IEECAS OpenIR  > 现代环境研究室
High precise dating on the variation of the Asian summer monsoon since 37 ka BP
Li, Ting-Yong1; Wu, Yao2; Shen, Chuan-Chou3; Li, Jun-Yun2; Chiang, Hong-Wei8; Lin, Ke3,9; Tan, Liang-Cheng4; Jiang, Xiu-Yang5; Cheng, Hai6,7; Edwards, R. Lawrence7
通讯作者Li, Ting-Yong(cdlity@163.com) ; Shen, Chuan-Chou(river@ntu.edu.tw)
2021-04-30
发表期刊SCIENTIFIC REPORTS
ISSN2045-2322
卷号11期号:1页码:14
摘要Comprehensive comparison of paleoclimate change based on records constrained by precise chronology and high-resolution is essential to explore the correlation and interaction within earth climate systems. Here, we propose a new stalagmite-based multidecadal resolved Asian summer monsoon (ASM) record spanning the past thirty-seven thousand years (ka BP, before ad 1950) from Furong Cave, southwestern China. This record is consistent with the published Chinese stalagmite sequences and shows that the dominant controls of the ASM dynamics include not only insolation and solar activity but also suborbital-scale hydroclimate events in the high latitudes of the northern hemisphere, such as the Heinrich events, BOlling-AllerOd (BA), and Younger Dryas (YD). Benefit from the unprecedented accurate chronology, the timings of these events are precisely dated, with uncertainties of, at most, 40 years (2 sigma). The onset of the weak ASM during the YD began at 12.92 ka BP and lasted for 430 years. The occurrence of the 200-yr Older Dryas during the BA period was dated from 13.87 to 14.06 ka BP. The durations of the three Heinrich (H) events, H1, H2, and H3, are 14.33-18.29, 23.77-24.48, and 28.98-30.46 ka BP, respectively. Furong record shows surprisingly variable onset transitions of 980, 210, and 40 years for the corresponding weak ASM events. These discrepancies suggest different influences of the H events on ASM dynamics. During the periods of H 1-3, the obvious difference between our Furong record and NGRIP delta O-18 record indicated the decoupling correlation between the mid-low latitudes and high latitudes. On the other hand, synchronous climate change in high and low latitudes suggests another possibility which different to the dominant role of Northern high latitudes in triggering global climate change. Our high quality records also indicate a plausible different correlation between the high and mid-low latitudes under glacial and inter-glacial background, especially for the ASM regimes.
DOI10.1038/s41598-021-88597-7
关键词[WOS]ABRUPT CLIMATE-CHANGE ; NORTH-ATLANTIC OCEAN ; HIGH-RESOLUTION ; GREENLAND TEMPERATURE ; MILLENNIAL-SCALE ; ENSO VARIABILITY ; HEINRICH EVENTS ; FURONG CAVE ; HOLOCENE ; RECORD
收录类别SCI ; SCI
语种英语
资助项目National Natural Science Foundation of China (NSFC)[41772170] ; National Natural Science Foundation of China (NSFC)[42011530078] ; Fundamental Research Funds for the Central Universities, China[XDJK2017A010] ; Fundamental Research Funds for the Central Universities, China[XDJK2020D005] ; NSFC[41888101] ; U.S. NSF[1702816] ; Science Vanguard Research Program of the Ministry of Science and Technology[108-2119-M-002-012] ; National Taiwan University[105R7625] ; Higher Education Sprout Project of the Ministry of Education[108L901001]
WOS研究方向Science & Technology - Other Topics
项目资助者National Natural Science Foundation of China (NSFC) ; Fundamental Research Funds for the Central Universities, China ; NSFC ; U.S. NSF ; Science Vanguard Research Program of the Ministry of Science and Technology ; National Taiwan University ; Higher Education Sprout Project of the Ministry of Education
WOS类目Multidisciplinary Sciences
WOS记录号WOS:000656497500023
出版者NATURE RESEARCH
引用统计
被引频次:18[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/361006/16685
专题现代环境研究室
通讯作者Li, Ting-Yong; Shen, Chuan-Chou
作者单位1.Yunnan Normal Univ, Fac Geog, Yunnan Key Lab Plateau Geog Proc & Environm Chang, Kunming 650500, Yunnan, Peoples R China
2.Southwest Univ, Sch Geog Sci, Chongqing Key Lab Karst Environm, Chongqing 400715, Peoples R China
3.Natl Taiwan Univ, Dept Geosci, High Precis Mass Spectrometry & Environm Change L, Taipei 10617, Taiwan
4.Chinese Acad Sci, Inst Earth Environm, State Key Lab Loess & Quaternary Geol, Xian 710075, Peoples R China
5.Fujian Normal Univ, Coll Geog Sci, Fuzhou 350007, Peoples R China
6.Xi An Jiao Tong Univ, Inst Global Environm Change, Xian 710049, Peoples R China
7.Univ Minnesota, Dept Earth & Environm Sci, Minneapolis, MN 55455 USA
8.Natl Taiwan Univ, Dept Geosci, Taipei 10617, Taiwan
9.Nanyang Technol Univ, Earth Observ Singapore, Singapore 639798, Singapore
推荐引用方式
GB/T 7714
Li, Ting-Yong,Wu, Yao,Shen, Chuan-Chou,et al. High precise dating on the variation of the Asian summer monsoon since 37 ka BP[J]. SCIENTIFIC REPORTS,2021,11(1):14.
APA Li, Ting-Yong.,Wu, Yao.,Shen, Chuan-Chou.,Li, Jun-Yun.,Chiang, Hong-Wei.,...&Edwards, R. Lawrence.(2021).High precise dating on the variation of the Asian summer monsoon since 37 ka BP.SCIENTIFIC REPORTS,11(1),14.
MLA Li, Ting-Yong,et al."High precise dating on the variation of the Asian summer monsoon since 37 ka BP".SCIENTIFIC REPORTS 11.1(2021):14.
条目包含的文件
条目无相关文件。
个性服务
推荐该条目
保存到收藏夹
查看访问统计
导出为Endnote文件
谷歌学术
谷歌学术中相似的文章
[Li, Ting-Yong]的文章
[Wu, Yao]的文章
[Shen, Chuan-Chou]的文章
百度学术
百度学术中相似的文章
[Li, Ting-Yong]的文章
[Wu, Yao]的文章
[Shen, Chuan-Chou]的文章
必应学术
必应学术中相似的文章
[Li, Ting-Yong]的文章
[Wu, Yao]的文章
[Shen, Chuan-Chou]的文章
相关权益政策
暂无数据
收藏/分享
所有评论 (0)
暂无评论
 

除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。