Thesis (Ph.D.) -- University of Adelaide, Dept. of History , 2002. / "June 2002" Bibliography: leaves 229-270.

Thesis (doctoral)--University of Adelaide, 2002.

Diss. Univ. Zürich, 2006. / Register. Literaturverz.

A more descriptive title for the dissertation might be "Early historiography in Purang-Guge and its relationship between orality, kingship, and Tibetan identity: a close study of a recently uncovered 12th century historical manuscript from Tholing monastery in West Tibet." The present study is therefore a close textual analysis of all the outer and inner features of the Tholing Manuscript. When reading the text, there is the gradual realization that the archaic peculiarities in script, binding, spelling, vocabulary, prose, and narrative twists, all highlight the work as a wholly rare and different version from those early histories typically found in Central Tibet. The key difference lies primarily in the focal point of the narrative. Whereas most similar narratives from the time of the phyi dar (11th-13th centuries) onwards place at the core of their structure the history of Buddhism in Tibet, the Tholing text puts as its central focus kingship and the history of kings in Tibet. For this reason, while Buddhism plays an essential and integral part of the story as a whole, the text can be viewed as a more secular work then any comparable monastic history of the period. The narrative structure of the manuscript, with its heavy use of rhythmical prose, similes, archaic topoi and motifs, is hauntingly familiar to those parallel passages found among Old Tibetan Documents and is emblematic of the liminal period in which the text was written. At this time, histories were transitioning from disperse and possibly oral transmissions to predominantly formal organized written traditions. The poetic nature of the text, together with its unusual physical features, raises questions relating to its purpose and function, with the possibility of its use as a ritual manuscript for royal legitimization. Through a close study of the text, I offer some insights on the formative nature of early Tibetan historiography in establishing the sacred and political power of the kings of West Tibet.

No description available.

published_or_final_version / Earth Sciences / Master / Master of Philosophy

Previous studies on reconstructing the paleoclimate on the Tibetan Plateauare commonly based on a single proxy, and have thus limited the usage of their results. Therefore this study was designed firstly to evaluate the applicability of organic carbon isotopes from modern plants in the Tibetan Plateau as a paleo-environmental proxy, and secondly to apply palynology, organic geochemistry and biomarkers to the reconstructions ofpaleo-environmental history of central Tibet. The new, comprehensive records reveal the history of regional precipitation, temperature and vegetation change in responding to Holocene climatic changesin the region. Organic carbon isotope (δ13C) and lipid n-alkanes were measured from plant samples collected from various altitudes and environments across the study area. The δ13C results indicate the importance of availability of water to C3/C4 herbs distribution in this alpine region. The molecular distributions of trees, shrubs, herbs and submergent macrophytes show distinctive features in a number of indices. These indices are considered to be useful for paleo-environmental reconstructions. A 5.8m-long peat core, which were dated back to 95,000 yr BP was obtained from a river valley at an altitude of 4300 m above sea level. The pollen data from the core reveals a sparse herbaceous vegetation in the catchment area during early Holocene, suggesting non-favourable conditions for vegetation growth. The environment became wetter during the early mid-Holocene around 8100-7000 cal. yr BP, and since then a sedge-dominated wetland habitat was developed. This vegetation changed little until about 1100 cal. yr BP; from which an increase of drought-tolerant herbs was indicated by the pollen data, implying a slightly drier condition of the latter part of late Holocene. The pollen record suggests that the optimum precipitation in central Tibet occurred later and lasted longer than that in the East Asian Monsoon region. Finally, bulk sample carbon geochemistry(TOC, δ13C) as well as the biomarkers analysis on n-alkanes and GDGTs as paleo-limnology and paleo-temperature indicators respectively were applied to the core. Before 1500 cal. yr BP, the wetland was dominated by both vascular herbs as suggested by the δ13Cdata and aquatic floating/submerged macrophytes as indicated by mid-chain n-alkanes. The relative proportion of the two sources of organic matter input varied slightly, and vascular herbs increased in two episodes(5400 -4700 and 2800 -2300 cal. yr BP) indicated by the increase of long-chain n-alkanes (>n-C25). Considering of the soil water content variation by the ratios of iGDGTs to bGDGTs, the change between the two plant communities could to be caused by different lake status. GDGTs paleo-temperature reconstruction indicates a warm period from 6700 to 6000 cal. yr BP, which is believed to be the warmest and highly humid in central Tibetan region. Then the temperature decreased towards the late Holocene, consistent with other paleo climate records across the Plateau region, i.e. largely controlled by change of solar insolation. Along the decreasing trend, a warm episode at about 1200 yr BP that inferred from MAAT was suggested corresponding with the North Hemisphere Medieval Warming. / published_or_final_version / Earth Sciences / Doctoral / Doctor of Philosophy

Texte remanié de: Ph. D.--Philosophie de l'éducation--Université de Stockholm, 1993.

Zugl.: Berlin, Humboldt-Univ., Diss., 2008

Thesis (M.A.)--Guo li zheng zhi da xue, 1976. / Reproduced on double leaves from typescript. Includes bibliographical references.