12 ART. i'. M. YOKOYAMA. 



l)e tolerably niiinerous. The species, however, \Yhich I have been 

 able to distinguish luunber only three, viz. : 



1. ConiopterU nitidula x. sp. 



2. Glossozamiies Hoheneggeri (Schenk). 



3. Podozamites lanceolatus (Lindl. et Hutt.). 

 Glossozamiies Hoheneggeri is a species hitherto found only 



in the Wernsdorf beds of the Northern Carpathians ; while 

 Co7iio2yteris nitidula, although new, shows a great affinity to 

 C. Cordai (Schenk) of the German Wealden, Podozamites lan- 

 ceolatus is a form ran^in«; from Khœtic to Cenomanian. Therefore 

 it is fairly certain, that we have here a formation which corres- 

 ponds to the Neocomian of Europe. 



b. Sha-chi-miao, Ho-Chou.^^ 



This place is situated to the east of Ching-tu-Fu, and in 

 the midst of the Mesozoic Busin. The plants are imbedded in 

 a light grey cleavablu shale, associated with the coal-layers of 

 the district. The specimens belong to the following three 

 species : — 



1. Gladophlebis sr. 



2. Glossozamiies Hoheneggeri (Schenk). 



3. Glossozamiies aciiminatus n. sp. 



A glance at these forms immediately suggests the same 

 formation as at Shi-kuan-tzu, especially as the genus Glossozamiies 

 occurs mostly in the Lower Cretaceous. 



1) ^'}Wâ>mm- 



