New research shows the Chicxulub asteroid impact 66 million years ago generated an impermeable fine-dust cloud that trapped thermal radiation near Earth’s surface, creating extreme heat conditions and global wildfires that far exceeded earlier temperature models and devastated terrestrial life.
When the roughly six-mile-wide asteroid struck Mexico’s Yucatán Peninsula 66 million years ago, it did far more than carve out the massive Chicxulub crater and unleash earthquakes and tsunamis. Scientists once suspected that a brutal, years-long winter starved the dinosaurs in the aftermath. New research paints a far more violent picture of the immediate aftermath, suggesting that an atmospheric blanket of fine debris baked the planet’s surface within hours.
How Fine Dust Turned Thermal Radiation Into an Oven
The impact released energy equivalent to 1023 joules, hurling more than 1,000 cubic kilometers of rock and vapor into space. As that material reentered Earth’s atmosphere, molten droplets known as spherules separated from vaporized rock and fell back down at several miles per second. Friction with the atmosphere generated intense heat during their descent, creating a global thermal pulse.
Earlier calculations treated this falling material as a global broiler that was deadly to thin-skinned animals but too weak to ignite widespread vegetation. However, a study published in the Journal of Geophysical Research: Biogeosciences by researchers at Purdue University and the University of Colorado, Boulder, points to a missing ingredient: a thick layer of fine silicate dust.
“We found that the cloud layer was so impermeable that it trapped almost all of the heat from the falling spherules near the surface of the planet. The dust is essentially acting like a lid on a pot.”
Alexandria Johnson, Purdue University
Evidence for this impact-derived dust layer emerged in 2023 at the Tanis fossil site in North Dakota, where researchers identified fine material deposited directly above the spherules. Additional documentation surfaced at the K–Pg boundary in the Raton Basin across the Colorado–New Mexico border.
Lethal Heat Pulses and the Origins of Global Wildfires
This dust blanket prevented thermal radiation from escaping into space, redirecting intense heat toward Earth’s surface. Planetary scientist Brandon Johnson of Purdue University noted that the kinetic energy from the collision had to go somewhere, and it ultimately converted into severe surface heat.
“We’re in the realm where we might be essentially killing off everything within that first hour or two.”
Brandon Johnson, planetary scientist at Purdue University
The resulting surface heat pulse was roughly 3.5 times more intense than models that factored in falling spherules alone. Exposed terrestrial animals may have received thermal doses about 17 times higher than the limit considered lethal to humans. While the radiation might not have directly ignited thick timber, it easily exceeded ignition thresholds for grass, lichen, and pine needles. That triggered massive fires across the landscape, though physical wildfire evidence of this scale currently remains confined to North America, as noted by University College London paleontologist Alfio Alessandro Chiarenza.
Contrasting Theories on the Chicxulub Impact Structure
The physical nature of the Chicxulub impact itself has also faced re-evaluation regarding whether the disaster started with a single rock or a twin strike. Earlier research and computer simulations led by Katarina Miljković at the Institute of Earth Physics in Paris indicate that binary asteroids can generate single craters if the two rocks are close enough upon impact.

Because about 15 per cent of near-Earth asteroids are binary, simulations suggest Earth experiences binary impacts more often than the crater record shows. Petr Pravec of the Academy of Sciences of the Czech Republic pointed out that recent gravity surveys of the buried Chicxulub crater reveal distinct asymmetries, supporting the hypothesis that the site may stem from a binary impactor measuring 7 to 10 kilometers in combined diameter.
Survival Strategies and the Long Impact Winter
Creatures that survived the initial hours of intense thermal radiation and wildfires faced a bleak environment.

Only animals able to burrow, swim, or shelter in water had a meaningful chance of surviving the initial heat pulse. Afterward, the very same atmospheric dust that trapped heat lingered for years or decades, blocking sunlight and ushering in the prolonged impact winter that ultimately eradicated roughly 75% of Earth’s plant and animal species.
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