MOE Key Lab of Environmental Remediation and Ecosystem Health, College of Environmental and Resource Science, Zhejiang University, Hangzhou, China.
Centre for Microbiome Research, School of Biomedical Sciences, Queensland University of Technology (QUT), Translational Research Institute, Woolloongabba, QLD, Australia.
ISME J. 2021 Dec;15(12):3683-3692. doi: 10.1038/s41396-021-01044-3. Epub 2021 Jun 28.
Methanotrophic microorganisms play a critical role in controlling the flux of methane from natural sediments into the atmosphere. Methanotrophs have been shown to couple the oxidation of methane to the reduction of diverse electron acceptors (e.g., oxygen, sulfate, nitrate, and metal oxides), either independently or in consortia with other microbial partners. Although several studies have reported the phenomenon of methane oxidation linked to selenate reduction, neither the microorganisms involved nor the underlying trophic interaction has been clearly identified. Here, we provide the first detailed evidence for interspecies electron transfer between bacterial populations in a bioreactor community where the reduction of selenate is linked to methane oxidation. Metagenomic and metaproteomic analyses of the community revealed a novel species of Methylocystis as the most abundant methanotroph, which actively expressed proteins for oxygen-dependent methane oxidation and fermentation pathways, but lacked the genetic potential for selenate reduction. Pseudoxanthomonas, Piscinibacter, and Rhodocyclaceae populations appeared to be responsible for the observed selenate reduction using proteins initially annotated as periplasmic nitrate reductases, with fermentation by-products released by the methanotrophs as electron donors. The ability for the annotated nitrate reductases to reduce selenate was confirmed by gene knockout studies in an isolate of Pseudoxanthomonas. Overall, this study provides novel insights into the metabolic flexibility of the aerobic methanotrophs that likely allows them to thrive across natural oxygen gradients, and highlights the potential role for similar microbial consortia in linking methane and other biogeochemical cycles in environments where oxygen is limited.
产甲烷微生物在控制甲烷从自然沉积物向大气中释放通量方面起着关键作用。已证明产甲烷菌可以将甲烷氧化与多种电子受体(如氧气、硫酸盐、硝酸盐和金属氧化物)的还原偶联,无论是独立进行还是与其他微生物伙伴一起进行。尽管有几项研究报告了与硒酸盐还原相关的甲烷氧化现象,但涉及的微生物和潜在的营养相互作用尚未明确确定。在这里,我们提供了第一个详细证据,证明在与甲烷氧化相关的硒酸盐还原的生物反应器群落中,细菌种群之间存在种间电子转移。对群落的宏基因组和宏蛋白质组分析揭示了一种新型的甲基球菌(Methylocystis)作为最丰富的产甲烷菌,它积极表达了依赖氧气的甲烷氧化和发酵途径的蛋白质,但缺乏硒酸盐还原的遗传潜力。假单胞菌、Piscinibacter 和 Rhodocyclaceae 种群似乎负责利用最初注释为周质硝酸盐还原酶的蛋白质观察到的硒酸盐还原,产甲烷菌释放的发酵副产物作为电子供体。通过对假单胞菌分离株的基因敲除研究证实了注释的硝酸盐还原酶还原硒酸盐的能力。总的来说,这项研究为好氧产甲烷菌的代谢灵活性提供了新的见解,这可能使它们能够在自然氧梯度中茁壮成长,并强调了类似微生物共生体在连接甲烷和其他生物地球化学循环中的潜在作用,在氧气有限的环境中。