38 resultados para Mosteiro da Madre de Deus (Lisboa, Portugal)

em Repositório Científico da Universidade de Évora - Portugal


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O pintor Jorge Afonso (c. 1480-1540) ocupou cargos da maior importância e foi mestre de alguns dos mais importantes artistas da primeira metade do século XVI. Por laços familiares, por ligações profissionais, ou como representante régio no fornecimento e controle de empreitadas, esteve no centro das grandes obras artísticas do seu tempo. Fez uma carreira como oficial de armaria dentro da reestruturação manuelina, o que o tornou, também do ponto de vista simbólico, uma figura importante da corte do Venturoso. A Jorge Afonso são atribuídas as grandes tábuas da Charola do Convento de Cristo de Tomar, oito pinturas do mosteiro da Madre de Deus e o retábulo do Convento de Jesus de Setúbal. A dissertação reanalisa os dados biográficos do pintor, estuda as pinturas incluindo o seu desenho subjacente, e reelabora a compreensão da pintura portuguesa do tempo, vista sob a influência desta figura tutelar; ABSTRACT: Jorge Afonso. An essential quest on Portuguese primitive painting. Painter Jorge Afonso (1480-1540), held positions of major importance and was master of some of the most remarkable artists of the first half of the 16th century. By family links, by professional connections or as Royal representative for the supply and control of works, he was at the very center of the great artistic works of his time. He built a career as Herald what made him an important figure in King D. Manuel’s court . To Jorge Afonso are attributed the large paintings of the ‘Christ’s Convent’ Ambulatory in Tomar, eight paintings from the ‘Madre de Deus’ monastery and the ‘Covent of Jesus’ altarpiece in Setubal. This dissertation reanalysis the painter biographical data, studies the paintings including its underdrawing and reconstructs the understanding of Portuguese painting of that time, perceived under the influence of this tutelary figure.

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Portugal apresenta uma actividade sísmica que resulta em grande parte da sua proximidade à fronteira entre as placas tectónicas Euro-asiática (EA) e Nubia (NU), numa faixa que se estende desde Gibraltar até ao arquipélago dos Açores. A fractura litosférica contida nessa faixa é habitualmente designada por Fractura Açores-Gibraltar. A forte interacção entre os dois blocos, manifesta-se por um aumento da sismicidade nesta faixa, fortemente influenciada pela interacção entre os dois blocos tectónicos. No prolongamento para Ocidente deste acidente atinge-se a Crista Média Atlântica (CMA) num ponto localizado a noroeste do arquipélago dos Açores, e que constitui a fronteira entre a placa Americana (AM) e as placas EA e NU. Este ponto também é conhecido por Junção Tripla dos Açores. A interacção entre os três limites de placas confere à região dos Açores a actividade sísmica que se lhe conhece, uma das mais significativas no contexto nacional. Toda esta zona, devido ao potencial e efectivo risco sísmico testemunhado pelos eventos sísmicos recentes e pelos grandes terremotos historicamente documentados, é alvo de um elevado esforço que nos últimos anos resultou, de forma integrada, em avanços como: 1) melhoria da capacidade de observação do fenómeno sísmico –a existência dos meios mínimos de monitorização sísmica é hoje uma realidade que reconhecemos, salientando contudo, o muito que há a fazer em domínios como: a instalação de estações sísmicas submarinas (OBS) capazes de suprir as lacunas verificadas; a compatibilização de dados e o livre acesso aos mesmos; a criação de uma rede de acelerómetros capaz de registar os movimentos fortes; 2) aumento da capacidade de investigação – o recrutamento de novos investigadores através de projectos multi-disciplinares em domínios como a sismicidade, fonte sísmica e mecanismos focais, geomagnetismo, gravimetria, geodesia e análise estrutural....

