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Updated: Jul 6, 2026

Laboratory Simulation of an Iron(II)-rich Precambrian Marine Upwelling System to Explore the Growth of Photosynthetic Bacteria
09:45

Laboratory Simulation of an Iron(II)-rich Precambrian Marine Upwelling System to Explore the Growth of Photosynthetic Bacteria

Published on: July 24, 2016

Comentario sobre "Las restricciones de isótopos de hierro en el estado redox del océano arcaico y paleoproterozoico"

Kosei E Yamaguchi1, Hiroshi Ohmoto

  • 1Institute for Research on Earth Evolution (IFREE), Japan, Agency for Marine-Earth Science and Technology (JAMSTEC),2-15 Natsushima, Yokosuka 237-0061, Japan. kosei@jamstec.go.jp

Science (New York, N.Y.)
|January 18, 2006
PubMed
Resumen

Los isótopos de hierro en los sulfuros sedimentarios pueden no reflejar con precisión la antigua oxidación atmosférica. La mala interpretación del origen de estos minerales desafía las conclusiones anteriores sobre la Tierra.

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