There are several LIPs around the world, but each has its own unique characteristics and external factors around it. Which are the most important to control the after effects and of colonization and why some with high distresses potential do not achieve the expected for the dimensions of these provinces (e.g. Deccan, Siberian Traps, CAMP, Karoo and PEMP).
In the following paper it was calculated Carbon-based greenhouse gas fluxes associated with the North Atlantic Igneous Province magma at sub-millennial resolution by linking measurements of the mantle convection process that generated NAIP magma.
“Large Igneous Province thermogenic greenhouse gas flux could have initiated Paleocene-Eocene Thermal Maximum climate change”. Nature Communications Volume 10, Article number: 5547 (2019).
https://www.nature.com/articles/s41467-019-12957-1
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