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

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 phytolith...

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Main Authors: Waseem Qader, Reyaz Ahmad Dar, Ishfaq Ul Rehman, Irfan Rashid, Suhail Hussain Sheikh
Format: Article
Language:English
Published: Elsevier 2024-12-01
Series:Quaternary Science Advances
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Online Access:http://www.sciencedirect.com/science/article/pii/S2666033424000765
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author Waseem Qader
Reyaz Ahmad Dar
Ishfaq Ul Rehman
Irfan Rashid
Suhail Hussain Sheikh
author_facet Waseem Qader
Reyaz Ahmad Dar
Ishfaq Ul Rehman
Irfan Rashid
Suhail Hussain Sheikh
author_sort Waseem Qader
collection DOAJ
description 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.
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spelling doaj-art-2937f678838d45c5853a35c5e58c1e7c2024-12-06T05:14:33ZengElsevierQuaternary Science Advances2666-03342024-12-0116100238Assessing phytolith preservation in a Late Quaternary loess-paleosol sequence from the Kashmir Valley, Northwest Himalaya, IndiaWaseem Qader0Reyaz Ahmad Dar1Ishfaq Ul Rehman2Irfan Rashid3Suhail Hussain Sheikh4Department of Earth Sciences, University of Kashmir, Srinagar, 190006, Jammu and Kashmir, IndiaDepartment of Earth Sciences, University of Kashmir, Srinagar, 190006, Jammu and Kashmir, India; Corresponding author.Department of Botany, University of Kashmir, Srinagar, 190006, Jammu and Kashmir, IndiaDepartment of Botany, University of Kashmir, Srinagar, 190006, Jammu and Kashmir, IndiaDepartment of Earth Sciences, University of Kashmir, Srinagar, 190006, Jammu and Kashmir, IndiaPhytolith 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.http://www.sciencedirect.com/science/article/pii/S2666033424000765PhytolithsPaleovegetationPaleoclimateLoess-paleosolsPreservationKashmir Himalaya
spellingShingle Waseem Qader
Reyaz Ahmad Dar
Ishfaq Ul Rehman
Irfan Rashid
Suhail Hussain Sheikh
Assessing phytolith preservation in a Late Quaternary loess-paleosol sequence from the Kashmir Valley, Northwest Himalaya, India
Quaternary Science Advances
Phytoliths
Paleovegetation
Paleoclimate
Loess-paleosols
Preservation
Kashmir Himalaya
title Assessing phytolith preservation in a Late Quaternary loess-paleosol sequence from the Kashmir Valley, Northwest Himalaya, India
title_full Assessing phytolith preservation in a Late Quaternary loess-paleosol sequence from the Kashmir Valley, Northwest Himalaya, India
title_fullStr Assessing phytolith preservation in a Late Quaternary loess-paleosol sequence from the Kashmir Valley, Northwest Himalaya, India
title_full_unstemmed Assessing phytolith preservation in a Late Quaternary loess-paleosol sequence from the Kashmir Valley, Northwest Himalaya, India
title_short Assessing phytolith preservation in a Late Quaternary loess-paleosol sequence from the Kashmir Valley, Northwest Himalaya, India
title_sort assessing phytolith preservation in a late quaternary loess paleosol sequence from the kashmir valley northwest himalaya india
topic Phytoliths
Paleovegetation
Paleoclimate
Loess-paleosols
Preservation
Kashmir Himalaya
url http://www.sciencedirect.com/science/article/pii/S2666033424000765
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