Early Devonian organic-walled microfossils from outcrop samples of the Cordob´es Formation, Durazno Group, Norte Basin, Uruguay

Autores
Daners, Gloria; Rodriguez Amenabar, Cecilia; Uriz, Norberto Javier; Rojas, Alejandra
Año de publicación
2018
Idioma
inglés
Tipo de recurso
documento de conferencia
Estado
versión publicada
Descripción
The Durazno Group documented an Early Devonian transgressive-regressive cycle of sedimentation in the southernmost portion of the intracratonic Paran´a Basin, in Uruguay known as the Norte Basin. The group comprises from base to top the Cerrezuelo, Cordobes and La Paloma Formations. The Cordobes Formation was deposited during the maximum flooding of the transgressive event, and contains Malvinokaffric marine invertebrates that inhabited Gondwanan cold marine waters, acanthodian fishes and trace fossils. The first palynological studies of the Cordobes Formation date from the 60?s and 70?s, from one outcrop, which reports the presence of phytoplankton and miospores but they only described a few acritarchs. In recent years, works referred to this unit have notably increased due to hydrocarbons exploration, but the results come from samples obtained mainly from boreholes. In order to expand the knowledge regarding Devonian palynofloras of Uruguay, in this contribution, we document the palynological assemblages collected from outcrop samples of the Cordobès Formation, near Blanquillo town in the Durazno Department. Some identified species allowed constraining the age of the unit and its correlation with other Early Devonian assemblages from South America. The studied samples contain acritarchs, prasinophytes, chlorophytes, chitinozoans, scolecodonts and miospores. The most representative phytoplankton species are Cordobesia urguayensis, Dictyotidium dictyotum, Estiastra uruguaia, Exochoderma arca, E. triangularis, Palacanthus ledanoisii, Polyedrixium fragosulum, Triangulina alargada, Quadrisporites horridus, Veryhachium trispinosum and V. woodii. The miospores include the following species: Apiculiretusispora brandtii, Cymbohilates sp., Emphanisporites rotatus, Dibolisporites echinaceus, Dictyotriletes emsiensis and Knoxisporites riondae. The presence of the acritarch Veryachium woodii, recently described from borehole samples of the Cordobes Formation, allows to constrain the age at the proximity of the Pragian-Emsian boundary, where also Knoxisporites riondae becomes a common taxa. Cordobesia species and Dictyotriletes emsiensis are forms restricted to Gondwana. Besides this, Dictyotriletes emsiensis allows the correlation with Furnas and Ponta Grossa Formations (Brazil) and Talacasto Formation (Argentina). The Early Devonian age is also supported by fossil invertebrates as well as U-Pb ages of detrital zircons obtained from the Duranzo Group.
Fil: Daners, Gloria. Universidad de la República; Uruguay
Fil: Rodriguez Amenabar, Cecilia. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Estudios Andinos "Don Pablo Groeber". Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Estudios Andinos "Don Pablo Groeber"; Argentina. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Departamento de Geología. Cátedra de Paleontología; Argentina. Ministerio de Relaciones Exteriores, Comercio Interno y Culto. Dirección Nacional del Antártico. Instituto Antártico Argentino; Argentina
Fil: Uriz, Norberto Javier. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo; Argentina
Fil: Rojas, Alejandra. Universidad de la República; Uruguay
5th International Palaeontological Congress
Paris
Francia
International Palaeontological Association
Materia
MICROFOSILES ORGANICOS
DEVÒNICO TEMPRANO
GRUPO DURAZNO
URUGUAY
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:11336/228739

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network_name_str CONICET Digital (CONICET)
