Abstract The influence of redox reactions involving carbon‐iron coupling (organic carbon and iron oxides) on nitrous oxide (N 2 O) production in paddy soils remains poorly understood. In this study, two microcosm experiments were conducted to investigate the effects of carbon‐iron coupling on N 2 O emissions, and the underlying mechanisms were verified using quantitative denitrification functional genes ( nirS , nirK , nosZ I and nosZ II) and high‐throughput sequencing. The results showed that ferrihydrite (iron) significantly promoted N 2 O‐N emissions ( p < 0.05) after adding ammonium nitrogen, while glucose (carbon) significantly inhibited N 2 O‐N emissions ( p < 0.05). Carbon‐iron coupling significantly decreased N 2 O‐N emissions ( p < 0.05) but did not affect soil total nitrogen loss and increased nitrogen (N 2 ) emissions. After adding high concentrations of acetylene (10% C 2 H 2 ), the N 2 O‐N emissions from carbon‐iron coupling treatment increased significantly from 6.4 to 11.9 mg N kg −1 ( p < 0.05), which confirmed that the carbon‐iron coupling reduced the N 2 O emissions by promoting the conversion of N 2 O to N 2 . The mechanisms behind carbon‐iron coupling promoting complete denitrification and reducing N 2 O emissions were attributed to glucose promoting iron reduction and carbon‐iron coupling enhancing the abundance of nosZ I (42.7%) and nosZ II (16.6%).