Buctouche Spit is an 11-km long sandy spit on the northeast shore of New Brunswick, Canada. It is a typical flying spit, having a narrow proximal section which is characterized by a single foredune that is prone to overwash and transgression, and a much wider prograding distal section which is characterized by a well-developed foredune backed by a series of relict foredunes. An optical-luminescence dating method in which infrared stimulation is used on potassium feldspars was developed for this study. It is a very promising method for dating Holocene deposits, yielding good resolution and having simplicity of measurement. The luminescence ages obtained indicate that Buctouche Spit extended at a rate of ~4 m yr −1 between 715 ± 45 years ago and 240 ± 25 years ago. This extension rate equates to a distal end accumulation rate of ~ 56,000 m 3 yr −1 for this period. At this rate of accretion, the present Buctouche Spit would have formed during the past 2000 years. The core data indicate that the spit is ⩾2200 years old, which is consistent with the preceding estimate. Since 240 ± 25 years ago, the rate of sediment accumulation at Buctouche Spit has apparently been falling. The accumulation rate between 1839 and 1945 was ~23,000 m 3 yr −1, less than half of the historic rate of ~56,000 m 3 yr −1. Since 1945, the distal end of Buctouche Spit has not prograded/extended measurably. This is because Buctouche Spit's present vertical growth rate is, at most, equal to the rate of relative sea-level rise at the spit and may be as little as half of the rate of relative sea-level rise. Present sediment supply to Buctouche Spit is probably < 16,000 m 3 yr −1. It is likely that the much larger sediment supply required to sustain an historic accretion rate of ~ 56,000 m 3 yr −1 was derived from the reworking of a former sandy barrier located seaward, and possibly updrift of, the present spit. Buctouche Spit is now in a limited sediment supply situation and it has become a constrained spit. Sediment is being eroded from the centre section of the spit, transported to the distal end, and then carried away by ebb-tidal currents. The centre section of the spit will likely breach within the next hundred years. If a breach (or breaches) becomes permanently established in the centre section of the spit, the distal end will suffer significant erosion and may be destroyed. After this, the cycle of rebuilding and landward migration would likely start again at a new location landward of the present spit as relative sea level continues to rise. It is concluded that the key to understanding Buctouche Spit's long-term evolution is recognizing that it is migrating landward both by continuous processes like overwash, and by the more discrete and catastrophic process of overstepping.