Thursday, January 31, 2013

Nature Geoscience contents: February 2013 Volume 6 Number 2 pp77-152

Nature Geoscience

TABLE OF CONTENTS

February 2013 Volume 6, Issue 2

Editorials
Correspondence
Commentary
In the press
Research Highlights
News and Views
Letters
Articles
Erratum


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GEOMICROBIOLOGY FROM THE ISME JOURNAL

Manganese Uptake Systems In Marine Bacteria
RT Green et al ¦ doi: 10.1038/ismej.2012.140

Carbon cycling in deep-sea sediments
DJ Mayor et al ¦ doi:10.1038/ismej.2012.14
 

Editorials

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Communication at risk   p77
doi:10.1038/ngeo1728
The L'Aquila earthquake trial tragically highlights that risk communication is integral to Earth science training.

Expanding spheres of interest   p77
doi:10.1038/ngeo1729
Extrasolar planet research is booming. We welcome submissions with links to the geosciences.
See also: Commentary by Pierrehumbert

Correspondence

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Caprock corrosion   pp79 - 80
P. J. Armitage, D. R. Faulkner & R. H. Worden
doi:10.1038/ngeo1716

Commentary

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Strange news from other stars   pp81 - 83
Raymond T. Pierrehumbert
doi:10.1038/ngeo1711
The dawn of exoplanet discovery has unearthed a rich tapestry of planets different from anything encountered in the Solar System. Geoscientists can and should be in the vanguard of investigating what is out there in the Universe.
See also: Editorial

In the press

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Soil or sea for ancient fossils?   p84
Nicola Jones
doi:10.1038/ngeo1713

Research Highlights

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Geodynamics: Dense mountain roots | Palaeoceanography: Sea level trigger | Planetary science: Ridged terrain | Climate science: Shifting storm tracks

News and Views

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Palaeoclimate: Weathering away warmth   pp86 - 87
Brian A. Haley
doi:10.1038/ngeo1714
At the end of the Eocene epoch, permanent ice cover developed over Antarctica as the Earth began to cool from greenhouse warmth. Sediment records off the Antarctic coast show spikes in weathering rate at the onset of ice growth that may indicate synchronous consumption of atmospheric carbon dioxide.
See also: Letter by Basak & Martin

Climate science: The heat is on in Antarctica   pp87 - 88
Eric J. Steig & Anais J. Orsi
doi:10.1038/ngeo1717
The Antarctic Peninsula has long been thought to be the only part of Antarctica that has warmed in recent decades. Careful detective work confirms that West Antarctica is also warming rapidly.
See also: Article by Bromwich et al.

Deep Earth: Core–mantle boundary landscapes   pp89 - 90
Sebastian Rost
doi:10.1038/ngeo1715
The molten-iron alloy of the core meets the mantle's silicate rock at Earth's core–mantle boundary. Seismological images reveal hummocks of iron-enriched material above the boundary, highlighting the heterogeneous nature of the mantle.

Cryosphere: Interglacial ice sheet survival   p90
Alicia Newton
doi:10.1038/ngeo1721

Palaeoclimate: Asian connections   pp91 - 92
Carrie Morrill
doi:10.1038/ngeo1718
About 8,200 years ago, the overturning circulation in the Atlantic Ocean slowed and the Northern Hemisphere cooled. A speleothem record from China reveals a period of drying that occurred almost simultaneously with the cooling recorded by the Greenland ice cores.
See also: Letter by Liu et al.

Geoscience
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ETH Zurich
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Letters

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Solid-state plastic deformation in the dynamic interior of a differentiated asteroid   pp93 - 97
B. J. Tkalcec, G. J. Golabek & F. E. Brenker
doi:10.1038/ngeo1710
Diogenite meteorites are thought to represent mantle rocks that formed as cumulates in magma chambers on 4 Vesta or a similar differentiated asteroid. Microstructural analysis of olivine grains from a diogenite meteorite show that the preferred orientation of their crystal lattice was formed through plastic deformation, indicating dynamic, planet-like processes in its parent body.

Enhanced seasonal forecast skill following stratospheric sudden warmings   pp98 - 102
M. Sigmond, J. F. Scinocca, V. V. Kharin & T. G. Shepherd
doi:10.1038/ngeo1698
Advances in seasonal forecasting have brought widespread socio-economic benefits. A modelling study suggests that tropospheric forecast skill is enhanced when the forecast model is initialized at the onset of a stratospheric sudden warming event.

Hotspots of anaerobic ammonium oxidation at land-freshwater interfaces   pp103 - 107
Guibing Zhu, Shanyun Wang, Weidong Wang, Yu Wang, Leiliu Zhou, Bo Jiang, Huub J. M. Op den Camp, Nils Risgaard-Petersen, Lorenz Schwark, Yongzhen Peng, Mariet M. Hefting, Mike S. M. Jetten & Chengqing Yin
doi:10.1038/ngeo1683
Anammox, anaerobic ammonium oxidation, accounts for over 50% of nitrogen loss in marine ecosystems. A field study in north China reveals hotspots of anammox activity in sediments sampled from land–lake interfaces.

