With the exception of systems containing Cu 2+ , complex metal oxides containing paramagnetic transitionmetal cations in square-planar coordination are rare. However, by either introducing chalcogenide, pnictide, or halide anions to form mixed-anion systems or by utilizing low-temperature topochemical reduction via anion deintercalation, an extensive range of phases containing square-planar MO 4 units can be prepared. The crystal chemistry of a series of transition-metal A 2 MO 2 X 2 oxyhalide and A 2 MO 2 B 2 X 2 oxychalcogenide and oxypnictide phases is reviewed along with how their magnetic behavior changes as a function of the transition-metal and electron count. As a contrast, these mixed-anion phases are then compared to a series of topochemically reduced, metastable transition-metal oxides that also contain square-planarcoordinated transition metals, to more fully illustrate the magnetic properties of extended frameworks of square-planar MO 4 units.