New Geological Evidence of the 1755 Lisbon Tsunami from the Rock of Gibraltar (Southern Iberian Peninsula)

This paper presents the easternmost mineralogical and geochemical evidence of the 1755 Lisbon tsunami found in the Western Mediterranean. This multidisciplinary analysis of a sediment core obtained in Gibraltar (southern Iberian Peninsula) has allowed us to differentiate a tsunamiite from an old lag...

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Detalles Bibliográficos
Autores: Ruiz Muñoz, Francisco, Pozo, Manuel, González Regalado, María Luz, Rodríguez Vidal, Joaquín, Cáceres, Luis Miguel, Abad, Manuel, Izquierdo, Tatiana, Prudencio, María Isabel, Dias, María Isabel, Marques, Rosa, Muñoz Pichardo, Juan Manuel, Tosquella, Josep, Gómez, Paula, Toscano, Antonio, Romero, Verónica, Arroyo, Marta
Tipo de recurso: artículo
Estado:Versión publicada
Fecha de publicación:2021
País:España
Institución:Universidad de Sevilla (US)
Repositorio:idUS. Depósito de Investigación de la Universidad de Sevilla
OAI Identifier:oai:idus.us.es:11441/134944
Acceso en línea:https://hdl.handle.net/11441/134944
https://doi.org/10.3390/min11121397
Access Level:acceso abierto
Palabra clave:1755 Lisbon tsunami
Tsunamiite
Geological features
Gibraltar
Southern Iberian Peninsula
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spelling New Geological Evidence of the 1755 Lisbon Tsunami from the Rock of Gibraltar (Southern Iberian Peninsula)Ruiz Muñoz, FranciscoPozo, ManuelGonzález Regalado, María LuzRodríguez Vidal, JoaquínCáceres, Luis MiguelAbad, ManuelIzquierdo, TatianaPrudencio, María IsabelDias, María IsabelMarques, RosaMuñoz Pichardo, Juan ManuelTosquella, JosepGómez, PaulaToscano, AntonioRomero, VerónicaArroyo, Marta1755 Lisbon tsunamiTsunamiiteGeological featuresGibraltarSouthern Iberian PeninsulaThis paper presents the easternmost mineralogical and geochemical evidence of the 1755 Lisbon tsunami found in the Western Mediterranean. This multidisciplinary analysis of a sediment core obtained in Gibraltar (southern Iberian Peninsula) has allowed us to differentiate a tsunamiite from an old lagoon (The Inundation). This tsunamigenic layer has increased levels of calcite and aragonite and higher concentrations of Ba and ferromagnesian elements in comparison with the underlying lagoonal sediments of this core. This layer is also differentiated by its paleontological record, with the introduction of marine species within this lagoon. The uppermost part of the core includes a transition from swampy/marsh paleoenvironments to terrestrial scenarios, with a final anthropogenic filling occurring during the last century.MDPIEstadística e Investigación Operativa2021info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionapplication/pdfapplication/pdfhttps://hdl.handle.net/11441/134944https://doi.org/10.3390/min11121397reponame:idUS. Depósito de Investigación de la Universidad de Sevillainstname:Universidad de Sevilla (US)InglésMinerals, 11, 2-12.https://doi.org/10.3390/min11121397info:eu-repo/semantics/openAccessoai:idus.us.es:11441/1349442026-06-17T12:51:07Z
dc.title.none.fl_str_mv New Geological Evidence of the 1755 Lisbon Tsunami from the Rock of Gibraltar (Southern Iberian Peninsula)
title New Geological Evidence of the 1755 Lisbon Tsunami from the Rock of Gibraltar (Southern Iberian Peninsula)
spellingShingle New Geological Evidence of the 1755 Lisbon Tsunami from the Rock of Gibraltar (Southern Iberian Peninsula)
Ruiz Muñoz, Francisco
1755 Lisbon tsunami
Tsunamiite
Geological features
Gibraltar
Southern Iberian Peninsula
title_short New Geological Evidence of the 1755 Lisbon Tsunami from the Rock of Gibraltar (Southern Iberian Peninsula)
title_full New Geological Evidence of the 1755 Lisbon Tsunami from the Rock of Gibraltar (Southern Iberian Peninsula)
