Long considered an object captured from the Kuiper belt, the third largest moon of the planet Neptune, Nereid, may actually be a primordial moon that survived a cosmic catastrophe.
For decades, the prevailing theory held that Nereid came from the Kuiper belt, that vast region of icy bodies beyond Neptune. The main argument rested on its highly eccentric and irregular orbit, rare among original moons. Furthermore, the capture of Triton, Neptuneâs largest moon, by the planetâs gravity should have scattered or destroyed any preexisting satellite. Yet Nereid remains, intact.

Image of Neptune and several of its moons taken by the James Webb Space Telescope.
Credit: NASA/ESA/CSASTScI
The James Webb Space Telescope was used by a team of researchers to determine Nereidâs origins. With just about ten minutes of observation, they gathered enough data to show that Nereid is very different from known Kuiper belt objects. Richer in water ice, much brighter and more reflective, and bluer in color, it also lacks the typical volatile organic compounds of those distant objects.
Nereidâs composition therefore contradicts the hypothesis of a capture from the Kuiper belt. To support this idea, scientists ran simulations of the Neptunian systemâs dynamics in its early days, at the time when Triton was captured. These models show that Tritonâs violent arrival could have thrown Nereid onto its current orbit, very inclined and elongated, without destroying it.
The history of this moon dates back to 1949, when it was discovered by astronomer Gerard Kuiper, who named it and sensed its importance for understanding Neptuneâs strange system.

Color mosaic of Triton, taken in 1989 by the Voyager 2 probe during its flyby of the Neptunian system.
Credit: NASA/JPL/USGS