Hope of education : Somali families and social connection

This thesis examines Somali parents' experience of their children's education after settling in Melbourne following the outbreak of civil war in Somalia in 1991. The research found that Somali parents instigate connections with teachers to generate social capital to enhance their children's education.

Researching the relationship between physical activity and motherhood in older Somali women

This thesis explores participation in physical activity by a group of older Somali women living in Melbourne, Australia. First, it describes the methodological challenges faced by a white researcher conducting cross-cultural research; second, it explores how participants' experiences of motherhood and physical activity in Somalia and Australia influence their participation in physical activity. This research contributes data to address the scarcity of knowledge and research on physical activity amongst older African and Muslim women.

Do fracasso à reforma das operações de paz das Nações Unidas (2000-2010)

Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)

LIZARDS AND SNAKES (LEPIDOSAURIA, SQUAMATA) FROM THE LATE QUATERNARY OF THE STATE OF CEARA IN NORTHEASTERN BRAZIL

We present the first formal report on the squamate assemblage from Parque Nacional de Ubajara. This park contains the most important cave complex in the state of Ceara in northeastern Brazil, called Provincia Espeleologica de Ubajara. The material comes from the Urso Fossil cave at Pendurado Hill. All previously reported fossil remains found in this cave are tentatively attributed to the Quaternary (late Pleistocene-early Holocene). Probably only Arctotherium brasiliense represents a relictual fossil bear from the late Pleistocene megafauna. The taxa recognized in this paper belong to Tropidurus sp., Ameiva sp., cf. Epicrates, and cf. Crotalus durissus, adding to the knowledge of the Brazilian Quaternary squamate fauna as a whole, and contribute to a major taxonomic refinement of the squamate assemblages from the early Holocene of northeastern Brazil.

"Även om jag bor här i 100 år så blir det inte samma" : En kvalitativ studie av fem ensamkommande ungdomar och deras personliga identitetsutveckling i mottagarlandet.

SAMMANFATTNING: Människor tvingas fly ifrån sina hemländer på grund av våld för att söka säkerhet någon annanstans. Att människor lämnar ett land eller tvingas fly har skett under alla tider. Människor flyr från förföljelse, fattigdom, svält eller krig. Uppskattningsvis finns 19,2 miljoner människor på flykt runt om i världen och nära hälften av dessa är barn. Av de barn som befinner sig på flykt är de ensamkommande ungdomarna en viktig grupp att urskilja. Då de ensamkommande asylsökande ungdomarna är i behov av särskilt skydd. Under 2003 var de flesta ensamkommande ungdomar i Sverige från Somalia, Irak, Serbien och Montenegro. Vårt syfte är att få ökad förståelse för ensamkommande ungdomars upplevelser av hur deras identitet formats i hemlandet och senare i mottagarlandet i samspel med människor i sin omgivning. Samt vilken betydelse asylprocessen och tidigare trauman har haft för ungdomarnas personliga identitetsutveckling. De faktorer som berörts som viktiga för ungdomens personliga identitetsutveckling är förluster, boende, ovisshet, familjeåterförening och nätverk samt språket.Vi har valt att göra en explorativ studie som innefattar kvalitativa halvstrukturerade intervjuer med fem ensamkommande ungdomar. Resultatet i form av empiri och analys har utförts utifrån tidigare forskning och från Cullbergs kristeori samt relevanta begrepp som etnicitet och identitet utifrån symbolisk interaktionism. Studien har visat att samtliga ungdomar upplevt att den ovisshet de levt i under asylprocessen samt tidigare trauman har påverkat dem mycket både psykiskt och fysiskt. De ungdomar vi har intervjuat upplever alla att de idag har en ny personlighet efter att ha fått uppehållstillstånd. Den nya identiteten har enligt ungdomarna påverkats bland annat av föräldrarnas uppfostran och de nya människor de möter i mottagarlandet samt av de nya miljöerna ungdomarna befinner sig i.

Flujos meridionales en el Océano Índico Ecuatorial

[ES]Un modelo estacionario propuesto por Joyce (1988a) es evaluado en el Océano Índico ecuatorial, usando el estrés de vientos NCEP y temperaturas y salinidades de WOA05 y Argo. El transporte zonal integrado de los datos WOA05 se parece al de los datos Argo en el monzón de invierno (WM) y en los periodos de transición (TP), presentando valores mayores en el caso de datos Argo. En cambio, para el monzón de verano (SM) los transportes zonales integrados de los datos WOA05 y Argo tienen direcciones opuestas debido a que en los datos de WOA05 la Corriente de Somalia (SC) es débil y casi inexistente. Aunque los datos Argo tienen mayor cantidad de estructuras mesoscalares que los datos WOA05, los datos Argo obtienen una SC que se ajusta mejor a los estudios previos y, en consecuencia, los datos Argos son los únicos que serán utilizados para estimar transporte de volumen y calor. Los datos Argo muestran una SC que fluye hacia el sur durante el WM y hacia el norte durante el SM, y un flujo en el océano interior contrario a la corriente. Durante el WM, la SC es somera (~200dbar) y bajo ella fluye una contracorriente. El transporte de calor meridional estimado para datos Argo muestra una inversión estacional. El transporte de calor neto en cada estación tiene la misma dirección que el calor transportado por la SC.

