110 CATALOGUE OP FOSSIL PLANTS 



KNOREIA, Sternberg. 



Knorria Volkmannianum (Sternberg, sp.) 



Type — Lepidodendron Yolkmannianum, Sternb.,Vers.I, 



pi. 53, f. 3. 



Stem. 



Lepidolepis imbricata, Sternb., Yers. I., pi. 27. 



Knorria ,, Sternb., Yers I., pi. 38. 



,, Selloni, Sternb., Yers., pi. 57. 



,, ,, L. etH., Foss. Mora, pi 97. 



,, ,, Boulay, Terr. Houill. JSTord 



France, pi. 4, f.3, 3 bis 

 Lepidodendron Volkmannianum, Stur, Culm Flora, Heft II., 



taf.l8,f.4; taf.23, 

 f. 2, 4, 5, only. 

 Sagenana Volkmanniana, Sternb., Yers. II., t. 68, f. 8. 



,, affinis, Sternb., Yers. II., t. 68, f. 9. 



Lepidodendron Volkmannianum, Brongt., Prod., p. 85. 



Foliage. 



Lepidodendron longifolium, L. etH., Foss. Flora, pi. 161. 

 ? ,, dichotoma, Sternb., Yers. I., pi. 3. 



Sagenaria ,, Geinitz, Yers. Steinkf. Sachs., 



pi. 3, f. 1. 



220. — Knorria Sellonii, L. et H Type specimen, F. F., pi. 97. 



Hutton's label, " Felling, L. M.," is attached to this specimen. 

 There is no generic or specific name, merely the above, and it 

 was found among the numerous unarranged specimens. It is 

 so badly figured in plate 97 that one might be inclined to 

 doubt the identity of the specimen with the plate 97, but the 

 number of rows of scars is the same on each, and there are 

 other unmistakable evidences that the drawing has been made 

 from this specimen, although the drawing is inverted and the 

 shading of the leaf scars erroneous. It would seem that the 

 drawing only was sent to Lindley and that he has described 

 from it, otherwise he would not have said, p. 42, " The place 

 of the processes is occupied by flattened projections, broke at 

 their ends, and marked by a very shallow furrow which passes 

 from the point downwards, losing itself on the surface of the 

 stem." Iu the specimen, instead of a very shallow furrow, 

 there is a distinct ridge proceeding upwards three-eighths of 

 an inch till it is lost on the general surface, and two furrows, 

 one on each side of the ridge, deep at their origin near the 



