70 BERRY: FLORA OF THE MATAWAN FORMATION 
The specimen is an unusually perfect one and shows that the 
nearly straight lateral margins which become very thin are not 
usually preserved. There is no indication of the apical point 
figured by Hollick; on the contrary the apex is evenly rounded. 
In outline and size it is very similar to the scale from Tottenville, 
Staten Island, doubtfully referred by Hollick to Dammara borealis 
Heer. In the present collections these scales are not as abundant 
as in those of the previous season, although they still form a 
decided element in this flora. 
CUNNINGHAMITES ELEGANS (Corda) Endl. (PLATE 3, FIGURES 7, 8 
OG, 11.) 
Last summer’s collections contain numerous unmistakable frag- 
ments of this species, one a twig 7.7 cm. long. 
CUNNINGHAMITES SQUAMOSUS Heer. 
Remains of this species are not so common as in the previous 
season’s collections, but several good specimens were collected 
including some twigs 8 cm. long. The portions of stems shown 
on plate 5, figures 2 and 3, are of this species or the preceding. 
MorIconia CYCLOTOXON Deb. & Ett. 
Sparingly represented in the collections of 1903 by the same 
large-sized forms as those previously found. 
FRENELOPsIS Schenk, Palaeont. 19': 13. 1869 
Several species of Cretaceous plants have been referred to this 
genus, so named from their resemblance to the existing species of 
frenela of the Australian region. The consensus of opinion seems 
to be that they are referable to the Cupresseae, although Heer is 
inclined to ally them with Zphedra among the Guetales, and 
Schimper includes them in the Zaraceae. In lower Cretaceous 
times they ranged from the Mediterranean region of Europe to 
Greenland and North America, and their latest known appearance 
is in the Senonian of Westphalia. That these somewhat peculiar 
forms did not become extinct is evidenced by the remains re- 
ferred to the closely allied, if not identical, genera Widdringtonia, 
Widdringtonites (Frenelites) and Callitris which occur both in 
Europe and in America, where they are common in the Creta- 
