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Preliminary elemental analysis of fossil insects from the Middle Jurassic of Daohugou, Inner Mongolia and its taphonomic implications

机译:内蒙古道虎沟中侏罗统化石昆虫的初步元素分析及其对胶结学的启示

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摘要

Fossil insects from the Middle Jurassic of Daohugou, Inner Mongolia were investigated using Scanning Electron Microscope (SEM) for the first time, and portions and distribution of some elements in compression and pyrited fossils were also revealed by X-ray Energy Dispersive Spectroscopy (EDS) attached to SEM. Most of compression fossil insects from the Daohugou Biota are preserved in organic remains (diagenetic products of the original organic components). A small part of compression fossils retain a comparatively high Fe concentration which probably resulted from the absorption of Fe by biopolymers during the decaying period. Pyritized insect fossils suggest that the "fossil envelop" model found in the Early Cretaceous Jehol Biota probably also occurs in the Daohugou Biota. Different preservation modes show various mechanisms of fossilization, and also suggest that several different microenvironments are present in Daohugou palaeolakes.
机译:首次使用扫描电子显微镜(SEM)研究了内蒙古道虎沟中侏罗世的化石昆虫,并通过X射线能量色散光谱法(EDS)揭示了压缩和黄化化石中某些元素的成分和分布。附加到SEM。稻湖沟生物群的大部分压缩化石昆虫都保存在有机残余物中(原始有机成分的成岩产物)。一小部分受压的化石保留了较高的铁浓度,这可能是由于生物聚合物在衰落期间吸收了铁所致。黄化昆虫化石表明,早白垩世热河生物群中发现的“化石包裹”模型也可能出现在稻湖沟生物群中。不同的保存方式显示出多种化石机制,也表明稻湖沟古湖存在几种不同的微环境。

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