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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:58/0  |  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.


  
Hepatic NADH reductive stress underlies common variation in metabolic traits 期刊论文
NATURE, 2020, 583 (7814) : 122-+
作者:  Skov, Laurits;  Coll Macia, Moises;  Sveinbjoernsson, Gardar;  Mafessoni, Fabrizio;  Lucotte, Elise A.;  Einarsdottir, Margret S.;  Jonsson, Hakon;  Halldorsson, Bjarni;  Gudbjartsson, Daniel F.;  Helgason, Agnar;  Schierup, Mikkel Heide;  Stefansson, Kari
收藏  |  浏览/下载:43/0  |  提交时间:2020/07/03

The cellular NADH/NAD(+) ratio is fundamental to biochemistry, but the extent to which it reflects versus drives metabolic physiology in vivo is poorly understood. Here we report the in vivo application of Lactobacillus brevis (Lb)NOX1, a bacterial water-forming NADH oxidase, to assess the metabolic consequences of directly lowering the hepatic cytosolic NADH/NAD(+) ratio in mice. By combining this genetic tool with metabolomics, we identify circulating alpha-hydroxybutyrate levels as a robust marker of an elevated hepatic cytosolic NADH/NAD(+) ratio, also known as reductive stress. In humans, elevations in circulating alpha-hydroxybutyrate levels have previously been associated with impaired glucose tolerance(2), insulin resistance(3) and mitochondrial disease(4), and are associated with a common genetic variant in GCKR(5), which has previously been associated with many seemingly disparate metabolic traits. Using LbNOX, we demonstrate that NADH reductive stress mediates the effects of GCKR variation on many metabolic traits, including circulating triglyceride levels, glucose tolerance and FGF21 levels. Our work identifies an elevated hepatic NADH/NAD(+) ratio as a latent metabolic parameter that is shaped by human genetic variation and contributes causally to key metabolic traits and diseases. Moreover, it underscores the utility of genetic tools such as LbNOX to empower studies of '  causal metabolism'  .


The authors identify an increased hepatic NADH/NAD(+) ratio as an underlying metabolic parameter that is shaped by human genetic variation and contributes causally to key metabolic traits and diseases.


  
Addendum to "Hydrometric Data Rescue in the Parana River Basin" by Andres Antico, Ricardo O. Aguiar, and Mario L. Amsler 期刊论文
WATER RESOURCES RESEARCH, 2020, 56 (2)
作者:  Antico, Andres;  Mendizabal, Sophie;  Ferreira, Lorena J.;  Aguiar, Ricardo O.;  Amsler, Mario L.
收藏  |  浏览/下载:15/0  |  提交时间:2020/07/02
Parana River  South America  data rescue  water levels  river discharges  El Nino 1877-1878  
Earthquake Hydrogeology 期刊论文
WATER RESOURCES RESEARCH, 2019, 55 (7) : 5212-5216
作者:  Ingebritsen, S. E.;  Manga, Michael
收藏  |  浏览/下载:6/0  |  提交时间:2019/11/27
earthquakes  permeability  streamflow  water levels  stress  
New Insights on Coastal Foredune Growth: The Relative Contributions of Marine and Aeolian Processes 期刊论文
GEOPHYSICAL RESEARCH LETTERS, 2018, 45 (10) : 4965-4973
作者:  Cohn, Nicholas;  Ruggiero, Peter;  de Vries, Sierd;  Kaminsky, George M.
收藏  |  浏览/下载:7/0  |  提交时间:2019/04/09
coastal dunes  progradation  intertidal sandbar  beach  morphodynamics  total water levels  
Choosing a Functional Form for an International Benefit Transfer: Evidence from a Nine-country Valuation Experiment 期刊论文
ECOLOGICAL ECONOMICS, 2017, 134
作者:  Czajkowski, Mikolaj;  Ahtiainen, Heini;  Artell, Janne;  Meyerhoff, Juergen
收藏  |  浏览/下载:21/0  |  提交时间:2019/04/09
Benefit transfer  Functional forms  Explanatory variables  Transfer errors  Minimum tolerance levels  International  Contingent valuation  Water quality