Most of life on Earth will be EXECUTED in a billion years as a result of an extreme dip in oxygen levels, scientists warn
- Researchers from Japan and the US have modeled the future of Earth’s atmosphere
- The increasing brightness of the sun affects surface temperatures and photosynthesis
- This will cause rapid atmospheric deoxygenation in about a billion years
- The finding has implications for the way we look for habitable planets elsewhere
An extreme dip in atmospheric oxygen levels will wipe out most of life on Earth in a billion years, a study has predicted.
Researchers from Japan and the US have modeled how our planet’s atmosphere will change in the light of various biological, climatic and geological processes.
Deoxygenation will result from the sun’s increasing energy flow as it brightens, increasing surface temperatures and reducing photosynthesis.
They found that in about a billion years, deoxygenation will return the atmosphere to an inhospitable, methane-rich compound – one reminiscent of early Earth.
This fate, they added, will occur before the advent of so-called humid greenhouse conditions in which water will leak irreversibly from the planet’s atmosphere.
The findings suggest that airborne oxygen is not a permanent part of habitable planets, which has implications for our search for life on other worlds.

An extreme dip in atmospheric oxygen levels will wipe out most of life on Earth in a billion years, a study has predicted. Pictured: The decrease in oxygen that the team predicted
Before 2.4 billion years ago, the Earth’s atmosphere was rich in methane, ammonia, water vapor, and the noble gas neon, but lacked free oxygen.
This was introduced in an episode geologists call the Great Oxygenation Event, in which cyanobacteria living in the oceans began to produce significant amounts of oxygen through photosynthesis, radically altering the atmosphere.
This influx of oxygen has been attributed to paving the way to broadly support multicellular life, although this also came with a price – the death of many anaerobic bacteria, in what is believed to be Earth’s first mass extinction .
The new findings suggest that Earth’s atmosphere could swing the other way in the future – and potentially give the world back to anaerobic microorganisms.
“We discover that future deoxygenation is an inevitable consequence of increasing solar fluxes,” the research duo wrote in their paper.
“The precise timing is modulated by the exchange flux of reducing power between the mantle and the ocean-atmosphere crust system.”
“Our results suggest that the planetary carbonate-silicate cycle will lead to terminally CO2-restricted biospheres and rapid atmospheric deoxygenation.”
The oxygenation of the atmosphere is generally seen as an indication of the Earth’s current biosphere, plants and photosynthetic activity. Therefore, the logic goes, we should look for similar oxygen-rich worlds in our pursuit of extraterrestrial life.
However, the findings suggest that – from the point of view of a hypothetical distant alien observer – detection of atmospheric oxygen on Earth may only be possible for about two to three-tenths of our planet’s lifespan.
If this is also true of other planets, the researchers argue, we may need to adjust our search for life elsewhere in the universe to look for additional biosignatures that indicate life persists beyond a planet’s oxygen-rich period.
The full findings of the study are published in the journal Nature Geoscience.