Tuesday, September 5, 2017

Nature Geoscience contents: September 2017 Volume 10 Number 9 pp615-708

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TABLE OF CONTENTS

September 2017 Volume 10, Issue 9

Editorial
Commentary
News and Views
Reviews
Articles
 
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Editorial

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Skewed demographics   p615
doi:10.1038/ngeo3026
Scientists based in North America and men are overrepresented in our authors' reviewer suggestions.

Commentary

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Acts of God, human influence and litigation   pp616 - 619
Sophie Marjanac, Lindene Patton & James Thornton
doi:10.1038/ngeo3019
Developments in attribution science are improving our ability to detect human influence on extreme weather events. By implication, the legal duties of government, business and others to manage foreseeable harms are broadening, and may lead to more climate change litigation.

News and Views

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Cryospheric science: Asia's glacier changes   pp621 - 622
Daniel Farinotti
doi:10.1038/ngeo2995
Mass changes in High Mountain Asia's glaciers have been under dispute for almost a decade. An analysis of satellite data archives provides an observation-based mass budget for every single glacier in the region.
See also: Article by Brun et al.

Venus: Jet-setting atmosphere   pp622 - 623
Alain Hauchecorne
doi:10.1038/ngeo3022
A fast equatorial jet in the Venusian cloud layer has been revealed by the Akatsuki orbiter by tracking cloud movement in near-infrared images. The findings suggest that the Venusian atmosphere is more variable than previously thought.
See also: Article by Horinouchi et al.

Plate tectonics: Crustal recycling evolution   pp623 - 624
Valentina Magni
doi:10.1038/ngeo3015
The processes that form and recycle continental crust have changed through time. Numerical models reveal an evolution from extensive recycling on early Earth as the lower crust peeled away, to limited recycling via slab break-off today.
See also: Article by Chowdhury et al.

Deep mantle: Enriched carbon source detected   pp625 - 627
Peter H. Barry
doi:10.1038/ngeo3001
Estimates of carbon in the deep mantle vary by more than an order of magnitude. Coupled volcanic CO2 emission data and magma supply rates reveal a carbon-rich mantle plume source region beneath Hawai'i with 40% more carbon than previous estimates.
See also: Article by Anderson & Poland

Sketch-up: Snowstorms on Mars   p625
James Tuttle Keane
doi:10.1038/ngeo3023
See also: Article by Spiga et al.

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Reviews

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Metal availability and the expanding network of microbial metabolisms in the Archaean eon   pp629 - 636
Eli K. Moore, Benjamin I. Jelen, Donato Giovannelli, Hagai Raanan & Paul G. Falkowski
doi:10.1038/ngeo3006
Microbial metabolisms depend on enzymes that contain trace metals. A synthesis of molecular and geochemical data shows that these metabolic pathways evolved alongside changing marine availability of trace metals during the Precambrian.
 

Tidal controls on river delta morphology   pp637 - 645
A. J. F. Hoitink, Z. B. Wang, B. Vermeulen, Y. Huismans & K. Kastner
doi:10.1038/ngeo3000
River deltas are shaped by interactions between fluvial and tidal processes. Tides act to stabilize delta morphology, but sediment depletion due to human activities disrupts the balance and leads to erosion and scour.
 

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Articles

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Equatorial jet in the lower to middle cloud layer of Venus revealed by Akatsuki   pp646 - 651
Takeshi Horinouchi, Shin-ya Murakami, Takehiko Satoh, Javier Peralta, Kazunori Ogohara et al.
doi:10.1038/ngeo3016
Venus is covered by thick clouds that move with the prevailing winds. Images from JAXA's Akatsuki orbiter taken in July 2016 reveal more variability deep in the cloud layer than expected, including a feature consistent with an equatorial jet.
See also: News and Views by Hauchecorne

Snow precipitation on Mars driven by cloud-induced night-time convection   pp652 - 657
Aymeric Spiga, David P. Hinson, Jean-Baptiste Madeleine, Thomas Navarro, Ehouarn Millour et al.
doi:10.1038/ngeo3008
The Martian atmosphere hosts water-ice clouds, but it is thought that any snow precipitation settles slowly, rather than in storms. Martian meteorology simulations suggest that localized convective snowstorms can occur on Mars during the night.
See also: News and Views by Keane

Large sulfur isotope fractionations in Martian sediments at Gale crater   pp658 - 662
H. B. Franz, A. C. McAdam, D. W. Ming, C. Freissinet, P. R. Mahaffy et al.
doi:10.1038/ngeo3002
Ancient Mars may have had an active sulfur cycle. In situ analyses by the Curiosity rover reveal large variations in the current sulfur isotopic composition of Martian sediments that can be explained by geologic and atmospheric processes.
 

