Desenvolvimento regional: um debate sobre as políticas industriais no Rio Grande do Norte

The discussion of economic development emphasizes the emergence of a gradual change of economic structure, which would rise from an agrarian to the industrial stage, and later with a predominant tertiary sector. However, the high Brazilian regional inequality resulted in the coexistence of modern spaces and other arrears. Such disparities are visible not only in economics, but spatial, social and environmental. Although Brazil has gone through changes in the production structure and the location of these activities, space - territorial disparities manifest themselves in a high level of regional heterogeneity. In this context, the Northeast emerged as a region that has historically been characterized by socioeconomic backwardness and the presence of the worst indicators of inequality. The presence of these indicators showing the socioeconomic backwardness of the other fronts region contributes to the priority of action aimed at reverting this regional disparity public policy. The historical account of the development policies of regional studies shows that the state played a pivotal role in ensuring regional planning. Besides the creation of development agencies such as the Northeast Sudene, tax and financial incentives have been widely used strategies in the region to foster greater national integration. However, the use of incentives is much discussed in view of the possible advantages and disadvantages brought by its use. Thus, this study aims to build a theoretical framework tool for building effective public policies for industrialization in the Northeast, specifically in Rio Grande do Norte.

Análise da dinâmica deposicional das praias de Cacimbinha e do Madeiro, Tibau do Sul-RN, Brasil

The Cacimbinha and Madeiro beaches are located in the eastern coast of Rio Grande do Norte state, in the municipality of Tibau do Sul. Given the indicative of erosion in the coast of this district and the coastal processes acting on the beaches, the global aim of this project is comprehend the evolution of depositional environment on the Cacimbinha beach, moreover, the project seeks to characterize deposits from the Cacimbinha and Madeiro beaches, according to the geomorphologic compartments identified on these beaches; distinguish the coastal features which possibly interact with the Cacimbinha beach; identify the potential relationship between the sediments from the coastal features and the deposits from Cacimbinha beach; understand which depositional processes that prevail at each facies deposited on the beach; and identify the probable sedimentary environments and its energy of deposition through of the materials recorded on the Cacimbinha beach. This study was based on previous bibliographic and field research, both guided by academic works, laws, concepts and theories concerning the physical geography, geomorphology of the quaternary, sedimentary geology and stratigraphy. Thus, the methodology was divided in three steps: Prefield step: office work was performed; Field step: Sampling of facies of sedimentation; PosField step: analysis and integration of data obtained during the research period. Thus, the results showed deposicional facies with distinguished energy in the relief compartments, beach and terrace. After the sedimentary analysis and its interpretation linked to the architecture of the mounted sections based on drilling, it became possible to trace the evolutionary history of this stretch of beach. Therefore, it can be stated that studies performed on coastal areas are of great importance, as long as, around the world, the most part of urban zones are seated on deposits of quaternary age and, then this work improve the knowledge regarding the sedimentary dynamics of this beach, becoming scientific support for management and planning of this area which focus on, mainly, the foreign tourism

A relevância dos eventos culturais para a economia criativa - pesquisa qualitativa na Praia da Pipa, Tibau do Sul/RN

Creative industry has promoted and strengthened the growth of various economic sectors in Brazil and abroad, thus stimulating the local economy in places with attractive and innovative sceneries for the consumer market. This essay focuses on studying the relevance of cultural events for the creative economy, and these may contribute to the social, cultural and economic development in Pipa, located in Rio Grande do Norte (Brazil). Cultural events promote a themed and creative environment which has worked as attraction mechanism for the increase of cultural, gastronomic and social leisure consumptions. Cultural and thematic events has been held in Pipa, such as Festival Literário da Pipa, Fest Bossa & Jazz da Pipa, Festival Literário Alternativo da Pipa and Festival Gastronômico da Pipa, which can attract the local, state, national and international audience. The research is characterized as a qualitative research about the problem approach. The field research is characterized by the ethnographic approach, using the techniques of participant observation, semi-structured interviews and photographic record. With the research results, we can point that Pipa promotes cultural events that move the economic dynamics, social and cultural, inserting new cultural habits in this urban space, and in some cases, rescuing the history of the place. In each event, the economic and political forces connect themselves to promote the infrastructure of these events, supporting the provision of services and products from the creative and cultural sectors. The theming of the studied events plunges the audience into stories that may have (or not) a connection to the local history. Therefore, it is perceived that this work brings the light to a place that presents itself as the protagonist of the state of Rio Grande do Norte in terms of renewal and economic, social and cultural change in its infrastructure and its potential for tourist attraction from the creative and cultural sectors.

