Lybia.

Mode of access: Internet.

Les vidéos de gay bashing : des agresseurs à YouTube

La recherche portera sur la montée des vidéos de gay bashing depuis 2013. Par vidéo de gay bashing, nous entendons des vidéos documentant l’abus physique ou verbal d’individus perçus par les agresseurs comme étant gais, lesbiennes, bisexuels, transgenres ou queer, mais nous nous concentrerons spécifiquement sur des vidéos montrant des agressions envers des hommes. Ces vidéos peuvent être enregistrées par les agresseurs eux-mêmes ou par des témoins de la scène. Il s’agira de situer cette montée dans un contexte politique de retour de lois et sentiments anti-LGBT dans les pays d’où proviennent certaines des vidéos étudiées et par rapport aux différentes théories anthropologiques et socio-historiques concernant les sources et motivations derrière les actes de violence homophobe. Le corpus se composera de trois vidéos venant de Russie («Putin’s Crackdown on LGBT Teens un Russia»), de Lybie («Gay torture and violent in Lybia») et des États-Unis («Attack at gay pride event in Detroit»). L’analyse du corpus se fera en trois temps : d’abord l’analyse de la forme et du contenu des vidéos en tant que tels, ensuite, l’analyse de leur circulation et des différents utilisateurs qui distribuent les vidéos en ligne, et, finalement, l’analyse de la réception des vidéos en portant attention aux commentaires des utilisateurs. Il s’agira de montrer comment les vidéos de gay-bashing effectuent une rupture par rapport à une vision de YouTube, et autres médias sociaux, comme libérateurs et comme lieux d’expression de soi (particulièrement pour les membres des communautés LGBT) et les transforment en lieux d’une humiliation triplée par l’enregistrement de l’humiliation physique et sa diffusion sur le web. Il s’agira ensuite de voir comment la circulation et la redistribution de ces vidéos par différents groupes et utilisateurs les instrumentalisent selon différents agendas politiques et idéologiques, pour finalement se questionner, en s’inspirant du triangle de l’humiliation de Donald Klein, sur le rôle ambivalent du témoin (physique ou virtuel) dont la présence est nécessaire pour qu’il y ait humiliation. Finalement, nous nous intéresserons aux vidéos de témoignages de gay-bashing, vidéos faites par les victimes elles-mêmes, racontant leur traumatisme à la caméra, renouant ainsi avec les vidéos de coming out sous la forme de l’aveu et de la spectacularisation du soi. La présente recherche sera également l’occasion de développer des outils théoriques et méthodologiques propres aux nouveaux médias et aux nouvelles formes et contenus qui s’y développent.

Discurso, retórica e poder na Antiguidade tardia: a construção do ethos político em Sinésio de Cirene

Pós-graduação em História - FCHS

Geochemistry on Holocene sediments from the Mediterranean

The enhanced accumulation of organic matter in Eastern Mediterranean sapropels and their unusually low d15N values have been attributed to either enhanced nutrient availability which led to elevated primary production and carbon sequestration or to enhanced organic matter preservation under anoxic conditions. In order to evaluate these two hypothesis we have determined Ba/Al ratios, amino acid composition, N and organic C concentrations and d15N in sinking particles, surface sediments, eight spatially distributed core records of the youngest sapropel S1 (10-6 ka) and older sapropels (S5, S6) from two locations. These data suggest that (i) temporal and spatial variations in d15N of sedimentary N are driven by different degrees of diagenesis at different sites rather than by changes in N-sources or primary productivity and (ii) present day TOC export production would suffice to create a sapropel like S1 under conditions of deep-water anoxia. This implies that both enhanced TOC accumulation and d15N depletion in sapropels were due to the absence of oxygen in deep waters. Thus preservation plays a major role for the accumulation of organic-rich sediments casting doubt on the need of enhanced primary production for sapropel formation.

