Quick
Search: 
 
advanced search
 GSW Home    GeoRef Home    My GSW Alerts    Contact GSW    About GSW    Journals List    Help 
  Journal of the Geological Society   Signup for GSW Email News
JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS

Journal of the Geological Society; August 1992; v. 149; no. 4; p. 631-636; DOI: 10.1144/gsjgs.149.4.0631
© 1992 Geological Society of London
This Article
Right arrow Full Text (PDF)
Right arrow References
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 reprints & permissions
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by CONWAY MORRIS, S.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Article

Burgess Shale-type faunas in the context of the ‘Cambrian explosion’: a review

S. CONWAY MORRIS

Department of Earth Sciences, University of Cambridge, Downing Street, Cambridge CB2 3EQ, UK

Burgess Shale-type faunas are now known from almost 40 lower and middle Cambrian localities, although those from British Columbia (Canada), Yunnan (China) and Peary Land (Greenland) are of paramount significance. The diverse faunas are dominated by animals with an otherwise negligible fossilization potential, and their stratigraphical position makes them of unique importance in documenting the major adaptive radiations at this time (‘Cambrian explosion’).

Important features of these faunas include the presence of taxa surviving from the late Precambrian Ediacaran faunas, the discovery of articulated material that throws new light on scleritome organization in various Cambrian skeletal taxa, and the significance of the degree of anatomical disparity among Cambrian animals. In addition, these soft-bodied faunas offer some hope of reconciling soft-part data with trace fossil occurrences. New discoveries of Burgess Shale-type faunas are inevitable, and such finds will continue to enhance our under­standing of early animal evolution.




This article has been cited by other articles:


Home page
Geological Society, London, Special PublicationsHome page
R. J. F. Jenkins and C. Nedin
The provenance and palaeobiology of a new multi-vaned, chambered frondose organism from the Ediacaran (later Neoproterozoic) of South Australia
Geological Society, London, Special Publications, January 1, 2007; 286(1): 195 - 222.
[Abstract] [Full Text] [PDF]


Home page
Journal of PaleontologyHome page
A NEW SOFT-BODIED FAUNA: THE PIOCHE FORMATION OF NEVADA
Journal of Paleontology, July 1, 2003; 77(4): 674 - 690.





JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 2009 by Geological Society of London