Estudo do balanço de umidade por meio de modelos regionais para o clima do passado e do futuro sobre a América do Sul

In the context of climate change over South America (SA) has been observed that the combination of high temperatures and rain more temperatures less rainfall, cause different impacts such as extreme precipitation events, favorable conditions for fires and droughts. As a result, these regions face growing threat of water shortage, local or generalized. Thus, the water availability in Brazil depends largely on the weather and its variations in different time scales. In this sense, the main objective of this research is to study the moisture budget through regional climate models (RCM) from Project Regional Climate Change Assessments for La Plata Basin (CLARIS-LPB) and combine these RCM through two statistical techniques in an attempt to improve prediction on three areas of AS: Amazon (AMZ), Northeast Brazil (NEB) and the Plata Basin (LPB) in past climates (1961-1990) and future (2071-2100). The moisture transport on AS was investigated through the moisture fluxes vertically integrated. The main results showed that the average fluxes of water vapor in the tropics (AMZ and NEB) are higher across the eastern and northern edges, thus indicating that the contributions of the trade winds of the North Atlantic and South are equally important for the entry moisture during the months of JJA and DJF. This configuration was observed in all the models and climates. In comparison climates, it was found that the convergence of the flow of moisture in the past weather was smaller in the future in various regions and seasons. Similarly, the majority of the SPC simulates the future climate, reduced precipitation in tropical regions (AMZ and NEB), and an increase in the LPB region. The second phase of this research was to carry out combination of RCM in more accurately predict precipitation, through the multiple regression techniques for components Main (C.RPC) and convex combination (C.EQM), and then analyze and compare combinations of RCM (ensemble). The results indicated that the combination was better in RPC represent precipitation observed in both climates. Since, in addition to showing values be close to those observed, the technique obtained coefficient of correlation of moderate to strong magnitude in almost every month in different climates and regions, also lower dispersion of data (RMSE). A significant advantage of the combination of methods was the ability to capture extreme events (outliers) for the study regions. In general, it was observed that the wet C.EQM captures more extreme, while C.RPC can capture more extreme dry climates and in the three regions studied.

Evolução dos sistemas de falhas de borda do Rifte Potiguar com base em curvas de crescimento de falhas

The discussion about rift evolution in the Brazilian Equatorial margin during the South America-Africa breakup in the Jurassic/Cretaceous has been focused in many researches. But rift evolution based on development and growth of faults has not been well explored. In this sense, we investigated the Cretaceous Potiguar Basin in the Equatorial margin of Brazil to understand the geometry of major faults and the influence of crustal heterogeneity and preexisting structural fabric in the evolution of the basin internal architecture. Previous studies pointed out that the rift is an asymmetrical half-graben elongated along the NE-SW direction. We used 2D seismic, well logs and 3D gravity modeling to analyze four major border fault segments and determine their maximum displacement (Dmax) and length (L) ratio in the Potiguar Rift. We constrained the 3D gravity modeling with well data and the interpretation of seismic sections. The difference of the fault displacement measured in the gravity model is in the order of 10% compared to seismic and well data. The fault-growth curves allowed us to divide the faulted rift border into four main fault segments, which provide roughly similar Dmax/L ratios. Fault-growth curves suggest that a regional uniform tectonic mechanism influenced growth of the rift fault segments. The variation of the displacements along the fault segments indicates that the fault segments were formed independently during rift initiation and were linked by hard and soft linkages. The latter formed relay ramps. In the interconnection zones the Dmax/L ratios are highest due to interference of fault segment motions. We divided the evolution of the Potiguar Rift into five stages based on these ratios and correlated them with the major tectonic stages of the breakup between South America and Africa in Early Cretaceous.

