936 resultados para Jülich-Berg


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24 Briefe zwischen Richard Bach und Max Horkheimer, 1938-1940; 2 Briefe zwischen Alfred Chalk und Max Horkheimer, 17.10.1939, 14.11.1939; 3 Briefe von Morduch Lexandrowitsch und der American Consulate General, 1939; 4 Briefe von der American Consulate General und Max Horkheimer, 1938-1939; 1 Brief von Max Horkheimer an das Amtstgericht Berlin, 15.03.1939; 1 Brief von Max Horkheimer an Stiedry, 05.12.1938; 1 Brief von Max Horkheimer an den Collector of Custom, 26.10.1938; 2 Briefe zwischen Josef Maier und Carson Alexandrowitsch, 28.06.1938, 29.06.1938; 1 Brief von Margarete Baruch an Alice Maier, 11.04.1938; 1 Brief von Emanuel List an Carson Alexandrowitsch, 23.02.1938; 1 Abschrift des Briefes von der Metropolitan Opera Association New York an Morduch Lexandrowitsch, 22.02.1938; 1 Brief von Jacques Barzun an Max Horkheimer, 09.07.1947; 4 Briefe zwischen K. Baschwitz und Max Horkheimer, 1938-1946; 2 Briefe zwischen E. Bauer und Max Horkheimer, 08.04.1935, 27.05.1935; 4 Briefe zwischen Fritz Bauer und Max Horkheimer, 1937-1938; 2 Briefe zwischen Lina Bauer und Max Horkheimer, 20.07.1942, 16,08,1942; 4 Briefe zwsichen Rudolf Bauer und Max Horkheimer, 1937; 15 Briefe zwischen Gertrud Bauer und Max Horkheimer, 1938-1941; 1 Brief von Max Horkheimer an den Collector of Customs, 15.03.1940; 2 Briefe zwischen I. Hannah Davidson vom Jewish Community Center San Francisco und Max Horkheimer, 19.09.1938, 29.09.1938; 2 Briefe zwsichen I. Bauer und Max Horkheimer, 25.09.1938, 29.09.1938; 1 Brief von Max Horkheimer an Klopfer, 27.09.1938; 3 Briefe zwischen Y.M.H.A. - Y.W.H.A The Jewish Center of Saint Louis und Max Horkheimer, 19.09.1938, 1938; 1 Brief von Max Horkheimer an Julius Rosenberg, 17.09.1938; 1 Brief von Max Horkheimer an das Jwish Center Salt Lake City, Utah, 07.09.1938; 1 Brief von Max Horkheimer an das Jewish Community Center San Fransisco, 07.09.1938; 3 Briefe zwischen dem New York Section of the National Council of Jewish Women und Max Horkheimer, 07.04.1938, 1938; 2 Briefe zwischen Baum und Max Horkheimer, 12.03.1946, 25.05.1946; 1 Brief von Max Horkheimer an Charles A. Beard , 12.12.1934; 1 Brief von Charles A. Beard an C. A. Beard; 5 Briefe von Friedrich Pollock an Charles A. Beard, 1940-1941; 5 Briefe zwischen Lilo Beck und Max Horkheimer, 1940-1941; 7 Briefe zwischen Maximilian Beck und Max Horkheimer, 1939-1940; 1 Brief von Paul Tillich an Max Horkheimer , 01.10.1940; 1 Brief von dem Emergency Committee in Aid of Displaced Foreign Scholars New York an Max Horkheimer, 19.04.1940; 5 Briefe zwischen Konrad Bekker und Max Horkheimer, 1936-1939; 2 Briefe von Max Horkheimer an Ludwig Bendix, 1921, 1937; 1 Brief von Peter Bendmann an Max Horkheimer; 1 Brief von Max Horkheimer an Ruth Benedict, 30.07.1937; 1 Brief von Eric Russel Bentley an Max Horkheimer, 30.01.1945; 1 Brief von George Berg an Max Horkheimer, 12.07.1945; 2 Briefe zwischen Egon Bergel und Max Horkheimer, 18.08.1938, 22.08.1938; 1 Brief von Marie Jahoda an Max Horkheimer, 14.07.1928; 1 Brief von Theodor W. Adorno an Kurt Bergel, 09.09.1939; 15 Briefe zwischen Klaus Berger und Max Horkheimer, 1936-1943; 1 Brief von Frederick Pollock an Philip M. Hayden von der Columbia University New York, 05.03.1942; 1 Brief von Hans Venedey an Max Horkheimer, 05.03.1938; 1 Brief von Max Horkheimer an Ida Berger-Chevant, 18.02.1939;

