On the hydrogeology of the Lower Tagus Basin and its Cenozoic geologic evolution

The chemical features of the ground water in the Lower Tagus Cenozoic deposits are strongly influenced by lithology, by the velocity and direction of the water movement as well as by the localization of the recharge and discharge zones. The mineralization varies between 80 and 900 mg/l. It is minimal in the recharge zones and in the Pliocene sand and maximum in the Miocene carbonated and along the alluvial valley. Mineralization always reflects the time of permanence, the temperature and the pressure. The natural process of water mineralization is disturbed in agricultural areas because the saline concentration of the infiltration water exceeds that of the infiltrated rainwater. In the discharge zones, the rise of the more mineralized, some times thermal deep waters related to tectonic accidents give rise to anomalies in the distribution of the aquiferous system mineralization model. The diversity of the hydrochemical facies of the ground water may be related to several factors whose identification is some times difficult.

Lithostratigraphy, sequence stratigraphy and depositional setting of the Pliensbachian and Toarcian series in the Lusitanian Basin, Portugal

In the Lusitanian Basin (Central Portugal), the Middle-Upper Liassic series are characterized by an expressive marly limestone accumulation, sediments that were deposited on a homoclinal carbonate ramp. These series belong to the Vale das Fontes, Lemede, S. Gião (and the lateral equivalents Prado and Cabo Carvoeiro Formations) and, partially, to the Póvoa da Lomba Formations. These units, in great part controlled by an accurate ammonite biostratigraphic scale, are organized into two secondorder transgressive-regressive sequences. The first one (SP) is dated of early Pliensbachian/lowermost early Toarcian age; the second (ST) is dated of early Toarcian to early Aalenian.

Calcareous nannofossil assemblages across the Pliensbachian/Toarcian boundary at the Peniche section (Ponta do Trovão, Lusitanian Basin)

The Peniche section has revealed moderately-to-well preserved calcareous nannofossil assemblages across the Pliensbachian/Toarcian boundary. This good record has allowed the proposition of a refined biostratigraphic scheme. The stage boundary, as defined by ammonites, is comprised within the NJ5b C. impontus (NW Europe; BOWN & COOPER, 1998) or the NJT5b L. sigillatus (Mediterranean Tethys; MATTIOLI & ERBA, 1999) nannofossil subzones. Since in the Lusitanian Basin a mixing of N- and S-Tethyan taxa is observed, both biozonation schemes can be applied. Some nannofossil events (mainly first occurrences) are observed earlier in Portugal than in other Tethyan settings. It is still unclear if these events are real first occurrences. A diversification phase occurred across the Pliensbachian/Toarcian boundary. This phase is well recorded at Peniche, where a change is observed passing from the Pliensbachian, when assemblages are dominated by muroliths, to the Toarcian showing assemblages where placoliths are abundant. A quantification of nannofossils per gram of rock shows that absolute abundances are the highest across the Pliensbachian/Toarcian boundary. Indeed, Peniche exhibits nannofossil abundances very high with respect to correlative levels in other Tethyan settings. The pelagic carbonate fraction (produced by nannofossils) is important in the marly hemi-couplets of Peniche. In some levels, nannofossils account for more than 50% of the total carbonate fraction.

Orbital forcing of stratal patterns in an inner platform carbonate sucession: an example from an Upper Hauterivian series of the Lusitanian Basin, Portugal

With an example taken from a late-Hauterivian series of the Lusitanian Basin (Portugal), we will demonstrate the sedimentary record of orbital pattern variations and, consequently, climate variations in an inner platform environment with patterns and isolation changes, allows us to establish 4 major orders of periodicity related to orbital components:- The large cycles ob bed thickness variation, constituted by 31-32 beds, recording the 400 ky eccentricity cycle component;- The medium cycles, represented by byndles of 8-9 beds, related to the 100 ky eccentricity cycle component; - The small cycles, of 3-5 beds, recording the 41 ky obliquity components;- The very small cycles, of 2 beds, related to the 22 ky and 26 ky precession components. The mean duration of each bed is around 11.8 ky, a number very close to that of the precession hemi-cycle. Climatic control on qualitative production is confirmed by the close relation between the bed thickness variations, the insolation variability and the variation of micritized elements concentrations.

