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  1. Back to the Future: Using long-term observational and paleo-proxy reconstructions to improve model projections of Antarctic climate

    Quantitative estimates of future Antarctic climate change are derived from numerical global climate models. Evaluation of the reliability of climate model projections involves many lines of evidence on past performance […]

    Read more of: Back to the Future: Using long-term observational and paleo-proxy reconstructions to improve model projections of Antarctic climate
  2. 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