Atmospheric iodine levels influenced by sea surface emissions of inorganic iodine   pp108 - 111
Lucy J. Carpenter, Samantha M. MacDonald, Marvin D. Shaw, Ravi Kumar, Russell W. Saunders, Rajendran Parthipan, Julie Wilson & John M. C. Plane
doi:10.1038/ngeo1687
Naturally occurring bromine- and iodine-containing compounds substantially reduce regional, and possibly global, tropospheric ozone levels. Experimental and model results suggest that the reaction of ozone with iodide could account for around 75% of observed iodine oxide levels over the tropical Atlantic Ocean.

Sea surface temperature in the north tropical Atlantic as a trigger for El Niño/Southern Oscillation events   pp112 - 116
Yoo-Geun Ham, Jong-Seong Kug, Jong-Yeon Park and Fei-Fei Jin
doi:10.1038/ngeo1686
The El Niño/Southern Oscillation in the Pacific Ocean influences temperature in other tropical ocean basins. Reanalysis data and model simulations suggest that temperature anomalies in the north tropical Atlantic may also influence the development of La Niña events.

Links between the East Asian monsoon and North Atlantic climate during the 8,200 year event   pp117 - 120
Y-H. Liu, G. M. Henderson, C-Y. Hu, A. J. Mason, N. Charnley, K. R. Johnson & S-C. Xie
doi:10.1038/ngeo1708
A period of cooling in the North Atlantic region 8,200 years ago affected climate throughout the Northern Hemisphere. A speleothem record from central China indicates that a dry period lasting 150 years was associated with the 8,200 year event.
See also: News and Views by Morrill

Antarctic weathering and carbonate compensation at the Eocene–Oligocene transition   pp121 - 124
Chandranath Basak & Ellen E. Martin
doi:10.1038/ngeo1707
During the Eocene–Oligocene transition, a permanent ice sheet was established on Antarctica. Marine sediment geochemistry indicates a period of intense weathering associated with the inception of the ice sheet.
See also: News and Views by Haley

Bioavailability of zinc in marine systems through time   pp125 - 128
Clint Scott, Noah J. Planavsky, Chris L. Dupont, Brian Kendall, Benjamin C. Gill, Leslie J. Robbins, Kathryn F. Husband, Gail L. Arnold, Boswell A. Wing, Simon W. Poulton, Andrey Bekker, Ariel D. Anbar, Kurt O. Konhauser & Timothy W. Lyons
doi:10.1038/ngeo1679
Zinc is a marine nutrient that may have been limited in the early oceans. Estimates of marine zinc availability through time suggest that values were instead near-modern during the Proterozoic eon.

Highly vesicular pumice generated by buoyant detachment of magma in subaqueous volcanism   pp129 - 132
Melissa D. Rotella, Colin J. N. Wilson, Simon J. Barker & Ian C. Wright
doi:10.1038/ngeo1709
Deposits of highly vesicular pumice that blanket submarine volcanoes are often attributed to explosive eruptions. Density and textural analysis of clasts dredged from the submarine Macauley Volcano, southwest Pacific Ocean, however, reveal an eruptive style that is neither explosive nor effusive, with clasts instead forming from buoyant detachment of a magma foam.

Articles

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Groundwater activity on Mars and implications for a deep biosphere   pp133 - 138
Joseph R. Michalski, Javier Cuadros, Paul B. Niles, John Parnell, A. Deanne Rogers & Shawn P. Wright
doi:10.1038/ngeo1706
The subsurface of Mars could potentially have contained a vast microbial biosphere. An evaluation of the possibility of groundwater upwelling, which might provide clues to subsurface habitability, reveals evidence in the deep McLaughlin crater for clays and carbonates that probably formed in an alkaline, groundwater-fed lacustrine setting.

Central West Antarctica among the most rapidly warming regions on Earth   pp139 - 145
David H. Bromwich, Julien P. Nicolas, Andrew J. Monaghan, Matthew A. Lazzara, Linda M. Keller, George A. Weidner & Aaron B. Wilson
doi:10.1038/ngeo1671
The West Antarctic Ice Sheet is contributing to sea-level rise, but temperature trends in the region have remained uncertain. A complete temperature record for Byrd Station in central West Antarctica, spanning from 1958 to 2010, establishes West Antarctica as one of the fastest-warming regions globally.
See also: News and Views by Steig & Orsi

Atlantic Ocean CO2 uptake reduced by weakening of the meridional overturning circulation   pp146 - 152
Fiz F. Péréz, Herlé Mercier, Marcos Vázquez-Rodríguez, Pascale Lherminier, Anton Velo, Paula C. Pardo, Gabriel Rosón & Aida F. Ríos
doi:10.1038/ngeo1680
Uptake of atmospheric carbon dioxide in the subpolar North Atlantic Ocean declined rapidly between 1990 and 2006. An analysis of oceanographic data suggests that the slowdown of the meridional overturning circulation was largely responsible.

Erratum

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Primary surface ruptures of the great Himalayan earthquakes in 1934 and 1255   p152
S. N. Sapkota, L. Bollinger, Y. Klinger, P. Tapponnier, Y. Gaudemer & D. Tiwari
doi:10.1038/ngeo1720

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