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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RANALES. 147<br />
LAU_OPH_L_U_<br />
E_CA_S HolHck.<br />
Lau,rophylh_m degans ttollick, Mon. U. S. Geol, Surv., vol. 50:<br />
8I, pl..27, f. 1-5, I9o 7.<br />
Berry, Bull. Torrey Club, vol. 36: 255, I9o 9.<br />
La_rus plu.tonia t-lolliek, Trans. N. Y. Aead. Sei., rot. I I : 99,<br />
P[. 3, [. 3, 4, 1892; Ibid., vol. 12: 236, pl. 6, [. I, 189<strong>3.</strong><br />
Proteoides dapI_nogenoides I-Iolliek, Ann, N. Y. Aead. Sei., vol.<br />
II :4_o, pl. 36, f..2, 1898.<br />
Description.--Leaves elongate-taneeolate in outline, somewhat<br />
flexuous, about 12 ctu. to 13 era. in length, by at_ut 2 em.<br />
in greatest width, which is about midway between <strong>the</strong> apex and<br />
<strong>the</strong> base. From this point narrowing, gradually d{stad into<br />
an antennuated, acuminate, usually ct_rved tip and basalty into<br />
a tong, narrowly cuneate base. Midrib stout, stouter than in<br />
Lau,rophyllun_ nerviIlos_r_ Hollick. Secondaries mm_erous,<br />
usually less close and somewhat coarser than in <strong>the</strong> latter species ;<br />
<strong>the</strong>y branch from <strong>the</strong> midrib at an acute angle below', which<br />
becomes more open above <strong>the</strong> base <strong>of</strong> <strong>the</strong> leaf..<strong>The</strong>y are usually<br />
more curved than in L. n_erviIloxwrraand more distinctly camptodrome.<br />
Tertiaries, transverse throughout<br />
<strong>The</strong>se leaves were recorded ori_nally by Hollick as Laimts<br />
ph_tonict, Heer, and" are later compared by <strong>the</strong> former author<br />
with Laud'us ang_t,_ta.Heer, which latter species <strong>the</strong>y resemble<br />
more than <strong>the</strong>y do <strong>the</strong> former. In outline <strong>the</strong>y are not unlike<br />
Le_,rophyllu_ qn_gustifoliu.m, <strong>New</strong>b., from Woodbridge, N. J.,<br />
but differ decidedly in venation. 'Phey are also similar, but<br />
quite Nstinct from Laurophyllur_ _eruillosum,, F_ol_ick, and<br />
Lau,rophytlum reticulatu,m_ Lesq,, <strong>of</strong> <strong>the</strong> Dakota Group.<br />
<strong>The</strong> specimens outside <strong>of</strong> those recorded in <strong>the</strong> present contribution<br />
from <strong>New</strong> Jersey and those which are as yet unl_ublished<br />
from <strong>the</strong> region south <strong>of</strong> <strong>New</strong> Jersey, are from transi_rted<br />
materials associated with <strong>the</strong> temlitmt moraine, from<br />
which numerous specimens have been c_llected. Those from<br />
Totteuville, <strong>State</strong>n Island, are undoubtedly <strong>of</strong> Raritatz age, while<br />
NEW JERSEY GEOLOGICAL SURVEY