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Phytolith-Occluded Carbon Sequestration Potential of Oil Palm Plantation in Tamil Nadu

[Image: see text] Oil palm (Elaeis guineensis) has proven to be a phytolith-occluded carbon (PhytOC)-rich species that plays a vital role in acting as a carbon sink for reducing atmospheric carbon dioxide (CO(2)) concentration. The present research estimated the silicon, phytolith, and PhytOC conten...

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Autores principales: Davamani, Veeraswamy, Sangeetha Piriya, Ramasamy, Rakesh, Srirangarayan Subramanian, Parameswari, Ettiyagounder, Paul Sebastian, Selvaraj, Kalaiselvi, Periasamy, Maheswari, Muthunalliappan, Santhi, Rangasamy
Formato: Online Artículo Texto
Lenguaje:English
Publicado: American Chemical Society 2022
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8792923/
https://www.ncbi.nlm.nih.gov/pubmed/35097277
http://dx.doi.org/10.1021/acsomega.1c05592
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author Davamani, Veeraswamy
Sangeetha Piriya, Ramasamy
Rakesh, Srirangarayan Subramanian
Parameswari, Ettiyagounder
Paul Sebastian, Selvaraj
Kalaiselvi, Periasamy
Maheswari, Muthunalliappan
Santhi, Rangasamy
author_facet Davamani, Veeraswamy
Sangeetha Piriya, Ramasamy
Rakesh, Srirangarayan Subramanian
Parameswari, Ettiyagounder
Paul Sebastian, Selvaraj
Kalaiselvi, Periasamy
Maheswari, Muthunalliappan
Santhi, Rangasamy
author_sort Davamani, Veeraswamy
collection PubMed
description [Image: see text] Oil palm (Elaeis guineensis) has proven to be a phytolith-occluded carbon (PhytOC)-rich species that plays a vital role in acting as a carbon sink for reducing atmospheric carbon dioxide (CO(2)) concentration. The present research estimated the silicon, phytolith, and PhytOC contents in four (OP4), eight (OP8), and fifteen (OP15)-year-old oil palm plantations. Qualitative analysis using a scanning electron microscope (SEM) revealed the presence of abundant globular echinate phytoliths with varied diameter (8.484–10.18 μm) in fronds, empty fruit bunches, and roots. Furthermore, a wide band (400–490 cm(–1)) underlined a higher relative abundance of Si–OH groups in empty fruit bunches, fronds, and roots, which emphasized the amorphous nature of silica. Quantitative analysis revealed that the phytolith (phytolith/dry biomass), PhytOC (PhytOC/phytolith), and PhytOC (PhytOC/dry biomass) contents in all oil palms differed significantly (p < 0.05) and increased with age. The PhytOC stock showed significant variation, with the trend of OP15 > OP8 > OP4. The belowground biomass of OP4 (16.43 g kg(–1)) and OP8 (17.13 g kg(–1)) had a maximum PhytOC concentration compared to the aboveground biomass, and the belowground proportion varied from 20.62 to 20.65%. The study demonstrated a positive correlation between the phytolith and PhytOC contents of oil palm; thereby, oil palm should be cultivated for enhanced long-term sequestration as a phytolith accumulator.
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spelling pubmed-87929232022-01-28 Phytolith-Occluded Carbon Sequestration Potential of Oil Palm Plantation in Tamil Nadu Davamani, Veeraswamy Sangeetha Piriya, Ramasamy Rakesh, Srirangarayan Subramanian Parameswari, Ettiyagounder Paul Sebastian, Selvaraj Kalaiselvi, Periasamy Maheswari, Muthunalliappan Santhi, Rangasamy ACS Omega [Image: see text] Oil palm (Elaeis guineensis) has proven to be a phytolith-occluded carbon (PhytOC)-rich species that plays a vital role in acting as a carbon sink for reducing atmospheric carbon dioxide (CO(2)) concentration. The present research estimated the silicon, phytolith, and PhytOC contents in four (OP4), eight (OP8), and fifteen (OP15)-year-old oil palm plantations. Qualitative analysis using a scanning electron microscope (SEM) revealed the presence of abundant globular echinate phytoliths with varied diameter (8.484–10.18 μm) in fronds, empty fruit bunches, and roots. Furthermore, a wide band (400–490 cm(–1)) underlined a higher relative abundance of Si–OH groups in empty fruit bunches, fronds, and roots, which emphasized the amorphous nature of silica. Quantitative analysis revealed that the phytolith (phytolith/dry biomass), PhytOC (PhytOC/phytolith), and PhytOC (PhytOC/dry biomass) contents in all oil palms differed significantly (p < 0.05) and increased with age. The PhytOC stock showed significant variation, with the trend of OP15 > OP8 > OP4. The belowground biomass of OP4 (16.43 g kg(–1)) and OP8 (17.13 g kg(–1)) had a maximum PhytOC concentration compared to the aboveground biomass, and the belowground proportion varied from 20.62 to 20.65%. The study demonstrated a positive correlation between the phytolith and PhytOC contents of oil palm; thereby, oil palm should be cultivated for enhanced long-term sequestration as a phytolith accumulator. American Chemical Society 2022-01-10 /pmc/articles/PMC8792923/ /pubmed/35097277 http://dx.doi.org/10.1021/acsomega.1c05592 Text en © 2022 The Authors. Published by American Chemical Society https://creativecommons.org/licenses/by-nc-nd/4.0/Permits non-commercial access and re-use, provided that author attribution and integrity are maintained; but does not permit creation of adaptations or other derivative works (https://creativecommons.org/licenses/by-nc-nd/4.0/).
spellingShingle Davamani, Veeraswamy
Sangeetha Piriya, Ramasamy
Rakesh, Srirangarayan Subramanian
Parameswari, Ettiyagounder
Paul Sebastian, Selvaraj
Kalaiselvi, Periasamy
Maheswari, Muthunalliappan
Santhi, Rangasamy
Phytolith-Occluded Carbon Sequestration Potential of Oil Palm Plantation in Tamil Nadu
title Phytolith-Occluded Carbon Sequestration Potential of Oil Palm Plantation in Tamil Nadu
title_full Phytolith-Occluded Carbon Sequestration Potential of Oil Palm Plantation in Tamil Nadu
title_fullStr Phytolith-Occluded Carbon Sequestration Potential of Oil Palm Plantation in Tamil Nadu
title_full_unstemmed Phytolith-Occluded Carbon Sequestration Potential of Oil Palm Plantation in Tamil Nadu
title_short Phytolith-Occluded Carbon Sequestration Potential of Oil Palm Plantation in Tamil Nadu
title_sort phytolith-occluded carbon sequestration potential of oil palm plantation in tamil nadu
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8792923/
https://www.ncbi.nlm.nih.gov/pubmed/35097277
http://dx.doi.org/10.1021/acsomega.1c05592
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