Depleted arc volcanism in the Alboran Sea and shoshonitic volcanism in Morocco: geochemical and isotopic constraints on Neogene tectonic processes

Samples of volcanic rocks from Alboran Island, the Alboran Sea floor and from the Gourougou volcanic centre in northern Morocco have been analyzed for major and trace elements and Sr-Nd isotopes to test current theories on the tectonic geodynamic evolution of the Alboran Sea. The Alboran Island samples are low-K tholeiitic basaltic andesites whose depleted contents of HFS elements (similar to0.5xN-MORB), especially Nb (similar to0.2xN-MORB), show marked geochemical parallels with volcanics from immature intra-oceanic arcs and back-arc basins. Several of the submarine samples have similar compositions, one showing low-Ca boninite affinity. Nd-143/Nd-144 ratios fall in the same range as many island-arc and back-arc basin samples, whereas Sr-87/Sr-86 ratios (on leached samples) are somewhat more radiogenic. Our data point to active subduction taking place beneath the Alboran region in Miocene times, and imply the presence of an associated back-arc spreading centre. Our sea floor suite includes a few more evolved dacite and rhyolite samples with (Sr-87/Sr-86)(0) up to 0.717 that probably represent varying degrees of crustal melting. The shoshonite and high-K basaltic andesite lavas from Gourougou have comparable normalized incompatible-element enrichment diagrams and Ce/Y ratios to shoshonitic volcanics from oceanic island arcs, though they have less pronounced Nb deficits. They are much less LIL- and LREE-enriched than continental arc analogues and post-collisional shoshonites from Tibet. The magmas probably originated by melting in subcontinental lithospheric mantle that had experienced negligible subduction input. Sr-Nd isotope compositions point to significant crustal contamination which appears to account for the small Nb anomalies. The unmistakable supra-subduction zone (SSZ) signature shown by our Alboran basalts and basaltic andesite samples refutes geodynamic models that attribute all Neogene volcanism in the Alboran domain to decompression melting of upwelling asthenosphere arising from convective thinning of over-thickened lithosphere. Our data support recent models in which subsidence is caused by westward rollback of an eastward-dipping subduction zone beneath the westemmost Mediterranean. Moreover, severance of the lithosphere at the edges of the rolling-back slab provides opportunities for locally melting lithospheric mantle, providing a possible explanation for the shoshonitic volcanism seen in northern Morocco and more sporadically in SE Spain. (C) 2004 Elsevier B.V. All rights reserved.

Modeling of in-situ crystallization processes in the Permian mafic layered intrusion of Mont Collon (Dent Blanche nappe, western Alps)

The Mont Collon mafic complex is one of the best preserved examples of the Early Permian magmatism in the Central Alps, related to the intra-continental collapse of the Variscan belt. It mostly consists (> 95 vol.%) of ol+hy-nonnative plagioclase-wehrlites, olivine- and cpx-gabbros with cumulitic structures, crosscut by acid dikes. Pegmatitic gabbros, troctolites and anorthosites outcrop locally. A well-preserved cumulative, sequence is exposed in the Dents de Bertol area (center of intrusion). PT-calculations indicate that this layered magma chamber emplaced at mid-crustal levels at about 0.5 GPa and 1100 degrees C. The Mont Collon cumulitic rocks record little magmatic differentiation, as illustrated by the restricted range of clinopyroxene mg-number (Mg#(cpx)=83-89). Whole-rock incompatible trace-element contents (e.g. Nb, Zr, Ba) vary largely and without correlation with major-element composition. These features are characteristic of an in-situ crystallization process with variable amounts of interstitial liquid L trapped between the cumulus mineral phases. LA-ICPMS measurements show that trace-element distribution in the latter is homogeneous, pointing to subsolidus re-equilibration between crystals and interstitial melts. A quantitative modeling based on Langmuir's in-situ crystallization equation successfully duplicated the REE concentrations in cumulitic minerals of all rock facies of the intrusion. The calculated amounts of interstitial liquid L vary between 0 and 35% for degrees of differentiation F of 0 to 20%, relative to the least evolved facies of the intrusion. L values are well correlated with the modal proportions of interstitial amphibole and whole-rock incompatible trace-element concentrations (e.g. Zr, Nb) of the tested samples. However, the in-situ crystallization model reaches its limitations with rock containing high modal content of REE-bearing minerals (i.e. zircon), such as pegmatitic gabbros. Dikes of anorthositic composition, locally crosscutting the layered lithologies, evidence that the Mont Collon rocks evolved in open system with mixing of intercumulus liquids of different origins and possibly contrasting compositions. The proposed model is not able to resolve these complex open systems, but migrating liquids could be partly responsible for the observed dispersion of points in some correlation diagrams. Absence of significant differentiation with recurrent lithologies in the cumulitic pile of Dents de Bertol points to an efficiently convective magma chamber, with possible periodic replenishment, (c) 2005 Elsevier B.V. All rights reserved.

