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dc.rights.licenseCopyright © 2021, Mary Ann Liebert, Inc.-
dc.contributor.authorRazzell Hollis, J.-
dc.contributor.authorFornaro, T.-
dc.contributor.authorRapin, W.-
dc.contributor.authorWade, J.-
dc.contributor.authorVicente Retortillo, Á.-
dc.contributor.authorSteele, A.-
dc.contributor.authorBhartia, R.-
dc.contributor.authorBeegle, W.-
dc.date.accessioned2022-02-15T14:13:06Z-
dc.date.available2022-02-15T14:13:06Z-
dc.date.issued2021-01-25-
dc.identifier.citationAstrobiology 21(5): 511-525(2021)es
dc.identifier.issn1531-1074-
dc.identifier.otherhttps://www.liebertpub.com/doi/abs/10.1089/ast.2020.2362-
dc.identifier.urihttp://hdl.handle.net/20.500.12666/575-
dc.description.abstractThe search for organic biosignatures on Mars will depend on finding material protected from the destructive ambient radiation. Solar ultraviolet can induce photochemical degradation of organic compounds, but certain clays have been shown to preserve organic material. We examine how the SHERLOC instrument on the upcoming Mars 2020 mission will use deep-ultraviolet (UV) (248.6 nm) Raman and fluorescence spectroscopy to detect a plausible biosignature of adenosine 5′-monophosphate (AMP) adsorbed onto Ca-montmorillonite clay. We found that the spectral signature of AMP is not altered by adsorption in the clay matrix but does change with prolonged exposure to the UV laser over dosages equivalent to 0.2–6 sols of ambient martian UV. For pure AMP, UV exposure leads to breaking of the aromatic adenine unit, but in the presence of clay the degradation is limited to minor alteration with new Raman peaks and increased fluorescence consistent with formation of 2-hydroxyadenosine, while 1 wt % Mg perchlorate increases the rate of degradation. Our results confirm that clays are effective preservers of organic material and should be considered high-value targets, but that pristine biosignatures may be altered within 1 sol of martian UV exposure, with implications for Mars 2020 science operations and sample caching.es
dc.description.sponsorshipThis work was funded by a NASA Postdoctoral Program Fellowship awarded to Joseph Razzell Hollis, administered by the Universities Space Research Association on behalf of NASA, and Teresa Fornaro was supported by the Geophysical Laboratory of the Carnegie Institution of Washington and the Italian Space Agency (ASI) grant agreement ExoMars number 2017-48-H.0. William Rapin was funded by an MSL-Curiosity Participating Scientist grant to Bethany Ehlmann. (c) 2019California Institute of Technology; government sponsorship acknowledged.es
dc.language.isoenges
dc.publisherMary Ann Liebert Publisherses
dc.subjectDeep UV spectroscopyes
dc.subjectMarses
dc.subjectBiosignature detectiones
dc.subjectPhotochemical degradationes
dc.subjectMars 2020es
dc.titleDetection and Degradation of Adenosine Monophosphate in Perchlorate-Spiked Martian Regolith Analog, by Deep-Ultraviolet Spectroscopyes
dc.typeinfo:eu-repo/semantics/articlees
dc.identifier.doi10.1089/ast.2020.2362-
dc.identifier.e-issn1557-8070-
dc.contributor.funderAgenzia Spaziale Italiana (ASI)-
dc.description.peerreviewedPeerreviewes
dc.identifier.funderhttp://dx.doi.org/10.13039/501100003981-
dc.type.hasVersioninfo:eu-repo/semantics/publishedVersion-
dc.rights.accessRightsinfo:eu-repo/semantics/restrictedAccess-
dc.identifier.pmid33493410-
dc.type.coarhttp://purl.org/coar/resource_type/c_2df8fbb1-
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