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Metatranscriptomic Analysis of Arctic Peat Soil Microbiota

机译:北极泥炭土壤微生物群落的转录组分析

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Recent advances in meta-omics and particularly metatranscriptomic approaches have enabled detailed studies of the structure and function of microbial communities in many ecosystems. Molecular analyses of peat soils, ecosystems important to the global carbon balance, are still challenging due to the presence of coextracted substances that inhibit enzymes used in downstream applications. We sampled layers at different depths from two high-Arctic peat soils in Svalbard for metatranscriptome preparation. Here we show that enzyme inhibition in the preparation of metatranscriptomic libraries can be circumvented by linear amplification of diluted template RNA. A comparative analysis of mRNA-enriched and nonenriched metatranscriptomes showed that mRNA enrichment resulted in a 2-fold increase in the relative abundance of mRNA but biased the relative distribution of mRNA. The relative abundance of transcripts for cellulose degradation decreased with depth, while the transcripts for hemicellulose debranching increased, indicating that the polysaccharide composition of the peat was different in the deeper and older layers. Taxonomic annotation revealed that Actinobacteria and Bacteroidetes were the dominating polysaccharide decomposers. The relative abundances of 16S rRNA and mRNA transcripts of methanogenic Archaea increased substantially with depth. Acetoclastic methanogenesis was the dominating pathway, followed by methanogenesis from formate. The relative abundances of 16S rRNA and mRNA assigned to the methanotrophic Methylococcaceae, primarily Methylobacter, increased with depth. In conclusion, linear amplification of total RNA and deep sequencing constituted the preferred method for metatranscriptomic preparation to enable high-resolution functional and taxonomic analyses of the active microbiota in Arctic peat soil.
机译:元组学特别是元转录组学方法的最新进展使得能够对许多生态系统中微生物群落的结构和功能进行详细研究。由于共提取物质的存在会抑制下游应用中使用的酶,因此对全球碳平衡至关重要的生态系统泥炭土壤进行分子分析仍然具有挑战性。我们从斯瓦尔巴特群岛的两个高北极泥炭土中取样了不同深度的层,以进行超转录组制备。在这里,我们显示了通过稀释模板RNA的线性扩增可以避免在转录组学文库制备过程中产生酶抑制作用。对mRNA富集的和非富集的转录组的比较分析表明,mRNA富集导致mRNA的相对丰度增加了2倍,但偏向了mRNA的相对分布。纤维素降解的转录本的相对丰度随深度而降低,而半纤维素脱支的转录本则增加,表明泥炭的多糖组成在较深和较老的层中是不同的。分类学注释显示,放线菌和拟杆菌属是主要的多糖分解物。产甲烷的古细菌的16S rRNA和mRNA转录本的相对丰度随着深度的增加而显着增加。破骨细胞产甲烷是主要的途径,其次是甲酸盐的产甲烷。分配给甲烷营养型甲基球菌科(主要是甲基细菌)的16S rRNA和mRNA的相对丰度随深度增加。总之,总RNA的线性扩增和深度测序构成了转录组学制备的首选方法,从而能够对北极泥炭土壤中的活性菌群进行高分辨率的功能和分类学分析。

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