65-G6 



TABLE III. 



Comparison of 1*ermian and Mesozoic Stratigraphy and vSuccession of 

 Faunal Zones in New Zealand and New Caledonia. 



hieflv after Woods and Trechmann. 



Danian ? 



Foramiferal limestone with teeth 

 of Carcharod^n and Isurus 



Lyto- 



Kossinaliceras, BacuUtes 

 ceras ? Anisoceras ? 



GaudryceraSj Trigonia, C 

 thyra 

 ' Area" Cardium, Alaria 



Cimoliasaurus, Lelodon. 



Regression and minor unconformity 

 or conformity claimed here 



Ibian. (Local development only.) 



tlinidrii' >r(is sayca 

 T in illiii.s circumtoeniatus 

 1 H'" ' I'l III us concenticus 

 Liintt, Aucelliiia, Trigonia. 



Great Poat-Hokonui Orogeny and 

 intrusion of ultrabaaic, basic and 

 perhaps acid Plutonic rocks. 



Neocomian. 



Plant Beds — Awanui and F^ast 

 Coast Inoceramus beds pro- 

 bably extending down into 

 Jurassic rocks 

 TiUionian. 



Berriasella novo-zealandica, Streb- 

 lites, &c., with Inoceramus 

 concluding a conformable .series 

 of J urassic marine and fresh 

 water beds ranging down into 

 Bajoccian and Liassic strata. 

 (Details not yet available.) 

 Rh^lic. 



Arcestes cf. rheticus 



Meiitzelia, Clavigera lumida 



Spirijtrina diomeda 



H'foinonotis ochotica 

 (zcme locally missing) 



udumonotis rickmondiana (very 

 abundant) 



(zone locally mi.ssing) 



Mylilii.s prdiU maticuii (abuiul 



MMt) 



Uahbia .pp. 



Mifoiihoi-id Hugtjeien 



llulnnUn sp. Spirif,nna>]K 



Lfulino-Curnic. 

 Spiriferina cf. fragilis 

 Daonr.lla indica 



Middle and Lower t Triamic. 

 (Jreai thiikncss of unfossiliferou; 

 bed of whiclt the relation tc 

 the underlying formation is not 

 clear. Various authorities sug 

 gest that there is perfect con- 

 formity, or a minor or majoi 

 unconformity, the last involv 

 ing plutonic int 



Arinrlid beds. 



S,nnfna, I'hitu'o-hismu 



After Piroutet. 



Reg: 



and folduiii 



Senonian. 



Ko88inaticerafi, liaculiles, Lyto 



ceras. Anisoceras. 

 Gaudryceras, Trigonia. 



Arcfiy C'ardiunh Alaria. 



Regression of the strand and i 

 unconformity. 



Eocretaceou/i C»>al Measuros and 

 Marine Beds with E-ragyra. 



TiUionian. 



Berriasella cf. novo-zealandica. 

 Trifjonia, Alaria, Gasterojods. 



The majority of Upper Jurassic, 

 the Middle and Lower Jurassic, 

 and RhE'tic arc absent. 



Some orogenic movement o<'curred 

 and Tithonian rests with marked 

 unconformity on the None. 



Noric. 



J.'iscoj hyllitPM ef. debili'! 

 Pseudoinonotis sp. 

 Cepha'opods lihynchonrl'ii spp. 



Pseudomonoti.'irichmotuliiUKi{i\iiuni\- 



ant). 

 Spirigera, Spirijerina, &e. 



Fseudomowitis sp. and liatobiu ef. 

 rare, striate (zone locally missing). 



Hnlnbia hocftstetleri. H. aitstrinra 

 Further zonal subdivision proposed. 



(Nine sub-zones in all.) 

 Spirigera wreyi, Diftcophyllites 

 Arcestes^ various typcj*. 



Ilalobia ef. austriara 

 lialobia hochsletteri 

 Myophoria, OaMeropvds 

 Helzia, Halorflla, lihymhimrlht, 

 Spiriferina 



My i H.- prMematiri's (abund- 

 ant ) 



Ilaloina zittcli, lialobia spp 



Myophoria. Halobia sp. 



Spiriferina cf. fragilii 

 Hhynrkonella sp. Tcnhnitnh sp. 



Middle Tria 

 Daonclla t 



'seudoinonttlis alT. pninkhnndana 

 Ophiceras, FlvmnnngHr.% Mcako- 

 ceras, Aspidites, Koninckites, 

 Danubites, Dorycraniics. 



Apha.n 

 Stnrhrn. 

 I'optinii 

 Wangt-n 



