We combine infrared absorption, Raman scattering, and
diamond anvil
cell techniques to explore the properties of FePS3 and
CrPS4 under pressure, comparing our findings with a symmetry
analysis, lattice dynamics calculations, and an examination of the
energy landscape. Although these complex chalcogenides are considered
to be members of the same family of materials, they display remarkably
different phase progressions on account of the metal center orbital
filling, character of the P–P linkage, layer corrugation, and
differing size of the van der Waals gap. We discuss the space group
progressions, structure–property relations, and development
of pressure-induced metallicity in terms of the competition between
local and long-range symmetry transformations and structural distortion
pathways. These findings place the properties of FePS3 and
CrPS4 on a firm foundation for work under strain control
and in the single layer limit.