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Interacting effects of CO2 partial pressure and temperature on photosynthesis and calcification in a scleractinian coral

机译:CO2分压和温度对巩膜珊瑚光合作用和钙化的相互作用

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We show here that CO2 partial pressure (pCO(2)) and temperature significantly interact on coral physiology. The effects of increased pCO(2) and temperature on photosynthesis, respiration and calcification rates were investigated in the scleractinian coral Stylophora pistillata. Cuttings were exposed to temperatures of 25degreesC or 28degreesC and to pCO(2) values of ca. 460 or 760 muatm for 5 weeks. The contents of chlorophyll c(2) and protein remained constant throughout the experiment, while the chlorophyll a content was significantly affected by temperature, and was higher under the 'high-temperature-high-pCO(2)' condition. The cell-specific density was higher at 'high pCO(2)' than at 'normal pCO(2)' (1.7 vs. 1.4). The net photosynthesis normalized per unit protein was affected by both temperature and pCO(2), whereas respiration was not affected by the treatments. Calcification decreased by 50% when temperature and pCO(2) were both elevated. Calcification under normal temperature did not change in response to an increased pCO(2). This is not in agreement with numerous published papers that describe a negative relationship between marine calcification and CO2. The confounding effect of temperature has the potential to explain a large portion of the variability of the relationship between calcification and pCO(2) reported in the literature, and warrants a re-evaluation of the projected decrease of marine calcification by the year 2100.
机译:我们在这里显示,CO2分压(pCO(2))和温度在珊瑚生理上有显着相互作用。研究了scleractinian珊瑚Stylophora pistillata中pCO(2)和温度升高对光合作用,呼吸作用和钙化速率的影响。钻屑暴露在25摄氏度或28摄氏度的温度下,并且暴露于约pCO(2)的值。 460或760 muatm,持续5周。在整个实验过程中,叶绿素c(2)和蛋白质的含量保持恒定,而叶绿素a含量受温度的显着影响,并且在“高温-高-pCO(2)”条件下更高。 “高pCO(2)”下的细胞比密度比“正常pCO(2)”下的高(1.7 vs. 1.4)。标准化的每单位蛋白质的净光合作用受温度和pCO(2)的影响,而呼吸不受处理的影响。当温度和pCO(2)都升高时,钙化降低50%。在正常温度下钙化没有改变以增加pCO(2)。这与描述海洋钙化与CO2负相关的众多发表的论文不一致。温度的混杂效应有可能解释文献中报道的钙化与pCO(2)之间关系的大部分变化,并有必要对到2100年海洋钙化的预计减少进行重新评估。

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