Frey Desta L, Gagnon Patrick
Department of Ocean Sciences, Ocean Sciences Centre, Memorial University of Newfoundland, St. John's, Newfoundland and Labrador, Canada, A1C 5S7.
PLoS One. 2015 Mar 16;10(3):e0118583. doi: 10.1371/journal.pone.0118583. eCollection 2015.
In eastern Canada, the destruction of kelp beds by dense aggregations (fronts) of the omnivorous green sea urchin, Strongylocentrotus droebachiensis, is a key determinant of the structure and dynamics of shallow reef communities. Recent studies suggest that hydrodynamic forces, but not sea temperature, determine the strength of urchin-kelp interactions, which deviates from the tenets of the metabolic theory of ecology (MTE). We tested the hypothesis that water temperature can predict short-term kelp bed destruction by S. droebachiensis in calm hydrodynamic environments. Specifically, we experimentally determined relationships among water temperature, body size, and individual feeding in the absence of waves, as well as among wave velocity, season, and aggregative feeding. We quantified variation in kelp-bed boundary dynamics, sea temperature, and wave height over three months at one subtidal site in Newfoundland to test the validity of thermal tipping ranges and regression equations derived from laboratory results. Consistent with the MTE, individual feeding during early summer (June-July) obeyed a non-linear, size- and temperature-dependent relationship: feeding in large urchins was consistently highest and positively correlated with temperature <12°C and dropped within and above the 12-15°C tipping range. This relationship was more apparent in large than small urchins. Observed and expected rates of kelp loss based on sea temperature and urchin density and size structure at the front were highly correlated and differed by one order of magnitude. The present study speaks to the importance of considering body size and natural variation in sea temperature in studies of urchin-kelp interactions. It provides the first compelling evidence that sea temperature, and not only hydrodynamic forces, can predict kelp bed destruction by urchin fronts in shallow reef communities. Studying urchin-seaweed-predator interactions within the conceptual foundations of the MTE holds high potential for improving capacity to predict and manage shifts in marine food web structure and productivity.
在加拿大东部,杂食性的绿海胆(Strongylocentrotus droebachiensis)密集聚集(前沿)对海带床的破坏,是浅海礁石群落结构和动态的关键决定因素。最近的研究表明,水动力而非海水温度决定了海胆与海带相互作用的强度,这与生态代谢理论(MTE)的原则相悖。我们检验了这样一个假设:在平静的水动力环境中,水温可以预测绿海胆对海带床的短期破坏。具体而言,我们通过实验确定了在无波浪情况下水温、体型与个体摄食之间的关系,以及波速、季节与聚集性摄食之间的关系。我们在纽芬兰的一个潮下带地点,对三个月内海带床边界动态、海水温度和波高的变化进行了量化,以检验从实验室结果得出的热临界范围和回归方程的有效性。与生态代谢理论一致,初夏(6月至7月)期间个体摄食遵循一种非线性的、与体型和温度相关的关系:大型海胆的摄食率一直最高,且与低于12°C的温度呈正相关,在12 - 15°C的临界范围内及以上则下降。这种关系在大型海胆中比小型海胆中更明显。基于前沿地带的海水温度、海胆密度和体型结构观察到的和预期的海带损失率高度相关,但相差一个数量级。本研究表明在海胆与海带相互作用的研究中考虑体型和海水温度的自然变化很重要。它提供了首个令人信服的证据,即海水温度,而不仅仅是水动力,能够预测浅海礁石群落中海胆前沿对海带床的破坏。在生态代谢理论的概念框架内研究海胆 - 海藻 - 捕食者的相互作用,对于提高预测和管理海洋食物网结构及生产力变化的能力具有很大潜力。