The Al rich variety of perrierite has been found in sapphirine -quartz bearing ultrahigh temperature (UHT) gneiss from Mt. Riiser Larsen in the Napier Complex, East Antarctica. The major constituents of this perrierite bearing gneiss are quartz, orthopyroxene, sapphirine, and osumilite, with minor biotite, K feldspar, and cordierite. Perrierite, zircon, monazite, and rutile are accessory phases. The perrierite grains have diameters in the range 50 500 μm and are pale brownish orange in color. . Both perrierite and monazite may have been stable accessory phases during UHT metamorphism, and the occurrence of perrierite in this sample is possibly controlled by the relatively low phosphorous and high REE and titanium contents.