Record of the last interglacial sea level highstand based on new coastal deposits in the Cantabrian margin (northern Iberian Peninsula)

Quaternary sea level fluctuations have been responsible for significant remodelling of coastal landscapes, generating distinctive sea level indicators at different positions and altitudes that are still visible today. Raised coastal deposits are among the characteristic features of significant value...

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Detalles Bibliográficos
Autores: Bilbao Lasa, Peru, Aranburu Artano, Arantza, Álvarez González, Irantzu, Del Val Blanco, Miren, Cheng, Hai, Arriolabengoa Zubizarreta, Martín, Iriarte Avilés, Eneko
Tipo de recurso: artículo
Fecha de publicación:2023
País:España
Institución:Universidad del País Vasco
Repositorio:Addi. Archivo Digital para la Docencia y la Investigación
OAI Identifier:oai:addi.ehu.eus:10810/71041
Acceso en línea:http://hdl.handle.net/10810/71041
Access Level:acceso abierto
Palabra clave:Sea level highstand, MIS 5 Interglacial, geochronology, Quaternary, Northern Iberia
sea level highstand
MIS 5 Interglacial
geochronology
quaternary
northern Iberia
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spelling Record of the last interglacial sea level highstand based on new coastal deposits in the Cantabrian margin (northern Iberian Peninsula)Bilbao Lasa, PeruAranburu Artano, ArantzaÁlvarez González, IrantzuDel Val Blanco, MirenCheng, HaiArriolabengoa Zubizarreta, MartínIriarte Avilés, EnekoSea level highstand, MIS 5 Interglacial, geochronology, Quaternary, Northern Iberiasea level highstandMIS 5 Interglacialgeochronologyquaternarynorthern IberiaQuaternary sea level fluctuations have been responsible for significant remodelling of coastal landscapes, generating distinctive sea level indicators at different positions and altitudes that are still visible today. Raised coastal deposits are among the characteristic features of significant value in reconstructing the tectonic and sea-level history of the areas in which they are preserved. To date, few remnants of Quaternary coastal deposits have been described and directly dated along the coast of the Cantabrian margin (on the north of the Iberian Peninsula). In this work, two new deposits located in the towns of Castro-Urdiales and Mendexa were analysed and dated using U/Th geochronology and Optically Stimulated Luminescence. Considering the ages and altitudes of these deposits, it seems most likely that they correlate to the Marine Isotope Stage (MIS) 5e. Furthermore, the data acquired suggest that most of the Cantabrian margin underwent a similar tectonic evolution, with no significant tectonic uplift, since at least MIS 5e.Elsevier202420242023info:eu-repo/semantics/articleapplication/pdfhttp://hdl.handle.net/10810/71041reponame:Addi. Archivo Digital para la Docencia y la Investigacióninstname:Universidad del País VascoIngléshttps://doi.org/10.1016/j.csr.2023.105096info:eu-repo/semantics/openAccesshttp://creativecommons.org/licenses/by-nc-nd/3.0/es/© 2023 Elsevier under CC BY-NC-NDoai:addi.ehu.eus:10810/710412026-06-18T09:23:17Z
dc.title.none.fl_str_mv Record of the last interglacial sea level highstand based on new coastal deposits in the Cantabrian margin (northern Iberian Peninsula)
title Record of the last interglacial sea level highstand based on new coastal deposits in the Cantabrian margin (northern Iberian Peninsula)
spellingShingle Record of the last interglacial sea level highstand based on new coastal deposits in the Cantabrian margin (northern Iberian Peninsula)
Bilbao Lasa, Peru
Sea level highstand, MIS 5 Interglacial, geochronology, Quaternary, Northern Iberia
sea level highstand
MIS 5 Interglacial
geochronology
quaternary
northern Iberia
title_short Record of the last interglacial sea level highstand based on new coastal deposits in the Cantabrian margin (northern Iberian Peninsula)
