Les licenciements collectifs au Québec : portée et efficacité de la règle de droit

Au cours des dernières années, le Québec fut durement touché par des vagues massives de licenciements collectifs. Après l’industrie du textile et du vêtement, c’est maintenant au tour de l’industrie forestière de subir, de plein fouet, les contrecoups d’une économie en pleine mutation. Les résultats des entrevues réalisées au printemps 2008, auprès des travailleurs de la Louisiana-Pacific de Saint-Michel-des-Saints, attestent de l’incapacité des dispositions sur le licenciement collectif à prendre adéquatement en charge les travailleurs victimes de ces fermetures d’usines. Pour évaluer le degré d’efficacité des dispositions sur le licenciement collectif, nous partons d’une étude empirique visant le processus de restructuration d’une grande entreprise papetière, qui conduit à la fermeture de son usine de traitement du bois à St-Michel-des-Saints. Des entretiens conduits auprès des travailleurs, des acteurs locaux comme des dirigeants du syndicat et de la communauté locale, et d’autres acteurs syndicaux et gouvernementaux permettent de reconstruire les étapes conduisant aux licenciements collectifs et à leur suite. Seule la mobilisation syndicale (blocus de l’usine) a permis de bonifier les faibles mesures palliatives prévues initialement par la loi. Cette mobilisation n’a toutefois pas empêché de constater des effets négatifs marqués (appauvrissement, sentiment d’exclusion, tensions familiales, etc.) chez les travailleurs victimes de ce licenciement massif.

Mobilités de travail et (re)construction des rapports sociaux au sein d’une communauté Hmong de Chine (province du Guizhou)

La mobilité rurale-urbaine est sans contredit l’un des phénomènes les plus marquants que la Chine a connus depuis ses réformes des années 1980. D’une ampleur colossale, elle a constitué un fondement essentiel de sa transition et de son développement économiques. Or, si l’impact social de cette mobilité a été abondamment étudié dans les villes où séjournent les paysans, il demeure peu connu dans leur communauté d’origine, et encore moins en contexte de « nationalité minoritaire ». Reposant sur une enquête de terrain de plus d’une année, cette thèse en géographie sociale examine la (re)construction sociale dans une communauté rurale et minoritaire (c.àd. Hmong ou Miao) de Chine en lien avec le phénomène de la mobilité de travail. D’une intensité croissante, la pratique de la mobilité de travail par les membres de cette communauté est double. Les migrants sont soit des herboristes ambulants dans les villes de l’espace régional, soit des travailleurs salariés dans les villes orientales du pays. L’utilisation d’une approche du changement social intégrant les sphères du réel et de l’imagination et prenant en compte les dimensions territoriale et économique du phénomène migratoire est originale. De même, l’importance égale portée aux discours et aux actions des migrants et des non-migrants dans le processus de transformation sociale se veut novatrice. Dans ses résultats, cette thèse fait état, premièrement, d’une refonte des logiques territoriales et économiques de la communauté étudiée sous l’effet du phénomène migratoire. De toute évidence, les fondements géographiques de son territoire se sont récemment complexifiés et multipliés. Désormais, une variété de lieux, de frontières, de réseaux sociaux et d’échelles se dessine dans les configurations territoriales de ses membres. Les implications économiques sont tout aussi patentes. Outre la forte dominance des transferts d’argent des migrants dans les budgets familiaux, les questions du développement et des inégalités aux différentes échelles de la communauté renvoient aujourd’hui essentiellement au fait migratoire. Deuxièmement, cette thèse montre la forte empreinte laissée par la mobilité dans la sphère sociale. Nécessitant soutien aux extrémités de leur parcours, les migrants sollicitent de plus en plus l’aide de leurs réseaux lignagers, claniques, villageois et matrilinéaires. Et dans ce processus, il n’est pas rare qu’ils enfreignent consciemment les principes hiérarchiques traditionnels de leurs rapports familiaux. Aussi, au travers de la mobilité, des groupes longtemps marginalisés, tels les femmes et les jeunes adultes, ont acquis estime, autonomie et pouvoir décisionnel. Parallèlement, l’ordre social s’est bouleversé. Ce n’est plus le volume de la production agricole, mais le nombre de travailleurs migrants qui détermine aujourd’hui les différentes classes sociales de la communauté. Finalement, dans le contexte plus large des populations rurales et minoritaires de Chine et du Massif sud-est asiatique, cette thèse fait ressortir l’importance d’aborder la question de l’impact social de la mobilité au-delà des paradigmes de la modernisation et de l’intégration. Contrairement à la plupart des écrits touchant à cette question, il ne suffit pas de porter le regard sur l’influence que les urbains et leur mode de vie soi-disant moderne exercent sur les migrants. Il est également nécessaire de reconnaître les capacités d’initiative et d’innovation sociale des membres de ces populations, migrants et non-migrants. Mais aussi, cette recherche démontre que la question identitaire se doit d’être prise en compte. Les sentiments de marginalité et de subordination demeurent vivaces au travers du phénomène migratoire. Et de tels sentiments semblent se traduire, le plus souvent, par un renforcement des liens sociaux et intracommunautaires au sein même de ces populations minoritaires.

