968 resultados para Guarani Indians.


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The Pirambóia Formation is a lithostratigraphic unit of the Paraná Basin, positioned between the Corumbataí (lower) and Botucatu (upper) Formations on the eastern edge of the basin. This unit is focused by many studies due to its great importance as an essential component in the Guarani Aquifer System (SAG) and the petroleum system “Irati-Pirambóia”, as excellent reservoirs. The Pirambóia Formation is historically the subject of several controversies on issues like age, contact relationships with the upper unit and depositional paleoenvironment. Despite these aspects, the Pirambóia Formation is commonly taken to be of Triassic age and is considered a product of wet aeolian systems, with plenty of wet interdunes and subordinate fluvial facies. In this work, by using techniques such as facies analysis, depositional architecture and facies association, facies of this unit were characterized and their depositional paleoenvironment was inferred particularly in Jundu Mining, region of Descalvado in northeastern São Paulo. Techniques such as grain size and petrographic analyses, aimed to characterize this unit as a potential reservoir rock. Five facies were described for the Pirambóia Formation in the studied region: St, Sh, Sm, Sr and Gt facies, generated by sedimentary processes of the bottom load type, mostly under low flow regime (with exception for the Sh facies, which is formed by upper flow regime processes). In addition to that, four facies associations were recognized from the architectural elements, primarily contained within the main channel: complex channel bars, composed by foreset macroforms (FM), sandy bedforms (SB) and gravel bars and bedforms (GB); flood deposits, constituted by laminated sand sheets (LS); deposits of hyperconcentrated flows and eolian deposits. It was interpreted that the Pirambóia Formation in Descalvado (SP) is the record of the sedimentation of braided rivers, with dunes and interdunes deposits...

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

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The term model refers to any representation of a real system. The use of models in Hydrogeology can be valuable predictive tools for management of groundwater resources. The numeric models of groundwater flow, object of this study, consist on a set of differential equations that describe the water flow in the porous medium. In this context, numeric simulations were made for a sub-basin located at Cara Preta farm – Santa Rita do Passa Quatro – SP. The aquifer at the local is composed by rocks of Pirambóia Formation, which is part of Guarani Aquifer System. It was developed a conceptual model from previous studies in the area, and from that, simulations were made through the software Visual Modflow®. The conceptual model established previously was considered consistent through the results of simulation.

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O objetivo deste trabalho é estudar a lírica tupi de Pe. José de Anchieta, discutindo a possibilidade de análise do acento da língua tupi antiga, via métrica adotada pelo autor em seus poemas. De toda a sua obra poética, 18 poemas foram escritos inteiramente em língua tupi, 10 deles servindo como corpus para esta pesquisa. Como aporte teórico para essa análise foi utilizada a Fonologia não-linear - mais precisamente a Teoria Métrica de Hayes (1995) - e um modelo de abordagem baseado em Massini-Cagliari (1995,1999 e aorientações na área) para com o português arcaico. As poesias em enfoque foram observadas em várias versões da obra disponíveis (Anchieta 1954, 1984, 2004). Para a base do estudo tupi, foram utilizadas as gramáticas de Anchieta (1933) e Lemos Barbosa (1956), além de livros e textos de Navarro (2006a, 2006b) e Ayron Rodrigues (1958)

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A existência de índios em cidades como São Paulo, Campo Grande, Manaus, Belém, dentre outras, cada vez se torna mais evidente, com implicações que provocam dificuldades sociais, econômicas, saúde dentre outros agravantes. Em função desta realidade, os órgãos públicos envolvidos na Política Nacional Indígena do Brasil reconhecem esta população como índios urbanos. É o que ocorre com as comunidades existentes na região metropolitana de São Paulo. Reconhece-se a existência de quatro aldeias indígenas, três delas é Tupi-Guarani e a outra é da etnia Pankararu. O presente trabalho surgiu da discussão das dificuldades de sobrevivência das comunidades indígenas da região metropolitana de São Paulo e da resolução de seus problemas de saúde. Para esta reflexão, foi preciso inserir o tema numa análise mais ampla da Política Nacional de Saúde Indígena como parte integrante da Política Nacional de Saúde brasileira. A partir dos questionamentos tecidos e discutidos temos como objetivo principal a saúde coletiva da população indígena no traçar de seu perfil epidemiológico e demográfico e a caracterização de sua vivência cotidiana e condição de saúde do índio urbano. Tomamos como procedimento metodológico o uso de fontes orais, uma que é capaz de traduzir com uma maior confiabilidade o cotidiano dos indivíduos e de sua comunidade... (Resumo completo, clicar acesso eletrônico abaixo)

