New early permian tetrapod fauna from Namibia
- Autores
- Marsicano, Claudia Alicia; Smith, Roger; Mancuso, Adriana Cecilia; Mocke, Helke; Abdala, Fernando; Gaetano, Leandro Carlos
- Año de publicación
- 2018
- Idioma
- inglés
- Tipo de recurso
- documento de conferencia
- Estado
- versión publicada
- Descripción
- The earliest tetrapods in Western Gondwana are the mesosaurs, a group of specializedendemic aquatic parareptiles known only from Artinskian strata of Namibia, South Africa,Uruguay, and Brazil. Recent finds from early Permian beds in northern Brazil revealed a newfreshwater fauna from tropical Gondwana. However, it was not until the Guadalupian (middlePermian) that diverse temnospondyl amphibian and amniote faunas became widespreadacross south-central Gondwana. A new source of evidence lies in the Carboniferous-Permiancontinental strata from the Huab Basin (Tsarabis, Huab and Gai-As formations) ofnorthwestern Namibia. These strata have yielded scattered tetrapod remains (temnospondyls,Mesosaurus) reported several years ago. The Gai-As Formation was deposited in a freshwaterrift valley lake at approximately 60°S palaeolatitude. The lake opened westwards into theParana Basin and eastwards it was closed off by river deltas. It is in this transition betweenaquatic and terrestrial environments that most of the fossils are preserved. To date, we havecollected 75 fossils of mainly fishes (actinopterygian and chondrichthyan) and temnospondylamphibians from a single lower Gai-As locality just above the Mesosaurus-bearing levels.Absolute zircon dates from ash beds in the upper Gai-As (265.5±2.2 Ma), and the underlyingMesosaurus-bearing beds (270±1 Ma) constrain the new fauna to the Roadian. At least threedifferent temnospondyl taxa are represented by partial remains of a long-snouted form, and ashort-snouted (parabolic) one with a highly vaulted skull-roof. The third taxon, whichincludes near-complete large (3 m-long) skeletons, presents character states that place it inthe edopoid clade, a basal temnospondyl group only previously known from theCarboniferous-early Permian of Euroamerica and the uppermost Permian of Niger. Theseinclude exclusion of the vomers and palatines from the interpterygoid vacuities, whichthemselves are relatively small and taper strongly anteriorly, and the presence ofintertemporal ossification in the skull table. This new Namibian fauna that lived in andaround saline to brackish water lakes and fjords, helps to fill a crucial ca. 10 Ma gap in thefossil record of tetrapods in the Southern Hemisphere and presents a previously unknownradiation of Laurasian lineages into the region during the Rodian.
Fil: Marsicano, Claudia Alicia. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Estudios Andinos "Don Pablo Groeber". Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Estudios Andinos "Don Pablo Groeber"; Argentina
Fil: Smith, Roger. University of the Witwatersrand; Sudáfrica
Fil: Mancuso, Adriana Cecilia. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Provincia de Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Universidad Nacional de Cuyo. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales; Argentina
Fil: Mocke, Helke. National Earth Science Museum; Namibia
Fil: Abdala, Fernando. University of the Witwatersrand; Sudáfrica
Fil: Gaetano, Leandro Carlos. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Estudios Andinos "Don Pablo Groeber". Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Estudios Andinos "Don Pablo Groeber"; Argentina
20th Biennial Conference of the Palaeontological Society of Southern Africa
Sudáfrica
University Witwatersrand - Materia
-
Tetrapoda
Namibia
Permian
Fauna - Nivel de accesibilidad
- acceso abierto
- Condiciones de uso
- https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
- Repositorio
- Institución
- Consejo Nacional de Investigaciones Científicas y Técnicas
- OAI Identificador
- oai:ri.conicet.gov.ar:11336/227230
