The Hirnantian-Early Llandovery transition sequence in the Paraná basin, Eastern Paraguay

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 assign...

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Autores principales: Cingolani, Carlos Alberto, Uriz, Norberto Javier, Alfaro, Marta Beatríz, Tortello, Marcelo Franco, Bidone, Andrea Rosa, Galeano Inchausti, Julio César
Formato: Objeto de conferencia
Lenguaje:Inglés
Publicado: 2011
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Acceso en línea:http://sedici.unlp.edu.ar/handle/10915/153693
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spelling I19-R120-10915-1536932023-05-31T04:07:17Z http://sedici.unlp.edu.ar/handle/10915/153693 isbn:978-84-7840-857-3 The Hirnantian-Early Llandovery transition sequence in the Paraná basin, Eastern Paraguay Cingolani, Carlos Alberto Uriz, Norberto Javier Alfaro, Marta Beatríz Tortello, Marcelo Franco Bidone, Andrea Rosa Galeano Inchausti, Julio César 2011 2011 2023-05-30T18:39:28Z en Ciencias Naturales SW Gondwana Paraná Basin Eastern Paraguay Normalograptus persculptus Biozone Hirnantian-Llandovery transition 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 Objeto de conferencia Objeto de conferencia http://creativecommons.org/licenses/by-nc-sa/4.0/ Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0) application/pdf 103-108
institution Universidad Nacional de La Plata
institution_str I-19
repository_str R-120
collection SEDICI (UNLP)
language Inglés
topic Ciencias Naturales
SW Gondwana
Paraná Basin
Eastern Paraguay
Normalograptus persculptus Biozone
Hirnantian-Llandovery transition
spellingShingle Ciencias Naturales
SW Gondwana
Paraná Basin
Eastern Paraguay
Normalograptus persculptus Biozone
Hirnantian-Llandovery transition
Cingolani, Carlos Alberto
Uriz, Norberto Javier
Alfaro, Marta Beatríz
Tortello, Marcelo Franco
Bidone, Andrea Rosa
Galeano Inchausti, Julio César
The Hirnantian-Early Llandovery transition sequence in the Paraná basin, Eastern Paraguay
topic_facet Ciencias Naturales
SW Gondwana
Paraná Basin
Eastern Paraguay
Normalograptus persculptus Biozone
Hirnantian-Llandovery transition
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).
format Objeto de conferencia
Objeto de conferencia
author Cingolani, Carlos Alberto
Uriz, Norberto Javier
Alfaro, Marta Beatríz
Tortello, Marcelo Franco
Bidone, Andrea Rosa
Galeano Inchausti, Julio César
author_facet Cingolani, Carlos Alberto
Uriz, Norberto Javier
Alfaro, Marta Beatríz
Tortello, Marcelo Franco
Bidone, Andrea Rosa
Galeano Inchausti, Julio César
author_sort Cingolani, Carlos Alberto
title The Hirnantian-Early Llandovery transition sequence in the Paraná basin, Eastern Paraguay
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 hirnantian-early llandovery transition sequence in the paraná basin, eastern paraguay
publishDate 2011
url http://sedici.unlp.edu.ar/handle/10915/153693
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