The Role of PP2A Regulatory Subunit B56 in Dictyostelium Discoideum Motility

Protein Phosphatase 2A, PP2A, is a heterotrimeric threonine/serine phosphatase system that is involved in a variety of cellular processes. This phosphatase is composed ofthree subunits: a catalytic subunit (C subunit), a scaffolding subunit (A subunit), and a regulatory subunit (B subunit). The regulatory subunit B is divided into four subclasses, B, B' (B56), B'' and B'' '. Studies showed that PP2A/B56 complexes regulate development of Dictyostelium and other metazoan cells. In addition to development, our experimental data suggest that PP2A/B56 complex also plays an important role in Dictyostelium cell motility. Cells lacking B56 was generated previously in our laboratory (Lee et al., 2008). Further studies showed that b56- cells are compromised in random cell motility compared to the wild type (AX3) cells. In contrast, b56 cells with re-introduced B56 displayed wild-type like motilities. Furthermore, one of the colleagues in our laboratory found that one of the Dictyostelium Ras species, RasG, associates with PP2A/B56 complex and RasG activation is compromised in b56- cells. Considering that Ras proteins are central in cellular motility regulation, PP2A/B56 complex may modulate cell motility through regulating Ras. We propose to determine if an introduction of constitutive active RasG proteins improves compromised b56- cell motility.

The function of the Saccharomyces Cerevisiae ribonucleotide reductase second [beta] subunit in DNA repair

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

Aerosol properties associated with air masses arriving into the North East Atlantic during the 2008 Mace Head EUCAARI intensive observing period: an overview

As part of the EUCAARI Intensive Observing Period, a 4-week campaign to measure aerosol physical, chemical and optical properties, atmospheric structure, and cloud microphysics was conducted from mid-May to mid-June, 2008 at the Mace Head Atmospheric Research Station, located at the interface of Western Europe and the N. E. Atlantic and centered on the west Irish coastline. During the campaign, continental air masses comprising both young and aged continental plumes were encountered, along with polar, Arctic and tropical air masses. Polluted-continental aerosol concentrations were of the order of 3000 cm(-3), while background marine air aerosol concentrations were between 400-600 cm(-3). The highest marine air concentrations occurred in polar air masses in which a 15 nm nucleation mode, with concentration of 1100 cm(-3), was observed and attributed to open ocean particle formation. Continental air submicron chemical composition (excluding refractory sea salt) was dominated by organic matter, closely followed by sulphate mass. Although the concentrations and size distribution spectral shape were almost identical for the young and aged continental cases, hygroscopic growth factors (GF) and cloud condensation nuclei (CCN) to total condensation nuclei (CN) concentration ratios were significantly less in the younger pollution plume, indicating a more oxidized organic component to the aged continental plume. The difference in chemical composition and hygroscopic growth factor appear to result in a 40-50% impact on aerosol scattering coefficients and Aerosol Optical Depth, despite almost identical aerosol microphysical properties in both cases, with the higher values been recorded for the more aged case. For the CCN/CN ratio, the highest ratios were seen in the more age plume. In marine air, sulphate mass dominated the sub-micron component, followed by water soluble organic carbon, which, in turn, was dominated by methanesulphonic acid (MSA). Sulphate concentrations were highest in marine tropical air - even higher than in continental air. MSA was present at twice the concentrations of previously-reported concentrations at the same location and the same season. Both continental and marine air exhibited aerosol GFs significantly less than ammonium sulphate aerosol pointing to a significant organic contribution to all air mass aerosol properties.

The function of the Saccharomyces Cerevisiae ribonucleotide reductase second [beta] subunit in DNA repair

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

Molecular mechanism of activation-triggered subunit exchange in Ca(2+)/calmodulin-dependent protein kinase II.

