The isotopic and material composition of bottom deposits, examined in the Kara-Bogaz-Gol Gulf, Lake Issyk-Kul, and the Aral Sea, is considered. The obtained data are used to characterize variations in the regime of the water bodies in the Holocene.
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ACKNOWLEDGMENTS This study was conducted in accordance with the research programs of the Water Problems Institute, Russian Academy of Sciences; All-Russia Institute of Hydrogeology and Engineering Geology; Institute of Water and Power Problems, Academy of Sciences of Kyrgyzstan; and Great Lakes Observatory, University of Minnesota, and was supported by the INCO– COPERNICUS Project IC-150CT96-0112, European Union.
Copyright 2008 Elsevier B.V., All rights reserved.
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