Latest Cretaceous palaeogeographic evolution of northeast Iberia: Insights from the Campanian continental Montalbán subbasin (Spain)

This work characterizes for the first time the 500–700 m-thick uppermost Cretaceous continental sedimentarysuccession of the Allueva Fm recorded in the northeastern margin of the Iberian basin, in the Montalb´an subbasin(Maestrazgo domain, Spain). The middle-upper Campanian age of this unit constrai...

Descripción completa

Detalles Bibliográficos
Autores: Aurell Marcos, Torromé, Diego, Gasca, José M., Calvín, Pablo, Pérez-Pueyo, Manuel, Parrilla-Bel, Jara, Medrano-Aguado, Eduardo, Martín-Closas, Carles, Vicente Rodriguez, Alba, Sierra-Campos, Pablo, Canudo, José L.
Tipo de recurso: artículo
Estado:Versión aceptada para publicación
Fecha de publicación:2022
País:España
Institución:Varias* (Consorci de Biblioteques Universitáries de Catalunya, Centre de Serveis Científics i Acadèmics de Catalunya)
Repositorio:Recercat. Dipósit de la Recerca de Catalunya
OAI Identifier:oai:recercat.cat:2445/219222
Acceso en línea:https://hdl.handle.net/2445/219222
Access Level:acceso abierto
Palabra clave:Magnetoestratigrafia
Paleontologia
Dinosaures
Estratigrafia
Sedimentologia
Cretaci
Península Ibèrica
Magnetostratigraphy
Paleontology
Dinosaurs
Stratigraphic geology
Sedimentology
Cretaceous Period
Iberian Peninsula
id ES_bfc7904c1ea554985c8b71fc02ae2e6b
oai_identifier_str oai:recercat.cat:2445/219222
network_acronym_str ES
network_name_str España
repository_id_str
spelling Latest Cretaceous palaeogeographic evolution of northeast Iberia: Insights from the Campanian continental Montalbán subbasin (Spain)Aurell MarcosTorromé, DiegoGasca, José M.Calvín, PabloPérez-Pueyo, ManuelParrilla-Bel, JaraMedrano-Aguado, EduardoMartín-Closas, CarlesVicente Rodriguez, AlbaSierra-Campos, PabloCanudo, José L.MagnetoestratigrafiaPaleontologiaDinosauresEstratigrafiaSedimentologiaCretaciPenínsula IbèricaMagnetostratigraphyPaleontologyDinosaursStratigraphic geologySedimentologyCretaceous PeriodIberian PeninsulaThis work characterizes for the first time the 500–700 m-thick uppermost Cretaceous continental sedimentarysuccession of the Allueva Fm recorded in the northeastern margin of the Iberian basin, in the Montalb´an subbasin(Maestrazgo domain, Spain). The middle-upper Campanian age of this unit constrained here by new paleomagneticand biostratigraphic data involves major revision of previous stratigraphic and palaeogeographic interpretations.The uplift of the northern marginal areas of the Montalb´an subbasin onwards from the middleCampanian supplied the coarse terrigenous-clastic sediments common in the alluvial Allueva Fm. Moreover, asharp increase of the sedimentation rates (from 4 to 19 cm/ky) from the lower to the middle-upper part of theAllueva Fm has been related to further increase of the tectonic activity during the middle part of the lateCampanian. Also relevant are the new discovered vertebrate sites mostly found in the marginal areas of a largelacustrine-palustrine carbonate system developed during the latest Campanian. Vertebrate sites include a fossilassemblage with abundance of titanosaur sauropod dinosaurs as well as the presence of ornithopod dinosaursand crocodylomorphs. A review of the dinosaur fossil sites recorded in other Iberian subbasins shows a similarfossil assembage occurrence during the late Campanian–earliest Maastrichtian timespan, previous to the faunalturnover that took place in the Ibero-Armorican landmass around the onset