This paper aims to contribute to the understanding of fluvial system response to climate change during the last glacial-interglacial cycle. Fluvial and aeolian successions have been studied in the opencast brown-coal mine Nochten in eastern Germany. An absolute chronology was established by luminescence an
During the final revision and submission phase, Sebastian Kreutzer was supported by the DFG Heisenbe...
Understanding and interpreting climate response from ancient fluvial deposits requires a combined ap...
On a straight slope within the lake catchment of Kleiner Tornowsee (Brandenburg, Germany) a sequence...
Cryoturbated organic beds and channel fills, intercalated with sandy and gravelly fluvial units, hav...
Climate change during the Last Glacial is considered as a major forcing factor of fluvial system cha...
In the Weichselian, the Lower Rhine in the Dutch-German border region has used three courses, dissec...
The Niers valley was part of the Rhine system that came into existence during the maximum Saalian gl...
We inferred past climate conditions from lacustrine sediments intercalated in Weichselian Early Glac...
The Weichselian Late Pleniglacial and Lateglacial aeolian stratigraphy (Older Coversand I, Beuningen...
Optically Stimulated Luminescence (OSL) dating allows the age determination of sediments deposited d...
Luminescence dating was applied to Last Glacial and Early Holocene fluvial deposits derived from the...
Little is known about the impact of Late Devensian (Weichselian) aridity on lowland British landscap...
The study of the outcropping glacial sediments of Stolzenhagen combines detailed sedimentological an...
During the Weichselian (MIS 4-2) the Rhine entered the Netherlands through three different branches,...
We present results of research into fluvial to aeolian successions at four sites in the foreland of ...
During the final revision and submission phase, Sebastian Kreutzer was supported by the DFG Heisenbe...
Understanding and interpreting climate response from ancient fluvial deposits requires a combined ap...
On a straight slope within the lake catchment of Kleiner Tornowsee (Brandenburg, Germany) a sequence...
Cryoturbated organic beds and channel fills, intercalated with sandy and gravelly fluvial units, hav...
Climate change during the Last Glacial is considered as a major forcing factor of fluvial system cha...
In the Weichselian, the Lower Rhine in the Dutch-German border region has used three courses, dissec...
The Niers valley was part of the Rhine system that came into existence during the maximum Saalian gl...
We inferred past climate conditions from lacustrine sediments intercalated in Weichselian Early Glac...
The Weichselian Late Pleniglacial and Lateglacial aeolian stratigraphy (Older Coversand I, Beuningen...
Optically Stimulated Luminescence (OSL) dating allows the age determination of sediments deposited d...
Luminescence dating was applied to Last Glacial and Early Holocene fluvial deposits derived from the...
Little is known about the impact of Late Devensian (Weichselian) aridity on lowland British landscap...
The study of the outcropping glacial sediments of Stolzenhagen combines detailed sedimentological an...
During the Weichselian (MIS 4-2) the Rhine entered the Netherlands through three different branches,...
We present results of research into fluvial to aeolian successions at four sites in the foreland of ...
During the final revision and submission phase, Sebastian Kreutzer was supported by the DFG Heisenbe...
Understanding and interpreting climate response from ancient fluvial deposits requires a combined ap...
On a straight slope within the lake catchment of Kleiner Tornowsee (Brandenburg, Germany) a sequence...
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