To “know thy planet” one must “know thy star”. When a planet is discovered by the transit method the tiny dip in the amount of light received from the star provides a measure only of the size of the planet relative to the size of the star. Thanks to asteroseismology we can measure the size of the star extremely precisely, allowing the absolute size of the planet to be fixed with a high level of confidence. Next, we want to check if the planet lies in the habitable zone of the star, not too close or too far away, but just right for liquid water to potentially be present on the surface of the planet. The location of this so-called “Goldilocks Zone” depends on the intrinsic brightness of the star, for which we again need the precise asteroseismic size of the star. Should the planet be an Earth-like or rocky body orbiting in the habitable zone, we would of course want to know its age. This we can get from the age of the star, a property that asteroseismology is uniquely equipped to estimate since the waves that penetrate the core provide a direct probe of the beating heart of the star, its central “ticking clock”.