Sixty-six million years ago, an asteroid roughly the size of Malta slammed into the Yucatán Peninsula in Mexico.
The cataclysmic impact, and its immediate aftermath, obliterated over three-quarters of the Earth’s species. All dinosaurs, bar birds, met their end.
The picture of what happened next has, until now, been sketchy. Remains from the immediate aftermath of what’s known as the K-T (for Cretaceous-Tertiary) extinction are hard to come by.
But an analysis of extraordinary deposits in Colorado, published in the journal Science, tracks life in exquisite detail over the crucial first million years after the K-T extinction
“If you had to choose one million years in Earth’s history that you really want to look at carefully, this would be it,” says palaeobotanist Ian Miller from the Denver Museum of Nature & Science.
The Denver Basin, an area extending eastwards from Denver in the north and Colorado Springs in the south, is not new to palaeontologists, who have been exploring the area for over 100 years. But in 2016, Tyler Lyson from the Denver Museum changed the way he searched for fossils at Corral Bluffs in the southern part of the basin.
Instead of scanning the landscape for bones poking out of the ground, Lyson, who led the new study, looked for concretions – egg-shaped rocks that can form around fossils.
“That’s how we cracked the code and blew it wide open. I split open a concretion and saw a mammal skull smiling back at me,” he says. “Then I looked around and saw concretions just littering the landscape and was like, ‘Oh man, here we go’.”
Lyson and his colleagues unearthed thousands of fossils from mammals, reptiles and plants at Corral Bluffs, in sites that span the first million years after the mass extinction. These, along with pollen samples, were then used to reconstruct the process of ecosystem recovery that took place.
The work shows that during the first 100,000 years, mammals were already beginning to diversify.
At 300,000 years after the asteroid struck, mammals got bigger, too. Maximum body size increased three-fold and was accompanied by an increase in diversity of large plants.
More large animals crop up around 700,000 years post-extinction, at a time that energy-rich plants, such as legumes, first appear in the record.
Both of these bursts in plant and animal life coincided with pulses of warming.
“We documented changes in the landscape after the impact, from a world dominated by palms to a world dominated by a more diverse group of trees. And then we saw the animal species change in lockstep fashion,” says Miller.
“Their record is particularly strong in that it is really densely sampled through that first million years,” says palaeontologist Tom Williamson from the New Mexico Museum of Natural History & Science, who wasn’t involved in the study. “We can’t say that for really anywhere else, so that is pretty spectacular.”
It will be interesting, Williamson adds, to see if they can get similar records from elsewhere in western North America, including in the San Juan Basin where he works.
Originally published by Cosmos as How mammals inherited the Earth
Dyani Lewis is a freelance science journalist based in Melbourne, Australia.
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