Wednesday, November 2, 2016

Nature Geoscience contents: November 2016 Volume 9 Number 11 pp797-853

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Nature Geoscience

TABLE OF CONTENTS

November 2016 Volume 9, Issue 11

Editorial
Commentary
News and Views
Letters
Articles
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Editorial

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Of rocks and social justice   p797
doi:10.1038/ngeo2836
Despite much emphasis on diversity in the US, geoscience remains one of the least diverse scientific disciplines. If we want to achieve and maintain diversity, we need to make our work environments welcoming to a broad spectrum of voices.

Commentary

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Pathways to zero emissions   pp799 - 801
Jeffrey D. Sachs, Guido Schmidt-Traub & Jim Williams
doi:10.1038/ngeo2826
To keep global warming below 2 °C, countries need long-term strategies for low-emission development. Without these, immediate emissions reductions may lock-in high-emitting infrastructure, hamper collaboration and make climate goals unachievable.

News and Views

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Palaeoclimate: CO2 and late Palaeozoic glaciation   pp803 - 804
Timothy S. Myers
doi:10.1038/ngeo2832
Large glacial–interglacial fluctuations occurred during the late Palaeozoic. Geochemical and fossil data show these cycles were marked by coincident shifts in the carbon cycle and terrestrial biosphere.
See also: Letter by Montañez et al.

Ocean acidification: Emergence from pre-industrial conditions   p804
Eithne Tynan
doi:10.1038/ngeo2834

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Letters

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Gender differences in recommendation letters for postdoctoral fellowships in geoscience   pp805 - 808
Kuheli Dutt, Danielle L. Pfaff, Ariel F. Bernstein, Joseph S. Dillard & Caryn J. Block
doi:10.1038/ngeo2819
Gender disparities in science are well documented. An analysis of 1,224 recommendation letters from 54 countries for geoscience postdoctoral fellowships reveals that women are half as likely to receive an excellent letter as men.

Skilful predictions of the winter North Atlantic Oscillation one year ahead   pp809 - 814
Nick Dunstone et al.
doi:10.1038/ngeo2824
The North Atlantic Oscillation profoundly influences European and North American winter weather. Dynamical model predictions now exhibit skill in prediction of the winter North Atlantic Oscillation more than one year in advance.

Nutrient budgets in the subtropical ocean gyres dominated by lateral transport   pp815 - 819
Robert T. Letscher, François Primeau & J. Keith Moore
doi:10.1038/ngeo2812
Upward fluxes have been thought to dominate nutrient replenishment at the ocean surface. A numerical model reveals that lateral transfer is an important source of phosphorus and nitrogen for all five subtropical gyres.

Substantial energy input to the mesopelagic ecosystem from the seasonal mixed-layer pump   pp820 - 823
Giorgio Dall'Olmo, James Dingle, Luca Polimene, Robert J. W. Brewin & Hervé Claustre
doi:10.1038/ngeo2818
Life at ocean depths below ∼100 m requires organic carbon from the upper ocean. Analyses of satellite and Argo-float data reveal that seasonal changes in mixed-layer depth supply substantial amounts of carbon to this deep and dark ecosystem.

Climate, pCO2 and terrestrial carbon cycle linkages during late Palaeozoic glacial–interglacial cycles   pp824 - 828
Isabel P. Montañez et al.
doi:10.1038/ngeo2822
The late Palaeozoic was marked by a series of glacial-interglacial cycles. Geochemical and fossil data suggest a role for terrestrial vegetation–carbon cycle feedbacks in the climate response to orbital forcing.
See also: News and Views by Myers

Triggering of the 2014 M w7.3 Papanoa earthquake by a slow slip event in Guerrero, Mexico   pp829 - 833
M. Radiguet et al.
doi:10.1038/ngeo2817
Links between subduction zone earthquakes and slow slip on the plate interface are unclear. Reconstructions of a slow slip event in the Guerrero subduction zone segment, in Mexico, suggest that the event triggered the 2014 Papanoa earthquake.

Earthquake potential revealed by tidal influence on earthquake size–frequency statistics   pp834 - 837
Satoshi Ide, Suguru Yabe & Yoshiyuki Tanaka
doi:10.1038/ngeo2796
Tidal triggering of earthquakes is debated. Analysis of global earthquake catalogue data compared with tidal stress histories suggests that the probability of a large earthquake is greater during times of maximum tidal stress amplitude.

Articles

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Twenty-five winters of unexpected Eurasian cooling unlikely due to Arctic sea-ice loss   pp838 - 842
Kelly E. McCusker, John C. Fyfe & Michael Sigmond
doi:10.1038/ngeo2820
Winter cooling over Eurasia has been suggested to be linked to Arctic sea-ice loss. Climate model simulations reveal no evidence for such a link and instead suggest that a persistent atmospheric circulation pattern is responsible.

Late Miocene global cooling and the rise of modern ecosystems   pp843 - 847
Timothy D. Herbert et al.
doi:10.1038/ngeo2813
A period of continental aridification and ecosystem change occurred about seven million years ago. A global sea surface temperature reconstruction identifies cooling temperatures and a strengthened meridional temperature gradient at this time.

Large-scale subduction of continental crust implied by India-Asia mass-balance calculation   pp848 - 853
Miquela Ingalls, David B. Rowley, Brian Currie & Albert S. Colman
doi:10.1038/ngeo2806
Buoyant continental crust is thought to resist subduction. Calculation of the crustal mass balance during the collision between India and Eurasia indicates that about 50% of pre-collisional continental crust has been subducted into the mantle.

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