Behaviours of methane metabolism and community dynamics of methane anaerobic oxidation microbes on carbonate rocks with long-term cultivation in cold seep environment

被引:0
|
作者
Li, Cun [1 ,2 ,3 ,4 ,5 ]
Feng, Jing-Chun [1 ,2 ,5 ]
Chen, Xiao [1 ]
Zhou, Yingli [1 ]
Liang, Jianzhen [2 ,5 ]
Zhang, Si [1 ,2 ,4 ]
机构
[1] Southern Marine Sci & Engn Guangdong Lab Guangzhou, Guangzhou 511458, Peoples R China
[2] Guangdong Univ Technol, Inst Environm & Ecol Engn, Guangdong Prov Key Lab Water Qual Improvement & Ec, Guangzhou 510006, Peoples R China
[3] Univ Chinese Acad Sci, Beijing 100049, Peoples R China
[4] Chinese Acad Sci, South China Sea Inst Oceanol, Guangzhou 510301, Peoples R China
[5] Guangdong Basic Res Ctr Excellence Ecol Secur & Gr, Guangzhou 510006, Peoples R China
基金
中国国家自然科学基金;
关键词
Cold seep; Methane mitigation; Anaerobic oxidation of methane; Carbonate; Prokaryotic communities; AUTHIGENIC CARBONATE; MARINE BACTERIUM; HYDRATE RIDGE; GEN; NOV; SEDIMENTS; DISSOLUTION; SEA; BIOMINERALIZATION; TEMPERATURE; GENOMES;
D O I
10.1016/j.apenergy.2024.123296
中图分类号
TE [石油、天然气工业]; TK [能源与动力工程];
学科分类号
0807 ; 0820 ;
摘要
The anaerobic oxidation of methane (AOM) and sulfate reduction processes in cold seep environments can control methane emission sources and thus mitigate the pressure of increasing global greenhouse gas concentrations. The surfaces of carbonate rocks in cold seep host an abundance of microorganisms that participate in AOM reactions. Investigating the metabolism and conversion of methane by these microbes is instrumental in advancing the exploration and utilization of deep-sea methane energy. Previous studies primarily focused on insitu investigations of microbial communities on carbonate rocks in cold seep environments, while the dynamic balance of carbonate mineralization caused by microbial community changes and the characteristics of methane consumption in carbonate samples remains unclear. In this study, we used methane as the sole carbon source, enriched and cultured carbonate samples under high pressure, and monitored the community dynamics regularly. The results demonstrated that methane consumption and metabolic pathways played a crucial role in influencing community succession and carbonate mineralization. AOM processes, coupled with sulfate reduction and nitrate reduction, which are dominated by ANME-2c, facilitate the precipitation of calcium carbonate. Conversely, the acetate production process, dominated by ANME-1, may hinder the efficiency of calcium carbonate mineralization. Additionally, the impact of bacterial groups in the enrichment process, through the production of extracellular enzymes, organic acid pathways, and the expression of carbonic anhydrase pathways on carbonate mineralization, should not be disregarded. These findings highlight the significance of diverse pathway methane metabolism in the dynamics of methane consumption, deep-sea microbial communities, carbonate kinetics, and marine biological carbon sequestration processes.
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页数:10
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