The Cambrian explosion more than 500 million years ago is often considered biology’s “big bang”.
Virtually all the major kinds of animals evolved in life’s greatest ever burst of evolution, rapidly populating a weird and biologically sparse planet with everything from jellyfish to vertebrates, and turning it into the Earth we recognise today.
But our recent study, published this week in PNAS, shows this burst of rapid evolutionary innovation also ended surprisingly quickly.
Animals took perhaps only 20 million years to fill most of the empty ecological niches (ways to make a living) on our entire planet. From then on, the pace of evolution slowed drastically, reverting to rates considered more normal and which have held sway for most of the subsequent 520 million years up to the present.
Our work suggests that evolution can fill even huge ecological vacuums extremely rapidly.
This has implications given the widespread global changes currently being wrought by humans. Ecological niches are being destroyed and created more rapidly than at any time since the mass extinction that killed the dinosaurs 66 million years ago.
The largest adaptive radiation of all time
Adaptive radiation is when a species finds itself surrounded by empty niches, and rapidly evolves into a range of different species with different lifestyles (such as herbivores or carnivores) to fill the entire vacuum.
As the environment becomes saturated, evolution gradually slows down to normal rates. Famous examples of adaptive radiation include marsupials in Australia and anole lizards in the Caribbean.
The biggest adaptive radiation of all is the Cambrian Explosion. Life first appeared at least 3.5 billion years ago, but for the subsequent 3 billion years little more than microbes and simple blobs existed.
At (or shortly before) the start of the Cambrian Period (541 million years ago), modern animals evolved. They rapidly diversified into all the major groups (phyla) of animals we see today, such as jellyfish and corals, segmented worms (such as earthworms), molluscs (such as snails), arthropods (such as crabs), and even vertebrates (backboned animals, which eventually included ourselves).
The strange-yet-familiar evolutionary products of the Cambrian period are exquisitely preserved in spectacular fossil sites around the world, such as the Burgess Shale in Canada and Chengjiang in China. Australia has its own: the Emu Bay Shale on Kangaroo Island.
There is widespread agreement that evolution must have been turbocharged during the Cambrian explosion. But we didn’t really know for sure how long this unprecedented burst of rapid innovation and adaptation lasted.
If sustained across most of the Cambrian Period (which stretches from 541 million to 485 million years ago), then this would suggest that animals took more than 50 million years to fill up our planet.
Over in a (geological) eyeblink
Our study is the most thorough and mathematically precise measurement of evolution across the Cambrian Period.
Evolutionary rates are usually hard to calculate, partly because of the patchy fossil record. The complicated chain of events required for a dead organism to turn to stone means most carcasses are lost to time.
There are certainly rare instances where an evolving population is preserved across successively younger deposits, providing irrefutable evidence of evolution-in-action. More often, though, we find (say) a jaw bone in one place, followed by a limb bone on a different continent that is millions of years younger.
We circumvented the patchiness of the Cambrian fossil record in two ways. First, we focused on the dominant creatures of the Cambrian, the trilobites (an extinct group of marine arthropods related to other jointed-legged creatures like crabs, spiders and insects).
Trilobites are diverse and abundant (giving us a large and dense sample of fossils to work with), and also have very complex, robustly mineralised exoskeletons or “shells” (giving us lots of anatomical traits to measure).
When faced with incomplete data, these methods don’t try to do the impossible and spit out a single precise answer. Rather, they cleverly infer the universe of probable answers given the fuzzy information at hand.
Our study reveals that evolution had subsided to the more normal rates within the early Cambrian – by at least 520 million years ago. Thus, the Cambrian explosion was over much earlier than many had suspected, indeed almost as soon as the first trilobites appeared.
If modern animals first evolved at the very beginning of the Cambrian, then their global adaptive radiation took a mere 20 million years.
While this is still substantial, it represents only 0.5% of the 3.5-billion-year history of life on Earth: a surprisingly brief interval to fill the Earth with body plans as disparate as starfish, snails, shrimps and fish.
Life finds a way
The rapid rise of animals suggested by our study emphasises the ability of evolution to quickly take advantage of every opportunity.
The Cambrian explosion represented the first time animals evolved to fill the planet. Since then, several mass extinctions – such as the meteorite impact that contributed to the extinction the non-avian dinosaurs and much else – have partially cleared the decks.
Every time, life has rebounded rapidly.
Today, as humans transform and stress our planet, we are facing another mass extinction. Evolutionary niches are being destroyed and created at a rate faster than at any time since the dinosaur age.
The rapidity of evolution in the past might lead to optimism that life might adapt to the worst that humans can throw at it.
But this artificially rapid global change might be too fast for many species. Furthermore, much of the rapid evolution triggered by humans is far from desirable.
Swallows that evolve wingshapes to better manoeuvre through heavy traffic might be cute. But superbugs resistant to every known antibiotic, and subterranean mosquitos adapted to feast on London tube commuters, are less so!
Mike Lee received funding for this research from the Australian Research Council and Flinders University
Greg Edgecombe receives funding from the Leverhulme Trust.
John Paterson receives funding from the Australian Research Council.