of the late Maastrichtian. Thestratigraphic, sedimentological and paleontological characterization of the successions recorded during theinitial stages of development of the Montalb´an subbasin have major implication to understand the latestCretaceous palaeogeographic evolution of northeast Iberia. Comparative review to other latest Cretaceouscontinental successions deposited in other domains of the Iberian basin indicates a south to north migration ofnewly developed subsident subbasins: during the Campanian (South Iberian domain), during the middle-lateCampanian (northern Maestrazgo domain), and during the Maastrichtian (central Castillian domain).Elsevier B.V.2025202520222025info:eu-repo/semantics/articleinfo:eu-repo/semantics/acceptedVersion26 p.application/pdfhttps://hdl.handle.net/2445/219222Articles publicats en revistes (Dinàmica de la Terra i l'Oceà)reponame:Recercat. Dipósit de la Recerca de Catalunyainstname:Varias* (Consorci de Biblioteques Universitáries de Catalunya, Centre de Serveis Científics i Acadèmics de Catalunya)InglésReproducció del document publicat a: https://doi.org/https://doi.org/10.1016/j.earscirev.2022.104251Earth-Science Reviews, 2022, vol. 235https://doi.org/https://doi.org/10.1016/j.earscirev.2022.104251cc-by-nc-nd (c) The Author(s), 2022http://creativecommons.org/licenses/by-nc-nd/4.0/info:eu-repo/semantics/openAccessoai:recercat.cat:2445/2192222026-05-29T05:05:01Z
dc.title.none.fl_str_mv Latest Cretaceous palaeogeographic evolution of northeast Iberia: Insights from the Campanian continental Montalbán subbasin (Spain)
title Latest Cretaceous palaeogeographic evolution of northeast Iberia: Insights from the Campanian continental Montalbán subbasin (Spain)
spellingShingle Latest Cretaceous palaeogeographic evolution of northeast Iberia: Insights from the Campanian continental Montalbán subbasin (Spain)
Aurell Marcos
Magnetoestratigrafia
Paleontologia
Dinosaures
Estratigrafia
Sedimentologia
Cretaci
Península Ibèrica
Magnetostratigraphy
Paleontology
Dinosaurs
Stratigraphic geology
Sedimentology
Cretaceous Period
Iberian Peninsula
title_short Latest Cretaceous palaeogeographic evolution of northeast Iberia: Insights from the Campanian continental Montalbán subbasin (Spain)
title_full Latest Cretaceous palaeogeographic evolution of northeast Iberia: Insights from the Campanian continental Montalbán subbasin (Spain)
title_fullStr Latest Cretaceous palaeogeographic evolution of northeast Iberia: Insights from the Campanian continental Montalbán subbasin (Spain)
title_full_unstemmed Latest Cretaceous palaeogeographic evolution of northeast Iberia: Insights from the Campanian continental Montalbán subbasin (Spain)
title_sort Latest Cretaceous palaeogeographic evolution of northeast Iberia: Insights from the Campanian continental Montalbán subbasin (Spain)
dc.creator.none.fl_str_mv Aurell Marcos
Torromé, Diego
Gasca, José M.
Calvín, Pablo
Pérez-Pueyo, Manuel
Parrilla-Bel, Jara
Medrano-Aguado, Eduardo
Martín-Closas, Carles
Vicente Rodriguez, Alba
Sierra-Campos, Pablo
Canudo, José L.
author Aurell Marcos
author_facet Aurell Marcos
Torromé, Diego
Gasca, José M.
Calvín, Pablo
Pérez-Pueyo, Manuel
Parrilla-Bel, Jara
Medrano-Aguado, Eduardo
Martín-Closas, Carles
Vicente Rodriguez, Alba
Sierra-Campos, Pablo
Canudo, José L.
author_role author
author2 Torromé, Diego
Gasca, José M.
Calvín, Pablo
Pérez-Pueyo, Manuel
Parrilla-Bel, Jara
Medrano-Aguado, Eduardo
Martín-Closas, Carles
Vicente Rodriguez, Alba
Sierra-Campos, Pablo
Canudo, José L.
