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
Google Scholar
Right arrow Articles by McILROY, D.
Right arrow Articles by LANG, A. S.
GeoRef
Right arrow GeoRef Citation
Journal of the Geological Society; 2009; v. 166; issue.6; p. 1117-1121;
DOI: 10.1144/0016-76492009-073
© 2009 Geological Society of London

Research Article

Smothering of microbial mats by macrobiota: implications for the Ediacara biota

DUNCAN McILROY1, MARTIN D. BRASIER2 & ANDREW S. LANG3

1 Department of Earth Sciences, Memorial University, St. John's, Newfoundland, NL A1B 3X5, Canada
2 Department of Earth Sciences, Parks Road, Oxford University OX1 3PR, UK
3 Department of Biology, Memorial University, St. John's, Newfoundland, NL A1B 3X5, Canada

*Corresponding author (e-mail: dmcilroy{at}mun.ca)

Recent advances in understanding the preservation of the soft-bodied Neoproterozoic Ediacara biota have centred upon the role of microbes in casting the morphologies of static or dead macrobiota on the Precambrian sea floor. This experimental study explores the preservational effects brought about by the passive movement of dead macro-organisms upon a pre-established marine microbial mat under laboratory conditions. This demonstrates the potential for making multiple impressions of body tissues on the surface of microbial mats by means of passive transport alone. This throws doubt on the evidence for active feeding in Ediacaran fossils such as Dickinsonia and Yorgia.

Supplementary material: Methods are available at http://www.geolsoc.org.uk/SUP18375.





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]