An interpretation of the deep seismic lines from the Penninic Alps of Valais (Switzerland)

The upper part of three deep seismic lines running across the Penninic Swiss Alps of Valais have been studied. Numerous reflectors illustrate the nappe structure of this internal part of the orogen. These reflectors, even at great depths (20-25 km), can be correlated with outcropping geological features and are most likely produced by lithological boundaries rather than by mylonites zones, which are hardly reflective in such an environment. Our interpretations, largely constrained by projections of the outcropping geology, have improved our knowledge of the deep structure of this segment of the Alpine belt, enhancing the importance of the backfolding and the crustal scale deformation phase which produced the Rawil-Valpelline depression and the Aar-Toce culmination. Furthermore we have here the possibility of correlating seismic patterns produced by ductile folds with the outcropping structures.

La ración de mantenimiento, la densidad de mantenimiento y la eficiencia de crecimiento de Engraulis ringens y Sardinops sagax como una medida de su potencia ecológica

Presentamos en este estudio resultados calculados sobre la potencia ecológica de la anchoveta y sardina peruana mediante el procesamiento de datos de los gastos metabólicos, velocidad de natación.e ingestión de alimento en relación a diferentes tallas de peces, temperaturas y densidades de alimento. Como medida de la potencia ecológica hemos calculado: (1) ración de mantenimiento, (2) la eficiencia de crecimiento y (3) densidad del alimento para mantenimiento. (para larvas). Asumiendo un alimento mixto de fito y zooplancton {1 g peso húmedo = 1000 cal) y una eficiencia de asimilación de 0.7 tenemos para la ración de mantenimiento expresada en calorías por individuo por día y en porcentaje del peso húmedo por día.

Palaeopigment accumulation and implcations for paleolimnology over the lost century for two Ontario lakes

Crawford Lake is a meromictic lake, which is 24 m deep and has an area of 2.5 ha, and has never been reported to have mixed below 16 m. Lady Evelyn Lake, which became a reservoir when a dam was built in 1916, is dimictic with a maximum depth of about 35 m. 1 My research proved that both native chlorophylls and the ratio of chlorophyll derivatives to total carotenoids were better preserved in the shallower lake (Crawford Lake) because it was meromictic. Thus the anaerobic conditions in Crawford Lake below 16 m (monimolimnion) provide excellent conditions for pigment preservation. Under such conditions, the preservation of both chlorophylls and carotenoids, including oscillaxanthin and myxoxanthophyll, are extremely good compared with those of Lady Evelyn Reservoir, in which anaerobic conditions are rarely encountered at the mud-water interface. During the period from 1500 to 1900 A. D. in Crawford Lake, the accumulation rates of oscillaxanthin and myxoxanthophyll were extremely high, but those of chlorophyll derivatives and total carotenoids were relatively low. This was correlated with the presence of a dense benthic mat of cyanobacteria near the lake's chemocline. Competition for light between the deep dwelling cyanobacteria and overlying phytoplankton in this meromictic lake would have been intensified as the lake became more and more eutrophic (1955-1991 A. D.). During the period from 1955 to 1991 A. D., the accumulation rates of chlorophyll derivatives and total carotenoids in the sediment core from Crawford Lake (0-7.5 cm, 1955-present) increased. During this same period, the accumulation rates of cyanobacterial pigments (Le. oscillaxanthin and myxoxanthophyll) declined as the lake became more eutrophic. Because the major cyanobacteria in Crawford Lake are benthic mat forming Lyngbya and Oscillatoria and not phytoplankton, eutrophication resulted in a decline of the mat forming algal pigments. This is important because in previous palaeolimnological studies the concentrations of oscillaxanthin and myxoxanthophyll have been used as correlates with lake trophic levels. The results of organic carbon a13c analysis on the Crawford Lake sediment core supported the conclusions from the pigment study as noted above. High values of a13c at the depth of 34-48 cm (1500-1760 A. D.) were related to a dense population of benthic Oscillatoria and Lyngbya living on the bottom of the lake during that period. The Oscillatoria and Lyngbya utilized the bicarbonate, which had a high a 13C value. Very low values were found at 0-7 cm in the Crawford sediment core. At this time phytoplankton was the main primary producer, which enriched 12C by photosynthetic assimilation.

