Microfossils
Mostrando 1-12 de 17 artigos, teses e dissertações.
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1. Microfósseis não polínicos como indicadores de mudanças ambientais no Holoceno médio da Lagoa Comprida, Parque Nacional da Restinga de Jurubatiba, Estado do Rio de Janeiro, Brasil
RESUMO O trabalho teve como objetivo identificar e descrever a morfologia de microfósseis não polínicos ocorrentes nos sedimentos de um testemunho retirado próximo à barra da Lagoa Comprida, Estado do Rio de Janeiro, Brasil. Foram identificadas oito formas de fungos, dois tipos de algas Chlorococcales em estágio colonial, um tipo de zygósporo de alga
Hoehnea. Publicado em: 10/06/2019
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2. Acritarchs of the Ediacaran Frecheirinha Formation, Ubajara Group, Northeastern Brazil
We report for the first time the occurrence of organic-walled microfossils in Ediacaran limestones and marls of the Frecheirinha Formation, Ubajara Group, and the first Precambrian acritarchs so far reported for northeastern Brazil. The assemblage of the Frecheirinha Formation represents a low-diversity microflora comprising Leiosphaeridia, Lophosphaeridium
An. Acad. Bras. Ciênc.. Publicado em: 2015-06
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3. Análise e identificação de microvestígios vegetais de cálculo dentário para a reconstrução de dieta sambaquieira: estudo de caso de Jabuticabeira II, SC / Analysis and identification of plant microfossils from dental calculus for the reconstruction of shellmound builder\ s diet: a case study from Jabuticabeira II, SC
Embora os indivíduos construtores dos sambaquis constituam o grupo pré-histórico brasileiro melhor estudado, várias questões continuam em aberto. Algumas delas estão ligadas a estratégias de subsistência. Sabe-se que a economia desses indivíduos era baseada na pesca e que a coleta de moluscos teria papel complementar na alimentação. Mas, atualment
IBICT - Instituto Brasileiro de Informação em Ciência e Tecnologia. Publicado em: 26/06/2012
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4. Microfossils in micrites from Serra da Bodoquena (MS), Brazil: taxonomy and paleoenvironmental implications
Diversos microfósseis provenientes de micritos quaternários da Serra da Bodoquena, estado de Mato Grosso do Sul, Brasil são aqui descritos pela primeira vez. Os taxa descritos são os seguintes: a) ostracodes: Candona sp., Candonopsis sp., Cyclocypris sp., Cypria sp., Cypridopsis sp., Notodromas sp., Ilyocypris sp., Cyprideis sp., Wolburgiopsis cf. chinam
Anais da Academia Brasileira de Ciências. Publicado em: 12/04/2012
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5. Micropaleontolgy applied to the stratigraphic and paleoclimatic interpretation of the transition between the Paranoá Group and São Francisco Supergroup (Neoproterozoic, Cabeceiras, Goiás) / Micropaleontologia aplicada na interpretação estratigráfica e paleoclimática da transição entre o Grupo Paranoá e o Supergrupo São Francisco (Neoproterozóico, Cabeceiras, GO)
The Proterozoic record of the Fazenda Funil, near Cabeceiras, GO, includes three sedimentary units: carbonate at the top of Paranoá Group, diamictite of the Jequitaí Formation, and a succession of shale, marl-shale rhythmites, and carbonate of the Sete Lagoas Formation. Microfossiliferous chert occurs in these three units in the form of lenses in the Paran
Publicado em: 2010
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6. Taxonomia, distribuição estratigráfica e paleoecologia de ostracodes do Cretáceo Superior, Coniaciano, ao Mioceno da Bacia de Santos, Margem Continental Sul do Brasil
The Santos basin is located the continental southern margin of Brazil. One hundred twenty two cutting samples recovered from three wells in Santos basin, two located in the shelf, 1- SPS-5A and 1-SPS-9, and one in slope, 1-SCS-9A. Relative dating based on microfossils, the lower portions of the wells 1-SPS-5A, 1-SCS-9A and 1-SPS-9 are attributed to the Conia
Publicado em: 2009
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7. Microbiota fóssil em sílex da Formação Assistência (Subgrupo Irati, Permiano, Bacia do Paraná) no Estado de São Paulo / Fossil microbiota in chert from Assistência Formation (Irati Subgroup, Permian, Paraná Basin) in São Paulo State
The study of petrographic thin sections of early diageneteic chert from diverse levels and localities of the Assistência Formation in the state of São Paulo, Brazil, revealed for the first time an exceptionally well-preserved assemblage of delicate fossil microorganisms in this important stratigraphic and paleontological Early Permian marker unit of the Pa
Publicado em: 2008
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8. Caracterização mineralógica e tecnológica dos lutitos diatomáceos da Península de Santa Elena, Equador
The diatoms lutite, that had been studied in this these, are inserted in the Villingota Member of the Tosagua Formation, in the Progreso Basin, in the Santa Elena Peninsula, that constitutes an important area located to the southwest of the coast of Ecuador. Arenites in some levels of the Tosagua Formation had also been researched, which had its presence as
Publicado em: 2008
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9. Fossil microorganisms from the approximately 2800 to 2500 million-year-old Bulawayan stromatolite: Application of ultramicrochemical analyses
Microfossils, probably representing members of Precambrian photosynthetic communities of bacteria and blue-green algae, have been found in the approximately 2800-2500 million-year-old Bulawayan stromatolites from Rhodesia. Several populations of coccoid and elongate microfossils have been observed in the dark, carbon-rich stromatolite laminae. Some of these
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10. Pellet microfossils: Possible evidence for metazoan life in Early Proterozoic time
Microfossils resembling fecal pellets occur in acid-resistant residues and thin sections of Middle Cambrian to Early Proterozoic shale. The cylindrical microfossils average 50 × 110 μm and are the size and shape of fecal pellets produced by microscopic animals today. Pellets occur in dark gray and black rocks that were deposited in the facies that also pre
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11. Resistant tissues of modern marchantioid liverworts resemble enigmatic Early Paleozoic microfossils
Absence of a substantial pretracheophyte fossil record for bryophytes (otherwise predicted by molecular systematics) poses a major problem in our understanding of earliest land-plant structure. In contrast, there exist enigmatic Cambrian–Devonian microfossils (aggregations of tubes or sheets of cells or possibly a combination of both) controversially inter
National Academy of Sciences.
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12. Proterozoic and early Cambrian protists: evidence for accelerating evolutionary tempo.
In rocks of late Paleoproterozoic and Mesoproterozoic age (ca. 1700-1000 million years ago), probable eukaryotic microfossils are widespread and well preserved, but assemblage and global diversities are low and turnover is slow. Near the Mesoproterozoic-Neoproterozoic boundary (1000 million years ago), red, green, and chromophytic algae diversified; molecula