96 WYNNE : GEOLOGY OF KTJTCH. [PART I. 



groupsj the beds with marine fossils and those with plants, together 

 form ' physically' one great continuous series. 



Hence, although the plant-laeis occupy a stratigraphical position, 

 perhaps actually newer than the European ' upper' Jurassic or possibly 

 synchronous with some portion of the succeeding formations, still it is, 

 on the evidence derived from this district, impossible to assert that they 

 are of this (?) cretaceous age. 



With regard to the tertiary fossils which have been collected, the 

 progress as yet made in their examination hardly warrants any asser- 

 tion as to the precise place of those sub-divisions which overlie the 

 Kutch Nummulitic group. 



( 96 ) 



