Biological studies in the vicinity of a shallow-sea tidal mixing front III. Seasonal and spatial distribution of heterotrophic uptake of glucose

Abstract

Heterotrophic incorporation and respiration of 14C-labelled glucose (tracer approach) and natural concentrations of glucose were measured, as part of a multidisciplinary research projection five cruises in the western Irish Sea from M arch to September 1980. The investigations were carried out along a transect across a shallow-sea tidal mixing front and its adjacent stratified and vertically mixed water masses. The spatial distribution pattern in relation to hydrographical conditions, diurna changes observed at drogue stations, and seasonal developments are described. High turnover rates of [14C]glucose were strongly associated with stratification, both spatially as well as seasonally, starting with low rates early in spring at the beginning of stratification, increasing to maxim um rates in July after the phytoplankton bloom, and subsequent y declining in autumn when stratification weakened. Turnover rates were consistently and significantly higher in the waters above the pycnocline than below it or in the vertically mixed water masses to the east of the front. No distinct diurnal rhythm s were recognized. The mixed water column, in particular, was totally uniform in heterotrophic uptake of glucose whereas the surface of the stratified water showed greater variability. A fairly constant proportion of, on average, 32 % of the glucose carbon was respired. Natural glucose concentration ranged from less than 30 to 322 nM, mean 116 nM. No particular pattern in its distribution could be detected in the different water masses despite considerable changes in use of glucose. Turnover rates of glucose were unrelated to numbers of bacterial cells or their biomass. Glucose uptake per bacterial cell (uptake index) was estimated and showed pronounced seasonal increase during sum m er in the surface stratified water mass, especially, in the vicinity of the front. The importance of the surface waters of the stratified water body and the frontal zone in respect to carbon flux and potential bacterial biomass production is discussed.