by L.F. Spath. 



53 



CONCLUSIONS. 



j Ammonoidea, described up to the present from 

 listed below and it will be seen that they mostly are 

 identical with forms that occur in the well-known 



(Campanian + Maestrichtian) deposits of the classical 

 t from those mentioned in the table, the Charente, 

 ie Cotentin of France, or Nagorzany in Poland, whence 



been described by Kner before the closely similar 

 deni, the commonest Pondoland Ammonite, was made 

 sy. Mr. Woods has drawn attention to the close 

 t exists between the Pondoland fauna and those of 

 d Valudayur groups of Southern India. The Kaye 

 sction in the British Museum, from the Valudayur 

 herry in Southern India, studied by Kossmat and 

 the Lower Campanian by Pervinquiere, includes, in 

 >es' types of Hauericeras rembda ( + dura a), which is 



