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琥珀中具有内源性几丁质的 4400 万年前叶甲(鞘翅目:叶甲科)的形态和有机光谱研究。

Morphological and organic spectroscopic studies of a 44-million-year-old leaf beetle (Coleoptera: Chrysomelidae) in amber with endogenous remains of chitin.

机构信息

Department of Physics, University of Regina, Regina, SK, S4S 0A2, Canada.

Royal Saskatchewan Museum, 2445 Albert St., Regina, SK, S4P 4W7, Canada.

出版信息

Sci Rep. 2023 Apr 11;13(1):5876. doi: 10.1038/s41598-023-32557-w.

DOI:10.1038/s41598-023-32557-w
PMID:37041264
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC10090159/
Abstract

This study details the quality of preservation of amber deposits in the Eocene. Through Baltic amber crack-out studies using Synchrotron Micro-Computed Tomography and Scanning Electron Microscopy it was found that the cuticle of a specimen of leaf beetle (Crepidodera tertiotertiaria (Alticini: Galerucinae: Chrysomelidae)) is exceptionally well preserved. Spectroscopic analysis using Synchrotron Fourier Transform Infrared Spectroscopy suggests presence of degraded [Formula: see text]-chitin in multiple areas of the cuticle, and Energy Dispersive Spectroscopy supports the presence of organic preservation. This remarkable preservation is likely the result of several factors such as the favourable antimicrobial and physical shielding properties of Baltic amber as compared to other depositional media, coupled to rapid dehydration of the beetle early in its taphonomic process. We provide evidence that crack-out studies of amber inclusions, although inherently destructive of fossils, are an underutilised method for probing exceptional preservation in deep time.

摘要

本研究详细介绍了始新世琥珀矿床的保存质量。通过使用同步辐射微计算机断层扫描和扫描电子显微镜对波罗的海琥珀进行破裂研究,发现叶甲(Crepidodera tertiotertiaria(Alticini:Galerucinae:Chrysomelidae))标本的表皮保存得异常完好。使用同步辐射傅里叶变换红外光谱进行的光谱分析表明,表皮的多个区域存在降解的[Formula: see text]-几丁质,能量色散光谱支持有机保存的存在。这种显著的保存很可能是多种因素共同作用的结果,例如与其他沉积介质相比,波罗的海琥珀具有有利的抗菌和物理屏蔽特性,再加上甲虫在其埋藏过程中早期迅速脱水。我们提供的证据表明,尽管对琥珀内含物的破裂研究本质上具有破坏性,但它是一种利用不足的方法,可以深入探究远古时期的卓越保存。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/7174/10090159/1f9aaf498f8a/41598_2023_32557_Fig4_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/7174/10090159/d63aeaf0a35f/41598_2023_32557_Fig1_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/7174/10090159/5aa7351ad18d/41598_2023_32557_Fig2_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/7174/10090159/6e4b732e00d7/41598_2023_32557_Fig3_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/7174/10090159/1f9aaf498f8a/41598_2023_32557_Fig4_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/7174/10090159/d63aeaf0a35f/41598_2023_32557_Fig1_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/7174/10090159/5aa7351ad18d/41598_2023_32557_Fig2_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/7174/10090159/6e4b732e00d7/41598_2023_32557_Fig3_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/7174/10090159/1f9aaf498f8a/41598_2023_32557_Fig4_HTML.jpg

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