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Ballasted Flocs Capture Pelagic Primary Production and Alter the Local Sediment Characteristics in the Coastal German Bight (North Sea)

机译:压载的絮凝物捕获了沿海德国湾(北海)的浮游初级产物并改变了当地的沉积物特征。

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摘要

Suspended, organic matter, especially in the form of adhesive extracellular polymers (EPS), tends to form flocs, which may also incorporate suspended lithogenic particles in coastal environments. With an increased settling velocity, these ballasted flocs form in a narrow zone along the coast and potentially represent a major source of pelagic primary production for the benthic community. We sought support for this hypothesis by examining our measurements of the mud content, porosity, permeability, pigment content, and specific respiration rate of sediment from the German Bight (North Sea) for signs that the pelagic zone of ballasted floc formation is affecting the local sediment characteristics. Based on a simple bottom-shear stress model and by employing empirical correlations of sediment characteristics we were able to find strong indications that this is actually the case. Our results demonstrate how ballasted flocs contribute to the benthic pelagic coupling in a high turbulence environment.
机译:悬浮的有机物,特别是粘附性细胞外聚合物(EPS)的形式,容易形成絮凝物,这些絮凝物也可能在沿海环境中掺入悬浮的致石颗粒。随着沉降速度的提高,这些压载絮状物在沿海狭窄区域形成,并可能代表底栖生物上层初级生产的主要来源。通过检查我们对德国湾(北海)沉积物的泥浆含量,孔隙率,渗透率,颜料含量和比呼吸速率的测量结果,以寻找压载絮凝物形成的中上层带正在影响当地沉积物的迹象,我们寻求这一假设的支持。沉积物特征。基于一个简单的底部剪切应力模型,并利用沉积物特征的经验相关性,我们能够找到有力的迹象,表明确实如此。我们的结果表明,在高湍流环境中,压载絮凝物是如何促进底栖浮游耦合的。

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