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Sedimentology and chemostratigraphy of the terminal Ediacaran Dengying Formation at the Gaojiashan section, South China
The late Ediacaran Dengying Formation (ca. 551.1–538.8 Ma) in South China is one of two successions where Ediacara-type macrofossils are preserved in carbonate facies along with skeletal fossils and bilaterian animal traces. Given the remarkable thickness of carbonate-bearing strata deposited in les...
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| Vydáno v: | Geol Mag |
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| Hlavní autoři: | , , , , , |
| Médium: | Artigo |
| Jazyk: | Inglês |
| Vydáno: |
2019
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| Témata: | |
| On-line přístup: | https://ncbi.nlm.nih.gov/pmc/articles/PMC6800678/ https://ncbi.nlm.nih.gov/pubmed/31631899 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1017/S0016756819000293 |
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