268 



GEOLOGY OF THE ISLE OF WIGHT. 



TABLE III. — Upper Cretaceous. 



The letters refer to the authorities by whom the fossils have been recorded. 

 See p. 257. 



Those fossils marked S. were collected from the " Lower Chalk " as mapped 

 in 1852. That subdivision included the Lower and Middle Chalk of the 

 present survey. 



The Middle Chalk of Barrois includes the Chalk Rock and about 20 feet of 

 chalk above it. 



The Upper Greensand of Barrois includes about 35 feet of beds now 

 included in the Gault. That of Fitton includes the Chloritic Marl. 



The numbers indicate the localities enumerated below : — 



1. Isle of Wight, exact 



locality not specified. 



2. Needles. 



3. Alum Bay. 



4. High Down. 



5. Main Bench. 



6. Freshwater. 



7. AfCon Down. 



8. Compton Bay. 



9. Shalcombe. 



10. Brook Road cutting. 



11. Motteston Down. 



12. Brixton and Cal- 



bourne Road. 



PlantcB. 



Algae . . . 



Chondrites fastigiatus, 

 Ster7ib, 



*Clathrai'ia Lyellii, 3Iant. 



Coniferous wood - 



38 Pi. & 

 M. 



38 Sur. 



35 1. 



3SPa. 

 35 N. 



Fucoides Targioni., see Chondrites fastigiatus. 



Spongida. 



Axinella stylus, Hinde. - 



Craticularia (Brachio- 

 lites) Fittoni, Mant. 



Chenendopora 



Doryderma 



Heterostinia (Chenendo- 

 pora) obliqua, Ben, 



Cliona cretacea, Portl. - 



Bendrospongia fene$tralis, F. Boem., see Craticularia Fittoni 



• Steephill and East End. 



Hinde. 



35 

 Hinde. 



35 M. 



1 S. 



IS. 



1S.,1L 



iBa. 

 12 Sur. 



!4 Sur. 



IS. 



