Bioestratigrafía de la Formación Barranca Final, Neógeno de la Cuenca del Colorado, Argentina

Autores
Guler, Maria Veronica; Guerstein, Gladys Raquel; Malumian, Norberto
Año de publicación
2002
Idioma
español castellano
Tipo de recurso
artículo
Estado
versión publicada
Descripción
Dinoflagellate cysts from the Barranca Final Formation type section are diverse and well preserved. The assemblages are dominated by the Order Gonyaulacales, with subordinate Peridiniales represented only by protoperidiniaceans. Based on selected dinoflagellate cyst events, and in accordance with the foraminiferal data, we suggest a Middle to Late Miocene age for the section. Piasecki ranges from latest Early Miocene or early Middle Miocene through Late Miocene has its range base within the Middle Miocene. The occurrences of these species together with the presence of (Wall) Reid confirms an age no older than Middle Miocene for the bottom of the section. The low representation of oceanic species, such as Nematosphaeropsis rigida 150% Wrenn (inner to outer? neritic), the diverse representation of protoperidinacean species (inner neritic), and the abundance of euryhaline forms, particularly specimens of the Operculodinium centrocarpum/israelianum Tuberculodinium vancampoae Lingulodinium hemicystum, reflect estuarine to inner neritic conditions for the lower part of the section palaeoenvironmental, the occurrence of oceanic to neritic markers coinciding with a glauconitic section, suggest a marine flooding surface.
Fil: Guler, Maria Veronica. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Bahía Blanca. Instituto Geológico del Sur. Universidad Nacional del Sur. Departamento de Geología. Instituto Geológico del Sur; Argentina
Fil: Guerstein, Gladys Raquel. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Bahía Blanca. Instituto Geológico del Sur. Universidad Nacional del Sur. Departamento de Geología. Instituto Geológico del Sur; Argentina
Fil: Malumian, Norberto. Secretaría de Industria y Minería. Servicio Geológico Minero Argentino; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
Materia
Formación Barranca Final
Dinoflagelados
Neogeno
Cuenca del Colorado
Nivel de accesibilidad
acceso abierto
Condiciones de uso
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
Repositorio
CONICET Digital (CONICET)
Institución
Consejo Nacional de Investigaciones Científicas y Técnicas
OAI Identificador
oai:ri.conicet.gov.ar:11336/81303
Acceder
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network_name_str CONICET Digital (CONICET)
spelling Bioestratigrafía de la Formación Barranca Final, Neógeno de la Cuenca del Colorado, ArgentinaBiostratigraphy of the Neogene Baranca Final Formation of the Colorado Basin, ArgentinaGuler, Maria VeronicaGuerstein, Gladys RaquelMalumian, NorbertoFormación Barranca FinalDinoflageladosNeogenoCuenca del Coloradohttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1Dinoflagellate cysts from the Barranca Final Formation type section are diverse and well preserved. The assemblages are dominated by the Order Gonyaulacales, with subordinate Peridiniales represented only by protoperidiniaceans. Based on selected dinoflagellate cyst events, and in accordance with the foraminiferal data, we suggest a Middle to Late Miocene age for the section. Piasecki ranges from latest Early Miocene or early Middle Miocene through Late Miocene has its range base within the Middle Miocene. The occurrences of these species together with the presence of (Wall) Reid confirms an age no older than Middle Miocene for the bottom of the section. The low representation of oceanic species, such as Nematosphaeropsis rigida 150% Wrenn (inner to outer? neritic), the diverse representation of protoperidinacean species (inner neritic), and the abundance of euryhaline forms, particularly specimens of the Operculodinium centrocarpum/israelianum Tuberculodinium vancampoae Lingulodinium hemicystum, reflect estuarine to inner neritic conditions for the lower part of the section palaeoenvironmental, the occurrence of oceanic to neritic markers coinciding with a glauconitic section, suggest a marine flooding surface.Fil: Guler, Maria Veronica. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Bahía Blanca. Instituto Geológico del Sur. Universidad Nacional del Sur. Departamento de Geología. Instituto Geológico del Sur; ArgentinaFil: Guerstein, Gladys Raquel. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Bahía Blanca. Instituto Geológico del Sur. Universidad Nacional del Sur. Departamento de Geología. Instituto Geológico del Sur; ArgentinaFil: Malumian, Norberto. Secretaría de Industria y Minería. Servicio Geológico Minero Argentino; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; ArgentinaAsociación Paleontológica Argentina2002-12info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/81303Guler, Maria Veronica; Guerstein, Gladys Raquel; Malumian, Norberto; Bioestratigrafía de la Formación Barranca Final, Neógeno de la Cuenca del Colorado, Argentina; Asociación Paleontológica Argentina; Ameghiniana; 39; 1; 12-2002; 103-1100002-70141851-8044CONICET DigitalCONICETspainfo:eu-repo/semantics/altIdentifier/url/http://www.ameghiniana.org.ar/index.php/ameghiniana/article/view/2651info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-29T09:44:16Zoai:ri.conicet.gov.ar:11336/81303instacron: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:34982025-09-29 09:44:16.8CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Bioestratigrafía de la Formación Barranca Final, Neógeno de la Cuenca del Colorado, Argentina
Biostratigraphy of the Neogene Baranca Final Formation of the Colorado Basin, Argentina
title Bioestratigrafía de la Formación Barranca Final, Neógeno de la Cuenca del Colorado, Argentina
