U-Pb ages from the neoproterozoic Doushantuo Formation, China.

@article{Condon2005UPbAF,
  title={U-Pb ages from the neoproterozoic Doushantuo Formation, China.},
  author={Daniel J Condon and Maoyan Zhu and S. P. K. Bowring and Wei Wang and Aihua Yang and Yugan Jin},
  journal={Science},
  year={2005},
  volume={308 5718},
  pages={95-8}
}
U-Pb zircon dates from volcanic ash beds within the Doushantuo Formation (China) indicate that its deposition occurred between 635 and 551 million years ago. The base records termination of the global-scale Marinoan glaciation and is coeval with similar dated rocks from Namibia, indicating synchronous deglaciation. Carbon isotopic and sequence-stratigraphic data imply that the spectacular animal fossils of the Doushantuo Formation are for the most part younger than 580 million years old. The… CONTINUE READING
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