34 resultados para Linked-data


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Dissertation submitted in partial fulfilment of the requirements for the Degree of Master of Science in Geospatial Technologies

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Dissertação apresentada como requisito parcial para obtenção do grau de Mestre em Ciência e Sistemas de Informação Geográfica

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Dissertação apresentada na Faculdade de Ciências e Tecnologiea da Universidade Nova de Lisboa, para obtenção do Grau de Mestre em Engenharia Biomédica

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In this paper, a synopsis on the already known data, and the study of further specimens either new (*) or hither to undescribed are presented. The specimens dealt with have been collected at the Condeixa travertines; in the Tagus terraces near Carregado(*) and at Foz do Enxarrique(*); in the mousterian, about 31000 BP infilling from the Figueira Brava cave(*); and at Algar de Joao Ramos(*). Some specimens are ascribed to Elephas antiquus, the best represented form. Material from Figueira Brava cave and Algar de João Ramos is ascribed to Mammuthus primigenius, a species recognized here for the first time in Portugal.

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Dissertação apresentada na Faculdade de Ciências e Tecnologia da Universidade Nova de Lisboa para obtenção do grau de Mestre em Engenharia Electrotécnica e de Computadores

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The study of new abundant coral crops and a systematic revision of the historie collections allow us to extend significantly the data about the Upper Oligocene and Miocene Scleractinia of the French atlantic basins. The SW and W-NW France faunas have been considered, and complete lists of the different defined taxa are presented. The general lines of the evolution of this group are specified, and linked to the paleoclimatic and paleobiogeographic changes.

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The Mid Miocene marine formations of Salles area (former "Sallomacian" stage) have been studied again from numerous outcrops and cores. The deep structural framework influences notably of the characteristics and distribution of the deposits, which are neritic. The stratigraphy is stated precisely thanks to the planktonic fauna and floradetailed examination (probably Serravallian zones NN6 - N12). Several paleobiofacies are reconstituted from the rich invertebrate faunas, which give also paleoclimatic data.

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Climatic changes that affected the Northeastern Atlantic frontage are analyzed on the basis of the evolution of faunas and floras from the late Oligocene onwards. The study deals with calcareous nannoplankton, marine micro- and macrofaunas, some terrestrial vertebrates and vegetal assemblages. The climate, first tropical, underwent a progressive cooling (North-South thermic gradient). Notable climatic deteriorations (withdrawal towards the South or disappearance of taxa indicative of warm climate and appearance of "cold" taxa) are evidenced mainly during the Middle Miocene and the late Pliocene. Faunas and floras of modern pattern have regained, after the Pleistocene glaciations, a new climatic ranging of a temperate type in the northern part.

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The main goal of the present work is the use of mineralogical data corresponding to sediment fine fractions (silt and clay) of Quaternary littoral deposits for the definition of a more detailed vertical zonography and to discriminate the most significant morphoclimatic changes concerned with sediment source areas and sediment deposition areas. The analysis of the available mineralogical data reveals a vertical evolution of the mineral composition. The following aspects deserve particular reference: 1) fine fractions (<38 nm) are composed of quartz and phyllosilicates associated to feldspars, prevailing over other minerals; however in certain sections iron hydroxides and evaporitic minerals occur in significant amounts; 2) clay fractions (<2 nm) show a general prevalence of illite associated with kaolinite and oscillations, in relative terms, of kaolinite and illite contents. Qualitative and quantitative lateral and vertical variations of clay and non clay minerals allow the discrimination of sedimentary sequences and the establishment of the ritmicity and periodicity of the morphoclimatic Quaternary episodes that occurred in the Cortegaça and Maceda beaches. To each one of the sedimentary sequences corresponds, in a first stage, a littoral environment that increasingly became more continental. Climate would be mild to cold, sometimes with humidity - aridity oscillations. Warmer and moister episodes alternated with cooler and dryer ones.

