roimdedly obtuse. The venation is caniptodromic. Prom a rather fine midrib 
issue on each side five line simple secondary veins. Of tertiary veins and 
the reticulation, nothing has been preserved. The fossil appears to belong 
either to the Oleacem (LigmtrumJ or the Daphnoidae (Daphne) . It has, 
however, the greatest similarity with the leaves of Licjustrum. 
Locality and Horizon. — With the preceding species. 
Phyllites pyriformis, sp. nor. 
Johnston, Notes, etc., Papers and Froc. R. Soc. Tasmania, for 1881 [8th Plate], fig. 23. 
Ohs. — A broadly elliptical, entire, shortly petiolate leaf of apparently 
delicate texture, slightly acuminate at the base, but more acuminate towards 
the apex, which is somewhat injured. The venation is caniptodromic, the 
few secondary veins ascending, bifurcating towards their ends, and forming 
apparently small loops at the margin. The tertiary veins are too imperfectly 
preserved to furnish a character. As far as it is possible to judge from the 
unmistakable characters present, the fossil appears to belong to the Pomacesc, 
where in Cydonia and Lyras similar forms of leaf occur. 
Locality and Horizon. — With the preceding species. 
Phyllites phaseolites, sp. nor. 
Johnston, Notes, etc., Papers and Proc. R. Soc. Tasmania, for 1881 [6th Plate], fig. 4. 
Ohs . — A small leaf, whose inequilateral development suggests a leaf- 
let. It has an almost cordate form, a comparatively long pctiolule and an 
apparently caniptodromic venation. The margin is very indistinct. Suppos- 
ing the margin to be entire, the leaflet should belong to the Phaseolctc, where, 
namely, species of Kennedy a t show very similar leaflets. 
Locality and Horizon. — With the preceding species. 
Phyllites sopiior^sformis, sp. nor. 
Johnston, Notes, etc., Papers and Proc. R. Soc., Tasmania, for 1881 [6th Plate], fig. 9. 
Ohs. — This fossil likewise appears to lie a leaflet of one of the Papilio- 
nacete. It reveals a thinner texture, is elliptical, asymmetrical in its two 
