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ORIGINAL RESEARCH article

Front. Earth Sci.

Sec. Biogeoscience

Volume 13 - 2025 | doi: 10.3389/feart.2025.1569387

This article is part of the Research Topic Regulation of Biogeochemical Processes by Ecological Stoichiometry View all articles

Altitudinal patterns of soil and microbial C:N:P stoichiometry in subtropical forests in Daming Mountain, South China

Provisionally accepted
  • 1 Guangxi University, Nanning, Guangxi Zhuang Region, China
  • 2 Nanning Normal University, Nanning, China

The final, formatted version of the article will be published soon.

    Altitude-induced variations in hydrothermal conditions and vegetation affect the carbon (C), nitrogen (N), and phosphorus (P) contents in both soil and microbial biomass. However, the specific patterns of changes in these nutrients and their stoichiometry in response to altitudinal changes remain unclear. Therefore, in this study, we analyzed the altitudinal patterns of soil and microbial biomass C:N:P stoichiometry across three soil layers (0–20, 20–40, and 40–60 cm) in the subtropical mountain ecosystems on Daming Mountain, South China. Our results revealed that soil C content and C:N ratio in the 0–20 cm layer initially increased and then decreased with increasing altitude. Meanwhile, soil P content in the 40–60 cm layer decreased. Soil microbial biomass P content initially decreased and then increased with altitude across all soil layers, whereas soil microbial biomass C:P and N:P ratios exhibited opposite trends. For soil and microbial biomass C:P and N:P ratios along the altitudinal gradient, soil microbial growth was mainly restricted by P, with this limitation being more pronounced at mid-to-low altitudes. Soil microbial biomass C, N, and P contents were positively correlated with soil C, N, and P contents and their ratios, available N (AN), available P (AP), and soil water content (SWC), but negatively correlated with bulk density and soil pH. In contrast, microbial biomass C, N, and P stoichiometric ratios exhibited the opposite or non-significant relationships with these factors. Notably, AN, AP, and SWC were the dominant factors affecting soil microbial biomass C:N:P stoichiometry. These findings contribute to the understanding of soil nutrient stoichiometry and their responses to environmental changes in subtropical mountain ecosystems.

    Keywords: altitude, nutrient limitation, soil microbial biomass, Ecological stoichiometry, Daming Mountain

    Received: 31 Jan 2025; Accepted: 27 Mar 2025.

    Copyright: © 2025 Huo, Zhang, Luo and Hu. This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) or licensor are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.

    * Correspondence:
    Yinghua Luo, Guangxi University, Nanning, Guangxi Zhuang Region, China
    Gang Hu, Nanning Normal University, Nanning, China

    Disclaimer: All claims expressed in this article are solely those of the authors and do not necessarily represent those of their affiliated organizations, or those of the publisher, the editors and the reviewers. Any product that may be evaluated in this article or claim that may be made by its manufacturer is not guaranteed or endorsed by the publisher.

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