La construction de l'europe sociale entreprises, territoires, circulation de main d'oeuvre

The building of social Europe: companies, territories, movement of the workforce. For ten years, companies have been obliged to standardize the quality of their products interaationally, which goes along with a dismantling of the landmarks of the territories of political action in France. This article presents some current research about the movement of the labour force in Europe and raise the issue of coordination between the different legitimate categories and the attitude of the various administrations (work, health) concemed by this phenomenon.

Estudo Estratigráfico e Paleontológico do Jurássico do Algarve Ocidental

Algarve Province, Southern Portugal, corresponds in part to a meso-cenozoic basin running along the coast from Cabo S. Vicente to beyond Spanish border. Structurally it is a big monocline plunging southwards much deformed mainly by two East-West longitudinal flexures. Lithostratigraphical and chronostratigraphical studies dealt specially with Jurassic formations. This and the geological mapping of the post-Hercynian sedimentary formations allow us to define the following units: Triassic-Lower Liassic Arenitos de Silves (Silves sandstones sensu P. Choffat, pro parte) - At their base the Silves sandstones (0-150m) are represented mainly by cross-bedded red sandstones. This unit is Upper Triassic (Keuper) in age, on the evidence of some Brachiopoda. Complexo margo-carbonatado de Silves (Silves marl-limestone complex=Silves sandstones sensu P. Choffat, pro parte) (80-200m) overlies the preceding, it may be reported to the Upper Triassic-Hettangian. It consists of a thick pelite-marl-dolomite-limestone series with many intercalations of greenstones. Since no fossils were found it is not possible to conclude whether it is still Hettangian or if it does correspond, in the whole or in part, already to the Sinemurian. Liassic Dolomitos e calcários dolomíticos de Espiche (Espiche dolomite-rocks and dolomitic-limestones) - The usually massive and finely crystalline or saccharoidal dolomites and dolomitic-limestones are the toughest strata of the Algarve margin giving rise to several hills. Its thickness attains in certain points 60 metres at least. Based on geometry and on lithological similarities with the carbonated complex of the northern basin of Tagus river (Peniche, São Pedro de Muel, Quiaios), this formation can be accepted as Sinemurian in age. As it happens with the carbonated complex, here also the first dolomite beds are non-isochronal throughout the region; upper time-limit of the dolomitic facies is either Lower Carixian, Lower Toarcian or even Lower Dogger. The dolomitization is secondary but not much later than sedimentation. However, between Cabo S. Vicente-Vila do Bispo there is evidence of an even later secondary dolomitization related to the regional fault complex. Calcário dolomítico com nódulos de silex da praia de Belixe (Belixe beach dolomitic-limestone with silex nodules) (50-55m) - Ascribed to Lower or Middle Carixian on the basis of Platypleuroceras sp., Metaderoceras sp. nov. and M. gr. Venarense. Calcário cristalino compacto com Protogrammoceras, Fuciniceras e ? Argutarpites de Belixe (Belixe compact crystalline limestone with Protogrammoceras, Fuciniceras and ? Argutarpites) (30m) - Ascribed to Lower Domerian. Middle and Upper Domerian are indicated but by a single specimen of ? Argutarpites. Calcários margosos e margas com Dactylioceras semicelatum e Harpoceratídeos de Armação Nova (Armação Nova marly limestones and marls with D. semicelatum and Harpoceratidae) (25m) -Ascribed to Lower Toarcian. Middle and Upper Toarcian formations are not known in the Algarve. Dogger Calcários oolíticos, c. corálicos, c. pisolíticos, c. calciclásticos, c. dolomíticos e dolomitos de Almadena (Almadena oolitic-limestones, coral-reef-limestones, pisolite-limestones, limeclastic-limestones, dolomitic-limestones and dolomite-rocks) (more than 50 metres), with lagoonal facies. Ascribed to Aalenian-Bathonian-? Callovian. Margas acinzentadas e calcários detríticos com Zoophycos da praia de Mareta (Mareta beach greyish marls and detritical limestones with Zoophycos) (40m) - Pelagic transreef facies with Upper Bajocian and Bathonian ammonites. Calcários margosos e margas da praia de Mareta (Mareta beach pelagic marly-limestones and marls) (110m) - Ascribed to the Callovian on its ammonites. Malm Near Cabo S. Vicente and Sagres the first Upper Jurassic level consists of a yellowish-brown nodular, compact, locally phosphated and ferruginous, sometimes conglomeratic, marly limestone (0,35-1,50m) containing a rich macrofauna, which includes: 1) Callovian forms unknown at Lower Oxfordian; 2) Upper Callovian forms that still survived in Lower and Middle Oxfordian; 3) Lower Oxfordian forms (Mariae and Cordatum Zones); 4) Lower and Middle Oxfordian forms (Mariae to Plicatilis Zone); 5) Middle Oxfordian forms (plicatilis Zone), and some ones appearing in Middle Oxfordian. This condensed deposit is therefore dated from Middle Oxfordian (Plicatilis Zone). The other