Na 1 Nachlass Max Horkheimer, 673 - Forschungsprojekte über Antisemitismus, Vorurteil, Autorität: Einzeluntersuchungen (p. IX 139 - IX 140.1-14)

Assignements. Anweisungen zu Einzeluntersuchungen des Antisemitismus-Projekts, 1943 und ohne Datum, 15 Blatt; Zum 'Berkeley Projekt on Antisemitism', 1944-1946; Sitzungsprotokolle und Memoranden der 'Los Angeles Branch of the Berkeley Research Project on Social Discrimination', 19.03.1946 - 11.04.1946, Typoskript, 11 Blatt; Frenkel-Brunswik, Else: 1 Brief mit Unterschrift an Max Horkheimer, ohne Ort, 10.01.1944, 6 Blatt; Interview- und Testprotokolle, Typoskript, 33 Blatt; Horkheimer, Max: 1 Brief an Theodor W. Adorno, ohne Ort, 11.10.1945, 5 Blatt; "Traits of the Authoritatian Character", a) Typoskript, 2 Blatt; b) Typoskript, 2 Blatt; c) Typoskript mit eigenhändigen Korrekturen und Ergänzungen, von Max Horkheimer, 2 Blatt; "Hypothese concerning indirect questions of Berkeley Questionaire". Als Typoskript vervielfältigt, 4 Blatt; Frenkel-Brunswik, Else; Sanford, R. Nevitt: "Some Personality Factors in Anti-Semitism", Sonderdruck aus: The Journal of Psychology, 1945, 20, S. 271-291; Levison, Daniel J.; Sanford, R. Nevitt: "A Scale for the Measurement of Anti-Semitism", Sonderdrucke aus: The Journal of Psychology, 1944,17, S.339-370; "'Unconscious' Facism", Excerpt aus: Propaganda Analysis, No. 7, L938, Typoskript 1 Blatt; Löwenthal, Leo: 1 Brief mit Unterschrift an Max Horkheimer, New York, 31.05.1945; Deutsch, Monroe E.: 2 Briefe mit Unterschrift an Max Horkheimer, Berkeley, 1945; 4 Briefe und Beantwortung von Max Horkheimer, Pacific Palisades, 1945; Lundberg, O.: 5 Briefe von Max Horkheimer, Pacific Palisades, 1945-1946; Sanfort, Nevitt: 1 Brief von Samuel H. Flowerman, ohne Ort, 14.06.1947; Statement for Berkeley Public Opinio Study Group Accounts, 19 Blatt;

Late Quaternary calcareous nannofossils in ODP Leg 139 holes

Upper Quaternary calcareous nannofossils contained in drill cores taken in the heavily sedimented Middle Valley of the northern Juan de Fuca Ridge in the northeast Pacific Ocean (Ocean Drilling Program Leg 139) are investigated. The host sediments have been subjected at depth to high temperatures and hot hydrothermal fluids that have altered or destroyed in part or in toto the nannofossil assemblages, thereby raising at several sites the level of the first (deepest) stratigraphic occurrence of nannofossils or of the important Emiliania huxleyi datum. The degree of alteration of the nannofossil assemblages is dependent on the intensity of the hydrothermal activity, which is indicated by paleotemperatures derived independently from studies of color alteration of palynomorphs and by vitrinite reflectance (Mao et al., this volume). State of preservation and the downhole level at which assemblages have been destroyed correlate well with the inferred paleotemperature estimates. Destruction of the assemblages appears to be species selective and follows in general the dissolution rankings determined independently by others for Recent nannofossils of the Pacific basin. More systematic correlation of these phenomena is hampered, however, by the fact that nannofossil preservation is already quite variable at the time of deposition because of the predominance of turbidite activity in the study area.

Piglia, Ricardo. Formas breves. Buenos Aires, Temas de Grupo Editorial, 1999, 139 págs

Fil: Príncipi, Ana Sofía. Universidad Nacional de La Plata. Facultad de Humanidades y Ciencias de la Educación; Argentina.

Piglia, Ricardo. Formas breves. Buenos Aires, Temas de Grupo Editorial, 1999, 139 págs

Fil: Príncipi, Ana Sofía. Universidad Nacional de La Plata. Facultad de Humanidades y Ciencias de la Educación; Argentina.

Mineral, chemical and isotopic compositions of hydrothermally altered sediments from the Middle Valley (Juan de Fuca Ridge), ODP Site 139-858

Li and Li isotopes have been measured in the clay fraction of sediments recovered from the Middle Valley hydrothermal site on the Juan De Fuca Ridge. The Li content of pure detrital clays is 51 ppm while hydrothermal clays and carbonates have lower Li (22+/-11 ppm). However, there is no clear relationship between the mineralogy of the hydrothermal alteration products and their Li content. The d7Li value of the detrital clays is +5.8?. Hydrothermal clays and carbonates have d7Li in the range of -3.9? to +7.8?; these values do not seem to be dependent on the temperature at which they formed. Modelling of the Li and Li isotope systematics indicates that the fluid from which the alteration products form is significantly enriched in Li (higher than 10000 µmol/kg) relative to pore fluids recovered from within the sediments (up to 589 µmol/kg; [Wheat, C.G., M.J. Mottl, 1994. Data report: trace metal composition of pore water from Sites 855 through 858, Middle valley, Juan De Fuca Ridge. In Mottl, M.J., Davis, E.E., Fisher, A.T., Slack, J.F. (Eds.), Proc. ODP, Sci. Res. 139: 749-755; doi:10.2973/odp.proc.sr.139.269.1994]), and that this Li is derived from sediment. Thus, the alteration products are not in equilibrium with their conjugate pore fluids; rather, the alteration minerals formed at lower water/sediment ratios. This suggests that fluid flow pathways at Middle Valley were more diffuse in the past than they are today.