Mg ⁄ Ca and Sr ⁄ Ca ratios in calcium carbonate are important components of many palaeoclimate studies. We present an isotope dilution method relying on a single mixed spike containing 25 Naturally occurring calcium carbonate in corals, sclerosponges, foraminifera, otoliths, speleothems, etc. contains magnesium and strontium as minor components. Notwithstanding the complex mechanisms involved in the incorporation of these elements in calcitic or aragonitic matrices, a number of studies indicate that their spatial distribution