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Herzschuh, Ulrike; Böhmer, Thomas; Li, Chenzhi; Cao, Xianyong; Dolman, Andrew M; Postl, Alexander; Heim, Birgit; Wieczorek, Mareike (2023): Description of sampling sites in the Asian region [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.933112

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Keyword(s):
fossil pollen; Neotoma; paleoecology; taxonomically harmonized
Coverage:
Median Latitude: 46.489435 * Median Longitude: 113.877667 * South-bound Latitude: 18.383333 * West-bound Longitude: 45.466667 * North-bound Latitude: 75.333333 * East-bound Longitude: -170.248270
Date/Time Start: 1959-06-17T00:00:00 * Date/Time End: 2011-08-11T00:00:00
Minimum ELEVATION: -479 m a.s.l. * Maximum ELEVATION: 5058 m a.s.l.
Event(s):
11-CH-12A  * Latitude: 72.398881 * Longitude: 102.288566 * Date/Time: 2011-08-11T00:00:00 * Elevation: 60.0 m * Location: Taymyr peninsula, northern Siberia * Campaign: RU-Land_2011_Khatanga (Chatanga2011) * Basis: AWI Arctic Land Expedition * Method/Device: Gravity corer, UWITEC (GCUWI) * Comment: Lake radius: 90 m
ACHIT8  * Latitude: 49.500000 * Longitude: 90.600000 * Date/Time: 1978-06-30T00:00:00 * Elevation Start: 1435.0 m * Elevation End: 2.8 m * Location: Achit-Nur, Mongolia
ACHITNUR (Achit Nur Lake)  * Latitude: 49.500000 * Longitude: 90.600000 * Location: Asia
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
Event labelEventHerzschuh, Ulrike
Reference/sourceReferenceHerzschuh, UlrikeEvent
IdentificationIDHerzschuh, UlrikeSite
IdentificationIDHerzschuh, UlrikeDataset
SiteSiteHerzschuh, Ulrike
LONGITUDELongitudeHerzschuh, UlrikeGeocode
LATITUDELatitudeHerzschuh, UlrikeGeocode
ContinentContHerzschuh, Ulrike
ELEVATIONElevationm a.s.l.Herzschuh, UlrikeGeocode
10 TypeTypeHerzschuh, Ulrikeof data
11 Location typeLoc typeHerzschuh, Ulrike
12 Sample amountN#Herzschuh, UlrikePollen samples in core
13 Reference/sourceReferenceHerzschuh, UlrikeAgeModel
14 Age, minimum/youngAge minkaHerzschuh, Ulrike
15 Age, maximum/oldAge maxkaHerzschuh, Ulrike
16 DescriptionDescriptionHerzschuh, UlrikeSite Description from Neotoma
17 Reference/sourceReferenceHerzschuh, UlrikeLiterature source #1
18 Uniform resource locator/link to referenceURL refHerzschuh, UlrikeLiterature source #1
19 Reference/sourceReferenceHerzschuh, UlrikeLiterature source #2
20 Uniform resource locator/link to referenceURL refHerzschuh, UlrikeLiterature source #2
21 Reference/sourceReferenceHerzschuh, UlrikeLiterature source #3
22 Uniform resource locator/link to referenceURL refHerzschuh, UlrikeLiterature source #3
23 Reference/sourceReferenceHerzschuh, UlrikeLiterature source #4
24 Uniform resource locator/link to referenceURL refHerzschuh, UlrikeLiterature source #4
25 Reference/sourceReferenceHerzschuh, UlrikeLiterature source #5
26 Uniform resource locator/link to referenceURL refHerzschuh, UlrikeLiterature source #5
27 Reference/sourceReferenceHerzschuh, UlrikeLiterature source #6
Status:
Curation Level: Enhanced curation (CurationLevelC)
Size:
6869 data points

Data

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


Event

Reference
(Event)

ID
(Site)

ID
(Dataset)

Site

Longitude

Latitude

Cont

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)
27 
Reference
(Literature source #6)
Adycha_River Neotoma1111Konus Exposure, Adycha River135.58333367.750000Asia130RawRiver13AWI1.0079.817Exposure on slope. Surrounding vegetation: open Larix dahurica forest.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.
AKULININ Neotoma1919Akulinin Exposure P1282138.55000047.116667Asia20RawRiver29AWI4.81044.906Exposure in river terrace. Physiography: river valley in mountains. Surrounding vegetation: secondary Betula forest.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Kind, N.V., 1974. Geochronology of the late Anthropogene by isotopic data. Nauka, Moscow (in Russian).Korotkii, A.M., Karaulova, L.P. and Troitskaya, T.S., 1980. The Quaternary deposits of Primor'ye. Nauka, Novosibirsk (in Russian).Korotky, A.M., Kovalyukh, N.N. and Volkov, V.G., 1989. Radiocarbon dating of Quaternary deposits (south Far East). Preprint. Far East Branch of the USSR Academy of Sciences, Vladivostok (in Russian).Korotky, A.M., Pletnev, S.P., Pushkar, V.S., Grebennikova, T.A., Raszhigaeva, N.T., Sahebgareeva, E.D. and Mohova, L.M., 1988. Evolution environment of south Far East (late Pleistocene and Holocene). Nauka, Moscow (in Russian).
ALUT Neotoma3131Alut Lake152.31277860.136667Asia480RawLake117AWI-0.06634.322Tectonic lake. Physiography: valley in mountains. Surrounding vegetation: Larix forest.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Anderson, P.M., Lozhkin, A.V., Belaya, B.V. and Stetsenko, T.V., 1998. New data about the stratigraphy of late Quaternary deposits of northern Priokhot'ye. In: Environmental changes in Beringia during the Quaternary ed. by K.V. Simakov (pp.69-87). North East Interdisciplinary Research Institute, Far East Branch, Russian Academy of Sciences, Magadan (in Russian).Anderson, P.M. and Lozhkin, A.V., 2001. The latest Pleistocene interstade (Karginskii/Boutellier interval) of Beringia: variations in paleoenvironments and implications for paleoclimatic interpretations. Quaternary Science Reviews, 20(1-3), pp.93-125.doi:10.1016/S0277-3791(00)00129-3
AMBA Neotoma3333Amba River Exposure 596131.81666743.316667Asia5RawMarine8AWI1.6135.706Exposure of alluvial and lagoon sediment. Physiography: coastal plain. Surrounding vegetation: Quercus-Carpinus-Abies holophylla forest.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Korotky, A.M., Karaulova, L.P. and Troitskaya, T.S., 1980. The Quaternary deposits of Primor'ye. Nauka, Novosibirsk (in Russian).
AMGUEMA1 Neotoma6868Amguema River Valley Exposure 1178.70000067.750000Asia175RawRiver4AWI1.78825.242Exposure in a mine excavation. Physiography: river valley in glacial outwash. Surrounding vegetation: shrub tundra.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Kotov, A.N., 1997. Cryolithogenesis in the ablation zone of late Pleistocene glaciers. In: Results of fundamental investigations of the cryosphere of earth in the Arctic and Subarctic, 1996 (pp.249-259). Nauka, Novosibirsk (in Russian).Lozhkin, A.V., Trumpe, M.A., Polujan, A.I., Kotova, L.N. and Takmazyan, E.D., 1995. Radiocarbon dates for upper Quaternary sequences in northeastern Asia and Alaska. In: History of climate and vegetation in Beringia during the late Cenozoic ed. by Y.M. Bychkov and A.V. Lozhkin (pp.169-184). North East Interdisciplinary Research Institute, Far East Branch, Russian Academy of Sciences, Magadan (in Russian).
AMGUEMA2 Neotoma6969Amguema River Valley Exposure 2178.60000067.666667Asia87RawRiver8AWI1.8883.039Exposure in river bank. Physiography: river valley in glacial outwash. Surrounding vegetation: shrub tundra.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Kotov, A.N., 1997. Cryolithogenesis in the ablation zone of late Pleistocene glaciers. In: Results of fundamental investigations of the cryosphere of earth in the Arctic and Subarctic, 1996 (pp.249-259). Nauka, Novosibirsk (in Russian).Lozhkin, A.V., Trumpe, M.A., Polujan, A.I., Kotova, L.N. and Takmazyan, E.D., 1995. Radiocarbon dates for upper Quaternary sequences in northeastern Asia and Alaska. In: History of climate and vegetation in Beringia during the late Cenozoic ed. by Y.M. Bychkov and A.V. Lozhkin (pp.169-184). North East Interdisciplinary Research Institute, Far East Branch, Russian Academy of Sciences, Magadan (in Russian).
BARABA Neotoma228230Lower Barabaschevka River Exposure 594131.60000043.133333Asia5RawRiver6AWI4.85310.240Exposure in alluvium-marine terrace. Physiography: lower river valley. Surrounding vegetation: Quercus-Carpinus-Abies holophylla forest.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Korotky, A.M., Karaulova, L.P. and Troitskaya, T.S., 1980. The Quaternary deposits of Primor'ye. Nauka, Novosibirsk (in Russian).
BELSKALA Neotoma251256Belaya Skala Exposure134.56666743.250000Asia4RawCoast14AWI0.3576.845Lagoon terrace. Physiography: coastal plain. Surrounding vegetation: Quercus mongolica-Betula forest.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Korotky, A.M. and Karaulova, L.P., 1975. New data about the stratigraphy of Quaternary deposits of Primor'ye. In: Questions of geomorphology and Quaternary geology of the southern Far East ed. by A.M. Korotky and A.P. Kulakov (pp.79-110). Far Eastern Branch, USSR Academy of Sciences, Vladivostok (in Russian).Korotky, A.M., Karaulova, L.P. and Troitskaya, T.S., 1980. The Quaternary deposits of Primor'ye. Nauka, Novosibirsk (in Russian).
Indigirka_Lowland Neotoma253259Berelyekh River, Indigirka Lowland145.00000070.583333Asia20RawRiver16AWI8.51520.446Exposure on river terrace. Physiography: river valley. Surrounding vegetation: shrub tundra.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Lozhkin, A.V., 1977. Environment of the Berelyekh mammoth population. In: Mammoth fauna of the Russian plain and Eastern Siberia ed. by O.A. Skarlato (pp.67-68). Zoological Institute, USSR Academy of Sciences, Leningrad (in Russian).Lozhkin, A.V., 1998. Questions concerning radiocarbon data and palynological characteristics of the mammoth burials, Berelyekh River, lower Indigirka drainage. In: Environmental changes in Beringia during the Quaternary ed. by K.V. Simakov (pp.45-62). North East Interdisciplinary Research Institute, Far East Branch, Russian Academy of Sciences, Magadan (in Russian).Vereschagin, N.K., 1977. Berelyekh mammoth \cemetery\. In: Mammoth fauna of the Russian plain and Eastern Siberia ed. by O.A. Skarlato (pp.5-50). Zoological Institute, USSR Academy of Sciences, Leningrad (in Russian).
BETENK Neotoma255261Betenkyos Exposure, Adycha River135.58333367.666667Asia135RawRiver10AWI-0.0612.967Floodplain exposure. Physiography: river valley. Surrounding vegetation: open Larix dahurica forest.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.
BLUD Neotoma278284Bludlivaya River148.40000069.066667Asia100RawRiver3AWI26.44042.569Exposure in alluvial terrace. Physiography: river valley in lowland. Surrounding vegetation: Larix dahurica forest with bogs and lichen.
BOLOTNYI Neotoma293299Bolotnyii Stream Exposure 117132.78333342.850000Asia4RawLake16AWI30.07144.254Exposure on stream terrace. Physiography: coastal plain. Surrounding vegetation: Quercus mongolica-Betula forest.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.
Byllatskoye Neotoma320327Byllatskoye Exposure, Byllat River, Indigirka Basin140.06250069.165278Asia316RawRiver6AWI2.92443.921Exposure in river channel. Physiography: river valley. Surrounding vegetation: open Larix forest.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.
CAMPING Neotoma328335Chistoye Lake Exposure151.83333359.550000Asia91RawLake13AWI0.1877.555Peat exposure along lake shore. Physiography: tectonic basin. Surrounding vegetation: Larix dahurica muskeg.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Anderson, P.M., Belaya, B.V., Glushkova, O.Y. and Lozhkin, A.V., 1997. New data about the vegetation history of northern Priokhot'ye during the Late Pleistocene and Holocene. In: Late Pleistocene and Holocene of Beringia ed. by M.K. Gagiev (pp.33-54). North East Interdisciplinary Research Institute, Far East Branch, Russian Academy of Sciences, Magadan (in Russian).
CHABADA2 Neotoma346354Chabada Lake129.37787561.976835Asia290RawLake116AWI-0.02713.451Thermokarst lake. Physiography: Lena Plain. Surrounding vegetation: taiga.Tarasov, P.E., Harrison, S.P., Saarse, L., Pushenko, M.Y., Andreev, A.A., Aleshinskaya, Z.V., Davydova, N.N., Dorofeyuk, N.I., Efremov, Y.V., Khomutova, V.I., Sevastyanov, D.V., Tamosaitis, J., Uspenskaya, O.N., Yakushko, O.F. and Tarasova, I.V., 1994. Lake status records from the former Soviet Union and Mongolia: data base documentation. Paleoclimatology Publications Series 2, World Data Center-A for Paleoclimatology, NOAA Paleoclimatology Program, Boulder, Colorado, USA.Andreev, A.A., Klimanov, V.A., Sulerzhitsky, L.D. and Khotinsky, N.A., 1989. Chronology of environmental changes in central Yakutia during the Holocene. In: Paleoklimaty golotsena i pozdnelednikov'ya [Paleoclimates of Holocene and late glacial) (pp.115-121). Nauka, Moscow, Russia (in Russian).
CHERYAR Neotoma356364Chernyii Yar Exposure 955134.43333343.183333Asia4RawRiver36AWI0.53613.220Alluvium-lagoon terrace. Physiography: swampy area of lower river valley. Surrounding vegetation: Larix-Alnus-Betula forest and bogs.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Golubeva, L.V. and Karaulova, L.P., 1983. The vegetation and stratigraphy of the Pleistocene and Holocene of the southern Far East. Nauka, Moscow (in Russian).Korotky, A.M. and Karaulova, L.P., 1975. New data about the stratigraphy of Quaternary deposits of Primor'ye. In: Questions of geomorphology and Quaternary geology of the southern Far East ed. by A.M. Korotky and A.P. Kulakov (pp.79-110). Far Eastern Branch, USSR Academy of Sciences, Vladivostok (in Russian).Korotkii, A.M., Karaulova, L.P. and Troitskaya, T.S., 1980. The Quaternary deposits of Primor'ye. Nauka, Novosibirsk (in Russian).Pushkar, V.S., 1979. Biostratigraphy of sediments of the late Anthropogene of the southern Far East. Nauka, Moscow (in Russian).
CHESNOK Neotoma357365Chesnok Peat, Irtysh River66.50000060.000000Asia42RawPeat36AWI0.22910.712Peat exposure in river bank. Physiography: river valley lowland. Surrounding vegetation: Pinus sylvestris-P. sibirica-Betula.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Bakhareva, V.A., 1985. The palynological characteristics of late Quaternary and Holocene deposits in the vicinity of Perschino village on the Irtysh River. In: The palynostratigraphy of the Mesozoic and Cenozoic of Siberia ed. by V.S. Volkova, and A.F. Khlonova (pp.115-120). Nauka, Novosibirsk (in Russian).Volkov, I.A., Gurtovaya, E.E. and Firsov, L.V., 1973. The structure, age and history of Holocene peat near Gorno-Slinkino village on the Irtysh River. In: The Pleistocene of Siberia and neighboring regions ed. by V.N. Saks (pp.55-68). Nauka, Moscow (in Russian).Volkova, V.S., 1966. The Quaternary deposits of the lower Irtysh River and their biostratigraphic characteristics. Nauka, Novosibirsk (in Russian).
DERPUT Neotoma664682Derput124.11666757.033333Asia700RawPeat52AWI0.44312.871Section of ancient peat (hill now). Physiography: neotectonic fall by the Yakokit river. Surrounding vegetation: open larch forest, shrub birch, Sphagnum.Andreev, A.A. and Klimanov, V.A., 1991. Izmeneniya rastitel'nost i klimatamezhdurech'ya rek Ungra i Yakokit (Yuzhnaya Yakutia) v golotsene [Vegetation history and climate changes in the interfluve of the rivers Ungra and Yakokit (Southern Yakutia) during the Holocene]. Botanichesky Zhurnal, 76(3), pp.334-351.
Dlinnoye_Lake Neotoma695715Dlinnoye Lake-178.84226067.756725Asia280RawLake11AWI-0.0381.336Morainally dammed lake. Physiography: glacio-fluvial features in uplands. Surrounding vegetation: graminoid-Salix-Ericales tundra.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.
EK4 Neotoma769788Elikchan 4 Lake151.88333360.750000Asia810RawLake126AWI0.03563.528Morainally dammed lake. Physiography: valley lowland in mountainous region. Surrounding vegetation: Larix forest.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Anderson, P.M., Lozhkin, A.V. and Belaya, B.V., 1998. Younger Dryas in western Beringia (northeastern Siberia). In: Environmental changes in Beringia during the Quaternary ed. by K.V. Simakov (pp.28-44). North East Interdisciplinary Research Institute, Far East Branch, Russian Academy of Sciences, Magadan (in Russian).Anderson, P.M. and Lozhkin, A.V., 2001. The Stage 3 interstadial complex (Karginskii/middle Wisconsinan interval) of Beringia: variations in paleoenvironments and implications for paleoclimatic interpretations. Quaternary Science Reviews, 20(1-3), pp.93-125.doi:10.1016/S0277-3791(00)00129-3Lozhkin, A.V., 1995. A late Quaternary pollen record from Elikchan 4 Lake, northeast Siberia. Geology of the Pacific Ocean, 14, pp.18-22.Lozhkin, A.V., Anderson, P.M. and Belaya, B.V., 1995. Radiocarbon dates and carbon zones from lacustrine sediments from the region of the Kolyma-Okhotsk drainage divide. Doklady Akademii Nauk, 343(3), pp.396-399 (in Russian).
ICDP5011-1 Neotoma772791Elgygytgyn Stream Section172.08333367.416667Asia490RawStream4AWI5.2215.975Section on small stream. Physiography: impact crater. Surrounding vegetation: low shrub-lichen tundra with Salix.Glushkova, O.Y., Lozhkin, A.V. and Solomatkina, T.B., 1996. Stratigraphy and palaeogeography of the Elgygytgyn Lake in the Holocene (northwestern Chukotka). Geology of the Pacific Ocean, 12(4), pp.617-628 (in Russian).
ELGENNYA Neotoma773792Elgennya Lake149.00000062.083333Asia1040RawLake52AWI-0.05118.547Morainally dammed lake. Physiography: narrow upland valley bordered by mts. Surrounding vegetation: larch forest-tundra.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Anderson, P.M., Lozhkin, A.V., Belaya, B.V., Glushkova, O.Y. and Brubaker, L.B., 1997. A lacustrine pollen record from near altitudinal forest limit, upper Kolyma region, northeastern Siberia. The Holocene, 7(3), pp.331-335.doi:10.1177/095968369700700309Lozhkin, A.V., Anderson, P.M., Belaya, B.V., Glushkova, O.Y., Kozhevinkova, M.V. and Kotova, L.N., 1996. Palynological characteristics and radiocarbon dates of sediments from Elgennya Lake, Upper Kolyma. In: Quaternary climates and vegetation of western Beringia ed. by Bychkov, Y.M. (pp.50-64). North East Interdisciplinary Research Institute, Far East Branch, Russian Academy of Sciences, Magadan (in Russian).
ENM109 Neotoma779799Enmyvaam River, 2.5-3 m terrace172.16666767.433333Asia491RawRiver10AWI2.06510.865Alluvial terrace. Physiography: impact crater. Surrounding vegetation: low shrub tundra.Glushkova, O., Lozhkin, A.V. and Solomatkina, T.B., 1996. Stratigraphy and palaeogeography of the Elgygytgyn Lake in the Holocene (northwestern Chukotka). Geology of the Pacific Ocean, 12(4), pp.617-628 (in Russian).Kaplina, T.N. and Chekovskii, A.L., 1987. Reconstruction of paleogeographic conditons during the Holocene climatic optimum in the Primorski Lowlands of Yakutia. In: Quaternary period of northeast Asia (pp.141-151). SVKNII, DVO USSR Academy of Sciences, Magadan, Russia (in Russian).Lozhkin, A.V. and Vazhenina, L.N., 1987. The characteristics of vegetational development from the Kolyma lowland in the early Holocene. In: Quaternary period of northeast Asia ed. by V.P. Pokhialainen (pp.135-144). North East Interdisciplinary Research Institute, Far East Branch, USSR Academy of Sciences, Magadan (in Russian).
ENMYN Neotoma781801Enmynveem River166.00000068.250000Asia500RawRiver16AWI2.88110.881Exposure of peat and colluvium. Physiography: river valley in rolling uplands. Surrounding vegetation: open Larix dahurica forest.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.
ENTARNOY Neotoma784804Entarnoye Peat Exposure78.33333359.000000Asia65RawPeat30AWI0.89716.136River bank exposure. Physiography: river lowland. Surrounding vegetation: Pinus-Betula taiga.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Arkhipov, S.A., Levina, T.P. and Panychev, V.A., 1980. Palynological characteristics of two Holocene peats from the middle and lower Ob River valley. In: Paleopalynology of Siberia ed. by V.N. Saks (pp.123-127). Nauka, Moscow (in Russian).Neishtadt, M.I., 1976. About environmental changes in middle taiga of western Siberia during the Holocene. In: Palynology of the USSR ed. by E.D. Zaklinskaya and M.I. Neishtadt (pp.156-161). Nauka, Moscow (in Russian).
GEK Neotoma838866Gek Lake147.65000063.383333Asia969RawLake22AWI0.0239.896Morainally dammed lake. Physiography: glacial terrain in broad mt. valley. Surrounding vegetation: Larix dahurica forest-shrub tundra.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Stetsenko, T.V., 1998. A pollen record from Holocene Lake deposits in the Malyk-Siena depression, upper Kolyma basin. In: Environmental changes in Beringia during the Quaternary ed. by K.V. Simakov (pp.63-68). North East Interdisciplinary Research Institute, Far East Branch, Russian Academy of Sciences, Magadan (in Russian).
GLADKOYE Neotoma847876Gladkoye Bog83.33333355.000000Asia80RawPeat57AWI0.13311.153Peat bog. Physiography: river valley. Surrounding vegetation: meadows-Betula-Populus forest.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Firsov, L.V., Volkova, V.S., Levina, T.P., Nikolaeva, I.V., Orlova, L.A., Panychev, V.A. and Volkov, I.A., 1982. The stratigraphy, geochronology, and standard spore-pollen diagram for Holocene peat, Gladkoye Bog, Novosibirsk. In: Problems of stratigraphy and paleogeography of the Pleistocene of Siberia ed. by S.A. Arkhipov (pp.96-107). Nauka, Novosibirsk (in Russian).Orlova, L.A., 1990. The Holocene of Baraba (stratigraphy and radiocarbon chronology). Joint Institute for Geology, Geophysics and Mineralogy, Siberia Branch, USSR Academy of Sciences, Novosibirsk (in Russian).
GLUPEAT Neotoma851880Peat Exposure, Glukhoye Lake149.91666759.750000Asia10RawPeat6AWI3.5277.866Peat exposure. Physiography: coastal lowland. Surrounding vegetation: Larix-Betula forest; graminoid meadows.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Lozhkin, A.V., Skorodumov, I.N., Meshkov, A.P. and Rovako, L.G., 2014. Changed paleogeographic environments in the region of Glukhoye Lake (north coast of the Okhotsk Sea) during the Pleistocene-Holocene transition. Doklady Akademii Nauk, 316(1), pp.184-188 (in Russian).
GOLUBOY Neotoma939968Goluboye Lake152.26666761.116667Asia810RawLake41AWI0.12913.471Lake formed by colluvial fan blockage. Physiography: glacial terrain in broad mt. valley. Surrounding vegetation: Larix dahurica-lichen woodland.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Lozhkin, A.V., Anderson, P.M., Belaya, B.V., Glushkova, O.Y. and Stetsenko, T.V., 2000. Vegetation change in northeast Siberia at the Pleistocene-Holocene boundary and during the Holocene. In: The Quaternary period of Beringia ed. by K.V. Simakov (pp.53-75). North East Interdisciplinary Research Institute, Far East Branch, Russian Academy of Sciences, Magadan (in Russian).
GURSKII Neotoma966997Gurskii Peat [Site 4381]137.08333350.066667Asia15RawPeat31AWI0.20313.840Peat exposure in drainage channel. Physiography: river valley. Surrounding vegetation: bog shrubs and Sphagnum.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Korotky, A.M., 1982. Paleographic conditions of the formation of Quaternary peats (south of Far East). In: Modern sedimentation and morpholithogenesis of the Far East ed. by S.P. Pletnev and V.S. Pushkar (pp.58-71). Far Eastern Science Center, USSR Academy of Sciences, Vladivostok (in Russian).Korotky, A.M., Kovalyukh, N.N. and Volkov, V.G., 1989. Radiocarbon dating of Quaternary deposits (south Far East). Preprint. Far East Branch of the USSR Academy of Sciences, Vladivostok (in Russian).Sochava, V.B., 1968. The map of vegetation of the Amur Basin. Geodesy and Cartography Administration, Leningrad (in Russian).
GYTGYKAI Neotoma967998Gytgykai Lake175.00000063.166667Asia102RawLake68AWI6.30623.813Physiography: glacial terrain in tectonic valley. Surrounding vegetation: Pinus pumila-Alnus fruticosa tundra.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Lozhkin, A.V., Anderson, P.M., Brubaker, L.B., Kotov, A.N., Kotova, L.N., Prokhorova, T.P. and Simakov, K.V., 1998. The herb pollen zone from sediments of glacial lakes. In: Environmental Changes in Beringia During the Quaternary ed. by K.V. Simakov (pp.96-111). North East Interdisciplinary Research Institute, Far East Branch, Russian Academy of Sciences, Magadan (in Russian).
IGARKA Neotoma11081141Igarka Peat Exposure86.00000067.666667Asia45RawPeat22AWI5.65511.190Buried peat exposed in river terrace. Physiography: lower river valley. Surrounding vegetation: Picea obovata-Larix sibirica forest.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Il'ina, N.S., Lapshina, E.I. and Lavrenko, N.I., 1985. The vegetation cover of the western Siberia continental plateau. Nauka, Siberia Branch, Novosibirsk (in Russian).Kats, S.V., 1953. History of vegetation of western Siberia during the Holocene. Bulletin of commission for study the Quaternary. Nauka, Moscow, 13, pp.118-123 (in Russian).Levkovskaya, G.M., Kind, N.V., Zavel'skii, F.S. and Forova, V.S., 1970. Absolute age of peat from the Igarka region and Holocene zonal sequences of western Siberia. Bulletin of commission for study the Quaternary. Nauka, Moscow, 37, pp.94-101 (in Russian).Orlova, V.V., 1962. Climate of the USSR: western Siberia. Gidrometizdat, Leningrad (in Russian).
Ilinka_Terrace Neotoma11111144Il'inka Terrace142.16666747.966667Asia3RawMarine4AWI0.6462.698Exposure in marine terrace. Physiography: river mouth on sea coast. Surrounding vegetation: meadows and bogs.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Korotky, A., Grebennikova, T., Razjigaeva, N., Volkov, V., Mokhova, L., Ganzey, L. and Bazarova, V., 1997. Marine terraces of western Sakhalin Island. Catena, 30(1), pp.61-81.doi:10.1016/S0341-8162(97)00002-7Korotkiy, A.M., Pushkar, V.S., Grebennikova, T.A., Razzhigaeva, N.G., Karaulova, L.P., Mokhova, L.M., Ganzey, L.A., Cherepanova, M.N., Bazarova, V.B., Volkov, V.G. and Kovalyukh, N.N., 1997. Marine terraces and Quaternary history of the Sakhalin Shelf. Dal'nauka, Vladivostok (in Russian).
Izylmetevskaya Neotoma11221156Izylmet'evskaya Terrace Exposure 3410141.96666748.816667Asia4RawCoast15AWI3.0154.817Exposure in marine terrace. Physiography: coastal plain. Surrounding vegetation: Larix forest with bogs.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Korotky, A., Grebennikova, T., Razjigaeva, N., Volkov, V., Mokhova, L., Ganzey, L. and Bazarova, V., 1997. Marine terraces of western Sakhalin Island. Catena, 30(1), pp.61-81.doi:10.1016/S0341-8162(97)00002-7Korotkiy, A.M., Pushkar, V.S., Grebennikova, T.A., Razzhigaeva, N.G., Karaulova, L.P., Mokhova, L.M., Ganzey, L.A., Cherepanova, M.N., Bazarova, V.B., Volkov, V.G. and Kovalyukh, N.N., 1997. Marine terraces and Quaternary history of the Sakhalin Shelf. Dal'nauka, Vladivostok (in Russian).
JACKLOND Neotoma11241158Jack London Lake149.50000062.166667Asia820RawLake60AWI0.20817.872Morainally dammed lake. Physiography: glacial topography in mountains. Surrounding vegetation: larch forest.Lozhkin, A.V., Anderson, P.M., Eisner, W.R., Ravako, L.G., Hopkins, D.M., Brubaker, L.B., Colinvaux, P.A. and Miller, M.C., 1993. Late Quaternary lacustrine pollen records from southwestern Beringia. Quaternary Research, 39(3), pp.314-324.doi:10.1006/qres.1993.1038
Wrangle_Island_JackLondonLake Neotoma11261161Jack London Lake179.62361170.894167Asia7RawLake20AWI0.32115.024Shallow lake on coastal plain. Surrounding vegetation: Cyperaceae-Poaceae tundra.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Lozhkin, A.V., Anderson, P.M., Vartanyan, S.L., Brown, T.A., Belaya, B.V. and Kotov, A.N., 2001. Late Quaternary paleoenvironments and modern pollen data from Wrangel Island (Northern Chukotka). Quaternary Science Reviews, 20(1-3), pp.217-233.doi:10.1016/S0277-3791(00)00121-9
KALIST Neotoma13971433Kalistratikha Exposure83.25000053.333333Asia190RawRiver14AWI14.72246.052Exposure on 50 m terrace of the Ob River. Physiography: river valley. Surrounding vegetation: Betula-Pinus forest with Poaceae meadows.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Panychev, V.A. and Orlova, L.A., 1973. The radiocarbon age of Kalmanskoii suite of Biisko-Barnaul'skoii Depression. In: Pleistocene of Siberia and neighboring region ed. by V.N. Saks (pp.51-54). Nauka, Moscow (in Russian).Zudin, A.N. and Votakh, M.R., 1977. The stratigraphy of Pliocene and Quaternary strata of Priobskogo Plateau. Nauka, Novosibirsk (in Russian).
KARASYE Neotoma14021439Karasye Lake70.22000053.030000Asia435RawLake38AWI-0.0376.204Tectonic lake with outlet. Physiography: Kokchetav massif, low granite hills. Surrounding vegetation: pine forest.Tarasov, P.E., Harrison, S.P., Saarse, L., Pushenko, M.Y., Andreev, A.A., Aleshinskaya, Z.V., Davydova, N.N., Dorofeyuk, N.I., Efremov, Y.V., Khomutova, V.I., Sevastyanov, D.V., Tamosaitis, J., Uspenskaya, O.N., Yakushko, O.F. and Tarasova, I.V., 1994. Lake status records from the former Soviet Union and Mongolia: data base documentation. Paleoclimatology Publications Series 2, World Data Center-A for Paleoclimatology, NOAA Paleoclimatology Program, Boulder, Colorado, USA.Kremenetski, C., Tarasov, P. and Cherkinsky, A., 1997. Postglacial development of Kazakhstan pine forests. Geographie physique et Quaternaire, 51(3), pp.391-404.doi:10.7202/033138arTarasov, P.E. and Kremenetskii, K.V., 1995. Geochronology and stratigraphy of the Holocene lacustrine-bog deposits in northern and central Kazakhstan. Stratigraphy and Geological Correlation, 3(1), pp.73-80.
