Nutritional modulation of innate immune parameters in the epidermal mucus of Senegalese sole (Solea senegalensis)=Influência da dieta nos parâmetros da resposta imunitária inata do muco de linguado (Solea senegalensis)

Dissertação mest., Biologia Marinha, Universidade do Algarve, 2008

Contribuição parental do linguado do Senegal, Solea senegalensis (KAUP 1858), em aquacultura

Dissertação mest., Biologia Marinha, Universidade do Algarve, 2008

Evaluation of enzymatic and metabolic parameters of quality in sole eggs (Solea Senegalensis, Kaup, 1858)=Avaliação dos parâmetros enzimáticos e metabólicos de qualidade em ovos de linguado (Solea senegalensis, Kaup, 1858)

Dissertação de mest., Biologia Marinha, Faculdade de Ciências do Mar e Ambiente, Univ. do Algarve, 2008

Avaliação da inclusão de EVOCOL em dietas formuladas para juvenis de Linguado (Solea senegalensis, Kaup 1858)

Dissertação de mest., Biologia Marinha, Faculdade de Ciências do Mar e do Ambiente, Univ. do Algarve, 2010

EVOLUÇÃO DOS CONHECIMENTOS SOBRE AS COQUINAS-RESERVATÓRIO DA FORMAÇÃO LAGOA FEIA NO TREND BADEJO-LINGUADO-PAMPO, BACIA DE CAMPOS

É feita uma análise da evolução dos conhecimentos sobre as coquinas-reservatório da Formação Lagoa Feia, com base em cinco publicações de geologia de desenvolvimento dos campos de Badejo, Linguado e Pampo. Trata-se de uma única acumulação, onde o controle é misto, ou seja, estrutural, estratigráfico e principalmente diagenético. Falhas antitéticas herdadas do rifteamento pós-basáltico exercem um importante papel no controle das coquinas, promovendo crescimento da seção nos blocos baixos, e servindo de conduto para a circulação de água meteórica, relacionada à discordância pós-coquina que promove dissolução e criação de porosidade secundária nas coquinas. A compreensão do modelo de acumulação do óleo é fundamental tendo em vista oportunidades para projetos de recuperação suplementar de óleo.

Estudo do reservatório de coquinas do grupo Lagoa Feia (Eocretáceo) na acumulação de Linguado, sudoeste da Bacia de Campos

The Linguado Field is located in the extreme southwest portion of Campos Basin. It’s associated with Structural Badejo High and can be divided in two groups of faults: one manly formed by antithetic faults, with NW-SE direction, continuous to Badejo Fault, and another identified by N-S faults. Besides these faults had affected the basement and the stratification of basin, these systems also had contributed to coquina permoporosity development, that show 80% of recoverable oil volume of the field. The carbonate marine sequence, Albian age, it was deposited under the salt. This forms structures as like as pillows and raft as a result of the halocinese. Structurally the Linguado Field coquina has monoclinal direction with east dip, it’s cut by faults with slip up to 50 meters. In addition to structural control, stratigraphy and diagenesis also were important to carbonate trap oil. The identification of recoverable oil levels in the low phase of the coquina from Lagoa Feia Group was done by well data. The seismic 2D and 3D, with the well data, was used to structural interpretation to regional scale either to reservoir scale.

Análises tectono-estratigráfica e faciológico-diagenética da coquina-reservatório Lagoa Feia, Campo de Linguado, Bacia de Campos

A tectono-stratigraphic study of bivalve coquina-reservoir of Linguado Field allowed to identify two trends of permoporosity development. The delineation of these depositional-diagenetic traps were made through structural and stratigrafic cross-sections and maps. It resulted in the identification of shelf-ramp systems (tilted to SSE), it tickens from 60 to 70 meters and ends against an antithetic fault. The main coquina is bounded by fine siliciclastic units, white clay (low Gamma Ray values) or shale (high Gamma Ray values) lithologies, influencing diagenesis of basal or top coquina limestones (cimented, non-porous). Also in the middle of coquina-reservoir the “clayer” material is also associated with cemented carbonates, with also compartimentalize the reservoir into two subzones. The coquina porosity of the subzones is taken from density-neutron logs, while induction log estimates permeabilities and fluid saturations. It’s noticed the porosity development into pairs, good one followed by a regular/poor one and vice versa. These pairs form verticals succession, pair cycles where porosity improves or decreases upwards. These two scales of pore heterogeneity impose strong layering to the reservoir, and influences fluid saturations, oil-water contacts and porosity cut-offs. In a cross-section with density and induction logs, it can be observed the porosity variation along the shelf-ramp coquina (between 3LI_0004_RJS e 3RJS_0157C_RJ), the porosity is better developed in a downdip direction in the case of the two shelf wells, and also be the three ramp wells. The southern west downdip, 3RJS_0157C_RJ well, has best porosity pairs-cycles; however, its lowest structural conditions favour water saturation. Therefore it is fundamental for reservoir fluid evaluation a cross-plot analysis of RHOB-NPHI and Induction logs

Evolução tectônica do Trend Badejo-Linguado-Pampo, bacia de Campos (RJ)

