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Part II - State of New Jersey

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ears a line <strong>of</strong> prominent sockets. Lateral margins <strong>of</strong> the otherwisesmooth occludent surface beaded. JVrist shorter and higher than themajor wrist.Neasurements: length <strong>of</strong> propodus 25.1 mm., length <strong>of</strong> palm 19mm., hcight <strong>of</strong> palm 12.3 mm., thickness 6.4 mm. (ANSP 19669, figuredsyntype) ;length <strong>of</strong> propo~los 22.7 mm., length <strong>of</strong> palm l5.G mm. height<strong>of</strong> palm 13.4 mm. thickness 6.2 mm. (YPM 126) ; length <strong>of</strong> palm 20mm., length <strong>of</strong> wrist 17.5 mm. length <strong>of</strong> arm 13 mm. (WFIS 10095).Remarks.-ProtocalLianassa mortoni is the commonest Upper Cretaceousdecapod in Xeu~ <strong>Jersey</strong>. The palms vary considerably in snrfacetexture, number and arrangement <strong>of</strong> tlie papillae and sockets andin the ratio <strong>of</strong> the length to the height. Dccort,icated specimens maylook quite different from those retaining either the inner or the outerlayer <strong>of</strong> the integument.In spite <strong>of</strong> these differences, two races <strong>of</strong> the species can be dist,inguished: race a-height to length ratio varies from 1 :1.32 to 1 :1.62for major palms, and from 1 :1.1 to 1 :1.28 for minor palms; race b-rat,io for major palms is 1 :1.19 to 1 :1.25, and 1 :1.35 to 1 :1.48 for minorpalms. Race a is the commoncr <strong>of</strong> the two, at least in <strong>New</strong> <strong>Jersey</strong> whereit is particularly ahundant in the JIerchantrille formation. The syntypehands described by Pilsbry (1001, pl. 1, figs. 1-4, 8-10) belong torace a. Sixteen <strong>of</strong> tlie 442 <strong>New</strong> <strong>Jersey</strong> and Dclalvare specimens studiedby tlie writer are race b indivirluals, as are the following:1) broad palms from A'e~r. <strong>Jersey</strong>, Delaware and Maryland citedby Pilsbry (1916, p. 365) ;2) bolotype <strong>of</strong> Cnlliai~assa. clnrki Pilsbry (1916, p. 368, p1. 11,fig. 8) ;3) specimens figured by Rathbun (192fi> p1. 67, figs. 1, 4-9) fromCoon Creek beds in Tennessee.Both races range from Aferchantville age to Tinton age. Although raceb hands are rare in Xelv <strong>Jersey</strong> and Delaware, to the south in Tenncsseeand Tvfississippi they appear to be the predominant form.Rathbun's (1935, p. 30) record <strong>of</strong> this species in the Woodburyclay at Lorillard is based 011 an indeterminable impression <strong>of</strong> a smallhand (NJ St. 11 No. 9511).The figured type <strong>of</strong> Callin~lassa eonrndi Pilsbry is in the collection<strong>of</strong> the Wagner Free Institute <strong>of</strong> Science (No. 5478W), not in the <strong>New</strong><strong>Jersey</strong> <strong>State</strong> Mnsenm as reported by Rathhun, 1935, p. 30.Distribution in ATew .<strong>Jersey</strong>.-3rerchantviIle formation: Bordentown(12a), Lenola (l5), lfaple Shade (16). lT1enonah formation:Cramford's Corner (34), Marlboro (35). Aft. Lanrel/Navesink formation:Atlantic Highlands (37) ; Bruere's Pit, S. <strong>of</strong> TValnford; CreamRidge (45) ; Afiddletown (Crcdner, 1870, p. 242) ; Afnllica Hill (53) ;near <strong>New</strong> Egypt (48). Tinton formation: Beers Hill (62), TintonFalls (63).NEW JERSEY GEOLOGICAL SURVEY

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