Tectonomagmatic evolution of Western Amazonia: Geochemical characterization and zircon U-Pb geochronologic constraints from the Peruvian Eastern Cordilleran granitoids

The results of a coupled, in situ laser ablation-inductively coupled plasma-mass spectrometry (LA-ICP-MS) U-Pb study on zircon and geochemical characterization of the Eastern Cordilleran intrusives of Peru reveal 1.15 Ga of intermittent magmatism along central Western Amazonia, the Earth's oldest active open continental margin. The eastern Peruvian batholiths are volumetrically dominated by plutonism related to the assembly and breakup of Pangea during the Paleozoic-Mesozoic transition. A Carboniferous-Permian (340-285 Ma) continental arc is identified along the regional orogenic strike from the Ecuadorian border (6 degrees S) to the inferred inboard extension of the Arequipa-Antofalla terrane in southern Peru (14 degrees S). Widespread crustal extension and thinning, which affected western Gondwana throughout the Permian and Triassic resulted in the intrusion of the late- to post-tectonic La Merced-San Ramon-type anatectites dated between 275 and 220 Ma, while the emplacement of the southern Cordillera de Carabaya peraluminous granitoids in the Late Triassic to Early Jurassic (220-190 Ma) represents, temporally and regionally, a separate tectonomagmatic event likely related to resuturing of the Arequipa-Antofalla block. Volcano-plutonic complexes and stocks associated with the onset of the present Andean cycle define a compositionally bimodal alkaline suite and cluster between 180 and 170 Ma. A volumetrically minor intrusive pulse of Oligocene age (ca. 30 Ma) is detected near the southwestern Cordilleran border with the Altiplano. Both post-Gondwanide (30-170 Ma), and Precambrian plutonism (691-1123 Ma) are restricted to isolated occurrences spatially comprising less than 15% of the Eastern Cordillera intrusives. Only one remnant of a Late Ordovician intrusive belt is recognized in the Cuzco batholith (446.5 +/- 9.7 Ma) indicating that the Famatinian arc system previously identified in Peru along the north-central Eastern Cordillera and the coastal Arequipa-Antofalla terrane also existed inboard of this parautochthonous crustal fragment. Hitherto unknown occurrences of late Mesoproterozoic and middle Neoproterozoic granitoids from the south-central cordilleran segment define magmatic events at 691 +/- 13 Ma, 751 +/- 8 Ma, 985 +/- 14 Ma, and 1071-1123 +/- 23 Ma that are broadly coeval with the Braziliano and Grenville-Sunsas orogenies, respectively. Our data suggest the existence of a continuous orogenic belt in excess of 3500 km along Western Amazonia during the formation of Rodinia, its ``early'' fragmentation prior to 690 Ma, and support a model of reaccretion of the Paracas-Arequipa-Antofalla terrane to western Gondwana in the Early Ordovician with subsequent detachment of the Paracas segment in form of the Mexican Oaxaquia microcontinent in Middle Ordovician. A tectonomagmatic model involving slab detachment, followed by underplating of cratonic margin by asthenospheric mantle is proposed for the genesis of the volumetrically dominant Late Paleozoic to early Mesozoic Peruvian Cordilleran batholiths.

Stable isotope (C, O, S) systematics of the mercury mineralization at Idrija, Slovenia: constraints on fluid source and alteration processes

