Comparison between supergene carbonates of the Skorpion and the Rosh Pinah deposits. Carbon and oxygen isotope geochemistry applied to smithsonite, calcite and dolomite. Same smithsonite δ18O in both deposits: similar ore-forming fluids. Skorpion calcite and smithsonite formed in meteoric waters with comparable oxygen isotopic compositions. Different δ13C values in the two deposits speak for distinct C-origin.