Calcareous dinoflagellate cysts in surface sediments from the Mediterranean Sea

The distribution of calcareous dinoflagellate cysts in surface sediments from the Mediterranean Sea was quantitatively analysed. The samples contain 11 cyst species and the vegetative coccoid Thoracosphaera heimii. Cyst abundance increases towards the deeper parts of the basins and is generally higher in the eastern Mediterranean Sea. Three major distribution characteristics exist: (1) different assemblages in oceanic and neritic regions, (2) little agreement with the associations of areas studied so far like the Atlantic Ocean, and (3) a unique oceanic assemblage in the eastern Mediterranean Sea. A gradual change in cyst assemblages from the western to the eastern Mediterranean Sea was observed and statistically compared with the main environmental gradients in the upper water column. Temperature, nitrate concentration and possibly salinity appear to be the most important factors controlling cyst production. Three groups containing cysts with similar environmental preferences can be distinguished: (1) an eastern Mediterranean group related to relatively high temperature and salinity but low nitrate concentration, (2) a group of more or less consistently abundant cosmopolitan species tolerating or even preferring relatively low temperature and salinity but high nitrate concentration, and (3) a group containing species that are possibly adapted to neritic environments and have probably been transported from coastal areas into the studied regions. In contrast to other calcareous plankton, calcareous dinoflagellate cysts correlate strongly with the main environmental gradients in the Mediterranean Sea, bearing a high potential for palaeoenvironmental reconstructions.

Calcareous dinoflagellate cysts and geochemistry of Mediterranean Sea sediments

Comparison of calcareous dinoflagellate cyst assemblages with Ba, Al, Mn, and Fe records from three sediment cores collected in the eastern Mediterranean Sea indicate that calcareous dinoflagellate cysts are generally resistant to postdepositional dissolution. Cyst association changes during and after sapropel S1 formation can therefore be closely related to variability in surface water productivity. Two groups of cysts are defined: those having highest abundances within the sapropelic and postsapropelic sediments. The temporal cyst distributions suggest increased freshwater input mainly from the Nile and a shallowing of the pycnocline as the most important processes increasing nutrient concentration in the photic zone, thus leading to increased productivity and organic carbon fluxes during sapropel formation. Furthermore, a general warming trend at the beginning of S1 formation and a slight salinity decrease are reconstructed.

Individual dinoflagellate cysts species of surface sediment samples from the Mediterranean Sea

To determine the relationship between the spatial dinoflagellate cyst distribution and oceanic environmental conditions, 34 surface sediments from the Eastern and Western Mediterranean Sea have been investigated for their dinoflagellate cyst content. Multivariate ordination analyses identified sea-surface temperature, chlorophyll-a , nitrate concentration, salinity, and bottom oxygen concentration as the main factors affecting dinoflagellate cyst distribution in the region. Based on the relative abundance data, two associations can be distinguished that can be linked with major oceanographic settings. (1) An offshore eastern Mediterranean regime where surface sediments are characterized by oligotrophic, warm, saline surface water, and high oxygen bottom water concentrations (Impagidinium species, Nematosphaeropsis labyrinthus, Pyxidinopsis reticulata and Operculodinium israelianum). Based on the absolute abundance, temperature is positively related to the cyst accumulation of Operculodinium israelianum. Temperature does not form a causal factor influencing the accumulation rate of the other species in this association. Impagidinium species and Nematosphaeropsis labyrinthus show a positive relationship between cyst accumulation and nitrate availability in the upper waters. (2) Species of association 2 have highest relative abundances in the Western Mediterranean Sea, Strait of Sicily/NW Ionian Sea, and/or the distal ends of the Po/Nile/Rhône River plumes. At these stations, surface waters are characterized by (relative to the other regime) higher productivity associated with lower sea-surface temperature, salinity, and lower bottom water oxygen concentrations (Selenopemphix nephroides, Echinidinium spp., Selenopemphix quanta, Quinquecuspis concreta, Brigantedinium spp. and Lingulodinium machaerophorum). Based on both the absolute and relative abundances, Selenopemphix nephroides is suggested to be a suitable indicator to trace changes in the trophic state of the upper waters. The distribution of Lingulodinium machaerophorum is related to the presence of river-influenced surface waters, notably the Nile River. We suggest that this species might form a suitable marker to trace past variations in river discharge, notably from the Nile.