Ever since John Hooper (c.1500-1555), the future Bishop of Gloucester and Worcester, made his famous stand against wearing vestments that placed him in opposition to the leading English clergy, he has been branded in the history of the English Reformation by many as a renegade and a radical. However, this thesis presents Hooper as one who saw himself as a conformist who sought to create the reformed community he desired within the established political and religious customs of his day. To explore this idea, this thesis examines how Hooper imagined a Protestant community for the kingdom of England or elsewhere. It identifies what Hooper considered to be the sources of God’s authority in the community; how that authority was exercised through officials within the community and through godly laws, strong clerical preaching and a universal commitment to vocation. It examines how the people should respond to leaders who brought the successful introduction of Protestantism to their community. Hooper’s vision was advanced in a series of tracts and letters written in Zurich and shortly after his return to England (1547-1551). They were composed at a time when Hooper enjoyed the greatest freedom to articulate his ideas in the company of his mentor, Heinrich Bullinger (1504-1575), and refined through his tenure as a bishop in the Church of England. The reformed community that Hooper envisioned was one that was dependent upon a strong magistrate but also required the acceptance and participation of its members in fully embracing their own vocation and reform. Hooper strongly affirmed that leaders – both ecclesiastical and civil – had a duty to model their reformation in accordance with God’s Law, the Ten Commandments. He assumed that the people would abide by the authority of the Decalogue and practice the Protestant faith together. He also believed that living in such a community would usher in a period of peace and prosperity. Hooper’s zeal for reform was demonstrated by his belief that the Reformation required wholehearted embrace by everyone, but he was willing to operate within established English traditions, in order to see his Protestant beliefs realised within the community.

Mesozooplankton community structure in the vicinity of the Prince Edward Islands (PEIs) was investigated during six surveys conducted in late austral summer (April/May), 1996 to 1999. Each year zooplankton samples were collected with a bongo net (300 µm mesh) at stations upstream (west), between and downstream (east) of the islands. Chlorophyll a concentrations were determined fluorometrically, corresponding with each net tow. The positions of the Subantarctic Front (SAF) and the Antarctic Polar Front (APF), in relation to the islands in the upstream region, were determined by a line of CTD and/or XBT stations. Both the SAF and the APF were characterised by a high degree of meridional variation in position. Changes in position of the fronts were shown to occur very rapidly. In 1999 the APF moved southwards by ~40nm and the SAF northwards by ~60nm in a period of two weeks, while in 1996 the SAF appeared to move ~120nm northwards in a two week period. The positions of the SAF and APF appeared to have a significant impact on phytoplankton biomass in the vicinity of the PEIs, through the alteration of local flow dynamics. Water retention in 1996, associated with the location of the SAF and APF far to the north and south of the PEIs respectively, corresponded with high chlorophyll a concentrations in the inter-island region (reaching 1.54 mg.m^(-3)). When the fronts were close to the islands, in 1997 and 1999, and a flow through environment existed, chlorophyll a concentrations in the inter-island region were comparatively low. Although biomass enhancement was only observed at the SAF in 1996, phytoplankton size structure in 1999 indicated that, when close to the PEIs, frontal production may be transported to the island system. This is potentially an important source of allochthonous input into the island system. Zooplankton assemblages were a mix of sub-Antarctic and Antarctic communities, with a weak presence of sub-tropical species. Cluster analysis showed that during each survey the region in the vicinity of the PEIs was divided into different, spatially separated zooplankton communities, associated with water masses of different origins. These communities were identified by variations in the abundance and biomass of species rather than variation in species composition and, in general, there was a relatively high degree of similarity both within and between surveys. Inter-annual community analysis revealed that, in many cases, there was greater similarity between communities from different years than communities within years, indicating that short-term variability exceeded inter-annual variability. Multiple regression analysis showed that the major correlate with zooplankton community structure during all surveys was sea temperature, accounting for as much as 77% of the variation in community structure. Temperature was indicative of the relative contribution of sub-Antarctic and Antarctic communities, with low temperatures being characterised by an increased predominance of Antarctic communities and vice versa. The differentiation between sub-Antarctic and Antarctic waters, and their respective communities, was particularly pronounced when the SAF and APF were in close proximity to the islands. Surface salinity and sounding had limited effect on community structure. The affect of sounding was intrinsically related to zooplankton interaction with the island ecosystem. Predation by the islands' land based predators and benthic fish appears to decrease zooplankton biomass over the island shelf, particularly the macrozooplankton size fraction. However, this may only be an important factor under conditions of water retention when replenishment of zooplankton stocks is low. The low densities of many macrozooplankton species, and other deep migrators, on the island shelf may be due to their limited advection onto shallow topography. By contrast, there are indications that zooplankton species occurring at shallower depths may be concentrated in the inter-island region by mesoscale flow patterns. Analysis of the population structure of the copepod Calanus simillimus showed that this species occurred at different stages in its life cycle during different years, even though sampling took place in the same calendar months, indicating that there was inter-annual variation in the timing of the biological season. Differences in the population structure of species, and consequently their contribution to abundance and biomass, may therefore have been an important contributor to inter-annual variation in community structure. Evidence is provided for a long-term trend of southward movement of the SAF. This may have a significant affect on the PEI ecosystem, increasing the proportion of allochthonous input and altering the tropho-dynamics of the island ecosystem