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NEW DATA ON THE CHRONOLOGY OF THE VALE DO FORNO SEDIMENTARY SEQUENCE (LOWER TAGUS RIVER TERRACE STAIRCASE) AND ITS RELEVANCE AS FLUVIAL ARCHIVE OF THE MIDDLE PLEISTOCENE IN WESTERN IBERIA Pedro P. Cunha 1, António A. Martins 2, Jan-Pieter Buylaert 3,4, Andrew S. Murray 4, Luis Raposo 5, Paolo Mozzi 6, Martin Stokes 7 1 MARE - Marine and Environmental Sciences Centre, Department of Earth Sciences, University of Coimbra, Portugal: pcunha@dct.uc.pt 2 MARE - Marine and Environmental Sciences Centre, Dep. Geociências, University of Évora, Portugal; aam@uevora.pt 3 Centre for Nuclear Technologies, Technical University of Denmark, Risø Campus, Denmark; jabu@dtu.dk 4 Nordic Laboratory for Luminescence Dating, Aarhus University, Risø DTU, Denmark; anmu@dtu.dk 5 Museu Nacional de Arqueologia, Lisboa, Portugal; 3raposos@sapo.pt 6 Department of Geosciences, University of Padova, Italy; paolo.mozzi@unipd.it 7 School of Geography, Earth and Environmental Sciences, University of Plymouth, UK; m.stokes@plymouth.ac.uk The stratigraphic units that record the evolution of the Tagus River in Portugal (study area between Vila Velha de Ródão and Porto Alto villages; Fig. 1) have different sedimentary characteristics and lithic industries (Cunha et al., 2012): - a culminant sedimentary unit (the ancestral Tagus, before the drainage network entrenchment) – SLD13 (+142 to 262 m above river bed – a.r.b.; with probable age ca. 3,6 to 1,8 Ma), without artefacts; - T1 terrace (+84 to 180 m; ca. 1000? to 900 ka), without artefacts; - T2 terrace (+57 to 150 m; top deposits with a probable age ca. 600 ka), without artefacts; - T3 terrace (+43 to 113 m; ca. 460 to 360? ka), without artefacts; - T4 terrace (+26 to 55 m; ca. 335 a 155 ka), Lower Paleolithic (Acheulian) at basal and middle levels but early Middle Paleolithic at top levels; - T5 terrace (+5 to 34 m; 135 to 73 ka), Middle Paleolithic (Mousterian; Levallois technique); - T6 terrace (+3 to 14 m; 62 to 32 ka), late Middle Paleolithic (late Mousterian); - Carregueira Sands (aeolian sands) and colluvium (+3 a ca. 100 m; 32 to 12 ka), Upper Paleolithic to Epipaleolithic; - alluvial plain (+0 to 8 m; ca. 12 ka to present), Mesolithic and more recent industries. The differences in elevation (a.r.b.) of the several terrace staircases results from differential uplift due to active faults. Longitudinal correlation with the terrace levels indicates that a graded profile ca. 200 km long was achieved during terrace formation periods and a strong control by sea base level was determinant for terrace formation. The Neogene sedimentary units constituted the main source of sediments for the fluvial terraces (Fig. 2). Geomorphological mapping, coupled with lithostratigraphy, sedimentology and luminescence dating (quartz-OSL and K-feldspar post-IRIR290) were used in this study focused on the T4 terrace, which comprises a Lower Gravels (LG) unit and an Upper Sand (US) unit. The thick, coarse and dominantly massive gravels of the LG unit indicate deposition by a coarse bed-load braided river, with strong sediment supply, high gradient and fluvial competence, during conditions of rapidly rising sea level. Luminescence dating only provided minimum ages but it is probable that the LG unit corresponds to the earlier part of the MIS9 (ca. 335 to 325 ka), immediately postdating the incision promoted by the very low sea level (reaching ca. -140 m) during MIS10 (362 to 337 ka), a period of relatively cold climate conditions with weak vegetation cover on slopes and low sea level. Fig. 1. Main Portuguese reaches in which the Tagus River can be divided (Lower Tagus Basin): I – from the Spanish border to Arneiro (a general E–W trend, mainly consisting of polygonal segments); II – from Arneiro to Gavião (NE–SW); III – from Gavião to Arripiado (E–W); IV – from Arripiado to Vila Franca de Xira (NNE-SSW); V – from Vila Franca de Xira to the Atlantic shoreline. The faults considered to be the limit of the referred fluvial sectors are: F1 – Ponsul-Arneiro fault (WSW-ENE); F2 – Gavião fault (NW-SE); F3 – Ortiga fault (NW-SE); F4 – Vila Nova da Barquinha fault (W-E); F5 – Arripiado-Chamusca fault (NNE-SSW). 