Archaeometallurgical study of artefacts from Castro de Vila Nova de São Pedro (Azambuja, Portugal)

Dissertação para obtenção do Grau de Mestre em Conservação e Restauro

The early metallurgy in Southwestern Iberia: metals from the Chalcolithic Settlement of São Pedro (Redondo)

Archaeological excavations carried out in the archaeological site of São Pedro (Southern Portugal) revealed a Chalcolithic settlement occupied in different moments of the 3rd millennium BC. The material culture recovered includes different types of materials, such as ceramics, lithics and metals. The later comprises about 30 artefacts with different typologies such as tools (e.g. awls, chisels and a saw) and weapons (e.g. daggers and arrowheads) mostly belonging to the 2nd and 3rd quarter of the 3rd millennium BC. In the present work the collection of chalcolithic metallic artefacts recovered in São Pedro was characterized. Analytical studies involved micro energy dispersive X-ray fluorescence spectrometry (micro-EDXRF) to determine elemental composition, together with optical microscopy and Vickers microhardness testing for microstructural characterisation and hardness determination. Main results show copper with variable amounts of arsenic and very low content of other impurities, such as iron. Moreover, nearly half of the collection is composed by arsenical copper alloys (As > 2 wt.%) and an association was found between arsenic content and typology since the weapons group (mostly daggers) present higher values than tools (mostly awls). These results suggest some criteria in the selection of arsenic-rich copper ores or smelting products. Furthermore, after casting an artefact would have been hammered, annealed and sometimes, finished with a hammering operation. Additionally, microstructural variations in this collection reveal somewhat different operational conditions during casting, annealing and forging, as expected in such a primitive metallurgy. Moreover the operational sequence seems to be used to achieve the required shape to the object, rather than to intentionally make the alloy harder. Overall, this study suggests that Chalcolithic metallurgists might have a poor control of the addition of arsenic and/or were unable to use this element to increase the hardness of tools and weapons. Finally, the compositions, manufacturing processes and hardness were compared to those from neighbouring regions and different chronological periods.

Análise de desempenho das entidades gestoras concessionárias dos serviços de águas em Portugal continental

Dissertação para obtenção do Grau de Mestre em Engenharia do Ambiente, perfil de Engenharia Ecológica

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.

Sedimentation pelagique et encroûtements cryptalgaires: les calcaires gremeleux du Carixien portugais

In Portugal, Carixian is generally represented by alternative layers of marly limestones characterized by nodule and lumpy levels. These layers are particularly developped [show preferential development] on passage areas to a sedimentary basin, particularly along the slope of tilted blocks between the Meseta and Berlenga's horst. This facies is included in the range of the «nodular limestone» and of the «ammonitico-rosso». Limestones are radiolaria micrites with fragments of pelagic organisms (ammonoids, thin shelled gastropods). These layers can be affected by intensive bioturbation (Brenha) which is responsible for dismantlement, specially where the initial thickness does not exceed a few centimetres. This process can lead to the isolation of residual nodules (Brenha, São Pedro de Muel, Peniche) which can be mobilised by massive sliding (Peniche). The isolated elements, shell fragments or residual nodules, can also be incrustated, thus developing oncolitic cryptalgal structures. At Brenha the lump structure developed progressively into a sequence overlapping the normal sedimentary one (thick limestone beds alternating with bituminous shales). Cryptalgal structures correspond to rather unstable environment conditions on mobile margins. These structures are known in deep pelagic sediments corresponding to well defined events of the geodynamic evolution (end of the initial rifting). Cryptalgal accretions disappear towards the sedimentary basin, and the nodular levels are less important. In the articulation areas with the Tomar platform, small mounds and cupules (Alcabideque) developed within the alternating marly-limestone levels. They represent the so called «mud mounds» of metric dimensions. The upper part of these «mud mounds» is hardened, showing track remains and supporting some brachiopods and pectinids. Hence the lumpy facies of Portugal is included among the range of sedimentaty environments and can be used as «geodynamic tracer».

