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在石英骨架晶体中发现的油包裹体表明古代生长环境周围存在有机物。

Oil Inclusions Found in Skeleton Crystals of Quartz Indicated the Existence of Organic Matter Surrounding Ancient Growth Environments.

作者信息

Sugiura Yuki, Tobita Naoko, Tobita Takashi, Taga Masaru, Nakachi Shu, Yokota Kazumichi, Yamada Etsuko, Horie Masanori, Momma Koichi, Matsubara Satoshi

机构信息

Health and Medical Research Institute, National Institute of Advanced Industrial Science and Technology (AIST), 2217-14, Hayashi-cho, Takamatsu 761-3095, Kagawa, Japan.

Research Planning Office, Headquarters of Department of Life Science and Biotechnology, National Institute of Advanced Industrial Science and Technology (AIST), 1-1-1, Umezono, Tsukuba 305-0035, Ibaraki, Japan.

出版信息

ACS Omega. 2023 Jun 5;8(24):21464-21473. doi: 10.1021/acsomega.3c00272. eCollection 2023 Jun 20.

DOI:10.1021/acsomega.3c00272
PMID:37360484
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC10286290/
Abstract

In nature, minerals record various origins and information for geology and geobiochemistry. Here, we investigated the origin of organic matter and growth mechanism of quartz with oil inclusion revealing fluorescence under short ultraviolet (UV) light, obtained from the clay vein at Shimanto-cho, Kochi, Shikoku Island, Japan. Geological investigation indicated that the oil-quartz was formed in hydrothermal metamorphic veins found in the late Cretaceous interbedded sandstone and mudstone. The obtained oil-quartz crystals are mostly double-terminated. Micro-X-ray computed tomography (microCT) indicated that oil-quartz crystals have various veins originating as skeleton structures along the quartz crystal {111} and {1-11} faces. Spectroscopic and chromatographic studies indicated that aromatic ester and tetraterpene (lycopene) molecules, which revealed fluorescence, were detected. Large molecular weight sterol molecules, such as C40, were also detected in the vein of oil-quartz. This investigation indicated that organic inclusions in mineral crystals would form with ancient microorganism culture environments.

摘要

在自然界中，矿物记录着地质和地球生物化学的各种起源及信息。在此，我们研究了来自日本四国岛高知县四万十町黏土脉中、在短紫外线（UV）下呈现荧光的含油包裹体石英的有机质起源及生长机制。地质调查表明，油石英形成于白垩纪晚期互层砂岩和泥岩中发现的热液变质脉。所获得的油石英晶体大多为两端晶形。微X射线计算机断层扫描（microCT）表明，油石英晶体有沿石英晶体{111}和{1-11}面作为骨架结构起源的各种矿脉。光谱和色谱研究表明，检测到了呈现荧光的芳香酯和四萜（番茄红素）分子。在油石英矿脉中还检测到了大分子量的甾醇分子，如C40。这项研究表明，矿物晶体中的有机包裹体是在古代微生物培养环境中形成的。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/d58d/10286290/6220c8cabcf7/ao3c00272_0014.jpg
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