705 resultados para Lex Frisionum.
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Signatur des Originals: S 36/G01128
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Signatur des Originals: S 36/G01214
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Signatur des Originals: S 36/G01215
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Signatur des Originals: S 36/G01220
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Signatur des Originals: S 36/G02198
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Tabla de contenidos: El rescate del discurso oral / Pedro Luis Barcia. Uma introduçao ao estudo e cultural da música na Grécia antiga / Fábio Vergara Cerqueira. Lenguaje, discurso y meta-teatralidad en los cantos corales de Séneca / Zelia de Almeida Cardoso. Actualidad y pervivencia del discurso político romano / Gregorio Hinojo Andrés. Lenguaje, discurso y civilización en Baquílides 11 / Ana María González de Tobia. Los ditirambos de Baquílides : Lenguaje, estructura y religiosidad / Fernando García Romero. La represión del adulterio por la Lex iulia de adulteriis coercendis / Marha Patricia Irigoyen Troconis. El imaginario empedocleo / Giuseppina Grammatico. El género lírico entre autoridad poética y prácticas enunciativas : De Goethe a Safo / Claude Calame. La isla y el exilio : Lenguaje y recuperación de la civilización en Odisea / Graciela Cristina Zecchin de Fasano. Homéridas y rehenes / Jaume Pòrtulas. Virgilio y la palabra poética / Antonio Alvar Ezquerra. Falsedad genuina y falsedad verbal en Platón / María Isabel Santa Cruz. El origen de las ideas sobre el espacio y el tiempo / Héctor Vucetich. Homero y Heródoto / Christopher Pelling. Traços teológicos comuns à tragédias de Esquilo : A Teologia de Esquilo no drama Prometheus Demótes / Jaa Torrano. Onoma, érgon y lógos en Helena de Eurípides / Juan Tobías Nápoli. Atenas y Delfos : Adivinación, ley y lenguaje en la Orestíada / Angus Bowie. Linguaggio, discorso e veritá nella Repubblica di Platone / Giovanni Casertano. El estribillo en la poesía clásica, o el poder de la repetición / David Konstan.
Resumo:
A 100-m-thick Paleocene sequence of mainly pelagic sediments at ODP Site 1121, on the eastern flanks of the Campbell Plateau, contains few to common radiolarians of relatively low diversity in the lower 40 m (Early to early Late Paleocene) and abundant, diverse radiolarian assemblages in the upper 60 m (mid-Late Paleocene). The 150 taxa recorded from the entire Paleocene interval are thought to under-represent the actual species diversity by at least one half as many morphotypes have not been differentiated below the level of genus. Assemblages in the lower 40 m are similar to those described from onland New Zealand and DSDP Site 208 (northern Lord Howe Rise); they are correlated with South Pacific radiolarian zones RP4 and RP5. Assemblages in the upper 60 m differ from other known Late Paleocene assemblages in the great abundance of plagiacanthids and cycladophorids. Similarities are noted with later Cenozoic cool-water assemblages. This upper interval is correlated with South Pacific zone RP6, as revised herein, based on comparison with faunas from Site 208 and Marlborough, New Zealand. The interval is also correlated with the upper part of North Atlantic zone RP6 (RP6b-c) based on the presence of Aspis velutochlamydosaurus, Plectodiscus circularis and Pterocodon poculum. Other species, such as Buryella tetradica and Buryella pentadica, are valuable for local correlation but exhibit considerable diachroneity between the Pacific, Indian and Atlantic Oceans. An age model for the Paleocene interval at Site 1121, based on well-constrained nannofossil and radiolarian datums, indicates that the rate of compacted sediment accumulation doubles from 15 to 30 mm/ka at the RP5/RP6 zonal boundary. In large part this is due to a sudden and pronounced increase in accumulation rates for all siliceous fossils; radiolarians and larger diatoms increase from <100 to >10 000 specimens/cm2/ka. This apparent increase in biosiliceous productivity is age-equivalent to a mid-Paleocene cooling event (57-59 Ma) identified from global stable isotope records that is associated with the heaviest delta13C values for the entire Cenozoic.