Biostratigraphie et paléoécologie des peuplements d'ostracodes dans le Domérien du Bassin Lusitanien, Portugal

The Domerian sections from the Lusitanian Basin of São Pedro de Muel, Rabaçal and Tomar have provided us with more than 1100 Ostracods belonging from 18 genus and about 48 species. The faunal diversity and density of the associations decrease in space (from Tomar to Rabaçal and São Pedro de Muel) and time, with favourable environments for the proliferation of Ostracods at the lower part of the sections (Stokesi subzone) and more hostile at the upper part (Ragazzonii subzone). The Monestieri and Nitescens horizons and the Subnodosus subzone are characterized by a typical assemblage of Ostracods. The palaeoecological Ostracod indexes reveal the fluctuations of the oxygenation, temperature, depth and hydrodynamism of the water, on the different sections and on the whole platform. They display a diachronous cooling in the Lower Domerian series. In the upper part of the Middle and in the Upper Domerian, the deeper, less oxygenated and cooler waters prevent the development of the Ostracod faunas.

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

Palaeodiversity 3: 59–87; Stuttgart 30 December 2010

Contribuição para o estudo da remoção em ETAR de 17β-estradiol e de 17α-etinilestradiol no tratamento biológico

Dissertação para obtenção do Grau de Mestre em Engenharia do Ambiente – Perfil Engenharia Sanitária

Contribuição para o estudo da presença de disruptores endócrinos em lamas de ETAR

Dissertação para obtenção do Grau de Mestre em Engenharia do Ambiente – Perfil Engenharia Sanitária

Earth mortars from pre-historic habitat settlements in south Portugal. Case studies

J. Iberian Archaeology 13 (2010), 51-67

Inquietações da alma: Reflexões sobre o simbolismo presente nos temas coadjuvantes de núcleos azulejares portugueses

Revista do IHA, N.3 (2007), pp.182-197

A Cidade da Ribeira Grande, Cabo Verde: Urbanismo e Arquitetura (Séculos XV a XVIII).

A história de Cabo Verde começa com a chegada dos portugueses em 1460. O local selecionado para a primeira ocupação humana, num território anteriormente deserto, recai na zona denominada Ribeira Grande, ilha de Santiago, em consequência da sua ribeira, fonte de água e razão principal de escolha da fixação. É nesse espaço, limitado pelas montanhas acidentadas, pela ribeira e pela topografia irregular que uma pequena povoação nasceu. Nela foi implantada uma área urbana e arquitetónica, fruto de regras de construção do colonizador: Portugal. A génese urbana inicia-se ainda no século XVI, junto a uma baía, designada mais tarde por largo do Pelourinho, bastante orgânica e organizada a partir do porto, do Hospital e da Igreja da Misericórdia. Seguiu-se, ao longo de Quinhentos, o bairro de São Pedro, o maior de todos, também orgânico. O bairro de São Brás, espaço ocupado maioritariamente pelos jesuítas desenvolveu-se de forma paralela à costa. O último bairro intitulado São Sebastião, elevado a partir de meados do século XVI, já foi projetado respeitando os cânones do urbanismo moderno. A cidade conseguiu atrair, pressionada pelos religiosos, pelos monarcas e pelas populações locais, instituições religiosas, régias e privadas que apostaram em obras arquitetónicas marcantes na evolução da urbe, entre as quais a igreja de Nossa Senhora do Rosário, o convento e igreja de São Francisco, a Sé e o paço Episcopal, a fortaleza Real de São Filipe e o Pelourinho.