Upper Jurassic lithostratigraphical units were also mapped but their detailed study is not presented in this work. Correlations between lithostratigraphical and chronostratigraphical scales from P. Choffat, J. Pratsch, C. Palain and from the author are stated. Further correlations are attempted between zonc scales of Carixian-Lower Toarcian and Upper Bajocian-Middle Oxfordian of France, Spain (Asturias, Iberian and Betic Chains), Argel (Orania) and Portugal (northern Tagus basin and Algarve). The study of pyritous fossil assemblages common in Upper Bathonian-Lower Callovian marly levels of the praia da Mareta seems to suggest that these sediments were deposited in a bay or in an almost closed coastal re-entrance virtually without deep water circulation. Although such conditions may occur at any depth one may suppose that these ones actually correspond to an infralittoral neritic environment. The thaphocoenosis collected there are almost entirely composed of nektonic (ammonites, Belemnites) and planktonic (Bositra) faunas. The sedentary (crinoids, brachiopods) or free (sea-urchins, gastropods) epibenthonic forms are very scarce; endobenthonic forms are not known. The palaeontological study of all Nautiloids and Ammonoids of the Liassic and Dogger is presented (except Kosmoceratidae and Perisphinctaceae). Among the thirty one taxa dealt with, one is new (Metaderoceras sp. nov.) and the great majority of the others has been identified for the first time in Algarve. Some others have never been reported before in Portuguese formations. The evolution, during Jurassic times, of the sedimentary basins of the Portuguese plate margin is described. The absence of Cephalopods in the very extensive marly and dolomitic limestones, partly marine, suggests that, during Lower Liassic, palaeogeography underwent no great changes. Dolomitic-limestone with silex nodules from Cabo S. Vicente contain the first ammonites recorded at the base of the Middle Liassic. This facies, although very common in Tethys, is unknown north of the Tagus. The faunal assemblage has a mediterranean to submediterranean character. Comparisons between faunal assemblage" from Algarve with the ones known north of the Tagus show that communications between Boreal Europe and Tethys, virtually non-existent during Lower and Middle Carixian, became very easy during Lower Domerian. In earlier Pliensbachian times two distinct seas were adjacent to the Iberian plate. One, an epicontinental sea with a tethyan fauna, extended southwards from the Meseta margin. Another, was a boreal sea; during its transgressive episodes boreal faunas attained into the basin north of the Tagus. During Middle Carixian and Lower Domerian, owing to simultaneous transgressions, these two seas joined together allowing faunal exchanges along the epicontinental areas which limited the emerging hercynian chains belts. During Liassic, the Algarve belonged undoubtedly to the tethyan submediterranean province. The area north of the Tagus, on the contrary, was a complex realm where subboreal and tethyan affinities alternatively prevailed. In the Algarve the first Middle Jurassic deposits do frequently show lateral thickness reductions as well as unconformities contemporaneous with other generalized disturbances on the sedimentation processes in other parts of Europe. By this time, near Sagres, a barrier reef developed separating lagoonal or ante-reef facies from the transreef pelagic zone. The presence of tethyan fauna, the abundance of Phylloceratidae and the absence of boreal forms allow us to consider the Algarve basin as a submediterranean province. The presence of Callovian pelagic fossiliferous formations in the Loulé area shows that during Middle Jurassic the marl-limestone transreef sedimentation was not confined to the western Algarve. They would extend eastwards where they only can be seen in the core of some anticlines. This is due to the progressive sinking of the meso-cenozoic formations as we proceed towards the South of the Sagres-Algoz-Querença flexure. In the whole of the Peninsule, and as for the Middle Callovian, an important regression can be clearly recognized on the evidence of an erosion surface which strikes obliquely the Middle and Upper Callovian strata. The geographic boundaries of the different faunal provinces are not changed by the presence of many Kosmoceratidae in the phosphate nodules since they are but a minority in comparison with the tethyan forms. An abstract model can be constructed showing that in Western Europe the Kosmoceratidae may have migrated South and westwards through a channel of the sea that linked Paris basin to Poitou and Aquitaine. By migrating between the Iberian meseta and the Armorican massif this fauna reached northern Tagus basin at the beginning of Upper Callovian (Athleta Zone); this south and southwest bound migration would have proceeded, allowing such forms to reach Algarve basin only in latest Callovian times (Lamberti Zone). This migration means that during Middle Jurassic a widely spread North Atlantic sea would exist, flooding the western part of Portugal up to the Poitou.

