Wednesday, January 3, 2018

Nature Geoscience contents: January 2018 Volume 11 Number 1

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Nature Geoscience
TABLE OF CONTENTS

January 2018 Volume 11, Issue 1

Editorial
Comment
News & Views
Perspectives
Review Articles
Articles
 

Editorial

 

A decade of Earth science    p1
doi:10.1038/s41561-017-0052-x

Comment

 

Exploring ocean worlds on Earth and beyond    pp2 - 4
Kevin Peter Hand & Christopher R. German
doi:10.1038/s41561-017-0045-9

Atmospheric science looks to Venus    pp4 - 5
Kevin McGouldrick
doi:10.1038/s41561-017-0037-9

News & Views

 

Methane multiplication    pp6 - 7
Thomas A. Laakso
doi:10.1038/s41561-017-0043-y

Intra-plate volcanism    p8
James Tuttle Keane
doi:10.1038/s41561-017-0048-6

From orogenies to oxygen    pp9 - 10
Noah Planavsky
doi:10.1038/s41561-017-0040-1

Hydrothermal stamp on the oceans    pp10 - 12
Susan Q. Lang
doi:10.1038/s41561-017-0044-x

Slow warming and the ocean see-saw    pp12 - 13
Yu Kosaka
doi:10.1038/s41561-017-0038-8

Mantle signatures in the surface    p14
Amy Whitchurch
doi:10.1038/s41561-017-0050-z

New directions for ocean nutrients    pp15 - 16
Tim DeVries
doi:10.1038/s41561-017-0042-z

Telltale tungsten and the Moon    pp16 - 18
Kaveh Pahlevan
doi:10.1038/s41561-017-0047-7

Regional climate goes global    pp18 - 19
Helen McGregor
doi:10.1038/s41561-017-0046-8

Tropical interchange    p20
Alicia Newton
doi:10.1038/s41561-017-0049-5

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Perspectives

 

The Martian subsurface as a potential window into the origin of life    pp21 - 26
Joseph R. Michalski, Tullis C. Onstott, Stephen J. Mojzsis, John Mustard, Queenie H. S. Chan et al.
doi:10.1038/s41561-017-0015-2

Ancient hydrothermal deposits formed in the Martian subsurface may be the best targets for finding evidence for ancient life on Mars, and clues about the origin of life on Earth.

 

Review Articles

 

Influence of diatom diversity on the ocean biological carbon pump    pp27 - 37
Paul Tréguer, Chris Bowler, Brivaela Moriceau, Stephanie Dutkiewicz, Marion Gehlen et al.
doi:10.1038/s41561-017-0028-x

Size, morphology, silica content and life cycle of diatoms affect their contribution to the export of carbon to the deep ocean, suggests a literature review.

 

Articles

 

Southward shift of the global wind energy resource under high carbon dioxide emissions    pp38 - 43
Kristopher B. Karnauskas, Julie K. Lundquist & Lei Zhang
doi:10.1038/s41561-017-0029-9

Wind power for energy generation is projected to decrease in northern mid-latitudes and increase in the tropics and Southern Hemisphere, suggests an analysis of climate model simulations utilizing an industry wind turbine power curve.

 

Substantial large-scale feedbacks between natural aerosols and climate    pp44 - 48
C. E. Scott, S. R. Arnold, S. A. Monks, A. Asmi, P. Paasonen et al.
doi:10.1038/s41561-017-0020-5

Extratropical feedbacks between climate and aerosols from landscape fire and biogenic secondary organic aerosols are significant, according to a global aerosol model that is constrained by observations.

 

Subsurface iceberg melt key to Greenland fjord freshwater budget    pp49 - 54
T. Moon, D. A. Sutherland, D. Carroll, D. Felikson, L. Kehrl et al.
doi:10.1038/s41561-017-0018-z

Iceberg melt is the largest annual freshwater source in a south Greenland fjord, with release largely below 20 m depth, according to iceberg-model simulations. Furthermore, iceberg melt peaks later in the year than other sources of freshwater.

 

Effects of primitive photosynthesis on Earth's early climate system    pp55 - 59
Kazumi Ozaki, Eiichi Tajika, Peng K. Hong, Yusuke Nakagawa & Christopher T. Reinhard
doi:10.1038/s41561-017-0031-2

Amplification of the methane cycle by anyoxygenic photosynthesis could have warmed early Earth and countered the faint young Sun, geochemical modelling suggests. A combination of H2-based and Fe2+-based photosynthesis acts to enhance methane fluxes.

 

Creeping subduction zones are weaker than locked subduction zones    pp60 - 64
Jeanne L. Hardebeck & John P. Loveless
doi:10.1038/s41561-017-0032-1

The faults in creeping segments of subduction zones are weaker than those in locked segments, according to analyses of stress orientations and GPS data from subduction zones globally.

 

Water-rich sublithospheric melt channel in the equatorial Atlantic Ocean    pp65 - 69
Fares Mehouachi & Satish C. Singh
doi:10.1038/s41561-017-0034-z

A water-rich layer of partial melt marks the base of the lithosphere in the equatorial Atlantic Ocean, according to analyses of seismic data.

 

Western US volcanism due to intruding oceanic mantle driven by ancient Farallon slabs    pp70 - 76
Quan Zhou, Lijun Liu & Jiashun Hu
doi:10.1038/s41561-017-0035-y

Volcanism in the western US may result from warm oceanic mantle beneath the Pacific Ocean being drawn eastwards by mantle flow induced by the sinking of Farallon slabs, according to numerical model simulations.

 

Heterogeneous delivery of silicate and metal to the Earth by large planetesimals    pp77 - 81
S. Marchi, R. M. Canup & R. J. Walker
doi:10.1038/s41561-017-0022-3

Collisions of large differentiated impactors during the late stages of Earth's accretion may have heterogeneously mixed projectile material into the Earth, explaining observed chemical and isotopic heterogeneities in mantle materials.

 

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