467 resultados para Plautus, Titus Maccius
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4 Briefe und 8 Beilagen zwischen Gerhard Tinter und Max Horkheimer, 1938; 1 Brief von Hans Tischler an Max Horkheimer, 08.12.1938; 4 Briefe zwischen Bernhard H. Titcomb und Max Horkheimer, 22.09.1935, 1935; 2 Briefe zwischen Paul Titus und Max Horkheimer, 07.06.1942, 09.06.1942; 1 Brief von Ferdinand Tönnies an Max Horkheimer, 17.10.1935; 1 Brief von Tonetti Juliette Favez, 21.11.1935; 1 Brief vom Treasury Department an Max Horkheimer, 11.02.1937; 1 Brief von Edith A. Trotter an Max Horkheimer, 13.02.1941; 2 Briefe zwischen The Twentieth Century Fund und Max Horkheimer, 22.12.1942, 02.01.1943; 4 Briefe zwischen Robert Ulich und F. Pollock, 1936, 10.04.1941, 1941; 1 Brief von Max Horkheimer an United States of America Commissioner for Immigration and Naturalisation, 01.11.1940; 1 Brief von Max Horkheimer an das United States of America Department of Agriculture, 15.01.1940; 1 Brief von Max Horkheimer an das United States of America Department of State, 07.10.1941; 1 Brief von Herbert Marcuse an das United States of America Department of State, 07.10.1941; 1 Brief von Max Horkheimer an das Universität Frankfurt Kuratorium der Johann Wolfgang Goethe Universität, 05.07.1935; 1 Briefkopie von Max Horkheimer an die Universität Frankfurt, Der Rektor, 28.07.1933; 1 Brief und 1 Beilage von der University of Buffalo an Max Horkheimer, 06.03.1940; 5 Briefe zwischen der University of California Berkeley und Max Horkheimer, 1940; 2 Briefe zwischen der University of Colorado Libraries und Max Horkheimer, 17.10.1940, 25.10.1940; 3 Briefe zwischen der University of Newark und Max Horkheimer, 1935, 08.04.1938, 1938; 6 Briefe zwischen Jiri Veltruský und Max Horkheimer, 1948-1949; 1 Brief von Leon Verhille an Max Horkheimer, 19.12.1949; 5 Briefe zwischen Salka Viertel und Max Horkheimer, 1938, 1940; 1 Heiratsanzeige von Edward Walter Violin, 1949; 1 Notiz von Max Horkheimer an Edward Walter Violin; 1 Brief von Stitschan Voehard an Max Horkheimer, 03.01.1950;
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Bei der Foliierung wurden Blätter übergangen und nachfoliiert als Bl. 35a, 96a und 164a.
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The occurrences of ten datum events for the Quaternary and top Pliocene nannofossils are identified at nine Leg 115 sites. A quantitative investigation of Paleogene nannofossils in 470 samples selected from 11 holes at 9 sites yielded 197 taxa, including one new species and 10 unidentified taxa that are likely to be new species. Regional differences in the timing of some biostratigraphically important events are recognized, and a set of datum events useful for biostratigra- phy in the tropical Indian Ocean is presented. Biogeographical differences are minor for Paleogene cores from the tropical sites (Sites 707-716); however, the Quaternary and late early Oligocene floras observed at the two subtropical sites (Sites 705 and 706) differ significantly from the corresponding floras of the tropical sites. Bathymetrically controlled dissolution is recognized by the reduction of species diversity in the Paleogene flora. Selective dissolution of nannofossils is also evidenced by the percentage reduction of three holococcolith taxa, Lanternithus minutus, Zygrhablithus bijugatus, and Holococcolith type A as well as by the increase of Coccolithus pelagicusand Cribrocentrum reticulatumin the deeper sites.
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El presente trabajo se propone: 1. Determinar las distintas formas de testar que adoptó el derecho romano, a lo largo de su evolución histórica. 2. Caracterizar la captatio testamenti, una profesión insólita y lucrativa cuya existencia se constata ya en la Roma republicana, a través del testimonio de Plauto en el Miles gloriosus y que se difundió notablemente durante los primeros siglos del Imperio, en los que se convirtió en un medio de progreso social. 3. Analizar esta actividad desde diferentes perspectivas de acuerdo con los tipos humanos que participan en ella: los captatores testamentorum o heredipetae y los testatores. El corpus trabajado abarca a Plauto (Miles gloriosus), Horacio (Sátira 2,5), Séneca (De beneficiis y Epist. 95), Marcial (Epigramas), Petronio (Satiricón), Juvenal (Sátira 12), Plinio el Viejo (Hist. Natural), Plinio el Joven (Epist. 2, 20).
