XVI FOSSIL ARCHEGONIATES 59i 



different in form from those of Lycopodiiim. The spores are 

 very pecuhar in having a sort of wing, suggesting the append- 

 ages of the pollen-spores of Pinits. 



It seems extremely probable that in some of the Palaeozoic 

 Lycopodinese seeds were developed. The fossil seed described 

 as Cardiocarpon has been shown to be borne upon a cone which 

 is almost identical with Lcpidostrobiis. 



PSILOTACE^ 



Certain fossil remains have been classed with the Psilotacese, 

 but there is much doubt as to the accuracy of these conclusions. 

 Solms-Laubach (2) says: 'The statements respecting fossil 

 remains of the family Psilotacese are few and uncertain, nor is 

 this surprising in such simple and slightly differentiated forms. 

 If Psilofites .... does really belong to this group, a point which 

 I am unable to determine from the figures, we should be able 

 to follow the type as far down as the period of the Coal- 

 measures." 



The genus PsUophyton, which has been found in the upper 

 Silurian, is regarded by Dawson as related to the Psilotacese, 

 but there seems to be much question about the accuracy of his 

 conclusions. 