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New early permian tetrapod fauna from NamibiaMarsicano, Claudia AliciaSmith, RogerMancuso, Adriana CeciliaMocke, HelkeAbdala, FernandoGaetano, Leandro CarlosTetrapodaNamibiaPermianFaunahttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1The earliest tetrapods in Western Gondwana are the mesosaurs, a group of specializedendemic aquatic parareptiles known only from Artinskian strata of Namibia, South Africa,Uruguay, and Brazil. Recent finds from early Permian beds in northern Brazil revealed a newfreshwater fauna from tropical Gondwana. However, it was not until the Guadalupian (middlePermian) that diverse temnospondyl amphibian and amniote faunas became widespreadacross south-central Gondwana. A new source of evidence lies in the Carboniferous-Permiancontinental strata from the Huab Basin (Tsarabis, Huab and Gai-As formations) ofnorthwestern Namibia. These strata have yielded scattered tetrapod remains (temnospondyls,Mesosaurus) reported several years ago. The Gai-As Formation was deposited in a freshwaterrift valley lake at approximately 60°S palaeolatitude. The lake opened westwards into theParana Basin and eastwards it was closed off by river deltas. It is in this transition betweenaquatic and terrestrial environments that most of the fossils are preserved. To date, we havecollected 75 fossils of mainly fishes (actinopterygian and chondrichthyan) and temnospondylamphibians from a single lower Gai-As locality just above the Mesosaurus-bearing levels.Absolute zircon dates from ash beds in the upper Gai-As (265.5±2.2 Ma), and the underlyingMesosaurus-bearing beds (270±1 Ma) constrain the new fauna to the Roadian. At least threedifferent temnospondyl taxa are represented by partial remains of a long-snouted form, and ashort-snouted (parabolic) one with a highly vaulted skull-roof. The third taxon, whichincludes near-complete large (3 m-long) skeletons, presents character states that place it inthe edopoid clade, a basal temnospondyl group only previously known from theCarboniferous-early Permian of Euroamerica and the uppermost Permian of Niger. Theseinclude exclusion of the vomers and palatines from the interpterygoid vacuities, whichthemselves are relatively small and taper strongly anteriorly, and the presence ofintertemporal ossification in the skull table. This new Namibian fauna that lived in andaround saline to brackish water lakes and fjords, helps to fill a crucial ca. 10 Ma gap in thefossil record of tetrapods in the Southern Hemisphere and presents a previously unknownradiation of Laurasian lineages into the region during the Rodian.Fil: Marsicano, Claudia Alicia. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Estudios Andinos "Don Pablo Groeber". Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Estudios Andinos "Don Pablo Groeber"; ArgentinaFil: Smith, Roger. University of the Witwatersrand; SudáfricaFil: Mancuso, Adriana Cecilia. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Provincia de Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Universidad Nacional de Cuyo. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales; ArgentinaFil: Mocke, Helke. National Earth Science Museum; NamibiaFil: Abdala, Fernando. University of the Witwatersrand; SudáfricaFil: Gaetano, Leandro Carlos. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Estudios Andinos "Don Pablo Groeber". Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Estudios Andinos "Don Pablo Groeber"; Argentina20th Biennial Conference of the Palaeontological Society of Southern AfricaSudáfricaUniversity WitwatersrandUniversity Witwatersrand2018info:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/conferenceObjectConferenciaJournalhttp://purl.org/coar/resource_type/c_5794info:ar-repo/semantics/documentoDeConferenciaapplication/pdfapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/227230New early permian tetrapod fauna from Namibia; 20th Biennial Conference of the Palaeontological Society of Southern Africa; Sudáfrica; 2018; 1-1CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/https://nasmus.co.za/wp-content/uploads/2019/01/PSSA-2018-BOOK-OF-ABSTRACTS.pdfInternacionalinfo:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-03T09:44:29Zoai:ri.conicet.gov.ar:11336/227230instacron:CONICETInstitucionalhttp://ri.conicet.gov.ar/Organismo científico-tecnológicoNo correspondehttp://ri.conicet.gov.ar/oai/requestdasensio@conicet.gov.ar; lcarlino@conicet.gov.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:34982025-09-03 09:44:30.173CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse |
dc.title.none.fl_str_mv |
New early permian tetrapod fauna from Namibia |
title |
New early permian tetrapod fauna from Namibia |
spellingShingle |
