Vol. 58.] THE FOSSILIFEROUS SILURIAN BEDS OF KERRY. 245 
Horiostoma globosum, Schloth. Lichas sp. 
H, discors (4) Sow. Proetus sp. 
Encrinurus Stokesi, M‘Coy. Phacops sp. 
Lichas anglicus, Beyrich. Crinoidal ossicles. 
At the same horizon, on the north side of the Cove, we obtained 
Syringopora bifurcata, Lonsd., and Encrinurus sp. The occurrence 
of Stricklandinia lens and Pentamerus oblongus is strongly suggestive 
of a Llandovery age for these beds; but the general facies of the 
fauna is of Wenlock type. 
A third fossiliferous horizon occurs near the base of. the series at 
Coonakeel, yielding :-— 
Spirifer bijugosus, M‘Coy. Horiostoma discors, Sow. 
Orthis elegantula, Dalm. Encrinurus Stokesi, M‘Coy. 
O. hybrida, Sow. E.. punctatus (?) Brinn. 
O. basalis (2) Dalm. Phacops Downingie, Murch. 
Atrypa reticularis (Linn.). Crotalocrinus sp. 
Stricklandinia lirata, Sow. Orinoidal ossicles. 
Stropheodonta filosa, Sow. 
The beds of the third horizon appear at intervals along the southern 
coast of Doon Point, and near the extreme end have yielded :— 
Cyathophyllum sp. Horiostoma globosum, Schloth. 
Lindstremia Eee M‘Coy. | Proetus sp. 
Orthis calligramma, var. Davidsoni, Lichas sp. 
de Vern. Encrinurus Stokest, M‘Coy. 
Orthis sp. Crinoidal ossicles. 
Horiostoma discors, Sow. | 
C(10). This well-marked band of coarse conglomerate is first met 
with in the inlet known as Coonakeel, from which spot it can be 
Fi ig. 14.—Section through Ferriter’s Castle Cove. (For explanation 
of CY, ete. see pp. 240, 244, ete.) 
C (15) C (14) Oia C(ey Gases ae =O (9) 
C (11) C (10) 
[Horizontal scale: 1 inch=60 feet. ] 
followed almost continuously to the end of Doon Point. The 
existence of the point is, in fact, largely due to it. It contains 
pebbles of quartz, jasper, rhyolite, ash, diabase, purple sandstone, 
dark limestone, and fine conglomerate. Some of the pieces are 
as much as 12 inches long. 
Good sections through the beds from (C 10) to (C14) are seen in 
the little cove opposite Carriganeena, and in that south of the ruins 
s 2 
