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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.

Fields of science (EuroSciVoc)

Topic(s)

Data not available

Call for proposal

Data not available

Funding Scheme

RGI - Research grants (individual fellowships)

Coordinator

CENTRE NATIONAL DE LA RECHERCHE SCIENTIFIQUE
EU contribution
No data
Address
Rue Notre Dame des Pauvres 15
54501 VANDOEUVRE-LES-NANCY
France
Total cost
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