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Hydroclimate variability of central Indo-Pacific region during the Holocene
Chawchai, Sakonvan1; Tan, Liangcheng2,3,4; Lowemark, Ludvig5; Wang, Hao-Cheng5,6,7; Yu, Tsai-Luen5,6,8; Chung, Yun-Chuan5,6,7; Mii, Horng-Sheng9; Liu, Guangxin10; Blaauw, Maarten11; Gong, Shou-Yeh12; Wohlfarth, Barbara13,14; Shen, Chuan-Chou5,6,7
通讯作者Chawchai, Sakonvan(sakonvan.c@chula.ac.th) ; Shen, Chuan-Chou(river@ntu.edu.tw)
2021-02-01
发表期刊QUATERNARY SCIENCE REVIEWS
ISSN0277-3791
卷号253页码:12
摘要Here we present a decadal-resolved hydroclimate record covering the past 11 thousand years based on delta O-18 data of three stalagmites from Kiang Cave (TK) on the Thai-Malay Peninsula, southern Thailand. The delta O-18 values indicate wetter conditions/more rainfall during the early Holocene from 11 to 7 thousand years before present (kyr BP). A large increase of 2 parts per thousand in delta O-18 is observed from 7.0 to 6.0 kyr BP, indicating a millennial drying period followed by drought conditions between 6.0 and 5.2 kyr BP. After a long hiatus (5.2-2.7 kyr BP), delta O-18 data show a millennium-long trend toward dry conditions. An abrupt positive change of 0.8-1.0 parts per thousand in delta O-18 is noticed between 8.29 and 8.17 kyr BP, reflecting the 8.2-ka event; however, the amplitude of the delta O-18 shift is much smaller comparing to that of the event of 6.0-5.2 kyr BP. On orbital time-scales, the TK record agrees with insolation-dominated speleothem records in the Asian-Australian monsoon realm. Noticeable inconsistencies among records in the Southeast Asia region (between 8 degrees N and 4 degrees N-8 degrees S) have been documented on multi-centennial scales. Lower delta O-18 values are likely associated with the mean position of the Intertropical Convergence Zone (ITCZ). A new reconstruction of Holocene ITCZ shifts index within the central Indo-Pacific region, based on stalagmite delta O-18 records from Kiang Cave (8 degrees N) and Liang Luar Cave (8 degrees S), shows that the ITCZ played an important role in hydroclimate variability in the Asian-Australian monsoon regions. The southward shift of the ITCZ in the central Indo-Pacific region, controlled by the interhemispheric extratropical insolation gradient, may strongly correlate with the El Nino-Southern Oscillation (ENSO) activities in the Holocene. (C) 2020 Elsevier Ltd. All rights reserved.
关键词Stalagmite Thai-Malay peninsula Holocene ITCZ Central Indo-Pacific region
DOI10.1016/j.quascirev.2020.106779
关键词[WOS]INTERTROPICAL CONVERGENCE ZONE ; GLACIAL LAKE AGASSIZ ; ASIAN MONSOON ; ISOTOPIC COMPOSITION ; MILLENNIAL-SCALE ; HIGH-RESOLUTION ; SUMMER MONSOON ; GLOBAL MONSOON ; CLIMATE-CHANGE ; EL-NINO
收录类别SCI ; SCI
语种英语
资助项目DPST Research grant, Thailand[042/2558] ; Science Vanguard Research Program of the Ministry of Science and Technology (MOST)[108-2119-M-002-012] ; Science Vanguard Research Program of the Ministry of Science and Technology (MOST)[109-2123-M-002-001] ; National Taiwan University[109L8926] ; Higher Education Sprout Project of the Ministry of Education, Taiwan ROC[109L901001] ; Ministry of Science and Technology (MOST)[106-2116-M-002 -021] ; Strategic Priority Research Program of Chinese Academy of Sciences, China[XDB40000000] ; Swedish Research Council (VR)[621-2008-2855] ; Swedish Research Council (VR)[621-2011-4684] ; Swedish Research Council (VR)[348-2008-6071]
WOS研究方向Physical Geography ; Geology
项目资助者DPST Research grant, Thailand ; Science Vanguard Research Program of the Ministry of Science and Technology (MOST) ; National Taiwan University ; Higher Education Sprout Project of the Ministry of Education, Taiwan ROC ; Ministry of Science and Technology (MOST) ; Strategic Priority Research Program of Chinese Academy of Sciences, China ; Swedish Research Council (VR)
WOS类目Geography, Physical ; Geosciences, Multidisciplinary
WOS记录号WOS:000610835200021
出版者PERGAMON-ELSEVIER SCIENCE LTD
引用统计
被引频次:9[WOS]   [WOS记录]     [WOS相关记录]
文献类型期刊论文
条目标识符http://ir.ieecas.cn/handle/361006/16041
专题现代环境研究室
第四纪科学与全球变化卓越创新中心
通讯作者Chawchai, Sakonvan; Shen, Chuan-Chou
作者单位1.Chulalongkorn Univ, Fac Sci, Dept Geol, Morphol Earth Surface & Adv Geohazards Southeast, Bangkok 10330, Thailand
2.Chinese Acad Sci, Inst Earth Environm, State Key Lab Loess & Quaternary Geol, Xian 710075, Peoples R China
3.Xi An Jiao Tong Univ, Inst Global Environm Change, Xian 710049, Peoples R China
4.Chinese Acad Sci, Ctr Excellence Quaternary Sci & Global Change, Xian 710061, Peoples R China
5.Natl Taiwan Univ, Dept Geosci, Taipei 10617, Taiwan
6.Natl Taiwan Univ, Dept Geosci, High Precis Mass Spectrometry & Environm Change L, Taipei 10617, Taiwan
7.Natl Taiwan Univ, Res Ctr Future Earth, Taipei 10617, Taiwan
8.Natl Acad Marine Res, Marine Ind & Engn Res Ctr, Kaohsiung 80661, Taiwan
9.Natl Taiwan Normal Univ, Dept Earth Sci, Taipei 10617, Taiwan
10.Yunnan Univ, Res Ctr Earth Syst Sci, Kunming 650500, Yunnan, Peoples R China
11.Queens Univ Belfast, Sch Nat & Built Environm, Archaeol & Palaeoecol, Belfast BT7 1NN, Antrim, North Ireland
12.Natl Museum Nat Sci, Dept Geol, Taichung 40419, Taiwan
13.Stockholm Univ, Dept Geol Sci, S-10691 Stockholm, Sweden
14.Stockholm Univ, Bolin Ctr Climate Res, S-10691 Stockholm, Sweden
推荐引用方式
GB/T 7714
Chawchai, Sakonvan,Tan, Liangcheng,Lowemark, Ludvig,et al. Hydroclimate variability of central Indo-Pacific region during the Holocene[J]. QUATERNARY SCIENCE REVIEWS,2021,253:12.
APA Chawchai, Sakonvan.,Tan, Liangcheng.,Lowemark, Ludvig.,Wang, Hao-Cheng.,Yu, Tsai-Luen.,...&Shen, Chuan-Chou.(2021).Hydroclimate variability of central Indo-Pacific region during the Holocene.QUATERNARY SCIENCE REVIEWS,253,12.
MLA Chawchai, Sakonvan,et al."Hydroclimate variability of central Indo-Pacific region during the Holocene".QUATERNARY SCIENCE REVIEWS 253(2021):12.
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