The impact of questions rotation in response accuracy

Dissertação apresentada como requisito parcial para obtenção do grau de Mestre em Estatística e Gestão de Informação

Critical reappraisal of Late Mesozoic-Cenozoic Central and North Atlantic, Caribbean and Mediterranean evolution

(l) The Pacific basin (Pacific area) may be regarded as moving eastwards like a double zip fastener relative to the continents and their respective plates (Pangaea area): opening in the East and closing in the West. This movement is tracked by a continuous mountain belt, the collision ages of which increase westwards. (2) The relative movements between the Pacific area and the Pangaea area in the W-EfE-W direction are generated by tidal forces (principle of hypocycloid gearing), whereby the lower mantle and the Pacific basin or area (Pacific crust = roof of the lower mantle?) rotate somewhat faster eastwards around the Earth's spin axis relative to the upper mantle/crust system with the continents and their respective plates (Pangaea area) (differential rotation). (3) These relative West to East/East to West displacements produce a perpetually existing sequence of distinct styles of opening and closing oeean basins, exemplified by the present East to West arrangement of ocean basins around the globe (Oceanic or Wilson Cycle: Rift/Red Sea style; Atlantic style; Mediterranean/Caribbean style as eastwards propagating tongue of the Pacific basin; Pacific style; Collision/Himalayas style). This sequence of ocean styles, of which the Pacific ocean is a part, moves eastwards with the lower mantle relative to the continents and the upper-mantle/crust of the Pangaea area. (4) Similarly, the collisional mountain belt extending westwards from the equator to the West of the Pacific and representing a chronological sequence of collision zones (sequential collisions) in the wake of the passing of the Pacific basin double zip fastener, may also be described as recording the history of oceans and their continental margins in the form of successive Wilson Cycles. (5) Every 200 to 250 m.y. the Pacific basin double zip fastener, the sequence of ocean styles of the Wilson Cycle and the eastwards growing collisional mountain belt in their wake complete one lap around the Earth. Two East drift lappings of 400 to 500 m.y. produce a two-lap collisional mountain belt spiral around a supercontinent in one hemisphere (North or South Pangaea). The Earth's history is subdivided into alternating North Pangaea growth/South Pangaea breakup eras and South Pangaea growth/North Pangaea breakup eras. Older North and South Pangaeas and their collisional mountain belt spirals may be reconstructed by rotating back the continents and orogenic fragments of a broken spiral (e.g. South Pangaea, Gondwana) to their previous Pangaea growth era orientations. In the resulting collisional mountain belt spiral, pieced together from orogenic segments and fragments, the collision ages have to increase successively towards the West. (6) With its current western margin orientated in a West-East direction North America must have collided during the Late Cretaceous Laramide orogeny with the northern margin of South America (Caribbean Andes) at the equator to the West of the Late Mesozoic Pacific. During post-Laramide times it must have rotated clockwise into its present orientation. The eastern margin of North America has never been attached to the western margin of North Africa but only to the western margin of Europe. (7) Due to migration eastwards of the sequence of ocean styles of the Wilson Cycle, relative to a distinct plate tectonic setting of an ocean, a continent or continental margin, a future or later evolutionary style at the Earth's surface is always depicted in a setting simultaneously developed further to the West and a past or earlier style in a setting simultaneously occurring further to the East. In consequence, ahigh probability exists that up to the Early Tertiary, Greenland (the ArabiaofSouth America?) occupied a plate tectonic setting which is comparable to the current setting of Arabia (the Greenland of Africa?). The Late Cretaceous/Early Tertiary Eureka collision zone (Eureka orogeny) at the northern margin of the Greenland Plate and on some of the Canadian Arctic Islands is comparable with the Middle to Late Tertiary Taurus-Bitlis-Zagros collision zone at the northern margin of the Arabian Plate.

