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Laboratory Simulation of an Iron(II)-rich Precambrian Marine Upwelling System to Explore the Growth of Photosynthetic Bacteria
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Published on: July 24, 2016

Las condiciones ferruginosas dominaron más tarde la química de aguas profundas del neoproterozoico

Donald E Canfield1, Simon W Poulton, Andrew H Knoll

  • 1Nordic Center for Earth Evolution and Institute of Biology, Campusvej 55, University of Southern Denmark, 5230 Odense, Denmark. dec@biology.sdu.dk

Science (New York, N.Y.)
|July 19, 2008
PubMed
Resumen

Los océanos de la Era Neoproterozoica eran en gran parte anóxicos y ferruginosos, lo que indica un retorno a la química oceánica antigua. Esto sugiere que la oxigenación fue limitada durante este período crítico de la historia de la Tierra.

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