996 resultados para Eiriksson, Magnús, 1806-1881.
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Mode of access: Internet.
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Mode of access: Internet.
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Mode of access: Internet.
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Mode of access: Internet.
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I. Robespierre. Carlyle. Byron. Macaulay. Emerson. --II. Vauvenargues. Turgot. Condorcet. Joseph de Maistre. --III. On popular culture. The death of Mr. Mill. Mr. Mill's Autobiography. The life of George Eliot. On Pattison's Memoirs. Harriet Martineau. W.R. Greg; a sketch. France in the eighteenth century. The expansion of England. Auguste Comte.
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Map on lining-paper.
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t. 1. 1. section. De la destruction des jésuites. 2. section. Des dernières années du règne de Louis XV. 3. section. Du règne de Louis XVI jusqu'a l'Assemblée des notables.--t. 2. 4. section. Du fameux procés du collier. 5. section. De la révolution français.--t. 3-5. [5. section, suite] De la révolution française.--t. 6. Sur la route de poste de Fribourg en Brisgaw à Saint-Pétersbourg. Voyage à Saint-Pétersbourg.
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von Hans Meyer
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Fil: Calandria, María Sol. Universidad Nacional de La Plata. Facultad de Humanidades y Ciencias de la Educación. Instituto de Investigaciones en Humanidades y Ciencias Sociales (UNLP-CONICET); Argentina.
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Passerine spermatozoa exhibit apomorphies that distinguish them from non-passerine neognaths and palaeognaths. The acrosome is longer than the nucleus (excepting the suboscines, most Corvida, and a few Passerida). A perforatorium and endonuclear canals are absent. The proximal centriole is absent (except in the suboscines). The distal centriole is secondarily short, contrasting with its elongate condition in palaeognaths and Galloanserae. In the Passerida a single mitochondrial strand winds extensively along the axoneme (restricted to the anterior axoneme in suboscines and Corvida). A fibrous, or amorphous, periaxonemal sheath, seen in palaeognaths and many non-passerines, respectively, is absent. The acrosome in Myrmecocichla formicivora and Philetairus socius is bipartite: an acrosome core is surmounted by an acrosome crest; the core is ensheathed by a layer which is a posterior extension of the crest. The acrosome helix is a lateral extension of the crest and the crest layer with (Myrmecocichla) or without (Philetairus) protrusion of material of the acrosome core into it. In M. formicivora, as in other muscicapoids, a fibrous helix is intertwined with at least the more proximal region of the mitochondrial helix. The fibrous helix is absent at maturity in Philetairus and other described passeroid spermatozoa with the possible exception of Passer italiae. In Philetairus a granular helix precedes the mitochondrial helix.
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O presente estudo analisou a implantação e a prática educativa do trabalho da missionária metodista norte-americana Martha Hite Watts na virada do século XIX e início do século XX, na cidade de Piracicaba, situada no estado de São Paulo. Os eixos de análise para interpretar as interfaces históricas do período baseiam-se em três aspectos: gênero, educação e missão. Martha Watts, é considerada a primeira educadora metodista no Brasil. Sua atuação se deu a partir de 1881, na cidade de Piracicaba, onde fundou o Colégio Piracicabano, que permanece em funcionamento até o presente momento. Sua experiência educacional foi relevante para o desempenho das escolas metodistas ao adotar uma pedagogia inovadora, nos moldes dos países europeus e de sua terra natal. No Brasil do final do século XIX, Martha Watts mostrou determinação ao enfrentar as diferenças de uma nova cultura e novo ambiente com hábitos, gestos e palavras estranhas para ela. O estudo procurou, a partir do diálogo com as cartas deixadas pela missionária, contribuir para a linha de pesquisa em História da Educação Brasileira. A obra da missionária Martha Watts se configura como um valioso legado para o estudo da História da Educação, História das Mulheres e Gênero.(AU)
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The Journal has been Queen's main student newspaper since it was founded in 1873. It appears twice a week on campus with a mix of news, sports, and entertainment stories, editorials, letters to the editor, and photographs. The paper is students' most important source of news and general information and has been a training ground for scores of Canadian journalists.
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The Journal has been Queen's main student newspaper since it was founded in 1873. It appears twice a week on campus with a mix of news, sports, and entertainment stories, editorials, letters to the editor, and photographs. The paper is students' most important source of news and general information and has been a training ground for scores of Canadian journalists.
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Fossil associations from the middle and upper Eocene (Bartonian and Priabonian) sedimentary succession of the Pamplona Basin are described. This succession was accumulated in the western part of the South Pyrenean peripheral foreland basin and extends from deep-marine turbiditic (Ezkaba Sandstone Formation) to deltaic (Pamplona Marl, Ardanatz Sandstone and Ilundain Marl formations) and marginal marine deposits (Gendulain Formation). The micropalaeontological content is high. It is dominated by foraminifera, and common ostracods and other microfossils are also present. The fossil ichnoasssemblages include at least 23 ichnogenera and 28 ichnospecies indicative of Nereites, Cruziana, Glossifungites and ?Scoyenia-Mermia ichnofacies. Body macrofossils of 78 taxa corresponding to macroforaminifera, sponges, corals, bryozoans, brachiopods, annelids, molluscs, arthropods, echinoderms and vertebrates have been identified. Both the number of ichnotaxa and of species (e. g. bryozoans, molluscs and condrichthyans) may be considerably higher. Body fossil assemblages are comparable to those from the Eocene of the Nord Pyrenean area (Basque Coast), and also to those from the Eocene of the west-central and eastern part of South Pyrenean area (Aragon and Catalonia). At the European scale, the molluscs assemblages seem endemic from the Pyrenean area, although several Tethyan (Italy and Alps) and Northern elements (Paris basin and Normandy) have been recorded. Palaeontological data of studied sedimentary units fit well with the shallowing process that throughout the middle and late Eocene occurs in the area, according to the sedimentological and stratigraphical data.
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Ralf Regener ; Patrick Jopp ; Max Lankau ; Lena von Zelewski