TABLE OF CONTENTS |
February 2013 Volume 6, Issue 2 |
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 | Editorials Correspondence Commentary In the press Research Highlights News and Views Letters Articles Erratum
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Editorials | Top |
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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.
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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 |
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Correspondence | Top |
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Caprock corrosion pp79 - 80 P. J. Armitage, D. R. Faulkner & R. H. Worden doi:10.1038/ngeo1716
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Commentary | Top |
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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 |
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In the press | Top |
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Soil or sea for ancient fossils? p84 Nicola Jones doi:10.1038/ngeo1713
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Research Highlights | Top |
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Geodynamics: Dense mountain roots | Palaeoceanography: Sea level trigger | Planetary science: Ridged terrain | Climate science: Shifting storm tracks |
News and Views | Top |
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Letters | Top |
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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.
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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.
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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.
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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.
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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.
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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 |
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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 |
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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.
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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.
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Articles | Top |
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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.
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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 |
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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.
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Erratum | Top |
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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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