Since the proposal of the chemiosmotic theory(1) there has been a continuing debate about how protons that have been pumped across membranes reach another membrane protein that utilizes the established pH gradient. Evidence has been gathered in favour of a ’delocalized’ theory, in which the pumped protons equilibrate with the aqueous bulk phase before being consumed, and a ’localized’ one, in which protons move exclusively along the membrane surface(2,3). We report here that after proton release by an integral membrane protein, long-range proton transfer along the membrane surface is faster than proton exchange with the bulk water phase. The rate of lateral proton diffusion can be calculated by considering the buffer capacity of the membrane surface. Our results suggest that protons can efficiently diffuse along the membrane surface between a source and a sink (for example H+-ATP synthase) without dissipation losses into the aqueous bulk.