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生态学杂志 ›› 2025, Vol. 44 ›› Issue (9): 2907-2918.doi: 10.13292/j.1000-4890.202509.015

• 研究报告 • 上一篇    下一篇

热带次生林生态恢复过程中土壤真菌群落构建演变及其与土壤有机碳稳定性的关系

羊美秋1,邓丹婷1,孙延菲2*,龙文兴2   

  1. 1海南大学热带农林学院, 海口 570228; 2海南大学生态学院, 海口 570228)
  • 出版日期:2025-09-10 发布日期:2025-09-03

Soil fungal community structure dynamics and its relationship with soil organic carbon stability during ecological restoration of tropical secondary forests.

YANG Meiqiu1, DENG Danting1, SUN Yanfei2*, LONG Wenxing2   

  1. (1School of Tropical Agriculture and Forestry, Hainan University, Haikou 570228, China; 2School of Ecology, Hainan University, Haikou 570228, China).

  • Online:2025-09-10 Published:2025-09-03

摘要: 热带次生林土壤有机碳变化对于全球碳平衡至关重要,而土壤真菌在土壤碳分解中扮演着重要角色。然而,关于热带次生林恢复过程中土壤真菌群落对有机碳稳定性的影响机制尚不清楚。本研究以海南热带雨林国家公园霸王岭片区刀耕火种恢复早期(<30 a)、中期(>40 a)、后期(>70 a)的次生林及老龄林(>300 a)为对象,采集腐殖质层(Ah)和淋溶层(E)土壤样品。通过傅里叶变换红外光谱法测定土壤有机碳化学组分含量,并结合土壤真菌群落多样性、组成和网络稳定性等分析,探究其与有机碳化学稳定性的关系。结果表明,随着热带次生林恢复,土壤总有机碳含量并未发生显著变化,但不同化学组分表现出显著的动态特征:多糖碳和芳香碳含量呈先增加后减少的趋势,脂肪碳则呈相反的变化趋势。恢复中期次生林的土壤有机碳化学组成稳定性最强。Ah层土壤总有机碳及其化学组分显著高于E层。土壤真菌α多样性在次生林恢复过程中无显著变化,但随着土壤深度增加,真菌丰富度显著降低。由分子生态网络分析可知,次生林恢复和土壤深度增加显著增强了真菌群落网络稳定性,关键物种主要为外生菌根真菌和腐生真菌,包括红菇属(Russula)、丝盖伞属(Inocybe)、蜡壳菌属(Sebacina)、粉褶蕈属(Entoloma)、青霉属(Penicillium)、曲霉属(Aspergillus)和被孢霉属(Mortierella)真菌。结构方程模型结果表明,热带次生林恢复主要通过影响土壤真菌关键物种来调控有机碳化学组分的稳定性。本研究揭示了热带次生林恢复过程中土壤真菌在有机碳稳定性调控中的核心作用,为理解热带次生林土壤碳动态的微生物机制及次生林生态管理提供了重要的理论支持。


关键词: 热带低地次生林, 土壤真菌群落, 分子生态网络, 土壤有机碳化学组分, 土壤有机碳稳定性

Abstract: Changes in soil organic carbon in tropical secondary forests are critical to global carbon balance, with soil fungi playing a key role in soil carbon decomposition. However, the effect of soil fungal communities on the stability of soil organic carbon during the restoration of tropical secondary forests remains unclear. We investigated the secondary forests at the early (<30 years), middle (>40 years), and late (>70 years) stages of restoration and the old-growth forests (>300 years) in the Bawangling Branch of National Park of Hainan Tropical Rainforest, Hainan Island, China. Soil samples were collected from the humus (Ah) and eluvial (E) horizons. The chemical composition of soil organic carbon was analyzed using Fourier transform infrared spectroscopy. We further examined the relationships of fungal community diversity, composition, and network stability with organic carbon chemical stability. The results showed that total organic carbon content remained stable during forest restoration. However, polysaccharide carbon and aromatic carbon contents increased initially and then decreased, whereas aliphatic carbon showed an opposite trend. The chemical stability of soil organic carbon was highest in the middle-stage secondary forests. The Ah horizon exhibited significantly higher total organic carbon and its chemical fractions than the E horizon. While secondary forest restoration did not affect soil fungal alpha diversity, fungal richness declined markedly with increasing soil depth. Molecular ecological network analysis showed that the stability of the fungal community network increased with forest restoration and soil depth. Keystone fungal species were primarily ectomycorrhizal and saprophytic fungi, including Russula, Inocybe, Sebacina, Entoloma, Penicillium, Aspergillus, and Mortierella. Structural equation modeling demonstrated that the restoration of tropical secondary forests mainly regulated the stability of organic carbon by influencing the keystone fungal species. These findings provide insights into the microbial mechanisms regulating soil organic carbon dynamics during tropical secondary forest restoration and provide theoretical support for the ecological management of tropical secondary forests.


Key words: tropical lowland secondary forest, soil fungal community, molecular ecological network, soil organic carbon chemical fraction, soil organic carbon stability