Article contents
I.—The Gigantic Ceratopsidæ, or Horned Dinosaurs, of North America1
Published online by Cambridge University Press: 01 May 2009
Extract
Two years ago at the Bath Meeting of the British Association, I had the honour to present a paper in which I compared the principal known Dinosaurs of Europe with those of America. In this communication I referred to some peculiar reptilian remains from the Gosau formation of Austria, and compared them with certain Laramie fossils from America, about which I hoped soon to have more definite information. As an indication of the rapidity with which knowledge of ancient life is advancing, it may be interesting to know what has been learned in two years concerning this single group of the remarkable reptiles known as Dinosauria. This group I have termed the Ceratopsidæ, and I shall refer especially to the forms I have recently investigated, and hope to describe more fully later on, under the auspices of the United States Geological Survey.
- Type
- Original Articles
- Information
- Copyright
- Copyright © Cambridge University Press 1891
Footnotes
Read before Section C, of the British Association for the Advancement of Science, at the Leeds Meeting, September 4, 1890. See also American Journal of Science (3), vol. xxxvi. p. 477, December, 1888; vol. xxxviii. p. 334, April, 1889; vol. xxxviii. p. 173. August, 1889, p. 501. December, 1889; and vol. xxxix. p. 81, January. 1890, P. 418, May, 1890.
References
page 193 note 2 For Plate IV. see the April Number GEOL. MAG.
page 193 note 3 Report of the British Association for the Advancement of Science for 1888, p. 660. London. 1889.Google Scholar Abstract, American Journal (3), vol. xxxvii. p. 323, 04, 1889.Google Scholar See also GEOL. MAG. 1890, pp. 1–5, and Pl. I.Google Scholar
page 194 note 1 Plate IV. appeared in the April Number, 1891; Plate V. is in the present Number.
page 194 note 2 The name usually applied to this aperture is misleading, as in Chameleo and some other reptiles the foramen is not in or near the parietal bones. It may more properly be called the “pineal foramen.”
- 2
- Cited by