

The lunar surface may hold a surprisingly detailed record of ancient stars that exploded millions of years ago.
Researchers have devised a new method to interpret this complex history, potentially turning moon dust into an astronomical archive detailing our solar system’s passage through the Milky Way.
The study, led by Emily Costello from the University of Hawaiʻi at Mānoa, was published in *Physical Review Letters*.
Massive stars end their lives in spectacular explosions known as supernovae, which release matter into space—including radioactive elements capable of traveling hundreds of light-years.
Some of this radioactive debris eventually makes its way to Earth and the moon.
While evidence of ancient supernovae has been previously found in deep-sea sediments on Earth, these layers typically only record events from about the past 10 million years. The moon’s preserved soil could reveal a much longer history.
Costello suggests that lunar soil, or regolith, might contain evidence dating back 80 to 100 million years or even more.
Deciphering this record is challenging because the lunar surface is constantly being reshaped.
Unlike Earth, the moon lacks a thick atmosphere to shield it from space debris. Impacting meteoroids—ranging from tiny particles to sizable asteroids—continually collide with its surface. Over time, these impacts—referred to as “impact gardening”—disrupt and mix lunar material.
This process means that radioactive substances deposited by supernovae don’t remain in distinct layers but are gradually redistributed through the soil.
To address this, Costello and her team developed a mathematical model to reconstruct this tangled history. The model factors in multiple simultaneous processes: impacts that expose or bury material, soil compaction, radioactive decay, and modifications caused by space exposure.
The model estimates when radioactive elements from specific supernova events arrived on the moon and predicts how they moved within the lunar soil over vast timescales.
Previous studies have shown that supernovae occurring hundreds of light-years away sent radioactive particles toward our solar system about 2.3 million and 7.3 million years ago.
To validate their model, scientists compared its predictions with actual measurements from lunar soil samples collected during the Apollo missions. The results closely matched observed patterns of radioactive isotope distribution at various depths.
The model also accurately predicted the presence of iron-60, a radioactive isotope linked to supernova activity, in those lunar samples.
Building on this, researchers projected how other rare radioactive elements—like plutonium-244, iodine-129, hafnium-182, and curium-247—could have been buried and diffused through the lunar soil over millions of years.
This research holds particular significance as humanity prepares to explore the Moon further, with NASA’s Artemis program aiming to gather new samples, including deeper cores that might contain ancient material not yet accessible.
By combining these upcoming samples with the new modeling techniques, scientists could trace supernova activity over tens of millions of years. Such insights might reveal when stars exploded and dispersed material across our solar system, offering clues about the paths of the sun, Earth, and Moon through the galaxy.
In essence, ordinary moon dust could act as a time capsule, preserving the remains of stars that vanished millions of years ago.
Source: KSR.









