Acidic soils account for approximately 50% of the world's potentially arable lands but significantly limit crop production (Kochian, Hoekenga, & Piñeros, 2004). Many crops grow poorly in acid soils because of acid soil syndrome, which consists of multiple stress factors, including phytotoxicity to excess ions such as aluminum (Al 3+), protons (H +), and manganese (Mn 2+), and/or deficiencies of essential minerals such as calcium (Ca), magnesium (Mg), and phosphorus (P) (Kochian et al., 2004). In particular, Al 3+ stress causes inhibition of nutrient uptake or transport (Lee & Pritchard, 1984; Mariano & Keltjens, 2005) and suppression of root growth (Kinraide, 2003); therefore, Al 3+ rhizotoxicity is an important factor limiting plant productivity. In addition, excess Al 3+ and H + compete with other cations for apoplastic binding sites (Horst, Wang, &