1000 resultados para Litoral continental português


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We used high-resolution swath-bathymetry data to characterise the morphology of the abandoned subaqueous Sol de Riu delta lobe in the Ebro Delta, Western Mediterranean Sea. This study aims to assess the influence of an abandoned delta lobe on present-day coastal dynamics in a micro-tidal environment. Detailed mapping of the relict Sol de Riu lobe also showed a set of bedforms interpreted as footprints of human activities: seasonal V-shaped depressions on the middle shoreface due to boat anchoring and old trawling marks between 16 and 18 m water depth. Estimations of the mobility of bottom sediment showed that the shallowest shoreface (i.e. less than 7 m depth) is the most dynamic part of the relict lobe, while the middle shoreface experienced significant morphological changes since the lobe was abandoned. The deepest shoreface (i.e. water depth in excess of 15 m), which corresponds to the front of the lobe, is defined by a very small potential for morphological change. Simulations showed that while the relict lobe does not significantly affect the typical short period waves (Tp ≈4 s) in the study area, it does interfere with the most energetic wave conditions (Tp ≥ 7 s) acting as a shoal leading to the concentration of wave energy along the shoreline northwest of the lobe. The consequence of such modification of the high-energy wave propagation pattern by the relict lobe is an alteration of the wave-induced littoral sediment dynamics with respect to a situation without the lobe.

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A construção de um Atlas que garanta a visualização da situação do país face aos principais temas que surgem como referência para o U&OT nos documentos políticos europeus, responde à necessidade de conhecer o território nacional para promover acções específicas em sede de planeamento e ordenamento que garantam o desenvolvimento coerente e suportado do território assegurando aos cidadãos acesso a condições que promovam a sua qualidade de vida.Como o presente trabalho disponibiliza-se uma base de referência ao nível do continente português dos principais indicadores que correspondem às preocupações políticas europeias no domínio do território. A necessidade de promover um território coeso, participado e preparado para garantir a qualidade de vida dos seus utilizadores sem hipotecar o futuro das gerações vindouras (cf. CLRAE, 1992, EU, 2007a & EU, 2007b), está suportado no conhecimento específico dos factores que condicionam, ou podem condicionar esse processo.A necessidade de um equilíbrio territorial, entre as áreas mais urbanizadas e as áreas rurais (cf. EU, 2007b) assume-se como um ponto de partida para a definição da estrutura do trabalho aqui apresentado. A necessidade de entender as paridades e disparidades do território, as ofertas e as debilidades entre as áreas mais urbanizadas e as áreas mais rurais, evidencia a necessidade de estratificar o território segundo os seus níveis de urbanização. Garante-se assim a análise separada de duas realidades distintas, por um lado as áreas urbanizadas, com concentrações humanas mais elevadas e que exigem serviços específicos, por outro as áreas rurais, muitas vezes em abandono, que interessa entender até que ponto a oferta ou falha nas condições existentes para a promoção da qualidade de vida nessas áreas condiciona a fixação de população.O Atlas que se apresenta [Atlas de Portugal (Continental), Conforma às Políticas Europeias em matéria de U&OT – AP_PEUOT] é a imagem de Portugal Continental, em 2001 – ano de disponibilização dos dados referentes ao último Censo – com os indicadores seleccionados com base nos documentos, políticas e princípios europeus sobre U&OT, apresentando-se também uma evolução histórica entre os anos de 1991 e 2001 – anos de recenseamento geral da população e da habitação – estratificados em áreas urbanas, mediamente urbanas e rurais com base no trabalho do INE/DGOTDU de 1998 (cf. INE/DGOTDU 1998) (cf. Ponto 3.1.2 do presente trabalho).

