Abstract. We studied CO oxidation on FeO(111) films on Pt(111) at sub-monolayer oxide coverages at ultra-high vacuum (UHV) and near-atmospheric pressure conditions. The FeO (111) bilayer islands are inert towards CO2 formation. In contrast, the FeO2-x trilayer structure shows substantial CO2 production that reaches a maximum at(~40%) coverage at both, UHV and realistic, pressure conditions. The results provide compelling evidence that the FeO2-x/Pt (111) interface is the most active in CO oxidation. Although FeO2-x boundaries possesses weakly bound oxygen species, strong binding of CO to Pt favors the reaction at the FeO2-x/Pt interface as compared to the FeO2-x/FeO one, thus giving a rationale to the reactivity enhancement observed in systems exposing metal/oxide boundaries. In addition, oxygen diffusion from the interior of an FeO2-x island to the active edge sites may be effective for the oxygen replenishment in the CO oxidation catalytic cycle.