Na 1 Nachlass Max Horkheimer, 28 - Korrespondenzen mit u.a. Siegfried Kracauer (p. I 14, 115-368)

95 Briefe und Beilagen zwischen Siegfried Kracauer und Max Horkheimer, 1936-1949; 2 Briefe zwischen Else Staudinger vom American Committee for Refugee Scholars, Writers and Artists New York und Max Horkheimer, 10.07.1945, 24.07.1945; 2 Briefe zwischen Meyer Schapiro und Siegfried Kracauer 19.11.1937, 03.12.1937; 2 Briefe von Leo Löwenthal an Schapiro Meyer, 1940, 1941; 1 Brief und 1 Beilage von Max Horkheimer an A. Schütz, 02.08.1940; 1 Brief von Max Horkheimer an Trude Krautheimer, 30.07.1940; 1 Brief von Max Horkheimer an das Hebrew Sheltering and Immigrant Aid New York, 10.06.1940; 2 Briefe ziwschen dem Department of State Washington und Max Horkheimer, 05.04.1939, 1939; 2 Briefe zwischen Betty Drury Max Horkheimer, 05.11.1938, 07.11.1938; 2 Briefe zwischen Margaret Krafft und Max Horkheimer, 1938, 1939; 1 Brief von Gertrud Kurth-Kieslinger an Max Horkheimer, 02.10.1939; 2 Briefe zwischen Werner Kraft und Max Horkheimer, 19.01.1940, 01.03.1940; 1 Brief und 1 Beilage von Friedrich Krause an Max Horkheimer, 05.01.1939; 2 Briefe zwischen Karl Krayl und Max Horkheimer, 201.10.1937, 25.11.1937; 11 Briefe zwischen Ernst Krenek und Max Horkheimer, 1937-1941; 1 Brief von S. Krezel an Max Horkheimer, 12.02.1936; 1 Brief von Charles I. Krieger an Max Horkheimer, 01.08.1940; 1 Brief von H. Kronstein an Max Horkheimer, 20.05.1935; 3 Briefe zwischen Germaine Krull und Max Horkheimer, 1934, 06.09.1937, 1937; 3 Briefe zwischen Lawrence S. Kubie Sekretär der American Psychoanalytic Association, New York und Max Horkheimer, 11.05.1938, 1938; 5 Briefe und Beilagen zwsichen Julius Kühl und Max Horkheimer, 18.10.1939-1940; 1 Brief von Max Horkheimer an Herr Guggenheim, 20.02.1940; 1 Brief von Julius Kühl an die ESKA, 31.03.1945; 4 Briefe zwischen B. Kugelmann und Max Horkheimer, 1934, 1938, 1939; 1 Brief von Georg Kunzel an Max Horkheimer, 01.08.1930;

Na 50 Nachlass Arthur Schopenhauer - 'Schopenhauer-Archiv', 368 - Bedauern gegnüber N.N. wegen der Nichtteilnahme an einem geplanten Treffen

2 Seiten

Ms.Ff.F.Stoltze 3. 368 - Brief von Friedrich Stoltze an Feodor Körber

Frankfurter Latern, Manuskript

Josep Maria Ruiz Simon, A arte de Raimundo Lúlio e a teoria escolástica da ciência, trad. Fernando Salles, Instituto Brasileiro de Filosofía e Ciência “Raimundo Lúlio" (Ramon Llull), Sâo Paulo, 2004. ISBN: 85 - 89294 - 05 - 6. 368 p.

Fil: Mendoza, José María Felipe.

(Table 2) Chemistry of the organic matter at DSDP Leg 62 Holes

The wide distribution of sapropelic deposits in the sedimentary cover of the oceans, their Cretaceous age, and their possible oil- and gas-generating characteristics allow us to regard these deposits as a regular global stage in the history of oceanic sedimentation. So, Cretaceous sapropelic deposits are a unique object for study. Cretaceous sapropelic deposits of DSDP Sites 463, 465, and 466, as well as similar sediments of the Atlantic and Indian Oceans, are characterized by enrichment in organic matter, which sometimes reaches 33% (Cape Verde Basin, DSDP Sites 367 and 368). The objective of this study is the elucidation of genesis, paleogeographic environment of sedimentation, and oil-generating potential of Cretaceous sapropelic deposits at these sites. Attention is given to petrographic composition and distribution of the organic matter.

