THE RATE OF SEDIMENTATION IN LAKE ARAKHLEI (central Transbaikalia), FROM RADIOGEOCHEMICAL AND PALYNOLOGICAL DATA
a:2:{s:4:"TEXT";s:148:"A.B. Ptitsyn1, G. Chu2, A.V. Dar’in3, L.V. Zamana1, I.A. Kalugin3, S.A. Reshetova1";s:4:"TYPE";s:4:"html";}
1Institute of Natural Resources, Ecology and Cryology, Siberian Branch of the Russian Academy of Sciences, ul. Nedorezova 16a, Chita, 672014, Russia
2Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, China
3V.S. Sobolev Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of Sciences, pr. Akademika Koptyuga 3, Novosibirsk, 630090, Russia
Keywords: Sediment genesis, lake, bottom sediments, radioisotope method, palynology
Abstract
Chemical, radioisotopic, and palynological studies of the bottom sediments of mesotrophic Lake Arakhlei have been carried out for paleoclimatic reconstructions and estimation of the sedimentation rate.
DOI: http://dx.doi.org/10.1016/j.rgg.2014.01.018
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