KARGA Neotoma14041441Karginskii Cape Peat Exposure85.00000070.000000Asia60RawPeat19AWI1.1609.026Peat exposure in river bluff. Physiography: river valley. Surrounding vegetation: Pinus sylvestris-P. sibirica-tree Betula.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Firsov, L.V., Levina, T.P. and Troitskii, S.L., 1972. The Holocene climatic changes in northern Siberia. In: Climatic changes in arctic areas during the last ten thousand years ed. by V. Vasari, H. Hyvarinen, and S. Hicks (pp.341-349). Acta Universitatis Onlensis. Section A., Scientitae Rerum Naturalium Number 3, Geologica Number 3. University of Oula, Oula.Kind, N.V., 1969. Late glacial and post-glacial times in Siberia (new data about absolute geochronology). In: Holocene ed. by M.I. Neishtadt (pp.195-202). Nauka, Moscow (in Russian).Levina, T.P. and Nikitin, V.P., 1973. Paleobotanical characteristics of Holocene peat in the Karginskii Cape region of the Yenisei River. In: The Pleistocene of Siberia and bordering oblasts ed. by V.N. Saks (pp.80-85). Nauka, Moscow (in Russian).
KARGOPOL Neotoma14051442Kargopolovo Exposure83.00000055.000000Asia75RawRiver16AWI0.0777.233Exposure in floodplain terrace. Physiography: river valley. Surrounding vegetation: Poaceae-Cyperaceae.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Arkhipov, S.A. and Votakh, M.R., 1973. History of the vegetation during the middle and late Wurm and the Holocene in the upper Ob valley. In: The Pleistocene of Siberia and neighboring regions ed. by V.N. Saks (pp.130-143). Nauka, Moscow (in Russian).
KAYAKSK Neotoma14071444Kayakskoye Zaimitschye81.00000055.000000Asia150RawPeat31AWI0.6047.220Peat from exposure. Physiography: lower river valley. Surrounding vegetation: Betula-Pinus forest.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Levina, T.P., Orlova, L.A., Panychev, V.A. and Ponomareva, E.A., 1987. Radiochronometry and pollen stratigraphy of Holocene peat of Kayakskoye Zaimitschye (Barabinskaya forest-steppe). In: Regional Geochronology of Siberia and Far East ed. by I.V. Nikolayeva (pp.136-143). Nauka, Novosibirsk (in Russian).
Khlebnikova_Stream Neotoma14761513Khlebnikov Stream Exposure 5858145.48820043.733860Asia3RawCoast14AWI0.3745.478Exposure in lagoon terrace. Physiography: coastal plain. Surrounding vegetation: boggy meadow. Surrounding vegetation: Quercus crispula, Acer, Phellodendron amurense, Juglans, Betula, Aralia, Acer, Picea microsperma, Abies mayriana, Abies sachalinensis.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Korotky, A.M., Razzhigaeva, N.G., Mokhova, L.M., Ganzey, L.A., Grebennikova, T.A. and Bazarova, V.B., 1996. Coastal dunes as an indicator of period of global climatic deterioration (Kunashir Island, Kuriles). Geology of the Pacific Ocean, 13, pp.73-84.Korotky, A.M., Razjigaeva, N.G., Grebennikova, T.A., Ganzey, L.A., Mokhova, L.M., Bazarova, V.B. and Sulerzhitsky, L.D., 1995. Holocene marine terraces of Kunashir Island. The Quaternary Research (Daiyonki-Kenkyu), 34(5), pp.359-375 (in Japanese).doi:10.4116/jaqua.34.5_359Korotky, A.M., Razjigaeva, N.G., Grebennikova, T.A., Ganzey, L.A., Mokhova, L.M., Bazarova, V.B., Sulerzhitsky, L.D. and Lutaenko, K.A., 2000. Middle-and late-Holocene environments and vegetation history of Kunashir Island, Kurile Islands, northwestern Pacific. The Holocene, 10(3), pp.311-331.doi:10.1191/095968300667552216
KHOMUR Neotoma14781515Bol'shoi Khomus-Yuryakh River153.75000070.125000Asia25RawPeat2AWI9.5539.979Buried peat and alluvium, yedoma section. Physiography: yedoma-alas relief. Surrounding vegetation: Betula-Salix shrub tundra.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Kaplina, T.N. and Lozhkin, A.V., 1982. The history of vegetation of the Primorskikh lowland of Yakutia in the Holocene. In: Evolution of the environment of the territory of the USSR during the late Pleistocene and Holocene ed. by A.A. Velichko, I.I. Spasskaya, and N.A. Khotinskiy (pp.2017-220). Nauka, Moscow (in Russian).
KOLYMA Neotoma15041542Berelyekh River147.75000063.283333Asia800RawRiver20AWI0.93121.708Peat and alluvium,glacio-fluvial terrace. Physiography: river valley in mountains. Surrounding vegetation: Larix dahurica forest.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Lozhkin, A.V. and Postolenko, G.A., 1989. New data about the environmental evolution of the mountain region of the Kolyma region during the late Anthropogene. Doklady Akademii Nauk, 307(5), pp.1184-1188 (in Russian).
CHESNOKNeotoma15051543Komaritsa Peat Exposure69.00000057.500000Asia42RawPeat28AWI0.10310.553Buried peat exposed in river terrace. Physiography: river valley. Surrounding vegetation: Pinus-Picea-Abies.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Khotinskiy, N.A., 1977. Holocene of northern Eurasia. Nauka, Moscow (in Russian).Neishtadt, M.I., 1967. About the absolute age of bogs of western Siberia. Revue Roumaine de Biologic Ser Botanique, 12, pp.1981-1986.Volkov, I.A., Gurtovaya, E.E. and Firsov, L.V., 1973. The structure, age and history of Holocene peat near Gorno-Slinkino village on the Irtysh River. In: The Pleistocene of Siberia and neighboring regions ed. by V.N. Saks (pp.55-68). Nauka, Moscow (in Russian).Volkova, V.S., 1966. The Quaternary deposits of the lower Irtysh River and their biostratigraphic characteristics. Nauka, Novosibirsk (in Russian).
Kosmodemyanskaya-1 Neotoma15071545Gulf of Kosmodem'yanskaya-1 Exposure 5706145.94106044.151410Asia6RawCoast10AWI0.9806.671The 6-m-thick exposure was found on low marine terrace near the mouth of Prozrachnyii Stream, which empties into Golovin Gulf. Physiography: marine terrace. Surrounding vegetation: Picea-Abies taiga with Picea microsperma, Abies mayriana, A. sachalinensis, Quercus crispula, Acer, Phellodendron amurense, Juglans, Betula, Aralia.Korotky, A.M., Razjigaeva, N.G., Grebennikova, T.A., Mokhova, L.M., Ganzey, L.A., Pushkar, V.S. and Bazarova, V.B., 1994. 3/4 mu mu mu mu mu 3/43/4 3/41/4 3/43/4 1/4 mu 3/4 mu 1/4 mu [Marine terraces and coastal evolution of Kunashir Island during the Pleistocene]. Special Publication 3033-94. All Union Institute Science and Technical Information, Vladivostok, Russia (in Russian).Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Korotky, A.M., Razzhigaeva, N.G., Mokhova, L.M., Ganzey, L.A., Grebennikova, T.A. and Bazarova, V.B., 1996. Coastal dunes as an indicator of period of global climatic deterioration (Kunashir Island, Kuriles). Geology of the Pacific Ocean, 13, pp.73-84.Korotky, A.M., Razjigaeva, N.G., Grebennikova, T.A., Ganzey, L.A., Mokhova, L.M., Bazarova, V.B. and Sulerzhitsky, L.D., 1995. Holocene marine terraces of Kunashir Island. The Quaternary Research (Daiyonki-Kenkyu), 34(5), pp.359-375 (in Japanese).doi:10.4116/jaqua.34.5_359Korotky, A.M., Razjigaeva, N.G., Grebennikova, T.A., Ganzey, L.A., Mokhova, L.M., Bazarova, V.B., Sulerzhitsky, L.D. and Lutaenko, K.A., 2000. Middle-and late-Holocene environments and vegetation history of Kunashir Island, Kurile Islands, northwestern Pacific. The Holocene, 10(3), pp.311-331.doi:10.1191/095968300667552216
Kosmodemyanskaya-2 Neotoma15081546Gulf of Kosmodem'yanskaya-2 Exposure 5705145.94102044.151360Asia6RawCoast12AWI0.2616.811Exposure occurs in the lowest (6 m high) marine t at the mouth of Prozrachnyii Stream. Physiography: river mouth on sea coast. Surrounding vegetation: Picea-Abies taiga with Quercus crispula, Acer, Phellodendron amurense, Juglans, Betula, Aralia, Picea microsperma, Abies mayriana, A. sachalinensis.Korotky, A.M., Razjigaeva, N.G., Grebennikova, T.A., Mokhova, L.M., Ganzey, L.A., Pushkar, V.S. and Bazarova, V.B., 1994. 3/4 mu mu mu mu mu 3/43/4 3/41/4 3/43/4 1/4 mu 3/4 mu 1/4 mu [Marine terraces and coastal evolution of Kunashir Island during the Pleistocene]. Special Publication 3033-94. All Union Institute Science and Technical Information, Vladivostok, Russia (in Russian).Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Korotky, A.M., Razzhigaeva, N.G., Mokhova, L.M., Ganzey, L.A., Grebennikova, T.A. and Bazarova, V.B., 1996. Coastal dunes as an indicator of period of global climatic deterioration (Kunashir Island, Kuriles). Geology of the Pacific Ocean, 13, pp.73-84.Korotky, A.M., Razjigaeva, N.G., Grebennikova, T.A., Ganzey, L.A., Mokhova, L.M., Bazarova, V.B. and Sulerzhitsky, L.D., 1995. Holocene marine terraces of Kunashir Island. The Quaternary Research (Daiyonki-Kenkyu), 34(5), pp.359-375 (in Japanese).doi:10.4116/jaqua.34.5_359Korotky, A.M., Razjigaeva, N.G., Grebennikova, T.A., Ganzey, L.A., Mokhova, L.M., Bazarova, V.B., Sulerzhitsky, L.D. and Lutaenko, K.A., 2000. Middle-and late-Holocene environments and vegetation history of Kunashir Island, Kurile Islands, northwestern Pacific. The Holocene, 10(3), pp.311-331.doi:10.1191/095968300667552216
Kosmodemyanskaya-3 Neotoma15091547Gulf of Kosmodem'yanskaya-3 Exposure 5815145.93986044.152200Asia6RawCoast14AWI4.7627.368The 3.1-m-thick Kosmodem'yanskaya-3 exposure is located in 5-to-6-m-high marine terrace near tlie mouth of Prozrachnyii Stream. Physiography: coastal plain. Surrounding vegetation: Picea-Abies taiga. Surrounding vegetation: Picea-Abies taiga with Quercus crispula, Acer, Phellodendron amurense, Juglans, Betula, Aralia, Picea microsperma, Abies mayriana, A. sachalinensis.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Korotky, A.M., Razzhigaeva, N.G., Mokhova, L.M., Ganzey, L.A., Grebennikova, T.A. and Bazarova, V.B., 1996. Coastal dunes as an indicator of period of global climatic deterioration (Kunashir Island, Kuriles). Geology of the Pacific Ocean, 13, pp.73-84.Korotky, A.M., Razjigaeva, N.G., Grebennikova, T.A., Ganzey, L.A., Mokhova, L.M., Bazarova, V.B. and Sulerzhitsky, L.D., 1995. Holocene marine terraces of Kunashir Island. The Quaternary Research (Daiyonki-Kenkyu), 34(5), pp.359-375 (in Japanese).doi:10.4116/jaqua.34.5_359Korotky, A.M., Razjigaeva, N.G., Grebennikova, T.A., Ganzey, L.A., Mokhova, L.M., Bazarova, V.B., Sulerzhitsky, L.D. and Lutaenko, K.A., 2000. Middle-and late-Holocene environments and vegetation history of Kunashir Island, Kurile Islands, northwestern Pacific. The Holocene, 10(3), pp.311-331.doi:10.1191/095968300667552216
KOTYRKOL Neotoma15111549Kotyrkol' Peat Bog70.38044052.962220Asia439RawPeat22AWI-0.0683.919Betula/Populus/Carex swamp.Tarasov, P.E., 1992. Holocene palaeogeography of the steppe zone of northern and central Kazakhstan. Doctoral dissertation. Moscow State University, Moscow, Russia (in Russian).Tarasov, P.E., 1991. The features of the late Holocene for the Kokchetav Highland. Vestnik Moskovskogo Universiteta, Ser. 5, Geography, 6, pp.54-60 (in Russian).Tarasov, P.E. and Kremenetskii, K.V., 1995. Geochronology and stratigraphy of the Holocene lacustrine-bog deposits in northern and central Kazakhstan. Stratigraphy and Geological Correlation, 3(1), pp.73-80.
KREST Neotoma15131551Kresta Gulf Exposure-179.00000066.000000Asia5RawPeat10AWI2.84510.083Coastal exposure of peat and sand. Physiography: coastal lowland. Surrounding vegetation: Cyperaceae tundra.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Ivanov, V.F., 1986. Quaternary deposits of the coast of eastern Chukotka. North East Interdisciplinary Research Institute, Far East Branch, USSR Academy of Sciences, Vladivostok (in Russian).
KUBAGA Neotoma15151553Bol'shaya Kuobakh-Baga River, Terrace Site143.37500064.983333Asia500RawRiver11AWI1.2526.837Exposure along river terrace. Physiography: river valley in mountains. Surrounding vegetation: Larix-Populus-Chosenia forest.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.
KURO11 Neotoma15211559East Siberian Sea Coast 11156.25000071.066667Asia8RawRiver9AWI4.2999.57310-m-high alas exposure. Physiography: yedoma-alas relief. Surrounding vegetation: Salix-graminoid tundra.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Lozhkin, A.V., Prokhorova, T.P. and Parii, V.P., 2014. Radiocarbon dates and palynological characteristics of sediments of the alas complex of the Kolyma Lowland. Doklady Akademii Nauk, 224(6), 1395-1398 (in Russian).
KUROP7 Neotoma15241562Bol'shaya Kuropatoch'ya River (KUROP7)156.75000070.666667Asia7RawRiver7AWI0.3437.277Silt and peat exposed in river cutbank. Physiography: coastal lowland. Surrounding vegetation: Betula-Salix-herb tundra.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.
KURPEAT Neotoma15251563Bol'shaya Kuropatoch'ya River (KURPEAT)156.37500069.966667Asia47RawPeat10AWI7.10812.602Exposed buried peat in alas sediments. Physiography: yedoma-alas relief. Surrounding vegetation: Betula-Salix-graminoid tundra.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Lozhkin, A.V. and Vazhenina., L.N., 1987. The characteristics of vegetational development from the Kolyma lowland in the early Holocene. In: Quaternary period of northeast Asia ed. by V.P. Pokhialainen (pp.135-144). North East Interdisciplinary Research Institute, Far East Branch, USSR Academy of Sciences, Magadan (in Russian).
Kyurbe-Yuryakh-2 Neotoma15281566Kyurbe-Yuryakh-2138.61666768.598611Asia650RawRiver4AWI2.6999.346Exposure in river terrace. Physiography: river valley. Surrounding vegetation: open Larix forest.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.
LEDOBOZ Neotoma15771623Ledovyi Obryu Exposure, Southern Section171.18333364.100000Asia44RawLake9AWI9.99720.081Lake sediments in yedoma exposure. Physiography: mountain valley. Surrounding vegetation: Larix forest-tundra.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Dort-Gol'ts, Y.E., 1982. Characteristic form of late Pleistocene yedoma complex in southeastern Chukotka. In: Frozen geological processes and paleography of the lowlands of northeast Asia (pp.75-81). Magadan Publishing House, Magadan (in Russian).Kaplin, P.A., 1980. Recent deposits and Pleistocene paleogeography of Chukotka. Nauka, Moscow (in Russian).Kotov, A.N., Lozhkin, A.V. and Ryabchun, V.K., 1989. Glacial facies and conditions of sediment forms for upper Quaternary sediments of the Main River valley, Chukotka. In: Form relief and sediment correlation and precious metals of north east USSR ed. by V.F. Ivanov and B.F. Palymskii (pp.117-131). North East Interdisciplinary Research Institute, Far East Branch, USSR Academy of Sciences, Magadan (in Russian).Kotov, A.N. and Ryabchun, V.K., 1986. Cryogenic complex of late Pleistocene deposits of the Main River Valley. In: Ust'-Algan mammoth exposures ed. by A.V. Lozhkin. North East Interdisciplinary Research Institute, Far East Branch, USSR Academy of Sciences, Magadan (in Russian).Lozhkin, A.V., Kotov, A.N. and Ryabchun, V.K., 2000. Palynological and radiocarbon data of the Ledovyi Obryv exposure (the south east of Chukotka). In: The Quaternary Period of Beringia ed .by K.V. Simakov (pp.118-131). North East Interdisciplinary Research Institute, Far East Branch, Russian Academy of Sciences, Magadan (in Russian).
Lesnaya_River Neotoma15801627Lesnaya River Exposure145.75000044.000000Asia6RawPeat25AWI0.3867.457Exposure of lake and lagoon deposits. Physiography: lower river valley. Surrounding vegetation: Picea-Abies-Quercus forest.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Korotky, A.M., Razzhigaeva, N.G., Mokhova, L.M., Ganzey, L.A., Grebennikova, T.A. and Bazarova, V.B., 1996. Coastal dunes as an indicator of period of global climatic deterioration (Kunashir Island, Kuriles). Geology of the Pacific Ocean, 13, pp.73-84.Korotky, A.M., Razjigaeva, N.G., Grebennikova, T.A., Ganzey, L.A., Mokhova, L.M., Bazarova, V.B. and Sulerzhitsky, L.D., 1998. Holocene marine terraces of Kunashir Island, Kuril Islands. The Quaternary Research (Daiyonki-Kenkyu) 34(5), pp.359-375 (in Japanese).doi:10.4116/jaqua.34.5_359
Lesnoye_Lake Neotoma15811628Lesnoye Lake151.86666759.583333Asia95RawLake39AWI-0.05719.464Lake in tectonic depression. Physiography: coastal tectonic depression. Surrounding vegetation: Larix dahurica muskeg.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Anderson, P.M., Belaya, B.V., Glushkova, O.Y. and Lozhkin, A.V., 1997. New data about the vegetation history of northern Priokhot'ye during the Late Pleistocene and Holocene. In: Late Pleistocene and Holocene of Beringia ed. by M.K. Gagiev (pp.33-54). North East Interdisciplinary Research Institute, Far East Branch, Russian Academy of Sciences, Magadan (in Russian).
Lorino Neotoma16121664Lorino Exposure-171.70000065.500000Asia12RawPeat16AWI4.17722.365Exposure of peat and alluvium. Physiography: coastal lowland. Surrounding vegetation: graminoid-Salix-Betula tundra.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Ivanov, V.F., 1986. Quaternary deposits of the coast of eastern Chukotka. North East Interdisciplinary Research Institute, Far East Branch, USSR Academy of Sciences, Vladivostok (in Russian).
LUKA Neotoma16261680Lukaschin Yar Peat Exposure78.50000061.000000Asia65RawPeat25AWI0.40611.541Peat exposure in river terrace. Physiography: river valley. Surrounding vegetation: Pinus-Picea-Abies taiga.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Neishtadt, M.I., 1976. Holocene processes in western Siberia and associated problems. In: Studying and mastering the environment ed. by M.I. Neishtadt (pp.90-99). USSR Academy of Sciences, Institute of Geography, Moscow (in Russian).
MADJAGA Neotoma16321687Lake Madjagara120.96666764.833333Asia160RawLake66AWI0.1907.183Thermokarst lake. Physiography: early Pleistocene terrace with sands. Surrounding vegetation: larch forest.Tarasov, P.E., Harrison, S.P., Saarse, L., Pushenko, M.Y., Andreev, A.A., Aleshinskaya, Z.V., Davydova, N.N., Dorofeyuk, N.I., Efremov, Y.V., Khomutova, V.I., Sevastyanov, D.V., Tamosaitis, J., Uspenskaya, O.N., Yakushko, O.F. and Tarasova, I.V., 1994. Lake status records from the former Soviet Union and Mongolia: data base documentation. Paleoclimatology Publications Series 2, World Data Center-A for Paleoclimatology, NOAA Paleoclimatology Program, Boulder, Colorado, USA.Andreev, A.A. and Klimanov, V.A., 1989. Vegetation and climate history of central Yakutia during the Holocene and Late Pleistocene. In: Formirovanie rel'efa, korelyatnykh otlozheny i rossypei Severo-Vostoka SSSR [Formation of deposits and placers on northeast of the USSR] ed. by B.F. Ivanov and B.F. Palymsky (pp.28-51). Publishing House of SVKNII, Magadan, Russia (in Russian).
MAIN Neotoma16331688Ledovyi Obryv Exposure, Northern Section171.18333364.100000Asia57RawValley21AWI21.89846.158Physiography: mountain valley. Surrounding vegetation: open Larix forest.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Kind, N.V., 1974. Geochronology of the late Anthropogene by isotopic data. Nauka, Moscow (in Russian).Kotov, A.N., Lozhkin, A.V. and Ryabchun, V.K., 1989. Glacial facies and conditions of sediment forms for upper Quaternary sediments of the Main River valley, Chukotka. In: Form relief and sediment correlation and precious metals of north east USSR ed. by V.F. Ivanov and B.F. Palymskii (pp.117-131). North East Interdisciplinary Research Institute, Far East Branch, USSR Academy of Sciences, Magadan (in Russian).Kotov, A.N. and Ryabchun, V.K., 1986. Cryogenic complex of late Pleistocene deposits of the Main River Valley. In: Ust'-Algan mammoth exposures ed. by A.V. Lozhkin. North East Interdisciplinary Research Institute, Far East Branch, USSR Academy of Sciences, Magadan (in Russian).Lozhkin, A.V., Kotov, A.N. and Ryabchun, V.K., 2000. Palynological and radiocarbon data of the Ledovyi Obryv exposure (the south east of Chukotka). In: The Quaternary Period of Beringia ed. by K.V. Simakov (pp.118-131). North East Interdisciplinary Research Institute, Far East Branch, Russian Academy of Sciences, Magadan (in Russian).
MALTAN Neotoma16401695Maltan River Exposure151.61666760.883333Asia735RawRiver22AWI1.01212.026Exposure along river terrace. Physiography: river valley in mountains. Surrounding vegetation: Larix dahurica forest.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Lozhkin, A.V. and Glushkova, O.Y., 1997. Boreal peats in the upper Kolyma basin. In: Late Pleistocene and Holocene of Beringia ed. by M.K. Gagiev (pp.55-62). North East Interdisciplinary Research Institute, Far East Branch, Russian Academy of Sciences, Magadan (in Russian).Vazhenina, L.N., 1997. Early Holocene seed flora from peat, Maltan River, upper Kolyma. In: Late Pleistocene and Holocene of Beringia ed. by M.K. Gagiev (pp.63-69). North East Interdisciplinary Research Institute, Far East Branch, Russian Academy of Sciences, Magadan (in Russian).
MAMENM Neotoma16411696Enmynveem River (mammoth site)165.93333368.166667Asia400RawPeat11AWI9.20737.202Peat and colluvium exposed during mining. Physiography: river valley in mountains. Surrounding vegetation: open Larix dahurica forest.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Lozhkin, A.V., Pavlov, G.F., Ryabchun, V.K., Gorbachev, A.L., Zadal'skii, S.V. and Shubert, E.E., 1988. A new mammoth discovery in Chukotka. Doklady Akademii Nauk, 302(6), pp.1440-1444 (in Russian).
Mereya_River Neotoma16801736Mereya River, Lagoon Terrace Exposure S4000(30)142.91666746.616667Asia4RawMarine28AWI0.90817.389Marine terrace capped by peat. Physiography: coastal plain. Surrounding vegetation: Picea-Abies forest.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.
Nizmennyii_Cape Neotoma17511809Cape Nizmennyii Exposure C3352142.01666749.166667Asia5RawMarine9AWI0.3718.786Exposure of lake, lagoon, beach deposits. Physiography: dissected coastal plain. Surrounding vegetation: Picea-Abies forest.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Korotky, A., Grebennikova, T., Razjigaeva, N., Volkov, V., Mokhova, L., Ganzey, L. and Bazarova, V., 1997. Marine terraces of western Sakhalin Island. Catena, 30(1), pp.61-81.doi:10.1016/S0341-8162(97)00002-7Korotkiy, A.M., Pushkar, V.S., Grebennikova, T.A., Razzhigaeva, N.G., Karaulova, L.P., Mokhova, L.M., Ganzey, L.A., Cherepanova, M.N., Bazarova, V.B., Volkov, V.G. and Kovalyukhand, N.N., 1997. Marine terraces and Quaternary history of the Sakhalin Shelf. Dal'nauka, Vladivostok (in Russian).
NIZVAR Neotoma17521810Nizhnevartovskoye Exposure77.00000061.250000Asia55RawPeat33AWI0.11712.594Peat overlying 1st river terrace. Physiography: river valley. Surrounding vegetation: Picea, Abies, Pinus.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Firsov, L.V., Panychev, V.A. and Orlova, L.A., 1985. Catalog of radiocarbon dates. Novosibirsk Geological Institute, Siberian Branch, USSR Academy of Sciences, Novosibirsk (in Russian).Il'ina, N.S., Lapshina, E.I. and Lavrenko, N.I., 1985. The vegetation cover of the western Siberia continental plateau. Nauka, Siberia Branch, Novosibirsk (in Russian).Neishtadt, M.I., 1976. Holocene processes in western Siberia and associated problems. In: Studying and mastering the environment ed. by M.I. Neishtadt (pp.90-99). USSR Academy of Sciences, Institute of Geography, Moscow (in Russian).
ONEMEN Neotoma17731832Northern Coast of Onemen Gulf176.16666764.783333Asia18RawRiver16AWI31.56344.112Exposure in river bank. Physiography: lower river valley in coastal region. Surrounding vegetation: shrub tundra.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Korotky, A.M., 1991. Cryolithological charcteristics of ice complex near the mouth of the Anadyr River. In: Interdisciplinary cryolithological investigations of Chukotka (pp.5-18). North East Interdisciplinary Research Institute, Far East Branch, Russian Academy of Sciences, Magadan (in Russian).Korotky, A.M. and Brazhnik, S.N., 1991. Underground ice and cryomorphogenesis. Guide book of science excursion to Onemen Gulf, Cape Rogozhnyi Exposure: Preprint. North East Interdisciplinary Research Institute, Far East Branch, Russian Academy of Sciences, Magadan (in Russian).Korotky, A.M., Trumpe, M.A., Polujan, A.I., Kotova, L.N. and Takmazyan, E.D., 1985. Radiocarbon dates for upper Quaternary sequences in northeastern Asia and Alaska. In: History of climate and vegetation in Beringia during the late Cenozoic ed. by Yu.M. Bychkov and A.V. Lozhkin (pp.169-184). North East Interdisciplinary Research Institute, Far East Branch, Russian Academy of Sciences, Magadan (in Russian).
Opasnaya_River Neotoma17771836Headwaters Opasnaya River138.48333348.233333Asia1320RawPeat18AWI5.66061.455Raised peat. Physiography: oligotrophic peatland with frost mounds. Surrounding vegetation: sparse Picea forest and mountain tundra.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Korotky, A.M., Pletnev, S.P., Pushkar, V.S., Grebennikova, T.A., Razzhigaeva, N.G., Sakhebgareeva, E.D. and Mokhova, L.M. 1988. Evolution environment of south Far East (late Pleistocene and Holocene). Nauka, Moscow (in Russian).
OPASMS Neotoma17781837Headwaters Opasnaya River (mine shaft)138.48333348.233333Asia1320RawRiver13AWI4.6527.595Section exposed in mine shaft. Physiography: upper portion of river valley. Surrounding vegetation: mixed mountain tundra and Picea forest.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Korotky, A.M., 1982. Paleographic conditions of the formation of Quaternary peats (south of Far East). In: Modern sedimentation and morpholithogenesis of the Far East ed. by S.P. Pletnev and V.S. Pushkar (pp.58-71). Far Eastern Science Center, USSR Academy of Sciences, Vladivostok (in Russian).Korotky, A.M., Mokhova, L.M. and Pushkar, V.S., 1985. The climate changes of the Holocene and landscape evolution of bald mountains of central Yam-Alin'. In: Paleogeographic investigations in the Far East ed. by A.M. Korotky and V.S. Pushkar (pp.5-22). Far Eastern Science Center of the USSR Academy of Sciences, Vladivostok (in Russian).Korotky, A.M., Pletnev, S.P., Pushkar, V.S., Grebennikova, T.A., Razzhigaeva, N.G., Sakhebgareeva, E.D. and Mokhova, L.M. 1988. Evolution environment of south Far East (late Pleistocene and Holocene). Nauka, Moscow (in Russian).
Oumi Neotoma17831842Oumi Exposure138.40000048.216667Asia990RawPeat29AWI0.2772.786Lake formed by naturally dammed river. Physiography: river valley. Surrounding vegetation: bog with Larix.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.
OVRA1 Neotoma17841843Ovrazhnyii-1 Stream Exposure134.56666743.250000Asia8RawRiver36AWI0.20345.547Exposure in river terrace. Physiography: coastal zone bordering gulf. Surrounding vegetation: Quercus mongolica-Betula forest.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Korotky, A.M. and Karaulova, L.P., 1975. New data about the stratigraphy of Quaternary deposits of Primor'ye. In: Questions of geomorphology and Quaternary geology of the southern Far East ed. by A.M. Korotky and A.P. Kulakov (pp.79-110). Far Eastern Branch, USSR Academy of Sciences, Vladivostok (in Russian).Korotky, A.M., Karaulova, L.P. and Troitskaya, T.S., 1980. The Quaternary deposits of Primor'ye. Nauka, Novosibirsk (in Russian).Korotky, A.M., Kovalyukh, N.N. and Volkov, V.G., 1989. Radiocarbon dating of Quaternary deposits (south Far East). Preprint. Far East Branch of the USSR Academy of Sciences, Vladivostok (in Russian).Shilo, N.A., 1987. Resolution: Interagency Stratigraphic meeting of Quaternary system of eastern USSR. North East Interdisciplinary Research Institute, Far East Branch, USSR Academy of Sciences, Magadan (in Russian).
Ovrazhnyii_Stream-2 Neotoma17851844Ovrazhnyii-2 Exposure 667-842134.56666743.250000Asia10RawLake16AWI0.82235.984Exposure of lake and bog sediments. Physiography: sea coast. Surrounding vegetation: Larix-Alnus-Betula forest with bogs.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Korotky, A.M. and Karaulova, L.P., 1975. New data about the stratigraphy of Quaternary deposits of Primor'ye. In: Questions of geomorphology and Quaternary geology of the southern Far East ed. by A.M. Korotky and A.P. Kulakov (pp.79-110). Far Eastern Branch, USSR Academy of Sciences, Vladivostok (in Russian).Pushkar, V.S., 1979. Biostratigraphy of sediments of the late Anthropogene of the southern Far East. Nauka, Moscow (in Russian).
OZERKI Neotoma17861845Ozerki80.46666750.416667Asia227RawRiver48AWI-0.04215.294Swamp. Physiography: Irtish River valley. Surrounding vegetation: birch-poplar forests and cultivated fields.Tarasov, P.E., Harrison, S.P., Saarse, L., Pushenko, M.Y., Andreev, A.A., Aleshinskaya, Z.V., Davydova, N.N., Dorofeyuk, N.I., Efremov, Y.V., Khomutova, V.I., Sevastyanov, D.V., Tamosaitis, J., Uspenskaya, O.N., Yakushko, O.F. and Tarasova, I.V., 1994. Lake status records from the former Soviet Union and Mongolia: data base documentation. Paleoclimatology Publications Series 2, World Data Center-A for Paleoclimatology, NOAA Paleoclimatology Program, Boulder, Colorado, USA.Kremenetsky, C.V., Tarasov, P.E. and Cherkinsky, A.E., 1994. Istoriya ostrovnykh borov Kazakhstana v golotsene [Holocene history of the Kazakhstan \island\ pine forests]. Botanicheskiy Zhurnal, 79(3), pp.13-29 (in Russian).Kremenetski, C.V., Tarasov, P.E. and Cherkinsky, A.E., 1997. Postglacial development of Kazakhstan pine forests. Geographie physique et Quaternaire, 51(3), pp.391-404.doi:10.7202/033138arTarasov, P.E. and Kremenetskii, C.V., 1995. Geochronology and stratigraphy of the Holocene lacustrine-bog deposits in northern and central Kazakhstan. Stratigraphy and Geological Correlation, 3(1), pp.73-80.
