Na 1 Nachlass Max Horkheimer, 48 - Korrespondenzen u.a. an Thorsten Sellin (p. I 22, 227-395)

2 Briefe zwischen Luther L. Gobbel und Max Horkheimer, 28.09.1938, 03.10.1938; 2 Briefe zwischen Russell M. Story und Max Horkheimer, 15.03.1938; 1 Brief von Max Horkheimer an Ralph E. Boothby, 14.03.1938; 1 Brief von Max Horkheimer an Roswell G. Ham, 13.01.1938; 2 Briefe von Carl Schurz von der Memorial Foundation Philadelphia an Max Horkheimer, 1940; 7 Briefe zwischen Helen Schuster und Max Horkheimer, 1936, 1937, 1947-1948; 1 Brief von Liesel Schwaibold an Max Horkheimer, 19.01.1937; 6 Briefe zwischen Ph. Schwartz und Max Horkheimer, 1936-1937; 4 Briefe zwischen Ph. Schwart an Ludwig Jekels, 1936, 1937; 1 Brief von Ph. Schwartz an Karl Landauer,; 1 Brief von Eugen Schwarz an den Vater von Max Horkheimer, 08.12.1937; 1 Brief von Max Horkheimer an Eugen Schwarz, 31.12.1937; 5 Briefe zwischen Olga Therese Schwarz und Max Horkheimer, 1942; 8 Briefe zwischen Alfred Schweizer und Max Horkheimer, 1940-1941; 1 Lebenslauf von Arthur Heinrich Schweitzer und 1 Bericht über Arthur Heinrich Schweitzer; 1 Brief von Josef Schwoner an Max Horkheimer, 20.06.1941; 1 Brief von Max Horkheimer an L. H. Seelye, 01.04.1935; 1 Brief von Max Horkheimer an Dora Segall-Ziegellaub, 01.10.1935; 6 Briefe zwischen Matyes Seiber und Max Horkheimer, Juli 1936, 1936; 2 Briefe zwischen Alfred Seidenmann und Max Horkheimer, 29.02.1940, 12.03.1940 sowie Briefwechsel mit dem American Freinds Service Committee, Phiadelphia; 2 Briefe zwischen dem American Friends Service Committee und Max Horkheimer, 12.09.1940; 3 Rundschreiben von der Selbsthilfe Deutscher Ausgewanderter New York, 1937-1938; Antworten auf einen Fragebogen des Selective Service Occupational Questionnaire von Max Horkheimer, 27.10.1942; 1 Brief vom Selfhelp of Emigres from Central Europe an Margot von Mendelssohn, 22.12.1948; 8 Briefe zwischen Edwin R. A. Seligman und Max Horkheimer, 1938-1939; 1 Brief von Max Horkheimer an Eustace Seligman, 11.03.1940; 1 Brief von Seligmann und Cia an Friedrich Pollock, 06.04.1936; 2 Brife zwischen Milton C. Seligman und Max Horkheimer, 1947; 1 Brief Stephen Schäfer an Thorsten Sellin, 07.02.1939; 17 Briefe zwischen Thorsten Sellin und Max Horkheimer, 1938-1941; 1 Brief von der Sherwin Cody School of English an Max Horkheimer, 06.02.1939; 3 Briefe und 1 Beilage zwischen Edward A. Shils und Max Horkheimer, 1938; 10 Briefe zwischen James T. Shotwell und Max Horkheimer, 01.07.1940-1941;

Na 1 Nachlass Max Horkheimer, 531 - Korrespondenzen u.a. mit Paul Honigsheim (p. VI 11, 1 - 286)

98 Briefe zwischen Paul Honigsheim und Max Horkheimer, 1934 - 1941; 1 Brief von Selfhelp of Emigres from Central Europe (New York) an Leo Löwenthal, 14.01.1941; 1 Brief von Hertha Kraus an Paul Honigsheim, 01.04.1935; 1 Brief an die Rockefeller Foundation (Paris) von Max Horkheimer, 22.02.1935; 3 Briefe zwischen Max Horkheimer und Anne Mendelsohn, 1934; 1 Brief an Paul Honigsheim von Hubert Abrahamsohn, 07.06.1934; 40 Briefe zwischen Marie (Mitzi) Jahoda und Max Horkheimer, 1935 - 1949;

