A new short-snouted Rhinesuchid from the permian of southern Brazil

Detalhes bibliográficos
Autor(a) principal: Dias, Eliseu Vieira
Data de Publicação: 2020
Outros Autores: Silva, Sergio Dias da, Schultz, Cesar Leandro
Tipo de documento: Artigo
Idioma: eng
Título da fonte: Repositório Institucional da UFRGS
Texto Completo: http://hdl.handle.net/10183/229929
Resumo: A new basal stereospondyl taxon from the Permian is described. The material used to erect the new taxon consists of a series of mandibles and some postcranial elements. A single badly preserved short-snouted skull is considered as referred material. Rastosuchus hammeri gen. et sp. nov. presents conical teeth along all coronoid bones, the prearticular extending anteriorly at the level of the precoronoid and enlarged anterior meckelian foramina. Based on the referred material, R. hammeri gen. et sp. nov. also presents posterior premaxillary teeth larger than anterior ones, the cultriform process of the parasphenoid compressed laterally forming a medial ventral keel, posterolateral ramus of the vomer extends posterior to the palatine tusks, and rounded orbit with flat orbital bones at the same level of the skull roof, features shared with Australerpeton cosgriffi and other rhinesuchids. Australerpeton cosgriffi and Rastosuchus hammeri gen. et sp. nov. are from the upper layers of the Rio do Rasto Formation (Paraná Basin) in the Paraná State, southern Brazil, and its deposition in freshwater continental environments is reinforced by the presence of temnospodyls amphibians.
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spelling Dias, Eliseu VieiraSilva, Sergio Dias daSchultz, Cesar Leandro2021-09-17T04:27:53Z20201519-7530http://hdl.handle.net/10183/229929001131256A new basal stereospondyl taxon from the Permian is described. The material used to erect the new taxon consists of a series of mandibles and some postcranial elements. A single badly preserved short-snouted skull is considered as referred material. Rastosuchus hammeri gen. et sp. nov. presents conical teeth along all coronoid bones, the prearticular extending anteriorly at the level of the precoronoid and enlarged anterior meckelian foramina. Based on the referred material, R. hammeri gen. et sp. nov. also presents posterior premaxillary teeth larger than anterior ones, the cultriform process of the parasphenoid compressed laterally forming a medial ventral keel, posterolateral ramus of the vomer extends posterior to the palatine tusks, and rounded orbit with flat orbital bones at the same level of the skull roof, features shared with Australerpeton cosgriffi and other rhinesuchids. Australerpeton cosgriffi and Rastosuchus hammeri gen. et sp. nov. are from the upper layers of the Rio do Rasto Formation (Paraná Basin) in the Paraná State, southern Brazil, and its deposition in freshwater continental environments is reinforced by the presence of temnospodyls amphibians.application/pdfengRevista brasileira de paleontologia. Vol. 23, no. 2 (Apr./Jun. 2020), p. 98-122RhinesuchidaeTemnospondyliRastosuchusGuadalpianoLopingianoFormação Rio do RastoGuadalupian–LopingianRio do Rasto FormationA new short-snouted Rhinesuchid from the permian of southern Brazilinfo:eu-repo/semantics/articleinfo:eu-repo/semantics/otherinfo:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/openAccessreponame:Repositório Institucional da UFRGSinstname:Universidade Federal do Rio Grande do Sul (UFRGS)instacron:UFRGSTEXT001131256.pdf.txt001131256.pdf.txtExtracted Texttext/plain104954http://www.lume.ufrgs.br/bitstream/10183/229929/2/001131256.pdf.txt7a2bab3ea7f9f34dff6272fda538992aMD52ORIGINAL001131256.pdfTexto completo (inglês)application/pdf23181068http://www.lume.ufrgs.br/bitstream/10183/229929/1/001131256.pdf7c8d6221e41b2fba9ef4f129a4f49d45MD5110183/2299292021-10-02 04:45:03.567481oai:www.lume.ufrgs.br:10183/229929Repositório de PublicaçõesPUBhttps://lume.ufrgs.br/oai/requestopendoar:2021-10-02T07:45:03Repositório Institucional da UFRGS - Universidade Federal do Rio Grande do Sul (UFRGS)false
dc.title.pt_BR.fl_str_mv A new short-snouted Rhinesuchid from the permian of southern Brazil
title A new short-snouted Rhinesuchid from the permian of southern Brazil
spellingShingle A new short-snouted Rhinesuchid from the permian of southern Brazil
Dias, Eliseu Vieira
Rhinesuchidae
Temnospondyli
Rastosuchus
Guadalpiano
Lopingiano
Formação Rio do Rasto
Guadalupian–Lopingian
Rio do Rasto Formation
title_short A new short-snouted Rhinesuchid from the permian of southern Brazil
title_full A new short-snouted Rhinesuchid from the permian of southern Brazil
title_fullStr A new short-snouted Rhinesuchid from the permian of southern Brazil
title_full_unstemmed A new short-snouted Rhinesuchid from the permian of southern Brazil
title_sort A new short-snouted Rhinesuchid from the permian of southern Brazil
author Dias, Eliseu Vieira
author_facet Dias, Eliseu Vieira
Silva, Sergio Dias da
Schultz, Cesar Leandro
author_role author
author2 Silva, Sergio Dias da
Schultz, Cesar Leandro
author2_role author
author
dc.contributor.author.fl_str_mv Dias, Eliseu Vieira
Silva, Sergio Dias da
Schultz, Cesar Leandro
dc.subject.por.fl_str_mv Rhinesuchidae
Temnospondyli
Rastosuchus
Guadalpiano
Lopingiano
Formação Rio do Rasto
topic Rhinesuchidae
Temnospondyli
Rastosuchus
Guadalpiano
Lopingiano
Formação Rio do Rasto
Guadalupian–Lopingian
Rio do Rasto Formation
dc.subject.eng.fl_str_mv Guadalupian–Lopingian
Rio do Rasto Formation
description A new basal stereospondyl taxon from the Permian is described. The material used to erect the new taxon consists of a series of mandibles and some postcranial elements. A single badly preserved short-snouted skull is considered as referred material. Rastosuchus hammeri gen. et sp. nov. presents conical teeth along all coronoid bones, the prearticular extending anteriorly at the level of the precoronoid and enlarged anterior meckelian foramina. Based on the referred material, R. hammeri gen. et sp. nov. also presents posterior premaxillary teeth larger than anterior ones, the cultriform process of the parasphenoid compressed laterally forming a medial ventral keel, posterolateral ramus of the vomer extends posterior to the palatine tusks, and rounded orbit with flat orbital bones at the same level of the skull roof, features shared with Australerpeton cosgriffi and other rhinesuchids. Australerpeton cosgriffi and Rastosuchus hammeri gen. et sp. nov. are from the upper layers of the Rio do Rasto Formation (Paraná Basin) in the Paraná State, southern Brazil, and its deposition in freshwater continental environments is reinforced by the presence of temnospodyls amphibians.
publishDate 2020
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dc.relation.ispartof.pt_BR.fl_str_mv Revista brasileira de paleontologia. Vol. 23, no. 2 (Apr./Jun. 2020), p. 98-122
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