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Volcanic Mercury Implicated In Permian-Triassic Extinction Event Print E-mail
SciMed - Horizons
TS-Si News Service   
Sunday, 15 January 2012 04:00
Hamed Sanei.Calgary, Alberta, Canada. The influx of volcanic mercury into the ecosystem has been identified as possible new culprit likely involved in the Permian–Triassic extinction event.

Geologists estimate that the mercury released then could have been up to 30 times greater than today’s volcanic activity, making the event truly catastrophic.


Scientists have uncovered a lot about the Earth’s greatest extinction event that took place 250 million years ago when rapid climate change wiped out nearly all marine species and a majority of those on land. However, “No one had ever looked to see if mercury was a potential culprit. This was a time of the greatest volcanic activity in Earth’s history and we know today that the largest source of mercury comes from volcanic eruptions,” says co-author Dr. Steve Grasby, a research scientist at Natural Resources Canada and an adjunct professor at the University of Calgary.

This graphic shows historical variations of Mercury (Hg) deposition before and after the Latest Permian Extinction event 252.28 Ma (million years) ago, as recorded in a sedimentary section in the High Arctic, Canada. The vertical axis demonstrates the depth of the sedimentary section relative to the extinction boundary while the horizontal looks at the amount of mercury accumulation (concentration in the rock) as measured in milligram per kilogram. Image courtesy of Hamed Sanei, Steve Grasby and Benoit Beauchamp. (Sanei et al., 2012, Geology).
Click Pic for Details

The Mercury-Volcanic Link

This graphic shows historical variations of Mercury (Hg) deposition before and after the Latest Permian Extinction event 252.28 Ma (million years) ago, as recorded in a sedimentary section in the High Arctic, Canada.
Dr. Benoit Beauchamp, professor of geology at the University of Calgary, says this study is significant because it’s the first time mercury has been linked to the cause of the massive extinction that took place during the end of the Permian. “Geologists, including myself should be taking notes and taking another look at the other five big extinction events,” says Beauchamp, also a co-author of a paper published this month in the journal Geology.

During the late Permian, the natural buffering system in the ocean became overloaded with mercury contributing to the loss of 95 per cent of life in the sea. “Typically, algae acts like a scavenger and buries the mercury in the sediment, mitigating the effect in the oceans,” says lead-author Dr. Hamed Sanei, research scientist at Natural Resources Canada and an adjunct professor at the University of Calgary. “But in this case, the load was just so huge that it could not stop the damage.”

About 250 million years ago, a time long before dinosaurs ruled and when all land formed one big continent, themajority of life in the ocean and on land was wiped out. The generally accepted idea is that volcanic eruptions burned though coal beds, releasing CO2 and other deadly toxins. Direct proof of this theory was outlined in a paper that was published by these same authors last January in Nature Geoscience.

The mercury deposition rates could have been significantly higher in the late Permian when compared with today’s human-caused emissions. In some cases, levels of mercury in the late Permian ocean was similar to what is found near highly contaminated ponds near smelters, where the aquatic system is severely damaged, say researchers.

“We are adding to the levels through industrial emissions. This is a warning for us here on Earth today,” adds Beauchamp. Canada has taken a lead role in reducing emissions internationally. In North America, at least, there has been a steady decline through regulations controlling mercury.

No matter what happens, this study shows life’s tenacity. “The story is one of recovery as well. After the system was overloaded and most of life was destroyed, the oceans were still able to self clean and we were able to move on to the next phase of life,” says Sanei.

CitationLatest Permian mercury anomalies. Hamed Sanei, Stephen E. Grasby, and Benoit Beauchamp. Geology 2011; 40(1): 63-66. doi:10.1130/G32596.1

Abstract

A sedimentary record from the Buchanan Lake section, Canadian High Arctic, shows anomalous high levels of mercury (Hg) during the latest Permian extinction (LPE) on northwest Pangea. Significant influx of Hg progressively overwhelmed the marine system. Major disruption of the organic matter–mediated Hg drawdown process resulted in accumulation of dissolved Hg to maximum levels at the LPE boundary, affecting an already stressed global ecosystem. A switch to euxinic marine conditions at the LPE boundary led to chemical drawdown of Hg sulfides, as marked by progressive Hg mitigation. This allowed self-recovery from toxic Hg conditions, and ultimately led to reestablishment of the internal Hg–organic matter drawdown process. We hypothesize that anomalous Hg levels may be attributed to the significant natural atmospheric emissions caused by catastrophic Siberian Traps volcanic eruptions.

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Last Updated on Saturday, 14 January 2012 21:13