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      The tail of the Storegga Slide: insights from the geochemistry and sedimentology of the Norwegian Basin deposits : The tail of the Storegga Slide

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          Metabolic activity of subsurface life in deep-sea sediments.

          S D'Hondt (2002)
          Global maps of sulfate and methane in marine sediments reveal two provinces of subsurface metabolic activity: a sulfate-rich open-ocean province, and an ocean-margin province where sulfate is limited to shallow sediments. Methane is produced in both regions but is abundant only in sulfate-depleted sediments. Metabolic activity is greatest in narrow zones of sulfate-reducing methane oxidation along ocean margins. The metabolic rates of subseafloor life are orders of magnitude lower than those of life on Earth's surface. Most microorganisms in subseafloor sediments are either inactive or adapted for extraordinarily low metabolic activity.
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            The Origin and Distribution of Methane in Marine Sediments

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              Caught in the act: the 20 December 2001 gravity flow event in Monterey Canyon

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                Author and article information

                Journal
                Sedimentology
                Wiley-Blackwell
                00370746
                October 2010
                October 2010
                : 57
                : 6
                : 1409-1429
                Article
                10.1111/j.1365-3091.2010.01150.x
                d6cb64b7-6eb7-4d5d-812a-a6c44ba26af1
                © 2010

                http://doi.wiley.com/10.1002/tdm_license_1.1

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