899 resultados para sub-tropical and tropical climates


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O Sambaqui do Moa é um sítio arqueológico localizado em Itaúna, Saquarema, litoral do Estado do Rio de Janeiro. Três momentos de ocupação foram reconhecidos neste sítio: o estrato 3 na base correspondente ao início da ocupação deste sítio; o 2, intermediário, aponta para uma ocupação mais intensa, com grande concentração de carapaças de moluscos, ossos de peixes e sepultamentos humanos; e o 1, o mais superficial, relacionado à última ocupação. Para identificar as condições ambientais de desenvolvimento do Sambaqui do Moa foram coletadas amostras de sedimentos e material zooarqueológico nestes três estratos. O material zooarqueológico está representado por restos microscópicos de peixes (ictiólitos), compostos por microdentes com diferentes morfologias: caninos, incisivos e molares. Os sedimentos segundo análises por DRX são constituídos além de quartzo e caulinita, calcita, aragonita e por fluorapatita. Este último é o principal mineral do material zooarqueológico, enquanto calcita e aragonita refletem os restos de conchas contidos neles, abundantes no sítio. As análises mineralógicas foram confirmadas pelas análises químicas, em que os teores elevados de P2O5, CaO e PF (H2O, CO2), respondem pela fluorapatita, calcita e aragonita. Modificações químicas representadas pelas variações nos conteúdos de C e P nos microdentes sugerem que estes experimentaram mineralização, num processo inicial de fossilização, pósdeposição. Os dados de isótopos estáveis 13C e 15N permitiram definir a fonte de matéria orgânica do sambaqui do Moa como marinha/salobra, em que a vegetação representava-se, predominantemente, por plantas do tipo C3 de floresta tropical. As razões 87Sr/86Sr nos ictiólitos confirmam que o ambiente no entorno do sambaqui tenha sido estuarino. A morfologia dentária permitiu reconhecer cinco famílias até então não registradas para o sítio, como Labridae, Serranidae, Ariidae, Erythrinidae e Characidae, que confirmam o ambiente estuarino. A idade do sambaqui do Moa por datação radiocarbono a partir dos sedimentos mostrou perturbação no estrato 2, ocasionando a inversão das idades entre os estratos o que pode ser justificado por processos de formação e/ou mudanças dos rios que modificaram as configurações geológico-geomorfológicas da área. Outra explicação poderia ser a interferência humana, devido ao grande número de enterramentos (mais de 30), tenha perturbado a ordem dos momentos de ocupação do sambaqui do Moa, além de possíveis processos erosivos. O sambaqui do Moa se instalou, portanto, em uma área de transição marinho-estuarina.

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The Pantanal is a Quaternary sedimentary basin located at the left margin of the Upper Paraguay River, west-central Brazil. Basin infilling was mainly by siliciclastic sediments and the stratigraphic succession exhibits an overall finingupward pattern. The depositional system tract is composed by a large meandering fluvial plain and several marginal alluvial fans, being the Taquari megafan the most striking feature. The present landscape is a complex tropical wetland, with geomorphic features derived from the present conditions and other inherited from successive Pleistocene and Holocene climates. During the Pleistocene, the sedimentary environment was dominated by braided alluvial fans, the original geometry of which is preserved as relict forms, permitting remarkable patterns of distributary paleochannels to be easily recognized in satellite images. Eolian processes were active in some abandoned lobes, contemporaneously with sedimentation in active fan lobes. Closed ponds bordered by lunette sand dunes, originally salt pans produced by eolian deflation, are relict eolian landforms in the Pantanal landscape. Eolian processes were probably more effective at the glacial maximum. Landscape has been changing in the Pantanal area since the end of the Pleistocene in adaptation to a more humid and warmer environment prevailing during Holocene. Initiation of the modern wetland has occurred during the Pleistocene / Holocene transition, with the change to a more humid climate and the individualization of lacustrine systems. The modern Pantanal wetland is a vast expanse of poorly drained lowlands that experiences annual flooding from summer to fall months. Although climatic fluctuations have occurred during all the Holocene, the alluvial fans have remained active depositional systems and lobes were formed by progradation and abandonment. Abandoned lobes were subjected... (Complete abstract click electronic address below)

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Pós-graduação em Biometria - IBB

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Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)

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Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

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Pós-graduação em Genética e Melhoramento Animal - FCAV

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Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)

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Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

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Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)

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Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)

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XML similarity evaluation has become a central issue in the database and information communities, its applications ranging over document clustering, version control, data integration and ranked retrieval. Various algorithms for comparing hierarchically structured data, XML documents in particular, have been proposed in the literature. Most of them make use of techniques for finding the edit distance between tree structures, XML documents being commonly modeled as Ordered Labeled Trees. Yet, a thorough investigation of current approaches led us to identify several similarity aspects, i.e., sub-tree related structural and semantic similarities, which are not sufficiently addressed while comparing XML documents. In this paper, we provide an integrated and fine-grained comparison framework to deal with both structural and semantic similarities in XML documents (detecting the occurrences and repetitions of structurally and semantically similar sub-trees), and to allow the end-user to adjust the comparison process according to her requirements. Our framework consists of four main modules for (i) discovering the structural commonalities between sub-trees, (ii) identifying sub-tree semantic resemblances, (iii) computing tree-based edit operations costs, and (iv) computing tree edit distance. Experimental results demonstrate higher comparison accuracy with respect to alternative methods, while timing experiments reflect the impact of semantic similarity on overall system performance.

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Global dengue virus spread in tropical and sub-tropical regions has become a major international public health concern. It is evident that DENV genetic diversity plays a significant role in the immunopathology of the disease and that the identification of polymorphisms associated with adaptive responses is important for vaccine development. The investigation of naturally occurring genomic variants may play an important role in the comprehension of different adaptive strategies used by these mutants to evade the human immune system. In order to elucidate this role we sequenced the complete polyprotein-coding region of thirty-three DENV-3 isolates to characterize variants circulating under high endemicity in the city of São José de Rio Preto, Brazil, during the onset of the 2006-07 epidemic. By inferring the evolutionary history on a local-scale and estimating rates of synonymous (dS) and nonsynonimous (dN) substitutions, we have documented at least two different introductions of DENV-3 into the city and detected 10 polymorphic codon sites under significant positive selection (dN/dS > 1) and 8 under significant purifying selection (dN/dS < 1). We found several polymorphic amino acid coding sites in the envelope (15), NS1 (17), NS2A (11), and NS5 (24) genes, which suggests that these genes may be experiencing relatively recent adaptive changes. Furthermore, some polymorphisms correlated with changes in the immunogenicity of several epitopes. Our study highlights the existence of significant and informative DENV variability at the spatio-temporal scale of an urban outbreak.