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Enth. außerdem: Abris Des Harten Treffens Welches Am Alten Berg, Vnfern Von Nürnberg Zwischen Der Königlichen Scwedischen Vnd Dann Der Friedländischen, Vnd Baiierischen Armeen den 24. Avgvsti Vorgangen

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von C. Berg

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Clasts from the Cape Roberts Project cores CRP-2/2A and CRP-3 provide indications of glacially influenced depositional environments in Oligocene and Miocene strata in the western Victoria Land Basin, Antarctica. CRP-2/2A is interpreted to represent strongly glacially influenced, unconformity bound depositional sequences produced by repeated advance and retreat of floating and grounded ice across the shelf. A similar interpretation is extended to the upper 330 meters of the CRP-3 core, but the lower part of the core records shallow marine deposition with significantly less glacial influence. Clast shape analysis from selected coarse-grained facies throughout the cored interval indicates that most clasts are glacially sourced, with little distinction between diamictite and conglomeratic facies. Three dimensional clast fabric analysis from units immediately above sequence boundaries generally display weak or random fabrics and do not suggest that grounded ice actually reached the drillsite at these intervals. Striated and outsized clasts present in fine-grained lithofacies throughout the cores provide further evidence of sub-glacially transported sediment and iceberg rafting. The distribution of these striated and out-sized clasts indicate that a significant glacial influence persisted through most of the time represented by the cores with glaciers actively calving at sea-level introducing ice-berg rafted glacial debris even in the earliest Oligocene.

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Ecosystems at high northern latitudes are subject to strong climate change. Soil processes, such as carbon and nutrient cycles, which determine the functioning of these ecosystems, are controlled by soil fauna. Thus assessing the responses of soil fauna communities to environmental change will improve the predictability of the climate change impacts on ecosystem functioning. For this purpose, trait assessment is a promising method compared to the traditional taxonomic approach, but it has not been applied earlier. In this study the response of a sub-arctic soil Collembola community to long-term (16 years) climate manipulation by open top chambers was assessed. The drought-susceptible Collembola community responded strongly to the climate manipulation, which substantially reduced soil moisture and slightly increased soil temperature. The total density of Collembola decreased by 51% and the average number of species was reduced from 14 to 12. Although community assessment showed species-specific responses, taxonomically based community indices, species diversity and evenness, were not affected. However, morphological and ecological trait assessments were more sensitive in revealing community responses. Drought-tolerant, larger-sized, epiedaphic species survived better under the climate manipulation than their counterparts, the meso-hydrophilic, smaller-sized and euedaphic species. Moreover it also explained the significant responses shown by four taxa. This study shows that trait analysis can both reveal responses in a soil fauna community to climate change and improve the understanding of the mechanisms behind them.

