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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：21/0  |  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.


  
Direct measurements of ice-shelf flexure caused by surface meltwater ponding and drainage 期刊论文
NATURE COMMUNICATIONS, 2019, 10
作者:  Banwell, Alison F.;  Willis, Ian C.;  Macdonald, Grant J.;  Goodsell, Becky;  MacAyeal, Douglas R.
收藏  |  浏览/下载：5/0  |  提交时间：2019/11/27
Contribution of sea ice microbial production to Antarctic benthic communities is driven by sea ice dynamics and composition of functional guilds 期刊论文
GLOBAL CHANGE BIOLOGY, 2018, 24 (8) : 3642-3653
作者:  Wing, Stephen R.;  Leichter, James J.;  Wing, Lucy C.;  Stokes, Dale;  Genovese, Sal J.;  McMullin, Rebecca M.;  Shatova, Olya A.
收藏  |  浏览/下载：6/0  |  提交时间：2019/04/09
Antarctica  climate change  food web  organic matter  sea ice  sea ice algae  
Decoupled responses of soil bacteria and their invertebrate consumer to warming, but not freeze-thaw cycles, in the Antarctic Dry Valleys 期刊论文
ECOLOGY LETTERS, 2017, 20 (10)
作者:  Knox, Matthew A.;  Andriuzzi, Walter S.;  Buelow, Heather N.;  Takacs-Vesbach, Cristina;  Adams, Byron J.;  Wall, Diana H.
收藏  |  浏览/下载：7/0  |  提交时间：2019/04/09
Body size distribution  climate change  McMurdo Dry Valleys  Nematode  Scottnema lindsayae  soil fauna  soil microbe  traits  
Characterizing hyporheic exchange processes using high-frequency electrical conductivity-discharge relationships on subhourly to interannual timescales 期刊论文
WATER RESOURCES RESEARCH, 2017, 53 (5)
作者:  Singley, Joel G.;  Wlostowski, Adam N.;  Bergstrom, Anna J.;  Sokol, Eric R.;  Torrens, Christa L.;  Jaros, Chris;  Wilson, Colleen E.;  Hendrickson, Patrick J.;  Gooseff, Michael N.
收藏  |  浏览/下载：9/0  |  提交时间：2019/04/09
hyporheic zone  electrical conductivity  concentration-discharge  Antarctica