“…Since "anomalous diamagnetism" in perovskite orthovanadates was attributed to reversal of the Dzyaloshinskii vector, 1,2 the negative magnetization observed in these compounds was relatively small, less than 10 −2 emu/ g. 1,2 Negative magnetization was observed also in some manganites, such as ͑Dy, Ca͒MnO 3 , 3,4 Gd 0.67 Ca 0.33 MnO 3 , 5 La 1−x Gd x MnO 3 , 6 NdMnO 3+␦ , 7 Nd 1−x Ca x MnO y , 8 and ͑Nd, Ca͒͑Mn, Cr͒O 3 . 8 The reversal of magnetization in these compounds was attributed to a ferrimagneticlike behavior due to the interplay of two antiferromagnetically coupled magnetic sublattices: the rare-earth sublattice and the Mn sublattice. If the magnetizations of the two sublattices have different temperature dependences and, at decreasing temperature, the magnetization of the sublattice aligned antiparallel with the magnetic field ͑rare-earth sublattice͒ increases more rapidly than that aligned with the field, the net moment may point opposite to the applied magnetic field in a ferrimagneticlike state below the compensation temperature ͑T comp ͒.…”