The world-class Idrija mercury deposit (western Slovenia) is hosted by highly deformed Permocarboniferous to Middle Triassic sedimentary rocks within a complex tectonic structure at the transition between the External Dinarides and the Southern Alps. Concordant and discordant mineralization formed concomitant with Middle Triassic bimodal volcanism in an aborted rift. A multiple isotopic (C, O, S) investigation of host rocks and ore minerals was performed to put constraints on the source and composition of the fluid, and the hydrothermal alteration. The distributions of the delta(13)C and delta(18)O values of host and gangue carbonates are indicative of a fracture-controlled hydrothermal system, with locally high fluid-rock ratios. Quantitative modeling of the delta(13)C and delta(18)O covariation for host carbonates during temperature dependent fluid-rock interaction, and concomitant precipitation of void-filling dolomites points to a slightly acidic hydrothermal fluid (delta(13)Capproximate to-4parts per thousand and delta(18)Oapproximate to+10parts per thousand), which most likely evolved during isotopic exchange with carbonates under low fluid/rock ratios. The delta(34)S values of hydrothermal and sedimentary sulfur minerals were used to re-evaluate the previously proposed magmatic and evaporitic sulfur sources for the mineralization, and to assess the importance of other possible sulfur sources such as the contemporaneous seawater sulfate, sedimentary pyrite, and organic sulfur compounds. The delta(34)S values of the sulfides show a large variation at deposit down to hand-specimen scale. They range for cinnabar and pyrite from -19.1 to +22.8parts per thousand, and from -22.4 to +59.6parts per thousand, respectively, suggesting mixing of sulfur from different sources. The peak of delta(34)S values of cinnabar and pyrite close to 0parts per thousand is compatible with ore sulfur derived dominantly from a magmatic fluid and/or from hydrothermal leaching of basement rocks. The similar stratigraphic trends of the delta(34)S values of both cinnabar and pyrite suggest a minor contribution of sedimentary sulfur (pyrite and organic sulfur) to the ore formation. Some of the positive delta(34)S values are probably derived from thermochemical reduction of evaporitic and contemporaneous seawater sulfates.

Ore genesis of Pb-Zn deposits in the Nappe zone of Northern Tunisia: Constraints from Pb-S-C-O isotopic systems

The Jalta and Jebel Ghozlane ore deposits are located in the extreme North of Tunisia, within the Nappe zone. The mineralization of Jalta, hosted in Triassic dolostones and the overlying Mio-Pliocene conglomerates, consists of abundant galena, barite, and cerussite with accessory sphalerite, pyrite, and jordanite. At Jebel Ghozlane, large Pb-Zn concentrations occur in the Triassic dolostones and Eocene limestones. The mineral association consists of galena, sphalerite, barite, and celestite and their oxidation products (cerussite, smithsonite, and anglesite). Lead isotope ratios in galena from both districts are relatively homogeneous ((206)Pb/(204)Pb = 18.702-18.823, (207)Pb/(204)Pb = 15.665-15.677, (208)Pb/(204)Pb = 38.725-38.875). The delta(34)S values for sulfates from both areas (+12.2 to +16.2 parts per thousand at Jalta and + 14.3 to + 19.4 parts per thousand at Jebel Ghozlane) are compatible with a derivation of sulfur from marine sulfates, possibly sourced from the Triassic evaporites. The delta(34)S values of the sulfides have a range between -10 and +12.5 parts per thousand at Jalta, and between -9.1 and +22.1 parts per thousand at Jebel Ghozlane. The large range of values suggests reduction of the sulfate by bacterial and/or thermochemical reduction of sulfate to sulfur. The high delta(34)S values of sulfides require closed-system reduction processes. The isotopically light carbon in late calcites (-6.3 to -2.5 parts per thousand) and authigenic dolomite (-17.6 parts per thousand) suggests an organic source of at least some of the carbon in these samples, whereas the similarity of the delta(18)O values between calcite (+24.8 parts per thousand) and the authigenic dolomite (+24.7 parts per thousand) of Jalta and their respective host rocks reflects oxygen isotope buffering of the mineralizing fluids by the host rock carbonates. The secondary calcite isotope compositions of Jalta are compatible with a hydrothermal fluid circulation at approximately 100 to 200 degrees C, but temperatures as low as 50 degrees C may be indicated by the late calcite of Jebel Ghozlane (delta(18)O of +35.9 parts per thousand). Given the geological events related to the Alpine orogeny in the Nappe zone (nappe emplacement, bimodal volcanism, and reactivation of major faults, such as Ghardimaou-Cap Serrat) and the Neogene age of the host rocks in several localities, a Late-Miocene age is proposed for the Pb-Zn ore deposits considered in this study. Remobilization of deep-seated primary deposits in the Paleozoic sequence is the most probable source for metals in both localities considered in this study and probably in the Nappe zone as a whole. (C) 2011 Elsevier B.V. All rights reserved.

The "Abdominal Circulatory Pump": An Auxiliary Heart during Exercise?

