125 resultados para Late Palaeozoic


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The Catholic Church was profoundly affected by the 1872 Victorian Education Act, which made education secular, compulsory and free, and led to the withdrawal of state aid to religious schools. In order for the Church to run its own schools, it had to look overseas for help and invited religious teaching orders, such as the Faithful Companions of Jesus (FCJs) to set up schools in Victoria, Australia. In many instances purpose built buildings were designed by architects. William Wardell was well established in private practice in Sydney when he designed the new Convent and School, Kew, Victoria, for the FCJ Sisters, in the late 1880s. Building commenced just before the crash of Marvellous Melbourne. Less than half of the total concept of Wardell’s original plan was built. It opened for business in April 1891. Today this building forms the heart of the contemporary Genazzano FCJ College Kew. Many histories intersect in this commission. The vision for Catholic education in Victoria in the late 19th century is critical. The FCJs charism and their experience of teaching in Europe, in France, England, Ireland, Italy and Switzerland, provides a model for their work in Australia. At this time the importance of architecture to society is made manifest in education and its demands on building: if learning is valued then buildings should reflect this, for public buildings can shape morality. Wardell was trained as a Gothic Revival architect and his building participates in a broader medieval and Gothic tradition. Wardell’s original plan for this late Victorian Gothic style asymmetrical three-storeyed building, was designed to integrate a convent, school, chapel, and dormitories. This paper considers architectural history from diverse perspectives, educational, social, religious, economic and political, recognising the complexity of this project and the people who played a part in its conception and realisation.

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This study examines the morphological responses of Late Permian brachiopods to environmental changes. Quantitative analysis of body size data from Permian–Triassic brachiopods has demonstrated significant, directional changes in body size before, during and after the Late Permian mass extinction event. Brachiopod size significantly reduced before and during the extinction interval, increased for a short time in more extinction-resistant taxa in the latter stages of extinction and then dramatically reduced again across the Permian ⁄ Triassic boundary. Relative abundances of trace elements and acritarchs demonstrate that the body size reductions which happened before, during and after extinction were driven by primary productivity collapse, whereas declining oxygen levels had less effect. An episode of size increase in two of the more extinction-resistant brachiopod species is unrelated to environmental change and possibly was the result of reduced interspecific competition for resources following the extinction of competitors. Based on the results of this study, predictions can be made for the possible responses of modern benthos to present-day environmental changes.

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This article seeks to demonstrate how Janet Frame’s late fiction can be read as a theoretical engagement with the conceptual investigations of Gilles Deleuze and Félix Guattari, especially the notions of minor literature and the in her late novels Living in the Maniototo (1981) and The Carpathians (1989). For this reason, my approach must be sharply distinguished from a more commonplace analogical framing of Frame or a simple one-to-one translation of her fiction into alternative terms. By weaving theory through her fiction, Frame makes a significant contribution to literature that responds to the still-emerging field of Deleuzean literary critical theory.

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Many within the history profession today consider that we are experiencing an ‘emotional turn’, a perception that has been spurred by a recent proliferation of research centres and outpouring of publications exploring the concept of emotion. Interest in this field looks likely to grow, although there are methodological challenges that have yet to be overcome, as, of course, there are with any newly emerging field of study. One main concern is source material. Attempting to access such an elusive and intensely subjective area of historical inquiry as emotions requires seeking out new sources, as well as returning to old ones with a fresh eye, with new questions in mind. In the specific realm of the emotional lives of women living in Victorian and Edwardian Britain, fiction proves a promising source – popular fiction especially. This is due to the fact that this was the era that ushered in the modern bestseller, novels that more often than not explored the everyday and the emotional, novels that were thought to have been ‘devoured’ by women in particular. This essay plots recent developments in the burgeoning area of emotions history, as well as those that have taken place in relation to the use of fiction as evidence in a history of women’s interior lives. It argues that, at this point in the development of emotions history, when questions of methodology, interdisciplinarity and sources are being addressed more widely, consideration should be given to popular fiction as a readily available pathway, if not an uncomplicated one, into the emotions of the past.

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Numerous Permian limestone blocks exposed along the Yarlung-Zangbo Suture Zone have been named Tibetan facies exotic limestone blocks or Chitichun-type Permian deposits.The Gyanyima limestone block,one of those limestone blocks,is located in Burang County,southwestern Tibet.Fusulines are abundant in the Gyanyima limestone block especially for Middle Permian Xilanta Formation.The fusuline fauna comprises 10 genera,respectively Neoschwagerina, Yangchienia, Armenina, Verbeekina, Paraverbeekina, Kahlerina, Lantschichites, Codonofusiella,Chusenella, Nankinella.This fauna indicates a Midian age(Late Guadalupian or Lengwuan age of South China) in terms of the coexistence of Kahlerina, Lantschichites, Codonofusiella and Neoschwagerina.

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A fusuline fauna consisting of 9 species of 4 genera from the Xiala Formation of the Mujiucuo section, Xainza County, Tibet, China is described. The fusuline fauna is dominated by Nankinella and Chusenella and indicates a Midian (Late Guadalupian) age. The earliest record of fusuline fauna during the Midian in the Lhasa Block suggests that the block rifted later than the Qiangtang Block to the north and the Baoshan and Tengchong blocks to the east, all of which yield much earlier fusuline faunas of Yakhtashian (Artinskian) age, but had drifted away from Gondwana to a relatively warm temperate zone in the Late Guadalupian (Middle Permian).

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The Late Permian strata, namely Raggyorcaka Formation, is distributed along the line from Shuanghu agency to Raggyorcaka area. The Formation comprises two parts divided by fault. The lower part is mainly composed of shale and carbonate containing fusulinids and brachiopods while the upper part is dominated by flora-bearing sandstone and mudstone. Acording to the new materials got from 1∶250 000 scale Mayigangrimap, the upper terrestrial flora-bearing deposits conformably overlie the lower marine fusulinids-bearing deposits. So, based on the analysis of paleon to logy and litho stratigraphy, the original Raggyorcaka Format ion are divided in to two parts. The lower is Raggyorcaka Formation standing for fusulinids-bearing marine deposits and the upper is Heitugou Formation (P3h), a new lithostratigraphic name represen ting flora-bearing deposits.

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The uppermost 5-15 m of the Douling Formation in the southern Hunan area. South China, yields a diverse fauna comprised of ammonoids, bivalves, and brachiopods. The brachiopods reported in this paper consist of 51 species in 34 genera and are dominated by the Lopingian (Late Permian) species associated with a few species persisting from the underlying Maokouan (Late Guadalupian). This fauna is of earliest Wuchiapingian in age as precisely constrained by the associated conodont Clarkina postbitteri postbitteri and the Guadalupian-type ammonoid fauna of the Roadoceras-Doulingoceras Zone in the brachiopod horizon. The discovery of the Lopingian species-dominated brachiopod fauna in the earliest Wuchiapingian in southern Hunan suggests a much less pronounced effect of the pre-Lopingian crisis (end-Guadalupian mass extinction) than the end-Changhsingian mass extinction in terms of brachiopods, a contemporaneous onset of the Lopingian recovery/radiation during the pre-Lopingian crisis period, and taxonomic selectivity of the pre-Lopingian crisis in terms of different fossil groups. New taxa are Echinauris doulingensis n. sp., Pararigbyella quadrilobata n. gen. and n. sp. and P. doulingensis n. gen. and n. sp.