The three main marine depositional cycles of the Neogene of Portugal

The present work follows a stratigraphic model for the marine Neogene of Portugal based on the definition of three main marine sedimentary cycles. Conceptually the I, II and III Neogene Cycles can be defined as 2nd order sedimentary sequences with duration ranging from 5 to 8 Ma. The I Neogene Cycle is fully represented only in the Lower Tagus Basin. Ranging from the Early Aquitanian to the Late Burdigalian the I Neogene Cycle testify a transgressive episode in the region of Lisbon and Setúbal Peninsula. Rapid lateral facies variations suggest a shallowmarine basin. This cycle ends with an important Late Burdigalian tectonic compressive event expressed by uplift of the surrounding areas and deformation affecting the Early Miocene deposits of the Arrábida Chain. The II Neogene Cycle includes thick sedimentary sequences covering Paleozoic and Mesozoic formations in the Algarve and Alvalade-Melides regions and it extends as far north as Santarém in the Lower Tagus Basin. Mainly controlled by global eustasy, it was generated by the important positive eustatic trend that characterized the Middle Miocene worldwide to which the Portuguese continental margin acted more or less passively. This cycle ended with a second and the most important compression event starting after the end of the Serravallian affecting the entire Portuguese onshore and shelf areas. This led to an important depositional hiatus of marine sediments for more than 2.5 Ma. During the Early and the Middle Tortonian occurred the clockwise rotation of the Guadalquivir Basin. The thickmarine units deposited afterwards in this basin produced a litostatic load, which seems to have induced subsidence farther west resuming the Neogene marine sedimentation in the Cacela region (Eastern Algarve), during the Late Tortonian. This marks the beginning of the III Neogene Cycle. To the north, in the Sado Basin (Alvalade-Melides region), a similar depositional sequence starts its sedimentation during the Messinian. Further north, in the Pombal-Caldas da Rainha region, marine sedimentation started during the Late Pliocene (Piacenzian). The migration in time, from south to north for the beginning of the marine sedimentation of this cycle is interpreted as reflecting a visco-elastic propagation of the deformation from the Betic chain northwards.

Castor fiber na gruta do Caldeirão. Existência, distribuição e extinção do castor em Portugal

Beaver only had been found in Portugal in a Chalcolithic locality, the Vila Nova de S. Pedro castrum. It has now been identified in the Upper Paleolithic (Solutrean) from Gruta do Caldeirão, near Tomar. The species has been found recently at «Gruta do Almonda»; 4 teeth were collected in bed C, older than a Solutrean sequence (see Anexo for details). The species seems to have been rare, as it was also the case with portuguese Miocene Castoridae Enroxenomys minutus and Chalicomys jaegeri. If account is taken of the presence in the Middle Ages until Castille of words meaning beaver (relared to the popular latin Fiber/Biber), it is obvious that these animais still existed then. Such nouns were largely predominant over rhe rather erudite latin (greek deríved) words as Castor,-óris and derived ones, as it could be expected. This allowed us to recognize that veiro should be the corresponding word with Fiber affinities in archaic portuguese. It was previously supposed to mean only expensive furs then imported into Portugal. Indeed it was also a zoonym. Anywày, beaver should be scarce by XIIIth century since it is not included in the quite detailed price list imposed by the «Lei da Almotaçaria» from December 26, 1253 (see Quadro II). Toponyms in veiro and derived words (fig. 2; Quadro III) (plural, feminines, diminutives, inhabited places) give a resrrictive view of rhe Middle Age distribution. Some of them are certainly older than Portugal itself (firsr half of XIlth cenrury); others existed by the XIVth century bur were probably older. Some rare toponyms seem to be derived from the erudite latin Castor,-óris. Nothing suggests that these words were still in use as zoonyms during the Middle Ages. All toponyms are located in regions near rivers and other freshwaters ecologically suitable for beavers, so we can approximately retrace its former, Middle Age disrribution in Portugal (fig. 2; Quadro III). Most of them are locared in the Center-West and Northwest of Portugal, with a suitable c1imate (rainfall in general over 800 mílimerers per year); the only sure geographical exception is Veiros, in Alto Alentejo province, in a region with comparable precipitations and less dry climate conditions than mosr of the territories South of rhe Tagus. There are less and less of these toponyms towards rhe South and the inner part of the country, and they are enrirely lacking in all drier regions from Trás-os-Montes, Beira, Alentejo beyond Tagus' basin, and in Algarve. Nothing suggests beavers lived there, No post-medieval toponym is known, nor any reference after middle XVth century. No such locality was at, or close by to, any frontier. Hence the hypothesis of veiro (et al.} as meaning but points where expensive furs (supposedly known as veiros in general but without c1early saying from what animal they were obrained from) is to be discarded. During the Middle Ages, beaver discriburion concerned all the main river basins from Minho to Tagus ones. Quite rarefied in rhe XIIIth, the beavers may have disappeared from Portugal during the XVth century. Ecological requiremenrs restricted their former distriburion. Vulnerability to natural causes (i.e., severe drought) and to human pressure may have accounted heavily for this species' extinction. Last (1446) reference for Portugal known to us suggests the species was by then almost extinct.

