Your browser doesn't support javascript.
loading
Towards an integrated view on microbial CH4, N2O and N2 cycles in brackish coastal marsh soils: A comparative analysis of two sites.
Espenberg, Mikk; Pille, Kristin; Yang, Bin; Maddison, Martin; Abdalla, Mohamed; Smith, Pete; Li, Xiuzhen; Chan, Ping-Lung; Mander, Ülo.
Afiliación
  • Espenberg M; Institute of Ecology and Earth Sciences, University of Tartu, Tartu, Estonia; Institute of Biological and Environmental Sciences, University of Aberdeen, Aberdeen, United Kingdom. Electronic address: mikk.espenberg@ut.ee.
  • Pille K; Institute of Ecology and Earth Sciences, University of Tartu, Tartu, Estonia.
  • Yang B; State Key Laboratory of Estuarine and Coastal Research, Institute of Eco-Chongming, East China Normal University, Shanghai, China.
  • Maddison M; Institute of Ecology and Earth Sciences, University of Tartu, Tartu, Estonia.
  • Abdalla M; Institute of Biological and Environmental Sciences, University of Aberdeen, Aberdeen, United Kingdom.
  • Smith P; Institute of Biological and Environmental Sciences, University of Aberdeen, Aberdeen, United Kingdom.
  • Li X; State Key Laboratory of Estuarine and Coastal Research, Institute of Eco-Chongming, East China Normal University, Shanghai, China.
  • Chan PL; School of Science and Technology, Hong Kong Metropolitan University, Hong Kong, China.
  • Mander Ü; Institute of Ecology and Earth Sciences, University of Tartu, Tartu, Estonia.
Sci Total Environ ; 918: 170641, 2024 Mar 25.
Article en En | MEDLINE | ID: mdl-38325442
ABSTRACT
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.
Asunto(s)
Palabras clave

Texto completo: 1 Colección: 01-internacional Banco de datos: MEDLINE Asunto principal: Suelo / Humedales Límite: Humans Idioma: En Revista: Sci Total Environ Año: 2024 Tipo del documento: Article

Texto completo: 1 Colección: 01-internacional Banco de datos: MEDLINE Asunto principal: Suelo / Humedales Límite: Humans Idioma: En Revista: Sci Total Environ Año: 2024 Tipo del documento: Article