Nitrogen (N) and iron (Fe) are essential but often limiting nutrients in ecosystems. Microbial nitrogen fixation (MNF) by diazotrophs and dissimilatory ferric iron (Fe(Ⅲ)) reduction (DIR) are environmentally friendly processes that sustain N and Fe availability. However, the interactions between these processes remain unclear. This study demonstrates a synergistic relationship between MNF and DIR in both laboratory and field settings. N fixation significantly increased heterotrophic Fe(Ⅲ)-reducing rates in diazotrophic DIR bacteria (DIRB) Klebsiella sp. N7 and Geobacter sulfurreducens PCA by 14.7- and 3.3-fold, respectively, while Fe(Ⅲ) reduction enhanced 15N fixation by up to 100%. Similar synergies were found between diazotroph Azospirillum humicireducens SgZ-5T and DIRB Shewanella oneidensis MR-1. Transcriptomic analysis revealed that N fixation upregulated genes associated with anaerobic respiration, accelerating Fe(Ⅲ) reduction through N supply. Simultaneously, Fe(Ⅲ) reduction provided the energy and electrons required for N fixation derived from the oxidation of organic carbon. These findings, validated across environmental samples from aquifers, hot springs, marine sediments, and soils, provide new insights into the coupled N, Fe, and C cycles in natural ecosystems.