Integrating the theme approach with aspectual scenarios

Dissertação de Mestrado em Engenharia Informática

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

Critical reappraisal of Late Mesozoic-Cenozoic Central and North Atlantic, Caribbean and Mediterranean evolution

(l) The Pacific basin (Pacific area) may be regarded as moving eastwards like a double zip fastener relative to the continents and their respective plates (Pangaea area): opening in the East and closing in the West. This movement is tracked by a continuous mountain belt, the collision ages of which increase westwards. (2) The relative movements between the Pacific area and the Pangaea area in the W-E/E-W direction are generated by tidal forces (principle of hypocycloid gearing), whereby the lower mantle and the Pacific basin or area (Pacific crust = roof of the lower mantle?) rotate somewhat faster eastwards around the Earth's spin axis relative to the upper mantle/crust system with the continents and their respective plates (Pangaea area) (differential rotation). (3) These relative West to East/East to West displacements produce a perpetually existing sequence of distinct styles of opening and closing ocean basins, exemplified by the present East to West arrangement of ocean basins around the globe (Oceanic or Wilson Cycle: Rift/Red Sea style; Atlantic style; Mediterranean/Caribbean style as eastwards propagating tongue of the Pacific basin; Pacific style; Collision/Himalayas style). This sequence of ocean styles, of which the Pacific ocean is a part, moves eastwards with the lower mantle relative to the continents and the upper-mantle/crust of the Pangaea area. (4) Similarly, the collisional mountain belt extending westwards from the equator to the West of the Pacific and representing a chronological sequence of collision zones (sequential collisions) in the wake of the passing of the Pacific basin double zip fastener, may also be described as recording the history of oceans and their continental margins in the form of successive Wilson Cycles. (5) Every 200 to 250 m.y. the Pacific basin double zip fastener, the sequence of ocean styles of the Wilson Cycle and the eastwards growing collisional mountain belt in their wake complete one lap around the Earth. Two East drift lappings of 400 to 500 m.y. produce a two-lap collisional mountain belt spiral around a supercontinent in one hemisphere (North or South Pangaea). The Earth's history is subdivided into alternating North Pangaea growth/South Pangaea breakup eras and South Pangaea growth/North Pangaea breakup eras. Older North and South Pangaeas and their collisional mountain belt spirals may be reconstructed by rotating back the continents and orogenic fragments of a broken spiral (e.g. South Pangaea, Gondwana) to their previous Pangaea growth era orientations. In the resulting collisional mountain belt spiral, pieced together from orogenic segments and fragments, the collision ages have to increase successively towards the West. (6) With its current western margin orientated in a West-East direction North America must have collided during the Late Cretaceous Laramide orogeny with the northern margin of South America (Caribbean Andes) at the equator to the West of the Late Mesozoic Pacific. During post-Laramide times it must have rotated clockwise into its present orientation. The eastern margin of North America has never been attached to the western margin of North Africa but only to the western margin of Europe. (7) Due to migration eastwards of the sequence of ocean styles of the Wilson Cycle, relative to a distinct plate tectonic setting of an ocean, a continent or continental margin, a future or later evolutionary style at the Earth's surface is always depicted in a setting simultaneously developed further to the West and a past or earlier style in a setting simultaneously occurring further to the East. In consequence, ahigh probability exists that up to the Early Tertiary, Greenland (the ArabiaofSouth America?) occupied a plate tectonic setting which is comparable to the current setting of Arabia (the Greenland of Africa?). The Late Cretaceous/Early Tertiary Eureka collision zone (Eureka orogeny) at the northern margin of the Greenland Plate and on some of the Canadian Arctic Islands is comparable with the Middle to Late Tertiary Taurus-Bitlis-Zagros collision zone at the northern margin of the Arabian Plate.

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.

Employment of the side product of biodiesel production in the formation of surfactant like molecules

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

Static detection of anomalies in transactional memory programs

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

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.

Production optimization of rotavirus-like particles: a system biology approach

Dissertation presented to obtain a Ph.D. degree in Engineering and Technology Sciences, Systems Biology at the Instituto de Tecnologia Química e Biológica, Universidade Nova de Lisboa

Functional and therapeutical implications of ligand recognition by the scavenger-like lymphocyte receptors CD5 and CD6

Dissertação para obtenção do Grau de Mestre em Genética Molecular e Biomedicina

Structural characterization of the urea-unfolded state of Colicin Immunity Protein Im7 and Im9

Dissertação para obtenção do Grau de Mestre em Bioquímica Estrutural e Funcional

Observation of 2p3d(¹P°)→1s3d(¹Dᵉ) Radiative Transition in He-like Si, S, and Cl Ions

APS, Journals Phys. Rev. Lett., Volume 111, Issue 24

Smells Like Spleen Spirit: O Decadentismo na América da Segunda Metade do Século XX

Dissertação apresentada para cumprimento dos requisitos necessários à obtenção do grau de Mestre em Línguas Literaturas e Culturas