446 Br. Wheelton Hind — British Carboniferous Goniatites. 



Staffordshire: Below the Eough Rock, Millstone Grit, near Ipstones. 



Devonshire : Iiistow. 



Ireland : marine bands, Castlecomer Coalfield. 



Gastrioceras coronatum, Foord & Crick. Lower Coal-measures. 

 Lancashire; above the Mountain Mine, Bacup. 

 Yorkshire : above the Mountain Mine, Shibden. 



Genus Prolecanites, Mojsisovics. 

 Prolecanites compressus, J. Sowerby. 



A most important zone form denoting the base of the Pendleside 

 Series, and only occupying as a rule a few feet of beds, except on 

 Pendle Hill, River Hodder, and Longridge Pell, where a great local 

 expansion of the Pendleside Limestone occurs. 



Lancashire : Warsaw End, Hook Cliff, Little Mearley Clough, 

 Pendleton Clough, River Hodder below bathing cots, River Ribble 

 at Dinckley Hall, at dip 2° in stream about one mile N. of 

 Ciiipping. 



Yorkshire: River Hodder below Sandal Holm, Salterforth railway 

 cutting, Rilstone, Ingsbeck at base of Pendleside Limestone. 



Cheshire: Old limestone quarry near Astburv, below Congleton 

 Edge. 



Devonshire : Coddon Hill, near Barnstaple. 



Isle of Man : Scarlet Quarry. 



Ireland: Co. Cork, Little Island and Black Rock, Middleton, 

 Ballynabintra ; Co. Galway, 4 miles east of Loughrea. 

 Prolecanites micolobus, Phillips. 



Very rare. Phillips gave Bolland as the locality. 



Prolecanites discoides, Poord & Crick. Carboniferous Lime- 

 • stone, D2. 



Yorkshire : El Bolton, near Cracoe. 

 Derbyshire: Park Hill and Brassington. 



Prolecanites serpentinus, Phillips. 

 A very small shell. Base of Pendleside Series. 

 Lancashire : River Hodder, River Ribble at Dinckley Hall, 

 Black Hall. 



Pronorites, Mojsisovics. 

 Pronorites ctclolobus, Phillips. 

 Very rare. Carboniferous Limestone, D2. 



Yorkshire: El Bolton, probably ; Grassington is quoted in Phillips's 

 list of errata. 



Derbyshire : Thorpe Cloud. 



NEW GENUS. 

 Sagittoceras, Hind. 

 The genus is founded on a single specimen which consists of 

 three-fourths of a complete individual. A large portion of the body- 

 chamber is present, Avhich on removal reveals the greater part of 

 the penultimate whorl with the camerse and suture-lines. 



I obtained the specimen from Keal Hill, one of the well-known 



