LOCALITIES OF IRISH CARBONIFEROUS FOSSILS. 
23 
Name. 
Authority. 
' 0. R. S. 
[ Cal. SI. 
j Limest. 
j Coal. 
Localities. 
’ Other 
localities. 
ZOOPHYTA— continued. 
Fenestella frutex. 
M‘C. xxviii. 10. 
Killymeal. 
hemispherica. 
M‘C. xxix. 4. 
» 
* m 
MUlecent, Little Island. 
,, 
intertexta 
Port. T. 22. 3. 
* 
Benburb. 
laxa. 
Phil. P. F. 
* 
m 
Clonea, Belmore, Blacklion. 
membranacea a . 
Phil. G. Y. 
* 
m 
Bruckless, Cookstown. Millecent. 
4 
„ 
Morissii. 
M‘C. xxviii. 14. 
* 
m 
Carrowmably, Millecent, Little 
Island. 
multiporata. 
M‘C. xxviii. 9. * 
** 
* 
Carrowmably, Poulscadden, Mille¬ 
6 
cent. 
nodulosa a . 
Phil. G. Y. 
* 
Carrowmably, Rahoran, Blacklion. 
5 
,, 
oculata. 
M‘C. xxviii. 15. 
** 
Carrowmably, Ballinacourty. 
9? 
plebeia. 
M‘C. xxix. 3. 
** 
Malahide, Hook, Little Island. 
7 
r> 
polyporata a . 
Phil. G. Y. 
** 
* 
Lisnapaste, Carrowmably, Florence 
Court. 
quadradecimalis. 
M‘C. xxviii. 13. 
* 
* 
Carrowmably, Blacklion. 
tenuifila a . 
Phil. G. Y. 
* 
** 
Lisnapaste, Millecent, Little Island. 
,, 
undulata a . 
Phil. G. Y. 
* 
-i 
Malahide, St. Doulough’s, Carrowna- 
8 
nalt. 
varicosa. 
M‘C. xxviii. 8. 
* 
Blacklion. 
Hemitrypa Hibernica. 
Sco. MSS. xxix. 7. 
* 
Ballintrillick, Clare, Little Island. 
oculata. 
Phil. P. F. 
* 
Blacklion. 
Ichthyorachis Newenhami. 
M‘C. xxix. 8. 
* 
Meelick. 
Polypora dendroides. 
M‘C. xxix. 9. 
* 
Killeshandra, Poulscadden, Hook. 
„ 
marginata. 
M‘C. xxix. 5. 
Killymeal, Blacklion. 
„ 
papillata. 
M‘C. xxix. 10. 
Killymeal, Blacklion, Rathgillen. 
,, verrucosa. 
M‘C. xxix. 6. 
* 
Blacklion. 
Retepora flustriformis. 
Phil. G. Y. 
* 
Florence Court. 
irregularis. 
Port. T. 22. 2. 
* 
* 
Florence Court, Hook Head. 
„ 
prisca. 
Gold. T. 36. 19. 
m 
Ballinacourty, in limestone. Hook 
Head. 
” 
undata. 
M‘C. xxix. 11. 
* 
** 
Lisnapaste, Millecent, Ballyduff. 
a Fenestella 
, was Retepora. 
In the foregoing Table, at page 11, there are five species of Do- 
labra enumerated, which were got at Cultra, in the soft yellow mag¬ 
nesian limestone. This limestone was formerly quarried here and 
carried to England for manufacturing purposes, and it was out of a 
few blocks of it that remain on the shore the imperfect casts were 
got which Mr. M‘Coy described, and which I believe he was told 
were carboniferous. Those casts do resemble the Cuculleae of the 
“ Palaeozoic fossils,” but I think they are Permian, or belonging to 
the Magnesian limestone. They are Doldbra angusta, D, complanata , 
D. Hardingii , D. trapezium , and D. unilateralis. 
