Another thermophilic "miocene survivor" from the italian pliocene: A geologically young occurrence of the pelagic eagle ray aetobatus in the euro-mediterranean region [Un autre "survivant miocène" thermophile du pliocène italien: Une occurrence précoce de l'aigle de mer pélagique aetobatus dans la région euro-méditerranéenne.]

Aetobatus (Myliobatiformes: Aetobatidae) is a living genus of eagle rays that occurs in shal-low-marine, tropical and subtropical environments of the Atlantic, Pacific, and Indian Oceans. Nowa-days, Aetobatus does not inhabit the cool-to warm-temperate European and Mediterranean waters, though it is known from this broad region by virtue of several fossil teeth ranging chronostratigra-phically from the lower Palaeogene to the upper Neogene. The present paper reports on a fossil aeto-batid tooth discovered in mid-Pliocene (upper Zanclean to lower Piacenzian, 3.82-3.19 Ma) marine deposits exposed in the vicinities of Certaldo (Tuscany, Italy) and identified as belonging to †Aetobatus cf. cappettai. This specimen comprises the youngest occurrence of Aetobatus along the coasts of main-land Europe; furthermore, together with previous finds from roughly coeval deposits of Mallorca (Balearic Islands, Spain), it represents the most recent record of this genus in the whole Euro-Mediter-ranean region. In light of the environmental preferences of extant Aetobatus spp., our discovery suggests palaeoenvironmental conditions favourable to the persistence of tropical/subtropical taxa of "Mio-cene survivors" along the Pliocene coasts of Tuscany. In addition, it raises the question of whether or not the Messinian Salinity Crisis really resulted in the complete collapse of the Mediterranean marine biota and in the subsequent recolonisation of the Mediterranean Basin from the adjoining Atlantic waters and/or scattered marginal intrabasinal refugia at the beginning of the Pliocene. The possibility of Aetobatus recolonising the Mediterranean Sea through the Suez Canal in the near future is dis-cussed.