Monday, October 1, 2012

Nature Geoscience contents: October 2012 Volume 5 Number 10 pp675-754

Nature Geoscience

TABLE OF CONTENTS

October 2012 Volume 5, Issue 10

Editorial
Correspondence
Commentary
In the press
Books and Arts
Research Highlights
News and Views
Correction
Progress Article
Letters
Articles
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Nature Geoscience web focus - Rivers

Rivers connect the highest mountains with the ocean's depth, carving up the land as they flow. En route, they transport and transform large quantities of terrestrial material, and exchange elements with the atmosphere, land and sea. In this web focus we present opinion pieces and research articles that examine the topographic, biogeochemical and cultural significance of rivers.

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Editorial

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Rivers in transition   p675
doi:10.1038/ngeo1606
Rivers run through nearly every landscape on Earth. Ascertaining the influence of this flux on carbon dynamics is necessary for a full understanding of the climate system.

Correspondence

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Problematic plate reconstruction   pp676 - 677
Brian E. Tucholke & Jean-Claude Sibuet
doi:10.1038/ngeo1596
See also: Correspondence by Bronner et al.

Reply to 'Problematic plate reconstruction'   p677
Adrien Bronner, Daniel Sauter, Gianreto Manatschal, Gwén Peron-Pinvidic & Marc Munschy
doi:10.1038/ngeo1597
See also: Correspondence by Tucholke & Sibuet

Commentary

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An expanded role for river networks   pp678 - 679
Jonathan P. Benstead & David S. Leigh
doi:10.1038/ngeo1593
Estimates of stream and river area have relied on observations at coarse resolution. Consideration of the smallest and most dynamic streams could reveal a greater role for river networks in global biogeochemical cycling than previously thought.

In the press

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The state of the seas   p680
Mark Schrope
doi:10.1038/ngeo1592

Books and Arts

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Tributaries through time   p681
Anna Armstrong reviews Rivers: A Very Short Introduction by Nick Middleton
doi:10.1038/ngeo1598

Research Highlights

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Tsunami: Onshore shake-up | Planetary science: Mars bedevilled | Palaeoclimate: Circulation shrinkage | Biogeochemistry: Arctic nitrogen fix

News and Views

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Planetary science: Uninhabitable martian clays?   pp683 - 684
Brian Hynek
doi:10.1038/ngeo1560
Clay minerals on Mars have been interpreted as an indication for a warm, wet early climate. A new hypothesis proposes that the minerals instead formed during brief periods of magmatic degassing, diminishing the prospects for signs of life in these settings.
See also: Article by Meunier et al.

Biogeochemistry: Riverine carbon unravelled   p684
Anna Armstrong
doi:10.1038/ngeo1599

Air quality: Emissions versus climate change   pp685 - 686
Christian Hogrefe
doi:10.1038/ngeo1591
Climate change is likely to offset some of the improvements in air quality expected from reductions in pollutant emissions. A comprehensive analysis of future air quality over North America suggests that, on balance, the air will still be cleaner in coming decades.

Volcanology: A volcano's sharp intake of breath   pp686 - 687
Andrew Hooper
doi:10.1038/ngeo1584
Shallow magma bodies that feed regularly erupting volcanoes are usually considered enduring features that grow steadily between eruptions. Measurements of deformation at Santorini, however, reveal sudden rapid magma accumulation after half a century of rest.
See also: Article by Parks et al.

Geomorphology: Tectonically twisted rivers   pp688 - 689
Eric Kirby
doi:10.1038/ngeo1594
Tracking diffuse, shearing deformation of continents is difficult. Numerical modelling of drainage evolution in the Southern Alps, New Zealand, suggests that rivers can act as dynamic markers of tectonic deformation over geological timescales.