title_full Record of the last interglacial sea level highstand based on new coastal deposits in the Cantabrian margin (northern Iberian Peninsula)
title_fullStr Record of the last interglacial sea level highstand based on new coastal deposits in the Cantabrian margin (northern Iberian Peninsula)
title_full_unstemmed Record of the last interglacial sea level highstand based on new coastal deposits in the Cantabrian margin (northern Iberian Peninsula)
title_sort Record of the last interglacial sea level highstand based on new coastal deposits in the Cantabrian margin (northern Iberian Peninsula)
dc.creator.none.fl_str_mv Bilbao Lasa, Peru
Aranburu Artano, Arantza
Álvarez González, Irantzu
Del Val Blanco, Miren
Cheng, Hai
Arriolabengoa Zubizarreta, Martín
Iriarte Avilés, Eneko
author Bilbao Lasa, Peru
author_facet Bilbao Lasa, Peru
Aranburu Artano, Arantza
Álvarez González, Irantzu
Del Val Blanco, Miren
Cheng, Hai
Arriolabengoa Zubizarreta, Martín
Iriarte Avilés, Eneko
author_role author
author2 Aranburu Artano, Arantza
Álvarez González, Irantzu
Del Val Blanco, Miren
Cheng, Hai
Arriolabengoa Zubizarreta, Martín
Iriarte Avilés, Eneko
author2_role author
author
author
author
author
author
dc.subject.none.fl_str_mv Sea level highstand, MIS 5 Interglacial, geochronology, Quaternary, Northern Iberia
sea level highstand
MIS 5 Interglacial
geochronology
quaternary
northern Iberia
topic Sea level highstand, MIS 5 Interglacial, geochronology, Quaternary, Northern Iberia
sea level highstand
MIS 5 Interglacial
geochronology
quaternary
northern Iberia
description Quaternary sea level fluctuations have been responsible for significant remodelling of coastal landscapes, generating distinctive sea level indicators at different positions and altitudes that are still visible today. Raised coastal deposits are among the characteristic features of significant value in reconstructing the tectonic and sea-level history of the areas in which they are preserved. To date, few remnants of Quaternary coastal deposits have been described and directly dated along the coast of the Cantabrian margin (on the north of the Iberian Peninsula). In this work, two new deposits located in the towns of Castro-Urdiales and Mendexa were analysed and dated using U/Th geochronology and Optically Stimulated Luminescence. Considering the ages and altitudes of these deposits, it seems most likely that they correlate to the Marine Isotope Stage (MIS) 5e. Furthermore, the data acquired suggest that most of the Cantabrian margin underwent a similar tectonic evolution, with no significant tectonic uplift, since at least MIS 5e.
publishDate 2023
dc.date.none.fl_str_mv 2023
2024
2024
dc.type.none.fl_str_mv info:eu-repo/semantics/article
format article
dc.identifier.none.fl_str_mv http://hdl.handle.net/10810/71041
url http://hdl.handle.net/10810/71041
dc.language.none.fl_str_mv Inglés
language_invalid_str_mv Inglés
dc.relation.none.fl_str_mv https://doi.org/10.1016/j.csr.2023.105096
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
http://creativecommons.org/licenses/by-nc-nd/3.0/es/
© 2023 Elsevier under CC BY-NC-ND
eu_rights_str_mv openAccess
rights_invalid_str_mv http://creativecommons.org/licenses/by-nc-nd/3.0/es/
© 2023 Elsevier under CC BY-NC-ND
dc.format.none.fl_str_mv application/pdf
dc.publisher.none.fl_str_mv Elsevier
publisher.none.fl_str_mv Elsevier
dc.source.none.fl_str_mv reponame:Addi. Archivo Digital para la Docencia y la Investigación
instname:Universidad del País Vasco
instname_str Universidad del País Vasco
reponame_str Addi. Archivo Digital para la Docencia y la Investigación
collection Addi. Archivo Digital para la Docencia y la Investigación
repository.name.fl_str_mv
repository.mail.fl_str_mv
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score 15,812455

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