Distribuição ambiental e temporal das comunidades de macroalgas de riachos da Serra da Prata, Estado do Paraná, Sul do Brasil

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

Efeitos da previdência rural na agricultura familiar da microrregião Serra de São Miguel - RN

The objective of the present work is to verify the effects of Rural Social welfare in the family agriculture of the microrregião Serra de São Miguel-RN. The study based on available bibliography on the theme, in secondary data and in a rising amostral accomplished in three municipal districts (Encanto, São Miguel and Riacho de Santana) of the microrregião. The universe of the study was the establishments of the family agriculture appeared in the Agricultural Census of 2006, in those municipal districts. The unit of considered analysis was the rural family, with the interviews being applied close to the farmers' families with and without retired rural. The sample was of 94 present families in the family establishments. The results demonstrate that the Rural Precaution reaches a significant covering degree in the rural area of the researched municipal districts, with an average of 1,57 beneficiaries for home in the families with retired. The data of the research attest that the family agriculture in the microrregião Serra de São Miguel-RN it has few favorable conditions for his/her development, once, besides the shortage of lands and of the climatic factor of the area, the returned public politics the family farmers' totality - like PRONAF and PAA -, it has been unable to give effective answers for the improvement of the life conditions in the rural way, have seen the minimum amount of families reached by those politics, be in function of the drawing or of the atmosphere where they are done. In this context, he/she stands out the importance of the Rural Precaution that, in function of the application of the constitutional devices that you/they guaranteed his/her universalization, it has been the only relevant public politics that, in fact, it has been reaching her/it all their beneficiary potentials. Given the general situation of the family agriculture of the microrregião and of the specific characteristics of the researched family establishments, the hypothesis was corroborated that the rural retirement doesn't contribute directly to the increase / making possible of the family agriculture. In spite of 57,4% of the families with retired have declared to use resources of the retirement in the costing of the rural activity carried out by the family, the annual medium value of the expense just located around 7,02% of the annual value of the retirements gained by the families in the year of 2010. Data the low levels in that the social reproduction of the great majority of the family establishments of the microrregião, the maintenance of the families is operated represents the main destiny of the resources precautions. It was also confirmed the hypothesis that the Rural Precaution constitutes the main monetary contribution of the families with retired. For more than 93% of the families with retired, the retirements doing 50% or more of the total of the family monetary income, and in the composition of the rural income of the families with retired and pensioners, the originating from income the rural retirements are equal to 65,24% of the total of the annual income obtained by the families. It is ended, because, that the rural precaution, given to the adversities for the development of the family agriculture, of the operational inefficacy of the public politics and of the few opportunities of generation of existent income in the local savings, it is the main responsible for the reduction of the poverty and, consequently, for the improvements of the conditions of life of the families of and with seniors in the rural way of the microrregião Serra de São Miguel-RN

Dinâmica Costeira dos Campos petrolíferos Macau/Serra, litoral setentrional do Estado do Rio Grande do Norte

