Wednesday, September 30, 2015

Nature Geoscience contents: October 2015 Volume 8 Number 10 pp735-813

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Nature Geoscience

TABLE OF CONTENTS

October 2015 Volume 8, Issue 10

Editorial
Correspondence
Commentaries
News and Views
Letters
Articles
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Editorial

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Finite Earth   p735
doi:10.1038/ngeo2556
The world has agreed on 17 Sustainable Development Goals, to be adopted this week. This is great progress towards acknowledging that the planet's finite resources need to be managed carefully in the face of humanity's unlimited aspirations.

Correspondence

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Active Atlantic hurricane era at its end?   pp737 - 738
P. Klotzbach, W. Gray and C. Fogarty
doi:10.1038/ngeo2529

Commentaries

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Balancing green and grain trade   pp739 - 741
Yiping Chen, Kaibo Wang, Yishan Lin, Weiyu Shi, Yi Song & Xinhua He
doi:10.1038/ngeo2544
Since 1999, China's Grain for Green project has greatly increased the vegetation cover on the Loess Plateau. Now that erosion levels have returned to historic values, vegetation should be maintained but not expanded further as planned.

Sustainability rooted in science   pp741 - 745
Jane Lubchenco, Allison K. Barner, Elizabeth B. Cerny-Chipman & Jessica N. Reimer
doi:10.1038/ngeo2552
The United Nations' Sustainable Development Goals emphasize the importance of evidence-based decision-making. This is a clarion call for Earth scientists to contribute directly to the health, prosperity and well-being of all people.

Sustainable early-career networks   pp745 - 746
Florian Rauser, Vera Schemann & Sebastian Sonntag
doi:10.1038/ngeo2541
A truly global science community for the next generation of researchers will be essential if we are to tackle Earth system sustainability. Top-down support from funders should meet bottom-up initiatives — at a pace fast enough to meet that of early-career progress.

News and Views

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Planetary science: Carbon in the Moon   pp747 - 748
Bruno Scaillet
doi:10.1038/ngeo2530
The Moon was once thought to be depleted in volatile elements. Analyses of the carbon contents of lunar volcanic glasses reveal that carbon monoxide degassing could have produced the fire-fountain eruptions from which these glasses were formed.
See also: Letter by Wetzel et al.

Biogeochemistry: Soil carbon in a beer can   pp748 - 749
Eric A. Davidson
doi:10.1038/ngeo2522
Decomposition of soil organic matter could be an important positive feedback to climate change. Geochemical properties of soils can help determine what fraction of soil carbon may be protected from climate-induced decomposition.
See also: Letter by Doetterl et al.

William R. Dickinson: Plate tectonic pioneer   p750
Timothy F. Lawton
doi:10.1038/ngeo2551

Atmospheric chemistry: Breathing easier in the Amazon   pp751 - 752
Christine Wiedinmyer
doi:10.1038/ngeo2550
Fires related to Amazonian deforestation are a large source of particulate matter emissions. Satellite measurements and models reveal that reductions in deforestation and fire emissions since 2001 have prevented hundreds of premature deaths each year.
See also: Letter by Reddington et al.

Land-use Change: Deforestation by land grabbers   pp752 - 753
Tom Rudel
doi:10.1038/ngeo2549
Leases of land concessions in Cambodia have accelerated in the last ten years. An analysis using high-resolution maps and official documents shows that deforestation rates in the land concessions are higher than in other areas.
See also: Letter by Davis et al.

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Letters

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Carbon content and degassing history of the lunar volcanic glasses   pp755 - 758
Diane T. Wetzel, Erik H. Hauri, Alberto E. Saal & Malcolm J. Rutherford
doi:10.1038/ngeo2511
The volatile-rich eruptions required to produce the lunar volcanic glasses are at odds with a volatile-poor Moon. Analyses of the glasses suggest that there was enough of the volatile element carbon in the parent magmas to drive the eruptions.
See also: News and Views by Scaillet

Two distinct influences of Arctic warming on cold winters over North America and East Asia   pp759 - 762
Jong-Seong Kug, Jee-Hoon Jeong, Yeon-Soo Jang, Baek-Min Kim, Chris K. Folland, Seung-Ki Min & Seok-Woo Son
doi:10.1038/ngeo2517
Possible impact of Arctic warming on the mid-latitudes has sparked interest. Analyses of observations and climate model simulations reveal two distinct patterns of Arctic warming that affect East Asia and North America, respectively.
Watch an audio-visual summary of the paper here

Rainfall consistently enhanced around the Gezira Scheme in East Africa due to irrigation   pp763 - 767
Ross E. Alter, Eun-Soon Im & Elfatih A. B. Eltahir
doi:10.1038/ngeo2514
Land-use changes can modify regional climate patterns. A comparison of climate simulations and observations show that a large-scale irrigation scheme in East Africa inhibits rainfall over the irrigation scheme, while enhancing it further away.
Watch an audio-visual summary of the paper here

