While heating a seawater spiral shell (Euplica scripta), thermally induced aragonite−calcite (A−C) transformation occurred within the temperature region of multistep thermal dehydration. Here, the kinetic interplay between the A−C transformation and thermal dehydration was studied as a possible cause of the reduction in the A−C transformation temperatures. The kinetics of the A−C transformation was systematically investigated under isothermal conditions by powder X-ray diffractometry and under linear nonisothermal conditions by Fourier transform infrared spectroscopy. The thermal dehydration was characterized as a partially overlapping, three-step process by thermogravimetry−differential thermal analysis coupled with mass spectroscopy for the evolved gases. The A−C transformation occurred in the temperature range of the final part of the second dehydration step and the initial part of the third dehydration step. The kinetics of A−C transformation and thermal dehydration were characterized by contracting geometry-type models, in which the respective transformations were regulated by a constant linear advancement rate and diffusional removal of water vapor, respectively. Based on the kinetic results, the mutual interaction of those thermally induced processes is discussed as a possible cause of the reduction in the A−C transformation temperature.