II.—Description of a Fossil Shark (Ctenacanthus costellatus) from the Lower Carboniferous Rocks of Eskdale, Dumfriesshire

R. H. Traquair

doi:10.1017/S0016756800164416

Extract

The deficiency of our knowledge of the organization and configuration of the Palaeozoic Selachii is an unfortunate fact too well known to biologists to render it necessary for me to dilate upon here. Immense numbers of genera and species have been founded upon detached teeth and spines; but as yet very few specimens have occurred, which threw any light upon the general organization and configuration of the ancient possessors of these now scattered relics.

References

^{page 3 note 1} See A. Heim, Mechanismus der Gebirgsbilding, Band II. s. 17.Google Scholar

^{page 6 note 1} Poissons Fossiles, vol. iii. p. 23.Google Scholar

^{page 6 note 2} In connexion with the dentition of Tristychius, see a paper by Mr. T. Stock in Ann. and Mag. Nat. Hist. Sept. 1883.Google Scholar

^{page 7 note 1} Poissons Fossiles, vol. iii. p. 171.Google Scholar

^{page 7 note 2} Quart. Journ. Geol. Soc. 1853, p. 282.Google Scholar

^{page 7 note 3} Pal. Ohio, vol. ii. p. 54.Google Scholar

^{page 7 note 4} Ann. and Mag. Nat. Hist. (4) ix., 1872, p. 260.Google Scholar

^{page 7 note 5} Trans. Geol. Soc. Glasgow, vol. iv. (1861), p. 59–62.Google Scholar

^{page 7 note 6} Bull. Soc. Nat. Moscow, vol. xxxvii. (1864), pp. 157–170.Google Scholar

^{page 7 note 7} Proc. Koy. Soc. New South Wales, 3 Oct. 1881.Google Scholar

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II.—Description of a Fossil Shark (Ctenacanthus costellatus) from the Lower Carboniferous Rocks of Eskdale, Dumfriesshire

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II.—Description of a Fossil Shark (Ctenacanthus costellatus) from the Lower Carboniferous Rocks of Eskdale, Dumfriesshire

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