Changes in spring-mass model characteristics during repeated running sprints.

This study investigated fatigue-induced changes in spring-mass model characteristics during repeated running sprints. Sixteen active subjects performed 12 × 40 m sprints interspersed with 30 s of passive recovery. Vertical and anterior-posterior ground reaction forces were measured at 5-10 m and 30-35 m and used to determine spring-mass model characteristics. Contact (P < 0.001), flight (P < 0.05) and swing times (P < 0.001) together with braking, push-off and total stride durations (P < 0.001) lengthened across repetitions. Stride frequency (P < 0.001) and push-off forces (P < 0.05) decreased with fatigue, whereas stride length (P = 0.06), braking (P = 0.08) and peak vertical forces (P = 0.17) changes approached significance. Center of mass vertical displacement (P < 0.001) but not leg compression (P > 0.05) increased with time. As a result, vertical stiffness decreased (P < 0.001) from the first to the last repetition, whereas leg stiffness changes across sprint trials were not significant (P > 0.05). Changes in vertical stiffness were correlated (r > 0.7; P < 0.001) with changes in stride frequency. When compared to 5-10 m, most of ground reaction force-related parameters were higher (P < 0.05) at 30-35 m, whereas contact time, stride frequency, vertical and leg stiffness were lower (P < 0.05). Vertical stiffness deteriorates when 40 m run-based sprints are repeated, which alters impact parameters. Maintaining faster stride frequencies through retaining higher vertical stiffness is a prerequisite to improve performance during repeated sprinting.

The Anarak, Jandaq and Posht-e-Badam metamorphic complexes in central Iran: New geological data, relationships and tectonic implications

The Anarak, Jandaq and Posht-e-Badam metamorphic complexes occupy the NW part of the Central-East Iranian Microcontinent and are juxtaposed with the Great Kavir block and Sanandaj-Sirjan zone. Our recent findings redefine the origin of these complexes, so far attributed to the Precambrian-Early Paleozoic orogenic episodes, and now directly related to the tectonic evolution of the Paleo-Tethys Ocean. This tectonic evolution was initiated by Late Ordovician-Early Devonian rifting events and terminated in the Triassic by the Eocimmerian collision event due to the docking of the Cimmerian blocks with the Asiatic Turan block. The ``Variscan accretionary complex'' is a new name we proposed for the most widely distributed metamorphic rocks connected to the Anarak and Jandaq complexes. This accretionary complex exposed from SW of Jandaq to the Anarak and Kabudan areas is a thick and fine grain siliciclastic sequence accompanied by marginal-sea ophiolitic remnants, including gabbro-basalts with a supra-subduction-geochemical signature. New Ar-40/Ar-39 ages are obtained as 333-320 Ma for the metamorphism of this sequence under greenschist to amphibolite facies. Moreover, the limy intercalations in the volcano-sedimentary part of this complex in Godar-e-Siah yielded Upper Devonian-Tournaisian conodonts. The northeastern part of this complex in the Jandaq area was intruded by 215 +/- 15 Ma arc to collisional granite and pegmatites dated by ID-TIMS and its metamorphic rocks are characterized by Some Ar-40/Ar-39 radiometric ages of 163-156 Ma. The ``Variscan'' accretionary complex was northwardly accreted to the Airekan granitic terrane dated at 549 +/- 15 Ma. Later, from the Late Carboniferous to Triassic, huge amounts of oceanic material were accreted to its southern side and penetrated by several seamounts such as the Anarak and Kabudan. This new period of accretion is supported by the 280-230 Ma Ar-40/Ar-39 ages for the Anarak mild high-pressure metamorphic rocks and a 262 Ma U-Pb age for the trondhjemite-rhyolite association of that area. The Triassic Bayazeh flysch filled the foreland basin during the final closure of the Paleo-Tethys Ocean and was partly deposited and/or thrusted onto the Cimmerian Yazd block. The Paleo-Tethys magmatic arc products have been well-preserved in the Late Devonian-Carboniferous Godar-e-Siah intra-arc deposits and the Triassic Nakhlak fore-arc succession. On the passive margin of the Cimmerian block, in the Yazd region, the nearly continuous Upper Paleozoic platform-type deposition was totally interrupted during the Middle to Late Triassic. Local erosion, down to Lower Paleozoic levels, may be related to flexural bulge erosion. The platform was finally unconformably covered by Liassic continental molassic deposits of the Shemshak. One of the extensional periods related to Neo-Tethyan back-arc rifting in Late Cretaceous time finally separated parts of the Eocimmerian collisional domain from the Eurasian Turan domain. The opening and closing of this new ocean, characterized by the Nain and Sabzevar ophiolitic melanges, finally transported the Anarak-Jandaq composite terrane to Central Iran, accompanied by large scale rotation of the Central-East Iranian Microcontinent (CEIM). Due to many similarities between the Posht-e-Badam metamorphic complex and the Anarak-Jandaq composite terrane, the former could be part of the latter, if it was transported further south during Tertiary time. (C) 2007 Elsevier B.V. All rights reserved.