Main features of the labour policy in Portugal

In this working paper is presented information on the Portuguese labour market developed with the support of the European project WORKS-“Work organisation and restructuring in the knowledge society”. Is still a on the process article and thus commentaries are welcome. The structure is based on the following topics: a) The employment policy (Time regimes - time use, flexibility, part-time work, work-life balance -, and the work contracts regimes – wages, contract types, diversity); b) Education and training (skilling outcomes, rules on retraining and further training, employability schemes, transferability of skills); c) Equal opportunities (relevance of equal opportunity regulation for restructuring outcomes, the role of gender and age regulation); d) Restructuring effects (policy on transfer of personnel, policy on redundancies, and participation or voice in restructuring).

Molecular diversity of bla genes in Klebsiella pneumoniae and Escherichia coli isolates

Dissertation presented to obtain a Ph.D. degree in Biology, speciality Microbiology, by Universidade Nova de Lisboa, Faculdade de Ciências e Tecnologia

Wetland Habitat Studies using various Classification Techniques on Multi-Spectral Landsat Imagery: Case study: Tram chim National Park, Dong Thap Vietnam

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

The contribution of multitemporal information from multispectral satellite images for automatic land cover classification at the national scale

Thesis submitted to the Instituto Superior de Estatística e Gestão de Informação da Universidade Nova de Lisboa in partial fulfillment of the requirements for the Degree of Doctor of Philosophy in Information Management – Geographic Information Systems

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

Castor fiber na gruta do Caldeirão Existência, distribuição e extinção do castor em Portugal

Beaver only had been found in Portugal in a Chalcolithic locality, the Vila Nova de S. Pedro castrum. It has now been idenrified in the Upper Paleolithic (Solurrean) from Gruta do Caldeirão, near Tomar. The species has been found recently at «Gruta do Almonda»; 4 teeth were collected in bed C, older than a Solutrean sequence (see Anexo for details). The species seems to have been rare, as it was also the case with portuguese miocene Castoridae Enroxenomys minutus and Chalicomys jaegeri. If account is taken of the presence in the Middle Ages until Castille of words meaning beaver (related to the popular latin Fiber/Biber), it is obvious that these animals still existed then. Such nouns were largely predominant over the rather erudite larin (greek derived) words as Castor, -óris and derived ones, as it could be expected. This allowed us to recognize that veiro should be the corresponding word with Fiber affinities in archaic portuguese. It was previously supposed to mean only expensive furs then imported into Portugal. Indeed it was also a zoonym. Anyway, beaver should be scarce by XIIIth century since it is not included in the quite detailed price list imposed by the «Lei da Almotaçaria» from December 26, 1253 (see Quadro II). Toponyms in veiro and derived words (fig. 2; Quadro III) (plural, feminines, diminutives, inhabited places) give a restrictive view of the Middle Age distribution. Some of them are certainly older than Portugal itself (first half of XIIth century); others existed by the XIVth century but were probably older. Some rare toponyms seem to be derived from rhe erudite latin Castor, -óris. Nothing suggests that these words were still in use as zoonyms during the Middle Ages. All toponyms are located in regions near rivers and other freshwaters ecologically suitable for beavers, so wecan approximately retrace irs former, Middle Age distribution in Portugal (fig. 2; Quadro III). Most of them are located in the Center-West and Northwest of Portugal, with a suitable c1imate (rainfall in general over 800 milimeters per year); the only sure geographical exception is Veiros, in Alto Alentejo province, in a region with comparable precipitations and less dry climare conditions than most of the territories South of the Tagus. There are less and less of these toponyms towards the South and the inner part of the country, and they are enrirely lacking in ali drier regions from Trás-os-Montes, Beira, Alentejo beyond Tagus' basin, and in Algarve. Nothing suggests beavers lived there, No pose-medieval toponym is known, nor any reference after middle XVth century. No such locality was at, or close by to, any frontier. Hence the hypothesis of veiro (e: al.) as meaning but points where expensive furs(supposedly known as veiros in general but without clearly saying from what animal they were obtained from) is to be discarded. During the Middle Ages, beaver distribution concerned all the main river basins from Minho to Tagus ones. Quice racefied in the XIIIth, the beavers may have disappeared from Portugal during the XVth century. Ecological requirements restricted their former distribution. Vulnerability to natural causes (i.e., severe drought) and to human pressure may have accounted heavily for this species extinction. Last (1446) reference for Portugal known to us suggests the species was by then almost extinct.

