Recycling of anoxic sediment weakens the arc magmas oxidation in paleo-oceanic subduction zone

The Supplementary Material contains: Figure S1, photomicrographs of HQL rocks; Figure S2, the long-term reproducibility of δ98/95Mo in the Alfa Mo standard solution for nearly half a year; Figure S3, concordia diagrams of LA-ICP-MS zircon U-Pb data and representative zircon CL images; Figure S4, chondrite-normalized REE patterns of zircons for the HQL rocks; Figure S5, plots of Rb, Sr, Ba, (87Sr/86Sr)i, δ98/95Mo, and Fe3+/∑Fe values versus loss on ignition (LOI) values; Figure S6 plots of (a) Th, (b) Nd, (c) La, (d) Ba, (e) Ce, and (f) Yb contents versus Zr contents; Figure S7, plots of (87Sr/86Sr)i, εNd(t),δ98/95Mo, and Fe3+/∑Fe values versus MgO contents; Figure S8, plots of δ98/95Mo values versus TiO2, Ba/Sr, Dy/Yb, and Cu/Mo values; Figure S9, diagram of zircon εHf(t) values; Table S1, LA-ICP-MS zircon trace element compositions for HQL rocks; Table S2, LA–ICP–MS U–Pb isotope data of zircons for HQL rocks; Table S3, LA-MC-ICPMS zircon Hf isotopes; Table S4, whole-rock major and trace element compositions; Table S5, whole-rock Rb-Sr, Sm-Nd and Lu-Hf isotopic compositions; Table S6, Mo isotopic compositions and wet-chemical Fe3+/∑Fe values; Table S7, elemental and isotopic compositions of the end members used for mixing model.