Tuesday, February 2, 2016

Nature Geoscience contents: February 2016 Volume 9 Number 2 pp85-180

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TABLE OF CONTENTS

February 2016 Volume 9, Issue 2

Editorial
Correspondence
Commentary
News and Views
Review
Letters
Articles
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Editorial

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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.

Correspondence

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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.

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.

Commentary

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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.

News and Views

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Groundwater: How much and how old?   pp93 - 94
Ying Fan
doi:10.1038/ngeo2609
A global picture of the age structure and flow path of groundwater is lacking. Tritium concentrations and numerical modelling shed light on both the most recently replenished and the longest stored groundwater within Earth's continents.
See also: Article by Gleeson et al.

Biogeochemistry: Better living through mercury   pp94 - 95
Jeffra K. Schaefer
doi:10.1038/ngeo2638
Mercury is a toxic element with no known biological function. Laboratory studies demonstrate that mercury can be beneficial to microbial growth by acting as an electron acceptor during photosynthesis.
See also: Letter by Grégoire & Poulain

Palaeoclimate: Aptian mystery solved   pp95 - 96
Heather M. Stoll
doi:10.1038/ngeo2634
The volcanic eruption that created the Ontong Java Plateau released large quantities of carbon dioxide. A reconstruction of CO2 concentrations suggests that the eruption promoted climate change and the expansion of ocean anoxia.
See also: Letter by Naafs et al.

Sustainability: Your feet's too big   pp97 - 98
James N. Galloway & Allison M. Leach
doi:10.1038/ngeo2647
Humanity's nitrogen pollution footprint has increased by a factor of six since the 1930s. A global analysis reveals that a quarter of this nitrogen pollution is associated with the production of internationally traded products.
See also: Letter by Oita et al.

Groundwater: India's drought below ground   p98
Tamara Goldin
doi:10.1038/ngeo2648

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Review

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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.

Letters

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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.

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

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.

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

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.

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.

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

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.

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.

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.

Articles

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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.

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

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.

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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