Tertiary evolution of the São Vicente and Setúbal submarine canyons, Southwest Portugal: insights from seismic stratigraphy

The Setúbal and São Vicente canyons are two major modern submarine canyons located in the southwest Iberian margin of Portugal. Although recognised as Pliocene to Quaternary features, their development during the Tertiary has not been fully understood up to date. A grid of 2D seismic data has been used to characterise the sedimentary deposits of the adjacent flanks to the submarine canyons. The relationship between the geological structure of the margin and the canyon's present location has been investigated. The interpretation of the main seismic units allowed the recognition of three generations of ravinements probably originated after middle Oligocene. Six units grouped in two distinctive seismic sequences have been identified and correlated with offshore stratigraphic data. Seismic Sequence 2 (SS2), the oldest, overlies Mesozoic and upper Eocene deformed units. Seismic Sequence I (SS1) is composed of four different seismic packages separated from SS2 by an erosional surface. The base of the studied sediment ridges is marked by an extensive erosional surface derived from a early/middle Oligocene relative sea-level fall. Deposition in the adjacent area to the actual canyons was reinitiated in late Oligocene in the form of transgressive and channel-fill deposits. A new depositional hiatus is recorded onshore during the Burdigalian, coincident with the unconformity separating SS1 and SS2. This can be correlated with the Arrábida unconformity and with the paroxysmal Burdigalian phase of the Betic domain. Presently, the Setúbal and São Vicente submarine canyons locally cut SS1 and SS2, forming distinctive channels from those recognised on the seismic data. On the upper shelf both dissect highly deformed areas subject to important erosion.

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.

Multiple sequence alignment correction using constraints

Trabalho apresentado no âmbito do European Master in Computational Logics, como requisito parcial para obtenção do grau de Mestre em Computational Logics

Caracterização da função do monóxido de azoto e glutationo hepáticos na sensabilidade periférica à insulina

