Towards an integrated view on microbial CH4, N2O and N2 cycles in brackish coastal marsh soils: A comparative analysis of two sites

被引:9
作者
Espenberg, Mikk [1 ,2 ]
Pille, Kristin [1 ]
Yang, Bin [3 ]
Maddison, Martin [1 ]
Abdalla, Mohamed [2 ]
Smith, Pete [2 ]
Li, Xiuzhen [3 ]
Chan, Ping-Lung [4 ]
Mander, Uelo [1 ]
机构
[1] Univ Tartu, Inst Ecol & Earth Sci, Tartu, Estonia
[2] Univ Aberdeen, Inst Biol & Environm Sci, Aberdeen, Scotland
[3] East China Normal Univ, Inst Ecochongming, State Key Lab Estuarine & Coastal Res, Shanghai, Peoples R China
[4] Hong Kong Metropolitan Univ, Sch Sci & Technol, Hong Kong, Peoples R China
基金
中国国家自然科学基金;
关键词
Carbon cycle; Nitrogen cycle; Coastal ecosystems; Nitrous oxide; Methane; Greenhouse gases; ANAEROBIC METHANE OXIDATION; SPARTINA-ALTERNIFLORA; CLIMATE-CHANGE; NITROUS-OXIDE; EMISSIONS; BACTERIA; NITRATE; DENITRIFICATION; EUTROPHICATION; NITRIFICATION;
D O I
10.1016/j.scitotenv.2024.170641
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Coastal ecosystems, facing threats from global change and human activities like excessive nutrients, undergo alterations impacting their function and appearance. This study explores the intertwined microbial cycles of carbon (C) and nitrogen (N), encompassing methane (CH4), nitrous oxide (N2O), and nitrogen gas (N2) fluxes, to determine nutrient transformation processes between the soil -plant -atmosphere continuum in the coastal ecosystems with brackish water. Water salinity negatively impacted denitrification, bacterial nitrification, N fixation, and n-DAMO processes, but did not significantly affect archaeal nitrification, COMAMMOX, DNRA, and ANAMMOX processes in the N cycle. Plant species age and biomass influenced CH4 and N2O emissions. The highest CH4 emissions were from old Spartina and mixed Spartina and Scirpus sites, while Phragmites sites emitted the most N2O. Nitrification and incomplete denitrification mainly governed N2O emissions depending on the environmental conditions and plants. The higher genetic potential of ANAMMOX reduced excessive N by converting it to N2 in the sites with higher average temperatures. The presence of plants led to a decrease in the N fixers' abundance. Plant biomass negatively affected methanogenetic mcrA genes. Microbes involved in n-DAMO processes helped mitigate CH4 emissions. Over 93 % of the total climate forcing came from CH4 emissions, except for the Chinese bare site where the climate forcing was negative, and for Phragmites sites, where almost 60 % of the climate forcing came from N2O emissions. Our findings indicate that nutrient cycles, CH4, and N2O fluxes in soils are context -dependent and influenced by environmental factors and vegetation. This underscores the need for empirical analysis of both C and N cycles at various levels (soil -plant -atmosphere) to understand how habitats or plants affect nutrient cycles and greenhouse gas emissions.
引用
收藏
页数:12
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