Estudo e descrição de uma nova icnoespécie de artrópode da formação Botucatu (jurássico superior — cretáceo inferior) da bacia do Paraná, Estado de São Paulo, Brasil

Detalhes bibliográficos
Ano de defesa: 2017
Autor(a) principal: Peixoto, Bernardo de Campos Pimenta e Marques
Orientador(a): Fernandes, Marcelo Adorna lattes
Banca de defesa: Não Informado pela instituição
Tipo de documento: Dissertação
Tipo de acesso: Acesso aberto
Idioma: por
Instituição de defesa: Universidade Federal de São Carlos
Câmpus São Carlos
Programa de Pós-Graduação: Programa de Pós-Graduação em Ecologia e Recursos Naturais - PPGERN
Departamento: Não Informado pela instituição
País: Não Informado pela instituição
Palavras-chave em Português:
Palavras-chave em Inglês:
Área do conhecimento CNPq:
Link de acesso: https://repositorio.ufscar.br/handle/ufscar/11528
Resumo: Here we describe the new ichnospecies Lithographus araraquarensis isp. nov.. A trackway composed by two rows, whose internal width between the rows is less than 1/3 of the external width; with alternating to staggered series, composed of three elliptical tracks that can vary from slightly elongated, tapered or circular. The slabs were found in the Araraquara region, São Paulo State, in the yellowish/reddish sandstones of the Botucatu Formation, interpreted as a testimony of a gigantic aeolian depositional system, a sandsea (erg), with an arid climate that developed during the Late Jurassic to Early Cretaceous in the Center-South part of Gondwana. Through comparisons with neoichnological studies and morphological deduction, the production of these trackways is assigned to the pterygote insects, which have walked over the unconsolidated sandy substrate. Lithographus araraquarensis isp. nov. was probably produced by beetles that had a flexible diet and were part of the fauna of detritivores omnivores that fed on biomass particles that accumulated in the slipface of the dunes of the Botucatu paleodesert, being able to adopt herbivorous and saprophagous diet when opportune. The description of this new trackway amplifies the knowledge about the faunistic composition of the Botucatu paleodesert and provides subsidies to better understand its paleoenvironment and the ecological relations prevailing at the time. Probably, the producer of Lithographus araraquarensis isp. nov., together with the producers of Taenidium isp. and Skolithos linearis, ware a source of food for primary consumers, represented by arachnids, such as scorpions and spiders, and small mammaliforms. The above trophic level was constituted by theropod dinosaurs of the group Coelurosauria and Carnosauria, and large mammaliforms, which predated smaller theropods and dinosaurs of the Ornithopoda group. Any new occurrences of Lithographus araraquarensis isp. nov. in stratigraphic units of other localities, representing other times, should be analyzed in the light of the ichnofacies model. The recurrence of Lithographus araraquaraensis isp. nov. in aeolian units, and with differentiated abundance in relation to non-aeolian units, could indicate an analogous paleoenvironment to the Botucatu Formation, that is, an arid desert. Both the confirmation and the refutation of recurrence would enrich the theoretical framework of the invertebrate ichnofacies Octopodichnus-Entradichnus for eolian environment.
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spelling Peixoto, Bernardo de Campos Pimenta e MarquesFernandes, Marcelo Adornahttp://lattes.cnpq.br/6709493251686592http://lattes.cnpq.br/05734237939481122019-07-18T17:55:43Z2019-07-18T17:55:43Z2017-04-10PEIXOTO, Bernardo de Campos Pimenta e Marques. Estudo e descrição de uma nova icnoespécie de artrópode da formação Botucatu (jurássico superior — cretáceo inferior) da bacia do Paraná, Estado de São Paulo, Brasil. 