Ms.Ff.F.Stoltze 3. 364 - Brief von Friedrich Stoltze an Feodor Körber

Frankfurter Latern: Probenummer, Korrektur, Revision, Satzanweisungen, "Frankfurter Nikelose-Zeitung"

Na 1 Nachlass Max Horkheimer, 632 - Aufsätze für die "Zeitschrift für Sozialforschung" (p. IX 4-IX 6)

"Zum Rationalismusstreit in der gegenwärtigen Philosophie" (GS 3, S.163-220), veröffentlicht in: Zeitschrift für Sozialforschung III, 1934, S. 1-53, a) Teilstück, Typoskript mit handschriftlichen Korrekturen, 16 Blatt, b) englische Fassung mit dem Titel "Rationalism and Irrationalism in Recent German Philosophy", Typoskript mit eigenhändigen Korrekturen, 75 Blatt; "Zum Problem der Wahrheit" (GS 3, S.277 - 325), veröffentlicht in: Zeitschrift für Sozialforschung IV, 1935, S. 321-364, englische Fassung mit dem Titel "The Problem of Truth", 45 Blatt; "Egoismus und Freiheitsbewegung" (GS 4, S.9-88), veröffentlicht in: Zeitschrift für Sozialforschung V, 1936, S.161-234, englische Fassung mit dem Titel "Egoism and the Struggle for Freedom", a) Typoskript mit handschriftlichen Korrekturen, 91 Blatt, b) Typoskript mit handschriftlichen Korrekturen, 77 Blatt;

Na 1 Nachlass Max Horkheimer, 655 - Vorträge über Antisemitismus (p. IX 40.1-2-IX 48.1-2)

