“…Starting from an initial value of ∼0.699 in chondrites, 17 the 87 Sr/ 86 Sr ratio evolved through time with the radioactive decay of 87 Rb -> 87 Sr ( t 1/2 = 49.61 ± 0.16 Ga) and through geochemical partitioning between Rb, a K-like monovalent alkali metal, and Sr, a Ca-like divalent alkaline-earth metal, resulting in a typical ∼15% variation of the 87 Sr/ 86 Sr value in geological materials. This large range of the 87 Sr/ 86 Sr value has been used for years for different applications, from cosmochemistry, 17,18 mantle and crust geochemistry, 19,20 isotope stratigraphy, 21,22 human and animal past mobility, 23,24 archaeological artifact provenance, 25,26 to forensics 27,28 and goods of value authentication. 29,30…”