The rate of oxygen decline from the Earth's atmosphere has speeded up over the past 100 years, driven by burning of fossil fuels, which consumes oxygen and produces carbon dioxide, says a study.
Researchers from Princeton University compiled 30 years of data to construct the first ice core-based record of atmospheric oxygen concentrations spanning the past 800,000 years, according to the paper published in the journal Science.
‘Extra carbon dioxide emitted due to declining oxygen concentrations in the atmosphere stimulates silicate weathering.’
The record showed that atmospheric oxygen has declined 0.7 percent relative to current atmospheric-oxygen concentrations, a reasonable pace by geological standards, the researchers said.
During the past 100 years, however, atmospheric oxygen has declined by a comparatively speedy 0.10 percent because of the burning of fossil fuels, which consumes oxygen and produces carbon dioxide.
"This record represents an important benchmark for the study of the history of atmospheric oxygen," said Assistant Professor of Geosciences John Higgins.
"Understanding the history of oxygen in Earth's atmosphere is intimately connected to understanding the evolution of complex life," Higgins noted.
Curiously, the decline in atmospheric oxygen over the past 800,000 years was not accompanied by any significant increase in the average amount of carbon dioxide in the atmosphere, though carbon dioxide concentrations do vary over individual ice age cycles.
To explain this apparent paradox, the researchers called upon a theory for how the global carbon cycle, atmospheric carbon dioxide and the Earth's temperature are linked on geologic timescales.
"The planet has various processes that can keep carbon dioxide levels in check," said first author Daniel Stolper.
The researchers discussed a process known as "silicate weathering" in particular, wherein carbon dioxide reacts with exposed rock to produce, eventually, calcium carbonate minerals, which trap carbon dioxide in a solid form.
As temperatures rise due to higher carbon dioxide in the atmosphere, silicate-weathering rates are hypothesised to increase and remove carbon dioxide from the atmosphere faster.
The study suggests that the extra carbon dioxide emitted due to declining oxygen concentrations in the atmosphere stimulated silicate weathering, which stabilised carbon dioxide but allowed oxygen to continue to decline.
"The Earth can take care of extra carbon dioxide when it has hundreds of thousands or millions of years to get its act together. In contrast, humankind is releasing carbon dioxide today so quickly that silicate weathering can't possibly respond fast enough," Higgins noted.
"The Earth has these long processes that humankind has short-circuited," Higgins said.
The researchers built their history of atmospheric oxygen using measured ratios of oxygen-to-nitrogen found in air trapped in Antarctic ice. This method was established by co-author Michael Bender.