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Pós-graduação em Relações Internacionais (UNESP - UNICAMP - PUC-SP) - FFC

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Pós-graduação em Agronomia - FEIS

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

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Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)

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Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)

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This paper deals with a reconstruction of the Benedictine missionary work in the Rio Branco valley (1909-1947), referenced to the relations established between the monks from the Monastery of São Bento do Rio de Janeiro and Macushi, people of Carib linguistic affiliation in the Guiana region. Such reconstitution reveals the tone of relations between the Indians and missionaries on the ritual production, seeking to interpret its possible meanings.

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The aim of this study is to investigate and analyze the conceptions of sexuality and female sexual behavior and conduct, formed from the merger of information and securities purchased under the eyes, rules and guidelines established relations with the Holy Office during his visit to Inquisitorial Brazil in the late sixteenth century. It is a survey of historical methodology in which we used as the exploratory research and literature. In the sixteenth century the Church increases the pressure to change the sexual mores that were free in the Middle Ages, a fact which influences the rules and regulations that are adopted by the Holy Office regarding the person's sex life. The first structure was based on Brazilian sexual alliance between Indians and settlers, which led to sugar, by the Portuguese, the customs of the land, which included sexual practices free since the Indians were out of Christian influence. Supported by the absence of white women, the settlers took them wives of the earth, usually more than one, creating conflict with the Jesuits who condemned Indian polygamy. In this context, in 1591, landed on Brazilian soil Heitor Furtado de Mendonca, and with it, the First Visitation of the Holy Office to investigate, arguing, exploring feelings and behaviors, to discover the true facts, finally, to demonstrate the errors Faith and punish them with the rigor of ecclesiastical law. His passing opens us to visualize traces of sexuality in the current "Tropic" a racist, misogynist world where black women and degraded land could be subject to the wishes of the white man, with whom he could mate at will. Alone and forgotten, women have not found the colony margin to denounce or to speak and were stigmatized by the look of travelers and writers have been through here.

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The presidency of Evo Morales, indigenous leader and who heads the party Movement Towards Socialism (MAS), opens a series of transformations in several dimensions. The changes in socio-economic and political power express the critic of long-term coloniality relations between a dominant white elite and an indigenous subordinate majority that deepens after national independence. Following this perspective, present in sectors of support to the government, the strategy of the MAS cannot follow the tradition of social revolutions that operated structural breaks in the mode of production and the state organization, but points to a new decolonizing revolution, cultural and political, articulating an indigenism of broad nature, flexible and open to popular social movements. This view is facing critics in sectors of the left that identify the renewal of capitalist modernization process initiated in 1952 under the leadership of the Nationalist Revolutionary Movement (MNR), extending citizenship and democratizing access to the state for recognition of Indians as such. From this perspective, the transformations proposed by MAS tend to favor a system restoration by diversifying its economic and social base. From the contrast provided by these two lines of interpretation, we intend to analyze the structural possibilities of the strategy of the government of Evo Morales, taking as historical reference the transformations wrought by the nationalist revolution of 1952 and the neoliberal reforms initiated in 1980.

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Radiogenic He-4 is produced by the decay of uranium and thorium in the Earths mantle and crust. From here, it is degassed to the atmosphere(1-5) and eventually escapes to space(1,5,6). Assuming that all of the He-4 produced is degassed, about 70% of the total He-4 degassed from Earth comes from the continental crust(2,-5,7). However, the outgoing flux of crustal He-4 has not been directly measured at the Earths surface(2) and the migration pathways are poorly understood(2-4,7,8). Here we present measurements of helium isotopes and the long-lived cosmogenic radio-isotope Kr-81 in the deep, continental-scale Guarani aquifer in Brazil and show that crustal He-4 reaches the atmosphere primarily by the surficial discharge of deep groundwater. We estimate that He-4 in Guarani groundwater discharge accounts for about 20% of the assumed global flux from continental crust, and that other large aquifers may account for about 33%. Old groundwater ages suggest that He-4 in the Guarani aquifer accumulates over half- to one-million-year timescales. We conclude that He-4 degassing from the continents is regulated by groundwater discharge, rather than episodic tectonic events, and suggest that the assumed steady state between crustal production and degassing of He-4, and its resulting atmospheric residence time, should be re-examined.