Ms. hebr. oct. 143 - Sefer tagin

Vorbesitzer: Eljāqīm Carmoly; Abraham Merzbacher

Ms. Barth. 143 - Margarita Decreti

Vorbesitzer: Bartholomaeusstift Frankfurt am Main

Na 50 Nachlass Arthur Schopenhauer - 'Schopenhauer-Archiv', 865 - Geburtstagsgrüße

abgedruckt in: Schopenhauer-Jahrbuch 30 (1943), S. 211-212

Na 50 Nachlass Arthur Schopenhauer - 'Schopenhauer-Archiv', 143 - Anfrage nach der Qualität der Übersetzung des Oupnek'hat von Thaddäus Anselm Rixner 1808

u.a.: Portrait Schopenhauers von der Hermannschen Buchhandlung; Museum Frankfurt; 2. Auflage der Parerga und Paralipomena, Preisschrift Leipziger Fakultät; Immanuel Kant; Friedrich Schleiermacher; Thaddaeus Anselm Rixner;

Ms. Praed. 143 - Manipulus florum

Vorbesitzer: Dominikanerkloster Frankfurt am Main

Ms.Ff.F.Stoltze 3. 143 - Brief von Karl Holthof an Friedrich Stoltze

Demokratischer Verein

Na 1 Nachlass Max Horkheimer, 675 - Forschungsprojekte über Antisemitismus, Vorurteil, Autorität: Einzeluntersuchungen (p. IX 143)

Institut of Social Research: "Studies in Antisemitism. Volume II: III. American Antisemitic Agitators"; enthält: Studien über Martin Luther Thomas, Georg Allison Phelps und 'Conversations with Antisemitis'; Typoskript, gebunden, 436 Blatt;

Ms. lat. oct. 143 - Theologische Sammelhandschrift

Die Foliierung geht nur bis Bl. 276; zusätzlich gibt es das Blatt 120a.

Geochemical parameters of sediments and water of the Black Sea, data of Cruise 8 of R/V Vityaz-2

The book presents results of comprehensive geological investigations carried out during Cruise 8 of R/V "Vityaz-2" to the western part of the Black Sea in 1984. Systematic studies in the Black Sea during about hundred years have not weakened interest in the sea. Lithological and geochemical studies of sediments in estuarine areas of the Danube and the Kyzyl-Irmak rivers, as well as in adjacent parts of the deep sea and some other areas were the main aims of the cruise. Data on morphological structures of river fans, lithologic and chemical compositions of sediments in the fans and their areal distribution, forms of occurrence of chemical elements, role of organic matter and gases in sedimentation and diagenesis are given and discussed in the book.

(Table 1) Boron-isotope measurements of shallow-dwelling planktonic foraminifera of ODP Holes 144-817A, 144-872C and 143-865C

Knowledge of the evolution of atmospheric carbon dioxide concentrations throughout the Earth's history is important for a reconstruction of the links between climate and radiative forcing of the Earth's surface temperatures. Although atmospheric carbon dioxide concentrations in the early Cenozoic era (about 60 Myr ago) are widely believed to have been higher than at present, there is disagreement regarding the exact carbon dioxide levels, the timing of the decline and the mechanisms that are most important for the control of CO2 concentrations over geological timescales. Here we use the boron-isotope ratios of ancient planktonic foraminifer shells to estimate the pH of surface-layer sea water throughout the past 60 million years, which can be used to reconstruct atmospheric CO2 concentrations. We estimate CO2 concentrations of more than 2,000 p.p.m. for the late Palaeocene and earliest Eocene periods (from about 60 to 52 Myr ago), and find an erratic decline between 55 and 40 Myr ago that may have been caused by reduced CO2 outgassing from ocean ridges, volcanoes and metamorphic belts and increased carbon burial. Since the early Miocene (about 24 Myr ago), atmospheric CO2 concentrations appear to have remained below 500 p.p.m. and were more stable than before, although transient intervals of CO2 reduction may have occurred during periods of rapid cooling approximately 15 and 3 Myr ago.