Differential effects of glutamate transporter inhibitors on the global electrophysiological response of astrocytes to neuronal stimulation

Astrocytes are responsible for regulating extracellular levels of glutamate and potassium during neuronal activity. Glutamate clearance is handled by glutamate transporter subtypes glutamate transporter 1 and glutamate-aspartate transporter in astrocytes. DL-threo-beta-benzyloxyaspartate (TBOA) and dihydrokainate (DHK) are extensively used as inhibitors of glial glutamate transport activity. Using whole-cell recordings, we characterized the effects of both transporter inhibitors on afferent-evoked astrocyte currents in acute cortical slices of 3-week-old rats. When neuronal afferents were stimulated, passive astrocytes responded by a rapid inward current followed by a persistent tail current. The first current corresponded to a glutamate transporter current. This current was inhibited by both inhibitors and by tetrodotoxin. The tail current is an inward potassium current as it was blocked by barium. Besides inhibiting transporter currents, TBOA strongly enhanced the tail current. This effect was barium-sensitive and might be due to a rise in extracellular potassium level and increased glial potassium uptake. Unlike TBOA, DHK did not enhance the tail current but rather inhibited it. This result suggests that, in addition to inhibiting glutamate transport, DHK prevents astrocyte potassium uptake, possibly by blockade of inward-rectifier channels. This study revealed that, in brain slices, glutamate transporter inhibitors exert complex effects that cannot be attributed solely to glutamate transport inhibition.

O efeito do sorriso na percepção psicológica da pessoa

O objectivo do estudo foi o de verificar o efeito do sorriso na percepção psicológica da pessoa em jovens, adultos, idosos e jovens negros. Pretendia-se verificar se o sorriso contribui para os traços diferenciais entre os grupos humanos em estudo e se o mesmo era descritor de género. O estudo envolveu um delineamento transversal analítico ou estudo não-experimental, também classificado por estudo pós-facto, estudo de observação passiva ou estudo correlacional e de observação, de comparação entre grupos, mediante o juízo ou julgamento psicológico da face neutra e do tipo de sorriso contrastados, de matriz factorial 4 x 2 x 2 (face neutra, sorriso fechado, sorriso superior, sorriso largo; género dos estímulos; género dos respondentes) e a sua finalidade foi descrever a percepção psicológica do sorriso em função das variáveis género do estímulo, género do respondente e grupo étnico, na Escala de Percepção do Sorriso (EPS), em formato diferenciador semântico, com 19 itens bipolares opostos, tendo a avaliação sido feita numa escala ordinal de 1 a 7 pontos, nas dimensões Avaliação (12 itens) e Movimento Expressivo (7 itens) resultante dos estudos preliminares sobre a atractividade facial (estudo preliminar 1) e a escolha de dípolos de adjectivos preditores para percepção psicológica da face neutra (estudo preliminar 2). Nos estudos principais 1, 2 e 3 foram utilizados 24 estímulos fotográficos apresentando o tipo de sorriso (fechado, superior e largo) e a face neutra (12 do estímulo mulher e 12 do estímulo homem) referentes aos três grupos etários (18-25 anos, 40-50 anos e 60-70 anos) e a Escala de Percepção do Sorriso (EPS) foi aplicada a uma amostra não probabilística ou intencional do tipo homogénea de 480 participantes portugueses de ambos os géneros (240 mulheres e 240 homens) distribuídos por grupos etários de jovens (80 mulheres e 80 homens, média: 22.2 anos), adultos (80 mulheres e 80 homens, média: 43.1 anos) e idosos (80 mulheres e 80 homens, média: 65.0 anos) No estudo principal 4, foram utilizados 8 estímulos fotográficos apresentando o tipo de sorriso (fechado, superior e largo) e a face neutra (4 do estímulo mulher e 4 do estímulo homem) de universitários de Cabo Verde, a estudar em Portugal, e a Escala de Percepção do Sorriso (EPS) foi aplicada a uma amostra não probabilística ou intencional do tipo homogénea de 160 participantes de ambos os géneros (80 mulheres e 80 homens) e estudantes universitários portugueses (média: 21.8 anos). Os resultados revelam e confirmam o efeito do sorriso na percepção psicológica da pessoa, à semelhança de outros estudos, isto é, sorrir torna a percepção psicológica mais positiva ou negativa e verifica-se que tal sucede em função do género do estímulo e do género do respondente. As diferenças significativas na percepção da face neutra e tipo de sorriso contrastados são justificadas pela pertença de género de quem os percepciona e pela pertença do género de quem é percepcionado. Tal apenas não sucede no factor Avaliação do grupo dos adultos. Os resultados obtidos indicam que, quer no factor Avaliação quer no factor Movimento Expressivo, os tipos de sorriso largo e superior são os que registam médias ponderadas mais elevadas. Pelo contrário, a face neutra e o sorriso fechado registam valores menos elevados na percepção. A análise da percepção da pessoa em função da face neutra e tipo de sorriso contrastados revelou uma correspondência entre a expressão facial, o género do estímulo e o género do respondente. No factor Avaliação, a mulher é percepcionada mais positivamente que o homem, verificando-se o inverso no factor Movimento Expressivo no grupo dos adultos e dos idosos. Verificou-se efeito do sorriso na percepção psicológica dos estímulos de cor negra. No grupo dos jovens que percepcionaram estímulos de cor negra, o homem é considerado mais positivo que a mulher em ambos os factores. O efeito significativo do género revela que a sua percepção é condicionada pelo seu próprio género. Os resultados apontam ainda para a configuração pronunciada de uma hierarquização ascendente da face neutra e tipo de sorriso contrastados em dois conjuntos bem delimitados e distinguindo diferentes formas topográficas de sorrir: a face neutra e o sorriso fechado e o sorriso superior e o sorriso largo.

