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Microboring in a Freshwater Fluvial Unionid Bivalve Substrate

机译:淡水河床黄藻类双壳类动物基质中的微孔。

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Samples of the unionid bivalve Elliptio complanata were collected from the channel of the freshwater Saint John River, from Fredericton, New Brunswick, Canada. Scanning electron microscopy imaging of prepared shell samples revealed an assemblage of microborings. No borings are noted on the periostracum or prismatic shell layers. Boring structures are instead confined to the underlying nacreous aragonitic shell material, together with its associated organic conchiolin layers. Three main styles of boring are encountered, encompassing both predominantly surficial structures and penetrative tubular borings. Surficial structures are represented by a polygonal network on an exposed conchiolin shell layer. The penetrative borings take two forms, one being simple unbranched tubes, steeply aligned (perpendicular to the shell surface) and traversing the full thickness of the nacreous shell layer. The other penetrative boring style, again occurring within the nacreous layer, comprises a complex irregular network of randomly oriented rarely branching tubular borings. Borings generally display diameters of micron scale. Biofilm and extracellular polymeric substances, with bacterial, diatomaceous and filamentous components are also observed, often displaying a close association with both the borings and the conchiolin layers within the shell. The formation of the borings may be attributed to cyanobacteria, cyanophyte or fungal progenitors.
机译:从加拿大新不伦瑞克省弗雷德里克顿的淡水圣约翰河河道收集了双生双壳类双壳纲Elliptio complanata的样品。制备的壳样品的扫描电子显微镜成像揭示了微孔的集合。在骨膜或棱柱形壳层上未发现钻孔。取而代之的是将钻孔结构及其相关的有机贝壳杉醇层限制在下面的珍珠质贝壳状壳材料中。遇到了三种主要的钻孔样式,包括主要的表面结构和穿透性管状钻孔。表面结构由裸露的贝壳杉壳层上的多边形网络表示。渗透性钻孔有两种形式,一种是简单的无分支管,陡峭地排列(垂直于壳表面),并且遍及整个珍珠质壳层。另一种渗透性钻探样式再次出现在珍珠层内,包括复杂的不规则网络,其随机定向,很少分支的管状钻探。钻孔通常显示微米级的直径。还观察到了具有细菌,硅藻和丝状成分的生物膜和细胞外聚合物,它们通常与壳内的钻探层和贝壳菌素层密切相关。钻孔的形成可能归因于蓝细菌,蓝藻或真菌祖细胞。

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