Abstract
Palaeomagnetic measurements have been carried out on Eocene to Pleistocene sediments on the Ionian island
of Zakynthos, NW Greece. Magnetostratigraphic constraints, biostratigraphic analyses of planktonic foraminifera and
calcareous nannofossils provide a reliable time frame for these deposits. The results show that no significant rotation
occurred between 8.11 and 0.77 Ma, but that Zakynthos
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