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PODOZAMITES ANGUSTIFOLIUS (Eichw.) Schimp. 
(PLATE 71, Fic. 8.) 
Podozamites angusttfolius Schimp. Paléont. Véget. 2: 160. 
Zamites angustifolius Eichw. Lethaea Rossica, 2: 39. pl. 2, f 7. 
A number of fragments, referred provisionally to the genus Podo- 
zamites, have been found on Staten Island, Long Island, Block 
Island and Martha’s Vineyard, but this is the only specimen in which 
specific identification has been satisfactory. It is not rare in the Cre- 
taceous of New Jersey and may be found described and figured by 
Newberry in the Flora of the Amboy Clays (7. c. 44. pl. 23, f. 7-4). 
’ Formation and locality: Cretaceous shale; Glen Cove, Long 
Island, N. Y. 
SEQUOIA sp. 
(PLATE 72, FIG. 2.) 
This specimen is too imperfect for any except generic determina- 
tion, although it might be more or less satisfactorily compared with 
some one or another of several species, according to the particular 
figure selected, as for example, S. swédudata Heer (Fl. Foss. Arct. 
3 (Kreide-Fl.): pf. 34, f. za; thid. 0: pl. 77, f. 1), S. Retchen- 
éacht (Gein.) Heer (FI. Foss. Arct. 3 (Kreide-Fl.): p/. 72, f. 
7a; pl. 20, f. 7a; pl. 22, f. Sf; pl. 36, f. 1-8), S. fastigiata 
(Sternb.) Heer (Fl. Foss. Arct. 3 (Kreide-Fl.): A. 27, f. 5, 63 
Pl. 38, Ff. 17), S. concinna Heer (FI. Foss. Arct. 7: pl. sz, f. 93 
pl. 53, f. 16) or S. condita Lesq. (8th Ann. Rept. U. 5. Geol. 
and Geog. Surv. Terr. p/. 4, f. 7). 
Of the above species the only one definitely recorded from this 
region is S. Retchenbachi, which has been found at Cliffwood and 
Woodbridge, New Jersey, and on Staten Island, but no represen- 
tative of the genus has heretofore been found on Long Island. 
Formation and locality: Cretaceous shale; Glen Cove, Long 
Island, 
DAMMARA MICROLEPIS Heer. 
(PLATE 71, FIGS. 9, 10.) 
Dammara microlepis Heer, Fl. Foss. Arct. 6?: 55. pl. 40, f. 5. 
Formation and locality: Cretaceous shale; Glen Cove, Long 
Island, N. 
FRENELOPSIS HOHENEGGERI (Ettingsh.) Schenk? 
(PLATE 72, FIG. I. 
firenelopsis Hohenegger? Schenk (Foss. Pfl. Wernsdorfer 
