730 MR. F. CHAPMAN ON THE BARGATE BEDS OF SURREY. [Nov. 1 894, 



was just such as in a smaller or less clearly exposed section 

 would be ascribed to an unconformity, but it was clearly false- 

 bedding. He thought that the Society was much indebted to the 

 Author of the paper for his microscopical work, which he hoped 

 would be continued, because it would be an advantage if certain 

 beds of the Lower Greensand could be correlated thereby ; for 

 instance, if the beds of the Horsham Road-cutting could be corre- 

 lated by means of the foraminifera, a great result would be obtained 

 by the examination of these small organisms. 



Prof. Judd called attention to the great importance of the 

 Author's researches, not only in increasing our knowledge of the 

 Cretaceous microzoa, but in giving evidence of the existence in the 

 immediate neighbourhood of the district described by him of 

 Jurassic rocks, for he has found a Lower Greensand rock filled with 

 derived grains of oolite, like those occurring in the Richmond boring. 



Mr. Whitakee, Dr. G. J. Hinde, Mr. Topley, and Prof. T. 

 Rupert Jones also spoke. 



[Note. — In the abstract of this paper — which was submitted to 

 the Secretary by the Author — an unconformity was inadvertently 

 mentioned as occurring between the Folkestone and the Bargate 

 Beds. As in the paper itself, it should have been referred to as an 

 •eroded surface (contemporaneous erosion). — Sept. 7th, 1894.] 



