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Metabolic Microenvironmental Control by Photosynthetic Biofilms under Changing Macroenvironmental Temperature and pH Conditions

机译:在变化的大环境温度和pH条件下光合生物膜对代谢微环境的控制

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摘要

Ex situ microelectrode experiments, using cyanobacterial biofilms from karst water creeks, were conducted under various pH, temperature, and constant-alkalinity conditions to investigate the effects of changing environmental parameters on cyanobacterial photosynthesis-induced calcification. Microenvironmental chemical conditions around calcifying sites were controlled by metabolic activity over a wide range of photosynthesis and respiration rates, with little influence from overlying water conditions. Regardless of overlying water pH levels (from 7.8 to 8.9), pH at the biofilm surface was approximately 9.4 in the light and 7.8 in the dark. The same trend was observed at various temperatures (4°C and 17°C). Biological processes control the calcium carbonate saturation state (Ω) in these and similar systems and are able to maintain Ω at approximately constant levels over relatively wide environmental fluctuations. Temperature did, however, have an effect on calcification rate. Calcium flux in this system is limited by its diffusion coefficient, resulting in a higher calcium flux (calcification and dissolution) at higher temperatures, despite the constant, biologically mediated pH. The ability of biological systems to mitigate the effects of environmental perturbation is an important factor that must be considered when attempting to predict the effects of increased atmospheric partial CO2 pressure on processes such as calcification and in interpreting microfossils in the fossil record.
机译:使用岩溶水小溪中的蓝藻生物膜在不同的pH,温度和恒定碱度条件下进行了异位微电极实验,以研究变化的环境参数对蓝藻光合作用诱导的钙化的影响。在广泛的光合作用和呼吸速率范围内,代谢活动控制着钙化部位周围的微环境化学条件,而上覆水条件的影响很小。不管上方的水pH值(从7.8到8.9)如何,生物膜表面的pH值在明亮时约为9.4,在黑暗时约为7.8。在各种温度(4°C和17°C)下观察到相同的趋势。在这些系统和类似系统中,生物过程控制着碳酸钙饱和状态(Ω),并且能够在相对较大的环境波动下将Ω维持在近似恒定的水平。然而,温度确实对钙化速率有影响。该系统中的钙通量受到其扩散系数的限制,尽管在生物学上介导的pH值恒定,但在较高的温度下会导致较高的钙通量(钙化和溶解)。生物系统缓解环境扰动影响的能力是一个重要因素,当试图预测大气中二氧化碳分压升高对钙化等过程以及化石记录中的微化石的解释时,必须考虑这一重要因素。

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