Prévention de la violence commise par les spectateurs lors de manifestations sportives : étude des mesures préventives et de la responsabilité de l'organisateur à la lumière du droit comparé, du droit suisse et du droit associatif

Introduction 1. Généralités : Le sport occupe une place importante dans notre société, de manière active par la pratique d'une ou de plusieurs activités sportives, ou de manière passive, au travers de la presse, de la radio et de la télévision. Le sport est ainsi un acte de participation, d'appartenance, de revendication et d'intégration à la société en général ou à un groupe. Il stimule l'imagination et permet de rêver aux héros sportifs. Enfin, non seulement il améliore la santé de ceux qui le pratique, mais il a une dimension éducative et joue un rôle social, culturel et récréatif. Toutefois, le sport est également un spectacle qui provoque des passions et engendre des émotions de la part des supporters, dont certains s'exaltent pour leur équipe fétiche. Il arrive que ce supportérisme soit à tel point exacerbé qu'il mène à des dérives pouvant aboutir à des actes de violence dans et en dehors des stades, ceci tant avant, pendant qu'après le match. A titre d'exemple tragique, les téléspectateurs garderont longtemps en mémoire les scènes auxquelles ils ont assisté le 29 mai 1985, en direct, lorsque, avant le début de la rencontre, des hooligans anglais ont attaqué des supporters italiens dans les gradins du bloc Z du stade du Heysel à Bruxelles, lors de la finale de la Coupe d'Europe des champions, opposant le FC Liverpool à la Juventus de Turin; 39 personnes en sont mortes et 600 ont été blessées. La Suisse, longtemps épargnée par le phénomène, en regard de la situation qui a prévalu dans d'autres Etats européens, ne peut échapper, depuis quelques années, au triste constat selon lequel les stades constituent désormais des environnements propices à des actions de violence, de racisme et, plus rarement, d'extrémisme. Le cas le plus révélateur a eu lieu le 13 mai 2006, lorsque des fauteurs de trouble ont envahi le terrain du Parc Saint-Jacques de Bâle après le coup de sifflet final du match de championnat opposant le FC Bâle au FC Zurich, match dont l'enjeu était la première place du classement du championnat de Super League, pour attaquer à coups de pied et à coups de poing des joueurs, des accompagnants et des personnes chargées de la sécurité. Les affrontements ont continué dans la rue jusque tard dans la soirée. Il s'en est suivi une centaine de blessés et des dégâts d'un demi million de francs. De tels débordements mettent en danger la sécurité du public, des équipes et des arbitres. Il s'agit de tout mettre en oeuvre afin que les spectateurs qui assistent à une manifestation sportive puissent prendre du plaisir aux performances des sportifs sans devoir craindre pour leur sécurité. De même, les acteurs sur le terrain doivent pouvoir exercer leur sport sans craindre un envahissement de l'aire de jeu. Ainsi, les Etats et les associations sportives ont élaboré des textes juridiques afin d'éviter des débordements ou tout autre événement qui pourraient mettre en danger des personnes ou des biens matériels lors de manifestations sportives. Sous l'angle du droit étatique helvétique, cela s'est traduit, notamment en vue du déroulement en Suisse du Championnat d'Europe de football de l'UEFA en 2008 (EURO 2008) et du Championnat du monde de hockey sur glace en 2009, par l'adoption de mesures préventives permettant de lutter contre les actes de violence lors de manifestations sportives, introduites dans la Loi fédérale du 21 mars 1997 instituant des mesures visant au maintien de la sûreté intérieure (LMSI). Elles se concrétisent par l'inscription d'individus ayant commis des actes de violence dans une banque de données nationale, ainsi que par le recours au périmètre d'exclusion, à l'interdiction de sortie du territoire, à l'obligation de s'annoncer à la police et, en dernier ressort, à la garde à vue; enfin, il est également possible de saisir, séquestrer ou confisquer du matériel de propagande5. La mise en place de telles mesures relève de l'Etat, garant de la sécurité et de l'ordre publics à l'extérieur des enceintes sportives. L'organisateur, chargé quant à lui d'assurer la sécurité à l'intérieur du stade, n'est toutefois pas en marge, puisque les fédérations et associations sportives ont édicté des règlements dont il est le destinataire. Ces textes prévoient, à sa charge, notamment les mesures suivantes: le prononcé d'interdictions de stade à l'encontre de supporters violents, la fouille accrue des spectateurs, l'engagement d'un service de sécurité privé, l'obligation de désigner un responsable de la sécurité, la séparation des différents groupes de supporters, etc.. Il appartient ainsi aux associations sportives, aux organisateurs, aux chargés de la sécurité au sein des clubs et aux forces de l'ordre public d'appliquer de la meilleure façon que ce soit les mesures proposées et de collaborer afin de combattre les débordements des spectateurs de manière effective. Prévenir et supprimer la violence dans les manifestations sportives exige ainsi la mobilisation et la collaboration de tous les protagonistes concernés.

