Micropaleontology of the Agrio Formation (Lower Cretaceous) in different areas of the Neuquén Basin

Autores
Concheyro, A.; Lescano, M.; Caramés, A.; Ballent, S.
Año de publicación
2009
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
The nanoflora and microfauna from the Agrio Formation are analyzed in three different areas of the Neuquén Basin to establish its age and paleonvironmental variations. In the northern area of the basin, the oldest Agrio Fomation sedimentites are recognized and assigned to the Lower Valanginian through ammonites. A monospecific Epistomina loncochensis Ballent microfauna is recovered from these levels, which indicates disoxic environments. Up to the top of the section, siltstones contain a diverse foraminifera microfauna of normal shelves, which are replaced by an impoverished fauna related to shallowing processes. The age defined by calcareous nannofossils is Late Valanginian-Late Hauterivian. In the central and southern position of the Neuquén Basin, the nannofossil assemblages indicate the Upper Valanginian-Upper Hauterivian for the Agrio Formation. The benthic microfauna suggests frequent eustatic variations ranging from shelves to shallow marine environments. In the austral sector of the basin, a poorly diversified foraminiferal assemblage is recorded and a high ostracods/foraminifera ratio indicates a restricted marine environment, and normal salinity. The presence of a level with abundant attached foraminifera indicates high energy episodes. The high diversified Platycopida ostracods suggest warm-temperate to subtropical waters.
Fil:Concheyro, A. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina.
Fil:Lescano, M. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina.
Fil:Caramés, A. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina.
Fuente
Rev. Asoc. Geol. Argent. 2009;65(2):342-361
Materia
Argentina
Biostratigraphy
Mesozoic
Microfossils
Nannofossils
Paleoecology
biostratigraphy
calcareous alga
fauna
foraminifera
fossil assemblage
Mesozoic
microfossil
micropaleontology
paleoecology
paleoenvironment
Argentina
Neuquen Basin
Epistomina
Foraminifera
Ostracoda
Platycopida
Nivel de accesibilidad
acceso abierto
Condiciones de uso
http://creativecommons.org/licenses/by/2.5/ar
Repositorio
Biblioteca Digital (UBA-FCEN)
Institución
Universidad Nacional de Buenos Aires. Facultad de Ciencias Exactas y Naturales
OAI Identificador
paperaa:paper_00044822_v65_n2_p342_Concheyro

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oai_identifier_str paperaa:paper_00044822_v65_n2_p342_Concheyro
network_acronym_str BDUBAFCEN
repository_id_str 1896
network_name_str Biblioteca Digital (UBA-FCEN)
spelling Micropaleontology of the Agrio Formation (Lower Cretaceous) in different areas of the Neuquén Basin Concheyro, A.Lescano, M.Caramés, A.Ballent, S.ArgentinaBiostratigraphyMesozoicMicrofossilsNannofossilsPaleoecologybiostratigraphycalcareous algafaunaforaminiferafossil assemblageMesozoicmicrofossilmicropaleontologypaleoecologypaleoenvironmentArgentinaNeuquen BasinEpistominaForaminiferaOstracodaPlatycopidaThe nanoflora and microfauna from the Agrio Formation are analyzed in three different areas of the Neuquén Basin to establish its age and paleonvironmental variations. In the northern area of the basin, the oldest Agrio Fomation sedimentites are recognized and assigned to the Lower Valanginian through ammonites. A monospecific Epistomina loncochensis Ballent