THE EOCENE PERIOD. 



295 



been found in any Tertiary stratum; but the internal skeletons 

 of Cuttle-fishes (such as Belosepia) are not unknown. 



Remains of Fishes are very abundant in strata of Eocene 

 age, especially in certain localities. The most famous depot 

 for the fossil fishes of this period is the limestone of Monte 

 Bolca, near Verona, which is interstratified with beds of vol- 

 canic ashes, the whole being referable to the Middle Eocene. 

 The fishes here seem to have been suddenly destroyed by a 

 volcanic eruption, and are found in vast numbers. Agassiz 

 has described over one hundred and thirty species of Fishes 

 from this locality, belonging to seventy-seven genera. All 

 the species are extinct; but about one-half of the genera are 

 represented by living forms. The great majority of the 



Fig. 223. — Rhoinhits iniiiiiniis, a small fossil Turbot from the Eocene Tertiary, 

 Alonte Bolca. 



Eocene Fishes belong to the order of the " Bony Fishes " 

 {Teleosteans), so that in the main the forms of Fishes charac- 

 terising the Eocene are similar to those which predominate 

 in existing seas. In addition to the above, a few Ganoids and 

 a large number of Placoids are known to occur in the Eocene 

 rocks. Amongst the latter are found numerous teeth of true 

 Sharks, such as Otodics (fig. 224) and Ca?r/iarodon. The 

 pointed and serrated teeth of the latter sometimes attain a 

 length of over half a foot, indicating that these predaceous 

 fishes attained gigantic dimensions; and it is interesting to 

 note that teeth, in external appearance very similar to those 

 of the early Tertiary genus Ca?rharodon, have been dredged 

 from great depths during the recent expedition of the Chal- 

 lenger. There also occur not uncommonly the flattened 