1 – estuary; 2 – terraces; 3 – faults; 4 – Tagus main channel. The main Iberian drainage basins are also represented (inset). The lower and middle parts of the US unit, comprising an alternation of clayish silts with paleosols and minor sands to the east (flood-plain deposits) and sand deposits to the west (channel belt), have a probable age of ca. 325 to 200 ka. This points to formation during MIS9 to MIS7, under conditions of high to medium sea levels and warm to mild conditions. The upper part of the US unit, dominated by sand facies and with OSL ages of ca. 200 to 154 ka, correlates with the early part of the MIS6. During this period, progradation resulted from climate deterioration and relative depletion of vegetation that promoted enhanced sediment production in the catchment, coupled with initiation of sea-level lowering that increased the longitudinal slope. The Vale do Forno and Vale da Atela archaeological sites (Alpiarça, central Portugal) document the earliest human occupation in the Lower Tagus River, well established in geomorphological and environmental terms, within the Middle Pleistocene. The Lower Palaeolithic sites were found on the T4 terrace (+26 m, a.r.b.). The oldest artefacts previously found in the LG unit, display crude bifacial forms that can be attributed to the Acheulian, with a probable age of ca. 335 to 325 ka. The T4 US unit has archaeological sites stratigraphically documenting successive phases of an evolved Acheulian, that probably date ca. 325 to 300 ka. Notably, these Lower Palaeolithic artisans were able to produce tools with different sophistication levels, simply by applying different strategies: more elaborated reduction sequences in case of bifaces and simple reduction sequences to obtain cleavers. Fig. 2. . Simplified geologic map of the Lower Tagus Cenozoic basin, adapted from the Carta Geológica de Portugal, 1/500000, 1992). The study area (comprising the Vale do Forno and Vale de Atela sites) is located on the more upstream sector of the Lower Tagus River reach IV, between Arripiado and Chamusca villages. 1 – alluvium (Holocene); 2 – terraces (Pleistocene); 3 – sands, silts and gravels (Paleogene to Pliocene); 4 – Sintra Massif (Cretaceous); 5 – limestones, marls, silts and sandstones (Mesozoic); 6 – quartzites (Ordovician); 7 – basement (Proterozoic to Palaeozoic); 8 – main fault. The main Portuguese reaches of the Tagus River are identified (I to V). The VF3 site (Milharós), containing a Final Acheulian industry, with fine and elaborated bifaces) found in a stratigraphic level located between the T4 terrace deposits and a colluvium associated with Late Pleistocene aeolian sands (32 to 12 ka), has an age younger than ca. 154 ka but much older than 32 ka. In the study area, the sedimentary units of the T4 terrace seem to record the river response to sea-level changes and climatically-driven fluctuations in sediment supply. REFERENCES Cunha P. P., Almeida N. A. C., Aubry T., Martins A. A., Murray A. S., Buylaert J.-P., Sohbati R., Raposo L., Rocha L., 2012, Records of human occupation from Pleistocene river terrace and aeolian sediments in the Arneiro depression (Lower Tejo River, central eastern Portugal). Geomorphology, vol. 165-166, pp. 78-90.