Paramonovskii_Stream Neotoma17911850Paramonovskii Stream Exposure 4980133.75000043.200000Asia120RawRiver7AWI0.69242.075River terrace. Physiography: river valley. Surrounding vegetation: broadleaf-Pinus koraiensis forest.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Korotky, A.M., Karaulova, L.P. and Troitskaya, T.S., 1980. The Quaternary deposits of Primor'ye. Nauka, Novosibirsk (in Russian).Korotky, A.M., Volkov, V.G., Bazarova, V.B. and Kovalyukh, N.N., 1993. The catalog of radiocarbon dates of Quaternary deposits of the Far East. Far Eastern Branch, Russian Academy of Sciences, Vladivostok (in Russian).Shilo, N.A., 1987. Resolution: Interagency Stratigraphic meeting of Quaternary system of eastern USSR. North East Interdisciplinary Research Institute, Far East Branch, USSR Academy of Sciences, Magadan (in Russian).
PASHENN Neotoma17981860Pashennoe75.39858049.367710Asia871RawLake34AWI-0.04913.295Tectonic basin, lake with floating bogs. Physiography: Karkaralinsk Mtns, granite hills, 1000 m. Surrounding vegetation: Betula, Pinus, steppe.Tarasov, P.E., Harrison, S.P., Saarse, L., Pushenko, M.Y., Andreev, A.A., Aleshinskaya, Z.V., Davydova, N.N., Dorofeyuk, N.I., Efremov, Y.V., Khomutova, V.I., Sevastyanov, D.V., Tamosaitis, J., Uspenskaya, O.N., Yakushko, O.F. and Tarasova, I.V., 1994. Lake status records from the former Soviet Union and Mongolia: data base documentation. Paleoclimatology Publications Series 2, World Data Center-A for Paleoclimatology, NOAA Paleoclimatology Program, Boulder, Colorado, USA.Kremenetsky, C.V., Tarasov, P.E. and Cherkinsky, A.E., 1994. Istoriya ostrovnykh borov Kazakhstana v golotsene [Holocene history of the Kazakhstan \island\ pine forests]. Botanicheskiy Zhurnal, 79(3), pp.13-29 (in Russian).Tarasov, P.E. and Kremenetskii, K.V., 1995. Geochronology and stratigraphy of the Holocene lacustrine-bog deposits in northern and central Kazakhstan. Stratigraphy and Geological Correlation, 3(1), pp.73-80.
PAVLOVKA Neotoma18051867Pavlovka Exposure 988134.00000044.316667Asia300RawFluvial16AWI1.83247.908Exposure in fluvial terrace. Physiography: river valley in mountains. Surrounding vegetation: valley coniferous-broadleafed forest.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Korotky, A.M., Karaulova, L.P. and Troitskaya, T.S., 1980. The Quaternary deposits of Primor'ye. Nauka, Novosibirsk (in Russian).
PENZHIN Neotoma18211885Penzhinskaya Gulf165.41666762.416667Asia32RawPeat11AWI2.6899.168Buried peat exposed in coastal bluff. Physiography: coastal. Surrounding vegetation: Betula-Alnus shrub tundra.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Ivanov, V.F., Lozhkin, A.V., Kal'nichenko, S.S., Kyshtymov, A.I., Narkhinova, V.E. and Terekhova, V.E., 1984. The late Pleistocene and Holocene of Chukchi Peninsula to the north of Kamchatka. In: Geology and useful minerals of northeast Asia ed. by V.I. Goncharov (pp.33-42). Far East Branch, USSR Academy of Sciences, Vladivostok (in Russian).
PEPELNOY Neotoma18221886Pepel'noye Lake150.61666759.850000Asia115RawLake24AWI-0.0174.398Lake. Physiography: tectonic depression. Surrounding vegetation: Larix dahurica forest.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Lozhkin, A.V., Anderson, P.M., Belaya, B.V., Glushkova, O.Y., Kotova, L.N. and Trumpe, M.A., 2000. Palynological characteristics and radiocarbon dates from late Holocene lacustrine sediments of northern Priokhot'ye. In: The Quaternary period of Beringia ed. by K.V. Simakov (pp.76-87). North East Interdisciplinary Research Institute, Far East Branch, Russian Academy of Sciences, Magadan (in Russian).
PESCHANK Neotoma18251889Peschanka Exposure 155132.11666743.300000Asia12RawRiver17AWI10.40642.103River terrace. Physiography: river valley. Surrounding vegetation: Quercus-Abies holophylla-Carpinus forest.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.
PODKOVA Neotoma18951959Podkova Lake152.10000059.950000Asia660RawLake28AWI-0.0196.214Kettle lake. Physiography: recessional moraine complex, mt. valley. Surrounding vegetation: Larix dahurica forest.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Anderson, P.M., Lozhkin, A.V., Belaya, B.V. and Stetsenko, T.V., 2000. New data about the development of vegetation in northern Priokhot'ye during the second part of the Holocene. In: The Quaternary period of Beringia ed. by K.V. Simakov (pp.88-98). North East Interdisciplinary Research Institute, Far East Branch, Russian Academy of Sciences, Magadan (in Russian).Anderson, P.M., Belaya, B.V., Glushkova, O.Y. and Lozhkin, A.V., 1997. New data about the vegetation history of northern Priokhot'ye during the Late Pleistocene and Holocene. In: Late Pleistocene and Holocene of Beringia ed. by M.K. Gagiev (pp.33-54). North East Interdisciplinary Research Institute, Far East Branch, Russian Academy of Sciences, Magadan (in Russian).
POSYET Neotoma19041969Pos'yet Bay130.80000042.633333Asia-19RawMarine29AWI0.2969.862Marine core on shallow shelf. Physiography: offshore shelf. Surrounding vegetation: none.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Korotky, A.M., 1982. Oscillations of sea levels of the Sea of Japan during the Quaternary period (northwestern shelf). In: Oscillation of sea levels ed. by P.A. Kaplin, R.K. Klige, and A.L. Chepalyga (pp.104-114). Moscow State University, Moscow (in Russian).Korotky, A.M. and Lobanova, L.A., 1984. Radiocarbon dating and paleographic boundaries of the late Pleistocene-Holocene. In: Paleogeograhic boundaries and methods for their study ed. by A.M. Korotky and V.S. Pushkar (pp.106-114). Far Eastern Science Center, USSR Academy of Sciences, Vladivostok (in Russian).Korotky, A.M., Pletnev, S.P., Pushkar, V.S., Grebennikova, T.A., Razzhigaeva, N.G., Sakhebgareeva, E.D. and Mokhova, L.M., 1988. Evolution environment of south Far East (late Pleistocene and Holocene). Nauka, Moscow (in Russian).
PRIYAT Neotoma19131979Priyatnoye Lake151.71666761.033333Asia980RawLake45AWI-0.05115.282NAAnderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Anderson, P.M., Lozhkin, A.V., Belaya, B.V., Stetsenko, T.V. and Simakov, K.V., 1998. New data about the stratigraphy of late Quaternary deposits of northern Priokhot'ye. In: Environmental changes in Beringia during the Quaternary ed. by Simakov, K.V. (pp.69-87). North East Interdisciplinary Research Institute, Far East Branch, Russian Academy of Sciences, Magadan (in Russian).Kind, N.V., 1974. Geochronology of the late Anthropogene by isotopic data. Nauka, Moscow (in Russian).Lozhkin, A.V., Anderson, P.M., Glushkova, O.Y., Solomatkina, T.B. and Federova, I.N., 2000. About features of development of lakes in the mountain regions of the upper Kolyma. In: The Quaternary Period of Beringia ed. by K.V. Simakov (pp.22-45). North East Interdisciplinary Research Institute, Far East Branch, USSR Academy of Sciences, Magadan (in Russian).
PURTAZ Neotoma19191986Pur-Taz Peatland79.73333366.700000Asia50RawPeat70AWI4.79310.429Peat bank along thermokarst lake. Physiography: extensive low-elevation peatlands. Surrounding vegetation: open Larix forest.Peteet, D.M., Andreev, A.A., Bardeen, W. and Mistretta, F., 1998. Long-term Arctic peatland dynamics, vegetation and climate history of the Pur-Taz region, western Siberia. Boreas, 27(2), pp.115-126.doi:10.1111/j.1502-3885.1998.tb00872.x
Rock_Island_Lake Neotoma21922268Rock Island Lake149.50000062.166667Asia870RawLake14AWI-0.0576.611Kettle in end moraine. Physiography: rolling hills in mountain valley. Surrounding vegetation: open larch forest.Lozhkin, A.V., Anderson, P.M., Eisner, W.R., Ravako, L.G., Hopkins, D.M., Brubaker, L.B., Colinvaux, P.A. and Miller, M.C., 1993. Late Quaternary lacustrine pollen records from southwestern Beringia. Quaternary Research, 39(3), pp.314-324.doi:10.1006/qres.1993.1038
RYAZANOV Neotoma22382317Ryazanovka Exposure131.36666742.833333Asia6RawRiver10AWI0.5616.056Exposure in alluvial-lagoon terrace. Physiography: lower river valley. Surrounding vegetation: Quercus-Carpinus-Abies-Pinus forest.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Korotky, A.M., Karaulova, L.P. and Troitskaya, T.S., 1980. The Quaternary deposits of Primor'ye. Nauka, Novosibirsk (in Russian).Shilo, N.A., 1987. Resolution: Interagency Stratigraphic meeting of Quaternary system of eastern USSR. North East Interdisciplinary Research Institute, Far East Branch, USSR Academy of Sciences, Magadan (in Russian).
SELEN1 Neotoma22762358Selennyakhskaya-1 Exposure137.82222269.240278Asia354RawRiver6AWI3.28113.260Exposure in river bank. Physiography: stream valley in tectonic depression. Surrounding vegetation: open Larix forest.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.
SELEN2 Neotoma22772359Selennyakhskaya-2 Exposure137.90000069.293056Asia360RawStream4AWI0.43618.321Exposure along stream bank. Physiography: stream valley in tectonic depression. Surrounding vegetation: open Larix forest.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.
SELEN4 Neotoma22792361Selennyakhskaya-4 Exposure138.05555669.113889Asia354RawRiver4AWI1.2989.807Exposure in river bank. Physiography: stream valley in tectonic depression. Surrounding vegetation: open Larix forest.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.
Selitkan-1 Neotoma22802362Selitkan-1 Exposure135.05000053.216667Asia1320RawPeat56AWI-0.0147.857Exposure on peat hillock. Physiography: river valley in mountains. Surrounding vegetation: shrub-herb mountain tundra.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Korotky, A.M. and Kovalyukh, N.N., 1987. Rhythms of perrenial permafrost: a reflection of climate changes during the late Pleistocene and Holocene. In: Paleogeographic investigations in the Far East ed. by A.M. Korotky and V.S. Pushkar (pp.20-36). Far Eastern Science Center of the USSR Academy of Sciences, Vladivostok (in Russian).Korotky, A.M., Mokhova, L.M. and Pushkar, V.S., 1985. The climate changes of the Holocene and landscape evolution of bald mountains of central Yam-Alin'. In: Paleogeographic investigations in the Far East ed. by Korotky, AM and Pushkar, VS (pp.5-22). Far Eastern Science Center of the USSR Academy of Sciences, Vladivostok (in Russian).Korotky, A.M., Mayuchaya, L.V. and Gvozdeva, I.G., 1985. Indicator species of broadleaf vegetation and the structure of subfossil complex in different climates of the south Far East. In: Ancient climates and vegetation in far eastern Asia ed. by A.M. Korotky and V.S. Pushkar (pp.4-15). Far Eastern Science Center of the USSR Academy of Sciences, Vladivostok (in Russian).Korotky, A.M., Kovalyukh, N.N. and Volkov, V.G., 1989. Radiocarbon dating of Quaternary deposits (south Far East). Preprint. Far East Branch of the USSR Academy of Sciences, Vladivostok (in Russian).Korotky, A.M., Pletnev, S.P., Pushkar, V.S., Grebennikova, T.A., Raszhigaeva, N.T., Sahebgareeva, E.D. and Mohova, L.M., 1988. Evolution environment of south Far East (late Pleistocene and Holocene). Nauka, Moscow (in Russian).
Selitkan-2 Neotoma22812363Selitkan-2 Exposure135.03333353.216667Asia1300RawPeat17AWI0.2706.608Exposure in boggy terrain in mountains. Physiography: upper river valley in mountains. Surrounding vegetation: shrub tundra.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Korotky, A.M., Pletnev, S.P., Pushkar, V.S., Grebennikova, T.A., Raszhigaeva, N.T., Sahebgareeva, E.D. and Mohova, L.M., 1988. Evolution environment of south Far East (late Pleistocene and Holocene). Nauka, Moscow (in Russian).Volkov, I.A. and Arkhipov, S.A., 1978. Quaternary deposits of the Novosibirsk Region. Joint Institute for Geology, Geophysics and Mineralogy, Siberia Branch, USSR Academy of Sciences, Novosibirsk (in Russian).
Selitkan-3 Neotoma22822364Selitkan-3 Exposure135.06666753.216667Asia1310RawRiver10AWI1.50811.282River terrace. Physiography: river valley in mountains. Surrounding vegetation: shrub tundra.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Korotky, A.M. and Kovalyukh, N.N., 1987. Rhythms of perrenial permafrost: a reflection of climate changes during the late Pleistocene and Holocene. In: Paleogeographic investigations in the Far East ed. by A.M. Korotky and V.S. Pushkar (pp.20-36). Far Eastern Science Center of the USSR Academy of Sciences, Vladivostok (in Russian).
Sergeevskii Neotoma22862368Sergeevskii Peat142.08333349.233333Asia6RawPeat57AWI1.6198.107Peat. Physiography: stream valley. Surrounding vegetation: Picea-Abies forest.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Korotky, A., Grebennikova, T., Razjigaeva, N., Volkov, V., Mokhova, L., Ganzey, L. and Bazarova, V., 1997. Marine terraces of western Sakhalin Island. Catena, 30(1), pp.61-81.doi:10.1016/S0341-8162(97)00002-7Korotkiy, A.M., Pushkar, V.S., Grebennikova, T.A., Razzhigaeva, N.G., Karaulova, L.P., Mokhova, L.M., Ganzey, L.A., Cherepanova, M.N., Bazarova, V.B., Volkov, V.G. and Kovalyukh, N.N., 1997. Marine terraces and Quandary history of the Sakhalin shelf. Dalnauka, Vladivostok (in Russian).Korotky, A.M., Kovalyukh, N.N. and Volkov, V.G., 1989. Radiocarbon dating of Quaternary deposits (south Far East). Preprint. Far East Branch of the USSR Academy of Sciences, Vladivostok (in Russian).
Sergeevka_River Neotoma22872369Mouth of Sergeevka River142.08333349.233333Asia2RawRiver10AWI0.0512.171Exposure in lagoon terrace. Physiography: river mouth on coast. Surrounding vegetation: Picea-Abies taiga.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Korotky, A., Grebennikova, T., Razjigaeva, N., Volkov, V., Mokhova, L., Ganzey, L. and Bazarova, V., 1997. Marine terraces of western Sakhalin Island. Catena, 30(1), pp.61-81.doi:10.1016/S0341-8162(97)00002-7Korotkiy, A.M., Pushkar, V.S., Grebennikova, T.A., Razzhigaeva, N.G., Karaulova, L.P., Mokhova, L.M., Ganzey, L.A., Cherepanova, M.N., Bazarova, V.B., Volkov, V.G. and Kovalyukh, N.N., 1997. Marine terraces and Quandary history of the Sakhalin shelf. Dalnauka, Vladivostok (in Russian).
Seryebryanka_Stream Neotoma22892371Seryebryanka Stream Exposure 5822145.85827044.050830Asia5RawCoast14AWI0.0705.775Lagoon sediments in marine terrace. Physiography: sea coast. Surrounding vegetation: Picea-Abies-broadleaf forest. Surrounding vegetation: Quercus crispula, Acer, Phellodendron amurense, Juglans, Betula, Aralia, Picea microsperma, Abies mayriana, Abies sachalinensis.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Korotky, A.M., Razzhigaeva, N.G., Mokhova, L.M., Ganzey, L.A., Grebennikova, T.A. and Bazarova, V.B., 1996. Coastal dunes as an indicator of period of global climatic deterioration (Kunashir Island, Kuriles). Geology of the Pacific Ocean, 13, pp.73-84.Korotky, A.M., Razjigaeva, N.G., Grebennikova, T.A., Ganzey, L.A., Mokhova, L.M., Bazarova, V.B. and Sulerzhitsky, L.D., 1995. Holocene marine terraces of Kunashiri Island, Kurile Islands. The Quaternary Research (Daiyonki-Kenkyu), 34(5), pp.359-375 (in Japanese).doi:10.4116/jaqua.34.5_359Korotky, A.M., Razjigaeva, N.G., Grebennikova, T.A., Ganzey, L.A., Mokhova, L.M., Bazarova, V.B., Sulerzhitsky, L.D. and Lutaenko, K.A., 2000. Middle-and late-Holocene environments and vegetation history of Kunashir Island, Kurile Islands, northwestern Pacific. The Holocene, 10(3), pp.311-331.doi:10.1191/095968300667552216
SILYAR2 Neotoma23062388Siluyanov Yar-2 Exposure137.83333346.133333Asia25RawFluvial14AWI2.71944.720Exposure in fluvial terrace. Physiography: river valley. Surrounding vegetation: Betula-broadleaf forest.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Korotky, A.M. and Lobanova, L.A., 1984. Radiocarbon dating and paleographic boundaries of the late Pleistocene-Holocene. In: Paleogeograhic boundaries and methods for their study ed. by A.M. Korotky and V.S. Pushkar (pp.106-114). Far Eastern Science Center, USSR Academy of Sciences, Vladivostok (in Russian).Korotky, A.M., Pletnev, S.P., Pushkar, V.S., Grebennikova, T.A., Raszhigaeva, N.T., Sahebgareeva, E.D. and Mohova, L.M., 1988. Evolution environment of south Far East (late Pleistocene and Holocene). Nauka, Moscow (in Russian).
SMOR Neotoma24952579Smorodinovoye Lake141.11666764.766667Asia800RawLake76AWI0.03528.281Glacial lake. Physiography: valley in mountains. Surrounding vegetation: Larix forest.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Anderson, P.M., Lozhkin, A.V., Belaya, B.V. and Simakov, K.V., 1998. Younger Dryas in western Beringia (northeastern Siberia). In: Environmental Changes in Beringia During the Quaternary ed. by K.V. Simakov (pp.28-44). North East Interdisciplinary Research Institute, Far East Branch, Russian Academy of Sciences, Magadan (in Russian).
Sosednee_Lake Neotoma24992583Sosednee Lake149.50000062.166667Asia822RawLake41AWI-0.06326.447Morainally dammed lake. Physiography: glacial topography in mountains. Surrounding vegetation: open larch forest.Lozhkin, A.V., Anderson, P.M., Eisner, W.R., Ravako, L.G., Hopkins, D.M., Brubaker, L.B., Colinvaux, P.A. and Miller, M.C., 1993. Late Quaternary lacustrine pollen records from southwestern Beringia. Quaternary Research, 39(3), pp.314-324.doi:10.1006/qres.1993.1038
STAD Neotoma25112596Stadukhinskaya Protoka Channel (Alas section)159.50000068.666667Asia12RawPeat11AWI6.9369.800Buried peat and lake silts, alas section. Physiography: yedoma-alas relief. Surrounding vegetation: open Larix dahurica forest.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Lozhkin, A.V. and Prokhorova, T.P., 1982. New data about the history of alas deposits from the Kolyma lowland (radiocarbon and palynological material). In: Stratigraphy and paleogeography of the late Cenozoic of eastern USSR ed. by S.F. Biske (pp.96-102). North East Interdisciplinary Research Institute, Far East Branch, USSR Academy of Sciences, Magadan (in Russian).
SUMINSK Neotoma25232612Suminskoye Zaimitschye Peat Exposure80.25000055.000000Asia135RawPeat16AWI0.0623.828Buried in kettlehole exposed by river. Physiography: river valley. Surrounding vegetation: bog in treeless landscape.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Khotinskiy, N.A., 1977. Holocene of northern Eurasia. Nauka, Moscow (in Russian).Klimanov, V.A., 1976. To the method of reconstruction of quantitative parameters of past climate. Vestnik MGU, Geographic Series, 2, pp.92-98 (in Russian).Klimanov, V.A., Levina, T.P., Orlova, L.A. and Panychev, V.A., 1987. Climate changes in the Barabinskaya plain during the Subatlantic period of the Holocene as recorded by Suminskoye Zaimitschye peat. In: Regional Geology of Siberia and the Far East ed. by I.V. Nikolayeva (pp.143-149). Nauka, Novosibirsk (in Russian).Shnitnikov, A.V., 1976. The lakes of Sredinnogo region and some ways to use them. In: The lakes of Sredinnogo region ed. by L.K. Davydov (pp.5-133). Nauka, Leningrad (in Russian).
SUOLLAKH Neotoma25252614Suollakh123.85000057.050000Asia810RawPeat51AWI2.76013.015NAAndreev, A.A. and Klimanov, V.A., 1991. Izmeneniya rastitel'nost i klimatamezhdurech'ya rek Ungra i Yakokit (Yuzhnaya Yakutia) v golotsene [Vegetation history and climate changes in the interfluve of the rivers Ungra and Yakokit (Southern Yakutia) during the Holocene]. Botanichesky Zhurnal, 76(3), pp.334-351 (in Russian).
SVERDRUP Neotoma25282618Sverdrup79.45742074.520900Asia7RawPeat8AWI9.21713.251Buried peat bog 6 m from sea. Physiography: low-relief arctic island. Surrounding vegetation: herb tundra.Tarasov, P.E., Andreev, A.A., Romanenko, F.A. and Sulerzhitskii, L.D., 1995. Palynostratigraphy of upper Quaternary deposits of Sverdrup Island, the Kara Sea. Stratigraphy and Geological Correlation, 3(2), pp.190-196.
TANON Neotoma25372627Tanon River [Quarry Site]151.20000059.666667Asia40RawPeat29AWI6.65948.459Peat, paleosols, alluvium section. Physiography: coastal river valley. Surrounding vegetation: Larix dahurica forest.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Lozhkin, A.V. and Glushkova, O.Y., 1997. New palynological assemblages and radiocarbon dates from the late Quaternary deposits of northern Priokhot'ye. In: Late Pleistocene and Holocene of Beringia ed. by M.K. Gagiev (pp.70-79). North East Interdisciplinary Research Institute, Far East Branch, Russian Academy of Sciences, Magadan (in Russian).
TIKHAN Neotoma25522643Tikhangou Exposure132.78333342.833333Asia4RawRiver25AWI0.02230.071Lagoon-alluvial exposure. Physiography: river mouth on coast. Surrounding vegetation: Quercus-Betula-broadleaf forest.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Korotkii, A.M., Karaulova, L.P. and Troitskaya, T.S., 1980. The Quaternary deposits of Primor'ye. Nauka, Novosibirsk (in Russian).Troitskaya, T.S., Korotky, A.M., Karaulova, L.P. and Tsar'ko, E.I., 1971. New data about postglacial transgression on the western coast of the Sea of Japan. Doklady Akademii Nauk, 196(2), pp.433-436 (in Russian).Pushkar, V.S. and Korotky, A.M., 1975. Paleogeographic condition of sedimentation in the Holocene lagoon of Vostok Gulf. In: Questions of geomorphology and Quaternary geology of the southern Far East ed. by A.M. Korotky and A.P. Kulakov (pp.111-117). Far Eastern Branch, USSR Academy of Sciences, Vladivostok (in Russian).
TOLMACH Neotoma25582649Tolmachevsko-Krivodanovskii Peat84.00000055.000000Asia110RawPeat30AWI1.37713.918Exposure in river terrace + terrace core. Physiography: river valley.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Orlova, L.A., 1990. The Holocene of Baraba (stratigraphy and radiocarbon chronology). Joint Institute for Geology, Geophysics and Mineralogy, Siberia Branch, USSR Academy of Sciences, Novosibirsk (in Russian).Volkov, I.A. and Arkhipov, S.A., 1978. Quaternary deposits of the Novosibirsk Region. Joint Institute for Geology, Geophysics and Mineralogy, Siberia Branch, USSR Academy of Sciences, Novosibirsk (in Russian).
TOM1 Neotoma25592650Tom' River Peat84.00000056.166667Asia100RawPeat25AWI0.21610.886peat section in river bluff. Physiography: river valley. Surrounding vegetation: Pinus sibirica, Picea, Abies.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Arkhipov, S.A. and Votakh, M.R., 1980. Palynological characteristics and the absolute age of peat near the mouth of the Tom' River. In: The palynology of Siberia ed. by V.N. Saks (pp.112-118). Nauka, Moscow (in Russian).Orlova, V.V., 1962. Klimat SSSR: Zapadnaya Sibir [Climate of the USSR: Western Siberia]. Gidrometizdat, Leningrad (in Russian).
TS Neotoma25682660Taloye Lake152.33333361.016667Asia750RawLake36AWI-0.06710.397Kettle in area of dead-ice relief. Physiography: glacial terrain in mountains. Surrounding vegetation: Larix dahurica forest.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Lozhkin, A.V., Anderson, P.M., Belaya, B.V., Glushkova, O.Y. and Stetsenko, T.V., 2000. Vegetation change in northeast Siberia at the Pleistocene-Holocene boundary and during the Holocene. In: The Quaternary period of Beringia, ed. by K.V. Simakov (pp.53-75). North East Interdisciplinary Research Institute, Far East Branch, Russian Academy of Sciences, Magadan (in Russian).doi:10.1016/S0277-3791(00)00121-9
Ulakhan_Adycha_River Neotoma27892884Ulakhan Exposure, Adycha River135.58333367.833333Asia130RawRiver9AWI5.1219.130River terrace exposure. Physiography: river valley in coastal lowland. Surrounding vegetation: open Larix dahurica forest.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.
UNASCHI Neotoma27902885Unaschi Exposure133.16666742.950000Asia35RawRiver6AWI8.53421.409Exposure in river terrace. Physiography: valley. Surrounding vegetation: farmland.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Korotky, A.M., Karaulova, L.P. and Troitskaya, T.S., 1980. The Quaternary deposits of Primor'ye. Nauka, Novosibirsk (in Russian).Golubeva, L.V. and Karaulova, L.P., 1983. The vegetation and stratigraphy of the Pleistocene and Holocene of the southern Far East. Nauka, Moscow (in Russian).
Vechernii_River Neotoma28072904Vechernii River147.75000063.283333Asia800RawRiver28AWI-0.0616.202Man-made exposure of alluvium and peat. Physiography: river valley in mountains. Surrounding vegetation: Larix dahurica forest.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.
VENYU1 Neotoma28082905Venyukovka-1 Exposure138.58333347.116667Asia5RawRiver14AWI-0.0140.834Floodplain terrace of river. Physiography: river valley. Surrounding vegetation: meadow, bog and floodplain forest.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Korotky, A.M., Karaulova, L.P. and Troitskaya, T.S., 1980. The Quaternary deposits of Primor'ye. Nauka, Novosibirsk (in Russian).Korotky, A.M., Pletnev, S.P., Pushkar, V.S., Grebennikova, T.A., Razzhigaeva, N.G., Sakhebgareeva, E.D. and Mokhova, L.M., 1988. Evolution environment of south Far East (late Pleistocene and Holocene). Nauka, Moscow (in Russian).
Venyukovka-2 Neotoma28092906Venyukovka-2 Exposure138.58333347.033333Asia6RawMarine24AWI0.3063.059Lower river valley on coast. Physiography: exposure in marine terrace. Surrounding vegetation: boggy meadows with shrubs.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Korotky, A.M., Karaulova, L.P. and Troitskaya, T.S., 1980. The Quaternary deposits of Primor'ye. Nauka, Novosibirsk (in Russian).
Venyukovka-3 Neotoma28102907Venyukovka-3 Exposure138.58333347.116667Asia5RawRiver19AWI1.4875.967Alluvial-lagoon terrace. Physiography: river mouth on coast. Surrounding vegetation: bog with Betula-Larix forest.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Korotky, A.M., Karaulova, L.P. and Troitskaya, T.S., 1980. The Quaternary deposits of Primor'ye. Nauka, Novosibirsk (in Russian).
VOSTOK_neotoma Neotoma28232920Vostok Gulf132.75000042.900000Asia5RawMarine15AWI1.5596.129Marine terrace in lower river valley. Physiography: coastal plain. Surrounding vegetation: Quercus mongolica-Betula forest.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Korotky, A.M., Karaulova, L.P. and Troitskaya, T.S., 1980. The Quaternary deposits of Primor'ye. Nauka, Novosibirsk (in Russian).
Wrangel_Island_wr12 Neotoma29423040Wrangel Island Exposure 12-179.75000071.166667Asia200RawRiver31AWI10.33113.692Section in river bluff. Physiography: low rolling hills. Surrounding vegetation: graminoid tundra.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Lozhkin, A.V., Anderson, P.M., Vartanyan, S.L., Brown, T.A., Belaya, B.V. and Kotov, A.N., 2001. Late Quaternary paleoenvironments and modern pollen data from Wrangel Island (Northern Chukotka). Quaternary Science Reviews, 20(1-3), pp.217-233.doi:10.1016/S0277-3791(00)00121-9
DIMA1 Neotoma6723077Kirgirlakh Stream, Berelyekh River Basin147.98333362.666667Asia700RawRiver9AWI2.13228.085Exposure along river terrace. Physiography: valley in mountainous region. Surrounding vegetation: Larix dahurica forest-tundra.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Shilo, N.A., Lozhkin, A.V., Titov, E.E. and Shumilov, Y.V., 1983. Kirgirlakh mammoth: paleography aspect. Nauka, Moscow (in Russian).
DIMA2 Neotoma6723078Kirgirlakh Stream, Berelyekh River Basin147.98333362.666667Asia700RawRiver16AWI0.17133.235Exposure along river terrace. Physiography: valley in mountainous region. Surrounding vegetation: Larix dahurica forest-tundra.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Shilo, N.A., Lozhkin, A.V., Titov, E.E. and Shumilov, Y.V., 1983. Kirgirlakh mammoth: paleography aspect. Nauka, Moscow (in Russian).
DIMA3 Neotoma6723079Kirgirlakh Stream, Berelyekh River Basin147.98333362.666667Asia700RawRiver11AWI35.70147.993Exposure along river terrace. Physiography: valley in mountainous region. Surrounding vegetation: Larix dahurica forest-tundra.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Shilo, N.A., Lozhkin, A.V., Titov, E.E. and Shumilov, Y.V., 1983. Kirgirlakh mammoth: paleography aspect. Nauka, Moscow (in Russian).Lozhkin, A.V., 1991. The questions of geochronology and the paleogeography of the Quaternary period, northeast USSR. In: The geology of the zone between the continent and the ocean of northeast Asia ed. by A.A. Sidorov and A.P. Milov (pp.47-59). North East Interdisciplinary Research Institute, Far East Branch, USSR Academy of Sciences, Magadan (in Russian).
DIMA4 Neotoma6723080Kirgirlakh Stream, Berelyekh River Basin147.98333362.666667Asia700RawRiver10AWI1.3687.122Exposure along river terrace. Physiography: valley in mountainous region. Surrounding vegetation: Larix dahurica forest-tundra.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Shilo, N.A., Lozhkin, A.V., Titov, E.E. and Shumilov, Y.V., 1983. Kirgirlakh mammoth: paleography aspect. Nauka, Moscow (in Russian).
