alnus, Betula, and Salix.	Spooner, I.S., Mazzucchi, D., Osborn, G., Gilbert, R. and Larocque, I., 2002. A multi-proxy holocene record of environmental change fromthe sediments of Skinny Lake, Iskut region, northern British Columbia, Canada. Journal of Paleolimnology, 28(4), pp.419-431.	https://doi.org/10.1023/A:1021689328179
FARGHER	Neotoma	10184	15344	Fargher Pond	-122.519190	45.886765	Western North America	202	Raw	Lake	130	AWI	19.255	57.859	Fargher Pond was formed >58,000 cal yr BP following the recession of early to middle Wisconsin glaciers in the western Cascade Range. Surrounding vegetation: Pseudotsuga menziesii, T. heterophylla, Thuja plicata, and Alnus rubra. Minor amounts of Abies grandis and Pinus monticola.	Grigg, L.D. and Whitlock, C., 2002. Patterns and causes of millennial-scale climate change in the Pacific Northwest during Marine Isotope Stages 2 and 3. Quaternary Science Reviews, 21(18-19), pp.2067-2083.	https://doi.org/10.1016/S0277-3791(02)00017-3
STEWARTB	Neotoma	10191	15356	Stewart Bog	-105.722000	35.832000	Western North America	3115	Raw	Bog	208	AWI	-0.030	14.178	Alpine bog within a suite of moraines. Surrounding vegetation: Subalpine coniferous forest with Picea engelmannii, Abies lasiocarpa, Pinus aristata, P. menziesii, P. strobiformis, Populus tremuloides, and Juniperus communis.	Jimenez-Moreno, G., Fawcett, P.J. and Anderson, R.S., 2008. Millennial-and centennial-scale vegetation and climate changes during the late Pleistocene and Holocene from northern New Mexico (USA). Quaternary Science Reviews, 27(13-14), pp.1442-1452.	https://doi.org/10.1016/j.quascirev.2008.04.004
SPILLWAY	Neotoma	10192	15359	Spillway Pond	-130.068815	56.239975	Western North America	852	Raw	Lake	18	AWI	-0.017	0.910	Spillway Pond is a moraine dammed lake. Surrounding vegetation is a mature forest of mountain hemlock and subalpine fir with a dense understorey of tall shrubs, including Alnus viridis, Salix, Sorbus, and Vaccinium. Meadow species (Lupinus arcticus, Valeriana sitchensis, Veratrum viride, Senecio triangularis) are common at the edges of the pone, while pioneering plants (willow, alder, grasses, sedges, and willow-herb) are dominant on nearby well drained sites.	Clague, J.J. and Mathewes, R.W., 1996. Neoglaciation, glacier-dammed lakes, and vegetation change in northwestern British Columbia, Canada. Arctic and Alpine Research, 28(1), pp.10-24.	https://doi.org/10.2307/1552081	Clague, J.J., Wohlfarth, B., Ayotte, J., Eriksson, M., Hutchinson, I., Mathewes, R.W., Walker, I.R. and Walker, L., 2004. Late Holocene environmental change at treeline in the northern Coast Mountains, British Columbia, Canada. Quaternary Science Reviews, 23(23-24), pp.2413-2431.	https://doi.org/10.1016/j.quascirev.2004.01.009
BLUEBONN	Neotoma	10195	15368	Blue Lake Wetlands	-114.031395	40.499960	Western North America	1297	Raw	Peat	52	AWI	-0.054	14.805	The Blue Lake wetland system is a large geothermal spring-fed system, ranking among the largest extant wetland habitats in the region. Surrounding vegetation: Dense marsh vegetation dominated by several species of bulrush (Schoenoplectus), sedges (Carex sp.), and spikerush (Eleocharis rostellata). Vegetation at the site consists of spongy peat currently vegetated in saltgrass.	Louderback, L.A. and Rhode, D.E., 2009. 15,000 years of vegetation change in the Bonneville basin: the Blue Lake pollen record. Quaternary Science Reviews, 28(3-4), pp.308-326.	https://doi.org/10.1016/j.quascirev.2008.09.027	Louderback, L.A., 2007. Changes in vegetation and human adaptation from the latest Pleistocene to late Holocene in the Eastern Great Basin: The Blue Lake pollen record. Master's thesis. University of Nevada, Reno, Nevada, USA.
FLYBASIN	Neotoma	10204	15385	Flycatcher Basin	-121.573000	41.015000	Western North America	924	Raw	Peat	41	AWI	0.013	8.105	One of several small closed basins supporting wetlands located within a large landslide (the Flycatcher Embayment). Surrounding vegetation: Closed-canopy Quercus garryana woodland with Pinus ponderosa. Other trees and shrubs occuring locally are Pseudotsuga mensiessii, Juniperus occidentalis, wild rose, waxberry, Rhus trilobata, Ceanothus cuneatus, and Purshia tridentata. Growing within the basin itself are Cyperaceae, Rumex, Verbascum thapsus, Plantago, and patches of Scirpus and Juncus in wetter areas.	Anderson, R.S., Smith, S.J., Jass, R.B. and Spaulding, W.G., 2008. A late Holocene record of vegetation and climate from a small wetland in Shasta County, California. Madrono, 55(1), pp.15-25.	https://doi.org/10.3120/0024-9637(2008)55%5B15:ALHROV%5D2.0.CO;2
LASFLORE	Neotoma	10208	15396	Las Flores Arroyo	-117.460500	33.291000	Western North America	6	Raw	River	12	AWI	-0.030	3.992	A deeply incised Holocene alluvial terrace. Surrounding vegetation: Cottonwood/Willow Riparian Woodland (Populus fremontii, P. balsamifera, Salix gooddingii, S. lasiolepis, S. laevigata, Platanus racemosa, Artemisia douglasianna, Baccharis salicifolia, Conium maculatum, Xanthium strumarium, Urtica dioica, Vitis girdiana). There is also Southern Willow Scrub vegetation on the alluvial desposit (various Salix species, Toxicodendron diversilobum, Ambrosia psilostachya, Urtica dioica, Artemisia douglasianna).	Anderson, R.S. and Byrd, B.F., 1998. Late-Holocene vegetation changes from the Las Flores Creek coastal lowlands, San Diego County, California. Madrono, 45(2), pp.171-182.
LONGLAST	Neotoma	10209	15399	Long Last Lake	-137.228500	61.564000	Western North America	985	Raw	Lake	49	AWI	-0.039	10.081	The lake occupies a shallow basin in rolling to highly irregular moraine veneer near the north end of Aishihik Lake. Surrounding vegetation: Open stands of white spruce interspersed with grassy openings. Salix, dwarf Betula, and Shepherdia candensis are common on the lower slopes.	Keenan, T.J. and Cwynar, L.C., 1992. Late Quaternary history of black spruce and grasslands in southwest Yukon Territory. Canadian Journal of Botany, 70(7), pp.1336-1345.	https://doi.org/10.1139/b92-168	Keenan, T.J., 1991. Late-Quaternary history of Black Spruce and grasslands in southwest Yukon Territory. Master's thesis. University of New Brunswick, Fredericton, New Brunsiwck, Canada.
JANLAKE	Neotoma	10212	15406	Jan Lake	-143.917720	63.564660	Western North America	503	Raw	Lake	54	AWI	-0.017	14.652	Lake dammed by alluvium of the Tanana River. Watershed is formed by metamorphic bedrock hills on three sides. Surrounding vegetation: White spruce, white birch, and trembling aspen occupy hillslopes surrounding the lake. Black spruce muskegs and balsam poplar are nearby.	Carlson, L.J., 2003. Describing the postglacial pattern and rate of Picea expansion in Alaska using paleoecological records. Doctoral dissertation. University of Washington, Seattle, Washington, USA.		Carlsonl, L.J. and Finney, B.P., 2004. A 13000-year history of vegetation and environmental change at Jan Lake, east-central Alaska. The Holocene, 14(6), pp.818-827.	https://doi.org/10.1191/0959683604hl762rp
NICHOLSM	Neotoma	10213	15408	Nichols Meadow	-119.578500	37.423500	Western North America	1515	Raw	Meadow	38	AWI	-0.037	15.097	Meadow located in the Nelder Grove of the Sierra National Forest. Surrounding vegetation: Overstory species of incense cedar, white fir, ponderosa pine, sugar pine, and black oak are found with deer brush, currant, bear berry, and rose as the understory. Meadow plants (grasses, sedges, corn-lily, various herbs) are also found.	Koehler, P.A. and Anderson, R.S., 1994. The paleoecology and stratigraphy of Nichols Meadow, Sierra National Forest, California, USA. Palaeogeography, Palaeoclimatology, Palaeoecology, 112(1-2), pp.1-17.	https://doi.org/10.1016/0031-0182(94)90132-5
SEQUOIA	Neotoma	10213	15410	Nichols Meadow	-119.578500	37.423500	Western North America	1515	Raw	Meadow	13	AWI	12.050	22.540	Meadow located in the Nelder Grove of the Sierra National Forest. Surrounding vegetation: Overstory species of incense cedar, white fir, ponderosa pine, sugar pine, and black oak are found with deer brush, currant, bear berry, and rose as the understory. Meadow plants (grasses, sedges, corn-lily, various herbs) are also found.	Koehler, P.A. and Anderson, R.S., 1994. The paleoecology and stratigraphy of Nichols Meadow, Sierra National Forest, California, USA. Palaeogeography, Palaeoclimatology, Palaeoecology, 112(1-2), pp.1-17.	https://doi.org/10.1016/0031-0182(94)90132-5
PARADOX	Neotoma	10214	15413	Paradox Lake	-150.759030	60.622880	Western North America	81	Raw	Lake	48	AWI	-0.044	13.048	Lake occupies a glacially deepened trough that may have been a postglacial spillway in the Kenai lowlands region. Surrounding vegetation: Pice glauca, P. mariana, Betula kenaica. Additional trees and shrubs are Populus tremuloides, Alnus crispa, Sambucus racemosa, Rosa acicularis, Viburnum edule, Linnaea borealis, Rubus, Echinopanax horridum, Ribes, and Ledum palustre. Plants common in moist areas around the lake include Salix, Myrica gale, Menziesia ferruginea, Spriaea, Betula nana, Streptopus amplexifolius, Lycopodium, Equisetum silvaticum, and E. arvense.	Anderson, R.S., Hallett, D.J., Berg, E., Jass, R.B., Toney, J.L., De Fontaine, C.S. and DeVolder, A., 2006. Holocene development of boreal forests and fire regimes on the Kenai Lowlands of Alaska. The Holocene, 16(6), pp.791-803.	https://doi.org/10.1191/0959683606hol966rp
RASPBERY	Neotoma	10216	15417	Rasberry Bog	-130.829355	57.484395	Western North America	802	Raw	Bog	16	AWI	0.174	7.959	NA
PYRAMDBC	Neotoma	10218	15420	Pyramid Lake	-129.833915	58.892150	Western North America	1439	Raw	Lake	35	AWI	0.132	16.070	Small tarn in the Cassiar Mountains. Surrounding vegetation: Alpine tundra consisting of grass, sedge, Alnus sinuate, Salix arctica, S. planifolia, Betula glandulosa, and krummholz subalpine fir. On the steep slopes and ridges above the lake, vegetation is sparse with occasional patches of decisuous shrubs, grasses, and sedges.	Mazzucchi, D., Spooner, I.S., Gilbert, R. and Osborn, G., 2003. Reconstruction of Holocene climate change using multiproxy analysis of sediments from Pyramid Lake, British Columbia, Canada. Arctic, Antarctic, and Alpine Research, 35(4), pp.520-529.	https://doi.org/10.1657/1523-0430(2003)035%5B0520:ROHCCU%5D2.0.CO;2
HUALCU	Neotoma	10243	15494	Hual Cu Cuish Meadow	-116.583000	32.967000	Western North America	1451	Raw	Meadow	6	AWI	9.924	13.328	Mountain meadow ~500x100 m in size. Core site was in a Typha marsh alongside a small stream that bisects the meadow. Surrounding vegetation dominated by Pinus ponderosa, Quercus, Calocedrus decurrens, and Abies. Quercus species include Q. kelloggii, Q. chrysolepis, and Q. agrifolia var. oxyadenia. Salix also present.	Wahl, E.R., 2002. Paleoecology and testing of paleoclimate hypotheses in southern California during the Holocene. Doctoral dissertation. University of Minnesota, Minneapolis, Minnesota, USA.		Ohlwein, C. and Wahl, E.R., 2012. Review of probabilistic pollen-climate transfer methods. Quaternary Science Reviews, 31, pp.17-29.	https://doi.org/10.1016/j.quascirev.2011.11.002
VANWYCK	Neotoma	10277	15580	Van Wyck	-116.152150	44.517850	Western North America	2255	Raw	Meadow	37	AWI	-0.043	13.805	Wet meadow in a cirque basin. Physiography: West Moutains (fault block range). Surrounding vegetation: Lodgepole pine, Englemann spruce, fir.	Doerner, J.P. and Carrara, P.E., 1999. Deglaciation and postglacial vegetation history of the West Mountains, west-central Idaho, USA. Arctic, Antarctic, and Alpine Research, 31(3), pp.303-311.	https://doi.org/10.1080/15230430.1999.12003313
MCCALL	Neotoma	10279	15586	McCall Fen	-116.048300	44.925300	Western North America	1615	Raw	Peat	42	AWI	-0.046	19.760	Fen in area of ponds/fens. Physiography: Fault-block valley with moraines. Surrounding vegetation: Artemisia, Poaceae.	Doerner, J.P. and Carrara, P.E., 2001. Late Quaternary vegetation and climatic history of the Long Valley area, west-central Idaho, USA. Quaternary Research, 56(1), pp.103-111.	https://doi.org/10.1006/qres.2001.2247
SKUNKCAB	Neotoma	10282	15591	Skunk Cabbage Meadow	-116.666020	33.774330	Western North America	2417	Raw	Meadow	8	AWI	3.452	6.969	San Jacinto Mountains, Peninsular Range. Wet mountain meadow ~60 m in diameter. Montane with Abies concolor, Pinus ponderosa, Pinus jeffreyii, Pinus lambertiana, ferns, Symphoricarpos sp.	Wahl, E.R., 2002. Paleoecology and testing of paleoclimate hypotheses in southern California during the Holocene. Doctoral dissertation. University of Minnesota, Minneapolis, Minnesota, USA.		Ohlwein, C. and Wahl, E.R., 2012. Review of probabilistic pollen-climate transfer methods. Quaternary Science Reviews, 31, pp.17-29.	https://doi.org/10.1016/j.quascirev.2011.11.002
TAQUITZ	Neotoma	10284	15594	Taquitz Meadow	-116.663610	33.768570	Western North America	2405	Raw	Meadow	22	AWI	0.339	9.237	Wet mountain meadow ~60 m in diameter. Surrounding vegetation Pinus ponderosa/P. jeffreyi/Abies concolor forest.	Wahl, E.R., 2002. Paleoecology and testing of paleoclimate hypotheses in southern California during the Holocene. Doctoral dissertation. University of Minnesota, Minneapolis, Minnesota, USA.		Ohlwein, C. and Wahl, E.R., 2012. Review of probabilistic pollen-climate transfer methods. Quaternary Science Reviews, 31, pp.17-29.	https://doi.org/10.1016/j.quascirev.2011.11.002
PORTAGAK	Neotoma	10298	15627	Portage Lake	-150.533000	60.716495	Western North America	78	Raw	Lake	26	AWI	-0.044	11.610	The lake was formed 10,000 years ago with the retreat of mountain glaciers. Surrounding vegetation: Picea mariana/Betula papyrifera dominated boreal forest.	Anderson, R.S., Hallett, D.J., Berg, E., Jass, R.B., Toney, J.L., De Fontaine, C.S. and DeVolder, A., 2006. Holocene development of boreal forests and fire regimes on the Kenai Lowlands of Alaska. The Holocene, 16(6), pp.791-803.	https://doi.org/10.1191/0959683606hol966rp	Lynch, J.A., Clark, J.S., Bigelow, N.H., Edwards, M.E. and Finney, B.P., 2002. Geographic and temporal variations in fire history in boreal ecosystems of Alaska. Journal of Geophysical Research: Atmospheres, 108(D1), p.8152.	https://doi.org/10.1029/2001JD000332
BLUFFCA	Neotoma	10309	15646	Bluff Lake	-122.559870	41.346515	Western North America	1926	Raw	Lake	32	AWI	0.273	13.798	Bluff Lake lies in a southeast-facing valley on the south side of South China Mountain. Surrounding vegetation: Open forest composed of Pinus jeffreyi, P. contorta, P. monticola, Abies concolor, Calocedrus decurrens, and Pseudotsuga menziesii. Understorey shrubs include Quercus vaccinifolia, Ceanothus prostratus, Arcostaphylos patula, and A. nevadensis.	Mohr, J.A., Whitlock, C. and Skinner, C.N., 2000. Postglacial vegetation and fire history, eastern Klamath Mountains, California, USA. The Holocene, 10(5), pp.587-601.	https://doi.org/10.1191/095968300675837671	Mohr, J.A., 1997. Postglacial vegetation and fire history near Bluff Lake, Klamath Mountains, California. Master's thesis. University of Oregon, Eugene, Oregon, USA.
BUCKBOG	Neotoma	10319	15667	Buckbean Bog	-119.683050	49.119050	Western North America	1803	Raw	Bog	131	AWI	-0.058	11.551	Buckbean Bog occupies a near-circular basin in a depression between two ridges on the north shoulder of Mount Kobau. Surrounding vegetation: The bog is covered by a floating mat of aquatic vegetation (Menyanthes trifoliata, Carex) and is surrounded by patchy nonuniform aged mixtures of lodgepole pine, Engelmann spruce, and subalpine fir.	Heinrichs, M.L., 1999. A late-Quaternary paleoecological analysis in the Engelmann Spruce-Subalpine Fir biogeoclimatic zone of the Okanagan/Ashnola region, British Columbia, Canada. Doctoral dissertation. University of Victoria, Victoria, British Columbia, Canada.		Heinrichs, M.L., Hebda, R.J. and Walker, I.R., 2001. Holocene vegetation and natural disturbance in the Engelmann Spruce Subalpine Fir biogeoclimatic zone at Mount Kobau, British Columbia. Canadian journal of forest research, 31(12), pp.2183-2199.	https://doi.org/10.1139/x01-157
BUNKERCA	Neotoma	10325	15680	Bunker Lake	-120.386415	39.053590	Western North America	1995	Raw	Lake	25	AWI	-0.044	13.776	Bunker Lake lies in a glacially scoured basin. Surrounding vegetation: Forest vegetation around the lake is dominated by white and red fir, with sugar pine, Jeffrey pine, and western white pine also present. Montane chaparral is present in much of the area surrounding Bunker Lake. Close to the lake, the chaparral contains bracken fern, serviceberry, mountain ash, and western azalea. Emergent sedges and submersed quillwort are found in the lake.	Edlund, E.G., 1996. Late Quaternary environmental history of montane forests of the Sierra Nevada. Doctoral dissertation. University of California Berkeley, Berkeley, California, USA.