Evolução dos sistemas de falhas de borda do Rifte Potiguar com base em curvas de crescimento de falhas

The discussion about rift evolution in the Brazilian Equatorial margin during the South America-Africa breakup in the Jurassic/Cretaceous has been focused in many researches. But rift evolution based on development and growth of faults has not been well explored. In this sense, we investigated the Cretaceous Potiguar Basin in the Equatorial margin of Brazil to understand the geometry of major faults and the influence of crustal heterogeneity and preexisting structural fabric in the evolution of the basin internal architecture. Previous studies pointed out that the rift is an asymmetrical half-graben elongated along the NE-SW direction. We used 2D seismic, well logs and 3D gravity modeling to analyze four major border fault segments and determine their maximum displacement (Dmax) and length (L) ratio in the Potiguar Rift. We constrained the 3D gravity modeling with well data and the interpretation of seismic sections. The difference of the fault displacement measured in the gravity model is in the order of 10% compared to seismic and well data. The fault-growth curves allowed us to divide the faulted rift border into four main fault segments, which provide roughly similar Dmax/L ratios. Fault-growth curves suggest that a regional uniform tectonic mechanism influenced growth of the rift fault segments. The variation of the displacements along the fault segments indicates that the fault segments were formed independently during rift initiation and were linked by hard and soft linkages. The latter formed relay ramps. In the interconnection zones the Dmax/L ratios are highest due to interference of fault segment motions. We divided the evolution of the Potiguar Rift into five stages based on these ratios and correlated them with the major tectonic stages of the breakup between South America and Africa in Early Cretaceous.

Evolução morfotectônica da porção centro-sul da Bacia Paraíba

Recent endogenous processes provide dynamic movements in the lithosphere and generate the varied forms of relief, even in areas of passive continental margins, such as the research area of this work located in northeastern Brazil. The reactivation of Precambrian basement structures, after the breakup between South America and Africa in the Cretaceous played an important role in the evolution of basins, which provided generated forms of relief. These morphodynamic characteristics can be easily observed in marginal basins that exhibit strong evidence fault reactivations. The purpose of this study is to investigate the influence of morphotectonic processes in the landscape structuring of Paraíba Basin. Therefore, we used aeromagnetic, high–resolution images of the Shuttle Radar Topographic Mission–SRTM, structural geological data, deep well data and geological field data. Based on the results of the data was observed that some preexisting structures in the crystalline basement coincide with magnetic and topographic lineaments interpreted as fault reactivation of the Post–Miocene units in the Paraíba Basin. Faults that offset lithostratigraphic units provided evidence that tectonic activity associated with the deposition and erosion in the Paraíba Basin occurred from Cretaceous to the Quaternary. The neotectonic activity that occurred in Paraíba Basin was able to influence the deposition of sedimentary units and landforms. It indicates that the deposition of post–Cretaceous units was influenced by reactivation of Precambrian basement structures in this part of the Brazilian continental margin.

Crisis Económica en África Occidental: el caso de Dakar, 1929-1939

En este artículo se explora el impacto socio-económico de la crisis internacional de 1929 en Senegal y más concretamente en la ciudad-puerto de Dakar. Se analizan las consecuencias de la dependencia externa y la extroversión económica que caracterizaba a las estructuras productivas coloniales, destacando también la respuesta organizada de los movimientos sociales africanos. Por otra parte, se estudia la evolución de las infraestructuras y actividad portuaria, observando la metropolización regional de Dakar durante este periodo.

A especialização tecnológica local como indutora do empreendedorismo e do desenvolvimento regional: o caso do Vale da Eletrônica brasileiro

Este trabalho apresenta a percepção dos empreendedores quanto a influência da especialização tecnológica local promovida pelas instituições de ensino superior e seus reflexos no empreendedorismo regional, com base na experiência do Instituto Nacional de Telecomunicações – Inatel, localizado em Santa Rita do Sapucaí, sul de Minas Gerais. O objetivo da pesquisa foi identificar os efeitos tangíveis da transferência de conhecimento de alta tecnologia da universidade para a sociedade produtiva regional. A abordagem metodológica escolhida teve caráter qualitativo, valendo-se de uma pesquisa exploratório-descritiva, que visou ampliar a compreensão do papel dos agentes educacionais locais, especificamente envolvidos no ensino técnico e tecnológico, na geração do desenvolvimento regional. A coleta de dados foi baseada em levantamento documental, bibliográfico e na aplicação de questionários dirigidos aos empreendedores locais, delimitados no escopo geográfico do estudo. Os resultados obtidos permitem concluir que houve evolução nos indicadores socioeconômicos da região.

