. Acadian geology [microform] : the geological structure, organic remains and mineral resources of Nova Scotia, New Brunswick and Prince Edward Island. Geology; Paleontology; Geology; Geology; Geologie; Paléontologie; Géologie; Géologie. FOSSILS OF TIIR CAKnONIPEROUS UMKSTONES. 2o:i "This snmll h\\c\1 in very nliundivnt in the wlicU liincstono of Ilrook- fifld, SluilMMmcadio, niid in some other hicnlities in Nova iSeotin, where, it is alwiiys with .S/). rristalus, of whieh it may iierhivps after all he no nioro than a niodilieation. " and It/ii/nr/i(inr
. Acadian geology [microform] : the geological structure, organic remains and mineral resources of Nova Scotia, New Brunswick and Prince Edward Island. Geology; Paleontology; Geology; Geology; Geologie; Paléontologie; Géologie; Géologie. FOSSILS OF TIIR CAKnONIPEROUS UMKSTONES. 2o:i "This snmll h\\c\1 in very nliundivnt in the wlicU liincstono of Ilrook- fifld, SluilMMmcadio, niid in some other hicnlities in Nova iSeotin, where, it is alwiiys with .S/). rristalus, of whieh it may iierhivps after all he no nioro than a niodilieation. " and It/ii/nr/i(inrlln.âThe rcferahle to these geiieni .sent nio \)y Dr Dawson, as well as those bron}j;ht to England l)y Sir C. liycll, nro generally very small, and not in nil cases snllieiently complete to warrant a satisfactory determination. 1 have, however, carefully represented the principal forms. Fig. M {(i),â ('ameroi>horia tjlulmliiiii, Phillips; nut. ami mnijnijlal; (fc) variety vj'thc "â Camarophoria (?) glohullna (?), Phillips (Fig 92, «, i). " Tercbratula fflobulina, Phillips, Encycl. Mctr., vol. iv., article 'Geology,' pi. 3, fig. H, 1834. 'â ^ Terchratula r/iomboidca, Phillips, Lleol. Yorksh., vol. ii., p. '222, pi. 12, figs. 18, 20, 1836. " llemilhyris longa, M'Coy, British Pal. Foss., p. 440, pi. 3, D., fig. 24, IBSf). " Of this very small shell I have been able to examine only three specimens; but it is stated to bo abundant in a yellow arenaceous limestone at De Bert River, where, according to Dr Dawson's expe- rience, it is always small. I have also felt .somewhat puzzled in the determination of this fossil; but, after having consulted Professor De Koninck, I concluded to refer the specimens to the same species, not- withstanding the apparent difference they present. Professor Do Koninck referred one of them to T. rhomboidca, Phillips, which is a syuonymc of Camarophoria gli)buUna ; and after minutely comparing th
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Keywords: ., boo, bookcentury1800, booksubjectgeology, booksubjectpaleontology
