A high-resolution absolute-dated Late Pleistocene monsoon record from Hulu Cave, China

Oxygen isotope records of five stalagmites from Hulu Cave near Nanjing bear a remarkable resemblance to oxygen isotope records from Greenland ice cores, suggesting that East Asian Monsoon intensity changed in concert with Greenland temperature between 11,000 and 75,000 years before the present (yr....

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Bibliographic Details
Published in:Science
Main Authors: Wang, YJ, Cheng, H, Edwards, RL, An, ZS, Wu, JY, Shen, CC, Dorale, JA
Format: Article in Journal/Newspaper
Language:English
Published: AMER ASSOC ADVANCEMENT SCIENCE 2001
Subjects:
Science & Technology - Other Topics
NORTH-ATLANTIC
GREENLAND ICE
CLIMATE
PALEOCLIMATE
INSTABILITY
HISTORY
EVENTS
Multidisciplinary Sciences
Greenland
Hulu
Greenland ice cores
Greenland Ice Sheet Project
Ice Sheet
North Atlantic
Online Access:http://ir.ieecas.cn/handle/361006/11819
https://doi.org/10.1126/science.1064618
Description
Summary:Oxygen isotope records of five stalagmites from Hulu Cave near Nanjing bear a remarkable resemblance to oxygen isotope records from Greenland ice cores, suggesting that East Asian Monsoon intensity changed in concert with Greenland temperature between 11,000 and 75,000 years before the present (yr. B.P.). Between 11,000 and 30,000 yr. B.P., the timing of changes in the monsoon, as established with Th-230 dates, generally agrees with the timing of temperature changes from the Greenland Ice Sheet Project Two (GISP2) core, which supports GISP2's chronology in this interval. Our record links North Atlantic climate with the meridional transport of heat and moisture from the warmest part of the ocean where the summer East Asian Monsoon originates.

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