author2_role author
author
author
author
author
author
author
author
author
author
dc.subject.none.fl_str_mv Magnetoestratigrafia
Paleontologia
Dinosaures
Estratigrafia
Sedimentologia
Cretaci
Península Ibèrica
Magnetostratigraphy
Paleontology
Dinosaurs
Stratigraphic geology
Sedimentology
Cretaceous Period
Iberian Peninsula
topic Magnetoestratigrafia
Paleontologia
Dinosaures
Estratigrafia
Sedimentologia
Cretaci
Península Ibèrica
Magnetostratigraphy
Paleontology
Dinosaurs
Stratigraphic geology
Sedimentology
Cretaceous Period
Iberian Peninsula
description This work characterizes for the first time the 500–700 m-thick uppermost Cretaceous continental sedimentarysuccession of the Allueva Fm recorded in the northeastern margin of the Iberian basin, in the Montalb´an subbasin(Maestrazgo domain, Spain). The middle-upper Campanian age of this unit constrained here by new paleomagneticand biostratigraphic data involves major revision of previous stratigraphic and palaeogeographic interpretations.The uplift of the northern marginal areas of the Montalb´an subbasin onwards from the middleCampanian supplied the coarse terrigenous-clastic sediments common in the alluvial Allueva Fm. Moreover, asharp increase of the sedimentation rates (from 4 to 19 cm/ky) from the lower to the middle-upper part of theAllueva Fm has been related to further increase of the tectonic activity during the middle part of the lateCampanian. Also relevant are the new discovered vertebrate sites mostly found in the marginal areas of a largelacustrine-palustrine carbonate system developed during the latest Campanian. Vertebrate sites include a fossilassemblage with abundance of titanosaur sauropod dinosaurs as well as the presence of ornithopod dinosaursand crocodylomorphs. A review of the dinosaur fossil sites recorded in other Iberian subbasins shows a similarfossil assembage occurrence during the late Campanian–earliest Maastrichtian timespan, previous to the faunalturnover that took place in the Ibero-Armorican landmass around the onset of the late Maastrichtian. Thestratigraphic, sedimentological and paleontological characterization of the successions recorded during theinitial stages of development of the Montalb´an subbasin have major implication to understand the latestCretaceous palaeogeographic evolution of northeast Iberia. Comparative review to other latest Cretaceouscontinental successions deposited in other domains of the Iberian basin indicates a south to north migration ofnewly developed subsident subbasins: during the Campanian (South Iberian domain), during the middle-lateCampanian (northern Maestrazgo domain), and during the Maastrichtian (central Castillian domain).
publishDate 2022
dc.date.none.fl_str_mv 2022
2025
2025
2025
dc.type.none.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/acceptedVersion
format article
status_str acceptedVersion
dc.identifier.none.fl_str_mv https://hdl.handle.net/2445/219222
url https://hdl.handle.net/2445/219222
dc.language.none.fl_str_mv Inglés
language_invalid_str_mv Inglés
dc.relation.none.fl_str_mv Reproducció del document publicat a: https://doi.org/https://doi.org/10.1016/j.earscirev.2022.104251
Earth-Science Reviews, 2022, vol. 235
https://doi.org/https://doi.org/10.1016/j.earscirev.2022.104251
dc.rights.none.fl_str_mv cc-by-nc-nd (c) The Author(s), 2022
http://creativecommons.org/licenses/by-nc-nd/4.0/
info:eu-repo/semantics/openAccess
rights_invalid_str_mv cc-by-nc-nd (c) The Author(s), 2022
http://creativecommons.org/licenses/by-nc-nd/4.0/
eu_rights_str_mv openAccess
dc.format.none.fl_str_mv 26 p.
application/pdf
dc.publisher.none.fl_str_mv Elsevier B.V.
publisher.none.fl_str_mv Elsevier B.V.
dc.source.none.fl_str_mv Articles publicats en revistes (Dinàmica de la Terra i l'Oceà)
reponame:Recercat. Dipósit de la Recerca de Catalunya
instname:Varias* (Consorci de Biblioteques Universitáries de Catalunya, Centre de Serveis Científics i Acadèmics de Catalunya)
instname_str Varias* (Consorci de Biblioteques Universitáries de Catalunya, Centre de Serveis Científics i Acadèmics de Catalunya)
reponame_str Recercat. Dipósit de la Recerca de Catalunya
collection Recercat. Dipósit de la Recerca de Catalunya
repository.name.fl_str_mv
repository.mail.fl_str_mv
_version_ 1869418420818149376
score 15.812429