999 resultados para 541


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O Plenário votou todo o capítulo da Política Urbana. Os pontos principais aprovados garantem o desenvolvimento das funções sociais das cidades e o bem-estar de seus habitantes. Concluída a votação da Reforma Urbana, os constituintes se reúnem para tentar um acordo sobre o próximo capítulo: a Reforma Agrária. Duas comissões irão tratar dos temas mais polêmicos. Discutir a função social da terra, a insusceptibilidade de desapropriação, a política agrária, a política de reforma agrária e da política agrícola, compatibilizando com a planificação nacional. A pequena e média propriedade não será passível de desapropriação, bem como a propriedade produtiva, que cumpra a função social. Chegar a um texto comum é a expectativa dos constituintes.

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Zooplankton was studied in four alpine lakes in Switzerland, France and Italy. The presence the presence of the invertebrate predator Heterocope in three lakes was stated. It is then discussed why in three of these four lakes, the copepod Arctodiaptomus denticornis is present in the absence of Arctodiaptomus bacillifer, and vice versa respectively in the second and first parts of the lacustrine summer.

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u.a.: Johanna Schopenhauer; Heinrich Floris Schopenhauer; Gottlieb Ernst Schulze; Justus Radius;

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109 Briefe zwischen Leo Löwenthal und Max Horkheimer, 1943; 4 Briefe von der Office War Information (Washington) an Leo Löwenthal, Januar 1943; 1 Brief von J. H. Randall an Leo Löwenthal, 24.11.1942; 1 Brief von Dan Levin an Leo Löwenthal, 10.01.1943;

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Sediment cored within the Barbados subduction complex at Sites 541 and 542 are underconsolidated. Underconsolidation and changes in physical properties of the cored section can be related to excess pore water pressure that equals the lithostatic load at Site 542 and to major thrust faulting observed at Site 541. Apparently, the pore fluids within the subduction complex are absorbing the tectonic shock of underthrusting. Sediment sampled from the reference Site 543 on the adjacent Atlantic Plate are also underconsolidated. However, underconsolidation in Hole 543 is apparently due to the movement of excess nitrogen gas observed deeper in the hole. Excess gas was not observed at Sites 541 and 542.

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The calcite compensation depth (CCD) fluctuates as a result of changes in the water-mass system, thereby producing a distinct dissolution pattern. Differential dissolution changes the composition of the foraminiferal assemblages, reflecting the depositional environment in respect to the fluctuating CCD. The dissolution pattern for the comparatively shallow Site 541 on the Barbados Ridge indicates a depositional environment mostly above the CCD, but below the foraminiferal lysocline during the late Miocene to early Pleistocene. In contrast, sediments of the deeper-water Site 543 indicate a depositional environment above the CCD during the late Pliocene to early Pleistocene only. Furthermore, similarities in the dissolution pattern of corresponding time intervals of Site 541 (represented by superimposed faulted intervals termed Tectonic Units A and B) are recognizable. Sediments deposited clearly above the foraminiferal lysocline are rare