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Multi-Stage Silicification of Pliocene Wood: Re-Examination of an 1895 Discovery from Idaho, USA

机译:上新世木材的多阶段硅化作用:对来自美国爱达荷州的1895年发现物的重新检验

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The 1895 discovery of a petrified tree near Clover Creek in south-central Idaho, USA, attracted worldwide attention and resulted in the naming of a new species of ancient oak, Quercinium pliocaenicum Schuster. For more than a century, the discovery has largely been forgotten, even though specimens reside in reputable museums. Reinvestigation of the locality in 2014/2015 resulted in newly-collected specimens and a wealth of new data. Optical microscopy confirms the cellular anatomy used for the original taxonomic study. X-ray diffraction, scanning electron microscopy, energy-dispersive electron spectroscopy, Raman spectroscopy and cathodoluminescence microscopy reveal details of the mineralization, showing the presence of opal-CT as the primary component, with chalcedony as a lesser constituent. This mineralogy suggests petrifaction occurred in at least two stages, beginning with opalization of cellular tissue, leaving open vessels that became filled with chalcedony during a later mineralization episode. Clover Creek oak represents relict flora growing in a wetter climate before the uplift of the Cascade Range created a rain shadow that caused profound desertification of the inland Pacific Northwest.
机译:1895年,在美国爱达荷州中南部的四叶草溪附近发现一棵石化树,引起了全世界的关注,并命名了一种新的古栎命名为Quercinium pliocaenicum Schuster。一个多世纪以来,即使标本存放在著名的博物馆中,这一发现也基本上被遗忘了。 2014/2015年对该地区进行的重新调查产生了新收集的标本和大量新数据。光学显微镜确认了用于原始分类学研究的细胞解剖结构。 X射线衍射,扫描电子显微镜,能量分散电子光谱,拉曼光谱和阴极发光显微镜揭示了矿化的细节,表明存在蛋白石-CT作为主要成分,而玉髓为次要成分。这种矿物学特征表明,石化作用至少发生在两个阶段,首先是细胞组织的不透明化,而在随后的矿化过程中,留下了充满玉髓的开放血管。三叶草溪橡树代表了在潮湿气候下生长的残lic植物群,然后在喀斯喀特山脉的隆起造成了一个雨影,导致西北太平洋内陆地区发生了严重的沙漠化。

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