Na 1 Nachlass Max Horkheimer, 54 - Korrespondenzen u.a. mit Jiri Veltruský (p. I 25, 242-321)

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;

Grundzüge der vergleichenden Anatomie und Physiologie

von Carl Gustav Carus

Inc. qu. 1108 - Historiae Romanae decades, ital.

Bei der Foliierung wurden Blätter übergangen und nachfoliiert als Bl. 35a, 96a und 164a.

Psychologie der Hebräer

Friedrich August Carus

Quaternary and Paleogene calcareous nannofossils of ODP Leg 115

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.

Calcareous nannofossils of ODP Holes 114-699A and 114-700B

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.

Eocene-Oligocene nannofossils from the Labrador Sea

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.

Género literario y finalidad discursiva en el DRN

Dentro de la rica tradición histórica de estudios acerca del De rerum natura llama la atención la diversidad de opiniones en cuanto al carácter genérico (principalmente su carácter épico y didáctico) y la finalidad o funcionalidad del poema, puesto que a su vez estos asuntos han sido puntos de inflexión del que se desprenden diversas interpretaciones del texto y aún en nuestros días genera disyuntivas entre los estudiosos. La situación no ha resultado tarea fácil, pues, mientras algunos investigadores declaran a Lucrecio como legislador de la norma didáctica, otros prefieren poner en relieve opiniones diferentes que no apuntan a considerar el poema como una obra de naturaleza didáctica. Así, pues, ante la creciente diversidad de razonamientos que se ha generado en torno a este asunto, consideramos oportuno, tanto a partir de taxonomías genéricas de la antigüedad misma, como de la moderna teoría de los géneros literarios, poner a dialogar algunas de las opiniones más relevantes sobre el particular en busca de aclarar un poco este horizonte, a la vez que agregamos a la discusión que el texto también posee un carácter didáctico en tanto que posee una estructura proléptica

Cretaceous and Paleogene calcareous nannofossils from ODP Leg 123

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.

Elección del verso sobre la prosa en el De Rerum Natura de Lucrecio : La poesía al servicio de la enseñanza

Una acostumbrada y debatida concepción considera inadecuado expresar temas filosóficos por medio del uso de la poesía, pues en líneas generales la poesía no satisface el rigor y claridad necesarios para desarrollar temas científicos. Este conflicto entre contenido y forma es reconocido como una característica de la poesía didáctica que se manifiesta muy bien en el poema de Lucrecio. Sin embargo, Lucrecio no fue el primero en intentar este acercamiento poético a la filosofía con fines persuasivo-instructivos; esta elección, a pesar de contradecir los preceptos de Epicuro, estaba acorde con el modelo de discurso escrito empleado por algunos pensadores pre-socráticos para transmitir conocimientos sobre fenómenos naturales. El estudio de esta preferencia estilística en la obra de Lucrecio nos ayudará a comprender mejor la intención persuasivo-instructiva a la que apunta este controvertido texto y mostrar, a partir de ahí, nuevas luces que puedan ayudar a alcanzar una mejor interpretación del mismo

Paleogene calcareous nannofossil record of the Tasmanian gateway

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.