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Ocean Drilling Program (ODP) Leg 114 recovered nannofossil-bearing sediments from seven sites in the high latitudes of the South Atlantic Ocean. Cretaceous sections were recovered from Sites 698 and 700, located on the Northeast Georgia Rise and its lower flanks, respectively. These contain distinctive high-latitude nannofossil floras similar to those from high-latitude areas of the Northern Hemisphere. Most of the biostratigraphic datums used to date the upper Campanian to Maestrichtian interval appear to lie at approximately the same level in both hemispheres. The FAD of Nephrolithus frequens is confirmed to be diachronous with an earlier occurrence in high latitudes. The LAD of Monomarginatus primus n. sp. also appears to be diachronous with a later LAD in the high latitudes of the Southern Hemisphere. Fossiliferous Paleocene to lowermost Miocene sediments were recovered at all seven sites, from the Northeast Georgia Rise in the west to the Meteor Rise in the east. These nannofossil floras, although restricted in diversity and only poorly preserved, are sufficiently distinctive to allow the recognition of 19 zones and three subzones, which are used to date and correlate the cores recovered. Only Site 704 on the Meteor Rise yielded a substantial section of Miocene to Quaternary nannofossil-rich sediments. The nannofossil floras of this section are of very low diversity, with usually fewer than eight species present. Some stratigraphic ranges of important biostratigraphic datum species are observed to be different in the high-latitude sections from those recorded from low-latitude areas. The LAD of Reticulofenestra bisecta, when calibrated by magnetostratigraphy, appears to occur earlier in Hole 699A (within Chron C6CR) than in Hole 703A and possibly Hole 704B and in other published accounts of lower latitude sites in the South Atlantic. The FAD of Nannotetrina fulgens/N. cristata appears to occur later in Hole 702B (Chron C20R) than it does in other published accounts of lower latitude sites in the South Atlantic. Diachroneity is also suspected in the stratigraphic ranges of Chiasmolithus solitus and Chiasmolithus oamaruensis, although poor magnetostratigraphic results through the critical interval prevent confirmation of this. Differences in the relative stratigraphic ranges of lsthmolithus recurvus and Cribrocentrum coenurumlC. reticulatum at Sites 699 and 703 are noted. These possibly suggest warmer surface waters on the eastern side (Site 703) of the middle to late Eocene South Atlantic than those on the western side (Site 699). The diversities of the nannofossil floras and the presence of the warm-water genera Discoaster, Sphenolithus, Helicosphaera, and Amaurolithus reflect the changing surface water temperatures throughout the Cenozoic. Warmer periods are inferred for the late Paleocene to early middle Eocene, late middle Eocene to late Eocene, latest Oligocene to earliest Miocene, and possibly the Pliocene. Colder periods are inferred for the middle Eocene, most of the Oligocene, and the Miocene. Dramatic changes in the nannofossil floras of the Pleistocene of Site 704 are thought to reflect a rapidly changing environment. Monomarginatus primus, a new species from the Upper Cretaceous strata of Hole 700B, is described.
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During Ocean Drilling Program (ODP) Leg 105, a thick sequence of lower Eocene to lower Oligocene sediments was recovered from Hole 647A in the southern Labrador Sea. These sediments contain diverse, well-preserved, high-latitude calcareous nannofossil flora. The nannofossil biostratigraphy of the hole indicates the presence of a minor hiatus between Zones NP 16 and NP 17 in the upper middle Eocene and a barren interval separating Zones NP 13 and NP 15. Species abundance is highest within the lower to middle Eocene and starts to decline near the base of the upper Eocene. No major change in the nannoflora was observed across the Eocene/Oligocene boundary, although a slight decrease in species abundance was recorded. The Paleogene calcareous nannofossils of nearby DSDP Site 112 were reexamined and compared with those of Site 647. Several cores were reassigned to different nannofossil zones. The calcareous nannoflora are dominated by high-latitude indicative species and also exhibit a high diversity, which suggests the influence of more temperate water masses in this region during Eocene and Oligocene time. One new subspecies from the middle Eocene, Sphenolithus furcatolithoides labradorensis, is described.
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Two of five holes drilled at two separate sites during Leg 123 of the Ocean Drilling Program intersected thick and relatively complete sections of Upper Cretaceous-Paleogene nannofossiliferous sediments. Although dominated by turbidite deposition in the upper part, Hole 765C contains a thick and relatively complete Albian-Oligocene section, including a particularly thick Aptian interval, with abundant and fairly well-preserved nannofossils. Several unconformities are confidently interpreted in this section that span much of the Santonian, late Campanian, Maestrichtian, late Eocene, and early Oligocene. Hole 766A contains a thick and relatively complete Albian-lower Eocene section having generally abundant and well-preserved nannofossils. Several unconformities also have been identified in this section that span much of the Coniacian, early Campanian, Maestrichtian, and late Eocene through early Pliocene. The chronostratigraphic position and length of all these unconformities may have considerable significance for reconstructing the sedimentary history and for interpreting the paleoceanography of this region. A particularly thick section of upper Paleocene-lower Eocene sediments, including a complete record across the Paleocene/Eocene boundary, also was cored in Hole 766A that contains abundant and diverse nannofossil assemblages. Although assemblages from this section were correlated successfully using a standard low-latitude zonation, difficulties were encountered that reduced biostratigraphic resolution. Several lines of evidence suggest a mid-latitude position for Site 766 during this time, including (1) high assemblage diversity characteristic of mid-latitude zones of upwelling and (2) absence of certain ecologically controlled markers found only in low latitudes.
