BIODEGRADATION OF DEEPWATER HORIZON PETROLEUM HYDROCARBONS IN BARATARIA BAY MARSHES: GEOMICROBIOLOGY AND CLAY MINERAL ENHANCEMENT
Repeated sampling is now underway to 1) characterize petroleum hydrocarbon biodegradation in the marshes; 2) characterize both aerobic and anaerobic microbial function; and 3) test the hypothesis that clays may enhance biodegradation of Deepwater Horizon petroleum hydrocarbons. Experimental plots were established in September, 2010, several months after emplacement of the contaminants, and amended with high-charge montmorillonite; control areas were also established. Serial analyses include petroleum hydrocarbons by GC/MS, clay mineralogy by XRD, microbial composition and function by analyses of functional gene transcripts using RT-PCR, quantitative PCR, and clone library. Experimental microcosms have also been initiated to model biodegradation with varying clay content.
Natural marsh clay mineralogy is heterogeneous, with kaolinite, illite, and smectite, consistent with Mississippi Basin drainage. Experimental sites show enhanced smectite:kaolinite ratios by XRD, providing a basis for documenting clay amendment. GC/MS analyses show the expected dominance of n-alkane components of petroleum hydrcarbons; detailed forensic biomarker fingerprinting and time-series compound ratio analyses are forthcoming. Transcript analyses of functional genes indicate Fe-reducing, sulfate-reducing, and methanogenic prokaryotic communities are metabolically active at both control and experimental plots. Such communities have been linked to petroleum hydrocarbon biodegradation in previous studies, and likely represent the main agents of biodegradation in the Barataria Bay marshes.