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  • About
  • The Global ETD Search service is a free service for researchers to find electronic theses and dissertations. This service is provided by the Networked Digital Library of Theses and Dissertations.
    Our metadata is collected from universities around the world. If you manage a university/consortium/country archive and want to be added, details can be found on the NDLTD website.
1

The Identification of Fossil Angiosperm Pollen and Its Bearing on the Time and Place of the Origin of Angiosperms

Zavada, M. S. 01 January 2007 (has links)
Studies in the 1970's reporting the occurrence of fossil pollen types in the Cretaceous, coupled with surveys of extant pollen morphology of primitive flowering plants, laid the foundation for proposing a Lower Cretaceous origin of angiosperms. Over the last 30 years, morphological, ultrastructural, and ontogenetic studies of both extant and fossil pollen have provided an array of new characters, as well as greater resolution in defining character polarities. Moreover, a range of fossil pollen types exhibiting angiosperm characters occur in low frequency within Triassic and Jurassic sediments. The pollen data provide evidence of a pre-Cretaceous origin of angiosperms. Speciation and extinction rates were likely equal during the Triassic and Jurassic, resulting in the paucity of angiosperm pollen types from different geographic areas in the Atlantic - South American/African rift zone. It was not until the Lower Cretaceous that origination rates exceed extinction rates, resulting in the subsequent diversification of angiosperms and the origin of the eudicots.
2

Análise da variação longitudinal do esqueleto axial em Serpentes (Squamata) empregando ferramentas de morfometria geométrica / Analysis of the longitudinal variation in the axial skeleton of Serpentes (Squamata) using geometric morphometrics techniques

Machado, Fabio de Andrade 29 November 2010 (has links)
As cobras são um grupo de vertebrados extremamente bem sucedido. Apesar da aparente simplicidade, elas conseguiram ocupar uma grande diversidade de habitats. O esqueleto axial das serpentes apresenta relação com vários aspectos da vida que puderam ter tido influência direta em seu sucesso evolutivo. Além disso, a forma dos elementos vertebrais possui valor taxonômico, fato que desperta particular interesse, visto que a maior parte do registro fóssil deste grupo é constituído por elementos vertebrais desarticulados. A morfometria geométrica utiliza informações sobre a posição de pontos em duas ou três dimensões, localizados sobre estruturas anatômicas para análise estatística da variação da forma. Esse conjunto de técnicas tem se mostrado eficaz em avaliar variações da forma que não seriam diagnosticadas por métodos tradicionais. O presente trabalho buscou avaliar as vértebras do esqueleto pré-cloacal de Serpentes no contexto da morfometria geométrica, considerando as influências ecológicas e filogenéticas sob estas estruturas, e investigando ainda a utilidade taxonômica da forma vertebral. Os resultados apresentados aqui sugerem a existência de uma padronização do esqueleto axial de serpentes que é conservada ao longo da história evolutiva desse grupo. Análises ecomorfológicas demonstram que a forma vertebral é fortemente influenciada por hábitos de vida como fossorialidade e constrição. A despeito da ausência de sinal filogenético, as análises de classificação de elementos vertebrais dissociados demonstram que a forma vertebral pode ser utilizada para a diagnose de vértebras isoladas. Esses resultados reforçam a necessidade de realização de análises de variação longitudinal para a identificação correta de material fóssil referente a este grupo. / Snakes are an extremely successful group of vertebrates. Despite their apparent morphological simplicity, they managed to occupy a great diversity of habitats. The axial skeleton of snakes has relationships with various aspects of their life history that could have had direct influence in the evolutionary success of these animals. Furthermore, the shape of the vertebrae is recognized as being of taxonomic value, a fact that elicits a special interest, since the majority of the fossil record of this group is composed of disarticulated vertebral elements. Geometric morphometrics methods use information about the position of landmarks in two or three dimensions, placed over anatomical structures for statistical analyses of shape variation. This group of techniques has been shown to identify shape variations that would not be diagnosed through traditional methods. The present work sought to evaluate the vertebrae of the pre-cloacal skeleton of Serpentes in the context of geometric morphometrics, evaluating the influences of ecology and phylogeny over the shape of these structures, and also investigating the taxonomic usefulness of vertebral shape. Results presented here suggest the existence of a patterning of the axial skeleton that is conserved throughout the evolutionary history of the group. An ecomorphological analysis demonstrates that the vertebral shape is highly influenced by life-history traits such as fossoriality and constriction. Despite the absence of phylogenetic signal, analyzes of classification of dissociated vertebral elements show that the vertebral shape can be used to diagnose isolated vertebrae. These results reiterate the necessity of performing studies of longitudinal variation in order to correctly identify fossil material associated with this group.
3

