The Permian-Triassic boundary in Northern Patagonia (Argentina): Geochronological and palaeobiolontological issues of the Los Menucos Basin

Autores
Falco, Juan Ignacio; Bodnar, Josefina; Coturel, Eliana Paula; Erra, Georgina; Napoli, Matias
Año de publicación
2022
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
In the last five years, a profound revision of the stratigraphy and geochronology of northern Patagonia has been carried out. The volcanic and sedimentary succession of the LosMenucos Basin has become the focus of paleontological and geochronological studies to determine and correlate the Permian-Triassic boundary in Argentina. Luppo et al. (2018) have initially proposed a correlative of the P-T boundary (Fig. 1) within a 6 km thick concordant volcanic and sedimentary succession, which was dated between 257 ± 2 and 248 ± 2 Ma (SHRIMP U-Pb inzircon). More recently, Falco et al. (2020, 2022a, 2022b) revised the volcanic and sedimentary stratigraphy of the same succession, proposing the existence of a low angle unconformity betweenthe volcanic and sedimentary beds. With this unconformity in mind, a novel stratigraphic scheme for the Los Menucos Group was proposed, in which the P-T boundary is expected to be foundwithin the succession because it was constrained between 253 ± 3 (LAICMPS U-Pb in zircon) and 250 ± 2 Ma (see further details in Falco et al., 2020, 2022b).
Fil: Falco, Juan Ignacio. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Patagonia Norte. Instituto de Investigaciones en Diversidad Cultural y Procesos de Cambio. Universidad Nacional de Río Negro. Instituto de Investigaciones en Diversidad Cultural y Procesos de Cambio; Argentina
Fil: Bodnar, Josefina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; Argentina. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Área Paleobotánica; Argentina
Fil: Coturel, Eliana Paula. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; Argentina. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Área Paleobotánica; Argentina
Fil: Erra, Georgina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; Argentina. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Área Paleobotánica; Argentina
Fil: Napoli, Matias. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Área Paleobotánica; Argentina
Materia
PERMIAN-TRIASSIC BOUNDARY
NORTHERN PATAGONIA (ARGENTINA)
GEOCHRONOLOGICAL
LOS MENUCOS BASIN
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:11336/224622
Acceder
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network_acronym_str CONICETDig
repository_id_str 3498
network_name_str CONICET Digital (CONICET)
spelling The Permian-Triassic boundary in Northern Patagonia (Argentina): Geochronological and palaeobiolontological issues of the Los Menucos BasinFalco, Juan IgnacioBodnar, JosefinaCoturel, Eliana PaulaErra, GeorginaNapoli, MatiasPERMIAN-TRIASSIC BOUNDARYNORTHERN PATAGONIA (ARGENTINA)GEOCHRONOLOGICALLOS MENUCOS BASINhttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1In the last five years, a profound revision of the stratigraphy and geochronology of northern Patagonia has been carried out. The volcanic and sedimentary succession of the LosMenucos Basin has become the focus of paleontological and geochronological studies to determine and correlate the Permian-Triassic boundary in Argentina. Luppo et al. (2018) have initially proposed a correlative of the P-T boundary (Fig. 1) within a 6 km thick concordant volcanic and sedimentary succession, which was dated between 257 ± 2 and 248 ± 2 Ma (SHRIMP U-Pb inzircon). More recently, Falco et al. (2020, 2022a, 2022b) revised the volcanic and sedimentary stratigraphy of the same succession, proposing the existence of a low angle unconformity betweenthe volcanic and sedimentary beds. With this unconformity in mind, a novel stratigraphic scheme for the Los Menucos Group was proposed, in which the P-T boundary is expected to be foundwithin the succession because it was constrained between 253 ± 3 (LAICMPS U-Pb in zircon) and 250 ± 2 Ma (see further details in Falco et al., 2020, 2022b).Fil: Falco, Juan Ignacio. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Patagonia Norte. Instituto de Investigaciones en Diversidad Cultural y Procesos de Cambio. Universidad Nacional de Río Negro. Instituto de Investigaciones en Diversidad Cultural y Procesos de Cambio; ArgentinaFil: Bodnar, Josefina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; Argentina. