Late paleozoic brachiopod zonation in west and east-central Argentina and its correlation with other south american basins

Autores
Cisterna, Gabriela Adriana; Sterren, Andrea Fabiana
Año de publicación
2021
Idioma
inglés
Tipo de recurso
documento de conferencia
Estado
versión publicada
Descripción
Brachiopods, one of the most abundant and diversified groups in the late Paleozoic benthic marine communities, are not particularly time-sensitive fossils but have been considered good tools for characterizing, correlating and assigning a relative age to the sedimentary successions. Although the Argentinian brachiopod faunas are among the better known for the late Paleozoic of South America, the absence of more precise biostratigraphic markers, the scarce radiometric data available and the strong faunal provincialism, prevent developing a high-resolution scheme. However, the marine stratigraphic record of the Mississippian–Pennsylvanian in central-western Argentina, considered to be one of the most complete in the region, allows the confection of a brachiopod zonation that provides the basis for correlations with other South American basins. Five brachiopod zones are proposed, namely Azurduya chavelensis (Tournaisian–Visean) restricted to the Río Blanco Basin and also identified in northern Chile; Levipustula levis (late Serpukhovian–early Bashkirian), typically associated to the postglacial transgression of the second glacial episode identified in the region, and also recorded from the Bolivian Tarija Basin; Marginovatia peregrina-Maemia tenuiscostata (late Bashkirian–early Moscovian), a zone of local value defined in the Barreal Hill of the Calingasta-Uspallata basin; Tivertonia jachalensis-Streptorhynchus inaequiornatus (Moscovian), the most widely distributed and diversified in the Precordillera, developed in relatively warm temperate conditions; and the youngest Costatumlulus amosi (?Sakmarian–?Artinskian), a low-diversity brachiopod assemblage only recorded in the southernmost part the Calingasta-Uspallata Basin, whose biostratigraphic relationships with the TivertoniaStreptorhynchus Fauna still needs revision. It is also important to note that brachiopods of the Levipustula levis zone have a relatively coeval postglacial fauna (Aseptella-Tuberculatella/Rhipidomella-Micraphelia). The significant compositional differences identified between both faunas have been explained by a group of abiotic factors directly related to glacial retreat dynamics and the coastal configuration. Age of the brachiopod zones mentioned above is mainly based on the palynological-palaeofloristic information but radiometric data have been also provided for the Levipustula levis zone (319.57±0.09 Ma U-Pb ages dated from the Guandacol Formation) and the Tivertonia jachalensis-Streptorhynchus inaequiornatus zone (312.82±0.11 Ma U-Pb ages from the transgressive marine deposits of the Tupe Formation). In eastcentral Argentina, in the Sauce Grande Basin, brachiopod assemblages integrate the Tomiopsis harringtoni zone herein proposed, restricted to pre-Sakmarian because of the SHRIMP age of 280.8±1.9 Ma from tuff-rich levels in the Tunas Formation. This fauna appears typically associated with the postglacial Eurydesma Fauna also identified in the glacial sequences of the Paraná Basin, Brazil, as the Eurydesma-Lyonia Fauna.
Fil: Cisterna, Gabriela Adriana. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Tucumán. Instituto Superior de Correlación Geológica. Universidad Nacional de Tucumán. Facultad de Ciencias Naturales e Instituto Miguel Lillo. Departamento de Geología. Cátedra Geología Estructural. Instituto Superior de Correlación Geológica; Argentina
Fil: Sterren, Andrea Fabiana. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Córdoba. Centro de Investigaciones en Ciencias de la Tierra. Universidad Nacional de Córdoba. Facultad de Ciencias Exactas Físicas y Naturales. Centro de Investigaciones en Ciencias de la Tierra; Argentina
XII Congreso de la Asociación Paleontológica Argentina
Ciudad Autónoma de Buenos Aires
Argentina
Asociación Paleontológica Argentina
Materia
BRACHIOPODS
LATE PALEOZOIC
BIOSTRATIGRAPHY
SOUTH AMERICA
Nivel de accesibilidad
acceso abierto
Condiciones de uso
https://creativecommons.org/licenses/by-nd/2.5/ar/
Repositorio
CONICET Digital (CONICET)
Institución
Consejo Nacional de Investigaciones Científicas y Técnicas
OAI Identificador
oai:ri.conicet.gov.ar:11336/237678

