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中国西南地区大型湖泊和水库中甲烷氧化菌群落与活性的垂直分布

Vertical profiles of community and activity of methanotrophs in large lake and reservoir of Southwest China.

作者信息

Wang Jiayi, Wu Debin, Wu Qiusheng, Chen Jingan, Zhao Yuan, Wang Heng, Liu Fukang, Yuan Quan

机构信息

State Key Laboratory of Environment Geochemistry, Institute of Geochemistry, Chinese Academy of Science, Guiyang 550081, China; University of Chinese Academy of Sciences, Beijing 100049, China.

State Key Laboratory of Environment Geochemistry, Institute of Geochemistry, Chinese Academy of Science, Guiyang 550081, China; Guizhou Province Field Scientific Observation and Research Station of Hongfeng Lake Reservoir Ecosystem, Guiyang 551499, China.

出版信息

Sci Total Environ. 2024 Dec 20;957:177782. doi: 10.1016/j.scitotenv.2024.177782. Epub 2024 Dec 2.

Abstract

Microbial methane oxidation plays a significant role in regulating methane emissions from lakes and reservoirs. However, the differences in methane oxidation activity and methanotrophic community between lakes and reservoirs remain inadequately characterized. In this study, sediment and water samples were collected from the large shallow lake (Dianchi) and deep reservoirs (Dongfeng and Hongjiadu) located in karst area, Southwest China. The results indicated that the rates of aerobic oxidation of methane (AeOM) in lake sediment ranged from 7.1 to 27.7 μg g d, which was higher than that in reservoirs sediment (1.92 to 11.56 μg g d). Similarly, the average AeOM in the water column of lake (104.7 μg L d) was much higher than that of reservoirs (46 μg L d). The content of sediment organic carbon and dissolved inorganic carbon were important factors that influenced the rates of AeOM in sediment and water column, respectively. 16S rRNA genes sequencing revealed a higher relative abundance of methanotrophs in lake sediments compared to reservoir sediments. The dominant methanotrophic taxa in lake was Methylococcaceae (type Ib), while Methylomonadaceae (type Ia) was predominant in reservoirs. Meanwhile, anaerobic methane-oxidizing microorganisms Candidatus Methylomirabilis and Candidatus Methanoperedens were also abundant in sediments of reservoirs. However, metatranscriptomic analysis revealed that the type I methanotrophs, especially Methylobacter, was most active in the sediment of both lake and reservoir. Water depth and conductivity could be the key controlling factors of the structures of methanotrophic communities in sediment and water column, respectively. Metagenome-assembled genomes suggested that type I methanotrophs exhibited greater motility, as evidenced by a higher number of flagellar assembly genes, while type II methanotrophs demonstrated advantages in metabolic processes such as carbon, phosphorus, and methane metabolism.

摘要

微生物甲烷氧化在调节湖泊和水库的甲烷排放中起着重要作用。然而,湖泊和水库之间甲烷氧化活性和甲烷营养群落的差异仍未得到充分表征。在本研究中,从中国西南部喀斯特地区的大型浅水湖泊(滇池)和深水水库(东风和洪家渡)采集了沉积物和水样。结果表明,湖泊沉积物中甲烷的好氧氧化速率(AeOM)范围为7.1至27.7μg g d,高于水库沉积物中的速率(1.92至11.56μg g d)。同样,湖泊水柱中的平均AeOM(104.7μg L d)远高于水库(46μg L d)。沉积物有机碳和溶解无机碳的含量分别是影响沉积物和水柱中AeOM速率的重要因素。16S rRNA基因测序显示,与水库沉积物相比,湖泊沉积物中甲烷营养菌的相对丰度更高。湖泊中占主导地位的甲烷营养分类群是甲基球菌科(Ib型),而甲基单胞菌科(Ia型)在水库中占主导地位。同时,厌氧甲烷氧化微生物“Candidatus Methylomirabilis”和“Candidatus Methanoperedens”在水库沉积物中也很丰富。然而,宏转录组分析表明,I型甲烷营养菌,尤其是甲基杆菌,在湖泊和水库的沉积物中最为活跃。水深和电导率可能分别是沉积物和水柱中甲烷营养群落结构的关键控制因素。宏基因组组装基因组表明,I型甲烷营养菌表现出更大的运动性,这通过更多的鞭毛组装基因得到证明,而II型甲烷营养菌在碳、磷和甲烷代谢等代谢过程中表现出优势。

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