The crystal structure of $Ag^+$-exchanged zeolite A vacuum-dehydrated at $370^{circ}C$ and then treated with carbon monoxide at $$23^{circ}C$ has been determined by single crystal x-ray diffraction methods in the cubic space group Pm3m at $23^(1){circ}C$ ; a = 12.116 (2)${AA}$. The structure was refined to the final error indices $R_1;=;0.061;and;R_2$(weighted) = 0.068 using 349 independent reflections for which I > 3${sigma}(I).;3.6;Ag_+-CO$ complexes, where -CO may represent -CHO or -$CH_2OH$, were found in each large cavity. By coordination to silver atoms followed by reaction with $Ag^{circ}and;H^+$ within the zeolite, carbon monoxide has been partially reduced. In about 28% of the sodalite units, a $Ag_6(Ag^+)_2$ cluster may be present. In about 37% of the sodalite units, three $Ag^+$ ions are found on threefold axes where they may be bridged by three water molecules. The remaining 35% of the sodalite units are empty of silver species. Two $Ag^+$ ions per unit cell are associated with 8-ring oxygens. The remaining ca $$3Ag^+$ ions per unit cell have been reduced during the synthesis and have migrated to form small silver crystallities on the surface of the zeolite single crystal.