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Main page appearance: Ediacara biota
This is a note to let the main editors of Ediacara biota know that the article will be appearing as today's featured article on June 13, 2012. You can view the TFA blurb at Today's featured article/June 13, 2012. If you prefer that the article appear as TFA on a different date, or not at all, please ask featured article director or his delegate, or start a discussion at Wikipedia talk:Today's featured article/requests. If the previous blurb needs tweaking, you might change it—following the instructions at Today's featured article/requests/instructions. If this article needs any attention or maintenance, it would be preferable if that could be done before its appearance on the Main Page. The blurb as it stands now is below:



The Ediacara biota consisted of enigmatic tubular and frond-shaped, mostly sessile organisms which lived during the Ediacaran Period (c. 635–542 Ma). Trace fossils of these organisms have been found worldwide, and represent the earliest known complex multicellular organisms. The Ediacara biota radiated in an event called the Avalon Explosion,, after the Earth had thawed from the Cryogenian period's extensive glaciation, and largely disappeared contemporaneous with the rapid appearance of biodiversity known as the Cambrian explosion. Most currently existing body-plans of animals first appeared only in the fossil record of the Cambrian rather than the Ediacaran. For macroorganisms, the Cambrian biota completely replaced the organisms that populated the Ediacaran fossil record. (more...) UcuchaBot (talk) 23:01, 12 June 2012 (UTC)

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