A new interpolation method to measure delta evolution and sediment flux: Application to the late Holocene coastal plain of the Argens River in the western Mediterranean

International audience Rapid environmental changes along the Mediterranean coasts influenced the sedimentary dynamics, shoreline position and human settlements in deltaic areas over the last millennia. An innovative and multiproxy approach using geostatistical modelling was developed to estimate geo...

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Published in:Marine Geology
Main Authors: Degeai, Jean-Philippe, Bertoncello, Frédérique, Vacchi, Matteo, Augustin, Laurent, de Moya, Alain, Ardito, Luigi, Devillers, Benoît
Other Authors: Archéologie des Sociétés Méditerranéennes (ASM), Université Paul-Valéry - Montpellier 3 (UPVM)-Centre National de la Recherche Scientifique (CNRS)-Ministère de la Culture (MC), Culture et Environnements, Préhistoire, Antiquité, Moyen-Age (CEPAM), Université Nice Sophia Antipolis (1965 - 2019) (UNS)-Centre National de la Recherche Scientifique (CNRS)-Université Côte d'Azur (UniCA), Centre européen de recherche et d'enseignement des géosciences de l'environnement (CEREGE), Institut de Recherche pour le Développement (IRD)-Aix Marseille Université (AMU)-Collège de France (CdF (institution))-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE), Division technique INSU/SDU (DTI), Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS), Bureau de Recherches Géologiques et Minières (BRGM)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2020
Subjects:
Online Access:https://brgm.hal.science/hal-02911834
https://brgm.hal.science/hal-02911834/document
https://brgm.hal.science/hal-02911834/file/Degeai-etal_2019_MarineGeology_Manuscript_revised.pdf
https://doi.org/10.1016/j.margeo.2020.106159
id ftbrgm:oai:HAL:hal-02911834v1
record_format openpolar
institution Open Polar
collection BRGM: HAL (Bureau de Recherches Géologiques et Minières)
op_collection_id ftbrgm
language English
topic Mediterranean delta
Coastal environment
Sediment flux
Elevation modelling
Inorganic geochemistry
Molluscan fauna
Late Holocene
Western Mediterranean
[SHS.ENVIR]Humanities and Social Sciences/Environmental studies
[SHS.ARCHEO]Humanities and Social Sciences/Archaeology and Prehistory
[SDU.STU]Sciences of the Universe [physics]/Earth Sciences
[SDE.MCG]Environmental Sciences/Global Changes
spellingShingle Mediterranean delta
Coastal environment
Sediment flux
Elevation modelling
Inorganic geochemistry
Molluscan fauna
Late Holocene
Western Mediterranean
[SHS.ENVIR]Humanities and Social Sciences/Environmental studies
[SHS.ARCHEO]Humanities and Social Sciences/Archaeology and Prehistory
[SDU.STU]Sciences of the Universe [physics]/Earth Sciences
[SDE.MCG]Environmental Sciences/Global Changes
Degeai, Jean-Philippe
Bertoncello, Frédérique
Vacchi, Matteo
Augustin, Laurent
de Moya, Alain
Ardito, Luigi
Devillers, Benoît
A new interpolation method to measure delta evolution and sediment flux: Application to the late Holocene coastal plain of the Argens River in the western Mediterranean
topic_facet Mediterranean delta
Coastal environment
Sediment flux
Elevation modelling
Inorganic geochemistry
Molluscan fauna
Late Holocene
Western Mediterranean
[SHS.ENVIR]Humanities and Social Sciences/Environmental studies
[SHS.ARCHEO]Humanities and Social Sciences/Archaeology and Prehistory
[SDU.STU]Sciences of the Universe [physics]/Earth Sciences
[SDE.MCG]Environmental Sciences/Global Changes
description International audience Rapid environmental changes along the Mediterranean coasts influenced the sedimentary dynamics, shoreline position and human settlements in deltaic areas over the last millennia. An innovative and multiproxy approach using geostatistical modelling was developed to estimate geomorphic evolution and sediment fluxes in deltaic areas, while palaeoecological conditions and environmental changes were assessed from geochemistry and cluster analyses of molluscan fauna. This method was applied to the coastal plain of the Argens River (southern France) in the western Mediterranean. The study of facies associations led to the identification of depositional environments representative of prodelta, delta front, river channel, floodplain, marsh and abandoned channel. The late Holocene sediment flux in the Argens River bayhead delta ranged from 15,800 ± 2300 to 52,000 + 8500 m3.yr-1. The highest rates of sediment deposition and delta growth occurred between 2500 and 2000 cal yr BP during a period of high flood frequency in the western Mediterranean. A geomorphically-induced decrease in subaqueous sediment flux over the past 2500 years and an increase in fluvial activity from 1600 to 500 cal yr BP were primarily controlled by autogenic processes due to change in accommodation space, delta slope and tributary junctions. A sharp increase in subaerial sediment flux from 500 to 0 cal yr BP was probably driven by hydroclimatic change characterized by more frequent flooding during the Little Ice Age. High sediment fluxes and climate-driven fluvial activity were associated with a southward shift of the North Atlantic westerlies or a northward migration of the intertropical convergence zone.
