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

被引：2580

作者：

Wang, YJ

Cheng, H

Edwards, RL ^{[1
]}

An, ZS

Wu, JY

Shen, CC

Dorale, JA

机构：

[1] Univ Minnesota, Dept Geol & Geophys, Minneapolis, MN 55455 USA

[2] Nanjing Normal Univ, Coll Geog Sci, Nanjing 210097, Peoples R China

[3] Chinese Acad Sci, Inst Earth Environm, State Key Lab Loess & Quaternary Geol, Xian 710054, Peoples R China

[4] Nanjing Univ, State Key Lab Mineral Deposits Res, Nanjing 210008, Peoples R China

[5] Natl Cheng Kung Univ, Dept Earth Sci, Tainan, Taiwan

[6] Univ Missouri, Dept Geol Sci, Columbia, MO USA

来源：

SCIENCE | 2001年 / 294卷 / 5550期

关键词：

D O I：

10.1126/science.1064618

中图分类号：

O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];

学科分类号：

07 ; 0710 ; 09 ;

摘要：

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.

引用

页码：2345 / 2348

页数：4

共 34 条

[21] Oxygen and carbon isotopic characteristics of rainwater, drip water and present speleothems in a cave in Guilin area, and their environmental meanings [J].