Sedimentological perspective on phytolith analysis in palaeoecological reconstruction

Phytoliths are essential palaeoecological proxies that play an immensely important role in palaeoclimatic studies. Their inert composition and general hardiness allow phytoliths to be preserved in geological settings, even when other plant fossils perish. This partially explains their utility for in...

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Published inEarth-science reviews Vol. 244; p. 104549
Main Authors Qader, Waseem, Mir, Showkat Hamid, Meister, Julia, Dar, Reyaz Ahmad, Madella, Marco, Rashid, Irfan
Format Journal Article
LanguageEnglish
Published Elsevier B.V 01.09.2023
Subjects
Analysis
archaeology
Bias
caves
fossils
microstructure
morphs
Palaeoecology
paleoclimatology
paleoecology
Phytoliths
Sediment
sediment transport
sediments
Soil
transportation
weather
Phytoliths
Soil
Palaeoecology
Sediment
Bias
Analysis
Online AccessGet full text
ISSN0012-8252
1872-6828
DOI10.1016/j.earscirev.2023.104549

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Abstract Phytoliths are essential palaeoecological proxies that play an immensely important role in palaeoclimatic studies. Their inert composition and general hardiness allow phytoliths to be preserved in geological settings, even when other plant fossils perish. This partially explains their utility for investigating plant communities and plant-human interactions on short and long timescales. Phytoliths also happen to be the most reliable source of fossil evidence for tracking the evolutionary history of grasses, arguably among the most crucial extant plant families. In the last two decades, the number of studies and publications in all fields of phytolith analysis has grown exponentially, mainly due to a diversification of research topics. Although significant progress has been made in applying phytolith analysis to answer archaeological, palaeoenvironmental, palaeoclimatological, evolutionary, and taxonomic questions, phytolith assemblages can be subject to pre- and post-depositional processes that might affect their preservation and thus could bias interpretation. This article reviews the importance of phytolith research in palaeoecology, discusses the constraints and taphonomic processes affecting phytolith analysis, and highlights the challenges in phytolith studies across various sediments. It emphasizes the significance of identifying phytolith transportation modes and understanding the impacts of taphonomic processes. Specific sampling strategies, such as targeting environments protected from surface weather conditions and selecting sediments with lower translocation rates or little horizon development, are suggested to preserve a diverse range of phytolith morphotypes. Caves and deltas are proposed as suitable alternatives to neritic marine sediments and carbonate-rich sites. This review also emphasizes the importance of sediment analysis, including grain size, sediment transport trend analysis, and micromorphology, complemented by analytical techniques and multi-proxy approaches. The inclusion of thin section studies, micromorphology, SEM, EDS, FT-IR, XRD, AAS/AES, XRF, and ICP-MS/AES is recommended to minimize depositional biases and help understand biases related to phytolith formation. Using mathematical models and correlation measurements to assess the impact of taphonomy on phytolith assemblages is also valuable. To conclude, we discuss some analytical considerations and suggest a methodological framework that integrates phytolith analysis with a sedimentological perspective. This approach aims to minimize the biases in phytolith analysis and enhance our understanding of palaeoecology.
AbstractList Phytoliths are essential palaeoecological proxies that play an immensely important role in palaeoclimatic studies. Their inert composition and general hardiness allow phytoliths to be preserved in geological settings, even when other plant fossils perish. This partially explains their utility for investigating plant communities and plant-human interactions on short and long timescales. Phytoliths also happen to be the most reliable source of fossil evidence for tracking the evolutionary history of grasses, arguably among the most crucial extant plant families. In the last two decades, the number of studies and publications in all fields of phytolith analysis has grown exponentially, mainly due to a diversification of research topics. Although significant progress has been made in applying phytolith analysis to answer archaeological, palaeoenvironmental, palaeoclimatological, evolutionary, and taxonomic questions, phytolith assemblages can be subject to pre- and post-depositional processes that might affect their preservation and thus could bias interpretation. This article reviews the importance of phytolith research in palaeoecology, discusses the constraints and taphonomic processes affecting phytolith analysis, and highlights the challenges in phytolith studies across various sediments. It emphasizes the significance of identifying phytolith transportation modes and understanding the impacts of taphonomic processes. Specific sampling strategies, such as targeting environments protected from surface weather conditions and selecting sediments with lower translocation rates or little horizon development, are suggested to preserve a diverse range of phytolith morphotypes. Caves and deltas are proposed as suitable alternatives to neritic marine sediments and carbonate-rich sites. This review also emphasizes the importance of sediment analysis, including grain size, sediment transport trend analysis, and micromorphology, complemented by analytical techniques and multi-proxy approaches. The inclusion of thin section studies, micromorphology, SEM, EDS, FT-IR, XRD, AAS/AES, XRF, and ICP-MS/AES is recommended to minimize depositional biases and help understand biases related to phytolith formation. Using mathematical models and correlation measurements to assess the impact of taphonomy on phytolith assemblages is also valuable. To conclude, we discuss some analytical considerations and suggest a methodological framework that integrates phytolith analysis with a sedimentological perspective. This approach aims to minimize the biases in phytolith analysis and enhance our understanding of palaeoecology.
ArticleNumber 104549
Author Qader, Waseem
Meister, Julia
Dar, Reyaz Ahmad
Madella, Marco
Mir, Showkat Hamid
Rashid, Irfan
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  givenname: Waseem
  surname: Qader
  fullname: Qader, Waseem
  organization: Department of Earth Sciences, University of Kashmir, Srinagar 190006, Jammu and Kashmir, India
– sequence: 2
  givenname: Showkat Hamid
  surname: Mir
  fullname: Mir, Showkat Hamid
  organization: Department of Botany, University of Kashmir, Srinagar 190006, Jammu and Kashmir, India
– sequence: 3
  givenname: Julia
  surname: Meister
  fullname: Meister, Julia
  organization: Institute of Geography and Geology, University of Würzburg, Am Hubland, 97074 Würzburg, Germany
– sequence: 4
  givenname: Reyaz Ahmad
  surname: Dar
  fullname: Dar, Reyaz Ahmad
  organization: Department of Earth Sciences, University of Kashmir, Srinagar 190006, Jammu and Kashmir, India
– sequence: 5
  givenname: Marco
  surname: Madella
  fullname: Madella, Marco
  organization: CaSEs Research Group (Culture and Socio-Ecological Dynamics), Department of Humanities - Universitat Pompeu Fabra, Spain
– sequence: 6
  givenname: Irfan
  surname: Rashid
  fullname: Rashid, Irfan
  email: irfanrashid@uok.edu.in
  organization: Department of Botany, University of Kashmir, Srinagar 190006, Jammu and Kashmir, India
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Snippet Phytoliths are essential palaeoecological proxies that play an immensely important role in palaeoclimatic studies. Their inert composition and general...
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SubjectTerms Analysis
archaeology
Bias
caves
fossils
microstructure
morphs
Palaeoecology
paleoclimatology
paleoecology
Phytoliths
Sediment
sediment transport
sediments
Soil
transportation
weather
Title Sedimentological perspective on phytolith analysis in palaeoecological reconstruction
URI https://dx.doi.org/10.1016/j.earscirev.2023.104549
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Volume 244
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