Holocene paleoenvironmental reconstructions in the Bay of Brest

International audience The Bay of Brest is a semi-enclosed basin of 180 km2 subject to tidal dynamics and to the fluvial influences of both Aulne and Elorn Rivers, which drain watersheds representing 2600 km2 around the Bay, the major one being the Aulne River catchment. This coastal environment, at...

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Main Authors: Valero, Clara, Lambert, Clément, Vidal, Muriel, Stéphan, Pierre, Pailler, Yvan, Ehrhold, Axel, Penaud, Aurélie
Other Authors: Geo-Ocean (GEO-OCEAN), Université de Bretagne Sud (UBS)-Institut Français de Recherche pour l'Exploitation de la Mer (IFREMER)-Université de Brest (UBO)-Centre National de la Recherche Scientifique (CNRS), Littoral, Environnement, Télédétection, Géomatique (LETG - Brest), Université de Brest (UBO)-Université de Rennes 2 (UR2)-Institut Universitaire Européen de la Mer (IUEM), Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Brest (UBO)-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Centre National de la Recherche Scientifique (CNRS)-Nantes Université (Nantes Univ)-Littoral, Environnement, Télédétection, Géomatique UMR 6554 (LETG), Université de Brest (UBO)-Université de Rennes 2 (UR2)-Centre National de la Recherche Scientifique (CNRS)-Institut de Géographie et d'Aménagement Régional de l'Université de Nantes (Nantes Univ - IGARUN), Nantes Université - pôle Humanités, Nantes Université (Nantes Univ)-Nantes Université (Nantes Univ)-Nantes Université - pôle Humanités, Nantes Université (Nantes Univ)-Nantes Université (Nantes Univ)-Institut de Géographie et d'Aménagement Régional de l'Université de Nantes (Nantes Univ - IGARUN), Nantes Université (Nantes Univ), Association des Sédimentologistes Français
Format: Conference Object
Language:English
Published: HAL CCSD 2022
Subjects:
Online Access:https://hal.science/hal-03908154
id ftinsu:oai:HAL:hal-03908154v1
record_format openpolar
institution Open Polar
collection Institut national des sciences de l'Univers: HAL-INSU
op_collection_id ftinsu
language English
topic Holocene
Bay of Brest
Palynology
Precipitation regimes
Anthropisation
[SDU.STU.GM]Sciences of the Universe [physics]/Earth Sciences/Geomorphology
spellingShingle Holocene
Bay of Brest
Palynology
Precipitation regimes
Anthropisation
[SDU.STU.GM]Sciences of the Universe [physics]/Earth Sciences/Geomorphology
Valero, Clara
Lambert, Clément
Vidal, Muriel
Stéphan, Pierre
Pailler, Yvan
Ehrhold, Axel
Penaud, Aurélie
Holocene paleoenvironmental reconstructions in the Bay of Brest
topic_facet Holocene
Bay of Brest
Palynology
Precipitation regimes
Anthropisation
[SDU.STU.GM]Sciences of the Universe [physics]/Earth Sciences/Geomorphology
description International audience The Bay of Brest is a semi-enclosed basin of 180 km2 subject to tidal dynamics and to the fluvial influences of both Aulne and Elorn Rivers, which drain watersheds representing 2600 km2 around the Bay, the major one being the Aulne River catchment. This coastal environment, at the land-sea interface, is subject to natural climate oscillations, typical of the North Atlantic Basin, with the superimposed paleoenvironmental transformations inherited from the post-glacial sea level rise and the anthropogenic forcing increasing from the Neolithic (6,950 ka BP) and especially from the Bronze Age (4,200 ka BP). Therefore, it is an ideal site for the reconstruction of the interactions and retroactions between climate, environment and human dynamics at the western tip of Brittany. To that end, a Holocene paleoenvironmental study was conducted thanks to eight cores collected around the Bay of Brest in four different subtidal areas (i.e., the Roscanvel Bay, the Brest Harbour, the South of the Plougastel peninsula and the mouth of the Aulne River) more or less impacted by oceanic vs. fluvial influences. First, a spatial comparison of pollen and dinoflagellate cyst (or dinocyst) assemblages (terrestrial and aquatic bioindicators, respectively) was conducted thanks to cores retrieved at the mouth of the Aulne River (twin cores "F" and "KS22"; major fluvial influence) and close to the Brest Harbour (twin cores "KS06" and "KS05"; increasing oceanic influence), on same time intervals encompassing 200 years: i) first around 4 ka BP and ii) second around 1 ka BP. Both spatial comparisons allowed recognizing fluvialpalynological tracers among palynological assemblages (Alnus and Corylus for pollen taxa; L. machaerophorum for dinocyst ones). This spatio-temporal investigation was then discussed in parallel with palynological data acquired on the southern Brittany shelf over the last 7 kyrs BP (core CBT-CS11). This allowed discussing the synchronous character of environmental observations considered as ...
