44 AET. S. — H. YABE. 



The Japanese species is so much Uke E. Burchardi Schenk 

 from the European Wealden formation, that there is a doubt 

 that they are really different plants. However, their identity 

 being not yet fully verified, tlie above name has been here 

 adopted. 



GENERAL REMARKS AND CONCLUSIONS. 



Constitution of the fossil flora ' — Though sufficient material 

 has not yet been collected to warrant an exhaustive discussion of 

 the fossil flora, yet there are some points of importance with 

 regard to the geological age of the Naktong series and its floral 

 constitution, which call for a brief statement in this place. In- 

 deed, the geological importance of these fossils lies in the cir- 

 cumstance that they are derived from the base of a very thick 

 complex which affords no other reliable organic remains for de- 

 termining its geological age. 



As will be seen from the above description, the writer was 

 enabled to distinguish the following twenty-one species of plants, 

 of which 3 are new, and 7 of doubtful affinity. 



Diciyozamites falcatits (Moeris) common. 



Nilssonia orienialU He. abundant. 



N. sp. rare. 



Diooniies (?) sp. rare. 



Clenophyllum (?) sp. rare. 



Podozmnites Reinii Geylee rare. 