New early permian tetrapod fauna from Namibia Marsicano, Claudia Alicia Tetrapoda Namibia Permian Fauna |
title_short |
New early permian tetrapod fauna from Namibia |
title_full |
New early permian tetrapod fauna from Namibia |
title_fullStr |
New early permian tetrapod fauna from Namibia |
title_full_unstemmed |
New early permian tetrapod fauna from Namibia |
title_sort |
New early permian tetrapod fauna from Namibia |
dc.creator.none.fl_str_mv |
Marsicano, Claudia Alicia Smith, Roger Mancuso, Adriana Cecilia Mocke, Helke Abdala, Fernando Gaetano, Leandro Carlos |
author |
Marsicano, Claudia Alicia |
author_facet |
Marsicano, Claudia Alicia Smith, Roger Mancuso, Adriana Cecilia Mocke, Helke Abdala, Fernando Gaetano, Leandro Carlos |
author_role |
author |
author2 |
Smith, Roger Mancuso, Adriana Cecilia Mocke, Helke Abdala, Fernando Gaetano, Leandro Carlos |
author2_role |
author author author author author |
dc.subject.none.fl_str_mv |
Tetrapoda Namibia Permian Fauna |
topic |
Tetrapoda Namibia Permian Fauna |
purl_subject.fl_str_mv |
https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
dc.description.none.fl_txt_mv |
The earliest tetrapods in Western Gondwana are the mesosaurs, a group of specializedendemic aquatic parareptiles known only from Artinskian strata of Namibia, South Africa,Uruguay, and Brazil. Recent finds from early Permian beds in northern Brazil revealed a newfreshwater fauna from tropical Gondwana. However, it was not until the Guadalupian (middlePermian) that diverse temnospondyl amphibian and amniote faunas became widespreadacross south-central Gondwana. A new source of evidence lies in the Carboniferous-Permiancontinental strata from the Huab Basin (Tsarabis, Huab and Gai-As formations) ofnorthwestern Namibia. These strata have yielded scattered tetrapod remains (temnospondyls,Mesosaurus) reported several years ago. The Gai-As Formation was deposited in a freshwaterrift valley lake at approximately 60°S palaeolatitude. The lake opened westwards into theParana Basin and eastwards it was closed off by river deltas. It is in this transition betweenaquatic and terrestrial environments that most of the fossils are preserved. To date, we havecollected 75 fossils of mainly fishes (actinopterygian and chondrichthyan) and temnospondylamphibians from a single lower Gai-As locality just above the Mesosaurus-bearing levels.Absolute zircon dates from ash beds in the upper Gai-As (265.5±2.2 Ma), and the underlyingMesosaurus-bearing beds (270±1 Ma) constrain the new fauna to the Roadian. At least threedifferent temnospondyl taxa are represented by partial remains of a long-snouted form, and ashort-snouted (parabolic) one with a highly vaulted skull-roof. The third taxon, whichincludes near-complete large (3 m-long) skeletons, presents character states that place it inthe edopoid clade, a basal temnospondyl group only previously known from theCarboniferous-early Permian of Euroamerica and the uppermost Permian of Niger. Theseinclude exclusion of the vomers and palatines from the interpterygoid vacuities, whichthemselves are relatively small and taper strongly anteriorly, and the presence ofintertemporal ossification in the skull table. This new Namibian fauna that lived in andaround saline to brackish water lakes and fjords, helps to fill a crucial ca. 10 Ma gap in thefossil record of tetrapods in the Southern Hemisphere and presents a previously unknownradiation of Laurasian lineages into the region during the Rodian. Fil: Marsicano, Claudia Alicia. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Estudios Andinos "Don Pablo Groeber". Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Estudios Andinos "Don Pablo Groeber"; Argentina Fil: Smith, Roger. University of the Witwatersrand; Sudáfrica Fil: Mancuso, Adriana Cecilia. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Provincia de Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Universidad Nacional de Cuyo. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales; Argentina Fil: Mocke, Helke. National Earth Science Museum; Namibia Fil: Abdala, Fernando. University of the Witwatersrand; Sudáfrica Fil: Gaetano, Leandro Carlos. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Estudios Andinos "Don Pablo Groeber". Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Estudios Andinos "Don Pablo Groeber"; Argentina 20th Biennial Conference of the Palaeontological Society of Southern Africa Sudáfrica University Witwatersrand |
