Sorbonne Université, CNRS, UMR 7144 AD2M, Station Biologique de Roscoff, Place Georges Teissier, Roscoff, F-29680, France.
FOCUS unit, Systematics and Animal Diversity, University of Liège, Sart Tilman B6c, B-4000, Liège, Belgium.
J Phycol. 2020 Dec;56(6):1481-1492. doi: 10.1111/jpy.13041. Epub 2020 Aug 11.
A high proportion of the kelp Laminaria hyperborea production is exported from kelp forests following seasonal storms or natural annual old blade loss. Transport of drifting kelp fragments can lead to temporary accumulations in benthic subtidal habitats. We investigated the degradation processes of L. hyperborea in a low subtidal sandy bottom ecosystem by setting up a 6-month cage experiment to simulate accumulations of kelp fragments on the seafloor. We monitored temporal changes in biomass, nutritional quality (C:N ratio), respiration, quantum efficiency of photosystem II (F /F ), bacterial colonization, and chemical defense concentrations. Biomass decomposition started after 2 weeks and followed a classic negative exponential pattern, leading to 50% degradation after 8 weeks. The degradation process seemed to reach a critical step after 11 weeks, with an increase in respiration rate and phlorotannin concentration in the tissues. These results likely reflect an increase in bacterial activity and a weakening of the kelp cell wall. After 25 weeks of degradation, only 16% of the initial biomass persisted, but the remaining large fragments looked intact. Furthermore, photosystems were still responding to light stimuli, indicating that photosynthesis persisted over time. Reproductive tissues appeared on some fragments after 20 weeks of degradation, showing a capacity to maintain the reproductive function. Our results indicate that L. hyperborea fragments degrade slowly. As they maintain major physiological functions (photosynthesis, reproduction, etc.) and accumulate on adjacent ecosystems, they may play a long-term ecological role in coastal ecosystem dynamics.
由于季节性风暴或自然年度老叶片损失,海带林的高比例海带产量会在海带离开海带林后被输出。漂流海带碎片的运输可能导致底栖亚潮带生境中的临时积聚。我们通过设置一个为期 6 个月的笼式实验来模拟海底海带碎片的积聚,研究了低亚潮带沙质底生态系统中 Laminaria hyperborea 的降解过程。我们监测了生物量、营养质量(C:N 比)、呼吸作用、光系统 II 的量子效率(F / F )、细菌定殖和化学防御浓度的时间变化。生物量分解在 2 周后开始,并遵循经典的负指数模式,导致 8 周后降解 50%。降解过程在 11 周后似乎达到了一个关键步骤,组织中的呼吸速率和岩藻黄质浓度增加。这些结果可能反映了细菌活性的增加和海带细胞壁的弱化。经过 25 周的降解,只有初始生物量的 16%得以保留,但剩余的大碎片看起来完好无损。此外,光系统仍然对光刺激做出反应,表明光合作用随着时间的推移而持续。在降解 20 周后,一些碎片上出现了生殖组织,显示出维持生殖功能的能力。我们的研究结果表明,Laminaria hyperborea 碎片降解缓慢。由于它们保持着主要的生理功能(光合作用、繁殖等)并在相邻的生态系统中积累,它们可能在沿海生态系统动态中发挥长期的生态作用。