No rastro de dores : trajetórias de vida e registros de superação em narrativas de mulheres negras com experiência de relações afetivo-sexuais com outras mulheres

Tese (doutorado)—Universidade de Brasília, Instituto de Ciências Sociais, Departamento de Antropologia, Programa de Pós-graduação em Antropologia Social, 2015.

“Culture Stops Development!”: Bijagó Youth and the Appropriation of Developmentalist Discourse in Guinea-B

African Studies Review, Volume 52, Number 2, pp. 69–

Continental margin architecture : the palynological signature of glacioeustasy /

Palynomorphs from two siliciclastic margins were examined to gain insights into continental margin architecture. Sea level change is thought to be one of the primary controls on continental margin architecture. Because Late Neogene glacioeustasy has been well studied marine sediments deposited during the Late Neogene were examined to test this concept. Cores from the outer shelf and upper slope were taken from the New Jersey margin in the western North Atlantic Ocean and from the Sunda Shelf margin in the South China Sea. Continental margin architecture is often described in a sequence stratigraphic context. One of the main goals of both coring projects was to test the theoretical sequence stratigraphic models developed by a research group at Exxon (e.g. Wilgus et al., 1988). Palynomorphs provide one of the few methods of inferring continental margin architecture in monotonous, siliciclastic marine sediments where calcareous sediments are rare (e.g. New Jersey margin). In this study theoretical models of the palynological signature expected in sediment packages deposited during the various increments of a glacioeustatic cycle were designed. These models were based on the modem palynomorph trends and taphonomic factors thought to control palynomorph distribution. Both terrestrial (pollen and spores) and marine (dinocysts) palynomorphs were examined. The palynological model was then compared with New Jersey margin and Sunda Shelf margin sediments. The predicted palynological trends provided a means of identifying a complete cycle of glacioeustatic change (Oxygen Isotope Stage 5e to present) in the uppermost 80 meters of sediment on the slope at the New Jersey margin. Sediment availability, not sea meters of sediment on the slope at the New Jersey margin. Sediment availability, not sea level change, is thought to be the major factor controlling margin architecture during the late Pleistocene here at the upper slope. This is likely a function of the glacial scouring of the continents which significantly increases sediment availability during glacial stages. The subaerially exposed continental shelf during the lowstand periods would have been subject to significant amounts of erosion fi:om the proglacial rivers flowing fi-om the southern regions of the ice-sheet. The slope site is non-depositional today and was also non-depositional during the last full interglacial period. The palynomorph data obtained fi-om the South China Sea indicate that the major difference between the New Jersey Margin sites and the Sunda Shelf margin sites is the variation in sediment supply and the rate of sediment accumulation. There was significantly less variation in sediment supply between glacial and interglacial periods and less overall sediment accumulation at the Sunda Shelf margin. The data presented here indicate that under certain conditions the theoretical palynological models allow the identification of individual sequence stratigraphic units and therefore, allow inferences regarding continental margin architecture. The major condition required in this approach is that a complete and reliable database of the contemporaneous palynomorphs be available.

Palynology of late-glacial and postglacial sediments in Georgian Bay, Ontario, Canada, as related to the Great Lakes history /

This investigation comprises three parts: (1) the source, mechanism of transport, and distribution of pollen, spores and other palynomorphs in Georgian Bay bottom sediments and a comparison of these data with the contemporary vegetation, (2) the relative significance of fluvial transportation of pollen and spores, and (3) the late- and postglacial history of vegetational and climatic changes in the Georgicin Bay region. Modem pollen and spore assemblages in Georgian Bay do reflect the surrovinding vegetation when preservation and pollen production by the different species are considered and accounted for. Relative pollen percentage and concentration isopoll patterns indicate that rivers contribute large quantities of pollen and spores to Georgian Bay. This is further substantiated by large amounts of pollen and spores which were caught in traps in the Moon, Muskoka, and Nottawasaga Rivers which flow into Georgian Bay. The majority of pollen and spores caught in these traps were washed into the rivers by surface water runoff and so reflect the vegetation of the watershed in a regional sense. In a 12.9 metre long sediment core from northeastern Georgian Bay the relative percentage and absolute pollen concentrations allow correlation of Georgian Bay Lake phases with climatic and forest history. Four distinct pollen zones are distinguished: zone GB IV which is the oldest, reflects the succession from open spruce woodland to boreal forest; zone GB III represents a period of pine-mixed hardwoods forests from about 10,000 to 7,500 years ago. A pine-maplehemlock association dominated in zone GB II, although during the culmination of postglacial warming about 4,000 to 5,000 years ago the Georgian Bay forests had a more deciduous character. Zone GB I clearly shows European man's disturbance of the forest by logging activities.

