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Temperature Modulates Coccolithophorid Sensitivity of Growth, Photosynthesis and Calcification to Increasing Seawater pCO2

机译:温度调节生长,光合作用和钙化对增加海水pCO2的球墨镜的敏感性

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摘要

Increasing atmospheric CO2 concentrations are expected to impact pelagic ecosystem functioning in the near future by\uddriving ocean warming and acidification. While numerous studies have investigated impacts of rising temperature and\udseawater acidification on planktonic organisms separately, little is presently known on their combined effects. To test for\udpossible synergistic effects we exposed two coccolithophore species, Emiliania huxleyi and Gephyrocapsa oceanica, to a CO2\udgradient ranging from ,0.5–250 mmol kg21 (i.e. ,20–6000 matm pCO2) at three different temperatures (i.e. 10, 15, 20uC for\udE. huxleyi and 15, 20, 25uC for G. oceanica). Both species showed CO2-dependent optimum-curve responses for growth,\udphotosynthesis and calcification rates at all temperatures. Increased temperature generally enhanced growth and\udproduction rates and modified sensitivities of metabolic processes to increasing CO2. CO2 optimum concentrations for\udgrowth, calcification, and organic carbon fixation rates were only marginally influenced from low to intermediate\udtemperatures. However, there was a clear optimum shift towards higher CO2 concentrations from intermediate to high\udtemperatures in both species. Our results demonstrate that the CO2 concentration where optimum growth, calcification and\udcarbon fixation rates occur is modulated by temperature. Thus, the response of a coccolithophore strain to ocean\udacidification at a given temperature can be negative, neutral or positive depending on that strain’s temperature optimum.\udThis emphasizes that the cellular responses of coccolithophores to ocean acidification can only be judged accurately when\udinterpreted in the proper eco-physiological context of a given strain or species. Addressing the synergistic effects of\udchanging carbonate chemistry and temperature is an essential step when assessing the success of coccolithophores in the\udfuture ocean.
机译:预计大气中CO2浓度的增加将在不久的将来通过推动海洋变暖和酸化影响中上层生态系统的功能。尽管大量研究分别研究了温度升高和海水酸化对浮游生物的影响,但目前对它们的综合影响知之甚少。为了测试\不可能的协同作用,我们在三种不同温度(即10、15、15、10、15)下,将两种葫芦科植物,Emiliania huxleyi和Gephyrocapsa oceanica暴露于0.5-250 mmol kg21(即20-6000 matm pCO2)的CO2梯度。 ,对于huxleyi为20uC,对大肠埃希菌为15、20、25uC)。两种物种在所有温度下均表现出依赖于二氧化碳的最佳曲线响应,用于生长,光合作用和钙化速率。升高的温度通常会提高生长和繁殖速度,并改善代谢过程对增加CO2的敏感性。二氧化碳的最佳生长,钙化和固定有机碳的浓度仅受低温至中温的影响很小。然而,在两个物种中,都有一个明显的最佳转变,即从较高的温度向较高的高温转变为较高的CO2浓度。我们的结果表明,发生最佳生长,钙化和\碳固定的二氧化碳浓度受温度调节。因此,根据给定温度下的温度,球石藻菌株对海洋\ udacidization的响应可以是负,中性或正。\ ud这强调只有在解释时,才能准确判断球墨镜对海洋酸化的细胞响应在给定菌株或物种的适当生态生理环境下。在评估未来海洋中球墨镜的成功性时,解决碳酸盐化学和温度变化的协同效应是必不可少的步骤。

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