. The geology of Nova Scotia, New Brunswick, and Prince Edward Island, or, Acadian geology [microform]. Geology; Geology, Stratigraphic; Paleontology; Geology, Economic; Géologie; Géologie stratigraphique; Paléontologie; Géologie économique. '^ Camarophma (?) ginhdinn (?), Phillips (Fig 02, a, 6). " Tercbralvla gloliidiiin, IMiillips, ICncycl. Metr., vol. iv., article 'Geology,' pi. 3, fig. ;J, 1834. '* Tcrehralula r/ioiiilioi'dea, IMiillips, Geol. Yorksh., vol. ii., p. 222, pi. 12, figs. IS, 20, " Ilemithyris lonr/a, M'Coy, British Pal. Foss., p. 440, pi. 3, D., fig, 24, 1855


. The geology of Nova Scotia, New Brunswick, and Prince Edward Island, or, Acadian geology [microform]. Geology; Geology, Stratigraphic; Paleontology; Geology, Economic; Géologie; Géologie stratigraphique; Paléontologie; Géologie économique. '^ Camarophma (?) ginhdinn (?), Phillips (Fig 02, a, 6). " Tercbralvla gloliidiiin, IMiillips, ICncycl. Metr., vol. iv., article 'Geology,' pi. 3, fig. ;J, 1834. '* Tcrehralula r/ioiiilioi'dea, IMiillips, Geol. Yorksh., vol. ii., p. 222, pi. 12, figs. IS, 20, " Ilemithyris lonr/a, M'Coy, British Pal. Foss., p. 440, pi. 3, D., fig, 24, 1855. " Of this very small shell I have been able to examine only three specimens; but it is stated to be abundant in a yellow arenaceous limestone at Do Ben liivcr, where, according to Dr Dawson's expe- rience, it is always small. I have also felt somewhat puzzled in the (Ictennination of this fossil; but, after having consulted Professor Do Koninck, I concluded to refer the specimens to the same species, not- withstanding the apparent difTerence tliey present. Professor De Koninck referred one of them to T. rhuiitboidca, Phillips, which is a synonyme of Camarophoria glohnlina ; and after minutely comparing tlio Nova-Scotian specimens with the Carboniferous and Permian types, I could perceive no difrcrcncc sufficient to warrant the creation of a new species. The three specimens were exactly of the same size, namely, three lines in length by three in width, and two and a half in depth. The uncertainty which both Professor De Koninck and myself liavc experienced refers to a specimen which much rcsci \ in minia- ture, a form of Rhynchondla acuminata; but when w. remember. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original Dawson, J. W. (John William), Sir, 1820-1899. London : Macmillan; Montreal : Dawson


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Keywords: ., boo, bookcentury1800, booksubjectgeology, booksubjectpaleontology