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富营养化淡水湖泊沉积物中细菌生物量和活性的垂直分布变化。

Vertical variation of bulk and metabolically active prokaryotic community in sediment of a hypereutrophic freshwater lake.

机构信息

Center for Regional Environmental Research, National Institute for Environmental Studies (NIES), 16-2 Onogawa, Tsukuba, Ibaraki, 305-8506, Japan.

Institute for Agro-Environmental Sciences, National Agriculture and Food Research Organization (NARO), 3-1-3 Kannondai, Tsukuba, Ibaraki, 305-8604, Japan.

出版信息

Environ Sci Pollut Res Int. 2019 Mar;26(9):9379-9389. doi: 10.1007/s11356-019-04465-y. Epub 2019 Feb 26.

Abstract

This study was conducted to acquire novel insight into differences between bulk (16S rDNA) and metabolically active (16S rRNA) prokaryotic communities in the sediment of a hypereutrophic lake (Japan). In the bulk communities, the class Deltaproteobacteria and the order Methanomicrobiales were dominant among bacteria and methanogens. In the metabolically active communities, the class Alphaproteobacteria and the order Methanomicrobiales and the family Methanosaetaceae were frequently found among bacteria and methanogens. Unlike the bulk communities of prokaryotes, the composition of the metabolically active communities varied remarkably vertically, and their diversities greatly decreased in the lower 20 cm of sediment. The metabolically active prokaryotic community in the sediment core was divided into three sections based on their similarity: 0-6 cm (section 1), 9-18 cm (section 2), and 21-42 cm (section 3). This sectional distribution was consistent with the vertical pattern of the sedimentary stable carbon and nitrogen isotope ratios and oxidation-reduction potential in the porewater. These results suggest that vertical disturbance of the sediment may influence the communities and functions of metabolically active prokaryotes in freshwater lake sediments. Overall, our results indicate that rRNA analysis may be more effective than rDNA analysis for evaluation of relationships between actual microbial processes and material cycling in lake sediments.

摘要

本研究旨在深入了解富营养化湖泊沉积物中细菌和产甲烷菌的宏基因组(16S rDNA)和代谢活跃组(16S rRNA)之间的差异。在宏基因组中,变形菌纲(Deltaproteobacteria)和甲烷微菌目(Methanomicrobiales)是细菌和产甲烷菌中的主要类群。在代谢活跃组中,α变形菌纲(Alphaproteobacteria)、甲烷微菌目(Methanomicrobiales)和甲烷杆菌科(Methanosaetaceae)是细菌和产甲烷菌中的主要类群。与宏基因组中的细菌和产甲烷菌不同,代谢活跃组的组成在垂直方向上变化显著,其多样性在沉积物的下部 20cm 处大大降低。根据相似性,将沉积物芯中的代谢活跃的原核生物群落分为三个部分:0-6cm(第 1 部分)、9-18cm(第 2 部分)和 21-42cm(第 3 部分)。这种分区分布与孔隙水沉积稳定碳和氮同位素比以及氧化还原电位的垂直模式一致。这些结果表明,沉积物的垂直扰动可能会影响淡水湖泊沉积物中代谢活跃的原核生物群落和功能。总的来说,我们的研究结果表明,与 rDNA 分析相比,rRNA 分析可能更有效地评估湖泊沉积物中实际微生物过程与物质循环之间的关系。

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