dc.creator | Abad, M | es |
dc.creator | Rodríguez Vidal, Joaquín | es |
dc.creator | Aboumaria, K. | es |
dc.creator | Zaghloul, M. N. | es |
dc.creator | Ruiz, F. | es |
dc.creator | Martínez Aguirre, Aránzazu | es |
dc.creator | Izquierdo, Tatiana | es |
dc.creator | Chamorro, S. | es |
dc.date.accessioned | 2022-09-14T10:53:26Z | |
dc.date.available | 2022-09-14T10:53:26Z | |
dc.date.issued | 2013 | |
dc.identifier.citation | Abad, M., Rodríguez Vidal, J., Aboumaria, K., Zaghloul, M.N., Ruiz, F., Martínez Aguirre, A.,...,Chamorro, S. (2013). Evidence of MIS 5 sea-level highstands in Gebel Mousa coast (Strait of Gibraltar, North of Africa). Geomorphology, 182 (January 2013), 133-146. | |
dc.identifier.issn | 0169-555X | es |
dc.identifier.uri | https://hdl.handle.net/11441/137056 | |
dc.description.abstract | The Last Interglacial is considered the most suitable episode from which to infer patterns of rapid sea-level change since its climatic
conditions were similar to those of the present interglacial. However, specifying the true position of its sea level with high accuracy is
very troublesome in the absence of sedimentological, erosional or even palaeontological markers. This study investigates the
morphosedimentary evidence (beach deposits, cliff, notch and shore platform) of two highstands registered and dated during MIS 5
stage by U-series dating in the North of Morocco (Strait of Gibraltar). Bioerosive notches and mixed siliciclastic and carbonate
deposits, high energy beaches with algal bioherms, were formed in coastal environments during MIS 5a. A sea-level height of +10 m
asl can be inferred for this substage. The record of MIS 5e substage is less defined in the geomorphological record, consisting of
backshore/foreshore deposits located at +13 to +15 m asl. A tectonic uplift rate of ~0.1 mm/yr has been estimated for the last 130
kyr. These data are consistent with models of coastal uplifting calculated for the Strait of Gibraltar. | es |
dc.description.sponsorship | Ministerio de Ciencia e Innovación CGL2010-15810/BTE | es |
dc.format | application/pdf | es |
dc.format.extent | 14 | es |
dc.language.iso | eng | es |
dc.publisher | Elsevier | es |
dc.relation.ispartof | Geomorphology, 182 (January 2013), 133-146. | |
dc.rights | Attribution-NonCommercial-NoDerivatives 4.0 Internacional | * |
dc.rights.uri | http://creativecommons.org/licenses/by-nc-nd/4.0/ | * |
dc.subject | Marine terrace | es |
dc.subject | Notch | es |
dc.subject | MIS 5 | es |
dc.subject | U-series dating | es |
dc.subject | Strait of Gibraltar | es |
dc.subject | Morocco | es |
dc.title | Evidence of MIS 5 sea-level highstands in Gebel Mousa coast (Strait of Gibraltar, North of Africa) | es |
dc.type | info:eu-repo/semantics/article | es |
dcterms.identifier | https://ror.org/03yxnpp24 | |
dc.type.version | info:eu-repo/semantics/submittedVersion | es |
dc.rights.accessRights | info:eu-repo/semantics/openAccess | es |
dc.contributor.affiliation | Universidad de Sevilla. Departamento de Física Aplicada I | es |
dc.relation.projectID | CGL2010-15810/BTE | es |
dc.relation.publisherversion | https://www.sciencedirect.com/science/article/pii/S0169555X12005016?via%3Dihub | es |
dc.identifier.doi | 10.1016/j.geomorph.2012.11.004 | es |
dc.journaltitle | Geomorphology | es |
dc.publication.volumen | 182 | es |
dc.publication.issue | January 2013 | es |
dc.publication.initialPage | 133 | es |
dc.publication.endPage | 146 | es |
dc.identifier.sisius | 20455742 | es |
dc.contributor.funder | Ministerio de Ciencia e Innovación (MICIN). España | es |