7 
7954 “Above the base of the Beaverfoot 230 feet” 
Rhynchotrema increbescens var. occidens n. var. 
7932 “Above the base of the Beaverfoot 268 feet” 
Holy sites rohustus n. sp. 
Dipkyphyllumt primum n. sp. 
Favositee cf . favosus (Goldfuss) 
Streptelasma prolongatum n. sp. 
Rhynchotrema kananaskia n. sp. 
Rhynchotrema ef. increbescens var. occidens n. var. 
Brachiopod undtd. 
Actinoceras sp. 
The fossil assemblage of this bed suggests a transition zone. There are 
present fossils, some of which are associated elsewhere with an undoubted 
Richmond fauna and others which are more characteristic of a Silurian age. 
(8) Fairmont Springs. Two localities representing the same beds 
furnished the following species: 
7851 
7793 Streptelasnia prolongatum n. sp. 
Streptelasma distinctum n. sp. 
Halysites robu&tus n. sp. 
Rhynchotrema increbescens var. occidens n. var. 
Rhynchotrema pisina n. sp. 
Dinorthis Columbia n. sp. 
(9) Near Columbia lake 
7841 Halysites delicatulus n. sp. 
Rhynchotrema sp. 
Brachiopod undtd. 
(10) Harrogate from two exposures of the beds 
7806 Dark grey to blackish dolomitic beds 
Streptelasma cf. prolongatum n. sp. 
Paleofavosites asper (d’Orbigny) 
Crinoid disks 
Brachiopod undtd. 
7816 Grey, heavy-bedded dolomite 
Halysites cylindricus n. sp. 
Favorites cf. hisingeri M.-Ed. and H. 
Paleofavosites asper (d'Orbigny) 
Columnaria cf. oalicina Nicholson 
Diphyphyllumt halysitoides n. sp. 
Syringopora columbiana n. sp. 
Rhynchotrema increbescens var. occidens n. var. 
Feet 
500 
450 
These beds appear to belong to a transitional zone. Rhynchotrema 
increbescens var. occidens and Paleofavosites asper are characteristic of 
beds of undoubted Richmond age, but the assemblage of corals in this lot 
suggests a Silurian facies. 
