HOLOCENE CLIMATE CHANGES IN SOUTHERN WEST SIBERIA BASED ON OSTRACOD ANALYSIS
L.B. Khazin1, I.V. Khazina1, S.K. Krivonogov2,3, Ya.V. Kuzmin2,4, A.A. Prokopenko5, S. Yi6, G.S. Burr7
1A.A. Trofimuk Institute of Petroleum Geology and Geophysics, Siberian Branch of the Russian Academy of Sciences, pr. Akademika Koptyuga 3, Novosibirsk, 630090, Russia
2V.S. Sobolev Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of Sciences, pr. Akademika Koptyuga 3, Novosibirsk, 630090, Russia
3Novosibirsk State University, ul. Pirogova 2, Novosibirsk, 630090, Russia
4Tomsk State University, ul. Lenina 35, Tomsk, 634050 Russia
5University of Cologne, 100 Albertus-Magnus-Platz, D-50923, Cologne, Germany
6Korean Institute of Geoscience and Mineral Resources, Gwang-ro 124, Yuseong-gu, 305-350, Daejeon, South Korea
7University of Arizona, Tucson, AZ 85721, USA
Keywords: Ostracods, Holocene, paleontology, climatostratigraphy, paleoecology, southern West Siberia
Abstract
The study presents a summary of the latest data on ostracod microfaunas from Middle-Upper Holocene lacustrine deposits of southern West Siberia collected from lakes Malye Chany, Bol’shaya Lozhka, Beloe, and paleolake Chicha. A total of 28 ostracod species were identified. The identified ostracod assemblages reveal local variations in the lake ecosystems as well as general trends, which can be correlated with both regional and global climate changes. A cooling episode during the second half of the Subboreal is marked by the transition from a warm-water mesohaline assemblage to cold-water candonid ostracods at ca. 3.4 cal ka BP. The widespread occurrence of mesopolythermophilic ostracod species at 1.9-0.6 cal ka BP indicates the end of cooling and lowering of lake-water level. From 0.6 cal ka BP to present, the ostracod assemblages area characterized by the high specific diversity, which is probably an indication of the increased variability of aquatic ecosystems due to fluctuations in salinity and water levels of the lakes. Climate changes identified by ostracod assemblages are consistent with the climatic trend constrained by early palynological studies.
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