Ms.Ff.F.Stoltze 3. 166 - Brief von Theobald Kerner an Friedrich Stoltze

Dank für ein Gedicht, Ludwig Pfau, Übersendung eines Gedichts, Carl Mayer

Na 1 Nachlass Max Horkheimer, 691 - "Materialien zum Antisemitismus", "Die deutschen Arbeiter und Angestellten", "Neue Enquêten über Folgen der Arbeitslosigkeit" (p. IX 164 - IX 166.1-13)

"Materialien zum Antisemitismus" (1940-65): Zeitungsausschnitte, Broschüren, Drucksachen; "Die deutschen Arbeiter und Angestellten" (1930-38):; 1. Inhaltsverzeichnisse, Typoskripte, 5 Blatt; 2. Fragebogen zur Erhebung, Druck, 4 Blatt; 3. Statistische Auswertung der Fragebögen; 4. Max Horkheimer: eigenhändige Notzizen zur Erhebung, 1 Blatt; 5. Robert S. Lynd: 1 Brief (Abschrift) an Erich Fromm, New York, 7.2.1938; 6. "Arbeiter und Angestellten-Enquête". Zum Stand der Ausarbeitung, 1937, Typoskript, 3 Blatt; 7. Bibliographien, Typoskripte, 42 Blatt; "Neue Enquêten über Folgen der Arbeitslosigkeit" (1936-37):; 1. Liste der Erhebungen in Österreich, Palestina, USA, 5 Blatt; 2. "Remarque générale sur l'enquête". Typoskript mit eigenhändigen Korrekturen, 9 Blatt; 3. - 6. Protokolle von Familieninterviews in Wien, 1937; 7. "Literatur über die psychologischen Wirkungen der Arbeitslosigkeit" (1936). Typoskript, 15 Blatt; 8. Hilde Oppenheimer-Bluhm: 1 Brief mit Unterschrift an Friedrich Pollock, Jerusalem, 7.12.1936, 1 Blatt; 9. Paul F. Lazarsfeld: "Memorandum Subject: Remarks on the French Questionaire" (12.3.1937). Typoskript, 1 Blatt; 10. Paul F. Lazarsfeld: "Report on the University of Newark Research Center". Als Typoskript vervielfältigt, 9 Blatt; 11. "Publications Directed and Distributed by Bureau of Social Research, Municipal University of Omaha, Omaha, Nebraska". Als Typoskript viervielfältigt, 3 Blatt; 12. Programm zur Conférence Internationale des Sciences Sociales, Paris, 1937, Drucksachen, 3 Blatt; 13. The American Sociological Society: Rundschreiben, Drucksache, 2 Blatt;

Ms. lat. oct. 166 - Collectanea theologica et litteraria

Vorbesitzer: Bernhard Waldschmidt;

Mineralogic, elemental, and stable isotopic composition of bulk carbonate sediments from ODP Leg 166 sites

An intensive mineralogic and geochemical investigation was conducted on sediments recovered during Ocean Drilling Program Leg 166 from the western Great Bahama Bank at Sites 1006, 1008, and 1009. Pleistocene through middle Miocene sediments recovered from Site 1006, the distal location on the Leg 166 transect, are a mixture of bank-derived and pelagic carbonates with lesser and varying amounts of siliciclastic clays. A thick sequence of Pleistocene periplatform carbonates was recovered near the platform edge at Sites 1008 and 1009. Detailed bulk mineralogic, elemental (Ca, Mg, Sr, and Na), and stable isotopic (d18O and d13C) analyses of sediments are presented from a total of 317 samples from all three sites.

Fernando Martin De Blassi, Consideraciones sobre la justicia en Tomás de Aquino, CEFIM – SS&CC Ediciones, Mendoza 2013 (Cuadernos Medievales de Cuyo 7), 166 pp., ISBN 978-950-9064-90-4

Fil: Peretó Rivas, Rubén.

Whole rock geochemistry and stable isotopes of rocks, fragments and foraminifers from two ODP Leg 166 holes

Total carbon and carbonate contents, quantitative carbonate mineralogy, trace metal concentrations, and stable isotope compositions were determined on a suite of samples from the Miocene sections at Sites 1006 and 1007. The Miocene section at Site 1007, located at the toe-of-slope, contains a relatively high proportion of bank-derived components and becomes fully lithified at a depth of ~300 meters below seafloor (mbsf). By contrast, Miocene sediments at Site 1006, situated in Neogene drift deposits in the Straits of Florida and composed primarily of pelagic carbonates, do not become fully lithified until a depth of ~675 mbsf. Diagenetic and compositional contrasts between Sites 1006 and 1007 are reflected in geochemical data derived from sediment samples from each site.

Interstitial water d13C and sediment geochemistry of ODP Leg 166 sites

A review of interstitial water samples collected from Sites 1003-1007 of the Bahamas Transect along with a shore-based analysis of oxygen and carbon isotopes, minor and trace elements, and sediment chemistry are presented. Results indicate that the pore-fluid profiles in the upper 100 meters below seafloor (mbsf) are marked by shifts between 20 and 40 mbsf that are thought to be caused by changes in sediment reactivity, sedimentation rates, and the influence of strong bottom currents that have been active since the late Pliocene. Pore-fluid profiles in the lower Pliocene-Miocene sequences are dominated by diffusion and do not show significant evidence of subsurface advective flow. Deeper interstitial waters are believed to be the in situ fluids that have evolved through interaction with sediments and diffusion. Pore-fluid chemistry is strongly influenced by carbonate recrystallization processes. Increases in pore-fluid Cl- and Na+ with depth are interpreted to result mainly from carbonate remineralization reactions that are most active near the platform margin. A lateral gradient in detrital clay content observed along the transect, leads to an overall lower carbonate reactivity, and enhances preservation of metastable aragonite further away from the platform margin. Later stage burial diagenesis occurs at slow rates and is limited by the supply of reactive elements through diffusion.