Activation triggers the exchange of subunits in Ca(2+)/calmodulin-dependent protein kinase II (CaMKII), an oligomeric enzyme that is critical for learning, memory, and cardiac function. The mechanism by which subunit exchange occurs remains elusive. We show that the human CaMKII holoenzyme exists in dodecameric and tetradecameric forms, and that the calmodulin (CaM)-binding element of CaMKII can bind to the hub of the holoenzyme and destabilize it to release dimers. The structures of CaMKII from two distantly diverged organisms suggest that the CaM-binding element of activated CaMKII acts as a wedge by docking at intersubunit interfaces in the hub. This converts the hub into a spiral form that can release or gain CaMKII dimers. Our data reveal a three-way competition for the CaM-binding element, whereby phosphorylation biases it towards the hub interface, away from the kinase domain and calmodulin, thus unlocking the ability of activated CaMKII holoenzymes to exchange dimers with unactivated ones.

Molecular mechanism of activation-triggered subunit exchange in Ca(2+)/calmodulin-dependent protein kinase II.

Activation triggers the exchange of subunits in Ca(2+)/calmodulin-dependent protein kinase II (CaMKII), an oligomeric enzyme that is critical for learning, memory, and cardiac function. The mechanism by which subunit exchange occurs remains elusive. We show that the human CaMKII holoenzyme exists in dodecameric and tetradecameric forms, and that the calmodulin (CaM)-binding element of CaMKII can bind to the hub of the holoenzyme and destabilize it to release dimers. The structures of CaMKII from two distantly diverged organisms suggest that the CaM-binding element of activated CaMKII acts as a wedge by docking at intersubunit interfaces in the hub. This converts the hub into a spiral form that can release or gain CaMKII dimers. Our data reveal a three-way competition for the CaM-binding element, whereby phosphorylation biases it towards the hub interface, away from the kinase domain and calmodulin, thus unlocking the ability of activated CaMKII holoenzymes to exchange dimers with unactivated ones.

Richard Aldington’s Images, the Metropolis and the Masses.

Richard Aldington’s city poems in the latter part of his 1915 collection Images are concerned with the masses who inhabit the modern city. Aldington is at pains to stress his distinction from those he perceives as an increasingly homogenized crowd. This paper examines the literary, linguistic and rhetorical strategies by which Aldington ‘others’ the masses, and sets them in the context of contemporary studies of the crowd, focusing on the work of Gustave Le Bon and C. F. G. Masterman. Aldington’s poetry is a product of the environment he sees as unsatisfactory, but he searches for solutions in a range of literary traditions which write the city.

Structure, transports and transformations of the water masses in the Atlantic Subpolar Gyre

We discuss the distributions and transports of the main water masses in the North Atlantic Subpolar Gyre (NASPG) for the mean of the period 2002–2010 (OVIDE sections 2002–2010 every other year), as well as the inter-annual variability of the water mass structure from 1997 (4x and METEOR sections) to 2010. The water mass structure of the NASPG, quantitatively assessed by means of an Optimum MultiParameter analysis (with 14 water masses), was combined with the velocity fields resulting from previous studies using inverse models to obtain the water mass volume transports. We also evaluate the relative contribution to the Atlantic Meridional Overturning Circulation (AMOC) of the main water masses characterizing the NASPG, identifying the water masses that contribute to the AMOC variability. The reduction of the magnitude of the upper limb of the AMOC between 1997 and the 2000s is associated with the reduction in the northward transport of the Central Waters. This reduction of the northward flow of the AMOC is partially compensated by the reduction of the southward flow of the lower limb of the AMOC, associated with the decrease in the transports of Polar Intermediate Water and Subpolar Mode Water (SPMW) in the Irminger Basin. We also decompose the flow over the Reykjanes Ridge from the East North Atlantic Basin to the Irminger Basin (9.4 ± 4.7 Sv) into the contributions of the Central Waters (2.1 ± 1.8 Sv), Labrador Sea Water (LSW, 2.4 ± 2.0 Sv), Subarctic Intermediate Water (SAIW, 4.0 ± 0.5 Sv) and Iceland–Scotland Overflow Water (ISOW, 0.9 ± 0.9 Sv). Once LSW and ISOW cross over the Reykjanes Ridge, favoured by the strong mixing around it, they leave the Irminger Basin through the deep-to-bottom levels. The results also give insights into the water mass transformations within the NASPG, such as the contribution of the Central Waters and SAIW to the formation of the different varieties of SPMW due to air–sea interaction.

