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来自一个废弃太阳能盐场的新型嗜盐甲烷八叠球菌科宏基因组组装基因组的产甲烷作用和耐盐基因

Methanogenesis and Salt Tolerance Genes of a Novel Halophilic Methanosarcinaceae Metagenome-Assembled Genome from a Former Solar Saltern.

作者信息

Bueno de Mesquita Clifton P, Zhou Jinglie, Theroux Susanna M, Tringe Susannah G

机构信息

Department of Energy, Joint Genome Institute, Lawrence Berkeley National Laboratory, Berkeley, CA 94720, USA.

Southern California Coastal Water Research Project, Costa Mesa, CA 92626, USA.

出版信息

Genes (Basel). 2021 Oct 13;12(10):1609. doi: 10.3390/genes12101609.

DOI:10.3390/genes12101609
PMID:34681003
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC8535929/
Abstract

Anaerobic archaeal methanogens are key players in the global carbon cycle due to their role in the final stages of organic matter decomposition in anaerobic environments such as wetland sediments. Here we present the first draft metagenome-assembled genome (MAG) sequence of an unclassified Methanosarcinaceae methanogen phylogenetically placed adjacent to the and genera that appears to be a distinct genus and species. The genome is derived from sediments of a hypersaline (97-148 ppt chloride) unrestored industrial saltern that has been observed to be a significant methane source. The source sediment is more saline than previous sources of and . We propose a new genus name, , to house this genome, which we designate with the strain name SBSPR1A. The MAG was binned with CONCOCT and then improved via scaffold extension and reassembly. The genome contains pathways for methylotrophic methanogenesis from trimethylamine and dimethylamine, as well as genes for the synthesis and transport of compatible solutes. Some genes involved in acetoclastic and hydrogenotrophic methanogenesis are present, but those pathways appear incomplete in the genome. The MAG was more abundant in two former industrial salterns than in a nearby reference wetland and a restored wetland, both of which have much lower salinity levels, as well as significantly lower methane emissions than the salterns.

摘要

厌氧古菌产甲烷菌是全球碳循环中的关键参与者,因为它们在湿地沉积物等厌氧环境中有机物分解的最后阶段发挥作用。在这里,我们展示了一种未分类的甲烷八叠球菌科产甲烷菌的首个宏基因组组装基因组(MAG)序列草图,该产甲烷菌在系统发育上与[具体属名1]和[具体属名2]属相邻,似乎是一个独特的属和种。该基因组源自一个高盐(氯化物含量为97 - 148 ppt)且未修复的工业盐田沉积物,该盐田已被观测到是一个重要的甲烷源。源沉积物的盐度比之前[具体属名1]和[具体属名2]的来源更高。我们提议一个新的属名[新属名]来容纳这个基因组,我们将其命名为菌株SBSPR1A。该MAG通过CONCOCT进行分箱,然后通过支架扩展和重新组装得到改进。该基因组包含从三甲胺和二甲胺进行甲基营养型产甲烷的途径,以及相容性溶质的合成和运输基因。存在一些参与乙酸裂解型和氢营养型产甲烷的基因,但这些途径在基因组中似乎不完整。该MAG在两个 former industrial salterns 中比在附近一个参考湿地和一个修复湿地中更为丰富,后两者的盐度水平要低得多,甲烷排放量也明显低于盐田。 (注:原文中“former industrial salterns”表述不太准确,推测可能是“former industrial salt pans”之类意思更准确,但按要求未做修改。)

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/4360/8535929/b5486243d10f/genes-12-01609-g005.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/4360/8535929/34cc54703f20/genes-12-01609-g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/4360/8535929/4114b8bca462/genes-12-01609-g002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/4360/8535929/de6eec12f652/genes-12-01609-g003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/4360/8535929/a374f59a8744/genes-12-01609-g004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/4360/8535929/b5486243d10f/genes-12-01609-g005.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/4360/8535929/34cc54703f20/genes-12-01609-g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/4360/8535929/4114b8bca462/genes-12-01609-g002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/4360/8535929/de6eec12f652/genes-12-01609-g003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/4360/8535929/a374f59a8744/genes-12-01609-g004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/4360/8535929/b5486243d10f/genes-12-01609-g005.jpg

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