O efeito do sorriso na percepção psicológica da pessoa

O objectivo do estudo foi o de verificar o efeito do sorriso na percepção psicológica da pessoa em jovens, adultos, idosos e jovens negros. Pretendia-se verificar se o sorriso contribui para os traços diferenciais entre os grupos humanos em estudo e se o mesmo era descritor de género. O estudo envolveu um delineamento transversal analítico ou estudo não-experimental, também classificado por estudo pós-facto, estudo de observação passiva ou estudo correlacional e de observação, de comparação entre grupos, mediante o juízo ou julgamento psicológico da face neutra e do tipo de sorriso contrastados, de matriz factorial 4 x 2 x 2 (face neutra, sorriso fechado, sorriso superior, sorriso largo; género dos estímulos; género dos respondentes) e a sua finalidade foi descrever a percepção psicológica do sorriso em função das variáveis género do estímulo, género do respondente e grupo étnico, na Escala de Percepção do Sorriso (EPS), em formato diferenciador semântico, com 19 itens bipolares opostos, tendo a avaliação sido feita numa escala ordinal de 1 a 7 pontos, nas dimensões Avaliação (12 itens) e Movimento Expressivo (7 itens) resultante dos estudos preliminares sobre a atractividade facial (estudo preliminar 1) e a escolha de dípolos de adjectivos preditores para percepção psicológica da face neutra (estudo preliminar 2). Nos estudos principais 1, 2 e 3 foram utilizados 24 estímulos fotográficos apresentando o tipo de sorriso (fechado, superior e largo) e a face neutra (12 do estímulo mulher e 12 do estímulo homem) referentes aos três grupos etários (18-25 anos, 40-50 anos e 60-70 anos) e a Escala de Percepção do Sorriso (EPS) foi aplicada a uma amostra não probabilística ou intencional do tipo homogénea de 480 participantes portugueses de ambos os géneros (240 mulheres e 240 homens) distribuídos por grupos etários de jovens (80 mulheres e 80 homens, média: 22.2 anos), adultos (80 mulheres e 80 homens, média: 43.1 anos) e idosos (80 mulheres e 80 homens, média: 65.0 anos) No estudo principal 4, foram utilizados 8 estímulos fotográficos apresentando o tipo de sorriso (fechado, superior e largo) e a face neutra (4 do estímulo mulher e 4 do estímulo homem) de universitários de Cabo Verde, a estudar em Portugal, e a Escala de Percepção do Sorriso (EPS) foi aplicada a uma amostra não probabilística ou intencional do tipo homogénea de 160 participantes de ambos os géneros (80 mulheres e 80 homens) e estudantes universitários portugueses (média: 21.8 anos). Os resultados revelam e confirmam o efeito do sorriso na percepção psicológica da pessoa, à semelhança de outros estudos, isto é, sorrir torna a percepção psicológica mais positiva ou negativa e verifica-se que tal sucede em função do género do estímulo e do género do respondente. As diferenças significativas na percepção da face neutra e tipo de sorriso contrastados são justificadas pela pertença de género de quem os percepciona e pela pertença do género de quem é percepcionado. Tal apenas não sucede no factor Avaliação do grupo dos adultos. Os resultados obtidos indicam que, quer no factor Avaliação quer no factor Movimento Expressivo, os tipos de sorriso largo e superior são os que registam médias ponderadas mais elevadas. Pelo contrário, a face neutra e o sorriso fechado registam valores menos elevados na percepção. A análise da percepção da pessoa em função da face neutra e tipo de sorriso contrastados revelou uma correspondência entre a expressão facial, o género do estímulo e o género do respondente. No factor Avaliação, a mulher é percepcionada mais positivamente que o homem, verificando-se o inverso no factor Movimento Expressivo no grupo dos adultos e dos idosos. Verificou-se efeito do sorriso na percepção psicológica dos estímulos de cor negra. No grupo dos jovens que percepcionaram estímulos de cor negra, o homem é considerado mais positivo que a mulher em ambos os factores. O efeito significativo do género revela que a sua percepção é condicionada pelo seu próprio género. Os resultados apontam ainda para a configuração pronunciada de uma hierarquização ascendente da face neutra e tipo de sorriso contrastados em dois conjuntos bem delimitados e distinguindo diferentes formas topográficas de sorrir: a face neutra e o sorriso fechado e o sorriso superior e o sorriso largo.

Trunk neuromuscular responses to a single whole-body vibration session in patients with chronic low back pain: a cross-sectional study.

OBJECTIVE: Whole-body vibration (WBV) exercise is progressively adopted as an alternative therapeutic modality for enhancing muscle force and muscle activity via neurogenic potentiation. So far, possible changes in the recruitment patterns of the trunk musculature after WBV remain undetermined. The main objective of this study was to evaluate the short-term effects of a single WBV session on trunk neuromuscular responses in patients with chronic low back pain (cLBP) and healthy participants. METHODS: Twenty patients with cLBP and 21 healthy participants performed 10 trunk flexion-extensions before and after a single WBV session consisting of five 1-minute vibration sets. Surface electromyography (EMG) of erector spinae at L2-L3 and L4-L5 and lumbopelvic kinematic variables were collected during the trials. Data were analyzed using 2-way mixed analysis of variance models. RESULTS: The WBV session led to increased lumbar EMG activity during the flexion and extension phases but yielded no change in the quiet standing and fully flexed phases. Kinematic data showed a decreased contribution to the movement of the lumbar region in the second extension quartile. These effects were not different between patients with cLBP and healthy participants. CONCLUSIONS: Increased lumbar EMG activity after a single WBV session most probably results from potentiation effects of WBV on lumbar muscles reflex responses. Decreased EMG activity in full trunk flexion, usually observed in healthy individuals, was still present after WBV, suggesting that the ability of the spine stabilizing mechanisms to transfer the extension torque from muscles to passive structures was not affected.