Determining the antiquity of dog origins: canine domestication as a model for the consilience between molecular genetics and archaeology

Raisor, Michelle Jeanette 15 November 2004 (has links)
Archaeologists have favored a date of 14,000-15,000 years before present (BP) for canine domestication. However, recent studies of mutations in the mitochondrial DNA sequence by molecular geneticists have implied that dogs were domesticated over 100,000 years ago, which has challenged traditional theory. Geneticists have further hypothesized that dogs originated from wolf ancestors based upon the number of substitutions observed in dog and wolf haplotypes. Although both disciplines provide substantial evidence for their theories, the origin of dog domestication remains controversial. Several areas continue to be debatable. First, both geneticists and archaeologists incorrectly use the term domestication to describe events that clearly can not be proven to under human control. Second, the evolutionary development of canines is viewed by molecular biologists as well as archaeologist to be indicators of domestication without any further exploration of other probable causes. Third, the studies in canine genetics are so complex that most archaeologists have difficulty in providing evidence that would be contradictory to molecular theory. Fourth, both fields of study continually ignore innate behavioral characteristics of wolves that would make domestication highly improbable. Fifth, geneticists rely heavily on data gathered from sequencing of mitochondrial DNA, which has been assumed to maternally inherited. However recent human studies have shown that this assumption has now been proven to be incorrect. And finally, not only are morphological traits of fossilized dogs and wolves so similar that making a taxonomic identification improbable, but also the amount of archaeological remains available are too sparse and fragmented for accurate affiliation. An alternate theory of canine domestication will be proposed utilizing data gathered from the archaeological record and molecular research. I hypothesize that dogs diverged naturally from wolves 100,000 years ago as a result of the natural course of evolution, not human intervention, and had already evolved into a dog prior to being domesticated by humans 14,000-15,000 years ago. Evidence will be presented to clearly show that this hypothesis is a more accurate scenario of canine domestication.
4

Modelos de nicho ecológico, registros fósseis e o pressuposto de equilíbrio das distribuições das espécies com o clima / Ecological niche models, fossil records and the assumption of climate equilibrium with species distribution

