Marine and transitional Middle/Upper Eocenen units of the Southeastern Pyrenean Foreland Basin (NE Spain)

The stratigraphic basis of this work has allowed the use of larger foraminifers in the biostratigraphic characterisation of the new Shallow Benthic Zones (SBZ). This part of the volume presents a description of the sedimentary cycles formed by the transgressive-regressive systems of the Lutetian and...

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Autores: Serra Kiel, Josep, Travé i Herrero, Anna, Mató, E., Saula, E., Ferràndez i Cañadell, Carles, Busquets, Pere (Busquets i Buezo), Tosquella Angrill, Josep, Vergés i Masip, Jaume
Tipo de documento: artigo
Data de publicação:2003
País:España
Recursos:Universidad de Huelva (UHU)
Repositório:Arias Montano. Repositorio Institucional de la Universidad de Huelva
Idioma:inglês
OAI Identifier:oai:ariasmontano.uhu.es:10272/7609
Acesso em linha:http://hdl.handle.net/10272/7609
Access Level:Acceso aberto
Palavra-chave:Marine units
Middle/Upper Eocene
Lithostratigraphy
Biostratigraphy
Pyrenean basin.
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spelling Marine and transitional Middle/Upper Eocenen units of the Southeastern Pyrenean Foreland Basin (NE Spain)Serra Kiel, JosepTravé i Herrero, AnnaMató, E.Saula, E.Ferràndez i Cañadell, CarlesBusquets, Pere (Busquets i Buezo)Tosquella Angrill, JosepVergés i Masip, JaumeMarine unitsMiddle/Upper EoceneLithostratigraphyBiostratigraphyPyrenean basin.The stratigraphic basis of this work has allowed the use of larger foraminifers in the biostratigraphic characterisation of the new Shallow Benthic Zones (SBZ). This part of the volume presents a description of the sedimentary cycles formed by the transgressive-regressive systems of the Lutetian and Bartonian in the southeastern sector of the Ebro Foreland Basin. Concerning the Lutetian deposits studied in the Amer-Vic and Empordà areas, four sedimentary cycles have been characterised. The first and second are found within the Tavertet/Girona Limestone Formation (Reguant, 1967; Pallí, 1972), while the third and fourth cycles cover the Coll de Malla Marl Formation (Clavell et al., 1970), the Bracons Formation (Gich, 1969, 1972), the Banyoles Marl Formation (Almela and Ríos, 1943), and the Bellmunt Formation (Gich, 1969, 1972). In the Bartonian deposits studied in the Igualada area, two transgressive-regressive sedimentary cycles have been characterised in the Collbàs Formation (Ferrer, 1971), the Igualada Formation (Ferrer, 1971), and the Tossa Formation (Ferrer, 1971). The Shallow Benthic Zones (SBZs) recognised within the Lutetian are the following: SBZ 13, from the Early Lutetian, in the transgressive system of the first cycle; SBZ 14, from the Middle Lutetian, in the second cycle and the lower part of the transgressive system of the third cycle; SBZ 15, from the Middle Lutetian, in the remaining parts of the third system; SBZ 16, from the Late Lutetian, throughout the fourth cycle. The association of larger foraminifers in the first and second cycles of the Bartonian in the Igualada area has been used as the basis for the definition of SBZs 17 and 18 recognised in the Bartonian of the western Tethys.Institut de Ciències de la Terra "Jaume Almera"Universidad de BarcelonaInstitut de Diagnosi Ambiental i Estudis de l'AiguaUniversidad Autónoma de BarcelonaConsejo Superior de Investigaciones CientíficasInstitut Geològic de Catalunya20032003-01-0120032003-01-01journal articlehttp://purl.org/coar/resource_type/c_6501info:eu-repo/semantics/articleapplication/pdfhttp://hdl.handle.net/10272/7609reponame:Arias Montano. Repositorio Institucional de la Universidad de Huelvainstname:Universidad de Huelva (UHU)Inglésengopen accesshttp://purl.org/coar/access_right/c_abf2Atribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/info:eu-repo/semantics/openAccessoai:ariasmontano.uhu.es:10272/76092026-06-02T14:58:11Z
dc.title.none.fl_str_mv Marine and transitional Middle/Upper Eocenen units of the Southeastern Pyrenean Foreland Basin (NE Spain)
title Marine and transitional Middle/Upper Eocenen units of the Southeastern Pyrenean Foreland Basin (NE Spain)
spellingShingle Marine and transitional Middle/Upper Eocenen units of the Southeastern Pyrenean Foreland Basin (NE Spain)
Serra Kiel, Josep
Marine units
Middle/Upper Eocene
Lithostratigraphy
Biostratigraphy
Pyrenean basin.
title_short Marine and transitional Middle/Upper Eocenen units of the Southeastern Pyrenean Foreland Basin (NE Spain)
title_full Marine and transitional Middle/Upper Eocenen units of the Southeastern Pyrenean Foreland Basin (NE Spain)
title_fullStr Marine and transitional Middle/Upper Eocenen units of the Southeastern Pyrenean Foreland Basin (NE Spain)