Onondaga chert : geological and palynological studies as applied to archaeology /

Cherts from the Middle Devonian Onondaga Formation of the Niagara Peninsula in Southern Ontario and Western New York State can now be distinguished from those of the Early Devonian Bois Blanc Formation of the same area based on differences in petrology, acritarchs, spores, and "Preservation Ratio" values. The finely crystalline, carbonate sediments of the Bois Blanc Formation were deposited under shallow, low energy conditions characterised by the acritarchs Leiofusa bacillum and L. minuta and a high relative abundance of the spore, Apiculiretusispora minor. The medio crystalline and bioclastic carbonate sediments of the Onondaga Formation were deposited under shallow, high energy conditions except for the finely crystalline lagoonal sediments of the Clarence Member which is characterised by the acritarchs Leiofusa navicula, L. sp. B, and L. tomaculata . The author has subdivided and correlated the Clarence Member of the Onondaga Formation using the "Preservation Ratio" values derived from the palynomorphs contained in the cherts. Clarence Member cherts were used by the Archaic people of the Niagara Peninsula for chipped-stone tools. The source area for the chert is considered to be the cobble beach deposits along the north shore of Lake Erie from Port Maitland to Nanticoke

Pollen and grain size records in abyssal sediments of the northwest Pacific Ocean as proxies of Plio-Pleistocene climate change /

A distinctive period of global change occurred during the PUocene between the warm Miocene and subsequent Quaternary cooling. Samples from Ocean Drilling Project Site 11 79 (-5586 mbsl, 41°4'N, 159°57'E), Site 881 (-5765 mbsl, 47°6.133'N, 161°29.490'E) and Site 882 (-3255 mbsl, 50°22'N, 167°36'E) were studied to determine the magnitude and composition ofterrigenous flux to the western mid-latitude North Pacific and its relation to climate change in East Asia since the mid-Pliocene. Dust-sized particles (including pollen), sourced from the arid regions and loess plateaus in East Asia are entrained by prevailing westerly winds and transported to the midlatitude northwest North Pacific Ocean. This is recorded by peaks in the total concentration of pollen and spores, as well as the mean grain size of allochthonous and autochthonous silicate material in abyssal marine sediments. Aridification of the Asian interior due to the phased uplift of the Himalayan-Tibetan Plateau created the modem East Asian Monsoon system dominated by a strengthening of the winter monsoon. The winter monsoon is further enhanced during glacials due to the expansion of desert and steppe environments at the expense ofwoodlands and forests recorded by the composition of palynological assemblages. The late Pliocene-Pleistocene glacials at ODP Sites 1 179, 881, and 882 are characterized by increases in grain size, magnetic susceptibility, pollen and spore concentrations around 3.5-3.3, 2.6-2.4, 1.7-1.6, and 0.9-0.7 Ma (ages based on magnetostratigraphic and biostratigraphic datums). The peaks during these times are relatively rich in pollen taxa derived primarily from steppe and boreal vegetation zones, recording cool, dry climates. The overall size increase of sediment and abundance of terrestrial palynomorphs record enhanced wind strength. The increase in magnitude of pollen and spore concentrations as well as grain size record global cooling and Northern Hemisphere glaciation. The peaks in grain size as well as pollen and spore abundance in marine sediments correlate with the mean grain size of loess in East Asia, consistent with the deflation of unarmoured surfaces during glacials. The transport of limiting nutrients to marine environments enhanced sea surface productivity and increased the rate of sediment accumulation.

