were observed during the room-temperature adsorption of CO over NaY zeolite. This was accompanied by the appearance of a prominent band at 2356 cm -1 along with the sidebands at 2336, 2342-2348, and 2364-2370 cm -1 in the ν 3 region of CO 2 vibrations. The intensity and the frequency of these bands showed monotonic changes on evacuation, temperature rise, and exchange of Na + ions with a proton or a group IIA cation and also on using the isotopically labeled CO. For instance, the adsorption of isotopic 13 C 16 O and 12 C 18 O gases gave rise to a uniform red shift in all the major ν(CO) bands, corresponding to a frequency ratio of ν( 13 CO)/ν( 12 CO) ≈ 0.978 and ν(C 18 O)/ν(C 16 O) ≈ 0.976. Similarly, all the asymmetric stretching bands of CO 2 showed a uniform isotopic shift corresponding to ν( 13 C)/ν( 12 C) ≈ 0.971. Furthermore, the intensity of most of the above-mentioned bands in ν(CO) and ν 3 (CO 2 ) regions exhibited an exponential type growth behavior with increasing adsorbate pressure, though the extent of this growth was different for individual vibrations. No significant change was, however, observed in the frequency and the intensity of the hydroxyl region bands on adsorption of CO under experimental conditions of this study. Arguments are presented to show that the observations of this study are not in harmony with the reported modes of direct CO adsorption at the specific zeolitic sites such as the charge-balancing cations, Al 3+ sites, or the Bronsted acid sites. Instead, the formation of the weakly held (CO) n and (CO 2 ) n molecular clusters occluded in the zeolitic cavities and stabilized under the cation field is in conformity with the data of this study.