Many physical and chemical properties of the light rare-earths and actinides are governed by the active role of f electrons, and despite intensive efforts the details of the mechanisms of phase stability and transformation are not fully understood. A prominent example which has attracted a lot of interest, both experimentally and theoretically over the years is the isostructural γ − α transition in cerium. We have determined by inelastic X-ray scattering, the complete phonon dispersion scheme of elemental cerium across the γ → α transition, and compared it with theoretical results using ab initio lattice dynamics. Several phonon branches show strong changes in the dispersion shape, indicating large modifications in the interactions between phonons and conduction electrons. This is reflected as well by the lattice Grüneisen parameters, particularly around the X point. We derive a vibrational entropy change ΔS γ−α vib ≈ ð0.33 AE 0.03Þk B , illustrating the importance of the lattice contribution to the transition. Additionally, we compare first principles calculations with the experiments to shed light on the mechanism underlying the isostructural volume collapse in cerium under pressure.T he rich phase diagram of elemental cerium (see Fig. 1) reflects how even modest changes in pressure and/or temperature can effect the correlation between electrons. The famous isostructural transition between the low density fcc phase (γ) and the high density fcc phase (α) was discovered more than seven decades ago 1, 2) and remains the only solid-solid transition in an element that ends at a critical point. At ambient temperature, the first order transition occurs at 0.75 GPa, and leads to a volume decrease of the fcc lattice by 15%. It is generally believed that the transition arises from changes in the degree of localization and correlation of the 4f electron. Currently, there are two competing models for the transition. Within the Mott transition picture (3, 4) the 4f electron is localized and nonbinding in the γ-phase and becomes itinerant (metallic) and binding in the α-phase. Accordingly, the phase transition is dependent on the kinetic energy of the 4f electron. Within the Kondo volume collapse model (5, 6) the 4f electrons, hybridized with the spd conduction electrons, are in a local moment regime and do not participate in bonding, whereas they form coherent quasi-particle bands in the α-phase and thus participate in bonding. Recent theoretical work actually suggests that the two scenarios are quite similar at finite temperatures (7-9). In a wider context it is now understood that many physical and chemical properties of the light rare-earths and actinides are governed by the active role of f electrons. However, despite intensive efforts, the detailed mechanisms of phase stability and transformation remain poorly understood.Aside from the underlying physical model, the role played by the crystalline lattice in the transition is currently an area of debate. In particular, the role of entropy in the transition is an area o...