
An early stage of planet formation, a body that can grow into a full planet.A planetary embryo is an intermediate stage in planet formation, a solid body roughly the size of the Moon to Mars that has grown by accumulating smaller planetesimals. These embryos are the building blocks of terrestrial planets and the cores of gas giants. In the early solar system, hundreds of such embryos formed within a few million years, and their subsequent collisions — sometimes merging, sometimes shattering — sculpted the final architecture of planetary systems. Understanding embryos is key to explaining why some planets become rocky worlds and others become gas giants, and why some systems have hot Jupiters while ours does not.
The concept of planetary embryos emerged in the 1970s and 1980s from numerical simulations of planet formation, particularly the work of George Wetherill and later the 'Nice model' team, who showed how embryos evolve into the current planets.
Planet formation begins with dust grains in a protoplanetary disk that stick together to form pebbles and then kilometer-sized planetesimals. These planetesimals gravitationally attract each other and merge, growing into embryos. The process is self-limiting: as embryos grow, they stir up the surrounding planetesimals, increasing their relative velocities and making further accretion less efficient. This 'oligarchic growth' phase ends when the disk gas dissipates, leaving a set of embryos that then undergo giant impacts over tens of millions of years to form full-sized planets.
Embryo formation models guide the search for exoplanets, helping predict which stellar systems are likely to harbor Earth-like planets and informing observations of protoplanetary disks with ALMA and JWST.
The Moon is thought to be the result of a giant impact between the early Earth and a Mars-sized planetary embryo, a collision that vaporized the outer layers of both bodies and formed a disk that coalesced into our satellite.





















