Quelques mastodontes miocènes du Portugal

Detalhes bibliográficos
Autor(a) principal: Antunes, M. Telles
Data de Publicação: 2008
Outros Autores: Mazo, A. V.
Tipo de documento: Artigo
Idioma: fra
Título da fonte: Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos)
Texto Completo: http://hdl.handle.net/10362/1512
Resumo: From a paleontological point of view previous determinations for some specimens as Tetralophodon longirostris can be confirmed from Azambujeira (upper level), Valverde and Vale de Matança. A so far undescribed and rare D3 (from Azambujeira, middle level) has been studied. For the first time in Portugal a Gomphotherium angustidens transitional to «Tetralophodon» grandincisivus is reported (from Portas do Sol). Teeth from Lisbon formerly reported (in part) to T. longirostris are now ascribed to G. angustidens. The presence of T. longirostris at Vale de Matança excludes a Pliocene age for Marateca Formation. This and some other evidence clearly points out towards an early Vallesian age. G. angustidens transitional to T. grandincisivus found at Portas do Sol is enough to ascribe this locality to the latest Middle Miocene or earliest Upper Miocene. Therefore it is possible to correlate overlying Santarém limestones to the Vallesian Cartaxo and Almoster ones which are better dated.
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spelling Quelques mastodontes miocènes du PortugalMastodontsMiddle MioceneTagus basinSado basinUpper MiocenePortugalFrom a paleontological point of view previous determinations for some specimens as Tetralophodon longirostris can be confirmed from Azambujeira (upper level), Valverde and Vale de Matança. A so far undescribed and rare D3 (from Azambujeira, middle level) has been studied. For the first time in Portugal a Gomphotherium angustidens transitional to «Tetralophodon» grandincisivus is reported (from Portas do Sol). Teeth from Lisbon formerly reported (in part) to T. longirostris are now ascribed to G. angustidens. The presence of T. longirostris at Vale de Matança excludes a Pliocene age for Marateca Formation. This and some other evidence clearly points out towards an early Vallesian age. G. angustidens transitional to T. grandincisivus found at Portas do Sol is enough to ascribe this locality to the latest Middle Miocene or earliest Upper Miocene. Therefore it is possible to correlate overlying Santarém limestones to the Vallesian Cartaxo and Almoster ones which are better dated.RUNAntunes, M. TellesMazo, A. V.2008-07-282008-07-28T00:00:00Z2008-07-28T00:00:00Zinfo:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/articleapplication/pdfhttp://hdl.handle.net/10362/1512frainfo:eu-repo/semantics/openAccessreponame:Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos)instname:Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informaçãoinstacron:RCAAP2024-03-11T03:31:32Zoai:run.unl.pt:10362/1512Portal AgregadorONGhttps://www.rcaap.pt/oai/openaireopendoar:71602024-03-20T03:14:44.880816Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) - Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informaçãofalse
dc.title.none.fl_str_mv Quelques mastodontes miocènes du Portugal
title Quelques mastodontes miocènes du Portugal
spellingShingle Quelques mastodontes miocènes du Portugal
Antunes, M. Telles
Mastodonts
Middle Miocene
Tagus basin
Sado basin
Upper Miocene
Portugal
title_short Quelques mastodontes miocènes du Portugal
title_full Quelques mastodontes miocènes du Portugal
title_fullStr Quelques mastodontes miocènes du Portugal
title_full_unstemmed Quelques mastodontes miocènes du Portugal
title_sort Quelques mastodontes miocènes du Portugal
author Antunes, M. Telles
author_facet Antunes, M. Telles
Mazo, A. V.
author_role author
author2 Mazo, A. V.
author2_role author
dc.contributor.none.fl_str_mv RUN
dc.contributor.author.fl_str_mv Antunes, M. Telles
Mazo, A. V.
dc.subject.por.fl_str_mv Mastodonts
Middle Miocene
Tagus basin
Sado basin
Upper Miocene
Portugal
topic Mastodonts
Middle Miocene
Tagus basin
Sado basin
Upper Miocene
Portugal
description From a paleontological point of view previous determinations for some specimens as Tetralophodon longirostris can be confirmed from Azambujeira (upper level), Valverde and Vale de Matança. A so far undescribed and rare D3 (from Azambujeira, middle level) has been studied. For the first time in Portugal a Gomphotherium angustidens transitional to «Tetralophodon» grandincisivus is reported (from Portas do Sol). Teeth from Lisbon formerly reported (in part) to T. longirostris are now ascribed to G. angustidens. The presence of T. longirostris at Vale de Matança excludes a Pliocene age for Marateca Formation. This and some other evidence clearly points out towards an early Vallesian age. G. angustidens transitional to T. grandincisivus found at Portas do Sol is enough to ascribe this locality to the latest Middle Miocene or earliest Upper Miocene. Therefore it is possible to correlate overlying Santarém limestones to the Vallesian Cartaxo and Almoster ones which are better dated.
publishDate 2008
dc.date.none.fl_str_mv 2008-07-28
2008-07-28T00:00:00Z
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