title_full_unstemmed Marine and transitional Middle/Upper Eocenen units of the Southeastern Pyrenean Foreland Basin (NE Spain)
title_sort Marine and transitional Middle/Upper Eocenen units of the Southeastern Pyrenean Foreland Basin (NE Spain)
dc.creator.none.fl_str_mv Serra Kiel, Josep
Travé i Herrero, Anna
Mató, E.
Saula, E.
Ferràndez i Cañadell, Carles
Busquets, Pere (Busquets i Buezo)
Tosquella Angrill, Josep
Vergés i Masip, Jaume
author Serra Kiel, Josep
author_facet Serra Kiel, Josep
Travé i Herrero, Anna
Mató, E.
Saula, E.
Ferràndez i Cañadell, Carles
Busquets, Pere (Busquets i Buezo)
Tosquella Angrill, Josep
Vergés i Masip, Jaume
author_role author
author2 Travé i Herrero, Anna
Mató, E.
Saula, E.
Ferràndez i Cañadell, Carles
Busquets, Pere (Busquets i Buezo)
Tosquella Angrill, Josep
Vergés i Masip, Jaume
author2_role author
author
author
author
author
author
author
dc.contributor.none.fl_str_mv
dc.subject.none.fl_str_mv Marine units
Middle/Upper Eocene
Lithostratigraphy
Biostratigraphy
Pyrenean basin.
topic Marine units
Middle/Upper Eocene
Lithostratigraphy
Biostratigraphy
Pyrenean basin.
description The stratigraphic basis of this work has allowed the use of larger foraminifers in the biostratigraphic characterisation of the new Shallow Benthic Zones (SBZ). This part of the volume presents a description of the sedimentary cycles formed by the transgressive-regressive systems of the Lutetian and Bartonian in the southeastern sector of the Ebro Foreland Basin. Concerning the Lutetian deposits studied in the Amer-Vic and Empordà areas, four sedimentary cycles have been characterised. The first and second are found within the Tavertet/Girona Limestone Formation (Reguant, 1967; Pallí, 1972), while the third and fourth cycles cover the Coll de Malla Marl Formation (Clavell et al., 1970), the Bracons Formation (Gich, 1969, 1972), the Banyoles Marl Formation (Almela and Ríos, 1943), and the Bellmunt Formation (Gich, 1969, 1972). In the Bartonian deposits studied in the Igualada area, two transgressive-regressive sedimentary cycles have been characterised in the Collbàs Formation (Ferrer, 1971), the Igualada Formation (Ferrer, 1971), and the Tossa Formation (Ferrer, 1971). The Shallow Benthic Zones (SBZs) recognised within the Lutetian are the following: SBZ 13, from the Early Lutetian, in the transgressive system of the first cycle; SBZ 14, from the Middle Lutetian, in the second cycle and the lower part of the transgressive system of the third cycle; SBZ 15, from the Middle Lutetian, in the remaining parts of the third system; SBZ 16, from the Late Lutetian, throughout the fourth cycle. The association of larger foraminifers in the first and second cycles of the Bartonian in the Igualada area has been used as the basis for the definition of SBZs 17 and 18 recognised in the Bartonian of the western Tethys.
publishDate 2003
dc.date.none.fl_str_mv 2003
2003-01-01
2003
2003-01-01
dc.type.none.fl_str_mv journal article
http://purl.org/coar/resource_type/c_6501
dc.type.openaire.fl_str_mv info:eu-repo/semantics/article
format article
dc.identifier.none.fl_str_mv http://hdl.handle.net/10272/7609
url http://hdl.handle.net/10272/7609
dc.language.none.fl_str_mv Inglés
eng
language_invalid_str_mv Inglés
language eng
dc.rights.none.fl_str_mv open access
http://purl.org/coar/access_right/c_abf2
Atribución-NoComercial-SinDerivadas 3.0 España
http://creativecommons.org/licenses/by-nc-nd/3.0/es/
dc.rights.openaire.fl_str_mv info:eu-repo/semantics/openAccess
rights_invalid_str_mv open access
http://purl.org/coar/access_right/c_abf2
Atribución-NoComercial-SinDerivadas 3.0 España
http://creativecommons.org/licenses/by-nc-nd/3.0/es/
eu_rights_str_mv openAccess
dc.format.none.fl_str_mv application/pdf
dc.publisher.none.fl_str_mv Institut de Ciències de la Terra "Jaume Almera"
Universidad de Barcelona
Institut de Diagnosi Ambiental i Estudis de l'Aigua
Universidad Autónoma de Barcelona
Consejo Superior de Investigaciones Científicas
Institut Geològic de Catalunya
publisher.none.fl_str_mv Institut de Ciències de la Terra "Jaume Almera"
Universidad de Barcelona
Institut de Diagnosi Ambiental i Estudis de l'Aigua
Universidad Autónoma de Barcelona
Consejo Superior de Investigaciones Científicas
Institut Geològic de Catalunya
dc.source.none.fl_str_mv reponame:Arias Montano. Repositorio Institucional de la Universidad de Huelva
instname:Universidad de Huelva (UHU)
instname_str Universidad de Huelva (UHU)
reponame_str Arias Montano. Repositorio Institucional de la Universidad de Huelva
collection Arias Montano. Repositorio Institucional de la Universidad de Huelva
repository.name.fl_str_mv
repository.mail.fl_str_mv
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score 15.812455

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