工业革命以来由于化石燃料的大量燃烧,大气CO<sub>2</sub>水平不断增加,预计在21世纪末将增至现有水平的两倍,达到750 μL/L。作为全球初级生产力的重要贡献者,浮游植物应对CO<sub>2</sub>水平升高的生理生态响应必然会对水生生态系统和碳、氮等元素的生物地球化学循环产生重要影响。全球CO<sub>2</sub>水平的升高将显著改变水体的碳化学环境,淡水生态系统(湖泊和河流)由于容量小变化比海洋更为显著。水体碳化学环境的改变首先会影响浮游植物个体,在高CO<sub>2</sub>水平下,浮游植物的细胞会有变小的趋势,并且细胞的光合作用强度也会有不同程度的增加,其中细胞较小或者不具有碳浓缩机制(CCM)的浮游植物增加较多,此外浮游植物细胞的化学元素计量值也将显著改变。随后浮游植物个体水平上的变化会进一步影响水生生态系统,例如水体初级生产力水平的提高,浮游植物、浮游动物群落结构组成以及水体微食物网结构的变化等。此外浮游植物对CO<sub>2</sub>水平升高的生理生态响应程度还与水体的营养水平有关。总结了大气CO<sub>2</sub>水平升高对浮游植物生理生态影响的研究方法,展望了未来可能的研究方向。;With the increase of global carbon emissions since the industrial revolution, atmospheric CO<sub>2</sub> level is expected to be twice higher than the present level at the end of this century, reaching to 750 μL/L. As atmospheric CO<sub>2</sub> is the most important source of soluble CO<sub>2</sub> in water due to the deliberate CO<sub>2</sub> sequestration, global CO<sub>2</sub> elevation would significantly alter carbonate chemical environments of aquatic ecosystems. When atmospheric CO<sub>2</sub> concentration doubles at the end of century, it is predicted that pH value of surface oceans would drop approximately 0.3 units, the concentration of bicarbonate ion would increase by 6%, and carbonate ion concentration would decrease by 50%. Considering the smaller buffering capacity of freshwater ecosystems than that of oceans, carbonate chemical environments of freshwater lakes and rivers may change more notably after the increase of CO<sub>2</sub> level. The shift of carbonate chemistry would in turn have dramatic effects on aquatic ecosystems. Phytoplankton has been used widely as an indicator of changes of aquatic ecosystems because this relatively short-lived organism responds rapidly to subtle changes. Meanwhile, it contributes approximately 50% of the total global primary productivity, which plays a vital role in global carbon cycling. Therefore, the physiological and ecological responses of phytoplankton to global CO<sub>2</sub> elevation would have great significance on water ecosystems and biogeochemical cycle. Elevated carbon resource could enhance the photosynthetic activity of phytoplankton, particularly small phytoplankton or non-CCM (non-carbon concentration mechanism) phytoplankton. When CO<sub>2</sub> level increases, the cell size of phytoplankton would potentially decrease, and the elemental ratio of carbon to nitrogen in phytoplankton cell would increase up to more than 10%. Then, those changes in the individual phytoplankton cell would cause certain variations in the ecological level. Primary productivity would rise significantly as a result of enhanced photosynthetic activity of phytoplankton. The shift in assemblage composition of phytoplankton, and the variation of elemental ratio could affect the edibility of phytoplankton, which would alter the abundances and the community structure of zooplankton. Furthermore, the accumulating concentration of organic carbon in water would promote the growth and reproduction of heterotrophic bacterioplankton, which would strengthen the competition between bacterioplankton and phytoplankton for nutrients, such as nitrogen and phosphorus. More importantly, elevated CO<sub>2</sub> effects differ between oligotrophic and eutrophic water body. It is expected that effects on algal productivity in eutrophic aquatic ecosystems could be potentially larger, since in eutrophic water the input of nitrogen and phosphorus to the global biochemical cycle exceeds that of the carbon input by several orders of magnitude. Finally, we summarized the development of the methodology for studying the effect of enhanced CO<sub>2</sub> level on water ecosystems. Long-term in situ simulating experiment would be the best approach for studying the effect of enhanced CO<sub>2</sub> on natural phytoplankton community. In future research, picophytoplankton will attract more attention, since they are sensitive to the change of CO<sub>2</sub> level compared with large ones because of their high surface-area-to-volume ratio. In addition, more efforts should be exerted for freshwater ecosystems with respect to elevated CO<sub>2</sub> effects, as they are far less investigated than marine ecosystems even though they are closely linked to the survival of human being.