WorldWideScience

Sample records for late imperial china

  1. Temperature and precipitation effects on agrarian economy in late imperial China

    Science.gov (United States)

    Pei, Qing; Zhang, David D.; Li, Guodong; Forêt, Philippe; Lee, Harry F.

    2016-06-01

    Climate change has been statistically proven to substantially influence the economy of early modern Europe, particularly in the long term. However, a detailed analysis of climate change and the economy of historical China remains lacking, particularly from a large-scale and quantitative perspective. This study quantitatively analyzes the relationship between climate change and the economy in late imperial China (AD 1600-1840) at the national level. This study also compares the findings on the relationship between climate change and the economy in late imperial China with those in early modern Europe. Results of multivariate regression and Granger causality analyses indicate that (1) climate change induces economic fluctuations in late imperial China, particularly in the long term; (2) given that the economic center is located in South China during the study period, temperature has a greater influence on the economy than precipitation; (3) the population of China is statistically proven to primarily act as consumers in the long term; and (4) given the long-term role of the Chinese population, the economic vulnerability in late imperial China under climate change is further increased and is higher than that in early modern Europe, whose population mainly acts as producers in the long term. In conclusion, the late imperial Chinese society has a high economic vulnerability to climate change. These findings revisit Malthusian theory and ‘Great Divergence’ theory by including the perspective of economic vulnerability under climate change during the study period. The role of the population must be investigated further to address the socioeconomic vulnerabilities under climate change.

  2. Benevolence for Obedience: Policies on Muslims in Late Imperial and Modern China

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    James D. Frankel

    2009-04-01

    Full Text Available In telling the story of Islam in China, scholars have tended to depict the historical encounter of China’s Muslim population with the social, political and cultural forces of Chinese state and society in terms of either “conflict or concord.” This generalization, which reduces a complex and nuanced history to a simple binary, is flawed not because it is completely untrue, but rather because its truth is incomplete. Chinese Muslims’ responses to the social and cultural context in which they live have been diverse and multifaceted, and the phenomenon of Islam in China is no more a monolith than either of the two great, multifaceted civilizations that lend it its name. In late imperial China, within the same century, albeit at different ends of the Empire, examples of both types of Muslim response to Chinese hegemony were witnessed: intellectual rapprochement and armed rebellion. In between those extremes, however, we see varying degrees of Muslim assimilation to the norms of Chinese society and a variety of positions adopted by the imperium and officialdom vis-à-vis the Empire’s Muslim subjects. In many ways, this pattern is repeated in the People’s Republic of China (PRC today.

  3. [The anatomical revolution and the transition of anatomical conception in late imperial china].

    Science.gov (United States)

    Sihn, Kyu Hwan

    2012-04-30

    This paper aimed to examine the anatomical revolution from Yilingaicuo (Correcting the Errors of Medicine) and Quantixinlun(Outline of Anatomy and Physiology) in late imperial China. As the cephalocentrism which the brain superintend human operation of the mind was diffused in China since 16th century, the cephalocentrism and the cardiocentrism had competed for the hegemony of anatomical conception. Because of the advent of Yilingaicuo and Quantixinlun, the cephalocentrism became the main stream in the anatomical conception. The supporters of the Wang Yangming's Xinxue(the Learning of Heart and Mind) argued that the heart was the central organ of perception, sensitivity, and morality of the human body in medicine since 16th century. Even reformist and revolutionary intellectuals like Tan sitong and Mao zedong who had supported the Wang Yangming's Xinxue embraced the cephalocentrism in the late 19th century and the early 20th century. May Fourth intellectuals had not obsessed metaphysical interpretation of human body any more in the New Culture Movement in 1910s. They regarded human body as the object of research and writing. The anatomy was transformed into the instrumental knowledge for mutilation of the body. Yilingaicuo challenged the traditional conception of body, and Chinese intellectuals drew interest in the anatomy knowledge based on real mutilation. Quantixinlun based on Western medicine fueled a controversy about anatomy. Though new knowledge of anatomy was criticized by traditional Chinese medical doctors from the usefulness and morality of anatomy, nobody disavowed new knowledge of anatomy from the institutionalization of Western medicine in medical school. The internal development of cephalocentrism and positivism had influence on anatomy in China since 16th century. The advent of Yilingaicuo and Quantixinlun provided the milestone of new anatomy, though both sides represented traditional Chinese medicine and Western medicine respectively. They

  4. Political Reforms in a Global Context: Some Foreign Perspectives on Constitutional Thought in Late Imperial China

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    Egas Moniz Bandeira

    2017-04-01

    Full Text Available This paper presents some outside views on the emergence of Chinese constitutional thought. It shows that Chinese constitutionalism in the beginning of the 20th century did matter to the outside world and did attract a large interest on a global scale. Foreign views were quite diverse. While most observers welcomed the adoption of a constitution in principle, there were many words of caution that such a transition should not be rushed, notedly among diplomats and politicians. Foreign powers thus adopted a policy of not pressuring China to adopt a constitution. In particular, this paper redefines the role of the Japanese statesman Itô Hirobumi, who continually tried to give his advice to the Qing government up until his death in 1909.

  5. Social Factors to Aggravate Disasters in Yunnan in Late Imperial China%清末民初云南灾荒加剧的社会因素

    Institute of Scientific and Technical Information of China (English)

    蒋立文

    2012-01-01

    云南的自然环境极具灾害性。明清以降至清末民初,由于人口急速膨胀、农田过度开垦和山林矿藏的掠夺式开发,云南生态环境迅速恶化,进而加速加剧了各类自然灾害的发生;农业与家庭手工业相结合的自然经济又从根本上限制了社会抗灾减荒能力的生成与提高。封建剥削、战乱兵祸及列强的经济掠夺、迷信赌毒等造成社会环境的全面恶化,各族民众极度贫困,加重了灾后饥荒疾疫的蔓延与流行。中央与地方政府的荒政长久缺失,导致云南赈灾救荒活动严重乏力。总之,清末民初的云南已完全陷入人为破坏生态环境加剧自然灾害频发、逢灾必荒的结果加速了社会环境的恶化、社会环境恶化又加重了饥荒的蔓延这一恶性循环过程。%Yunnan is prone to natural disasters due to its environment. From the Ming and Qing dynasties to late imperial China, population explosion, over-farming, predatory exploitation of forests and minerals, and ecological damages aggravated all kinds of natural disasters in Yunnan on one hand, and on the other hand, natural economy of agriculture and household handicrafts weakened the power of society to prevent and reduce disasters. Feudal exploitation, government's taxes, wars, bandits, economic plunder of imperialists, superstition, gambling and drugs deteriorated social environment, and extreme poverty of ethnic people speeded.up the wide spread of famine and epidemic after disasters. Neither the central government nor the local governments made policies to deal with natural disasters. As a result, disaster relief in Yunnan was seriously weak. All in all, Yunnan in late imperial China was ecological damages leading to frequent natural disasters which totally stuck into a vicious circle of man-made then would deteriorate social environment, and which in turn would result in prolonged famines.

  6. Review - China's Last Imperial Frontier and The Sichuan Frontier and Tibet

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    Robert Entenmann

    2012-12-01

    Full Text Available Review of: Yingcong Dai. 2009. The Sichuan Frontier and Tibet: Imperial Strategy in the Early Qing. Seattle and London: University of Washington Press. xiv+368. Maps, notes, glossary of Chinese characters, bibliography, index. ISBN: 978-0-2959-8951-8 (hardcover, 80USD, 978-0-2959-8952-5 (paperback, 30USD. and Xiuyu Wang. 2011. China's Last Imperial Frontier: Late Qing Expansion in Sichuan's Tibetan Borderlands. Lanham, Maryland: Lexington Books. xv+291. Notes, tables, glossary of Chinese characters, bibliography, index. ISBN: 978-0-7391-6809-7 (hardcover, 80USD 978-0-7391-6810-3 (ebook, 79.99USD. Until recently, historians have not paid much attention to Qing China's Tibetan frontier, but two excellent new studies address this neglect. One is Yingcong Dai's The Sichuan Frontier and Tibet: Imperial Strategy in the Early Qing, which examines the Qing conquest of the Khams region up to the end of the eighteenth century and its effect on Sichuan. The other is China's Last Imperial Frontier: Late Qing Expansion in Sichuan's Tibetan Borderlands by Xiuyu Wang, in which he describes Qing efforts to impose direct administration on the Khams region in the last years of the dynasty. The Qing annexation of eastern Khams was part of the regime's attempt to secure military control of Tibet and deny it to the Zunghar Mongols. As Dai shows, Tibet's strategic importance to the Qing directly shaped Sichuan's development. Although Sichuan was long an integral part of China, its demographic collapse during the ...

  7. El servicio civil en la China imperial

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    Omar Martínez Legorreta

    2005-01-01

    Full Text Available El texto describe la concepción del imperio chino y la estructura de gobierno que lo sostenía: la burocracia de los eruditos-funcionarios (mandarines, una clase numéricamente pequeña que ostentaba todo el poder y era la mayor propietaria de grandes extensiones de tierra. Todas las funciones de administración y mediación estaban a cargo de esos funcionarios, quienes eran preparados según los principios filosóficos del confucianismo y ocuparon una posición estratégica desde la que influían en toda política del gobierno y aseguraban así su permanencia. De ese modo se estableció un servicio civil de carrera de por vida, que a la vez que gobernaba y administraba, daba al régimen imperial la sanción racional y ética que necesitaba para el ejercicio de su autoridad. El secreto de su continuidad y supervivencia estaba en el sistema de exámenes para reclutar funcionarios para el Estado.

  8. Infection, contagion, and public health in late medieval and early modern German imperial towns.

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    Kinzelbach, Annemarie

    2006-07-01

    From today's point of view, the concepts of "miasma" and "contagion" appear to be two mutually exclusive perceptions of the spread of epidemic diseases, and quite a number of historians have tried to discuss the history of public health and epidemic diseases in terms of a progression from the miasmic to the contagionist concept. More detailed local studies, however, indicate how extremely misleading it may be to separate such medical concepts and ideas from their actual historical context. The article presented here, based on local studies in late medieval and early modern imperial towns in southern Germany, demonstrates to what extent the inhabitants of these towns had notions of both "miasma" and "contagion." Furthermore, a contextual analysis of language shows that they did not see a necessity to strictly distinguish between these different concepts relating to the spread of diseases. Tracing the meaning of "infection" and "contagion," we find that these terms were used in connection with various diseases, and that a change in the use of the expressions does not necessarily imply a change of the corresponding notion. Moreover, a coexistence of differing perceptions cannot--as some historians have suggested--be attributed to a divergence between the academic medicine and the popular ideas of that period. A survey of measures and actions in the public health sector indicates that a coexistence of--from our point of view--inconsistent concepts helped the authorities as well as the individuals to find means of defense and consolation during all those crises caused by epidemic diseases--crises that occurred very frequently in these towns during the late medieval and early modern periods. As the article demonstrates, the interaction during such crises reveals the continuity of ancient rituals and concepts as well as the adoption of new insights resulting from changes in the economical, political, scientific, religious, and social structures.

  9. The historical trend of Ming China: An imperial agric-mercantile society%明代中国历史趋势:帝制农商社会

    Institute of Scientific and Technical Information of China (English)

    赵轶峰

    2008-01-01

    Majority of contemporary Chinese historians have been employing a conceptual framework focusing on the difficulty of capitalistic development in China to analyze the historical trend and potentials of late imperial China. This approach based upon the presupposition of viewing the pattern of Chinese history as abnormal reflects with the remaining influence of the Western-centric methodology. Further, based upon a "normal" point of view, seven fundamental, irreversible, and systematical changes to the Ming society could be identified. By conclusion, China in the Ming period was transforming into an imperial agric-mercantile society. This process proves that late imperial China was not stagnate society without "history," meanwhile, its pattern of development was clearly not identical to the Westem style modernization progress.%中国史学界长期运用资本主义发生学障碍思想模式来分析明清中国历史演变的基本趋势,这其实是一种把明清史当作"变态"来看待的方法,带有强烈的西方中心论色彩.在讨论这种思想模式多方面的问题之后,从"正常"的视点出发,可得出明代中国正在发生七种历史性的转变、其趋势是演变成为一种帝制农商社会的结论.这一历程以独特而又合乎逻辑的方式展现了人类社会转变的一种非西方模式.

  10. Local responses to French medical imperialism in late nineteenth-century Algeria.

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    Gallois, William

    2007-08-01

    This article offers the first account of the lives of Algerian-born doctors working in the French colonial medical service between 1870 and 1900. Their stories reveal the manner in which the idea of medical imperialism had collapsed in Algeria, as a result of maladministration, racial policies, competition between civil and military authorities, budgetary constraints and the rise of the colons. The article also indicates the way in which medicine became a locus of opposition to French rule. It shows how the first decades of the Third Republic were critical in terms of a shift from the earlier idea of medicine serving as an emblem of the mission civilisatrice to the ideological potential of medicine being seen in much more nuanced terms by both French settlers and Algerian locals. It is argued that the notion of cultural resistance to imperialism through medicine emerges in the 1870s and 1880s, thereby prefiguring the work of Fanon and the Front de Liberation Nationale's later analysis of the 'sickness' of colonial Algerian society.

  11. YAKUTSKAYA OBLAST IN ALL-IMPERIAL SPACE (BASING ON GOVERNORS’ ALL-NATIONAL REPORTS (LATE XIX – EARLY XX CENTURIES

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    Alena I. Arkhipova

    2011-01-01

    Full Text Available The article considers governors’ reports in terms of imperial narrative presence. The author attempts to show Yakutskaya Oblast Governors V.N. Skrypitsyn and I.I. Kraft’s attitude towards non-Russian inhabitants, their views of region further development and its place in all-Imperial space.

  12. The Last State Monopoly Iron Works in Imperial China: The Zunhua Iron Works of the Ming Dynasty

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    Chen, Hongli; Liu, Haifeng; Qian, Wei

    2016-10-01

    The Zunhua iron works was the last state monopoly iron industry in Imperial China. Its history could be a clue to explain why such a well-developed iron industry in ancient China faded after the works collapse. From the available historical record, the study found that the iron works had a complex history with several openings, closings and relocations. In order to prove this, field investigations were carried out and three locations were finally confirmed, and a well-preserved furnace and many iron- and steel-making relics were found. Lastly, these relics, including the fuel, iron ores, and flux, were analyzed in order to infer the relevant iron- and steel-making technology in use at that time.

  13. Linguistic Imperialism

    DEFF Research Database (Denmark)

    Phillipson, Robert

    2013-01-01

    The study of linguistic imperialism focuses on how and why certain languages dominate internationally, and attempts to account for such dominance in a theoretically informed way.......The study of linguistic imperialism focuses on how and why certain languages dominate internationally, and attempts to account for such dominance in a theoretically informed way....

  14. Imperial Governance

    DEFF Research Database (Denmark)

    Gravier, Magali

    2015-01-01

    of this concept, which is ‘tailored’ to analyse only one type of empire, the colonial empire, and to disregard the existence of another type of empire. To escape this trap, the article suggests the use of two concepts, ‘inwards imperial governance’ and ‘outwards imperial governance’. These concepts make...

  15. 中国对日、韩、越三国科举的影响%Influence of China's imperial examinations on Japan, Korea and Vietnam

    Institute of Scientific and Technical Information of China (English)

    刘海峰

    2007-01-01

    中国科举对东亚世界产生了巨大影响.日本曾在公元8-10世纪仿行过科举,取士科目主要有秀才、明经、进士、明法及医、针等.韩国(朝鲜)的科举是中国之外实行最长、也最为完备的.越南则是世界上最晚废止科举的国家.东亚国家效法中国建立科举制,有力地促进了本国文化水平的提升.%China's imperial examinations greatly influenced the East Asian world. Japan imitated it during the eighth to tenth centuries; its subjects include xiucai, mingjing, jinshi, mingfa, as well as medicine and acupuncture. Korean imperial examinations are the longest and most comprehensive ones among other East Asian countries. Vietnam was the last to abolish the imperial examinations. All three East Asian countries imitated China in their imperial examinations, which greatly raised their cultural levels.

  16. Por que não houve capitalismo na China imperial? Uma contribuição neomarxista

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    Tiago Nasser Appel

    2015-12-01

    Full Text Available RESUMO O artigo parte do debate marxista da transição para lançar a seguinte pergunta: por que a China do início da Era Moderna (1500-1800 não conseguiu fazer a transição para o capitalismo, tal como viemos a conhecê-lo no Ocidente? Concluindo que as lutas de classe não nos dão uma resposta satisfatória ao problema, o autor busca ingredientes teóricos na escola de economia política braudeliana/arrighiana, que estabelece uma distinção entre capitalismo e economia de mercado. Partindo dessa distinção, sugere que, malgrado a China estivesse à altura da Europa em características econômicas decisivas - comercialização e comodificação de bens, terra e trabalho - até o século XVIII, tal como Gunder Frank argumenta em sua obra ReOrient, ela não embarcou em uma trajetória de acumulação capitalista, no sentido empregado por Braudel, por causa do "fato do Império". Carecendo do nível de dificuldades fiscais encontradas na Europa no início da Idade Moderna, a China imperial não precisou taxar pesadamente os comerciantes e os notáveis; portanto, não precisou negociar direitos e obrigações com a classe mercantil. De outro modo, os oficiais chineses não precisaram fazer concessões à nascente classe capitalista - concessões que granjearam às elites voz sem precedentes no governo, com a qual elas realizaram reformas que todas as sociedades pretéritas haviam considerado antinaturais.

  17. Review Essay: Knowing Society, Cultivating Citizens, and Making the State in Post-Imperial China

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    Robert Culp

    2013-03-01

    Full Text Available Tong Lam. A Passion for Facts: Social Surveys and the Construction of the Chinese Nation-State, 1900–1949. Berkeley: University of California Press, 2011. 280 pp. $60 (cloth.Janet Y. Chen. Guilty of Indigence: The Urban Poor in China, 1900–1953. Princeton: Princeton University Press, 2012. 320 pp. $45 (cloth/eBook.Understanding society and building the national community were, in many ways, paired common goals for China’s intellectuals and political leaders during the first half of the twentieth century. Complementary new books by Tong Lam and Janet Chen illuminate key dynamics of those processes. Lam’s A Passion for Facts: Social Surveys and the Construction of the Chinese Nation-State, 1900–1949 tracks the development of the social survey movement (shehui diaocha yundong during the first half of the twentieth century. Chen’s Guilty of Indigence: The Urban Poor in China, 1900–1953 analyzes efforts to explain poverty, categorize the poor, and extend to the needy “active relief,” which was meant to transform them from “parasites” into productive citizens. Together the books demonstrate how new systems of knowledge served to map the social field and how institutions of governance defined and reshaped social groups for the project of national mobilization, with Lam concentrating more on the development of modern technologies of knowledge and Chen focusing more on the development of governmental institutions and the imposition of social discipline. Through their analyses these books help to explain the process whereby abstract academic fields and research methodologies, along with theories and techniques of social governance, had material effects that transformed millions of people’s daily lives. They provide, in other words, striking examples of what Wen-hsin Yeh, Eddy U, and I have elsewhere characterized as “organized knowledge in action” (Culp, U, and Yeh n.d....

  18. 日俄战争后的日本《帝国国防方针》与中国东北%Japan's Imperial Defense Policy after the Japanese-Russian War and Northeast of China

    Institute of Scientific and Technical Information of China (English)

    吕秀一; 聂奎全

    2012-01-01

    Japan decided its "continental policy" for expansion as early as the late 19th century.In order to further clarify its national orientation,the Imperial Defense Policy was formulated with the purpose of replacing "defensive strategy" with "offensive strategy" in 1907 after the Japanese-Russian War.The Policy set Russia and US as imaginary enemies,elaborated its military strategy in Northeast of China against Russia and brought out detailed schemes of the power and interests search in this area.Generally speaking,Imperial Defense Policy is considered a manifestation of the developed "continental policy".%19世纪末,日本基本确立了旨在对外扩张的大陆政策。日俄战争以后,日本为了进一步明确日本的国家发展方向,于1907年制定了《帝国国防方针》,其主要宗旨是以"攻势战略"来替代"守势战略"。该方针以俄国、美国为假想敌国,不仅全面阐述了日本在中国东北防御俄国的军事战略,而且还对日后在东北所要获取的重要利权提出了具体方案。这一企图全面扩大日本在东北权益的《帝国国防方针》,是日本业已形成发展的大陆政策的具体表现。

  19. Syllabus for Use in Imperial Chinese History.

    Science.gov (United States)

    Husum, Carol

    This syllabus is for a one semester course in the history of Imperial China, a study of the development of the world's oldest civilization still in existence. Emphasis is placed upon the cultural as well as the political and economic development of China until 1644. Major topics in the course outline are: 1) The Origins and Geography of China; 2)…

  20. Sexological deliberation and social engineering: Albert Moll and the sterilisation debate in late imperial and Weimar Germany.

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    Bryant, Thomas

    2012-04-01

    The physician and sexologist Albert Moll, from Berlin, was one of the main protagonists within the German discourse on the opportunities and dangers of social engineering, by eugenic interventions into human life in general, as well as into reproductive hygiene and healthcare policy in particular. One of the main sexological topics that were discussed intensively during the late-Wilhelminian German Reich and the Weimar Republic was the question of the legalisation of voluntary and compulsory sterilisations on the basis of medical, social, eugenic, economic or criminological indications. As is clear from Moll's conservative principles of medical ethics, and his conviction that the genetic knowledge required for eugenically indicated sterilisations was not yet sufficiently elaborated, he had doubts and worries about colleagues who were exceedingly zealous about these surgical sterilisations--especially Gustav Boeters from Saxony.

  1. Sexological Deliberation and Social Engineering: Albert Moll and the Sterilisation Debate in Late Imperial and Weimar Germany

    Science.gov (United States)

    Bryant, Thomas

    2012-01-01

    The physician and sexologist Albert Moll, from Berlin, was one of the main protagonists within the German discourse on the opportunities and dangers of social engineering, by eugenic interventions into human life in general, as well as into reproductive hygiene and healthcare policy in particular. One of the main sexological topics that were discussed intensively during the late-Wilhelminian German Reich and the Weimar Republic was the question of the legalisation of voluntary and compulsory sterilisations on the basis of medical, social, eugenic, economic or criminological indications. As is clear from Moll’s conservative principles of medical ethics, and his conviction that the genetic knowledge required for eugenically indicated sterilisations was not yet sufficiently elaborated, he had doubts and worries about colleagues who were exceedingly zealous about these surgical sterilisations – especially Gustav Boeters from Saxony. PMID:23002295

  2. Late Cretaceous Aquatic Angiosperms from Jiayin, Heilongjiang,Northeast China

    Institute of Scientific and Technical Information of China (English)

    QUAN Cheng; SUN Ge

    2008-01-01

    Three taxa of Late Cretaceous aquatic angiosperms, Queruexia angulata (Lesq.) Krysht., Cobbania corrugate. (Lesq.) Stockey et al. and Nelumbites cf. extenuinervis Upchurch et al. from Jiayin of Heilongjiang, NE China, are described in detail. Among them, Cobbania and Nelumbites from the Upper Cretaceous in China are reported for the first time. The aquatic angiosperm assemblage of Queruexia-Cobbania-Nelumbites appears to imply a seasonal, warm and moist environment in the Jiayin area during the Santonian-Campanian time.

  3. 编年史视角下的日本在华鸦片贸易%"Imperial Japanese"Drug Trafficking in China:Historiographic Perspectives

    Institute of Scientific and Technical Information of China (English)

    若林正(加拿大); 王山峰(译)

    2014-01-01

    This historiographic study places "imperial Japanese"opium operations -largely run through Chi-nese collaborator regimes-in the context of postwar Japanese scholarly debates on World War Two in Asia .This approach may seem circuitous and convoluted .Why not just describe the opium operations directly .Three factors necessitate this tactical detour .First, not all "imperial Japanese"were ethnic Japanese;colonial peoples such as Koreans and Taiwanese also plied the drug trade in their capacity as Japanese imperial subjects .Second , this topic suffers acute neglect in Japan today owing to a form of postwar political correctness that warrants as much attention as the wartime opium operations themselves .Third, such ideological constraints on historical scholarship warp our understanding of Japanese aggression in China -including the role played by colonial subjects .Below, I briefly out-line the geopolitical contours of "imperial Japanese"opium operations on the Asian continent from 1895 to 1945 , and then tackle the prickly issue of why academic historians in postwar Japan feel a need to portray Chinese and Ko -reans solely as victims of a "Fifteen-Year War"between 1931 and 1945 .In other words , it is hoped that this study of Japanese drug trafficking will also unlock other doors .%二战期间日本在华的毒品走私,很大程度上是通过日本在华的协作者,即汉奸政权开展的,这也是绝大多数日本学者在战后讨论此问题时一个大的语境,这一研究路径看起来似乎有些迂回复杂。为什么不直接研究鸦片贸易呢?有三个方面的因素证明迂回研究的必要性。第一,并非所有的“日本人”都是种族上的日本人,日本殖民下的朝鲜人和台湾人也充当了日本在华鸦片走私的工具。第二,这一问题在战后政治正确的框架下未获得研究许可并被严重忽略了。第三,正因为有上述意识形态方面的强制,历史学者对于日本侵

  4. Late Silurian trilete spores from northern Jiangsu, China.

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    Wang; Li

    2000-08-01

    The Late Silurian is generally considered to a particular significant key period in the study of early land vascular plants. A trilete spore assemblage of the Upper Silurian is described from northern Jiangsu, China. This assemblage comprises 11 genera and 20 species of trilete spores (including laevigate, apiculate, perinotrilite, patinate, rarely distally murornate and equatorially crassitate, and three indeterminate trilete miospores forms). It has similarities to those described from coeval assemblages from around the world (e.g., England and South Wales; Tripolitania, Libya; Cornwallis Island, Canadian Arctic; Northwest Spain). The rare cryptospore, only one specimen (Tetrahedraletes sp.) had been found to be associated with the Chinese trilete spore assemblage. The discovery of the trilete spores from Late Silurian rocks indicates the existence of early land plants, some possibly vascular, at that time in northern Jiangsu, China.

  5. CHINA NATIONAL POLICY IN THE LATE 1950'S TO THE LATE 1970'S

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    D. V. Buyarov

    2016-01-01

    Full Text Available This article discusses the key features of the national policy of the Chinese government in respect of nonHan peoples. The relevance of this work is due to important national issue for China. Traditionally, China has evolved as a multinational state, which was caused solely as a factor of external influence, for example, the Mongol and Manchu invasion and implementation of foreign policy objectives aimed at expanding the boundaries, resulting in a connection of Xinjiang and Tibet. A key feature of China as a multiethnic state has always been a numerical predominance of one ethnic group - the Han, as a rule, makes up almost all periods of the history of China, about 90% of the population. At the same time, China has always been inhabited by many ethnic minorities, which are not only occasionally something borrowed from Han people, but also constantly subjected Sinification. Sinification it was and remains one of the leading destinations for small nations. With the formation of the PRC in 1949, before the new communist government faced the problem of alignment of the national policy with regard to national minorities. The national policy of the Communist Party of China in its development has passed through three stages. In this article is considered the second period of this policy since the late 1950‟s. When starting to implement policies "Great Leap Forward" and the end of 1970‟s., as a result of the reforms of Deng Xiaoping began to change and the situation of small nations. To date, the Chinese government's policy towards national minorities in general, aims to accelerate the socio-economic and cultural development of ethnic groups on the tightening of national areas to the level of the developed regions of China, which should consolidate the Chinese citizens and prevent separatist actions. Ethnic identity of small nations overshadowed and leveled.

  6. Study on the Late Permian Claraia in South China

    Institute of Scientific and Technical Information of China (English)

    YANG; Fengqing

    2001-01-01

    [1]Nakazawa, K., On Claraia of Kashmir and Iran, J. Paleont. Soc. Idia., 1977, 20: 194-204.[2]Kulikov, M. V., Tkachuk, G. A., On finding of Claraia (Bivalvia) in Upper Permian deposits of Northern Caucasus,Doklady Akad. Nauk. USSR, 1979, 245(4): 905-908.[3]Yin. H. F.. Uppermost Permian (Changxingian) Pectinacea from South China, Riv. Ital. Paleont., 1982, 88(3): 337-386.[4]Yin. H. F.. Bivalves near the Permian-Triassic boundary in South China, J. Paleo.,1985, 59(3): 572-600.[5]Yang. Z. Y.. Yin H. F., Wu, S. B. et al., Permian-Triassic Boundary Stratigraphy and Fauna of South China (in Chinese).Geological Memoirs, Ser. 2, No. 6, Beijing: Geological Publishing House, 1987, 56-57, 236-237.[6]Guo. F. X.. Bivalves Fossil of Yunnan (in Chinese), Kunming: Yunnan Technology Press, 1985.[7]Fang. Z. J., Discussion on Late Permian “Claraia”, Act. Palaeo. Sini. (in Chinese),1993, 2(6):653-661.[8]Zhang. Z. M.. Discussion on the ligament structure of Claraia and its evolution, Act. Palaeo. Sini. (in Chinese), 1980,19(6): 433-443.[9]Nanjing Institute of Geology and Paleontology, Academia Sinica, The Bivalves of China (in Chinese), Beijing: Science Press, 1976.[10]Zhou. Z. R.. Two ecological types of Permian Ammonoids, Science in China (in Chinese), Ser. B, 1985, (7): 648-657.[11] Stanley. S. M., Relation of shell form to life habitats of the Bivalvia (Mollusca), Geol. Soc. Amer., 1970, 125: 1-496.[12]Stanley, S. M.. tunctional morphology and evolution of byssally attached bivalve mollusks, J. Paleont, 1972, 46(2): 165-207.[13]Yin, H. F.. Ding, M. H., Zhang, K. X. et al., Late Permian-Middle Triassic Ecostratigraphy of the Yangtze Platform and Its Margins, Beijing: Science Press, 1995, 69-76.[14]Leonardi, E. Trias inferiore delle Venezie, Mem. Inst. Geol. Univ. Padova., 1935, II, 1-136.[15]Ichikawa. K. Zur Taxonomie und Phylogenie der Triadischen Pteriidae (Lamellibranch), Palaeotog., 1958, III, A, 132-212.

  7. Imperial expansion, public investment, and the long path of history: China's initial political unification and its aftermath.

    Science.gov (United States)

    Fang, Hui; Feinman, Gary M; Nicholas, Linda M

    2015-07-28

    The Neolithic (ca. 8000-1900 B.C.) underpinnings of early Chinese civilization had diverse geographic and cultural foundations in distinct traditions, ways of life, subsistence regimes, and modes of leadership. The subsequent Bronze Age (ca. 1900-221 B.C.) was characterized by increasing political consolidation, expansion, and heightened interaction, culminating in an era of a smaller number of warring states. During the third century B.C., the Qin Dynasty first politically unified this fractious landscape, across an area that covers much of what is now China, and rapidly instituted a series of infrastructural investments and other unifying measures, many of which were maintained and amplified during the subsequent Han Dynasty. Here, we examine this historical sequence at both the national and macroscale and more deeply for a small region on the coast of the Shandong Province, where we have conducted several decades of archaeological research. At both scales, we examine apparent shifts in the governance of local diversity and some of the implications both during Qin-Han times and for the longer durée.

  8. The Rise of Women's Modern Schooling in Late Qing China (1840-1911)

    Science.gov (United States)

    Liu, Xiaoyi

    2009-01-01

    The rise of women's modern schooling in late Qing China was deemed to be, by the historical trend of modern China, a progress that coincided with China's modernization and national self-strengthening movement after the humiliating defeat of the Opium War. This article is an examination of this process from 1840 to 1911, which had undergone three…

  9. Late Pleistocene glaciation of the Changbai Mountains in northeastern China

    Institute of Scientific and Technical Information of China (English)

    ZHANG Wei; NIU YunBo; YAN Ling; CUI ZhiJiu; LI ChuanChuan; MU KeHua

    2008-01-01

    The Changbai Mountains (2749 m a.s.l.) in northeastern China are one of the typical mountain regions with glaciation since late Pleistocene as evidenced by well-preserved erosive and accumulative land-forms at elevations above 2000 m a.s.l. Formed by glaciers around the crater lake, Tianchi Lake. Cirque glaciers developed on both the inner and outer sides of the volcanic cone. Well-preserved cirques, glacial trough valleys, glacial threholds, polished surfaces of the glacial erratics and the moraine ridges indicate that several glaciation processes took place during the last glacial period in this region. Re-sults of optically stimulated luminescence (OSL) dating on the moraine sediments, and the K/Ar, ther-mal ionization mass spectrometry (TIMS), electronic spinning resonance (ESR) dating on the volcanic rocks suggest two periods of glacier advances. One is named the Black Wind Mouth glacier advance taking place on the west and north slopes of the volcanic cone at an elevation of 2000-2100 m a.s.l.,which is dated to about 20 ka, being the result of the Last Glacial Maximum (LGM). The other is named the Meteorological Station glacier advance at the elevation of 2400--2600 m a.s.l., dated to 11 ka during the late glacial period, and is tentatively correlated to the Younger Dryas stage. The scope of the former glacier advance is larger than that of the latter. Regional comparisons showed that the glacial se-quences in the Changbai Mountains are similar to other glaciated areas in eastern Asia during the later part of the last glacial cycle.

  10. Paleoenvironmental reconstruction of the late Cenozoic Qaidam Basin, China

    Science.gov (United States)

    Zhang, C.; Wang, Y.; Li, Q.; Wang, X.; Deng, T.; Tseng, Z. J.; Takeuchi, G.; Xie, G.; Xu, Y.

    2011-12-01

    Reconstruction of paleoenvironments in the Tibetan region is important to understanding the linkage between tectonic force and climate change. Here we report new isotope data from the Qaidam Basin, China, which is located on the northeastern Tibetan Plateau, including stable C and O isotope analyses of a wide variety of late Cenozoic mammalian tooth enamel samples (including deer, giraffe, horse, rhino, and elephant), and O isotope compositions of phosphate (δ18Op) in fish bone samples. Mammalian tooth enamel δ13C values, when combined with fossil assemblage and other geological evidence, indicate that the Qaidam Basin was warmer and more humid during the late Miocene and early Pliocene, and that there was lush C3 vegetation with significant C4 components at that time, although the C4 plants were not consistently utilized. In contrast, the modern Qaidam Basin is dominated by C3 plants. Fish bone δ18Op values showed statistically significant enrichment from the Tuxi-Shengou-Naoge interval (late Miocene) to the Yahu interval (early Pliocene) and from the Yahu interval to the present day. This most likely reflects increases in the δ18O of lake water over time, as a result of increased aridification of the Qaidam Basin. Assuming that mammals drank exclusively from the lake, temperatures were calculated from average δ18Op values and average δ18Ow derived from large mammal tooth enamel δ18O. Temperatures were also estimated from δ18Op and δ18Ow estimated from co-ocurring large mammal tooth enamel δ18O. The temperature estimates were all lower than the average temperature of the modern Qinghai Lake surface water during the summer, and mostly too low to be reasonable, indicating that the fish and the large mammals were not in equilibrium with the same water. Assuming the relationship between salinity and δ18Ow observed for the modern Qinghai Lake and its surrounding lakes and ponds applied in the past, we calculated the paleosalinities of lake waters to be ~0 to

  11. An ancestral turtle from the Late Triassic of southwestern China.

    Science.gov (United States)

    Li, Chun; Wu, Xiao-Chun; Rieppel, Olivier; Wang, Li-Ting; Zhao, Li-Jun

    2008-11-27

    The origin of the turtle body plan remains one of the great mysteries of reptile evolution. The anatomy of turtles is highly derived, which renders it difficult to establish the relationships of turtles with other groups of reptiles. The oldest known turtle, Proganochelys from the Late Triassic period of Germany, has a fully formed shell and offers no clue as to its origin. Here we describe a new 220-million-year-old turtle from China, somewhat older than Proganochelys, that documents an intermediate step in the evolution of the shell and associated structures. A ventral plastron is fully developed, but the dorsal carapace consists of neural plates only. The dorsal ribs are expanded, and osteoderms are absent. The new species shows that the plastron evolved before the carapace and that the first step of carapace formation is the ossification of the neural plates coupled with a broadening of the ribs. This corresponds to early embryonic stages of carapace formation in extant turtles, and shows that the turtle shell is not derived from a fusion of osteoderms. Phylogenetic analysis places the new species basal to all known turtles, fossil and extant. The marine deposits that yielded the fossils indicate that this primitive turtle inhabited marginal areas of the sea or river deltas.

  12. Late Carboniferous and Early Permian algal microflora (Liuzhou, South China)

    Energy Technology Data Exchange (ETDEWEB)

    Li Chun (Nanjing Inst. of Geology and Paleontology, Nanjing (China)); Mamet, B. (Montreal Univ., PQ (Canada))

    1993-03-01

    Paleozoic algae are important contributors to the formation of carbonate sediments. A study was conducted to compare an Upper Carboniferous-Lower Permian carbonate succession of South China with what is generally observed in the Tethys Sea and North America. The sequence studied was in the Maping Limestone at the Loutishan section in Liuzhou, with some additional information derived from the Maping Limestone at Shangxinping and from the Chuanshan Limestone at Yuhuangshan and in the Nanjing Hills. In the Late Carboniferous, the beresellid algae are important builders and the Tubiphytes-Archaeolithophyllum community is locally replaced by a Tubiphytes-Ungdarella association. Early Permian oncolites were formed by complex Osagia, then by Esmerella. The Asselian Sphaeroschwagerina fauna is underlined by the outburst of epimastoporid dasycladales and phylloid Anchicodiaceae. Microcodium is observed at the contact of the Sphaeroschwagerina moelleri/sphaerica Zones. The overlying and paraconformable Chihsia Limestone is characterized by a Gymnocodium-Gyroporella-Mizzia flora. In most cases, the base of the fusulinid zones, therefore, coincides with an important local floristic change. 72 refs., 4 figs.

  13. The Garden and the Jungle: Burnett, Kipling and the Nature of Imperial Childhood

    Science.gov (United States)

    Goodwin, Mary

    2011-01-01

    Imperial British India is the point of origin for protagonists in both Frances Hodgson Burnett's "The Secret Garden" (1911) and Rudyard Kipling's "The Jungle Books" (1894-1895), two influential children's stories in which late Victorian notions of childhood education and nature converge with those of national and imperial identity. In Burnett's…

  14. From a Reliant Land to a Kingdom in Asia: Premodern Geographic Knowledge and the Emergence of the Geo-Body in Late Imperial Vietnam

    Directory of Open Access Journals (Sweden)

    Liam C. Kelley

    2016-09-01

    Full Text Available This article examines a change in how members of the educated elite in Vietnam viewed their kingdom’s place in the world. It argues that, prior to the twentieth century, Vietnamese scholars saw their kingdom as being connected to, or reliant on, the empire to its north, which we now refer to as “China.” In particular, Vietnamese literati believed that moral virtue from the North had spread southward over time and enabled the Southern Kingdom, as they sometimes called their land, to emerge. The flow of geomantic energy from north to south played a similar role. In 1908, however, a reformist scholar named Lương Trúc Đàm published a geography textbook, Geography of the Southern Kingdom (Nam Quốc địa dư, that disconnected the Southern Kingdom from any form of reliance on the North. In this work, Đàm also sought to nurture in his readers patriotic feelings toward the Southern Kingdom. In so doing, Đàm contributed to the creation of what historian Thongchai Winichakul has referred to as a “geo-body,” an identifiable and separate geographical entity for which students are taught to develop patriotic emotions.

  15. 中国古代宫内正殿太极殿的建置及其与东亚诸国的关系%Institution of Establishing the Main Pavilion Taijidian in the Imperial Palace of Ancient China and Its involvement in the Relationship between Then China and Other East Asian Countries

    Institute of Scientific and Technical Information of China (English)

    王仲殊

    2003-01-01

    From the Wei period in the third century, the main pavilion in the imperial palace of successive Chinese dynasties was called "Taijidian 太极殿," which had not changed down to the Tang period starting from the seventh century. In the Koguryo, Paekche and Silla kingdoms of the Korean Peninsula, Chinese institutions and culture were upheld to different extents. But even if the "Taijidian" was deeply admired in these kingdoms, by legal principle they could not adopted this name to the palaces of their own because they were protectorates of China according to the titles their rulers accepted from the Chinese emperor. In Japan, the Tang style was upheld to the greatest extent. On the other hand, from the early seventh century onward, the Japanese ruler insisted on "diplomacy on an equal basis" and had not been under the titling by China''s emperor. Therefore in the Asuka period of the seventh century, the Nara period of the eighth century and the Heian period from final years of the eighth century, the main pavilion in the Japanese imperial palace had all along been called "Daigokuden太极殿" in imitation of the Chinese institution.

  16. CHINA NATIONAL POLICY IN THE LATE 1950'S TO THE LATE 1970'S

    OpenAIRE

    D. V. Buyarov

    2016-01-01

    This article discusses the key features of the national policy of the Chinese government in respect of nonHan peoples. The relevance of this work is due to important national issue for China. Traditionally, China has evolved as a multinational state, which was caused solely as a factor of external influence, for example, the Mongol and Manchu invasion and implementation of foreign policy objectives aimed at expanding the boundaries, resulting in a connection of Xinjiang and Tibet. A key featu...

  17. Public Finance in China since the Late Qing Dynasty

    NARCIS (Netherlands)

    B. Krug (Barbara)

    2008-01-01

    textabstractHow is "public finance" organized in China? Is China’s public finance system different from that of other countries? Can we detect features which link today’s system to the past? Public finance refers to more than annual state budgets and constitutional procedures. It includes foreign

  18. Public Finance in China since the Late Qing Dynasty

    NARCIS (Netherlands)

    B. Krug (Barbara)

    2008-01-01

    textabstractHow is "public finance" organized in China? Is China’s public finance system different from that of other countries? Can we detect features which link today’s system to the past? Public finance refers to more than annual state budgets and constitutional procedures. It includes foreign de

  19. Public Finance in China since the Late Qing Dynasty

    OpenAIRE

    Krug, Barbara

    2008-01-01

    textabstractHow is "public finance" organized in China? Is China’s public finance system different from that of other countries? Can we detect features which link today’s system to the past? Public finance refers to more than annual state budgets and constitutional procedures. It includes foreign debt, state monopolies or monetary policies, all of which played a crucial role in China’s public finance during the last hundred years. A purely legislative definition obscures the fact that changes...

  20. Occurrence and Geological Genesis of Pyrites in Late Paleozoic Coals in North China

    Institute of Scientific and Technical Information of China (English)

    刘大锰; 杨起; 等

    2000-01-01

    The occurrence and geological genesis of pyrites in Late Paleozoic colas of North china have been systematically studied in terms of coal petrology,coal chemistry,elemental geochemistry and sulfur isotope geochemistry.The results suggest that eight types of pyrite,i.e.,framboidal,automorphic graular,oolitic,massive,homogeneous spherical,allotriomorphic,nodular,joint-and fisure-filling pyrintes can be subdivided under the microscope,Four generations of pyrite are also reconized according to the shape,size,coexisting assemblage,spacial distribution relationship with macerals,the contents of sulfur and iron.atomic S/Fe ratios and associated elements in pryites.Sulfur in Late Palozoic colas of North China is of diverse source as evidenced by sulfur isotope variations in the pyrites.The δ34S values of pyrite generated at the early stage ted to be negative,and at the late stage,positive.

  1. A basal tyrannosauroid dinosaur from the Late Jurassic of China.

    Science.gov (United States)

    Xu, Xing; Clark, James M; Forster, Catherine A; Norell, Mark A; Erickson, Gregory M; Eberth, David A; Jia, Chengkai; Zhao, Qi

    2006-02-01

    The tyrannosauroid fossil record is mainly restricted to Cretaceous sediments of Laurasia, although some very fragmentary Jurassic specimens have been referred to this group. Here we report a new basal tyrannosauroid, Guanlong wucaii gen. et sp. nov., from the lower Upper Jurassic of the Junggar Basin, northwestern China. G. wucaii is the oldest known tyrannosauroid and shows several unexpectedly primitive pelvic features. Nevertheless, the limbs of G. wucaii share several features with derived coelurosaurs, and it possesses features shared by other coelurosaurian clades. This unusual combination of character states provides an insight into the poorly known early radiation of the Coelurosauria. Notably, the presumed predatory Guanlong has a large, fragile and highly pneumatic cranial crest that is among the most elaborate known in any non-avian dinosaur and could be comparable to some classical exaggerated ornamental traits among vertebrates.

  2. [Selection of medical talents under the influence of imperial examination system in the Tang Dynasty.

    Science.gov (United States)

    Wang, Zhen-Guo; Zang, Shou-Hu

    2005-10-01

    The Tang Dynasty was an important period in which China's ancient imperial examination system was formed and perfected. The medical examination at that time was influenced by imperial examination system, too. Medical talents were chosen according to a clear regulation of exam subjects imitating "Examination based on Imperial College law", "Ming Jing" and "Ming Fa" in the Tang Dynasty. The ways of choosing sheng tu, gong jü, zhi jü, dai zhao were also used for choosing medical talents, and the practical subjects of medical examination and qualified standard were also made, which can be used as a reference for TCM education, examination, selecting and checking of TCM talents today.

  3. Belgium’s Expansionist History between 1870 and 1930: Imperialism and the Globalisation of Belgian Business

    OpenAIRE

    Abbeloos, Jan-Frederik

    2008-01-01

    This chapter considers if and how the political action of imperialism and the globalisation of business influenced each other in Belgium between 1870 and 1930. In addition to the role that Belgian King Leopold II played in the territorial partition of Africa and the opening up of China, the period sees a growing amount of capital and industrial know-how from Belgium being invested in markets outside Europe. Before World War I, the globalisation of Belgian business and Belgian imperialism oper...

  4. [The emergence of China's Railway Health Services and its motivation in the late Qing Dynasty].

    Science.gov (United States)

    Huang, Huaping

    2014-03-01

    In the late Qing Dynasty, the railway authority of China commenced establishing their self-run medical institutions, setting up the hygienic standards of railway system, and opening a new prospects of railway health services and epidemic prevention, reflecting the emergence of China's Railway Health Services. The motivations of all these approaches were related to three factors, that is,"the eastward dissemination of western medicine","the medical requirement of railway employees", and"the emergent situation of railway health and epidemic prevention".

  5. Absolute Cultural Imperialism is Impossible

    Institute of Scientific and Technical Information of China (English)

    张爽

    2014-01-01

    As globalization develops quickly no matter in its depth and its scope, the worry about whether globalization equals cultural imperialism is also increasing. This article proposes to see this problem from a dialectical view. It first notices the complexity of globalization itself so that proves the inequality between globalization and cultural imperialism. And then that the confused identity globalization causes should not be neglected is pointed out. The essential part of this article lies in encouraging developing countries to seize the opportunity to prosper their national cultures.

  6. Imperial vertigo and the themed experience: Yuanmingyuan and Disneyland compared

    Directory of Open Access Journals (Sweden)

    Erik Ringmar

    2013-05-01

    Full Text Available This article compares the morphological structures of two parks: Disneyland and Yuanmingyuan, the “summer palace” of the emperor of China. Despite obvious differences, the two parks were intended for the entertainment of the sovereigns of their respective countries — the emperor of China and “the people” in the case of the United States. Both parks were also designed to bring ontological reassurance to the sovereigns of two empires that only recently had attained their hegemonic, imperial, status. The parks provided a vision of a universe organized according to each sovereign’s specifications. The need for reassurance is reflected in the morphology of the two parks: the use of techniques of dislocation and idealization; the model-making and the use of thematized environments. A study of the morphology of the parks is for that reason a study of imperial ideology.

  7. [Physical anthropology studies at Keijo Imperial University Medical School].

    Science.gov (United States)

    Kim, Ock-Joo

    2008-12-01

    Medical research during the Japanese Colonial Period became systematic and active after the Keijo Imperial University Medical School was established in 1926. Various kinds of research were conducted there including pharmacological, physiological, pathological and parasitological research. The Keijo Imperial University was give a mission to study about Korea. Urgent topics for medical research included control of infectious diseases, hygiene and environmental health that might have affected colonizing bodies of the Japanese as well as the colonized. The bodies of Koreans had been studied by Japanese even before the establishment of the University. The Keijo Imperial University research team, however, organized several field studies for physical anthropology and blood typing research at the national scale to get representative sampling of the people from its north to its south of the Korean peninsula. In the filed, they relied upon the local police and administrative power to gather reluctant women and men to measure them in a great detail. The physical anthropology and blood typing research by the Japanese researchers was related to their eagerness to place Korean people in the geography of the races in the world. Using racial index R.I.(= (A%+AB%)/(B%+AB%)), the Japanese researchers put Koreans as a race between the Mongolian and the Japanese. The preoccupation with constitution and race also pervasively affected the medical practice: race (Japanese, Korean, or Japanese living in Korea) must be written in every kind of medical chart as a default. After the breakout of Chinese-Japanese War in 1937, the Keijo Imperial University researchers extended its physical anthropology field study to Manchuria and China to get data on physics of the people in 1940. The Japanese government and research foundations financially well supported the Keijo Imperial University researchers and the field studies for physical anthropology in Korea, Manchuria and China. The physical

  8. The succession of late Palaeozoic and Triassic plant assemblages of eastern China

    Science.gov (United States)

    Xingxue, Li; Xiuyuan, Wu

    This is a study dealing with the succession of the megafloras or plant assemblages of China's eastern part, ranging from the early Devonian to later Triassic. The plant assemblages in ascending order are as follows: 1. In the three floras formerly recognized for the early, middle and late Devonian, the latter two are here revised as the Protolepidodendron flora and the Leptophloeum-Archaeopteris flora, respectively. 2. Since the two-fold system of the Carboniferous has been currently accepted in China and the mid-Carboniferous boundary in NW China is drawn at the top of the Tsingyuan Formation (s.s.), the latest plant assemblage of the Lower Carboniferous is better named the Eleutherophyllum waldenburgense-Linopteris densissima-Pecopteris aspera Assemblage and its corresponding plant assemblage in SE China being tentatively named the Paripteris gigantea-Karinopteris acuta f. obtusa Assemblage. Moreover, recent studies on the Penchi flora of north China reveal that some typical Cathaysian elements, e.g. Lepidodendron posthumii, Tingia spp., occurred in the Penchi Formation, of which the plant assemblage is revised as the Paripteris gigantea-Linopteris neuropteroides-Conchophyllum richthofeni Assemblage, known probably as the first assemblage assigned to the early Cathaysian flora in east Asia. 3. The latest Permian (Tartarian) of north China is represented by the Ullmannia bronnii-Yuania magnifolia Assemblage based on recent studies of the flora of the Shihchienfeng (Sunjiagou) Formation. 4. Recent studies on the early Triassic flora in north China disclose that the flora may be named the Pleuromeia flora, which can be subdivided into the early Triassic Pl. jiaochengensis assemblage and the late early Triassic Pl. sternbergii Assemblage. In addition, problems about the correlation for some of the representative formations and their palaeophytogeographical regions are also discussed.

  9. Manufacturing Ancient Imperial Silk

    Institute of Scientific and Technical Information of China (English)

    1997-01-01

    China was the first country in the world to develop silkworm breeding silk reeling, silk weaving, dying and embroidering. Located in the middle and lower reaches of the Yangtze River, Zhejiang Province has a long history of silk production. At the Qianshanyang Remains, which date back 4,800 years, silk fabrics were excavated. All rulers of past ages had special organizations responsible for

  10. Imperial boyhood: piracy and the play ethic.

    Science.gov (United States)

    Deane, Bradley

    2011-01-01

    Representations of perpetual boyhood came to fascinate the late Victorians, partly because such images could naturalize a new spirit of imperial aggression and new policies of preserving power. This article traces the emergence of this fantasy through a series of stories about the relationship of the boy and the pirate, figures whose opposition in mid-Victorian literature was used to articulate the moral legitimacy of colonialism, but who became doubles rather than antitheses in later novels, such as R.L. Stevenson's "Treasure Island" and Joseph Conrad's "Lord Jim." Masculine worth needed no longer to be measured by reference to transcendent, universal laws, but by a morally flexible ethic of competitive play, one that bound together boyishness and piracy in a satisfying game of international adventure.

  11. Late Mesozoic basin and range tectonics and related magmatism in Southeast China

    Directory of Open Access Journals (Sweden)

    Dezi Wang

    2012-03-01

    Full Text Available During the Late Mesozoic Middle Jurassic–Late Cretaceous, basin and range tectonics and associated magmatism representative of an extensional tectonic setting was widespread in southeastern China as a result of Pacific Plate subduction. Basin tectonics consists of post-orogenic (Type I and intra-continental extensional basins (Type II. Type I basins developed in the piedmont and intraland during the Late Triassic to Early Jurassic, in which coarse-grained terrestrial clastic sediments were deposited. Type II basins formed during intra-continental crustal thinning and were characterized by the development of grabens and half-grabens. Graben basins were mainly generated during the Middle Jurassic and were associated with bimodal volcanism. Sediments in half-grabens are intercalated with rhyolitic tuffs and lavas and are Early Cretaceous in age with a dominance of Late Cretaceous–Paleogene red beds. Ranges are composed of granitoids and bimodal volcanic rocks, A-type granites and dome-type metamorphic core complexes. The authors analyzed lithological, geochemical and geochronological features of the Late Mesozoic igneous rock assemblages and proposed some geodynamical constraints on forming the basin and range tectonics of South China. A comparison of the similarities and differences of basin and range tectonics between the eastern and western shores of the Pacific is made, and the geodynamical evolution model of the Southeast China Block during Late Mesozoic is discussed. Studied results suggest that the basin and range terrane within South China developed on a pre-Mesozoic folded belt was derived from a polyphase tectonic evolution mainly constrained by subduction of the western Pacific Plate since the Late Mesozoic, leading to formation of various magmatism in a back-arc extensional setting. Its geodynamic mechanism can compare with that of basin and range tectonics in the eastern shore of the Pacific. Differences of basin and range

  12. Anthropogenic forcing of shift in precipitation in Eastern China in late 1970s

    Directory of Open Access Journals (Sweden)

    T. Wang

    2013-05-01

    Full Text Available Observation shows that eastern China has experienced an interdecadal shift in the summer precipitation during the second half of the 20th century. The summer precipitation increased in the middle and lower reaches of the Yangtze River Valley, whereas it decreased in northern China. Here we use a coupled ocean–atmosphere general circulation model and multi-ensemble simulations to show that the interdecadal shift is mainly caused by the combined effect of increasing global greenhouse gases and regional aerosol emissions over China. The rapidly increasing greenhouse gases induce tropical warming and a westward shift of the western Pacific subtropical high, leading to more precipitation in Yangtze River Valley. At the same time the aerosol cooling effect over land contributes to a reduced summer land–sea thermal contrast and therefore to a weakened East Asian summer monsoon and to drought in northern China. Consequently, an anomalous precipitation pattern starts to emerge in eastern China in late 1970s. Our results highlight the important role of anthropogenic forcing agents in shaping the weakened East Asian summer monsoon and associated anomalous precipitation in eastern China.

  13. Language Teaching=Linguistic Imperialism?

    Science.gov (United States)

    Muhlhausler, Peter

    1994-01-01

    Linguistic imperialism is the expansion of a small number of privileged languages at the cost of a large number of others. The language teaching profession needs to address the ecological impact of language teaching and focus on the well-being of the inhabitants of a language ecology rather than on the economic benefits of the teaching…

  14. Huanglong Cave, a new late Pleistocene hominid site in Hubei Province, China

    Institute of Scientific and Technical Information of China (English)

    WU Xianzhu; LIU Wu; GAO Xing; YIN Gongming

    2006-01-01

    For the past 20 years the modern human origins debate has received a significant amount of attention in paleoanthropological research. Primarily supported by the evidence of earlier dates of anatomically modern human fossils and genetic studies, the "Out of Africa" hypothesis is based on the belief that the ancestor of all modern humans, including modern Chinese, came from Africa. The opposite hypothesis "Mutiregional evolution" proposes that continuous evolution occurred on a regional scale, for which human paleontology offers strong support. However, due to the paucity of hominid fossils in China between 100 and 50 ka, support to the latter hypothesis is currently weak. This is a report here of five human fossil teeth, and associated stone tools and mammal fossils from a newly discovered cave site, Huanglong Cave, located in Yunxi County,Hubei Province, China. Preliminary studies indicate:(1) the morphological features of the human fossils resemble those of late Pleistocene human fossils from China; (2) the stone tools display patterns of both the southern and northern Paleolithic cultures of China; (3) the mammal fossils represent the "Ailuropoda-Stegodon" faunal unit which lived in southern China throughout the Pleistocene. ESR and U-series dating on animal teeth and a stalagmite derived from the same layer as the human teeth indicate two possible ages: 103±1.6 ka and 44±12.5 ka. In addition to other evidence presented here, it is believed that hominid occupation of the cave was likely around 100 ka. If this age is further substantiated, Huanglong Cave will be the first late Pleistocene hominid fossil site in China where anatomically modern humans lived about 100 ka. The human fossils and other related materials from Huanglong Cave will provide important information for research on the origin of modern Chinese.

  15. Spatial distributions of floating seaweeds in the East China Sea from late winter to early spring.

    Science.gov (United States)

    Mizuno, S; Ajisaka, T; Lahbib, S; Kokubu, Y; Alabsi, M N; Komatsu, T

    2014-01-01

    Floating seaweeds play an important role as a habitat for many animals accompanying or attaching to them in offshore waters. It was in 2000 that the first report described abundant distributions of floating seaweeds in offshore waters in the East China Sea in spring. Young individuals of the yellowtail Seriola quinqueradiata are captured for aquaculture purposes from floating seaweeds in the East China Sea. Therefore, a sound understanding of the distributions of floating seaweeds in the East China Sea is needed. Detailed information is especially important during the late winter to early spring, which corresponds to the juvenile period of the yellowtail. Thus, field surveys using R/V Tansei-Maru were conducted in the Japanese Exclusive Economic Zone in the East China Sea from late winter to early spring in 2010 and 2011. We obtained positions of the vessel by GPS and transversal distances from the vessel to a raft by visual observation. Distance sampling method (Thomas et al. 2010) was applied to estimation of floating seaweed densities (rafts km(-2)). Seaweed rafts were also randomly sampled using nets during the research cruises. In the East China Sea, seaweed rafts were distributed mainly on the continental shelf west of the Kuroshio, especially in waters between 26° N and 30° N. Collected rafts consisted of only one species, Sargassum horneri (Turner) C. Agardh. Taking into account surface currents and geographical distribution of S. horneri, it is estimated that these floating seaweeds originated from natural beds along the coast between mid and south China. Considering the approximate travel times, it is suggested that floating patches are colonized by yellowtails early on during their trips, i.e., close to the Chinese coast.

  16. Strong winter monsoon wind causes surface cooling over India and China in the Late Miocene

    Directory of Open Access Journals (Sweden)

    H. Tang

    2015-01-01

    Full Text Available Modern Asian winter monsoon characterised by the strong northwesterly wind in East Asia and northeasterly wind in South Asia, has a great impact on the surface temperature of the Asian continent. Its outbreak can result in significant cooling of the monsoon region. However, it is still unclear whether such an impact existed and is detectable in the deep past. In this study, we use temperature reconstructions from plant and mammal fossil data together with climate model results to examine the co-evolution of surface temperature and winter monsoon in the Late Miocene (11–5 Ma, when a significant change of the Asian monsoon system occurred. We find that a stronger-than-present winter monsoon wind might have existed in the Late Miocene due to the lower Asian orography, particularly the northern Tibetan Plateau and the mountains north of it. This can lead to a pronounced cooling in southern China and northern India, which counteracts the generally warmer conditions in the Late Miocene compared to present. The Late Miocene strong winter monsoon was characterised by a marked westerly component and primarily caused by a pressure anomaly between the Tibetan Plateau and Northern Eurasia, rather than by the gradient between the Siberian High and the Aleutian Low. As a result, the close association of surface temperature with winter monsoon strength on inter-annual scale as observed at present may not have established in the Late Miocene.

  17. Sedimentary-tectonic evolution from late Palaeozoic to Triassic in south of North China block

    Energy Technology Data Exchange (ETDEWEB)

    Chen, S. [University of Petroleum, Dongying (China). Dept of Resource

    2000-09-01

    The sedimentary facies of some typical profiles as in Hancheng, Jiyuan, Denfeng and Huainan, and the characteristic of regional palaeogeography in the south of North China block were researched. The result shows that the research area had an evolution from the epeiric sea to a lake basin during Palaeozoic to Triassic. This transition was controlled by the collision progeny of Qinling orogenic belt directly. The collision began along the Shangnan-Zhenping-Tongbai line, making the south of North China block compressed and subsided, and transferred from a structural high land to an epeiric sea in Late Carboniferous. The western part of North Qinling began to uplift and became a source of terrigenous clastic sediments to North China basin. In the Permian, the compression strengthened further and the North Qinling-North Huaiyang structural belt uplifted, making the epeiric sea transits to a marginal lake basin. In the Triassic, the Qinling orogenic belt uplifted rapidly and the large scale depression lake basin developed in its north side, and the centre of the basin also transferred to the orogenic belt in the Late Triassic. 7 refs., 4 figs.

  18. When the Chinese met the West: A Review of the Dissemination and Influence of Indian, Arabic and European Astronomy and Astrology in the Imperial China

    Science.gov (United States)

    Shi, Yunli

    2012-09-01

    In traditional Chinese ideology, the tianwen (Celestial Patterns) and lifa (Calendar) are important matters in the legitimization and maintenance of a regime. From very early times, astrology and astronomy became a crucial element in statecraft and establishments were always installed in the government to take care of these matters, which formed a tradition very scrupulously observed and documented by every Chinese dynasty without substantial interruption in thousands of years. A special system consisting of astrology and astronomy was developed and kept on developing on its own track. Such a long and well established tradition did not prevent China from receiving, though sometimes with reluctance and selection, arts and knowledge in astronomy and astrology from outside that might supplement and enhance the indigenous ones. This talk will give a survey on the history of the Chinese reception of astronomical and astrological knowledge from ``the West'', namely, India in the 7th to 10th centuries, Arabic area in the 13th to 15th centuries and Europe in the 16th to 18th centuries. Except tracing down the cultural impacts of the new knowledge from outside, I will concentrate on how the new knowledge was appropriated by Chinese governments, as well as by Chinese astronomers and astrologers.

  19. ["Imperial madness" - truth or legend?].

    Science.gov (United States)

    V Zerssen, D

    2011-03-01

    The notion of "imperial madness" was coined in the historical literature and belles-lettres of the 19th century. Around that time up to the first quarter of the 20th century, it was adopted by a few German psychiatrists. Two of them viewed "imperial madness" as ordinary forms of insanity which became excessive only due to reactions of the social environment. Another one, however, classified it as one of "mental borderland states" in between insanity and normality, although he conceived the final stage of the disorder as a paranoid one. In agreement with the historians he postulated that "imperial madness" resulted from unlimited power of predisposed rulers. In recent times the whole concept of "imperial madness" was referred to the realm of legends by historians of antiquity and other historically interested authors. Yet the existence of the phenomenon cannot be denied. Despite its rarity it has played and is still playing an important role with often catastrophic consequences in various cultures all over the world. Therefore, psychiatrists and other physicians as well as clinical psychologists should be acquainted with it. From a modern point of view, it is not a paranoid disorder but rather a syndrome of addiction-like behavioural excesses representing an intensification of a Hybris syndrome as described by Anglo-Saxon psychiatrists. According to the present authors' view, it should be classified nosologically as a chronic adjustment disorder. In this case, the underlying stresses need to be extended to situations of temptation (here: the temptation to abuse almost unlimited power). © Georg Thieme Verlag KG Stuttgart · New York.

  20. Space Agriculture, Tourism and Health - Lessons from British Imperial History

    Science.gov (United States)

    Sivier, D. J.

    Advocates of space commercialisation and colonisation have drawn on previous centuries' experience of the exploration and exploitation of terrestrial New Worlds. Although so far chiefly confined to the colonisation of the Americas and exploration of the Antarctic, a proper examination of the problems and solutions faced and found by the late 19th - early 20th century Jamaican tourist trade, mid-Victorian planter agriculturalists in Sri Lanka and the impact of climatic theories of health on early 20th century White colonists in Kenya and Rhodesia, can, if properly applied to today's conditions affecting modern space businesses, offer important insights to the psychological impact and aetiology of disease amongst future space colonists, and the success- ful establishment and management of tourism and agriculture in space. By following the precedents set by the imperial pioneers, it should be possible to apply their founding principles in these sectors successfully, while avoiding the pitfalls and excesses of terrestrial imperialism.

  1. OLDEST STEM TELEOSTEI FROM THE LATE LADINIAN (MIDDLE TRIASSIC OF SOUTHERN CHINA

    Directory of Open Access Journals (Sweden)

    ANDREA TINTORI

    2015-11-01

    Full Text Available The origin of the largest modern vertebrate group, the Teleostei, saw major refinements in the last decades, thanks to newly discovered and stratigraphically closely spaced Triassic Lagerstätten. Here we report the oldest Pholidophoriformes (stem teleosts that were collected during a large scale yet detailed excavation of Upper Ladinian (Middle Triassic marine deposits in Xingyi City, Guizhou Province, China. Taxonomic comparisons support the erection of a new pholidophorid genus, Malingichthys gen. nov., with two species. The new genus shows a partially fused skull roof, a preopercular bone with a hockey-stick shape and, for the first time in Pholidophoridae, supraneural elements. Most Triassic marine vertebrate clades (fishes and reptiles, Malingichthys included first emerged in the South China Block, with Late Ladinian most showing an important faunal transformation that was strengthened by our last findings. The material here described is about 2 million years older than the previous records for pholidophorids. 

  2. Rare earth elements stratigraphic significance in late Permian coal measure from Bijie City, Guizhou Province, China

    Institute of Scientific and Technical Information of China (English)

    WANG Qiang; YANG Ruidong; BAO Miao

    2008-01-01

    Rare earth elements (REEs) are good geological indicators. In order to understand REEs stratigraphic significance, REEs m Late Permian coal measure from Bijie City, western Guizhou Province, China were studied. The results showed that the contents of both light rare earth element (LREE) and ∑ REE were sharply increased in the boundary between Longtan Formation and Changxing Formation, which resulted from the gyration and discontinuity eruption of Emeishan basalt (REEs source) and frequent transgression-regression during forming coal. The coal measure and strata could be subdivided and correlate, and the sea-level change could be under stood by studying REEs content variation in coal measure.

  3. A basal alvarezsauroid theropod from the early Late Jurassic of Xinjiang, China.

    Science.gov (United States)

    Choiniere, Jonah N; Xu, Xing; Clark, James M; Forster, Catherine A; Guo, Yu; Han, Fenglu

    2010-01-29

    The fossil record of Jurassic theropod dinosaurs closely related to birds remains poor. A new theropod from the earliest Late Jurassic of western China represents the earliest diverging member of the enigmatic theropod group Alvarezsauroidea and confirms that this group is a basal member of Maniraptora, the clade containing birds and their closest theropod relatives. It extends the fossil record of Alvarezsauroidea by 63 million years and provides evidence for maniraptorans earlier in the fossil record than Archaeopteryx. The new taxon confirms extreme morphological convergence between birds and derived alvarezsauroids and illuminates incipient stages of the highly modified alvarezsaurid forelimb.

  4. Androecium of Archaefructus, the Late Jurassic Angiosperms from Western Liaoning, China

    Institute of Scientific and Technical Information of China (English)

    SUN Ge; ZHENG Shaolin; SUN Chunlin; SUN Yuewu; David L. DILCHER; MIAO Yuyan

    2002-01-01

    Androecium of the earliest known flowering plant Archaefructus liaoningensis was found from the Upper Jurassic Jianshangou Formation of western Liaoning, China. The androecium consists of numerous stamens bearing in pair on the reproductive axes below conduplicate carpels. The stamens are composed of a short filament and basifixed anther for each. Monosulcate pollen in situ are found from the anthers. The characters of the androecium reveals that Archaefructus are probably protandrous, and the paired stamens and monosulcate pollen appear to indicate that Archaefructus, as primitive angiosperms,might be derived from extinct seed -ferns during the Older Mesozoic. Archaefructus is considered Late Jurassic in age.

  5. Joanna Handlin Smith,The Art of Doing Good. Charity in Late MingChina

    OpenAIRE

    Laliberté, André

    2010-01-01

    Joanna Handlin Smith,The Art of Doing Good. Charity in Late MingChina,Berkeley, University of California Press, 2009, 406 p. Directrice du prestigieux Harvard Journal of Asiatic Studies, Joanna Handlin Smith a rassemblé dans cet ouvrage le fruit de plus de plus de deux décennies de recherche, les matériaux présentés dans cette monographie ayant déjà fait l’objet de publications dans les périodiques scientifiques Journal for Asian Studies et Journal for the Economic and Social History of the O...

  6. Joanna Handlin Smith, The Art of Doing Good: Charity in Late Ming China

    OpenAIRE

    Laliberté, André

    2010-01-01

    Joanna Handlin Smith, The Art of Doing Good: Charity in Late Ming China, Berkeley, University of California Press, 2009, 406 pp. Joanna Handlin Smith is chief editor of the prestigious Harvard Journal of Asiatic Studies. The material she has gathered together in this volume is the fruit of more than two decades of research, and has been published previously in academic journals such as the Journal for Asian Studies and the Journal for the Economic and Social History of the Orient, as well as ...

  7. Has the prediction of the South China Sea summer monsoon improved since the late 1970s?

    Science.gov (United States)

    Fan, Yi; Fan, Ke; Tian, Baoqiang

    2016-12-01

    Based on the evaluation of state-of-the-art coupled ocean-atmosphere general circulation models (CGCMs) from the ENSEMBLES (Ensemble-based Predictions of Climate Changes and Their Impacts) and DEMETER (Development of a European Multimodel Ensemble System for Seasonal to Interannual Prediction) projects, it is found that the prediction of the South China Sea summer monsoon (SCSSM) has improved since the late 1970s. These CGCMs show better skills in prediction of the atmospheric circulation and precipitation within the SCSSM domain during 1979-2005 than that during 1960-1978. Possible reasons for this improvement are investigated. First, the relationship between the SSTs over the tropical Pacific, North Pacific and tropical Indian Ocean, and SCSSM has intensified since the late 1970s. Meanwhile, the SCSSM-related SSTs, with their larger amplitude of interannual variability, have been better predicted. Moreover, the larger amplitude of the interannual variability of the SCSSM and improved initializations for CGCMs after the late 1970s contribute to the better prediction of the SCSSM. In addition, considering that the CGCMs have certain limitations in SCSSM rainfall prediction, we applied the year-to-year increment approach to these CGCMs from the DEMETER and ENSEMBLES projects to improve the prediction of SCSSM rainfall before and after the late 1970s.

  8. Late Cenozoic evolution of the East China continental margin: Insights from seismic, gravity, and magnetic analyses

    Science.gov (United States)

    Shang, Lu-Ning; Zhang, Xun-Hua; Jia, Yong-Gang; Han, Bo; Yang, Chuan-Sheng; Geng, Wei; Pang, Yu-Mao

    2017-02-01

    Seismic reflection profiles reveal the structural characteristics beneath the East China Sea shelf margin and the Okinawa Trough, and provide new constraints on the Late Cenozoic evolution of the East China continental margin. The Frontal Shelf Basin between the Taiwan-Sinzi Uplift and the trough axis occupies the western half of the Northern-Middle Okinawa Trough. In this basin, the Middle-Late Miocene sediments are confined to grabens or half-grabens dominated by listric faults, whereas the overlying Pliocene-Quaternary sequence is characterized by a uniform thickness and dense planar-type faults, suggesting that rifting of the Northern-Middle Okinawa Trough initiated during the Middle Miocene but slowed down during the earliest Pliocene. Since that time, the opening of the Okinawa Trough has been dominated by diffuse rifting. The Southern Okinawa Trough is predominately filled by Quaternary sediments, indicating that its back-arc rifting began during the earliest Pleistocene. Contractional structures identified in the pre-Quaternary sequence beneath the continental slope, along with an erosional Pleistocene-pre-Pleistocene unconformity in the Southern Okinawa Trough, demonstrate the existence of pre-rifting compression and uplifting in this region. We use this evidence and previously published results, to propose an evolutionary model of the East China continental margin during the Late Cenozoic. The Northern-Middle Okinawa Trough began rifting during the Middle Miocene on a paleo-uplift. The Luzon Arc initially impinged upon the Eurasian continental margin during the Late Miocene near the southeastern end of the Miyako Fault Belt and activated the proto-Taiwan Orogeny in today's Southern Okinawa Trough and adjacent regions. During the Late Miocene-Pliocene, the orogeny quickly propagated southwestward along with the west-northwest-moving Philippine Sea Plate. Subsequently, the rifting of the Southern Okinawa Trough was initiated during the earliest Pleistocene

  9. The Decadal Shift of the Summer Climate in the Late 1980s over Eastern China and Its Possible Causes

    Institute of Scientific and Technical Information of China (English)

    ZHANG Renhe; WU Bingyi; ZHAO Ping; HAN Jinping

    2008-01-01

    In this paper, it is pointed out that a notable decadal shift of the summer climate in eastern China occurred in the late 1980s. In association with this decadal climate shift, after the late 1980s more precipita-tion appeared in the southern region of eastern China (namely South China), the western Pacific subtropical high stretched farther westward with a larger south-north extent, and a strengthened anticyclone at 850 hPa appeared in the northwestern Pacific. The decadal climate shift of the summer precipitation in South China was accompanied with decadal changes of the Eurasian snow cover in boreal spring and sea surface temperature (SST) in western North Pacific in boreal summer in the late 1980s. After the late 1980s, the spring Eurasian snow cover apparently became less and the summer SST in western North Pacific increased obviously, which were well correlated with the increase of the South China precipitation. The physical pro-cesses are also investigated on how the summer precipitation in China was affected by the spring Eurasian snow cover and summer SST in western North Pacific. The change of the spring Eurasian snow cover could excite a wave-train in higher latitudes, which lasted from spring to summer. Because of the wave-train, an abnormal high appeared over North China and a weak depression over South China, leading to more precip-itation in South China. The increase of the summer SST in the western North Pacific reduced the land-sea thermal contrast and thus weakened the East Asian summer monsoon, also leading to more precipitation in South China.

  10. Dynamic simulations of the late MIS 3 transgressions in the East China Sea and southern Yellow Sea, China

    Institute of Scientific and Technical Information of China (English)

    YE Liangtao; YU Ge; LIAO Mengna; LI Yongfei

    2016-01-01

    Abundant evidences of higher sea levels from Jiangsu and Fujian coasts have proved a marine transgression event during 30–40 ka BP, suggesting that there was a stage with high sea level and a warm climate when ice sheets shrank in the Northern Hemisphere. The duration of 30–40 ka BP spanned a period in the late Marine Isotope Stage 3 (MIS 3) and was in nature an interstadial epoch during the Last Glacial period of the Quaternary. Different from the glacial period with a cold climate, this marine transgression considered as a penultimate higher sea level during the Quaternary remains a puzzle that why the evidence is contrary to the Quaternary glacial theory. It is important to understand sea level rise for these areas sensitively responding to the global changes in the future. To recognize the key issues on sea level changes, the eustatic sea level (HS) was defined as the glaciation-climate-forced sea levels, and the relative sea level change (HR) was defined as that a sea level record was preserved in sediment that experienced multiple secondary actions of land and sea effects. On the basis as defined above, we constructed multi-level models of climate-driven glacio-eustatic changes and land-sea systems. By integrating data sets from eight borehole cores and prescribing the boundary conditions, we simulated the changes of HS and HR in the East China Sea and southern Yellow Sea areas in the late MIS 3. The marine transgression strata from the borehole core data was identified at ca. 30 m below present sea level as a result of the collective influence of ice melting water, neotectonic subsidence, sediment compaction and terrestrial sediment filling since ca. 35 ka ago, whereas the simulated relative sea-levels turned out to be –26.3––29.9 m a.s.l. The small error involved in the simulation results of ±(2.5–4.5) m demonstrated the credibility of the results. Our results indicated that sea level change in the late MIS 3 was dominated by glacial effects

  11. Pattern and timing of late Cenozoic rapid exhumation and uplift of the Helan Mountain,China

    Institute of Scientific and Technical Information of China (English)

    2010-01-01

    The Helan Mountain, an intraplate deformation belt in the North China Craton, is located in the northern portion of the China North-South seismic belt, and at the northwestern margin of the Ordos Block. The Cenozoic deformation history of the Helan Mountain is characterized by extension along the eastern Helan Mountain fault (EHSF), resulting in the exhumation and uplift of the Helan Mountain, relative to the rifting of the adjacent Yinchuan Basin. Here we present new apatite fission track (AFT) data from several transects adjacent to the EHSF in the central and northern Helan Mountain. AFT ages from the northern Helan Mountain (Dawukou and Zhengyiguan transects) range from 10 Ma to 89 Ma, whereas AFT ages from the southern Helan Mountain (Suyukou transect) are greater than 71 Ma. The AFT data analysis reveals initiation of rapid uplift and exhumation of the Helan Mountain at 10–12 Ma. Additionally, a plot of the AFT ages versus their mean track length shows a distinctive "boomerang" pattern indicating that the Helan Mountain experienced a discrete phase of accelerated exhumation beginning at 10-12 Ma. Spatially, AFT samples systematically increase in age away from the EHSF and are consistent with late Cenozoic exhumation that was slow in the southwestern Helan Mountain and rapid in the northeastern Helan Mountain, as well more rapid adjacent to the EHSF and slower away from the EHSF. Obviously, the spatial distribution of late Cenozoic exhumation indicates that normal faulting of the EHSF is related to southwestward tilting and rapid exhumation of the Helan Mountain beginning at 10–12 Ma. The uplift and exhumation of the Helan Mountain was a response to the intensive extension of the northwestern margin of the Ordos Block in the late Cenozoic; this occurred under a regional extensional stress field oriented NW-SE along the Yinchuan-Jilantai-Hetao and the Weihe-Shanxi graben systems adjacent to the Ordos Block.