The regional geological work for the oil industry, in order to find potential areas for hydrocarbon exploration and understand the geological parameters responsible for the formation of the deposit are known importance. This work fits into that scenario, with regional research with the aid of wells and 2D and 3D seismic sold by DBEP (Database Exploration and Production). Were also used as GeoGraphix software package Landmarks modules Prizm and SeisWork 2D and 3D, and the Surfer 8 and ArcGIS 9.2 with the infrastructure provided by the 05 PRH - ANP with LSGI (Laboratory of Seismic and Geological Interpretation) located at UNESP -- Campus de Rio Claro. The work focuses on study the trend of oil-Badejo-Linguado-Pampo, producing fields since the beginning of offshore holdings. The Campos Basin is now known as the offshore basin of the country more productive, and the high structural Badejo is a structure of great importance in the basin presents itself as largely responsible for the conditioning of hydrocarbon fields Pampo, Linguado and Badejo. Therefore this work also aims to increase knowledge of the region in terms of tectonic and stratigraphic characterize the geometry of the structures associated with this major regional structure. For this we used structural contour maps of the main chrono-horizons, and Isopach maps for the purpose of better understanding the tectono-sedimentary evolution of the Campos Basin locally.

Desenvolvimento de um novo protocolo alimentar para Linguado, Solea senegalensis, à base de copépodes congelados

A qualidade do alimento é essencial para que as larvas obtenham os nutrientes necessários para um desencolvimento normal. Como as larvas de peixes marinhos têm um elevado potencial de crescimento, têm igualmente necessidades nutritivas específicas e elevadas. Copépodes são considerados o melhor alimento para a maioria das larvas marinhos, uma vez que o perfil nutricional preenche os requisitos das larvas de peixes. Os copépodes são uma uma excelente fonte de ácidos gordos insaturados (HUFAs) e poliinsaturados (PUFAs), não necessitando de enriquecimento, como a Artemia spp.. A utilização de copépodes congelados (Planktonic AS, Noruega) é uma nova e vantajosa alternativa para a aquacultura, no qual estão disponiveis durante todo o ano e mantêm a composição bioquímica ao longo do ano. Inicialmente estudou-se o comportamento alimentar do linguado face a este novo produto, pois o mesmo não apresenta movimento. Foi desenvolvido um protocolo para a coloração dos copépodes congelados. Taxa de ingestão e/ou comportamento alimentar foram avaliados quando as larvas foram alimentadas com copépodes corados, não corados e artémia. Observou-se que a coloração aumenta a ingestão de copépodes congelados pelas larvas de peixe, embora a uma taxa inferior quando comparado com a artémia. O objetivo deste estudo foi desenvolver um protocolo alimentar à base de copépodes congelados, em substituição das presas habitualmente utilizadas (rotíferos e artémia), durante o período larvar do linguado, Solea senegalensis. Foram testados 2 protocolos alimentares, 50:50 e Agressivo, com a substituição de 50% e 90%, respectivamente, de presas vivas do protocolo alimentar para liguado habitualmente utilizado na Estação Piloto de Piscicultura de Olhão (EPPO), sendo este consideradoo Controlo. O ensaio larvar decorreu desde a abertura de boca até aos 40 dias após a eclosão (DAE). As amostras foram recolhidas periodicamente para avaliar o crescimento, sobrevivência e a condição nutricional das larvas, através da determinação do índice ARN:ADN e da proteína total. Para avaliar a condição das pós-larvas, peixes de todos os tratamentos foram sujeitos a um desmame aos 40 DAE, com uma dieta inerte com incorporação de 10% de copépodes. O desempenho dos peixes foi seguido até aos 50 DAE. As larvas do tratamento Controlo apresentaram maior crescimento e uma maior taxa de ingestão de presas vivas, no entanto as larvas do protocolo 50:50 apresentaram um melhor índice de ARN:ADN. Estes dados sugerem que para o linguado, os copépodes podem substituir quase 50% das presas vivas.

ANÁLISE SOCIOAMBIENTAL DO FECHAMENTO DO CANAL DO LINGUADO/SC

Este trabalho tem como objetivo apresentar uma análise socioambiental das conseqüências do fechamento do canal do Linguado, localizado no nordeste do estado de Santa Catarina/Brasil, parte integrante da Baía da Babitonga. A região tem no município de Joinville/SC o maior pólo industrial do setor metal mecânico e o porto em São Francisco do Sul como porta de importação e exportação de produtos diversos. Para dar maior segurança e facilitar a construção do sistema rodo-ferroviário de ligação entre os municípios de Joinville, Araquari e São Francisco do Sul, com menor custo financeiro, optou-se pelo fechamento do canal na década de 1930. Por conseqüência, a população, paisagem e o ecossistema da região sofreram um impacto jamais imaginável naquela época. Os resultados dessa análise foram obtidos através de saídas a campo, pesquisas in loco, entrevistas e leitura de levantamentos bibliográficos.

