Na 50 Nachlass Arthur Schopenhauer - 'Schopenhauer-Archiv', 583 - Übersendung eines Kontoauszuges

u.a.: Bankgeschäfte; Mexikanische Anleihe; Goll & Söhne;

Na 50 Nachlass Arthur Schopenhauer - 'Schopenhauer-Archiv', 257 - Mitteilung über Schwierigkeiten mit den Bankgeschäften

u.a.: Kredit von Goll & Söhne; Schöneberger Zinsen;

Na 50 Nachlass Arthur Schopenhauer - 'Schopenhauer-Archiv', 259 - Mitteilung über eine zugemessene Provision

u.a.: Schöneberger Quittungen;

Na 50 Nachlass Arthur Schopenhauer - 'Schopenhauer-Archiv', 21 - Konzeptschreiben an das Londoner Bankhaus John Louis Lemmé & Co anlässlich eines geplanten Wechsels (Conversion) von Mexikanischen Papieren ins englische Pfund

u.a.: Lizardi, Bansa;

Zusammenstellung der Moose und Flechten des Kaiserstuhles

Von Pfarrer Goll

Die Flechten des Kaiserstuhles

Goll

Botanische Streifzüge um Schiltach

Von Pfarrer Goll

Botanische Streifzüge um Schiltach

Pfr. Goll

Flechten um Schramberg

Von Pfr. Goll

Flechten um Schramberg

Von Pfr. Goll

Enhancing Yield and Biological Nitrogen Fixation of Common Beans

Two studies were conducted at the ISU Horticulture Station to evaluate potential limitations on yield and atmospheric nitrogen fixation by common bean (Phaseolus vulgaris L.). This legume is a food staple for small landholder farm families worldwide. But it has a limited capacity for nitrogen fixation and often yields only a fraction of its genetic potential. In these studies, we examined the dependence of pod filling on current assimilate supply, as well as the potential to improve nitrogen fixation using an inoculant shown to enhance biological nitrogen fixation under stressful conditions.

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.