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Application of computer-aided tomography to visualize and quantify biogenic structures in marine sediments

机译:计算机辅助层析成像技术在可视化和定量化海洋沉积物中生物成因结构中的应用

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ABSTRACT: We used computer-aided tomography (CT) for 3D visualization and 2D analysis of marine sediment cores from 3 stations (at 10, 75 and 118 m depths) with different environmental impact. Biogenic structures such as tubes and burrows were quantified and compared among stations. Subsequent to CT scanning, the animals and other material in the cores were collected to validate the image analysis. The shallowest (10 m) station was the most anthropogenically impacted, having horizontally stratified sediment with few biogenic structures close to the sediment surface but many shells and relic tubes (i.e. tubes with no connection to the sediment–water interface) deeper in the sediment. The sediment at the reference station (75 m) and the deepest station (118 m, previously impacted by hypoxia) had large numbers of polychaete tubes throughout the sediment down to at least 30 cm, although many of the tubes deeper down in the sediment were considered relic tubes. Inhabited tubes had a similar density to shells and seem to persist in the sediment for many years. Water volume of inhabited tubes was largest close to the sediment–water interface, whereas water volume in relic tubes was greater between depths of about 3 cm to 30 cm. Many bivalves, particularly Thyasira equalis, were distributed in the middle and deep part of the sediment at the 75 and 118 m stations. Water volume of inhabited tubes was greatest at the 118 m station, showing that benthic fauna recovering from previous hypoxic events can establish burrows and tubes with greater volumes, and probably with greater impact on biogeochemical processes, than at a reference station with more stable environmental conditions. This investigation demonstrated that utilization of CT scanning and software can be applied to visualize and quantify physical and biological structures within sediment thicknesses of several decimetres.
机译:摘要:我们使用计算机辅助断层扫描(CT)对来自3个站点(深度分别为10、75和118 m)的海洋沉积物芯进行3D可视化和2D分析,并对环境造成不同的影响。定量并比较了站间的生物结构,例如管和洞穴。在进行CT扫描之后,收集了核心中的动物和其他材料以验证图像分析。最浅的站(10 m)是人为影响最大的站,其水平分层沉积物几乎没有生物结构靠近沉积物表面,但在沉积物中更深处有许多壳和遗物管(即与沉积物-水界面没有联系的管)。参考站(75 m)和最深站(118 m,先前受缺氧影响)的沉积物在整个沉积物中至少有30 cm处具有大量的多毛管,尽管许多在沉积物中更深的管是被认为是遗物管。有人居住的试管的密度与贝壳相似,并且似乎可以在沉积物中持续多年。靠近沉积物-水界面的有人管的水量最大,而在约3 cm至30 cm的深度之间,文物管中的水量更大。在75和118 m台站的沉积物的中部和深部,分布着许多双壳类动物,特别是 Thyasira equalis 。在118 m站,有人居住的试管的水量最大,这表明与先前环境条件更稳定的参考站相比,从先前的低氧事件中恢复的底栖动物可以建立更大的洞穴和试管,并且可能对生物地球化学过程产生更大的影响。 。这项研究表明,利用CT扫描和软件可以将沉积物厚度在几分之一米之内的物理和生物结构可视化和量化。

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