2017. Dissertação (Mestrado em Ecologia e Recursos Naturais) – Universidade Federal de São Carlos, São Carlos, 2017. Disponível em: https://repositorio.ufscar.br/handle/ufscar/11528.https://repositorio.ufscar.br/handle/ufscar/11528Here we describe the new ichnospecies Lithographus araraquarensis isp. nov.. A trackway composed by two rows, whose internal width between the rows is less than 1/3 of the external width; with alternating to staggered series, composed of three elliptical tracks that can vary from slightly elongated, tapered or circular. The slabs were found in the Araraquara region, São Paulo State, in the yellowish/reddish sandstones of the Botucatu Formation, interpreted as a testimony of a gigantic aeolian depositional system, a sandsea (erg), with an arid climate that developed during the Late Jurassic to Early Cretaceous in the Center-South part of Gondwana. Through comparisons with neoichnological studies and morphological deduction, the production of these trackways is assigned to the pterygote insects, which have walked over the unconsolidated sandy substrate. Lithographus araraquarensis isp. nov. was probably produced by beetles that had a flexible diet and were part of the fauna of detritivores omnivores that fed on biomass particles that accumulated in the slipface of the dunes of the Botucatu paleodesert, being able to adopt herbivorous and saprophagous diet when opportune. The description of this new trackway amplifies the knowledge about the faunistic composition of the Botucatu paleodesert and provides subsidies to better understand its paleoenvironment and the ecological relations prevailing at the time. Probably, the producer of Lithographus araraquarensis isp. nov., together with the producers of Taenidium isp. and Skolithos linearis, ware a source of food for primary consumers, represented by arachnids, such as scorpions and spiders, and small mammaliforms. The above trophic level was constituted by theropod dinosaurs of the group Coelurosauria and Carnosauria, and large mammaliforms, which predated smaller theropods and dinosaurs of the Ornithopoda group. Any new occurrences of Lithographus araraquarensis isp. nov. in stratigraphic units of other localities, representing other times, should be analyzed in the light of the ichnofacies model. The recurrence of Lithographus araraquaraensis isp. nov. in aeolian units, and with differentiated abundance in relation to non-aeolian units, could indicate an analogous paleoenvironment to the Botucatu Formation, that is, an arid desert. Both the confirmation and the refutation of recurrence would enrich the theoretical framework of the invertebrate ichnofacies Octopodichnus-Entradichnus for eolian environment.Descreve-se aqui uma nova icnoespécie, Lithographus araraquarensis isp. nov., pista composta por duas trilhas, cuja largura interna entre as trilhas é menor que 1/3 da largura externa; com séries alternadas a sub-alternadas, compostas por três pegadas elípticas que podem variar de levemente alongadas, adelgadas (forma de gota) a circulares. As Pistas foram encontradas na região de Araraquara, Estado de São Paulo, nos arenitos amarelos/avermelhados da Formação Botucatu, interpretada como testemunho de um gigantesco sistema deposicional eólico, um mar de dunas (erg), com clima árido que se desenvolveu durante o final do Jurássico até o início do Cretáceo, na parte centro-sul do Gondwana. Por meio de comparações com estudos neoicnológicos e dedução morfológica, a produção dessas pistas é atribuída aos insetos pterigotos caminhando sobre o substrato arenoso inconsolidado. Lithographus araraquarensis isp. nov., provavelmente, foi produzido por besouros com dieta flexível e que faziam parte da fauna de onívoros detritívoros, os quais se alimentavam de partículas de biomassa que se acumulavam no sotavento das dunas do paleodeserto Botucatu, podendo adotar dieta herbívora e saprófaga quando oportuno. A descrição dessa nova pista amplia o conhecimento sobre a composição faunística do paleodeserto Botucatu e fornece subsídios para entender melhor seu paleoambiente e as relações ecológicas vigentes à época. Provavelmente, o produtor de Lithographus araraquarensis isp. nov., junto aos produtores de Taenidium isp. e Skolithos linearis, seriam fonte de alimento para os consumidores primários, representados por aracnídeos, como escorpiões e aranhas, e mamaliformes de pequeno porte. O nível trófico acima seria constituído por dinossauros terópodes do grupo Coelurosauria e Carnosauria, e por mamaliformes de maior porte, que predavam terópodes menores e dinossauros do grupo Ornithopoda. Novas ocorrências de Lithographus araraquarensis isp. nov. em unidades estratigráficas de outras épocas e localidades, devem ser analisadas à luz do modelo de icnofácies. A recorrência de Lithographus araraquaraensis isp. nov. em formações eólicas, e com abundância diferenciada em relação às unidades não eólicas, poderia indicar paleoambiente análogo ao da Formação Botucatu, ou seja, um deserto árido. Desta forma, tanto a confirmação quanto a refutação de recorrência enriquecer-se-ia o arcabouço teórico da icnofácies de invertebrados Octopodichnus–Entradichnus para ambiente eólico.Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)porUniversidade Federal de São CarlosCâmpus São CarlosPrograma de Pós-Graduação em Ecologia e Recursos Naturais - PPGERNUFSCarMesozoicoInsetosEólicoAmérica do SulContinentalDesertoPaleoergGondwanaMesozoicInsectsAeolianSouth AmericaTrackwayDesertCIENCIAS BIOLOGICAS::ECOLOGIAEstudo e descrição de uma nova icnoespécie de artrópode da formação Botucatu (jurássico superior — cretáceo inferior) da bacia do Paraná, Estado de São Paulo, BrasilStudy and description of a new ichnospecies of arthropod of the Botucatu Formation (late jurassic – early cretaceous) of Paraná basin, São Paulo State, Brazilinfo:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/masterThesisOnlineinfo:eu-repo/semantics/openAccessreponame:Repositório Institucional da UFSCARinstname:Universidade Federal de São Carlos (UFSCAR)instacron:UFSCARORIGINALDissBCPMP.pdfDissBCPMP.pdfapplication/pdf27271593https://{{ getenv "DSPACE_HOST" "repositorio.ufscar.br" }}/bitstream/ufscar/11528/1/DissBCPMP.pdf7240b79b65315b6fa0d1f3205cbbaea3MD51LICENSElicense.txtlicense.txttext/plain; charset=utf-81957https://{{ getenv "DSPACE_HOST" "repositorio.ufscar.br" }}/bitstream/ufscar/11528/2/license.txtae0398b6f8b235e40ad82cba6c50031dMD52TEXTDissBCPMP.pdf.txtDissBCPMP.pdf.txtExtracted texttext/plain121575https://{{ getenv "DSPACE_HOST" "repositorio.ufscar.br" }}/bitstream/ufscar/11528/3/DissBCPMP.pdf.txtb8f8e8d2d254e86e2f6362daae80803bMD53THUMBNAILDissBCPMP.pdf.jpgDissBCPMP.pdf.jpgIM Thumbnailimage/jpeg10644https://{{ getenv "DSPACE_HOST" "repositorio.ufscar.br" }}/bitstream/ufscar/11528/4/DissBCPMP.pdf.jpg53ce786e2bcd8905e3c68ca00ebc2da8MD54ufscar/115282020-10-08 12:04:34.261oai:repositorio.ufscar.br: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Repositório InstitucionalPUBhttps://repositorio.ufscar.br/oai/requestopendoar:43222023-05-25T12:54:55.857935Repositório Institucional da UFSCAR - Universidade Federal de São Carlos (UFSCAR)false
dc.title.por.fl_str_mv Estudo e descrição de uma nova icnoespécie de artrópode da formação Botucatu (jurássico superior — cretáceo inferior) da bacia do Paraná, Estado de São Paulo, Brasil
dc.title.alternative.eng.fl_str_mv Study and description of a new ichnospecies of arthropod of the Botucatu Formation (late jurassic – early cretaceous) of Paraná basin, São Paulo State, Brazil
title Estudo e descrição de uma nova icnoespécie de artrópode da formação Botucatu (jurássico superior — cretáceo inferior) da bacia do Paraná, Estado de São Paulo, Brasil
spellingShingle Estudo e descrição de uma nova icnoespécie de artrópode da formação Botucatu (jurássico superior — cretáceo inferior) da bacia do Paraná, Estado de São Paulo, Brasil
Peixoto, Bernardo de Campos Pimenta e Marques
Mesozoico
Insetos
Eólico
América do Sul
Continental
Deserto
Paleoerg
Gondwana
Mesozoic
Insects
Aeolian
South America
Trackway
Desert
CIENCIAS BIOLOGICAS::ECOLOGIA
title_short Estudo e descrição de uma nova icnoespécie de artrópode da formação Botucatu (jurássico superior — cretáceo inferior) da bacia do Paraná, Estado de São Paulo, Brasil
title_full Estudo e descrição de uma nova icnoespécie de artrópode da formação Botucatu (jurássico superior — cretáceo inferior) da bacia do Paraná, Estado de São Paulo, Brasil
title_fullStr Estudo e descrição de uma nova icnoespécie de artrópode da formação Botucatu (jurássico superior — cretáceo inferior) da bacia do Paraná, Estado de São Paulo, Brasil
title_full_unstemmed Estudo e descrição de uma nova icnoespécie de artrópode da formação Botucatu (jurássico superior — cretáceo inferior) da bacia do Paraná, Estado de São Paulo, Brasil
title_sort Estudo e descrição de uma nova icnoespécie de artrópode da formação Botucatu (jurássico superior — cretáceo inferior) da bacia do Paraná, Estado de São Paulo, Brasil
author Peixoto, Bernardo de Campos Pimenta e Marques
author_facet Peixoto, Bernardo de Campos Pimenta e Marques
author_role author
dc.contributor.authorlattes.por.fl_str_mv http://lattes.cnpq.br/0573423793948112
dc.contributor.author.fl_str_mv Peixoto, Bernardo de Campos Pimenta e Marques
dc.contributor.advisor1.fl_str_mv Fernandes, Marcelo Adorna
dc.contributor.advisor1Lattes.fl_str_mv http://lattes.cnpq.br/6709493251686592
contributor_str_mv Fernandes, Marcelo Adorna
dc.subject.por.fl_str_mv Mesozoico
Insetos
Eólico
América do Sul
Continental
Deserto
