Production of carbon occluded in phytolith is season-dependent in a bamboo forest in subtropical China.

Carbon (C) occluded in phytolith (PhytOC) is a stable form of C; when PhytOC is returned to the soil through litterfall it is stored in the soil which can be an effective way for long-term C sequestration. However, few estimates on the rate of PhytOC input to the soil are available. To better unders...

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Autores principales: Zhang-Ting Huang, Pei-Kun Jiang, Scott Xiaochuan Chang, Yan Zhang, Yu-Qi Ying
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Publicado: Public Library of Science (PLoS) 2014
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Acceso en línea:https://doaj.org/article/593712278d1f4aa7b2b404a534f8bd3d
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spelling oai:doaj.org-article:593712278d1f4aa7b2b404a534f8bd3d2021-11-25T06:01:46ZProduction of carbon occluded in phytolith is season-dependent in a bamboo forest in subtropical China.1932-620310.1371/journal.pone.0106843https://doaj.org/article/593712278d1f4aa7b2b404a534f8bd3d2014-01-01T00:00:00Zhttps://www.ncbi.nlm.nih.gov/pmc/articles/pmid/25188462/pdf/?tool=EBIhttps://doaj.org/toc/1932-6203Carbon (C) occluded in phytolith (PhytOC) is a stable form of C; when PhytOC is returned to the soil through litterfall it is stored in the soil which can be an effective way for long-term C sequestration. However, few estimates on the rate of PhytOC input to the soil are available. To better understand the seasonal dynamics of PhytOC production and the annual rate of stable C sequestration through PhytOC input, we quantified the monthly litterfall, phytolith and PhytOC return to the soil over a year in a typical Lei bamboo (Phyllostachys praecox) forest in subtropical China. The monthly litterfall ranged between 14.81 and 131.18 g m(-2), and the phytolith concentration in the monthly litterfall samples ranged between 47.21 and 101.68 g kg(-1) of litter mass, with the PhytOC concentration in the phytolith ranged between 29.4 and 44.9 g kg(-1) of phytolith, equivalent to 1.8-3.6 g kg(-1) of PhytOC in the litterfall (based on litterfall dry mass). The amount of phytolith input to the soil system was 292.21 ± 69.12 (mean ± SD) kg ha(-1) yr(-1), sequestering 41.45 ± 9.32 kg CO2-e ha(-1) yr(-1) of C in the studied Lei bamboo forest. This rate of C sequestration through the formation of PhytOC found in this study falls within the range of rates for other grass-type species reported in the literature. We conclude that return of C occluded in phytolith to the soil can be a substantial source of stable soil C and finding means to increase PhytOC storage in the soil should be able to play a significant role in mitigating the rapidly increasing atmospheric CO2 concentration.Zhang-Ting HuangPei-Kun JiangScott Xiaochuan ChangYan ZhangYu-Qi YingPublic Library of Science (PLoS)articleMedicineRScienceQENPLoS ONE, Vol 9, Iss 9, p e106843 (2014)
institution DOAJ
collection DOAJ
language EN
topic Medicine
R
Science
Q
spellingShingle Medicine
R
Science
Q
Zhang-Ting Huang
Pei-Kun Jiang
Scott Xiaochuan Chang
Yan Zhang
Yu-Qi Ying
Production of carbon occluded in phytolith is season-dependent in a bamboo forest in subtropical China.
description Carbon (C) occluded in phytolith (PhytOC) is a stable form of C; when PhytOC is returned to the soil through litterfall it is stored in the soil which can be an effective way for long-term C sequestration. However, few estimates on the rate of PhytOC input to the soil are available. To better understand the seasonal dynamics of PhytOC production and the annual rate of stable C sequestration through PhytOC input, we quantified the monthly litterfall, phytolith and PhytOC return to the soil over a year in a typical Lei bamboo (Phyllostachys praecox) forest in subtropical China. The monthly litterfall ranged between 14.81 and 131.18 g m(-2), and the phytolith concentration in the monthly litterfall samples ranged between 47.21 and 101.68 g kg(-1) of litter mass, with the PhytOC concentration in the phytolith ranged between 29.4 and 44.9 g kg(-1) of phytolith, equivalent to 1.8-3.6 g kg(-1) of PhytOC in the litterfall (based on litterfall dry mass). The amount of phytolith input to the soil system was 292.21 ± 69.12 (mean ± SD) kg ha(-1) yr(-1), sequestering 41.45 ± 9.32 kg CO2-e ha(-1) yr(-1) of C in the studied Lei bamboo forest. This rate of C sequestration through the formation of PhytOC found in this study falls within the range of rates for other grass-type species reported in the literature. We conclude that return of C occluded in phytolith to the soil can be a substantial source of stable soil C and finding means to increase PhytOC storage in the soil should be able to play a significant role in mitigating the rapidly increasing atmospheric CO2 concentration.
format article
author Zhang-Ting Huang
Pei-Kun Jiang
Scott Xiaochuan Chang
Yan Zhang
Yu-Qi Ying
author_facet Zhang-Ting Huang
Pei-Kun Jiang
Scott Xiaochuan Chang
Yan Zhang
Yu-Qi Ying
author_sort Zhang-Ting Huang
title Production of carbon occluded in phytolith is season-dependent in a bamboo forest in subtropical China.
title_short Production of carbon occluded in phytolith is season-dependent in a bamboo forest in subtropical China.
title_full Production of carbon occluded in phytolith is season-dependent in a bamboo forest in subtropical China.
title_fullStr Production of carbon occluded in phytolith is season-dependent in a bamboo forest in subtropical China.
title_full_unstemmed Production of carbon occluded in phytolith is season-dependent in a bamboo forest in subtropical China.
title_sort production of carbon occluded in phytolith is season-dependent in a bamboo forest in subtropical china.
publisher Public Library of Science (PLoS)
publishDate 2014
url https://doaj.org/article/593712278d1f4aa7b2b404a534f8bd3d
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AT scottxiaochuanchang productionofcarbonoccludedinphytolithisseasondependentinabambooforestinsubtropicalchina
AT yanzhang productionofcarbonoccludedinphytolithisseasondependentinabambooforestinsubtropicalchina
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