Purificação e caracterização de proteínas Gla nos modelos peixe e mamífero

Dissertação de Mestrado, Biologia Molecular e Microbiana, Faculdade de Ciências e Tecnologia, Universidade do Algarve, 2010

Evolution, gene regulation and functional analysis of BMP2 in fish

Bone morphogenetic proteins (BMPs) are multifunctional growth factors belonging to the transforming growth factor β (TGFβ) superfamily with a central role in bone formation and mineralization. BMP2, a founding member of this family, has demonstrated remarkable osteogenic properties and is clinically used to promote bone repair and fracture healing. Lack of basic data on factors regulating BMP2 expression and activity have hampered a better understanding of its role in bone formation and bone-related diseases. The objective of this work was to collect new functional data and determine spatiotemporal expression patterns in a fish system aiming towards a better understanding of BMP2 function and regulation. Transcriptional and post-transcriptional regulation of gilthead seabream BMP2 gene was inferred from luciferase reporter systems. Several bone- and cartilage-related transcription factors (e.g. RUNX3, MEF2c, SOX9 and ETS1) were found to regulate BMP2 transcription, while microRNA 20a was shown to affect stability of the BMP2 transcript and thus the mineralogenic capacity of fish bone-derived host cells. The regulation of BMP2 activity through an interaction with the matrix Gla protein (MGP) was investigated in vitro using BMP responsive elements (BRE) coupled to luciferase reporter gene. Although we demonstrated the functionality of the experimental system in a fish cell line and the activation of BMP signaling pathway by seabream BMP2, no conclusive evidence could be collected on a possible interaction beween MGP and BMP2. The evolutionary relationship among the members of BMP2/4/16 subfamily was inferred from taxonomic and phylogenetic analyses. BMP16 diverged prior to BMP2 and BMP4 and should be the result of an ancient genome duplication that occurred early in vertebrate evolution. Structural and functional data suggested that all three proteins are effectors of the BMP signaling pathway, but expression data revealed different spatiotemporal patterns in teleost fish suggesting distinct mechanisms of regulation. In this work, through the collection of novel data, we provide additional insight into the regulation, the structure and the phylogenetic relationship of BMP2 and its closely related family members.

Geologia das coquinas-reservatório do Campo de Pampo, Bacia de Campos

The Pampo oil field is located in the southwest of the trend Badejo-Linguado-Pampo in an accumulation of single - mixed trap: structural-stratigraphic-diagenetic. Its main reservoir is a coquina shell of bivalves (the lowest) in the Lagoa Feia Group. During the rift phase, the Badejo-Linguado-Pampo trend´s accumulations evolve according to three tectono-stratigraphic cycles. The first two cycles are formed by siliciclastic rocks with fining up sequences and carbonates coquinas bivalves. The youngest cycle related to Alagoas age is a transgressive event represented by the presence of an evaporitic layer in the top (anhydrite). This study aims to characterize the reservoir Coqueiros Formation based on the analysis of 2D and 3D seismic data and well data-correlation profiles. The structural map of the top of coquinas reservoir indicates a curvilinear contour of Pampo Fault as described on the literature. This fault was interpreted on seismic data as a basement´s high, and it doesn´t show influence on the horizons above the top of Lagoa Feia Group. The Pampo fault is responsible for the division of the field into two blocks: the hanginwall in the West and the footwall to the East. This division is well marked on the reservoir´s isopach map where a greater thickness of reservoir is observed on the lower block. In the Southeast extreme of Badejo-Linguado-Pampo trend, on Pampo Field, the thick siliciclastic´s interval ends laterally to the basement, and its lower´s cycle forms a wedge, as consequence the carbonate-coquina overlaps directly the basement. Another implication of the higher and distal position of Pampo field is that the third cycle is absent, truncated by the unconformity pre-Macaé Group (Albian)

Caracterização tectono-sedimentar do Grupo Lagoa Feia (Eocretáceo) no Campo de Pampo, sudoeste da Bacia de Campos

The Lagoa Feia Group (Early Cretaceous) is widely distributed around the Campos Basin, forming deep prospects in the basin. It has two large coquinas platforms shellfish, and the lower deck constituent important reservoir in the southwestern of this basin, a producer of oil in the trend-Badejo-Linguado-Pampo. Due to the rising national energy demand is necessary to see the incorporation of technical knowledge and training of human resources in the knowledge of petroleum reservoirs. In this sense, the Pampo Field, as well as other fields of the trend, fall as interesting target area for study. Accumulations of hydrocarbons are partitioning structural - stratigraphic only for the three fields. They are mixed origin of traps, with influence of structural, stratigraphic and diagenetic. With the development of catchment areas of the latter condition has manifested itself in such a way to verify parts with nonproducing wells, which are observed in the intervals coquinas are closed, with reduced thickness and / or low quality porous. The understanding of these accumulations, by testing structural, stratigraphic and reservoir and the use of geological and geophysical techniques, will bring a better understanding of the portions relating to economic accumulation or subeconomic development of hydrocarbons in this region, contributing to the scientific knowledge of the Pampo Field.

Effects of ocean warming and acidification on the early stages of marine fishes

Tese de doutoramento, Ciências do Mar, Universidade de Lisboa, Faculdade de Ciências, 2016