Na 50 Nachlass Arthur Schopenhauer - 'Schopenhauer-Archiv', 325 - Angebot an Professor Hugo von Meltzl zur Mitarbeit in der Zeitschrift "Schopenhaueriana"

u.a.: Gustav Wilhelm Körber; Arthur Schopenhauer; Giacomo Leopardi;

Na 1 Nachlass Max Horkheimer, 520 - Korrespondenzen mit Walter Benjamin (Kopien) (p. VI 5A, 168 - 325)

4 Briefe zwischen Walter Benjamin und Cecilia Razovsky; 6 Briefe zwischen Cecilia Razovsky und Max Horkheimer; 1 Brief von Cecilia Razovsky an den American Consul, 17.11.1939; 1 Brief von Antonio Sols an Max Horkheimer, 30.10.1940; 1 Brief von Max Horkheimer an Antonio Sols, 11.10.1940; 1 Brief (Abschrift, Auszug) an A. R. L. Gurland von Frau Gurland, 11.10.1940; 3 Briefe zwischen dem Emergency Rescue Committee (New York) und Max Horkheimer, August 1940; 1 Brief von Max Horkheimer an Pastor del Rio, 17.07.1940; 1 Brief von Max Horkheimer an J. Wavrinek, 17.07.1940; 1 Brief von Theodor W. Adorno an Gershom Scholem, 16.07.1940; 1 Brief von Max Horkheimer an Hans Schaudinger, 13.07.1940; 1 Brief von Max Horkheimer an George S. Messersmith, 08.07.1940; 1 Brief von Max Horkheimer an Adolph Kates, 05.07.1940; 1 Brief von Max Horkheimer an Adolph Kates, 29.06.1940; 2 Briefe zwischen dem Refugee Section of the American Friends Service Committee (Philadelphia) und Max Horkheimer, Mai 1940; 2 Briefe von Egon Wissing an Max Horkheimer, 1940; 1 Brief von Max Horkheimer an die Economy Blue Print Co. (New York), 25.05.1940; 1 Brief von Werner Kraft an Max Horkheimer, 30.04.1940;

Ms.Ff.F.Stoltze 3. 325 - Brief von Friedrich Stoltze an Kaspar Susenbeth

Bitte um einen Band Conversationslexikon

Great Barrier Reef coral element/Ca and stable isotope data and U-Th ages from IODP Expedition 325

Tropical south-western Pacific temperatures are of vital importance to the Great Barrier Reef (GBR), but the role of sea surface temperatures (SSTs) in the growth of the GBR since the Last Glacial Maximum remains largely unknown. Here we present records of Sr/Ca and d18O for Last Glacial Maximum and deglacial corals that show a considerably steeper meridional SST gradient than the present day in the central GBR. We find a 1-2 °C larger temperature decrease between 17° and 20°S about 20,000 to 13,000 years ago. The result is best explained by the northward expansion of cooler subtropical waters due to a weakening of the South Pacific gyre and East Australian Current. Our findings indicate that the GBR experienced substantial meridional temperature change during the last deglaciation, and serve to explain anomalous deglacial drying of northeastern Australia. Overall, the GBR developed through significant SST change and may be more resilient than previously thought.