114 Geological Society. 



withstanding defects the skull belongs to a most interesting 

 Anomodont, indicating a new family of fossil lieptilia. 



The skull is fully described in the paper, and its relationships 

 are discussed. The Author has already given reasons for regarding 

 JElurosaurus felinus, Lycosaurus curvimola, and their allies as 

 referable to a suborder Oennetotheria, which is nearly related appa- 

 rently to the Pehjcosauria, and lies midway between the typical 

 Theriodontia and the Dicynodontia. It is to this suborder that 

 Delphinognathus may be referred, though it forms a family-type 

 distinct from the yElurosauridte, distinguished by the conical 

 parietal with a large foramen, the anterior supra-condylar notch in 

 the squamosal bone, and other modifications of the skull and 

 teeth. 



2. "On Further Evidence of EndotJiiodon hatliystoma (Owen) 

 from Oude Kloof, in the Nieuwveldt Mountains, Cape Colony." By 

 Prof. H. G. Seeley, F.R.S., F.G.S. 



Two bones found by Mr. T. Bain at Oude Kloof consist of the 

 left ramus of the mandible and what the Author regards as the left 

 squamosal bone of E. hathystoma. The small cranial fragment pre- 

 served shows that the cerebral region probably conformed to the type 

 of skull seen in some of the Dicynodonts. 



A description of the remains is given, and the Author notices 

 that the form of the articular condyle indicates a difference from 

 Dicynodontia and all other Anomodontia hitherto described ; it 

 implies an oblique forward inclination of the quadrate bone — a 

 character important in defining the suborder Endolhiodontia. All 

 the characters of the dentition of the animal suggest near affinity 

 wath the Theriodontia, especially the long lanceolate teeth strongly 

 serrated. 



3. " On the Discovery of Mammoth and other Remains in 

 Endsleigh Street, and on Sections exposed in Endsleigh Gardens, 

 Gordon Street, Gordon Square, and Tavistock Square, N.W." By 

 Henry Hicks, M.D., F.E..S., Secretary of the Geological Society. 



In this paper the Author gives a description of the deposits over- 

 lying the loam in which the remains of the Mammoth and other 

 animals were found in Endsleigh Street, N.W. Under about 6 feet 

 of made ground there was about 10 feet of a yellowish-brown clay 

 containing flints and much ' race.' Below the clay there was 

 about 5 feet of sand and gravel, and under this about 1 foot of 

 clayey loam, in which most of the bones were embedded. This 

 loam contained many seeds, recognized by Mr. Clement Reid, 

 F.G.S., as being those of plants usually found in marshy places or 

 ponds and having a range at present from the Arctic Circle to the 

 South of Europe. A list of the bones found is given by Mr. E. T. 

 Newton, F.G.S., of the Museum of Practical Geology, Jermyn 

 Street, who describes them as being those of one full-grown 