Nothing New (Ethically) Under the Sun: Policy & Clinical Implications of Nanomedicine

Article

Lecture d'une ambivalence identitaire de la société martiniquaise. Essai psychanalytique d’une aliénation

Comme une grande partie des îles de la Caraïbe, pour des raisons économiques basées sur le mercantilisme, justifiées par une législation, la Martinique, née il y a trois siècles, a connu un emmêlement massif de diverses ethnies. Suite à l’abolition de l’esclavage en 1848 et à la crise agricole qui en découla, c’est un brassage de coutumes qui s’opéra avec l’immigration des Hindous, des Africains, des Chinois et des Indochinois. Ce faisant, ces coutumes ont conservé leurs traditions et croyances propres, expliquant ainsi la fusion d'éléments de ces cultures, encore présente aujourd’hui. En abolissant l’esclavage, la « Loi » abolit également la réification, rétablissant ainsi l’humanité de l’homme, puisque l’esclave noir était considéré comme un bien meuble . Il en résulte la création d’un nouveau monde, modifiant la vie culturelle, déployant des habitus, ainsi qu’une manière de penser et d’agir. Aussi, un nouveau langage se structure progressivement. En 1946, la Martinique est reconnue département français d’Amérique. Aujourd’hui, elle se trouve dans une dépendance économique et sociale. De cet état de fait, un conflit s’impose à l’Afro-Martiniquais quant à la question de l’identité. Il se trouve partagé entre le contexte franco-européen et le milieu afro-antillais. Cette contradiction émane aussi de situations de confrontation, d’où se dégage souvent un ressenti de « fatalité » voire de « malédiction » entraînant « un sentiment de culpabilité collective » d’oser défier l’ordre social en place. Notre recherche vise à analyser ce dilemme de la dépendance à partir de l’énoncé des malédictions puis des considérations historiques suivies d'une perspective psychanalytique.

Apprendre à composer sainement avec les technologies de l'information et de la communication (TIC): le soutien de l'entourage des jeunes dans ses fonctions d'accompagnement et d'éducation aux médias numériques

Essai critique de stage d'intervention présenté à la faculté des arts et des sciences en vue de l'obtention du grade de Maîtrise ès sciences (M. Sc.) en service social

Las fuentes naturales del término municipal de Sant Feliu de Guíxols (Girona)

The behaviour of 21 natural springs in a granític massif is studied in this survey. Geomorphological features of the zone are described as well as water circulation and rising 25 parametres of each of them are analysed ans conclusions are withdrawn regarding geological conditions of rising, course, chemism and potability

A GIS-based empirical model for vegetation prediction in Lefka Ori, Crete

The aim of the study was to establish and verify a predictive vegetation model for plant community distribution in the alti-Mediterranean zone of the Lefka Ori massif, western Crete. Based on previous work three variables were identified as significant determinants of plant community distribution, namely altitude, slope angle and geomorphic landform. The response of four community types against these variables was tested using classification trees analysis in order to model community type occurrence. V-fold cross-validation plots were used to determine the length of the best fitting tree. The final 9node tree selected, classified correctly 92.5% of the samples. The results were used to provide decision rules for the construction of a spatial model for each community type. The model was implemented within a Geographical Information System (GIS) to predict the distribution of each community type in the study site. The evaluation of the model in the field using an error matrix gave an overall accuracy of 71%. The user's accuracy was higher for the Crepis-Cirsium (100%) and Telephium-Herniaria community type (66.7%) and relatively lower for the Peucedanum-Alyssum and Dianthus-Lomelosia community types (63.2% and 62.5%, respectively). Misclassification and field validation points to the need for improved geomorphological mapping and suggests the presence of transitional communities between existing community types.

