Lyell Collection
Journal of the Geological Society
Lyell Centre  |   Lyell Collection  |   Subscriptions   |   Geological Society  |   Email alerts  |   Online bookshop  |   Help

Keywords:
Author:
Advanced search>>
This Article
Right arrow Figures Only
Right arrow Full Text
Right arrow Full Text (PDF)
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Right arrow Citation Map
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow Request Permissions
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via Web of Science (8)
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Antcliffe, J. B.
Right arrow Articles by Brasier, M. D.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation
Journal of the Geological Society; 2007; v. 164; issue.1; p. 49-51;
DOI: 10.1144/0016-76492006-080
© 2007 Geological Society of London

Short Communication

Charnia and sea pens are poles apart

Jonathan B. Antcliffe & Martin D. Brasier

Department of Earth Sciences, University of Oxford, Parks Road, Oxford OX1 3PR, UK(e-mail: jonathanantcliffe@univ.ox.ac.uk)

Charnia from the Ediacara biota is here examined in terms of its growth and development. The Ediacara biota comes from the critical period of evolution just before the Cambrian Explosion and is key to our understanding of the origin of animal life. We show that Charnia cannot be related to the modern cnidarian group the sea pens (Pennatulacea) with which it has for so long been compared, as generative zones cannot be homologized between these forms.





This article has been cited by other articles:


Home page
 GeologyHome page
A. G. Liu, D. Mcllroy, and M. D. Brasier
First evidence for locomotion in the Ediacara biota from the 565 Ma Mistaken Point Formation, Newfoundland
Geology, 2010; 38: 123 - 126.
[Abstract] [Full Text] [PDF]

Home page
 Journal of PaleontologyHome page
B. SHEN, S. XIAO, C. ZHOU, and X. YUAN
YANGTZIRAMULUS ZHANGI NEW GENUS AND SPECIES, A CARBONATE-HOSTED MACROFOSSIL FROM THE EDIACARAN DENGYING FORMATION IN THE YANGTZE GORGES AREA, SOUTH CHINA
Journal of Paleontology, 2009; 83: 575 - 587.
[Abstract] [Full Text] [PDF]

Home page
 Journal of the Geological SocietyHome page
M. D. Brasier and J. B. Antcliffe
Evolutionary relationships within the Avalonian Ediacara biota: new insights from laser analysis
Journal of the Geological Society, 2009; 166: 363 - 384.
[Abstract] [Full Text] [PDF]

Home page
 Journal of PaleontologyHome page
E. L. Bamforth, G. M. Narbonne, and M. M. Anderson
Growth and Ecology of a Multi-branched Ediacaran Rangeomorph from the Mistaken Point Assemblage, Newfoundland
Journal of Paleontology, 2008; 82: 763 - 777.
[Abstract] [Full Text] [PDF]

Home page
 Phil Trans R Soc BHome page
G. E Budd
The earliest fossil record of the animals and its significance
Phil Trans R Soc B, 2008; 363: 1425 - 1434.
[Abstract] [Full Text] [PDF]

Home page
 Geological Society, London, Special PublicationsHome page
J. B. Antcliffe and M. D. Brasier
Towards a morphospace for the Ediacara biota
Geological Society, London, Special Publications, 2007; 286: 377 - 386.
[Abstract] [Full Text] [PDF]