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The fishes of the order Perciformes are characterized as an important model for understanding the genetic structure of marine populations, because besides they present examples of conservation chromosomal, also they present the karyotype diversification for some groups. Gobiidae family is the most specious in the marine environment. Among its representatives, many species are part of a cryptic fauna little noticed and studied, a wide distribution with behavioral and reproductive characteristics, that make them conducive to the action of biogeographical barriers. Morphologically this family presents reduced body structures through simplification and regressions. Despite their importance in evolutionary inferences, cytogenetics data are incipient facing their species diversity, especially with western Atlantic species. In order to estimate the evolutionary diversity in Gobiidae, it were developed cytogenetic analysis and the standards body, through geometric morphometrics in five species on the Brazilian coast, Coryphopterus glaucofraenum, Bathygobius mystacium, B. soporator, Ctenogobius smaragdus e C. Boleosoma. The data show significant karyotype and morphological diversity among the species. The pericentric inversions and mergers play an important role in chromosomal evolution of this family, causing karyotypic structural and numerical differences in all species. Karyotypic and morphological comparisons among geographic samples of B. soporator from the coast of Maranhão, Rio Grande do Norte and Bahia showed cytogenetics patterns commons, but different morphological patterns. A sample from the Atol das Rocas revealed conspicuous morphological and karyotypic differentiation of another continental populations, confirming the presence of a new island species. The approaches done reveal diversification consistent with characteristics of a group of low vagile and largely able to environmental selection due from peculiar ecological requirements

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This dissertation the results of a research developed in the area of São Bento do Norte and Caiçara do Norte, northern coast of the State of Rio Grande do Norte, during the period of June of 2000 to August of 2001, in the ambit of the projects MAMBMARÉ (CNPq/CTPETRO) and PROBRAL (CAPES/DAAD). The objective principal of this research was the characterization of the sedimentary dynamics of this coast, with base in data of coastal process (winds, currents, waves and tides), with topographical risings (beach profiles and dunes), satellite images and sedimentary analyses. The more specific objectives were accomplished the coastal monitoring of this coast, to verify the maintenance of an erosive tendency or progradacional after the groynes construction for contention of the erosion in the beach of Caiçara do Norte, as well as to verify the influence of the features of bottom of the platform interns adjacent on the pole petroliferous of Guamaré. The executed monitoramento allowed to identify that the movement of the sediments, along the year, in that area, is cyclical, reaching the largest oscillations during the months of winter (deposition) and they will summer (erosion). The sedimentologic studies indicated a general tendency for sands quartzosas, with gravel presence, moderately to good selected, with asymmetry predominantly negative. In agreement with the parameter of Dean (1957), used in the identification of the state morfodinâmico of the beaches, monitored beaches, are basically reflectivas with tendency to middlemen, what frames that space of the coast norte-riograndense, as a space strongly vulnerable to erosive processes. The studies developed in the platform, it interns of this area, allowed to visualize for the first time, in large scale, the distribution of the features of the submarine bottom to the batométrico coat of 25 meters. Being pointed out the presence of a high one topographical submerged, with about 5 meters of height, 1 km of width and more than 24 meters of extension, located in the platform it interns in front of São Bento do Norte; coincident with the trend of the system of flaws of Carnaubais. This feature relay an important paper on the control of the sedimentary processes and oceanographic, as well as in the coastal evolution of this area of the RN state, and they affect the area of the pole petroliferous of Guamaré directly. These results contribute to a better knowledge of the processes in the area, and consequently as subsidies implantation of measures of coastal and environmental protection for the cities of São Bento do Norte and Caiçara do Norte, as well as to understand how the geological-sedimentary processes and oceanographic, in this area, are influencing the characteristics geoambientais of the pole petroliferous of Guamaré

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This thesis presents the results of application of SWAN Simulating WAves Nearshore numerical model, OF third generation, which simulates the propagation and dissipation of energy from sea waves, on the north continental shelf at Rio Grande do Norte, to determine the wave climate, calibrate and validate the model, and assess their potential and limitations for the region of interest. After validation of the wave climate, the results were integrated with information from the submarine relief, and plant morphology of beaches and barrier islands systems. On the second phase, the objective was to analyze the evolution of the wave and its interaction with the shallow seabed, from three transverse profiles orientation from N to S, distributed according to the parallel longitudinal, X = 774000-W, 783000-W e 800000-W. Subsequently, it was were extracted the values of directional waves and winds through all the months between november 2010 to november 2012, to analyze the impact of these forces on the movement area, and then understand the behavior of the morphological variations according to temporal year variability. Based on the results of modeling and its integration with correlated data, and planimetric variations of Soledade and Minhoto beach systems and Ponta do Tubarão and Barra do Fernandes barrier islands systems, it was obtained the following conclusions: SWAN could reproduce and determine the wave climate on the north continental shelf at RN, the results show a similar trend for the measurements of temporal variations of significant height (HS, m) and the mean wave period (Tmed, s); however, the results of parametric statistics were low for the estimates of the maximum values in most of the analyzed periods compared data of PT 1 and PT 2 (measurement points), with alternation of significant wave heights, at times overrated with occasional overlap of swell episodes. By analyzing the spatial distribution of the wave climate and its interaction with the underwater compartmentalization, it was concluded that there is interaction of wave propagation with the seafloor, showing change in significant heights whenever it interacts with the seafloor features (beachrocks, symmetric and asymmetric longitudinal dunes, paleochannel, among others) in the regions of outer, middle and inner shelf. And finally, it is concluded that the study of the stability areas allows identifications of the most unstable regions, confirming that the greatest range of variation indicates greater instability and consequent sensitivity to hydrodynamic processes operating in the coastal region, with positive or negative variation, especially at Ponta do Tubarão and Barra do Fernandes barrier islands systems, where they are more susceptible to waves impacts, as evidenced in retreat of the shoreline

