Reconstructing past sea-level changes from storm-built beach ridges

Autores
Rovere, Alessio; Pappalardo, Marta; Richiano, Sebastián Miguel; Ryan, Deirdre D.; Rubio Sandoval, Karla; Ruiz, Patricio Martin; Montes, Alejandro; Gowan, Evan J.
Año de publicación
2025
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
Storm-built beach ridges, built by waves on sedimentary coasts, can be used as geomorphological indicators of past sea level. However, quantifying the relationship between the geomorphological elements of the ridge and the paleo sea level at the time of deposition is difficult, as a beach ridge is primarily correlated to wave energy and only secondarily to the position of sea level. In this work, we propose a methodology to quantify the upper and lower limits of a storm-built beach ridge based on remote sensing data. We use the tidal model FES2022, data from the Copernicus Marine Service and beach slope gathered from satellite imagery as inputs to different wave runup models, that are used to calculate the limits of the storm-built beach ridge. We test our approach on a particularly well-preserved Pleistocene storm-built beach ridge in Patagonia, Argentina. Our results show that the paleo relative sea level reconstructed using remote sensing data coincides (82.8 % similarity) with that obtained from measured modern analog landforms at the same location.
Fil: Rovere, Alessio. Universitat Bremen; Alemania. Universita' Ca' Foscari Di Venezia; Italia
Fil: Pappalardo, Marta. Università degli Studi di Pisa; Italia
Fil: Richiano, Sebastián Miguel. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Centro Nacional Patagónico. Instituto Patagónico de Geología y Paleontología; Argentina
Fil: Ryan, Deirdre D.. Università degli Studi di Pisa; Italia
Fil: Rubio Sandoval, Karla. Universitat Bremen; Alemania
Fil: Ruiz, Patricio Martin. Universidad Nacional de la Patagonia "San Juan Bosco". Facultad de Ciencias Naturales - Sede Comodoro. Departamento de Geología; Argentina
Fil: Montes, Alejandro. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; Argentina. Universidad Nacional de Tierra del Fuego, Antártida e Islas del Atlántico Sur. Instituto de Ciencias Polares, Ambientales y Recursos Naturales; Argentina
Fil: Gowan, Evan J.. Kumamoto University; Japón. KIKAI Institute for Coral Reef Sciences; Japón
Materia
PLEISTOCENE SEA LEVEL
BEACH RIDGES
PATAGONIA ARGENTINA
PALEO SEA LEVEL
Nivel de accesibilidad
acceso abierto
Condiciones de uso
https://creativecommons.org/licenses/by/2.5/ar/
Repositorio
CONICET Digital (CONICET)
Institución
Consejo Nacional de Investigaciones Científicas y Técnicas
OAI Identificador
oai:ri.conicet.gov.ar:11336/260512
Acceder
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network_acronym_str CONICETDig
repository_id_str 3498
network_name_str CONICET Digital (CONICET)
spelling Reconstructing past sea-level changes from storm-built beach ridgesRovere, AlessioPappalardo, MartaRichiano, Sebastián MiguelRyan, Deirdre D.Rubio Sandoval, KarlaRuiz, Patricio MartinMontes, AlejandroGowan, Evan J.PLEISTOCENE SEA LEVELBEACH RIDGESPATAGONIA ARGENTINAPALEO SEA LEVELhttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1Storm-built beach ridges, built by waves on sedimentary coasts, can be used as geomorphological indicators of past sea level. However, quantifying the relationship between the geomorphological elements of the ridge and the paleo sea level at the time of deposition is difficult, as a beach ridge is primarily correlated to wave energy and only secondarily to the position of sea level. In this work, we propose a methodology to quantify the upper and lower limits of a storm-built beach ridge based on remote sensing data. We use the tidal model FES2022, data from the Copernicus Marine Service and beach slope gathered from satellite imagery as inputs to different wave runup models, that are used to calculate the limits of the storm-built beach ridge. We test our approach on a particularly well-preserved Pleistocene storm-built beach ridge in Patagonia, Argentina. Our results show that the paleo relative sea level reconstructed using remote sensing data coincides (82.8 % similarity) with that obtained from measured modern analog landforms at the same location.Fil: Rovere, Alessio. Universitat Bremen; Alemania. Universita' Ca' Foscari Di Venezia; ItaliaFil: Pappalardo, Marta. Università degli Studi di Pisa; ItaliaFil: Richiano, Sebastián Miguel. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Centro Nacional Patagónico. Instituto Patagónico de Geología y Paleontología; ArgentinaFil: Ryan, Deirdre D.. Università degli Studi di Pisa; ItaliaFil: Rubio Sandoval, Karla. Universitat Bremen; AlemaniaFil: Ruiz, Patricio Martin. Universidad Nacional de la Patagonia "San Juan Bosco". Facultad de Ciencias Naturales - Sede Comodoro. Departamento de Geología; ArgentinaFil: Montes, Alejandro. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; Argentina. Universidad Nacional de Tierra del Fuego, Antártida e Islas del Atlántico Sur. Instituto de Ciencias Polares, Ambientales y Recursos Naturales; ArgentinaFil: Gowan, Evan J.. Kumamoto University; Japón. KIKAI Institute for Coral Reef Sciences; JapónElsevier Science2025-05info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/260512Rovere, Alessio; Pappalardo, Marta; Richiano, Sebastián Miguel; Ryan, Deirdre D.; Rubio Sandoval, Karla; et al.; Reconstructing past sea-level changes from storm-built beach ridges; Elsevier Science; Geomorphology; 476; 109659; 5-2025; 1-100169-555XCONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/https://www.sciencedirect.com/science/article/pii/S0169555X25000698info:eu-repo/semantics/altIdentifier/doi/10.1016/j.geomorph.2025.109659info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-03T09:47:42Zoai:ri.conicet.gov.ar:11336/260512instacron:CONICETInstitucionalhttp://ri.conicet.gov.ar/Organismo científico-tecnológicoNo correspondehttp://ri.conicet.gov.ar/oai/requestdasensio@conicet.gov.ar; lcarlino@conicet.gov.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:34982025-09-03 09:47:42.331CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Reconstructing past sea-level changes from storm-built beach ridges
title Reconstructing past sea-level changes from storm-built beach ridges
spellingShingle Reconstructing past sea-level changes from storm-built beach ridges
Rovere, Alessio
PLEISTOCENE SEA LEVEL
BEACH RIDGES
PATAGONIA ARGENTINA
PALEO SEA LEVEL
title_short Reconstructing past sea-level changes from storm-built beach ridges
title_full Reconstructing past sea-level changes from storm-built beach ridges
title_fullStr Reconstructing past sea-level changes from storm-built beach ridges
title_full_unstemmed Reconstructing past sea-level changes from storm-built beach ridges
title_sort Reconstructing past sea-level changes from storm-built beach ridges
dc.creator.none.fl_str_mv Rovere, Alessio
Pappalardo, Marta
Richiano, Sebastián Miguel
Ryan, Deirdre D.
Rubio Sandoval, Karla
Ruiz, Patricio Martin
Montes, Alejandro
Gowan, Evan J.
author Rovere, Alessio
author_facet Rovere, Alessio
Pappalardo, Marta
Richiano, Sebastián Miguel
Ryan, Deirdre D.
Rubio Sandoval, Karla
Ruiz, Patricio Martin
Montes, Alejandro
Gowan, Evan J.
author_role author
author2 Pappalardo, Marta
Richiano, Sebastián Miguel
Ryan, Deirdre D.
Rubio Sandoval, Karla
Ruiz, Patricio Martin
Montes, Alejandro
Gowan, Evan J.
author2_role author
author
author
author
author
author
author
dc.subject.none.fl_str_mv PLEISTOCENE SEA LEVEL
BEACH RIDGES
PATAGONIA ARGENTINA
PALEO SEA LEVEL
topic PLEISTOCENE SEA LEVEL
BEACH RIDGES
PATAGONIA ARGENTINA
PALEO SEA LEVEL
purl_subject.fl_str_mv https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
dc.description.none.fl_txt_mv Storm-built beach ridges, built by waves on sedimentary coasts, can be used as geomorphological indicators of past sea level. However, quantifying the relationship between the geomorphological elements of the ridge and the paleo sea level at the time of deposition is difficult, as a beach ridge is primarily correlated to wave energy and only secondarily to the position of sea level. In this work, we propose a methodology to quantify the upper and lower limits of a storm-built beach ridge based on remote sensing data. We use the tidal model FES2022, data from the Copernicus Marine Service and beach slope gathered from satellite imagery as inputs to different wave runup models, that are used to calculate the limits of the storm-built beach ridge. We test our approach on a particularly well-preserved Pleistocene storm-built beach ridge in Patagonia, Argentina. Our results show that the paleo relative sea level reconstructed using remote sensing data coincides (82.8 % similarity) with that obtained from measured modern analog landforms at the same location.