  12. Atenas, República Imperial

    OpenAIRE

    2015-01-01

    El presente texto intenta exponer los motivos de por qué Atenas, una vez convertida en Imperio, y pese a ciertas convulsiones internas, logró mantener viva la democracia en la ciudad. Es decir, de por qué a pesar del ejercicio de una dominación imperial en el exterior, que recurría a la violencia cuando era necesario incluso contra los propios aliados, la democracia ateniense subsistió: al principio, porque los éxitos facilitaron la integración de todas las clases sociales en el ámbito públic...

  13. Allogenic succession in Late Ordovician reefs from southeast China: a response to the Cathaysian orogeny

    Directory of Open Access Journals (Sweden)

    Qijian Li

    2015-02-01

    Full Text Available Several Late Ordovician (late Katian reef complexes are known from the border area of Jiangxi and Zhejiang provinces in southeast China. We studied two coral–stromatoporoid reefs exposed in the Xiazhen Formation at Zhuzhai (Yushan, Jiangxi. The reefs have a combined thickness of 7.4 m and are metazoan-dominated with most reef-builders in growth position. Stromatoporoids and tabulate corals constitute the framework of the reefs. Stromatoporoids (mostly Clathrodictyon dominate the first unit and show a vertical increase in proportion and dominance from the middle part to the top of the unit, whereas tabulate corals (dominated by Catenipora and Agetolites are the main reef-builders in the second unit where stromatoporoids are rare. We attribute this change to a greater tolerance of tabulate corals to turbidity, allowing them to thrive in the muddy facies of the upper unit. This facies change is probably related to the increasing terrestrial input from the northwestward expansion of the Cathaysian Land during the late Katian. The Cathaysian orogeny also led to a short-term exposure of the sea floor in the study area, which terminated the reef growth.

  14. Accounting for Impact at Imperial College London

    DEFF Research Database (Denmark)

    Perkmann, Markus; Fini, Riccardo; Ross, Jan-Michael

    We report findings of a study of academic engagement and commercialisation at Imperial College London. We detail the extent of collaboration with industry, consulting, patenting and entrepreneurship by Imperial academics, as well as individuals’ motivations and perceived barriers to engagement. T...

  15. Situated Interpretations of Nationalism, Imperialism, and Cosmopolitanism

    DEFF Research Database (Denmark)

    Zhang, Chenchen

    2014-01-01

    liberal nationalism and imperialism. This article seeks to complicate these theses by looking at the interpretations of nationalism, imperialism, and cosmopolitanism provided by Liang Qichao, one of the most influential Chinese intellectuals in early twentieth century, during his exile in Japan when...

  16. Mid-Late Miocene vegetation and environments in Southeast China: Insights from a marine palynological record in northwestern Taiwan

    Science.gov (United States)

    Hao, Xiu-dong; Weng, Chengyu; Huang, Chi-Yue; Ouyang, Xu-hong

    2017-05-01

    Taiwan Island represents the exposed accretionary prism developed by eastward subduction of South China Sea (SCS) oceanic lithosphere beneath the Philippine Sea Plate since the middle Miocene. There are many well-documented data about the biostratigraphic correlation, except for palynological studies. Here, we present a new palynological record of mid-Late Miocene deposits from the Chuhuangkeng section, Miaoli, northwestern Taiwan, which reveals a vegetation and paleoelevation reconstruction in Southeast China, during the Middle to Late Miocene, corresponding to the time interval of about 14.5-5.5 Ma. Most samples yielded well-preserved palynomorphs, and the palynological results suggest that the dominant vegetation was the mixed coniferous-broadleaved forests in the Coastal Mountains of Southeast China (CMSC) during the Mid-Late Miocene. Moreover, based on large amounts of Tsuga and Picea pollen, we hypothesized that a subalpine conifer forest then flourished in the CMSC, and the estimated maximum paleoelevation might be up to ∼3000 m above sea level (a.s.l.) during the Mid-Late Miocene, being 1000-1500 m higher than today. These findings offer a new perspective to comprehend the paleotopographic evolution of China and the source area of Taiwan's spruce forests. Additionally, the high abundance of Pinus, Tsuga, Picea pollen and fern spores also suggests an enhancement of the EASM during the Mid-Late Miocene.

  17. Linguistic Imperialism and Chinese Language and Culture Protection

    Institute of Scientific and Technical Information of China (English)

    曾杰

    2014-01-01

    Influenced by the English imperialism theory proposed by Danish linguist Robert Philipson,the rapid development and popularity of English in the whole world have aroused debates among English hegemony.Some scholars in China are much concerned about the hegemony’s threat to Chinese language and culture and raised the concept of language and culture protection.Nevertheless,the author maintain that while caring about the adverse impact caused by English hegemony,the Chinese language and culture need to be protected,meanwhile,al-inclusive attitude shal be adopted towards English and western culture to enhance the communication and interaction between Chinese and English languages and cultures.

  18. The Garden and the Jungle: Burnett, Kipling and the Nature of Imperial Childhood

    Science.gov (United States)

    Goodwin, Mary

    2011-01-01

    Imperial British India is the point of origin for protagonists in both Frances Hodgson Burnett's "The Secret Garden" (1911) and Rudyard Kipling's "The Jungle Books" (1894-1895), two influential children's stories in which late Victorian notions of childhood education and nature converge with those of national and imperial…

  19. Rehabilitation of the imperial examination system

    Institute of Scientific and Technical Information of China (English)

    Liu Haifeng

    2006-01-01

    Since the abolishment of the imperial examination system (the IES) in 1905,the system has been the target of severe criticism by most Chinese people.This paper is intended to clear up the misunderstanding of the IES in seven respects based on some ideas of rehabilitation of the IES over the past 100 years.In the author's opinion,the IES is actually not so contemptible as most people think,at least it is not a bad system.The examination system was an attempt to recruit men on the basis of merit rather than because of social position or political connections,which is a great invention of China.Although it was abolished,the method to select talents by means of examination has not yet been and cannot be exterminated,and it is still proper to be used in the present society.The IES with a 1,300-year history has rich experiences and valuable lessons,which have implications to various examination reforms.

  20. National ornament and the imperial masquerade

    Directory of Open Access Journals (Sweden)

    Nóra Veszprémi

    2015-12-01

    Full Text Available Review of Rebecca Houze, Textiles, Fashion, and Design Reform in Austria–Hungary before the First World War: Principles of Dress: Rebecca Houze’s book is a thoroughly researched and original study of the impact of design reform on textile production and fashion in Austria-Hungary in the late nineteenth and early twentieth century which centres its argument around the Bekleidungsprinzip (“principle of dress” put forward by Gottfried Semper. It discusses the role of newly founded applied arts museums, industrial exhibitions, the concept of “house industry,” and the upsurge of interest in folk crafts in this process, while also placing a strong emphasis on the role of women as producers of textiles. One of the main virtues of the book is its wide scope which manages to investigate endeavours informed by different and sometimes opposed national and imperial interests in their complicated interconnectedness. It is a pity that this broad perspective is narrowed down in the second part of the book which focuses on with turn-of-the-century Vienna and does not deal with modernist tendencies in Hungarian design. Nevertheless, this part of the book also provides a fascinating discussion of its own subject, and the monograph as a whole is a valuable contribution to its field of study.

  1. Regime shift of the South China Sea SST in the late 1990s

    Science.gov (United States)

    Thompson, Bijoy; Tkalich, Pavel; Malanotte-Rizzoli, Paola

    2017-03-01

    Decadal variability of the South China Sea (SCS) sea surface temperature (SST) during 1982-2014 is investigated using observations and ocean reanalysis datasets. The SCS SST shows an abrupt transition from a cold-to-warm regime in the late 1990s. Based on the long-term SST variability two epochs are defined, 1982-1996 and 2000-2014 as cold and warm regimes respectively, spanning on either side of the 1997-1999 SCS warming. Despite the occurrence of strong El Nino induced warming events, the SST anomalies tend to be negative in the cold regime. Conversely during the warm regime, the positive SST anomalies have dominated over the La Nina driven cooling events. The cold (warm) SST regime is marked by net heat gain (loss) by the SCS. The long-term variations of net surface heat flux are mainly driven by the latent heat flux anomalies while the short wave flux plays a secondary role. Low-frequency variability of the South China Sea throughflow (SCSTF) appears to be closely related to the SCS SST regime shift. The SCSTF shows reversing trends during the cold and warm epochs. The weakened SCSTF in the warm regime has promoted the SCS warming by limiting the outward flow of warm water from the SCS. Meanwhile, enhanced SCSTF during the cold regime acts as a cooling mechanism and lead to persistent negative SST anomalies. The change in trend of the SCSTF and SST regime shift coincides with the switching of pacific decadal oscillation from a warm to cold phase in the late 1990s.

  2. A Qualified Optimistic Analysis of Imperial Russia

    Directory of Open Access Journals (Sweden)

    Christine D. Worobec

    2016-10-01

    Full Text Available In his magnum opus on Russia’s imperial history B.N. Mironov characterizes himself as a positivist thinker who marshals impressive amounts of statistics and other types of hard evidence, and employs economic theory, sociological paradigms to understand Russian social structures and development, political analysis, anthropology, and at times psychology to Russia over the longue durée. With this arsenal at hand, he argues against Russian exceptionalism and identifies Russia instead as a typical European state. In so doing, he emphasizes Imperial Russia’s successes as a state, the social and economic foundations of which, he argues, did not cause revolution and attributes revolution to political causes. As he has tried to do previously, the author does not begin with the revolutions of the early twentieth century and largely does not read history backwards, but rather delineates Russia’s historical development within a robust comparative European context (occasionally broadening that context to include the United States. More specifically, B.N. Mironov charts Russia’s modernization through the creation of well-defined estates in the late eighteenth century and the subsequent breakdown of those estates in the post-reform period as a result of greater social mobility; gradual urbanization; industrialization; the beginnings of a demographic transformation; improvements in the standard of living; an increase in literacy; the development of a civil society; the spread of private property among all social groups; the growth of individualism; and the eventual establishment of the rule of law, all of which constitute the attributes of a modern European state. The author’s largely negative perceptions of the Russian peasants’ mentalité, however, sit uneasily with his claims about advancements in the countryside by the turn of the twentieth century. Equating peasants’ collectivism with authoritarianism and conflating it with the Bolshevik

  3. A toothed turtle from the Late Jurassic of China and the global biogeographic history of turtles.

    Science.gov (United States)

    Joyce, Walter G; Rabi, Márton; Clark, James M; Xu, Xing

    2016-10-28

    Turtles (Testudinata) are a successful lineage of vertebrates with about 350 extant species that inhabit all major oceans and landmasses with tropical to temperate climates. The rich fossil record of turtles documents the adaptation of various sub-lineages to a broad range of habitat preferences, but a synthetic biogeographic model is still lacking for the group. We herein describe a new species of fossil turtle from the Late Jurassic of Xinjiang, China, Sichuanchelys palatodentata sp. nov., that is highly unusual by plesiomorphically exhibiting palatal teeth. Phylogenetic analysis places the Late Jurassic Sichuanchelys palatodentata in a clade with the Late Cretaceous Mongolochelys efremovi outside crown group Testudines thereby establishing the prolonged presence of a previously unrecognized clade of turtles in Asia, herein named Sichuanchelyidae. In contrast to previous hypotheses, M. efremovi and Kallokibotion bajazidi are not found within Meiolaniformes, a clade that is here reinterpreted as being restricted to Gondwana. A revision of the global distribution of fossil and recent turtle reveals that the three primary lineages of derived, aquatic turtles, including the crown, Paracryptodira, Pan-Pleurodira, and Pan-Cryptodira can be traced back to the Middle Jurassic of Euramerica, Gondwana, and Asia, respectively, which resulted from the primary break up of Pangaea at that time. The two primary lineages of Pleurodira, Pan-Pelomedusoides and Pan-Chelidae, can similarly be traced back to the Cretaceous of northern and southern Gondwana, respectively, which were separated from one another by a large desert zone during that time. The primary divergence of crown turtles was therefore driven by vicariance to the primary freshwater aquatic habitat of these lineages. The temporally persistent lineages of basal turtles, Helochelydridae, Meiolaniformes, Sichuanchelyidae, can similarly be traced back to the Late Mesozoic of Euramerica, southern Gondwana, and Asia. Given

  4. Latisemenia longshania, gen. et sp. nov., a new Late Devonian seed plant from China.

    Science.gov (United States)

    Wang, De-Ming; Basinger, James F; Huang, Pu; Liu, Le; Xue, Jin-Zhuang; Meng, Mei-Cen; Zhang, Ying-Ying; Deng, Zhen-Zhen

    2015-10-22

    The earliest known ovules in the Late Devonian (Famennian) are borne terminally on fertile branches and are typically enclosed in a cupule. Among these ovules are some that have terete integumentary lobes with little or no fusion. Here, we report a new taxon, Latisemenia longshania, from the Famennian of South China, which bears cupulate ovules that are terminal as well as opposite on the fertile axis. Each ovule has four broad integumentary lobes, which are extensively fused to each other and also to the nucellus. The cupule is uniovulate, and the five flattened cupule segments of each terminal ovule are elongate cuneate and shorter than the ovule. Associated but not attached pinnules are laminate and Sphenopteris-like, with an entire or lobate margin. Latisemenia is the earliest known plant with ovules borne on the side of the fertile axis and may foreshadow the diverse ovule arrangements found among younger seed plant lineages that emerge in the Carboniferous. Following the telome theory, Latisemenia demonstrates derived features in both ovules and cupules, and the shape and fusion of integumentary lobes suggest effective pollination and protection to the nucellus. Along with other recent discoveries from China, Latisemenia extends the palaeogeographic range of the earliest seed plants. © 2015 The Author(s).

  5. Environmental and Archaeological Implications of a Late Quaternary Palynological Sequence, Poyang Lake, Southern China

    Science.gov (United States)

    Jiang, Qinhua; Piperno, Dolores R.

    1999-09-01

    Paleoecological data from Poyang Lake, southern China, indicate that significant natural and human-induced vegetational changes have occurred during the Late Quaternary in the Middle Yangtze River valley, the likely location of rice (Oryza sativa L.) domestication. During the late Pleistocene (from ca. 12,830 to ca. 10,500 yr B.P.), the climate was cooler and drier than today's. The subtropical, mixed deciduous-evergreen broad-leaved forest which constitutes the modern, potential vegetation was reduced and herbaceous vegetative cover expanded. A hiatus in sedimentation occurred in Poyang Lake, beginning sometime after ca. 10,500 yr B.P. and lasting until the middle Holocene (ca. 4000 yr B.P.). At ca. 4000 yr B.P., the regional vegetation was a diverse, broad-leaved forest dominated by many of the same arboreal elements (e.g., Quercus, Castanopsis, Liquidambar) that grow in the area today. A significant reduction of arboreal pollen and an increase of herbaceous pollen at ca. 2000 yr B.P. probably reflect human influence on the vegetation and the expansion of intensive rice agriculture into the dryland forests near the river valleys.

  6. Taxonomy and Stratigraphy of Late Mesozoic Anurans and Urodeles from China

    Institute of Scientific and Technical Information of China (English)

    WANG Yuan

    2004-01-01

    Three anurans (Callobatrachus sanyanensis, Liaobatrachus grabaui, Mesophryne beipiaoensis) and six urodeles (Laccotriton subsolanus, Liaoxitriton zhongjiani, Jeholotriton paradoxus, Sinerpeton fengshanensis,Chunerpeton tianyiensis, Liaoxitriton daohugouensis) are reported from the late Mesozoic tuff-interbedded lacustrine deposits (mostly of the Jehol Group) in northeastern China. They document the first discovery of Chinese Mesozoic lissamphibians, and their old geological age, superb preservation condition, and large taxonomic diversity are unique compared with other findings worldwide. The anurans occupy a higher evolutionary position than typical Jurassic taxa,supporting a post-Late Jurassic age of the fossil horizons. The urodeles all have unicapitate ribs, suggesting an evolutionary grade at the cryptobranchoid level, and are advanced in osteological features over non-urodeles from the Middle and Upper Jurassic in England and Central Asia. Some urodeles (Jeholotriton and Chunerpeton) exhibit neotenic features, representing the earliest occurrence among such findings. Six fossil horizons are recognized for the known Chinese Mesozoic anurans and urodeles: the Daohugou fossil bed, the Dabeigou Formation, the Lujiatun Bed,Jianshangou Bed and Dawangzhangzi Bed of the Yixian Formation, and the Jiufotang Formation. As implied from the osteological and phylogenetical studies, the geological age of these anurans and urodeles is the Early Cretaceous.

  7. No Red River capture since the late Oligocene: Geochemical evidence from the Northwestern South China Sea

    Science.gov (United States)

    Zhao, Meng; Shao, Lei; Liang, Jianshe; Li, Qianyu

    2015-12-01

    Rare earth elements (REE) in the sediment samples of six industrial wells from the Yinggehai-Song Hong Basin in the Northwestern South China Sea were analyzed and compared with the detrital zircon U-Pb data from earlier studies to extrapolate sediment provenance. The results reveal that the Red River (Song Hong River), Hainan Island and Central Vietnam have been the main provenances of the Yinggehai-Song Hong Basin since the late Oligocene. The Red River has been supplying sediments with positive Eu anomalies from basic-ultrabasic metamorphic and volcanic parent rocks to most parts of the basin, while Hainan Island has delivered sediments with negative Eu anomalies from granitic and sedimentary parent rocks to the eastern slope area of the basin. The progradational downlap structures in the seismic profiles also support the finding that the sediment supply is mainly from the Red River and from Hainan Island. The metamorphic rocks, which are widespread within the Red River drainage, not only provided high volumes of sediments to the basin but also contributed to the positive Eu anomalies observed. Because their REE and U-Pb signatures are similar to those of the Red River source, the metamorphic and igneous rocks of the Song Ma Suture Zone, Kontum Massif, and Jinghong area were probably parts of a large basic provenance region before being separated by strike-slip movements along the Ailao Shan-Red River shear zone. Furthermore, our results indicate that the Red River drainage area has been relatively stable since the late Oligocene. Therefore, if a drainage capture from the Red River occurred, it is likely to have taken place before the late Oligocene.

  8. Fluvial responses to late Quaternary climate change in the Shiyang River drainage system, western China

    Science.gov (United States)

    Gao, Hongshan; Li, Zongmeng; Pan, Baotian; Liu, Fenliang; Liu, Xiaopeng

    2016-04-01

    As a drainage system located in arid western China, the Shiyang River, combined with considerable fluvial strata and landform information, provides an environmental context within which to investigate fluvial responses to late Quaternary climate change. Sedimentological analysis and optically stimulated luminescence (OSL) dating enabled us to reconstruct the processes and fluvial styles of three sedimentary sequences of the Shagou and Hongshui rivers in the Shiyang drainage system. Our results present a variety of river behaviors during the late Quaternary in these areas. In the upstream Shiyang River, Zhangjiadazhuang (ZJDZ) profile of the Shagou was dominated by aggradation and a meandering channel pattern at 10.6-4.2 ka, while a noticeable channel incision occurred at ~ 4.2 ka followed by lateral channel migration. In the downstream Shiyang River, Datugou (DTG) profile of the Hongshui was an aggrading meandering river from 39.7 to 7.2 ka while channel incision occurred at 7.2 ka. Another downstream profile, Wudunwan (WDW) of the Hongshui was also characterized by aggradation from 22.4 to 4.8 ka; however, its channel pattern shifted from braided to meandering at ~ 13 ka. A discernable downcutting event occurred at ~ 4.8 ka, followed by three channel aggradation and incision episodes prior to 1.8 ka. The last 1.8 ka has been characterized by modern channel and floodplain development. The fluvial processes and styles investigated have a close correlation with late Quaternary climate change in the Shiyang River drainage. During cold phases, the WDW reach was dominated by aggradation with a braided channel pattern. During warm phases, the rivers that we investigated were also characterized by aggradation but with meandering channel patterns. Channel incision events and changes of fluvial style occurred mainly during climate transitions.

  9. [Kyongsong Imperial University Medical College].

    Science.gov (United States)

    Kee, C D

    1992-01-01

    Japan annexed Korea in 1910 and with the promulgation of the Chosen Kyoyuk Ryong (the Korea Education Decree) in 1911, it began to conduct education for the Korean people. However, this was only a matter of formality and a policy for liquidating the spirit of the Korean people. It finally resulted in the uprising of March 1, 1919 of the Korean people that has a cultural tradition of a high level. This event served as a cause of widely spread censure among the Korean people as well as the people of the whole world. Even in Japan voice of criticism rose high. Such being the situation, Japan amended the Korean educational law under the pretext of shifting to a so-called civil-rule policy. The Japanese authorities adopted the same educational system as was practiced in Japan proper, for primary and middle school education. As for higher education, they placed under a strict control the educational facilities already established by Korean people and foreign missionaries, suppressing even minor expansions of existing facilities. However, the movement by some Korean educators to establish a private university and efforts by some missionaries to integrate the existing educational organizations into a university made it inevitable for the Japanese authorities to set up a university of their own in Korea. Thus, they hurriedly established the Kyonsong Imperial University in which was included a medical college that was an indispensable organization for colonial education. They professed that the medical college was established for the purpose of providing equal opportunities and privileges to Korean and Japanese students, but, on the contrary, the operation of the college was done strictly under their colonial policy. The system of the Kyongsong Imperial University was enforced acording to the Japanese Imperial University Law, and all the faculty members and the administratial officials were Japanese. As for Koreans, a few graduates of the university was named nonpaid deputy

  10. [The Constantinople Imperial Bacteriology Institute].

    Science.gov (United States)

    Huet, M

    2000-01-01

    The Constantinople Imperial Bacteriology Institute (CIBI) allowed the development of a common medical effort between France and Turkey at a time when the main European powers were competing to have an influence on the Ottoman Empire. In 1887, Turkey sent Zoreos Pacha, a medical doctor, to Paris to learn anti-rabies immunization techniques, and he started a rabies control institute after his coming back. In 1893, a cholera epidemic in Constantinople was vanquished by A. Chantemesse, sent by Pasteur, and France was allowed to start another microbiologic Institute. The first director of this Constantinople Imperial Bacteriology Institute was Maurice Nicolle. A brillant man, but suffering from a lack of diplomacy; he encountered numerous difficulties and regularly threatened to turn in his resignation. His successor, Paul Remlinger, arrived in 1900. His main research topic was rabies, and he became later a world-class expert on the subject. His position was taken over in 1911 by Paul-Louis Simond, unjustly forgotten nowadays despite his major discovery in 1898 showing that the plague was transmitted by ratfleas. The next director was a veterinary doctor, P. Forgeot, but his tenure was cut short by World War I, and he was the last French director of the CIBI. Since that time, Turkey has felt some gratitude towards France for its medical efforts. It organized in 1957 in Istambul a very congenial celebration for the 70th anniversary of the Rabies Control Institute, which numerous Pasteur Institute alumni attended. There is a clear contrast between the CIBI, the target of many intrigues and hostile maneuvers, and the North African Pasteur Institutes, which were making crucial discoveries during the same period. This contrast was mostly due to the absolute power of the Sultan, who would arbitrarily oppose some directors decisions, whereas the French government allowed the balanced growth of the Pasteur Institutes in territories under his control.

  11. Globalization, Imperialism and Christianity: The Nigerian ...

    African Journals Online (AJOL)

    FIRST LADY

    of imperialist domination which modern globalization manifest in Christian religion in ... as we study the effects of imperialism and globalization on these churches. ... country's power and influence in the world through political relations or.

  12. Imperial County geothermal development annual meeting: summary

    Energy Technology Data Exchange (ETDEWEB)

    1983-01-01

    All phases of current geothermal development in Imperial County are discussed and future plans for development are reviewed. Topics covered include: Heber status update, Heber binary project, direct geothermal use for high-fructose corn sweetener production, update on county planning activities, Brawley and Salton Sea facility status, status of Imperial County projects, status of South Brawley Prospect 1983, Niland geothermal energy program, recent and pending changes in federal procedures/organizations, plant indicators of geothermal fluid on East Mesa, state lands activities in Imperial County, environmental interests in Imperial County, offshore exploration, strategic metals in geothermal fluids rebuilding of East Mesa Power Plant, direct use geothermal potential for Calipatria industrial Park, the Audubon Society case, status report of the Cerro Prieto geothermal field, East Brawley Prospect, and precision gravity survey at Heber and Cerro Prieto geothermal fields. (MHR)

  13. Imperial College Alumni Association in Switzerland

    CERN Multimedia

    2003-01-01

    Are you a graduate of Imperial College London? If so, you might be interested in its new Swiss alumni association for graduate engineers and scientists. The aim of the founder members is to create a network of the several hundred graduates of Imperial College working at CERN, in Geneva, Lausanne and Zurich with a view to organising social and scientific events, informing members of the studies and research done by Imperial College, setting up a link between the College and Swiss academic institutes and, of course, building up an alumni directory. Membership applications and requests for further information should be sent to: Imperial College Alumni (ICA) - Swiss chapter Case Postale CH-1015 Lausanne Tel. : + 41 22 794 57 94 Fax : + 41 22 794 28 14 Email : imperialcollegeswissalumni@epfl.ch

  14. Accounting for Impact at Imperial College London

    DEFF Research Database (Denmark)

    Perkmann, Markus; Fini, Riccardo; Ross, Jan-Michael

    We report findings of a study of academic engagement and commercialisation at Imperial College London. We detail the extent of collaboration with industry, consulting, patenting and entrepreneurship by Imperial academics, as well as individuals’ motivations and perceived barriers to engagement. T....... The data stems from archival records held by the College, complemented by external databases, and a survey conducted among all academic staff in 2013....

  15. Validation of Late Season Cornstalk Nitrate Test under Different Natural and Social Environments for Better Fertilizer Management in China

    Directory of Open Access Journals (Sweden)

    Guangwei Huang

    2014-01-01

    Full Text Available While the current food security is fulfilled in China, the substantial nitrogen fertilizer use has caused many far-reaching environmental problems. Therefore, reforming the fertilizer management is the key toward sustainable agriculture for 1.3 billion people. The present study is intended to test the applicability of a nitrogen fertilizer management approach for corn production developed in U.S. to regions with different climates in China. Through field work, it was found that the so-called Late Season Cornstalk Nitrate Test approach may have to be adapted to dry continental climate and irrigation water conditions, but meanwhile appeared workable under sub-humid warm temperate continental monsoon climate in China. A hypothesis was made to explain the findings and a simple cure was suggested. Moreover, the importance of applying this approach to China was discussed in relation to GHG emission reduction and national fertilizer subsidy policy. Finally, a new fertilizer management scheme was proposed.

  16. Small mammal tooth enamel carbon isotope record of C4 grasses in late Neogene China

    Science.gov (United States)

    Arppe, Laura; Kaakinen, Anu; Passey, Benjamin H.; Zhang, Zhaoqun; Fortelius, Mikael

    2015-10-01

    The spatiotemporal pattern of the late Cenozoic spread of C4 vegetation is an important indicator of environmental change that is intertwined with the uplift of the Himalaya and Tibetan Plateau, and the development of the East Asian monsoons. To explore the spread of C4 vegetation in China and shed new light on regional climatic evolution, we measured δ13C values of more than 200 small mammal teeth (primarily rodents and lagomorphs) using a laser ablation isotope ratio mass spectrometry approach. Small mammals are highly sensitive indicators of their environment because they have limited spatial ranges and because they have minimal time-averaging of carbon isotope signatures of dietary components. The specimens originate from four classic Late Miocene fossil localities, Lufeng, Yuanmou, Lingtai, and Ertemte, along a southwest-northeast transect from Yunnan Province to Inner Mongolia. In Yunnan (Lufeng, Yuanmou) and on the Loess Plateau (Lingtai), the small mammal δ13C values record nearly pure C3 ecosystems, and mixed but C3-based ecosystems, respectively, in agreement with previous studies based on carbon isotopes of large herbivores and soil carbonates. In Inner Mongolia, the micromammalian tooth enamel δ13C record picks up the presence of C4 vegetation where large mammal samples do not, indicating a mixed yet C3-dominated ecosystem at ~ 6 Ma. As a whole, the results support a scenario of northward increasing C4 grass abundance in a pattern that mirrors northward decreasing precipitation of the summer monsoon system. The results highlight differences between large and small mammals as indicators of C4 vegetation in ancient ecosystems, particularly the ability of small mammal δ13C values to detect the presence of minor components of the vegetation structure.

  17. Late Presentation of HIV Infection: Prevalence, Trends, and the Role of HIV Testing Strategies in Guangzhou, China, 2008–2013

    Directory of Open Access Journals (Sweden)

    Weibin Cheng

    2016-01-01

    Full Text Available Background. The prevalence, trends, and the role of different HIV testing strategies in late presentation of HIV infection in China were unknown. Methods. Data of newly reported HIV cases in Guangzhou between 2008 and 2013 was analyzed to examine the prevalence, trends, and characteristics of late presentation of HIV infection by three types of HIV testing strategies. Results. Overall, 53.2% (1412/2653 and 27.3% (724/2653 met the criteria of late presentation and presentation with advanced HIV disease. The overall trend of late presentation of HIV infection within the study period was declining. Late presentation was 62.9% in 2008 and dropped to 43.3% in 2013 (P<0.001; presentation with advanced HIV disease was 40.3% in 2008 and dropped to 15.2% in 2013 (P<0.001. Of the three testing strategies, PITC presented higher odds of both late presentation [AOR (95% CI: PITC versus VCT: 1.37 (1.09, 1.73; PITC versus MHT: 3.09 (2.16, 4.42] and presentation with advanced HIV disease [AOR (95% CI: PITC versus VCT: 1.65 (1.29, 2.11; PITC versus MHT: 13.14 (8.47, 20.39]. Conclusions. Although the late presentation of HIV infection was declining, it was still high in Guangzhou. The worse situation among PITC cases urges the policy adjustment in medical settings to increase early HIV diagnosis.

  18. Pliocene Invertebrates From the Travertine Point Outcrop of the Imperial Formation, Imperial County, California

    Science.gov (United States)

    Powell, Charles L.

    2008-01-01

    Forty-four invertebrate taxa, including one coral, 40 mollusks (30 bivalves and 10 gastropods), and three echinoids are recognized from a thin marine interval of the Imperial Formation near Travertine Point, Imperial County, California. The Travertine Point outcrop lies about midway between exposures of the Imperial Formation around Palm Springs, Riverside County, and exposures centered at Coyote Mountain in Imperial and San Diego Counties. Based on faunal comparisons, the Travertine Point outcrop corresponds to the Imperial and San Diego outcrops. The Travertine Point fauna is inferred to have lived in subtropical to tropical waters at littoral to inner sublittorial (<50 m) water depths. Coral and molluscan species from the Travertine Point outcrop indicate a Pliocene age. Two extant bivalve mollusks present have not previously been reported as fossils Anadara reinharti and forms questionably referred to Dosinia semiobliterata.

  19. New ommatids from the Late Jurassic of western Liaoning, China (Coleoptera: Archostemata)

    Institute of Scientific and Technical Information of China (English)

    JING-JINGTAN; DONGREN; MINGLIU

    2005-01-01

    A new genus Amblomma gen. nov. of fossil beetles is erected and can be assignedto the family Ommatidae because its two procoxal cavities are contiguous and the articulations of the abdominal ventrites are abutting. The new genus is similar to Zygadenia Handlirsch, 1906 (=Notocupes Ponomarenko, 1964), Tetraphalerus Waterhouse, 1901,Rhobdocupes Ponomarenko, 1966 and Sinocupes Lin, 1976, but can be distinguished from other genera according to the following characters: the second segment of antennae is shorterthan the third one in length; the posterior tarsi with the basal segment is obviously shorter than the three following taken together in length; the antennae reach the posterior ridge of prothroax in length, and the sides of the prothroax with serrulate margin. Four new species of the new genus are described and figured: Amblomma psilata gen. et sp. nov., Amblomma rudis gen. et sp. nov., Amblomma epicharis gen. et sp. nov., and Amblomma stabilis gen. etsp. nov. A key to species within this new genus is provided. All the specimens are collected from the Late Jurassic Yixian Formation of western Liaoning and are now housed in the College of Life Science, Capital Normal University, Beijing, China.

  20. The late Paleoproterozoic extension event:aulacogens and dyke Swarms in the North China craton

    Institute of Scientific and Technical Information of China (English)

    2006-01-01

    The extension structures and tectonic implication in the North China Craton (NCC) are discussed in this paper based on the mafic dyke swarms and geochronology, combining with the geochronology of aulacogens. The late Paleoproterozoic time is the important turning point in the Precambrian evolution of the NCC. The extension system (e. g. aulacogens and dyke swarms) is widespread in the NCC, which marks the carbonization of the NCC with the rigid characteristic similar to the modern plate. The paleostress field modeling suggests that the dyke swarms and aulacogens are arogenic extension marking the start of the supercontinent, not synorogenic and postorogenic extension. The mafic dyke swarms in the NCC mainly ranged from 1.83 to 1.77 Ga. The extension of the NCC is very limited brittle extension, the average extension ratio is only 0.35 % given by mafic dyke swarms extension calculation, so most of extension in the NCC is contributed by the aulacogens. The mafic dyke swarms are related with the aulacogens in the origin.

  1. Genetic relationships between swamp microenvironment and sulfur distribution of the Late Paleozoic coals in North China

    Institute of Scientific and Technical Information of China (English)

    汤达祯; 杨起; 周春光; 康西栋; 刘大锰; 黄文辉

    2001-01-01

    The genetic relationships between microenvironment of the Late Paleozoic peat-forming swamp and the sulfur contents of coal in North China have been studied by using coal-facies parameters involving gelification degree, tissue preservation index, vegetation index, transportation index, groundwater influence index, water medium indicator and swamp type index, etc. Among the various controlling factors of swamp microenvironment, swamp water medium elaborates a dominant action to sulfur accumulation in the marine-influenced coals; while coal-forming plant type, hydrodynamic state and water covering depth are more important to sulfur accumulation in the fresh water-influenced coals. Geological fractionation of sulfur isotopes reflects that sulfur accumulation experienced multi-stages evolution. Pyrite sulfurs formed earlier than organic sulfur and the sulfur isotopic d 34Sp shows lower values than organic sulfur isotopic d 34So. In the brine-influenced coals, sulfur accumulation processed relatively a long time span, the distribution of sulfur isotopes dispersed,and the coals are provided with high sulfur contents. In the fresh-water-influenced coals, sulfur accumulation occurred mainly at the syngenetic-penesyngenetic stage and the early diagenetic stage, and the total sulfur is lower and mainly composed of organic sulfur.

  2. Geochemistry of the barkinite liptobiolith (Late Permian) from the Jinshan Mine, Anhui Province, China.

    Science.gov (United States)

    Sun, Yuzhuang; Lin, Mingyue; Qin, Peng; Zhao, Cunliang; Jin, Kankun

    2007-02-01

    This paper discusses the geochemistry and mineralogy of the barkinite liptobiolith of the Late Permian age from the Jinshan Mine, Guangde County, Anhui Province, China. Samples were examined using inductively coupled plasma-mass spectroscopy, X-ray fluorescence, cold-vapor atomic absorption spectrometry, ion-selective electrode, sequential chemical extraction, scanning electron microscopy equipped with energy-dispersive X-ray, and optical microscopy. The coal is a medium-ash and high-sulfur resource. Minerals in the coal are composed of kaolinite, pyrite, calcite, and quartz. Pyrite and calcite are derived from seawater during peat accumulation. Quartz in the coal is of authigenic origin. Part of the kaolinite is from a land-source region, and part occurs as cell-fillings and is of authigenic origin. The results also indicate that the barkinite liptobiolith contains some toxic elements in high concentrations. Elements including Li, Be, Si, Sc, Ti, V, Cr, Fe, Ga, Se, Y, Zr, Mo, the rare earth elements (REEs), W, Hg, Tl, Pb, Th, and U in the coals are enriched in the barkinite liptobiolith. Results of sequential chemical extraction showed that Li, Sc, Ti, Cr, Y, Zr, REEs, and Th in the coal mainly occur as silicates, while Be and W are related to organic matter. Pyrite is the dominant source of S, Mo, Hg, Tl, and Pb. Gallium only occurs in silicate, and U and V occur both in organic and silicate associations.

  3. On Geodynamic Evolution of Simao Region (Southwestern Yunnan, China) during Late Paleozoic and Triassic

    Institute of Scientific and Technical Information of China (English)

    2001-01-01

    Over the last years, the Simao region, southwestern Yunnan, China, turned out to be a very promising target to elucidate plate-tectonic processes around the Permian-Triassic boundary within the Tethyan domain of Asia. New data from this area reveal that Upper Paleozoic compressional deformations occurred along the Lancangjiang and in areas to the east. Along Lancangjiang, an angular unconformity is exposed, which separates quartz-phyllites-formed during a Carboniferous tectono-metamorphic event-from Triassic red beds to roofing rhyolites. The acidic volcanics were often said to be remnants of a volcanic arc that was active during the Triassic subduction and closure of an oceanic realm along the Lancangjiang zone. According to our new data, however, these volcanics indicate most probably an Upper Triassic stage of rifting. In the Yunxian anticline (NW of Simao), an angular unconformity of intra-Permian age is exposed where Carboniferous to lower Middle Permian strata, which were deposited in a rather deep basin, are unconformably overlain by a shallow marine sequence of upper Middle to Upper Permian sediments. The angular unconformity is of the same age as the syn-orogenous sediments filst described and dated from the Phetchabun region in Thailand and hence a convincing argument for a Late Variscan orogeny forming an extensive zone of mountain-building that can be traced through the central parts of mainland Southeast-Asia.``

  4. Redescription of Cobitis longipectoralis Zhou, 1992 (Cypriniformes: Cobitidae) from late early Miocene of East China

    Institute of Scientific and Technical Information of China (English)

    CHANG; Mee-Mann

    2010-01-01

    Here we revise a fossil cobitid species ■Cobitis longipectoralis Zhou, 1992, based mainly on a well-preserved specimen collected recently from the taxon’s type locality of the late early Miocene of Shanwang, Shandong Province, East China. The new specimen, along with those collected by Zhou, enables us to provide an emended diagnosis and more detailed description of the species by focusing on the characters such as the structures of the suborbital spine and the presence and shape of the lamina circularis at the base of the second pectoral fin ray in adult males, the presence of a frontoparietal fontanelle, and a quad- rate-metapterygoid fenestra, etc. The long pectoral fin, initially considered by Zhou as the most important character of the spe- cies, however, turns out to be not diagnostic for the species. ■Cobitis longipectoralis Zhou, 1992 is not only the most informative and best-preserved early cobitid fossil known thus far but also the only and earliest cobitid fossil from East Asia.

  5. Geochemistry of the barkinite liptobiolith (Late Permian) from the Jinshan Mine, Anhui Province, China

    Energy Technology Data Exchange (ETDEWEB)

    Sun, Y.Z.; Lin, M.Y.; Qin, P.; Zhao, C.L.; Jin, K.K. [Hebei University of Engineering, Handan (China)

    2007-02-15

    This paper discusses the geochemistry and mineralogy of the barkinite liptobiolith of the Late Permian age from the Jinshan Mine, Guangde County, Anhui Province, China. Samples were examined using inductively coupled plasma-mass spectroscopy, X-ray fluorescence, cold-vapor atomic absorption spectrometry, ion-selective electrode, sequential chemical extraction, scanning electron microscopy equipped with energy-dispersive X-ray, and optical microscopy. The coal is a medium-ash and high-sulfur resource. Minerals in the coal are composed of kaolinite, pyrite, calcite, and quartz. Pyrite and calcite are derived from seawater during peat accumulation. Quartz in the coal is of authigenic origin. Part of the kaolinite is from a land-source region, and part occurs as cell-fillings and is of authigenic origin. The results also indicate that the barkinite liptobiolith contains some toxic elements in high concentrations. Elements including Li, Be, Si, Sc, Ti, V, Cr, Fe, Ga, Se, Y, Zr, Mo, the rare earth elements (REEs), W, Hg, Tl, Pb, Th, and U in the coals are enriched in the barkinite liptobiolith. Results of sequential chemical extraction showed that Li, Sc, Ti, Cr, Y, Zr, REEs, and Th in the coal mainly occur as silicates, while Be and W are related to organic matter. Pyrite is the dominant source of S, Mo, Hg, Tl, and Pb. Gallium only occurs in silicate, and U and V occur both in organic and silicate associations.

  6. Soft-sediment deformation structures in cores from lacustrine slurry deposits of the Late Triassic Yanchang Fm. (central China

    Directory of Open Access Journals (Sweden)

    Yang Renchao

    2016-09-01

    Full Text Available The fine-grained autochthonous sedimentation in the deep part of a Late Triassic lake was frequently interrupted by gravity-induced mass flows. Some of these mass flows were so rich in water that they must have represented slurries. This can be deduced from the soft-sediment deformation structures that abound in cores from these lacustrine deposits which constitute the Yanchang Fm., which is present in the Ordos Basin (central China.

  7. Discovery of the Middle-Late Triassic elasmobranch ichthyoliths from the Guanling area, Guizhou, SW China

    Institute of Scientific and Technical Information of China (English)

    翟裕生

    2003-01-01

    Abundant Middle-Late Triassic (Ladinian-Carnian) elasmobranch ichthyoliths (microscopic shark dermaldenticles and teeth) from the Zhuganpo and Xiaowa Formations in the Guanling area, Guizhou Province, south-western China, are described and illustrated. The fauna includes a single tooth possibly belonging to Hybodontidaeand 7 paragenera and paraspecies of dermal denticles, i.e.: Lobaticorona cf. floriditurris, Sacrisubcorona cf. circaba-sis, Glabrisubcorona cf. arduidevexa, Parvicorona dacrysulca n. gen. n. sp. s. f., Annulicorona pyramidalis n. gen.n. sp. s. f., and new (?) paragenera A and B. This is the first time that shark dermal denticles are reported fromthe Metapolygnathus polygnathiformis M. nodosus conodont zones. The application of microfossils of chondrichthyesin the strafgraphic division of the Triassic and the intercontinental correlation of Triassic chondrichthyes in south-western China and those in equivalent strata in North America are also discussed.%应用Johns等(1997)的形态分类系统,对首次报道出现于贵州关岭地区中上三叠统的软骨鱼类的微体化石进行了初步研究,描述了其中的1个牙齿化石(可能属于弓鲛鲨科的)和7个鳞片类化石的形态属种,其中包括两个鳞片类化石的新属种,即Lobaticorona cf. floriditurris,Sacrisubcorona cf. circabasis,Glabrisubcorona cf. arduidevexa,Parvi-corona dacrysulca n.gen.et n.sp s f,Annulicorona pyramidalis n.gen.et.n.sp s f,new(?)paragenera A和new(?)paragenera B.还初步探讨了软骨鱼类微体化石在三叠纪地层划分中的应用,以及中国西南部三叠纪软骨鱼类与北荚相当地层中软骨鱼类的洲际对比.

  8. Crust-Mantle Interaction in Dabie Orogenic Belt, Central China: Geochemical Evidence from Late Cretaceous Basalts

    Institute of Scientific and Technical Information of China (English)

    匡少平; 张本仁

    2003-01-01

    It has been suggested that eclogites in the Dabie orogenic belt are exhumation prod-ucts, which had subducted into the deep-seated mantle and undergone ultra-high pressure meta-morphism during the Triassic. But no direct evidence supports this process except the calculatedp-T conditions from mineral thermobarometers. The Late Cretaceous basalts studied in the pres-ent paper, however, have provided some geochemical evidence for crust-mantle interaction inthe area. These basalts are distributed in Mesozoic faulted basins in central and southern Dabieorogenic belt. Since little obvious contamination from continental crust and differentiation-crys-tallization were observed, it is suggested, based on a study of trace elements, that the basaltsare alkaline and resultant from batch partial melting of the regional mantle rocks, and share thesame or similar geochemical features with respect to their magma source. In the spider diagramnormalized by the primitive mantle, trace element geochemistry data show that their mantlesources are enriched in certain elements concentrated in the continental crust, such as Pb, K,Rb and Ba, and slightly depleted in some HFSE such as Hf, P and Nb. Pb-Sr-Nd isotopic com-positions further suggest the mantle is the mixture of depleted mantle (DM) and enriched one( EMI + EMII). This interaction can.explain the trace element characteristics of basaltic mag-mas, i.e. , the enrichment of Pb and the depletion of Hr, P and Nb in basalts can be interpre-ted by the blending of the eclogites in DOB (enriched in Pb and depleted in Hf, P and Nd)with the East China depleted mantle (As compared to the primitive mantle, it is neither en-riched in Pb nor depleted in Hf, P and Nb). It is also indicated that the eclogites in the Dabieorogenic belt were surely derived from the exhumation materials, which had delaminated into thedeep-seated mantle. Moreover, the process subsequently resulted in compositional variation ofthe mantle (especially in trace elements

  9. Chinese Jingdezhen blue and white imperial porcelain

    Institute of Scientific and Technical Information of China (English)

    WU; Juan; LI; Jiazhi; DENG; Zequn; WANG; Changsui

    2004-01-01

    Jingdezhen blue and white imperial porcelain specimens from the Yuan, Ming and Qing dynasties have been systematically analyzed using a nondestructive test method--?energy dispersive X-ray fluorescence analysis (EDXRF). The derived data of major and trace element compositions have been treated by correspondence analysis. The variation laws of the composition patterns for Jingdezhen blue and white imperial porcelain in different historical periods owing to the change in raw materials, recipe and technology have been discussed, and a time model related to variation of element composition has been preliminarily established, It would be helpful for scientific dating of Jingdezhen blue and white imperial porcelain, and even for the studies on the whole field of identification of ancient ceramics.

  10. Evidence of fire use of late Pleistocene humans from the Huanglong Cave, Hubei Province, China

    Institute of Scientific and Technical Information of China (English)

    LIU Wu; WU XianZhu; LI YiYin; DENG ChengLong; WU XiuJie; PEI ShuWen

    2009-01-01

    Since 2004, three excavations have been carried out at a late Pleistocene human fossil site of Huan-glong Cave in Yunxi County, Hubei Province of China, which unearthed seven human teeth, dozens of stone tools, mammal fossils and other evidence indicating human activities. During the third excava-tion in 2006, in the same layer as the human teeth, we found some patches of black materials embed-ded in the deposit. We doubted that this black deposit layer is the remains of burning or even human use of fire at the cave. To further explore the possibility of human fire use at the Huanglong Cave, we examined samples directly taken from the black deposit layer and compared them with samples taken from several places in the cave using three methods: micromorphology, element content determination and deposit temperature analysis. Our results indicate that the contents of carbon element in the black deposit reach 64.59%-73.29%. In contrast, contents of carbon element of the comparative samples from other parts in the cave are only 5.82%-9.49%. The micromorphology analysis of the black de-posit samples reveals a plant structure like axial parenchyma, fibrocyte, uniseriate ray and vessel.High-temperature magnetic susceptibility measurements suggest that the stratum possibly underwent a high temperature in the nature. Based on these lab analyses, we are sure that the black layer in the Huanglong Cave is the remains of fire and combustion did occur in the cave 100000 years ago. Taking other evidence of human activities found in the Huanglong Cave into consideration, we believe that the evidence of fire from the Huanglong Cave was caused by the human activities of controlled use of fire.

  11. A lacustrine record from Lop Nur, Xinjiang, China: Implications for paleoclimate change during Late Pleistocene

    Science.gov (United States)

    Chao, L.; Zicheng, P.; Dong, Y.; Weiguo, L.; Zhaofeng, Z.; Jianfeng, H.; Chenlin, C.

    2009-01-01

    Climate variability during the Late Pleistocene is studied from the proxies in core CK-2 drilled from the Luobei Depression (91??03???E, 40??47???N), Lop Nur in the eastern Tarim Basin, Xinjiang, China. Geophysical and geochemical properties, including magnetic susceptibility, granularity, chroma, carbonate content, loss on ignition and trace elements, have been determined to reconstruct the environmental evolution of the area during 32-9 ka BP. The chronology is established by uranium-thorium disequilibrium dating techniques. Our data suggest four paleoclimate stages, indicating glacial variations between cold-humid and warm-arid environments. A period of extreme humidity occurred during 31,900-19,200 yr BP is attributed the last glacial maximum (LGM). The period was followed by a warm-arid episode during 19,200-13,500 yr BP. Then a cold-humid interval during 13,500-12,700 yr BP may correspond to another cooling phases at high latitudes of the Northern Hemisphere. The last stage from 12,700 to 9000 yr BP has a trend that the climate turned warm and arid. The Lop Nur region is characterized by particularly humid stadials and arid interstadials. The climate variability in Lop Nur was constrained by global climate change because it is correlated with Dansgaard-Oeschger and Heinrich events, which were observed at the northern high latitudes. The synchroneity of the palaeoclimatic events suggested that cold air activity at the northern high latitudes was the most important factor that influenced the climate evolution in the Lop Nur region. A probable mechanism that involves the migration of westerly winds is proposed to interpret this synchroneity. ?? 2008 Elsevier Ltd.

  12. Situated Interpretations of Nationalism, Imperialism, and Cosmopolitanism

    DEFF Research Database (Denmark)

    Zhang, Chenchen

    2014-01-01

    The idea of the nation has been considered to have delivered political modernity from its native Europe to the rest of the world. The same applies, though more implicitly, to those paradoxes inherent to the nationalist ideology – that between universalism and national particularity and that between...... liberal nationalism and imperialism. This article seeks to complicate these theses by looking at the interpretations of nationalism, imperialism, and cosmopolitanism provided by Liang Qichao, one of the most influential Chinese intellectuals in early twentieth century, during his exile in Japan when...

  13. Imperialism and the English Language in Hong Kong.

    Science.gov (United States)

    Boyle, Joseph

    1997-01-01

    Considers whether the charge of linguistic imperialism can be appropriately leveled against the British government during its colonial rule of Hong Kong. The article analyzes the concept of linguistic imperialism, considers landmarks in the history of the English language in Hong Kong, and applies the concept of linguistic imperialism to the…

  14. Episodic euxinia in the Changhsingian (late Permian) of South China: Evidence from framboidal pyrite and geochemical data

    Science.gov (United States)

    Wei, Hengye; Algeo, Thomas J.; Yu, Hao; Wang, Jiangguo; Guo, Chuan; Shi, Guo

    2015-04-01

    A multiproxy study of a new Upper Permian-Lower Triassic section (Xiaojiaba) in Sichuan Province, China, documents large changes in marine productivity, redox conditions and detrital input prior to the latest Permian mass extinction. Marine productivity, as proxied by total organic carbon content (TOC), biogenic SiO2, and excess barium, displays a long-term decline through most of the Changhsingian stage (late late Permian), culminating in very low values around the Permian-Triassic boundary. Concurrently, redox proxies including pyrite framboid, δ34Spy, Moauth and Uauth, and Corg/P document a shift from suboxic to dysoxic/oxic conditions that was interrupted by several episodes of benthic euxinia, and detrital siliciclastic proxies (Al, Hf, Nb, and REEs) suggest an increased flux of weathered material from land areas. The long-term changes in productivity, redox conditions, and terrigenous detrital fluxes were probably caused by a regional sea-level fall across the South China Craton. On the other hand, the brief euxinic episodes occurring during the late Permian had oceanographic causes, probably related to the transient upward expansion of the chemocline at the top of the oceanic oxygen-minimum zone. These euxinic episodes may have been harbingers of the more widespread anoxia that developed concurrently with the latest Permian mass extinction and that may have played a major role in triggering the largest biotic crisis of the Phanerozoic.

  15. Imperial College London mascot visits CERN

    CERN Multimedia

    Hills, Stephanie

    2014-01-01

    Boanerges (‘Son of Thunder’) is one of the mascots of Imperial College and is looked after by volunteer students of the City and Guilds College Motor Club. Team Bo visited CERN as part of a wider tour of France and Switzerland.

  16. Realities and Myths of Linguistic Imperialism.

    Science.gov (United States)

    Phillipson, Robert

    1997-01-01

    Responds to Alan Davies's review article "Ironising the Myth of Linguicism," summarizing principles for the analysis of linguistic imperialism and demonstrating that the phenomenon is far from mythical. The article responds to some of the points raised by Davies to show that his generalizations are not justified. (41 references) (Author/CK)

  17. Linguistic Imperialism, Cultural Integrity, and EIL.

    Science.gov (United States)

    Modiano, Marko

    2001-01-01

    Argues that while linguistic imperialism is real and needs to be addressed, one way for the language instructor to come to terms with the cultural imposition of English language teaching is to define English as an international language. Suggests promoting "prestige varieties" positions the practitioner as purveyor of Anglo-American hegemony and…

  18. Language Science and Orientalism in Imperial Germany

    Science.gov (United States)

    Kaplan, Judith R. H.

    2012-01-01

    This dissertation addresses a significant gap in the historiography of science: the nature of the language sciences as "science." Focusing on disciplinary and intellectual developments in the context of Imperial Germany (1871-1918), the project anticipates, complicates, and helps to explain a widely recognized theoretical shift, namely,…

  19. The Linguistic Imperialism of Neoliberal Empire

    Science.gov (United States)

    Phillipson, Robert

    2008-01-01

    The article explores the transition from the linguistic imperialism of the colonial and postcolonial ages to the increasingly dominant role of English as a neoimperial language. It analyzes "global" English as a key dimension of the U.S. empire. U.S. expansionism is a fundamental principle of the foreign policy of the United States that can be…

  20. "Economics Imperialism", Education Policy and Educational Theory

    Science.gov (United States)

    Allais, Stephanie

    2012-01-01

    This paper examines how economics imperialism (the increasing colonization of other disciplines by neoclassical economics) has affected contemporary education policies. I suggest that an increasing preoccupation with education meeting the needs of the economy, together with the prevalence of economic concepts outside of economics, have contributed…

  1. Experimental Particle Physics at Imperial College London

    CERN Multimedia

    2008-01-01

    Last friday Imperial's rector Sir Richard Sykes visited CERN, in particular CMS and LHCb; the visit was supervised by CERN's VIP service, a guaranteee that nothing can go wrong. A quite impressive organization that has not much in common with the usual "pivate" visits of LHCb or CMS.

  2. Geochemistry and mineralogy of the Late Permian coals from the Songzao Coalfield, Chongqing,southwestern China

    Institute of Scientific and Technical Information of China (English)

    DAI ShiFeng; ZHOU YiPing; REN DeYi; WANG XiBo; LI Dan; ZHAO Lei

    2007-01-01

    Mineralogy and geochemistry of the four main workable coal seams (No.6, No.7, No.8, and No.11) of Late Permian age from the Songzao Coalfield, Chongqing, Southwest China, were examined using inductively coupled plasma-mass spectrometry (ICP-MS), X-ray fluorescence spectrometry (XRF),cold-vapor absorption spectrometry (CV-AAS), ion-selective electrode (ISE), scanning electron microscopy equipped with an energy-dispersive X-ray spectrometer (SEM-EDX), and X-ray diffraction analysis (XRD). The results showed that the main workable No.8 Coal that accounts for about 60% of the total coal reserves in the Songzao Coalfield was not enriched in hazardous trace elements. The No.11 Coal has high concentrations of alkaline elements, Be (9.14 μg/g), SC (12.9 μg/g), Ti (9508 μg/g),Mn (397 μg/g), Co (23.7 μg/g), Cu (108 μg/g), Zn (123 μg/g), Ga (32 μg/g), Zr (1304 μg/g), Nb (169 μg/g), Hf (32.7 μg/g), Ta (11.4 μg/g), W (24.8 μg/g), Hg (0.28 μg/g), Pb (28.1 μg/g), Th (24.1 μg/g), and rare earth elements (509.62 μg/g). The concentration of Nb and Ta in the No. 11 Coal is higher than the industrial grade, and their potential utilization should be further studied. Besides pyrite, quartz, calcite, and clay minerals, trace minerals including chalcopyrite, marcasite, siderite, albite, mixed-layer clay minerals of illite and smectite, monazite, apatite, anatase, chlorite, and gypsum were found in the No.11 Coal. It should be noted that alabandite of hydrothermal origin and anatase occurring as cement were identified in coal. In addition, the clayey microbands derived from alkaline volcanic ashes were identified in the coal. The dominant compositions of these clayey microbands were mixed-layer clay minerals of illite and smectite, which were interlayered with organic bands. The modes of occurrence of alkaline volcanic ash bands indicate that the volcanic activities were characterized by the multiple eruptions,short time interval and small scale for each eruption during

  3. Geochemistry and mineralogy of the Late Permian coals from the Songzao Coalfield, Chongqing,southwestern China

    Institute of Scientific and Technical Information of China (English)

    2007-01-01

    Mineralogy and geochemistry of the four main workable coal seams (No.6, No.7, No.8, and No.11) of Late Permian age from the Songzao Coalfield, Chongqing, Southwest China, were examined using in- ductively coupled plasma-mass spectrometry (ICP-MS), X-ray fluorescence spectrometry (XRF), cold-vapor absorption spectrometry (CV-AAS), ion-selective electrode (ISE), scanning electron mi- croscopy equipped with an energy-dispersive X-ray spectrometer (SEM-EDX), and X-ray diffraction analysis (XRD). The results showed that the main workable No.8 Coal that accounts for about 60% of the total coal reserves in the Songzao Coalfield was not enriched in hazardous trace elements. The No.11 Coal has high concentrations of alkaline elements, Be (9.14 μg/g), Sc (12.9 μg/g), Ti (9508 μg/g), Mn (397 μg/g), Co (23.7 μg/g), Cu (108 μg/g), Zn (123 μg/g), Ga (32 μg/g), Zr (1304 μg/g), Nb (169 μg/g), Hf (32.7 μg/g), Ta (11.4 μg/g), W (24.8 μg/g), Hg (0.28 μg/g), Pb (28.1 μg/g), Th (24.1 μg/g), and rare earth elements (509.62 μg/g). The concentration of Nb and Ta in the No. 11 Coal is higher than the industrial grade, and their potential utilization should be further studied. Besides pyrite, quartz, calcite, and clay minerals, trace minerals including chalcopyrite, marcasite, siderite, albite, mixed-layer clay minerals of illite and smectite, monazite, apatite, anatase, chlorite, and gypsum were found in the No.11 Coal. It should be noted that alabandite of hydrothermal origin and anatase occurring as cement were identi- fied in coal. In addition, the clayey microbands derived from alkaline volcanic ashes were identified in the coal. The dominant compositions of these clayey microbands were mixed-layer clay minerals of illite and smectite, which were interlayered with organic bands. The modes of occurrence of alkaline volcanic ash bands indicate that the volcanic activities were characterized by the multiple eruptions, short time interval and small scale for each eruption

  4. A high-resolution multi-proxy record of late Cenozoic environment change from central Taklimakan Desert, China

    Directory of Open Access Journals (Sweden)

    X. Wang

    2013-05-01

    Full Text Available The Taklimakan Desert in the Tarim Basin is the largest desert in Central Asia, and is regarded as one of the main dust sources to the Northern Hemisphere. Late Cenozoic sedimentary sequences with intercalated in-situ aeolian dune sands in this area preserve direct evidence for the Asian desertification. Herein, we report a high-resolution multi-proxy climatic record from the precise magnetostratigraphic dated Hongbaishan section in the central Taklimakan Desert. Our results show that a fundamental climate change, characterized by significant cooling, enhanced aridity, and intensified atmospheric circulation, occurred at 2.8 Ma. Good correlations between climate records in the dust sources and downwind areas suggest a broadly consistent climate evolution of northwestern China during the late Cenozoic, which is probably driven by the uplift of the Tibet Plateau and the Northern Hemisphere glaciation.

  5. Plants of Leptostrobus Heer (Czekanowskiales) from the Early Cretaceous and Late Triassic of China, with Discussion of the Genus

    Institute of Scientific and Technical Information of China (English)

    2006-01-01

    Inveetlgation of the Meeozoic seed plant Leptostrobus Heer from the Yangcaogou Formation of the Late Triassic and the Yixian Formation of the Early Cretaceous, Liaoning Province, China, provides new insight into its general morphology and geographical distribution. The materials of L. cancer from the Yixian Formation described herein are later than all the past findings of this species and add to the record of L. cancerduring the Early Cretaceous. Based on well-preserved specimens, the specific diagnosis is slightly emended and the reconstruction of L. cancer is perfected. The materials from the Yangcaogou Formation of the Late Triassic are placed in L. sphaericus. in addition, we review the history of investigation of the genus Leptostrobus since its establishment in 1876 and discuss the main characteristics of each species.

  6. Late Miocene wood flora associated with the Yuanmou hominoid fauna from Yunnan, southwestern China and its palaeoenvironmental implication

    Directory of Open Access Journals (Sweden)

    Ye-Ming Cheng

    2014-07-01

    Full Text Available The Upper Miocene Xiaohe Formation of the Yuanmou Basin in Yunnan Province, southwestern China, is famous for its hominoid fauna and is important for studying the Late Cenozoic human and mammal evolution. Abundant fossil wood was found associated with this fauna, which provided important evidence for palaeoenvironmental reconstruction of the basin. Among the fossil wood, two different taxa have been identified namely, Quercoxylon sp. (Fagaceae and Pterocarya sp. (Juglandaceae. Based on the habitats of their Nearest Living Relatives (NRLs, it is suggested that upland subtropical evergreen broad-leaved forest dominated by Quercus/Lithocarpus was common around the basin, while a lowland deciduous broad-leaved forest dominated by Pterocarya was present on the river bank of the basin during the Late Miocene.

  7. Discovery of Late Paleozoic retrograded eclogites from the middle part of the northern margin of North China Craton

    Institute of Scientific and Technical Information of China (English)

    NI Zhiyao; ZHAI Mingguo; WANG Renmin; TONG Ying; SHU Guiming; HAl Xiuling

    2004-01-01

    The retrograded eciogites have been discovered in the middle part of the northern margin of the North China Craton, which occur as lens or boudin within biotite-plagioclase gneisses in Paleoproterozoic Hongqiyingzi Group. The peak eclogite facies (P > 1.40-1.50 GPa, T = 680-730℃) mineral assemblage is composed of garnet, omphacite and rutile (+ quartz), which was overprinted by the granulite facies mineral assemblage of vermicular symplectite of sodic clinopyroxene and plagioclase which replaced the precursory omphacite, and then amphibolite facies retrograded minerals with characterization of Amp+Pl kelyphitic rim and symplectite, and amphibole replaced clinopyroxene. The protolith of retrograded eclogites is oceanic basalt formed at 438 + 11 Ma. The peak eclogite facies metamorphic age of the retrograded eclogite is 325 + 4 Ma. These relict eclogites may be formed by the subduction of Paleo-Asian oceanic crust beneath the North China Craton during Late Paleozoic. The discovery of relict eclogite in this paper provides a new insight into farther understanding of tectonic evolution of the northern margin of the North China Craton, and the relationship between the Paleo-Asian Ocean and the North China Craton.

  8. Copper Factories in North China Suspended Production Extensively, Consumption Release May Appear in Late September

    Institute of Scientific and Technical Information of China (English)

    2015-01-01

    Recently,it was discovered that many copper factories in North China market one after another entered production suspension status.According to manufacturers in Tianjin area,in order to guarantee successful proceeding of China’s Military Parade in early September,high pollution and high energy consumingsmelting&processing; enterprises in North China received notice of production suspension

  9. Late Mesozoic-Cenozoic décollement structure and its deep geological background in western Shandong,China

    Institute of Scientific and Technical Information of China (English)

    Li Li; Dalai Zhaong; Xiupeng Shi; Zibo Tang; Qiuyuan Hu; Yi Xu; Zhiwei Li

    2009-01-01

    Data from seismic reflection profiles,drilling,stratigraphy,structural deformation studies and physical rock properties reveal the existence of drcollement structures in both shallow and deep levels in western Shandong,China.The most outstanding shallow décollement structures occur along the regional unconformity surface between the Cambrian and Archean,and the disconformity surface between the Carboniferous and Ordovician.The drcollement structure surface manifests as a fault zone with cataclastic rocks and asymmetrical folds.Some of the cataclastic rocks underwent dynamic metamorphism and hydrothermal alteration,including silicification,marbleization and specularite mineralization.Above the decollement structure,the bottom of the Cambrian might be missing or overprinted because of decollement.The striations,asymmetrical folds and boudinage structures indicate the direction of the main décollement tothe NNW and NNE.A deep level decollement structure occurs at a depth of 12-22 km and up to 30 km distance to the south.The early Cretaceous and Eocene are two main periods of activity,with the Cretaceous decollement probably initiated by mantle upwelling derived from subduction and collision of the Yangtze Plate with the North China Plate along the Tancheng-Lujiang Fault in the late Triassicearly Jurassic.This circumstance implies a multidirection of subduction and collision of these two plates in the early late Mesozoic.(C) 2009 National Natural Science Foundation of China and Chinese Academy of Sciences.Published by Elsevier Limited and Science in China Press.All rights reserved.

  10. Statistical modeling of CMIP5 projected changes in extreme wet spells over China in the late 21st century

    Science.gov (United States)

    Zhu, Lianhua; Li, Yun; Jiang, Zhihong

    2017-08-01

    The observed intensity, frequency, and duration (IFD) of summer wet spells, defined here as extreme events with one or more consecutive days in which daily precipitation exceeds a given threshold (the 95th percentile), and their future changes in RCP4.5 and RCP8.5 in the late 21st century over China, are investigated by using the wet spell model (WSM) and by extending the point process approach to extreme value analysis. Wet spell intensity is modeled by a conditional generalized Pareto distribution, frequency by a Poisson distribution, and duration by a geometric distribution, respectively. The WSM is able to realistically model summer extreme rainfall spells during 1961-2005, as verified with observations at 553 stations throughout China. To minimize the impact of systematic biases over China in the global climate models (GCMs) of the Coupled Model Intercomparison Project Phase 5 (CMIP5), five best GCMs are selected based on their performance to reproduce observed wet spell IFD and average precipitation during the historical period. Furthermore, a quantile-quantile scaling correction procedure is proposed and applied to produce ensemble projections of wet spell IFD and corresponding probability distributions. The results show that in the late 21st century, most of China will experience more extreme rainfall and less low-intensity rainfall. The intensity and frequency of wet spells are projected to increase considerably, while the duration of wet spells will increase but to a much less extent. The IFD changes in RCP8.5 are in general much larger than those in RCP4.5.

  11. Post-Pliocene establishment of the present monsoonal climate in SW China: evidence from the late Pliocene Longmen megaflora

    Science.gov (United States)

    Su, T.; Jacques, F. M. B.; Spicer, R. A.; Liu, Y.-S.; Huang, Y.-J.; Xing, Y.-W.; Zhou, Z.-K.

    2013-08-01

    The paleoclimate of the late Pliocene Longmen flora from Yongping County located at the southeastern boundary of the Qinghai-Tibet Plateau was reconstructed using two leaf-physiognomy-based methods, i.e., leaf margin analysis (LMA) and Climate Leaf Analysis Multivariate Program (CLAMP), to understand the paleoclimate condition and geographical pattern of monsoonal climate in southwestern China during the late Pliocene. The mean annual temperatures (MATs) estimated by LMA and CLAMP are 17.4 ± 3.3 °C and 17.4 ± 1.3 °C, respectively, compared with 15.9 °C at present. Meanwhile, the growing season precipitation (GSP) estimated by CLAMP is 1735.5 ± 217.7 mm in the Longmen flora, compared with 986.9 mm nowadays. The calculated monsoon intensity index (MSI) of the Longmen flora is significantly lower than that of today. These results appear consistent with previous studies on the late Pliocene floras in western Yunnan based on the coexistence approach (CA), and further suggest that there was a slightly warmer and much wetter climate during the late Pliocene than the present climate in western Yunnan. We conclude that the significant change of the monsoonal climate might have been resulted from the continuous uplift of mountains in western Yunnan, as well as the intensification of the eastern Asian winter monsoon, both occurring concurrently in the post-Pliocene period.

  12. Climatic and tectonic controls on Late Triassic to Middle Jurassic sedimentation in northeastern Guangdong Province, South China

    Science.gov (United States)

    Pang, Chong-Jin; Li, Zheng-Xiang; Xu, Yi-Gang; Wen, Shu-Nv; Krapež, Bryan

    2016-05-01

    Stratigraphic analyses document climatic and tectonic controls on the filling of a Late Triassic to early Middle Jurassic (T3-J2) basin that developed on top of a young orogenic belt in southeastern South China. About 2700 m of Carnian to Bajocian sedimentary rocks is documented in the Meizhou region, Guangdong Province. The Carnian to Rhaetian sequence is characterized by deltaic facies that are succeeded by Hettangian fluvial, shallow marine and volcaniclastic facies, and by Sinemurian to early Toarcian interdistributary bay and floodplain facies. The late Toarcian to Bajocian sequence comprises proximal alluvial to lacustrine facies that changed upwards to fluvial facies. Fossil assemblages indicate that climatic conditions changed from tropical/subtropical warm humid, to temperate humid, and then to hot arid through the Late Triassic to the Middle Jurassic. Climatically induced changes (e.g., in precipitation, vegetation and erosion) exerted a strong influence on sediment supply, whereas tectonics played a dominant role in stratigraphic evolution, accommodation generation, sedimentation pattern and volcanism. Tectonostratigraphic analysis shows that the T3-J2 basin was initiated on an orogenic belt during late-stage orogeny, and evolved into shallow-marine and volcanic environments and then back to terrestrial facies during the post-orogenic stage. This was followed by regional uplift and the development of a basin-and-range province. The order of these events is similar to that of the central Rocky Mountains, western North America during the Palaeogene. The Mesozoic basin of South China and the Eocene basins of the central Rocky Mountains highlight the importance of subduction-related subsidence above young and broad orogens.

  13. Tectonic implications of Late Paleozoic stratigraphic distribution in Northeast China and adjacent region

    Institute of Scientific and Technical Information of China (English)

    WANG ChengWen; SUN YueWu; LI Ning; ZHAO GuoWei; MA XiaoQin

    2009-01-01

    An analysis of the distribution of the Late Paleozoic strata on Northeast Chinaand adjacent region re-veals a zonal pattern of the distribution around the core of the Jiamusi-Mongolia Block. The main part of Late Paleozoic marine strata in this area is considered the continental margin deposits of the Jia-musi-Mongolia Block by analyzing the stratigraphic contact relationship, lithofacies, etc. The results are exhibited in a series of tectonic paleogeographic maps. This presents an important proof for the foundation of the Jiamusi-Mongolia Block, and confines the forming time of Jiamusi-Mongolia Block to the Late Silurian.

  14. Multi-proxy evidence for Late Pleistocene-Holocene climatic and environmental changes in Lop-Nur, Xinjiang, Northwest China

    Science.gov (United States)

    Luo, C.; Yang, D.; Peng, Z.; Zhang, Z.; Weiguo, L.; He, J.; Zhou, C.

    2008-01-01

    A 10.35-m-long sediment core from the Luobei depression in Lop-Nur, Xinjiang, Northwest China, provides detailed information about environmental changes during the Late Pleistocene. The samples taken every 5 cm of the core were analyzed for 10 environmental proxies, including magnetic susceptibility, granularity, chroma, carbonate and loss on ignition (LOI), and pH value. The chronology data are provided by the uranium/thorium disequilibrium dates. The sediments of the section were deposited during the last 32000 years. The results of analysis of 10 proxies were examined using multivariate statistical analysis, and the principal components were calculated. According to the results, the Late Pleistocene sequence contains four climatic and environmental stages appearing in the cycles of cold-wet and warm-dry changes. During 10-9 ka BP, it was the earliest warm episode in the Holocene. Environmental changes in this district were restricted by global change, as suggested by the analysis of glacial-interglacial cycles. But it was different from the mutative trend of a monsoon region in East China because of its own characteristics, which was the situation of cold-wet and warm-dry climate-environment change. The candidate reason may be the uplift of the Tibet Plateau and the westerly wind circulation. ?? Science Press, Institute of Geochemistry, CAS and Springer-Verlag GmbH 2008.

  15. Multi-proxy evidence for Late Pleistocene Holocene climatic and environmental changes in Lop-Nur, Xinjiang, Northwest China

    Institute of Scientific and Technical Information of China (English)

    LUO Chao; YANG Dong; PENG Zicheng; ZHANG Zhaofeng; LIU Weiguo; HE Jianfeng; ZHOU Chenlin

    2008-01-01

    A 10.35-m-long sediment core from the Luobei depression in Lop-Nur, Xinjiang, Northwest China, provides detailed information about environmental changes during the Late Pleistocene. The samples taken every 5 cm of the core were unalyzed for 10 environmental proxies, including magnetic susceptibility, granularity, chroma, carbonate and loss on ignition (LOI), and pH value. The chronology data are provided by the uranium/thorium disequilibrium dates. The sediments of the section were deposited during the last 32000 years. The results of analysis of 10 proxies were examined using multivariate statistical analysis, and the principal components were calculated. According to the results, the Late Pleistocene sequence contains four climatic and environmental stages appearing in the cycles of cold-wet and warm-dry changes. During 10-9 ka BP, it was the earliest warm episode in the Holocene.Environmental changes in this district were restricted by global change, as suggested by the analysis of glacial-interglacial cycles. But it was different from the mutative trend of a monsoon region in East China because of its own characteristics, which was the situation of cold-wet and warm-dry climate-environment change. The candidate reason may be the uplift of the Tibet Plateau and the westerly wind circulation.

  16. Molecular composition and indigenity of organic matter in Late Neoproterozoic sedimentary rocks from the Yangtze region, South China

    Institute of Scientific and Technical Information of China (English)

    LI Meijun; WANG Tieguan; WANG Chunjiang; ZHANG Weibiao

    2006-01-01

    Diamictites from Late Neoproterozoic Nantuo tillites (~600 Ma), and dolomites from the overlying Dousantuo and Dengying formations in the Yangtze region, southern China, were analyzed for solvent extractable hydrocarbons. Even though all these samples have low contents of TOC and have undergone overmature thermal evolution, there has been still preserved quite a large amount of hydrocarbons. Analysis of the extracts by gas chromatography-mass spectrometry (GC-MS) revealed the presence of n-alkanes, regular acyclic isoprenoids, tricyclic terpanes, hopanes, gammacerane, steranes, and polyaromatic hydrocarbons. Strict experimental measurements were performed in the analytical procedure to prevent any potential contaminants from being introduced. All these bitumens have molecular markers of Precambrian characteristics and no external organics derived from current contamination events or migrated hydrocarbons from younger strata. The maturity parameters for bitumens indicate that the hydrocarbons are of over-maturity, which is consistent with the thermal maturity of the host rocks. Consequently, it is concluded that the Late Neoproterozoic bitumens in the Yangtze region, South China, are indigenous to their host rocks, which provides the basis for our organic geochemical research on "Snowball Earth" and "Cambrian Explosion."

  17. The end of corporate imperialism.

    Science.gov (United States)

    Prahalad, C K; Lieberthal, Kenneth

    2003-08-01

    As they search for growth, multinational corporations will have no choice but to compete in the big emerging markets of China, India, Indonesia, and Brazil. But while it is still common to question how such corporations will change life in those markets, Western executives would be smart to turn the question around and ask how multinationals themselves will be transformed by these markets. To be successful, MNCs will have to rethink every element of their business models, the authors assert in this seminal HBR article from 1998. During the first wave of market entry in the 1980s, multinationals operated with what might be termed an imperialist mind-set, assuming that the emerging markets would merely be new markets for their old products. But this mind-set limited their success: What is truly big and emerging in countries like China and India is a new consumer base comprising hundreds of millions of people. To tap into this huge opportunity, MNCs need to ask themselves five basic questions: Who is in the emerging middle class in these countries? How do the distribution networks operate? What mix of local and global leadership do you need to foster business opportunities? Should you adopt a consistent strategy for all of your business units within one country? Should you take on local partners? The transformation that multinational corporations must undergo is not cosmetic--simply developing greater sensitivity to local cultures will not do the trick, the authors say. To compete in the big emerging markets, multinationals must reconfigure their resources, rethink their cost structures, redesign their product development processes, and challenge their assumptions about who their top-level managers should be.

