302 



Annals of the South African Museiim. 



1884. Eriphyla lenticularis, Holzapfel, Zeitschr. d. deutsch. geol. 



Gesellsch., vol. xxxvi., p. 458, pi. vi., figs. 1, 2. 



1885. Dozyia lenticularis, J. Bohm, Verhandl. d. nat. Verein. d. 



preussisch. Eheinl., vol. xlii., p. 126. 



1888. Astartc {Eriphyla) lenticularis, G. Miiller, Jahrb. d. k. preus- 



sisch. geol. Landesanst. fiir 1887, p. 424. 



1889. Eriphyla lenticularis, Fritscb, Stud, im Gebiete der bohm. 



Kreideformat. iv. Teplitzer Schicht. p. 78. 

 1889. Eriphyla lenticularis, Holzapfel, Die Mollusk. Aachen. Kreide 



(Palseontographica, vol. xxxv.), p. 195, pi. xiv., figs. 5-7. 

 1891. Lucina lenticularis, Langenhahn and Grundy, Das Kieslings- 



walder Gestein und seine Versteinerungen, p. 11, pi. iii., 



fig. 21. 



1893. Erijjhyla lenticularis, Fritsch, Stud, im Gebiete der bohm. 



Kreideformat. v. Priesener Schicht., p. 91. 



1894. Eriphyla lenticularis, Lundgren, Mollusk-faunan i Mamillatus 



och Mucronata zonerna (K. Svenska Vet.-Akad. Hand!., 

 N. F. xxvi., No. 6), p. 48. 



1897. Eriphyla leiiticularis , Fritsch, Stud, im Gebiete der bohm. 



Kriedeformat. vi., Chlomek. Schicht., p. 55. 



1898. Eriphyla lenticularis, G. Miiller, Mollusk. d. Untersenon v. 



Braunschweig u. Ilsede, p. 56, pi. viii., fig. 3. 



1900. Eriphyla lenticularis, Gagel and Kaunhowan, Jahrb. d. k. 



preussisch. geol. Landesanst. fiir 1899, p. 232. 



1901. Eriphyla lenticularis, Sturm, Jahrb. d. k. preussisch. geol. 



Landesanst. fiir 1900, vol. xxi., p. 76, pi. vi., fig. 6. 

 1904. Eriphyla lenticularis, Etheridge, Second Eeport Geol. Survey 

 Natal and Zululand, p. 79, pi. i., figs. 20, 21. 



Bemarks. — There are three examples of Astarte {Eriphyla) lenticu- 

 laris — two belonging to the Survey Collection and one to the Ham- 

 burg Museum. The latter shows the hinge clearly. This species 

 has been recognised by Etheridge from Umkwelane Hill (Zululand), 

 and by Stohczka from the Trichinopoli Group of Southern India. 

 It occurs in the Senonian and Turonian of various parts of Europe, 

 as may be seen from the references given above. The type came 

 from the Aachen Greensand, 



