“…For example, among the possible markers, rare-earth elements (REE: La, Ce, Pr, Nd, Sm, Eu, Gd, Tb, Dy, Ho, Er, Tm, Yb, Lu, and Sc and Y) have been shown to be particularly effective in discriminating different types of cherts and solving provenance issues (Elefanti et al, 2021;Finkel et al, 2019;Olofsson & Rodushkin, 2011;Ramacciotti et al, 2019a). Indeed, robust geochemical studies proved that different sedimentary environments distinguish chert through characteristic REE levels and fractionation (Murray, 1994) and they were used as provenance markers in studies carried out on a wide range of geoarchaeological materials (Aura Tortosa et al, 2020;Gallello et al, 2016;Lecuit et al, 2018;Ramacciotti et al, 2019bRamacciotti et al, , 2020. However, discriminating between chert deposits is often a challenging task since chert is composed almost entirely of silicon dioxide (SiO 2 ), and most metals are found at trace concentrations with frequently overlapping distributions, especially working at a local scale and with outcrops within the same geological levels (Speer, 2016), although these analytical approaches have also been successfully used (Parish & Werra, 2018).…”