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  1. Elemental compositions of smectites reveal detailed sediment provenance changes during glacial and interglacial periods: The Southern Drake Passage and Bellingshausen Sea, Antarctica

    Variations in clay mineral assemblages have been widely used to understand changes in sediment provenance during glacial and interglacial periods. Smectite clay minerals, however, have a range of various elemental […]

    Read more of: Elemental compositions of smectites reveal detailed sediment provenance changes during glacial and interglacial periods: The Southern Drake Passage and Bellingshausen Sea, Antarctica