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希特卡溪底层沉积物中产甲烷古菌的鉴定。

Identification of methanogenic archaea in the hyporheic sediment of Sitka stream.

机构信息

Department of Ecology and Environmental Sciences - Laboratory of Aquatic Microbial Ecology, Faculty of Science, Palacky University, Olomouc, Olomouc, Czech Republic.

出版信息

PLoS One. 2013 Nov 20;8(11):e80804. doi: 10.1371/journal.pone.0080804. eCollection 2013.

Abstract

Methanogenic archaea produce methane as a metabolic product under anoxic conditions and they play a crucial role in the global methane cycle. In this study molecular diversity of methanogenic archaea in the hyporheic sediment of the lowland stream Sitka (Olomouc, Czech Republic) was analyzed by PCR amplification, cloning and sequencing analysis of the methyl coenzyme M reductase alpha subunit (mcrA) gene. Sequencing analysis of 60 clones revealed 24 different mcrA phylotypes from hyporheic sedimentary layers to a depth of 50 cm. Phylotypes were affiliated with Methanomicrobiales, Methanosarcinales and Methanobacteriales orders. Only one phylotype remains unclassified. The majority of the phylotypes showed higher affiliation with uncultured methanogens than with known methanogenic species. The presence of relatively rich assemblage of methanogenic archaea confirmed that methanogens may be an important component of hyporheic microbial communities and may affect CH4 cycling in rivers.

摘要

产甲烷古菌在缺氧条件下将甲烷作为代谢产物产生,它们在全球甲烷循环中起着至关重要的作用。在这项研究中,通过聚合酶链反应(PCR)扩增、克隆和甲基辅酶 M 还原酶 α 亚基(mcrA)基因的测序分析,分析了低地溪流锡特卡(捷克奥洛穆茨)潜流带沉积物中产甲烷古菌的分子多样性。对 60 个克隆的测序分析显示,潜流带沉积物中的 mcrA 基因有 24 种不同的基因型,深度可达 50 厘米。基因型与甲烷微菌目、甲烷杆菌目和甲烷球菌目有关。只有一个基因型尚未分类。大多数基因型与未培养的产甲烷菌的亲缘关系比与已知的产甲烷菌更为密切。产甲烷古菌的丰富组合的存在证实了产甲烷菌可能是潜流带微生物群落的重要组成部分,并可能影响河流中的 CH4 循环。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/46fa/3835567/ca9ba870af7c/pone.0080804.g001.jpg

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