Climate change: Tropical extremes   pp689 - 690
Geert Lenderink
doi:10.1038/ngeo1587
Climate model projections of future precipitation extremes in the tropics are highly uncertain. Observations of year-to-year variations in extremes of present-day climate help to narrow down these projections to a rise in extreme rainfall by 6-14% per °C of warming.
See also: Letter by O'Gorman

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Correction

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Hydrology: Supply and demand   p690
doi:10.1038/ngeo1607

Progress Article

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An update on Earth's energy balance in light of the latest global observations   pp691 - 696
Graeme L. Stephens, Juilin Li, Martin Wild, Carol Anne Clayson, Norman Loeb, Seiji Kato, Tristan L'Ecuyer, Paul W. Stackhouse, Jr, Matthew Lebsock & Timothy Andrews
doi:10.1038/ngeo1580
Climate change is governed by changes to the global energy balance. A synthesis of the latest observations suggests that more longwave radiation is received at the Earth's surface than previously thought, and that more precipitation is generated.

Letters

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Sensitivity of tropical precipitation extremes to climate change   pp697 - 700
Paul A. O'Gorman
doi:10.1038/ngeo1568
Precipitation extremes increase in intensity over many regions of the globe in simulations of a warming climate, but not always consistently. Observational constraints, together with a close relationship between model responses to interannual variability and climate change, suggest a high sensitivity of tropical extreme precipitation to warming.
See also: News and Views by Lenderink

Modelled suppression of boundary-layer clouds by plants in a CO2-rich atmosphere   pp701 - 704
Jordi Vilà-Guerau de Arellano, Chiel C. van Heerwaarden & Jos Lelieveld
doi:10.1038/ngeo1554
Boundary-layer clouds modify the near-surface climate and interact with the water and carbon cycles. Biophysical modelling suggests that rising atmospheric CO2 levels and the associated closing of plant stomata may suppress boundary-layer cloud formation in the mid-latitudes, and demonstrates how biological and physical aspects of the climate system are intertwined.

Elevation-dependent influence of snow accumulation on forest greening   pp705 - 709
Ernesto Trujillo, Noah P. Molotch, Michael L. Goulden, Anne E. Kelly & Roger C. Bales
doi:10.1038/ngeo1571
Increased temperatures and declines in water availability have influenced the productivity of mountain forests over the past half century. An analysis of 25 years of observational and satellite data suggests that mid-elevation forest greenness is strongly regulated by snow accumulation.

Biogeochemically diverse organic matter in Alpine glaciers and its downstream fate   pp710 - 714
Gabriel A. Singer, Christina Fasching, Linda Wilhelm, Jutta Niggemann, Peter Steier, Thorsten Dittmar & Tom J. Battin
doi:10.1038/ngeo1581
Glaciers store and transform organic carbon, which, on release, could support downstream microbial life. An analysis of 26 glaciers in the European Alps suggests that a significant fraction of glacier organic matter is available for microbial consumption.

Dependence of riverine nitrous oxide emissions on dissolved oxygen levels   pp715 - 718
Madeline S. Rosamond, Simon J. Thuss & Sherry L. Schiff
doi:10.1038/ngeo1556
Nitrous oxide is a potent greenhouse gas that destroys stratospheric ozone. Measurements of nitrous oxide emissions from a Canadian river suggest that future increases in nitrate export to rivers will not necessarily lead to higher nitrous oxide emissions, but more widespread hypoxia most likely will.

Significant contribution to climate warming from the permafrost carbon feedback   pp719 - 721
Andrew H. MacDougall, Christopher A. Avis & Andrew J. Weaver
doi:10.1038/ngeo1573
Permafrost soils contain almost twice as much carbon as the current atmospheric carbon pool. Climate model simulations suggest that the feedback generated by future permafrost carbon release could lead to a further warming of 0.13-1.69 °C by 2300.

