Ancient Air Bubbles Trapped in Antarctic Ice Point to Cause of Oxygen Decline

Yuzhen Yan in Antarctica

Yuzhen Yan in Antarctica in December 2015. Credit: Yuzhen Yan

Research suggests that glaciers could be the culprits behind the gradual reduction of atmospheric oxygen over the past 800,000 years due to their role in promoting weathering, which consumes oxygen. This process became more pronounced as glacial cycles lengthened from about 40,000 to 100,000 years ago, aligning with the timing of the oxygen decline.

An unknown culprit has been removing oxygen from our atmosphere for at least 800,000 years, and an analysis of air bubbles preserved in Antarctic ice for up to 1.5 million years has revealed the likely suspect.

“We know atmospheric oxygen levels began declining slightly in the late Pleistocene, and it looks like glaciers might have something to do with that,” said Rice University’s Yuzhen Yan, corresponding author of the geochemistry study published in Science Advances. “Glaciation became more expansive and more intense about the same time, and the simple fact that there is glacial grinding increases weathering.”

Weathering refers to the physical and chemical processes that break down rocks and minerals, and the oxidation of metals is among the most important. The rusting of iron is an example. Reddish iron oxide forms quickly on iron surfaces exposed to atmospheric oxygen, or O2.

“When you expose fresh crystalline surfaces from the sedimentary reservoir to O2, you get weathering that consumes oxygen,” said Yan, a postdoctoral research associate in Rice’s Department of Earth, Environmental and Planetary Sciences.

Another way glaciers could promote the consumption of atmospheric oxygen is by exposing organic carbon that had been buried for millions of years, Yan said.

Air Bubbles in Disk of Antarctic Ice

Researchers studied Earth’s ancient atmosphere by capturing tiny bubbles of air that were preserved in Antarctic ice for up to 1.5 million years. Credit: Yuzhen Yan

During Yan’s Ph.D. studies in the labs of Princeton University’s Michael Bender and John Higgins, Yan worked on a 2016 study led by Daniel Stolper, now an assistant professor at the University of California, Berkeley, that used air bubbles in ice cores to show the proportion of oxygen in Earth’s atmosphere had declined by about 0.2% in the past 800,000 years.

In the Science Advances study, Yan, Higgins and colleagues from Oregon State University, the University of Maine and the University of California, San Diego, analyzed bubbles in older ice cores to show the O2 dip began after the length of Earth’s glacial cycles more than doubled around 1 million years ago.

The ice age Earth is in today began about 2.7 million years ago. Dozens of glacial cycles followed. In each, ice caps alternately grew, covering up to a third of the planet, and then retreated toward the poles. Each cycle lasted around 40,000 years until about 1 million years ago. At roughly the same time atmospheric oxygen began to decline, glacial cycles began lasting about 100,000 years.

“The reason for the decline is the rate of O2 being produced is lower than the rate of O2 being consumed,” Yan said. “That’s what we call the source and the sink. The source is what produces O2, and the sink is what consumes or drags on O2. In the study, we interpret the decline to be a stronger drag on O2, meaning more is being consumed.”

Ice Core Drilling in Allan Hills, East Antarctica

A scientific drilling mission to Allan Hills, East Antarctica, in 2015-16 yielded ice cores with trapped bubbles of ancient air, including some that predated the ice age that began 2.7 million years ago. Credit: Yuzhen Yan

Yan said Earth’s biosphere didn’t contribute to the decline because it is balanced, drawing as much O2 from the atmosphere as it produces. Weathering, on a global scale, is the most likely geological process capable of consuming enough excess O2 to account for the decline, and Yan and colleagues considered two scenarios for increased weathering.

Global sea level falls when glaciers are advancing and rises when they retreat. When the length of glacial cycles more than doubled, so did the magnitude of swings in sea level. As coastlines advanced, land previously covered by water would have been exposed to the oxidizing power of atmospheric O2.

“We did some calculations to see how much oxygen that might consume and found it could only account for about a quarter of the observed decrease,” Yan said.

Because the extent of ice coverage isn’t precisely known for each glacial cycle, there’s a wider range of uncertainty about the magnitude of chemical weathering from glacial erosion. But Yan said the evidence suggests it could draw enough oxygen to account for the decline.

“On a global scale, it’s very hard to pinpoint,” he said. “But we did some tests about how much additional weathering would be needed to account for the O2 decline, and it’s not unreasonable. Theoretically, it could account for the magnitude of what’s been observed.”

Reference: “Ice core evidence for atmospheric oxygen decline since the Mid-Pleistocene transition” by Yuzhen Yan, Edward J. Brook, Andrei V. Kurbatov, Jeffrey P. Severinghaus and John A. Higgins, 15 December 2021, Science Advances.
DOI: 10.1126/sciadv.abj9341

Additional co-authors include Edward Brook of Oregon State, Andrei Kurbatov of the University of Maine and Jeffrey Severinghaus of UC San Diego. The research was supported by the National Science Foundation (1443263, 1443276, 1443306, 0538630, 0944343, 1043681 and 1559691) and a Poh-Hsi Pan Postdoctoral Fellowship from Rice University.

6 Comments on "Ancient Air Bubbles Trapped in Antarctic Ice Point to Cause of Oxygen Decline"

  1. I want to congratulate the authors of this paper for the unusual (for climatology) attention paid to significant figures for their calculations and measurements. They demonstrate an awareness and concern for uncertainty that is refreshing to find in a paper related to climatology.

    But then, they are geochemists and not self-described climatologists.

  2. David Naugler, Ph.D. | January 9, 2022 at 11:14 pm | Reply

    It suggests a larger quantity of animal biomass in the biosphere. More cattle, more humans, more fish, more birds? Long recovery from the KT extinction?

  3. The earth is only about 6000 years old;sorry folks, back to the drawing board!

  4. There were over 60 million buffalo on the Great Plains before white man came. There are less than 30 million cattle now. Climate change has been going on for 4.6 billion years!

  5. I may be just your average idiot.. but wouldnt the real issue be the trees we cut down while reproducing at an exponential rate be the real and main issue. Trees and foliage that add the balance we keep tearing down. I understand no one wants to admit it, but humans are the problem. And these natural causes that would help keep numbers down keep being cured. Between our selfish modern medical science to save the few we’re screwing the many. Topped with the destruction we leave in our wake and no one wanting to face the truths.. we’re destined to collapse in on ourselves. Running out of land and oxygen and water and our time is more limited than people realize. Especially with the rate we reproduce now. China alone is almost a million people each year. Combine this number with the trees and wildlife we tear through. . But im just another average idiot whose not a pedestal.

  6. Science Drama! Cant cure cant stop just temporary banaids . Yes i will pop a pill so to endure the experience knowing its a temporary fix kinda like nature and its designers purging an overgrown forest because someone’s science says dont cut the trees the owl needs them more so !

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