Downstream change in leucine aminopeptidase activity and leucine assimilation by epilithic microbiota along the River Swale, northern England.

Parallel determinations of epilithic extracellular leucine aminopeptidase activity and leucine assimilation were made at five sites along 112 km of the River Swale and also in two tributaries, the River Wiske and Cod Beck. Epilithic leucine aminopeptidase activity along the Swale increased with distance downstream; this increase was gradual, rather than stepwise in response to specific sewage-works outfalls. Epilithic leucine assimilation, in contrast, did not consistently increase along the river. Epilithic leucine aminopeptidase activity and leucine assimilation were both potentially controlled by epilithic microbial variables (bacterial abundance and chlorophyll a) while leucine aminopeptidase activity was also strongly related to water-quality variables, especially temperature, pH and conductivity. Epilithic leucine aminopeptidase activity and leucine assimilation were coupled, but the magnitude of aminopeptidase activity was always substantially greater than that of leucine assimilation. Arguments are presented, however, which suggest that this did not necessarily indicate the constant availability of excess leucine, and by inference amino-acid nitrogen, to epilithic bacteria. Values of epilithic leucine aminopeptidase activity and leucine assimilation, expressed relative to rates in overlying water, suggested that most activity and assimilation was epilithic rather than planktonic, although the planktonic contribution was proportionately greater at the deeper, more downstream, sites. In the tributaries, River Wiske and Cod Beck, values of epilithic leucine aminopeptidase activity and epilithic microbial abundance, as well as those of many water-quality variables, resembled values in the middle and lower Swale. Thus, these tributaries were essentially lowland, enriched watercourses being very different from the headstreams of the main river.