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 ...
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198 THE RARITA2N FLORA.<br />
parable with <strong>the</strong> similar variations in <strong>the</strong> leaves <strong>of</strong> <strong>the</strong> modern<br />
Sassafras due to position and age.<br />
<strong>The</strong>re seems to be no basis for maintaining <strong>the</strong> distinction<br />
between Aralia palmata and A. polymorpha <strong>New</strong>b. <strong>The</strong> species<br />
is abundant in <strong>the</strong> <strong>Raritan</strong>, and survives in <strong>the</strong> overlying Magothy<br />
formation in a slightly modified form, which may prove<br />
eventually to be a distinct species.<br />
<strong>The</strong> genus Aralia, to which this and <strong>the</strong> several following<br />
species are referred, is an important element in <strong>the</strong> Cretaceous<br />
<strong>flora</strong>s <strong>of</strong> <strong>the</strong> globe, with many species especially in <strong>the</strong> Dakota<br />
Group and <strong>the</strong> Bohemian Cenomanian. <strong>The</strong> large number <strong>of</strong><br />
species, seven in all, in <strong>the</strong> <strong>Raritan</strong> furnishes corroborative evidence<br />
<strong>of</strong> its Cenomanian age.<br />
Occurrence. Woodbridge. ]<br />
Collections.--N. Y. Botanical Garden.<br />
ARALIA QUINQUEPARTITA Lesq.<br />
Plate XX, Fig. 8; Plate XXIV, Fig. 5.<br />
Aralia quinquepartita Lesq, Ann. Rept. U. S. Geol. and Geog.<br />
Surv. Terr., 1871; 302, I872; Bull. U. S. Geol. Surv.<br />
Terr., vol. I : 394, I876; Cret. FI. 9o, pl. 15, [. 6, 1874;<br />
F1. Dakota Group, 136, 1892.<br />
<strong>New</strong>b., F1. Amboy Clays, ii5, pl. 4o, [. I, 2, I896; Mon.<br />
U. S. Geol. Surv., vol. XXXV. : I23, pl. 9, f' I, 1898.<br />
Description.--Leaves generally <strong>of</strong> large size and coriaceous<br />
texture, from 5 era. to 17 era. in length by from 9 cm. to 17 cm.<br />
or possibly more in greatest breadth between <strong>the</strong> tips <strong>of</strong> <strong>the</strong><br />
lateral lobes, petiolate. Palmately 5-lobed. Lobes long,<br />
linear or lanceolate in outline, obtusely pointed. Terminal lobe<br />
<strong>of</strong> <strong>the</strong> same size as <strong>the</strong> principal lateral lobes from which it is<br />
separated by narrow but rounded sinuses extending threequarters<br />
<strong>of</strong> <strong>the</strong> distance to <strong>the</strong> base. <strong>The</strong> ground plan <strong>of</strong> <strong>the</strong><br />
leaf is trilobate, with each <strong>of</strong> <strong>the</strong> lateral lobes more or Iess deeply<br />
divided into two almost equal divisions, <strong>the</strong> basal one <strong>of</strong> which<br />
is more or less subordinate. Primaries stout, 3 in number<br />
NEW JERSEY GEOLOGICAL SURVEY