This thesis describes the general behavior of the northern shore of the State of Rio Grande do Norte relating beach profile morphology with hydrodynamic and sedimentological parameters. The Macau and Serra Oil Field are inserted on this area and are under accelerated coastal erosion. At these oil fields are installed oil wells from PETROBRAS, nowadays located directly in the shoreline, under constant attacks of coastal processes (e.g. waves, tides and currents), which promote an intense morphodynamic variability of this sandy coast. The area was monitored for 24 months in three different stations (P01, P02 and P03). The methodology applied involved current techniques of beach profiles, hydrodynamical processes, remote sensing and geophysics. A synthesis of results obtained through the use of different time scales (monthly, lunar cycle, seasonal, annual) from a coastal dynamics study is presented. The average wind direction corresponded to 77ºAz (NE). The steepness of the berm and of the shoreface, as well as coastal current direction, do not present major changes, with an average of 36º for the steepness of the berm, 15º for the shoreface and 15º for the coastal current direction. This data set allows us to infer that the months of larger coastal erosion were November/2000 and April/2001, because of the largest wave parameter during this time. The months of worse coastal erosion in this area are related with the increasing wavy energy. This in turn, seems to be related to seasonal climatic variations, with the wave energy and tide currents speed increasing during months of minor precipitations (June to January). The months of worse coastal erosion were September and November, when the largest wave parameters and speed currents are measured in the area. Since these months are included on the period of minor precipitations, we related the coastal erosion to seasonal climatic variations. The results obtained during these 24 months of monitoring confirms a situation of accentuated erosion, mainly in Profile 03 (Barra do Corta-Cachorro), where the wave height, period, and coastal current speed are always larger than the values found in Profile 02 (Macau5). Probably these values are more expressive in Profile 03, because it does not present any natural structure of protection against the wave impacts, as the barrier island located at Ponta do Tubarão, or the sand banks in front of Macau5. The transport of the sediments occurs from East to West, and the sand accumulation is more pronounced on Profile 03 intertidal zone, where there are embrionary dunes in dryer months. The tidal currents speed, on the other hand, is more accentuated in the Macau5 area (Profile 02). At Ponta do Tubarão, the tidal currents presented a preferential direction for NE, at times of flood, currents and for NW, at times of ebb current; at Barra do Corta-Cachorro the direction of the currents were predominantly for NW, independent of the tide phase, coinciding with the preferential direction of the longshore current. This currents inversion at Ponta do Tubarão is attributed to the presence of the Ponta do Tubarão island barrier and by the communication channel of the lagoon with the sea. The tide currents are better observed in protected areas, as in the Ponta do Tubarão, when they present inversion in their direction accordingly to the flood and ebb tide. In open areas, as in Barra do Corta-Cachorro, the tide currents are overprinted by the longshore currents. Sediment analysis does not show important modifications in grain size related to seasonality (dry- and rainy seasons). On the foreshore and backshore zones, the sediments vary from fine to medium sand, while in the shoreface they very from fine to very sands. The grains are mostly spheres, varying from sub rounded to sub angled. Quartz is the main component alongside Feldspat and heavy minerals as accessory components. Biogenic content is also present and mainly represented by mollusks fragments. The calculated sediment transport show values around 100 m3/day. The morphodynamic studies indicated that this is a reflexive area from October to April, and intermediate from May to September. The Relative Tide Range-RTR for this area is 4 < RTR < 15, and so classified in the mixed wave-tide group. Having this exposed we can affirm that the more active natural factors in this area are the currents, followed by the tides and the winds. The anthropic factors are exclusively local and punctual (Macau and Serra Oil Field). Taking in account the economic importance of the area, as well as the intensity of coastal processes acting on this shore, it is important a continuity of the monthly environmental monitoring looking for variations on longer-period cycles. These data have been stored on the geo-referenced database of the projects MARPETRO and PETRORISCO (REDE 05), aiming to model the coastal and sea environment, susceptible to oil spills and their derivatives

Estudos sedimentológicos e o contexto estrutural da formação Serra do Martins, nos platôs de Portalegre, Martins e Santana/RN

