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

dc.contributor.authorEspenberg, Mikk
dc.contributor.authorPille, Kristin
dc.contributor.authorYang, Bin
dc.contributor.authorMaddison, Martin
dc.contributor.authorAbdalla, Mohamed
dc.contributor.authorSmith, Pete
dc.contributor.authorLi, Xiuzhen
dc.contributor.authorChan, Ping-Lung
dc.contributor.authorMander, Ülo
dc.date.accessioned2026-04-09T08:17:18Z
dc.date.available2026-04-09T08:17:18Z
dc.date.issued2024
dc.description.abstractCoastal 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.
dc.identifier.urihttps://doi.org/10.1016/j.scitotenv.2024.170641
dc.identifier.urihttps://hdl.handle.net/10062/120176
dc.language.isoen
dc.publisherScience of The Total Environment
dc.relationinfo:eu-repo/grantAgreement/EC/HORIZON.4.1.2/101079192///LiWeFor
dc.rightsinfo:eu-repo/semantics/openAccess
dc.rights.urihttps://creativecommons.org/licenses/by-nc-nd/4.0/
dc.subjectCarbon cycle
dc.subjectNitrogen cycle
dc.subjectCoastal ecosystems
dc.subjectNitrous oxide
dc.subjectMethane
dc.subjectGreenhouse gases
dc.titleTowards an integrated view on microbial CH4, N2O and N2 cycles in brackish coastal marsh soils: A comparative analysis of two sites
dc.typeinfo:eu-repo/semantics/article

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