Erratum to “A Perspective on Stratigraphic, Vertically-Upward “Displacements or Dislocations” of Conodont-Elements: An Example From the Upper Devonian, Pre-Lithified, Black Shales of the Chattanooga Shale Formation In Tennessee, USA” ...

Michael Iannicelli
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Abstract

Even though the author already incorporated the citation of Sinninghe-Damste & Schouten (2006) into the text of the paper, the author regrets having failed to include their full citation within the Reference Section of my above paper which is: Sinninghe-Damste, J. S. & Schouton, S. (2006). Biological markers for anoxia in the photic zone of the water column. In, Volkman, J. K. (ed.), Marine Organic Matter: Biomarkers, Isotopes and DNA, (pp. 127 – 163). The Handbook of Environmental Chemistry, vol. 2N. Springer: Berlin and Heidelberg. https://doi.org/10.1007/698_2_005 The author also needs to paraphrase a statement made in the last three lines of the 2nd paragraph on page 40 where it reads as: “Thus, we may conclude here that paleo-upfreezing of any conodont-element(s) originally buried in the pre-lithified, light-colored shale occurred in order to account for their presence in black shale”. Instead, in lieu of that statement, it should read as “At this point in time of the study, we may tentatively conclude here while completely concluding later in the study, that conodont-elements originally existing in the underlying, pre-lithified, light-colored shale, had to paleo-upfreeze vertically upward into pre-lithified, black shale sediment in order to account for their presence in lithified black shale”.
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“牙形刺元素垂直向上的地层“位移或错位”的视角:以美国田纳西州查塔努加页岩组上泥盆统、前岩化黑色页岩为例”的勘误
尽管作者已经将Sinninghe-Damste & Schouten(2006)的引文纳入了论文的文本中,但作者遗憾的是没有将他们的完整引文纳入我的上述论文的参考文献部分,即:Sinninghe-Damste, j.s. & Schouton, S.(2006)。水柱光带缺氧的生物标记。在,Volkman, J. K.(主编),海洋有机物:生物标志物,同位素和DNA,(第127 - 163页)。《环境化学手册》第2卷第n期。斯普林格:柏林和海德堡。https://doi.org/10.1007/698_2_005作者还需要改写第40页第2段最后三行中的一句话:“因此,我们可以在这里得出结论,为了解释它们在黑色页岩中的存在,任何最初埋在石化前浅色页岩中的牙形刺元素都发生了古冻结。”相反,它应该读作“在研究的这个时间点上,我们可以暂时得出结论,而在研究的后期完全得出结论,牙形刺元素最初存在于下伏的,预岩化的浅色页岩中,必须垂直向上古冻结到预岩化的黑色页岩沉积物中,以便解释它们在岩化的黑色页岩中的存在”。
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