Chicxulub Impact-Induced Vaporization: S and C Species and Their Affect on Global Climate

Physics

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Chicxulub, Devolatilization, Extinction, Global Climate/Aerosols, Impacts: Cretaceous-Tertiary

Scientific paper

Thick deposits of anhydrite at the Chicxulub impact site suggests that large quantities of sulfur oxides were released during the impact event. Oxidation of sulfur oxides emplaced in the stratosphere would produce long-lived sulfuric acid aerosols capable of substantially cooling Earth's surface. Recent radiative transfer modeling shows that a stratospheric H2SO4 loading of 5 Gt of sulfur is capable of reducing solar transmission below the photosynthesis limit of the biosphere, provided i) the sulfuric acid aerosols contain sufficient impurities, and ii) the reduction in solar transmission lasts for a sufficiently long time. Such calculations raise several questions: 1) How much impact-liberated S is transported to the stratosphere?; 2) Is S primarily in the form of SO2 or SO3?; 3) Are the required impurity levels plausible?. Each of these questions is addressed below. In general, the answers support the sulfuric acid aerosol scenario of Pope et al.

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