<p>The study investigates the role of CPUT libraries in supporting research and how academics perceive this role. CPUT is a new university of technology and aims at improving its research record. Research is crucial to South Africa to develop economically, socially and to compete globally. Research is fundamental to the existence of universities. Universities of technology libraries face the challenge of providing support for research. Previously the colleges / technikon libraries provided support for undergraduate and underdiplomates only. Today, they have to provide support for researchers at masters, doctoral, and post-doctoral levels.</p>

<p>In South Africa, poverty engendered by the apartheid regime has long been part of the fabric of the economy. Against this background of social marginalisation, material deprivation and individual vulnerability, tourism has over the years increasingly been mooted as a strategically important and lucrative sector that, if fully explored and exploited, would lead to sustained poverty alleviation in the Republic of South Africa. The central aim of this study was to establish whether tourism as evident in the Spier Tourism model is a sustainable poverty-reduction strategy. The specific objectives of this study were to examine the socio-economic impact of Spier tourism initiatives on its workers (previously disadvantaged individuals) and the local population, to assess the pro-poor tourism practices as implemented by Spier in relation to Rogerson&rsquo / s pro-poor approach, to identify the challenges that Spier is facing in its pro-poor tourism approach with respect to poverty reduction goals, to provide recommendations on how the challenges can be met most effectively and to examine how pro-poor tourism can be promoted and enhanced in South Africa. The study employed both the qualitative and quantitative research designs. Data were collected through different qualitative and quantitative techniques (in-depth interviews, focus group discussions, questionnaire). Summary findings indicate that Spier has positively contributed to the socio-economic improvement in the living standards (contribution to livelihood &ndash / increased income, enhanced health and food status), through job creation, improved education/healthcare, empowerment through training and skill development, investment in the corporate social responsibility. However, Spier is still grappling with challenges such as racial disputes, insufficient income of employees and unqualified staff to mention a few. This study makes several recommendations which are based on the findings.</p>

The main premise of this thesis is to demonstrate how the Gypsies, (Roma)---both Muslim and Christian, both settled and nomadic---were marginalized by the Ottoman State and society in Rumelia (Rumili) and Istanbul during the "Classical Age" of this tri-continental Islamic Empire. / The Ottoman state and the society's attitudes towards this marginal group are analyzed through the examination of the Muhimme Registers of the second half the sixteenth century and four major Kanunnames concerning the Gypsies issued in the fifteenth and sixteenth centuries. Travelers' accounts and Turkish oral traditions have also been used to explore the social status of the Gypsies in Ottoman society, as well as their image in Ottoman popular culture. / The history of people who were marginal and voiceless in their societies is not just important for its own sake but for what it reveals about the nature of the societies in which they lived. Thus, this present work not only sheds light upon the history of the Gypsies but also attempts to open new grounds for further discussions on the functioning of the "Plural Society" of the Ottoman Empire.

