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2016/06/30

Nature Geoscience contents: July 2016 Volume 9 Number 7 pp471-560

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Nature Geoscience

TABLE OF CONTENTS

July 2016 Volume 9, Issue 7

Editorial
Commentary
News and Views
Review
Letters
Articles
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Editorial

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Subtle signals at sea   p471
doi:10.1038/ngeo2762
The ocean overturning circulation is potentially sensitive to climate change. In the north and south alike, human influence is less pronounced than we thought, but that is no reason to relax our watchfulness.

Commentary

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Cassini's Grand Finale   pp472 - 473
Scott G. Edgington & Linda J. Spilker
doi:10.1038/ngeo2753
After more than a decade exploring Saturn and its moons, the Cassini mission is in its closing act. Cassini's last year is an encore performance stuffed with science, including a final plunge into Saturn's atmosphere.

News and Views

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Atmospheric chemistry: The return of ethane   pp475 - 476
Hannele Hakola & Heidi Hellén
doi:10.1038/ngeo2736
Ethane emissions can lead to ozone pollution. Measurements at 49 sites show that long-declining atmospheric ethane concentrations started rising in 2010 in the Northern Hemisphere, largely due to greater oil and gas production in the USA.
See also: Letter by Helmig et al.

Planetary science: Salty Ceres   pp476 - 477
Mikhail Zolotov
doi:10.1038/ngeo2756
Anomalously bright spots are seen on the dark cratered surface of the dwarf planet Ceres. The Dawn spacecraft's detection of sodium carbonates in bright areas is consistent with aqueous activity in an ice-poor and salty regolith.
See also: Article by Bland et al.

Climate change: Carbon losses in the Alps   pp478 - 479
Guy Kirk
doi:10.1038/ngeo2747
Soil carbon stocks depend on inputs from decomposing vegetation and return to the atmosphere as CO2. Monitoring of carbon stocks in German alpine soils has shown large losses linked to climate change and a possible positive feedback loop.
See also: Article by Prietzel et al.

Ocean science: Vagaries of Atlantic overturning   pp479 - 480
Thomas W. N. Haine
doi:10.1038/ngeo2748
A weakening of the Atlantic meridional overturning circulation has emerged from noise after years of painstaking measurements. Three independent lines of evidence suggest that an anthropogenic influence on this overturning is not yet detectable.
See also: Letter by Böning et al. | Letter by Robson et al. | Letter by Jackson et al.

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Review

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Continent-sized anomalous zones with low seismic velocity at the base of Earth's mantle   pp481 - 489
Edward J. Garnero, Allen K. McNamara & Sang-Heon Shim
doi:10.1038/ngeo2733
Two large zones through which seismic waves travel unusually slowly are found at the base of Earth's mantle. These zones are thermally and chemically distinct from the surrounding mantle and may be a source for mantle plumes.

Letters

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Reversal of global atmospheric ethane and propane trends largely due to US oil and natural gas production   pp490 - 495
Detlev Helmig, Samuel Rossabi, Jacques Hueber, Pieter Tans, Stephen A. Montzka et al.
doi:10.1038/ngeo2721
Atmospheric non-methane hydrocarbon concentrations began declining in the 1970s. Surface and column measurements show that Northern Hemisphere ethane concentrations are now rising, probably due to North American oil and natural gas emissions.
See also: News and Views by Hakola & Hellén

Space-based detection of missing sulfur dioxide sources of global air pollution   pp496 - 500
Chris A. McLinden, Vitali Fioletov, Mark W. Shephard, Nick Krotkov, Can Li et al.
doi:10.1038/ngeo2724
Sulfur dioxide is a key air contaminant. A satellite-based emissions inventory reveals a number of hitherto unknown sources, with a cluster around the Persian Gulf, and identifies large discrepancies with conventional inventories in some regions.

Organic carbon decomposition rates controlled by water retention time across inland waters   pp501 - 504
Núria Catalán, Rafael Marcé, Dolly N. Kothawala & Lars. J. Tranvik
doi:10.1038/ngeo2720
Organic carbon decays as it travels through inland waters from soils to the sea. Analysis of data from across the continuum of inland and marine aquatic systems reveals that the rate of organic carbon decay depends on water retention time.

Partial decoupling of primary productivity from upwelling in the California Current system   pp505 - 508
Lionel Renault, Curtis Deutsch, James C. McWilliams, Hartmut Frenzel, Jun-Hong Liang et al.
doi:10.1038/ngeo2722
Eastern boundary coastal upwelling systems are locations of high ocean productivity. Numerical simulations reveal that wind alters current- and eddy-driven nutrient supply, which affects net primary productivity in the California Current system.