Internationalization strategy: Dom Pedro Hotel Group - São Paulo

A Work Project, presented as part of the requirements for the Award of a Masters Degree in Management from the NOVA – School of Business and Economics

Reutilização das águas residuais urbanas tratadas

As crescentes preocupações relativamente à escassez de água levam à necessidade de uma urgente reflexão sobre as aplicações actuais da água para consumo humano. Há que encontrar fontes de água alternativas para aplicações não potáveis. Nesta dissertação apresenta-se uma revisão bibliográfica sobre a reutilização de água no Mundo e sobre a viabilidade de um projecto de reutilização de água residual urbana tratada (ARUT). São revistas as linhas de orientação para o uso de águas residuais na rega em Portugal e das tecnologias de desinfecção que se aplicam a este efluente e tipo de uso. São referidos os aspectos a considerar na segurança da distribuição e gestão do armazenamento da água residual urbana tratada. É apresentado um caso de estudo sobre a viabilidade de rega do Parque da Paz, em Almada, com águas residuais urbanas tratadas provenientes da ETAR da Mutela.

Contribuição para o estudo de compostos desreguladores endócrinos (EDC) em estações de tratamento de águas residuais

Desde os anos 90 que se suspeita que um vasto leque de compostos, que estão presentes no ambiente aquático é susceptível de causar disrupção endócrina, podendo provocar efeitos adversos na nível do sistema reprodutor de vários organismos, de entre os quais os surfactantes não-iónicos alquifenois polietoxilatos(APEO), estrogénios, compostos organoclorados, entre outros. Estes, têm sido amplamente utilizados nos últimos 50 anos numa vasta diversidade de aplicações domésticas e comerciais. Durante o tratamento de águas residuais urbanas e industriais, os APEO são degradados sucessivamente até formas menos biodegradáveis, como por exemplo o NP (nonilfenol) e o OP (octilfenol), acabando por ser descarregados no ambiente aquático. A informação disponível, relativamente ao efeito das elevadas descargas nos meios receptores e da sua potencial toxicidade é ainda muito limitada, nomeadamente em sistemas aquáticos. Por outro lado, a informação sobre remoção de EDC em estações de tratamento de águas residuais (ETAR) é igualmente muito escassa, circunstância que impede a realização de estimativas de balanços materiais, indispensáveis à previsão dos correspondentes impactes nos meios hídricos, pelo que, este estudo teve como principal objectivo, a avaliação do potencial estrogénico de um efluente de uma ETAR com tratamento terciário. O presente estudo foi realizado na ETAR de Chelas, em Lisboa (Portugal). O efluente da ETAR é caracterizado por não ser só, efluente doméstico mas também ser constituído por quantidades significativas de efluente industrial. A escolha desta ETAR para realizar este estudo recaiu também na sua linha de tratamento, isto é, a ETAR possui tratamento terciário com remoção de azoto e desinfecção final do efluente através de U.V. De forma a detectar e quantificar o potencial estrogénico de uma água seleccionaramse compostos específicos, isto é alguns EDC “alvo”, nomeadamente: (i) nonilfenol e octilfenol (NP e OP); (ii) bisfenol A (BPA) e (iii) 17 β-estradiol (E2). Foram utilizadas três técnicas diferentes para identificar e quantificar os EDC seleccionados ELISA, LC-MS-MS e HPLC. As técnicas foram igualmente comparadas. Em todos os casos, isto é, independentemente da técnica analítica usada ficou demonstrado que os EDC seleccionados estavam presentes no efluente da ETAR,variando as suas concentrações de composto para composto e também ao longo da linha de tratamento da ETAR, e que ainda são descarregadas, no Estuário do Tejo,níveis de concentrações que poderão causar efeitos fisiológicos na vida animal. Contudo, devido ao elevado nível de diluição existente no Estuário do Tejo (caudais muito grandes) os efeitos nos organismos poderão não ser relevantes e,ou imediatos. Os níveis mais elevados de APE (NP e OP) foram detectados no afluente à ETAR e os menores no efluente da ETAR. O valor mais elevado de E2 foi registado após a decantação primária. A variação de E2 ao longo da linha de tratamento foi pouco significativa, facto este que poderá estar relacionado também com a “cross-reactivity”, bem como a própria actividade microbiológica existente numa água residual. Os maiores valores para o BPA foram obtidos nas lamas primárias (acima dos limites de detecção), tendo sido registada uma redução significativa deste composto ao longo da linha de tratamento, o que poderá indicar que a ETAR de Chelas remove eficientemente este composto.