Contributions to late Archaean sulphur cycling by life on land   pp722 - 725
Eva E. Stüeken, David C. Catling & Roger Buick
doi:10.1038/ngeo1585
Life on land dates back at least 2.7 billion years, but the effects of this early terrestrial biosphere on biogeochemical cycling are poorly constrained. Marine sulphur data and geochemical modelling suggest that microbial pyrite weathering has transferred a substantial amount of sulphur to the oceans for at least 2.5 billion years.

Mantle flow deflected by interactions between subducted slabs and cratonic keels   pp726 - 730
Meghan S. Miller & Thorsten W. Becker
doi:10.1038/ngeo1553
Subducting slabs can influence mantle flow, but the importance of neighbouring continental cratons is little understood. Geodynamical modelling, constrained by seismic data that identify regions of mantle flow beneath the Caribbean-South American Plate margin, shows that the deep-rooted South American craton acts to deflect and enhance mantle flow into a narrow channel.

Episodic tremor and slow slip potentially linked to permeability contrasts at the Moho   pp731 - 734
Ikuo Katayama, Tatsuya Terada, Keishi Okazaki & Wataru Tanikawa
doi:10.1038/ngeo1559
Slow earthquakes in subduction zones have been linked to high pore-fluid pressures. Laboratory measurements reveal a high permeability contrast between crust and mantle rocks, implying that water released from the subducting slab could accumulate at the crust-mantle boundary of the overlying plate, raising pore-fluid pressures and generating slow earthquakes.

Hotspot trails in the South Atlantic controlled by plume and plate tectonic processes   pp735 - 738
John M. O'Connor, Wilfried Jokat, Anton P. le Roex, Cornelia Class, Jan R. Wijbrans, Stefanie Keβling, Klaudia F. Kuiper & Oliver Nebel
doi:10.1038/ngeo1583
Seamount chains in the southeast Atlantic Ocean are thought to have formed above plumes sourced from the deep mantle. Dating of lavas erupted along the trails show that the formation and distribution of the seamount chains is also controlled by the motion and structure of the African Plate.

Articles

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Magmatic precipitation as a possible origin of Noachian clays on Mars   pp739 - 743
Alain Meunier, Sabine Petit, Bethany L. Ehlmann, Patrick Dudoignon, Frances Westall, Antoine Mas, Abderrazak El Albani & Eric Ferrage
doi:10.1038/ngeo1572
Hydrous clay minerals detected on the ancient martian crust have been proposed to have formed by aqueous weathering on a warm, wet early Mars. However, analyses of terrestrial clay minerals and comparisons to Mars suggest that the Noachian clays could have alternatively formed by precipitation from magmatic fluids.
See also: News and Views by Hynek

River drainage patterns in the New Zealand Alps primarily controlled by plate tectonic strain   pp744 - 748
Sébastien Castelltort, Liran Goren, Sean D. Willett, Jean-Daniel Champagnac, Frédéric Herman & Jean Braun
doi:10.1038/ngeo1582
The persistence of dendritic drainage patterns implies that rivers reorganize after a tectonic perturbation, preserving no long-term record of that tectonic event. Numerical simulations of the evolution of drainage patterns in the Southern Alps, New Zealand, however, reveal rivers that resist reorganization and thus preserve a record of plate tectonic strain over 10 million years.

Evolution of Santorini Volcano dominated by episodic and rapid fluxes of melt from depth   pp749 - 754
Michelle M. Parks, Juliet Biggs, Philip England, Tamsin A. Mather, Paraskevi Nomikou, Kirill Palamartchouk, Xanthos Papanikolaou, Demitris Paradissis, Barry Parsons, David M. Pyle, Costas Raptakis & Vangelis Zacharis
doi:10.1038/ngeo1562
Santorini Volcano in Greece was thought to be continually charged by small injections of magma. Measurements of surface deformation show that magma equivalent to 10-50% of that emitted in previous small eruptions has been injected beneath Santorini since January 2011, implying that the volcano is instead charged by rapid, episodic fluxes of melt.
See also: News and Views by Hooper

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