spellingShingle Bioestratigrafía de la Formación Barranca Final, Neógeno de la Cuenca del Colorado, Argentina
Guler, Maria Veronica
Formación Barranca Final
Dinoflagelados
Neogeno
Cuenca del Colorado
title_short Bioestratigrafía de la Formación Barranca Final, Neógeno de la Cuenca del Colorado, Argentina
title_full Bioestratigrafía de la Formación Barranca Final, Neógeno de la Cuenca del Colorado, Argentina
title_fullStr Bioestratigrafía de la Formación Barranca Final, Neógeno de la Cuenca del Colorado, Argentina
title_full_unstemmed Bioestratigrafía de la Formación Barranca Final, Neógeno de la Cuenca del Colorado, Argentina
title_sort Bioestratigrafía de la Formación Barranca Final, Neógeno de la Cuenca del Colorado, Argentina
dc.creator.none.fl_str_mv Guler, Maria Veronica
Guerstein, Gladys Raquel
Malumian, Norberto
author Guler, Maria Veronica
author_facet Guler, Maria Veronica
Guerstein, Gladys Raquel
Malumian, Norberto
author_role author
author2 Guerstein, Gladys Raquel
Malumian, Norberto
author2_role author
author
dc.subject.none.fl_str_mv Formación Barranca Final
Dinoflagelados
Neogeno
Cuenca del Colorado
topic Formación Barranca Final
Dinoflagelados
Neogeno
Cuenca del Colorado
purl_subject.fl_str_mv https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
dc.description.none.fl_txt_mv Dinoflagellate cysts from the Barranca Final Formation type section are diverse and well preserved. The assemblages are dominated by the Order Gonyaulacales, with subordinate Peridiniales represented only by protoperidiniaceans. Based on selected dinoflagellate cyst events, and in accordance with the foraminiferal data, we suggest a Middle to Late Miocene age for the section. Piasecki ranges from latest Early Miocene or early Middle Miocene through Late Miocene has its range base within the Middle Miocene. The occurrences of these species together with the presence of (Wall) Reid confirms an age no older than Middle Miocene for the bottom of the section. The low representation of oceanic species, such as Nematosphaeropsis rigida 150% Wrenn (inner to outer? neritic), the diverse representation of protoperidinacean species (inner neritic), and the abundance of euryhaline forms, particularly specimens of the Operculodinium centrocarpum/israelianum Tuberculodinium vancampoae Lingulodinium hemicystum, reflect estuarine to inner neritic conditions for the lower part of the section palaeoenvironmental, the occurrence of oceanic to neritic markers coinciding with a glauconitic section, suggest a marine flooding surface.
Fil: Guler, Maria Veronica. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Bahía Blanca. Instituto Geológico del Sur. Universidad Nacional del Sur. Departamento de Geología. Instituto Geológico del Sur; Argentina
Fil: Guerstein, Gladys Raquel. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Bahía Blanca. Instituto Geológico del Sur. Universidad Nacional del Sur. Departamento de Geología. Instituto Geológico del Sur; Argentina
Fil: Malumian, Norberto. Secretaría de Industria y Minería. Servicio Geológico Minero Argentino; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
description Dinoflagellate cysts from the Barranca Final Formation type section are diverse and well preserved. The assemblages are dominated by the Order Gonyaulacales, with subordinate Peridiniales represented only by protoperidiniaceans. Based on selected dinoflagellate cyst events, and in accordance with the foraminiferal data, we suggest a Middle to Late Miocene age for the section. Piasecki ranges from latest Early Miocene or early Middle Miocene through Late Miocene has its range base within the Middle Miocene. The occurrences of these species together with the presence of (Wall) Reid confirms an age no older than Middle Miocene for the bottom of the section. The low representation of oceanic species, such as Nematosphaeropsis rigida 150% Wrenn (inner to outer? neritic), the diverse representation of protoperidinacean species (inner neritic), and the abundance of euryhaline forms, particularly specimens of the Operculodinium centrocarpum/israelianum Tuberculodinium vancampoae Lingulodinium hemicystum, reflect estuarine to inner neritic conditions for the lower part of the section palaeoenvironmental, the occurrence of oceanic to neritic markers coinciding with a glauconitic section, suggest a marine flooding surface.
publishDate 2002
dc.date.none.fl_str_mv 2002-12
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/11336/81303
Guler, Maria Veronica; Guerstein, Gladys Raquel; Malumian, Norberto; Bioestratigrafía de la Formación Barranca Final, Neógeno de la Cuenca del Colorado, Argentina; Asociación Paleontológica Argentina; Ameghiniana; 39; 1; 12-2002; 103-110
0002-7014
1851-8044
CONICET Digital
CONICET
url http://hdl.handle.net/11336/81303
identifier_str_mv Guler, Maria Veronica; Guerstein, Gladys Raquel; Malumian, Norberto; Bioestratigrafía de la Formación Barranca Final, Neógeno de la Cuenca del Colorado, Argentina; Asociación Paleontológica Argentina; Ameghiniana; 39; 1; 12-2002; 103-110
0002-7014
1851-8044
CONICET Digital
CONICET
dc.language.none.fl_str_mv spa
language spa
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/url/http://www.ameghiniana.org.ar/index.php/ameghiniana/article/view/2651
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
eu_rights_str_mv openAccess
rights_invalid_str_mv https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
dc.format.none.fl_str_mv application/pdf
application/pdf
application/pdf
application/pdf
dc.publisher.none.fl_str_mv Asociación Paleontológica Argentina
publisher.none.fl_str_mv Asociación Paleontológica Argentina
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 13.070432

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