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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226 THE RARITAN FLORA.<br />
were collected. He seems disposed to attach considerable weight<br />
to <strong>the</strong>ir resemblance to a helianthoid flower, and points out that<br />
<strong>the</strong>y differ from <strong>the</strong> typical Williamsonias in <strong>the</strong> apparent absence<br />
<strong>of</strong> <strong>the</strong> internal seed-bearing cone. <strong>The</strong> nature <strong>of</strong> <strong>the</strong> remains<br />
does not enable one to form a positive opinion, never<strong>the</strong>less<br />
<strong>the</strong>ir resemblance to well-preserved Williamsonias which are<br />
undoubtedly cycadean, lends more support to a <strong>the</strong>ory <strong>of</strong> relationship<br />
with <strong>the</strong> latter group <strong>of</strong> plants than with <strong>the</strong> essentially<br />
modern Compositm. <strong>The</strong> increased interest in <strong>the</strong> Cycadales<br />
called forth in recent years, has served to establish <strong>the</strong> cycadean<br />
affinity <strong>of</strong> a number <strong>of</strong> species <strong>of</strong> Williamsonia, and structural<br />
material has in a measure cleared up <strong>the</strong>ir morphology, so that<br />
while this order <strong>of</strong> plants had commenced its final decline in <strong>Raritan</strong><br />
time, it must be remembered that it was exceedingly abundant<br />
in <strong>the</strong> older Cretaceous deposits <strong>of</strong> Maryland and Virginia,<br />
and remnants <strong>of</strong> cycad fronds are by no means uncommon in <strong>the</strong><br />
<strong>Raritan</strong> deposits.<br />
Mauy supposed Williamsonias have been described, most <strong>of</strong><br />
those from Americat_ rocks being founded upon exceedingly imperfect<br />
material. Perhaps <strong>the</strong> form most like <strong>the</strong> present species<br />
is Williamso_2g ddaware*_ds Berry _ described from <strong>the</strong> Magothy<br />
formation <strong>of</strong> Delaware. It may be questioned if <strong>the</strong> forms from<br />
Marthas Vineyard which Hollick (loc. eft.) refers to William-<br />
SO_liaproblematica are not more properly referable to WilliamsoJffa<br />
delawarends, This is especially true <strong>of</strong> this author's figures<br />
29 to 32, while figures .07 and 28 may be lateral views <strong>of</strong> <strong>the</strong><br />
compressed transverse views <strong>of</strong> <strong>the</strong> objects described as Williczmso**ia<br />
Niesii, From nearly hon_otaxial horizons Williamsonia<br />
elocate has been described by Lesquereux 2 from <strong>the</strong><br />
Dakota sandstone, and Williamao*_ia cretacea has been described<br />
from <strong>the</strong> Atane beds <strong>of</strong> Greenland by Heer a. <strong>The</strong> Williamsonias<br />
described by Ward from <strong>the</strong> older Cretaceous are all extremely<br />
poor and <strong>of</strong> doubtful affinities, but Williamsonia virgi_ie*2sis described<br />
by Fontaine from <strong>the</strong> older Potomac <strong>of</strong> Virginia, is<br />
a Johns Hopkins Univ. Circulars, No. I99, 19o7, p. 84, /e 4.<br />
Lesq., FI. Dakota Group, 87, pl. _,, _. 9, 9a, 1892.<br />
_Heer, FI. Foss. Arct., vol. VI, ._bth. 2:59, pL re, f. z; pl. I3, f. 9, I882.<br />
NEW JERSEY GEOLOGICAL SURVEY