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A model of estuarine circulation in the Pliocene Mediterranean based on new ostracod evidence Dick van Harten
Geological Institute, University of Amsterdam, Nieuwe Prinsengracht 130, 1018 VZ Amsterdam, The Netherlands
The recent discovery of the psychrospheric ostracod Agrenocythere pliocenica (Seguenza) in Zanclean marls of eastern Crete1 expands the reach of early Pliocene deep-oceanic circulation far into the eastern Mediterranean. Current models of Pliocene water-mass circulation, though allowing for the Atlantic psychrosphere to flow freely into the western basin, consider the eastern basin as being largely stagnant2,3. I propose here a new model of estuarine circulation affecting both west and east Mediterranean. This circulation was associated with increased atmospheric humidity and driven by upwelling. The model is compatible with organic-rich sedimentation in parts of the eastern Mediterranean and does not imply an excessively deep or wide connection with the Atlantic.
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