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具有高丰度古菌介导甲烷厌氧氧化的陆地泥火山微生物群落的多样性和代谢潜力

Diversity and Metabolic Potential of the Terrestrial Mud Volcano Microbial Community with a High Abundance of Archaea Mediating the Anaerobic Oxidation of Methane.

作者信息

Merkel Alexander Y, Chernyh Nikolay A, Pimenov Nikolai V, Bonch-Osmolovskaya Elizaveta A, Slobodkin Alexander I

机构信息

Research Center of Biotechnology, Winogradsky Institute of Microbiology, Russian Academy of Sciences, Leninskiy Prospect, 33, Bld. 2, 119071 Moscow, Russia.

出版信息

Life (Basel). 2021 Sep 11;11(9):953. doi: 10.3390/life11090953.

DOI:10.3390/life11090953
PMID:34575103
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC8470020/
Abstract

Terrestrial mud volcanoes (TMVs) are important natural sources of methane emission. The microorganisms inhabiting these environments remain largely unknown. We studied the phylogenetic composition and metabolic potential of the prokaryotic communities of TMVs located in the Taman Peninsula, Russia, using a metagenomic approach. One of the examined sites harbored a unique community with a high abundance of anaerobic methane-oxidizing archaea belonging to ANME-3 group (39% of all 16S rRNA gene reads). The high number of ANME-3 archaea was confirmed by qPCR, while the process of anaerobic methane oxidation was demonstrated by radioisotopic experiments. We recovered metagenome-assembled genomes (MAGs) of archaeal and bacterial community members and analyzed their metabolic capabilities. The ANME-3 MAG contained a complete set of genes for methanogenesis as well as of ribosomal RNA and did not encode proteins involved in dissimilatory nitrate or sulfate reduction. The presence of multiheme -type cytochromes suggests that ANME-3 can couple methane oxidation with the reduction of metal oxides or with the interspecies electron transfer to a bacterial partner. The bacterial members of the community were mainly represented by autotrophic, nitrate-reducing, sulfur-oxidizing bacteria, as well as by fermentative microorganisms. This study extends the current knowledge of the phylogenetic and metabolic diversity of prokaryotes in TMVs and provides a first insight into the genomic features of ANME-3 archaea.

摘要

陆地泥火山是甲烷排放的重要天然来源。栖息在这些环境中的微生物在很大程度上仍不为人所知。我们采用宏基因组学方法研究了位于俄罗斯塔曼半岛的泥火山原核生物群落的系统发育组成和代谢潜力。其中一个被检测的地点拥有一个独特的群落,富含属于ANME-3组的厌氧甲烷氧化古菌(占所有16S rRNA基因读数的39%)。通过定量PCR证实了ANME-3古菌的高数量,同时通过放射性同位素实验证明了厌氧甲烷氧化过程。我们获得了古菌和细菌群落成员的宏基因组组装基因组(MAG),并分析了它们的代谢能力。ANME-3 MAG包含一套完整的产甲烷基因以及核糖体RNA,并且不编码参与异化硝酸盐或硫酸盐还原的蛋白质。多血红素型细胞色素的存在表明ANME-3可以将甲烷氧化与金属氧化物的还原或与种间电子转移到细菌伙伴耦合起来。该群落的细菌成员主要由自养、硝酸盐还原、硫氧化细菌以及发酵微生物组成。这项研究扩展了当前对陆地泥火山中原核生物系统发育和代谢多样性的认识,并首次深入了解了ANME-3古菌的基因组特征。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/3097/8470020/0f5dc244efcb/life-11-00953-g004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/3097/8470020/013ed2ca5414/life-11-00953-g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/3097/8470020/75ed1d7b2062/life-11-00953-g002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/3097/8470020/77f0a428542a/life-11-00953-g003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/3097/8470020/0f5dc244efcb/life-11-00953-g004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/3097/8470020/013ed2ca5414/life-11-00953-g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/3097/8470020/75ed1d7b2062/life-11-00953-g002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/3097/8470020/77f0a428542a/life-11-00953-g003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/3097/8470020/0f5dc244efcb/life-11-00953-g004.jpg

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