Petrography, Petrochemistry and petrogenesis of Huronian volcanic rocks of the Elliot Lake region, Ontario

In the Elliot lake region of northern Ontario, Yolcanlc lava piles represent the lowermost units of the Huronian SUpergroup. These rocks general1y trend east-west and belong to the Elliot lake Group. They are s1tuated on the north and south limbs or the QuIrke lake Syncline. The volcanIc rocks of this study contain a secondary minerai assemblage consisting of actinolite, biotite, chlorIte, eptdote/cllnozoislte tttanomagnettte and calcite characteristic of greenschist metamorphism. Compilation of data suggests that metamorphism of the volcanic rocks proceeded between 325- and 425-C and between 2.4 and 4.7 kb. Geochemtcally these lavas represent tholeiitic and calc-alkaline assemblages. The tholeiites are character1sttcally enriched tn Fe and Tt and consist mainly of basalts, basaltic andesites and andesites. These rocks are believed to have formed by the partIal melting of a peridottte source at low P-T. In contrast, the calc-alkaline rocks are depleted in Fe and TI, but show a signIficant enrichment In 51 and Zr; andesIte Is the major rock type for thIs assemblage. I·t Is postUlated that the calc-alkalIne sU1te of rocks was the result of eIther the partIal meltIng of abasaltic·magma at shallow depth, or the melttng of s1al1c crustal materIal due to the added we1ght of tholeiitIc material on an unstable crust and to downwarplng processes Inttlated by convection cells.

The sedimentology of the lower Silurian whirlpool sandstone in subsurface Lake Erie, Ontario

The lower Silurian Whirlpool Sandstone is composed of two main units: a fluvial unit and an estuarine to transitional marine unit. The lowermost unit is made up of sandy braided fluvial deposits, in shallow valleys, that flowed towards the northwest. The fluvial channels are largely filled by cross-bedded, well sorted, quartzose sands, with little ripple crosslaminated or overbank shales. Erosionally overlying this lower unit are brackish water to marine deposits. In the east, this unit consists of estuarine channels and tidal flat deposits. The channels consist of fluvial sands at the base, changing upwards into brackish and tidally influenced channelized sandstones and shales. The estuarine channels flowed to the southwest. Westwards, the unit contains backbarrier facies with extensive washover deposits. Separating the backbarrier facies from shoreface sandstone facies to the west, are barrier island sands represented by barrier-foreshore facies. The barrier islands are dissected by tidal inlets characterized by fining upward abandonment sequences. Inlet deposits are also present west of the barrier island, abandoned by transgression on the shoreface. The sandy marine deposits are replaced to the west by carbonates of the Manitoulin Limestone. During the latest Ordovician, a hiatus in crustal loading during the Taconic Orogeny led to erosional offloading and crustal rebound, the eroded material distributed towards the west, northwest and north as the terrestrial deposits of the fluvial Whirlpool. The "anti-peripheral bulge" of the rebound interfered with the peripheral bulge of the Michigan Basin, nulling the Algonquin Arch, and allowing the detritus of the fluvial Whirlpool to spread onto the Algonquin Arch. The Taconic Orogeny resumed in the earliest Silurian with crustal loading to the south and southeast, and causing tilting of the surface slope in subsurface Lake Erie towards the ii southwest. Lowstand terrestrial deposits were scoured into the new slope. The new crustal loading also reactivated the peripheral bulge of the Appalachian Basin, allowing it to interact with the bulge of the Michigan Basin, raising the Algonquin Arch. The crustal loading depressed the Appalachian basin and allowed transgression to occur. The renewed Algonquin Arch allowed the early Silurian transgression to proceed up two slopes, one to the east and one to the west. The transgression to the east entered the lowstand valleys and created the estuarine Whirlpool. The rising arch caused progradation of the Manitoulin carbonates upon shoreface facies of the Whirlpool Sandstone and upon offshore facies of the Cabot Head Formation. Further crustal loading caused basin subsidence and rapid transgression, abandoning the Whirlpool estuary in an offshore setting.

