Holocene palaeohydrological changes in the northern Mediterranean borderlands as reflected by the lake-level record of Lake Ledro, northeastern Italy

International audience A lake-level record of Lake Ledro (northern Italy) spans the entire Holocenewith a chronology derived from51 radiocarbon dates. It is based on a specific sedimentological approach that combines data fromfive sediment profiles sampled in distinct locations in the littoral zone....

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Published in:Quaternary Research
Main Authors: Magny, Michel, Joannin, Sébastien, Galop, Didier, Vannière, Boris, Haas, Jean Nicolas, Bassetti, M., Bellintani, Paolo, Scandolari, Romana, Desmet, Marc
Other Authors: Laboratoire Chrono-environnement (UMR 6249) (LCE), Centre National de la Recherche Scientifique (CNRS)-Université de Franche-Comté (UFC), Université Bourgogne Franche-Comté COMUE (UBFC)-Université Bourgogne Franche-Comté COMUE (UBFC), Maison des Sciences de l'Homme et de l'Environnement Claude Nicolas Ledoux (UAR 3124) (MSHE), 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), Géographie de l'environnement (GEODE), Université Toulouse - Jean Jaurès (UT2J), Université de Toulouse (UT)-Université de Toulouse (UT)-Centre National de la Recherche Scientifique (CNRS), Universität Innsbruck Innsbruck, Universita “La Sapienza” Roma (Istituto CNR), Università degli Studi di Roma "La Sapienza" = Sapienza University Rome (UNIROMA), Soprintendenza per i Beni Archeologici di trento, Museo delle Palafitte del Lago di Ledro, Musée de Ledro, Transferts continentaux : forçages anthropiques, climatiques et géodynamiques, Institut des Sciences de la Terre d'Orléans (ISTO), Institut national des sciences de l'Univers (INSU - CNRS)-Université d'Orléans (UO)-Université de Tours (UT)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université d'Orléans (UO)-Université de Tours (UT)-Centre National de la Recherche Scientifique (CNRS), ANR-05-BLAN-0140,JCLAMA,Méthodes mixtes, visualisation et optimisation(2005)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2012
Subjects:
Online Access:https://hal.science/hal-00669616
https://hal.science/hal-00669616/document
https://hal.science/hal-00669616/file/Magny%20et%20al_%202012_cor.pdf
https://doi.org/10.1016/j.yqres.2012.01.005
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record_format openpolar
institution Open Polar
collection Institut national des sciences de l'Univers: HAL-INSU
op_collection_id ftinsu
language English
topic Mediterranean Lake-level fluctuations Lacustrine sediments Palaeohydrology Holocene
Mediterranean
Lake-level fluctuations
Lacustrine sediments
Palaeohydrology
Holocene
[SHS.ENVIR]Humanities and Social Sciences/Environmental studies
spellingShingle Mediterranean Lake-level fluctuations Lacustrine sediments Palaeohydrology Holocene
Mediterranean
Lake-level fluctuations
Lacustrine sediments
Palaeohydrology
Holocene
[SHS.ENVIR]Humanities and Social Sciences/Environmental studies
Magny, Michel
Joannin, Sébastien
Galop, Didier
Vannière, Boris
Haas, Jean Nicolas
Bassetti, M.
Bellintani, Paolo
Scandolari, Romana
Desmet, Marc
Holocene palaeohydrological changes in the northern Mediterranean borderlands as reflected by the lake-level record of Lake Ledro, northeastern Italy
topic_facet Mediterranean Lake-level fluctuations Lacustrine sediments Palaeohydrology Holocene
Mediterranean
Lake-level fluctuations
Lacustrine sediments
Palaeohydrology
Holocene
[SHS.ENVIR]Humanities and Social Sciences/Environmental studies
description International audience A lake-level record of Lake Ledro (northern Italy) spans the entire Holocenewith a chronology derived from51 radiocarbon dates. It is based on a specific sedimentological approach that combines data fromfive sediment profiles sampled in distinct locations in the littoral zone. On a millennial scale, the lake-level record shows two successive periods from 11,700 to 4500 cal yr BP and from 4500 cal yr BP to the present, characterized by lower and higher average lake levels, respectively. In addition to key seasonal and inter-hemispherical changes in insolation, the major hydrological change around 4500 cal yr BP may be related to a non-linear response of the climate system to orbitally-driven gradual decrease in insolation. The Ledro record questions the notion of an accentuated summer rain regime in the northern Mediterranean borderlands during the boreal insolation maximum. Moreover, the Ledro record highlights that the Holocenewas punctuated by successive centennial-scale highstands. Correlations with the Preboreal oscillation and the 8.2 ka event, and comparisonwith the atmospheric 14C residual record, suggest that short-lived lake-level fluctuations developed at Ledro in response to (1) final steps of the deglaciation in the North Atlantic area and (2) variations in solar activity.
