Abstract

Plantation management practices could markedly change the sequestration of phytolith-occluded carbon (PhytOC) in plants and soils. However, for Moso bamboo (Phyllostachys pubescens) plantations, the effect of intensive plantation management (including fertilization, tillage, and removal of understory vegetation) on the accretion rate of PhytOC in the soil-plant system is much less understood than extensive management (without fertilization, tillage, and removal of understory vegetation). The objectives of this study were to investigate the effect of intensive and extensive management practices on the production, accumulation, and runoff of PhytOC and their distribution in physical fractions in Moso bamboo plantations. Our results showed that intensive management (1) increased PhytOC production mainly due to increased forest productivity; (2) increased PhytOC storage in the heavy fraction but decreased its storage in the light fraction of organic matter, resulting in the lack of effect on soil PhytOC storage; (3) increased the rate of dissolution of phytolith and the loss of PhytOC in runoff; and (4) promoted PhytOC sequestration in the soil-plant system, mostly in the plants, due to the greater rate of PhytOC production than the rate of loss. We conclude that intensive bamboo plantation management practices are beneficial to increasing long-term PhytOC sequestration in the soil-plant system.

Highlights

  • Phytoliths are ergastic siliceous substances abundantly present within intercellular spaces and inside the cells of numerous plants [1,2]

  • Studies about phytolith-occluded carbon (PhytOC) sequestration have mainly been focused on plants

  • Intensive management decreased the mean value of total soil SiO2 concentration in the

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Summary

Introduction

Phytoliths are ergastic siliceous substances abundantly present within intercellular spaces and inside the cells of numerous plants [1,2]. Of organic carbon (C) can be occluded within the phytoliths [3,4]. In terrestrial ecosystems is highly resistant to decomposition [5,6] and may accumulate in the soil for centuries and millennia. The PhytOC can contribute 15–37% of long-term biogeochemical C sequestration [7]. In forest ecosystems, studies about PhytOC sequestration have mainly been focused on plants, especially aboveground plant components [4,8,9,10,11,12,13]. Little is known about PhytOC sequestration in the soil-plant system and PhytOC storage in the soil has been overlooked

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