Ms. Praed. 177 - Dominikanergebetbuch

Vorbesitzer: Dominikanerkloster Frankfurt am Main

Ms.Ff.F.Stoltze 3. 177 - Brief von Siegmund Leopold Kohn-Speyer an Friedrich Stoltze

Johann Albrecht Varrentrapp, Sauerländer, Tod Ernst Schalcks

Na 1 Nachlass Max Horkheimer, 370 - Korrespondenzen u.a. mit Ludwig Neundörfer und Oskar Negt (p. V 128, 1-177)

2 Briefe zwischen der Buchhandlung Peter Naacher und Max Horkheimer, 1966-1968; 1 Brief von E. Nabulon an Max Horkheimer, 1971; 13 Briefe und Beilage zwischen dem Dozenten Georg Nádor und Max Horkheimer, 1964-1967; 4 Briefe zwischen Cornelia Nass und Max Horkheimer sowie der Beilage: Vortrag von Val. Giscard d'Estaing über "die neue Gesellschaft" Brüssel 1970, 1970-1972; 6 Briefe zwischen Else Nassauer und Max Horkheimer, 1967-1973; 3 Briefe zwischen S.Andhil Fineberg und Max Horkheimer, 1967-1969; 1 Brief von Dr. med. Horst Naujoks an Max Horkheimer, 1963; 3 Briefe von Max Horkheimer an die Zeitschrift Nebelspalter, 1964-1969; 7 Briefe zwischen Max Horkheimer und Carl Nedelmann, 1964; 2 Briefe und Beilage zwischen Dr. Renate Neef-Cramer und Max Horkheimer, 1972; 3 Briefe zwischen Walter Neef und Max Horkheimer, 1965; 1 Brief an Dr. Oskar Negt von Max Horkheimer, 1964; 9 Briefe zwischen Dr. Günther Nenning und Max Horkheimer, 1962-1972; 4 Briefe zwischen der Neuen Deutschen Biographie und Max Horkheimer, 1969-1970; 4 Briefe und Beilage zwischen der Wochenschrift Neue Politik und Max Horkheimer, 1971; 6 Briefe zwischen Joachim Günther und Max Horkheimer, 1969-1970; 10 Briefe zwischen der Neuen Rundschau Rudolf Hartung und Max Horkheimer, 1964-1968; 1 Brief an Heinz Friedrich von Max Horkheimer, 1969; 9 Briefe zwischen Dr. Günther Nenning und Max Horkheimer, 1969-1972; 4 Briefe zwischen dem Rektor Günther Neuhardt und Max Horkheimer, 1970; 7 Briefe zwischen Rexa Neumeister und Max Horkheimer, 1967; 28 Briefe und Beilage zwischen dem Professor Ludwig Neundörfer und Max Horkheimer, 1955-1971; 1 Brief an den Professor John J. Neunaier von Max Horkheimer, 1965; 2 Briefe zwischen der Newton Compton Editori und Max Horkheimer, 1970; 3 Briefe zwischen der New York Times und Max Horkheimer, 1959-1960; 4 Briefe und Beilage zwischen Stephen Ney und Max Horkheimer, 1967; 4 Briefe und Beilage zwischen dem Student Claus Niederberger und Max Horkheimer, 1973; 1 Brief an Dr. Friedrich Niewöhner von Max Horkheimer, 1973; 4 Briefe zwischen dem Professor August Nietschke und Max Horkheimer, 1965; 1 Dankesbrief von N.N. an Maidon Horkheimer, 1963; 1 Brief [Hinweis auf eine Krebstherapie] von N.N. an Max Horkheimer; 1 Brief [gegen den Kommunismus] von N.N. an Max Horkheimer, 1955; 1 Brief [Ansichtskarte, Unterzeichnet mit D.C.] von N.N. an Max Horkheimer, 1953; 1 Telegramm [Mitteilung über Schiffverbindung] von N.N. an Max Horkheimer, 1949; 3 Briefe und Beilage zwischen dem Northern Life Insurance Co. Seattle, Wash. und Max Horkheimer, 1951-1953; 4 Briefe und Beilage zwischen den Nürnberger Nachrichten und Max Horkheimer sowie einem Interview mit Max Horkheimer, 1973; 1 Brief von der Nymphenburger Verlagshandlung an Max Horkheimer, 1968;

Ms. lat. oct. 177 - Sammelhandschrift des Frankfurter Pfarrers Bernhard Waldschmidt

Vorbesitzer: Bernhard Waldschmidt

Plio-Pleistocene diatom biostratigraphy from ODP Leg 177, Atlantic sector of the Southern Ocean

