Pleistocene paleoclimatic events in Western and Midlle Siberia during MIS-5
Entailing <sup>230</sup>Th/U and <sup>14</sup>C dating of the Pleistocene key sections of the Western and eastern part of Middle Siberia was registered succession of paleoclimatic events which were obtained by paleobotanic events. This succession was compared with paleoclimatic curve which reflected Greenland ice core (GRIP Summit). In result the paleoclimatic analogues of MIS-5a,d,c on west and MIS-5a,b on east of Western Siberia were detected in Kazantsevian Horizon. Also tracks of paleoclimatic events 5e5-1 were revealed.