We present a systematic study of the magnetic coupling between iron and gadolinium layers
intermediated by 4d and 5d transition metals using density functional theory. We demonstrate that
it is possible to nd a magnetic coupling for most of them. In particular, for the early transition
metals (d1, d2, d3 and d4) , a ferromagnetic coupling occurs even stronger than the 3d interlayers.
Atomic size and the electronic conguration of the transition metals are crucial for the nature of the
coupling. All the open shell transition metals present induced magnetic moments. By increasing the
number of interlayers, an oscillating behavior in the magnetic coupling was found and the magnetic
coupling goes to zero after four spacer layers. Using Monte carlo simulations, we demonstrate that
the interlayer strongly enhances the critical temperature in the Gd layers closest to the interface.