THE FEE-ADAMITE EARTH. 



FOUETH JURASSIC PERIOD. 



357. The strata deposited in this period, called by D'Orbigny 

 the Bajocian stage, from the French town of Bayeux (Bajoce), 

 correspond with the inferior Oolite of British geologists. Its 

 course on the surface is indicated on the map (fig. 153) by the 

 shading number 10. 



358. The animal kingdom of this period is shown in the 

 following table : 



Synopsis of the Animal Kingdom (exclusive of the Annulata) during the 

 Fourth Jurassic Period. 



359. Of the terrestrial fauna of this period nothing is known, 

 and a few plants only, consisting of Cicadea) and doubtful 

 Monocotyledons remain. 



FIFTH JURASSIC PERIOD. 



360. This stage, the Bathonian of D'Orbigny and D'Halloy, 

 corresponds with the great Bath oolite, Forest marble, and Stones- 

 field slate of British geologists. 



361. When tranquillity was re-established after the catastrophe 

 which terminated the fourth period, a new creation appeared on 

 the earth, of which the chief part is shown in the following 

 table : 



