TABLE OF CONTENTS |
May 2017 Volume 10, Issue 5 |
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| Editorial Correspondence Book and Arts News and Views Perspective Articles Addendum
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npj Climate and Atmospheric Science: open for submissions
An open access, online-only journal providing researchers, policy makers and the public with the latest research on weather and climate, publishing high-quality papers that focus on topics including climate dynamics, climate variability, weather and climate prediction, climate change, weather extremes, atmospheric composition including aerosols, the hydrological cycle and atmosphere-ocean interactions.
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Editorial | Top |
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Where credit is due p323 doi:10.1038/ngeo2949 Authors of research manuscripts should be aware of their authorship, have read the paper and agree with it. What else is required for co-authorship — and what merits only a mention in the acknowledgements — is less clear.
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Correspondence | Top |
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Save northern high-latitude catchments pp324 - 325 Hjalmar Laudon, Christopher Spence, Jim Buttle, Sean K. Carey, Jeffrey J. McDonnell et al. doi:10.1038/ngeo2947
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Book and Arts | Top |
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Exhibition: A flame-filled history p326 doi:10.1038/ngeo2944
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News and Views | Top |
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Perspective | Top |
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The cold and relatively dry nature of mantle forearcs in subduction zones pp333 - 337 G. A. Abers, P. E. van Keken and B. R. Hacker doi:10.1038/ngeo2922 Dehydration of subducting slabs could create a reservoir of water in the overlying mantle. A synthesis of thermal model results, however, shows that slab dehydration is slow over geological time scales, so such reservoirs are probably rare.
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npj Clean Water: open for submissions
An open access, online-only journal, dedicated to publishing high-quality papers that describe the significant and cutting-edge research that continues to ensure the supply of clean water to populations.
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Articles | Top |
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Geomorphological evidence for ground ice on dwarf planet Ceres pp338 - 343 Britney E. Schmidt, Kynan H. G. Hughson, Heather T. Chilton, Jennifer E. C. Scully, Thomas Platz et al. doi:10.1038/ngeo2936 Despite evidence for an ice-rich outer shell, little water ice has been observed on the surface of Ceres. Lobate morphologies observed on Ceres that are increasingly prevalent towards the dwarf planet's poles are consistent with ice-rich flows.
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A post-accretionary lull in large impacts on early Mars pp344 - 348 William F. Bottke and Jeffrey C. Andrews-Hanna doi:10.1038/ngeo2937 The timing and number of large impact basins on early Mars are poorly constrained. Gravity and topographic analyses support a lull in basin-forming impacts following the main stage of accretion.
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Experimental and observational evidence for plume-induced subduction on Venus pp349 - 355 A. Davaille, S. E. Smrekar and S. Tomlinson doi:10.1038/ngeo2928 Venus lacks plate tectonics, but some trenches on Venus resemble subduction zones. Laboratory experiments suggest that upwelling plumes can initiate localized subduction of a thin lithosphere such as the one on Venus. See also: News and Views by Crameri |
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Microbial formation of labile organic carbon in Antarctic glacial environments pp356 - 359 H. J. Smith, R. A. Foster, D. M. McKnight, J. T. Lisle, S. Littmann et al. doi:10.1038/ngeo2925 Bioavailable glacial carbon has been thought to be largely ancient or anthropogenic. Analyses of carbon dynamics in an Antarctic supraglacial stream reveal that non-photosynthetic production relies on organic carbon from photosynthetic microbes. See also: News and Views by Kujawinski |
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Microbially driven export of labile organic carbon from the Greenland ice sheet pp360 - 365 Michaela Musilova, Martyn Tranter, Jemma Wadham, Jon Telling, Andrew Tedstone et al. doi:10.1038/ngeo2920 Glacial systems are important sources of dissolved organic carbon to downstream ecosystems. Observations of carbon dynamics on the Greenland ice sheet reveal substantial melt season production and export of microbial dissolved organic carbon. See also: News and Views by Kujawinski |
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Inland thinning on the Greenland ice sheet controlled by outlet glacier geometry pp366 - 369 Denis Felikson, Timothy C. Bartholomaus, Ginny A. Catania, Niels J. Korsgaard, Kurt H. Kjaer et al. doi:10.1038/ngeo2934 Greenland's ice loss depends on propagation of mass loss from the marine glacier termini to the interior. An analysis of surface elevation change in 16 glacier catchments shows that the up-glacier extent of thinning is limited by glacier geometry.
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River piracy and drainage basin reorganization led by climate-driven glacier retreat pp370 - 375 Daniel H. Shugar, John J. Clague, James L. Best, Christian Schoof, Michael J. Willis et al. doi:10.1038/ngeo2932 River piracy—the diversion of one stream's headwaters into another—has occurred on long timescales. An analysis of streamflow and digital elevation models documents river re-routing in response to glacier retreat in Yukon, Canada in May 2016. See also: News and Views by Headley |
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Groundwater salinity influenced by Holocene seawater trapped in incised valleys in the Red River delta plain pp376 - 381 Flemming Larsen, Long Vu Tran, Hoan Van Hoang, Luu Thi Tran, Anders Vest Christiansen et al. doi:10.1038/ngeo2938 Brackish to salty waters have been found in inland areas of delta aquifers. Geophysical data and modelling suggest that salty groundwater in the Red River delta originates from trapped seawater contained in underlying Holocene marine deposits.
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Onset and ending of the late Palaeozoic ice age triggered by tectonically paced rock weathering pp382 - 386 Yves Godderis, Yannick Donnadieu, Sebastien Carretier, Markus Aretz, Guillaume Dera et al. doi:10.1038/ngeo2931 The late Palaeozoic was characterized by glacial cycles. Numerical simulations suggest that increased silicate weathering due to mountain uplift and soil removal caused atmospheric CO2 to fall below the threshold for glaciation.
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Rise of Earth's atmospheric oxygen controlled by efficient subduction of organic carbon pp387 - 392 Megan S. Duncan and Rajdeep Dasgupta doi:10.1038/ngeo2939 Little is known about the deep carbon cycle during the Archaean. High- pressure and -temperature experiments indicate that the subduction of organic carbon on a hotter, younger Earth was efficient, helping to sequester carbon in Earth's interior.
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Addendum | Top |
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Addendum: Large-scale subduction of continental crust implied by India-Asia mass-balance calculation p393 Miquela Ingalls, David B. Rowley, Brian Currie and Albert S. Colman doi:10.1038/ngeo2930
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