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Conductive Iron Oxides Promote Methanogenic Acetate Degradation by Microbial Communities in a High-Temperature Petroleum Reservoir

机译:导电氧化铁促进高温石油储层中微生物群落的产甲烷乙酸盐降解。

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Supplementation with conductive magnetite particles promoted methanogenic acetate degradation by microbial communities enriched from the production water of a high-temperature petroleum reservoir. A microbial community analysis revealed that Petrothermobacter spp. (phylum Deferribacteres ), known as thermophilic Fe(III) reducers, predominated in the magnetite-supplemented enrichment, whereas other types of Fe(III) reducers, such as Thermincola spp. and Thermotoga spp., were dominant under ferrihydrite-reducing conditions. These results suggest that magnetite induced interspecies electron transfer via electric currents through conductive particles between Petrothermobacter spp. and methanogens. This is the first evidence for possible electric syntrophy in high-temperature subsurface environments.
机译:补充导电磁铁矿颗粒可通过从高温石油储层采出水中富集的微生物群落促进产甲烷乙酸盐的降解。微生物群落分析表明,Petrothermobacter spp。 (铁杆菌属),称为嗜热Fe(III)还原剂,主要是在磁铁矿补充的富集物中,而其他类型的Fe(III)还原剂,例如Thermincola spp。在减少水铁矿的条件下,Thermo and Thermotoga spp。占主导地位。这些结果表明,磁铁矿通过Petrothermobacter spp之间的导电颗粒通过电流进行种间电子转移。和产甲烷菌。这是在高温地下环境中可能发生电同生的第一个证据。

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