226 
Casts of brachiopods, indet.—343-345, 347 - 35 °> 35 2 355 - 
Crustacean fragments, indet.—348, 352. 
No identifiable fossils.—351. 
Age, Silurian (probably Yeringian). 
Fossiliferous Sandstone. First Gully E. of Argyle Mine, Jordan 
Mine.—Nos. 356-358. Coll, by Mr. 0 . A. L. Whitelaw. 
Brachiopod fragments, indet.—356, 357 = 
Fossil remains, indet.—358. 
Rock of shallow-water origin, showing distinct cross-bedding. 
Age, Silurian (probably Yeringian). 
Fossilif erous Shale. Spur between Jordan River and B. B. Creek. —- 
Nos. 359-377. Coll, by Mr. 0 . A. L. Whitelaw. 
Panenka gippslandica , McCoy sp.—375-377. 
Panenka sp. ( ? P. gippslandica , juv.).—360, 371, 377. 
( 7 )Paracardumi. —367, 370, 377. 
Actinopteria sp.—359, 364. 
A pelecypod, indet. 
Tentaculites matlockie?isis , Chap.—361, 364. 
Styliola pissurella, J. Hall, var. multistriata , Chapm.—361, 363, 364,, 
368, 371. 
( })Orthoceras. —369. 
Ceratiocaris sp. ; carapace and caudal appendages.—372, 373. 
Ceratiocaris body segments.—361, 366, 371. 
Crustacean carapace, cf. Ceratiocaris .—365. 
(P)Tracks of Ceratiocaris. —374. 
Indet.—362. 
Nos. 359, 370, 373, 375, 377 retained for further examination. 
The littoral conditions under which these ochreous and banded shales 
were deposited are clearly indicated by the presence of true ripple-mark^ 
and numerous tracks in all probability due to Crustacea. 
Shales and Limestone. Thomson River, Walhalla, &c. Quarter 
Sheet 22 S.W. 
Near N. Boundary, Thomson River. {Monograptus dubius beds).— 
Nos. 378-392. 
Haliserites ■ Dechenianus , Goppert sp. (See Appendix).—378, 379, 
figvd. specs. 390 and 391. 
Ceratiocaris sp. (appendages).—386, 387. 
Ceratiocaris cf. salteriana , Jones and Woodward. (See Appendix).— 
380 (retained for comparison). 
Fossil remains, indet.—381, 382, 384, 385, 389, 392. 
Fossiliferous Sandstone, Limestone, Mudstone, and Cherry Rocks. 
Thomson River, Aberfeldy Divide.—Nos. 393-407, 410-451. Collected 
by Messrs. A. A. Henderson and J. P. L. Kenny. 
( })Cyathophyllmn. —414. 
( ?)Cydthophyllum , cf. truncatum , Linn. sp.—410 (retained for com¬ 
parison). 
