New Data on the Geological Development of the Southern Part of the East Siberian Sea in the Late Pleistocene

New Data on the Geological Development of the Southern Part of the East Siberian Sea in the Late Pleistocene–Holocene

Published:2022-12 Issue:6 Volume:62 Page:903-918
ISSN:0001-4370
Container-title:Oceanology
language:en
Short-container-title:Oceanology

Author:

Ryabchuk D. V.,Sergeev A. Yu.,Budanov L. M.,Zhamoida V. A.,Nosevich E. S.,Pushina Z. V.,Grigoriev A. G.,Neevin I. A.,Bashirova L. D.,Ponomarenko E. V.,Prishchepenko D. V.

Publisher

Pleiades Publishing Ltd

Subject

Oceanography

Link

https://link.springer.com/content/pdf/10.1134/S0001437022400041.pdf

Reference45 articles.

1. M. A. Anisimov, V. E. Tumskoi, and L. M. Savatyugin, “On the issue of changes in the natural conditions of the New Siberian Islands in the Late Pleistocene and Holocene,” Izv. Ross. Geogr. O-va. 134 (5), 32–37 (2002).

2. On the relative level of the Laptev and East Siberian seas in the postglacial;F. E. Are,1982

3. S. A., Bondarenko, V. A. Vinogradov, Yu. V. Goryachev, et al., State Geological Map of the Russian Federation. Scale 1 : 1 000 000 (Third Generation). Chukotka Series. Sheet R-1, 2—Wrangel Island. Explanatory Note (VSEGEI Cartographic Factory, St. Petersburg, 2014) [in Russian].

4. S. L. Vartanyan, Wrangel Island at the End of the Quaternary: Geology and Paleogeography (Izd. Ivana Limbakha, St. Petersburg, 2007) [in Russian].

5. I. G. Veinbergs, Doctoral Dissertation in Geography (Moscow, 1990).

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