The Hirnantian-Early Llandovery transition sequence in the Paraná basin, Eastern Paraguay
- Autores
- Cingolani, Carlos Alberto; Uriz, Norberto Javier; Alfaro, Marta Beatríz; Tortello, Marcelo Franco; Bidone, Andrea Rosa; Galeano Inchausti, Julio César
- Año de publicación
- 2011
- Idioma
- inglés
- Tipo de recurso
- documento de conferencia
- Estado
- versión publicada
- Descripción
- The Lower Paleozoic Itacurubí Group (Harrington, 1972) is exposed in the western border of the intracratonic Paraná Basin of eastern Paraguay (Fig. 1). This group (c. 350 m thick) includes from base to top the Eusebio Ayala, Vargas Peña and Cariy siliciclastic formations. It was traditionally assigned to the Llandovery (e.g. Harrington, 1950; Dyck, 1991; Benedetto et al., 1992; Benedetto, 2002; Galeano Inchausti and Poiré, 2006; Uriz et al., 2008a, 2008b and references therein) based on a marine fossil record mainly of graptolites, shelly fauna, and palynofacies assemblages. The new records of graptolites and some trilobites from the Eusebio Ayala Formation, exposed in clay quarries to the east of Asunción allow the comparison with other sequences bearing similar faunal associations known in west Gondwana. These records are discussed here, taken into account that the mentioned interval was a relevant paleobiogeographical time slice during the Lower Paleozoic (Cocks, 2001).
Facultad de Ciencias Naturales y Museo - Materia
-
Ciencias Naturales
SW Gondwana
Paraná Basin
Eastern Paraguay
Normalograptus persculptus Biozone
Hirnantian-Llandovery transition - Nivel de accesibilidad
- acceso abierto
- Condiciones de uso
- http://creativecommons.org/licenses/by-nc-sa/4.0/
- Repositorio
- Institución
- Universidad Nacional de La Plata
- OAI Identificador
- oai:sedici.unlp.edu.ar:10915/153693
Ver los metadatos del registro completo
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The Hirnantian-Early Llandovery transition sequence in the Paraná basin, Eastern ParaguayCingolani, Carlos AlbertoUriz, Norberto JavierAlfaro, Marta BeatrízTortello, Marcelo FrancoBidone, Andrea RosaGaleano Inchausti, Julio CésarCiencias NaturalesSW GondwanaParaná BasinEastern ParaguayNormalograptus persculptus BiozoneHirnantian-Llandovery transitionThe Lower Paleozoic Itacurubí Group (Harrington, 1972) is exposed in the western border of the intracratonic Paraná Basin of eastern Paraguay (Fig. 1). This group (c. 350 m thick) includes from base to top the Eusebio Ayala, Vargas Peña and Cariy siliciclastic formations. It was traditionally assigned to the Llandovery (e.g. Harrington, 1950; Dyck, 1991; Benedetto et al., 1992; Benedetto, 2002; Galeano Inchausti and Poiré, 2006; Uriz et al., 2008a, 2008b and references therein) based on a marine fossil record mainly of graptolites, shelly fauna, and palynofacies assemblages. The new records of graptolites and some trilobites from the Eusebio Ayala Formation, exposed in clay quarries to the east of Asunción allow the comparison with other sequences bearing similar faunal associations known in west Gondwana. These records are discussed here, taken into account that the mentioned interval was a relevant paleobiogeographical time slice during the Lower Paleozoic (Cocks, 2001).Facultad de Ciencias Naturales y Museo2011info:eu-repo/semantics/conferenceObjectinfo:eu-repo/semantics/publishedVersionObjeto de conferenciahttp://purl.org/coar/resource_type/c_5794info:ar-repo/semantics/documentoDeConferenciaapplication/pdf103-108http://sedici.unlp.edu.ar/handle/10915/153693enginfo:eu-repo/semantics/altIdentifier/isbn/978-84-7840-857-3info:eu-repo/semantics/openAccesshttp://creativecommons.org/licenses/by-nc-sa/4.0/Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0)reponame:SEDICI (UNLP)instname:Universidad Nacional de La Platainstacron:UNLP2025-09-03T11:11:48Zoai:sedici.unlp.edu.ar:10915/153693Institucionalhttp://sedici.unlp.edu.ar/Universidad públicaNo correspondehttp://sedici.unlp.edu.ar/oai/snrdalira@sedici.unlp.edu.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:13292025-09-03 11:11:49.129SEDICI (UNLP) - Universidad Nacional de La Platafalse |