Cambios del clima, durante los últimos cinco millones de años, observados en el África Atlántica (Islas Canarias)

[ES] En las Canarias orientales, testimonios geológicos del inicio del Plioceno hasta la actualidad han permitido constatar la evolución paleoclimática desde una importante posición en el margen sahariano atlántico. Esta evolución revela la existencia de oscilaciones climáticas caracterizadas por la sucesión de climas que pasan de húmedos y cálidos a cálidos y áridos y que coinciden, respectivamente, con el inicio y el final de períodos interglaciales durante los que el mar fue transgresivo.

Conhecendo a anatomia: a integração da universidade com a educação básica

v. 12, n. 2, jun./dez. 2016.

A Bacia do Algarve: estratigrafia, paleogeografia e tectónica

A “Bacia do Algarve” corresponde, segundo a literatura científica tradicional, aos terrenos mesocenozóicos que orlam o Sul de Portugal, desde o Cabo de São Vicente ao rio Guadiana (~140km), penetrando irregularmente para o interior entre 3 km a 25 km, sobre terrenos de idade carbónica da Zona Sul Portuguesa. O hiato, de aproximadamente 70 milhões de anos, materializado pela discordância angular entre as rochas sedimentares de tipo flysch do Carbónico, metamorfizadas e deformadas durante a orogenia varisca, e as rochas sedimentares continentais do Triásico inferior provável, separa dois ciclos de Wilson. Os sedimentos carbónicos metamorfizados resultam do empilhamento orogénico de um possível prisma de acrecção associado à orogenia varisca e ao fecho de um oceano paleozóico e formação da Pangeia, enquanto que os sedimentos continentais triásicos resultam do fim do colapso e do arrasamento do orógeno varisco e início do estiramento continental que viriam a culminar com a separação das placas litosféricas África, Eurásia e América.Os sedimentos mais recentes do Mesozóico e os mais antigos bem datados do Cenozóico encontram-se separados por um outro hiato que ultrapassa ligeiramente os 70 milhões de anos na área emersa. Este hiato resulta duma alteração tectónica radical no contexto onde nessa época geológica se inseria a Bacia do Algarve. Esta mudança, que ocorreu no fim do Cenomaniano, resultou da rotação do vector de deslocamento da trajectória de África em relação à Eurásia, de aproximadamente NW-SE para SW-NE (segundo as coordenadas actuais, e.g. Dewey et al, 1989), poria termo ao regime distensivo e de bacia de tipo rifte na Bacia do Algarve, com o fim do regime transtensivo entre a região noroeste da placa África e sudoeste da placa Eurásia e início da colisão.

Uso do habitat pela Lontra longicaudis no extremo sul do Brasil

A Lontra longicaudis, mamífero semiaquático, que usa corpos d’água doce e salgada e ambientes adjacentes para forrageio, descanso e proteção, ocorre do México ao Uruguai. Devido ao seu hábito esquivo, a maioria dos estudos foi desenvolvida por meio da análise de evidências indiretas (fezes, muco, pegadas, arranhados). Além da distribuição e do “status” populacional, tornam-se essenciais estudos de preferência de hábitat, pois possibilitam a melhor compreensão das necessidades da espécie. Assim, o objetivo deste trabalho foi verificar o uso de hábitat da L. longicaudis, na Planície Costeira do sul do Rio Grande do Sul, Brasil, a partir da análise da frequência dos sinais encontrados, no período de um ano (2012-2013), em relação à disponibilidade dos hábitats (área aberta, árvores esparsas, área construída, árvores solitárias e mata ciliar) e à sazonalidade. Foram encontrados 394 vestígios (88% fezes ou sinais e fezes). Entre os ambientes, a área construída foi usada com maior frequência, apesar da sua baixa disponibilidade. Já, a área aberta, mesmo com a maior disponibilidade, foi menos utilizada. Entre estações, a lontra selecionou distintos hábitats, com maior atividade no inverno e menor no verão no Taim e no Vargas, e maior atividade na primavera e menor no inverno no Marmeleiro. A lontra usou constantemente os hábitats e demonstrou preferência por ambientes que oferecem maior proteção e por locais com barranco, o que evidencia a importância da manutenção da integridade dos ecossistemas regionais para a preservação da espécie.