author2 Geo-Ocean (GEO-OCEAN)
Université de Bretagne Sud (UBS)-Institut Français de Recherche pour l'Exploitation de la Mer (IFREMER)-Université de Brest (UBO)-Centre National de la Recherche Scientifique (CNRS)
Littoral, Environnement, Télédétection, Géomatique (LETG - Brest)
Université de Brest (UBO)-Université de Rennes 2 (UR2)-Institut Universitaire Européen de la Mer (IUEM)
Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Brest (UBO)-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Centre National de la Recherche Scientifique (CNRS)-Nantes Université (Nantes Univ)-Littoral, Environnement, Télédétection, Géomatique UMR 6554 (LETG)
Université de Brest (UBO)-Université de Rennes 2 (UR2)-Centre National de la Recherche Scientifique (CNRS)-Institut de Géographie et d'Aménagement Régional de l'Université de Nantes (Nantes Univ - IGARUN)
Nantes Université - pôle Humanités
Nantes Université (Nantes Univ)-Nantes Université (Nantes Univ)-Nantes Université - pôle Humanités
Nantes Université (Nantes Univ)-Nantes Université (Nantes Univ)-Institut de Géographie et d'Aménagement Régional de l'Université de Nantes (Nantes Univ - IGARUN)
Nantes Université (Nantes Univ)
Association des Sédimentologistes Français
format Conference Object
author Valero, Clara
Lambert, Clément
Vidal, Muriel
Stéphan, Pierre
Pailler, Yvan
Ehrhold, Axel
Penaud, Aurélie
author_facet Valero, Clara
Lambert, Clément
Vidal, Muriel
Stéphan, Pierre
Pailler, Yvan
Ehrhold, Axel
Penaud, Aurélie
author_sort Valero, Clara
title Holocene paleoenvironmental reconstructions in the Bay of Brest
title_short Holocene paleoenvironmental reconstructions in the Bay of Brest
title_full Holocene paleoenvironmental reconstructions in the Bay of Brest
title_fullStr Holocene paleoenvironmental reconstructions in the Bay of Brest
title_full_unstemmed Holocene paleoenvironmental reconstructions in the Bay of Brest
title_sort holocene paleoenvironmental reconstructions in the bay of brest
publisher HAL CCSD
publishDate 2022
url https://hal.science/hal-03908154
op_coverage Brest, France
genre North Atlantic
genre_facet North Atlantic
op_source 18ème Congrès Français de Sédimentologie
https://hal.science/hal-03908154
18ème Congrès Français de Sédimentologie, Association des Sédimentologistes Français, Sep 2022, Brest, France
op_relation hal-03908154
https://hal.science/hal-03908154
_version_ 1790604659965034496
spelling ftinsu:oai:HAL:hal-03908154v1 2024-02-11T10:06:45+01:00 Holocene paleoenvironmental reconstructions in the Bay of Brest Valero, Clara Lambert, Clément Vidal, Muriel Stéphan, Pierre Pailler, Yvan Ehrhold, Axel Penaud, Aurélie Geo-Ocean (GEO-OCEAN) Université de Bretagne Sud (UBS)-Institut Français de Recherche pour l'Exploitation de la Mer (IFREMER)-Université de Brest (UBO)-Centre National de la Recherche Scientifique (CNRS) Littoral, Environnement, Télédétection, Géomatique (LETG - Brest) Université de Brest (UBO)-Université de Rennes 2 (UR2)-Institut Universitaire Européen de la Mer (IUEM) Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Brest (UBO)-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Centre National de la Recherche Scientifique (CNRS)-Nantes Université (Nantes Univ)-Littoral, Environnement, Télédétection, Géomatique UMR 