CRATERBC	Neotoma	10340	15713	Crater Lake	-120.095850	49.192250	Western North America	2101	Raw	Lake	99	AWI	-0.058	12.916	One of a pair of lakes on Crater Mountain, the more northly basin. Surrounding vegetation is parkland forest composed of: Picea engelmannii, Pinus contorta, Abies lasiocarpa. Low shrubs, (mainly Vaccinium scoparium,) herbs (mainly Lupinus arcticus), and grasses make up the understory.	Heinrichs, M.L., Hebda, R.J., Walker, I.R. and Palmer, S.L., 2002. Postglacial paleoecology and inferred paleoclimate in the Engelmann spruce-subalpine fir forest of south-central British Columbia, Canada. Palaeogeography, Palaeoclimatology, Palaeoecology, 184(3-4), pp.347-369.	https://doi.org/10.1016/S0031-0182(02)00274-2
DEADHORS	Neotoma	10341	15715	Dead Horse Lake	-120.775000	42.558000	Western North America	2251	Raw	Lake	27	AWI	-0.042	16.641	Dead Horse Lake is located behind a late-Pleistocene moraine on Dead Horse Rim. Surrounding vegetation: The lake is located in the Tsuga mertensiana zone of the Sierran vegetation series. Surrounded by lodgepole pine, western white pine, and whitebark pine with little understory vegetation. Cercocarpus ledifolius, Artemisia tridentata, rock spirea, and gooseberry are present on rocky slopes near the southeastern lakeshore.	Minckley, T.A., Whitlock, C. and Bartlein, P.J., 2007. Vegetation, fire, and climate history of the northwestern Great Basin during the last 14,000 years. Quaternary Science Reviews, 26(17-18), pp.2167-2184.	https://doi.org/10.1016/j.quascirev.2007.04.009
DUNEAK	Neotoma	10345	15724	Dune Lake	-149.897625	64.421000	Western North America	134	Raw	Lake	70	AWI	-0.047	12.638	Dune Lake lies within a sand dune field that formed 10,000 years ago when dune activity ceased. Surrounding vegetation: Picea/Betula dominated boreal forest. Open-canopy forest is located mostly on well drained south-facing dune slopes, where a mix of white spruce, paper birch, green alder, and occasional black spruce occurs. At the southern end of the lake there is a mixed community of white spruce, black spurce, and patches of hardwood species (paper birch and quaking aspen dominate).	Bigelow, N.H., 1997. Late-Quaternary vegetation and climate in Central Alaska. Doctoral dissertation. University of Alaska, Fairbanks, Alaska, USA.		Lynch, J.A., Clark, J.S., Bigelow, N.H., Edwards, M.E. and Finney, B.P., 2002. Geographic and temporal variations in fire history in boreal ecosystems of Alaska. Journal of Geophysical Research: Atmospheres, 108(D1), pp.8152.	https://doi.org/10.1029/2001JD000332
GRASSYCA	Neotoma	10349	15734	Grassy Lake	-120.664685	39.700855	Western North America	1921	Raw	Lake	26	AWI	-0.041	15.186	Grassy Lake lies in the glacially scoured 'Lakes Basin'. Surrounding vegetation: mixed conifer forest with red and white fir, Jeffrey pine, lodgepole pine, and western white pine. The lake margin is swampy. Quaking aspen, alder, and willow occur along the margin, while a variety of aquatic plants (sedges, pondweed, water lily, quillwort) grow in the lake itself.	Edlund, E.G., 1996. Late Quaternary environmental history of montane forests of the Sierra Nevada. Doctoral dissertation. University of California Berkeley, Berkeley, California, USA.
HARRISSK	Neotoma	10351	15738	Harris Lake	-109.904460	49.666560	Western North America	1230	Raw	Lake	119	AWI	0.240	10.354	Harris Lake is in a meltwater channel that formed approximately 12k years ago. Surrounding vegetation: North of the lake is mixed prairie, while a variety of other upland communities found in the Cypress Hills are also found near the lake.	Sauchyn, M.A. and Sauchyn, D.J., 1991. A continuous record of Holocene pollen from Harris Lake, southwestern Saskatchewan, Canada. Palaeogeography, Palaeoclimatology, Palaeoecology, 88(1-2), pp.13-23.	https://doi.org/10.1016/0031-0182(91)90012-G
LILYCA	Neotoma	10361	15762	Lily Lake	-120.210015	41.976925	Western North America	2047	Raw	Lake	85	AWI	-0.041	11.715	Landslide-dammed lake in the northern Warner Mountains. Surrounding vegetation: Lily Lake lies in the pine-fir zone of the Sierran vegetation series. Forests surrounding the lake are composed of Abies concolor, Pinus ponderosa, Pinus contorta, Pinus monticola, Calocedrus decurrens, and Juniperus occidentalis. Also present in the watershed are Artemisia ludoviciana, Amelanchier pallida, Rosa woodsii, rock spirea, and gooseberry.	Minckley, T.A., Whitlock, C. and Bartlein, P.J., 2007. Vegetation, fire, and climate history of the northwestern Great Basin during the last 14,000 years. Quaternary Science Reviews, 26(17-18), pp.2167-2184.	https://doi.org/10.1016/j.quascirev.2007.04.009
LILYPDCA	Neotoma	10363	15766	Lilypad Lake	-118.994070	36.982290	Western North America	1982	Raw	Lake	34	AWI	-0.047	18.369	Lake in an advanced stage of paludification. Surrounding vegetation: Dominated by ponderosa and jeffrey pine, along with firs, incense cedar, sugar pine, lodgepole pine, and a few black oaks. Alder and willow grow along the lake shore. Most open areas are covered by greenleaf manzanita. Common understory plants include Ceanothus, Ribes, and Symphoricarpos. Within the pond itself, sedges predominate at the margin, while the middle of the pond is densely packed with Nuphar polysepalum.	Edlund, E.G., 1996. Late Quaternary environmental history of montane forests of the Sierra Nevada. Doctoral dissertation. University of California Berkeley, Berkeley, California, USA.
LOSTLKOR	Neotoma	10364	15768	Lost Lake	-123.579300	45.824085	Western North America	452	Raw	Lake	47	AWI	-0.062	8.508	Lost Lake lies on a fault block 30 km east of the Pacific Ocean. Surrounding vegetation: Forest composed primarily of Tsuga heterophylla, Thuja plicata, and Alnus rubra with some Picea sitchensis and Abies grandis. Understory species include Salix spp., Rubus spectabilis, Acer circinatum, with Dryopteris spinulosa on more mesic settings and Pteridium aquillinum in drier disturbed areas.	Long, C.J., Whitlock, C. and Bartlein, P.J., 2007. Holocene vegetation and fire history of the Coast Range, western Oregon, USA. The Holocene, 17(7), pp.917-926.	https://doi.org/10.1177/0959683607082408
MARTENS	Neotoma	10366	15772	Martens Slough (PL-77-20)	-106.381298	52.043500	Western North America	511	Raw	Peat	13	AWI	2.088	13.086	Slough. Physiography: Undulating till plain. Surrounding vegetation: Grasslands and farmland.	Mott, R.J. and Christiansen, E.A., 1981. Palynological study of slough deposits from central Saskatchewan. Current Research, Geological Survey of Canada Paper, 21(1B), pp.133-136.
MCMURRAY_neotoma	Neotoma	10368	15776	McMurray Lake	-120.648640	39.460400	Western North America	1778	Raw	Lake	32	AWI	-0.039	14.859	Surrounding vegetation: Dense forest of white and red fir, sugar pine, western white pine, and ponderosa pine. Black oak and incense cedar are also present near the lake. Alder is common along the southern lake margin.	Edlund, E.G., 1996. Late Quaternary environmental history of montane forests of the Sierra Nevada. Doctoral dissertation. University of California Berkeley, Berkeley, California, USA.
MONOLK	Neotoma	10369	15778	Mono Lake	-119.025500	38.007950	Western North America	1945	Raw	Lake	47	AWI	-0.033	13.151	Mono Lake is a large hypersaline lake at the heart of a closed basin. Surrounding vegetation: Sagebrush scrub. In riparian areas: jeffrey and lodgepole pine, aspen, black cottonwood, willow, wild rose, sweet sage, lupine, and desert paintbrush.	Davis, O.K., 1999. Pollen analysis of a late-glacial and Holocene sediment core from Mono Lake, Mono County, California. Quaternary Research, 52(2), pp.243-249.	https://doi.org/10.1006/qres.1999.2063
MORAINBC	Neotoma	10370	15781	Moraine Bog	-124.900000	51.330000	Western North America	891	Raw	Bog	27	AWI	-0.068	4.602	Small wetland that occupies a closed depression, located north of Tiedemann Glacier. It is bordered on the southwest by the outermost lateral moraine. Surrounding vegetation: Tsuga mertensiana and Abies amabilis dominate the surrounding forest. Abies lasiocarpa, Picea engelmannii, Tsuga heterophylla, and Pinus monticola are also locally present. The understorey consists mainly of Alnus viridis shrubs and a variety of ferns. Sphagnum is present on the wetland surface. Cyperaceae and Menyanthes trifoliata colonize small wet patches in the wetland and open shallow water supports Nuphar lutea.	Arsenault, T.A., Clague, J.J. and Mathewes, R.W., 2007. Late Holocene vegetation and climate change at Moraine Bog, Tiedemann Glacier, southern Coast Mountains, British Columbia. Canadian Journal of Earth Sciences, 44(5), pp.707-719.	https://doi.org/10.1139/e06-135
MS-74-11	Neotoma	10371	15783	Moraine Lake	-124.470000	71.860000	Western North America	30	Raw	Lake	55	AWI	-0.050	12.679	Small lake on moraine, possibly kettle lake. Near the south coast of Banks Island. Surrounding vegetation: Shrub and herb tundra plants.
MS-74-12	Neotoma	10372	15785	Stewert Point Pond	-120.220000	72.351500	Western North America	220	Raw	Lake	33	AWI	0.304	12.158	Small lake near the east coast of Banks Island. Physiography: Hilly glacial deposits. Surrounding vegetation: Herb and shrub tundra plants.	Wang, X.C., 1991. Holocene pollen records of Banks Island, Northwest territories, Canada. A report to the Geological Survey of Canada in partial fulfillment of the requirements for the Contract 23397-0-1626/01-SZ, Geological Survey of Canada.
MS-74-15	Neotoma	10374	15789	Caribou Lake (MS-74-15)	-120.276500	73.513900	Western North America	120	Raw	Lake	62	AWI	0.122	16.230	Small lake in rolling glacial terrain. Surrounding vegetation: Herb and shrub tundra plants.	Wang, X.C., 1991. Holocene pollen records of Banks Island, Northwest territories, Canada. A report to the Geological Survey of Canada in partial fulfillment of the requirements for the Contract 23397-0-1626/01-SZ, Geological Survey of Canada.
NUTELLA	Neotoma	10385	15811	Nutella Lake	-147.391720	63.052000	Western North America	931	Raw	Lake	23	AWI	-0.049	7.450	Treeline altitude lake. Surrounding vegetation: Mesic shrub and heath tundra mixture.	Rohr, M., 2001. Paleoenvironmental changes at treeline: A 6,500 year long pollen and stable isotope record. Master's thesis. University of Alaska, Fairbanks, Alaska, USA.		Edwards, M.E. and Rohr, M., 2005. A 6500-year long pollen record at treeline from Swampbuggy and Nutella Lakes in central Alaska: Pollen records. Bonanza Creek Long-term Ecological Research website.
SWAMPBUG	Neotoma	10386	15814	Swampbuggy Lake	-147.420660	63.054550	Western North America	813	Raw	Lake	38	AWI	-0.064	8.196	Treeline altitude lake. Surrounding vegetation: Open forest. Mesic shrub tundra of mostly alder and some birch.	Rohr, M., 2001. Paleoenvironmental changes at treeline: A 6,500 year long pollen and stable isotope record. Master's thesis. University of Alaska, Fairbanks, Alaska, USA.		Edwards, M.E. and Rohr, M., 2005. A 6500-year long pollen record at treeline from Swampbuggy and Nutella Lakes in central Alaska: Pollen records. Bonanza Creek Long-term Ecological Research website.
TOPLAKE	Neotoma	10408	15872	Top Lake	-130.944895	54.476010	Western North America	33	Raw	Lake	35	AWI	-0.044	15.903	Top Lake is surrounded by blanket bog, rocky outcrops, and some steep areas with scrub forest. Surrounding vegetation: Callitropsis nootkatensis, Pinus contorta, Tsuga heterophylla, Taxus brevifolia, Gaultheria shallon, Ledum, Veratrum viride, Lysichiton americanum, Nuphar polysepalum, Pteridium aquilinum, Empetrum nigrum, Blechnum spicant, Eriophorum chamissonis, Kalmia microphylla occidentalis, Myrica gale, Pinguicula villosa, Vaccinium uliginosum, Viola langsdorfii, and several Sphagnum species.	McLaren, D., Hebda, R.J. and Mackie, Q., 2008. Dundas Island Archipelago vegetation history as reconstructed through pollen analysi. Society for American Archaeology Annual Conference, Society for American Archaeology, Vancouver, British Columbia, Canada.		McLaren, D., 2008. Sea level change and archaeological site locations on the Dundas Island Archipelago of north coastal British Columbia. Doctoral dissertation. University of Victoria, Victoria, British Columbia, Canada.
TULARECA	Neotoma	10410	15876	Tulare Lake	-119.780000	36.052000	Western North America	55	Raw	Lake	83	AWI	-0.032	29.531	At its historic maximum (AD 1770-1850), Tulare Lake was the largest body of fresh water in the United States west of the Mississippi. Diversion of inflowing streams for agriculture resulted in its demise. Surrounding vegetation (pre-settlement): Mosaic of grassland and oak savanna. Scirpus marsh lined the southern margin of the lake and saltbrush scrub covered much of the eastern and western margins.	Davis, O.K., 1999. Pollen analysis of Tulare Lake, California: Great Basin-like vegetation in Central California during the full-glacial and early Holocene. Review of Palaeobotany and Palynology, 107(3-4), pp.249-257.	https://doi.org/10.1016/S0034-6667(99)00020-2
TUMALO	Neotoma	10411	15878	Tumalo Lake	-121.542500	44.021950	Western North America	1543	Raw	Lake	34	AWI	-0.052	11.854	Tumalo Lake lies at the head of a small glacial trough on the eastern flank of the Cascade Range. Surrounding vegetation: dominant arboreal species include Abies grandis, A. amabilis, Picea engelmannii, along with scattered Tsuga mertesiana on moist slopes and Pinus contorta, P. ponderosa, and some P. monticola on dry slopes. Common nonarboreal species include Ceanothus velutinus, Arctostaphylos nevadensis, with Stipa occidentalis and occasional Epilobium angustifolium on open slopes. Shrub and herb cover is minimal under closed pine and fir canopies.	Long, C.J., Power, M.J. and Bartlein, P.J., 2011. The effects of fire and tephra deposition on forest vegetation in the central Cascades, Oregon. Quaternary Research, 75(1), pp.151-158.	https://doi.org/10.1016/j.yqres.2010.08.010
WOODSBC	Neotoma	10421	15902	Woods Lake	-127.269325	51.004365	Western North America	2	Raw	Lake	52	AWI	0.018	14.345	Woods Lake is a small freshwater lake that lies approximately 30 m from the southern shoreline of Seymour Inlet. Surrounding vegetation: Tsuga heterophylla, Picea sitchensis, and Thuja plicata along with Gaultheria shallon in the understory. Poaceae, Cyperaceae, and Gaultheria shallon are common around the lakeshore, with intermittent Ledum groenlandicum and mosses.	Stolze, S., Roe, H.M., Patterson, R.T. and Monecke, T., 2007. A record of Lateglacial and Holocene vegetation and climate change from Woods Lake, Seymour Inlet, coastal British Columbia, Canada. Review of Palaeobotany and Palynology, 147(1-4), pp.112-127.	https://doi.org/10.1016/j.revpalbo.2007.07.002	Stolze, S., 2004. A record of late quaternary vegetation and climate change from Woods Lake, Seymour Inlet, coastal British Columbia, Canada. Master's thesis. Carleton University, Ottawa, Ontario, Canada.
STONEMAN	Neotoma	10449	15967	Stoneman Lake	-111.517775	34.778865	Western North America	2047	Raw	Lake	24	AWI	-0.045	10.140	Lies within a caldera. Physiography: southern edge of the Colorado Plateau. Surrounding vegetation: ponderosa pine.	Hasbargen, J., 1994. A Holocene paleoclimatic and environmental record from Stoneman Lake, Arizona. Quaternary Research, 42(2), pp.188-196.	https://doi.org/10.1006/qres.1994.1068	Hasbargen, J., 1993. The plaeoenvironment of Stoneman Lake, Arizona. Master's thesis. Northern Arizona University, Flagstaff, Arizona, USA.
FAREWELL	Neotoma	10450	15970	Farewell Lake	-153.648820	62.559145	Western North America	320	Raw	Lake	47	AWI	-0.060	12.868	Large lake, glacial origin. Physiography: Moraine and outwash covered piedmont. Surrounding vegetation: Picea sp., Betula papyrifera, Populus sp.	Hu, F.S., Brubaker, L.B. and Anderson, P.M., 1996. Boreal ecosystem development in the northwestern Alaska range since 11,000 yr BP. Quaternary Research, 45(2), pp.188-201.	https://doi.org/10.1006/qres.1996.0019
GRANDPOP	Neotoma	10453	15976	Grandfather Lake	-158.539950	59.796230	Western North America	142	Raw	Lake	40	AWI	-0.040	15.686	Moraine-dammed lake. Physiography: Uplands bordering Nushagak Lowland. Surrounding vegetation: Picea glauca, dense Alnus thickets.	Hu, F.S., Brubaker, L.B. and Anderson, P.M., 1995. Postglacial vegetation and climate change in the northern Bristol Bay region, southwestern Alaska. Quaternary Research, 43(3), pp.382-392.	https://doi.org/10.1006/qres.1995.1044
SECRET	Neotoma	10465	16016	Secret Valley Marsh	-120.265050	40.572000	Western North America	1359	Raw	Marsh	38	AWI	-0.052	11.473	Marsh at north end of Secret Valley. Physiography: Great Basin, volcanic landscape. Surrounding vegetation: Scirpus, Typha, Carex, Juncus.	West, G.J. and McGuire, K.R., 2002. 9,500 years of burning recorded in a high desert marsh. In: Spring-fed Wetlands: Important Scientific and Cultural Resources of the Intermountain Region Conference Proceedings.