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RESUMO Esta comunicação integra-se numa investigação no âmbito das humanidades digitais, uma transdisciplina recente que procura adequar os métodos das Ciências Humanas às novas tecnologias. Os acervos patrimoniais móveis têm vindo a ser digitalizados, inseridos em sistemas de informação e progressivamente disponibilizados em linha, permitindo um acesso global e ubíquo à informação. A fase seguinte é a otimização deste acesso, aplicando-o a um espólio de objetos do culto católico, em função das exigências e das expetativas dos investigadores de Humanidades e, com isso, prosseguir na construção do “museu imaginário” idealizado por Malraux.

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Introduction: Cartilage degradation biomarkers are a potential tool for early diagnosis of degenerative joint disease (DJD). In young horses, Coll2-1 and Coll2-1NO2 have been studied in serum and reported to be useful in the assessment of joint disease. Fib3-2 has been described to be higher in serum of humans with osteoarthritis but was never assessed in horses. The aim of the current study was to evaluate biomarkers’ changes with age, sex and exercise and correlate them with DJD. Material and Methods: Blood collection and radiographic examination were performed in 51 Lusitanian horses. Moreover, inertial sensor-based detection of lameness was used to assess pain together with subjective examination. Results: Females presented significantly higher concentrations of Coll2-1 (p = 0.015) and Coll2-1NO2 (p = 0.014) compared to males. We have found significant influence of high level of work in lower concentration of Coll2-1 (p = 0.001) and significant influence of sex in concentration of Coll2-1NO2 (p = 0.030). There was no influence of sex, age and work on Fib3-2. All biomarkers were increased in the DJD group (n= 35) compared to healthy controls (n = 16). This difference was significant for Coll2-1 (p = 0.015). When sorted by sex and age groups, significant difference in Coll2-1 between disease and healthy controls disappeared in old horses and females. Discussion/ Conclusion: Coll2-1 is a good marker of cartilage degradation in horses with DJD, being more specific in young horses and males. Fib3-2 may be further explored to help identify disease in particular cases.

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In Portugal, Veterinary Pathology is developing rapidly, and in recent years we assist to the emergence of private laboratories and the restructuring of universities,polytechnics and public laboratories.The Portuguese Society of Animal Pathology,through its actions and its associates has been keeping the discussion among its peers in order to standardizethe criteria of description,classification and evaluation of cases which are the subject of our daily work.One of the last challenges is associated with the use of routine histochemical techniques and immunohistochemistry, in an effort to establish standardized panels for tumour diagnosis, which could eventually reduce each analysis cost.For this purpose a simple survey was built, in which all collaborators answered questions about the markers used for carcinoma, sarcoma and round cell tumour diagnosis, as well as general questions related with the subject. We obtained twenty-one answered to the questions, from public and private laboratories.In general, in most cases immunohistochemical and histochemical methods are used for diagnosis.The wide spectrum cytokeratins are universally used to confirm carcinoma, and vimentin for sarcoma. The CD3 marker is used by all laboratories to identify T lymphocytes. For the diagnosis of B-cell lymphoma, the marker used is not consensual. In each laboratory there are different markers for more specific situations and only two labs perform PCR techniques for diagnosis. These data will be presented to promote extended discussion,namely to reach a consensus when different markers are used.

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Solving a complex Constraint Satisfaction Problem (CSP) is a computationally hard task which may require a considerable amount of time. Parallelism has been applied successfully to the job and there are already many applications capable of harnessing the parallel power of modern CPUs to speed up the solving process. Current Graphics Processing Units (GPUs), containing from a few hundred to a few thousand cores, possess a level of parallelism that surpasses that of CPUs and there are much less applications capable of solving CSPs on GPUs, leaving space for further improvement. This paper describes work in progress in the solving of CSPs on GPUs, CPUs and other devices, such as Intel Many Integrated Cores (MICs), in parallel. It presents the gains obtained when applying more devices to solve some problems and the main challenges that must be faced when using devices with as different architectures as CPUs and GPUs, with a greater focus on how to effectively achieve good load balancing between such heterogeneous devices.

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O livro contém uma síntese histórica sobre a ação da Companhia de Jesus em Portugal desde a sua fundação ( século XVI) até à atualidade.