Apart from its role as a flow generator for ventilation the diaphragm has a circulatory role. The cyclical abdominal pressure variations from its contractions cause swings in venous return from the splanchnic venous circulation. During exercise the action of the abdominal muscles may enhance this circulatory function of the diaphragm. Eleven healthy subjects (25 ± 7 year, 70 ± 11 kg, 1.78 ± 0.1 m, 3 F) performed plantar flexion exercise at ~4 METs. Changes in body volume (ΔVb) and trunk volume (ΔVtr) were measured simultaneously by double body plethysmography. Volume of blood shifts between trunk and extremities (Vbs) was determined non-invasively as ΔVtr-ΔVb. Three types of breathing were studied: spontaneous (SE), rib cage (RCE, voluntary emphasized inspiratory rib cage breathing), and abdominal (ABE, voluntary active abdominal expiration breathing). During SE and RCE blood was displaced from the extremities into the trunk (on average 0.16 ± 0.33 L and 0.48 ± 0.55 L, p < 0.05 SE vs. RCE), while during ABE it was displaced from the trunk to the extremities (0.22 ± 0.20 L p < 0.001, p < 0.05 RCE and SE vs. ABE respectively). At baseline, Vbs swings (maximum to minimum amplitude) were bimodal and averaged 0.13 ± 0.08 L. During exercise, Vbs swings consistently increased (0.42 ± 0.34 L, 0.40 ± 0.26 L, 0.46 ± 0.21 L, for SE, RCE and ABE respectively, all p < 0.01 vs. baseline). It follows that during leg exercise significant bi-directional blood shifting occurs between the trunk and the extremities. The dynamics and partitioning of these blood shifts strongly depend on the relative predominance of the action of the diaphragm, the rib cage and the abdominal muscles. Depending on the partitioning between respiratory muscles for the act of breathing, the distribution of blood between trunk and extremities can vary by up to 1 L. We conclude that during exercise the abdominal muscles and the diaphragm might play a role of an "auxiliary heart."

Aspectos epidemiológicos, clínicos, hematológicos e anatomopatológicos da leucemia eritroide aguda (LMA M6) em gatos

Os aspectos epidemiológicos, clínicos, hematológicos e anatomopatológicos da leucemia eritroide aguda (LMA M6) foram estudados em 10 gatos que morreram em consequência dessa condição. Os resultados obtidos diferem daqueles previamente descritos na literatura nos seguintes aspectos: 1) a doença ocorreu na forma de um modelo bimodal relacionado à idade dos gatos afetados, em que 50% tinham 1-3 anos de idade e 50% tinham 10 anos de idade ou mais; 2) quase todos os gatos afetados (87,5%) demonstravam policromasia, possivelmente decorrente de eritropoese extramedular; 3) em todos os casos havia múltiplos focos de células hematopoéticas, principalmente eritropoeticas, em múltiplos órgãos, que incluíam baço (85,7%), linfonodos (71,4%), fígado (57,1%) e rim (28,6%); 4) em alguns casos (28,6%) esses focos podiam ser vistos macroscopicamente, na forma de metástases, mas sempre diferiam histologicamente da medula óssea quanto à proporção dos precursores eritroides envolvidos; 5) em pelo menos um caso ocorreu um continuum patologicum até outra forma de LMA (LMA M4), um fenômeno denominado "infidelidade de linhagem". Esse artigo discute essas diferenças e reforça os critérios fundamentais para se estabelecer o diagnóstico definitivo dessa que é a forma mais importante de leucemia em gatos na nossa região.

Structure-related magnetic fabric studies : implications for deformed and undeformed Precambrian rocks