LTWILLOW	Neotoma	10473	16054	Little Willow Lake	-121.389935	40.411500	Western North America	1829	Raw	Lake	65	AWI	0.001	16.248	Volcanic basin. Physiography: Cascade volcano field. Surrounding vegetation: lodgepole pine, mountain hemlock. Local vegetation at site: marsh.	West, G.J., 2003, April. A late Pleistocene-Holocene pollen record of vegetation change from Little Willow Lake, Lassen Volcanic National Park, California. In: Proceedings of the Twentieth Annual Pacific Climate Workshop, Asilomar Conference Grounds, Pacific Grove, California (pp. 65-80).
CEDARCA	Neotoma	10476	16061	Cedar Lake	-122.497100	41.207280	Western North America	1737	Raw	Lake	52	AWI	0.129	12.428	Alpine lake. Physiography: Trinity Divide. Surrounding vegetation: pine, fir, cedar, various Ericaceae.	West, G.J., 1989. Late Pleistocene/Holocene vegetation and climate. In: Prehistory of the Sacramento River Canyon, Shasta County, California ed. by M.E. Basgall and W.R. Hildebrandt. Center for Archaeological Research at Davis, Davis, California, USA.
ELKHORN	Neotoma	10477	16063	Elkhorn Slough	-121.764150	36.825350	Western North America	0	Raw	River	20	AWI	-0.036	6.454	Estuarine. Physiography: relic river valley with tectonic action. Surrounding vegetation: Salicornia, Scirpus, Typha, saltgrass.	Dietz, S.A., Hildebrandt, W.R. and Jones, T., 1988. Archaeological investigations at Elkhorn Slough: CA-MNT-229 A Middle Period site on the central California coast. Papers in Northern California Anthropology, Northern California Anthropological Group, Berkeley, California, USA.
PILOTRDG	Neotoma	10478	16065	CA-HUM-558 (Pilot Ridge)	-123.669100	40.661700	Western North America	1250	Raw	Peat	37	AWI	0.060	5.482	Marsh. Physiography: North Coast Ranges. Surrounding vegetation: Douglas fir, pine, oak, cedar, white fir.	Hildebrandt, W.R. and Hayes, J.F., 1983. Archaeological investigations on Pilot Ridge Six Rivers National Forest. U.S. Forest Service Contract 53-9JHA-2-140, Anthropological Studies Center Sonoma State University and Center for Anthropological Research San Jose State University, San Jose, California, USA.
TULE	Neotoma	10482	16073	Tule Lake	-123.035480	39.489633	Western North America	1340	Raw	Lake	24	AWI	-0.031	9.838	Landslide dammed lake. Physiography: Klamath Ranges, mountain ridges. Surrounding vegetation: sedges, pine, fir, oak, cedar.	West, G.J., 1982. Pollen analysis of sediments from Tule Lake: A record of Holocene vegetation/climatic changes in the Mendocino National Forest, California. In: Proceedings of the Symposium of Climate and Archeology of California's Coast and Desert. San Diego, California, USA.		West, G.J., 1993. The late Pleistocene-Holocene pollen record and prehistory of California's north coast ranges. In: There Grows a Green Tree: Papers in Honor of David A Fredrickson ed. by G. White, P. Mikkelsen, W.R. Hildebrandt, and M.E. Basgall (pp.219-235). Center for Archaeological Research, Davis, California, USA.
GRASSCA	Neotoma	10483	16075	Grass Lake	-122.167150	41.649600	Western North America	1537	Raw	Lake	184	AWI	0.516	35.183	Valley blocked by volcanic deposits. Physiography: Cascade Range. Surrounding vegetation: pine, juniper, sagebrush.	Hakala, K.J. and Adam, D.P., 2004. Late Pleistocene vegetation and climate in the southern Cascade Range and the Modoc Plateau region. Journal of Paleolimnology, 31(2), pp.189-215.	https://doi.org/10.1023/B:JOPL.0000019231.58234.fb
COOKBANK	Neotoma	10493	16096	Cook Bank	-128.400000	51.000000	Western North America	0	Raw	Marine	3	AWI	11.484	11.888	Paleosol with rooted conifer remains at a water depth of 95 m. This terrestrial surface on the continental shelf was exposed when relative sea level was 95 m lower than modern. Modern physiography: submarine valley.	Lacourse, T., Mathewes, R.W. and Fedje, D.W., 2003. Paleoecology of late-glacial terrestrial deposits with in situ conifers from the submerged continental shelf of western Canada. Quaternary Research, 60(2), pp.180-188.	https://doi.org/10.1016/S0033-5894(03)00083-8	Luternauer, J.L., Clague, J.J., Conway, K.W., Barrie, J.V., Blaise, B. and Mathewes, R.W., 1989. Late Pleistocene terrestrial deposits on the continental shelf of western Canada: Evidence for rapid sea-level change at the end of the last glaciation. Geology, 17(4), pp.357-360.	https://doi.org/10.1130/0091-7613(1989)017%3C0357:LPTDOT%3E2.3.CO;2
LOGANIN	Neotoma	10494	16099	Logan Inlet	-131.689722	52.780417	Western North America	0	Raw	Marine	26	AWI	11.465	13.316	Formerly subaerial basin. Physiography: Submerged shelf.	LaCourse, T. and Mathewes, R.W., 2005. Terrestrial paleoecology of Haida Gwaii and the continental shelf: Vegetation, climate, and plant resources of the coastal migration route. In: Haida Gwaii: Human History and Environment from the Time of Loon to the Time of the Iron People ed. by D.W. Fedje and R.W. Mathewes (pp.38-58). UBC Press, Vancouver, British Columbia, Canada.		Lacourse, T., 2004. A Late-Pleistocene pollen record from the continental shelf of western Canada. Current Research in the Pleistocene, 21, pp.87-89.
GRAYSGL1	Neotoma	10500	16111	Grays Lake	-111.437950	43.066190	Western North America	1195	Raw	Lake	135	AWI	1.470	69.607	Tectonic origin. Physiography: lava flows and sedimentary rocks. Surrounding vegetation: marsh, scirpus americanus.	Beiswenger, J.M., 1987. Late quaternary vegetational history of Grays Lake, Idaho and the Ice Slough, Wyoming. Doctoral dissertation. University of Wyoming, Laramie, Wyoming, USA.		Beiswenger, J.M., 1991. Late quaternary vegetational history of Grays Lake, Idaho. Ecological Monographs, 61(2), pp.165-182.	https://doi.org/10.2307/1943006
GRAYSGL6	Neotoma	10500	16113	Grays Lake	-111.437950	43.066190	Western North America	1195	Raw	Lake	56	AWI	4.844	66.739	Tectonic origin. Physiography: lava flows and sedimentary rocks. Surrounding vegetation: marsh, scirpus americanus.	Beiswenger, J.M., 1987. Late quaternary vegetational history of Grays Lake, Idaho and the Ice Slough, Wyoming. Doctoral dissertation. University of Wyoming, Laramie, Wyoming, USA.		Beiswenger, J.M., 1991. Late quaternary vegetational history of Grays Lake, Idaho. Ecological Monographs, 61(2), pp.165-182.	https://doi.org/10.2307/1943006
LOSPENAS	Neotoma	10501	16115	Los Penasquitos Lagoon	-117.252870	32.931121	Western North America	0	Raw	Lagoon	17	AWI	-0.021	3.820	Medium sized estuary. Physiography: Estuary. Surrounding vegetation: Pinus torreyana.	Cole, K.L. and Wahl, E., 2000. A late Holocene paleoecological record from Torrey Pines state reserve, California. Quaternary Research, 53(3), pp.341-351.	https://doi.org/10.1006/qres.1999.2121
MISSIONX	Neotoma	10507	16131	Mission Cross Bog	-115.483650	41.784700	Western North America	2424	Raw	Lake	41	AWI	-0.025	9.845	Spring-fed fen. Growing on the fen are Sphagnum, sedges, Menyanthes trifoliata, Pedicularis groenlandica, Thalictrum spp., and Salix spp. On the northern slope bordering the fen, fields of Balsamorhiza sagittata grow with Lupinus. To the east, south, and west are scattered stands of Populus tremuloides.	Thompson, R.S., 1984. Late Pleistocene and Holocene environments in the Great Basin. Doctoral dissertation. University of Arizona, Tucson, Arizona, USA.
RUBYMRSH	Neotoma	10508	16133	Ruby Marsh	-115.504900	41.133950	Western North America	1818	Raw	River	64	AWI	-0.033	37.954	Spring-fed marsh/shallow lake. Physiography: valley bottom near toeslope. Surrounding vegetation: Artemisia, Chrysothamnus, Juniperus, Pinus. Local vegetation: Dasyphora, Distichilis, Juncus, Typha.	Thompson, R.S., 1984. Late Pleistocene and Holocene environments in the Great Basin. Doctoral dissertation. University of Arizona, Tucson, Arizona, USA.		Thompson, R.S., 1992. Late Quaternary environments in Ruby Valley, Nevada. Quaternary Research, 37(1), pp.1-15.	https://doi.org/10.1016/0033-5894(92)90002-Z	Thompson, R.S., Toolin, L.J., Forester, R.M. and Spencer, R.J., 1990. Accelerator-mass spectrometer (AMS) radiocarbon dating of Pleistocene lake sediments in the Great Basin. Palaeogeography, Palaeoclimatology, Palaeoecology, 78(3-4), pp.301-313.	https://doi.org/10.1016/0031-0182(90)90219-W
BENICIA	Neotoma	10519	16184	Benicia State Park	-122.193056	38.073472	Western North America	0	Raw	Marsh	26	AWI	-0.018	1.469	Tidal marsh. Physiography: San Francisco Bay estuary, north side. Surrounding vegetation: Salicornia virginica, Distichlis spicata.	Malamud-Roam, F. and Ingram, B.L., 2004. Late Holocene 13C and pollen records of paleosalinity from tidal marshes in the San Francisco Bay estuary, California. Quaternary Research, 62(2), pp.134-145.	https://doi.org/10.1016/j.yqres.2004.02.011
CHINACMP	Neotoma	10520	16186	China Camp	-122.493333	38.007500	Western North America	0	Raw	Marsh	33	AWI	0.005	3.710	Tidal marsh. Physiography: San Pablo Bay, SF Bay estuary. Surrounding vegetation: Scirpus spp, Typha latifolia, Salicornia virginica.	Goman, M., Malamud-Roam, F. and Ingram, B.L., 2008. Holocene environmental history and evolution of a tidal salt marsh in San Francisco Bay, California. Journal of Coastal Research, 24(5), pp.1126-1137.	https://doi.org/10.2112/08A-0005.1	Malamud-Roam, F. and Ingram, B.L., 2004. Late Holocene 13C and pollen records of paleosalinity from tidal marshes in the San Francisco Bay estuary, California. Quaternary Research, 62(2), pp.134-145.	https://doi.org/10.1016/j.yqres.2004.02.011
MOUNTAIN	Neotoma	10522	16197	Mountain Lake	-122.470765	37.788260	Western North America	37	Raw	Lake	54	AWI	-0.051	1.618	Dune lake carved by wind action. Physiography: Relic dune field, low hills. Surrounding vegetation: Monterey Pine, Blue gum, Cypress, Willow.	Reidy, L.M., 2001. Evidence of environmental change over the last 2000 years at Mountain Lake, in the northern San Francisco Peninsula, California. Master's thesis. University of California at Berkeley, Berkeley, California, USA.
BLACKMTN	Neotoma	10531	16222	Black Mountain Lake	-107.235360	37.846820	Western North America	3413	Raw	Lake	32	AWI	8.984	15.073	High elevation lake 100-15 m below timberline in the San Juan Mountains. Local vegetation Picea engelmannii/Abies lasiocarpa forest.	Jodry, M.A.B., 1999. Paleoindian stage paleoecological records. In: Colorado prehistory: a context for the Rio Grande Basin ed. by M.A. Martorano, T. Hoeffer III, M.A. Jodry, V. Spero, and M.L. Taylor (pp.12-26). Colorado Council of Professional Archaeologists, Denver, Colorado, USA.		Jodry, M.A.B., 1999. Folsom technological and socioeconomic strategies: views from Stewart's Cattle Guard and the Upper Rio Grande Basin, Colorado. Doctoral dissertation. American University, Washington, D.C., USA.		Reasoner, M.A. and Jodry, M.A., 2000. Rapid response of alpine timberline vegetation to the Younger Dryas climate oscillation in the Colorado Rocky Mountains, USA. Geology, 28(1), pp.51-54.	https://doi.org/10.1130/0091-7613(2000)28%3C51:RROATV%3E2.0.CO;2
SKYPOND	Neotoma	10532	16224	Sky Pond	-105.669170	40.277895	Western North America	3320	Raw	Lake	34	AWI	9.025	14.230	Cirque lake directly above timberline. Physiography: Black Mountains.	Reasoner, M.A. and Jodry, M.A., 2000. Rapid response of alpine timberline vegetation to the Younger Dryas climate oscillation in the Colorado Rocky Mountains, USA. Geology, 28(1), pp.51-54.	https://doi.org/10.1130/0091-7613(2000)28%3C51:RROATV%3E2.0.CO;2
REDGREEN	Neotoma	10537	16236	Red Green Lake	-149.681235	68.654210	Western North America	668	Raw	Lake	38	AWI	-0.049	8.474	Irregular topography, coarse soils. Physiography: Arctic Foothills. Surrounding vegetation: Sedges, prostrate shrubs, mosses.	Oswald, W.W., Brubaker, L.B., Hu, F.S. and Kling, G.W., 2003. Holocene pollen records from the central Arctic Foothills, northern Alaska: testing the role of substrate in the response of tundra to climate change. Journal of Ecology, 91(6), pp.1034-1048.	https://doi.org/10.1046/j.1365-2745.2003.00833.x
TUKUTO	Neotoma	10538	16238	Tukuto Lake	-157.030100	68.498800	Western North America	505	Raw	Lake	72	AWI	0.022	36.605	Rolling hills within morainal ridges. Physiography: Arctic Foothills. Surrounding vegetation: Betula, Eriophorum, Vaccinum, Ledum, Salix.	Oswald, W.W., Brubaker, L.B. and Anderson, P.M., 1999. Late Quaternary vegetational history of the Howard Pass area, northwestern Alaska. Canadian Journal of Botany, 77(4), pp.570-581.	https://doi.org/10.1139/b99-027
UPPERCAP	Neotoma	10539	16241	Upper Capsule Lake	-149.416925	68.631444	Western North America	805	Raw	Lake	48	AWI	-0.055	12.045	Gently rolling topography, fine soils. Physiography: Arctic Foothills. Surrounding vegetation: Dwarf shrubs, tussock sedge, sphagnum.	Oswald, W.W., Brubaker, L.B., Hu, F.S. and Kling, G.W., 2003. Holocene pollen records from the central Arctic Foothills, northern Alaska: testing the role of substrate in the response of tundra to climate change. Journal of Ecology, 91(6), pp.1034-1048.	https://doi.org/10.1046/j.1365-2745.2003.00833.x
CYCLOID1	Neotoma	527	17292	Cycloid Lake	-105.266667	55.266667	Western North America	369	Raw	Lake	39	AWI	-0.054	10.145	NA	Mott, R.J., 1973. Palynological studies in central Saskatchewan. Pollen stratigraphy from lake sediment sequences. Geological Survey of Canada, Ottawa, Ontario, Canada, pp.49-72.
CLEVELND	Neotoma	11560	17296	Lake Cleveland	-113.649550	42.321290	Western North America	2519	Raw	Lake	32	AWI	-0.031	16.407	Cirque lake which is morainally dammed. Physiography: Mount Harrison, south edge of Snake River Plain. Surrounding vegetation: Abies lasiocarpa, Pinus contorta.	Davis, O.K., 1981. Vegetation migration in southern Idaho during the late Quaternary and Holocene. Doctoral dissertation. University of Minnesota, Minneapolis, Minnesota, USA.		Davis, O.K., Sheppard, J.C. and Robertson, S., 1986. Contrasting climatic histories for the Snake River Plain, Idaho, resulting from multiple thermal maxima. Quaternary Research, 26(3), pp.321-339.	https://doi.org/10.1016/0033-5894(86)90093-1
MIDBUTTE	Neotoma	3585	17298	Middle Butte Cave	-112.616667	43.366667	Western North America	1590	Raw	Cave	21	AWI	3.188	34.476	NA	Davis, O.K., Sheppard, J.C. and Robertson, S., 1986. Contrasting climatic histories for the Snake River Plain, Idaho, resulting from multiple thermal maxima. Quaternary Research, 26(3), pp.321-339.	https://doi.org/10.1016/0033-5894(86)90093-1	McDonald, H.G., Anderson, E., White, J.A. and Soiset, J.M., 1980. Lava blisters as carnivore traps. Geological Society of America Abstracts with Programs 12, p.280.
IDAVAIN	Neotoma	11571	17320	Idavain Lake	-155.945095	58.772294	Western North America	223	Raw	Lake	57	AWI	-0.010	17.274	NA	Brubaker, L.B., Anderson, P.M. and Hu, F.S., 2001. Vegetation ecotone dynamics in southwest Alaska during the late Quaternary. Quaternary Science Reviews, 20(1-3), pp.175-188.	https://doi.org/10.1016/S0277-3791(00)00124-4
SNIPE	Neotoma	11572	17322	Snipe Lake	-154.303475	60.626010	Western North America	579	Raw	Lake	28	AWI	0.337	14.406	Morainally dammed lake. Physiography: rolling foothills. Surrounding vegetation: open Picea forest and Betula/Alnus shrub tundra. Isolated stands of Picea glauca occur in mixtures with Betula glandulosa shrubs and Alnus crispa thickets.	Brubaker, L.B., Anderson, P.M. and Hu, F.S., 2001. Vegetation ecotone dynamics in southwest Alaska during the late Quaternary. Quaternary Science Reviews, 20(1-3), pp.175-188.	https://doi.org/10.1016/S0277-3791(00)00124-4
IMNAVAIT	Neotoma	11573	17324	Imnavait Creek	-149.358787	68.666190	Western North America	875	Raw	Bog	24	AWI	0.179	12.954	String bog formed in creek basin. Physiography: surrounded by till-covered hills. Surrounding vegetation: Dwarf birch, Cyperaceae.	Eisner, W.R., 1991. Palynological analysis of a peat core from Imnavait Creek, the North Slope, Alaska. Arctic, 44, pp.279-282.
