232 HISTORICAL PALEONTOLOGY. 



(19) "On Dicynodon" 'Trans. Geol. Soc., ' vol. iii., 1845. 



Owen. 



(20) ' Descriptive Catalogue of Fossil Reptilia and Fishes in 



the Museum of the Royal College of Surgeons, Eng- 

 land. ' Owen. 



(21 ) " On Species of Labyrinthodon from Warwickshire " 



Trans. Geol. Soc., ' ser. 2, vol. vi. Owen. 



(22) "On a Carnivorous Reptile" (Cynodraco major), &c. 

 ' Quart. Journ. Geol. Soc., ' vol. xxxii., 1876. Owen. 



(23) "On Evidences of Theriodonts in Permian Deposits," 

 &c. ' Quart. Journ. Geol Soc., ' vol. xxxii., 1876. Owen. 



(24) " On the Stagonolepis Robertsoni, " &c. ' Quart. Journ. 



Geol. Soc., ' vol. xv., 1859. Huxley. 



(25) "On a New Specimen of Telerpeton Elginense " 



'Quart. Journ. Geol. Soc., ' vol. xxiii., 1866. Huxley. 



(26) " On Hyperodapedon " ' Quart. Journ. Geol. Soc., ' vol. 

 xxv., 1869. Huxley. 



(27) " On the Affinities between the Deinosaurian Reptiles 



and Birds " ' Quart. Journ. Geol. Soc., ' vol xxvi., 1870. 

 Huxley. 



(28) "On 1 the Classification of the Deinosauria. " &c. 



' Quart. Journ. Geol. Soc., ' vol. xxvi., 1870. Huxley. 



(29) " Palneontologica Indica " ' Memoirs of the Geol. Sur- 



vey of India. ' 



(30) " On the Geological Position and Geographical Distribu- 

 tion of the Dolomitic Conglomerate of the Bristol Area " 

 ' Quart. Journ. Geol. Soc., ' vol. xxvi., 1870. R. Ethe- 

 ridge, sen. 



(31) "Remains of Labyrinthodonta from the Keuper Sand- 



stone of Warwick " ' Quart. Journ. Geol. Soc., ' vol. 

 xxx., 1874. Miall. 



(32) ' Manual of Geology. ' Dana. 



(33) ' Synopsis of Extinct Batrachia and Reptilia of North 



America. ' Cope. 



(34) 'Fossil Footmarks.' Hitchcock. 



(35) ' Ichnology of New England.' Hitchcock. 



(36) ' Traite de Paleontologie Vegetale. ' Schimper. 



(37) ' Histoire des Vegetaux Fossiles. ' Brongniart. 



(38) ' Monographic der Fossilen Coniferen. ' Gceppert. 



CHAPTER XVI. 

 THE JURASSIC PERIOD. 



Resting upon the Trias, with perfect conformity, and with 

 an almost undeterminable junction, we have the great series of 



