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Reconstruction of sea-surface temperatures in the Canary Islands during Marine Isotope Stage 11

Published online by Cambridge University Press:  20 November 2019

Thibault Clauzel Open the ORCID record for Thibault Clauzel [Opens in a new window] ,
Chloé Maréchal ,
François Fourel ,
Abel Barral ,
Romain Amiot ,
Juan-Francisco Betancort ,
Alejandro Lomoschitz ,
Joaquín Meco  and
Christophe Lécuyer
Thibault Clauzel
Affiliation:
Laboratoire de Géologie de Lyon, CNRS UMR 5276, Université Claude Bernard Lyon 1, France
Chloé Maréchal
Affiliation:
Observatoire des Sciences de l'Univers de Lyon, Université Claude Bernard, Lyon 1, France
François Fourel
Affiliation:
Laboratoire d'Ecologie des Hydrosystèmes Naturels et Anthropisés, CNRS UMR 5023, Université Claude Bernard, Lyon 1, France
Abel Barral
Affiliation:
Laboratoire de Géologie de Lyon, CNRS UMR 5276, Université Claude Bernard Lyon 1, France
Romain Amiot
Affiliation:
Laboratoire de Géologie de Lyon, CNRS UMR 5276, Université Claude Bernard Lyon 1, France
Juan-Francisco Betancort
Affiliation:
Departamento de Biología, Universidad de Las Palmas de Gran Canaria, 35017Las Palmas de Gran Canaria, Canary Islands, Spain
Alejandro Lomoschitz
Affiliation:
Instituto de Oceanografía y Cambio Global, Unidad Asociada de Investigación, desarrollo e innovación al Consejo Superior de Investigaciones Científicas, Universidad de Las Palmas de Gran Canaria, 35017Las Palmas de Gran Canaria, Canary Islands, Spain
Joaquín Meco
Affiliation:
Departamento de Biología, Universidad de Las Palmas de Gran Canaria, 35017Las Palmas de Gran Canaria, Canary Islands, Spain
Christophe Lécuyer*
Affiliation:
Laboratoire de Géologie de Lyon, CNRS UMR 5276, Université Claude Bernard Lyon 1, France
*
*Corresponding author e-mail address: christophe.lecuyer@univ-lyon1.fr (C. Lécuyer).
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Abstract

The study of paleoclimates enables us to improve and better constrain climate models in order to forecast future climate variations. Marine Isotope Stage 11 (MIS11), which began around 425,000 yr BP and lasted about 65,000 yr, is a warm isotope stage of paramount importance, because the astronomical configuration was similar to the one characterizing the Holocene. Therefore, this warm isotope stage is the most appropriate analog to present-day climate known to date. This study aims to provide new data on sea-surface temperatures (SSTs) inferred from the carbon and oxygen isotope compositions of skeletal carbonates of marine invertebrates preserved in two marine deposits of the Canary Islands located at Piedra Alta, Lanzarote, and Arucas, Gran Canaria. According to published isotopic fractionation equations the marine deposit from Arucas recorded SSTs of 15.9 ± 2.2°C on average, while the tsunamite from Piedra Alta recorded SSTs of 21.2 ± 1.9°C on average. Absolute dating, mollusc assemblages, and calculated marine temperatures suggest that the Arucas marine deposit corresponds to the beginning of MIS11, while the Piedra Alta tsunamite was formed during MIS11c. These results show that low latitudes also experienced sizable SST changes during interglacial stages.

Keywords

Stable isotopeSea-surface temperatureTsunamiMolluscCanary archipelagoMIS11Climate change
Type
Research Article
Information
Quaternary Research , Volume 94 , March 2020 , pp. 195 - 209
Copyright
Copyright © University of Washington. Published by Cambridge University Press, 2019

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Footnotes

§

Also at Institut Universitaire de France, Paris, France.

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