“…The Paratethys formed to the north of the future Mediterranean Sea, as a marginal sea, with restricted exchanges with the open marine environment of the Tethys (Schultz et al, 2005). A number of marine fossil fishes or ichthyofaunas are know from deposits of the Paratethys region that are considered to be Oligocene or might include Oligocene sediments, including those, for example, from the Rhine Graben of France and Germany, the Carpathian region of Poland, Czech Republic, Romania, and Ukraine, and the Caucasus region of Russia and neighboring areas including Azerbaijan (e.g., Jerzmańska, 1968;Tyler et al, 1993;Micklich and Parin, 1996;Pharisat and Micklich, 1998;Constantin, 1999;Bieńkowska, 2004;Prokofiev, 2006Prokofiev, , 2007Popov et al, 2008;Přikryl, 2009;Bieńkowska-Wasiluk, 2010;Přikryl et al, 2011). These deposits have provided a wealth of fishes, representing over 40 families of teleost and selachian taxa.…”