In a Remote Stellar System, a Pluto-Esque Planet Persisted Up to the Final Moment


For the very first time, astronomers have witnessed an event that appears to mimic Pluto colliding with a white dwarf, the remnants of a medium-sized star.

The white dwarf, designated WD 1647+375, is situated roughly 260 light-years from our planet. Despite this significant distance, the system of this deceased star may have mirrored our solar system, potentially featuring a region similar to the Kuiper Belt with comets and icy dwarf planets, as indicated by recent studies.

NASA’s Hubble Space Telescope facilitated this revelation by examining material descending onto the white dwarf, enabling researchers to infer the types of planets and cosmic entities that once revolved around the star.

Essentially, the surrounding debris of a white dwarf offers valuable insights into the exoplanets that a star previously supported.

“I am incredibly excited that we have now pinpointed a system that closely resembles the objects found in the freezing outer regions of our solar system,” stated Boris Gänsicke, the principal investigator of the Hubble program and a researcher at the University of Warwick. “Assessing the composition of an exo-Pluto significantly aids our comprehension of the formation and evolution of these celestial bodies.”

The latest findings imply that icy entities in the outer edges of a planetary system might endure for a considerable period after their star has perished. This could provide valuable information regarding the future of our solar system following the sun’s end. The findings were published in the Monthly Notices of the Royal Astronomical Society.

Generally, when a medium-sized star perishes, it expels the majority of its material. The Hubble discovery astonished astronomers, as they had anticipated that the distant icy realms would either be destroyed or cast away long before the star transitioned into a white dwarf.

Hubble detected debris surrounding the white dwarf in ultraviolet light, revealing chemical signatures of carbon, nitrogen, sulfur, and water ice, akin to Pluto’s makeup. Given that white dwarfs have uncomplicated atmospheres of hydrogen and helium, any heavier elements found must originate from something else colliding with the star.

“We are aware that Pluto’s surface is adorned with nitrogen ices,” commented Snehalata Sahu, an astronomer from the University of Warwick and the primary author of the paper. “We believe that the white dwarf [gathered] fragments of the crust and mantle of a dwarf planet.”

Nonetheless, researchers cannot dismiss alternate origins. Relying solely on chemical composition, they cannot ascertain whether the Pluto-like entity was originally part of the star’s system or an interstellar traveler, akin to the comet 3I/ATLAS currently navigating our solar system.

If this entity were a distant dwarf planet from its planetary system’s outskirts, how did it find itself so near the star?

As a sun-like star ages, it swells into a red giant before transforming into a white dwarf, potentially scorching or consuming its inner planets. In our solar system, Mercury and Venus, followed by Earth, are projected to be the first casualties.

By the time the star evolves into a white dwarf, only the gas and ice giant worlds in the outer regions remain. This causes disorder, as the diminished mass and gravity of the deceased star destabilize previously stable orbits, allowing giant planets to drive icy worlds into extreme trajectories, ultimately bringing them closer to the white dwarf.

This Pluto-like entity likely spent billions of years far from the star, remaining in a frozen state. However, as it neared the white dwarf, it was torn apart in a swift, violent event.

The discovery not only sheds light on the fate of planetary systems when their stars die but also aids scientists in comprehending how water and other elements traverse between worlds.

Many astronomers believe that Earth’s oceans originated from comets and asteroids colliding with the planet. While some researchers propose that primitive Earth released gases 4.5 billion years ago, forming an atmosphere conducive to rain, others argue that extraterrestrial rocks from the outer solar system brought water.

The research team identified considerable water ice, constituting approximately 64 percent of the Pluto-like debris, linking the investigation to larger enigmas regarding how icy objects endure and possibly transport water in space.

“If a distant alien observer were to look upon our solar system in the far-off future,” Sahu remarked, “they might perceive the same kind of debris that we observe today surrounding this white dwarf.”