Early Mars serpentinization-derived CH4 reservoirs, H2 -induced warming and paleopressure evolution

Author:

Chassefière E.1,Lasue J.23,Langlais B.4,Quesnel Y.5

Affiliation:

1. GEOPS; Univ. Paris-Sud; CNRS; Université Paris-Saclay; Rue du Belvédère Bât. 504-509 91405 Orsay France

2. Université de Toulouse; UPS-OMP; IRAP; Toulouse France

3. CNRS; IRAP; 9 Av. colonel Roche BP 44346 F-31028 Toulouse Cedex 4 France

4. LPG-CNRS & Université de Nantes; Nantes France

5. Aix-Marseille Université; CNRS; IRD; CEREGE UM34; Aix-en-Provence France

Funder

Institut National des Sciences de l'Univers

Centre National d’Etudes Spatiales

Centre National de la Recherche Scientifique

Publisher

Wiley

Subject

Space and Planetary Science,Geophysics

Reference69 articles.

1. Mariner 6 and 7 ultraviolet spectrometer experiment: Analysis of hydrogen Lyman-alpha data;Anderson;Journal of Geophysical Research,1971

2. Polar wander of Mars: Evidence from giant impact basins;Arkani-Hamed;Icarus,2009

3. Methane and related trace species on Mars: Origin, loss, implications for life, and habitability;Atreya;Planetary and Space Science,2006

4. The petrological expression of early Mars volcanism;Baratoux;Journal of Geophysical Research: Planets,2013

5. Testing the early Mars H2-CO2 greenhouse hypothesis with a 1-D photochemical model;Batalha;Icarus,2015

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