Ocean waters prevent release of ancient methane

January 17, 2018, University of Rochester
Katy Sparrow ’17 (PhD) and John Kessler collaborated with researchers from several universities, as well as researchers from the US Geological Survey and the National Oceanic and Atmospheric Administration. From left to right: Kathryn Schreiner, assistant professor of chemistry and biochemistry (Univ. of Minnesota Duluth); PhD candidate Fenix Garcia-Tigreros (UR); Sparrow; and Kessler, associate professor of earth and environmental sciences, aboard the research vessel in Prudhoe Bay, Alaska. Credit: University of Rochester photo / John Kessler

Ocean sediments are a massive storehouse for the potent greenhouse gas methane.

Trapped in ocean sediments near continents lie ancient reservoirs of called . These ice-like water and methane structures encapsulate so much methane that many researchers view them as both a potential energy resource and an agent for environmental change. In response to warming ocean waters, hydrates can degrade, releasing the methane gas. Scientists have warned that release of even part of the giant reservoir could significantly exacerbate ongoing climate change.

However, methane only acts as a greenhouse gas if and when it reaches the —a scenario that would occur only if the liberated methane travelled from the point of release at the seafloor to the surface waters and the atmosphere.

With that in mind, environmental scientist Katy Sparrow '17 (PhD) set out to study the origin of methane in the Arctic Ocean.

"While a logical suspect for arctic is degrading hydrates, there are several other potential methane sources. Our goal was to fingerprint the source of methane in the Arctic Ocean to determine if ancient methane was being liberated from the seafloor and if it survives to be emitted to the atmosphere," says Sparrow, who conducted the study, published in Science Advances, as part of her doctoral research at the University of Rochester.

Sparrow; her advisor, John Kessler, an associate professor of earth and environmental sciences; and a team of scientists from the Universities of Rochester, California Irvine, Minnesota Duluth, and Colorado Boulder, as well as the US Geological Survey and the National Oceanic and Atmospheric Administration, conducted fieldwork just offshore of the North Slope of Alaska, near Prudhoe Bay. Sparrow calls the spot "ground zero" for oceanic methane emissions resulting from ocean warming. In some parts of the Arctic Ocean, the shallow regions near continents may be one of the settings where methane hydrates are breaking down now due to warming processes over the past 15,000 years. In addition to methane hydrates, carbon-rich permafrost that is tens of thousands of years old—and found throughout the Arctic on land and in seafloor sediments—can produce methane once this material thaws in response to warming. With the combination of the aggressive warming occurring in the Arctic and the shallow water depths, any released methane has a short journey from emission at the seafloor to release into the atmosphere.

The researchers used radiocarbon dating to fingerprint the origin of methane from their samples. By employing a technique they developed that involves collecting methane from roughly ten thousand gallons of seawater per sample, they made a surprising discovery: ancient-sourced methane is indeed being released into the ocean; but very little survives to be emitted to the atmosphere, even at surprisingly shallow depths.

"We do observe ancient methane being emitted from the seafloor to the overlying seawater, confirming past suspicions," Kessler says. "But, we found that this ancient methane signal largely disappears and is replaced by a different methane source the closer you get to the surface waters." The methane at the surface is instead from recently produced organic matter or from the atmosphere.

Although the researchers did not examine in this study what prevents methane released from the seafloor from reaching the atmosphere, they suspect it is biodegraded by microorganisms in the ocean before it hits the surface waters. Mihai Leonte, a PhD candidate in Kessler's research group, observed this process—in which microbes aggressively biodegrade methane as methane emissions increase—in a paper published last year.

"We found that very little ancient methane reaches surface waters even in the relatively shallow depths of 100 feet. Exponentially less methane would be able to reach the atmosphere in waters that are thousands of feet deep at the very edge of the shallow seas near continents, which is the area of the where the bulk of methane hydrates are," Sparrow says. "Our data suggest that even if increasing amounts of methane are released from degrading hydrates as climate change proceeds, catastrophic emission to the atmosphere is not an inherent outcome."

Sparrow and Kessler's results on the role of ancient methane sources are consistent with the findings of their Rochester colleague Vasilii Petrenko, an associate professor of earth and environmental sciences, who also radiocarbon dated methane. However, while Sparrow and Kessler dated methane found in modern-day seawater, Petrenko radiocarbon dated methane from the ancient atmosphere that was preserved in the ice of Arctic glaciers.

"Petrenko and his co-authors studied a rapid warming event from the past that serves as a modern-day analog," Sparrow says. "They found that the emissions of methane from ancient methane sources during this warming event were minimal relative to contemporary sources like wetlands."

Kessler adds, "Our results agree with this conclusion, showing that ancient methane emissions to the atmosphere in an area that is experiencing some of the greatest warming today, is actually quite small, especially when compared to more direct emissions from human activities."

Explore further: Methane hydrate dissociation off Spitsbergen not caused by climate change

More information: Limited contribution of ancient methane to surface waters of the U.S. Beaufort Sea shelf, Science Advances  17 Jan 2018: Vol. 4, no. 1, eaao4842, DOI: 10.1126/sciadv.aao4842 , http://advances.sciencemag.org/content/4/1/eaao4842.full

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