126 Geological Society. 



Fullers' Earth {zigzag) . 



r.S ./ r I- ^^^bWy Beds. ^ ,. , . ^ Clypens-Gvit of the 



\ ^%-l II. ^«a6acia-Liniestones. ^ ^'"^^''-^'f.^ff l Mid and North 

 Inferior J | « llll. Doulting Stone. J -^--''"■) J Cotteswolds. 



IV. Upper Coral-Bed {TriieUn) 



Oolite. 



(Non-Sequence) 

 Lias. 



C =' Coralline Beds' 



(. of Dundry. 



V. Dundry Freestone {Usually absent.) 



VI. Upper Trigonia-Gv'it (GarantiancB). 



In oue appendix Mr. S. S. Buckman indicates the deposits in 

 Dorset equivalent to the ahove ; in another the late Mr. J. F. 

 Walker and Mr. Ptichardson deal with the Brachiopoda of the 

 Fullers' Earth, naming seven new species ; and in a third, 

 Mr. Richardson describes a new Amherleya and Sjnrorbis. The 

 micro-fauna of the Upper Coral-Bed is dealt with by Mr. C. Upton, 

 who obtained from material fui'nished him from Midford and 

 Timsbury Sleight most of the micro-brachiopoda such as were 

 found by Charles Moore at Dundry Hill. 



2. ' The Inferior Oolite and Contiguous Deposits of the District 

 between the Rissingtons and Burford.' By Linsdall Richardson, 

 F.G.S. 



This paper is presented with the preceding, because there are 

 several points of similarity between the two districts described. 

 Both are near lines of country along which movements of upheaval 

 were frequent during the time of formation of the Inferior-Oolite 

 rocks. 



In the Bath-Doulting district, above the Upper Trigonia-Gnt 

 (which rests upon the Upper Lias) over a restricted area is the 

 Dundry Freestone, and over a greater the Upper Coral-Bed. Then 

 come the Doulting Beds. The Doulting Beds are equivalent to the 

 Cly2:>eus-Gr\t of the district here dealt with : the Bubbly Beds to the 

 Rubbly Beds, and the .4na6aHa-Limestones, plus the Doulting Stone, 

 to the ' Massive Beds' of the C1ypeus-Gv\t. The basal portion of the 

 Fullers' Earth in the neighbourhood of Midford is of ziyzag hemera. 

 There is no reason for assigning the thin clay-bed, with its median 

 band of Ostrea-acuminata Limestone at Great Rissington, to any 

 other hemera. Whatever is the case elsewhere, there is no deposit 

 in the Rissington district between the Clypeus-Grit and the 

 Fullers' Earth. 



3. ' The Flora of the Inferior Oolite of Brora (Sutherland).' By 

 Miss M. C. Stopes, D.Sc, Ph.D., Lecturer in the Victoria Univer- 

 sity of Manchester. 



This paper is to place on record the discovery of a bed containing 

 impressions of plants, which represent a flora bearing a strong like- 

 ness to that of the Inferior Oolite of the Yorkshire coast. Previously, 



