990 resultados para 154-929


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Vorbesitzer: Dominikanerkloster Frankfurt am Main

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Gustav Kanngießer, Stoltze: Gesammelte Werke, Frankfurt: Oberbürgermeister

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56 Briefe und Beilage zwischen dem Professor Alfred Schmidt und Max Horkheimer,1955-1973; 3 Briefe von Max Horkheimer an Erika Busch, 1971-1973; 1 Brief von Max Horkheimer an Professor Hans-Gerd Schumann, 1971; 1 Brief von Max Horkheimer an Professor Ludwig Preller, 1964;

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H. Marschner. [Text] von E. Geibel

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"Visual Project" (Datierung unklar), 17 Photographien, Testmaterial; "Über Autoritätsbeziehungen in einer Familie. Protokoll einer sozial-psychologischen Familienbeobachtung" (Datierung und Zugehörigkeit unklar). Typoskript, englisch, 3 Blatt; "Impact of the Palestine Situation on the American People" (Datierung unklar, nicht vor 1946):; 1. "A Study Proposal". Als Typoskript vervielfältigt, 6 Blatt; 2. William B. Ziff: "The Rape of Palestine", New York 1946, 118 Seiten;

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Vorbesitzer: Bernhard Diell;

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The climate evolution of the South Shetland Islands during the last c. 2000 years is inferred from the multiproxy analyses of a long (928 cm) sediment core retrieved from Maxwell Bay off King George Island. The vertical sediment flux at the core location is controlled by summer melting processes that cause sediment-laden meltwater plumes to form. These leave a characteristic signature in the sediments of NE Maxwell Bay. We use this signature to distinguish summer and winter-dominated periods. During the Medieval Warm Period, sediments are generally finer which indicates summer-type conditions. In contrast, during the Little Ice Age (LIA) sediments are generally coarser and are indicative of winter-dominated conditions. Comparison with Northern and Southern Hemisphere, Antarctic, and global temperature reconstructions reveals that the mean grain-size curve from Maxwell Bay closely resembles the curve of the global temperature reconstruction. We show that the medieval warming occurred earlier in the Southern than in the Northern Hemisphere, which might indicate that the warming was driven by processes occurring in the south. The beginning of the LIA appears to be almost synchronous in both hemispheres. The warming after the LIA closely resembles the Northern Hemisphere record which might indicate this phase of cooling was driven by processes occurring in the north. Although the recent rapid regional warming is clearly visible, the Maxwell Bay record does not show the dominance of summer-type sediments until the 1970s. Continued warming in this area will likely affect the marine ecosystem through meltwater induced turbidity of the surface waters as well as an extension of the vegetation period due to the predicted decrease of sea ice in this area.

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