132 AUSTRALIAN TERTIARY POLYZOA. 
species as occurring in the Orakei Bay Greensand, viz., Cellepora 
Gambi , Mellicerita angustiloba, Busk, and makes man 
critical remarks on some of the other Australian forms, which 
will be referred to hereafter. 
So far as my acquaintance with the present subject goes, — 
appears to have again been a lapse of time before any furt 
the fossil organic remains of Vi ictoria, tana u - pelea 
e only Tertiary Polyzoa mentioned are Letepora 
same deposit of one of the Orakei Bay forms, Spiroparina ver- 
tebralis, Stoliezka. 
n the “ Monthly notices of Papers and Proceedings of the 
’ the same age 
as the Flemington series near Me . 
again referring to this Saeer reer “ Third Progress 
Report” for 1876, Mr. Smyth places the Stasrdl ferruginous bed 
on the horizon of the oldest gold drift (Lower Pliocene).? 
? Melbourne, ae pe. 35-36. . 
‘thd: Ls pp. 13- 
io 
_ 5 pp. 48, 71, and 81. Fossils were first found here by Mr. Bernard Smith 
in 1872, but it is due to the researches of my frien - _— former colleague, 
Mr. Norman 
oO Taylor, that we owe seco we 
covery at the Hetome R ush. (See his ‘‘ Report on ate Stawell Gold Field,’ 
yth’s “ Progress Report,” 1876, pp. 263-64.) 
: Le “i ytaet % pate 
zi ate er ce a Sas Lhe ia a) la 
Se ee es eas eS ee EE Ra eS ee 
I I oR Ie ais a oe ER Sn OD a 
