TABLE OF CONTENTS
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January 2018 Volume 11, Issue 1 |
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| Editorial Comment News & Views Perspectives Review Articles Articles | |
Editorial | |
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A decade of Earth science p1 doi:10.1038/s41561-017-0052-x |
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Comment | |
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Exploring ocean worlds on Earth and beyond pp2 - 4 Kevin Peter Hand & Christopher R. German doi:10.1038/s41561-017-0045-9 |
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Atmospheric science looks to Venus pp4 - 5 Kevin McGouldrick doi:10.1038/s41561-017-0037-9 |
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News & Views | |
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Perspectives | |
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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. |
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Review Articles | |
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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. |
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Articles | |
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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. |
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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. |
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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. |
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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. |
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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. |
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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. |
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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. |
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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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