Fil: Rovere, Alessio. Universitat Bremen; Alemania. Universita' Ca' Foscari Di Venezia; Italia
Fil: Pappalardo, Marta. Università degli Studi di Pisa; Italia
Fil: Richiano, Sebastián Miguel. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Centro Nacional Patagónico. Instituto Patagónico de Geología y Paleontología; Argentina
Fil: Ryan, Deirdre D.. Università degli Studi di Pisa; Italia
Fil: Rubio Sandoval, Karla. Universitat Bremen; Alemania
Fil: Ruiz, Patricio Martin. Universidad Nacional de la Patagonia "San Juan Bosco". Facultad de Ciencias Naturales - Sede Comodoro. Departamento de Geología; Argentina
Fil: Montes, Alejandro. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; Argentina. Universidad Nacional de Tierra del Fuego, Antártida e Islas del Atlántico Sur. Instituto de Ciencias Polares, Ambientales y Recursos Naturales; Argentina
Fil: Gowan, Evan J.. Kumamoto University; Japón. KIKAI Institute for Coral Reef Sciences; Japón
description Storm-built beach ridges, built by waves on sedimentary coasts, can be used as geomorphological indicators of past sea level. However, quantifying the relationship between the geomorphological elements of the ridge and the paleo sea level at the time of deposition is difficult, as a beach ridge is primarily correlated to wave energy and only secondarily to the position of sea level. In this work, we propose a methodology to quantify the upper and lower limits of a storm-built beach ridge based on remote sensing data. We use the tidal model FES2022, data from the Copernicus Marine Service and beach slope gathered from satellite imagery as inputs to different wave runup models, that are used to calculate the limits of the storm-built beach ridge. We test our approach on a particularly well-preserved Pleistocene storm-built beach ridge in Patagonia, Argentina. Our results show that the paleo relative sea level reconstructed using remote sensing data coincides (82.8 % similarity) with that obtained from measured modern analog landforms at the same location.
publishDate 2025
dc.date.none.fl_str_mv 2025-05
dc.type.none.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
http://purl.org/coar/resource_type/c_6501
info:ar-repo/semantics/articulo
format article
status_str publishedVersion
dc.identifier.none.fl_str_mv http://hdl.handle.net/11336/260512
Rovere, Alessio; Pappalardo, Marta; Richiano, Sebastián Miguel; Ryan, Deirdre D.; Rubio Sandoval, Karla; et al.; Reconstructing past sea-level changes from storm-built beach ridges; Elsevier Science; Geomorphology; 476; 109659; 5-2025; 1-10
0169-555X
CONICET Digital
CONICET
url http://hdl.handle.net/11336/260512
identifier_str_mv Rovere, Alessio; Pappalardo, Marta; Richiano, Sebastián Miguel; Ryan, Deirdre D.; Rubio Sandoval, Karla; et al.; Reconstructing past sea-level changes from storm-built beach ridges; Elsevier Science; Geomorphology; 476; 109659; 5-2025; 1-10
0169-555X
CONICET Digital
CONICET
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/url/https://www.sciencedirect.com/science/article/pii/S0169555X25000698
info:eu-repo/semantics/altIdentifier/doi/10.1016/j.geomorph.2025.109659
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by/2.5/ar/
eu_rights_str_mv openAccess
rights_invalid_str_mv https://creativecommons.org/licenses/by/2.5/ar/
dc.format.none.fl_str_mv application/pdf
application/pdf
dc.publisher.none.fl_str_mv Elsevier Science
publisher.none.fl_str_mv Elsevier Science
dc.source.none.fl_str_mv reponame:CONICET Digital (CONICET)
instname:Consejo Nacional de Investigaciones Científicas y Técnicas
reponame_str CONICET Digital (CONICET)
collection CONICET Digital (CONICET)
instname_str Consejo Nacional de Investigaciones Científicas y Técnicas
repository.name.fl_str_mv CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicas
repository.mail.fl_str_mv dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar
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score 13.13397

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