Dinocyst biochronology and palynofacies : inferred systems tract character of Miocene sequences from New Jersey mid-Atlantic transect (ODP legs 174A and 174AX) /

One of the main objectives of the mid-Atlantic transect is to improve dating resolution of sequences and unconfonnity surfaces. Dinoflagellate cysts from two Ocean Drilling Program boreholes, the onshore Leg 174AX Ocean View Site and Leg 174A continental shelf Site 1071, are used to provide age estimates for sequences and unconfonnities fonned on the New Jersey continental margin during the Miocene epoch. Despite the occasional lack of dinocysts in barren and oxidized sections, dinocyst biochronology still offers greater age control than that provided by other microfossils in marginal marine environments. An early Miocene to late Miocene chronology based on ages detennined for the two study sites is presented. In addition, .palynofacies are used to unravel the systems tract character of the Miocene sequences and provide insight into the effects of taphonomy and preservation of palynomorphs in marginal marine and shelf environments under different ~ea level conditions. More precise placement of maximum flooding surfaces is possible through the identification of condensed sections and palynofacies shifts can also reveal subaerially exposed sections and surfaces not apparent in seismic or lithological analyses. The problems with the application of the pollen record in the interpretation of Miocene climate are also discussed. Palynomorphs provide evidence for a second-order lowering of sea level during the Miocene, onto which higher order sea level fluctuations are super-imposed. Correlation of sequences and unconfonnities is attempted between onshore boreholes and from the onshore Ocean View borehole to offshore Site 1071.

Ontological constructivism : Negri and the philosophical foundations of a future communism

As we find in Empire and Multitude, Antonio Negri's political project IS a thoroughly Marxist analysis and critique of global or late capitalism. By modifying and updating Marx's conceptual tools, he is able to provide a clear account of capitalism's processes, its expanding reach, and the revolutionary potential that functions as its motor. By turning to Negri's philosophical works, however, we find that this political analysis is founded on a series of concepts and theoretical positions. This paper attempts to clarify this theoretical foundation, highlighting in particular what I term "ontological constructivism" - Negri's radical reworking of traditional ontology. Opposing the long history of transcendence in epistemology and metaphysics (one that stretches from Plato to Kant), this reworked ontological perspective positions individuals - not god or some other transcendent source - as the primary agents responsible for molding the ontological landscape. Combined with his understanding of kairos (subjective, immeasurable time), ontological constructivism lays the groundwork for opposing transcendence and rethinking contemporary politics.

All of My Blood is Red: Contemporary Metis Visual Culture and Identity

This thesis explores notions of contemporary Metis identity through the lens of visual culture, as articulated in the works of three visual artists of Metis ancestry. I discuss the complexities of being Metis with reference to specific art works by Christi Belcourt, David Garneau and Rosalie Favell. In addition to a visual culture analysis of these three Metis artists, I supplement my discussion of Metis identity with a selection of autoethnographic explorations of my identity as a Metis woman through out this thesis. The self-reflexive aspect of this work documents the ways in which my understanding of myself as a Metis woman have been deepened and reworked in the process of conducting this research, while also offering an expanded conception of contemporary Metis culture. I present this work as an important point of departure for giving a greater presence to contemporary Metis visual culture across Canada:

DINOFLAGELLATE CYSTS FROM THE LATEST MIOCENE THROUGH MIDDLE PLEISTOCENE OF THE CARIBBEAN SEA, ODP SITE 1000: BIOSTRATIGRAPHY, PALEOCEANOGRAPHY, AND SHOALING OF THE CENTRAL AMERICAN SEAWAY

This is the first detailed study of organic-walled dinoflagellate cysts (dinocysts) and acritarchs for the latest Miocene–Middle Pleistocene of Ocean Drilling Program Site 1000 in the Caribbean Sea. Well-preserved and moderately diverse dinocysts and other palynomorphs reflect the interplay between neritic (carbonate-platform sourced) and oceanic species. The dinocyst biostratigraphy is tied to an existing marine isotope stratigraphy for the interval 5.5–2.2 Ma. For the interval 5.5–3.8 Ma, palynological samples are coupled to published sea-surface temperature estimates based on planktonic foraminiferal Mg/Ca. Changes in dinocyst assemblage composition are noted at ca. 4.6 Ma when shoaling of the Central American Seaway caused a temperature rise in the Caribbean, ca. 3.8–3.6 Ma, during the cold Marine Isotope Stage M2 when pronounced warming occurred, at ca. 2.7 Ma where possible weak cooling may reflect the onset of Northern Hemisphere glaciation, and in the Middle Pleistocene presumably reflecting global cooling and sea-level fall.

