Many previous studies have examined the transfer of organic carbon in river systems within suspended sediment (fine particles carried in suspension making the water appear muddy etc..), however, few have looked at how much carbon is transported with bedload (coarser sand and pebbles that bounce along the base of the channel). This paper looks at the fluxes of carbon in the bedload and finds they are a far smaller percentage than that carried as suspended load, but may be more important for long term sinks or stores of carbon as they are more readily deposited in sediments that may become buried for a considerable period of time.