The issue is not just the increase in CO2 at the P/T boundary, but the unusual persistence of high CO2 levels for 5 million years. In contrast, the CO2 spike from the CAMP flood basalts lasted only 300 thousand years. The paper proposes that the ocean became enriched in dissolved silica due to the loss of silica-secreting microorganisms (as indicated by lack of chert deposits during this time), and that this caused enhanced "reverse weathering" that kept CO2 levels high.
https://pubs.geoscienceworld.org/gsa/geology/article/50/6/65...
The issue is not just the increase in CO2 at the P/T boundary, but the unusual persistence of high CO2 levels for 5 million years. In contrast, the CO2 spike from the CAMP flood basalts lasted only 300 thousand years. The paper proposes that the ocean became enriched in dissolved silica due to the loss of silica-secreting microorganisms (as indicated by lack of chert deposits during this time), and that this caused enhanced "reverse weathering" that kept CO2 levels high.