OROKESS Neotoma17793499Orokess River Mouth Exposure 4036142.00000048.850000Asia6RawRiver28AWI0.6507.654Marine terrace near Orokess River mouth. Physiography: coastal plain. Surrounding vegetation: Picea-Abies-Larix taiga.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Alexandrova, A.N., 1982. The Pleistocene of Sakhalin. Nauka, Moscow (n Russian).Korotky, A., Grebennikova, T., Razjigaeva, N., Volkov, V., Mokhova, L., Ganzey, L. and Bazarova, V., 1997. Marine terraces of western Sakhalin Island. Catena, 30(1), pp.61-81.doi:10.1016/S0341-8162(97)00002-7Korotkiy, A.M., Pushkar, V.S., Grebennikova, T.A., Razzhigaeva, N.G., Karaulova, L.P., Mokhova, L.M., Ganzey, L.A., Cherepanova, M.N., Bazarova, V.B., Volkov, V.G. and Kovalyukh, N.N., 1997. Marine terraces and Quaternary history of the Sakhalin Shelf. Dal'nauka, Vladivostok (in Russian).
STAD2 Neotoma25113776Stadukhinskaya Protoka Channel (Alas section)159.50000068.666667Asia12RawPeat3AWI3.3209.572Buried peat and lake silts, alas section. Physiography: yedoma-alas relief. Surrounding vegetation: open Larix dahurica forest.Anderson, P.M. and Lozhkin, A.V., 2002. Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia.Lozhkin, A.V. and Prokhorova, T.P., 1982. New data about the history of alas deposits from the Kolyma lowland (radiocarbon and palynological material). In: Stratigraphy and paleogeography of the late Cenozoic of eastern USSR ed. by S.F. Biske (pp.96-102). North East Interdisciplinary Research Institute, Far East Branch, USSR Academy of Sciences, Magadan (in Russian).
ACHIT8 Neotoma29623861Achit-Nur90.49975049.480790Asia1435RawLake20AWI-0.04914.852NATarasov, P.E., Harrison, S.P., Saarse, L., Pushenko, M.Y., Andreev, A.A., Aleshinskaya, Z.V., Davydova, N.N., Dorofeyuk, N.I., Efremov, Y.V., Khomutova, V.I., Sevastyanov, D.V., Tamosaitis, J., Uspenskaya, O.N., Yakushko, O.F. and Tarasova, I.V., 1994. Lake status records from the former Soviet Union and Mongolia: data base documentation. Paleoclimatology Publications Series 2, World Data Center-A for Paleoclimatology, NOAA Paleoclimatology Program, Boulder, Colorado, USA.Tarasov, P.E., Webb III, T., Andreev, A.A., Afanas' eva, N.B., Berezina, N.A., Bezusko, L.G., Blyakharchuk, T.A., Bolikhovskaya, N.S., Cheddadi, R., Chernavskaya, M.M. and Chernova, G.M., 1998. Present-day and mid-Holocene biomes reconstructed from pollen and plant macrofossil data from the former Soviet Union and Mongolia. Journal of Biogeography, 25(6), pp.1029-1053.doi:10.1046/j.1365-2699.1998.00236.x
BAIDARA Neotoma29943898Baidara66.90000068.850000Asia30RawCoast67AWI4.40520.241Open section. Physiography: the third terrace of Kara sea. Surrounding vegetation: tundra with dwarf birch.Andreev, A.A., Tarasov, P.E., Romanenko, F.A., Sulerzhitskii, L.D. and Terekhov, K.I., 1998. Vegetation of the western coast of the Baidaratskaya Bay at the end of the Late Pleistocene. Stratigraphy and Geological Correlation, 6(5), pp.520-525.
BOGUDA Neotoma30293945Lake Boguda123.24559063.667310Asia120RawLake58AWI0.38011.136Thermokarst lake. Physiography: early Pleistocene terrace with sands. Surrounding vegetation: larch forest with pine and birch.Andreev, A.A. and Klimanov, V.A., 1989. Vegetation and climate history of central Yakutia during the Holocene and Late Pleistocene. In: Formirovanie rel'efa, korelyatnykh otlozheny i rossypei Severo-Vostoka SSSR [Formation of deposits and placers on northeast of the USSR] ed. by B.F. Ivanov and B.F. Palymsky (pp.28-51). Publishing House of SVKNII, Magadan, Russia (in Russian).
BUGRIST Neotoma30383956Bugristoe85.16666758.250000Asia100RawPeat67AWI4.57511.630Palsa bog surrounded by raised bog. Physiography: ancient narrow gully. Surrounding vegetation: Pinus sylvestris, Pinus sibirica, Betula pendula.Blyakharchuk, T.A., 1989. Istorija rastitel'nosti yugovostoka Zapadnoi Sibiri v golotsene po dannym botanicheskogo i sporovo-pyl'tsevogo analiza torfa [The Holocene history of vegetation of south-eastern West Siberia by botanical and pollen analyses of peat deposits]. Doctoral dissertation. Tomsk State University, Tomsk, Russia.Blyakharchuk, T.A., 1989. Detal'noe raschlenenie rannego i srednego golotsena po dannym issledovaniya azonal'nogo merzlogo torfyanika na yugeZapadnoi Sibiri [Middle and early Holocene by study of unzonal palsa bog in the south of West Siberia]. In: Abstract: Palinologiya i poleznye iskopaemye [Palynology and mineral sources] (p.26). Minsk, Byelorussia.
CHABADA1 Neotoma3463975Chabada Lake129.37787561.976835Asia290RawLake62AWI0.0799.111Thermokarst lake. Physiography: Lena Plain. Surrounding vegetation: taiga.Andreev, A.A. and Klimanov, V.A., 1989. Vegetation and climate history of central Yakutia during the Holocene and Late Pleistocene. In: Formirovanie rel'efa, korelyatnykh otlozheny i rossypei Severo-Vostoka SSSR [Formation of deposits and placers on northeast of the USSR] ed. by B.F. Ivanov and B.F. Palymsky (pp.28-51). Publishing House of SVKNII, Magadan, Russia (in Russian).Andreev, A.A., Klimanov, V.A., Sulerzhitsky, L.D. and Khotinsky, N.A., 1989. Chronology of environmental changes in central Yakutia during the Holocene. In: Paleoklimaty golotsena i pozdnelednikov'ya [Paleoclimates of Holocene and late glacial) (pp.115-121). Nauka, Moscow, Russia (in Russian).
CHERNOE Neotoma30543984Chernoe Lake106.64653050.964745Asia500RawLake10AWI1.0798.321Lake ca 500 m in diameter. Surrounding vegetation: Betula, Pinus sylvestris, Larix, Picea.Tarasov, P.E., Pushenko, M.Y., Harrison, S.P., Saarse, L., Andreev, A.A., Aleshinskaya, Z.V., Davydova, N.N., Dorofeyuk, N.I., Efremov, Y.V., Elina, G.A., Elovicheva, Y.K., Filimonova, L.V., Gunova, V.S., Khomutova, V.I., Kvavadze, E.V., Neustrueva, I.Y., Pisareva, V.V., Volkova, V.S., Shelekhova, T.S., Subetto, D.A., Uspenskaya, O.N. and Zernitskaya, V.P., 1996. Lake Status Records from the Former Soviet Union and Mongolia: Documentation of the Second Version of the Data Base. NOAA Paleoclimatology Publications Series Report No. 5. NOAA, Boulder, Colorado, USA.
CHERNYAR Neotoma30553985Cherny Yar161.00000056.066667Asia148RawRiver15AWI0.47614.741Physiography: the second terrace.
DABA8 Neotoma30764010Daba-Nur98.76251048.189240Asia2465RawLake25AWI-0.04613.502NATarasov, P.E., Pushenko, M.Y., Harrison, S.P., Saarse, L., Andreev, A.A., Aleshinskaya, Z.V., Davydova, N.N., Dorofeyuk, N.I., Efremov, Y.V., Elina, G.A., Elovicheva, Y.K., Filimonova, L.V., Gunova, V.S., Khomutova, V.I., Kvavadze, E.V., Neustrueva, I.Y., Pisareva, V.V., Volkova, V.S., Shelekhova, T.S., Subetto, D.A., Uspenskaya, O.N. and Zernitskaya, V.P., 1996. Lake Status Records from the Former Soviet Union and Mongolia: Documentation of the Second Version of the Data Base. NOAA Paleoclimatology Publications Series Report No. 5. NOAA, Boulder, Colorado, USA.Tarasov, P.E., Webb III, T., Andreev, A.A., Afanas' eva, N.B., Berezina, N.A., Bezusko, L.G., Blyakharchuk, T.A., Bolikhovskaya, N.S., Cheddadi, R., Chernavskaya, M.M. and Chernova, G.M., 1998. Present-day and mid-Holocene biomes reconstructed from pollen and plant macrofossil data from the former Soviet Union and Mongolia. Journal of Biogeography, 25(6), pp.1029-1053.doi:10.1046/j.1365-2699.1998.00236.x
DOOD4 Neotoma30854020Dood-Nur99.38333351.333333Asia1538RawLake19AWI0.30514.441Lake subdivided into 3 subbasins (Targan; Dund; Harmai), fed by many rivers and springs. Moraines from Mid-Pleistocene glaciation found in catchment.Tarasov, P.E., Pushenko, M.Y., Harrison, S.P., Saarse, L., Andreev, A.A., Aleshinskaya, Z.V., Davydova, N.N., Dorofeyuk, N.I., Efremov, Y.V., Elina, G.A., Elovicheva, Y.K., Filimonova, L.V., Gunova, V.S., Khomutova, V.I., Kvavadze, E.V., Neustrueva, I.Y., Pisareva, V.V., Volkova, V.S., Shelekhova, T.S., Subetto, D.A., Uspenskaya, O.N. and Zernitskaya, V.P., 1996. Lake Status Records from the Former Soviet Union and Mongolia: Documentation of the Second Version of the Data Base. NOAA Paleoclimatology Publications Series Report No. 5. NOAA, Boulder, Colorado, USA.Tarasov, P.E., Webb III, T., Andreev, A.A., Afanas' eva, N.B., Berezina, N.A., Bezusko, L.G., Blyakharchuk, T.A., Bolikhovskaya, N.S., Cheddadi, R., Chernavskaya, M.M. and Chernova, G.M., 1998. Present-day and mid-Holocene biomes reconstructed from pollen and plant macrofossil data from the former Soviet Union and Mongolia. Journal of Biogeography, 25(6), pp.1029-1053.doi:10.1046/j.1365-2699.1998.00236.x
ERAVNOE Neotoma30954030Bol'shoe Eravnoe Lake111.50050052.624200Asia947RawLake10AWI0.4089.079Lake. Surrounding vegetation: Larix, Betula, Pinus sylvestris.Tarasov, P.E., Harrison, S.P., Saarse, L., Pushenko, M.Y., Andreev, A.A., Aleshinskaya, Z.V., Davydova, N.N., Dorofeyuk, N.I., Efremov, Y.V., Khomutova, V.I., Sevastyanov, D.V., Tamosaitis, J., Uspenskaya, O.N., Yakushko, O.F. and Tarasova, I.V., 1994. Lake status records from the former Soviet Union and Mongolia: data base documentation. Paleoclimatology Publications Series 2, World Data Center-A for Paleoclimatology, NOAA Paleoclimatology Program, Boulder, Colorado, USA.
GUNNUR Neotoma31374081Gun-Nur106.61880050.261800Asia600RawLake36AWI-0.06811.117Small lake in topographic depression in limno-fluvial lowland, with mountains rising to 1554 m.Tarasov, P.E., Pushenko, M.Y., Harrison, S.P., Saarse, L., Andreev, A.A., Aleshinskaya, Z.V., Davydova, N.N., Dorofeyuk, N.I., Efremov, Y.V., Elina, G.A., Elovicheva, Y.K., Filimonova, L.V., Gunova, V.S., Khomutova, V.I., Kvavadze, E.V., Neustrueva, I.Y., Pisareva, V.V., Volkova, V.S., Shelekhova, T.S., Subetto, D.A., Uspenskaya, O.N. and Zernitskaya, V.P., 1996. Lake Status Records from the Former Soviet Union and Mongolia: Documentation of the Second Version of the Data Base. NOAA Paleoclimatology Publications Series Report No. 5. NOAA, Boulder, Colorado, USA.Dorofeyuk, N.I. and Tarasov, P.E., 1998. Vegetation and lake levels of northern Mongolia since 12,500 yr BP based on the pollen and diatom records. Stratigraphy and Geological Correlation, 6(1), pp.70-83.Tarasov, P.E., Webb III, T., Andreev, A.A., Afanas' eva, N.B., Berezina, N.A., Bezusko, L.G., Blyakharchuk, T.A., Bolikhovskaya, N.S., Cheddadi, R., Chernavskaya, M.M. and Chernova, G.M., 1998. Present-day and mid-Holocene biomes reconstructed from pollen and plant macrofossil data from the former Soviet Union and Mongolia. Journal of Biogeography, 25(6), pp.1029-1053.doi:10.1046/j.1365-2699.1998.00236.x
HOTON Neotoma31494097Hoton-Nur88.28455048.672560Asia2083RawLake37AWI0.37624.108Lake. Physiography: intermontane depression dammed by morain. Surrounding vegetation: steppe and meadow-steppe.Tarasov, P.E., Harrison, S.P., Saarse, L., Pushenko, M.Y., Andreev, A.A., Aleshinskaya, Z.V., Davydova, N.N., Dorofeyuk, N.I., Efremov, Y.V., Khomutova, V.I., Sevastyanov, D.V., Tamosaitis, J., Uspenskaya, O.N., Yakushko, O.F. and Tarasova, I.V., 1994. Lake status records from the former Soviet Union and Mongolia: data base documentation. Paleoclimatology Publications Series 2, World Data Center-A for Paleoclimatology, NOAA Paleoclimatology Program, Boulder, Colorado, USA.Tarasov, P., Dorofeyuk, N. and 'TSEVA, E.M., 2000. Holocene vegetation and climate changes in Hoton-Nur basin, northwest Mongolia. Boreas, 29(2), pp.117-126.doi:10.1111/j.1502-3885.2000.tb01205.xTarasov, P.E., Webb III, T., Andreev, A.A., Afanas' eva, N.B., Berezina, N.A., Bezusko, L.G., Blyakharchuk, T.A., Bolikhovskaya, N.S., Cheddadi, R., Chernavskaya, M.M. and Chernova, G.M., 1998. Present-day and mid-Holocene biomes reconstructed from pollen and plant macrofossil data from the former Soviet Union and Mongolia. Journal of Biogeography, 25(6), pp.1029-1053.doi:10.1046/j.1365-2699.1998.00236.x
HUBSUGUL_neotoma Neotoma31544102Hubsugul100.22665050.628600Asia1645RawLake15AWI-0.0607.067Large freshwater lake fed by 46 rivers and streams; western shore is steep and rocky; eastern shore relatively flat and swampy.Tarasov, P.E., Pushenko, M.Y., Harrison, S.P., Saarse, L., Andreev, A.A., Aleshinskaya, Z.V., Davydova, N.N., Dorofeyuk, N.I., Efremov, Y.V., Elina, G.A., Elovicheva, Y.K., Filimonova, L.V., Gunova, V.S., Khomutova, V.I., Kvavadze, E.V., Neustrueva, I.Y., Pisareva, V.V., Volkova, V.S., Shelekhova, T.S., Subetto, D.A., Uspenskaya, O.N. and Zernitskaya, V.P., 1996. Lake Status Records from the Former Soviet Union and Mongolia: Documentation of the Second Version of the Data Base. NOAA Paleoclimatology Publications Series Report No. 5. NOAA, Boulder, Colorado, USA.Tarasov, P.E., Webb III, T., Andreev, A.A., Afanas' eva, N.B., Berezina, N.A., Bezusko, L.G., Blyakharchuk, T.A., Bolikhovskaya, N.S., Cheddadi, R., Chernavskaya, M.M. and Chernova, G.M., 1998. Present-day and mid-Holocene biomes reconstructed from pollen and plant macrofossil data from the former Soviet Union and Mongolia. Journal of Biogeography, 25(6), pp.1029-1053.doi:10.1046/j.1365-2699.1998.00236.x
KARASEOZ Neotoma31824138Karasieozerskoe60.75000056.766667Asia230RawPeat31AWI0.1707.342Drained peatland. Physiography: low elevation mountains. Surrounding vegetation: Pinus sylvestris, Betula pubescens.Panova, N.K., 1997. Palinologicheskoe issledovanie Karasieozerskogo torfyanika na srednem Urale [Palynological study of Karasieozerskiy peatland on Middle Ural]. Materialy nauchnykh chteniy posvyaschennykh pamyati B.P. Kolesnikova [Investigations of Ural forests. Proceedings of scientific reports in the memory of B.P. Kolesnikov]. Ekaterinburg, Institute of Forest (in Polish).
MAKSIMKI Neotoma32684245Maksimkin Yar86.78551558.695235Asia150RawPeat48AWI0.0129.113Section of raised bog in valley of Ket'. Physiography: first terrase of Ket' River. Surrounding vegetation: Pinus sylvestris, Pinus sibirica, Betula, Picea.Blyakharchuk, T.A., 1980. Sporovo-pyl'zevaya kharakteristika bolot verhneketskogo raiona [Spore and pollen characteristics of peatlands of the Verhneketskii region during the Holocene]. In: Molodye uchoenye narodnomy khozyaistvy Ekonomicheskaya ozenka landshafta Tomskoi oblasti [Abstracts of the Conference \Young Scientist for Peoples Economy: Economical Evaluation of the Tomsk Region\] (pp.24-25). Tomsk University Press, Tomsk, Russia.Blyakharchuk, T.A., 1989. Istorija rastitel'nosti yugovostoka Zapadnoi Sibiri v golotsene po dannym botanicheskogo i sporovo-pyl'tsevogo analiza torfa [The Holocene history of vegetation of south-eastern West Siberia by botanical and pollen analyses of peat deposits]. Doctoral dissertation. Tomsk State University, Tomsk, Russia.
NULSAVEI Neotoma33244316Nulsaveito70.16666767.533333Asia57RawPeat30AWI6.1468.782Peat section open by thermoabrasion. Physiography: sandy plain cut by numerous streams. Surrounding vegetation: Betula nana, shrub Salix, mosses.Panova, N.K., 1990. Novye dannye po paleoekologii i istorii rastitelnosti yuzhnogo Yamala v golotsene [New data for paleoecology and vegetation history of southern Yamal during the Holocene]. In: Chetvertichnyi period: metody issledovania, stratigrafia i ekologia. VII Vseseoyuznoe soveschanie [Quaternary: methods, stratigraphy and ecology. VII All-Union conference, Abstracts] (pp.45-46). Volume 3 (in Czech).
NUOCHAGA Neotoma33254317Lake Nuochaga129.55584061.300580Asia260RawLake45AWI0.0416.718NAAndreev, A.A. and Klimanov, V.A., 1989. Vegetation and climate history of central Yakutia during the Holocene and Late Pleistocene. In: Formirovanie rel'efa, korelyatnykh otlozheny i rossypei Severo-Vostoka SSSR [Formation of deposits and placers on northeast of the USSR] ed. by B.F. Ivanov and B.F. Palymsky (pp.28-51). Publishing House of SVKNII, Magadan, Russia (in Russian).
PETROP Neotoma33504347Petropavlovka82.92709558.381420Asia100RawPeat66AWI-0.02810.826Raised bog. Physiography: First terrace of Ob' River. Surrounding vegetation: Pinus sylvestris, Pinus sibirica, Betula p.Blyakharchuk, T.A., 1989. Istorija rastitel'nosti yugovostoka Zapadnoi Sibiri v golotsene po dannym botanicheskogo i sporovo-pyl'tsevogo analiza torfa [The Holocene history of vegetation of south-eastern West Siberia by botanical and pollen analyses of peat deposits]. Doctoral dissertation. Tomsk State University, Tomsk, Russia.
TEGULD Neotoma34624481Teguldet88.16666757.333333Asia150RawBog55AWI0.0357.340Mesotrophic bog. Physiography: ancient valley of Chulym River. Surrounding vegetation: Betula pendula, Pinus sylvestris, Pinus sibirica, Abies s.Blyakharchuk, T.A., 1989. Istorija rastitel'nosti yugovostoka Zapadnoi Sibiri v golotsene po dannym botanicheskogo i sporovo-pyl'tsevogo analiza torfa [The Holocene history of vegetation of south-eastern West Siberia by botanical and pollen analyses of peat deposits]. Doctoral dissertation. Tomsk State University, Tomsk, Russia (in Russian).
URMIA20 Neotoma34844504Lake Urmia45.46666737.583333Asia1265RawLake51AWI3.49814.829Saline lake. Physiography: basin in plateau. Surrounding vegetation: Artemisia fragratis and remnants of Quercetea brantii.Bottema, S., 1987. Chronology and climatic phases in the near east from 16,000 to 10,000 BP. In: Chronologies in the Near East: Relative Chronologies and Absolute Chronology, 16000-4000 B.C. British Archaeological Reports S379 ed. by O. Aurenche, J. Evin, and F. Hours (pp.295-310). Oxford: British Archaeological Reports, Oxford, United Kingdom.Bottema, S., 1986. A late Quaternary pollen diagram from Lake Urmia (northwestern Iran). Review of palaeobotany and palynology, 47(3-4), pp.241-261.doi:10.1016/0034-6667(86)90039-4Kelts, K. and Shahrabi, M., 1986. Holocene sedimentology of hypersaline Lake Urmia, northwestern Iran. Palaeogeography, Palaeoclimatology, Palaeoecology, 54(1-4), pp.105-130.doi:10.1016/0031-0182(86)90120-3van Zeist, W. and Bottema, S., 1977. Palynological investigations in western Iran. Palaeohistoria, 19, pp.19-85.Wright Jr, H.E., McAndrews, J.H. and van Zeist, W., 1967. Modern pollen rain in western Iran, and its relation to plant geography and Quaternary vegetational history. Journal of Ecology, 55, pp.415-443.doi:10.2307/2257886
USTMASH Neotoma34854505Ust'Mashevskoe57.88333356.316667Asia220RawPeat51AWI-0.0308.404Raised bog of first terrace of Ufa river. Physiography: plateau. Surrounding vegetation: Picea obovata, Betula pubescens, Pinus.Panova, N.K., Makovsky, V.I. and Erokhin, N.G., 1996. Golotsenovaya dinamika rastitelnosti v raione Krasnoufimskoi stepi [Holocene dynamics of vegetation in Krasnoufimskaya forest-steppe area]. In: Lesoobrazovatel'nyi protses na Urale i Zaural'e [Forest Formation Processes in the Urals and Transural Region] (pp.80-93). Intitute of forest, Ekaterinburg, Russia (in Russian).
ZERIBAR Neotoma35214548Lake Zeribar46.11666735.533333Asia1288RawLake142AWI2.53948.694Lake. Physiography: valley. Surrounding vegetation: cultivated fields and oak forest.Bottema, S., 1987. Chronology and climatic phases in the near east from 16,000 to 10,000 BP. In: Chronologies in the Near East: Relative Chronologies and Absolute Chronology, 16000-4000 B.C. British Archaeological Reports S379 ed. by O. Aurenche, J. Evin, and F. Hours (pp.295-310). Oxford: British Archaeological Reports, Oxford, United Kingdom.van Zeist, W. and Bottema, S., 1977. Palynological investigations in western Iran. Palaeohistoria, 19, pp.19-85.
HACHI-NU Neotoma857813079Hachiman-Numa140.86666739.950000Asia1580RawBog23AWI-0.0176.408Bog. Physiography: gentle slope. Surrounding vegetation: Sphagnum moor.Morita, Y., 1985. The vegetational history of the subalpine zone in northeast Japan. II. The Hachimantai Mountains. Japanese Journal of Ecology, 35(3), pp.411-420 (in Japanese).
Iwaya Neotoma960614134Iwaya site135.88674035.517630Asia20RawPeat94AWI-0.00150.894Rice paddy. Physiography: small basin. Surrounding vegetation: rice paddy. Lies in a basin ~1.2 km in diameter.Takahara, H. and Takeoka, M., 1992. Vegetation history since the last glacial period in the Mikata lowland, the Sea of Japan area, western Japan. Ecological Research, 7(3), pp.371-386.doi:10.1007/BF02347104Takahara, H., Ito, T. and Takeoka, M., 1988. Woods invaded by the sugi bark borer, Semanotus japonicus Lacordaire (Coleoptera: Cerambycidae), about 3,000 years ago, and the forest vegetaion at that time. Journal of the Japanese Forestry Society, 70(4), pp.143-150 (in Japanese).doi:10.11519/jjfs1953.70.4_143
HURLEG Neotoma986114612Hurleg Lake96.90074037.274460Asia2817RawLake61AWI0.00413.656Lake is located in the Qaidam Basin, an arid intermontane basin, on the NE Tibetan Plateau, surrounded by the Kunlun Mountains to the south, the Altun Mountains to the west, and the Qilian Mountains to the north and east. Surrounding desert vegetation dominated by Amaranthaceae (Salsola abrotanoides, Kalidium gracile, Ceratoides latens, Haloxylon ammodendron, and Sympegma regelii), Ephedra, Nitraria, and Asteraceae (Artemisia, Ajania fruticulosa, and Asterothamnus centrali-asiaticus)Zhao, Y., Yu, Z., Chen, F., Ito, E. and Zhao, C., 2007. Holocene vegetation and climate history at Hurleg Lake in the Qaidam Basin, northwest China. Review of Palaeobotany and Palynology, 145(3-4), pp.275-288.doi:10.1016/j.revpalbo.2006.12.002
ZOIGE08C1 Neotoma986414619Zoige Basin102.63333333.450000Asia3467RawPeat153AWI-0.06010.168Large inter-valley peatland in the Zoige Basin, a low-relief plateau in the eastern Tibetan Plateau. Upland vegetation dominated by Kobresia spp., other Cyperaceae, Artemisia, Poaceae, and Ranunculaceae. Peatland vegetation dominated by Cyperaceae, including Carex muliensis and Kobresia humilis.Zhao, Y., Yu, Z. and Zhao, W., 2011. Holocene vegetation and climate histories in the eastern Tibetan Plateau: controls by insolation-driven temperature or monsoon-derived precipitation changes?. Quaternary Science Reviews, 30(9-10), pp.1173-1184.doi:10.1016/j.quascirev.2011.02.006
TIANCHI Neotoma987714648Tianchi Lake106.30884035.264675Asia2430RawLake72AWI-0.0575.919Clossed basin lake is located in the Liupan Mountains on the southwestern Loess Plateau. Natural vegetation: temperate steppe forest dominated by Betula platyphylla, B. albo-sinensis, Quercus liaotungensis, Q. variabilis, Q. aliena, Populus davidiana, Pinus armandii, and Ostryopsis davidiana. Lowland steppe dominated by Artemisia gmelinii and Stipa bacialensis. Forest steppe at 1700-2300 m; forest above 2300 m. Natural vegetation mostly destroyed since the 1950s, and the current vegetation is dwarf-shrub.Sun, H., Zhou, A., Zhang, X. and Chen, F., 2011. Fir trees disappeared 500 years ago in the Liupan Mountains on the southwestern Loess Plateau, China. Review of Palaeobotany and Palynology, 166(1-2), pp.69-75.doi:10.1016/j.revpalbo.2011.05.003Zhao, Y., Chen, F., Zhou, A., Yu, Z. and Zhang, K., 2010. Vegetation history, climate change and human activities over the last 6200 years on the Liupan Mountains in the southwestern Loess Plateau in central China. Palaeogeography, Palaeoclimatology, Palaeoecology, 293(1-2), pp.197-205.doi:10.1016/j.palaeo.2010.05.020Zhou, A., Sun, H., Chen, F., Zhao, Y., An, C., Dong, G., Wang, Z. and Chen, J., 2010. High-resolution climate change in mid-late Holocene on Tianchi Lake, Liupan Mountain in the Loess Plateau in central China and its significance. Chinese Science Bulletin, 55(20), pp.2118-2121.doi:10.1007/s11434-010-3226-0
HACHIHAM Neotoma1029315612Hachihama133.95054034.552260Asia6RawCoast57Neotoma 10.00055.000Sewage disposal plant. Physiography: reclaimed land. Surrounding vegetation: paddy field.Miyoshi, N., 1994. Pollen Analytical Study about the Vegetational Change and Climate Change on the Low Land of the Coast of the Inland Sea. The Study Report by the Ryobi Entei commemoration Foundation Research Grant, pp.43-51 (in Japanese).
HOSOIKE Neotoma1029715624Hosoike Moor134.13333335.350000Asia970RawPeat59AWI-0.03145.723Moor located on the southwestern slope of Mt. Gorin in the northeastern Chugoku Mountans. Moor a complex of open water with Nymphaea tetragona, Cyperaceae fen, and Sphagnum moorland. Overstory vegetation is Ilex crenata and Symplocos coreana. Upland vegetation around the moor dominatd by Cryptomeria japonica and Larix leptolepis, also deciduous forest with Fagus crenata, Quercus mongolica var. grosseserrata, Sorbus commixta, and Acer crataegifolium.Miyoshi, N., 1989. Vegetation history of the Hosoike Moor in the Chugoku Mountains, western Japan during the Late Pleistocene and Holocene. Japanese Journal of Palynology, 35(2), pp.27-42 (in Japanese).
IKENOKOC Neotoma1031015649Ikenokochi Moor136.13079035.653925Asia300RawPeat41AWI-0.06113.628Sphagnum moor in a small basin. Abundant Menyanthes trifoliata. Upland vegetation Cryptomeria japonica forest and Pinus densiflora secondary forest.Takahara, H., Nishida, S. and Takemura, K., 1995. Vegetation history since the late-glacial period around the Ikenokochi Moor, Fukui Prefecture, Japan. Japanese Journal of Palynology, 41(2), pp.99-108 (in Japanese).
MAKURA Neotoma1031815665Makura Moor132.38750034.730556Asia720RawBog19AWI-0.03110.591Sphagnum bog with Ilex crenata in a small basin.Miyoshi, N. and Hada, Y., 1977. Pollen analysis studies of moor sediments in Chugoku, Japan. IV. makura moor (Hiroshima Pref.). Japanese Journal of Ecology, 27(4), pp.285-290 (in Japanese).
OHNUMA Neotoma1032415678Ohnuma Moor134.56666735.408333Asia610RawPeat37AWI0.05123.881Sphagnum moor occupying a volcanic crater on the southeast slope of Mt. Torokawa in the Chugoku Mountains. Fen vegetation dominated by Sphagnum, Ilex crenata, and Carex dispalata. Upland vegetation is secondary forest dominated by Castanea crenata, Quercus serrata, and Pinus densiflora.Miyoshi, N. and Yano, N., 1986. Late Pleistocene and Holocene vegetational history of the Ohnuma moor in the Chugoku mountains, western Japan. Review of palaeobotany and palynology, 46(3-4), pp.355-376.doi:10.1016/0034-6667(86)90022-9
UBUKA Neotoma1033515704Ubuka Basin131.58611134.490278Asia390RawPeat53AWI-0.02429.405Small basin in the Ubuka sedimentary basin at the western edge of the Chugoku Mountains. Today occupied by rice paddies.Hatanaka, K. and Miyoshi, N., 1980. History of the late Pleistocene and Holocene vegetation in the Ubuka basin, southwestern Japan. Japanese Journal of Ecology, 30, pp.239-244 (in Japanese).
YABITSU Neotoma1033815709Yabitsuyachi140.90000040.616667Asia1080RawPeat30AWI0.5079.151Sphagnum moor in a small basin.Morita, Y., 1987. The vegetational history of the subalpine zone in northeast Japan: III. The Hakkoda Mountains. Japanese Journal of Ecology, 37(2), pp.107-117 (in Japanese).Morita, Y., and Aizawa, S., 1986. Pollen-analytical study on the vegetational history of the subalpine zone in the northern Tohoku district. Annals of The Tohoku Geographycal Asocciation, 38(1), pp.24-31 (in Japanese).doi:10.5190/tga1948.38.24
STLAWR2 Neotoma1158017340St. Lawrence Section 2-171.54791763.667222Asia0RawPeat26AWI0.42610.119Peat section on sea cliff exposure. Physiography: coastal area of island. Surrounding vegetation: Betula-graminoid tundra.Lozhkin, A.V., Hopkins, D.M., Solomatkina, T.B., Eisner, W.R. and Brigham-Grette, J., 1998. Radiocarbon dates and palynological characteristics of peat from St Lawrence Island, Alaska. In: Environmental changes in Beringia during the Quaternary (pp.9-27). North East Interdisciplinary Research Institute, Far East Branch, Russian Academy of Sciences, Magadan, Russia.
