Ecosystem subsidies, the movement of resources across ecosystem boundries (Polis 1997), are an important part of organic matter cycling in aquatic systems. The reciprical transfer of resources between aquatic and terrestrial systems is common (Nakano 2001), however the input of terrestrial organic matter to aquatic systems is an especially significant flux of material since, this subsidy has been shown to support metabolism and secondary production in a majority of lentic and lotic ecosystems(Marcarelli 2011). Organic matter subsidies from terrestrial to aquatic ecosystems are dominated by detrital plant material either as dissolved (DOC) or particulate (POC) organic carbon, and can substantially augment autochthonous organic matter production (Hodkinson 1975, GASITH 1976, (citation n