• 责任者：Cui Yingfang (College of Geography Science ; Nanjing Normal University ; Nanjing 210046 ; China) ; Wang Yongjin
• 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 ; 末次冰期 ; last glacial age ; 亚洲 ; Asia ; 极地 ; polar region
• 页码：p.101-107
• 图表：4 illus., 1 table, 36 refs.
• 分类号：1400
• issnNo：ISSN0256-1492
• isbnNo：CN37-1117/P

A 10-year resolution oxygen isotope record from the Wulu Cave, based on 9 precise ²³⁰Th dates and 1 317 oxygen isotope measurements, provides a detailed history of the Asian Monsoon from 39.1 ka B.P. to 29.2 ka B.P., spanning the marine isotope stage 3. The fairly good replication of δ¹⁸O signal between the Wulu Cave and the Hulu Cave during the same growth periods indicates that the δ¹⁸O signals well recorded climatic changes and the changes in the monsoon system were are similar over a large area of China. The comparison between the Wulu Cave and Greenland ice core record indicates that the frequency of centennial and millennial scale monsoon events match well with the temperature in North high latitude.