Na 50 Nachlass Arthur Schopenhauer - 'Schopenhauer-Archiv', 210 - Mitteilung von A. Scheuter über die psychische Krankheit von Pfarrer Grim

u.a.: Heilanstalt in Eltville;

8° Hs 210 - De statu animae

Vorbesitzer: Senckenbergische Bibliothek Frankfurt am Main

Na 1 Nachlass Max Horkheimer, 455 - Korrespondenzen u.a. mit Margo H. Wolff und Karl August Wittfogel (p. V 173, 210-429)

19 Briefe zwischen Lisa Witherell (geb. Richter) und Max Horkheimer, 1963-1971; 2 Briefe zwischen Werner Wittayer (stud. phil.) und Max Horkheimer, 1964; 4 Drucksachen vom Landtagspräsidenten Otto Witte an Max Horkheimer, 1952-1954; 2 Briefe an Otto Witte von Max Horkheimer, 1952-1953; 1 Todesanzeige, 1963; 4 Briefe zwischen der Studentin Ulrike Wittenberg und Max Horkheimer, 1972-1973; 4 Briefe zwischen dem Professor Karl A. Wittfogel und Max Horkheimer, 1972; 3 Briefe zwischen dem Oberstudiendirektor Dr. Kurt Debus und Max Horkheimer, 1967; 3 Briefe zwischen David Wodlinger und Max Horkheimer, 1960; 2 Briefe zwischen Dr. Herman Wohlstein und Max Horkheimer, 1965; 16 Briefe an Johanna Woitschach von Max Horkheimer, 1970-1973 (die Briefe an Max Horkheimer wurden zurückverlangt); 1 Brief von Ernst Wolf an Max Horkheimer, San Francisco, 1954; 3 Briefe zwischen dem Diplom-Psychologen Heinz E. Wolf und Max Horkheimer, 1958; 13 Briefe zwischen dem Oberstudiendirektor Oskar Wolfenstädter und Max Horkheimer, 1968-1969; 4 Briefe zwischen der Ordensschwester Katherine Wolff und Max Horkheimer, 1970-1971; 25 Briefe zwischen Margo H. Wolff und Max Horkheimer, 1962-1973; 11 Briefe zwischen dem Professor Max Wolff und Max Horkheimer, 1960; 3 Briefe zwischen dem Professor Manfred Wolfson und Max Horkheimer, 1971; 6 Briefe von der Physiotherapeutin Helga Wolk an Max Horkheimer, 1970-1971; 13 Briefe zwischen Hedwig G. de Wollenberger und Max Horkheimer, 1966-1970; 1 Brief an den Professor Günther Wollheim von Max Horkheimer, 1965; 4 Briefe zwischen Johanna Wopperer-Ege und Max Horkheimer, 1970; 5 Briefe zwischen Anton Wopperer und Max Horkheimer, 1969-1970; 3 Briefe an die World Future Society von Max Horkheimer, 1969-1973; 2 Briefe zwischen dem World Jewish Congress und Max Horkheimer, 1970; 2 Briefe zwischen dem Professor Theodor Würtenberger und Max Horkheimer, 1964; 3 Briefe zwischen der Würtembergischen Landesbibliothek und Max Horkheimer, 1969; 16 Briefe zwischen Rösle Wüstholz und Max Horkheimer, 1951-1959; 2 Briefe zwischen Christoph Wulf und Max Horkheimer, 1973; 1 Brief an Jssy Wygoda von Max Horkheimer, 1964; 2 Briefe zwischen Dr. Hans von Wyl und Max Horkheimer, 1971; 2 Briefe zwischen Jacques Wyler und Max Horkheimer, 1973; 1 Brief von Gisela Wysocki an Max Horkheimer, o.J. (1973?);

Ms.Ff.F.Stoltze 3. 210 - Brief von Robert Oettel an Friedrich Stoltze

Dank für ein Gedicht in der Frankfurter Latern, Zu seinem Enkel Otto Kienitz

Na 1 Nachlass Max Horkheimer, 599 - Korrespondenzen u.a. mit Friedrich Pollock und Karl August Wittfogel (p. VI 42, 1-210)

Briefwechsel zwischen Max Horkheimer, Frederick Pollock und Karl August und Olga Wittfogel; 1 Brief von Karl August Wittfogel an Stephen Duggan, 02.08.1936; 2 Briefe an Max Horkheimer von Karl August Wittfogel, November 1937; 1 Brief von Karl August Wittfogel an Carter, 16.07.1936; 1 Brief an den American Consul General (Tientein, China) von Max Horkheimer, 03.04.1936; 1 Brief von Max Horkheimer an Owen Lattimore, 28.12.1935;