  18. Spatial distributions of floating seaweeds in the East China Sea from late winter to early spring

    OpenAIRE

    Mizuno, S.; Ajisaka, T.; Lahbib, S.; Kokubu, Y.; Alabsi, M. N.; Komatsu, T

    2013-01-01

    Floating seaweeds play an important role as a habitat for many animals accompanying or attaching to them in offshore waters. It was in 2000 that the first report described abundant distributions of floating seaweeds in offshore waters in the East China Sea in spring. Young individuals of the yellowtail Seriola quinqueradiata are captured for aquaculture purposes from floating seaweeds in the East China Sea. Therefore, a sound understanding of the distributions of floating seaweeds in the East...

  19. A Hominin Femur with Archaic Affinities from the Late Pleistocene of Southwest China: e0143332

    National Research Council Canada - National Science Library

    Darren Curnoe; Xueping Ji; Wu Liu; Zhende Bao; Paul S C Taçon; Liang Ren

    2015-01-01

      The number of Late Pleistocene hominin species and the timing of their extinction are issues receiving renewed attention following genomic evidence for interbreeding between the ancestors of some...

  20. Representation and Imperialism in Edward Said

    Directory of Open Access Journals (Sweden)

    Bruno Sciberras de Carvalho

    2010-12-01

    Full Text Available Based on the idea that culture and identities involve a politically built process, the importance of the concepts of representation and imperialism in the work of Edward Said is discussed. The article analyses two of the author’s general proposals. Firstly, the thesis of the centrality of cultural dimension in political relations, which leads to the review of postulates that consider culture as a mere reflection of a phenomena seen as essential or as a sphere isolated from the power practices. Secondly, the study examines how the author’s conception of imperialism is used as a means of identification that keep structures of authority and hegemony, which, in turn, may be defied by processes of resistance. Finally, the validity of the open character of Said’s political theory is debated, which encompasses both the power of representations and an action of political questioning.

  1. Late Permian to Triassic intraplate orogeny of the southern Tianshan and adjacent regions, NW China

    Directory of Open Access Journals (Sweden)

    Wei Ju

    2014-01-01

    Based on previous studies and recent geochronogical data, we suggest that the final collision between the Tarim Craton and the North Asian continent occurred during the late Carboniferous. Therefore, the Permian was a period of intracontinental environment in the southern Tianshan and adjacent regions. We propose that an earlier, small-scale intraplate orogenic stage occurred in late Permian to Triassic time, which was the first intraplate process in the South Tianshan Orogen and adjacent regions. The later large-scale and well-known Neogene to Quaternary intraplate orogeny was induced by the collision between the India subcontinent and the Eurasian plate. The paper presents a new evolutionary model for the South Tianshan Orogen and adjacent regions, which includes seven stages: (I late Ordovician–early Silurian opening of the South Tianshan Ocean; (II middle Silurian–middle Devonian subduction of the South Tianshan Ocean beneath an active margin of the North Asian continent; (III late Devonian–late Carboniferous closure of the South Tianshan Ocean and collision between the Kazakhstan-Yili and Tarim continental blocks; (IV early Permian post-collisional magmatism and rifting; (V late Permian–Triassic the first intraplate orogeny; (VI Jurassic–Palaeogene tectonic stagnation and (VII Neocene–Quaternary intraplate orogeny.

  2. Did the Paleo-Asian Ocean between North China Block and Mongolia Block exist during the late Paleozoic? First paleomagnetic evidence from central-eastern Inner Mongolia, China

    Science.gov (United States)

    Zhao, Pan; Chen, Yan; Xu, Bei; Faure, Michel; Shi, Guanzhong; Choulet, Flavien

    2013-05-01

    The tectonic evolution of the Paleo-Asian Ocean between the North China Block (NCB) and the Mongolia Block (MOB) is a contentious issue, and geodynamic models remain speculative. In an effort to puzzle out this controversy, a paleomagnetic study was carried out on the Silurian to Permian formations in central-eastern Inner Mongolia (China). More than 680 sedimentary and volcanic samples were collected from 86 sites. We have established titanium-poor magnetite and hematite as the principal magnetic carriers. Anisotropy of the magnetic susceptibility measurements demonstrate negligible deformation of the majority of study rocks with sedimentary fabrics. From primary magnetizations, a Late Devonian and a Permian pole are calculated for Inner Mongolia Block (IMB) at λ = 46.8°N, φ = 349.1°E, dp = 14.6°, dm = 27.3° with N = 3 and λ = 48.7°N, φ = 3.7°E, dp = 5.2°, dm = 9.1° with N = 6, respectively. Two stages of secondary magnetization are also identified probably due to Early Permian and Early Cretaceous magmatic events. As preliminary results, the comparison of our new paleomagnetic poles with available data from NCB, MOB, and Siberia indicates that (1) the paleolatitudes of IMB, NCB, and MOB are consistent between Late Devonian and Permian, suggesting pre-Late Devonian closure of the Paleo-Asian Ocean and further evaluation of these three blocks as a single entity and (2) post-Permian intracontinental deformation was significant and characterized by block rotations, which are due to strike-slip faulting within the welded NCB-IMB-MOB block.

  3. El Museo Imperial de Guerra en Londres

    Directory of Open Access Journals (Sweden)

    Graciela Dacosta

    2013-11-01

    Full Text Available Generalidades sobre algunos tipos de materiales especiales existen en el “Imperial War Museum” de Gran Bretaña. Se observa: a una superposición de métodos manuales y automatizados para el procesamiento técnico de las colecciones no tradicionales; b diferentes grabados de desarrollo en la implementación de sistemas computarizados.

  4. Foreword: French Language Acquisition in Imperial Russia

    Directory of Open Access Journals (Sweden)

    Derek Offord

    2013-11-01

    Full Text Available The foreword to Vivliofika’s cluster of articles on French language acquisition in Imperial Russia mentions the scholarly project and conference out of which the cluster arises, briefly describes the UK-based project, states the importance of study of education in it, summarises a few of the main educational questions that are germane in this connection and, finally, simply introduces the contents of the cluster.

  5. Fast Food Paradox: Freedom and Cultural Imperialism

    OpenAIRE

    Lelia Voinea

    2012-01-01

    Fast food is often regarded as a form of cultural imperialism. Fast-food products, originating in the U.S.A., are considered by the critics of this phenomenon as responsible for eroding the interest in local food traditions and affecting their continuity. Based on the results of some researches realized at international and national level, the paper highlights the main issues underlying young people preference for fast-food. The consumption of fast food is associated with the idea of independ...

  6. How Neoliberal Imperialism is Expressed by Programming Strategies of Phoenix TV: A Critical Case Study

    Directory of Open Access Journals (Sweden)

    Shuang Xie

    2013-05-01

    Full Text Available This project is a case study of Phoenix Television, which is a Hong Kong-based satellite TV network broadcasting to the global Chinese-speaking community, primarily to the mainland of China. In the theoretical framework of media imperialism and neoliberal imperialism, this study focuses on the programming strategies of Phoenix TV and examines how the global trend of neoliberalism, the Chinese government’s tight control of the media, and the sophisticated ownership of Phoenix TV intertwined to influence on its programming. The analysis of the format, content, naming, and scheduling reveals that US-inspired neoliberalism is expressed in the network’s programming strategies. This expression, in fact, is the balance that Phoenix found between the tension of global and Chinese interests, the tension between revenue making and public service, and the tension between Party-control and profit seeking.

  7. Optical legacy of Imperial College London

    Science.gov (United States)

    Kidger Webb-Moore, Tina E.

    2016-10-01

    The Industrial Revolution, beginning primarily in the UK, generated an increasing need for highly skilled technical people. Throughout the 19th century, technical instruction increased dramatically and the formation of schools specializing in science and technology grew quickly. In England, there was much motivation in favour of a national prestige center for science and technology centered in London. Central among the motivating forces was Queen Victoria's husband, Prince Albert. Although there were already existing specialist science and technology institutions in major English cities, the growth of superior institutions in other countries within Europe, especially Germany and the Charlottenburg area of Berlin (e.g., the Berlin Technical High School), encouraged important English dignitaries to become more competitive with continental Europe. As a result of this strong continental motivation, several science and technology institutions were built in the south Kensington part of London during the latter half of the 19th century. Imperial College, founded at the start of the 20th century, was a culmination and consolidation of several of these 19th century English institutions. Optical science and technology was an early beneficiary of the founding of Imperial College. This paper will attempt to provide the reader with an understanding of how great was the influence of the optical section of Imperial College in the further development of the world's optical science and technology.

  8. From Cycles to Sequences: Sequence Stratigraphy and Relative Sea Level Change for the Late Cambrian of the North China Platform

    Institute of Scientific and Technical Information of China (English)

    MEI Mingxiang; MA Yongsheng; DENG Jun; CHEN Huijun

    2005-01-01

    In the Late Cambrian, the North China Platform was a typical carbonate ramp platform. The Upper Cambrian of the northern part of the North China Platform is famous for the development of bioherm limestones and storm calcirudites and can be divided from bottom to top into the Gushan, Changshan and Fengshan formations. In this set of strata, the deep-ramp mudstone and marls and the shallow-ramp packstones and grainstones constitute many carbonate meter-scale cycles of subtidal type. More tidal-flat dolomites are developed in the Upper Cambrian of the southern margin of the North China platform, in which limestone and dolomite beds also constitute many carbonate meter-scale cycles of the peritidal type. These cycles are marked by a variety of litho-facies successions. There are regularly vertical stacking patterns of meter-scale cycles in long-term third-order sequences, which is the key to discerning such sequences. Thirdorder sequence is marked by a particular sedimentary-facies succession that is the result of the environment-changing process of deepening and shoaling, which is genetically related to third-order sea level changes. Furthermore, four thirdorder sequences can be grouped in the Upper Cambrian of the North China Platform. The main features of these four thirdorder sequences in the northern part of the platform can be summarized as follows: firstly, sequence-boundaries are characterized by drowning unconformities; secondly, the sedimentary-facies succession is generally constituted by one from deep-ramp facies to shallow-ramp facies; thirdly, a succession of "CS (?)+HST" (i.e., "condensed section and highstand system") forms these four third-order sequences. The chief features for the third-order sequences in the southern part of the North China Platform comprises: more dolomites are developed in the HSTs of third-order sequences and also developed more carbonate meter-scale cycles of peritidal types; the sedimentary-facies succession of the third

  9. Contribution of the phase transition of Pacific Decadal Oscillation to the late 1990s' shift in East China summer rainfall

    Science.gov (United States)

    zhu, yali

    2016-04-01

    Based on our previous study, the interdecadal changes in summer rainfall over East China in the late 1990s are further explored here. The increased local rising motion is implicated as the dominant factor of increased rainfall in the lower Huang-Huai River valley (LHR). Both the observation and numerical experiments using Community Atmosphere Model, version 4 suggest that the negative Pacific Decadal Oscillation (PDO) mode can result in rising anomalies and thus more rainfall in the LHR. The East Asian westerly jet stream (EAWJS) is suggested as a bridge to link the Pacific sea surface temperature anomalies and East Asian summer rainfall. Model results reveal that the negative PDO mode can lead to significant easterly anomalies over East Asia. As a result, the EAWJS is weakened and shifts poleward, which coincides with observed changes in EAWJS after the late 1990s. In addition, weakened and poleward shifted EAWJS can result in an anomalous ascending motion to its south (in the LHR) by modulating the jet-related secondary meridional-vertical circulation. Consequently, rainfall increased in the LHR after the late 1990s. Besides, the positive Atlantic Meridional Oscillation can only induce insignificant changes over East Asia and partly counteract the negative PDO effect there.

  10. Post-Pliocene establishment of the present monsoonal climate in SW China: evidence from the late Pliocene Longmen megaflora

    Directory of Open Access Journals (Sweden)

    T. Su

    2013-04-01

    Full Text Available The paleoclimate of the late Pliocene Longmen flora from Yongping County located at the southeastern boundary of the Qinghai-Tibet Plateau was reconstructed using two leaf physiognomy based methods, i.e. Leaf Margin Analysis (LMA and Climate Leaf Analysis Multivariate Program (CLAMP, to understand the paleoclimate condition and geographical pattern of monsoonal climate in southwestern China during the late Pliocene. The mean annual temperatures (MATs estimated by LMA and CLAMP are 17.4 ± 3.3 °C and 17.4 ± 1.3 °C, respectively, compared with 15.9 °C at present. Meanwhile, the growing season precipitation (GSP estimated by CLAMP is 1735.5 ± 217.7 mm in the Longmen flora, compared with 986.9 mm nowadays. The calculated monsoon index (MSI of the Longmen flora is significantly lower than that of today. These results appear consistent with previous studies based on the coexistence approach (CA, and further suggest that there was a slightly warmer and much wetter climate during the late Pliocene than the present climate in western Yunnan. We conclude that the significant change of the monsoonal climate might have been resulted from the continuous uplift of mountains in western Yunnan, as well as the intensification of eastern Asian winter monsoon, both occurring concurrently in the post-Pliocene period.

  11. Mineralogical and Geochemical Characteristics of Late Permian Coals from the Mahe Mine, Zhaotong Coalfield, Northeastern Yunnan, China

    Directory of Open Access Journals (Sweden)

    Xibo Wang

    2015-07-01

    Full Text Available This paper reports the mineralogical and geochemical compositions of the Late Permian C2, C5a, C5b, C6a, and C6b semianthracite coals from the Mahe mine, northeastern Yunnan, China. Minerals in the coals are mainly made up of quartz, chamosite, kaolinite, mixed-layer illite/smectite (I/S, pyrite, and calcite; followed by anatase, dolomite, siderite, illite and marcasite. Similar to the Late Permian coals from eastern Yunnan, the authigenic quartz and chamosite were precipitated from the weathering solution of Emeishan basalt, while kaolinite and mixed-layer I/S occurring as lenses or thin beds were related to the weathering residual detrital of Emeishan basalt. However, the euhedral quartz and apatite particles in the Mahe coals were attributed to silicic-rock detrital input. It further indicates that there has been silicic igneous eruption in the northeastern Yunnan. Due to the silicic rock detrital input, the Eu/Eu* value of the Mahe coals is lower than that of the Late Permian coals from eastern Yunnan, where the detrital particles were mainly derived from the basalt. The high contents of Sc, V, Cr, Co, Ni, Cu, Ga, and Sn in the Mahe coals were mainly derived from the Kangdian Upland.

  12. 清前期宫廷西洋科学仪器的种类和来源/Types and Sources of Scientific Instruments in the Imperial Court of the Early Qing Dynasty

    Directory of Open Access Journals (Sweden)

    Fuxiang GUO

    2015-12-01

    Since the late Ming and the early Qing Dynasty, a far-reaching wave of cultural exchange was formed by Christian missionaries, with Jesuits as the mainstay. This exchange is different from previous ones in that science becomes the most important medium connecting the west and China. A comprehensive examination of this sino-western exchange shows that if lay communication is believed to be dominated by religion and science, the imperial court was turned into an arena where Chinese emperors utilized western science and techniques. It is for this reason that the Palace Museum has housed a considerable collection of western scientific instruments. This paper presents a comparatively full introduction to the collection and an exploration into the collection process by reviewing documents and physical objects.

  13. Imperial Matter: Ancient Persia and the Archaeology of Empires

    OpenAIRE

    Khatchadourian, Lori

    2016-01-01

    What is the role of the material world in shaping the tensions and paradoxes of imperial sovereignty? Scholars have long shone light on the complex processes of conquest, extraction, and colonialism under imperial rule. But imperialism has usually been cast as an exclusively human drama, one in which the world of matter does not play an active role. Lori Khatchadourian argues instead that things—from everyday objects to monumental buildings—profoundly shape social and political life under emp...

  14. Extension structural records in the Qinshui basin (North China) since the Late Mesozoic

    Science.gov (United States)

    Wang, Ying; Zhang, Qinglong; Zhu, Wenbin; Wang, Liangshu; Xie, Guoai; Liu, Chao; Zou, Xu

    2014-11-01

    Qinshui basin has abundant coal-bed methane resources and has been undergoing intensive intracontinental rifting and extensional tectonics since the Late Mesozoic. Some fractures, which were previously considered as conjugate shear fractures, are interpreted as joint sets with extension characteristics, for the first time in the Qinshui basin. The widely distributed joint sets with stable attitudes can be divided into four sets. This paper presents updated results of fault-slip datasets collected in different zones of the Qinshui basin and addresses the changes in the direction of extensional stresses since the Late Mesozoic. Based on the analysis results of the slickenline of normal faults, joint sets in the field, and focal mechanism solutions data from the Shanxi Province, we identified four main directions of extension since the Late Mesozoic in the Qinshui basin: (1) Early Cenozoic ENE-WSW (85 ± 15°) extension; (2) Palaeogene NNE-SSW (30 ± 5°) extension; (3) Miocene NW-SE (135 ± 15°) extension; and (4) Late Pliocene-quaternary NNW-SSE (170 ± 5°) extension. The principal extension directions in the Qinshui basin seem to have undergone a counterclockwise rotation from the Early Cenozoic to the Miocene. We prefer that the extension deformation events in the Qinshui basin since the Late Mesozoic were mainly related to the back-arc spreading induced by westward subduction of the paleo-Pacific plate under the Eurasian continent.

  15. Late Permian to Triassic intraplate orogeny of the southern Tianshan and adjacent regions, NW China

    Institute of Scientific and Technical Information of China (English)

    Wei Ju; Guiting Hou

    2014-01-01

    The South Tianshan Orogen and adjacent regions of Central Asia are located in the southwestern part of the Central Asian Orogenic Belt. The formation of South Tianshan Orogen was a diachronous, scissors-like process, which took place during the Palaeozoic, and its western segment was accepted as a site of the final collision between the Tarim Craton and the North Asian continent, which occurred in the late Palaeozoic. However, the post-collisional tectonic evolution of the South Tianshan Orogen and adjacent regions remains debatable. Based on previous studies and recent geochronogical data, we suggest that the final collision between the Tarim Craton and the North Asian continent occurred during the late Carboniferous. Therefore, the Permian was a period of intracontinental environment in the southern Tianshan and adjacent regions. We propose that an earlier, small-scale intraplate orogenic stage occurred in late Permian to Triassic time, which was the first intraplate process in the South Tianshan Orogen and adjacent regions. The later large-scale and well-known Neogene to Quaternary intraplate orogeny was induced by the collision between the India subcontinent and the Eurasian plate. The paper presents a new evolutionary model for the South Tianshan Orogen and adjacent regions, which includes seven stages: (I) late Ordovicianeearly Silurian opening of the South Tianshan Ocean;(II) middle Silurianemiddle Devonian subduction of the South Tianshan Ocean beneath an active margin of the North Asian continent; (III) late Devonianelate Carboniferous closure of the South Tianshan Ocean and collision between the Kazakhstan-Yili and Tarim continental blocks;(IV) early Permian post-collisional magmatism and rifting;(V) late PermianeTriassic the first intraplate orogeny;(VI) JurassicePalaeogene tectonic stagnation and (VII) NeoceneeQuaternary intraplate orogeny.

  16. The miscarriages of Justice in late Qing Dynasty——analysis focused on the original trial Judge Liu Xitong In the case of Yang Naiwu and Xiao Baicai

    Institute of Scientific and Technical Information of China (English)

    ZHENG Ding; YANG Ang

    2006-01-01

    This article introduces the case of Yang Naiwu and Xiao Baicai,a famous case in late imperial China,and its important value for the study of legal history of the Qing Dynasty.Based on the analysis of this case,this article focuses on the issue of the responsibility of the magistrate Liu xitong,the judge of this ease,who analyzed the mentation of his miscarriage under the pressure of the rules about judges responsibilities in their judgment through which reveal the stimulation and passive infection of the judgment of the judges.

  17. Linking Tarim Basin sea retreat (west China) and Asian aridification in the late Eocene

    NARCIS (Netherlands)

    Bosboom, R.; Dupont-Nivet, G.; Grothe, A.; Brinkhuis, H.; Villa, G.; Mandic, O.; Stoica, M.; Huang, W.; Yang, W.; Guo, Z.; Krijgsman, W.

    2014-01-01

    The Tarim Basin in western China formed the easternmost margin of a shallow epicontinental sea that extended across Eurasia and was well connected to the western Tethys during the Paleogene. Climate modelling studies suggest that the westward retreat of this sea from Central Asia may have been as im

  18. Succession and global correlation of Late Tremadoc graptolite zones from South China

    Institute of Scientific and Technical Information of China (English)

    Bernd-D.; ERDTMANN

    2009-01-01

    The Tremadocian is the first stage of the Ordovician System and is subdivided into two parts in general. The Upper Tremadocian, spanning a temporal interval of ca. 8 Ma, yields graptolite faunas crucial for biostratigraphic division and correlation in high resolution. Relatively complete successions of Upper Tremadoc graptolite zones have been proposed in Scandinavia, and North and South America. In South China, the coeval graptolite strata are widespread in deep water facies, but the successions of grapto- lite zones recognized so far are quite incomplete and thus very difficult to be correlated with those in other countries. In recent years, we have sampled bed by bed the Nanba section in the Yiyang area, Hunan Province and, below the Tetragraptus approximatus Zone, identified four Upper Tremadoc graptolite zones in descending order: the Hunnegraptus copiosus Zone, the Araneograptus murrayi Zone, the Aorograptus victoriae Zone and the Adelograptus tenellus Zone. To date, the Nanba section is the only section in China that presents a relatively complete and globally comparable succession of Upper Tremadoc graptolite zones. Therefore, this study not only confirms the existence of some Upper Tremadoc graptolite zones that were never found before in China, but also facilitates a highly resolved division and correlation for the Upper Tremadoc graptolite strata in China.

  19. New magnetochronology of Late Miocene mammal fauna, NE Tibetan Plateau, China : Mammal migration and paleoenvironments

    NARCIS (Netherlands)

    Ao, Hong; Zhang, Peng; Dekkers, Mark J.; Roberts, Andrew P.; An, Zhisheng; Li, Yongxiang; Lu, Fengyan; Lin, Shan; Li, Xingwen

    2016-01-01

    Lanzhou Basin lies on the northeastern margin of the Tibetan Plateau in western China and is a rich source of Oligocene-Miocene mammalian fossils. Obtaining precise age determinations for these fossils is important to address key questions concerning mammalian and environmental evolution in Asia

  20. Lithology, kinematics and geochronology related to Late Mesozoic basin-mountain evolution in the Nanxiong-Zhuguang area, South China

    Institute of Scientific and Technical Information of China (English)

    SHU; Liangshu; DENG; Ping; WANG; Bin; TAN; Zhengzhong; YU

    2004-01-01

    The Nanxiong red-bed basin and its adjacent Zhuguang granite form a distinctive basin-mountain landform in the Nanling region, South China. Research results suggest that the Zhuguang granite is a polyphase composite pluton developed on the metamorphic basement of the paleo-Tethys-paleo-Asian tectonic regime and possesses geometrical and kinematic features of hot-doming extensional tectonics at the middle-upper crustal level, which is considered as a magmatic complex that resulted from the collision-orogeny during the Indosinian Period, the subduction-consuming during the Early Yanshanian Period and the intra-continental basaltic underplating and deep-seated geodynamics during the Late Yanshanian Period. The Nanxiong basin is a Late Cretaceous-Paleogene asymmetric faulted basin that is characterized by a fault boundary on the northern side and an uncomformable boundary on the southern side, its deposit center was migrated gradually from south to north. Structural kinematic results on the basin-mountain coupled zone demonstrate that the ductile and the brittle rheological layers show a quite coincident sense of shear, implying that it is a continuous process from the ductile extensional deformation followed by locally sinistral strike-slip shear at a middle-crustal level to the brittle tensional deformation at a upper-crustal level during formation of granitic doming extensional tectonics. The Zhuguang granite and the Nanxiong faulted basin constructed a semi-graben tectonic system. Lithological and geochemical results suggest that the Late Triassic to Jurassic granitic bodies in the Zhuguang have some similar features: high SiO2, Al2O3, K2O contents, alkalinity index > 2.8, ANKC value > 1.1, LREE-enriched pattern with high REE contents, marked negative Eu anomalies, enrichment in Rb and Th, depletion in Ba and Nb, showing a K-rich and Al-rich calc-alkaline affinity, which suggest a continuous magmatic evolution from Late Triassic to Jurassic. Formation of

  1. Soft-sediment deformation structures in cores from lacustrine slurry deposits of the Late Triassic Yanchang Fm. (central China)

    Science.gov (United States)

    Yang, Renchao; Loon, A. J. (Tom) van; Yin, Wei; Fan, Aiping; Han, Zuozhen

    2016-09-01

    The fine-grained autochthonous sedimentation in the deep part of a Late Triassic lake was frequently interrupted by gravity-induced mass flows. Some of these mass flows were so rich in water that they must have represented slurries. This can be deduced from the soft-sediment deformation structures that abound in cores from these lacustrine deposits which constitute the Yanchang Fm., which is present in the Ordos Basin (central China). The flows and the resulting SSDS were probably triggered by earthquakes, volcanic eruptions, shear stress of gravity flows, and/or the sudden release of overburden-induced excess pore-fluid pressure. The tectonically active setting, the depositional slope and the high sedimentation rate facilitated the development of soft-sediment deformations, which consist mainly of load casts and associated structures such as pseudonodules and flame structures. Sediments with such deformations were occasionally eroded by slurries and became embedded in their deposits.

  2. A new genus of aplodontid rodent (Mammalia, Rodentia) from the late Oligocene of northern Junggar Basin, China.

    Science.gov (United States)

    Bi, Shundong; Meng, Jin; McLean, Sarah; Wu, Wenyu; Ni, Xijun; Ye, Jie

    2013-01-01

    A new genus and species of aplodontid rodent, Proansomys dureensis, from the late Oligocene of the northern Junggar Basin of China is described. The new genus is referred to as Ansomyinae because the ectoloph on the upper cheek teeth, although not fully crested, has attained the same characteristic bucket-handle-shaped configuration as other members of the subfamily. It represents the earliest record of the subfamily yet discovered in Asia and is more plesiomorphic than species of the genus Ansomys in having a partly crested ectoloph, a lower degree of lophodonty, and less complex tooth basins (lacking accessory lophules). Proansomys has transitional features between Prosciurus and Ansomys, suggesting that the Ansomyinae derived from a group of aplodontids related to Prosciurus, as did other advanced aplodontid rodents. This provides new light on the paleobiogeography of the Ansomyinae.

  3. Coupling relationships between brachiopods and Girvanella during the Late Devonian F-F transition in Guilin,South China

    Institute of Scientific and Technical Information of China (English)

    XU Ran; GONG YiMing; ZENG JianWei

    2008-01-01

    The abundance curves derived from area proportions of brachiopods and Girvanella in the thin sections from the Yangdi section,South China,exhibits complex relationships during the Late Devonian Frasnian-Famennian transition.The living activity of brachiopods such as grazing and borrowing did great damage to the growth of Girvanella.However,there was more to just a mere a survival competing relationship between them,Girvanella actually improved marine environments by oxygenating the dysoxic ambient sea-water through photosynthesis in the lower KeUwasser Horizon.Profited from this improvement brachiopods' abundance increased subsequently and suppressed Girvanella again.Nonetheless,without Girvanella's photosynthesis,brachiopods were wiped out by the farther anoxic environments in the upper Kellwasser Horizon.The complex relationships between Girvanella and brachiopods may be a key to unlocking the relationships between geomicrobes and metazoans in the geological overturn periods.

  4. Coupling relationships between brachiopods and Girvanella during the Late Devonian F-F transition in Guilin, South China

    Institute of Scientific and Technical Information of China (English)

    2008-01-01

    The abundance curves derived from area proportions of brachiopods and Girvanella in the thin sections from the Yangdi section, South China, exhibits complex relationships during the Late Devonian Frasnian-Famennian transition. The living activity of brachiopods such as grazing and borrowing did great damage to the growth of Girvanella. However, there was more to just a mere a survival competing relationship between them, Girvanella actually improved marine environments by oxygenating the dysoxic ambient sea-water through photosynthesis in the lower Kellwasser Horizon. Profited from this improvement brachiopods’ abundance increased subsequently and suppressed Girvanella again. Nonetheless, without Girvanella’s photosynthesis, brachiopods were wiped out by the farther anoxic environments in the upper Kellwasser Horizon. The complex relationships between Girvanella and brachiopods may be a key to unlocking the relationships between geomicrobes and metazoans in the geological overturn periods.

  5. Climatic and ecological implications of Late Pliocene palynoflora from Longling, Yunnan, China

    Energy Technology Data Exchange (ETDEWEB)

    Xu, J.X.; Ferguson, D.K.; Li, C.S.; Wang, Y.F.; Du, N.Q. [Chinese Academy of Science, Beijing (China). Inst. of Botany

    2004-07-01

    The Longling Coal Mine (W. Yunnan) is situated in an area of substantial geotectonic activity. Its Late Pliocene palynollora is of considerable interest, since the area represents a centre of biodiversity.Eighty-two palynomorphs belonging to 61 families were recovered from the lignite. The palynoflora is dominated by angiosperms (68.3%), with ferns (24.4%), gymnosperms (4.9%) and algae (2.4%). Comparisons indicate that most of the palynoflora was derived from the Montane Humid Evergreen Broad-leaved Forest, with lesser contributions from the Tsuga dumosa Forest and Evergreen Coniferous Broad-leaved Mixed Forest, as well as the Montane Mossy Evergreen Broad-leaved Forest. This indicates that the Late Pliocene climate was cooler than that of the present. In the course of the accumulation of the lignite, the climate underwent five major phases of warming and cooling.

  6. Study on REEs as tracers for late permian coal measures in Bijie City, Guizhou Province, China

    Institute of Scientific and Technical Information of China (English)

    WANG Qiang; YANG Ruidong

    2008-01-01

    Analyses of Rare Earth Elements (REEs) in 13 coal samples collected from Late Permian coal measures of Bijie City in western Guizhon Province were conducted using Inductively Coupled Plasma-Mass-Spectrometry (ICP-MS). The results indicated that REEs patterns were not controlled by materials from the sea, whereas the contribution of land plants was about 1%. The major sources of REEs were from terrigenous material as indicated by negative Eu anomaly. There were similar distribution curves of REEs between Bijie's coal and Emeishan basalt. M12 coal seam, which had the highest ∑REE, appeared near the boundary between Longtan Formation and Changxing Formation, which was closely correlated to the eruption of Emeishan basalt. The Emeishan basalt contributed to REEs enrichment of M12. So the sources of REEs were controlled by terrigenous material, and the Emeishan basalt was the predominant source of terrigenous material, which dominated the enrichment and pattern of REEs in Late Permian coal measure from Bijie.

  7. Paleoecology of Late Carboniferous Phylloid Algae in Southern Guizhou,SW China

    Institute of Scientific and Technical Information of China (English)

    2007-01-01

    Phylloid algae are important reef-builders in the late Carboniferous. This paper focuses on the paleoecology of phylloid algae in the Late Carboniferous on well-exposed reefs in Ziyun County,Guizhou Province. Phylloid algae growing closely packed are attached via holdfast or similar structure to substrate. They were growing in environments such as shallow water, photic zone and below the wave base with medium energy currents. They have a variety of morphological forms, such as single cup-shaped, cabbage-shaped and clustering cup-shaped. The thalli are of certain tenacity and intensity. In the areas dominated by phylloid algae, other marine organisms are relatively scarce.Obviously, phylloid algae are stronger competitors for living space than other co-occurring organisms.

  8. The evolution of the lepidosaurian lower temporal bar: new perspectives from the Late Cretaceous of South China.

    Science.gov (United States)

    Mo, Jin-You; Xu, Xing; Evans, Susan E

    2010-01-22

    Until recently, it was considered axiomatic that the skull of lizards and snakes arose from that of a diapsid ancestor by loss of the lower temporal bar. The presence of the bar in the living New Zealand Tuatara, Sphenodon, was thus considered primitive, corroborating its status as a 'living fossil'. A combination of new fossils and rigorous phylogeny has demonstrated unequivocally that the absence of the bar is the primitive lepidosaurian condition, prompting questions as to its function. Here we describe new material of Tianyusaurus, a remarkable lizard from the Late Cretaceous of China that is paradoxical in having a complete lower temporal bar and a fixed quadrate. New material from Jiangxi Province is more complete and less distorted than the original holotype. Tianyusaurus is shown to be a member of the Boreoteiioidea, a successful clade of large herbivorous lizards that were dispersed through eastern Asia, Europe and North America in the Late Cretaceous, but disappeared in the end-Cretaceous extinction. A unique combination of characters suggests that Tianyusaurus took food items requiring a large gape.

  9. Ar-Ar geochronology of Late Mesozoic volcanic rocks from the Yanji area,NE China and tectonic implications

    Institute of Scientific and Technical Information of China (English)

    LI ChaoWen; GUO Feng; FAN WeiMing; GAO XiaoFeng

    2007-01-01

    Ar-Ar dating results of late Mesozoic-Cenozoic volcanic rocks from the Yanji area, NE China provide a new volcano-sedimentary stratigraphic framework. The previously defined "Triassic-Jurassic" volcanic rocks(including those from Sanxianling, Tuntianying, Tianqiaoling and Jingouling Fms.)were erupted during 118-106Ma,corresponding to Early Cretaceous. The new eruption age span is slightly younger than the main stage(130-120 Ma)of the extensive magmatism in the eastern Central Asian Orogenic Belt and its adjacent regions. Subduction-related adakites occurring in the previously defined Quanshuicun Fm. Were extruded at ca.55 Ma. Based on these new Ar-Ar ages, the late Mesozoic to Palaeocene volcano-sedimentary sequences is rebuilt as:Tuopangou Fm., Sanxianling/Tuntianying Fm.(118-115 Ma),Malugou/Tianqiaoling Fm.(K1),Huoshanyan/Jingouling Fm.(108-106 Ma),Changcai Fm.(K2),Quanshuicun Fm.(~55 Ma)and Dalazi Fm. Our results suggest that subduction of the Palaeo-Pacific Ocean beneath the East Asian continental margin occurred during 106to 55 Ma. Consistent with the paleomagnetic observations and magmatic records which indicated that the Izanagi-Farallon ridge subduction beneath the southwestern Japan took place during 95-65 Ma.

  10. Ar-Ar geochronology of Late Mesozoic volcanic rocks from the Yanji area, NE China and tectonic implications

    Institute of Scientific and Technical Information of China (English)

    2007-01-01

    Ar-Ar dating results of late Mesozoic-Cenozoic volcanic rocks from the Yanji area, NE China provide a new volcano-sedimentary stratigraphic framework. The previously defined “Triassic-Jurassic” volcanic rocks (including those from Sanxianling, Tuntianying, Tianqiaoling and Jingouling Fms.) were erupted during 118―106 Ma, corresponding to Early Cretaceous. The new eruption age span is slightly younger than the main stage (130―120 Ma) of the extensive magmatism in the eastern Central Asian Orogenic Belt and its adjacent regions. Subduction-related adakites occurring in the previously defined Quanshuicun Fm. were extruded at ca. 55 Ma. Based on these new Ar-Ar ages, the late Mesozoic to Palaeocene volcano-sedimentary sequences is rebuilt as: Tuopangou Fm., Sanxianling/Tuntianying Fm. (118―115 Ma), Malugou/Tianqiaoling Fm. (K1), Huoshanyan/Jingouling Fm. (108―106 Ma), Changcai Fm. (K2), Quanshuicun Fm. (~55 Ma) and Dalazi Fm. Our results suggest that subduction of the Pa- laeo-Pacific Ocean beneath the East Asian continental margin occurred during 106 to 55 Ma, consistent with the paleomagnetic observations and magmatic records which indicated that the Izanagi-Farallon ridge subduction beneath the southwestern Japan took place during 95―65 Ma.

  11. A New High-resolution Late Glacial-Holocene Climatic Record from Eastern Nanling Mountains in South China

    Institute of Scientific and Technical Information of China (English)

    XUE Jibin; ZHONG Wei; ZHENG Yanming; MA Qiaohong; CAI Ying; OUYANG Jun

    2009-01-01

    A 350-cm-long sediment core sequence from Dahu Swamp situated in the eastern Nanling Mountains was selected for high-resolution paleoclimatic reconstruction since the Late Glacial period. The multi-proxy records of this paper reveal several evidently dry and cold events that may coincide with the Oldest Dryas, the Older Dryas, the Younger Dryas in the late deglacial period. Two relatively wetter and warmer phases occurred in ca. 15,000-14,400 cal yr B.P. And 13,500-12,800 cal yr B.P. Respectively may correspond to the Boiling and Allerod warming events. The Younger Dryas event(ca. 12,800-11,500 cal yr B.P.) revealed by multi-proxies was characterized by relatively colder and drier climate. A warmer and wetter climate, occurred in ca. 10,000-6000 cal yr B.P., was consistent with the Holo-cene Optimum, which coincided with the maximum Northern Hemisphere insolation. The "8.2kyr cool event" and even the "8.8kyr cool event" were indicated as well from our sediment core. A dry mid-Holocene period (ca. 6000-3000 cal yr B.P.) indicated by multi-proxies does not follow the traditional concept of the wet mid-Holoeene conditions observed in other regions in China.

  12. Imperial Valley College 2+2+2 Project Handbook.

    Science.gov (United States)

    Marquez, Ralph

    This handbook of the Imperial Valley College (IVC) 2+2+2 Project provides an overview of the development of an articulated education program for business and law enforcement careers, involving six local high schools and San Diego State University, Imperial Valley Campus. Following a brief introduction to the 2+2+2 project in section I, section II…

  13. A Study of Imperial Maids Life Through Tangs Poetry

    Directory of Open Access Journals (Sweden)

    Xuc Lin

    2012-09-01

    Full Text Available Article observed the life of Tangs imperial maids through the poetry of Tang Dynasty. . Imperial maids were started from Sui Dynasty, especially Emperor Sui Yangdis period, and Tangs imperial maids were many. Emperor with various kind of reasons, in most every year would choose some girls and took them into his palace and they worked as imperial maids. They were girls from ordinary people, respectable, and noble families. Those girls who once entered imperial palace, theyb would be very hard to come out. They had to obey the regulation in the palace. Through some poetry it could be portrayed the imperial maids lifetime in serving the emperor, imperial concubines and got rest after midnight. Except for working, they werent able to come out from palace, they couldnt go home to visit their family, even got married, their lives were full of loneliness. If they were sick, or old, the emperor wouldnt like them anymore, they would be sent away anytime. Even if they left imperial palace, and got their freedom, but most of them lived tragically.

  14. Concentrations and modes of occurrence of trace elements in the Late Permian coals from the Puan Coalfield, southwestern Guizhou, China

    Energy Technology Data Exchange (ETDEWEB)

    Yang, J.Y. [Xian University of Science & Technology, Xian (China)

    2006-12-15

    The concentration, mode of occurrence, and origin of trace elements in the Late Permian coals from the Puan Coalfield, southwestern Guizhou, China, were examined using inductively coupled plasma-mass spectrometry (ICP-MS), X-ray fluorescence (XRF), cold-vapor atomic absorption spectrometry (CV-AAS), ion-selective electrode method (ISE), sequential chemical extraction procedure (SCEP), scanning electron microscopy equipped with energy-dispersive X-ray (SEM-EDX), and optical microscope. Results show that minerals in the No. 2 Coal from the Puan Coalfield were mainly made up of epigenetic pyrite of low-temperature hydrothermal fluid origin and kaolinite of detrital terrigenous origin. Elements including As (36.9 {mu} g/g), Cd (10.2 {mu} g/g), Cr (167.3 {mu} g/g), Cu (365.4 {mu} g/g), Hg (2.82 {mu} g/g), Mo (92.6 {mu} g/g), Ni (82.6 {mu} g/g), Pb (184.6 {mu} g/g), Se (6.23 {mu} g/g), Zn (242.3 {mu} g/g), and U (132.7 {mu} g/g) are significantly enriched in the No. 2 Coal from the Puan Coalfield. However, concentrations of trace elements in the other four coals, the No. 1, No. 8, No. 11, and No. 18 Coals, were close to the usual ranges found for Guizhou of China, China, and USA. Results of SEM-EDX and SCEP showed that As, Cd, Hg, Mo, Ni, Pb, and Zn occur mainly in veined pyrite, while Cr, Cu, and U distribute mainly in kaolinite, indicating that the low-temperature hydrothermal fluid and detrital materials of terrigenous origin are the main contributors to the enrichment of these trace elements in the No. 2 Coal.

  15. Establishment of the South Asian high over the Indo-China Peninsula during late spring to summer

    Science.gov (United States)

    Wang, Lijuan; Dai, Aiguo; Guo, Shuaihong; Ge, Jing

    2017-02-01

    The establishment of the upper-level South Asian high (SAH) over the Indo-China Peninsula (ICP) during late boreal spring and its possible causes are investigated using long-term NCEP-NCAR and ERA-40 reanalysis and satellite-observed OLR data. Results show that, from early March to mid-April, deep convection stays south of 6°N over the northern Sumatran islands. As the maximum solar radiation moves over the latitudes of the ICP (10°-20°N) in late April, the air over the ICP becomes unstable. It ascends over the ICP and descends over the adjacent waters to the east and west. This triggers deep convection over the ICP that induces large latent heating and strong updrafts and upper-level divergence, leading to the formation of an upper-level anticyclonic circulation and the SAH over the ICP. During early to mid-May, deep convection over the ICP intensifies and extends northwards to the adjacent waters. Strong latent heating from deep convection enhances and maintains the strong updrafts and upper-level divergence, and the SAH is fully established by mid-May. Thus, the seasonal maximum solar heating and the land-sea contrast around the ICP provide the basic conditions for deep convection to occur preferentially over the ICP, which leads to the formation of the SAH over the ICP from late April to mid-May. Simulations using RegCM4 also indicate that the diabatic heating over the ICP is conducive to the generation and development of upperlevel anticyclonic circulation, which leads to an earlier establishment of the SAH.

  16. Alluvial fan facies of the Yongchong Basin: Implications for tectonic and paleoclimatic changes during Late Cretaceous in SE China

    Science.gov (United States)

    Chen, Liuqin; Steel, Ronald J.; Guo, Fusheng; Olariu, Cornel; Gong, Chenglin

    2017-02-01

    Late Cretaceous continental redbeds, the Guifeng Group of the Yongchong Basin in SE China have been investigated to conduct detailed fan facies description and interpretation. Tectonic activities determined the alluvial fan development along the basin margin, but the alluvial facies was linked with paleoclimate changes. The Guifeng Group is divided into the Hekou, Tangbian and Lianhe formations in ascending order. The Hekou conglomerates are typically polymict, moderately sorted with erosional bases, cut-and-fill features, normal grading and sieve deposits, representing dominant stream-flows on alluvial fans during the initial opening stage of the basin infill. The Tangbian Formation, however, is characterized by structureless fine-grained sediments with dispersed coarse clasts, and couplets of conglomerate and sandstone or siltstone and mudstone, recording a change to a playa and ephemeral lake environments with occasional stream flooding, thus indicating a basin expanding stage. The hallmark of the Lianhe Formation is disorganized, poorly sorted conglomerates lack of erosional bases, and a wide particle-size range from clay to boulders together reflect mud-rich debris-flows accumulating on fans, likely related to reactivation of faulting along the northwestern mountain fronts during a post-rift stage. The depositional system changes from stream-flows up through playa with ephemeral streams to debris-flows during the accumulation of the three formations are thus attributed to different source rocks and climatic conditions. Therefore, the fluvial-dominated fans of the Hekou Formation recorded a subhumid paleoclimate (Coniacian-Santonian Age). The dominant semiarid climate during the Campanian Age produced abundant fine-grained sediments in the playa and ephemeral lake environments of the Tangbian Formation. A climatic change towards more humidity during the late stage of the Guifeng Group (Maastrichtian Age) probably yielded high deposition rate of coarse clasts in

  17. Late Cretaceous lithospheric extension in SE China: Constraints from volcanic rocks in Hainan Island

    Science.gov (United States)

    Zhou, Yun; Liang, Xinquan; Kröner, Alfred; Cai, Yongfeng; Shao, Tongbin; Wen, Shunv; Jiang, Ying; Fu, Jiangang; Wang, Ce; Dong, Chaoge

    2015-09-01

    Petrological, geochemical and in-situ zircon U-Pb dating and Hf-isotope analyses have been carried out on a suite of basalt-andesite-rhyolite volcanic rocks exposed in the Liuluocun area, Hainan Island, SE China. Zircon analyses show that these volcanic rocks crystallized in the Early Cretaceous (ca. 102 Ma). The basalts are characterized by low MgO contents and mg-numbers but high rare earth element, high field strength element and large ion lithophile element contents and Nb-Ta negative anomalies. They have relatively uniform Sr-Nd isotope compositions with εNd(t) values of - 4.09 to - 3.63. The andesites show enrichment of high field strength element and rare earth element with negligible Eu anomalies. They have εNd(t) values of - 2.35 to - 3.88 and εHf(t) values of - 9.73 to - 1.13. The rhyolites have high K2O and SiO2 contents. They are characterized by prominent Eu, P and Ti negative anomalies and enrichment in large ion lithophile element, and show εHf(t) values of - 7.51 to + 0.47 and εNd(t) values of - 2.49 to - 2.69. Petrogenetic analysis indicates that the Liuluocun volcanic rocks were produced by incomplete reaction of the mantle wedge peridotite with felsic melts derived from partial melting of subducted sediment. All these characteristics, combined with geological observations, suggest that their formation was related to regional lithospheric extension in the South China Craton during the Early Cretaceous, which may have been caused by subduction of the Paleo-Pacific plate beneath the continental plate of China.

  18. Late Changhsingian radiolarian biostratigraphy from Guangxi,South China and its correlation to conodonts

    Institute of Scientific and Technical Information of China (English)

    2008-01-01

    A well-preserved, abundant radiolarian fauna was obtained from three sections: the Dongpan, Liuqiao, and Paibi sections, in southern Guangxi, South China. Sixteen species belonging to Albaillella and Neoalbaillella, including seven undetermined species, are recognized. On the basis of stratigraphic distribution of these species, two radiolarian zones, the Albaillella triangularis Zone and the Albaillella yaoi Zone, are established. The correlation between radiolarian zones and conodont zones is suggested based on the discovery of coexisting conodonts. Albaillella triangularis and Albaillella yaoi zones correspond to Neogondolella postwangi and Neogondolella yini zones respectively.

  19. Late Paleozoic rift-related basalts from central Inner Mongolia, China

    Science.gov (United States)

    Zhu, Wenping; Tian, Wei; Wei, Chunjing; Shao, Ji-an; Fu, Bin; Fanning, C. Mark; Chen, Mimi; Wang, Bin

    2017-08-01

    Late Paleozoic basaltic volcanism widely occurred in central Inner Mongolia, the southeastern part of the Central Asia Orogenic Blet (CAOB). Three volcanic pulses are identified by ion microprobe (SHRIMP II) zircon U-Pb analysis, which are Late Carboniferous (ca. 315 Ma), the latest Carboniferous (ca. 303 Ma) and early Permian (ca. 284 Ma). Basalts in the earliest stage are characterized by flat HREE, depletion in Nb and Ta, MORB-like Th/Yb ratios and depleted mantle (DM)-like Hf isotopic ratios. These are similar to forearc basalts, that have been generated by melting of a fluxed depleted mantle in an extensional environment. The latest Carboniferous basalts (sample D1363) have no Zr-Hf anomalies, relatively radiogenic Hf isotopic ratios (εHf(t) = +12.1 to +19.7) and high δ18O values up to 8.5‰, VSMOW. These are likely to be magmas originated from decompressional melting of a depleted mantle that interacted with ocean floor pillow basalts during their ascending through the crust. The early Permian sample D1380 have variable 206Pb/238U zircon ages with an interpreted magma crystallization age of 284.4 ± 2.5 Ma. These zircons have scattered Hf isotope (εHf(t) = +5 to +14) and δ18O (1.8-11.0‰, VSMOW), which suggest the involvement of a relatively enriched mantle source. Overall the temporal evolution of the Late Paleozoic basaltic volcanism from central Inner Mongolia suggests a rift-related tectonic setting.

  20. Discovery of sponge body fossils from the late Meishucunian (Cambrian) at Jinsha, Guizhou, south China

    Institute of Scientific and Technical Information of China (English)

    YANG Xinglian; ZHAO Yuanlong; WANG Yue; WANG Pingli

    2005-01-01

    Here we report discovery of a sponge body fossil Triticispongia sp. from the base of lower Cambrian Niutitang Formation at Jinsha, Guizhou. Stratigraphically, the fossil horizon is located below Ni-Mo ore layer with the Niutitang Biota above, and is equivalent to the late Meishucunian. The species is global in shape with skeletons composed of stauractins and monaxons. Triticispongia sp. reported here may be the earliest sponge body fossils of Cambrian, which provides new informationfor understanding early evolution and radiation of sponge animals.

  1. The Imperial College Thermophysical Properties Data Centre

    Science.gov (United States)

    Angus, S.; Cole, W. A.; Craven, R.; de Reuck, K. M.; Trengove, R. D.; Wakeham, W. A.

    1986-07-01

    The IUPAC Thermodynamic Tables Project Centre in London has at its disposal considerable expertise on the production and utilization of high-accuracy equations of state which represent the thermodynamic properties of substances. For some years they have been content to propagate this information by the traditional method of book production, but the increasing use of the computer in industry for process design has shown that an additional method was needed. The setting up of the IUPAC Transport Properties Project Centre, also at Imperial College, whose products would also be in demand by industry, afforded the occasion for a new look at the problem. The solution has been to set up the Imperial College Thermophysical Properties Data Centre, which embraces the two IUPAC Project Centres, and for it to establish a link with the existing Physical Properties Data Service of the Institution of Chemical Engineers, thus providing for the dissemination of the available information without involving the Centres in problems such as those of marketing and advertising. This paper outlines the activities of the Centres and discusses the problems in bringing their products to the attention of industry in suitable form.

  2. Imperial climatographies from Tyrol to Turkestan.

    Science.gov (United States)

    Coen, Deborah R

    2011-01-01

    This article argues for the importance of Europe's continental empires, Habsburg and Romanov, to the emergence of a physical-dynamical model of the global climate before World War I. It begins to identify a set of questions and methods that were distinctive of climatology as a continental-imperial science of "regionalization" with a global vision. The focus is on studies of mountain climatology by Heinrich von Ficker and A. I. Voeikov in the ecologically vulnerable regions of Tyrol and western Turkestan. This continental-imperial context deserves historians' attention because it suggests a new model for the globalization of knowledge: not simply a matter of scaling up, globalization must be understood as a process of seeing across scales, of recognizing causal connections between local, regional, and planetary phenomena. "For a change, the material for a dissertation was procured mostly with the feet." Heinz Ficker, of his research on the föhn wind in Tyrol, 1906 "Science is something beautiful, especially when you can do it on horseback." Ficker in his journal in 1913, in a mountain pass in central Asia.

  3. Biotic recovery from the Late Devonian F-F mass extinction event in China

    Institute of Scientific and Technical Information of China (English)

    廖卫华

    2002-01-01

    The Frasnian-Famennian (F-F) mass extinction is one of the five great extinctions of marine life during the Phanerozoic. The F-F event killed most of the Devonian reefs, the characteristic Devonian corals, stromatoporoids, bryozoans, nearly all tentaculites, a few superfamilies of brachiopods, such as Atrypacea and Pentameracea and some important elements of goniatites, such as Manticoceras.``The end-Frasnian was a phase of mass extinction. A large number of shelly benthos were killed by the F-F event. Early and middle Famennian was the survival interval. The marine faunas were very rare at that time. The late Famennian was the recovery interval. There appeared to have many new taxa in the Strunian stage. It lacked a radiation interval in Late Devonian Famennian because another event (the D-C mass extinction) happened at the Devonian-Carboniferous boundary.``Several causes for the F-F mass extinction have been proposed by some geologists, which have been grouped into two broad types, terrestrial and extraterrestrial. The former is related to sea level changes, climate changes and anoxic water event. The latter is linked with some forms of meteorite impact.``A large-scale eustatic change of sea level and black shales representing an anoxic environment has been invoked to explain one of the causes for the F-F mass extinction.``

  4. Features of Late Cenozoic Deepwater Sedimentation in Southern Qiongdongnan Basin,Northwestern South China Sea

    Institute of Scientific and Technical Information of China (English)

    Yuan Shengqiang; Yao Genshun; Lü Fuliang; Hu Bing; He Xiaosu; Wang Bin; Li Li

    2009-01-01

    Based on high resolution 2D and 3D seismic data acquired in recent years,using sequence stratigraphy analysis and geophysical methods,we discuss the features of Late Cenozoic deepwater sedimentation in the southern Qiongdongnan (琼东南) basin.The study area entered a bathyal slope environment in the Miocene.The channel developed in the Sanya (三亚) Formation was controlled by a fault break,and its shingled seismic characteristics represent multiple erosion and fill,which may indicate that turbidite current developed in the slope environment.The polygon faults found in mudstone of the Meishan (梅山) Formation represent the deepwater hungry sedimentary environment.The large-scale channels developed on the top of HuangUu (黄流) Formation could be the result of a big sea level drop and an increase of sediment supply.The fantastic turbidite channel developed in Late Quaternary in the slope environment has "fan-like" body and long frontal tiny avuision channel The analysis of these features suggests that the sediment supply of the study area in the post-rifting period was dominant from the Vietnam uplift in the southwest.These deepwater sedimentary features could be potential reservoirs or migration pathways for deepwater petroleum systems.

  5. Estimation of the shortening rate since late Pleistocene in the Aksu area on the southern flank of the Tianshan, China

    Institute of Scientific and Technical Information of China (English)

    WANG; Xin

    2001-01-01

    [1]Molnar, P., Tapponnier, P., Cenozoic tectonics of Asia: Effects on a continental collision, Science, 1975, 189: 419-426.[2]Molnar, P., Deng Qidong, Faulting associated with large earthquakes and the average rate of deformation in central and eastern Asia, J. Geophys. Res., 1984, 89: 6203-6227.[3]Hendrix, M. S., Dumitru, T. A., Graham, S. A., Late Oligocene-early Miocene unroofing in the Chinese Tianshan: An early effect of the India-Asia collision, Geology, 1994, 22: 487-490.[4]Sobel, R. E., Dumitru, T. A., Thrusting and exhumation around the margins of the western Tarim Basin during the India-Asia collision, J. Geophys. Res., 1997, 102: 5043-5063.[5]Ghose, S., Hamburger, M. W., Virieux, J., Three-dimentional velocity structure and earthquake locations beneath the northern Tianshan of Kyrgyzstan, central Asia, J. Geophys. Res., 1998, 103: 2725-2748.[6]Ghose, S., Hamburger, M. W., Ammon, C. J., Source parameters of moderate-sized earthquakes in the Tianshan, central Asia from regional moment tensor inversion, Geophys. Res. lett., 1998, 25: 3181-3184.[7]Abdrakhmatov, K. Ye, Aldazhanov, S. A., Hager, B. H. et al., Relatively recent construction of the Tianshan inferred from GPS measurements of present-day curstal deformation rates, Nature, 1996, 384: 450-452.[8]Wang Qi, Ding Guoyu, Qiao Xuejun et al., Present-day Tianshan's quick shortening and the south-north block's relative movement, Chinese Science Bulletin (in Chinese), 2000, 45(14): 1543-1547.[9]Zhu Wenyao, Wang Xiaoya, Chen Yuyi et al., Crustal motion of Chinese mainland monitored by GPS, Science in China, Ser. D, 2000, 43(2): 394-400.[10]Avouac, J. P., Tapponnier, P., Bai, M. et al., Active thrusting and folding along the northern Tianshan and late cenozoic rotation of the Tarim relative to Dzungaria and Kazakhstan, J. Geopgys. Res., 1993, 98: 6755-6804.[11]Burtman, V. S.,Skobelev, S. F., Molnar, P., Late cenozoic slip on the Talas-Ferghana fault, the Tianshan

  6. Archaeopteris halliana from the Late Devonian(Famennian) of Anhui Province,China

    Institute of Scientific and Technical Information of China (English)

    GUO Yun; WANG Deming

    2009-01-01

    New materials from the Upper Devonian(Famennian)Wutong Formation of Chizhou District,Anhui Province,South China,allow description of fertile and sterile characters of Archaeopteris halliana.This plant has penultimate axes attached by sterile leaves and paired ultimate branches in the same ontogenetic spiral.Sterile leaves are narrowly cuneate in shape and bear distal margins dissected deeply.These leaves are spirally arranged on sterile ultimate axes.Non-laminated sporophyllls occur spirally on the ultimate axes and bifurcate once or twice.Elongate sporangia with longitudinal dehiscence are borne adaxially below or above the dividing points of the sporophylis.Despite the leaf shape resembling that of Archaeopteris macilenta,our plant is assigned to A.halliana because of its non-laminated sporophylls.Fertile characters should be given priority or enough consideration in identifying species of Archaeopteris.

  7. Neotectonic impact and Palaeohydrology of Gaxun Nur Basin (NW China) during the Late Quaternary

    Science.gov (United States)

    Hartmann, K.; Wünnemann, B.; Zhang, H.

    2009-04-01

    . The displacements of lake sediments at the southern margin of the modern Gaxun Nur basin imply a subsidence of at least 0.81m/1000 yrs since 25 kyr as a result of a pull-apart development due to the left stepping faults in a sinistral system. Frequently lakes are of tectonic origin. Their sediments and nearby catchment topography provide an excellent archive for reconstructing young tectonic movement. In this respect palaeohydrological reconstruction of lake catchments has to consider the occurrence of tectonic. In classical proxies of hydrological changes, both signals in the same archive interfere with each other. Complex system variables derived from large datasets by multivariate approaches are able to dissolve the processes (Hartmann & Wünnemann 2007). References Hartmann, K. (2003): Spätpleistozäne und holozäne Morphodynamik im nördlichen Gaxun Nur Becken, Innere Mongolei, NW China. Ph D-Thesis, Dept. of Geosciences, Freie Universitaet Berlin. Hartmann, K. & B. Wünnemann (2009): Hydrological changes and Holocene climate variations in NW China, inferred from lake sediments of Juyanze palaeolake by factor analyses. Quaternary International 194, 28-44. Hölz, S., Polag, D., Becken, M. Fiedler-Volmer, R., Zhang, HC., Hartmann,K., Burkhardt, H. (2007): Electromagnetic and Geoelectric Investigation of the Gurinai Structure, Inner Mongolia, NW China. Tectonophysics 445, (Issues 1-2): 26-48. Wünnemann, B., Hartmann, K., Altmann, N., Pachur, H.-J., Hambach, U. (2007): Glacial and Interglacial fingerprints from lake deposits in the Gobi Desert, NW China. In: Siroko, F., Clausen & M. Sanchez-Goni (Editors): The Climate of the Past Interglacials, pp. 323-348, Elevier, Amsterdam, N.Y..

  8. A new Mammutidae (Proboscidea, Mammalia) from the Late Miocene of Gansu Province, China.

    Science.gov (United States)

    Mothé, Dimila; Avilla, Leonardo S; Zhao, Desi; Xie, Guangpu; Sun, Boyang

    2016-03-01

    The "Yanghecun specimen", a proboscidean specimen represented by a mandible from Miocene of China and previously described as Gomphotheriidae, is here reviewed and described as a new genus and species of Mammutidae: Sinomammut tobieni. This taxon is a longirostrine mastodon, lacking lower tusks, and bearing a wide last molar with oblique and non-inflated lophids, broad transverse interlophids, and yoke-like wear figures. Phylogenetic analysis of Mammutidae based on dental and mandibular features recovered S. tobieni as sister group of the mastodon Mammut. The longirostrine condition and the well-developed lower incisors seem to be primitive for Mammutidae, while the brevirostry is the derived condition, probably emerged during the middle Miocene (12-11 Mya). However, two derived conditions are recognized to the lower tusks: the absence of lower tusks (S. tobieni) and the occasional presence of vestigial lower tusks (Mammut).

  9. A new Mammutidae (Proboscidea, Mammalia from the Late Miocene of Gansu Province, China

    Directory of Open Access Journals (Sweden)

    DIMILA MOTHÉ

    2016-03-01

    Full Text Available ABSTRACT The "Yanghecun specimen", a proboscidean specimen represented by a mandible from Miocene of China and previously described as Gomphotheriidae, is here reviewed and described as a new genus and species of Mammutidae: Sinomammut tobieni. This taxon is a longirostrine mastodon, lacking lower tusks, and bearing a wide last molar with oblique and non-inflated lophids, broad transverse interlophids, and yoke-like wear figures. Phylogenetic analysis of Mammutidae based on dental and mandibular features recovered S. tobieni as sister group of the mastodon Mammut. The longirostrine condition and the well-developed lower incisors seem to be primitive for Mammutidae, while the brevirostry is the derived condition, probably emerged during the middle Miocene (12-11 Mya. However, two derived conditions are recognized to the lower tusks: the absence of lower tusks (S. tobieni and the occasional presence of vestigial lower tusks (Mammut.

  10. Osteoarchaeological Studies of Human Systemic Stress of Early Urbanization in Late Shang at Anyang, China

    Science.gov (United States)

    Zhang, Hua; Merrett, Deborah C.; Jing, Zhichun; Tang, Jigen; He, Yuling; Yue, Hongbin; Yue, Zhanwei; Yang, Dongya Y.

    2016-01-01

    Through the analysis of human skeletal remains and mortuary practice in Yinxu, this study investigates the impact of early urbanization on the commoners during the Late Shang dynasty (ca. 1250–1046 B.C.). A total of 347 individuals examined in this study represent non-elites who were recovered from two different burial contexts (formally buried in lineage cemeteries and randomly scattered in refuse pits). Frequencies of enamel hypoplasia (childhood stress), cribra orbitalia (childhood stress and frailty) and osteoperiostitis (adult stress) were examined to assess systemic stress exposure. Our results reveal that there was no significant difference in the frequency of enamel hypoplasia between two burial groups and between sexes, suggesting these urban commoners experienced similar stresses during childhood, but significantly elevated levels of cribra orbitalia and osteoperiostitis were observed in the refuse pit female cohort. Theoretically, urbanization would have resulted in increased population density in the urban centre, declining sanitary conditions, and increased risk of resource shortage. Biologically, children would be more vulnerable to such physiological disturbance; as a result, high percentages of enamel hypoplasia (80.9% overall) and cribra orbitalia (30.3% overall) are observed in Yin commoners. Adults continued to suffer from stress, resulting in high frequencies of osteoperiostitis (40.0% total adults); in particular, in the refuse pit females who may also reflect a compound impact of gender inequality. Our data show that the non-elite urban population in the capital city of Late Shang Dynasty had experienced extensive stress exposure due to early urbanization with further social stratification only worsening the situation, and eventually contributing to collapse of the Shang Dynasty. PMID:27050400

  11. Osteoarchaeological Studies of Human Systemic Stress of Early Urbanization in Late Shang at Anyang, China.

    Science.gov (United States)

    Zhang, Hua; Merrett, Deborah C; Jing, Zhichun; Tang, Jigen; He, Yuling; Yue, Hongbin; Yue, Zhanwei; Yang, Dongya Y

    2016-01-01

    Through the analysis of human skeletal remains and mortuary practice in Yinxu, this study investigates the impact of early urbanization on the commoners during the Late Shang dynasty (ca. 1250-1046 B.C.). A total of 347 individuals examined in this study represent non-elites who were recovered from two different burial contexts (formally buried in lineage cemeteries and randomly scattered in refuse pits). Frequencies of enamel hypoplasia (childhood stress), cribra orbitalia (childhood stress and frailty) and osteoperiostitis (adult stress) were examined to assess systemic stress exposure. Our results reveal that there was no significant difference in the frequency of enamel hypoplasia between two burial groups and between sexes, suggesting these urban commoners experienced similar stresses during childhood, but significantly elevated levels of cribra orbitalia and osteoperiostitis were observed in the refuse pit female cohort. Theoretically, urbanization would have resulted in increased population density in the urban centre, declining sanitary conditions, and increased risk of resource shortage. Biologically, children would be more vulnerable to such physiological disturbance; as a result, high percentages of enamel hypoplasia (80.9% overall) and cribra orbitalia (30.3% overall) are observed in Yin commoners. Adults continued to suffer from stress, resulting in high frequencies of osteoperiostitis (40.0% total adults); in particular, in the refuse pit females who may also reflect a compound impact of gender inequality. Our data show that the non-elite urban population in the capital city of Late Shang Dynasty had experienced extensive stress exposure due to early urbanization with further social stratification only worsening the situation, and eventually contributing to collapse of the Shang Dynasty.

  12. On fault evidence for a large earthquake in the late fifteenth century, Eastern Kunlun fault, China

    Science.gov (United States)

    Junlong, Zhang

    2017-06-01

    The EW-trending Kunlun Fault System (KFS) is one of the major left-lateral strike-slip faults on the Tibetan Plateau. It forms the northern boundary of the Bayan Har block. Heretofore, no evidence has been provided for the most recent event (MRE) of the 70-km-long eastern section of the KFS. The studied area is located in the north of the Zoige Basin (northwest Sichuan province) and was recognized by field mapping. Several trenches were excavated and revealed evidence of repeated events in late Holocene. The fault zone is characterized by a distinct 30-60-cm-thick clay fault gouge layer juxtaposing the hanging wall bedrock over unconsolidated late Holocene footwall colluvium and alluvium. The fault zone, hanging wall, and footwall were conformably overlain by undeformed post-MRE deposits. Samples of charred organic material were obtained from the top of the faulted sediments and the base of the unfaulted sediments. Modeling of the age of samples, earthquake yielded a calibrated 2σ radiocarbon age of A.D. 1489 ± 82. Combined with the historical earthquake record, the MRE is dated at A.D. 1488. Based on the over 50 km-long surface rupture, the magnitude of this event is nearly M w 7.0. Our data suggests that a 200-km-long seismic gap could be further divided into the Luocha and Maqu sections. For the last 1000 years, the Maqu section has been inactive, and hence, it is likely that the end of its seismic cycle is approaching, and that there is a potentially significant seismic hazard in eastern Tibet.

  13. Osteoarchaeological Studies of Human Systemic Stress of Early Urbanization in Late Shang at Anyang, China.

    Directory of Open Access Journals (Sweden)

    Hua Zhang

    Full Text Available Through the analysis of human skeletal remains and mortuary practice in Yinxu, this study investigates the impact of early urbanization on the commoners during the Late Shang dynasty (ca. 1250-1046 B.C.. A total of 347 individuals examined in this study represent non-elites who were recovered from two different burial contexts (formally buried in lineage cemeteries and randomly scattered in refuse pits. Frequencies of enamel hypoplasia (childhood stress, cribra orbitalia (childhood stress and frailty and osteoperiostitis (adult stress were examined to assess systemic stress exposure. Our results reveal that there was no significant difference in the frequency of enamel hypoplasia between two burial groups and between sexes, suggesting these urban commoners experienced similar stresses during childhood, but significantly elevated levels of cribra orbitalia and osteoperiostitis were observed in the refuse pit female cohort. Theoretically, urbanization would have resulted in increased population density in the urban centre, declining sanitary conditions, and increased risk of resource shortage. Biologically, children would be more vulnerable to such physiological disturbance; as a result, high percentages of enamel hypoplasia (80.9% overall and cribra orbitalia (30.3% overall are observed in Yin commoners. Adults continued to suffer from stress, resulting in high frequencies of osteoperiostitis (40.0% total adults; in particular, in the refuse pit females who may also reflect a compound impact of gender inequality. Our data show that the non-elite urban population in the capital city of Late Shang Dynasty had experienced extensive stress exposure due to early urbanization with further social stratification only worsening the situation, and eventually contributing to collapse of the Shang Dynasty.

  14. Late Pleistocene to Holocene soil development and environments in the Long Gang Volcanic Field area, Jilin Province, NE China

    Science.gov (United States)

    Sauer, Daniela; Zhang, Xinrong; Knöbel, Jette; Maerker, Lutz

    2014-05-01

    Late Pleistocene to Holocene shifts of climate and vegetation in the Long Gang Volcanic Field in NE China have been reconstructed, e. g. by Steblich et al. (2009), based on Maar lake sediment cores. In this study, we investigated soil development during the Late Pleistocene and Holocene and linked it to the climate and vegetation reported in the literature. Three pedons were described and analyzed on a crater wall surrounding a maar. The lower part of the slope is covered by basic pyroclastics that are obviously younger than the maar itself. Pedon 1 is located on the upper slope, where the younger pyroclastics are not present; thus it developed over the entire Holocene and part of the Late Pleistocene. Pedon 2 is on the toe slope and developed from the young basic pyroclastics. Vegetation remains, charred by fire that was caused by the volcanic ash fall, were found in the lowermost part of the pyroclastics layer, on top of a paleosol. Charcoal fragments were dated to 18950-18830 cal BP (using INTCAL 09). Thus, pedon 2 developed since around 18.9 ka BP, whereas the development of the paleosol that was buried under the pyroclastics (pedon 3), was stopped at this time. Pedons 1 and 2 are Vitric Andosols, developed mainly from basic pyroclastics, as evidenced by the composition of rock fragments in the soils, comprising 78 / 81 mass % lapilli and 22 / 19 mass % gneiss fragments, respectively. Pedon 3 is a Cutanic Luvisol (Chromic) that developed entirely from gneiss fragments produced by the maar explosion. Lab data suggest increasing intensity of pedogenesis in the direction: Pedon 3 (paleosol) < Pedon 2 < Pedon 1, reflected e. g. in increasing Fed/Fet ratios, decreasing molar ratios of (Ca+K+Na)/Al, and decreasing pH. However, it needs to be considered that lapilli are more readily weatherable than gneiss fragments. The profile morphology of the paleosol, characterized by reddish-brown color (7.5YR), strong angular blocky structure and well-expressed illuvial clay

  15. Paleoenvironmental Reconstruction of Late Quaternary Insect Fossils, Halashazi Site, Altai Region, China.

    Science.gov (United States)

    Zhang, Tianshu; Elias, Scott; Angus, Robert

    2017-04-01

    The Altai region northwest China, is located in the middle of arid central Asia and is therefore sensitive to climate change. However, there is a debate on the heat-moisture pattern (warm-dry pattern or cold-dry pattern) during the early Holocene in the Altai region, and a debate on the dominant atmospheric circulation (westerlies or monsoon) control for central Asian climate changes during the Holocene, and the mechanisms that cause the arid early Holocene in central Asia. Thus, the principal aim of the project is use the MCR method to produce quantified temperature and precipitation estimates, and a high-precision palaeoclimatic record for the Altai region, based on fossil beetle assemblages, to reveal the heat-moisture pattern and its mechanisms. This project will begin to fill in the blank of Quaternary beetle research in China. Using Quaternary beetles to reconstruct palaeoenvironments is a new research method for this region, and has never before been done in China, which will provide new evidence for the palaeoenvironmental study in this area. Furthermore, this project will contribute to the beetle faunal research in Eurasia. The sample site for this project - Halashazi Wetland (048°06'54"N, 088°21'48"E), is located at the crossroad of the Altai Mountains and the Dzungarian Basin, where two ecosystems meet. Thus the fossil beetle assemblages should show dramatic change in response to changes of climate. The sampled deposits are made up entirely of sedge peat. Two different profiles were sampled, with depths of 160 cm and 200 cm, respectively. Both profiles were sampled at 5 cm intervals, with approximately 2 kg of material in each unit. The results of the radiocarbon dating will be available in December 2016. Based on other previous studies, the bottom of the peat sediment is 11,500 cal yr BP, so project focuses on the Holocene period approximately from 10,000 cal yr BP. More than 80 species of Coleoptera from 55 genera, 22 families have been recognised so

  16. Provenance analysis of the Late Paleozoic sedimentary rocks in the Xilinhot Terrane, NE China, and their tectonic implications

    Science.gov (United States)

    Han, Jie; Zhou, Jian-Bo; Wilde, Simon A.; Song, Min-Chun

    2017-08-01

    The Xilinhot Terrane is located in the eastern segment of the Central Asian Orogenic Belt in NE China, and is a key to a hotly debated issue on the Paleozoic tectonic evolution of this giant progenic belt. To constrain the tectonic evolution of the Xilinhot Terrane in the Late Paleozoic, we undertook zircon U-Pb dating and geochemical analyses of the Zhesi and Benbatu formations in the Suolun and Xi Ujimqin areas in the Xilinhot Terrane. Samples of the Benbatu Formation yield detrital zircon U-Pb ages ranging from 2659 Ma to 316 Ma, with four age populations at: 2659-1826 Ma, 1719-963 Ma, 590-402 Ma, and 396-316 Ma, whereas samples from the Zhesi Formation yield detrital zircon U-Pb ages ranging from 1967 Ma to 250 Ma, with four age populations at: 1967-1278 Ma, 971-693 Ma, 561-403 Ma, and 399-250 Ma. The age groups of both the Benbatu and Zhesi formations in the Xilinhot Terrane are similar to those in other parts of the Central Asian Orogenic Belt (CAOB). This evidence indicates that the Xilinhot Terrane is a microcontinent, and not an accretionary complex as previously thought. Furthermore, the youngest zircon grains in the Benbatu and Zhesi formations yield weighted mean 206Pb/238U ages of 322 ± 12 Ma (MSDW = 0.12, n = 4) and 257 ± 2.8 Ma (MSDW = 1.6, n = 8), respectively. Combined with fossil data, our new data suggest that the Benbatu and Zhesi formations in the Xilinhot Terrane were possibly deposited at ∼322 Ma and ∼257 Ma, respectively. Based on the provenance of the Carboniferous-Permian sandstones came from the blocks of NE China, we speculate that the Xilinhot Terrane is the western part of the Songliao block.

  17. Middle and Late Devonian brachiopod assemblages,sea level change and paleogeography of Hunan,China

    Institute of Scientific and Technical Information of China (English)

    2010-01-01

    Givetian through middle Famennian brachiopods of Hunan are used to define five biozones,comprising,in ascending order,the Stringocephalus Abundance Zone,the Ambocoeliid-Leiorhynchid Assemblage Zone,the Cyrtospiriferid Assemblage Zone,the Yunnanellina-Sinospirifer Assemblage Zone,and the Yunnanella-Hunanospirifer Assemblage Zone.They correspond approximately to the Po.hemiansatus Zone to Po.varcus Zone,S.hermanni Zone to Pa.punctata Zone,Pa.hassi Zone to Pa.linguiformis Zone,Pa.triangularis Zone to Upper Pa.crepida Zone,and Uppermost Pa.crepida Zone to Pa.marginifera Zone,respectively.Intensified rifting activity in South China during the Devonian began in the middle of the Lower Po.varcus Zone(a level marked by the first appearance of Po.rhenanus),which is consistent with the Lower-Middle Givetian substage boundary suggested by the International Subcommission on Devonian Stratigraphy(SDS).This assumed that rifting activity in the Lower Po.varcus Zone was signified by the deposition of the Baqi Formation in Guangxi and was marked largely by the extensive deposition of the Qiziqiao Formation in central Hunan,which probably led to an opposite pattern of relative sea level change-rising in deeper water trough areas and lowering in carbonate platform areas.The previously recognized S.hermanni Zone sea level rise in platform margin areas of Guangxi can be identified not only in the trough areas but also in platform areas,which probably indicates an overall marine transgression at this time,rather than tectonically induced sea level change.Similarly,this level coincides with the Middle-Upper Givetian substage boundary suggested by the SDS.Although the sea level rise may have occurred in the deeper water trough areas of South China towards the end of the Givetian,platformal areas experienced uplifting at various degrees,especially in the central and northern regions of Hunan where Early Frasnian deposits were apparently absent in many places.Similarly,the end

  18. Late Pleistocene/Holocene wetland events recorded in southeast Tengger Desert lake sediments, NW China

    Institute of Scientific and Technical Information of China (English)

    D. B. Madsen; CHEN Fahu; Ch. G. Oviatt; ZHU Yan; P. J. Brantingham; R. G. Elston; R. L. Bettinger

    2003-01-01

    The area along the eastern and southeastern margins of the Tengger Desert, NW China, which is sensitive to the summer monsoon variations, was selectedfor studying the environmental conditions surrounding the transition between Paleolithic foragers and Neolithic farmer/pastoral- ists. Short cores were obtained from four lake basins in the southwestern Tengger using a hand-driven piston coring device. Proxies from these cores were supplemented by ra- diocarbon ages obtained from lake sediment cores, shoreline features and spring mound deposits. Together these records provide evidence of millennial-scale climate change events from the Pleistocene-Holocene transition to the present. Lake/wetland events, representing periods of more intensive summer monsoon, occur in the records at ~12.7-11.6, ~10.1, ~9.3, ~8.0, ~5.4, ~1.5, and ~0.8 ka BP. They do suggest that century- to millennial-scale climatic cycles are characteristic of the Holocene in the southeastern Tengger Desert although the chronology must be considered extremely tentative.

