Lead fall-out isotopic signal over French northern Alps : Timing and sources constraints from distant lake sediment records

We present time-series of lead concentration and isotopic ratio in sediments from two French alpine lakes: Lac du Bourget , a suburban lake, and Lac d'Anterne, a mountain lake nearby the Mont-Blanc Range. This approach aims at differentiating "local" from "regional" inputs b...

Full description

Bibliographic Details
Main Authors: Arnaud, Fabien, Revel, Marie, Winiarski, Thierry, Bosch, Delphine, Chapron, Emmanuel, Desmet, Marc, Tribovillard, Nicolas
Other Authors: Environnements, Dynamiques et Territoires de la Montagne (EDYTEM), Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS), Laboratoire de Géodynamique des Chaines Alpines (LGCA), Observatoire des Sciences de l'Univers de Grenoble (OSUG), Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Centre National de la Recherche Scientifique (CNRS), Laboratoire de Tectonophysique (Tectonophysique), Université Montpellier 2 - Sciences et Techniques (UM2)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS), Renard Centre of Marine Geology, University of Gent, Processus et bilan des domaines sédimentaires (PBDS), Université de Lille, Sciences et Technologies-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2003
Subjects:
Online Access:https://hal.science/hal-00120492
https://doi.org/10.1051/jp4:20030243
id ftunivnantes:oai:HAL:hal-00120492v1
record_format openpolar
institution Open Polar
collection Université de Nantes: HAL-UNIV-NANTES
op_collection_id ftunivnantes
language English
topic Northern Alps
France
lake sediment
[SDU.STU.AG]Sciences of the Universe [physics]/Earth Sciences/Applied geology
[SDE.MCG]Environmental Sciences/Global Changes
spellingShingle Northern Alps
France
lake sediment
[SDU.STU.AG]Sciences of the Universe [physics]/Earth Sciences/Applied geology
[SDE.MCG]Environmental Sciences/Global Changes
Arnaud, Fabien
Revel, Marie
Winiarski, Thierry
Bosch, Delphine
Chapron, Emmanuel
Desmet, Marc
Tribovillard, Nicolas
Lead fall-out isotopic signal over French northern Alps : Timing and sources constraints from distant lake sediment records
topic_facet Northern Alps
France
lake sediment
[SDU.STU.AG]Sciences of the Universe [physics]/Earth Sciences/Applied geology
[SDE.MCG]Environmental Sciences/Global Changes
description We present time-series of lead concentration and isotopic ratio in sediments from two French alpine lakes: Lac du Bourget , a suburban lake, and Lac d'Anterne, a mountain lake nearby the Mont-Blanc Range. This approach aims at differentiating "local" from "regional" inputs by comparing distant sedimentary records. 210Pb and 137Cs dating methods were validated by historical events recognition [1-2] providing confident age-depth models spanning the last 250 years. In both lakes the sediment is lead-enriched compared to upper continental crust over the whole records. The human impact reached its maximum around 1970 AD, and then presents a rapid decline. Lead concentration and isotopic composition are correlated. When compared to data from a Mont Blanc ice core [3], Lac d'Anterne time-series yields excellent correlation over the last 250 years, confirming the accuracy of both dating process and record of atmospheric lead fall-out. Record from Lac du Bourget presents a similar pattern until 1985 AD when the signal from the high elevation sites ones, both in concentrations and isotopic ratio. Our data confirm the date of 1970 as the maximum of atmospheric lead fall-out over Western Europe. Today, Lac d'Anterne still records a weak airborne contamination, while Lac du Bourget is mostly influenced by local sources.
author2 Environnements, Dynamiques et Territoires de la Montagne (EDYTEM)
Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)
Laboratoire de Géodynamique des Chaines Alpines (LGCA)
Observatoire des Sciences de l'Univers de Grenoble (OSUG)
Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Centre National de la Recherche Scientifique (CNRS)
Laboratoire de Tectonophysique (Tectonophysique)
Université Montpellier 2 - Sciences et Techniques (UM2)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)
Renard Centre of Marine Geology
University of Gent
Processus et bilan des domaines sédimentaires (PBDS)
Université de Lille, Sciences et Technologies-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)
format Article in Journal/Newspaper
author Arnaud, Fabien
Revel, Marie
Winiarski, Thierry
Bosch, Delphine
Chapron, Emmanuel
Desmet, Marc
Tribovillard, Nicolas
author_facet Arnaud, Fabien
Revel, Marie
Winiarski, Thierry
Bosch, Delphine
Chapron, Emmanuel
Desmet, Marc
Tribovillard, Nicolas
