• 责任者：Jiang Xiuyang (College of Geography Science ; Fujian Normal University ; Fuzhou 350007 ; China) ; Li Zhizhong
• 刊名：Marine Geology & Quaternary Geology
• 出版年：2011
• 卷期：31(3)
• 关键词：古气候 ; paleoclimate ; 石笋微层 ; stalagmite microbanding ; 福建 ; Fujian Province
• 页码：p.117-122
• 图表：4 illus., 1 table, 28 refs.
• 分类号：1400
• issnNo：ISSN0256-1492
• isbnNo：CN37-1117/P

The authors present in this paper the ²³⁰Th-dated stalagmite stable isotope record from Tian’e Cave in Fujian Province, Southeast China. This record provides an Asian Monsoon (AM) history during a time interval from 2 100~590 a B.P.. In the TE2 δ¹⁸O record, the long-term decreasing trend correlates well with the Heshang Cave δ¹⁸O change, supporting that the Asian Monsoon intensity is controlled by the migration of Inter-tropical Convergence Zone (ITCZ). A comparison between the stalagmite δ¹⁸O record and the Total Solar Irradiance record provides strong evidence for solar forcing of East Asian monsoon on centennial to multi-decadal time-scales.