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Zanclean (∼ Brunssumian) to early Piacenzian (∼ early-middle Reuverian) climate from 4° to 54° north latitude (West Africa West Europe and West Mediterranean areas)
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Evolution of the Messinian Mediterranean environments: the Tripoli Formation at Capodarso (Sicily Italy)
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Warny, S., 1999. Marine and continental environmental changes in the Gibraltar Arc area during the Late Neogene (8-2.7 Ma) linked to the evolution of global climate and to Atlantic Ocean-Mediterranean Sea relationships. A palynological contribution to the Messinian salinity crisis through dinoflagellate cysts and pollen analysis. PhD thesis, University of Louvain la Neuve, Louvain la Neuve.
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