2024 Study Traces 10-Km Dinosaur-Killing Asteroid to Beyond Jupiter
Updated
Updated · spacedaily.com · Aug 1
2024 Study Traces 10-Km Dinosaur-Killing Asteroid to Beyond Jupiter
3 articles · Updated · spacedaily.com · Aug 1
Summary
A 2024 Science study tied the Chicxulub impactor to the outer solar system, concluding the asteroid that struck Earth 66 million years ago formed beyond Jupiter.
Ruthenium isotopes from impact-layer samples in Denmark, Italy and Spain matched carbonaceous chondrites, pointing to a primitive outer-system asteroid rather than a comet or inner-system rock.
That impactor was estimated at 10 to 15 kilometers wide and carved the 180-kilometer Chicxulub crater in today’s Yucatán, helping drive an extinction that killed roughly three-quarters of species.
Researchers say the finding is strong but not final, because it rests on one geochemical tracer even as multiple lines of evidence had already established the impact itself.
Objects this large are thought to hit only every tens of millions of years, and no known large near-Earth asteroid is currently on a collision course with Earth.
If the dinosaur-killing asteroid originated beyond Jupiter, what violent cosmic event hurled this dark rock directly toward our planet?
Since primitive chondrites carry organics, did the exact rock that ended the dinosaurs also deliver crucial building blocks for future life?
Could the apocalyptic crater that wiped out 75% of life have secretly incubated new microbial ecosystems in its boiling hydrothermal vents?
The Chicxulub Impactor Unveiled: How Rare CO Chondrites from the Outer Solar System Caused Earth’s Last Mass Extinction and What It Means for Planetary Defense
Overview
Around 66 million years ago, a massive space rock struck Earth, creating the Chicxulub crater and triggering a chain of catastrophic events. The impact pulverized both the asteroid and Earth's surface, sending ultra-fine silicate dust high into the atmosphere. This dust stayed aloft for up to 15 years, blocking sunlight, cooling the planet by as much as 15°C, and causing a near-total shutdown of photosynthesis for almost two years. This collapse of primary productivity led to the starvation and extinction of about 75% of all species, including the dinosaurs. Recent isotopic studies revealed the impactor was a rare, low-sulfur CO carbonaceous chondrite, meaning sulfur aerosols played a smaller role than previously thought, and the dust shroud was the main driver of extinction.