Enhanced subglacial discharge from Antarctica during meltwater pulse 1A
Li, Tao4,5,6; Robinson, Laura F.3,5; Macgilchrist, Graeme A.1,2; Chen, Tianyu4; Stewart, Joseph A.5; Burke, Andrea1; Wang, Maoyu4; Li, Gaojun4; Chen, Jun4; Rae, James W. B.1
刊名NATURE COMMUNICATIONS
2023-11-13
卷号14期号:1页码:10
DOI10.1038/s41467-023-42974-0
通讯作者Li, Tao(taoli@nigpas.ac.cn)
英文摘要Subglacial discharge from the Antarctic Ice Sheet (AIS) likely played a crucial role in the loss of the ice sheet and the subsequent rise in sea level during the last deglaciation. However, no direct proxy is currently available to document subglacial discharge from the AIS, which leaves significant gaps in our understanding of the complex interactions between subglacial discharge and ice-sheet stability. Here we present deep-sea coral 234U/238U records from the Drake Passage in the Southern Ocean to track subglacial discharge from the AIS. Our findings reveal distinctively higher seawater 234U/238U values from 15,400 to 14,000 years ago, corresponding to the period of the highest iceberg-rafted debris flux and the occurrence of the meltwater pulse 1A event. This correlation suggests a causal link between enhanced subglacial discharge, synchronous retreat of the AIS, and the rapid rise in sea levels. The enhanced subglacial discharge and subsequent AIS retreat appear to have been preconditioned by a stronger and warmer Circumpolar Deep Water, thus underscoring the critical role of oceanic heat in driving major ice-sheet retreat. This study presents seawater uranium isotope records based on deep-sea corals from the Drake Passage to track subglacial discharge from the Antarctic Ice Sheet, demonstrating a causal link between enhanced subglacial discharge, retreat of the ice sheet, and the rapid rise in sea levels.
资助项目National Natural Science Foundation of China (National Science Foundation of China)[NBP11-03] ; National Natural Science Foundation of China[41991325] ; Strategic Priority Research Program of Chinese Academy of Sciences[XDB40010200] ; European Research Council ; Natural Environmental Research Council ; U.S. National Science Foundation[PLR-1425989] ; UK Research and Innovation[MR/W013835/1] ; National Oceanic and Atmospheric Administration (NOAA) Ocean Exploration Trust ; State Key Laboratory of Palaeobiology and Stratigraphy
WOS关键词SEA-LEVEL ; SOUTHERN-OCEAN ; ICE SHELF ; OVERTURNING CIRCULATION ; SEAWATER U-234/U-238 ; EAST ANTARCTICA ; COLLAPSE ; WATER ; VARIABILITY ; CORALS
WOS研究方向Science & Technology - Other Topics
语种英语
出版者NATURE PORTFOLIO
WOS记录号WOS:001126808200004
资助机构National Natural Science Foundation of China (National Science Foundation of China) ; National Natural Science Foundation of China ; Strategic Priority Research Program of Chinese Academy of Sciences ; European Research Council ; Natural Environmental Research Council ; U.S. National Science Foundation ; UK Research and Innovation ; National Oceanic and Atmospheric Administration (NOAA) Ocean Exploration Trust ; State Key Laboratory of Palaeobiology and Stratigraphy
内容类型期刊论文
源URL[http://ir.nigpas.ac.cn/handle/332004/42888]  
专题中国科学院南京地质古生物研究所
通讯作者Li, Tao
作者单位1.Univ St Andrews, Sch Earth & Environm Sci, St Andrews, Scotland
2.Princeton Univ, Program Atmospher & Ocean Sci, Princeton, NJ USA
3.Univ York, Dept Environm & Geog, York, England
4.Nanjing Univ, Dept Earth & Planetary Sci, Nanjing, Peoples R China
5.Univ Bristol, Sch Earth Sci, Bristol, England
6.Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, State Key Lab Palaeobiol & Stratig, Nanjing, Peoples R China
推荐引用方式
GB/T 7714
Li, Tao,Robinson, Laura F.,Macgilchrist, Graeme A.,et al. Enhanced subglacial discharge from Antarctica during meltwater pulse 1A[J]. NATURE COMMUNICATIONS,2023,14(1):10.
APA Li, Tao.,Robinson, Laura F..,Macgilchrist, Graeme A..,Chen, Tianyu.,Stewart, Joseph A..,...&Rae, James W. B..(2023).Enhanced subglacial discharge from Antarctica during meltwater pulse 1A.NATURE COMMUNICATIONS,14(1),10.
MLA Li, Tao,et al."Enhanced subglacial discharge from Antarctica during meltwater pulse 1A".NATURE COMMUNICATIONS 14.1(2023):10.
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