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Profiling Microbial Communities in Manganese Remediation Systems Treating Coal Mine Drainage

机译:在处理煤矿排水的锰修复系统中分析微生物群落

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Water discharging from abandoned coal mines can contain extremely high manganese levels. Removing this metal is an ongoing challenge. Passive Mn(II) removal beds (MRBs) contain microorganisms that oxidize soluble Mn(II) to insoluble Mn(III/IV) minerals, but system performance is unpredictable. Using amplicon pyrosequencing, we profiled the bacterial, fungal, algal, and archaeal communities in four MRBs, performing at different levels, in Pennsylvania to determine whether they differed among MRBs and from surrounding soil and to establish the relative abundance of known Mn(II) oxidizers. Archaea were not detected; PCRs with archaeal primers returned only nontarget bacterial sequences. Fungal taxonomic profiles differed starkly between sites that remove the majority of influent Mn and those that do not, with the former being dominated by Ascomycota (mostly Dothideomycetes) and the latter by Basidiomycota (almost entirely Agaricomycetes). Taxonomic profiles for the other groups did not differ significantly between MRBs, but operational taxonomic unit-based analyses showed significant clustering by MRB with all three groups (P < 0.05). Soil samples clustered separately from MRBs in all groups except fungi, whose soil samples clustered loosely with their respective MRB. Known Mn(II) oxidizers accounted for a minor proportion of bacterial sequences (up to 0.20%) but a greater proportion of fungal sequences (up to 14.78%). MRB communities are more diverse than previously thought, and more organisms may be capable of Mn(II) oxidation than are currently known.
机译:从废弃煤矿排放的水可能含有极高的锰含量。去除这种金属是一个持续的挑战。被动式Mn(II)去除床(MRB)包含可将可溶性Mn(II)氧化为不溶性Mn(III / IV)矿物的微生物,但系统性能不可预测。使用扩增子焦磷酸测序,我们在宾夕法尼亚州的四个MRB中以不同的水平进行了细菌,真菌,藻类和古细菌群落的分析,以确定它们在MRB和周围土壤之间是否存在差异,并确定了已知Mn(II)的相对丰度。氧化剂。未检测到古细菌。具有古细菌引物的PCR仅返回非靶细菌序列。真菌分类学特征在去除大部分进水锰的位点和未去除锰的位点之间截然不同,前者主要由子囊菌(主要是十二指肠菌)占优势,而后者则由担子菌(几乎全部是真菌菌)占主导。其他组的分类学概况在MRB之间没有显着差异,但是基于操作分类学的分析显示,MRB在所有三个组中均具有显着的聚类性(P <0.05)。除真菌外,所有组中的土壤样品均与MRB分开聚集,而真菌则与各自的MRB松散地聚集在一起。已知的Mn(II)氧化剂占细菌序列的一小部分(最高0.20%),但占真菌序列的大部分(最高14.78%)。 MRB群落比以前认为的要多样化,并且比目前已知的,更多的生物可能具有Mn(II)氧化能力。

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