(Table 1) Characteristics of Klebsormidium (filamentous green algae) strains from the Antarctic, Arctic and Slovakia

The freezing and desiccation tolerance of 12 Klebsormidium strains, isolated from various habitats (aero-terrestrial, terrestrial, and hydro-terrestrial) from distinct geographical regions (Antarctic - South Shetlands, King George Island, Arctic - Ellesmere Island, Svalbard, Central Europe - Slovakia) were studied. Each strain was exposed to several freezing (-4°C, -40°C, -196°C) and desiccation (+4°C and +20°C) regimes, simulating both natural and semi-natural freeze-thaw and desiccation cycles. The level of resistance (or the survival capacity) was evaluated by chlorophyll a content, viability, and chlorophyll fluorescence evaluations. No statistical differences (Kruskal-Wallis tests) between strains originating from different regions were observed. All strains tested were highly resistant to both freezing and desiccation injuries. Freezing down to -196°C was the most harmful regime for all studied strains. Freezing at -4°C did not influence the survival of studied strains. Further, freezing down to -40°C (at a speed of 4°C/min) was not fatal for most of the strains. RDA analysis showed that certain Antarctic and Arctic strains did not survive desiccation at +4°C; however, freezing at -40°C, as well as desiccation at +20 °C was not fatal to them. On the other hand, other strains from the Antarctic, the Arctic, and Central Europe (Slovakia) survived desiccation at temperatures of +4°C, and freezing down to -40°C. It appears that species of Klebsormidium which occupy an environment where both seasonal and diurnal variations of water availability prevail, are well adapted to freezing and desiccation injuries. Freezing and desiccation tolerance is not species-specific nor is the resilience only found in polar strains as it is also a feature of temperate strains.

Early Oligocene continental climate ofthe Paleogene Basin in Hungary and Slovenia

This paper concentrates on the Early Oligocene palaeoclimate of the southern part of Eastern and Central Europe and gives a detailed climatological analysis, combined with leaf-morphological studies and modelling of the palaeoatmospheric CO2 level using stomatal and d13 C data. Climate data are calculated using the Coexistence Approach for Kiscellian floras of the Palaeogene Basin (Hungary and Slovenia) and coeval assemblages from Central and Southeastern Europe. Potential microclimatic or habitat variations are considered using morphometric analysis of fossil leaves from Hungarian, Slovenian and Italian floras. Reconstruction of CO2 is performed by applying a recently introduced mechanistic model. Results of climate analysis indicate distinct latitudinal and longitudinal climate patterns for various variables which agree well with reconstructed palaeogeography and vegetation. Calculated climate variables in general suggest a warm and frost-free climate with low seasonal variation of temperature. A difference in temperature parameters is recorded between localities from Central and Southeastern Europe, manifested mainly in the mean temperature of the coldest month. Results of morphometric analysis suggest microclimatic or habitat difference among studied floras. Extending the scarce information available on atmospheric CO2 levels during the Oligocene, we provide data for a well-defined time-interval. Reconstructed atmospheric CO2 levels agree well with threshold values for Antarctic ice sheet growth suggested by recent modelling studies. The successful application of the mechanistic model for the reconstruction of atmospheric CO2 levels raises new possibitities for future climate inference from macro-flora studies.

Pollen records from two outcrop profiles in the Kakitu Mountain of Tibet

There is a great similarity between pollen types which occur in the early Holocene NE Tibetan pollen spectra and those which are commonly considered to be typical for the Würm Late Glacial period in Central Europe and for the Würm Pleniglacial period in Southern Europe. Evidently, this similarity is due to a remarkable general conformity of plant taxa growing in cold-arid regions of the northern hemisphere. The improvement of the climate and the retreat of the glaciers that commenced at the end of the Würm period had already terminated definitely before 9500 BP. In addition, the climatic situation as well as the vegetation belts must have remained rather constant during the following 3000 yr, i.e. through most parts of the climatic optimum of the Holocene.