Crocodylomorph ungual phalanxes from Bauru Basin (Late Cretaceous, Brazil)
Autor(a) principal: | |
---|---|
Data de Publicação: | 2004 |
Outros Autores: | , , |
Tipo de documento: | Artigo |
Idioma: | por |
Título da fonte: | Anuário do Instituto de Geociências (Online) |
Texto Completo: | https://revistas.ufrj.br/index.php/aigeo/article/view/6263 |
Resumo: | The ungual phalanxes of recent crocodylomorphs are modified into queratin covered claws. They are conical, ventrally curved with a sharp distal end. They are used during locomotion, digging and female sizing on copula. Nevertheless, fossil crocodylomorphs claws present a wider morphological and functional diversity. It was analysed fossil claws from the Late Cretaceous rocks of Adamantina (General Salgado County) and Marília (Uberaba County) Formations of the Bauru Basin. The claws found in the Adamantina Formation were associated with skeletal remains of a baurusuchid. They are laterally compressed, more ventrally curved and stronger than those of recent crocodylomorphs. They also present, at their base, many furrows related to muscle attachment. The claws found in the Marília Formation were associated to the remains of a peirosaurid. They show a great lateral compression and a blade-like ventral edge. They also present a slight ventral curvature and strong furrows in their base for muscle attachment. The morphological data obtained from these claws allow the investigation of the autoecology of these Cretaceous crocodylomorphs. |
id |
UFRJ-21_463fb859fabb3c97af093c564b6433eb |
---|---|
oai_identifier_str |
oai:www.revistas.ufrj.br:article/6263 |
network_acronym_str |
UFRJ-21 |
network_name_str |
Anuário do Instituto de Geociências (Online) |
repository_id_str |
|
spelling |
Crocodylomorph ungual phalanxes from Bauru Basin (Late Cretaceous, Brazil)Falanges ungueais de crocodilomorfos da Bacia Bauru (Cretáceo Superior, Brasil)The ungual phalanxes of recent crocodylomorphs are modified into queratin covered claws. They are conical, ventrally curved with a sharp distal end. They are used during locomotion, digging and female sizing on copula. Nevertheless, fossil crocodylomorphs claws present a wider morphological and functional diversity. It was analysed fossil claws from the Late Cretaceous rocks of Adamantina (General Salgado County) and Marília (Uberaba County) Formations of the Bauru Basin. The claws found in the Adamantina Formation were associated with skeletal remains of a baurusuchid. They are laterally compressed, more ventrally curved and stronger than those of recent crocodylomorphs. They also present, at their base, many furrows related to muscle attachment. The claws found in the Marília Formation were associated to the remains of a peirosaurid. They show a great lateral compression and a blade-like ventral edge. They also present a slight ventral curvature and strong furrows in their base for muscle attachment. The morphological data obtained from these claws allow the investigation of the autoecology of these Cretaceous crocodylomorphs.As falanges ungueais dos crocodilomorfos atuais são modificadas em garras cônicas, curvas ventralmente, com extremidade distal pontiaguda, recoberta por camadas de queratina. São utilizadas comoauxílio para tração durante o deslocamento, escavação e apreensão da fêmea durante a cópula. Entretanto, os crocodilomorfos fósseis apresentam maior diversidade morfológica e possivelmente funcional destas garras. Foram analisadas garras fósseis oriundas de rochas do Cretáceo Superior da Bacia Bauru, nas formações Adamantina (Município de General Salgado) e Marília (Município de Uberaba). As garras encontradas na Formação Adamantina estavam associadas a restos esqueléticos de um baurussuquídeo. Apresentam achatamento lateral, curvatura ventral intensa e robustez maior que a observada entre crocodilomorfos recentes, e várias estrias relacionadas aos ligamentos musculares na base da garra. As garras encontradas na Formação Marília estão associadas aos ossos de um peirossaurídeo. São robustas e intensamente comprimidas lateralmente; sua face ventral é comprimida e possui aspecto laminado. Apresentam pequena curvatura ventral e fortes estrias de fixação muscular em sua base. As características morfológicas destas garras podem auxiliar na investigação dos hábitos de vida destes crocodilomorfos cretácicos.Universidade Federal do Rio de Janeiro2004-01-01info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionapplication/pdfhttps://revistas.ufrj.br/index.php/aigeo/article/view/626310.11137/2004_0_53-63Anuário do Instituto de Geociências; Vol 27 (2004); 53-63Anuário do Instituto de Geociências; Vol 27 (2004); 53-631982-39080101-9759reponame:Anuário do Instituto de Geociências (Online)instname:Universidade Federal do Rio de Janeiro (UFRJ)instacron:UFRJporhttps://revistas.ufrj.br/index.php/aigeo/article/view/6263/4860Copyright (c) 2004 Anuário do Instituto de Geociênciashttp://creativecommons.org/licenses/by/4.0info:eu-repo/semantics/openAccessVasconcellos, Felipe Mesquita deArruda, João TadeuRocha-Barbosa, OscarCarvalho, Ismar de Souza2022-10-13T17:13:58Zoai:www.revistas.ufrj.br:article/6263Revistahttps://revistas.ufrj.br/index.php/aigeo/indexPUBhttps://revistas.ufrj.br/index.php/aigeo/oaianuario@igeo.ufrj.br||1982-39080101-9759opendoar:2022-10-13T17:13:58Anuário do Instituto de Geociências (Online) - Universidade Federal do Rio de Janeiro (UFRJ)false |
