Biology
Scientific paper
Dec 2009
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2009agufm.p43c1451t&link_type=abstract
American Geophysical Union, Fall Meeting 2009, abstract #P43C-1451
Biology
[1060] Geochemistry / Planetary Geochemistry, [1094] Geochemistry / Instruments And Techniques, [5200] Planetary Sciences: Astrobiology, [5494] Planetary Sciences: Solid Surface Planets / Instruments And Techniques
Scientific paper
A range of clays have been detected on the surface of Mars lending support to the presence of an early water-rich epoch dramatically different than the planet’s current environment. The potential preservation of ancient chemical habitability signatures in clays could drive future missions such as NASA’s Mid-Range Rover to such “phyllosilicate regions”. Various laboratory studies have focused on the incorporation and preservation of organic material, such as amino acids, nucleobases, and more complex biomarkers, in terrestrial clays. Laser-based time-of-flight mass spectrometry (TOF-MS) may be one technique capable of conducting such analyses in situ without extensive sample preparation. We are testing the capabilities of a miniature TOF-MS to analyze clay minerals and any associated organic molecules. We have recorded baseline mass spectra of terrestrial source clays SWy-2 (Na-Montmorillonite), KGa-1b (Kaolinite), and SAz-2 (Ca-Montmorillonite) obtained via the Source Clays Project of the Clay Minerals Society. Here we will present the first results of our measurements of the selected clays in their natural state, as well as spiked with an amino acids standard. The focus of this presentation will be both on the absorption of the amino acids as well an on the detection capability of the TOF-MS instrument.
Brinckerhoff William B.
Cornish T.
Getty S.
ten Kate Inge Loes
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