Acquisition de la maladie du légionnaire suite à une exposition domestique

Mémoire numérisé par la Direction des bibliothèques de l'Université de Montréal.

PKCbêta1 intervient dans l'action d'une concentration élevée en glucose sur l'expression de l'angiotensinogène et l'hypertrophie des IRPTC

Mémoire numérisé par la Direction des bibliothèques de l'Université de Montréal.

Altération des mécanismes physiologiques et moléculaires par un supplément sodique au cours de la gestation chez la rate : modèle animal de pré-éclampsie

Thèse numérisée par la Direction des bibliothèques de l'Université de Montréal.

Études des différences sexuelles dans les systèmes cérébraux régulateurs de la réponse de stress et des émotions chez le rat

Mémoire numérisé par la Direction des bibliothèques de l'Université de Montréal.

Étude du rôle de l'acide rétinoïque dans le développement de la prostate

Mémoire numérisé par la Direction des bibliothèques de l'Université de Montréal.

Les actions proinflammatoires de l'angiotensine II sont dépendantes de la phosphorylation de p65 par le complexe IkappaB kinase

Mémoire numérisé par la Direction des bibliothèques de l'Université de Montréal.

Modulation des neurones dopaminergiques du mésencéphale par la neurotensine

Thèse numérisée par la Direction des bibliothèques de l'Université de Montréal.

Développement d'une approche expérimentale permettant l'évaluation de la cinématique tridimensionnelle de l'articulation glénohumérale

Mémoire numérisé par la Direction des bibliothèques de l'Université de Montréal.

Analyse des mécanismes d'échec des endoprothèses couvertes et stimulation de la formation néointimale in vitro : vers un meilleur traitement des anévrismes de l'aorte abdominale

Mémoire numérisé par la Direction des bibliothèques de l'Université de Montréal.

Contribution des réserves calciques présynaptiques et gliales dans la modulation de la transmission synaptique à la jonction neuromusculaire de la grenouille Rana pipiens

Thèse numérisée par la Direction des bibliothèques de l'Université de Montréal.

Principes de communication et rôle social du chercheur en matière de transfert de connaissances : une dualité source de questionnements éthiques

Essai / Essay

Mineralogical (bulk rock and clay fraction) and stable isotope composition (d13C, d18O) of Aptian deposits of the Bir Oum Ali succession, central Tunisia

Alternations between siliciclastic, carbonate and evaporitic sedimentary systems, as recorded in the Aptian mixed succession of southern Tunisia, reflect profound palaeoceanographic and palaeoclimatic changes in this area of the southern Tethyan margin. The evolution from Urgonian-type carbonates (Berrani Formation, lower Aptian) at the base of the series, to intervals dominated by gypsum or detrital deposits in the remainder of the Aptian is thought to result from the interplay between climate change and tectonic activity that affected North Africa. Based on the evolution of clay mineral assemblages, the early Aptian is interpreted as having been dominated by slightly humid conditions, since smectitic minerals are observed. Near the early to late Aptian boundary, the onset of a gypsiferous sedimentation is associated with the appearance of palygorskite and sepiolite, which supports the installation of arid conditions in this area of the southern Tethyan margin. The evaporitic sedimentation may have also been promoted by the peculiar tectonic setting of the Bir Oum Ali area during the Aptian, where local subsidence may have been tectonically enhanced linked to the opening of northern and central Atlantic. Stress associated with the west and central African rift systems may have triggered the development of NW-SE, hemi-graben structures. Uplifted areas may have constituted potential new sources for clastic material that has been subsequently deposited during the late Aptian. Chemostratigraphic (d13C) correlation of the Bir Oum Ali succession with other peri-Tethyan regions complements biostratigraphic findings, and indicates that a potential expression of the Oceanic Anoxic Event (OAE) 1a may be preserved in this area of Tunisia. Although the characteristic negative spike at the base of this event is not recognized in the present study, a subsequent, large positive excursion with d13C values is of similar amplitude and absolute values to that reported from other peri-Tethyan regions, thus supporting the identification of isotopic segments C4-C7 of the OAE1a. The absence of the negative spike may be linked to either non preservation or non deposition: the OAE1a occurred in a global transgressive context, and since the Bir Oum Ali region was located in the innermost part of the southern Tethyan margin during most of the Aptian, stratigraphic hiatuses may have been longer than in other regions of the Tethys. This emphasizes the importance of integrating several stratigraphic disciplines (bio-, chemo- and sequence stratigraphy) when performing long-distance correlation.

n-alkane carbon isotope ratios in plants and recent lake sediments from Cameroon

Trees and shrubs in tropical Africa use the C3 cycle as a carbon fixation pathway during photosynthesis, while grasses and sedges mostly use the C4 cycle. Leaf-wax lipids from sedimentary archives such as the long-chain n-alkanes (e.g., n-C27 to n-C33) inherit carbon isotope ratios that are representative of the carbon fixation pathway. Therefore, n-alkane d13C values are often used to reconstruct past C3/C4 composition of vegetation, assuming that the relative proportions of C3 and C4 leaf waxes reflect the relative proportions of C3 and C4 plants. We have compared the d13C values of n-alkanes from modern C3 and C4 plants with previously published values from recent lake sediments and provide a framework for estimating the fractional contribution (areal-based) of C3 vegetation cover (fC3) represented by these sedimentary archives. Samples were collected in Cameroon, across a latitudinal transect that accommodates a wide range of climate zones and vegetation types, as reflected in the progressive northward replacement of C3-dominated rain forest by C4-dominated savanna. The C3 plants analysed were characterised by substantially higher abundances of n-C29 alkanes and by substantially lower abundances of n-C33 alkanes than the C4 plants. Furthermore, the sedimentary d13C values of n-C29 and n-C31 alkanes from recent lake sediments in Cameroon (-37.4 per mil to -26.5 per mil) were generally within the range of d13C values for C3 plants, even when from sites where C4 plants dominated the catchment vegetation. In such cases simple linear mixing models fail to accurately reconstruct the relative proportions of C3 and C4 vegetation cover when using the d13C values of sedimentary n-alkanes, overestimating the proportion of C3 vegetation, likely as a consequence of the differences in plant wax production, preservation, transport, and/or deposition between C3 and C4 plants. We therefore tested a set of non-linear binary mixing models using d13C values from both C3 and C4 vegetation as end-members. The non-linear models included a sigmoid function (sine-squared) that describes small variations in the fC3 values as the minimum and maximum d13C values are approached, and a hyperbolic function that takes into account the differences between C3 and C4 plants discussed above. Model fitting and the estimation of uncertainties were completed using the Monte Carlo algorithm and can be improved by future data addition. Models that provided the best fit with the observed d13C values of sedimentary n-alkanes were either hyperbolic functions or a combination of hyperbolic and sine-squared functions. Such non-linear models may be used to convert d13C measurements on sedimentary n-alkanes directly into reconstructions of C3 vegetation cover.