Food and Bioproduct Sciences, University of Saskatchewan, Saskatoon, SK, Canada.
J Microbiol. 2013 Oct;51(5):558-69. doi: 10.1007/s12275-013-3075-z. Epub 2013 Sep 14.
The microbial diversity and biogeochemical potential associated with a northern Saskatchewan uranium mine water-tailings interface was examined using culture-dependent and -independent techniques. Morphologically-distinct colonies from uranium mine water-tailings and a reference lake (MC) obtained using selective and non-selective media were selected for 16S rRNA gene sequencing and identification, revealing that culturable organisms from the uranium tailings interface were dominated by Firmicutes and Betaproteobacteria; whereas, MC organisms mainly consisted of Bacteroidetes and Gammaproteobacteria. Ion Torrent (IT) 16S rRNA metagenomic analysis carried out on extracted DNA from tailings and MC interfaces demonstrated the dominance of Firmicutes in both of the systems. Overall, the tailings-water interface environment harbored a distinct bacterial community relative to the MC, reflective of the ambient conditions (i.e., total dissolved solids, pH, salinity, conductivity, heavy metals) dominating the uranium tailings system. Significant correlations among the physicochemical data and the major bacterial groups present in the tailings and MC were also observed. Presence of sulfate reducing bacteria demonstrated by culture-dependent analyses and the dominance of Desulfosporosinus spp. indicated by Ion Torrent analyses within the tailings-water interface suggests the existence of anaerobic microenvironments along with the potential for reductive metabolic processes.
采用培养依赖和非依赖技术,研究了萨斯喀彻温省北部铀矿废水-尾矿界面相关的微生物多样性和生物地球化学潜力。使用选择性和非选择性培养基从铀矿废水-尾矿和参照湖(MC)中分离出形态独特的菌落,进行 16S rRNA 基因测序和鉴定,结果表明,可培养的铀尾矿界面生物主要由厚壁菌门和β变形菌门组成;而 MC 生物主要由拟杆菌门和γ变形菌门组成。对来自尾矿和 MC 界面的提取 DNA 进行的 Ion Torrent(IT)16S rRNA 宏基因组分析表明,两种系统中厚壁菌门均占优势。总体而言,尾矿-水界面环境与 MC 相比具有独特的细菌群落,反映了主导铀尾矿系统的环境条件(即总溶解固体、pH 值、盐度、电导率、重金属)。还观察到尾矿和 MC 中主要细菌群与理化数据之间存在显著相关性。通过培养依赖分析检测到硫酸盐还原菌的存在,以及 Ion Torrent 分析表明脱硫菌属的优势,表明在尾矿-水界面存在厌氧微环境和潜在的还原代谢过程。