microfauna is recovered from these levels, which indicates disoxic environments. Up to the top of the section, siltstones contain a diverse foraminifera microfauna of normal shelves, which are replaced by an impoverished fauna related to shallowing processes. The age defined by calcareous nannofossils is Late Valanginian-Late Hauterivian. In the central and southern position of the Neuquén Basin, the nannofossil assemblages indicate the Upper Valanginian-Upper Hauterivian for the Agrio Formation. The benthic microfauna suggests frequent eustatic variations ranging from shelves to shallow marine environments. In the austral sector of the basin, a poorly diversified foraminiferal assemblage is recorded and a high ostracods/foraminifera ratio indicates a restricted marine environment, and normal salinity. The presence of a level with abundant attached foraminifera indicates high energy episodes. The high diversified Platycopida ostracods suggest warm-temperate to subtropical waters.Fil:Concheyro, A. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina.Fil:Lescano, M. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina.Fil:Caramés, A. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina.2009info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfhttp://hdl.handle.net/20.500.12110/paper_00044822_v65_n2_p342_ConcheyroRev. Asoc. Geol. Argent. 2009;65(2):342-361reponame:Biblioteca Digital (UBA-FCEN)instname:Universidad Nacional de Buenos Aires. Facultad de Ciencias Exactas y Naturalesinstacron:UBA-FCENenginfo:eu-repo/semantics/openAccesshttp://creativecommons.org/licenses/by/2.5/ar2025-10-16T09:30:13Zpaperaa:paper_00044822_v65_n2_p342_ConcheyroInstitucionalhttps://digital.bl.fcen.uba.ar/Universidad públicaNo correspondehttps://digital.bl.fcen.uba.ar/cgi-bin/oaiserver.cgiana@bl.fcen.uba.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:18962025-10-16 09:30:14.554Biblioteca Digital (UBA-FCEN) - Universidad Nacional de Buenos Aires. Facultad de Ciencias Exactas y Naturalesfalse
dc.title.none.fl_str_mv Micropaleontology of the Agrio Formation (Lower Cretaceous) in different areas of the Neuquén Basin
title Micropaleontology of the Agrio Formation (Lower Cretaceous) in different areas of the Neuquén Basin
spellingShingle Micropaleontology of the Agrio Formation (Lower Cretaceous) in different areas of the Neuquén Basin
Concheyro, A.
Argentina
Biostratigraphy
Mesozoic
Microfossils
Nannofossils
Paleoecology
biostratigraphy
calcareous alga
fauna
foraminifera
fossil assemblage
Mesozoic
microfossil
micropaleontology
paleoecology
paleoenvironment
Argentina
Neuquen Basin
Epistomina
Foraminifera
Ostracoda
Platycopida
title_short Micropaleontology of the Agrio Formation (Lower Cretaceous) in different areas of the Neuquén Basin
title_full Micropaleontology of the Agrio Formation (Lower Cretaceous) in different areas of the Neuquén Basin
title_fullStr Micropaleontology of the Agrio Formation (Lower Cretaceous) in different areas of the Neuquén Basin
title_full_unstemmed Micropaleontology of the Agrio Formation (Lower Cretaceous) in different areas of the Neuquén Basin
title_sort Micropaleontology of the Agrio Formation (Lower Cretaceous) in different areas of the Neuquén Basin
dc.creator.none.fl_str_mv Concheyro, A.
Lescano, M.
Caramés, A.
Ballent, S.
author Concheyro, A.
author_facet Concheyro, A.
Lescano, M.
Caramés, A.
Ballent, S.
author_role author
author2 Lescano, M.
Caramés, A.
Ballent, S.
