from the Red Crag. 359 
I here subjoin a list of all the species of Mammalia known to 
occur in the Red Crag. 
TERRESTRIAL. 
Ursus Arvernensis, Crotzet & Jobert. (Occurs also at Auvergne, 
South France.) 
Hyeena antiqua, Lankester. 
Felis pardoides, Owen. (Similar species at Epplesheim : Miocene.) 
Canis primigenius, Lankester. 
Pterodon, sp., Owen. 
Sus paleeochcerus, Kaup. (Occurs at Epplesheim.) 
Sus antiquus. (Ditto.) 
Equus, sp., Owen. 
Hipparion, sp., Owen. (Occurs at Epplesheim.) 
Mastodon angustidens, Owen. (Ditto.) 
Rhinoceros Schleiermacheri, Kaup. (Ditto.) 
Tapirus priscus, Kaup. ( Ditto.) 
Cervus dicranoceros, Kaup. (Ditto.) 
Megaceros, sp., Owen. 
Castor veterior, Lankester. 
Coryphodon, Hyracotherium, Paleeotherium. (Derived from Eocene 
strata.) 
MARINE *, 
Baleena definita, Owen. (Occurs also in Middle Crag of Antwerp.) 
emarginata, Owen. (Ditto.) 
affinis, Owen. (Ditto.) 
gibbosa, Owen. Ditto.) 
Balenodon physaloides, Owen. (Also at Antwerp.) [Several spe- 
cies, probably, are included under this name. | 
Belemnoziphius declivis, Owen. | 
planus, Owen. | 
angustus, Owen. 
angulatus, Owen. 
undatus, Owen. 
— gibbus, Owen. 
compressus, Hualey. 
Delphinus (Phoczena) uncidens, Lankester. 
orcoides, Lankester. 
see homeeyn leis and Belemnoziphius 
occur also at Antwerp. 
It will be observed, as a noticeable feature in these two lists, 
that the Mammalia in the former all have their analogues and 
representatives 11 Miocene + or early Pliocene strata, whilst 
those of the latter are met with elsewhere in later Pliocene strata. 
This, when taken into consideration with the worn and sea- 
rolled nature of the dental remains and with certain facts de- 
ducible from the study of the Mollusca of the Suffolk and Ant- 
* This part of the list is necessarily very imperfect; but the author 
hopes soon to be able to enlarge and correct it considerably. 
t+ Thefragments of Coryphodon, &c., of course, form an exception to this. 