Guimaraes, Tulio Max de Oliveira 23 April 2014 (has links)
Submitted by Cláudia Bueno (claudiamoura18@gmail.com) on 2015-10-20T17:21:43Z No. of bitstreams: 2 Dissertação - Túlio Max de Oliveira Guimarães - 2014.pdf: 2190502 bytes, checksum: 95a9c8660ff6a8f4fee3c71a61784e47 (MD5) license_rdf: 23148 bytes, checksum: 9da0b6dfac957114c6a7714714b86306 (MD5) / Approved for entry into archive by Luciana Ferreira (lucgeral@gmail.com) on 2015-10-21T10:06:29Z (GMT) No. of bitstreams: 2 Dissertação - Túlio Max de Oliveira Guimarães - 2014.pdf: 2190502 bytes, checksum: 95a9c8660ff6a8f4fee3c71a61784e47 (MD5) license_rdf: 23148 bytes, checksum: 9da0b6dfac957114c6a7714714b86306 (MD5) / Made available in DSpace on 2015-10-21T10:06:29Z (GMT). No. of bitstreams: 2 Dissertação - Túlio Max de Oliveira Guimarães - 2014.pdf: 2190502 bytes, checksum: 95a9c8660ff6a8f4fee3c71a61784e47 (MD5) license_rdf: 23148 bytes, checksum: 9da0b6dfac957114c6a7714714b86306 (MD5) Previous issue date: 2014-04-23 / Coordenação de Aperfeiçoamento de Pessoal de Nível Superior - CAPES / Understand how species are spatially distributed has been exhaustively discussed in ecology over the last decades. Recently, frameworks based on Ecological Niche Models (ENM) have emerged to avoid problems related to the lack of species geographical information, once it identify which environmental suitable conditions of geographic space enable the persistence of species. Recently this approach has become a significant component in Systematic Conservation Planning, helping managers to select better areas to create reserves. Several factors limit the fundamental niche of species and poor geographical information about species distribution may lead to be an underestimation of suitable conditions that one specie occur,, revealing an non-equilibrium with climate. Thus, using good fossil records to construct ecological niche models can be a better way to evaluate and improve ENM predictions and it allows us to estimate other suitable conditions not seen before. Thereby, our aim was to investigate if ENMs built for Mauritia flexuosa, and Tapirus terrestris improve with the addition of fossil information. So, different ENMs were built using, first, current records and, second, using different proportions of fossil data. The results showed that species closer to equilibrium with climate (M. flexuosa) had an improvement in model’s performance with the addition of fossil records, while species with higher non-equilibrium (T. terrestris) decreased the model’s performance. / Entender como as espécies estão espacialmente distribuídas pelo planeta tem sido um assunto exaustivamente discutido em ecologia ao longo das últimas décadas. Recentemente, abordagens baseadas nos Modelos de Nicho Ecológico têm surgido com o intuito de eliminar problemas relacionados à lacuna de informação geográfica sobre as espécies, uma vez que identifica locais no espaço geográfico que apresenta as condições ambientais favoráveis à persistência das mesmas. Vários fatores limitam o nicho fundamental das espécies e informações geográficas enviesadas acerca de sua distribuição podem levar a uma subestimativa das condições adequadas à ocorrência, revelando um desequilíbrio com o clima. Deste modo, a utilização de registros fósseis na construção dos Modelos de Nicho Ecológico pode ser uma maneira de melhorar as predições dos modelos, já que adiciona novas informações ambientais que não haviam sido encontradas atualmente. Deste modo, nosso objetivo foi investigar se os Modelos de Nicho Ecológico construídos para Mauritia flexuosa e Tapirus terrestris apresentaram melhora no poder preditivo pela adição de informação fóssil. Para isso, foram construídos diferentes modelos utilizando dados atuais apenas e modelos utilizando tanto informação atual quanto informação fóssil, em diferentes porcentagens. Através de uma Análise de Variância Fatorial, medimos se a adição de informação fóssil apresentava melhora significativa no poder preditivo dos modelos. Nossos resultados mostram que quando há pouca variação na informação ambiental adicionada (M. flexuosa), os modelos apresentam uma melhora significativa no poder preditivo, ao passo que para aqueles dados com maior variação (T. terrestris) o efeito é inverso. Isso se deve pela variação dos erros de omissão e comissão gerados durante o processo de modelagem.
5

Análise da variação longitudinal do esqueleto axial em Serpentes (Squamata) empregando ferramentas de morfometria geométrica / Analysis of the longitudinal variation in the axial skeleton of Serpentes (Squamata) using geometric morphometrics techniques

