Ms.Ff.F.Stoltze 3. 128 - Brief von Otto Hörth an Friedrich Stoltze

Ziegenhain, Pfarrer Jost, Kassel, Frankfurter Latern, Persönliche Nachrichten

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;

Na 1 Nachlass Max Horkheimer, 371 - Korrespondenzen u.a. mit Franz Neumann (p. V 128, 178-268)

20 Briefe zwischen dem Studenten Iwan Nagel und Max Horkheimer, 1952-1953; 20 Briefe und Beilage zwischen Theodor W. Adorno sowie Max Horkheimer und Iwan Nagel, 1952-1953; Material "Gegen N. aus der NS-Zeit" von Professor Hans Naujoks an Max Horkheimer, 1954; 3 Briefe zwischen dem Professor John U.Nef und Max Horkheimer, 1953; 7 Briefe zwischen der Studentin Dorothee Neff und Max Horkheimer, 1951-1956; 3 Briefe an den Historiker und Sozialwissenschaftler Benjamin Nelson von Max Horkheimer, 1959; 31 Briefe und Beilage zwischen dem Professor Franz L. Neumann und Max Horkheimer, 1950-1954;

Ms. lat. oct. 128 - [Sammelband in 2 Teilen: Konvolut aus Handschrift und Inkunabel]

Vorbesitzer: Antonius Forsch de Meiningen; Adolf von Glauburg; Johann Ernst von Glauburg

Na 1 Nachlass Max Horkheimer, 583 - Korrespondenzen mit Friedrich (Frederick) Pollock (p. VI 35, 128-314)

2 Briefe zwischen Frederick Pollock und der Southern Counties Gas Company of California (Santa Monica), Dezember 1946; 1 Brief von Frederick Pollock an Pacific Electric Railway Co. (West Los Angeles), 16.05.1946;

Hypomnema, Psalmi 128. in quo beatus betaq[ue] coniunx depingitur : In honorem ornatissimi Viri, pietate, iustitia & pruidentia praestantis D. Theobaldi ab Hechsted Hagenoensis ... sponsi. & Sponsae eiusdem, pudicae Virginis Annae Struppiae Gelnhusanae &c Epithalamij loco loco scriptum

a Balthasare Straubio

Ms. lat. qu. 128 - Delle tratte ed estrazioni

Vorbesitzer: Johann Hieronymus Zum Jungen

(Table 1) Nd and Sr isotopic analyses of ODP Leg 127 basalts

Sr and Nd isotopic compositions are reported for basaltic rocks collected during ODP Leg 127 from the Yamato Basin, a rifted backarc basin in the Japan Sea. The basalts are classified into two groups in terms of Nd isotopic composition: the upper sills at Site 797 are characterized by higher 143Nd/144Nd ratios (0.513083-0.513158, epsilon-Nd = 8.68-10.14) and the basalts from Site 794 and the lower sills at Site 797 have lower 143Nd/144Nd ratios (0.512684-0.512862, epsilon-Nd = 0.90-4.37). All of the basalts show higher Sr isotopic compositions than those of the mantle array, which is attributed to seawater alteration. The basalts with lower Nd isotopic values ranging in age from 20.6 to 17.3 Ma have tapped an enriched subcontinental upper mantle (SCUM) with the minor involvement of a depleted asthenospheric mantle (AM). Subsequent change in composition through the physical replacement of SCUM by AM yielded the basalts of the upper sills of higher Nd isotopic compositions. This event within the upper mantle was associated with the breakup of the overlying lithosphere during the rifting of the Japan Sea backarc basin.

Sediment geochemistry of ODP Leg 127 sites

The relative effects of paleoceanographic and paleogeographic variations, sediment lithology, and diagenetic processes on the final preserved chemistry of Japan Sea sediments are evaluated by investigating the rare earth element (REE), major element, and trace element concentrations in 59 squeeze-cake whole-round and 27 physical-property sample residues from Sites 794, 795, and 797, cored during ODP Leg 127. The most important variation in sedimentary chemical composition is the increase in SiO2 concentration through the Pliocene diatomaceous sequences, which dilutes most other major and trace element components by various degrees. This biogenic input is largest at Site 794 (Yamato Basin), moderately developed at Site 797 (Yamato Basin), and of only minor importance at Site 795 (Japan Basin), potentially reflecting basinal contrasts in productivity with the Yamato Basin recording greater biogenic input than the Japan Basin and with the easternmost sequence of Site 794 lying beneath the most productive waters. There are few systematic changes in solid-phase chemistry resulting from the opal-A/opal-CT or opal-CT/quartz silica phase transformations. Most major and trace element concentrations are controlled by the aluminosilicate fraction of the sediment, although the effects of diagenetic silica phases and manganese carbonates are of localized importance. REE total abundances (Sum REE) in the Japan Sea are strongly dependent upon the paleoceanographic position of a given site with respect to terrigenous and biogenic sources. REE concentrations at Site 794 overall correspond well to aluminosilicate chemical indices and are strongly diluted by SiO2 within the upper Miocene-Pliocene diatomaceous sequence. Eu/Eu* values at Site 794 reach a maximum through the diatomaceous interval as well, most likely suggesting an association of Eu/Eu* with the siliceous component, or reflecting slight incorporation of a detrital feldspar phase. SumREE at Site 795 also is affiliated strongly with aluminosilicate phases and yet is diluted only slightly by siliceous input. At Site 797, SumREE is not as clearly associated with the aluminosilicate fraction, is correlated moderately to siliceous input, and may be sporadically influenced by detrital heavy minerals originating from the nearby rifted continental fragment composing the Yamato Rise. Ce/Ce* profiles at all three sites increase essentially monotonically with depth and record progressive diagenetic LREE fractionation. The observed Ce/Ce* increases are not responding to changes in the paleoceanographic oxygenation state of the overlying water, as there is no independent evidence to suggest the proper oceanographic conditions. Ce/Ce* correlates slightly better with depth than with age at the two Yamato Basin sites. The downhole increase in Ce/Ce* at Sites 794 and 797 is a passive response to the diagenetic transfer of LREE (except Ce) from sediment to interstitial water. At Site 795, the overall lack of correlation between Ce/Ce* and Lan/Ybn suggests that other processes mask the diagenetic behavior of all LREEs. First-order calculations of the Ce budget in Japan Sea waters and sediment indicate that ~20% of the excess Ce adsorbed by settling particles is recycled within the water column and that an additional ~38% is recycled at or near the seafloor. Thus, because the remaining excess Ce is only ~10% of the total Ce, there is not a large source of Ce to the deeply buried sediment, further suggesting that the downhole increase in Ce/Ce* is a passive response to diagenetic behavior of the other LREEs. The REE chemistry of Japan Sea sediment therefore predicts successive downhole addition of LREEs to deeply buried interstitial waters.