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V.—On Goniatites Evolutus, Phillips and Nautilus Tetragonus, Phillips; With a list of the Species Belonging to the Genus Subclymenia

Published online by Cambridge University Press:  01 May 2009

Extract

In 1836, Prof. J. Phillips described and figured from the Carboniferous Limestone, Goniatites evolutus, and for this species D'Orbigny, in 1850, instituted the genus Subclymenia.

Type
Original Articles
Copyright
Copyright © Cambridge University Press 1896

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References

page 413 note 2 Geol. Yorkshire,” pt. ii, 1836, p. 237, pl. xx, figs. 65–68.Google Scholar

page 413 note 3 Prod. de Paléont.,” vol. i, 1850, p. 114.Google Scholar

page 413 note 4 Animaux Fossiles,” Suppl., p. 711, pl. lx, figs. 3a–d.Google Scholar

page 413 note 5 Faune Calc. Carb. de la Belgique,” pt. ii, p. 83Google Scholar, pl. xlv, figs. 5, 6: Ann. Mus. Roy. d'Hist. nat. de Belgique, sér. Paléont., vol. v.Google Scholar

page 414 note 1 Hyatt, A., “Carboniferous Cephalopods”, Second Paper: 4th Ann. Rep. Geol. Surv. Texas, 1892 (1893), p. 414.Google Scholar

page 414 note 2 Op. cit., pt. ii, 1836, p. 233, pl. xxii, figs. 33, 34; pl. xvii, fig. 24 (26? 27? in explanation of plate on p. 250).

page 414 note 3 Cat. Brit. Foss.,” 2nd ed., 1854, p. 309.Google Scholar

page 414 note 4 M'Coy, F., “Synop. Carb. Foss. Ireland,” 1844, p. 17.Google Scholar

page 414 note 5 Cat. Foss. Ceph. British Museum.” pt. ii, 1891, p. 87.Google Scholar

page 414 note 6 Platnauer, H. M., “List of Figured Specimens in York Museum”: Ann. Rep. Yorks. Philos. Soc. 1890, p. 79.Google Scholar The locality there given (“Flaxby”) is an error; Mr. Platnauer informs me that it should have been “Flasby.”

page 414 note 7 B. M. No. C. 5336.

page 414 note 8 A specimen in the Gilbertson collection in the British Museum (No. C. 237c) is believed to be this figured example. It is but a fragment, and greatly resembles “Nautilus subsulcatus,” Phillips (=Clonautilus subsulcatus). It certainly does not agree with the specimen figured by Phillips in pl. xvii, fig. 24. The figure differs in some respects from the specimen. The periphero-lateral angles should have been represented more obtuse, and the suture-line with a narrower and shallower sinus on the periphery.

page 415 note 1 Nautilus quadratus, Fleming, J., “Hist. Brit. Anim.,” 1828, p. 231.Google Scholar

page 415 note 2 Morris, J., “Cat. Brit. Foss.,” 2nd ed., 1854, p. 303Google Scholar; Sharman, G. and Newton, E. T., “Geol. N. Derbyshire,” 2nd ed., 1887, Appendix 1, p. 182: Mem. Geol. Surv.Google Scholar; Etheridge, R., “Brit. Foss.”, vol. i, Palæozoic, 1888, p. 311Google Scholar; Morton, G. H., Proc. Liverpool Nat. Field Club for 1894, p. 23, 1895.Google Scholar

page 416 note 1 Hyatt, A., “Fossil Cephalopoda in the Museum of Comparative Zoology”: Proc. Amer. Assoc. for the advancement of Science, vol. xxxii, 1883, p. 333.Google Scholar

page 418 note 1 From Graig fawr, Prestatyn, Flintshire, and kindly sent to me for examination by Mr. G. H. Morton, F.G.S., Liverpool.

page 418 note 2 i.e. converging towards the plane of symmetry external to the periphery.

page 418 note 3 Sharman, G. and Newton, E. T., “Geol. N. Derbyshire,” 2nd ed., 1887, Appendix 1, p. 182: Mem. Geol. Surv.Google Scholar

page 418 note 4 Cumming, J. H., “Isle of Man,” 1848, p. 357.Google Scholar

page 418 note 5 Proc. Liverpool Nat. Field Club for 1894 (1895), p. 23.