Ms. hebr. oct. 145 - Ele Toledot Yitsḥak

Vorbesitzer: Mardokai Šemūʾēl Ghirondi ; Abraham Merzbacher

Ms. Barth. 145 - Summa de casibus et matrimonio cum apparatu

Vorbesitzer: Bartholomaeusstift Frankfurt am Main

Ms. Praed. 145 - [Sammelband in 3 Teilen: Konvolut aus Handschrift und Inkunabeln]

Vorbesitzer: Dominikanerkloster Frankfurt am Main;

Na 50 Nachlass Arthur Schopenhauer - 'Schopenhauer-Archiv', 145 - Ankündigung der Veröffentlichung: "Über die Philosophie Arthur Schopenhauers. Ein Sendschreiben an einen Geistlichen"

u.a.: Kritik an den Philosophieprofessor Trendelenburg; Philosophische Ausbildung durch Jean Paul, Friedrich Schleiermacher und Arthur Schopenhauer; Seneca; Dr. Friedrich Ernst Suchsland;

Na 50 Nachlass Arthur Schopenhauer - 'Schopenhauer-Archiv', 882 - Weiterleitung von Adele Schopenhauers eines Briefes von Herrn Arndt sowie eingefügte Mitteilung von Sibylle Mertens-Schaaffhausen der schweren Erkrankung Adele Schopenhauers

u.a. Aufenthalt von Sibylle Mertens-Schaaffhausen in Rom; Weimar;

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, 507 - Korrespondenzen mit Theodor W. Adorno (p. VI 1E, 1 - 145 b)

Briefwechsel zwischen Theodor W. Adorno, Gretel Adorno und Max Horkheimer, 1949-1954; Briefwechsel zwischen Alice Maier uind Max Horkheimer; Briefwechsel zwischen dem Hessischen Minister für Erziehung und Volksbildung und Theodor W. Adorno sowie Max Horkheimer; 1 Brief zwischen Alice Maier und Leo Löwenthal; 1 Brief zwischen Melvin J. Lasky und Theodor W. Adorno, 14.01.1950;

Ms.Ff.F.Stoltze 3. 145 - Brief von E. Huhn an Georg Zimmermann

Maria Stoltze: Gesuch an den Großherzog wegen Stoltzes Pressprozess

Bericht über die bis 145. April d. J. in der Anstalt eingegangenen Meldungen der Auskunftsstellen für Pflanzenschutz und deren Vertrauensmänner

Hiltner

Ouverture zu Demetrius von Schiller : für großes Orchester ; op. 145

componirt von Ferdinand Hiller

Fragm. lat. I 73 - Psalterium (Umfangreiche Textabschnitte aus Ps 16 - 145; Cantica Veteris et Novi Testamenti)

Trägerbände: Inc. qu. 664; Inc. oct. 212; Inc. oct. 321; Inc. oct. 366; Inc. oct. 429; Vorbesitzer: Dominikanerkloster Frankfurt am Main

Na 1 Nachlass Max Horkheimer, 677 - Forschungsprojekte über Antisemitismus, Vorurteil, Autorität: Einzeluntersuchungen (p. IX 144-IX 145)

Excerpts of Radio Talks by G. Allison Phelps, Radio Station KMTR; Institute of Social Research: An American Disciple of Adolf Hitler. A Study of the Nazi Propaganda Methods Used by Joseph E. McWilliams of the American Destiny Party in 1940 Election Campaign;

(Table 1) Carbohydrates, free sugars, and acid-extractable sugar at DSDP Leg 64 Holes

We analyzed 10 core samples of Pleistocene and Pliocene sediment for residual carbohydrates. All yielded positive results for total carbohydrates and acid-extractable glucose. We also detected galactose, mannose, arabinose, xylose, and traces of ribose and fucose in the Pleistocene samples. In the Pliocene samples we found only rare mannose. Only one Pleistocene sample yielded measurable cellulose and amylose.

Age determination of ODP Hole 145-887

Atmospheric carbon dioxide concentrations were significantly lower during glacial periods than during intervening interglacial periods, but the mechanisms responsible for this difference remain uncertain. Many recent explanations call on greater carbon storage in a poorly ventilated deep ocean during glacial periods (Trancois et al., 1997, doi:10.1038/40073; Toggweiler, 1999, doi:10.1029/1999PA900033; Stephens and Keeling, 2000, doi:10.1038/35004556; Marchitto et al., 2007, doi:10.1126/science.1138679; Sigman and Boyle, 2000, doi:10.1038/35038000), but direct evidence regarding the ventilation and respired carbon content of the glacial deep ocean is sparse and often equivocal (Broecker et al., 2004, doi:10.1126/science.1102293). Here we present sedimentary geochemical records from sites spanning the deep subarctic Pacific that -together with previously published results (Keigwin, 1998, doi:10.1029/98PA00874)- show that a poorly ventilated water mass containing a high concentration of respired carbon dioxide occupied the North Pacific abyss during the Last Glacial Maximum. Despite an inferred increase in deep Southern Ocean ventilation during the first step of the deglaciation (18,000-15,000 years ago) (Marchitto et al., 2007, doi:10.1126/science.1138679; Monnin et al., 2001, doi:10.1126/science.291.5501.112), we find no evidence for improved ventilation in the abyssal subarctic Pacific until a rapid transition ~14,600 years ago: this change was accompanied by an acceleration of export production from the surface waters above but only a small increase in atmospheric carbon dioxide concentration (Monnin et al., 2001, doi:10.1126/science.291.5501.112). We speculate that these changes were mechanistically linked to a roughly coeval increase in deep water formation in the North Atlantic (Robinson et al., 2005, doi:10.1126/science.1114832; Skinner nd Shackleton, 2004, doi:10.1029/2003PA000983; McManus et al., 2004, doi:10.1038/nature02494), which flushed respired carbon dioxide from northern abyssal waters, but also increased the supply of nutrients to the upper ocean, leading to greater carbon dioxide sequestration at mid-depths and stalling the rise of atmospheric carbon dioxide concentrations. Our findings are qualitatively consistent with hypotheses invoking a deglacial flushing of respired carbon dioxide from an isolated, deep ocean reservoir periods (Trancois et al., 1997, doi:10.1038/40073; Toggweiler, 1999, doi:10.1029/1999PA900033; Stephens and Keeling, 2000, doi:10.1038/35004556; Marchitto et al., 2007, doi:10.1126/science.1138679; Sigman and Boyle, 2000, doi:10.1038/35038000; Boyle, 1988, doi:10.1038/331055a0), but suggest that the reservoir may have been released in stages, as vigorous deep water ventilation switched between North Atlantic and Southern Ocean source regions.