Fabio de Andrade Machado 29 November 2010 (has links)
As cobras são um grupo de vertebrados extremamente bem sucedido. Apesar da aparente simplicidade, elas conseguiram ocupar uma grande diversidade de habitats. O esqueleto axial das serpentes apresenta relação com vários aspectos da vida que puderam ter tido influência direta em seu sucesso evolutivo. Além disso, a forma dos elementos vertebrais possui valor taxonômico, fato que desperta particular interesse, visto que a maior parte do registro fóssil deste grupo é constituído por elementos vertebrais desarticulados. A morfometria geométrica utiliza informações sobre a posição de pontos em duas ou três dimensões, localizados sobre estruturas anatômicas para análise estatística da variação da forma. Esse conjunto de técnicas tem se mostrado eficaz em avaliar variações da forma que não seriam diagnosticadas por métodos tradicionais. O presente trabalho buscou avaliar as vértebras do esqueleto pré-cloacal de Serpentes no contexto da morfometria geométrica, considerando as influências ecológicas e filogenéticas sob estas estruturas, e investigando ainda a utilidade taxonômica da forma vertebral. Os resultados apresentados aqui sugerem a existência de uma padronização do esqueleto axial de serpentes que é conservada ao longo da história evolutiva desse grupo. Análises ecomorfológicas demonstram que a forma vertebral é fortemente influenciada por hábitos de vida como fossorialidade e constrição. A despeito da ausência de sinal filogenético, as análises de classificação de elementos vertebrais dissociados demonstram que a forma vertebral pode ser utilizada para a diagnose de vértebras isoladas. Esses resultados reforçam a necessidade de realização de análises de variação longitudinal para a identificação correta de material fóssil referente a este grupo. / Snakes are an extremely successful group of vertebrates. Despite their apparent morphological simplicity, they managed to occupy a great diversity of habitats. The axial skeleton of snakes has relationships with various aspects of their life history that could have had direct influence in the evolutionary success of these animals. Furthermore, the shape of the vertebrae is recognized as being of taxonomic value, a fact that elicits a special interest, since the majority of the fossil record of this group is composed of disarticulated vertebral elements. Geometric morphometrics methods use information about the position of landmarks in two or three dimensions, placed over anatomical structures for statistical analyses of shape variation. This group of techniques has been shown to identify shape variations that would not be diagnosed through traditional methods. The present work sought to evaluate the vertebrae of the pre-cloacal skeleton of Serpentes in the context of geometric morphometrics, evaluating the influences of ecology and phylogeny over the shape of these structures, and also investigating the taxonomic usefulness of vertebral shape. Results presented here suggest the existence of a patterning of the axial skeleton that is conserved throughout the evolutionary history of the group. An ecomorphological analysis demonstrates that the vertebral shape is highly influenced by life-history traits such as fossoriality and constriction. Despite the absence of phylogenetic signal, analyzes of classification of dissociated vertebral elements show that the vertebral shape can be used to diagnose isolated vertebrae. These results reiterate the necessity of performing studies of longitudinal variation in order to correctly identify fossil material associated with this group.
6

Quantitative Estimates of Time-Averaging in Brachiopod Shell Accumulations from a Holocene Tropical Shelf (SW Brazil)

Carroll, Monica 06 August 2001 (has links)
Time-averaging, the mixing of fossils of different ages within a single bed, defines the limit of temporal resolution of the fossil record. Quantitative estimates of this resolution threshold have not been acquired for any group other than mollusks. This study provides the first quantitative estimates of time-averaging for brachiopods, extending our understanding of intrinsic, or group specific controls on this process. Estimates were obtained by direct dating of individual terebratulid brachiopod shells Bouchardia rosea (Mawe) collected from modern surficial shelly accumulations in the Southeast Brazilian Bight (SW Atlantic). Using amino acid racemization dating calibrated with radiocarbon, 82 individual brachiopod shells, collected from four nearshore localities, were dated. The shells vary in age from modern to 3000 years, standard deviation = 680 years. The age distribution is significantly right-skewed (K3=2.48). At 50-year resolution, the temporal completeness is 75% for the last 1000 years and declines to 20% completeness for 1000-2000 yr. BP. Preservational quality (taphonomy) of modern (<50 yr.) shells is statistically indistinguishable from that of older shells, demonstrating that shell taphonomy is not a good predictor of within-assemblage relative age. These results conform to previously published results for mollusks. Therefore, brachiopods can show considerable time-averaging and this time-averaging can be on a scale similar to aragonitic mollusks despite the apparent lack of robustness of calcitic brachiopod shells. This suggests that the brachiopod fossil record can be notably time-averaged, but estimates of this mixing cannot be reliably deciphered from the taphonomic condition of shells. / Master of Science
7

Establishing “The Fossil Record”: A Database of Vertebrate Paleontological Sites Across the State of Tennessee

