Sauropod diversity (Dinosauria: Sauropoda) of Cerro Overo – La Invernada (Bajo de la Carpa Formation, Santonian), northeastern Neuquén Basin, and paleoecological implications for Upper Cretaceous sauropod faunas

The Upper Cretaceous fossil vertebrate fauna of the Bajo de la Carpa Formation (Santonian), derived from several different locations in the Neuquén Basin, is relatively abundant and diverse, comprising mainly small to medium-sized reptiles, birds and fishes. The Cerro Overo – La Invernada locality (...

Descripción completa

Guardado en:
Detalles Bibliográficos
Autores principales: Filippi, Leonardo Sebastián, Bellardini, Flavio, Carballido, José Luis, Pérez Moreno, Agustín, Garrido, Alberto Carlos
Formato: Articulo
Lenguaje:Inglés
Publicado: 2024
Materias:
Acceso en línea:http://sedici.unlp.edu.ar/handle/10915/167629
Aporte de:
id I19-R120-10915-167629
record_format dspace
spelling I19-R120-10915-1676292024-07-01T20:11:02Z http://sedici.unlp.edu.ar/handle/10915/167629 Sauropod diversity (Dinosauria: Sauropoda) of Cerro Overo – La Invernada (Bajo de la Carpa Formation, Santonian), northeastern Neuquén Basin, and paleoecological implications for Upper Cretaceous sauropod faunas Diversidad de saurópodos (Dinosauria: Sauropoda) de Cerro Overo – La Invernada (Formación Bajo de la Carpa, Santoniano), noroeste de la Cuenca Neuquina e implicaciones paleobiológicas de la fauna de saurópodos del cretácico superior Filippi, Leonardo Sebastián Bellardini, Flavio Carballido, José Luis Pérez Moreno, Agustín Garrido, Alberto Carlos 2024 2024-07-01T14:48:02Z en Paleontología Sauropoda Titanosauria Diversity Upper Cretaceous Neuquén Basin Diversidad Cretácico Superior Cuenca Neuquina The Upper Cretaceous fossil vertebrate fauna of the Bajo de la Carpa Formation (Santonian), derived from several different locations in the Neuquén Basin, is relatively abundant and diverse, comprising mainly small to medium-sized reptiles, birds and fishes. The Cerro Overo – La Invernada locality (CO – LI), in the north of the basin, records a similar faunal component for that age, but stands out for its relatively greater abundance and diversity of titanosaur sauropods. The study of the materials presented here allows us to establish the presence of specimens of sauropods other than Overosaurus, the only titanosaur recorded so far in the area, the coexistence of small–medium sized forms with larger forms, which in turn represent some forms with more basal characteristics and others with more derived features. The abundance of the record of sauropods in CO – LI shows both morphological and evolutionary variations, so the discovery of more complete specimens will allow paleofaunistic, paleobiological, and paleoecological studies to be carried out. This will provide a better understanding of the role of titanosaurian sauropods in Late Cretaceous ecosystems. La fauna de vertebrados fósiles del Cretácico Superior proveniente de la Formación Bajo de la Carpa (Santoniano) de diferentes localidades de la Cuenca Neuquina, es relativamente abundante y diversa; está compuesta principalmente por formas de reptiles, aves y peces de pequeño y mediano tamaño. La localidad de Cerro Overo – La Invernada (CO – LI), en el norte de la cuenca, registra para dicha edad, un componente faunístico similar, pero destacándose por una abundancia y diversidad relativamente mayor de saurópodos titanosaurios. El estudio de los materiales presentados aquí permite establecer la presencia de especímenes de saurópodos diferentes a Overosaurus, el único titanosaurio registrado hasta el momento en el área, y la coexistencia de formas de pequeño-mediano tamaño con formas más grandes, que representan a su vez algunas formas con características más basales y otras con rasgos más derivados. La abundancia del registro de saurópodos en CO – LI muestra variaciones tanto morfológicas como evolutivas, por lo que el hallazgo de ejemplares más completos permitirá llevar adelante estudios paleofaunísticos, paleobiológicos y paleoecológicos. Esto brindará una mejor comprensión del papel de los saurópodos titanosaurios en los ecosistemas del Cretácico Superior. Facultad de Ciencias Naturales y Museo Articulo Articulo http://creativecommons.org/licenses/by-nc/4.0/ Creative Commons Attribution-NonCommercial 4.0 International (CC BY-NC 4.0) application/pdf 71-96
institution Universidad Nacional de La Plata
institution_str I-19
repository_str R-120
collection SEDICI (UNLP)
language Inglés
topic Paleontología
Sauropoda
Titanosauria
Diversity
Upper Cretaceous
Neuquén Basin
Diversidad
Cretácico Superior
Cuenca Neuquina
spellingShingle Paleontología
Sauropoda
Titanosauria
Diversity
Upper Cretaceous
Neuquén Basin
Diversidad
Cretácico Superior
Cuenca Neuquina
Filippi, Leonardo Sebastián
Bellardini, Flavio
Carballido, José Luis
Pérez Moreno, Agustín
Garrido, Alberto Carlos
Sauropod diversity (Dinosauria: Sauropoda) of Cerro Overo – La Invernada (Bajo de la Carpa Formation, Santonian), northeastern Neuquén Basin, and paleoecological implications for Upper Cretaceous sauropod faunas
topic_facet Paleontología
Sauropoda
Titanosauria
