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.

表S1 新生代以来太平洋富稀土元素与钇（REY）深海样品（沉积物或鱼牙）的年龄及采样位点。
表S2 本研究讨论的GC112岩芯主量元素与微量元素原始数据。
表S3 GC112岩芯的磁化率（χ）、频率依赖性磁化率百分含量（χfd%）、非滞后剩磁（ARM）与软磁组分（IRMsoft）原始数据。
表S4 本研究讨论的GC112岩芯铁同位素及两组标准偏差（2sd）原始数据。