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.

Supplement to: Grüger, Eberhard; Jordan, Heinz; Meischner, Dieter; Schlie, Peter (1994): Mittelpleistozäne Warmzeiten in Göttingen, Bohrungen Ottostrasse und Akazienweg (Middle Pleistocene warm phases in Göttingen, boreholes at Ottostrasse and Akazienweg). Geologisches Jahrbuch, Reihe A, 134, 167-210