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Showing 1–6 of 6 results
Advanced filters: Author: Saiko T. Sugisaki Clear advanced filters
  • The West Antarctic Ice Sheet responded to different natural forcing mechanisms than the East Antarctic Ice Sheet through the mid-Pliocene due to a greater sensitivity to oceanic feedbacks, according to iceberg-rafted debris records and ice-sheet modelling experiments.

    • Molly O. Patterson
    • Christiana Rosenberg
    • Robert McKay
    Research
    Nature Geoscience
    Volume: 19, P: 182-188
  • The East Antarctic ice sheet is considered to be largely insensitive to temperature changes in the Southern Ocean. Marine sediment records indicate the East Antarctic ice sheet repeatedly retreated by several hundred kilometres during intervals of Pliocene warmth.

    • Carys P. Cook
    • Tina van de Flierdt
    • Masako Yamane
    Research
    Nature Geoscience
    Volume: 6, P: 765-769
  • Changes in climate preconditioned large-scale, recurrent Miocene to Pleistocene Antarctic submarine landslides through variations in biological productivity, ice proximity and ocean circulation, posing tsunami risk to Southern Hemisphere populations.

    • Jenny A. Gales
    • Robert M. McKay
    • Zhifang Xiong
    ResearchOpen Access
    Nature Communications
    Volume: 14, P: 1-16