The strength of the meridional overturning circulation of the stratosphere   pp663 - 667
Marianna Linz, R. Alan Plumb, Edwin P. Gerber, Florian J. Haenel, Gabriele Stiller et al.
doi:10.1038/ngeo3013
The strength of the global meridional overturning circulation in the stratosphere is uncertain. An analysis of satellite data, reanalyses and model simulations reveals a strength of 6.3-7.6 × 109 kg s-1, but no convergence at higher altitudes.
 

A spatially resolved estimate of High Mountain Asia glacier mass balances from 2000 to 2016   pp668 - 673
Fanny Brun, Etienne Berthier, Patrick Wagnon, Andreas Kaab & Desiree Treichler
doi:10.1038/ngeo2999
Glacier mass balances in High Mountain Asia are uncertain. Satellite stereo-imagery allows a spatially resolved estimate for about 92% of the glacierized area and yields a region-wide average of about 16 Gt yr-1 for 2000 to 2016.
See also: News and Views by Farinotti

Small fraction of marine cloud condensation nuclei made up of sea spray aerosol   pp674 - 679
P. K. Quinn, D. J. Coffman, J. E. Johnson, L. M. Upchurch & T. S. Bates
doi:10.1038/ngeo3003
Sea spray aerosols are thought to alter cloud properties in remote ocean regions. Aerosol analyses over four ocean regions reveal that these aerosols represent less than 30% of cloud condensation nuclei in typical marine boundary layer clouds.
 

Rapid post-seismic landslide evacuation boosted by dynamic river width   pp680 - 684
Thomas Croissant, Dimitri Lague, Philippe Steer & Philippe Davy
doi:10.1038/ngeo3005
How rivers evacuate large landslide deposits is crucial for predicting post-seismic hazards. A 2D hydro-sedimentary model demonstrates that a narrowing river channel increases sediment transport, which reduces export time by orders of magnitude.
 

Fluid-driven metamorphism of the continental crust governed by nanoscale fluid flow   pp685 - 690
Oliver Plumper, Alexandru Botan, Catharina Los, Yang Liu, Anders Malthe-Sorenssen et al.
doi:10.1038/ngeo3009
Fluid flow in Earth's crust redistributes minerals. Nanoscale imaging and molecular dynamics simulations suggest this flow is controlled by electrokinetic transport phenomena, highlighting the importance of nanoscale processes in metamorphism.
 

Anatomy of a meltwater drainage system beneath the ancestral East Antarctic ice sheet   pp691 - 697
Lauren M. Simkins, John B. Anderson, Sarah L. Greenwood, Helge M. Gonnermann, Lindsay O. Prothro et al.
doi:10.1038/ngeo3012
The East Antarctic ice sheet was larger than present during past cold periods. Seafloor geophysical data show that in the Ross Sea, the extended ice sheet was underlain by an active hydrologic system during the glacial termination.
 

Emergence of silicic continents as the lower crust peels off on a hot plate-tectonic Earth   pp698 - 703
Priyadarshi Chowdhury, Taras Gerya & Sumit Chakraborty
doi:10.1038/ngeo3010
The processes for crustal recycling during the Archaean are unclear. Numerical simulations suggest that dense lower crust would have peeled off into the mantle, leading to a rapid concentration of buoyant silicic rocks that formed the continents.
See also: News and Views by Magni

Abundant carbon in the mantle beneath Hawai'i   pp704 - 708
Kyle R. Anderson & Michael P. Poland
doi:10.1038/ngeo3007
Estimates of the carbon content of Earth's mantle and magmas vary. Analysis and modelling of gas emissions at Hawai'i indicate that the amount of carbon in the Hawaiian mantle plume and CO2 in Hawaiian lavas is 40% greater than previously thought.
See also: News and Views by Barry

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