O plano de deslocações urbanas e a resposta estratégica que falta aos PROTs e PDMs: A descentralização do planeamento do território e dos transportes

The sustainable urban mobility plan is the framework of planning and organisation of mobility system. It is a strategic and operational plan with consequences in the planning and organisation of territorial and transport systems. When it’s defining the principles and the objectives of sustainable development and when it’s working in the scenarios of modal shift more favourable to the alternative modes than the car, the planning and the organisation of territory will be integrated on the political of reduction of road circulation volumes, in the reduction of GEE, waste of space and time, in the improvement of quality of urban environment. The Urbanism Agencies and the Urban Transport Authorities will get their selves in the urban mobility plan, in territory scenarios development, mobility and transports, with the objective to understand the sustainable politics in the accessibilities which are available by the transportation bill. In Portugal, although the authorities are not yet working, the law (1/2009) recently approved in last December and published at the beginning of the year, they have the sustainable urban mobility plans forward in this strategy.

Assessment of climate change statistical downscaling methods: Application and comparison of two statistical methods to a single site in Lisbon

Dissertação apresentada na Faculdade de Ciências e Tecnologia da Universidade Nova de Lisboa para a obtenção do grau de Mestre em Engenharia do Ambiente

The making of saudade. National identity and ethnic psychology in Portugal

Roots and rituals.The construction of ethnic identities, Ton Dekker, John Helsloot Carla Wijers editors, p. 267-268; Selected papers of the 6TH SIEF conference on 'Roots & rituals', Amsterdam 20-25 April 1998.

Pliocene-quaternary upwelling in the SoutheasternAtlantic may reflect changes in water mass production

Proceedings of tile 1" R.C.A.N.S. Congress, Lisboa, October 1992

Os reais hospitais militares em Portugal administrados e fundados pelos Irmãos Hospitaleiros de S. João de Deus 1640-1834

