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Nature Geoscience Focus on Groundwater
In this focus, we present a collection of research papers and opinion pieces that discuss the influence of groundwater on hydrological, environmental and geological processes.
Read the article, The global volume and distribution of modern groundwater, free to registered users until the 2 March 2016. | | |
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TABLE OF CONTENTS
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February 2016 Volume 9, Issue 2 |
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| Editorial Correspondence Commentary News and Views Review Letters Articles | |
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Editorial | Top |
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Groundwater exposed p85 doi:10.1038/ngeo2655 Groundwater flow meddles with hydrological, environmental and geological processes. As water scarcity issues mount for people living above ground, the vast stores of freshwater in the subsurface require research attention. |
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Correspondence | Top |
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Integrity of lunar soil samples p87 Lawrence A. Taylor, Yang Liu & Gary Lofgren doi:10.1038/ngeo2637 See also: Correspondence by Cooper et al. |
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Reply to 'Integrity of lunar soil samples' p87 B. L. Cooper, K. Thaisen, B. C. Chang, T. S. Lee & D. S. McKay doi:10.1038/ngeo2645 See also: Correspondence by Taylor et al. |
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Commentary | Top |
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Drought in the Anthropocene pp89 - 91 Anne F. Van Loon, Tom Gleeson, Julian Clark, Albert I. J. M. Van Dijk, Kerstin Stahl et al. doi:10.1038/ngeo2646 Drought management is inefficient because feedbacks between drought and people are not fully understood. In this human-influenced era, we need to rethink the concept of drought to include the human role in mitigating and enhancing drought. |
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News and Views | Top |
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Review | Top |
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Climate-sensitive northern lakes and ponds are critical components of methane release pp99 - 105 Martin Wik, Ruth K. Varner, Katey Walter Anthony, Sally MacIntyre & David Bastviken doi:10.1038/ngeo2578 Lakes are sources of the greenhouse gas methane. A synthesis of measurements of methane emissions reveals that lakes and ponds above 50 °N emit 16.5 Tg methane annually, and emissions may increase by 20 to 50% with longer ice-free seasons. |
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Letters | Top |
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Amplification of El Niño by cloud longwave coupling to atmospheric circulation pp106 - 110 Gaby Rädel, Thorsten Mauritsen, Bjorn Stevens, Dietmar Dommenget, Daniela Matei et al. doi:10.1038/ngeo2630 The El Niño/Southern Oscillation (ENSO) affects weather patterns worldwide. Numerical experiments with an Earth system model suggest that cloud feedbacks act to amplify ENSO variability by a factor of two or more. |
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Substantial nitrogen pollution embedded in international trade pp111 - 115 Azusa Oita, Arunima Malik, Keiichiro Kanemoto, Arne Geschke, Shota Nishijima et al. doi:10.1038/ngeo2635 Anthropogenic emissions of reactive nitrogen have had severe environmental impacts. An analysis of reactive nitrogen emissions from the production, consumption and transport of commodities attributes roughly a quarter to international trade. See also: News and Views by Galloway & Leach |
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Nitrous oxide sinks and emissions in boreal aquatic networks in Québec pp116 - 120 C. Soued, P. A. del Giorgio & R. Maranger doi:10.1038/ngeo2611 Aquatic ecosystems are important sources of the greenhouse gas nitrous oxide. Measurements of nitrous oxide concentrations from 321 rivers, lakes and ponds in Canada reveal that some boreal aquatic systems can act as net nitrous oxide sinks. |
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A physiological role for HgII during phototrophic growth pp121 - 125 D. S. Grégoire & A. J. Poulain doi:10.1038/ngeo2629 Bacteria have been shown to be involved in the reduction of HgII to elemental mercury. Laboratory experiments with HgII and different carbon sources reveal that purple bacteria can use HgII as an electron acceptor, promoting bacterial growth. See also: News and Views by Schaefer |