Mclaurine, Sarah 01 May 2024 (has links) (PDF)
Fossil localities across the state of Tennessee and the data related to those sites were compiled from Tennessee Division of Geology Bulletin 84, titled “Tennessee’s Prehistoric Vertebrates,” and stored in a Microsoft Access geodatabase housed by the Department of Collections at the East Tennessee State University Museum of Natural History located at the Gray Fossil Site. Included in the database are forms to enter new site localities, view information about those already entered, view and add data to a master faunal list for the state, view sites repository information and store and add documents that are key-word searchable from the main menu. This database was compiled to give researchers a straightforward and easy to use means of analyzing known information about paleontological sites across the state, with the potential to be expanded worldwide. Conservation of data is crucial and can be lost over time unless data preservation efforts are made.
8

A duração das linhagens e a dinâmica macroevolutiva de Ruminantia (Mammalia) / Lineage duration and the macroevolutionary dynamics of Ruminantia (Mammalia)

Sousa, Matheus Januario Lopes de 11 June 2019 (has links)
O objetivo geral desta dissertação é testar hipóteses relacionadas à duração das linhagens (i.e. o intervalo de tempo definido pela origem e extinção das diferentes linhagens) e à dinâmica da diversificação dos ruminantes. Para isso, nós usamos compilações públicas de dados fósseis e modelos probabilísticos. Como a literatura macroevolutiva se aproveita das múltiplas escalas taxonômicas onde é possível estudar a mudança da biodiversidade no tempo, os dois capítulos desta dissertação testam suas hipóteses no níveis de espécie e gênero na tentativa de iluminar o papel da escala na manifestação dos padrões macroevolutivos. No primeiro capítulo, nós investigamos se tratamentos taxonômicos distintos aplicados aos dados brutos alteram os resultados obtidos por um método macroevolutivo. Nossos resultados sugerem que os dados, mesmo após passar por diferentes tratamentos, indicam similares dinâmicas de diversificação tanto no nível taxonômico dos gêneros quanto no nível das espécies. Por outro lado, as comparações entre dois conjuntos de dados inicialmente distintos podem gerar diferenças consideráveis na dinâmica da diversificação e inclusive indicar diferenças entre escalas taxonômicas. Esses resultados são robustos mesmo que as imperfeições do registro fóssil sejam consideradas de diferentes maneiras pelo método usado. No segundo capítulo, nós usamos modelos probabilísticos para testar uma importante hipótese macroevolutiva que é também considerada uma premissa para vários estudos da área: a de que a probabilidade de extinção de qualquer linhagem é independente da sua longevidade, ou seja, do intervalo de tempo que a linhagem já viveu. Nossos resultados sugerem um padrão consistente de diminuição na probabilidade de extinção conforme as espécies vivem por mais tempo, enquanto que o padrão observado do no nível dos gêneros é menos claro. Este resultado não só enriquece o nosso conhecimento a respeito da dinâmica da extinção de linhagens, como sugere que a premissa de independência de idade na probabilidade de extinção (importante para vários estudos macroevolutivos) pode não ser válida, pelo menos para Ruminantia. Nós esperamos que os dados e ideias aqui expostos interajam com novas ideias e dados do leitor, estimulando o desenvolvimento da macroevolução / The main goal of this dissertation is to test hypotheses related to the duration of the lineages (i.e. the time interval between the origin and extinction of each lineage) and to the diversification dynamics of the ruminants. To achieve this goal, we used public compilations of fossil data and probabilistic models. As the macroevolutionary literature take advantage of multiple taxonomic scales in which is possible to study biodiversity changes through time, the two chapters of this dissertation tested different hypotheses in both the species and genus levels, as na attempt to shed some light on the role of scale influencing the macroevolutionary phenomena. In the first chapter, we investigated if different taxonomic treatments applied over the raw data significantly change the results obtained from a macroevolutionary method. Our results suggest that the same data, even passing through different data curations, indicate similar diversification dynamics in species and genus taxonomic levels. On the other hand, data that comes from different sources may present considerable differences in the diversification dynamics, and even indicate differences between taxonomic scales. These results are robust to different considerations of the preservation biases of the fossil record by the method. In the second chapter, we used probabilistic models to test an importante macroevolutionary hypothesis that is also considered a premise of several macroevolutionary studies: that the probability of extinction of any lineage is independent of its longevity (the time span determined by the origination and extinction of each lineage). Our results suggest a consistent pattern of decreasing extinction probability as species live for longs periods of time, but the pattern presented by the genera is less clear. These results not only enhance our knowledge about extinction dynamics, but it also suggests that the premise of age independence in the extinction probability (important for several macroevolutionary studies) might not be valid, at least for Ruminatia. We hope our data and ideas interact with new ideas and data from the reader to stimulate the development of the macroevolutionary field
9

