甲烷八叠球菌
巴氏甲烷八叠球菌
地杆菌
生物修复
醋酸激酶
生物
产甲烷
环境化学
甲烷微生物
化学
生物化学
生态学
细菌
甲烷
污染
遗传学
大肠杆菌
生物膜
基因
作者
Dawn E. Holmes,Roberto Orelana,Ludovic Giloteaux,Li-Ying Wang,Pravin Malla Shrestha,Kenneth H. Williams,Derek R. Lovley,Amelia‐Elena Rotaru
标识
DOI:10.1007/s00248-018-1165-5
摘要
Previous studies of acetate-promoted bioremediation of uranium-contaminated aquifers focused on Geobacter because no other microorganisms that can couple the oxidation of acetate with U(VI) reduction had been detected in situ. Monitoring the levels of methyl CoM reductase subunit A (mcrA) transcripts during an acetate-injection field experiment demonstrated that acetoclastic methanogens from the genus Methanosarcina were enriched after 40 days of acetate amendment. The increased abundance of Methanosarcina corresponded with an accumulation of methane in the groundwater. In order to determine whether Methanosarcina species could be participating in U(VI) reduction in the subsurface, cell suspensions of Methanosarcina barkeri were incubated in the presence of U(VI) with acetate provided as the electron donor. U(VI) was reduced by metabolically active M. barkeri cells; however, no U(VI) reduction was observed in inactive controls. These results demonstrate that Methanosarcina species could play an important role in the long-term bioremediation of uranium-contaminated aquifers after depletion of Fe(III) oxides limits the growth of Geobacter species. The results also suggest that Methanosarcina have the potential to influence uranium geochemistry in a diversity of anaerobic sedimentary environments.
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