期刊
CHINESE SCIENCE BULLETIN
卷 55, 期 21, 页码 2306-2314出版社
SCIENCE PRESS
DOI: 10.1007/s11434-010-3215-3
关键词
Holocene; inner shelf of the East China Sea; mud areas; grain size; clay mineral; elemental analysis; East Asia winter monsoon
资金
- Coastal Investigation and Research Project of China [908-ZC-1-05, 908-02-02-05]
- Marine Public Welfare Research Project [200805063]
- National Natural Science Foundation of China [40431002]
AMS(14)C dating and analysis of grain size, major elements and clay minerals were applied to Core MZ01 from the mud area on the inner shelf of the East China Sea. Based on the environmentally sensitive grain size, clay mineral and major element assemblages, the history of the East Asia winter monsoon since the mid-Holocene could be reconstructed. These three proxies, mean grain size (>9.71 mu m), chemical index of alteration (CIA) and ratio of smectite to kaolinite in particular, show similar fluctuation patterns. Furthermore, 10 extreme values corresponding to the contemporary cooling events could be recognized since the mid-Holocene; these extreme values are likely to have been caused by the strengthening of the East Asia winter monsoon. The cooling events correlated well with the results of the delta O-18 curves of the Dunde ice core and GISP2, which therefore revealed a regional response to global climate change. Four stages of the East Asia winter monsoon were identified, i.e. 8300-6300 a BP, strong and unstable; 6300-3800 a BP, strong but stable; 3800-1400 a BP, weak and unstable; after 1400 a BP, weak but stable.
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