Klem — Revision of the Palaeozoic Palaeechinoidea. 71 



1874. Eocidaris Verneuiliana . Loveu, Konffl. Svens. Vet- 

 ens. Akad. Handl., Bd. 11, no. 7, p. 43. 



Spines perforated and placed on elevated bases. Basal 

 ring crenulated radiately. Plates have a concave depression, 

 surrounded by an elliptical border of small tubercles in a 

 single series. Two kinds of spines known — one, muricated 

 and the other, striated longitudinally. 



Geological formation and locality: Shell-Limestone, 

 Tunstall Hill and Humbleton Quarry. 



UNDETERMINED OR INSUFFICIENTLY DETERMINED SPECIES. 



1. Eocidaris drtdenensis Vanauxem. 



1842. Echinus drydenensis . Vanauxem, Rep. Third Geol. 



Dist., p. 184. 

 1867. Eocidaris Drydenensis. Hall, 20th Rep. State Cab. 



Nat. Hist. New York, p. 298. 

 1874. Eocidaris drydenensis. Loven, Kongl. Svens. Vetens. 



Akad. Handl., bd. 11, no. 7, p. 43. 

 1889. Eocidaris drydenensis. Miller, N. Amer. Geol. Pal., 



p. 242. 



1895. Archaeocidarisdrydeiiensis. Keyes, Proc. Iowa Acad. 

 Sci., vol. 2, p. 184. 



1896. Archaeocidaris drydenensis. Jackson, Bull. Geol. Soc. 

 Amer., vol. 7, p. 214. 



Geological formation and locality : Devonian, Chemung 

 Sandstone, Dryden, New York. 



2. Eocidaris scROBicuLATA Sandberger. 



Cidaris scrobiculata. Sandberger, Verst. Rhein. 



Schichtensystems, p. 382, pi. 35, fig. 3. 

 1858. Eocidaris scrobiculata. Desor, Syn., p. 157, tab. 21, 



fig. 17. 

 1862. Eocidaris scrobicidata. Dujardin et Hupe, Echinoder- 



mes, p. 467. 