author2 Laboratoire Chrono-environnement (UMR 6249) (LCE)
Centre National de la Recherche Scientifique (CNRS)-Université de Franche-Comté (UFC)
Université Bourgogne Franche-Comté COMUE (UBFC)-Université Bourgogne Franche-Comté COMUE (UBFC)
Maison des Sciences de l'Homme et de l'Environnement Claude Nicolas Ledoux (UAR 3124) (MSHE)
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)
Géographie de l'environnement (GEODE)
Université Toulouse - Jean Jaurès (UT2J)
Université de Toulouse (UT)-Université de Toulouse (UT)-Centre National de la Recherche Scientifique (CNRS)
Universität Innsbruck Innsbruck
Universita “La Sapienza” Roma (Istituto CNR)
Università degli Studi di Roma "La Sapienza" = Sapienza University Rome (UNIROMA)
Soprintendenza per i Beni Archeologici di trento
Museo delle Palafitte del Lago di Ledro
Musée de Ledro
Transferts continentaux : forçages anthropiques, climatiques et géodynamiques
Institut des Sciences de la Terre d'Orléans (ISTO)
Institut national des sciences de l'Univers (INSU - CNRS)-Université d'Orléans (UO)-Université de Tours (UT)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université d'Orléans (UO)-Université de Tours (UT)-Centre National de la Recherche Scientifique (CNRS)
ANR-05-BLAN-0140,JCLAMA,Méthodes mixtes, visualisation et optimisation(2005)
format Article in Journal/Newspaper
author Magny, Michel
Joannin, Sébastien
Galop, Didier
Vannière, Boris
Haas, Jean Nicolas
Bassetti, M.
Bellintani, Paolo
Scandolari, Romana
Desmet, Marc
author_facet Magny, Michel
Joannin, Sébastien
Galop, Didier
Vannière, Boris
Haas, Jean Nicolas
Bassetti, M.
Bellintani, Paolo
Scandolari, Romana
Desmet, Marc
author_sort Magny, Michel
title Holocene palaeohydrological changes in the northern Mediterranean borderlands as reflected by the lake-level record of Lake Ledro, northeastern Italy
title_short Holocene palaeohydrological changes in the northern Mediterranean borderlands as reflected by the lake-level record of Lake Ledro, northeastern Italy
title_full Holocene palaeohydrological changes in the northern Mediterranean borderlands as reflected by the lake-level record of Lake Ledro, northeastern Italy
title_fullStr Holocene palaeohydrological changes in the northern Mediterranean borderlands as reflected by the lake-level record of Lake Ledro, northeastern Italy
title_full_unstemmed Holocene palaeohydrological changes in the northern Mediterranean borderlands as reflected by the lake-level record of Lake Ledro, northeastern Italy
title_sort holocene palaeohydrological changes in the northern mediterranean borderlands as reflected by the lake-level record of lake ledro, northeastern italy
publisher HAL CCSD
publishDate 2012
url https://hal.science/hal-00669616
https://hal.science/hal-00669616/document
https://hal.science/hal-00669616/file/Magny%20et%20al_%202012_cor.pdf
https://doi.org/10.1016/j.yqres.2012.01.005
genre North Atlantic
genre_facet North Atlantic
op_source ISSN: 0033-5894
EISSN: 1096-0287
Quaternary Research
https://hal.science/hal-00669616
Quaternary Research, 2012, 77 (3), pp.382-396. ⟨10.1016/j.yqres.2012.01.005⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1016/j.yqres.2012.01.005
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op_rights info:eu-repo/semantics/OpenAccess
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container_title Quaternary Research
container_volume 77