Marine productivity along the western Antarctic Peninsula (WAP) is declining. The WAP is site of the fastest regional warming in the southern hemisphere, and has experienced atmospheric and oceanic temperature increases leading to increased glacial inputs and reduced winter sea-ice cover. Sea-ice is a key link between climate and phytoplankton production, as melting sea-ice stratifies the water column and provides a source of micronutrients to surface waters. Reductions in ice cover have been accompanied by declining chlorophyll (chl; a proxy for phytoplankton biomass), and a shift to smaller cell sizes in phytoplankton communities. These reductions have implications for carbon drawdown and production available to higher trophic levels. However, little is known about phytoplankton shifts at the community level, as existing studies are based on satellite records and photosynthetic pigment analyses. To elucidate the nature of the changes within phytoplankton assemblages, high-resolution time-series data of diatom speciation are coupled to environmental data from five years in Ryder Bay (Adelaide Island, WAP). Long-term monitoring at this site by the British Antarctic Survey has identified a strong relationship between chl and water column stratification, and this study spans a wide range of physical conditions and biological production. By comparing high- and low-chl phytoplankton assemblages, this study investigates the mechanisms underlying productivity changes and the manner in which these changes impact nutrient cycling, drawdown and trophic transfer. The results presented here are the first full season in-situ records documenting differences in phytoplankton and diatom assemblages between highand low-chl years. The primary difference between chl conditions is a dramatic decline in diatom abundance. This analysis indicates that the mechanism producing low-chl seasons is less stratified surface waters, where light levels are much more variable than in high-chl years. Overall production is reduced, and small increases are seen in biomass of prymnesiophytes, which are better adapted to variable light. These shifts in phytoplankton composition and size structure are consistent with a southward propagation of observed climate change effects. Within the diatom community, changes in seasonal succession and a decrease in species richness occurred following low winter sea-ice. As the main component of high productivity and that most efficiently transferred to higher trophic levels, variation in diatom production due to environmental conditions is a mechanism to explain the observed WAP ecosystem changes and chl decline. Changes in phytoplankton stocks and composition also affect nutrient use, and here the use of silicon and iron (Si and Fe, respectively, which limit productivity in large areas of the Southern Ocean) is investigated. Seasonal Si budgets estimated from Si isotopes indicate a 40 – 70% decline in Si use between high-chl and intermediate-chl years, in agreement with other indices of productivity. The consequences of reduced demand and changing supply suggest future accumulation of Si in WAP surface waters. This should increase Si export away from the WAP shelf, which may act as a mechanism to enhance productivity and carbon drawdown in the wider Southern Ocean. Sources of Fe were assessed by direct measurement and naturally occurring radioisotopes of radium. These reveal significant inputs at the surface (due to glacial sources) and to deep waters (from shelf/slope sediments), which dominate supply to the surface mixed layer at different times. Iron availability and nutrient drawdown indicate that Fe is supplied to WAP surface waters in excess of biological demand. Projected changes to Fe sources and sinks indicate that continued warming will increase the WAP Fe inventory. As for Si, this excess Fe may also be advected away from the shelf, making this region a net Fe source to the Southern Ocean.

The Lyttelton Volcanic Complex, north-western Banks Peninsula, New Zealand, is comprised of five overlapping volcanic cones. Two magma systems are postulated to have fed Banks Peninsula’s basaltic intraplate volcanism, with simultaneous volcanism occurring in both the north-western and south-eastern regions of Banks Peninsula, to form Lyttelton and Akaroa Volcanic Complexes respectively. The elongate form of Banks Peninsula is postulated to relate to the upward constraining of magmatism in a north-west / south-east fault bounded zone. The Lyttelton Volcanic Complex resulted from the development of a pull-apart basin, with a number of releasing bend faults, controlling the location of eruptive sites. Cone structure further influenced the pathway magma propagated, with new eruptive sites developing on the un-buttressed flanks, resulting in the eruption and formation of a new cone, or as further cone growth recorded as an eruptive package. Each cone formed through constructional or eruptive phases, termed an eruptive package. Eruptive packages commonly terminate with a rubbly a’a to blocky lava flow, identified through stratigraphic relationships, lava flow trends and flow types, a related dyking regime, and radial erosional features (i.e. ridges and valleys). Within the overall evolving geochemical trend of the Lyttelton Volcanic Complex, are cyclic eruptive phases, intrinsically linked to eruptive packages. Within an eruptive package, crystal content fluctuates, but there is a common trend of increasing feldspar content, with peak levels corresponding to a blocky lava flow horizon, indicating the role of increased crystalinity and lava flow rheology. Cyclic eruptive phases relate to discreet magma batches within the higher levels of the edifice, with crystal content increasing as each magma batch evolves, limiting the ability of the volcanic system, over time, to erupt. Evolving magmas resulted in explosive eruptions following effusive eruptives, and / or result in the intrusion of hypabyssal features such as dykes and domes, of more evolved compositions (i.e. trachyte). Each eruptive package hosts a radial dyke swarm, reflecting the stress state of a shallow level magma chamber or a newly developed stress field due to gravitational relaxation in the newly constructed edifice, at the time of emplacement. Two distinct erosional structures are modelled; radial valleys and cone-controlled valleys. Radial valleys reflect radial erosion about a cone’s summit, while cone-controlled valleys are regions where eruptive packages and cones from different centres meet, allowing stream development. Interbedded epiclastic deposits within the Lyttelton lava flow sequences indicate volcanic degradation during volcanic activity. As degradation of the volcanic complex progressed, summit regions coalesced, later becoming unidirectional breached, increasing the area of the drainage basin and thus the potential to erode and transport extensive amounts of material away, ultimately forming Lyttelton Harbour, Gebbies Pass, and the infilled Mt Herbert region. Epiclastic deposits on the south-eastern side of Lyttelton Harbour indicate a paleo-valley system (paleo-Lyttelton Harbour) existed prior to 8.1 Ma, while the morphology of the Lyttelton Volcanic Complex directed the eruptive sites, style and resultant morphology of the proceeding volcanic groups.

