Uranus And Neptune Look Like Twins But Have Startlingly Different Chemical Histories
Astronomy

Uranus And Neptune Look Like Twins But Have Startlingly Different Chemical Histories

New carbon monoxide data suggests Neptune and Uranus formed through different chemical processes, revealing distinct histories for our solar system’s giants.

By Aisha Ahmed
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Atmospheric models suggest Uranus and Neptune formed from different ingredients, but uncertain mixing leaves their origins open. (CREDIT: NASA/JPL-Caltech/B. Jónsson)

Though they are often grouped together as the solar system’s “ice giants,” new research suggests that Uranus and Neptune may be distant chemical cousins rather than planetary twins. A study published in Astronomy & Astrophysics indicates that the two worlds likely formed from different reservoirs of raw materials, hinting at distinct evolutionary paths in the early solar system.

Led by researchers including Olivier Mousis of the Southwest Research Institute, the team employed complex atmospheric models to peer beneath the opaque, featureless cloud decks of both planets. Because water and other key compounds remain buried deep within their atmospheres, the scientists used carbon monoxide as an indirect proxy to trace the chemical signatures of the planets’ deep interiors.

This figure explains where the building blocks for Uranus and Neptune may have formed in the protoplanetary disk orbiting the young Sun.
This figure explains where the building blocks for Uranus and Neptune may have formed in the protoplanetary disk orbiting the young Sun. (CREDIT: SWRI)

Unlocking the secrets of the deep atmosphere

The researchers found that while both planets share a gaseous exterior dominated by hydrogen and helium, their deeper reservoirs differ significantly. By analyzing carbon monoxide—which becomes “frozen” into the atmosphere as gases circulate between high-pressure depths and the cooler upper layers—the team inferred that Neptune possesses a significantly more oxygen-rich deep atmosphere than Uranus.

To reach these conclusions, the team utilized high-resolution data from the Atacama Large Millimeter/submillimeter Array. They determined that Neptune exhibits an oxygen enrichment level roughly 222 to 342 times that of the protosolar value, whereas Uranus shows a lower enrichment range of approximately 62 to 177 times. These findings suggest that the planets were constructed from varying proportions of “building blocks” found at different locations within the protoplanetary disk surrounding the young Sun.

Meridional temperature structure at 2 bars for Uranus (light green) and Neptune (dark green). The dashed lines are disk-averaged measurements, and the solid lines result from the radiative-convective model of Milcareck et al. (2024), seasonally averaged.
Meridional temperature structure at 2 bars for Uranus (light green) and Neptune (dark green). The dashed lines are disk-averaged measurements, and the solid lines result from the radiative-convective model of Milcareck et al. (2024), seasonally averaged. (CREDIT: Dr. Olivier Mousis et al, Astronomy & Astrophysics 2026)

Clues from the protoplanetary disk

The chemical variation implies that the two worlds may have originated in distinct regions of the early solar system where different ice lines dictated the availability of carbon and oxygen. Neptune’s lower carbon-to-oxygen ratio, for example, points toward a formation environment where water ice was abundant, a scenario consistent with the theory that the planet may have formed closer to the Sun before migrating to its current, distant orbit.

However, the researchers caution that these findings are not definitive. Vertical mixing—the process by which gases move between different atmospheric pressures—remains the greatest source of uncertainty in their models. If mixing operates differently on Uranus than on Neptune, it could potentially account for some of the observed chemical disparities, narrowing the gap between the two worlds.

Fits of the upper tropospheric methane mole fraction as a function of latitude. For Uranus (top), we fitted the data of Sromovsky et al. (2014). We show 113 data points between 4°N and 80°N in blue. These values were mirrored in the southern hemisphere. For Neptune (bottom), we used the profiles of Irwin et al. (2021).
Fits of the upper tropospheric methane mole fraction as a function of latitude. For Uranus (top), we fitted the data of Sromovsky et al. (2014). We show 113 data points between 4°N and 80°N in blue. These values were mirrored in the southern hemisphere. For Neptune (bottom), we used the profiles of Irwin et al. (2021). (CREDIT: Dr. Olivier Mousis et al, Astronomy & Astrophysics 2026)

The need for direct exploration

Since the Voyager 2 flybys in the 1980s, our understanding of these worlds has relied primarily on remote sensing. The study highlights the critical need for a dedicated mission, such as the proposed Uranus Orbiter and Probe, to conduct in-situ measurements. A probe descending into the atmosphere could provide ground-truth data, allowing scientists to confirm their models and resolve the ambiguity surrounding the planets’ deep chemical inventories.