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RESUMO ABSTRACT Comunicações orais e Posters Oral communications and posters Este formulário, após preenchido, e aceites as condições descritas no regulamento das Comunicações orais e Posters deve ser enviado para isnr@porto.ucp.pt After complete this form and accept the conditions described in the oral communications and posters regulation, please sent to isnr@porto.ucp.pt Tipo de comunicação (comunicação oral ou poster): Comunicação oral Type of communication: (oral communication or poster): Oral comunication Título (Title): “CAPACITAR O DOENTE ONCOLÓGICO COM DOENÇA AVANÇADA E/OU O CUIDADOR PARA A GESTÃO DA DOR EM DOMICÍLIO” “EMPOWER THE ONCOLOGIC PATIENT WITH ADVANCED DISEASE AT HOME AND/OR THE CAREGIVER FOR THE MANAGEMENT OF PAIN” Autoria (Authors): CORREIA, Isabel* (doutoranda em Enfermagem na Universidade de Lisboa) LOPES, Manuel (orientador do projeto) Afiliação dos autores (Authors affiliation): – Professora adjunta na Universidade de Évora, Escola Superior de Enfermagem de São João de Deus de Évora, doutoranda em enfermagem Universidade de Lisboa - – Professor Doutor em Enfermagem, Diretor da Escola Superior de Enfermagem de São João de Deus de Évora, Universidade de Évora E-mail: icorreia@uevora.pt - 964078445 mjl@uevora.pt Resumo (3000 caracteres com espaços) INTRODUÇÃO Um dos sintomas mais frequentes no doente oncológico com doença avançada é a dor. Segundo Palliative Care in European, a dor oncológica, tem uma importância especial porque o cancro é a segunda causa de morte em Portugal e por existir dor moderada a intensa em mais de 90% dos doentes em situação oncológica terminal. O desenvolvimento de um programa estruturado de intervenção de enfermagem que vá de encontro às necessidades do doente oncológico com doença avançada e/ou cuidador, relativamente à gestão da dor, poderá ter um impacto muito significativo no controlo da dor e de outros sintomas. OBJETIVOS Avaliar o efeito de um programa de Intervenção de Enfermagem na capacidade de gestão da dor por parte do doente oncológico com doença avançada e/ou o cuidador em domicílio. MATERIAIS E MÉTODOS A implementação do programa tem a duração prevista para 6 semanas. Compreende duas sessões educativas, três telefonemas e uma sessão de avaliação final. O programa foi elaborado, após uma Revisão sistemática de Literatura, com base no programa “ THE PRO-SELF”, nas Orientações Genéricas preconizadas pelo Plano Nacional de Luta Contra a dor e na Intervenção de enfermagem “Controle da Dor” da Nursing Intervention Classification (NIC). RESULTADOS O projeto encontra-se na fase de implementação e avaliação do programa educativo. No início os doentes não apresentam informação relativamente à gestão da dor, no final demonstram capacidade para a monitorização da dor e de outros sintomas e para a gestão da terapêutica, realizando os registos num diário de bordo. A literacia, a situação clínica e a disponibilidade interferem na capacidade de gestão. A proximidade da morte e a alteração do estado de consciência interferem na autonomia e na tomada de decisão. CONCLUSÃO Em fase de colheita e análise de dados. REFERÊNCIAS BIBLIOGRÁFICAS 1. FREIXO, Manuel. Metodologia Cientifica - Fundamentos, Metodos e Tecnicas. s.l. : Piaget, 2011. 2. Bulechek, Gloria M. e etal. Classificaçaõ das Intervenções de Enfermagem (NIC). Rio de Janeiro : elsevier, 2010. 3. Tsigaroppoulos, T. e etal. Problems faced by relatives caring for cancer patients at home. International Journal Of Nursing Practice. 15, 2009, Vol. 1, Nursing Pratice. 4. west, C.:Dodd,M., et al. Pain Control Program-an effective approach for cancer pain management. Oncology Nursing Forum. 1, 2003, Vol. 30, Oncology Nursing. 5. NR/rdonlyres/6861126B-C57A-46E1-B065-316C0CF8DACD/0/ControlodaDor.pdf, . (2008). . Consultado em 30 de Novembro de 2012 a partir de. Direcção-Geral da Saúde . http://www.portaldasaude.pt. [Online] 2008. [Citação: 30 de Novembro de 2012.] http://www.portaldasaude.pt/NR/rdonlyres/6861126B-C57A-46E1-B065-316COCF8DACD/0/Controlodador.pdf . Abstract (3000 characters with spaces) INTRODUCTION One of the most frequent symptoms in oncological patient with advanced disease is pain. According to Palliative Care in European, oncological pain, has a special importance because the cancer is the second most common cause of death in Portugal and there is moderate to severe pain in more than 90 % of patients in oncological terminal situation. The development of a structured program of nursing intervention that will meet the needs of the oncological patient with advanced disease and/or caregiver at home on pain management, will be able to provide for the management of pain, increasing knowledge for the control of pain while minimizing the associated symptoms that influence the quality of life of the patient and the caregiver's anxiety. PURPOSE/GOAL/AIM To evaluate the effect of an educational program of Nursing Intervention on pain management by the oncological patient with advanced disease and/or caregiver. RESEARCH/PROBLEM What is the effect of a structured program of nursing intervention directed to the patient and/or oncological patient caregiver with advanced disease at home, in the management of pain? METHODOLOGY Almost experimental study, with assessment of the management capacity of the oncological patient pain with advanced disease at home and/or informal caregiver, before and after the intervention of nursing (educational program) and transverse evaluation throughout the study. Population: oncological patients with advanced disease at home, with more than 18 years, and or family caregiver, attending an Oncology Unit – Hospital during the day. RESULTS Made an application in an Oncology service in oncological patients with advanced disease at home, it was found that at the beginning the patients did not present information regarding pain management, at the end demonstrated capacity for monitoring of pain and other symptoms and therapeutic management, performing a logbook records. CONCLUSION In the process of collection and analysis of data. KEYWORDS Educational Program; oncological patient; oncological pain.

