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Elevated atmospheric CO 2 can alter nitrogen availability through the regulation of ammonia oxidation in paddy soils. However, most previous research has focused on abrupt CO 2 enrichment, which does not reflect the gradual increase in atmospheric CO 2 under future climate change scenarios. Consequently, the effects of progressive versus abrupt CO 2 enrichment on ammonia oxidizers remain underexplored. Three CO 2 treatments were established using an automated CO 2 regulation system: ambient CO 2 (CK), progressive CO 2 increase (PI; +40 ppm yr. −1 to +200 ppm), and abrupt CO 2 increase (AI; +200 ppm). Compared with CK, PI increased nitrification potential by 22.28%, whereas AI showed no significant effect. The abundance of ammonia‐oxidizing archaea (AOA) remained unchanged across CO 2 enrichment treatments. However, PI significantly elevated the abundances of ammonia‐oxidizing bacteria (AOB) and complete ammonia oxidizers (Comammox) by 41.26% and 208.64%, respectively. The CO 2 enrichment treatments significantly altered the community structure of AOB but had no significant effects on those of AOA or Comammox. Soil dissolved organic carbon and NH 4 + ‐N were the key factors influencing ammonia‐oxidizer communities and nitrification potential. Overall, PI exerted stronger stimulatory effects than AI. Additionally, nitrification potential was more closely associated with AOB abundance and community structure than with those of AOA or Comammox.
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Ren et al. (2026) studied this question.
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