The new discovery of complete ammonia oxidizers (comammox), single organisms capable of oxidizing ammonia into nitrate, redefined the traditional view of nitrification. However, little is known about the relative contributions of comammox and other nitrifiers to nitrification, particularly in agricultural soils with long-term intensive input of nutrients. Herein, we investigated the communities of ammonia-oxidizing bacteria (AOB), ammonia-oxidizing archaea (AOA) and comammox Nitrospira in agricultural soils under nutrients input gradient of nitrogen (0-675 kg N ha-1 year-1), phosphorus (0-405 kg P2O5 ha-1 year-1), and potassium (0-675 kg K2O ha-1 year-1) fertilizers for 19 years. The results showed that N and K fertilizers input significantly (P < 0.05) increased the AOB-amoA gene abundance, while AOA were not as sensitive as AOB. The comammox-amoA gene copies were increased in all fertilizer treatments and was significantly correlated (P < 0.05) with the amount of N fertilizer added. Terminal restriction fragment length polymorphism (T-RFLP) combined with clone-library assays of comammox-amoA gene showed that increasing gradient of nutrients input increased the relative abundance of 73 bp T-RF (assigned to Clade A) but decreased the relative abundance of 198 bp T-RF (representing Clade B). Correlation analyses and stepwise linear regression analyses demonstrated that AOB were the dominate contributors to soil potential nitrification, while comammox Nitrospira did not play a significant role (P > 0.05). This study provided insights into the adaptive responses of comammox Nitrospira and canonical ammonia oxidizers to long-term fertilizations and their relative contributions to potential nitrification in arable soils.
Keywords: AOA; AOB; Arable soil; Comammox Nitrospira; Fertilizers; Nitrification.
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