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

14 C 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 intercon...

Full description

Bibliographic Details
Published in:Radiocarbon
Main Authors: Kaplin, P. A., Svitoch, A. A., Parunin, O. B.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1993
Subjects:
General Earth and Planetary Sciences
Archeology
Chukotka
Kamchatka
Siberia
Online Access:http://dx.doi.org/10.1017/s0033822200060410
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0033822200060410
Description
Summary:14 C 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.

Similar Items