spelling Early Devonian organic-walled microfossils from outcrop samples of the Cordob´es Formation, Durazno Group, Norte Basin, UruguayDaners, GloriaRodriguez Amenabar, CeciliaUriz, Norberto JavierRojas, AlejandraMICROFOSILES ORGANICOSDEVÒNICO TEMPRANOGRUPO DURAZNOURUGUAYhttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1The Durazno Group documented an Early Devonian transgressive-regressive cycle of sedimentation in the southernmost portion of the intracratonic Paran´a Basin, in Uruguay known as the Norte Basin. The group comprises from base to top the Cerrezuelo, Cordobes and La Paloma Formations. The Cordobes Formation was deposited during the maximum flooding of the transgressive event, and contains Malvinokaffric marine invertebrates that inhabited Gondwanan cold marine waters, acanthodian fishes and trace fossils. The first palynological studies of the Cordobes Formation date from the 60?s and 70?s, from one outcrop, which reports the presence of phytoplankton and miospores but they only described a few acritarchs. In recent years, works referred to this unit have notably increased due to hydrocarbons exploration, but the results come from samples obtained mainly from boreholes. In order to expand the knowledge regarding Devonian palynofloras of Uruguay, in this contribution, we document the palynological assemblages collected from outcrop samples of the Cordobès Formation, near Blanquillo town in the Durazno Department. Some identified species allowed constraining the age of the unit and its correlation with other Early Devonian assemblages from South America. The studied samples contain acritarchs, prasinophytes, chlorophytes, chitinozoans, scolecodonts and miospores. The most representative phytoplankton species are Cordobesia urguayensis, Dictyotidium dictyotum, Estiastra uruguaia, Exochoderma arca, E. triangularis, Palacanthus ledanoisii, Polyedrixium fragosulum, Triangulina alargada, Quadrisporites horridus, Veryhachium trispinosum and V. woodii. The miospores include the following species: Apiculiretusispora brandtii, Cymbohilates sp., Emphanisporites rotatus, Dibolisporites echinaceus, Dictyotriletes emsiensis and Knoxisporites riondae. The presence of the acritarch Veryachium woodii, recently described from borehole samples of the Cordobes Formation, allows to constrain the age at the proximity of the Pragian-Emsian boundary, where also Knoxisporites riondae becomes a common taxa. Cordobesia species and Dictyotriletes emsiensis are forms restricted to Gondwana. Besides this, Dictyotriletes emsiensis allows the correlation with Furnas and Ponta Grossa Formations (Brazil) and Talacasto Formation (Argentina). The Early Devonian age is also supported by fossil invertebrates as well as U-Pb ages of detrital zircons obtained from the Duranzo Group.Fil: Daners, Gloria. Universidad de la República; UruguayFil: Rodriguez Amenabar, Cecilia. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Estudios Andinos "Don Pablo Groeber". Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Estudios Andinos "Don Pablo Groeber"; Argentina. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Departamento de Geología. Cátedra de Paleontología; Argentina. Ministerio de Relaciones Exteriores, Comercio Interno y Culto. Dirección Nacional del Antártico. Instituto Antártico Argentino; ArgentinaFil: Uriz, Norberto Javier. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo; ArgentinaFil: Rojas, Alejandra. Universidad de la República; Uruguay5th International Palaeontological CongressParisFranciaInternational Palaeontological AssociationInternational Palaeontological Association2018info:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/conferenceObjectCongresoBookhttp://purl.org/coar/resource_type/c_5794info:ar-repo/semantics/documentoDeConferenciaapplication/pdfapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/228739Early Devonian organic-walled microfossils from outcrop samples of the Cordob´es Formation, Durazno Group, Norte Basin, Uruguay; 5th International Palaeontological Congress; Paris; Francia; 2018; 528-528CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/https://ipc5.sciencesconf.org/data/IPC5_Abstract_Book.pdfInternacionalinfo:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-03T09:55:54Zoai:ri.conicet.gov.ar:11336/228739instacron: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 09:55:55.606CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Early Devonian organic-walled microfossils from outcrop samples of the Cordob´es Formation, Durazno Group, Norte Basin, Uruguay
