Kynan Hughson/Georgia Tech/NASA/MPS/DLR

Cryo-hydrologic processes have been active on Ceres

Latest Research

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    Phosphorus remobilized from seafloor sediments due to a reduced influx of iron-oxide from land led to widespread anoxia during the end-Permian mass extinction, according to palaeoredox and phosphorus speciation proxy records from Svalbard.

    • Martin Schobben
    • , William J. Foster
    • , Arve R. N. Sleveland
    • , Valentin Zuchuat
    • , Henrik H. Svensen
    • , Sverre Planke
    • , David P. G. Bond
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  • Article |

    Mounds within Ceres’s Occator crater may have formed by freezing of water-rich impact-induced melt, by a process analogous to that of pingo formation on Earth, according to an analysis of data from NASA’s Dawn mission.

    • B. E. Schmidt
    • , H. G. Sizemore
    • , K. H. G. Hughson
    • , K. D. Duarte
    • , V. N. Romero
    • , J. E. C. Scully
    • , P. M. Schenk
    • , D. L. Buczkowski
    • , D. A. Williams
    • , A. Nathues
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    • , J. C. Castillo-Rogez
    • , C. A. Raymond
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    In one earthquake, an oceanic transform fault ruptured in one direction and then backwards at a speed exceeding that of shear-wave propagation, according to an analysis of data recorded by nearby seafloor and global seismometers.

    • Stephen P. Hicks
    • , Ryo Okuwaki
    • , Andreas Steinberg
    • , Catherine A. Rychert
    • , Nicholas Harmon
    • , Rachel E. Abercrombie
    • , Petros Bogiatzis
    • , David Schlaphorst
    • , Jiri Zahradnik
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News & Comment

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    Soils store vast quantities of carbon and have the potential to help mitigate or exacerbate climate change. We need to better understand the interplay of chemical, physical and biological processes that govern soil carbon cycling and stability.

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    The Archaean atmosphere may have been well oxygenated, according to a reconsideration of sulfur cycling at that time. This challenges the view that sedimentary sulfur records oxygen-poor conditions during Earth’s first two billion years.

    • Desiree Roerdink
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    Organic carbon in the top metre of Earth’s soils is far older than previously thought, averaging 4,800 years old. These radiocarbon-derived age estimates require us to recalibrate our expectations of ecosystem gains and losses of carbon.

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    Nature Geoscience aims to publish important science, but the journal also strives to offer a platform to voices driving change within the geoscience community. We welcome submissions on community issues that encourage reader engagement and inspire action.

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    Compositional signatures of subducted crust in the deep-mantle sources of ocean island volcanoes in the Atlantic Ocean but not the Pacific reveal that plate motions on Earth’s surface influence the characteristics of Earth’s deepest interior.

    • Richard W. Carlson

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