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...
Published in: | Radiocarbon |
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Main Authors: | , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Cambridge University Press (CUP)
1993
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Subjects: | |
Online Access: | http://dx.doi.org/10.1017/s0033822200060410 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0033822200060410 |
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. |
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