Alfred Döblin [Illustration] : Porträtskizze

Kurt Harald Isenstein

Heinrich Heine [Illustration] : Plastik

Kurt Harald Isenstein

Na 1 Nachlass Max Horkheimer, 16 - Korrespondenzen u.a. mit Gerhart Jacoby Gordon (p. I 8, 202-379)

2 Briefe von A. Gandon an Max Horkheimer, Februrar 1936; 1 Brief von Max Horkheimer an Lloyd K. Garrison, 25.03.1941; 4 Briefe zwischen Moritz Geiger und Max Horkheimer, 01.12.1935, 1935; 1 Lebenslauf von Alvin Johnsson an Friedrich Pollock; 1 Brief von Alvon Johnson an Friedrich Pollock, 39.09.1940; 1 Brief von Max Horkheimer an Harald Genssler, 04.09.1949; 1 Brief von der George Washington University Washington an Max Horkheimer, 01.03.1939; 2 Briefe von Wolfgang Gerloff an Max Horkheimer, 1934, 1939; 2 Briefe zwsichen Hans Gerth und Max Horkheimer, 28.10.1937, 16.11.1937; 1 Brief von M. Getzer anMax Horkheimer, 04.05.1934; 12 Briefe zwsichen Edgar V. M. Gilbert und Max Horkheimer, 1935-1940; 1 Brief von der Gillespie, Kinsports & Bears Travel Agency New York an Max Horkheimer, 16.04.1935; 1 Entwurf von Max Horkheimer an Morris Ginsberg, Dezember 1935; 19 Briefe zwsichen Morris Ginsberg, Ethel Ginsberg und Max Horkheimer, 1935-1938; 2 Briefe zwischen Robert Morrison MacIver und Max Horkheimer, 18.08.1937, 16.08.1937; 1 Brief von H. Girsberger an Max Horkheimer, 17.08.1938; 1 Brief von Max Horkheimer an Glass, 24.12.1940; 1 Brief von der Glidden Buick Corporation New York an Max Horkheimer, 05.06.1940; 1 Heiratsanzeige von Vera Gold; 4 Briefe zwischen Oskar Goldberg und Max Horkheimer, 1941, 27.08.1941; 10 Briefe zwischen Hans Goldmann und Max Horkheimer, 1934-1937; 14 Briefe zwischen Alfons Goldschmidt und Max Horkheimer, 1936-1938; 7 Briefe zwsichen dem Greater New York Coordinating Committee for German Refugees, New York und Max Horkheimer, 1937-1939; 1 Brief von Max Horkheimer an Simon Guggenheim, 24.01.1938; 3 Briefe zwischen Aron Goldschmidt und Max Horkheimer, 02.02.1939, Mai 1942; 2 Briefe zwischen Berta Goldschmidt und Max Horkheimer, 14.01.1941, 25.02.1941; 4 Briefe von Emma Goldschmidt an Juliette Favez, 1938-1940; 5 Briefe zwischen Emma Goldschmidt und Max Horkheimer, 1938-1940; 2 Briefe zwischen Ernst L. Goldschmidt und Max Horkheimer, 08.07.1937, 18.06.1937; 1 Brief von Thea Goldschmidt an Max Horkheimer, 16.04.1935; 14 Briefe zwischen Kurt Goldstein und Max Horkheimer, 1934-1941; 19 Briefe zwsichen Gerhart Jacoby Gordon und Max Horkheimer, 1934-1937;

Water stable oxygen isotope records from six Antarctic ice core sites for the present and last interglacial periods

We compare the present and last interglacial periods as recorded in Antarctic water stable isotope records now available at various temporal resolutions from six East Antarctic ice cores: Vostok, Taylor Dome, EPICA Dome C (EDC), EPICA Dronning Maud Land (EDML), Dome Fuji and the recent TALDICE ice core from Talos Dome. We first review the different modern site characteristics in terms of ice flow, meteorological conditions, precipitation intermittency and moisture origin, as depicted by meteorological data, atmospheric reanalyses and Lagrangian moisture source diagnostics. These different factors can indeed alter the relationships between temperature and water stable isotopes. Using five records with sufficient resolution on the EDC3 age scale, common features are quantified through principal component analyses. Consistent with instrumental records and atmospheric model results, the ice core data depict rather coherent and homogenous patterns in East Antarctica during the last two interglacials. Across the East Antarctic plateau, regional differences, with respect to the common East Antarctic signal, appear to have similar patterns during the current and last interglacials. We identify two abrupt shifts in isotopic records during the glacial inception at TALDICE and EDML, likely caused by regional sea ice expansion. These regional differences are discussed in terms of moisture origin and in terms of past changes in local elevation histories, which are compared to ice sheet model results. Our results suggest that elevation changes may contribute significantly to inter-site differences. These elevation changes may be underestimated by current ice sheet models

Eocene to Early Miocene palaeoclimate of Saxony, Germany (Table 4)

In the present study, proxy data concerning changes in atmospheric CO2 and climatic conditions from the Late Eocene to the Early Miocene were acquired by applying palaeobotanical methods. Fossil floras from 10 well-documented locations in Saxony, Germany, were investigated with respect to (1) stomatal density/index of fossil leaves from three different taxa (Eotrigonobalanus furcinervis, Laurophyllum pseudoprinceps and Laurophyllum acutimontanum), (2) the coexistence approach (CA) based on nearest living relatives (NLR) and (3) leaf margin analysis (LMA). Whereas the results of approach (1) indicate changes in atmospheric CO2 concentration, approaches (2) and (3) provide climate data. The results of the analysis of stomatal parameters indicate that the atmospheric CO2 concentration was higher during the Late Eocene than during the Early Oligocene and increased towards the Late Oligocene. A lower atmospheric pCO2 level after the Late Eocene is also suggested by an increase in marine palaeoproductivity at this time. From the Late Oligocene onwards, no changes in atmospheric CO2 concentration can be detected with the present data. For the considered sites, the results of the coexistence approach and of the leaf margin analysis document a significant cooling event from the Late Eocene to the Early Oligocene. The pCO2 decrease from the Late Eocene to the Early Oligocene indicated by the stomatal data raised in this study was thus coupled to a temperature decrease which is reflected by the present datasets. From the Early Oligocene onwards, however, no further fundamental climate change can be inferred for the considered locations. The pCO2 increase from the Early Oligocene to the Late Oligocene, which is indicated by the present data, is thus not accompanied by a climate change at the considered sites. A warming event during the Late Oligocene is, however, recorded by marine climate archives. According to the present data, no change in pCO2 occurred during the cooling event at the Oligocene/Miocene boundary, which is also indicated by marine data. The quality and validity of stomatal parameters as sensors for atmospheric CO2 concentration are discussed.