Die Magenstrukturen der Brachyura (Crustacea, Decapoda)

Brösing, Andreas 27 November 2002 (has links)
Innerhalb der Decapoda stellt das Taxon Brachyura eines der artenreichsten Taxa mit bis zu 10000 Arten dar. Die Phylogenie der Brachyura wird aufgrund morphologischer und molekularer Untersuchungen seit mehr als ein Jahrhundert kontrovers diskutiert. Zur Klärung phylogenetischer Fragestellungen wurde mit den vergleichenden Untersuchungen der Magenossikel und der Magenzähne von 66 Taxa der Brachyura ein neuer phylogenetischer Ansatz gewählt. Mit Anwendung eines spezifischen Färbepigmentes, Alizarin-Rot S, konnten sechs neue Magenossikel einer bereits existierenden Nomenklatur hinzugefügt werden, so dass jetzt 41 Magenossikel für das Grundmuster der Brachyura angenommen werden können. Im Ergebnis der phylogenetischen Analyse wird ein monophyletisches Taxon Brachyura einschließlich der Taxa Dromiidae und Raninidae unterstützt. Die von Guinot (1977, 1978) als Monophyla postulierten Teiltaxa Podotremata und Heterotremata finden hier keine Unterstützung. Taxa wie Raninidae und Cymonomidae, welche aufgrund der coxalen Position ihrer Genitalporen dem Taxon Podotremata sensu Guinot zugeschrieben werden, weisen nach vorliegenden Daten eine nähere Verwandtschaft zu den "höheren" Krabben auf. Eine Monophylie eines Taxons Thoracotremata sensu Guinot kann dagegen basierend auf den analysierten Magenstrukturen, aber auch auf der Grundlage molekularer Studien (Schubart et al. 2000a, 2000b) und dem vorliegenden Daten zum Fossilbericht angenommen werden. Eine basale Stellung der Dynomenidae und Dromiidae im Ergebnis der kladistischen Analyse lässt sich mit den Fossilfunden aus dem mittleren Jura in Übereinstimmung bringen. Des weiteren kann für die meisten Taxa der "höheren" Krabben ein gemeinsamer Vorfahre für die obere Kreide bzw. bis zum Beginn des Tertiärs postuliert werden. / Within the Decapoda the taxon Brachyura is the species-richest taxon with up to 10000 species. The phylogeny of the Brachyura has been discussed based on morphological and molecular investigations since more than a century. The investigation of the foregut-ossicles and gastric-teeth of 66 brachyuran species, is a new approach to answer important phylogenetic questions. Using a specific staining pigment Alizarin Red S, six new described foregut-ossicles are added to an existing nomenclature. As a result of this method the presence of 41 foregut-ossicles is proposed for the ground pattern of the Brachyura. The cladistic analysis supports a monophyletic origin of the Brachyura including the Dromiidae and the Raninidae. The taxa Podotremata and Heterotremata, postulated as monophyletic by Guinot (1977, 1978), are not supported in the present study. The Dromiidae and Raninidae, which are placed within the Podotremata sensu Guinot, are closer related to the "higher crabs". Based on the analysed foregut-characters, several molecular studies (Schubart et al. 2000a, 2000b), and the data of the fossil record, a monophyletic origin of the Thoracotremata sensu Guinot is suggested. The analysed basal position of the Dynomenidae and Dromiidae is in agreement with the brachyuran fossil record. A common ancestor for most of the "higher" brachyuran crabs is suggested for the period between the upper Cretaceous and the beginning of the Tertiary.
10