xi RESUMO A acção da insulina no músculo esquelético depende de um reflexo parassimpático hepático que conduz à libertação de uma substância hepática sensibilizadora da insulina, designada por HISS, responsável por cerca de 55% do efeito hipoglicemiante da insulina. A acção da HISS é finamente regulada pelo monóxido de azoto (NO) hepático e pelo estado prandial, aumentando no período pós-prandial imediato e diminuindo progressivamente com as horas de jejum. A secreção da HISS pode ser inibida cirúrgica ou farmacologicamente, quer por desnervação selectiva do plexo anterior hepático, quer por administração de atropina, quer por inibição do sintase do NO (NOS) hepático. O objectivo geral do trabalho apresentado nesta dissertação foi a caracterização da via de transdução de sinal que conduz à libertação da HISS. O modelo utilizado neste estudo foi o rato Wistar. A sensibilidade à insulina foi avaliada através do teste rápido de sensibilidade à insulina (RIST). A primeira hipótese de trabalho testada foi que a sequência de eventos que conduzem à secreção da HISS inicia-se com a activação do sistema parassimpático hepático seguida de activação do NOS hepático com subsequente produção de NO e activação do guanilato ciclase (GC). Observou-se que a administração de um dador de NO reverteu a resistência à insulina induzida, quer por inibição do NOS hepático, quer por antagonismo dos receptores muscarínicos com atropina. Em contraste, a resistência à insulina produzida por inibição do NOS hepático não foi revertida por administração intraportal de acetilcolina (ACh). Constatou-se que a inibição do GC hepático diminuiu a sensibilidade à insulina. Estes resultados sugerem que: a ACh libertada no fígado induz a síntese de NO hepático que conduz à libertação da HISS, que por sua vez é modulada pelo GC hepático. A libertação da HISS em resposta à insulina é regulada pelo estado prandial. Uma vez que os níveis hepáticos de glutationo (GSH) se encontram, tal como a HISS, diminuídos no estado de jejum e aumentados após a ingestão de uma refeição, testou-se a hipótese de que o GSH hepático está envolvido na secreção da HISS. Observou-se que a depleção do GSH hepático induziu resistência à insulina, comparável à obtida após inibição do NOS hepático. Estes resultados suportam a hipótese de que o GSH hepático desempenha um papel crítico na acção periférica da insulina. Considerando que, no estado de jejum, tanto os níveis de GSH hepático como os níveis de NO hepático são baixos, testou-se a hipótese de que a co-administração intraportal de um dador de GSH e de um dador de NO promove um aumento da sensibilidade à insulina no estado de jejum, devido ao restabelecimento do mecanismo da HISS. Observou-se que a administração sequencial de dadores de GSH e de NO no fígado provocou um aumento na sensibilidade à insulina, dependente da dose de dador de GSH administrada. Concluiu-se portanto que ambos, GSH e NO, são essenciais para que o mecanismo da HISS esteja completamente funcional. O GSH e o NO reagem para formar um S-nitrosotiol, o S-nitrosoglutationo (GSNO). Os resultados supra-mencionados conduziram à formulação da hipótese de que a secreção/acção da HISS depende da formação de GSNO. Observou-se que a administração intravenosa de S-nitrosotióis (RSNOs) aumentou a sensibilidade à insulina, em animais submetidos a um período de jejum, ao contrário da administração intraportal destes fármacos, o que RSNOs têm uma acção periférica, mas não hepática, na sensibilidade à insulina. Os resultados obtidos conduziram à reformulação da hipótese da HISS, sugerindo que a ingestão de uma refeição activa os nervos parassimpáticos hepáticos levando à libertação de ACh no fígado que, por sua vez activa o NOS. Simultaneamente, ocorre um aumento dos níveis de GSH hepático que reage com o NO hepático para formar um composto nitrosado, o GSNO. Este composto mimetiza a acção hipoglicemiante da HISS no músculo esquelético. SUMMARY Insulin action at the skeletal muscle depends on a hepatic parasympathetic reflex that promotes the release of a hepatic insulin sensitizing substance (HISS) from the liver, which contributes 55% to total insulin action. HISS action is modulated by hepatic nitric oxide (NO) and also by the prandial status so as to, in the immediate ostprandial state, HISS action is maximal, decreasing with the duration of fasting. HISS secretion may be inhibited by interruption of the hepatic parasympathetic reflex, achieved either by surgical denervation of the liver or by cholinergic blockade with atropine, or by prevention of hepatic NO release, using NO synthase (NOS) antagonists. The main objective of this work was to characterize the signal transduction pathways that lead to HISS secretion by the liver. Wistar rats were used and insulin sensitivity was evaluated using the rapid insulin sensitivity test (RIST). The first hypothesis tested was that the sequence of events that lead to HISS secretion starts with an increase in the hepatic parasympathetic tone, followed by the activation of hepatic NOS and subsequent triggering of guanylate cyclase (GC). We observed that insulin resistance produced either by muscarinic receptor antagonism with atropine or by hepatic NOS inhibition was reversed by the intraportal administration of an NO donor. In contrast, intraportal acetylcholine (ACh) did not restore insulin sensitivity after NOS inhibition. We also observed that GC inhibition lead to a decrease in insulin sensitivity.These results suggest that the release of ACh in the liver activates hepatic NO synthesis in order to allow HISS secretion, through a signaling pathway modulated by GC. HISS release in response to insulin is controlled by the prandial status. The second hypothesis tested was that glutathione (GSH) is involved in HISS secretion since the hepatic levels of GSH are, like HISS action, decreased in the fasted state and increased after ingestion of a meal. We observed that hepatic GSH depletion led to insulin resistance of the same magnitude of that observed after inhibition of hepatic NOS. These results support the hypothesis that hepatic GSH is crucial in peripheral insulin action. Since, in the fasted state, both hepatic GSH and NO levels are low, we tested the hypothesis that intraportal o-administration of a GSH donor and an NO donor enhances insulin sensitivity in fasted Wistar rats, by restoring HISS secretion. We observed that GSH and NO increased insulin sensitivity in a GSH dose-dependent manner. We concluded that HISS secretion requires elevated levels of both GSH and NO in the liver. GSH and NO react to form a S-nitrosothiol, S-nitrosoglutathione (GSNO). The last hypothesis tested in this work was that HISS secretion/ action depends on the formation of GSNO. We observed that intravenous administration of -nitrosothiols (RSNOs) increased insulin sensitivity in animals fasted for 24 h, in contrast with the intraportal administration of the drug. This result suggests that RSNOs enhanced insulin sensitivity through a peripheral, and not hepatic, mechanism. The results obtained led to a restructuring of the HISS hypothesis, suggesting that the ingestion of a meal triggers the hepatic parasympathetic nerves, leading to the release of Ach in the liver, which in turn activates NOS. Simultaneously, hepatic GSH levels increase and react with NO to form a nitrosated compound, GSNO. S-nitrosoglutathione mimics HISS hypoglycaemic action at the skeletal muscle.

DNA nanoprobes for molecular detection

Dissertação apresentada para obtenção do Grau de Doutor em Engenharia Biológica – especialidade Engenharia Genética, pela Universidade Nova de Lisboa, Faculdade de Ciências e Tecnologia

Light controlled synthesis of nucleic acids

Dissertação apresentada para obtenção do grau de Doutor em Bioquímica - especialidade Biotecnologia, pela Universidade Nova de Lisboa,Faculdade de Ciências e Tecnologia

Every normal logic program has a 2-valued semantics: theory, extensions, applications, implementations

Trabalho apresentado no âmbito do Doutoramento em Informática, como requisito parcial para obtenção do grau de Doutor em Informática