真菌群落结构调节武功山草甸土壤有机碳组分的海拔变化

IF 4.2 2区 生物学 Q2 MICROBIOLOGY
Jinping Wang, Jihong Yuan, Qiong Ren, Liyin Zhou, Huanhuan Zeng, Lujun Miao, Zhiyong Sun, Fang Wan, Yuanying Yan
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引用次数: 0

摘要

土壤有机碳(SOC)组分是土壤有机碳稳定性的重要内在指标,而土壤真菌则是土壤碳循环的关键驱动力。然而,人们对高山草甸土壤有机碳组分沿海拔梯度的变化以及真菌群落在调节这些变化中的作用还知之甚少,尤其是在亚热带地区。本研究在中国东南部武功山草甸的中华鹅掌楸群落中建立了一个海拔梯度实验(实验地点分别为 1500、1700 和 1900 米),以阐明海拔对土壤真菌群落组成、微生物残碳和 SOC 分量的影响。结果表明,土壤微生物残碳对SOC的贡献率仅为16.1%,而土壤真菌残碳对SOC的贡献率(15.3%)远大于细菌残碳(0.3%)。海拔的升高改变了真菌群落的结构和多样性,尤其是表层土壤(0-20 厘米深)与底层土壤(20-40 厘米深)的真菌群落结构和多样性,但并不影响两层土壤中的真菌残碳。当把 SOC 分成矿物相关有机碳(MAOC)和颗粒有机碳(POC)时,我们发现矿物相关有机碳对 SOC 的贡献率(66.6%)明显高于颗粒有机碳(20.6%)。虽然海拔的升高并不影响 SOC 的浓度,但却显著改变了表土和底土中的 SOC 分量。土壤中 POC 的浓度及其对 SOC 的贡献随着海拔的升高而增加,而土壤中 MAOC 的反应则相反。SOC 分量和 POC/MAOC 比率的海拔变化受真菌群落结构和总氮的共同调控。我们的研究结果表明,高山草甸的 SOC 稳定性随着海拔的升高而降低,并受真菌群落结构的驱动,这为亚热带地区高山草甸的 SOC 固碳和稳定提供了科学指导。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The Fungal Community Structure Regulates Elevational Variations in Soil Organic Carbon Fractions in a Wugong Mountain Meadow.

Soil organic carbon (SOC) fractions are vital intrinsic indicators of SOC stability, and soil fungi are the key drivers of soil carbon cycling. However, variations in SOC fractions along an elevational gradient in mountain meadows and the role of the fungal community in regulating these variations are largely unknown, especially in subtropical areas. In this study, an elevation gradient experiment (with experimental sites at 1500, 1700, and 1900 m) was set up in a Miscanthus sinensis community in a meadow on Wugong Mountain, Southeast China, to clarify the effects of elevation on soil fungal community composition, microbial residue carbon, and SOC fractions. The results showed that the contribution of soil microbial residue carbon to SOC was only 16.1%, and the contribution of soil fungal residue carbon to SOC (15.3%) was far greater than that of bacterial residue carbon (0.3%). An increase in elevation changed the fungal community structure and diversity, especially in the topsoil (0-20 cm depth) compared with that in the subsoil (20-40 cm depth), but did not affect fungal residue carbon in the two soil layers. When separating SOC into the fractions mineral-associated organic carbon (MAOC) and particulate organic carbon (POC), we found that the contribution of MAOC (66.6%) to SOC was significantly higher than that of POC (20.6%). Although an increased elevation did not affect the SOC concentration, it significantly changed the SOC fractions in the topsoil and subsoil. The soil POC concentration and its contribution to SOC increased with an increasing elevation, whereas soil MAOC showed the opposite response. The elevational variations in SOC fractions and the POC/MAOC ratio were co-regulated by the fungal community structure and total nitrogen. Our results suggested that SOC stabilization in mountain meadows decreases with an increasing elevation and is driven by the fungal community structure, providing scientific guidance for SOC sequestration and stability in mountain meadows in subtropical areas.

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来源期刊
Journal of Fungi
Journal of Fungi Medicine-Microbiology (medical)
CiteScore
6.70
自引率
14.90%
发文量
1151
审稿时长
11 weeks
期刊介绍: Journal of Fungi (ISSN 2309-608X) is an international, peer-reviewed scientific open access journal that provides an advanced forum for studies related to pathogenic fungi, fungal biology, and all other aspects of fungal research. The journal publishes reviews, regular research papers, and communications in quarterly issues. Our aim is to encourage scientists to publish their experimental and theoretical results in as much detail as possible. Therefore, there is no restriction on paper length. Full experimental details must be provided so that the results can be reproduced.
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