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Acid rain, ozone depletion contributed to ancient extinction

Date:
November 22, 2013
Source:
Carnegie Institution
Summary:
Around 250 million years ago, at the end of the Permian period, there was a mass extinction so severe that it remains the most traumatic known species die-off in Earth's history. Some researchers have suggested that this extinction was triggered by contemporaneous volcanic eruptions in Siberia. New results show that the atmospheric effects of these eruptions could have been devastating.

Base of the Siberian Traps volcanic sequence along Kotuy River in Arctic Siberia.
Credit: Image courtesy of Carnegie Institution

Around 250 million years ago, at the end of the Permian period, there was a mass extinction so severe that it remains the most traumatic known species die-off in Earth's history. Some researchers have suggested that this extinction was triggered by contemporaneous volcanic eruptions in Siberia. New results from a team including Director of Carnegie's Department of Terrestrial Magnetism Linda Elkins-Tanton show that the atmospheric effects of these eruptions could have been devastating. Their work is published in Geology.

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The mass extinction included the sudden loss of more than 90 percent of marine species and more than 70 percent of terrestrial species and set the stage for the rise of the dinosaurs. The fossil record suggests that ecological diversity did not fully recover until several million years after the main pulse of the extinction.

One leading candidate for the cause of this event is gas released from a large swath of volcanic rock in Russia called the Siberian Traps. Using advanced 3-D modeling techniques, the team, led by Benjamin Black of the Massachusetts Institute of Technology, was able to predict the impacts of gas released from the Siberian Traps on the end-Permian atmosphere.

Their results indicate that volcanic releases of both carbon dioxide (CO2) and sulfur dioxide (SO2) could have created highly acidic rain, potentially leaching the soil of nutrients and damaging plants and other vulnerable terrestrial organisms. Releases of halogen-bearing compounds such as methyl chloride could also have resulted in global ozone collapse.

The volcanic activity was likely episodic, producing pulses of acid rain and ozone depletion. The team concluded that the resulting drastic fluctuations in pH and ultraviolet radiation, combined with an overall temperature increase from greenhouse gas emissions, could have contributed to the end-Permian mass extinction on land.

The team also included Jean-François Lamarque, Christine Shields, and Jeffrey Kiehl of the National Center for Atmospheric Research.


Story Source:

The above story is based on materials provided by Carnegie Institution. Note: Materials may be edited for content and length.


Journal Reference:

  1. B. A. Black, J.-F. Lamarque, C. A. Shields, L. T. Elkins-Tanton, J. T. Kiehl. Acid rain and ozone depletion from pulsed Siberian Traps magmatism. Geology, 2013; DOI: 10.1130/G34875.1

Cite This Page:

Carnegie Institution. "Acid rain, ozone depletion contributed to ancient extinction." ScienceDaily. ScienceDaily, 22 November 2013. <www.sciencedaily.com/releases/2013/11/131122165651.htm>.
Carnegie Institution. (2013, November 22). Acid rain, ozone depletion contributed to ancient extinction. ScienceDaily. Retrieved March 5, 2015 from www.sciencedaily.com/releases/2013/11/131122165651.htm
Carnegie Institution. "Acid rain, ozone depletion contributed to ancient extinction." ScienceDaily. www.sciencedaily.com/releases/2013/11/131122165651.htm (accessed March 5, 2015).

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