• Evidence for a Highly Dynamic West Antarctic Ice Sheet During the Pliocene 

      Gohl, Karsten; Uenzelmann-Neben, Gabriele; Gille-Petzoldt, Johanna; Hillenbrand, Claus-Dieter; Klages, Johann P.; Bohaty, Steven M.; Passchier, Sandra; Frederichs, Thomas; Wellner, Julia S.; Lamb, Rachel; Leitchenkov, G; Klaus, A.; Kulhanek, D.; Bauersachs, T.; Courtillat, M.; Cowan, E.; De Lira Mota, Lira; Esteves, Mariana; Fegyveresi, J.; Gao, L.; Halberstadt, A.; Horikawa, K.; Iwai, M.; Kim, J.; King, T.; Penkrot, M.; Prebble, J.; Rahaman, W.; Reinardy, B.; Renaudie, J.; Robinson, D.; Scherer, R.; Siddoway, C.; Wu, L.; Yamane, M. (Journal article; Tidsskriftartikkel; Peer reviewed, 2021-07-03)
      Major ice loss in the Amundsen Sea sector of the West Antarctic Ice Sheet (WAIS) is hypothesized to have triggered ice sheet collapses during past warm periods such as those in the Pliocene. International Ocean Discovery Program (IODP) Expedition 379 recovered continuous late Miocene to Holocene sediments from a sediment drift on the continental rise, allowing assessment of sedimentation processes ...