17 
4. Eavosites mtjltipora ? Lonsdale. 
Favosites milUipora^ Lonsdale, 1839, in Murchison’s Silurian System, p. G83, pi. 15 Us, fig. 5- 
,, „ Milne Edwards and J. Haime, 1852, Mon. Brit. Boss. Corals, pi. 258, 
pi. 60, fig. 1. 
The calices in this coral are almost equal to one another, and are 
fairly regularly arranged in the form of slightly elongated hexagons about a 
millimetre in diameter. 
Horizon and Localities . — I am not quite certain that the single 
specimen from Burrawang submitted to me, and which I refer to this species, 
really belongs to it ; however, I am acquainted with none other to which it 
approaches more closely. 
6. Eavosites fibeosa, Goldfass. 
Calamopora fibrosa, 'Ndx.tuberoso-ramosa, Goldfuss, 1829, Pretref. Germ., I, p. 82, 
pi. 28, fig. 3rt, 2>b {cmt. excl.) 
A-lveolites fibrosa, Lonsdale, 1839, in Murchison’s Silurian System, p. 68, pi. 15 bis, fig. 1, 
and 15 bis, fig. 6. 
Favosites fbrosus, Milne Edwards and J. Haime, 1853, Mon. Brit. Eoss. Corals, p. 297, pi. 
6, fig. 5. 
Stenopora fibrosa, Salter, 1859, in Murchison’s Siluria, p. 534, pi. 40, fig. 6, and pi. 41, fig. 1. 
Coral cylindrical, pyriform, or composed of several branches, either 
isolated or adjacent. Corallites radiating from the centre towards the sur- 
face, straight or slightly curved ; tabulae close together, with a series of 
mural pores on the angles of the corallites. Diameter of the calices averaging 
half a millimetre. 
Horizon and Localities. to Milne Edwards and Haime 
this species occurs in the Lower and Upper Silurian and in the Lower 
Devonian. A single specimen has been collected in a greyish limestone at 
Limekilns, between Wattle Elat and Bathurst. 
