New vertebrate remains from the Batoví Member (Late Jurassic-?Early Cretaceous) of the Tacuarembó Formation (Uruguay) and the southernmost occurrence of mawsoniid coelacanths
- Autores
- Soto, M.; Carvalho, M. S. S. de; Maisey, J. G.; Mesa, V.
- Año de publicación
- 2010
- Idioma
- inglés
- Tipo de recurso
- documento de conferencia
- Estado
- versión publicada
- Descripción
- The Batoví Member of the Tacuarembó Formation comprises fossiliferous sandstones and pelites of mainly fluviolacustrine origin, which have yielded a fossil assemblage of Late Jurassic-?Early Cretaceous age. Vertebrates known from the Los Rosanos locality include ?semionotiform bones and scales, dipnoan tooth-plates (Ceratodus africanus Haug), a rostrum of a pholidosaurid mesoeucrocodylian (Meridiosaurus vallisparadisi Mones), and teeth of indeterminate crocodyliforms and theropod dinosaurs. Herein we describe several coelacanth bones (including an operculum, a postparietal, a dentary, and a pterygoid), the ornamentation, morphology and size of which allow us to refer them to the Mawsoniidae, and probably to Mawsonia, being the southernmost record of the genus. Mawsonia, the largest coelacanth, was restricted to non-marine environments of the Tithonian-Cenomanian of Brazil and Africa. The genus has been recently reviewed, only two species being currently recognized. Other mawsoniids from Western Gondwana include Axelrodichthys, Lualabaea and the recently described Parnaibaia. The Uruguayan record is one of the oldest occurrences of the family. Coelacanths are regarded as possible prey of the hybodontid Priohybodus. Other new remains from Los Rosanos include a large theropod tooth (crown height = 56mm) and a crocodyliform skull roof fragment. The tooth, albeit fragmentary, can be referred either to the Ceratosauridae or the Carcharodontosauridae (both taxa being already recorded in the Batoví Member). The skull fragment shows sutured frontals, which indicates it belongs to the Mesoeucrocodylia. All these remains provide valuable information about the fossil assemblages of the Tacuarembó Formation, including the largest fishes and theropods ever recorded in this unit.
Sesiones libres
Facultad de Ciencias Naturales y Museo - Materia
-
Ciencias Naturales
Paleontología - 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:10915/16970
Ver los metadatos del registro completo
id |
SEDICI_44b7ea8f9ee8bedc850e1e81ade29b71 |
---|---|
oai_identifier_str |
oai:sedici.unlp.edu.ar:10915/16970 |
network_acronym_str |
SEDICI |
repository_id_str |
1329 |
network_name_str |
SEDICI (UNLP) |
spelling |
New vertebrate remains from the Batoví Member (Late Jurassic-?Early Cretaceous) of the Tacuarembó Formation (Uruguay) and the southernmost occurrence of mawsoniid coelacanthsSoto, M.Carvalho, M. S. S. deMaisey, J. G.Mesa, V.Ciencias NaturalesPaleontologíaThe Batoví Member of the Tacuarembó Formation comprises fossiliferous sandstones and pelites of mainly fluviolacustrine origin, which have yielded a fossil assemblage of Late Jurassic-?Early Cretaceous age. Vertebrates known from the Los Rosanos locality include ?semionotiform bones and scales, dipnoan tooth-plates (Ceratodus africanus Haug), a rostrum of a pholidosaurid mesoeucrocodylian (Meridiosaurus vallisparadisi Mones), and teeth of indeterminate crocodyliforms and theropod dinosaurs. Herein we describe several coelacanth bones (including an operculum, a postparietal, a dentary, and a pterygoid), the ornamentation, morphology and size of which allow us to refer them to the Mawsoniidae, and probably to Mawsonia, being the southernmost record of the genus. Mawsonia, the largest coelacanth, was restricted to non-marine environments of the Tithonian-Cenomanian of Brazil and Africa. The genus has been recently reviewed, only two species being currently recognized. Other mawsoniids from Western Gondwana include Axelrodichthys, Lualabaea and the recently described Parnaibaia. The Uruguayan record is one of the oldest occurrences of the family. Coelacanths are regarded as possible prey of the hybodontid Priohybodus. Other new remains from Los Rosanos include a large theropod tooth (crown height = 56mm) and a crocodyliform skull roof