STLAWR3 Neotoma1158417347St. Lawrence Island Section 3-171.58194463.673889Asia0RawPeat37AWI-0.03917.836Exposure along sea cliffs. Physiography: sea cliff. Surrounding vegetation: herb tundra.Lozhkin, A.V., Hopkins, D.M., Solomatkina, T.B., Eisner, W.R. and Brigham-Grette, J., 1998. Radiocarbon dates and palynological characteristics of peat from St Lawrence Island, Alaska. In: Environmental changes in Beringia during the Quaternary (pp.9-27). North East Interdisciplinary Research Institute, Far East Branch, Russian Academy of Sciences, Magadan, Russia.
Naskak_neotoma Neotoma1299919264Naskak_neotoma-171.45401063.641012Asia1RawPeat27AWI-0.0459.994Peat exposure located on the eastern beach of a small lake on the coast of St. Lawrence Island. The lake is separated from the Bering Sea by a spit of sand and pebbles that is ~150 m wide. Surroundig vegetation: diverse herb-Salix tundra, with Salix polaris and S. pulchra being the most common woody species in the local vegetation. Graminoids are especially abundant with Alopecurus alpinus typical of boggy areas. Although the relief is modest, south-facing slopes support Artemisia tilesii, A. borealis, Salix arctica, and S. ovalifolia. Salix arctica, S. polaris, S. reticulata, S. ovalifolia, and S. pulchra are found near the. lagoon beach.Lozhkin, A.V., Anderson, P., Eisner, W.R. and Solomatkina, T.B., 2011. Late glacial and Holocene landscapes of central Beringia. Quaternary Research, 76(3), pp.383-392.doi:10.1016/j.yqres.2011.08.003
AGHNAGHA Neotoma1300019266Aghnaghak-171.55381563.656005Asia1RawPeat35AWI-0.03517.560Peat exposure located on the coast of St. Lawrence Island. Surroundig vegetation: diverse herb-Salix tundra, with Salix polaris and S. pulchra being the most common woody species in the local vegetation. Graminoids are especially abundant with Alopecurus alpinus typical of boggy areas. Although the relief is modest, south-facing slopes support Artemisia tilesii, A. borealis, Salix arctica, and S. ovalifolia. Salix arctica, S. polaris, S. reticulata, S. ovalifolia, and S. pulchra are found near the. lagoon beach.Lozhkin, A.V., Anderson, P., Eisner, W.R. and Solomatkina, T.B., 2011. Late glacial and Holocene landscapes of central Beringia. Quaternary Research, 76(3), pp.383-392.doi:10.1016/j.yqres.2011.08.003
LAHI Neotoma1345420188Lake Hill-170.24827057.178240Asia37RawLake81AWI-0.03511.312Crater Lake (maar) with steep sides on all sides except to NNW, which is gently sloping. Remnants of old fence visible along lakeshore and a US military radar installation is built on the highest point of crater wall, on western side.Graham, R.W., Belmecheri, S., Choy, K., Culleton, B.J., Davies, L.J., Froese, D., Heintzman, P.D., Hritz, C., Kapp, J.D., Newsom, L.A. and Rawcliffe, R., 2016. Timing and causes of mid-Holocene mammoth extinction on St. Paul Island, Alaska. Proceedings of the National Academy of Sciences, 113(33), pp.9310-9314.doi:10.1073/pnas.1604903113
KAKITU1 Neotoma1580424294Kakitu Mountain96.46666738.050000Asia4620RawPeat27AWI8.03110.956Peat bog layer exposed by a small river. Physiography: Qinghai-Xizang plateau. Surrounding vegetation: Subnival cushion.Beug, H.J., 1987. Palynological studies on a peat layer in Kakitu Mountain, Northeastern Quinhai-Xizang plateau. In: Reports of the Qinghai-Xizang (Tibet) Plateau ed. by J. Hovermann and W. Wenying ( pp.496-501). Science Press, Beijing.
CS98-10 Neotoma1671226563Cape Shpindler62.80000069.716667Asia20RawMarine38AWI1.37416.081Coastal cliff. Physiography: Thermokarst depression. Surrounding vegetation: Betula n.,Salix,Dryas.& mosses. Vegetation formation: Subarctic tundra.Andreev, A.A., Manley, W.F., Ingolfsson, O. and Forman, S.L., 2001. Environmental changes on Yugorski Peninsula, Kara Sea, Russia, during the last 12,800 radiocarbon years. Global and Planetary Change, 31(1-4), pp.255-264.doi:10.1016/S0921-8181(01)00123-0
Lyadhej-To Neotoma1671326565Lyadhej-To lake65.79111068.246555Asia150RawLake72AWI0.16710.903Lake. Surrounding vegetation: Tundra Polar Ural. Vegetation formation: Tundra.Andreev, A.A., Tarasov, P.E., Ilyashuk, B.P., Ilyashuk, E.A., Cremer, H., Hermichen, W.D., Wischer, F. and Hubberten, H.W., 2005. Holocene environmental history recorded in Lake Lyadhej-To sediments, polar Urals, Russia. Palaeogeography, Palaeoclimatology, Palaeoecology, 223(3-4), pp.181-203.doi:10.1016/j.palaeo.2005.04.004
KNS11B Neotoma1791730184Kanas Lake87.07225048.802645Asia1365RawLake123AWI-0.02613.667Moraine dammed lake formed by a valley glacier during the last glaciation; located on the south side of the Altai Mountains. Regional vegetation: tundra vegetation 3000-3500 m elevation; sub-alpine and alpine meadow 2300-3000 m; Siberian taiga forest (Abies sibirica, Larix sibirica, Pinus obovata, P sibirica, Populus tremula, Betula pendula, B. pubescens) 1300-2300 m; desert and desert steppe 500-1300 m.Huang, X., Peng, W., Rudaya, N., Grimm, E.C., Chen, X., Cao, X., Zhang, J., Pan, X., Liu, S., Chen, C. and Chen, F., 2018. Holocene vegetation and climate dynamics in the Altai Mountains and surrounding areas. Geophysical Research Letters, 45(13), pp.6628-6636.doi:10.1029/2018GL078028
KTK1 Neotoma2369240990Lake Kotokel108.13333352.783333Asia458RawLake128AWI-0.02415.049Fresh-water lake. Physiography: Intermountain depression. Surrounding vegetation: Boreal coniferous and deciduous forests.Tarasov, P.E., Bezrukova, E.V. and Krivonogov, S.K., 2009. Late Glacial and Holocene changes in vegetation cover and climate in southern Siberia derived from a 15 kyr long pollen record from Lake Kotokel. Climate of the Past, 5(3), pp.285-295.doi:10.5194/cp-5-285-2009
Baikal_Lake-CON01-603-5 Neotoma2369640997Lake Baikal108.91361153.954722Asia465RawLake137AWI-0.01516.871Baikal lake.Demske, D., Heumann, G., Granoszewski, W., Nita, M., Mamakowa, K., Tarasov, P.E. and Oberhansli, H., 2005. Late glacial and Holocene vegetation and regional climate variability evidenced in high-resolution pollen records from Lake Baikal. Global and Planetary Change, 46(1-4), pp.255-279.doi:10.1016/j.gloplacha.2004.09.020
PG1756 Neotoma2374941098Lake Billyakh126.76994565.289100Asia340RawLake80AWI-0.05414.627Lake Billyakh is situated in the middle part of the western foreland of the Verkhoyansk Mountains, occupying a longitudinal depression between the Tekir-Khaya Ridge and the Muosutchanskiy Ridge. Floristically, the study area belongs to the boreal forest zone. Larix dahurica forest with Pinus sylvestris, Betula platyphylla, and shrubs dominate the vegetation. In the understorey, Ericales are abundant, including Vaccinium vitis-idaea, V. uliginosum, Arctous alpina, Ledum palustre, Cassiope sp., and Empetrum nigrum, together with members of the Rosaceae family, grasses, and sedges. Mosses and lichens are also common.Muller, S., 2009. Late Quaternary environmental changes in Yakutia (NE Siberia, Russia) inferred from pollen and testate amoebae records. Doctoral dissertation. University of Berlin, Berlin, Germany.Muller, S., Bobrov, A.A., Schirrmeister, L., Andreev, A.A. and Tarasov, P.E., 2009. Testate amoebae record from the Laptev Sea coast and its implication for the reconstruction of Late Pleistocene and Holocene environments in the Arctic Siberia. Palaeogeography, Palaeoclimatology, Palaeoecology, 271(3-4), pp.301-315.doi:10.1016/j.palaeo.2008.11.003Muller, S., Tarasov, P.E., Andreev, A.A. and Diekmann, B., 2009. Late Glacial to Holocene environments in the present-day coldest region of the Northern Hemisphere inferred from a pollen record of Lake Billyakh, Verkhoyansk Mts, NE Siberia. Climate of the Past, 5(1), pp.73-84.doi:10.5194/cp-5-73-2009Muller, S., Tarasov, P.E., Andreev, A.A., Tutken, T., Gartz, S. and Diekmann, B., 2010. Late Quaternary vegetation and environments in the Verkhoyansk Mountains region (NE Asia) reconstructed from a 50-kyr fossil pollen record from Lake Billyakh. Quaternary Science Reviews, 29(17-18), pp.2071-2086.doi:10.1016/j.quascirev.2010.04.024
PG1755 Neotoma2374941138Lake Billyakh126.76994565.289100Asia340RawLake107AWI0.42049.892Lake Billyakh is situated in the middle part of the western foreland of the Verkhoyansk Mountains, occupying a longitudinal depression between the Tekir-Khaya Ridge and the Muosutchanskiy Ridge. Floristically, the study area belongs to the boreal forest zone. Larix dahurica forest with Pinus sylvestris, Betula platyphylla, and shrubs dominate the vegetation. In the understorey, Ericales are abundant, including Vaccinium vitis-idaea, V. uliginosum, Arctous alpina, Ledum palustre, Cassiope sp., and Empetrum nigrum, together with members of the Rosaceae family, grasses, and sedges. Mosses and lichens are also common.Muller, S., 2009. Late Quaternary environmental changes in Yakutia (NE Siberia, Russia) inferred from pollen and testate amoebae records. Doctoral dissertation. University of Berlin, Berlin, Germany.Muller, S., Bobrov, A.A., Schirrmeister, L., Andreev, A.A. and Tarasov, P.E., 2009. Testate amoebae record from the Laptev Sea coast and its implication for the reconstruction of Late Pleistocene and Holocene environments in the Arctic Siberia. Palaeogeography, Palaeoclimatology, Palaeoecology, 271(3-4), pp.301-315.doi:10.1016/j.palaeo.2008.11.003Muller, S., Tarasov, P.E., Andreev, A.A. and Diekmann, B., 2009. Late Glacial to Holocene environments in the present-day coldest region of the Northern Hemisphere inferred from a pollen record of Lake Billyakh, Verkhoyansk Mts, NE Siberia. Climate of the Past, 5(1), pp.73-84.doi:10.5194/cp-5-73-2009Muller, S., Tarasov, P.E., Andreev, A.A., Tutken, T., Gartz, S. and Diekmann, B., 2010. Late Quaternary vegetation and environments in the Verkhoyansk Mountains region (NE Asia) reconstructed from a 50-kyr fossil pollen record from Lake Billyakh. Quaternary Science Reviews, 29(17-18), pp.2071-2086.doi:10.1016/j.quascirev.2010.04.024
NOVO-USP Neotoma2380041235Novo-Uspenka84.16666756.616667Asia150RawFen40AWI-0.0165.964Fen in the flood plain of Ob' river. Physiography: Flood plain. Surrounding vegetation: Pinus sylvestris, Betula pendula.Blyakharchuk, T.A., 1989. The Holocene history of vegetation of south-eastern West Siberia by botanical and pollen analyses of peat deposits. Doctoral dissertation. Tomsk State University, Tomsk, Russia (in Russian).
NIZHNIVA Neotoma2380141237Nizhnevartovsk76.66666762.000000Asia56RawRiver37AWI-0.06612.259Physiography: First terrace above flood-plain of river. Surrounding vegetation: Sphagnum bog.Neustadt, M.I., and E.M. Zelikson. 1971. Neue Angaben zur stratiraphie der Torfmoore Westsibiriens. Julkaisuaika, Acta Agralia fennica, 123, pp.27-32 (in German).
BAYANCH Neotoma2380541245Lake Bayanchagan115.22542541.632845Asia1355RawLake90AWI0.57811.644Lake Bayanchagan is a closed-basin lake situated on the northern edge of the summer Monsoon. The lake is almost totally dry, with patches of shallow water maintained by summer rain.The region is located in the transition zone between desert and steppe.Jiang, W., Guiot, J., Chu, G., Wu, H., Yuan, B., Hatte, C. and Guo, Z., 2010. An improved methodology of the modern analogues technique for palaeoclimate reconstruction in arid and semi-arid regions. Boreas, 39(1), pp.145-153.doi:10.1111/j.1502-3885.2009.00115.xJiang, W.Y. and Liu, T.S., 2007. Timing and spatial distribution of mid-Holocene drying over northern China: Response to a southeastward retreat of the East Asian Monsoon. Journal of Geophysical Research: Atmospheres, 112(D24).doi:10.1029/2007JD009050Jiang, W., Guo, Z., Sun, X., Wu, H., Chu, G., Yuan, B., Hatte, C. and Guiot, J., 2006. Reconstruction of climate and vegetation changes of Lake Bayanchagan (Inner Mongolia): Holocene variability of the East Asian monsoon. Quaternary Research, 65(3), pp.411-420.doi:10.1016/j.yqres.2005.10.007
TIANCHIYL Neotoma2380641247Lake Tianchi99.27974025.870850Asia2550RawLake53AWI0.23318.665Lake Tianchi is in the subalpine zone of the Hengduan Mountains, formerly dominated by Tsuga dumosa. Vegetation today is dominated by Pinus yunnanensis, accompanied by Castanopsis delavayi, Cyclobalanopsis delavayi, Alnus nepalensis, Celtis tetrandra, Sapindus delavayi, Pistacia chinensis, Quercus variabilis, Gleditsia delavayi and Docynia delavayi. At present, Tsuga dumosa is rare in the area due to human activity. The natural lake is currently submerged under Tianchi Reservoir.Jiang, W., Leroy, S.A., Yang, S., Zhang, E., Wang, L., Yang, X. and Rioual, P., 2019. Synchronous strengthening of the Indian and East Asian monsoons in response to global warming since the last deglaciation. Geophysical Research Letters, 46(7), pp.3944-3952.doi:10.1029/2019GL082084
K7/P2 Neotoma2380941252Dyanushka K7P2125.03694465.039444Asia123RawPeat75AWI-0.01512.658Permafrost peat. Physiography: Dyanushka River, flat plain. Surrounding vegetation: Open cold deciduous forests.Werner, K., Tarasov, P.E., Andreev, A.A., Muller, S., Kienast, F., Zech, M., Zech, W. and Diekmann, B., 2010. A 12.5-kyr history of vegetation dynamics and mire development with evidence of Younger Dryas larch presence in the Verkhoyansk Mountains, East Siberia, Russia. Boreas, 39(1), pp.56-68.doi:10.1111/j.1502-3885.2009.00116.x
FADEYEVS Neotoma2381141262Faddeyevskiy143.83333375.333333Asia30RawRiver8AWI26.29446.875Riverine. Physiography: River valley. Surrounding vegetation: Tundra.Andreev, A.A., Peteet, D.M., Tarasov, P.E., Romanenko, F.A., Filimonova, L.V. and Sulerzhitsky, L.D., 2001. Late Pleistocene Interstadial Environment on Faddeyevskiy Island, East-Siberian Sea, Russia. Arctic, Antarctic, and Alpine Research, 33(1), pp.28-35.doi:10.1080/15230430.2001.12003401
Nikolay Neotoma2381241264Nikolay Lake124.20000073.333333Asia35RawLake22AWI-0.05211.491Is the largest body of water in the Lena River Delta region and is situated in the northwestern part of Arga Island.The island is one of the major geomorphologic elements of the Lena Delta and is characterised by numerous lakes with a submeridional orientation of the long axis typifying lake depressions. Nikolay Lake consists of five subbasins and is about 8 km wide from east to west and about 6 km long from north to south. Approximately 70% of the lake basin has a water depth of less than 2 m. A maximum water depth of 30 m was recorded in one subbasin.Andreev, A.A., Tarasov, P.E., Schwamborn, G., Ilyashuk, B.I., Ilyashuk, E.A., Bobrov, A.A., Klimanov, V.A., Rachold, V. and Hubberten, H.W., 2004. Holocene paleoenvironmental records from Nikolay Lake, Lena river delta, arctic Russia. Palaeogeography, Palaeoclimatology, Palaeoecology, 209(1-4), pp.197-217.doi:10.1016/j.palaeo.2004.02.010
Barbarina_Tumsa Neotoma2387541397Barbarina Tumsa123.35000073.566667Asia10RawLake19AWI0.5606.788Lakes bordered by Laptev sea&Lena river. Physiography: Thermokarst origin. Surrounding vegetation: Tundra. Vegetation formation: Arctic climate.Andreev, A.A., Tarasov, P.E., Schwamborn, G., Ilyashuk, B.I, Ilyashuk, E.A., Bobrov, A.A., Klimanov, V.A., Rachold, V. and Hubberten, H.W., 2004. Holocene paleoenvironmental records from Nikolay Lake, Lena river delta, arctic Russia. Palaeogeography, Palaeoclimatology, Palaeoecology, 209(1-4), pp.197-217.doi:10.1016/j.palaeo.2004.02.010
TMGM2 Neotoma2417342417Gomishan54.05666737.151667Asia-26RawLake38AWI0.06810.889Salt marsh. Physiography: Dried lagoon, endorheing lake. Surrounding vegetation: Cultivated area.Leroy, S.A.G., Kakroodi, A.A., Kroonenberg, S., Lahijani, H.K., Alimohammadian, H. and Nigarov, A., 2013. Holocene vegetation history and sea level changes in the SE corner of the Caspian Sea: relevance to SW Asia climate. Quaternary Science Reviews, 70, pp.28-47.doi:10.1016/j.quascirev.2013.03.004
ALMALOU3 Neotoma2417542421Lake Almalou46.63194437.665278Asia2410RawLake53AWI0.0103.663Peat bog. Physiography: Volcanic crater wetland complex. Surrounding vegetation: Cultivated fields.Djamali, M., de Beaulieu, J.L., Andrieu-Ponel, V., Berberian, M., Miller, N.F., Gandouin, E., Lahijani, H., Shah-Hosseini, M., Ponel, P., Salimian, M. and Guiter, F., 2009. A late Holocene pollen record from Lake Almalou in NW Iran: evidence for changing land-use in relation to some historical events during the last 3700 years. Journal of Archaeological Science, 36(7), pp.1364-1375.doi:10.1016/j.jas.2009.01.022Djamali, M., Ponel, P., Andrieu-Ponel, V., de Beaulieu, J.L., Guibal, F., Miller, N.F., Ramezani, E., Berberian, M., Lahijani, H. and Lak, R., 2010. Notes on arboricultural and agricultural practices in ancient Iran based on new pollen evidence. Paleorient, pp.175-188.doi:10.3406/paleo.2010.5394
MAHARLOU Neotoma2417942539Maharlou Lake52.75972229.477222Asia1455RawLake67AWI0.2494.565Hypersaline lake. Physiography: Closed basin. Surrounding vegetation: Xeromorphic dwarf-shrub cultivated lands. Vegetation formation: Pistacia-Amygdalus open scrub.Djamali, M., De Beaulieu, J.L., Miller, N.F., Andrieu-Ponel, V., Ponel, P., Lak, R., Sadeddin, N., Akhani, H. and Fazeli, H., 2009. Vegetation history of the SE section of the Zagros Mountains during the last five millennia; a pollen record from the Maharlou Lake, Fars Province, Iran. Vegetation History and Archaeobotany, 18(2), pp.123-136.doi:10.1007/s00334-008-0178-2Djamali, M., Ponel, P., Andrieu-Ponel, V., de Beaulieu, J.L., Guibal, F., Miller, N.F., Ramezani, E., Berberian, M., Lahijani, H. and Lak, R., 2010. Notes on arboricultural and agricultural practices in ancient Iran based on new pollen evidence. Paleorient, pp.175-188.doi:10.3406/paleo.2010.5394
GS18 Neotoma2601645092GS1851.10111141.548056Asia-479RawMarine114AWI2.45415.268Marine. Physiography: Basin. Vegetation formation: Irano-Turanian area.Leroy, S.A.G., Lopez-Merino, L., Tudryn, A., Chalie, F. and Gasse, F., 2014. Late Pleistocene and Holocene palaeoenvironments in and around the middle Caspian basin as reconstructed from a deep-sea core. Quaternary Science Reviews, 101, pp.91-110.doi:10.1016/j.quascirev.2014.07.011
LL13 Neotoma2602645111Langarud50.14750037.185556Asia-22RawPeat15AWI-0.0530.601Coastal wetland. Physiography: Depression. Surrounding vegetation: Agricultural land.Haghani, S., Leroy, S.A., Khdir, S., Kabiri, K., Naderi Beni, A. and Lahijani, H.A.K., 2016. An early 'Little Ice Age'brackish water invasion along the south coast of the Caspian Sea (sediment of Langarud wetland) and its wider impacts on environment and people. The Holocene, 26(1), pp.3-16.doi:10.1177/0959683615596835
KBG801 Neotoma2604345164Kara-Bogaz Gol53.25000041.850000Asia-29RawLake17AWI-0.0530.128Coastal black throat lake. Physiography: Bay.Leroy, S.A.G., Marret, F., Giralt, S. and Bulatov, S.A., 2006. Natural and anthropogenic rapid changes in the Kara-Bogaz Gol over the last two centuries reconstructed from palynological analyses and a comparison to instrumental records. Quaternary International, 150(1), pp.52-70.doi:10.1016/j.quaint.2006.01.007
BAIKA2 Neotoma2656246449Baika46.75513061.268400Asia44RawPeat33AWI-0.00510.551Floodplain of Vychegda river mouth. Physiography: basin in plain. Surrounding vegetation: spuce forest with birch.Sidorchuk, A.Y., A.V. Panin, O.K. Borisova, and N.N. Kovalyukh. 2001. Late-glacial and Holocene palaeohydrology of the lower Vychegda river, western Russia. In: River Basin Sediment Systems: Archives of Environmental Change ed by D. Maddy, M.G. Macklin, and J.C. Woodward (pp.265-295). Balkema, Rotterdam.Borisova, O.K., 2002. The Holocene flora and vegetation of the northern Russian Plain (the Vychegda River basin). Gu Sheng wu xue bao= Acta Palaeontologica Sinica, 41(4), pp.478-486 (in Chinese).
KHARINEI Neotoma2658146488Lake Kharinei62.75000067.366667Asia110RawLake100AWI0.03111.186Lake. Physiography: depression in Pechora river basin. Surrounding vegetation: forest-tundra.Salonen, J.S., Seppa, H., Valiranta, M., Jones, V.J., Self, A., Heikkila, M., Kultti, S. and Yang, H., 2011. The Holocene thermal maximum and late-Holocene cooling in the tundra of NE European Russia. Quaternary Research, 75(3), pp.501-511.doi:10.1016/j.yqres.2011.01.007
Khorpiya Neotoma2658346492Khorpyia60.05000061.033333Asia120RawPeat52AWI0.2415.200Peat bog. Physiography: floodplain of Loz'va river. Surrounding vegetation: larch, birch & pine taiga.Antipina, T.G., Panova, N.K. and Korona, O.M., 2014. The holocene dynamics of vegetation and environmental conditions on the eastern slope of the Northern Urals. Russian journal of ecology, 45(5), pp.351-358.doi:10.1134/S1067413614050026
KHARTYM Neotoma2658846512Man'inskii Khartym60.90000064.383333Asia112RawPeat40AWI2.3646.649Peat bog. Physiography: Floodplain of Man'ya River. Surrounding vegetation: Scots pine, stone pine & dwarf birch.Antipina, T.G. and Panova, N.K., 2016. The Holocene dynamics of vegetation and climatic conditions on the eastern slope of the Subpolar Urals. Russian journal of ecology, 47(4), pp.329-337.doi:10.1134/S1067413616040056
MOKHOVOE Neotoma170446523Mokhovoye64.25000053.766667Asia178RawPeat33AWI-0.0516.635Carex/Phragmites fen. Physiography: Undulating plain. Vegetation formation: Steppe.Kremenetsky, K.V., Tarasov, P.E. and Cherkinsky, A.E., 1994. Holocene history of the Kazakhsta ''island'' pine forests. Botaniceskij zurnal, 79(3), pp.13-29 (in Czech).Kremenetski, C., Tarasov, P. and Cherkinsky, A., 1997. Postglacial development of Kazakhstan pine forests. Geographie physique et Quaternaire, 51(3), pp.391-404.doi:10.7202/033138arTarasov, P.E. and Kremenetskii, K.V., 1995. Geochronology and stratigraphy of the Holocene lacustrine-bog deposits in northern and central Kazakhstan. Stratigraphy and Geological Correlation, 3(1), pp.73-80.
KARAKOL Neotoma2707047663Karakol77.39250042.838889Asia2353RawLake75AWI-0.0133.926Subalpine lake with an outlet on the eastern shore. Picea schrenkiana dense stands on north-, east- and west-facing slopes. Pastures and meadows around the lake.Beer, R. and Tinner, W., 2008. Four thousand years of vegetation and fire history in the spruce forests of northern Kyrgyzstan (Kungey Alatau, Central Asia). Vegetation History and Archaeobotany, 17(6), pp.629-638.doi:10.1007/s00334-008-0142-1
KICHIKOL Neotoma2707247669Kichikol73.55193039.987670Asia2541RawLake75AWI0.0386.201Unclear origin. Fed by groundwater and no major inlets or outlets. Juniperus semiglobosa stands, pastures and meadows.Beer, R., Heiri, O. and Tinner, W., 2007. Vegetation history, fire history and lake development recorded for 6300 years by pollen, charcoal, loss on ignition and chironomids at a small lake in southern Kyrgyzstan (Alay Range, Central Asia). The Holocene, 17(7), pp.977-985.doi:10.1177/0959683607082413
BAKALY_neotoma Neotoma2707347671Bakaly71.96008041.867340Asia1859RawLake93AWI-0.0336.891Open woodlands of Juniperus turkestanica, Juniperus semiglobosa, Picea schrenkiana, Abies semenovii, Juglans regia, Acer turkestanicum, Betula pubescens, Malus kirghisorum, Prunus spp. and Crataegus spp.Beer, R., Kaiser, F., Schmidt, K., Ammann, B., Carraro, G., Grisa, E. and Tinner, W., 2008. Vegetation history of the walnut forests in Kyrgyzstan (Central Asia): natural or anthropogenic origin?. Quaternary Science Reviews, 27(5-6), pp.621-632.doi:10.1016/j.quascirev.2007.11.012
NIZHNEE Neotoma2707447673Nizhnee72.96399041.309350Asia1371RawLake58AWI-0.0041.508No major inlet or outlet. Rather dense forest stands dominated by Juglans regia.Beer, R., Kaiser, F., Schmidt, K., Ammann, B., Carraro, G., Grisa, E. and Tinner, W., 2008. Vegetation history of the walnut forests in Kyrgyzstan (Central Asia): natural or anthropogenic origin?. Quaternary Science Reviews, 27(5-6), pp.621-632.doi:10.1016/j.quascirev.2007.11.012
VERKHNEE Neotoma2708147681Verkhnee72.95762041.309120Asia1440RawLake74AWI-0.0161.532No major inlet or outlet. Rather dense forest stands dominated by Juglans regia.Beer, R., Kaiser, F., Schmidt, K., Ammann, B., Carraro, G., Grisa, E. and Tinner, W., 2008. Vegetation history of the walnut forests in Kyrgyzstan (Central Asia): natural or anthropogenic origin?. Quaternary Science Reviews, 27(5-6), pp.621-632.doi:10.1016/j.quascirev.2007.11.012
AKTEREK Neotoma2708247683Ak Terek72.83431041.281500Asia1748RawMire18AWI-0.0337.644Sloping mire close to a village surrounded by forests and plantations of Juglans regia.Beer, R., Kaiser, F., Schmidt, K., Ammann, B., Carraro, G., Grisa, E. and Tinner, W., 2008. Vegetation history of the walnut forests in Kyrgyzstan (Central Asia): natural or anthropogenic origin?. Quaternary Science Reviews, 27(5-6), pp.621-632.doi:10.1016/j.quascirev.2007.11.012
ORTOK_neotoma Neotoma2708347685Ortok73.26452041.245650Asia1786RawLake24AWI-0.0310.854Lake in transition into a mire. A mat 50-100 cm thick of Phragmites and Telypteris roots cover the lake surface. The depth reported is beneath the root mat. North-facing slope: Juglans regia and Malus kirghisorum forest. South-facing slope: Acer turkestanicum and Crataegus are important.Beer, R., Kaiser, F., Schmidt, K., Ammann, B., Carraro, G., Grisa, E. and Tinner, W., 2008. Vegetation history of the walnut forests in Kyrgyzstan (Central Asia): natural or anthropogenic origin?. Quaternary Science Reviews, 27(5-6), pp.621-632.doi:10.1016/j.quascirev.2007.11.012
WENQUAN1 Neotoma2715647817Wenquan wetland81.03134044.973730Asia1300RawPeat89AWI-0.02410.296The study area is the Bortala River National Wetland Park which is situated in Wenquan County in the Tien Shan Mountains, Xinjiang Autonomous Region, Northwest China. The wetland covers a surface area of about 3840 ha. The mean values of annual temperature and precipitation at the meteorological station of Wenquan County are 3.9 C and 225 mm, respectively. The region has a typical arid continental climate dominated primarily by the mid-latitude westerly circulation.Li, J. and Wang, N., 2020. Holocene grassland fire dynamics and forcing factors in continental interior of China. Geophysical Research Letters, 47(13), p.e2020GL088049.doi:10.1029/2020GL088049
CHAOCH1 Cao et al.1100001Chaohu Lake CH1117.39433331.562333Asia10RawLake98AWI0.00211.248NAWu, L., Wang, X.Y., Zhang, G.S. and Xiao, X.Y., 2008. Vegetation evolution and climate change since the Holocene recorded by pollen-charcoal assemblages from lacustrine sediments of Chaohu Lake in Anhui Province. Journal of Palaeogeography, 10(2), pp.183-192 (in Chinese).
LONGGAN Cao et al.2100002Longgan Lake116.11666729.966667Asia31DigitizedLake72AWI-0.0423.428NATong, G.B., Shi, Y., Wu, R.J., Yang, X.D. and Qu, W.C., 1997. Vegetation and climatic quantitative reconstruction of Longgan Lake since the past 3000 years. Marine Geology and Quaternary Geology, 17(2), pp.53-61 (in Chinese).
DONGGAN Cao et al.3100003Dongganchi115.78333339.533333Asia49RawFluvial190AWI1.09719.049NAZhang, J.H., Kong, Z.C. and Du, N.Q., 1997. An analysis of different sedimentary environment influence on pollen deposit in Beijing. Acta Sedimentologica Sinica, 15(suppl.), pp.57-63 (in Chinese).Zhang, J.H., Kong, Z.C. and Du, N.Q., 1999. Vegetation and environmental changes in the Fangshan area of Beijing from 16000-7000 Years B.P. Acta Micropalaeontologica Sinica, 16(4), pp.421-430 (in Chinese).
FENZHU Cao et al.4100004Fenzhuang115.90000039.566667Asia49RawFluvial53AWI11.79820.302NAZhang, J.H., Kong, Z.C. and Du, N.Q., 1997. An analysis of different sedimentary environment influence on pollen deposit in Beijing. Acta Sedimentologica Sinica, 15(suppl.), pp.57-63 (in Chinese).
MAWEI32 Cao et al.5100005Mawei ZK32119.63333326.050000Asia7DigitizedCoast32AWI0.58610.082NAWu, X.Z., 1993. Holocene sporopollen assemblage in Mawei, Fuzhou City and their geological significance. Geology of Fujian, 12(6), pp.292-299 (in Chinese).
