Abstract

The results of the investigation of three permafrost cores from 3.6 Myr old Lake Elgygytgyn impact crater are presented here. Paleobotanical reconstructions are based on palinological studies and involve mostly late glacial time and Holocene. Our results are more detailed in comparison to the data based on lake sediments studies due to very low sedimentation rate in Lake Elgygytgyn. The age models rely on radiocarbon dates and also on correlations between our results with previously published data.

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