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Content archived on 2024-05-15

Molybdenum, rhenium and osmium isotopes in banded iron formations as paleo-redox indicators for the ocean oxidation state in early proterozoic time.

Objective

Between 2300 to 1800 million years ago the Earth's oceans became toxic. Potential paleo-redox indicators will be identified in Proterozoic marine sediments, in order to study this important change that influenced climate and development of life on Earth.

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Coordinator

CENTRE NATIONAL DE LA RECHERCHE SCIENTIFIQUE
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Address
Rue Notre Dame des Pauvres 15
54501 VANDOEUVRE-LES-NANCY
France

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