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对摩洛哥废弃的凯塔拉磁黄铁矿尾矿中存在的细菌和古菌群落进行深入表征。

In-depth characterization of bacterial and archaeal communities present in the abandoned Kettara pyrrhotite mine tailings (Morocco).

作者信息

Bruneel Odile, Mghazli N, Hakkou R, Dahmani I, Filali Maltouf A, Sbabou L

机构信息

Laboratoire de Microbiologie et Biologie Moléculaire, LMBM, Faculté des Sciences, Université Mohammed V, Av Ibn Batouta, BP1014, Rabat, Morocco.

Laboratoire HydroSciences Montpellier, UMR5569 (CNRS/IRD/UM), Université de Montpellier, CC0057 (MSE), 16, rue Auguste Broussonet, 34090, Montpellier, France.

出版信息

Extremophiles. 2017 Jul;21(4):671-685. doi: 10.1007/s00792-017-0933-3. Epub 2017 Apr 26.

Abstract

In Morocco, pollution caused by closed mines continues to be a serious threat to the environment, like the generation of acid mine drainage. Mine drainage is produced by environmental and microbial oxidation of sulfur minerals originating from mine wastes. The fundamental role of microbial communities is well known, like implication of Fe-oxidizing and to a lesser extent S-oxidizing microorganism in bioleaching. However, the structure of the microbial communities varies a lot from one site to another, like diversity depends on many factors such as mineralogy, concentration of metals and metalloids or pH, etc. In this study, prokaryotic communities in the pyrrhotite-rich tailings of Kettara mine were characterized using the Illumina sequencing. In-depth phylogenetic analysis revealed a total of 12 phyla of bacteria and 1 phyla of Archaea. The majority of sequences belonged to the phylum of Proteobacteria and Firmicutes with a predominance of Bacillus, Pseudomonas or Corynebacterium genera. Many microbial populations are implicated in the iron, sulfur and arsenic cycles, like Acidiferrobacter, Leptospirillum, or Alicyclobacillus in Fe; Acidiferrobacter and Sulfobacillus in S; and Bacillus or Pseudomonas in As. This is one of the first description of prokaryotic communities in pyrrhotite-rich mine tailings using high-throughput sequencing.

摘要

在摩洛哥,关闭的矿山造成的污染继续对环境构成严重威胁,例如酸性矿山排水的产生。矿山排水是由源自矿山废弃物的硫矿物质的环境和微生物氧化作用产生的。微生物群落的基本作用是众所周知的,比如铁氧化微生物以及在较小程度上硫氧化微生物在生物浸出中的作用。然而,微生物群落的结构因地点而异,例如多样性取决于许多因素,如矿物学、金属和类金属的浓度或pH值等。在本研究中,利用Illumina测序对凯塔拉矿富含磁黄铁矿的尾矿中的原核生物群落进行了表征。深入的系统发育分析揭示了总共12个细菌门和1个古细菌门。大多数序列属于变形菌门和厚壁菌门,其中芽孢杆菌属、假单胞菌属或棒杆菌属占主导地位。许多微生物种群参与了铁、硫和砷的循环,比如在铁循环中有嗜酸铁杆菌属、钩端螺旋菌属或嗜酸环脂芽孢杆菌属;在硫循环中有嗜酸铁杆菌属和硫杆菌属;在砷循环中有芽孢杆菌属或假单胞菌属。这是首次使用高通量测序对富含磁黄铁矿的矿山尾矿中的原核生物群落进行描述之一。

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