For most of Earth’s inhabited history, an astronomer on another world could have studied our atmosphere and missed the most important fact about it.

Life was present by at least 3.5 billion years ago, yet oxygen and ozone became reliable remotely detectable signs only during roughly the past 500 million years. That leaves an approximate three-billion-year interval in which Earth was inhabited but could have failed a search built mainly around oxygen.

An oxygen search would have missed it.

That history matters as NASA develops the Habitable Worlds Observatory, a future space telescope intended to directly image potentially Earth-like planets around nearby stars. HWO would not literally see nothing. It could see a planet and measure parts of its atmosphere, but it might find no decisive evidence that the world was alive.

The three-billion-year gap is an approximation

The headline comparison combines two broad milestones. Geological evidence indicates that Earth had a biosphere by at least 3.5 billion years ago. Yet a 2017 Astrobiology study of Earth through time concluded that atmospheric oxygen and ozone would have been poor remote signs of that biosphere for all but the past 500 million years or so.

This does not mean early organisms produced no oxygen. Oxygenic photosynthesis evolved long before the atmosphere reached its modern composition. For much of that history, oxygen reacted with reduced material in the oceans, rocks and volcanic gases instead of accumulating to levels that would make a strong spectral signal.

The Great Oxidation Event began around 2.4 billion years ago, but oxygen remained far below present levels through much of the Proterozoic. A distant telescope could therefore have encountered a living Earth without finding the oxygen-rich atmosphere familiar today.

HWO is still a mission concept

NASA describes the Habitable Worlds Observatory as its next major astrophysics flagship after the Nancy Grace Roman Space Telescope. It remains in an early design and technology-maturation stage, rather than being a newly launched observatory.

The proposed telescope would block the glare of a star, directly image a small planet beside it and separate the reflected light into a spectrum. According to NASA’s HWO science outline, that spectrum could be searched for gases including water vapour, oxygen, ozone, methane and carbon dioxide.

Its central challenge is contrast. A planet like Earth is extremely faint beside a Sun-like star, so HWO would require a coronagraph thousands of times more capable than any yet flown and optical stability measured at extraordinary precision. NASA awarded technology contracts in January 2026 to advance some of those systems, but the observatory’s final design and launch timetable have not been fixed.

A model tested Earth at different ages

A 2026 modelling study accepted by The Astrophysical Journal generated the spectra HWO might record if it observed Earth during the Archean, Proterozoic and Phanerozoic eons. The researchers varied the spectral resolution to ask which atmospheric gases could be recovered and how long observations might take.

The results make the false-negative problem concrete. In visible light, the model found that a resolving power of 140 could identify oxygen in an atmosphere resembling the recent Phanerozoic Earth. Detecting the much lower oxygen abundance expected for the Proterozoic would require detector dark current more than ten times lower than the study’s baseline case.

This is one modelling study, not a final instrument specification. Its exposure estimates depend on assumed clouds, atmospheric composition, telescope design and detector noise. The work nevertheless shows why using modern Earth as the only template for an inhabited planet would be risky.

No oxygen does not mean no life

The planet would still be there.

HWO could potentially detect water, carbon dioxide or other atmospheric features even when oxygen was weak. The 2026 model also found that ultraviolet observations of ozone could provide an indirect route to low oxygen in some cases. Methane might add another clue, although its abundance and origin would have to be assessed alongside the planet’s star and chemistry.

No single gas is an automatic verdict. Oxygen can be produced without biology under some planetary conditions, creating a false positive. Biology can also remain active without leaving enough atmospheric oxygen to detect, creating a false negative. Clouds, surface pressure, ultraviolet radiation and geological activity all affect the spectrum.

The target is a chemical pattern

HWO’s search will therefore depend on combinations of evidence. Water may indicate potentially habitable conditions. Oxygen or ozone can be compelling when they appear in the right context. Methane alongside an oxidising gas could strengthen the case, while carbon monoxide or the host star’s radiation might point towards non-biological explanations.

Early Earth is a warning against treating silence at one wavelength as an empty world. For most of the time life has occupied this planet, oxygen alone would not have announced it across interstellar space.

A future telescope could look directly at an inhabited planet and come away without a confident detection of life. That is not the same as seeing nothing. It is the harder result: seeing a world clearly enough to know that the evidence remains ambiguous.