Neoglacial Antarctic sea-ice expansion driven by mid-Holocene retreat of the Ross Ice Shelf.
James A Bendle1, Kate Newton2, Robert M Mckay3, Xavier Crosta4, Johan Etourneau5, Albot B Anya6, Osamu Seki7, Nicholas R Golledge8,9, Nancy A.N. Bertler3,8, Veronica Willmott10, Stefan Schouten11,12, Christina R Riesselman13, Guillaume Masse14 and Robert B Dunbar15, (1)University of Birmingham, School of Geography, Earth and Environmental Sciences, Birmingham, United Kingdom, (2)University of Birmingham, Birmingham, United Kingdom, (3)Victoria University of Wellington, Antarctic Research Centre, Wellington, New Zealand, (4)University of Bordeaux, CNRS, UMR 5805 EPOC, Pessac Cedex, France, (5)Université de Bordeaux, Environments et Paléoenvironments Océaniques et Continentaux, Bordeaux, France, (6)Victoria University of Wellington, Wellington, New Zealand, (7)Hokkaido University, Institute of Low Temperature Science, Sapporo, Japan, (8)GNS Science-Institute of Geological and Nuclear Sciences Ltd, Lower Hutt, New Zealand, (9)Antarctic Research Centre, Victoria University of Wellington, Wellington, New Zealand, (10)Alfred Wegener Institut Fur Polar, Bremerhaven, Germany, (11)NIOZ Royal Netherlands Institute for Sea Research, Department of Marine Microbiology and Biogeochemistry, Texel, Netherlands, (12)Utrecht University, Department of Earth Sciences, Utrecht, Netherlands, (13)University of Otago, Departments of Geology and Marine Science, Dunedin, New Zealand, (14)Université Laval, Québec, QC, Canada, (15)Stanford University, Oceans, Stanford, United States
