主催: 日本地球化学会年会要旨集
会議名: 2025年度日本地球化学会第72回年会講演要旨集
回次: 72
開催日: 2025/09/07 - 2025/09/19
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Changes in global climate have accelerated ice loss in Antarctica, where the highest melt rates are found in the Amundsen Sea (AS), West Antarctica. Ice mass loss results from the incursion of relatively warm modified Circumpolar Deep Water (mCDW), which flows under the fringing ice shelves, including the Dotson Ice Shelf (DIS). Here, we report dissolved REE concentrations, with an emphasis on Nd, and Nd isotopes from nine stations located off of the DIS. We show REE enrichment near between ~ 300-400 meters, within the depth range of maximum outflow velocities and meltwater fractions. This implications has significance in the context of REE contribution from Antarctic glacial melting.