  19. A New Titanosaurian Sauropod from Late Cretaceous of Nei Mongol, China

    Institute of Scientific and Technical Information of China (English)

    2006-01-01

    A specimen collected from the Upper Cretaceous Erlian Formation of Nei Mongol (Inner Mongolia), China, represents a new genus and species of titanosaurian sauropod. The new taxon is named and described on the basis of the holotype and the only known specimen, which comprises several dorsal, sacral, and caudal vertebrae, several dorsal ribs, one anterior chevron, and much of the pelvis. Diagnostic features of the new species include a thick ridge extending down from the postzygapophysis on the lateral surface of the neural arch of the posterior dorsal vertebrae, a transversely oriented accessory lamina present between the anterior centroparapophyseal limina and the lateral centraprezygapophyseal lamina of the posterior dorsal vertebrae, long, anteroventrally directed caudal rib that bears two distinctive fossae on its posterior margin on the anterior caudal vertebrae and a prominent vertical ridge above the pubic peduncle on the medial surface of the ilium,among others. The ilium is pneumatic, a feature not common among non-avian dinosaurs. The new taxon has an unusual combination of primitive and derived character states. Preliminary character analysis shows a complex character distribution within the Titanosauriformes. Recent titanosauriform discoveries suggest that a significant radiation occurred in Asia early in the titanosauriform evolution.

  20. Late Quaternary upper-water column structure in upwelling areas of the South China Sea

    Institute of Scientific and Technical Information of China (English)

    2001-01-01

    Based on a quantitative analysis of planktonic foraminifera in two gravity cores (17928 and 17954), the history of the upper-water structure of the eastern and western slopes of the South China Sea (SCS) over the last 220 Ka was reconstructed using the transfer function technique. Our results show that lower sea surface temperature (SST) and shallower depth of thermocline (DOT) exist at Core 17928, off Luzon, in the glacial periods; on the contrary, the same situation turned up in the interglacial at Core 17954, off Vietnam. These changes of the upper-water column structure in the two areas are induced by coastal upwelling, which in turn is driven by monsoons, namely, winter monsoon leads to upwelling at the eastern slope, and summer monsoon gives birth to upwelling on the western slope. Moreover, the intensity of upwellings is also closely related to the evolution of the East Asian monsoon. Therefore, we assume that the changes of the upwelling in the two sites indicate strengthenning of winter and su mmer monsoon during the glacial and interglacial periods, respectively.

  1. Evolutionary Significance of Pylentonemid Radiolarians and Their Late Devonian Species from Southwestern Tianshan, China

    Institute of Scientific and Technical Information of China (English)

    LIU Yu; HAO Shougang

    2006-01-01

    A group of radiolarian fossils with a complete morphological gradient of increasing polarization are reported from upper Devonian successions in southwestern Tianshan,China.Specifically, the important transitional mophotypes, Pylentonema transitorum sp. nov., Archocyrtium medium sp. nov. and Quadrapesus transitivus sp. nov., were found. Based on the fact that the new transitional radiolarian fossils resemble more closely to pylentonemids (cyrtoid nassellarians) than to entactinids (spumellarians) in morphology, they are assigned to pylentonemids. Pylentonemids share characters of both the Nassellaria (e.g., horned cephalis, basal opening with pylome) and Spumellaria (e.g., system of trabecular spicules), and they are thus of evolutionary significance. The evolutionary trend from spumellarians to nassellarians is characterized by (1) internal spicule: from simple trabecular spicules to complicate components (A;lr,ll;D;V;Lr,Li;MB); (2) polarization of the radiolarian tests due to rearrangment of spine, from radial to an axial symmetry; (3) the gradual formation of a basal opening (aperture, pylome, or podome); and the transition from a pseudopylome,a primative pylome with a narrow margin on the outer shell, to a true pylome rimmed with a narrow,elevated impermite wall.

  2. Fine grain IRSL and GLSL dating of late Quaternary sediments from North China

    Institute of Scientific and Technical Information of China (English)

    2001-01-01

    A possible approach to assess the fine grain OSL dating isdiscussed through comparison of equivalent dose (DE) values and ages obtained by IRSL and GLSL of fine grains for 31 sediment samples from North China. The IRSL and GLSL were measured with the same aliquots for each sample, i.e. shine-down was by 100 s of IRSL (880 nm) followed by 100 s of GLSL (514 nm) on the same discs. The DE values and ages found by IRSL are in good agreement with those by GLSL within 1-2σfor 80% samples, especially for aeolian loess samples. Considering that IRSL from feldspar differs obviously from GLSL dominated from quartz in dose response, thermal stability and optical bleaching characteristic, the agreement between the DE values may be taken as evidence that the two clocks of IRSL and GLSL had been well reset during deposition. The consistent ages of IRSL and GLSL, in turn, may be referred to an indicator to evaluate the fine grain OSL dating of sediments.

  3. Late Quaternary strata and carbon burial records in the Yellow River delta, China

    Science.gov (United States)

    Zhao, Guangming; Ye, Siyuan; Li, Guangxue; Ding, Xigui; Yuan, Hongming

    2015-06-01

    Sediment carbon sequestration plays an essential role in mitigating atmospheric CO2 increases and the subsequently global greenhouse effect. To clarify the late Quaternary strata and carbon burial records in Yellow River delta (YRD), detailed analysis of benthic foraminifera, total carbon (TC), organic carbon (Corg), sedimentary characteristics and moisture contents of sediments, was performed on core ZK3, 30.3 m in length and obtained from YRD in 2007. Eight depositional units (designated U1-U8 in ascending order) were identified. A comprehensive analysis method of historical geography and sedimentary geology was used to determine the precise depositional ages of the modern Yellow River delta (MYRD), from which pre-MYRD ages were deduced. The results indicates that the maximum burial rates of TC, inorganic carbon (IC) and Corg occurred in the delta front (U5), and the minimum in the shallow sea (U3). Remarkable high sedimentation rates in the MYRD are responsible for burial efficiency of carbon, with an average rate of Corg burial reaching 2087±251 g (m2 yr)-1, and that of IC reaching 13741±808 g (m2 yr)-1, which are much higher than those of other regions with high contents of Corg. Therefore, YRD has a significant burial efficiency for carbon sequestration.

  4. The Power of Interconnectivity: Tan Sitong's Invention of Historical Agency in Late Qing China

    Directory of Open Access Journals (Sweden)

    Hung-yok Ip

    2015-02-01

    Full Text Available To explore how Chinese Buddhists acted as trailblazers of Engaged Buddhism, I shall analyze a late nineteenth-century thinker, Tan Sitong 譚嗣同 (1865–1898. The focus of my analysis is his masterpiece, Renxue 仁學. From his position of Buddhist eclecticism, Tan discoursed at length on non-differentiation as the truth of the universe to reflect on the creative disposition of human agency. He described in Renxue how this disposition would contribute to the agendas defining Chinese modernity. In addition, discussing the meanings of non-differentiation, Tan also generalized about the nature of the human agency he attempted to advocate: while he perceived the human agency blessed with a non-differentiating mindset as an omnipotent history-making force, he also argued that it did not confer upon its owner the status of world savior. In fact, in his view, the efficacy of a non-differentiating mind was determined by the world it aimed to help. Tan's signature piece, I argue, provides a lens through which we can observe modern Chinese Buddhism's role as an important part of the global formation of Engaged Buddhism.

  5. Late Glacial and Holocene vegetation history and paleoclimate of the Tengger Desert, northwestern China

    Institute of Scientific and Technical Information of China (English)

    MA Yuzhen; ZHANG Hucai; H.-J. Pachur; B. Wünnemann; LI Jijun; FENG Zhaodong

    2003-01-01

    Sediments spanning the last 30000 yr BP were obtained from two sections in the southern part of the Teng- ger Desert, northwestern China (38°10′46″N, 102°45′53″E). The pollen assemblage suggested a Picea forest domination under a wetter and cooler environment from 27580 to 23510 yr BP. During the following period from 23510 to 21880 yr BP a Cyperaceae meadow occurred under a wet and cold climate. Wetter and cooler conditions returned and a Picea forest re-occupied this region between 21880 and 20910 yr BP. From 20910 to 15590 yr BP a steppe under a dry environment dominated the region. The first temperature increase started at ca.15590 yr BP. The pollen assemblage covering the period between 15590 and 10890 yr BP can be divided into six minor zones, suggesting that the vegetation compositions changed rapidly under unstable climate. Between 10710 and 10370 yr BP the climate became cold and dry again. The climatic conditions became warmer and more humid between 10260 and 9140 yr BP. From 8450 to 7950 yr BP a steppe landscape under a dry climate occupied this region. Between 7950 and 7290 yr BP climate seemed more humid. The following period from 7290 to 5670 yr BP wasgenerally warm. The period between 5670 and 3510 yr BP was characterized by dramatic climatic oscillations. Relatively cold intervals appeared around 7760 and 7380, 6490-6290, 5670-5010, 4470-3510 yr BP. Two pronounced dry events occurred in 6290-5670 and 5010-4470 yr BP with a marked wet spell from 3510 to 3000 yr BP.

  6. Paleoclimatological change in the Late Neoproterozoic: Evidence from oxygen isotopes of phosphorite in Yangtze Platform, China

    Science.gov (United States)

    Ling, H.-F.; Jiang, S.-Y.; Feng, H.-Z.; Chen, J.-H.; Chen, Y.-Q.; Yang, J.-H.

    2003-04-01

    Seawater and its isotopic composition is the most promising recorder for the climate change of the Earth. Chemical sediments such as carbonate and phosphorite has long been used to reveal the seawater chemistry in the past. The d13C of carbonate with least diagenesis has proved to be sensitive proxy for paleo-environment and paleo-productivity and for chemostratigrphy (e.g. Shen, 2002; Yang et al., 1999; Lambert et al., 1987). However, d18O of carbonate are more prone to suffering diagenesis, and therefore the implications of Phanerozoic d18O curve are controversial (cf. Veizer et al., 1999). Recent study of Wenzel et al. (2000) shows that Silurian phosphatic conodont retained primary oxygen isotopes whereas the d18O values of the coeval calcitic brachiopod shells were altered by diagenesis. Here, we presented and compared oxygen, carbon isotopic compositions and trace and rare earth element concentrations of Neoproterozoic phosphorite and coeval dolomite from the Yangtze platform in an attempt to reconstruct the paleoclimatological and paleooceanographic change during Neoproterozoic. The Yangtze platform possesses excellent record of Late Neoproterozoic-Cambrian strata. In this study, we collected samples systematically from late Neoproterozoic Doushantuo Formation at the Wengan section, Guizhou province. The Doushantuo Fm, overlying on the late Vendian tillite of Nantuo Fm and overlain by dolostone of Dengying Fm which underlain the basal Cambrian black shale, consists mainly of phosphorite and minor interbeded dolostone with total thickness of about 70 m. Our results show large variations of d18Odolo(SMOW) for the dolomite (17.6 ~ 25.9‰) which has no correlation with their d13Cdolo values and other geochemical parameters. In contrast, phosphorites display rather limited variations of the d18Ophos (SMOW) values (10.7 ~ 15.0‰). Further more, the d18Ophos and d13Cdolo values, Ce anomaly and Pb/Th ratio consistently increased from the lower to upper part of the

  7. Chondritic osmium isotopic composition of late Archean convecting upper mantle:Evidence from Zunhua podiform chromitites, Hebei, North China

    Institute of Scientific and Technical Information of China (English)

    XIA Qiongxia; ZHI Xiachen; LI Jianghai; HUANG Xiongnan

    2004-01-01

    Podiform chromite deposits are a characteristic feature of the mantle sequences of harzburgitic ophiolites. The chromites usually have very low Re and high Os contents, which makes it the most resistant phase remaining from the primary magmatic history of the ultramafic sections of ophiolites. The podiform chromite is one of the robust indicators of initial Os isotopic compositions of the ophiolites where podiform chromites were derived from, which provides strong evidence for the origin and evolution of oceanic lithosphere. The Re and Os contents and the Os isotopic compositions of seven podiform chromitites from Zunhua ophiolitic mélange belt, North China are reported in this study. The Re contents range from 0.019 to 0.128 ng/g, Os from 8.828 to 354.0 ng/g, and the 187Os/188Os ratio from 0.11003 to 0.11145. Three massive chromitites among the sample set have very high Os contents (>300 ng/g), and their 187Os/188Os ratios range from 0.11021 to 0.11030, averaging 0.11026 ± 0.00005 (σ), equivalent to a γOs = -0.12 ± 0.06 at 2.6 Ga, which means that the Os isotopic composition of convecting upper mantle is chondritic in late Archean. It is the Os isotopic composition of podiform chromitites that are derived from the oldest ophiolite in the world till now.

  8. An enlarged parietal foramen in the late archaic Xujiayao 11 neurocranium from Northern China, and rare anomalies among Pleistocene Homo.

    Directory of Open Access Journals (Sweden)

    Xiu-Jie Wu

    Full Text Available We report here a neurocranial abnormality previously undescribed in Pleistocene human fossils, an enlarged parietal foramen (EPF in the early Late Pleistocene Xujiayao 11 parietal bones from the Xujiayao (Houjiayao site, northern China. Xujiayao 11 is a pair of partial posteromedial parietal bones from an adult. It exhibits thick cranial vault bones, arachnoid granulations, a deviated posterior sagittal suture, and a unilateral (right parietal lacuna with a posteriorly-directed and enlarged endocranial vascular sulcus. Differential diagnosis indicates that the perforation is a congenital defect, an enlarged parietal foramen, commonly associated with cerebral venous and cranial vault anomalies. It was not lethal given the individual's age-at-death, but it may have been associated with secondary neurological deficiencies. The fossil constitutes the oldest evidence in human evolution of this very rare condition (a single enlarged parietal foramen. In combination with developmental and degenerative abnormalities in other Pleistocene human remains, it suggests demographic and survival patterns among Pleistocene Homo that led to an elevated frequency of conditions unknown or rare among recent humans.

  9. Response of surface processes to climatic change in the dunefields and Loess Plateau of North China during the late Quaternary

    Science.gov (United States)

    Lu, H.; Mason, J.A.; Stevens, T.; Zhou, Y.; Yi, S.; Miao, X.

    2011-01-01

    This paper draws on recent optically stimulated luminescence (OSL) dating to evaluate the long-held assumption that dust accumulation rates in the Loess Plateau and the extent of active aeolian sand in the dunefields to the north have varied together over time, because both are controlled by the strength of the Asian monsoons and also possibly because the dunefields are proximal loess sources. The results show there is little evidence that high rates of loess accumulation coincided with well-dated episodes of extensive dune activity in the Mu Us, Otindag, and Horqin dunefields, at 11-8ka and 1-0ka. Explanations for the apparent lack of coupling include local variation in the trapping of dust and post-depositional preservation of the loess and dune sediments, in response to varying local environmental conditions. In addition, a substantial portion of the loess may be transported directly from source areas where dust emission has somewhat different climatic and geomorphic controls than aeolian sand activity within the dunefields. The results of this study cast doubt on the use of loess accumulation rate as a palaeoclimatic proxy at millennial timescale. The dunefield and loess stratigraphic records are interpreted as primarily recording changes in effective moisture at a local scale, but the timing of late Quaternary dune activity, along with a variety of other evidence, indicates that moisture changes in many of the drylands of northern China may not be in phase with precipitation in core regions of the Asian monsoons. ?? 2011 John Wiley & Sons, Ltd.

  10. Composition and mode of occurrence of minerals in Late Permian coals from Zhenxiong County, northeastern Yunnan, China

    Institute of Scientific and Technical Information of China (English)

    Tian Li; Shi-Feng Dai; Jian-Hua Zou; Sen Zhang; He-Hing Tian; Li-Xin Zhao

    2014-01-01

    Minerals in the Late Permian coals from the Niuchang-Yigu mining area, Zhenxiong County, northeastern Yunnan, China, were investigated using optical microscopy and low temperature ashing plus X-ray diffraction (LTA ? XRD). The results showed that minerals in the coal LTAs are mainly quartz, kaolinite, chamosite, mixed-layer illite/smectite (I/S), pyrite, and calcite, with trace amounts of marcasite, dolomite, and bassanite. The authigenic quartz generally occurs in collodetrinite or as a filling in cleats or cell cavities. This silica was mainly derived from aqueous solutions produced by the weathering of basaltic rocks in the Kangdian Upland and from hydrothermal fluids. The presence of b-quartz paramorph grains in collodetrinite probably indicates that these grains were detrital and came from a volcanic ash. Clay minerals are generally embedded in collodetrinite and occur as cell-fillings. Pyrite occurs as framboidal, anhedral, and euhedral grains and a cell-filling. The coals are high in pyrite and the high pyrite content probably results from seawater invading during the stage of peat accumulation. Calcite generally occurs as vein-fillings, indicating an epigenetic origin.

  11. Formation and evolution of yardangs activated by Late Pleistocene tectonic movement in Dunhuang, Gansu Province of China

    Science.gov (United States)

    Wang, Yanjie; Wu, Fadong; Zhang, Xujiao; Zeng, Peng; Ma, Pengfei; Song, Yuping; Chu, Hao

    2016-12-01

    Developed in the Anxi-Dunhuang basin, the yardangs of Dunhuang (western China) are clearly affected by tectonic movement. Based on fieldwork, this study ascertained three levels of river terrace in the area for the first time. Through the analysis of river terraces formation and regional tectonic movement, the study ascertained that the river terraces were formed mainly by Late Pleistocene tectonic uplift, which had activated the evolution of yardangs in the study area. By electron spin resonance (ESR) dating and optically stimulated luminescence (OSL) dating, the starting time and periodicity of the evolution of the yardangs were determined. The river terraces designated T3, T2 and T1 began to evolve at 109.0 ˜98.5, 72.9 ˜66.84 and 53.2 ˜38.0 kaBP, respectively, which is the evidence of regional neotectonic movement. And, the formation of the yardangs was dominated by tectonic uplift during the prenatal stage and mainly by wind erosion in the following evolution, with relatively short stationary phases. This research focused on the determination of endogenic processes of yardangs formation, which would contribute to further understanding of yardangs formation from a geological perspective and promote further study of yardang landform.

  12. Formation and evolution of yardangs activated by Late Pleistocene tectonic movement in Dunhuang, Gansu Province of China

    Indian Academy of Sciences (India)

    Yanjie Wang; Fadong Wu; Xujiao Zhang; Peng Zeng; Pengfei Ma; Yuping Song; Hao Chu

    2016-12-01

    Developed in the Anxi-Dunhuang basin, the yardangs of Dunhuang (western China) are clearly affected by tectonic movement. Based on fieldwork, this study ascertained three levels of river terrace in the area for the first time. Through the analysis of river terraces formation and regional tectonic movement, the study ascertained that the river terraces were formed mainly by Late Pleistocene tectonic uplift, which had activated the evolution of yardangs in the study area. By electron spin resonance (ESR) dating and optically stimulated luminescence (OSL) dating, the starting time and periodicity of the evolution of the yardangs were determined. The river terraces designated T3, T2 and T1 began to evolve at 109.0∼98.5, 72.9∼66.84 and 53.2∼38.0 kaBP, respectively, which is the evidence of regional neotectonic movement.And, the formation of the yardangs was dominated by tectonic uplift during the prenatal stage and mainly by wind erosion in the following evolution, with relatively short stationary phases. This research focused on the determination of endogenic processes of yardangs formation, which would contribute to further understanding of yardangs formation from a geological perspective and promote further study of yardang landform.

  13. Late Neolithic phytolith and charcoal records of human activities and vegetation change in Shijiahe culture, Tanjialing site, China.

    Science.gov (United States)

    Zhu, Xiao Hong; Li, Bing; Ma, Chun Mei; Zhu, Cheng; Wu, Li; Liu, Hui

    2017-01-01

    There is significant archaeological evidence marking the collapse of the Shijiahe culture in the middle reaches of the Yangtze River in China during the late Neolithic Period. However, the causes for this cultural collapse remain unclear. Our sedimentary records from a 3.3 m long profile and 76 phytolith and charcoal samples from the Tanjialing archaeological sites provide records of interactions between an ancient culture and vegetation change. During the early Shijiahe culture (c, 4850-4400 cal BP), the climate was warm and humid. Fire was intensively used to clear the vegetation. In the mid-period of the Shijiahe culture (c, 4400-4200 cal BP), the climate became slightly dry-cold and this was accompanied by decreasing water, leading to settlements. From c, 4200 cal BP, severe drought eroded the economic foundation of rice-cultivation. These conditions forced people to abandon the Shijiahe ancient city to find water in other regions, leading to the collapse of the Shijiahe culture.

  14. Emergence of ancient cities in relation to geopolitical circumstances and climate change during late Holocene in northeastern Tibetan Plateau, China

    Science.gov (United States)

    Dong, Guanghui; Liu, Honggao; Yang, Yishi; Yang, Ying; Zhou, Aifeng; Wang, Zhongxin; Ren, Xiaoyan; Chen, Fahu

    2016-09-01

    The study of the history of human activities in ancient cities has provided valuable evidences for understanding the evolution of human-land relations during the late Holocene. Numerous ancient cities were discovered through archaeological surveys of the east Qinghai Province, located on the northeastern border of the Tibetan Plateau, China; however, the mystery of when or why these cities were built remains unsolved. As recorded in this paper, we sampled reliable dating materials from 47 ancient cities in the area, determined their ages by radiocarbon dating, and compared the dating results with historical documents and high resolution paleoclimate records to explore the influencing factors for the development of these ancient cities. The 54 radiocarbon dates indicated that most of these cities were built or repaired during the Han Dynasty (202 BC‒AD 220), Tang Dynasty (AD 618‒AD 907), the Five Dynasties and Ten Kingdoms period (AD 907‒AD 960), the Song dynasty (AD 960‒AD 1279), and the Ming Dynasty (AD 1368‒AD 1644). The radiocarbon dates correspond well with historical records of the area. Our work suggests the ancient cities in east Qinghai Province were likely built primarily for military defense, and may have also have been affected by climate change.

  15. Emergence of ancient cities in relation to geopolitical circumstances and climate change during late Holocene in northeastern Tibetan Plateau, China

    Science.gov (United States)

    Dong, Guanghui; Liu, Honggao; Yang, Yishi; Yang, Ying; Zhou, Aifeng; Wang, Zhongxin; Ren, Xiaoyan; Chen, Fahu

    2016-12-01

    The study of the history of human activities in ancient cities has provided valuable evidences for understanding the evolution of human-land relations during the late Holocene. Numerous ancient cities were discovered through archaeological surveys of the east Qinghai Province, located on the northeastern border of the Tibetan Plateau, China; however, the mystery of when or why these cities were built remains unsolved. As recorded in this paper, we sampled reliable dating materials from 47 ancient cities in the area, determined their ages by radiocarbon dating, and compared the dating results with historical documents and high resolution paleoclimate records to explore the influencing factors for the development of these ancient cities. The 54 radiocarbon dates indicated that most of these cities were built or repaired during the Han Dynasty (202 BC‒AD 220), Tang Dynasty (AD 618‒AD 907), the Five Dynasties and Ten Kingdoms period (AD 907‒AD 960), the Song dynasty (AD 960‒AD 1279), and the Ming Dynasty (AD 1368‒AD 1644). The radiocarbon dates correspond well with historical records of the area. Our work suggests the ancient cities in east Qinghai Province were likely built primarily for military defense, and may have also have been affected by climate change.

  16. Clay mineral records of East Asian monsoon evolution during late Quaternary in the southern South China Sea

    Institute of Scientific and Technical Information of China (English)

    LIU Zhifei; C. Colin; A. Trentesaux; D. Blamart

    2005-01-01

    High-resolution clay mineral records combined with oxygen isotopic stratigraphy over the past 190 ka during late Quaternary from core MD01-2393 off the Mekong River in the southern South China Sea are reported to reconstruct a history of East Asian monsoon evolution.The dominating clay mineral components indicate a strong glacial-interglacial cyclicity, with high glacial illite, chlorite, and kaolinite contents and high interglacial smectites content. The provenance analysis indicates the direct input of clay minerals via the Mekong River drainage basin.Illite and chlorite derived mainly from the upper reach of the Mekong River, where physical erosion of meta-sedimentary rocks is dominant. Kaolinite derived mainly from active erosion of inhered clays from reworked sediments in the middle reaches. Smectites originated mainly through bisiallitic soils in the middle to lower reaches of the Mekong River. The smectites/(illite+chlorite)and smectites/kaolinite ratios are determined as mineralogical indicators of East Asian monsoon variations. Relatively high ratios occur during interglacials and indicate strengthened summer-monsoon rainfall and weakened winter-monsoon winds; relatively lower ratios happened in glacials, indicating intensified winter monsoon and weakened summer monsoon. The evolution of the summer and winter monsoons provides an almost linear response to the summer insolation of the Northern Hemisphere, implying an astronomical forcing of the East Asian monsoon evolution.

  17. Differences in Late Quaternary primary productivity between the western tropical Pacific and the South China Sea: Evidence from coccoliths

    Science.gov (United States)

    Su, Xiang; Liu, Chuanlian; Beaufort, Luc; Barbarin, Nicolas; Jian, Zhimin

    2015-12-01

    Changes in Late Quaternary oceanic primary productivity in the western tropical Pacific were reconstructed using coccolith counts from the improved SYRACO system in piston core MD01-2386 retrieved from the Halmahera Sea near northwest New Guinea. The calculated primary productivity exhibits cycles on obliquity and precession timescales over the last 192 ka. There are marked differences between primary productivity records from the western tropical Pacific and the South China Sea (SCS), with the former being dominated by precession, and the latter showing all three Milankovitch cycles (eccentricity, obliquity and precession). Empirical Orthogonal Function (EOF) analyses reveal two significant EOF modes in the western tropical Pacific and SCS records. EOF-1 accounts for 38% of the total variance and exhibits obvious precessional cycles corresponding to Northern Hemisphere summer insolation, while EOF-2 accounts for 22% of the total variance and exhibits strong 41-kyr periodicity, suggesting different biological responses to hydroclimate changes in the two regions. A more complex hydroclimate regime influenced by the East Asian monsoon and the large contrast in regional topography and circulation during glacial cycles are considered to be the primary drivers of the stronger temporal variability in productivity in the SCS compared to the relatively stable western tropical Pacific.

  18. A Non-Destructive Study of Printing Materials of an Imperial China Green Engraved Coiling Dragon Stamp%清代绿色蟠龙邮票印刷材料无损分析

    Institute of Scientific and Technical Information of China (English)

    甘清; 季金鑫; 姚娜; 王纪刚; 周文华; 周忠; 施继龙

    2016-01-01

    利用超景深三维视频显微镜,激光显微共聚焦拉曼光谱仪和扫描电镜-能谱仪对一张清代绿色蟠龙邮票样品的纸张,油墨等印刷材料进行无损分析。结果表明,该样票采用手工雕刻凹版印刷,所用承印物为长纤维机制纸,未经过涂布,无水印,背胶;纸张填料中含有 Al,Si 等元素,推断纸张填料可能是高岭土(Al2 O3·2SiO2·2H2 O)之类的物质。绿色油墨包含了蓝色普鲁士蓝(Prussian Blue,Fe4[Fe(CN)6]3·14-16 H2 O)和黄色铬酸铅[Lead(Ⅱ)chromate,PbCrO4]颜料,根据印刷色彩学色料减色和色光加色理论分析,邮票样品呈现的绿色是由蓝色颜料普鲁士蓝和黄色颜料铬酸铅混合呈色的结果;油墨填料中含有 Na,Mg, S,Cl,K,Ca,V,Zn,Ba等元素,推断油墨填料为MgCO3,CaCO3,BaSO4等物质。上述三项技术联用,在邮票等纸质品的无损分析中具有广阔的应用前景。%Non-destructive measurement methods including video microscopy (VM),Raman spectrometer (RS),and scanning electron microscopy-energy dispersive spectroscopy (SEM-EDS)were employed to analyze the printing materials of a green curled-up dragon stamp sample from the late Qing Dynasty in terms of the paper and ink.The results indicated that the plate-making process of the sample belonged to handcrafted gravure while the slender and dense paper fiber with no coating,water-mark,or gumming.Elements of Al and Si were inspected in fillers of paper,therefore,it could be inferred that kaolin (Al2 O3 · 2SiO2·2H2O)wasthefillerofpaper.GreeninkwasmadeupofbluepigmentPrussianBlue(Fe4[Fe(CN)6]3·14-16H2O)and yellow pigment Lead(II)chromate(PbCrO4 ).According to theories of additive color and subtractive color,ink presented green color due to the effect of Prussian blue and Lead chromate mixed together.Elements of Na,Mg,S,Cl,K,Ca,V,Zn and Ba were measured from fillers of the ink and it could be inferred that MgCO3 ,BaSO4 ,CaCO3 and other substances might be con-tained in ink

  19. Genetic relationships between swamp microenvironment and sulfur distribution of the Late Paleozoic coals in North China

    Institute of Scientific and Technical Information of China (English)

    TANG; Dazhen

    2001-01-01

    [1]Yang, Q., Coal resources of China, in Move Toward Science Together, Hundreds Academicians' Series Reports on Science and Technology (Part 1) (in Chinese), Beijing: Xinhua Press, 1997, 276-286.[2]Flores, R. M., Geologic and geomorphic controls of coal development in some Tertiary rocky mountain basins, USA, Int. J. Coal Geol., 1993, 23: 43-73.[3]Hacquebard, P. A., Petrology and facies studies of the Carboniferous coals at Mabou Mines and the Port Hood, St. Rose and Sydney coalfields of Cape Breton Island, Nova Scotia, Canada, Int. J. Coal Geol., 1993, 24: 7-46.[4]Kalkreuth, W. D., McIntyre, D. J., Richardson, R. J. H., The geology, petrography and palynology of Tertiary coals from the Eureka Sound Group at Strathcona Fiord and Bache Peninsula, Ellesmere Island, Arctic Canada, Int. J. Coal Geol., 1993, 24: 75-111.[5]Price, F. T., Shieh, Y. H., Correlation between the d 34S of pyritic and organic sulfur in coal and oil shale, Chemical Geol-ogy, 1986, 58: 333-337.[6]Prosser, D. J., Daws, J. A., Fallick, A. E. et al., The occurrence and d 34S of authigenic pyrite in Middle Jurassic Brent Group sediments, Journal Petrol. Geol., 1994, 17(4): 407-428.[7]Spiker, E. C., Pierce, B. S., Bates, A. L. et al., Isotopic evidence for the source of sulfur in the Upper Freeport coal bed, west-central Pennsylvania, USA, Chemical Geology, 1994, 114: 115-130.[8]Berner, R. A., Sedimentary pyrite formation:An update, Geochim. Cosmochim. Acta, 1984, 48: 605-615.[9]Francois, R., A study of sulphur enrichment in the humic fraction of marine sediments during early diagenesis, Geochim. Cosmochim. Acta, 1987, 51: 17-27.[10]Canfield, D. E., Berner, R. A., Dissolution and pyritization of magnetite in anoxic marine sediments, Geochim. Cosmo-chim. Acta, 1987, 51: 645-660.[11]Sang, S. X., Liu, H. J., Shi, J., Study of the sulfur of the mangrove peat and its genesis in Hainandao, Geology and Explo-ration of Coalfield(in Chinese), 1993, 21(1): 12-17.

  20. ENSO-Type Signals Recorded in the Late Cretaceous Laminated Sediments of Songliao Basin, Northeast China

    Science.gov (United States)

    Yu, E.; Wang, C.; Hinnov, L. A.; Wu, H.

    2014-12-01

    The quasi-periodic, ca. 2-7 year El Niño Southern Oscillation (ENSO) phenomenon globally influences the inter-annual variability of temperature and precipitation. Global warming may increase the frequency of extreme ENSO events. Although the Cretaceous plate tectonic configuration was different from today, the sedimentary record suggests that ENSO-type oscillations had existed at the time of Cretaceous greenhouse conditions. Cored Cretaceous lacustrine sediments from the Songliao Basin in Northeast China (SK-1 cores from the International Continental Drilling Program) potentially offer a partially varved record of Cretaceous paleoclimate. Fourteen polished thin sections from the depth interval 1096.12-1096.53 m with an age of 84.4 Ma were analyzed by optical and scanning electron microscopy (SEM). ImageJ software was applied to extract gray scale curves from optical images at pixel resolution. We tracked minimum values of the gray scale curves to estimate the thickness of each lamina. Five sedimentary structures were recognized: flaser bedding, wavy bedding, lenticular bedding, horizontal bedding, and massive layers. The mean layer thicknesses with different sedimentary structures range from 116 to 162mm, very close to the mean sedimentation rate estimated for this sampled interval, 135mm/year, indicating that the layers bounded by pure clay lamina with the minimum gray values are varves. SEM images indicate that a varve is composed, in succession, of one lamina rich in coarse silt, one lamina rich in fine silt, one clay-rich lamina with some silt, and one clay-rich lamina. This suggests that a Cretaceous year featured four distinct depositional seasons, two of which were rainy and the others were lacking precipitation. Spectral analysis of extended intervals of the tuned gray scale curve indicates the presence of inter-annual periodicities of 2.2-2.7 yr, 3.5-6.1 year, and 10.1-14.5 year consistent with those of modern ENSO cycles and solar cycles, as well as

  1. Bird Use of Imperial Valley Crops [ds427

    Data.gov (United States)

    California Department of Resources — Agriculture crops in the Imperial Valley of California provide valuable habitat for many resident and migratory birds and are a very important component of the...

  2. Selenium in aquatic habitats at Imperial National Wildlife Refuge

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — During 1991 and 1992, selenium levels were studied in aquatic communities at Imperial National Wildlife Refuge on the lower Colorado River. Composite samples of...

  3. Joint Effect of Education and Main Lifetime Occupation on Late Life Health: A Cross-Sectional Study of Older Adults in Xiamen, China

    OpenAIRE

    Manqiong Yuan; Wei Chen; Cheng-I Chu; Ya Fang

    2015-01-01

    Background The effects of education and occupation on health have been well documented individually, but little is known about their joint effect, especially their cumulative joint effect on late life health. Methods We enrolled 14,292 participants aged 60+ years by multistage sampling across 173 communities in Xiamen, China, in 2013. Heath status was assessed by the ability to perform six basic activities of daily life. Education was classified in four categories: ‘Illiterate’, ‘Primary’, ‘J...

  4. Late Mesozoic crust-mantle interaction and lower crust components in South China: A geochemical study of mafic granulite xenoliths from Cenozoic basalts

    Institute of Scientific and Technical Information of China (English)

    YU; Jinhai; (于津海); XU; Xisheng; (徐夕生); ZHOU; Xinmin; (周新民)

    2003-01-01

    Mafic granulite xenoliths collected from Cenozoic basalts in SE China can be classified as magmatic granulite and cumulate granulite. Magmatic granulites are characterized by highly concentrated Al2O3, K2O, P2O5, Ba, Sr, Pb and REE, and low contents of Nb, Zr, Hf and Th, and have an incompatible element abundance pattern similar to that of continental arc basalts. Cumulate granulites aredepleted in K2O, P2O5, Rb, Cs and Ba. These granulite xenoliths were the products of crystallization and recrystallization of the basaltic magma underplating into crust-mantle boundary in Late Mesozoic. Sr and Nd isotopic compositions and variation trend of these mafic rocks are the result of crust-mantle mixing and controlled by assimilation and fractional crystallization process (AFC). However,trace element and major element variations were mainly controlled by fractionalcrystallization. The granulites are similar in geochemistry to surface Late Mesozoic gabbro and basalt in the study area, suggesting a close petrogenetic link between them. Late Mesozoic basaltic magma activities are the most important cause for the formation of extensive contemporaneous granite and rhyolite in the study area. This study and previous data indicate that the lower crust beneath South China is composed of a variety of Paleo- to Meso-proterozoic metamorphic rocks and Late Mesozoic mafic granulites.

  5. Multiproxy biomarker, isotopic and pollen reconstructions of the middle to late Holocene paleoclimate of the Loess Plateau in centre China

    Science.gov (United States)

    Sun, H.; Seki, O.; Zhou, A.; Chen, F.; Schouten, S.; Toney, J. L.; Bendle, J.

    2011-12-01

    The Asian monsoon is a key component of the earth's climate system that directly affects the livelihood of 50 million people on the loess plateau of central China. At the far edge of monsoonal influence, this region is especially vulnerable to future changes in temperature and evaporation / precipitation. Therefore, paleoclimatic information on the natural sensitivity of the region to changes in monsoon driven aridity are crucial. Despite the need for multiproxy records of Holocene climate from this region, reconstructions are rare, because of the low resolution of loess deposits and the scarcity of other paleoclimate archives (e.g. natural lakes, speleothems). Here we present multiple proxy records from Tianchi lake, one of the few nature lakes on the loess plateau and central China. The chronology is well constrained by a high-resolution (20 AMS 14C dates) radiocarbon age-model, spanning the past 6200 years. Here we present pollen, Glycerol dibiphytanyl glycerol tetraethers (GDGTs), lake macrophyte and higher plant-wax biomarkers to reconstruct regional climate change during the middle to late Holocene. Evidence from pollen data suggest that deciduous trees decreased from 6200 cal yr BP and then more rapidly from 1000 yr BP. Modern and downcore molecular distribution patterns of n-alkanes and n-alkanoic acids, especially n-alkane Paq values, suggest increasing relative abundance of macrophytes over this time, which we interpret (based on lake morphology) as decreasing lake-level. Using the recent Sun et al (2011) regional calibration we derive mean annual GDGT based temperatures (MBT/CBT-MATs) with reasonable ranges. Our temperature reconstruction closely correlates on millennial to centennial timescales with the independent D/H measurements on C28 fatty acid methyl esters (C28 FAMEs), whose signal is assumed to derive primarily from terrestrial plant waxes and the δD values to reflect local changes in relative humidity. Comparisons of our independent GDGT

  6. Petrogenesis and tectonic implications of the Early Carboniferous to the Late Permian Barleik plutons in the West Junggar (NW China)

    Science.gov (United States)

    Liu, Bo; Han, Bao-Fu; Ren, Rong; Chen, Jia-Fu; Wang, Zeng-Zhen; Zheng, Bo

    2017-02-01

    The Paleozoic accretionary orogenesis and continental crustal growth in Central Asia are thought to have close relationship with the evolution of the Paleo-Asian Ocean (PAO). The well-exposed plutons in the northern Barleik Mountains of the West Junggar region, NW China, may provide essential insights into the evolution of the Junggar Ocean, a branch of the PAO, and mechanism of continental crustal growth. Our work on the Barleik plutons indicates an early suite of 324-320 Ma diorite and a late suite of 314-259 Ma quartz syenite and granitic porphyry. All the plutons are characterized by high-K calc-alkaline to shoshonitic signatures, varying depletion in Nb, Ta, Sr, P, Eu, and Ti, low initial 87Sr/86Sr ratios (0.70241-0.70585), strongly positive εNd(t) values (+ 5.7-+7.7), and young one-stage Nd model ages (390-761 Ma), suggesting that they resulted from different batches of magma that were produced by fractional crystallization of a metasomatized mantle source with minor crustal contamination. The diorite is coeval with the youngest arc magmatic rocks, indicating a subduction-related origin. By contrast, the quartz syenite and granitic porphyry are geochemically similar to A2-type granites, with high Zr, Ga, and FeOT/[FeOT + MgO], and are coeval with the widespread plutons in the West Junggar. This, together with the occurrence of Late Carboniferous fluvial deposits and the lack of < 320 Ma ophiolitic and subduction-related metamorphic lithologies, definitively indicates a post-collisional setting after the closure of the Junggar Ocean. Slab breakoff accompanied by asthenospheric upwelling and basaltic underplating is a possible geodynamic process that is responsible for the post-collisional magmatism and vertical crustal growth in the region. Thus a tectonic switch from subduction to post-collision started at the end of the Early Carboniferous ( 320 Ma), probably as a result of the final closure of the Junggar Ocean.

  7. Late-Stage Ductile Deformation in Xiongdian-Suhe HP Metamorphic Unit, North-Western Dabie Shan, Central China

    Institute of Scientific and Technical Information of China (English)

    Suo Shutian; Zhong Zengqiu; Zhou Hanwen; You Zhendong

    2004-01-01

    New structural and petrological data unveil a very complicated ductile deformation history of the Xiongdian-Suhe HP metamorphic unit, north-western Dabie Shan, central China. The fine-grained symplectic amphibolite-facies assemblage and coronal structure enveloping eclogite-facies garnet, omphacite and phengite etc., representing strain-free decompression and retrogressive metamorphism, are considered as the main criteria to distinguish between the early-stage deformation under HP metamorphic conditions related to the continental deep subduction and collision, and the late-stage deformation under amphibolite to greenschist-facies conditions occurred in the post-eclogite exhumation processes. Two late-stages of widely developed, sequential ductile deformations D3 and D4, are recognized on the basis of penetrative fabrics and mineral aggregates in the Xiongdian-Suhe HP metamorphic unit, which shows clear, regionally, consistent overprinting relationships. D3 fabrics are best preserved in the Suhe tract of low post-D3 deformation intensity and characterized by steeply dipping layered mylonitic amphibolites associated with doubly vergent folds. They are attributed to a phase of tectonism linked to the initial exhumation of the HP rocks and involved crustal shortening with the development of upright structures and the widespread emplacement of garnet-bearing granites and felsic dikes. D4 structures are attributed to the main episode of ductile extension (D14) with a gently dipping foliation to the north and common intrafolial, recumbent folds in the Xiongdian tract, followed by normal sense top-to-the north ductile shearing (D24) along an important tectonic boundary, the so-called Majiawa-Hexiwan fault (MHF), the westward continuation of the Balifan-Mozitan-Xiaotian fault (BMXF) of the northern Dabie Shan. It is indicated that the two stages of ductile deformation observed in the Xiongdian-Suhe HP metamorphic unit, reflecting the post-eclogite compressional or extrusion

  8. The British Museum: An Imperial Museum in a Post-Imperial World

    Directory of Open Access Journals (Sweden)

    Emily Duthie

    2011-12-01

    Full Text Available This article examines the British Museum’s imperialist attitudes towards classical heritage. Despite considerable pressure from foreign governments, the museum has consistently refused to return art and antiquities that it acquired under the aegis of empire. It is the contention of this article that the British Museum remains an imperialist institution. The current debates over the British Museum’s collections raise profound questions about the relationship between museums and modern nation states and their nationalist claims to ancient heritage. The museum’s inflexible response to repatriation claims also encapsulates the challenges inherent in presenting empire and its legacy to contemporary, post-imperial audiences.

  9. New imperialism and beyond: why the new imperialism will fail and unseat the Bush Administration?

    Directory of Open Access Journals (Sweden)

    Petri Minkkinen

    2008-12-01

    Full Text Available Tras los atentados terroristas del 11S de 2001, los Estados Unidos implantaron una política de nuevo imperialismo y de construcción de un nuevo tipo de imperio mundial. Las políticas globales norteamericanas pueden dividirse en economista, cooperativista y reglada por el idealismo Wilsoneano, y el imperialismo Rooseveltiano, basado en un nacionalismo agresivo, militarismo, unilateralismo y governanza global  basada en reglas directas, presencia física y coerción. Las políticas de la administraciones Bush representan esta última vertiente y la Guerra contra el Terror puede ser interpretada como una Primera Guerra Mundial y una guerra civil en los Estados Unidos. Se proclama que un nuevo imperialismo fracasará debido a diversas razones de tipo económica, política, étnica e histórica, y que esta política está debilitando la posición global de Estados Unidos. Al final, se explica cómo en el contexto de una Nueva Contención Pacífica, los ciudadanos norteamericanos y los ciudadanos del resto del mundo pueden utilizar la democracia en contra del nuevo imperialismo y apoyar un cambio de régimen democrático en Estados Unidos, procediendo a la construcción conjunta de un  mundo democrático y justo.________________ABSTRACT:After the terrorist attacks of S-11-2001 the US engaged in the policies of new imperialism and in the construction of a new kind of world-empire. US global policies can be divided in detached, economist, cooperative, rule-based Wilsonian Idealism and Theodore Rooseveltian Imperialism, based on aggressive nationalism, militarism, unilateralism and global governance based on direct rule, physical presence and coercion. The Bush administrations policies represent the latter and the War on Terror and Non-White Others can be seen as a First World War and an Internal Civil War in the US. It is claimed that the new imperialism will fail due to various economic, political, ethical and historical reasons and that this

  10. Molecular Records of Primary Producers and Sedimentary Environmental Conditions of Late Permian Rocks in Northeast Sichuan, China

    Institute of Scientific and Technical Information of China (English)

    Ruan Xiaoyan; Luo Genming; Hu Shouzhi; Chen Feng; Sun Si; Wu Wenjun; Guo Qiaozhen; Liu Guoquan

    2008-01-01

    A series of biomarkers were identified in the aliphatic and aromatic fractions of the extracts from Late Permian Dalong (大隆) and Wujiaping (吴家坪) formations in Shangsi (上寺) Section, Northeast Sichuan (四川), South China, on the basis of the analysis of gas chromatography-mass spectrometry (GC-MC). The dominance of lower-molecular-weight n-alkanes throughout the profile suggests the dominant contribution of algae and bacteria to the organics preserved in the marine section. Wujiaping Formation is characterized by the elevated contribution from algae as well as other photoantotrophs such as photosynthetic bacteria as shown by the molecular ratios of hopanes to steranes or tricyclic terpanes as well as the ratio of pristane (Pr) and phytane (Ph) to C17 and C18 n-alkanes. This is in accord with the data from the microscopic measurement on the calcareous algae. In contrast, Dalong Formation is featured by enhanced contribution from bacteria and probably terrestrial organics indicated by the enhanced C24 tetracyclic terpanes relative to tricyclic terpanes. The two formations also show a distinct discrimination in sedimentary environmental conditions including redox condition and salinity. The anoxic condition was only found in the middle of the Dalong Formation as shown by the ratios of Pr/Ph and dibenzothiophene to phenanthrene, consistent with the reported data of Mo and U. An enhancedsalinity indicated by the homohopane index is observed at the shallow Wujiaping Formation. On the basis of the composition of primary productivity and the redox condition, Dalong Formation is proposed, herein, to be potential hydrocarbon source rocks in the study site. It is notable that the topmost end-Permian is characterized by a large perturbance in both the redox condition and salinity, with oxic conditions being frequently interrupted by short-term anoxia, likely showing a causal relationship with the episodic biotic crisis across the Permian-Triassic boundary.

  11. Osteoarthritis, labour division, and occupational specialization of the Late Shang China - insights from Yinxu (ca. 1250 - 1046 B.C.).

    Science.gov (United States)

    Zhang, Hua; Merrett, Deborah C; Jing, Zhichun; Tang, Jigen; He, Yuling; Yue, Hongbin; Yue, Zhanwei; Yang, Dongya Y

    2017-01-01

    This research investigates the prevalence of human osteoarthritis at Yinxu, the last capital of the Late Shang dynasty (ca. 1250-1046 B.C.), to gain insights about lifeways of early urban populations in ancient China. A total of 167 skeletal remains from two sites (Xiaomintun and Xin'anzhuang) were analyzed to examine osteoarthritis at eight appendicular joints and through three spinal osseous indicators. High osteoarthritis frequencies were found in the remains with males showing significantly higher osteoarthritis on the upper body (compared to that of the females). This distinctive pattern becomes more obvious for males from Xiaomintun. Furthermore, Xiaomintun people showed significantly higher osteoarthritis in both sexes than those from Xin'anzhuang. Higher upper body osteoarthritis is speculated to be caused by repetitive lifting and carrying heavy-weight objects, disproportionately adding more stress and thus more osseous changes to the upper than the lower body. Such lifting-carrying could be derived from intensified physical activities in general and specialized occupations in particular. Higher osteoarthritis in males may reveal a gendered division of labour, with higher osteoarthritis in Xiaomintun strongly indicating an occupational difference between the two sites. The latter speculation can be supported by the recovery of substantially more bronze-casting artifacts in Xiaomintun. It is also intriguing that relatively higher osteoarthritis was noticed in Xiaomintun females, which seems to suggest that those women might have also participated in bronze-casting activities as a "family business." Such a family-involved occupation, if it existed, may have contributed to establishment of occupation-oriented neighborhoods as proposed by many Shang archaeologists.

  12. Apatite fission-track thermochronological constraints on the pattern of late Mesozoic-Cenozoic uplift and exhumation of the Qinling Orogen, central China

    Science.gov (United States)

    Chen, Hong; Hu, Jianmin; Wu, Guoli; Shi, Wei; Geng, Yingying; Qu, Hongjie

    2015-12-01

    The Qinling Orogen of central China was formed by intracontinental collision between the North and South China Blocks. The orogen comprises several micro-blocks bounded by sutures and faults, and has undergone long-term intracontinental deformation since the Late Triassic. The micro-blocks include the southern margin of the North China Block (S-NCB), the Northern Qinling Belt (NQB), the Southern Qinling Belt (SQB), and the northern margin of the South China Block (N-SCB). Under a uniform tectonic setting in late Mesozoic-Cenozoic, these micro-blocks have been subjected to a range of deformation styles, as demonstrated by their structural deformation, history of magmatism, and the development of sedimentary basins. To investigate the differences among the micro-blocks and to quantify their uplift and exhumation, we obtained 45 rock samples from eight Mesozoic granites in these micro-blocks, and conducted apatite fission-track (AFT) thermochronological modeling. The results reveal that the Qinling Orogen underwent four distinct stages of rapid cooling histories during the late Mesozoic-Cenozoic, and showed variation in uplift and exhumation whereby the intracontinental deformation started in the south (the N-SCB) and propagated to the north (S-NCB). In the first stage, during the Late Jurassic-Early Cretaceous (ca. 160-120 Ma), rock cooling occurred mainly in the N-SCB, attributed to the clockwise rotation and northward subduction of the South China Block beneath the Qinling Orogen. In the second stage, compression- and extension-related uplift was initiated during the late Early Cretaceous-early Late Cretaceous (ca. 120-90 Ma) in the SQB, consistent with the southward subduction of the North China Block and broadly extensional deformation in the eastern China continent. In the third stage, a gentle regional-scale cooling event that occurred during the latest Cretaceous-Paleocene (ca. 90-50 Ma) started in the NQB and became widespread in the Qinling Orogen. This

  13. Communication imperialism and dependency: a conceptual clarification.

    Science.gov (United States)

    Lee, P S

    1988-01-01

    Communications imperialism has to do with the domination of a country's media activities by another. The ownership, structure, distribution or content of the media in 1 country are affected by pressures from media interests of another country or group out of proportion with those of that country. To determine if this is happening we should consider the country's policies, the private sector;s efforts to export communications elements, and actions of the dominant country against the dominated. The 4 aspects of international media in this situation are television program exportation, foreign ownership and control of media distribution, the infringement of capital opinions on other societies, and the transfer of commercialism and broadcasting norms. In addition to the software and hardware and the other forms of communication such as satellites, computers, and transportation of the mass media, there are the cultural effects on the developing countries. In the case of involuntary of voluntary dependency of the recipient country, the effect of the unbalanced international communication can be harmful or beneficial. Communication dependency may not be harmful to the culture of the recipient country. In determining the theory of unbalanced international communications 3 factors should be considered. There are: the role of the interacting countries, the nature of the dependency of the recipient country, and the beneficial or harmful effect of unbalanced communication pattern on that country.

  14. Tracker electronics testing at Imperial College London

    CERN Document Server

    PPARC, UK

    2006-01-01

    Jonathon Fulcher and Rob Bainbridge testing a rack of CMS Tracker readout electronics at Imperial College London. The signals from the front end APV chips will be transmitted optically to racks of electronics ~100m away in an adjacent underground cavern where they are fed into ~20 crates where 500 CMS Front End Driver boards (FEDs) are located. The FED inputs are 8 fibre ribbons, each ribbon consisting of 12 fibres, each fibre carrying the serially multiplexed data originating from 2 APVs. To test the FEDs special tester boards have been designed to produce simulated APV data in optical form. In the picture the yellow cables are the fibres, which originate from the FED tester boards on the left hand side of the crate as 96 individual fibres, which are then combined into the 8 fibre ribbons feeding the FED board on the right hand side of the crate. Fig. 2 shows an APV25 test board mounted in the X-ray irradiation setup, Fig. 3 the X-ray machine where the chips are irradiated and Fig. 4 the MGPA (Multi-Gain Pre...

  15. [Brief history of cosmetology in the imperial palace of China].

    Science.gov (United States)

    Li, C; Li, J; Liu, D

    2001-07-01

    The development of Chinese Palace's cosmetology is divided into three periods. It is in its embryonic stage that from the Xia to the Western Jin. The drugs and perfumes related to cosmetology were taken seriously by the Palace. The formulation of facial beauty was established. From the Eastern Jin to the end of Tang Dynasty was the forming periods. Cosmetology has been fully developed, and became the physical civilization which could enjoy by both nobels and common people. The developing and enriching time was from the Wu Dai to the end of the Qing Dynasty. The theory of cosmetology achieved a great development. The number of prescriptions of the Palace's cosmetology were increased greatly.

  16. Discovery of a Late Permian Angara-Cathaysia mixed flora from Acheng of Heilongjiang,China,with discussions on the closure of the Paleoasian Ocean

    Institute of Scientific and Technical Information of China (English)

    DENG ShengHui; WAN ChuanBiao; YANG JianGuo

    2009-01-01

    This work documents a new flora from the Upper Permian Hongshan Formation of Acheng County,Heilongjiang Province,Northwest China.The flora consists of 20 species:Paracalamites sp.,Pecopteris tangwangheensis Huang,Callipteris obese Huang,Callipteris shenshuensis Huang,C.tangwangheensis Huang,C.heilongjiangensis Huang,C.zeilleri Zalessky,C.sp.,Comia yichunensis Huang,C.tenueaxis Huang,Iniopteris sibirica Zalessky,Supaia teiliensis Huang,Compsopteris tchirkovae Zalessky,C.cf.adzvensis Zalessky,Nilssonia sp.1,Nil.sp.2,Taeniopteris cf.densissima Halle,T.cf.nystraemfi Halle,T.sp.and Noeggerathiopsis derzavinfi Neub.It is dominated by Angara species but mixed with some typical Cathaysian elements.The age of the flora is assigned to late of the Late Permian according to the stratigraphic ranges of the known species and the comparisons of it with the similar floras.The new discovery indicates that the final collision between the North China Plate and Siberian Plate occurred in Late Permian along the Xar Moron River-Changchun-Yanji sutured zone,and the Paleoasian Ocean was finally closed at the end of the Permian.

  17. Discovery of a Late Permian Angara-Cathaysia mixed flora from Acheng of Heilongjiang,China,with discussions on the closure of the Paleoasian Ocean

    Institute of Scientific and Technical Information of China (English)

    2009-01-01

    This work documents a new flora from the Upper Permian Hongshan Formation of Acheng County, Heilongjiang Province, Northwest China. The flora consists of 20 species: Paracalamites sp., Pecopteris tangwangheensis Huang, Callipteris obese Huang, Callipteris shenshuensis Huang, C. tangwangheensis Huang, C. heilongjiangensis Huang, C. zeilleri Zalessky, C. sp., Comia yichunensis Huang, C. tenueaxis Huang, Iniopteris sibirica Zalessky, Supaia teiliensis Huang, Compsopteris tchirkovae Zalessky, C. cf. adzvensis Zalessky, Nilssonia sp. 1, Nil. sp. 2, Taeniopteris cf. densissima Halle, T. cf. nystraemii Halle, T. sp. and Noeggerathiopsis derzavinii Neub. It is dominated by Angara species but mixed with some typical Cathaysian elements. The age of the flora is assigned to late of the Late Permian according to the stratigraphic ranges of the known species and the comparisons of it with the similar floras. The new discovery indicates that the final collision between the North China Plate and Siberian Plate occurred in Late Permian along the Xar Moron River-Changchun-Yanji sutured zone, and the Paleoasian Ocean was finally closed at the end of the Permian.

  18. West Nile virus in the endangered Spanish imperial eagle.

    Science.gov (United States)

    Höfle, Ursula; Blanco, Juan M; Crespo, Elena; Naranjo, Victoria; Jiménez-Clavero, Miguel Angel; Sanchez, Azucena; de la Fuente, José; Gortazar, Christian

    2008-05-25

    The Spanish imperial eagle (Aquila adalberti) is considered to be the most endangered European eagle. The species is an endemic resident in the Southwestern Iberian Peninsula. We used RT-PCR, immunohistochemistry and seroneutralization to test samples from 13 wild and 18 captive eagles. WNV was detected by RT-PCR in tissues and/or oropharyngeal swabs of eight of 10 (80%) imperial eagles analyzed, and both in apparently clinically healthy birds, and in animals that died due to secondary infections but had symptoms/lesions compatible with WNV. Immunohistochemistry detected WNV antigen in Purkinje cells in the cerebellum, epithelial cells of the gizzard and duodenum, perivascular inflammatory cells, and in Kupffer-cells and hepatocytes. Serum antibodies against WNV were detected in a total of five out of 21 imperial eagles (23.8%), including free-living nestlings (two out of nine samples, 22.2%) and captive adult eagles (three out of 12 samples, 25%). Our results evidence WNV circulation among free-living and captive Spanish imperial eagles in South-central Spain, a dry inland region with no previous WNV evidence, throughout 6 consecutive years. They also indicate the need for further research into this important zoonosis in order to better understand its epidemiology in the Mediterranean ecosystem and in order to understand the role of WNV in the population dynamics of the critically endangered Spanish imperial eagle.

  19. Paleoecologies and paleoclimates of late cenozoic mammals from Southwest China: Evidence from stable carbon and oxygen isotopes

    Science.gov (United States)

    Biasatti, Dana; Wang, Yang; Gao, Feng; Xu, Yingfeng; Flynn, Lawrence

    2012-01-01

    To examine paleodiets and habitats of extinct taxa and to understand long-term regional climate change, we determined the carbon and oxygen isotopic compositions of fossil herbivore teeth and soil samples from six localities in Yunnan Province, Southwest China, ranging in age from ˜10 Ma to the present. Although limited in spatial and temporal coverage, these initial results reveal significant changes in the environments and diets of mammalian taxa over the last 10 million years. Prior to 2-3 Ma, while most mammals examined had pure or nearly pure C 3 diets, some individuals consumed a small amount of C 4 grasses (up to 20% C 4). Since then, C 4 grasses became a significant dietary component for most herbivores as indicated by higher enamel-δ 13C values in the Pleistocene Yuanmou Formation and at Shangri-La, most likely reflecting an increased C 4 biomass in the region. The carbon isotope results show that the diets of mammals of ˜2.5-1.75 Ma from Shangri-La ranged from pure C 3 to pure C 4 while 1.7 Ma horses from Yuanmou had 0-70% C 4 grasses in their diets. Mammals living at ˜8-7 Ma in the Yuanmou and Lufeng region had very similar diets and habitats, with similar climatic conditions. Increased C 4 biomass after ˜3-4 Ma suggests a significant change in certain aspects of regional climate, such as increased seasonality of rainfall or an increase in seasonal drought and fires as these factors are important to modern grasslands. The data also show that unlike the Siwalik fauna in the Indian subcontinent, mammals in Yunnan on the southeast side of the Himalayan-Tibetan Plateau lived in an environment dominated by dense forests until ˜3-4 Ma. Nonetheless, both δ 13C values of paleosol carbonates and fossil enamels indicate that C 4 grasses were present in the Yuanmou region in the latest Miocene and Pliocene (˜8-3.5 Ma), likely in greatly dispersed, small patches of open habitats where the forest canopy was broken or on flood plains, and the C 4 biomass

  20. Late Triassic tuff intervals in the Ordos basin, Central China: Their depositional, petrographic, geochemical characteristics and regional implications

    Science.gov (United States)

    Qiu, Xinwei; Liu, Chiyang; Mao, Guangzhou; Deng, Yu; Wang, Feifei; Wang, Jianqiang

    2014-02-01

    Tuff intervals of Upper Triassic Yanchang Formation are laterally widespread in the Ordos basin, Central China. This paper focuses on magmatic origins and potential source regions of these tuff intervals through detail depositional, petrographic and geochemical analyses. Most of the tuff intervals are well-documented at the bottom of the Chang7 oil reservoir unit and can be correlated laterally, and certain tuff beds are reworked by turbidity current or seismic activity. Petrographic studies of the Chang7 tuffs indicate that they are composed of crystal shards, lithic shards and altered glass shards, and the crystal shards include plagioclase, quartz and biotite. Alteration of the Chang7 tuffs is ubiquitous, thus, most of these tuffs transformed into illite/smectite (I/S) mixed-layers which are identified by scanning electron microscopy (SEM) and X-ray diffraction (XRD). Less common minerals are also detected in the Chang7 tuffs such as zircon, hematite, siderite, anatase. Major elements are determined by the X-ray fluorescence (XRF) analysis, the results indicate that the Chang7 tuffs are enriched in K2O (average 4.21%), the ratio of SiO2/Al2O3 ranges from 1.73 to 2.85 (average 2.17), and the ratio of TiO2/Al2O3 varies between 0.006 and 0.032 (average 0.017), which imply that the Chang7 tuffs originated from a felsic parental magma. Trace elements are determined by inductively coupled plasma mass spectrometry (ICP-MS), indicating the total rare earth element (∑REE) concentrations are variable, and range from 117.46 to 466.83 ppm (average 251.88 ppm). REE distribution pattern of the Chang7 tuffs presents a LREE rightward incline with flat HREE curve. The value of δEu ranges from 0.151 to 0.837 (average 0.492), suggesting a strong to weak negative Eu anomaly. The Chang7 tuffs show positive anomalies in Rb, Th and U and negative anomalies in Nb, Sr and Eu on a primitive mantle normalized spidergram. A preliminary analysis of the geochemical composition of the

  1. Rapid sea-level change in the Late Guadalupian (Permian) on the Tethyan side of South China: litho- and biostratigraphy of the Chaotian section in Sichuan.

    Science.gov (United States)

    Isozaki, Yukio; Yao, Jianxin; Ji, Zhangshen; Saitoh, Masafumi; Kobayashi, Noritada; Sakai, Harutaka

    2008-01-01

    The Capitanian (Late Guadalupian) Maokou Formation at Chaotian in northern Sichuan, South China, is composed mainly of shallow marine shelf carbonates deposited on the Tethyan side of South China. By detailed field mapping and scientific drilling, we newly found out unique fossil assemblages and a sharp lithologic change in the upper part of the Maokou Formation. The main part of the Maokou Formation (over 130 m thick) is composed of algal packstone with Wordian-Capitanian large-tested fusulines, rugose corals and other sessile benthos, whereas the Uppermost Member (13 m thick) is composed of black limy mudstone/chert with Capitanian offshore biota (ammonoids, radiolarians, and conodonts). The topmost Capitanian conodont zones are missing; however, the Maokou Formation is disconformably overlain by 260+/-4 Ma volcanic ash (Wangpo bed) and the Early Lopingian Wujiaping Formation with plant-bearing coaly mudstone and shallow marine carbonates (packstone). The newly identified facies change indicates that northern Sichuan has experienced rapid sea-level changes in the late Guadalupian, i.e., first a transgression in the mid-Capitanian and then a regression across the Guadalupian-Lopingian boundary. As the end-Guadalupian is characterized by a global regression, such a volatile sea-level fluctuation, in particular the sea-level rise, is unique to the Tethyan side of South China. The newly recognized relatively deep-water late Guadalupian sequence adds new paleo-environmental information and further provides a paleotectonic interpretation of the low-latitude eastern Tethyan margin immediately before the end-Guadalupian mass extinction.

  2. Cultural Nationalism, Orientalism, Imperial Ambivalence: The Colored American Magazine and Pauline Elizabeth Hopkins

    Directory of Open Access Journals (Sweden)

    Yu-Fang Cho

    2011-12-01

    Full Text Available

    This essay examines African American novelist Pauline Hopkins’s deployment of the trope of respectable domesticity to contest black disenfranchisement in the context of African Americans’ ambivalent relationship to late-nineteenth-century US imperial expansion in the Asia Pacific. This essay analyzes Contending Forces (1900 in relation to two crucial yet underexplored contexts: first, Hopkins’s commentaries on international race relations; second, African American intellectuals’ commentaries on US imperial ventures in the Asia Pacific and on Chinese immigration in the Colored American Magazine, where Hopkins’s fictional works were serialized. Situated within these contexts of comparative racialization, Hopkins’s works offer critical responses to the masculine nationalist representations of black–Asian relations, illuminating the divisive effects of nationalist identification on differentially racialized subjects, the uneven effects of marriage on the black community, and this institution’s structural ties to imperialism and to the color-based class hierarchy within the imagined black community—all of which call for radical reimagining of race relations beyond the nation form.

  3. INTERNATIONAL SECURITY RELATIONS AND POST-IMPERIAL ORDERS

    Directory of Open Access Journals (Sweden)

    Radu-Sebastian UNGUREANU

    2011-08-01

    Full Text Available This paper intends to investigate the relations between former imperial powers and new sovereign states succeeding an empire in the field of international security, particularly when involving the use of force. Despite their stated attachment to the normative principles of what we usually call “Westphalian order”, former imperial powers continue to interfere in the domestic affairs of these new states, especially those unable to exercise their sovereignty efficiently and legitimately. One could say that, by military interventions, these powers deny the sovereignty of weak states in the regions once under their control; but the preparation of these missions makes the actions not to be interpreted as expressions of an imperialist attitude. I consider there are two major ideal-types that could better explain such interventions. In a power-oriented post-imperial order, the intervention of a former empire is the result of the projection of its national interests and identities. In a norm-oriented post-imperial order, the sense of moral responsibility of the former imperial power is the main reason for its interference. The intervention’s legitimacy and suitability require domestic and international support. This paper, grounded on a constructivist approach, intends to contribute to the understanding of international security issues in terms of a world shaped by actors’ interests and identities and the dynamics of their relations. The identified ideal-types of post-imperial orders consider both material and cultural factors. The analytical elements that may link extremely different situations are the socially variable interpretations of past and present.

  4. SLC26A4 gene polymorphism and late-onset Alzheimer's disease in a Han Chinese population from Qingdao,China

    Institute of Scientific and Technical Information of China (English)

    Jifang Zhang; Yantuan Li

    2013-01-01

    In a recent genome-wide association study, the SLC26A4 gene rs2072064 polymorphism was found to be associated with late-onset Alzheimer's disease in Caucasians. Here, we investigated this association in a large Northern Han Chinese cohort consisting of 599 sporadic late-onset Alzheimer's disease patients and 598 healthy controls matched for sex and age in a Northern Han Chinese population from Qingdao, China. Genotyping by the polymerase chain reaction-ligase detection reaction revealed that there were significant differences in the genotype (P = 0.017) and allele (P = 0.007) frequencies of the rs2072064 polymorphism between late-onset Alzheimer's disease patients and controls. The A allele of this polymorphism was significantly associated with a reduced risk of late-onset Alzheimer's disease (odds ratio (OR) = 0.792, 95% confidence interval (CI) = 0.670–0.937, P = 0.007). When the data were stratified by the apolipoprotein E ε4 status, there was a significant difference only among apolipoprotein E ε4 non-carriers (genotypic P = 0.001, allelic P = 0.001). Furthermore, the association between rs2072064 and late-onset Alzheimer's disease remained significant by logistic regression analysis after adjustment for age, gender, and the apolipoprotein E ε4 carrier status (dominant model: OR = 0.787, 95% CI = 0.619–1.000, P = 0.050; recessive model: OR = 0.655, 95% CI = 0.448–0.959, P = 0.030; additive model: OR = 0.792, 95% CI = 0.661–0.950, P = 0.012). These findings suggest that SLC26A4 is a susceptibility gene for late-onset Alzheimer's disease in a Northern Han Chinese population from the Qingdao area.

  5. A Critique of the 'American Accent' and Linguistic Imperialism

    Institute of Scientific and Technical Information of China (English)

    康建刚

    2007-01-01

    Linguistic imperialism has been widespread throughout the world, especially when English has become the dominant has brought about the abundance of a lot of training programmes and websites such as www.americanaccent.com.This essay analyses this website from the perspectives of micro- and macro-indexicalities and presents a critique of the linguistic imperialism.Moreover, the article gives suggestions as to how to take advantage of the language resources for our best benefit and at the same time how to resist the linguistic hegemony in our teaching and learning of the English language.

  6. Rethinking imperialist theory and US imperialism in Latin America

    Directory of Open Access Journals (Sweden)

    James Petras

    2011-10-01

    Full Text Available En este artículo criticamos la teorización contemporánea sobre el imperialismo por su reducción al ámbito económico y su carencia de un análisis de clase e institucional específico dentro del estado imperialista. En el contexto de este argumento, establecemos la importancia del análisis de clase para aprovechar las dinámicas de cambio del poder imperialista procediendo a argumentar la alineación de las fuerzas de clase en el mundo de la economía, en sus interacciones con la configuración del poder imperialista, dejando la realineación del poder económico en el sistema mundial capitalista que constituye el mayor cambio para el imperialismo estadounidense en sus operaciones en América Latina. En la sección final del artículo explicamos las discontinuidades y continuidades en las relaciones imperialistas estadounidenses con Latinoamérica, y las potencialidades y contrastes de estas relaciones en el crecimiento económico y el desarrollo.Palabras clave: teoría imperialista, imperialismo estadounidense, Latinoamérica_____________________Abstract:In this paper we criticize contemporary theorizing about imperialism for its economic reductionism and a lack of class analysis and institutional specificity regarding the imperial state. In the context of this argument we establish the importance of class analysis for grasping the changing dynamics of imperial power before proceeding to argue how specific alignments of class forces in the world economy, in their interactions with existing imperial power configurations, is leading to a realignment of economic power in the world capitalist system that constitutes a major challenge for US imperialism in its Latin American operations. In the final section of the paper we point to the discontinuities and continuities in US imperial relations with Latin America, and the potentialities and constraints of these relations on economic growth and development.Keywords: Imperialism Theory, US

  7. 78 FR 894 - Interim Final Determination To Stay Sanctions, Imperial County Air Pollution Control District

    Science.gov (United States)

    2013-01-07

    ... AGENCY 40 CFR Part 52 Interim Final Determination To Stay Sanctions, Imperial County Air Pollution... of revisions to the Imperial County Air Pollution Control District (ICAPCD) portion of the California... such as unpaved roads and disturbed soils in open and agricultural areas in Imperial County....

  8. Risk factors associated with late preterm births in the underdeveloped region of China: A cohort study and systematic review

    Directory of Open Access Journals (Sweden)

    Liqun Lu

    2015-12-01

    Conclusion: A number of factors are associated with late preterm births, and the incidence in underdeveloped regions is high. The inconsistent results between our study and previous reports indicate more attention towards preventing late preterm births in undeveloped regions is needed.

  9. Surface displacement on the Imperial and Superstition Hills faults triggered by the Westmorland, California, earthquake of 26 April 1981

    Science.gov (United States)

    Sharp, R.V.; Lienkaemper, J.J.; Rymer, M.J.

    1982-01-01

    Parts of the Imperial and the Superstition Hills faults moved right-laterally at the ground surface at the time of or shortly following the ML 5.6 Westmorland earthquake of 26 April 1981. The displacements occurred prior to any significant aftershocks on either fault and thus are classed as sympathetic. Although the main shock was located in an exceptionally seismogenic part of Imperial Valley, about 20 km distant from either fault, no clear evidence of surface faulting has yet been found in the epicentral area. Horizontal displacement on the Imperial and Superstition Hills faults, southeast and southwest of the epicenter, respectively, reached maxima of 8 mm and 14 mm, and the discontinuous surface ruptures formed along approximately equal lengths of northern segments of the two structures (16.8 km and 15.7 km, respectively). The maximum vertical component of slip on the Imperial fault, 6 ram, was observed 3.4 km north of the point of largest horizontal slip. Vertical movement on the Superstition Hills fault was less than 1 mm. No new displacement was found along the traces of the Brawley fault zone, the San Andreas fault, or the part of the Coyote Creek fault that slipped during the 1968 Borrego Mountain earthquake. A careful search in the epicentral area of the main shock failed to locate any definite evidence of surface faulting. Concentrations of late aftershocks north and northeast of Calipatria near the southeastward projection of the San Andreas fault occurred mostly after our field check; this area was not investigated.

  10. Recently Exposed Fumarole Fields Near Mullet Island, Imperial County, California

    Science.gov (United States)

    Lynch, D. K.; Hudnut, K.; Adams, P.; Bernstein, L.

    2011-12-01

    New field observations, lidar measurements, aerial imaging and preliminary laboratory measurements of mud samples are reported of three formerly submerged fumarole fields in the Salton Trough near Mullet Island in southeastern California, USA. The fumarole fields have recently been exposed as the Salton Sea level has dropped. The largest of the three fields visited in January 2011 is irregular in outline with a marked northeast elongation. It is roughly 400 meters long and 120 meters wide. The field consists of approximately one hundred warm to boiling hot (100° C) mud volcanoes (0.1 - 2 m in height), several hundred mud pots, and countless CO2 gas vents. Unusual shaped mud volcanoes in the form of vertical tubes with central vents were observed in many places. Lidar measurements were obtained in the time period Nov 9-13, 2010 using an Optech Orion 200M lidar from an elevation 800 m AGL. They reveal that the terrain immediately surrounding the two fields that are above water level reside on a low (~0.5 m high) gently sloping mound about 500 m across that shows no evidence of lineaments indicative of surface faulting. With other geothermal features, the fumaroles define a well-defined line marking the probable trace of the Calipatria fault. Although the precise locations is uncertain, it appears to define a straight line 4 km long between the Davis-Schrimpf mud volcanoes and Mullet Island. Mullet Island is one of five late Quaternary rhyolitic volcanic necks in the immediate area of the fumaroles. The Calipatria fault is subparallel to the San Andreas and Imperial faults and only one of many verified or suspected faults (including cross faults) in the complex tectonic setting of the Salton Trough. Mud from several volcanoes was analyzed using scanning electron microscopy (SEM), and energy dispersive X-ray spectroscopy (EDS). One sample contained boussingaultite, (NH4)2Mg(SO4)2.6(H2O), a rare mineral that is known to sublime under fumarolic conditions, possibly by

  11. Mantle xenoliths from Late Cretaceous basalt in eastern Shandong Province: New constraint on the timing of lithospheric thinning in eastern China

    Institute of Scientific and Technical Information of China (English)

    YAN Jun; CHEN Jiangfeng; XIE Zhi; ZHOU Taixi

    2003-01-01

    The age of the alkali basalt from Daxizhuang in Jiaozhou, eastern Shandong, was determined to be 73.5 ± 0.3Ma by40Ar-39Ar technique. The basalt gave high εNd(t) values of +7.5 and +7.6, suggesting that the primitive magma was derived from depleted asthenospheric mantle with a formation depth of about 65-95 km. Spinel-lherzolite xenoliths have been discovered in the basalt. The Fo values of olivine from the xenoliths range from 88 to 89. The estimated equilibrium P-T conditions of spinel-lherzolite xenoliths are about 2.0 GPa and 1010-1140℃, suggesting an equilibrium depth of about 65 km. Geochemical characteristics of the Late Mesozoic (125-115 Ma) mantle-derived rocks in Shahdong Province suggest an enriched lithospheric mantle along the southern margin of the North China block. However,geochemical characteristics of the Late Cretaceous basalts in Daxizhuang and the equilibrium P-T condition estimated from the xenoliths suggest that the lithosphere at 73 Ma ago was as thick as that of the Cenozoic in the region. Additionally, the xenoliths are rich in basaltic-component, suggesting a derivation from a newly-formed lithosphere. Therefor,lithospheric thinning took place at a time interval between about 120 and 73 Ma along the southern margin of the North China block.

  12. GEM in the marine atmosphere and air-sea exchange of Hg during late autumn and winter cruise campaigns over the marginal seas of China

    Science.gov (United States)

    Wang, Yan; Liu, Ruhai; Li, Yanping; Cui, Xueqing; Zhou, Jianping; Liu, Shixuan; Zhang, Yuqing

    2017-07-01

    East Asia is one of the primary sources of atmospheric gaseous elemental mercury (GEM) among the world. In this study, GEM concentrations were measured during two cruises in late autumn and winter of 2012 and 2013 which passed through the marginal seas of China. The results show that the mean GEM concentration was 1.65 ng/m3 from the South China Sea to the Yellow Sea during the 2012 cruise. While the mean GEM concentration was 2.38 ng/m3 in the South Yellow Sea, and 1.75 ng/m3 in the North Yellow and Bohai Seas during the 2013 cruise. High GEM contents were detected when the steering wind was offshore. There is a significant positive relationship between GEM and air temperature for these two cruises. Low GEM content was presented when the cold northerly monsoon prevailed while air masses mainly came from the clean northern oceanic region. Dissolved gaseous mercury (DGM) concentration in the surface water of the south Yellow and Bohai seas were 74.4 ± 28 pg/L. DGM concentrations were correlated with water temperature (r = 0.244, p polluted air and low wind speed. High flux values were caused by the northerly monsoon which carried remote clean air to the sea, with large wind speeds. The northerly monsoon is an important factor affecting the GEM transport offshore to marginal sea and the cycle of mercury in the sea in late autumn and winter.

