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Large spinose microfossils in Ediacaran rocks as resting stages of early animals
Large (>100 μm), profusely ornamented microfossils comprise a distinctive paleontological component of sedimentary rocks deposited during the Ediacaran Period (635–542 million years ago). Smaller spinose fossils in Paleozoic rocks have commonly been interpreted as algal cysts or phycomata, but th...
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| Main Authors: | , , |
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| Formáid: | Artigo |
| Teanga: | Inglês |
| Foilsithe: |
National Academy of Sciences
2009
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| Ábhair: | |
| Rochtain Ar Líne: | https://ncbi.nlm.nih.gov/pmc/articles/PMC2672526/ https://ncbi.nlm.nih.gov/pubmed/19366668 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.0902322106 |
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