Developpement et application du moniteur de tabagisme passif MoNIC

A passive sampling device, called Monitor of NICotine (MoNIC), was constructed and evaluated by the laboratory of the Institute for Work and Health to determine nicotine in Environmental Tobacco Smoke (ETS). To support a large campaign on the subject of passive smoking, the CIPRET Valais gracefully distributed more than 1500 MoNIC badges to the Swiss population in order to measure ETS. Non-stimulated saliva was also collected to determine nicotine/cotinine levels of participating volunteers. The inhaled Cigarette Equivalents (CE) by non-smokers was calculated for non-smokers, based on a reference of 0.2 mg of nicotine per cigarette. Using the detected CE on the badge for non-smokers, and comparing it to the nicotine/cotinine levels in saliva, we could confirm the use of the CE concept for estimating exposure to ETS

Dessalinização da Água do Mar Através da Energia Solar - Caso de Estudo Salamansa – Cabo Verde

principal objectivo deste trabalho é o estudo da viabilidade técnica e económica da dessalinização da água do mar, utilizando a energia solar, tomando como caso de aplicação uma pequena comunidade rural de Cabo Verde, a vila piscatória de Salamansa, local onde há graves problemas com a disponibilidade de água potável. No entanto, a proximidade do mar e a disponibilidade de energia solar sugerem a dessalinização como processo para mitigar a falta de água. A dessalinização da água do mar pode ser obtida através de diversas técnicas que podem ser agrupadas de acordo com os princípios em que estes processos se baseiam: processos de dessalinização térmica (destilação solar, destilação multi-estágio, destilação multi-efeito, etc.) e processos de dessalinização por membranas (electrodiálise e osmose inversa). A destilação solar passiva foi a tecnologia de dessalinização estudada neste trabalho e que se pode vir a tornar uma alternativa promissora para um fornecimento regular de água. Por outro lado, o uso de fontes alternativas de energia, como a solar, apresenta-se como uma solução para viabilizar a dessalinização em meios semi-áridos como o deste caso de estudo. Fez-se uma modelação matemática da unidade de destilação solar proposta utilizando o Engineering Equation Solver (EES) como ferramenta para ajudar a resolver as equações de balanço térmico. O projecto do destilador solar proposto poderá atender às necessidades de água doce para consumo de 18 famílias constituídas por 5 agregados (92 pessoas) e apresenta uma eficiência média diária de aproximadamente 78% no Verão e 77% no Inverno.

Prevention of age-associated dementia.

The advancement of medical sciences during the last century has resulted in a considerable increase in life expectancy. As more people live to old age, one of the most fundamental questions of the 21st century is whether the number of individuals suffering from dementia will also continue to increase. Alzheimer's disease (AD) accounts for the majority of cases of dementia in the elderly, but there is currently no curative treatment available. Several strategies have been introduced for treatment, the most recent strategy of which was the immunization of patients using antibodies against Abeta, which is a naturally occurring, even though misfolded peptide in the AD brain. Both active and passive immunization routes have been shown to reduce the pathology associated with Abeta accumulation in brains of genetically designed animal models. However, despite tremendous efforts, no unequivocal proof of therapeutic efficacy could be shown in AD patients. Particularly, the persistence of the neurofibrillary tangles in immunized brains and the issue of inducing cerebral amyloid angiopathy are major limiting factors of antibody therapy. Furthermore, physical activity, a healthy immune system and nutritional habits are suggested to protect against the onset of age-associated dementia. Thus, accumulative evidence suggests that an early integrated strategy, combining pharmacological, immunological, nutritional and life-style factors, is the most pragmatic approach to delay the onset and progression of age-associated dementia.

Tertiary Himalayan structures and metamorphism in the Kulu Valley (Mandi-Khoksar transect of the Western Himalaya) - Shikar-Beh-nappe and crystalline nappe

The Crystalline Nappe of the High Himalayan Crystalline has been examined along the Kulu Valley and its vicinity (Mandi-Khoksar transect). This nappe was believed to have undergone deformation related only to its transport towards the SW essentially during the `'Main Central Thrust event''. New data has led to the conclusion that during the Himalayan orogeny, two distinctive phases, related to two opposite transport directions, characterize the evolution of this part of the chain, before the creation of the late NE-vergent backfolding. The first phase corresponds to an early NE-vergent folding and thrusting, creating the Tandi Syncline and the NE-oriented Shikar Beh Nappe stack, with a displacement amplitude of about 50 km. Two schistosities, together with a strong stretching lineation are developed at a deep tectonic level under amphibolite facies conditions (kyanite-staurolite-garnet-two mica schists). At a higher tectonic level and in the southern part of the section (Tandy Syncline and southern Kulu Valley between Kulu and Mandi) one or two schistosities are developed in the greenschist facies grade rocks (garnet-biotite and biotite schists). These structures and the associated Barrovian type metamorphism are all related to the NE-verging Shikar Beh Nappe. The creation of the NE-verging Shikar Beh Nappe may be explained by the reactivation of a SW dipping listric normal fault of the N Indian flexural passive margin, during the early stages of the Himalayan orogeny. In the second phase, the still hot metamorphic rocks of the Shikar Beh Nappe were folded and thrust towards the SW (mainly along the MBT and the MCT with a displacement in excess of 100 km) onto the cold, low-grade metamorphic rocks of the Larji-Kulu-Rampur Window or, near Mandi, on the non-metamorphic sandstones of the Ganges Molasse (Siwaliks). Sense of shear criteria and a strong NE-SW stretching-lineation indicate that the Crystalline Nappe has been overthrusted towards the SW. Thermometry on synkinematically crystallised garnet-biotite and garnet-hornblende pairs reveals the lower amphibolite facies temperature conditions related to the Crystalline Nappe formation. From the muscovite and biotite Rb-Sr cooling ages, the Shikar Beh Nappe emplacement occurred before 32 Ma and the southwestward thrusting of the Crystalline Nappe began before 21 Ma. Our model involving two opposite directions of thrusting goes against the conventional idea of only one main SW-oriented transport direction in the High Himalayan Crystalline Nappes.

