© MARK GARLICK/SCIENCE PHOTO LIBRARY/Getty ImagesThe re-establishment of species diversity following an extinction event is consistently slower than evolutionary theory predicts.
Yet, the paleontological record suggests that this doesn't happen at anywhere near the expected pace. Now, research published in the journal Nature Ecology and Evolution argues that understanding something called "morphospace" might help us find the cause.
Extinction events happen with alarming regularity: there's the "big five", but a host of slightly smaller, yet still devastating extinctions have peppered the planet's history.
Scientists now worry that we might be in the middle of one of our own making, so this makes it all the more important to understand how the natural world bounces back from such catastrophes.
Perhaps the most well-known of the earth's mass extinctions is the Cretaceous-Paleogene (K-Pg) extinction event. This took place 66 million years ago when an asteroid smacked into the earth next to what is now the Yucatán Peninsula, creating the nearly 200-kilometre-wide depression known as the Chicxulub crater. This impact drove the extinction of all the non-avian dinosaurs, and much else besides.
Comment: A daytime meteor was also seen earlier that day over Alabama, Florida, Georgia, Kentucky, North Carolina, South Carolina, Tennessee and Virginia