"Summer institute on Modern European Culture" (1947?); 1. Ankündigung für eine Vorlesungsreihe von Max Horkheimer, Theodor W. Adorno, Leo Löwenthal, Herbert Marcuse, Friedrich Pollock. a) Typoskript mit eigenhändigen Ergänzungen, 20 Blatt b) Typoskript mit handschriftlichen Ergänzungen, 19 Blatt; 2. Herbert Marcuse: "Philosophie allemande et francaise 1871-1933". Typoskript mit eigenhändigen Korrekturen, 18 Blatt; "Tentative Program for the Course of Antisemitism". Vorlesungsankündigung 1948 von Max Horkheimer, Theodor W. Adorno, Friedrich Pollock. Typoskript 2 Blatt; Max Horkheimer: Bericht über die Antisemitismus-Forschungen des Instituts für Sozialforschung (GS 12, S. 165-171). Vortrag gehalten am 16.4.1943, englischer Text. a) Typoskript mit eigenhändigen Korrekturen, 5 Blatt b) Typoskript mit eigenhändigen Korrekturen, 8 Blatt c) Typoskript mit handschriftlichen Korrekturen, 8 Blatt; Max Horkheimer: Bericht über die Antisemitismus-Forschungen des Instituts für Sozialforschung (GS 12, S. 172-183). Vortrag gehalten am 30.4.1943, Temple Israel. a) Typoskript mit eigenhändigen Korrekturen und Ergänzungen, 12 Blatt b) Typoskript mit handschriftlichen Korrekturen, 11 Blatt c) Typoskript mit eigenhändigen Korrekturen, 14 Blatt; Max Horkheimer: Über die Psychologie des Judentums und des Antisemitismus; 1. Vortrag, gehalten am 7.10.1943 im Department of Psychology, UCLA, eigenhändige Notizen, 1 Blatt; 2. Auszüge aus Schriften und Arbeitspapieren von: G.M. Davidson, Salomon Andhil Fineberg, A.R.L. Gurland, Oscar I. Janomsky, Paul W. Massing, Typoskript mit eigenhändigen Ergänzungen, 8 Blatt; Max Horkheimer: Anti-Semitism as a Social Phenomenon (GS 5, S.364-372); 1. Vortrag, gehalten am 17.6.1944 in San Francisco, Psychoanalytic Society, veröffentlicht unter dem Titel 'Sociological Background of the Psychoanalytic Approach". In: Ernst Simmel (ed.), "Anti-Semitism. A Social Disease", New York, 1946, S.1-10. a) Typoskript, 13 Blatt, b) Teilstück, Typoskript, 1 Blatt, c) Teilstück, Typoskript mit eigenhändigen Korrekturen, 2 Blatt d) Typoskript mit handschriftlichen Korrekturen, 9 Blatt; 2. "Notes to the Speech in San Francisco", Notizen, 4 Blatt; 3. eigenhändige Notizen zum Vortrag, 5 Blatt; 4. Rede für Maurice Karpf, Typoskript mit eigenhändigen Korrekturen, 2 Blatt; 5. Theodor W. Adorno: "Mammoth Motives", Notizen zum Verhältnis von Soziologie und Psychologie des Antisemitismus, 3 Blatt; 6. Theodor W. Adorno: "Patterns of Anti-Democratic Propaganda", veröffentlicht in: Ernst Simmel, "Anti-Semitism. A Social Disease", New York, 1946, S.125-137. a) Typoskript, 15 Blatt, b) Typoskript, 14 Blatt;; 7. Einladung, Drucksache, 2 Blatt; 8. Max Horkheimer: 2 Brief an Donald MacFerlane, Pacific Palisades, 22.5.1944, 1 Blatt; Max Horkheimer: Vorträge 1944-45; 1. "Report for the N.C.R.A.C.". Über Forschungsprojekte des American Jewish Committee and des American Jewish Congress, vorgetragen am 14.1.1944, Typoskript, 4 Blatt; 2. Notizen zu 1: Über Kurt Lewin, Typoskript, 3 Blatt; 3. eigenhändige Notizen zu 1., 3 Blatt; 4. Über die europäische Tradition der Arbeiten des Instituts für Sozialforschung. Vortrag, gehalten am 8.12.1944. Eigenhändige Notizen, 1 Blatt; 5. Über psychologische Aspekte der Antisemitismusforschung des Instituts für Sozialforschung. Vortrag, gehalten am 19.4.1945. Eigenhändige Notizen, 2 Blatt; 6. Über sozioökonomische Aspekte des Antisemitismus in Europa und in der Arbeiterschaft der USA. Vortrag, gehalten am 8.6.1945. Psychosomatic Society a) Notizen zum Vortrag, 4 Blatt, b) eigenhändige Notizen, 3 Blatt; 7. Notizen zu 6., Typoskript, 17 Blatt,; 8. Notizen zu 6. "Quotations from Labor Study", Typoskript, 12 Blatt; 9. Über neue Forschungsprojekte des Instituts für Sozialforschung zum Antisemitismus. Vortrag, gehalten am 24.10.1945. Eigenhändige Notizen, 2 Blatt; 10. Über Antisemitismus. Vortrag, gehalten am 3.12.1945. Eigenhändige Notizen, 2 Blatt; 11.-15. Vorträge über Antisemitismus. Datierung unklar (etwa 1945) (u.a. "Mountvernon Speech" und "Breakfast Speech"), 17 Blatt; 16. Über Judentum und Katholizismus in der neueren Geschichte. Eigenhändige Notizen zu einem Vortrag, Datierung unklar, 3 Blatt; 17. Über Vorurteil, Vortrag oder Diskussion in einer Synagoge, Datierung unklar, eigenhändige Notizen, 1 Blatt; Max Horkheimer: Über die Antisemitismus-Forschungen des Instituts für Sozialforschung. Vortrag, gehalten beim U.C.R.A.C.-Meeting, 15.-17.6.1946, Chicago:; 1. eigenhändige Notizen, 13 Blatt; 2. Fragebogen, als Typoskript vervielfältigt, mit eigenhändigen Ergänzungen, 6 Blatt;

Occurrence of hiatuses PH and NH 1 through NH 7 in DSDP holes

Miocene paleoceanographic evolution exhibits major changes resulting from the opening and closing of passages, the subsequent changes in oceanic circulation, and development of major Antarctic glaciation. The consequences and timing of these events can be observed in variations in the distribution of deep-sea hiatuses, sedimentation patterns, and biogeographic distribution of planktic organisms. The opening of the Drake Passage in the latest Oligocene to early Miocene (25-20 Ma) resulted in the establishment of the deep circumpolar current, which led to thermal isolation of Antarctica and increased global cooling. This development was associated with a major turnover in planktic organisms, resulting in the evolution of Neogene assemblages and the eventual extinction of Paleogene assemblages. The erosive patterns of two widespread hiatuses (PH, 23.0-22.5 Ma; and NH 1, 20-18 Ma) indicate that a deep circumequatorial circulation existed at this time, characterized by a broad band of carbonate-ooze deposition. Siliceous sedimentation was restricted to the North Atlantic and a narrow band around Antarctica. A major reorganization in deep-sea sedimentation and hiatus distribution patterns occurred near the early/middle Miocene boundary, apparently resulting from changes in oceanic circulation. Beginning at this time, deep-sea erosion occurred throughout the Caribbean (hiatus NH 2, 16-15 Ma), suggesting disruption of the deep circumequatorial circulation and northward deflection of deep currents, and/or intensification of the Gulf Stream. Sediment distribution patterns changed dramatically with the sudden appearance of siliceous-ooze deposition in the marginal and east equatorial North Pacific by 16.0 to 15.5 Ma, coincident with the decline of siliceous sedimentation in the North Atlantic. This silica switch may have been caused by the introduction of Norwegian Overflow Water into the North Atlantic acting as a barrier to outcropping of silica-rich Antarctic Bottom Water. The main aspects of the present oceanic circulation system and sediment distribution pattern were established by 13.5 to 12.5 Ma (hiatus NH 3), coincident with the establishment of a major East Antarctic ice cap. Antarctic glaciation resulted in a broadening belt of siliceous-ooze deposition around Antarctica, increased siliceous sedimentation in the marginal and east equatorial North Pacific and Indian Oceans, and further northward restriction of siliceous sediments in the North Atlantic. Periodic cool climatic events were accompanied by lower eustatic sea levels and widespread deep-sea erosion at 12 to 11 Ma (NH 4), 10 to 9 Ma (NH 5), 7.5 to 6.2 Ma (NH 6), and 5.2 to 4.7 Ma (NH 7).

