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PTERODACTYLES (Gr. for wing-fingers)

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Originally appearing in Volume V22, Page 616 of the 1911 Encyclopedia Britannica.
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PTERODACTYLES (Gr. for wing-fingers)  , an See also:extinct See also:order of flying See also:reptiles, variously known as Pterosauria (Gr. for wing-lizards) or Ornithosauria (Gr. for See also:bird-lizards), whose remains occur in all Mesozoic formations from the See also:Lower See also:Lias to the Upper Cretaceous inclusive . Their bones are of very See also:light, though strong construction, and hollow like those of flying birds, with well-fitting articulations, quite different from those of See also:ordinary reptiles . The See also:head is large and remarkably bird-like in shape, while it is fixed on the See also:neck at the same See also:angle as in birds . The See also:brain is small, but resembles that of birds in its See also:general conformation . The See also:trunk is relatively small, with few slender ribs and a keeled breastbone (sternum) . The fore-limbs are always a pair of wings, the fifth See also:digit or " little " See also:finger being enormously elongated for the support of a smooth flying membrane (seen in specimens from the lithographic See also:stone of See also:Bavaria) . The wings are thus constructed on the same See also:plan as those of a See also:bat, but instead of four fingers, only one is elongated to See also:bear the membrane . The See also:hind-limbs are comparatively feeble, and must have been of very little use for walking . The remains of See also:pterodactyles are found chiefly in marine deposits, so that these reptiles must have frequented the See also:coast-lines . They probably fed partly on See also:fish, partly on See also:insects; but no traces of See also:food have hitherto been observed within the fossil skeletons . The See also:oldest satisfactorily known member of the See also:group is Dimorphodon from the Lower Lias of See also:Dorsetshire . The typical See also:species has a See also:skull about 20 centim. in length, with large See also:teeth in front, smaller teeth behind: its tail is much elongated and slender .

Equally See also:

fine skeletons of Campylognaehus have been found in the Upper Lias of See also:Wurttemberg . Other See also:long-tailed pterodactyles occur well preserved in the Upper See also:Jurassic (lithographic stone) of Bavaria and Wurttemberg, which is so fine-grained as to show impressions of the wing-membrane . In Rhamphorhynchus there is also a rhomboidal expansion of membrane at the end of the tail . The See also:short-tailed Pterodactylus itself, sometimes no larger than a See also:sparrow, is also found in the same formation . It was originally described by Collini in 1784 as an unknown See also:sea-See also:animal, and its true nature was first deter-See also:mined by See also:Cuvier in 1809, when he named it " Pterodactyle." The Pterosaurians of the Cretaceous See also:period, just before their extinction both in See also:Europe and in See also:North See also:America, were of enormous See also:size, and some became toothless . A pair of wings of the toothless Pteranodon from the See also:Chalk of See also:Kansas, now in the See also:British Museum, See also:measures about five and a See also:half metres in span . Fragments of equally large pterodactyles with teeth are found in the See also:English Chalk . See H . G . See also:Seeley, The Ornithosauria (See also:Cambridge, 187o) and Dragons of the See also:Air (See also:London, 1901) ; S . W . Williston, See also:paper in Kansas University Quarterly (1897), v1 .

35; G . F . See also:

Eaton, papers in Amer . Journ . See also:Science (1903-1904), 4th See also:series, vols. xvi., xvii . (A . S .

End of Article: PTERODACTYLES (Gr. for wing-fingers)
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