Luo Yonghong, Cheng Jiming, Mahmood Mohsin, Wei Shuhua, Peng Liqing, Zhang Chao, Zhang Min, Zhang Jinfeng, Yang Hui, Wang Jiazhi, Hao Zhenggang, Yan Xingfu
School of Biological Science and Engineering, North Minzu University, Yinchuan, 750021, China.
School of Ecology and Environment, Inner Mongolia University, Hohhot, 010000, China.
Sci Rep. 2025 May 6;15(1):15752. doi: 10.1038/s41598-025-00326-6.
Nitrogen (N) and phosphorus (P) are vital nutrients in terrestrial ecosystems, essential for vegetation growth, plant survival, development, and the maintenance of plant diversity. While the effects of N and P additions on plant nutrient concentrations and diversity have been extensively studied, the impact of various stages of natural forest ecosystem restoration after disturbance, particularly on plant N, P nutrients, and diversity, is less understood. This study investigates the influence of anthropogenic disturbance on soil N: P ratios, plant community-level N: P, and species diversity in Liaodong oak forests in northern China during early (about 10 years), mid-to-late (about 30 years), and late (about 40 years) restoration stages (it is a space for time substitution method). We observed that soil total nitrogen to total phosphorus ratio (TN: TP) and soil available nitrogen to phosphorus ratio (AN: AP) were significantly lower in the mid-to-late and late stages of restoration compared to the early restoration stages. Concurrently, plant community level leaf nitrogen-phosphorus ratio (CWM) were notably lower in these later stages. Additionally, species richness showed a decline as restoration time increased. These findings highlight that decreasing soil N: P ratio over time exacerbates plant N limitation and reduces plant richness, emphasizing the critical role of soil nutrient dynamics in forest restoration post-disturbance. Our results provide important insights for forest management and restoration practices, contributing to a better understanding of ecosystem restoration processes.
氮(N)和磷(P)是陆地生态系统中的重要养分,对植被生长、植物存活、发育以及植物多样性的维持至关重要。虽然氮和磷添加对植物养分浓度和多样性的影响已得到广泛研究,但干扰后天然森林生态系统恢复的各个阶段,特别是对植物氮、磷养分和多样性的影响,却鲜为人知。本研究调查了人为干扰对中国北方辽东栎林在早期(约10年)、中晚期(约30年)和晚期(约40年)恢复阶段(采用空间换时间方法)的土壤氮磷比、植物群落水平氮磷比和物种多样性的影响。我们观察到,与早期恢复阶段相比,恢复的中晚期和晚期土壤全氮与全磷比(TN:TP)以及土壤有效氮与磷比(AN:AP)显著降低。同时,这些后期阶段的植物群落水平叶氮磷比(CWM)明显较低。此外,物种丰富度随着恢复时间的增加而下降。这些发现突出表明,随着时间推移土壤氮磷比降低会加剧植物的氮限制并降低植物丰富度,强调了土壤养分动态在干扰后森林恢复中的关键作用。我们的结果为森林管理和恢复实践提供了重要见解,有助于更好地理解生态系统恢复过程。