Prominent deformation features and interpretation of sediment core CRP-2/2A (Table 1)

Sediment deformation features in CRP-2/2A were described during normal logging procedures and from core-scan images. In this paper the origin of soft-sediment folding, contorted bedding, microfaulting, clastic dykes, shear zones and intraformational breccias is discussed. The features have a stratigraphic distribution related to major unconformities and sequence boundaries. Hypotheses for the origins of sediment deformation include hydrofracturing, subglacial shearing, slumping, and gas hydrate formation. Shear zones, microfaults, clastic dykes and contorted bedding within rapidly deposited sediments, suggest that slumping in an ice-distal environment occurred in the early Oligocene. A till wedge beneath a diamictite at 364 mbsf the mid-Oligocene section represents the oldest evidence of grounded ice in CRP-2/2A. Shear zones with a subglacial origin in the early late Oligocene and early Miocene sections of the core are evidence of further grounding events. The interpretation of sediment deformation in CRP-2/2A is compared to other Antarctic stratigraphic records and global eustatic change between the late Eocenel/early Oligocene and the middle Miocene.

Contiunous surface water uncorrected and quench-corrected active fluorescence and derived chlorophyll a concentration using calibration by HPLC pigments during POLARSTERN cruise ANT-XXV/1

The relationship between phytoplankton assemblages and the associated optical properties of the water body is important for the further development of algorithms for large-scale remote sensing of phytoplankton biomass and the identification of phytoplankton functional types (PFTs), which are often representative for different biogeochemical export scenarios. Optical in-situ measurements aid in the identification of phytoplankton groups with differing pigment compositions and are widely used to validate remote sensing data. In this study we present results from an interdisciplinary cruise aboard the RV Polarstern along a north-to-south transect in the eastern Atlantic Ocean in November 2008. Phytoplankton community composition was identified using a broad set of in-situ measurements. Water samples from the surface and the depth of maximum chlorophyll concentration were analyzed by high performance liquid chromatography (HPLC), flow cytometry, spectrophotometry and microscopy. Simultaneously, the above- and underwater light field was measured by a set of high spectral resolution (hyperspectral) radiometers. An unsupervised cluster algorithm applied to the measured parameters allowed us to define bio-optical provinces, which we compared to ecological provinces proposed elsewhere in the literature. As could be expected, picophytoplankton was responsible for most of the variability of PFTs in the eastern Atlantic Ocean. Our bio-optical clusters agreed well with established provinces and thus can be used to classify areas of similar biogeography. This method has the potential to become an automated approach where satellite data could be used to identify shifting boundaries of established ecological provinces or to track exceptions from the rule to improve our understanding of the biogeochemical cycles in the ocean.

Phycoerythrin concentration during POLARSTERN cruises ANT-XXIV/4, ANT-XXV/1, and ANT-XXVI/4

Phycobiliproteins are a family of water-soluble pigment proteins that play an important role as accessory or antenna pigments and absorb in the green part of the light spectrum poorly used by chlorophyll a. The phycoerythrins (PEs) are one of four types of phycobiliproteins that are generally distinguished based on their absorption properties. As PEs are water soluble, they are generally not captured with conventional pigment analysis. Here we present a statistical model based on in situ measurements of three transatlantic cruises which allows us to derive relative PE concentration from standardized hyperspectral underwater radiance measurements (Lu). The model relies on Empirical Orthogonal Function (EOF) analysis of Lu spectra and, subsequently, a Generalized Linear Model with measured PE concentrations as the response variable and EOF loadings as predictor variables. The method is used to predict relative PE concentrations throughout the water column and to calculate integrated PE estimates based on those profiles.