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Paleolandscape evolution along the coasts of the Baixo Alentejo (Portugal) during the Quaternary

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dc.contributor.authorGoy, J.L.
dc.contributor.authorRoquero, E.
dc.contributor.authorZazo Cardeña, Caridad
dc.contributor.authorMoura, D. Maria
dc.contributor.authorDabrio, Cristino José
dc.contributor.authorBoski, Tomasz
dc.contributor.authorMartínez Graña, Antonio Miguel
dc.contributor.authorLario Gómez, Javier
dc.contributor.authorBardají, Teresa
dc.contributor.orcidhttps://orcid.org/0000-0002-0952-6805
dc.contributor.orcidhttps://orcid.org/0000-0003-2462-4179
dc.contributor.orcidhttps://orcid.org/0000-0003-2242-5192
dc.contributor.orcidhttps://orcid.org/0000-0003-2988-8077
dc.date.accessioned2025-01-09T11:10:54Z
dc.date.available2025-01-09T11:10:54Z
dc.date.issued2024-10-01
dc.descriptionThis is the Accepted Manuscript of an article published by Elsevier in "Quaternary International" on 2024, available online: https://doi.org/10.1016/j.quaint.2024.07.006 Este es el manuscrito aceptado de un artículo publicado por Elsevier en "Quaternary International" on 2024, disponible en línea: https://doi.org/10.1016/j.quaint.2024.07.006
dc.description.abstractA detailed geomorphological mapping allowed to understand the complex relationships interplayed between local tectonics and sedimentation across the coastal area of the Baixo Alentejo (Portugal) all along the Quaternary. Different outcrops of coastal sediments between Sines and Vilanova de Milfontes permitted to reconstruct a general sequence of up to fifteen stair-cased marine terraces, while wide sequences of alluvial fans develop in the hinterland. The distinct geomorphological disposition of these alluvial fans together with the presence/absence of marine terraces, have allowed to define different phases of paleolandscape evolution based both in sea level changes and differential uplift. A dune system has been attributed to MIS 5e in basis of OSL, and 14C and U-series dating permitted the adscription of a beach unit to MIS 5. These data allowed to stablish the relative chronology of the entire marine terrace sequence and to determine the vertical movement rates along the studied coastal area. The results give values ranging from slight uplift (+0.015mm/a) to subtle subsidence (−0.030 mm/a), coinciding with other author's determinations.en
dc.description.versionversión final
dc.identifier.citationGOY, J.L.; ROQUERO, E.; ZAZO, C.; MOURA, D.; DABRIO, C.J.; BOSKI, T.; MARTÍNEZ-GRAÑA, A.; LARIO, J.; BARDAJÍ, T. (2024). Paleolandscape evolution along the coasts of the Baixo Alentejo (Portugal) during the Quaternary. Quaternary International, 706, 60-75. https://doi.org/10.1016/j.quaint.2024.07.006.
dc.identifier.doihttps://doi.org/10.1016/j.quaint.2024.07.006
dc.identifier.issn1040-6182
dc.identifier.urihttps://hdl.handle.net/20.500.14468/25144
dc.journal.titleQuaternary International
dc.journal.volume706
dc.language.isoen
dc.page.final75
dc.page.initial60
dc.publisherELSEVIER
dc.relation.centerFacultad de Ciencias
dc.relation.departmentCiencias Analíticas
dc.relation.researchgroupGeología Aplicada al Medio Ambiente (GAMA)
dc.rightsinfo:eu-repo/semantics/openAccess
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/4.0/deed.es
dc.subject.keywordsgeomorphological mappingen
dc.subject.keywordsmarine terracesen
dc.subject.keywordsmorphostructural analysesen
dc.subject.keywordscoastal vertical motionen
dc.titlePaleolandscape evolution along the coasts of the Baixo Alentejo (Portugal) during the Quaternaryen
dc.typeartículoes
dc.typejournal articleen
dspace.entity.typePublication
person.familyNameLario Gómez
person.givenNameJavier
person.identifier.orcid0000-0002-2582-5354
relation.isAuthorOfPublication2f4b8f5c-b4e0-4ed9-a55b-3d876e694b19
relation.isAuthorOfPublication.latestForDiscovery2f4b8f5c-b4e0-4ed9-a55b-3d876e694b19
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