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A High-Resolution Absolute-Dated Late Pleistocene Monsoon Record from Hulu Cave, China
Y. J. Wang,13H. Cheng,2R. L. Edwards,2*Z. S. An,3J. Y. Wu,4C.-C. Shen,5J. A. Dorale6
Oxygen isotope records of five stalagmites from Hulu
Cave near Nanjing bear a remarkable resemblance to oxygen isotope
recordsfrom Greenland ice cores, suggesting that East Asian Monsoon
intensitychanged in concert with Greenland temperature between 11,000 and75,000 years before the present (yr. B.P.). Between 11,000 and30,000 yr. B.P., the timing of changes in the monsoon, as establishedwith 230Th dates, generally agrees with the timing of
temperature changesfrom the Greenland Ice Sheet Project Two (GISP2)
core, which supportsGISP2's chronology in this interval. Our record
links North Atlanticclimate with the meridional transport of heat and
moisture fromthe warmest part of the ocean where the summer East Asian
Monsoonoriginates.
1 College of Geography Science, Nanjing Normal
University, Nanjing 210097, China.
2 Department of
Geology and Geophysics, University of Minnesota, MN 55455, USA.
3 State Key Laboratory of Loess and Quaternary
Geology, Institute of Earth Environment, Chinese Academy of Sciences,
Xi'an 710054, China.
4 State Key Laboratory for
Mineral Deposits Research, Nanjing University, Nanjing 210008, China.
5 Department of Earth Sciences, National Cheng Kung
University, Tainan, Taiwan, China.
6 Department of Geological Sciences,
University of Missouri, Columbia, MO, USA.
*
To whom correspondence should be addressed: E-mail:
edwar001{at}umn.edu
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