(Table 2) Concentration of phytoplankton pigments in Adventfjorden in spring and summer of 1997

The study was carried out from April 30 until July 13 of 1997 in Adventfjorden (Spitsbergen). Formation of a less saline and warmer surface water (~1 m thick) caused by melting of the ice was observed in the fjord during the first days of May. In summer the less saline surface layer was about 3 m thick. Euphotic depth measured under the ice sheet reached 12 m, whereas load of mineral matter brought with riverine discharge in summer (content of total particulate matter in the fjord reached 1.66 kg/m**2) dramatically reduced euphotic zone depth to 0.35 m. By pigment measurement three phases of phytoplankton development in Adventfjorden were distinguished: (1) spring bloom that has started under fast ice and reached maximum in the mid of May, (2) stagnation period in June, (3) increase of pigment concentration in July, what could indicate start of the next algae bloom. Analyses of chlorophylls and carotenoids revealed that diatoms (chl c, fucoxanthin), and green algae (chl b, lutein) dominated phytoplankton community in the fjord. Moreover, presence of peridinin indicates presence of Dinophyta and alloxanthin - occurence of Cryptophyta. In May and June 1997 phytoplankton appeared mainly in the surface of water, while in July, as a result of inflow of turbulent riverine waters into Adventfjorden, algae cells were pushed down and the highest numbers were observed at depth ~20 m. Great phaeopigments to chl a ratio (= 0.54) found in fjord seston in June and July probably shows strong impact of zooplankton grazing on phytoplankton development. High contribution of chlorophyllide a in porphyrin a poll in samples collected under fast ice (chlorophyllide a / chl a ratio = 0.18) reflects the final stage of algal communitie succession in ice, just before spring ice melt and release of biota to oceanic water. Chlorophyllide a content during summer was minor or not detectable, demonstrating that diatom cells were in good physiological condition. High chl a allomer / chl a ratio (average = 0.11 for the period investigated) confirms high oxygen concentration in environment of Adventfjorden.

Elemental and isotope compositions of lipids, kerogens and asphaltenes from samples of DSDP Hole 41-368

The thermal effects of three (one major and two minor) Miocene diabase intrusions on Cretaceous black shales from DSDP site 41-368 have been analyzed. A concentration gradient was observed, especially for the hydrocarbons, decreasing towards the major intrusion and between the three sills. The thermally-altered samples in the proximity of and between the sills contained elemental sulfur and an excess of thermally-derived pristane over phytane. whereas, the unaltered sediments contained no elemental sulfur, and more phytane than pristane. A maximum yield of the extractable hydrocarbons was observed at a depth of 7 m below the major sill. Two classes of molecular markers were present in this bitumen suite. The first was sesqui-, di- and triterpenoids and steranes. which could be correlated with both terrigenous and autochthonous sources. They were geologically mature and showed no significant changes due to the thermal stress. The second class was found in the altered samples, which contained only polynuclear aromatic hydrocarbons with low alkyl substitution and sulfur and oxygen heterocyclic aromatic compounds. These compounds were derived from pyrolytic reactions during the thermal event. Kerogen was isolated from all of these samples, but only traces of humic substances were present. The H/C, N/C, d13C, d34S and dD all exhibit the expected effects of thermal stress. The kerogen becomes more aromatized and richer in 13C, 34S and D in the proximity of and between the sills. Maturation trends were also measured by the vitrinite reflectance and electron spin resonance, where the thermal stress could be correlated with an elevated country rock temperature and an increased degree of aromaticity. The effects of in situ thermal stress on the organic-rich shales resulted in the generation and expulsion of petroliferous material from the vicinity of the sills.

Carolina Barry (2009). Evita capitana : El Partido Peronista Femenino 1949-1955. Editorial Eduntref. 368 páginas

Fil: Rey, Clara Fabiana. Universidad Nacional de La Plata. Facultad de Humanidades y Ciencias de la Educación; Argentina.

Acción Argentina. Un antifascismo nacional en tiempos de guerra mundial, de Andrés Bisso, Buenos Aires, Prometeo Libros, 2005, 368 páginas

Fil: Garguín, Enrique. Universidad Nacional de La Plata. Facultad de Humanidades y Ciencias de la Educación; Argentina.