Abstract Pressure-induced polymorphic phase transitions are important in fundamental physics, chemistry, materials science, and geoscience. The isosymmetric phase transition is unique in that it retains crystal symmetry through the transition and exhibits both first- and second-order characteristics. However, the underlying mechanisms of the isosymmetric second-order phase transition have not been well constrained under high pressures. Here, we report a novel case of pressure-induced isosymmetric phase transition in cerite, a rare earth element (REE) mineral, using a diamond anvil cell combined with in-situ synchrotron single-crystal X-ray diffraction. This phase transition is triggered by an increase in coordination number (CN) and exhibits characteristics of second-order. By combining our findings with previous research, we identify five distinct types of pressure-induced isosymmetric phase transitions. Furthermore, we propose an explanation for the nature (first- or second-order) of phase transitions triggered by coordination number increases under pressure. The complexity of a mineral's crystal structure plays a crucial role in determining the type of isosymmetric phase transition observed. Single-building unit crystal structures tend to exhibit first-order transitions, while those with multiple building units exhibit greater flexibility and are more prone to second-order transitions. This study provides new evidence for pressure-induced coordination number increase-triggered isosymmetric second-order phase transitions and offers valuable insights into the mechanisms governing pressure-induced isosymmetric phase transitions.
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