With the first solids forming around HOPS-315, astronomers have finally witnessed the earliest seeds of planets taking root.
This process begins as hot gas cools and condenses, forming tiny crystals that collide, stick, and gradually grow into larger pebbles and boulders.
Gravity becomes the architect, pulling these fragments together until they reach critical mass as kilometer-sized “planetesimals,” the basic building blocks of all planets.
In the solar system, evidence of this process comes from meteorites called chondrites, which preserve calcium-aluminium-rich inclusions (CAIs) dating back to the dawn of planetary assembly.
By studying these ancient relics, scientists can reconstruct the temperature, pressure, and chemical environment of the Sun’s earliest days.
The new data from HOPS-315 reveal similar conditions, with the first solids condensing just twice as far from the star as Earth orbits the Sun.
Researchers estimate this phase lasts only about 160,000 years—a cosmic blink—making it incredibly rare to catch in action.
Finding it now in a young star so far away confirms that planet-building follows predictable steps across the galaxy.
As planetesimals grow, they sweep up more material, eventually forming full-fledged planets, moons, and the debris belts that circle young stars.
This dynamic, violent process sets the stage for everything to come—worlds, atmospheres, and perhaps even the preconditions for life.
With this real-time glimpse, scientists can finally piece together the timeline of planet birth, refining theories that stretch from Earth to the edge of the cosmos.