The aim of this thesis research was to gain a better understanding of the emplacement of rapakivi granite intrusions, as well as the emplacement of gold-bearing hydrothermal fluids in structurally controlled mineralizations. Based on investigations of the magnetic fabric, the internal structures could be analysed and the intrusion mechanisms for rapakivi granite intrusions and respectively different deformation stages within gold-bearing shear and fault zones identified. Aeromagnetic images revealed circular structures within the rapakivi granite batholiths of Wiborg, Vehmaa and Åland. These circular structures represent intrusions that eventually build up these large batholiths. The rapakivi granite intrusions of Vehmaa, Ruotsinpyhtää within the Wiborg batholith and Saltvik intrusions within the Åland batholith all show bimodal magnetic susceptibilities with paramagnetic and ferromagnetic components. The distribution of the bimodality is related to different magma batches of the studied intrusions. The anisotropy of magnetic susceptibility (AMS) reveals internal structures that cannot be studied macroscopically or by microscope. The Ruotsinpyhtää and Vehmaa intrusions represent similar intrusion geometries, with gently to moderately outward dipping magnetic foliations. In the case of Vehmaa, the magnetic lineations are gently plunging and trend in the directions of the slightly elongated intrusion. The magnetic lineations represent magma flow. The shapes of the AMS ellipsoids are also more planar (oblate) in the central part of the intrusion, whereas they become more linear (prolate) near the margin. These AMS results, together with field observations, indicate that the main intrusion mechanism has involved the subsidence of older blocks with successive intrusion of fractionated magma during repeated cauldron subsidence. The Saltvik area within the Åland batholith consists of a number of smaller elliptical intrusions of different rapakivi types forming a multiple intrusive complex. The magnetic fabric shows a general westward dipping of the pyterlite and eastward dipping of the contiguous even-grained rapakivi granite, which indicates a central inflow of magma batches towards the east and west resulting from a laccolitic emplacement of magma batches, while the main mechanism for space creation was derived from subsidence. The magnetic fabric of structurally controlled gold potential shear and fault zones in Jokisivu, Satulinmäki and Koijärvi was investigated in order to describe the internal structures and define the deformation history and emplacement of hydrothermal fluids. A further aim of the research was to combine AMS studies with palaeomagnetic methods to constrain the timing for the shearing event relative to the precipitation of ferromagnetic minerals and gold. All of the studied formations are dominated by monoclinic pyrrhotite. The AMS directions generally follow the tectonic structures within the formations. However, internal variations in the AMS direction as well as the shapes of the AMS ellipsoids are observed within the shear zones. In Jokisivu and Satulinmäki in particular, the magnetic signatures of the shear zone core differ from the margins. Furthermore, the shape of the magnetic fabric in the shear zone core of Jokisivu is dominated by oblate shapes, whereas the margins exhibit prolate shapes. These variations indicate a later effect of the hydrothermal fluids on the general shear event. The palaeo-magnetic results reveal a deflection from the original Svecofennian age geomagnetic direction. These results, coupled with correlations between the orientation of the NRM vectors and the magnetic and rock fabrics, imply that the gold-rich hydrothermal fluids were emplaced pre/syntectonically during the late stages of the Svecofennian orogeny.

Dinâmica da produção e decomposição da serapilheira do araribá (Centrolobium tomentosum Guill. ex Benth. - Fabaceae) em uma mata ciliar, Rio Jacaré-Pepira, São Paulo

O estudo foi realizado em um fragmento de mata ciliar (42 ha) onde a espécie arbórea, secundária inicial e decídua Centrolobium tomentosum Guill. ex Benth. é dominante no estrato superior da floresta estacional semidecidual. A espécie apresentou grande produção de serapilheira (4,2 kg.ind-1) com um comportamento bimodal de deposição (janeiro/fevereiro _ 25,1% e julho/agosto _ 52,3%), e grande capacidade de transferência de nutrientes para o solo (g.ind-1.ano-1): 74,7 N; 6,1 P; 29,0 K; 73,9 Ca; 25,8 Mg e 14,1 S. A decomposição da fração foliar da serapilheira apresentou padrão sazonal, resultando em cerca de 19,5 meses para seu desaparecimento. A qualidade e quantidade da serapilheira produzida por C. tomentosum indicam um alto potencial de utilização dessa espécie em programas de reabilitação funcional e estrutural das matas ciliares no Estado de São Paulo.

