If microscopic life evolves on a planet which is subsequently ejected from orbiting its star, then the planet would cool down. How deep into the interior of the planet could organisms reach, assuming the mantle had cooled down enough?
For example, on Earth there are rock-boring bacteria that have tunneled their way 3 km into the crust.
The limiting factor for depth of bacteria on Earth seems to be temperature, but presumably if the mantle had cooled down then at some depth other factors would come into play such as pressure or rock hardness or composition.
