Abstract
Biochronostratigraphy for the Tethyan and Boreal mid-Cretaceous (Barremian-Albian) is traditionally based on ammonites. Because of the lack of useful ammonites in the Australian mid-Cretaceous, and the existence of strong faunal and floral latitudinal contrasts, to date chronostratigraphic correlation between the different realms is not straightforward. In the present study dinoflagellate
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