Erythrocyte phosphoglucomutase activity of bipolar I patients currently using lithium or carbamazepine

Lithium has been used for the last five decades to treat bipolar disorder, but the molecular basis of its therapeutic effect is unknown. Phosphoglucomutase is a key enzyme in the metabolism of glycogen. In yeast, rabbit and human HEK293 cells, it is inhibited by lithium in the therapeutic concentration range. We measured the phosphoglucomutase activity in erythrocytes and the inhibitor constant for lithium in a population of healthy subjects and compared them to those of bipolar patients treated with lithium or carbamazepine. The specific activity of phosphoglucomutase measured in vitro in erythrocytes from control subjects presented a normal distribution, with the difference between the lowest and the highest activity being approximately 2-fold (0.53-1.10 nmol mg Hb-1 min-1). Comparison of phosphoglucomutase activity in untreated bipolar patients and control subjects showed no significant difference, whereas comparison between bipolar patients treated with carbamazepine or lithium revealed significantly lower mean values in patients treated with carbamazepine (747.3 ± 27.6 vs 879.5 ± 35.9 pmol mg Hb-1 min-1, respectively). When we studied the concentration of lithium needed to inhibit phosphoglucomutase activity by 50%, a bimodal distribution among the population tested was obtained. The concentration of LiCl needed to inhibit phosphoglucomutase activity by 50% was 0.35 to 1.8 mM in one group of subjects and in the other it was 3 to 4 mM. These results suggest that phosphoglucomutase activity may be significant in patients with bipolar disorder treated with lithium and carbamazepine.

Efeito do tamanho dos grânulos nas características estruturais e físico-químicas do amido de trigo

A distribuição de tamanho dos grânulos influencia diretamente a composição química do amido, afetando sua funcionalidade, características de gelatinização, susceptibilidade enzimática, e cristalinidade. Os grânulos de amido de trigo possuem distribuição bimodal de tamanho e são divididos em grânulos tipo A (10-40 µm) e B (<10 µm). Neste trabalho amidos de trigo obtidos de quatro diferentes cultivares foram isolados e fracionados por tamanho. Amidos de diferentes tamanhos foram analisados quanto ao teor de lisofosfolipídeos e amilose, difração de raios-X, microscopia eletrônica de varredura, susceptibilidade enzimática, poder de inchamento e propriedades térmicas e de pasta. O fracionamento possibilitou a divisão dos grânulos em grandes (>15 µm) e pequenos (<10 µm). Independente da cultivar, grânulos grandes apresentaram diâmetro médio de 22 µm e formato lenticular, enquanto grânulos pequenos mostraram diâmetro médio de 6 µm e forma arredondada. Grânulos grandes apresentaram menor teor de lisofosfolipídeos, maior teor de amilose e menor índice de cristalinidade (IC) quando comparados aos pequenos. Apesar da maior cristalinidade, os grânulos pequenos foram mais susceptíveis à hidrólise que os grânulos grandes, sugerindo que a susceptibilidade enzimática dos grânulos pequenos está relacionada à sua maior área superficial.

Crosstalk entre osso e tecido adiposo na doença renal crônica

Dentro do conceito de que os hormônios são regulados por um ciclo de reciprocidade, o fato de osteoblastos e adipócitos serem desenvolvidos a partir de células-tronco mesenquimais e da remodelação óssea ser regulada pela leptina, traz a ideia de possíveis participações do osso no metabolismo energético e vice-versa. Estudos recentes têm demonstrado que a diferenciação e as funções das células ósseas são reguladas pela leptina, que parece desencadear uma resposta bimodal central, via sistema nervoso simpático, e uma local, na qual a leptina agiria sobre o osso. De fato, estudos têm revelado complexa interação entre osso, tecido adiposo e cérebro; no entanto, existem poucos estudos sobre esse crosstalk em pacientes com doença renal crônica (DRC). Como tais pacientes têm tendência à diminuição da densidade mineral óssea e elevados níveis de leptina, o presente artigo apresentou uma revisão sobre o possível envolvimento entre tecido adiposo e massa óssea, em pacientes com DRC.

