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首页> 外文期刊>Frontiers in Marine Science >Potential Structuring Forces on a Shelf Edge Upper Mesophotic Coral Ecosystem in the US Virgin Islands
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Potential Structuring Forces on a Shelf Edge Upper Mesophotic Coral Ecosystem in the US Virgin Islands

机译:在美属维尔京群岛的搁板边缘上中生珊瑚生态系统中的潜在结构力

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Mesophotic coral ecosystems are extensive light-dependent habitats that typically form between 30 – 150 m depth in the tropical oceans. The forces that structure the benthic communities in these ecosystems are poorly understood but this is rapidly changing with technological advances in technical diving and remote observation that allow large-scale scientific investigation. Recent observations of southeastern Puerto Rican Shelf of the US Virgin Islands have shown that this Caribbean mesophotic coral ecosystem has distinct habitats within the same depth ranges and across small horizontal distances (25%. High-resolution bathymetric mapping of the shelf edge revealed a topographically distinct semi-continuous 71 km-long relict barrier reef bank system. The purpose of this study was to characterize the pattern of mesophotic habitat development of the shelf edge and use this data to narrow the potential long-term and large-scale structuring forces of this mesophotic coral ecosystem. We hypothesized from limited preliminary observations that the shelf edge coral cover was limited in shallower portions of the bank and on the seaward orientation. Through stratified random surveys we found that increasing depth and decreasing wave driven benthic orbital velocities were positively related to coral abundance on the shelf edge. In addition, low coral cover habitats of the shelf edge contrasted strongly with adjacent on shelf banks surveyed previously in the same depth range, which had relatively high coral cover (>30%). Predictions of benthic orbital velocities during major storms suggested that mechanical disturbance combined with low rates of coral recovery as a possible mechanism structuring the patterns of coral cover, and these factors could be targets of future research.
机译:中生珊瑚生态系统是广泛的依赖光的栖息地,通常在热带海洋中形成30至150 m的深度。人们很少了解在这些生态系统中构成底栖生物群落的力量,但是随着技术潜水和远程观察技术的进步(允许进行大规模的科学调查),这种力量正在迅速改变。对美属维尔京群岛东南波多黎各架东南部的最新观察表明,这个加勒比海的中生珊瑚生态系统在相同的深度范围内和较小的水平距离内具有独特的栖息地(25%。架子边缘的高分辨率测深图显示了地形上独特的半连续71公里长的遗迹屏障珊瑚礁库系统,本研究的目的是表征大陆架边缘中生境生境的发育模式,并利用这些数据来缩小该区域潜在的长期和大规模构造力中生珊瑚生态系统。我们从有限的初步观察中假设,大陆架边缘的珊瑚覆盖仅限于河岸较浅的部分和向海的方向。通过分层随机调查,我们发现增加的深度和减少的波浪驱动底栖轨道速度与架子边缘的珊瑚丰富,此外,低珊瑚覆盖的栖息地f架子边缘与先前在相同深度范围内进行调查的相邻架子银行形成强烈对比,后者具有相对较高的珊瑚覆盖率(> 30%)。对大风暴期间底栖轨道速度的预测表明,机械扰动加上低的珊瑚恢复率是构造珊瑚覆盖模式的可能机制,这些因素可能成为未来研究的目标。

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