223 
T etragr aptus decipiens, T. S. Hall. Nos. 2342, 2343, 2346, 2350, 
-35 2 > 2 359> 2360 (?), 2362, 2363. 
The remainder are indeterminate. 
The horizon is Lancefieldian. The rocks are bright red in colour, 
and very hard. The specimens are poorly preserved, and it is almost 
impossible to clear them. 
From Bendigo. 
Garden Gully Line, 10 chains N. of Spring Gully Reservoir. Collected 
by Mr. S. Waters. Nos. 1485-1502. 
All the slabs contain specimens of Tetragraptus fruticosus, excepting 
No. 1491, which shows T. bryonoides. The only other species present 
which can be identified is Phyllograptus typus, which is very common. 
The beds are typical Bendigonian. 
(b) Carshalton Line, Lansell’s and Mundy’s Shaft.. Collected by Mr. 
S. Waters. Nos. 1503-1518. 
Clonograptus magnificus, Pritchard; is apparently present on Nos. 1503 
and 1518 (counterparts). 
Goniograptus ihureaui, McCoy. No. 1510. 
Tetragraptus serra. No. 1504. 
Most of the other slabs bear T. fruticosus, and a few show Phyllo¬ 
graptus sp. 
The beds are Bendigonian, and probably Clonograptus magnificus is 
indicative of a low horizon in the series. 
■(c) New Chum Line, Windmill Hill. Collected by Mr. H. S. Whitelaw. 
Nos. 1519-1538. 
Goniogr aptus macer. No. 1533. 
G. thureaui. Nos. 1519 (?), 1521, 1523, 1525, 1526, 1533, 1534. 
Dichograptus octobrac hiatus. Nos. 1520, 1527, 1530, 1533. 
Tetragraptus bryonoides. No. 1525. 
T. fruticosus. Nos. 1522, 1524, 1525, 1527, 1528, 1529, 1530, 1531, 
1 53 2 > i533> 1 535- 1536, i537> i53 8 - • 
T. pendens. Nos. 1519, 1527. 
Didymograptus extensus. Nos. 1521, 1525 (counterparts). 
All the species are typically Bendigonian. 
From Daylesford. Collected by Mr. W. Forbes. No. 1636. 
Phyllograptus sp. and Tetragraptus ? 
From Daylesford. 
(a) Jim Crow Creek, W. of Hepburn. Collected by Mr. W. Barag- 
wanaih, sen. Nos. 1676-1679. 
T etragr aptus fruticosus. Nos. 1676, 1679. 
T. pendens. 1676. 
Phyllograptus typus. No. 1676. 
Didymograptus bifidus. No. 1678. 
D. caduceus. No. 1678. 
D. extensus. No. 1678. 
No. 1677 i s indeterminate. 
Probably the extreme upper limit of the Bendigonian. 
