Assessing phytolith preservation in a Late Quaternary loess-paleosol sequence from the Kashmir Valley, Northwest Himalaya, India

IF 2.9 Q2 GEOGRAPHY, PHYSICAL
Waseem Qader , Reyaz Ahmad Dar , Ishfaq Ul Rehman , Irfan Rashid , Suhail Hussain Sheikh
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Abstract

Phytolith content and its preservation in soils form a robust tool for paleoecological reconstruction. Post-depositional processes, however, influence the preservation of phytolith assemblages in soils thus making the paleoecological inferences biased. Here we evaluated the preservation of phytoliths in a Late Quaternary loess-paleosol sequence (LPS) from Kashmir Valley, northwest Himalaya. The soil micromorphological study, physicochemical parameters, phytolith morphometry, and phytolith translocation rates were employed to assess phytolith preservation and absence (not recorded) in the various litho-units of the Wanihama LPS. The comparison of phytolith content and soil physio-chemical parameters including pH, electrical conductivity, available N, P, K, organic carbon, extractable Fe, Zn, Mn and Cu do not show any significant correlation. This suggests that soil physicochemical parameters have a minor role in regulating the preservation of phytoliths in the LPS. The depth distribution of phytoliths exhibits an inconsistent pattern and phytolith content doesn't decrease systematically with depth. The phytolith content usually follows the loess-paleosol stratigraphy, with low concentrations in loess units and high concentrations in paleosols indicating that phytolith assemblages in the LPS have not been altered or translocated as a result of pedogenic processes. The micromorphological observations suggest weak pedogenesis and the sequence does not seem to be significantly mixed by bioturbation activities. This is augmented by the low translocation rate of <18%, and phytolith morphometry suggesting well-preserved phytoliths with minimum morphological alterations along the depth. The absence of phytoliths at certain stratigraphic units in the LPS thus suggests that climatic conditions rather than physicochemical parameters determine the phytolith preservation and their content in the Kashmir LPS.

评估印度西北喜马拉雅克什米尔山谷第四纪晚期黄土-页岩序列中的植物岩石保存情况
土壤中的植生石含量及其保存方式是重建古生态的有力工具。然而,沉积后的过程会影响土壤中植物碎屑的保存,从而使古生态推断产生偏差。在此,我们评估了喜马拉雅西北部克什米尔山谷第四纪晚期黄土-古溶胶序列(LPS)中植物碎屑的保存情况。通过土壤微观形态研究、理化参数、植物石形态测量和植物石迁移率,评估了瓦尼哈马黄土页岩序列各岩相单元中植物石的保存和缺失(未记录)情况。植物石含量与土壤理化参数(包括 pH 值、电导率、可利用的氮、磷、钾、有机碳、可提取的铁、锌、锰和铜)的比较未显示出任何显著的相关性。这表明,土壤理化参数对植物体在植被覆盖层中的保存作用不大。植生石块的深度分布呈现出不一致的模式,植生石块的含量并没有随着深度的增加而系统地减少。植生石含量通常遵循黄土-古沉积地层,黄土层中含量低,古沉积层中含量高,这表明低洼地带的植生石组合并没有因为成土过程而发生改变或迁移。微观形态观察结果表明,成土作用较弱,序列似乎没有明显的生物扰动活动。此外,18%的低移位率和植物岩石形态测量表明,植物岩石保存完好,沿深度方向的形态变化极小。因此,克什米尔低地层中某些地层单元没有植生岩的现象表明,克什米尔低地层中植生岩的保存及其含量是由气候条件而非物理化学参数决定的。
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来源期刊
Quaternary Science Advances
Quaternary Science Advances Earth and Planetary Sciences-Earth-Surface Processes
CiteScore
4.00
自引率
13.30%
发文量
16
审稿时长
61 days
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