DADIWAN07 Cao et al.6100006Dadiwan_2007105.91483335.000000Asia1400RawLoess166AWI0.02215.201NATang, L.Y., Li, C.H., An, C.B. and Wang, W.G., 2007. Vegetation history of the western Loess Plateau of China during the last 40ka based on pollen record. Acta Palaeontologica Sinica, 46(1), pp.45-61 (in Chinese).
DADIWAN08 Cao et al.7100007Dadiwan_2008105.91466735.013000Asia1471RawLoess130AWI0.06013.056NASun, A.Z., Feng, Z.D., Tang, L.Y. and Ma, Y.Z., 2008. Vegetation and climate changes in the western part of the Loess Plateau since 13 ka BP. Acta Geographica SInica, 63(3), pp.280-292 (in Chinese).
DINGXI Cao et al.8100008Dingxi104.60933335.548167Asia1750RawPaleosol25AWI0.1453.877NATang, L.Y., Li, C.H., An, C.B. and Wang, W.G., 2007. Vegetation history of the western Loess Plateau of China during the last 40ka based on pollen record. Acta Palaeontologica Sinica, 46(1), pp.45-61 (in Chinese).
LANZHOU Cao et al.11100011Lanzhou103.85000036.066667Asia2000RawFluvial12AWI0.25511.482NAWang, S.L., Chen, F.H. and Cao, J.X., 1991. The pollen assemblage and climate fluctuations in Lanzhou River Basin since 10000 aB.P. Journal of Glaciology and Geocryology, 13(4), pp.307-314 (in Chinese).
MAYING Cao et al.12100012Maying104.98983335.338333Asia1800DigitizedPaleosol30AWI-0.0618.852NATang, L.Y., Li, C.H., An, C.B. and Wang, W.G., 2007. Vegetation history of the western Loess Plateau of China during the last 40ka based on pollen record. Acta Palaeontologica Sinica, 46(1), pp.45-61 (in Chinese).
SANJIAO Cao et al.13100013Sanjiaocheng103.33750039.006333Asia1320DigitizedLake43AWI7.19511.457NAZhu, Y., Chen, F. and David, M., 2002. The environmental signal of an early Holocene pollen record from the Shiyang River basin lake sediments, NW China. Chinese Science Bulletin, 47(4), pp.267-273.doi:10.1360/02tb9065Zhu, Y., Ju, T.Z., Chen, F.H.and Zhang, J.W., 2001. Vegetation and environmental changes based on high resolution pollen records in Shiyang River basin, arid lands NW China during early Holocene. Acta Botanica Boreali-Occidentalia Sinica, 21(6), pp.1059-1069 (in Chinese).
SUANFENG Cao et al.14100014Suancigou_Feng105.81000035.510000Asia1840DigitizedLoess34Cao et al.11.45047.500NAFeng, Z.D., Tang, L.Y., Ma, Y.Z., Zhai, Z.X., Wu, H.N., Li, F., Zou, S.B., Yang, Q.L., Wang, W.G., Derbyshire, E. and Liu, K.B., 2007. Vegetation variations and associated environmental changes during marine isotope stage 3 in the western part of the Chinese Loess Plateau. Palaeogeography, Palaeoclimatology, Palaeoecology, 246(2-4), pp.278-291.doi:10.1016/j.palaeo.2006.10.004
SUANTANG Cao et al.15100015Suancigou_Tang105.83333335.500000Asia1850DigitizedLoess211AWI14.62750.586NATang, L.Y., Li, C.H., An, C.B. and Wang, W.G., 2007. Vegetation history of the western Loess Plateau of China during the last 40ka based on pollen record. Acta Palaeontologica Sinica, 46(1), pp.45-61 (in Chinese).
SUJIA06 Cao et al.16100016Sujiawan_2006104.52283335.538833Asia1950DigitizedLoess44AWI0.48114.378NAFeng, Z.D., Tang, L.Y., Wang, H.B., Ma, Y.Z. and Liu, K.B., 2006. Holocene vegetation variations and the associated environmental changes in the western part of the Chinese Loess Plateau. Palaeogeography, Palaeoclimatology, Palaeoecology, 241(3-4), pp.440-456.doi:10.1016/j.palaeo.2006.04.009
HONGSHU03 Cao et al.17100017Hongshui River_2003102.76500038.179400Asia1452DigitizedFluvial31AWI10.12724.843NAMa, Y.Z., Zhang, H.C., Pachur, H.G.,Wunnemann, B., Li, J.J., Feng, Z.D., 2003. Late Glacial and Holocene vegetation history and paleoclimate of the Tengger Desert, northwestern China. Chinese Science Bulletin, 48(14), pp.1457-1463.doi:10.1360/02wd0274
WUYING Cao et al.18100018Wuying River105.82000035.760000Asia1400DigitizedLoess43AWI-0.04511.470NAXia, D.S., Ma, Y.Z., Chen, F.H. and Wang, J.M., 1998. High-resolution vegetation and climate variations in Longxi Loess Plateau during Holocene. Journal of Lanzhou University (Natural Sciences), 34(1), pp.119-127 (in Chinese).
ZOIGERM Cao et al.19100019Zoige RM102.35000033.950000Asia3401RawPeat48AWI-0.05913.546NASheng, C.M., Tang, L.Y. and Wang, S.M., 1996. Vegetation and climate during the past 250000 years in Zoige Region. Acta Micropalaeontologica Sinica, 13(4), pp.373-385 (in Chinese).Sheng, C.M., Tang, L.Y. and Wang, S.M., 1996. Vegetation and climate during the past 22000 years in Zoige Region. Acta Micropalaeontologica Sinica, 13(4), pp.401-406 (in Chinese).
CHENGCH2 Cao et al.20100020Chenghai CH2116.80000023.483333Asia5RawPeat43AWI4.22960.853NAZheng, Z., 1990. Holocene pollen flora and paleoenvironment in Chaoshan Plain. Tropical Oceanography, 9(2), pp.31-38 (in Chinese).Zheng, Z., 1991. Pollen flora and paleoclimate of the Chao-Shan Plains during the last 50000 years. Acta Micropalaeontologica Sinica, 8(4), pp.461-480 (in Chinese).
DONGGUPK16 Cao et al.21100021Dongguan_PK16113.71666722.733333Asia15RawPeat8AWI1.69922.036NAZhang, Z.Y., Huang, Z.G., Li, P.R., Li, K.H. and He, R.R., 1982. Climate changes in the Zhujiang Delta region since Late Pleistocene based on sporo-pollen analysis. Tropic Geography, 1, pp.21-28 (in Chinese).
HUANGH24 Cao et al.22100022Huangsha H24113.23333323.133333Asia40RawDelta26AWI0.84213.428NALi, P.R., Fang, G.X. and Huang, G.Q., 1991. Environmental evolution in Zhujiang Delta during Holocene. Quaternary Sciences, (2), pp.130-138 (in Chinese).Li, P.R., 1991. Climate changes reflected by spore-pollen in Guangzhou area in the past 2000 years. Tropic Geography, 11(1), pp.16-24 (in Chinese).
LINGDINGL2 Cao et al.24100024Lingdingyang L2113.81666722.350000Asia-3RawMarine10AWI2.12840.478NAChen, M.H., Zhao, H.T., Wen, X.S., Zhang, Q.M. and Song, C.J., 1994. Quaternary foraminiferal group and sporopollen zones in cores L2 and L16 in the Lingdingyang Estuary. Marine Geology and Quaternary Geology, 14(1), pp.11-22 (in Chinese).
SHANTSH5 Cao et al.25100025Shantou SH5116.66666723.450000Asia8RawDelta33AWI4.33512.088NAZheng, Z., 1990. Holocene pollen flora and paleoenvironment in Chaoshan Plain. Tropical Oceanography, 9(2), pp.31-38 (in Chinese).Zheng, Z., 1991. Pollen flora and paleoclimate of the Chao-Shan Plains during the last 50000 years. Acta Micropalaeontologica Sinica, 8(4), pp.461-480 (in Chinese).
SHUIDOA1 Cao et al.26100026Shuidong A1111.66666721.550000Asia-9RawMarine10AWI0.1836.551NAShi, Y.F. and Yu. G., 2003. Warm-humid climate and transgressions during 40-30 ka B.P. and their potential mechanisms. Quaternary Sciences, 23(1), pp.1-11 (in Chinese).Zheng, Z., 1990. Holocene pollen flora and paleoenvironment in Chaoshan Plain. Tropical Oceanography, 9(2), pp.31-38 (in Chinese).Zheng, Z., 1991. Pollen flora and paleoclimate of the Chao-Shan Plains during the last 50000 years. Acta Micropalaeontologica Sinica, 8(4), pp.461-480 (in Chinese).
SHUNDEZK08 Cao et al.27100027Shunde ZK08113.25000022.833333Asia4DigitizedDelta8AWI0.28818.910NASheng, C.M., Wang, K.F. and Chen, P.H., 1989. Late Quaternary palynological assemblages in the Zhujiang (Pearl) River Delta. Tropic Oceanology, 8(4), pp.61-69 (in Chinese).
TIANYANTY1 Cao et al.28100028Tianyang TY1110.35000020.350000Asia90RawLake55AWI2.90485.071NALei, Z.Q. and Zheng, Z., 1993. Quaternary sporo-pollen flora and paleoclimate of the Tianyang volcanic lake basin, Leizhou Peninsula. Acta Botanica Sinica, 35(suppl.), pp.128-138 (in Chinese).
ZHONGPK19 Cao et al.29100029Zhongshan PK19113.30000021.800000Asia6RawDelta10AWI0.99543.573NAHuang, Z.G., Li, P.R., Zhang, Z.Y., Li, K.H. and Qiao, P.N., 1982. Generation, Development and Evolution of the Zhujiang River Delta. Guangzhou Popular Science Press, Guangzhou.
BAJIAO Cao et al.30100030Bajiaotian110.20000025.200000Asia1800RawPeat27AWI0.60210.562NALi, W.Y., Liu, G.X., Xu, Q.H, and Liang, Y.L., 1993. Forest vegetational history and environmental change in Bajiaotian, Miaoer Mountain. In: Vegetation and Environment of Late Quaternary in Northern and Middle Subtropics of China (pp.121-132). China Ocean Press, Beijing.
BEIHAIGK10 Cao et al.31100031Beihai GK10109.08333321.533333Asia-2DigitizedLake30AWI0.36210.399NALi, G.Z., Liang, W., Liao, S.M. and Fang, G.X., 1996. Climatic changes since Holocene along Guangxi coast. Marine Geology and Quaternary Geology, 16(3), pp.49-60 (in Chinese).Zhang, G.W., Yang, Z.G., Wang, S.J.,1996. Characteristics of surface textures of Quaternary quartz sand in the south Yellow Sea and environmental significance. Marine Geology and Quaternary Geology, 16(3), pp.37-47 (in Chinese).
NANTUN Cao et al.34100034Nantun104.23333326.700000Asia2197DigitizedLake70AWI0.23813.352NAChen, P.Y., Zhou, Q.Y. and Lin, S.J., 1991. Palaeoenvironment from 15000 aB.P. to the present in Weining County, Guizhou: A study of Nantun peat-bed section. Geology of Guizhou, 8(2), pp.141-152 (in Chinese).
SUOMA Cao et al.35100035Suoma105.83333326.033333Asia1085RawFluvial12AWI-0.05410.542NALei, G.L., 1990. A record of climate and environmental changes of Holocene Epoch in western Guizhou based on pollen analysis. Guizhou Science, 8(4), pp.41-51 (in Chinese).
XIAOHE Cao et al.36100036Xiaoheitu105.91666726.233333Asia1384DigitizedPeat71AWI11.76928.794NAChen, P.Y., Zhou, Q.Y., Lin, S.J., Qiao, Y.L. and Sun, Y.M., 1994. The late Pleistocene palaeovegetation and palaeoclimate of Xiaoheitu, Anshun, Guizhou. Guizhou Science, 12(2), pp.24-31 (in Chinese).
SHUANGSC1 Cao et al.39100039Shuangchi Maar Lake SC1110.18333319.950000Asia90DigitizedLake43AWI-0.0438.198NAZheng, Z., Wang, J., Wang, B., Liu, C., Zou, H., Zhang, H., Deng, Y. and Bai, Y., 2003. High-resolution records of Holocene from the Shuangchi Maar lake in Hainan Island. Chinese Science Bulletin, 48(5), pp.497-502.doi:10.1007/BF03183259
BAIHE Cao et al.40100040Baihe115.85000040.866667Asia865RawFluvial15AWI0.5562.299NAXu, Q.H. and Yang, X.L. 1998. Ancient vegetation interpreted by alluvial pollen at northern mountain area of Hebei Province. Scientia Geographica Sinica, 18(5), pp.486-492 (in Chinese).
BAIYANGGY Cao et al.41100041Baiyangdian Lake GY115.91666738.833333Asia10RawLake20AWI0.0839.696NAGuang, X.J., Xu, Q.H., Yang, X.L. and Sun, L.M., 2000. Younger Dryas record from North China Plain sediments. Yunnan Geographic Environment Research, 12(1), pp.21-29 (in Chinese).
CANGUMI Cao et al.42100042Cangumiao118.60000038.966667Asia70DigitizedPeat34AWI-0.0495.289NAXu, Q.H., Yang, X.L., Yang, Z.J., Liang, W.D. and Sun, L.M., 2004. Reconstruction of climatic changes of Yanshan Mountain area since 5000 aB.P. inferred from pollen data. Scientia Geographica Sinica, 24(3), pp.339-345 (in Chinese).Xu, Q.H., Kong, Z.C., Yang, X.L., Liang, W.D. and Sun, L.M., 2002. Vegetation changes and human influences on Qianan Basin since the Middle Holocene. Acta Botanica Sinica, 44(5), pp.611-616 (in Chinese).
DAZIYIN Cao et al.43100043Daziying119.17000039.333333Asia50RawPeat9AWI8.38711.026NALi, W.Y. and Liang, Y.L., 1985. Vegetation and environment of the hypsithermal interval of Holocene in eastern Hebei Plain. Acta Botanica Sinica, 27(6), pp.640-651 (in Chinese).
FENGNIN Cao et al.44100044Fengning116.63333341.200000Asia645DigitizedFluvial22AWI-0.0601.947NAXu, Q.H., Yang, X.L. and Yang, Z.J., 2004. Relationship between pollen assemblages and vegetation in alluvial sediments of Luanhe River Basin. Journal of Palaeogrography, 6(1), pp.69-77 (in Chinese).Xu, Q.H. and Yang, X.L., 1998. Ancient vegetation interpreted by alluvial pollen at northern mountain area of Hebei Province. Scientia Geographica Sinica, 18(5), pp.486-492 (in Chinese).
HUANGJI Cao et al.45100045Huangjiapu115.15000040.566667Asia500DigitizedFluvial28AWI-0.05816.716NASun, L.M., Xu, Q.H., Yang, X.L., Liang, W.D. and Kong, Z.C., 2001. Vegetation and environmental changes in the Xuanhua Basin of Hebei Province since postglacial. Journal of Geomechanics, 7(4), pp.303-308 (in Chinese).
MAOHEBE Cao et al.46100046Maohebei119.17000039.500000Asia50RawPeat23AWI1.40812.030NALi, W.Y. and Liang, Y.L., 1985. Vegetation and environment of the hypsithermal interval of Holocene in eastern Hebei Plain. Acta Botanica Sinica, 27(6), pp.640-651 (in Chinese).
MENGCUN Cao et al.47100047Mengcun117.11666738.050000Asia5RawCoast38AWI0.77328.088NAXu, Q.H., Wu, C., Wang, Z.H., Tong, G.B., Wu, S.J., Zhang, J.P., Du, N.Q. and Kong, Z.C., 1993. Approach to palaeo-environment in the west coast of Bohai Bay since 25000 a.B.P. Acta Phytoecologica et Geobotanica Sinica, 17(1), pp.20-32 (in Chinese).
NANWANG Cao et al.48100048Nanwangzhuang114.91666738.450000Asia24DigitizedFluvial41AWI0.1382.683NAGuo, S.Q., Shi, Y., Yang, L.J., Cao, J.D., Zhang, W.Q., Zhang, J., Lin, F. and He, JX., 1999. A study of paleoclimatic fluctuations in the last 2600 years in the Ningjin Lake area, Hebei Province. Journal of Geomechanics, 5(4), pp.73-79 (in Chinese).
YANGERZ Cao et al.50100050Yangerzhuang117.35000038.350000Asia5RawCoast50AWI0.64930.473NAXu, Q.H., Wu, C., Wang, Z.H., Tong, G.B., Wu, S.J., Zhang, J.P., Du, N.Q. and Kong, Z.C., 1993. Approach to palaeo-environment in the west coast of Bohai Bay since 25000 a.B.P. Acta Phytoecologica et Geobotanica Sinica, 17(1), pp.20-32 (in Chinese).
YANGJIA Cao et al.51100051Yangjiapo118.68333340.016667Asia70DigitizedFluvial13AWI11.51729.934NAXu, Q.H., Yang, X.L., Ke, Z.M., Liang, W.D. and Yang, Z.J., 2002. Environment changes in Yanshan Mountain area during the latest Pleistocene. Geography and Territorial Research, 18(2), pp.69-72 (in Chinese).
YANGYUANCA Cao et al.52100052Yangyuan-Caocun, Yangyuan County, Hebei Province114.40000040.100000Asia875DigitizedPaleosol48AWI3.01564.518NAWang, Y., Wang, S.B., Jiang, F.C., Tong, G.B. and Zhao, Z.Z., 2003. Characteristics of a sporo-pollen assemblage in the section of Caocun, Yangyuan, Hebei, and its paleoclimatic significance. Geological Bulletin of China, 22(9), pp.665-669 (in Chinese).
YANGYUANXI Cao et al.53100053Yangyuan-Xipu114.21666740.116667Asia912DigitizedPaleosol7AWI0.16019.232NAWang, Y., Wang, S.B., Jiang, F.C., Tong, G.B., 2003. Palynological Records in Xipu Section,Yangyuan. Journal of Geomechanics, 9(2), pp.171-175 (in Chinese).
YANSHEN Cao et al.54100054Yanshengang118.86666739.866667Asia23DigitizedFluvial38AWI2.51013.531NAKong, Z.C., Xu, Q.H., Yang, X.L., Sun, L.M. and Liang, W.D., 2000. Saptial and temporal Holocene vegetation change from alluvium pollen analysis in the Yinma River Basin of Hebei Province. Acta Phytoecologica Sinica, 24(6), pp.724-730 (in Chinese).
BEIDAWA Cao et al.55100055Beidawan134.70000048.133333Asia60RawPeat14AWI0.5426.217NAXia, Y.M., 1988. Preliminary study on vegetational development and climatic changes in the Sanjiang Plain in the last 12000 years. Scientia Geographica Sinica, 8(3), pp.240-249 (in Chinese).
CHUANGY Cao et al.56100056Chuangye134.46666748.333333Asia50RawPeat27AWI1.06813.781NAXia, Y.M., 1988. Preliminary study on vegetational development and climatic changes in the Sanjiang Plain in the last 12000 years. Scientia Geographica Sinica, 8(3), pp.240-249 (in Chinese).
MINZHU Cao et al.57100057Minzhuqiao133.86666747.533333Asia52RawPeat15AWI0.4966.733NAXia, Y.M., 1988. Preliminary study on vegetational development and climatic changes in the Sanjiang Plain in the last 12000 years. Scientia Geographica Sinica, 8(3), pp.240-249 (in Chinese).
QINDEL Cao et al.58100058Qindeli133.66666747.883333Asia52RawPeat35AWI0.46614.104NAXia, Y.M., 1988. Preliminary study on vegetational development and climatic changes in the Sanjiang Plain in the last 12000 years. Scientia Geographica Sinica, 8(3), pp.240-249 (in Chinese).Xia, Y.M., 1992. Climatic and environmental conditions of Holocene Hypsithermal in Sanjiang Plain. In: The Climates and Environments of Holocene Megathermal in China (pp.19-24). China Ocean Press, Beijing.
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TUQIANG Cao et al.61100061Tuqiang122.80000052.233333Asia400RawPeat19AWI0.5822.781NAXia, Y.M., 1996. Study on record of spore-pollen in high moor peat and development and successive process of peat in Da and Xiao Hinggan Mountains. Scientia Geographica Sinica, 16(4), pp.337-344 (in Chinese).
CHADIAN Cao et al.63100063Chadianpo114.40000036.100000Asia65DigitizedPaleosol23AWI3.3777.583NAZhang, Z.Q., Xu, Q.H., Li, Y.C., Yang, X.L., Jing, Z.C. and Tang, J.G., 2007. Environmental change of the Yin ruins area based on pollen analysis. Quaternary Research, 27(3), pp.461-468 (in Chinese).
DENGJIAC Cao et al.64100064Dengjiacun113.65000034.468933Asia133DigitizedFluvial33AWI1.22418.141NAZhang, Z.Y., Zhou, K.S., Yang, R.X., Zhang, S.L., Cai, Q.F., Lu, P., Hao, L.M. and Wang, C., 2007. Environmental archaeology in the Shuangji River basin. Quaternary Research, 27(3), pp.453-460 (in Chinese).
GUANGRU1 Cao et al.65100065Guangrunpo 1114.53333336.016667Asia56DigitizedPaleosol25AWI3.4417.670NAZhang, Z.Q., Xu, Q.H., Li, Y.C., Yang, X.L., Jing, Z.C. and Tang, J.G., 2007. Environmental change of the Yin ruins area based on pollen analysis. Quaternary Research, 27(3), pp.461-468 (in Chinese).
WANGJIAD Cao et al.66100066Wangjiadian profile114.66916736.161000Asia67RawPaleosol99AWI3.40512.027NACao, X., Xu, Q., Jing, Z., Tang, J., Li, Y. and Tian, F., 2010. Holocene climate change and human impacts implied from the pollen records in Anyang, central China. Quaternary International, 227(1), pp.3-9.doi:10.1016/j.quaint.2010.03.019
XISHAN Cao et al.67100067Xishan113.53000034.911667Asia141DigitizedLoess36AWI1.4488.130NAWang, X.L., He, Y., Jia, T.F. and Li, R.Q., 2004. Living environment of ancient man since 7000 a B.P. at Xishan Relic Site of Zhengzhou in Henan Province. Journal of Palaeogeography, 6(2), pp.234-240 (in Chinese).
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JIANGLING Cao et al.69100069Jiangling112.33333330.133333Asia30DigitizedFluvial52AWI0.4129.463NAXie, Y.Y., Li, C.A., Wang, Q.L. and Yin, H.F., 2008. Palynological records of early human activities in Holocene at Jiangling area, Hubei Province. Scientia Geographica Sinica, 28(2), pp.276-281 (in Chinese).
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MIANCHEM1 Cao et al.71100071Miancheng M1113.21666730.183333Asia24RawLake174AWI0.68214.522NAYang, X.D., Zhu, Y.X., Jiang, X.Z., Wu, Y.H. and Wang, S.M., 1998. Environmental changes from spore-pollen record of Mianyang region over the past 10000 years. Journal of Lake Sciences, 10(2), pp.23-29 (in Chinese).Zhu,Y.X., Wang, S.M., Yang, X.D. and Wu, R.J., 1999. Lake sediment records of human activity in Mid-Late Holocene at Miancheng area, Jianghan Plain. Journal of Lake Sciences, 11(1), pp.33-39 (in Chinese).
TAIBAITN1 Cao et al.72100072Taibai Lake TN1115.80733329.995667Asia44DigitizedLake120AWI-0.0611.398NATong, X.F., Xiao, X.Y., Yang, X.D., Wang, S.M. and Xiao, J.Y., 2009. Climatic changes and human activities revealed by pollen records in Lake Taibai, Hubei Province, the middle and lower reaches of the Yangtze River region over the past 1500 years. Journal of Lake Science, 21(5), pp.732-740 (in Chinese).
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ANGUNUR Cao et al.74100074Anguli Nur Lake114.36666741.333333Asia1000RawLake9AWI10.36924.727NALi R.Q., Zheng L.M. and Zhu G.R., 1990. Lakes and Environmental Change in the Inner Mongolian Plateau. Beijing Normal University Press, Beijing.
BAAHNUUR Cao et al.75100075Baahar Nuur Lake109.26666739.316667Asia1278DigitizedLake77AWI-0.0525.529NAHuang, C.Q., Feng, Z.D., Ma, Y.Z., Guo, L.L. and Wang, W., 2009. Holocene palaeoenvironment changes recorded by pollen of Baahar Nuur Lake. Journal of Lanzhou University (Natural Sciences), 45(1), pp.7-12. (in Chinese).
BAYANBY Cao et al.76100076Bayanchagan Lake BY115.21000041.650000Asia1355DigitizedLake45AWI0.97511.806NAJiang, W., Guo, Z., Sun, X., Wu, H., Chu, G., Yuan, B., Hatte, C. and Guiot, J., 2006. Reconstruction of climate and vegetation changes of Lake Bayanchagan (Inner Mongolia): Holocene variability of the East Asian monsoon. Quaternary Research, 65(3), pp.411-420.doi:10.1016/j.yqres.2005.10.007
CHARIMUCH Cao et al.77100077Charisu/Muchang profile122.35000042.950000Asia249DigitizedPeat31AWI-0.0675.790NALi, Y.H., Yin, H.N., Zhang, X.Y.and Chen, Z.J., 2003. The environment disaster events and the evolution of man-land relation in the west Liaoning during 5000 aBP. Journal of Glaciology and Geocryology 25(1), pp.19-26 (in Chinese).
CHIFEQIGU Cao et al.78100078Chifeng-Qiguo Mt.118.96666742.283333Asia562DigitizedFluvial21AWI0.4379.094NAXu, Q.H., Yang, Z.J., Cui, Z.J., Yang, X.L. and Liang, W.D., 2002. A study on pollen analysis of Qiguoshan section and ancestor living environment in Chifeng area, Nei Mongol. Scientia Geographica Sinica, 22(4), pp.453-457 (in Chinese).
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DALAINUR Cao et al.81100081Dalai Nur Lake-Haiyan116.58333343.283333Asia1200RawLake22AWI2.42947.799NALi, R.Q., Zheng, L.M. and Zhu, G.R., 1990. Lakes and Environment in the Neimenggu Plateau. Beijing Normal University Press, Beijing.
DIAOJIAO Cao et al.82100082Diaojiaohaizi DJ112.35000041.300000Asia1800RawLake98AWI2.32911.897NASong, C.Q., Wang, B.Y. and Sun, X.J., 1996. Implication of paleovegetational changes in Diaojiao Lake, Inner Mongolia. Acta Botanica Sinica, 38(7), pp.568-575 (in Chinese).
GAOXI Cao et al.83100083Gaoximage115.36683342.954000Asia1253DigitizedLake39AWI-0.0525.859NALi, C.Y., Xu, Z.L. and Kong, Z.C., 2003. A preliminary investigation on the Holocene vegetation changes from pollen analysis in the Gaoxigema section, Hunshandak Sand Land. Acta Phytoecologica Sinica, 27(6), pp.797-803 (in Chinese).
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DALINURJIAN Cao et al.90100090Dali Nur-Jiangjunpaozi Lake117.47000042.374000Asia1490DigitizedLake15AWI-0.04511.633NAWang, H., Liu, H., Liu, Y. and Cui, H., 2004. Mineral magnetism of lacustrine sediments and Holocene palaeoenvironmental changes in Dali Nor area, southeast Inner Mongolia Plateau, China. Palaeogeography, Palaeoclimatology, Palaeoecology, 208(3-4), pp.175-193.doi:10.1016/j.palaeo.2004.02.026Liu, H., Cui, H. and Huang, Y., 2001. Detecting Holocene movements of the woodland-steppe ecotone in northern China using discriminant analysis. Journal of Quaternary Science: Published for the Quaternary Research Association, 16(3), pp.237-244.doi:10.1002/jqs.598
JUYAN Cao et al.91100091Juyan Lake101.85000041.890000Asia892RawLake65AWI1.70410.666NAHerzschuh, U., Tarasov, P., Wunnemann, B. and Hartmann, K., 2004. Holocene vegetation and climate of the Alashan Plateau, NW China, reconstructed from pollen data. Palaeogeography, Palaeoclimatology, Palaeoecology, 211(1-2), pp.1-17.doi:10.1016/j.palaeo.2004.04.001
DALINURLIU Cao et al.92100092Dali Nur-Liuzhouwan Lake116.68300042.707333Asia1365DigitizedLake25AWI1.04416.539NAWang, H., Liu, H., Cui, H. and Abrahamsen, N., 2001. Terminal Pleistocene/Holocene palaeoenvironmental changes revealed by mineral-magnetism measurements of lake sediments for Dali Nor area, southeastern Inner Mongolia Plateau, China. Palaeogeography, Palaeoclimatology, Palaeoecology, 170(1-2), pp.115-132.doi:10.1016/S0031-0182(01)00231-0
QASQ Cao et al.93100093Qasq111.13333340.666667Asia1000RawPeat108AWI-0.00310.505NAWang, B.Y., Song, C.Q., Cheng, Q.G. and Sun, X.J., 1998. Palaeoclimate reconstruction by adopting the pollen-climate response surface model to analysis the Chasuqi deposition section. Acta Botanica Sinica, 40(11), pp.1067-1074 (in Chinese).Wang, B.Y., Song, C.Q. and Sun, X.J., 1997. Palynological record of paleovegetation change during Holocene at north tumote plain in Inner Mongolia, China. Acta Geographica Sinica, 52(5), pp.430-438 (in Chinese).Wang, B.Y., 2001. Research on pollen-climate response surface model in northern China and the Holocene environmental change in middle Inner Mongolia. Huawen Press, Beijing.
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DAHU Cao et al.110100110Dahu Lake115.03333324.250000Asia250DigitizedPeat33AWI1.37218.603NAZhou, W.J., Yu, X.F., Jull, A.J.T., Burr, G., Xiao, J.Y., Lu, X.F. and Xian, F., 2004. High-resolution evidence from southern China of an early Holocene optimum and a mid-Holocene dry event during the past 18,000 years. Quaternary Research, 62(1), pp.39-48.doi:10.1016/j.yqres.2004.05.004
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KOTYR Cao et al.124100124Kotyrkol70.41666752.966667Asia439RawPeat22AWI-0.0494.965NATarasov, P.E. and Kremenetskii, K.V., 1995. Geochronology and stratigraphy of the Holocene lacustrine-bog deposits in northern and central Kazakhstan. Stratigraphy and Geological Correlation, 3(1), pp.73-80.Tarasov, P.E., 1991. The features of the late Holocene for the Kokchetav Highland. Vestnik Moskovskogo Universiteta. Ser. 5. Geographia. 6, pp.54-60 (in Russian).Tarasov, P.E., 1992. Holocene palaeogeography of the steppe zone of northern and central Kazakhstan. Thesis Cand. Sc. (Geography), Moscow State University, Moscow, Russia (in Russian).
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AKTEREKCao et al.127100127Ak Terek72.83333341.283333Asia1748DigitizedPeat39Cao et al.0.0007.600NABeer, R., Kaiser, F., Schmidt, K., Ammann, B., Carraro, G., Grisa, E. and Tinner, W., 2008. Vegetation history of the walnut forests in Kyrgyzstan (Central Asia): natural or anthropogenic origin?. Quaternary Science Reviews, 27(5-6), pp.621-632.doi:10.1016/j.quascirev.2007.11.012
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MAILI Cao et al.135100135Maili122.88333342.866667Asia155DigitizedPeat31AWI-0.0183.491NARen, G.Y. and Zhang, L.S., 1997. Late Holocene vegetation in Maili region, Northeast China, as inferred from a high-resolution pollen record. Journal of Integrative Plant Biology, 39(4), in Chinese.
