Unnamed 2nd series of the Cambrian
Cambrian Series 2 |
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A map of Earth 515 million years ago during the Cambrian's 2nd series, Stage 3 |
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−540 — – −535 — – −530 — – −525 — – −520 — – −515 — – −510 — – −505 — – −500 — – −495 — – −490 — – −485 — – | | | |
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| Subdivision of the Cambrian according to the ICS, as of 2023.[1]Vertical axis scale: Millions of years ago |
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Name formality | Informal |
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Celestial body | Earth |
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Regional usage | Global (ICS) |
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Time scale(s) used | ICS Time Scale |
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Chronological unit | Epoch |
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Stratigraphic unit | Series |
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Time span formality | Formal |
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Lower boundary definition | Not formally defined |
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Lower boundary definition candidates | FAD of Trilobites |
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Lower boundary GSSP candidate section(s) | None |
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Upper boundary definition | FAD of Oryctocephalus indicus. |
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Upper boundary GSSP | Wuliu-Zengjiayan, Guizhou, China 26°04′51″N 108°24′50″E / 26.0807°N 108.4138°E / 26.0807; 108.4138 |
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Upper GSSP ratified | 2018[2] |
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Cambrian Series 2 is the unnamed 2nd series of the Cambrian. It lies above the Terreneuvian series and below the Miaolingian. Series 2 has not been formally defined by the International Commission on Stratigraphy, lacking a precise lower boundary and subdivision into stages. The proposed lower boundary is the first appearance of trilobites which is estimated to be around 521 million years ago.[3][4]
- ^ "International Chronostratigraphic Chart" (PDF). International Commission on Stratigraphy. September 2023. Retrieved November 10, 2024.
- ^ Zhao; et al. (June 2019). "Global Standard Stratotype-Section and Point (GSSP) for the conterminous base of the Miaolingian Series and Wuliuan Stage (Cambrian) at Balang, Jianhe, Guizhou, China" (PDF). Episodes. 42: 165–184. Archived (PDF) from the original on 2022-03-04. Retrieved 2024-04-02.
- ^ "GSSP Table - Paleozoic Era". Archived from the original on 2023-10-08. Retrieved 2024-04-02.
- ^ Wu, Tong; Yang, Ruidong; Gao, Junbo; Li, Jun (1 January 2021). "Age of the lower Cambrian Vanadium deposit, East Guizhou, South China: Evidences from age of tuff and carbon isotope analysis along the Bagong section". Open Geosciences. 13 (1): 999–1012. doi:10.1515/geo-2020-0287. ISSN 2391-5447.