380 PEOE. T. JEFFEET PAEKEli ON THE CEANTAL OSTEOLOGY, 



4. Emeus, species -y. 

 The cranium on a skeleton from Hamilton Swamp, named I), gravis by Prof. Hutton. 

 (Otago Univ. Mus.) 



This skull agrees in general characters with the present genus, but has right- 

 angled orbits — a character I have never observed in any of the preceding species. 

 Figured in outline, Plate LXI. figs. 34 & 40, and Plate LXII. fig. 58. 



3. A Comparative Account of the Skull in the Dinoenithid^. 



The skulls of the Moas are usually found in a more or less fragmentary condition, 

 and it will be advisable, for the sake of convenience, to take this circumstance into 

 consideration and to describe the skull under the following heads : — 



a. Cranium. 



b. Premaxilla. 



c. Maxillo-jugal arch, 



d. Vomer, palatine, and pterygoid. 



e. Quadrate. 

 /. Mandible. 

 g. Hyoid. 



The cranium is the part most commonly found • in large deposits of Moa-bones 

 crania may occur in hundreds, whilst other portions of the skull are of comparatively 

 rare occurrence. Premaxillse, quadrates, and lower jaws are not uncommon, while a 

 complete maxillo-jugal arch is rare, and very few skulls have been found with the 

 palatines, pterygoids, and vomer uninjured. 



a. The Cranium. 

 In the cranium the following regions may be distinguished : — 

 i. The occipital region, including the whole posterior portion of the skull ; it contains 

 the occipital condyles and foramen and is produced at the sides into the large 

 and prominent paroccipital processes, 

 ii. The cranial roof, continuous behind with the occipital region. 



iii. The lase of the slcull, also continuous behind with the occipital region ; posteriorly 

 it is raised into a prominent squarish elevation, the basitemporal jjlatform ; 

 anteriorly it is continued into a more or less cylindrical rod of bone, the 

 rostrum, which forms the axis of the beak, 

 iv. The lateral surface of the cranium, presenting three well-marked depressions — the 

 orbit in front ; the temi^oral fossa immediately behind the orbit and separated 

 fi-om it by a downward projection of the skull-roof, i\\e postorbital process ; and 

 the tympanic cavity, bounded above and separated from the temporal fossa by 

 an outstanding mass of bone, the squamosal prominence, and bounded behind 

 by the paroccipital process. 



