High precise dating on the variation of the Asian summer monsoon since 37 ka BP
文献类型：期刊论文
| 作者 | 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
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| 刊名 | SCIENTIFIC REPORTS
 |
| 出版日期 | 2021-04-30 |
| 卷号 | 11期号:1页码:14 |
| ISSN号 | 2045-2322 |
| DOI | 10.1038/s41598-021-88597-7 |
| 通讯作者 | Li, Ting-Yong(cdlity@163.com) ; Shen, Chuan-Chou(river@ntu.edu.tw) |
| 英文摘要 | 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. |
| WOS关键词 | ABRUPT CLIMATE-CHANGE ; NORTH-ATLANTIC OCEAN ; HIGH-RESOLUTION ; GREENLAND TEMPERATURE ; MILLENNIAL-SCALE ; ENSO VARIABILITY ; HEINRICH EVENTS ; FURONG CAVE ; HOLOCENE ; RECORD |
| 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 |
| 语种 | 英语 |
| 出版者 | NATURE RESEARCH |
| WOS记录号 | WOS:000656497500023 |
| 资助机构 | 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 |
| 源URL | [http://ir.ieecas.cn/handle/361006/16684]  |
| 专题 | 地球环境研究所_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. |
入库方式： OAI收割
来源：地球环境研究所
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