Stable Carbon Isotope Fractionation during Bacterial Acetylene Fermentation: Potential for Life Detection in Hydrocarbon-Rich Volatiles of Icy Planet(oid)s

We report the first study of stable carbon isotope fractionation during microbial fermentation of acetylene (C2H2) in sediments, sediment enrichments, and bacterial cultures. Kinetic isotope effects (KIEs) averaged 3.7 +/- 0.5 parts per thousand for slurries prepared with sediment collected at an intertidal mudflat in San Francisco Bay and 2.7 +/- 0.2 parts per thousand for a pure culture of Pelobacter sp. isolated from these sediments. A similar KIE of 1.8 +/- 0.7 parts per thousand was obtained for methanogenic enrichments derived from sediment collected at freshwater Searsville Lake, California. However, C2H2 uptake by a highly enriched mixed culture (strain SV7) obtained from Searsville Lake sediments resulted in a larger KIE of 9.0 +/- 0.7 parts per thousand. These are modest KIEs when compared with fractionation observed during oxidation of C-1 compounds such as methane and methyl halides but are comparable to results obtained with other C-2 compounds. These observations may be useful in distinguishing biologically active processes operating at distant locales in the Solar System where C2H2 is present. These locales include the surface of Saturn's largest moon Titan and the vaporous water- and hydrocarbon-rich jets emanating from Enceladus. Key Words: AcetyleneFermentationIsotope fractionationEnceladusLife detection. Astrobiology 15, 977-986.