LOSING WEIGHT: UNDERSTANDING THE METHANOGENIC METABOLISM OF HEAVY HYDROCARBONS IN FOSSIL ENERGY RESERVOIRS
Thus, we sought to determine whether heavier hydrocarbons are susceptible to methanogenic decay, using a 3-ringed aromatic (phenanthrene, PHEN) and a waxy paraffin (C28H58, octacosane, OCT) as model compounds. In PHEN-amended cultures, including enrichments from Alberta’s heavily biodegraded oil sands, enhanced levels of CH4 and hydrocarbon depletion were observed relative to controls, providing evidence for methanogenic PHEN degradation. GC-MS analysis of PHEN-amended cultures revealed putative metabolites that were not present in controls, providing clues as to how phenanthrene may be metabolized. In OCT-amended enrichments, significantly enhanced CH4 was also seen compared to substrate-free controls, suggesting methanogenic degradation of C28H58. Microbial community sequencing of this culture revealed syntrophs often associated with anoxic alkane metabolism and diverse methanogens. Further, the detection of the assA gene (the key gene for anaerobic alkane metabolism) substantiated methanogenic OCT biodegradation. Overall, we found that heavier hydrocarbons are susceptible to methanogenic biodegradation, not only broadening the range of hydrocarbons that can be metabolized, but offering promise for the application of microbial technologies to a broader range of fossil energy reservoirs.