The Relationship between Teachers and Students in the Classroom: Communicative Language Teaching Approach and Cooperative Learning Strategy to Improve Learning

The aim of this research is to to investigate how a supportive relationship between teachers and students in the classroom can improve the learning process. By having a good relationship with students, teachers can offer to students chances to be motivated and feel engaged in the learning process. Students will be engaged actively in the learning instead of being passive learners. I wish to investigate how using communicative approach and cooperative learning strategies while teaching do affect and improve students’ learning performance. To achieve these goals qualitative data collection was used as the primary method. The results show that teachers and students value a supportive and caring relationship between them and that interaction is essential to the teacher-student relationship. This sense of caring and supporting from teachers motivates students to become a more interested learner. Students benefit and are motivated when their teachers create a safe and trustful environment. And also the methods and strategies teachers uses, makes students feel engaged and stimulated to participate in the learning process. The students have in their mind that a positive relationship with their teachers positively impacts their interest and motivation in school which contributes to the enhancement of the learning process.

Ler melhor através dos temas e mitos na literatura cabo-verdiana : uma análise comparativista

Esta dissertação teve como ponto de partida a pergunta “Como se comportaram alguns temas e mitos ao longo da história da literatura de Cabo Verde? Que caminho percorreram?” Para tentar dar-lhe resposta recorremos à metodologia comparativista, com o objetivo de analisar as evoluções e possíveis mudanças ocorridas ao longo dos tempos, a partir do cruzamento transversal entre temas e mitos em épocas diferentes. Foi assim necessário abordar a literatura cabo-verdiana, na sua relação profunda com a história do país, considerando os seus três grandes momentos: um tempo “ indefinido” que vai até 1936, um segundo que vai de 1936 até 1975 e, por último, o que vai desde essa data até à atualidade. Ao longo dessa análise, e a partir de um corpus textual necessariamente circunscrito, fomos detetando as variantes, as diferentes atualizações ocorridas nesta literatura, geralmente provocadas por fatores de ordem geográfica, pela evolução histórico-social, por fatores ideológicos que se prenderam sobretudo com a falta de liberdade vivida até 1975. Esta abordagem comparativista, a análise intertextual que lhe é inerente, proporcionou, não uma simples comparação, mas o desvendar de relações múltiplas existentes entre as obras, o corpus literário escolhido, e os tempos que lhes deram origem, permitindo assim conhecer as partes e, consequentemente o todo através do “desocultamento do oculto”. Constatou-se uma migração dos temas e dos mitos entre as literaturas dos três momentos. Em certos casos, alguns elementos permaneceram, mas com novas representações, noutros assumem significados radicalmente diferentes dados os atuais contextos da sua recepção. Relativamente aos mitos, observou-se a sua crescente dessacralização, em sintonia com o progresso que o país foi conhecendo após a independência nacional. A leitura que fomos fazendo conduziu-nos deste modo a uma viagem ao passado do país. Esta leitura transversal, alicerçada na história, dando conta das transformações ocorridas ao longo dos tempos, mostrou-nos ainda de forma cabal a necessidade de se introduzirem mudanças no ensino da literatura nas escolas cabo-verdianas. Uma mudança que deverá passar por uma abordagem comparativista, que privilegia as relações entre textos de diferentes épocas, a sua perspetivação interdisciplinar com outras formas de expressão, capaz de transformar o aluno-mero-receptor num leitor ativo, implicado numa realidade que lhe diz respeito.

Contribution to the geology of Southern Turkey: new insights from the Mersin mélanges and from the Lycian and Antalya nappes

