Soft body reconstruction of a reptile fossil by the nondestructive elemental mapping with a newly designed XRF

IF 1 4区 地球科学 Q4 GEOSCIENCES, MULTIDISCIPLINARY Island Arc Pub Date : 2023-08-16 DOI:10.1111/iar.12495
Wei Wang, Ling Shu, Deqi Wang
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Abstract

Vertebrate fossils usually consist only of mineralized skeletons and rarely preserve soft body parts. However, the buried soft body releases the degraded material into the surrounding sediments. The degraded material can be preserved as invisible signals of some chemicals or authigenic minerals, which can be revealed by the elemental distribution of the fossils' surface and their surrounding rock. As a method for surface elemental mapping, X-ray fluorescence (XRF) measurement requires the samples to be ground and polished as a mirror-like plane that keeps a stable distance of X-ray source-sample-detector. This destructive pretreatment is undesirable for precious fossils. To rectify this problem, a nondestructive XRF for element mapping of the fossils' 3D surface is newly invented. The new equipment can follow the 3D shape model to keep the distance for every XRF scanned point. We performed the element mapping of Ca and Fe on the surface of a marine sauropterygian fossil (Keichousaurus hui) and its surrounding sediments, and found that the soft tissue around the thoracic cage is thicker than the abdomen. The abnormal elemental distribution on the area of the angular and surangular of the skull can be explained as unprofessionally prepared. In addition, this research found that elemental mapping revealed the invisible signals of the paleoenvironment around fossils and information for the reconstruction of soft-tissue anatomy. We also give an example that based on the wide application of the “Internet of Things” and “Industrial Network,” the design and development of specialized equipment for paleontologists' requirements are going simple.

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用新设计的XRF进行非破坏性元素映射的爬行动物化石软体重建
脊椎动物化石通常只由矿化的骨骼组成,很少保存柔软的身体部分。然而,被埋的软体将降解物质释放到周围的沉积物中。降解物质可以作为一些化学物质或自生矿物的不可见信号保存下来,这些化学物质或自生矿物可以通过化石表面及其周围岩石的元素分布来揭示。作为表面元素映射的一种方法,X射线荧光(XRF)测量需要将样品研磨和抛光为镜面状平面,以保持X射线源-样品-探测器之间的稳定距离。这种破坏性的预处理对于珍贵的化石是不可取的。为了解决这个问题,新发明了一种用于化石三维表面元素映射的无损XRF。新设备可以按照三维形状模型来保持每个XRF扫描点的距离。我们对一具海生龙化石(Keichousaurus hui)及其周围沉积物表面进行了钙、铁元素作图,发现其胸廓周围的软组织比腹部厚。颅骨角、角区元素分布异常可解释为非专业制作。此外,本研究还发现元素映射揭示了化石周围古环境的隐形信号和软组织解剖重建的信息。我们还举了一个例子,基于“物联网”和“工业网络”的广泛应用,满足古生物学家需求的专用设备的设计和开发正在变得简单。
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来源期刊
Island Arc
Island Arc 地学-地球科学综合
CiteScore
2.90
自引率
26.70%
发文量
32
审稿时长
>12 weeks
期刊介绍: Island Arc is the official journal of the Geological Society of Japan. This journal focuses on the structure, dynamics and evolution of convergent plate boundaries, including trenches, volcanic arcs, subducting plates, and both accretionary and collisional orogens in modern and ancient settings. The Journal also opens to other key geological processes and features of broad interest such as oceanic basins, mid-ocean ridges, hot spots, continental cratons, and their surfaces and roots. Papers that discuss the interaction between solid earth, atmosphere, and bodies of water are also welcome. Articles of immediate importance to other researchers, either by virtue of their new data, results or ideas are given priority publication. Island Arc publishes peer-reviewed articles and reviews. Original scientific articles, of a maximum length of 15 printed pages, are published promptly with a standard publication time from submission of 3 months. All articles are peer reviewed by at least two research experts in the field of the submitted paper.
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