Miller Cale A, Gazeau Frédéric, Lebrun Anaïs, Alliouane Samir, Urrutti Pierre, Schlegel Robert W, Gattuso Jean-Pierre, Comeau Steeve
CNRS, Laboratoire d'Océanographie de Villefranche Sorbonne Université Villefranche-sur-Mer France.
Present address: Department of Earth Sciences Geosciences, Utrecht University Utrecht The Netherlands.
Ecol Evol. 2024 Sep 29;14(10):e70183. doi: 10.1002/ece3.70183. eCollection 2024 Oct.
Fjord systems in the Norwegian Arctic are experiencing an increasing frequency and magnitude of marine heatwaves. These episodic heat stress events can have varying degrees of acute impacts on primary production and nutrient uptake of mixed kelp communities, as well as modifying the biogeochemical cycling in nearshore systems where vast areas of kelp create structural habitat. To assess the impact of future marine heatwaves on kelp communities, we conducted a 23 day mesocosm experiment exposing mixed kelp communities to warming and heatwave scenarios projected for the year 2100. Three treatments were considered: a constant warming (+1.8°C from the control), a medium magnitude and long duration heatwave event (+2.8°C from the control for 13 days), and two short-term, more intense, heatwaves(5 day long scenarios with temperature peaks at +3.9°C from the control). The results show that both marine heatwave treatments reduced net community production, whereas the constant warm temperature treatment displayed no difference from the control. The long marine heatwave scenario resulted in reduced accumulated net community production, indicating that prolonged exposure had a greater severity than two high magnitude, short-term heatwave events. We estimated an 11°C temperature threshold at which negative effects to primary production appeared present. We highlight that marine heatwaves can induce sublethal effects on kelp communities by depressing net community production. These results are placed in the context of potential physiological resilience of kelp communities and implications of reduced net community production to future Arctic fjord environmental conditions.
挪威北极地区的峡湾系统正在经历海洋热浪的频率和强度不断增加的情况。这些偶发的热应激事件会对混合海带群落的初级生产和养分吸收产生不同程度的急性影响,同时还会改变近岸系统中的生物地球化学循环,在这些近岸系统中,大片海带形成了结构性栖息地。为了评估未来海洋热浪对海带群落的影响,我们进行了一项为期23天的中尺度实验,将混合海带群落暴露在预测的2100年变暖及热浪情景下。考虑了三种处理方式:持续变暖(比对照组高1.8°C)、中等强度和持续时间较长的热浪事件(比对照组高2.8°C,持续13天),以及两次短期、强度更大的热浪(5天的情景,温度峰值比对照组高3.9°C)。结果表明,两种海洋热浪处理方式都降低了群落净产量,而持续温暖温度处理与对照组没有差异。长期海洋热浪情景导致群落净产量累计减少,这表明长时间暴露的严重程度高于两次高强度、短期的热浪事件。我们估计,当温度阈值达到11°C时,对初级生产会出现负面影响。我们强调,海洋热浪会通过抑制群落净产量对海带群落产生亚致死效应。这些结果是在海带群落潜在生理恢复力的背景下得出的,以及群落净产量减少对未来北极峡湾环境条件的影响。