Contribution of periphytic biofilm of paddy soils to carbon dioxide fixation and methane emissions

Rice paddies are major contributors to anthropogenic greenhouse gas emissions via methane (CH) flux. The accurate quantification of CH emissions from rice paddies remains problematic, in part due to uncertainties and omissions in the contribution of microbial aggregates on the soil surface to carbon...

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Detalles Bibliográficos
Autores: Wang, Sichu, Sun, Pengfei, Zhang, Guangbin, Gray, Neil, Dolfing, Jan, Esquivel-Elizondo, Sofia, Peñuelas, Josep|||0000-0002-7215-0150, Wu, Yonghong
Tipo de recurso: artículo
Fecha de publicación:2022
País:España
Institución:Universitat Autònoma de Barcelona
Repositorio:Dipòsit Digital de Documents de la UAB
Idioma:inglés
OAI Identifier:oai:ddd.uab.cat:250554
Acceso en línea:https://ddd.uab.cat/record/250554
https://dx.doi.org/urn:doi:10.1016/j.xinn.2021.100192
Access Level:acceso abierto
Palabra clave:Periphytic biofilm
Rice paddy
Greenhouse gas emissions
Carbon fluxes
Redox potential
Descripción
Sumario:Rice paddies are major contributors to anthropogenic greenhouse gas emissions via methane (CH) flux. The accurate quantification of CH emissions from rice paddies remains problematic, in part due to uncertainties and omissions in the contribution of microbial aggregates on the soil surface to carbon fluxes. Herein, we comprehensively evaluated the contribution of one form of microbial aggregates, periphytic biofilm (PB), to carbon dioxide (CO) and CH emissions from paddies distributed across three climatic zones, and quantified the pathways that drive net CH production as well as CO fixation. We found that PB accounted for 7.1%-38.5% of CH emissions and 7.2%-12.7% of CO fixation in the rice paddies. During their growth phase, PB fixed CO and increased the redox potential, which promoted aerobic CH oxidation. During the decay phase, PB degradation reduced redox potential and increased soil organic carbon availability, which promoted methanogenic microbial community growth and metabolism and increased CH emissions. Overall, PB acted as a biotic converter of atmospheric CO to CH, and aggravated carbon emissions by up to 2,318 kg CO equiv ha -1 season -1. Our results provide proof-of-concept evidence for the discrimination of the contributions of surface microbial aggregates (i.e., PB) from soil microbes, and a profound foundation for the estimation and simulation of carbon fluxes in a potential novel approach to the mitigation of CH emissions by manipulating PB growth.