title Early Devonian organic-walled microfossils from outcrop samples of the Cordob´es Formation, Durazno Group, Norte Basin, Uruguay
spellingShingle Early Devonian organic-walled microfossils from outcrop samples of the Cordob´es Formation, Durazno Group, Norte Basin, Uruguay
Daners, Gloria
MICROFOSILES ORGANICOS
DEVÒNICO TEMPRANO
GRUPO DURAZNO
URUGUAY
title_short Early Devonian organic-walled microfossils from outcrop samples of the Cordob´es Formation, Durazno Group, Norte Basin, Uruguay
title_full Early Devonian organic-walled microfossils from outcrop samples of the Cordob´es Formation, Durazno Group, Norte Basin, Uruguay
title_fullStr Early Devonian organic-walled microfossils from outcrop samples of the Cordob´es Formation, Durazno Group, Norte Basin, Uruguay
title_full_unstemmed Early Devonian organic-walled microfossils from outcrop samples of the Cordob´es Formation, Durazno Group, Norte Basin, Uruguay
title_sort Early Devonian organic-walled microfossils from outcrop samples of the Cordob´es Formation, Durazno Group, Norte Basin, Uruguay
dc.creator.none.fl_str_mv Daners, Gloria
Rodriguez Amenabar, Cecilia
Uriz, Norberto Javier
Rojas, Alejandra
author Daners, Gloria
author_facet Daners, Gloria
Rodriguez Amenabar, Cecilia
Uriz, Norberto Javier
Rojas, Alejandra
author_role author
author2 Rodriguez Amenabar, Cecilia
Uriz, Norberto Javier
Rojas, Alejandra
author2_role author
author
author
dc.subject.none.fl_str_mv MICROFOSILES ORGANICOS
DEVÒNICO TEMPRANO
GRUPO DURAZNO
URUGUAY
topic MICROFOSILES ORGANICOS
DEVÒNICO TEMPRANO
GRUPO DURAZNO
URUGUAY
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 Durazno Group documented an Early Devonian transgressive-regressive cycle of sedimentation in the southernmost portion of the intracratonic Paran´a Basin, in Uruguay known as the Norte Basin. The group comprises from base to top the Cerrezuelo, Cordobes and La Paloma Formations. The Cordobes Formation was deposited during the maximum flooding of the transgressive event, and contains Malvinokaffric marine invertebrates that inhabited Gondwanan cold marine waters, acanthodian fishes and trace fossils. The first palynological studies of the Cordobes Formation date from the 60?s and 70?s, from one outcrop, which reports the presence of phytoplankton and miospores but they only described a few acritarchs. In recent years, works referred to this unit have notably increased due to hydrocarbons exploration, but the results come from samples obtained mainly from boreholes. In order to expand the knowledge regarding Devonian palynofloras of Uruguay, in this contribution, we document the palynological assemblages collected from outcrop samples of the Cordobès Formation, near Blanquillo town in the Durazno Department. Some identified species allowed constraining the age of the unit and its correlation with other Early Devonian assemblages from South America. The studied samples contain acritarchs, prasinophytes, chlorophytes, chitinozoans, scolecodonts and miospores. The most representative phytoplankton species are Cordobesia urguayensis, Dictyotidium dictyotum, Estiastra uruguaia, Exochoderma arca, E. triangularis, Palacanthus ledanoisii, Polyedrixium fragosulum, Triangulina alargada, Quadrisporites horridus, Veryhachium trispinosum and V. woodii. The miospores include the following species: Apiculiretusispora brandtii, Cymbohilates sp., Emphanisporites rotatus, Dibolisporites echinaceus, Dictyotriletes emsiensis and Knoxisporites riondae. The presence of the acritarch Veryachium woodii, recently described from borehole samples of the Cordobes Formation, allows to constrain the age at the proximity of the Pragian-Emsian boundary, where also Knoxisporites riondae becomes a common taxa. Cordobesia species and Dictyotriletes emsiensis are forms restricted to Gondwana. Besides this, Dictyotriletes emsiensis allows the correlation with Furnas and Ponta Grossa Formations (Brazil) and Talacasto Formation (Argentina). The Early Devonian age is also supported by fossil invertebrates as well as U-Pb ages of detrital zircons obtained from the Duranzo Group.
