Spatio-temporal variations of activity of nitrate-driven anaerobic oxidation of methane and community structure of Candidatus Methanoperedens-like archaea in sediment of Wuxijiang river

被引:4
|
作者
Cheng, Haixiang [1 ]
Yang, Yuling [2 ]
He, Yefan [2 ]
Zhan, Xugang [3 ]
Liu, Yan [4 ]
Hu, Zhengfeng [5 ]
Huang, Hechen [2 ]
Yao, Xiaochen [2 ]
Yang, Wangting [2 ]
Jin, Jinghao [2 ]
Ren, Bingjie [2 ]
Liu, Jiaqi [2 ]
Hu, Qinan [2 ]
Jin, Yuhan [2 ]
Shen, Lidong [2 ]
机构
[1] Quzhou Univ, Coll Chem & Mat Engn, Quzhou 324000, Peoples R China
[2] Nanjing Univ Informat Sci & Technol, Sch Appl Meteorol, Inst Ecol, Nanjing 210044, Peoples R China
[3] Quzhou Bur Ecol & Environm, Quzhou 324000, Peoples R China
[4] Wuxi River Drinking Water Source Protect & Managem, Quzhou 324000, Peoples R China
[5] Ecoenvironm Sci Res & Design Inst Zhejiang Prov, Hangzhou 310007, Peoples R China
基金
中国国家自然科学基金;
关键词
Methanoperedens-like archaea; CH4; mitigation; Riverine system; Temperature; NH4+content; Organic carbon content; CARBON; METHANOTROPHY; REDUCTION; NITRITE;
D O I
10.1016/j.chemosphere.2023.138295
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Nitrate-driven anaerobic oxidation of methane (AOM), catalyzing by Candidatus Methanoperedens-like archaea, is a new addition in the global CH4 cycle. This AOM process acts as a novel pathway for CH4 emission reduction in freshwater aquatic ecosystems; however, its quantitative importance and regulatory factors in riverine eco-systems are nearly unknown. Here, we examined the spatio-temporal changes of the communities of Meth-anoperedens-like archaea and nitrate-driven AOM activity in sediment of Wuxijiang River, a mountainous river in China. These archaeal community composition varied significantly among reaches (upper, middle, and lower reaches) and between seasons (winter and summer), but their mcrA gene diversity showed no significant spatial or temporal variations. The copy numbers of Methanoperedens-like archaeal mcrA genes were 1.32 x 105-2.47 x 107 copies g- 1 (dry weight), and the activity of nitrate-driven AOM was 0.25-1.73 nmol CH4 g-1 (dry weight) d-1, which could potentially reduce 10.3% of CH4 emissions from rivers. Significant spatio-temporal variations of
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页数:11
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