Psalm 137

E. Simonson

Psalm 137 : (aus "Ost und West")

E. Simonson

Juda's Klage : frei nach dem 137. Psalm

A. Levy

Ms. Barth. 137 - Theologische Sammelhandschrift

Vorbesitzer: Bartholomaeusstift Frankfurt am Main

Ms. Praed. 137 - [Sammelband in 5 Teilen: Konvolut aus Handschrift, Inkunabel und Postinkunabeln]

Vorbesitzer: Dominikanerkloster Frankfurt am Main

Na 1 Nachlass Max Horkheimer, 333 - Korrespondenzen u.a. mit Siegfried Kracauer (p. V 105, 137-208)

57 Briefe und Beilage zwischen Kreuz-Verlag und Max Horkheimer, 1965-1973, sowie Manuskripte von 2 Rundfunksendungen:; a) Ansgar Skriver: Israel im Frühjahr, 1965; b) Reimar Lenz: Zersetzung, Diagnose eines epidemischen Begriffs, 1965; 17 Briefe und Beilage zwischen Professor Gerhard [u. Erna] Krüger und Max Horkheimer, 1952-1955;

Na 50 Nachlass Arthur Schopenhauer - 'Schopenhauer-Archiv', 137 - Übersendung von philosophischen Reimen

u.a.: Wille, Immanuel Kant; Aphorismen zur Lebensweisheit; Parerga und Paralipomena; Vorschlag zur Publikation gegen französische Kritiker; Immanuel Kant;

Ms.Ff.F.Stoltze 3. 137 - Brief von Otto Hörth an Lyda Stoltze

Stoltze

Ms. lat. oct. 137 - Epistula ad Eberhardum de Ippelbrunn decanum Moguntinum

Vorbesitzer: Dominikanerkloster Frankfurt am Main

Inc. qu. 504 (Ausst. 137) - Wahl Maximilians zum Römischen König zu Frankfurt a. M. am 16.II.1486

Vorbesitzer: Stadtarchiv Frankfurt am Main

Major and trace element concentrations of sediments from the IODP Exp302 sites

We analyzed a suite of sediment samples recovered in the central Arctic Ocean for major, trace, and rare earth elements in order to assess changes in terrigenous source material throughout the Cenozoic. The terrigenous component consists of two end-members. Input from a shale-like composition dominates bulk sediments, especially those deposited during the Paleocene and since the Miocene, and may represent sediment supply from the eastern Laptev Sea. Therefore, even though the environment and transport mechanisms may have varied from ice free to ice dominated, sequences of the early Paleogene and later Neogene appear to have been influenced by a single major terrigenous source. This suggests similar transport capabilities and trajectories for both ocean and drift currents through significant parts of the Cenozoic. Influence from a more mafic source appears to be more important through the early Eocene to the middle Miocene and most likely represents material from the western Laptev Sea or Kara Sea. Thus, Eocene major changes in surface water productivity appear broadly synchronous with those in terrigenous provenance. A combination of regional sea level variations, local shelf processes, and transport mechanisms are among the more probable causes for the observed source changes. Although the assignment of sources using chemistry presently is constrained by a lack of data from certain regions (e.g., eastern Siberian Sea) our results generally agree with inferences based on mineralogy or radiogenic isotopes and shed further light on long-term reconstructions of the central Arctic Ocean.