Neoglacial Antarctic sea-ice expansion driven by mid-Holocene retreat of the Ross Ice Shelf.

James A Bendle1, Kate Newton1, Robert M Mckay2, Xavier Crosta3, Johan Etourneau4, Albot B Anya2, Osamu Seki5, Nicholas R Golledge6,7, Nancy A.N. Bertler6,7, Veronica Willmott8, Stefan Schouten9,10, Christina R Riesselman11, Guillaume Masse12 and Robert B Dunbar13, (1)University of Birmingham, Birmingham, B15, United Kingdom, (2)Victoria University of Wellington, Wellington, New Zealand, (3)Université de Bordeaux, Environnements et Paléoenvironnements Océaniques et Continentaux, Bordeaux, France, (4)Université de Bordeaux, Environments et Paléoenvironments Océaniques et Continentaux, Bordeaux, France, (5)Hokkaido University, Sapporo, Japan, (6)GNS Science-Institute of Geological and Nuclear Sciences Ltd, Lower Hutt, New Zealand, (7)Victoria University of Wellington, Antarctic Research Centre, Wellington, New Zealand, (8)Alfred Wegener Institut Fur Polar, Bremerhaven, Germany, (9)NIOZ Royal Netherlands Institute for Sea Research, Department of Marine Microbiology and Biogeochemistry, Texel, Netherlands, (10)Utrecht University, Department of Earth Sciences, Utrecht, Netherlands, (11)University of Otago, Dunedin, New Zealand, (12)Université Laval, Québec, QC, Canada, (13)Stanford University, School of Earth Sciences, Stanford, CA, United States