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Scleractinian Corals of the Arctic and High Latitudes of the North Atlantic Ocean

机译:北极和北大西洋高纬度的巩膜珊瑚珊瑚

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摘要

Only two species of scleractinian corals were found in the high latitudes of the Arctic Ocean west of the Barents Sea: Lophelia pertusa (Linne, 1758) and Flabellum macandrewi Gray, 1849. The first species has a cosmopolitan distribution; the second inhabits the Atlantic Ocean only. An analysis of the hydrodynamic environment in which these species exist has led us to conclude that the species L. pertusa preferring solid sediments is favored by increased water hydrodynamics. Fl. macandrewi, which lives on loose sediments, is also exposed to powerful water flows, which cause instability and the mobility of sandy or finely gravel sediments on the bottom, breaking the fragile skeletons of these corals. However, they adapt to such living conditions due to their extraordinary ability to regenerate. We argue that the presence of coral polyps of this species can be a marker of highly dynamic waters. Scleractinian corals are completely absent in the central parts of the Arctic Ocean, which is explained by the geological history of this region, possibly affected by water desalination, fluctuations in water salinity, and sharp changes in the intensity of phytoplankton development.
机译:在巴伦斯海西部的北极海洋高纬度地区只发现了两种菌膜珊瑚:Lophelia Pertusa(Linne,1758)和Flabellum Macandrewi Gray,1849年。第一个物种具有国际化分布;第二个居住在大西洋。对这些物种存在的流体动力学环境的分析使我们得出结论,物种L. pertusa优选的固体沉积物受到增加的水流体动力学的青睐。佛罗里达州生活在松散的沉积物上的Macandrewi也暴露在强大的水流中,这导致底部砂质或精细砾石沉积物的不稳定和移动性,破坏了这些珊瑚的脆弱骨架。然而,由于他们的特殊能力,他们适应了这种生活条件。我们认为这种物种的珊瑚息肉的存在可以是高度动态水的标记。 Scleractinian珊瑚完全在北极海洋的中央部分缺席,这是由该地区的地质历史来说解释的,可能受水脱盐的影响,水盐度波动,以及浮游植物强度的急剧变化。

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