Wenwen Huang, Yi Tang, Mengchen Lu, Zhenzhen Peng, Shubing Li, Xunsen Chen, Fangrong Wei, Teng Guo, JinShao Ye, Yan Long
{"title":"环境依赖的甲烷厌氧氧化:对甲烷排放减缓的见解","authors":"Wenwen Huang, Yi Tang, Mengchen Lu, Zhenzhen Peng, Shubing Li, Xunsen Chen, Fangrong Wei, Teng Guo, JinShao Ye, Yan Long","doi":"10.1016/j.jenvman.2025.125896","DOIUrl":null,"url":null,"abstract":"<div><div>Anaerobic oxidation of methane (AOM) exhibits context-dependent metabolic versatility, governed by electron acceptor heterogeneity and anthropogenic perturbations. This study investigates the AOM potential by simulating three environments, high-dissolved organic carbon (DOC), high-nitrate with moderate sulfate, and sulfate-enhanced conditions, to investigate AOM potential under controlled perturbations. Substrate conversion dynamics were observed by monitoring the variation of methane, sulfate, nitrate, iron, etc., and microbial community shifts were analyzed by 16S rDNA high-throughput sequencing. In the high-carbon condition, characterized by high DOC (5.65–21.83 mmolC·L<sup>−1</sup>) but low nitrate and sulfate (both <1 mmol L<sup>−1</sup>) levels, methanogens such as <em>Methanobacterium</em> sp. IM1 and <em>Thermoplasmata</em> dominated the stage, overpowering anaerobic methanotrophic archaea (ANME), while no methane oxidation but obvious methane production occurred. Shifting to the scenario with high nitrate (3.51 mmolN·L<sup>−1</sup>) and moderate sulfate (1.36 mmolS·L<sup>−1</sup>), ammonium accumulation played the role of a spoiler. It weakened AOM process (K<sub>mo</sub> = 0.58 d<sup>−1</sup>) and stirred up a competitive relationship between sulfur-driven ammonium-oxidizing archaea (e.g., <em>Nitrososphaeraceae</em>, <em>Nitrosotaleaceae</em>) and methanotrophs (e.g., Marine group II, <em>Wosearchaeales</em>, <em>Roseiarcus</em>). However, once nitrate was consumed to a low level, sulfate reduction relieved the ammonium pressure and re-activated iron, the suppression of AOM eased (K<sub>mo</sub> = 1.44 d<sup>−1</sup>). Under the sulfate-enhanced circumstances, where the sulfate level increased to 1.47–2.55 mmolS·L<sup>−1</sup>, the AOM process accelerated (K<sub>mo</sub> = 4.02 d<sup>−1</sup>) even under high-nitrate conditions (1.66 ± 0.12 mmolN·L<sup>−1</sup>). Methanotrophs and sulfur-metabolizing bacteria then co-thrived, showing a close display of cooperation. Our findings offer a pivotal framework to clarify AOM's contribution to natural methane emissions and give a new perspective for the development of methane mitigation technologies.</div></div>","PeriodicalId":356,"journal":{"name":"Journal of Environmental Management","volume":"387 ","pages":"Article 125896"},"PeriodicalIF":8.0000,"publicationDate":"2025-05-23","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Context-dependent anaerobic oxidation of methane: Insight for methane emission mitigation\",\"authors\":\"Wenwen Huang, Yi Tang, Mengchen Lu, Zhenzhen Peng, Shubing Li, Xunsen Chen, Fangrong Wei, Teng Guo, JinShao Ye, Yan Long\",\"doi\":\"10.1016/j.jenvman.2025.125896\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><div>Anaerobic oxidation of methane (AOM) exhibits context-dependent metabolic versatility, governed by electron acceptor heterogeneity and anthropogenic perturbations. This study investigates the AOM potential by simulating three environments, high-dissolved organic carbon (DOC), high-nitrate with moderate sulfate, and sulfate-enhanced conditions, to investigate AOM potential under controlled perturbations. Substrate conversion dynamics were observed by monitoring the variation of methane, sulfate, nitrate, iron, etc., and microbial community shifts were analyzed by 16S rDNA high-throughput sequencing. In the high-carbon condition, characterized by high DOC (5.65–21.83 mmolC·L<sup>−1</sup>) but low nitrate and sulfate (both <1 mmol L<sup>−1</sup>) levels, methanogens such as <em>Methanobacterium</em> sp. IM1 and <em>Thermoplasmata</em> dominated the stage, overpowering anaerobic methanotrophic archaea (ANME), while no methane oxidation but obvious methane production occurred. Shifting to the scenario with high nitrate (3.51 mmolN·L<sup>−1</sup>) and moderate sulfate (1.36 mmolS·L<sup>−1</sup>), ammonium accumulation played the role of a