Sedimentology and taphonomy of storm-generated shell beds from the Verulam formation (Ordovician), Lakefield and Gamebridge quarries, Southern Ontario, Canada /

The Verulam Formation (Middle Ordovician) at the Lakefield Quarry and Gamebridge Quarry, southern Ontario, is comprised of five main lithofacies. These include shoal deposits consisting of Lithofacies 1, winnowed crinoidal grainstones and, shelf deposits consisting of: Lithofacies 2, wackestones, packstones, grainstones, and rudstones; Lithofacies 3, laminated calcisiltites; Lithofacies 4, nodular wackestones and mudstones; and, Lithofacies 5, laminated mudstones and shales. The distribution of the lithofacies was influenced by variations in storm frequency and intensity during a relative sea level fall. Predominant convex-up attitudes of concavo-convex shells within shell beds suggest syndepositional reworking during storm events. The bimodal orientations of shell axes on the upper surfaces of the shell beds indicates deposition under wave-generated currents. The sedimentary features and shell orientations indicate that the shell beds were deposited during storm events and not by the gradual accumulation of shelly material. Cluster and principal component analysis of relative abundance data of the taxa in the shell beds, interbedded nodular wackestones and mudstones, and laminated mudstones and shales, indicates one biofacies comprised of three main assemblages: a strophomenid (Sowerbyelladominated) assemblage, a transitional mixed strophomenid-atrypid assemblage and an atrypid (Zygospira-dominatQd) assemblage. The occurrence of the strophomenid, the strophomenid-atrypid and atrypid assemblages were controlled by storm-driven allogenic taphonomic feedback.

Structural, stratigraphic and geochemical studies of the Horwood Peninsula - Gander Bay Area, Northeast Newfoundland /

The Horwood Peninsula - Gander Bay area is located at NE Newfoundland in the Botwood Zone (Williams et a1., 1974) or in the Dunnage Zone (Williams, 1979) of the Central Mobile Belt of the Newfoundland Appalachians. The area is underlain by Middle Ordovician to possible Lower Silurian rocks of the Davidsville and Indian Islands Groups, respectively. Three conformable formations named informally : the Mafic Volcanic Formation, the Greywacke and Siltstone Formation and the Black Slate Formation, have been recognized in the Davidsville Group. The Greywacke and the Black Slate Formations pass locally into a Melange Formation. From consideration of regional structure and abundant locally-derived mafic volcanic olisto- 1iths in the melange, it is considered to have originated by gravity sliding rather than thrusting. Four formations have been recognized in the Indian Islands Group. They mainly contain silty slate and phyllite, grey cherty siltstone, green to red micaceous siltstone and limestone horizons. Repetition of lithological units by F1 folding are well-demonstrated in one of formations in this Group. The major structure in this Group on the Horwood Peninsula is interpreted to be a synclinal complex. The lithology of this Group is different from the Botwood Group to the west and is probably Late Ordovician and/or Early Silurian in age. The effects of soft-sediment deformation can be seen from the lower part of the Davidsville Group to the middle part of the Indian Islands Group indicating continuous and/or episodic slumping and sliding activities throughout the whole area. However, no siginificant depOSitional and tectonic break that could be assigned to the Taconian Orogeny has been recognized in this study. Three periods of tectonic deformation were produced by the Acadian Orogeny. Double boudinage in thin dikes indicates a southeast-northwest sub-horizontal compression and main northeast-southwest sub-horizontal extension during the D1 deformation. A penetrative, axial planar slaty cleavage (Sl) and tight to isocJ.ina1 F1 folds are products of this deformation. The D2 and D3 deformations formed S2 and S3 fabrics associated with crenulations and kink bands which are well-shown in the slates and phyllites of the Indian Islands Group. The D2 and D3 deformations are the products of vertical and northeast-southwest horizontal shortening respectively. The inferred fault between the Ordovician slates (Davidsville Group) and the siltstones (Indian Islands Group) suggested by Williams (1963, 1964b, 1972, 1978) is absent. Formations can be followed without displacement across this inferred fault. Chemically, the pillow lavas, mafic agglomerates, tuff beds and diabase dikes are subdivided into three rock suites : (a) basaltic komatiite (Beaver Cove Assemblage), (b) tholeiitic basalt (diabase dikes), (c) alkaline basalt (Shoal Bay Assemblage). The high Ti02 , MgO, Ni contents and bimodal characteristic of the basaltic komatiite in the area are comparable to the Svartenhuk Peninsula at Baffin Bay and are interpreted to be the result of an abortive volcano-tectonic rift-zone in a rear-arc basin. Modal and chemical analyses of greywackes and siltstones show the trend of maturity of these rocks increasing from poorly sorted Ordovician greywackes to fairly well-sorted Silurian siltstones. Rock fragments in greywackes indicate source areas consisting of plagiogranite, low grade metamorphic rocks and ultramafic rocks. Rare sedimentary structures in both Groups indicate a southeasterly provenance. Trace element analyses of greywackes also reveal a possible island-arc affinity.