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ILAN Cao et al.187100187Ilan121.73333324.750000Asia410RawFluvial36AWI0.8983.471NALin, S.F., Liu, P.M. and Lai, T.H., 2004. Late Holocene pollen sequence of the Ilan Plain, northeastern Taiwan, and its environmental and climatic implications. Terrestrial Atmospheric and Oceanic Sciences, 15(2), pp.221-238.doi:10.3319/TAO.2004.15.2.221(T)
SUNMOON Cao et al.188100188Sun-moon Lake120.91666723.866667Asia746RawLake117AWI0.02712.149NALou, W.C., 1996. Pollen analysis of lacustrine sediments in Sun-Moon Lake Basin since the last glacial maximum. Master thesis. National Taiwan University, Taipei, Taiwan, China.Tsukada, M., 1967. Vegetation in subtropical Formosa during the Pleistocene glaciations and the Holocene. Palaeogeography, Palaeoclimatology, Palaeoecology, 3, pp.49-64.doi:10.1016/0031-0182(67)90005-3
TOUSHE Cao et al.189100189Toushe Lake120.90000023.820000Asia650RawPeat133AWI1.68022.142NALiew, P.M., Kuo, C.M., Huang, S.Y. and Tseng, M.H., 1998. Vegetation change and terrestrial carbon storage in eastern Asia during the Last Glacial Maximum as indicated by a new pollen record from central Taiwan. Global and Planetary Change, 16, pp.85-94.doi:10.1016/S0921-8181(98)00014-9Liew, P.M., Lee, C.Y. and Kuo, C.M., 2006. Holocene thermal optimal and climate variability of East Asian monsoon inferred from forest reconstruction of a subalpine pollen sequence, Taiwan. Earth and Planetary Science Letters, 250(3-4), pp.596-605.doi:10.1016/j.epsl.2006.08.002
BARKOLBLK6E Cao et al.190100190Barkol Lake BLK06E92.80000043.616667Asia1575DigitizedLake97AWI-0.0258.917NATao, S.C., An, C.B., Chen, F.H., Tang, L.Y., Lv, Y.B. and Zheng, T.M., 2009. Holocene vegetation changes interpreted from pollen records in Balikun Lake, Xinjiang, China. Acta Palaeontologica Sinica, 48(2), pp.194-199 (in Chinese).
BEILIKEK Cao et al.191100191Beilikekule Lake89.00000036.666667Asia4680RawLake12AWI0.80515.956NAHuang, C.X., Van Campo, E. and Li, S.K., 1996. Holocene environmental changes of western and northern Qinghai-Xizang Plateau based on pollen analysis. Acta Micropalaeontologica Sinica, 13(4), pp.423-432 (in Chinese).
Bosten Cao et al.192100192Bosten Lake86.55000041.966667Asia1050DigitizedLake31AWI0.07613.843NAXu, Y.Q., 1998. The assemblage of Holocene spore pollen and its environment in Bosten Lake area, Xinjiang. Arid Land Geogr, 2, pp.43-49 (in Chinese).
CAOTAN2002 Cao et al.193100193Caotanhu 200286.02383344.418333Asia380RawPeat58AWI-0.0488.969NAZhang, Y., Kong, Z., Ni, J., Yan, S. and Yang, Z., 2008. Pollen record and environmental evolution of Caotanhu wetland in Xinjiang since 4550 cal. a BP. Chinese Science Bulletin, 53(7), pp.1049-1061 (in Chinese).
CHAIWOCKF Cao et al.194100194Chaiwopu Lake CKF87.78333343.550000Asia1100RawLake22AWI0.12012.316NALi, W.Y. and Yan, S., 1990. Quaternary spore and pollen research in Chaiwopu Basin. In: The Quaternary climo-environment changes and hydrogeological condition of Chaiwopu Basin in Xinjiang region (pp.46-74). China Ocean Press, Beijing.Wen, Q.Z. and Qiao, Y.L., 1990. Preliminary probe of climatic sequence in the last 13 000 years in Xinjiang Region. Quaternary Sciences, 4, pp.363-371 (in Chinese).
DAMAGOU Cao et al.196100196Damagou80.70000037.000000Asia1380RawFluvial18AWI1.37315.967NALin, M.C., 1994. Spore-pollen analysis of Quaternary in Xinjiang Region. Quaternary Geology and Environment of Xinjinag Region. In: Quaternary Geology and Environment of Xinjinag Region, China (pp.68-94). China. Agricultural Press of China, Beijing.Wen, Q.Z. and Qiao, Y.L., 1990. Preliminary probe of climatic sequence in the last 13 000 years in Xinjiang Region. Quaternary Sciences, 4, pp.363-371 (in Chinese).
DAXIGOU Cao et al.197100197Daxigou86.85000043.116667Asia3450RawFluvial52AWI0.1004.007NAZhang, Y., Kong, Z.C., Yang, Z.J., Yan, S. and Ni, J. 2004. Vegetation changes and environmental evolution in the Urumqi River Head, central Tianshan Mountains since 3.6 ka B.P.: a case study of Daxigou profile. Journal of Integrative Plant Biology, 46(6), pp.655-667 (in Chinese).
DONGDAO Cao et al.198100198Dongdaohaizi B89.56000044.696667Asia430RawLake64AWI-0.0065.280NAYan, S., Li, S.F., Kong, Z.C., Yang, Z.J. and Ni, J., 2004. The pollen analyses and environment changes of the Dongdaohaizi area in Urumqi, Xinjiang. Quaternary Sciences, 24(4), pp.463-468 (in Chinese).
EBINUR Cao et al.199100199Ebinur Lake82.45000044.550000Asia212RawLake14AWI0.03113.916NALin, M.C., 1994. Spore-pollen analysis of Quaternary in Xinjiang Region. Quaternary Geology and Environment of Xinjinag Region. In: Quaternary Geology and Environment of Xinjinag Region, China (pp.68-94). China. Agricultural Press of China, Beijing.Wen, Q.Z. and Qiao, Y.L., 1990. Preliminary probe of climatic sequence in the last 13 000 years in Xinjiang Region. Quaternary Sciences, 4, pp.363-371 (in Chinese).
EBINURSW Cao et al.200100200Ebinur Lake SW82.80000045.000000Asia212RawLake9AWI1.2108.214NALin, M.C., 1994. Spore-pollen analysis of Quaternary in Xinjiang Region. Quaternary Geology and Environment of Xinjinag Region. In: Quaternary Geology and Environment of Xinjinag Region, China (pp.68-94). Agricultural Press of China, Beijing.
HUASHUWO Cao et al.201100201Huashuwozi89.13333343.800500Asia1320RawPaleosol52AWI-0.0452.341NAZhang, Y., Kong, Z., Yan, S., Yang, Z. and Ni, J., 2006. Fluctuation of Picea timber-line and paleo-environment on the northern slope of Tianshan Mountains during the late Holocene. Chinese Science Bulletin, 51(14), pp.1747-1756 (in Chinese).
LOPNURK1 Cao et al.202100202Lop Nur K190.25000040.283333Asia780RawLake64AWI1.81432.218NAYan, S., Mu, G.J., Xu, Y.Q. and Zhao, Z.H., 1998. Quaternary environmental evolution of the Lop Nur region, China. Acta geographica sinica, 53(4), pp.332-339 (in Chinese).Yan, S., Mu, G.J. and Xu, Y.Q., 2000. Quaternary environmental evolution of the Lop Nur region, NW China. Acta Micropalaeontologica Sinica, 17(2), pp.165-169 (in Chinese).
LOPNURLUO4 Cao et al.203100203Lop Nur Luo490.25000040.333333Asia800RawLake16AWI0.64424.902NAYan, F.H., Ye, Y.Y. and Mai, X.S., 1983. The sporo-pollen assemblage in the Luo 4 drilling of Lop Lake in Xinjiang and its significance. Seismology and Geology, 5(4), pp.75-80 (in Chinese).
MANASLM1 Cao et al.204100204Manas Lake LM-185.91666745.833333Asia251RawLake60AWI0.49716.591NASun, X.J., Du, N.Q., Weng, C.Y., Lin, R.F. and Wei, K.Q., 1994. Paleovegetation and paleoenvironment of Manasi Lake, Xinjiang, NW China during the last 14000 years. Quaternary Sciences, 3, pp.239-248 (in Chinese).
NIYA Cao et al.205100205Niya River82.76666737.733333Asia1373RawPeat22AWI0.0633.659NAShu, Q. 2001. Study on the Changes of Historic Paleoclimate and Paleoenvironment and Man-Land Relationship of Southern Xinjiang. Master thesis. Xinjiang University, Urumqi, Xinjiang, China.
SICHANG Cao et al.206100206Sichanghu Lake89.14333344.310000Asia589RawLake19AWI0.0501.011NAYan, S., Kong, Z.C. and Yang, Z.J., 2003. Pollen analysis and its significance of the Sichanghu section in Jimusaer county Xinj iang. Acta Botanica Boreali-Occidentalia Sinica, 23(4), pp.531-536 (in Chinese).Zhang, Y., Kong, Z.C., Yan, S., Yang, Z.J. and Ni, J., 2004. \Medieval Warm Period\ in Xinjiang: Rediscussion on paleoenvironment of the Sichanghu Profile in Gurbantunggut Desert. Quaternary Sciences, 24(6), pp.701-708 (in Chinese).
TAGLE Cao et al.207100207Tagle80.76666737.033333Asia1368RawPeat20AWI-0.0030.634NAZhong, W., Xiong, H.G., Teyibai, T. and Li, Q., 1998. Preliminary study on spore-pollen combination and paleoenvironmental features of the Holocene lacustrine sediment of Bosten Lake. The Water Resources, Environment and Management of Tarim River Watershed, pp.160-164 (in Chinese).
TIANSHUISI2 Cao et al.208100208Tianshuihai SI279.51666735.350000Asia4836RawLake11AWI19.50025.515NALi, S.J., Zheng, B.X. and Jiao, K.Q., 1991. Preliminary research on lacustrine deposit and lake evolution on the south slope of the west Kunlun Mountains. Scientia Geographica Sinica, 11(4), pp.306-314 (in Chinese).
TIANSHUITS95 Cao et al.209100209Tianshuihai TS9579.51666735.350000Asia4900RawLake80AWI22.222226.593NALiu, G.X., Wang, R., Li, S.J., Li, B.Y. and Zhu, Z.Y. 1998. Palynological evidence of ecological environment change since 240 ka BP for the Tianshuihai Lake,West Kunlun Mountains. Journal of Glaciology and Geocryology, 20(1), pp.21-24 (in Chinese).
WULUNGU2004 Cao et al.210100210Wulungu Lake WLG-200487.30000047.216667Asia479RawLake110AWI-0.0388.379NALiu, X.Q., Herzschuh, U., Shen, J., Jiang, Q.F. and Xiao, X.Y., 2008. Holocene environmental and climatic changes inferred from Wulungu Lake in northern Xinjiang, China. Quaternary Research, 70(3), pp.412-425.doi:10.1016/j.yqres.2008.06.005
XIAOSHA Cao et al.213100213Xiaoshazi Lake90.83333336.783333Asia4106RawLake11AWI-0.04613.440NAHuang, C.X., Van Campo, E. and Li, S.K., 1996. Holocene environmental changes of western and northern Qinghai-Xizang Plateau based on pollen analysis. Acta Micropalaeontologica Sinica, 13(4), pp.423-432 (in Chinese).
XIAOXI Cao et al.214100214Xiaoxigou89.12166743.800167Asia1360RawArchaeological38AWI-0.0575.025NAZhang, Y., Kong, Z., Yan, S., Yang, Z. and Ni, J., 2006. Fluctuation of Picea timber-line and paleo-environment on the northern slope of Tianshan Mountains during the late Holocene. Chinese Science Bulletin, 51(14), pp.1747-1756 (in Chinese).
YUETE2 Cao et al.215100215Yuetegan 279.91666737.150000Asia1277RawFluvial29AWI-0.0583.525NAWang, L.G., 2003. Study on climatic and environmental changes during the past 4.0 ka in the southern margin of Tarim Basin, southern Xinjiang. Master thesis. Xinjiang University, Urumqi, Xinjiang, China.
BANGONG Cao et al.217100217Bangong Co Lake79.00000030.233333Asia4300RawLake40AWI-0.04611.567NAHuang, C.X., Zhang, Q.S. and Liu, F.T., 1989. A preliminary study of paleovegetation and paleoclimate in the later period of late Pleistocene in Bangongcuo Lake region of Xizang. Journal of Natural Researches, 4(3), pp.247-253 (in Chinese).Fontes, J.C., Gasse, F. and Gibert, E., 1996. Holocene environmental changes in Lake Bangong basin (Western Tibet). Part 1: Chronology and stable isotopes of carbonates of a Holocene lacustrine core. Palaeogeography, Palaeoclimatology, Palaeoecology, 120(1-2), pp.25-47.doi:10.1016/0031-0182(95)00032-1
HIDDENHL1 Cao et al.218100218Hidden Lake HL192.53950029.812833Asia4980DigitizedLake28AWI-0.03813.027NATang, L.Y., Shen, C.M., Liu, K.B., Overpeck, J.T. and Yu, S.Y., 2000. Climatic and hydrological changes in the southeastern Qinghai-Tibetan Plateau during the past 18 000 years. Acta Micropalaeontologica Sinica, 17(2), pp.113-124 (in Chinese).
NGION Cao et al.219100219Ngion Co91.50000030.466667Asia4515DigitizedLake56AWI-0.0395.965NAShen, C., Liu, K.B., Morrill, C., Overpeck, J.T., Peng, J. and Tang, L., 2008. Ecotone shift and major droughts during the mid-late Holocene in the central Tibetan Plateau. Ecology, 89(4), pp.1079-1088.doi:10.1890/06-2016.1Shen, C., 2003. Millennial-scale variations and centennial-scale events in the southwest Asian monsoon: pollen evidence from Tibet. Doctoral dissertation. Louisiana State University and Agricultural and Mechanical College, Baton Rouge, Louisiana, USA.
PEIKU Cao et al.220100220Peiku Co85.33333328.833333Asia4590RawLake98AWI5.66914.736NAHuang, F., 2000. Vegetation and climate between 13ka to 5ka BP in Peiku CO, Tibet. Acta Palaeontologica Sinica, 39(3), pp.441-448 (in Chinese).
QONGJI Cao et al.221100221Co Qongjiamong92.37283329.812833Asia4980DigitizedLake73AWI0.13113.954NAShen, C., 2003. Millennial-scale variations and centennial-scale events in the southwest Asian monsoon: pollen evidence from Tibet. Doctoral dissertation. Louisiana State University and Agricultural and Mechanical College, Baton Rouge, Louisiana, USA.
RENR1 Cao et al.222100222Ren Co R196.68283330.732833Asia4450DigitizedLake39AWI1.98920.538NATang, L.Y., Shen, C.M., Liu, K.B. and Overpeck, J.T., 1999. New high-resolution pollen records from two lakes in Xizang (Tibet). Acta Botanica Sinica, 41(8), pp.896-902 (in Chinese).
SELINCK8803 Cao et al.223100223Selin Co CK880388.51666731.566667Asia4530RawLake53AWI0.31914.114NASun, X.J., Dunaiqiu., Chen, Y.S., Gu, Z.Y., Liu, J.Q., Yuan, B.Y., 1993. Holocene palynological records in lake Selincuo, northern Xizang. Acta Botanica Sinica, 35(12), pp.943-950 (in Chinese).
WASONG Cao et al.224100224Wasong section103.05240032.991300Asia3490DigitizedValley45AWI4.27729.431NAYan, G., Wang, F.B., Shi, G.R. and Li, S.F., 1999. Palynological and stable isotopic study of palaeoenvironmental changes on the northeastern Tibetan plateau in the last 30,000 years. Palaeogeography, Palaeoclimatology, Palaeoecology, 153(1-4), pp.147-159.doi:10.1016/S0031-0182(99)00064-4
WUMAQU Cao et al.225100225Wumaqu91.38333330.533333Asia4370RawPeat19AWI3.11912.125NAWang, P.F., Xia, Y.M. and Wang, M.H., 1988. An approach to the spore-pollen assemblages of paet in the Holocene and the evolution of natural environment in southern Xizang. In: Study of Mire in China (pp. 257-265). Science Press, Beijing.
XUGUO Cao et al.226100226Xuguo Co90.33333331.950000Asia4595DigitizedLake51AWI-0.0108.381NAShen, C., 2003. Millennial-scale variations and centennial-scale events in the southwest Asian monsoon: pollen evidence from Tibet. Doctoral dissertation. Louisiana State University and Agricultural and Mechanical College, Baton Rouge, Louisiana, USA.
YANGHU Cao et al.227100227Yanghu Lake84.65000035.433333Asia4778RawLake18AWI0.76413.141NAZhao, Z.M., Liu, A.M., Peng, W., Ji, W.H., Li, R.S., Wang, Y.Z. and Zhu, Y.T., 2007. Holocene environmental changes of northern Qinghai-Tibetan Plateau based on spore-pollen analysis. Arid Land Geography, 30, pp.381-391 (in Chinese).
ZABUZK2 Cao et al.228100228Zabuye Lake ZK284.04000031.210000Asia4421DigitizedLake40AWI4.92142.483NAWu, Y.S. and Xiao, J.Y., 1996. A pollen record during the past 30000 years from the Zabuye Lake, T ibet. M arine Geology& Q uaternary Geology, 16(3), pp.115-122 (in Chinese).
ZIGETANG Cao et al.229100229Zigetang Co90.90000032.000000Asia4560RawLake67AWI0.03510.752NAHerzschuh, U., Winter, K., Wunnemann, B. and Li, S., 2006. A general cooling trend on the central Tibetan Plateau throughout the Holocene recorded by the Lake Zigetang pollen spectra. Quaternary International, 154, pp.113-121.doi:10.1016/j.quaint.2006.02.005
ERHAIES Cao et al.230100230Erhai Lake ES100.20000025.766667Asia1974DigitizedLake67AWI-0.04312.763NAZhou, J., Wang, S.M. and Lv, J., 2003. Climatic and environmental changes from the sediment record of Erhai Lake over the past 10000 years. Journal of Lake Sciences, 15(2), pp.104-111 (in Chinese).
GANLAN Cao et al.231100231Ganlanba100.60000022.483333Asia500DigitizedPeat23AWI0.3088.306NAXu, Q.H., Yang, X.L., Wang, Z.H., Li, W.Y., Sanpu, X. and Shichuan, S., 1998. Pollen analysis on a peat section at Ganlan Basin, Xishuangbanna, Yunnan Province. Yunnan Geographic Environment Research, 10(2), pp. 34-42 (in Chinese).
MANXING Cao et al.232100232Manxing Lake100.48333321.950000Asia1200RawLake18AWI0.86732.284NATang, L.Y., 1992. Vegetation and climate history at Menghai, Yunnan during the past 42,000 years. Acta Micropalaeontologica Sinica, 9(4), pp.433-455 (in Chinese).
HEMUDUHMD1 Cao et al.234100234Hemudu HMD-1121.35000029.966667Asia6DigitizedDelta71AWI1.88120.353NALi, C.H., Tang, L.Y., Wan, H.W., Wang, S.M., Yao, S.C. and Zhang, D.F., 2009. Vegetation and human activity in Yuyao inferred from the sporo-pollen record since the Late Pleistocene. Acta Micropalaeontologica Sinica, 26(1), pp.48-56 (in Chinese).
KUAHUQ2 Cao et al.235100235Kuahuqiao 2120.20000030.250000Asia0DigitizedArchaeological36AWI7.3609.290NAZong, Y., Chen, Z., Innes, J.B., Chen, C., Wang, Z. and Wang, H., 2007. Fire and flood management of coastal swamp enabled first rice paddy cultivation in east China. Nature, 449(7161), pp.459-462.doi:10.1038/nature06135
LUOJI Cao et al.236100236Luojiang121.36253329.984367Asia4DigitizedDelta32AWI0.20612.999NAAtahan, P., Itzstein-Davey, F., Taylor, D., Dodson, J., Qin, J., Zheng, H. and Brooks, A., 2008. Holocene-aged sedimentary records of environmental changes and early agriculture in the lower Yangtze, China. Quaternary Science Reviews, 27(5-6), pp.556-570.doi:10.1016/j.quascirev.2007.11.003
TIANCHILA Cao et al.237100237Tianchi Lake106.31000037.260000Asia2194RawLake72AWI-0.0485.930NAZhao, Y., Chen, F., Zhou, A., Yu, Z. and Zhang, K., 2010. Vegetation history, climate change and human activities over the last 6200 years on the Liupan Mountains in the southwestern Loess Plateau in central China. Palaeogeography, Palaeoclimatology, Palaeoecology, 293(1-2), pp.197-205.doi:10.1016/j.palaeo.2010.05.020
AKKOL Cao et al.238100238Akkol Lake89.62500050.250000Asia2204DigitizedLake54AWI-0.04314.047NABlyakharchuk, T.A., Wright, H.E., Borodavko, P.S., van der Knaap, W.O. and Ammann, B., 2007. Late glacial and Holocene vegetational history of the Altai mountains (southwestern Tuva Republic, Siberia). Palaeogeography, Palaeoclimatology, Palaeoecology, 245(3-4), pp.518-534.doi:10.1016/j.palaeo.2006.09.010
BAIKAL606-3 Cao et al.239100239Baikal CON01-606-3105.86533352.083333Asia130DigitizedLake63AWI-0.05026.154NADemske, D., Heumann, G., Granoszewski, W., Nita, M., Mamakowa, K., Tarasov, P.E. and Oberhansli, H., 2005. Late glacial and Holocene vegetation and regional climate variability evidenced in high-resolution pollen records from Lake Baikal. Global and Planetary Change, 46(1-4), pp.255-279.doi:10.1016/j.gloplacha.2004.09.020
GRUSHA Cao et al.240100240Grusha Lake89.41666750.383333Asia2413DigitizedLake41AWI1.55014.486NABlyakharchuk, T.A., Wright, H.E., Borodavko, P.S., van der Knaap, W.O. and Ammann, B., 2007. Late glacial and Holocene vegetational history of the Altai mountains (southwestern Tuva Republic, Siberia). Palaeogeography, Palaeoclimatology, Palaeoecology, 245(3-4), pp.518-534.doi:10.1016/j.palaeo.2006.09.010
KENDEGEL Cao et al.241100241Kendegelukol Lake87.64166750.505500Asia2050DigitizedLake59AWI-0.04916.353NABlyakharchuk, T.A., Wright, H.E., Borodavko, P.S., van der Knaap, W.O. and Ammann, B., 2004. Late Glacial and Holocene vegetational changes on the Ulagan high-mountain plateau, Altai Mountains, southern Siberia. Palaeogeography, Palaeoclimatology, Palaeoecology, 209(1-4), pp.259-279.doi:10.1016/j.palaeo.2004.02.011
TASHKOL Cao et al.242100242Tashkol Lake87.67083350.450000Asia2150DigitizedLake53AWI2.92416.339NABlyakharchuk, T.A., Wright, H.E., Borodavko, P.S., van der Knaap, W.O. and Ammann, B., 2004. Late Glacial and Holocene vegetational changes on the Ulagan high-mountain plateau, Altai Mountains, southern Siberia. Palaeogeography, Palaeoclimatology, Palaeoecology, 209(1-4), pp.259-279.doi:10.1016/j.palaeo.2004.02.011
UZUNKOL Cao et al.243100243Uzunkol Lake87.10833350.483333Asia1985DigitizedLake83AWI-0.04917.248NABlyakharchuk, T.A., Wright, H.E., Borodavko, P.S., van der Knaap, W.O. and Ammann, B., 2004. Late Glacial and Holocene vegetational changes on the Ulagan high-mountain plateau, Altai Mountains, southern Siberia. Palaeogeography, Palaeoclimatology, Palaeoecology, 209(1-4), pp.259-279.doi:10.1016/j.palaeo.2004.02.011
Gur_sample Cao et al.244100244Gur137.05000050.000000Asia35DigitizedPeat65AWI-0.04021.688NAMokhova, L., Tarasov, P., Bazarova, V. and Klimin, M., 2009. Quantitative biome reconstruction using modern and late Quaternary pollen data from the southern part of the Russian Far East. Quaternary Science Reviews, 28(25-26), pp.2913-2926.doi:10.1016/j.quascirev.2009.07.018
Kiya Cao et al.245100245Kiya135.66666747.833333Asia100DigitizedPeat42AWI0.05310.031NABazarova, V.B., Klimin, M.A., Mokhova, L.M. and Orlova, L.A., 2008. New pollen records of Late Pleistocene and Holocene changes of environment and climate in the Lower Amur River basin, NE Eurasia. Quaternary International, 179(1), pp.9-19.doi:10.1016/j.quaint.2007.08.015
Pobochnoye Cao et al.246100246Pobochnoye51.84166753.033333Asia65DigitizedPeat27AWI-0.05215.499NAKremenetski, C.V., Bottger, T., Junge, F.W. and Tarasov, A.G., 1999. Late-and postglacial environment of the Buzuluk area, middle Volga region, Russia. Quaternary Science Reviews, 18(10-11), pp.1185-1203.doi:10.1016/S0277-3791(98)00074-2
TYAPKA Cao et al.247100247Tyapka140.11666753.700000Asia4DigitizedPeat86AWI0.02211.691NABazarova, V.B., Klimin, M.A., Mokhova, L.M. and Orlova, L.A., 2008. New pollen records of Late Pleistocene and Holocene changes of environment and climate in the Lower Amur River basin, NE Eurasia. Quaternary International, 179(1), pp.9-19.doi:10.1016/j.quaint.2007.08.015
ARAL86 Cao et al.248100248Aral Lake59.98333344.420000Asia53RawLake33AWI-0.05515.543NAAleshinskaya, Z.V., Tarasov, P.E. and Harrison, S.P., 1996. Aral Sea, Kazakhstan-Uzbekistan. Lake Status Records FSU and Mongolia (pp.108-114).
GANTANG Cao et al.249100249Gantang119.00000027.000000Asia1007DigitizedPeat185AWI0.01848.776NAYue, Y., Zheng, Z., Huang, K., Chevalier, M., Chase, B.M., Carre, M., Ledru, M.P. and Cheddadi, R., 2012. A continuous record of vegetation and climate change over the past 50,000 years in the Fujian Province of eastern subtropical China. Palaeogeography, Palaeoclimatology, Palaeoecology, 365, pp.115-123.doi:10.1016/j.palaeo.2012.09.018
HUGUAN Cao et al.250100250Huguangyan Maar lake110.28333321.150000Asia88DigitizedLake29AWI0.75075.099NAMingram, J., Schettler, G., Nowaczyk, N., Luo, X., Lu, H., Liu, J. and Negendank, J.F., 2004. The Huguang maar lake-a high-resolution record of palaeoenvironmental and palaeoclimatic changes over the last 78,000 years from South China. Quaternary International, 122(1), pp.85-107.doi:10.1016/j.quaint.2004.02.001Lu, H.Y., Liu, J.Q., Chu, G.Q., Gu, Z.Y., Negendank, J., Schettler, G. and Mingram, J. 2003. A study on pollen and environment in the Huguangyan Maar Lake since the last glaciation. Acta Palaeontologica Sinica 42(2): 284-291 (in Chinese).
JINGBO Cao et al.251100251Jingbo Lake128.75000043.908500Asia350DigitizedLake225AWI-0.0389.533NALi, C., Wu, Y. and Hou, X., 2011. Holocene vegetation and climate in Northeast China revealed from Jingbo Lake sediment. Quaternary International, 229(1-2), pp.67-73.doi:10.1016/j.quaint.2009.12.015
XINGKAI Cao et al.252100252Xingkai Lake132.50900045.206000Asia69DigitizedLake185AWI0.12228.648NAWu, J. and Shen, J., 2010. Paleoenviromental and paleoclimatic changes in lake Xingkai inferred from stable carbon and nitrogen isotopes of bulk organic matter since 28 ka BP. Acta Sedimentologica Sinica, 28(2), pp.365-372 (in Chinese).Ji, M., Shen, J., Wu, J. and Wang, Y., 2015. Paleovegetation and paleoclimate evolution of past 27.7 cal ka BP recorded by pollen and charcoal of Lake Xingkai, Northeastern China. In: Earth Surface Processes and Environmental Changes in East Asia (pp. 81-94). Springer, Tokyo.
QIGANUR Cao et al.253100253Qigai Nuur109.50000039.500000AsiaDigitizedLake222AWI-0.01610.754NASun, A. and Feng, Z., 2013. Holocene climatic reconstructions from the fossil pollen record at Qigai Nuur in the southern Mongolian Plateau. The Holocene, 23(10), pp.1391-1402.doi:10.1177/0959683613489581
11-CH-12A Cao et al.25410025411-CH-12A Lake102.28856672.398881Asia60DigitizedLake65AWI0.0067.119NAKlemm, J., Herzschuh, U. and Pestryakova, L.A., 2016. Vegetation, climate and lake changes over the last 7000 years at the boreal treeline in north-central Siberia. Quaternary Science Reviews, 147, pp.422-434.doi:10.1016/j.quascirev.2015.08.015
ACHITNUR Cao et al.255100255Achit Nur Lake90.60000049.500000Asia1435DigitizedLake20AWI0.41214.821NAGunin, P.D., Vostokova, E.A., Dorofeyuk, N.I., Tarasov, P.E. and Black, C.C., 1999. Natural and anthropogenic factors and the dynamics of vegetation distribution in Mongolia. In: Vegetation dynamics of Mongolia (pp. 7-43). Springer, Dordrecht.
