[PENHALLOW] CRETACEOUS AND TERTIARY PLANTS OF CANADA 81 
TAXODIUM DISTICHUM MIOCENUM, Heer. 
Heer, Flora Foss. Sachalinensis, 22, Pl. I., 9. 
Flora of Northern Greenland (1869), 463, Pl. XLIII., 4, 5. 
Miocene Flora of Spitzbergen (1870), 32, Pl. II. & III. 
Dawson, Trans. R. Soc. Can., VIII., iv., 79: I. (1882), iv., 33 & 34. 
Newberry, Later Extinct Floras of the U.S., XXXV., 22, Pl. XLVII., 6; L, 3; 
eae Os 
Miocene of Greenland; Birch Bay, Washington and John Day Valley, Oregon. 
Fort Union Group of Montana. Eocene of Elko Station, Nevada and 
Red Deer River, Canada. Miocene of the Similkameen Valley, British 
Columbia, and Mackenzie River. 
This widely spread and familiar species appears in the Paskapoo 
series of the Red Deer River in the form of several fragments of 
leafy branches, but without fruit. They show the characteristic 
features of the species. 
GLYPTOSTROBUS EUROPÆUS (Brongt.), Heer. 
Dawson, Trans. R. Soc. Can., VIII., iv., 791 (1882), iv., 34. 
Newberry, Later Extinct Floras of the U.S., XXXV., 24, Pl. XXVI., 6 & 8a; 
LV., 3, 4. 
Lesquereux, Tertiary Floras, VII., 74, Pl. VII., 1, 2. 
Cretaceous and Tertiary Floras, VIII., 222, Pl. XLVI., 1. 
Eocene of the Paskapoo Series, Red Deer River, Canada. 
Miocene of Stump Lake and the Similkameen Valley, B.C. 
Miocene of the Bad Lands and the Yellowstone Valley. 
Fort Union Group of Dakota and Birch Bay, Washington. 
Green River Group of Florissant, Colorado. 
In the Paskapoo series, Glyptostrobus europeus is represented 
by one small, leafy stem only. In the Flora of the Similkameen Val- 
ley, Sir William Dawson figured a small specimen of Glyptostrobus 
which he hesitated to identify, although admitting its close resem- 
blance to G. europæus from the Miocene of Europe. It would seem 
to me that there is no real ground for hesitation in admitting the 
identity of this species. 
TYPHA, sp. 
Eocene of the Paskapoo Series, Red Deer River, N.W.T. 
Leaf narrowly lanceolate, apex acute (?), margin entire. Veins 
numerous, about 36 to the cm., unequal, and not equidistant; trans- 
verse veinlets none. 
The specimen upon which the above diagnosis is founded is about 
11-5 em. long and 17 mm. broad at the lower end where it has been 