fragment. The tooth, albeit fragmentary, can be referred either to the Ceratosauridae or the Carcharodontosauridae (both taxa being already recorded in the Batoví Member). The skull fragment shows sutured frontals, which indicates it belongs to the Mesoeucrocodylia. All these remains provide valuable information about the fossil assemblages of the Tacuarembó Formation, including the largest fishes and theropods ever recorded in this unit.Sesiones libresFacultad de Ciencias Naturales y Museo2010info:eu-repo/semantics/conferenceObjectinfo:eu-repo/semantics/publishedVersionResumenhttp://purl.org/coar/resource_type/c_5794info:ar-repo/semantics/documentoDeConferenciaapplication/pdfhttp://sedici.unlp.edu.ar/handle/10915/16970enginfo:eu-repo/semantics/altIdentifier/isbn/978-987-95849-7-2info:eu-repo/semantics/reference/url/https://sedici.unlp.edu.ar/handle/10915/25738info: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:UNLP2025-09-29T10:53:03Zoai:sedici.unlp.edu.ar:10915/16970Institucionalhttp://sedici.unlp.edu.ar/Universidad públicaNo correspondehttp://sedici.unlp.edu.ar/oai/snrdalira@sedici.unlp.edu.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:13292025-09-29 10:53:04.194SEDICI (UNLP) - Universidad Nacional de La Platafalse |
dc.title.none.fl_str_mv |
New vertebrate remains from the Batoví Member (Late Jurassic-?Early Cretaceous) of the Tacuarembó Formation (Uruguay) and the southernmost occurrence of mawsoniid coelacanths |
title |
New vertebrate remains from the Batoví Member (Late Jurassic-?Early Cretaceous) of the Tacuarembó Formation (Uruguay) and the southernmost occurrence of mawsoniid coelacanths |
spellingShingle |
New vertebrate remains from the Batoví Member (Late Jurassic-?Early Cretaceous) of the Tacuarembó Formation (Uruguay) and the southernmost occurrence of mawsoniid coelacanths Soto, M. Ciencias Naturales Paleontología |
title_short |
New vertebrate remains from the Batoví Member (Late Jurassic-?Early Cretaceous) of the Tacuarembó Formation (Uruguay) and the southernmost occurrence of mawsoniid coelacanths |
title_full |
New vertebrate remains from the Batoví Member (Late Jurassic-?Early Cretaceous) of the Tacuarembó Formation (Uruguay) and the southernmost occurrence of mawsoniid coelacanths |
title_fullStr |
New vertebrate remains from the Batoví Member (Late Jurassic-?Early Cretaceous) of the Tacuarembó Formation (Uruguay) and the southernmost occurrence of mawsoniid coelacanths |
title_full_unstemmed |
New vertebrate remains from the Batoví Member (Late Jurassic-?Early Cretaceous) of the Tacuarembó Formation (Uruguay) and the southernmost occurrence of mawsoniid coelacanths |
title_sort |
New vertebrate remains from the Batoví Member (Late Jurassic-?Early Cretaceous) of the Tacuarembó Formation (Uruguay) and the southernmost occurrence of mawsoniid coelacanths |
dc.creator.none.fl_str_mv |
Soto, M. Carvalho, M. S. S. de Maisey, J. G. Mesa, V. |
author |
Soto, M. |
author_facet |
Soto, M. Carvalho, M. S. S. de Maisey, J. G. Mesa, V. |
author_role |
author |
author2 |
Carvalho, M. S. S. de Maisey, J. G. Mesa, V. |
author2_role |
author author author |
dc.subject.none.fl_str_mv |
Ciencias Naturales Paleontología |
topic |
Ciencias Naturales Paleontología |
dc.description.none.fl_txt_mv |
The Batoví Member of the Tacuarembó Formation comprises fossiliferous sandstones and pelites of mainly fluviolacustrine origin, which have yielded a fossil assemblage of Late Jurassic-?Early Cretaceous age. Vertebrates known from the Los Rosanos locality include ?semionotiform bones and scales, dipnoan tooth-plates (Ceratodus africanus Haug), a rostrum of a pholidosaurid mesoeucrocodylian (Meridiosaurus vallisparadisi Mones), and teeth of indeterminate crocodyliforms and theropod dinosaurs. Herein we describe several coelacanth bones (including an operculum, a postparietal, a dentary, and a pterygoid), the ornamentation, morphology and size of which allow us to refer them to the Mawsoniidae, and probably to Mawsonia, being the southernmost record of the genus. Mawsonia, the largest coelacanth, was restricted to non-marine environments of the Tithonian-Cenomanian of Brazil and Africa. The genus has been recently reviewed, only