Vascular plant diversity and climate change in the alpine zone of the Lefka Ori, Crete

The aim of this study is to analyse the vascular flora and the local climate along an altitudinal gradient in the Lefka Ori massif Crete and to evaluate the potential effects of climate change on the plant diversity of the sub-alpine and alpine zones. It provides a quantitative/qualitative analysis of vegetation-environment relationships for four summits along an altitude gradient on the Lefka Ori massif Crete (1664-2339 m). The GLORIA multi-summit approach was used to provide vegetation and floristic data together with temperature records for every summit. Species richness and species turnover was calculated together with floristic similarity between the summits. 70 species were recorded, 20 of which were endemic, belonging to 23 different families. Cretan endemics dominate at these high altitudes. Species richness and turnover decreased with altitude. The two highest summits showed greater floristic similarity. Only 20% of the total flora recorded reaches the highest summit while 10% is common among summits. Overall there was a 4.96 degrees C decrease in temperature along the 675 m gradient. Given a scenario of temperature increase the ecotone between the sub-alpine and alpine zone would be likely to have the greatest species turnover. Southern exposures are likely to be invaded first by thermophilous species while northern exposures are likely to be more resistant to changes. Species distribution shifts will also depend on habitat availability. Many, already threatened, local endemic species will be affected first.

A GIS-based empirical model for vegetation prediction in Lefka Ori, Crete

The aim of the study was to establish and verify a predictive vegetation model for plant community distribution in the alti-Mediterranean zone of the Lefka Ori massif, western Crete. Based on previous work three variables were identified as significant determinants of plant community distribution, namely altitude, slope angle and geomorphic landform. The response of four community types against these variables was tested using classification trees analysis in order to model community type occurrence. V-fold cross-validation plots were used to determine the length of the best fitting tree. The final 9node tree selected, classified correctly 92.5% of the samples. The results were used to provide decision rules for the construction of a spatial model for each community type. The model was implemented within a Geographical Information System (GIS) to predict the distribution of each community type in the study site. The evaluation of the model in the field using an error matrix gave an overall accuracy of 71%. The user's accuracy was higher for the Crepis-Cirsium (100%) and Telephium-Herniaria community type (66.7%) and relatively lower for the Peucedanum-Alyssum and Dianthus-Lomelosia community types (63.2% and 62.5%, respectively). Misclassification and field validation points to the need for improved geomorphological mapping and suggests the presence of transitional communities between existing community types.

Towards a European tephrochronological framework for Termination 1 and the Early Holocene

The record of deposition of tephras in Europe and the North Atlantic during the period 18.5–8.0 ¹⁴C ka BP (the Last Termination and Early Holocene) is reviewed. Altogether, 34 tephras originating from four main volcanic provinces (Iceland, the Eifel district, the Massif Central and Italy) have been identified so far in geological sequences spanning this time–interval. Most of the records have been based, until very recently, on observations of visible layers of tephras. Here, we report on the potential for extending the areas over which some of the tephras can be traced by the search for layers of micro–tephra, which are not visible to the naked eye, and on the use of geochemical methods to correlate them with known tephra horizons. This approach has greatly extended the area in Northern Europe over which the Vedde Ash can be traced. The same potential exists in southern Europe, which is demonstrated for the first time by the discovery of a distinct layer of micro–tephra of the Neapolitan Yellow Tuff in a site in the Northern Apennines in Italy, far to the north of the occurrences of visible records of this tephra. The paper closes by considering the potential for developing a robust European tephrostratigraphy to underpin the chronology of records of the Last Termination and Early Holocene, thereby promoting a better understanding of the nature, timing and environmental effects of the abrupt climatic changes that characterized this period.