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spelling Late paleozoic brachiopod zonation in west and east-central Argentina and its correlation with other south american basinsCisterna, Gabriela AdrianaSterren, Andrea FabianaBRACHIOPODSLATE PALEOZOICBIOSTRATIGRAPHYSOUTH AMERICAhttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1Brachiopods, one of the most abundant and diversified groups in the late Paleozoic benthic marine communities, are not particularly time-sensitive fossils but have been considered good tools for characterizing, correlating and assigning a relative age to the sedimentary successions. Although the Argentinian brachiopod faunas are among the better known for the late Paleozoic of South America, the absence of more precise biostratigraphic markers, the scarce radiometric data available and the strong faunal provincialism, prevent developing a high-resolution scheme. However, the marine stratigraphic record of the Mississippian–Pennsylvanian in central-western Argentina, considered to be one of the most complete in the region, allows the confection of a brachiopod zonation that provides the basis for correlations with other South American basins. Five brachiopod zones are proposed, namely Azurduya chavelensis (Tournaisian–Visean) restricted to the Río Blanco Basin and also identified in northern Chile; Levipustula levis (late Serpukhovian–early Bashkirian), typically associated to the postglacial transgression of the second glacial episode identified in the region, and also recorded from the Bolivian Tarija Basin; Marginovatia peregrina-Maemia tenuiscostata (late Bashkirian–early Moscovian), a zone of local value defined in the Barreal Hill of the Calingasta-Uspallata basin; Tivertonia jachalensis-Streptorhynchus inaequiornatus (Moscovian), the most widely distributed and diversified in the Precordillera, developed in relatively warm temperate conditions; and the youngest Costatumlulus amosi (?Sakmarian–?Artinskian), a low-diversity brachiopod assemblage only recorded in the southernmost part the Calingasta-Uspallata Basin, whose biostratigraphic relationships with the TivertoniaStreptorhynchus Fauna still needs revision. It is also important to note that brachiopods of the Levipustula levis zone have a relatively coeval postglacial fauna (Aseptella-Tuberculatella/Rhipidomella-Micraphelia). The significant compositional differences identified between both faunas have been explained by a group of abiotic factors directly related to glacial retreat dynamics and the coastal configuration. Age of the brachiopod zones mentioned above is mainly based on the palynological-palaeofloristic information but radiometric data have been also provided for the Levipustula levis zone (319.57±0.09 Ma U-Pb ages dated from the Guandacol Formation) and the Tivertonia jachalensis-Streptorhynchus inaequiornatus zone (312.82±0.11 Ma U-Pb ages from the transgressive marine deposits of the Tupe Formation). In eastcentral Argentina, in the Sauce Grande Basin, brachiopod assemblages integrate the Tomiopsis harringtoni zone herein proposed, restricted to pre-Sakmarian because of the SHRIMP age of 280.8±1.9 Ma from tuff-rich levels in the Tunas Formation. This fauna appears typically associated with the postglacial Eurydesma Fauna also identified in the glacial sequences of the Paraná Basin, Brazil, as the Eurydesma-Lyonia Fauna.Fil: Cisterna, Gabriela Adriana. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Tucumán. Instituto Superior de Correlación Geológica. Universidad Nacional de Tucumán. Facultad de Ciencias Naturales e Instituto Miguel Lillo. Departamento de Geología. Cátedra Geología Estructural. Instituto Superior de Correlación Geológica; ArgentinaFil: Sterren, Andrea Fabiana. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Córdoba. Centro de Investigaciones en Ciencias de la Tierra. Universidad Nacional de Córdoba. Facultad de Ciencias Exactas Físicas y Naturales. Centro de Investigaciones en Ciencias de la Tierra; ArgentinaXII Congreso de la Asociación Paleontológica ArgentinaCiudad Autónoma de Buenos AiresArgentinaAsociación Paleontológica ArgentinaAsociación Paleontológica Argentina2021info:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/conferenceObjectCongresoJournalhttp://purl.org/coar/resource_type/c_5794info:ar-repo/semantics/documentoDeConferenciaapplication/pdfapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/237678Late paleozoic brachiopod zonation in west and east-central Argentina and its correlation with other south american basins; XII Congreso de la Asociación Paleontológica Argentina; Ciudad Autónoma de Buenos Aires; Argentina; 2021; 164-1642469-0228CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/https://www.apaleontologica.org.ar/reuniones-anteriores-capa/info:eu-repo/semantics/altIdentifier/url/https://www.peapaleontologica.org.ar/index.php/peapa/article/view/422Internacionalinfo:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nd/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-03T09:55:47Zoai:ri.conicet.gov.ar:11336/237678instacron: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 09:55:47.261CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Late paleozoic brachiopod zonation in west and east-central Argentina and its correlation with other south american basins
