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Part II - State of New Jersey

Part II - State of New Jersey

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188 CRETACEOUS FOSSILSand the first tooth. The third tooth is placed at the widest part <strong>of</strong> thecarapace. It is directed obliquely forward and is more acutely triangularthan the first tooth. Tlic posterior m;~rgin <strong>of</strong> the third toothis distinctly concave and is provided ~~itli a carinate edge which becomescontinuous with the lateral edge <strong>of</strong> the carapace posteriorly.Cardiac field barrel-shaped, limited laterally by faint branchiocardiacgrooves which connect distally with a pair <strong>of</strong> deep thumbnail musclescars. Hepatic area slightly concave. >Ioutl~ficld nearly half as longas the carapace, its lateral cdgcs parallel and out\~ardly arcuate. \Vlienviewed from the ventral surface, the subhepatic f~~rrow and the promincntsubhcpatic carina estcrior to it are parallel to cach other and tothe lateral margin <strong>of</strong> the carapace. Surface <strong>of</strong> carapace minntely andevenly granulate.lleasurcmcnts <strong>of</strong> holotype: length 13> greatest \~idtli 9.6, frontoorbitalwidth 6 mm.Remarks.-Resenlbles A. clongota Milne Edwards (1862, p. 493;Brocchi, 1877, p. 4, pl. 29, figs. 4, 5) from the Cenomanian <strong>of</strong> France,hut is broader than that species, has the front truncate instead <strong>of</strong>rounded and has the muscle-scars placed farther for~~ard.Distributioiu in <strong>New</strong> <strong>Jersey</strong>.-<strong>II</strong>erchantville formation: GrahamBrick Company pits, Maple Shade.Oz~tside distr&t~tio?~.-Delannarc: Spoil bank north <strong>of</strong> C and DCanal, about 1/4 mile east <strong>of</strong> Summit liridge (type locality) ; Merchantvilleformation.ITo1otype.-ANSP19737 (Summit Bridge, Delaware).Raninella sp.Steinkerns <strong>of</strong> three carapaces (YI'PM 17904) from the \Voodburyformation at Lorillard, <strong>New</strong> <strong>Jersey</strong>, arc referable to Rnninella. Thelateral teeth and the details <strong>of</strong> the front are not knon~n, but the concaveposterolateral margins and the position <strong>of</strong> the muscle scars: wliiclireach nearly to the middle <strong>of</strong> the carapace, clearly distinguish thesespecimens from the preceding species, R. tridens. Although none <strong>of</strong>the specimens is well enough preserved to permit <strong>of</strong> aclcquatc sl~ecificdescription, a brief eharacterizatio~~ <strong>of</strong> the species may be desirable.The carapace is ohovate, widest at the distal third ant1 about one anda qnarter times longer than wide. The pr<strong>of</strong>ile <strong>of</strong> the dorsal surface isnearly straight. The front is narrower than the posterior margin, andthe p~"~erolateral margins are concave. The distal ext,remities <strong>of</strong> themuscle sears almost reach to the midlength <strong>of</strong> the carapace. All threespecimens are enlhcdded in n~;~tl.ir by their ventral snrfaces. The largestexample is 22.1 mm. long and 145 mlo. at the greatcst \vidt,h.NEW JERSEY GEOLOGICAL SURVEY

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