This dissertation deals with sedimentological and structural framework of the siliciclastic rock of the Serra do Martins Formation (FSM) in the Portalegre, Martins and Santana plateau, located to the south of Potiguar Basin, in the southwest and central Rio Grande do Norte state. This formation, regarded as of Oligo-Miocene age based on intrusive relations of the Miocene Macau volcanics, has a still disputable age due to the lack of appropriate bio and/or chronostratigraphic markers. The FSSM deposits crop out along 650 to 750 m high plateau, as a remanescent sedimentary cover directly overlying topographically uplifted pre-cambrian crystalline rocks. During the last decades, these deposits were interpreted according to a Tertiary paleoclimatic evolutionary model, associated to pedogenetic processes. The sedimentological characterization of the FSM was done through a detailed study of its facies, petrography and diagenetic features. The facies study was based on description of field relations, textures and structures, the piling up of the strata and their lateral variations. The FSM was deposited by an anastomosing to coarse-meandering fluvial system, including deposits of lag, cannel-fill, ouver-bank and flood plain. The petrographic composition of the sediments, coupled to their facies and paleocurrent directions, suggest a rather distal sourcearea, to the south of the present plateau. The diagenetic study identified an incipient grain mechanical compaction, pronounced dissolution of the framework, matrix and/or cement components, intense precipitation of kaolinite, silic and, eventually, iron oxides, besides mechanical infiltration of the clays. Most of these events, regarded in the literature as associated to near-surface conditions (eo or telodiagenesis), indicate the FSM sediments were never deeply buried. Topographic relations along longitudinal and transversal sections reaching the Potiguar Basin to the north identified regional dips that allow to discuss stratigraphic correlations between the FSM and the basin formations. The sedimentological features of the different units and the intrusive relations of the Macau volcanics were also considered in these correlations,which support the Oligo-Miocene age previously accepted for the FSM. Concerning the tectonic framework of the FSM, this work investigated the pre-cambrian to cretaceous heritage and the cenozoic deformation, allowing the recognition of pre-, sin and post-FSM structures. The crystalline basement, belonging to the Seridó Belt, displays NE and WNW foliation trends related to the Brasiliano-age ductile shear zones. In this terrain, brittle-ductile and brittle NE- and NW-trending structures, associated with extensional joints filled with pegmatites and quartz veins, are related to an E-W compression by the end of Brasiliano Cycle. The E-W joints and NE-trending fractures were reactivated by N-S to N-S to NW extension during late Jurassic to Cretaceous times, controlling the emplacement of the Rio Ceará-Mirim basic dyke swarm and the opening of the Potiguar rift basin

Vascular flora of Serra do Japi Biological Reserve, Jundiaí, southeastern Brazil

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

Estratigrafia de seqüências das formações Serra Alta, Teresina e Rio do Rasto (permiano, Bacia do Paraná) na porção nordeste do Paraná e centro-sul de São Paulo

Pós-graduação em Geologia Regional - IGCE

Diversidade e distribuição dos anfíbios anuros do núcleo Curucutu, Parque Estadual da Serra do Mar, SP

Pós-graduação em Ciências Biológicas (Zoologia) - IBRC

Estrutura da comunidade de anfíbios do Parque Nacional da Serra da Bocaina, São Paulo, Brasil

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

Políticas públicas, turismo e unidades de conservação municipais: uma experiência em Cancão, Serra do Navio, Amapá

Versa sobre a problemática das políticas públicas de turismo e meio ambiente, enfocando a discussão acerca das categorias novas de estudo que são as Unidades de Conservação municipais – UCM, tratando sobre o Parque Natural Municipal do Cancão, além de destacar uma breve análise sobre a questão sociocultural da cidade, que foi uma das primeiras cidades-empresa de exploração mineral na Amazônia. O objetivo desta pesquisa é o de analisar a dinâmica do turismo e da gestão ambiental, centrada nas UCM, no município de Serra do Navio, enfatizando também como está sendo trata a questão sociocultural na cidade, a partir de um contexto de que esta antes era uma empresa. A metodologia do trabalho compôs-se de pesquisa bibliográfica e documental em Belém/PA e Macapá/AP; pesquisa de campo na cidade de Serra do Navio, utilizando-se de entrevistas e questionários, com o poder público municipal e estadual, setor privado, e a comunidade em geral, fazendo também, registro visual dos residentes e da localidade, por fim a análise dos dados, quantitativos e qualitativos, a partir da coleta de campo. Os resultados preliminares apontam que o turismo, está aos poucos, se inserindo no município, sendo fomentado pelo governo estadual e também municipal, e que a questão ambiental é um tema significativo para a cidade, já que está possui um dos primeiros espaços com característica de UCM do norte do Brasil, e por fim, que a sociedade serrana ainda guarda uma memória grande acerca da vivencia da antiga empresa mineradora Indústria e Comercio de Mineração – ICOMI.

