School of Biological, Earth and Environmental Science, Environmental Research Institute, University College Cork, Cork, Ireland.
Irish Centre for Research in Applied Geosciences, Marine and Renewable Energy Institute, University College Cork, Cork, Ireland.
Sci Rep. 2020 Nov 10;10(1):19433. doi: 10.1038/s41598-020-76446-y.
Strong currents are a key component of benthic habitats by supplying food and nutrients to filter-feeding organisms such as cold-water corals. Although field measurements show that cold-water coral habitats exist in areas of elevated bottom currents, flume studies show that cold-water corals feed more effectively at lower flow speeds. This research aims to explore this disconnect in situ by utilising high spatial resolution ROV photogrammetric data coupled with high temporal resolution in situ acoustic doppler current profile measurements at seven study sites within the upper Porcupine Bank Canyon (uPBC), NE Atlantic. Object-based image analysis of photogrammetric data show that coral habitats vary considerably within the upper canyon. Although there is a regional hydrodynamic trend across the uPBC, this variation is likely driven locally by topographic steering. Although live coral tends not to face directly into the prevailing current direction, preferring lower local flows speeds, they can tolerate exposure to high-flow speeds of up to 114 cm s, the highest recorded in a Desmophyllum pertusum habitat. Not only do these high flow speeds supply food and nutrients, they may also help contribute to coral rubble production through physical erosion. These results can be incorporated into simulations of future deep-water habitat response to changing environmental conditions while extending the upper current speed threshold for cold-water corals.
强流是底栖生境的一个关键组成部分,为滤食性生物如冷水珊瑚提供食物和营养。尽管实地测量表明冷水珊瑚生境存在于底流升高的区域,但水槽研究表明冷水珊瑚在较低的流速下更有效地进食。本研究旨在通过利用高空间分辨率 ROV 摄影测量数据和高时间分辨率原位声学多普勒流速剖面测量,在东北大西洋上波丘派恩银行峡谷(uPBC)的七个研究点原位探索这种不匹配。摄影测量数据的基于对象的图像分析表明,珊瑚生境在上峡谷内有很大差异。尽管整个 uPBC 存在区域水动力趋势,但这种变化很可能是由地形引导造成的局部变化。尽管活珊瑚往往不直接面对主流方向,而是倾向于较低的局部流速,但它们可以耐受高达 114 厘米/秒的高速流,这是在 Desmophyllum pertusum 生境中记录到的最高流速。这些高速流不仅提供了食物和营养,还可能通过物理侵蚀帮助促进珊瑚碎石的产生。这些结果可以纳入对未来深海生境对环境变化的模拟中,同时扩展冷水珊瑚的上流速阈值。