Geologists find parallels between ancient, global-scale extinction events and modern threats to Earth’s oceans.
A series of mass extinctions that rocked the Earth’s oceans during the Devonian Period over 300 million years ago may have been triggered by the evolution of tree roots. This is according to a research study led by scientists at Indiana University–Purdue University Indianapolis (IUPUI), along with colleagues in the United Kingdom.
Evidence for this new view of a remarkably volatile period in Earth’s pre-history was reported on November 9 in the scientific journal Geological Society of America Bulletin. It is one of the oldest and most respected publications in the field of geology. 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.
“Our analysis shows that the evolution of tree roots likely flooded past oceans with excess nutrients, causing massive algae growth,” Filippelli said. “These rapid and destructive algae blooms would have depleted most of the oceans’ oxygen, triggering catastrophic mass extinction events.”
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. Credit: John Marshall, University of Southampton
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 percent 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 fueling broad “dead zones” in the Great Lakes and the Gulf of Mexico, as excess nutrients from fertilizers and other agricultural runoff trigger massive algae blooms that consume all of the water’s oxygen.
The difference is that these past events were likely fueled 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.
Gabrielle Filippelli. Credit: Liz Kaye, Indiana University
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 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.
Matthew Smart. Credit: Photo courtesy Matthew Smart
“It’s not easy to peer over 370 million years into the past,” said Smart. “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.”
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 fertilizers, 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.
“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,” Fillipelli said.
