DESCEIPTIONS OF SPECIES. 41 



CuNNiNGHAMiTES ELEGANS (Corda) Endlicher. 

 PI. m.fig. 1. 



Cunninghamites elegans (Corda) Endl., Synop. Conif., 1847, p. 270; Newberry, Mon. U. S. Geol. Survey, vol. 26 

 (Fl. Amboy Clays), 1895 (1896), p. 48, pi. 5, figs. 1-7; Hollick, Trans. New York Acad. Sci., vol. 16, 1897, 

 p. 129, pi. 11, fig. 2; BuU. New York Bot. Gard., vol. 2, 1902, p. 402, pi. 41, fig. 11 ; Berry, Bull. New York 

 Bot. Gard., vol. 3, 1903, p. 64 (?); BuU. Torrey Bot. Club, vol. 31, 1904, p. 70, pi. 3, figs. 7-9, 11. 



Cunninghamia elegaTis Corda, in Reuss, Verstein. Bolim. Kreideform. (abth. 2), 1846, p. 93, pi. 49, figs. 29-31. 



The single specimen of this well-defined species here figured is the only one thus 

 far found within the insular area, although it is not rare in both the Raritan and 

 Cliff wood formations in New Jersey. It occurs in the upper Cretaceous of Europe, in 

 the Patoot beds of Greenland, and has recently been identified fi-om the Judith River 

 beds of Montana," but, so far as I am aware, has never been recorded from any 

 typical Dakota group locahty. We have generally regarded it as one of the charac- 

 teristic eastern Cretaceous species which served to indicate the closer relationship 

 ■ with the Cretaceous of Greenland and Europe than with that of the western United 

 States, but this view, in the light of the above-mentioned discovery, must now be 

 somewhat modified. 



Locality: Chappaquiddick, Marthas Vineyard. Collected by Arthur Hollick. 

 Specimen in Mus. New York Bot. Gard. 



Sequoia heterophtlla Velenovsky. 



PI. Ill, figs. 2, 3. 



SequoiaheterophyUaVd., Gjmnosp. Bohm. Kreideform, 1885, p. 22, pi. 12, fig. 12; pl. 13, figs. 2-4, 6-9; Hollick, 

 Ti-ans. New York Acad. Sci., vol. 12, 1892, p. 30, pl. 1, fig. 21; Newberry, Mon. U. S. Geol. Survey, vol. 26 

 (Fl. Amboy Clays), 1895 (1896), p. 49, pl. 6, figs. 1-13. 



Fragmentary remains of tins species occur in the clays at Kreischerville, Staten 

 Island, but thus far they have not been found elsewhere within the area covered by 

 this monograph, although the species is abundantly represented in the Amboy clays 

 of New Jersey, and is reported from the Potomac of Virginia and the Judith River 

 beds of Montana. It is a characteristic element in the Cretaceous of Europe, and 

 it is somewhat remarkable that it has not been recorded from any of the Greenland 

 horizons. 



Locality: Kreischerville, Staten Island. Collected by Arthur Hollick. Fig. 2, 

 specimen in Mus. New York Bot. Gard.; fig. 3, specimen in Mus. Staten Island 

 Assn. Arts and Sci. 



Sequoia ambigua Heer. 



Pl. Ill, figs. 7, 8. 



Sequoia ambigua Heer, Fl. Foss. Arct., vol. 3 (abtb. 2), 1874, p. 78, pl. 21, figs. 1, 2a-9a, 10a, 10c, 11 ; White, Am. 

 Jour. Sci., vol. 39, 1890, p. 97, pl. 2, figs. 2, 3;-UMer, Trans. Md. Acad. Sci., vol. 1, 1892 (1901), p. 207; 

 Hollick, BuU. Geol. Soc. Am., vol. 7, 1895, p. 13. 



The recorded occurrence of this species within the insular area is thus far con- 

 fined to the Gay Head locality, and it has not as yet been reported from any of the 



oKnowlton, F. H., Fossil plants of the Judith River beds: Bull. U. S. Geol. Survey No. 257, 1905, p. 135, pl. 15, fig. 1. 