dc.title.none.fl_str_mv |
The Hirnantian-Early Llandovery transition sequence in the Paraná basin, Eastern Paraguay |
title |
The Hirnantian-Early Llandovery transition sequence in the Paraná basin, Eastern Paraguay |
spellingShingle |
The Hirnantian-Early Llandovery transition sequence in the Paraná basin, Eastern Paraguay Cingolani, Carlos Alberto Ciencias Naturales SW Gondwana Paraná Basin Eastern Paraguay Normalograptus persculptus Biozone Hirnantian-Llandovery transition |
title_short |
The Hirnantian-Early Llandovery transition sequence in the Paraná basin, Eastern Paraguay |
title_full |
The Hirnantian-Early Llandovery transition sequence in the Paraná basin, Eastern Paraguay |
title_fullStr |
The Hirnantian-Early Llandovery transition sequence in the Paraná basin, Eastern Paraguay |
title_full_unstemmed |
The Hirnantian-Early Llandovery transition sequence in the Paraná basin, Eastern Paraguay |
title_sort |
The Hirnantian-Early Llandovery transition sequence in the Paraná basin, Eastern Paraguay |
dc.creator.none.fl_str_mv |
Cingolani, Carlos Alberto Uriz, Norberto Javier Alfaro, Marta Beatríz Tortello, Marcelo Franco Bidone, Andrea Rosa Galeano Inchausti, Julio César |
author |
Cingolani, Carlos Alberto |
author_facet |
Cingolani, Carlos Alberto Uriz, Norberto Javier Alfaro, Marta Beatríz Tortello, Marcelo Franco Bidone, Andrea Rosa Galeano Inchausti, Julio César |
author_role |
author |
author2 |
Uriz, Norberto Javier Alfaro, Marta Beatríz Tortello, Marcelo Franco Bidone, Andrea Rosa Galeano Inchausti, Julio César |
author2_role |
author author author author author |
dc.subject.none.fl_str_mv |
Ciencias Naturales SW Gondwana Paraná Basin Eastern Paraguay Normalograptus persculptus Biozone Hirnantian-Llandovery transition |
topic |
Ciencias Naturales SW Gondwana Paraná Basin Eastern Paraguay Normalograptus persculptus Biozone Hirnantian-Llandovery transition |
dc.description.none.fl_txt_mv |
The Lower Paleozoic Itacurubí Group (Harrington, 1972) is exposed in the western border of the intracratonic Paraná Basin of eastern Paraguay (Fig. 1). This group (c. 350 m thick) includes from base to top the Eusebio Ayala, Vargas Peña and Cariy siliciclastic formations. It was traditionally assigned to the Llandovery (e.g. Harrington, 1950; Dyck, 1991; Benedetto et al., 1992; Benedetto, 2002; Galeano Inchausti and Poiré, 2006; Uriz et al., 2008a, 2008b and references therein) based on a marine fossil record mainly of graptolites, shelly fauna, and palynofacies assemblages. The new records of graptolites and some trilobites from the Eusebio Ayala Formation, exposed in clay quarries to the east of Asunción allow the comparison with other sequences bearing similar faunal associations known in west Gondwana. These records are discussed here, taken into account that the mentioned interval was a relevant paleobiogeographical time slice during the Lower Paleozoic (Cocks, 2001). Facultad de Ciencias Naturales y Museo |
description |
The Lower Paleozoic Itacurubí Group (Harrington, 1972) is exposed in the western border of the intracratonic Paraná Basin of eastern Paraguay (Fig. 1). This group (c. 350 m thick) includes from base to top the Eusebio Ayala, Vargas Peña and Cariy siliciclastic formations. It was traditionally assigned to the Llandovery (e.g. Harrington, 1950; Dyck, 1991; Benedetto et al., 1992; Benedetto, 2002; Galeano Inchausti and Poiré, 2006; Uriz et al., 2008a, 2008b and references therein) based on a marine fossil record mainly of graptolites, shelly fauna, and palynofacies assemblages. The new records of graptolites and some trilobites from the Eusebio Ayala Formation, exposed in clay quarries to the east of Asunción allow the comparison with other sequences bearing similar faunal associations known in west Gondwana. These records are discussed here, taken into account that the mentioned interval was a relevant paleobiogeographical time slice during the Lower Paleozoic (Cocks, 2001). |
publishDate |
2011 |
dc.date.none.fl_str_mv |
2011 |
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eng |
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