Abiotic Fe(II) oxidation by O commonly occurs in the presence of mineral sorbents and organic matter (OM) in soils and sediments; however, this tertiary system has rarely been studied. Therefore, we examined the impacts of mineral surfaces (goethite and γ-AlO) and organic matter [Suwannee River fulvic acid (SRFA)] on Fe(II) oxidation rates and the resulting Fe(III) (oxyhydr)oxides under 21 and 1% pO at pH 6. We tracked Fe dynamics by adding Fe(II) to Fe-labeled goethite and γ-AlO and characterized the resulting solids using Fe Mössbauer spectroscopy. We found Fe(II) oxidation was slower at low pO and resulted in higher-crystallinity Fe(III) phases. Relative to oxidation of Fe(II) alone, both goethite and γ-AlO surfaces increased Fe(II) oxidation rates regardless of pO levels, with goethite being the stronger catalyst. Goethite surfaces promoted the formation of crystalline goethite, while γ-AlO favored nano/small particle or disordered goethite and some lepidocrocite; oxidation of Fe(II) alone favored lepidocrocite. SRFA reduced oxidation rates in all treatments except the mineral-free systems at 21% pO, and SRFA decreased Fe(III) phase crystallinity, facilitating low-crystalline ferrihydrite in the absence of mineral sorbents, low-crystalline lepidocrocite in the presence of γ-AlO, but either crystalline goethite or ferrihydrite when goethite was present. This work highlights that the oxidation rate, the types of mineral surfaces, and OM control Fe(III) precipitate composition.