Abstract
The palynostratigraphy of two sediment cores
from Soppensee, Central Switzerland (596 m asl) was
correlated with nine regional pollen assemblage zones
defined for the Swiss Plateau. This biostratigraphy
shows that the sedimentary record of Soppensee includes
the last 15 000 years, i.e. the entire Late-glacial and
Holocene environmental history. The vegetation history
of the Soppensee catchment was
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