The X-ray photoelectron spectra for Re3Fe5O12 garnets, ReFeO3 ortho -f e r r i t e s and ReVO4 orthovanadates have been measured by using Mg Κ 0 . radiation. The O s, Re 4d, Fe 2p, and V 2p photoelectron spectra were studied. A very big difference was observed between ReFeO3 orthoferrites and ReVO4 orthovanadates, mainly the Fe 2p 3 /2 lines were double broader than V 2p3 /2 ones, and the O s line is split by about 1.6 eV for orthofer rites, while this line is single for orthovanadates. The O s peak at 531.8 eV with intensity about 70% of the main peak is interpreted as originated from a charge fluctuation between oxygen and iron ions due to superexchange interaction.