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Metatranscriptomic Analysis of Arctic Peat Soil Microbiota

机译:北极泥炭土微生物的元素转录组学分析

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摘要

Recent advances in meta-omics and particularly metatranscriptomic approaches have enabled detailed studies of the structureand function of microbial communities in many ecosystems. Molecular analyses of peat soils, ecosystems important to the globalcarbon 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 amplificationof diluted template RNA. A comparative analysis of mRNA-enriched and nonenriched metatranscriptomes showed thatmRNA 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 hemicellulosedebranching 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. Therelative abundances of 16S rRNA and mRNA transcripts of methanogenic Archaea increased substantially with depth. Acetoclasticmethanogenesis was the dominating pathway, followed by methanogenesis from formate. The relative abundances of 16SrRNA 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 preparationto 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人们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。由于存在共提取物质,这些物质对下游应用中使用的酶具有抑制作用,因此对全球碳平衡至关重要的生态系统的泥炭土壤进行分子分析仍然具有挑战性。我们从斯瓦尔巴德群岛的两种高北极泥炭土中不同深度的层进行了采样,以用于转录组的制备。在这里,我们显示了通过线性稀释稀释的模板RNA可以避免在制备超转录组文库中的酶抑制作用。对富集和不富集mRNA的转录组进行比较分析表明,富集mRNA会使mRNA的相对丰度增加2倍,但会使mRNA的相对分布产生偏差。纤维素降解的转录本相对丰度随深度而降低,而针对纤维素降解的转录本相对丰度则降低。半纤维素脱支增加,表明泥炭的多糖组成在较深和较老的层中有所不同。毒理学注释显示,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。破骨细胞甲烷生成是主要途径,其次是甲酸盐的甲烷生成。分配给甲烷营养型甲基球菌科(主要是甲基细菌)的16SrRNA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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