TABLE OF CONTENTS
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November 2012 Volume 5, Issue 11 |
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| The publication of this issue was delayed due to Hurricane Sandy closing our New York offices temporarily. We apologize for any inconvenience caused. |
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Editorial | Top |
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Eastern promise p755 doi:10.1038/ngeo1636 Research in Asia, and particularly in China, is catching up with the traditional hotbeds of science. The next step towards a more even geographical distribution of research will be a higher proportion of top-level publications led by scientists at Chinese labs. |
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Correspondence | Top |
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Giant Lake Geneva tsunami in ad 563 pp756 - 757 Katrina Kremer, Guy Simpson & Stéphanie Girardclos doi:10.1038/ngeo1618 |
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Commentary | Top |
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Restoration sedimentology pp758 - 759 Douglas A. Edmonds doi:10.1038/ngeo1620 River regulation and sea-level rise have damaged deltaic ecosystems as well as the sedimentological processes that support them. More scientific effort needs to be directed towards restoring land-building processes in our vanishing deltas. |
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In the press | Top |
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Iron man's impact p760 Mark Schrope doi:10.1038/ngeo1621 |
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Books and Arts | Top |
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A most excellent adventure through time p761 Euan G. Nisbet reviews How to Build a Habitable Planet by Charles H. Langmuir and Wally Broecker doi:10.1038/ngeo1624 |
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Research Highlights | Top |
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Planetary science: Vesta's veneer | Palaeoclimate: Sun and wind | Marine chemistry: Oceanic oxygen loss | Deep earth: Anomalous mantle |
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News and Views | Top |
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Progress Article | Top |
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Biological processes on glacier and ice sheet surfaces pp771 - 774 Marek Stibal, Marie Šabacká & Jakub Žárský doi:10.1038/ngeo1611 Glacial ice covers around 10% of the Earth's continents. A review of the literature suggests that microbes living on glaciers and ice sheets are an integral part of both the glacial environment and the Earth's ecosystem. |
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Letters | Top |
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Compositional evidence for an impact origin of the Moon's Procellarum basin pp775 - 778 Ryosuke Nakamura, Satoru Yamamoto, Tsuneo Matsunaga, Yoshiaki Ishihara, Tomokatsu Morota, Takahiro Hiroi, Hiroshi Takeda, Yoshiko Ogawa, Yasuhiro Yokota, Naru Hirata, Makiko Ohtake & Kazuto Saiki doi:10.1038/ngeo1614 The nearside and farside of the Moon are compositionally distinct. The detection of low-calcium pyroxene around large impact basins suggests that the huge Procellarum basin on the nearside may be an ancient impact structure and a relic scar of the violent collision that produced the lunar dichotomy. |
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Direct measurement of hydroxyl in the lunar regolith and the origin of lunar surface water pp779 - 782 Yang Liu, Yunbin Guan, Youxue Zhang, George R. Rossman, John M. Eiler & Lawrence A. Taylor doi:10.1038/ngeo1601 Over the past few years, it has become clear that the Moon's surface is not entirely dry. The direct identification of hydroxyl in glasses produced in lunar soils by the impact of micrometeorites supports the idea that water was delivered to the lunar surface by the solar wind. See also: News and Views by Chaussidon |
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A stratospheric connection to Atlantic climate variability pp783 - 787 Thomas Reichler, Junsu Kim, Elisa Manzini & Jürgen Kröger doi:10.1038/ngeo1586 Stratospheric circulation is known to affect weather in the troposphere. Climate modelling reveals a connection between variations in the stratospheric and North Atlantic ocean circulation over the past 30 years, and demonstrates that the stratosphere is an important component of climate over multidecadal timescales. |
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Atlantic Ocean influence on a shift in European climate in the 1990s pp788 - 792 Rowan T. Sutton & Buwen Dong doi:10.1038/ngeo1595 The Atlantic Ocean has been suggested as an important driver of variability in European climate on decadal timescales. Analyses of ocean and atmosphere temperature data from observations suggest that the shift in European climate during the 1990s was a result of warming in the North Atlantic Ocean. |
