Chironomid-based reconstruction of Lateglacial summer temperatures from the Ech palaeolake record (French western Pyrenees)

Chironomid head capsules were extracted and identified in 52 samples along a sediment core retrieved from the Ech palaeololake, (710 m a.s.l. in the west-central Pyrenees). The pollen stratigraphy together with radiocarbon dates provided the basis for the chronology of the record. Since temperature...

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Published in:Palaeogeography, Palaeoclimatology, Palaeoecology
Main Authors: Millet, L., Rius, D., Galop, D., Heiri, O., Brooks, S. J.
Format: Article in Journal/Newspaper
Language:unknown
Published: Elsevier 2012
Subjects:
Online Access:https://edoc.unibas.ch/69376/
https://doi.org/10.1016/j.palaeo.2011.11.014
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spelling ftunivbasel:oai:edoc.unibas.ch:69376 2023-05-15T17:23:40+02:00 Chironomid-based reconstruction of Lateglacial summer temperatures from the Ech palaeolake record (French western Pyrenees) Millet, L. Rius, D. Galop, D. Heiri, O. Brooks, S. J. 2012 https://edoc.unibas.ch/69376/ https://doi.org/10.1016/j.palaeo.2011.11.014 unknown Elsevier Millet, L. and Rius, D. and Galop, D. and Heiri, O. and Brooks, S. J. (2012) Chironomid-based reconstruction of Lateglacial summer temperatures from the Ech palaeolake record (French western Pyrenees). Palaeogeography, Palaeoclimatology, Palaeoecology, 315-316. pp. 86-99. doi:10.1016/j.palaeo.2011.11.014 info:isi/000300269200008 urn:ISSN:0031-0182 info:eu-repo/semantics/closedAccess Article PeerReviewed 2012 ftunivbasel https://doi.org/10.1016/j.palaeo.2011.11.014 2023-03-05T07:21:41Z Chironomid head capsules were extracted and identified in 52 samples along a sediment core retrieved from the Ech palaeololake, (710 m a.s.l. in the west-central Pyrenees). The pollen stratigraphy together with radiocarbon dates provided the basis for the chronology of the record. Since temperature changes were identified as one of the major determining factors for shifts in the Ech chironomid assemblages during the Lateglacial, July air temperatures were tentatively inferred from the chironomid record using a transfer function based on a combined Swiss and Norwegian calibration dataset. The model reconstructed July air temperatures between 10 and 13 degrees C during the Oldest Dryas, a two step increase in temperatures to 16 and 17.5 degrees C during the first part of the Interstadial followed by a decrease to 16.5 degrees C at the end of the Interstadial. The Ech record features three centennial-scale 1.5 degrees C coolings during the Interstadial. Inferred temperatures decreased to 15-15.5 degrees C during the Younger Dryas, and reached ca. 17 degrees C at the beginning of the Holocene. The applicability of the combined Swiss-Norwegian transfer function to the Pyrenean fossil record was substantiated by the good statistics of the inference and the similar distribution of taxa with respect to temperature in the Alps and the Pyrenees. The reliability of the Ech record, including its chronology, was supported by its good concordance with other previously published chironomid-based lateglacial temperature reconstructions from Europe and the NGRIP delta O-18 record. Article in Journal/Newspaper NGRIP University of Basel: edoc Palaeogeography, Palaeoclimatology, Palaeoecology 315-316 86 99
institution Open Polar
collection University of Basel: edoc
op_collection_id ftunivbasel
language unknown
description Chironomid head capsules were extracted and identified in 52 samples along a sediment core retrieved from the Ech palaeololake, (710 m a.s.l. in the west-central Pyrenees). The pollen stratigraphy together with radiocarbon dates provided the basis for the chronology of the record. Since temperature changes were identified as one of the major determining factors for shifts in the Ech chironomid assemblages during the Lateglacial, July air temperatures were tentatively inferred from the chironomid record using a transfer function based on a combined Swiss and Norwegian calibration dataset. The model reconstructed July air temperatures between 10 and 13 degrees C during the Oldest Dryas, a two step increase in temperatures to 16 and 17.5 degrees C during the first part of the Interstadial followed by a decrease to 16.5 degrees C at the end of the Interstadial. The Ech record features three centennial-scale 1.5 degrees C coolings during the Interstadial. Inferred temperatures decreased to 15-15.5 degrees C during the Younger Dryas, and reached ca. 17 degrees C at the beginning of the Holocene. The applicability of the combined Swiss-Norwegian transfer function to the Pyrenean fossil record was substantiated by the good statistics of the inference and the similar distribution of taxa with respect to temperature in the Alps and the Pyrenees. The reliability of the Ech record, including its chronology, was supported by its good concordance with other previously published chironomid-based lateglacial temperature reconstructions from Europe and the NGRIP delta O-18 record.
format Article in Journal/Newspaper
author Millet, L.
Rius, D.
Galop, D.
Heiri, O.
Brooks, S. J.
spellingShingle Millet, L.
Rius, D.
Galop, D.
Heiri, O.
Brooks, S. J.
Chironomid-based reconstruction of Lateglacial summer temperatures from the Ech palaeolake record (French western Pyrenees)
author_facet Millet, L.
Rius, D.
Galop, D.
Heiri, O.
Brooks, S. J.
author_sort Millet, L.
title Chironomid-based reconstruction of Lateglacial summer temperatures from the Ech palaeolake record (French western Pyrenees)
title_short Chironomid-based reconstruction of Lateglacial summer temperatures from the Ech palaeolake record (French western Pyrenees)
title_full Chironomid-based reconstruction of Lateglacial summer temperatures from the Ech palaeolake record (French western Pyrenees)
title_fullStr Chironomid-based reconstruction of Lateglacial summer temperatures from the Ech palaeolake record (French western Pyrenees)
title_full_unstemmed Chironomid-based reconstruction of Lateglacial summer temperatures from the Ech palaeolake record (French western Pyrenees)
title_sort chironomid-based reconstruction of lateglacial summer temperatures from the ech palaeolake record (french western pyrenees)
publisher Elsevier
publishDate 2012
url https://edoc.unibas.ch/69376/
https://doi.org/10.1016/j.palaeo.2011.11.014
genre NGRIP
genre_facet NGRIP
op_relation Millet, L. and Rius, D. and Galop, D. and Heiri, O. and Brooks, S. J. (2012) Chironomid-based reconstruction of Lateglacial summer temperatures from the Ech palaeolake record (French western Pyrenees). Palaeogeography, Palaeoclimatology, Palaeoecology, 315-316. pp. 86-99.
doi:10.1016/j.palaeo.2011.11.014
info:isi/000300269200008
urn:ISSN:0031-0182
op_rights info:eu-repo/semantics/closedAccess
op_doi https://doi.org/10.1016/j.palaeo.2011.11.014
container_title Palaeogeography, Palaeoclimatology, Palaeoecology
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