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Doushantuo embryos preserved inside diapause egg cysts.

Leiming Yin1, Maoyan Zhu, Andrew H Knoll

  • 1State Key Laboratory of Paleobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing 210008, China. leimingyin@yahoo.com.cn

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Phosphatized microfossils from the Doushantuo Formation are likely early animal embryos, not bacteria. These early cleavage-stage embryos were found preserved within organic vesicles, providing evidence of animal life after Neoproterozoic glaciation.

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Area of Science:

  • Paleontology
  • Geology
  • Developmental Biology

Background:

  • Ediacaran Doushantuo Formation microfossils have been debated as early animal embryos.
  • Previous research confirmed embryo preservation but lacked definitive evidence for Doushantuo fossils.
  • Alternative hypotheses suggested these microfossils were giant sulfur-oxidizing bacteria.

Observation:

  • New observations reveal embryo-like Doushantuo fossils within large, ornamented organic vesicles (acritarchs).
  • These acritarchs contained structures indicative of eukaryotic cells.
  • Large, spiny microfossils containing these potential embryos appear in strata above a 632.5 Myr old ash bed.

Findings:

  • The presence of Doushantuo fossils within acritarchs strongly supports their eukaryotic origin.
  • The findings indicate these microfossils represent early cleavage-stage embryos within diapause egg cysts.
  • This provides compelling evidence against the giant sulfur-oxidizing bacteria hypothesis.

Implications:

  • Confirms Doushantuo microfossils as early animal embryos, resolving phylogenetic questions.
  • Suggests that stem-group animals existed in shallow seas shortly after Neoproterozoic glaciation.
  • Enhances understanding of early animal evolution and preservation biases in the fossil record.