Lakes and lake sediments from four areas around the Antarctic Peninsula are described. The concentrations of trace metals in sediment are found to be a useful tool in distinguishing between the different sedimentary phases during a transition from marine to limnic environment. A tephrochronology based on Deception Island tephra is developed, and used to cross date sediments from different lakes in order to overcome the radiocarbon dating problem of the area. The fluctuating concentrations of copper and phosphorus from penguin guano in the sediment of Lake Boeckella are used as a proxy for the penguin inpact on the sediment, and the size of the penguin rookery on the shores of the lake. Anthropogenic activities in the area, as well as climatic changes are discussed in relation to the rookery size. A radiocarbon dating model developed for the sediment of Lake Boeckella showed that the radiocarbon correction factor in the sediment depends on the amount and apparent age of the penguin guano washed down into the lake, and the amount of particulate carbon from the watershed present in the sediment. Neither the "old" meltwater from the glaciers nor dissolved carbonates contributes significantly to the correction factor. The model is used to achieve more accurate radiocarbon dates of the Lake Boeckella sediment. This model, or a modified version, may contribute to a higher dating accuracy and a better understanding of the dating problems in Antarctica. Deglaciation dates, as well as data on the climatic and environmental history of Byers Peninsula on Livingston Island, South Shetland Islands, of Hope Bay, Antarctic Peninsula and of Hidden Lake area, James Ross Island are given. / <p>Diss. (sammanfattning) Umeå : Umeå universitet, 1993, härtill 6 uppsatser.</p> / digitalisering@umu

No description available.

The western Antarctic Peninsula (WAP) is a hotspot of climatic and oceanographic change, with a 6°C rise in winter atmospheric temperatures and >1°C warming of the surface ocean since the 1950s. These trends are having a profound impact on the physical environment at the WAP, with widespread glacial retreat, a 40% decline in sea ice coverage and intensification of deep water upwelling. The main objective of this study is to assess the response of phytoplankton productivity to these changes, and implications for the marine carbon and nitrogen cycles in the WAP coastal zone. An extensive suite of biogeochemical and physical oceanographic data was collected over five austral summer growing seasons in northern Marguerite Bay between 2004 and 2010. Concentrations and isotopic compositions ( 15N, 13C, 14C) of dissolved nitrate, dissolved inorganic carbon species, particulate nitrogen, organic carbon and chlorophyll a are used in the context of a substantial ancillary dataset to investigate nutrient supply, phytoplankton productivity and nutrient uptake, export flux and the fate of organic material, and the factors underpinning pronounced seasonal and interannual variability. High-resolution biogeochemical time-series data for surface and underlying seawater, sea ice brine, sediment trap material and coretop sediments allow detailed examination of carbon and nitrogen cycle processes under contrasting oceanographic conditions and the interaction between these marine processes and air-sea exchange of climate-relevant CO2. This study shows that the WAP marine environment is currently a summertime sink for atmospheric CO2 in most years due to high productivity and biological carbon uptake sufficient to offset the CO2 supply from circumpolar deep waters, which act as a persistent source of heat, nutrients and CO2 across the shelf. For the first time, CO2 sink/source behaviour is parameterised in terms of nitrate utilisation, by exploiting the relationship between CO2 and nitrate concentrations, and deriving the nitrate depletion at which surface ocean CO2 is undersaturated relative to atmosphere and carbon sink behaviour is achieved. This could have vast utility in examining CO2 sink/source dynamics over greater spatial and temporal scales than by direct CO2 measurements, of which availability is more limited. This study documents abrupt changes in phytoplankton productivity, nitrate utilisation and biological CO2 uptake during a period of rapid sea ice decline. In fact, nitrate utilisation, particulate organic matter production and biological CO2 uptake all decrease by at least 50 % between a sea ice-influenced, high productivity season and one of low sea ice and low productivity. The key driver of interannual variability in production and export of organic material is found to be upper ocean stratification and its regulation of light availability to phytoplankton. Productivity, CO2 uptake and export are maximal when stratification is sufficient to provide a stable well-lit surface environment for phytoplankton growth, but with some degree of mixing to promote export of suspended organic matter. Strong stratification causes intense initial production, but retention of suspended organic particles in the surface ocean induces a self-shading effect, and overall productivity, CO2 uptake and export fluxes are low. When stratification is weak, mixing of phytoplankton over a larger depth range exposes cells to a wider range of light levels and reduces photosynthetic efficiency, thus total productivity and CO2 uptake. A conceptual model is developed here, which attempts to describe the mechanism by which sea ice dynamics exert the principal control on stratification and therefore productivity and CO2 uptake at the WAP, with potential application to other regions of the Antarctic continental shelf. Although meteoric waters (glacial melt and precipitation) are more prevalent in surface waters throughout the study, sea ice meltwater variability is driven by large and rapid spring/early summer pulses, which stabilise the upper ocean and initiate phytoplankton growth. The timing and magnitude of these sea ice melt pulses then exert the key control on stratification and seasonal productivity. In a low sea ice year of this study, the sea ice trigger mechanism was absent and productivity was low. This strongly suggests that ongoing sea ice decline at the WAP and greater frequency of such low sea ice years is likely to drive a dramatic reduction in productivity and export, which would substantially reduce the capacity of the summertime CO2 sink in this region. Ongoing warming and ecosystem change are thus likely to have severe impacts on net CO2 sink/source behaviour at the WAP over the annual cycle, and the role of the Southern Ocean in regulating atmospheric CO2 and global climate. Finally, factors influencing the stable isotopic signature of particulate organic carbon ( 13CPOC), a common paleo-proxy, are assessed. 13CPOC is greatly influenced by seasonal shifts in diatom assemblages and isotopically heavy sea ice material, so cannot be used as a robust proxy for ambient CO2 in the coastal Southern Ocean.

