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首页> 外文期刊>Marine biology research >Recent trends in the abundance of plaice Pleuronectes platessa and cod Gadus morhua in shallow coastal waters of the Northeastern Atlantic continental shelf - a review
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Recent trends in the abundance of plaice Pleuronectes platessa and cod Gadus morhua in shallow coastal waters of the Northeastern Atlantic continental shelf - a review

机译:东北大西洋大陆架浅海沿海水域Pleuronectes platesa和cod Gadus morhua的丰度最新趋势-综述

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Shallow, near-shore water habitats on the continental shelf of the Northeast Atlantic have been productive fishing areas in the past. Here, we review the present knowledge about (i) recent trends in the abundance of plaice and cod in these habitats and (ii) hypotheses regarding the factors responsible for any trends. At present, only a few studies exist on the trends of abundance of plaice or cod, namely from the Bay of Biscay, the North Sea and the Skagerrak/Kattegat. They suggest a declining abundance in coastal, shallow areas and - at least for plaice - a latitudinal gradient with an erosion of the southern distribution boundary in the Bay of Biscay and deepening of stocks in the North Sea. In contrast, no trend in shallow water abundance of plaice similar to a decline in deep-water stocks during the 1970s and their slow recovery during the 2000s is apparent in the Skagerrak/Kattegat. Although shallow habitats fundamentally differ from deeper areas by the prevalence of juvenile stages, the declining trends coincide with decreasing abundance/landings and spatial stock relocations in the deeper areas. Whether this indicates a common trend pointing at connectivity between shallow and deep water remains open. Fundamental differences exist in the suggested causes of the trends in different geographical areas. High fishing pressure together with low local recruitment apparently prevents the recovery of overexploited plaice and cod stocks in the Skagerrak/Kattegat. In contrast, the responses of juveniles and adult fish to increasing seawater temperature are the main hypotheses for changes in distribution and abundance of both fish species in the North Sea/Bay of Biscay. However, temperature alone cannot explain the observed decline of fish in coastal areas, and the causes may be more complex, involving nutrient loading, primary productivity or food availability, although at present, knowledge of these factors is insufficient.
机译:过去,东北大西洋大陆架上的浅水,近岸水生境曾经是高产捕鱼区。在这里,我们回顾了有关(i)这些栖息地中和鳕鱼数量的最新趋势以及(ii)有关导致任何趋势的因素的假设的当前知识。目前,只有很少的关于d或鳕鱼丰富趋势的研究,即来自比斯开湾,北海和Skagerrak / Kattegat的研究。他们认为沿海,浅水区的丰度在下降,并且(至少对于而言)是一种纬度梯度,比斯开湾的南部分布边界受到侵蚀,北海的种群不断加深。相反,在Skagerrak / Kattegat,没有明显的浅水的趋势,类似于1970年代的深水种群减少和2000年代的缓慢复苏。尽管由于幼年阶段的流行,浅层生境与深层生境在根本上是不同的,但下降趋势与深层生境的丰度/着陆量和空间种群的重新安置相吻合。这是否表明有一个共同的趋势指向浅水和深水之间的连通性,仍然是未知数。在不同地理区域趋势的建议起因中存在根本差异。较高的捕捞压力和较低的本地招聘显然可以防止Skagerrak / Kattegat地区过度开发的和鳕鱼种群的恢复。相反,在北海/比斯开湾,这两种鱼类的分布和丰度发生变化的主要假设是幼鱼和成鱼对海水温度升高的反应。然而,仅靠温度不能解释沿海地区鱼类的下降,其原因可能更为复杂,涉及养分含量,初级生产力或食物供应,尽管目前对这些因素的了解还不够。

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