Crocodylomorph ungual phalanxes from Bauru Basin (Late Cretaceous, Brazil)

Detalhes bibliográficos
Autor(a) principal: Vasconcellos, Felipe Mesquita de
Data de Publicação: 2004
Outros Autores: Arruda, João Tadeu, Rocha-Barbosa, Oscar, Carvalho, Ismar de Souza
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.
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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
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identifier_str_mv 10.11137/2004_0_53-63
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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
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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)
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