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2013/05/30

Nature Geoscience contents: June 2013 Volume 6 Number 6 pp413-503

Nature Geoscience

TABLE OF CONTENTS

June 2013 Volume 6, Issue 6

Editorials
Correspondence
Commentary
In the press
Research Highlights
News and Views
Progress Article
Letters
Articles
Corrigendum
Errata


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Nature Geoscience web focus: 5 years after the Wenchuan Earthquake

The Wenchuan earthquake of 2008 killed more than 80,000 people and displaced millions. The most recent quake in April 2013 wreaked further havoc in the region. This web focus discusses the mechanisms for the Wenchuan quake and the implications for our understanding of the eastern margin of the Tibetan Plateau, the on-going risk from quake-induced landslides, and the societal impacts.

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Produced with support from the National Natural Science Foundation of China.
 

Editorials

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Plants, clouds and climate   p413
doi:10.1038/ngeo1852
Plant–cloud interactions have the potential to both cool and warm the climate. Ascertaining how these processes balance out at the global scale will require close collaboration between climate scientists and plant biologists.

Double-blind peer review   p413
doi:10.1038/ngeo1853
Allowing authors of research papers to be anonymous to referees has long been recommended. We will offer such an option, as a trial, from 10 June 2013.

Correspondence

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Energy budget constraints on climate response   pp415 - 416
Alexander Otto, Friederike E. L. Otto, Olivier Boucher, John Church, Gabi Hegerl, Piers M. Forster, Nathan P. Gillett, Jonathan Gregory, Gregory C. Johnson, Reto Knutti, Nicholas Lewis, Ulrike Lohmann, Jochem Marotzke, Gunnar Myhre, Drew Shindell, Bjorn Stevens and Myles R. Allen
doi:10.1038/ngeo1836

Commentary

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The fourth food revolution   pp417 - 418
Paolo D'Odorico and Maria Cristina Rulli
doi:10.1038/ngeo1842
In areas of the developing world that have benefited only marginally from the intensification of agriculture, foreign investments can enhance productivity. This could represent a step towards greater food security, but only if we ensure that malnourished people in the host countries benefit.

In the press

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Plumbing Old Faithful's depths   p419
Nicola Jones
doi:10.1038/ngeo1839

Research Highlights

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Atmospheric science: Central Pacific cyclones | Planetary science: Wet martian mantle | Palaeoclimate: Cold and dry | Tectonics: Failed break-up

News and Views

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Planetary science: Go and catch a falling star   pp422 - 423
Erik Asphaug
doi:10.1038/ngeo1840
Patches of deposits containing unusual mafic minerals are observed in and around some large lunar impact craters. Numerical simulations suggest that in the slowest of these impacts, asteroidal material, alien to the Moon, could have survived.
See also: Letter by Yue et al.

Palaeoclimate: When the dust settles   pp423 - 424
Eun Young Kwon and Eric D. Galbraith
doi:10.1038/ngeo1838
The amount of carbon stored in the deep ocean varied over glacial–interglacial cycles. Southern Ocean sediments from the past 360,000 years show that carbon storage also fluctuated within glacial periods, in concert with the fertilization of the Southern Ocean by wind-borne dust.
See also: Letter by Ziegler et al.

Earth's inner core: Variable rotation   pp424 - 426
Kenneth C. Creager
doi:10.1038/ngeo1831
Different measurements of inner core rotation have delivered inconsistent results. An analysis of seismic data provides a resolution of this discrepancy by suggesting decadal variations in inner core rotation rate.
See also: Article by Tkalčić et al.

Geochemistry: Subsurface sustenance   pp426 - 427
Steven D'Hondt
doi:10.1038/ngeo1843
High-temperature water–rock reactions produce large quantities of hydrogen, which must be transported to cooler settings to sustain life. Lower-temperature hydrogen generation could potentially support life in situ and free subsurface microbes from photosynthetic constraints.
See also: Article by Mayhew et al.

