产甲烷
巴氏甲烷八叠球菌
甲烷八叠球菌
生物
甲烷菌
缺氧水域
甲烷微生物
广域古菌界
铁质
氧化还原
甲烷杆菌
环境化学
细菌
甲烷
古细菌
无机化学
化学
生态学
遗传学
有机化学
作者
Peter M. van Bodegom,Johannes C. M. Scholten,Alfons J. M. Stams
标识
DOI:10.1016/j.femsec.2004.03.017
摘要
Observed inhibition of methanogenesis under Fe(III)-reducing conditions is usually explained by competition of methanogens and Fe(III)-reducing bacteria for the common substrates acetate and hydrogen. However, substrate competition alone cannot explain the strong inhibition of methanogenesis during Fe(III)-reduction. We demonstrate direct inhibition of methanogenesis by amorphous Fe(OH)3 at concentrations between 0 and 10 mM in experiments with pure cultures of methanogens. The sensitivity toward Fe(III) was higher for Methanospirillum hungatei and Methanosarcina barkeri grown with H2/CO2 than for Methanosaeta concilii and Methanosarcina barkeri grown with acetate. Cultures of Methanosarcina barkeri grown with H2/CO2 and methanol demonstrated a capacity for Fe(III) reduction, which suggests that Fe(III)-reduction by methanogens may also contribute to Fe(III) inhibition of methanogenesis. Our results have important implications for kinetic modelling of microbial redox processes in anoxic soils and sediments.
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