title: Biogeochemical evidence of microbial activity on Mars.
abstract: We suggest a new interpretation of the data on so-called SNC meteorites and delta 13C values of the calcium carbonate minerals and organic matter discovered in them.  The delta 13C value of calcite (up to 15 ppt) is accounted for by the microbial reaction CO2 + H2 ---> CH4 + H2O.  Methane-forming bacteria also synthesize organic carbon (in the form of biomass) from CO2, and this process is accompanied by 12C fractionation.  Therefore, the organic carbon of SNC meteorites is enriched with 12C (delta 13C as low as -35 ppt).  The environmental conditions under which the calcite of SNC meteorites was formed were favorable for the activity of methanogens.
authors.affiliation: Institute for Microbiology, Russian Academy of Science, Moscow.
authors.forename: M V
authors.initials: MV
authors.lastname: Ivanov
authors.lastname: Lein AYu
mesh_terms: D001421:Bacteria, Anaerobic / Q000378:metabolism; D018533:Biomass; D002119:Calcium Carbonate / Q000032:analysis; D002245:Carbon Dioxide / Q000378:metabolism; D002247:Carbon Isotopes; D005591:Chemical Fractionation; D019605:Euryarchaeota / Q000378:metabolism*; D018559:Exobiology; D019015:Geologic Sediments / Q000032:analysis / Q000737:chemistry; D018535:Mars; D019110:Meteoroids; D008697:Methane / Q000737:chemistry / Q000378:metabolism; D012988:Soil Microbiology
chemical_list: D002247:Carbon Isotopes; D002245:Carbon Dioxide; D002119:Calcium Carbonate; D008697:Methane