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In situ response of Antarctic under-ice primary producers to experimentally altered pH

机译:南极冰原主产地对实验改变的pH值的原位响应

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摘要

Elevated atmospheric CO2 concentrations are contributing to ocean acidification (reduced seawater pH and carbonate concentrations), with potentially major ramifications for marine ecosystems and their functioning. Using a novel in situ experiment we examined impacts of reduced seawater pH on Antarctic sea ice-associated microalgal communities, key primary producers and contributors to food webs. pH levels projected for the following decades-to-end of century (7.86, 7.75, 7.61), and ambient levels (7.99), were maintained for 15 d in under-ice incubation chambers. Light, temperature and dissolved oxygen within the chambers were logged to track diurnal variation, with pH, O2, salinity and nutrients assessed daily. Uptake of CO2 occurred in all treatments, with pH levels significantly elevated in the two extreme treatments. At the lowest pH, despite the utilisation of CO2 by the productive microalgae, pH did not return to ambient levels and carbonate saturation states remained low; a potential concern for organisms utilising this under-ice habitat. However, microalgal community biomass and composition were not significantly affected and only modest productivity increases were noted, suggesting subtle or slightly positive effects on under-ice algae. This in situ information enables assessment of the influence of future ocean acidification on under-ice community characteristics in a key coastal Antarctic habitat.
机译:大气中CO2浓度升高正在促进海洋酸化(海水pH值和碳酸盐浓度降低),并可能对海洋生态系统及其功能产生重大影响。我们使用新颖的原位实验研究了海水pH值降低对南极海冰相关微藻群落,主要初级生产者和食物网贡献者的影响。在冰下孵化室中,预计下一个世纪到下个世纪末的pH值(7.86、7.75、7.61)和环境水平(7.99)保持15 d。记录室内的光,温度和溶解氧,以跟踪日变化,每天评估pH,O2,盐度和营养素。在所有处理中均发生CO 2吸收,在两种极端处理中pH值均显着升高。在最低pH值下,尽管生产性微藻利用了CO2,但pH值未恢复到环境水平,碳酸盐饱和度状态仍然很低。利用这种冰底栖息地的生物可能会担心。但是,微藻群落的生物量和组成并未受到显着影响,仅注意到适度的生产率提高,表明对冰下藻类产生微妙或轻微的积极影响。这些原位信息可以评估未来海洋酸化对南极主要沿海生境中冰下群落特征的影响。

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