Abstract
The Tortonian/Messinian boundary is marked by the first occurrence datum (FOD) of Globorotalia conomiozea
which is found all over Crete in open-marine marls with good palaeomagnetic properties. Within the framework of
the MIOMAR project, the previously studied sections of Langereis et al. [1] have been extended and (partly)
resampled. Here, we present new
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