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Taphonomical Aspects Of Silica Phytoliths In The Loess Sediments Of Theargentinean Pampas

机译:黄柏沉积物黄柏沉积物中二氧化硅硅石的排污作用

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摘要

Although Pampean loess and pedostratigraphy processes in the Pampas have been widely studied, phytoliths observed in these sediments have been only mentioned without further quantitative or qualitative studies. The present work is a first step towards an understanding of the environmental significance of loess phytolith datasets and their validity for palaeoenvironmental reconstructions, and to comprehend the environmental conditions of loess formation. The research focused on the taphonomy of loess phytoliths investigating the loess morphological and sedimentological characteristics, variability in the qualitative and quantitative assemblage composition, the phytolith frequency and were also phytolith extraction techniques. The results highlight that the phytolith pool of loess deposits still retains information about the past vegetation and phytolith analysis from these deposits can be a useful exercise to further comprehend past climatic and environmental conditions under which loess-palaeosol sequences formed.
机译:尽管对潘帕斯邦的潘邦黄土和地层学过程进行了广泛研究,但仅提及这些沉积物中观察到的植物石层,而没有进行进一步的定量或定性研究。目前的工作是迈向了解黄土植物石料数据集的环境意义及其在古环境重建中的有效性的第一步,并理解了黄土形成的环境条件。该研究的重点是黄土植物硅石的形态学,研究了黄土的形态和沉积特征,定性和定量组合组成的变异性,植物石的频率以及植物石体的提取技术。结果表明,黄土沉积物的植物岩层池仍保留着有关过去植被的信息,这些沉积物中的植物岩层分析可能是进一步了解黄土-古土壤序列形成的过去气候和环境条件的有用练习。

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