  13. US Imperialism, Transmodernism and Education: A Marxist Critique

    Science.gov (United States)

    Cole, Mike

    2004-01-01

    The author begins by discussing David Geoffrey Smith's analysis of the enantiomorphism inherent in the rhetoric of New American Imperialism. He goes on to examine critically Smith's defence of Enrique Dussel's advocacy of transmodernism as a way of understanding this enantiomorphism and of moving beyond what are seen as the constraints of both…

  14. Strategic environmental management of air in Mexicali-Imperial border.

    Directory of Open Access Journals (Sweden)

    José María Ramos García

    2011-07-01

    Full Text Available This article analyzes the importance of an approach on local environmental management regarding the quality of air in the Mexicali and Imperial Valley region. The paper discusses that the absence of a strategic approach in the environmental local policy will enhance the air pollution in the region

  15. Ironic imperialism : how Russian patriots are reclaiming postmodernism

    NARCIS (Netherlands)

    Noordenbos, Boris

    2011-01-01

    This essay analyzes the recent appearance in Russian letters of ultra-nationalist fantasies about the restoration of Russia's imperial or totalitarian status. This new trend has its roots not only in the increasingly patriotic tone of Russian society and politics, but also in the dynamics of the lit

  16. (Re)experiencing Hegemony: The Linguistic Imperialism of Robert Phillipson.

    Science.gov (United States)

    Berns, Margie; Barrett, Jeanelle; Chan, Chak; Chikuma, Yoshiki; Friedrich, Patricia; Hadjidimos, Olga-Maria; Harney, Jill; Hislope, Kristi; Johnson, David; Kimball, Suzanne; Low, Yvonne; McHenry, Tracey; Palaiologos, Vivienne; Petray, Marnie; Shapiro, Rebecca; Shook, Anna Ramirez

    1998-01-01

    Reading Phillipson's "Linguistic Imperialism" in a World Englishes graduate seminar at Purdue University prompted intense discussion not only on the issues the author raised, but also on the rhetorical style and strategies that he chose to present a story of oppression. This article documents the reactions of the students.(Author/VWL)

  17. Language Choice and Cultural Imperialism: A Nigerian Perspective.

    Science.gov (United States)

    Bisong, Joseph

    1995-01-01

    Argues against the thesis put forth in Phillipson's "Linguistic Imperialism," that the relationship between core English-speaking countries and periphery-English countries is one of dominant and dominated languages, as it applies to Nigeria. It is maintained that the sociolinguistic and sociocultural realities of the country have not been properly…

  18. Bologna Goes Global: A New Imperialism in the Making?

    Science.gov (United States)

    Hartmann, Eva

    2008-01-01

    This paper argues that imperialism continues to exist today. It focuses on the ideational dimension of such power constellation and highlights the role of "educational diplomacy". Specifically, it examines norm-settings within international educational politics as a way of identifying shifts within what might be called benevolent…

  19. The Civilisers, British Engineers, Imperialism and Africa 1880-1914

    DEFF Research Database (Denmark)

    Andersen, Casper

    2009-01-01

    as an interconnected dynamic unity in which engineers were situated; the geographical and ideological context in which their activities took place. The thesis can be read as a contribution to recent re-conceptualisations of the British Empire as a zone bind together by ‘colonial connections' and ‘imperial networks...

  20. Imperial Contradictions: Is the Valley a Watershed, Region, or Cyborg?

    Science.gov (United States)

    Rudy, Alan P.

    2005-01-01

    Is California's Imperial Valley a watershed? If so, at what level and by what topographic logic? Is it a region? If so, at what level and by what geographic logic? Are its boundaries natural, political, or multivalent on different scales? In short, this essay looks at the special (re)production of environmental conditions within a cyborg world.…

  1. Late Cenozoic sedimentary process and its response to the slip history of the central Altyn Tagh fault, NW China

    Institute of Scientific and Technical Information of China (English)

    陈正乐; 张岳桥; 陈宣华; 王小凤; A.S.Ramon; W.B.Zack

    2001-01-01

    The ENE-striking Altyn Tagh fault (ATF), extending along the northern edge of the Tibetan Plateau, is one of the major important strike-slip faults, and has been known as one of the key areas to debate the eastward extrusion and crustral shortening models of the Tibetan Plateau during and after India-Asia collision. This paper mainly presents new evidence of Late Cenozoic sedimentary process to reconstruct the slip history of the ATF during the Late Cenozoic. Field measurements and laboratory analyses of the sedimentary characteristics in the Late Cenozoic basins in the central Altyn Tagh fault suggest that Late Cenozoic sedimentary sequence should be divided into three units according to facies changes. The paleo-topography reconstruction shows that the sedimentation in these basins was tightly related with the fault, indicating that the ATF has experienced at least three stages of strike slipping in the Late Cenozoic. New geological data from the Late Cenozoic sedimentary basins and the formation of th

  2. 帝国主义—从帝国主义到文化帝国主义%Cultural Imperialism—From Imperialism to Cultural Imperialism

    Institute of Scientific and Technical Information of China (English)

    高秀石

    2012-01-01

    Imperialism has gone through three phases: geographical imperialism, economical imperialism and cultural imperialism. These three forms are connected with each other. The society has entered a new era of globalization, modernization and information, followed by the transition from imperialism to cultural imperialism. Imperialism is different from cultural imperialism in four aspects. China’s attitude towards cultural imperialism is to protect own heritage openly and tolerantly.%帝国主义经历了三个阶段: 地域性帝国主义、帝国主义和文化帝国主义。这三种形式彼此联系。现代社会进入了一个新时代,全球化、现代化和信息化。伴随着帝国主义过渡到文化帝国主义。文化帝国主义在四个方面不同于帝国主义。中国对待文化帝国主义的立场应该是用开放和宽容的态度接纳并保护独有的文化遗产。

  3. CIDADES NEGRAS – PETRÓPOLIS IMPERIAL

    Directory of Open Access Journals (Sweden)

    Renata Aquino

    2014-12-01

    Full Text Available Cidade negra e população negra são o enfoque deste artigo sobre a cidade de Petrópolis na Região Serrana do estado do Rio de Janeiro, visando estabelecer novos parâmetros para discussão do espaço geográfico da região da cidade de Petrópolis por meio de outras explicações sobre o povoamento e desenvolvimento desta localidade. Cidade que a história oficial consagrou como cidade imperial e de colonização alemã, negando de forma ideológica as atividades econômicas da cidade e da região e tornando invisível a existência de população de maioria afrodescendente. Apresentamos neste artigo uma discussão sobre a ideologia da colonização alemã como solução para o Brasil, o que explica a imigração alemã para a localidade e também permite compreender a formação da ideologia sobre as origens populacionais e econômicas deste lugar. Argumentamos contra tal ideologia, reafirmando e investigando a existência de colonizadores africanos a partir das diversas fontes que podem levar ao encontro das inscrições afro, materiais e imateriais, na história e na cultura da região. Partimos da ideia da constituição de um território no período colonial que se deu devido ao fluxo de populações dos arredores, não somente devido à Estrada do Ouro. A base do povoamento da região veio das fazendas que exploravam o trabalho escravizado. Do território ocupado por africanos e afrodescendentes, nasceu a cidade que, posteriormente, instalou alguns grupos de alemães e, nesta fusão populacional, constituiu-se a forte presença de populações negra e mesmo branca, de outra origem que não a alemã. Local que devido à existência da Estrada do Ouro, ligando cidades mineiras ao porto do Rio de Janeiro, recebeu as inscrições de povoamento de africanos e afrodescendente pelos dois séculos antes da fundação oficial da cidade. O artigo se concentra nos documentos que demonstram a existência de população negra na localidade.

  4. Instability of seawater pH in the South China Sea during the mid-late Holocene: Evidence from boron isotopic composition of corals

    Science.gov (United States)

    Liu, Yajing; Liu, W.; Peng, Z.; Xiao, Y.; Wei, G.; Sun, W.; He, J.; Liu, Gaisheng; Chou, C.-L.

    2009-01-01

    We used positive thermal ionization mass spectrometry (PTIMS) to generate high precision ??11B records in Porites corals of the mid-late Holocene from the South China Sea (SCS). The ??11B values of the Holocene corals vary significantly, ranging from 22.2??? to 25.5???. The paleo-pH records of the SCS, reconstructed from the ??11B data, were not stable as previously thought but show a gradual increase from the Holocene thermal optimal and a sharp decrease to modern values. The latter is likely caused by the large amount of anthropogenic CO2 emissions since the Industrial Revolution but variations of atmospheric pCO2 cannot explain the pH change of the SCS before the Industrial Revolution. We suggest that variations of monsoon intensity during the mid-late Holocene may have driven the sea surface pH increase from the mid to late Holocene. Results of this study indicate that the impact of anthropogenic atmospheric CO2 emissions may have reversed the natural pH trend in the SCS since the mid-Holocene. Such ocean pH records in the current interglacial period can help us better understand the physical and biological controls on ocean pH and possibly predict the long-term impact of climate change on future ocean acidification. ?? 2008 Elsevier Ltd. All rights reserved.

  5. Geochemistry of Late Triassic pelitic rocks in the NE part of Songpan-Ganzi Basin, western China: Implications for source weathering, provenance and tectonic setting

    Directory of Open Access Journals (Sweden)

    Yan Tang

    2012-09-01

    Full Text Available Major, trace and rare earth element (REE concentrations of Late Triassic sediments (fine-grained sandstones and mudstones from Hongcan Well 1 in the NE part of the Songpan-Ganzi Basin, western China, are used to reveal weathering, provenance and tectonic setting of inferred source areas. The Chemical Index of Alteration (CIA reflects a low to moderate degree of chemical weathering in a cool and somewhat dry climate, and an A-CN-K plot suggests an older upper continental crust provenance dominated by felsic to intermediate igneous rocks of average tonalite composition. Based on the various geochemical tectonic setting discrimination diagrams, the Late Triassic sediments are inferred to have been deposited in a back-arc basin situated between an active continental margin (the Kunlun-Qinling Fold Belt and a continental island arc (the Yidun Island Arc. The Triassic sediments in the study area underwent a rapid erosion and burial in a proximal slope-basin environment by the petrographic data, while the published flow directions of Triassic turbidites in the Aba-Zoige region was not supported Yidun volcanic arc source. Therefore, we suggest that the Kunlun-Qinling terrane is most likely to have supplied source materials to the northeast part of the Songpan-Ganzi Basin during the Late Triassic.

  6. Three new species of mesosciophilid gnats from the Middle-Late Jurassic of China (insecta: Diptera: Nematocera: Mesosciophilidae).

    Science.gov (United States)

    Zhang, J F

    2008-11-15

    Three extinct new species from the Callovian or Oxfordian (uppermost Middle Jurassic or lowermost Upper Jurassic) Daohugou beds in Inner Mongolia, China is described as Mesosciophila abstracta sp. n., Mesosciophilodes synchrona sp. n. and Paramesosciophilodes eximia sp. n. (Family Mesosciophilidae). All the records of mesosciophilid gnats are briefly reviewed.

  7. Late Permian to Early Oligocene granitic magmatism of the Phan Si Pan uplift area, NW Vietnam: their relationship to Phanerozoic crustal evolution of Southwest China

    Science.gov (United States)

    Pham, T. T.; Shellnutt, G.

    2015-12-01

    The Phan Si Pan uplift area of NW Vietnam is a part of the Archean to Paleoproterozoic Yangtze Block, Southwest China. This area is of particular interest because it experienced a number of Phanerozoic crustal building events including the Emeishan Large Igneous Province, the India-Eurasia collision and Ailaoshan - Red River Fault displacement. In the Phan Si Pan uplift area, there are at least three different geochronological complexes, including: (1) Late Permian, (2) Eocene and (3) Early Oligocene. (1) The Late Permian silicic rocks are alkali ferroan A1-type granitic rocks with U/Pb ages of 251 ± 3 to 254 ± 3 Ma. The Late Permian silicic rocks of Phan Si Pan uplift area intrude the upper to middle crust and are considered to be part of the ELIP that was displaced during the India-Eurasian collision along the Ailaoshan-Red River Fault shear zone and adjacent structures (i.e. Song Da zone). Previous studies suggest the Late Permian granitic rocks were derived by fractional crystallization of high - Ti basaltic magma. (2) The Eocene rocks are alkali ferroan A1-type granites (U/Pb ages 49 ± 0.9 Ma) and are spatially associated with the Late Permian granitic rocks. The trace element ratios of this granite are similar to the Late Permian rocks (Th/Nb=0.2, Th/Ta = 2.5, Nb/U = 24, Nb/La =1.2, Sr/Y=1). The origin of the Eocene granite is uncertain but it is possible that it formed by fractional crystallization of a mafic magma during a period of extension within the Yangtze Block around the time of the India-Eurasia collision. (3) The Early Oligocene granite is characterized as a peraluminous within-plate granite with U/Pb ages of 31.3 ± 0.4 to 34 ± 1 Ma. The Early Oligocene granite has trace element ratios (Th/Nb = 2.1, Th/Ta = 22.6, Nb/U = 4.4, Nb/La = 0.4, Sr/Y = 60.4) similar to crust melts. The high Sr/Y ratio (Sr/Y = 20 - 205) indicates a lower crust source that was garnet-bearing. The Phan Si Pan uplift was neither a subduction zone nor an arc environment

  8. A grain-size record from Beijing region in Northern China: Late Quaternary paleoclimate oscillation in response to global change

    Institute of Scientific and Technical Information of China (English)

    Guifang YANG; Zhiliang GE; Qing DAI; Jie CHENG; Gongming YIN; Lihong ZAN; Jingwei LIU

    2009-01-01

    Numerous samples taken from one core at the Beijing plain were utilized to characterize the paleocli-matic configuration of the study area and its possible relation to global control since the last interglaciation. We presented here a detailed grain-size record for the full length of Late Pleistocene, along with the optical simulated luminescence (OSL) dating. Our findings revealed that Late Pleistocene of the study area started approximately at 110 ka B.P. represented by the thick sediments of 31 m in Changping depression. Four sedimentary cycles were outlined in the core during Late Pleistocene, corresponding to marine isotope stage (MIS) 5 to 2. Controlled by regional geology and global climatic setting, eight paleoclimatic periods were identified simultaneously in the study area on the time scale of 104 year, with the warm and moist climate being found at 110- 96, 92- 76, 67- 56,and 28-18ka B.P.. The climatic instabilities on a millennial scale in Late Pleistocene were characterized largely by the occurrence of 6 strong Heinrich events shown by comparatively coarse groups. These variations correlate well with those documented in the GRIP Greenland and in the Northern Atlantic Ocean, though more complex features may exist on the long time scale.

  9. Amalgamation of East Eurasia Since Late Paleozoic: Constraints from the Apparent Polar Wander Paths of the Major China Blocks

    Science.gov (United States)

    Wu, L.; Kravchinsky, V. A.; Potter, D. K.

    2014-12-01

    It has been a longstanding challenge in the last few decades to quantitatively reconstruct the paleogeographic evolution of East Eurasia because of its great tectonic complexities. As the core region, the major China cratons including North China Block, South China Block and Tarim Block hold the key clues for the understanding of the amalgamation history, tectonic activities and biological affinity among the component blocks and terranes in East Eurasia. Compared with the major Gondwana and Laurentia plates, however, the apparent polar wander paths of China are not well constrained due to the outdated paleomagnetic database and relatively loose pole selection process. With the recruitment of the new high-fidelity poles published in the last decade, the rejection of the low quality data and the strict implementation of Voo's grading scheme, we build an updated paleomagnetic database for the three blocks from which three types of apparent polar wander paths (APWP) are computed. Version 1 running mean paths are constructed during the pole selection and compared with those from the previous publications. Version 2 running mean and spline paths with different sliding time windows are computed from the thoroughly examined poles to find the optimal paths with the steady trend, reasonable speed for the polar drift and plate rotation. The spline paths are recommended for the plate reconstructions, however, considering the poor data coverage during certain periods. Our new China APWPs, together with the latest European reference path, the geological, geochronological and biological evidence from the studied Asian plates allow us to reevaluate the paleogeographic and tectonic history of East Eurasia.

  10. Why was there no capitalism in early modern China?

    Directory of Open Access Journals (Sweden)

    TIAGO NASSER APPEL

    Full Text Available ABSTRACT In this paper, we ask the following question: why couldn’t Early Modern China make the leap to capitalism, as we have come to know it in the West? We suggest that, even if China compared well with the West in key economic features - commercialization and commodification of goods, land, labor - up to the 18th century, it did not traverse the path to Capitalism because of the “fact of empire”. Lacking the scale of fiscal difficulties encountered in Early Modern Europe, Late Imperial China did not have to heavily tax merchants and notables; therefore, it did not have to negotiate rights and duties with the mercantile class. More innovatively, we also propose that the relative lack of fiscal difficulties meant that China failed to develop a “virtuous symbiosis” between taxing, monetization of the economy and public debt. This is because, essentially, it was the mobilization of society’s resources - primarily by way of public debt or taxes - towards the support of a military force that created the first real opportunities for merchants and bankers to amass immense and unprecedented wealth.

  11. Middle and Late Devonian microbial carbonates, reefs and mounds in Guilin, South China and their sequence stratigraphic, paleoenvironmental and paleoclimatic significance

    Institute of Scientific and Technical Information of China (English)

    SHEN Jianwei; TENG Jianbin; Pedoja Kevin

    2005-01-01

    Microbial precipitation of calcium carbonate has played a major role in formation of carbonate platforms since the Archean. Also, microbial carbonates and biologically induced cement are important contributors to reef framework volume and rigidity in carbonate platform systems during times of significant environmental change including transgressive events in platform environments and the recovery interval following the major biotic crisis. The stratigraphic distribution of different types of microbial carbonates appears to vary within the sequence stratigraphic framework. Reefs and mounds within the Late Devonian carbonate platforms in Guilin, South China are formed primarily by calcimicrobes and biologically induced cement, representing the microbe-dominated and characteristic carbonate buildups within a reefal ecosystem that nearly all reef-building metazoans were absent after the Frasnian/Famennian biotic crisis. Microbial community and microbialite seem to be linked with specific palaeoenvironment and palaeoclimate, suggesting that they could be used as indicators of environmental change and biotic events.

  12. Late Paleozoic Fluid Systems and Their Ore-forming Effects in the Yuebei Basin, Northern Guangdong, China

    Institute of Scientific and Technical Information of China (English)

    2005-01-01

    Based on detailed and systematic researches of the geology of ore deposits, fluid inclusions and isotope geochemistry etc., and regarding the Late Paleozoic fluid system of the Yuebei Basin as an integrated object in this paper,we have revealed the temporo-spatial evolution law of the basin's fluid system and discussed its ore-forming effects by simulating and analyzing the distribution of ore-forming elements, the fluid thermodynamics and dynamics of evolution processes of this basin. The results show that Late Paleozoic ore-forming fluid systems of the Yuebei Basin include four basic types as follows. (1) The sea floor volcanic-exhalation system developed during the rapid basin slip-extension stage in the Mid-Late Devonian, which affected the Dabaoshan region. It thus formed the Dabaoshan-type Cu-Pb-Zn-Fe sea floor volcanic-exhalation sedimentary deposits. (2) The compaction fluid system developed during the stable spreading and thermal subsidence-compression stage of the basin in the Mid-Late Devonian. The range of its effects extended all over the whole basin. It resulted in filling-metasomatic deposits, such as the Hongyan-type pyrite deposits and pyrite sheet within the Fankou-type Cu-Pb-Zn-S deposits. (3) The hot water circulation system of sea floor developed during the stage of basin uplifting and micro-aulacogen from the late Late Carboniferous to Middle Carboniferous. The range of its effects covered the Fankou region. It thus formed MVT deposits, such as the main orebody of the Fankou-type Pb-Zn-S deposits.(4) The gravity fluid system developed during the stage of fold uplifting and the basin closed from Middle Triassic to Jurassic, forming groundwater hydrothermal deposits, e.g. the veinlet Pb-Zn-calcite orebodies of the Fankou-type Pb-Zn-S deposits. Migration and concentration of the ore-forming fluids were constrained by the state of temporo-spatial distribution of its fluid potential. Growth faults not only converged the fluids and drove them to

  13. Siberia on Russian mental maps: The imperial and national space

    Directory of Open Access Journals (Sweden)

    Subotić Milan

    2012-01-01

    Full Text Available Starting from the theoretical problem of understanding the nation-building process within continental empires, this paper investigates the various meanings of ‘Siberia’ in the Russian imperial and national imagination. Analyzing discursive practices that create various representations of the geographical space, this study shows the changes in Russian perceptions of Siberia from the ‘alien’ space and the ‘colony’, to an unalienable part of the national territory (‘Russian land’ or ‘homeland’. Tracing the creation of ‘Russianness’ of Siberia, the author interprets this concept as a part of broader debates about ‘Russian identity’ and the relationship between ‘European’ and ‘Asiatic’ Russia. Therefore, the principal aim of the present study is to examine one of the most important aspects of the process Russia’s transformation from imperial to a ‘nationalizing State’.

  14. Obreras y empresarias en el Periodo Romano Alto Imperial

    Directory of Open Access Journals (Sweden)

    Pilar Fernández Uriel

    2011-01-01

    Full Text Available Análisis de la situación laboral y las diferentes medios y trabajos de las mujeres en el contexto de la Roma alto Imperial, frente a la situación mentalidad tradicional femenina a través de la documentación que proporcionan las fuentes históricas. Se contempla su relación con la sociedad, su ámbito doméstico e incluso la posible repercusión que pudiera existir en la cultura y mentalidad de este momento histórico.Analysis of the labor situation and the different ways and works of women in the context of high Imperial Rome, facing the situation traditionally minded women through the documentation provided by historical sources. It sees its relationship with society, its domestic and even the possible impact that might exist in the culture and mentality of this historical moment.

  15. Late Quaternary clay minerals off Middle Vietnam in the western South China Sea: Implications for source analysis and East Asian monsoon evolution

    Institute of Scientific and Technical Information of China (English)

    2007-01-01

    High-resolution clay mineral records combined with oxygen isotopic stratigraphy over the past 450 ka during late Quaternary from Core MD05-2901 off Middle Vietnam in the western South China Sea are reported to reconstruct a history of East Asian monsoon evolution.Variations in Illite,chlorite,and kaolinite contents indicate a strong glacial-interglacial cyclicity,while changes in smectite content present a higher frequency cyclicity.The provenance analysis indicates a mixture of individual clay minerals from various sources surrounding the South China Sea.Smectite derived mainly from the Sunda shelf and its major source area of the Indonesian islands.Illite and chlorite originated mainly from the Mekong and Red rivers.Kaolinite was provided mainly by the Pearl River.Spectral analysis of the kaolinite/(illite+chlorite) ratio displays a strong eccentricity period of 100 ka,implying the ice sheet-forced winter monsoon evolution; whereas higher frequency changes in the smectite content show an ice sheet-forced obliquity period of 41 ka,and precession periods of 23 and 19 ka and a semi-precession period of 13 ka as well,implying the tropical-forced summer monsoon evolution.The winter monsoon evolution is generally in coherence with the glacial-interglacial cyclicity,with intensified winter monsoon winds during glacials and weakened winter monsoon winds during interglacials; whereas the summer monsoon evolution provides an almost linear response to the summer insolation of low latitude in the Northern Hemisphere,with strengthened summer monsoon during higher insolation and weakened summer monsoon during lower insolation.The result suggests that the high-latitude ice sheet and low-latitude tropical factor could drive the late Quaternary evolution of East Asian winter and summer monsoons,respectively,implying their diplex and self-contained forcing mechanism.

  16. Imperial Senate: American Legislative Debates on Empire, 1898-1917

    Science.gov (United States)

    2013-09-01

    with the opposition to imperialism, and links the legislative agitation of 1898–1900 to subsequent resistance to the Treaty of Versailles .45 Welch...century attempts, starting with the rejection of the Treaty of Versailles in 1919. The related debates reflected not only a change in the role of this...culminating in his successful opposition to President Wilson over the Treaty of Versailles in 1919.111 While the diehard administration partisans were

  17. Population analysis relative to geothermal energy development, Imperial County, California

    Energy Technology Data Exchange (ETDEWEB)

    Pick, J.B.; Jung, T.H.; Butler, E.

    1977-01-01

    The historical and current population characteristics of Imperial County, California, are examined. These include vital rates, urbanization, town sizes, labor force composition, income, utility usage, and ethnic composition. Inferences are drawn on some of the important social and economic processes. Multivariate statistical analysis is used to study present relationships between variables. Population projections for the County were performed under historical, standard, and geothermal projection assumptions. The transferability of methods and results to other geothermal regions anticipating energy development is shown. (MHR)

  18. Aesthetics and Empire: The Sense of Feminine Beauty in the Making of the US Imperial Archipelago

    Directory of Open Access Journals (Sweden)

    Thompson, Lanny

    2013-12-01

    Full Text Available This article examines the “sense of beauty” in the United States imperial archipelago, composed of the island territories of Cuba, Hawai`i, Philippines, and Puerto Rico, all acquired in 1898. The theoretical connection among these two elements –aesthetics and empire– is provided by a revision of the concepts “economy of colonial desire” and “complex of visuality.” This paper analyzes the most advanced visual technology of the late nineteenth century: the mass- produced, printed photograph. In particular, it focuses upon the representations of feminine beauty as found the illustrated “new-possessions” books which described recent island acquisitions of the United States. The connections between aesthetics and the forms of governance in each territory will also be elucidated.Este artículo examina el “sentido de belleza” en el archipiélago imperial estadounidense, compuesto de los territorios isleños de Cuba, Hawai`i, Filipinas y Puerto Rico, todos adquiridos en 1898. La conexión teórica entre estos dos elementos –estética e imperio– se establece mediante una revisión de los conceptos de “economía de deseo colonial” y el “complejo de visualidad”. Este artículo analiza la tecnología visual más avanzada del siglo diecinueve tardío: la fotografía impresa. En particular, se enfoca en las representaciones de belleza femenina en los libros ilustrados de las “nuevas posesiones” los cuales describían las adquisiciones recientes de los Estados Unidos. También, se dilucidarán las conexiones entre estética y las formas de gobernanza en cada territorio.

  19. Late Quaternary climatic forcing on the terrigenous supply in the northern South China Sea: Input from magnetic studies

    Science.gov (United States)

    Chen, Quan; Kissel, Catherine; Liu, Zhifei

    2017-08-01

    The detrital component of marine sediment is a powerful recorder of paleoenvironmental changes in a marginal sea such as the South China Sea. This is in particular valid for the magnetic fraction that is one of the key parameters for paleoenvironmental studies in the South China Sea, although poorly used so far. We report here on the analysis of the magnetic properties of a 50 m-long sedimentary sequence retrieved from the northern South China Sea, on the continental slope off the Pearl River mouth. Magnetic minerals with different coercivities (magnetite, pyrrhotite, and hematite) are mixed. The variations in relative content of these magnetic minerals illustrate influences of various external forcing mechanisms at different timescales. The pyrrhotite content exhibits a long-term increase, which is also observed in illite + chlorite content, indicating a continuous enhancement of supply from Taiwan most likely related to active Taiwan orogeny. Glacial-interglacial fluctuations are characterized by more magnetite and pyrrhotite with coarser silt and magnetic grains during glacials than interglacials. This is attributed to sea-level changes with the enormous continental shelf exposed during glacials, in turn affecting the sediment transport distance and pathway. On a shorter timescale, larger hematite inputs in fine-grained sediments coincide with precession minima. We suggest that this periodic hematite supply change is related to the eolian dust deposited at the studied site in addition to the fluvial and oceanic transported materials.

  20. Parental status and late-life well-being in rural China: the benefits of having multiple children.

    Science.gov (United States)

    Guo, Man

    2014-01-01

    This study examined potential differences among childless elders, elders with one child, and elders with multiple children in rural China in their levels of depression and life satisfaction, and investigated the mechanism behind the potential differences. The sample consisted of 1224 older adults in rural Anhui province, China. ANOVA tests were carried out to compare the three groups in depression and life satisfaction, respectively. Multiple regressions were carried out to predict depression and life satisfaction, with (1) parental status, (2) individual attributes (i.e., sociodemographic variables and functional health), and (3) variables representing family relations (i.e., living arrangement, intergenerational contact, and family support) entered sequentially in each regression. Overall, childless elders in rural China had significantly higher level of depression and lower level of life satisfaction than did older parents. The primary reason for such group differences was lack of monetary support from adult children, the effect of which was conditioned upon the income level of older adults. With a high level of income, the benefit of monetary support from children was negligible. However, the mere presence of multiple children was associated with a higher life satisfaction, independent of personal attributes and potential monetary support from children. This study contributed to the 'missing link' in the explanation by identifying the pathways through which parental status affect individual well-being. The findings indicate that local contexts such as affluence, social norms, and available formal support all play a role in shaping the consequences of childlessness in later life.

  1. Selfies of Imperial Cormorants (Phalacrocorax atriceps): What Is Happening Underwater?

    Science.gov (United States)

    Gómez-Laich, Agustina; Yoda, Ken; Zavalaga, Carlos; Quintana, Flavio

    2015-01-01

    During the last few years, the development of animal-borne still cameras and video recorders has enabled researchers to observe what a wild animal sees in the field. In the present study, we deployed miniaturized video recorders to investigate the underwater foraging behavior of Imperial cormorants (Phalacrocorax atriceps). Video footage was obtained from 12 animals and 49 dives comprising a total of 8.1 h of foraging data. Video information revealed that Imperial cormorants are almost exclusively benthic feeders. While foraging along the seafloor, animals did not necessarily keep their body horizontal but inclined it downwards. The head of the instrumented animal was always visible in the videos and in the majority of the dives it was moved constantly forward and backward by extending and contracting the neck while travelling on the seafloor. Animals detected prey at very short distances, performed quick capture attempts and spent the majority of their time on the seafloor searching for prey. Cormorants foraged at three different sea bottom habitats and the way in which they searched for food differed between habitats. Dives were frequently performed under low luminosity levels suggesting that cormorants would locate prey with other sensory systems in addition to sight. Our video data support the idea that Imperial cormorants’ efficient hunting involves the use of specialized foraging techniques to compensate for their poor underwater vision. PMID:26367384

  2. Between universalism and regionalism: universal systematics from imperial Japan.

    Science.gov (United States)

    Lee, Jung

    2015-12-01

    Historiographic discussions of the universality and regionality of science have to date focused on European cases for making regional science universal. This paper presents a new perspective by moving beyond European origins and illuminating a non-European scientist's engagement with the universality and regionality of science. It will examine the case of the Japanese botanist Nakai Takenoshin (1882-1952), an internationally recognized authority on Korean flora based at Tokyo Imperial University. Serving on the International Committee on Botanical Nomenclature in 1926, Nakai endorsed and acted upon European claims of universal science, whilst simultaneously unsettling them with his regionally shaped systematics. Eventually he came to promote his own systematics, built regionally on Korean flora, as the new universal. By analysing his shifting claims in relation to those of other European and non-European botanists, this paper makes two arguments. First, universalism and regionalism were not contradictory foundations of scientific practice but useful tools used by this non-European botanist in maintaining his scientific authority as a representative Japanese systematist. Second, his claims to universality and regionalism were both imperially charged. An imperially monopolized study of Korean plants left a regional imprint on Nakai's systematics. In order to maintain his scientific authority beyond its region of origin he had to assert either the expanding regionalism of 'East Asia' or universalism.

  3. Palaeomagnetism of Precambrian dyke swarms in the North China Shield: The ˜1.8 Ga LIP event and crustal consolidation in late Palaeoproterozoic times

    Science.gov (United States)

    Piper, John D. A.; Jiasheng, Zhang; Huang, Baochung; Roberts, Andrew P.

    2011-06-01

    a ˜1.83-1.76 Ga APW swathe from the North China Shield permits a comparison with other shields and yields a constraint to continental configurations during the late Palaeoproterozoic. A quasi-integral reconstruction of Palaeopangaea is tested here and supported by conformity of predominantly of uplift-related palaeopoles from the ˜1.90-1.70 Ga tectono-thermal belts and from SW → NE trending APW implied by the distribution of poles from the ˜1.80 Ga igneous suites including the LIP events. This trend incorporates the A2 → A1 migration and the granulite terrane cooling polar swathe from North China. The reconstruction indicates that continental crust consolidated in Palaeoproterozoic times by accretion of ˜2.3-1.7 Ga orogenic belts around a hemispheric and crescent-shape core already established by Late Archaean times. The North China Shield is interpreted to have bordered the western cratonic margin of the Indian Shield in a proximity supported by correlation of geological features and suggested by a number of previous workers. The Central Orogenic Zone of the North China shield characterised by tectono-thermal activity prior to ˜1.85 Ga was then contiguous with a comparable zone running through the centre of the Indian Shield and continuing into the Capricorn Belt of Western Australia. The ˜1.78-1.76 Ga dykes in North China continue into dyke swarms in the South India Shield and may have been sourced in a plume-related LIP focussed near the continental margin in the Xiong'er Aulacogen.

  4. Terrestrial mollusk evidence for the origin and sedimentary environment of the Late Tertiary Red Clay Formation in the Loess Plateau, China

    Institute of Scientific and Technical Information of China (English)

    PEI Yunpeng; WU Naiqin; LI Fengjiang

    2004-01-01

    The origin and sedimentary environment of the Late Tertiary (Neogene) Red Clay Formation in northern China had long been controversial. A new mollusk record from the Xifeng red clay (red-earth) sequence in the central Loess Plateau provides the biological evidence for addressing questions of its origin and environmental implication. The study of composition and preservation condition of seventy mollusk fossil assemblages reveals the initial ecological condition of the red clay formation, avoiding the effect of post-deposited alteration. The result shows that all of identifiable mollusk species are composed of terrestrial taxa, most of them are the common species found in the overlying Quaternary loess-paleosol sequence. Most of fossil individuals preserved in the red clay strata are in living conditions based on the investigation of fieldwork, indicating the original population. Thus, the mollusk fossil assemblages can be used as an indicator of primary environment of the red clay formation. The mollusk record from the Xifeng red clay sequence supports the view that the red clay is an aeolian origin, similar to the overlying Quaternary loess deposits. Our data also reveal the history of environmental changes at Xifeng from 6.2-2.4 Ma, which is coupled in phase with the formation and development of the Arctic ice sheets and the process of the Tibetan Plateau uplift. Both may be the major cause and forcing mechanisms of the late Tertiary environmental changes in the Loess Plateau.

  5. Characteristics of Late Permian Deep-Water Sedimentary Environments: A Case Study of Shaiwa Section, Ziyun County, Guizhou Province, Southwestern China

    Institute of Scientific and Technical Information of China (English)

    Gao Yongqun; Yang Fengqing; Peng Yuanqiao

    2005-01-01

    Sediments of carbonate gravity flows and terrigenous debris turbidites, and normal bathyal deposits were found at the Shaiwa Section, Ziyun County, Guizhou Province, southwestern China. Through grain-size analysis of some typical sediments at this section, the changing patterns of the grain parameters and the grain-size cumulations were recovered. Results show that the study area was deposited under turbidite control during the Late Permian period, which we also recognized at the outcrop section upon sedimentary characteristics of the sediments. In addition, fossils are abundant in the Upper Permian of the Shaiwa Section, including radiolarians, sponge-spicules, bivalves, brachiopods, ammonoids and trace fossils. Radiolarians and siliceous sponge-spicules are typical deep water assemblages. Bivalves are dominated by genera of Hunanopecten and Claraia, both showing deep water living characteristics. Ammonoids are composed of planktonic types, showing characteristics of smooth and flat shells. Brachiopods are dominated by a small and thin shelled assemblage, which are commonly flat in shape and usually of slight ornamentations on shells. In addition, trace fossils found at the Shaiwa Section are also common types of deep water facies. Thus, the fossil evidence of the Shaiwa Section also suggests a deep water environment, possibly from the bathyal slope to the basin margin facies, of the studied area during the Late Permian period.

  6. Paleoclimate change recorded in the red earth and brown-yellow sediment of Late Quaternary for northeastern part of Guangdong Province, south to the Nanling Mountains, China

    Institute of Scientific and Technical Information of China (English)

    LI BaoSheng; NIU DongFeng; YANG Yi; WEN XiaoHao; DAVID DianZhang; QIU ShiFan; DONG YüXiang; LI ZhiWen; DU ShuHuan; QIU XianJiao; LI HouXin

    2008-01-01

    The paleoenvironment indicated by the geochronology, major oxides-SiO2, AI203 and TOFE (Fe203 +FeO), and CIA (Chemical Index of Alteration) value of the red earth and brown-yellow silt primarily characterized by the Linjiang stratigraphic section, based on the geological investigation of Late Quaternary along the river banks of northeastern part of China's Guangdong Province, south to the Nanling Mountains, allow us to hypothesize that the red earth on the first terrace in northeastern part of Guangdong belongs to reticulated red clay developed in a hot-wet environment of the last interglacial period (132-73 ka BP), similar to the monsoon environment in the northern margin of modern tropical zone, while the overlying brown-yellow silt layer mainly accumulated in a monsoon environment of warm temperate zone in the last glacial period (73-11 ka BP), with the aeolian sand LJ3 representing an extreme period of worsening climate. Such a hypothesis corresponds well with predecessors' research on the paleoenvironment indicated by abundant fossils in both south and east to the Nanling Mountains. Hence, it follows that the bioclimatic zone did experience a large and rapid vicissitude in northeastern part of China's Guangdong Province, and even in the full extent of the region south to the Nanling Mountains from the last interglacial period to the last glacial period, with the red earth being replaced by the brown-yellow silty sediment, and even maybe with the Ailuropoda-Stegodon Fauna being replaced by the Penghu Fauna. This study may provide an important geological demonstration for the environmental response to global change in China's low latitudes on a 10 ka scale.

  7. The review of Northwestern China charities in late Qing Dynasty%晚清时期西北地区慈善事业述评

    Institute of Scientific and Technical Information of China (English)

    许德雅

    2012-01-01

    It is a very important period for the development of Northwestern China charities in the late Qing Dynasty. The routine charities and famine relief were the continuance and development of the traditional charities, and they were still the mainstream of the charities development in this period. The incoming of church charity injected fresh blood into the traditional charities, and it promoted the charity's modernization transformation by objective. Though the development of Northwestern China charities lagged behind the Beijing-Tianjin region and the southeast region of China, it still worked on maintaining social stability as a safety net.%晚清时期是西北地区慈善事业发展的重要时期,常态慈善和灾荒救济作为传统慈善的延续和发展,仍然是这一时期慈善事业发展的主流。教会慈善的传入为该地区传统慈善事业发展注入了一股"新鲜血液",客观上推动了这一时期慈善事业的近代化转型。尽管西北地区慈善事业的发展明显滞后于同时期京津地区和江南地区,但它在缓解社会矛盾、稳定社会秩序方面,仍然起到"安全网"的作用。

  8. Late Miocene Woods of Taxodiaceae from Yunnan, China%云南中新世杉科化石木研究

    Institute of Scientific and Technical Information of China (English)

    扆铁梅; 李承森; 徐景先

    2003-01-01

    利用光学显微镜和扫描电镜首次对云南省楚雄州晚中新世石灰坝组石鼓村层的钙化木材进行了解剖学研究.鉴定出两种类型的木材:柳杉型落羽杉型木(Taxodioxylon cryptomeripsoides Schonfeld)和杉木型落羽杉型木(Taxodioxylon cunninghamioides Watari).二者分别与现代柳杉属和杉木属具有最接近的亲缘关系.根据这两种杉科化石木现存最近亲缘种的生态环境,并综合其他资料,推测该地区在晚中新世为温暖湿润的亚热带气候环境.%Late Miocene woods were investigated from the Lühe Basin in Chuxiong Borough, central Yunnan, China. The calcified woods preserved in the Shigucun member of the Shihuiba Formation, are represented by fallen logs and stumps. Two species of fossil wood, Taxodioxylon cryptomeripsoides Schonfeld 1953 and T. cunninghamioides Watari 1948, are described. Their anatomical structure shows striking similarities to the woods of Cryptomeria and Cunninghamia respectively. That the two fossil woods are classed in the Taxodiaceae suggest a subtropical, humid, and warm environment in Lühe during Late Miocene. They compare favorably to other fossil specimens and species reported from localities ranging from Cretaceous to Pliocene. This is the first record of the presence of the species T. cryptomeripsoides and T. cunninghamioides in Late Miocene of Yunnan.

  9. Informal Imperialism and the 1879 Hesperia Incident : Containing Cholera and Challenging Extraterritoriality in Japan

    OpenAIRE

    FUESS, Harald

    2014-01-01

    Informal empire is a classical term of diplomatic history to designate the British role in East Asia after the Opium Wars. This paper looks at informal imperialism more broadly to question the interaction of foreign powers and their citizens with and within Japan. It argues for a contested complexity of the extraterritorial arrangements such that Japanese independence was not only advocated against foreign imperialism but partly with the support of imperial powers and their nationals, accordi...

  10. Science Applied for the Investigation of Imperial Gate from Eighteenth Century Wooden Church of Nicula Monastery

    OpenAIRE

    I. Bratu; Monk Siluan; C. Măruţoiu; Kacso, I.; S. Garabagiu; V. C. Măruţoiu; C. Tănăselia; Popescu, D.; D. L. Postolache; Pop, D

    2017-01-01

    Part of an indestructible component of any orthodox church, the Imperial Gates represent an important symbol in our cultural heritage. But in many cases the Imperial Gates from the wooden churches were damaged. In order to preserve and restore them, the scientific investigations of the Imperial Gate belonging to Nicula Monastery wooden church were performed by employing nondestructive and destructive methods. The wood essence was established, with its “health” status being investigated by FTI...

  11. Geochronological and sedimentological evidences of Panyangshan foreland basin for tectonic control on the Late Paleozoic plate marginal orogenic belt along the northern margin of the North China Craton

    Science.gov (United States)

    Li, Jialiang; Zhou, Zhiguang; He, Yingfu; Wang, Guosheng; Wu, Chen; Liu, Changfeng; Yao, Guang; Xu, Wentao; Zhao, Xiaoqi; Dai, Pengfei

    2017-08-01

    There is a wide support that the Inner Mongolia Palaeo-uplift on the northern margin of the North China Craton has undergone an uplifting history. However, when and how did the uplift occurred keeps controversial. Extensive field-based structural, metamorphic, geochemical, geochronological and geophysical investigations on the Inner Mongolia Palaeo-uplift, which suggested that the Inner Mongolia Palaeo-uplift was an uplifted region since the Early Precambrian or range from Late Carboniferous-Early Jurassic. The geochemical characteristics of the Late Paleozoic to Early Mesozoic intrusive rocks indicated that the Inner Mongolia Palaeo-uplift was an Andean-type continental margin that is the extensional tectonic setting. To address the spatial and temporal development of the Inner Mongolia Palaeo-uplift, we have carried out provenance analysis of Permian sedimentary rocks which collected from the Panyangshan basin along the northern margin of the North China Craton. The QFL diagram revealed a dissected arc-recycled orogenic tectonic setting. Moreover, the framework grains are abundant with feldspar (36-50%), indicating the short transport distance and unstable tectonic setting. Detrital zircon U-Pb analysis ascertained possible provenance information: the Precambrian basement ( 2490 and 1840 Ma) and continental arc magmatic action ( 279 and 295 Ma) along the northern margin of the North China Craton. The projection in rose diagrams of the mean palaeocurrent direction, revealing the SSW and SSE palaeoflow direction, also shows the provenance of the Panyangshan basin sources mainly from the Inner Mongolia Palaeo-uplift. The andesite overlying the Naobaogou Formation has yielded U-Pb age of 277.3 ± 1.4 Ma. The additional dioritic porphyry dike intruded the Naobaogou and Laowopu Formations, which has an emplacement age of 236 ± 1 Ma. The above data identify that the basin formed ranges from Early Permian to Middle Triassic (277-236 Ma). Accordingly, the Inner Mongolia

  12. Early to late Yanshanian I-type granites in Fujian Province, SE China: Implications for the tectonic setting and Mo mineralization

    Science.gov (United States)

    Yang, Yu-Long; Ni, Pei; Yan, Jun; Wu, Chang-Zhi; Dai, Bao-Zhang; Xu, Ying-Feng

    2017-04-01

    The Cathaysia Block is the southeastern part of the South China Block in Southeast (SE) China, and it hosts voluminous late Mesozoic I-, S-, and A-type granitoids, as well as minor highly fractionated granites. We present here zircon U-Pb age data and Nd-Hf isotopic data for the Dayang and Juzhou granites, together with new petrological and geochemical analyses. The Dayang pluton consists of fine-grained two-mica monzonitic granites in which the plagioclases exhibit zoning and poikilitic textures. In contrast, the Juzhou pluton consists of medium- to coarse-grained biotite K-feldspar granites that lack zoning and poikilitic textures. The emplacement ages are 143 ± 2.3 Ma for the Dayang pluton and 133 ± 2.1 Ma for the Juzhou pluton according to zircon U-Pb isotope analyses. The Dayang and Juzhou granites are both metaluminous and belong to the shoshonitic series. The Dayang granite exhibits very flat REE patterns, showing the tetrad effect, and the spidergrams show striking negative Ba, Sr, Nb, and Ti anomalies and a positive Ta anomaly. In contrast, the Juzhou granite has sloping REE patterns, but like the Dayang granite it also has striking negative Ba, Sr, Nb, Ta, and Ti anomalies. Petrographic and geochemical evidence indicates that the Dayang granite is a highly fractionated I-type granite and that the Juzhou granite is a typical I-type granite. The tetrad effect in the Dayang granite can be interpreted in terms of melt-rock interactions at a late stage of magma evolution, whereas the main mechanism during the evolution of the Juzhou magma was fractionation of plagioclase, biotite, hornblende, apatite, zircon, and allanite. Nd-Hf isotope data suggest that the Dayang and Juzhou granites were both formed partial melting of Paleoproterozoic basement rock and juvenile material (underplating basalts or Mayuan Group amphibolites), with the Juzhou granite having a greater contribution from juvenile material than the Dayang granite. Our new data, together with

  13. Clay mineralogical and geochemical proxies of the East Asian summer monsoon evolution in the South China Sea during Late Quaternary

    Science.gov (United States)

    Chen, Quan; Liu, Zhifei; Kissel, Catherine

    2017-01-01

    The East Asian summer monsoon controls the climatic regime of an extended region through temperature and precipitation changes. As the East Asian summer monsoon is primarily driven by the northern hemisphere summer insolation, such meteorological variables are expected to significantly change on the orbital timescale, influencing the composition of terrestrial sediments in terms of both mineralogy and geochemistry. Here we present clay mineralogy and major element composition of Core MD12-3432 retrieved from the northern South China Sea, and we investigate their relationship with the East Asian summer monsoon evolution over the last 400 ka. The variability of smectite/(illite + chlorite) ratio presents a predominant precession periodicity, synchronous with the northern hemisphere summer insolation changes and therefore with that of the East Asian summer monsoon. Variations in K2O/Al2O3 are characterized by eccentricity cycles, increasing during interglacials when the East Asian summer monsoon is enhanced. Based on the knowledge of sediment provenances, we suggest that these two proxies in the South China Sea are linked to the East Asian summer monsoon evolution with different mechanisms, which are (1) contemporaneous chemical weathering intensity in Luzon for smectite/(illite + chlorite) ratio and (2) river denudation intensity for K2O/Al2O3 ratio of bulk sediment. PMID:28176842

  14. Clay mineralogical and geochemical proxies of the East Asian summer monsoon evolution in the South China Sea during Late Quaternary.

    Science.gov (United States)

    Chen, Quan; Liu, Zhifei; Kissel, Catherine

    2017-02-08

    The East Asian summer monsoon controls the climatic regime of an extended region through temperature and precipitation changes. As the East Asian summer monsoon is primarily driven by the northern hemisphere summer insolation, such meteorological variables are expected to significantly change on the orbital timescale, influencing the composition of terrestrial sediments in terms of both mineralogy and geochemistry. Here we present clay mineralogy and major element composition of Core MD12-3432 retrieved from the northern South China Sea, and we investigate their relationship with the East Asian summer monsoon evolution over the last 400 ka. The variability of smectite/(illite + chlorite) ratio presents a predominant precession periodicity, synchronous with the northern hemisphere summer insolation changes and therefore with that of the East Asian summer monsoon. Variations in K2O/Al2O3 are characterized by eccentricity cycles, increasing during interglacials when the East Asian summer monsoon is enhanced. Based on the knowledge of sediment provenances, we suggest that these two proxies in the South China Sea are linked to the East Asian summer monsoon evolution with different mechanisms, which are (1) contemporaneous chemical weathering intensity in Luzon for smectite/(illite + chlorite) ratio and (2) river denudation intensity for K2O/Al2O3 ratio of bulk sediment.

  15. Red pigments and Boraginaceae leaves in mortuary ritual of late Neolithic China: A case study of Shengedaliang site.

    Science.gov (United States)

    Wu, Yan; Guo, XiaoNing; Wang, WeiLin; Chen, XiangLong; Zhao, Zhijun; Xia, Xiumin; Yang, YiMin

    2017-02-01

    Investigation of mortuary ritual is an important method to reconstruct many aspects of past societies. Due to the lack of relevant analytical work, little evidence related to organic materials in a burial can be found in China. Here we report materials collected from a burial during the excavation of the Shengedaliang site. The recovered materials were analyzed using Raman spectroscopy and plant analysis: flotation, pollen and phytolith analysis. The red pigments found scattered over the human remains were identified as cinnabar. Extracted phytoliths associated with the burial are mainly leaves from the Boraginaceae family. This is the first time that a covering of leaves have been identified with a burial in Neolithic China. The presence of "special" leaves fossil may indicate a type of "plant worship" and the identification of an important plant used in traditional Chinese medicine. The finding of the two materials allows us to better identify indicators of funerary ritual and its relationship to social inequality. © 2016 Wiley Periodicals, Inc.

  16. Late Mesozoic Thermotectonic Evolution of the Jueluotage Range,Eastern Xinjiang, Northwest China: Evidence from Apatite Fission Track Data

    Institute of Scientific and Technical Information of China (English)

    ZHU Wenbin; WAN Jinglin; SHU Liangshu; ZHANG Zhiyong; SU Jinbao; SUN Yan; GUO Jichun; ZHANG Xueyun

    2008-01-01

    Although many authors have emphasized the Cenozoic history of deformation, exhumation and cooling in the Tiaushan area related to the India-Asia collision, very little is known about the Mesozoic history of compression and uplift within the Tianshan. In order to obtain information about the Mesozoic exhumation history and processes of cooling in eastern Tianshan, fission track methods on apatite were used. Sampling was made in the Jueluotage Range. Three samples (Z001-Z003) were taken from granite in borehole ZK6301 of Yandong pluton; the ages range from 97.0 to 87.6 Ma that are much younger than the pluton age which was dated by U-Pb zircon at 334±2 Ma. Two samples in northern piedmont of the Jueluotage Range were collected from Jurassic strata in Dikaner (DK001) and Dananhu (D001) whose ages are 91.5 and 93.4 Ma respectively. The average apparent exhumation rate is 0.039 mm/a calculated by extrapolation on the basis of Yandong samples, indicating an extremely slow exhumation in the Jueluotage Range since the Late Cretaceous. Two Jurassic samples reached the maximum depths after deposition and experienced the maximum temperatures of ca. 105 and 108℃ until the late Early Cretaceous before a period of cooling and exhumation occurred at 114 and 106 Ma.

  17. Evolution of strontium isotopic composition of sea-water from Late Permian to Early Triassic based on study of marine carbonates,Zhongliang Mountain,Chongqing,China

    Institute of Scientific and Technical Information of China (English)

    2008-01-01

    Collected from a Late Permian to Early Triassic sedimentary section in the Zhongliang Mountain of Chongqing, Southwest China, sixty marine carbonate samples were measured for the 87Sr/86Sr ratios, and corresponding evolution curve was constructed. The concentrations of SiO2, CaO, MgO, Mn and Sr are used to evaluate reservation of strontium isotopic composition for original seawater and the credi-bility of the dissolution method for sample preparation. The results show that most of the samples (except seven samples with the Mn/Sr ratios higher than 2) contain the original geochemistry signa-tures of ancient seawater. Compared to the published 87Sr/86Sr ratios from the Late Permian to Early Triassic, our database reported here is the largest and the curve constructed is the most complete. The strontium isotopic curve from Late Permian to Early Triassic is consistent globally and exhibits a gen-eral trend of steady increase during this period. The minimum of 87Sr/86Sr ratios (0.707011) occurs in the Late Permian (30 m in thickness below the Permian-Triassic boundary), and the maximum (0.708281), near the Early-Middle Triassic boundary. The lack of land plants and the rapid continental weathering result in the increase of 87Sr/86Sr ratios during the interval. The Permian-Triassic boundary in Zhongli-ang Mountain Section has been accepted internationally. The 87Sr/86Sr ratios of six samples near the boundary vary from 0.70714 to 0.70715 with an average of 0.70714, which is consistent with the value of 0.70715 (samples are from articulate brachiopod shells) from Korte et al. published in 2006 (within the error range in experiment). Accordingly, the strontium isotope composition in the Permian-Triassic boundary in this paper is of global significance. It can be confirmed that the 87Sr/86Sr ratios of the sea-water in the Permian-Triassic transition are in the range of 0.70714―0.70715.

  18. A new Euprox from the Late Miocene of Yuanmou, Yunnan Province, China, with interpretation of its paleoenvironment

    Institute of Scientific and Technical Information of China (English)

    2003-01-01

    The Yuanmou Basin of Yunnan Province is a hotspot for the research of early hominid evolution and its environmental background. During the implementation of the Program "Research of the Origin and Evolution of Early Man and Its Environmental Background" from 1998 to 2001, a huge quantity of hominoid and mammal fossils were collected. The present report systematically describes an Euprox robustus sp. nov. identified during the recent laboratory work on the collected material. Euprox is a group of earliest cervids with true antlers. The new species is the third one of the genus discovered in China. Judged by its morphologic characteristics, the new species feed on juicy and tender leaves of dicotyledon. It implies that the vegetation of its epoch in the Yuanmou Basin is a kind of southern subtropical evergreen forest and the climate is humid and temperate with evident seasonality. The latter is mostly influenced by the monsoon and secondly by the latitude.

  19. A New Genus of Fossil Cycads Yixianophyllum gen. nov. from the Late Jurassic Yixian Formation, Western Liaoning, China

    Institute of Scientific and Technical Information of China (English)

    2005-01-01

    A new genus of fossil Cycads, Yixianophyllum gen. nov., is reported here. The specimens were collected from the southern hill of Jinjiagou village, Toudaohezi Town, Yixian County, western Liaoning Province, China. The fossil plant-bearing bed belongs to the lower part, the Zhuanchengzi bed, of the Upper Jurassic Yixian Formation (Yixianian). The new genus in leaf shape, venation and epidermal structure shows a transitional form between Mesozoic Cycads (Ctenis, Nilssonia) and modern Cycads (Stangeria and Encephalartos). Since the features of these specimens differ from any known genera of Cycads, a new genetic name Yixianophyllum is proposed for these leaves. Typical species, Yixianophyllum jinjiagouense gen. et sp. nov. is described here. A supposed evolutionary tendency of Cycadean leaf-forms with Taeniopteris-type is discussed.

  20. Geochemistry of Metamafic Dykes from the Quanji Massif:Petrogenesis and Further Evidence for Oceanic Subduction, Late Paleoproterozoic, NW China

    Institute of Scientific and Technical Information of China (English)

    Hassan Abdelslam Mustafa; Qinyan Wang; Nengsong Chen; Fanxi Liao; Min Sun; Meshaal Abdelgadir Salih

    2016-01-01

    A suite of ~1.84–1.92 Ga metamafic dykes within the paragneiss suite (khondalite) of the Quanji massif in NW China, has been chosen in this study for further understanding the tectonic evo-lution and possible links to the global Columbia supercontinent. Occurrence and field relations sug-gest that they were formed coevally with a previous studied ~1.83–1.85 Ga metamafic dyke swarms. Whole-rock major and trace elemental geochemistry suggests precursor magma of the amphibolites being generated from a volcanic arc-related tectonic setting rather than a back-arc environment where the metamafic dyke swarms were emplaced. The metamafic dykes show enrichment of LREE and strongly negative anomalies for Ta-Nb, Zr-Hf and Ti, have high SiO2 (49.3 wt.%–52.5 wt.%) but low MgO (6.40 wt.%–7.76 wt.%) contents and Mg# (Mg#=[100×(MgO/40.3)]/[MgO/40.3+FeO/71.8]) values (45.7–52.1), suggesting evolved precursor magma. The high values of La/Ta (22.2–42.8) and La/Nb (1.71–2.47), mildly negativeεNd(t) values (-2.51–0.15), with depleted mantle model ages (TDM) of 2.45–2.84 Ga, suggest that their precursor magmas were possibly derived from a subduction-related fluid metasomatized Archean sub-continental lithospheric mantle. This study provides further evi-dence for oceanic plate subduction prevailing before or around ~1.85 Ga, which confirms a prolonged subduction-accretion-collision history in the NW China which is possibly linked to the assembly of the Columbia supercontinent.

  1. Climate changes in East China since the Late-glacial inferred from high-resolution mountain peat humification records

    Institute of Scientific and Technical Information of China (English)

    MA ChunMei; ZHU Cheng; ZHENG ChaoGui; YIN Qian; ZHAO ZhiPing

    2009-01-01

    High-resolution peat humification records were obtained from Dajiuhu of the Shennongjia Mountains and Qianmutian of the Tianmu Mountains to study climate changes in East China. The analyses of pollen, organic matters, TOC, and Rb/Sr indicate a high degree of peat humification and thus strong decomposition of organic matter when climate was dry. Conversely, when climate was humid, the de gree of humification is low because peat was preserved in a waterlogged condition. Peat humification from Dajiuhu occurred not only during the Younger Dryas (about 11.4-12.6 cal ka BP), the Bol ling-Allerφd Warm Period (12.6-15.2 cal ka BP), and the Oldest Dryas (about 15.2-16.0 cal ka BP), but also during the early Holocene (about 11.4-9.4 cal ka BP), the 8.2 cal ka BP cold event, and the Holo cene Optimum (about 7.0-4.2 cal ka BP). Both peat humification records since nearly 5 ka BP are consistent, showing that mountain peaUand has synchronous responses to the East Asia mon soon-induced precipitation. The LOI data confirm the above observation. The monsoon precipitation since nearly 5 ka BP recorded in these two peat profiles can be divided into three phases. During 4.9 3.5 ka BP, precipitation amount was high but fluctuated greatly. During 3.5-0.9 ka BP, precipitation amount was low. During 0.9-0 ka BP, degree of humification reduced gradually, indicating the increase of monsoon precipitation. Contrast to other high-resolution records from East China monsoon region shows that the monsoon precipitation records of the two peat profiles since nearly 16 ka BP are con trolled by a common forcing mechanism of summer solar radicalization in the Northern Hemisphere.

  2. Late Carboniferous N-MORB-type basalts in central Inner Mongolia, China: Products of hydrous melting in an intraplate setting?

    Science.gov (United States)

    Pang, Chong-Jin; Wang, Xuan-Ce; Xu, Bei; Zhao, Jian-Xin; Feng, Yue-Xing; Wang, Yan-Yang; Luo, Zhi-Wen; Liao, Wen

    2016-09-01

    Petrogenesis of the ca. 310 Ma Benbatu basalts in central Inner Mongolia is crucial for constraining the evolution of the Xing'an Mongolia Orogenic Belt (XMOB), eastern segment of the Central Asian Orogenic Belt. The Benbatu basalts have low initial 87Sr/86Sr ratios (0.7042-0.7048), positive εNd(t) (+ 8.99 to + 9.24) and εHf(t) values (+ 15.38 to + 15.65), and are characterized by relatively flat rare earth element patterns and enrichment of Rb, U, Pb, Zr and Hf, but depletion of Nb, Ta, Sr and Ti, resembling those of the normal Mid-Ocean-Ridge Basalt (N-MORB). Variations of trace element ratios (e.g., Sm/Yb and La/Sm) suggest that the basalts were derived from spinel peridotites, with a melting depth of recycling water in the generation of the Late Carboniferous magmatism in this region.

  3. [The influenza pandemic of 1782, with special reference to its occurrence in the Imperial City of Nuremberg].

    Science.gov (United States)

    Vasold, Manfred

    2011-01-01

    In Germany, very little research has been done on the flu pandemic of 1782. The year before, in 1781, an epidemic of dysentery had ravaged Central Europe quite seriously. The flu pandemic began in Germany in spring 1782. It took its origin in the Far East, probably in Imperial China. From there it slowly traveled westward and finally hit Russia and Germany. In early 1782, it arrived in eastern Prussia. Mortality rose, in Königsberg (Kaliningrad) mainly people over 30 died. From the German coast on the Baltic Sea the virus soon crossed over to England and Scotland. Within Germany it slowly moved southward, to places like Berlin, Weimar and further south. In Berlin very many people became sick. In spring 1782, in many parts of Germany, from east to west, people were bed-ridden. In Nuremberg, a young doctor described the symptoms of the disease and the therapy he gave to his patients in a pamphlet but apart from that there are few sources. Probably not many people consulted a doctor. Mortality in Nuremberg, it seems, did not rise very much. The city had been in decline since the 1750s, its population now shrunk even further. When this scourge hit Central Europe, the Holy Roman Empire was in decline, after an attack of famine and pestilence in the early 1770s and that epidemic of dysentery in 1781. It finally collapsed some 25 years later, in 1806, and the Imperial City of Nuremberg was absorbed by the Kingdom of Bavaria.

  4. Gold deposits of the northern margin of the North China craton: Multiple late Paleozoic-Mesozoic mineralizing events

    Science.gov (United States)

    Hart, C.J.R.; Goldfarb, R.J.; Qiu, Y.; Snee, L.; Miller, L.D.; Miller, M.L.

    2002-01-01

    The northern margin of the North China craton is well-endowed with lode gold deposits hosting a resource of approximately 900 tonnes (t) of gold. The ???1,500-km-long region is characterized by east-trending blocks of metamorphosed Archean and Proterozoic strata that were episodically uplifted during Variscan, Indosinian, and Yanshanian deformational and magmatic events. At least 12 gold deposits from the Daqinshan, Yan-Liao (includes the Zhangjiakou, Yanshan, and Chifeng gold districts), and Changbaishan gold provinces contain resources of 20-100 t Au each. Most deposits are hosted in uplifted blocks of Precambrian metamorphic rocks, although felsic Paleozoic and Mesozoic plutons are typically proximal and host ???30% of the deposits. The lodes are characterized by sulfide-poor quartz veins in brittle structures with low base metal values and high Au:Ag ratios. Although phyllic alteration is most common, intensive alkali feldspar metasomatism characterizes the Wulashan, Dongping, and Zhongshangou deposits, but is apparently coeval with Variscan alkalic magmatism only at Wulashan. Stepwise 40Ar-39Ar geochronology on 16 samples from gangue and alteration phases, combined with unpublished SHRIMP U-Pb dates on associated granitoids, suggest that gold mineralizing events occured during Variscan, Indosinian, and Yanshanian orogenies at circa 350, 250, 200, 180, 150, and 129 Ma. However, widespread Permo-Triassic (???250 Ma) and Early Jurassic (???180 Ma) thermal events caused variable resetting of most of the white mica and K-feldspar argon spectra, as well as previously reported K-Ar determinations. Compiled and new stable isotope and fluid inclusion data show that most ??18O values for ore-stage veins range from 8 to 14???, indicating a fluid in equilibrium with the Precambrian metamorphic basement rocks; ??D values from fluid inclysions range widely from -64 to -154???, which is indicative of a local meteoric component in some veins; and highly variable ??34S data

  5. Joint effect of education and main lifetime occupation on late life health: a cross-sectional study of older adults in Xiamen, China.

    Science.gov (United States)

    Yuan, Manqiong; Chen, Wei; Chu, Cheng-I; Fang, Ya

    2015-01-01

    The effects of education and occupation on health have been well documented individually, but little is known about their joint effect, especially their cumulative joint effect on late life health. We enrolled 14,292 participants aged 60+ years by multistage sampling across 173 communities in Xiamen, China, in 2013. Heath status was assessed by the ability to perform six basic activities of daily life. Education was classified in four categories: 'Illiterate', 'Primary', 'Junior high school' and 'Senior high school and beyond'. Main lifetime occupation was also four categorized: 'Employed', 'Farmer', 'Jobless' and 'Others'. Odds ratios (ORs) were estimated by random-intercept multilevel models regressing health status on education and main lifetime occupation with or without their interactions, adjusting by some covariates. Totally, 13,880 participants had complete data, of whom 12.5% suffered from disability, and 'Illiterate' and 'Farmer' took up the greatest proportion (33.01% and 42.72%, respectively). Participants who were higher educated had better health status (ORs = 0.62, 0.46, and 0.44 for the 'Primary', 'Junior high school', and 'Senior high school and beyond', respectively, in comparison with 'Illiterate'). Those who were long term jobless in early life had poorest heath (ORs = 1.88, 95% CI 1.47 to 2.40). Unexpectedly, for the farmers, the risk of poor health gradually increased in relation to higher education level (ORs = 1.26, 1.28, 1.40 and 2.24, respectively). For the 'Employed', similar ORs were obtained for the 'Junior high school' and 'Senior high school and beyond' educated (both ORs = 1.01). For the 'Farmer' and 'Jobless', participants who were 'Illiterate' and 'Primary' educated also showed similar ORs. Both education and main lifetime occupation were associated with late life health. Higher education was observed to be associated with better health, but such educational advantage was mediated by main lifetime occupation.

  6. Joint effect of education and main lifetime occupation on late life health: a cross-sectional study of older adults in Xiamen, China.

    Directory of Open Access Journals (Sweden)

    Manqiong Yuan

    Full Text Available The effects of education and occupation on health have been well documented individually, but little is known about their joint effect, especially their cumulative joint effect on late life health.We enrolled 14,292 participants aged 60+ years by multistage sampling across 173 communities in Xiamen, China, in 2013. Heath status was assessed by the ability to perform six basic activities of daily life. Education was classified in four categories: 'Illiterate', 'Primary', 'Junior high school' and 'Senior high school and beyond'. Main lifetime occupation was also four categorized: 'Employed', 'Farmer', 'Jobless' and 'Others'. Odds ratios (ORs were estimated by random-intercept multilevel models regressing health status on education and main lifetime occupation with or without their interactions, adjusting by some covariates.Totally, 13,880 participants had complete data, of whom 12.5% suffered from disability, and 'Illiterate' and 'Farmer' took up the greatest proportion (33.01% and 42.72%, respectively. Participants who were higher educated had better health status (ORs = 0.62, 0.46, and 0.44 for the 'Primary', 'Junior high school', and 'Senior high school and beyond', respectively, in comparison with 'Illiterate'. Those who were long term jobless in early life had poorest heath (ORs = 1.88, 95% CI 1.47 to 2.40. Unexpectedly, for the farmers, the risk of poor health gradually increased in relation to higher education level (ORs = 1.26, 1.28, 1.40 and 2.24, respectively. For the 'Employed', similar ORs were obtained for the 'Junior high school' and 'Senior high school and beyond' educated (both ORs = 1.01. For the 'Farmer' and 'Jobless', participants who were 'Illiterate' and 'Primary' educated also showed similar ORs.Both education and main lifetime occupation were associated with late life health. Higher education was observed to be associated with better health, but such educational advantage was mediated by main lifetime occupation.

  7. Leaf evolution in early-diverging ferns: insights from a new fern-like plant from the Late Devonian of China.

    Science.gov (United States)

    Wang, De-Ming; Xu, Hong-He; Xue, Jin-Zhuang; Wang, Qi; Liu, Le

    2015-06-01

    With the exception of angiosperms, the main euphyllophyte lineages (i.e. ferns sensu lato, progymnosperms and gymnosperms) had evolved laminate leaves by the Late Devonian. The evolution of laminate leaves, however, remains unclear for early-diverging ferns, largely represented by fern-like plants. This study presents a novel fern-like taxon with pinnules, which provides new insights into the early evolution of laminate leaves in early-diverging ferns. Macrofossil specimens were collected from the Upper Devonian (Famennian) Wutong Formation of Anhui and Jiangsu Provinces, South China. A standard degagement technique was employed to uncover compressed plant portions within the rock matrix. A new fern-like taxon, SHOUGANGIA BELLA GEN ET SP NOV: , is described and represents an early-diverging fern with highly derived features. It has a partially creeping stem with adventitious roots only on one side, upright primary and secondary branches arranged in helices, tertiary branches borne alternately or (sub)oppositely, laminate and usually lobed leaves with divergent veins, and complex fertile organs terminating tertiary branches and possessing multiple divisions and numerous terminal sporangia. Shougangia bella provides unequivocal fossil evidence for laminate leaves in early-diverging ferns. It suggests that fern-like plants, along with other euphyllophyte lineages, had independently evolved megaphylls by the Late Devonian, possibly in response to a significant decline in atmospheric CO2 concentration. Among fern-like plants, planate ultimate appendages are homologous with laminate pinnules, and in the evolution of megaphylls, fertile organs tend to become complex. © The Author 2015. Published by Oxford University Press on behalf of the Annals of Botany Company. All rights reserved. For Permissions, please email: journals.permissions@oup.com.

  8. Intelligent predictive model of ventilating capacity of imperial smelt furnace

    Institute of Scientific and Technical Information of China (English)

    唐朝晖; 胡燕瑜; 桂卫华; 吴敏

    2003-01-01

    In order to know the ventilating capacity of imperial smelt furnace (ISF), and increase the output of plumbum, an intelligent modeling method based on gray theory and artificial neural networks(ANN) is proposed, in which the weight values in the integrated model can be adjusted automatically. An intelligent predictive model of the ventilating capacity of the ISF is established and analyzed by the method. The simulation results and industrial applications demonstrate that the predictive model is close to the real plant, the relative predictive error is 0.72%, which is 50% less than the single model, leading to a notable increase of the output of plumbum.

  9. Impacts of land use and land cover changes on biogenic emissions of volatile organic compounds in China from the late 1980s to the mid-2000s: implications for tropospheric ozone and secondary organic aerosol

    Directory of Open Access Journals (Sweden)

    Yu Fu

    2014-11-01

    Full Text Available Based on the MEGAN (Model of Emissions of Gases and Aerosols from Nature module embedded within the global chemical transport model (GEOS-Chem, we estimate the changes in emissions of biogenic volatile organic compounds (BVOCs and their impacts on surface-layer O3 and secondary organic aerosols (SOA in China between the late 1980s and the mid-2000s by using the land cover dataset derived from remote sensing images and land use survey. The land cover change in China from the late 1980s to the mid-2000s can be characterised by an expansion of urban areas (the total urban area in the mid-2000s was four times that in the late 1980s and a reduction in total vegetation coverage by 4%. Regionally, the fractions of land covered by forests exhibited increases in southeastern and northeastern China by 10–30 and 5–15%, respectively, those covered by cropland decreased in most regions except that the farming–pastoral zone in northern China increased by 5–20%, and the factions of grassland in northern China showed a large reduction of 5–30%. With changes in both land cover and meteorological fields, annual BVOC emission in China is estimated to increase by 11.4% in the mid-2000s relative to the late 1980s. With anthropogenic emissions of O3 precursors, aerosol precursors and aerosols fixed at year 2005 levels, the changes in land cover and meteorological parameters from the late 1980s to the mid-2000s are simulated to change the seasonal mean surface-layer O3 concentrations by −4 to +6 ppbv (−10 to +20% and to change the seasonal mean surface-layer SOA concentrations by −0.4 to +0.6 µg m−3 (−20 to +30% over China. We find that the decadal changes in meteorological parameters had larger collective effects on BVOC emissions and surface-layer concentrations of O3 and SOA than those in land cover and land use alone. We also perform a sensitivity simulation to compare the impacts of changes in anthropogenic emissions on concentrations of O3

  10. The Perversion of Empire: Edmund Burke and the Nature of Imperial Responsibility.

    Science.gov (United States)

    Bass, Jeff D.

    1995-01-01

    Proposes an alternative interpretation of imperial responsibility, founded upon Edmund Burke's rhetorical denunciation of the East India Company in 1783. Shows how Burke constructed a new understanding of imperial responsibility, in which the need to protect foreign peoples from unscrupulous Britons was stressed instead of any sense of racial…

  11. Breaking the Boundaries of Victorian Imperialism or Extending a Reformed 'Paternalism'? Mary Carpenter and India.

    Science.gov (United States)

    Watts, Ruth

    2000-01-01

    Discusses the debate on gender and imperialism in India by examining the case of Mary Carpenter, a nineteenth century English educationist and social reformer, in order to provide more information on the debate. Addresses where Carpenter stood in the discourse on imperialism. (CMK)

  12. 78 FR 896 - Revisions to the California State Implementation Plan, Imperial County Air Pollution Control...

    Science.gov (United States)

    2013-01-07

    ... is finalizing approval of revisions to the Imperial County Air Pollution Control District (ICAPCD...)(2)). List of Subjects in 40 CFR Part 52 Environmental protection, Air pollution control... AGENCY 40 CFR Part 52 Revisions to the California State Implementation Plan, Imperial County...

  13. A Study of Imperial Maids’ Life Through Tang’s Poetry

    Directory of Open Access Journals (Sweden)

    Xuc Lin

    2012-10-01

    Full Text Available Article observed the life of Tang’s imperial maids through the poetry of Tang Dynasty. . Imperial maids were started from Sui Dynasty, especially Emperor Sui Yangdi’s period, and Tang’s imperial maids were many. Emperor with various kind of reasons, in most every year would choose some girls and took them into his palace and they worked as imperial maids. They were girls from ordinary people, respectable, and noble families. Those girls who once entered imperial palace, theyb would be very hard to come out. They had to obey the regulation in the palace. Through some poetry it could be portrayed the imperial maids’ lifetime in serving the emperor,imperial concubines and got rest after midnight. Except for working, they weren’t able to come out from palace, they couldn’t go home to visit their family, even got married, their lives were full of loneliness. If they were sick, or old, the emperor wouldn’t like them anymore, they would be sent away anytime. Even if they left imperial palace, and got their freedom, but most of them lived tragically. 

  14. The Contemporary Reality of Canadian Imperialism: Settler Colonialism and the Hybrid Colonial State

    Science.gov (United States)

    Barker, Adam J.

    2009-01-01

    The author's fundamental contention is this: Canadian society remains driven by the logic of imperialism and engages in concerted colonial action against Indigenous peoples whose claims to land and self-determination continue to undermine the legitimacy of Canadian authority and hegemony. The imperial ambitions of the Canadian state and its…

  15. 78 FR 922 - Revisions to the California State Implementation Plan, Imperial County Air Pollution Control...

    Science.gov (United States)

    2013-01-07

    ... Pollution Control District AGENCY: Environmental Protection Agency (EPA). ACTION: Proposed rule. SUMMARY: EPA is proposing to approve revisions to the Imperial County Air Pollution Control District (ICAPCD... disturbed soils in open and agricultural areas in Imperial County. We are proposing to approve local...

  16. A New Oviraptorid Dinosaur (Dinosauria: Oviraptorosauria) from the Late Cretaceous of Southern China and Its Paleobiogeographical Implications

    Science.gov (United States)

    Lü, Junchang; Pu, Hanyong; Kobayashi, Yoshitsugu; Xu, Li; Chang, Huali; Shang, Yuhua; Liu, Di; Lee, Yuong-Nam; Kundrát, Martin; Shen, Caizhi

    2015-07-01

    The Ganzhou area of Jiangxi Province, southern China is becoming one of the most productive oviraptorosaurian localities in the world. A new oviraptorid dinosaur was unearthed from the uppermost Upper Cretaceous Nanxiong Formation of Ganzhou area. It is characterized by an anterodorsally sloping occiput and quadrate (a feature shared with Citipati), a circular supratemporal fenestra that is much smaller than the lower temporal fenestra, and a dentary in which the dorsal margin above the external mandibular fenestra is strongly concave ventrally. The position of the anteroventral corner of the external naris in relation to the posterodorsal corner of the antorbital fenestra provides new insight into the craniofacial evolution of oviraptorosaurid dinosaurs. A phylogenetic analysis recovers the new taxon as closely related to the Mongolian Citipati. Six oviraptorid dinosaurs from the Nanxiong Formation (Ganzhou and Nanxiong) are distributed within three clades of the family. Each of the three clades from the Nanxiong Formation has close relatives in Inner Mongolia and Mongolia, and in both places each clade may have had a specific diet or occupied a different ecological niche. Oviraptorid dinosaurs were geographically widespread across Asia in the latest Cretaceous and were an important component of terrestrial ecosystems during this time.

