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首页> 外文期刊>Applied and Environmental Microbiology >Microbial Community Structure and Activity Linked to Contrasting Biogeochemical Gradients in Bog and Fen Environments of the Glacial Lake Agassiz Peatland
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Microbial Community Structure and Activity Linked to Contrasting Biogeochemical Gradients in Bog and Fen Environments of the Glacial Lake Agassiz Peatland

机译:冰川湖阿加西兹泥炭地沼泽和芬环境中的微生物群落结构和活性与生物地球化学梯度形成反差

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摘要

The abundances, compositions, and activities of microbial communities were investigated at bog and fen sites in the Glacial Lake Agassiz Peatland of northwestern Minnesota. These sites contrast in the reactivity of dissolved organic matter (DOM) and the presence or absence of groundwater inputs. Microbial community composition was characterized using pyrosequencing and clone library construction of phylogenetic marker genes. Microbial distribution patterns were linked to pH, concentrations of dissolved organic carbon and nitrogen, C/N ratios, optical properties of DOM, and activities of laccase and peroxidase enzymes. Both bacterial and archaeal richness and rRNA gene abundance were >2 times higher on average in the fen than in the bog, in agreement with a higher pH, labile DOM content, and enhanced enzyme activities in the fen. Fungi were equivalent to an average of 1.4% of total prokaryotes in gene abundance assayed by quantitative PCR. Results revealed statistically distinct spatial patterns between bacterial and fungal communities. Fungal distribution did not covary with pH and DOM optical properties and was vertically stratified, with a prevalence of Ascomycota and Basidiomycota near the surface and much higher representation of Zygomycota in the subsurface. In contrast, bacterial community composition largely varied between environments, with the bog dominated by Acidobacteria (61% of total sequences), while the Firmicutes (52%) dominated in the fen. Acetoclastic Methanosarcinales showed a much higher relative abundance in the bog, in contrast to the dominance of diverse hydrogenotrophic methanogens in the fen. This is the first quantitative and compositional analysis of three microbial domains in peatlands and demonstrates that the microbial abundance, diversity, and activity parallel with the pronounced differences in environmental variables between bog and fen sites.
机译:在明尼苏达州西北部的冰川湖阿加西兹泥炭地的沼泽和站点调查了微生物群落的丰度,组成和活动。这些位置形成了溶解有机物(DOM)的反应性以及是否存在地下水输入的对比。使用焦磷酸测序和系统发育标记基因克隆文库构建来表征微生物群落组成。微生物的分布模式与pH,溶解的有机碳和氮的浓度,C / N比,DOM的光学特性以及漆酶和过氧化物酶的活性有关。 bacterial中细菌和古细菌的丰富度以及rRNA基因的丰度均比沼泽平均高2倍以上,这与较高的pH值,不稳定的DOM含量和enhanced中的酶活性增强相一致。通过定量PCR检测,真菌平均相当于原核生物总数的1.4%。结果揭示了细菌和真菌群落之间的统计学上独特的空间格局。真菌的分布不随pH和DOM光学特性变化,而是垂直分层的,在表层附近普遍存在子囊菌和担子菌,而在地下菌丝体的代表性更高。相比之下,细菌群落组成在不同环境之间变化很大,其中沼泽以酸杆菌为主导(占总序列的61%),而Fimicutes(52%)则以the为主导。与et中各种氢营养型产甲烷菌的优势形成相比,乙状结肠甲烷化甲烷菌在沼泽中显示出更高的相对丰度。这是泥炭地中三个微生物域的首次定量和组成分析,表明微生物的丰度,多样性和活性与沼泽和站点之间环境变量的显着差异平行。

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