550-million-year-old creatures’ message to the present.
Earth is currently in the midst of a mass extinction, losing thousands of species each year. New research suggests environmental changes caused the first such event in history, which occurred millions of years earlier than scientists previously realized.
“We’ve shown a true decrease in the abundance of organisms.” — Chenyi Tu
Most dinosaurs famously disappeared 66 million years ago at the end of the Cretaceous period. Prior to that, a majority of Earth’s creatures were snuffed out between the Permian and Triassic periods, roughly 252 million years ago.
Thanks to the efforts of researchers at the University of California, Riverside (UCR) and Virginia Tech, it’s now known that a similar extinction occurred 550 million years ago, during the Ediacaran period. This discovery is documented in a Proceedings of the National Academy of Sciences paper.
Although unclear whether this represents a true “mass extinction,” the percentage of organisms lost is similar to these other events, including the current, ongoing one.
The researchers believe environmental changes are to blame for the loss of approximately 80% of all Ediacaran creatures, which were the first complex, multicellular life forms on the planet.
“Geological records show that the world’s oceans lost a lot of oxygen during that time, and the few species that did survive had bodies adapted for lower oxygen environments,” said Chenyi Tu, UCR paleoecologist and study co-author.
Unlike later events, this earliest one was more difficult to document because the creatures that perished were soft-bodied and did not preserve well in the fossil record.
“We suspected such an event, but to prove it we had to assemble a massive database of evidence,” said Rachel Surprenant, UCR paleoecologist, and study co-author. The team documented nearly every known Ediacaran animal’s environment, body size, diet, ability to move, and habits.
With this project, the researchers sought to disprove the charge that the major loss of animal life at the end of the Ediacaran period was something other than an extinction. Some previously believed the event could be explained by the right data not being collected, or a change in animal behavior, like the arrival of predators.
“We can see the animals’ spatial distribution over time, so we know they didn’t just move elsewhere or get eaten — they died out,” said Chenyi. “We’ve shown a true decrease in the abundance of organisms.”
They also tracked creatures’ surface area to volume ratios, a measurement that suggests declining oxygen levels were to blame for the deaths. “If an organism has a higher ratio, it can get more nutrients, and the bodies of the animals that did live into the next era were adapted in this way,” said UCR paleoecologist Heather McCandless, study co-author.
This project came from a graduate class led by UCR paleoecologist Mary Droser and her former graduate student, now at Virginia Tech, Scott Evans. For the next class, the students will investigate the origin of these animals, rather than their extinction.
Ediacaran creatures would be considered strange by today’s standards. Many of the animals could move, but they were unlike anything now living. Among them were Obamus coronatus, a disc-shaped creature named for the former president, and Attenborites janeae, a tiny ovoid resembling a raisin named for English naturalist Sir David Attenborough.
“These animals were the first evolutionary experiment on Earth, but they only lasted about 10 million years. Not long at all, in evolutionary terms,” Droser said.
Though it’s not clear why oxygen levels declined so precipitously at the end of the era, it is clear that environmental change can destabilize and destroy life on Earth at any time. Such changes have driven all mass extinctions including the one currently occurring.
“There’s a strong correlation between the success of organisms and, to quote Carl Sagan, our ‘pale blue dot,’” said Phillip Boan, UC Riverside geologist and study co-author.
“Nothing is immune to extinction. We can see the impact of climate change on ecosystems and should note the devastating effects as we plan for the future,” Boan said.
Reference: “Environmental drivers of the first major animal extinction across the Ediacaran White Sea-Nama transition” by Scott D. Evans, Chenyi Tu, Adriana Rizzo, Rachel L. Surprenant, Phillip C. Boan, Heather McCandless, Nathan Marshall, Shuhai Xiao and Mary L. Droser, 7 November 2022, Proceedings of the National Academy of Sciences.
Very interesting, would like to hear more.
Two to three billion years ago, the first mass extinctions was the extinction of the anaerobic bacteria. They were victims of pollution, when cyanobacteria produced so much oxygen that most of the anaerobic bacteria could not survive.
A painstaking research into the animal world with a view to preserving endangered species and biodiversity generally. I warmly recommend this masterpiece for students inclining towards biogeography, zoology, ecology, and environmental planning and protection.
A painstaking research into the natural environment with a view to preserving endangered species and biodiversity generally. I warmly recommend this masterpiece for students inclining towards biogeography, zoology, ecology, and environmental planning and protection.
“Earth is currently in the midst of a mass extinction, losing thousands of species each year.”
That is undocumented, is guesswork… and is nonsense. Taxonomists are describing new species every year. Listing thousands of species as “endangered” is not extinction.
And, to compound the problem, the temporal resolution of events several hundred million years ago is very poor compared today. Furthermore, fossilization is a rather rare event so ancient rates of extinction are problematic.
There have been some recent announcements of creatures that were thought to have become extinct, and living specimens were found. The classic example is the coelacanth, which had been thought to be extinct since the end of the Cretaceous, 65 million years ago. A living specimen was captured off the coast of Madagascar in 1938. One can have declines in population or range, without becoming extinct.
“Geological records show that the world’s oceans lost a lot of oxygen during that time.” ???
The only way that oxygen can be lost is to have a “sink” for it. And there is none during the Ediacaran. In fact all of the sediments that preserve nothing but impressions are strongly oxidized. The organic matter is gone!
Ag chemicals have consequences.