The study shows U-Pb dating reveals significant REY enrichment in bioapatite from the late Miocene, indicating geological phenomena in the Clarion-Clipperton Fracture Zone.
Table S1: LA-ICP-MS in situ trace elements data of bioapatite from core MG026. Table S2: LA-ICP-MS in situ U-Pb dating data of bioapatite from core MG026.
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Chen et al. (2025) studied this question.
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