首页> 外文期刊>Palaios: An International Journal of the Society of Economic Paleontologists & Mineralogists >Modern Nautilus (cephalopoda) taphonomy in a subtidal to backshore environment, Lifou (Loyalty Islands)
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Modern Nautilus (cephalopoda) taphonomy in a subtidal to backshore environment, Lifou (Loyalty Islands)

机译:Lifou(忠诚岛)在近潮水到近海环境中的现代鹦鹉螺(头足类)拓朴技术

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Thirty-two samples of submerged Nautilus macromphalus shells were recovered in 2008 from Lifou, Loyalty Islands in the South Pacific Ocean. Specimens were collected from carbonate-dominated sediment in water depths of 1-3 m. Some specimens were partly buried, whereas others rested on the seafloor. The majority of the specimens (66%) were recovered in a horizontal position, whereas 34% of the specimens were oriented vertically. Some specimens were pristine, with sharp color stripes and little encrustation by algae, cyanobacteria, or epizoans. The majority of specimens have substantial algal and cyanobacterial overcoats with some epizoans. In some specimens, the overcoats also trapped substantial amounts of carbonate sediment. Comparison of the 2008 collection of subtidal specimens to 43 beached Nautilus shells collected in 2002 from the same location reveals that the nearshore taphonomic pathways for drift cephalopod shells can be more complicated than published theoretical models suggest. Nautilus shells may or may not float directly to the beach. Shells not immediately deposited on the beach sink in the shallow water in a vertical position. Weight added by attached organisms and water infiltration, causes the submerged shells to eventually assume a horizontal position. Waves, currents, and bioturbation can then flip the shells over from side to side. Eventually submerged shells are buried, broken apart, or transported onto the beach. Beached shells that follow this taphonomic pathway have conspicuous algal coatings compared to those that simply float to shore. The Lifou subtidal population represents the first substantial modern externally shelled cephalopod collection from a shallow water environment to be analyzed to determine its taphonomic pathways. Conclusions from this analysis can be applied to nearshore deposits that contain externally shelled, fossilized cephalopods.
机译:2008年,从南太平洋忠诚岛利富(Lifou)回收了32只淹没的鹦鹉螺贝壳样本。从水深为1-3 m的碳酸盐为主的沉积物中收集标本。一些标本被部分掩埋,而其他标本则搁在海底。大部分标本(66%)是水平放置的,而34%的标本是垂直放置的。一些标本是原始的,带有清晰的彩色条纹,几乎没有藻类,蓝细菌或附生动物的结壳。大多数标本具有大量的藻类和蓝细菌外层,并带有一些附生动物。在某些标本中,外涂层还捕获了大量碳酸盐沉积物。将2008年潮间标本与2002年从同一地点采集的43滩鹦鹉螺贝壳进行比较,发现漂移头足类贝壳的近岸自相干途径可能比已发表的理论模型所提示的更为复杂。鹦鹉螺的贝壳可能会漂浮也可能不会直接漂浮在海滩上。没有立即沉积在沙滩上的贝壳在垂直位置沉入浅水中。附着生物和水的渗透增加了重量,使被淹没的贝壳最终处于水平位置。然后,波浪,水流和生物扰动会使壳从一侧翻转到另一侧。最终,被淹没的贝壳被掩埋,破碎或运输到海滩上。与仅漂浮到岸上的那些相比,遵循这种垂体途径的滩涂壳具有明显的藻类涂层。 Lifou潮下种群代表了来自浅水环境的第一个重要的现代带壳头足纲动物,需要对其进行分析以确定其汗道途径。该分析得出的结论可应用于含有外壳化石化头足类动物的近岸沉积物。

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