Hostname: page-component-6bf8c574d5-vmclg Total loading time: 0 Render date: 2025-02-16T17:01:47.482Z Has data issue: false hasContentIssue false
  • English
  • Français

The Use of Graphs in Palaeontology

Published online by Cambridge University Press:  01 May 2009

H. H. Swinnerton
H. H. Swinnerton
Affiliation:
University College, Nottingham
Get access Rights & Permissions [Opens in a new window]

Extract

To illustrate the value of graphic methods when changes in a number of distinct structural elements are studied, examples may be taken from the Carboniferous corals. These are well suited to the purpose, because thin slices yield so much information and are easily measured. In Fig. 4 a diagrammatic section is shown of one of the most highly organized corals, which exhibits the following important structural units: epitheca, tabulæ, septa, dissepiments, tabellæ, lamellæ, columella.

Type
Original Articles
Information
Geological Magazine , Volume 58 , Issue 9 , September 1921 , pp. 397 - 408
Copyright
Copyright © Cambridge University Press 1921

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

page 400 note 1 Vaughan, , Quart. Journ. Geol. Soc., vol. lxi, 1905, p. 183.Google Scholar

page 400 note 2 Carruthers, , Geol. Mag., 1908, p. 158.CrossRefGoogle Scholar

page 402 note 1 Carruthers, , Quart. Journ. Geol. Soc., vol. lxvi, 1910, p.523.CrossRefGoogle Scholar

page 404 note 1 Vaughan, , Quart. Journ. Geol. Soc., vol. lxxi, 1915, p. 36.Google Scholar

page 407 note 1 Osborn, H. F., American Naturalist, 1917, p. 449.CrossRefGoogle Scholar

page 408 note 1 Osborn, , Bull. Amer. Mus. Nat. Hist., 1902, pp. 77–89.Google Scholar