Methane-Eating Bacteria Discovered Deep Beneath Antarctic Ice Sheet Could be Curbing Global Warming

Updated | Bacteria that eat methane, a greenhouse gas, have been discovered in an Antarctic lake that has been isolated from the atmosphere for thousands of years. Their presence could significantly reduce the potential risk of warming posed by reservoirs of gas locked up in the ice, scientists say.

Scientists found the bacteria by drilling in Lake Whillans, a large body of water located 800 meters (2,600 feet) underneath the West Antarctic ice sheet. After the team successfully broke through the ice sheet in 2013, they collected water and sediment samples—deposited about 120,000 years ago—from this long-hidden lake.

Their analysis of the samples, published in Nature Geoscience, revealed bacteria that digest methane. The microbes were in the upper lake sediment, indicating they prevent the greenhouse gas from entering the water—ensuring this Earth-heating compound is then unable to reach the ocean and escape into the atmosphere.

Methane is far more potent than carbon dioxide, another greenhouse gas. Made of hydrogen and carbon, its warming effects have a shorter duration but are much stronger than carbon dioxide. According to the Intergovernmental Panel on Climate Change, the planet-heating of methane is 86 times greater than that of carbon dioxide.  

Scientists believe a major methane reservoir lies beneath the West Antarctic ice sheet, in addition to the huge amount held within the permanently frozen ground of the Arctic permafrost. Climate scientists are concerned that as global temperatures increase, methane released from warmed permafrost will cause additional warming—potentially resulting in runaway climate change. The bacteria that eat this chemical could be preventing its release into the atmosphere, limiting global warming in the process.

antarctic A NASA image of the Antarctic. Scientists have found methane-eating bacteria 800 meters beneath the West Antarctic ice sheet. NASA

Consuming methane is a matter of survival for these bacteria. Cut off from heat and sunlight, they turn to this gas for energy. “Bacterial oxidation consumes [more than] 99 percent of the methane and represents a significant methane sink,” the scientific team wrote. 

Understanding the vast systems of lakes and rivers beneath the Antarctic ice sheet is important to climate science. But these ecologies are still largely unexplored, making it difficult to predict how much methane they might release in the future. According to the study authors, vast “microbial ecosystems capable of cycling important greenhouse gases” exist beneath the Antarctic ice.

“It took more than a decade of scientific and logistical planning to collect the first clean samples from an Antarctic subglacial environment, but the results have transformed the way we view the Antarctic continent,” study co-author John Priscu, a polar scientist and professor in Montana State University’s Department of Land Resources and Environmental Sciences said in a statement.

Concluding, the team wrote, “The bacterial conversion of [methane] to [carbon dioxide] beneath the West Antarctic ice sheet reduces the warming potential of subglacial gases that may be released to downstream ice sheet margin environments and to the atmosphere during episodes of ice sheet retreat.”

This story has been updated with a correction to the elements that make up methane. An earlier version included an error introduced during the editing process. 

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