Histoire, fiction et mémoire dans l’œuvre de Boubacar Boris Diop

Cette thèse tente de réfléchir sur l’écriture de Boubacar Boris Diop. Les romans de cet écrivain doivent une grande part de leur originalité à la présence obsédante des discours de la mémoire et de l’histoire. Son esthétique s’inscrit dans une revisitation permanente des récits de l'historiographie. Cette écriture convoque le passé et l'investit comme matériau dans cette exploration des formes du roman. Une telle démarche scripturale semble être la pierre angulaire de cette fiction aux confluences desquelles se rencontrent et s'intègrent systématiquement, aussi bien les genres romanesques hétérogènes de l'oralité (contes, épopées, mythes...), que des disciplines non romanesques. Cette stratégie de construction romanesque traduit, au-delà d'une simple exploration formelle et innovatrice des possibles du roman, une esthétique de distanciation et d'hétérogénéité qui traverse en filigrane l'œuvre de Boubacar Boris Diop. Cette forme d’écriture singularise son esthétique et constitue une rupture épistémologique dans le champ littéraire africain, qui a été souvent caractérisé par des récits linéaires classiques. L’usage de ces discours de l’histoire et de la mémoire, dans l’esthétique romanesque de Boubacar Boris Diop, s’articule d’abord dans une démarche de renouvellement des habitudes dans le champ littéraire africain, et ouvre aussi cette «phase autoréférentielle» (Sob, 2007 : 8) du roman en inscrivant son discours dans la modernité. Ensuite, cette pratique scripturale se construit sur l’élaboration d’un style romanesque particulier, se déployant dans une mise en scène et une parodisation permanentes du fonctionnement et des modalités de l’écriture. Sur fond d’une déconstruction perpétuelle des procédés de composition romanesque, se dessinent les contours d’une esthétique qui promeut et institue l’ambivalence généralisée comme le mode principal de son déploiement. Une telle pratique intertextuelle permet à l’écriture romanesque de se construire en confrontant les discours officiels de l’historiographie en général et l’histoire africaine contemporaine en particulier. En légitimant la déconstruction systématique comme dispositif de la composition romanesque, l’écriture se place dans une dynamique de «soupçon» qui sous-tend l’esthétique romanesque de Boubacar Boris Diop. La présente étude a le dessein de répertorier et d'analyser d'abord l'intégration des discours de l'histoire et de la mémoire, dans leurs manifestations et configurations dans l'œuvre de Diop, et ensuite, d'étudier leurs modalités d'insertion et d'utilisation dans l’élaboration de la fiction. Il s'agira, dans un cadre intertextuel, de voir comment ces discours sont investis et retravaillés par la fiction et, au-delà, d’essayer de repérer les motifs et les modalités discursives qui gouvernent leur usage. Une telle approche nous permettra d’appréhender les dimensions significatives de cette démarche scripturale et de voir éventuellement, s’il existe une poétique de la mémoire chez Boubacar Boris Diop. Les différentes théories sur la fiction, la mémoire et le discours historiographique nous serviront de charpente théorique qui sous-tendra notre thèse.

Développement et validation de l'échelle de mesure du climat de santé mentale

Ce mémoire a comme objectif de vérifier la validité de construit et la cohérence interne d’une nouvelle échelle de mesure du climat de santé mentale. Il vise également à observer la validité concomitante en fonction des associations entre les dimensions du climat de santé mentale et les dimensions de l’épuisement professionnel et le bien-être. Le concept du climat de santé mentale ainsi que son échelle de mesure ont été développés par l’Équipe de Recherche sur le Travail et la Santé Mentale. Le climat de santé mentale est considéré comme une ressource importante pour les travailleurs pour qu’ils puissent faire face aux difficultés qui se présentent dans leurs milieux de travail. Le climat de santé mentale se définit comme étant les perceptions partagées des politiques, procédures et pratiques organisationnelles qui témoignent d’une préoccupation pour le stress et la santé mentale au travail. Afin de valider cette nouvelle échelle de mesure, nous avons utilisé les données primaires de 410 civils et policiers du Service de Police de la Ville de Montréal (SPVM). L’analyse des résultats indique que l’échelle initiale à dix items mérite d’être retravaillée. Nous avons donc fait quelques modifications à cette échelle pour proposer une échelle de mesure du climat de santé mentale à huit items ou une échelle courte à trois items. Les résultats font ressortir l’importance du rôle des gestionnaires à assurer un climat de santé mentale positif au sein de leur organisation.

