A.V. Darin, I.A. Kalugin, M.A. Maksimov, G.A. Tretyakov, Ya.V. Rakshun
Issue: 2
, Volume: 77
, Уear of publication: 2013
Serial edition: Bulletin of the Russian Academy of Sciences: Physics
Pages: 185-187
Abstract
The interannual and interseasonal variations in the trace element composition of annual layers in bottom sediments of Lake Shira (Khakassia) are studied by means of X-ray scanning microanalysis with synchrotron radiation on the VEPP-3 (Novosibirsk) and BESSY-II (Berlin) storage rings. The relationship between sediment composition and weather and climatic conditions is established. The possibility of paleoclimatic reconstructions with annual temporal resolution is demonstrated.