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Substantial proportion of global streamflow less than three months old pp126 - 129 Scott Jasechko, James W. Kirchner, Jeffrey M. Welker & Jeffrey J. McDonnell doi:10.1038/ngeo2636 Streamflow is a mixture of precipitation of various ages. Oxygen isotope data suggests that a third of global river discharge is sourced from rainfall within the past few months, which accounts for less than 0.1% of global groundwater. |
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Sea-level constraints on the amplitude and source distribution of Meltwater Pulse 1A pp130 - 134 Jean Liu, Glenn A. Milne, Robert E. Kopp, Peter U. Clark & Ian Shennan doi:10.1038/ngeo2616 Sea level rose rapidly during Meltwater Pulse 1A, about 14,500 years ago. A reassessment of sea-level rise and isostatic adjustment suggests sea level rose roughly 8 to 15 m in total, with 0 to 10 m derived from the Antarctic ice sheets. |
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Gradual and sustained carbon dioxide release during Aptian Oceanic Anoxic Event 1a pp135 - 139 B. D. A. Naafs, J. M. Castro, G. A. De Gea, M. L. Quijano, D. N. Schmidt et al. doi:10.1038/ngeo2627 A period of ocean anoxia about 120 million years ago coincided with high temperatures. A reconstruction of CO2 concentrations shows that volcanic outgassing from the Ontong Java Plateau caused CO2 levels to double during the anoxic event. See also: News and Views by Stoll |
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Rapid biological speciation driven by tectonic evolution in New Zealand pp140 - 144 Dave Craw, Phaedra Upton, Christopher P. Burridge, Graham P. Wallis & Jonathan M. Waters doi:10.1038/ngeo2618 Plate tectonic motions can influence biological systems. Numerical modelling of the topographic evolution of New Zealand, combined with fish phylogenetic analyses suggest mountain growth directly influenced biological diversification. |
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Massive and prolonged deep carbon emissions associated with continental rifting pp145 - 149 Hyunwoo Lee, James D. Muirhead, Tobias P. Fischer, Cynthia J. Ebinger, Simon A. Kattenhorn et al. doi:10.1038/ngeo2622 Transfer of CO2 from Earth's interior to the atmosphere happens largely by volcanic degassing. Measurements of CO2 emissions from faults in the East African Rift system imply that tectonic degassing is also important for deep carbon release. |
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A mixed seismic–aseismic stress release episode in the Andean subduction zone pp150 - 154 J. C. Villegas-Lanza, J.-M. Nocquet, F. Rolandone, M. Vallée, H. Tavera et al. doi:10.1038/ngeo2620 Subduction zone earthquakes can be followed by aseismic slip. Analysis of fault slip in northern Peru reveals transient aseismic slip that lasted for seven months and released more than 1,000% of the energy expelled by the quake that preceded it. |
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Articles | Top |
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Degree of simulated suppression of Atlantic tropical cyclones modulated by flavour of El Niño pp155 - 160 Christina M. Patricola, Ping Chang and R. Saravanan doi:10.1038/ngeo2624 El Niño events tend to suppress Atlantic hurricane activity. Simulations with high-resolution climate models show that the efficiency of this suppression mechanism varies with the flavour of the El Niño event. |
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The global volume and distribution of modern groundwater pp161 - 167 Tom Gleeson, Kevin M. Befus, Scott Jasechko, Elco Luijendijk & M. Bayani Cardenas doi:10.1038/ngeo2590 Groundwater recharged less than 50 years ago is vulnerable to contamination and land-use changes. Data and simulations suggest that up to 6% of continental groundwater is modern—forming the largest component of the active hydrologic cycle. See also: News and Views by Fan |
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Links between tropical Pacific seasonal, interannual and orbital variability during the Holocene pp168 - 173 J. Emile-Geay, K. M. Cobb, M. Carré, P. Braconnot, J. Leloup et al. doi:10.1038/ngeo2608 The frequency and amplitude of the El Niño/Southern Oscillation varied during the Holocene. A comparison of proxy records and model simulations suggests that any link between orbital forcing and this variability is either complex or non-existent. |
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Himalayan megathrust geometry and relation to topography revealed by the Gorkha earthquake pp174 - 180 J. R. Elliott, R. Jolivet, P. J. González, J.-P. Avouac, J. Hollingsworth et al. doi:10.1038/ngeo2623 How Himalayan topography is built is unclear. Analysis of surface displacement during the 2015 Gorkha earthquake suggests that large earthquakes may lower the high Himalayan mountains, and topography may grow during the interseismic phase. |
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