“…Therefore, a carbonate reference material is essential for in situ Sr isotope analysis to calibrate inter-laboratory bias and allow quality assessment of the corrections made in the data reduction protocol. Many reference materials have been developed for in situ Sr isotope analysis, such as apatite (e.g., AP1, Eppawala-AP, Durango, MAD, Otter Lake, and Slyudyanka), 18,24,[32][33][34][35] clinopyroxene (e.g., CPX05G, JJG1424, YY09-47, YY09-04, YY09-24, YY12-01, YY12-02, HNB), 16,22 plagioclase (e.g., BDL, JH56, MkAn, YG0440, YG0383, YG4301), 31,[36][37][38][39] K-feldspar (Tuyk), 37 scheelite (XJSW and HTPW), 15 aragonite (JCp-1, JCt-1), 40,41 and synthetic carbonate pellets (MACS-1, MACS-3 and NanoSr). [42][43][44] However, JCp-1 and JCt-1 are unavailable and cannot meet the requirements of the geochemistry community.…”