The overlooked role of microbial iron reduction for the enrichment of rare earth elements in deep-sea sediments

Table S1. Ages and locations of REY-rich deep-sea samples (sediments or fish teeth) in the Pacific since the Cenozoic. Table S2. Raw data of major and trace elements of the GC112 core discussed in this study. Table S3. Raw data of susceptibility (χ), frequency-dependent susceptibility (χfd%), anhysteresis remanent magnetization (ARM), and soft magnetic component (IRMsoft) of GC112. Table S4. Raw data of Fe isotope and two standard deviations (2sd) of the GC112 core discussed in this study.