spoiler. It weakened AOM process (K<sub>mo</sub> = 0.58 d<sup>−1</sup>) and stirred up a competitive relationship between sulfur-driven ammonium-oxidizing archaea (e.g., <em>Nitrososphaeraceae</em>, <em>Nitrosotaleaceae</em>) and methanotrophs (e.g., Marine group II, <em>Wosearchaeales</em>, <em>Roseiarcus</em>). However, once nitrate was consumed to a low level, sulfate reduction relieved the ammonium pressure and re-activated iron, the suppression of AOM eased (K<sub>mo</sub> = 1.44 d<sup>−1</sup>). Under the sulfate-enhanced circumstances, where the sulfate level increased to 1.47–2.55 mmolS·L<sup>−1</sup>, the AOM process accelerated (K<sub>mo</sub> = 4.02 d<sup>−1</sup>) even under high-nitrate conditions (1.66 ± 0.12 mmolN·L<sup>−1</sup>). Methanotrophs and sulfur-metabolizing bacteria then co-thrived, showing a close display of cooperation. Our findings offer a pivotal framework to clarify AOM's contribution to natural methane emissions and give a new perspective for the development of methane mitigation technologies.</div></div>\",\"PeriodicalId\":356,\"journal\":{\"name\":\"Journal of Environmental Management\",\"volume\":\"387 \",\"pages\":\"Article 125896\"},\"PeriodicalIF\":8.0000,\"publicationDate\":\"2025-05-23\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Journal of Environmental Management\",\"FirstCategoryId\":\"93\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S0301479725018729\",\"RegionNum\":2,\"RegionCategory\":\"环境科学与生态学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q1\",\"JCRName\":\"ENVIRONMENTAL SCIENCES\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of Environmental Management","FirstCategoryId":"93","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0301479725018729","RegionNum":2,"RegionCategory":"环境科学与生态学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"ENVIRONMENTAL SCIENCES","Score":null,"Total":0}
Context-dependent anaerobic oxidation of methane: Insight for methane emission mitigation
Anaerobic oxidation of methane (AOM) exhibits context-dependent metabolic versatility, governed by electron acceptor heterogeneity and anthropogenic perturbations. This study investigates the AOM potential by simulating three environments, high-dissolved organic carbon (DOC), high-nitrate with moderate sulfate, and sulfate-enhanced conditions, to investigate AOM potential under controlled perturbations. Substrate conversion dynamics were observed by monitoring the variation of methane, sulfate, nitrate, iron, etc., and microbial community shifts were analyzed by 16S rDNA high-throughput sequencing. In the high-carbon condition, characterized by high DOC (5.65–21.83 mmolC·L−1) but low nitrate and sulfate (both <1 mmol L−1) levels, methanogens such as Methanobacterium sp. IM1 and Thermoplasmata dominated the stage, overpowering anaerobic methanotrophic archaea (ANME), while no methane oxidation but obvious methane production occurred. Shifting to the scenario with high nitrate (3.51 mmolN·L−1) and moderate sulfate (1.36 mmolS·L−1), ammonium accumulation played the role of a spoiler. It weakened AOM process (Kmo = 0.58 d−1) and stirred up a competitive relationship between sulfur-driven ammonium-oxidizing archaea (e.g., Nitrososphaeraceae, Nitrosotaleaceae) and methanotrophs (e.g., Marine group II, Wosearchaeales, Roseiarcus). However, once nitrate was consumed to a low level, sulfate reduction relieved the ammonium pressure and re-activated iron, the suppression of AOM eased (Kmo = 1.44 d−1). Under the sulfate-enhanced circumstances, where the sulfate level increased to 1.47–2.55 mmolS·L−1, the AOM process accelerated (Kmo = 4.02 d−1) even under high-nitrate conditions (1.66 ± 0.12 mmolN·L−1). Methanotrophs and sulfur-metabolizing bacteria then co-thrived, showing a close display of cooperation. Our findings offer a pivotal framework to clarify AOM's contribution to natural methane emissions and give a new perspective for the development of methane mitigation technologies.
期刊介绍:
The Journal of Environmental Management is a journal for the publication of peer reviewed, original research for all aspects of management and the managed use of the environment, both natural and man-made.Critical review articles are also welcome; submission of these is strongly encouraged.