De como a raposa encontrou a serra do sol: discurso, memória e identidades

Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)

Atividade sazonal e uso do ambiente por anfíbios da Mata Atlântica no alto da Serra do Mar

Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)

Biologia e ciclo de vida de Astyanax cf. scabripinnis paranae Eigenmann, 1914 (Characidae, Tetragonopterinae), no Ribeirão Grande, Parque Estadual da Serra do Mar, núcleo Santa Virginia, SP

Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)

O caminho novo: o Vale Histórico da Serra da Bocaina - opulência e decadência da sub-região paraibana paulista (reintegração de um espaço geográfico 'deprimido')

A pesquisa resgata o trecho paulista do “Caminho Novo”, antiga estrada geral de São Paulo, ligação terrestre com o Rio de Janeiro, a partir do século XVIII. No chamado Vale Histórico da Serra da Bocaina, cujo relevo se apresenta muito movimentado, a cultura do café penetrou em território paulista. Esta sub-região do Vale do Paraíba tornou-se uma das mais prósperas do país. A fase posterior, de queda na produção cafeeira, transformou-a numa região “deprimida” e estagnada. Atualmente, existem esforços para, através dos diversos ramos do turismo, reativar e dinamizar esta região vale-paraibana paulista, de modo a reintegrá-la ao pujante sistema econômico de São Paulo.

Composição e estrutura arbórea em floresta estacional semidecidual no Espinhaço Meridional (Serra do Cipó, MG)

Estudos florísticos e fitossociológicos têm sido feitos em áreas de Mata Atlântica, sendo parte desses em remanescentes de Floresta Estacional Semidecidual. Entretanto, no cômputo geral, as florestas na Serra do Espinhaço têm sido pouco estudadas. Este trabalho objetiva descrever e analisar a composição e estrutura de espécies arbóreas de uma área de Floresta Estacional Semidecidual na face leste da Serra do Cipó, porção meridional da Serra do Espinhaço (MG). O método de ponto-quadrante foi utilizado para estudo fitossociológico, sendo o levantamento florístico total incrementado por coletas não-sistematizadas. Foram calculados: área basal total, densidade, frequência e dominância relativas, além do índice de valor de importância. O levantamento florístico total registrou 280 espécies, número que destaca a riqueza da área, cuja maior afinidade florística é com outras áreas florestais localizadas nas bacias dos Rios Doce e Paraíba do Sul. Os parâmetros fitossociológicos destacam a predominância de espécies pioneiras e secundárias iniciais, o que, assim como os valores estruturais, caracteriza um estádio secundário inicial a intermediário de regeneração. Os dados deste trabalho realçam a importância da preservação das florestas estacionais da Mata Atlântica e, particularmente, de áreas florestais na porção leste do Espinhaço.

Estudo das propriedades físico-químicas do queijo Serra da Estrela

O objetivo deste trabalho foi avaliar as características físicas e químicas de queijo Serra da Estrela de pasta semi mole e correlacionar estes resultados com os resultados da análise sensorial. Foram alvo de estudo 29 amostras de queijo Serra da Estrela produzidas com 6 ecótipos de cardo diferentes. Os queijos foram produzidos em várias queijarias da região demarcada para a produção do queijo Serra da Estrela, mais propriamente dos concelhos de Penalva do Castelo, Oliveira do Hospital e Fornos de Algodres. Procedeu-se à avaliação das propriedades químicas como a humidade, o pH, cloretos, cinzas e proteínas, de propriedades físicas, como a textura e a cor e uma avaliação sensorial. Dos resultados obtidos foi possível verificar que os valores da humidade variaram entre 34, 9% e 49,8%. As cinzas e a proteína encontram-se abaixo dos valores na literatura (3,4%–5,5% e 13,0%–21,9%, respetivamente). Os cloretos variaram entre 1,1% e 3,0% e o pH entre 4,8 e 5,7. Verificou-se que com mais dias de maturação, e portanto menor humidade, as amostras apresentam, maior firmeza, menos adesividade e menos pegamento da pasta. Os valores da dureza da casca e da pasta variam entre 1,56N e 9,40N e 0,4 N e 3,4 N, respetivamente. A adesividade é bastante elevada (de -26,29 N.sec a -2,21 N.sec), o que traduz o caráter amanteigado destes queijos. Nas coordenadas de cor os valores de L* variaram entre 53,57 a 64,34, os de a* entre -4,53 e 1,29 e os de b* entre 15,56 e 29,03, revelando uma cor amarelada. Os resultados da análise sensorial não apresentam grande variabilidade entre os diferentes ecótipos e verificou-se que, em geral, as análises instrumentais realizadas acabaram por confirmar a percepção dos provadores.