The Holstein interglacial is classified as the period between the end of the Elster glaciation to the beginning of the Fuhne glaciation. The deposits in Brandenburg are supplied by limnic to fluviatile sedimentary regimes. Thus, the deposits consist of organic mud and silt as well as bituminous peat. Related to higher energetic levels, the fluvial associated deposits are made up of sand. The stratigraphic classification is based on palynostratigraphy and on the occurrence of the index fossil Viviparus diluvianus.
In this study, a new map is constructed that focuses on the distribution of limnetic sediments. Contrary to this, the existing maps summarise the limnetic and fluviatile deposits including the sediments of the lower Saale. Two sets of maps have been published since 1971 (Lithofazieskarte Quartär - scale 1:50 000 and Zwirner & Ziermann 2010 - scale 1:1 000 000).
Based on more than 400 palynostratigraphically proven locations (via drillings), a map will be published that achieves a significant extension and clarification of the distribution of the limnetic Holstein. The accumulation area of these deposits can be associated with numerous channel systems and paleo-basins initiated during the Elster glaciation. Furthermore, transgressive pathways are revised in this study. These were derived from Holstein Stage sea-level changes that resulted in transgressive and regressive successions with brackish to marine facies in northwest Brandenburg.
Zwirner & Ziermann 2010. „Verbreitung und Tiefenlage der Holstein-Warmzeit und frühsaalezeitlicher Ablagerungen“ in Stackebrandt, W. (Hrsg.). Atlas zur Geologie von Brandenburg. Landesamt für Bergbau, Geologie und Rohstoffe Brandenburg, 53.