Coherence and phase locking disruption in electromyograms of patients with amyotrophic lateral sclerosis

Dissertação para obtenção do Grau de Mestre em Engenharia Biomédica

Contribuição para o estudo da anexina V na apoptose celular em concentrados de eritrócitos

A hemoterapia moderna baseia-se na utilização correcta dos diversos componentes sanguíneos, associados a um maior controle de qualidade do sangue, o que a torna mais segura e, actualmente, muitos doentes sao beneficiados pois, a transfusão de componentes sanguineos, em situaçoes várias, está na linha da frente na manutenção da vida e em casos extremos, o último recurso que salva vidas. A qualidade e a segurança nas transfusões de sangue são grandes preocupações da área médica, autoridades de saúde e doente1. O sangue obtido pelos Centros de Sangue provem de dadores voluntários, dotados de uma enorme sensibilidade social, que periodicamente assumem uma postura benevola e altruista e consequentemente mantêm os bancos de sangue providos de um produto imprescindivel no tratamento de diversas patologias. O produto final disponível – concentrado de eritrócitos (CE´s), plasma e concentrado plaquetário – tem de assumir um carácter seguro e viável de modo a que os riscos para o doente sejam diminutos2. O controlo de qualidade aplicado a todo o sangue doado realiza provas de conformidade nas unidades com especificações previamente definidas, sendo a hémolise um dos parâmetros importantes na avaliação da qualidade dos concentrados de eritrócitos, pois, pode ocasionar implicações clinicas para o receptor. Para além disso a avaliação da concentração de hemoglobina (Hg) no sangue doado mostra-se um controlo imprescindivel que salvaguarda a qualidade e segurança do componente a transfundir3;4.Até se obter um CE há todo um processo moroso e de responsabilidade vital. Todo o sangue obtido passa por várias etapas fundamentais até à obtenção do componente pretendido (analise, produção e armazenamento). Os CE’s obtidos quando armazenados, num ambiente de refrigeração, têm uma vida útil de 42 dias. Após este período, o sangue deve ser inutilizado por se verificar alterações bioquímicas, biomecânicas, e imunológicas nos CE’s e por consequência a sua instabilidade vital no que ao tratamento de patologias, para as quais este componente está indicado, diz respeito5. Foi realizado um estudo experimental com o objetivo de avaliar a contribuição da Anexina V na apoptose celular nos concentrados de eritrócitos, constatando a degradação dos mesmos ao longo de todo o período de armazenamento e validar o paradigma que a ciência preconiza: “Os CE’s após os 42 dias armazenados, em condições específicas (2 a 6º centígrados), são inviaveis para transfundir”6;7. A avaliação dos níveis de apoptose por citometria de fluxo é geralmente realizada por métodos que utilizam Anexina V como marcador vital, que se associa aos resíduos de fosfatidilserina, externalizados no início do processo apoptótico. A Anexina V é uma proteína humana endógena dependente do ião Ca+2, amplamente distribuída intracelularmente em altas concentrações na placenta e em concentrações mais baixas nos eritrócitos, plaquetas e monócitos. Apresenta como principal característica a capacidade de se ligar à fosfatidilserina, um fosfolipído presente na camada interna da bicamada lipídica, que durante a apoptose celular é translocada para a camada externa da membrana celular. A determinação da Anexina V é normalmente utilizada para verificar se as células são viáveis, apoptóticas ou necróticas por meio de diferenças na integridade da membrana plasmática. Assim, ao conjugar a Anexina V ao FITC (Isotiocianato de fluoresceína) é possível identificar e quantificar as células apoptóticas por citometria de fluxo7. Numa amostra de 15 CE’s, a qual foi induzida a hemólise, verificou-se, por citometria de fluxo, que a viabilidade deste componente se desvanesce ao longo do tempo, confirmando assim que o tratamento, manuseamento e armazenamento do sangue compromete a vitalidade terapeutica deste insubstituivel produto vital.

Fisheries Safety Management

Fisheries is one of the most dangerous professions in the world. Fatal accidents and injuries in the fisheries are characterized as well as particular circumstances that may cause or aggravate the risk of accidents. Aspects of safety management of fishing vessels are covered in this paper: areas of concern when doing a risk assessment in fishing vessels, fundamental elements on a safety management system for the fisheries and the need for international and national level instruments as well as legal and compulsory measures

An approach to health and safety in E.U. forestry operations – Hazards and preventive measures

Forestry in general and logging in particular continue to be among the three most hazardous sectors in European countries. The aim of this article is to characterize health and safety problems and solutions in E.U. forestry operations, and particularly in Portuguese operations. Forest types, production, employment and ownership are used to characterize the forest sector. Forestry accidents and health problems data are mentioned. Typical hazards associated to the nature of logging operations are systematized. Preventive measures, focused on a wide spectrum of measures, making safety considerations an integral feature of all operational activities from planning to organization to execution and supervision of work are emphasized in this article.

The Neogene of the Lower Tagus Basin (Portugal)

Revista Española de Paleontologia 19 (2), 229-242

The Serravallian-Tortonian boundary in the lower Tagus Basin (Portugal) and the new GSSP of the Tortonian stage

Revista electrónica de Ciências da Terra,http://e-terra.geopor.pt,Geociences on-line journal, Vol. 6, nº1

Is ambient intelligence a truly human-centric paradigm in industry? Current research and application scenario

Based on the paper presented at the International Conference “Autonomous Systems: inter-relations of technical and societal issues”, organized by IET with the support of the Portuguese-German collaboration project on “Technology Assessment of Autonomous Robotics” (DAAD/CRUP) at FCT-UNL, Biblioteca da UNL, Campus de Caparica on 5-6 November 2009.

