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Journal of Undergraduate Research

Keywords

hydrocarbon biodegradation, hypersaline aqueous, isotopic, HCO3

College

Life Sciences

Department

Microbiology and Molecular Biology

Abstract

In order to demonstrate the presence of hydrocarbon biodegradation in a hypersaline aqueous environment an isotopic method of analysis was employed. The relative 13C abundance of Great Salt Lake’s HCO3- in equilibrium with atmosphere and fossil hydrocarbon are quite different. By creating microcosms using the sediment of Rozel Point and allowing the microbial activity to occur over a 12 week timeframe, data were collected regarding the change of CO2 concentration and the isotopic signature of the 13C in HCO3- of the microcosm water. A shift in the isotopic signature from the 13C levels of the HCO3- in equilibrium with atmosphere toward that of hydrocarbon 13C levels in the live microcosms, but not in the killed microcosm would suggest that hydrocarbon biodegradation is occurring.

Included in

Microbiology Commons

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