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  • Testing Raman spectroscopy for the trace analysis of biomarkers for Mars exobiological studies

    Paper number

    IAC-10.A1.5.8

    Author

    Prof. Jan Jehlicka, Charles University, Czech Republic

    Coauthor

    Prof. Howell G.M. Edwards, United Kingdom

    Coauthor

    Mr. Petr Vitek, Czech Republic

    Coauthor

    Mr. Adam Culka, Czech Republic

    Year

    2010

    Abstract
    Within the future  payloads designed by ESA and NASA for several  missions focussing on life detection on Mars, Raman spectroscopy has been proposed as an important non-destructive analytical tool for the in-situ identification of biomarkers on planetary and moon surfaces or near sub-surfaces. Raman spectroscopy is an ideal technique for the identification of biomolecules and minerals for astrobiological applications. Raman spectroscopic instrumentation  has been shown to be  potentially valuable for the  in-situ detection of spectral biomarkers originating from rock samples containing remnants of terrestrial endolithic colonisation. A potential limitation for the use of Raman spectroscopic techniques is the detection  of trace amounts of biomolecules in rock matrices. 
    
    Portable Raman systems equipped with  785 nm lasers permit the detection of pure organic minerals, aminoacids, carboxylic acids, as well as NH-containing compounds outdoors at –20°C and at an altitude of 3300 m. The detection of  beta-carotene and  aminoacids has been achieved in the field using a portable Raman system in admixture with  crystalline powders of sulphates and halite. 
    
    Laboratory systems (514.5 nm laser excitation) permit the  detection of these  biomolecules at even  lower concentrations  at sub-ppm level of the order of 0.1 to 1 mg kg-1. The comparative evaluation of laboratory versus field measurements permits the identification of critical issues for future field applications and directs attention to the improvements needed  in the instrumentation. A comparison between systems using different laser excitation wavelengths shows excellent results especially for 785 nm laser excitation. The results of this study will inform the acquisition parameters  necessary for the deployment of robotic miniaturised Raman spectrosocpic instrumentation intended for the detection of spectral signatures of extant or relict life on Mars. With respect to the “habitability potential” of evaporitic rocks found on Mars, we can assume that if beta-carotene could have been synthesized by potential Martian biota it could then have been subsequently preserved in subsurface evaporites in detectable amounts for Raman spectroscopic analysis equipped with a 785 or 514.5 nm laser excitation.
    Abstract document

    IAC-10.A1.5.8.brief.pdf

    Manuscript document

    (absent)