Arbuscular mycorrhizal fungi (AMF) establish mutualistic relationships with the majority of terrestrial plants, increasing plant uptake of soil nitrogen (N) in exchange for photosynthates. And may influence soil ammonia (NH) volatilization and nitrous oxide (NO) emissions directly by improving plant N uptake, and/or indirectly by modifying soil bacterial community composition for the soil C availability increasing. However, the effects of AMF on soil NH volatilization and NO emissions and their underlying mechanisms remain unclear. We carried out two independent experiments using contrasting methods, one with a compartmental box device (in 2016) and the other with growth pot experiment (in 2020) to examine functional relationships between AMF and soil NH volatilization and NO emissions under varying N input. The presence of AMF significantly reduced soil NH volatilization and NO emissions while enhancing plant biomass and plant N acquisition, and reducing soil NH and NO, even with high N input. The presence of AMF also significantly reduced the relative abundance within the bacterial orders Sphingomonadales and Rhizobiales. Sphingomonadales correlated significantly and positively with soil NH volatilization in 2016 and NO emissions, whereas Rhizobiales correlated positively with soil NO emissions. High N input significantly increased soil NH volatilization and NO emissions with increasing relative abundance of Sphingomonadales and Rhizobiales. These findings demonstrate the contribution of AMF in regulating NH and NO emission by improving plant N uptake and altering soil bacterial communities. They also suggest that altering the rhizosphere microbiome might offer additional potential for restoration of N-enriched agroecosystems.
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http://dx.doi.org/10.1007/s00248-023-02172-3 | DOI Listing |
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