Air quality and human health improvements from reductions in deforestation-related fire in Brazil   pp768 - 771
C. L. Reddington, E. W. Butt, D. A. Ridley, P. Artaxo, W. T. Morgan, H. Coe & D. V. Spracklen
doi:10.1038/ngeo2535
Fires are used to clear tropical forests. Satellite measurements and simulations show that reductions in deforestation and associated fires in Brazil have reduced emissions of particulate matter, preventing between 400 and 1,700 deaths annually.
See also: News and Views by Wiedinmyer

Accelerated deforestation driven by large-scale land acquisitions in Cambodia   pp772 - 775
Kyle Frankel Davis, Kailiang Yu, Maria Cristina Rulli, Lonn Pichdara & Paolo D'Odorico
doi:10.1038/ngeo2540
More than 2 million hectares of Cambodian land have been leased to investors since 2000. Combined satellite and local records show that deforestation on leased land is 29% to 105% higher than in comparable unleased areas.
See also: News and Views by Rudel

Formation of soil organic matter via biochemical and physical pathways of litter mass loss   pp776 - 779
M. Francesca Cotrufo, Jennifer L. Soong, Andrew J. Horton, Eleanor E. Campbell, Michelle L. Haddix, Diana H. Wall & William J. Parton
doi:10.1038/ngeo2520
Soil organic matter is a large global carbon pool. Isotopic labelling of litter in the lab and the field reveals that soil organic matter forms from labile organic compounds and litter fragments early and late in decomposition, respectively.
Watch an audio-visual summary of the paper here

Soil carbon storage controlled by interactions between geochemistry and climate   pp780 - 783
Sebastian Doetterl, Antoine Stevens, Johan Six, Roel Merckx, Kristof Van Oost, Manuel Casanova Pinto, Angélica Casanova-Katny, Cristina Muñoz, Mathieu Boudin, Erick Zagal Venegas & Pascal Boeckx
doi:10.1038/ngeo2516
Rising temperature can increase soil organic matter decomposition and CO2 emissions. In a 4,000 km north–south transect in Chile and Antarctica, soil geochemistry, which can be modified by climate, is the dominant direct control of carbon storage.
See also: News and Views by Davidson

Estimates of volcanic-induced cooling in the Northern Hemisphere over the past 1,500 years   pp784 - 788
Markus Stoffel, Myriam Khodri, Christophe Corona, Sébastien Guillet, Virginie Poulain, Slimane Bekki, Joël Guiot, Brian H. Luckman, Clive Oppenheimer, Nicolas Lebas, Martin Beniston & Valérie Masson-Delmotte
doi:10.1038/ngeo2526
Model and proxy-based estimates of climate cooling from volcanic eruptions have disagreed. Refined simulations and tree-ring time series converge on a total of 0.8 to 1.3 °C of cooling in the Northern Hemisphere from the 1257 and 1815 eruptions.

Minimal erosion of Arctic alpine topography during late Quaternary glaciation   pp789 - 792
Endre F. Gjermundsen, Jason P. Briner, Naki Akçar, Jørn Foros, Peter W. Kubik, Otto Salvigsen & Anne Hormes
doi:10.1038/ngeo2524
Alpine topography in Europe has been shaped by recent glaciations. Cosmogenic dating of summits in Svalbard suggest that Arctic alpine topography is a million years old and that subsequent glaciations have preserved rather than eroded the landscape.

Open-system dynamics and mixing in magma mushes   pp793 - 796
G. W. Bergantz, J. M. Schleicher & A. Burgisser
doi:10.1038/ngeo2534
Magma in Earth's crust is in a crystal-rich mushy state, yet must be fluidized before eruptions. Numerical simulations show that rapid injection of new magma into a reservoir creates a mixing bowl of fluid and crystals that are able to erupt.

Cratonic root beneath North America shifted by basal drag from the convecting mantle   pp797 - 800
Mikhail K. Kaban, Walter D. Mooney & Alexey G. Petrunin
doi:10.1038/ngeo2525
Continental cores, or cratons, are thought to have been stable for billions of years. Analysis of seismic images, however, suggests that the craton root deep beneath North America may have been shifted by mantle flow.

Articles

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Coastal vulnerability across the Pacific dominated by El Niño/Southern Oscillation   pp801 - 807
Patrick L. Barnard, Andrew D. Short, Mitchell D. Harley, Kristen D. Splinter, Sean Vitousek, Ian L. Turner, Jonathan Allan, Masayuki Banno, Karin R. Bryan, André Doria, Jeff E. Hansen, Shigeru Kato, Yoshiaki Kuriyama, Evan Randall-Goodwin, Peter Ruggiero, Ian J. Walker & Derek K. Heathfield
doi:10.1038/ngeo2539
The dynamic components of coastal water level can add metres to water levels during extreme events. A data synthesis reveals that Pacific regional wave and water level fluctuations are closely related to the El Niño/Southern Oscillation.

Secular change in Archaean crust formation recorded in Western Australia   pp808 - 813
Huaiyu Yuan
doi:10.1038/ngeo2521
It is unclear how Archaean crust formed. Analysis of seismic data from Western Australia suggests that ancient crust first formed in mantle plume-like settings and later in subduction zones, possibly in response to secular cooling of the mantle.

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