• The Eocene-Oligocene transition: A review of marine and terrestrial proxy data, models and model-data comparisons 

      Hutchinson, D.K.; Coxall, Helen; Lunt, Daniel J.; Steinthorsdottir, Margret; De Boer, Agatha M.; Baatsen, Michiel L. J.; Von Der Heydt, Anna; Huber, Matthew; Kennedy-Asser, Alan T.; Kunzmann, Lutz; Ladant, Jean-Baptiste; Lear, Caroline H.; Moraweck, Karolin; Pearson, Paul; Piga, Emanuela; Pound, Matthew J.; Salzmann, Ulrich; Scher, Howie D.; Sijp, Willem P.; Å liwińska, Kasia K.; Wilson, Paul A.; Zhang, Zhongshi (Peer reviewed; Journal article, 2021)
      The Eocene–Oligocene transition (EOT) was a climate shift from a largely ice-free greenhouse world to an icehouse climate, involving the first major glaciation of Antarctica and global cooling occurring ∼34 million years ...
    • Hydrological impact of Middle Miocene Antarctic ice-free areas coupled to deep ocean temperatures 

      Bradshaw, Catherine; Langebroek, Petra; Lear, Caroline H.; Lunt, Daniel J.; Coxall, Helen; Sosdian, Sindia M.; De Boer, Agatha (Peer reviewed; Journal article, 2021)
      Oxygen isotopes from ocean sediments (δ18O) used to reconstruct past continental ice volumes additionally record deep water temperatures (DWTs). Traditionally, these are assumed to be coupled (ice-volume changes cause DWT ...