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O nemátode da madeira do pinheiro (NMP), Bursaphelenchus xylophiius, tem uma extensa distribuição na América do Norte, e encontra-se atualmente distribuído ao longo da maioria dos territórios de Canadá e dos Estados Unidos. Durante o último século, esta espécie foi transportada pelo Homem para outras regiões do mundo (não-nativas), associadas com o comércio e o fluxo global de produtos de origem florestal. Atualmente, esta espécie invasiva está reportada para algumas regiões do SE asiático (China, Japão, Coreia e Taiwan) e mais recentemente para a Europa (Portugal). Devido ao impacto que este organismo agente da doença da murchidão dos pinheiros causa nas florestas nativas destas regiões esta espécie assume uma elevada importância económica a nível mundial Em Portugal, a distribuição do NMP encontra-se confinada a uma área restrita e limitada (500 000 ha), a sul de Lisboa (península de Setúbal); contudo, constitui uma das maiores ameaças às florestas de pinheiro do país e da UE. Ate recentemente, nenhum consenso existia quanto à origem do NMP em Portugal. Diversas hipóteses têm sido colocadas para explicar esta introdução, nomeadamente a partir de zonas onde o nematode ocorre naturalmente (América do Norte), ou de outras áreas (não-nativas) onde o nematode se comporta como uma espécie invasiva (Leste da Ásia). A fim de avaliar a variabilidade genética do NMP proveniente da área afetada em Portugal, foram utilizadas várias técnicas moleculares, designadamente o random amplified polymorphic DNA (RAPD-PCR) e o satellite DNA (satDNA). No caso do RAPD-PCR, foram utilizados 24 isolados do NMP provenientes de Portugal, 1 proveniente da América do Norte e 1 da Ásia, tendo sido utilizado como out-group um isolado de B. mucronatus. A partir dos 28 RAPD primers utilizados obtiveram-se 640 fragmentos. No caso do satDNA, foram utilizados 21 isolados do NMP provenientes de Portugal, obtendo-se no total 206 sequências da família MspI. Ambos os métodos revelaram uma elevada similaridade genética entre os vários isolados do NMP da área afetada em Portugal O nível reduzido de diversidade genética obtido entre os isolados portugueses do NMP, permite concluir que se trata de uma única introdução deste organismo em Portugal, e proveniente de uma região asiática. A inexistência de uma de correlação entre a variabilidade genética e a distribuição geográfica do NMP dentro da área afetada em Portugal, indica que o NMP se encontra distribuído de forma uniforme ao longo de toda a área afetada, provavelmente relacionado com a distribuição e a expansão natural do inseto vector. The pinewood nematode (PWN), Bursaphelenchus xylophilus, has a wide distribution in North America, and is present throughout most of the territories of Canada and the United Stata. During the last century, this species has been transported by man to several non-native regions of the world, associated with trade and the global flow of forest products. Up to date, this invasive species has been reported from Asia (PR China, Japan, Korea and Taiwan) and more recently in Europe (Portugal). Due to the impact on native pine forests of these regions, this nematode species, the causal agent of pine wilt disease, is of great economic importance worldwide. In Portugal, the distribution of the PWN has been constrained to a relatively small area (500 000 ha) in the south of Lisbon (Setúbal Peninsula); however, it has become the most serious threat to pine forests in the country. Until recently, no consensus had emerged on the possible pathway of the PWN introduction in Portugal. Several hypotheses have been put forward to explain this introduction, such as an origin from endemic areas where the nematode naturally occurs (North America), or non-endemic areas where the nematode behaves as an exotic pest (East Asia). Random amplified polymorphic DNA (RAPD-PCR) and satellite DNA (satDNA) techniques were used in order to assess the level of genetic variability and genetic relationships, among several isolates of the PWN, representative of the entire affected area in Portugal. In the case of RAPD-PCR, 24 Portuguese isolates, plus two additional isolates of B. xylophilus, representing North America and East Asia were included. B. mucronatus was used as an out-group. Twenty-eight random primers generated a total of 640 DNA fragments. With satDNA, 206 Mspl sequence repeats were obtained from 21 Portuguese isolates of B. xylophilus. Both molecular methods revealed a high genetic similarity among the Portuguese isolates, and the low level of genetic diversity strongly suggests that they were dispersed recently from a single introduction, and from East Asia. The lack of apparent relationship between the genetic variability and the geographic distribution of the PWN within the affected area, suggests that the recent introduction of this pest (and pathogen) in Portugal has been uniformly distributed since its establishment, probably following the natural distribution and expansion of the insect vector.

