White lupin (Lupinus albus) is able to adapt to phosphorus deficiency by producing proteoid roots that release a huge amount of organic acids, resulting in mobilization of sparingly soluble soil phosphate in rhizosphere. The mechanisms responsible for the release of organic acids by proteoid root cells, especially the trans-membrane transport processes, have not been elucidated. Because of high cytosolic pH, the release of undissociated organic acids is not probable. In the present study, we focused on H ϩ export by plasma membrane H ϩ ATPase in active proteoid roots. In vivo, rhizosphere acidification of active proteoid roots was vanadate sensitive. Plasma membranes were isolated from proteoid roots and lateral roots from P-deficient and -sufficient plants. In vitro, in comparison with two types of lateral roots and proteoid roots of P-sufficient plants, the following increase of the various parameters was induced in active proteoid roots of P-deficient plants: (a) hydrolytic ATPase activity, (b) V max and K m , (c) H ϩ ATPase enzyme concentration of plasma membrane, (d) H ϩ -pumping activity, (e) pH gradient across the membrane of plasmalemma vesicles, and (f) passive H ϩ permeability of plasma membrane. In addition, lower vanadate sensitivity and more acidic pH optimum were determined for plasma membrane ATPase of active proteoid roots. Our data support the hypothesis that in active proteoid root cells, H ϩ and organic anions are exported separately, and that modification of plasma membrane H ϩ ATPase is essential for enhanced rhizosphere acidification by active proteoid roots.P is one of the most important plant nutrients that significantly affect growth and metabolism. Although the total amount of P in soil may be high, it is often present in unavailable forms such as phytic acid (Richardson, 1994), or Ca, Fe, and Al phosphates (Holford, 1997). Low availability of P is a major constraint for crop production in many low-input systems of agriculture worldwide, especially in the highly weathered soils of the humid tropics and subtropics, in many sandy soils of the semiarid tropics, and in calcareous soils of the temperate regions, where crop productivity is severely compromised through lack of available P (Raghothama, 1999). Also, after application of P to the soil the recovery of applied P by crop plants in a growing season is very low, because in the soil more than 80% of the P becomes immobile and unavailable for plant uptake due to adsorption on Al or Fe oxides/hydroxides, precipitation with Ca, or conversion to organic forms (Holford, 1997).Higher plants have developed various strategies of acquiring sparingly soluble nutrients from soil. In response to P deficiency, various species from different families develop so-called proteoid roots. These are bottlebrush-like clusters of rootlets of limited growth with an average length of 0.5 to 1 cm. The rootlets are closely arranged along lateral roots and are usually covered with long and dense root hairs (Purnell, 1960; Dinkelaker et al., 1995;Watt and Evans...