224 PALEONTOLOGY OF OHIO. 



CORALS OF THE CLINTON FORMATION. 



Genus FAVOSITES, Lamarck, 1816. 

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



Favosites Gothlandica, Lamarck. 



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



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



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



Calamopora Gothlandica, Goldfuss; Petref. Germ., Vol. I., p. 78, pi. 20, figs. 3a, 35, 3c, 



3c, and 3d. 

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

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



Calamopora Gothlandica (pars), Mowen ; Descr. Cor. i;Q Belg. Report, p. 72. 

 Calamopora Gothlandica, Stephen Kutorga; Beitr. zur Geogr. and Paleont. Dorpat's, 



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

 Calamopora basaltica, 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 Paleont., Vol. I., p. 49. 

 i^awsJtes (?o</i?rtridica, 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. 

 Favo^tes Goldfussi, D'Orbigny; Prodr. de Paleont, 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., A^ol. XIV., No. 1, p. 41. 

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



1874. 

 Favosites Gothlandica, Nicholson ; Report on the Palaeontology 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 