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Abstract text Introduction: Cysticercosis results from the ingestion Taenia solium eggs directly by faecal-oral route or contaminated food or water. While, still considered a leading cause of acquired epilepsy in developed countries, this zoonosis has been controlled or eradicated in industrialized countries due to significant improvements in sanitation, pig rearing and slaughterhouse control systems. Objectives: the health burden of human cysticercosis in Portugal. Material and Metodes: We developed a retrospective study on human neurocysticercosis (NCC) hospitalisations based on the national database resulting from National Health Service (NHS) hospital episodes except those of Madeira and Azores Islands. Results: Between 2006 and 2013 there were 357 hospitalized NCC cases in Portugal. Annual frequency of cases between 2006-2013 kept stable (mean 45). NCC was most frequent in those aged 25-34 years (59; 16,5%) and those >75 years (65; 18,2%). Overall, mean age was 47,3 years (median age 45, standard deviation 41,1, mode 28) and 176 cases were in males (49,3%); no significant differences were observed between age and gender (t-student, p>0,05). In Norte Region cases tended to be older than in Lisboa and Vale do Tejo Region. Conclusions: The Directorate-General of Health established the National Observatory of Cysticercosis and Teniiasis which will define criteria for NCC cases monitoring and surveillance (hospitalized and non-hospitalized cases).

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R&D investments are seen has having an enormous potential impact on the competitive position of regions and perhaps on regional convergence (or divergence) too. The aim of the paper is to study both the localization of R&D investments and regional income distribution among the NUTs 3 regions of Portugal to conclude if these variables are related or not. To study the spatial convergence (approximation) of per capita income (GDPpc) and R&D investments in the regions of Portugal, we use a standard methodology of spatial econometrics. We conclude that regions with higher GDPpc are not the same with the highest concentration of R&D investments, with the exception of the northern coastline. The R&D investments are geographically linked to the network of higher education institutions, especially in the interior regions of the country. The northern regions reveal more dynamic in terms of R&D, which apparently is not felt in the population's standard of living measured by GDPpc.

