Abstract
As one of the lakes on the Yunnan-Guizhou plateau, Lake Chenghai, which is a typical closed lake with the precipitation accounting for one-third or more of the annual water input, has a high total salinity (almost like a saline lake). The inorganic C, O isotopic composition of lake sediments bears much sensitive information about environmental change in the catchment, while their correlations revealed the hydrological conditions under which the lake was closed. Their compositional variations are controlled by temperature, precipitation, photosynthesis, dissolving equilibrium of the carbonate system and hydrological condition. According to our research on inorganic C, O isotopic composition of Lake Chenghai sediments, we investigated the environmental change of this catchment several decades ago. The results showed that Lake Chenghai has kept good hydrological closing conditions in the past several decades, as indicated by the good correlation of inorganic C, O isotopic composition of sediments; and that the environmental change in this catchment shows a tendency of periodical evolution on a 10−11-years scale, although the signal noise is relatively high at the bottom of the sediment core. And we also can extend C, O isotopes, a sensitive environmental indicator, to nearly saline lake environments with a high degree of mineralization.
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Chen Jing'an, Wan Guojiang, Tang Degui, and Huang Ronggui, 2000, The response of sediment particle size and isotope to modern climate change of Erhai Lake [J]: Natural Science Progress, v. 3, p. 253–259 (in Chinese).
Herczeg, A. L. and R. G. Fairbands, 1987, Anomalous carbon isotope fractionation between atmospheric CO2 and dissolved inorganic carbon induced by intense photosynthesis [J]: Geochimica et Cosmochimica Acta, v. 51, p. 895–899.
Li Hongchun and T. L. Ku, 1997, δ13C-δ18O covariance as a paleo-hydrological indicator for closed basin lakes [J]: Paleeo-geography, Palaeo-climatology, Palaeo-ecology, v. 133, p. 69–80.
Schelske Claire, L. and Hodell David, 1991, Recent changes in productivity and climate of lake Ontario detected by isotopic analysis of sediments [J]: Limnology, Oceanography, v. 36, n. 5, p. 961–975.
Stuiver, M, 1970, Oxygen and carbon isotope ratio of fresh-water carbonates as climatic indicators [J]: Journal of Geophysics Research, v. 75, p. 5247–5257.
Talbot, M. R., 1980, A review of the palaeo-hydrological interpretation of carbon and oxygen isotopic ratios in primary lacustrine carbonates [J]: Chemical Geology, v. 80, p. 261–279.
Wang Fushun, Wan Guojiang, and Huang Ronggui, 2000, The progress of environmental record of cave sediments [J]: Geological Geochemistry, v. 28, n. 3, p. 83–87.
Wang Shumin and Dou Hongsheng, 1998, Lake in China [M]: Beijing, Science Press, 580p.
Yu Yufu et al., 1994, Environmental chemistry [M]: Shanghai, Fudan University Press, 325p.
Zhao Lunshan and Zhang Benren, 1988, Geochemistry [M]: Beijing, Geological Publishing House, 404p.
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Fushun, W., Guojiang, W., Congqiang, L. et al. The correlation of inorganic C, O isotopic values for Lake Chenghai sediments and its environmental implications. Chin. J. Geochem. 21, 186–192 (2002). https://doi.org/10.1007/BF02873777
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DOI: https://doi.org/10.1007/BF02873777