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Molecular identification of fungi microfossils in a Neoproterozoic shale rock

机译:Neoproterozoic Shale岩石真菌微基质的分子鉴定

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摘要

Precambrian fossils of fungi are sparse, and the knowledge of their early evolution and the role they played in the colonization of land surface are limited. Here, we report the discovery of fungi fossils in a 810 to 715 million year old dolomitic shale from the Mbuji-Mayi Supergroup, Democratic Republic of Congo. Syngenetically preserved in a transitional, subaerially exposed paleoenvironment, these carbonaceous filaments of ~5 μm in width exhibit low-frequency septation (pseudosepta) and high-angle branching that can form dense interconnected mycelium-like structures. Using an array of microscopic (SEM, TEM, and confocal laser scanning fluorescence microscopy) and spectroscopic techniques (Raman, FTIR, and XANES), we demonstrated the presence of vestigial chitin in these fossil filaments and document the eukaryotic nature of their precursor. Based on those combined evidences, these fossil filaments and mycelium-like structures are identified as remnants of fungal networks and represent the oldest, molecularly identified remains of Fungi.
机译:FINAMBRIAN FOSSILS的真菌是稀疏的,以及他们早期演变的知识和他们在陆地表面定植中发挥的作用是有限的。在这里,我们向MBuji-Mayi超级刚果民主共和国的MBuji-Mayi超级群体中的810至715万年的Dolomitic页岩中发现了真菌化石的发现。在过渡性的亚胚暴露的古环境中,这些含有〜5μm的宽度的过渡性含有〜5μm的含碳丝(假瘤)和高角度支化,其可以形成致密的互连的菌丝状结构。使用微观(SEM,TEM和共聚焦激光扫描荧光显微镜)和光谱技术(Raman,FTIR和Xanes),我们证明了这些化石细丝中的病毒壳蛋白的存在,并记录其前体的真核性质。基于那些组合的证据,这些化石长丝和菌丝体状结构被鉴定为真菌网络的残余物,代表最古老的,分子鉴定的真菌遗骸。

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