Un procès dans la famille des Ibn Tibbon (Marseille, 1255-1256)

par Isidore Loeb

Na 1 Nachlass Max Horkheimer, 2 - Korrespondenzen u.a. an Raymond Aron (p. I 1, 206-333)

16 Briefe zwischen Ruth Nanda Anshen und Max Horkheimer, 1938-1941; 5 Briefe zwischen Peter Appel und Max Horkheimer, 1937; 1 Drucksache der Arbeitsgemeinschaft Sozialistischer Ärzte in Hessen, Juli 1949; 1 Brief der Arbeitsgemeinschaft für Soziale Betriebsgestaltung in Heidelberg an Max Horkheimer, 18.10.1949; 2 Briefe zwischen Lois Archer und Max Horkheimer, 24.07.1947, 04.08.1947; 2 Briefe zwischen Camille Arnaud und Max Horkheimer, 03.03.1946, 22.03.1946; 39 Briefe zwischen Raymond Aron und Max Horkheimer, 1935-1938; 2 Briefe zwischen Ruth Arrau und Max Horkheimer, 28.06.1949, 10.10.1949; 3 Briefe zwischen S. Aufhauser und Max Horkheimer, 1939-1941, 16.04.1941; 8 Briefe zwischen der Zeitschrift 'Aufbau' und Max Horkheimer, 1944-1944; 3 Briefe zwischen der Automobile Club of New York und Max Horkheimer, 1937, 10.08.1937;

Na 50 Nachlass Arthur Schopenhauer - 'Schopenhauer-Archiv', 206 - Danksagung wegen des positiven Urteils über die herausgegebenen Kantschen Werke

u.a.: Studienreise; Bearbeitung des Nachlasses von Immanuel Kant; Bellavesne;

Na 1 Nachlass Max Horkheimer, 446 - Korrespondenzen mit der UNESCO (p. V 168, 145-206)

Drucksachen und Schriftwechsel der UNESCO (Paris, Hamburg, Gauting), 1957-1965; 69 Briefe zwischen Dr. Gilda Mara, UNESCO und Max Horkheimer, 1959-1965; 12 Briefe zwischen Dr. Helga Timm, UNESCO und Max Horkheimer, 1957-1958;

Na 1 Nachlass Max Horkheimer, 539 - Korrespondenzen mit Leo Löwenthal und Friedrich Pollock (p. VI 15, 1 - 206)

113 Briefe zwischen Max Horkheimer und Leo Löwenthal; 1 Brief von Leo Löwenthal an Moritz Horkheimer, 25.08.1942; 1 Brief von Leo Löwenthal an Alfredo Mendizabel, 19.08.1942; 1 Brief von Eileen A. Fry an Max Horkheimer, 19.08.1942; 4 Briefe zwischen Leo Löwenthal und Frederick Pollock, 1942; 1 Brief von Max Horkheimer an Frederick Pollock, 11.12.1942;

Ms.Ff.F.Stoltze 3. 206 - Brief von Karl Gustav Odermann an Friedrich Stoltze

Stoltze: Gedicht in den Berichten des Freien Deutschen Hochstifts (1880, S. 395), Bitte um Abschrift des Stoltze-Gedichts zu Friedrich Schillers 100. Geburtstag

Na 1 Nachlass Max Horkheimer, 553 - Korrespondenzen mit Leo Löwenthal (p. VI 22, 1-206)

126 Briefe zwischen Max Horkheimer und Leo Löwenthal, Januar - August 1948; 1 Brief von J. D. Scott an Max Horkheimer, 28.04.1948; 1 Telegramm von Fred May an Leo Löwenthal, 22.04.1948; 2 Briefe zwischen David Riesmann und Leo Löwenthal, Februar - März 1948; 1 Brief von Max Horkheimer an Herbert Macuse, 1948; 1 Brief von Leo Löwenthal an William Dieterle, 27.02.1948; 2 Briefe zwischen Theodor W. Adorno und Leo Löwenthal, 1948; 1 Brief von Max Horkheimer an Samuel H. Flowerman, 20.02.1948; 1 Brief von Irving Howe an Leo Löwenthal, 02.09.1948; 3 Briefe zwischen Erich Preiser und Leo Löwental, 1948; 1 Brief von Walter Hallstein an Max Horkheimer, 02.07.1948; 1 Brief von Max Horkheimer an M. Fiske Lissance, 05.02.1948; 1 Brief und 1 Memorandum an John Slawson von Max Horkheimer, 10.01.1948;

Ausst. 206 - De vitanda vsvra ex Greco in Latinvm tradvctvs

Vorbesitzer: Heinrich Anton Cornill-d'Orville (Exlibris im Vorderdeckel)

Ms. lat. oct. 206 - Annotata ad Burkhardi Gotthelfi Struvii Bibliothecam iuris selectam

Vorbesitzer: Familie von Holzhausen;

In-situ Iron isotope measurements and mineral compositions from ODP Hole 206-1256D and IODP Hole 335-U1256D

In-situ Fe isotope measurements have been carried out to estimate the impact of the hydrothermal metamorphic overprint on the Fe isotopic composition of Fe-Ti-oxides and Fe-sulfides of the different lithologies of the drilled rocks from IODP Hole 1256D (eastern equatorial Pacific; 15 Ma crust formed at the East Pacific Rise). Most igneous rocks normally have a very restricted range in their 56Fe/54Fe ratio. In contrast, Fe isotope compositions of hot fluids (> 300 °C) from mid-ocean-ridge spreading centers define a narrow range that is shifted to lower delta 56Fe values by 0.2 per mil - 0.5 per mil as compared to igneous rocks. Therefore, it is expected that mineral phases that contain large amounts of Fe are especially affected by the interaction with a fluid that fractionates Fe isotopes during exsolution/precipitation of those minerals. We have used a femtosecond UV-Laser ablation system to determine mineral 56Fe/54Fe ratios of selected samples with a precision of < 0.1 per mil (2 sigma level) at micrometer-scale. We have found significant variations of the delta 56Fe (IRMM-014) values in the minerals between different samples as well as within samples and mineral grains. The overall observed scale of delta 56Fe (magnetite) in 1256D rocks ranges from - 0.12 to + 0.64 per mil, and of delta 56Fe (ilmenite) from - 0.77 to + 0.01 per mil. Pyrite in the lowermost sheeted dike section is clearly distinguishable from the other investigated lithological units, having positive delta 56Fe values between + 0.29 and + 0.56 per mil, whereas pyrite in the other samples has generally negative delta 56Fe values from - 1.10 to - 0.59 permil. One key observation is that the temperature dependent inter-mineral fractionations of Fe isotopes between magnetite and ilmenite are systematically shifted towards higher values when compared to theoretically expected values, while synthesized, well equilibrated magnetite-ilmenite pairs are compatible with the theoretical predictions. Theoretical considerations including beta-factors of different aqueous Fe-chlorides and Rayleigh-type fractionations in the presence of a hydrous, chlorine-bearing fluid can explain this observation. The disagreement between observed and theoretical equilibrium fractionation, the fact that magnetite, in contrast to ilmenite shows a slight downhole trend in the delta 56Fe values, and the observation of small scale heterogeneities within single mineral grains imply that a general re-equilibration of the magnetite-ilmenite pairs is overprinted by kinetic fractionation effects, caused by the interaction of magnetite/ilmenite with hydrothermal fluids penetrating the upper oceanic crust during cooling, or incomplete re-equilibration at low temperatures. Furthermore, the observation of significant small-scale variations in the 56Fe/54Fe ratios of single minerals in this study highlights the importance of high spatial-resolution-analyses of stable isotope ratios for further investigations.