A sub-decadal record of East Antarctic biological productivity, and ocean-ice interactions over the Holocene from an ultra-expanded continental shelf sediment drift.
Robert M Mckay1, Katelyn M Johnson2, Kate Newton3, Albot B Anya1, James A Bendle4, Francisco J Jimenez5, Johan Etourneau6, Xavier Crosta7, Christina R Riesselman8, Huw Joseph Horgan2, Nancy A.N. Bertler9, Carlota Escutia10 and Robert B Dunbar11, (1)Victoria University of Wellington, Wellington, New Zealand, (2)Victoria University of Wellington, Antarctic Research Centre, Wellington, New Zealand, (3)University of Birmingham, Birmingham, United Kingdom, (4)University of Birmingham, School of Geography, Earth and Environmental Sciences, Birmingham, United Kingdom, (5)University of Granada, Granada, Spain, (6)Instituto Andaluz de Ciencias de la Tierra, CSIC-Universidad Granada, Granada, Spain, (7)Université de Bordeaux, Environnements et Paléoenvironnements Océaniques et Continentaux, Bordeaux, France, (8)University of Otago, Departments of Geology and Marine Science, Dunedin, New Zealand, (9)Victoria University of Wellington and GNS Science, Antarctic Research Centre, Wellington, New Zealand, (10)I Andaluz de Ciencias Tierra, Armilla, Granada, Spain, (11)Stanford University, School of Earth Sciences, Stanford, CA, United States