O tempo geológico no ensino fundamental e médio: os estudantes e os livros didáticos / The geological time in elementary and high school: students and textbooks

Oliveira, Jeferson Botelho de 04 April 2006 (has links)
A análise das colunas geológicas consultadas a partir de diferentes livros didáticos, possibilitou compreender como o tempo geológico aparece no ensino de evolução, junto à disciplina de biologia do ensino médio e na disciplina de geografia do ensino fundamental, enfocando a origem e as transformações do relevo terrestre ao longo das eras geológicas. Foi possível observar inúmeras informações heterogêneas e problemáticas didáticas, revelando problemas de ordem estrutural e cognitiva, que podem prejudicar professores e alunos no entendimento do tempo profundo, apresentando eventos desorganizados ou omitidos. Procurou-se ressaltar os principais marcos da construção da coluna geológica assim como os principais personagens envolvidos; citando James Hutton, John Playfair, Charles Lyell, Charles Darwin. Responsáveis estes parcialmente pelas modificações do pensamento filosófico-científico da Europa durante os séculos XVIII e XIX, destituindo o antigo pragmatismo dominante da crença de um planeta com 6000 anos de idade. As escalas temporais envolvidas como o mega-intervalo Pré-Cambriano, com 4,0 bilhões de anos de duração ou representando cerca de 85% do tempo geológico, muitas vezes foi apresentado graficamente diminuído ou omitido nas colunas geológicas analisadas. Detectou-se também problemas gráficos visuais com o Eon Fanerozóico, exibindo superdimensionamento das eras e períodos sem nenhuma justificativa aparente, e ressaltando com freqüência, graficamente, a Era Cenozóica com distinto grau de importância, apesar desta apresentar o menor intervalo de tempo registrado na coluna geológica, aproximadamente 65 milhões de anos. A compreensão cognitiva do tempo geológico é complexa e os livros didáticos pouco ajudam seu aprendizado. As evidências fósseis são tomadas como decisivas para a compreensão do tempo geológico. Como parte do trabalho, foram analisadas entrevistas com crianças e adolescentes moradores de jazigos fossilíferos, a fim de compreender como as evidências que lhes são próximas possivelmente influenciaram as idéias que elaboravam sobre o passado do planeta. O trabalho termina discutindo implicações didáticas de diferentes perspectivas. / The analysis of the geologic column consulted from different didatic books hás made possible comprehend how the geologic time appears in the evolution teaching, as a discipline of the biology in the high school, and in the discipline of geography in the school focus in the origin and the transformation of the earth through the geologic era. It was possible to observe uncountable heterogeneous information, and didatic problems, revealing troubles of structural and cognitive order, which difficult teachers and students in the understanding of the deep time, introducing unordered and ommited events. It was highlighted the main steps of the construction of the geologic column as well as the characters involved: citing James Hutton, John Playfair, Charles Lyell, Charles Darwin. These were responsible by the changes of the cientific-filosofic thinking of the Europe during the XVIII and XIX, destroying the old pragmatism of the faith of a planet with 6000 years old. The temporal scales involved with the Pre-Cambrian mega interval, with 4.0 billion years or representing circa 85% of the geologic time, many times was presented graphically shorted or omitted in in the geologic columns revised. It has been detected too graphic troubles with the Eon Fanerozoic, showing over dimensioning of the era and periods without any real motive, and highligting frequently the Cenozoic Era with distinct degree of importance, however it has one of the shortest length in the geologic column, with about 65 million years. The cognitive comprehension of the geologic time is complex and the didatic books softly help your learning. The fossil evidence are considered decisive to the comprehension of the geologic time. As part of the work, it was analyzed some interviews with children and teenagers living near animals and plants fossils samples, to comprehend how the neighborhood evidence could had influence the ideas that made it about the planet past. The manuscript and discussing didatic implications, from different perspectives.

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