Internal displacement and the Kampala Convention: an opportunity for development actors

According to the African Union (AU), Africa is "a continent disproportionately affected by internal displacement". The African region, with almost 10 million people internally displaced in 22 countries by armed conflict and other forms of violence, hosts more than one third of the 26.4 million internally displaced persons (IDPs) worldwide at the end of 2011. Sudan, the Democratic Republic of the Congo and Somalia rank globally among the states with the five biggest displacement situations. Even in African countries with smaller figures, very large percentages of people may be in displacement in regions primarily affected by violence. Such violence has multiple causes, including the long-lasting consequences of colonial heritage, outside intervention, crises of identity in multi-ethnic countries and conflicts over resources. Today, political exclusion and inequality between ethnic, regional or religious groups are particularly important drivers of violence.

Representing Afghanistan: The United States and Democracy's Imposition

There is an ongoing mission in Afghanistan; a mission driven by external political forces. At its core this mission hopes to establish peace, to protect the populace, and to install democracy. Each of these goals has remained just that, a goal, for the past eight years as the American and international mission in Afghanistan has enjoyed varied levels of commitment. Currently, the stagnant progress in Afghanistan has led the international community to become increasingly concerned about the viability of a future Afghan state. Most of these questions take root in the question over whether or not an Afghan state can function without the auspices of international terrorism. Inevitably, the normative question of what exactly that government should be arises from this base concern. In formulating a response to this question, the consensus of western society has been to install representative democracy. This answer has been a recurring theme in the post Cold War era as states such as Bosnia and Somalia bear witness to the ill effects of external democratic imposition. I hypothesize that the current mold of externally driven state-building is unlikely to result in what western actors seek it to establish: representative democracy. By primarily examining the current situation in Afghanistan, I claim that external installation of representative democracy is modally flawed in that its process mandates choice. Representative democracy by definition constitutes a government reflective of its people, or electorate. Thus, freedom of choice is necessary for a functional representative democracy. From this, one can deduce that because an essential function of democracy is choice, its implementation lies with the presence of choice. State-building is an imposition that eliminates that necessary ingredient. The two stand as polar opposites that cannot effectively collaborate. Security, governing capacity, and development have all been targeted as measurements of success in Afghanistan. The three factors are generally seen as mutually constitutive; so improved security is seen as improving governing capacity. Thus, the recent resurgence of the Taliban in Afghanistan and a deteriorating security environment moving forward has demonstrated the inability of the Afghan government to govern. The primary reason for the Afghan government’s deficiencies is its lack of legitimacy among its constituency. Even the use of the term ‘constituency’ must be qualified because the Afghan government has often oscillated between serving the people within its territorial borders and the international community. The existence of the Afghan state is so dependent on foreign aid and intervention that it has lost policy-making and enforcing power. This is evident by the inability of Afghanistan to engage in basic sovereign state activities as maintaining a national budget, conducting elections, providing for its own national security, and deterring criminality. The Afghan state is nothing more than a shell of a government, and indicative of the failings that external state-building has with establishing democracy.

Benthic foraminiferal fauna and isotope record in Holocene sediments of the northwest Indian Ocean

Historically, the Holocene has been considered an interval of relatively stable climate. However, recent studies from the northern Arabian Sea (Netherlands Indian Ocean Program 905) suggested high-amplitude climate shifts in the early and middle Holocene based on faunal and benthic isotopic proxy records. We examined benthic foraminiferal faunal and stable isotopic data from Ocean Drilling Program (ODP) Site 723 and total organic carbon data from ODP Site 724, Oman Margin (808 and 593 m water depths, respectively). At Site 723 the mid-Holocene shift in d18O values of infaunal benthic species Uvigerina peregrina (1.4 per mil) is 3 times larger than that of epifaunal benthic species Cibicides kullenbergi recorded at Site NIOP 905 off Somalia. However, none of the five other benthic species we measured at Hole 723A exhibits such a shift in d18O. We speculate that the late Holocene d18O decrease in U. peregrina represents species-specific changes in ecological habitat or food preference in response to changes in surface and deep ocean circulation. While the stable isotopic data do not appear to indicate a middle Holocene climatic shift, our total organic carbon and benthic faunal assemblage data do indicate that the early Holocene deep Arabian Sea was influenced by increased ventilation perhaps by North Atlantic Deep Water and/or Circumpolar Deep Water incursions into the Indian Ocean, leading to remineralization of organic matter and a relatively weak early Holocene oxygen minimum zone in the northwest Arabian Sea in spite of strong summer monsoon circulation.