Living between two cultures : personality and adaptation in Chinese immigrant youth /

The aim of the present study was to examine the relationship between shyness and acculturation modes of Chinese immigrant youth in Canada and whether shyness moderates the relationship between acculturation and adaptation. In addition, I examined whether shyness, in conjunction with sociability, moderates the relationship between acculturation and adaptation. Ninety-nine young Chinese immigrants (42 men), ranging in age from 16 to 26 years old, completed a questionnaire that assessed their demographic information, acculturation modes, shyness, sociability, psychological adaptation Oife satisfaction, self-esteem, and depression), and socio-cultural adaptation. Results showed that Chinese orientation was significantly and negatively correlated with age, generation status, English proficiency, and length of residence in Canada. In contrast, Canadian orientation was significantly and positively correlated with generation status, English proficiency, and length of residence in Canada. Canadian orientation was also significantly and negatively correlated with shyness and positively correlated with sociability and psychological and socio-cultural adaptation. Participants who were shyer were more likely to have poorer psychological and socio-cultural adaptation, and to report lower life satisfaction and self-esteem and higher depression. Results from hierarchical multiple regression analyses indicated that Chinese immigrant youth who were separated had higher scores on shyness than those who were integrated and assimilated. There were no significant differences in shyness between youth who were separated and youth who were marginalized, nor were there differences between youth who were integrated and those who were assimilated. Furthermore, integrated Chinese youth reported significantly higher scores in sociability than those who were separated and marginalized but not significantly higher than those who were assimilated.' Shyness did not moderate the relationship between acculturation modes and psychological and socio-cultural adaptation. Unfortunately, the hypothesis to examine if shyness, in combination with sociability, moderated the relationship between acculturation and psychological adaptation could not be tested in the present study because of limitations in cell sizes. The findings suggested that how Chinese immigrant youth acculturate in the receiving country might not be the crucial factor in determining their adaptation. Instead, other factors, such as personality characteristics and nature of the acculturating group, may playa more crucial role. Shyness may have important ramifications for the acculturation and adaptation of young Chinese immigrants to a new society.

Two rows : assimilative transformations impacting Six Nations' educational and communal circles

This study examines the current educational and community realities faced by a large First Nations community in Canada. First, the research explores the voices of youth and parents to determine the current issues and trends of an Aboriginal community. Second, the work discusses the transformation of Six Nations youth and parents and its impacts on student educational and community life. Third, I relate my personal experiences as a First Nation student, parent, and community agency representative.

The Art of Resisting Colonial Education

This thesis explores the efforts of discipline and resistance in the Indian Residential School (IRS) system in Canada. The IRS has origins in eighteenth and nineteenth century colonial policies of assimilation. While its goals aimed to transform Aboriginal children into Euro-Canadian adults the system has largely been proven ineffective and highly damaging to First Nation communities. This research discusses the complex connection between colonial curriculum and student resistance within the IRS. The discussion emphasizes students‟ abilities to creatively subvert disciplinary tactics and the methods of resistance used in the IRS context - with a focus on art and cultural persistence. It highlights a complicated relationship of disciplinary tactics and student resistance within the context of the IRS focusing on the relationship between curriculum and student product.

