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在瓜伊马斯盆地热液沉积物中,存在着多种厌氧产甲烷菌和多碳烷烃代谢古菌,它们共存并表现出活性。

Diverse anaerobic methane- and multi-carbon alkane-metabolizing archaea coexist and show activity in Guaymas Basin hydrothermal sediment.

机构信息

Microbiology Division, School of Life Sciences and Biotechnology, Shanghai Jiao Tong University, Shanghai 200240, China.

State Key Laboratory of Microbial Metabolism, Shanghai Jiao Tong University, Shanghai 200240, China.

出版信息

Environ Microbiol. 2019 Apr;21(4):1344-1355. doi: 10.1111/1462-2920.14568. Epub 2019 Mar 18.

DOI:10.1111/1462-2920.14568
PMID:30790413
Abstract

Anaerobic oxidation of methane greatly contributes to global carbon cycling, yet the anaerobic oxidation of non-methane alkanes by archaea was only recently detected in lab enrichments. The distribution and activity of these archaea in natural environments are not yet reported and understood. Here, a combination of metagenomic and metatranscriptomic approaches was utilized to understand the ecological roles and metabolic potentials of methyl-coenzyme M reductase (MCR)-based alkane oxidizing (MAO) archaea in Guaymas Basin sediments. Diverse MAO archaea, including multi-carbon alkane oxidizer Ca. Syntrophoarchaeum spp., anaerobic methane oxidizing archaea ANME-1 and ANME-2c as well as sulfate-reducing bacteria HotSeep-1 and Seep-SRB2 that potentially involved in MAO processes, coexisted and showed activity in Guaymas Basin sediments. High-quality genomic bins of Ca. Syntrophoarchaeum spp., ANME-1 and ANME-2c were retrieved. They all contain and expressed mcr genes and genes in Wood-Ljungdahl pathway for the complete oxidation from alkane to CO in local environment, while Ca. Syntrophoarchaeum spp. also possess beta-oxidation genes for multi-carbon alkane degradation. A global survey of potential multi-carbon alkane metabolism archaea shows that they are usually present in organic rich environments but are not limit to hydrothermal or marine ecosystems. Our study provided new insights into ecological and metabolic potentials of MAO archaea in natural environments.

摘要

甲烷的厌氧氧化对全球碳循环有重要贡献,但古菌对非甲烷烷烃的厌氧氧化直到最近才在实验室富集物中被检测到。这些古菌在自然环境中的分布和活性尚未得到报道和理解。在这里,我们结合宏基因组学和宏转录组学方法,以了解古菌甲基辅酶 M 还原酶(MCR)-依赖的烷烃氧化(MAO)在古马雅格斯盆地沉积物中的生态作用和代谢潜力。古菌中存在多种多样的 MAO 古菌,包括多碳烷烃氧化菌 Ca. Syntrophoarchaeum spp.、厌氧甲烷氧化古菌 ANME-1 和 ANME-2c 以及硫酸盐还原菌 HotSeep-1 和 Seep-SRB2,它们可能参与了 MAO 过程,在古马雅格斯盆地沉积物中共同存在并表现出活性。从古马雅格斯盆地沉积物中获得了 Ca. Syntrophoarchaeum spp.、ANME-1 和 ANME-2c 的高质量基因组框。它们都包含并表达 mcr 基因和 Wood-Ljungdahl 途径中的基因,用于将烷烃完全氧化为当地环境中的 CO,而 Ca. Syntrophoarchaeum spp. 还具有多碳烷烃降解的β-氧化基因。对潜在的多碳烷烃代谢古菌的全球调查表明,它们通常存在于富含有机物的环境中,但不限于热液或海洋生态系统。我们的研究为自然环境中 MAO 古菌的生态和代谢潜力提供了新的见解。

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