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Progress Article

Top

A middle Eocene carbon cycle conundrum   pp429 - 434
Appy Sluijs, Richard E. Zeebe, Peter K. Bijl and Steven M. Bohaty
doi:10.1038/ngeo1807
A 500,000-year-long period of warmth in the middle Eocene was marked by high atmospheric carbon dioxide concentrations and prolonged dissolution of carbonate in the deep oceans. Numerical simulations attempting to capture these features identify gaps in our understanding of the causes of this and similar perturbations.

Letters

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Projectile remnants in central peaks of lunar impact craters   pp435 - 437
Z. Yue, B. C. Johnson, D. A. Minton, H. J. Melosh, K. Di, W. Hu and Y. Liu
doi:10.1038/ngeo1828
Unusual minerals observed in lunar craters were thought to originate from beneath the Moon's surface. Numerical simulations show that rather than being vaporized, much of the impactor material can survive in the crater, implying that the unusual minerals come from the impactor and may not be indigenous to the Moon.
See also: News and Views by Asphaug

Warming-induced increase in aerosol number concentration likely to moderate climate change   pp438 - 442
Pauli Paasonen, Ari Asmi, Tuukka Petäjä, Maija K. Kajos, Mikko Äijälä, Heikki Junninen, Thomas Holst, Jonathan P. D. Abbatt, Almut Arneth, Wolfram Birmili, Hugo Denier van der Gon, Amar Hamed, András Hoffer, Lauri Laakso, Ari Laaksonen, W. Richard Leaitch, Christian Plass-Dulmer, Sara C. Pryor, Petri Räisänen, Erik Swietlicki, Alfred Wiedensohler, Douglas R. Worsnop, Veli-Matti Kerminen and Markku Kulmala
doi:10.1038/ngeo1800
Atmospheric aerosol particles can significantly influence the climate system. Analyses of observations and observation-based modelling data reveal that biogenic aerosol emissions soar in response to warming, exerting a cooling effect in a negative feedback loop.

Cloud droplet number enhanced by co-condensation of organic vapours   pp443 - 446
David Topping, Paul Connolly and Gordon McFiggans
doi:10.1038/ngeo1809
The brightness and lifetime of clouds is determined by cloud droplet number concentration, which is in turn dictated by the number of available seed particles. Model simulations suggest that condensation of semi-volatile organic compounds enhances the formation of cloud droplets, with consequences for cloud dynamics.

Robust direct effect of carbon dioxide on tropical circulation and regional precipitation   pp447 - 451
Sandrine Bony, Gilles Bellon, Daniel Klocke, Steven Sherwood, Solange Fermepin and Sébastien Denvil
doi:10.1038/ngeo1799
Predicting the response of tropical rainfall to climate change remains a challenge. An analysis of climate model simulations suggests that in an emission scenario without mitigation, a large fraction of tropical precipitation change will be independent of global surface warming over the twenty-first century.

Boreal carbon loss due to poleward shift in low-carbon ecosystems   pp452 - 456
Charles D. Koven
doi:10.1038/ngeo1801
Climate change can be thought of in terms of geographical shifts in climate properties. Tracking the geographical movement of analogous climate conditions between historical and future climate model simulations, and calculating the impact of such shifts on vegetation carbon storage, suggests that boreal forests will lose carbon as low-carbon ecosystems shift in.

Millennial-scale changes in atmospheric CO2 levels linked to the Southern Ocean carbon isotope gradient and dust flux   pp457 - 461
Martin Ziegler, Paula Diz, Ian R. Hall and Rainer Zahn
doi:10.1038/ngeo1782
In the Southern Ocean, the biological cycling of dissolved CO2 is thought to be influenced by the delivery of iron by dust particles. Reconstructions of nutrient utilization from the South Atlantic Ocean show millennial-scale links between dust flux and the efficiency of the biological pump.
See also: News and Views by Kwon & Galbraith

Andean structural control on interseismic coupling in the North Chile subduction zone   pp462 - 467
Marta Béjar-Pizarro, Anne Socquet, Rolando Armijo, Daniel Carrizo, Jeff Genrich and Mark Simons
doi:10.1038/ngeo1802
Ridges on the down-going plate in a subduction zone can segment the seismogenic zone and influence earthquake occurrence, but the role of the overriding plate is unclear. InSAR and GPS satellite measurements indicate that segmentation of the subduction zone in northern Chile correlates with a 1-km-high coastal scarp, implying that overriding plate structure can influence seismicity.