The North Atlantic Oscillation as a driver of rapid climate change in the Northern Hemisphere   pp509 - 512
Thomas L. Delworth, Fanrong Zeng, Gabriel A. Vecchi, Xiaosong Yang, Liping Zhang et al.
doi:10.1038/ngeo2738
The North Atlantic Oscillation has varied markedly on multidecadal timescales. Analyses of climate simulations show that these variations have contributed to Arctic sea ice loss, Northern Hemisphere warming and tropical storm activity.

A reversal of climatic trends in the North Atlantic since 2005   pp513 - 517
Jon Robson, Pablo Ortega & Rowan Sutton
doi:10.1038/ngeo2727
The mid-1990s' warming of the North Atlantic subpolar gyre was probably related to strengthened overturning. Observations and numerical models suggest that a climate reversal to a cooling trend occurred around 2005.
See also: News and Views by Haine

Recent slowing of Atlantic overturning circulation as a recovery from earlier strengthening   pp518 - 522
Laura C. Jackson, K. Andrew Peterson, Chris D. Roberts & Richard A. Wood
doi:10.1038/ngeo2715
The Atlantic meridional overturning circulation has weakened over the past decade. Examination of a global reanalysis that matches independent observations shows that the decline is consistent with recovery from an earlier invigoration.
See also: News and Views by Haine

Emerging impact of Greenland meltwater on deepwater formation in the North Atlantic Ocean   pp523 - 527
Claus W. Böning, Erik Behrens, Arne Biastoch, Klaus Getzlaff & Jonathan L. Bamber
doi:10.1038/ngeo2740
Freshwater release from melting polar ice could weaken the Atlantic overturning circulation. Eddy-resolving ocean simulations reveal that the freshening has not yet significantly affected meridional overturning, but an effect may emerge soon.
See also: News and Views by Haine

Oceanic transport of surface meltwater from the southern Greenland ice sheet   pp528 - 532
Hao Luo, Renato M. Castelao, Asa K. Rennermalm, Marco Tedesco, Annalisa Bracco et al.
doi:10.1038/ngeo2708
Meltwater runoff from the Greenland ice sheet alters ocean surface salinity. Numerical simulations show that meltwater from southeastern Greenland is transported to the Labrador Sea more efficiently than that from southwestern Greenland.

Himalayan strain reservoir inferred from limited afterslip following the Gorkha earthquake   pp533 - 537
David Mencin, Rebecca Bendick, Bishal Nath Upreti, Danda Pani Adhikari, Ananta Prasad Gajurel et al.
doi:10.1038/ngeo2734
Great Himalayan earthquakes are rare. Analysis of surface motions in the months after the 2015 Gorkha earthquake reveals negligible aseismic slip, implying that stress may be stored in the crust to be tapped during future great earthquakes.

Articles

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Composition and structure of the shallow subsurface of Ceres revealed by crater morphology   pp538 - 542
Michael T. Bland, Carol A. Raymond, Paul M. Schenk, Roger R. Fu, Thomas Kneissl et al.
doi:10.1038/ngeo2743
The dwarf planet Ceres is thought to have an ice-rich layer in its shallow subsurface. The morphologies of craters, however, suggest little relaxation by viscous flow has occurred and instead indicate a subsurface that is less than 40% ice.
See also: News and Views by Zolotov

Organic matter losses in German Alps forest soils since the 1970s most likely caused by warming   pp543 - 548
Jörg Prietzel, Lothar Zimmermann, Alfred Schubert & Dominik Christophel
doi:10.1038/ngeo2732
Soil carbon concentrations are sensitive to climate warming. Pairs of measurements of forest soil carbon stocks in the German Alps reveal that topsoil carbon concentrations declined as air temperatures rose between 1976 and 2011.
See also: News and Views by Kirk

Southern Ocean warming delayed by circumpolar upwelling and equatorward transport   pp549 - 554
Kyle C. Armour, John Marshall, Jeffery R. Scott, Aaron Donohoe & Emily R. Newsom
doi:10.1038/ngeo2731
Unlike the Arctic, the Southern Ocean has shown little warming. An analysis of observations and numerical simulations suggests that Southern Ocean warming patterns are shaped by meridional overturning more than surface heating.

Crustal-scale duplexing beneath the Yarlung Zangbo suture in the western Himalaya   pp555 - 560
Rui Gao, Zhanwu Lu, Simon L. Klemperer, Haiyan Wang, Shuwen Dong et al.
doi:10.1038/ngeo2730
The fate of the Indian plate during collision with Asia is debated. Seismic images of the western Himalaya reveal large-scale thrust faults that transfer Indian crust upwards, into the overriding Asian plate.

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