The Sphene-Centered Ocellar Texture: An Effect of Grain-Supported Flow and Melt Migration in a Hyperdense Magma Mush

The sphene-centered ocellar texture consists of leucocratic ocelli with sphene (titanite) crystals at the center, enclosed in a biotite-rich matrix. This texture has been recognized worldwide in hybrid intermediate rocks. On the basis of structural, petrological, and geochronological data from selected outcrops of the Variscan Ribadelago pluton (NW Iberian Massif), we propose that the ocelli were formed by migration and accumulation of a residual melt through a plagioclase- and biotite-dominated crystalline framework. At the late stage of crystallization, the magma acted as a hyperdense suspension and reacted to the pressure gradient caused by the regional stress field, entering the domain of grain-supported flow. Microstructures reveal that aligned crystal domains arose in the crystal framework from the shearing and compaction of the crystal mush and behaved as magmatic microshears. Relative displacement of adjacent crystal clusters along these microshears corresponded to the onset of Reynolds dilatancy that generated an expansion of the crystal mush, involving melt migration and pore aperture. The mineralogy of the ocelli, dominated by andesine and sphene, represents the composition of the migrating melt. The chemistry of this late, Ti-rich melt stems from the incongruent melting of biotite. Magmatic sphene from the ocelli yields a U-Pb age of 317 +/- 1 Ma, which represents the final crystallization of the hybridized magmatic system. Moreover, this texture offers an opportunity to better understand the rheological behavior of highly crystallized magmas.

GEOCHEMISTRY AND U-PB ZIRCON AGE OF THE INTERNAL OSSA-MORENA ZONE OPHIOLITE SEQUENCES: A REMNANT OF RHEIC OCEAN IN SW IBERIA

The Early Paleozoic geodynamic evolution in SW Iberia is believed to have been dominated by the opening of the Rheic Ocean. The Rheic Ocean is generally accepted to have resulted from the drift of peri-Gondwanan terranes such as Avalonia from the northern margin of Gondwana during Late Cambrian-Early Ordovician times. The closure of the Rheic Ocean was the final result of a continent-continent collision between Gondwana and Laurussia that produced the Variscan orogen. The Ossa-Morena Zone is a peri-Gondwana terrane, which preserves spread fragments of ophiolites - the Internal Ossa-Morena Zones Ophiolite Sequences (IOMZOS). The final patchwork of the IOMZOS shows a complete oceanic lithospheric sequence with geochemical characteristics similar to the ocean-floor basalts, without any orogenic fingerprint and/or crustal contamination. The IOMZOS were obducted and imbricated with high pressure lithologies. Based on structural, petrological and whole-rock geochemical data, the authors argue that the IOMZOS represent fragments of the oceanic lithosphere from the Rheic Ocean. Zircon SHRIMP U-Pb geochronological data on metagabbros point to an age of ca. 480 Ma for IOMZOS, providing evidence of a well-developed ocean in SW Iberia during this period, reinforcing the interpretation of the Rheic Ocean as a wide ocean among the peri-Gondwanan terranes during Early Ordovician times.

Mafic dykes at the southwestern margin of Eastern Ghats belt: Evidence of rifting and collision

The southwestern margin of the Eastern Ghats Belt characteristically exposes mafic dykes intruding massif-type charnockites. Dykes of olivine basalt of alkaline composition have characteristic trace element signatures comparable with Ocean Island Basalt (OIB). Most importantly strong positive Nb anomaly and low values of Zr/Nb ratio are consistent with OIB source of the mafic dykes. K-Ar isotopic data indicate two cooling ages at 740 and 530 Ma. The Pan-African thermal event could be related to reactivation of major shear zones and represented by leuco-granite vein along minor shear bands. And 740 Ma cooling age may indicate the low grade metamorphic imprints, noted in some of the dykes. Although no intrusion age could be determined from the present dataset, it could be constrained by some age data of the host charnockite gneiss and Alkaline rocks of the adjacent Prakasam Province. Assuming an intrusion age of similar to 1.3 Ga, Sr-Nd isotopic composition of the dykes indicate that they preserved time-integrated LREE enrichment. In view of the chemical signatures of OIB source, the mafic dykes could as well be related to continental rifting, around 1.3 Ga, which may have been initiated by intra-plate volcanism.

Age and geochemistry of mantle peridotites and diorite dykes from the Baldissero body: Insights into the Paleozoic-Mesozoic evolution of the Southern Alps