topic Mesozoico
Insetos
Eólico
América do Sul
Continental
Deserto
Paleoerg
Gondwana
Mesozoic
Insects
Aeolian
South America
Trackway
Desert
CIENCIAS BIOLOGICAS::ECOLOGIA
dc.subject.eng.fl_str_mv Paleoerg
Gondwana
Mesozoic
Insects
Aeolian
South America
Trackway
Desert
dc.subject.cnpq.fl_str_mv CIENCIAS BIOLOGICAS::ECOLOGIA
description Here we describe the new ichnospecies Lithographus araraquarensis isp. nov.. A trackway composed by two rows, whose internal width between the rows is less than 1/3 of the external width; with alternating to staggered series, composed of three elliptical tracks that can vary from slightly elongated, tapered or circular. The slabs were found in the Araraquara region, São Paulo State, in the yellowish/reddish sandstones of the Botucatu Formation, interpreted as a testimony of a gigantic aeolian depositional system, a sandsea (erg), with an arid climate that developed during the Late Jurassic to Early Cretaceous in the Center-South part of Gondwana. Through comparisons with neoichnological studies and morphological deduction, the production of these trackways is assigned to the pterygote insects, which have walked over the unconsolidated sandy substrate. Lithographus araraquarensis isp. nov. was probably produced by beetles that had a flexible diet and were part of the fauna of detritivores omnivores that fed on biomass particles that accumulated in the slipface of the dunes of the Botucatu paleodesert, being able to adopt herbivorous and saprophagous diet when opportune. The description of this new trackway amplifies the knowledge about the faunistic composition of the Botucatu paleodesert and provides subsidies to better understand its paleoenvironment and the ecological relations prevailing at the time. Probably, the producer of Lithographus araraquarensis isp. nov., together with the producers of Taenidium isp. and Skolithos linearis, ware a source of food for primary consumers, represented by arachnids, such as scorpions and spiders, and small mammaliforms. The above trophic level was constituted by theropod dinosaurs of the group Coelurosauria and Carnosauria, and large mammaliforms, which predated smaller theropods and dinosaurs of the Ornithopoda group. Any new occurrences of Lithographus araraquarensis isp. nov. in stratigraphic units of other localities, representing other times, should be analyzed in the light of the ichnofacies model. The recurrence of Lithographus araraquaraensis isp. nov. in aeolian units, and with differentiated abundance in relation to non-aeolian units, could indicate an analogous paleoenvironment to the Botucatu Formation, that is, an arid desert. Both the confirmation and the refutation of recurrence would enrich the theoretical framework of the invertebrate ichnofacies Octopodichnus-Entradichnus for eolian environment.
publishDate 2017
dc.date.issued.fl_str_mv 2017-04-10
dc.date.accessioned.fl_str_mv 2019-07-18T17:55:43Z
dc.date.available.fl_str_mv 2019-07-18T17:55:43Z
dc.type.status.fl_str_mv info:eu-repo/semantics/publishedVersion
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dc.identifier.citation.fl_str_mv PEIXOTO, Bernardo de Campos Pimenta e Marques. Estudo e descrição de uma nova icnoespécie de artrópode da formação Botucatu (jurássico superior — cretáceo inferior) da bacia do Paraná, Estado de São Paulo, Brasil. 2017. Dissertação (Mestrado em Ecologia e Recursos Naturais) – Universidade Federal de São Carlos, São Carlos, 2017. Disponível em: https://repositorio.ufscar.br/handle/ufscar/11528.
dc.identifier.uri.fl_str_mv https://repositorio.ufscar.br/handle/ufscar/11528
identifier_str_mv PEIXOTO, Bernardo de Campos Pimenta e Marques. Estudo e descrição de uma nova icnoespécie de artrópode da formação Botucatu (jurássico superior — cretáceo inferior) da bacia do Paraná, Estado de São Paulo, Brasil. 2017. Dissertação (Mestrado em Ecologia e Recursos Naturais) – Universidade Federal de São Carlos, São Carlos, 2017. Disponível em: https://repositorio.ufscar.br/handle/ufscar/11528.
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dc.publisher.program.fl_str_mv Programa de Pós-Graduação em Ecologia e Recursos Naturais - PPGERN
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publisher.none.fl_str_mv Universidade Federal de São Carlos
Câmpus São Carlos
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institution UFSCAR
reponame_str Repositório Institucional da UFSCAR
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