935 resultados para Carus, Marcus Aurelius, Roman Emperor, d. 283.


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The Roman Jakobson’s criticism of the Saussurean langue/parole distinction, in his La théorie saussurienne en retrospection, is based on the acceptance of a given object in Bachelards sense: the language (langage) as a complex unity which we only have to analyze. It contains no theorization of langue as a norm. On the contrary, the Saussurean langue/parole distinction is at the same time epistemological and theoretical: It amounts to delimiting an object in the whole language (langage) and to theorizing the dimension of communication which is inherent to human language. Thus, the Saussurean distinction appears to be at the foundation of the theorization of langue, which founds linguistics, but whose necessity is dissimulated, in a linguistic theory like Jakobson’s, by the language(langage) as a given object and the langue/parole problematics following from it.

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von Schalom Asch. [Übertr. von Georg Richter]

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S. Poljakoff [Salomom L'vovič Poljakov]. Aus d. Russ. von Z. Holm

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von Artur Landsberger

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von Max Joseph [d.i. Maximilian Joseph Pfeiffer]

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Lion Feuchtwanger

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Frankfurter Latern

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von I. M. Weis. Aus d. Engl. frei übers. von E. Schmerler

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von Heinrich Siemer. Mit einem Geleitwort von Max Brod

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The Hawaiian-Emperor hotspot track has a prominent bend, which has served as the basis for the theory that the Hawaiian hotspot, fixed in the deep mantle, traced a change in plate motion. However, paleomagnetic and radiometric age data from samples recovered by ocean drilling define an age-progressive paleolatitude history, indicating that the Emperor Seamount trend was principally formed by the rapid motion (over 40 millimeters per year) of the Hawaiian hotspot plume during Late Cretaceous to early-Tertiary times (81 to 47 million years ago). Evidence for motion of the Hawaiian plume affects models of mantle convection and plate tectonics, changing our understanding of terrestrial dynamics.

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We have measured the carbon isotopic composition of dissolved inorganic carbon in bottom waters of the Ontong Java Plateau (western equatorial Pacific) and on the northern Emperor Seamounts (northwest Pacific). Each of these locations is several hundred miles from the nearest Geochemical Ocean Sections Study (GEOSECS) stations, and the observed delta13C values at each site differ substantially from regionally averaged GEOSECS delta13C profiles. We discuss the possible causes of these differences, including horizontal variability, near-bottom effects, and problems with the Pacific GEOSECS delta13C data. We also measured the isotopic composition (C and O) of core top C. wuellerstorfi from a depth transect of cores at each location. The delta18O data are used to verify that our samples are Holocene. Comparison of foraminiferal and bottom water delta13C values shows that this species faithfully records bottom water delta13C at both sites and demonstrates that there is no depth-related artifact in the dissolved inorganic carbon-C. wuellerstorfi delta13C relationship at these sites.

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Este artículo analiza la contaminación que de los idilios 13 y 22 de Teócrito y de los versos II 282-283 del poema de Apolonio de Rodas realiza Propercio en su elegía 1, 20.