School of Environmental Science and Engineering, Nanjing University of Information Science and Technology, Nanjing 210044, China; Key Laboratory of Ecosystem Carbon Source and Sink, China Meteorological Administration (ECSS-CMA), School of Ecology and Applied Meteorology, Nanjing University of Information Science and Technology, Nanjing 210044, China.
Key Laboratory of Ecosystem Carbon Source and Sink, China Meteorological Administration (ECSS-CMA), School of Ecology and Applied Meteorology, Nanjing University of Information Science and Technology, Nanjing 210044, China.
Sci Total Environ. 2024 Jul 1;932:173134. doi: 10.1016/j.scitotenv.2024.173134. Epub 2024 May 9.
Methane (CH) is a potent greenhouse gas, with lake ecosystems significantly contributing to its global emissions. Denitrifying anaerobic methane oxidation (DAMO) process, mediated by NC10 bacteria and ANME-2d archaea, links global carbon and nitrogen cycles. However, their potential roles in mitigating methane emissions and removing nitrogen from lake ecosystems remain unclear. This study explored the spatial variations in activities of nitrite- and nitrate-DAMO and their functional microbes in Changdanghu Lake sediments (Jiangsu Province, China). The results showed that although the average abundance of ANME-2d archaea (5.0 × 10 copies g) was significantly higher than that of NC10 bacteria (2.1 × 10 copies g), the average potential rates of nitrite-DAMO (4.59 nmol CO g d) and nitrate-DAMO (5.01 nmol CO g d) showed no significant difference across all sampling sites. It is estimated that nitrite- and nitrate-DAMO consumed approximately 6.46 and 7.05 mg CH m d, respectively, which accordingly achieved 15.07-24.95 mg m d nitrogen removal from the studied lake sediments. Statistical analyses found that nitrite- and nitrate-DAMO activities were both significantly related to sediment nitrate contents and ANME-2d archaeal abundance. In addition, NC10 bacterial and ANME-2d archaeal community compositions showed significant correlations with sediment organic carbon content and water depth. Overall, this study underscores the dual roles of nitrite- and nitrate-DAMO processes in CH mitigation and nitrogen elimination and their key environmental impact factors (sediment organic carbon and inorganic nitrogen contents, and water depth) in shallow lake, enhancing the understanding of carbon and nitrogen cycles in freshwater aquatic ecosystems.
甲烷(CH)是一种强效温室气体,湖泊生态系统对其全球排放有重大贡献。由 NC10 细菌和 ANME-2d 古菌介导的反硝化厌氧甲烷氧化(DAMO)过程将全球碳氮循环联系起来。然而,它们在减轻甲烷排放和从湖泊生态系统中去除氮方面的潜在作用尚不清楚。本研究探讨了中国江苏省长荡湖沉积物中硝酸盐-DAMO 和亚硝酸盐-DAMO 及其功能微生物活性的空间变化。结果表明,尽管 ANME-2d 古菌(5.0×10 拷贝 g)的平均丰度明显高于 NC10 细菌(2.1×10 拷贝 g),但所有采样点的硝酸盐-DAMO(5.01 nmol CO g d)和亚硝酸盐-DAMO(4.59 nmol CO g d)的平均潜在速率没有显著差异。估计硝酸盐-DAMO 和亚硝酸盐-DAMO 分别消耗了约 6.46 和 7.05 mg CH m d,相应地从研究的湖底沉积物中去除了 15.07-24.95 mg m d 的氮。统计分析发现,硝酸盐-DAMO 和亚硝酸盐-DAMO 活性均与沉积物硝酸盐含量和 ANME-2d 古菌丰度显著相关。此外,NC10 细菌和 ANME-2d 古菌群落组成与沉积物有机碳含量和水深呈显著相关。总的来说,本研究强调了硝酸盐-DAMO 和亚硝酸盐-DAMO 过程在 CH 减排和氮去除中的双重作用及其在浅水湖泊中的关键环境影响因素(沉积物有机碳和无机氮含量以及水深),增强了对淡水水生生态系统碳氮循环的理解。