  17. Robert Hart and China Customs in Late Qing Dynasty%赫德与晚清海关

    Institute of Scientific and Technical Information of China (English)

    周瑶

    2011-01-01

    鸦片战争之后,英国政府凭借强大军事实力与清政府签订一系列不平等条约,夺取在华政治、经济和军事特权。赫德担任中国海关总税务司这一要职期间,掌握了中国对外进出口贸易的税收大权,在发展对华贸易中维护英国的利益,但是其实行的海关体制方面的改革,也为中国海关走向近代化奠定了一定基础。%After the Opium war, the British Government forced Qing Dynasty to sign a series of unequal treaties by its powerful military force, winning the privilege in the political, economic and military fields. Inspectorate General of Customs in the charge of Hard mastered the tax of China's export and import trade to safeguard the interests of Britain during the course of developing trade with China. However, the system reform of the customs he made laid a solid foundation for the modernization of customs.

  18. Origin of Minerals and Elements in the Late Permian Coal Seams of the Shiping Mine, Sichuan, Southwestern China

    Directory of Open Access Journals (Sweden)

    Yangbing Luo

    2016-07-01

    Full Text Available Volcanic layers in coal seams in southwestern China coalfields have received much attention given their significance in coal geology studies and their potential economic value. In this study, the mineralogical and geochemical compositions of C19 and C25 coal seams were examined, and the following findings were obtained. (1 Clay minerals in sample C19-r are argillized, and sedimentary layering is not observed. The acicular idiomorphic crystals of apatite and the phenocrysts of Ti-augite coexisting with magnetite in roof sample C19-r are common minerals in basaltic rock. The rare earth elements (REE distribution pattern of C19-r, which is characterized by positive Eu anomalies and M-REE enrichment, is the same as that of high-Ti basalt. The concentrations of Ti, V, Co, Cr, Ni, Cu, Zn, Nb, Ta, Zr, and Hf in C19-r are closer to those of high-Ti basalt. In conclusion, roof sample C19-r consists of tuffaceous clay, probably with a high-Ti mafic magma source. (2 The geochemical characteristics of the C25 coals are same as those reported for coal affected by alkali volcanic ash, enrichment in Nb, Ta, Zr, Hf, and REE, causing the C25 minable coal seams to have higher potential value. Such a vertical study of coals and host rocks could provide more information for coal-forming depositional environment analysis, for identification of volcanic eruption time and magma intrusion, and for facilitating stratigraphic subdivision and correlation.

  19. A Possible Long-tailed Bird with a Pygostyle from the Late Mesozoic Yixian Formation,Western Liaoning,China

    Institute of Scientific and Technical Information of China (English)

    L(U) Junchang; HOU Lianhai

    2005-01-01

    An incomplete caudal vertebral series (IVPP V11309) from the Yixian Formation of late Mesozoic,Jianshangou area of B eipiao, western Liaoning Province, may represent a new bird. The tail is composed of at least 12 free caudal vertebrae and the most distal 5 caudal vertebrae co-ossified into a pygostyle. The pygostyle is plate-like and slightly curved dorsally. The anterior free caudals are amphiplatyan. The anterior caudal surfaces of the last three free caudals are concave, but their posterior articular surfaces are convex. The pygostyle is regarded as the first appeared flight apparatus during the evolutionary process from Archaeopteryx to neornithes. The pygostyle appeared in most early fossil birds and almost all the modern birds. Although their morphologies are different, they are basically formed by at least four last caudal vertebrae. The specimen V11309 is regarded as a bird rather than a non-avian theropod dinosaur based on the following characters: short caudal vertebrae, numerous pits present on the surfaces of the centra and, a foramen present between the basal part of the fused neural spines, which is similar to that of Struthio camelus. The discoveries of pygostyles from the therizinosauroids and oviraptorosaurs may provide strong evidence for supporting the origin of birds from small theropod dinosaurs. The structure of the pygostyle in specimen V11309 is different from those of Beipiaosaurus (Therizinosauroid) and Nomingia (oviraptorosaur). The most parsimonious interpretation is that these pygostyle-like structures are independently acquired by Beipiaosaurus and Nomingia during their evolutionary process.

  20. The age measures and its layer sequence tratigraphy of Late Quaternary sediment in Lushan Dajiaochang of China

    Institute of Scientific and Technical Information of China (English)

    Hu Dongsheng; Hu Rong; Li Xiaoyu; Hu Wenxuan; Wang Xulong; Tian Xingong; Liu Weiguo; Zhang Guowei

    2013-01-01

    Through the scientific investigation on Lushan for a long time,detailed studies have been carried out on the geologic stratum section of Late Quaternary in Dajiaochang. The series age data of complete stratigraphic section and full time formation since 400 kaBP were based on the results of the analyses using the dating methods with various instruments such as the ancient geomagnetism,electronics spin resonance (ESR),36Cl and lumines-cence dating,etc. Corresponding to these data,it identified the paleomagnetic polarity events including Biwa-Ⅲevent (320 kaBP),Biwa-Ⅱevent (260 kaBP),Biwa-Ⅰevent (180 kaBP,scarcity due to the disturbance of the iron dish),Blake event (100 kaBP) and Laschamp event (20 kaBP,didn’t grow due to the activities of the surface), etc. Combined with the sequence stratigraphy,layer type characteristics and its sediment environment,the strati-graphic can be divided into 4 stages of development respectively:StageⅠis the climate period of glacial epoch (200~400 kaBP);stageⅡis the climate period of interglacial epoch (100~200 kaBP);stageⅢis the climate peri-od of periglacial epoch (10~100 kaBP);stageⅣis the climate period of postglacial epoch (0~10 kaBP).

  1. 77 FR 55224 - Notice of Availability of the Proposed Imperial Sand Dunes Recreation Area Management Plan and...

    Science.gov (United States)

    2012-09-07

    ... Bureau of Land Management Notice of Availability of the Proposed Imperial Sand Dunes Recreation Area... Impact Statement (EIS), for the Imperial Sand Dunes Recreation Area (ISDRA), and by this notice is... Register. ADDRESSES: Copies of the Proposed Imperial Sand Dunes RAMP and CDCA Plan Amendment/Final EIS...

  2. 78 FR 36568 - Notice of Availability of the Record of Decision for the Approved Imperial Sand Dunes Recreation...

    Science.gov (United States)

    2013-06-18

    ... Bureau of Land Management Notice of Availability of the Record of Decision for the Approved Imperial Sand... Management (BLM) announces the availability of the Imperial Sand Dunes Recreation Area Record of Decision... receive a reply during normal business hours. SUPPLEMENTARY INFORMATION: The Imperial Sand...

  3. 75 FR 45653 - Notice of Re-Opening of Comment Period for the Draft Imperial Sand Dunes Recreation Area...

    Science.gov (United States)

    2010-08-03

    ... Bureau of Land Management Notice of Re-Opening of Comment Period for the Draft Imperial Sand Dunes... of the comment period on the Draft Imperial Sand Dunes Recreation Area Management Plan (RAMP) and... So. 4th St., El Centro, California 92243. Copies of the Draft Imperial Sand Dunes RAMP/EIS...

  4. Late Quaternary Planktic Foraminifer Fauna andMonsoon Upwelling Records from the Western South China Sea, Near the Vietnam

    Directory of Open Access Journals (Sweden)

    Pai-Sen Yu

    2008-01-01

    Full Text Available Marine sediment core MD012394 from the Vietnam coastal upwelling area in the western South China Sea was investigated in order to reconstruct the last Quaternary monsoon upwelling based on planktic foraminifer fauna assemblages and fauna-based sea surface temperature (SST estimates. The age model of core MD012394 was constructed using oxygen isotope stratigraphy of the planktic foraminifer G. sacculifer, with 10 accelerator mass spectrometry (AMS 14C dating of planktic foraminifers from the sediment samples. Our studies on the relative and absolute abundances of planktic foraminifer assemblages reveal eight dominant species in core MD012394: N. dutertrei + N. pachyderma (right coiling, G. ruber, G. glutinata, G. sacculifer, P. obliquiloculata, G. menardii + G. tumida, G. calida, and G. inflata. In a Q-mode factor analysis of the fauna abundance data, the fauna factors show variations that do not parallel the glacial/interglacial changes throughout the last 135 kyr. The relative abundance patterns of G. inflata and N. dutertrei (including N. pachyderma-R are interpreted as hydrographic proxies for East Asian summer and winter monsoon, respectively, in the current study. We calculated the fluctuations in the SST using the Revised Analog Method (RAM in MD012394 and found that the abundance changes of the summer monsoon upwelling indicator G. inflata were similar and nearly synchronous. This suggests that the summer monsoon-driven upwelling signal was strong near the local summer insolation maximum, which induced low SSTs, particular around ~11, 33, 59, and 83 kya. Our studies support the view that the strengths of both summer insolation and the East Asian summer monsoon have determined the relative abundance of planktic foraminifers and the SSTs in the western SCS during the last 135 kyr.

  5. Petrogenesis of late Paleozoic-to-early Mesozoic granitoids and metagabbroic rocks of the Tengchong Block, SW China: implications for the evolution of the eastern Paleo-Tethys

    Science.gov (United States)

    Zhu, Ren-Zhi; Lai, Shao-Cong; Qin, Jiang-Feng; Zhao, Shao-Wei

    2017-06-01

    This paper presents precise zircon U-Pb, bulk-rock geochemical, and Sr-Nd-Pb isotopic data for metagabbro, quartz diorite, and granite units within the Tengchong Block of SW China, which forms the southeastern extension of the Himalayan orogeny and the southwestern section of the Sanjiang orogenic belt, a key region for furthering our understanding of the evolution of the eastern Paleo-Tethys. These data reveal four groups of zircon U-Pb ages that range from the late Paleozoic to the early Mesozoic, including a 263.6 ± 3.6 Ma quartz diorite, a 218.5 ± 5.4 Ma two-mica granite, a 205.7 ± 3.1 Ma metagabbroic unit, and a 195.5 ± 2.2 Ma biotite granite. The quartz diorite in this area contains low concentrations of SiO2 (60.71-64.32 wt%), is sodium-rich, and is metaluminous, indicating formation from magmas generated by a mixed source of metamafic rocks with a significant metapelitic sedimentary material within lower arc crust. The two-mica granites contain high concentrations of SiO2 (73.2-74.3 wt%), are strongly peraluminous, and have evolved Sr-Nd-Pb isotopic compositions, all of which are indicative of a crustal source, most probably from the partial melting of felsic pelite and metagreywacke/psammite material. The metagabbros contain low concentrations of SiO2 (50.17-50.96 wt%), are sodium-rich, contain high concentrations of Fe2O3T (9.79-10.06 wt%) and CaO (6.88-7.12 wt%), and are significantly enriched in the Sr (869-894 ppm) and LREE (198.14-464.60 ppm), indicative of derivation from magmas generated by a metasomatized mantle wedge modified by the sedimentary-derived component. The biotite granites are weakly peraluminous and formed from magmas generated by melting of metasedimentary sources dominated by metagreywacke/psammite material. Combining the petrology and geochemistry of these units with the regional geology of the Indosinian orogenic belt provides evidence for two stages of magmatism: an initial stage that generated magmas during partial melting of

  6. Spatiotemporal changes in precipitation extremes over Yangtze River basin, China, considering the rainfall shift in the late 1970s

    Science.gov (United States)

    Gao, Tao; Xie, Lian

    2016-12-01

    Precipitation extremes are the dominated causes for the formation of severe flood disasters at regional and local scales under the background of global climate change. In the present study, five annual extreme precipitation events, including 1, 7 and 30 day annual maximum rainfall and 95th and 97.5th percentile threshold levels, are analyzed relating to the reference period 1960-2011 from 140 meteorological stations over Yangtze River basin (YRB). A generalized extreme value (GEV) distribution is applied to fit annual and percentile extreme precipitation events at each station with return periods up to 200 years. The entire time period is divided into preclimatic (preceding climatic) period 1960-1980 and aftclimatic (after climatic) period 1981-2011 by considering distinctly abrupt shift of precipitation regime in the late 1970s across YRB. And the Mann-Kendall trend test is adopted to conduct trend analysis during pre- and aftclimatic periods, respectively, for the purpose of exploring possible increasing/decreasing patterns in precipitation extremes. The results indicate that the increasing trends for return values during aftclimatic period change significantly in time and space in terms of different magnitudes of extreme precipitation, while the stations with significantly positive trends are mainly distributed in the vicinity of the mainstream and major tributaries as well as large lakes, this would result in more tremendous flood disasters in the mid-lower reaches of YRB, especially in southeast coastal regions. The increasing/decreasing linear trends based on annual maximum precipitation are also investigated in pre- and aftclimatic periods, respectively, whereas those changes are not significantly similar to the variations of return values during both subperiods. Moreover, spatiotemporal patterns of precipitation extremes become more uneven and unstable in the second half period over YRB.

  7. The relationship between species diversity and ecosystem function (productivity) of the late Middle Permian brachiopods community at the region of Hechuan, Chongqing, China

    Institute of Scientific and Technical Information of China (English)

    ZENG Yong; JIANG LiJun; KE Yan; L(U) Qian; ZHAO Li; LIANG JiaDong; HU Han; LINGHU Bo

    2012-01-01

    The relationship between species diversity and ecosystem function is a hot topic in ecology and environics.This paper investigates the evolution of diversity of the late Middle Permian brachiopods community in Hechuan,Chongqing,China,and discusses the relationship between species diversity and community productivity in terms of the geohistorical development.This paper shows that the species diversity is externalized by several indexes,and the relationship between diversity and productivity is too complex to be described by a single assumption.The relationship between species diversity and community productivity is restricted by environment and community evolution.When the community succeeds normally,the relationship between species richness index,species diversity index,and species evenness index to productivity is in linear dependence relation to each other,which is met with the third assumption.But,when the environment interference surpasses the bearing capability of the community,not only the community succession will be terminated and be replaced by another one,but also the relationship between species richness index,species diversity index,and species evenness index to productivity is also inversed to negative correlation by the interference from environment.Only the relationship between ecological dominance and productivity is in linear dependence relation to each other and approximately met with the third assumption.It is illustrated that the assumption that the productivity is in linear dependence relation with diversity should be established on the presupposition that the community succession is normal.

  8. Late winter larval fish assemblage in the southern East China Sea, with emphasis on spatial relations between mesopelagic and commercial pelagic fish larvae

    Science.gov (United States)

    Sassa, Chiyuki; Konishi, Yoshinobu

    2015-10-01

    We examined larval fish assemblages in the southern East China Sea during late winter where large spawning grounds of several commercial pelagic fishes are formed. Our samples include a total of 187 species or taxa of larval fish belonging to 118 genera, 96 families, and 18 orders. Mesopelagic fish larvae, mainly Stomiiformes, Aulopiformes, and Myctophiformes, accounted for 66.5% of the total catch, while commercial species such as Trachurus japonicus, Scomber spp., and Trichiurus japonicus for 16.6%. Based on the species composition, three assemblages were recognized: Kuroshio (KUR), Shelf-Break (BRE), and Shelf (SHE) assemblages. KUR assemblage was mainly characterized by various mesopelagic fishes such as Sigmops gracilis, Diaphus spp., and Myctophum asperum, BRE assemblage by both commercial pelagic and mesopelagic species, SHE assemblage by demersal species such as Lepidotrigla spp. and Gobiidae spp. Both abundance and diversity were highest in KUR assemblage, although food availability for the larvae would be poorest. The combination of variables of sea surface temperature-chlorophyll a concentrations best explained the larval distribution. Except for Benthosema pterotum, the center of distribution of mesopelagic fish larvae was clearly separated from that of the commercial species by the Kuroshio front. However, a northward intrusion of the Kuroshio transported mesopelagic fish larvae onto the shelf, forming the BRE assemblage. Competition for prey between mesopelagic and commercial pelagic fish larvae would potentially occur if the intrusion is strong.

  9. On Cleaning: Student Activism in the Corporate and Imperial University

    Directory of Open Access Journals (Sweden)

    Kristi Carey

    2016-11-01

    Full Text Available In the past year, over 100 university campuses in the United States and elsewhere have witnessed student protest, specifically against institutionalized racism and in response to symptoms of the university’s neoliberal, capitalist and imperial culture. This article outlines the emergence and confluence of the corporate and imperial university, producing and reproducing the violence of consumer culture, academic containment, and institutional control. This case study of a small, elite, liberal arts college in the United States will unravel the messiness of the contact zone where university administration and student protest meet, and its meanings for those of us who find ourselves ever-contained within spaces of higher education. Through critical discourse analysis and participant observation, I provide some preliminary mapping of how the university sanitizes—how it keeps itself ‘clean’—and the different ways this is interpreted, confirmed, and resisted by its campus community. Queer and feminist readings of pollution, dirt, and bacteria contextualize the university’s response to student activism, and daily operation, in the politics of containment and cleanliness.

  10. Contemporaneity of colonialism: Capitalist modernity, imperial racism and necropolitics

    Directory of Open Access Journals (Sweden)

    Šefik Tatlić

    2016-06-01

    Full Text Available This text articulates global capitalism as an imperial formation, it deems that modernity is a particular project and/or discursive rhetoric, as well as it articulates necropolitics as the dominant form of politics in capitalism in the post 9/11 era. Hence, global capitalism is being treated here as the imperial formation and a relation of dominance which fundamentally resides on colonial epistemologies and governing logic. Modernity is, therefore, being articulated as a particular discursive rhetoric of the First World which universalizes modernity in order to conceal and/or repress other formats of organizing modernity and, in order to apply and normalize various premodern logics and ideologies, such as racism, as foundations on the basis of which social differentiation and capitalist hierarchies of exploitation are being organized. Finally, this text articulates the concept of necropolitics which is an obscene form of politics that has, in the post 9/11 era, been reduced to a form of management of death and to a machinistic form of governing that treats the world as if it is just a commodifiable category.

  11. Modeling Events in the Lower Imperial Valley Basin

    Science.gov (United States)

    Tian, X.; Wei, S.; Zhan, Z.; Fielding, E. J.; Helmberger, D. V.

    2010-12-01

    The Imperial Valley below the US-Mexican border has few seismic stations but many significant earthquakes. Many of these events, such as the recent El Mayor-Cucapah event, have complex mechanisms involving a mixture of strike-slip and normal slip patterns with now over 30 aftershocks with magnitude over 4.5. Unfortunately, many earthquake records from the Southern Imperial Valley display a great deal of complexity, ie., strong Rayleigh wave multipathing and extended codas. In short, regional recordings in the US are too complex to easily separate source properties from complex propagation. Fortunately, the Dec 30 foreshock (Mw=5.9) has excellent recordings teleseismically and regionally, and moreover is observed with InSAR. We use this simple strike-slip event to calibrate paths. In particular, we are finding record segments involving Pnl (including depth phases) and some surface waves (mostly Love waves) that appear well behaved, ie., can be approximated by synthetics from 1D local models and events modeled with the Cut-and-Paste (CAP) routine. Simple events can then be identified along with path calibration. Modeling the more complicated paths can be started with known mechanisms. We will report on both the aftershocks and historic events.

  12. Imperialism and Financialism: A Story of a Nexus

    Directory of Open Access Journals (Sweden)

    Shimshon Bichler

    2012-03-01

    Full Text Available Over the past century, the nexus of imperialism and financialism has become a major axis of Marxist theory and praxis. Many Marxists consider this nexus to be a cause of worldly ills, but the historical role they ascribe to it has changed dramatically over time. The key change concerns the nature and direction of surplus and liquidity flows. The first incarnation of the nexus, articulated at the turn of the twentieth century, explained the imperialist scramble for colonies to which finance capital could export its ‘excessive’ surplus. The next version posited a neo-imperial world of monopoly capitalism where the core’s surplus is absorbed domestically, sucked into a ‘black hole’ of military spending and financial intermediation. The third script postulated a World System where surplus is imported from the dependent periphery into the financial core. And the most recent edition explains the hollowing out of the U.S. core, a ‘red giant’ that has already burned much of its own productive fuel and is now trying to ‘financialize’ the rest of the world in order to use the system’s external liquidity. This paper outlines this chameleon-like transformation, assesses what is left of the nexus and asks whether it is worth keeping.

  13. Late Quaternary environmental changes inferred from n-alkane evidence in coastal area of southern Hainan Island, China

    Science.gov (United States)

    Wang, Mengyuan; Zheng, Zhuo

    2016-04-01

    The studied core was a coastal core in Hainan Island, China. It is in length of 49.01m and divided into four Units (MIS 1~MIS 6) according to lithology description. The Optically Stimulated Luminescence (OSL) attributes the sediments from Unit 3 to the Oxygen Isotope Stage of MIS 5e (Unit 3b and 3c) and 5d (Unit 3a). To interpret the origination of organic carbons and to reconstruct paleovegetation changes, n-alkane, δ13C and TOC have been used in the present research. The result of n-alkanes distribution indicates a series of changes of sedimentary environment and terrestrial input. The shallow water facies at Unit 2, 3a and 4 is mainly characterized by short carbon chain n-alkanes and relatively low concentration. Contrasting with that of deep-water marine facies of MIS 5e (Unit 3b), the n-alkane pattern is typical bimodal and the main peaks are both in short and long carbon chains. During Unit 3b-1 (MIS 5e), more terrestrial original n-alkanes contribute to the concentration of TOC than oceanic. Organic matter source is mainly terrestrial origination. Total organic matter input mechanism of TLG-01 correlates with sediment grain size (average grain size). Total organic carbon input is enhanced with the increasing of fine grain size component. The variation of CPI (25-33) value in this study correlates with hydrological energy. The highest CPI (25-33) value is shown in the high sea level period of MIS 5e, comparing with that in MIS 5d and MIS 1. High CPI value corresponds to high TOC and average grain size (Φ) value. In the weak hydrological energy sedimentary environment, more terrestrial organic matter, together with TOC, deposit in the study area. ACL (25-33) index display higher values in the interglacial period (MIS 5 and MIS 1) than MIS 3 (sediments weathered during MIS 2) and MIS 6. Paq proxy, together with δ13C, estimates the mangrove growing depth in MIS 5e. The correlation between δ13C and each carbon chain alkane state stabilize and turbulence of

  14. Opening of the Tethys in southwest China and its significance to the breakup of East Gondwanaland in late Paleozoic: Evidence from SHRIMP U-Pb zircon analyses for the Garzê ophiolite block

    Institute of Scientific and Technical Information of China (English)

    YAN Quanren; WANG Jianguo; ZHANG Dehui; ZHAO Jian; WANG Zongqi; LIU Shuwen; LI Qiugen; ZHANG Hongyuan; WANG Tao; LIU Dunyi; SHI Yuruo; JIAN Ping

    2005-01-01

    SHRIMP U-Pb zircon analyses for a gabbro sample from the Garzê ophiolite block yielded a mean 206Pb/238U age of 292±4 Ma, which indicated that the spreading time of the Garzê-Litang Tethys was most likely at the earliest Permian. Combined with previous studies, we suggest that the opening of the Tethys in southwest China was derived from breakup of the East Gondwanaland in the late Paleozoic.

  15. Formation of Medical Units in Response to Epidemics in the Australian Imperial Force in Palestine 1918

    Directory of Open Access Journals (Sweden)

    Prof. G Dennis Shanks MD

    2014-06-01

    Full Text Available In the closing days of the First World War, British cavalry operations defeated the Turkish Armies in Palestine. Australian Light Horse Regiments as part of the Australian Imperial Forces (AIF were prominent in the capture of Amman, Beirut and Damascus. Epidemic infectious diseases were part of the severe desert environment faced by soldiers in the Middle East. Cholera and dysentery epidemics required reformation of medical units to emphasize mobility in an austere environment. A large epidemic of falciparum malaria coinciding with pandemic influenza shut down military operations and caused many deaths in late 1918. Three separate military medical units were formed in Egypt to address epidemic infectious diseases during mobile operations in the desert: ANZAC Field Laboratory, 5th Malaria Diagnosis Station and 7th Mobile Sanitary Section. Laboratory and preventive medicine units were critical to the military’s ability to conduct operations in the Middle East in 1918 and are likely to become vital for future missions in developing countries. As was the case in 1918, military medical units may have to be acutely restructured to control infectious disease outbreaks

  16. Preliminary research on Mesalake Jilantai-Hetao in the arid areas of China during the Late Quaternary

    Institute of Scientific and Technical Information of China (English)

    GHEN FaHu; FAN YuXin; CHUN Xi; D.B. MADSEN; G.G. OVIATT; ZHAO Hui; YANG LiPing; SUN Yang

    2008-01-01

    preserved on the top of profiles in the embankments at higher elevations. All this evidence suggests that there was once a huge palaeo-lake covering the Jilantai region and most part of the Hetao Plain with the highest lake level reaching ~1080 m a.s.l. We refer to the huge paleolake, which was larger than modern Lake Baikal, as "Megalake Jilantai-Hetao." OSL dating results indicate that the megalake formed before ~60-50 ka, and the four shorelines at elevations between 1060 and 1035 m a.s.l, likely represent the lake level variations from ~60-~50 ka to the early Holocene. The discovery of the Megalake Jilantai-Hetao likely will impact understanding of the development of the Yellow River during the late Quaternary, the evolution of the Ulan Buh and Kubq deserts, neotectonism in the region, and possibly regional climatic changes.

  17. The identification of the pigments used to paint statues of Feixiange Cliff in China in late 19th century by micro-Raman spectroscopy and scanning electron microscopy/energy dispersive X-ray analysis

    Science.gov (United States)

    Jin, Pu-jun; Huang, Wei; Jianhua-Wang; Zhao, Gang; Wang, Xiao-ling

    2010-11-01

    The application of micro-Raman spectroscopy (μ-RS) and scanning electron microscopy (SEM)/energy dispersive X-ray spectrometer (EDS) to the research of pigments collected from Statues of Feixiange Cliff No. 67 and No. 69 niche of Tang Dynasty in China is reported. Five kinds of pigments were found in the experimental data, including black (carbon), white (gypsum + quartz), blue (lapis lazuli) and green (Paris green + Barium sulphate). After synthesized in 1814, Paris green was reported for a large import as a light and bright green pigment to paint architectures in China from the late 19th century. The analyzed blue pigment demonstrated the similar Raman spectra to the Lâjvardina blue glazed ceramics, which indicated lapis lazuli was an artificial product. This confirmed the painting of Feixiange Cliff in the early Republic of China as the historical record, and also reveals that some pigments were imported from abroad.

  18. Turning pedagogy into a science: teachers and psychologists in late imperial Russia (1897-1917).

    Science.gov (United States)

    Byford, Andy

    2008-01-01

    The article explores the Russian teachers' tortuous campaign at the beginning of the twentieth century to rise above the status of "semiprofessionals" by rooting the legitimacy of their professional expertise, training institutions, and working practices in the authority of "science." This involved a radical reshaping of traditional pedagogy and its fusion with new, controversial approaches to child psychology. It also led to a proliferation of teacher-training courses and conferences devoted to "pedagogical psychology," "experimental pedagogy," and "pedology." The article analyzes how the teachers' professional aspirations interacted with the conflicting agendas of rival groups of psychologists, who were themselves engaged in bitter squabbles over the legitimate identity of psychology as a scientific discipline.

  19. Late Quaternary evolution of the East Asian summer monsoon: Clay and magnetic mineralogical records retrieved from the northern South China Sea

    Science.gov (United States)

    Chen, Q.; Liu, Z.; Kissel, C.

    2016-12-01

    East Asian monsoon is a major component of global monsoon system. Acting as the largest marginal sea in the western Pacific, the South China Sea is a natural laboratory recording East Asian monsoon evolution. In order to reconstruct the late Quaternary evolution of the monsoon, we analyzed in details the 50.8-m-long Core MD12-3432 retrieved from the northern South China Sea at 2125 m water depth. Carbonate and magnetic stratigraphy indicates that Core MD12-3432 covers the last 400 ka. Clay mineralogical analysis was performed every 10 cm using XRD method. Bulk magnetic properties (susceptibility, NRM, ARM, and IRM) were measured on u-channel samples with a resolution of 2 cm. Cumulative log Gaussian decomposition analysis was performed on 33 high resolution IRM acquisition curves to evaluate the contribution of coercivity components. Three-axis thermal demagnetization was conducted on 14 samples to identify the nature of magnetic minerals. Clay mineral assemblage of Core MD12-3432 is dominated by smectite (23-59%) and illite (22-43%), with minor chlorite (13-27%) and kaolinite (4-13%). Because smectite is formed by rapid chemical weathering of volcanic rocks in Luzon, while illite and chlorite are primary minerals formed by physical erosion, smectite/(illite+chlorite) ratio constitutes a proxy of chemical weathering intensity. Magnetic fraction of Core MD12-3432 is composed by minerals with different coercivities, the relative proportion of which varies along the core. The high coercivity is carried by hematite and the low coercivity fraction is mainly composed by magnetite with some iron-sulphides. Luzon is the most efficient source of magnetite because of the rapid eluviation and weathering of volcanic rocks, while the Pearl River basin is the only source that produces hematite mainly through physical degradation of bedrocks. Thus, the bulk coercivity as indicated by S-ratio can serve as a proxy of chemical weathering. Both indicators, smectite

  20. Reconciling late Quaternary transgressions in the Bohai Sea, China to the global sea level changes, and new linkage of sedimentary records to three astronomical rhythms

    Science.gov (United States)

    Yi, Liang

    2013-04-01

    Terminations. Science 326, 248-252. Ding, Z.L., Yu, Z.W., Rutter, N.W., Liu, T.S., 1994. Towards an orbital time scale for chinese loess deposits. Quaternary Science Reviews 13, 39-70. IOCAS (Institute of Oceanology, Chinese Academy of Sciences), 1985. Bohai Sea Geology. Science Press, Beijing, China. Liu, T., 2009. Loess and Arid Environment. Anhui Science & Techonology Press, Hefei, China. Wang, Y., Cheng, H., Edwards, R.L., An, Z., Wu, J., Chen, C.-C., Dorale, J.A., 2001. A High-Resolution Absolute-Dated Late Pleistocene Monsoon Record from Hulu Cave, China. Science 294, 2345-2348. Wang, Y., Cheng, H., Edwards, R.L., Kong, X., Shao, X., Chen, S., Wu, J., Jiang, X., Wang, X., An, Z., 2008. Millennial- and orbital-scale changes in the East Asian monsoon over the past 224,000 years. Nature 451, 1090-1093. Yi, L., Yu, H., Ortiz, J.D., Xu, X., Chen, S., Ge, J., Hao, Q., Yao, J., Shi, X., Peng, S., 2012a. Late Quaternary linkage of sedimentary records to three astronomical rhythms and the Asian monsoon, inferred from a coastal borehole in the south Bohai Sea, China. Palaeogeography, Palaeoclimatology, Palaeoecology 329-310, 101-117. Yi, L., Lai, Z.P., Yu, H.J., Xu, X.Y., Su, Q., Yao, J., Wang, X.L., Shi, X., 2012b. Chronologies of sedimentary changes in the south Bohai Sea, China: Constraints from luminescence and radiocarbon dating. Boreas, doi: 10.1111/j.1502-3885.2012.00271.x. Yi, L., Yu, H.J., Ortiz, J.D., Xu, X.Y., Qiang, X.K., Huang, H.J., Shi, X., Deng, C.L., 2012c. A reconstruction of late Pleistocene relative sea level in the south Bohai Sea, China, based on sediment grain-size analysis. Sedimentary Geology 281, 88-100. Zhao, S., Yang, G., Cang, S., Zhang, H., Huang, Q., Xia, D., Wang, Y., Liu, F., Liu, C., 1978. Transgression's stratas and shoreline changes in the south coast of Bohai Bay, China. Oceanologia et Limnologia Sinica 9, 15-25.

  1. 清末民初保定经济近代化初探%The Economic Modernization of Baoding in Late Qing Dynasty and Early Republic of China

    Institute of Scientific and Technical Information of China (English)

    葛宝森

    2013-01-01

      清末民初,在晚清新政带动下,保定经济迅速向近代化过渡,一个传统的封建政治中心也出现了很浓厚的现代气息。但随着天津迅速崛起,保定无论是政治地位还是经济地位都相对衰落了,保定的经济体系已经纳入到以天津为中心的沿海经济体系圈之中,从而服从于天津的经济领导地位。从整体来看,清末民初,保定经济已经开始了近代化进程,但是由于沉重的历史包袱、地理位置的劣势、政治中心地位的下降,保定的经济形态依然是以传统的经济形态为主,具体表现为资本少,生产规模有限,技术力量薄弱,保定依然以传统性的中小消费性城市为基调。%At the late of Qing Dynasty and the beginning of the Republic of China , the economy of Baoding was quickly transferred to modernization driven by the New Deal of late Qing Dynasty .As a traditional feudal political center, there appeared very strong modern circumstance .With rapid growing-up of Tianjin, the political and eco-nomic status of Baoding was declined , and the economic system of Baoding was integrated into Tianjin ’ s coastal e-conomic circle, and thus is subject to the economic leadership of Tianjin .Overall, at that time, Baoding economy had begun the process of modernization .But due to the heavy historical burden , the geographical disadvantage , its political status was declined , and the economic form of Baoding was still based on the traditional economic patterns . The shortage of capital and technology constrained the production scale .Baoding was still kept as a traditional small and medium-sized consumer city .

  2. Astronomical forcing of sedimentary cycles of Late Eocene Liushagang Formation in the Bailian Sag, Fushan Depression, Beibuwan Basin, South China Sea

    Institute of Scientific and Technical Information of China (English)

    曹海洋; 金思丁; 孙鸣; 王华

    2016-01-01

    Sediments in the Liushagang Formation of Late Eocene form a group of key hydrocarbon play fairways in the Beibuwan Basin, South China Sea. As an important reservoir-forming combination, the Liushagang Formation consists of deltaic siliciclastic and show clear sedimentary cyclicity. According to paleontology research and stratigraphic correlation, the boundary between Liushagang Formation (Els) and Weizhou Formation (Ewz) is regarded as the Eocene-Oligocene boundary. The oxygen isotope dating for well cores from the top of the first Member of Liushagang Formation (Els1) and the bottom of the third Member of Weizhou Formation (Ewz3) give an isochron age of 35.2 Ma. Here, we use GR logging data as a paleoenvironmental proxy to conduct a detailed cyclostratigraphic study of the Els1 in the Bailian Sag, Fushan Depression. Power spectra, evolutionary fast Fourier transformation and wavelet analysis all reveal significant sedimentary cycles in Els1. The ratios of cycle wavelengths in these stratigraphic units are 21׃5׃2.8׃1.2׃1, and are interpreted as Milankovitch cycles of 400 ka and 96 ka eccentricity, 52 ka obliquity, 22 ka and 19 ka precession cycles, respectively. An astronomical time scale is established by tuning filtered 96 ka eccentricity cycles to a target curve of Well L2 in the Bailian Sag. Based on regional stratigraphic framework, combined with seismic, cores and logging data, the HST of the first member of the Liushagang Formation (Els1) delta in Well L2 was divided into six parasequence sets named Ps1-Ps6. According to the spectrum analysis by Simple Lomb periodogram from PAST program packages, the sediment accumulation rate of each parasequence sets first increased and then decreased as time went by. The sediment accumulation rate of Ps4 reached the maximum (0.127 m/ka) during the most prosperous period of delta prograding. Finally, the duration of each period of parasequence sets and more accurate geological age were calculated on the basis of

  3. A late Holocene winter monsoon record inferred from the palaeo-aeolian sand dune in the southeastern Mu Us Desert, northern China

    Institute of Scientific and Technical Information of China (English)

    Bing Liu; HeLing Jin; Fan Yang

    2016-01-01

    The variation of the Asian winter monsoonal strength has seriously affected the climate and environmental conditions in the Asian monsoonal region, and even in marginal islands and the ocean in the East Asian region. However, relevant under-standing remains unclear due to the lack of suitable geological materials and effective proxies in the key study areas. Here, we present a grain-size record derived from the palaeo-aeolian sand dune in the southeastern Mu Us Desert, together with other proxies and OSL dating, which reflect a relatively detailed history of the winter monsoon and abrupt environmental events during the past 4.2 ka. Our grain-size standard deviation model indicated that>224μm content can be considered as an indicator of the intensity of Asian winter monsoon, and it shows declined around 4.2–2.1 ka, enhanced but unstable in 2.1–0.9 ka, and obviously stronger since then. In addition, several typical climate events were also documented, forced by the periodic variation of winter monsoonal intensity. These include the cold intervals of 4.2, 2.8, 1.4 ka, and the Little Ice Age (LIA), and relatively warm sub-phases around 3.0, 2.1, 1.8 ka, and the Medieval Warm Period (MWP), which were roughly accordant with the records of the aeolian materials, peat, stalagmites, ice cores, and sea sediments in various lat-itudes of the Northern Hemisphere. Combined with the previous progresses of the Asian summer monsoon, we prelimi-narily confirmed a millennial-scale anti-correlation of Asian winter and summer monsoons in the Late Holocene epoch. This study suggests that the evolution of the palaeo-aeolian sand dune has the potential for comprehending the history of Asian monsoon across the desert regions of the modern Asian monsoonal margin in northern China.

  4. Two Late Cretaceous A-type granites related to the Yingwuling W-Sn polymetallic mineralization in Guangdong province, South China: Implications for petrogenesis, geodynamic setting, and mineralization

    Science.gov (United States)

    Zheng, Wei; Mao, Jingwen; Zhao, Haijie; Zhao, Caisheng; Yu, Xiaofei

    2017-03-01

    Major and trace elements, whole rock Sr-Nd-Pb isotopes, LA-ICP-MS U-Pb zircon dating, zircon trace elements and Hf isotope data are reported for a suite of A-type granites from Yingwuling pluton in western Guangdong province, South China. Zircon U-Pb ages obtained by laser ablation-inductively coupled plasma-mass spectrometry (LA-ICP-MS) show that biotite granite and alkali feldspar granite were emplaced in 81.3 ± 0.6 Ma and 80.6 ± 0.5 Ma, respectively. Both of the two suites have the petrographic and geochemical characteristics of A-type granite. These granitic rocks are metaluminous to weakly peraluminous and have pronounced contents of total alkalis (Na2O + K2O = 7.80-8.84%), Fe2O3T/MgO and Ga/Al ratios. They exhibit low MgO, CaO and TiO2 contents, enrichment in some LILEs and HFSEs (except for Zr, Eu and Y), depletion in Ba, Sr, P and Ti. They show A2 subtype affinity and were probably formed a temperature of 800 °C. The Yingwuling biotite granite has relatively high (87Sr/86Sr)i ratios of 0.70655 to 0.70928, low εNd(t) values of - 5.8 to - 4.2 and zircon εHf(t) values (- 5.70-1.37). Whole-rock Nd isotopic and zircon Hf isotopic two-stages model ages mostly vary from 1057 to 1506 Ma. The alkali feldspar granite display bulk rock εNd(t) values and (87Sr/86Sr)i ratios in the range of - 6.6 to - 6.1 and 0.70640 to 0.71077, respectively, and zircon εHf(t) values from - 5.44 to 0.54, with Mesoproterozoic T2DM for both Nd and Hf isotopes. Geochemical and isotopic data indicate the Yingwuling A-type granitic magmas were drived from mantle-crust interaction. Zircon grains of Yingwuling granites have relatively low Eu/Eu* and Ce4 +/Ce3 + ratios, indicating low oxygen fugacity. The visible tetrad effect in the Yingwuling granites indicates that it experienced strong fractionation and is close relationship to the W-Sn mineralization. Our new data together with previous published data indicate that Late Mesozoic A-type granitiods or alkaline intrusive rocks in South

  5. A Late Carboniferous-Early Permian slab window in the West Junggar of NW China: Geochronological and geochemical evidence from mafic to intermediate dikes

    Science.gov (United States)

    Yin, Jiyuan; Long, Xiaoping; Yuan, Chao; Sun, Min; Zhao, Guochun; Geng, Hongyan

    2013-08-01

    The Late Carboniferous to Early Permian is a critical period for the formation of particular high-temperature magmatic associations in West Junggar, NW China and the geodynamic processes of ridge subduction and related slab windows in the Central Asian Orogenic Belt. Mafic to intermediate dikes, exposed in the central and southeastern West Junggar extensively, mainly consist of Nb-enriched and magnesian suites. The Nb-enriched dikes (305 Ma) are characterized by high Nb contents (5.63-9.08 ppm) and large variations of major element contents, exhibiting high-K to medium-K calc-alkaline characteristics with high Na2O/K2O (1.33-3.85) and low Sr/Y (9-32) ratios. The dikes have moderate Mg# (44.6-52.9), LREE-rich and sub-horizontal HREE patterns ((La/Yb)N = 3.05-7.18; (Gd/Yb)N = 1.43-1.78) with weak Eu anomalies (Eu*/Eu = 0.81-1.10) and positive εNd (t) values (+ 5.2 to + 8.0), and likely originate from partial melting of mantle peridotite that was metasomatized by subducted sediment-derived melts and slab fluids. The medium-K magnesian dikes (305 Ma) are characterized by high MgO (3.05-7.28 wt.%), Cr (22.3-311 ppm) and Ni (32.6-199 ppm) contents and all plot in the field of high-Mg andesite. Some have very high Mg numbers (Mg# > 60), suggesting a primitive melt composition. These samples display positive Ba, Sr, K and negative Nb-Ta-Ti anomalies as well as strongly-depleted HREE patterns with weak positive Eu anomalies. They have high Sr/Y (27-126) and relatively high εNd (t) values (+ 6.0 to + 8.3), which suggest a similar petrogenesis as the Nb-enriched dikes, but were metasomatized by adakitic melts. The high-K magnesian dikes (284 Ma) are high-K calc-alkaline and have lower MgO (3.63-5.57 wt.%) compared with the medium-K suite. They have high Sr (422-819 ppm), Sr/Y (26-62) ratios and εNd (t) values (+ 7.0 to + 7.1) with relatively flat REE patterns ((La/Yb)N = 2.4-5.5), probably originating from partial melting of K-enriched mantle wedge peridotite metasomatized

  6. (ETHNO-)MEDICAL ETHICS IN GLOBALIZING CHINA: TRACING LOCAL KNOWLEDGE AND ADAPTATION OF BIOMEDICINE.

    Science.gov (United States)

    Micollier, Evelyne

    2015-12-01

    Encounters between several bodies of therapeutic knowledge have led to a restructuring of the entire health system, including a transformation in medical ethics. Defining "new ethics" with both Chinese and international characteristics, is part of the ongoing knowledge production process: plural health ideas, practices and medical sciences develop within the broader framework of social and economic transition. Such transition simultaneously reveals and encourages China's influence and position in an era of globalization including in the technical and knowledge production domains. Re-alignments in medical ethics in Reform China (post-1979) highlight a rather under-explored aspect of medical plurality enabling these ethics to be used as an analytical lens to provide information about social and political issues. In this article, two sets of ethical principles, one from Late Imperial China (Late Ming Era), the other from post-Mao China (1980s), are detailed and analysed. They were selected as case-studies mainly because they reflected at the time of their emergence an on-going radical change in society in the realm of health and medicine. Therefore both sets unveil the process of legitimizing a "Chinese medicine" in a context of epistemological shift: such a process takes various conceptual and practicalforms framed along the lines of the current dominant ideological system and constrained by socio-economic and political factors. Finally, issues relative to research ethics, bioethics and the New Health Reform guidelines raised in the 2000s, which represents also a significant historical turn for China, are discussed. Drawn from the overall discussion throughout the text, several concluding remarks contribute to advocate for "win-win" encounters--from the East to the West and from the South to the South, and for more implementable transnational/global ethics designing.

  7. Road infrastructure and mobility of consumption in the Mexicali-Imperial Valley border area

    Directory of Open Access Journals (Sweden)

    Alejandro Mungaray-Moctezuma

    2015-06-01

    Full Text Available The objective of this study is to analyze the mobility of consumption in the Mexicali-Imperial Valley border area. The study shows that the population in the Mexicali sections closer to border crossings generates the greatest amount of consumption dynamics with places located in Imperial Valley. Conversely, Imperial Valley sections that are more distant from the border concentrate a greater number of destination sites for these cross-border trips. It is concluded that a higher quality and more integrated road infrastructure allows the new consumption centers in Imperial Valley to be located farther away from the border and that the Mexicali population with visas can cross indiscriminately through any border crossing by taking longer journeys toward these centers.

  8. 77 FR 73391 - Approval of Air Quality Implementation Plans; California; Eastern Kern, Imperial County, Placer...

    Science.gov (United States)

    2012-12-10

    ..., Air pollution control, Carbon monoxide, Greenhouse gases, Incorporation by reference... four permitting rules submitted for the Eastern Kern Air Pollution Control District (EKAPCD), Imperial County Air Pollution Control District (ICAPCD), Placer County Air Pollution Control District...

  9. 77 FR 73316 - Approval of Air Quality Implementation Plans; California; Eastern Kern, Imperial, Placer, and...

    Science.gov (United States)

    2012-12-10

    ... pollution control, Carbon monoxide, Greenhouse gases, Incorporation by reference, Intergovernmental... rules submitted for the Eastern Kern Air Pollution Control District (EKAPCD), Imperial County Air Pollution Control District (ICAPCD), Placer County Air Pollution Control District (PCAPCD), and...

  10. 身体、皇权和明初法律文化%The emperor's four bodies: Embodied rulership and legal culture in early Ming China

    Institute of Scientific and Technical Information of China (English)

    吴艳红; 姜永琳

    2007-01-01

    This essay explores how the emperor's body was perceived in the imperial rulership and treated uniquely in legal culture in early Ming China.It argues that the ruling elite articulated four types of imperial bodies,i.e.,the body cosmic,the body politic,the body social,and the body physical,each of which exemplified a specific dimension of rulership.The emperor's four bodies are manifested in the imperial laws.The imperial laws place the emperor's body cosmic inferior to Heaven,ensure the emperor's sole authority in communicating with Heaven,require the officials' faithful service to the ruler,urge the ruler to observe rules,and strictly protect the emperor's physical body.The imperial laws,by regulating the different relationships in the embodied rulership,serve as the essential instrument to create the ideal cosmic order.

  11. The Imperial Japanese Army as a Factor in Spreading Militarism and Fascism in Prewar Japan

    OpenAIRE

    2012-01-01

    Although a broad variety of aspects concerning militarism and fascism in Japan have been focal points of research, little attention has been given to the Imperial Japanese Army as an actor in spreading militarist and fascist ideology among the Japanese populace. Japan lacked a fascist mass movement centered in a fascist political party. Nonetheless, the majority of the populace supported the government’s policies, the Imperial Japanese Army's adventurism, and right wing terrorism. In order to...

  12. Diet of Saker Falcon (Falco cherrug and Eastern Imperial Eagle (Aquila heliaca from Central Kazakhstan

    Directory of Open Access Journals (Sweden)

    Nedko Nedyalkov

    2014-06-01

    Full Text Available We present results from a study on the diet of Saker falcon (n = 15 nests and Eastern imperial eagle (n = 2 nests from south Kazakhstan, on the basis of food remains and pellets collected during the 2009 breeding season. The main prey for Saker falcon was predominantly rodents living in middle-size colonies – Spermophilus erytrogenys and Rhombomys opimus. We also present the results from the diet of two pairs of Eastern imperial eagles nesting close to Balkhash Lake.

  13. The Silver Dragon and the Golden Fish: an imperial Ottoman symbol

    OpenAIRE

    Alexander, David

    2003-01-01

    This article studies and catalogues a group of ottoman swords decorated with dragon and fish emblems on their hilts. Both animals were associated to the imperial power according the oriental traditon.

    Este trabajo estudia y cataloga un grupo de espadas otomanas decoradas con dragones y peces en sus empuñaduras. Estos animales fueron asociados con el poder imperial según la tradición oriental.

  14. The Silver Dragon and the Golden Fish: an imperial Ottoman symbol

    Directory of Open Access Journals (Sweden)

    Alexander, David

    2003-12-01

    Full Text Available This article studies and catalogues a group of ottoman swords decorated with dragon and fish emblems on their hilts. Both animals were associated to the imperial power according the oriental traditon.

    Este trabajo estudia y cataloga un grupo de espadas otomanas decoradas con dragones y peces en sus empuñaduras. Estos animales fueron asociados con el poder imperial según la tradición oriental.

  15. Geochemical constraints on the origin of Late Mesozoic andesites from the Ningwu basin in the Middle-Lower Yangtze Valley, South China

    Science.gov (United States)

    Chen, Long; Zheng, Yong-Fei; Zhao, Zi-Fu

    2016-06-01

    during subduction of the Cathaysia oceanic crust beneath the Yangtze Craton in the Neoproterozoic, whereas the Mesozoic mafic magmatism in the Middle-Lower Yangtze Valley is essentially caused by reactivation of the fertile and enriched mantle sources due to lithospheric extension in response to the subduction of Pacific plate beneath the eastern China continent. Therefore, the geochemical composition of andesites is primarily governed by their mantle sources that were generated by reaction of the mantle wedge peridotite with hydrous felsic melts originated from the subducted terrigenous sediment in Andean-type subduction zones, though such sources may be partially melt either immediately following generation or at a later time. Late-stage magma evolution processes such as fractional crystallization and magma mixing would have further modified the lithochemical composition of andesites but they are not the governing factors for their trace element and radiogenic isotope compositions.

  16. 陕西府谷晚中新世蓝牛化石%LATE MIOCENE BOSELAPHINI (BOVIDAE, ARTIODACTYLA) FROM FUGU, SHAANXI PROVINCE, CHINA

    Institute of Scientific and Technical Information of China (English)

    张兆群

    2005-01-01

    尽管中国发现的中新羚(偶蹄目,牛科,蓝牛族)化石较少,但由于其重要的生物年代学意义而备受重视,被作为与欧洲Vallesian期动物群对比的重要分子.描述了新近在陕西府谷喇嘛沟发现的头骨标本.依据下颌骨形态与牙齿特征,将其归入Miotragocerus gregarius (Schlosser,1903).新发现的材料完善了该种的鉴定特征:中等大小的蓝牛类;角心强烈后倾,中等分散度,具前后两条棱,横断面呈椭圆形;雄性个体角心前的额骨部分强烈隆升,雌性个体则无明显隆起;脑颅部分成梯形,其最大宽度在角心后,最小宽度在枕骨位置上;基枕骨前后突之间没有沟槽发育;P2与P3具发育且后置的次尖;p4下后尖前后向扩展.对比研究表明,该种较Miotragocerus spectabilis原始,而后者为中国发现的蓝牛类的最后代表且于中新世末期绝灭.对比巴基斯坦以及欧洲的蓝牛,认为中国的Miotragocerus可能与欧洲的种类关系较为密切,而不同于巴基斯坦的Tragoportax.最新的研究资料表明,Miotragocerus在中国主要发现于晚中新世中晚期(Turolian期),可能在8 Ma之前从欧洲迁移至东亚,由于剧烈的气候及生态环境的改变于晚中新世末期与Urmiatheriinae等大型牛科化石一起绝灭.%Though rarely reported from china, Miotragocerus has long been considered as one of the Vallesian equivalent indicators in the comparison with European faunas. Study on new specimens of Miotragocerus gregarius improves its diagnostic characters. Comparison with European and Pakistan taxa reveals that Miotragocerus possibly migrated into Eastern Asia before 8 Ma, and evolved independently into M. Spectabilis, which went extinct at the end of Lated Miocene together with some large bovids, such as all genera of Urmiatheriinae, due to dramatically climated and ecological changes at the and of the Late Miocene.

  17. A high-pyrite semianthracite of Late Permian age in the Songzao Coalfield, southwestern China: Mineralogical and geochemical relations with underlying mafic tuffs

    Energy Technology Data Exchange (ETDEWEB)

    Dai, Shifeng; Wang, Xibo; Chen, Wenmei [State Key Laboratory of Coal Resources and Safe Mining, China University of Mining and Technology, Beijing 100083, (China); Li, Dahua [Research Center of State Key Laboratory of Coal Resources and Safe Mining, Chongqing 400042, (China); Chou, Chen-Lin [Illinois State Geological Survey (Emeritus), 615 East Peabody Drive, Champaign, IL 61820, (United States); Zhou, Yiping [Yunnan Institute of Coal Geology Prospection, Kunming 650218, (China); Zhu, Changsheng; Li, Hang [Research Center of State Key Laboratory of Coal Resources and Safe Mining, Chongqing 400042, (China); Zhu, Xingwei; Xing, Yunwei; Zhang, Weiguo; Zou, Jianhua [State Key Laboratory of Coal Resources and Safe Mining, China University of Mining and Technology, Beijing 100083, (China)

    2010-09-01

    The No. 12 Coal (Late Permian) in the Songzao Coalfield, Chongqing, southwestern China, is characteristically high in pyrite and some trace elements. It is uniquely deposited directly above mafic tuff beds. Samples of coal and tuffs have been studied for their mineralogy and geochemistry using inductively coupled plasma-mass spectrometry, X-ray fluorescence, plasma low-temperature ashing plus powder X-ray diffraction, and scanning electron microscopy equipped with energy-dispersive X-ray analysis. The results show that the minerals of the No. 12 Coal are mainly composed of pyrite, clay minerals (kaolinite, chamosite, and illite), ankerite, calcite, and trace amounts of quartz and boehmite. Kaolinite and boehmite were mainly derived from sediment source region of mafic tuffs. Chamosite was formed by the reaction of kaolinite with Fe-Mg-rich fluids during early diagenesis. The high pyrite (S{sub p,d} 8.83%) in the coal was related to marine transgression over peat deposits and abundant Fe derived from the underlying mafic tuff bed. Ankerite and calcite were precipitated from epigenetic fluids. Chemical compositions of incompatible elements indicate that the tuffs were derived from enriched mantle and the source magmas had an alkali-basalt character. Compared to other coals from the Songzao Coalfield and common Chinese coals, the No. 12 Coal has a lower SiO{sub 2}/Al{sub 2}O{sub 3} (1.13) but a higher Al{sub 2}O{sub 3}/Na{sub 2}O (80.1) value and is significantly enriched in trace elements including Sc (13.5 {mu}g/g), V (121 {mu}g/g), Cr (33.6 {mu}g/g), Co (27.2 {mu}g/g), Ni (83.5 {mu}g/g), Cu (48.5 {mu}g/g), Ga (17.3 {mu}g/g), Y (68.3 {mu}g/g), Zr (444 {mu}g/g), Nb (23.8 {mu}g/g), and REE (392 {mu}g/g on average). Above mineralogical compositions, as well as similar ratios of selected elements (e.g., SiO{sub 2}/Al{sub 2}O{sub 3} and Al{sub 2}O{sub 3}/Na{sub 2}O) and similar distribution patterns of incompatible elements (e.g., the mantle-normalized diagram for

  18. Generation of Late Mesozoic Qianlishan A2-type granite in Nanling Range, South China: Implications for Shizhuyuan W-Sn mineralization and tectonic evolution

    Science.gov (United States)

    Chen, Yuxiao; Li, He; Sun, Weidong; Ireland, Trevor; Tian, Xufeng; Hu, Yongbin; Yang, Wubin; Chen, Chen; Xu, Deru

    2016-12-01

    The Late Mesozoic Qianlishan granitic complex in the western Nanling Range, South China is associated with the Shizhuyuan giant W-Sn-Mo-Bi polymetallic deposit. It mainly consists of three phases of intrusions, P-1 porphyritic biotite granite, P-2 equigranular biotite granite and P-3 granite porphyry. All three phases of granite contain quartz, plagioclase, K-feldspar and Fe-rich biotite. They have geochemical affinities of A-type granites, e.g., high FeOT/(FeOT + MgO) ratios (0.84-0.99), total alkali (Na2O + K2O, 7.50-9.04 wt.%), high Ga/Al ratios (10,000*Ga/Al > 2.6) and high Zr + Nb + Y + Ce concentrations (> 350 ppm). High Y/Nb ratios (> 1.2) suggest that the Qianlishan complex belongs to A2-type granite. Zircon U-Pb ages indicate a short age interval decreasing from 158-157 Ma, to 158-155 Ma and to 154 Ma for the P-1, P-2 and P-3 granites, respectively. These ages are similar to the mineralization age of the Shizhuyuan tungsten polymetallic deposit, within error. The Qianlishan granites were generated at low oxygen fugacity conditions based on the low values of zircon Ce4 +/Ce3 + ratios (1.53-198) and significantly negative Eu anomalies (EuN/EuN*, 0.03-0.13) in apatite. New zircon εHf(t) values for the P-3 granite range from - 13.0 to - 4.4, similar to those previously obtained for the P-1 and P-2 granites. Both the granite and apatite grains therein are characterized by high F but low Cl concentrations, suggesting the influx of a high F/Cl component. The P-2 granites especially contain higher F contents (1840-8690 ppm) and W (7-158 ppm) and Sn (6-51 ppm) concentrations and with stronger evolution features. Positive trends between F and W and Sn of Qianlishan complex indicate that high F source is crucial for mineralization of W and Sn. We consider that the lithospheric mantle source may have been metasomatized by subduction fluids in the far end of subduction zones to produce the A2 feature of the Qianlishan granite and the fluorine was introduced through

  19. Late Permian basalts in the Yanghe area, eastern Sichuan Province, SW China: Implications for the geodynamics of the Emeishan flood basalt province and Permian global mass extinction

    Science.gov (United States)

    Li, Hongbo; Zhang, Zhaochong; Santosh, M.; Lü, Linsu; Han, Liu; Liu, Wei

    2017-02-01

    We report the finding of a ∼20 m thick sequence of massive pyroxene-plagioclase-phyric basalt lava flows in the Yanghe area of the northeastern Sichuan Basin, within the Yangtze craton of SW China, which were previously considered to be located outside the Emeishan flood basalt province. This basaltic sequence above the middle Permian Maokou Formation (Fm.) is overlain by the late Permian Longtan Fm. Thus, the Yanghe basalts should be stratigraphically correlated with the Emeishan flood basalts. The Yanghe basalts show typical oceanic island basalt (OIB) affinity, and geochemically resemble Emeishan basalts, especially in the case of high-Ti (HT) basalts from the eastern domain of the Emeishan flood basalt province. The rocks have low age-corrected (87Sr/86Sr)t (t = 260 Ma) ratios (0.704158-0.704929) and Pb isotopic ratios [206Pb/204Pb(t) (18.264-18.524), 207Pb/204Pb(t) (15.543-15.58), and 208Pb/204Pb(t) (38.147-38.519)], and positive εNd(t) values (+3.15 to +3.61), suggesting that the lavas have not undergone any significant crustal contamination. The crystallization temperature of clinopyroxene is estimated to be 1368-1420 °C, suggesting anomalously thermal inputs from a mantle source and a possible plume-head origin. The fractionation of middle rare earth elements (MREE) to heavy REE (HREE) suggests that these rocks were produced by small degrees of partial melting of mantle peridotite within the garnet-spinel transition region. The stratigraphic relationships and similar geochemical signatures with the Emeishan flood basalts suggest that the Yanghe basalts are part of the Emeishan flood basalt province and can be considered as the northeastern limit of the Emeishan flood basalt province. Our finding extends the diameter of the Emeishan flood basalt province to ∼1200-1400 km, covering an area of up to ∼7 × 105 km2, two times more than previously estimated. The larger areal extent and giant eruption volume, incorporating the Sichuan Basin, lend support

  20. Depositional architecture and evolution of the Late Miocene slope channel-fan-system in the northeastern shelf-margin of South China Sea

    Science.gov (United States)

    Jiang, Jing; Lin, Changsong; Zhang, Zhongtao; Tian, Hongxun; Tao, Ze; Liu, Hanyao

    2016-04-01

    The Upper Miocene in the Pearl River Mouth Basin of northwestern shelf-margin of South China Sea Basin contains a series of slope channel - fan systems. Their depositional architecture and evolution are documented in this investigation based on an integrated analysis of cores, logs, and seismic data. Four depositional-palaeogeomorphological elements have been identified in the slope channel-fan systems as follows: broad, shallow and unconfined or partly confined outer-shelf to shelf-break channels; deeply incised and confined unidirectionally migrating slope channels; broad or U-shaped, unconfined erosional-depositional channels; frontal splays-lobes and nonchannelized sheets. The slope channels are mostly oriented NW-SE, which migrated unidirectionally northeastwards and intensively eroded almost the whole shelf-slope zone. The channel infillings are mainly mudstones, interbedded with siltstones. They might be formed by gravity flow erosion as bypassing channels. They were filled with limited gravity flow sediments at the base and mostly filled with lateral accretionary packages of bottom current deposits. At the end of the channels, a series of small-scale slope fans developed and coalesced into fan aprons along the base of the slope. The unconfined erosional-depositional channels at the upper parts of the fan-apron-systems display compound infill patterns, and commonly have concave erosional bases and convex tops. The frontal splays-lobes representing middle to distal deposits of fan-apron-systems have flat-mounded or gull-wing geometries, and the internal architectures include bidirectional downlap, progradation, and chaotic infillings. The distal nonchannelized turbidite sheets are characterized by thin-bedded, parallel to sub-parallel sheet-like geometries. Three major unconformities or obvious erosional surfaces in the channel-fan systems of the Upper Miocene are recognized, and indicate the falling of sea-level. The depositional architecture of sequences

  1. A high-pyrite semianthracite of Late Permian age in the Songzao Coalfield, southwestern China: Mineralogical and geochemical relations with underlying mafic tuffs

    Science.gov (United States)

    Dai, S.; Wang, X.; Chen, W.; Li, D.; Chou, C.-L.; Zhou, Y.; Zhu, Chen; Li, H.; Zhu, Xudong; Xing, Y.; Zhang, W.; Zou, J.

    2010-01-01

    The No. 12 Coal (Late Permian) in the Songzao Coalfield, Chongqing, southwestern China, is characteristically high in pyrite and some trace elements. It is uniquely deposited directly above mafic tuff beds. Samples of coal and tuffs have been studied for their mineralogy and geochemistry using inductively coupled plasma-mass spectrometry, X-ray fluorescence, plasma low-temperature ashing plus powder X-ray diffraction, and scanning electron microscopy equipped with energy-dispersive X-ray analysis.The results show that the minerals of the No. 12 Coal are mainly composed of pyrite, clay minerals (kaolinite, chamosite, and illite), ankerite, calcite, and trace amounts of quartz and boehmite. Kaolinite and boehmite were mainly derived from sediment source region of mafic tuffs. Chamosite was formed by the reaction of kaolinite with Fe-Mg-rich fluids during early diagenesis. The high pyrite (Sp,d=8.83%) in the coal was related to marine transgression over peat deposits and abundant Fe derived from the underlying mafic tuff bed. Ankerite and calcite were precipitated from epigenetic fluids.Chemical compositions of incompatible elements indicate that the tuffs were derived from enriched mantle and the source magmas had an alkali-basalt character. Compared to other coals from the Songzao Coalfield and common Chinese coals, the No. 12 Coal has a lower SiO2/Al2O3 (1.13) but a higher Al2O3/Na2O (80.1) value and is significantly enriched in trace elements including Sc (13.5??g/g), V (121??g/g), Cr (33.6??g/g), Co (27.2??g/g), Ni (83.5??g/g), Cu (48.5??g/g), Ga (17.3??g/g), Y (68.3??g/g), Zr (444??g/g), Nb (23.8??g/g), and REE (392??g/g on average). Above mineralogical compositions, as well as similar ratios of selected elements (e.g., SiO2/Al2O3 and Al2O3/Na2O) and similar distribution patterns of incompatible elements (e.g., the mantle-normalized diagram for incompatible elements and chondrite-normalized diagram for rare earth elements) of coal and tuff, indicated that

  2. The Key to Success: English Language Testing in China

    Science.gov (United States)

    Cheng, Liying

    2008-01-01

    The testing and examination history in China can be traced back to the imperial period nearly two thousand years ago. The existence of English language testing (tests), on the other hand, has a much shorter history. These English tests, developed and administered over the past 20 years, however, are taken by billions of learners of the English…

  3. Late Triassic paleomagnetic result from the Baoshan Terrane, West Yunnan of China: Implication for orientation of the East Paleotethys suture zone and timing of the Sibumasu-Indochina collision

    Science.gov (United States)

    Zhao, Jie; Huang, Baochun; Yan, Yonggang; Zhang, Donghai

    2015-11-01

    In order to better understand the paleogeographic position of the Baoshan Terrane in the northernmost part of the Sibumasu Block during formation of the Pangea supercontinent, a paleomagnetic study has been conducted on Late Triassic basaltic lavas from the southern part of the Baoshan Terrane in the West Yunnan region of Southwest China. Following detailed rock magnetic investigations and progressive thermal demagnetization, stable characteristic remanent magnetizations (ChRMs) were successfully isolated from Late Triassic Niuhetang lava flows. The ChRMs are of dual polarity and pass fold and reversal tests with magnetic carriers dominated by magnetite and subordinate oxidation-induced hematite; we thus interpret them as a primary remanence. This new paleomagnetic result indicates that the Baoshan Terrane was located at low paleolatitudes of ∼15°N in the Northern Hemisphere during Late Triassic times. Together with available paleomagnetic data from the Baoshan Terrane and surrounding areas, a wider paleomagnetic comparison supports the view that the East Paleotethys Ocean separated the Sibumasu and Indochina blocks and closed no later than Late Triassic times. We argue that the currently approximately north-to-south directed Changning-Menglian suture zone is very likely to have been oriented nearly east-to-west at the time of the Sibumasu-Indochina collision.

  4. Jejak-jejak Imperial dalam Beragam Nasionalisme Asia Tenggara

    Directory of Open Access Journals (Sweden)

    Ihsan Ali-Fauzi

    2013-12-01

    Full Text Available Anthony Reid, Imperial Alchemy: Nationalism and Political Identity in Southeast Asia (New York: Cambridge University Press. 2010, xiii + 248 pages.Reid has long been widely known as a senior historian with a specialty in the history of Aceh, Sumatra, and the Indonesian revolution. Recently, he has begun to write about the history of Southeast Asia. Inspired by French historian Fernand Braudel, this work presents what Reid calls a “total history” of this region. In this approach wars, royal dynasties, and foreign traders are not prioritized over the diets, health, and pastimes of ordinary people. Through this work, Reid has begun to strengthen the study of Southeast Asia. As one of the pioneers and masters of the study of Asia and the Pacific, particularly Southeast Asia, Reid is uniquely positioned to offer new insights about this region’s history. In this book, Reid offers a new understanding of the historical data collected on the link between ethnic identity, nationalism, and history of Southeast Asia.Copyright (c 2014 by SDI. All right reserved.DOI: 10.15408/sdi.v20i3.516

  5. Records of urbanism, imperialism, & environmental change in southeastern Turkey

    Science.gov (United States)

    Nicoll, K.

    2012-04-01

    Assessing the "human footprint" on the landscape since prehistory requires some comparison of the degree and pace of such changes, and the cause-and-effect, as well as the ability to resolve the anthropogenic signal from from patterns of "natural" environmental variation. The deep archaeological record provides valuable insights regarding the timeframe prior to the European industrial revolution; studies at specific localities may help resolve differences between anthropogenically-mediated changes and "natural" climatic changes. Results of various archaeological and palaeoecological archives across the Fertile Crescent indicates that rapid changes on landforms and biota have occurred since the beginnings of agriculture and urbanization. Work at key localities suggests that periods of imperialism such as the Neo-Assyrian ~9th century BCE are synchronous with sediment disturbances and deforestation in southeastern Turkey. New findings from geomorphic and archaeological survey and investigation in the Tigris watershed near Diyarbakir are correlated with various records across the broader region (e.g., Lake Van, Konya lakes, etc) in order to assess the spatial and temporal changes brought about by human population growth and increased exploitation of natural resources during phases of empire-building.

  6. El Águila Imperial Ibérica

    Directory of Open Access Journals (Sweden)

    M. Ferrer Baena

    2005-01-01

    Full Text Available El Á guila Imperial Ibérica es una de las aves más amenazadas de extinción del mundo. Actualmente, la población mundial de la especie está estimada en un poco más de 200 parejas. Todas ellas se encuentran en territorio peninsular español, en los bosques mediterráneos del cuadrante suroccidental, repartidas en una serie de subpoblaciones de pequeño tamaño (menos de 30 parejas con un nivel de intercambio medio‐bajo, estando algunas de ellas claramente aisladas. Este tipo de distribución es típicamente inestable y paso previo habitual de los procesos de extinción. Entre las principales amenazas a la especie se encuentran la disminución de las poblaciones de conejo, que constituye su principal presa, y la mortalidad por electrocución en tendidos eléctricos.

  7. Imperial power,gentry power and clan power: Western and Chinese cultural traditions in a comparative perspective

    Institute of Scientific and Technical Information of China (English)

    Wang Bing; Wang Dan

    2006-01-01

    The differences between China and Western countries in human and physical environment has brought about two distinctive models of state.In the Chinese-style state of quasi-consanguinity,in which family and state have a similar structure,imperial power,gentry power,and clan power are the product of common ownership of consanguineous groups.The similarity in the structures of these three kinds of power derives from the fact that they are all restricted by the power of lineage generated from the self-sufficient small farmer economy,and must obey the conventions of ancestors which hold the benefits of the group as supreme.The relationship between these three kinds of power,is definitely not the one that is based on the division of power that is founded on individual private ownership in Western countries.where'public power'and'individual private ownership'are antithetic.but are three aspects of the patriarchal dictatorship that complement each other.Therefore,village rule in China and autonomy in the West are two totally different concepts,and gentry power is also not the'authorized power'from the state.

  8. Analysis of the apiclutural industry in relation to geothermal development and agriculture in the Imperial Valley, Imperial County, California

    Energy Technology Data Exchange (ETDEWEB)

    Atkins, E.L.

    1979-04-01

    PART I: Continuous exposure to 30 ppB H/sub 2/S increased lifespan of caged worker honey bees, Apis mellifera L., 33%; whereas, bees exposed > 13 days to 100 ppB and 300 ppB H/sub 2/S the lifespan was shortened 32% and 51%, respectively, over unexposed bees; bees exposed > 15 days to a combination of 300 ppB H/sub 2/S + 50 ppM CO/sub 2/ the lifespan was shortened 4.4% more that 300 ppB H/sub 2/S alone. The mean temperature and/or relative humidity did not exert a direct effect on the hazard to bees. A continuous exposure to 300 ppB SO/sub 2/ was detrimental to caged worker honey bees; and, a mean temperature of 27.2/sup 0/C was 75.7% more toxic than the same dosage at 16.7/sup 0/C. Worker bee lifespans exposed to 300 ppB SO/sub 2/ at 16.7/sup 0/C were shortened 13.5% and 79%, respectively, compared to unexposed bees. Therefore, both dosage and temperature exert direct effects on the hazards to bees. PART II: The status of the apicultural industry in Imperial County, California, was outlined giving a short characterization of the area in relation to the apicultural industry. Agriculture utilizes 500,000 intensely farmed acres which generated a 11-year average income of $370 million. Over 40 agricultural commodities are produced. The apicultural industry is intimately involved in 25% of the total gross agricultural income. In addition, most of the flora growing in the desert community which comprises the remainder of the county are very important to honey bees by providing sustaining nectar and/or pollen for brood rearing. The bee foraged flora provides substantial bee forage when colonies are located outside of the agriculutral area. It is concluded that geothermal resource development in the Imperial Valley is contemplated to have minimal effects on the apicultural industry.

  9. Sistema radicular do fórmio, sisal e bambu imperial Root systems of new zealand flax, sisal, and imperial bamboo

    Directory of Open Access Journals (Sweden)

    Júlio César Medina

    1963-01-01

    Full Text Available Os autores apresentam e discutem os resultados de estudos preliminares sôbre o sistema radicular do fórmio (Phormium tenax Forster, sisal (Agave sisalana Perrine e bambu .imperial (Bambusa vulgaris Schrad. var. vittata A. ,& C, Riv.. Concluem, que o sistema radicular do fórmio é relativamente raso, o do sisal bastante superficial é o do bambu imperial se limitada às primeiras carnadas do solo.Results of preliminary studies on root-systems of New Zealand flax (Phormium tenax Forster, sisal (Agave sisalana Perrine, and imperial bamboo (Bambusa vulgaris Schrad. var. vittata A. & C. Riv. plants by the method of soil block, are apresented and discussed by the authors. According to local soil conditions, it is concluded that the root-system of New Zealand flax is relatively superficial, with the main concentration of roots in the 12 in. soil top layer. In sisal, the root-systems of the three plants investigated were found to occur in the soil surface layer, with more of 90% of the roots in the top 6 in. Finally, in the imperial bamboo clump atudied, the main concentration of roots was found in the layer 6-12 in. deep.

  10. Biogeochemical studies of wintering waterfowl in the Imperial and Sacramento Valleys

    Energy Technology Data Exchange (ETDEWEB)

    Koranda, J.J.; Stuart, M.; Thompson, S.; Conrado, C.

    1979-10-01

    Trace and major elemental composition were determined in the organs of wintering waterfowl in the Imperial and Sacramento Valleys of California, and in soils, sediments, and agricultural fertilizer that constitute the various sources of elements in the waterfowl. These data provide a biogeochemical baseline for waterfowl populations wintering in an area being developed for geothermal power. This baseline in the Imperial Valley is affected by soil and sediment composition, agricultural effluents in irrigation and stream water, and spent shot deposited by hunters in waterfowl habitats. The waterfowl acquire a set of trace elements from these sources and concentrations increase in their organs over the wintering period. Nickel, arsenic, selenium, bromine, and lead are the primary elements acquired from soil sources, agricultural effluents, and spent shot in the Imperial Valley. The assessment of effects from geothermal effluents on waterfowl populations in complex because there are large influxes of materials into the Imperial Valley ecosystem that contain trace elements, i.e., irrigation water, phosphatic fertilizers, pesticides, and lead shot. Multiple sources exist for many elements prominent in the expected geothermal effluents. The relationships between the two California valleys, the Imperial and Sacramento, are apparent in the trace element concentrations in the organs of waterfowl obtained in those two valleys. Arsenic is absent in the waterfowl organs obtained in the Sacramento Valley and relatively common in the Imperial Valley waterfowl. The effect of any release of geothermal effluent in the Imperial Valley waterfowl habitats will be difficult to describe because of the complexity of the biogeochemical baseline and the multiple sources of trace and major elements in the ecosystem.

  11. 北宋太学办学经费扩充探析%An Analysis on Imperial College Funds Expansion of the Northern Song Dynasty

    Institute of Scientific and Technical Information of China (English)

    罗玉霞; 喻本伐

    2012-01-01

      As one of the main forms of higher education in ancient China. The Imperial College of the Northern Song Dynasty is outstanding. even taking the first place in the Chinese educational history. The successful handling of the Northern Song Dynasty Imperial College is insepara-ble to the sufficient provision ,which source of funds comes from two main channels:one is government funding;the other independent financing. the main subdivision consists of learning field rent,given money, house rent ,sale income of printing books, interest rate, minister money, folk dona-tion. Because of its funding source is wider, and allowing for independent financing, so the Northern Song Dynasty Imperial College can be healthy managed.%  太学是中国古代高等教育的主要形式之一。北宋太学在中国教育史上出类拔萃,乃至独占鳌头。北宋太学的成功办理,与其经费供应的相对充足是密不可分的。其经费来源,主要有两个渠道:一是政府拨款;二是太学自主筹措。若细分,计有赡学钱、赐钱、学田租、房租屋课、光监钱、刊印经籍销售款、公使钱、息钱、民间捐资等。正因为其来源较广,并允许自主筹措,故使北宋太学得以健康办理。

  12. Evolution process of the Late Silurian–Late Devonian tectonic environment in Qimantagh in the western portion of east Kunlun, China: Evidence from the geochronology and geochemistry of granitoids

    Indian Academy of Sciences (India)

    Nana Hao; Wanming Yuan; Aikui Zhang; Yunlei Feng; Jianhui Cao; Xiaoning Chen; Xueqin Cheng; Xuanxue Mo

    2015-02-01

    The East Kunlun Orogenic Belt has undergone a composite orogenic process consisting of multiple orogenic cycles and involving many types of magmatic rocks spread over the whole district. However, due to bad natural geographical conditions and complex superimposed orogenic processes, most of the Caledonian orogenic traces were modified by the late tectonic uplift and denudation, so these rocks are poorly studied. Multiperiodic magmatic activity during the Late Silurian (approximately 420 Ma)–Late Devonian (approximately 380 Ma) exists in the Qimantagh area. We obtained 5 zircon U–Pb ages from the Late Silurian–Late Devonian granitoids in the Qimantagh area. Those ages are 420.6 ± 2.6 Ma(Nalingguole biotite monzogranite), 421.2 ± 1.9 Ma (Wulanwuzhuer potassium granite), 403.7 ± 2.9 Ma (Yemaquan granodiorite), 391.3 ± 3.2 Ma (Qunli granite porphyry), and 380.52 ± 0.92 Ma (Kayakedengtage granodiorite). These granitoids belong to the sub-alkaline, high-K calc-alkaline, metaluminous or weakly or strongly peraluminous series. The rocks are right oblique types, having overall relative LREE enrichment and HREE depletion, though rocks from different times may exhibit different degrees of Eu anomalies or overall moderate Eu depletion. The rocks are rich in large ion lithophile elements (LILE), such as Rb, Th, and K, and high field strength elements (HFSE), such as Zr and Hf, and are depleted in Ba, Nb, Ta, Sr, P, Eu, and Ti. The rocks have complex composition sources. The Late Silurian granitoids are mainly crust-derived. Most of the Devonian granitoids are crust-mantle mixed-source and only some parts of them are crust-derived, especially the Middle Devonian granitoids. Those mid-acidic and acidic intrusive rocks are formed in a post-collision tectonic setting, lithosphere delamination may have occurred in the Early Devonian (407 Ma), and the study area subsequently experienced an underplating of the mantle-derived magma at least until the Late Devonian (380 Ma).