Diversity
Upper Cretaceous
Neuquén Basin
Diversidad
Cretácico Superior
Cuenca Neuquina
description The Upper Cretaceous fossil vertebrate fauna of the Bajo de la Carpa Formation (Santonian), derived from several different locations in the Neuquén Basin, is relatively abundant and diverse, comprising mainly small to medium-sized reptiles, birds and fishes. The Cerro Overo – La Invernada locality (CO – LI), in the north of the basin, records a similar faunal component for that age, but stands out for its relatively greater abundance and diversity of titanosaur sauropods. The study of the materials presented here allows us to establish the presence of specimens of sauropods other than Overosaurus, the only titanosaur recorded so far in the area, the coexistence of small–medium sized forms with larger forms, which in turn represent some forms with more basal characteristics and others with more derived features. The abundance of the record of sauropods in CO – LI shows both morphological and evolutionary variations, so the discovery of more complete specimens will allow paleofaunistic, paleobiological, and paleoecological studies to be carried out. This will provide a better understanding of the role of titanosaurian sauropods in Late Cretaceous ecosystems.
format Articulo
Articulo
author Filippi, Leonardo Sebastián
Bellardini, Flavio
Carballido, José Luis
Pérez Moreno, Agustín
Garrido, Alberto Carlos
author_facet Filippi, Leonardo Sebastián
Bellardini, Flavio
Carballido, José Luis
Pérez Moreno, Agustín
Garrido, Alberto Carlos
author_sort Filippi, Leonardo Sebastián
title Sauropod diversity (Dinosauria: Sauropoda) of Cerro Overo – La Invernada (Bajo de la Carpa Formation, Santonian), northeastern Neuquén Basin, and paleoecological implications for Upper Cretaceous sauropod faunas
title_short Sauropod diversity (Dinosauria: Sauropoda) of Cerro Overo – La Invernada (Bajo de la Carpa Formation, Santonian), northeastern Neuquén Basin, and paleoecological implications for Upper Cretaceous sauropod faunas
title_full Sauropod diversity (Dinosauria: Sauropoda) of Cerro Overo – La Invernada (Bajo de la Carpa Formation, Santonian), northeastern Neuquén Basin, and paleoecological implications for Upper Cretaceous sauropod faunas
title_fullStr Sauropod diversity (Dinosauria: Sauropoda) of Cerro Overo – La Invernada (Bajo de la Carpa Formation, Santonian), northeastern Neuquén Basin, and paleoecological implications for Upper Cretaceous sauropod faunas
title_full_unstemmed Sauropod diversity (Dinosauria: Sauropoda) of Cerro Overo – La Invernada (Bajo de la Carpa Formation, Santonian), northeastern Neuquén Basin, and paleoecological implications for Upper Cretaceous sauropod faunas
title_sort sauropod diversity (dinosauria: sauropoda) of cerro overo – la invernada (bajo de la carpa formation, santonian), northeastern neuquén basin, and paleoecological implications for upper cretaceous sauropod faunas
publishDate 2024
url http://sedici.unlp.edu.ar/handle/10915/167629
work_keys_str_mv AT filippileonardosebastian sauropoddiversitydinosauriasauropodaofcerrooverolainvernadabajodelacarpaformationsantoniannortheasternneuquenbasinandpaleoecologicalimplicationsforuppercretaceoussauropodfaunas
AT bellardiniflavio sauropoddiversitydinosauriasauropodaofcerrooverolainvernadabajodelacarpaformationsantoniannortheasternneuquenbasinandpaleoecologicalimplicationsforuppercretaceoussauropodfaunas
AT carballidojoseluis sauropoddiversitydinosauriasauropodaofcerrooverolainvernadabajodelacarpaformationsantoniannortheasternneuquenbasinandpaleoecologicalimplicationsforuppercretaceoussauropodfaunas
AT perezmorenoagustin sauropoddiversitydinosauriasauropodaofcerrooverolainvernadabajodelacarpaformationsantoniannortheasternneuquenbasinandpaleoecologicalimplicationsforuppercretaceoussauropodfaunas
AT garridoalbertocarlos sauropoddiversitydinosauriasauropodaofcerrooverolainvernadabajodelacarpaformationsantoniannortheasternneuquenbasinandpaleoecologicalimplicationsforuppercretaceoussauropodfaunas
AT filippileonardosebastian diversidaddesauropodosdinosauriasauropodadecerrooverolainvernadaformacionbajodelacarpasantonianonoroestedelacuencaneuquinaeimplicacionespaleobiologicasdelafaunadesauropodosdelcretacicosuperior
AT bellardiniflavio diversidaddesauropodosdinosauriasauropodadecerrooverolainvernadaformacionbajodelacarpasantonianonoroestedelacuencaneuquinaeimplicacionespaleobiologicasdelafaunadesauropodosdelcretacicosuperior
AT carballidojoseluis diversidaddesauropodosdinosauriasauropodadecerrooverolainvernadaformacionbajodelacarpasantonianonoroestedelacuencaneuquinaeimplicacionespaleobiologicasdelafaunadesauropodosdelcretacicosuperior
AT perezmorenoagustin diversidaddesauropodosdinosauriasauropodadecerrooverolainvernadaformacionbajodelacarpasantonianonoroestedelacuencaneuquinaeimplicacionespaleobiologicasdelafaunadesauropodosdelcretacicosuperior
AT garridoalbertocarlos diversidaddesauropodosdinosauriasauropodadecerrooverolainvernadaformacionbajodelacarpasantonianonoroestedelacuencaneuquinaeimplicacionespaleobiologicasdelafaunadesauropodosdelcretacicosuperior
_version_ 1807223537203675136