Slip weakening as a mechanism for slow earthquakes   pp468 - 472
Matt J. Ikari, Chris Marone, Demian M. Saffer and Achim J. Kopf
doi:10.1038/ngeo1818
Slow earthquakes form part of a spectrum of fault behaviour between steady creep and fast rupture during a normal earthquake. Laboratory simulations of slow slip in rock samples taken from the Nankai subduction zone, Japan, reveal similar characteristics to fast earthquakes, implying that some slow slip events could be prematurely arrested earthquakes.

Graphite formation by carbonate reduction during subduction   pp473 - 477
Matthieu E. Galvez, Olivier Beyssac, Isabelle Martinez, Karim Benzerara, Carine Chaduteau, Benjamin Malvoisin and Jacques Malavieille
doi:10.1038/ngeo1827
Carbon is carried into the Earth at subduction zones. Geochemical analysis of subducted sediments now exhumed in Alpine Corsica, France, reveal the formation of graphite during shallow subduction, implying that carbonate transformation to graphite aids transport into the deeper Earth.

Articles

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Hydrogen generation from low-temperature water–rock reactions   pp478 - 484
L. E. Mayhew, E. T. Ellison, T. M. McCollom, T. P. Trainor and A. S. Templeton
doi:10.1038/ngeo1825
Hydrogen is commonly produced during the high-temperature hydration of mafic and ultramafic rocks. Laboratory experiments suggest that water–rock reactions also generate hydrogen at lower temperatures, potentially fuelling microbial life in ultramafic aquifers in oceanic and terrestrial crust.
See also: News and Views by D'Hondt

The effect of sea level on glacial Indo-Pacific climate   pp485 - 491
Pedro N. DiNezio and Jessica E. Tierney
doi:10.1038/ngeo1823
The Indo-Pacific warm pool is the largest source of heat and moisture vapour to the atmosphere. Proxy reconstructions and model simulations suggest that during the Last Glacial Maximum, the exposure of the Sunda Shelf of Southeast Asia weakened deep convection over the warm pool.

Permanent deformation caused by subduction earthquakes in northern Chile   pp492 - 496
A. Baker, R. W. Allmendinger, L. A. Owen and J. A. Rech
doi:10.1038/ngeo1789
Earth's crust is thought to eventually rebound following an earthquake so that deformation is not permanent. Field analysis in the Atacama Desert, northern Chile, however, identifies numerous large cracks in the crust, implying that the crust here has been permanently deformed by thousands of earthquakes that have occurred over the past million years.

The shuffling rotation of the Earth's inner core revealed by earthquake doublets   pp497 - 502
Hrvoje Tkalčić, Mallory Young, Thomas Bodin, Silvie Ngo and Malcolm Sambridge
doi:10.1038/ngeo1813
Earth's inner core rotates at a different rate than the mantle, and discrepancies exist between rotation rates derived from geophysical observations and geodynamical simulations. An inverse analysis of seismic data from repeating earthquakes over the past 50[thinsp]years suggests that the rotation rate of the inner core fluctuates on decadal timescales.
See also: News and Views by Creager

Corrigendum

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Greenland meltwater as a significant and potentially bioavailable source of iron to the ocean   p503
Maya P. Bhatia, Elizabeth B. Kujawinski, Sarah B. Das, Crystaline F. Breier, Paul B. Henderson and Matthew A. Charette
doi:10.1038/ngeo1833

Errata

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Continental-scale temperature variability during the past two millennia   p503
PAGES 2k Consortium
doi:10.1038/ngeo1834

Continental-scale temperature variability during the past two millennia   p503
PAGES 2k Consortium
doi:10.1038/ngeo1849

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