Directive cadre sur l’eau - Bassin Loire-Bretagne. Contrôle de surveillance dans les masses d’eau côtières et de transition. Actions menées par Ifremer en 2014

Le contrôle de surveillance 2014 pour la DCE appliquée dans les eaux littorales de Loire Bretagne a porté sur les 25 masses d’eau côtières (sur 39 au total) et les 16 masses d’eau de transition (sur 30 au total) retenues au titre du contrôle de surveillance. L’ensemble des résultats acquis, aussi bien sur les paramètres biologiques que chimiques, a permis de mettre à jour l’évaluation de l’état des masses d’eau affiché sur l’atlas DCE accessible sur la page web d’Envlit correspondante.

Expertise sur 3 masses d’eau de la Réunion (étangs de Saint-Paul et du Gol) et de Martinique (étang des Salines) : typologie et surveillance DCE

Trois masses d’eau situées sur le littoral de l’île de la Réunion et de la Martinique présentent des fonctionnements et des caractéristiques atypiques, ce qui pose actuellement des difficultés dans le cadre de l’application de la DCE. Les deux masses d’eau réunionnaises, l’étang du Gol et l’étang de Saint-Paul, sont actuellement identifiées en tant que plans d’eau au titre de la DCE. La masse d’eau martiniquaise, l’étang des Salines, est quant à elle identifiée en tant que masse d’eau de transition. L’objectif de cette étude est d’apporter une expertise, sur la base des données disponibles et des échanges avec les experts locaux et nationaux, concernant : · la typologie des masses d’eau, · les paramètres chimiques, physico-chimiques et biologiques pertinents à suivre dans le cadre de la surveillance DCE, · des pistes de travail pour consolider des grilles de diagnostic sur les masses d’eau. Cette expertise s’appuie également sur les retours d’expériences et les études réalisées dans le cadre de la mise en oeuvre de la DCE sur les lagunes des bassins Rhône Méditerranée et Corse, dont la morphologie et le fonctionnement se rapprochent des trois masses d’eau étudiées. L’analyse des données et études fournies sur les étangs réunionnais du Gol et de Saint-Paul conduit à poser la question de la pertinence de leur maintien dans le référentiel des masses d’eau au titre de la DCE. Si le choix est cependant fait de conserver ces étangs en tant que masses d’eau DCE, leurs caractéristiques correspondraient à la typologie des eaux de transition et à la gamme de salinité oligohaline. Des recommandations sont formulées en termes d’études complémentaires visant à préciser le fonctionnement hydrologique de ces étangs et de priorisation des suivis de leur qualité physico-chimique et biologique, pour aboutir à une surveillance DCE pérenne. Les recommandations formulées à partir des données fournies sur l’étang martiniquais des Salines concernent l’évaluation des pressions anthropiques pesant sur cette masse d’eau, la priorisation des suivis de sa qualité chimique, physico-chimique et biologique dans le cadre de la surveillance DCE. Des pistes sont également données pour l’élaboration et la consolidation de grilles de diagnostic adaptées à cet étang.

Calculable lepton masses, seesaw relations, and four neutrino mixings in a 3-3-1 model with an extra U(1) symmetry

We propose a scheme in which the masses of the heavier leptons obey seesaw type relations. The light lepton masses, except the electron and the electron neutrino ones, are generated by one loop level radiative corrections. We work in a version of the 3-3-1 electroweak model that predicts singlets (charged and neutral) of heavy leptons beyond the known ones. An extra U(1)(Omega) symmetry is introduced in order to avoid the light leptons getting masses at the tree level. The electron mass induces an explicit symmetry breaking at U(1)(Omega). We discuss also the mixing matrix among four neutrinos. The new energy scale required is not higher than a few TeV.