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SUPPLEMENT TO THE BRITISH 



114. Terebratula galeiformis, M'Coy, MS. Dav., Ool. Mon., p. 59, PI. XIII, fig. 11 



(under the name of T. Bentteyi, 

 var. sub-Bentleyi) ; and Appendix to 

 Vol. I, p. 19, PI. A, fig. 15. 



Nothing new. Continues to be very rare. Only recorded from the Inferior Oolite, 

 near Minchinhampton. 



115. Terebratula elabellum, Desl. Dav., Ool. Mon., p. 62, PI. XII, figs. 19 — 21. 

 Nothing new. Bradford Clay. 



116. Terebratula hemispheric^, Sow. Dav., Ool. Mon., p. 64, PI. XIII, figs. 17, 18. 



Mr. C. Moore informs me that this species has the loop of a Terebratula, and must 

 therefore be removed from Terebratella. I have never, however, seen the perfect loop, 

 and I cannot therefore speak authoritatively upon the subject. 



Mr. Etallon has described under the name of Megerlia tenuicostata, and the Erere 

 Ogerien under the name of T. Dallozi, a small shell (which I cannot distinguish from 

 T. hemisphcBricd) from Valfin, near St. Claude, in Erance, and which Mr. Bayan has also 

 found at Tonnerre in beds of a similar age. This bed, according to Mr. Bayan, corre- 

 sponds to the base of the Kimmeridge Clay, or the middle of that formation which the 

 French geologists now term Sequanien. 



T. hemispharica occurs in the Great Oolite in England at Hampton Cliff, near Bath ; 

 and larger examples have been met with in the same formation at Luc and Langrune, in 

 Normandy. 



117. Terebratula minuta, Moore. Sup., PI. XVII, figs. 11, 12. 



Terebratula ? minuta, Moore. The Geologist, vol. iv, p. 191, pi. ii, figs. 21, 22, 1861. 



Shell minute, broadly rounded, nearly straight in front, slightly longer than wide. 

 Dorsal valve moderately biconvex or longitudinally divided by a narrow depression ; 

 ventral valve evenly convex, beak very slightly incurved and truncated by a circular 