  13. Imperial Parallels: Analyzing the U.S. Army Regionally Aligned Force Strategy in the Context of Historical Imperialism

    Science.gov (United States)

    2014-06-13

    military power, the corruption of public responsibility by private interests, the blatant ethnocentric and egotistic outlook of most Americans. A...article entitled “Special Report: China Storms Africa.” In it he provides a startling analysis of the rate at which China is virtually consuming

  14. The Shangzhuang Fe-Ti oxide-bearing layered mafic intrusion, northeast of Beijing (North China): Implications for the mantle source of the giant Late Mesozoic magmatic event in the North China Craton

    Science.gov (United States)

    Liu, Ping-Ping; Zhou, Mei-Fu; Yan, Dan-Ping; Zhao, Guo-Chun; Su, Shang-Guo; Wang, Xiao-Lin

    2015-08-01

    The Early Cretaceous Shangzhuang Fe-Ti oxide-bearing layered mafic intrusion in the Yanshan Belt northeast of Beijing is coeval with the giant Late Mesozoic igneous province in the eastern part of the North China Craton (NCC). This magmatic event was associated with lithospheric thinning and thus the igneous rocks have been used to characterize the nature of the Mesozoic mantle beneath the NCC. The Shangzhuang mafic pluton intruded a large granodioritic complex and crystallized at ~ 850-872°C at a depth of 13-14 km. It is composed, from the base upward, of troctolite, Fe-Ti oxide-bearing gabbronorite and gabbro. Rocks from this intrusion have low initial 87Sr/86Sr ratios (0.7053-0.7058), negative initial εNd values (- 9.4 to - 10.7), highly differentiated LREE and nearly flat HREE patterns indicative of an EMI-like mantle source unaffected by upper crustal contamination. The occurrence of Fe-Ti oxide ore layers, magnetite-ilmenite exsolution lamellae in hornblende and high TiO2 contents of the silicate rocks indicate that they formed from Fe- and Ti-rich ferrobasaltic magmas, which may have been generated by addition of magmas from a deeper mantle source. The presence of orthopyroxene, high-Mg ilmenite (up to 8.5 wt %), hornblende, biotite and high oxygen fugacities calculated from coexisting titanomagnetite-ilmenite pairs can be explained by derivation from an enriched EMI-type mantle modified by fluids from a subducted slab and mixed with asthenospheric or deeper-mantle materials in an extensional setting. Exposure of the complex occurred during large-scale uplift (at least 13 km) and exhumation of the Yanshan orogenic belt in the Early Cretaceous. Chemical metasomatism triggered by water and enhanced by heat from a deep magma source may have played an important role in removing the ancient cratonic root, generating partial melting of the lithospheric mantle and producing coeval magmatic activity in the Mesozoic eastern NCC.

  15. Phylogeny and biogeography of the imperial pigeons (Aves: Columbidae) in the Pacific Ocean.

    Science.gov (United States)

    Cibois, Alice; Thibault, Jean-Claude; Bonillo, Céline; Filardi, Christopher E; Pasquet, Eric

    2017-05-01

    We reconstruct the phylogeny of imperial pigeons (genus Ducula) using mitochondrial and nuclear sequence data. We evaluate the most likely biogeographic scenario for the evolution of this group that colonized many islands of the Pacific Ocean. The divergence time analysis suggests that the basal divergences within Ducula occurred more recently than in the fruit doves (genus Ptilinopus), a group that is also well diversified in Oceania. The imperial pigeons colonized the Melanesian region several times independently, and the diversification within this region led to several species in sympatry, in particular in the Bismarck archipelago. Central Polynesia was also colonized several times, first by a lineage during the Miocene that led to the large D. latrans, sister to the New Caledonian endemic D. goliath, then more recently by the widespread D. pacifica, during the Pleistocene. The phylogenetic pattern obtained with the extant Ducula species showed that the Eastern Polynesian endemics do not form a monophyletic group, with the Pacific Imperial Pigeon D. pacifica sister species with good support to the Polynesian Imperial Pigeon D. aurorae. However, the impact of recent anthropic extinctions has been important for the imperial pigeons, more than for the smaller fruit doves, suggesting that several Ducula lineages might be missing today. Copyright © 2017 Elsevier Inc. All rights reserved.

  16. Herman Merivale’s black legend: rethinking the intellectual history of free trade imperialism

    Directory of Open Access Journals (Sweden)

    Daniel Rood

    2008-12-01

    Full Text Available Focusses on the lectures and theories of economist and colonial bureaucrat Herman Merivale on the imperial transition of British colonialism from slave labour to free labour, and toward free trade, in 1839. Author specifically shows how Merivale propagated the free trade imperialism of the reformed British Empire by using the "Black Legend" way of thinking, i.e. criticizing Spanish colonialism, to caricaturize the second British Empire, and thus justify imperial policy reforms. Author elaborates on this Black Legend tradition, going back to writings of Las Casas, and how it served as justification for "better" imperialisms of other colonial powers than Spain, and how Merivale's views followed this tradition. He shows how Merivale as part of this criticized the mismanagement, slavery, brutality, mercantilism, and the concentration of power and wealth in Cuba and other Spanish colonies, as negative examples contrasted to the British approach. Author points out, however, how Merivale's views were in part paradoxical and ambiguous, as he favoured a social hierarchy and an imperial authoritarianism limiting free labour.

  17. Science Applied for the Investigation of Imperial Gate from Eighteenth Century Wooden Church of Nicula Monastery

    Directory of Open Access Journals (Sweden)

    I. Bratu

    2017-01-01

    Full Text Available Part of an indestructible component of any orthodox church, the Imperial Gates represent an important symbol in our cultural heritage. But in many cases the Imperial Gates from the wooden churches were damaged. In order to preserve and restore them, the scientific investigations of the Imperial Gate belonging to Nicula Monastery wooden church were performed by employing nondestructive and destructive methods. The wood essence was established, with its “health” status being investigated by FTIR (Fourier Transform Infrared spectroscopy and DSC (Differential Scanning Calorimetry thermal analysis. The painting materials employed by popular artists were determined by FTIR and XRF (X-ray fluorescence spectroscopy as gypsum, calcite (rear background, lead white (Archangel Clothes, lead-minium (Archangel Clothes, leaf, iron oxide (Imperial Gate frame, malachite (green, Prussian blue (blue, orpiment (yellow, aliphatic, ester, and protein (probably egg yolk degradation products. Using similar colors as in the original artwork (resulting from the scientific investigation of the pigments a 3D reconstruction has been performed. The restored Imperial Gates are placed in the old Nicula wooden church, being included into a tourist and religious circuit.

  18. Imperial County geothermal development. Quarterly report, April 1, 1980-June 30, 1981

    Energy Technology Data Exchange (ETDEWEB)

    1981-01-01

    Three areas are reported: Geothermal Administration, Geothermal Planning; and other Geothermal Activities. Geothermal Administration addresses the status of the Imperial Valley Environmental Project (IVEP) transfer, update of the Geothermal Resource Center, and findings of Geothermal field inspections. Field inspections will cover the four new wells drilled by Magma at the Salton Sea in preparation for 28 MW power plant, the progress at Sperry at East Mesa, and the two on-line power plants in East Mesa and North Brawley. Evaluation of cooperative efforts will cover the Geothermal Subsidence Detection Network Resurvey, Master EIR for the Salton Sea and the Annual Imperial County Geothermal meeting. The status of Geothermal development throughout the County will cover existing proposed facilities. The summary of the Geothermal meeting (Appendix A) will also provide the status of several projects. Geothermal Planning addresses the EIR Notice of Exemption from CEQA, progress on the Master EIR for the Salton Sea, and the EIR for Phillips Petroleum for 6 exploratory wells in the Truckhaven area. Other Geothermal Activity addresses the Department of Energy Region IX meeting hosted by Imperial County, the Annual Imperial County Geothermal meeting, Class II-1 geothermal hazardous waste disposal siting study, and Imperial County Geothermal Direct Heat Study.

  19. [The history of smallpox vaccination in the Imperial Moscow foster house].

    Science.gov (United States)

    Sher, S A

    2011-01-01

    The article deals with the history of vaccination against natural smallpox which is directly connected to the Imperial Moscow foster house which became one of smallpox vaccination centers in Russia of XIX century. In 1801, when variolations were substituted by more safe cowpox vaccinations, in Russia the first vaccination using the method of Jenner was made exactly in in the Imperial Moscow foster house. From 1805, the smallpox vaccination received the status of force of law, the Imperial Moscow foster house began to produce and to distribute the smallpox vaccine all over the country and apply the smallpox vaccination not only to its foster children but to all turned to and, besides that, to train the smallpox vaccination. In 1857, the Imperial Moscow foster house became the first establishment in Russia where the revaccination was applied. In 1980, the WHO proclaimed that the implementation of the global program of smallpox irradiation resulted in the natural smallpox elimination on Earth. The smallpox became the first communicable disease defeated due to mass vaccination. One third of Earth population was vaccinated by the Soviet vaccine, which originated mainly because of the activities of physicians of the Imperial Moscow foster house.

  20. The imperial image of the new world order: Is this political realism?

    Directory of Open Access Journals (Sweden)

    Vicente Palacio de Oteyza

    2003-12-01

    Full Text Available This article analyses the different images of the world order belonging to the realist theory of international relations, and their relationship to the neo-conservative doctrines of the American imperial order. It deals with answering the question of whether or notthe current Republican administration’s unipolar-imperial image of the world order can be considered a form of political realism. Both the defenders of the unipolar-imperial order and its detractors often ascribe this image to the tradition of realism, where two other images subsequent to the end of the Cold War can be placed: the geo-economic and multipolar images. However, an analysis of the different images reveals that the neoconservative doctrines of the new imperial order depart considerably from realism at the descriptive, prescriptive and predictive levels, to the point where they become incompatible with it. This study concludes that the imperial image is an anomaly not only with respect to political realism but also with respect to the unipolar image itself.

  1. A westward propagating slab tear model for Late Triassic Qinling Orogenic Belt geodynamic evolution: Insights from the petrogenesis of the Caoping and Shahewan intrusions, central China

    Science.gov (United States)

    Hu, Fangyang; Liu, Shuwen; Zhang, Wanyi; Deng, Zhengbin; Chen, Xu

    2016-10-01

    Late Triassic granitoid intrusions are widespread in the South Qinling Belt (SQB), providing excellent subjects to understand the geodynamic evolution of the Qinling Orogenic Belt and the collision between the North China Craton (NCC) and Yangtze Craton (YZC). This study shows newly obtained geological, geochemical and zircon U-Pb-Hf isotopic data of the Caoping and Shahewan intrusions, revealing that the Caoping intrusion consists of ~ 215 Ma fined-grained granites, and ~ 221-215 Ma porphyritic and coarse to medium-grained tonalites, granodiorites and monzogranites, which assemble with coeval mafic magmatic enclaves (MMEs). The Shahewan intrusion is composed of ~ 215-210 Ma porphyritic granodiorites and monzogranites, which also assemble with coeval MMEs. The fine-grained granites from the Caoping intrusion are characterized by high SiO2, Rb and (La/Yb)N ratio, but low MgO, CaO and Sc contents, with εHf(t) values of - 8.6 to + 4.3 and TDM2(Hf) ages of 883-1596 Ma, suggesting that they are mainly derived from partial melting of the Meso- to Neoproterozoic metagreywackes. The porphyritic and coarse to medium-grained granitoid rocks from both Caoping and Shahewan intrusions are characterized by higher MgO, CaO, Sc, Mg# values, but low SiO2, Rb contents and (La/Yb)N ratio, with εHf(t) values of - 0.7 to + 2.8 and TDM2(Hf) values of 961-1158 Ma, suggesting that they are mainly formed by magma mixing between melts that were derived from Meso- to Neoproterozoic basement rocks of the SQB and metasomatized lithospheric mantle. The MMEs from Caoping and Shahewan intrusions are characterized by low SiO2, Sr/Y ratio, high MgO, K2O, Rb, Sc, total REE contents, with εHf(t) values of + 0.5 to + 6.1 and TDM(Hf) values of 661-846 Ma, suggesting that they are produced by partial melting of metasomatized lithospheric mantle. The rapakivi-like textures of the rocks from Shahewan intrusion may be caused by continued underplating and injection of mafic magma resulting in higher

  2. Neoliberalismo: neo-imperialismo Neoliberalism: neo-imperialism

    Directory of Open Access Journals (Sweden)

    Gérard Duménil

    2007-04-01

    Full Text Available O neoliberalismo é uma nova fase do capitalismo, que se impôs a partir do começo dos anos 1980. Considerando seus traços mais gerais nos países do Centro, como nos Estados Unidos e na Europa, destacam-se três características: uma dinâmica mais favorável da mudança tecnológica e da rentabilidade, a criação de rendas a favor das classes mais abastadas, e a redução da taxa de acumulação. O imperialismo na era neoliberal pode se caracterizar pela hegemonia dos Estados Unidos, que drenam fluxos enormes de renda do resto do mundo. Mas esse domínio é solapado pelos desequilíbrios externos crescentes do país, a expressão de uma onda extraordinária de consumo por parte das famílias.Neoliberalism is a new phase of capitalism which was asserted at the beginning of the 1980s. Considering its more general features as in the United States and Europe, it can be characterized by: a more favorable dynamic of technical change and profitability, the creation of income flows to the benefit of the most accommodated classes of the population, and diminished rates of accumulation. A central feature of imperialism in the neoliberal era is U.S. hegemony, a country which is draining huge flows of income from the rest of the world. This domination is, however, undermined by increasing external disequilibria, the expression of an extraordinary wave of consumption from households.

  3. Characterization of elements in trace amounts in imperial topaz through neutron activation analysis; Caracterizacao de elementos em teores de traco em topazio imperial atraves da analise por ativacao neutronica

    Energy Technology Data Exchange (ETDEWEB)

    Oliveira, Ester Figueiredo de [Centro de Desenvolvimento da Tecnologia Nuclear (CDTN), Belo Horizonte, MG (Brazil); Sabioni, Antonio C. S. [Ouro Preto Univ., MG (Brazil). Dept de Fisica; Ferreira, Cesar M. [Ouro Preto Univ., MG (Brazil). Dept de Geologia

    2000-07-01

    This work deals with the mineral characterization of the elements in trace amounts of imperial topaz, original form Mina Capao da Lama, Ouro Preto, MG, Brazil, through the neutron activation analysis. Recent results have permitted to quantify Cr, Cs, Mn, Na, Ga, Sb and Au. The main goal of this study is the contribution to the mineral and gemological research of the imperial topaz.

  4. De la res publica al Imperium: Poder y subjetividad en la Roma Imperial

    Directory of Open Access Journals (Sweden)

    Juan Carlos Barrassús Herrero

    2013-05-01

    Full Text Available Este artículo pretende caracterizar la forma de poder imperial romano y las formas de subjetividad que aparecen tras la irrupción de un poder absoluto e irresistible propio del Principado. Trataremos de identificar los elementos de continuidad y discontinuidad que se dan en el ámbito del pensamiento político y de la subjetividad en el período republicano así como en el imperial. Los textos claves para comprender tal paso se encuentran tanto en los escritos de los últimos republicanos ‘convencidos’ así como en una literatura política de la primera época imperial que mira al pasado republicano con nostalgia y veneración, al tiempo que trata de ajustar cuentas con el presente mediante la narración de su corrupción

  5. Cooperative geochemical investigation of geothermal resources in the Imperial Valley and Yuma areas. Final report

    Energy Technology Data Exchange (ETDEWEB)

    Coplen, T.B.

    1973-10-01

    Preliminary studies indicate that the Imperial Valley has a large geothermal potential. In order to delineate additional geothermal systems a chemical and isotopic investigation of samples from water wells, springs, and geothermal wells in the Imperial Valley and Yuma areas was conducted. Na, K, and Ca concentrations of nearly 200 well water, spring water, hot spring, and geothermal fluid samples from the Imperial Valley area were measured by atomic absorption spectrophotometry. Fournier and Truesdell's function was determined for each water sample. Suspected geothermal areas are identified. Hydrogen and oxygen isotope abundances were determined in order to determine and to identify the source of the water in the Mesa geothermal system. (JGB)

  6. 78 FR 37845 - Meeting of the Imperial Sand Dunes Recreation Area (ISDRA) Subgroup of the California Desert...

    Science.gov (United States)

    2013-06-24

    ... From the Federal Register Online via the Government Publishing Office DEPARTMENT OF THE INTERIOR Bureau of Land Management Meeting of the Imperial Sand Dunes Recreation Area (ISDRA) Subgroup of the... 92-463 and 94-579, that the Imperial Sand Dunes Recreation Area Subgroup of the California...

  7. 78 FR 4981 - Pacific Imperial Railroad, Inc.-Change in Operator Exemption-Rail Line of San Diego and Arizona...

    Science.gov (United States)

    2013-01-23

    ... San Diego and Arizona Eastern Railway Company Pacific Imperial Railroad, Inc. (PIR), a noncarrier, has filed a verified notice of exemption under 49 CFR 1150.31 to change operators from San Diego & Imperial... Diego and Arizona Eastern Railway Company (SD&AE). The change in operators for the line is being...

  8. A Closer Look at China-Iran Relations, Roundtable Report. Revision 1

    Science.gov (United States)

    2010-09-01

    the Ming Dynasty . The strongest symbol of this was the multiple visits to Persia by the Chinese imperial fleet during the famous voyages commanded...by eunuch admiral Zheng He.’ One participant noted that later in the Ming dynasty , China ended its maritime presence virtually overnight, and with...participant argued that China is signing deals with Iran with a larger regional security strategy in mind, and cited a 2000 article by Tang Shiping in China’s

  9. Description of Imperial Valley, California for the assessment of impacts of geothermal energy development

    Energy Technology Data Exchange (ETDEWEB)

    Layton, D.; Ermak, D.

    1976-08-26

    Impending geothermal development in the Imperial Valley of California has raised concern over the possible impacts of such development. As an initial step in impact assessment of geothermal projects, relevant features of the valley's physical and human environments are described. Particular attention is placed on features that may either influence development or be affected by it. Major areas of consideration include the valley's physical resources (i.e., land, air, water, and biological resources), economic, fiscal, and social characteristics of Imperial County, and geothermal laws.

  10. COZINHEIRO IMPERIAL - Ou a nova arte do cozimento e do copeiro em todos os seus ramos

    Directory of Open Access Journals (Sweden)

    Daniela Pereira de Vargas

    2011-12-01

    Full Text Available Resumo: O Cozinheiro Imperial Ou Nova Arte Do Cozinheiro E Do Copeiro Em Todos Os Seus Ramos é uma referencia tanto na culinária como na bibliografia brasileira, por tratar-se do primeiro livro de receitas editado no Brasil. De autor anônimo, foi reeditado em 1996 pela Best Seller. A Universidade de São Paulo digitalizou os originais, que hoje são parte de sua Coleção Brasiliana. Pela importância cultural do material, ele é destacado nesta edição de RRV. Palavras chave: Gastronomia. Cultura Brasileira. Cozinheiro Imperial

  11. Extension activities of Kazan Imperial University in the 19th century

    Directory of Open Access Journals (Sweden)

    Zhuravleva Evgenia

    2017-01-01

    Full Text Available Based primarily on archival documents, this article explores the development of additional education in Kazan province, Russia, in the 19th century. Its genesis is found in the varying order of Kazan Imperial University extension activities which take the form of foreign academic and scientific mobility; individual mentoring practice of recognised scholars; masters’ advancement at Pedagogical Institute; creation of the Pedagogical Society in the framework of University Extension Movement. The historiography shows that in the course of its development additional education in Kazan Imperial University largely relied on the international experience and enthusiasm of its teaching staff.

  12. Geotechnical environmental aspects of geothermal power generation at Herber, Imperial Valley, California

    Energy Technology Data Exchange (ETDEWEB)

    1976-10-01

    The feasibility of constructing a 25-50 MWe geothermal power plant using low salinity hydrothermal fluid as the energy source was assessed. Here, the geotechnical aspects of geothermal power generation and their relationship to environmental impacts in the Imperial Valley of California were investigated. Geology, geophysics, hydrogeology, seismicity and subsidence are discussed in terms of the availability of data, state-of-the-art analytical techniques, historical and technical background and interpretation of current data. Estimates of the impact of these geotechnical factors on the environment in the Imperial Valley, if geothermal development proceeds, are discussed.

  13. Late Paleozoic tectonics of the Solonker Zone in the Wuliji area, Inner Mongolia, China: Insights from stratigraphic sequence, chronology, and sandstone geochemistry

    Science.gov (United States)

    Shi, Guanzhong; Song, Guangzeng; Wang, Hua; Huang, Chuanyan; Zhang, Lidong; Tang, Jianrong

    2016-09-01

    The geology in the Wuliji area (including the Enger Us and Quagan Qulu areas) is important for understanding the Late Paleozoic tectonics of the Solonker Zone. Ultramafic/mafic rocks in the Enger Us area, previously interpreted as an ophiolitic suture, are actually lava flows and sills in a Permian turbiditic sequence and a small body of fault breccia containing serpentinite. Subduction zone features, such as accretionary complexes, magmatic arc volcanics or LP/HP metamorphism are absent. Early Permian N-MORB mafic rocks and Late Permian radiolarian cherts accompanied by turbidites and tuffeous rocks indicate a deep water setting. In the Quagan Qulu area, outcrops of the Late Carboniferous to Permian Amushan Formation are composed of volcano-sedimenary rocks and guyot-like reef limestone along with a Late Permian volcano-sedimentary unit. A dacite lava in the Late Permian volcano-sedimentary unit yields a zircon U-Pb age of 254 Ma. The gabbros in the Quagan Qulu area are intruded into the Amushan Formation and caused contact metamorphism of country rocks. Sandstones in the Upper Member of the Amushan Formation contain detrital clasts of volcanic fragments and mineral clasts of crystalline basement rocks (i.e. biotite, muscovite and garnet). Geochemical analysis of volcaniclastic sandstones shows a magmatic affinity to both continental island arc (CIA) and active continental margin (ACM) tectonic settings. A Late Permian incipient rift setting is suggested by analyzing the lithostratigraphic sequence and related magmatism in the Wuliji area. The volcano-sedimentary rocks in the Wuliji area experienced a nearly N-S shortening that was probably related to the Early Mesozoic nearly N-S compression well developed in other areas close to the Wuliji area.

  14. 长白山现代理论雪线和古雪线高度%Present and Late Pleistocene equilibrium line altitudes in Changbai Mountains, Northeast China

    Institute of Scientific and Technical Information of China (English)

    张威; 崔之久; 闫玲

    2009-01-01

    According to the glacial landforms and deposits with the optically stimulated lumi nescence (OSL) dating results, two glacial stages of the last glacial cycle (LGC) and Late Glacial were identified. The Late Glacial stage (Meteorological Station glacier advance) tool place about 11 ka (11.3±1.2 ka), and the last glacial maximum (LGM), named Black Wind Mouth glacier advance, occurred at 20 ka (20.0±2.1 ka). Based on the Ohmura's formula in which there is a relationship between summer (JJA) atmospheric temperature (T) and the annual precipitation (P) at ELA, the present theoretical equilibrium line altitude (ELAt) in Changbai Mountains was 3380+100 m. Six methods of accumulation-area ratio (AAR) maximum elevation of lateral moraines (MELM), toe-to headwall altitude ratios (THAR), the terminal to summit altitudinal (TSAM), the altitude of cirque floor (CF), and the terminal to average elevation of the catchment area (Hofer) were used for calculation of the former ELAs in different stages. These methods provided the ELA for a range of 2250-2383 m with an average value of 2320±20 m during the LGM, which is 200 m higher than the value of previ- ous investigation. The snowlines during the Late Glacial are 2490 m on northern slope, and 2440 m on western slope. The results show that the snowline on northern slope is 50 m higher than that on western slope during the Late Glacial, and the average snowline is 2465m. The △ELA values were more than 1000 m during the LGM, and about 920 m lower than now during the Late Glacial stage respectively. Compared with Taiwanese and Japanese moun- tains in East Asia during the LGM, the effect of the uplift on EI_A in Changbai Mountains dur- ing the glaciations (i.e. 20 m uplift in the LGM and 11 m in the Late Glacial) is not obvious.

  15. Entre o altar e o trono: iniciativas de escolarização na capital imperial - Between the altar and throne: initiatives of schooling in imperial capital

    Directory of Open Access Journals (Sweden)

    Aline de Morais Limeira

    2012-08-01

    Full Text Available Ao reconhecer que a produção da forma escolar moderna se efetivou por intermediações de forças distintas, investigamos iniciativas particulares de educação promovidas pela Igreja Católica. A partir das propagandas do Almanak Laemmert e de diversas informações do jornal O Apóstolo, foi possível localizar vestígios acerca da estrutura física, planos de estudos e valores propostos por alguns colégios particulares na Corte Imperial. O recorte cronológico abrange as décadas de 1870 e 1880, que compreendem a época da reforma Leôncio de Carvalho (1879. Também procuramos refletir acerca das relações estabelecidas entre o Estado Imperial e a Igreja Católica, e observar imbricações entre poderes públicos e privados, fenômeno que ultrapassa a sociedade oitocentista.Palavras-chave: ensino primário, colégios religiosos, Corte Imperial. BETWEEN THE ALTAR AND THRONE: INITIATIVES OF SCHOOLING IN IMPERIAL CAPITALAbstractRecognizing that adherence to the way modern school was made by different forces, we investigate private education initiatives promoted by the Catholic Church in the Imperial Court. From the advertisements that circulated Almanak Laemmert and O Apóstolo the newspaper was unable to locate information about the physical structure, curricula and amounts charged for those colleges. Establishing the chronological cut the 1870s and 1880s, which comprise the time of Reformation Leôncio de Carvalho (1879, we also reflect on the relationships established between the Imperial State and the Catholic Church an expression of the imbrications of public and private, a brandsociety in the nineteenth century.Key-words: primary education, religious colleges, the Imperial Court. ENTRE EL ALTAR Y EL TRONO: INICIATIVAS INSTRUCCIÓN EN IMPERIAL CAPITALResumenReconociendo que la construcción de forma de la escuela moderna fue dado por el área de fuerzas distintas, investigar iniciativas privadas de educación promovidos por la Iglesia

  16. 清末日本对华新闻活动考察%An Investigation on Japanese Journalism in China during the Late Qing Dynasty

    Institute of Scientific and Technical Information of China (English)

    刘爱君; 姜明

    2013-01-01

    A lot of newspapers were published by Japanese in China from the end of the 19th century to the first half of the 20th century. Before the Russo-Japanese War (1904-1905), early Japanese newspapers published in China, to a certain extent, showed sympathy for Chinese revolution and propagated on reform, which were favored by the Chinese progressive intellectuals. After the Russo-Japanese War, with the Japanese military expansion in China, most of these newspapers changed their attitude to protect Japan’s interests in China, cultivated pro-Japanese forces and focused on the expansion of the Japanese national sovereignty, becoming a tool of the Japanese government to propagate its colonial control policy. The study of the Chinese newspapers published by Japanese in China and on the essence of Japanese journalism within China in early times is one of the most important researches of Japanese aggression in journalism in China.%19世纪末至20世纪上半叶,日本在中国创办了大量报刊。以日俄战争为界,早期报刊在一定程度上同情中国革命,宣传维新改革,创办初期受到中国进步知识分子的欢迎;日俄战争后,伴随着日本对华军事扩张,大多数报纸以维护日本的在华利益,培植亲日势力,扩张日本国权为目的,成为日本政府宣传其大陆政策的御用报纸。考察清末日本在华创办的中文报刊,探讨日本早期对华新闻活动的实质,是日本侵华新闻史研究的重要课题之一。

  17. 新疆东北部晚侏罗世一新的柱齿兽%A NEW LATE JURASSIC DOCODONT (MAMMALIA) FROM NORTHEASTERN XINJIANG,CHINA

    Institute of Scientific and Technical Information of China (English)

    胡耀明; 孟津; 詹姆斯 M.克拉克

    2007-01-01

    A new genus and species of docodontid(Docodonta,Mammalia),Acuodulodon sunae,represented by a partial left lower jaw and dentition,is described.It is from the upper part of the Shishugou Formation in the Wucaiwan area of the Junggar Basin in northeastern Xinjiang,China,with an estimated age of 159~161 Ma(Oxfordian,early Late Jurassic).The new mammal is typical of docodonts in having a cusp b in front of cusp a,a cusp c distolingual to cusp a and a cusp g mesiolingual to cusp a on lower molariforms.Differing from other docodonts,it has no cusp e or crest b-e developed on lower molariforms.Unique among docodonts.cusps a and c of the new animal maintained their sharpness while cusp g and crest b-g wore away fast,indicating that both shearing and crushing/grinding occurred in the chewing cycle and probably last for most of the life span of the animal.Phylogenetic analysis of a data matrix with 24 lower molariform characters across 15 taxa recovers a monophyletic Docodonta,which has distinct diagnostic characters in lower molariforms.Within docodonts,Docodon and Borealestes are successively basal to other docodonts;Acuodulodon and Itatodon +(Simpsonodon,Castorocauda+(Tegotherium+Sibirotherium))form a monophyletic clade.Tegotheriid genera are nested within Docodontidae,but a monophyletic tegotheriid clade composed of Tegotherium,Sibirotherium,hatodon,and Tashkumyrodon is not recovered.The dentary of Acuodulodon is typical of docodonts.It has a shallow postdentary trough and a wide and sharp medial ridge,both of which do not extend onto the medial side of the condylar peduncle,indicating looser contact between postdentary bones and the dentary than in morganucodontids,a more derived condition in the evolution toward the definitive mammalian middle ear.%描述了哺乳纲柱齿兽目柱齿兽科(Docodontidae,Docodonta,Mammalia)一新属种--孙氏尖钝齿兽(Acuodulodon sunae gen.et sp.nov.).标本产于新疆东北部准噶尔盆地五彩湾地区上侏罗

  18. Late Carboniferous to early Permian sedimentary–tectonic evolution of the north of Alxa, Inner Mongolia, China: Evidence from the Amushan Formation

    Directory of Open Access Journals (Sweden)

    Haiquan Yin

    2016-09-01

    Full Text Available The late Paleozoic evolution of the Wulijishanhen (WSH-Shangdan (SD area near to the Chaganchulu Ophiolite belt is reinterpreted. Analysis of the upper Carboniferous to lower Permian sedimentary sequence, biological associations, detrital materials, sandstone geochemistry and volcanic rocks indicates that the SD area was an epicontinental sea and rift during the late Paleozoic rather than a large-scale ocean undergoing spreading and closure. This study reveals that the actual evolution of the study area is from the late Carboniferous to the early Permian. The fusulinids Triticites sp. and Pseudoschwagerina sp. in the limestones demonstrate that the Amushan Formation develops during the late Carboniferous to the early Permian. The limestones at the base of the SD section indicate that it is a stable carbonate platform environment, the volcanic rocks in the middle of the sequence support a rift tectonic background, and the overlying conglomerates and sandstones are characteristic of an epicontinental sea or marine molasse setting. The rift volcanism made the differences in the fossil content of the SD and WSH sections and led to two sections expose different levels within the Amushan Formation and different process of tectonic evolution. Moreover, the geochemical characteristics and detrital materials of the sandstones show that the provenance and formation of the sandstones were related to the setting of active continental margin. The quartz-feldspar-lithic fragments distribution diagram indicates that the material source for the sandstones was a recycled orogenic belt. Thus, the source area of the sandstones may have been an active continental margin before the late Carboniferous–early Permian. The characteristics of the regional tectonic evolution of the area indicate that the region may form a small part of the Gobi–Tianshan rift of southern Mongolia.

  19. Late Carboniferous to early Permian sedimentaryetectonic evolution of the north of Alxa, Inner Mongolia, China:Evidence from the Amushan Formation

    Institute of Scientific and Technical Information of China (English)

    Haiquan Yin; Hongrui Zhou; Weijie Zhang; Xiaoming Zheng; Shengyu Wang

    2016-01-01

    The late Paleozoic evolution of the Wulijishanhen (WSH)-Shangdan (SD) area near to the Chaganchulu Ophiolite belt is reinterpreted. Analysis of the upper Carboniferous to lower Permian sedimentary sequence, biological associations, detrital materials, sandstone geochemistry and volcanic rocks indicates that the SD area was an epicontinental sea and rift during the late Paleozoic rather than a large-scale ocean undergoing spreading and closure. This study reveals that the actual evolution of the study area is from the late Carboniferous to the early Permian. The fusulinids Triticites sp. and Pseudoschwagerina sp. in the limestones demonstrate that the Amushan Formation develops during the late Carboniferous to the early Permian. The limestones at the base of the SD section indicate that it is a stable carbonate platform environment, the volcanic rocks in the middle of the sequence support a rift tectonic back-ground, and the overlying conglomerates and sandstones are characteristic of an epicontinental sea or marine molasse setting. The rift volcanism made the differences in the fossil content of the SD and WSH sections and led to two sections expose different levels within the Amushan Formation and different process of tectonic evolution. Moreover, the geochemical characteristics and detrital materials of the sandstones show that the provenance and formation of the sandstones were related to the setting of active continental margin. The quartz-feldspar-lithic fragments distribution diagram indicates that the material source for the sandstones was a recycled orogenic belt. Thus, the source area of the sandstones may have been an active continental margin before the late Carboniferouseearly Permian. The charac-teristics of the regional tectonic evolution of the area indicate that the region may form a small part of the GobieTianshan rift of southern Mongolia.

  20. Trap catches of the sweetpotato whitefly (Homoptera: Aleyrodidae) in the Imperial Valley, California, from 1996 to 2002

    Institute of Scientific and Technical Information of China (English)

    CHANG-CHI CHU; EDWARD BARNES; ERIC T. NATWICK; TIAN-YE CHEN; DAVID RITTER; THOMAS J. HENNEBERRY

    2007-01-01

    An outbreak of the sweetpotato whitefly, Bemisia tabaci (Gennadius), biotype B occurred in the Imperial Valley, California in 1991. The insects destroyed melon crops and seriously damaged other vegetables, ornamentals and row crops. As a result of the need for sampling technology, we developed a whitefly trap (named the CC trap) that could be left in the field for extended time periods. We used the traps to monitor populations of B. tabaci adults during year-round samplings from 1996 to 2002 to study variations in the weekly trap catches of the insect. The greatest number of B. tabaci adults was recorded in 1996, followed by a continuing annual decrease in trap catches each year through 2002. The overall decline of B. tabaci is attributed in part to the adoption of an integrated pest management (IPM) program initiated in 1992 and reduced melon hectares from 1996 to 2002. Other factors may also have contributed to the population reductions. Seasonally, B. tabaci trap catches decreased during the late summer and fall concurrent with decreasing minimum temperatures that are suggested to be a significant factor affecting seasonal activity and reproduction.

  1. 广西平乐鸡母岩发现的晚更新世人类牙齿化石%LATE PLEISTOCENE HOMININ TEETH FROM THE JIMUYAN CAVE,PINGLE COUNTY, GUANGXI,SOUTH CHINA

    Institute of Scientific and Technical Information of China (English)

    王頠; 黄超林; 谢绍文; 鄢成林

    2011-01-01

    Five hominin teeth are recently discovered at the Jimuyan Cave in Pingle County, Southern China. The Jimuyan Cave is located at Juntang Village(24° 29' 52. 8" N,110° 50' 0. 79" E) ,20km southeast to the Pingle Town,with 163. 2m above the sea level. Mammalian fauna of the cave consists of eleven species,including: Macaca sp. ,Pongo pygmaeus weidenreichi, Hystrix cf. Subcristata, Ursus thibetanus ,Ahuropoda melanoleuca baconi ,Stegodon orhentalis, Tapirus sinensis,Sus scrofa,Muntiacus sp.,Cervus sp. And Bovidae gen. Et sp. Indet. This faunal assemblage contains four genera that are either extinct or no longer present in this region, including Stegodon, Tapirus, Ailuropoda and Pongo, which is distinctly different from that of Holocene, however similar to that of Late Pleistocene in Southern China. Thus, age of this fauna is dated to Late Pleistocene by biostratigraphy comparison. The hominin teeth in Jimuyan Cave are morphologically different from those of already known Homo erectus and Early Homo sapiens, nevertheless, similar to those of Late Homo sapiens in South China. This finding presents significant fossil evidence for the study of modern hunan origin and evolution in East Asia.The origin of modern humans is a controversial scientific topic at present. Based on fossil evidence of Homo sapiens in Africa are more ancient than that in Eastern Asia. With the results of molecular biology analysis, most of the anthropologists and geneticists support the hypothesis of modern humans originated in Africa. So far,the oldest fossils come from Omo-Kibish and Herto in Ethiopia, with the age of 160ka and 190ka respectively. The characteristics of these fossil skulls are intervenient between Homo sapiens and Homo heidelbergensis. Some of the hominin fossils,dated to 74 ~ 134ka,have been discovered at Klasies estuary in South Africa, but it is difficult to confirm whether these materials belong to modern human. Fossil hominin unearthed at Qafzeh and Skhul in Israel, Middle

  2. 76 FR 28453 - Cesar Chavez Special Resource Study-Alameda, Fresno, Imperial, Kern, Los Angeles, Monterey...

    Science.gov (United States)

    2011-05-17

    ... site for NPS Planning, Environment and Public Comment, and will be advertised in a newsletter which... National Park Service Cesar Chavez Special Resource Study--Alameda, Fresno, Imperial, Kern, Los Angeles..., Stanislaus, Tulare and Ventura Counties, CA, and Maricopa and Yuma Counties, AZ AGENCY: National Park...

  3. A Friction of Cultural Values and Characteristics of Imperial Mosque in Ternate

    Directory of Open Access Journals (Sweden)

    muhammad tayeb

    2015-06-01

    Full Text Available Indonesia has many religious culture that should be preserved one of  which is the imperial mosque. Most of the imperial mosque has its own characteristics in carrying out activities both religious and cultural. Sultanate of Ternate is the largest sultanates in eastern Indonesia which would give other peculiarities that need to be raised as a typical Indonesian culture. The purpose of this study is to identify the type of tradition in doing at the mosque sultanate by people of Ternate and changes in cultural values of the people of Ternate in the imperial mosque. In this study found the phenomenon characteristic changes in cultural values by linking changes in the physical aspect and non-physical. To determine the effect of these factors, the method used is the method of observation of physical traces. This method is expected to be able to explain the effect of the change occurred. Based on the results of the study indicate compliance is still customary rules of religious traditions in the imperial mosque although some traditions that formerly taboo has been done, the progress of the times, increase knowledge, and make the implementation of the reform and renewal of cultural values carried by the community for various reasons theTernate.

  4. A Groundwater Model to Assess Water Resource Impacts at the Imperial East Solar Energy Zone

    Energy Technology Data Exchange (ETDEWEB)

    Quinn, John [Argonne National Lab. (ANL), Argonne, IL (United States); Greer, Chris [Argonne National Lab. (ANL), Argonne, IL (United States); O' Connor, Ben L. [Argonne National Lab. (ANL), Argonne, IL (United States); Tompson, Andrew F.B. [Lawrence Livermore National Lab. (LLNL), Livermore, CA (United States)

    2013-12-01

    The purpose of this study is to develop a groundwater flow model to examine the influence of potential groundwater withdrawal to support the utility-scale solar energy development at the Imperial East Solar Energy Zone (SEZ) as a part of the Bureau of Land Management’s (BLM) solar energy program.

  5. "In Defence of Cricket": The Imperial Games Ethic in Victorian English Canada.

    Science.gov (United States)

    Bennett, Paul L.

    1989-01-01

    Illustrates how societies can be judged by the athletic games they play through presentation of an exchange of letters appearing in the 1872 issues of the Upper Canada College newspaper. Shows how cricket, representing imperial society and muscular Christianity, was threatened by the Yankees and "American baseball." (LS)

  6. 76 FR 39357 - Revisions to the California State Implementation Plan, Imperial County Air Pollution Control...

    Science.gov (United States)

    2011-07-06

    ... Pollution Control District, Kern County Air Pollution Control District, and Ventura County Air Pollution... proposing to approve revisions to the Imperial County Air Pollution Control District (ICAPCD), Kern County Air Pollution Control District (KCAPCD), and Ventura County Air Pollution Control District...

  7. ERDA test facilities, East Mesa Test Site. Geothermal resource investigations, Imperial Valley, California

    Energy Technology Data Exchange (ETDEWEB)

    1976-01-01

    Detailed specifications which must be complied with in the construction of the ERDA Test Facilities at the East Mesa Site for geothermal resource investigations in Imperial Valley, California are presented for use by prospective bidders for the construction contract. The principle construction work includes a 700 gpm cooling tower with its associated supports and equipment, pipelines from wells, electrical equipment, and all earthwork. (LCL)

  8. Imperial scientists lead the way in preparation for the biggest experiment on earth

    CERN Multimedia

    Reeves, Danielle

    2006-01-01

    "An international team of over 2'000 scientist, led by Professor Tejinder Virdee from Imperial College London's Departement of Physics is stepping up preparations for the world's largest ever physics experiment, starting next year at CERN near Geneva, Switzerland." (1 page)

  9. Jane Austen and Imperialism--A Rereading of "Pride and Prejudice"

    Science.gov (United States)

    Xu, Runjiang; Li, Yucheng

    2009-01-01

    This thesis attempts to search for the clues related to British domestic exploitation of the peasant labors and overseas colonization of other countries after rereading the novel "Pride and Prejudice," with an aim to bring out Austen's intimacy with Imperialism. It will offer some insights into a better understanding of provincial world…

  10. Linguistic Globalization and the Call Center Industry: Imperialism, Hegemony or Cosmopolitanism?

    Science.gov (United States)

    Sonntag, Selma K.

    2009-01-01

    Linguistic imperialism, linguistic hegemony and linguistic cosmopolitanism are broad and contrasting conceptualizations of linguistic globalization that are frequently, if implicitly, invoked in the literature, both academic and non-academic, on language practices and perceptions in the call center industry. I begin with outlining each of these…

  11. International Students: Constructions of Imperialism in the "Chronicle of Higher Education"

    Science.gov (United States)

    Rhee, Jeong-eun; Sagaria, Mary Ann Danowitz

    2004-01-01

    This article links colonial/neocolonial and feminist literature with discourses on international students to examine how a discourse of imperialism constructs and represents international students in U.S. universities. Applying a critical discourse analysis to 78 articles published in the "Chronicle of Higher Education" between 1996 and 1999, the…

  12. Greene/Feizi - U of Penn; Imperial College | Division of Cancer Prevention

    Science.gov (United States)

    Principal Investigator: Mark Greene, MD, PhDInstitution: University of Pennsylvania, Philadelphia, PA Subcontract Principal Investigator: Ten Feizi, MD, FmedSciInstitution: Imperial College London Former Principal Investigator: Minoru Fukuda, PhD (retired)Institution: Sanford Burnham Medical Research Institute, La Jolla, CA |

  13. 77 FR 72968 - Revisions to the California State Implementation Plan, for Imperial County, Placer County and...

    Science.gov (United States)

    2012-12-07

    ... County and Ventura County Air Pollution Control Districts AGENCY: Environmental Protection Agency (EPA). ACTION: Direct final rule. SUMMARY: EPA is taking direct final action to approve revisions to the Imperial County Air Pollution Control District (ICAPCD), Placer County Air Pollution Control...

  14. 76 FR 12280 - Revisions to the California State Implementation Plan, for Imperial County, Kern County, and...

    Science.gov (United States)

    2011-03-07

    ... County, and Ventura County; Air Pollution Control Districts AGENCY: Environmental Protection Agency (EPA). ACTION: Direct final rule. SUMMARY: EPA is taking direct final action to approve revisions to the Imperial County Air Pollution Control District (ICAPCD), Kern County Air Pollution Control District...

  15. 75 FR 27975 - Revisions to the California State Implementation Plan; Imperial County Air Pollution Control...

    Science.gov (United States)

    2010-05-19

    ... Pollution Control District AGENCY: Environmental Protection Agency (EPA). ACTION: Proposed rule. SUMMARY: EPA is proposing to approve revisions to the Imperial County Air Pollution Control District (ICAPCD... Clean Air Act as amended in 1990 (CAA or the Act). We are taking comments on this proposal and plan...

  16. 76 FR 7142 - Revisions to the California State Implementation Plan, Imperial County Air Pollution Control...

    Science.gov (United States)

    2011-02-09

    ... Pollution Control District AGENCY: Environmental Protection Agency (EPA). ACTION: Proposed rule. SUMMARY: EPA is proposing to approve revisions to the Imperial County Air Pollution Control District (ICAPCD... pollution sources. We are taking comments on this proposal and plan to follow with a final action....

  17. 76 FR 39303 - Revisions to the California State Implementation Plan, Imperial County Air Pollution Control...

    Science.gov (United States)

    2011-07-06

    ... Pollution Control District, Kern County Air Pollution Control District, and Ventura County Air Pollution Control District AGENCY: Environmental Protection Agency (EPA). ACTION: Direct final rule. SUMMARY: EPA is taking direct final action to approve revisions to the Imperial County Air Pollution Control...

  18. 77 FR 25109 - Revisions to the California State Implementation Plan, Imperial County Air Pollution Control...

    Science.gov (United States)

    2012-04-27

    ... Pollution Control District AGENCY: Environmental Protection Agency (EPA). ACTION: Proposed rule. SUMMARY: EPA is proposing to approve revisions to the Imperial County Air Pollution Control District (ICAPCD...). We are taking comments on this proposal and plan to follow with a final action. DATES: Any...

  19. 78 FR 23677 - Revisions to the California State Implementation Plan, Imperial County Air Pollution Control...

    Science.gov (United States)

    2013-04-22

    ... Pollution Control District AGENCY: Environmental Protection Agency (EPA). ACTION: Final rule. SUMMARY: EPA is finalizing approval of revisions to the Imperial County Air Pollution Control District (ICAPCD...) emissions from sources of fugitive dust such as unpaved roads and disturbed soils in open and...

  20. Late Budgets

    DEFF Research Database (Denmark)

    Andersen, Asger Lau; Lassen, David Dreyer; Nielsen, Lasse Holbøll Westh

    The budget forms the legal basis of government spending. If a budget is not in place at the beginning of the fiscal year, planning as well as current spending are jeopardized and government shutdown may result. This paper develops a continuous-time war-of-attrition model of budgeting...... in a presidential style-democracy to explain the duration of budget negotiations. We build our model around budget baselines as reference points for loss averse negotiators. We derive three testable hypotheses: there are more late budgets, and they are more late, when fiscal circumstances change; when such changes...... are negative rather than positive; and when there is divided government. We test the hypotheses of the model using a unique data set of late budgets for US state governments, based on dates of budget approval collected from news reports and a survey of state budget o¢ cers for the period 1988...

  1. Late Budgets

    DEFF Research Database (Denmark)

    Andersen, Asger Lau; Lassen, David Dreyer; Nielsen, Lasse Holbøll Westh

    are negative rather than positive; and when there is divided government. We test the hypotheses of the model using a unique data set of late budgets for US state governments, based on dates of budget approval collected from news reports and a survey of state budget o¢ cers for the period 1988......The budget forms the legal basis of government spending. If a budget is not in place at the beginning of the fiscal year, planning as well as current spending are jeopardized and government shutdown may result. This paper develops a continuous-time war-of-attrition model of budgeting...... in a presidential style-democracy to explain the duration of budget negotiations. We build our model around budget baselines as reference points for loss averse negotiators. We derive three testable hypotheses: there are more late budgets, and they are more late, when fiscal circumstances change; when such changes...

  2. Late Permian high-Mg andesite and basalt association from northern Liaoning, North China: Insights into the final closure of the Paleo-Asian ocean and the orogen-craton boundary

    Science.gov (United States)

    Yuan, Lingling; Zhang, Xiaohui; Xue, Fuhong; Lu, Yinghuai; Zong, Keqing

    2016-08-01

    High-Mg andesites (HMAs) and related basalts constitute a volumetrically minor, but genetically important occurrence along most convergent plate margins of various ages on Earth. The details of their petrogenesis can contain critical information for resolving essential geodynamic and crustal evolutionary issues. This zircon U-Pb dating and geochemical study documents the late Permian metamorphosed high-Mg basaltic to andesitic suite from Kaiyuan of northern Liaoning, North China. These rocks feature SiO2 contents ranging from 48.7 to 63.2 wt.%, high Mg# values of 63-75, an enrichment in large-ion lithophile elements (LILE), and depletion in high field strength elements (HFSE). They possess whole-rock initial 87Sr/86Sr ratios of 0.70417-0.70457, εNd(t) values from - 0.4 to 5.0, and εHf(t) values from 5.1 to 11, as well as zircon εHf(t) values from - 9.4 to 0.4. These features indicate that their petrogenesis most likely involved precursory metasomatism of mantle peridotites by melts from subduction-related sediments, and subsequent partial melting. With a depleted mantle source and possible tectonic link to post-subduction slab break-off, the Kaiyuan suite could present a spatial reference not only for defining the demarcation line between the North China craton (NCC) and the Central Asian Orogenic belt (CAOB) in the region, but also for tracing the final location of the cryptic suturing zone of the Paleo-Asian Ocean. Synthesizing the suite with coeval igneous episodes as well as concomitant metamorphic events along the Solonker-Xra Moron-Changchun zone leads to the characterization of the eventual closure of the Paleo-Asian Ocean within a double-sided subduction system during late Permian-Early Triassic.

  3. Pollen and phytolith evidence for rice cultivation and vegetation change during the mid-late holocene at the Jiangli site, Suzhou, East China.

    Directory of Open Access Journals (Sweden)

    Zhenwei Qiu

    Full Text Available Pollen and phytolith analyses were undertaken at the Jiangli site in Suzhou, Jiangsu Province, combined with studies on macrofossils by flotation. The concentration of pollen decreased while the percentage of Poaceae pollen in the profile increased from the late phase of the Majiabang Culture to the Songze Culture suggesting that human impact on the local environment intensified gradually. The discovery of rice paddy implies a relatively advanced rice cultivation in this area during the middle-late Holocene. Other than phytoliths, the high percentage of Oryza-type Poaceae pollen (larger than 40 µm supplied robust evidence for the existence of rice paddy. Moreover, the fact that the farther from the rice paddy, the lower the concentration and percentage of Poaceae pollen also proves that the dispersal and deposition of pollen is inversely proportional to the distance.

  4. Pollen and phytolith evidence for rice cultivation and vegetation change during the mid-late holocene at the Jiangli site, Suzhou, East China.

    Science.gov (United States)

    Qiu, Zhenwei; Jiang, Hongen; Ding, Jinlong; Hu, Yaowu; Shang, Xue

    2014-01-01

    Pollen and phytolith analyses were undertaken at the Jiangli site in Suzhou, Jiangsu Province, combined with studies on macrofossils by flotation. The concentration of pollen decreased while the percentage of Poaceae pollen in the profile increased from the late phase of the Majiabang Culture to the Songze Culture suggesting that human impact on the local environment intensified gradually. The discovery of rice paddy implies a relatively advanced rice cultivation in this area during the middle-late Holocene. Other than phytoliths, the high percentage of Oryza-type Poaceae pollen (larger than 40 µm) supplied robust evidence for the existence of rice paddy. Moreover, the fact that the farther from the rice paddy, the lower the concentration and percentage of Poaceae pollen also proves that the dispersal and deposition of pollen is inversely proportional to the distance.

  5. Pollen and phytolith evidence for rice cultivation and vegetation change during the mid-late Holocene at the Jiangli site, Suzhou, East China.

    Directory of Open Access Journals (Sweden)

    Zhenwei Qiu

    Full Text Available Pollen and phytolith analyses were undertaken at the Jiangli site in Suzhou, Jiangsu Province, combined with studies on macrofossils by flotation. The concentration of pollen decreased while the percentage of Poaceae pollen in the profile increased from the late phase of the Majiabang Culture to the Songze Culture suggesting that human impact on the local environment intensified gradually. The discovery of rice paddy implies a relatively advanced rice cultivation in this area during the middle-late Holocene. Other than phytoliths, the high percentage of Oryza-type Poaceae pollen (larger than 40 μm supplied robust evidence for the existence of rice paddy. Moreover, the fact that the farther from the rice paddy, the lower the concentration and percentage of Poaceae pollen also proves that the dispersal and deposition of pollen is inversely proportional to the distance.

  6. German's School Policy towards China in the Late Qing Dynasty and the Establishment of Elementary School in Qingdao%清末德国对华学校政策与青岛蒙养学堂的创办

    Institute of Scientific and Technical Information of China (English)

    赵少峰; 崔文龙

    2016-01-01

    德国在华建立中小学校是其海外学校事业的重要组成部分,是强化德国文化对中国影响的体现.早期的教会学校是为解决在华德国子女教育问题和培养传教助手服务的.清季德占青岛之初,德国殖民者精力集中在基础设施建设上,技术和语言学校是应急之需,没有制定系统的中小学教育计划.随着殖民统治的深入,教育、文化的影响力突显,德国对华学校政策发生了变化.建立官办新式学堂,让中国的年轻一代学习德国的语言,熟悉和亲近德国的文化,获取更大的在华权力,成为德国殖民者的重要政策.在德国殖民当局的支持下,为德国文化政策服务的蒙养学堂得以在租借地内迅速建立.%Establishing primary and secondary schools in China,as an important part of German's overseas school career,is an embodiment of strengthening its cultural impact on China.The building-up of early missionary schools was to solve the education problems for German children who resided in China and to provide services for training missionary helpers.In the Late Qing Dynasty,when Germany first occupied Qingdao,they focused on the construction of infrastructure.Technical and language schools were in urgent need and there wasn't any specific education programs for primary and secondary schools.With the deepening of colonial rule,the influence of education and culture was growing,German's school policy towards China also changed.Establishing new-style and government-run schools,letting Chinese young generations to learn German language,making them be familiar with and close to the German culture,as well as seeking more power in China have become important policies of German colonists.With the support of German colonial authorities,the elementary schools serving German's cultural policy were quickly established in the leased territory.

  7. U-Pb zircon ages and geochemistry of the Wuguan complex in the Qinling orogen, central China: Implications for the late Paleozoic tectonic evolution between the Sino-Korean and Yangtze cratons

    Science.gov (United States)

    Chen, Longyao; Liu, Xiaochun; Qu, Wei; Hu, Juan

    2014-04-01

    The tectonic evolution of the Qinling orogen, central China, is the key to understanding the assembly of the Sino-Korean and Yangtze cratons. The Wuguan complex, between the early Paleozoic North Qinling and Mesozoic South Qinling tectonic belts, can provide important constraints on the late Paleozoic evolutionary processes in the Qinling orogen. U-Pb zircon analyses, using laser ablation-multicollector-inductively coupled plasma-mass spectrometry, reveal protolith ages of 446 ± 2 Ma for a garnet amphibolite, 368 ± 3 Ma for a meta-andesite, and 351 ± 2 Ma for a mylonitized granitic dike from the Wuguan complex. Elemental geochemistry indicates typical island arc affinities for all the above rocks, but some amphibolites of unknown age have E-MORB signatures. Detrital zircons from a metaquartzite have an age spectrum with a major peak at 462 Ma, two subordinate peaks at 828 and 446 Ma, and a youngest weighted mean age of 423 ± 5 Ma. This suggests that at least some of metasedimentary rocks from the Wuguan complex belong to the part of the Devonian turbidite sequence of the Liuling Group, which was deposited in a fore-arc basin along the southern accreted margin of the Sino-Korean craton, whereas the late Ordovician precursors of the amphibolite might be derived from the Danfeng Group. The occurrence of late Devonian-early Carboniferous arc-related rocks in the Wuguan complex implies penecontemporaneous oceanic subduction, and therefore the Paleo-Qinling Ocean was not finally closed until the early Carboniferous. On the other hand, metamorphic zircon grains from two amphibolites yielded ages of 321 ± 2 and 318 ± 3 Ma. Hence, the Wuguan complex in the Qinling orogen and the Guishan complex in the Tongbai orogen constitute a medium-pressure Carboniferous metamorphic belt that is more than 500 km long, and which was formed in the hanging wall of a subduction zone.

  8. Evidence of Arid to Semi-arid Climate Near Western Pacific Warm Pool During Sea-Level Lowstands: Caliche Surfaces in Late Cenozoic Carbonates of Nansha Islands, South China Sea

    Science.gov (United States)

    Gong, S.; Mii, H.; Horng, C.; Huang, F.; Chi, W.; Yui, T.; Torng, P.; Huang, S.; Wang, S.; Wu, J.; Yang, K.

    2003-12-01

    Whether the climate of tropical seas during glacial periods became cold and dry has been an open debate. Models by different authors proposed the tropical sea-surface temperature (SST) during the Last Glacial Maximum (LGM) to be about 2\\deg lower, or 5-6\\deg lower than present. The controversy partly arise from disparate reconstructions of temperature from stable oxygen isotope archives of marine sediments. In this paper, we provide field evidence of semi-arid or arid climate during late Cenozoic sea-level lowstands from an atoll located in central South China Sea near the Western Pacific Warm Pool (WPWP). Lower rainfall and higher evaporation associated with the dry conditions might have resulted in less meteoric water component in the surface sea-water, and this factor should be taken into considerations in deciphering temperature from isotopic records. Taiping Islet (Itu Aba), located at N10\\deg 23' and E114\\deg 22' is part of the Nansha (Spratly) Islands near the northwestern margin of the Western Pacific Warm Pool. Rock cores of a borehole at Taiping became accessible to the authors in the recent years. We identified at least four subaerial exposure surfaces (SES) in the late Cenozoic carbonates. Caliche deposits are recognized on each of the four surfaces on the basis of alveolar texture, micro-rhizolith, caliche glaebules and corroded limestone nodules in reddish matrix (terra-rossa). Caliche developed on limestones typically forms in semi-arid to arid areas with annual precipitation from about 500 to 1000mm, while the modern annual rainfall of Nansha Island is 1800-2100mm. The occurrence of the Nansha caliche suggests the climate was much drier than present during the sea-level lowstands represented by the four SES. During the sea-level falls, reduced surface area of South China Sea with continental shelves exposed might have resulted in less moistures in the atmosphere and therefore less precipitation and higher evaporation rates. As a result, the

  9. Late Mesozoic orogenesis along the coast of Southeast China and its geological significance%华南陆缘晚中生代造山及其地质意义

    Institute of Scientific and Technical Information of China (English)

    崔建军; 张岳桥; 董树文; 江博明; 徐先兵; 马立成; 李建华; 苏金宝; 李勇

    2013-01-01

    The Changle-Nan'ao zone is situated along the southeastern margin of the Southeast China continent, hence it may hold a key to understanding the interactions between the Eurasian and Paleo-pacific plates and geological evolution of the coastal areas in Late Mesozoic. The T3-J1 sedimentary rocks in the coastal zone are unconformably overlain by Lower Cretaceous Nanyuan Formation or occur as amphibolite fades enclaves in late Jurassic -early Cretaceous gneissic granites. The metasedimentary rocks (T3 -J1) enclaves with penetrative migmatization were deformed together with the wall rocks (gneissic granites) and intruded by insignificantly deformed Cretaceous granitic plutons or dykes. Metamorphism and deformation in the late Triassic to early Jurassic (T3-J1) metasedimentary rocks are characterized by cratonward (NW) weakening. The Lower Cretaceous Nanyuan Formation is characterized by extensive folding and greenschist facies metamorphism and unconformably covered by the Upper Cretaceous Shimaoshan Group, showing no signs of metamorphism. The major stratigraphic units and tectonics in the Changle-Nan'ao zone indicate that the continental margins underwent two stages of compression (orogenesis) in Late Mesozoic. During the first episode of orogenesis, the late Triassic to early Jurassic (T3-J1) continental sediments were folded and metamorphosed. Subsequently, the folded and metamorphosed T3-J1 sedimentary rocks were exhumed together with other rocks from the depth of middle and upper crusts in early Cretaceous, accompanied by large scale synkinematic magmatism (147-135 Ma) and regional migmatization. During the second stage of compression in Late Mesozoic, the Nanyuan Formation was folded and metamorphosed. The 110-100 Ma magmatic complex, the 100-90 Ma A-type granites, and the 90-80 Ma bimodal igneous rocks in coastal areas of Southeast China might be correlated with the middle Cretaceous crustal contraction and the subsequent crustal extensions, respectively

  10. Purposes and Bibliographic Objectives of a Pioneer Library Catalog in China

    Science.gov (United States)

    Lee, Hur-Li; Lan, Wen-Chin

    2009-01-01

    This research aims to ascertain the conceptual basics underlying the design of the "Seven Epitomes", the first library catalog to establish the bibliographic model in imperial China. The analytical framework for the study consists of a reconstructed version of the catalog and its historical contexts. In analyzing the surviving text of…

  11. Purposes and Bibliographic Objectives of a Pioneer Library Catalog in China

    Science.gov (United States)

    Lee, Hur-Li; Lan, Wen-Chin

    2009-01-01

    This research aims to ascertain the conceptual basics underlying the design of the "Seven Epitomes", the first library catalog to establish the bibliographic model in imperial China. The analytical framework for the study consists of a reconstructed version of the catalog and its historical contexts. In analyzing the surviving text of the catalog,…

  12. 科举制度的废除与绅士阶层的分化%On Abolition of the Imperial Examination System and the Polarization of Gentry' Class

    Institute of Scientific and Technical Information of China (English)

    王红

    2012-01-01

    清末科举制度的废除对中国政治、社会、文化产生了多方面影响,尤其直接改变了中国社会阶级结构。科举制度是士绅阶层存在的支柱,而科举制度的停废,意味着其原有阶层流动的渠道不再畅通,于是绅士便分流到新式教育、经济、军事等各个部门,绅士的社会角色和价值观念发生了空前的变动。但是,作为统治中国社会特权等级阶层的绅士地位和身份的变化对清末民初的社会产生了深远的影响。%In the late Qing dynasty, the abolition of the imperial examination system influenced Chinese politics, society and cul- ture, especially directly changing Chinese social class structure. The imperial examination system is the pillar of the gentry' class' existence and the stopping and wasting of imperial examination system means that the original flow channel is no longer unimpeded, and then gentry class went to the latest education, economic, military, and so on each department. The social role and value of the gentry class experienced unprecedented change. As the privilege level class, the change of status and identify had far - reaching influence on the society in the late Qing dynasty.

  13. Mid-Late Triassic metamorphic event for Changhai meta-sedimentary rocks from the SE Jiao-Liao-Ji Belt, North China Craton: Evidence from monazite U-Th-Pb and muscovite Ar-Ar dating

    Science.gov (United States)

    Liu, Fulai; Wang, Fang; Liou, J. G.; Meng, En; Liu, Jianhui; Yang, Hong; Xiao, Lingling; Cai, Jia; Shi, Jianrong

    2014-11-01

    The precise constraints on the timing of metamorphism of the Changhai metamorphic complex is of great importance considering the prolonged controversial issue of the north margin and the extension of the Sulu-Dabie HP-UHP Belt. While the monazite U-Th-Pb and muscovite 40Ar/39Ar techniques are widely accepted as two of the most powerful dating tools for revealing the thermal histories of medium-low grade metamorphic rocks and precisely constraining the timing of metamorphism. The Changhai metamorphic complex at the SE Jiao-Liao-Ji Belt, North China Craton consists of a variety of pelitic schist and Grt-Ky-bearing paragneiss, and minor quartzite and marble. Analyses of mineral inclusions and back-scattered electric (BSE) images of monazites, combined with LA-ICP-MS U-Th-Pb ages for monazites and 40Ar/39Ar ages for muscovites, provide evidence of the origin and metamorphic age of the Changhai metamorphic complex. Monazites separates from various Grt-Mus schists and Grt-Ky-St-Mus paragneisses exhibit homogeneous BSE images from cores to rims, and contain inclusion assemblages of Grt + Mus + Qtz ± Ctd ± Ky in schist, and Grt + Ky + St + Mus + Pl + Kfs + Qtz inclusions in paragneiss. These inclusion assemblages are very similar to matrix minerals of host rocks, indicating they are metamorphic rather than inherited or detrital in origin. LA-ICP-MS U-Th-Pb dating reveals that monazites of schist and paragneiss have consistent 206Pb/238U ages ranging from 228.1 ± 3.8 to 218.2 ± 3.7 Ma. In contrast, muscovites from various schists show slightly older 40Ar/39Ar plateau ages of 236.1 ± 1.5 to 230.2 ± 1.2 Ma. These geochronological and petrological data conclude that the pelitic sediments have experienced a metamorphic event at the Mid-Late Triassic (236.1-218.2 Ma) rather than the Paleoproterozoic (1950-1850 Ma), commonly regarded as the Precambrian basement for the Jiao-Liao-Ji Belt. Hence, the Changhai metamorphic complex should be considered as a discrete

  14. The amalgamation of the supercontinent of North China Craton at the end of Neo-Archaean and its breakup during late Palaeoproterozoic and Meso-Proterozoic

    Institute of Scientific and Technical Information of China (English)

    翟明国; 卞爱国; 赵太平

    2000-01-01

    The most important geological events in the formation and evolution of the North China Craton concentrate at two stages: 2 600-2 400 Ma and 2 000-1 700 Ma (briefly, we call them 2.5 Ga event and 1.8 Ga event respectively in this paper). We propose that the essences of these two events are: Several Archaean micro-continents amalgamated to form one supercontinent according to the plate tectonic principle with a small scale at about 2.5 Ga, and the supercontinent broke down by upwelling of an ancient mantle plume at about 1.8 Ga.

  15. Palaeo-earthquake events during the late Early Palaeozoic in the central Tarim Basin (NW China: evidence from deep drilling cores

    Directory of Open Access Journals (Sweden)

    He Bizhu

    2014-07-01

    Full Text Available Various millimetre-, centimetre- and metre-scale soft-sediment deformation structures (SSDS have been identified in the Upper Ordovician and Lower-Middle Silurian from deep drilling cores in the Tarim Basin (NW China. These structures include liquefied-sand veins, liquefaction-induced breccias, boudinage-like structures, load and diapir- or flame-like structures, dish and mixed-layer structures, hydroplastic convolutions and seismic unconformities. The deformed layers are intercalated by undeformed layers of varying thicknesses that are petrologically and sedimentologically similar to the deformed layers.

  16. A review of the geological characteristics and geodynamic setting of Late Paleozoic porphyry copper deposits in the Junggar region, Xinjiang Uygur Autonomous Region, Northwest China

    Science.gov (United States)

    Yang, Fuquan; Mao, Jingwen; Pirajno, Franco; Yan, Shenghao; Liu, Guoren; Zhou, Gang; Zhang, Zhixin; Liu, Feng; Geng, Xinxia; Guo, Chunli

    2012-04-01

    In this review, we describe the geological characteristics of porphyry copper deposits in Junggar region, Xinjiang, and place these into their metallogenic-tectonic context. These porphyry copper deposits are mainly found in four metallogenic belts: (1) a Late Silurian to Early Devonian Cu-Mo metallogenic belt in the Qiongheba area; (2) the Late Devonian Kalaxiange'er Cu metallogenic belt; (3) the Early Carboniferous Xilekuduke-Suoerkuduke porphyry-skarn Cu-Mo metallogenic belt; and (4) the Late Carboniferous Baogutu porphyry Cu metallogenic belt. The ages of mineralization can be divided into three broad intervals: copper deposits range mainly from 300 to 180 °C. Salinity ranges from 0.5 to 21.7 wt.% NaCl equiv and 28.9 to 66.76 wt.% NaCl equiv. Ore-forming fluids in the Baogutu and Yunyingshan deposits in the Baogutu and Qiongheba belts, were mainly derived from magmatic fluids, whereas those in the Halasu, Yulekenhalasu and Xilekuduke deposits in the Kalaxiange'er and Xilekuduke-Suoerkuduke belts were mainly derived from magmatic fluids, with some contributions from meteoric water. Sulfur isotope compositions of some porphyry copper deposits cluster around 0‰, indicating that the sulfur was probably derived from mantle-related magmas. The ore-forming processes in all porphyry copper deposits are closely related to the emplacement of intermediate, intermediate-felsic and felsic porphyry intrusions. Porphyry copper deposits in Junggar region developed in a range of tectonic regimes including continental arc, ocean island arc and post collisional settings.

  17. Procopius of Caesarea: A Case Study in Imperial Criticism

    Directory of Open Access Journals (Sweden)

    James Michael GILMER

    2013-10-01

    Full Text Available This paper seeks to analyze the methods of Procopius of Caesarea and reconcile the apparent contradictions the historian presents in his treatment of the reign of the Emperor Justinian. To that end, the tone of each work is considered and compared to similar works of Late Antiquity. This paper will endeavor to demonstrate that the attitudes of Procopius toward the Emperor Justinian and many elements of his reign were universally hostile, veiled only by the conventions of the genres in which Procopius chose to write.

  18. A new prediction model for grain yield in Northeast China based on spring North Atlantic Oscillation and late-winter Bering Sea ice cover

    Science.gov (United States)

    Zhou, Mengzi; Wang, Huijun; Huo, Zhiguo

    2017-04-01

    Accurate estimations of grain output in the agriculturally important region of Northeast China are of great strategic significance for guaranteeing food security. New prediction models for maize and rice yields are built in this paper based on the spring North Atlantic Oscillation index and the Bering Sea ice cover index. The year-to-year increment is first forecasted and then the original yield value is obtained by adding the historical yield of the previous year. The multivariate linear prediction model of maize shows good predictive ability, with a low normalized root-mean-square error (NRMSE) of 13.9%, and the simulated yield accounts for 81% of the total variance of the observation. To improve the performance of the multivariate linear model, a combined forecasting model of rice is built by considering the weight of the predictors. The NRMSE of the model is 12.9% and the predicted rice yield explains 71% of the total variance. The corresponding cross-validation test and independent samples test further demonstrate the efficiency of the models. It is inferred that the statistical models established here by applying year-to-year increment approach could make rational prediction for the maize and rice yield in Northeast China before harvest. The present study may shed new light on yield prediction in advance by use of antecedent large-scale climate signals adequately.

  19. Species Diversity and Abundance Distribution of Pelagic Siphonophores in Nan Wan Bay of Taiwan, China, in Late Autumn and Early Winter

    Institute of Scientific and Technical Information of China (English)

    2005-01-01

    Zooplankton surveys were carried out on November 2-3 and December 8-10, 2001at 12 stations in the Nan Wan Bay of Taiwan, China. Altogether 92 quantitative zooplankton samples were collected from subsurface water and bottom water layers with two conical plankton nets (180 cm in length, 45 cm in opening diameter, 333 μm and 200 μm in mesh size).A total of 31 species of Siphonophores were identified, among them 7 species are new records in the waters around Taiwan Island, of which Rocacea cymbiformis is a new record in China.Dominated by Chelophyes appendiculata, Bassia bassensis, Diphyes bojani, Diphyes dispar,Abylopsis eschscholtzi and Chelophyes contorta, these species accounted for over 76 % and 63 % of the total abundance in November and December. The species number and Siphonophores abundance in December (25 species, 1.99 inds/m3) were more than those in November (19 species, 0.438 inds/m3), and they were more in the surface water layer than in the bottom layer at most sampling stations. In early winter, the offshore high salinity water mass was a main factor influencing the distribution. The sampling efficiency for two plankton nets is discussed and the seasonal variation of species number and abundance in the Nan Wan Bay is compared with that in the neighboring waters.

  20. Late Quaternary normal faulting and its kinematic mechanism of eastern piedmont fault of the Haba-Yulong Snow Mountains in northwestern Yunnan, China

    Institute of Scientific and Technical Information of China (English)

    2009-01-01

    The regional geologic and geomorphic observations show that an active arcuate normal fault constitutes the main boundary fault of the Haba-Yulong Snow Mountains (HYSM). This fault is called eastern piedmont fault of Haba-Yulong Snow Mountains (HYPF). The fault consists of two segments with differential trend; the northern segment is NW-trending and NE-dipping and the southern section is S-N trending and E-dipping. Three sets of fault scarps cutting late Quaternary landforms and their dating results indicate that the fault is a prominent Holocene active fault and its throw rates are 0.3―1.4 mm/a during late Quaternary. The geometry and kinematics of the fault suggest that the arcuate normal faulting or rifting are typical surface deformation pattern at the two tips of the Z-shaped rift zone of northwestern Yunnan, which is related to regional east-west extension accompanying clockwise rota- tion of micro-block.

  1. Late Quaternary normal faulting and its kinematic mechanism of eastern piedmont fault of the Haba-Yulong Snow Mountains in northwestern Yunnan, China

    Institute of Scientific and Technical Information of China (English)

    WU ZhongHai; ZHANG YongShuang; HU DaoGong; ZHAO XiTao; YE PeiSheng

    2009-01-01

    The regional geologic and geomorphic observations show that an active arcuate normal fault consti-tutes the main boundary fault of the Haba-Yulong Snow Mountains (HYSM). This fault is called eastern piedmont fault of Haba-Yulong Snow Mountains (HYPF). The fault consists of two segments with dif-ferential trend; the northern segment is NW-trending and NE-dipping and the southern section is S-N trending and E-dipping. Three sets of fault scarps cutting late Quaternary landforms and their dating results indicate that the fault is a prominent Holocene active fault and its throw rates are 0.3-1.4 mm/a during late Quaternary. The geometry and kinematics of the fault suggest that the arcuate normal faulting or rifting are typical surface deformation pattern at the two tips of the Z-shaped rift zone of northwestern Yunnan, which is related to regional east-west extension accompanying clockwise rota-tion of micro-block.

  2. France and the Gulf of Tonkin Region: Shipping Markets and Political Interventions in South China in the 1890s

    Directory of Open Access Journals (Sweden)

    Bert Becker

    2015-09-01

    Full Text Available In the period of “new” imperialism in the late nineteenth and early twentieth centuries, France strived to create a sphere of influence in southwest China. To foster such imperialist policies, France’s policy makers regarded French companies operating in East Asia as instrumental. One such firm was Auguste Raphael Marty’s Tonkin Shipping Company, based in Haiphong, French Indochina, which operated steam coasters across the wider Gulf of Tonkin region. In the region’s highly competitive shipping market, Marty strived to achieve a monopoly when favorable conditions permitted during the final phase of the Sino-Japanese War. His profit-driven strategy caused huge losses for Chinese shippers and ultimately resulted in their boycotting his ships through the Tsap Yet syndicate. When French officials intervened on Marty’s behalf in negotiations with the Chinese government, the Syndicate was finally dissolved. It was followed by an agreement between the Chinese firm of Yuen Cheong Lee and Co. and the German firm of Jebsen and Co., based on long-established mutual trust between the owners. Although Marty received monetary compensation for his losses, he ruined his relationship with Chinese merchants. This case study presents little-known facts about the interactions among foreign firms in China and demonstrates the Chinese ability to react efficiently to unfair business practices.