The Sinemurian ammonites of the Lusitanian Basin (Portugal): an example of complex endemic evolutioin

Palaeodiversity 3: 59–87; Stuttgart 30 December 2010

Tectónica da região de Sintra

Photo-interpretation of aerial stereopairs of the Sintra region on the approx. 1/32 000 scale together with field work allowed the production of the present Tectonic Map of the Sintra region. It is now possible to separate structures which resulted from two different tectonic events: one, corresponding to the intrusion of the Late Cretaceous Sintra igneous diapir, and the other the Miocene compressive event, the most important tectonic inversion phase of the Lusitanian Basin. The former are present to the south, southeast and east of the intrusion and within the intrusion itself, affecting the peripheral granites and their contacts with the gabbro-syenite core. These structures comprehend: i) faults and conical fractures striking parallel to the massif boundary, which were intruded by dykes, ii) vertical faults and fractures of two conjugate sets, dextral NNW-SSE and sinistral NNE-SSW. These faults are certainly associated with the E-W striking massif's northwards directed thrust and indicate a N-S oriented horizontal maximum compressive stress. The Miocene compressive event reactivated most of the inherited structures as follows. The NNWSSE faults located on the Sintra southern platform were reactivated as dextral strike slip faults and the E-W thrust along the northern boundary of the massif was also reactivated. This thrust propagated to the east. It also enhanced the asymmetry of the rim-syncline, uplifted the massif and reactivated the NNE-SSW faults as sinistral lateral ramps, which also accommodated vertical throw. The present Tectonic Map of Sintra together with the available geophysical data (MOREIRA, 1984, KULLBERG et al., 1991, SILVA & MIRANDA, 1994) allowed reassessment of the models proposed for the emplacement of the Sintra, Sines and Monchique igneous massifs, which intruded during Late Cretaceous times along the deep dextral NNW-SSE oriented strike slip fault (RIBEIRO et al., 1979; TERRINHA, 1998; TERRINHA & KULLBERG, 1998).

Flaviviruses in mosquitoes from Southern Portugal, 2009-2010

Os flavivírus são vírus pertencentes à família Flaviviridae, género Flavivirus. Estes formam um grande grupo caraterizado pela sua ampla distribuição e diversidade genética. Os flavivírus são, na sua maioria, transmitidos por artrópodes vectores incluíndo agentes patogénicos para humanos e animais que podem potencialmente provocar grandes epidemias e causar elevadas taxas de mortalidade e morbidade. Nos últimos anos, tem-se registado uma grande expansão a nível da distribuição geográfica dos flavivirus e diversidade dos seus hospedeiros. O vírus do Nilo Ocidental tem sido continuamente detectado em toda a Europa recentemente, e também isolado de mosquitos colhidos no Sul de Portugal, onde já foram registados casos humanos e animais. O principal objectivo deste trabalho é o rastreio de flavivírus em mosquitos colhidos em duas regiões do Sul de Portugal, onde os mesmos foram anteriormente detectados. As colheitas de mosquitos foram realizadas em 24 locais em zonas húmidas nos districtos de Faro e Setúbal, através de armadilhas luminosas tipo CDC com CO2 e aspiradores mecânicos manuais para colheita de mosquitos em repouso em abrigos de animais. Os mosquitos colhidos foram agrupados por lotes contendo aproximadamente 50 espécimens cada, e rastreados para a presença de flavivírus por heminested RT-PCR, direccionado à amplificação de um pequeno fragmento do gene NS5 usando oligonucleótidos degenerados específicos para flavivírus. Entre Abril e Outubro de 2009 e 2010 foram colhidos no total 36273 mosquitos pertencentes às seguintes espécies: Anopheles algeriensis, An.atroparvus, Aedes berlandi, Ae.caspius, Ae.detritus, Coquillettidia richiardii, Culex laticinctus, Cx.pipiens, Cx.theileri, Cx.univittatus, Culiseta annulata, Cs.longiareolata, Cs.subochrea, e Uranotaenia unguiculata. As espécies mais abundantes foram Ae.caspius, Cx.theileri e Cx.pipiens, respectivamente. Contudo, as densidades de mosquitos foram variáveis de acordo com o método de colheita e área de amostragem. As densidades de mosquitos colhidos em 2010 foram quatro vezes superior às registadas no ano anterior. No total foram analisados 745 lotes dos quais 31% testaram positivos para a presença de sequências de flavivirus. As espécies que apresentaram taxas de positividade mais elevadas foram: An.algeriensis com uma Taxa Mínima de Infecção (TMI) de 56/1000 no Algarve em 2009, Cs.annulata TMI =22/1000 no Algarve em 2010, Cx.theileri e Cx.pipiens em Setúbal em 2010, TMI =20/1000. An. atroparvus, Ae. caspius, Ae. detritus e Cx. univittatus também produziram lotes positives. No geral, a positividade foi maior no Algarve. Análise das sequências virais obtidas revelou homologia das nossas sequências virais com sequências de referência de flavivírus específicos de mosquitos depositadas em bases de dados de acesso livre. A análise filogenética reflectiu a variabilidade genética dos flavivírus e revelou a relação genética das nossas sequências com as de outros flavivírus, especialmente os específicos de insectos. Tendo em consideração os anteriores isolamentos do vírus do Nilo Ocidental, o aumento acentuado nas densidades de mosquitos, o aumento de temperaturas que se tem vindo a registar, os casos recentes de transmissão de flavivírus por toda a Europa e o padrão desconhecido e imprevisível dos surtos destes vírus, os programas contínuos de vigilância epidemiológica têm-se revelado uma ferramenta indispensável para a Saúde Pública.

