A fossil discovery has revealed that complex ecosystems existed on Earth much earlier than previously thought
The discovery challenges our understanding of how quickly Life recovered from the greatest mass extinction in Earth’s history
About 250 million years ago, the Permian-Triassic mass extinction killed over 80% of the planet’s species.
In the aftermath, scientists believe that Life on Earth was dominated by simple species for up to ten million years before more complex ecosystems could evolve.
A fossilised ocean ecosystem
Until now, scientists have long theorised that scorching hot ocean conditions resulting from catastrophic climate change prevented the development of complex Life after the mass extinction.
This idea is based on geochemical evidence of ocean conditions at the time. Now the discovery of fossils dating back 250.8 million years near the Guizhou region of China suggests that complex ecosystems were present on Earth just one million years after the Permian-Triassic mass extinction, which is much earlier than previously thought.
Morgann Perrot, a former postdoctoral researcher at McGill University, now at Université du Québec à Montréal, said: “The fossils of the Guizhou region reveal an ocean ecosystem with diverse species making up a complex food chain that includes plant life, bony fish, ray-finned fish, crabs, lobsters, shrimp, and molluscs.
“In all, our team discovered 12 classes of organisms and even found fossilised faeces, revealing clues about the diets of these ancient animals.”
challenging an age-old theory
Previously, it was thought that complex ecosystems would need five to ten million years to evolve after an extinction.
However, the researchers found that the specimens in the Guizhou region evolved much quicker than that by using radiometric dating to date the rocks where the fossils were discovered.
Perrot, whose research focuses on Earth sciences and geochronology, added: “All of this has implications for our understanding of how quickly Life can respond to extreme crises. It also necessitates a re-evaluation of early Triassic ocean conditions.”
Image 1: Field photo of a Watsonulus fish fossil from the Gaopo section.
Image 2: Rocks from the Guizhou region, deposited at the bottom of an ancient ocean during the Permian-Triassic transition and containing the newly discovered fossils (Gujiao section).
Image 3: Field photo of a Coelacanth fish fossil from the Gujiao section.