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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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| 主要な著者: | , , |
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| フォーマット: | Artigo |
| 言語: | Inglês |
| 出版事項: |
National Academy of Sciences
2008
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| 主題: | |
| オンライン･アクセス: | 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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