The Imprint of Atmospheric Evolution in the D/H of Hesperian Clay Minerals on Mars
作者： PR Mahaffy , CR Webster , JC Stern , AE Brunner , SK Atreya
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摘要: The deuterium to hydrogen (D/H) ratio in strongly bound water or hydroxyl groups ancient martian clays retains the imprint of formation these minerals. Curiosity’s Sample Analysis at Mars (SAM) experiment measured thermally evolved and gas released between 550°C 950°C from samples Hesperian era Gale crater smectite determine this isotope ratio. D/H value is 3.0 (±0.2) times Standard Mean Ocean Water (SMOW). ~3 billion year old mudstone that half present atmosphere but substantially higher than expected very early indicates an extended history escape desiccation planet.
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