Using cluster analysis and a geographic information system (GIS), this study attempted to identify a settlement system in the Dingle Peninsula of Early Christian Ireland based on the morphological variability of ringforts. Cluster analysis was used to determine if an intuitive ringfort typological model created by the author had validity. Use of cluster analysis identified three distinct classes of univallate ringfort. Although these clusters have a higher variable mean than anticipated, they do appear to verify partial validity of the author's model. With the exception of Cluster 1, it appears that the assumption that as unvallate ringfort banks increase in elaboration, than so does their internal diameter.ARC/INFO, a GIS was used to help test the hypothesized relationship between ringfort clusters. It was assumed that the univallate ringforts with the smallest banks would be very close to and in the line of sight of bivallate and mulitvallate ringforts. Those with an intermediate bank size would tend to be farther away and not in the line of sight of bivallate and multivallate ringforts. These assumptions were determined to be invalid. / Department of Anthropology

This thesis examines the role and function translations played in Turkish history, especially within the framework of its Westernisation movement from the mid-nineteenth to the late twentieth centuries. A descriptive approach is adopted, aiming to identify cultural patterns which shape and reflect translational decisions and help to a better portrayal of the socio-cultural context of translation during the time span examined. To this end, the thesis seeks to describe in detail historical, political, literary and linguistic factors which have affected the translation activity. The main assumption of this thesis is that acculturation was used as the main strategy in translations from Western languages during the periods which were marked with an extensive translation activity, especially during the nineteenth century and the first decades of the Republican era. This acculturation strategy not only helped to enrich the target literary system, bringing new literary models (genres), new subject matter, developing the language and giving rise to a new Turkish literature, it also had an effect upon the broader socio-cultural polysystem, especially on the process of identity creation. The analysis of the social, political and cultural conditions and policies suggests that the status given both to the source and target cultures has been the main factor for the acculturation. As examined in the last part of the thesis, a shift of power relations in the Turkish context, especially after the 1980s, marked a new kind of an acculturation strategy and a certain movement of resistance. The thesis concludes that there is need to know more about different translation histories in order to learn more about the acculturation process and to move beyond a Eurocentric view, and an interdisciplinary approach should be taken for such research.