Du Hu, Liu Lu, Su Liang, Zeng Fuping, Wang Kelin, Peng Wanxia, Zhang Hao, Song Tongqing
Key Laboratory of Agro-Ecological Processes in Subtropical Region, Institute of Subtropical Agriculture, Chinese Academy of Sciences, Changsha, China.
Huanjiang Observation and Research Station for Karst Ecosystems, Institute of Subtropical Agriculture, Chinese Academy of Sciences, Huanjiang, China.
Front Plant Sci. 2019 Jan 11;9:2001. doi: 10.3389/fpls.2018.02001. eCollection 2018.
In karst ecosystems, plants absorbing smaller amounts of nutrients, owing to shallow soil, show limited growth. In addition, fine roots (diameter < 2 mm) contribute to the regulation of nutrient cycles in terrestrial ecosystems. However, the spatial and temporal variations of fine root biomass in different vegetation types of the karst region remains poorly understood. In this study, we investigated the seasonal and vertical variation in biomass, necromass, and total mass of fine roots using sequential soil coring under different stages of vegetation restoration (grassland, shrubland, secondary forest, and primary forest) in Southwest China. The results showed that the fine root biomass and necromass ranged from 136.99 to 216.18 g m and 47.34 to 86.94 g m, respectively. The total mass of fine roots and their production ranged from 187.00 to 303.11 g m and 55.74 to 100.84 g m year, respectively. They showed a single peak across the vegetation restoration gradient. The fine root biomass and total fine root mass also showed a single peak with seasonal change. In autumn, the fine root biomass was high, whereas the necromass was low. Most of the fine roots were concentrated in the surface soil layer (0-10 cm), which accounted more than 57% root biomass, and decreased with increasing soil depth. In addition, fine root production showed a similar vertical pattern of variation with biomass. Overall, our results suggested that fine roots show clear seasonal and vertical changes with vegetation succession. Moreover, there was a higher seasonal fluctuation and a greater vertical decreasing trend in late-successional stages than in the early-successional stages. The conversion of degraded land to forest could improve the productivity of underground ecosystems and vegetation restoration projects in the fragile karst region should, therefore, continue.
在喀斯特生态系统中,由于土壤浅薄,植物吸收的养分较少,生长受到限制。此外,细根(直径<2毫米)对陆地生态系统养分循环的调节起着重要作用。然而,喀斯特地区不同植被类型中细根生物量的时空变化仍知之甚少。在本研究中,我们在中国西南地区不同植被恢复阶段(草地、灌丛、次生林和原始林)下,采用连续土壤取芯法,研究了细根生物量、死根生物量和总生物量的季节和垂直变化。结果表明,细根生物量和死根生物量分别在136.99至216.18克/平方米和47.34至86.94克/平方米之间。细根总生物量及其生产量分别在187.00至303.11克/平方米和55.74至100.84克/平方米·年之间。它们在植被恢复梯度上呈现单峰变化。细根生物量和细根总生物量也随季节变化呈现单峰变化。秋季,细根生物量较高,而死根生物量较低。大多数细根集中在表层土壤层(0-10厘米),该层占根生物量的比例超过57%,且随土壤深度增加而减少。此外,细根生产量与生物量呈现相似的垂直变化模式。总体而言,我们的研究结果表明,细根随植被演替呈现明显的季节和垂直变化。此外,与早期演替阶段相比,后期演替阶段的季节波动更大,垂直下降趋势更明显。将退化土地转化为森林可以提高地下生态系统的生产力,因此,脆弱喀斯特地区的植被恢复项目应继续推进。