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Extreme weather events can have negative impacts on species survival and community structure when surpassing lethal thresholds. Extreme winter warming events in the Arctic rapidly melt snow and expose ecosystems to unseasonably warm air (2-10 °C for 2-14 days), but returning to cold winter climate exposes the ecosystem to lower temperatures by the loss of insulating snow. Soil animals, which play an integral part in soil processes, may be very susceptible to such events depending on the intensity of soil warming and low temperatures following these events. We simulated week-long extreme winter warming events - using infrared heating lamps, alone or with soil warming cables - for two consecutive years in a sub-Arctic dwarf shrub heathland. Minimum temperatures were lower and freeze-thaw cycles were 2-11 times more frequent in treatment plots compared with control plots. Following the second event, Acari populations decreased by 39%; primarily driven by declines of Prostigmata (69%) and the Mesostigmatic nymphs (74%). A community-weighted vertical stratification shift occurred from smaller soil dwelling (eu-edaphic) Collembola species dominance to larger litter dwelling (hemi-edaphic) species dominance in the canopy-with-soil warming plots compared with controls. The most susceptible groups to these winter warming events were the smallest individuals (Prostigmata and eu-edaphic Collembola). This was not apparent from abundance data at the Collembola taxon level, indicating that life forms and species traits play a major role in community assembly following extreme events. The observed shift in soil community can cascade down to the micro-flora affecting plant productivity and mineralization rates. Short-term extreme weather events have the potential to shift community composition through trait composition with potentially large consequences for ecosystem development.

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Exercícios físicos auxiliam na melhora do equilíbrio, entretanto há carência de protocolos específicos para trabalhar preventivamente o equilíbrio funcional (EF) e a possibilidade de quedas (PQ) em idosos da comunidade. O objetivo deste estudo foi avaliar o efeito de um Circuito de exercícios sensoriais (CE) sobre o EF e a PQ em mulheres idosas. Completaram o estudo 57 idosas, divididas em grupo experimental (G1= 32; 65,61±4,72 anos) e grupo controle (G2 = 25; 68,41±4,99 anos). G1 praticou 12 semanas de CE composto por 13 estaçoes em forma de circuito. Foram realizadas 2 aulas semanais de 50 minutos de duraçao, compostas por aquecimento, exercícios sensoriais e volta à calma. O grau de dificuldade foi progressivo ao longo do treinamento. EF e PQ foram avaliados antes e depois da intervençao, respectivamente pela Escala de Equilíbrio de Berg (EEB) e pelo Indice de Possibilidade de Quedas (IPQ). Utilizou-se estatística nao paramétrica para análise dos dados, adotando-se em todos os testes nível de significância 5(p¾0,05). G1 apresentou incremento significativo no EF (p = 0,001) e reduçao significativa na PQ (p = 0,013). Estes resultados indicam que a prática do Circuito de exercícios sensoriais é capaz de melhorar o equilíbrio e diminuir a possibilidade de quedas em idosas

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Exercícios físicos auxiliam na melhora do equilíbrio, entretanto há carência de protocolos específicos para trabalhar preventivamente o equilíbrio funcional (EF) e a possibilidade de quedas (PQ) em idosos da comunidade. O objetivo deste estudo foi avaliar o efeito de um Circuito de exercícios sensoriais (CE) sobre o EF e a PQ em mulheres idosas. Completaram o estudo 57 idosas, divididas em grupo experimental (G1= 32; 65,61±4,72 anos) e grupo controle (G2 = 25; 68,41±4,99 anos). G1 praticou 12 semanas de CE composto por 13 estaçoes em forma de circuito. Foram realizadas 2 aulas semanais de 50 minutos de duraçao, compostas por aquecimento, exercícios sensoriais e volta à calma. O grau de dificuldade foi progressivo ao longo do treinamento. EF e PQ foram avaliados antes e depois da intervençao, respectivamente pela Escala de Equilíbrio de Berg (EEB) e pelo Indice de Possibilidade de Quedas (IPQ). Utilizou-se estatística nao paramétrica para análise dos dados, adotando-se em todos os testes nível de significância 5(p¾0,05). G1 apresentou incremento significativo no EF (p = 0,001) e reduçao significativa na PQ (p = 0,013). Estes resultados indicam que a prática do Circuito de exercícios sensoriais é capaz de melhorar o equilíbrio e diminuir a possibilidade de quedas em idosas