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Ediacaran macroscopic ecosystems

Large, complex organisms became conspicuous in late Neoproterozoic seas before the Cambrian diversification of skeletonized animals.

Represented range575–538.8 Ma
RegionsGlobal marine shelves
CladesEdiacaran organisms · early animals

Claim ledger

fossil-range · high

CA–ID–TIMS U–Pb ages bracket the Gaskiers glaciation, and Avalon fossils appear in younger strata by about 571 Ma; this directly dates a regional assemblage, not the origin of animals or a global Ediacaran first appearance.

claim:event:ediacaran-biota

References

  1. Dodging snowballs: Geochronology of the Gaskiers glaciation and the first appearance of the Ediacaran biotaPu, J.P.; Bowring, S.A.; Ramezani, J.; Myrow, P.; Raub, T.D.; Landing, E.; Mills, A.; Hodgin, E.; Macdonald, F.A. · 2016 · DOI 10.1130/G38284.1
  2. The Ediacara biota: Neoproterozoic origin of animals and their ecosystemsNarbonne, G.M. · 2005 · DOI 10.1146/annurev.earth.33.092203.122519
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