Seven sites were drilled during Ocean Drilling Program Leg 177 in the Atlantic sector of the Southern Ocean (SO) on a transect over the Antarctic Circumpolar Current from the Subantarctic to the Antarctic Zone. At four sites sediments were recovered with a Pliocene/Pleistocene sediment package of up to 580 m allowing the refinement of previous diatom zonation concepts. Samples were analyzed on stratigraphic distribution and abundance of diatom species. A refined diatom biozonation tied to the geomagnetic polarity record is proposed. For the middle and late Pleistocene two zonations applicable to the northern and southern area of the SO were constructed, considering different latitudinal distributions of biostratigraphic diatom marker species. The southern zonation for the Pleistocene relies on the occurrence of species of the genus Rouxia, R. leventerae and R. constricta n. sp. as well as on a revised last occurrence datum (LOD) of Actinocyclus ingens (0.38 Ma, late marine isotope stage (MIS) 11). The use of these new stratigraphic marker species refines the temporal resolution for biostratigraphic age assignment to up to 0.1 Myr. In particular the LOD of R. leventerae as an indicator for the MIS 6/5 boundary (Termination II) will improve future dating of carbonate-free Antarctic sediments. These new data were obtained from sediments of Sites 1093 and 1094 (Antarctic Zone). The northern zonation for the middle and late Pleistocene time interval is based on the Pleistocene abundance pattern of Hemidiscus karstenii which was already proposed by previous investigations (e.g. Gersonde and Barcena, 1998). One new species (R. constricta) and two new combinations (Fragilariopsis clementia, Fragilariopsis reinholdii) are proposed in this study.

Stable isotope record of benthic and planktonic foraminifera in sediment cores of ODP Leg 177, Southern Ocean

While onboard ship during Leg 177, we used variations in sediment physical properties (mainly percent color reflectance) in conjunction with biomagnetostratigraphy to correlate among sites and predict the position of marine isotope stages (MISs) (e.g., see fig. F11 in Shipboard Scientific Party, 1999, p. 45). Our working assumption was that physical properties of Leg 177 sediments are controlled mainly by variations in carbonate content. Previous studies of Southern Ocean sediment cores have shown that carbonate concentrations are relatively high during interglacial stages and low during glacial stages at sites located within the Polar Frontal Zone (PFZ). Today, the PFZ marks a lithologic boundary in underlying sediment separating calcareous oozes to the north and silica-rich facies to the south (Hays et al., 1976). Although there is debate whether the position of the "physical" PFZ actually moved during glacial-interglacial cycles (Charles and Fairbanks, 1990; Matsumoto et al., 2001), the "biochemical" PFZ, as expressed by the CaCO3/opal boundary in sediments, certainly migrated north during glacials and south during interglacials. This gave rise to lithologic variations that are useful for stratigraphic correlation. At Leg 177 sites located north of the PFZ and at sublysoclinal depths, we expected the same pattern of carbonate variation because cores in the Atlantic basin are marked by increased carbonate dissolution during glacial periods and increased preservation during interglacials (Crowley, 1985).

Late Miocene-early Pliocene stable isotope record of benthic foraminifera from ODP Site 177-1088 in the sub-Antarctic South Atlantic

Benthic foraminiferal stable isotope records for the past 11 Myr from a recently drilled site in the sub-Antarctic South Atlantic (Site 1088, Ocean Drilling Program Leg 177, 41°S, 15°E, 2082 m water depth) provide, for the first time, a continuous long-term perspective on deep water distribution patterns and Southern Ocean climate change from the late Miocene through the early Pliocene. I have compiled published late Miocene through Pliocene stable isotope records to place the new South Atlantic record in a global framework. Carbon isotope gradients between the North Atlantic, South Atlantic, and Pacific indicate that a nutrient-depleted watermass, probably of North Atlantic origin, reached the sub-Antarctic South Atlantic after 6.6 Ma. By 6.0 Ma the relative proportion of the northern-provenance watermass was similar to today and by the early Pliocene it had increased to greater than the modern proportion suggesting that thermohaline overturn in the Atlantic was relatively strong prior to the early Pliocene interval of inferred climatic warmth. Site 1088 oxygen isotope values display a two-step increase between ~7.4 Ma and 6.9 Ma, a trend that parallels a published delta18O record of a site on the Atlantic coast of Morocco. This is perhaps best explained by a gradual cooling of watermasses that were sinking in the Southern Ocean. I speculate that relatively strong thermohaline overturn at rates comparable to the present day interglacial interval during the latest Miocene may have provided the initial conditions for early Pliocene climatic warmth. The impact of an emerging Central American Seaway on Atlantic-Pacific Ocean upper water exchange may have been felt in the North Atlantic beginning in the latest Miocene between 6.6 and 6.0 Ma, which would be ~1.5 Myr earlier than previously thought.