Fil: Daners, Gloria. Universidad de la República; Uruguay
Fil: Rodriguez Amenabar, Cecilia. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Estudios Andinos "Don Pablo Groeber". Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Estudios Andinos "Don Pablo Groeber"; Argentina. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Departamento de Geología. Cátedra de Paleontología; Argentina. Ministerio de Relaciones Exteriores, Comercio Interno y Culto. Dirección Nacional del Antártico. Instituto Antártico Argentino; Argentina
Fil: Uriz, Norberto Javier. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo; Argentina
Fil: Rojas, Alejandra. Universidad de la República; Uruguay
5th International Palaeontological Congress
Paris
Francia
International Palaeontological Association
description The Durazno Group documented an Early Devonian transgressive-regressive cycle of sedimentation in the southernmost portion of the intracratonic Paran´a Basin, in Uruguay known as the Norte Basin. The group comprises from base to top the Cerrezuelo, Cordobes and La Paloma Formations. The Cordobes Formation was deposited during the maximum flooding of the transgressive event, and contains Malvinokaffric marine invertebrates that inhabited Gondwanan cold marine waters, acanthodian fishes and trace fossils. The first palynological studies of the Cordobes Formation date from the 60?s and 70?s, from one outcrop, which reports the presence of phytoplankton and miospores but they only described a few acritarchs. In recent years, works referred to this unit have notably increased due to hydrocarbons exploration, but the results come from samples obtained mainly from boreholes. In order to expand the knowledge regarding Devonian palynofloras of Uruguay, in this contribution, we document the palynological assemblages collected from outcrop samples of the Cordobès Formation, near Blanquillo town in the Durazno Department. Some identified species allowed constraining the age of the unit and its correlation with other Early Devonian assemblages from South America. The studied samples contain acritarchs, prasinophytes, chlorophytes, chitinozoans, scolecodonts and miospores. The most representative phytoplankton species are Cordobesia urguayensis, Dictyotidium dictyotum, Estiastra uruguaia, Exochoderma arca, E. triangularis, Palacanthus ledanoisii, Polyedrixium fragosulum, Triangulina alargada, Quadrisporites horridus, Veryhachium trispinosum and V. woodii. The miospores include the following species: Apiculiretusispora brandtii, Cymbohilates sp., Emphanisporites rotatus, Dibolisporites echinaceus, Dictyotriletes emsiensis and Knoxisporites riondae. The presence of the acritarch Veryachium woodii, recently described from borehole samples of the Cordobes Formation, allows to constrain the age at the proximity of the Pragian-Emsian boundary, where also Knoxisporites riondae becomes a common taxa. Cordobesia species and Dictyotriletes emsiensis are forms restricted to Gondwana. Besides this, Dictyotriletes emsiensis allows the correlation with Furnas and Ponta Grossa Formations (Brazil) and Talacasto Formation (Argentina). The Early Devonian age is also supported by fossil invertebrates as well as U-Pb ages of detrital zircons obtained from the Duranzo Group.
publishDate 2018
dc.date.none.fl_str_mv 2018
dc.type.none.fl_str_mv info:eu-repo/semantics/publishedVersion
info:eu-repo/semantics/conferenceObject
Congreso
Book
http://purl.org/coar/resource_type/c_5794
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status_str publishedVersion
format conferenceObject
dc.identifier.none.fl_str_mv http://hdl.handle.net/11336/228739
Early Devonian organic-walled microfossils from outcrop samples of the Cordob´es Formation, Durazno Group, Norte Basin, Uruguay; 5th International Palaeontological Congress; Paris; Francia; 2018; 528-528
CONICET Digital
CONICET
url http://hdl.handle.net/11336/228739
identifier_str_mv Early Devonian organic-walled microfossils from outcrop samples of the Cordob´es Formation, Durazno Group, Norte Basin, Uruguay; 5th International Palaeontological Congress; Paris; Francia; 2018; 528-528
CONICET Digital
CONICET
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language eng
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publisher.none.fl_str_mv International Palaeontological Association
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