Indigenous Language Reclamation: The Learners Perspective

ABSTRACT This study explored the link between learning an Indigenous language and the meanings second language learners attach to their language recovery experiences. The study delves into the factors that motivate, enhance and serve as barriers to individual language revitalization efforts. With the goal of reasserting an Indigenous world view, the traditional teachings of the Ojibwe medicine wheel were combined with the lessons of the seven Grandfathers to provide a methodological basis for conducting ethical research with and for the benefit of First Nations people. Within the context of our relationships with self, community, spirit and environment, the pairing of Indigenous theory with the practical community experiences of Indigenous second language learners, demonstrates how Indigenous systems of thought and ontology lend themselves well to the critical understanding necessary to enhance the recovery our own endangered languages. These research findings indicate that there is a definite link between ancestral language reclamation and increased levels of self-esteem, a sense of grounded cultural identity and resilience, an overall sense of healing and the social responsibility that comes with receiving the gift of language. The barriers associated with learning an ancestral language intersect on multiple and often simultaneous levels making it difficult for the language learners to discover their origin.This research found that it was important for language learners to identify that they often carry a collective sense of shame associated with an internalized attachment to the modality of Indigeneity. Once the origin of this shame was acknowledged – as resulting from settler/assimilation logics, it was often possible for people to move forward in their language recovery journeys, while at the same time considering more broadly the structural barriers that make individual learning so difficult.

One of Us or One of Them: A Generic Qualitative Study on the Efficacy of the Funds of Knowledge Strategy to Reduce Teacher Ethnocentrism

The purpose of this study was to examine whether English a Second Language (ESL) instructors’ ethnocentrism could be reduced using multicultural education (MCE) principles. There were three focus group discussions and a Likert scale questionnaire. The findings demonstrated that while ESL instructors were conscious of systemic barriers, media stereotypes, and bullying, more diversity training is required in order to improve teachers’ attitudes, responses, and instructional strategies regarding integration issues due to the increasing diversity of learners present in classrooms today. The findings of the study also demonstrated that MCE principles could be used to effectively raise the awareness of ESL instructors when dealing with integration and assimilation issues. When immigration, human rights, and multicultural policies were examined critically, ESL instructors were able to improve their cross-cultural skills in the classroom to be more inclusive towards diverse ethnic groups by giving learners greater opportunities to express themselves. As a result, learners’ knowledge, experience, and skills were validated in the classroom leading to a more meaningful learning experience.

Seasonal reproductive endothermy in tegu lizards

With some notable exceptions, small ectothermic vertebrates are incapable of endogenously sustaining a body temperature substantially above ambient temperature. This view was challenged by our observations of nighttime body temperatures sustained well above ambient (up to 10°C) during the reproductive season in tegu lizards (~2 kg). This led us to hypothesize that tegus have an enhanced capacity to augment heat production and heat conservation. Increased metabolic rates and decreased thermal conductance are the same mechanisms involved in body temperature regulation in those vertebrates traditionally acknowledged as “true endotherms” : the birds and mammals. The appreciation that a modern ectotherm the size of the earliest mammals can sustain an elevated body temperature through metabolic rates approaching that of endotherms enlightens the debate over endothermy origins, providing support for the parental care model of endothermy, but not for the assimilation capacity model of endothermy. It also indicates that, contrary to prevailing notions, ectotherms can engage in facultative endothermy, providing a physiological analog in the evolutionary transition to true endothermy.