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spelling ftinsu:oai:HAL:hal-00669616v1 2024-02-11T10:06:30+01:00 Holocene palaeohydrological changes in the northern Mediterranean borderlands as reflected by the lake-level record of Lake Ledro, northeastern Italy Magny, Michel Joannin, Sébastien Galop, Didier Vannière, Boris Haas, Jean Nicolas Bassetti, M. Bellintani, Paolo Scandolari, Romana Desmet, Marc Laboratoire Chrono-environnement (UMR 6249) (LCE) Centre National de la Recherche Scientifique (CNRS)-Université de Franche-Comté (UFC) Université Bourgogne Franche-Comté COMUE (UBFC)-Université Bourgogne Franche-Comté COMUE (UBFC) Maison des Sciences de l'Homme et de l'Environnement Claude Nicolas Ledoux (UAR 3124) (MSHE) 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) Géographie de l'environnement (GEODE) Université Toulouse - Jean Jaurès (UT2J) Université de Toulouse (UT)-Université de Toulouse (UT)-Centre National de la Recherche Scientifique (CNRS) Universität Innsbruck Innsbruck Universita “La Sapienza” Roma (Istituto CNR) Università degli Studi di Roma "La Sapienza" = Sapienza University Rome (UNIROMA) Soprintendenza per i Beni Archeologici di trento Museo delle Palafitte del Lago di Ledro Musée de Ledro Transferts continentaux : forçages anthropiques, climatiques et géodynamiques Institut des Sciences de la Terre d'Orléans (ISTO) Institut national des sciences de l'Univers (INSU - CNRS)-Université d'Orléans (UO)-Université de Tours (UT)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université d'Orléans (UO)-Université de Tours (UT)-Centre National de la Recherche Scientifique (CNRS) ANR-05-BLAN-0140,JCLAMA,Méthodes mixtes, visualisation et optimisation(2005) 2012 https://hal.science/hal-00669616 https://hal.science/hal-00669616/document https://hal.science/hal-00669616/file/Magny%20et%20al_%202012_cor.pdf https://doi.org/10.1016/j.yqres.2012.01.005 en eng HAL CCSD Elsevier info:eu-repo/semantics/altIdentifier/doi/10.1016/j.yqres.2012.01.005 hal-00669616 https://hal.science/hal-00669616 https://hal.science/hal-00669616/document https://hal.science/hal-00669616/file/Magny%20et%20al_%202012_cor.pdf doi:10.1016/j.yqres.2012.01.005 info:eu-repo/semantics/OpenAccess ISSN: 0033-5894 EISSN: 1096-0287 Quaternary Research https://hal.science/hal-00669616 Quaternary Research, 2012, 77 (3), pp.382-396. ⟨10.1016/j.yqres.2012.01.005⟩ Mediterranean Lake-level fluctuations Lacustrine sediments Palaeohydrology Holocene Mediterranean Lake-level fluctuations Lacustrine sediments Palaeohydrology Holocene [SHS.ENVIR]Humanities and Social Sciences/Environmental studies info:eu-repo/semantics/article Journal articles 2012 ftinsu https://doi.org/10.1016/j.yqres.2012.01.005 2024-01-24T17:38:13Z International audience A lake-level record of Lake Ledro (northern Italy) spans the entire Holocenewith a chronology derived from51 radiocarbon dates. It is based on a specific sedimentological approach that combines data fromfive sediment profiles sampled in distinct locations in the littoral zone. On a millennial scale, the lake-level record shows two successive periods from 11,700 to 4500 cal yr BP and from 4500 cal yr BP to the present, characterized by lower and higher average lake levels, respectively. In addition to key seasonal and inter-hemispherical changes in insolation, the major hydrological change around 4500 cal yr BP may be related to a non-linear response of the climate system to orbitally-driven gradual decrease in insolation. The Ledro record questions the notion of an accentuated summer rain regime in the northern Mediterranean borderlands during the boreal insolation maximum. Moreover, the Ledro record highlights that the Holocenewas punctuated by successive centennial-scale highstands. Correlations with the Preboreal oscillation and the 8.2 ka event, and comparisonwith the atmospheric 14C residual record, suggest that short-lived lake-level fluctuations developed at Ledro in response to (1) final steps of the deglaciation in the North Atlantic area and (2) variations in solar activity. Article in Journal/Newspaper North Atlantic Institut national des sciences de l'Univers: HAL-INSU Quaternary Research 77 3 382 396