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Updated: Jun 10, 2026

Metal-silicate Partitioning at High Pressure and Temperature: Experimental Methods and a Protocol to Suppress Highly Siderophile Element Inclusions
11:50

Metal-silicate Partitioning at High Pressure and Temperature: Experimental Methods and a Protocol to Suppress Highly Siderophile Element Inclusions

Published on: June 13, 2015

Las restricciones de isótopos de hierro en el estado redox del océano arqueo y paleoproterozoico

Olivier J Rouxel1, Andrey Bekker, Katrina J Edwards

  • 1Marine Chemistry and Geochemistry Department, Geomicrobiology Group, Woods Hole Oceanographic Institution, Mail Stop 8, Woods Hole, MA 02543, USA. orouxel@whoi.edu

Science (New York, N.Y.)
|February 19, 2005
PubMed
Resumen

El estado redox del océano cambió con el aumento del oxígeno atmosférico hace 2.300 millones de años. Los datos de isótopos de hierro revelan cambios en el ciclo del hierro oceánico, lo que indica un aumento de la precipitación de sulfuro de hierro en un océano estratificado.

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