TRANSACTIONS OF WAGNER 



TERTIARY FAUNA OF FLORIDA 



*Lithophaga (Myoforceps) aristata Dill- 

 wyn. 



*Lithophaga (Diberus) bisulcata Orbigny. 



Coralliophaga elegantula Dall. 



Crassatellites deformis Heilprin. 



Cyrena pompholyx Dall, also C. 



Villorita floridana Dall, C. 



Venericardia serricosta Heilprin, also C. 



Cardita (Carditamera) tegea Dall. 



Chama chipolana Dall. 



Chama tampaensis Dall. 



Codakia sp., also Chipolan. 



Myrtsea vermiculata Dall. 



Phacoides domingensis Dall. 



Phacoides (Here) wacissanus Dall, also 

 Wacissa, Florida. 



Phacoides (Cavilucina) recurrens Dall. 



Phacoides (Lucinisca) calhounensis Dall. 



Phacoides (Miltha) hillsboroensis Heil- 

 prin. 



Diplodonta alta Dall. 



Cardium (Trachycardium) delphicum Dall. 



Cardium (Trachycardium) bowdenense 

 Dall. 



Cardium (Trachycardium), two sp. indet. 



Cardium (Cerastoderma) phlyctaena Dall. 



Cardium (Cerastoderma) taphrium? Dall. 

 Cardium (Trigoniocardia) alicula Dall. 

 Dosinia chipolana Dall. 

 Macrocallista acuminata Dall. 

 Callocardia (Agriopoma) sincera Dall. 

 Cytherea tarquinia Dall. 

 Cytherea (Artena) glyptoconcha Dall. 

 Cytherea (Artena) Shepardi Dall. 

 Chione (Lirophora) ballista Dall. 

 Chione (Chamelea) nuciformis Heilprin. 

 Chione (Chamelea) spada Dall. 

 Chione (Chamelea) rhodia Dall. 

 Anomalocardia floridana Conrad. 

 Venus halidona Dall. 

 Tellina segregata Dall. 

 Tellina merula Dall. 

 Tellina (Merisca) halidona Dall. 

 Macoma irma Dall. 

 Semele silicata Dall. 

 Corbula (Cuneocorbula) Burnsii Dall. 

 Corbula sarda Dall. 

 Panopea Whitfieldi Dall. 

 Gastrochsena (ovata Sowerby var. ?) ro- 

 tunda Dall. 



Orbitolites complanatus Lamarck. 



WHITE BEACH, LITTLE SARASOTA BAY. 



This formation is at the water's edge, near the northern end of the bay, 

 and is partly covered at high water. It is a coarse, calcareous rock, in which 

 the shells are represented by molds in the rock or by calcareous pseudomorphs 

 which have filled these molds after the latter had been more or less distorted, 

 and from which the surrounding limerock has been weathered away after 

 the formation of the pseudomorph. The body of the rock contains nothing 

 but molds; the surface, when subject to percolation, alone exhibits the pseudo- 

 morphs. The original rock seems to have been a coquina without any silicious 

 sand in it, which became a yellowish limestone which was then somewhat 

 crushed and near the surface infiltrated. There are traces of an unusual quan- 

 tity of polyzoa, corallines, wormtubes, etc., which seem to have grown over 



