Abstract
According to their microstratigraphical composition the laminated sediments of Baldeggersee
are true varves. Two varve time-series from freeze cores taken in the deepest part (66 m) of
Baldeggersee have been analysed for annual and seasonal layers. The varve time-series covers the
period of 1885 to 1993.
The two freeze-cores from Baldeggersee can be accurately
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