998 resultados para Althann, Michael Friedrich cardinal von -- Portraits


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von Georg Friedrich Händel

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von G. F. Händel. Übers. von G. G. Gervinus

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von G. F. Händel. Auf Grund der beiden ital. Partituren in Band 63 der großen Händel-Ausg. neu gestaltet von Josef Wenz

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von F. Dorguth

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von Friedrich Neckarthäler

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Von Oberlehrer Dr. F. Ludwig

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183 Briefe zwischen Herbert Marcuse und Max Horkheimer; 6 Briefe zwischen Margot von Mendelssohn und Herbert Marcuse, 1942 - 1949; 1 Brief von Friedrich Pollock an Max Horkheimer, 20.04.1943; 1 Brief von dem Office of Strategic Services (Washington) an Herbert Marcuse, 07.12.1942; 1 Brief von dem Office of War Information (Washington) an Herbert Marcuse, 16.11.1942; 3 Briefe zwischen Herbert Marcuse und Francis K. Ballaine, Januar 1942; 1 Brief an Friedrich Pollock von Herbert Marcuse, 18.07.1949; 1 Brief von Herbert Marcuse an Leo Löwenthal, 11.04.1949;

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von Friedrich Wrede

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From a 10.7 m long gravity core from the Sierra Leone Rise (5°39.5' N, 19°51' W) a detailed oxygen and carbon isotope record of both planktonic and benthonic foraminifera species was obtained extending from the Recent to Jaramillo event. The analysis yielded six major results. 1. Benthos oxygen isotopes varied by 1.8-2.2 per mil from interglacial to glacial times and may indicate a synglacial cooling of North Atlantic Deep Water at 2800 m depth by 1-3°C. 2. Variable anomalies between the benthos and plankton d18O record indicate a cooling of sea-surface temperatures (SST) by up to 6 °C during some glacial stages. 3. Southerly trade winds and equatorial upwelling may excert the primary control off SST variations, in particular of extremee values of cold and warm stages and of the abrupt character of climate transitions and their leads and lags, and finally, of variable sedimentation rates. 4. The benthos d13C record correlates well with the flux and preservation of organic matter. 5. A new time scale, CARPOR, was established from the assumption that terrigenous sediment supply was ± constant bit CaCO3 varied considerably. When applied to the d18O record, three major and numerous short-term variations of sedimentation rates (0.8 to 4.0 cm/kyr) can be distinguished. 6. The climatic record was modified by bioturbation much more strongly during cold than during warm stages.