Microbial communities in two production waters of a low-temperature and low-salinity petroleum reservoir in Canada were examined using cultural and molecular approaches. The predominant cultivated microorganisms were homoacetogens but sulfate-reducers, acetoclastic methanogens and denitrifiers also gave significant counts. The dominant members of the culturable population were affiliated with the Firmicutes, the "Deltaproteobacteria", the "Epsilonproteobacteria", the Spirochaetes and the Euryarchaeota. 16S rRNA gene clone libraries were also constructed from the total DNA collected from production waters. The bacterial library was entirely composed by a single phylotype related to Arcobacter. The archaeal phylotypes were generally very closely related to members of the orders Methanosarcinales and Methanomicrobiales. Consistent with earlier observations, our data suggest that methanogenesis is a dominant terminal process in the reservoir. Moreover, the cross-evaluation of culture-dependent and -independent techniques also indicates that, contrary to most studies, both acetoclastic and lithotrophic methanogens may be involved in this process. This first investigation of the microbial diversity in a non water-flooded low-temperature and low-salinity petroleum reservoir expands substantially our knowledge of the extent of microbial diversity and highlights the complexity of microbial communities involved in the oil field food chain.
Recent molecular characterizations of microbial communities from deep-sea hydrothermal sites indicate the predominance of bacteria belonging to the epsilon subdivision of Proteobacteria (epsilon Proteobacteria). Here, we report the first enrichments and characterizations of four epsilon Proteobacteria that are directly associated with Alvinella pompejana, a deep sea hydrothermal vent polychete, or with hydrothermal vent chimney samples. These novel bacteria were moderately thermophilic sulfur-reducing heterotrophs growing on formate as the energy and carbon source. In addition, two of them (Am-H and Ex-18.2) could grow on sulfur lithoautrotrophically using hydrogen as the electron donor. Optimal growth temperatures of the bacteria ranged from 41 to 45°C. Phylogenetic analysis of the small-subunit ribosomal gene of the two heterotrophic bacteria demonstrated 95% similarity to Sulfurospirillum arcachonense, an epsilon Proteobacteria isolated from an oxidized marine surface sediment. The autotrophic bacteria grouped within a deeply branching clade of the epsilon Proteobacteria, to date composed only of uncultured bacteria detected in a sample from a hydrothermal vent along the mid-Atlantic ridge. A molecular survey of various hydrothermal vent environments demonstrated the presence of two of these bacteria (Am-N and Am-H) in more than one geographic location and habitat. These results suggest that certain epsilon Proteobacteria likely fill important niches in the environmental habitats of deep-sea hydrothermal vents, where they contribute to overall carbon and sulfur cycling at moderate thermophilic temperatures.
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