Institute for Forest Resources & Environment of Guizhou, College of Forestry, Guizhou University, Guizhou University Institute of Soil Erosion and Ecological Restoration, Guiyang 550025, China.
Institute for Forest Resources & Environment of Guizhou, College of Forestry, Guizhou University, Guizhou University Institute of Soil Erosion and Ecological Restoration, Guiyang 550025, China; The Key Laboratory of Plant Resource Conservation and Germplasm Innovation in Mountainous Region, Ministry of Education, Collaborative Innovation Center for Mountain Ecology & Agro-Bioengineering (CICMEAB), Guizhou University, Guiyang, Guizhou 550025, China.
Sci Total Environ. 2020 Apr 10;712:136543. doi: 10.1016/j.scitotenv.2020.136543. Epub 2020 Jan 8.
In karst regions, shallow karst fissure (SKF) soil has proven to be an important plant habitat and soil resource. However, how plants affect the microbial abundance and community composition of SKF soil remains poorly studied. We explored the soil microbial community structure differences in fractured soil-plant systems by determining phospholipid fatty acid (PLFA) profiles under three vegetation types (herbs, shrubs and trees) in SKF and used a bare SKF without vegetation as the control in a karst rocky desertification area. The total microbial biomass and microbial community composition differed between surface soil and SKF soil. The total microbial biomass in surface soil was higher than that in SKF soil. In addition, in contrast to surface soil, the microbial communities in SKF soil were more vulnerable to the effects of environmental variables. Furthermore, plants had a significant positive effect on the accumulation of microbial biomass in surface and SKF soil: shrubs had the strongest effect, followed by trees. Vegetation types significantly affected the ratios of saturated PLFAs to monounsaturated PLFAs (SAT/MONO ratio) and cyclopropyl PLFAs to precursors (cy/pre ratio). In contrast to the SKF without vegetation, the SAT/MONO ratio and cy/pre ratio under grasslands, shrublands and trees were low. Herbs and shrubs had the greatest capacity to enhance the ability of soil to respond to environmental stress compared to trees. Our results suggest that, as an important plant habitat in karst regions, the condition of SKF soil should be urgently improved. The stereoscopic collocation of shrub-grass vegetation may be the preferred measure for vegetation restoration. Deep-rooted shrubs and grasses are best at improving soil and plant growth. Our study can be useful for developing strategies for vegetation rehabilitation in karst regions.
在喀斯特地区,浅层喀斯特裂隙(SKF)土壤已被证明是一种重要的植物栖息地和土壤资源。然而,植物如何影响 SKF 土壤的微生物丰度和群落组成仍研究甚少。我们通过在喀斯特石漠化地区确定三种植被类型(草本、灌木和乔木)下 SKF 中磷脂脂肪酸(PLFA)图谱,研究了裂隙土壤-植物系统中土壤微生物群落结构差异,并用无植被的裸露 SKF 作为对照。表层土壤和 SKF 土壤的微生物生物量和微生物群落组成存在差异。表层土壤的总微生物生物量高于 SKF 土壤。此外,与表层土壤不同,SKF 土壤中的微生物群落更容易受到环境变量的影响。此外,植物对表层和 SKF 土壤中微生物生物量的积累有显著的正向影响:灌木的影响最强,其次是乔木。植被类型显著影响饱和磷脂脂肪酸与单不饱和磷脂脂肪酸的比值(SAT/MONO 比值)和环丙基磷脂脂肪酸与前体的比值(cy/pre 比值)。与无植被的 SKF 相比,草地、灌丛和林地的 SAT/MONO 比值和 cy/pre 比值较低。与树木相比,草本植物和灌木具有最大的增强土壤对环境胁迫响应能力。我们的研究结果表明,作为喀斯特地区的重要植物栖息地,SKF 土壤的状况应亟待改善。灌草植被的立体配置可能是植被恢复的首选措施。深根灌木和草本植物最有利于改善土壤和植物生长。我们的研究可为喀斯特地区植被恢复策略的制定提供参考。