New age constraints on the Lower Jurassic Pliensbachian–Toarcian Boundary at Chacay Melehue (Neuquén Basin, Argentina)

Autores
Al Suwaidi, Aisha; Ruhl, Micha; Jenkyns, Hugh; Damborenea, Susana Ester; Manceñido, Miguel Oscar; Condon, Daniel J.; Angelozzi, Gladys Noemí; Kamo, Sandra L.; Storm, Marisa; Riccardi, Alberto Carlos; Hesselbo, Stephen P.
Año de publicación
2022
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
The Pliensbachian–Toarcian boundary interval is characterized by a ~ 3‰ negative carbon-isotope excursion (CIE) in organic and inorganic marine and terrestrial archives from sections in Europe, such as Peniche (Portugal) and Hawsker Bottoms, Yorkshire (UK). A new high-resolution organic-carbon isotope record, illustrating the same chemostratigraphic feature, is presented from the Southern Hemisphere Arroyo Chacay Melehue section, Chos Malal, Argentina, corroborating the global significance of this disturbance to the carbon cycle. The negative carbon-isotope excursion, mercury and organic-matter enrichment are accompanied by high-resolution ammonite and nannofossil biostratigraphy together with U–Pb CA-ID-TIMS geochronology derived from intercalated volcanic ash beds. A new age of ~ 183.73 + 0.35/− 0.50 Ma for the Pliensbachian–Toarcian boundary, and 182.77 + 0.11/− 0.15 for the tenuicostatum–serpentinum zonal boundary, is assigned based on high-precision U–Pb zircon geochronology and a Bayesian Markov chain Monte Carlo (MCMC) stratigraphic age model.
Fil: Al Suwaidi, Aisha. Khalifa University Of Science And Technology; Emiratos Arabes Unidos
Fil: Ruhl, Micha. Trinity College Dublin; Irlanda
Fil: Jenkyns, Hugh. University of Oxford; Reino Unido
Fil: Damborenea, Susana Ester. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Departamento de Paleontología Invertebrados; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; Argentina
Fil: Manceñido, Miguel Oscar. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Departamento de Paleontología Invertebrados; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; Argentina
Fil: Condon, Daniel J.. British Geological Survey (bgs);
Fil: Angelozzi, Gladys Noemí. YPF - Tecnología; Argentina
Fil: Kamo, Sandra L.. University of Toronto; Canadá
Fil: Storm, Marisa. Netherland Institute For Sea Research; Países Bajos
Fil: Riccardi, Alberto Carlos. 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. Departamento de Paleontología Invertebrados; Argentina
Fil: Hesselbo, Stephen P.. University of Exeter; Reino Unido
Materia
Pliensbachian?Toarcian
Carbon-Isotope Excursion
Neuquén Basin
Chemostratigraphy
Biostratigraphy
Geochronology
Nivel de accesibilidad
acceso abierto
Condiciones de uso
https://creativecommons.org/licenses/by/2.5/ar/
Repositorio
CONICET Digital (CONICET)
Institución
Consejo Nacional de Investigaciones Científicas y Técnicas
OAI Identificador
oai:ri.conicet.gov.ar:11336/188200
Acceder
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oai_identifier_str oai:ri.conicet.gov.ar:11336/188200
network_acronym_str CONICETDig
repository_id_str 3498
network_name_str CONICET Digital (CONICET)
spelling New age constraints on the Lower Jurassic Pliensbachian–Toarcian Boundary at Chacay Melehue (Neuquén Basin, Argentina)Al Suwaidi, AishaRuhl, MichaJenkyns, HughDamborenea, Susana EsterManceñido, Miguel OscarCondon, Daniel J.Angelozzi, Gladys NoemíKamo, Sandra L.Storm, MarisaRiccardi, Alberto CarlosHesselbo, Stephen P.Pliensbachian?ToarcianCarbon-Isotope ExcursionNeuquén BasinChemostratigraphyBiostratigraphyGeochronologyhttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1The Pliensbachian–Toarcian boundary interval is characterized by a ~ 3‰ negative carbon-isotope excursion (CIE) in organic and inorganic marine and terrestrial archives from sections in Europe, such as Peniche (Portugal) and Hawsker Bottoms, Yorkshire (UK). A new high-resolution organic-carbon isotope record, illustrating the same chemostratigraphic feature, is presented from the Southern Hemisphere Arroyo Chacay Melehue section, Chos Malal, Argentina, corroborating the global significance of this disturbance to the carbon cycle. The