Radiocarbon chronology of paleogeographic events of the late Pleistocene and Holocene in Russia

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Abstract

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. -Authors

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Kaplin, P. A., Svitoch, A. A., & Parunin, O. B. (1993). Radiocarbon chronology of paleogeographic events of the late Pleistocene and Holocene in Russia. Radiocarbon, 35(3), 399–407. https://doi.org/10.1017/S0033822200060410

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