RADIOCARBON CHRONOLOGY OF PALEOGEOGRAPHIC EVENTS OF THE LATE PLEISTOCENE AND HOLOCENE IN RUSSIA

C-14 chronology Of Late Pleistocene paleogeographical events in the Bl ack Sea-Caspian Sea region shows that the following transgressions par tly correlate with each other: Karangat and Khazarian; Neo-Euxinian an d Khvalyn; Holocene and Neo-Caspian. The main climatic events were syn chronous in intercontinental Siberia. In the far eastern region, the M iddle-Wisconsinan transgression is reflected by Chukotka and western K amchatka terraces and by submerged ancient shorelines in Primorye.