Ms. hebr. oct. 138 - Shevaʻ masekhtot ḳeṭanot Yerushalmiyot

Vorbesitzer: Abraham Merzbacher

Ms. lat. qu. 138 - Recueil des anciennes relations diplomatiques entre la Russie et la Prusse (gewidmet Friedrich Wilhelm III. von Preußen)

Akzessionsnummer: 37 G/76

Ms. Barth. 138 - Theologische Sammelhandschrift

Vorbesitzer: Heinrich Degen zum Burggrafen; Johann Ugelnheimer; Bartholomaeusstift Frankfurt am Main

Na 1 Nachlass Max Horkheimer, 260 - Korrespondenzen u.a. mit dem Direktor der Stadt- und Unibibliothek Frankfurt am Main Professor Clemens Köttelwesch (p. V 66, 138-320)

2 Briefe zwischen F. Champion Ward und Max Horkheimer, 1967; 1 Brief von Max Horkheimer an John Slawson, 1962; 21 Briefe zwischen dem Direktor der Stadt- und Unibibliothek Frankfurt am Main Professor Clemens Köttelwesch und Max Horkheimer, 1956-; 1 Brief an Hertha Dembitzer, 1974; 1 Brief von Hertha Dembitzer, 1974; Schenkungsbrief 1956; Hertha Dembitzer: 2 Briefe zwischen Hertha Dembitzer und Clemens Köttelwesch, 1974;

Na 50 Nachlass Arthur Schopenhauer - 'Schopenhauer-Archiv', 138 - Dankesschreiben anlässlich der Übersendung der "Welt als Wille und Vorstellung" im Jahre 1854 sowie der Parerga und Paralipomena

u.a.: Die Welt als Wille und Vorstellung; Schopenhauer als Reformator der Philosophie; Theismus; Unterschied zwischen Tiere und Pflanzen; Naturwissenschaften; Dr. Friedrich Ernst Suchsland; Professor Pomtov;

Ms. Praed. 138 - Theologische Sammelhandschrift

Vorbesitzer: Dominikanerkloster Frankfurt am Main;

Salix pentandra - alba mas Ritchl. (confer: Salices europaeae von F. Wimmer 138)

Von Dr. Schatz

Ms.Ff.F.Stoltze 3. 138 - Brief von Otto Hörth an Lyda Stoltze

Geschichte der Frankfurter Latern

Na 1 Nachlass Max Horkheimer, 672 - Forschungsprojekte über Antisemitismus, Vorurteil, Autorität: Einzeluntersuchungen (p. IX 136a-IX 138)

Gumperz, Julian: Resumé zu "Autorität und Familie", Entwurf, 1937?; a) Typoskript, 6 Blatt; b) Typoskript mit handschriftlichen Korrekturen, 6 Blatt; "Untersuchung über die Autoritätseinstellung von Studentinnen eines New Yorker Colleges", März 1937. Typoskript, 2 Blatt; Langerhans, Heint (?): "Verhalten der deutschen Bevölkerung gegenüber dem Antisemitischen-Programm der Nazi-Regierung"; Nicht vor 1942. Typoskript mit handschriftlichen Korrekturen, 104 Blatt [unzutreffender Autorenvermerk von Friedrich Pollock: H. Marcuse?]; Dupont, Grete: "Conversations with Antisemits", Gesprächsprotokolle und zusammenfassender Bericht, Mai-Oktober 1943, Typoskript, 87 Blatt; siehe auch IX 143;

Benthic foraminiferal stable isotope record from ODP Site 138-849 on the East Pacific Rise

Benthic foraminifer and delta13C data from Site 849, on the west flank of the East Pacific Rise (0°11 'N, 110°31'W; 3851 m), give relatively continuous records of deep Pacific Ocean stable isotope variations between 0 and 5 Ma. The mean sample spacing is 4 k.y. Most analyses are from Cibicides wuellerstorfi, but isotopic offsets relative to Uvigerina peregrina appear roughly constant. Because of its location west of the East Pacific Rise, Site 849 yields a suitable record of mean Pacific Ocean delta13C, which approximates a global oceanic signal. The ~100-k.y.-period climate cycle, which is prevalent in delta18O does not dominate the long-term delta13C record. For delta13C, variations in the ~400- and 41-k.y. periods are more important. Phase lags of delta13C relative to ice volume in the 41- and 23-k.y. bands are consistent with delta13C as a measure of organic biomass. A model-calculated exponential response time of 1-2 k.y. is appropriate for carbon stored in soils and shallow sediments responding to glacial-interglacial climate change. Oceanic delta13C leads ice volume slightly in the 100-k.y. band, and this suggests another process such as changes in continental weathering to modulate mean river delta13C at long periods. The delta13C record from Site 849 diverges from that of Site 677 in the Panama Basin mostly because of decay of 13C-depleted organic carbon in the relatively isolated Panama Basin. North Atlantic to Pacific delta13C differences calculated using published data from Sites 607 and 849 reveal variations in Pliocene deep water within the range of those of the late Quaternary. Maximum delta13C contrast between these sites, which presumably reflects maximum influx of high-delta13C northern source water into the deep North Atlantic Ocean, occurred between 1.3 and 2.1 Ma, well after the initiation of Northern Hemisphere glaciation. Export of high-delta13C North Atlantic Deep Water from the Atlantic to the circumpolar Antarctic, as recorded by published delta13C data from Subantarctic Site 704, appears unrelated to the North Atlantic-Pacific delta13C contrast. To account for this observation, we suggest that deep-water formation in the North Atlantic reflects northern source characteristics, whereas export of this water into the circumpolar Antarctic reflects Southern Hemisphere wind forcing. Neither process appears directly linked to ice-volume variations.