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    典型亚热带森林恢复过程中土壤微生物特性垂直分异特征

    Vertical differentiation characteristics of soil microbial properties during typical subtropical forest restoration

    • 摘要: 本文研究了森林恢复过程中土壤微生物群落及其养分代谢功能沿土壤垂直剖面变化的演变规律与驱动机制。以亚热带先锋树种为马尾松的针叶林、针阔混交林、次生常绿阔叶林和成熟常绿阔叶林组成的恢复序列为研究对象,按表层(0~10,10~20 cm)、亚表层(20~40,40~60 cm)和深层(60~80,80~100 cm)采集土壤样品,通过测定微生物磷脂脂肪酸、碳氮磷循环相关酶活性及微生物碳利用效率,系统分析了不同土层的微生物特征及其对环境因子的响应。结果显示:(1)森林恢复显著提高了不同土层微生物磷脂脂肪酸总量和各微生物类群生物量,但深层土壤呈现出明显的滞后性;表层和亚表层土壤的真菌/细菌随森林恢复显著下降;(2)森林恢复显著降低了各土层葡萄糖苷酶活性,而提高了其它水解酶和氧化酶活性,缓解了微生物碳限制,提升了微生物碳利用效率;(3)微生物群落的驱动机制呈现垂直分异,表层土壤主要受矿质氮驱动,亚表层受可溶性有机氮驱动,而深层则由碳有效性与 pH 的环境主导;(4)酶活性主要受碳、氮、磷含量及其化学计量比调控,主导因子从表层土壤的氮磷比转向亚表层和深层的碳磷比和土壤有机碳。综上,亚热带森林恢复通过提升土壤养分有效性及优化碳氮磷化学计量比,驱动了微生物代谢策略的转变,并对不同土层的生态功能实现差异化调控。未来亚热带森林恢复与管理应重视全剖面土壤碳稳定性与微生物介导的碳循环过程。

       

      Abstract: Background The study investigated the vertical distribution patterns and driving mechanisms of Soil microbial communities and their nutrient metabolic functions during forest restoration. Methods This study investigated a restoration sequence in a subtropical region, consisting of early-successional coniferous forest dominated by Pinus massoniana, conifer-broadleaf mixed forest, secondary evergreen broadleaf forest, and mature evergreen broadleaf forest. Soil samples were collected from the topsoil (0~10, 10~20 cm), subsurface soil (20~40, 40~60 cm), and deep soil (60~80, 80~100 cm) layers. By analyzing microbial phospholipid fatty acids (PLFAs), enzyme activities linked to carbon (C), nitrogen (N), and phosphorus (P) cycling, and microbial carbon use efficiency (CUE), to explored the microboal characteristics and their responses to environmental factors across soil layers. Results The results showed that: (1) forest restoration significantly increased total microbial PLFAs and the abundance of each microbial group across soil layers, though increases showed a delayed response in deep soil. Concurrently, restoration significantly lowered the ratio of fungal to bacterial biomass in both topsoil and subsurface soil. (2) Forest restoration significantly decreased β-glucosidase activity in all layers, while markedly increasing activities of other hydrolases and oxidases, alleviating microbial C limitation and improving microbial carbon use efficiency. (3) The drivers of microbial community assembly exhibited vertical stratification: the topsoil community was primarily governed by mineral N; the subsurface community by soluble organic N; and the deep soil community mainly by environmental filtering related to C availability and pH. (4) Enzyme activities were primarily regulated by soil C, N, and P contents and their stoichiometric ratios, with a shift in the primary regulation from the N:P ratio in topsoil C:P ratio and soil organic carbon in subsurface and deep soils. Conclusions The study demonstrates that regulating aboveground vegetation recovery processes and the improvements in soil nutrient availability and the optimization of C, N, and P stoichiometric ratios during subtropical forest restoration drive shifts in microbial metabolic strategies, thereby differentially regulating ecological functions across soil layers. Future subtropical forest restoration and management should emphasize whloe-profile soil carbon stabilization and microbe-mediated carbon cycling processes.

       

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