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Unusual Southern Hemisphere tree growth patterns induced by changes in the Southern Annular Mode pp793 - 798 Ricardo Villalba, Antonio Lara, Mariano H. Masiokas, Rocío Urrutia, Brian H. Luckman, Gareth J. Marshall, Ignacio A. Mundo, Duncan A. Christie, Edward R. Cook, Raphael Neukom, Kathryn Allen, Pavla Fenwick, José A. Boninsegna, Ana M. Srur, Mariano S. Morales, Diego Araneo, Jonathan G. Palmer, Emilio Cuq, Juan C. Aravena, Andres Holz & Carlos LeQuesne doi:10.1038/ngeo1613 Recent changes in the Southern Annular Mode are associated with warmer, drier conditions in the Southern Hemisphere. An analysis of tree-ring records there suggests that these changes have significantly altered tree growth. See also: News and Views by Jones |
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Ice-stream stability on a reverse bed slope pp799 - 802 Stewart S. R. Jamieson, Andreas Vieli, Stephen J. Livingstone, Colm Ó Cofaigh, Chris Stokes, Claus-Dieter Hillenbrand & Julian A. Dowdeswell doi:10.1038/ngeo1600 Marine ice streams whose beds deepen inland are thought to be inherently unstable. Numerical modelling of the Maguerite Bay ice-stream retreat in West Antarctica since the Last Glacial Maximum suggests that an ice stream can stabilize on an inland-sloping bed owing to increased lateral drag where the ice stream narrows. |
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Linking the historic 2011 Mississippi River flood to coastal wetland sedimentation pp803 - 807 Federico Falcini, Nicole S. Khan, Leonardo Macelloni, Benjamin P. Horton, Carol B. Lutken, Karen L. McKee, Rosalia Santoleri, Simone Colella, Chunyan Li, Gianluca Volpe, Marco D'Emidio, Alessandro Salusti & Douglas J. Jerolmack doi:10.1038/ngeo1615 In spring 2011, a record-breaking flood necessitated diversion of water from the lower Mississippi River to the Atchafalaya River Basin. A comparison between the dynamics in the two basins based on field-calibrated satellite observations and in situ data suggests that river-mouth dynamics and wetland sedimentation are directly linked. |
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Variability of the North Atlantic Oscillation over the past 5,200 years pp808 - 812 Jesper Olsen, N. John Anderson & Mads F. Knudsen doi:10.1038/ngeo1589 The North Atlantic Oscillation influences climate in the Arctic region and northern Europe. Reconstructions of circulation patterns associated with the North Atlantic Oscillation from a 5,200-year-long lake sediment record suggest that the atmospheric circulation responded to significant transitions in Northern Hemisphere climate. |
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Strength and geometry of the glacial Atlantic Meridional Overturning Circulation pp813 - 816 Jörg Lippold, Yiming Luo, Roger Francois, Susan E. Allen, Jeanne Gherardi, Sylvain Pichat, Ben Hickey & Hartmut Schulz doi:10.1038/ngeo1608 During the Last Glacial Maximum, the pattern of Atlantic Meridional Overturning Circulation was different from today. A combination of sediment chemistry and a scavenging model suggests that the glacial circulation was shallower and at least as vigorous as today. |
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North Atlantic forcing of Amazonian precipitation during the last ice age pp817 - 820 Nicole A. S. Mosblech, Mark B. Bush, William D. Gosling, David Hodell, Louise Thomas, Peter van Calsteren, Alexander Correa-Metrio, Bryan G. Valencia, Jason Curtis & Robert van Woesik doi:10.1038/ngeo1588 The last glacial period was marked by rapid reorganizations of oceanic and atmospheric circulation. Speleothem records from the Amazon Basin suggest that precipitation variability was linked to these events. |
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The 2011 Lorca earthquake slip distribution controlled by groundwater crustal unloading pp821 - 825 Pablo J. González, Kristy F. Tiampo, Mimmo Palano, Flavio Cannavó & José Fernández doi:10.1038/ngeo1610 Earthquake rupture is influenced by stress conditions in the crust before the quake. Analysis and modelling of surface deformation caused by the May 2011 earthquake in Lorca, Spain, indicate that groundwater extraction influenced the pattern of fault rupture. See also: News and Views by Avouac |
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Coupling at Mauna Loa and Kīlauea by stress transfer in an asthenospheric melt layer pp826 - 829 Helge M. Gonnermann, James H. Foster, Michael Poland, Cecily J. Wolfe, Benjamin A. Brooks & Asta Miklius doi:10.1038/ngeo1612 Over the past decade, Kilauea and Mauna Loa—adjacent volcanoes in Hawai'i—have inflated and deflated in tandem, yet their shallow volcanic plumbing systems are separate. Numerical modelling of the volcanoes shows that dynamic stress transfer by asthenospheric pore pressure is a viable mechanism for volcano coupling in Hawai'i. |
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Article | Top |
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Intensification of Northern Hemisphere subtropical highs in a warming climate pp830 - 834 Wenhong Li, Laifang Li, Mingfang Ting & Yimin Liu doi:10.1038/ngeo1590 Subtropical high-pressure systems influence atmospheric circulation and global climate. Model simulations and reanalysis data suggest that summertime high pressure systems in the Northern Hemisphere subtropics will intensify as a result of climate change. See also: News and Views by Nakamura |
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