Climatic signals recorded in shells in Xingcuo Lake, eastern Tibetan Plateau
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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
海洋湖沼学报(英文)2003年21卷第1期 页码:10-17
Affiliations:
1. Nanjing Institute of Geog. & Limn. Chinses Academy Sciences
2. Department of Atmospheric Observing Engineering IM PLAUST
3. Forschungszentrum Juelich
Author bio:
Funds:
This work was funded by the Key Innovation Project of the Chinese Academy of Sciences (KZCX1-10-02), the Natural Science Fundation of China (Grant: 49803001) and National “973” project and CAS Tibet Research (No: G1998040800).
Climatic signals recorded in shells in Xingcuo Lake, eastern Tibetan Plateau[J]. 海洋湖沼学报(英文), 2003,21(1):10-17.
Jinglu, W., Hong, Y., Schleser, G.H. et al. Climatic signals recorded in shells in Xingcuo Lake, eastern Tibetan Plateau., Chin. J. Ocean. Limnol. 21, 10–17 (2003). https://doi.org/10.1007/BF02842756
Climatic signals recorded in shells in Xingcuo Lake, eastern Tibetan Plateau[J]. 海洋湖沼学报(英文), 2003,21(1):10-17. DOI: 10.1007/BF02842756.
Jinglu, W., Hong, Y., Schleser, G.H. et al. Climatic signals recorded in shells in Xingcuo Lake, eastern Tibetan Plateau., Chin. J. Ocean. Limnol. 21, 10–17 (2003). https://doi.org/10.1007/BF02842756DOI:
Climatic signals recorded in shells in Xingcuo Lake, eastern Tibetan Plateau
摘要
Abstract
This paper presents the results of determining trace elements and σ13C
σ18O inGyraulus 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 σ18 proxy had certain correlation with air temperature in warm seasons
when the σ18 proxy was more sensitive; with the average ratio of them being 0.28×10−3/1C and the variation rate dσ18O/dT being 1.64×10−3/1C; that the Sr/Ca ratio and σ13C proxy
especially Sr/Ca ratio
had close correlation; and that dSr/Ca/dP was −0.045/mm.
关键词
Keywords
references
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