Avalon explosion

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The Avalon explosion (named from the Precambrian fauna of the Avalon Peninsula) is a proposed evolutionary event in the history of the Metazoa. It is the equivalent of the Cambrian explosion for the Ediacaran biota, and it happened around 33 million years earlier.

It was proposed by Virginia Tech paleontologists through the analysis of the morphological space change in several Ediacaran assemblages.[1] The discovery suggests that in the early evolution of animals, there may have been more than one explosive event.[2] The original analysis has been the subject of dispute in the literature.[3][4][5]

The Avalon explosion appears similar to the Cambrian explosion by the rapid increase in diversity of morphologies in a relatively small time frame, followed by diversification within the established body plans,[1][6] a pattern similar to that observed in other evolutionary events.[6]


  1. ^ a b Shen, B.; Dong, L.; Xiao, S.; Kowalewski, M. (2008). "The Avalon Explosion: Evolution of Ediacara Morphospace". Science 319 (5859): 81–84. doi:10.1126/science.1150279. PMID 18174439.  edit
  2. ^ "The Avalon Explosion". Astrobiology Magazine. January 8, 2008. Retrieved June 14, 2012. 
  3. ^ Freeman, G. (2009). "The rise of bilaterians". Historical Biology 21: 99–99. doi:10.1080/08912960903295843.  edit
  4. ^ Xiao, S.; Kowalewski, M.; Shen, B.; Dong, L.; Laflamme, M. (2009). "The rise of bilaterians: A reply". Historical Biology 21 (3–4): 239. doi:10.1080/08912960903471659.  edit
  5. ^ Freeman, G. (2010). "Comment on Xiao et al. (2009), response to: The rise of bilaterians". Historical Biology 22 (4): 430–432. doi:10.1080/08912960903562259.  edit
  6. ^ a b Xiao, S.; Laflamme, M. (January 2009). "On the eve of animal radiation: phylogeny, ecology and evolution of the Ediacara biota". Trends in Ecology and Evolution 24 (1): 31–40. doi:10.1016/j.tree.2008.07.015. PMID 18952316.  edit