| Инд. авторы: | Solotchina E.P., Sklyarov E.V., Solotchin P.A., Vologina E.G., Sklyarova O.A. |
| Заглавие: | Mineralogy and crystal chemistry of carbonates from the Holocene sediments of Lake Kiran (western Transbaikalia): Connection with paleoclimate |
| Библ. ссылка: | Solotchina E.P., Sklyarov E.V., Solotchin P.A., Vologina E.G., Sklyarova O.A. Mineralogy and crystal chemistry of carbonates from the Holocene sediments of Lake Kiran (western Transbaikalia): Connection with paleoclimate // Russian Geology and Geophysics. - 2014. - Vol.55. - Iss. 4. - P.472-482. - ISSN 1068-7971. - EISSN 1878-030X. |
| Внешние системы: | DOI: 10.1016/j.rgg.2014.03.005; РИНЦ: 21870227; SCOPUS: 2-s2.0-84897476652; WoS: 000334285000005; |
| Реферат: | eng: We present results of research into the Holocene sediments of Lake Kiran, one of the small saline lakes with carbonate sedimentation in western Transbaikalia. The sediments were studied by X-ray diffraction (XRD) analysis, IR spectroscopy, analysis of stable O and C isotopes, laser granulometry, element analysis (SRXFA), etc. By the mathematical modeling of complex XRD patterns of lacustrine sediments, Mg-calcites with different Mg contents and excess-Ca dolomites have been determined in the assemblage of endogenic carbonate minerals.The obtained carbonate record gives an insight into the stratigraphic distribution of endogenic carbonates of the calcite-dolomite series, in which the number and proportion of phases with different Mg contents are determined by the Mg/Ca ratio, salinity, and total alkalinity of the lake water in the past. The abundance of excess-Ca dolomites in the sediments indicates that the lake is of shallow playa type. The mineral composition and crystallochemical structure of carbonates are in high correlation with the data of lithological analysis, results of determination of stable isotopes (518O and 513C), and distribution of some geochemical indicators of sedimentation conditions. Several stages of the lake evolution depending on the regional climatic changes have been recognized. It has been established that the most arid conditions in southern Buryatia were in the Subatlantic. Despite the highly arid climate in the region in the period under study (from 7ka to the present), it underwent fluctuations toward humidification, in particular, at the Atlantic stage (the time of the lake formation) and in the recent decades, up to the present. © 2014.
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| Ключевые слова: | Transbaikalia; Russian Federation; Buryatia; X-ray diffraction; stable isotope; sediment chemistry; saline lake; paleoclimate; mineralogy; infrared spectroscopy; hydrogeochemistry; Holocene; geological record; dolomite; crystal chemistry; carbonate; XRD analysis; Western Transbaikalia; Stable isotopes; Saline lake; Paleoclimate; IR spectroscopy; Holocene; Geochemistry; Carbonates; Bottom sediments; |
| Издано: | 2014 |
| Физ. характеристика: | с.472-482 |