Trace element and isotopic data obtained for mantle spinel Iherzolites and diorite dykes from the Baldissero massif (Ivrea-Verbano Zone, Western Italy) provide new, valuable constraints on the petrologic and geodynamic evolution of the Southern Alps in Paleozoic to Mesozoic times. Whole rock and mineral chemistry indicates that Baldissero Iherzolites can be regarded as refractory mantle residues following limited melt extraction. In particular, the Light Rare Earth Elements (LREE)-depleted and fractionated compositions of whole rock and clinopyroxene closely match modelling results for refractory residues after low degrees (similar to 4-5%) of near-fractional melting of depleted mantle, possibly under garnet-facies conditions. Following this, the peridotite sequence experienced subsolidus re-equilibration at lithospheric spinel-facies conditions and intrusion of several generations of dykes. However, Iherzolites far from dykes show very modest metasomatic changes, as evidenced by the crystallisation of accessory titanian pargasite and the occurrence of very slight enrichments in highly incompatible trace elements (e.g. Nb). The Re-Os data for Iherzolites far from the dykes yield a 376 Ma (Upper Devonian) model age that is considered to record a partial melting event related to the Variscan orogenic cycle s.l. Dioritic dykes cutting the mantle sequence have whole rock, clinopyroxene and plagioclase characterised by high radiogenic Nd and low radiogenic Sr, which point to a depleted to slightly enriched mantle source. Whole rock and mafic phases of diorites have high Mg# values that positively correlate with the incompatible trace element concentrations. The peridotite at the dyke contact is enriched in orthopyroxene, iron and incompatible trace elements with respect to the Iherzolites far from dykes. Numerical simulations indicate that the geochemical characteristics of the diorites can be explained by flow of a hydrous, silica-saturated melt accompanied by reaction with the ambient peridotite and fractional crystallisation. The composition of the more primitive melts calculated in equilibrium with the diorite minerals show tholeiitic to transitional affinity. Internal Sm-Nd, three-point isochrons obtained for two dykes suggest an Upper Triassic-Lower Jurassic emplacement age (from 204 31 to 198 29 Ma). Mesozoic igneous events are unknown in the southern Ivrea-Verbano Zone (IVZ), but the intrusion of hydrous melts, mostly silica-saturated, have been well documented in the Finero region, i.e. the northernmost part of IVZ and Triassic magmatism with calc-alkaline to shoshonitic affinity is abundant throughout the Central-Eastern Alps. The geochemical and chronological features of the Baldissero diorites shed new light on the geodynamic evolution of the Southern Alps before the opening of the Jurassic Tethys. (C) 2010 Elsevier B.V. All rights reserved.

Conflicting structural and geochronological data from the Ibituruna quartz-syenite (SE Brazil): Effect of protracted ""hot"" orogeny and slow cooling rate?

The Ibituruna quartz-syenite was emplaced as a sill in the Ribeira-Aracuai Neoproterozoic belt (Southeastern Brazil) during the last stages of the Gondwana supercontinent amalgamation. We have measured the Anisotropy of Magnetic Susceptibility (AMS) in samples from the Ibituruna sill to unravel its magnetic fabric that is regarded as a proxy for its magmatic fabric. A large magnetic anisotropy, dominantly due to magnetite, and a consistent magnetic fabric have been determined over the entire Ibituruna massif. The magmatic foliation and lineation are strikingly parallel to the solid-state mylonitic foliation and lineation measured in the country-rock. Altogether, these observations suggest that the Ibituruna sill was emplaced during the high temperature (similar to 750 degrees C) regional deformation and was deformed before full solidification coherently with its country-rock. Unexpectedly, geochronological data suggest a rather different conclusion. LA-ICP-MS and SHRIMP ages of zircons from the Ibituruna quartz-syenite are in the range 530-535 Ma and LA-ICP-MS ages of zircons and monazites from synkinematic leucocratic veins in the country-rocks suggest a crystallization at similar to 570-580 Ma, i.e., an HT deformation >35My older than the emplacement of the Ibituruna quartz-syenite. Conclusions from the structural and the geochronological studies are therefore conflicting. A possible explanation arises from (40)Ar-(39)Ar thermochronology. We have dated amphiboles from the quartz-syenite, and amphiboles and biotites from the country-rock. Together with the ages of monazites and zircons in the country-rock, (40)Ar-(39)Ar mineral ages suggest a very low cooling rate: <3 degrees C/My between 570 and similar to 500 Ma and similar to 5 degrees C/My between 500 and 460 Ma. Assuming a protracted regional deformation consistent over tens of My, under such stable thermal conditions the fabric and microstructure of deformed rocks may remain almost unchanged even if they underwent and recorded strain pulses separated by long periods of time. This may be a characteristic of slow cooling ""hot orogens"" that rocks deformed at significantly different periods during the orogeny, but under roughly unchanged temperature conditions, may display almost indiscernible microstructure and fabric. (C) 2009 Elsevier B.V. All rights reserved.