OILLAKE	Neotoma	11574	17326	Oil Lake	-151.166806	70.292222	Western North America	745	Raw	Lake	41	AWI	-0.047	59.805	Lake basin overlying mid-Pleistocene til. Physiography: rolling uplands, Brooks Range foothills. Surrounding vegetation: various tundra communities.	Eisner, W.R. and Colinvaux, P.A., 1992. Late Quaternary pollen records from Oil Lake and Feniak Lake, Alaska, USA. Arctic and Alpine Research, 24(1), pp.56-63.	https://doi.org/10.2307/1551320
SANDSZ	Neotoma	11575	17328	Sands of Time Lake	-147.553310	66.029335	Western North America	242	Raw	Lake	35	AWI	-0.050	26.775	Lake in swale between low hills. Physiography: gently rolling loess mantled upland. Surrounding vegetation: black and white spruce forest.	Edwards, M.E. and Barker Jr, E.D., 1994. Climate and vegetation in northeastern Alaska 18,000 yr BP-present. Palaeogeography, Palaeoclimatology, Palaeoecology, 109(2-4), pp.127-135.	https://doi.org/10.1016/0031-0182(94)90172-4
SITHYLEM	Neotoma	11579	17338	Sithylemenkat Lake	-151.391555	66.123990	Western North America	213	Raw	Lake	51	AWI	0.169	16.877	NA	Anderson, P.M., Reanier, R.E. and Brubaker, L.B., 1990. A 14,000-year pollen record from Sithylemenkat Lake, north-central Alaska. Quaternary Research, 33(3), pp.400-404.	https://doi.org/10.1016/0033-5894(90)90065-S
WINDMILB	Neotoma	11585	17352	Windmill Lake	-148.805250	63.658900	Western North America	615	Raw	Lake	85	AWI	0.053	16.518	In moraine-dammed bedrock basin w/sedge. Physiography: moraine-mantled diabase ridge. Surrounding vegetation: birch, spruce, willow, tussocks.	Bigelow, N.H., 1997. Late-Quaternary vegetation and climate in Central Alaska. Doctoral dissertation. University of Alaska, Fairbanks, Alaska, USA.
BLAIR	Neotoma	11586	17354	Blair Lakes	-147.368165	64.360080	Western North America	257	Raw	Lake	19	AWI	0.185	13.689	Surrounding vegetation: Picea, Betula, Populus, Salix, Alnus. Northern boreal forest.
CLAMGULC	Neotoma	11588	17357	Clam Gulch	-151.362935	60.223930	Western North America	86	Raw	Lake	25	AWI	1.487	8.871	Surrounding vegetation: Picea mariana, Betula papyrifera, Alnus.
EIGHTMIL	Neotoma	11589	17359	Eightmile Lake	-149.251800	63.888645	Western North America	648	Raw	Lake	14	AWI	0.032	9.307	Physiography: Northern foothills of the Alaska Range. Vegetation at the site is dominated by the tussock-forming sedge, Eriophorum vaginatum, and deciduous shrub, Vaccinium uliginosum
HOMER	Neotoma	11596	17375	Homer Beach	-151.511900	59.633900	Western North America	10	Raw	Marine	26	AWI	0.111	13.865	NA
LONGMERE	Neotoma	11597	17377	Longmere Lake	-150.909920	60.500895	Western North America	78	Raw	Lake	48	AWI	0.000	13.299	NA
MOSQML1	Neotoma	11599	17381	Mosquito Pond	-145.540150	63.986445	Western North America	379	Raw	Lake	17	AWI	0.087	11.559	NA
OTTO_neotoma	Neotoma	11600	17383	Otto Lake	-149.035575	63.842250	Western North America	548	Raw	Lake	34	AWI	-0.018	6.587	NA
WATANA	Neotoma	11601	17385	Watana Triangle Pond	-148.247010	62.842885	Western North America	546	Raw	Lake	24	AWI	0.154	16.399	NA
ZAGOSKIN	Neotoma	11604	17391	Zagoskin Lake	-162.108380	63.448470	Western North America	7	Raw	Lake	151	AWI	0.051	43.037	Maar crater. Physiography: Basalt flows and pyroclastic deposits. Surrounding vegetation: Dwarf birch, blueberry, willow, sedges.	Ager, T.A., 2003. Late Quaternary vegetation and climate history of the central Bering land bridge from St. Michael Island, western Alaska. Quaternary Research, 60(1), pp.19-32.	https://doi.org/10.1016/S0033-5894(03)00068-1
SOUTHMEL	Neotoma	11608	17400	South Lake	-121.428540	69.080765	Western North America	775	Raw	Lake	22	AWI	-0.046	15.445	Lake appears to have resulted from impoundment by glacial deposits that run along its sourth shore. Surrounding vegetation: Herb tundra with scattered willows (Salix arctica). Dwarf birch (Betula glandulosa) is widespread in the surrounding lowlands.	Ruhland, K., Jacques, J.M.S., Beierle, B.D., Lamoureux, S.F., Dyke, A.S. and Smol, J.P., 2009. Lateglacial and Holocene paleoenvironmental changes recorded in lake sediments, Brock Plateau (Melville Hills), Northwest Territories, Canada. The Holocene, 19(7), pp.1005-1016.	https://doi.org/10.1177/0959683609340999
LITSWIFT	Neotoma	11609	17402	Little Swift Lake	-159.765670	60.216475	Western North America	572	Raw	Lake	35	AWI	0.000	12.814	Lake at the mouth of a valley tributary. Dammed by a lateral moraine. Surrounding vegetation: Betula nana, Salix spp., Polypodiaceae, Cyperaceae, Poaceae, Lycopodium, Sphagnum.	Axford, Y. and Kaufman, D.S., 2004. Late glacial and Holocene glacier and vegetation fluctuations at Little Swift Lake, Southwestern Alaska, USA. Arctic, Antarctic, and Alpine Research, 36(2), pp.139-146.	https://doi.org/10.1657/1523-0430(2004)036%5B0139:LGAHGA%5D2.0.CO;2
CUMBRES	Neotoma	11617	17419	Cumbres Bog	-106.450520	37.021745	Western North America	3100	Raw	Bog	75	AWI	0.268	19.798	Cumbres Bog lies ~40 km south of the upper Conejos River Valley, in the San Juan Mountains, and is situated near the headwaters of the Cumbres River. The small basin containing the bog is elevated slightly above the Cumbres River with no fluvial inputs. The bog is dammed by a recessional moraine formed by the Cumbres Glacier during the LGM. Surrounding vegetation: Modern vegetation in the San Juan Mountains is characterized. by Pinus edulis (Colorado pinon) - Juniperus monosperma (oneseed juniper) woodlands that occur on the lower slopes of the range from ~1800 to 2400 m. An upper montane coniferous forest, from ~2400 to 2700 m, features Pseudotsuga menziesii (Douglas fir), Abies concolor (white fir), Pinus strobiformis. (southwestern white pine), Pinus ponderosa (ponderosa pine), Picea pungens (Colorado blue spruce), Populus tremuloides (quaking aspen), Quercus gambelii (Gambel oak) and Acer glabrum (Rocky Mountain maple). Above 2700 m, a subalpine coniferous forest occurs with Picea engelmannii (Engelmann spruce) and Abies lasiocarpa (subalpine fir) as the most diagnostic trees. Vegetation above ~3500 m (treeline) is characterized by alpine tundra.	Johnson, B.G., 2010. Alpine and subalpine landscape response to post-glacial climate change in the San Juan mountains: A comparison of new landscape and climate records. Doctoral dissertation. University of North Carolina, Charlotte, North Caroline, USA.		Johnson, B.G., Eppes, M.C., Diemer, J.A., Jimenez-Moreno, G. and Layzell, A.L., 2011. Post-glacial landscape response to climate variability in the southeastern San Juan Mountains of Colorado, USA. Quaternary Research, 76(3), pp.352-362.	https://doi.org/10.1016/j.yqres.2011.08.006
LAKEASK	Neotoma	11747	17711	Lake A	-105.055315	55.331190	Western North America	378	Raw	Lake	62	AWI	-0.033	10.997	Small unnamed lake alongside the road. The lake is surrounded by predominantly black spruce forest. Much of the area surrounding the lake is covered by treed black spruce bog or open muskeg.	Wilson, M.A., 1981. The climatic and vegetational history of the postglacial in central Saskatchewan. Doctoral dissertation. University of Saskatchewan, Saskatoon, Saskatchewan, Canada.
NANISKAK	Neotoma	11748	17713	West Naniskak Lake	-104.938605	55.430905	Western North America	418	Raw	Lake	40	AWI	-0.030	9.565	West Naniskak Lake is the western basin of the Naniskak Lakes. The lake is surrounded by coniferous forest, with the dominant species being jackpine and aspen. There are some small areas of treed muskeg (black spruce bog) near to the lake, the main one being at the north end.	Wilson, M.A., 1981. The climatic and vegetational history of the postglacial in central Saskatchewan. Doctoral dissertation. University of Saskatchewan, Saskatoon, Saskatchewan, Canada.
KEALIA	Neotoma	11786	17832	Kealia Pond	-156.475355	20.794290	Western North America	0	Raw	Lake	34	AWI	0.009	2.614	Coastal lagoon with a sandy beach barrier. Surrounding vegetation: primarily Batis maritima (pickleweed) with a few isolated individuals of Prosopis pallida (kiawe) and Acacia farnesiana (klu) along the sand dunes to the south. Large sugarcane fields surround the site to the northwest.	Pau, S., MacDonald, G.M. and Gillespie, T.W., 2012. A dynamic history of climate change and human impact on the environment from Kealia Pond, Maui, Hawaiian Islands. Annals of the Association of American Geographers, 102(4), pp.748-762.	https://doi.org/10.1080/00045608.2011.652853
PELONCIL	Neotoma	11792	17859	Peloncillo Mountains	-109.094167	32.289083	Western North America	1400	Raw	Peat	36	AWI	0.088	34.041	The Peloncillo Mountains Wilderness Area is part of the Mexican Highland section of the Basin and Range Physiographic Province, which is characterized by several northwest-southeast trending fault-block ranges separated by closed topographic basins. Vegetation in the valleys and along the bajadas consists of Larrea tridentata with lesser amounts of Prosopis glandulosa, Acacia constricta, Flournesia. cernua, and Atriplex canescens. Hillslope. vegetation is dominated by L. tridentata, A. constricta, Parthenium incanum, F. cernua, Opuntia, Fouquieria splendens, Isocoma tenuisecta, and Pleuraphis cf. mutica. Other hillslope vegetation includes a variety of. shrubs and herbs (Abutilon incanum, Acacia greggii,Acourtia nana, Asclepias linearis, Calliandra, Castilleja, Celtis pallida, Cryptantha, Dasylirion wheeleri, Daucus, Descurainia, Ephedra trifurca, Eriogonum, Gutierrezia sarothrae, Hibiscus, Lepidium, Nolina. microcarpa, Plantago, Rhus microphylla, Senecio, Senna, Simmondsia chinensis, Sphaeralcea, Trixis californica, and Ziziphus obtusifolia), cacti and succulents. (Cylindropuntia spinosior, Opuntia phaeacanthatype, Opuntia leptocaulis, Mammilllaria, Peniocereus greggii, Ferocactus wislizenii, Yucca baccata, and Yucca. elata), and grasses (Aristida, Bothriochloa barbinodis, Bouteloua curtipendula, and Bouteloua gracilis). Juniperus cf. coahuilensis and Quercus cf. turbinella are rare, but present at the higher elevations in our study area. Near our midden sites, Celtis reticulata and Sapindus drummondii are each represented by a single. tree along a small mesic rock shelf with an intermittent spring. The presence of S. chinensis is notable because it represents an outlier population of this species, lying. 40 km east of the nearest populations.	Holmgren, C.A., Betancourt, J.L. and Rylander, K.A., 2006. A 36,000-yr vegetation history from the Peloncillo Mountains, southeastern Arizona, USA. Palaeogeography, Palaeoclimatology, Palaeoecology, 240(3-4), pp.405-422.	https://doi.org/10.1016/j.palaeo.2006.02.017
MITKOF	Neotoma	11854	17945	Mitkof Island	-132.936240	56.811570	Western North America	20	Raw	Peat	32	AWI	-0.055	12.729	Peat deposits near Petersburg, on Mitkof Island in the southern Alexander Archipelago of southeastern Alaska. Mitkof Island is separated from the west flank of the Coast Mountains of southeastern Alaska and by Frederick Sound to the east and north. Kupreanof Island lies immediately west of Mitkof Island. Surrounding vegetation: Most of Mitkof Island is covered by Pacific coastal rainforest interspersed with muskeg (bog and fen peatlands). The most common tree species on the island are western hemlock (Tsuga heterophylla) and Sitka spruce (Picea sitchensis). Mountain hemlock (Tsuga mertensiana) is common, particularly in upland forests. Also present are shore pine (Pinus. contorta ssp. contorta), yellow cedar (Chamaecyparis nootkatensis), and occasional red cedar (Thuja plicata). Red alder trees (Alnus rubra) and Sitka alder shrubs (Alnus crispa ssp. sinuata) are important elements of the island's vegetation. Red alder trees are common in lowlands, while Sitka alder shrubs often form dense thickets along rocky coastlines, along stream banks, in avalanche scars, at forest edges, and in the subalpine zone.	Ager, T.A., Carrara, P.E., Smith, J.L., Anne, V. and Johnson, J., 2010. Postglacial vegetation history of Mitkof Island, Alexander Archipelago, southeastern Alaska. Quaternary Research, 73(2), pp.259-268.	https://doi.org/10.1016/j.yqres.2009.12.005
BLUENV	Neotoma	11924	18106	Blue Lakes	-118.717135	41.679460	Western North America	2437	Raw	Lake	60	AWI	0.228	3.602	The Blue Lakes are located in the Pine Forest Mountains of northwest, NV. The surrounding vegetation composition is variable; limber pine, sagebrush (Artemisia sp.), mountain mahogany (Cercocarpus ledifolius), and grasses dominate most of the upland vegetation. Spatially, sagebrush steppe dominates the southeastfacing slope and a limber-pine forest the northwest-facing slope. Immediately surrounding the lakes is a quaking-aspen (Populus tremuloides) fringe.	Shriver, R.K. and Minckley, T.A., 2012. Late-Holocene response of limber pine (Pinus flexilis) forests to fire disturbance in the Pine Forest Range, Nevada, USA. Quaternary Research, 78(3), pp.465-473.	https://doi.org/10.1016/j.yqres.2012.07.010
NEL03	Neotoma	11925	18108	NEL03	-116.905000	49.496405	Western North America	2074	Raw	Lake	39	AWI	-0.051	9.602	NEL03 (unofficial name) is a small, subalpine cirque lake. The lake is within the Engelmann spruce-subalpine fir wet cold forest zone, dominated by subalpine fir (A. lasiocarpa), subalpine larch (Larix lyallii), Engelmann spruce (P. engelmannii); and some whitebark pine (Pinus albicaulis). Arboreal coverage is moderately dense and there is a significant understory of herbs, forbs, sedges, grasses and shrubs.	Mustaphi, C.J.C. and Pisaric, M.F., 2014. Holocene climate-fire-vegetation interactions at a subalpine watershed in southeastern British Columbia, Canada. Quaternary Research, 81(2), pp.228-239.	https://doi.org/10.1016/j.yqres.2013.12.002
PYATTS	Neotoma	11934	18127	Pyatts Lake	-115.769585	49.469660	Western North America	1080	Raw	Lake	19	AWI	0.067	6.912	Surrounding vegetation: Interior douglas fir forest.	Mustaphi, C.J.C. and Pisaric, M.F., 2014. A classification for macroscopic charcoal morphologies found in Holocene lacustrine sediments. Progress in Physical Geography, 38(6), pp.734-754.	https://doi.org/10.1177/0309133314548886	Mustaphi, C.C., Gedalof, Z.E., Daniels, L. and Pisaric, M., 2015. Paleoecological and sedimentological data from:\a classification for macroscopic charcoal morphologies found in Holocene lacustrine sediments\. Open Quaternary, 1(1).