Le cyberpunk vernaculaire de l’Amérique latine : dystopies, virtualités et résistances

Héritière de la tradition fantastique borgésienne, imprégnée d’une réalité composée de mythes précolombiens et des résidus industriels de la modernité, et développée à l’ère de la mondialisation, du post-modernisme, des jeux vidéos, du cinéma numérique et d’animation, la tendance cyberpunk latino-américaine est cultivée du Mexique jusqu’en Argentine, en passant par Cuba et d’autres pays souvent méconnus dans le monde de la science-fiction comme le Paraguay et la Bolivie. Pressenti dans les œuvres de certains écrivains canoniques comme Ricardo Piglia, Carmen Boullosa ou Edmundo Paz-Soldán, le cyberpunk se manifeste avec force dans l’écriture de jeunes artistes interdisciplinaires et de collaborateurs assidus des fanzines. Cette adaptation du sous-genre dans un continent où la référence reste encore le réel merveilleux et le réalisme magique, malgré l’apport des générations plus récentes comme celle de « McOndo » ou celle du « Crack », essaie d’élaborer une série de réponses aux questions issues de la conjoncture historique et artistique dans laquelle nous vivons : comment situer l’identité latino-américaine dans la nouvelle cartographie culturelle mondiale à travers une littérature qui cherche à se renouveler par rapport au canon littéraire et à la marginalité de son propre genre? Quelles sont les stratégies d’assimilation et de résistance qu’adoptent des jeunes auteurs latino-américains devant le cyberpunk anglo-américain littéraire et cinématographique? Peut-on parler d’un impact esthétique et philosophique du cyberpunk sur la culture latino-américaine, perçue habituellement comme une consommatrice passive de ces produits culturels et non comme une productrice? Ce travail cherche à parcourir l’ensemble de ces questions à partir d’une réflexion sur les principaux dispositifs constitutifs du cyberpunk – la dystopie et la virtualité – dans les discours (post)identitaires en Amérique Latine. Représentation presque mimétique de l’espace socioculturel et historique latino-américain à travers la violence et la répression politique, militaire, ethnique ou sexuelle, la dystopie est un moyen d’articuler certaines figures spatiales aux mythes nationaux et à la politique identitaire dans le contexte de la mondialisation. Cette dernière réalité socioculturelle, ainsi que l’idéologie esthétique que véhicule celle-ci à travers le cyberpunk, crée un conflit avec ces discours identitaires nationaux, conflit qui est accentué ou dissous par la représentation de la réalité virtuelle. La réalité virtuelle, comprise ici comme la direction que le récit prend pour défaire ou consolider la figure dystopique, mène à réfléchir également sur les enjeux de la (post)identité. Penser à une (post)identité (en gardant bien à l’esprit cette parenthèse) à travers le cyberpunk signifie poser une question sur la résistance au passé identitaire des mythes nationaux, au présent de la mondialisation culturelle, et aux discours post-humanistes qui semblent marquer le futur. À l’appui de travaux sur la dystopie et la réalité virtuelle dans le cyberpunk anglo-américain, ainsi que des études culturelles latino-américaines, je parcourrai un corpus composé des romans écrits entre 1990 et 2005. Ce corpus comprendra La Primera Calle de la Soledad (1993) de Gerardo Horacio Porcayo, Santa Clara Poltergeist (1991) de Fausto Fawcett, Ygdrasil (2005) de Jorge Baradit, et les films argentins No muera sin decirme adónde vas (1992) d’Eliseo Subiela et La sonámbula (1998) de Fernando Spiner. Dans ces oeuvres, la dystopie se configure aux possibilités narratives de la virtualité et traverse des thématiques identitaires comme les mythes sexuels et nationaux, la mémoire et le traumatisme ainsi que les projets utopiques des minorités.

Pensée de l'acte et conseil de l’action : La perspective proudhonienne du travail industrie

Comment conseiller l’action ? En la pensant bien et totalement pour qu’elle soit bonne et juste, dit-on, puisque conforme à la raison. La pensée de l’acte s’impose d’elle-même au sujet de l’action comme allant de soi, assurée de réussir, effective et efficace. Qui peut ainsi assigner au sujet rationnel la nécessité de son acte ? Le maître-penseur qu’est le théoricien de l’action. Cette figure de conseiller-philosophe de l’action est-elle constitutive de toute pensée de l’action ? Peut-on échapper à cette assimilation du sujet de l’action et de la pensée de l’acte qui transforme le conseil en ordre ? L’auteur examine les éléments philosophiques de cette illusion du conseil. L’analyse proudhonienne du travail industriel ne fournit-elle pas un moyen de surmonter cet obstacle épistémologique ?