On the roots of wetland plants such as rice, iron oxidation forms iron-rich plaques that modulate plant nutrient and metal uptake. An enduring question is whether microbes catalyze this iron oxidation and, furthermore, if these iron-oxidizers mediate other important biogeochemical and plant interactions. To investigate this, we studied the microbial communities, metagenomes, and geochemistry of iron plaque on field-grown rice, as well as the surrounding rhizosphere and bulk soil. Plaque iron content (per mass root) increased over the growing season, showing continuous deposition. Analysis of 16S rRNA genes showed abundant iron-oxidizing and iron-reducing bacteria (FeOB and FeRB) in plaque, rhizosphere and bulk soil. FeOB were enriched in plaque, suggesting FeOB affinity for the root surface. Gallionellaceae FeOBSideroxydanswere enriched during the vegetative and early reproductive rice growth stages, while aGallionellawas enriched during reproduction through grain maturity, suggesting distinct FeOB niches over the rice life cycle. FeRBAnaeromyxobacterandGeobacterincreased in plaque later, during reproduction and grain ripening, corresponding to increased plaque iron. Metagenome-assembled genomes reveal that the Gallionellaceae may grow mixotrophically using both Fe(II) and organics. TheSideroxydansare facultative, able to use non-Fe substrates, which may allow colonization of rice roots early in the season. FeOB genomes suggest adaptations for interacting with plants, including colonization, immunity, utilization of plant organics, and nitrogen fixation. Together, our results strongly suggest that rhizoplane and rhizosphere FeOB are specifically associated with the rice plants, catalyzing the formation of iron plaque, with the potential to contribute to plant growth.