MODPOND	Neotoma	11950	18159	Mod Pond	-120.586190	34.787670	Western North America	21	Raw	Lake	28	AWI	-0.063	2.789	Mod Pond is a small perennial pond. Surrounding vegetation: Coastal sage scrub. The dominant species is Artemisia californica. Other dominant species in this vegetation type include Eriogonum parvifolium, Salvia mellifera, Lotus scoparius, Baccharis pilularis, Toxicodendron diversilobum, as well as many other perennial and annual herbs. In addition to the above-listed coastal sage scrub plants, the local vegetation around Mod Pond includes A. californica, T. diversilobum, Lupinus sp., B. pilularis, S. mellifera and others growing on the dunes around the lake. Salix grows at the lake shoreline, with a grove of Eucalyptus trees. ca. 100 m to the north of the pond.	Anderson, R.S., Ejarque, A., Rice, J., Smith, S.J. and Lebow, C.G., 2015. Historic and Holocene environmental change in the San Antonio Creek Basin, mid-coastal California. Quaternary Research, 83(2), pp.273-286.	https://doi.org/10.1016/j.yqres.2014.11.005
TK-2-96	Neotoma	11928	19323	TK-2 Lake	-104.945735	66.347840	Western North America	234	Raw	Lake	55	AWI	0.140	9.143	Lake on Precambrian shield rocks. Upland supports a highly discontinuous cover of predominantly dwarf shrub-lichen vegetation. Dominant vascular plants are Betula glandulosa, Salix species, and species of the ericoid genera Arctostaphylos, Ledum and Vaccinium. The lake is within the distribution limit of Alnus but no Alnus was noted within the immediate vicinity of the lake. Poorly drained sites support peat with permafrost and associated patterned ground. dominated by sedges, cottongrasses, shrubs and mosses.	Seppa, H., Cwynar, L.C. and MacDonald, G.M., 2003. Post-glacial vegetation reconstruction and a possible 8200 cal. yr BP event from the low arctic of continental Nunavut, Canada. Journal of Quaternary Science, 18(7), pp.621-629.	https://doi.org/10.1002/jqs.793
PANTHPOT	Neotoma	13042	19358	Panther Potholes	-121.040950	48.658990	Western North America	1100	Raw	Lake	58	AWI	-0.007	10.631	Surrounding vegetation: The montane forest surrounding the Panther Potholes is transitional between low-elevation assemblages of Pseudotsuga menziesii, Thuja plicata, and Tsuga heterophylla, and high-elevation assemblages of Abies amabilis, A. lasiocarpa, Chamaecyparis nootkatensis, Picea. engelmannii, Pinus monticola, and Tsuga mertensiana. A. lasiocarpa is common along the lakeshore, and A. amabilis, P. menziesii, T. heterophylla, and T. plicata are common associates in upland forests. Numerous snags of P. monticola, associated with a white pine blister rust outbreak, indicate that this species was until recently a common stand associate. Pinus contorta is uncommon within the immediate study area but is locally abundant within 0.5 km of the study site along. a glacially carved ridgeline with shallow soils. Alnus sinuata is present on the lakeshore but is absent in upland forests.	Prichard, S.J., Gedalof, Z.E., Oswald, W.W. and Peterson, D.L., 2009. Holocene fire and vegetation dynamics in a montane forest, North Cascade Range, Washington, USA. Quaternary Research, 72(1), pp.57-67.	https://doi.org/10.1016/j.yqres.2009.03.008
TROUTYUK	Neotoma	13288	19814	Trout Lake	-138.744490	68.829105	Western North America	163	Raw	Lake	27	AWI	-0.042	15.923	The modern catchment vegetation around Trout Lake is dominated by heath tundra and fellfield communities, including boreal taxa such as Alnus crispa, Betula glandulosa and Salix, and herbs such as Empetrum nigrum, Vaccinium uliginosum, Vaccinium vitis-idaea, Arctous. alpina and Anemone sp.	Fritz, M., Herzschuh, U., Wetterich, S., Lantuit, H., De Pascale, G.P., Pollard, W.H. and Schirrmeister, L., 2012. Late glacial and Holocene sedimentation, vegetation, and climate history from easternmost Beringia (northern Yukon Territory, Canada). Quaternary Research, 78(3), pp.549-560.	https://doi.org/10.1016/j.yqres.2012.07.007
KILLBREW	Neotoma	13290	19820	Killebrew Lake Fen	-122.901450	48.605100	Western North America	88	Raw	Lake	94	AWI	0.196	13.781	Kettle lake with marginal fen located on Orcas Island, one of the San Juan Islands in the Salish Sea between manland Washington and Vancouver Island. Local upland vegetation dominated by Pseudotsuga menziesii with lesser amounts of Abies grandis.	Leopold, E.B., Dunwiddie, P.W., Whitlock, C., Nickmann, R. and Watts, W.A., 2016. Postglacial vegetation history of Orcas Island, northwestern Washington. Quaternary Research, 85(3), pp.380-390.	https://doi.org/10.1016/j.yqres.2016.02.004
CY	Neotoma	13375	19993	Cooley Lake	-117.645195	49.491360	Western North America	1515	Raw	Lake	76	AWI	-0.049	7.499	SurroundVeg: subalpine fir, englemann spruce, larix occidentalis, pinus contorta	Gavin, D.G., Hu, F.S., Lertzman, K. and Corbett, P., 2006. Weak climatic control of stand-scale fire history during the late Holocene. Ecology, 87(7), pp.1722-1732.	https://doi.org/10.1890/0012-9658(2006)87%5B1722:WCCOSF%5D2.0.CO;2
GERRY	Neotoma	13376	19995	Gerry Lake	-121.505480	53.645450	Western North America	893	Raw	Lake	69	Neotoma_Gavin et al, 2009	-0.038	11.220	The vegetation is a dense forest of Abies lasiocarpa (subalpine fir) and Picea glauca x engelmannii (hybrid white spruce), with minor amounts of Pseudotsuga menziesii (Douglas-fir) in the region. The lake is fringed by a wide (10-20 m) sedge fen and a submerged bench of marl sediments.	Gavin, D.G., Hu, F.S., Walker, I.R. and Westover, K., 2009. The northern inland temperate rainforest of British Columbia: old forests with a young history?. Northwest Science, 83(1), pp.70-78.	https://doi.org/10.3955/046.083.0107
WENT	Neotoma	459	19997	Wentworth Lake	-124.530695	48.009850	Western North America	58	Raw	Lake	54	AWI	0.363	14.161	Open water lake	Gavin, D.G. and Brubaker, L.B., 2015. Late Quaternary Vegetation and Fire History of the Olympic Peninsula. In: Late Pleistocene and Holocene Environmental Change on the Olympic Peninsula, Washington ed. by D.G. Gavin and L.B. Brubaker (pp.61-106). Springer International Publishing, Cham, Switzerland.	https://doi.org/10.1007/978-3-319-11014-1_4
CROCKER-CL	Neotoma	13377	20001	Crocker Lake	-122.880815	47.936655	Western North America	54	Raw	Lake	49	AWI	0.046	12.422	Forests in the area are heavily managed Douglas-fir stands; red alder. and western redcedar were likely important historically and especially along the. streams. Despite being in the Western hemlock zone, this late-successional species. is rare because of dominance of Douglas-fir after disturbance in this drier climate.	Gavin, D.G. and Brubaker, L.B., 2015. Late Quaternary Vegetation and Fire History of the Olympic Peninsula. In: Late Pleistocene and Holocene Environmental Change on the Olympic Peninsula, Washington ed. by D.G. Gavin and L.B. Brubaker (pp.61-106). Springer International Publishing, Cham, Switzerland.	https://doi.org/10.1007/978-3-319-11014-1_4	McLachlan, J.S. and Brubaker, L.B., 1995. Local and regional vegetation change on the northeastern Olympic Peninsula during the Holocene. Canadian Journal of Botany, 73(10), pp.1618-1627.	https://doi.org/10.1139/b95-175
CS2_neotoma	Neotoma	13382	20014	Cedar Swamp	-122.874860	47.905425	Western North America	60	Raw	Swamp	37	AWI	1.477	13.211	Cedar Swamp is a riparian swamp (ca. 10 ha) located in a flat seepage area that drains into Leland Lake 3 km south of Crocker Lake. Hydrologically, the swamp grades gently from a wet meadow to areas with > 1 m of standing water in the winter. The swamp is currently forested with second growth Alnus rubra and Thuja plicata, which are replacing a clear-cut stand of larger Thuja plicata, Alnus rubra, and Tsuga heterophylla. Understory species at the site include Rubus spectabilis, Maianthamum dilatatum, and Spiraea sp. Lysichitum americanum, Carex spp., and Nuphar polysepalum occupy progressively deeper aquatic areas, although trees grow on small topographic irregularities in even the deepest part of the swamp.	McLachlan, J.S. and Brubaker, L.B., 1995. Local and regional vegetation change on the northeastern Olympic Peninsula during the Holocene. Canadian Journal of Botany, 73(10), pp.1618-1627.	https://doi.org/10.1139/b95-175
DRAGONFL	Neotoma	13477	20281	Dragonfly Lake	-135.341245	60.812585	Western North America	760	Raw	Lake	48	AWI	0.113	10.897	Surrounding vegetation: Primarily spruce forest with occasional pine.	Edwards, M., Franklin-Smith, L., Clarke, C., Baker, J., Hill, S. and Gallagher, K., 2015. The role of fire in the mid-Holocene arrival and expansion of lodgepole pine (Pinus contorta var. latifolia Engelm. ex S. Watson) in Yukon, Canada. The Holocene, 25(1), pp.64-78.	https://doi.org/10.1177/0959683614556389
HAIRCUT	Neotoma	13479	20287	Haircut Lake	-133.209055	60.516075	Western North America	1000	Raw	Lake	26	AWI	0.564	8.055	Haircut Lake lies in a steep-sided basin. Surrounding vegetation is completely dominated by dense pine forest with very little understorey vegetation, and deciduous tree. species and shrubs are largely limited to the shoreline	Edwards, M., Franklin-Smith, L., Clarke, C., Baker, J., Hill, S. and Gallagher, K., 2015. The role of fire in the mid-Holocene arrival and expansion of lodgepole pine (Pinus contorta var. latifolia Engelm. ex S. Watson) in Yukon, Canada. The Holocene, 25(1), pp.64-78.	https://doi.org/10.1177/0959683614556389
MARCELLA	Neotoma	13480	20289	Marcella Lake	-133.806010	60.073495	Western North America	697	Raw	Lake	39	AWI	-0.067	9.010	Kettle pond located on a terrace of unconsolidated till and outwash related to a former melt-water channel. Surrounding vegetation: The catchment is dominated by pine and aspen, with open vegetation dominated by Artemisia frigida and grasses on well-drained, south-facing slopes. Spruce is present on the shoreline.	Edwards, M., Franklin-Smith, L., Clarke, C., Baker, J., Hill, S. and Gallagher, K., 2015. The role of fire in the mid-Holocene arrival and expansion of lodgepole pine (Pinus contorta var. latifolia Engelm. ex S. Watson) in Yukon, Canada. The Holocene, 25(1), pp.64-78.	https://doi.org/10.1177/0959683614556389
SALMO	Neotoma	13482	20295	Salmo Lake	-133.561605	60.445535	Western North America	866	Raw	Lake	37	AWI	-0.061	11.671	Small pond located within dead ice topography in a small east-west trending valley. Surrounding vegetation: Pine dominates to the north of the lake, but spruce is the predominant tree to the south, west, and immediately around the lake. An extensive area of low-lying muskeg (black spruce) is present in the river valley to the west.	Edwards, M., Franklin-Smith, L., Clarke, C., Baker, J., Hill, S. and Gallagher, K., 2015. The role of fire in the mid-Holocene arrival and expansion of lodgepole pine (Pinus contorta var. latifolia Engelm. ex S. Watson) in Yukon, Canada. The Holocene, 25(1), pp.64-78.	https://doi.org/10.1177/0959683614556389
HUNTERS	Neotoma	13486	20304	Hunters Lake	-106.843695	37.611035	Western North America	3516	Raw	Lake	39	AWI	-0.044	13.980	Lake is impounded by late-Pinedale glacial drift, although the natural dam was enhanced by homesteaders in the late 19th century to increase water delivery to downstream communities. Presently, it is situated 100 m below the upper treeline, surrounded by Picea. engelmannii-Abies lasiocarpa forest, with shrubs including Juniperus communis, Ribes sp., Sambucus microbotrys, Linnaea borealis, and Vaccinium myrtillus.	Anderson, R.S., Allen, C.D., Toney, J.L., Jass, R.B. and Bair, A.N., 2008. Holocene vegetation and fire regimes in subalpine and mixed conifer forests, southern Rocky Mountains, USA. International Journal of Wildland Fire, 17(1), pp.96-114.	https://doi.org/10.1071/WF07028
DAILEY	Neotoma	13487	20306	Dailey Lake	-110.816305	45.262475	Western North America	1598	Raw	Lake	87	AWI	-0.037	14.118	Dailey Lake occupies a shallow trench on a low bench carved by the late-Pleistocene northern Yellowstone outlet glacier; surrounding vegetation is primarily grassland and steppe dominated by Artemisia tridentata (big sagebrush), Ericameria nauseosa (rabbitbrush), Festuca idahoensis (Idaho fescue), and Leymus cinereus (Great Basin wild rye), with isolated populations of Juniperus scopulorum (Rocky Mountain Juniper)	Krause, T.R., Lu, Y., Whitlock, C., Fritz, S.C. and Pierce, K.L., 2015. Patterns of terrestrial and limnologic development in the northern Greater Yellowstone Ecosystem (USA) during the late-glacial/early-Holocene transition. Palaeogeography, Palaeoclimatology, Palaeoecology, 422, pp.46-56.	https://doi.org/10.1016/j.palaeo.2014.12.018
BLACKTA	Neotoma	273	20308	Blacktail Pond	-110.600710	44.956110	Western North America	2012	Raw	Lake	78	AWI	7.079	14.058	Blacktail Pond is situated in a remnant late-Pleistocene meltwater channel; surrounding vegetation is Pseudotsuga menziesii (Douglas-fir) parkland, which includes grassland and steppe communities dominated by Artemisia tridentata (big sagebrush), Festuca idahoensis (Idaho fescue), and Ericameria nauseosa (rabbitbrush).	Krause, T.R. and Whitlock, C., 2013. Climate and vegetation change during the late-glacial/early-Holocene transition inferred from multiple proxy records from Blacktail Pond, Yellowstone National Park, USA. Quaternary Research, 79(3), pp.391-402.	https://doi.org/10.1016/j.yqres.2013.01.005
FISHLKCA	Neotoma	13488	20316	Fish Lake	-123.683120	41.263960	Western North America	541	Raw	Lake	35	AWI	-0.056	2.886	Landslide origin lake located in oak woodland vegetation in the Klamath Mountains. Overstory vegetation at the site consists mainly of Pseudotsuga menziesii and Chamaecyparis lawsoniana, with lesser amounts of Notholithocarpus densiflorus, Pinus lambertiana, and Pinus jeffreyi. Salix spp. and Alnus spp. are well represented in riparian areas. Quercus spp. Poaceae, and Pteridium are very rare around the basin but are present in isolated, open-canopied areas.	Crawford, J.N., 2012. Evidence for Native American land-use impacts on forest structure and fire regimes in the Lower Klamath River Region of California. Doctoral dissertation. University of Nevada, Reno, Reno, Nevada, USA.		Crawford, J.N., Mensing, S.A., Lake, F.K. and Zimmerman, S.R., 2015. Late Holocene fire and vegetation reconstruction from the western Klamath Mountains, California, USA: A multi-disciplinary approach for examining potential human land-use impacts. The Holocene, 25(8), pp.1341-1357.	https://doi.org/10.1177/0959683615584205
SWANSONF	Neotoma	13516	20372	Swanson Fen	-150.831470	60.787275	Western North America	100	Raw	Fen	63	AWI	0.013	14.658	Swanson Fen is a small nutrient-poor fen. Surrounding vegetation: Picea mariana forest and an isolated Tsuga mertensiana stand	Jones, M.C., Peteet, D.M. and Sambrotto, R., 2010. Late-glacial and Holocene 15N and 13C variation from a Kenai Peninsula, Alaska peatland. Palaeogeography, Palaeoclimatology, Palaeoecology, 293(1-2), pp.132-143.	https://doi.org/10.1016/j.palaeo.2010.05.007	Jones, M.C., Peteet, D.M., Kurdyla, D. and Guilderson, T., 2009. Climate and vegetation history from a 14,000-year peatland record, Kenai Peninsula, Alaska. Quaternary Research, 72(2), pp.207-217.	https://doi.org/10.1016/j.yqres.2009.04.002
OGAROM	Neotoma	13575	20495	Ogaromtoc Lake	-123.541235	41.486105	Western North America	596	Raw	Lake	33	AWI	-0.059	3.386	Small lake formed by landslide. Site is located in the oak woodland vegetation zone. Overstory vegetation at the site consists mainly of Pseudotsuga menziesii and Calocedrus decurrens, with Quercus spp. (primarily Q. kelloggii), Notholithocarpus densiflorus, Pinus lambertiana, and Pinus jeffreyi.	Crawford, J.N., 2012. Evidence for Native American land-use impacts on forest structure and fire regimes in the Lower Klamath River Region of California. Doctoral dissertation. University of Nevada, Reno, Reno, Nevada, USA.		Crawford, J.N., Mensing, S.A., Lake, F.K. and Zimmerman, S.R., 2015. Late Holocene fire and vegetation reconstruction from the western Klamath Mountains, California, USA: A multi-disciplinary approach for examining potential human land-use impacts. The Holocene, 25(8), pp.1341-1357.	https://doi.org/10.1177/0959683615584205
NEWARKVP	Neotoma	13920	21415	Newark Valley Pond	-115.773980	39.672830	Western North America	1750	Raw	Lake	23	AWI	-0.059	22.510	Newark Valley Pond is ~7 m in diameter and flows through a wet meadow ~30*40 m to a pool ~20 mi in diameter, with a maximum water depth of 50 cm. Pool is surrounded by Typha and Carex in shallow water. Surrounding upland vegetation is Artemisia steppe dominated by Artemisia tridentata var. tridentata, A. t. var. wyomingensis, Chrysothamnus viscidiflorus, Sarbatus vermiculatus, and Atriplex confertifolia. Scattered Juniperus osteosperma grow on rocky slopes above the site. Pinus flexilis occurs at the highest elevations above ~3000 m.	Mensing, S., Smith, J., Norman, K.B. and Allan, M., 2008. Extended drought in the Great Basin of western North America in the last two millennia reconstructed from pollen records. Quaternary International, 188(1), pp.79-89.	https://doi.org/10.1016/j.quaint.2007.06.009	Mensing, S., Livingston, S. and Barker, P., 2006. Long-term fire history in Great Basin sagebrush reconstructed from macroscopic charcoal in spring sediments, Newark Valley, Nevada. Western North American Naturalist, 66(1), pp.64-77.	https://doi.org/10.3398/1527-0904(2006)66%5B64:LFHIGB%5D2.0.CO;2
KINGMEAD	Neotoma	13922	21418	Kingston Meadow	-117.165500	39.253180	Western North America	2400	Raw	Meadow	27	AWI	0.010	6.386	Wet meadow dominated by sedge (Carex rostrata and C. nebrascensis) along a riparian system in the Toiyabe Range of central Nevada. Surface water covers most of the meadow to a depth of approximately 10 cm. Upland vegetation Artemisia steppe with scattered Juniperus osteosperma.	Mensing, S., Smith, J., Norman, K.B. and Allan, M., 2008. Extended drought in the Great Basin of western North America in the last two millennia reconstructed from pollen records. Quaternary International, 188(1), pp.79-89.	https://doi.org/10.1016/j.quaint.2007.06.009
UPSQUAW	Neotoma	13923	21422	Upper Squaw Lake	-123.014855	42.032085	Western North America	930	Raw	Lake	48	Neotoma_Colombaroli & Gavin 2010	-0.057	1.928	Surrounding vegetation: Douglas-fir, Pacific madrone, ponderosa pine, canyon live oak. The bedrock of 90% of the watershed is graphitic. quartz-mica schist and serpentine.	Colombaroli, D. and Gavin, D.G., 2010. Highly episodic fire and erosion regime over the past 2,000 y in the Siskiyou Mountains, Oregon. Proceedings of the National Academy of Sciences, 107(44), pp.18909-18914.	https://doi.org/10.1073/pnas.1007692107	Morey, A.E., Goldfinger, C., Briles, C.E., Gavin, D.G., Colombaroli, D. and Kusler, J.E., 2013. Are great Cascadia earthquakes recorded in the sedimentary records from small forearc lakes?. Natural Hazards and Earth System Sciences, 13(10), pp.2441-2463.	https://doi.org/10.5194/nhess-13-2441-2013
HIPPA	Neotoma	14031	21770	Hippa Lake	-132.973333	53.531667	Western North America	230	Raw	Lake	74	AWI	0.160	13.955	Shallow lake on Hippa Island with no inflowing streams	Lacourse, T., Delepine, J.M., Hoffman, E.H. and Mathewes, R.W., 2012. A 14,000 year vegetation history of a hypermaritime island on the outer Pacific coast of Canada based on fossil pollen, spores and conifer stomata. Quaternary Research, 78(3), pp.572-582.	https://doi.org/10.1016/j.yqres.2012.08.008
MISTYBC	Neotoma	14032	21772	Misty Lake	-127.262830	50.607050	Western North America	70	Raw	Lake	65	AWI	0.062	14.316	Moderate-sized, humic lake, with a small stream that flows through 500m of wetland before entering the lake	Lacourse, T., 2005. Late Quaternary dynamics of forest vegetation on northern Vancouver Island, British Columbia, Canada. Quaternary Science Reviews, 24(1-2), pp.105-121.	https://doi.org/10.1016/j.quascirev.2004.05.008	Lacourse, T., 2009. Environmental change controls postglacial forest dynamics through interspecific differences in life-history traits. Ecology, 90(8), pp.2149-2160.	https://doi.org/10.1890/08-1136.1
MCNEILL	Neotoma	14033	21774	Port McNeill Bog	-127.072200	50.572500	Western North America	93	Raw	Bog	66	AWI	-0.033	10.497	Flat ombrotrophic bog along a roadside; surface vegetation dominated by ericaceous shrubs, Sphagnum capillifolium and Sphagnum fuscum. Open Pinus contorta bog-woodland surrounds the bog	Lacourse, T. and Davies, M.A., 2015. A multi-proxy peat study of Holocene vegetation history, bog development, and carbon accumulation on northern Vancouver Island, Pacific coast of Canada. the Holocene, 25(7), pp.1165-1178.	https://doi.org/10.1177/0959683615580201
ROEBC	Neotoma	14039	21788	Roe Lake	-123.303280	48.782700	Western North America	100	Raw	Lake	114	AWI	-0.064	9.899	Small lake with no inflowing streams in bedrock depression. Forests surrounding the lake are dominated by Pseudotsuga menziesii, Thuja plicata, and Abies grandis in the canopy, with Acer macrophyllum and A. glabrum present along the lake margin and Gaultheria shallon, Symphoricarpos albus, Polystichum munitum, and Pteridium aquilinum common in the understory. A stand of Alnus rubra is located along the southeastern margin of the lake. Xeric taxa, including Arbutus menziesii and Quercus garryana, are scattered on the adjacent ridges.	Lucas, J.D. and Lacourse, T., 2013. Holocene vegetation history and fire regimes of Pseudotsuga menziesii forests in the Gulf Islands National Park Reserve, southwestern British Columbia, Canada. Quaternary Research, 79(3), pp.366-376.	https://doi.org/10.1016/j.yqres.2013.03.001	Lucas, J.D., 2012. Holocene vegetation and fire history of Pender Island, British Columbia, Canada. Master's thesis. University of Victoria, Victoria, British Columbia, Canada.