ACHITNUUR Cao et al.256100256Achit Nuur90.51666749.416667Asia1444DigitizedLake80AWI-0.05220.608NASun, A., Feng, Z., Ran, M. and Zhang, C., 2013. Pollen-recorded bioclimatic variations of the last1/2 22,600 years retrieved from Achit Nuur core in the western Mongolian Plateau. Quaternary International, 311, pp.36-43.doi:10.1016/j.quaint.2013.07.002
Baikal_Lake-CON01-605-3 Cao et al.257100257Baikal Lake-CON01-605-3104.85472251.585000Asia675DigitizedLake86AWI8.97718.759NADemske, D., Heumann, G., Granoszewski, W., Nita, M., Mamakowa, K., Tarasov, P.E. and Oberhansli, H., 2005. Late glacial and Holocene vegetation and regional climate variability evidenced in high-resolution pollen records from Lake Baikal. Global and Planetary Change, 46(1-4), pp.255-279.doi:10.1016/j.gloplacha.2004.09.020
Baikal_Lake-CON01-605-5 Cao et al.258100258Baikal Lake-CON01-605-5104.85166751.583611Asia665DigitizedLake89AWI0.87611.608NADemske, D., Heumann, G., Granoszewski, W., Nita, M., Mamakowa, K., Tarasov, P.E. and Oberhansli, H., 2005. Late glacial and Holocene vegetation and regional climate variability evidenced in high-resolution pollen records from Lake Baikal. Global and Planetary Change, 46(1-4), pp.255-279.doi:10.1016/j.gloplacha.2004.09.020
Big_Yarovoe_Lake_2008-3 Cao et al.259100259Big Yarovoe Lake78.62668352.852600Asia79RawLake23AWI-0.0105.118NARudaya, N., Nazarova, L., Nourgaliev, D., Palagushkina, O., Papin, D. and Frolova, L., 2012. Mid-late Holocene environmental history of Kulunda, southern West Siberia: vegetation, climate and humans. Quaternary Science Reviews, 48, pp.32-42.doi:10.1016/j.quascirev.2012.06.002
Cheremushka_Bog Cao et al.260100260Cheremushka Bog108.08300052.750000Asia1500DigitizedBog73AWI-0.05141.810NAShichi, K., Takahara, H., Krivonogov, S.K., Bezrukova, E.V., Kashiwaya, K., Takehara, A. and Nakamura, T., 2009. Late Pleistocene and Holocene vegetation and climate records from Lake Kotokel, central Baikal region. Quaternary International, 205(1-2), pp.98-110.doi:10.1016/j.quaint.2009.02.005
Chernaya_Gorka Cao et al.261100261Chernaya Gorka65.35000067.083333Asia170DigitizedLake45AWI6.60410.624NAJankovska, V., Andreev, A.A. and Panova, N.K., 2006. Holocene environmental history on the eastern slope of the Polar Ural Mountains, Russia. Boreas, 35(4), pp.650-661.doi:10.1111/j.1502-3885.2006.tb01171.x
Dolgoe_Ozero Cao et al.262100262Dolgoe Ozero127.06666771.866667Asia40DigitizedLake73AWI-0.06116.468NAPisaric, M.F.J., MacDonald, G.M., Velichko, A.A. and Cwynar, L.C., 2001. The Lateglacial and Postglacial vegetation history of the northwestern limits of Beringia, based on pollen, stomate and tree stump evidence. Quaternary Science Reviews, 20(1-3), pp.235-245.doi:10.1016/S0277-3791(00)00120-7
Khanda Cao et al.265100265Khanda107.00000055.440000Asia713DigitizedPeat42AWI-0.0386.079NABezrukova, E.V., Belov, A.V. and Orlova, L.A., 2011. Holocene vegetation and climate variability in North Pre-Baikal region, East Siberia, Russia. Quaternary International, 237(1-2), pp.74-82.doi:10.1016/j.quaint.2011.01.012
Khanda-1 Cao et al.266100266Khanda-1107.00000055.440000Asia713DigitizedPeat53AWI0.0243.068NABezrukova, E.V., Belov, A.V. and Orlova, L.A., 2011. Holocene vegetation and climate variability in North Pre-Baikal region, East Siberia, Russia. Quaternary International, 237(1-2), pp.74-82.doi:10.1016/j.quaint.2011.01.012
LAB2-95 Cao et al.267100267LAB2-9599.86166772.381667Asia65RawPeat12AWI2.85213.771NAAndreev, A.A., Siegert, C., Klimanov, V.A., Derevyagin, A.Y., Shilova, G.N. and Melles, M., 2002. Late Pleistocene and Holocene vegetation and climate on the Taymyr lowland, northern Siberia. Quaternary Research, 57(1), pp.138-150.doi:10.1006/qres.2001.2302
KOTOKEL2010 Cao et al.268100268Lake Kotokel_2010108.11666752.783333Asia458DigitizedLake212AWI-0.01546.194NABezrukova, E.V., Tarasov, P.E., Solovieva, N., Krivonogov, S.K. and Riedel, F., 2010. Last glacial-interglacial vegetation and environmental dynamics in southern Siberia: Chronology, forcing and feedbacks. Palaeogeography, Palaeoclimatology, Palaeoecology, 296(1-2), pp.185-198.doi:10.1016/j.palaeo.2010.07.020
Lake_Lama Cao et al.269100269Lake Lama90.20000069.533333Asia77RawLake109AWI-0.00521.558NAAndreev, A.A., Tarasov, P.E., Klimanov, V.A., Melles, M., Lisitsyna, O.M. and Hubberten, H.W., 2004. Vegetation and climate changes around the Lama Lake, Taymyr Peninsula, Russia during the late Pleistocene and holocene. Quaternary International, 122(1), pp.69-84.doi:10.1016/j.quaint.2004.01.032
LAO13-94 Cao et al.270100270LAO13-9499.58330072.187500Asia65RawPeat13AWI0.21020.844NAAndreev, A.A., Siegert, C., Klimanov, V.A., Derevyagin, A.Y., Shilova, G.N. and Melles, M., 2002. Late Pleistocene and Holocene vegetation and climate on the Taymyr lowland, northern Siberia. Quaternary Research, 57(1), pp.138-150.doi:10.1006/qres.2001.2302
LAO6-96 Cao et al.271100271LAO6-9699.71500072.390000Asia65DigitizedPeat38AWI7.72228.546NAAndreev, A.A., Siegert, C., Klimanov, V.A., Derevyagin, A.Y., Shilova, G.N. and Melles, M., 2002. Late Pleistocene and Holocene vegetation and climate on the Taymyr lowland, northern Siberia. Quaternary Research, 57(1), pp.138-150.doi:10.1006/qres.2001.2302
Laptev_PM9462 Cao et al.272100272Laptev PM9462136.00500073.503333Asia0DigitizedMarine92Cao et al.0.2009.320NANaidina, O.D. and Bauch, H.A., 2001. A Holocene pollen record from the Laptev Sea shelf, northern Yakutia. Global and Planetary Change, 31(1-4), pp.141-153.doi:10.1016/S0921-8181(01)00117-5Bauch, H.A., Kassens, H., Naidina, O.D., Kunz-Pirrung, M. and Thiede, J., 2001. Composition and flux of Holocene sediments on the eastern Laptev Sea shelf, Arctic Siberia. Quaternary Research, 55(3), pp.344-351.doi:10.1006/qres.2000.2223Bauch, H.A., Kassens, H., Naidina, O.D., Kunz-Pirrung, M. and Thiede, J., 2001. Composition and flux of Holocene sediments on the eastern Laptev Sea shelf, Arctic Siberia. Quaternary Research, 55(3), pp.344-351.doi:10.1006/qres.2000.2223
PG1228 Cao et al.273100273Levinson-Lessing Lake98.63600074.473000Asia47RawLake90AWI-0.04734.498NAAndreev, A.A., Tarasov, P.E., Siegert, C., Ebel, T., Klimanov, V.A., Melles, M., Bobrov, A.A., Dereviagin, A.Y., Lubinski, D.J. and HUBBERTEN, H.W., 2003. Late Pleistocene and Holocene vegetation and climate on the northern Taymyr Peninsula, Arctic Russia. Boreas, 32(3), pp.484-505.doi:10.1111/j.1502-3885.2003.tb01230.x
Melkoye_Lake_core Cao et al.275100275Melkoye Lake175.23333364.858333Asia36RawLake31AWI-0.04939.391NALozhkin, A. and Anderson, P., 2013. Late Quaternary lake records from the Anadyr lowland, central Chukotka (Russia). Quaternary Science Reviews, 68, pp.1-16.doi:10.1016/j.quascirev.2013.02.007
Okunayka Cao et al.276100276Okunayka108.47000055.520000Asia1450DigitizedPeat53AWI-0.0448.973NABezrukova, E.V., Belov, A.V. and Orlova, L.A., 2011. Holocene vegetation and climate variability in North Pre-Baikal region, East Siberia, Russia. Quaternary International, 237(1-2), pp.74-82.doi:10.1016/j.quaint.2011.01.012
Patricia_Lake Cao et al.278100278Patricia Lake176.50000063.325000Asia121RawLake66AWI-0.05224.317NAAnderson, P.M. and Lozhkin, A.V., 2015. Late quaternary vegetation of Chukotka (Northeast Russia), implications for glacial and holocene environments of Beringia. Quaternary Science Reviews, 107, pp.112-128.doi:10.1016/j.quascirev.2014.10.016
Pernatoye_Lake Cao et al.279100279Pernatoye Lake155.39516750.040500Asia6RawLake61AWI0.03111.280NAAnderson, P., Minyuk, P., Lozhkin, A., Cherepanova, M., Borkhodoev, V. and Finney, B., 2015. A multiproxy record of Holocene environmental changes from the northern Kuril Islands (Russian Far East). Journal of paleolimnology, 54(4), pp.379-393.doi:10.1007/s10933-015-9858-y
Sakhalin_Island_Khoe Cao et al.280100280Sakhalin Island_Khoe142.14000051.340000Asia15DigitizedCoast113AWI-0.05242.291NALeipe, C., Nakagawa, T., Gotanda, K., Muller, S. and Tarasov, P.E., 2015. Late Quaternary vegetation and climate dynamics at the northern limit of the East Asian summer monsoon and its regional and global-scale controls. Quaternary Science Reviews, 116, pp.57-71.doi:10.1016/j.quascirev.2015.03.012
Salym-Yugan Cao et al.281100281Salym-Yugan72.08333360.016667Asia58DigitizedPeat50AWI0.21810.958NAPitkanen, A., Turunen, J., Tahvanainen, T. and Tolonen, K., 2002. Holocene vegetation history from the Salym-Yugan mire area, West Siberia. The Holocene, 12(3), pp.353-362.doi:10.1191/0959683602hl533rp
SHAAMAR Cao et al.282100282Shaamar105.20000050.200000Asia650DigitizedPaleosol65AWI-0.04737.217NAMa, Y., Liu, K.B., Feng, Z., Meng, H., Sang, Y., Wang, W. and Zhang, H., 2013. Vegetation changes and associated climate variations during the past1/2 38,000 years reconstructed from the Shaamar eolian-paleosol section, northern Mongolia. Quaternary International, 311, pp.25-35.doi:10.1016/j.quaint.2013.08.037
TSOKAR Cao et al.283100283Tso Kar Lake78.02516133.308839Asia4527DigitizedLake31AWI-0.04515.439NADemske, D., Tarasov, P.E., Wunnemann, B. and Riedel, F., 2009. Late glacial and Holocene vegetation, Indian monsoon and westerly circulation in the Trans-Himalaya recorded in the lacustrine pollen sequence from Tso Kar, Ladakh, NW India. Palaeogeography, Palaeoclimatology, Palaeoecology, 279(3-4), pp.172-185.doi:10.1016/j.palaeo.2009.05.008
TSOMOR Cao et al.284100284Tso Moriri Lake78.32333332.929444Asia4512DigitizedLake79AWI-0.05013.174NALeipe, C., Demske, D., Tarasov, P.E. and Members, H.P., 2014. A Holocene pollen record from the northwestern Himalayan lake Tso Moriri: implications for palaeoclimatic and archaeological research. Quaternary International, 348, pp.93-112.doi:10.1016/j.quaint.2013.05.005
PG1856-3 Cao et al.285100285Two-Yurts Lake_PG1856-3160.04027056.822670Asia275DigitizedLake23AWI3.0026.231NAHoff, U., Biskaborn, B.K., Dirksen, V.G., Dirksen, O., Kuhn, G., Meyer, H., Nazarova, L., Roth, A. and Diekmann, B., 2015. Holocene environment of Central Kamchatka, Russia: Implications from a multi-proxy record of Two-Yurts Lake. Global and Planetary Change, 134, pp.101-117.doi:10.1016/j.gloplacha.2015.07.011
PG1857-2 Cao et al.286100286Two-Yurts Lake_PG1857-2160.06748056.816750Asia275DigitizedLake18AWI0.0192.574NAHoff, U., Biskaborn, B.K., Dirksen, V.G., Dirksen, O., Kuhn, G., Meyer, H., Nazarova, L., Roth, A. and Diekmann, B., 2015. Holocene environment of Central Kamchatka, Russia: Implications from a multi-proxy record of Two-Yurts Lake. Global and Planetary Change, 134, pp.101-117.doi:10.1016/j.gloplacha.2015.07.011
PG1857-5 Cao et al.287100287Two-Yurts Lake_PG1857-5160.06778056.816750Asia275DigitizedLake15AWI2.6415.972NAHoff, U., Biskaborn, B.K., Dirksen, V.G., Dirksen, O., Kuhn, G., Meyer, H., Nazarova, L., Roth, A. and Diekmann, B., 2015. Holocene environment of Central Kamchatka, Russia: Implications from a multi-proxy record of Two-Yurts Lake. Global and Planetary Change, 134, pp.101-117.doi:10.1016/j.gloplacha.2015.07.011
Ukta_Creek_mouth Cao et al.288100288Ukta Creek mouth109.70000055.800000Asia906RawPeat33AWI-0.0255.219NABezrukova, E.V., Belov, A.V., Abzaeva, A.A., Letunova, P.P., Orlova, L.A., Sokolova, L.P., Kulagina, N.V. and Fisher, E.E., 2006, October. First high-resolution dated records of vegetation and climate changes on the Lake Baikal northern shore in the middle-late Holocene. In Doklady earth sciences (Vol. 411, No. 1, p. 1331). Springer Nature BV.doi:10.1134/S1028334X0608037X
Yenisei Cao et al.289100289Yenisei87.15000068.166667AsiaDigitizedPeat45AWI1.3576.745NAAndreev, A.A. and Klimanov, V.A., 2000. Quantitative Holocene climatic reconstruction from Arctic Russia. Journal of Paleolimnology, 24(1), pp.81-91.doi:10.1023/A:1008121917521
Julietta_Lake Cao et al.290100290Julietta154.55550061.337500Asia880RawLake130AWI1.22926.318NAAnderson, P.M., Lozhkin, A.V., Solomatkina, T.B. and Brown, T.A., 2010. Paleoclimatic implications of glacial and postglacial refugia for Pinus pumila in western Beringia. Quaternary Research, 73(2), pp.269-276.doi:10.1016/j.yqres.2009.09.008
KUHAI_neotoma Cao et al.292100292Kuhai Lake99.30950035.515833Asia4150RawLake60AWI0.18422.727NAWischnewski, J., Mischke, S., Wang, Y. and Herzschuh, U., 2011. Reconstructing climate variability on the northeastern Tibetan Plateau since the last Lateglacial-a multi-proxy, dual-site approach comparing terrestrial and aquatic signals. Quaternary Science Reviews, 30(1-2), pp.82-97.doi:10.1016/j.quascirev.2010.10.001Mischke, S., Zhang, C., Borner, A. and Herzschuh, U., 2010. Lateglacial and Holocene variation in aeolian sediment flux over the northeastern Tibetan Plateau recorded by laminated sediments of a saline meromictic lake. Journal of Quaternary science, 25(2), pp.162-177.doi:10.1002/jqs.1288
PINGWANG Cao et al.293100293Pingwang120.64027830.958333Asia2DigitizedPaleosol51AWI2.2607.700NAInnes, J.B., Zong, Y., Wang, Z. and Chen, Z., 2014. Climatic and palaeoecological changes during the mid-to Late Holocene transition in eastern China: high-resolution pollen and non-pollen palynomorph analysis at Pingwang, Yangtze coastal lowlands. Quaternary Science Reviews, 99, pp.164-175.doi:10.1016/j.quascirev.2014.06.013
QINGPU Cao et al.294100294Qingpu121.16666731.250000Asia3DigitizedDelta15Cao et al.1.5008.500NATao, J., Chen, M.T. and Xu, S., 2006. A Holocene environmental record from the southern Yangtze River delta, eastern China. Palaeogeography, Palaeoclimatology, Palaeoecology, 230(3-4), pp.204-229.doi:10.1016/j.palaeo.2005.07.015Stanley, D.J. and Chen, Z., 2000. Radiocarbon dates in China's Holocene Yangtze delta: record of sediment storage and reworking, not timing of deposition. Journal of Coastal Research, pp.1126-1132.
RETREAT Cao et al.295100295Retreat Lake121.43333324.483333Asia2230DigitizedLake31AWI0.0249.356NAKandasamy, S., Chen, C.A. and Lou, J., 2006, December. Holocene East Asian Monsoon Variability: Links to Solar and Tropical Pacific Forcing. In AGU Fall Meeting Abstracts (Vol. 2006, pp. PP43A-1210).doi:10.1029/2006GL028155Wang, L.C., Behling, H., Chen, Y.M., Huang, M.S., Chen, C.T.A., Lou, J.Y., Chang, Y.P. and Li, H.C., 2014. Holocene monsoonal climate changes tracked by multiproxy approach from a lacustrine sediment core of the subalpine Retreat Lake in Taiwan. Quaternary International, 333, pp.69-76.doi:10.1016/j.quaint.2014.02.014
AIBI Cao et al.296100296Aibi Lake82.83333345.016667Asia200DigitizedLake193AWI0.02920.744NAWang, W., Feng, Z., Ran, M. and Zhang, C., 2013. Holocene climate and vegetation changes inferred from pollen records of Lake Aibi, northern Xinjiang, China: A potential contribution to understanding of Holocene climate pattern in East-central Asia. Quaternary International, 311, pp.54-62.doi:10.1016/j.quaint.2013.07.034
BALIKUN Cao et al.297100297Balikun Lake92.80000043.675000Asia1575DigitizedLake87Cao et al.9.00030.500NAAn, C.B., Tao, S.C., Zhao, J., Chen, F.H., Lv, Y., Dong, W., Li, H., Zhao, Y., Jin, M. and Wang, Z., 2013. Late Quaternary (30.7-9.0 cal ka BP) vegetation history in Central Asia inferred from pollen records of Lake Balikun, northwest China. Journal of paleolimnology, 49(2), pp.145-154.doi:10.1007/s10933-012-9649-7
YILI_neotoma Cao et al.298100298Yili River81.96508343.857139Asia928DigitizedRiver81Cao et al.3.33814.940NALi, X., Zhao, K., Dodson, J. and Zhou, X., 2011. Moisture dynamics in central Asia for the last 15 kyr: new evidence from Yili Valley, Xinjiang, NW China. Quaternary Science Reviews, 30(23-24), pp.3457-3466.doi:10.1016/j.quascirev.2011.09.010
HALIGU Cao et al.299100299Haligu Lake100.18055627.003333Asia3277DigitizedLake40AWI-0.0579.205NASong, X.Y., Yao, Y.F., Wortley, A.H., Paudayal, K.N., Yang, S.H., Li, C.S. and Blackmore, S., 2012. Holocene vegetation and climate history at Haligu on the Jade Dragon snow mountain, Yunnan, SW China. Climatic Change, 113(3), pp.841-866.doi:10.1007/s10584-011-0364-6
SHUNDU Cao et al.300100300Shudu Lake99.94960027.910300Asia3630DigitizedLake23Cao et al.11.00022.000NACook, C.G., Jones, R.T., Langdon, P.G., Leng, M.J. and Zhang, E., 2011. New insights on Late Quaternary Asian palaeomonsoon variability and the timing of the Last Glacial Maximum in southwestern China. Quaternary Science Reviews, 30(7-8), pp.808-820.doi:10.1016/j.quascirev.2011.01.003Liu, G.X., Shen, Y.P., Wang, R. and Wang, S.M., 1995. The vegetation and climatic changes in Zoige during the last 20000 years determined by pollen records. Journal of Glacilolgy and Geocryology, 17(2), pp.132-137 (in Chinese).
TIANCHI2 Cao et al.301100301Tianchi106.30916735.264722Asia2430DigitizedLake253AWI-0.0555.095NAZhao, Y., Chen, F., Zhou, A., Yu, Z. and Zhang, K., 2010. Vegetation history, climate change and human activities over the last 6200 years on the Liupan Mountains in the southwestern Loess Plateau in central China. Palaeogeography, Palaeoclimatology, Palaeoecology, 293(1-2), pp.197-205.doi:10.1016/j.palaeo.2010.05.020Xiao, X., Haberle, S.G., Shen, J., Yang, X., Han, Y., Zhang, E. and Wang, S., 2014. Latest Pleistocene and Holocene vegetation and climate history inferred from an alpine lacustrine record, northwestern Yunnan Province, southwestern China. Quaternary Science Reviews, 86, pp.35-48.doi:10.1016/j.quascirev.2013.12.023
Malyi_Krechet_Lake Cao et al.302100302Malyi Krechet Lake175.53333364.800000Asia32RawLake46AWI-0.04949.572NALozhkin, A. and Anderson, P., 2013. Late Quaternary lake records from the Anadyr lowland, central Chukotka (Russia). Quaternary Science Reviews, 68, pp.1-16.doi:10.1016/j.quascirev.2013.02.007
DAJIUHU2013 Cao et al.303100303Dajiuhu_2013110.00194431.485556Asia1700DigitizedPeat151Cao et al.0.00041.200NALi, J., Zheng, Z., Huang, K., Yang, S., Chase, B., Valsecchi, V., Carre, M. and Cheddadi, R., 2013. Vegetation changes during the past 40,000 years in Central China from a long fossil record. Quaternary International, 310, pp.221-226.doi:10.1016/j.quaint.2012.01.009
DONGGI1790 Cao et al.304100304PG1790-Donggi Cona98.50000035.500000Asia4095DigitizedLake77AWI0.17216.145NAAichner, B., Herzschuh, U., Wilkes, H., Schulz, H.M., Wang, Y., Plessen, B., Mischke, S., Diekmann, B. and Zhang, C., 2012. Ecological development of Lake Donggi Cona, north-eastern Tibetan Plateau, since the late glacial on basis of organic geochemical proxies and non-pollen palynomorphs. Palaeogeography, Palaeoclimatology, Palaeoecology, 313, pp.140-149.doi:10.1016/j.palaeo.2011.10.015Wang, Y., Herzschuh, U., Shumilovskikh, L.S., Mischke, S., Birks, H.J.B., Wischnewski, J., Bohner, J., Schlutz, F., Lehmkuhl, F., Diekmann, B. and Wunnemann, B., 2014. Quantitative reconstruction of precipitation changes on the NE Tibetan Plateau since the Last Glacial Maximum-extending the concept of pollen source area to pollen-based climate reconstructions from large lakes. Climate of the Past, 10(1), pp.21-39.doi:10.5194/cp-10-21-2014
Kirek_Lake Cao et al.305100305Kirek Lake84.21666756.100000Asia90DigitizedLake48AWI0.20312.179NABlyakharchuk, T.A., 2003. Four new pollen sections tracing the Holocene vegetational development of the southern part of the West Siberan Lowland. The Holocene, 13(5), pp.715-731.doi:10.1191/0959683603hl658rp
Lake_Sokoch Cao et al.306100306Lake Sokoch157.75400053.254000Asia495DigitizedLake38AWI0.05310.341NADirksen, V., Dirksen, O., van den Bogaard, C. and Diekmann, B., 2015. Holocene pollen record from Lake Sokoch, interior Kamchatka (Russia), and its paleobotanical and paleoclimatic interpretation. Global and Planetary Change, 134, pp.129-141.doi:10.1016/j.gloplacha.2015.07.010
Zhukovskoye_Mire Cao et al.307100307Zhukovskoye mire84.83333356.333333Asia106RawPeat89AWI-0.04714.147NABorisova, O.K., Novenko, E.Y., Zelikson, E.M. and Kremenetski, K.V., 2011. Lateglacial and Holocene vegetational and climatic changes in the southern taiga zone of West Siberia according to pollen records from Zhukovskoye peat mire. Quaternary International, 237(1-2), pp.65-73.doi:10.1016/j.quaint.2011.01.015
AHUNG Cao et al.308100308Ahung Co92.07033331.616167Asia4450DigitizedLake19AWI3.1318.820NAShen, C., 2003. Millennial-scale variations and centennial-scale events in the southwest Asian monsoon: pollen evidence from Tibet. Doctoral dissertation. Louisiana State University and Agricultural and Mechanical College, Baton Rouge, Louisiana, USA.Morrill, C., Overpeck, J.T., Cole, J.E., Liu, K.B., Shen, C. and Tang, L., 2006. Holocene variations in the Asian monsoon inferred from the geochemistry of lake sediments in central Tibet. Quaternary Research, 65(02), pp.232-243.doi:10.1016/j.yqres.2005.02.014
LAOTANFA Cao et al.309100309Laotanfang103.20000026.100000Asia3579DigitizedLake35AWI0.2689.389NAZhang, W., Cui, Z., Feng, J., 2006. Pollen Records of the Deposits in Glacial Erosive Lake Section in Gongwang Mountain, Yunnan Province during the Holocene. Geography and Geo-Information Science, 22(1), pp.109-112 (in Chinese).
Elgygytgyn_Lake_P1 Cao et al.310100310El'gygytgyn Lake_P1172.21944467.373889Asia561RawLake23AWI3.16313.834NAAndreev, A.A., Morozova, E., Fedorov, G., Schirrmeister, L., Bobrov, A.A., Kienast, F. and Schwamborn, G., 2012. Vegetation history of central Chukotka deduced from permafrost paleoenvironmental records of the El'gygytgyn Impact Crater. Climate of the Past, 8(4), pp.1287-1300.doi:10.5194/cp-8-1287-2012
Elgygytgyn_Lake_P2 Cao et al.311100311El'gygytgyn Lake_P2172.12527867.547222Asia542DigitizedLake35AWI0.12713.927NAAndreev, A.A., Morozova, E., Fedorov, G., Schirrmeister, L., Bobrov, A.A., Kienast, F. and Schwamborn, G., 2012. Vegetation history of central Chukotka deduced from permafrost paleoenvironmental records of the El'gygytgyn Impact Crater. Climate of the Past, 8(4), pp.1287-1300.doi:10.5194/cp-8-1287-2012
KHUISIIN Cao et al.313100313Khuisiin Lake101.80000046.600000Asia2270DigitizedLake68Cao et al.-0.0471.108NATian, F., Herzschuh, U., Dallmeyer, A., Xu, Q., Mischke, S. and Biskaborn, B.K., 2013. Environmental variability in the monsoon-westerlies transition zone during the last 1200 years: lake sediment analyses from central Mongolia and supra-regional synthesis. Quaternary Science Reviews, 73, pp.31-47.doi:10.1016/j.quascirev.2013.05.005
Lake_Fernsehsee Cao et al.314100314Lake Fernsehsee60.49896752.828031Asia290RawLake39AWI0.3449.211NAStobbe, A., Gumnior, M., Ropke, A. and Schneider, H., 2015. Palynological and sedimentological evidence from the Trans-Ural steppe (Russia) and its palaeoecological implications for the sudden emergence of Bronze Age sedentarism. Vegetation History and Archaeobotany, 24(3), pp.393-412.doi:10.1007/s00334-014-0506-7
GONGHAI Cao et al.315100315Gonghai Lake112.23333338.900000Asia1860RawLake777AWI-0.05414.704NAXu, Q., Chen, F., Zhang, S., Cao, X., Li, J., Li, Y., Li, M., Chen, J., Liu, J. and Wang, Z., 2017. Vegetation succession and East Asian Summer Monsoon Changes since the last deglaciation inferred from high-resolution pollen record in Gonghai Lake, Shanxi Province, China. The Holocene, 27(6), pp.835-846.doi:10.1177/0959683616675941Chen, F., Xu, Q., Chen, J., Birks, H.J.B., Liu, J., Zhang, S., Jin, L., An, C., Telford, R.J., Cao, X. and Wang, Z., 2015. East Asian summer monsoon precipitation variability since the last deglaciation. Scientific reports, 5(1), pp.1-11.doi:10.1038/srep11186
QIGANHU Cao et al.316100316Qiganhu Lake119.30000042.900000Asia600RawLake145AWI5.76415.090NAHu, Y., Cao, X., Zhao, Z., Li, Y., Sun, Y. and Wang, H., 2016. The palaeoenvironmental and palaeoclimatic reconstruction and the relation with the human activities during the Early and Middle Holocene in the upper Western Liao river region. Quaternary Sci, 36, pp.530-541 (in Chinese).
SIHAILONG Cao et al.317100317Sihailongwan Lake126.60000042.283333Asia797RawLake356AWI-0.02317.155NAStebich, M., Rehfeld, K., Schluetz, F., Tarasov, P.E., Liu, J. and Mingram, J., 2015. Holocene vegetation and climate dynamics of NE China based on the pollen record from Sihailongwan Maar Lake. Quaternary Science Reviews, 124, pp.275-289.doi:10.1016/j.quascirev.2015.07.021Schettler, G., Liu, Q., Mingram, J., Stebich, M. and Dulski, P., 2006. East-Asian monsoon variability between 15 000 and 2000 cal. yr BP recorded in varved sediments of Lake Sihailongwan (northeastern China, Long Gang volcanic field). The Holocene, 16(8), pp.1043-1057.doi:10.1177/0959683606069388
Chaginskoe Cao et al.319100319Chaginskoe84.88333356.450000Asia80DigitizedPeat28AWI-0.0588.314NABlyakharchuk, T.A., 2003. Four new pollen sections tracing the Holocene vegetational development of the southern part of the West Siberan Lowland. The Holocene, 13(5), pp.715-731.doi:10.1191/0959683603hl658rp
SAYRAM Cao et al.320100320Sayram Lake81.15000044.566667Asia2072DigitizedLake146Cao et al.0.08013.796NAJiang, Q., Ji, J., Shen, J., Matsumoto, R., Tong, G., Qian, P., Ren, X. and Yan, D., 2013. Holocene vegetational and climatic variation in westerly-dominated areas of Central Asia inferred from the Sayram Lake in northern Xinjiang, China. Science China Earth Sciences, 56(3), pp.339-353.doi:10.1007/s11430-012-4550-9
SUMXI Cao et al.321100321Sumxi80.24392234.605803Asia5058RawLake99AWI-0.00314.878NAVan Campo, E. and Gasse, F., 1993. Pollen-and diatom-inferred climatic and hydrological changes in Sumxi Co Basin (Western Tibet) since 13,000 yr BP. Quaternary Research, 39(3), pp.300-313.doi:10.1006/qres.1993.1037
XIMEN Cao et al.322100322Ximen Co101.47000033.380000Asia4000RawLake91AWI0.03419.602NAZhang, C. and Mischke, S., 2009. A Lateglacial and Holocene lake record from the Nianbaoyeze Mountains and inferences of lake, glacier and climate evolution on the eastern Tibetan Plateau. Quaternary Science Reviews, 28(19-20), pp.1970-1983.doi:10.1016/j.quascirev.2009.03.007Herzschuh, U., Borkowski, J., Schewe, J., Mischke, S. and Tian, F., 2014. Moisture-advection feedback supports strong early-to-mid Holocene monsoon climate on the eastern Tibetan Plateau as inferred from a pollen-based reconstruction. Palaeogeography, Palaeoclimatology, Palaeoecology, 402, pp.44-54.doi:10.1016/j.palaeo.2014.02.022Mischke, S. and Zhang, C., 2010. Holocene cold events on the Tibetan Plateau. Global and Planetary Change, 72(3), pp.155-163.doi:10.1016/j.gloplacha.2010.02.001
ILIRNEY AWI324100324Ilirney168.32002567.351661Asia421RawLake66AWI0.31825.017NAVyse, S.A., Herzschuh, U., Andreev, A.A., Pestryakova, L.A., Diekmann, B., Armitage, S.J. and Biskaborn, B.K., 2020. Geochemical and sedimentological responses of arctic glacial Lake Ilirney, chukotka (far east Russia) to palaeoenvironmental change since1/2 51.8 ka BP. Quaternary Science Reviews, 247, p.106607.doi:10.1016/j.quascirev.2020.106607
RAUCHUAGY AWI325100325Rauchuagytgyn168.72908467.793743Asia421RawLake53AWI0.0269.338NAHuang, S., Herzschuh, U., Pestryakova, L.A., Zimmermann, H.H., Davydova, P., Biskaborn, B.K., Shevtsova, I. and Stoof-Leichsenring, K.R., 2020. Genetic and morphologic determination of diatom community composition in surface sediments from glacial and thermokarst lakes in the Siberian Arctic. Journal of Paleolimnology, 64, pp.225-242.doi:10.1007/s10933-020-00133-1
BOLSHOTO AWI326100326Bolshoe Toko PG2133130.53333356.266667Asia903RawLake67Cao et al.0.10234.500NACourtin, J., Andreev, A.A., Raschke, E., Bala, S., Biskaborn, B.K., Liu, S., Zimmermann, H., Diekmann, B., Stoof-Leichsenring, K.R., Pestryakova, L.A. and Herzschuh, U., 2021. Vegetation changes in southeastern Siberia during the Late Pleistocene and the Holocene. Frontiers in Ecology and Evolution, 9, p.233.doi:10.3389/fevo.2021.625096
EMANDA AWI327100327Emanda135.75916765.294000Asia671RawLake94AWI0.05656.658NABaumer, M.M., Wagner, B., Meyer, H., Leicher, N., Lenz, M., Fedorov, G., Pestryakova, L.A. and Melles, M., 2021. Climatic and environmental changes in the Yana Highlands of north-eastern Siberia over the last c. 57 000 years, derived from a sediment core from Lake Emanda. Boreas, 50(1), pp.114-133.doi:10.1111/bor.12476
OMOLOY-02B AWI328100328Omoloy 14-OM-02B132.67000070.720000Asia58RawLake18AWI-0.0537.763NALiu, S., Stoof-Leichsenring, K.R., Kruse, S., Pestryakova, L.A. and Herzschuh, U., 2020. Holocene vegetation and plant diversity changes in the north-eastern Siberian treeline region from pollen and sedimentary ancient DNA. Frontiers in Ecology and Evolution, 8, p.304.doi:10.3389/fevo.2020.560243
OMOLOY-12A AWI329100329Omoloy 14-OM-12A132.57000070.960000Asia60RawLake18AWI-0.0315.874NALiu, S., Stoof-Leichsenring, K.R., Kruse, S., Pestryakova, L.A. and Herzschuh, U., 2020. Holocene vegetation and plant diversity changes in the north-eastern Siberian treeline region from pollen and sedimentary ancient DNA. Frontiers in Ecology and Evolution, 8, p.304.doi:10.3389/fevo.2020.560243
OMOLOY-20B AWI330100330Omoloy 14-OM-20B132.91000070.530000Asia52RawLake18AWI-0.0354.973NALiu, S., Stoof-Leichsenring, K.R., Kruse, S., Pestryakova, L.A. and Herzschuh, U., 2020. Holocene vegetation and plant diversity changes in the north-eastern Siberian treeline region from pollen and sedimentary ancient DNA. Frontiers in Ecology and Evolution, 8, p.304.doi:10.3389/fevo.2020.560243