negative carbon-isotope excursion, mercury and organic-matter enrichment are accompanied by high-resolution ammonite and nannofossil biostratigraphy together with U–Pb CA-ID-TIMS geochronology derived from intercalated volcanic ash beds. A new age of ~ 183.73 + 0.35/− 0.50 Ma for the Pliensbachian–Toarcian boundary, and 182.77 + 0.11/− 0.15 for the tenuicostatum–serpentinum zonal boundary, is assigned based on high-precision U–Pb zircon geochronology and a Bayesian Markov chain Monte Carlo (MCMC) stratigraphic age model.Fil: Al Suwaidi, Aisha. Khalifa University Of Science And Technology; Emiratos Arabes UnidosFil: Ruhl, Micha. Trinity College Dublin; IrlandaFil: Jenkyns, Hugh. University of Oxford; Reino UnidoFil: Damborenea, Susana Ester. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Departamento de Paleontología Invertebrados; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; ArgentinaFil: Manceñido, Miguel Oscar. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Departamento de Paleontología Invertebrados; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; ArgentinaFil: Condon, Daniel J.. British Geological Survey (bgs);Fil: Angelozzi, Gladys Noemí. YPF - Tecnología; ArgentinaFil: Kamo, Sandra L.. University of Toronto; CanadáFil: Storm, Marisa. Netherland Institute For Sea Research; Países BajosFil: Riccardi, Alberto Carlos. 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. Departamento de Paleontología Invertebrados; ArgentinaFil: Hesselbo, Stephen P.. University of Exeter; Reino UnidoNature2022-12info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/188200Al Suwaidi, Aisha; Ruhl, Micha; Jenkyns, Hugh; Damborenea, Susana Ester; Manceñido, Miguel Oscar; et al.; New age constraints on the Lower Jurassic Pliensbachian–Toarcian Boundary at Chacay Melehue (Neuquén Basin, Argentina); Nature; Scientific Reports; 12; 1; 12-2022; 1-102045-23222045-2322CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/https://doi.org/10.1038/s41598-022-07886-xinfo:eu-repo/semantics/altIdentifier/doi/10.1038/s41598-022-07886-xinfo:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-03T09:48:31Zoai:ri.conicet.gov.ar:11336/188200instacron: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:34982025-09-03 09:48:32.123CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv New age constraints on the Lower Jurassic Pliensbachian–Toarcian Boundary at Chacay Melehue (Neuquén Basin, Argentina)
title New age constraints on the Lower Jurassic Pliensbachian–Toarcian Boundary at Chacay Melehue (Neuquén Basin, Argentina)
spellingShingle New age constraints on the Lower Jurassic Pliensbachian–Toarcian Boundary at Chacay Melehue (Neuquén Basin, Argentina)
Al Suwaidi, Aisha
Pliensbachian?Toarcian
Carbon-Isotope Excursion
Neuquén Basin
Chemostratigraphy
Biostratigraphy
Geochronology
title_short New age constraints on the Lower Jurassic Pliensbachian–Toarcian Boundary at Chacay Melehue (Neuquén Basin, Argentina)
title_full New age constraints on the Lower Jurassic Pliensbachian–Toarcian Boundary at Chacay Melehue (Neuquén Basin, Argentina)
title_fullStr New age constraints on the Lower Jurassic Pliensbachian–Toarcian Boundary at Chacay Melehue (Neuquén Basin, Argentina)
title_full_unstemmed New age constraints on the Lower Jurassic Pliensbachian–Toarcian Boundary at Chacay Melehue (Neuquén Basin, Argentina)
title_sort New age constraints on the Lower Jurassic Pliensbachian–Toarcian Boundary at Chacay Melehue (Neuquén Basin, Argentina)
dc.creator.none.fl_str_mv Al Suwaidi, Aisha
Ruhl, Micha
Jenkyns, Hugh
Damborenea, Susana Ester
Manceñido, Miguel Oscar
Condon, Daniel J.
Angelozzi, Gladys Noemí
Kamo, Sandra L.
Storm, Marisa
Riccardi, Alberto Carlos
Hesselbo, Stephen P.
author Al Suwaidi, Aisha
author_facet Al Suwaidi, Aisha
Ruhl, Micha
Jenkyns, Hugh
Damborenea, Susana Ester
Manceñido, Miguel Oscar
Condon, Daniel J.
Angelozzi, Gladys Noemí
Kamo, Sandra L.
Storm, Marisa
Riccardi, Alberto Carlos
Hesselbo, Stephen P.
author_role author
author2 Ruhl, Micha
Jenkyns, Hugh
Damborenea, Susana Ester
Manceñido, Miguel Oscar
Condon, Daniel J.
Angelozzi, Gladys Noemí
Kamo, Sandra L.