author_sort Arnaud, Fabien
title Lead fall-out isotopic signal over French northern Alps : Timing and sources constraints from distant lake sediment records
title_short Lead fall-out isotopic signal over French northern Alps : Timing and sources constraints from distant lake sediment records
title_full Lead fall-out isotopic signal over French northern Alps : Timing and sources constraints from distant lake sediment records
title_fullStr Lead fall-out isotopic signal over French northern Alps : Timing and sources constraints from distant lake sediment records
title_full_unstemmed Lead fall-out isotopic signal over French northern Alps : Timing and sources constraints from distant lake sediment records
title_sort lead fall-out isotopic signal over french northern alps : timing and sources constraints from distant lake sediment records
publisher HAL CCSD
publishDate 2003
url https://hal.science/hal-00120492
https://doi.org/10.1051/jp4:20030243
long_lat ENVELOPE(69.468,69.468,-49.461,-49.461)
geographic Mont Blanc
geographic_facet Mont Blanc
genre ice core
genre_facet ice core
op_source ISSN: 1155-4339
EISSN: 1764-7177
Journal de Physique IV Proceedings
https://hal.science/hal-00120492
Journal de Physique IV Proceedings, 2003, 107, pp.61-64. ⟨10.1051/jp4:20030243⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1051/jp4:20030243
hal-00120492
https://hal.science/hal-00120492
doi:10.1051/jp4:20030243
op_doi https://doi.org/10.1051/jp4:20030243
_version_ 1766029600971816960
spelling ftunivnantes:oai:HAL:hal-00120492v1 2023-05-15T16:39:16+02:00 Lead fall-out isotopic signal over French northern Alps : Timing and sources constraints from distant lake sediment records Arnaud, Fabien Revel, Marie Winiarski, Thierry Bosch, Delphine Chapron, Emmanuel Desmet, Marc Tribovillard, Nicolas Environnements, Dynamiques et Territoires de la Montagne (EDYTEM) Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS) Laboratoire de Géodynamique des Chaines Alpines (LGCA) Observatoire des Sciences de l'Univers de Grenoble (OSUG) Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Centre National de la Recherche Scientifique (CNRS) Laboratoire de Tectonophysique (Tectonophysique) Université Montpellier 2 - Sciences et Techniques (UM2)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS) Renard Centre of Marine Geology University of Gent Processus et bilan des domaines sédimentaires (PBDS) Université de Lille, Sciences et Technologies-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS) 2003-05 https://hal.science/hal-00120492 https://doi.org/10.1051/jp4:20030243 en eng HAL CCSD EDP Sciences info:eu-repo/semantics/altIdentifier/doi/10.1051/jp4:20030243 hal-00120492 https://hal.science/hal-00120492 doi:10.1051/jp4:20030243 ISSN: 1155-4339 EISSN: 1764-7177 Journal de Physique IV Proceedings https://hal.science/hal-00120492 Journal de Physique IV Proceedings, 2003, 107, pp.61-64. ⟨10.1051/jp4:20030243⟩ Northern Alps France lake sediment [SDU.STU.AG]Sciences of the Universe [physics]/Earth Sciences/Applied geology [SDE.MCG]Environmental Sciences/Global Changes info:eu-repo/semantics/article Journal articles 2003 ftunivnantes https://doi.org/10.1051/jp4:20030243 2023-02-08T10:34:03Z We present time-series of lead concentration and isotopic ratio in sediments from two French alpine lakes: Lac du Bourget , a suburban lake, and Lac d'Anterne, a mountain lake nearby the Mont-Blanc Range. This approach aims at differentiating "local" from "regional" inputs by comparing distant sedimentary records. 210Pb and 137Cs dating methods were validated by historical events recognition [1-2] providing confident age-depth models spanning the last 250 years. In both lakes the sediment is lead-enriched compared to upper continental crust over the whole records. The human impact reached its maximum around 1970 AD, and then presents a rapid decline. Lead concentration and isotopic composition are correlated. When compared to data from a Mont Blanc ice core [3], Lac d'Anterne time-series yields excellent correlation over the last 250 years, confirming the accuracy of both dating process and record of atmospheric lead fall-out. Record from Lac du Bourget presents a similar pattern until 1985 AD when the signal from the high elevation sites ones, both in concentrations and isotopic ratio. Our data confirm the date of 1970 as the maximum of atmospheric lead fall-out over Western Europe. Today, Lac d'Anterne still records a weak airborne contamination, while Lac du Bourget is mostly influenced by local sources. Article in Journal/Newspaper ice core Université de Nantes: HAL-UNIV-NANTES Mont Blanc ENVELOPE(69.468,69.468,-49.461,-49.461)