1484 



TRANSACTIONS OF WAGNER 



TERTIARY FAUNA OF FLORIDA 



end hardly rostrate ; hinge normal, basal margins finely crenate ; adductor 

 scars slightly raised. Length 18.0, height 15.2, diameter 8.0 mm. 



The nepionic shell in this species is smaller and smoother and the ribbing 

 of the disk less coarse than in the other species. The rostration, which is so 

 marked a feature in L. tellinoides, is not found in this or the lower Eocene 

 species. 



Lirodiscus protractus O. Meyer. 

 Plate 43, Figure 3. 



Astarte protracta O. Meyer, Bull. Ala. Geol. Survey, i., p. 80, pi. iii., figs. 18, i8a. 1886; 

 Dall, Trans. Wagner Inst., iii., p. 1199, 1900. 



Astarte smithvillensis (var. mediavia) Harris, Bull. Am. Pal., i., No. 4, p. 61, pi. v., fig. 4, 

 1896; not Harris, Proc. Acad. Nat. Sci. for 1895, p. 48, pi. i., figs. 8, 9, 1895. 



f Astarte subpontis Harris, Bull. Am. Pal., i.. No. 4, p. 62, pi. v., figs. 5a-b, 1896; upper- 

 most midwayan Eocene. 



Upper bed at Enterprise, Mississippi, lower Claibornian, O. Meyer; Na- 

 heola Landing, Tombigbee River, and Mathews Landing, Alabama River, mid- 

 wayan Eocene, Harris. 



This form appears to be very mutable, and the consolidation above indicated 

 is suggested on the basis of specimens named by Professor Harris in the collec- 

 tion of the National Museum. 



The A. smithvillensis of Harris is said to be the A. Conradi Buckley, 1874, 

 not of Dana, " Manual of Geology," 1863. 



The genus Goodalliopsis De Raincotirt and Munier-Chalmas, 1863, which 

 is placed by Fischer in the Astartidw, should be transferred to the Erycinidw 

 (as a synonym of Kellia), as previously indicated by Cossmann. Bernayia 

 Cossmann, 1887, accidentally omitted from my review of the Leptonacea, 

 should also, from the figures, belong in the vicinity of Kellia. 



A careful examination of the type of Plesiastarte Fischer, 1887, leads to 

 the conclusion that Deshayes in referring it to the Cyrenidce had much justifica- 

 tion. It has none of the characteristics of the AstartidcB. On the other hand, 

 a little shell described by Gould from Japan, under the name of Gouldia dilecta, 

 has identically the same hinge characters, except that the lateral lamina is not 

 cross-striated. I suspect the latter to be the very young shell of some Venerid 

 allied to Meretrix. 



I have not been able to examine authentic specimens of the Mesozoic Prce- 

 conia Stoliczka, 1871, and Pachytypus Munier-Chalmas, 1887. Parisiella 

 Cossmann, 1887, from the Parisian Eocene, is also only known to me by 



