by L. F. Spath. 



55 



aeneous deposits, now found to be fairly frequent, 

 riing against assuming contemporaneity of such diverse 

 3 as those here dealt with, and the three divisions of 

 and two zones of the Maestrichtian in Haug 1 probably 

 >art of the true succession of horizons. Equally great 

 orrelation, unfortunately, are experienced in other 

 ,s, e.g. Kilian & Reboul point out that Madrasites spp., 

 ugata, Gaudryceras varagurense and Tetragonites 

 r in the Upper Trichinopoly beds and that it was just 

 of species [all found in Pondoland] that characterised 



beds. They add "It follows from these comparisons 

 ious formations of the Islands Snow Hill and Seymour, 

 3tly correspond, by their faunistic characters, to the 

 -lato = Santonian-Maestrichtian) of the Trichinopoly 

 , with which they can be synchronised.'' 



added here that though the Pondoland Madrasites 

 semblance to the tuberculate Antarctic forms, they are 