author2 Archéologie des Sociétés Méditerranéennes (ASM)
Université Paul-Valéry - Montpellier 3 (UPVM)-Centre National de la Recherche Scientifique (CNRS)-Ministère de la Culture (MC)
Culture et Environnements, Préhistoire, Antiquité, Moyen-Age (CEPAM)
Université Nice Sophia Antipolis (1965 - 2019) (UNS)-Centre National de la Recherche Scientifique (CNRS)-Université Côte d'Azur (UniCA)
Centre européen de recherche et d'enseignement des géosciences de l'environnement (CEREGE)
Institut de Recherche pour le Développement (IRD)-Aix Marseille Université (AMU)-Collège de France (CdF (institution))-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)
Division technique INSU/SDU (DTI)
Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)
Bureau de Recherches Géologiques et Minières (BRGM)
format Article in Journal/Newspaper
author Degeai, Jean-Philippe
Bertoncello, Frédérique
Vacchi, Matteo
Augustin, Laurent
de Moya, Alain
Ardito, Luigi
Devillers, Benoît
author_facet Degeai, Jean-Philippe
Bertoncello, Frédérique
Vacchi, Matteo
Augustin, Laurent
de Moya, Alain
Ardito, Luigi
Devillers, Benoît
author_sort Degeai, Jean-Philippe
title A new interpolation method to measure delta evolution and sediment flux: Application to the late Holocene coastal plain of the Argens River in the western Mediterranean
title_short A new interpolation method to measure delta evolution and sediment flux: Application to the late Holocene coastal plain of the Argens River in the western Mediterranean
title_full A new interpolation method to measure delta evolution and sediment flux: Application to the late Holocene coastal plain of the Argens River in the western Mediterranean
title_fullStr A new interpolation method to measure delta evolution and sediment flux: Application to the late Holocene coastal plain of the Argens River in the western Mediterranean
title_full_unstemmed A new interpolation method to measure delta evolution and sediment flux: Application to the late Holocene coastal plain of the Argens River in the western Mediterranean
title_sort new interpolation method to measure delta evolution and sediment flux: application to the late holocene coastal plain of the argens river in the western mediterranean
publisher HAL CCSD
publishDate 2020
url https://brgm.hal.science/hal-02911834
https://brgm.hal.science/hal-02911834/document
https://brgm.hal.science/hal-02911834/file/Degeai-etal_2019_MarineGeology_Manuscript_revised.pdf
https://doi.org/10.1016/j.margeo.2020.106159
genre North Atlantic
genre_facet North Atlantic
op_source ISSN: 0025-3227
Marine Geology
https://brgm.hal.science/hal-02911834
Marine Geology, 2020, 424, pp.106159. ⟨10.1016/j.margeo.2020.106159⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1016/j.margeo.2020.106159
hal-02911834
https://brgm.hal.science/hal-02911834
https://brgm.hal.science/hal-02911834/document
https://brgm.hal.science/hal-02911834/file/Degeai-etal_2019_MarineGeology_Manuscript_revised.pdf
doi:10.1016/j.margeo.2020.106159
op_rights info:eu-repo/semantics/OpenAccess
op_doi https://doi.org/10.1016/j.margeo.2020.106159
container_title Marine Geology
container_volume 424
container_start_page 106159
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spelling ftbrgm:oai:HAL:hal-02911834v1 2024-05-19T07:45:28+00:00 A new interpolation method to measure delta evolution and sediment flux: Application to the late Holocene coastal plain of the Argens River in the western Mediterranean Degeai, Jean-Philippe Bertoncello, Frédérique Vacchi, Matteo Augustin, Laurent de Moya, Alain Ardito, Luigi Devillers, Benoît Archéologie des Sociétés Méditerranéennes (ASM) Université Paul-Valéry - Montpellier 3 (UPVM)-Centre National de la Recherche Scientifique (CNRS)-Ministère