Reconstruction of sea-surface temperatures in the Canary Islands during Marine Isotope Stage 11
Autor: | Chloé Maréchal, Joaquín Meco, Juan F. Betancort, Romain Amiot, François Fourel, Thibault Clauzel, Abel Barral, Christophe Lécuyer, Alejandro Lomoschitz |
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Přispěvatelé: | Laboratoire de Géologie de Lyon - Terre, Planètes, Environnement (LGL-TPE), École normale supérieure de Lyon (ENS de Lyon)-Université Claude Bernard Lyon 1 (UCBL), Université de Lyon-Université de Lyon-Institut national des sciences de l'Univers (INSU - CNRS)-Université Jean Monnet - Saint-Étienne (UJM)-Centre National de la Recherche Scientifique (CNRS), Laboratoire de Géologie de Lyon - Terre, Planètes, Environnement [Lyon] (LGL-TPE), Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Claude Bernard Lyon 1 (UCBL), Université de Lyon-Université de Lyon-École normale supérieure - Lyon (ENS Lyon), Université Claude Bernard Lyon 1 (UCBL), Université de Lyon, Laboratoire d'Ecologie des Hydrosystèmes Naturels et Anthropisés (LEHNA), Institut National de la Recherche Agronomique (INRA)-Université Claude Bernard Lyon 1 (UCBL), Université de Lyon-Université de Lyon-École Nationale des Travaux Publics de l'État (ENTPE)-Centre National de la Recherche Scientifique (CNRS), Universidad de Las Palmas de Gran Canaria, University of Las Palmas de Gran Canaria (ULPGC), Instituto de Oceanografía y Cambio Global (IOCAG), Université de Las Palmas de Gran Canaria [Espagne] (ULPGC), École normale supérieure - Lyon (ENS Lyon)-Université Claude Bernard Lyon 1 (UCBL), Université de Lyon-Université de Lyon-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS), Centre National de la Recherche Scientifique (CNRS)-Institut National de la Recherche Agronomique (INRA)-Université Claude Bernard Lyon 1 (UCBL), Université de Lyon-Université de Lyon-École Nationale des Travaux Publics de l'État (ENTPE) |
Jazyk: | angličtina |
Rok vydání: | 2020 |
Předmět: |
010504 meteorology & atmospheric sciences
[SDV]Life Sciences [q-bio] 010502 geochemistry & geophysics Piedra 01 natural sciences Isotopes of oxygen Marine Isotope Stage 11 Arts and Humanities (miscellaneous) Absolute dating medicine Climate change Holocene ComputingMilieux_MISCELLANEOUS 0105 earth and related environmental sciences Earth-Surface Processes Canary archipelago Sea-surface temperature Tsunami MIS11 Stable isotope ratio medicine.disease Stable isotope Sea surface temperature Oceanography 13. Climate action [SDU]Sciences of the Universe [physics] Interglacial General Earth and Planetary Sciences Mollusc [SDE.BE]Environmental Sciences/Biodiversity and Ecology Geology |
Zdroj: | Quaternary Research Quaternary Research, 2020, 94, pp.195-209. ⟨10.1017/qua.2019.65⟩ Quaternary Research, Elsevier, 2020, 94, pp.195-209. ⟨10.1017/qua.2019.65⟩ Quaternary Research, Elsevier, In press, ⟨10.1017/qua.2019.65⟩ |
ISSN: | 0033-5894 1096-0287 |
Popis: | 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. |
Databáze: | OpenAIRE |
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