336 Localities of Fossil Shells 



Bath, Somerset, 9 species, W, in Blue Lias. 



Spirifer Waicotti, t 377, f 2. [Green Sand. 

 Blackdown Hills, Devon., see vol. 59, p. 323, 21 species in 

 Rostellaria calcarata, t 349, f 6 and 7, 5 loii\ 



Parkinson! S. t 349, i 5, iid in 2^7 Bead: 



Turbo monilifer, t 395, f 1. [land Rock (Sand). 



Black-oang Chine, Isle of Wight, 8 m S of Newport, in Port- 



GrypliEea sinuata, t 336. 

 Black-Rock, near Cork*, see vol. 59, p. 324, 14 species, in 

 Derbyshire-peak I^imestone. 



Productus punctatus, t 323. 



Terebratula acuminata, t 324, f 1. [London Cla}'. 

 Bognor-Rocks, Sussex, see vol. 59, p. 324, 6 species, in 

 Pinna affinis, t 313, f. 2. 



Rostellaria Parkinsoni /3, t 349, f 3 & 4, 3 mid. 



Bolingbroke, Lincoln, (see vol. 52, p. 352) NE, in Woburn 



Ammonites plicomjjhalus, t 359 & 404. [Sand. 



Bourdeaux, in Gironde Dep. SSW of Paris, in London Clay? 



Sigaretus canaliculatus, t 384. [upper Oolite. 



Bradford, Wilts, see vol. 59, p. 324, 3 species, E, in Clay on 



Terebratula coarctata, t 312, f 1 to 4. 

 Braken-Vv^ood End, Lincoln., 3^ m SW of Horncastle, in 

 Ammonites mutabilis, t 405. [Clunch Clay. 



GrypliEea buUata, t 368. 

 Brambles-Chine, Isle of Wight, If m. SW of Yarmouth, in 

 Ancilla subulata, t 333, f 1 & 2. [London Clay. 



Brassington, Derb., 3 m W of Wirksvi^orth, in Derbyshire- 

 peak 3rd Limestone. 



Terebratula acuminata, t 324, f 1. [Strata. 



Bray, Berks, 3 m W of Windsor, SE, in London Deep-well 



Rostellaria Parkinsoni «, t 349, f 1, 2 up. 

 Breedon, Leicest., 4 ra NNE of Ashby-de-la-Zouch, in yellow 

 Productus humerosus, t 322. [Limestone. 

 Brighton, Sussex, see vol. 46, p. 215, 2 species, in upper Chalk. 



Pecten nitidus, t 394, f 1. 

 Buxton, Derb., see vol. 59, p. 324, 5 species, iji Derbyshire- 

 peak Lin)estoiie. 



Productus giganteus, t 320 (1st). 



punctatus, t 323 (3rd). 



Terebratula acuminata, t 324, f 1 (3rd). 



* See Mr. Parkinson's " Introduction to the Study of Fossil Organic 

 Remains," p. 244: and here I beg to ask the fovour of Mr. Miller to de- 

 fine, as accurately as lie may be able, the Situation, surface Range, and Dip, 

 and the under-lying and oVer-Iying Rocks, of the Limestone near Cork, 

 which he calls "Transition"?: is it between coarse Slate Strata, or Stea- 

 sc/iistiis Rocks? see " Annals of Philo." Hd Ser. IV. i22, and "Monthly 

 Mac." vol. 58, p. 250. 



Cal- 



