( 64) 
CUNNINGHAMITES squaMosuS Heer. Pl. 48. f. 14, 19. 
Cunninghamites syuamosus Heer, Beitr. Kreidfl. Qued- 
linb. 9. pl. z. f. 5-7. 18972. Hollick, Trans. N. Y. 
Acad. Sci. 16: 129. pl. rz. f. 3. 1897. (Not of Hosius 
and Von der Marck.) 
Remains of this species are the most abundant coniferous 
fossils in the clays at Cliffwood. They occur as twigs about 
the size of those figured by Hollick or smaller and demand 
no extended discussion. This is the only locality in this 
country where they have been found, but additional collec- 
tions from the Amboy Clays ought to disclose them. The 
two specimens figured are more robust than the majority of 
the remains and are ten sevenths of the average size, al- 
though several large specimens were collected. On the 
usual-sized specimens the leaves are about 6 mm. long, closely 
set, stout, incurved, very much crowded in some instances 
and quite different in appearance from those of Seguoza 
Reichenbacht with which it is often associated. 
CUNNINGHAMITES ELEGANS (Corda) Endl. 
Cunninghamia elegans Corda; Reuss, Verstein. Béhm. 
Kreidef. 93. pl. 49. f. 29-31. 1846. 
Cunninghamites elegans Endl. Syn. Conif. 270. 1847. 
Heer, Beitrag. Kreidefl. (Neue. Denkschr. Schweiz. 
Gesell.) 12. pl. 7. f. 14. 1869. Schimper, Pal. Vég. 2: 
256. Heer, Fl. Foss. Arct.'7: 17. p/. 53. fi 1. 1883. 
Newb. Fl. Amboy Clays, 48. g/. 5. 7. 1-7. 18096. 
Hollick, Trans. N. Y. Acad. Sci. 16: 129. pl. rr. f. 2. 
1897. Hollick, Bull. N. Y. Bot. Garden, 2: 402. i. 
41. f. 1%. 1902. (Knowlton, U. S. Geol. Surv. 
Bull. 163: 29. pl. 5. f. 3. 1900, probably belongs 
here.) 
Cunninghamites squamosus Hosius & Von der Marck, FI. 
Westfal. Kreide. 54. pl. 37. 4. 137-141. (Palaeonto- 
graphica, v. 26.) 1880. 
Originally described from Moletein in Moravia and Mseno 
in Bohemia (Cenomanian), then from the chalk of Westphalia ; 