Les casual games : définition à l’aide du savoir professionnel des designers de jeux

Le jeu casual est un phénomène majeur de l’industrie vidéoludique, pourtant il reste peu étudié et mal considéré. Les quelques définitions scientifiques recensées présentent des divergences importantes, ainsi qu’un décalage par rapport aux jeux produits. Les modèles théoriques en design de jeu, centrés sur le gameplay, semblent inadéquats face à ce phénomène. En utilisant le modèle du praticien réflexif de Donald Schön, l’objectif de notre recherche est d’apporter un nouvel éclairage sur le jeu casual grâce au savoir professionnel des designers de jeux. Notre approche est qualitative, d’inspiration phénoménologique : nous avons recueilli l’expérience de huit designers de jeux par l’intermédiaire d’entretiens semi-dirigés proches du récit de pratique. Nos résultats montrent que les concepts utilisés dans les modèles vidéoludiques traditionnels restent pertinents pour définir le jeu casual, mais demandent à être retravaillés afin de rendre compte des mutations de l’expérience de jeu. Ainsi, un challenge dans un jeu casual n’est pas un obstacle mais une opportunité d’action pour le joueur. De plus, la progression se fait par la variation des challenges plutôt que par l’augmentation de la difficulté. Ensuite, certains concepts qui semblaient pertinents pour définir les jeux casual, tels que la fiction positive, ont été rejetés par nos participants. Enfin, notre étude a permis de rassembler des informations sur le rôle du designer de jeu casual et le contexte dans lequel il exerce, ce qui permet d’expliquer certaines causes de la vision péjorative du jeu casual.

Living and fishing in a marine protected area : balancing traditional fisheries with conservation in Karimunjawa National Park, Indonesia

Cette recherche a porté sur quelques enjeux importants liés à la gestion des aires marines protégées (AMP) en Indonésie en examinant comment celles-ci sont en mesure d'adapter leurs politiques afin de mieux répondre à l'évolution des conditions socioéconomiques et écologiques, quels ont été les impacts socioéconomiques de ces aires, et quelles sont les préoccupations environnementales des acteurs locaux dont les moyens de subsistance dépendent des ressources règlementées. Le «livelihoods framework » a servi de guide pour notre analyse des changements socioéconomiques dans la région, tandis que la notion d’« environmentality » d’Agrawal a fourni les bases théoriques pour l'examen de la formation de sujets environnementaux au parc national de Karimunjawa. Cette étude a montré que les changements de politique apportés au plan de la gestion du parc sont un pas dans la bonne direction, mais que les objectifs importants liés sa cogestion n'ont jamais été entièrement réalisés dans la pratique. Les résultats montrent également que d'importants changements socioéconomiques surviennent dans le parc, de nombreux pêcheurs se tournent vers des moyens de subsistance alternatifs, afin de compenser la baisse des prises de poissons. Enfin, cette étude a révélé que d'importants changements positifs dans les préoccupations environnementales sont survenus depuis la modification du zonage du parc, mais que ceux-ci ne se sont pas entièrement traduits en conformité avec les règles et règlements de l'AMP.

Foraminiferal and Pteropod Records in the Late Quaternary Sequence off Northern Kerala and Their Oceanographic and Climatic Significance

In the present investigation, an attempt is made to study late Quaternary foraminiferal and pteropod records of the shelf of northern Kerala and to evaluate their potentiality in paleocenographic and paleoclimatic reconstruction. The study gives details of sediment cores, general characteristics of foraminifera and pteropod species recorded from the examined samples and their systematic classification, spatial distribution of Recent foraminifera and pteropods and their response to varying bathymetry, nature of substrate, organic matter content in sediment and hydrography across the shelf. An attempt is also made to establish an integrated chronostratigraphy for the examined core sections. An effort is also made to identify microfaunal criteria useful in biostratigraphic division in shallow marine core sections. An attempt is made to infer various factors responsible for the change in microfaunal assemblage. Reconstruction of sea level changes during the last 36,000 years was attempted based on the pteropod record. The study reveals a bathymetric control on benthic/planktic (BF/PF) foraminiferal and pteropods/planktic foraminiferal (Pt/PF) abundance ratio. Bathymetric distribution pattern of BF/PF ratio is opposite to the (Pt/PF) ratio with decreasing trend of former from the shore across the shelf. Quantitative benthic foraminiferal record in the surficial sediments reveals a positive correlation between the diversity and bathymetry. R-mode cluster analysis performed on 30n significant Recent benthic foraminiferal, determines three major assemblage.