Hurd Catriona L, Hepburn Christopher D, Currie Kim I, Raven John A, Hunter Keith A
Department of Botany, University of Otago, PO Box 56, Dunedin 9054, New ZealandNational Institute for Water and Atmospheric Research Ltd., Centre of Excellence for Chemical and Physical Oceanography, Department of Chemistry, University of Otago, PO Box 56, Dunedin 9054, New ZealandDivision of Plant Sciences, Scottish Crop Research Institute, University of Dundee at SCRI, Invergowrie, Dundee DD2 5DA, UKDepartment of Chemistry, University of Otago, PO Box 56, Dunedin 9054, New Zealand.
J Phycol. 2009 Dec;45(6):1236-51. doi: 10.1111/j.1529-8817.2009.00768.x. Epub 2009 Nov 13.
Ocean acidification describes changes in the carbonate chemistry of the ocean due to the increased absorption of anthropogenically released CO2 . Experiments to elucidate the biological effects of ocean acidification on algae are not straightforward because when pH is altered, the carbon speciation in seawater is altered, which has implications for photosynthesis and, for calcifying algae, calcification. Furthermore, photosynthesis, respiration, and calcification will themselves alter the pH of the seawater medium. In this review, algal physiologists and seawater carbonate chemists combine their knowledge to provide the fundamental information on carbon physiology and seawater carbonate chemistry required to comprehend the complexities of how ocean acidification might affect algae metabolism. A wide range in responses of algae to ocean acidification has been observed, which may be explained by differences in algal physiology, timescales of the responses measured, study duration, and the method employed to alter pH. Two methods have been widely used in a range of experimental systems: CO2 bubbling and HCl/NaOH additions. These methods affect the speciation of carbonate ions in the culture medium differently; we discuss how this could influence the biological responses of algae and suggest a third method based on HCl/NaHCO3 additions. We then discuss eight key points that should be considered prior to setting up experiments, including which method of manipulating pH to choose, monitoring during experiments, techniques for adding acidified seawater, biological side effects, and other environmental factors. Finally, we consider incubation timescales and prior conditioning of algae in terms of regulation, acclimation, and adaptation to ocean acidification.
海洋酸化描述的是由于海洋对人为排放的二氧化碳吸收增加而导致的海洋碳酸盐化学变化。阐明海洋酸化对藻类生物效应的实验并非易事,因为当pH值改变时,海水中的碳形态也会改变,这对光合作用以及钙化藻类的钙化作用都会产生影响。此外,光合作用、呼吸作用和钙化作用本身也会改变海水介质的pH值。在这篇综述中,藻类生理学家和海水碳酸盐化学家结合他们的知识,提供了理解海洋酸化如何影响藻类代谢复杂性所需的关于碳生理和海水碳酸盐化学的基础信息。已观察到藻类对海洋酸化的反应范围很广,这可能是由藻类生理差异、所测反应的时间尺度、研究持续时间以及改变pH值所采用的方法等因素造成的。有两种方法在一系列实验系统中被广泛使用:二氧化碳鼓泡法和添加盐酸/氢氧化钠法。这些方法对培养基中碳酸根离子形态的影响不同;我们讨论了这如何可能影响藻类的生物学反应,并提出了一种基于添加盐酸/碳酸氢钠的第三种方法。然后我们讨论了在开展实验之前应考虑的八个要点,包括选择哪种调节pH值的方法、实验过程中的监测、添加酸化海水的技术、生物学副作用以及其他环境因素。最后,我们从调节、驯化和适应海洋酸化的角度考虑了藻类的培养时间尺度和预先处理。