A HOLOCENE CLIMATIC RECORD INDICATED BY GEOCHEMICAL INDICATORS AND GRANULOMETRY FROM BANNOE LAKE IN THE SOUTHERN URAL

Abstract

The work is devoted to the geochemical and granulometry study of the Bannoe lake sediments. The main aim of this investigation is to identify the events and trends of environmental and climate changes in the Late Quaternary. The present study of grain size and organic geochemistry of core sediments from Bannoe Lake provides paleoclimatological record of South Ural for the Holocene Period.