title Late paleozoic brachiopod zonation in west and east-central Argentina and its correlation with other south american basins
spellingShingle Late paleozoic brachiopod zonation in west and east-central Argentina and its correlation with other south american basins
Cisterna, Gabriela Adriana
BRACHIOPODS
LATE PALEOZOIC
BIOSTRATIGRAPHY
SOUTH AMERICA
title_short Late paleozoic brachiopod zonation in west and east-central Argentina and its correlation with other south american basins
title_full Late paleozoic brachiopod zonation in west and east-central Argentina and its correlation with other south american basins
title_fullStr Late paleozoic brachiopod zonation in west and east-central Argentina and its correlation with other south american basins
title_full_unstemmed Late paleozoic brachiopod zonation in west and east-central Argentina and its correlation with other south american basins
title_sort Late paleozoic brachiopod zonation in west and east-central Argentina and its correlation with other south american basins
dc.creator.none.fl_str_mv Cisterna, Gabriela Adriana
Sterren, Andrea Fabiana
author Cisterna, Gabriela Adriana
author_facet Cisterna, Gabriela Adriana
Sterren, Andrea Fabiana
author_role author
author2 Sterren, Andrea Fabiana
author2_role author
dc.subject.none.fl_str_mv BRACHIOPODS
LATE PALEOZOIC
BIOSTRATIGRAPHY
SOUTH AMERICA
topic BRACHIOPODS
LATE PALEOZOIC
BIOSTRATIGRAPHY
SOUTH AMERICA
purl_subject.fl_str_mv https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
dc.description.none.fl_txt_mv Brachiopods, one of the most abundant and diversified groups in the late Paleozoic benthic marine communities, are not particularly time-sensitive fossils but have been considered good tools for characterizing, correlating and assigning a relative age to the sedimentary successions. Although the Argentinian brachiopod faunas are among the better known for the late Paleozoic of South America, the absence of more precise biostratigraphic markers, the scarce radiometric data available and the strong faunal provincialism, prevent developing a high-resolution scheme. However, the marine stratigraphic record of the Mississippian–Pennsylvanian in central-western Argentina, considered to be one of the most complete in the region, allows the confection of a brachiopod zonation that provides the basis for correlations with other South American basins. Five brachiopod zones are proposed, namely Azurduya chavelensis (Tournaisian–Visean) restricted to the Río Blanco Basin and also identified in northern Chile; Levipustula levis (late Serpukhovian–early Bashkirian), typically associated to the postglacial transgression of the second glacial episode identified in the region, and also recorded from the Bolivian Tarija Basin; Marginovatia peregrina-Maemia tenuiscostata (late Bashkirian–early Moscovian), a zone of local value defined in the Barreal Hill of the Calingasta-Uspallata basin; Tivertonia jachalensis-Streptorhynchus inaequiornatus (Moscovian), the most widely distributed and diversified in the Precordillera, developed in relatively warm temperate conditions; and the youngest Costatumlulus amosi (?Sakmarian–?Artinskian), a low-diversity brachiopod assemblage only recorded in the southernmost part the Calingasta-Uspallata Basin, whose biostratigraphic relationships with the TivertoniaStreptorhynchus Fauna still needs revision. It is also important to note that brachiopods of the Levipustula levis zone have a relatively coeval postglacial fauna (Aseptella-Tuberculatella/Rhipidomella-Micraphelia). The significant compositional differences identified between both faunas have been explained by a group of abiotic factors directly related to glacial retreat dynamics and the coastal configuration. Age of the brachiopod zones mentioned above is mainly based on the palynological-palaeofloristic information but radiometric data have been also provided for the Levipustula levis zone (319.57±0.09 Ma U-Pb ages dated from the Guandacol Formation) and the Tivertonia jachalensis-Streptorhynchus inaequiornatus zone (312.82±0.11 Ma U-Pb ages from the transgressive marine deposits of the Tupe Formation). In eastcentral Argentina, in the Sauce Grande Basin, brachiopod assemblages integrate the Tomiopsis harringtoni zone herein proposed, restricted to pre-Sakmarian because of the SHRIMP age of 280.8±1.9 Ma from tuff-rich levels in the Tunas Formation. This fauna appears typically associated with the postglacial Eurydesma Fauna also identified in the glacial sequences of the Paraná Basin, Brazil, as the Eurydesma-Lyonia Fauna.
