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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| Formato: | Objeto de conferencia |
| Lenguaje: | Inglés |
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2011
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| Acceso en línea: | http://sedici.unlp.edu.ar/handle/10915/153693 |
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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 |
| work_keys_str_mv |
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1767633995002019840 |