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Strong Depletion Of 13C in CO Induced By Photolysis Of CO2 In The Martian Atmosphere Calculated By A Photochemical Model – Astrobiology

Strong Depletion Of 13C in CO Induced By Photolysis Of CO2 In The Martian Atmosphere Calculated By A Photochemical Model – Astrobiology

Strong Depletion Of 13C in CO Induced By Photolysis Of CO2 In The Martian Atmosphere Calculated By A Photochemical Model – Astrobiology

Welcome to the Astrobiology Web,The isotopic signature of atmospheric carbon offers a unique tracer for the history of the Martian atmosphere and the origin of organic matter on Mars.,The isotopic signature of atmospheric carbon offers a unique tracer for the history of the Martian atmosphere and the origin of organic matter on Mars.

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