“…Although our measurements of the dMn-O are not a very high accuracy, they contradict the coexistence of the O and O ′ phase with the comparable volume fractions even at 220 K, and support formation of the nearly structural uniform phase below 230 K. The T −evolution of the structural parameters does not reveal any peculiarities in the anomalous T −range (T * ≈ 4 143 K ÷ 129 K ≈ T C ) which can be directly associated with the appearance of a two-phase structural state. Note that a character of the JT distortions in the x = 0.23 manganite below 150 K (dMn-O21 -dMn-O1 ≈ dMn-O1 -dMnO22), where it depends weakly on temperature [14], differs from that of the x = 0.25 manganite. Thus, the FI state and the anomalous critical behavior can occur at the different types of these distortions.…”