dc.title.none.fl_str_mv |
Crocodylomorph ungual phalanxes from Bauru Basin (Late Cretaceous, Brazil) Falanges ungueais de crocodilomorfos da Bacia Bauru (Cretáceo Superior, Brasil) |
title |
Crocodylomorph ungual phalanxes from Bauru Basin (Late Cretaceous, Brazil) |
spellingShingle |
Crocodylomorph ungual phalanxes from Bauru Basin (Late Cretaceous, Brazil) Vasconcellos, Felipe Mesquita de |
title_short |
Crocodylomorph ungual phalanxes from Bauru Basin (Late Cretaceous, Brazil) |
title_full |
Crocodylomorph ungual phalanxes from Bauru Basin (Late Cretaceous, Brazil) |
title_fullStr |
Crocodylomorph ungual phalanxes from Bauru Basin (Late Cretaceous, Brazil) |
title_full_unstemmed |
Crocodylomorph ungual phalanxes from Bauru Basin (Late Cretaceous, Brazil) |
title_sort |
Crocodylomorph ungual phalanxes from Bauru Basin (Late Cretaceous, Brazil) |
author |
Vasconcellos, Felipe Mesquita de |
author_facet |
Vasconcellos, Felipe Mesquita de Arruda, João Tadeu Rocha-Barbosa, Oscar Carvalho, Ismar de Souza |
author_role |
author |
author2 |
Arruda, João Tadeu Rocha-Barbosa, Oscar Carvalho, Ismar de Souza |
author2_role |
author author author |
dc.contributor.author.fl_str_mv |
Vasconcellos, Felipe Mesquita de Arruda, João Tadeu Rocha-Barbosa, Oscar Carvalho, Ismar de Souza |
description |
The ungual phalanxes of recent crocodylomorphs are modified into queratin covered claws. They are conical, ventrally curved with a sharp distal end. They are used during locomotion, digging and female sizing on copula. Nevertheless, fossil crocodylomorphs claws present a wider morphological and functional diversity. It was analysed fossil claws from the Late Cretaceous rocks of Adamantina (General Salgado County) and Marília (Uberaba County) Formations of the Bauru Basin. The claws found in the Adamantina Formation were associated with skeletal remains of a baurusuchid. They are laterally compressed, more ventrally curved and stronger than those of recent crocodylomorphs. They also present, at their base, many furrows related to muscle attachment. The claws found in the Marília Formation were associated to the remains of a peirosaurid. They show a great lateral compression and a blade-like ventral edge. They also present a slight ventral curvature and strong furrows in their base for muscle attachment. The morphological data obtained from these claws allow the investigation of the autoecology of these Cretaceous crocodylomorphs. |
publishDate |
2004 |
dc.date.none.fl_str_mv |
2004-01-01 |
dc.type.none.fl_str_mv |
|
dc.type.driver.fl_str_mv |
info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion |
format |
article |
status_str |
publishedVersion |
dc.identifier.uri.fl_str_mv |
https://revistas.ufrj.br/index.php/aigeo/article/view/6263 10.11137/2004_0_53-63 |
url |
https://revistas.ufrj.br/index.php/aigeo/article/view/6263 |
identifier_str_mv |
10.11137/2004_0_53-63 |
dc.language.iso.fl_str_mv |
por |
language |
por |
dc.relation.none.fl_str_mv |
https://revistas.ufrj.br/index.php/aigeo/article/view/6263/4860 |
dc.rights.driver.fl_str_mv |
Copyright (c) 2004 Anuário do Instituto de Geociências http://creativecommons.org/licenses/by/4.0 info:eu-repo/semantics/openAccess |
rights_invalid_str_mv |
Copyright (c) 2004 Anuário do Instituto de Geociências http://creativecommons.org/licenses/by/4.0 |
eu_rights_str_mv |
openAccess |
dc.format.none.fl_str_mv |
application/pdf |
dc.publisher.none.fl_str_mv |
Universidade Federal do Rio de Janeiro |
publisher.none.fl_str_mv |
Universidade Federal do Rio de Janeiro |
dc.source.none.fl_str_mv |
Anuário do Instituto de Geociências; Vol 27 (2004); 53-63 Anuário do Instituto de Geociências; Vol 27 (2004); 53-63 1982-3908 0101-9759 reponame:Anuário do Instituto de Geociências (Online) instname:Universidade Federal do Rio de Janeiro (UFRJ) instacron:UFRJ |
instname_str |
Universidade Federal do Rio de Janeiro (UFRJ) |
instacron_str |
UFRJ |
institution |
UFRJ |
reponame_str |
Anuário do Instituto de Geociências (Online) |
collection |
Anuário do Instituto de Geociências (Online) |
repository.name.fl_str_mv |
Anuário do Instituto de Geociências (Online) - Universidade Federal do Rio de Janeiro (UFRJ) |
repository.mail.fl_str_mv |
anuario@igeo.ufrj.br|| |
_version_ |
1797053541166088192 |