Stable ocean redox during the main phase of the Great Ordovician Biodiversification Event
The period leading up to the Great Ordovician Biodiversification Event was characterised by stable marine anoxic zones with a substantial increase in atmospheric oxygen occurring only after this, according to uranium isotope analyses of marine carbonates from southern Sweden
| Main Authors: | , , , , , |
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| Format: | Article |
| Language: | English |
| Published: |
Nature Portfolio
2022-09-01
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| Series: | Communications Earth & Environment |
| Online Access: | https://doi.org/10.1038/s43247-022-00548-w |