Eariy History of Lycopods 215 



also in the entire group, there is an evident relation to the Equisetales ; 

 hence it is of great interest that Nathorst has described, from the 

 Devonian of Bear Island in the Arctic regions, a new genus Pseudo- 

 bornia, consisting of large plants, remarkable for their highly com- 

 pound leaves which, when found detached, were taken for the fronds 

 of a Fern. The whorled arrangement of the leaves, and the habit 

 of the plant, suggest affinities either with the Equisetales or the 

 Sphenophyllales ; Nathoi'st makes the genua the type of a new class, 

 the Pseudoborniales\ 



The available data, though still very fragmentary, certainly suggest 

 that both Equisetales and Sphenophyllales may have sprung from a 

 common stock having certain fern-like characters. On the other hand 

 the Sphenophylls, and especially the peculiar genus Cheirostrobus, 

 have in their anatomy a good deal in common with the Lycopods, 

 and of late years they have been regarded as the derivatives of 

 a stock common to that class and the Equisetales. At any rate the 

 characters of the Sphenophyllales and of the new group Pseudo- 

 borniales suggest the existence, at a very early period, of a synthetic 

 race of plants, combining the characters of various phyla of the Vascular 

 Cryptogams. It may further be mentioned that the Psilotaceae, an 

 isolated epiphytic family hitherto referred to the Lycopods, have 

 been regarded by several recent authors as the last survivors of the 

 Sphenophyllales, which they resemble both in their anatomy and in 

 the position of their sporangia. 



The Lycopods, so far as their early history is known, are remark- 

 able rather for their high development in Palaeozoic times than for 

 any indications of a more primitive ancestry. In the recent Flora, 

 two of the four living genera^ (Selaginella and Isoetes) have spores 

 of two kinds, M'hile the other two (Lycopodium and Phylloglossum) 

 are homosporous. Curiously enough, no certain instance of a homo- 

 sporous Palaeozoic Lycopod has yet been discovered, though Mell- 

 prcserved fructifications are numerous. Wherever the facts have 

 been definitely ascertained, we find two kinds of spore, differentiated 

 quite as sharply as in any living members of the group. Some of 

 the Palaeozoic Lycopods, in fact, went further, and produced bodies 

 of the nature of seeds, some of which were actually regarded, for 

 many years, as the seeds of Gymnosperms. This specially advanced 

 form of fructification goes back at least as far as the Lower Carboni- 

 ferous, while the oldest known genus of Lycopods, Bothrodendron, 

 which is found in the Devonian, though not seed-bearing, was typically 

 heterosporous, if we may judge from the Coal-measure species. No 



1 A. G. Nathorst, " Zur Oberdevonischcn Flora der Baren-Infiel," Koiigl. Svenska 

 Vttensknps-Akademieiig Handlingar, Bd. 36, No. 3, Stockholm, 1902. 



2 Excluding Psilotaceae. 