Macrofauna epígea de besouros coprófilos em sistema de integração lavoura-pecuária

The soil macrofauna (organisms ≥ 2.0 mm) main function is to act indirectly on the decomposition of organic matter and control the population of microorganisms. This study aims to evaluate the density and richness of coprphilic dung beetles at different levels of nitrogen fertilization and grazing pressure on Crop-Livestock Integration System (ILP) and his opposition to morphotypes present in the native forests of the region. Was used a rural area in Abelardo Luz city, western state of Santa Catarina, on the border of southwest of Paraná, 26° 31' 18.8832" south latitude and 52° 15' 3.4986' west longitude and elevation 862 m for the installation of the experiment, which is already carried out the activity of agriculture and livestock. The study is part of the Integrated Project of Long Duration GISPA UTFPR Group, which evaluates the grazing pressure and time of fertilization deployed in April 2013. The experimental design was a randomized complete block design in a 2x2 factorial arrangement with three replications. The factors were "Nitrogen Application" (NP = N in the pasture and NG = N applied in corn) and "Height Grazing" (high and low). The native forest, which provided the parameters for assessing the degree of conservation, lies 700 meters northeast of the experimental area. Modified pitfall traps were used at ground level, on the bait trap and covered together to prevent dehydration. They were carried out 36 collections in bushland, within one year from 26 April 2013, in which we obtained a total of 16,301 individuals and 28 morphotypes. In ILP area specimens were collected from June to September 2014, totaling 23 collections, 74,586 individuals and 30 morphotypes. To carry out the statistics and faunal analysis, GENES programs were used, ANAFAU, NTIA/EMBRAPA and SigmaPlot version 12.5. Most of the correlations observed (90%) between the variables of insects and environmental conditions was significant. The largest number of insects was directly related to the temperature rise. There was a positive correlation between the application of nitrogen and the occurrence of coprophilous. There was a positive correlation between the number of insects and low grazing height. It was also found that some of the insects migrate from the culture to the area of native forest after reaching their peak population. The great similarity of results observed in the native forest and the ILP System indicates the ecological benefits of adopting this technology.

Rotatividade do mercado de trabalho no corede sul: uma análise ex-ante e ex-post a implementação do polo naval no munícipio de Rio Grande

A presente monografia tem como objetivo analisar a dinâmica do mercado de trabalho do Corede Sul, e avaliar a rotatividade dos trabalhadores a partir do impacto que o polo naval de Rio Grande trouxe para a região sul do estado do Rio Grande do Sul. As metodologias utilizadas foram dados em painel e modelos de diferenças em diferenças, nos períodos de 2003 a 2010 e 2003 a 2013 respectivamente, com o intuito de estimar os determinantes da rotatividade e analisar os impactos posteriores à implementação do polo na região. Foram estimados dois modelos, primeiramente um painel, mas o mesmo demonstrou problemas de endogenia entre as variáveis, e posteriormente um modelo de diferenças em diferenças, que foi estimado para melhor captar os efeitos para as cidades consideradas como tratadas no modelo, obtendo alguns coeficientes significativos. Foram gerados resultados estatisticamente representativos para as cidades de Rio Grande, Pelotas e São José do Norte, tendo a cidade de Rio Grande o maior resultado encontrado um aumento de 132% na rotatividade após 2006. Além disso, foi descoberto um processo de antecipação no mercado de trabalho no município de Rio Grande, em que a população já almejava uma melhor oportunidade de emprego, à medida que a construção do polo se consolidava.