Reactive Hyperemia as endothelial function determinant using plethysmography methods

L’atteinte de la fonction endothéliale représente une phase précoce de l’athérosclérose, un stade où les patients sont généralement asymptomatiques. Il existe donc un intérêt certain à détecter la dysfonction endothéliale. Nous avons développé une technique de mesure des variations de flot artériel au niveau des membres supérieurs, basée sur la spectroscopie proche infrarouge (NIRS). Cette approche permettrait d’étudier le niveau d’atteinte vasculaire et probablement de quantifier le degré de dysfonction endothéliale périphérique lors d’une hyperémie réactive. L'expérience a été exécutée sur deux cohortes de 13 et de 15 patients et a été comparée à la pléthysmographie par jauge de contrainte (SGP) qui est considérée comme une méthode de référence. Par la suite, nous avons caractérisé la réponse endothéliale par modélisation de la courbe hyperémique du flot artériel. Des études préliminaires avaient démontré que la réponse hyperémique adoptait majoritairement une forme bi-modale. Nous avons tenté de séparer les composantes endothéliales-dépendantes et endothéliales-indépendantes de l’hyperémie. La quantification des deux composantes de la réaction hyperémique permet de calculer un indice de la ‘santé’ du système endothélial local. Cet indice est nommé le ηfactor. Les résultats montrent une forte corrélation des mesures de flots entre la technique développée et la méthode de référence (r=0.91). Nous avons conclu que NIRS est une approche précise pour la mesure non-invasive du flot artériel. Nous avons obtenu une bonne répétabilité (ICC = 0.9313) pour le ηfactor indiquant sa robustesse. Cependant des études supplémentaires sont nécessaires pour valider la valeur de diagnostic du facteur défini. Mots clés: hyperémie réactive, réponse myogénique, oxyde nitrique, athérosclérose, spectroscopie proche infrarouge

Changements et évolution des universités conventionnelles sous l’influence des technologies de l’information et de la communication (TIC): le cas du contexte universitaire nord-américain

Cette recherche part du constat de l’utilisation des nouvelles technologies qui se généralise dans l’enseignement universitaire (tant sur campus qu’en enseignement à distance), et traite cette question sous trois aspects institutionnel, pédagogique et technologique. La recherche a été menée à travers quinze universités canadiennes où nous avons interrogé vingt-quatre universitaires, nommément des responsables de centres de pédagogie universitaire et des experts sur la question de l’intégration des technologies à l’enseignement universitaire. Pour le volet institutionnel, nous avons eu recours à un cadre théorique qui met en relief le changement de structure et de fonctionnement des universités à l’ère d’Internet, suivant le modèle théorique de l’Open System Communications Net de Kershaw et Safford (1998, 2001). Les résultats, à l’aune de ce modèle, confirment que les universités conventionnelles sont dans une phase de transformation due à l’utilisation des technologies de l'information et de la communication (TIC). De plus, les cours hybrides, la bimodalité, des universités entièrement à distance visant une clientèle estudiantine au-delà des frontières régionales et nationales, des universités associant plusieurs modèles, des universités fonctionnant à base d’intelligence artificielle, sont les modèles principaux qui ont la forte possibilité de s’imposer dans le paysage universitaire nord-américain au cours des prochaines décennies. Enfin, à la lumière du modèle théorique, nous avons exploré le rôle de l’université, ainsi en transformation, au sein de la société tout comme les rapports éventuels entre les institutions universitaires. S’agissant de l’aspect pédagogique, nous avons utilisé une perspective théorique fondée sur le modèle du Community of Inquiry (CoI) de Garrison, Anderson et Archer (2000), revu par Vaughan et Garrison (2005) et Garrison et Arbaugh (2007) qui prône notamment une nouvelle culture de travail à l’université fondée sur trois niveaux de présence. Les résultats indiquent l’importance d’éléments relatifs à la présence d’enseignement, à la présence cognitive et à la présence sociale, comme le suggère le modèle. Cependant, la récurrence -dans les trois niveaux de présence- de certains indicateurs, suggérés par les répondants, tels que l’échange d’information, la discussion et la collaboration, nous ont amenés à conclure à la non-étanchéité du modèle du CoI. De plus, certaines catégories, de par leur fréquence d’apparition dans les propos des interviewés, mériteraient d’avoir une considération plus grande dans les exigences pédagogiques que requiert le nouveau contexte prévalant dans les universités conventionnelles. C’est le cas par exemple de la catégorie « cohésion de groupe ». Enfin, dans le troisième volet de la recherche relatif à la dimension technologique, nous nous sommes inspirés du modèle théorique d’Olapiriyakul et Scher (2006) qui postule que l’infrastructure dans l’enseignement doit être à la fois une technologie pédagogique et une technologie d’apprentissage pour les étudiants (instructional technology and student learning technology). Partant de cette approche, le volet technologique de notre recherche a consisté à identifier les fonctionnalités exigées de la technologie pour induire une évolution institutionnelle et pédagogique. Les résultats à cet égard ont indiqué que les raisons pour lesquelles les universités choisissent d’intégrer les TIC à l’enseignement ne sont pas toujours d’ordre pédagogique, ce qui explique que la technologie elle-même ne revête pas forcément les qualités a priori requises pour une évolution pédagogique et institutionnelle. De ce constat, les technologies appropriées pour une réelle évolution pédagogique et institutionnelle des universités ont été identifiées.

