Los materiales del tránsito Triásico-Jurásico en la región de Villaviciosa (Asturias, España). Caracterización palinológica

A lithostratigraphic and palynologic study of the sediments corresponding to the Triassic-Jurassic transition at the Bárzana section, located in the Villaviciosa region (Asturias), has been carried out. Four lithostratigraphic units have been distinguished: A) Black and maroon lutites with evaporite...

ver descrição completa

Detalhes bibliográficos
Autores: Barrón, E., Gómez, J. J., Goy, Antonio
Tipo de documento: artigo
Data de publicação:2001
País:España
Recursos:Universidad de Huelva (UHU)
Repositório:Arias Montano. Repositorio Institucional de la Universidad de Huelva
Idioma:espanhol
OAI Identifier:oai:ariasmontano.uhu.es:10272/9498
Acesso em linha:http://hdl.handle.net/10272/9498
Access Level:Acceso aberto
Palavra-chave:Stratigraphy
Biochronostratigraphy
Palynomorphs
Rhaetian
Hettangian
id ES_e3302ea6b74f096955cf929ea96cf129
oai_identifier_str oai:ariasmontano.uhu.es:10272/9498
network_acronym_str ES
network_name_str España
repository_id_str
spelling Los materiales del tránsito Triásico-Jurásico en la región de Villaviciosa (Asturias, España). Caracterización palinológicaThe sediments of the Triassic-Jurassic transition in the Villaviciosa region (Asturias, Spain). Palynological characterizationBarrón, E.Gómez, J. J.Goy, AntonioStratigraphyBiochronostratigraphyPalynomorphsRhaetianHettangianA lithostratigraphic and palynologic study of the sediments corresponding to the Triassic-Jurassic transition at the Bárzana section, located in the Villaviciosa region (Asturias), has been carried out. Four lithostratigraphic units have been distinguished: A) Black and maroon lutites with evaporites Unit; B) Well bedded dolomites and limestones Unit; C) Lutites, evaporites and carbonates Unit, and D) Grey lutites and carbonate breccias Unit. Samples containing fossils of pollen and spores have been collected in successive levels. The 0 level, with Corollina meyeriana as dominant element, associated to Ovalipollis cf. pseudoalatus, and in neighbouring sections also with Rhaetipollis germanicus and Cerebropollenites pseudomasulae, can be considered as Triassic (Rhaetian). Level 1 8, with Cyathidites minor and Todisporites minor, associated to Corollina torosus and in adjacent areas to Ischyosporites variegatus and Cerebropollenites mesozoicus is Lower Jurassic in age. The biochronostratigraphic analysis indicate that the levels of the upper portion of the A Unit are Rhaetian. The Triassic-Jurassic boundary should be located inside the 8 Unit, below the level equivalent to the lumachellic bed which furnished a specimen of Caloceras pirondi (Reynés) south of Avilés. The sampled level at the base of the C Unit is considered as Hettangian by the persistence of Rhaetipollis germanicus SchulzSociedad Geológica de España20012001-01-0120012001-01-01journal articlehttp://purl.org/coar/resource_type/c_6501info:eu-repo/semantics/articleapplication/pdfhttp://hdl.handle.net/10272/9498reponame:Arias Montano. Repositorio Institucional de la Universidad de Huelvainstname:Universidad de Huelva (UHU)Españolspaopen 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:10272/94982026-06-02T14:58:11Z
dc.title.none.fl_str_mv Los materiales del tránsito Triásico-Jurásico en la región de Villaviciosa (Asturias, España). Caracterización palinológica
The sediments of the Triassic-Jurassic transition in the Villaviciosa region (Asturias, Spain). Palynological characterization
title Los materiales del tránsito Triásico-Jurásico en la región de Villaviciosa (Asturias, España). Caracterización palinológica
spellingShingle Los materiales del tránsito Triásico-Jurásico en la región de Villaviciosa (Asturias, España). Caracterización palinológica
Barrón, E.
Stratigraphy
Biochronostratigraphy
Palynomorphs
Rhaetian
Hettangian
title_short Los materiales del tránsito Triásico-Jurásico en la región de Villaviciosa (Asturias, España). Caracterización palinológica
title_full Los materiales del tránsito Triásico-Jurásico en la región de Villaviciosa (Asturias, España). Caracterización palinológica
title_fullStr Los materiales del tránsito Triásico-Jurásico en la región de Villaviciosa (Asturias, España). Caracterización palinológica
title_full_unstemmed Los materiales del tránsito Triásico-Jurásico en la región de Villaviciosa (Asturias, España). Caracterización palinológica
title_sort Los materiales del tránsito Triásico-Jurásico en la región de Villaviciosa (Asturias, España). Caracterización palinológica
dc.creator.none.fl_str_mv Barrón, E.
Gómez, J. J.
Goy, Antonio
author Barrón, E.
author_facet Barrón, E.
Gómez, J. J.
Goy, Antonio
author_role author
author2 Gómez, J. J.
Goy, Antonio
author2_role author
author
dc.contributor.none.fl_str_mv
dc.subject.none.fl_str_mv Stratigraphy
Biochronostratigraphy
Palynomorphs
Rhaetian
Hettangian
topic Stratigraphy
Biochronostratigraphy
Palynomorphs
Rhaetian
Hettangian
description A lithostratigraphic and palynologic study of the sediments corresponding to the Triassic-Jurassic transition at the Bárzana section, located in the Villaviciosa region (Asturias), has been carried out. Four lithostratigraphic units have been distinguished: A) Black and maroon lutites with evaporites Unit; B) Well bedded dolomites and limestones Unit; C) Lutites, evaporites and carbonates Unit, and D) Grey lutites and carbonate breccias Unit. Samples containing fossils of pollen and spores have been collected in successive levels. The 0 level, with Corollina meyeriana as dominant element, associated to Ovalipollis cf. pseudoalatus, and in neighbouring sections also with Rhaetipollis germanicus and Cerebropollenites pseudomasulae, can be considered as Triassic (Rhaetian). Level 1 8, with Cyathidites minor and Todisporites minor, associated to Corollina torosus and in adjacent areas to Ischyosporites variegatus and Cerebropollenites mesozoicus is Lower Jurassic in age. The biochronostratigraphic analysis indicate that the levels of the upper portion of the A Unit are Rhaetian. The Triassic-Jurassic boundary should be located inside the 8 Unit, below the level equivalent to the lumachellic bed which furnished a specimen of Caloceras pirondi (Reynés) south of Avilés. The sampled level at the base of the C Unit is considered as Hettangian by the persistence of Rhaetipollis germanicus Schulz
publishDate 2001
dc.date.none.fl_str_mv 2001
2001-01-01
2001
2001-01-01
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/10272/9498
url http://hdl.handle.net/10272/9498
dc.language.none.fl_str_mv Español
spa
language_invalid_str_mv Español
language spa
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 Sociedad Geológica de España
publisher.none.fl_str_mv Sociedad Geológica de España
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
_version_ 1869422478731771904
score 15,812455