We found, from the analysis of M vs. T curves of some manganese oxides (manganites), that these systems do not follow the traditional Maxwell-Boltzmann statistics, but the Tsallis statistics, within the normalized formalism. Curves were calculated within the mean field approximation, for various ferromagnetic samples and the results were compared to measurements of our own and to various other authors published data, chosen at random from the literature. The agreement between the experimental data and calculated M q vs. T * curve, where T * is an effective temperature, is excellent for all the compounds. The entropic parameter, q, correlates in a simple way with the experimental value of T c , irrespect the chemical composition of the compounds, heat treatment or other details on sample preparation. Examples include q < 1 (superextensivity), q = 1 (extensivity) and q > 1 (subextensivity) cases. Manganese oxides, or simply manganites, have, to a great extent, dominated the literature on magnetism for the last five years [1]. The number of yearly published papers on the subject since 1993 to present date, amounts to over 2000. All this interest lies on at least three different reasons: (i) the rich phase diagram of manganites exhibits a variety of transport, structural and magnetic phenomena [1,2], which stimulates new models in condensed matter [3]-[14] ; (ii) manganites can present the so-called colossal magnetoresistance (CMR), and therefore are interesting systems for industrial applications [15] and, (iii) samples are relatively easy to prepare [1]. In the literature of manganites, various models have appeared in different attempts to reproduce the electric and magnetic properties of these systems. Krivoruchko et al [3], Nunez-Regueiro et al. [4] and Dionne [5] are interesting examples of multiparameter models, but which failed to achieve full agreement to experimental data. Ravindranath et al. [6]compare resistivity data in La 0.6 Y 0.1 Ca 0.3 MnO 3 to different two-parameter models which do