Rapid coupling between ice volume and polar temperature over the past 150,000 years

K. M. Grant (), E. J. Rohling, M. Bar-Matthews, A. Ayalon, M. Medina-Elizalde, C. Bronk Ramsey, C. Satow and A. P. Roberts
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K. M. Grant: School of Ocean and Earth Science, University of Southampton, National Oceanography Centre, European Way, Southampton SO14 3ZH, UK
E. J. Rohling: School of Ocean and Earth Science, University of Southampton, National Oceanography Centre, European Way, Southampton SO14 3ZH, UK
M. Bar-Matthews: Geological Survey of Israel, 30 Malchei Israel Street, Jerusalem 95501, Israel
A. Ayalon: Geological Survey of Israel, 30 Malchei Israel Street, Jerusalem 95501, Israel
M. Medina-Elizalde: School of Ocean and Earth Science, University of Southampton, National Oceanography Centre, European Way, Southampton SO14 3ZH, UK
C. Bronk Ramsey: Research Laboratory for Archaeology and the History of Art, Dyson Perrins Building, University of Oxford, South Parks Road, Oxford OX1 3QY, UK
C. Satow: Queens Building, Royal Holloway University of London
A. P. Roberts: Research School of Earth Sciences, The Australian National University

Nature, 2012, vol. 491, issue 7426, 744-747

Abstract: A new approach to dating a continuous sea-level record, using speleothem U–Th ages, shows that past variations in global ice volume occurred within centuries of polar climate change, with rates of sea-level rise reaching at least 1 metre per century.

Date: 2012
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DOI: 10.1038/nature11593

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