Did liquid water once exist in the outer solar system? Study of Neptune's moons provides clue

The outer solar system is a frigid place where liquid water isn't expected to exist.
An illustration of Neptune against a black starry background. (Representative Cover Image Source: Getty | Mark Garlick)
An illustration of Neptune against a black starry background. (Representative Cover Image Source: Getty | Mark Garlick)

Scientists have found evidence that liquid water existed in the Neptunian system's past. Using information gathered by the James Webb Space Telescope (JWST), researchers have figured out the composition of the ice giant's tiny inner moons and rings. The data hinted at the presence of clay-like materials that can only be formed by long-term interaction with liquid water. Since Neptune lies quite far in the frigid outer reaches of the solar system, it is one of the last places such an indication was expected to come from. This has led to a couple of ideas about how the evolutionary story of the Neptunian moons unfolded, which is understood to be very different from that of planetary giants neighboring Neptune.



The research paper that describes these findings was published on in late July in Science Advances. Its lead author, Caltech (California Institute of Technology) graduate student Ryleigh Davis, said, "We see something that doesn't really look like anything else we've identified in the solar system." What Davis described are fingerprints of chemicals observed from the Neptunian rings and its three moons, Larissa, Galatea, and Proteus. These three irregularly shaped moons lie very close to their host planet, which had made it difficult for scientists to study them directly. However, thanks to spectroscopy performed with Webb's NIRSpec (Near Infrared Spectrograph), the scientists were able to make direct observations of the compositions of these moons.

Diagram showing some of the moons of Neptune. (Representative Image Source: NASA | ESA | A. Feild (STScI))
Diagram showing some of the moons of Neptune. [Representative Image Source: NASA | ESA | A. Feild (STScI)]

"We were very surprised when we got the data down," said Davis, while explaining that there appeared to be a presence of what are known as hydration bands. What this loosely translates to is not the evidence of free molecules of water, but its constituents—oxygen and hydrogen—bound directly into the rock's minerals. Moreover, the team also discovered spectra that point to the presence of magnesium-rich phyllosilicates, which are clay-like substances of a kind that need plenty of alteration by liquid water to form. The only plausible explanation was that these substances were formed deep inside a large enough icy moon of Neptune that was able to hold liquid water inside it in the past. Later events caused such a moon—or any other that would have originally been there—to be destroyed, leaving behind remnants that came together to create what we know as Larissa, Galatea, and Proteus.

This diagram illustrates the proposed origin for Neptune's present-day inner moon and ring system. Neptune once had a system of large moons that were destroyed when Triton—a captured Kuiper Belt object—arrived. (Representative Image Source: R. Davis)
This diagram illustrates the proposed origin for Neptune's present-day inner moon and ring system. Neptune once had a system of large moons that were destroyed when Triton—a captured Kuiper Belt object—arrived. (Representative Image Source: R. Davis)

The researchers think that the most likely scenario to explain how such a catastrophic event could take place is the arrival of Triton. The single largest moon of the ice giant, containing about 99 percent of the combined mass of all Neptunian moons, is quite atypical. Scientists think it is an object that came from the Kuiper Belt and is said to have been captured by the gravity of Neptune, which explains its retrograde orbit (revolving opposite to the host planet's rotation). When it became a moon of Neptune, its arrival disrupted the orbits of all the other existing moons, and destroyed others. In the process, the particular moon (or set of moons) that would have carried materials shaped by liquid water would have become exposed and ended up forming the inner moons of Neptune. The materials in these moons are also quite dark, and believed to be structurally quite strong given that they are still intact despite being within the Roche limit, the distance threshold beyond which tidal forces from Neptune rips loosely held objects apart.

Global color mosaic of Triton, taken in 1989 by Voyager 2 during its flyby of the Neptune system (Image Source: NASA/JPL/USGS)
Global color mosaic of Triton, taken in 1989 by Voyager 2 during its flyby of the Neptune system (Representative Image Source: NASA | JPL | USGS)

The explanation that assumes Triton's catastrophic arrival as the cause of all this also fits in with how the moon Nereid appears to be different from the other moons of Neptune, while being similar to moons expected to be found in the outer solar system. Nereid orbits Neptune far beyond Triton, leading scientists to believe that it is one of the ice giant's original moons that survived destruction. Although observations like these are creating a better picture of the planet's past, the Neptunian system still remains shrouded in much mystery. "Looking forward, understanding how that process actually proceeds would be interesting," added Davis.

More on Starlust

Scientists just found a bizarre new form of ice that could explain what’s inside Uranus and Neptune

NASA's Webb and Hubble reveal how tiny objects beyond Neptune still preserve their ancient origins

MORE STORIES

From progress in NASA's moon mission to discoveries about black holes, here's what happened this week.
11 hours ago
Astronomers are watching Sakurai’s Object reheat in real time, revealing a rare stage of evolution.
12 hours ago
Elias 2-24 b is the youngest by some distance, and could provide rare insights into planet formation.
1 day ago
The newly formed craters span the length of two football fields and can fit three vertically stacked yellow school buses.
1 day ago
The first class of 300 students will begin in 2028, with the permanent campus fully operational by 2031.
1 day ago
"There is much to do, but we are on our way to groundbreaking science."
2 days ago
Chariklo, the largest known Centaur, has a radius of just 125 km, but has two rings around it.
2 days ago
Denoted by Kp, the planetary K-index shows the intensity of disturbance in Earth's magnetosphere.
3 days ago
Mercury’s rocks may hold a surprising clue about the planet’s scorching volcanic past.
3 days ago
Missed the August 2026 solar eclipse? Don't worry. Read here to know all about the timings of the next five total solar eclipses.
6 days ago