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遗迹化石三维重建研究新进展

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遗迹化石的鉴定与分类是遗迹学研究的基础,而形态特征则是鉴定遗迹化石的关键.表生遗迹和底生遗迹在岩层面上就可以清楚了解其形态;但内生遗迹往往很难直接观察到其三维空间展布形态,从而给鉴定及后续研究带来了困难.因此,内生遗迹化石的三维形态研究历来是遗迹学研究的难点.以往的研究一般通过样品的连续切片获取内生遗迹的形态信息,完成对内生遗迹的三维重建.随着科技的日新月异,各种新方法陆续被应用到遗迹化石的研究中,使内生遗迹化石三维形态的高精度重建成为可能.X射线成像技术可以识别内生遗迹与围岩岩性的差异,其与连续切片相结合,可以更精确的重建内生遗迹的三维形态.核磁共振成像技术在遗迹化石研究中的应用,首次实现了内生遗迹化石三维空间形态的无损成像.笔者首次尝试利用X射线断层成像技术对内生遗迹化石进行了三维重建,也取得了良好的效果.另外,同步辐射X射线相衬显微断层成像技术近年来已成为实体化石无损三维显微成像研究的最佳方法,但还未应用于研究遗迹化石,该技术可望成为内生遗迹化石三维可视化研究的重要方法.
NEW ADVANCES IN THE THREE-DEMENSIONAL RECONSTRUCTION OF TRACE FOSSILS
Reliable identification and classification of trace fossils are essential to ichnological research,and the morphology of trace fossil is the key to taxonomic identification.Epichnia and hypichnia can be clearly observed on the bedding surface.However,the three-dimensional characterization of endichnia is difficult,and represents a major obstacle in ichnological research.In previous studies,three-dimensional reconstruction of trace fossils was generally based on the information obtained by serial grinding.However,with the development of new technologies,various methods have been used in ichnological research.X-ray imaging in combination with serial grinding can be used to visualize endichnia that are distinct from their host rocks in lithology and density,thus allowing their three-dimensional reconstruction.Magnetic resonance imaging is another method that can be used in the three-dimensional reconstruction of endichnia.In this paper,the authors report promising results from the application of X ray computed tomography in the three-dimensional morphological characterization of trace fossils.Phase contrast-based synchrotron X-ray microtomography is considered as the most optimal method in the three-dimensional characterization of body fossils,but it has not been used in the study of trace fossils yet;this technology has promise to be a powerful tool in the three-dimensional visualization of trace fossils in the future.

trace fossilthree-demensional reconstructionserial grinding sectionsX-raymagnetic resonance imagingx-ray computed tomography

丁奕、时敏敏、刘祎楠

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中国科学院南京地质古生物研究所 江苏南京210008

中国科学院大学 北京 100049

大庆油田有限责任公司第九采油厂 黑龙江大庆163853

西北大学地质学系 陕西西安 710069

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遗迹化石 三维重建 核磁共振成像 X射线成像 X射线断层成像

国家科技部973项目国家基金委重大项目

2011CB80890541290260

2016

地层学杂志
全国地层委员会 中国科学院南京地质古生物研究所

地层学杂志

CSTPCDCSCD北大核心
影响因子:0.824
ISSN:0253-4959
年,卷(期):2016.40(4)
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