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Part II - State of New Jersey

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CRETACEOUS FOSSILSSubgenus Palaenstac~ts Bell, 1850Enoploclytia IPalaeastacus) sp.Plate 80, Figures 3-5Descriptiou-Dactylus straight, ovate-triangular in section, graduallytapering distally. Teeth circular in section, about equal in sizeand spacing, more than their diameter apart. The distance betweenthe proximal (1st) tooth and the proximal end <strong>of</strong> the finger about equalto the spaee between the first and third tooth. Integument thick, studdedwith widely separated papillae and tubercles, the laster numerouson the upper surface <strong>of</strong> the dactylus where at least three arc on the midline.The posterior tubercle <strong>of</strong> this row <strong>of</strong> three forms an eqnilateraltriangle with a transverse row <strong>of</strong> two tubercles behind it. Articularnodes stout, conical, widely fiaired at the bases and placed slightly belowthe upper margin <strong>of</strong> the finger.The tip <strong>of</strong> this unique finger is lacking and most <strong>of</strong> the low subconicalto dome-shaped tubercles are broken. The occludenl surface haca median row <strong>of</strong> six teeth plus a tubercle which is situated to one side<strong>of</strong> the midline between the third and fourth tooth. The lateral surfaces<strong>of</strong> the finger are flattish.Measurement <strong>of</strong> figured specimen : length 55.7, height Behind proximaltooth 15.2, thickness behind proximal tooth 13.O mm.Remarks.-This is the second giant Enoplocl7~tia that has beenfound in the Americas, the first being E. (P.) zudkeri (JQ~itfield, 1880.p. 37, pl. 16, figs. 1 a-c; pl. 17, fig. 1 a; Upper Albian; Texas), a specieswith a strongly curved and tapered dactylus. The straight dactylaraxis and coarse surface tnberculation <strong>of</strong> our species agree with the description<strong>of</strong> E. (P.) image1 M'Coy (1849, p. 332 ; Senonian ; England) ;however, the dactylar teeth <strong>of</strong> M'Coy's species-which has never heenfigured-are said to be less than their diameter apart.Distributio?t.-Delaware: Merchantville formation: Spoil banknorth <strong>of</strong> Chesapeake and Delaware Canal about one-quarter mile east<strong>of</strong> Summit Bridge, Delaware.Figured specimen.-WFIS No. 17079.Enoploclytia suhgen. et sp. indet.Plate 8P, Figure 6A rectangular fragment 1neas.1ring 30 x 40 mm., from the spoil banknear Summit Bridge, Delaware, represents the co?lrirx lateral surface<strong>of</strong> a large palm. Spinous tubercles ornament the surface and the position<strong>of</strong> the carpopropodal articulation is marked by a broad, deepgroove. In the same block <strong>of</strong> clay close to the palm there is an imperfectmold <strong>of</strong> a large tubular finger. (ANSP 19734).NEW JERSEY GEOLOGICAL SURVEY

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