Carbon Emissions From Volcanic Rocks Can Create Global Warming

Greenhouse gas emissions released directly from the movement of volcanic rocks are capable of creating massive global warming effects.  (Image: via   pixabay  /  CC0 1.0)
Greenhouse gas emissions released directly from the movement of volcanic rocks are capable of creating massive global warming effects. (Image: via pixabay / CC0 1.0)

Greenhouse gas emissions released directly from the movement of volcanic rocks are capable of creating massive global warming effects — a discovery that could transform the way scientists predict climate change, a new study reveals.

Scientists’ calculations based on how carbon-based greenhouse gas levels link to movements of magma just below Earth’s surface suggest that such geological changes have caused the largest temporary global warming of the past 65 million years.

Large Igneous Provinces (LIPs) are extremely large accumulations of igneous rocks that occur when magma travels through the crust toward the surface. Geologists at the University of Birmingham have created the first mechanistic model of carbon emission changes during the Paleocene-Eocene Thermal Maximum (PETM) — a short interval of maximum temperature lasting around 100,000 years some 55 million years ago.

Scientists’ calculations based on how carbon-based greenhouse gas levels link to movements of magma just below earth’s surface suggest that such geological change has caused the largest temporary global warming of the past 65 million years. (Image: via pixabay / CC0 1.0)

Scientists’ calculations based on how carbon-based greenhouse gas levels link to movements of magma just below Earth’s surface suggest that such geological changes have caused the largest temporary global warming of the past 65 million years. (Image: via pixabay / CC0 1.0)

They published their findings in Nature Communications, after calculating carbon-based greenhouse gas fluxes associated with the North Atlantic Igneous Province (NAIP) — one of Earth’s largest LIPs that spans Britain, Ireland, Norway, and Greenland. Dr. Stephen Jones, Senior Lecturer in Earth Systems at the University of Birmingham, said:

The researchers’ simulations predict peak emissions flux of 0.2-0.5 PgC yr–1 and show that the NAIP could have initiated PETM climate change. Their work is the first predictive model of carbon emissions flux from any proposed PETM carbon source directly constrained by observations of the geological structures that controlled the emissions.

During PETM initiation, the release of 0.3–1.1 PgC yr–1 of carbon as greenhouse gases to the ocean-atmosphere system drove 4°-5°C of global warming over less than 20,000 years — a relatively short period of time.

During PETM initiation, release of 0.3–1.1 PgC yr–1 of carbon as greenhouse gases to the ocean-atmosphere system drove 4–5°C of global warming over less than 20,000 years - a relatively short period of time. (Image: via pixabay / CC0 1.0)

During PETM initiation, the release of 0.3–1.1 PgC yr–1 of carbon as greenhouse gases to the ocean-atmosphere system drove 4°-5°C of global warming over less than 20,000 years — a relatively short period of time. (Image: via pixabay / CC0 1.0)

Associations between LIPs and changes in global climate, ecosystems, and the carbon cycle during the Mesozoic period imply that greenhouse gases released directly by LIPs can initiate global change that persists over 10,000-100,000 years.

The PETM is the largest natural climate change event of Cenozoic time and is an important yardstick for theories explaining today’s long-term increase in the average temperature of Earth’s atmosphere as an effect of human industry and agriculture.

Provided by:  [Note: Materials may be edited for content and length.]

Follow us on Twitter or subscribe to our weekly email. Thanks.

Marcus Aurelius’ Meditations: Winning the Admiration of the Gods
Gamma-Ray Laser Moves a Step Closer to Reality