author2_role author
author
author
dc.subject.none.fl_str_mv Argentina
Biostratigraphy
Mesozoic
Microfossils
Nannofossils
Paleoecology
biostratigraphy
calcareous alga
fauna
foraminifera
fossil assemblage
Mesozoic
microfossil
micropaleontology
paleoecology
paleoenvironment
Argentina
Neuquen Basin
Epistomina
Foraminifera
Ostracoda
Platycopida
topic Argentina
Biostratigraphy
Mesozoic
Microfossils
Nannofossils
Paleoecology
biostratigraphy
calcareous alga
fauna
foraminifera
fossil assemblage
Mesozoic
microfossil
micropaleontology
paleoecology
paleoenvironment
Argentina
Neuquen Basin
Epistomina
Foraminifera
Ostracoda
Platycopida
dc.description.none.fl_txt_mv The nanoflora and microfauna from the Agrio Formation are analyzed in three different areas of the Neuquén Basin to establish its age and paleonvironmental variations. In the northern area of the basin, the oldest Agrio Fomation sedimentites are recognized and assigned to the Lower Valanginian through ammonites. A monospecific Epistomina loncochensis Ballent microfauna is recovered from these levels, which indicates disoxic environments. Up to the top of the section, siltstones contain a diverse foraminifera microfauna of normal shelves, which are replaced by an impoverished fauna related to shallowing processes. The age defined by calcareous nannofossils is Late Valanginian-Late Hauterivian. In the central and southern position of the Neuquén Basin, the nannofossil assemblages indicate the Upper Valanginian-Upper Hauterivian for the Agrio Formation. The benthic microfauna suggests frequent eustatic variations ranging from shelves to shallow marine environments. In the austral sector of the basin, a poorly diversified foraminiferal assemblage is recorded and a high ostracods/foraminifera ratio indicates a restricted marine environment, and normal salinity. The presence of a level with abundant attached foraminifera indicates high energy episodes. The high diversified Platycopida ostracods suggest warm-temperate to subtropical waters.
Fil:Concheyro, A. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina.
Fil:Lescano, M. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina.
Fil:Caramés, A. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina.
description The nanoflora and microfauna from the Agrio Formation are analyzed in three different areas of the Neuquén Basin to establish its age and paleonvironmental variations. In the northern area of the basin, the oldest Agrio Fomation sedimentites are recognized and assigned to the Lower Valanginian through ammonites. A monospecific Epistomina loncochensis Ballent microfauna is recovered from these levels, which indicates disoxic environments. Up to the top of the section, siltstones contain a diverse foraminifera microfauna of normal shelves, which are replaced by an impoverished fauna related to shallowing processes. The age defined by calcareous nannofossils is Late Valanginian-Late Hauterivian. In the central and southern position of the Neuquén Basin, the nannofossil assemblages indicate the Upper Valanginian-Upper Hauterivian for the Agrio Formation. The benthic microfauna suggests frequent eustatic variations ranging from shelves to shallow marine environments. In the austral sector of the basin, a poorly diversified foraminiferal assemblage is recorded and a high ostracods/foraminifera ratio indicates a restricted marine environment, and normal salinity. The presence of a level with abundant attached foraminifera indicates high energy episodes. The high diversified Platycopida ostracods suggest warm-temperate to subtropical waters.
publishDate 2009
dc.date.none.fl_str_mv 2009
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/20.500.12110/paper_00044822_v65_n2_p342_Concheyro
url http://hdl.handle.net/20.500.12110/paper_00044822_v65_n2_p342_Concheyro
dc.language.none.fl_str_mv eng
language eng
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
http://creativecommons.org/licenses/by/2.5/ar
eu_rights_str_mv openAccess
rights_invalid_str_mv http://creativecommons.org/licenses/by/2.5/ar
dc.format.none.fl_str_mv application/pdf
dc.source.none.fl_str_mv Rev. Asoc. Geol. Argent. 2009;65(2):342-361
reponame:Biblioteca Digital (UBA-FCEN)
instname:Universidad Nacional de Buenos Aires. Facultad de Ciencias Exactas y Naturales
instacron:UBA-FCEN
reponame_str Biblioteca Digital (UBA-FCEN)
collection Biblioteca Digital (UBA-FCEN)
instname_str Universidad Nacional de Buenos Aires. Facultad de Ciencias Exactas y Naturales
instacron_str UBA-FCEN
institution UBA-FCEN
repository.name.fl_str_mv Biblioteca Digital (UBA-FCEN) - Universidad Nacional de Buenos Aires. Facultad de Ciencias Exactas y Naturales
repository.mail.fl_str_mv ana@bl.fcen.uba.ar
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