  3. Yuan Shikai in the Institutional Changes in the Late Qing Dynasty --Review of McKinnon's Power and Politics in Late Imperial China Yuan Shikai in Tianjin and Beijing(1901--1908)%晚清制度变迁中的袁世凯——评麦金农著《中华帝国晚期的权力与政治:袁世凯在天津与北京(1901-1908)》

    Institute of Scientific and Technical Information of China (English)

    王先明; 牛秋实

    2011-01-01

    McKinnon's study on Yuan Shikai. and his new policy was mainly based on the following concerns: relatively speaking, we know little of the policy of the Qing Dynasty in Beijing and the external and internal pressures it suffered, even less of the empire's change of political power structure at the turn of the century. The author's research and new viewpoint were built on the basis of detailed historical data, in addition to extensive use of common historical data, such as Yuan Shikai' s Memorial, the relevant local records as Guanzong County Annals, archival material as files of the Ministry of Communications and "Customs report", the more use of the "British Foreign Office files (White Paper)" and proofread with Yuan Shileai' s Memorial. Meanwhile more materials are used from the Taipei Palace Museum, such files of the Military Confidential Administration as "the business files of Cuangxu Period, fang ben and the Memorial series". This naturally ensures the academic and credibility of the study.%麦金农对袁世凯和新政的研究,主要基于以下忧虑:相对说来,我们对清末北京政府所受的外部和内部压力知之甚少,对帝国在世纪之交的政治权力结构如何改变的情况知之更少。作者的研究和新见建立在翔实的史料基础之上,除大量运用常见史料如《袁世凯奏折》、相关地方志如《广宗县志》、档案资料如交通部档案以及“海关报告”外,更多地利用了“英国外交部档案(白皮书)”,并以此与《袁世凯奏折》比勘使用。同时,对于台北故宫博物院有关军机处的档案如“光绪朝的商务档、方本、奏编”也使用较多。这自然保证了此项研究的学术性和可信度。

  4. Spatiotemporal reconstruction of Late Mesozoic silicic large igneous province and related epithermal mineralization in South China: Insights from the Zhilingtou volcanic-intrusive complex

    Science.gov (United States)

    Wang, Guo-Guang; Ni, Pei; Zhao, Chao; Wang, Xiao-Lei; Li, Pengfei; Chen, Hui; Zhu, An-Dong; Li, Li

    2016-11-01

    Silicic large igneous provinces (SLIPs) generally reflect large-scale melting of lower crustal materials and represent significant metal reservoirs. The South China Block-Coastal Region (SCB-CR) SLIP hosts several large epithermal deposits. To better understand these deposits, we document the spatiotemporal framework of the host SLIP across the SCB-CR. Using zircon U-Pb dating and geochemical and isotopic analysis, we identify four stages of emplacement. Stage 1 felsophyre (circa 149 Ma) shows a chemical affinity to highly fractionated I-type granites. Stages 2 and 3 of low-Mg felsic volcanics (circa 128 to 111 Ma) and stage 4 felsite (circa 100 Ma) have higher ɛHf(t) and ɛNd(t) values than stage 1 felsophyre, suggesting a significant contribution of newly underplated juvenile crust to the magma sources. Stage 4 diabase (circa 101 Ma) was likely produced by melting of subduction˗metasomatized asthenospheric mantle. Together with reliable published data, we build a new spatiotemporal framework of volcanics and infer that the majority of the SCB-CR SLIP was related to the gradual northwestward subduction of the Izanagi plate beneath South China in a continental arc setting during circa 170 to 110 Ma, and minor contribution was from the eastward retreat of the subducting slab in a back-arc setting during circa 110 to 90 Ma. We conclude that the large-scale epithermal mineralization was generated by melting of the metal-rich, thin (30-40 km), newly underplated hydrous juvenile crust during the tectonic transition from arc to back-arc settings.

  5. Chronological record of the Early Mesozoic underplating in the northern margin of North China-U-Pb chronometry of zircons in the Late Mesozoic andesite from Western Liaoning

    Institute of Scientific and Technical Information of China (English)

    2007-01-01

    Cathodoluminescence spectroscopic analysis of zircons in the uppermost sanukites of the early Cretaceous Yixian Formation in Western Liaoning reveals zoning structures of the zircons in the volcanic rocks. LA-ICP-MS chronometry shows that the central part of the zircons is remnant zircon with a U-Pb dating of 254 Ma, which is consistent with the age of the Early Mesozoic underplating granulites, and that the periphery is zircon crystallizing out of the host magma with a U-Pb dating of 116 Ma, which is highly consistent with the Ar-Ar dating of the host volcanic rocks. Compositions of the clinopyroxenes xenocrystals in the sanukites are similar to those of the clinopyroxenes in the underplating granulites, indicating that the granulites accreted to the lower crust in the Early Mesozoic have been reformed and disrupted by the upwelling diapers of the asthenosphere and taken part in formation of the sanukites in the Late Mesozoic.

  6. Career development: domestic display as imperial, anthropological, and social trophy.

    Science.gov (United States)

    Wintle, Claire

    2008-01-01

    Analyzing the dynamics of collection and display in the colonial context, this essay considers the South Asian artifacts collected by Sir Richard Carnac Temple, Chief Commissioner of the Andaman and Nicobar Islands from 1894-1904. Temple exhibited the teak carvings, body adornments, and hunting tools that he amassed throughout his career in his home, The Nash, which became the foundation of his public persona as a triumphant colonial chief, a "shining light" in the emerging discipline of anthropology, and a wealthy, upper-class lord of the manor. The politics of consumption, decoration, and self-creation converge in The Nash, offering a glimpse into how material objects removed from India during the late nineteenth century were consumed in Britain and how domestic display contributed to the formation of British identity.

  7. Seismic refraction investigation of the Salton Sea geothermal area, Imperial Valley, California

    Energy Technology Data Exchange (ETDEWEB)

    Frith, R.B.

    1978-12-01

    Seven seismic refraction profiles and four long-distance refraction shots have been used to investigate the Salton Sea geothermal area. From these data, two models of the geothermal and adjacent area are proposed. Model 1 proposes a basement high within the geothermal area trending parallel to the axis of the Imperial Valley. Model 2 assumes a horizontal basement in the E-W direction, and proposes a seismic velocity gradient that increases the apparent basement velocity from east to west approximately 15% within the geothermal area. Both models propose basement dip of 3 degrees to the south, yielding a thickness of sediments of 6.6 km near Brawley, California, in the center of the Imperial Valley. Based on offsets inferred in the sedimentary seismic layers of the geothermal area, two NW-SE trending fault zones are proposed.

  8. Production Within and Beyond Imperial Boundaries: Goods, Exchange, and Power in Roman Europe

    Directory of Open Access Journals (Sweden)

    Peter S. Wells

    2015-08-01

    Full Text Available After Rome had conquered much of temperate Europe, the administration directed the establishment of industries important to the maintenance of military and economic control of the new provinces. These included stone quarries, pottery manufactures, and metal industries. Recent research shows that much production was not as centralized as has been believed; diverse industrial sites throughout the provincial landscapes indicate a variety of arrangements for supplying the needs of the empire. In many instances, Roman production systems relied upon indigenous traditions of manufacturing. The provincial economies depended also upon materials collected and processed beyond the imperial frontiers. Analysis of Roman imports in Germany, Scandinavia, and eastern Europe, and of the contexts in which they occur, suggesta that goods produced outside of the empire played a major role in the imperial economy. These commercial links, over which Roman authorities had no effective control, contributed to substantial changes in economics and in social and political configurations in societies beyond the Roman frontier.

  9. THE ROLE OF BRAZIL IN LATIN AMERICA: A BRIEF REFLECTION OF THE BRAZILIAN SUB IMPERIALISM

    Directory of Open Access Journals (Sweden)

    Bernard Teixeira Coutinho

    2013-04-01

    Full Text Available In this article, we intend to raise some conceptual propositions that help us understand the Brazilian role in Latin America and, start a debate on the contemporary Brazilian foreign policy and its practical applications in geopolitics inserted into the world economy. For that, we aim to explain the concept of “multiterritorialidade”, using the sub-imperialism thesis, by Ruy Mauro Marini, creating a dialogue with the concept of semi-periphery, formulated by Immanuel Wallerstein.

  10. Environmental assessmental, geothermal energy, Heber geothermal binary-cycle demonstration project: Imperial County, California

    Energy Technology Data Exchange (ETDEWEB)

    1980-10-01

    The proposed design, construction, and operation of a commercial-scale (45 MWe net) binary-cycle geothermal demonstration power plant are described using the liquid-dominated geothermal resource at Heber, Imperial County, California. The following are included in the environmental assessment: a description of the affected environment, potential environmental consequences of the proposed action, mitigation measures and monitoring plans, possible future developmental activities at the Heber anomaly, and regulations and permit requirements. (MHR)

  11. Solving Man-Induced Large-Scale Conservation Problems: The Spanish Imperial Eagle and Power Lines

    Science.gov (United States)

    López-López, Pascual; Ferrer, Miguel; Madero, Agustín; Casado, Eva; McGrady, Michael

    2011-01-01

    Background Man-induced mortality of birds caused by electrocution with poorly-designed pylons and power lines has been reported to be an important mortality factor that could become a major cause of population decline of one of the world rarest raptors, the Spanish imperial eagle (Aquila adalberti). Consequently it has resulted in an increasing awareness of this problem amongst land managers and the public at large, as well as increased research into the distribution of electrocution events and likely mitigation measures. Methodology/Principal Findings We provide information of how mitigation measures implemented on a regional level under the conservation program of the Spanish imperial eagle have resulted in a positive shift of demographic trends in Spain. A 35 years temporal data set (1974–2009) on mortality of Spanish imperial eagle was recorded, including population censuses, and data on electrocution and non-electrocution of birds. Additional information was obtained from 32 radio-tracked young eagles and specific field surveys. Data were divided into two periods, before and after the approval of a regional regulation of power line design in 1990 which established mandatory rules aimed at minimizing or eliminating the negative impacts of power lines facilities on avian populations. Our results show how population size and the average annual percentage of population change have increased between the two periods, whereas the number of electrocuted birds has been reduced in spite of the continuous growing of the wiring network. Conclusions Our results demonstrate that solving bird electrocution is an affordable problem if political interest is shown and financial investment is made. The combination of an adequate spatial planning with a sustainable development of human infrastructures will contribute positively to the conservation of the Spanish imperial eagle and may underpin population growth and range expansion, with positive side effects on other endangered

  12. Imperial County geothermal development. Quarterly report, April 1-June 30, 1982

    Energy Technology Data Exchange (ETDEWEB)

    1982-06-30

    The activities of the Geothermal Office during the quarter are discussed, including: important geothermal events, geothermal waste disposal, a grant award by the California Energy Commission, the geothermal development meeting, and the current status of geothermal development in Imperial County. Activities of the Geothermal Planner are addressed, including permits, processing of EIR's, and other planning activities. Progress on the direct heat study is reported.

  13. Motivations and experiences of museum visitors: The case of the Imperial War Museum, United Kingdom

    OpenAIRE

    Powell, Raymond; Kokkranikal, Jithendran

    2015-01-01

    This study explores motivations of visitors to the Imperial War Museum (North and South), United Kingdom, with a view to understanding why people visit museums associated with conflicts. Though museums are part of the education and leisure industry, the distinction between education and leisure is often blurred. There are a number of reasons why people visit museums. Motives of museum visitors can be grouped into intrinsic and extrinsic factors. This study analysed the extent to which museum ...

  14. Reflection of reading Three Women’s Texts and a Critique of Imperialism

    Institute of Scientific and Technical Information of China (English)

    王锐

    2012-01-01

    The author Spivak examines three women’s texts: Jane Eyre, Wide Sargasso Sea and Frankenstein. After comparison of these three texts, we will find that there is something common in these three works——something unspoken. In Spivak’s point of view, it is not only about the theme of western culture, but also about the imperialism imposed upon the third world.

  15. UFUS-Imperial: nova cultivar de soja para o Estado de Mato Grosso UFUS-Imperial: new soybean cultivar for the State of Mato Grosso, Brazil

    Directory of Open Access Journals (Sweden)

    Osvaldo Toshiyuki Hamawaki

    2007-01-01

    Full Text Available A fim de ampliar as opções ao cultivo da soja, a Universidade Federal de Uberlândia lançou a cultivar UFUS-Imperial, proveniente do cruzamento entre (Msoy 8411xMsoy 8914 x (Emgopa 313xTucano. A cultivar apresentou resistência ao acamamento, à deiscência da vagem e aos patógenos: Fusarium solani, Cercospora sojina, Peronospora manshurica, Xanthomonas campestris pv. glycines e Diaporthe phaseolorum f.sp. meridionalis, e resistência parcial a Septoria glycines, Erysiphe diffusa e Phakopsora pachyrhizi. O rendimento dessa cultivar, em ensaios regionais, foi 45% superior ao da testemunha Msoy 6101, e é indicada para o Estado de Mato Grosso.With the purpose of offering new options for soybean production, the Universidade Federal de Uberlândia released the cultivar UFUS-Imperial, originated from the crosses between (Msoy 8411xMsoy 8914 x (Emgopa 313xTucano. It showed resistance to lodging, to pod shattering, and to the pathogens Fusarium solani, Cercospora sojina, Peronospora manshurica, Xanthomonas campestris pv. glycines and Diaporthe phaseolorum f.sp. meridionalis, and partial resistance to Septoria glycines, Erysiphe diffusa, and Phakopsora pachyrhizi. Its average yield from uniform trials was 45% higher than that of the control Msoy 6101, and it is indicated for cultivation in the State of Mato Grosso.

  16. Depositional architecture and evolution of inner shelf to shelf edge delta systems since the Late Oliocene and their respone to the tectonic and sea level change, Pear River Mouth Basin, northern South China Sea

    Science.gov (United States)

    Lin, Changsong; Zhang, Zhongtao; liu, Jingyan; Jiang, Jing

    2016-04-01

    The Pear River Mouth Basin is located in the northern continent margin of the South China Sea. Since the Late Oligocene, the long-term active fluvial systems (Paleo-Zhujiang) from the western basin margin bebouched into the northern continental margin of the South China Sea and formed widespread deltaic deposits in various depositional geomorphologies and tectonic settings. Based of integral analysys of abundant seismic, well logging and drilling core data, Depositional architecture and evolution of these delta systems and their respone to the tectonic and sea level change are documented in the study. There are two basic types of the delta systems which have been recognized: inner shelf delta deposited in shallow water enviroments and the outer shelf or shelf-edge delta systems occurred in deep water settings. The paleowater depths of these delta systems are around 30 to 80m (inner shelf delta) and 400-1000m (shelf-edge delta) estimated from the thickness (decompaction) of the delta front sequences. The study shows that the inner shelf delta systems are characterized by relatively thin delta forests (20-40m), numereous stacked distributary channel fills, relative coarse river mouth bar deposits and thin distal delta front or distal bar and prodelta deposits. In contrast, the outer shelf or shelf edge delta systems are characteristic of thick (300-800m) and steep (4-60) of deltaic clinoforms, which commonly display in 3D seismic profiles as "S" shape reflection. Large scale soft-sediment deformation structures, slump or debris flow deposits consisting mainly of soft-sediment deformed beds, blocks of sandstones and siltstones or mudstones widely developed in the delta front deposits. The shelf edge delta systems are typically associated with sandy turbidite fan deposits along the prodelta slopes, which may shift basinwards as the progradation of the delta systems. The delta systems underwent several regional cycles of evolution from inner shelf deltas to shelf edge

  17. Natural Vegetation Pattern over Northeast China in Late 17th Century%中国东北地区17世纪后期的自然植被格局

    Institute of Scientific and Technical Information of China (English)

    张学珍; 王维强; 方修琦; 叶瑜; 李蓓蓓

    2011-01-01

    We collected multiple historical documents including gazettes, government archives, traveling notes and so on, from which the primary natural vegetation information is complied. Using the information, the primary natural vegetation pattern prior to significant agriculture (i. e. late 17th century) was reconstructed. The results show that woodland and grassland were dominant vegetation over the Northeast China in the late 17th century.Woodland occupied the mountain areas, of which the northem of the Da Higgan Mountains was occupied by boreal forest, southern of the Changbai Mountains were covered by temperate broadleaf deciduous forest and the other mountains were occupied by mixed forest. Grassland covered Northeast China Plain and Inner Mongolia Plateau.The boundaries between woodland and grassland were nearly consistent with topography contour lines. Besides,swamp had small area and nearly covered the whole Sanjiang Plain. The macro pattern of historical nature vegetation was similar with the potential natural vegetation; however, the boundaries of woodland and grassland from the two datasets were evidently different and there was no swamp in potential natural vegetation dataset.%通过整理、分析历史文献中的自然植被记录,复原了中国东北地区近代大规模农垦前(17世纪后期)的自然植被格局.结果表明,当时的主导植被类型是森林和草地,森林主要分布于山区,其中大兴安岭北端主要是寒温带落叶针叶林,长白山南端主要是温带落叶阔叶林,其余山区是针阔混交林,草地主要分布于东北平原和内蒙古高原,林-草的分界线与地表等高线有很好的对应关系;在三江平原分布有大面积的沼泽.潜在植被格局与历史自然植被格局基本一致,但是林-草分界线有明显差异,且潜在植被图中没有沼泽.

  18. Religious Education in Russia: Inter-Faith Harmony or Neo-Imperial Toleration?

    Directory of Open Access Journals (Sweden)

    Elena Lisovskaya

    2016-04-01

    Full Text Available This paper explores the approach to religious education that has been instituted in Russia since 2012. The new policy’s manifestly proclaimed goals seem convergent with the values of religious freedom, self-determination, tolerance, and inter-faith peace that are espoused by Western liberal democracies. Yet Russia’s hidden religious education curriculum is far more consistent with a neo-imperial model of ethno-religious (Russian Orthodox hegemony and limited toleration of selected, other faiths whose reach is restricted to politically peripheral ethno-territorial entities. This model embodies and revitalizes Russia’s imperial legacies. Yet the revitalization is, in itself, an outcome of strategic choices made by the country’s religious and secular elites in the course of its desecularization. Building on discourse analysis of five Russian textbooks and a teacher’s manual, this article shows how the neo-imperial model manifests itself in the suppression of exogenous and endogenous pluralism, cultivation of the ideology of “ethnodoxy”, and in essentially imperialist mythology. The paper concludes by predicting the new model’s potential instability.

  19. Potential effects of geothermal energy conversion on Imperial Valley ecosystems. [Seven workshop presentations

    Energy Technology Data Exchange (ETDEWEB)

    Shinn, J.H. (ed.)

    1976-12-17

    This workshop on potential effcts of geothermal energy conversion on the ecology of Imperial Valley brought together personnel of Lawrence Livermore Laboratory and many collaborators under the sponsorship of the ERDA Imperial Valley Environmental Project (IVEP). The LLL Integrated Assessment Team identified the electric power potential and its associated effluents, discharges, subsidence, water requirements, land use, and noise. The Working Groups addressed the ecological problems. Water resource management problems include forces on water use, irrigation methods and water use for crops, water production, and water allocation. Agricultural problems are the contamination of edible crops and the reclamation of soil. A strategy is discussed for predevelopment baseline data and for identification of source term tracers. Wildlife resources might be threatened by habitat destruction, powerline impacts, noise and disturbance effects, gas emissions, and secondary impacts such as population pressure. Aquatic ecosystems in both the Salton Sea and fresh waters have potential hazards of salinity and trace metal effects, as well as existing stresses; baseline and bioassay studies are discussed. Problems from air pollution resulting from geothermal resource development might occur, particularly to vegetation and pollinator insects. Conversion of injury data to predicted economic damage isneeded. Finally, Imperial Valley desert ecosystems might be threatened by destruction of habitat and the possible effects on community structure such as those resulting from brine spills.

  20. Religious Education in Russia: Inter-Faith Harmony or Neo-Imperial Toleration?

    Directory of Open Access Journals (Sweden)

    Elena Lisovskaya

    2016-04-01

    Full Text Available This paper explores the approach to religious education that has been instituted in Russia since 2012. The new policy’s manifestly proclaimed goals seem convergent with the values of religious freedom, self-determination, tolerance, and inter-faith peace that are espoused by Western liberal democracies. Yet Russia’s hidden religious education curriculum is far more consistent with a neo-imperial model of ethno-religious (Russian Orthodox hegemony and limited toleration of selected, other faiths whose reach is restricted to politically peripheral ethno-territorial entities. This model embodies and revitalizes Russia’s imperial legacies. Yet the revitalization is, in itself, an outcome of strategic choices made by the country’s religious and secular elites in the course of its desecularization. Building on discourse analysis of five Russian textbooks and a teacher’s manual, this article shows how the neo-imperial model manifests itself in the suppression of exogenous and endogenous pluralism, cultivation of the ideology of “ethnodoxy”, and in essentially imperialist mythology. The paper concludes by predicting the new model’s potential instability.

  1. 林则徐与科举%Lin Zexu And Imperial Examination

    Institute of Scientific and Technical Information of China (English)

    张媛媛

    2012-01-01

    Lin Zexu plays a decisive role in modern history, and in the imperial examinations, he also occupies a space. As the examination official, he reformed some of the disadvantages in imperial examination, and made some achievements. By the study of the relationship between Lin Zexu and the imperial examination , we can get some enlightenment.%林则徐是中国近代史上举足轻重的人物,在科举史上同样占有一席之地。在家庭以及社会的影响下林则徐走上了科举之路,并最终金榜题名。作为科考试官他公正衡文、选拔真才,并在江南乡试期间改革科场弊端,取得了一定成效。林则徐提倡“经世致用”,并且贯彻于书院教育和科举考试之中,以期士子能关注社会现实,解决社会实际问题。通过考察林则徐与科举的关系,试图从中得到一些启示。

  2. The Empire Bites Back: Sherlock Holmes as an Imperial Immune System

    Directory of Open Access Journals (Sweden)

    Laura Otis

    1998-01-01

    Full Text Available Trained as a physician in the bacteriological age, Sir Arthur Conan Doyle created a detective-hero who acts both like a masterful bacteriologist and an imperial immune system. Doyle's experiences as a doctor in South Africa taught him that the colonies' microbes were his Empire's worst enemy. In 1890, Doyle visited Berlin, where Robert Koch was testing a "cure" for tuberculosis, and in Doyle's subsequent character sketch of Koch, the scientist sounds remarkably like Sherlock Holmes. Based on Doyle's medical instructor Joe Bell, Holmes shares Koch's relentless drive to hunt down and unmask tiny invaders. Imperialism, by the 1880s, had opened Europe to the peoples, cultures, and diseases of the lands it claimed. Holmes plays a defensive role, as an imperial intelligence network to detect foreigners "passing" in British society. The revenge, blackmail, and counterfeiting around which the Holmes stories are built reflect readers' anxieties about infiltration, about punishment for their colonial theft, and about the legitimacy of their own identity in a socio-economic system built on contradictions. Holmes thus responds to conflicting social demands, exposing interlopers who mimic traditional signs of respectability, and protecting "respectable" citizens from the consequences of their colonial crimes.

  3. Mineralogical and compositional characteristics of Late Permian coals from an area of high lung cancer rate in Xuan Wei, Yunnan, China: Occurrence and origin of quartz and chamosite

    Science.gov (United States)

    Dai, S.; Tian, L.; Chou, C.-L.; Zhou, Y.; Zhang, M.; Zhao, L.; Wang, Jingyuan; Yang, Z.; Cao, H.; Ren, D.

    2008-01-01

    Some townships in Xuan Wei County, Yunnan Province, have one of the highest lung cancer mortality rates in China and the epidemic disease in the area has generally been attributed to the polycyclic aromatic hydrocarbons (PAHs) released from domestic coal burning. However, the cancer-causing culprit is not settled as Tian [Tian, L., 2005. Coal Combustion Emissions and Lung Cancer in Xuan Wei, China. Ph.D. thesis, University of California, Berkeley.] found nanometer quartz in these coals, soot emissions, and lung cancer tissues. We have conducted mineralogical and geochemical studies of the coals from Xuan Wei for the purpose of shedding light on the minerals which may be related to the epidemic lung cancer. In this paper, abundances, modes of occurrence, and origins of minerals and elements in the coals from two mines in Xuan Wei have been studied using optical microscope, low-temperature ashing, X-ray diffraction analysis, scanning electron microscope equipped with energy-dispersive X-ray spectrometer, and inductively-coupled plasma mass spectrometry. The minerals in the coals are mainly composed of quartz, chamosite, kaolinite, and calcite. The particle size of quartz is rather small, mostly less than 20????m and it is of authigenic origin. Chamosite occurs mainly as cell-fillings. The occurrence of quartz and chamosite indicates that they were derived from the hydrothermal fluids. Epigenetic calcite is derived from calcic fluids. Kaolinite is derived mainly from sediment source region of Kangdian Oldland to the west of coal basin. The composition of Xuan Wei coal is high in SiO2, Fe2O3, TiO2, CaO, MnO, V, Co, Ni, Cu, and Zn. The high SiO2 content is attributed to quartz, and the Fe2O3 content to chamosite. The high Mn and low Mg contents in the coal indicate the inputs of hydrothermal fluids. CaO occurs mainly in epigenetic calcite. Elements Ti, Co, Ni, Cu, Zn, and rare earth elements were derived from the basaltic rocks at sediment source region. ?? 2008

  4. Sequence of Late Jurassic-Early Cretaceous magmatic-hydrothermal events in the Xiong'ershan region, Central China: An overview with new zircon U-Pb geochronology data on quartz porphyries

    Science.gov (United States)

    Deng, Jun; Gong, Qingjie; Wang, Changming; Carranza, Emmanuel John M.; Santosh, M.

    2014-01-01

    Recent investigations have revealed several large Au and Mo deposits in the Xiong'ershan region, Central China. Most quartz porphyries associated with the mineralization occur as dikes and apophyses, or as rubbles cemented in mineralized breccia pipes. Three types of quartz porphyries were sampled from the Leimengou Mo deposit, the Qiyugou Au deposit, and the Niutougou Au deposit. LA-ICP-MS zircon U-Pb analysis was performed in zircons from two quartz porphyries; the results yielded ages of 125.4 ± 0.77 Ma for Leimengou Mo deposit and 150.1 ± 1.1 Ma for Qiyugou Au deposit. The magma source of Leimengou quartz porphyry is similar to that of the mineralized cementing material in breccia pipes of the Qiyugou Au deposit, whereas the magma source of Qiyugou quartz porphyry is the same as that of quartz porphyries in Niutougou Au deposit. Based on the new U-Pb isotopic ages of granitic plutons reported in this study, together with the age data in the literature, we identify distinct magmatic pulses in the Xiong'ershan region at ca.160, 150, 143, 133, 125, and 115 Ma during the Late Jurassic-Early Cretaceous. The ages of Au and Mo mineralization coincide with the thermal events at about 115, 125, 133, and 143 Ma are considered to be co-eval with granitic magmatism. No mineralization ages of 150 and 160 Ma thermal events have been previously reported. Our study demonstrates Late Jurassic-Early Cretaceous multiple magmatic pulses and mineralization in the Xiong'ershan region.

  5. Geochemistry and zircon ages of mafic dikes in the South Qinling, central China: evidence for late Neoproterozoic continental rifting in the northern Yangtze block

    Science.gov (United States)

    Zhu, Xiyan; Chen, Fukun; Liu, Bingxiang; Zhang, He; Zhai, Mingguo

    2015-01-01

    Neoproterozoic volcanic-sedimentary sequences of the southern Qinling belt, central China, were intruded by voluminous mafic dikes. secondary ion mass spectrometry zircon U-Pb dating indicates that these dikes were emplaced at 650.8 ± 5.2 Ma, coeval with mafic rocks occurring at the northern margin of the Yangtze block. The dikes are characterized by enrichment of large ion lithophile elements, high Ti contents (up to 3.73 wt%) and Nb/Ta ratios between 14.5 and 19.6, suggesting a mantle source of oceanic island basalt affinity. Initial 87Sr/86Sr ratios show positive correlation with SiO2 contents and negative correlation with Zr/Nb ratios, implying that these rocks were affected by crustal contamination during the magma ascend and emplacement process. The dikes have initial ɛ Nd values of +0.2 to +3.3, low 206Pb/204Pb ratios of 16.96-17.45, and moderate 87Sr/86Sr ratios of 0.7043-0.7076, likely pointing to the involvement of an enriched mantle source. The mafic dikes and coeval mafic volcanic equivalents in the South Qinling and the northern Yangtze are hypothesized to be related with the prolonged breakup of the supercontinent Rodinia, suggesting that continental rifting lasted until ca. 650 Ma.

  6. Composition and distribution of planktonic ciliates in the southern South China Sea during late summer: Comparison between surface and 75 m deep layer

    Science.gov (United States)

    Liu, Huaxue; Shen, Pingping; Li, Chunhou; Chen, Zuozhi; Qi, Zhanhui; Huang, Honghui

    2016-02-01

    Ciliates are very important components in most marine ecosystem. They are trophic link between the microbial food web and grazing food chain. In this study, ciliates were collected from 11 sites in the southern South China Sea (SCS) during August 25 to September 28, 2011. Their composition and distribution at the surface and 75 m deep depth of the ocean were studied. A total of 30 species belonging to 22 genera were identified, and 22 species of 15 genera were Tintinnids. Eutintinnus fraknoii and E. stramentus were the most common species. The other dominants were strombidiids ciliates including Strombidium conicum and S. globosaneum, which were followed by the tide form, Mesodinium pulex. Ciliates abundance ranged from 46 ind L-1 to 368 ind L-1 in the open sites, 46-368 ind L-1 at surface and 73-198 ind L-1 at 75 m deep layer. In the Yongshu reef, ciliates abundance ranged from 167 ind L-1 to 365 ind L-1 in the water column, similar to that in Sanya coral reef waters. Ciliates composition showed obvious difference between surface and 75 m deep layer at station S2 ( P deep layer, salinity was negatively related to mixed layer depth ( P < 0.05), but positively to chlorophyll a concentration ( P < 0.05), indicating that the change of vertical mixing in water column influenced vertical distribution of ciliates in the southern SCS.

  7. An endemic rat species complex is evidence of moderate environmental changes in the terrestrial biodiversity centre of China through the late Quaternary

    Science.gov (United States)

    Ge, Deyan; Lu, Liang; Cheng, Jilong; Xia, Lin; Chang, Yongbin; Wen, Zhixin; Lv, Xue; Du, Yuanbao; Liu, Qiyong; Yang, Qisen

    2017-01-01

    The underlying mechanisms that allow the Hengduan Mountains (HDM), the terrestrial biodiversity centre of China, to harbour high levels of species diversity remain poorly understood. Here, we sought to explore the biogeographic history of the endemic rat, Niviventer andersoni species complex (NASC), and to understand the long-term persistence of high species diversity in this region. In contrast to previous studies that have proposed regional refuges in eastern or southern of the HDM and emphasized the influence of climatic oscillations on local vertebrates, we found that HDM as a whole acted as refuge for the NASC and that the historical range shifts of NASC mainly occurred in the marginal regions. Demographic analyses revealed slight recent population decline in Yunnan and south-eastern Tibet, whereas of the populations in Sichuan and of the entire NASC were stable. This pattern differs greatly from classic paradigms of temperate or alpine and holarctic species. Interestingly, the mean elevation, area and climate of potential habitats of clade a (N. excelsior), an alpine inhabitant, showed larger variations than did those of clade b (N. andersoni), a middle-high altitude inhabitant. These species represent the evolutionary history of montane small mammals in regions that were less affected by the Quaternary climatic changes. PMID:28393882

  8. Models of pure CO2 and pure CH4 adsorption on the late paleozoic coals from the Kailuan Coalfield, Hebei, China

    Science.gov (United States)

    Dai, S.; Zhang, B.; Peng, S.; Zhang, X.; Chou, C.

    2009-01-01

    Isothermal adsorption experiments of pure CO2 and CH4 on different coals in rank (the No. 11 Coal from the Linnancang Mine and the No. 9 Coal from the Majiagou Mine) from the Kailuan Coalfield of Hebei Province, China, have been studied. Four different models (Langmuir, BET, D-R, and D-A) were used to fit the experimental data of CO2 and CH4 adsorption and their fitting degree were investigated. The results showed that the adsorption capacity of the Majiagou coal(Ro, ran = 1. 21%) is higher than that of the Linnancang coal (Ro, ran = 0. 58%). The adsorption capacity of CO2 is higher than that of CH4 on the same coal under the same pressure. The adsorption isotherms of pure CO 2 and pure CH4 on the Majiagou coal can be classified as Type I and their fitting errors of curves are very weak; thus the experimental data can be presented using the Langmuir isotherm. However, the adsorption of Linnancang coal is more complicated, and can be presented using D-A model because of its minimum error. Monolayer adsorption occurs during the adsorption of pure CO2 and pure CH4 on the No. 11 Coal and that of pure CH4 on the No. 9 Coal.

  9. Application of geochemical logging for palaeoenvironmental research in the Late Cretaceous Qingshankou Formation from the Chinese Continental Scientific Drilling Project-SK-2e, Songliao Basin, NE China

    Science.gov (United States)

    Peng, Cheng; Zou, Changchun; Pan, Li; Niu, Yixiong

    2017-08-01

    The Chinese Continental Scientific Drilling Project of the Cretaceous Songliao Basin (CCSD-SK) provides an excellent opportunity to understand the response of terrestrial environments to greenhouse climate change in the Cretaceous. We conducted a palaeoenvironmental study of the Late Cretaceous Qingshankou Formation (K2qn) based on geochemical log data from the SK-2 east borehole. According to the characteristic of Ti mainly from terrigenous minerals, the content of authigenic elements was calculated. Correlation space was proposed to study the variation of the correlation between two log curves along the depth. Palaeoenvironmental proxies were selected from log data to study the evolution of the climate and lake, productivity of the paleolake, and organic matter deposition. The results demonstrate that the productivity of the paleolake was driven by chemical weathering in K2qn, in which the first section of the Qingshankou Formation (K2qn1) has higher productivity than the second and third sections of the Qingshankou Formation (K2qn2+3). The high content of pyrite in several thin layers reveals lake water of high sulfate concentration. This may have been caused by acid rain related to large volcanic activity. In K2qn2+3, several periods of high productivity without the formation of source rocks and high organic matter content were identified. This may show that organic matter deposition was limited by low accommodation space or oxidation environment. Therefore, the preservation condition is suggested as the main controlling factor of organic matter deposition in K2qn.

  10. Cultural imperialism or ”soft imperial power” in the XXIst century global order1 (Imperialismul cultural sau „puterea imperială soft” în ordinea globală a secolului XXI

    Directory of Open Access Journals (Sweden)

    Mădălina Virginia ANTONESCU

    2014-09-01

    Full Text Available Although some of the authors of the relevant literature believe that the phrase “cultural imperialism” is a subtle, “soft” form of domination, which does not involve an open, visible or military political control (in realistic terms, other scholars maintain that this is one of the methods most commonly used by imperial policy in today’s globalist age. The connection of this term with paradigms such as “the clash of civilisations”, “the end of history” or “complex interdependencies” provides a multi-layered perspective on the postmodern world at the beginning of 21st century, a world where soft power is exercised at global, regional, transnational or infra-local level, within an economic, social and cultural framework that has not yet been regulated as such by the classical institutions of the Westphalian order.

  11. Contribution of Chinese students studying physics in Japan to from the late 19th to early 20th century modern physics in China%清末民初留日物理学生及其科学贡献

    Institute of Scientific and Technical Information of China (English)

    咏梅; 冯立昇

    2011-01-01

    Aim Introduce the general situation of Chinese students who studied physics in Japan in the late 19th and early 20th century to provide new clue for the study of the history of physics. Methods Literature research and statistical analysis. Results Analyze statistically their school distribution in Japan, and introduce briefly 109 students'materials such as their native places, their major subjects, their schools in Japan, as well as their work;and study their work and activities in the physics fields when they came back to China. We describe their contribution to the spread and education of physics science, to the determination of technical terms, as well as to the academic study in the field of physics. Conclusion The Chinese students studying physics in Japan had played an important role to the development of Physics in China in the early 20th century after returning to China.%目的 清理清末民初留日物理学生的总体脉络,为研究中国近代物理学史提供新线索.方法 文献调研和统计分析.结果 统计分析中国留日学生就读学校的分布情况;收集109名晚清留日物理学生的资料,介绍其籍贯、在日就读学校、专业及事迹,考查清末民初留日学生归国后的有关物理学方面的活动.阐述了这批留学生对于民国时期的物理学普及、物理学教育、物理术语创制、物理研究等方面的贡献.结论 认为清末的留日物理学生为中国物理学的体制化发挥了重要作用.

  12. 西藏申扎地区晚古生代地层岩石磁学研究%Rock Magnetism of the Late Paleozoic in Xainza area of Tibet,West China

    Institute of Scientific and Technical Information of China (English)

    程鑫; 闫昭圣; 鱼磊; 彭喜明; 魏娜娜; 吴汉宁; 郭强; 侯宝宁; 王宝江; 康伟伟; 梁利平; 石月; 刘钊

    2012-01-01

    目的 研究西藏申扎地区晚古生代地层载磁矿物特征,为构造磁学等提供依据.方法 运用饱和等温剩磁( SIRM),三轴等温剩磁(SIRM)热退磁,磁化率-温度(x-T)曲线和NRM热退磁实验等方法进行综合分析.结果 中—上二叠统样品中含较多针铁矿、赤铁矿;下二叠统和石炭系样品中以磁铁矿为主;泥盆系样品中富集铁硫化物.结论 该套沉积地层中具有不同磁学特征的磁性矿物共生组合,可能导致岩石剩磁获得过程相对复杂;剖面上磁性矿物组合的变化,蕴含着沉积环境演化的信息.%Aim The Gandise block located in the northern margin of Gondwana continent. Gandise marine depos-its can help to trace evolutionary history of the Paleo-Tethys in northern Gondwana. Late Paleozoic successions, yielding diversified fossils, are well-exposed in the Xainza area, located in the central part of the Gandise block. Paleozoic strata seen in Zakang of Xainza is known as the best developed in northern Tibet and would provide key insights into the study of Paleozoic tectonic movement and evolution of the Qinghai-Tibet Plateau. This study pro-vides new insights for studying paleomagnetism and magnetostratigraphy in the Xainza area of Tibet, west China. Methods Rock Magnetism experiments, including progressive acquisition of IRM, thermal demagnetization of a three-component IRM, temperature-dependent magnetic susceptibility measurements, and the thermal demagnetiza- tion, were conducted on the Late Paleozoic deposits recovered from the Zakang section. Results The results show that middle and late Permian sediments have high contents of goethite and hematite; early Permian and Carbonifer-ous sediments are dominated by magnetite; and Devonian sediments are rich in ferromagnetic iron sulfides. Conclu-sion The diversified magnetic mineral paragenesis in a set of sedimentary strata, may lead to the rock IRM acqui-sition a relatively complex process; magnetic mineral

  13. Charonosaurus jiayinensis n.g., n.sp.,a lambeosaurine dinosaur from the Late Maastrichtian of northeastern ChinaCharonosaurus jiayinensis n.g., n.sp., un dinosaure lambéosauriné du Maastrichtien supérieur du Nord-Est de la Chine.

    Science.gov (United States)

    Godefroit, Pascal; Zan, Shuqin; Jin, Liyong

    2000-06-01

    Large bonebeds have been excavated in the Late Maastrichian Yuliangze Formation near Jiayin (Heilongjang Province, northeastern China). The greatest part of the discovered fossils belong to a new lambeosaurine dinosaur, Charonosaurus jiayinensis n.g., n.sp. Phylogenetic analysis, based on 33 cranial, dental and postcranial characters, indicates that this new taxon may be closer to Parasaurolophus than any other known Lambeosaurinae. The Late Maastrichtian dinosaur faunas currently known in northeastern Asia are dominated by Lambeosaurinae, although these dinosaurs are not represented any more in synchronous North American and European localities.

  14. High-precision U-Pb geochronologic constraints on the Late Cretaceous terrestrial cyclostratigraphy and geomagnetic polarity from the Songliao Basin, Northeast China

    Science.gov (United States)

    Wang, Tiantian; Ramezani, Jahandar; Wang, Chengshan; Wu, Huaichun; He, Huaiyu; Bowring, Samuel A.

    2016-07-01

    The Cretaceous continental sedimentary records are essential to our understanding of how the terrestrial geologic and ecologic systems responded to past climate fluctuations under greenhouse conditions and our ability to forecast climate change in the future. The Songliao Basin of Northeast China preserves a near-complete, predominantly lacustrine, Cretaceous succession, with sedimentary cyclicity that has been tied to Milankocitch forcing of the climate. Over 900 meters of drill-core recovered from the Upper Cretaceous (Turonian to Campanian) of the Songliao Basin has provided a unique opportunity for detailed analyses of its depositional and paleoenvironmental records through integrated and high-resolution cyclostratigraphic, magnetostratigraphic and geochronologic investigations. Here we report high-precision U-Pb zircon dates (CA-ID-TIMS method) from four interbedded bentonites from the drill-core that offer substantial improvements in accuracy, and a ten-fold enhancement in precision, compared to the previous U-Pb SIMS geochronology, and allow a critical evaluation of the Songliao astrochronological time scale. The results indicate appreciable deviations of the astrochronologic model from the absolute radioisotope geochronology, which more likely reflect cyclostratigraphic tuning inaccuracies and omitted cycles due to depositional hiatuses, rather than suspected limitations of astronomical models applied to distant geologic time. Age interpolation based on our new high-resolution geochronologic framework and the calibrated cyclostratigraphy places the end of the Cretaceous Normal Superchon (C34n-C33r chron boundary) in the Songliao Basin at 83.07 ± 0.15 Ma. This date also serves as a new and improved estimate for the global Santonian-Campanian stage boundary.

  15. Population Structure of the Raccoon Dog on the Grounds of the Imperial Palace, Tokyo, Revealed by Microsatellite Analysis of Fecal DNA.

    Science.gov (United States)

    Saito, Wataru; Amaike, Yosuke; Sako, Takako; Kaneko, Yayoi; Masuda, Ryuichi

    2016-10-01

    The raccoon dog (Nyctereutes procyonoides, Canidae, Carnivora) is highly adaptable to urban environments. Populations of carnivorans inhabiting urban areas sometimes differ ecologically and genetically from those in rural areas. However, there is little information on urban raccoon dogs. This study focused on raccoon dog populations in Tokyo, one of the most highly urbanized cities in the world. We examined the genotypes of 10 microsatellites for 101 fecal samples from raccoon dogs inhabiting the grounds of the Imperial Palace, a green space in central Tokyo. We successfully genotyped 58 samples originating from 31 individuals. We also analyzed muscle tissue samples from raccoon dogs from the grounds of the Imperial Palace, the Akasaka Imperial Grounds (a green space close to the Imperial Palace), and the surrounding urban area, and then investigated the genetic structure and diversity of these populations, and the genetic differentiation among them. The population on the grounds of the Imperial Palace was genetically differentiated from that in the Akasaka Imperial Grounds, suggesting that the roads and buildings act as barriers to gene flow. In addition, the population on the grounds of the Imperial Palace showed greater genetic difference from that in the surrounding area than that in the Akasaka Imperial Grounds. We speculate that the moats around the Imperial Palace restrict individual ranges within the palace grounds and limit migration and gene flow to other areas.

  16. Detrital zircon dating and tracing the provenance of dinosaur bone beds from the Late Cretaceous Wangshi Group in Zhucheng, Shandong, East China

    Directory of Open Access Journals (Sweden)

    Wei An

    2016-01-01

    Full Text Available The mass burial of dinosaur bone fossils in the Late Cretaceous Wangshi Group in Zhucheng, Shandong Province has been a research focus in recent years. However, the provenance of the dinosaur bone fossils and the accurate depositional age of the bone beds remain ambiguous. Through U–Pb dating of detrital zircons collected from six conglomerate samples from the dinosaur bone beds, we found that the youngest single grain age (YSG of sample 090414-24-D was 77.3 Ma, representing the maximum depositional age of the dinosaur fossil beds and sediments. This also indicates that the Hongtuya Formation was deposited during the Campanian. Dating results revealed an age peak of 120–110 Ma, which corresponds with the peak age of volcanic rocks of the Lower Cretaceous Qingshan Group. The volcanic rocks of the Qingshan Group are mainly exposed in Laiyang, to the north of Zhucheng, although a few also appear to the south and northwest. Through analysis of conglomerate composition and palaeocurrents in the sediments containing the bone beds, we found that the three different data sets of gravel compositions of the conglomerates were mainly composed of volcanic or pyroclastic rocks. Three different data sets of palaeocurrents suggested that the main sediment source of the Wangshi Group dinosaur bone beds was from the north−northwest of the Basin. Only one data set had a provenance south of the basin. This study revealed that the areas of Laiyang and the Yishu Fault Zone were the main provenance areas of both the dinosaur bone fossils and the sediments of the Wangshi Group in Zhucheng. The southern margin of the Zhucheng Basin may be a secondary source area. This research provides an important basis for judging the deposition time and the sediment source of fossil layers in the Wangshi Group, as well as reconstructing the palaeogeography of the Wangshi Group in the Jiaolai Basin.

  17. Crustal-mantle detachment of the North China craton in Late Mesozoic: Rheological constraints%华北克拉通晚中生代壳-幔拆离作用:岩石流变学约束

    Institute of Scientific and Technical Information of China (English)

    刘俊来; 纪沫; 夏浩然; 刘正宏; 周永胜; 余心起; 张宏远; 程素华

    2009-01-01

    Rheological structure of the continental lithosphere fundamentally influences on the deep processes of the lithosphere (crust/mantle process), which is directly shown by the crust-mantle structure of the lithosphere and also by shallow structures. Crustal extension, detachment faulting and thinning of the crust during thinning of the lithosphere of North China craton in Late Mesozoic are exactly shown by occurrence and variation of macro-and micro-structures, and due to changing rheology of the crust. The inhomogeneity of Late Mesozoic lithosphere is deduced from the present geophysical lithosphere structure and regional structural analysis. Lithosphere rheology is influenced by several factors including the absence and presence of H_2O dominated geological fluids. Coupling and decoupling relationships of the crust and mantle during regional extension of the lithosphere of North China craton are discussed from the variation of thicknesses of the crust, the lithosphere mantle and the lithosphere, and the varying contents of water in rocks from the lower crust and upper mantle. We present the crust-mantle detachment model to interpret the basic phenomena and deep processes for lithosphere thinning of North China craton during Late Mesozoic. We would argue that regional extension is the dominant dynamic factor of lithosphere thinning during Late Mesozoic. During this event, the crust and mantle are decoupled in the eastern part of the craton, and therefore, the upper crust, the lower crust and the upper mantle are detached at the same time, but in different ways. There is, however, a coupling relationship in the western part of the craton. Thus the lower crust and the upper mantle constitute a layer of high rheological strength and they are not strongly detached during extension of the lithosphere in Late Mesozoic.%大陆岩石圈的流变学结构对于岩石圈深部过程(壳/幔过程)有着深刻的影响,直接表现在岩石圈壳-幔结构与浅部构造上.

  18. FLUCTUACIONES ECONÓMICAS EN LA AMPURIAS ROMANA DE ÉPOCA ALTO-IMPERIAL (Economic fluctuations in Roman Ampurias during early imperial times

    Directory of Open Access Journals (Sweden)

    Pascual Izquierdo-Egea

    2010-09-01

    Full Text Available La aplicación del método de valoración contextual al análisis del gasto funerario en la Ampurias romana de época alto-imperial, ha evidenciado la enorme utilidad de esta herramienta en la reconstrucción económica y social del pasado de esta ciudad. Se han aislado las diversas fluctuaciones económicas registradas en los ajuares de las tumbas, desde la época de Augusto hasta la primera mitad del siglo II de nuestra era, confirmando lo que ya apuntaban las fuentes literarias y arrojando más luz sobre la naturaleza de tales cambios. También se han detectado crisis tan relevantes como la de tiempos de Tiberio y oscilaciones monetarias. Todo ello viene a probar la extraordinaria importancia de esta metodología para ampliar nuestro conocimiento objetivo de la sociedad romana y de muchas otras civilizaciones y pueblos de la antigüedad. ENGLISH: The application of a contextual appraisal method to the analysis of funerary expense in early imperial Roman Ampurias, has shown the enormous utility of this tool for the economic and social reconstruction of the history of this city. Various economic fluctuations have been documented in the record of grave goods, from the time of Augustus to the first half of the second century AD, confirming information already indicated by literary sources and shedding more light on the nature of these changes. Economic crises were identified, including some as significant as those experienced during the Tiberius period, as well as currency fluctuations. This serves to demonstrate the extraordinary importance of the contextual approach to expand not only our knowledge of Roman society, but also of many other civilizations and peoples of antiquity.

  19. [Academic presentation of neurology and psychiatry of Keijo Imperial University at annual meetings].

    Science.gov (United States)

    Kanekawa, Hideo

    2012-01-01

    The origin of Keijo Imperial University, Medical School, Psychiatry course, and presentation at the Annual Meetings of the Japanese Society of Psychiatry and Neurology and The Japanese Society of Psychiatry and Neurology were investigated from its establishment to 1945. Keijo was the name used for the capital city of Korea, Seoul, when Korea was under Japanese rule. We believe the Keijo Imperial University evolved out of the Governor-General of Korea Hospital and Keijo Medical Professional School. The first Professor at the University was Shinji Suitsu, who studied under Shuzo Kure. He visited Shizuoka prefecture when he collaborated in Kure's "Actual situation and statistical observation on home custody of mental patients" (1918). This was confirmed by photographic materials from this time. The year after the visit to Shizuoka, Suitsu was sent to the Korean Peninsula. In 1913, Suitsu established the Department of Psychiatry at the Governor-General of Korea Hospital, and the institution had 500 tsubo (approximately 1,650 m2) of land within Keijo (Seoul), with floor space of 160 tsubo (approximately 528 m2) and 24 beds. Treatments were performed by Suitsu, an assistant, and 8-9 nurses. The number of hospitalized patients was 30-50 patients per year. Cells had floor heating. Keijo Imperial University was established in 1924, and was called Jodai. In 1925, Suitsu retired from his Professorship of Psychiatry at Keijo Medical Professional School. Suitsu was from Kyoto Imperial University, and had studied abroad. In 1925, Suitsu's father-in-law, and a long-time friend of Shuzo Kure, Seiji Yamane, passed away. The professor who took up the position after Suitsu was Kiyoji Kubo, who was originally supposed to go to Hokkaido Imperial University. When the medical school was established at Keijo Imperial University in 1926, Kubo was offered a professorship there. Jodai was under the jurisdiction of the Governor-General of Korea, and not the Ministry of Education. Later

  20. 中国晚中新世陆相哺乳动物群序列: 陕西蓝田的新证据%LAND MAMMAL FAUNAL SEQUENCE OF THE LATE MIOCENE OF CHINA:NEW EVIDENCE FROM LANTIAN, SHAANXI PROVINCE

    Institute of Scientific and Technical Information of China (English)

    2002-01-01

    Newly discovered fossil taxa and preliminary revision of the old collection from the Bahe and Lantian formations allow a re-interpretation of the mammalian faunal sequence of the Chinese Late Miocene.The distribution of fossil taxa in the strata shows a major turnover event within the late Miocene, at a time slightly preceding the edimentological change represented by the boundary between the Bahe and Lantian Formations (ca. 7Ma). The mammal fauna postdating the change shows a strong resemblance to the classic Baodean mammal faunas of North China. Based on this turnover event a resurrection of the Bahean Land Mammal Age, predating the Baodean LMA within the late Miocene, would be possible. The Bahear/Baodean turnover event was ecological as well as taxonomic and suggests significant climatic change at this time, possibly driven by onset or intensification of the East Asian summer monsoon circulation system.

  1. The Chronology and Characteristics of Sediments Since Late Glacial in Huahai Lake, Hexi Corridor, NW China%河西走廊花海剖面晚冰期以来年代学及沉积特征研究

    Institute of Scientific and Technical Information of China (English)

    王乃昂; 李卓仑; 李育; 朱金峰

    2011-01-01

    选择位于河西走廊的花海古湖泊沉积剖面作为研究对象,根据13个普通14C和5个AMS14C年代结果,以沉积物岩性特征为主要指标,建立了晚冰期以来花海湖泊沉积的年代框架及环境变化过程.结果表明:花海地区新仙女木期和晚冰期花海湖泊主要以芒硝沉积为主,指示了较低的温度环境.芒硝沉积中的淤泥细线为短暂升温标志,芒硝-淤泥-芒硝的沉积韵律揭示了晚冰期和新仙女木期气候的不稳定性和温度的周期性变化.根据沉积过程和岩性特征,全新世花海湖泊在千年尺度上存在干湿变化特征.10.47 cal ka BP之前的早全新世气候较为干旱,以冲洪积和风成砂为主的沉积过程,10.47~8.87 cal ka BP的早全新世湖相沉积所揭示的气候由干到湿的转变期,8.87~5.5 cal ka BP存在深湖相沉积的气候湿润期,5.5 cal ka BP至今沉积间断所揭示的中晚全新世气候呈现干旱化趋势,湖泊趋于萎缩干涸.%From the profile which is located in the Hexi Corridor, NW China. 13 samples were collected for conventional 14C dating and 5 samples were collected for AMS 14C dating. The materials used for 14C dating were seeds, mud and wood. Based on the dating results, we reconstructed the age framework of Huahai Lake since the Late Glacial period. And then, we concluded that the sediments between 0.73 ~ 6.83 m were deposited during Holocene. Between 6.83 ~ 7.35 m, the sediments were deposited during the early Holocene and the late Younger Dryas. The sediments of 7.35 ~ 10.44 m were deposited during the Late Glacial and early Younger Dryas. Based on the mineral analysis of the sediments during the Younger Dryas and late glacial, mirabilite was the main component in the sediments, indicating the low-temperature environment. According to the chemical composition analysis , the main ingredient of the pure mirabilite deposition is Na2SO4 0 10H2O, which is an indicator of the cold-dry environment

  2. 从商标牌号纠纷诉讼看清末民初商民的商标法律意识%Trademark Legal Awareness of Merchants in the Late Qing Dynasty and the Early Republic of China

    Institute of Scientific and Technical Information of China (English)

    王雪梅

    2015-01-01

    1923年《商标法》颁布之前的清末民初,我国民商事活动仍然处于商标制定法缺失时期。从当时国内商标牌号的一些纠纷诉讼案及其裁判、处罚情况,可以看出清末民初我国商民的商标法律意识的一些特点:商标专用权意识薄弱;对商标侵权的内涵界定认识不清;商标注册意识淡薄;对商标的保护和对商标纠纷诉讼的裁判、处罚仍摆脱不了传统行为方式和商业惯例的影响等等。这些特点是由于我国长期以来缺少对知识产权的保护,商民商标法律意识、观念的形成与提升滞后于商标法制建设本身所致。这些情况又进而降低了《商标法》实施的实际效果。%The period of the late Qing dynasty and the early Republic of China before 1923 when the Trademark Act was issued was still a period lack of legislation of trademark laws in civil commercial ac⁃tivity. Based on the dispute lawsuits concerning the trademarks and brands in China at that time as well as their judgments and punishment, features of legal awareness in trademarks then can be concluded as weak awareness of exclusive right to trademark use and of trademark registration, implicit knowledge on the connotative definition of trademark infringement. Trademark protection and judgments and punishment of the trademark lawsuits were greatly influenced by traditional behaviors and business practices. All those features originate from the lack of intellectual property protection, along with the forming and upgrading of the legal awareness and concepts concerning trademarks lagging behind the legal construction of trade⁃mark, which reduces the actual effect of Trademark Act implementation.

  3. Geochronology and geochemistry of late Carboniferous-middle Permian I- and A-type granites and gabbro-diorites in the eastern Jiamusi Massif, NE China: Implications for petrogenesis and tectonic setting

    Science.gov (United States)

    Bi, Jun-Hui; Ge, Wen-Chun; Yang, Hao; Wang, Zhi-Hui; Xu, Wen-Liang; Yang, Jin-Hui; Xing, De-He; Chen, Hui-Jun

    2016-12-01

    Late Carboniferous-middle Permian magmatism in the Jiamusi Massif of northeast China, in the eastern segment of the Central Asian Orogenic Belt (CAOB), provides critical evidence regarding the tectonic history and geodynamic processes in the region. The gabbro-diorites of the Longtouqiao pluton and two groups of coeval granite in the study area comprise a bimodal magmatic suite. Precise LA-ICP-MS U-Pb zircon ages indicate that the granitoids and gabbro-diorites were emplaced in the late Carboniferous-middle Permian (302-267 Ma). Group I granites have high SiO2 (70.75-77.04 wt.%) and K2O (3.65-5.89 wt.%) contents, are enriched in LILEs (e.g., Rb, Th, and U) relative to HFSEs and LREEs, and have negative Nb, Ta, P, and Ti anomalies, which collectively indicate affinities with subduction-related magmas. Group II granites are weakly peraluminous (A/CNK = 1.03-1.07) and are characterized by enrichment in alkalis (Na2O + K2O = 8.22-8.90 wt.%), low MgO (0.04-0.09 wt.%) and P2O5 (0.01-0.04 wt.%) contents, high Zr and Nb contents, high 10,000 × Ga/Al ratios, and they are geochemically similar to aluminous A-type granites. All the magmatic zircons in these granitoids have great variations of εHf(t) (+ 7.89 to - 5.60) and two-stage Hf model ages (TDM2) of 0.8-1.7 Ga, which suggest that the precursor magmas originated from a heterogeneous source that involved juvenile components derived from a depleted mantle source during magma generation. The aluminous A-type granite magmas were probably derived by high-temperature partial melting of a felsic crustal source, whereas the other granite magmas probably resulted from partial melting of a mafic lower crust. The gabbro-diorites of the Longtouqiao pluton are depleted in Nb, Ta, P, and Ti, and show flat distributions of most LILEs and HFSEs, except for large positive anomalies in Ba, K, and Pb. These features reflect a limited degree of crustal contamination associated with the subduction-related magmatic processes. These data

  4. Geochemical and geochronological characteristics of Late Cretaceous to Early Paleocene granitoids in the Tengchong Block, Southwestern China: Implications for crustal anatexis and thickness variations along the eastern Neo-Tethys subduction zone

    Science.gov (United States)

    Zhao, Shao-wei; Lai, Shao-cong; Qin, Jiang-feng; Zhu, Ren-Zhi; Wang, Jiang-bo

    2017-01-01

    The Tengchong Block of Southwestern China is key to tracing the eastward subduction of Neo-Tethys and collision between Indian and Asian continents. The block contains a magmatic belt that represents the southeastward continuation of the Gangdese belt, produced by the eastward subduction of eastern Neo-Tethyan oceanic lithosphere. In this paper we present geochemical and geochronological data of Late Cretaceous to Early Paleocene ( 64 Ma) granitic rocks of the Guyong and Husa batholiths in the Tengchong Block. These can be subdivided into high-silica peraluminous granites and low-silica metaluminous granodiorites, and all belong to the high-K calc-alkaline series, are enriched in LILE, and depleted in HFSE. The Guyong granitoids have high initial Sr ratios of 0.706511-0.711753, negative εNd(t) values of - 9.2 to - 11.6, two-stage model ages of 1.39-1.55 Ga, and Pb isotopic compositions that indicate a crustal affinity. The Husa granodiorites also have high initial Sr ratios of 0.716496, negative εNd(t) value of - 16.5, two-stage model age of 1.89 Ga, variable εHf(t) values of 3.4 to - 18.1 and Pb isotopic compositions similar to lower crustal values. These geochemical and isotopic data indicate that the Guyong granitoids were likely derived from partial melting of ancient crustal metapelite or mixed pelite-greywacke sources, while the Husa granodiorites were derived from the partial melting of lower crustal mixed sources involving metasedimentary and metaigneous rocks. To understand the thermal state and architecture of the Late Cretaceous to Early Paleocene magmatic arc crust, the crust-derived intermediate to acidic igneous rocks of the southern-central Lhasa and Tengchong blocks and eastern Himalayan syntaxis are compared. We infer that partial melting of crust occurred at great depth in the southern Lhasa Block, intermediate depths in the eastern Himalayan syntaxis, and shallow depths in the central Lhasa and Tengchong Block. Sr/Y ratios indicate that the

  5. Victorian naturalists in China: science and informal empire.

    Science.gov (United States)

    Fan, Fa-ti

    2003-03-01

    This paper discusses the research of British naturalists in China during the period between the Opium War and the collapse of the Qing dynasty (1839-1911). China was defeated in the Opium War and forced to open treaty ports for trade with the Westerners. The foreign powers, particularly Britain, imposed upon the Qing government treaties, concession leases, favourable trade conditions, legal privileges and so on to reduce its political autonomy. In the shadow of the informal empire, not only did the British have more freedom to travel in China, first at the treaty ports and later in the interior, but they successively established diplomatic , commercial and missionary institutions in dozens of Chinese cities. The most important of them - the British Consular Service, the Chinese Maritime Customs and the Protestant missionary organizations - provided the talent and infrastructure for natural historical research and became networks for scientific information. The research into China's natural history epitomized the characteristics of British research on China in general: it engaged in collecting and circulating an ever-increasing amount of information and aimed at producing 'factual' and 'useful' knowledge about China. The paper modified current literature on scientific imperialism, which has dealt primarily with the colonial context, by examining the role of nineteenth-century British imperial science in the context of informal empire.

  6. Patterns of geothermal lease acquisition in the Imperial Valley: 1958--1974

    Energy Technology Data Exchange (ETDEWEB)

    Sullivan, M.; McDougal, S.; Van Huntley, F.

    1974-08-01

    Patterns for the development of geothermal resources in the Imperial Valley are analyzed, with particular consideration of corporate behavior in geothermal development. Actions of the companies were examined over a period of time to discover patterns of involvement, investment, and likelihood of further development. Discussion is presented under the following section headings: research organization; legal aspects; characteristics of development; location of geothermal leases; analysis of major leaseholders; and findings and conclusions. The addendum is entitled Federal Land Lease Sales: An analysis in terms of Lease Acquisition Patterns. The three appendices are: research methodology; a methodological note on the maps; and exploratory drilling sites. (JGB)

  7. Your name is not good enough: introducing the ORCID researcher identifier at Imperial College London

    Directory of Open Access Journals (Sweden)

    Torsten Reimer

    2015-11-01

    Full Text Available The ORCID researcher identifier ensures that research outputs can always reliably be traced back to their authors. ORCID also makes it possible to automate the sharing of research information, thereby increasing data quality, reducing duplication of effort for academics and saving institutions money. In 2014, Imperial College London created ORCID identifiers (iDs for academic and research staff. This article discusses the implementation project in the context of the role of ORCID in the global scholarly communications system. It shows how ORCID can be used to automate reporting, help with research data publication and support open access (OA.

  8. The Entangled Sovereignties of Air Police: Mapping the Boundary of the International and the Imperial

    DEFF Research Database (Denmark)

    Munro, Campbell Alexander Omoluaye

    2015-01-01

    above,’ yet this designation obfuscates the concomitant occupation of airspaces entailed by drones and other aerial technologies. Such occupations constitute an assertion of jurisdiction in nominally sovereign airspaces authorised by latent imperial legality. The history of air policing reveals......The contemporary proliferation of drones and other forms of aerial interventions herald the (re)emergence of air policing as the principal modality for the fabrication of order in the global periphery. Air policing is predomi- nantly framed by international legal analysis as merely ‘killing from...

  9. The Imperial Congress and Frontier Stability: the Case of Iraq, 2003

    Directory of Open Access Journals (Sweden)

    Frank H. Wallis

    2009-12-01

    Full Text Available Este artículo examinará el interés del Congreso de los Estados Unidos de América, durante las administraciones de Clinton y Bush II, con respecto a los problemas asociados del petróleo y de Sadam Hussein, demostrando una pauta de conducta de una élite dominante a favor de un mercado del petróleo estable y de un Golfo Pérsico ordenado de acuerdo a los intereses del gobierno de los Estados Unidos. En los comienzos de 2003 el Congreso mostraría cuan ansioso estaba de de abrazar la política de estabilización imperial de Bush II, concediendo dinero, mandando tropas, declarando la guerra y repeliendo una imaginaria invasión. El Congreso alcanzó un consenso durante las eras de Clinton y Bush II, a pesar de unos pocos disidentes, acerca de que Saddam estaba en el camino del progreso de América y de un petróleo a precio razonable. Un Congreso cómplice de esta actitud imperial votó a favor de la invasión de Iraq y de la sustitución de su gobierno y estructura socio-política, estabilizando esta lucrativa nueva frontera, absorbiéndola dentro del imperio corporativista estadounidense._______________________ABSTRACT:This article will examine United States congressional interest, over the course of the Clinton and Bush II administrations, in the associated problems of oil and Saddam Hussein, demonstrating a ruling elite bias in favor of a stable oil market and a stable Persian Gulf imposed by the U.S. government (USG. In the run up to 2003 Congress would show how eager it was to embrace the imperial stabilization policy of Bush II, borrow money, raise troops, declare war, and repel an imagined invasion. Congress reached a consensus over the Clinton and Bush II eras, despite a few dissenters, that Saddam was in the way of American progress and affordable oil. A compliant imperial Congress voted to invade Iraq and replace its entire government and socio-political structure, stabilizing this lucrative new frontier, absorbing it into the U

  10. Assessment of geothermal development in the Imperial Valley of California. Volume 1. Environment, health, and socioeconomics

    Energy Technology Data Exchange (ETDEWEB)

    Layton, D. (ed.)

    1980-07-01

    Utilization of the Imperial Valley's geothermal resources to support energy production could be hindered if environmental impacts prove to be unacceptable or if geothermal operations are incompatible with agriculture. To address these concerns, an integrated environmental and socioeconomic assessment of energy production in the valley was prepared. The most important impacts examined in the assessment involved air quality changes resulting from emissions of hydrogen sulfide, and increases in the salinity of the Salton Sea resulting from the use of agricultural waste waters for power plant cooling. The socioeconomics consequences of future geothermal development will generally be beneficial. (MHR)

  11. Exploring imperial expansion using an isotopic analysis of paleodietary and paleomobility indicators in Chachapoyas, Peru.

    Science.gov (United States)

    Toyne, J Marla; Church, Warren B; Luis Coronado Tello, Jose; Morales Gamarra, Ricardo

    2017-01-01

    Inca imperial strategies of political and territorial expansion varied across conquered regions depending on local ecology and cultural resistance, and Chachapoya peoples in Peru's forested northeastern Andes were renowned for their rebellions against the invaders. The cliff tombs of Los Pinchudos (AD 1470-1535) present opportunities to use stable isotopes to: (1) explore dietary and mobility patterns from a mortuary community interred at a site attributed to the poorly-known Chachapoya culture during the period of Inca domination, and (2) explore the origins of the individuals as either local or foreign (Inca). Using biochemical tracers, we can help resolve the impact of foreign influence and changes in population and social structure during imperial occupation. While it is difficult to reconstruct individual life histories from incomplete skeletons, stable isotopic analysis of multiple skeletal tissues provides a direct means of characterizing diet and residential mobility. Values of stable carbon (δ(13) C), nitrogen (δ(15) N), and oxygen isotope (δ(18) O) ratios were determined in bone and dentine collagen and bone and enamel carbonate from 28 samples (11 paired tissues) from males, females, and juveniles from Los Pinchudos. Dietary signatures are consistent with a mixed but more C3 -based plant and protein-based diet with moderate proportions of terrestrial animals. Oxygen isotopic values demonstrate limited variation between paired tissues, with a few possible nonlocal individuals buried in one particular tomb at the site. Compared to other Andean areas that underwent imperial domination, these data do not demonstrate expected dietary shifts. These are the first isotopic data from a Chachapoya site and our research shows evidence for minimal non-local presence in this commingled burial assemblage. The regional diet reconstructed at Los Pinchudos (2850 masl) focused on resources of higher altitude tuber crops, beans, and grains (C3 ) and terrestrial protein

  12. Study of the influential leaders, power structure, community decisions, and geothermal energy development in Imperial County, California

    Energy Technology Data Exchange (ETDEWEB)

    Butler, E.W.; Hall, C.H.; Pick, J.B.

    1980-04-01

    The economy of Imperial County, California, is now dominated by agriculture, but economic studies indicate that the emerging geothermal sector could grow to a size comparable to that of agriculture. The purpose of this study is to discover the kind of power structure operating in Imperial County, the influential leaders, the source of their power, their probable reactions to geothermal development, and the possible effects geothermal development will have on the power structure. Several social science research methods are used to identify the influential leaders and to describe the power structure in Imperial County. An analysis of the opinions of leadership and the public shows the likely response to geothermal development. The power structure analysis, combined with forecasts of the economic effects of geothermal development, indicates the ways in which the power structure itself may change.

  13. A Brief Discussion on School Concerts in the Late Qing Dynasty and the Early Period of the Republic of China%清末民初学校音乐会初探

    Institute of Scientific and Technical Information of China (English)

    关心

    2012-01-01

    During the period between the late Qing Dynasty and the early Republic of China,the emergence of school concerts was a product of the mutual exchanges,engagement and interaction between the Chinese music culture and that of the West.On the one hand,music education in schools had laid a foundation for school concerts,and on the other,the emergence and thriving of professional music education had greatly boosted the development of school concerts.In the development process of school concerts,the explorations of relevant music groups and music organizations had played a pioneering role;the performances and workshops given by foreign musicians had played a leading and exemplary role;the publicity work by the media had played a propagating role;and the competitions between Chinese folk music and overseas music had played a mutually reinforcing role.%清末民初学校音乐会的出现是中西音乐文化相互交流、碰撞和融合的产物。学校音乐教育为学校音乐会奠定了基础,专业音乐教育的兴起推动了学校音乐会发展。在此过程中,音乐团体和音乐机构的探索起了开路先锋的作用,来华外国音乐人士的表演和讲习起了示范和带动作用,报刊媒体的宣传起了舆论推进的作用,外来音乐和民族音乐的博弈与竞争起了相互促进的作用。

  14. Funeral Customs of Zhangj iakou in the Late Qing Dynasty and the Early Republic of China%清末民初张家口地区丧祭礼俗探研

    Institute of Scientific and Technical Information of China (English)

    张欣

    2014-01-01

    以清末民初张家口地区民间丧祭礼俗对传统的继承和革新为例,窥视当时广大乡村和内陆地区丧祭礼俗的沿革演变。清末民初是中国社会转型的典型时期,中国传统丧祭礼俗发生了深刻变化,但是这种变化是不均衡的。对清末民初张家口地区民间丧祭礼俗进行探研,不仅有利于对张家口地区民俗文化发展的研究,也有利于进一步了解广大乡村和内陆地区传统丧祭礼俗的发展和变迁。%Taking the heritance and reformation of traditional funeral etiquettes and customs of Zhangjiakou in the late Qing Dynasty and the early Republic of China as an example,the paper analyzes the evolution of funeral customs in vast rural and inland areas at that time.This is a typical period of China’s social transformation,in which profound changes had taken place for traditional Chinese sacrificial rites,but this kind of change was uneven.This research is not only beneficial to the study of folk cultures in this are-a,but also helpful for the further research on the evolution and development of traditional sacrificial rites in the rural and inland areas.

  15. A persistent Holocene wetting trend in arid central Asia, with wettest conditions in the late Holocene, revealed by multi-proxy analyses of loess-paleosol sequences in Xinjiang, China

    Science.gov (United States)

    Chen, Fahu; Jia, Jia; Chen, Jianhui; Li, Guoqiang; Zhang, Xiaojian; Xie, Haichao; Xia, Dunsheng; Huang, Wei; An, Chengbang

    2016-08-01

    There are significant differences in the interpretation of the moisture (precipitation) history of arid central Asia (ACA) during the Holocene, as inferred on one hand from speleothem oxygen isotope records, and on the other from lake sediments. Here we present the results of measurements of climatically-sensitive magnetic properties and soil color from four well-dated loess-paleosol sequences from the northern slopes of the Tienshan Mountains and the Yili River valley, Xinjiang, China, in the core area of ACA. Our results demonstrate that the characteristic Holocene paleosol, indicating relatively moist conditions, generally formed after ∼6 ka (1 ka = 1000 cal yr BP) in the study region, and that the accumulation of unweathered loess prevailed during the early Holocene, indicating a dry climate at that time. The magnetic proxies further reveal a trend of generally increasing moisture since the Last Glacial Maximum, with the wettest climate occurring during the late Holocene. This trend of increasing moisture during the Holocene is representative of the Xinjiang region and possibly of the whole of the core area of ACA, and is in marked contrast both to the mid-Holocene moisture maximum observed in the East Asian summer monsoon region and to the general decrease in the strength of the Indian summer monsoon since the early Holocene. Our findings are supported by the results of a climate simulation which indicate a trend of increasing summer and winter precipitation during the Holocene in the core area of ACA, caused mainly by an increase in the strength of the westerlies effected by an increasing latitudinal insolation gradient and by a negative trend of the Arctic Oscillation (AO) or North Atlantic Oscillation (NAO).

  16. [Medicine and orientalism in the late nineteenth century Korea].

    Science.gov (United States)

    Lee, Jong-Chan

    2002-06-01

    The paper investigates medical missionaries that exerted a significant role in establishing Western medicine in the late nineteenth century Chosun, in relation to orientalism, an academically popularized concept introduced by Edward Said. Historical analysis is focused on several important medical missionaries such as Horace N. Allen, William B. Scranton, John W. Heron, C. C. Vinton, and Oliver R. Avison to explain how their activism as medical missionary contributed to the formation of medical orientalism in which Western medicine was 'taught, studied, administered, and judged' in that period. In addition, I explore into how medical orientalism was in service of Japanese imperialism by showing that medical missionaries had to be under imperial surveillance by Japanese colonizers. The article explores the medical system of the Koryo Dynasty period and its social characteristics. First, the structure of medical system and roles of medical institutions during the Koryo Dynasty period will be summarized. Then the characteristics of the medical system will be identified through exploring the principles of its formation in a view of social recognition of medical care and a view of social recognition of medical care and a view of public policy.

  17. West Meets East: The Early Civilizations of India and China. Grade 6 Model Lesson for Unit IV. California History-Social Science Course Models.

    Science.gov (United States)

    Zachlod, Michelle, Ed.

    This unit for sixth graders focuses on the origins of Chinese civilization, the rise of early Chinese imperial centers, and the breakdown of order by the beginning of the sixth century B.C. Among the topics in the unit are: Early history and geography of India; Buddhism; Early history and geography of China; Confucius; and Culture, politics,…

  18. 华南中-晚二叠世之交碳酸盐岩磁学特征及环境意义%Magnetic Properties of Middle-Late Permian Carbonates in South China and Their Environmental Significances

    Institute of Scientific and Technical Information of China (English)

    李波; 薛武强; 颜佳新; 朱宗敏; 王艳; 马志鑫

    2015-01-01

    As a reliable proxy for paleoclimate and paleoenvironment,magnetic parameter could provide valuable data for the re-search of global environmental changes and climatic processes.A detailed study has been carried out on rock magnetism in order to reveal the change of climate and environment and its reasons across Guadalupian-Lopingian (G-L)boundary at Tieqiao sec-tion in Laibin area,Guangxi,China.The results show that the dominant magnetic minerals from Tieqiao section are paramag-netic minerals with a small amount of magnetite and hematite as well.There is a remarkable change in the properties of rock magnetism near the G-L boundary.Magnetic susceptibility increases first and then decreases.Magnetic carriers show the trend of being transformed from hard magnetic minerals (hematite)to soft magnetic mineral (magnetite)and then turning to hard magnetic minerals (hematite).All of these changes occur within 4 m-thick strata interval above and below the G-L boundary, and synchronize with the fluctuation of sea-level and ancient seawater temperature during late Middle Permian.The significant changes in magnetic parameters for Middle-Late Permian carbonates suggest that the migration and conversion of magnetic minerals between different spheres in earth system has shifted,which resulted from the climatic and environmental changes. High sea-level during Late Guadalupian and Early Lopingian resulted in the decrease in terrigenous supply in South China. Therefore,the magnetic carriers in Tieqiao section mainly are hematite through aeolian transportation during this period.How-ever,pronounced regression during the Middle-Late Permian transition led to the expansion of exposed land area.Meanwhile, land plants experienced widespread extinction,which led to increased sediment source.The magnetic carriers in contemporane-ous sediments of Tieqiao section are mainly fluvial magnetite.%磁学参数作为可靠的古气候和古环境指标,能为全球环境变化、气候过程

  19. Cultural Imperialism of the West in the Work of Edward W. Said

    Directory of Open Access Journals (Sweden)

    Ranka Jeknić

    2006-09-01

    Full Text Available This article presents the main ideas and views of Edward W. Said on the relationship between culture and imperialism, and also on the link between Western culture and the formation of imperialism. Hence, special attention is given to Said’s interpretation of novels as constructions of the geopolitical reality: i.e. the characteristics of “imperialism” are examined as found in such English and French writers as Jane Austen, Rudyard Kipling, Joseph Conrad and Albert Camus, illustrating the way how novels as an aesthetic form participated in the “cultural construction” of colonialism. In the next part of the discussion, the paper presents another main topic of Edward Said that reveals how “cultural imperialism”, “orientalism” and “covering Islam” are still, unfortunately, current topics. Special attention is given to Said's demystification of the opposition between “us” and “them”, or “the West” and “Others”, through the example of the relationship between “the West” and “Islam”. Behind this issue, unequal power relations exist, as well as unequal relations of power and knowledge; “anti-systemic movements”, especially, and the “post-colonial discourse”, in general, warns us of this.

  20. Bioindicators from Mosquitofish (Gambusia affinis) Sampled from the Imperial Valley in Southern California

    Science.gov (United States)

    Jenkins, Jill A.; Draugelis-Dale, Rassa O.

    2006-01-01

    The Sonny Bono Salton Sea National Wildlife Refuge (SSNWR) is located 64 km north of the Mexican border at the southern end of the Salton Sea in California's Imperial Valley. Freshwater ponds and managed habitats at the SSNWR, Calipatria, Calif. are supplied with Colorado River water that carries compounds from upstream sources. Components include municipal and industrial discharges, agricultural drainage, and sewage plant inputs. Aquatic animals in these ecosystems are continuously exposed to multiple constituents, several of which have been demonstrated to be associated with hormonal disturbances. We investigated possible endocrine impacts to fish in the Imperial Valley, Calif., by addressing the null hypothesis that aquatic species in impacted sites did not exhibit evidence of endocrine disruption as compared with those from nonimpacted sites. The results presented are intended to provide managers with science-based information and interpretations about the condition of the animals in their ecosystems for the minimization of potential adverse effects to trust fish and wildlife resources and for the maximization of available water resources.