de la Culture (MC) Culture et Environnements, Préhistoire, Antiquité, Moyen-Age (CEPAM) Université Nice Sophia Antipolis (1965 - 2019) (UNS)-Centre National de la Recherche Scientifique (CNRS)-Université Côte d'Azur (UniCA) Centre européen de recherche et d'enseignement des géosciences de l'environnement (CEREGE) Institut de Recherche pour le Développement (IRD)-Aix Marseille Université (AMU)-Collège de France (CdF (institution))-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE) Division technique INSU/SDU (DTI) Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS) Bureau de Recherches Géologiques et Minières (BRGM) 2020-06 https://brgm.hal.science/hal-02911834 https://brgm.hal.science/hal-02911834/document https://brgm.hal.science/hal-02911834/file/Degeai-etal_2019_MarineGeology_Manuscript_revised.pdf https://doi.org/10.1016/j.margeo.2020.106159 en eng HAL CCSD Elsevier info:eu-repo/semantics/altIdentifier/doi/10.1016/j.margeo.2020.106159 hal-02911834 https://brgm.hal.science/hal-02911834 https://brgm.hal.science/hal-02911834/document https://brgm.hal.science/hal-02911834/file/Degeai-etal_2019_MarineGeology_Manuscript_revised.pdf doi:10.1016/j.margeo.2020.106159 info:eu-repo/semantics/OpenAccess ISSN: 0025-3227 Marine Geology https://brgm.hal.science/hal-02911834 Marine Geology, 2020, 424, pp.106159. ⟨10.1016/j.margeo.2020.106159⟩ Mediterranean delta Coastal environment Sediment flux Elevation modelling Inorganic geochemistry Molluscan fauna Late Holocene Western Mediterranean [SHS.ENVIR]Humanities and Social Sciences/Environmental studies [SHS.ARCHEO]Humanities and Social Sciences/Archaeology and Prehistory [SDU.STU]Sciences of the Universe [physics]/Earth Sciences [SDE.MCG]Environmental Sciences/Global Changes info:eu-repo/semantics/article Journal articles 2020 ftbrgm https://doi.org/10.1016/j.margeo.2020.106159 2024-05-02T00:12:28Z International audience Rapid environmental changes along the Mediterranean coasts influenced the sedimentary dynamics, shoreline position and human settlements in deltaic areas over the last millennia. An innovative and multiproxy approach using geostatistical modelling was developed to estimate geomorphic evolution and sediment fluxes in deltaic areas, while palaeoecological conditions and environmental changes were assessed from geochemistry and cluster analyses of molluscan fauna. This method was applied to the coastal plain of the Argens River (southern France) in the western Mediterranean. The study of facies associations led to the identification of depositional environments representative of prodelta, delta front, river channel, floodplain, marsh and abandoned channel. The late Holocene sediment flux in the Argens River bayhead delta ranged from 15,800 ± 2300 to 52,000 + 8500 m3.yr-1. The highest rates of sediment deposition and delta growth occurred between 2500 and 2000 cal yr BP during a period of high flood frequency in the western Mediterranean. A geomorphically-induced decrease in subaqueous sediment flux over the past 2500 years and an increase in fluvial activity from 1600 to 500 cal yr BP were primarily controlled by autogenic processes due to change in accommodation space, delta slope and tributary junctions. A sharp increase in subaerial sediment flux from 500 to 0 cal yr BP was probably driven by hydroclimatic change characterized by more frequent flooding during the Little Ice Age. High sediment fluxes and climate-driven fluvial activity were associated with a southward shift of the North Atlantic westerlies or a northward migration of the intertropical convergence zone. Article in Journal/Newspaper North Atlantic BRGM: HAL (Bureau de Recherches Géologiques et Minières) Marine Geology 424 106159