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Imaging Oxygen Distribution in Marine Sediments. The Importance of Bioturbation and Sediment Heterogeneity

机译:成像海洋沉积物中的氧气分布。生物扰动和沉积物非均质性的重要性

摘要

The influence of sediment oxygen heterogeneity, due to bioturbation, on diffusive oxygen flux was investigated. Laboratory experiments were carried out with 3 macrobenthic species presenting different bioturbation behaviour patterns:the polychaetes Nereis diversicolor and Nereis virens, both constructing ventilated galleries in the sediment column, and the gastropod Cyclope neritea, a burrowing species which does not build any structure. Oxygen two-dimensional distribution in sediments was quantified by means of the optical planar optode technique. Diffusive oxygen fluxes (mean and integrated) and a variability index were calculated on the captured oxygen images. All species increased sediment oxygen heterogeneity compared to the controls without animals. This was particularly noticeable with the polychaetes because of the construction of more or less complex burrows. Integrated diffusive oxygen flux increased with oxygen heterogeneity due to the production of interface available for solute exchanges between overlying water and sediments. This work shows that sediment heterogeneity is an important feature of the control of oxygen exchanges at the sediment–water interface.
机译:研究了由于生物扰动引起的沉积物氧异质性对扩散氧通量的影响。进行了三种具有不同生物扰动行为模式的大型底栖动物的实验室实验:多头杂种Nereis diversicolor和Nereis virens,它们都在沉积物柱中构建通风通道,而腹足纲Cyclope neritea是一种没有任何结构的穴居物种。利用光学平面光电技术对沉积物中的氧二维分布进行了定量。在捕获的氧气图像上计算了扩散氧气通量(均值和积分)和变异性指数。与没有动物的对照组相比,所有物种都增加了沉积物氧异质性。由于构造或多或少复杂的洞穴,这在多羚羊群中尤为明显。由于产生了可用于上覆水和沉积物之间的溶质交换的界面,因此积分扩散氧气通量随着氧气异质性的增加而增加。这项工作表明,沉积物非均质性是控制沉积物-水界面处的氧交换的重要特征。

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