Avaliação das propriedades antioxidantes e antimutagénicas de diferentes cultivares de Vaccinium spp, do grupo “Southern Highbush”, produzidas em Portugal

Dissertação para obtenção do Grau de Mestre em Tecnologia e Segurança Alimentar

Archaeometallurgical study of pre and protohistoric production remains and artefacts from Southern Portugal

Dissertação para obtenção do Grau de Doutor em Conservação e Restauro, especialidade Ciências da Conservação

Assessing the impacts of land use and land cover change on hydrology of watershed: a case study on Gigel-Abbay Watershed, Lake Tana Basin, Ethiopia

Dissertation submitted in partial fulfillment of the requirements for the Degree of Master of Science in Geospatial Technologies.

Comparing exchange market pressure in West and Southern African countries

We compare the performance of Cape Verde and Mozambique concerning financial credibility as measured by Exchange Market Pressure, an institutional feature that has often been overlooked in the literature as a relevant institution for economies. Drawing on previous research by Macedo et al. (2009), we expand their analysis and, using several definitions of “financial credibility”, all related to different angles on Exchange Market Pressure indices, we conclude that - against reasonable benchmarks in their respective regions - financial credibility has been very good for Cape Verde and fairly good for Mozambique.

Southern Modernisms. Critical Stances through Regional Appropriations. Conference proceedings

The hegemonic definition of Modernism has been subjected to an intense critical revision process that began several decades ago. This process has contributed to the significant broadening of the modernist canon by challenging its primal essentialist assumptions and formalist interpretations in the fields of both the visual arts and architecture. This conference aims to further expand this revision, as it seeks to discuss the notion of “Southern Modernisms” by considering the hypothesis that regional appropriations, both in Southern Europe and the Southern hemisphere, entailed important critical stances that have remained unseen or poorly explored by art and architectural historians. In association with the Southern Modernisms research project (FCT – EXPL/CPC-HAT/0191/2013), we want to consider the entrenchment of southern modernisms in popular culture (folk art and vernacular architecture) as anticipating some of the premises of what would later become known as critical regionalism. It is therefore our purpose to explore a research path that runs parallel to key claims on modernism’s intertwinement with bourgeois society and mass culture, by questioning the idea that an aesthetically significant regionalism – one that resists to the colonization of international styles and is supported by critical awareness – occurred only in the field of architecture, and can only be represented as a postmodernist turn. (...)

Southern modernisms from A to Z and back again

The book now being published results from a research project entitled Southern Modernisms that ran from March 2014 to May 2015 with FCT funding. The aim of the project was to explore the possibility of constructing a more inclusive, plural notion of modernism through the revision of Modernism’s prevailing definition – its stylistic focus, its formalist and anti-representative bias, as well as its autonomic assumptions, or, as far as architecture is concerned, its functionalist credo. This critical undertaking was grounded on the hypothesis that southern European modernisms featured a strong entrenchment in popular culture (folk art and vernacular architecture), and that this characteristic could be understood as anticipating some of the premises of, what would later become known as, critical regionalismo. (...)