Salinity changes and anoxia resulting from enhanced run-off during the late Permian global warming and mass extinction event
The late Permian biotic crisis had a major impact on marine and terrestrial environments. Rising CO<sub>2</sub> levels following Siberian Trap volcanic activity were likely responsible for expanding marine anoxia and elevated water temperatures. This study focuses on one of the strati...
| Main Authors: | , , |
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| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2018-04-01
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| Series: | Climate of the Past |
| Online Access: | https://www.clim-past.net/14/441/2018/cp-14-441-2018.pdf |