Planktonic foraminifera of ODP Site 117-722

Quantitative analysis of the late Cenozoic planktonic foraminiferal record from western Arabian Sea Site 722 revealed long term trends in the history of oceanography and climate. The modern western Arabian Sea surface waters are highly influenced by the monsoonal wind system. Summer upwelling, a result of southwestern winds, occurs along the coast of Somalia which produces distinct foraminiferal assemblages which are dominated by G. bulloides d'Orbigny. Consequently, variations in the distribution record of G. bulloides through time monitor the upwelling history associated with monsoonal activities. G. bulloides was a minor constituent of the foraminiferal fauna from the bottom of the hole (~14.5 Ma) until about 8.6 Ma ago. Then a rapid shift occurred toward higher values, up to 53% at 7.4 Ma. We interpret this rapid increase as a major step in the evolution of the monsoonal history. It is either the establishment of the system or at least a strong intensification of the monsoonal winds. At 5.5 Ma a significant drop of the G. bulloides relative abundance occurred which may indicate less upwelling, or alternatively other biota may have been favored in this period. From 5.0 Ma to Recent the G. bulloides record indicates that upwelling has occurred with minor fluctuations.

Benthic respiration and physical oceanography on two contrasting continental margins in the western Indian Ocean: the Yemen-Somali upwelling region and the margin off Kenya

During the Netherlands Indian Ocean Project (NIOP, 1992-1993) sediment community oxygen consumption (SCOC) was measured on two continental margins in the Indian Ocean with different productivity: the productive upwelling region off Yemen-Somalia and the supposedly less productive Kenyan margin, which lacks upwelling. The two margins also differ in terms of river input (Kenya) and the more severe oxygen minimum in the Arabian Sea. Simultaneously with SCOC, distributions of benthic biomass and phytodetritus were studied. Our expectation was that benthic processes in the upwelling margin of the Arabian Sea would be relatively enhanced as a result of the higher productivity. On the Kenyan margin, SCOC (range 1-36 mmol/m**2/d) showed a clear decrease with increasing water depth, and little temporal variation was detected between June and December. Highest SCOC values of this study were recorded at 50 m depth off Kenya, with a maximum of 36 mmol/m**2/d in the northernmost part. On the margin off Yemen-Somalia, SCOC was on average lower and showed little downslope variation, 1.8-5.7 mmol/m**2/d, notably during upwelling, when the zone between 70 and 1700 m was covered with low O2 water (10-50 µM). After cessation of upwelling, SCOC at 60 m depth off Yemen increased from 5.7 to 17.6 mmol/m**2/d concurrently with an increase of the near-bottom O2 concentration (from 11 to 153 µM), suggesting a close coupling between SCOC and O2 concentration. This was demonstrated in shipboard cores in which the O2 concentration in the overlying water was raised after the cores were first incubated under in situ conditions (17 µM O2). This induced an immediate and pronounced increase of SCOC. Conversely, at deeper stations permanently within the oxygen minimum zone (OMZ), SCOC showed little variation between monsoon periods. Hence, organic carbon degradation in sediments on a large part of the Yemen slope appears hampered by the oxygen deficiency of the overlying water. Macrofauna biomass and the pooled biomass of smaller organisms, estimated by the nucleic acid content of the sediment, had comparable ranges in the two areas in spite of more severe suboxic conditions in the Arabian Sea. At the Kenyan shelf, benthic fauna (macro- and meiofauna) largely followed the spatial pattern of SCOC, i.e. high values on the northern shelf-upper slope and a downslope decrease. On the Yemen-Somali margin the macrofauna distribution was more erratic. Nucleic acids displayed no clear downslope trend on either margin owing to depressed values in the OMZ, perhaps because of adverse effects of low O2 on small organisms (meiofauna and microbes). Phytodetritus distributions were different on the two margins. Whereas pigment levels decreased downslope along the Kenya margin, the upper slope off Yemen (800 m) had a distinct accumulation of mainly refractory carotenoid pigments, suggesting preservation under low 02. Because the accumulations of Corg and pigments on the Yemen slope overlap only partly, we infer a selective deposition and preservation of labile particles on the upper slope, whereas refractory material undergoes further transport downslope.