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Originally published in Science Express on 15 July 2004
Science 20 August 2004:
Vol. 305. no. 5687, pp. 1141 - 1144
DOI: 10.1126/science.1099727
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Reports

Modular Construction of Early Ediacaran Complex Life Forms

Guy M. Narbonne

Newly discovered, exceptionally preserved, soft-bodied fossils near Spaniard's Bay in eastern Newfoundland exhibit features not previously described from Ediacaran (terminal Neoproterozoic) fossils. All of the Spaniard's Bay taxa were composed of similar architectural elements—centimeter-scale frondlets exhibiting three orders of fracticality in branching. Frondlets were combined as modules atop semi-rigid organic skeletons to form a wide array of larger constructions, including frondose and plumose structures. This architecture and construction define the "rangeomorphs," a biological clade that dominated the Mistaken Point assemblage (575 to 560 million years ago) but does not appear to be ancestral to any Phanerozoic or modern organisms.

Department of Geological Sciences and Geological Engineering, Queen's University, Kingston, Ontario K7L 3N6, Canada. E-mail: narbonne{at}geol.queensu.ca

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THIS ARTICLE HAS BEEN CITED BY OTHER ARTICLES:
Growth and Ecology of a Multi-branched Ediacaran Rangeomorph from the Mistaken Point Assemblage, Newfoundland.
E. L. Bamforth, G. M. Narbonne, and M. M. Anderson (2008)
Journal of Paleontology 82, 763-777
   Abstract »    Full Text »    PDF »
EDIACARAN BIOTA ON BONAVISTA PENINSULA, NEWFOUNDLAND, CANADA.
H. J. HOFMANN, S. J. O'BRIEN, and A. F. KING (2008)
Journal of Paleontology 82, 1-36
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Charnia and sea pens are poles apart.
J. B. Antcliffe and M. D. Brasier (2007)
Journal of the Geological Society 164, 49-51
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The provenance and palaeobiology of a new multi-vaned, chambered frondose organism from the Ediacaran (later Neoproterozoic) of South Australia.
R. J. F. Jenkins and C. Nedin (2007)
Geological Society, London, Special Publications 286, 195-222
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Discoidal fossils of the Ediacaran biota: a review of current understanding.
B. A. MacGabhann (2007)
Geological Society, London, Special Publications 286, 297-313
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Poriferan paraphyly and its implications for Precambrian palaeobiology.
E. A. Sperling, D. Pisani, and K. J. Peterson (2007)
Geological Society, London, Special Publications 286, 355-368
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The nature of vendobionts.
A. Seilacher (2007)
Geological Society, London, Special Publications 286, 387-397
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Lower Cambrian vendobionts from china and early diploblast evolution..
D.-G. Shu, S. C. Morris, J. Han, Y. Li, X.-L. Zhang, H. Hua, Z.-F. Zhang, J.-N. Liu, J.-F. Guo, Y. Yao, et al. (2006)
Science 312, 731-734
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Historical contingency and the purported uniqueness of evolutionary innovations.
G. J. Vermeij (2006)
PNAS 103, 1804-1809
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A re-examination of the Nama-type Vendian organism Rangea schneiderhoehni.
D. GRAZHDANKIN and A. SEILACHER (2005)
Geological Magazine 142, 571-582
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A uniquely preserved Ediacaran fossil with direct evidence for a quilted bodyplan.
S. Xiao, B. Shen, C. Zhou, G. Xie, and X. Yuan (2005)
PNAS 102, 10227-10232
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U-Pb sensitive high-resolution ion microprobe ages from the Doushantuo Formation in south China: Constraints on late Neoproterozoic glaciations.
S. Zhang, G. Jiang, J. Zhang, B. Song, M. J. Kennedy, and N. Christie-Blick (2005)
Geology 33, 473-476
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Tempo and mode of early animal evolution: inferences from rocks, Hox, and molecular clocks.
K. J. Peterson, M. A. McPeek, and D. A. D. Evans (2005)
Paleobiology 31, 36-55
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Science. ISSN 0036-8075 (print), 1095-9203 (online)