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The opening of the Tasmanian Gateway between Australia and Antarctica has long been considered a critical element in the initiation of the Antarctic Circumpolar Current, thermal isolation of Antarctica, and Cenozoic global cooling. The timing for the opening of the gateway to shallow-water circulation and subsequently to deep-water circulation was poorly known, however, and the dating of these events was a major objective of ODP Leg 189. Nannofossil data from Leg 189 sites and DSDP Site 281 in the Tasmanian Gateway suggest a 41-42 Ma age for the initiation of widespread glauconite deposition in the region, which coincided with a sharp drop in sedimentation rate. This is interpreted to be the opening of the gateway to shallow-water circulation, which occurred within the middle of the 51-33 Ma long-term cooling. The change from siliciclastic sediments to pelagic carbonates, the most conspicuous sedimentological and paleontological change in the region for the last 70 Ma and presumably the indicator for the opening of the gateway to deep-water circulation, is dated at about 31 Ma. This event is more than 2 my younger than the major high-latitude cooling in the earliest Oligocene, and thus cannot be the cause for the latter.
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La crítica tradicional trató asiduamente las diferencias entre las dramaturgias plautinas y terenciana. En este artículo se intenta escudriñar esas canónicas divergencias a partir de la categorización 'teatralidades psicofísica y cognitiva', para lo cual se postula pensar el texto dramático terenciano en términos retóricos, desde los que éste podría formularse como una máquina discursiva tendiente al convencimiento y a la persuasión de una idea (el diseño de un público capaz de realizar una actividad cognitiva predominante), mientras el de Plauto se presenta apelando a la conmoción al focalizar aspectos lúdicos asociados más a la percepción primaria del hecho espectacular
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A partir del excepcional estudio hecho por Karl Brugmann sobre la importancia del valor deíctico de los demostrativos y considerando las numerosas investigaciones que dicho estudio inspiró, este artículo se propone resaltar la presencia fundamental de estos frecuentes elementos en la comedia Casina, modelo representativo de la madurez plautina. El análisis centra su atención en las funciones dramáticas principales de los demostrativos desde el punto de vista escénico: la deíctica y la fórica
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Esta publicación, que reproduce literalmente una conferencia dictada por la autora en el Curso 'La Comedia Latina', impartido en colaboración con A. Pociña en el Centro de Estudios Latinos de la Universidad de La Plata, en el mes de septiembre de 2010, consiste en un recorrido por algunos aspectos importantes de las Comedias de Plauto (vida, comedias en general, cronología, modelos, recursos cómicos, ediciones y traducciones al español, pervivencia); la autora hace especial referencia a la situación de los conocimientos, tal como se encontraba a la altura de 2007, fecha de la publicación del libro de A. López y A. Pociña Comedia romana, subrayando aquellos aspectos que siguen pendientes de nuevos estudios, así como los que son susceptibles de indudables mejoras si se les presta la debida atención
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La crítica tradicional trató asiduamente las diferencias entre las dramaturgias plautinas y terenciana. En este artículo se intenta escudriñar esas canónicas divergencias a partir de la categorización 'teatralidades psicofísica y cognitiva', para lo cual se postula pensar el texto dramático terenciano en términos retóricos, desde los que éste podría formularse como una máquina discursiva tendiente al convencimiento y a la persuasión de una idea (el diseño de un público capaz de realizar una actividad cognitiva predominante), mientras el de Plauto se presenta apelando a la conmoción al focalizar aspectos lúdicos asociados más a la percepción primaria del hecho espectacular
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A partir del excepcional estudio hecho por Karl Brugmann sobre la importancia del valor deíctico de los demostrativos y considerando las numerosas investigaciones que dicho estudio inspiró, este artículo se propone resaltar la presencia fundamental de estos frecuentes elementos en la comedia Casina, modelo representativo de la madurez plautina. El análisis centra su atención en las funciones dramáticas principales de los demostrativos desde el punto de vista escénico: la deíctica y la fórica
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Esta publicación, que reproduce literalmente una conferencia dictada por la autora en el Curso 'La Comedia Latina', impartido en colaboración con A. Pociña en el Centro de Estudios Latinos de la Universidad de La Plata, en el mes de septiembre de 2010, consiste en un recorrido por algunos aspectos importantes de las Comedias de Plauto (vida, comedias en general, cronología, modelos, recursos cómicos, ediciones y traducciones al español, pervivencia); la autora hace especial referencia a la situación de los conocimientos, tal como se encontraba a la altura de 2007, fecha de la publicación del libro de A. López y A. Pociña Comedia romana, subrayando aquellos aspectos que siguen pendientes de nuevos estudios, así como los que son susceptibles de indudables mejoras si se les presta la debida atención