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Eight depositional sequences (DS) delimited by regional disconformities had been recognized in the Miocene of Lisbon and Setúbal Peninsula areas. In the case of the western coast of the Setúbal Peninsula, outcrops consisting of Lower Burdigalian to Lower Tortonian sediments were studied. The stratigraphic zonography and the environmental considerations are mainly supported on data concerning to foraminifera, ostracoda, vertebrates and palynomorphs. The first mineralogical and geochemical data determined for Foz da Fonte, Penedo Sul and Penedo Norte sedimentary sequences are presented. These analytical data mainly correspond to the sediments' fine fractions. Mineralogical data are based on X-ray diffraction (XRD), carried out on both the less than 38 nm and 2 nm fractions. Qualitative and semi-quantitative determinations of clay and non-clay minerals were obtained for both fractions. The clay minerals assemblages complete the lithostratigraphic and paleoenvironmental data obtained by stratigraphic and palaeontological studies. Some palaeomagnetic and isotopic data are discussed and correlated with the mineralogical data. Multivariate data analysis (Principal Components Analysis) of the mineralogical data was carried out using both R-mode and Q-mode factor analysis.

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Dissertação apresentada para obtenção do grau de Doutor em Bioquímica,especialidade Bioquímica-Física, pela Universidade Nova de Lisboa, Faculdade de Cincias e Tecnologia

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Preliminary results of the systematic and biostratigraphical study of the ostracods from the Lower Toarcian (Polymorphum and Levisoni Zones) of Peniche are presented. Most of the identified species are recognized in other European countries. Biodiversity and species abundance are high in the first Zone, decreasing dramatically in the second one.

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Climatic reconstructions based on palynological data from Aquitaine outcrops emphasize an important degradation phase during the Lower Serravallian. Climatic and environmental changes can be related to sea-level variations (Bur 5 / Lan 1, Lan 2 / Ser 1 and Ser 2 cycles). Transgressive phases feature warmer conditions and more open environments whereas regressive phases are marked by a cooler climate and an extent of the forest cover. From Langhian to Middle Serravallian, a general cooling is highlighted, with disappearance of most megathermic taxa and a transition from warm and dry climate to warm-temperate and much more humid conditions. Conclusions are consistent with studies on bordering areas and place the major degradation phase around 14 My. The palynologic data allow filling a gap in the climatic evolution of Southern France, as a connection between Lower and Upper Miocene, both well recorded. These results document, on Western Europe scale, latitudinal climatic gradient across Northern hemisphere while featuring a transition between Mediterranean area and northeastern Atlantic frontage.

