首页> 外文期刊>Journal of marine systems: journal of the European Association of Marine Sciences and Techniques >Seafloor characterization and benthic megafaunal distribution of an active submarine canyon and surrounding sectors: The case of Gioia Canyon (Southern Tyrrhenian Sea)
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Seafloor characterization and benthic megafaunal distribution of an active submarine canyon and surrounding sectors: The case of Gioia Canyon (Southern Tyrrhenian Sea)

机译:活跃的海底峡谷及其周围地区的海底特征和底栖大型动物分布:以Gioia峡谷(南第勒尼安海)为例

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In this paper, we used multibeam bathymetry and backscatter, high-resolution seismic profiles, ROV video images and sediment samples to identify the principal morpho-sedimentary features and related megabenthic communities along the upper reach of the Gioia Canyon (depth < 600 m) and the surrounding shelf and slope areas. Interpretation of the multidisciplinary dataset was undertaken to evaluate the relationships between sea floor characteristics and faunal distribution along a submarine canyon in an active tectonic setting. The results from this study indicate that physical disturbance on the seafloor at the canyon head and surrounding shelf, related to high sedimentation rates and occasional turbidite flows, may limit the variability of megabenthic communities. Evidence of diffuse trawl marks over soft sedimentary bottoms indicates anthropogenic impact due to fishing activities, which could explain low abundances of megabenthic species observed locally. The canyon margins and flanks along the continental slope host octocorals Funiculina quadrangularis and Isidella elongate, species that are indicative of vulnerable marine ecosystems (VMEs) and relevant in terms of sustainable management priorities. At the Palmi Ridge, the occurrence of outcropping rocks and bottom currents related to the presence of Levantine Intermediate Waters, provide conditions for the development of hard-bottom assemblages, including the black coral Antipathella subpinnata and deep-sea sponges fields. (C) 2016 Elsevier B.V. All rights reserved.
机译:在本文中,我们使用了多波束测深和反向散射,高分辨率地震剖面,ROV视频图像和沉积物样本,来识别Gioia峡谷(深度<600 m)和河床上游的主要形态沉积特征和相关的大型底栖动物群落。周围的架子和斜坡区域。进行了多学科数据集的解释,以评估活跃构造环境中海底特征与沿海底峡谷的动物区系分布之间的关系。这项研究的结果表明,与高沉积速率和偶尔的浊流有关的峡谷头和周围大陆架海底物理干扰可能会限制大型底栖动物群落的变异性。在柔软的沉积物底部弥漫的拖网痕迹的迹象表明,由于捕鱼活动而对人为产生影响,这可以解释在当地观察到的巨底栖生物数量少。沿大陆斜坡的峡谷边缘和侧翼是八角形的Funiculina quadrangularis和Isidella拉长的物种,这些物种指示着脆弱的海洋生态系统(VME),并且在可持续管理方面具有重要意义。在帕尔米岭,与黎凡特中间水域的存在有关的露头岩石和底部洋流的出现,为硬底组合的发展提供了条件,包括黑珊瑚安提帕西娜(Antipathella subpinnata)和深海海绵田。 (C)2016 Elsevier B.V.保留所有权利。

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