In order to identify the origin of the giant isotope effect observed on the magnetic properties of YFe 2 A 4.2 compounds (A ¼ H, D) and probe the role of the cell volume difference, we have compared the effect of hydrostatic pressure up to 1.0 GPa on the ferro-antiferromagnetic transition temperatures T F-AF and spontaneous magnetization of YFe 2 D 4.2 and YFe 2 H 4.2. Using compressibility value of 0.013 GPa À1 and the remarkably different negative pressure slopes of T F-AF , the existence of critical volume where the ferromagnetism is suppressed at 0 K, V C ¼ 501.7 6 0.3 A 3 , was demonstrated. This consequently established the crucial role of volume on the huge isotope effect observed on the magnetic properties. V