N0j 2- ] PAL^O-GEOGRAPHICAL REMARKS. 145 



against Neumayr. I would not even attach too great importance to the 

 report of the existence of hastate Belemnites far up in the north. Nor does 

 the fauna of the Callovian of Cape Flora as yet bring any new material 

 which might turn the balance in favour of Neumayr's advocates or of his 

 opponents. 



If new collections in the region of Cape Flora should prove that the 

 Bajocian in this locality really contains a fauna of decided Central-European 

 character, the region of the Jura of Cape Flora would then supply the most 

 weighty argument for the incorrectness of Neumayr's theory. 



19 



