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The fate of the Arctic seaweed Fucus distichus under climate change: an ecological niche modeling approach

机译:气候变化下北极海藻岩藻的命运:一种生态位建模方法

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Abstract 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.
机译:摘要预计到本世纪末,气温上升将融化北极所有常年的冰盖,从而为温带和亚北极物种开放合适的栖息地。形成冠层的海藻提供了理想的系统,可以预测气候变化对石质海岸生态系统的潜在影响,因为它们直接依赖于温度及其在生态系统中的关键作用。我们的主要目的是预测气候变化引起的褐藻岩藻(Fusus distichus)的变迁,岩藻岩藻是北极和北极弧下潮间带的主要树冠形成大型藻类。更具体地讲,我们问:北半球的哪些北极/南北极和温带海岸将显示F的最大分布变化。迪氏菌,这将如何影响利基与温带地区的海藻重叠?我们使用MAXENT程序开发了具有主要范围限制因素和169个发生记录的相关生态位模型。使用三种气候变化情景,我们预测了F的栖息地适宜性。 distichus?¢ ????及其生态位与三个优势温带大型藻类重叠直到2200年。最高海面温度被认为是限制F的基本生态位的最重要因素。 tic预计气温上升对该物种的南部分布范围影响较小,但将其北部分布范围向北极极移。在温带至弧下地区,预计F之间会出现新的利基重叠区域。迪氏hu和潮间带大型藻类从南方迁徙。气候变化虽然威胁着温带地区的潮间带海藻,但海带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,但它也将引发北极潮间带生态系统结构和功能的不可预测的变化。

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