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Research of Marius Stoica Biostratigraphic and stable isotope constraints on the paleoenvironmental evolution of the Paratethys |
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| This project aims to
study the paleoenvironmental evolution of the Paratethys basins from a
biostratigraphic and isotopic point of view. High-resolution magnetostratigraphic
records have recently been developed for the Mio-Pliocene sediments of
the South and East Carpathian basins, for the first time providing accurate
ages to the foredeep sediments (Vasiliev et al., 2004).
Detailed biostratigraphic and isotopic studies can now provide a major step forward to a better understanding of the depositional environment, paleogeographic evolution and climatic history of the Paratethys region. This project will form a substantial contribution to unraveling the paleogeography of the Paratethys system during its Miocene and Pliocene evolution, i.e. the time when the Mediterranean experienced its dramatic desiccation event of the Messinian Salinity Crisis.
Reconnaissance of the Madulari section (S. Carpathians) Detailed isotopic studied on the high-resolution biostratigraphic dataset can provide crucial information when gateways between Western (Transylvanian/ Pannonian) - Eastern Paratethys - Mediterranean were created and/or disrupted. |
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2011
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