Ausst. 210 - HIerinen sind begriffen vier bücher von menschlicher Proportion durch Albrechten Dürer von Nürenberg erfunden vnd beschriben zu nutz allen denen so zu diser kunst lieb tragen

Vorbesitzer: Heinrich Anton Cornill-d'Orville (Exlibris im Vorderdeckel)

Ms. lat. oct. 210 - Certificat du Comité de Surveillance Révolutionnaire

Vorbesitzer: O. Borelli

Suite : Prélude, Pavane, Chanson de Louis XIII varié, Gavotte et Musette, Tambourin ; für Pianoforte und Violine ; op. 210

von Joachim Raff

Age model and Nd isotope ratios of DSDO Hole 43-386 and ODP Hole 210-1276A

Modern thermohaline circulation plays a role in latitudinal heat transport and in deep-ocean ventilation, yet ocean circulation may have functioned differently during past periods of extreme warmth, such as the Cretaceous. The Late Cretaceous (100-65 Ma) was an important period in the evolution of the North Atlantic Ocean, characterized by opening ocean gateways, long-term climatic cooling and the cessation of intermittent periods of anoxia (oceanic anoxic events, OAEs). However, how these phenomena relate to deep-water circulation is unclear. We use a proxy for deep-water mass composition (neodymium isotopes; e-Nd) to show that, at North Atlantic ODP Site 1276, deep waters shifted in the early Campanian (~78-83 Ma) from e-Nd values of ~-7 to values of ~-9, consistent with a change in the style of deep-ocean circulation but >10 Myr after a change in bottom water oxygenation conditions. A similar, but more poorly dated, trend exists in e-Nd data from DSDP Site 386. The Campanian e-Nd transition observed in the North Atlantic records is also seen in the South Atlantic and proto-Indian Ocean, implying a widespread and synchronous change in deep-ocean circulation. Although a unique explanation does not exist for the change at present, we favor an interpretation that invokes Late Cretaceous climatic cooling as a driver for the formation of Southern Component Water, which flowed northward from the Southern Ocean and into the North Atlantic and proto-Indian Oceans.

Elisa Moyano (coord.). La literatura de Salta. Espacios de reconocimiento y formas de olvido. Salta, Universidad Nacional de Salta, 2005, 210 p.

Fil: Zapata Viani, María Alejandra.

Isotope composition of dolomite, calcite and pore-waters of ODP Leg 210 samples

Early diagenetic dolomite beds were sampled during the Ocean Drilling Programme (ODP) Leg 201 at four reoccupied ODP Leg 112 sites on the Peru continental margin (Sites 1227/684, 1228/680, 1229/681 and 1230/685) and analysed for petrography, mineralogy, d13C, d18O and 87Sr/86Sr values. The results are compared with the chemistry, and d13C and 87Sr/86Sr values of the associated porewater. Petrographic relationships indicate that dolomite forms as a primary precipitate in porous diatom ooze and siliciclastic sediment and is not replacing the small amounts of precursor carbonate. Dolomite precipitation often pre-dates the formation of framboidal pyrite. Most dolomite layers show 87Sr/86Sr-ratios similar to the composition of Quaternary seawater and do not indicate a contribution from the hypersaline brine, which is present at a greater burial depth. Also, the d13C values of the dolomite are not in equilibrium with the d13C values of the dissolved inorganic carbon in the associated modern porewater. Both petrography and 87Sr/86Sr ratios suggest a shallow depth of dolomite formation in the uppermost sediment (<30 m below the seafloor). A significant depletion in the dissolved Mg and Ca in the porewater constrains the present site of dolomite precipitation, which co-occurs with a sharp increase in alkalinity and microbial cell concentration at the sulphate-methane interface. It has been hypothesized that microbial 'hot-spots', such as the sulphate-methane interface, may act as focused sites of dolomite precipitation. Varying d13C values from -15 per mil to +15 per mil for the dolomite are consistent with precipitation at a dynamic sulphate-methane interface, where d13C of the dissolved inorganic carbon would likewise be variable. A dynamic deep biosphere with upward and downward migration of the sulphate-methane interface can be simulated using a simple numerical diffusion model for sulphate concentration in a sedimentary sequence with variable input of organic matter. Thus, the study of dolomite layers in ancient organic carbon-rich sedimentary sequences can provide a useful window into the palaeo-dynamics of the deep biosphere.

Alejandra Torres Torres, Lectura y sociedad en los sesenta: a propósito de Alfa y Arca : Montevideo, Yauguru, 2012, 210 páginas

Fil: Añón, Valeria. Universidad Nacional de La Plata. Facultad de Humanidades y Ciencias de la Educación; Argentina.