Department of Biology, University of Bergen, Bergen, Norway.
University Centre in Svalbard, Longyearbyen, Norway.
Glob Chang Biol. 2017 Dec;23(12):5318-5330. doi: 10.1111/gcb.13797. Epub 2017 Jul 31.
Light is a central driver of biological processes and systems. Receding sea ice changes the lightscape of high-latitude oceans and more light will penetrate into the sea. This affects bottom-up control through primary productivity and top-down control through vision-based foraging. We model effects of sea-ice shading on visual search to develop a mechanistic understanding of how climate-driven sea-ice retreat affects predator-prey interactions. We adapt a prey encounter model for ice-covered waters, where prey-detection performance of planktivorous fish depends on the light cycle. We use hindcast sea-ice concentrations (past 35 years) and compare with a future no-ice scenario to project visual range along two south-north transects with different sea-ice distributions and seasonality, one through the Bering Sea and one through the Barents Sea. The transect approach captures the transition from sub-Arctic to Arctic ecosystems and allows for comparison of latitudinal differences between longitudes. We find that past sea-ice retreat has increased visual search at a rate of 2.7% to 4.2% per decade from the long-term mean; and for high latitudes, we predict a 16-fold increase in clearance rate. Top-down control is therefore predicted to intensify. Ecological and evolutionary consequences for polar marine communities and energy flows would follow, possibly also as tipping points and regime shifts. We expect species distributions to track the receding ice-edge, and in particular expect species with large migratory capacity to make foraging forays into high-latitude oceans. However, the extreme seasonality in photoperiod of high-latitude oceans may counteract such shifts and rather act as a zoogeographical filter limiting poleward range expansion. The provided mechanistic insights are relevant for pelagic ecosystems globally, including lakes where shifted distributions are seldom possible but where predator-prey consequences would be much related. As part of the discussion on photoperiodic implications for high-latitude range shifts, we provide a short review of studies linking physical drivers to latitudinal extent.
光是生物过程和系统的核心驱动因素。海冰消退改变了高纬度海洋的光照景观,更多的光将穿透海水。这会通过初级生产力对底层控制产生影响,并通过基于视觉的觅食对顶层控制产生影响。我们模拟了海冰遮荫对视觉搜索的影响,以深入了解气候驱动的海冰消退如何影响捕食者-猎物相互作用。我们对适用于冰盖水域的猎物遭遇模型进行了改编,在这种模型中,浮游鱼类的猎物探测性能取决于光周期。我们使用过去 35 年的海冰浓度回溯数据,并与未来无冰情景进行比较,以预测两条南北向横截线上的视觉范围,这两条横截线的海冰分布和季节性不同,一条穿过白令海,一条穿过巴伦支海。横截线方法捕捉到了从亚北极生态系统向北极生态系统的过渡,并允许比较不同经度之间的纬度差异。我们发现,过去海冰的消退使得视觉搜索的速度每十年增加 2.7%至 4.2%,高于长期平均值;对于高纬度地区,我们预测清除率将增加 16 倍。因此,顶层控制预计会加剧。这将对极地海洋生物群落和能量流动产生生态和进化影响,可能也会产生临界点和制度转变。我们预计物种分布将跟踪退缩的冰缘,特别是具有较大迁徙能力的物种将进入高纬度海洋进行觅食。然而,高纬度海洋光周期的极端季节性可能会抵消这种转变,而更像是一个地理过滤因素,限制了极地范围的扩展。所提供的机制性见解与全球浮游生态系统有关,包括那些分布变化很少可能但捕食者-猎物影响将非常相关的湖泊。作为对高纬度范围转移的光周期影响的讨论的一部分,我们提供了一个简短的综述,将物理驱动因素与纬度范围联系起来。