OOLITIC SEEIES. 75' 



Finusprimiem, L. & H. = Conites primesva (L. & H.). 



PI. cxxxv. 183-1. Near Towcester. 



Inferior Oolite. 

 Zamia pectinata, Erongu. = Williamsonia pecten (Phill.). 



PI. clxxii. 1835. Stonesfield Slate. 



Type - specimen iu the Oxford 



Museum. 

 Zamia taxina, Ij. & K. = W. pecten (PhiU.) . 



PI. clxxv. 1835. Stonesfield Slate. 

 Sphenopteris cysteoides, L. & H. = Sphenopteris, sp. ». 



PI. clxxTis. Stonesfield Slate. 

 Tteniopteris vittata, Brongn. = Tceniopteris vittata, Brongn. 



PI. clxxyii. Stonesfield Slate. 

 Carpolithes arnica, L. & H. = Carpolithes conicus, L. & H. 



PI. clxxxix. figs. 1, 2, 4. Coralline 



Oolite, Malton. Type - specimen 



(L. & H., fig. 4) iu the Manchester 



Museum, jSfo. 360. 

 Carpolithes £ticklancli, L. & H., ex 



"Will. MS. = Carpolithes eonieus, L. & H. 



PI. clxxxix. figs. 3, 5. Coralline 



Oolite, Malton. [A specimen in the 



Manchester Museum, No. 361, may 



possibly be the original of fig. 5.] 

 Carpolithes. = Carpolithes, sp., and Araiicarites, sp.. 



Pl. cxoiiia, figs. 1-4. Stonesfield 



Slate. 



In addition to the plants included in tte above list there are- 

 others described in more recent years, but we possess no systematic 

 account of Oolitic plants as a wbole. Mr. Carruthers has added 

 considerably to our knowledge of Jurassic plants by his numerous- 

 papers on Oolitic species from various localities, but reference is- 

 made to the work of this author under the head of the species 

 which he has described. 



In Damon's Qeology of Weymouth ' we find a few references to- 

 fossil plants from the Kimeridge Clay and other horizons. In 

 Strahan's Survey memoir allusion is made to the so-called 

 Kimeridge coal, a highly bituminous shaly substance from which 

 ' coal-money ' was formerly manufactured.^ Eeference should also 



1 Damon (84). 



'^ Strahan (98) ; see also Buokland & De la Beche (36), and an article in 

 the Gentleman's Magazine, vol. xxxviii. p. Ill, 1768. 



