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首页> 外文期刊>Applied and Environmental Microbiology >Functional Gene Analysis of Freshwater Iron-Rich Flocs at Circumneutral pH and Isolation of a Stalk-Forming Microaerophilic Iron-Oxidizing Bacterium
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Functional Gene Analysis of Freshwater Iron-Rich Flocs at Circumneutral pH and Isolation of a Stalk-Forming Microaerophilic Iron-Oxidizing Bacterium

机译:富含铁的淡水絮凝剂在环境pH值下的功能基因分析和形成茎的微需氧铁氧化细菌的分离

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Iron-rich flocs often occur where anoxic water containing ferrous iron encounters oxygenated environments. Culture-independent molecular analyses have revealed the presence of 16S rRNA gene sequences related to diverse bacteria, including autotrophic iron oxidizers and methanotrophs in iron-rich flocs; however, the metabolic functions of the microbial communities remain poorly characterized, particularly regarding carbon cycling. In the present study, we cultivated iron-oxidizing bacteria (FeOB) and performed clone library analyses of functional genes related to carbon fixation and methane oxidization (cbbM and pmoA, respectively), in addition to bacterial and archaeal 16S rRNA genes, in freshwater iron-rich flocs at groundwater discharge points. The analyses of 16S rRNA, cbbM, and pmoA genes strongly suggested the coexistence of autotrophic iron oxidizers and methanotrophs in the flocs. Furthermore, a novel stalk-forming microaerophilic FeOB, strain OYT1, was isolated and characterized phylogenetically and physiologically. The 16S rRNA and cbbM gene sequences of OYT1 are related to those of other microaerophilic FeOB in the family Gallionellaceae, of the Betaproteobacteria, isolated from freshwater environments at circumneutral pH. The physiological characteristics of OYT1 will help elucidate the ecophysiology of microaerophilic FeOB. Overall, this study demonstrates functional roles of microorganisms in iron flocs, suggesting several possible linkages between Fe and C cycling.
机译:富含铁的絮凝物经常发生在含亚铁的缺氧水遇到氧化环境的地方。不依赖培养物的分子分析已揭示了与多种细菌相关的16S rRNA基因序列的存在,包括富铁絮凝物中的自养铁氧化剂和甲烷营养菌。然而,微生物群落的代谢功能仍然差强人意,特别是在碳循环方面。在本研究中,我们在淡水铁中除细菌和古细菌16S rRNA基因外,还培养了铁氧化细菌(FeOB),并进行了与碳固定和甲烷氧化相关的功能基因(分别为cbbM和pmoA)的克隆文库分析。地下水排放点富含絮凝物。对16S rRNA,cbbM和pmoA基因的分析强烈表明,絮凝物中同时存在自养铁氧化剂和甲烷营养菌。此外,分离并形成了新的茎形成微需氧FeOB菌株OYT1,并在系统发育和生理上进行了表征。 OYT1的16S rRNA和cbbM基因序列与Betaproteobacteria的Gallionellaceae家族中其他微需氧FeOB的序列有关,这些蛋白是从周围环境pH值的淡水环境中分离出来的。 OYT1的生理特性将有助于阐明微需氧的FeOB的生态生理学。总的来说,这项研究表明了微生物在铁絮中的功能作用,表明了铁和碳循环之间的几种可能的联系。

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