Abstract The study of fossil Tethyan continental margins implies the consideration of the oceanic domains to which they were connected. The advent of plate tectonics confirmed the importance of the detection of accretion-related mélanges. Ophiolitic mélanges are derived from both an upper ophiolitic obducting plate and a lower oceanic plate. Besides ophiolitic elements, the mélanges may incorporate parts of a magmatic arc and dismembered fragments of a passive continental margin. As the lower plate usually totally disappears during the obduction process, it can only be reconstructed from its elements found in the mélanges. Because of their key location at active margin boundaries, preserved accretion-related mélanges provide strong constraints on the geological evolution of former oceanic domains and their adjacent margins. The identification of Palaeotethyan remnants as accretionary series or reworked during the Late Triassic Eo-Cimmerian event, as well as the recognition of HugluPindos marginal sequences in southern Turkey and in the external Hellenides represent the main achievements of this work, making possible to establish new palaeogeographical correlations. The Mersin mélanges (Turkey), together with the Antalya and Mamonia (Cyprus) domains, are characterized by a series of exotic units found now south of the main Taurus range and compose the South-Taurides Exotic Units. The Mersin mélanges are subdivided in a Triassic and a Late Cretaceous unit. These units consist of the remnants of three major Tethyan oceans, the Palaeotethys, the Neotethys and the Huglu-Pindos. The definition and inventory of the Upper Antalya Nappes (Turkey) are still a matter of controversies and often conflicting interpretations. The recognition of Campanian radiolarians on top of the Kerner Gorge unit directly overlain by the Ordovician Seydi§ehir Fm. of the Tahtah Dag Nappe outlines a tectonic contact and demonstrates that the Upper Antalya Nappes system is composed of three different nappes, the Kerner Gorge, Bakirli and the Tahtah Dag nappes. Additionally, a limestone block in a doubtful tectonic position at the base of the Upper Antalya Nappes yielded for the first time two middle Viséan associations of foraminifers and problematic algae. The Tavas Nappe in the Lycian Nappes (Turkey) is classically divided into the Karadag, Teke Dere, Köycegiz and Haticeana units. As for the Mersin mélanges, the Tavas Nappe is highly composite and includes dismembered units belonging to the Palaeotethyan, Neotethyan and HugluPindos realms. The Karadag unit consists of a Gondwana-type platform succession ranging from the Late Devonian to the Late Triassic. It belongs to the Cimmerian Taurus terrane and was part of the northern passive margin of the Neotethys. The Teke Dere unit is composed of different parts of the Palaeotethyan succession including Late Carboniferous OIB-type basalts, Carboniferous MORB-type basalts, an Early Carboniferous siliciclastic series and a Middle Permian arc sequence. The microfauna and microflora identified in different horizons within the Teke Dere unit share strong biogeographical affinities with the northern Palaeotethyan borders. Kubergandian limestones in primary contact above the Early Carboniferous siliciclastics yielded a rich and diverse microfauna and microflora also identified in reworked cobbles within the Late Triassic Gevne Fm. of the Aladag unit (Turkey). The sedimentological evolution of the Köycegiz and Haticeana series is in many points similar to classical Pindos sequences. These series originated in the Huglu-Pindos Ocean along the northern passive margin of the Anatolian (Turkish transect) and Sitia-Pindos (Greek transect) terranes. Conglomerates at the base of the Lentas Unit in southern Crete (Greece) yielded a microfauna and microflora presenting also strong affinities with the northern borders of the Palaeotethys. This type of reworked sediments at the base of Pindos-like series would suggest a derivation from the Palaeotethyan active margin. -Résumé (French abstract) L'étude des marges continentales fossiles de l'espace téthysien implique d'étudier les domaines océaniques qui y étaient rattachés. Les progrès de la tectonique des plaques ont confirmé l'importance de la reconnaissance des mélanges d'accrétion. Les mélanges ophiolitiques dérivent d'une plaque supérieure ophiolitique qui obducte, et d'une plaque inférieure océanique. En plus d'éléments ophiolitiques, les mélanges peuvent aussi incorporer des parties d'un arc magmatique, ou des fragments d'une marge continentale passive. Comme la plaque inférieure disparaît généralement complètement durant le processus d'obduction, elle ne peut être reconstruite qu'au travers de ses éléments trouvés dans les mélanges. A cause de leur situation aux limites de marges actives, les mélanges d'accrétion bien préservés permettent de contraindre l'évolution géologique d'anciens océans et de leurs marges. L'identification de vestiges de la Paléotéthys en série d'accrétion ou remaniés lors de l'orogenèse éo-cimmérienne au Trias supérieur, ainsi que l'observation de séquences marginales de Huglu-Pinde en Turquie du sud et dans les Hellénides externes représentent les principaux résultats de ce travail, permettant d'établir de nouvelles corrélations paléogéographiques. Les mélanges de Mersin (Turquie), avec les domaines d'Antalya et de Mamonia (Chypre), sont caractérisés par des unités exotiques se trouvant au sud de la chaîne taurique, et forment les Unités Exotiques Sud-Tauriques. Les mélanges de Mersin sont subdivisés en une unité triasique, et une autre du Crétacé supérieur. Ces unités comprennent les reliques de trois principaux océans téthysiens, la Paléotéthys, la Néotéthys et Huglu-Pinde. L'inventaire et la définition des nappes supérieures d'Antalya (Turquie) sont encore matière à controverse et donne lieu à des interprétations conflictuelles. La découverte de radiolaires campaniens au sommet de l'unité de la Gorge de Kemer, directement recouverts par la formation ordovicienne de Seydisehir de la nappe du Tahtali Dag met en évidence un contact tectonique et démontre que les nappes supérieures sont composées de trois différentes nappes, celle de la Gorge de Kemer, celle du Bakirli et celle Tahtali Dag. De plus, un bloc de calcaire dont la position tectonique demeure incertaine à la base des nappes supérieures a fourni pour la première fois deux associations viséennes de foraminifères et d'algues problématiques. La nappe de Tavas dans les nappes lyciennes (Turquie) est séparée en unités du Karadag, du Teke Dere, de Köycegiz et d'Haticeana. Comme pour les mélanges de Mersin, la nappe de Tavas est composite et inclut des unités appartenant à la Paléotéthys, à la Néotéthys et à Huglu-Pinde. L'unité du Karadag est une plateforme carbonatée de type Gondwana se développant du Dévonien supérieur au Trias supérieur. Elle appartient au domaine cimmérien du Taurus et formait la marge nord de la Néotéthys. L'unité du Teke Dere est composée de différentes écailles paléotéthysiennes et inclut des basaltes d'île océanique du Carbonifère supérieur, des basaltes de ride océanique du Carbonifère, une série siliciclastique du Carbonifère supérieur et un arc du Permien moyen. Les microfaunes et -flores trouvées à différents niveaux de la série du Teke Dere partagent de fortes affinités paléogéographiques avec les marges nord de la Paléotéthys. Des calcaires du Kubergandien en contact primaire au-dessus de la série siliciclastique a donné de riches microfaunes et -flores, également identifiées dans des galets remaniés dans la formation de Gevne du Trias supérieur de l'Aladag. L'évolution sédimentologique des séries de Köycegiz et d'Haticeana sont très similaires aux séries classiques du Pinde. Ces séquences prennent leur racine dans l'océan de Huglu-Pinde, le long de la marge passive nord anatolienne (profil turc) et de la marge de Sitia-Pinde (profil grec). Des conglomérats à la base de l'unité de Lentas au sud de la Crète (Grèce) ont donné des microfaunes et flores partageant également de fortes similitudes avec les bordures nord de la Paléotéthys. Le type de sédiments remaniés à la base d'unités de type Pinde suggère une dérivation depuis la marge active de la Paléotéthys. -Résumé grand public (non-specialized abstract) Au début du 20ème siècle, Alfred Wegener bouleverse les croyances géologiques de l'époque et publie plusieurs articles sur la dérive ou la translation des continents. En utilisant des arguments géographiques (similarités des lignes de côte), paléontologiques (faunes et flores similaires) et climatiques (dépôts tropicaux et glaciaires), Wegener explique qu'il y a plusieurs millions d'années, les terres émergées actuelles ne devaient former qu'un seul et grand continent. La fin du 20ème siècle verra l'avènement de la théorie de la tectonique des plaques suite à la reconnaissance du cycle de Wilson, des rides médio-océaniques, des anomalies magnétiques dans les océans et des sutures océaniques qui représentent les reliques d'océans disparus. Le Cycle de Wilson se caractérise par une suite d'évènements géologiques majeurs pouvant se résumer de la manière suivante : (1) séparation d'un craton continental en deux parties, créant une limite de plaque divergente. C'est ce que l'on appelle un rift; (2) développement et croissance d'un océan entre ces deux blocs. Des roches magmatiques remontent à la surface de la terre et forment une chaîne de montagne sous-marine que l'on appelle ride médio-océanique ou dorsale. L'océan continue de se développer, et des sédiments se déposent à sa surface formant la suite ophiolitique ou trinité de Steinmann; (3) après une phase d'expansion plus ou moins longue, les conditions imposées aux limites des plaques à la surface de la terre changent, et l'océan se met à se refermer par disparition progressive (subduction) de sa croûte océanique sous une croûte continentale par exemple. Ceci crée une nouvelle limite de plaque, convergente cette fois; (4) la subduction de la plaque océanique sous la plaque continentale provoque une remontée de magma formant des chaînes volcaniques à la surface de la Terre ; (5) une fois que la plaque océanique a complètement disparu, les deux blocs préalablement séparés par l'océan font collision, formant ainsi une chaîne de montagne. Les chaînes de montagnes sont de manière générale formées par un empilement plus ou moins complexe de nappes. C'est au coeur de certaines de ces nappes que se trouvent les vestiges de l'océan disparu. Un des objectifs de ce travail était la recherche de ces vestiges dans le domaine téthysien de la Méditerranée orientale. Pour ce faire, nous avons parcourus une grande partie du sud de la Turquie, nous sommes allés à Chypre, dans le Sultanat d'Oman, en Iran, en Crète, et nous avons visités quelques îles grecques du Dodécanèse. La région de la Méditerranée orientale est une zone qui a été tectoniquement très active, et qui continue de l'être de nos jours par des phénomènes de subduction (ex. les volcans de Santorin), et par des mouvements coulissants entre des plaques continentales (ex. la faille nord-anatolienne) qui donnent régulièrement lieu à des tremblements de terre. Pour le géologue, la complexité de ces zones d'étude réside dans le fait que les chaînes de montagne actuelles ne contiennent en général pas seulement les restes d'un océan, mais bien de plusieurs bassins océaniques qui se sont succédés dans l'espace et dans le temps. Les nappes qui se trouvent au sud de la Turquie et dans le Dodécanèse forment un important jalon dans la chaîne alpine qui s'étend depuis les Alpes jusque dans l'Himalaya. L'idée d'un continuum au coeur de ce système se basait principalement sur l'âge des océans et sur la reconnaissance de similarités dans l'évolution des séries sédimentaires. La localisation des vestiges de la Paléotéthys ainsi que l'identification des séries sédimentaires ayant appartenu à l'océan de HugluPinde repris sous forme de nappes en Turquie et en Grèce sont cruciales pour permettre de bonnes corrélations locales et régionales. La reconnaissance, la compréhension et l'interprétation de ces séries sédimentaires permettront d'élaborer un modèle d'évolution géodynamique régional, s'appuyant sur des faits de terrains indiscutables, et prenant en compte les contraintes globales que ce genre d'exercice implique.

