New research suggests the evolution of tree roots during the Devonian Period could have led to mass extinctions
The evolution of tree roots may have triggered a series of mass extinctions that rocked the Earth’s oceans during the Devonian Period over 300 million years ago, according to a study led by scientists at IUPUI, along with colleagues in the United Kingdom.
The study was led by Gabriel Filippelli, Chancellor’s Professor of Earth Sciences in the School of Science at IUPUI, and Matthew Smart, a Ph.D. student in his lab at the time of the study.
Filipelli said: “Our analysis shows that the evolution of tree roots likely flooded past oceans with excess nutrients, causing massive algae growth. These rapid and destructive algae blooms would have depleted most of the oceans’ oxygen, triggering catastrophic mass extinction events.”
The Devonian Period, which occurred 419 million to 358 million years ago, prior to the evolution of Life on land, is known for mass extinction events, during which it’s estimated nearly 70% of all Life on Earth perished.
The process outlined in the study – known scientifically as eutrophication – is remarkably similar to modern, albeit smaller-scale, phenomenon currently fuelling broad ‘dead zones’ in the Great Lakes and the Gulf of Mexico, as excess nutrients from fertilisers and other agricultural run-off trigger massive algal blooms that consume all of the water’s oxygen.
The difference is that these past events were likely fuelled by tree roots, which pulled nutrients from the land during times of growth, then abruptly dumped them into the Earth’s water during times of decay.
The theory is based upon a combination of new and existing evidence, Filippelli said.
tree root growth
Based upon a chemical analysis of stone deposits from ancient lake beds – whose remnants persist across the globe, including the samples used in the study from sites in Greenland and off the northeast coast of Scotland – the researchers were able to confirm previously identified cycles of higher and lower levels of phosphorus, a chemical element found in all Life on Earth.
They were also able to identify wet and dry cycles based upon signs of ‘weathering’ – or soil formation – caused by tree root growth, with greater weathering indicating wet cycles with more roots and less weathering indicating dry cycles with fewer roots.
Most significantly, the team found the dry cycles coincided with higher levels of phosphorous, suggesting dying roots released their nutrients into the planet’s water during these times.
Smart said: “It’s not easy to peer over 370 million years into the past, but rocks have long memories, and there are still places on Earth where you can use chemistry as a microscope to unlock the mysteries of the ancient world.”
extinction events
In light of the phosphorus cycles occurring at the same time as the evolution of the first tree roots – a feature of Archaeopteris, also the first plant to grow leaves and reach heights of 30 feet – the researchers were able to pinpoint the decay of tree roots as the prime suspect behind the Devonian Periods extinction events.
Fortunately, Filippelli said, modern trees don’t wreak similar destruction as Nature has since evolved systems to balance out the impact of rotting wood. The depth of modern soil also retains more nutrients compared to the thin layer of dirt that covered the ancient Earth.
But the dynamics revealed in the study shed light on other newer threats to Life in Earth’s oceans. The study’s authors note that others have made the argument that pollution from fertilisers, manure and other organic wastes, such as sewage, have placed the Earth’s oceans on the ‘edge of anoxia’, or a complete lack of oxygen.
Filipelli concluded: “These new insights into the catastrophic results of natural events in the ancient world may serve as a warning about the consequences of similar conditions arising from human activity today.”
The study was reported in the Geological Society of America Bulletin.
Image: Scientists collect rock samples on Ymer Island in eastern Greenland, one of several sites whose analysis provided insight into the chemical makeup of lake beds in the Devonian Period. © John Marshall, University of Southampton.
