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      Mo-total organic carbon covariation in modern anoxic marine environments: Implications for analysis of paleoredox and paleohydrographic conditions : MO-TOC COVARIATION IN ANOXIC SEDIMENTS

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      Paleoceanography

      American Geophysical Union (AGU)

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          Proterozoic ocean chemistry and evolution: a bioinorganic bridge?

          Recent data imply that for much of the Proterozoic Eon (2500 to 543 million years ago), Earth's oceans were moderately oxic at the surface and sulfidic at depth. Under these conditions, biologically important trace metals would have been scarce in most marine environments, potentially restricting the nitrogen cycle, affecting primary productivity, and limiting the ecological distribution of eukaryotic algae. Oceanic redox conditions and their bioinorganic consequences may thus help to explain observed patterns of Proterozoic evolution.
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            The geochemistry of redox sensitive trace metals in sediments

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              Rhenium and molybdenum enrichments in sediments as indicators of oxic, suboxic and sulfidic conditions of deposition

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                Author and article information

                Journal
                Paleoceanography
                Paleoceanography
                American Geophysical Union (AGU)
                08838305
                March 2006
                March 2006
                : 21
                : 1
                : n/a
                Article
                10.1029/2004PA001112
                © 2006
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