MCB1997	Neotoma	10507	21844	Mission Cross Bog	-115.483650	41.784700	Western North America	2424	Raw	Lake	34	AWI	0.000	1.776	Spring-fed fen. Growing on the fen are Sphagnum, sedges, Menyanthes trifoliata, Pedicularis groenlandica, Thalictrum spp., and Salix spp. On the northern slope bordering the fen, fields of Balsamorhiza sagittata grow with Lupinus. To the east, south, and west are scattered stands of Populus tremuloides.	Allan, M., 2003. A 2000 year record of vegetation and climate change in the Jarbidge Mountains of Northeastern Nevada. Master's thesis. University of Nevada, Reno, Reno, Nevada, USA.
ODP893A	Neotoma	14071	21893	ODP Hole 893A	-120.061345	34.278180	Western North America	0	Raw	Marine	61	AWI	11.133	18.142	Ocean Drilliing Project core, Santa Barbara Basin. Nearby coastal vegetation: Introduced herbs and grasses are common in the coastal plain. Coastal sage scrub grows on xeric sites, while Chaparral is found on more mesic sites and burns more frequently. Oaks dominate on north facing slopes, in canyons, and in mesic areas of the coastal marine terraces. California juniper grows in scattered stands.	Anderson, R., 2007. Stable isotope and pollen evidence for Late Quaternary climate change in southern coastal California. Doctoral dissertation. University of California, Berkeley, Berkeley, California, USA.
CSB	Neotoma	14163	22119	Cienega de San Bernadino	-109.256160	31.322150	Western North America	1118	Raw	Valley	52	AWI	-0.026	2.057	Cienega located on the floor of the San Bernadino Valley. Surrounding vegetation: Desert grassland and scrub (Atriplex canascens, Ephedra trifurca, Fouquieria splendens, Larrea tridentata, Flourensia cernua, Acacia neovernicosa). Bottomlands consist of a patchwork of Prosopis and fallow fields. Springs, wells, and seasonal streams in the cienega support areas of deciduous riparian scrub, stands of Populus fremontii,	Blissett, S.D., 2010. A late Holocene history of vegetation, fire, and climate from a desert wetland in southwest North America. Master's thesis. University of Utah, Salt Lake City, Utah, USA.
DOOLITL	Neotoma	14308	22397	Doolittle Ranch Meadow	-105.604060	39.676640	Western North America	2975	Raw	Meadow	14	AWI	-0.032	3.563	The Doolittle Ranch Meadow lies within the Doolittle Ranch basin, created by the Chicago Creek glacier, which deposited a lateral moraine across the mouth of a side-valley tributary. Surrounding vegetation: The meadow is dominated by grasses, sedges, and Salix. The meadow is mostly treeless. The moraine that dams the west side of the basin is covered with Picea engelmannii and Pinus contorta. The north side of the basin supports Populus tremuloides, Pinus aristata, and a few intermixed Pinus contorta. The east side of the basin is forested with a dense covering of Picea engelmannii and Pinus contorta. The south end of the basin contains dense stands of Picea engelmannii and Abies lasiocarpa, with a few scattered Pinus contorta and Pseudotsuga menziesii.	Doerner, J.P., 1994. The late-Quaternary environmental history of Mt. Evans: Pollen and stratigraphic evidence from Clear Creek, Colorado. Doctoral dissertation. University of Denver, Denver, Colorado, USA.
ECHOCO	Neotoma	14310	22400	Echo Lake	-105.603265	39.658220	Western North America	3230	Raw	Lake	67	AWI	-0.044	22.321	Echo Lake occupies a preglacial valley that was dammed by a lateral moraine. Surrounding vegetation: The south and west sides of the slope have forest composed of Picea engelmannii and Abies lasiocarpa, with a few scattered Pinus contorta near the margins of the meadow and lake. To the north, Pinus aristata is found in nearly pure stands, surrounded by mixed stands of Pinus engelmannii, Pinus contorta, and Pinus aristata. The surface of the meadow is treeless and dominated by Salix and Carex.	Doerner, J.P., 1994. The late-Quaternary environmental history of Mt. Evans: Pollen and stratigraphic evidence from Clear Creek, Colorado. Doctoral dissertation. University of Denver, Denver, Colorado, USA.
LL07D	Neotoma	14640	22969	Long Lake	-106.367885	41.499845	Western North America	2700	Raw	Lake	175	AWI	-0.067	12.857	Kettle lake on stagnation moraine. Upland vegetation montane conifer forest dominated by Pinus contorta, Picea engelmannii, and Abies bifolia. Populus tremuloides ecotone is ~200 m downslope. The lake margin contains various Poaceae, Cyperaceae, and Betula occidentalis. Hydrophytes include Nuphar lutea and Potamogeton alpinus.	Carter, V.A., Brunelle, A., Minckley, T.A., Shaw, J.D., DeRose, R.J. and Brewer, S., 2017. Climate variability and fire effects on quaking aspen in the central Rocky Mountains, USA. Journal of Biogeography, 44(6), pp.1280-1293.	https://doi.org/10.1111/jbi.12932	Carter, V.A., Brunelle, A., Minckley, T.A., Dennison, P.E. and Power, M.J., 2013. Regionalization of fire regimes in the Central Rocky Mountains, USA. Quaternary Research, 80(3), pp.406-416.	https://doi.org/10.1016/j.yqres.2013.07.009	Minckley, T.A., 2014. Postglacial vegetation history of southeastern Wyoming, USA. Rocky Mountain Geology, 49(1), pp.61-74.	https://doi.org/10.2113/gsrocky.49.1.61
NORTHFLT	Neotoma	15828	24354	North Flat Lake	-106.495240	53.611475	Western North America	522	Raw	Lake	57	AWI	-0.014	1.794	Lake in a shallow depression surrounded by forest consisting primarily of boreal forest species, including prolific pollen producers such as Pinus (mainly P. banksiana) and Picea (predominantly P. glauca), as well as many species typical of aspen parkland and grasslands.	Hart, C.L., 2009. High-resolution pollen analysis of two lakes at the boreal forest-aspen parkland ecotone in central Saskatchewan, Canada. Master's thesis. University of Regina, Regina, Saskatchewan, Canada.
BEEF2005	Neotoma	246	25551	Beef Pasture	-108.160375	37.473105	Western North America	3060	Raw	Peat	72	AWI	-0.059	2.049	Open wet meadow and fen occupying a depression formed by a landslide ~5000 BP in the La Plata Mountains. Local upland vegetation dominated by Picea engelmannii, Pseudotsuga menziesii, Populus tremuloides, and Alnus tenuifolia. Salix brachycarpa lines the edges of the wet meadow.	Wright, A.M., 2012. Low-frequency climate in the Mesa Verde region: Beef Pasture revisited. In: Emergence and collapse of early villages: models of central Mesa Verde archaeology ed. by T.A. Kohler and M.D. Varien (pp.41-57). University of California Press, Berkeley, California, USA.	https://doi.org/10.1525/california/9780520270145.003.0003	Wright, A.M., 2006. A low-frequency paleoclimatic reconstruction from the La Plata Mountains, Colorado and its implications for agricultural productivity in the Mesa Verde region. Master's thesis. Washington State University, Pullman, Washington, USA.
FLORBC	Neotoma	16614	26315	Florence Lake	-123.513045	48.458595	Western North America	81	Raw	Lake	30	AWI	-0.058	0.492	Most of the area has been developed for housing or mined for gravel. Minimal forest remains.	Pellatt, M.G., McCoy, M.M. and Mathewes, R.W., 2015. Paleoecology and fire history of Garry oak ecosystems in Canada: implications for conservation and environmental management. Biodiversity and conservation, 24(7), pp.1621-1639.	https://doi.org/10.1007/s10531-015-0880-1	McCoy, M.M., 2006. High Resolution fire and vegetation history of Garry oak ecosystems in British Columbia. Master's thesis. Simon Fraser, Burnaby, British Columbia, Canada.
GRANTS	Neotoma	23680	40976	Grant's Bog	-125.127100	49.788700	Western North America	80	Raw	Bog	102	AWI	-0.062	14.174	70 ha wetland complex that is mostely a Sphagnum and ericad-dominated bog, small lake (1.8 ha) in south-east corner	Lacourse, T., Beer, K.W., Craig, K.B. and Canil, D., 2019. Postglacial wetland succession, carbon accumulation and forest dynamics on the east coast of Vancouver Island, British Columbia, Canada. Quaternary Research, 92, pp.232-245.	https://doi.org/10.1017/qua.2018.146
GLENMIRE	Neotoma	23715	41030	Glenmire	-122.789614	37.990261	Western North America	167	Raw	Fen	40	AWI	-0.066	6.608	Fen lying in a depression in the Wildcat slide complex, a late Quaternary landslide within the weakly consolidated Santa Cruz Mudstone that partially overlaps the Monterey Formation along the Point Reyes coast. Site lies within closed canopy Pseudotsuga menziesii-mixed evergreen forest with Umbellularia californica and Quercus agrifolia, with adjacent patches of Baccharis pilularis chaparral. Local fen vegetation dominated by Scirpus, Typha, and Eleocharis.	Anderson, R.S., Ejarque, A., Brown, P.M. and Hallett, D.J., 2013. Holocene and historical vegetation change and fire history on the north-central coast of California, USA. The Holocene, 23(12), pp.1797-1810.	https://doi.org/10.1177/0959683613505344
HF98-2	Neotoma	23717	41034	Henrys Fork (upper exposure)	-110.360520	40.800420	Western North America	3550	Raw	Peat	7	AWI	3.966	8.119	Stream-cut exposure in a basin that was impounded by debris flow deposits. Surrounding vegetation: The primary tree species at timberline (approximately 3270 m asl) are Picea engelmannii and Abies lasiocarpa, although Pinus contorta is locally present and increases in abundance at lower elevations. Isolated patches of spruce/fir krummholz are also present.	Munroe, J.S., 2001. Late Quaternary history of the northern Uinta Mountains, northeastern Utah. Doctoral dissertation. University of Wisconsin, Madison, Wisconsin, USA.
GEMLAKE	Neotoma	23763	41140	Gem Lake	-106.734030	40.881000	Western North America	3101	Raw	Lake	19	AWI	0.002	1.395	The vegetation surrounding Gem Lake is closed spruce-fir forest, but ribbon forests and open meadows lie 200 m upslope, within 300 m laterally of the lake.	Calder, W.J., 2016. Interactions among climate change, wildfire, and vegetation shaping landscapes for the last 2000 years. Doctoral dissertation. University of Wyoming, Laramie, Wyoming, USA.		Calder, W.J. and Shuman, B., 2017. Extensive wildfires, climate change, and an abrupt state change in subalpine ribbon forests, Colorado. Ecology, 98(10), pp.2585-2600.	https://doi.org/10.1002/ecy.1959	Calder, W.J., Stefanova, I. and Shuman, B., 2019. Climate-fire-vegetation interactions and the rise of novel landscape patterns in subalpine ecosystems, Colorado. Journal of Ecology, 107(4), pp.1689-1703.	https://doi.org/10.1111/1365-2745.13138
SUMMIT_neotoma	Neotoma	23765	41146	Summit Lake	-106.682360	40.545455	Western North America	3149	Raw	Lake	74	AWI	-0.048	2.826	Continuous closed forests flank the east and west sides of the Summit Lake plateau, and ribbon forests primarily cover the plateau. Both the ribbon forests and continuous forests consist of Abies lasiocarpa (subalpine fir) and Picea engelmannii (Engelmann spruce). At lower elevations, Pinus contorta (lodgepole pine) and Populus tremuloides (aspen) form pure and mixed forests stands separately and with Picea engelmannii and Abies lasiocarpa. The ribbon forest consist of ~10 - 20 m wide bands of spruce and fir trees oriented approximately north to south. 30 - 70 m wide meadows separate forest ribbons.	Calder, W.J., 2016. Interactions among climate change, wildfire, and vegetation shaping landscapes for the last 2000 years. Doctoral dissertation. University of Wyoming, Laramie, Wyoming, USA.		Calder, W.J. and Shuman, B., 2017. Extensive wildfires, climate change, and an abrupt state change in subalpine ribbon forests, Colorado. Ecology, 98(10), pp.2585-2600.	https://doi.org/10.1002/ecy.1959	Calder, W.J., Stefanova, I. and Shuman, B., 2019. Climate-fire-vegetation interactions and the rise of novel landscape patterns in subalpine ecosystems, Colorado. Journal of Ecology, 107(4), pp.1689-1703.	https://doi.org/10.1111/1365-2745.13138	Calder, W.J., Parker, D., Stopka, C.J., Jimenez-Moreno, G. and Shuman, B.N., 2015. Medieval warming initiated exceptionally large wildfire outbreaks in the Rocky Mountains. Proceedings of the National Academy of Sciences, 112(43), pp.13261-13266.	https://doi.org/10.1073/pnas.1500796112
SEVEN	Neotoma	23770	41159	Seven Lakes	-106.682215	40.896140	Western North America	3276	Raw	Lake	27	AWI	0.050	4.189	Glacial scour lake. Surrounding vegetation: Ribbon forest. The ribbon forests are composed of alternating bands of spruce-fir forests approximately 10-20 m wide and separated by 30-70 m wide meadows	Calder, W.J., 2016. Interactions among climate change, wildfire, and vegetation shaping landscapes for the last 2000 years. Doctoral dissertation. University of Wyoming, Laramie, Wyoming, USA.		Calder, W.J. and Shuman, B., 2017. Extensive wildfires, climate change, and an abrupt state change in subalpine ribbon forests, Colorado. Ecology, 98(10), pp.2585-2600.	https://doi.org/10.1002/ecy.1959	Calder, W.J., Stefanova, I. and Shuman, B., 2019. Climate-fire-vegetation interactions and the rise of novel landscape patterns in subalpine ecosystems, Colorado. Journal of Ecology, 107(4), pp.1689-1703.	https://doi.org/10.1111/1365-2745.13138
GOLDCRK	Neotoma	23771	41161	Gold Creek Lake	-106.678960	40.781835	Western North America	2917	Raw	Lake	35	AWI	-0.052	2.021	Gold Creek Lake sits on the south side of a glacially carved canyon. Surrounding vegetation: Spruce-fir forests are the primary vegetation, while ribbon forests and a mix of open meadows cover much of the nearby landscape.	Calder, W.J., 2016. Interactions among climate change, wildfire, and vegetation shaping landscapes for the last 2000 years. Doctoral dissertation. University of Wyoming, Laramie, Wyoming, USA.		Calder, W.J., Parker, D., Stopka, C.J., Jimenez-Moreno, G. and Shuman, B.N., 2015. Medieval warming initiated exceptionally large wildfire outbreaks in the Rocky Mountains. Proceedings of the National Academy of Sciences, 112(43), pp.13261-13266.	https://doi.org/10.1073/pnas.1500796112	Calder, W.J., Stefanova, I. and Shuman, B., 2019. Climate-fire-vegetation interactions and the rise of novel landscape patterns in subalpine ecosystems, Colorado. Journal of Ecology, 107(4), pp.1689-1703.	https://doi.org/10.1111/1365-2745.13138
HIDDENCO	Neotoma	23772	41163	Hidden Lake	-106.607540	40.504665	Western North America	2704	Raw	Lake	32	AWI	0.043	2.561	Origin in Hidden Lake is uncertain, either a landslide origin or moraine dammed. Lake is surrounded primarily by lodgepole pine and spruce-fir forests, with aspen groves further upslope.	Calder, W.J., 2016. Interactions among climate change, wildfire, and vegetation shaping landscapes for the last 2000 years. Doctoral dissertation. University of Wyoming, Laramie, Wyoming, USA.		Calder, W.J., Parker, D., Stopka, C.J., Jimenez-Moreno, G. and Shuman, B.N., 2015. Medieval warming initiated exceptionally large wildfire outbreaks in the Rocky Mountains. Proceedings of the National Academy of Sciences, 112(43), pp.13261-13266.	https://doi.org/10.1073/pnas.1500796112	Calder, W.J., Stefanova, I. and Shuman, B., 2019. Climate-fire-vegetation interactions and the rise of novel landscape patterns in subalpine ecosystems, Colorado. Journal of Ecology, 107(4), pp.1689-1703.	https://doi.org/10.1111/1365-2745.13138
HINMAN	Neotoma	23775	41171	Hinman Lake	-106.827590	40.771620	Western North America	2501	Raw	Lake	19	AWI	-0.045	1.333	Hinman Lake is surrounded by open sagebrush parks and dense thickets of Quercus gambelii, combined with Picea-Abies, Pinus contorta, and aspen forests.	Calder, W.J., 2016. Interactions among climate change, wildfire, and vegetation shaping landscapes for the last 2000 years. Doctoral dissertation. University of Wyoming, Laramie, Wyoming, USA.		Calder, W.J., Parker, D., Stopka, C.J., Jimenez-Moreno, G. and Shuman, B.N., 2015. Medieval warming initiated exceptionally large wildfire outbreaks in the Rocky Mountains. Proceedings of the National Academy of Sciences, 112(43), pp.13261-13266.	https://doi.org/10.1073/pnas.1500796112	Calder, W.J., Stefanova, I. and Shuman, B., 2019. Climate-fire-vegetation interactions and the rise of novel landscape patterns in subalpine ecosystems, Colorado. Journal of Ecology, 107(4), pp.1689-1703.	https://doi.org/10.1111/1365-2745.13138
GOATLAKE	Neotoma	23778	41183	Goat Lake	-149.908460	60.258490	Western North America	550	Raw	Lake	52	AWI	-0.059	8.997	Glacial scour lake in the Kenai Mountains located near an outlet glacier fo the Harding Icefield. Surrounding vegetation dominated by Alnus sinuata and Tsuga mertensiana with some Picea glauca. Tsuga mertensiana is at its upper elevational limit.	Anderson, R.S., Kaufman, D.S., Berg, E., Schiff, C. and Daigle, T., 2017. Holocene biogeography of Tsuga mertensiana and other conifers in the Kenai Mountains and Prince William Sound, south-central Alaska. The Holocene, 27(4), pp.485-495.	https://doi.org/10.1177/0959683616670217
OCFCB	Neotoma	23917	41497	Old Crow Flats (Core CB)	-140.856560	68.108260	Western North America	292	Raw	Lake	19	AWI	1.613	14.600	Vast expanse of patterned peatland and shallow lakes. Surrounding vegetation: Closed forests of Picea glauca and P. mariana with dense understories of Alnus crispa, Betula glandulosa, and Shepherdia canadensis are found on valley slopes. Uplands are covered in birch-heath shrub tundra, with Eriophorum vaginatum tussock tundra on very gentle slopes. Treeline is formed by Picea glauca, the most northerly stands of which occur on south-facing slopes and in creek valleys.	Ovenden, L.E., 1985. Hydroseral histories of the Old Crow Peatlands, northern Yukon. Doctoral dissertation. University of Toronto, Toronto, Ontario, Canada.
