LATITUDE: 64.100000 * LONGITUDE: 171.183333 * MINIMUM DEPTH, sediment/rock: 0.1500 m * MAXIMUM DEPTH, sediment/rock: 36.3000 m

12/11/2014

text/tab-separated-values, 12 data points

https://doi.pangaea.de/10.1594/PANGAEA.838674

doi:10.1594/PANGAEA.838674

en

PANGAEA

Anderson, Patricia M; Lozhkin, Anatoly 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, YE (1982): Characteristic form of late Pleistocene yedoma complex in southeastern Chukotka [in Russian]. In: Frozen geological processes and paleography of the lowlands of northeast Asia. Magadan Publishing House, Magadan. Zoological Institute, USSR Academy of Sciences, Leningrad, 75-81

Kaplin, PA (1980): Recent deposits and Pleistocene paleogeography of Chukotka [in Russian]. Nauka, Moscow

Kotov, AN; Lozhkin, Anatoly V; Ryabchun, VK (1989): Glacial facies and conditions of sediment forms for upper Quaternary sediments of the Main River valley, Chukotka [in Russian]. In: V.F. Ivanov and B.F. Palymskii (eds.) Form relief and sediment correlation and precious metals of north east USSR. North East Interdisciplinary Research Institute, Far East Branch, USSR Academy of Sciences, Magadan, 117-131

Kotov, AN; Ryabchun, VK (1986): Cryogenic complex of late Pleistocene deposits of the Main River Valley [in Russian]. In: A.V. Lozhkin (ed.) Ust'-Algan mammoth exposures. North East Interdisciplinary Research Institute, Far East Branch, USSR Academy of Sciences, Magadan, 2

Lozhkin, Anatoly V; Kotov, AN; Ryabchun, VK (2000): Palynological and radiocarbon data of the Ledovyi Obryv exposure (the south east of Chukotka) [in Russian]. In: K.V. Simakov (ed.) The Quaternary Period of Beringia. North East Interdisciplinary Research Institute, Far East Branch, Russian Academy of Sciences, Magadan, 118-131

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