<p>Astronomers have found two distinct rings of planetary debris around the white dwarf J1328−1450. The gap between them may be held open by planetary bodies that survived the star’s transformation, according to a study reported in <em>Nature Astronomy</em>. The system offers a possible glimpse of what can remain after a Sun-like star dies.</p>

<p>The report, based on material provided by the European Southern Observatory (ESO), describes observations made with the X-Shooter instrument on ESO’s Very Large Telescope in Chile. X-Shooter analyzes light across a broad range of wavelengths, allowing researchers to study the material’s chemical makeup and motion. The observations show a double-disc structure that stands out from the single, flat debris discs previously reported around white dwarfs.</p>

<p>J1328−1450 is the exposed core of a star that expanded and shed its outer layers late in life. Stars similar to the Sun are expected to follow a comparable path. During that change, nearby planets may be engulfed, while more distant rocky objects can survive at first and later be broken apart by gravitational disturbances. Their remains can settle into a rotating disc around the stellar remnant.</p>

<p>The researchers suspect that two surviving planetesimals—small solid bodies—help maintain the rings. The proposed body associated with the inner ring may be only a few kilometres across. The one linked to the outer ring could be much larger, perhaps as large as Pluto or even the Moon. Neither body has been directly observed; their gravitational influence is a possible explanation for the rings’ separated arrangement.</p>

<p>The debris also carries chemical clues. The observations detect calcium, oxygen, magnesium and iron, elements common in rocky planetary material. The inner ring contains substantial magnesium gas, while the outer ring is largely depleted of it. That difference could mean the rings came from separate planets with different compositions. Another possibility raised in the report is that they contain material from different layers of one body, such as its crust and core.</p>

<p>Lead author Nicola Gentile Fusillo, an astronomer at the University of Trieste, describes the system as a complex example of a double debris disc with potentially surviving planetesimals. Co-author Felipe Lagos-Vilches, affiliated with the University of Warwick and the Universidad Técnica Federico Santa María, points to the rings’ apparent stability and the gap between them. The observations reveal an unusual structure; the proposed survivors and the origin of the chemical differences remain interpretations.</p>

<p>Billions of years from now, the Sun is expected to expand into a red giant, shed its outer layers and become a white dwarf. Earth may be destroyed during that transformation. The system around J1328−1450 shows that some planetary material can persist around a stellar remnant, but how our Solar System’s remains would be arranged is uncertain. Studying this distant system gives astronomers a rare way to investigate the long aftermath of a star’s evolution.</p>

<p>Source: ScienceDaily report on the ESO announcement</p>