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DOI | 10.1016/j.quascirev.2020.106218 |
Millennial-scale Asian monsoon variability during MIS 9 revealed by a high-resolution stalagmite δ18O record in Luoshui Cave; central China | |
Yang S.; Chen S.; Wang Y.; Shao Q.; Yu T.-L.; Shen C.-C.; Zhai X.; Edwards R.L.; Liu D.; Liang Y.; Wang Q.; Zhang Z.; Li C. | |
发表日期 | 2020 |
ISSN | 0277-3791 |
卷号 | 234 |
英文摘要 | A 67-yr-resolution δ18O profile of a230Th-dated stalagmite from Luoshui Cave, central China, is presented to refine the Asian summer monsoon (ASM) history from 336 to 290 kyr BP. The sub-stages of Marine Isotope Stage 9 (MIS 9) are clearly reflected in the Luoshui δ18O record, in line with changes in the Northern Hemisphere summer insolation (NHSI). The concurrency of eight weak monsoon intervals (WMIs) between 320 and 290 kyr BP and shifts in the Atlantic oceanic circulation suggest that monsoon weakening was forced by northern high-latitude climate oscillations with north-south shifts in the Intertropical Convergence Zone (ITCZ). Spectrum analyses show a cyclic change of 1–4 kyr between 320 and 290 kyr BP, similar to the Dansgaard-Oeschger cycles during the last glacial period. This suggests a relatively unstable monsoon state when the northern ice volume reached intermediate levels. The detrended δ18O agrees well with the δ13C record on the millennial to sub-millennial scales, suggesting a coupling of monsoon climate and cave environment. After removal of the summer insolation signal at 65°N, the residual Luoshui δ18O record is highly similar to orbital- and millennial-scale temperature changes in Antarctica in an anti-phased fashion, revealing the significant influence of Southern Hemispheric climates on ASM intensity. The absence of counterparts of the two WMIs between 315 and 310 kyr BP in Antarctica, however, indicates a complicated teleconnection. © 2020 Elsevier Ltd |
英文关键词 | Asian summer monsoon; Marine isotope stage 9; Millennial-scale variation; Oxygen isotope; Stalagmite |
语种 | 英语 |
scopus关键词 | Caves; Climatology; Incident solar radiation; Isotopes; Spectrum analysis; Asian summer monsoons; Marine isotope stages; Millennial-scale variation; Oxygen isotopes; Stalagmite; Atmospheric thermodynamics; insolation; intertropical convergence zone; marine isotope stage; monsoon; Northern Hemisphere; oceanic circulation; oxygen isotope; paleoclimate; spatial resolution; stalagmite; Antarctica; Atlantic Ocean; China; Luoshui; Yunnan |
来源期刊 | Quaternary Science Reviews
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文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/151530 |
作者单位 | School of Geography, Nanjing Normal University, Nanjing, 210023, China; Jiangsu Center for Collaborative Innovation in Geographical Information Resource Development and Application, Nanjing, 210023, China; High-Precision Mass Spectrometry and Environment Change Laboratory, Department of Geosciences, National Taiwan University, Taipei, 10617, Taiwan; Research Center for Future Earth, National Taiwan University, Taipei, 10617, Taiwan; Global Change Research Center, National Taiwan University, Taipei, 10617, Taiwan; Institute of Karst Geology, Chinese Academy of Geological Science International Research Center on Karst, Guiin, 54104, China; Department of Earth Sciences, University of Minnesota, Minneapolis, MN 55455, United States; Chongqing Key Laboratory of Earth Surface Processes and Environmental Remote Sensing in Three Gorges Reservoir Area, Chongqing, 401331, China; State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an, 710075, China; ... |
推荐引用方式 GB/T 7714 | Yang S.,Chen S.,Wang Y.,et al. Millennial-scale Asian monsoon variability during MIS 9 revealed by a high-resolution stalagmite δ18O record in Luoshui Cave; central China[J],2020,234. |
APA | Yang S..,Chen S..,Wang Y..,Shao Q..,Yu T.-L..,...&Li C..(2020).Millennial-scale Asian monsoon variability during MIS 9 revealed by a high-resolution stalagmite δ18O record in Luoshui Cave; central China.Quaternary Science Reviews,234. |
MLA | Yang S.,et al."Millennial-scale Asian monsoon variability during MIS 9 revealed by a high-resolution stalagmite δ18O record in Luoshui Cave; central China".Quaternary Science Reviews 234(2020). |
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