Expansion of Moso bamboo into Chinese fir stands persistently depletes rhizosphere bioavailable P pools: a seasonal, space-for-time approach

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Authors: Shuangbo Bi, Xuerong Shi, Chunju Peng, Tianyi Hu, Jing Chen, Jingchen Xie, Haicheng Li, Tingting Cao, Man Shi, Zhikang Wang, Quan Li, Xinzhang Song
Cited by: 1
References: 54

Abstract

Introduction Accurate understanding of soil phosphorus (P) fractions is crucial for enhancing plant productivity and deciphering forest succession patterns; however, the dynamics of rhizosphere soil P fractions and their influencing factors during forest succession or land-type conversion, particularly in highly weathered tropical and subtropical regions, have not been comprehensively elucidated. Methods Using a space-for-time replacement strategy, in this study, we examined how Moso bamboo ( Phyllostachys edulis ) expansion into Chinese fir ( Cunninghamia lanceolata ) forests affects P fractions in rhizosphere soil across various seasons within a subtropical region. The research focused on seasonal variations in soil P dynamics resulting from this invasive expansion. We further evaluated key drivers, encompassing soil physicochemical characteristics and microbial traits. Results and discussion Compared to pure Chinese fir forests, mixed bamboo–fir stands had significant reductions in total P (excluding spring), CaCl 2 -P, Citrate-P, Enzyme-P (excluding spring), and HCl-P (excluding winter) throughout the seasonal cycle ( p < 0.05). Pure bamboo forests showed further reduction in total P, Citrate-P, Enzyme-P, and HCl-P, along with reduced CaCl 2 -P (except summer and winter) ( p < 0.05), with most P fractions (except CaCl 2 -P in summer, Citrate-P and HCl-P in summer and autumn, and Enzyme-P in summer) being lower in these stands than in mixed forests, which showed a decreasing trend with increasing expansion intensity. CaCl 2 -P, citrate-P, and HCl-P levels were consistently higher in summer and autumn than in winter and spring across Moso bamboo, Chinese fir, and mixed forest stands. Variations in P fractions were under the major control of nitrogen components and soil pH. This study highlights the importance of clarifying P fraction dynamics to understand forest succession mechanisms and informing P management strategies for enhancing forest productivity.

Fields of Study & Subjects

Soil Carbon and Nitrogen Dynamics Ecology and Vegetation Dynamics Studies Soil Management and Crop Yield

Publication details

Journal / source
Frontiers in Plant Science
Publisher
Frontiers Media SA
Volume
16
Pages
1718574–1718574
Publication date
20 January 2026
Language
EN