Permafrost conditions in the Mediterranean region since the Last Glaciation

• Published in: Earth-Science Reviews
• Main Authors: Oliva, M., Žebre, M., Guglielmin, M., Hughes, P., Ciner, A., Vieira, G., Bodin, Xavier, Andrés, Nahuel, Colucci, R.R., Garcia-Hernandez, C., Mora, C., Nofre, J., Palacios, D., Pérez-Alberti, A., Ribolini, A., Ruiz-Fernández, J., Sarikaya, M., Serrano, E., Urdea, P., Valcárcel, M., Woodward, C., Yildirim, C.
• Other Authors: University of Barcelona, Geological Survey of Slovenia (GeoZS), Department of Theoretical and Applied Sciences Insubria, Universitá degli Studi dell’Insubria = University of Insubria Varese (Uninsubria), University of Manchester Manchester, Avrasya Yer Bilimleri Enstitüsü = Eurasia Institute of Earth Sciences Istanbul (AYBE), Istanbul Technical University (ITÜ), Universidade de Lisboa = University of Lisbon = Université de Lisbonne (ULISBOA), Environnements, Dynamiques et Territoires de Montagne (EDYTEM), Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS), Universidad Complutense de Madrid = Complutense University of Madrid Madrid (UCM), Universidad de Oviedo = University of Oviedo, Laboratoire de Physique Statistique de l'ENS (LPS), Fédération de recherche du Département de physique de l'Ecole Normale Supérieure - ENS Paris (FRDPENS), École normale supérieure - Paris (ENS-PSL), Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Centre National de la Recherche Scientifique (CNRS)-École normale supérieure - Paris (ENS-PSL), Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Diderot - Paris 7 (UPD7)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS), project CTM2017-87976-P of the Spanish Ministry of Economy, Industry and CompetitivenessRamón y Cajal Program of the Spanish Ministry of Economy and Competitiveness (RYC-2015-17597)Research Group ANTALP (Antarctic, Arctic, Alpine Environments; 2017-SGR-1102) funded by the Government of Catalonia through the AGAUR agencyTÜBİTAK (Project no: 101Y002, 107Y069, 110Y300, 112Y139, 114Y548T and 116Y155) for continuous support to the glacial/periglacial research in Turkey
• Format: Article in Journal/Newspaper
• Language: English
• Published: HAL CCSD 2018
• Subjects: Last Glacial Maximum; Holocene; deglaciation; permafrost; Mediterranean region; [SDE.MCG]Environmental Sciences/Global Changes; [SDE.BE]Environmental Sciences/Biodiversity and Ecology; [SDE.IE]Environmental Sciences/Environmental Engineering; [SDE.ES]Environmental Sciences/Environment and Society; [SHS.GEO]Humanities and Social Sciences/Geography; Ice
• Online Access: https://sde.hal.science/hal-01880586; https://doi.org/10.1016/j.earscirev.2018.06.018

International audience The relatively warm climate conditions prevailing today in the Mediterranean region limit cold geomorphological processes only to the highest mountain environments. However, climate variability during the Late Pleistocene and Holocene has led to significant spatio-temporal variations of the glacial and periglacial domain in these mountains, including permafrost conditions.Here, we examine the distribution and evolution of permafrost in the Mediterranean region considering five time periods: Last Glaciation, deglaciation, Holocene, Little Ice Age (LIA) and present-day. The distribution of inactive permafrost-derived features as well as sedimentary records indicates that the elevation limit of permafrost during the Last Glaciation was between 1000 m and even 2000 m lower than present. Permafrost was also widespread in non-glaciated slopes above the snowline forming rock glaciers and block streams, as well as meter-sized stone circles in relatively flat summit areas. As in most of the Northern Hemisphere, the onset of deglaciation in the Mediterranean region started around 19-20 ka. The ice-free terrain left by retreating glaciers was subject to paraglacial activity and intense periglacial processes under permafrost conditions. Many rock glaciers, protalus lobes and block streams formed in these recently deglaciated environments, though most of them became gradually inactive as temperatures kept rising, especially those at lower altitudes. Following the Younger Dryas glacial advance, the Early Holocene saw the last massive deglaciation in Mediterranean mountains accompanied by a progressive shift of permafrost conditions to higher elevations. It is unlikely that air temperatures recorded in Mediterranean mountains during the Holocene favoured the existence of widespread permafrost regimes, with the only exception of the highest massifs exceeding 2500-3000 m. LIA colder climate promoted a minor glacial advance and the spatial expansion of permafrost, with the development of new protalus ...