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    Amino acid photostability on the Martian surface

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    Author
    ten Kate, I. L.
    Garry, J. R. C.
    Peeters, Z.
    Quinn, R.
    Foing, B.
    Ehrenfreund, P.
    Issue Date
    2005-01-01
    Keywords
    Radiation
    organic matter
    Martian crust
    amino acids
    
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    Citation
    ten Kate, I. L., Garry, J. R., Peeters, Z., Quinn, R., Foing, B., & Ehrenfreund, P. (2005). Amino acid photostability on the Martian surface. Meteoritics & Planetary Science, 40(8), 1185-1193.
    Publisher
    The Meteoritical Society
    Journal
    Meteoritics & Planetary Science
    URI
    http://hdl.handle.net/10150/656031
    DOI
    10.1111/j.1945-5100.2005.tb00183.x
    Additional Links
    https://meteoritical.org/
    Abstract
    In the framework of international planetary exploration programs, several space missions are planned to search for organics and bio-signatures on Mars. Previous attempts have not detected any organic compounds in the Martian regolith. It is therefore critical to investigate the processes that may affect organic molecules on and below the planets surface. Laboratory simulations can provide useful data about the reaction pathways of organic material at Mars surface. We have studied the stability of amino acid thin films against ultraviolet (UV) irradiation and use those data to predict the survival time of these compounds on and in the Martian regolith. We show that thin films of glycine and D-alanine are expected to have half-lives of 22 +/- 5 hr and of 3 +/- 1 hr, respectively, when irradiated with Mars-like UV flux levels. Modelling shows that the half-lives of the amino acids are extended to the order of 10^7 years when embedded in regolith. These data suggest that subsurface sampling must be a key component of future missions to Mars dedicated to organic detection.
    Type
    Article
    text
    Language
    en
    ISSN
    1945-5100
    ae974a485f413a2113503eed53cd6c53
    10.1111/j.1945-5100.2005.tb00183.x
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    Meteoritics & Planetary Science, Volume 40, Number 8 (2005)

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