Synchronous and baroceptor-sensitive oscillations in skin microcirculation: evidence for central autonomic control.

To determine whether skin blood flow is local or takes part in general regulatory mechanisms, we recorded laser-Doppler flowmetry (LDF; left and right index fingers), blood pressure, muscle sympathetic nerve activity (MSNA), R-R interval, and respiration in 10 healthy volunteers and 3 subjects after sympathectomy. We evaluated 1) the synchronism of LDF fluctuations in two index fingers, 2) the relationship with autonomically mediated fluctuations in other signals, and 3) the LDF ability to respond to arterial baroreflex stimulation (by neck suction at frequencies from 0.02 to 0.20 Hz), using spectral analysis (autoregressive uni- and bivariate, time-variant algorithms). Synchronous LDF fluctuations were observed in the index fingers of healthy subjects but not in sympathectomized patients. LDF fluctuations were coherent with those obtained for blood pressure, MSNA, and R-R interval. LDF fluctuations were leading blood pressure in the low-frequency (LF; 0.1 Hz) band and lagging in the respiratory, high-frequency (HF; approximately 0.25 Hz) band, suggesting passive "downstream" transmission only for HF and "upstream" transmission for LF from the microvessels. LDF fluctuations were responsive to sinusoidal neck suction up to 0.1 Hz, indicating response to sympathetic modulation. Skin blood flow thus reflects modifications determined by autonomic activity, detectable by frequency analysis of spontaneous fluctuations.