OCFKE	Neotoma	23918	41499	Old Crow Flats (Core KE)	-140.826090	67.932750	Western North America	335	Raw	Lake	28	AWI	0.352	16.988	Vast expanse of patterned peatland and shallow lakes. Surrounding vegetation: Closed forests of Picea glauca and P. mariana with dense understories of Alnus crispa, Betula glandulosa, and Shepherdia canadensis are found on valley slopes. Uplands are covered in birch-heath shrub tundra, with Eriophorum vaginatum tussock tundra on very gentle slopes. Treeline is formed by Picea glauca, the most northerly stands of which occur on south-facing slopes and in creek valleys.	Ovenden, L.E., 1985. Hydroseral histories of the Old Crow Peatlands, northern Yukon. Doctoral dissertation. University of Toronto, Toronto, Ontario, Canada.
LEDC10-1	Neotoma	23926	41537	Lake Elsinore	-117.353400	33.660655	Western North America	376	Raw	Lake	258	AWI	6.646	32.516	Largest natural lake in Southern California, currently ~15 km^2. San Jacinto Rivier is main water source, and runoff from the Elsinore Mountains. Modern mean depth is ~3-13 m.	Heusser, L.E., Kirby, M.E. and Nichols, J.E., 2015. Pollen-based evidence of extreme drought during the last Glacial (32.6-9.0 ka) in coastal southern California. Quaternary Science Reviews, 126, pp.242-253.	https://doi.org/10.1016/j.quascirev.2015.08.029	Kirby, M.E., Heusser, L., Scholz, C., Ramezan, R., Anderson, M.A., Markle, B., Rhodes, E., Glover, K.C., Fantozzi, J., Hiner, C. and Price, B., 2018. A late Wisconsin (32-10k cal a BP) history of pluvials, droughts and vegetation in the Pacific south-west United States (Lake Elsinore, CA). Journal of Quaternary Science, 33(2), pp.238-254.	https://doi.org/10.1002/jqs.3018
HERMIT	Neotoma	23930	41580	Hermit Lake	-105.631660	38.088060	Western North America	3450	Raw	Lake	61	AWI	-0.054	13.814	Cirque lake in the Sangre de Cristo Mountains located ~200 m below tree line. Local vegetation north and east of the lake dominated by Picea engelmannii with some Abies bifolia, with debris slopes south and east.	Anderson, R.S., Soltow, H.R. and Jimenez-Moreno, G., 2018. Postglacial environmental change of a high-elevation forest, Sangre de Cristo Mountains of south-central Colorado. In: From saline to freshwater: the diversity of western lakes in space and time ed by S.W. Starratt and M.R. Rosen (Special Paper 536). Geological Society of America, Boulder, Colorado, USA.	https://doi.org/10.1130/2018.2536(13)
SUNSET	Neotoma	23940	41606	Sunset Lake	-124.652000	58.497000	Western North America	1530	Raw	Lake	37	AWI	-0.040	8.532	Sunset Lake is found within an east-west oriented valley, approximately 230 m above current treeline. Surrounding vegetation: Low-elevation forests in the region are dominated by Picea glauca, P. mariana, Pinus contorta, Betula papyrifera, and Populus tremuloides. With increasing elevation, forest cover gradually grades into forest-tundra. Above treeline, vegetation surrounding Sunset Lake is dominated by Betula glandulosa. Dwarf shrubs (Cassiope tetragona, Dryas integrifolia, Arctostaphylos, and Vaccinium) also occur, but their densities are low. An assortment of herbs, including Oxyria digyna, Potentilla uniflora, Poaceae, bryophytes, and lichens are also present. Salix often occurs near the edge of the lakes and along streams. A few dwarfed Picea glauca are growing along the shore of the lake.	Pisaric, M.F.J., 2001. Holocene environmental change at the subarctic alpine treeline in northern British Columbia and the southern Yukon Territory, Canada. Doctoral dissertation. Queen's University, Kingston, Ontario, Canada.
DEADSPR	Neotoma	23942	41612	Dead Spruce Lake	-124.549500	58.578500	Western North America	1378	Raw	Lake	31	AWI	-0.053	12.471	Surrounding vegetation: Low-elevation forests in the region are dominated by Picea glauca, P. mariana, Pinus contorta, Betula papyrifera, and Populus tremuloides. With increasing elevation, forest cover gradually grades into forest-tundra. A large number of trees around the lake were killed by a local fire of unknown timing.	Pisaric, M.F.J., 2001. Holocene environmental change at the subarctic alpine treeline in northern British Columbia and the southern Yukon Territory, Canada. Doctoral dissertation. Queen's University, Kingston, Ontario, Canada.
EMERALDL	Neotoma	23943	41614	Emerald Lake	-106.406280	39.151625	Western North America	3051	Raw	Lake	54	AWI	-0.069	10.255	Small Kettle Lake in the valley bottom along Halfmoon Creek. The lake lies in hummocky outwash between two Pinedale-age lateral moraines, which originated from an outlet glacier in the Sawatch Range. Surrounding vegetation is dominated by dense stands of Pinus contorta, with minor Picea engelmannii, Abies, and Populus tremuloides.	Jimenez-Moreno, G., Anderson, R.S., Shuman, B.N. and Yackulic, E., 2019. Forest and lake dynamics in response to temperature, North American monsoon and ENSO variability during the Holocene in Colorado (USA). Quaternary Science Reviews, 211, pp.59-72.	https://doi.org/10.1016/j.quascirev.2019.03.013
FOYMT	Neotoma	24040	41762	Foy Lake	-114.361200	48.164750	Western North America	1006	Raw	Lake	115	AWI	-0.022	12.464	Present vegetation in the Flathead Valley is a mixture of irrigated agricultural lands, native grasslands, conifer forests, and riparian woodland. Forests around Foy Lake are composed of Pseudotsuga menziesii, Pinus ponderosa, and Larix occidentalis. Larix occidentalis, Pinus ponderosa, and an occasional Juniperus scopulorum grow in open grassy woodlands along the west-facing slopes above the site. Stands of Pinus contorta are scattered throughout all habitats near Foy Lake.	Power, M.J., 2006. Recent and Holocene fire, climate, and vegetation linkages in the northern Rocky Mountains, USA. Doctoral dissertation. University of Oregon, Eugene, Oregon, USA.
WA01	Neotoma	24070	41864	Lake WA01	-136.929375	61.244410	Western North America	1000	Raw	Lake	126	AWI	-0.059	10.414	The vegetation surrounding the study site is characterized by the presence of low density boreal forests dominated by white spruce (Picea glauca). White spruce stands in the region tend to be found on well-drained soils and on the sides and tops of slopes. Stands of poplar and aspen, as well as birch and alder are also common, particularly in low-lying areas and on more poorly drained sites. In the understory, the vegetation includes juniper and willow as well as numerous herbaceous plants such as species of grasses and sedges, which tend to occur on more poorly drained sites. Epilobium and Shepherdia also form a small component of the modern vegetation, and are principally found on well-drained soils.	Ravindra, R., 2009. A high-resolution vegetation, fire, and climate history from the Aishihik Region, Yukon Territory, Canada. Master's thesis. University of Ottawa, Ottawa, Ontario, Canada.
ANTLER	Neotoma	24183	42547	Antler Pond	-107.119375	40.023090	Western North America	3128	Raw	Lake	99	AWI	-0.058	1.356	Small lake on a large lateral moraine adjacent to the Bear River. Lake is within the subalpine zone, surrounded by old-growth dead Picea engelmannii with and understory of P. engelmannii and some Abies bifolia. Pond is fringed by Cyperaceae, Poaceae, and Salix.	Anderson, R.S., Smith, S.J., Lynch, A.M. and Geils, B.W., 2010. The pollen record of a 20th century spruce beetle (Dendroctonus rufipennis) outbreak in a Colorado subalpine forest, USA. Forest Ecology and Management, 260(4), pp.448-455.	https://doi.org/10.1016/j.foreco.2010.05.001
WHITBARK	Neotoma	24187	42559	Whitebark Moraine Pond	-110.794225	43.788365	Western North America	2801	Raw	Lake	37	AWI	-0.005	7.793	Lake formed by damming of the upper reaches of Paintbrush Canyon by lateral and recesional Pinedale moraines. Located in the subalpine zone with Pinus albicaulis, Abies bifolia, and Picea engelmannii.	Kelly, K.E., 2014. Paleoecological reconstruction of a modern whitebark pine (Pinus albicaulis) population in Grand Teton National Park, WY. Master's thesis. Kansas State University, Manhattan, Kansas, USA.
SOLDIER	Neotoma	24232	42645	Soldier Creek Meadow	-109.920420	32.701770	Western North America	2860	Raw	Meadow	17	AWI	-0.026	1.284	Small, open meadow in the Pinaleno Mountains within the mixed-conifer forest, dominated by Picea engelmannii, Abies concolor, Pseudotsuga menziesii, Pinus strobiformis, and P. ponderosa.	Anderson, R.S. and Smith, S.J., 2009. Vegetation changes within the subalpine and mixed conifer forests on Mt. Graham, Arizona: Proxy evidence for Mt. Graham red squirrel habitat. In: The Last Refuge of the Mt. Graham Red Squirrel: Ecology of endangerment ed by H.R. Sanderson and J.L. Koprowski (pp.153-169). University of Arizona Press, Tucson, Arizona, USA.
SGANG	Neotoma	24236	42655	SGang Gwaay Pond	-131.212294	52.091542	Western North America	5	Raw	Lake	22	AWI	-0.019	1.699	Small pond on southeast side of Anthony Island about 700 m south of SGang Gwaay village (Ninstints), a UNESCO World Heritage Site.	Lacourse, T., Mathewes, R.W. and Hebda, R.J., 2007. Paleoecological analyses of lake sediments reveal prehistoric human impact on forests at Anthony island UNESCO world heritage site, Queen Charlotte islands (Haida Gwaii), Canada. Quaternary Research, 68(2), pp.177-183.	https://doi.org/10.1016/j.yqres.2007.04.005
WESTSIDE	Neotoma	24243	42675	West Side Pond	-131.791667	52.541667	Western North America	16	Raw	Lake	25	AWI	11.128	16.302	Small pond on Moresby Island about 300 m inland from the modern shore on the west side of Moresby Island.	Lacourse, T., Mathewes, R.W. and Fedje, D.W., 2005. Late-glacial vegetation dynamics of the Queen Charlotte Islands and adjacent continental shelf, British Columbia, Canada. Palaeogeography, Palaeoclimatology, Palaeoecology, 226(1-2), pp.36-57.	https://doi.org/10.1016/j.palaeo.2005.05.003
DFBANK	Neotoma	24244	42677	Dogfish Bank	-131.300000	53.870000	Western North America	0	Raw	Lake	12	AWI	15.533	17.137	Dogfish Bank, Hecate Strait, British Columbia, Core retrieved from aboard the CSS John P. Tully in June 1991 in 31 m of water, Core contains terrestrial sediments capped by Holocene-aged marine sediments.	Lacourse, T., Mathewes, R.W. and Fedje, D.W., 2005. Late-glacial vegetation dynamics of the Queen Charlotte Islands and adjacent continental shelf, British Columbia, Canada. Palaeogeography, Palaeoclimatology, Palaeoecology, 226(1-2), pp.36-57.	https://doi.org/10.1016/j.palaeo.2005.05.003
KEYHOLE	Neotoma	24278	42745	Keyhold Pond	-138.373465	61.078590	Western North America	826	Raw	Lake	101	AWI	-0.003	12.953	The slopes around the lake are steep and covered with grassland vegetation. The main components of the grasslands include Artemisia frigida and Agropyron yukonense. The boreal forest surrounding the grasslands is dominated by Picea glauca. Other important taxa in the area include Populus, Salix, and Betula glandulosa.	Whittmire, C.M., 2001. Vegetative and fire history of the area surrounding Keyhole Pond, Yukon Territory. Master's thesis. University of Regina, Regina, Saskatchewan, Canada.
MIRORCO	Neotoma	26173	45655	Mirror Lake	-106.432300	38.743205	Western North America	3347	Raw	Lake	44	AWI	0.008	3.814	Mirror Lake is a kettle lake formed by Pleistocene glaciers. Surrounding vegetation: Subalpine forest composed primarily of Picea engelmannii and Abies bifolia, with Picea pungens, Pinus contorta, P. latifolia, and Pseudotsuga menziesii occurring less frequently. Dominant riparian species consist of willow and several species of Salix. Juncus and Carex also occur near the shoreline. An isolated small population of Populus tremuloides occurs 300m above the lake.	Del Priore, T.M., 2007. 4,000 years of environmental change in central Colorado: a Paleoecological perspective. Master's thesis. University of Colorado, Boulder, CO, USA.