two species being currently recognized. Other mawsoniids from Western Gondwana include Axelrodichthys, Lualabaea and the recently described Parnaibaia. The Uruguayan record is one of the oldest occurrences of the family. Coelacanths are regarded as possible prey of the hybodontid Priohybodus. Other new remains from Los Rosanos include a large theropod tooth (crown height = 56mm) and a crocodyliform skull roof fragment. The tooth, albeit fragmentary, can be referred either to the Ceratosauridae or the Carcharodontosauridae (both taxa being already recorded in the Batoví Member). The skull fragment shows sutured frontals, which indicates it belongs to the Mesoeucrocodylia. All these remains provide valuable information about the fossil assemblages of the Tacuarembó Formation, including the largest fishes and theropods ever recorded in this unit. Sesiones libres Facultad de Ciencias Naturales y Museo |
description |
The Batoví Member of the Tacuarembó Formation comprises fossiliferous sandstones and pelites of mainly fluviolacustrine origin, which have yielded a fossil assemblage of Late Jurassic-?Early Cretaceous age. Vertebrates known from the Los Rosanos locality include ?semionotiform bones and scales, dipnoan tooth-plates (Ceratodus africanus Haug), a rostrum of a pholidosaurid mesoeucrocodylian (Meridiosaurus vallisparadisi Mones), and teeth of indeterminate crocodyliforms and theropod dinosaurs. Herein we describe several coelacanth bones (including an operculum, a postparietal, a dentary, and a pterygoid), the ornamentation, morphology and size of which allow us to refer them to the Mawsoniidae, and probably to Mawsonia, being the southernmost record of the genus. Mawsonia, the largest coelacanth, was restricted to non-marine environments of the Tithonian-Cenomanian of Brazil and Africa. The genus has been recently reviewed, only two species being currently recognized. Other mawsoniids from Western Gondwana include Axelrodichthys, Lualabaea and the recently described Parnaibaia. The Uruguayan record is one of the oldest occurrences of the family. Coelacanths are regarded as possible prey of the hybodontid Priohybodus. Other new remains from Los Rosanos include a large theropod tooth (crown height = 56mm) and a crocodyliform skull roof fragment. The tooth, albeit fragmentary, can be referred either to the Ceratosauridae or the Carcharodontosauridae (both taxa being already recorded in the Batoví Member). The skull fragment shows sutured frontals, which indicates it belongs to the Mesoeucrocodylia. All these remains provide valuable information about the fossil assemblages of the Tacuarembó Formation, including the largest fishes and theropods ever recorded in this unit. |
publishDate |
2010 |
dc.date.none.fl_str_mv |
2010 |
dc.type.none.fl_str_mv |
info:eu-repo/semantics/conferenceObject info:eu-repo/semantics/publishedVersion Resumen http://purl.org/coar/resource_type/c_5794 info:ar-repo/semantics/documentoDeConferencia |
format |
conferenceObject |
status_str |
publishedVersion |
dc.identifier.none.fl_str_mv |
http://sedici.unlp.edu.ar/handle/10915/16970 |
url |
http://sedici.unlp.edu.ar/handle/10915/16970 |
dc.language.none.fl_str_mv |
eng |
language |
eng |
dc.relation.none.fl_str_mv |
info:eu-repo/semantics/altIdentifier/isbn/978-987-95849-7-2 info:eu-repo/semantics/reference/url/https://sedici.unlp.edu.ar/handle/10915/25738 |
dc.rights.none.fl_str_mv |
info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by-nc-sa/4.0/ Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0) |
eu_rights_str_mv |
openAccess |
rights_invalid_str_mv |
http://creativecommons.org/licenses/by-nc-sa/4.0/ Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0) |
dc.format.none.fl_str_mv |
application/pdf |
dc.source.none.fl_str_mv |
reponame:SEDICI (UNLP) instname:Universidad Nacional de La Plata instacron:UNLP |
reponame_str |
SEDICI (UNLP) |
collection |
SEDICI (UNLP) |
instname_str |
Universidad Nacional de La Plata |
instacron_str |
UNLP |
institution |
UNLP |
repository.name.fl_str_mv |
SEDICI (UNLP) - Universidad Nacional de La Plata |
repository.mail.fl_str_mv |
alira@sedici.unlp.edu.ar |
_version_ |
1844615786055860224 |
score |
13.070432 |