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在德国盖斯勒塔尔发现的 4500 万年前的猴毛树(Coumoxylon hartigii)中鉴定出了树皮的标志性成分——软木脂。

Suberin, the hallmark constituent of bark, identified in a 45-million-year-old monkeyhair tree (Coumoxylon hartigii) from Geiseltal, Germany.

机构信息

Department of Pharmaceutical and Medicinal Chemistry, PharmaCenter Bonn, Pharmaceutical Institute, University of Bonn, An der Immenburg 4, 53121, Bonn, Germany.

Division of Paleontology, Institute of Geosciences, University of Bonn, Nussallee 8, 53115, Bonn, Germany.

出版信息

Sci Rep. 2024 Jan 2;14(1):118. doi: 10.1038/s41598-023-50402-y.

Abstract

Suberin, a complex biopolymer, forms a water- and gas-insoluble barrier that protects the inner tissues of plants. It is abundant in tree bark, particularly in the cork oak Quercus suber. Anatomically, fossil bark has been described since the Devonian. However, its distinctive constituent suberin has not yet been reported from the fossil record. Here we present unambiguous chemical evidence for intact suberin from the bark of a middle Eocene monkeyhair tree from Geiseltal, eastern Germany. High-performance liquid chromatography coupled to electrospray ionization mass spectrometry (HPLC-ESI-MS) detected constituents of suberin in the outer layer the fossil monkeyhair tree, which confirms previous morphological interpretation of this tissue as bark, and chemically differentiates this layer from the two tissues of the inner layer. Notably, this is the first study with compelling chemical evidence for suberin in fossil bark. Fluorescence microspectroscopy additionally supports the presence of suberin. Fossilization conditions in the Eocene Geiseltal deposit were likely mild, with low moisture and temperatures, contributing to the remarkable preservation of bark and inner laticifer mats of the monkeyhair trees growing there 45 million years ago.

摘要

化感物质是一种复杂的生物聚合物,形成了一种水和气体不可渗透的屏障,保护植物的内部组织。它在树皮中含量丰富,特别是在栓皮栎 Quercus suber 中。在解剖学上,自泥盆纪以来就已经描述了化石树皮。然而,其独特的组成部分化感物质尚未在化石记录中报道过。在这里,我们从德国东部盖塞特尔的中始新世猴毛树的树皮中提供了明确的化感物质完整化学证据。高效液相色谱-电喷雾电离质谱联用(HPLC-ESI-MS)检测到化石猴毛树外层化感物质的组成成分,这证实了该组织先前作为树皮的形态学解释,并从内层的两种组织化学上区分了这一层。值得注意的是,这是首次在化石树皮中具有令人信服的化学证据的化感物质研究。荧光微光谱学也支持化感物质的存在。4500 万年前,在始新世的盖塞特尔矿床中,化石形成条件可能很温和,湿度和温度较低,这有助于显著保存那里生长的猴毛树的树皮和内部乳汁管垫。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/d26a/10761729/89640bfc7e09/41598_2023_50402_Fig1_HTML.jpg

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