ANTHONY	Neotoma	26557	46290	Anthony Lake	-118.231425	44.959675	Western North America	2174	Raw	Lake	56	AWI	-0.009	7.727	Lake located in the Elkhorn Range of the Blue Mountains. Dominant arboreal species include Abies lasicocarpa (subalpine fir), Picea engelmannii (Engelmann spruce), Pinus contorta (lodgepole pine), and Pinus monticola (western white pine), along with scattered Tsuga mertesiana (mountain hemlock). Common nonarboreal species include Artemisia tridentata (sagebrush), Amelianchier alnifolia, (serviceberry), Vaccinium membranaceum (big huckleberry), Agropyron spicatum (bluebunch wheatgrass), and Xerophyllum tenax (bear grass) in an open forest-parkland structure. Riparian vegetation includes Alnus crispa (mountain alder) and several species of Carex (sedge).	Long, C.J., Shinker, J.J., Minckley, T.A., Power, M.J. and Bartlein, P.J., 2019. A 7600 yr vegetation and fire history from Anthony Lake, northeastern Oregon, USA, with linkages to modern synoptic climate patterns. Quaternary Research, 91(2), pp.705-713.	https://doi.org/10.1017/qua.2018.124
LWRTWIN	Neotoma	26558	46292	Twin Lakes	-113.910925	47.241520	Western North America	1263	Raw	Lake	75	AWI	-0.038	16.273	Twin Lakes consists of two small lakes located at the southwestern end of the Mission Range. This study is from the southeastern lake. The lake is surrounded by forests dominated by Pseudotsuga menziesii, Pinus ponderosa, Larix occidentalis, and Pinus contorta, with lesser amounts of Picea engelmannii, Abies grandis, and Thuja plicata. Riparian areas support Populus tremuloides, Populus balsamifera ssp.trichocarpa, and Salix spp. Common understory plants in the watershed include Acer glabrum, Holodiscus discolor,Prunus virginiana, Rosa woodsii, Physocarpus malvaceus, Xerophyllum tenax, and Vaccinium globulare. Species of Poaceae, Carex, Isoetes, Scirpus, and Typha grow along lake margins and in the lake.	Alt, M., McWethy, D.B., Everett, R. and Whitlock, C., 2018. Millennial scale climate-fire-vegetation interactions in a mid-elevation mixed coniferous forest, Mission Range, northwestern Montana, USA. Quaternary Research, 90(1), pp.66-82.	https://doi.org/10.1017/qua.2018.25
BDL12	Neotoma	26632	46603	Baldwin Lake	-116.806408	34.276446	Western North America	2060	Raw	Lake	89	AWI	15.855	102.140	Lake basin in Big Bear Valley of the San Bernardino Mountains. Lake is desiccated and dry most of the year, and throughout entire year in drought years.	Glover, K.C., Chaney, A., Kirby, M.E., Patterson, W.P. and MacDonald, G.M., 2020. Southern California Vegetation, Wildfire, and Erosion Had Nonlinear Responses to Climatic Forcing During Marine Isotope Stages 5-2 (120-15 ka). Paleoceanography and Paleoclimatology, 35(2), p.e2019PA003628.	https://doi.org/10.1029/2019PA003628	Glover, K.C., MacDonald, G.M., Kirby, M.E., Rhodes, E.J., Stevens, L., Silveira, E., Whitaker, A. and Lydon, S., 2017. Evidence for orbital and North Atlantic climate forcing in alpine Southern California between 125 and 10 ka from multi-proxy analyses of Baldwin Lake. Quaternary Science Reviews, 167, pp.47-62.	https://doi.org/10.1016/j.quascirev.2017.04.028
LWH081A	Neotoma	26634	46611	Little Windy Hill Pond	-106.336950	41.433255	Western North America	2980	Raw	Lake	108	AWI	0.016	17.338	Small groundwater-fed lake on the margin of a recessiona Pinedale moraine in the Medicine Bow Mountains. Forest surrounding the lake is old-growth Pinus contorta and Picea engelmannii, with Abies bifolia in the lower canopy. Understory includes Juniperus communis, Artemisia, Rosa, Ribes, Ericaceae, Poaceae, Asteraceae, and Amaranthaceae. Marginal fen is dominated by Carex, Kalmia microphylla, Pedicularis, and Picea engelmannii on raised surfaces.	Minckley, T.A., 2014. Postglacial vegetation history of southeastern Wyoming, USA. Rocky Mountain Geology, 49(1), pp.61-74.	https://doi.org/10.2113/gsrocky.49.1.61	Minckley, T.A. and Shriver, R.K., 2011. Vegetation responses to changing fire regimes in a Rocky Mountain forest. Fire Ecology, 7(2), pp.66-80.	https://doi.org/10.4996/fireecology.0702066	Minckley, T.A., Shriver, R.K. and Shuman, B., 2012. Resilience and regime change in a southern Rocky Mountain ecosystem during the past 17 000 years. Ecological Monographs, 82(1), pp.49-68.	https://doi.org/10.1890/11-0283.1
BEGBIE	Neotoma	26638	46630	Begbie Lake	-123.682930	48.585590	Western North America	188	Raw	Lake	65	AWI	-0.070	13.903	The vegetation immediately around Begbie Lake consists of multiple age classes. The tree stratum is dominated by Pseudotsuga menziesii, with lesser amounts of Tsuga heterophylla and Thuja plicata. Scattered Pinus contorta, Acer macrophyllum, Alnus rubra and Abies grandis occur around the basin. The understory contains small T. heterophylla trees as well as Gaultheria shallon, Mahonia nervosa and Polystichum munitum coupled with mosses. Aquatic vegetation includes Myrica gale, Cyperaceae, Potamogeton, and Nuphar.	Brown, K.J., Hebda, N.J.R., Schoups, G., Conder, N., Smith, K.A.P. and Trofymow, J.A., 2019. Long-term climate, vegetation and fire regime change in a managed municipal water supply area, British Columbia, Canada. The Holocene, 29(9), pp.1411-1424.	https://doi.org/10.1177/0959683619854523
LPAINTRK	Neotoma	26641	46645	Lower Paintrock Lake	-107.381835	44.392785	Western North America	2798	Raw	Lake	76	AWI	0.018	21.889	Glacial origin lake on the west slope of the Bighorn Mountains. Surrounded by mixed conifer forest of Pinus contorta, Picea engelmannii, and Pseudotsuga menziesii. Understory of Abies bifolia, Ribes lacustre, and Artemisia.	Rust, R.A. and Minckley, T.A., 2020. Fire and hydrologically mediated diversity change in subalpine forests through the Holocene. Journal of Vegetation Science, 31(3), pp.380-391.	https://doi.org/10.1111/jvs.12853
RNBWC	Neotoma	26644	46659	Rainbow Lake	-109.500240	44.936160	Western North America	2963	Raw	Lake	62	AWI	-0.044	19.932	The watershed is less than 20 ha on the crest of the Beartooth Mountains. Underlain by Archean granitic gneiss and drains seasonally into the Clarks Fork of the Yellowstone River. Mixed sub-alpine parkland dominated by Abies bifolia and Picea engelmannii. The understory and parkland matrix is a mix of Artemisia spp., Vaccinium myrtillus, and a variety of grasses and herbs (Poaceae, Asteraceae and Amaranthaceae).	Rust, R.A. and Minckley, T.A., 2020. Fire and hydrologically mediated diversity change in subalpine forests through the Holocene. Journal of Vegetation Science, 31(3), pp.380-391.	https://doi.org/10.1111/jvs.12853
HUMBIRD	Neotoma	26651	46672	Hummingbird Lake	-135.012050	56.551850	Western North America	46	Raw	Lake	45	AWI	-0.036	15.109	Lake is located on Baranof Island in the Alexander Archipelago. Lake is formed in a trough between bedrock ridges. Lake does not appear to have been overridden by glacial ice during the last glaical interval (Marine Isotope Stage 2). Vegetation is dense conifer forest of Tsuga heterophylla, Picea sitchensis, Tsuga mertensiana, Pinus contorta subsp. contorta, and Chamaecyparis nootkatensis.	Ager, T.A., 2019. Late Quaternary vegetation development following deglaciation of northwestern Alexander Archipelago, Alaska. Frontiers in Earth Science, 7, p.104.	https://doi.org/10.3389/feart.2019.00104
WLS	Neotoma	26658	46680	West LaSalle	-120.676060	53.519745	Western North America	878	Raw	Lake	52	AWI	-0.053	10.951	Vegetation surrounding the lake is composed of Tsuga heterophylla, Thuja plicata, Picea mariana and Abies lasiocarpa forest with shrubs and herbs typical of the ICHwk (e.g., Cornus canadensis, Oplopanax horribilis, Betula glandulosa, Betula pumila, Cornus stolonifera, Geum macrophyllum, three species each of Vaccinium and Salix, and four species of Rubus); ferns and mosses (e.g. Gymnocarpium dryopteris, Pleurozium schreiberii), ten species of Carex, and the aquatic Callitriche palustris.	White, A.L., 2014. Postglacial vegetation change in the interior temperate rainforest of British Columbia. Master's thesis. University of Oregon, Eugene, OR, USA.
PAISLEY2	Neotoma	26659	46682	Paisley Cave 2	-120.572770	42.756680	Western North America	1378	Raw	Cave	38	AWI	7.635	14.308	The Paisley Caves are in a basalt ridge on the southeastern end of the Summer Lake basin in Oregon. Cave 2 is approximately 7 m deep by 6 m wide. The surrounding shrub-steppe vegetation consists of various bunch grasses (Festuca idahoensis, Poa secunda, and Pseudoroegneria spicata) mixed with three main species of sagebrush (Artemisia arbuscula, A. rigida, and A. tridentata). Much of the area has exposed soils.	Jenkins, D.L., Davis, L.G., Stafford Jr, T.W., Campos, P.F., Connolly, T.J., Cummings, L.S., Hofreiter, M., Hockett, B., McDonough, K., Luthe, I. and O'Grady, P.W., 2013. In: Geochronology, archaeological context, and DNA at the Paisley Caves (pp.485-510). Texas A&M University Press, College Station, TX, USA.		Beck, C.W., Bryant, V.M. and Jenkins, D.L., 2018. Analysis of Younger Dryas-Early Holocene pollen in sediments of Paisley Cave 2, south-central Oregon. Palynology, 42(2), pp.168-179.	https://doi.org/10.1080/01916122.2017.1319883	Beck, C.W., Bryant, V.M. and Jenkins, D.L., 2020. Comparison of Neotoma (packrat) feces to associated sediments from Paisley Caves, Oregon, USA. Palynology, 44(4), pp.723-741.	https://doi.org/10.1080/01916122.2019.1702118
PAISRAT	Neotoma	26659	46684	Paisley Cave 2	-120.572770	42.756680	Western North America	1378	Raw	Cave	15	AWI	7.780	12.934	The Paisley Caves are in a basalt ridge on the southeastern end of the Summer Lake basin in Oregon. Cave 2 is approximately 7 m deep by 6 m wide. The surrounding shrub-steppe vegetation consists of various bunch grasses (Festuca idahoensis, Poa secunda, and Pseudoroegneria spicata) mixed with three main species of sagebrush (Artemisia arbuscula, A. rigida, and A. tridentata). Much of the area has exposed soils.	Jenkins, D.L., Davis, L.G., Stafford Jr, T.W., Campos, P.F., Connolly, T.J., Cummings, L.S., Hofreiter, M., Hockett, B., McDonough, K., Luthe, I. and O'Grady, P.W., 2013. In: Geochronology, archaeological context, and DNA at the Paisley Caves (pp.485-510). Texas A&M University Press, College Station, TX, USA.		Beck, C.W., Bryant, V.M. and Jenkins, D.L., 2018. Analysis of Younger Dryas-Early Holocene pollen in sediments of Paisley Cave 2, south-central Oregon. Palynology, 42(2), pp.168-179.	https://doi.org/10.1080/01916122.2017.1319883	Beck, C.W., Bryant, V.M. and Jenkins, D.L., 2020. Comparison of Neotoma (packrat) feces to associated sediments from Paisley Caves, Oregon, USA. Palynology, 44(4), pp.723-741.	https://doi.org/10.1080/01916122.2019.1702118
BEAUTY	Neotoma	26678	46730	Beauty Lake	-109.572015	44.968560	Western North America	2878	Raw	Lake	32	AWI	-0.051	15.014	Alpine lake in the Beartooth Mountain Range. The watershed contains sparse, alpine vegetation, and shallow soils with much exposed bedrock. Taller vegetation is largely in topographic depressions.	Spaulding, S.A., Stone, J.R., Norton, S.A., Nurse, A. and Saros, J.E., 2019. Paleoenvironmental context for the Late Pleistocene appearance of Didymosphenia in a North American alpine lake. Aquatic Sciences, 82(1), pp.1-15.	https://doi.org/10.1007/s00027-019-0681-9
MICA08	Neotoma	13879	46803	Mica Lake	-148.143440	60.686945	Western North America	100	Raw	Lake	70	AWI	-0.034	10.244	Lake located on Culross Island in western Prince William Sound. Upland vegetation is coastal spruce-hemlock forest, dominated by Picea sitchensis and Tsuga mertensiana, T. heterophylla, and Chamaecyparis nootkatensis. Common shrubs include Alnus sinuata, Vaccinium ovalifolium, Menziesia ferruginea, Oplopanax horridus, Cladothamnus pyrolaeflorus, Sorbus sitchensis, Rubus spectabilis, and Sambucus racemosa.	Anderson, R.S., Kaufman, D.S., Berg, E., Schiff, C. and Daigle, T., 2017. Holocene biogeography of Tsuga mertensiana and other conifers in the Kenai Mountains and Prince William Sound, south-central Alaska. The Holocene, 27(4), pp.485-495.	https://doi.org/10.1177/0959683616670217
SB-51B	Neotoma	26989	47506	Seal Beach wetland	-118.083540	33.739170	Western North America	1	Raw	Marsh	16	AWI	-0.055	1.910	Salt marsh in the Seal Beach National Wildlife Refuge. Surrounding vegetation: Spartina alterniflora, Sarcocornia pacifica, Jancus gerardii, and Monanthochloe littoralis.	Balmaki, B., Wigand, P.E., Frontalini, F., Shaw, T.A., Avnaim-Katav, S. and Rostami, M.A., 2019. Late Holocene paleoenvironmental changes in the Seal Beach wetland (California, USA): A micropaleontological perspective. Quaternary International, 530, pp.14-24.	https://doi.org/10.1016/j.quaint.2019.10.012
NUNAL15	Neotoma	26994	47535	Nunalleq	-161.844595	59.720390	Western North America	8	Raw	Archaeological	39	AWI	-0.007	0.470	The Nunalleq archaeological site is located in the Yukon-Kuskokwim delta, approximately 5 km south of the village of Quinhagak. The topography of the region is characterised by flat, low-lying treeless tundra dissected by rivers and dotted with small to medium sized lakes and ponds. The sampling location is located approximately 30 m east of the archaeological site. Surrounding vegetation: dwarf shrub lichen sphagnum permafrost plateau and undulating dwarf shrub tussock tundra. The shrub flora is dominated by Rubus chamaemorus, Betula nana, Empetrum nigrum, and Ledum palustre. Eriophorum angustifolium, Luzula, Hierochloe, and Festuca are common within the herbaceous component.	Ledger, P.M., 2018. Are circumpolar hunter-gatherers visible in the palaeoenvironmental record? Pollen-analytical evidence from Nunalleq, southwestern Alaska. The Holocene, 28(3), pp.415-426.	https://doi.org/10.1177/0959683617729447
CHICKREE	Neotoma	27028	47610	Chickaree Lake	-105.841095	40.334125	Western North America	2796	Raw	Lake	67	AWI	-0.060	6.052	Small, deep lake with no perennial streams feeding or draining the lake. Surrounded by even-aged stand of Pinus contorta. Subdominant trees include Picea engelmannii and Abies bifolia.	Dunnette, P.V., Higuera, P.E., McLauchlan, K.K., Derr, K.M., Briles, C.E. and Keefe, M.H., 2014. Biogeochemical impacts of wildfires over four millennia in a R ocky M ountain subalpine watershed. New Phytologist, 203(3), pp.900-912.	https://doi.org/10.1111/nph.12828	Chileen, B.V., 2019. Vegetation response to wildfire and climate forcing in a Rocky Mountain lodgepole pine forest over the past 2,500 years. Master's thesis. Kansas State University, Manhattan, Kansas, USA.
PEARSONS	Neotoma	27029	47621	Pearson's Pond	-122.256565	37.352695	Western North America	365	Raw	Lake	49	AWI	-0.029	3.769	Small pond formed by the Weeks Creek landslide. The pond is just below several slump blocks near the head of the slide. Vegetation around the pond is mainly grassland, but steep slopes support chaparral, and redwood and mixed evergreen forests occur along stream courses.	Adam, D.P., 1975. A late Holocene pollen record from Pearson's Pond, Weeks Creek Landslide, San Francisco Peninsula, California. Journal of Research of the US Geological Survey, 3(6), pp.721-731.	https://doi.org/10.3133/70007411
SWAN1962	Neotoma	27084	47687	Swan Lake	-111.992050	42.294395	Western North America	1450	Raw	Lake	44	AWI	-0.014	13.897	Swan Lake, a seasonal shallow pond, lies in Red Rock Pass at the north end of Cache Valley in the outlet area of pluvial Lake Bonneville. It was isolated from Lake Bonneville when it receded from the Provo level. Vegetation in the valley is Artemisia steppe with A. tridentata, Sarcobatus vermiculatus, Atriplix confertifolia, Ericameria spp., Suaeda spp., Salicornia rubra, Purshia tridentata, and Poaceae. Juniperus woodland and conifer forest occur at higher elevations in the mountains on either side of the valley. A dense stand of Typha latifolia, Scirpus/Schoenoplectus, and Sparganium fringes the pond.	Bright, R.C., 1966. Pollen and seed stratigraphy of Swan Lake, southeastern Idaho: Its relation to regional vegetational history and to Lake Bonneville history. Tebiwa, The Journal of the Idaho State University Museum, 9(2), pp.1-47.
SIL-04	Neotoma	27192	48361	Sunken Island Lake	-150.886230	60.593020	Western North America	76	Raw	Lake	59	AWI	-0.058	14.367	Kettle lake with two basins (northeast and southwest) separated by a low island that disappears with higher lake levels. A smaller sub-basin lies south of the island. The lake is formed in ice-marginal sands associated with the Moosehorn stadial moraine. It lies in the Kenai lowlands with post-fire successional forest dominated by Betula kenaica, Picea mariana, P. glauca, and Populus tremuloides. Additional trees and shrubs include Alnus viridis subsp. crispa, Populus trichocarpa, Sambucus racemosa, Rosa acicularis, Viburnum edule, Linnaea borealis, Rubus sp., Echinopanax horridum, Ribes sp., and Rhododendron tomentosum. Plants in moist areas around the lake include Salix sp., Myrica gale, Menziesia ferruginea, Spiraea beauverdiana, Betula nana, Streptopus amplexifolius, Lycopodium sp., Equisetum silvaticum, and E. arvense.	Anderson, R.S., Berg, E., Williams, C. and Clark, T., 2019. Postglacial vegetation community change over an elevational gradient on the western Kenai Peninsula, Alaska: pollen records from Sunken Island and Choquette Lakes. Journal of Quaternary Science, 34(4-5), pp.309-322.	https://doi.org/10.1002/jqs.3102
CL-06	Neotoma	27193	48363	Choquette Lake	-151.110580	59.945175	Western North America	517	Raw	Lake	59	AWI	-0.052	11.916	Lake lies on the southwest flank of the Caribou Hills. It is drained by fens on both ends. Much of the surrounding Caribou Hills is at or above treeline. Surrounding vegetation is opoen fens and sub-shrubland, including Betula nana, B. glandulosa, Salix arctica, Andromeda polifolia, Empetrum nigrum, Rubus chamaemorus and R. arctica, Vaccinium uliginosum, Pyrola asarifolia, Ledum palustre, Oxycoccus microcarpus and Spiraea beauverdiana. Immediately around the lake, Salix barclayi dominates. Picea glauca trees grew around Choquette Lake, but virtually all are now dead, killed by a recent spruce beetle (Dendroctonus) infestation.	Anderson, R.S., Berg, E., Williams, C. and Clark, T., 2019. Postglacial vegetation community change over an elevational gradient on the western Kenai Peninsula, Alaska: pollen records from Sunken Island and Choquette Lakes. Journal of Quaternary Science, 34(4-5), pp.309-322.	https://doi.org/10.1002/jqs.3102
WAWONA	Neotoma	27205	48549	Wawona Meadow	-119.645390	37.528580	Western North America	1275	Raw	Peat	20	AWI	-0.028	0.657	Site is a large northwest-southeast trending sedge meadow, located in the lower montane vegetation zone with Pinus ponderosa, Calocedrus decurrens, Pinus lambertiana, Abies concolor, Pseudotsuga menziesii, Quercus kelloggii and Cornus nuttallii. Meadow is dominated by Carex senta and C. nebraskensis, with Juncus nevadensis, J. mexicanus, Glyceria striata, and Agrostis. Willow shrubland occurs near the corring site, dominated by Salix lasiolepis, S. laegivata, S. lucida, and S. lemmonii. Pools contain Typha latifolia. Meadow drops from ~1280 m at SE end to ~1250 m at NW end.	Anderson, R.S. and Stillick Jr, R.D., 2013. 800 years of vegetation change, fire and human settlement in the Sierra Nevada of California, USA. The Holocene, 23(6), pp.823-832.	https://doi.org/10.1177/0959683612471985
MOR	Neotoma	27212	48616	Morkill Lake	-120.652279	53.606556	Western North America	780	Raw	Lake	37	AWI	-0.011	10.749	The immediate surroundings are flat and support Picea mariana bogs. The forest is composed of Picea engelmannii and Picea mariana, with Pinus contorta and few Pseudotsuga menziesii and Tsuga heterophylla. Shrubs include Betula sppand Ledum groenlandicum. The lake is ringed with a thick sphagnum layer. Water-edge and aquatic species noted include Menyanthes trifoliata, Nuphar polysepalum, Potamogeton spp. and Drosera rotundifolia.	Gavin, D.G., White, A., Sanborn, P.T. and Hebda, R.J., 2020. Deglacial landforms and Holocene vegetation trajectories in the northern interior cedar-hemlock forests of British Columbia. In: Untangling the Quaternary Period: A Legacy of Stephen C. Porter. ed by R.B. Waitt, G.D. Thackray, and A.R. Gillespie (pp.1-20). Geological Society of America.	https://doi.org/10.1130/2020.2548(05)
FloatingIsland_neotoma	Neotoma	811	70001	Floating Island Lake	-107.466667	44.550000	Western North America	2609	Raw	Lake	89	AWI	-0.014	12.464	Kettle lake with floating sedge mat. Physiography: Bighorn Mountains. Surrounding vegetation: lodgepole pine forest.	Burkart, M.R., 1976. Pollen biostratigraphy and late Quaternary vegetation history of the Bighorn Mountains, Wyoming. Doctoral dissertation. University of Iowa, Iowa City, Iowa, USA.