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CO 2  sequestration in deep-subsurface formations including oil reservoirs is a potential measure to reduce the CO 2  concentration in the atmosphere. However, the fate of the CO 2  and the ecological influences in carbon dioxide capture and storage (CDCS) facilities is not understood clearly. In the current study, the fate of CO 2  (in bicarbonate form; 0∼90 mM) with 10 mM of formate as electron donor and carbon source was investigated with high-temperature production water from oilfield in China. The isotope data showed that bicarbonate could be reduced to methane by methanogens and major pathway of methanogenesis could be syntrophic formate oxidation coupled with CO 2  reduction and formate methanogenesis under the anaerobic conditions. The bicarbonate addition induced the shift of microbial community. Addition of bicarbonate and formate was associated with a decrease of  Methanosarcinales , but promotion of  Methanobacteriales  in all treatments.  Thermodesulfovibrio  was the major group in all the samples and  Thermacetogenium  dominated in the high bicarbonate treatments. The results indicated that CO 2  from CDCS could be transformed to methane and the possibility of microbial CO 2  conversion for enhanced microbial energy recovery in oil reservoirs.

frontiers in microbiology

Formate-Dependent Microbial Conversion of CO2 and the Dominant Pathways of Methanogenesis in Production Water of High-temperature Oil Reservoirs Amended with Bicarbonate