“…Quite often, however, these DOF are deeply intertwined, leading to competing, coexisting, or even cooperative orders [1][2][3]. Such cooperative coupling between the lattice structure, electronic order, and the magnetic configuration occurs in a wide variety of transition metal oxides such as manganites [4], cobaltites [5], ferrites [6], vanadates [7], nickelates [8,9], and cuprates [10]. This arises due to the highly connected nature of the lattice [11][12][13][14] that results in an interplay between changes in electronic and magnetic order with many structural degrees of freedom such as distortions, octahedral rotations and cation displacements.…”