A global transition to ferruginous conditions in the early Neoproterozoic oceans

Guilbaud, R.; Poulton, S.W.; Butterfield, N.J.; Zhu, M.; Shields-Zhou, G.

doi:10.1038/ngeo2434

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A global transition to ferruginous conditions in the early Neoproterozoic oceans

Guilbaud, R.; Poulton, S.W.; Butterfield, N.J.; Zhu, M.; Shields-Zhou, G. (2015). A global transition to ferruginous conditions in the early Neoproterozoic oceans. Nature Geoscience 8(6): 466–470. http://dx.doi.org/10.1038/ngeo2434

In: Nature Geoscience. Nature Publishing Group: London. ISSN 1752-0894; e-ISSN 1752-0908

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Guilbaud, R. Poulton, S.W. Butterfield, N.J.	Zhu, M. Shields-Zhou, G.

Abstract

Deeper ocean waters were anoxic during the Neoproterozoic. Geochemical data suggest a transition from sulphidic to iron-rich mid-depth waters about one billion years ago, coincident with increased iron influx from the supercontinent Rodinia.

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