ROCKS OF SOUTH DEVOJS-. 501 



Identified by Messrs. Sharman and Newton : 



Atrypa aspera. j Scoliostoma (Turbo) texatum. 



desquamata. Heliolites porosus. 



Productus sLibaculeatus. j 



From Daddyhole Cove. Identified by M. Freeh on the spot : 



Cyrtina Whidboruei. j Caleeola sandalina. 



Pentamerus galeatus. | Monticulipora, allied to M. fibrosa. 



In red shaly limestones and shale under Daddyhole Knoll*, at 

 south end of Meadfoot sands, I obtained Atrypa, Leptcena resem- 

 bling laticosta, Spirifer like speciosus, Pliacops, Caleeola sandalina, 

 and Fenestella. 



In Torquay Cemetery irregular limestone beds, associated with 

 slate, furnished Atnjpa reticularis and Spirifer speciosus, identified 

 by Prof. Gosselet. 



In shaly limestones turned out of wells at Higher and Lower 

 Weston Farms, identified by Dr. Kayser : Atrypa reticularis, Spirifir 

 allied to speciosus, not apparently the speciosus with broader folds. 



Weston Wells. Identified by Messrs. Sharman and Newton : 



' Area. I Alveolites. 



Chonetes. Favosites Goldfussi. 



Orthis. I Cyathopbyllum damnoniense. 



Limestone north of Bridgetown, Totnes : 



Cystiphyllum vesiculosum. 



Limestone at Highlands, Totnes : 



Alveolites. I Oyathophyllum heliantboides. 



Stromatopora concentrica. | 



Reddish- weathered shaly limestones, at base of Brixham limestones, at Cburstcn 

 Station : 



Favosites Goldfussi. [ Heliolites porosus. 



As there is absolutely no line of demarcation between the upper 

 horizon of the Eifelian (the Calceolen-Kalk) and the bedded lime- 

 stones above, this separate treatment of Eifelian limestones and 

 limestones of the Stringocephalus horizon is purely arbitrary. 



2. Middle-Devonian Limestone (Stringocephalus-horizon). — The 

 Middle-Devonian Limestones of Dartington, Littlehempston, Bcrry- 

 Pomeroy, Gatcombe Park, Marldon, Daddyhole, London Bridge 

 (Torquay), of Anstey's Cove in part, and of Babbacombe-Down 

 cliffs belong to the same series ; they are usually bluish grey or dark 

 grey and distinctly bedded. The lower part, at least, of the Torbryau, 

 Denbury, and West-Ogwell limestone, and probably the limestones of 

 Whilborough and Abb ots-Kers well, and those between Bulley-Barton 

 and Wrigwell, south of Dainton, may be bracketed with the above. 

 But the limestones of Barton, Lummaton, and Yeadown, and those 



^' Kyamodes, a new genus of Ostracod, was obtained by the Rev. G. F. Whid- 

 borne in the lower part of the Daddyhole limestone (Eifelian). 



Q.J.G.S. NTo. 183. 2n 



