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Penetrative trace fossils from the late Ediacaran of Mongolia: early onset of the agronomic revolution
The Cambrian radiation of complex animals includes a dramatic increase in the depth and intensity of bioturbation in seafloor sediment known as the ‘agronomic revolution’. This bioturbation transition was coupled with a shift in dominant trace fossil style from horizontal surficial traces in the lat...
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| 出版年: | R Soc Open Sci |
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| 主要な著者: | , , , , , , , |
| フォーマット: | Artigo |
| 言語: | Inglês |
| 出版事項: |
The Royal Society Publishing
2018
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| 主題: | |
| オンライン･アクセス: | https://ncbi.nlm.nih.gov/pmc/articles/PMC5830798/ https://ncbi.nlm.nih.gov/pubmed/29515908 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1098/rsos.172250 |
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