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2016/04/29

Nature Geoscience contents: May 2016 Volume 9 Number 5 pp337-407

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TABLE OF CONTENTS

May 2016 Volume 9, Issue 5

Editorial
Correspondence
Commentary
News and Views
Letters
Articles
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Editorial

Top

Gender asymmetry   p337
doi:10.1038/ngeo2712
Investigations of sexual harassment are difficult and potentially destructive to all involved. It is imperative that they are carried out quickly, with high priority and acted upon decisively where misconduct is identified.

Correspondence

Top

Unclear causes for subduction   p338
Timothy E. Keenan & John Encarnación
doi:10.1038/ngeo2703
See also: Correspondence by Arculus et al. | Article by Arculus et al.

Reply to 'Unclear causes for subduction'   pp338 - 339
Richard J. Arculus, Osamu Ishizuka, Kara A. Bogus, Michael Gurnis, Rosemary Hickey-Vargas et al.
doi:10.1038/ngeo2704
See also: Correspondence by Keenan & Encarnación | Article by Arculus et al.

Commentary

Top

An actionable climate target   pp340 - 342
Oliver Geden
doi:10.1038/ngeo2699
The Paris Agreement introduced three mitigation targets. In the future, the main focus should not be on temperature targets such as 2 or 1.5 °C, but on the target with the greatest potential to effectively guide policy: net zero emissions.

News and Views

Top

Biogeochemistry: The fate of phosphorus   pp343 - 344
Julien Némery & Josette Garnier
doi:10.1038/ngeo2702
Phosphorus is essential for food production, but it is also a key cause of eutrophication. Estimates of phosphorus flux for the past 40–70 years reveal that large river basins can experience phases of phosphorus accumulation and depletion.
See also: Letter by Powers et al.

Natural hazards: Cracking cliffs feel the heat   pp344 - 345
Valentin S. Gischig
doi:10.1038/ngeo2698
Rockfall often seems to occur spontaneously without an obvious cause. Monitoring of a granitic cliff reveals that cyclical temperature variations can subtly act to slowly and incrementally damage hard rock until failure is inevitable.
See also: Article by Collins & Stock

Atmospheric methane: Shifting sources   p346
Alicia Newton
doi:10.1038/ngeo2710

Earthquakes: Megathrusts and mountain building   pp346 - 348
Rich Briggs
doi:10.1038/ngeo2697
Coastlines above subduction zones slowly emerge from the sea despite repeated drowning by great, shallow earthquakes. Analysis of the Chilean coast suggests that moderate-to-large, deeper earthquakes may be responsible for the net uplift.
See also: Article by Melnick

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Letters

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Large increases in Arctic biogenic volatile emissions are a direct effect of warming   pp349 - 352
Magnus Kramshøj, Ida Vedel-Petersen, Michelle Schollert, Åsmund Rinnan, Josephine Nymand et al.
doi:10.1038/ngeo2692
Volatile organic compounds can affect air quality and climate. Experimental warming of vegetated tundra plots in Greenland increased biogenic volatile organic compound emissions from vegetation and soils by 260%, as a direct effect.

Long-term accumulation and transport of anthropogenic phosphorus in three river basins   pp353 - 356
Stephen M. Powers, Thomas W. Bruulsema, Tim P. Burt, Neng Iong Chan, James J. Elser et al.
doi:10.1038/ngeo2693
Phosphorus fertilizer use has roughly quadrupled in the past century. Budgets constructed from historical data show that phosphorus rapidly accumulates in river basins during periods of high inputs and continues to mobilize after inputs decline.
See also: News and Views by Némery & Garnier

Importance and controls of anaerobic ammonium oxidation influenced by riverbed geology   pp357 - 360
K. Lansdown, B. A. McKew, C. Whitby, C. M. Heppell, A. J. Dumbrell et al.
doi:10.1038/ngeo2684
Anammox, an important N2 loss pathway in marine waters, is not well understood in rivers. In situ measurements of N2 production in UK rivers reveal that anammox can be the dominant N2 loss pathway in permeable but not in impermeable riverbeds.