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Área Paleobotánica; ArgentinaFil: Coturel, Eliana Paula. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; Argentina. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Área Paleobotánica; ArgentinaFil: Erra, Georgina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; Argentina. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Área Paleobotánica; ArgentinaFil: Napoli, Matias. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Área Paleobotánica; ArgentinaInternational Commission on Stratigraphy. Subcommission on Permian Stratigraphy2022-08info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/224622Falco, Juan Ignacio; Bodnar, Josefina; Coturel, Eliana Paula; Erra, Georgina; Napoli, Matias; The Permian-Triassic boundary in Northern Patagonia (Argentina): Geochronological and palaeobiolontological issues of the Los Menucos Basin; International Commission on Stratigraphy. Subcommission on Permian Stratigraphy; Permophiles; 73; 8-2022; 24-281684-59271684-5935CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/https://permian.stratigraphy.org/files/permophiles/Permophiles%2073.pdfinfo:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-29T10:15:24Zoai:ri.conicet.gov.ar:11336/224622instacron: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 10:15:24.328CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv The Permian-Triassic boundary in Northern Patagonia (Argentina): Geochronological and palaeobiolontological issues of the Los Menucos Basin
title The Permian-Triassic boundary in Northern Patagonia (Argentina): Geochronological and palaeobiolontological issues of the Los Menucos Basin
spellingShingle The Permian-Triassic boundary in Northern Patagonia (Argentina): Geochronological and palaeobiolontological issues of the Los Menucos Basin
Falco, Juan Ignacio
PERMIAN-TRIASSIC BOUNDARY
NORTHERN PATAGONIA (ARGENTINA)
GEOCHRONOLOGICAL
LOS MENUCOS BASIN
title_short The Permian-Triassic boundary in Northern Patagonia (Argentina): Geochronological and palaeobiolontological issues of the Los Menucos Basin
title_full The Permian-Triassic boundary in Northern Patagonia (Argentina): Geochronological and palaeobiolontological issues of the Los Menucos Basin
title_fullStr The Permian-Triassic boundary in Northern Patagonia (Argentina): Geochronological and palaeobiolontological issues of the Los Menucos Basin
title_full_unstemmed The Permian-Triassic boundary in Northern Patagonia (Argentina): Geochronological and palaeobiolontological issues of the Los Menucos Basin
title_sort The Permian-Triassic boundary in Northern Patagonia (Argentina): Geochronological and palaeobiolontological issues of the Los Menucos Basin
dc.creator.none.fl_str_mv Falco, Juan Ignacio
Bodnar, Josefina
Coturel, Eliana Paula
Erra, Georgina
Napoli, Matias
author Falco, Juan Ignacio
author_facet Falco, Juan Ignacio
Bodnar, Josefina
Coturel, Eliana Paula
Erra, Georgina
Napoli, Matias
author_role author
author2 Bodnar, Josefina
Coturel, Eliana Paula
Erra, Georgina
Napoli, Matias
author2_role author
author
author
author
dc.subject.none.fl_str_mv PERMIAN-TRIASSIC BOUNDARY
NORTHERN PATAGONIA (ARGENTINA)
GEOCHRONOLOGICAL
LOS MENUCOS BASIN
topic PERMIAN-TRIASSIC BOUNDARY
NORTHERN PATAGONIA (ARGENTINA)
GEOCHRONOLOGICAL
LOS MENUCOS BASIN
purl_subject.fl_str_mv https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
dc.description.none.fl_txt_mv In the last five years, a profound revision of the stratigraphy and geochronology of northern Patagonia has been carried out. The volcanic and sedimentary succession of the LosMenucos Basin has become the focus of paleontological and geochronological studies to determine and correlate the Permian-Triassic boundary in Argentina. Luppo et al. (2018) have initially proposed a correlative of the P-T boundary (Fig. 1) within a 6 km thick concordant volcanic and sedimentary succession, which was dated between 257 ± 2 and 248 ± 2 Ma (SHRIMP U-Pb inzircon). More recently, Falco et al. (2020, 2022a, 2022b) revised the volcanic and sedimentary stratigraphy of the same succession, proposing the existence of a low angle unconformity betweenthe volcanic and sedimentary beds. With this unconformity in mind, a novel stratigraphic scheme for the Los Menucos Group was proposed, in which the P-T boundary is expected to be foundwithin the succession because it was constrained between 253 ± 3 (LAICMPS U-Pb in zircon) and 250 ± 2 Ma (see further details in Falco et al., 2020, 2022b).