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This work focuses the geomorphological characterization and spatial data modeling in the shallow continental shelf within the Folha Touros limits (SB-25-CV-II), based on bathymetric data analysis and remote sensing products interpretation. The Rio Grande do Norte state is located in northeastern Brazil and the work area is located at the transition region between the eastern and northern portions of their coast. The bathymetric surveys were conduced between march and may 2009, using a 10 meters long vessel and 0.70 meters draught, equipped with global positioning system and echo sounder (dual beam, 200KHz , 14°). The fieldwork resulted in 44 bathymetric profiles espaced 1.5 km and 30 km average length. The bathymetric data amount were 111,200 points and were navigated 1395.7 km within na area about 1,850 km2. The bathymetric data were corrected for the tide level, vessel draught and were subsequently entered into a geographic information system for further processing. Analysis of remote sensing products was carried out using Landsat 7/ETM + band 1, from november 1999. The image was used for visualization and mapping submerged features. The results showed the presence of geomorphological features within the study area. Were observed, from the analysis of local bathymetry and satellite image, seven types of geomorphological features. The channels, with two longitudinals channels (e. g. San Roque and Cioba channels) and other perpendicular to the coast (e. g. Touros, Pititinga and Barretas). Coastal reef formations (Maracajaú, Rio do Fogo and Cioba). Longitudinal waves, described in the literature as longitudinal dunes. The occurrence of a transverse dune field. Another feature observed was the oceanic reefs, an rock alignment parallel to the coast. Were identified four riscas , from north to south: risca do Liso, Gameleira, Zumbi, Pititinga (the latter being described for the first time). Finally, an oceanic terrace was observed in the deepest area of study. Image interpretation corroborated with the in situ results, enabling visualization and description for all features in the region. The results were analysed in an integrating method (using the diferent methodologies applied in this work) and it was essential to describe all features in the area. This method allowed us to evaluate which methods generated better results to describe certain features. From these results was possible to prove the existence of submerged features in the eastern shallow continental shelf of Rio Grande do Norte. In this way, the conclusions was (1) this study contributed to the provision of new information about the area in question, particularly with regard to data collection in situ depths, (2) the method of data collection and interpretation proves to be effective because, through this, it was possible to visualize and interpret the features present in the study area and (3) the interpretation and discussion of results in an integrated method, using different methodologies, can provide better results

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Stranding of oceanic-pelagic elasmo branchs in the southeastern Brazil are reported. Data comes from animals observed in the coast of São Paulo state, between 1999 and 2012. Nine individuals of two species were recorded: Pteroplatytrygon violacea (n = 5; mostly during the winter) and Isurus oxyrinchus (n = 4; two in the winter and two in the summer). For P. violacea the strandings restricted to the austral winter suggest that the species follows the intrusion of high temperatures water masses recorded in southeastern Brazil during this season, bringing some individuals to shallow waters. For I. oxyrinchus is possible that individuals escaped from hooks of the commercial pelagic long line fishery and suffered injuries in the esophagus and in the gastric wall, stranding due to difficulties in locomotion and feeding. As these stranded sharks were not necropsied and only two animals were observed during the austral summer, we cannot exclude other causes of beaching such diseases or the intrusion of cold water masses in the continental shelf during this season.