description |
The earliest tetrapods in Western Gondwana are the mesosaurs, a group of specializedendemic aquatic parareptiles known only from Artinskian strata of Namibia, South Africa,Uruguay, and Brazil. Recent finds from early Permian beds in northern Brazil revealed a newfreshwater fauna from tropical Gondwana. However, it was not until the Guadalupian (middlePermian) that diverse temnospondyl amphibian and amniote faunas became widespreadacross south-central Gondwana. A new source of evidence lies in the Carboniferous-Permiancontinental strata from the Huab Basin (Tsarabis, Huab and Gai-As formations) ofnorthwestern Namibia. These strata have yielded scattered tetrapod remains (temnospondyls,Mesosaurus) reported several years ago. The Gai-As Formation was deposited in a freshwaterrift valley lake at approximately 60°S palaeolatitude. The lake opened westwards into theParana Basin and eastwards it was closed off by river deltas. It is in this transition betweenaquatic and terrestrial environments that most of the fossils are preserved. To date, we havecollected 75 fossils of mainly fishes (actinopterygian and chondrichthyan) and temnospondylamphibians from a single lower Gai-As locality just above the Mesosaurus-bearing levels.Absolute zircon dates from ash beds in the upper Gai-As (265.5±2.2 Ma), and the underlyingMesosaurus-bearing beds (270±1 Ma) constrain the new fauna to the Roadian. At least threedifferent temnospondyl taxa are represented by partial remains of a long-snouted form, and ashort-snouted (parabolic) one with a highly vaulted skull-roof. The third taxon, whichincludes near-complete large (3 m-long) skeletons, presents character states that place it inthe edopoid clade, a basal temnospondyl group only previously known from theCarboniferous-early Permian of Euroamerica and the uppermost Permian of Niger. Theseinclude exclusion of the vomers and palatines from the interpterygoid vacuities, whichthemselves are relatively small and taper strongly anteriorly, and the presence ofintertemporal ossification in the skull table. This new Namibian fauna that lived in andaround saline to brackish water lakes and fjords, helps to fill a crucial ca. 10 Ma gap in thefossil record of tetrapods in the Southern Hemisphere and presents a previously unknownradiation of Laurasian lineages into the region during the Rodian. |
publishDate |
2018 |
dc.date.none.fl_str_mv |
2018 |
dc.type.none.fl_str_mv |
info:eu-repo/semantics/publishedVersion info:eu-repo/semantics/conferenceObject Conferencia Journal http://purl.org/coar/resource_type/c_5794 info:ar-repo/semantics/documentoDeConferencia |
status_str |
publishedVersion |
format |
conferenceObject |
dc.identifier.none.fl_str_mv |
http://hdl.handle.net/11336/227230 New early permian tetrapod fauna from Namibia; 20th Biennial Conference of the Palaeontological Society of Southern Africa; Sudáfrica; 2018; 1-1 CONICET Digital CONICET |
url |
http://hdl.handle.net/11336/227230 |
identifier_str_mv |
New early permian tetrapod fauna from Namibia; 20th Biennial Conference of the Palaeontological Society of Southern Africa; Sudáfrica; 2018; 1-1 CONICET Digital CONICET |
dc.language.none.fl_str_mv |
eng |
language |
eng |
dc.relation.none.fl_str_mv |
info:eu-repo/semantics/altIdentifier/url/https://nasmus.co.za/wp-content/uploads/2019/01/PSSA-2018-BOOK-OF-ABSTRACTS.pdf |
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info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ |
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openAccess |
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https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ |
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Internacional |
dc.publisher.none.fl_str_mv |
University Witwatersrand |
publisher.none.fl_str_mv |
University Witwatersrand |
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reponame:CONICET Digital (CONICET) instname:Consejo Nacional de Investigaciones Científicas y Técnicas |
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CONICET Digital (CONICET) |
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Consejo Nacional de Investigaciones Científicas y Técnicas |
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dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar |
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