Inc. oct. 207 - [Sammelband in 2 Teilen: Konvolut aus Handschrift und Inkunabel]

Vorbesitzer: Dominikanerkloster Frankfurt am Main

Na 1 Nachlass Max Horkheimer, 554 - Korrespondenzen mit Leo Löwenthal (p. VI 22, 207-336)

126 Briefe zwischen Max Horkheimer und Leo Löwenthal, Januar - August 1948; 1 Brief von Max Horkheimer an Herbert Marcuse, 1948; 2 Briefe zwischen Theodor W. Adorno und Leo Löwenthal, 1948; 1 Brief von Leo Löwenthal an Samuel H. Flowerman, 15.06.1948; 3 Briefe zwischen Erich Preiser und Leo Löwenthal, 1948; 1 Brief von Max Horkheimer an Howard Wilson, 28.08.1948; 1 Brief von Paul Lazarsfeld an Leo Löwenthal, 26.08.1948; 1 Brief von Käte Hirsch an Leo Löwenthal, [1948]; 1 Brief von Willy Haas an Max Horkheimer, 15.07.1948; 1 Brief von Max Horkheimer an Moses Finley, 16.08.1948; 1 Brief von Max Horkheimer an Robert J. Havighurst, [August 1948]; 1 Brief (Auszug) von Hans Mayer an Max Horkheimer, 23.03.1948; 1 Brief von Julius Schwietering an Max Horkheimer, 18.02.1948; 1 Brief von E. Stein an Max Horkheimer, 26.06.1948;

Ausst. 207 - Missale se[cundu]m choru[m] [e]t Ritu[m] Eysteten[sis] Ecclesie

Vorbesitzer: Gabriel von Eyb, Bischof von Eichstätt; Kirche von Sappenfeld (Landkreis Eichstätt); Heinrich Anton Cornill-d'Orville (Exlibris im Vorderdeckel);

Ms. lat. oct. 207 - Annotata ad Burkhardi Gotthelfi Struvii Introductionem ad notitiam rei litterariae et usum bibliothecarum

Vorbesitzer: Familie von Holzhausen

Magnetostratigraphy of ODP Leg 207 sediments

Ocean Drilling Program (ODP) Sites 1257-1261 recovered thick sections of Upper Cretaceous-Eocene oceanic sediments on Demerara Rise off the east coast of Surinam and French Guiana, South America. Paleomagnetic and rock magnetic measurements of ~800 minicores established a high-resolution composite magnetostratigraphy spanning most of the Maastrichtian-Eocene. Magnetic behavior during demagnetization varied among lithologies, but thermal demagnetization steps >200°C were generally successful in removing present-day normal polarity overprints and a downward overprint induced during the ODP coring process. Characteristic remanent magnetizations and associated polarity interpretations were generally assigned to directions observed at 200°-400°C, and the associated polarity interpretations were partially based on whether the characteristic direction was aligned or apparently opposite to the low-temperature "north-directed" overprint. Biostratigraphy and polarity patterns constrained assignment of polarity chrons. The composite sections have a complete polarity record of Chrons C18n (middle Eocene)-C34n (Late Cretaceous).

Enrique D. Dussel: La dialéctica hegeliana. Supuestos y superación o del inicio originario del filosofar. Editorial Ser y Tiempo, Mendoza, 1972; 207 páginas

Fil: Prada, Gloria.

Cenomanian/Turonian sea surface temperatures of the equatorial Atlantic reconstructed from geochemical data

Oceanic anoxic event 2 (OAE-2) occurring during the Cenomanian/Turonian (C/T) transition is evident from a globally recognized positive stable carbon isotopic excursion and is thought to represent one of the most extreme carbon cycle perturbations of the last 100 Myr. However, the impact of this major perturbation on and interaction with global climate remains unclear. Here we report new high-resolution records of sea surface temperature (SST) based on TEX86 and d 18O of excellently preserved planktic foraminifera and stable organic carbon isotopes across the C/T transition from black shales located offshore Suriname/French Guiana (Demerara Rise, Ocean Drilling Program Leg 207 Site 1260) and offshore Senegal (Cape Verde Basin, Deep Sea Drilling Project Leg 41 Site 367). At Site 1260, where both SST proxy records can be determined, a good match between conservative SST estimates from TEX86 and d 18O is observed. We find that late Cenomanian SSTs in the equatorial Atlantic Ocean (33°C) were substantially warmer than today (27°-29°C) and that the onset of OAE-2 coincided with a rapid shift to an even warmer (35°-36°C) regime. Within the early stages of the OAE a marked (4°C) cooling to temperatures lower than pre-OAE conditions is observed. However, well before the termination of OAE-2 the warm regime was reestablished and persisted into the Turonian. Our findings corroborate the view that the C/T transition represents the onset of the interval of peak Cretaceous warmth. More importantly, they are consistent with the hypotheses that mid-Cretaceous warmth can be attributed to high levels of atmospheric carbon dioxide (CO2) and that major OAEs were capable of triggering global cooling through the negative feedback effect of organic carbon-burial-led CO2 sequestration. Evidently, however, the factors that gave rise to the observed shift to a warmer climate regime at the onset of OAE-2 were sufficiently powerful that they were only briefly counterbalanced by the high rates of carbon burial attained during even the most extreme interval of organic carbon burial in the last 100 Myr.