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Preconditioning to high CO2 exacerbates the response of the Caribbean branching coral Porites porites to high temperature stress

机译:对高CO2的预处理加剧了加勒比分支珊瑚Porites porites对高温胁迫的响应

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Climate change stress on coral reefs occurs as a result of increased temperature and ocean acidification. However, these stressors do not act uniformly: acidification is a 'press' disturbance characterized by chronic increases in CO2, whereas thermal stress is a 'pulse' disturbance characterized by acute episodes of anomalously warm temperatures. Therefore future episodes of thermal stress will develop within the context of pre-existing acidification. Many studies have investigated the effect of combined temperature and CO2 on corals, but no study has yet investigated whether pre-exposing corals to elevated CO2 affects their response to high temperature. We investigated this for the first time using replicate fragments of the Caribbean coral Porites porites preconditioned to either 390 ppm or 900 ppm CO2 at 26 degrees C for 3 mo. After this period, half of the corals from each CO2 level were exposed to 31 degrees C (i.e. 31 degrees C/390 ppm or 31 degrees C/900 ppm) for 2 mo, while the other half were maintained in their original treatments (26 degrees C/390 ppm or 26 degrees C/900 ppm). Calcification, feeding rate, and photochemical efficiency were measured. Corals preconditioned to high CO2 before thermal stress (i.e. 31 degrees C/900 ppm) showed 44% lower calcification rates than the control group, but single stress treatment groups did not experience significant growth reductions. Feeding rates increased for corals exposed to either high CO2 or high temperature singularly, but not when thermal stress was applied following CO2 preconditioning. Photochemical efficiency decreased by 25% for all treatment groups compared to the control. Together, these data suggest that preconditioning to elevated CO2 worsens holobiont response to thermal stress, potentially exacerbating the effects of climate change stressors on coral reefs.
机译:温度升高和海洋酸化导致气候变化对珊瑚礁的压力。但是,这些压力源的作用并不均匀:酸化是特征为CO2长期增加的“压力”扰动,而热应力是特征为异常温暖的温度的急性发作的“脉冲”扰动。因此,未来的热应力将在预先存在的酸化条件下发展。许多研究已经调查了温度和CO2的结合对珊瑚的影响,但是尚未研究过将珊瑚预先暴露于较高的CO2中是否会影响珊瑚对高温的反应。我们首次使用了在26摄氏度下3个月预适应390 ppm或900 ppm CO2的加勒比珊瑚Porites多孔岩的复制片段,对此进行了首次调查。在此期间之后,来自每个CO2水平的一半珊瑚在31摄氏度(即31摄氏度/ 390 ppm或31摄氏度/ 900 ppm)下暴露2个月,而另一半则保持其原始处理状态(26 C / 390 ppm或26 C / 900 ppm)。测量钙化,进料速率和光化学效率。在热应激之前(即31摄氏度/ 900 ppm),将珊瑚预处理至高CO2的情况下,其钙化率比对照组低44%,但单一应激处理组的生长没有明显降低。单独暴露于高CO2或高温的珊瑚的进食速率增加,但在CO2预处理后施加热应力时,进食速率却没有增加。与对照组相比,所有处理组的光化学效率降低了25%。总之,这些数据表明,对升高的CO2进行预处理会使holobiont对热应力的响应变差,从而有可能加剧气候变化压力源对珊瑚礁的影响。

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