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Future climate-driven shifts in distribution of Calanus finmarchicus.

机译:气候导致的 Calaus finmarchicus 分布的变化。

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摘要

Calanus finmarchicus is a key-structural species of the North Atlantic polar biome. The species plays an important trophic role in subpolar and polar ecosystems as a grazer of phytoplankton and as a prey for higher trophic levels such as the larval stages of many fish species. Here, we used a recently developed ecological niche model to assess the ecological niche (sensu Hutchinson) of C. finmarchicus and characterize its spatial distribution. This model explained about 65% of the total variance of the observed spatial distribution inferred from an independent dataset (data of the continuous plankton recorder survey). Comparisons with other types of models (structured population and ecophysiological models) revealed a clear similarity between modeled spatial distributions at the scale of the North Atlantic. Contemporary models coupled with future projections indicated a progressive reduction of the spatial habitat of the species at the southern edge and a more pronounced one in the Georges Bank, the Scotian Shelf and the North Sea and a potential increase in abundance at the northern edge of its spatial distribution, especially in the Barents Sea. These major changes will probably lead to a major alteration of the trophodynamics of North Atlantic ecosystems affecting the trophodynamics and the biological carbon pump.
机译:Calaus finmarchicus 是北大西洋极地生物群系的关键结构物种。该物种在亚极和极地生态系统中起着重要的营养作用,成为浮游植物的放牧者,并作为较高营养水平(例如许多鱼类的幼体阶段)的猎物。在这里,我们使用了最近开发的生态位模型来评估 C的生态位( sensu Hutchinson)。 finmarchicus 并描述其空间分布。该模型解释了从独立数据集(连续浮游生物记录仪调查的数据)推断出的观测空间分布的总方差的65%。与其他类型的模型(结构化人口模型和生态生理模型)的比较表明,在北大西洋范围内,模型化的空间分布之间存在明显的相似性。当代模型加上未来的预测表明,该物种在南部边缘的空间栖息地在逐渐减少,在乔治银行,斯科蒂货架和北海的物种的栖息地更为明显,其北部边缘的丰度可能会增加。空间分布,尤其是在巴伦支海。这些重大变化可能会导致北大西洋生态系统的营养动力学发生重大变化,从而影响营养动力学和生物碳泵。

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