26 



Transactions. 



The beds dip N. 40° E. at an angle of 18°. As shown above, the nodular 

 band is in this locality again followed by greensands. In the lower layers 

 of the latter, for some distance above the junction, I obtained no fossils, 

 and possibly the species detailed here represent the horizon of band e in 

 the All Day Bay section, the lower unfossiliferous portion representing band d. 

 About 15 chains north-east of this locality a channel sunk for drainage pur- 

 poses reveals very fine glauconitic sand, and, although an area of only two 

 or three square yards has been exposed, I collected the following species : 

 MaUetia australis Q. & G., Nucula Jiartvigiana Phil., Pecten {Pseudamussium) 

 huttoni Park, Lima colorata Hutt., Liniopsis aurita (Brocchi), Venericardia 

 australis Lamk., Macrocallista assimiUs (Hutt.), CrassateUites ohesus A. Ad. 



This bed represents the Awamoa horizon, and the dip of the beds at 

 Three Roads is such as to take them beneath these beds. 



Analysis of Fossil Lists. 



I have to thank Dr. Thomson for drawing up the following table showing 

 the range of the various species within the Kakanui district. 



1. Tuffs, &c., below the Kakanui limestone (Lower Ototaran). 



2. Kakanui limestone (Upper Ototaran). 



3. Hutchinson Quarry beds of Kakanui district (Hutchinsonian). 



4. Awamoa beds of All Day Bay (see Marshall, 1915, p. 384) and Three 

 Roads (Awamoan). 



