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通过分析小亚基核糖体RNA基因鉴定甲基汞污染尾矿中的硫酸盐还原菌。

Identification of sulfate-reducing bacteria in methylmercury-contaminated mine tailings by analysis of SSU rRNA genes.

作者信息

Winch Susan, Mills Heath J, Kostka Joel E, Fortin Danielle, Lean David R S

机构信息

Department of Earth Science, University of Ottawa, Ottawa, ON, Canada.

出版信息

FEMS Microbiol Ecol. 2009 Apr;68(1):94-107. doi: 10.1111/j.1574-6941.2009.00658.x.

Abstract

Sulfate-reducing bacteria (SRB) are often used in bioremediation of acid mine drainage because microbial sulfate reduction increases pH and produces sulfide that binds with metals. Mercury methylation has also been linked with sulfate reduction. Previous geochemical analysis indicated the occurrence of sulfate reduction in mine tailings, but no molecular characterization of the mine tailings-associated microbial community has determined which SRB are present. This study characterizes the bacterial communities of two geochemically contrasting, high-methylmercury mine tailing environments, with emphasis on SRB, by analyzing small subunit (SSU) rRNA genes present in the tailings sediments and in enrichment cultures inoculated with tailings. Novel Deltaproteobacteria and Firmicutes-related sequences were detected in both the pH-neutral gold mine tailings and the acidic high-sulfide base-metal tailings. At the subphylum level, the SRB communities differed between sites, suggesting that the community structure was dependent on local geochemistry. Clones obtained from the gold tailings and enrichment cultures were more similar to previously cultured isolates whereas clones from acidic tailings were more closely related to uncultured lineages identified from other acidic sediments worldwide. This study provides new insights into the novelty and diversity of bacteria colonizing mine tailings, and identifies specific organisms that warrant further investigation with regard to their roles in mercury methylation and sulfur cycling in these environments.

摘要

硫酸盐还原菌(SRB)常用于酸性矿山排水的生物修复,因为微生物硫酸盐还原可提高pH值并产生与金属结合的硫化物。汞甲基化也与硫酸盐还原有关。先前的地球化学分析表明尾矿中存在硫酸盐还原现象,但尚未对与尾矿相关的微生物群落进行分子表征以确定存在哪些SRB。本研究通过分析尾矿沉积物和接种尾矿的富集培养物中存在的小亚基(SSU)rRNA基因,对两个地球化学特征不同、甲基汞含量高的矿山尾矿环境中的细菌群落进行了表征,重点是SRB。在pH值中性的金矿尾矿和酸性高硫化物贱金属尾矿中均检测到了新的δ-变形菌纲和厚壁菌门相关序列。在亚门水平上,不同地点的SRB群落有所不同,这表明群落结构取决于当地的地球化学特征。从金矿尾矿和富集培养物中获得的克隆与先前培养的分离株更相似,而从酸性尾矿中获得的克隆与从全球其他酸性沉积物中鉴定出的未培养谱系关系更密切。本研究为定殖于尾矿中的细菌的新颖性和多样性提供了新的见解,并鉴定出了特定的生物体,这些生物体在这些环境中的汞甲基化和硫循环中的作用值得进一步研究。

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