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Impact winter and the Cretaceous/Tertiary extinctions: Results of a Chicxulub asteroid impact model
Abstract
The Chicxulub impact crater in Mexico is the site of the impact purported to have caused mass extinctions at the Cretaceous/Tertiary (K/T) boundary. 2-D hydrocode modeling of the impact, coupled with studies of the impact site geology, indicate that between 0.4 and 7.0 x 10(17) g of sulfur were vaporized by the impact into anhydrite target rocks. A small portion of the sulfur was released as SO3 or SO4, which converted rapidly into H2SO4 aerosol and fell as acid rain. A radiative transfer model, coupled with a model of coagulation indicates that the aerosol prolonged the initial blackout period caused by impact dust only if the aerosol contained impurities. A larger portion of sulfur was released as SO2, which converted to aerosol slowly, due to the rate-limiting oxidation of SO2. Our radiative transfer calculations, combined with rates of acid production, coagulation, and diffusion indicate that solar transmission was reduced to 10-20% of normal for a period of 8-13 yr. This reduction produced a climate forcing (cooling) of -300 Wm-2, which far exceeded the +8 Wm-2 greenhouse warming, caused by the CO2 released through the vaporization of carbonates, and therefore produced a decade of freezing and near-freezing temperatures. Several decades of moderate warming followed the decade of severe cooling due to the long residence time of CO2. The prolonged impact winter may have been a major cause of the K/T extinctions.
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“Given that the hypothesized (25) asteroid-induced cooling likely drove the extinction, a pulse of warming (with a similar magnitude as shown in our simulations) (9) just prior to the extinction may have acted as a buffer against cooling induced by the Chicxulub impact, ameliorating the physical effects of bolide impact (41).”
From Asteroid impact, not volcanism, caused the end-Cretaceous dinosaur extinction (2020) · cites this paper as [25]
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Research works printed but not linked: 30
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Cited by
Asteroid impact, not volcanism, caused the end-Cretaceous dinosaur extinction
Chiarenza, A. A., Farnsworth, A., Mannion, P. D., Lunt, D. J., Valdes, P. J., Morgan, J. V., & Allison, P. A. (2020) · Proceedings of the National Academy of Sciences · doi:10.1073/pnas.2006087117 · Cited by 228
Metadata
- Authors
- Pope, K. O., Baines, K. H., Ocampo, A. C., & Ivanov, B. A.
- Venue
- Earth and Planetary Science Letters
- Publisher
- Elsevier BV
- Published
- 1994-12
- Volume
- 128
- Issue
- 3-4
- Pages
- 719-725
- ISSN
- 0012-821X
- Cited by
- 145
- References
- 0
- Language
- en
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