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An oxygen isotope record from Lake Xiarinur in Inner Mongolia since the last deglaciation and its implication for tropical monsoon change

文献类型：期刊论文

作者Sun, Qing1; Chu, Guoqiang2; Xie, Manman1; Zhu, Qingzeng2; Su, Youliang3; Wang, Xisheng4
刊名GLOBAL AND PLANETARY CHANGE
出版日期2018-04-01
卷号163页码:109-117
ISSN号0921-8181
DOI10.1016/j.gloplacha.2018.01.017
文献子类Article
英文摘要We present a high-resolution oxygen isotope record from authigenic carbonate (delta O-18(carb)) from Lake Xiarinur (Inner Mongolia) since the last deglaciation. The lake is located at the modem northern limit of the monsoon, and is therefore sensitive to the extension of the East Asian summer monsoon. Based on calibration against the instrumental record, the delta O-18(car) variation has been interpreted as changes in atmospheric circulation pattern on decadal time scales. On longer time scales, the delta O-18(carb) in lake sediments could be mainly regulated by the relative contribution of nearby (remote) water-vapor sources associated with subtropical (tropical) monsoon through changes in the distance from sources to the site of precipitation. Increased remote water vapors from tropical monsoon would lead to lighter isotope value in our study site. Through time the delta O-18(carb) record in Lake Xiarinur indicate a notable weak tropical monsoon during the Younger Dryas, a gradual increasing monsoon from the early Holocene and weakening monsoon after the middle Holocene. Oxygen isotope records from lakes and stalagmite in the Asian monsoon region across different localities show a general similar temporal pattern since the last deglaciation, and highlight a fundamental role of the tropical monsoon.
WOS关键词HOLOCENE ASIAN MONSOON ; NORTHERN CHINA ; MILLENNIAL TIMESCALES ; EL-NINO ; CLIMATE ; PRECIPITATION ; VARIABILITY ; SEDIMENTS ; RAINFALL ; QINGHAI
WOS研究方向Physical Geography ; Geology
语种英语
WOS记录号WOS:000430771400010
出版者ELSEVIER SCIENCE BV
资助机构National Natural Science Foundation of China(41371219 ; National Natural Science Foundation of China(41371219 ; China Geological Survey(YYWF201618 ; China Geological Survey(YYWF201618 ; 41272198 ; 41272198 ; 12120113015400) ; 12120113015400) ; 41274047) ; 41274047) ; National Natural Science Foundation of China(41371219 ; National Natural Science Foundation of China(41371219 ; China Geological Survey(YYWF201618 ; China Geological Survey(YYWF201618 ; 41272198 ; 41272198 ; 12120113015400) ; 12120113015400) ; 41274047) ; 41274047) ; National Natural Science Foundation of China(41371219 ; National Natural Science Foundation of China(41371219 ; China Geological Survey(YYWF201618 ; China Geological Survey(YYWF201618 ; 41272198 ; 41272198 ; 12120113015400) ; 12120113015400) ; 41274047) ; 41274047) ; National Natural Science Foundation of China(41371219 ; National Natural Science Foundation of China(41371219 ; China Geological Survey(YYWF201618 ; China Geological Survey(YYWF201618 ; 41272198 ; 41272198 ; 12120113015400) ; 12120113015400) ; 41274047) ; 41274047)
源URL[http://ir.iggcas.ac.cn/handle/132A11/88277]  
专题地质与地球物理研究所_中国科学院新生代地质与环境重点实验室
通讯作者Sun, Qing; Chu, Guoqiang
作者单位1.Natl Res Ctr Geoanal, Beijing 100037, Peoples R China
2.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Cenozo Geol & Environm, Beijing 100029, Peoples R China
3.China Earthquake Adm, Inst Geophys, Beijing 100081, Peoples R China
4.Chinese Acad Geol Sci, Inst Geomech, MLR Key Lab Paleomagnetism & Paleotecton Reconst, Beijing 100081, Peoples R China
推荐引用方式
GB/T 7714		 Sun, Qing,Chu, Guoqiang,Xie, Manman,et al. An oxygen isotope record from Lake Xiarinur in Inner Mongolia since the last deglaciation and its implication for tropical monsoon change[J]. GLOBAL AND PLANETARY CHANGE,2018,163:109-117.
APA Sun, Qing,Chu, Guoqiang,Xie, Manman,Zhu, Qingzeng,Su, Youliang,&Wang, Xisheng.(2018).An oxygen isotope record from Lake Xiarinur in Inner Mongolia since the last deglaciation and its implication for tropical monsoon change.GLOBAL AND PLANETARY CHANGE,163,109-117.
MLA Sun, Qing,et al."An oxygen isotope record from Lake Xiarinur in Inner Mongolia since the last deglaciation and its implication for tropical monsoon change".GLOBAL AND PLANETARY CHANGE 163(2018):109-117.

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来源：地质与地球物理研究所

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