Bipolar seesaw control on last interglacial sea level

G. Marino (), E. J. Rohling, L. Rodríguez-Sanz, K. M. Grant, D. Heslop, A. P. Roberts, Jon Stanford and J. Yu
Additional contact information
G. Marino: Research School of Earth Sciences, The Australian National University
E. J. Rohling: Research School of Earth Sciences, The Australian National University
L. Rodríguez-Sanz: Research School of Earth Sciences, The Australian National University
K. M. Grant: Research School of Earth Sciences, The Australian National University
D. Heslop: Research School of Earth Sciences, The Australian National University
A. P. Roberts: Research School of Earth Sciences, The Australian National University
J. Yu: Research School of Earth Sciences, The Australian National University

Nature, 2015, vol. 522, issue 7555, 197-201

Abstract: A synthesis of new and existing data allows Heinrich Stadial 11 (HS11), a prominent Northern Hemisphere cold event, to be linked to the timing of peak sea-level rise during glacial termination T-II, whereas rapid sea-level rise in T-I is shown to clearly post-date Heinrich Stadial 1, so fundamentally different mechanisms seem to be at work during glacial terminations.

Date: 2015
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DOI: 10.1038/nature14499

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