References
- 1888 . Anthozoen und Bryozoen des Oberen Mittelrussischen Kohlenkalks . Mém. du Comité Géologique , v ( 4 )
- 1837 . Oryct. du Gouv. de Moscou , : 153 – 153 . pl. xxx. fig. 6
- Lewis . 1929 . Ann. & Mag. NAt. Hist. ser. 10 , iii : 456 – 456 .
- Lewis . 1924 . Quart. Journ. Geol. Soc. , lxxx : 389 – 407 . pls. xxvii.—xxx.
- The flattened appearance of these specimens is similar to that of corals figured by Dr. Salée A. Marbre noir de Dinée Bull. Soc. Gelge. de Géol. 1911 133 135 from thefigs. 1 & 2
- A similar arrangement of septa is seen in some species of Caninia, but in Pseudocaninia it is a more constant and pronounced feature (cf. Lewis Q. J. G. S. 1924 pl. xxviii. figs. 1 j & 1 k, and F. Heritsch, “A Caninia from Spitzbergen,” 1929, pls. iii. & iv.; see later p. 234)
- Wedekind , R. 1924 . Das Mitteldevon der Eifel 38 – 38 . Marburg 1 Teilfigs. 50 & 51
- 1854 . British Fossil Corals . Mem. Pal. Soc. , pl. lxvii. fig. 4 a
- 1929 . “ Eine Caninia aus dem Karbon des de Geer—Berges im Eisfjordgebiet auf Spitzbergen ” . In Skrifter om Svalbard og Ishavet Vol. 24 , Oslo pls. iii. & iv
- Robinson , W.J. 1917 . Trans. Connecticut Acad. of Arts & Sciences , xxi : 195 – 195 .