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From the CoverPNAS Plus: Reconciling fisheries catch and ocean productivity

机译:来自CoverPNAS Plus:兼顾渔业产量和海洋生产力

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摘要

Photosynthesis fuels marine food webs, yet differences in fish catch across globally distributed marine ecosystems far exceed differences in net primary production (NPP). We consider the hypothesis that ecosystem-level variations in pelagic and benthic energy flows from phytoplankton to fish, trophic transfer efficiencies, and fishing effort can quantitatively reconcile this contrast in an energetically consistent manner. To test this hypothesis, we enlist global fish catch data that include previously neglected contributions from small-scale fisheries, a synthesis of global fishing effort, and plankton food web energy flux estimates from a prototype high-resolution global earth system model (ESM). After removing a small number of lightly fished ecosystems, stark interregional differences in fish catch per unit area can be explained (r = 0.79) with an energy-based model that (i) considers dynamic interregional differences in benthic and pelagic energy pathways connecting phytoplankton and fish, (ii) depresses trophic transfer efficiencies in the tropics and, less critically, (iii) associates elevated trophic transfer efficiencies with benthic-predominant systems. Model catch estimates are generally within a factor of 2 of values spanning two orders of magnitude. Climate change projections show that the same macroecological patterns explaining dramatic regional catch differences in the contemporary ocean amplify catch trends, producing changes that may exceed 50% in some regions by the end of the 21st century under high-emissions scenarios. Models failing to resolve these trophodynamic patterns may significantly underestimate regional fisheries catch trends and hinder adaptation to climate change.
机译:光合作用为海洋食物网提供了燃料,但是全球分布的海洋生态系统中渔获量的差异远远超过净初级生产(NPP)的差异。我们认为以下假设:浮游植物向鱼类的浮游和底栖能量的生态系统水平变化,营养传递效率和捕捞努力可以以能量一致的方式从数量上协调这种对比。为了验证这一假设,我们采用了全球鱼类捕捞数据,其中包括以前被忽略的小规模渔业贡献,全球捕捞努力的综合结果以及来自高分辨率全球地球系统模型(ESM)的浮游生物食物网能量通量估计值。在去除了少量的轻度捕捞的生态系统之后,可以使用基于能量的模型来解释单位面积捕捞量的明显区域间差异(r = 0.79)(i)考虑连接浮游植物和底栖生物的底栖和中上层能量途径的动态区域间差异。鱼类;(ii)降低了热带地区的营养传递效率;(iii)不太重要的是,(iii)将较高的营养传递效率与底栖生物为主的系统联系在一起。模型渔获量估计值通常在跨越两个数量级的值的2倍之内。气候变化预测表明,用相同的宏观生态学模式解释了当代海洋中巨大的区域捕捞差异,加剧了捕捞趋势,到21世纪末,在高排放情景下,某些地区的变化可能超过50%。无法解决这些对流动力学模式的模型可能会大大低估了区域渔业的捕捞趋势,并阻碍了对气候变化的适应。

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