Deep CO₂ in the end-Triassic Central Atlantic Magmatic Province.

ABSTRACT: Large Igneous Province eruptions coincide with many major Phanerozoic mass extinctions, suggesting a cause-effect relationship where volcanic degassing triggers global climatic changes. In order to fully understand this relationship, it is necessary to constrain the quantity and type of degassed magmatic volatiles, and to determine the depth of their source and the timing of eruption. Here we present direct evidence of abundant CO₂ in basaltic rocks from the end-Triassic Central Atlantic Magmatic Province (CAMP), through investigation of gas exsolution bubbles preserved by melt inclusions. Our results indicate abundance of CO₂ and a mantle and/or lower-middle crustal origin for at least part of the degassed carbon. The presence of deep carbon is a key control on the e

SUBMITTER: Capriolo M 

PROVIDER: S-EPMC7138847 | biostudies-literature | 2020 Apr

REPOSITORIES: biostudies-literature