The role of Ag in simultaneously catalyzing NO reduction and C 3 H 6 oxidation was shown to be strongly dependent on the redox properties of its local environment. Under an atmosphere of 1,000 ppm NO, 3,000 ppm C 3 H 6 , and 1% O 2 and a GHSV of 30,000 h -1 , a perovskite La 0.88 Ag 0.12 FeO 3 prepared by reactive grinding is active giving a complete NO conversion and 92% C 3 H 6 conversion at 500°C. These values are much higher than the NO conversion of 55% and C 3 H 6 conversion of 45% obtained over a 3 wt.% Ag/Al 2 O 3 catalyst under the same conditions. Under an excess of oxygen (10% O 2 ) a good SCR performance with a plateau of N 2 yield above 97% over a wide temperature window of 350-500°C along with C 3 H 6 conversion of 90% at 500°C was observed over Ag/ Al 2 O 3 , while minor N 2 yields (~10% at 250-350°C) and high C 3 H 6 conversions (reaching~100% at 450°C) were obtained over La 0.88 Ag 0.12 FeO 3 . Abundant molecular oxygen is desorbed from Ag substituted perovskite after 10% O 2 adsorption as verified by O 2 -temperature programmed desorption (TPD). This reflects the strongly oxidative properties of La 0.88 Ag 0.12 FeO 3 , which lead to a satisfactory NO reduction at 1% O 2 due to the ease of nitrate formation but to a significant C 3 H 6 combustion above that value. The formation of nitrate species over the less oxidizing Ag/Al 2 O 3 was accelerated under an excess of oxygen resulting in an excellent lean NO reduction behavior. The redox properties of silver catalysts could be adjusted via mixing perovskite with alumina for an optimal elimination of both NO and C 3 H 6 over the whole range of oxygen concentration between 0 to 10%.