Department of Microbiology, Montana State University, 59717, Bozeman, Montana, USA.
Microb Ecol. 1982 Oct;8(2):115-26. doi: 10.1007/BF02010445.
Previous studies of an epilithic algal-bacterial community in a pristine mountain stream suggested that heterotrophic bacteria were responding to the metabolic activities of the phototrophic population. Subsequent studies were performed to follow the flow of labeled carbon, from its initial inorganic form, through the trophic levels of the mat community. A majority of primary production metabolites were excreted by the algal population during active growth; this shifted to an incorporation into cellular material as phototrophic activity declined. Results suggest that there was a direct flux of soluble algal products to the bacterial population, with little heterotrophic utilization of dissolved organics from the overlying stream water. Both phototrophic productivity and bacterial utilization of algal products peaked at approximately the same time of year. Activity of the diatom-dominated algal population declined as silica concentrations in the stream water dropped, leading to a situation in which the sessile bacteria were substrate limited. These events resulted in an almost complete disappearance of the community in early September.
先前对原始山溪中石生藻-细菌群落的研究表明,异养细菌对光养种群的代谢活动有响应。随后进行了进一步的研究,以追踪标记碳从其初始无机形式流经席状群落的营养级。在活跃生长过程中,藻类种群排出了大部分初级生产代谢物;随着光养活性的下降,这些代谢物转而被纳入细胞物质。结果表明,有可溶性藻类产物直接流向细菌种群,而对来自上覆溪流水中的溶解有机物的异养利用很少。光养生产力和细菌对藻类产物的利用都在同年的大致同一时间达到峰值。随着溪流水中硅浓度的下降,以硅藻为主的藻类种群的活动减少,导致固着细菌受到基质限制。这些事件导致该群落于 9 月初几乎完全消失。