71 
present two basal acrodromic, and besides, on either side, 4-5 camptodromic 
secondary veins. The leaf has some similarity to the leaves of Pop ulus ; but 
it might also belong to Ficus , or to the Sterculiacese. 
Locality and Horizon. — One-tree Point and Pipeclay Bluff, Carnelian 
Bay, Estuary of the Diver Derwent, Tasmania ; Upper Tertiary Leaf beds 
(sec It. M. Johnston, loc. cit., p. 14, &c.). 
Collection . — It. M. Johnston. 
PlIYLLITES FlClFORMIS, sp. 110 V. 
Johnston, Notes, etc., Papers and Proc. R. Soc. Tasmania, for 1881 [6th Plate], fig. 11. 
Obs. — The fossil shows one-half of a rather large fig-like leaf. It 
reveals a somewhat rigid texture. The margin is not preserved, but probably 
entire. The numerous secondary veins are camptodromic, and issue at slightly 
acute angles ; the tertiary veins proceed on both sides of the secondaries at 
acute angles, but on both sides of the midrib at right angles. 
Locality and Horizon. — With the preceding species. 
Phyllites juglandiformis, sp. nov. 
Johnston, Notes, etc., Papers and Proc. R. Soc. Tasmania, for 1881 [8th Plate], fig. 28. 
Obs. — The unequal sides indicate a leaflet. The texture appears to 
have been almost coriaceous. The form, supposing the missing apex to be 
restored, would be oblong ovate ; the margin entire. The midrib is very 
prominent ; the camptodromic secondary veins issue at slightly obtuse angles, 
5-7 on either side. The tertiary veins are short, inserted mostly at nearly 
right angles. The leaflet may belong to Juylans, with the leaflets of which 
it has most similarity ; but the Sapindacese, the Meliacese, and even the 
Papilionacetc and the Caesalpineae are, however, not excluded. It might have 
been possible to decide this if a little more of the reticulation had been 
visible. 
Locality and Horizon. — With the preceding species. 
Phyllites ligustroides, sp. nov. 
Johnston, Notes, etc., Papers and Proc. R. Soc. Tasmania, for 1881 [8tli Plate], fig. 22. 
Obs. — A leaf of delicate, more membranous texture, more oblong 
form, and entire margin. The base is acuminate, shortly petiolate, the apex 
