Published online by Cambridge University Press: 01 May 2009
The footprints from the fissile Keuper sandstones of Chillington comprise, in addition to the ordinary Cheirotherian impressions, two interesting series. A number of fragments of rock covered with worm tracks and castings, show several imperfectly preserved footprints of a small five-toed animal, with posterior limbs of much greater size than the anterior; and three portions of comparatively smooth slabs afford evidence of a larger animal, probably of the same genus, of which the impressions of the feet are preserved with remarkable distinctness. There are also singular reticulated markings upon the surface of another small slab from the same beds, which may be interpreted as the impression of reptilian (? or labyrinthodont) skin. (See Fig. 2, p. 217.)
page 216 note 1 Owen, R., “Description of an Extinct Lacertian Reptile, Rhynchosaurus articeps, Owen”: Trans. Cambridge Phil. Soc., vol. vii (1842), p. 355Google Scholar. Sir Richard Owen refers to the specimens described by Ward—, O. “On Footprints and Ripple Marks of the New Red Sandstone of Grinshill Hill, Shropshire,” Brit. Assoc. Rep., 1839, Trans. Sect., p. 75; also by Murchison and Strickland, Trans. Geol. Soc. [2], vol. v, p. 339, pl. xxviii, fig. 1, from the Keuper of Shrewley, Warwickshire.Google Scholar
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