Die Rechtsstellung der Reichspensionäre : (Artikel 33 (5), 3, 14, 19, 123 (1), 131, 134 Grundgesetz. § 77 des Gesetzes zu Art. 131 GG vom 11.5.51)

George Tzschirner

Ms. Praed. 51 - Moralphilosophische Sammelhandschrift

Vorbesitzer: Georg von Breidenbach; Dominikanerkloster Frankfurt am Main

Na 1 Nachlass Max Horkheimer, 302 - Korrespondenzen u.a. mit Arthur Hübscher (p. V 89, 51-199)

83 Briefe und Beilagen zwischen Arthur Hübscher und Max Horkheimer, 1963-1973; 15 Briefe und Beilagen zwischen Bundesminister a. D. Ewald Bucher und Max Horkheimer, 1966-1971; 1 Brief und Beilage von Dr. Christoph Meyer an Max Horkheimer, 1969; 6 Briefe zwischen Dr. Johann Joeden und Max Horkheimer, 1966; 5 Briefe zwischen dem Oberregierungsrat Gustav Adolf Hünniger und Max Horkheimer, 1951-1953; 2 Briefe und eine Empfehlung und ein Gutachten von Edith Hünniger an Max Horkheimer, 1952-1953;

Na 50 Nachlass Arthur Schopenhauer - 'Schopenhauer-Archiv', 51 - Kritik in Form einer Predigt

u.a.: Auseinandersetzung mit dem Willen; Bibelzitate; Kampf gegen die Amalakiter; Vergleich Schopenhauer mit Josua;

Ms. lat. qu. 51 - Centiloquium de medicis et infirmis

Vorbesitzer: Jakob Heller; Dominikanerkloster Frankfurt am Main

Inc. hebr. 51 - Talmud Bavli : Masekhet Shabat

Vorbesitzer: Abraham Merzbacher;

Na 1 Nachlass Max Horkheimer, 630 - Typoskripte zur Vorlesung "Praktische Philosophie" und zu zwei Referaten (p. VIII 50a.2-VIII 51)

"Praktische Philosophie" (Zur Genealogie der Moral), Vorlesung Sommersemester 1962, Nachschrift (von Hilmar Tillack?): Nachschrift von 20 Vorlesungen 7.5.- 23.7.62, Durchschläge (unvollständig), Typoskript, 135 Blatt; N.N.: "Probleme der Geschichtsphilosophie bei Kant", Referat, Typoskript, 8 Blatt; N.N.: "Geschichtsphilosophie der Südwestdeutschen Schule", Referat, Typoskript mit handschriftlichen Randbemerkungen von Max Horkheimer, 18 Blatt;

Ms.Ff.F.Stoltze 3. 51 - Brief von Ernst Emmerling an Friedrich Stoltze

Stoltze: Notiz in den "Volksblättern", Stuttgart 1866

Ms. lat. oct. 51 - Responsionale secundum usum ecclesiae S. Bartholomaei Francfordensis

Vorbesitzer: Henricus Schurer; Petrus Schmunck; Johann Jakob Hocheisen

Fragm. lat. I 18 - Micrologus (c. 23, 46 - 49, 51 - 61)

Trägerbände: Ms. Barth. 13; Ms. Barth. 18; Ms. Barth. 29; Ms. Barth. 41; Vorbesitzer: Bartholomaeusstift Frankfurt am Main

Age determinations from Bykovsky Peninsula, Siberia

A wide variety of environmental records is necessary for analysing and understanding the complex Late Quaternary dynamics of permafrost-dominated Arctic landscapes. A NE Siberian periglacial key region was studied in detail using sediment records, remote sensing data, and terrain modelling, all incorporated in a geographical information system (GIS). The study area consists of the Bykovsky Peninsula and the adjacent Khorogor Valley in the Kharaulakh Ridge situated a few kilometres southeast of the Lena Delta. In this study a comprehensive cryolithological database containing information from 176 sites was compiled. The information from these sites is based on the review of previously published borehole data, outcrop profiles, surface samples, and our own field data. These archives cover depositional records of three periods: from Pliocene to Early Pleistocene, the Late Pleistocene and the Holocene. The main sediment sequences on the Bykovsky Peninsula consist of up to 50 m thick ice-rich permafrost deposits (Ice Complex) that were accumulated during the Late Pleistocene. They were formed as a result of nival processes around extensive snowfields in the Kharaulakh Ridge, slope processes in these mountains (such as in the Khorogor Valley), and alluvial/proluvial sedimentation in a flat accumulation plain dominated by polygonal tundra in the mountain foreland (Bykovsky Peninsula). During the early to middle Holocene warming, a general landscape transformation occurred from an extensive Late Pleistocene accumulation plain to a strongly thermokarst-dominated relief dissected by numerous depressions. Thermokarst subsidence had an enormous influence on the periglacial hydrological patterns, the sediment deposition, and on the composition and distribution of habitats. Climate deterioration, lake drainage, and talik refreezing occurred during the middle to late Holocene. The investigated region was reached by the post-glacial sea level rise during the middle Holocene, triggering thermo-abrasion of ice-rich coasts and the marine inundation of thermokarst depressions.