NO3− is an important driver of nitrite-dependent anaerobic methane oxidation bacteria and CH4 fluxes in the reservoir riparian zone

Song, Shuang; Wang, Xiaoyan; Wang, Yubing; Li, Tingting; Huang, Jiung-Yao

doi:10.1007/s11356-021-16914-8

Cited by 9 publications

(1 citation statement)

References 50 publications

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“…Here, NO 3 − also influenced CH 4 uptake. The relative abundance of Methylomirabilaceae, which carry out nitritedependent anaerobic methane oxidation using CH 4 as an external C source and NO 3 − or NO 2 − as electron acceptors (Song et al 2022), was significantly higher in BB than in the other agroforestry systems.…”

Section: Relationship Among Ghgs Fluxes and Environmental Factors Und...mentioning

confidence: 93%

Agroforestry alters the fluxes of greenhouse gases of Moso bamboo plantation soil

Shi

Zhang

et al. 2022

Environ. Res. Lett.

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Agroforestry systems are widely applied in China and have both economic and ecological benefits. However, relatively few prior studies have investigated the relative ecological benefits of various agroforestry systems. In the present study, the static chamber method, qPCR, and high throughput sequencing were used to establish the differences in greenhouse gases (GHGs) fluxes and explore the bacterial and fungal populations affecting GHGs fluxes under different agroforestry systems, including pure Moso bamboo forest (CK), bamboo+Bletilla striata (BB), bamboo+Dictyophora indusiata (BD), and bamboo+chickens (BC). The highest cumulative CH4 uptake and N2O emission in spring occurred in BB while the highest cumulative CO2 emission and GWP in spring occurred in BC. The Methylomirabilaceae were the key methanotrophs influencing the comparative differences in NO3--associated CH4 uptake among the various agroforestry systems. N2O emission was associated with pH, and nitrifiers such as the ammonia-oxidizing archaea (AOA) and bacteria (AOB) (Nitrospiraceae and Nitrosomonadaceae) rather than denitrifiers may be the key microbes affecting N2O emission in different agroforestry systems. The bacteria Actinobacteriota and Fibrobacteres and the fungi Ascomycetes and Basidiomycota were the primary microbial taxa influencing CO2 emission. The lignin-decomposing Basidiomycota played more important roles in CO2 emission than the cellulose-decomposing fungi and bacteria under the various agroforestry systems. CO2 emission was positively correlated with NO3- in the bacterial community and was negatively correlated with NO3- in the fungal community, implying two C decomposition mechanisms caused by denitrification dominated in bacteria and those caused by microbial nitrogen mining dominated in fungi. The foregoing results suggested that bamboo+B. striata had comparatively higher ecological benefits as it is associated with low GWP and external C fixation. The present study provided valuable information for screening bamboo-based agroforestry systems with high ecological benefits. It also elucidated the microbial mechanism explaining the observed differences in GHGs fluxes between the various agroforestry systems.

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Section: Relationship Among Ghgs Fluxes and Environmental Factors Und...mentioning

confidence: 93%

Agroforestry alters the fluxes of greenhouse gases of Moso bamboo plantation soil

Shi

Zhang

et al. 2022

Environ. Res. Lett.

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Mechanisms Driving the Distribution and Activity of Mineralization and Nitrification in the Reservoir Riparian Zone

Wang²,

Wang³

et al. 2023

Microb Ecol

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Seasonal variations in dissolved CH4 and its controlling factors in two subtropical eutrophic reservoirs in China

Yue

2022

Arab J Geosci

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NO3− is an important driver of nitrite-dependent anaerobic methane oxidation bacteria and CH4 fluxes in the reservoir riparian zone

Cited by 9 publications

References 50 publications

Agroforestry alters the fluxes of greenhouse gases of Moso bamboo plantation soil

Agroforestry alters the fluxes of greenhouse gases of Moso bamboo plantation soil

Mechanisms Driving the Distribution and Activity of Mineralization and Nitrification in the Reservoir Riparian Zone

Seasonal variations in dissolved CH4 and its controlling factors in two subtropical eutrophic reservoirs in China

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