We have investigated the effect of iron substitution on the magnetocaloric properties of manganites with La 0.75 Ca 0.08 Sr 0.17 Mn 1−x Fe x O 3 (x = 0, 0.075, 0.15, 0.175, and 0.2) nominal composition. The magnetocaloric effect (MCE) was estimated, in terms of isothermal magnetic entropy change (− S M ), using the M(T , μ 0 H ) data and employing the thermodynamic Maxwell equation. The large magnetic entropy in AMn 1−x Fe x O 3 is attributed to the fieldinduced suppression of short-range charge-orbital ordering and antiferromagnetic fluctuations present above T C . The increase of the Fe concentration x is accompanied by a decrease of (− S M ), from 5.205 to 0.95 J/kg K for x = 0 and 0.20, respectively, with μ 0 H = 5 T. For all samples, we find quite large values of (− S M ), which are very close to that provided for Gd, the prototypical magnetocaloric material.