Lead concentrations and isotope ratios were measured in North Atlantic surface water samples collected in 1981 (29¿--79¿N, 6¿E--49¿W) and in 1989 (23¿--39¿N, 29¿--68¿W). In the early 1980s, 206Pb/207Pb ratios in the North African Basin averaged 1.193 ¿ 0.005 (1 σ). Similar radiogenic ratios within the level of analytical precision (average 0.29%) were found in the Labrador and Iceland Basins (1.198 ¿ 0.006) and in the Norwegian Sea (1.196 ¿ 0.008). These radiogenic mixed layer signatures along with atmospheric global lead emission patterns suggest that most North Atlantic lead in the early 1980s was derived from North American leaded gasoline. Samples in the East Iberian Basin near Portugal and France showed lower 206Pb/207Pb ratios, between 1.167 and 1.182, indicating a significant influence of less radiogenic atmospheric lead transported from Europe and possibly the influence of the Rio Tinto acid mine drainage very close to shore in the Gulf of Cadiz. across the entire North Atlantic Basin ranged between 54 and 145 pmol/kg, with the lowest values (54--74 pmol/kg) found at high latitudes (>65¿N). In the late 1980s, surface waters in the western subtropical North Atlantic (North American Basin/Sargasso Sea, >47¿W) and in the eastern subtropical North Atlantic (North African Basin/Central Iberian Basin, 53%). These elemental and isotopic results demonstrate the strongly variable isotopic and elemental signatures of North American and European lead throughout the North Atlantic Ocean, frequently dominated by high 206Pb/207Pb and North American signatures throughout the subtropical North Atlantic gyre.