Climatic oscillations in central Italy during the Last Glacial–Holocene transition: the record from Lake Accesa

This paper presents an event stratigraphy based on data documenting the history of vegetation cover, lake-level changes and fire frequency, as well as volcanic eruptions, over the Last Glacial–early Holocene transition from a terrestrial sediment sequence recovered at Lake Accesa in Tuscany (north-c...

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Published in:Journal of Quaternary Science
Main Authors: Magny, Michel, de Beaulieu, Jacques-Louis, Drescher-Schneider, Ruth, Vannière, Boris, Walter-Simonnet, Anne-Véronique, Millet, Laurent, Bossuet, Gilles, Peyron, Odile
Format: Article in Journal/Newspaper
Language:English
Published: Wiley-Blackwell 2006
Subjects:
Online Access:https://oceanrep.geomar.de/id/eprint/40831/
https://oceanrep.geomar.de/id/eprint/40831/1/Magnyetal2006.pdf
https://doi.org/10.1002/jqs.999
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spelling ftoceanrep:oai:oceanrep.geomar.de:40831 2023-05-15T16:39:16+02:00 Climatic oscillations in central Italy during the Last Glacial–Holocene transition: the record from Lake Accesa Magny, Michel de Beaulieu, Jacques-Louis Drescher-Schneider, Ruth Vannière, Boris Walter-Simonnet, Anne-Véronique Millet, Laurent Bossuet, Gilles Peyron, Odile 2006 text https://oceanrep.geomar.de/id/eprint/40831/ https://oceanrep.geomar.de/id/eprint/40831/1/Magnyetal2006.pdf https://doi.org/10.1002/jqs.999 en eng Wiley-Blackwell https://oceanrep.geomar.de/id/eprint/40831/1/Magnyetal2006.pdf Magny, M., de Beaulieu, J. L., Drescher-Schneider, R., Vannière, B., Walter-Simonnet, A. V., Millet, L., Bossuet, G. and Peyron, O. (2006) Climatic oscillations in central Italy during the Last Glacial–Holocene transition: the record from Lake Accesa. Journal of Quaternary Science, 21 (4). pp. 311-320. DOI 10.1002/jqs.999 <https://doi.org/10.1002/jqs.999>. doi:10.1002/jqs.999 info:eu-repo/semantics/restrictedAccess Article PeerReviewed 2006 ftoceanrep https://doi.org/10.1002/jqs.999 2023-04-07T15:37:08Z This paper presents an event stratigraphy based on data documenting the history of vegetation cover, lake-level changes and fire frequency, as well as volcanic eruptions, over the Last Glacial–early Holocene transition from a terrestrial sediment sequence recovered at Lake Accesa in Tuscany (north-central Italy). On the basis of an age–depth model inferred from 13 radiocarbon dates and six tephra horizons, the Oldest Dryas–Bølling warming event was dated to ca. 14 560 cal. yr BP and the Younger Dryas event to ca. 12 700–11 650 cal. yr BP. Four sub-millennial scale cooling phases were recognised from pollen data at ca. 14 300–14 200, 13 900–13 700, 13 400–13 100 and 11 350–11 150 cal. yr BP. The last three may be Mediterranean equivalents to the Older Dryas (GI-1d), Intra-Allerød (GI-1b) and Preboreal Oscillation (PBO) cooling events defined from the GRIP ice-core and indicate strong climatic linkages between the North Atlantic and Mediterranean areas during the last Termination. The first may correspond to Intra-Bølling cold oscillations registered by various palaeoclimatic records in the North Atlantic region. The lake-level record shows that the sub-millennial scale climatic oscillations which punctuated the last deglaciation were associated in central Italy with different successive patterns of hydrological changes from the Bølling warming to the 8.2 ka cold reversal. Copyright © 2006 John Wiley & Sons, Ltd. Article in Journal/Newspaper ice core North Atlantic OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) Journal of Quaternary Science 21 4 311 320
institution Open Polar
collection OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel)
op_collection_id ftoceanrep
language English
