258 THE SOOSOO 0V M. DE BORDA. 



tremely compressed, whilst that of this fossile is 

 broader than it is high. The teeth also are quite of 

 another form. Neither the level ahove the sea, nor 

 the relation of the specimen to the neighbouring 

 country, are rpporded in the source* whence we 

 have extracted tms truly interesting notice. 



