Arbuscular mycorrhiza has little influence on N2O potential emissions compared to plant diversity in experimental plant communities

Arbuscular Mycorrhizal Fungi Shift Soil Bacterial Community Composition and Reduce Soil Ammonia Volatilization and Nitrous Oxide Emissions

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 (NH₃) volatilization and nitrous oxide (N₂O) 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 NH₃ volatilization and N₂O 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 NH₃ volatilization and N₂O emissions under varying N input. The presence of AMF significantly reduced soil NH₃ volatilization and N₂O emissions while enhancing plant biomass and plant N acquisition, and reducing soil NH₄⁺ and NO₃^-, 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 NH₃ volatilization in 2016 and N₂O emissions, whereas Rhizobiales correlated positively with soil N₂O emissions. High N input significantly increased soil NH₃ volatilization and N₂O emissions with increasing relative abundance of Sphingomonadales and Rhizobiales. These findings demonstrate the contribution of AMF in regulating NH₃ and N₂O 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.

Arbuscular Mycorrhizae Shift Community Composition of N-Cycling Microbes and Suppress Soil N2O Emission

Mycorrhizae are ubiquitous symbiotic associations between arbuscular mycorrhizal fungi (AMF) and terrestrial plants, in which AMF receive photosynthates from and acquire soil nutrients for their host plants. Plant uptake of soil nitrogen (N) reduces N substrate for microbial processes that generate nitrous oxide (N₂O), a potent greenhouse gas. However, the underlying microbial mechanisms remain poorly understood, particularly in agroecosystems with high reactive N inputs. We examined how plant roots and AMF affect N₂O emissions, N₂O-producing (nirK and nirS) and N₂O-consuming (nosZ) microbes under normal and high N inputs in conventional (CONV) and organically managed (OM) soils. Here, we show that high N input increased soil N₂O emissions and the ratio of nirK to nirS microbes. Roots and AMF did not affect the (nirK + nirS)/nosZ ratio but significantly reduced N₂O emissions and the nirK/nirS ratio. They reduced the nirK/nirS ratio by reducing nirK-Rhodobacterales but increasing nirS-Rhodocyclales in the CONV soil while decreasing nirK-Burkholderiales but increasing nirS-Rhizobiales in the OM soil. Our results indicate that plant roots and AMF reduced N₂O emission directly by reducing soil N and indirectly through shifting the community composition of N₂O-producing microbes in N-enriched agroecosystems, suggesting that harnessing the rhizosphere microbiome through agricultural management might offer additional potential for N₂O emission mitigation.

Plants are a natural source of nitrous oxide even in field conditions as explained by 15N site preference

Plants are either recognized to produce nitrous oxide (N₂O) or considered as a medium to transport soil-produced N₂O. To date, it is not clear whether in their habitat plants conduit N₂O produced in soil or are a natural source. We aimed to understand role of plants in N₂O emissions in field conditions. Therefore, rubber plants (Ficus elastica) were planted in the field; then plant and soil chambers were deployed simultaneously to collect gas samples, and ¹⁵N site preference (SP) of N₂O was evaluated. The mean SP values of plant and soil emitted N₂O were -20.85 ± 2.8‰ and -8.85 ± 1.08‰, respectively, and were significantly different (p < 0.0001); while bulk ¹⁵N of plant and soil emitted N₂O were -10.83 ± 3.33‰ and -22.56 ± 3.37‰, respectively and were similar (p = 0.06). In the current study, soil always acted as a source of N₂O, while plants were both source and sink. Plant and soil N₂O fluxes had significant positive exponential relationship with both soil and air temperature. Soil water-filled pore space (WFPS) had significant negative linear relationship with only soil N₂O fluxes. Plant N₂O fluxes had significant positive linear relationship with plant respiration rates and negative linear relationship with plant surface areas. Based on the relationship between plant respiration rates and N₂O fluxes, we suggest that mitochondria are the possible sites of N₂O formation in plant cells while the relationship between plant surface areas and N₂O fluxes suggests that roots are the parts of its formation in natural and field conditions. Our results suggest that plants are a natural source of N₂O even at field conditions and challenge a view that plants are a medium to transport soil-produced N₂O into the atmosphere.