[WHITEAVES] PALLISER’S CRETACEOUS FOSSILS 109 
Natica (Lunatia) Moreauensis, Meek and Hayden. 1860, Zbid., vol. xii., p. 422. 
Lunatia concinna, Meek. 1876. Rep. U. S. Geol. Surv. Terr., vol. ix., p. 341, 
pl. 32, figs. 11 a, 6, c. 
éc cb Whiteaves. 1885. Contr. to Canad. Pal., vol. 1, pt. 1, p. 48. 
“Red Deer River, southwest of the Hand Hills, Dr. Hector, June, 
1859” : eleven specimens, each numbered 38, and evidently corresponding 
to that number on page 243 of Captain Palliser’s report. The specimens 
are either mere casts of the interior of the shell, or casts with part of the 
exfoliated test adherent thereto, so that their identity with J. concinna is 
not quite certain, though it is highly probable. 
BACULITES COMPRESSUS, Say. 
Baculites compressus, Say. 1821. Am. Journ. Sc. and Arts, vol. ii., p. 41; also of 
subsequent writers in the United States and Canada, 
EC 3 Etheridge. 1861. In Hector’s paper, Quart. Journ. Geol. Soc. 
Lond., vol. xvii., p. 415. 
eS oe Etheridge. 1863. No. 10 of the list on p. 242 of Capt. Pal 
liser’s Rep. 
Twenty-three specimens of Baculites in the collection, most of them 
mere fragments, are labelled “ No. 10, Baculites compressus, Elbow of 8. 
Saskatchewan.” Nineteen of these are fairly typical B. compressus, but 
three fragments appear to the writer to be probably referable to B. 
ovatus, though they are too waterworn to be identified with much cer- 
tainty. One specimen, a piece of a body-chamber nearly four inches 
long, labelled on one side, “ Elbow of S. Saskatchewan,” and on the 
other, “ Picked up in the bed of the river above Fort Pitt,’ seems to be 
intermediate in its characters between B. compressus and B. ovatus. 
Battle River, at the Elbow, the fragment referred to under the head- 
ing Liopistha undata. 
BACULITES OVATUS, Say. 
Baculites ovatus, Say. 1821. Am, Journ. Se. and Arts, vol. ii., p. 41; and of subse- 
quent American authors. 
| 
Elbow of South Saskatchewan, the three fragments referred to in 
the remarks upon the preceding species. One of the three is labelled 
also, “ Fort Pitt, from bed of river.” 
In addition to these species, there are in the collection three specimens 
of fossiliferous Cretaceous shale from Long River and Forked Creek, in 
the Souris Hills, Manitoba, two labelled No. 6, and one No. 7. As indi- 
cated by Mr. Etheridge, there are “scales of ctenoid fishes” upon both 
specimens labelled No. 6, and a fragment of an “annelid tube ” upon the 
specimen labelled No. 7. 
