Hostname: page-component-586b7cd67f-t7czq Total loading time: 0 Render date: 2024-11-30T16:09:42.969Z Has data issue: false hasContentIssue false

V.—Notes on the British Graptolites and their Allies

Published online by Cambridge University Press:  01 May 2009

Extract

In the following communication I intend to give a very brief outline of some of the chief results of my investigations among British Graptolites in those departments of inquiry which are more especially connected with consideratious of classification. I shall content myself with offering a concise statement of the main conclusions at which I have arrived, reserving all detail to the future, when I hope to adduce decisive evidence in support of the views here advanced. The special subjects to be noticed in this place are—the development, structure, classification, and geological distribution of that section of the Rhabdo-phora in which the complete polypary can be proved to be composed of one or more polyparies essentially similar to that in the unilateral and uniserial forms to which the name Graptolites (Graptolithus) is commonly applied. Those Rhabdophora supposed to be similar in structure to the genus Retiolites will be considered in conjunction, but no pretension is made to anything like the same certainty in this section.

Type
Original Articles
Copyright
Copyright © Cambridge University Press 1873

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 501 note 1 The sicula is probably identical with that portion of the polypary which Herr Richter has termed the “foot.” See Appendix.

page 501 note 2 See Appendix.