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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. hdl.handle.net/10.1038/ngeo2434
In: Nature Geoscience. Nature Publishing Group: London. ISSN 1752-0894, more
Peer reviewed article  

Available in Authors 

Keyword
    Marine

Authors  Top 
  • 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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