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rp-edged teeth of true Sharks are very abundant in some beds, such as the Upper Greensand, and are beautifully preserved. The teeth of some forms (_Carcharias_, &c.) attain occasionally a length of three or four inches, and indicate the existence in the Cretaceous seas of huge predaceous fishes, probably larger than any existing Sharks. The remains of _Cestracionts_ consist partly of the flattened teeth of genera such as _Acrodus_ and _Ptychodus_ (the latter confined to rocks of this age), and partly of the pointed teeth of _Hybodus_, a genus which dates from the Trias. In this genus the teeth (fig. 206) consist of a principal central cone, flanked by minor lateral cones; and the fin-spines (fig. 207) are longitudinally grooved, and carry a series of small spines on their hinder or concave margin. Lastly, the great modern order of the Bony Fishes or _Teleosteans_ makes its first appearance in the Upper Cretaceous rocks, where it is represented by forms belonging to no less than three existing groups--namely, the Salmon family (_Salmonidoe_), the Herring family (_Clupeidoe_), and the Perch family (_Percidoe_). All these fishes have thin, horny, overlapping scales, symmetrical ("homocercal") tails, and bony skeletons. The genus _Beryx_ (fig. 208, 1) is one represented by existing species at the present day, and belongs to the Perch family. The genus _Osmeroides_, again (fig. 208, 2), is supposed to be related to the living Smelts (_Osmerus_), and, therefore, to belong to the Salmon tribe. [Illustration: Fig. 205.--Guard of _Belemnitella mucronata_. White Chalk.] [Illustration: Fig. 206.--Tooth of _Hybodus_.] [Illustration: Fig. 207.--Fin-spine of _Hybodus_. Lower Greensand.] [Illustration: Fig. 208.--1, _Beryx Lewesiensis_, a Percoid fish from the Chalk; 2, _Osmeroides Mantelli_, a Salmonoid fish from the Chalk.] No remains of _Amphibians_ have hitherto been detected in any part of the Cretaceous series; but _Reptiles_ are extremely numerous, and belong to very varied types. As regards the great extinct groups of Reptiles which characterise the Mesozoic period as a whole, the huge "Enaliosaurs" or "Sea-Lizards" are still represented by the _Ichthyosaur_ and the _Plesiosaur_. Nearly allied to the latter of these is the _Elasmosaurus_ of the American Cretaceous, which combined the long tail of the Ichthyosaur with the long neck of the Plesiosaur. The length of this monstrous Reptile could not have been less th
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