Abstract. A magneto-orbital coupling mechanism is proposed to account for the weak energy gap at the Fermi energy in the (π, 0) ordered SDW state of a realistic three band model for iron pnictides involving d xz , d yz , and d xy Fe orbitals. The orbital mixing terms between the d xy and d xz /d yz orbitals, which are important in reproducing the orbital composition of the elliptical electron pockets at (±π, 0) and (0, ±π), are shown to play a key role in the energy gap formation in the SDW state.Magneto-orbital coupling in iron pnictides.