CORRELATION OF STRATOTYPE SECTIONS OF THE KARGINSKY AND KAZANTSEVSKY HORIZONS (NORTH OF WEST SIBERIA)
The following are compared: the altitudinal position of the sections, lithology, remains of macro - and microfauna, dating by OSL, EPR, and U-Th. The sections of the Karginsky and Kazantsevsky stratotypes are deposits of a single warm - water marine transgression, which can be correlated with the most of the marine isotope stage 5. In the north of Western Siberia, the deposits of the transgression are unevenly distributed, usually in some areas deposits of some stage are exposed, complete sections are absent, which entails behind itself the allocation of numerous suites.