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Part II - State of New Jersey

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152 CRETACEOUS FOSS<strong>II</strong>JSlonga in these same respects (see pl. 79, fig. 5a). It cannot be too stronglystressed, however, that at least some juvenile guards <strong>of</strong> B. americana..szrbfusiformis are indist,inguishable from the more slender andlonger jnrenile guard types occurring in 1:. amoricana var. americanaand that the number <strong>of</strong> the guards <strong>of</strong> both varieties studied in this respectis insufficient for any definite conclusions on the subject.Dktribzitwn and Stratiprapi~ica' Runye.-Within the state <strong>of</strong> <strong>New</strong><strong>Jersey</strong> B. americnna rar. s~rbfi~sifor~~zts, and the guards transitionalbetween it and other varietias <strong>of</strong> the species, have been encountered inalmost eyery one <strong>of</strong> the localities from which belemnite collections harebeen studied by the ~riter; it is, however, absent from such localitiesas Barnsboro and Glassboro, <strong>New</strong> Jerscy, and Reedy Point, Delaware,which is probably owing to t,he small amount <strong>of</strong> the gnards availahle(1 to 7) from these localities.The writer has seen specimens <strong>of</strong> R. americana var. subfusiforntisfrom the Nount Laurel sand as n7ell as from the Navesink marl, whichseems to indicate that it has the same stratigraphieal range as the rest<strong>of</strong> the varieties <strong>of</strong> t,he species.B. anlericana var. svbfusiformis is a rare form at most <strong>of</strong> its localities.Only from 1% to 15.20% <strong>of</strong> the guards have been found to hereferable to it at most <strong>of</strong> the localities studied.Range in <strong>New</strong> <strong>Jersey</strong>-JIOUNT LAUREL: Xutt Farm.NAVESINIC: Cream Ridge, Arneytown.Range oatside <strong>New</strong> <strong>Jersey</strong>-Chesapeake and Dela\xran: Canal between Reedy Point and St.Georges (Mount Laurel-Yavesink) ; Bohemia Mills, Maryland.Affinities and Differences.-The reduced value <strong>of</strong> the Schatsky Indexappears to be one <strong>of</strong> the r~~ost reliable (listinetinns between B. americnnarar. sitbfusifor~~bis on the one hand and R. nmericana var. americasa.R. a~~~erieunn var. .i11ter11ier7,ia, and 8. a~~rericana nov. var. indet.Tar. A and B on the other. There even seem to be relatively few specimens,that are transitional betmecn both groups <strong>of</strong> forms in this respect,.Also the pronouncedly laneeolate outline <strong>of</strong> its guard in ventral aspectand n~ostlyfeebly lanceolate outline in lateral nspeet readily distinguishR. an~ericann var. sabfiisifornlis from all other varieties with the eseeption<strong>of</strong> B. amcricana var. interntedia. This latter variety is, however,distinct from B. omoricana var. subfusiforz~lis in its greater value<strong>of</strong> the Schatsky Index, its much deeper alveolus, and in the acute, long:and almost nonmueronate outline <strong>of</strong> the apical end <strong>of</strong> its guard. Theshallower alveolus is also helpful in the differentiation <strong>of</strong> l3. antericannTar. subfusiforrnis from other varieties <strong>of</strong> the species.From B. anterica?aa Tar. polita nov. var., B. anzcrica?~a var. szrbftraiformisdiffers in the presence <strong>of</strong> relatively strongly developed sculpture<strong>of</strong> the surface <strong>of</strong> the guard, in its relatively much smaller, shorter, andNEW JERSEY GEOLOGICAL SURVEY

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