Replik an Herrn Professor Heinrich Ewald in Göttingen

Zacharias Frankel

Der Arbeitsplan der "religionsgeschichtlichen Kommission" in Göttingen

Marcus Brann

Köhlerglaube und Wissenschaft : eine Streitschrift gegen Hofrath Rudolph Wagner in Göttingen

von Carl Vogt

Untersuchungen aus dem Botanischen Laboratorium der Universität Göttingen

Hrsg. von J. Reinke

Na 50 Nachlass Arthur Schopenhauer - 'Schopenhauer-Archiv', 1405 - Nachschriften zu Vorlesungen in Göttingen

Bereitgestellt mit freundlicher Unterstützung der Staatsbibliothek zu Berlin - Preußischer Kulturbesitz

Na 50 Nachlass Arthur Schopenhauer - 'Schopenhauer-Archiv', 1406 - Nachschriften zu Vorlesungen in Göttingen

Bereitgestellt mit freundlicher Unterstützung der Staatsbibliothek zu Berlin - Preußischer Kulturbesitz

Na 50 Nachlass Arthur Schopenhauer - 'Schopenhauer-Archiv', 1407 - Nachschriften zu Vorlesungen in Göttingen

Bereitgestellt mit freundlicher Unterstützung der Staatsbibliothek zu Berlin - Preußischer Kulturbesitz

Pollen and macroremains from three sediment cores from Göttingen, Germany

In a borehole in the southern outskirts of the town of Göttingen, limnic sediments of several Pleistocene warm periods occur intercalated with coarse solifluction debris and gravel of the river Leine. Pollen analysis of the limnic sediments in a borehole at Ottostrasse gave evidence of three warm periods of interglacial character, followed by three interstadial phases. The warm phases are separated one from another by stadial phases with, at least in one case, indications of periglacial solifluction. This sequence belongs to the Brunhes magnetic epoch. The pollen data allow to exclude an Eemian or Holsteinian age of the warm period sediments. Thus a Cromerian age is assumed, though the exact position of the newly described warm periods within the ''Cromerian'' remains uncertain. A section in a borehole at Akazienweg is of Holsteinian age.

Pollen assemblages of modern soil samples from the Old Botanical Garden of the University of Göttingen

The importance of pollen analytical data for the reconstruction of the natural conditions and their changes caused by human impact in prehistorical and historical times is beyond all doubt. Pollen analysis can, however, be hampered by poor pollen preservation and low pollen concentrations. As an example pollen assemblages from excavation areas near Pompeii (see doi:10.1594/PANGAEA.777531) and from the Old Botanical Garden of the University of Göttingen are discussed. A pollen diagram (see doi:10.1594/PANGAEA.820590) from the site Höllerer See in Austria (N of the city of Salzburg) demonstrates the intensive agricultural influence on the vegetation of the area during Roman and Medieval times. Human influence was much weaker during the Iron and the Bronze ages. There is no indication of human impact on the vegetation during the Migration period.