Abstract
A detailed study has been made of Late Cenozoic ostracodes from closely
sampled sections and some isolated samples on the Aegean islands of Gavdos,
Crete, Karpathos and Rhodos.
The stratigraphic position of the studied lithostratigraphic units has been
determined by means of the evolutionary trends in Planorbulinella and in uniserial
Uvigerina, and by planktonic Foraminifera
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