06.03.2015 Views

Bulletin 3. The flora of the Raritan Formation, 1911 - State of New ...

Bulletin 3. The flora of the Raritan Formation, 1911 - State of New ...

Bulletin 3. The flora of the Raritan Formation, 1911 - State of New ...

SHOW MORE
SHOW LESS

Create successful ePaper yourself

Turn your PDF publications into a flip-book with our unique Google optimized e-Paper software.

82 THE RARITAN FLORA.<br />

"Brachyl_hyllun_ macrocarpulr_, <strong>New</strong>b., MSS name mentioned in<br />

footnote, p. 51, FI. Ambov Clays, 1896.<br />

Krtowltou, Bull. U. S. Geol. Surv., No. 163 : 29, pl. 4, f. 5,<br />

6, 19oo.<br />

HolIiek, Bull. N. Y. Bo.t. Garden, vol. 3 : 4°6, pl. 7o, f . 4,5,<br />

19o4; ,_5. S. Geol. Surv. Mort. 50:44, pl. 3, f. 9, Io,<br />

19o7.<br />

Berry, Ann. Rept. <strong>State</strong> Geol. (N. J.) for 19o5; 139, 19o6;<br />

" Bull. Torrey Club, vol. 32 : 44, pt..2, f. 9, 19o5 ; Ibid.,<br />

vol. 33: I68, pl. 9, 19o6.<br />

Hollick and Jeffrey, Amer. Nat., vol. 4o: 2oo, 19o6.<br />

? Moriconia cycloto.ron Deb. & Ett., Ileer, F1. Foss. Arct., vol. 7,<br />

pl. 54, f. zc, 1883' (non Heer's o<strong>the</strong>r figures).<br />

Descriptibn.--Stout twigs, pinnately branched, covered with<br />

large, thick, rhomboidal, squamate, densely crowded, appresged<br />

leaves attached by practically.<strong>the</strong>ir whole ventral surface. PhyIlotaxy<br />

spiral. Leaf-surface striated, <strong>the</strong> strife converging' toward<br />

<strong>the</strong> obtuse apex. Cones n_ positively determined.<br />

Brachyphyllum is chiefly an older Mesozoic type, but it remains<br />

abundant through <strong>the</strong> Lower Cretaceous, two species having beert<br />

described from <strong>the</strong> Potomac Group o,f Maryland and Virginia.<br />

It is a waning type in <strong>the</strong> Upper Cretaceous, represented by but<br />

a single species, <strong>the</strong> one under discussion,, which persists as high<br />

as <strong>the</strong> Seuonian. It is widely distributed, and is recorded fronl<br />

Long Island, <strong>State</strong>n Island, <strong>New</strong> Jersey and Delaware, in <strong>the</strong><br />

east, and from <strong>the</strong> Dakota Group, <strong>of</strong> Kansas, and <strong>the</strong> Montana<br />

Group <strong>of</strong> Wyoming, in <strong>the</strong> west? It is probably represented in<br />

<strong>the</strong> Patoot beds <strong>of</strong> Greenland, by <strong>the</strong> material which Heer erroneously<br />

refers (loc. cir.) to Moriconi_. While it is no_ recorded<br />

from Europe, Velenovsky has described remains from <strong>the</strong> Cenomanian<br />

<strong>of</strong> Bohemia, which appear to be identical with <strong>the</strong><br />

American repi'esefltatives, referring <strong>the</strong>m to <strong>the</strong> Jurassic genus<br />

Echi_wstrobus <strong>of</strong> Scllimperr ° Hollick and Jeffrey have recently<br />

• It has also been collected "0y<strong>the</strong> writer in North Carolina, South Carolina,<br />

Georgia and Alabama.<br />

' _Velen., Gym. B6hm. Kreidef. I885, p. I6, pl. vi, figs. 3, 64; Kvetena ceskebo<br />

cenomanu, I889, p. 9, pl. i, figs. II-I9; !01-ii, figs. I, 2.<br />

NEW JERSEY GEOLOGICAL SURVEY

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!