TactoColor : conception et évaluation d’une interface d’exploration spatiale du web pour malvoyants.

Nous nous intéressons, dans le cadre de cette recherche, à l’accès à l’internet des personnes malvoyantes. Plusieurs types d’outils destinés à ce public sont disponibles sur le marché, comme les lecteurs et les agrandisseurs d’écran, en fonction de l’acuité visuelle de la personne. Bien que ces outils soient utiles et régulièrement utilisés, les malvoyants (ainsi que les aveugles) évoquent souvent leur aspect frustrant. Plusieurs raisons sont citées, comme le manque d’organisation spatiale du contenu lu avec les lecteurs d’écran ou le fait de ne solliciter qu’un seul sens. La présente recherche consiste à adapter pour les malvoyants un système en développement le TactoWeb (Petit, 2013) qui permet une exploration audio-tactile du Web. TactoWeb a été conçu pour les handicapés ayant une cécité complète et n’offre donc aucune propriété visuelle. Nous proposons ici une adaptation du système pour les handicapés n’ayant qu’une déficience visuelle partielle. Nous espérons fournir à cette population des outils performants qui leur permettront de naviguer sur l’internet de façon efficace et agréable. En effet, grâce à une exploration non-linéaire (qui devrait améliorer l’orientation spatiale) et une interface multimodale (qui sollicite la vue, l’ouïe et le toucher), nous pensons réduire fortement le sentiment de frustration qu’évoquent les malvoyants. Nous avons posé l’hypothèse qu’une exploration non-linéaire et trimodale d’un site internet avec TactoColor est plus satisfaisante et efficace qu’une exploration non-linéaire bimodale avec TactoWeb (sans retour visuel). TactoColor a été adapté pour les malvoyants en ajoutant des indices visuels traduisant les composantes de la page (liens, menus, boutons) qui devraient rendre l’exploration plus aisée. Pour vérifier notre hypothèse, les deux versions du logiciel ont été évaluées par des malvoyants. Ainsi, les participants ont commencé soit avec TactoWeb, soit avec TactoColor afin de ne pas favoriser une des versions. La qualité de la navigation, son efficacité et son efficience ont été analysées en se basant sur le temps nécessaire à l’accomplissement d’une tâche, ainsi que la facilité ou la difficulté évoquée par le participant. Aussi, à la fin de chaque session, nous avons demandé leur avis aux participants, grâce à un questionnaire d’évaluation, ce qui nous a permis d’avoir leur retour sur notre logiciel après leur brève expérience. Tous ces relevés nous ont permis de déterminer que l’ajout des couleurs entraine une exploration plus rapide des pages web et une meilleure orientation spatiale. Par contre les performances très différentes des participants ne permettent pas de dire si la présence des couleurs facilite la complétion des tâches.