Jueterbock Alexander, Smolina Irina, Coyer James A, Hoarau Galice
Faculty of Biosciences and Aquaculture Nord University Universitetsalleen 11 8049 Bodø Norway.
Shoals Marine Laboratory University of New Hampshire Durham New Hampshire 03824 USA.
Ecol Evol. 2016 Feb 16;6(6):1712-24. doi: 10.1002/ece3.2001. eCollection 2016 Mar.
Rising temperatures are predicted to melt all perennial ice cover in the Arctic by the end of this century, thus opening up suitable habitat for temperate and subarctic species. Canopy-forming seaweeds provide an ideal system to predict the potential impact of climate-change on rocky-shore ecosystems, given their direct dependence on temperature and their key role in the ecological system. Our primary objective was to predict the climate-change induced range-shift of Fucus distichus, the dominant canopy-forming macroalga in the Arctic and subarctic rocky intertidal. More specifically, we asked: which Arctic/subarctic and cold-temperate shores of the northern hemisphere will display the greatest distributional change of F. distichus and how will this affect niche overlap with seaweeds from temperate regions? We used the program MAXENT to develop correlative ecological niche models with dominant range-limiting factors and 169 occurrence records. Using three climate-change scenarios, we projected habitat suitability of F. distichus - and its niche overlap with three dominant temperate macroalgae - until year 2200. Maximum sea surface temperature was identified as the most important factor in limiting the fundamental niche of F. distichus. Rising temperatures were predicted to have low impact on the species' southern distribution limits, but to shift its northern distribution limits poleward into the high Arctic. In cold-temperate to subarctic regions, new areas of niche overlap were predicted between F. distichus and intertidal macroalgae immigrating from the south. While climate-change threatens intertidal seaweeds in warm-temperate regions, seaweed meadows will likely flourish in the Arctic intertidal. Although this enriches biodiversity and opens up new seaweed-harvesting grounds, it will also trigger unpredictable changes in the structure and functioning of the Arctic intertidal ecosystem.
预计到本世纪末,气温上升将使北极地区所有常年冰盖融化,从而为温带和亚北极物种开辟适宜的栖息地。鉴于形成冠层的海藻直接依赖温度且在生态系统中发挥关键作用,它们为预测气候变化对岩岸生态系统的潜在影响提供了一个理想的系统。我们的主要目标是预测气候变化导致的北极和亚北极岩质潮间带中占主导地位的形成冠层的大型海藻——叉开网翼藻(Fucus distichus)的分布范围变化。更具体地说,我们提出以下问题:北半球哪些北极/亚北极和寒温带海岸将呈现叉开网翼藻最大的分布变化,以及这将如何影响其与温带地区海藻的生态位重叠?我们使用MAXENT程序,结合主要的范围限制因素和169个出现记录,开发相关的生态位模型。利用三种气候变化情景,我们预测了叉开网翼藻的栖息地适宜性——及其与三种主要温带大型海藻的生态位重叠——直至2200年。最高海表温度被确定为限制叉开网翼藻基本生态位的最重要因素。预计气温上升对该物种的南半部分布界限影响较小,但会使其北半部分布界限向极地移动至高北极地区。在寒温带至亚北极地区,预计叉开网翼藻与从南方迁入的潮间带大型海藻之间将出现新的生态位重叠区域。虽然气候变化威胁着暖温带地区的潮间带海藻,但海藻草甸可能会在北极潮间带蓬勃发展。尽管这丰富了生物多样性并开辟了新的海藻收获地,但也将引发北极潮间带生态系统结构和功能的不可预测变化。