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 (3)
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Brasier, M. D.
Right arrow Articles by Antcliffe, J. B.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation
Journal of the Geological Society; 2009; v. 166; issue.2; p. 363-384;
DOI: 10.1144/0016-76492008-011
© 2009 Geological Society of London

Research Article

Evolutionary relationships within the Avalonian Ediacara biota: new insights from laser analysis

Martin D. Brasier & Jonathan B. Antcliffe

Department of Earth Sciences, University of Oxford, Parks Road, Oxford OX1 3PR, UK

Corresponding author (e-mail: martinb{at}earth.ox.ac)

We report new high-resolution laser scanning of the type material for the earliest, complex Ediacaran genera Charnia, Bradgatia, Charniodiscus and Ivesheadia from Charnwood, UK, and compare these with Beothukis mistakensis gen. et sp. nov. and the recently described taxa Charnia wardi, Charnia antecedens and Fractofusus spp. from broadly coeval strata in Newfoundland. We use the laser and other techniques to map the similarities and differences in morphology between these Ediacaran rangeomorphs. Key features are suggested to include the number of growth axes, the number and placement of growth tips, the presence of radiating or subparallel axes for the first- and higher-order branches, the extent of displayed or undisplayed leaf-like ’rangeomorph' architecture, and the extent of furling of the margins of these leaf-like elements. These features are then used to propose suggested homologies between these taxa, leading to a preliminary phylogenetic hypothesis for the evolution of the Avalonian Ediacara biota.





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 the Geological SocietyHome page
D. McILROY, M. D. BRASIER, and A. S. LANG
Smothering of microbial mats by macrobiota: implications for the Ediacara biota
Journal of the Geological Society, 2009; 166: 1117 - 1121.
[Abstract] [Full Text] [PDF]


Home page
Journal of PaleontologyHome page
E. L. BAMFORTH and G. M. NARBONNE
NEW EDIACARAN RANGEOMORPHS FROM MISTAKEN POINT, NEWFOUNDLAND, CANADA
Journal of Paleontology, 2009; 83: 897 - 913.
[Abstract] [Full Text] [PDF]


Home page
Journal of PaleontologyHome page
G. M. NARBONNE, M. LAFLAMME, C. GREENTREE, and P. TRUSLER
RECONSTRUCTING A LOST WORLD: EDIACARAN RANGEOMORPHS FROM SPANIARD'S BAY, NEWFOUNDLAND
Journal of Paleontology, 2009; 83: 503 - 523.
[Abstract] [Full Text] [PDF]