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Lithological control on phytolith carbon sequestration in moso bamboo forests
Beilei Li1, Zhaoliang Song2, Hailong Wang3
1School of Environment and Resources, Zhejiang Agricultural and Forestry University, Lin'an, Zhejiang 311300, China.
Scientific Reports
|June 12, 2014
Summary
Phytolith-occluded carbon (PhytOC) in moso bamboo leaves is a stable carbon fraction. PhytOC accumulation varies by parent material, with granodiorite yielding the highest content, highlighting bamboo
Area of Science:
- Soil Science
- Ecology
- Biogeochemistry
Background:
- Phytolith-occluded carbon (PhytOC) represents a stable soil carbon pool.
- Understanding PhytOC dynamics is crucial for global carbon balance assessments.
- Moso bamboo (Phyllostachys edulis) is a significant terrestrial plant with potential for carbon sequestration.
Purpose of the Study:
- To quantify phytolith and PhytOC accumulation in moso bamboo leaves across diverse parent materials.
- To assess the impact of parent material on PhytOC content and production flux.
- To evaluate the potential of moso bamboo for carbon sequestration in China.
Main Methods:
- Analysis of phytolith and PhytOC content in moso bamboo leaves.
- Measurement of PhytOC production flux based on parent material.
- Estimation of net carbon sequestration by bamboo phytoliths in China.
Main Results:
- PhytOC content in moso bamboo leaves followed the order: granodiorite > granite > basalt > shale.
- PhytOC production flux varied significantly across parent materials, ranging from 1.0 to 64.8 kg CO₂ ha⁻¹ yr⁻¹.
- Moso bamboo phytoliths in China could sequester a net 4.7 × 10⁶–310.8 × 10⁶ kg CO₂ yr⁻¹.
Conclusions:
- Parent material significantly influences PhytOC accumulation in moso bamboo.
- Moso bamboo exhibits substantial potential for phytolith carbon sequestration, especially in China.
- Afforestation and soil amendment strategies, particularly in granodiorite-rich areas, can enhance carbon sequestration by bamboo.