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RESUMO: As infecções virais podem contribuir para o desenvolvimento do cancro, estando vários tumores malignos associados aos Herpesvirus (HHV). O vírus de Epstein-Barr (EBV) e o Herpesvirus 8, dois Herpesvirus, foram reconhecidos como agentes etiológicos de várias neoplasias. O astrocitoma pilocítico do cerebelo é um dos tumores cerebrais mais frequentes na criança, adolescentes e jovens adultos e a proliferação astrocitária ocorre geralmente após vários tipos de agressão, nomeadamente a infecção viral. Para investigar esta eventual interligação, estudámos 35 astrocitomas pilocíticos, pesquisando a presença dos 8 Herpesvirus. Neste estudo, foram utilizadas 10 amostras de biópsias do cerebelo de doentes que faleceram por doenças não relacionadas com infecção ou patologia tumoral. A maioria dos astrocitomas (33) eram tumores de baixa malignidade. As amostras foram analisadas por PCR (Polymerase Chain Reaction) quantitativa em tempo real (qPCR), com amplificação do gene da DNA polimerase viral. Treze astrocitomas e 7 controles revelaram pequenas quantidades de DNA viral (1-100 cópias/100ng DNA) de todos os Herpesvirus, com excepção do HHV6 A e B que estava ausente nas amostras. O EBV foi identificado em 9 dos 35 astrocitomas (26%) e em 7 dos 10 controles (70%) estando muito mais presente nos controles. As amostras positivas para o EBV foram também analisadas por imunohistoquímica, não tendo sido imunoreactivas para os anticorpos utilizados. A PCR com CODEHOP (consensus-degenerated hybrid oligonucleotide primers) foi utilizada para investigar a presença de um eventual Herpesvirus novo nestas amostras. Não foi identificada nenhuma sequência indicativa de um novo HHV por este método. 24. Em conclusão, os dados apontam para a presença de Herpesvirus, com particular relevância para o EBV, em tecido de cerebelo normal e em tumores cerebrais, embora em níveis demasiado baixos para poderem ser responsabilizados pela indução tumoral. A presença de sequências de DNA de Herpesvirus, nomeadamente do EBV, no Sistema Nervoso Central vem enriquecer a discussão sobre o significado da infecção viral na oncogénese humana, particularmente na neuro-oncogénese. ABSTRACT: Viral infections can contribute to the development of human cancer. Several human malignancies are linked with Human Herpesviruses (HHVs). Epstein-Barr virus and HHV8, two hHerpesvirus, have been recognized as etiologic agents of several neoplasms. Pilocytic astrocytoma of the cerebellum is one of the most common brain tumour in children, adolescents and young adults and astrocytary proliferation generally occurs after several types of injury, namely viral infection. To further explore this association, we have searched the tissue from 35 pilocytic astrocytoma, for all the 8 HHV. In this study, ten brain biopsies (cerebellum) from patients who died of unrelated diseases were used as controls. Most of the astrocytomas (33) were of low grade malignity. Samples were assessed by Real-time quantitative Polymerase Chain Reaction (q PCR) amplification of viral DNA polymerase gene. Thirteen astrocytoma and 7 controls showed low viral DNA levels (1-100 copies/100ng DNA) for all HHVs, with the exception of HHV6 that was absent. EBV was identified in 9 of the 35 astrocytoma (26 %) and in 7 of the 10 controls (70%) being more present in controls. EBV positive samples were also assessed by Immunohistochemistry (IHC) but none showed immunoreactivity for the antibodies used. PCR with consensus-degenerated hybrid oligonucleotide primers (CODEHOP) were also used to look for novel HHVs in these samples and no sequence indicative of a new HHV was detected. 26 Altogether the data indicate the presence of HHVs, with relevance for EBV in normal cerebellum tissue and also in brain tumours but at too low levels to be considered responsible for tumour induction. The presence of HHV DNA sequences, particularly EBV, in the studied brain tumours and control samples, further enriches the discussion about the relevance of viral infection in human oncogenesis, particularly neuro-oncogenesis.RÉSUMÉ: Les infections virales peuvent contribuer au développement du cancer. Les vírus de type Herpès sont associés à plusieurs néoplasies. Il est par exemple établi que les vírus Epstein-Barr et « human Herpesvirus 8 » (HHV-8) sont responsables de plusieurs tumeurs malignes. L´astrocytome pilocitique du cervelet est l’une des tumeurs les plus fréquentes chez les enfants, adolescents et adultes jeunes. En général la prolifération des astrocytes se produit en réponse à une agression. Posant l’hypothèse d’une agression d’origine virale, nous avons recherché la présence des 8 vírus Herpès dans les tissus de 35 astrocytomes. Dans cette étude, 10 échantillons de biopsie de cervelet de patients décédés suite à d’autres pathologies, ont été utilisés comme contrôles. La majorité des astrocytomes étaient de très basse malignité. Les échantillons ont été étudiés par PCR quantitative en temps réel, en amplifiant le gène de l’ADN-polymérase virale. Treize astrocytomes sur 35 (37%) et 7 contrôles sur 10 (70%) ont été trouvés positifs pour tous les HHV sauf l´HHV6, toujours avec un nombre de copies de polymérase virale bas (< 100 copies/100 ng d’ADN). Notamment l’EBV a été identifié 7 fois dans les contrôles (70%) et 9 fois dans les astrocytomes (26%). Les échantillons positifs pour l`EBV ont aussi été étudiés par immuno-histochimie. Aucun signal n’a été observé avec les anticorps utilisés. Enfin, une technique de PCR avec oligonucléotides dégénérés (CODEHOP ou consensus degenerated hybrid oligonucleotide primers) a été utilisée pour rechercher la présence d´un éventuel nouveau vírus Herpès dans les échantillons d’astrocytome. Aucun nouveau vírus n’a été identifié. 28 En résumé, nous avons établi la présence de vírus Herpès, en particulier l´EBV, dans le cervelet normal et dans les tumeurs du cerveau. Les quantités d’ADN viral retrouvées sont faibles et ne permettent pas d’attribuer à ces vírus la responsabilité de l’induction des tumeurs. Cependant, la présence d’ADN de vírus Herpès dans le cerveau sain ou pathologique vient enrichir la discussion sur le signification de l´infection virale dans les processus d´oncogenèse en général, et dans la neuroonco-genèse en particulier.

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Trabalho apresentado no âmbito do Mestrado em Engenharia Informática, como requisito parcial para obtenção do grau de Mestre em Engenharia Informática.