Inputs of allochthonous particulate organic matter were measured durin
g 1992-94 in a headwater conifer swamp stream in southern Ontario, Can
ada. Litter transported to the stream by surface runoff from saturated
areas of the swamp was compared to direct litterfall and lateral tran
sfer from stream banks. Litterfall contributed 61-63 % of the annual l
itter input to the stream in comparison to 14-16 % and 20-25 % for lat
eral bank transfer and swamp surface runoff, respectively. Litterfall
and bank inputs were seasonal with an autumn peak. In contrast, litter
transport by surface runoff occurred mainly in May-September during e
pisodes of rapid overland flow associated with thunderstorms. The annu
al composition of litterfall was approximately 48 % conifer needles, 3
2 % woody tissues and 17 % deciduous leaves. Lateral bank transfer con
tributed a smaller proportion of needles (37.5 %) and a higher proport
ion of leaves (22 %). Litter transported in runoff from the swamp was
mainly woody tissues (70 %) and the needle and leaf fraction comprised
<15 %, indicated that retention and decomposition occurred on the swa
mp surface. These results indicate that surface runoff from headwater
swamps increases the amount and alters the composition and seasonality
of litter inputs to streams.