Hudson J J, Taylor W D, Schindler D W
Department of Biological Sciences, University of Alberta, Edmonton, Canada.
Nature. 2000 Jul 6;406(6791):54-6. doi: 10.1038/35017531.
Phosphate is an important nutrient that restricts microbial production in many freshwater and marine environments. The actual concentration of phosphate in phosphorus-limited waters is largely unknown because commonly used chemical and radiochemical techniques overestimate the concentration. Here, using a new steady-state radiobioassay to survey a diverse set of lakes, we report phosphate concentrations in lakes that are orders of magnitude lower than estimates made spectrophotometrically or with the frequently used Rigler radiobioassay. Our results, combined with those from the literature, indicate that microbes can achieve rapid turnover rates at picomolar nutrient concentrations. This occurs even though these concentrations are about two orders of magnitude below the level where phosphate uptake is estimated to be half the saturation level for the pico-plankton community. Also, while phosphate concentration increased with the concentration of total phosphorus and soluble reactive phosphorus in the lakes we sampled, the proportion of phosphate in the total phosphorus pool decreased from oligotrophic to eutrophic lakes. Such information, as revealed by the phosphate assay that we use here, should allow us to address hypotheses concerning the concentration of phosphate available to planktonic microorganisms in aquatic systems.
磷酸盐是一种重要的营养物质,在许多淡水和海洋环境中限制着微生物的生长。在磷限制的水体中,磷酸盐的实际浓度很大程度上未知,因为常用的化学和放射化学技术会高估其浓度。在此,我们使用一种新的稳态放射生物测定法对一系列不同的湖泊进行调查,报告了湖泊中磷酸盐的浓度,这些浓度比用分光光度法或常用的里格勒放射生物测定法得出的估计值低几个数量级。我们的结果与文献中的结果相结合,表明微生物在皮摩尔级的营养浓度下能够实现快速周转速率。即使这些浓度比据估计磷吸收量为微微型浮游生物群落饱和水平一半时的浓度低约两个数量级,这种情况仍会发生。此外,虽然在我们采样的湖泊中,磷酸盐浓度随总磷和可溶性活性磷浓度的增加而增加,但在总磷池中磷酸盐的比例从贫营养湖到富营养湖是降低的。我们在此使用的磷酸盐测定法所揭示的此类信息,应能让我们验证有关水生系统中浮游微生物可利用的磷酸盐浓度的假设。