The world's tundra regions can be considered as the last unexploited terrestrial biome on the earth's surface. Bryophytes contribute significantly to primary production and nutrient cycling in tundra habitats but received considerably less attention than the vascular plants during research for the Tundra Biome Project of the International Biological Programme in the 1970s. The IBP synthesis recognised this and called for more bryophyte production data and improved methodology in future studies. The synthesis also identitied the need for more information on within-site variability, energy/chlorophyll relationships and mineral nutrient studies where tundra bryophyte production patterns are concerned. Marion Island in the sub-Antarctic has an oceanic "tundra" type of vegetation, and the island offers the characteristics of an ideal "natural laboratory" for conducting fundamental ecological research particularly in the field of primary production and energy flow. Studies at Marion Island paralleled those of the IBP but also concentrated on the vascular component of the vegetation. Bryophytes contribute up to 60% of the biomass and 90% of plant cover in the mires that dominate the well-vegetated coastal plain of Marion Island. Following the termination of IBP research therefore it was decided to extend these studies during the 1980s by measuring growth and characterising the major factors influencing growth patterns in Marion Island bryophytes. In this thesis information is given on the physical and biotic environment of Marion Island. Data is presented on the cover, biomass, seasonal and annual production values, and turn-over rates (decomposition) of 15 bryophyte species found across the full range of habit at types at Marion Island. An analysis is also made of growth-associated variables viz. soils, climate, plant energy, chlorophyll. water and mineral nutrient contents. Production was found to be related broadly to moisture-related variables, overlain by nutrient factors in some instances. Higher absolute production figures were obtained than at other tundra sites and interesting phenological data are discussed. The results suggest that decomposition is controlled mainly by tissue degradability factors and that decomposition is more significant than production in controlling biomass accumulation. A model is given for production/decomposition patterns across the range of habitat conditions at Marion Island. Several growth measurement techniques were tested and recommendations are made concerning methodology for future bryophyte production studies. By reference to ecological data collected during the study.

This study aims to uncover the synoptic weather circulation pattern which is associated with the occurrence of needle ice, snowfall and the zero-curtain effect. The method of study was done through an intensive ground climate measurement campaign from April 2008 to May 2009 with a temperature logger installed throughout the recording period. Results from data analyses indicate that the complex changes in climate parameters may lead to an equally complex response in terms of spatial soil frost dynamics and its direct and indirect effects on soil sediment displacement and ecosystem dynamics. Field evidence in the study suggests that on Marion Island needle ice developed in temperatures as high as -0.2 ºC in strong winds. This confirms that the wet environment of Marion Island, which is dominated by diurnal soil frost is fundamentally different from seasonal frost and permafrost environments. The scoria material is susceptible to needle ice growth and the compacted soil alters the micro-climatology of the affected area making it more susceptible to the formation of needle ice. Soil moisture for needle ice formation and growth is provided by the misty conditions associated with the advent of the cold front (pre-cyclonic). Furthermore, observations of needle ice on Marion show that needles are mostly clear with no sediment inclusion. This is indicative of needle ice formation that has not been interrupted by a shortage of moisture. The zero-curtain effect on Marion Island can occur either as a response to the thawing of the soil after the seasonal freeze. The synoptic assessment of snowfall on Marion Island indicates that; snowfall is associated with the passage of a cold front linked to a strong meridional system of low pressure just south of the island.

This thesis examines the evidences of pessimism in the poetry of each poet, substantiated when possible by parallel prose writings and other critical and biographical material; and finally, it reaches tentative conclusions about the direction of the change in pessimistic outlook of three poets.

This thesis is a study of oral histories and literary records covering the professional development and works of Edward Blake Jr., ASLA, (1947-2010). The study considers Blake’s design principles via newly collected oral histories and a review of his literary record within the continuum of landscape architecture history from 1970 to 2010. Additionally, the study explores Blake’s position within the ecological design community to establish his status as a possible founding voice of ecologically focused landscape architecture practice in the Coastal Plains Region of the southeastern United States. The primary sources include a newly developed oral history collection with questionnaire-based interviews of Blake’s eight colleagues, professional mentors, and collaborators, along with various forms of project and process documentation generated by Edward Blake Jr. and his practice, known as The Landscape Studio. The study concludes with a distillation of Blake’s design principles, lexicon, and contribution to the field of landscape architecture.

Scholarship on Gustav Mahler’s (1860–1911) late works is often overshadowed by the events of 1907: the death of his daughter, his resignation from the Vienna Court Opera, and the diagnosis of his heart condition. The subjective juxtaposition of this biographical detail on his last works—Das Lied von der Erde (1908), the Ninth Symphony (1909), and the Tenth Symphony (1910, unfinished)—has provoked the application of themes of death, transcendence, and farewell as extra-musical elements to his music. While scholars such as Vera Micznik, Henry-Louis de La Grange, and Stephen Hefling have called the acceptance of this program into question, there has yet to be a more objective analysis of Mahler’s last works via the lens of late style theory. This thesis explores two of Mahler’s last works, Das Lied and the Ninth, through the application of Edward Said’s theory of late style. Rather than approaching death with harmony, resolution, and transfiguration, the late artist in Said’s theory evokes “intransigence, difficulty, and unresolved contradiction”. Instead of a psychological or biographical interpretation of late style, Said’s theory focuses on irreconcilable characteristics that set the artist apart from the age in an anachronistic way. Following his more objective approach of interpreting late style, this thesis relies on the musical elements that characterize Mahler’s late style, categorized as anachronism, disintegration, and evasion of closure. Through the discourse of Said’s late style theory, this thesis reveals alternative means of interpreting Mahler’s late style that avoids the myth of the artist transfigured by death.

No description available.

No description available.

No description available.