Dynamic ocean redox conditions during the end-Triassic mass extinction: Evidence from pyrite framboids
(2022)
Journal Article
Li, J., Song, H., Tian, L., Bond, D. P., Song, H., Du, Y., Zhang, C., Chu, D., Wignall, P. B., & Tong, J. (2022). Dynamic ocean redox conditions during the end-Triassic mass extinction: Evidence from pyrite framboids. Global and planetary change, 218, Article 103981. https://doi.org/10.1016/j.gloplacha.2022.103981
The end-Triassic (∼201 Mya) records one of the five largest mass extinction events of the Phanerozoic. Extinction losses were coincident with large igneous province volcanism in the form of the Central Atlantic Magmatic Province (CAMP) and major carb... Read More about Dynamic ocean redox conditions during the end-Triassic mass extinction: Evidence from pyrite framboids.