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Recent ichnocoenosis in deep water macroids, Ryukyu Islands, Japan

机译:日本琉球群岛深水巨人鱼最近的鱼鳞病

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摘要

Macroids provide a stable and three-dimensional habitat to which seaweeds, coralline red algae and invertebrates can attach. Some of these organisms act as borers and leave traces which are preservable in the fossil material and are potentially paleoenvironmental indicators in palaeoenvironmental analysis. Although most investigations of ichnocoenoses have focused on shallow-water settings, boring organisms such as sponges, suspension-feeding bivalves, polychaetes and annelid worms may also act in deeper fore-reef settings. We describe for the first time the ichnocoenosis of Entobia, Gastrochaenolites, Trypanites and Maeandropolydora from deep water reef settings. This ichnocoenosis, commonly so far identified only in shallow-marine rockgrounds and hardgrounds and in firm, compacted, but unlithified substrates, occurs in living macroid assemblages ranging in water depth from 61 to 105 m, southwest of Kikai-jima, northern Ryukyu Islands (southern Japan). Importantly, this discovery strengthens the hypothesis that this ichnocoenosis can be utilized as a palaeoenvironmental indicator of low sedimentation rate and high turbulence rather than as a palaeobathymetric proxy.
机译:巨人提供了一个稳定的三维生境,海藻,珊瑚红藻和无脊椎动物可以附着在此。这些生物中的一些起bore虫的作用,并留下痕迹,这些痕迹可在化石材料中保存,并且在古环境分析中可能是古环境的指示剂。尽管鱼鳞病的大多数研究都集中在浅水环境,但是无聊的生物,例如海绵,悬浮饲料的双壳类,多毛类和无脊椎动物,也可能在更深的前礁环境中起作用。我们首次描述了来自深水礁环境的恩托比亚,胃肠蠕虫,锥虫和毛poly多角体的鱼鳞病。这种鱼鳞病通常仅在浅海岩石地和硬地中以及在坚固,压实但未结石的基质中才发现,这种现象发生在琉球北部奇凯岛西南部,水深范围为61至105 m的活体类巨猿组合中(日本南部)。重要的是,这一发现加强了这样的假说:鱼鳞囊菌病可被用作低沉积速率和高湍流的古环境指示物,而不是用作古生物计量学的替代物。

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