Storm, Marisa
Riccardi, Alberto Carlos
Hesselbo, Stephen P.
author2_role author
author
author
author
author
author
author
author
author
author
dc.subject.none.fl_str_mv Pliensbachian?Toarcian
Carbon-Isotope Excursion
Neuquén Basin
Chemostratigraphy
Biostratigraphy
Geochronology
topic Pliensbachian?Toarcian
Carbon-Isotope Excursion
Neuquén Basin
Chemostratigraphy
Biostratigraphy
Geochronology
purl_subject.fl_str_mv https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
dc.description.none.fl_txt_mv The Pliensbachian–Toarcian boundary interval is characterized by a ~ 3‰ negative carbon-isotope excursion (CIE) in organic and inorganic marine and terrestrial archives from sections in Europe, such as Peniche (Portugal) and Hawsker Bottoms, Yorkshire (UK). A new high-resolution organic-carbon isotope record, illustrating the same chemostratigraphic feature, is presented from the Southern Hemisphere Arroyo Chacay Melehue section, Chos Malal, Argentina, corroborating the global significance of this disturbance to the carbon cycle. The negative carbon-isotope excursion, mercury and organic-matter enrichment are accompanied by high-resolution ammonite and nannofossil biostratigraphy together with U–Pb CA-ID-TIMS geochronology derived from intercalated volcanic ash beds. A new age of ~ 183.73 + 0.35/− 0.50 Ma for the Pliensbachian–Toarcian boundary, and 182.77 + 0.11/− 0.15 for the tenuicostatum–serpentinum zonal boundary, is assigned based on high-precision U–Pb zircon geochronology and a Bayesian Markov chain Monte Carlo (MCMC) stratigraphic age model.
Fil: Al Suwaidi, Aisha. Khalifa University Of Science And Technology; Emiratos Arabes Unidos
Fil: Ruhl, Micha. Trinity College Dublin; Irlanda
Fil: Jenkyns, Hugh. University of Oxford; Reino Unido
Fil: Damborenea, Susana Ester. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Departamento de Paleontología Invertebrados; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; Argentina
Fil: Manceñido, Miguel Oscar. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Departamento de Paleontología Invertebrados; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; Argentina
Fil: Condon, Daniel J.. British Geological Survey (bgs);
Fil: Angelozzi, Gladys Noemí. YPF - Tecnología; Argentina
Fil: Kamo, Sandra L.. University of Toronto; Canadá
Fil: Storm, Marisa. Netherland Institute For Sea Research; Países Bajos
Fil: Riccardi, Alberto Carlos. 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. Departamento de Paleontología Invertebrados; Argentina
Fil: Hesselbo, Stephen P.. University of Exeter; Reino Unido
description The Pliensbachian–Toarcian boundary interval is characterized by a ~ 3‰ negative carbon-isotope excursion (CIE) in organic and inorganic marine and terrestrial archives from sections in Europe, such as Peniche (Portugal) and Hawsker Bottoms, Yorkshire (UK). A new high-resolution organic-carbon isotope record, illustrating the same chemostratigraphic feature, is presented from the Southern Hemisphere Arroyo Chacay Melehue section, Chos Malal, Argentina, corroborating the global significance of this disturbance to the carbon cycle. The negative carbon-isotope excursion, mercury and organic-matter enrichment are accompanied by high-resolution ammonite and nannofossil biostratigraphy together with U–Pb CA-ID-TIMS geochronology derived from intercalated volcanic ash beds. A new age of ~ 183.73 + 0.35/− 0.50 Ma for the Pliensbachian–Toarcian boundary, and 182.77 + 0.11/− 0.15 for the tenuicostatum–serpentinum zonal boundary, is assigned based on high-precision U–Pb zircon geochronology and a Bayesian Markov chain Monte Carlo (MCMC) stratigraphic age model.
publishDate 2022
dc.date.none.fl_str_mv 2022-12
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/11336/188200
Al Suwaidi, Aisha; Ruhl, Micha; Jenkyns, Hugh; Damborenea, Susana Ester; Manceñido, Miguel Oscar; et al.; New age constraints on the Lower Jurassic Pliensbachian–Toarcian Boundary at Chacay Melehue (Neuquén Basin, Argentina); Nature; Scientific Reports; 12; 1; 12-2022; 1-10
2045-2322
2045-2322
CONICET Digital
CONICET
url http://hdl.handle.net/11336/188200
identifier_str_mv Al Suwaidi, Aisha; Ruhl, Micha; Jenkyns, Hugh; Damborenea, Susana Ester; Manceñido, Miguel Oscar; et al.; New age constraints on the Lower Jurassic Pliensbachian–Toarcian Boundary at Chacay Melehue (Neuquén Basin, Argentina); Nature; Scientific Reports; 12; 1; 12-2022; 1-10
2045-2322
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://doi.org/10.1038/s41598-022-07886-x
info:eu-repo/semantics/altIdentifier/doi/10.1038/s41598-022-07886-x
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by/2.5/ar/
eu_rights_str_mv openAccess
rights_invalid_str_mv https://creativecommons.org/licenses/by/2.5/ar/
dc.format.none.fl_str_mv application/pdf
application/pdf
dc.publisher.none.fl_str_mv Nature
publisher.none.fl_str_mv Nature
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 13.13397

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