Environmental evolution of the Basque Coast Geopark estuaries (southern Bay of Biscay) during the last 10,000 years

In order to reconstruct the environmental evolution of the Deba and Urola estuaries located in the Basque Coast Geopark at millennial, centennial and decadal timescales, four long boreholes, three short cores and twelve surface samples were studied. Multiproxy analysis (foraminifera, trace metals an...

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Published in:Journal of Marine Systems
Main Authors: Cearreta, Alejandro, Irabien, María Jesús, Arozamena, José E. Gómez, El Bani Altuna, Naima, Goffard, Aintzane, García-Artola, Ane
Format: Article in Journal/Newspaper
Language:English
Published: Elsevier 2021
Subjects:
Online Access:https://hdl.handle.net/10037/21681
https://doi.org/10.1016/j.jmarsys.2021.103557
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author Cearreta, Alejandro
Irabien, María Jesús
Arozamena, José E. Gómez
El Bani Altuna, Naima
Goffard, Aintzane
García-Artola, Ane
author_facet Cearreta, Alejandro
Irabien, María Jesús
Arozamena, José E. Gómez
El Bani Altuna, Naima
Goffard, Aintzane
García-Artola, Ane
author_sort Cearreta, Alejandro
collection University of Tromsø: Munin Open Research Archive
container_start_page 103557
container_title Journal of Marine Systems
container_volume 219
description In order to reconstruct the environmental evolution of the Deba and Urola estuaries located in the Basque Coast Geopark at millennial, centennial and decadal timescales, four long boreholes, three short cores and twelve surface samples were studied. Multiproxy analysis (foraminifera, trace metals and radioisotopes) shows the temporal transformation of these estuaries in response to regional driving forces such as fresh-water discharge, relative sea-level (RSL) variation and the more recent impact of industrial development. At millennial and centennial timescales, the Deba estuary transformed from a tide-dominated to a river-dominated estuary at about 8000 yr cal BP following the decrease in RSL rise rate. This decrease also led to a reduction in both salinity and marine influence in the nearby tide-dominated Urola estuary. At decadal timescale, human disturbance on foraminiferal populations was found to be lower in the Deba estuary despite its higher level of contaminants in sediments. This was due to the greater impact of fresh-water discharge. In the Urola estuary, dredging operations altered severely the foraminiferal biota.
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genre Arctic
genre_facet Arctic
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op_doi https://doi.org/10.1016/j.jmarsys.2021.103557
op_relation Journal of Marine Systems
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FRIDAID 1906345
doi:10.1016/j.jmarsys.2021.103557
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spelling ftunivtroemsoe:oai:munin.uit.no:10037/21681 2025-04-13T14:11:29+00:00 Environmental evolution of the Basque Coast Geopark estuaries (southern Bay of Biscay) during the last 10,000 years Cearreta, Alejandro Irabien, María Jesús Arozamena, José E. Gómez El Bani Altuna, Naima Goffard, Aintzane García-Artola, Ane 2021-04-21 https://hdl.handle.net/10037/21681 https://doi.org/10.1016/j.jmarsys.2021.103557 eng eng Elsevier Journal of Marine Systems info:eu-repo/grantAgreement/RCN/SFF/223259/Norway/Centre for Arctic Gas Hydrate, Environment and Climate/CAGE/ FRIDAID 1906345 doi:10.1016/j.jmarsys.2021.103557 https://hdl.handle.net/10037/21681 openAccess Copyright 2021 The Author(s) VDP::Mathematics and natural science: 400::Geosciences: 450::Marine geology: 466 VDP::Matematikk og Naturvitenskap: 400::Geofag: 450::Marin geologi: 466 Journal article Tidsskriftartikkel Peer reviewed publishedVersion 2021 ftunivtroemsoe https://doi.org/10.1016/j.jmarsys.2021.103557 2025-03-14T05:17:55Z In order to reconstruct the environmental evolution of the Deba and Urola estuaries located in the Basque Coast Geopark at millennial, centennial and decadal timescales, four long boreholes, three short cores and twelve surface samples were studied. Multiproxy analysis (foraminifera, trace metals and radioisotopes) shows the temporal transformation of these estuaries in response to regional driving forces such as fresh-water discharge, relative sea-level (RSL) variation and the more recent impact of industrial development. At millennial and centennial timescales, the Deba estuary transformed from a tide-dominated to a river-dominated estuary at about 8000 yr cal BP following the decrease in RSL rise rate. This decrease also led to a reduction in both salinity and marine influence in the nearby tide-dominated Urola estuary. At decadal timescale, human disturbance on foraminiferal populations was found to be lower in the Deba estuary despite its higher level of contaminants in sediments. This was due to the greater impact of fresh-water discharge. In the Urola estuary, dredging operations altered severely the foraminiferal biota. Article in Journal/Newspaper Arctic University of Tromsø: Munin Open Research Archive Journal of Marine Systems 219 103557
spellingShingle VDP::Mathematics and natural science: 400::Geosciences: 450::Marine geology: 466
VDP::Matematikk og Naturvitenskap: 400::Geofag: 450::Marin geologi: 466
Cearreta, Alejandro
Irabien, María Jesús
Arozamena, José E. Gómez
El Bani Altuna, Naima
Goffard, Aintzane
García-Artola, Ane
Environmental evolution of the Basque Coast Geopark estuaries (southern Bay of Biscay) during the last 10,000 years
title Environmental evolution of the Basque Coast Geopark estuaries (southern Bay of Biscay) during the last 10,000 years
title_full Environmental evolution of the Basque Coast Geopark estuaries (southern Bay of Biscay) during the last 10,000 years
title_fullStr Environmental evolution of the Basque Coast Geopark estuaries (southern Bay of Biscay) during the last 10,000 years
title_full_unstemmed Environmental evolution of the Basque Coast Geopark estuaries (southern Bay of Biscay) during the last 10,000 years
title_short Environmental evolution of the Basque Coast Geopark estuaries (southern Bay of Biscay) during the last 10,000 years
title_sort environmental evolution of the basque coast geopark estuaries (southern bay of biscay) during the last 10,000 years
topic VDP::Mathematics and natural science: 400::Geosciences: 450::Marine geology: 466
VDP::Matematikk og Naturvitenskap: 400::Geofag: 450::Marin geologi: 466
topic_facet VDP::Mathematics and natural science: 400::Geosciences: 450::Marine geology: 466
VDP::Matematikk og Naturvitenskap: 400::Geofag: 450::Marin geologi: 466
url https://hdl.handle.net/10037/21681
https://doi.org/10.1016/j.jmarsys.2021.103557