Eddy diffusion coefficient computed on Uranus (left) and Neptune (right) as a function of pressure and latitude following the prescription of Wang et al. (2015). The dashed line corresponds to the transition latitude between the fast- and slow-rotating regimes.
Eddy diffusion coefficient computed on Uranus (left) and Neptune (right) as a function of pressure and latitude following the prescription of Wang et al. (2015). The dashed line corresponds to the transition latitude between the fast- and slow-rotating regimes. (CREDIT: Dr. Olivier Mousis et al, Astronomy & Astrophysics 2026)

As astronomers continue to discover exoplanets similar in size to these ice giants throughout the galaxy, unraveling the histories of Uranus and Neptune has become increasingly relevant. By decoding the chemical “fingerprints” left behind by their formation, researchers hope to better understand the diverse origins of planets in our own neighborhood and beyond.

Deep oxygen abundance with respect to the protosolar value as a function of latitude, fitting the upper tropospheric CO mole fraction measurement on Uranus using the V20r chemical scheme.
Deep oxygen abundance with respect to the protosolar value as a function of latitude, fitting the upper tropospheric CO mole fraction measurement on Uranus using the V20r chemical scheme. (CREDIT: Dr. Olivier Mousis et al, Astronomy & Astrophysics 2026)

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Reference(s)

  1. <https://www.aanda.org/articles/aa/full_html/2026/10/aa60770-26/aa60770-26.html>.
  2. “Southwest Research Institute | R&D From Deep Sea to Deep Space.” <https://www.swri.org/>.
  3. “Uranus Orbiter And Probe.” <https://science.nasa.gov/wp-content/uploads/2023/10/uranus-orbiter-and-probe.pdf>.
  4. Cavalié, T.., et al. “Detection of stratospheric HCN and tropospheric CO in Uranus and the implication for their sources.” Astronomy & Astrophysics, vol. 710, June 29, 2026, pp. A362 EDP Sciences, doi: 10.1051/0004-6361/202660695. <https://doi.org/10.1051/0004-6361/202660695>.
  5. Cavalié, Thibault., et al. “The Deep Composition of Uranus and Neptune from In Situ Exploration and Thermochemical Modeling.” Space Science Reviews, vol. 216, no. 4, May 18, 2020 Springer Science and Business Media LLC, doi: 10.1007/s11214-020-00677-8. <https://link.springer.com/article/10.1007/s11214-020-00677-8>.
  6. Venot, O.., et al. “New chemical scheme for giant planet thermochemistry.” Astronomy & Astrophysics, vol. 634, February 12, 2020, pp. A78 EDP Sciences, doi: 10.1051/0004-6361/201936697. <https://doi.org/10.1051/0004-6361/201936697>.
  7. Vorburger, Audrey., et al. “Mass Spectrometer Experiment for a Uranus Probe.” Space Science Reviews, vol. 220, no. 6, August 22, 2024 Springer Science and Business Media LLC, doi: 10.1007/s11214-024-01096-9. <https://link.springer.com/article/10.1007/s11214-024-01096-9>.
  8. Simon, Amy. “Uranus Orbiter and Probe: Mission Challenges and Concept Updates Since the Origins, Worlds, and Life Decadal Survey.”, vol. 7, no. 6, April 6, 2026 <https://ntrs.nasa.gov/citations/20260004996>.

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Ahmed, Aisha. “Uranus And Neptune Look Like Twins But Have Startlingly Different Chemical Histories.” BioScience. BioScience ISSN 2521-5760, 20 October 2026. <https://www.bioscience.com.pk/en/subject/astronomy/neptune-and-uranus-appear-to-have-significantly-different-chemical-origins>. Ahmed, A. (2026, October 20). “Uranus And Neptune Look Like Twins But Have Startlingly Different Chemical Histories.” BioScience. ISSN 2521-5760. Retrieved October 20, 2026 from https://www.bioscience.com.pk/en/subject/astronomy/neptune-and-uranus-appear-to-have-significantly-different-chemical-origins Ahmed, Aisha. “Uranus And Neptune Look Like Twins But Have Startlingly Different Chemical Histories.” BioScience. ISSN 2521-5760. https://www.bioscience.com.pk/en/subject/astronomy/neptune-and-uranus-appear-to-have-significantly-different-chemical-origins (accessed October 20, 2026).
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