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Climatic Signals Recorded in Shells in Xingcuo Lake, Eastern Tibetan Plateau

Climatic Signals Recorded in Shells in Xingcuo Lake, Eastern Tibetan Plateau
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摘要 This paper presents the results of determining trace elements and δ 13C, δ 18O in Gyraulus sibirica shell continuously preserved in Xingcuo Lake sediments in the recent 50 years. By coupling these indexes and instrumental meteorological data on its basin to determine the relations among them, we probed quantitatively the climatic signals recorded in Xingcuo Lake sediments. The results showed that gastropod shells in Xingcuo Lake were formed in warm seasons; that trace elements, and stable isotope in shells just recorded the climatic signals of the warm seasons instead of that of the whole year; that Mg/Ca ratio and δ 18O proxy had certain correlation with air temperature in warm seasons, when the δ 18O proxy was more sensitive; with the average ratio of them being 0.28×10 -3/℃ and the variation rate dδ 18O/dT being 1.64×10 -3/℃; that the Sr/Ca ratio and δ 13C proxy, especially Sr/Ca ratio, had close correlation; and that dSr/Ca/dP was -0.045/mm. This paper presents the results of determining trace elements and δ 13C, δ 18O in Gyraulus sibirica shell continuously preserved in Xingcuo Lake sediments in the recent 50 years. By coupling these indexes and instrumental meteorological data on its basin to determine the relations among them, we probed quantitatively the climatic signals recorded in Xingcuo Lake sediments. The results showed that gastropod shells in Xingcuo Lake were formed in warm seasons; that trace elements, and stable isotope in shells just recorded the climatic signals of the warm seasons instead of that of the whole year; that Mg/Ca ratio and δ 18O proxy had certain correlation with air temperature in warm seasons, when the δ 18O proxy was more sensitive; with the average ratio of them being 0.28×10 -3/℃ and the variation rate dδ 18O/dT being 1.64×10 -3/℃; that the Sr/Ca ratio and δ 13C proxy, especially Sr/Ca ratio, had close correlation; and that dSr/Ca/dP was -0.045/mm.
出处 《Chinese Journal of Oceanology and Limnology》 SCIE CAS CSCD 2003年第1期10-17,共8页 中国海洋湖沼学报(英文版)
基金 ThisworkwasfundedbytheKeyInnovationProjectoftheChineseAcademyofSciences(KZCX1 -1 0 -0 2 ) ,theNaturalSci enceFundationofChina (Grant:4 980 30 0 1 )andNational"973"projectandCASTibetResearch (No:G1 9980 4 0 80 0 ) .
关键词 Xingcuo Lake eastern Tibetan Plateau trace elements stable isotopes 气候标志 西藏高原 示踪元素 稳定同位素 湖泊沉积物 气候变化 碳同位素 氧同位素
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