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Bioregionalization of the George V Shelf, East Antarctica

机译:南极洲东部乔治五世大学图书馆的生物区划

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The East Antarctic continental shelf has had very few studies examining the macrobenthos structure or relating biological communities to the abiotic environment. In this study, we apply a hierarchical method of benthic habitat mapping to Geomorphic Unit and Biotope levels at the local (10s of kilometers) scale across the George V Shelf between longitudes 142 degrees E and 146 degrees E. We conducted a multi-disciplinary analysis of seismic profiles, multibeam sonar, oceanographic data and the results of sediment sampling to define geomorphology, surficial sediment and near-seabed water mass boundaries. Geographic information system models of these oceanographic and geophysical features increase the detail of previously known seabed maps and provide new maps of seafloor characteristics. Kriging surface modeling on data includes maps to assess uncertainty within the predicted models. A study of underwater photographs and the results of limited biological sampling provide information to infer the dominant trophic structure of benthic communities within geomorphic features. The study reveals that below the effects of iceberg scour (depths > 500 m) in the basin, broad-scale distribution of macrofauna is largely determined by substrate type, specifically mud content. In waters within the direct influence of glacial ice (depths < 500 m) on the banks, scouring by icebergs is a strong limiting factor in the distribution of macrobenthos. In areas protected from iceberg scour disturbance, such as on the outer shelf banks and slope, the direction and speed of oceanic currents are the likely dominant abiotic factor in the broad-scale distribution of macrofauna. This hierarchical method of benthic habitat mapping could be applied circum-Antarctic for comparison against other geographic areas, and would assist authorities responsible for developing ecosystem-based plans by identifying the different types of marine habitats and their associated biological communities at varying scales on the Antarctic shelf. (c) 2005 Elsevier Ltd. All rights reserved.
机译:南极东部大陆架很少研究大型底栖动物的结构或将生物群落与非生物环境联系起来。在这项研究中,我们对东经142度和146度之间的乔治五世陆架的局部(10公里)尺度上的地貌单元和生物群落水平应用了底栖生境制图的分层方法。我们进行了多学科分析地震剖面,多波束声纳,海洋学数据以及沉积物采样结果,以定义地貌,表层沉积物和近海水域边界。这些海洋和地球物理特征的地理信息系统模型增加了以前已知的海底地图的细节,并提供了新的海底特征地图。数据的Kriging曲面建模包括用于评估预测模型内不确定性的地图。对水下照片的研究和有限的生物采样结果为推断地貌特征内底栖生物群落的优势营养结构提供了信息。研究表明,在流域冰山冲刷(深度> 500 m)的影响下,大型动物的大规模分布在很大程度上取决于基质类型,特别是泥浆含量。在冰川冰直接影响(深度<500 m)对河岸的水域中,冰山冲刷是限制大型底栖动物分布的重要因素。在不受冰山冲刷扰动影响的区域,例如在外架子河岸和斜坡上,洋流的方向和速度是大型动物区系分布中可能的主要非生物因素。可以将这种底栖生境制图的分层方法应用于南极洲,与其他地理区域进行比较,并通过确定南极不同尺度上的不同类型的海洋生境及其相关的生物群落,协助负责制定基于生态系统计划的当局架。 (c)2005 Elsevier Ltd.保留所有权利。

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