Fil: Falco, Juan Ignacio. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Patagonia Norte. Instituto de Investigaciones en Diversidad Cultural y Procesos de Cambio. Universidad Nacional de Río Negro. Instituto de Investigaciones en Diversidad Cultural y Procesos de Cambio; Argentina
Fil: Bodnar, Josefina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; Argentina. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Área Paleobotánica; Argentina
Fil: Coturel, Eliana Paula. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; Argentina. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Área Paleobotánica; Argentina
Fil: Erra, Georgina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; Argentina. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Área Paleobotánica; Argentina
Fil: Napoli, Matias. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Área Paleobotánica; Argentina
description In the last five years, a profound revision of the stratigraphy and geochronology of northern Patagonia has been carried out. The volcanic and sedimentary succession of the LosMenucos Basin has become the focus of paleontological and geochronological studies to determine and correlate the Permian-Triassic boundary in Argentina. Luppo et al. (2018) have initially proposed a correlative of the P-T boundary (Fig. 1) within a 6 km thick concordant volcanic and sedimentary succession, which was dated between 257 ± 2 and 248 ± 2 Ma (SHRIMP U-Pb inzircon). More recently, Falco et al. (2020, 2022a, 2022b) revised the volcanic and sedimentary stratigraphy of the same succession, proposing the existence of a low angle unconformity betweenthe volcanic and sedimentary beds. With this unconformity in mind, a novel stratigraphic scheme for the Los Menucos Group was proposed, in which the P-T boundary is expected to be foundwithin the succession because it was constrained between 253 ± 3 (LAICMPS U-Pb in zircon) and 250 ± 2 Ma (see further details in Falco et al., 2020, 2022b).
publishDate 2022
dc.date.none.fl_str_mv 2022-08
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/11336/224622
Falco, Juan Ignacio; Bodnar, Josefina; Coturel, Eliana Paula; Erra, Georgina; Napoli, Matias; The Permian-Triassic boundary in Northern Patagonia (Argentina): Geochronological and palaeobiolontological issues of the Los Menucos Basin; International Commission on Stratigraphy. Subcommission on Permian Stratigraphy; Permophiles; 73; 8-2022; 24-28
1684-5927
1684-5935
CONICET Digital
CONICET
url http://hdl.handle.net/11336/224622
identifier_str_mv Falco, Juan Ignacio; Bodnar, Josefina; Coturel, Eliana Paula; Erra, Georgina; Napoli, Matias; The Permian-Triassic boundary in Northern Patagonia (Argentina): Geochronological and palaeobiolontological issues of the Los Menucos Basin; International Commission on Stratigraphy. Subcommission on Permian Stratigraphy; Permophiles; 73; 8-2022; 24-28
1684-5927
1684-5935
CONICET Digital
CONICET
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/url/https://permian.stratigraphy.org/files/permophiles/Permophiles%2073.pdf
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
dc.publisher.none.fl_str_mv International Commission on Stratigraphy. Subcommission on Permian Stratigraphy
publisher.none.fl_str_mv International Commission on Stratigraphy. Subcommission on Permian Stratigraphy
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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