148 BRITISH FOSSIL CORALS. 
Stenopora Macxkrorur, Geinitz, Verst. der Deutsch. Zechst., p. 17, tab. viii, fig. 10, 1848. 
Catamorora Mackrorut, King, Permian Fossils of England, p. 26, tab. iii, figs. 3—6, 1850. 
CuamTetes? Macxrotul, Milne Edwards and Jules Haime, Pol. Foss. des Terr. Paleoz., 
p- 274, 1851. 
“A branching Calamopora: with numerous slender, round or polygonal, transversely- 
wrinkled tubes, rising perpendicularly in the centre of the branches, and afterwards 
suddenly curving out to the surface. Interpolated or new tubes numerous, originating on 
the outside of the old ones. Margin of the apertures with from five to eight spine-like 
tubercles. 
“Tt is rather a common Coral, being found at Tunstall Hill, Humbleton Quarry, 
Dalton-le-Dale, Ryhope-Field House Farm, and Whitley, in the Shelly Limestone. The 
German localities, according to Schlotheim and Geinitz, are Milbitz and Corbusen, in the 
Lower Zechstein ; and Gliicksbrunn and Liebenstein, in the Zechstein Dolomite.” (Xing, 
loc. cit.) 
2. CHATETES P COLUMNARIS. 
CORALLIOLITES COLUMNARIS, Schlotheim, Taschenb. fiir die Ges. Miner., p.59, 1813. 
5 os Ft Akad. Miinch., vol. vi, p. 23, pl. iii, fig. 10, 1820. 
STENOPORA INCRUSTANS, King, Catal. of the Org. Rem. of the Permian Rocks, p. 6, 1848. 
— coLumNaRis, King, Perm. Foss. of England, p. 28, pl. iu, figs. 7, 8, and 9, 1850. 
CHATETES COLUMNARIS, Milne Edwards and Jules Haime, Pol. Foss. des Terr. Paleoz., 
p- 274, 1851. 
“An incrusting Stenopora. Polypidoms tubular, cylindrical, slightly wrmkled more 
or less transversely, and in close contact, except towards their orifice, where they are a 
little reduced in diameter, leaving rather wide imterspaces, which are often perforated 
with interpolated tubes. Apertures circular or slightly polygonal, with a tuberculated 
margin. 
“Tt occurs at Humbleton, Tunstall Hill, and Whitley; but is nowhere a common 
species. Geinitz’s Alveolites producti, which may be the same Coral, is found at 
Corbusen, in Saxony.” (Azng, op. cit.) 
3. CHazreres? Bucwana. 
Atveotites BucurtaNna, King, Perm. Foss. of England, p. 30, pl. ii, figs. 10, 11, & 12, 1850. 
Cuateres Bucuana, Milne Edwards and Jules Haime, Pol. Foss. des Terr. Palzoz., 
p- 274, 1851. 
“Tubes or cells adjoining, cylindrical, leaning, concavely arcuate ascendingly, alter- 
nately overlying each other, and slightly wrinkled more or less transversely. Apertures 
regularly arranged, circular, occasionally polygonal, margined by a circle of from twelve to 
fourteen small, closely-packed tubercles, which generally fill up the interspaces. 
“Tt is a scarce fossil, having only occurred to me once in the Shell Limestone at 
Humbleton Hill Quarry.” (Azzy, op. cit.) 
