364 WILMORE : THORNTON, MARTOX AND BROUGHTON-IN-CRAVEN. 
There is the same general assemblage of fossils all along 
the series. The chief types, neglecting the crinoids and the 
polyzoa, are as follows : — 
Corals : — 
Syringopora ramulosa (Goldfuss). 
Syringopora sp., with smaller, close-set tubes, rather 
unequal^ spaced, very much like Vaughan's 
Syringopora cf. reticulata.'^ The tubes are slightly 
larger as a rule, but the grouping and the relation 
of the connecting tubes seem to be the same. 
Zaphrentis Omaliusi v^ar. densa (R. G. Carruthers), var. 
ambigua (R. G. Carruthers), and a new variety 
not named. 
Caninia cornucopice (Michelin), probably mutation d. 
Caninia sp. no v. 
Cyathaxonia Rushiana (Vaughan), and probably a new 
species of Cyathaxonia. 
Michelinia sp. ; the same form as at Rain Hall, Gill 
Rock, and Thornton. 
Brachiopods : — 
Rhipidomella Michelini (L'Eveille). This is very 
common and seems exactly the same as the Thorn- 
ton form. 
A thy r is cf. planosidcata (PhilL). 
Orthotetes crenistria. Apparently' the same as that from 
Rain Hall Plantation. 
Productus pustulosus (Phill.). 
P. semireticulatus (Mart.). 
P. margaritaceiis (PhilL). 
Chonetcs Hardrensis (Phill.). 
C. papilionacea (PhilL). 
The latter has a hinge line reaching to over four 
inches in length. The forms are much like 
Davidson's jfigure, PL XLVI., Fig. 3. 
Spirifer hisulcaius (Sow.). 
Rhynchonella pleurodon (PhilL). 
* Q.J.G.S., Vol. LXII. No. 246, Plate XXIX., and p. 313. 
