Lithological control on phytolith carbon sequestration in moso bamboo forests

摘要

Phytolith-occluded carbon (PhytOC) is a stable carbon (C) fraction that has effects on long-term global C balance. Here, we report the phytolith and PhytOC accumulation in moso bamboo leaves developed on four types of parent materials. The results show that PhytOC content of moso bamboo varies with parent material in the order of granodiorite (2.0?g kgsup?1/sup) granite (1.6?g kgsup?1/sup) basalt (1.3?g kgsup?1/sup) shale (0.7?g kgsup?1/sup). PhytOC production flux of moso bamboo on four types of parent materials varies significantly from 1.0 to 64.8?kg COsub2/sub hasup?1/sup yrsup?1/sup, thus a net 4.7 × 10sup6/sup –310.8 × 10sup6/sup?kg COsub2/sub yrsup?1/sup would be sequestered by moso bamboo phytoliths in China. The phytolith C sequestration rate in moso bamboo of China will continue to increase in the following decades due to nationwide bamboo afforestation/reforestation, demonstrating the potential of bamboo in regulating terrestrial C balance. Management practices such as afforestation of bamboo in granodiorite area and granodiorite powder amendment may further enhance phytolith C sequestration through bamboo plants.