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On the coevolution of Ediacaran oceans and animals

Fe speciation and S-isotope of pyrite data from the terminal Proterozoic Sheepbed Formation in Canada and Doushantuo Formation in China reveal that ocean deep waters were anoxic after the global glaciations (snowball Earth) ending 635 million years ago, but that marine sulfate concentrations and inf...

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Detalhes bibliográficos
Main Authors: Shen, Yanan, Zhang, Tonggang, Hoffman, Paul F.
Formato: Artigo
Idioma:Inglês
Publicado em: National Academy of Sciences 2008
Assuntos:
Acesso em linha:https://ncbi.nlm.nih.gov/pmc/articles/PMC2375388/
https://ncbi.nlm.nih.gov/pubmed/18469138
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.0802168105
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