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End-Ediacaran extinction : ウィキペディア英語版
End-Ediacaran extinction
Evidence suggesting that a mass extinction occurred at the end of the Ediacaran period, , includes:
*A mass extinction of acritarchs
*The sudden disappearance of the Ediacara biota and calcifying organisms;
*The time gap before Cambrian organisms "replaced" them.
==Pre-Ediacaran organisms==
During the Ediacaran period, two main groups of organisms are found in the fossil record: the "Ediacara biota" of soft-bodied organisms, preserved by microbial mats; and calcifying organisms such as ''Cloudina'' and ''Namacalathus'', which had a carbonate skeleton. Because ''both ''these groups disappear abruptly at the end of the Ediacaran period, , their disappearance cannot simply represent the closure of a preservational window, as had previously been suspected.〔

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
ウィキペディアで「End-Ediacaran extinction」の詳細全文を読む



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