FOSSIL VASCULAR CRYPTOGAMS 



129 



measures. Very little is known of their stem, which appears, however, 

 to have resembled that of the Calamariese. 



More doubt rests on the affinity with the Equisetaceae of the group 

 of Sphexophylle.e. The remains of Sphenophylluin (Brongn.) are 

 found in abundance in the Carboniferous formation, but do not come 

 down to more recent times 

 than the Lower Permian. 

 The stem is divided into 

 distinct nodes and inter- 

 nodes, the latter usually 

 marked with conspicuous 

 ridges and furrows, which 

 are not alternate in adja- 

 cent internodes, but pass 

 continuously throuu;h the 

 nodes. At the swollen 

 nodes are whorls of leaves, 

 with occasional axillary 

 branches. Each whorl ap- 

 pears to consist always of 

 six leaves or of some mul- 

 tiple of six. They are ses- 

 sile, and obcuneate from a 

 narrow base, sometimes 

 denticulate and bifid at the 

 apex, but are not in any 



Each leaf 

 contains a number of 

 simple or dichotomous 

 'vascular' bundles. In 

 the centre of the stem is 

 a triangular bundle com- 

 posed of scalariform tra- 

 cheides, to which some 

 authorities add spiral tra- 

 cheides and others with 

 bordered pits ; the bundle passes through the node without material 

 change. This is often surrounded by some layers of secondary wood ; 

 the greater part of the stem, on transverse section, is occupied by a 

 small-celled parenchyme. 



The fructification of Sphenophyllum consists of cylindrical cone- 

 like spikes resembling those of Calamites. It is composed of whorls 



degree connate 



Fig. ioi. — i, 2, Fructification and branch of Asterophyl- 

 lites; 3, 4, fructification and branch oi Anmdaria; 5, 

 6, fructification and branch of Sphenophyllum. (After 

 Carruthers.) 