title_fullStr New Geological Evidence of the 1755 Lisbon Tsunami from the Rock of Gibraltar (Southern Iberian Peninsula)
title_full_unstemmed New Geological Evidence of the 1755 Lisbon Tsunami from the Rock of Gibraltar (Southern Iberian Peninsula)
title_sort New Geological Evidence of the 1755 Lisbon Tsunami from the Rock of Gibraltar (Southern Iberian Peninsula)
dc.creator.none.fl_str_mv Ruiz Muñoz, Francisco
Pozo, Manuel
González Regalado, María Luz
Rodríguez Vidal, Joaquín
Cáceres, Luis Miguel
Abad, Manuel
Izquierdo, Tatiana
Prudencio, María Isabel
Dias, María Isabel
Marques, Rosa
Muñoz Pichardo, Juan Manuel
Tosquella, Josep
Gómez, Paula
Toscano, Antonio
Romero, Verónica
Arroyo, Marta
author Ruiz Muñoz, Francisco
author_facet Ruiz Muñoz, Francisco
Pozo, Manuel
González Regalado, María Luz
Rodríguez Vidal, Joaquín
Cáceres, Luis Miguel
Abad, Manuel
Izquierdo, Tatiana
Prudencio, María Isabel
Dias, María Isabel
Marques, Rosa
Muñoz Pichardo, Juan Manuel
Tosquella, Josep
Gómez, Paula
Toscano, Antonio
Romero, Verónica
Arroyo, Marta
author_role author
author2 Pozo, Manuel
González Regalado, María Luz
Rodríguez Vidal, Joaquín
Cáceres, Luis Miguel
Abad, Manuel
Izquierdo, Tatiana
Prudencio, María Isabel
Dias, María Isabel
Marques, Rosa
Muñoz Pichardo, Juan Manuel
Tosquella, Josep
Gómez, Paula
Toscano, Antonio
Romero, Verónica
Arroyo, Marta
author2_role author
author
author
author
author
author
author
author
author
author
author
author
author
author
author
dc.contributor.none.fl_str_mv Estadística e Investigación Operativa
dc.subject.none.fl_str_mv 1755 Lisbon tsunami
Tsunamiite
Geological features
Gibraltar
Southern Iberian Peninsula
topic 1755 Lisbon tsunami
Tsunamiite
Geological features
Gibraltar
Southern Iberian Peninsula
description This paper presents the easternmost mineralogical and geochemical evidence of the 1755 Lisbon tsunami found in the Western Mediterranean. This multidisciplinary analysis of a sediment core obtained in Gibraltar (southern Iberian Peninsula) has allowed us to differentiate a tsunamiite from an old lagoon (The Inundation). This tsunamigenic layer has increased levels of calcite and aragonite and higher concentrations of Ba and ferromagnesian elements in comparison with the underlying lagoonal sediments of this core. This layer is also differentiated by its paleontological record, with the introduction of marine species within this lagoon. The uppermost part of the core includes a transition from swampy/marsh paleoenvironments to terrestrial scenarios, with a final anthropogenic filling occurring during the last century.
publishDate 2021
dc.date.none.fl_str_mv 2021
dc.type.none.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
format article
status_str publishedVersion
dc.identifier.none.fl_str_mv https://hdl.handle.net/11441/134944
https://doi.org/10.3390/min11121397
url https://hdl.handle.net/11441/134944
https://doi.org/10.3390/min11121397
dc.language.none.fl_str_mv Inglés
language_invalid_str_mv Inglés
dc.relation.none.fl_str_mv Minerals, 11, 2-12.
https://doi.org/10.3390/min11121397
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
eu_rights_str_mv openAccess
dc.format.none.fl_str_mv application/pdf
application/pdf
dc.publisher.none.fl_str_mv MDPI
publisher.none.fl_str_mv MDPI
dc.source.none.fl_str_mv reponame:idUS. Depósito de Investigación de la Universidad de Sevilla
instname:Universidad de Sevilla (US)
instname_str Universidad de Sevilla (US)
reponame_str idUS. Depósito de Investigación de la Universidad de Sevilla
collection idUS. Depósito de Investigación de la Universidad de Sevilla
repository.name.fl_str_mv
repository.mail.fl_str_mv
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score 15,300724

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