Global ocean redox changes before and during the Toarcian Oceanic Anoxic Event
Geochemical modeling shows that just a several percent expansion of O2-free areas with toxic sulfide build-up likely contributed to biodiversity loss or reorganization during the Toarcian mass extinction 183 million years ago.
| Main Authors: | , |
|---|---|
| Format: | Article |
| Language: | English |
| Published: |
Nature Portfolio
2023-02-01
|
| Series: | Nature Communications |
| Online Access: | https://doi.org/10.1038/s41467-023-36516-x |