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Pós-graduação em Geociências e Meio Ambiente - IGCE

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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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As ilhas da plataforma continental estão isoladas do continente, há cerca de 10.000 anos, após a última elevação do nível dos oceanos. O isolamento, a ocupação de novos habitats e/ou diferentes pressões ecológicas podem ter levado a alterações em caracteres genotípicos, fenotípicos e também comportamentais. Este trabalho visa o estudo dos padrões reprodutivos em populações de Thoropa taophora e suas adaptações no continente e em seis ilhas do litoral Norte do Estado de São Paulo. Como hipóteses tem se que fêmeas das populações insulares possuem ovócitos maiores e em menor número devido à redução na disponibilidade de sítios reprodutivos, e machos insulares devem apresentar testículos maiores e maior agressividade associada à defesa de territórios mais escassos. Foram avaliadas as variações de caracteres reprodutivos, como peso de testículos dos machos, número e tamanho dos ovócitos das fêmeas e esforço reprodutivo de 147 indivíduos adultos de T. taophora (87 machos e 60 fêmeas) de populações provenientes das ilhas de Toque-Toque, Redonda, Prumirim, Gatos, Couves, Porcos Pequena; e três localidades no continente: Tuim Parque - Barra do Una e Praia de Toque-Toque Grande no Município de São Sebastião-SP e Praia Domingas Dias no Município de Ubatuba-SP. Todos os indivíduos analisados foram coletados durante o verão (outubro a março) e encontram-se depositados na Coleção de Anfíbios (CFBH), UNESP - Rio Claro e Coleção do Museu de História Natural (ZUEC), UNICAMP. O comprimento rostrocloacal (CRC) das fêmeas variou de 26,7 – 78,3 mm, ao passo que o CRC dos machos variou de 55 – 93,8 mm. Os machos foram significativamente maiores que as fêmeas em quatro localidades. Nas fêmeas, o diâmetro dos ovócitos da população continental da praia Domingas Dias é maior que nas populações das ilhas dos Gatos, Toque-Toque e Redonda... (Resumo completo, clicar acesso eletrônico abaixo)

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O estuário Santista (SP) é uma das áreas mais impactadas do litoral paulista. A industrialização e a urbanização ocorridas no litoral central do estado de São Paulo, ao longo dos últimos 70 anos, acarretou significativas mudanças na dinâmica sedimentar do estuário e da baía de Santos, sem que se conheça o real impacto destas modificações na sequência sedimentar depositada na plataforma continental interna adjacente.

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O presente estudo de dissertação consiste no estudo da viabilidade económica e financeira de uma microempresa de Pescaturismo. Trata-se da apresentação de um plano de negócios turístico-pesqueiro, onde a principal ideia - através de um modelo de intraempreendedorismo marítimo de criação de valor social, económico e financeiro - é a conceção de uma unidade empresarial, sob o conceito de turismo marítimo-pesqueiro, estrategicamente posicionada no nicho de mercado de turismo criativo e costeiro, visando, por um lado, a satisfação das necessidades de todos aqueles que procuram experiências genuínas de vivências culturais em vilas historicamente viradas para o mar e, por outro, aumentar as fontes de rendimento das comunidades piscatórias e acrescentar valor à atividade de pesca, pela diversificação da atividade económica. Este trabalho também pretende constituir um modelo padrão de empreendedorismo a implementar junto dos profissionais da pesca artesanal e local, económica e financeiramente sustentável, dando ênfase às potencialidades dos recursos endógenos e embarcações disponíveis que criem produtos e serviços estratégicos de turismo ao ar livre e de animação turística. Assim, consideramos que a combinação do setor das pescas com o setor do turismo, na dimensão de animação turística, como as atividades marítimo-turísticas, enquanto setores estratégicos do desenvolvimento económico-social, constitui a base do modelo de Plano de Negócios de Pescaturismo apresentado. Pese embora a legislação portuguesa da Região Autónoma dos Açores reconheça a atividade, o conceito aplicado ao turismo e à pesca no Continente é novo e inovador. Também é um trabalho inovador uma vez que é o primeiro estudo de viabilidade de Pescaturismo em Portugal continental e ilhas, apresentando para o efeito um plano de negócio turístico compacto aplicável e adaptável a uma vasta gama de empreendedores marítimos. Para o efeito considera-se como base do estudo a comunidade piscatória de Vila Praia de Âncora e os seus recursos naturais, e construídos, de interesse turístico.