Redox state of Earth’s magma ocean and its Venus-like early atmosphere-Reference-Cited by-同舟云学术

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Redox state of Earth’s magma ocean and its Venus-like early atmosphere

Published:2020-11-27 Issue:48 Volume:6 Page:
ISSN:2375-2548
Container-title:Science Advances
language:en
Short-container-title:Sci. Adv.

Author:

Sossi Paolo A.¹²^ORCID,Burnham Antony D.³^ORCID,Badro James²,Lanzirotti Antonio⁴^ORCID,Newville Matt⁴^ORCID,O’Neill Hugh St.C.³^ORCID

Affiliation:

1. Institute of Geochemistry and Petrology, ETH Zürich, Sonneggstrasse 5, CH-8092 Zürich, Switzerland.

2. Université de Paris, Institut de Physique du Globe de Paris, CNRS, 75005 Paris, France.

3. Research School of Earth Sciences, Australian National University, 61 Mills Rd, 2601 Canberra, Australia.

4. Center for Advanced Radiation Sources, University of Chicago, Chicago, IL 60637, USA.

Abstract

Oxidation state of iron in Earth’s magma ocean indicates it would have produced a Venus-like early atmosphere upon cooling.

Funder

Australian Research Council

Schweizerischer Nationalfonds

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

Reference100 articles.

1. Atmospheric Evolution of the Terrestrial Planets

2. Origin and evolution of the atmospheres of early Venus, Earth and Mars

3. Building Terrestrial Planets

4. The origins and concentrations of water, carbon, nitrogen and noble gases on Earth

5. Volatile accretion history of the terrestrial planets and dynamic implications

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