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

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 Ita...

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Detalles Bibliográficos
Autores: Tzedakis, P. C., Drysdale, Russell N., Margari, Vasiliki, Skinner, Luke C., Menviel, Laurie, Rhodes, Rachael H., Taschetto, Andréa Sardinha, Hodell, David A., Crowhurst, Simon J., Hellstrom, John C., Fallick, Anthony Edward, Grimalt, Joan O., McManus, Jerry F., Martrat, Belen, Mokeddem, Zohra, Parrenin, Frédéric, Regattieri, Eleonora, Roe, K., Zanchetta, Giovanni
Tipo de recurso: artículo
Estado:Versión publicada
Fecha de publicación:2018
País:España
Institución:Consejo Superior de Investigaciones Científicas (CSIC)
Repositorio:DIGITAL.CSIC. Repositorio Institucional del CSIC
OAI Identifier:oai:digital.csic.es:10261/172977
Acceso en línea:http://hdl.handle.net/10261/172977
Access Level:acceso abierto
Palabra clave:Last interglacial
Interglacial
Descripción
Sumario: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. © 2018, The Author(s).

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