6554 (LETG) Université de Brest (UBO)-Université de Rennes 2 (UR2)-Centre National de la Recherche Scientifique (CNRS)-Institut de Géographie et d'Aménagement Régional de l'Université de Nantes (Nantes Univ - IGARUN) Nantes Université - pôle Humanités Nantes Université (Nantes Univ)-Nantes Université (Nantes Univ)-Nantes Université - pôle Humanités Nantes Université (Nantes Univ)-Nantes Université (Nantes Univ)-Institut de Géographie et d'Aménagement Régional de l'Université de Nantes (Nantes Univ - IGARUN) Nantes Université (Nantes Univ) Association des Sédimentologistes Français Brest, France 2022-09-28 https://hal.science/hal-03908154 en eng HAL CCSD hal-03908154 https://hal.science/hal-03908154 18ème Congrès Français de Sédimentologie https://hal.science/hal-03908154 18ème Congrès Français de Sédimentologie, Association des Sédimentologistes Français, Sep 2022, Brest, France Holocene Bay of Brest Palynology Precipitation regimes Anthropisation [SDU.STU.GM]Sciences of the Universe [physics]/Earth Sciences/Geomorphology info:eu-repo/semantics/conferenceObject Conference papers 2022 ftinsu 2024-01-24T17:27:39Z International audience The Bay of Brest is a semi-enclosed basin of 180 km2 subject to tidal dynamics and to the fluvial influences of both Aulne and Elorn Rivers, which drain watersheds representing 2600 km2 around the Bay, the major one being the Aulne River catchment. This coastal environment, at the land-sea interface, is subject to natural climate oscillations, typical of the North Atlantic Basin, with the superimposed paleoenvironmental transformations inherited from the post-glacial sea level rise and the anthropogenic forcing increasing from the Neolithic (6,950 ka BP) and especially from the Bronze Age (4,200 ka BP). Therefore, it is an ideal site for the reconstruction of the interactions and retroactions between climate, environment and human dynamics at the western tip of Brittany. To that end, a Holocene paleoenvironmental study was conducted thanks to eight cores collected around the Bay of Brest in four different subtidal areas (i.e., the Roscanvel Bay, the Brest Harbour, the South of the Plougastel peninsula and the mouth of the Aulne River) more or less impacted by oceanic vs. fluvial influences. First, a spatial comparison of pollen and dinoflagellate cyst (or dinocyst) assemblages (terrestrial and aquatic bioindicators, respectively) was conducted thanks to cores retrieved at the mouth of the Aulne River (twin cores "F" and "KS22"; major fluvial influence) and close to the Brest Harbour (twin cores "KS06" and "KS05"; increasing oceanic influence), on same time intervals encompassing 200 years: i) first around 4 ka BP and ii) second around 1 ka BP. Both spatial comparisons allowed recognizing fluvialpalynological tracers among palynological assemblages (Alnus and Corylus for pollen taxa; L. machaerophorum for dinocyst ones). This spatio-temporal investigation was then discussed in parallel with palynological data acquired on the southern Brittany shelf over the last 7 kyrs BP (core CBT-CS11). This allowed discussing the synchronous character of environmental observations considered as ... Conference Object North Atlantic Institut national des sciences de l'Univers: HAL-INSU