Oxides containing multivalent cations, such as  transition elements, are much more prone to be non-stoichiometric. Examples are  TiO2+x, BaTiO3-x and SrTiO3-x where Ti4+ ions can be easily reduced to Ti3+ creating oxygen deficiency of  order 1% within the limits of the stability of oxide i.e. before decomposition  and phase change. 
                        
                        Transition metal mono-oxide series Ni1-xO,  Co1-xO, Mn1-xO and Fe1-xO are the oxides in  which a fraction of the divalent cations is easily oxidized to the divalent  state resulting in cation deficiency, x . The deficiency is ~5x10-4   % for Ni1-xO, ~1% for Co1-xO, ~0.1% for Mn1-xO  and ~0.15% for Fe1-xO. FeO is seldom stoichiometric and it has a  minimum non-stoichiometry of 0.05%.