Na 50 Nachlass Arthur Schopenhauer - 'Schopenhauer-Archiv', 318 - Dankesschreiben an Professor Hugo von Meltzl wegen dessen positiven Rezension der Schopenhauer-Biographie sowie Anmerkungen zur Schopenhauer-Rezeption in Deutschland

u.a.: Besprechung der Publikation "Der Kampf ums Unbewusste" von Olga Plümacher 1881; Bedeutung des Oberappellationsgerichtsrates Johann August Becker für Schopenhauer; Apostel und Evangelisten; Schopenhauer Büste von Friedrich Schierholz; Wilhelm Gwinner; Elisabeth von Thüringen;

Ms.Ff.F.Stoltze 3. 318 - Brief von Adolf Stoltze an Marie Stoltze

Beschwerde wegen nicht erhaltener Post, Familienstreitigkeiten

Na 1 Nachlass Max Horkheimer, 592 - Korrespondenzen mit Friedrich (Frederick) Pollock (p. VI 38A, 1-318)

2 Briefe von Frederick Pollock an Leo Löwenthal; 1 Brief von Alice H. Maier an Frederick Pollock, 23.05.1957; 6 Briefe zwischen Frederick Pollock und Emmy Henne; 1 Brief von Frederick Pollock an Lix Weil, 24.12.1957; 1 Brief von Frederick Pollock an Alice H. Maier, 05.12.1957; 4 Briefe von Frederick Pollock an Emmy Henne; 3 Briefe zwischen Frederick Pollock und Leo Löwenthal; 1 Brief von Jos. N. Minissale an Frederick Pollock, 03.07.1957;

Sporomorphs and quantitative analysis of the Eocene record from IODP Hole 318-U1356A

The early Eocene epoch was characterized by extreme global warmth, which in terrestrial settings was characterized by an expansion of near-tropical vegetation belts into the high latitudes. During the middle to late Eocene, global cooling caused the retreat of tropical vegetation to lower latitudes. In high-latitude settings, near-tropical vegetation was replaced by temperate floras. This floral change has recently been traced as far south as Antarctica, where along the Wilkes Land margin paratropical forests thrived during the early Eocene and temperate Nothofagus forests developed during the middle Eocene. Here we provide both qualitative and quantitative palynological data for this floral turnover based on a sporomorph record recovered at Integrated Ocean Drilling Program (IODP) Site U1356 off the Wilkes Land margin. Following the nearest living relative concept and based on a comparison with modern vegetation types, we examine the structure and diversity patterns of the Eocene vegetation along the Wilkes Land margin. Our results indicate that the early Eocene forests along the Wilkes Land margin were characterized by a diverse canopy composed of plants that today occur in tropical settings; their richness pattern was similar to that of present-day forests from New Caledonia. The middle Eocene forests were characterized by a canopy dominated by Nothofagus and exhibited richness patterns similar to modern Nothofagus forests from New Zealand.

Paleomagnetic and rock magnetic properties of IODP Expedition 318 cores

The Integrated Ocean Drilling Program Expedition 318 to the Wilkes Land margin of Antarctica recovered a sedimentary succession ranging in age from lower Eocene to the Holocene. Excellent stratigraphic control is key to understanding the timing of paleoceanographic events through critical climate intervals. Drill sites recovered the lower and middle Eocene, nearly the entire Oligocene, the Miocene from about 17 Ma, the entire Pliocene and much of the Pleistocene. The paleomagnetic properties are generally suitable for magnetostratigraphic interpretation, with well-behaved demagnetization diagrams, uniform distribution of declinations, and a clear separation into two inclination modes. Although the sequences were discontinuously recovered with many gaps due to coring, and there are hiatuses from sedimentary and tectonic processes, the magnetostratigraphic patterns are in general readily interpretable. Our interpretations are integrated with the diatom, radiolarian, calcareous nannofossils and dinoflagellate cyst (dinocyst) biostratigraphy. The magnetostratigraphy significantly improves the resolution of the chronostratigraphy, particularly in intervals with poor biostratigraphic control. However, Southern Ocean records with reliable magnetostratigraphies are notably scarce, and the data reported here provide an opportunity for improved calibration of the biostratigraphic records. In particular, we provide a rare magnetostratigraphic calibration for dinocyst biostratigraphy in the Paleogene and a substantially improved diatom calibration for the Pliocene. This paper presents the stratigraphic framework for future paleoceanographic proxy records which are being developed for the Wilkes Land margin cores. It further provides tight constraints on the duration of regional hiatuses inferred from seismic surveys of the region.