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Radiocarbon Chronology of Paleogeographic Events of the Late Pleistocene and Holocene in Russia

Published online by Cambridge University Press:  18 July 2016

P. A. Kaplin ,
A. A. Svitoch  and
O. B. Parunin
P. A. Kaplin
Affiliation:
Laboratory of Recent Sediments and Pleistocene Paleogeography, Moscow State University Leninske Gory, Moscow 119899 Russia
A. A. Svitoch
Affiliation:
Laboratory of Recent Sediments and Pleistocene Paleogeography, Moscow State University Leninske Gory, Moscow 119899 Russia
O. B. Parunin
Affiliation:
Laboratory of Recent Sediments and Pleistocene Paleogeography, Moscow State University Leninske Gory, Moscow 119899 Russia
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Abstract

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14C chronology of Late Pleistocene paleogeographical events in the Black Sea–Caspian Sea region shows that the following transgressions partly correlate with each other: Karangat and Khazarian; Neo-Euxinian and Khvalyn; Holocene and Neo-Caspian. The main climatic events were synchronous in intercontinental Siberia. In the far eastern region, the Middle-Wisconsinan transgression is reflected by Chukotka and western Kamchatka terraces and by submerged ancient shorelines in Primorye.

Type
Geochronology and Paleogeography
Information
Radiocarbon , Volume 35 , Issue 3 , 1993 , pp. 399 - 407
Copyright
Copyright © The American Journal of Science 

References

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