Role of degassing of the Noril'sk nickel deposits in the Permian-Triassic mass extinction event
Proceedings of the National Academy of Sciences of the United States of America , Volume 114 - Issue 10 p. 2485- 2490
The largest mass extinction event in Earth's history marks the boundary between the Permian and Triassic Periods at circa 252 Ma and has been linked with the eruption of the basaltic Siberian Traps large igneous province (SLIP). One of the kill mechanisms that has been suggested is a biogenic methane burst triggered by the release of vast amounts of nickel into the atmosphere. A proposed Ni source lies within the huge Noril'sk nickel ore deposits, which formed in magmatic conduits widely believed to have fed the eruption of the SLIP basalts. However, nickel is a nonvolatile element, assumed to be largely sequestered at depth in dense sulfide liquids that formed the orebodies, preventing its release into the atmosphere and oceans. Flotation of sulfide liquid droplets by surface attachment to gas bubbles has been suggested as a mechanism to overcome this problem and allow introduction of Ni into the atmosphere during eruption of the SLIP lavas. Here we use 2D and 3D X-ray imagery on Noril'sk nickel sulfide, combined with simple thermodynamic models, to show that the Noril'sk ores were degassing while they were forming. Consequent "bubble riding" by sulfide droplets, followed by degassing of the shallow, sulfide-saturated, and exceptionally volatile and Cl-rich SLIP lavas, permitted a massive release of nickel-rich volcanic gas and subsequent global dispersal of nickel released from this gas as aerosol particles.
|Proceedings of the National Academy of Sciences of the United States of America|
|Organisation||Department of Earth Sciences|
Le Vaillant, M. (Margaux), Barnes, S.J. (Stephen J.), Mungall, J.E, & Mungall, E.L. (Emma L.). (2017). Role of degassing of the Noril'sk nickel deposits in the Permian-Triassic mass extinction event. Proceedings of the National Academy of Sciences of the United States of America, 114(10), 2485–2490. doi:10.1073/pnas.1611086114