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: Karl Dietrich Adam/Ludwigsburg; Jens Klein–Dieter Becker-Platen/Hannover; Gerhard W. Brmmer/ Bonn; Walter Carl (+)/Stuttgart; Claus Duphorn * Kiel; Peter von Egan-Krger/Heidelberg; Hans Ehrenberg/Mainz; Heinrich Karl Erben/Bonn; Helmut W. Flgel/Graz; Klaus Gallwitz/Karlsruhe; Helmut Haunschild/Mnchen; Hans-Georg Herbig/Kln; Heinrich Hiltermann/Bad Laer; Helmut Hlder/Stuttgart; Andreas Hoppe/Wiesbaden; Gnter Hoppe/Berlin; Rolf Kohring/Berlin; Karl Otto Kopp/Mnchen; Wolfhart Langer/Bonn; Gaston Mayer/Karlsruhe; Georg Matthess/ Kiel; Gert Michel/Krefeld; Ursula Patzke * Ahrensburg; Fritz A. Pfaffl/Zwiesel; Werner Prange/ Kiel; Ilse Rabien/Hochheim; Ernst Reiner/Gummersbach; Siegfried Ritzkowski/Gttingen; Peter Rothe/Mannheim (Nachlassteile Ludwig und Pauline Rger und Nachlass Ilse Plewe); Wolfgang Schirmer/ Dsseldorf; Horst Schneider/Freiburg; Erich Schroeder * Berlin; Max Schwab/Halle (Nachlass Rudolf Hohl); Eberhard Sittig * Rheinstetten; Walter Steiner/Weimar; Alexander Tollmann/Wien; Rudolf Trmpy/Ksnacht; Ida Valeton * Braunschweig; Freek R. van Veen/Delft; Ehrhard Voigt/Hamburg; Helmut Weiler/Mainz; Gerd Wiesemann/Isernhagen; Eugen Wirth/Erlangen; Zobel Barbara/Hannover. Da schon Missverstndnisse vorgekommen sind, sei darauf hingewiesen, dass es sich bei dem im Nachrichtenblatt der Deutschen Geologischen Gesellschaft (59, 4, Quartal 1996, S. 30) erwhnten “Geologenarchiv” um das Freiburger Archiv handelt.

Ohne Zusammenfassung:

Abstract: GLACIATION AND SEALEVEL — EARLY RESEARCH: Changes of sealevel positions depend on vertical crustal movements, different distributions of oceanic water masses and variations of ocean water volume. In spite of the fact that C. Maclaren explained the relations between the fluctuations of continental ice masses and ocean water volumes correctly in 1842, only two years after the classical paper of L. Agassiz, it took half a century to reach global agreement on the matter. Some examples of the different ways of research may illustrate the complex treatment of the problem, the fact that correct approaches were forgotten but wrong ideas were discussed for decades and the influence of geological authorities. However, some problems remain open even now, such as the exact dating of Pleistocene and Holocene sealevel fluctuations in different geological settings, or the influence of a changing geoid.