Enhanced climate instability in the North Atlantic and southern Europe during the Last Interglacial

P. C. Tzedakis (), R. N. Drysdale, V. Margari, L. C. Skinner, L. Menviel, R. H. Rhodes, A. S. Taschetto, D. A. Hodell, S. J. Crowhurst, J. C. Hellstrom, A. E. Fallick, J. O. Grimalt, J. F. McManus, B. Martrat, Z. Mokeddem, F. Parrenin, E. Regattieri, K. Roe and G. Zanchetta
Additional contact information
P. C. Tzedakis: University College London
R. N. Drysdale: The University of Melbourne
V. Margari: University College London
L. C. Skinner: University of Cambridge
L. Menviel: University of New South Wales
R. H. Rhodes: University of Cambridge
A. S. Taschetto: University of New South Wales
D. A. Hodell: University of Cambridge
S. J. Crowhurst: University of Cambridge
J. C. Hellstrom: The University of Melbourne
A. E. Fallick: Scottish Universities Environmental Research Centre
J. O. Grimalt: Institute of Environmental Assessment and Water Research (IDAEA)
J. F. McManus: Columbia University
B. Martrat: Institute of Environmental Assessment and Water Research (IDAEA)
Z. Mokeddem: Columbia University
F. Parrenin: Université Grenoble Alpes
E. Regattieri: University of Pisa
K. Roe: University College London
G. Zanchetta: University of Pisa

Nature Communications, 2018, vol. 9, issue 1, 1-14

Abstract: Abstract Considerable ambiguity remains over the extent and nature of millennial/centennial-scale climate instability during the Last Interglacial (LIG). Here we analyse marine and terrestrial proxies from a deep-sea sediment sequence on the Portuguese Margin and combine results with an intensively dated Italian speleothem record and climate-model experiments. The strongest expression of climate variability occurred during the transitions into and out of the LIG. Our records also document a series of multi-centennial intra-interglacial arid events in southern Europe, coherent with cold water-mass expansions in the North Atlantic. The spatial and temporal fingerprints of these changes indicate a reorganization of ocean surface circulation, consistent with low-intensity disruptions of the Atlantic meridional overturning circulation (AMOC). The amplitude of this LIG variability is greater than that observed in Holocene records. Episodic Greenland ice melt and runoff as a result of excess warmth may have contributed to AMOC weakening and increased climate instability throughout the LIG.

Date: 2018
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DOI: 10.1038/s41467-018-06683-3

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