A stratigraphic framework for the Miocene from the lower Tagus Basin (Lisbon, Setúbal Península, Portugal) Depositional sequences, biostratigraphy and isotopic ages

Rev. Soc. Geol. España, 12(1), ano 1999

Trypanites ichnofacies: palaeoenvironmental and tectonic implications. A case study from the miocene disconformity at Foz da Fonte (lower Tagus basin, Portugal)

Palaeogeography, Palaeoclimatology, Palaeoecology 292, 35–43

Aplicação do Método SFA (Safety Function Analisys) a um. Posto de Transformação de Energia Eléctrica da Renova

Riscos Industriais e Emergentes, 2009 pp. 827-844

Bio and magnetostratigraphy of two Lower Miocene sections, Tagus basin (Portugal)

The magnetostratigraphy of two sections in early Miocene marine deposits of the Tagus Basin is studied. Thermal demagnetization was used to isolate the primary component of magnetization for 45 samples from the Foz da Fonte section, and for 74 others from Trafaria section. The succession of the polarity zones found in these sections is tentatively correlated with the geomagnetic polarity time scale (GPTS) on the basis of the biostratigraphic data yielded by planktic Foraminifera. The planktic zones and magnetic polarities recognized in these sections can be adequately correlated with the part of the GPTS [table calibrated by BERGGRENET al. (1985)] corresponding to the Anomalies 6 and 5E (Foz da Fonte) and 5D (Trafaria). This correlations suggests ages between 19,35 and 18,14 Ma for Foz da Fonte section, and 17,90 to 16,98 Ma for Trafaria.

The Cristo Rei section (Lower Miocene). Distal fluviatile environments in a marine series, plants, vertebrates and other evidence, age

The section at Cristo Rei shows sandy beds with intercalated clayey lenses (IVb division from the Lisbon Miocene series) that correspond to a major regression event dated from between ca. 17.6 and 17 Ma. They also correspond to a distal position (relatively to the typical fluviatile facies in Lisbon), nearer the basin's axis. Geologic data and paleontological analysis (plant fossils, fishes, crocodilians, land mammals) allow the reconstruction of environments that were represented in the concerned area: estuary with channels and ox-bows; upstream, areas occupied by brackish waters where Gryphaea griphoides banks developped; still farther upstream, freshwaters sided by humid forests and low mountain subtropical forests under warm temperate and rainy conditions, as well as not far away, seasonally dry environments (low density tree or shrub cover, or steppe).

High resolution stratigraphy and miocene facies correlation in Lisbon and Setúbal Peninsula (Lower Tagus basin, Portugal)

Correlation between facies associations (marine, estuarine and distal fluviatile environments) and disconformities, observed between Foz da Fonte (SW of Setúbal Peninsula) and Santa Iria da Azóia (NE of Lisbon) are presented. The precise definition of the marine-continental facies relationships improved very much the chronology of the depositional sequence boundaries. Tectonic and eustatic controls are discussed on the basis of subsidence rates variation.

Miocene sediments from Foz da Fonte and Penedo sections (Lower Tagus basin): clay minerals and isotopic data

Eight depositional sequences (DS) delimited by regional disconformities had been recognized in the Miocene of Lisbon and Setúbal Peninsula areas. In the case of the western coast of the Setúbal Peninsula, outcrops consisting of Lower Burdigalian to Lower Tortonian sediments were studied. The stratigraphic zonography and the environmental considerations are mainly supported on data concerning to foraminifera, ostracoda, vertebrates and palynomorphs. The first mineralogical and geochemical data determined for Foz da Fonte, Penedo Sul and Penedo Norte sedimentary sequences are presented. These analytical data mainly correspond to the sediments' fine fractions. Mineralogical data are based on X-ray diffraction (XRD), carried out on both the less than 38 nm and 2 nm fractions. Qualitative and semi-quantitative determinations of clay and non-clay minerals were obtained for both fractions. The clay minerals assemblages complete the lithostratigraphic and paleoenvironmental data obtained by stratigraphic and palaeontological studies. Some palaeomagnetic and isotopic data are discussed and correlated with the mineralogical data. Multivariate data analysis (Principal Components Analysis) of the mineralogical data was carried out using both R-mode and Q-mode factor analysis.

High-resolution correlation of coastal cliff sections in the Lagos- Portimao Formation (Lower - Middle Miocene, central Algarve, Portugal)

This paper describes a high-resolution stratigraphic correlation scheme for the early to middle Miocene Lagos-Portimão Formation of central Algarve, southern Portugal. The Lagos Portimão-Formation of central Algarve is a 60 m thick package of horizontally bedded siliciclastics and carbonates. The bryozoan and mollusc dominated biofacies is typical of a shallow marine, warm-temperate climatic environment. We define four stratigraphic marker beds based on biofacies, lithology, and gamma-ray signatures. Marker bed 1 is a reddish shell bed composed predominantly of bivalve shells in various stages of fragmentation. Marker bed 2 is a fossiliferous sandstone / sandy rudstone characterized by bryozoan masses. Marker bed 3 is also a fossiliferous sandstone with abundant larger foraminifers and foliate bryozoans. Marker bed 4 is composed of three distinct layers; two fossiliferous sandstones with an intercalated shell bed. The upper sandstone unit displays thickets of the bryozoan Celleporaria palmate associated with the coral Culizia parasitica. This stratigraphic framework allows to correlate isolated outcrops within the stratigraphic context of the Lagos-Portimão Formation and to establish high resolution chronostratigraphic Sr-isotopic dating.