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In the Vi la de Rei arca (Central Portugal) the continental deposits ofthe Lower Tagus Tertiary 8asin lay upon the pediment of me Portuguese Central Chain. Three ronglomerate units are recorded from me base upwards. separated by regional or basinal unconfonnities: Conglomerados de Rio de Moinhos (RM); Conglomerados de Serra de Almeirim (SA) and Conglomerados de Vila de Rei (VR). The first two units (KM and SAl have been si les of gold exploitation in huge optn pit mines probably dunng Roman colonisation times. The contact ofthis units, on thc Paleozoie basement or on the Paleogene unil Grés de Monsanto, is unconfonn, defining in both limits a large nondepositional andlor erosional hiatus. Those conglomerates seal the scdimcntation ofthe Lower Tagus Tertiary Basin along irs northem border. Taking lnto account lhe significance /lssigned to their basinal unconfonnity limits, lhe uplift ofthe Portuguese Centra! Chain. and thc facl ofthis continental units yielded no fossils with chranostratigraphic significanee, they have been eonsidered ranging fram Uppcr Miocene to lhe beginning ofthe Qualemary. Finally, a lithostratigraphic equivalence with lhe Neogenic units ofthc Bierzo and Duema basins (NW ofthe Iberian Peninsula), where exploitalions from Roman limes are also evident, is presented.

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The Alcantarilha lowland, partly barred by a well developed barrier, including foredunes covering Pleistocene-Holocene beachrock and aeolianite, develops across the Alcantarilha infilled estuary, the beach-dune extending further SE until the Salgados lagoon. A topographic and coring survey revealed a peculiar feature at the leeward toe of the dune ridge close to the inlet area: a sandy fan with location, shape and morphology suggesting emplacement by single or multiple overwash of the barrier tip rather than tidal forcing. Its storm or tsunami origin and age are under investigation, and the only time-constrain available at present is that it should post-date ca. 6600 cal BP, the most recent in situ aeolianite (Moura et al., 2007) dated so far. METHODS, DATA SET AND RESULTS The fan boundaries are distinctive in aerial photos and satellite images: it is roughly ellipsoidal, ~200 m wide and ~300 m elongated paralleling the shoreline, rising ~ 0.9-1.2 m above the surrounding floodplain surface. Detailed topography shows that its short axis aligns with SW-NE elongated (though irregular) depressions in the dune crest, which link the beach with the fan. This could have favoured funnelling of, or erosion by, water overtopping the barrier but, in either case, the fan should correspond to extreme and abrupt event(s) of coastal flooding. 18 trenches and cores were performed in the exposed area of the fan and nearby flood plain to obtain samples and data on its sedimentology, lithostratigraphy and geometry. The fan consists of well sorted and rounded sand (Fig. 2). It thins away and wedges out landwards of the apex (located near Alc29T) where it is partly covered by dune sand. Its lower boundary is undulating and marked by textural contrast between sand (fan) and underlying mud (alluvial/lagoonal); an accumulation of marine-sourced perforated pebbles showing limited lateral continuity may pinpoint this boundary near the foredune (core Alc 25, ca. 80 m westward of profile in Fig.1); mud-balls were also observed immediately above this surface in cores and trenches. As the washover was probably emplaced in a barred lagoonal/estuarine floodplain setting, the fan’s northern outer belt is enclosed by low-energy sediments (not shown in Fig. 2).

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Portugal regista atualmente um dos mais baixos níveis de fecundidade da Europa e do mundo, resultado da redução do número de filhos e do adiamento dos nascimentos para idades mais tardias. As características individuais e a idade ao nascimento do primeiro filho são determinantes cruciais para o número de filhos que se tem e que se espera ter, variando em função do grau de instrução. Apesar das alterações comportamentais ao longo das últimas décadas, os contextos familiares e a conjugalidade continuam a ser centrais na vida dos portugueses, pois aqueles que não vivem com cônjuge ou companheiro apresentam fecundidades mais baixas. A dimensão familiar ideal é outro determinante crítico, dado que ideais mais baixos potenciam que se tenha menos filhos, dificultando a recuperação da fecundidade. O ideal parece corresponder ao número de filhos que permite manter um determinado nível de vida para a família e ainda garantir aos filhos mais oportunidades, mesmo que para tal se tenha apenas um filho. Daí também a atual relevância das questões económicas nas decisões de fecundidade. A alteração de mentalidades parece ter gerado um novo modelo social marcado por uma crescente valorização dos filhos.