﻿416 Revieivs — Australian Tertiary Geology and Fossils. 



Class CEUSTACEA. 



Subclass I. THOEACIPODA, H. Woodw. (or Mala- 

 costkaca). 

 Legion 1. PODOPHTHALMIA. 

 Order 1. Decapoda. 



Suborder (a) Beachyura 



„ (b) Anomura 



,, (c) Macrura 



Order 2. Stomapoda 



Legion 2. EDRIOPHTHALMIA. 



Order 3. Isopoda 



„ 4. TRILOBITA 



„ 5. AmpMpoda 



Subclass II. GNATHOPODA, H. Woodw. (or Ento- 

 mosthaca). 

 Legion 3. MEROSTOMATA. 



Order 6. Xiphosura, and Cyclus (?) 



„ 7. EURYPTERIBA 



Legion 4. BRANCHIOPODA. 



Order 8. Phyllopoda 



„ 9. Cladocera. 

 Legion 5. LOPHYROPODA. 



Order 10. Ostracoda 



,, 11. Copepoda. 

 Legion 6. ANCHORACEPHALA. 

 Order 12. EMzocepliala. 

 „ 13. Cirripedia. 



,, («) BALA-NIDiE 



„ {b) Lepadid^ 



Crustacean " Teeth," Eggs, and " Tracks" 



Genera. 



Species. 



Var. 



27 

 2 



22 

 2 



41 

 3 



52 

 4 





3 



51 



1 



3 

 304 



1 



18 



4 

 5 



16 



36 



4 



12 



55 



6 



55 



413 



41 



5 

 4 

 4 



18 



29 



4 



3 



197 



979 



72 



II. — 1. History of Australian Tertiary Geology. By the Eev. 

 J. E. Tenison-Woods, F.G.S., etc. — 2. Further Notes on 

 THE Tertiary Marine Beds op Table Cape, Tasmania, By 

 E. M. Johnston. — o. Notes on the Tertiary Fossils, Tas- 

 mania. By tlie Eev. J. E. T. Woods, F.G.S., etc. 

 (From the Papers and Proceedings of the R. Soc. Tasmania for 1876. Svo. pp. 



45. Hobart Town, 1876.) 



'N the first of the above papers the Eev. Mr. Woods, after a brief 

 notice of the chief works bearing on Australian Tertiary Geology, 

 passes to a consideration of some important questions arising therein. 

 For instance, he asks — Do the Tertiary formations of Australia ex- 

 hibit any sign of a persistence of the types common to the Secondary 

 formation of the continent? This question Mr. Woods tells us 

 may be answered in the negative. " Some of the Brachiopoda have 

 faint Secondary affinities, but the Echinodermata are certainly not 

 Mesozoic in character." The Secondary types in the Australian 

 Tertiary deposits are few and rare ; thej' may be summarized as 

 two species of Trigonia, both differing from existing forms, and a 

 Pleurotomaria} In other respects the resemblance between the 

 European and Australian Tertiary rocks is considerable, whilst there 



1 There are three Trigonice, viz. T. acuticostata, M'Coy; T. semiundiilatn, M'Coy ; 

 and T. Howitti, M'Coy. The first of these has recently been found living in Bass's 

 Straits. The Flmrotomaria referred to by Mr. Woods is F. Tertiaria, M'Coy. — 

 R. E., Jun. 



