“…In surface environments, the relative abundance of these isotopes can change during several biogeochemical processes including weathering and pedogenesis (Bigalke et al, 2011;Fernandez and Borrok, 2009;Suhr et al, 2018;Vance et al, 2016), mineral precipitation/dissolution (Veeramani et al, 2015;Wall et al, 2011), adsorption on solid surfaces (Bryan et al, 2015;Dong and Wasylenki, 2016;Guinoiseau et al, 2016), ion-exchange (Maréchal and Albarède, 2002), cellular homeostasis (Caldelas et al, 2011;Wanty et al, 2017), redox reactions and ore refining (smelting and electroplating, (Kavner et al, 2008;Sivry et al, 2008a;Sonke et al, 2002;Yin et al, 2018Yin et al, , 2015. The different mechanisms of Cu and Zn isotope fractionation, e.g, via kinetic or thermodynamic equilibrium, and the significant isotopic signature variability observed among different natural compartments and materials, enable these isotopes to be potential environmental indicators useful to detect trends of pollution over time periods, identifying sources of contamination and elucidate contaminant transport mechanisms (Babcsányi et al, 2016;El Azzi et al, 2013;Petit et al, 2015;Sivry et al, 2008;Thapalia et al, 2015).…”