However, analysis of zircons formed 4.4 Ga indicates that Earth's crust solidified about 100 million years after the planet's formation and that the planet quickly acquired oceans and an atmosphere, which may have been capable of supporting life.
Porén, as análises de circóns formados hai 4.400 Ma indican que a codia da Terra solidificou uns 100 Ma despois da formación do planeta e quen o planeta axiña adquiriu océanos e unha atmosfera, que puideron ter a capacidade de albergar vida.