392 
Cydostrema homalon, Verco 
C. harriettce, Petterd 
Eulima 'pinguicula, Chapm. 
and Gabr. 
Pyramidella jonesiana, Tate 
sp. 
Turbonilla weeahensis, Chapm. 
and Gabriel 
Calyptreea kalimnce, Chapm. 
and Gabr. 
Natica subinfundibulum , Tate, 
var. crassa, Tate 
Rissoa gatlifjiana, Chapm. and 
Gabr. 
This is a Kalimnan species in the bore, 
and here recorded fossil for the first 
time. It has persisted to the present 
day, being found off the coasts of 
Victoria and South Australia. 
Also recorded fossil for the first time. 
Living on the coasts of Victoria and 
Tasmania. 
A Kalimnan fossil, quite distinct in 
specific characters, and showing a 
relationship to Eulima inflata, Tate 
and May, a form living off the coasts 
of Victoria and Tasmania. 
This species was described by Tate 
from Werrikooian specimens ob¬ 
tained from the Tintinarra bore, 
South Australia. It is here typically 
a Kalimnan fossil, although appear¬ 
ing to range a little above and below 
that horizon. 
This is a new and quite distinct form 
of the genus. 
A new form found in the borings both 
of the Mallee and the Gippsland 
Lakes, occurring in the Kalimnan 
series. In the former locality it 
probably commences at a slightly 
lower horizon. 
This is a gigantic example of the variety 
crassa, originally described by Tate 
from Muddy Creek, Beaumaris, and 
the Murray Cliffs. The present ex¬ 
ample has a length of 50 mm. against 
Tate’s example with 20 mm. 
A new Kalimnan species of quite dis¬ 
tinct characters. 
Rissoa ( Onoba) bassiana, Hed- 
ley 
Rissoa (0.) chrysalida, Chapm. 
and Gabr. 
Turritella pagodula, Tate. .. 
This species was previously known as 
a living form off Devonport, Tas¬ 
mania, and from Port Albert, Vic¬ 
toria. It occurs here as a fossil for 
the first time, in Kalimnan beds. 
A characteristic Kalimnan form. It 
was previously named in MS. by 
Mr. Dennant from Muddy Creek 
(upper beds), where it is a fairly 
common fossil. 
A distinctly Kalimnan shell. Pre¬ 
viously recorded from the Gippsland 
Lakes, Beaumaris and Horsham. 
It is absent from Muddy Creek (up¬ 
per beds). It is a fairly common 
fossil in the Mallee bores. The dis¬ 
tribution points to the partial isola¬ 
tion of the Hamilton area in Kalim¬ 
nan times. 