RESUMO: Desde 1640 até data extrema de 1834, os Irmãos Hospitaleiros de S. João de Deus foram os responsáveis, directa e indirectamente, pela administração e corpo de enfermagem dos Reais Hospitais Militares em Portugal, actividades que analisamos ao longo dos séculos, desenvolvendo pressupostos temáticos relativamente a sua actuação no tempo e no espaço. É durante o séc. XVII até ao séc. XIX, que vemos os cuidados da corte para com a assistência aos soldados enfermos e doentes, ao publicar inúmera legislação relativamente à complexidade assistencial na área militar, a qual foi por nós compilada para melhor contextualização da importância dos Hospitais Militares em Portugal. Os Regimentos, os Alvarás, os Regulamentos e as Ordens do Dia, constituem um objecto fundamental de pesquisa e análise para caracterizar o quotidiano nesses mesmos locais. Os Hospitais Militares desde a sua fundação, dos primórdios das Guerras da Aclamação em 1640, até ao advento do liberalismo em 1834, eram centros de conhecimento técnico e científico com um corpo assistencial especializado, onde um conjunto pluridisciplinar de profissionais zelava qualitativamente pelos assistidos, e onde os Irmãos Hospitaleiros de S. João de Deus desempenhavam funções de administradores, enfermeiros e capelães. Nesse sentido elaboramos uma listagem cronológica para inter relacionar os Irmãos Hospitaleiros e os Hospitais Militares, pois é impossível separar a Ordem de S. João de Deus da componente assistencial aos enfermos e doentes militares em Portugal. A importância urbana e arquitectónica, que os Reais Hospitais Militares tiveram no contexto orgânico e defensivo nas Praças de Guerra, é realçado pela forma como estes se encontravam implantados e construídos, demarcando-se esteticamente da globalidade edificada, pois constituíam parte integrante dos equipamentos militares, como era teorizado pelos técnicos militares. Assim analisamos a localização dos imóveis, para além do próprio edifício hospitalar, com o meio, ou seja com a urbanidade das Praças de guerra. A sobriedade arquitectónica dos Hospitais Militares, integrada nos grandes ciclos das correntes culturais europeia e nacional, associada à riqueza decorativa e iconoclasta desenvolvida nesses locais, dá-nos uma dimensão da importância científica que esses núcleos assistenciais tiveram, contribuindo para a difusão do culto e circulação da imaginária de S. João de Deus em Portugal e dos Santos venerados nos Hospitais Militares. Desta forma compreendemos o alicerçar devocional que o reino tinha por este Santo, como o fundador do conceito assistencial do hospital moderno. Estando intrinsecamente ligado a este facto vemos o proliferar do culto e da imaginária de S. João de Deus em Portugal, centrando-se a iconografia artística do Santo em torno das localidades onde se enraizaram os Hospitais Militares. Hoje, nos imóveis hospitalares, não é difícil analisar uma lenta evolução da funcionalidade dos seus espaços, gravitando o desenvolvimento estrutural assistencial em torno das enfermarias e salas de cirurgia, mantendo-se perene este arquétipo arquitectónico desde o séc. XVII até meados do séc. XIX, as quais foram levantadas, comparadas e analisadas. Foi com a exclaustração das Ordens Religiosas, pelo Decreto de 29 de Maio de 1834, que acabou a extraordinária e valorosa acção administrativa, tutelar e corpo de enfermagem dos Irmãos Hospitaleiros de S. João de Deus, na área específica da assistência militar em Portugal, extinguindo-se, nalguns casos, os Hospitais Militares, pois o reino não estava preparado para substituir esses profissionais de saúde. O nosso estudo desenvolve-se por cerca de 295 anos, espaço temporal em que os Hospitais Militares foram administrados e fundados pelos Irmãos de S. João de Deus em Portugal.---------ABSTRACT: Since 1640 until 1834 the Hospitaller Brothers of S. John of God were the responsibles, direct and indirectly, for the administration and nursing body of the Royal Military Hospitals in Portugal, activities that we analyse throughout the centuries, developing thematic presuppositions regarding its performance in time and in space. It is during the 17th century until the 19th century, that we see the court’s care with the assistance of the wounded and sick by the publishing of much legislation regarding the assistance complexity in the military area, which was compiled by us in order to achieve a better comprehension of the importance of the Military Hospitals in Portugal. The Regiments, Charters, Regulations and Orders of Day constitute a fundamental object of research and analysis to characterise the quotidian of these locations. The Military Hospitals, since its foundation, in the beginning of the Wars of Acclamation in 1640, until the advent of liberalism in 1834, were centres of technical and scientific knowledge with a specialized assistance body, were a multidisciplinary set of professionals took qualitatively care of the attended, and where the Hospitaller Brothers of S. John of God performed the tasks of administrators, nurses and chaplains. In this perspective, we created a chronological listing in order to relate the Hospitaller Brothers with the Military Hospitals, since it is impossible to separate the Hospitaller Order of S. John of God from the component of assistance to the military sick and wounded in Portugal. The urban and architectural importance that the Royal Military Hospitals had in the organic and defensive context of the War Fortifications is emphasized by the way these were implanted and built and by its architectural demarcation of the edified whole, since they constituted an integrant part of the military equipments, as it was theorized for the military architecture. Therefore we analyse the location of the real estate, analysing not only the hospital building itself, but also its relation with the environment, i. e. with the urbanism of the war fortifications. The architectural sobriety of Military Hospitals, integrated in the big cycles of cultural streams in Europe and Portugal, associated to the decorative and iconoclastic wealth developed in these locations, give us a dimension of the scientific importance that these hospitals had, contributing to the diffusion of the cult and circulation of sculptures and paintings of S. John of God in Portugal and of the Saints revered in the Hospitals. In this way, we understand the consolidation of the devotion that the kingdom had for this Saint, the founder of the assistance concept of the modern hospital. The proliferation of the cult and iconography of S. John of God is intrinsically connected to this fact, the artistic iconography concentrating itself around the localities were the Military Hospitals were built. Today, in the assistance buildings, it is not difficult to analyse a slow evolution of the functionality of its spaces, gravitating the structural assistance development around the infirmaries and surgery rooms, this architectural archetype being perennial from the 17th century until the middle of the 19th century. These infirmaries were pointed out, compared and analysed. It was the expulsion of the Religious Orders, by the Decree of May 29th 1834, that ended with the extraordinary and valorous administrative and tutelary action and nursing body of the Hospitaller Brothers of S. John of God, in the specific area of military assistance in Portugal, extinguishing, in some cases, the Military Hospitals, since the kingdom wasn’t prepared to substitute these health professionals. Our study is developed in a timeframe of 295 years, period in which the Military Hospitals were administrated and founded by the Brothers of S. John of God in Portugal.

Crystallographic and biochemical studies on dissimilatory sulfite reductases

Thesis dissertation presented to obtain a PhD degree in Biochemistry at Instituto de Tecnologia Química e Biológica, Universidade Nova de Lisboa

“The past is a foreign country”? Acculturation theory and the anthropology of globalization

Etnográfica, 15 (2): 313-336