description This paper presents an event stratigraphy based on data documenting the history of vegetation cover, lake-level changes and fire frequency, as well as volcanic eruptions, over the Last Glacial–early Holocene transition from a terrestrial sediment sequence recovered at Lake Accesa in Tuscany (north-central Italy). On the basis of an age–depth model inferred from 13 radiocarbon dates and six tephra horizons, the Oldest Dryas–Bølling warming event was dated to ca. 14 560 cal. yr BP and the Younger Dryas event to ca. 12 700–11 650 cal. yr BP. Four sub-millennial scale cooling phases were recognised from pollen data at ca. 14 300–14 200, 13 900–13 700, 13 400–13 100 and 11 350–11 150 cal. yr BP. The last three may be Mediterranean equivalents to the Older Dryas (GI-1d), Intra-Allerød (GI-1b) and Preboreal Oscillation (PBO) cooling events defined from the GRIP ice-core and indicate strong climatic linkages between the North Atlantic and Mediterranean areas during the last Termination. The first may correspond to Intra-Bølling cold oscillations registered by various palaeoclimatic records in the North Atlantic region. The lake-level record shows that the sub-millennial scale climatic oscillations which punctuated the last deglaciation were associated in central Italy with different successive patterns of hydrological changes from the Bølling warming to the 8.2 ka cold reversal. Copyright © 2006 John Wiley & Sons, Ltd.
format Article in Journal/Newspaper
author Magny, Michel
de Beaulieu, Jacques-Louis
Drescher-Schneider, Ruth
Vannière, Boris
Walter-Simonnet, Anne-Véronique
Millet, Laurent
Bossuet, Gilles
Peyron, Odile
spellingShingle Magny, Michel
de Beaulieu, Jacques-Louis
Drescher-Schneider, Ruth
Vannière, Boris
Walter-Simonnet, Anne-Véronique
Millet, Laurent
Bossuet, Gilles
Peyron, Odile
Climatic oscillations in central Italy during the Last Glacial–Holocene transition: the record from Lake Accesa
author_facet Magny, Michel
de Beaulieu, Jacques-Louis
Drescher-Schneider, Ruth
Vannière, Boris
Walter-Simonnet, Anne-Véronique
Millet, Laurent
Bossuet, Gilles
Peyron, Odile
author_sort Magny, Michel
title Climatic oscillations in central Italy during the Last Glacial–Holocene transition: the record from Lake Accesa
title_short Climatic oscillations in central Italy during the Last Glacial–Holocene transition: the record from Lake Accesa
title_full Climatic oscillations in central Italy during the Last Glacial–Holocene transition: the record from Lake Accesa
title_fullStr Climatic oscillations in central Italy during the Last Glacial–Holocene transition: the record from Lake Accesa
title_full_unstemmed Climatic oscillations in central Italy during the Last Glacial–Holocene transition: the record from Lake Accesa
title_sort climatic oscillations in central italy during the last glacial–holocene transition: the record from lake accesa
publisher Wiley-Blackwell
publishDate 2006
url https://oceanrep.geomar.de/id/eprint/40831/
https://oceanrep.geomar.de/id/eprint/40831/1/Magnyetal2006.pdf
https://doi.org/10.1002/jqs.999
genre ice core
North Atlantic
genre_facet ice core
North Atlantic
op_relation https://oceanrep.geomar.de/id/eprint/40831/1/Magnyetal2006.pdf
Magny, M., de Beaulieu, J. L., Drescher-Schneider, R., Vannière, B., Walter-Simonnet, A. V., Millet, L., Bossuet, G. and Peyron, O. (2006) Climatic oscillations in central Italy during the Last Glacial–Holocene transition: the record from Lake Accesa. Journal of Quaternary Science, 21 (4). pp. 311-320. DOI 10.1002/jqs.999 <https://doi.org/10.1002/jqs.999>.
doi:10.1002/jqs.999
op_rights info:eu-repo/semantics/restrictedAccess
op_doi https://doi.org/10.1002/jqs.999
container_title Journal of Quaternary Science
container_volume 21
container_issue 4
container_start_page 311
op_container_end_page 320
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