The optical conductivity [σ(ω)] spectra of alkaline-earth-filled skutterudites with the chemical formula A 2+ M4Sb12 (A = Sr, Ba, M = Fe, Ru, Os) and a reference material La 3+ Fe4Sb12 were obtained and compared with the corresponding band structure calculations and with calculated σ(ω) spectra to investigate their electronic structures. At high temperatures, the energy of the plasma edge decreased with the increasing valence of the guest atoms A in the Fe4Sb12 cage indicating holetype conduction. A narrow peak with a pseudogap of 25 meV was observed in SrFe4Sb12, while the corresponding peak were located at 200 and 100 meV in the Ru-and Os-counterparts, respectively. The order of the peak energy in these compounds is consistent with the thermodynamical properties in which the Os-compound is located between the Fe-and Ru-compounds. This indicated that the electronic structure observed in the infrared σ(ω) spectra directly affects the thermodynamical properties. The band structure calculation implies the different electronic structure among these compounds originates from the different d states of the M ions.