• 责任者：Liu Dianbing (College of Geography Sciences ; Nanjing Normal University ; Nanjing 210023 ; China)
• 刊名：Geological Review
• 出版年：2013
• 卷期：59(5)
• 关键词：石笋微层 ; stalagmite microbanding ; 地质年代学 ; geochronology
• 页码：p.941-952
• 图表：143 refs.
• 分类号：1300
• issnNo：ISSN0371-5736
• isbnNo：CN11-1952/P

     The cave deposits, especially the stalagmites, are widely distributed and precisely dated terrestrial archives for paleoclimate studies, the stable oxygen isotope sequences from which were believed to duplicate well between spatially-seperated caves. Nevertheless, climatic interpretation of oxygen isotope from the stalagmites, particularly in the Asian monsoon regions, has been challenged due to insufficient quantitative studies. Thus, previous investigations on quantitative studies of speleothem indicators, i.e. δ18O, δ13C, trace element, layer thickness and growth dynamics are summarized in this issues are tentatively put forward involving calibration paper. Compared with other geologic records, some urgent with monitoring data, multi-proxy studies and combination with the regional tree-ring data. The aim for this paper is stalagmite proxies and climate, and promote the regional to further understand the quantitative relationship between and global comparison with the speleothem records.