Acidification of East Siberian Arctic Shelf waters through addition of freshwater and terrestrial carbon   pp361 - 365
Igor Semiletov, Irina Pipko, Örjan Gustafsson, Leif G. Anderson, Valentin Sergienko et al.
doi:10.1038/ngeo2695
Uptake of atmospheric CO2 contributes to ocean acidification. Measurements of seawater chemistry reveal that the extreme acidity of the East Siberian Arctic Shelf is driven by terrestrial organic matter and freshwater inputs.

Melting at the base of the Greenland ice sheet explained by Iceland hotspot history   pp366 - 369
Irina Rogozhina, Alexey G. Petrunin, Alan P. M. Vaughan, Bernhard Steinberger, Jesse V. Johnson et al.
doi:10.1038/ngeo2689
Basal melting is widespread in the north-central Greenland ice sheet. Geophysical data and numerical modelling suggest a geothermal anomaly in this region resulting from the earlier passage of Greenland over the Iceland mantle plume.

Regulation of ice stream flow through subglacial formation of gas hydrates   pp370 - 374
Monica Winsborrow, Karin Andreassen, Alun Hubbard, Andreia Plaza-Faverola, Eythor Gudlaugsson et al.
doi:10.1038/ngeo2696
Localized subglacial zones of high traction help to regulate ice sheet flow. Geophysical data from a palaeo-ice-stream suggest that methane gas accumulation and hydrate formation beneath ice sheets can produce such high-traction sticky spots.

Incursions of southern-sourced water into the deep North Atlantic during late Pliocene glacial intensification   pp375 - 379
David C. Lang, Ian Bailey, Paul A. Wilson, Thomas B. Chalk, Gavin L. Foster et al.
doi:10.1038/ngeo2688
Northern Hemisphere ice sheets expanded 2.7 million years ago. Sediment geochemistry suggests that at this time, the North Atlantic began to experience incursions of southern-sourced water during glacials, similar to the last glacial period.

Potential slab deformation and plunge prior to the Tohoku, Iquique and Maule earthquakes   pp380 - 383
Michel Bouchon, David Marsan, Virginie Durand, Michel Campillo, Hugo Perfettini et al.
doi:10.1038/ngeo2701
Megathrust earthquakes rupture the shallow plate boundary in subduction zones. Analysis of seismic activity preceding megathrust quakes in Japan and Chile reveals deep seismicity that may mark plunging of the slabs prior to main fault rupture.

Fault-controlled hydration of the upper mantle during continental rifting   pp384 - 388
G. Bayrakci, T. A. Minshull, D. S. Sawyer, T. J. Reston, D. Klaeschen et al.
doi:10.1038/ngeo2671
The mechanisms for mantle hydration are unclear. Seismic images offshore from Spain reveal a correlation between the amount of seawater-altered rocks and the extent of fault slip, suggesting that faults control water flux into the Earth.

Articles

Top

Long-lead predictions of eastern United States hot days from Pacific sea surface temperatures   pp389 - 394
K. A. McKinnon, A. Rhines, M. P. Tingley and P. Huybers
doi:10.1038/ngeo2687
Extreme summer temperatures are difficult to forecast. A statistical analysis reveals a pattern of Pacific sea surface temperature anomalies that provides skilful predictions of hot weather in the eastern US.

Rockfall triggering by cyclic thermal stressing of exfoliation fractures   pp395 - 400
Brian D. Collins & Greg M. Stock
doi:10.1038/ngeo2686
Some rockfalls occur without obvious triggers such as seismicity or freeze-thaw conditions. Temperature and deformation patterns on a granite cliff suggest that cyclical thermal forcing can progressively open fractures and trigger rockfalls.
See also: News and Views by Gischig

Rise of the central Andean coast by earthquakes straddling the Moho   pp401 - 407
Daniel Melnick
doi:10.1038/ngeo2683
Coastlines above subduction zones often uplift over geological timescales. Analysis of landscape evolution and seismicity at the central Andean margin suggests that earthquakes on the deep plate interface help build up coastal topography.
See also: News and Views by Briggs

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