“…2 The pioneering work of Maréchal et al 2 showed that the instrumental mass bias of MC-ICPMS can be corrected by a combination of standard/sample bracketing and elemental doping with Zn, which was further modied by using Ni 3,4 or Ga. 5,6 The overall consistency of the measurements of Cu isotope compositions by MC-ICPMS leads to the rapid development of applications in various elds such as cosmochemistry, 7,8 igneous, 9,10 ore, 11,12 sediment 13,14 and river 15,16 geochemistry, oceanography, 17,18 tracing atmospheric [19][20][21] and soil [22][23][24] pollution, assessing the diagnosis and prognosis of metabolic [25][26][27] and neurodegenerative [28][29][30] diseases, cancer, [31][32][33] but also in palaeoanthropology [34][35][36] and archaeology. [37][38][39] Prior to isotopic analysis, Cu needs to be separated from the matrix and further puried using ion-exchange chromatography. Many protocols exist, 3,[40][41][42] generally based on the use of the strongly basic AG MP-1 anion exchange resin (100-200 mesh, chloride form).…”