Survival of the Mýrdalsjökull ice cap through the Holocene thermal maximum: evidence from sulphur contents in Katla tephra layers (Iceland) from the last ∼8400 years

International audience The climate in Iceland was drier and warmer during the Holocene thermal maximum than it is today and it has been suggested that ice caps disappeared entirely. Katla, a volcano covered by the Mýrdalsjökull ice cap in southern Iceland, has erupted rather steadily throughout the...

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Bibliographic Details
Published in:Annals of Glaciology
Main Authors: Oladottir, Bergrun, Thordarson, T., Sigmarsson, Olgeir
Other Authors: Laboratoire Magmas et Volcans (LMV), Observatoire de Physique du Globe de Clermont-Ferrand (OPGC), Université Blaise Pascal - Clermont-Ferrand 2 (UBP)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Blaise Pascal - Clermont-Ferrand 2 (UBP)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Jean Monnet - Saint-Étienne (UJM)-Centre National de la Recherche Scientifique (CNRS), University of Iceland Reykjavik
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2007
Subjects:
Online Access:https://hal.science/hal-00338717
https://hal.science/hal-00338717/document
https://hal.science/hal-00338717/file/div-class-title-survival-of-the-myrdalsjokull-ice-cap-through-the-holocene-thermal-maximum-evidence-from-sulphur-contents-in-katla-tephra-layers-iceland-from-the-last-8400-years-div.pdf
https://doi.org/10.3189/172756407782282516