Pollen and macroremains from three sediment cores from Göttingen, Germany
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| Format: | Dataset Open Access |
| Sprache: | en |
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PANGAEA
1994
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| _version_ | 1867167662378844160 |
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| author | Grüger, Eberhard Jordan, Heinz Meischner, Dieter Schlie, Peter |
| author_facet | Grüger, Eberhard Jordan, Heinz Meischner, Dieter Schlie, Peter |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | 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. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_728993 |
| institution | PANGAEA |
| language | en |
| publishDate | 1994 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | Pollen and macroremains from three sediment cores from Göttingen, Germany Grüger, Eberhard Jordan, Heinz Meischner, Dieter Schlie, Peter Akazienweg; DRILL; Drilling/drill rig; Göttingen, Lower Saxony, Germany; HAND; Lower Saxony, Northern Germany; Ottostrasse; Sampling by hand; Wallensen 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. |
| title | Pollen and macroremains from three sediment cores from Göttingen, Germany |
| topic | Akazienweg; DRILL; Drilling/drill rig; Göttingen, Lower Saxony, Germany; HAND; Lower Saxony, Northern Germany; Ottostrasse; Sampling by hand; Wallensen |
| url | https://doi.org/10.1594/PANGAEA.728993 |