Fil: Cisterna, Gabriela Adriana. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Tucumán. Instituto Superior de Correlación Geológica. Universidad Nacional de Tucumán. Facultad de Ciencias Naturales e Instituto Miguel Lillo. Departamento de Geología. Cátedra Geología Estructural. Instituto Superior de Correlación Geológica; Argentina
Fil: Sterren, Andrea Fabiana. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Córdoba. Centro de Investigaciones en Ciencias de la Tierra. Universidad Nacional de Córdoba. Facultad de Ciencias Exactas Físicas y Naturales. Centro de Investigaciones en Ciencias de la Tierra; Argentina
XII Congreso de la Asociación Paleontológica Argentina
Ciudad Autónoma de Buenos Aires
Argentina
Asociación Paleontológica Argentina
description Brachiopods, one of the most abundant and diversified groups in the late Paleozoic benthic marine communities, are not particularly time-sensitive fossils but have been considered good tools for characterizing, correlating and assigning a relative age to the sedimentary successions. Although the Argentinian brachiopod faunas are among the better known for the late Paleozoic of South America, the absence of more precise biostratigraphic markers, the scarce radiometric data available and the strong faunal provincialism, prevent developing a high-resolution scheme. However, the marine stratigraphic record of the Mississippian–Pennsylvanian in central-western Argentina, considered to be one of the most complete in the region, allows the confection of a brachiopod zonation that provides the basis for correlations with other South American basins. Five brachiopod zones are proposed, namely Azurduya chavelensis (Tournaisian–Visean) restricted to the Río Blanco Basin and also identified in northern Chile; Levipustula levis (late Serpukhovian–early Bashkirian), typically associated to the postglacial transgression of the second glacial episode identified in the region, and also recorded from the Bolivian Tarija Basin; Marginovatia peregrina-Maemia tenuiscostata (late Bashkirian–early Moscovian), a zone of local value defined in the Barreal Hill of the Calingasta-Uspallata basin; Tivertonia jachalensis-Streptorhynchus inaequiornatus (Moscovian), the most widely distributed and diversified in the Precordillera, developed in relatively warm temperate conditions; and the youngest Costatumlulus amosi (?Sakmarian–?Artinskian), a low-diversity brachiopod assemblage only recorded in the southernmost part the Calingasta-Uspallata Basin, whose biostratigraphic relationships with the TivertoniaStreptorhynchus Fauna still needs revision. It is also important to note that brachiopods of the Levipustula levis zone have a relatively coeval postglacial fauna (Aseptella-Tuberculatella/Rhipidomella-Micraphelia). The significant compositional differences identified between both faunas have been explained by a group of abiotic factors directly related to glacial retreat dynamics and the coastal configuration. Age of the brachiopod zones mentioned above is mainly based on the palynological-palaeofloristic information but radiometric data have been also provided for the Levipustula levis zone (319.57±0.09 Ma U-Pb ages dated from the Guandacol Formation) and the Tivertonia jachalensis-Streptorhynchus inaequiornatus zone (312.82±0.11 Ma U-Pb ages from the transgressive marine deposits of the Tupe Formation). In eastcentral Argentina, in the Sauce Grande Basin, brachiopod assemblages integrate the Tomiopsis harringtoni zone herein proposed, restricted to pre-Sakmarian because of the SHRIMP age of 280.8±1.9 Ma from tuff-rich levels in the Tunas Formation. This fauna appears typically associated with the postglacial Eurydesma Fauna also identified in the glacial sequences of the Paraná Basin, Brazil, as the Eurydesma-Lyonia Fauna.
publishDate 2021
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Late paleozoic brachiopod zonation in west and east-central Argentina and its correlation with other south american basins; XII Congreso de la Asociación Paleontológica Argentina; Ciudad Autónoma de Buenos Aires; Argentina; 2021; 164-164
2469-0228
CONICET Digital
CONICET
url http://hdl.handle.net/11336/237678
identifier_str_mv Late paleozoic brachiopod zonation in west and east-central Argentina and its correlation with other south american basins; XII Congreso de la Asociación Paleontológica Argentina; Ciudad Autónoma de Buenos Aires; Argentina; 2021; 164-164
2469-0228
CONICET Digital
CONICET
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