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Ice retreat in Wilkes Basin of East Antarctica during a warm interglacial 期刊论文
NATURE, 2020, 583 (7817) : 554-+
作者:  T. Blackburn;  G. H. Edwards;  S. Tulaczyk;  M. Scudder;  G. Piccione;  B. Hallet;  N. McLean;  J. C. Zachos;  B. Cheney;  J. T. Babbe
收藏  |  浏览/下载:18/0  |  提交时间:2020/08/09

Uranium isotopes in subglacial precipitates from the Wilkes Basin of the East Antarctic Ice Sheet reveal ice retreat during a warm Pleistocene interglacial period about 400,000 years ago.


Efforts to improve sea level forecasting on a warming planet have focused on determining the temperature, sea level and extent of polar ice sheets during Earth'  s past interglacial warm periods(1-3). About 400,000 years ago, during the interglacial period known as Marine Isotopic Stage 11 (MIS11), the global temperature was 1 to 2 degrees Celsius greater(2)and sea level was 6 to 13 metres higher(1,3). Sea level estimates in excess of about 10 metres, however, have been discounted because these require a contribution from the East Antarctic Ice Sheet(3), which has been argued to have remained stable for millions of years before and includes MIS11(4,5). Here we show how the evolution of(234)U enrichment within the subglacial waters of East Antarctica recorded the ice sheet'  s response to MIS11 warming. Within the Wilkes Basin, subglacial chemical precipitates of opal and calcite record accumulation of(234)U (the product of rock-water contact within an isolated subglacial reservoir) up to 20 times higher than that found in marine waters. The timescales of(234)U enrichment place the inception of this reservoir at MIS11. Informed by the(234)U cycling observed in the Laurentide Ice Sheet, where(234)U accumulated during periods of ice stability(6)and was flushed to global oceans in response to deglaciation(7), we interpret our East Antarctic dataset to represent ice loss within the Wilkes Basin at MIS11. The(234)U accumulation within the Wilkes Basin is also observed in the McMurdo Dry Valleys brines(8-10), indicating(11)that the brine originated beneath the adjacent East Antarctic Ice Sheet. The marine origin of brine salts(10)and bacteria(12)implies that MIS11 ice loss was coupled with marine flooding. Collectively, these data indicate that during one of the warmest Pleistocene interglacials, the ice sheet margin at the Wilkes Basin retreated to near the precipitate location, about 700 kilometres inland from the current position of the ice margin, which-assuming current ice volumes-would have contributed about 3 to 4 metres(13)to global sea levels.


  
Prolonged Periodicity and Eastward Shift of the January North Pacific Oscillation Since the Mid-1990s and Its Linkage With Sea Ice Anomalies in the Barents Sea 期刊论文
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2020, 125 (13)
作者:  Xu, Zhiqing;  Fan, Ke
收藏  |  浏览/下载:10/0  |  提交时间:2020/08/18
January North Pacific Oscillation  prolonged periodicity  eastward shift  sea ice anomalies in the Barents Sea  the mid-1990s  
Subseasonal Prediction of Land Cold Extremes in Boreal Wintertime 期刊论文
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2020, 125 (13)
作者:  Xiang, Baoqiang;  Sun, Y. Qiang;  Chen, Jan-Huey;  Johnson, Nathaniel C.;  Jiang, Xianan
收藏  |  浏览/下载:12/0  |  提交时间:2020/08/18
subseasonal prediction  extremes  surface air temperature  predictability sources  land-atmosphere coupling  
Linking Marine Biological Activity to Aerosol Chemical Composition and Cloud-Relevant Properties Over the North Atlantic Ocean 期刊论文
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2020, 125 (13)
作者:  Mansour, Karam;  39;Dowd, Colin
收藏  |  浏览/下载:12/0  |  提交时间:2020/08/18
aerosol-cloud interactions  CCN  INP  marine aerosol  ocean-atmosphere interactions  oceanic biological activity  
Seasonally Modulated Stratospheric Aerosol Geoengineering Alters the Climate Outcomes 期刊论文
GEOPHYSICAL RESEARCH LETTERS, 2020, 47 (12)
作者:  Visioni, Daniele;  MacMartin, Douglas G.;  Kravitz, Ben;  Richter, Jadwiga H.;  Tilmes, Simone;  Mills, Michael J.
收藏  |  浏览/下载:46/0  |  提交时间:2020/08/18
Geoengineering  Stratospheric Sulfate  Climate Engineering  Stratospheric Aerosols  
Southern Ocean carbon sink enhanced by sea-ice feedbacks at the Antarctic Cold Reversal 期刊论文
NATURE GEOSCIENCE, 2020, 13 (7) : 489-+
作者:  Fogwill, C. J.;  Turney, C. S. M.;  Menviel, L.;  Baker, A.;  Weber, M. E.;  Ellis, B.;  Thomas, Z. A.;  Golledge, N. R.;  Etheridge, D.;  Rubino, M.;  Thornton, D. P.;  van Ommen, T. D.;  Moy, A. D.;  Curran, M. A. J.;  Davies, S.;  Bird, M., I;  Munksgaard, N. C.;  Rootes, C. M.;  Millman, H.;  Vohra, J.;  Rivera, A.;  Mackintosh, A.;  Pike, J.;  Hall, I. R.;  Bagshaw, E. A.;  Rainsley, E.;  Bronk-Ramsey, C.;  Montenari, M.;  Cage, A. G.;  Harris, M. R. P.;  Jones, R.;  Power, A.;  Love, J.;  Young, J.;  Weyrich, L. S.;  Cooper, A.
收藏  |  浏览/下载:14/0  |  提交时间:2020/06/29
Remote assessment of the fate of phytoplankton in the Southern Ocean sea-ice zone 期刊论文
NATURE COMMUNICATIONS, 2020, 11 (1)
作者:  Moreau, Sebastien;  Boyd, Philip W.;  Strutton, Peter G.
收藏  |  浏览/下载:5/0  |  提交时间:2020/06/22
Particle-Size Distributions and Solubility of Aerosol Iron Over the Antarctic Peninsula During Austral Summer 期刊论文
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2020, 125 (11)
作者:  Gao, Yuan;  Yu, Shun;  Sherrell, Robert M.;  Fan, Songyun;  Bu, Kaixuan;  Anderson, James R.
收藏  |  浏览/下载:13/0  |  提交时间:2020/08/18
aerosol iron  aerosol Fe solubility  aerosol particle size  Antarctic Peninsula  atmospheric iron deposition flux  
3D sedimentary architecture showing the inception of an Ice Age 期刊论文
NATURE COMMUNICATIONS, 2020, 11 (1)
作者:  Loseth, H.;  Dowdeswell, J. A.;  Batchelor, C. L.;  Ottesen, D.
收藏  |  浏览/下载:5/0  |  提交时间:2020/06/16
Exceptionally Warm and Prolonged Flow of Warm Deep Water Toward the Filchner-Ronne Ice Shelf in 2017 期刊论文
GEOPHYSICAL RESEARCH LETTERS, 2020, 47 (13)
作者:  Ryan, Svenja;  Hellmer, Hartmut H.;  Janout, Markus;  Darelius, Elin;  Vignes, Lucie;  Schroeder, Michael
收藏  |  浏览/下载:10/0  |  提交时间:2020/06/16
ocean-ice shelf interaction  Weddell Sea  warm inflow  Antarctic Slope Front  Filchner-Ronne Ice Shelf