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Published on: February 9, 2019
Phytolith Formation in Plants: From Soil to Cell.
Muhammad Amjad Nawaz1, Alexander Mikhailovich Zakharenko1, Ivan Vladimirovich Zemchenko1
1Education and Scientific Center of Nanotechnology, Far Eastern Federal University, 690950 Vladivostok, Russia.
Phytoliths, solid silica in plants, are crucial for taxonomy and environmental reconstruction. This review integrates current knowledge on silica uptake, transport, and deposition, exploring factors influencing phytolith formation and evolution.
Area of Science:
- Plant biology
- Biogeochemistry
- Paleoecology
Background:
- Silica deposition as phytoliths in plants is vital for taxonomy and reconstructing past environments.
- Understanding silicon transport and phytolith formation mechanisms is crucial but remains incomplete.
- Recent advances in silicon transporter genes offer insights into plant silica accumulation and phylogeny.
Purpose of the Study:
- To review and synthesize current knowledge on silica uptake, transport, and phytolith deposition in plants.
- To discuss factors influencing phytolith shape, size, and chemistry.
- To explore the evolution of biosilicification in plants and the roles of specific proteins.
Main Methods:
- Literature review and synthesis of recent research on plant silicon metabolism.
- Integration of findings on silicon transporter genes and associated proteins.
- Analysis of factors controlling phytolith morphology and evolution.
Main Results:
- Silica uptake and transport involve specific silicon transporters (channel-type and efflux).
- Proteins like proline-rich proteins and siliplant1 play roles in silica deposition.
- Phytoliths serve as mechanical barriers against stress and are valuable paleo-environmental proxies.
Conclusions:
- Phytolith research is a rapidly expanding interdisciplinary field.
- Further research is needed to fully elucidate the mechanisms of silica deposition and phytolith morphogenesis.
- Phytoliths have significant applications in plant science, ecology, and earth sciences.
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