“…With the development of 4‐D seismic monitoring in carbonate reservoirs (Grochau et al, ; Raef et al, ), a better understanding of the in situ evolution of elastic wave velocities of porous carbonates during production or CO 2 injection is clearly needed. If a significant number of laboratory studies were dedicated to the elastic wave velocities of carbonates, a large majority were performed at ambient or low pressures and focused on the effect of depositional environments and diagenesis processes (Brigaud et al, ), porosity (Anselmetti & Eberli, ; Assefa, McCann, & Sothcott, ), microporosity (Baechle et al, ; Regnet et al, ), or pore shape (Verwer, Braaksma, & Kenter, ).…”