(417) 
with those described by Newberry under the name 7yécalycites 
papyraceus (Fl. Amboy Clays, 2. c. 132. pl. 46, f. 30-378), and 
they merely differ in their larger size. In some specimens, as indi- 
cated in FIGS. § and 6, the appendages appear as if confluent at 
their bases, which is probably due to overlapping, and doubtless 
these specimens, if perfect, would present the appearance of three- 
lobed samarae. 
It is with some hesitation that I have included Fic. 7 in this 
species, for the reason that only two appendages are present, 
which are shorter and more coarsely striated than in the other speci- 
mens, but it may perhaps be merely an abnormal or defectively 
preserved one. It is almost certain that the specimen from the 
same locality previously described and figured by me as “ apparently 
a winged seed or samara” (Bull. Torrey Club, 21: 62. AZ. 180, f. 
ZI. 1894), should be regarded as one of the detached parts of this 
species. 
Formation and locality: Cretaceous shale; Glen Cove, Long 
Island, N. Y 
Calycites alatus sp. nov. 
(PLATE 72, FIG. 8.) 
Organism triangular in outline, consisting of a top-shaped nuc- 
leus, to which are attached two entire, broadly spatulate, ecu 
nally striated, wing-like appendages, each about 6 mm. long by 5 
mm. maximum width. 
This little organism may perhaps belong in the genus last 
mentioned, and it was in fact originally referred by me to 7récaly- 
cites papyraceus Newb. when first discovered (Trans. N. Y. 
Acad. Sci. 1§: 6. 1895), but I am now inclined to think that this 
reference was not warranted and that it should have a distinctive 
name. 
ee and locality: Cretaceous shale; Montauk Point, Long 
Island, N. 
Explanation of Plates 70-79 
PLATE 70 
Page. 
Fics. 1 and 2. Dammara (?) Northportensis sp. nov. 405 
FIG. 3. Cisaeat Be sp. nov. 406 
FIGs. he and 5. p Newb 406 
G. 6. Cocculus ere os nov 407 
Fic. 7 Paliurus ¢ Hollick 408 
Fics. 8 and 9. & ecalypeus (?) es Newb 408 
Fics. lo and 11. Laurus angusta Heer. 408 
Fics. 12 and 13. Celastrus arctica Heer 408 
