224 PALEONTOLOGY OF OHIO. 



CORALS OF THE CLINTON FORMATION. 



Genus FAVOSITES, Lamarck, 1816. 

 (Hist. des. An. sans Vert., Vol. II., p. 204.) 



Favosites Gothlandica, Lamarck. 



Favosites Gothlandica, Lamarck; Hist, des An. sans Vert., Vol. II., p. 206. 



Favosites Gothlandica, DeFrance; Diet. Sc. Nat., Vol. XVI., p. 298. 



Favosites Oothlandica, Lamouroux; Encyl. (Zooph.), p. 338. 



Calamopwa Gothlandica, Goldfuss; Petref. Germ., Vol. I., p. 78, pi. 26, figs. So, 36, 3c, 



3c, and 3d. 

 Favosites Gothlandicus, Eichwald; Zool. Spec., Vol. I., p. 194. 

 Favosites reticulum ?, Ibid. ; p. 194, pi. 11, fig. 14. 



Calamopora Gothlandica (pars), Mowen ; Descr. Cor. in Belg. Eeport, p. 72. 

 Calamopora Gothlandica, Stephen Kiitorga ; Beitr. zur Geogr. and Palfiont. Dorpat's, 



p. 24, pi. 5, fig. 2. 

 Calamopora hasaltica, Hisinger; Leth. Succ, p. 96, pi. 27, fig. 5. 

 Calamopora Gothlandica, Eichwald ; Sil. Syst. in Esthland, p. 198. 

 Favosites sub-basaltica, D'Orbigny; Prodr. de PaWont., Vol. I., p. 49. 

 Favosites Gothlandica, McCoy ; Pal. Foss., p. 20. 

 Favosites Gothlandica, Milne Edwards and Jules Haime; Pol. Foss. des Terr. Palseoz., 



p. 232. 

 Favosites Niagarensis, Hall ; Pal. N. Y., Vol. II., p. 125, pi. 34, A {bis), fig. 4, and p. 



324, pi. 73, fig. 1. 

 Favosites Goldfussi, D'Orbigny ; Prodr. de PaMont, Vol. I., p. 107. 

 Favosites Goldfussi, Milne Edwards and J. Haime; Pol. Foss. des Terr. Palseoz., pi. 20, 



fig. 3. 

 Favosites Goldfussi, Edwards and Haime ; British Foss. Corals, pi. 47, figs. 3, 3c. 

 Favosites Gothlandica, Billings; Canadian Journ., 2d Ser., Vol. IV., p. 99. 

 Favosites Gothlandica, Nicholson; Can. Journ., 2d Ser., Vol. XIV., No. 1, p. 41. 

 Favosites GoiHandica,' Nicholson and Hinde; Can. Jour., 2d Ser., Vol. XIV., No. 2, 



1874. 

 Favosites Gothlandica, Nicholson ; Eeport on the Palseontology of Ontario, p. 45, 1874. 



(The above includes only the more important synonyms of this widely distributed 

 and variable species.) 



Corallum massive, forming spheroidal, pyriform, or more or less hemi- 

 spheric masses, which often attain a very large size. Corallites in gen- 

 eral markedly polygonal, and for the most part tolerably uniform in their 



